FN Thomson Reuters Web of Science™
VR 1.0
PT J
AU Olsen, RE
Cox, RR
Afton, AD
Ankney, CD
AF Olsen, Richard E.
Cox, Robert R., Jr.
Afton, Alan D.
Ankney, C. Davison
TI Diet and Gut Morphology of Male Mallards During Winter in North Dakota
SO WATERBIRDS
LA English
DT Article
DE Anas platyrhynchos; diet; gut morphology; Osmerus mordax; Rainbow Smelt
ID LESSER SCAUP; VISCERAL MORPHOLOGY; ANAS-PLATYRHYNCHOS; NUTRIENT
RESERVES; DIGESTIVE ORGANS; FOOD-HABITS; WOOD DUCKS; SIZE; MISSISSIPPI;
MIDWINTER
AB A free-ranging Mallard (Anas platyrhynchos) population was investigated during winter (December-January 1996-1999) below the Garrison Dam, North Dakota, USA, to relate diet to gut morphology, variation in males. Four explanatory variables (fish consumption, male age, winter, and body size) were evaluated as to whether they influenced five response variables associated with gut characteristics of Mallards. Response variables were lower gastro-intestinal tract mass (LGIT), dry liver mass, dry gizzard mass, small intestine length, and ceca length. Diets of Mallards were comprised primarily of Rainbow Smelt (Osmerus mordax) and concomitantly variation in gizzard mass was small. LGIT mass of juveniles was larger than that of adults, greater for those that consumed fish, and greater during the coldest and snowiest winter. Liver mass and small intestine length of Mallards that consumed fish were greater than those that did not. Mallards may maintain lengthy intestines to increase digestive efficiency. Gut size variation was not entirely attributable to dietary composition but also influenced by body size and environmental conditions such that over-winter survival is maximized. Received 1 December 2009, accepted 9 December 2010.
C1 [Olsen, Richard E.] Minnesota Dept Nat Resources, Glenwood, MN 56334 USA.
[Cox, Robert R., Jr.] RC Store, Ipswich, SD 57451 USA.
[Afton, Alan D.] Louisiana State Univ, US Geol Survey, Louisiana Cooperat Fish & Wildlife Res Unit, Baton Rouge, LA 70803 USA.
[Ankney, C. Davison] Univ Western Ontario, Dept Biol, London, ON N6A 5B7, Canada.
RP Olsen, RE (reprint author), Minnesota Dept Nat Resources, 23070 N Lakeshore Dr, Glenwood, MN 56334 USA.
EM richard.olsen@state.mn.us
NR 46
TC 1
Z9 2
U1 0
U2 13
PU WATERBIRD SOC
PI WASHINGTON
PA NATL MUSEUM NATURAL HISTORY SMITHSONIAN INST, WASHINGTON, DC 20560 USA
SN 1524-4695
EI 1938-5390
J9 WATERBIRDS
JI Waterbirds
PD MAR
PY 2011
VL 34
IS 1
BP 59
EP 69
PG 11
WC Ornithology
SC Zoology
GA 736WD
UT WOS:000288524800007
ER
PT J
AU Franklin, J
Regan, HM
Hierl, LA
Deutschman, DH
Johnson, BS
Winchell, CS
AF Franklin, Janet
Regan, Helen M.
Hierl, Lauren A.
Deutschman, Douglas H.
Johnson, Brenda S.
Winchell, Clark S.
TI PLANNING, IMPLEMENTING, AND MONITORING MULTIPLE-SPECIES HABITAT
CONSERVATION PLANS
SO AMERICAN JOURNAL OF BOTANY
LA English
DT Article
DE biodiversity; conservation reserves; ecological monitoring; habitat
conservation plan; landscape; multiple species; prioritization
ID RESERVE SELECTION ALGORITHMS; BIODIVERSITY HOTSPOTS; BIOLOGICAL
DIVERSITY; LAND MANAGEMENT; PROTECTED AREAS; WILDLIFE; DESIGNS; TIME;
ASSESSMENTS; PRIORITIES
AB Premise of the study : Despite numerous recommendations for various aspects of the design and monitoring of habitat conservation plans, there remains a need to synthesize existing guidelines into a comprehensive scheme and apply it to real-world conservation programs.
Methods : We review tools for systematic conservation planning and elements for designing and implementing ecological monitoring in an adaptive management context. We apply principles of monitoring design to the San Diego Multiple Species Conservation Program (MSCP) in California, USA-one of the first multispecies habitat conservation plans, located in a landscape where high biodiversity and urban development converge.
Key results : Tools for spatial conservation planning are aimed to conserve biodiversity, often in the context of a limited budget. In practice, these methods may not accommodate legislative mandates, budgetary uncertainties, and the range of implementation mechanisms available across consortia of stakeholders. Once a reserve is implemented, the question becomes whether it is effective at conserving biodiversity, and if not, what actions are required to make it effective. In monitoring plan development, status and threats should be used to prioritize species and communities that require management action to ensure their persistence. Conceptual models documenting the state of knowledge of the system should highlight the main drivers affecting status and trends of species or communities. Monitoring strategies require scientifically justified decisions based on sampling, response, and data design.
Conclusions : Because the framework illustrated here tackles multiple species, communities, and threats at the urban-wildland interface, it will have utility for ecosystem managers struggling to design monitoring programs.
C1 [Franklin, Janet] Arizona State Univ, Sch Geog Sci & Urban Planning, Tempe, AZ 85287 USA.
[Regan, Helen M.] Univ Calif Riverside, Dept Biol, Riverside, CA 92521 USA.
[Hierl, Lauren A.; Deutschman, Douglas H.] San Diego State Univ, Dept Biol, San Diego, CA 92182 USA.
[Johnson, Brenda S.] Calif Dept Fish & Game, Habitat Conservat Branch, Sacramento, CA 95814 USA.
[Winchell, Clark S.] US Fish & Wildlife Serv, Carlsbad Fish & Wildlife Off, Carlsbad, CA 92011 USA.
RP Franklin, J (reprint author), Arizona State Univ, Sch Geog Sci & Urban Planning, POB 875302, Tempe, AZ 85287 USA.
EM Janet.Franklin@asu.edu
FU California Department of Fish and Game, NCCP [P0450009]; MSCP
FX The authors thank A. Atkinson, K. Greer, S. Wynn, T. Oberbauer, and R.
Fisher. The manuscript was greatly improved by comments from A. Syphard,
H. Possingham, and an anonymous reviewer. The opinions expressed and any
errors that remain in this paper are the authors'. This work was
supported by the California Department of Fish and Game, NCCP Local
Assistance Grant #P0450009, and in cooperation with the MSCP Monitoring
Partners, a multi-agency and multi-jurisdictional task force.
NR 88
TC 10
Z9 10
U1 3
U2 59
PU BOTANICAL SOC AMER INC
PI ST LOUIS
PA PO BOX 299, ST LOUIS, MO 63166-0299 USA
SN 0002-9122
J9 AM J BOT
JI Am. J. Bot.
PD MAR
PY 2011
VL 98
IS 3
BP 559
EP 571
DI 10.3732/ajb.1000292
PG 13
WC Plant Sciences
SC Plant Sciences
GA 734FU
UT WOS:000288320600027
PM 21613147
ER
PT J
AU Cross, A
Perakis, SS
AF Cross, Alison
Perakis, Steven S.
TI Complementary Models of Tree Species-Soil Relationships in Old-Growth
Temperate Forests
SO ECOSYSTEMS
LA English
DT Article
DE feedback; forest floor; mineral soil; nutrient availability; plant-soil
interactions; nitrogen; phosphorus; carbon; base cations; old-growth
ID NITROGEN MINERALIZATION; CANOPY TREE; ECOSYSTEM PROCESSES; GRADIENT;
MOUNTAINS; NUTRIENTS; HARDWOOD; OREGON; STANDS; CARBON
AB Ecosystem-level studies identify plant-soil feedbacks as important controls on soil nutrient availability, particularly for nitrogen and phosphorus. Although site- and species-specific studies of tree species-soil relationships are relatively common, comparatively fewer studies consider multiple co-existing species in old-growth forests across a range of sites that vary in underlying soil fertility. We characterized patterns in forest floor and mineral soil nutrients associated with four common tree species across eight undisturbed old-growth forests in Oregon, USA, and used two complementary conceptual models to assess tree species-soil relationships. Plant-soil feedbacks that could reinforce site-level differences in nutrient availability were assessed using the context-dependent relationships model, whereby relative species-based differences in each soil nutrient diverged or converged as nutrient status changed across sites. Tree species-soil relationships that did not reflect strong feedbacks were evaluated using a site-independent relationships model, whereby forest floor and surface mineral soil nutrient pools differed consistently by tree species across sites, without variation in deeper mineral soils. We found that the organically cycled elements carbon, nitrogen, and phosphorus exhibited context-dependent differences among species in both forest floor and mineral soil, and most often followed a divergence model, whereby species differences were greatest at high-nutrient sites. These patterns are consistent with theory emphasizing biotic control of these elements through plant-soil feedback mechanisms. Site-independent species differences were strongest for pools of the weatherable cations calcium, magnesium, potassium, as well as phosphorus, in mineral soils. Site-independent species differences in forest floor nutrients were attributable to one species that displayed significantly greater forest floor mass accumulation. Our findings confirm that site-independent and context-dependent tree species-soil relationships occur simultaneously in old-growth temperate forests, with context-dependent relationships strongest for organically cycled elements, and site-independent relationships strongest for weatherable elements with inorganic cycling phases. These models provide complementary explanations for patterns of nutrient accumulation and cycling in mixed-species old-growth temperate forests.
C1 [Perakis, Steven S.] US Geol Survey, Forest & Rangeland Ecosyst Sci Ctr, Corvallis, OR 97331 USA.
[Cross, Alison] Oregon State Univ, Dept Forest Ecosyst & Soc, Corvallis, OR 97331 USA.
RP Perakis, SS (reprint author), US Geol Survey, Forest & Rangeland Ecosyst Sci Ctr, 3200 SW Jefferson Way, Corvallis, OR 97331 USA.
EM steven.perakis@oregonstate.edu
FU US Geological Survey Forest and Rangeland Ecosystem Science Center;
Oregon Department of Forestry
FX We thank Chris Catricala and crew for assistance in the field and
laboratory, Lisa Ganio for statistical consulting, and David Hibbs,
Kermit Cromack, David Myrold, and two anonymous reviewers for comments
on the manuscript. This research was produced through the Cooperative
Forest Ecosystem Research Program, with funding provided by the US
Geological Survey Forest and Rangeland Ecosystem Science Center and the
Oregon Department of Forestry. Any use of trade names is for descriptive
purposes only and does not imply endorsement by the US Government.
NR 39
TC 6
Z9 6
U1 2
U2 37
PU SPRINGER
PI NEW YORK
PA 233 SPRING ST, NEW YORK, NY 10013 USA
SN 1432-9840
J9 ECOSYSTEMS
JI Ecosystems
PD MAR
PY 2011
VL 14
IS 2
BP 248
EP 260
DI 10.1007/s10021-010-9407-5
PG 13
WC Ecology
SC Environmental Sciences & Ecology
GA 732GF
UT WOS:000288172300006
ER
PT J
AU Cahoon, DR
Perez, BC
Segura, BD
Lynch, JC
AF Cahoon, Donald R.
Perez, Brian C.
Segura, Bradley D.
Lynch, James C.
TI Elevation trends and shrink-swell response of wetland soils to flooding
and drying
SO ESTUARINE COASTAL AND SHELF SCIENCE
LA English
DT Article
DE droughts; salt marsh elevation; continuous elevation sensor; USA,
Louisiana, Old Oyster Bayou; USA, Texas, McFaddin National Wildlife;
Refuge
ID HIGH-PRECISION MEASUREMENTS; SEA-LEVEL RISE; SEDIMENTATION-EROSION
TABLE; RIVER DELTAIC PLAIN; SALT-MARSH; SURFACE ELEVATION; ACCRETION;
BAY; SUBSIDENCE; LOUISIANA
AB Given the potential for a projected acceleration in sea-level rise to impact wetland sustainability over the next century, a better understanding is needed of climate-related drivers that influence the processes controlling wetland elevation. Changes in local hydrology and groundwater conditions can cause short-term perturbations to marsh elevation trends through shrink-swell of marsh soils. To better understand the magnitude of these perturbations and their impacts on marsh elevation trends, we measured vertical accretion and elevation dynamics in microtidal marshes in Texas and Louisiana during and after the extreme drought conditions that existed there from 1998 to 2000. In a Louisiana marsh, elevation was controlled by subsurface hydrologic fluxes occurring below the root zone but above the 4 m depth (i.e., the base of the surface elevation table benchmark) that were related to regional drought and local meteorological conditions, with marsh elevation tracking water level variations closely. In Texas, a rapid decline in marsh elevation was related to severe drought conditions, which lowered local groundwater levels. Unfragmented marshes experienced smaller water level drawdowns and more rapid marsh elevation recovery than fragmented marshes. It appears that extended drawdowns lead to increased substrate consolidation making it less resilient to respond to future favorable conditions. Overall, changes in water storage lead to rapid and large short-term impacts on marsh elevation that are as much as five times greater than the long-term elevation trend, indicating the importance of long-term, high-resolution elevation data sets to understand the prolonged effects of water deficits on marsh elevation change. (c) 2010 Elsevier Ltd. All rights reserved.
C1 [Cahoon, Donald R.; Lynch, James C.] US Geol Survey, Patuxent Wildlife Res Ctr, Beltsville, MD 20705 USA.
[Perez, Brian C.] US Geol Survey, Natl Wetlands Res Ctr, Lafayette, LA 70506 USA.
[Segura, Bradley D.] Johnson Controls World Serv Inc, Natl Wetlands Res Ctr, Lafayette, LA 70506 USA.
RP Perez, BC (reprint author), CH2M HILL,700 Main St,Suite 400, Baton Rouge, LA 70802 USA.
EM dcahoon@usgs.gov; bperez@ch2m.com; bsegura@jchance.com; jclynch@usgs.gov
NR 41
TC 17
Z9 19
U1 4
U2 36
PU ACADEMIC PRESS LTD- ELSEVIER SCIENCE LTD
PI LONDON
PA 24-28 OVAL RD, LONDON NW1 7DX, ENGLAND
SN 0272-7714
J9 ESTUAR COAST SHELF S
JI Estuar. Coast. Shelf Sci.
PD MAR 1
PY 2011
VL 91
IS 4
BP 463
EP 474
DI 10.1016/j.ecss.2010.03.022
PG 12
WC Marine & Freshwater Biology; Oceanography
SC Marine & Freshwater Biology; Oceanography
GA 734CH
UT WOS:000288310300001
ER
PT J
AU McKee, KL
AF McKee, Karen L.
TI Biophysical controls on accretion and elevation change in Caribbean
mangrove ecosystems
SO ESTUARINE COASTAL AND SHELF SCIENCE
LA English
DT Article
DE Belize; climate change; Florida; land loss; sedimentation; subsidence
ID SEA-LEVEL RISE; HIGH-PRECISION MEASUREMENTS; WETLAND SEDIMENT ELEVATION;
VERTICAL ACCRETION; SOIL FORMATION; SALT-MARSHES; FORESTS; RATES;
ACCUMULATION; VEGETATION
AB Habitat stability of coastal ecosystems, such as marshes and mangroves, depends on maintenance of soil elevations relative to sea level. Many such systems are characterized by limited mineral sedimentation and/or rapid subsidence and are consequently dependent upon accumulation of organic matter to maintain elevations. However, little field information exists regarding the contribution of specific biological processes to vertical accretion and elevation change. This study used biogenic mangrove systems in carbonate settings in Belize (BZ) and southwest Florida (FL) to examine biophysical controls on elevation change. Rates of elevation change, vertical accretion, benthic mat formation, and belowground root accumulation were measured in fringe, basin, scrub, and dwarf forest types plus a restored forest. Elevation change rates (mm yr(-1)) measured with Surface Elevation Tables varied widely: BZ-Dwarf (-3.7), BZ-Scrub (-1.1), FL-Fringe (0.6), FL-Basin (2.1), BZ-Fringe (4.1), and FL-Restored (9.9). Root mass accumulation varied across sites (82-739 g m(-2) yr(-1) and was positively correlated with elevation change. Root volumetric contribution to vertical change (mm yr(-1)) was lowest in BZ-Dwarf (1.2) and FL-Fringe (2.4), intermediate in FL-Basin (4.1) and BZ-Scrub (4.3), and highest in BZ-Fringe (8.8) and FL-Restored (11.8) sites. Surface growth of turf-forming algae, microbial mats, or accumulation of leaf litter and detritus also made significant contributions to vertical accretion. Turf algal mats in fringe and scrub forests accreted faster (2.7 mm yr(-1)) than leaf litter mats in basin forests (1.9 mm yr(-1)), but similarly to microbial mats in dwarf forests (2.1 mm yr(-1)). Surface accretion of mineral material accounted for only 0.2-3.3% of total vertical change. Those sites with high root contributions and/or rapid growth of living mats exhibited an elevation surplus (+2 to +8 mm yr(-1)), whereas those with low root inputs and low (or non-living) mat accumulation showed an elevation deficit (-1 to -5.7 mm yr(-1)). This study indicates that biotic processes of root production and benthic mat formation are important controls on accretion and elevation change in mangrove ecosystems common to the Caribbean Region. Quantification of specific biological controls on elevation provides better insight into how sustainability of such systems might be influenced by global (e.g., climate, atmospheric CO2) and local (e.g., nutrients, disturbance) factors affecting organic matter accumulation, in addition to relative sea-level rise. Published by Elsevier Ltd.
C1 US Geol Survey, Natl Wetlands Res Ctr, Lafayette, LA 70506 USA.
RP McKee, KL (reprint author), US Geol Survey, Natl Wetlands Res Ctr, 700 Cajundome Blvd, Lafayette, LA 70506 USA.
EM mckeek@usgs.gov
RI McKee, Karen/D-1365-2014
OI McKee, Karen/0000-0001-7042-670X
FU National Science Foundation [DEB-9981483]; Smithsonian Institution
FX This work was partially supported by the National Science Foundation's
Biocomplexity in the Environment Program (DEB-9981483) and by the
Smithsonian Institution's Caribbean Coral Reef Ecosystems Program. I
thank the Fisheries Department and Government of Belize for permission
to conduct research at Twin Cays and Mike Shirley and the Rookery Bay
National Estuarine Research Reserve for access to study sites and
logistical support in Florida. A. Anteau, D. Cahoon, P. Faulkner, M.
Finn, J. Lynch, T. McGinnis, J. Rooth, E. Travis, and W. Vervaeke
provided field and laboratory assistance. The manuscript was improved by
the comments of D. Cahoon, I. Mendelssohn, and two anonymous reviewers.
Any use of trade, product or firm names is for descriptive purposes only
and does not imply endorsement by the U.S. Government.
NR 42
TC 53
Z9 53
U1 9
U2 88
PU ACADEMIC PRESS LTD- ELSEVIER SCIENCE LTD
PI LONDON
PA 24-28 OVAL RD, LONDON NW1 7DX, ENGLAND
SN 0272-7714
J9 ESTUAR COAST SHELF S
JI Estuar. Coast. Shelf Sci.
PD MAR 1
PY 2011
VL 91
IS 4
BP 475
EP 483
DI 10.1016/j.ecss.2010.05.001
PG 9
WC Marine & Freshwater Biology; Oceanography
SC Marine & Freshwater Biology; Oceanography
GA 734CH
UT WOS:000288310300002
ER
PT J
AU Hower, JC
Ruppert, LF
AF Hower, James C.
Ruppert, Leslie F.
TI Splint coals of the Central Appalachians: Petrographic and geochemical
facies of the Peach Orchard No. 3 split coal bed, southern Magoffin
County, Kentucky
SO INTERNATIONAL JOURNAL OF COAL GEOLOGY
LA English
DT Article
DE Coal; Kentucky; Petrology; Geochemistry; Facies; Coal to liquids; Durain
ID EASTERN KENTUCKY; POWER-PLANT; PETROLOGY; FIRE; PALEOECOLOGY;
PALYNOLOGY; ORIGIN; ARCHITECTURE; KALIMANTAN; INDONESIA
AB The Bolsovian (Middle Pennsylvanian) Peach Orchard coal bed is one of the splint coals of the Central Appalachians. Splint coal is a name for the dull, inertinite-rich lithologies typical of coals of the region. The No. 3 Split was sampled at five locations in Magoffin County, Kentucky and analyzed for petrography and major and minor elements. The No. 3 Split coals contain semifusinite-rich lithologies, up to 48% (mineral-free basis) in one case. The nature of the semifusinite varies with position in the coal bed, containing more mineral matter of detrital origin in the uppermost durain. The maceral assemblage of these terminal durains is dominated by detrital fusinite and semifusinite, suggesting reworking of the maceral assemblage coincident with the deposition of the detrital minerals. However, a durain in the middle of the coal bed, while lithologically similar to the uppermost durains, has a degraded, macrinite-rich, texture. The inertinite macerals in the middle durain have less distinct edges than semifusinites in the uppermost terminal durains, suggesting degradation as a possible path to inertinite formation. The uppermost durain has higher ash and semifusinite contents at the eastern sites than at the western sites. The difference in the microscopic petrology indicates that megascopic petrology alone can be a deceptive indicator of depositional environments and that close attention must be paid to the individual macerals and their implications for the depositional setting, especially within the inertinite group. (C) 2011 Elsevier B.V. All rights reserved.
C1 [Hower, James C.] Univ Kentucky, Ctr Appl Energy Res, Lexington, KY 40511 USA.
[Ruppert, Leslie F.] US Geol Survey, Natl Ctr, Reston, VA 20192 USA.
RP Hower, JC (reprint author), Univ Kentucky, Ctr Appl Energy Res, 2540 Res Pk Dr, Lexington, KY 40511 USA.
EM hower@caer.uky.edu; lruppert@usgs.gov
OI Ruppert, Leslie/0000-0002-7453-1061
NR 45
TC 12
Z9 12
U1 0
U2 0
PU ELSEVIER SCIENCE BV
PI AMSTERDAM
PA PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS
SN 0166-5162
J9 INT J COAL GEOL
JI Int. J. Coal Geol.
PD MAR 1
PY 2011
VL 85
IS 3-4
BP 268
EP 275
DI 10.1016/j.coal.2010.12.012
PG 8
WC Energy & Fuels; Geosciences, Multidisciplinary
SC Energy & Fuels; Geology
GA 736DU
UT WOS:000288471600003
ER
PT J
AU Tucker, RD
Roig, JY
Macey, PH
Delor, C
Amelin, Y
Armstrong, RA
Rabarimanana, MH
Ralison, AV
AF Tucker, R. D.
Roig, J. Y.
Macey, P. H.
Delor, C.
Amelin, Y.
Armstrong, R. A.
Rabarimanana, M. H.
Ralison, A. V.
TI A new geological framework for south-central Madagascar, and its
relevance to the "out-of-Africa" hypothesis
SO PRECAMBRIAN RESEARCH
LA English
DT Article
DE U-Pb geochronology; Paleoproterozoic; Tectonics; East African Orogen;
Greater Dharwar Craton; Detrital zircons
ID U-PB GEOCHRONOLOGY; CAUVERY SHEAR ZONE; WEST-CENTRAL MADAGASCAR;
HIGH-GRADE ROCKS; SRI-LANKA; MOZAMBIQUE OCEAN; ZIRCON GEOCHRONOLOGY;
TECTONIC EVOLUTION; ISOTOPIC SYSTEMATICS; GONDWANA CONNECTIONS
AB The Precambrian shield of south-central Madagascar, excluding the Vohibory region, consists of three geologic domains, from north to south: Antananarivo. Ikalamavony-Itremo, and Anosyen-Androyen. The northern Antananarivo domain represents the Neoarchean sector of the Greater Dharwar Craton amalgamated at 2.52-2.48 Ga. The Greater Dharwar Craton is overlain by several groups of Meso- to Neoproterozoic supracrustal rocks (Ambatolampy, Manampotsy, Ampasary, Sahantaha, and Maha Groups) each with a common and diagnostic signature of Paleoproterozoic detrital zircons (2.2-1.8 Ga). The central domain (Ikalamavony-Itremo) consists of two distinct parts. The Itremo Sub-domain, in the east, is a structurally intercalated sequence of Neoarchean gneiss and shallow marine metasedimentary rocks of Paleo-Mesoproterozoic age (Itremo Group), the latter with Paleoproterozoic detrital zircons ranging in age between 2.2 and 1.8 Ga. The Ikalamavony Sub-domain, to the west, contains abundant volcano-clastic metasediments and lesser quartzite (Ikalamavony Group), formed between 1.03 Ga and 0.98 Ga, and intruded by igneous rocks (Dabolava Suite) of Stenian-Tonian age. Structurally intercalated with these are sheets of Neoarchean gneiss (similar to 2.5 Ga) and Neoproterozoic metaclastic rocks (Molo Group). Like the Itremo Group, quartzite of the Ikalamavony Group has detrital zircons of Paleoproterozoic age (2.1-1.8 Ga). The southern domain of Anosyen-Androyen consists of a newly recognized suite of Paleoproterozoic igneous rocks (2.0-1.8 Ga), and stratified supracrustal rocks also having Paleoproterozoic detrital zircons (2.3-1.8 Ga). The contact between the Anosyen-Androyen and Ikalamavony-Itremo domains, formerly known as the Ranotsara-Bongolava shear zone, is a tightly folded and highly flattened boundary that was ductilely deformed in Ediacaran time. It is roughly equivalent to the Palghat-Cauvery shear zone in south India, and it defines approximately the boundary between the Archean Greater Dharwar Craton (to the north) and the Paleoproterozoic terrane of Anosyen-Androyen (to the south). Published by Elsevier B.V.
C1 [Tucker, R. D.] US Geol Survey, Natl Ctr, Reston, VA 20192 USA.
[Roig, J. Y.; Delor, C.] Bur Rech Geol & Minieres, F-45060 Orleans 2, France.
[Macey, P. H.] Council Geosci Western Cape, ZA-7535 Bellville, South Africa.
[Amelin, Y.; Armstrong, R. A.] Australian Natl Univ, Res Sch Earth Sci, Canberra, ACT 0200, Australia.
[Rabarimanana, M. H.; Ralison, A. V.] Project Gouvernance Ressources Minerales, Antananarivo 101, Madagascar.
RP Tucker, RD (reprint author), US Geol Survey, Natl Ctr, MS 926A,12201 Sunrise Valley Dr, Reston, VA 20192 USA.
EM rtucker@usgs.gov
FU World Bank; PRGM (Madagascar)
FX Our collaborative research was funded by the World Bank, with a contract
from the PRGM (Madagascar) to the BRGM-USGS consortium, under the title
Syntheses Geologique de Madagascar a l'echelle du millionnieme. We
acknowledge, in particular, Drs. Enrique Ortega, Bernard Moine and
Dominique Rakotomanana, who financed our field work and U-Pb
geochronology through the PRGM, provided intellectual stimulation for
effort, and who granted permission to cite the Report of Consultants in
this paper. Bernard Moine, J.-L. Paquette, Greg Walsh, and Bill Burton
provided careful and constructive reviews of the manuscript.
NR 82
TC 54
Z9 54
U1 5
U2 13
PU ELSEVIER SCIENCE BV
PI AMSTERDAM
PA PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS
SN 0301-9268
J9 PRECAMBRIAN RES
JI Precambrian Res.
PD MAR
PY 2011
VL 185
IS 3-4
BP 109
EP 130
DI 10.1016/j.precamres.2010.12.008
PG 22
WC Geosciences, Multidisciplinary
SC Geology
GA 734QK
UT WOS:000288350700003
ER
PT J
AU Jones, DS
Barnes, CG
Premo, WR
Snoke, AW
AF Jones, Daniel S.
Barnes, Calvin G.
Premo, Wayne R.
Snoke, Arthur W.
TI The geochemistry and petrogenesis of the Paleoproterozoic Green Mountain
arc: A composite(?), bimodal, oceanic, fringing arc
SO PRECAMBRIAN RESEARCH
LA English
DT Article
DE Green Mountain arc; Yavapai; Big Creek Gneiss; Proterozoic; Crustal
growth; Geochemistry
ID SOUTHWESTERN NORTH-AMERICA; WEST-CENTRAL COLORADO; HIGH-ALUMINA BASALTS;
U-PB GEOCHRONOLOGY; BONIN-MARIANA ARC; ISLAND-ARC; VOLCANIC-ROCKS;
KERMADEC ARC; CHEMICAL CHARACTERISTICS; ARCHEAN TRONDHJEMITES
AB The inferred subduction affinity of the similar to 1780-Ma Green Mountain arc, a dominantly bimodal igneous terrane (together with immature marine and volcaniclastic sedimentary rocks) accreted to the southern margin of the Wyoming province, is integral to arc-accretion models of the Paleoproterozoic growth of southern Laurentia. Conversely, the dominantly bimodal nature of many putative arc-related igneous suites throughout southern Laurentia, including the Green Mountain arc, has also been used to support models of growth by extension of pre-existing crust. We report new geochemical and isotopic data from similar to 1780-Ma gabbroic and granodioritic to tonalitic rocks of the Big Creek Gneiss, interpreted as consanguineous with previously studied metavolcanic rocks of the Green Mountain Formation.
The similar to 1780-Ma Big Creek Gneiss mafic rocks show clear geochemical signatures of a subduction origin and provide no supporting evidence for extensional tectonism. The similar to 1780-Ma Big Creek Gneiss felsic rocks are attributed to partial melting of mafic and/or mixed lower-crustal material. The bimodal nature of the suite results from the combination of arc basalts and felsic crustal melts. The lack of andesite is consistent with the observed tholeiitic differentiation trend of the mafic magmas. The lower epsilon(Nd)(1780 Ma) values for the felsic rocks vs. the mafic rocks suggest that the unexposed lower crust of the arc may be older than the arc and that Trans-Hudson- or Penokean-aged rocks possibly form the substratum of the arc. Our results reinforce previous interpretations that arc-related magmatism played a key role in the Paleoproterozoic crustal growth of southern Laurentia, but also support the possibility of unexposed older crust as basement to the arcs. (C) 2011 Elsevier B.V. All rights reserved.
C1 [Jones, Daniel S.] Western Carolina Univ, Dept Geosci, Cullowhee, NC 28723 USA.
[Barnes, Calvin G.] Texas Tech Univ, Dept Geosci, Lubbock, TX 79409 USA.
[Premo, Wayne R.] US Geol Survey, Denver Fed Ctr, Denver, CO 80225 USA.
[Snoke, Arthur W.] Univ Wyoming, Dept Geol & Geophys, Laramie, WY 82071 USA.
RP Jones, DS (reprint author), Western Carolina Univ, Dept Geosci, Cullowhee, NC 28723 USA.
EM dsjones@wcu.edu
FU Geological Society of America [8559-07]; Wyoming NASA Space Grant
Consortium [NNG0G165H]; Wyoming Geological Association; Colorado
Scientific Society; Tobacco Root Geological Society; Department of
Geology and Geophysics at the University of Wyoming
FX This work is part of the PhD dissertation of Daniel S. Jones at the
University of Wyoming. Financial support was provided in part by the
Geological Society of America (#8559-07), Wyoming NASA Space Grant
Consortium (#NNG0G165H), Wyoming Geological Association, Colorado
Scientific Society, Tobacco Root Geological Society, and Department of
Geology and Geophysics at the University of Wyoming. We thank Phil
Nickerson and Mark Moyer for their assistance in the field, Melanie
Barnes for training and geochemical analyses, Jason Mailloux for
isotopic analyses, and Joe Wooden for training and assistance at the
SUMAC SHRIMP facility. Part of this work was completed in collaboration
with researchers at the U.S. Geological Survey in Denver. Colorado, in
conjunction with other research conducted for their Central Colorado
Assessment Project within the Survey's Central Region Earth Surfaces
Processes team. Reviews of the manuscript by Pat Bickford and Jim Cole
are gratefully acknowledged.
NR 111
TC 12
Z9 12
U1 0
U2 4
PU ELSEVIER SCIENCE BV
PI AMSTERDAM
PA PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS
SN 0301-9268
J9 PRECAMBRIAN RES
JI Precambrian Res.
PD MAR
PY 2011
VL 185
IS 3-4
BP 231
EP 249
DI 10.1016/j.precamres.2011.01.011
PG 19
WC Geosciences, Multidisciplinary
SC Geology
GA 734QK
UT WOS:000288350700010
ER
PT J
AU Brand, LA
Noon, BR
AF Brand, L. Arriana
Noon, Barry R.
TI SEASONAL FECUNDITY AND SOURCE-SINK STATUS OF SHRUB-NESTING BIRDS IN A
SOUTHWESTERN RIPARIAN CORRIDOR
SO WILSON JOURNAL OF ORNITHOLOGY
LA English
DT Article
ID REPRODUCTIVE SUCCESS; ABERTS TOWHEE; UNITED-STATES; BELLS VIREOS;
HABITAT; VEGETATION; SURVIVAL; TAMARIX; POPULATIONS; PARASITISM
AB Saltcedar (Tamarix spp.) has increasingly dominated riparian floodplains relative to native forests in the southwestern U.S., but little is known about its impacts on avian productivity or population status. We monitored 86 Arizona Bell's Vireo (Vireo bellii arizonae), 147 Abert's Towhee (Melozone aberti), and 154 Yellow-breasted Chat (Icteria virens) nests to assess reproductive parameters in cottonwood-willow (Populus-Salix), saltcedar, and mesquite (Prosopis spp.) stands along the San Pedro River, Arizona during 1999-2001. We also assessed source-sink status for each species in each vegetation type using field data combined with data from the literature. There were no significant differences in reproductive parameters between vegetation types for Abert's Towhee or Yellow-breasted Chat, although seasonal fecundity was quite low across vegetation types for the latter (0.75 +/- 0.14; mean SE). Bell's Vireo had extremely low seasonal fecundity in saltcedar (0.10 +/- 0.09) and significantly fewer fledglings per nest in saltcedar (0.09 +/- 0.09) compared with cottonwood (1.07 +/- 0.32). Point estimates of lambda were substantially < 1 for all three focal species in all habitats indicating the entire study area may be performing as a sink; 90% CI of lambda included 1 only for Abert's Towhee across vegetation types and Bell's Vireo in cottonwood vegetation. These results are surprising given the San Pedro is considered to be one of the best remaining occurrences of lowland native riparian vegetation in the southwestern United States. Received 15 April 2010. Accepted 8 October 2010.
C1 [Brand, L. Arriana] Univ Arizona, Dept Hydrol & Water Resources, Sustainabil Semiarid Hydrol & Riparian Areas SAHR, Tucson, AZ 85721 USA.
[Noon, Barry R.] Colorado State Univ, Dept Fish Wildlife & Conservat Biol, Ft Collins, CO 80523 USA.
RP Brand, LA (reprint author), US Geol Survey, Western Ecol Res Ctr, San Francisco Bay Estuary Field Stn, 505 Azuar Dr, Vallejo, CA 94592 USA.
EM arriana_brand@usgs.gov
FU Strategic Environment Research and Development (SERDP) [CS-1100]; SAHRA
(Sustainability of Semi-Arid Hydrology and Riparian Areas) under
National Science Foundation [EAR-9876800]; U.S. Environmental Protection
Agency [2003-STAR-G2]
FX We appreciate the work of the field crew that assisted with data
collection on the San Pedro River: Mark Faherty, Janine McCabe, Brian
Acord, Carey Hill. Devin Biggs, Chris Putnam, Brynne Langan, and Dolly
Crawford. The Bureau of Land Management, San Pedro Project Office,
provided access to the San Pedro National Conservation Area as well as
housing for the three summers of data collection effort. We are also
grateful for permission to work on lands granted by numerous private
landowners. We thank Steve Beissinger for discussions that contributed
to this research. We also thank Julie Stromberg, James Diffendorfer,
Clait Braun, and two anonymous reviewers for their helpful comments on
this manuscript. Karl Benedict kindly provided the map of the study
area. Data collection for this research was funded by the Strategic
Environment Research and Development (SERDP) project CS-1100. Analysis
and writing portions for LAB were supported by SAHRA (Sustainability of
Semi-Arid Hydrology and Riparian Areas) under the STC Program of the
National Science Foundation, Agreement #EAR-9876800, and the U.S.
Environmental Protection Agency "Integrated Modeling and Ecological
Valuation" EPA STAR GRANT Program #2003-STAR-G2.
NR 49
TC 4
Z9 4
U1 2
U2 20
PU WILSON ORNITHOLOGICAL SOC
PI WACO
PA 5400 BOSQUE BLVD, STE 680, WACO, TX 76710 USA
SN 1559-4491
EI 1938-5447
J9 WILSON J ORNITHOL
JI Wilson J. Ornithol.
PD MAR
PY 2011
VL 123
IS 1
BP 48
EP 58
DI 10.1676/10-061.1
PG 11
WC Ornithology
SC Zoology
GA 734TB
UT WOS:000288360100005
ER
PT J
AU Blank, PJ
Parks, JR
Dively, GP
AF Blank, Peter J.
Parks, Jared R.
Dively, Galen P.
TI WINTERING BIRD RESPONSE TO FALL MOWING OF HERBACEOUS BUFFERS
SO WILSON JOURNAL OF ORNITHOLOGY
LA English
DT Article
ID EASTERN NORTH-AMERICA; GRASSLAND BIRDS; FIELD BORDERS; CONSERVATION;
SHRUBLAND; COMMUNITIES; VEGETATION; PARTNERS; WILDLIFE; WIDTH
AB Herbaceous buffers are strips of herbaceous vegetation planted between working agricultural land and streams or wetlands. Mowing is a common maintenance practice to control woody plants and noxious weeds in herbaceous buffers. Buffers enrolled in Maryland's Conservation Reserve Enhancement Program (CREP) cannot be mowed during the primary bird nesting season between 15 April and 15 August. Most mowing of buffers in Maryland occurs in late summer or fall, leaving the vegetation short until the following spring. We studied the response of wintering birds to fall mowing of buffers. We mowed one section to 10-15 cm in 13 buffers and kept another section unmowed. Ninety-two percent of birds detected in buffers were grassland or scrub-shrub species, and 98% of all birds detected were in unmowed buffers. Total bird abundance, species richness, and total avian conservation value were significantly greater in unmowed buffers, and Savannah Sparrows (Passerculus sandwichenvis), Song Sparrows (Melospiza melodia), and White-throated Sparrows (Zonotrichia albicollis) were significantly more abundant in unmowed buffers. Wintering bird use of mowed buffers was less than in unmowed buffers. Leaving herbaceous buffers unmowed through winter will likely provide better habitat for wintering birds. Received 21 December 2009. Accepted 23 August 2010.
C1 [Parks, Jared R.; Dively, Galen P.] Univ Maryland, Dept Entomol, College Pk, MD 20742 USA.
[Blank, Peter J.] Univ Maryland, Marine Estuarine Environm Sci Program, College Pk, MD 20742 USA.
RP Blank, PJ (reprint author), USGS, Patuxent Wildlife Res Ctr, 12100 Beech Forest Rd, Laurel, MD 20708 USA.
EM blankpj@gmail.com
FU NRCS Agricultural Wildlife Conservation Center
FX We thank D. E. Gill, L. W. Adams, P. P. Marra, and G. L. Brewer for help
with study design. We thank the many farm owners that allowed us to work
on their properties. The Natural Resources Conservation Service (NRCS)
and the Farm Service Agency staff in Queen Anne's and Talbot counties
helped with locating CREP buffers and with technical information. J. E.
Gerber and the staff at Chesapeake Wildlife Heritage provided technical
information and advice. P. J. Barbour, C. A. Rewa, and S. V. Strati
provided comments on earlier versions of the manuscript. Funding was
provided by the NRCS Agricultural Wildlife Conservation Center.
NR 33
TC 1
Z9 1
U1 1
U2 11
PU WILSON ORNITHOLOGICAL SOC
PI WACO
PA 5400 BOSQUE BLVD, STE 680, WACO, TX 76710 USA
SN 1559-4491
EI 1938-5447
J9 WILSON J ORNITHOL
JI Wilson J. Ornithol.
PD MAR
PY 2011
VL 123
IS 1
BP 59
EP 64
DI 10.1676/09-202.1
PG 6
WC Ornithology
SC Zoology
GA 734TB
UT WOS:000288360100006
ER
PT J
AU Post, W
Sykes, PW
AF Post, William
Sykes, Paul W., Jr.
TI Reproductive Status of the Shiny Cowbird in North America
SO WILSON JOURNAL OF ORNITHOLOGY
LA English
DT Article
ID YELLOW-SHOULDERED BLACKBIRD; SOUTHEASTERN OLD-FIELD; PARASITISM
AB We collected 17 (13 females, 4 males) Shiny Cowbirds (Molothrus bonariensis) during the passerine nesting season in July 1999 and 2003 in Jasper County, southwestern South Carolina. Five females (38%) were laying eggs, as ascertained from the condition of their reproductive organs. Two females collected on 1 July 1999 and 19 July 2003 had eggs in their oviducts, and would have deposited eggs within 1 day. Shiny Cowbirds have been in North America for at least 24 years, but only males had been collected before this study. Most of those collected had enlarged testes, as did the four collected in the present study, but these data are not proof that breeding actually occurred. The reproductive condition of the females we collected provides material evidence that the species breeds in North America. It is not known which species are being parasitized by Shiny Cowbirds, but several species widespread in the southeastern United States are highly suitable hosts. Received 23 August 2010. Accepted 3 November 2010.
C1 [Post, William] Charleston Museum, Charleston, SC 29403 USA.
[Sykes, Paul W., Jr.] Univ Georgia, Warnell Sch Forest Resources, Patuxent Wildlife Res Ctr Athens, USGS, Athens, GA 30602 USA.
RP Post, W (reprint author), Charleston Museum, 360 Meeting St, Charleston, SC 29403 USA.
EM grackler@aol.com
NR 25
TC 1
Z9 2
U1 0
U2 3
PU WILSON ORNITHOLOGICAL SOC
PI WACO
PA 5400 BOSQUE BLVD, STE 680, WACO, TX 76710 USA
SN 1559-4491
J9 WILSON J ORNITHOL
JI Wilson J. Ornithol.
PD MAR
PY 2011
VL 123
IS 1
BP 151
EP 154
DI 10.1676/10-133.1
PG 4
WC Ornithology
SC Zoology
GA 734TB
UT WOS:000288360100021
ER
PT J
AU Bocetti, CI
AF Bocetti, Carol I.
TI Cruise Ships as a Source of Avian Mortality During Fall Migration
SO WILSON JOURNAL OF ORNITHOLOGY
LA English
DT Article
AB Avian mortality during fall migration has been studied at many anthropogenic structures, most of which share the common feature of bright lighting. An additional, unstudied source of avian mortality during fall migration is recreational cruise ships that are brightly lit throughout the night. I documented a single mortality event of eight Common Yellowthroats (Geothlypis trichas) on one ship during part of one night in fall 2003, but suggest this is a more wide-spread phenomenon. The advertised number of ship-nights for 50 cruise ships in the Caribbean Sea during fall migration in 2003 was 2,981. This may pose a significant, additional, anthropogenic source of mortality that warrants further investigation, particularly because impacts could be minimized if this source of avian mortality is recognized. Received 27 October 2009. Accepted 23 August 2010.
C1 [Bocetti, Carol I.] USGS, Patuxent Wildlife Res Ctr, California, PA 15419 USA.
RP Bocetti, CI (reprint author), Calif Univ Penn, 250 Univ Ave,Box 45, California, PA 15419 USA.
EM bocetti@calu.edu
NR 5
TC 3
Z9 3
U1 2
U2 8
PU WILSON ORNITHOLOGICAL SOC
PI WACO
PA 5400 BOSQUE BLVD, STE 680, WACO, TX 76710 USA
SN 1559-4491
EI 1938-5447
J9 WILSON J ORNITHOL
JI Wilson J. Ornithol.
PD MAR
PY 2011
VL 123
IS 1
BP 176
EP 178
DI 10.1676/09-168.1
PG 3
WC Ornithology
SC Zoology
GA 734TB
UT WOS:000288360100029
ER
PT J
AU Moran, SC
Newhall, C
Roman, DC
AF Moran, Seth C.
Newhall, Chris
Roman, Diana C.
TI Failed magmatic eruptions: late-stage cessation of magma ascent
SO BULLETIN OF VOLCANOLOGY
LA English
DT Article
DE Magmatic intrusions; Volcanic unrest; Eruption forecasting; Factors
influencing magmatic eruption
ID MOUNT ST-HELENS; SISTERS VOLCANIC CENTER; OREGON CASCADE RANGE;
SHISHALDIN-VOLCANO; EARTHQUAKE SWARM; UNZEN VOLCANO; ALASKA; SOUFRIERE;
DEFORMATION; PRECURSORS
AB When a volcano becomes restless, a primary question is whether the unrest will lead to an eruption. Here we recognize four possible outcomes of a magmatic intrusion: "deep intrusion", "shallow intrusion", "sluggish/viscous magmatic eruption", and "rapid, often explosive magmatic eruption". We define "failed eruptions" as instances in which magma reaches but does not pass the "shallow intrusion" stage, i.e., when magma gets close to, but does not reach, the surface. Competing factors act to promote or hinder the eventual eruption of a magma intrusion. Fresh intrusion from depth, high magma gas content, rapid ascent rates that leave little time for enroute degassing, opening of pathways, and sudden decompression near the surface all act to promote eruption, whereas decreased magma supply from depth, slow ascent, significant enroute degassing and associated increases in viscosity, and impingement on structural barriers all act to hinder eruption. All of these factors interact in complex ways with variable results, but often cause magma to stall at some depth before reaching the surface. Although certain precursory phenomena, such as rapidly escalating seismic swarms or rates of degassing or deformation, are good indicators that an eruption is likely, such phenomena have also been observed in association with intrusions that have ultimately failed to erupt. A perpetual difficulty with quantifying the probability of eruption is a lack of data, particularly on instances of failed eruptions. This difficulty is being addressed in part through the WOVOdat database. Papers in this volume will be an additional resource for scientists grappling with the issue of whether or not an episode of unrest will lead to a magmatic eruption.
C1 [Moran, Seth C.] US Geol Survey, Cascades Volcano Observ, Vancouver, WA 98683 USA.
[Newhall, Chris] Nanyang Technol Univ, Earth Observ Singapore, Singapore, Singapore.
[Roman, Diana C.] Univ S Florida, Dept Geol, Tampa, FL 33620 USA.
RP Moran, SC (reprint author), US Geol Survey, Cascades Volcano Observ, 1300 SE Cardinal Ct, Vancouver, WA 98683 USA.
EM smoran@usgs.gov; cnewhall@ntu.edu.sg; droman@usf.edu
NR 69
TC 45
Z9 45
U1 1
U2 23
PU SPRINGER
PI NEW YORK
PA 233 SPRING ST, NEW YORK, NY 10013 USA
SN 0258-8900
EI 1432-0819
J9 B VOLCANOL
JI Bull. Volcanol.
PD MAR
PY 2011
VL 73
IS 2
BP 115
EP 122
DI 10.1007/s00445-010-0444-x
PG 8
WC Geosciences, Multidisciplinary
SC Geology
GA 732US
UT WOS:000288215800001
ER
PT J
AU Roman, DC
Power, JA
AF Roman, Diana C.
Power, John A.
TI Mechanism of the 1996-97 non-eruptive volcano-tectonic earthquake swarm
at Iliamna Volcano, Alaska
SO BULLETIN OF VOLCANOLOGY
LA English
DT Article
DE Iliamna Volcano; VT earthquake; Earthquake swarms; Stress tensor
inversion; Fault-plane solutions
ID SATELLITE RADAR INTERFEROMETRY; REGIONAL STRESS TENSOR; MOUNT-SPURR
VOLCANO; SEISMICITY; JAPAN; DEFORMATION; MIGRATION
AB A significant number of volcano-tectonic (VT) earthquake swarms, some of which are accompanied by ground deformation and/or volcanic gas emissions, do not culminate in an eruption. These swarms are often thought to represent stalled intrusions of magma into the mid- or shallow-level crust. Real-time assessment of the likelihood that a VT swarm will culminate in an eruption is one of the key challenges of volcano monitoring, and retrospective analysis of non-eruptive swarms provides an important framework for future assessments. Here we explore models for a non-eruptive VT earthquake swarm located beneath Iliamna Volcano, Alaska, in May 1996-June 1997 through calculation and inversion of fault-plane solutions for swarm and background periods, and through Coulomb stress modeling of faulting types and hypocenter locations observed during the swarm. Through a comparison of models of deep and shallow intrusions to swarm observations, we aim to test the hypothesis that the 1996-97 swarm represented a shallow intrusion, or "failed" eruption. Observations of the 1996-97 swarm are found to be consistent with several scenarios including both shallow and deep intrusion, most likely involving a relatively small volume of intruded magma and/or a low degree of magma pressurization corresponding to a relatively low likelihood of eruption.
C1 [Roman, Diana C.] Univ S Florida, Dept Geol, Tampa, FL 33620 USA.
[Power, John A.] US Geol Survey, Alaska Volcano Observ, Anchorage, AK 99508 USA.
RP Roman, DC (reprint author), Univ S Florida, Dept Geol, Tampa, FL 33620 USA.
EM droman@cas.usf.edu; jpower@usgs.gov
NR 32
TC 5
Z9 5
U1 0
U2 7
PU SPRINGER
PI NEW YORK
PA 233 SPRING ST, NEW YORK, NY 10013 USA
SN 0258-8900
J9 B VOLCANOL
JI Bull. Volcanol.
PD MAR
PY 2011
VL 73
IS 2
BP 143
EP 153
DI 10.1007/s00445-010-0439-7
PG 11
WC Geosciences, Multidisciplinary
SC Geology
GA 732US
UT WOS:000288215800004
ER
PT J
AU Werner, CA
Doukas, MP
Kelly, PJ
AF Werner, Cynthia A.
Doukas, Mike P.
Kelly, Peter J.
TI Gas emissions from failed and actual eruptions from Cook Inlet
Volcanoes, Alaska, 1989-2006
SO BULLETIN OF VOLCANOLOGY
LA English
DT Article
DE Volcano; Gas; Emissions; Degassing; Magma; Eruption; Failed eruption;
Carbon; Sulfur; C/S; Decompression; Scrubbing
ID EASTERN ALEUTIAN ARC; REDOUBT VOLCANO; ILIAMNA VOLCANO; CARBON-DIOXIDE;
ELEMENT CHEMISTRY; AUGUSTINE VOLCANO; SUBDUCTION ZONE; CRATER PEAK;
MAGMAS; GEOCHEMISTRY
AB Cook Inlet volcanoes that experienced an eruption between 1989 and 2006 had mean gas emission rates that were roughly an order of magnitude higher than at volcanoes where unrest stalled. For the six events studied, mean emission rates for eruptions were similar to 13,000 t/d CO2 and 5200 t/d SO2, but only similar to 1200 t/d CO2 and 500 t/d SO2 for non-eruptive events ('failed eruptions'). Statistical analysis suggests degassing thresholds for eruption on the order of 1500 and 1000 t/d for CO2 and SO2, respectively. Emission rates greater than 4000 and 2000 t/d for CO2 and SO2, respectively, almost exclusively resulted during eruptive events (the only exception being two measurements at Fourpeaked). While this analysis could suggest that unerupted magmas have lower pre-eruptive volatile contents, we favor the explanations that either the amount of magma feeding actual eruptions is larger than that driving failed eruptions, or that magmas from failed eruptions experience less decompression such that the majority of H2O remains dissolved and thus insufficient permeability is produced to release the trapped volatile phase (or both). In the majority of unrest and eruption sequences, increases in CO2 emission relative to SO2 emission were observed early in the sequence. With time, all events converged to a common molar value of C/S between 0.5 and 2. These geochemical trends argue for roughly similar decompression histories until shallow levels are reached beneath the edifice (i.e., from 20-35 to similar to 4-6 km) and perhaps roughly similar initial volatile contents in all cases. Early elevated CO2 levels that we find at these high-latitude, andesitic arc volcanoes have also been observed at mid-latitude, relatively snow-free, basaltic volcanoes such as Stromboli and Etna. Typically such patterns are attributed to injection and decompression of deep (CO2-rich) magma into a shallower chamber and open system degassing prior to eruption. Here we argue that the C/S trends probably represent tapping of vapor-saturated regions with high C/S, and then gradual degassing of remaining dissolved volatiles as the magma progresses toward the surface. At these volcanoes, however, C/S is often accentuated due to early preferential scrubbing of sulfur gases. The range of equilibrium degassing is consistent with the bulk degassing of a magma with initial CO2 and S of 0.6 and 0.2 wt.%, respectively, similar to what has been suggested for primitive Redoubt magmas.
C1 [Werner, Cynthia A.; Doukas, Mike P.; Kelly, Peter J.] US Geol Survey, Volcano Sci Ctr, Cascades Volcano Observ, Vancouver, WA 98683 USA.
RP Werner, CA (reprint author), US Geol Survey, Volcano Sci Ctr, Cascades Volcano Observ, 1300 Cardinal Ct, Vancouver, WA 98683 USA.
EM cwerner@usgs.gov
FU US Geological Survey
FX This work was funded the US Geological Survey Volcano Hazards Program.
Helpful reviews were provided by William C. Evans, Larry Mastin,
Michelle Coombs, and one anonymous reviewer.
NR 77
TC 19
Z9 19
U1 1
U2 17
PU SPRINGER
PI NEW YORK
PA 233 SPRING ST, NEW YORK, NY 10013 USA
SN 0258-8900
J9 B VOLCANOL
JI Bull. Volcanol.
PD MAR
PY 2011
VL 73
IS 2
BP 155
EP 173
DI 10.1007/s00445-011-0453-4
PG 19
WC Geosciences, Multidisciplinary
SC Geology
GA 732US
UT WOS:000288215800005
ER
PT J
AU Crider, JG
Frank, D
Malone, SD
Poland, MP
Werner, C
Caplan-Auerbach, J
AF Crider, Juliet G.
Frank, David
Malone, Stephen D.
Poland, Michael P.
Werner, Cynthia
Caplan-Auerbach, Jacqueline
TI Magma at depth: a retrospective analysis of the 1975 unrest at Mount
Baker, Washington, USA
SO BULLETIN OF VOLCANOLOGY
LA English
DT Article
DE Quiescent degassing; Thermal unrest; Microgravity; Volcano deformation;
Stalled intrusion; Cascade Range
ID INCREASED HEAT EMISSION; KILAUEA VOLCANO; CARBON-DIOXIDE; MT BAKER;
AIRBORNE MEASUREMENTS; GRAVITY CHANGES; CENTRAL OREGON; 3 SISTERS;
ALASKA; SEISMICITY
AB Mount Baker volcano displayed a short interval of seismically-quiescent thermal unrest in 1975, with high emissions of magmatic gas that slowly waned during the following three decades. The area of snow-free ground in the active crater has not returned to pre-unrest levels, and fumarole gas geochemistry shows a decreasing magmatic signature over that same interval. A relative microgravity survey revealed a substantial gravity increase in the similar to 30 years since the unrest, while deformation measurements suggest slight deflation of the edifice between 1981-83 and 2006-07. The volcano remains seismically quiet with regard to impulsive volcano-tectonic events, but experiences shallow (< 3 km) low-frequency events likely related to glacier activity, as well as deep (> 10 km) long-period earthquakes. Reviewing the observations from the 1975 unrest in combination with geophysical and geochemical data collected in the decades that followed, we infer that elevated gas and thermal emissions at Mount Baker in 1975 resulted from magmatic activity beneath the volcano: either the emplacement of magma at mid-crustal levels, or opening of a conduit to a deep existing source of magmatic volatiles. Decadal-timescale, multi-parameter observations were essential to this assessment of magmatic activity.
C1 [Crider, Juliet G.; Malone, Stephen D.] Univ Washington, Dept Earth & Space Sci, Seattle, WA 98195 USA.
[Poland, Michael P.] US Geol Survey, Hawaiian Volcano Observ, Hawaii Natl Pk, HI USA.
[Werner, Cynthia] US Geol Survey, Cascades Volcano Observ, Vancouver, WA USA.
[Caplan-Auerbach, Jacqueline] Western Washington Univ, Dept Geol, Bellingham, WA 98225 USA.
RP Crider, JG (reprint author), Univ Washington, Dept Earth & Space Sci, Seattle, WA 98195 USA.
EM juliet.crider@ess.washington.edu
OI Poland, Michael/0000-0001-5240-6123
FU National Science Foundation [EAR 0538317]
FX We thank: Brendan Hodge and Kristin Hill Johnsen for their work on the
volcano; John Scurlock for aerial photography, including Fig. 2; Maisie
Nichols for sharing observations of DLPs; Seth Moran for prompting this
review; and Chris Newhall, Don Swanson, Glyn Williams-Jones, and David
Tucker for thoughtful reviews of our manuscript. National Science
Foundation Grant # EAR 0538317 to JGC and MPP supported revisiting the
gravity and deformation networks on Mount Baker.
NR 58
TC 7
Z9 7
U1 0
U2 14
PU SPRINGER
PI NEW YORK
PA 233 SPRING ST, NEW YORK, NY 10013 USA
SN 0258-8900
J9 B VOLCANOL
JI Bull. Volcanol.
PD MAR
PY 2011
VL 73
IS 2
BP 175
EP 189
DI 10.1007/s00445-010-0441-0
PG 15
WC Geosciences, Multidisciplinary
SC Geology
GA 732US
UT WOS:000288215800006
ER
PT J
AU Konikow, LF
AF Konikow, Leonard F.
TI The Secret to Successful Solute-Transport Modeling
SO GROUND WATER
LA English
DT Article
ID GRADIENT TRACER TEST; ADVECTION-DISPERSION EQUATION; TRANSIENT
GROUNDWATER-FLOW; HYDRAULIC CONDUCTIVITY; POROUS-MEDIA; CAPE-COD;
HETEROGENEOUS AQUIFER; CONTAMINANT TRANSPORT; EXPERIMENTAL-DESIGN;
DIFFUSION EQUATION
AB Modeling subsurface solute transport is difficult-more so than modeling heads and flows. The classical governing equation does not always adequately represent what we see at the field scale. In such cases, commonly used numerical models are solving the wrong equation. Also, the transport equation is hyperbolic where advection is dominant, and parabolic where hydrodynamic dispersion is dominant. No single numerical method works well for all conditions, and for any given complex field problem, where seepage velocity is highly variable, no one method will be optimal everywhere. Although we normally expect a numerically accurate solution to the governing groundwater-flow equation, errors in concentrations from numerical dispersion and/or oscillations may be large in some cases. The accuracy and efficiency of the numerical solution to the solute-transport equation are more sensitive to the numerical method chosen than for typical groundwater-flow problems. However, numerical errors can be kept within acceptable limits if sufficient computational effort is expended. But impractically long simulation times may promote a tendency to ignore or accept numerical errors. One approach to effective solute-transport modeling is to keep the model relatively simple and use it to test and improve conceptual understanding of the system and the problem at hand. It should not be expected that all concentrations observed in the field can be reproduced. Given a knowledgeable analyst, a reasonable description of a hydrogeologic framework, and the availability of solute-concentration data, the secret to successful solute-transport modeling may simply be to lower expectations.
C1 US Geol Survey, Reston, VA 20192 USA.
RP Konikow, LF (reprint author), US Geol Survey, Reston, VA 20192 USA.
EM lkonikow@usgs.gov
NR 65
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Z9 44
U1 2
U2 25
PU WILEY-BLACKWELL
PI HOBOKEN
PA 111 RIVER ST, HOBOKEN 07030-5774, NJ USA
SN 0017-467X
EI 1745-6584
J9 GROUND WATER
JI Ground Water
PD MAR-APR
PY 2011
VL 49
IS 2
BP 144
EP 159
DI 10.1111/j.1745-6584.2010.00764.x
PG 16
WC Geosciences, Multidisciplinary; Water Resources
SC Geology; Water Resources
GA 724NS
UT WOS:000287584100010
PM 21039449
ER
PT J
AU Seiler, RL
AF Seiler, Ralph L.
TI Po-210 in Nevada Groundwater and Its Relation to Gross Alpha
Radioactivity
SO GROUND WATER
LA English
DT Article
ID PARTICLE ACTIVITY; CARSON DESERT; WATER; POLONIUM; PROGENY; RA-226;
PB-210; WELLS
AB Polonium-210 (Po-210) is a highly toxic alpha emitter that is rarely found in groundwater at activities exceeding 1 pCi/L. Po-210 activities in 63 domestic and public-supply wells in Lahontan Valley in Churchill County in northern Nevada, United States, ranged from 0.01 +/- 0.005 to 178 +/- 16 pCi/L with a median activity of 2.88 pCi/L. Wells with high Po-210 activities had low dissolved oxygen concentrations (less than 0.1 mg/L) and commonly had pH greater than 9. Lead-210 activities are low and aqueous Po-210 is unsupported by Pb-210, indicating that the Po-210 is mobilized from aquifer sediments. The only significant contributors to alpha particle activity in Lahontan Valley groundwater are U-234/238, Rn-222, and Po-210. Radon-222 activities were below 1000 pCi/L and were uncorrelated with Po-210 activity. The only applicable drinking water standard for Po-210 in the United States is the adjusted gross alpha radioactivity (GAR) standard of 15 pCi/L. Po-210 was not volatile in a Nevada well, but volatile Po-210 has been reported in a Florida well. Additional information on the volatility of Po-210 is needed because GAR is an inappropriate method to screen for volatile radionuclides. About 25% of the samples had Po-210 activities that exceed the level associated with a lifetime total cancer risk of 1x10(-4) (1.1 pCi/L) without exceeding the GAR standard. In cases where the 72-h GAR exceeds the uranium activity by more than 5 to 10 pCi/L, an analysis to rule out the presence of Po-210 may be justified to protect human health even though the maximum contaminant level for adjusted GAR is not exceeded.
C1 US Geol Survey, Carson City, NV 89701 USA.
RP Seiler, RL (reprint author), US Geol Survey, 2730 N Deer Run Rd, Carson City, NV 89701 USA.
EM rseiler@usgs.gov
FU U.S. EPA [EM-96963201]; Churchill County; USGS
FX This study was supported by a grant from the U.S. EPA, EM-96963201, and
a cooperative agreement between Churchill County and the USGS. The
author thanks the residents of Lahontan Valley who gave permission to
collect samples from their wells, and Chris Pritsos (University of
Nevada, Reno) and Lisbeth Welniak (University of California at Davis),
his coauthors on the U.S. EPA grant proposal to investigate biological
effects of exposure to complex mixtures of trace elements and
radionuclides in natural groundwater. Chemical data for a naturally
contaminated well in Maryland was provided by Michelle Cutler, Charles
County Department of Utilities, Maryland. I greatly appreciate
conversations with Mike Arndt (Wisconsin State Laboratory of Hygiene) on
the contribution of 210Po to GAR. An earlier version of this
article was greatly improved by the valuable comments of Matt Leybourne
and two anonymous reviewers.
NR 41
TC 10
Z9 10
U1 4
U2 10
PU WILEY-BLACKWELL
PI MALDEN
PA COMMERCE PLACE, 350 MAIN ST, MALDEN 02148, MA USA
SN 0017-467X
J9 GROUND WATER
JI Ground Water
PD MAR-APR
PY 2011
VL 49
IS 2
BP 160
EP 171
DI 10.1111/j.1745-6584.2010.00688.x
PG 12
WC Geosciences, Multidisciplinary; Water Resources
SC Geology; Water Resources
GA 724NS
UT WOS:000287584100011
PM 20180863
ER
PT J
AU Minsley, BJ
Ajo-Franklin, J
Mukhopadhyay, A
Morgan, FD
AF Minsley, Burke J.
Ajo-Franklin, Jonathan
Mukhopadhyay, Amitabha
Morgan, Frank Dale
TI Hydrogeophysical Methods for Analyzing Aquifer Storage and Recovery
Systems
SO GROUND WATER
LA English
DT Article
ID DAMMAM FORMATION; KUWAIT; RESISTIVITY; GROUNDWATER; HYDROGEOLOGY;
RESOURCES; TRANSIENT; TRANSPORT; GEOLOGY; TIME
AB Hydrogeophysical methods are presented that support the siting and monitoring of aquifer storage and recovery (ASR) systems. These methods are presented as numerical simulations in the context of a proposed ASR experiment in Kuwait, although the techniques are applicable to numerous ASR projects. Bulk geophysical properties are calculated directly from ASR flow and solute transport simulations using standard petrophysical relationships and are used to simulate the dynamic geophysical response to ASR. This strategy provides a quantitative framework for determining site-specific geophysical methods and data acquisition geometries that can provide the most useful information about the ASR implementation. An axisymmetric, coupled fluid flow and solute transport model simulates injection, storage, and withdrawal of fresh water (salinity similar to 500 ppm) into the Dammam aquifer, a tertiary carbonate formation with native salinity approximately 6000 ppm. Sensitivity of the flow simulations to the correlation length of aquifer heterogeneity, aquifer dispersivity, and hydraulic permeability of the confining layer are investigated. The geophysical response using electrical resistivity, time-domain electromagnetic (TEM), and seismic methods is computed at regular intervals during the ASR simulation to investigate the sensitivity of these different techniques to changes in subsurface properties. For the electrical and electromagnetic methods, fluid electric conductivity is derived from the modeled salinity and is combined with an assumed porosity model to compute a bulk electrical resistivity structure. The seismic response is computed from the porosity model and changes in effective stress due to fluid pressure variations during injection/recovery, while changes in fluid properties are introduced through Gassmann fluid substitution.
C1 [Minsley, Burke J.; Morgan, Frank Dale] MIT, Dept Earth Atmospher & Planetary Sci, Cambridge, MA 02139 USA.
[Ajo-Franklin, Jonathan] Univ Calif Berkeley, Lawrence Berkeley Lab, Berkeley, CA 94720 USA.
[Mukhopadhyay, Amitabha] Kuwait Inst Sci Res, Safat 13109, Kuwait.
RP Minsley, BJ (reprint author), US Geol Survey, Denver Fed Ctr, MS964, Denver, CO 80225 USA.
EM bminsley@usgs.gov
RI Ajo-Franklin, Jonathan/G-7169-2015;
OI Ajo-Franklin, Jonathan/0000-0002-6666-4702; Minsley,
Burke/0000-0003-1689-1306
FU Kuwait-MIT Center for Natural Resources and the Environment; Kuwait
Foundation for the Advancement of Science
FX This work was funded by the Kuwait-MIT Center for Natural Resources and
the Environment, with support from the Kuwait Foundation for the
Advancement of Science. We are grateful for valuable suggestions
provided by reviewers Fred Day-Lewis, Paul Bedrosian, William Hutchings,
Dave Hart, and Joe Hughes.
NR 39
TC 12
Z9 12
U1 0
U2 17
PU WILEY-BLACKWELL
PI MALDEN
PA COMMERCE PLACE, 350 MAIN ST, MALDEN 02148, MA USA
SN 0017-467X
J9 GROUND WATER
JI Ground Water
PD MAR-APR
PY 2011
VL 49
IS 2
BP 250
EP 269
DI 10.1111/j.1745-6584.2010.00676.x
PG 20
WC Geosciences, Multidisciplinary; Water Resources
SC Geology; Water Resources
GA 724NS
UT WOS:000287584100019
PM 20180865
ER
PT J
AU Husak, GJ
Michaelsen, J
Kyriakidis, P
Verdin, JP
Funk, C
Galu, G
AF Husak, Gregory J.
Michaelsen, Joel
Kyriakidis, Phaedon
Verdin, James P.
Funk, Chris
Galu, Gideon
TI The Forecast Interpretation Tool - a Monte Carlo technique for blending
climatic distributions with probabilistic forecasts
SO INTERNATIONAL JOURNAL OF CLIMATOLOGY
LA English
DT Article
DE rainfall; forecast; probability; Monte Carlo simulation
ID GAMMA-DISTRIBUTION; RAINFALL; PRECIPITATION
AB Probabilistic forecasts are produced from a variety of outlets to help predict rainfall, and other meteorological events, for periods of 1 month or more. Such forecasts are expressed as probabilities of a rainfall event, e. g. being in the upper, middle, or lower third of the relevant distribution of rainfall in the region. The impact of these forecasts on the expectation for the event is not always clear or easily conveyed. This article proposes a technique based on Monte Carlo simulation for adjusting existing climatologic statistical parameters to match forecast information, resulting in new parameters defining the probability of events for the forecast interval. The resulting parameters are shown to approximate the forecasts with reasonable accuracy. To show the value of the technique as an application for seasonal rainfall, it is used with consensus forecast developed for the Greater Horn of Africa for the 2009 March-April-May season. An alternative, analytical approach is also proposed, and discussed in comparison to the first simulation-based technique. Copyright. (C) 2010 Royal Meteorological Society
C1 [Husak, Gregory J.; Michaelsen, Joel; Kyriakidis, Phaedon; Funk, Chris] Univ Calif Santa Barbara, Dept Geog, Santa Barbara, CA 93106 USA.
[Verdin, James P.; Funk, Chris] US Geol Survey, Earth Resources Observat & Sci Ctr, Sioux Falls, SD USA.
[Galu, Gideon] Famine Early Warning Syst Network, Nairobi, Kenya.
RP Husak, GJ (reprint author), Univ Calif Santa Barbara, Dept Geog, Santa Barbara, CA 93106 USA.
EM husak@geog.ucsb.edu
OI Kyriakidis, Phaedon/0000-0003-4222-8567
NR 19
TC 2
Z9 2
U1 0
U2 3
PU WILEY-BLACKWELL
PI MALDEN
PA COMMERCE PLACE, 350 MAIN ST, MALDEN 02148, MA USA
SN 0899-8418
J9 INT J CLIMATOL
JI Int. J. Climatol.
PD MAR
PY 2011
VL 31
IS 3
BP 461
EP 467
DI 10.1002/joc.2074
PG 7
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA 731EX
UT WOS:000288090200011
ER
PT J
AU Vander Pol, SS
Hobson, KA
Becker, PR
Day, RD
Ellisor, MB
Pugh, RS
Roseneau, DG
AF Vander Pol, Stacy S.
Hobson, Keith A.
Becker, Paul R.
Day, Rusty D.
Ellisor, Michael B.
Pugh, Rebecca S.
Roseneau, David G.
TI Geographic differences in organic contaminants and stable isotopes
(delta C-13, delta N-15) in thick-billed murre (Uria lomvia) eggs from
Alaska
SO JOURNAL OF ENVIRONMENTAL MONITORING
LA English
DT Article
ID TROPHIC POSITION; SEABIRD EGGS; FOOD-WEB; ORGANOCHLORINE; RESIDUES;
GULF; TRANSPORT; TRENDS; SEA
AB The contents from thick-billed murre (Uria lomvia) eggs collected at four Alaskan colonies in 2002 were analyzed for organic contaminants and carbon (delta C-13) and nitrogen (delta N-15) stable isotopes. Contaminant concentrations in the eggs varied from below detection limits to 230 ng g(-1) wet mass for 4,4'-DDE in one egg from St Lazaria Island in the Gulf of Alaska. Eggs from this colony generally contained higher levels of contaminants and exhibited significantly different patterns compared to eggs from the Bering and Chukchi seas. Stable isotope values also varied geographically; however, these differences appeared to be related to differences in C and N baselines in the food webs instead of differences in prey. Contaminant and stable isotope correlations were inconclusive, suggesting that better information on regional food web differences and differential offloading of contaminants and stable isotopes to the eggs must be obtained before these kinds of data can be fully incorporated into seabird egg contaminant monitoring programs.
C1 [Vander Pol, Stacy S.; Becker, Paul R.; Day, Rusty D.; Ellisor, Michael B.; Pugh, Rebecca S.] Natl Inst Stand & Technol, Div Analyt Chem, Hollings Marine Lab, Charleston, SC 29412 USA.
[Hobson, Keith A.] Environm Canada, Saskatoon, SK S7N 3H5, Canada.
[Roseneau, David G.] US Fish & Wildlife Serv, Homer, AK 99603 USA.
RP Vander Pol, SS (reprint author), Natl Inst Stand & Technol, Div Analyt Chem, Hollings Marine Lab, 331 Ft Johnson Rd, Charleston, SC 29412 USA.
EM stacy.vanderpol@nist.gov
FU Alaska Maritime National Wildlife Refuge
FX We would like to thank the Alaska Maritime National Wildlife Refuge for
supporting the STAMP program; Larua Greffenius, Susan Hatch, Arthur
Kettle, Dean Kildaw, Alexis Paul and the residents of Little Diomede
Island for collecting the 1999 common murre eggs; Adrian Gall, Earl
Kingik, Jackson Mokiyuk, Leslie Slater, and Julie Snorek for collecting
the 2002 thick-billed murre eggs; and Lesley Chappel and Kristin Simac
for helping to process them. Blanca Mora Alvarez prepared the samples
for stable isotope analyses and Myles Stocki made the isotopic
measurements.
NR 32
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U1 4
U2 12
PU ROYAL SOC CHEMISTRY
PI CAMBRIDGE
PA THOMAS GRAHAM HOUSE, SCIENCE PARK, MILTON RD, CAMBRIDGE CB4 0WF, CAMBS,
ENGLAND
SN 1464-0325
EI 1464-0333
J9 J ENVIRON MONITOR
JI J. Environ. Monit.
PD MAR
PY 2011
VL 13
IS 3
BP 699
EP 705
DI 10.1039/c0em00347f
PG 7
WC Chemistry, Analytical; Environmental Sciences
SC Chemistry; Environmental Sciences & Ecology
GA 732CH
UT WOS:000288160200025
PM 21253646
ER
PT J
AU Cadena, CD
Gutierrez-Pinto, N
Davila, N
Chesser, RT
AF Daniel Cadena, Carlos
Gutierrez-Pinto, Natalia
Davila, Nicolas
Chesser, R. Terry
TI No population genetic structure in a widespread aquatic songbird from
the Neotropics
SO MOLECULAR PHYLOGENETICS AND EVOLUTION
LA English
DT Article
DE Andes; Amazonia; Chrysomus icterocephalus; Icteridae; Phylogeography;
Yellow-hooded Blackbird
ID HISTORICAL DIVERSIFICATION; LANDSCAPE EVOLUTION; FOREST BIRDS;
DIFFERENTIATION; DIVERSITY; SOFTWARE; AMAZONIA; ECOLOGY; AVES
AB Neotropical lowland organisms often show marked population genetic structure, suggesting restricted migration among populations. However, most phylogeographic studies have focused on species inhabiting humid forest interior. Little attention has been devoted to the study of species with ecologies conducive to dispersal, such as those of more open and variable environments associated with watercourses. Using mtDNA sequences, we examined patterns of genetic variation in a widely distributed Neotropical songbird of aquatic environments, the Yellow-hooded Blackbird (Icteridae, Chrysomus icterocephalus). In contrast to many forest species, Yellow-hooded Blackbirds showed no detectable genetic structure across their range, which includes lowland populations on both sides of the Andes, much of northeastern South America, Amazonia, as well as a phenotypically distinct highland population in Colombia. A coalescent-based analysis of the species indicated that its effective population size has increased considerably, suggesting a range expansion. Our results support the hypothesis that species occurring in open habitats and tracking temporally dynamic environments should show increased dispersal propensities (hence gene flow) relative to species from closed and more stable environments. The phenotypic and behavioral variation among populations of our study species appears to have arisen recently and perhaps in the face of gene flow. (C) 2010 Elsevier Inc. All rights reserved.
C1 [Daniel Cadena, Carlos; Gutierrez-Pinto, Natalia; Davila, Nicolas] Univ Los Andes, Dept Ciencias Biol, Lab Biol Evolut Vertebrados, Bogota, Colombia.
[Chesser, R. Terry] Smithsonian Inst, Natl Museum Nat Hist, USGS Patuxent Wildlife Res Ctr, Washington, DC 20013 USA.
RP Cadena, CD (reprint author), Univ Los Andes, Dept Ciencias Biol, Lab Biol Evolut Vertebrados, Apartado 4976, Bogota, Colombia.
EM ccadena@uniandes.edu.co; n.gutierrez126@uniandes.edu.co;
nicodavila@hotmail.com; chessert@si.edu
FU Facultad de Ciencias at Universidad de los Andes; National Science
Foundation [DEB-0841729]; Office of Fellowships, Smithsonian Institution
FX Financial support for this study was provided by the Facultad de
Ciencias at Universidad de los Andes, the National Science Foundation
(Grant DEB-0841729 to R. T. Brumfield), and the Office of Fellowships,
Smithsonian Institution. We thank the American Museum of Natural History
(J. Cracraft and P. Sweet), the Field Museum of Natural History (J.
Bates and D. Willard), the Institut Nacional de Pesquisas de Amazonia
(M. Cohn-Haft), and the Louisiana State University Museum of Natural
Science (R. Brumfield and D. Dittmann) for tissue loans. Use of trade,
product, or firm names does riot imply endorsement by the US Government.
NR 33
TC 15
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U1 0
U2 16
PU ACADEMIC PRESS INC ELSEVIER SCIENCE
PI SAN DIEGO
PA 525 B ST, STE 1900, SAN DIEGO, CA 92101-4495 USA
SN 1055-7903
J9 MOL PHYLOGENET EVOL
JI Mol. Phylogenet. Evol.
PD MAR
PY 2011
VL 58
IS 3
BP 540
EP 545
DI 10.1016/j.ympev.2010.12.014
PG 6
WC Biochemistry & Molecular Biology; Evolutionary Biology; Genetics &
Heredity
SC Biochemistry & Molecular Biology; Evolutionary Biology; Genetics &
Heredity
GA 731ZX
UT WOS:000288151000012
PM 21195784
ER
PT J
AU Jordan, TH
Jones, LM
AF Jordan, Thomas H.
Jones, Lucile M.
TI Reply to 'A Second Opinion on "Operational Earthquake Forecasting: Some
Thoughts on Why and How," by Thomas H. Jordan and Lucile M. Jones,' by
Stuart Crampin
SO SEISMOLOGICAL RESEARCH LETTERS
LA English
DT Article
ID PREDICTION; PREDICTABILITY
C1 [Jordan, Thomas H.] Univ So Calif, So Calif Earthquake Ctr, Los Angeles, CA 90089 USA.
[Jones, Lucile M.] US Geol Survey, Multihazards Demonstrat Project, Pasadena, CA 91125 USA.
RP Jordan, TH (reprint author), Univ So Calif, So Calif Earthquake Ctr, Los Angeles, CA 90089 USA.
NR 12
TC 5
Z9 5
U1 0
U2 3
PU SEISMOLOGICAL SOC AMER
PI ALBANY
PA 400 EVELYN AVE, SUITE 201, ALBANY, CA 94706-1375 USA
SN 0895-0695
EI 1938-2057
J9 SEISMOL RES LETT
JI Seismol. Res. Lett.
PD MAR-APR
PY 2011
VL 82
IS 2
BP 231
EP 232
DI 10.1785/gssrl.82.2.231
PG 2
WC Geochemistry & Geophysics
SC Geochemistry & Geophysics
GA 731XO
UT WOS:000288144000011
ER
PT J
AU Saros, JE
Clow, DW
Blett, T
Wolfe, AP
AF Saros, Jasmine E.
Clow, David W.
Blett, Tamara
Wolfe, Alexander P.
TI Critical Nitrogen Deposition Loads in High-elevation Lakes of the
Western US Inferred from Paleolimnological Records
SO WATER AIR AND SOIL POLLUTION
LA English
DT Article
DE Critical load; Atmospheric nitrogen deposition; Alpine lake ecosystems;
Diatoms
ID UNITED-STATES; ALPINE LAKES; ATMOSPHERIC DEPOSITION; ROCKY-MOUNTAINS;
SURFACE WATERS; PHYTOPLANKTON; COLORADO; ACIDITY; REQUIREMENTS;
NUTRIENTS
AB Critical loads of nitrogen (N) from atmospheric deposition were determined for alpine lake ecosystems in the western US using fossil diatom assemblages in lake sediment cores. Changes in diatom species over the last century were indicative of N enrichment in two areas, the eastern Sierra Nevada, starting between 1960 and 1965, and the Greater Yellowstone Ecosystem, starting in 1980. In contrast, no changes in diatom community structure were apparent in lakes of Glacier National Park. To determine critical N loads that elicited these community changes, we modeled wet nitrogen deposition rates for the period in which diatom shifts first occurred in each area using deposition data spanning from 1980 to 2007. We determined a critical load of 1.4 kg N ha(-1) year(-1) wet N deposition to elicit key nutrient enrichment effects on diatom communities in both the eastern Sierra Nevada and the Greater Yellowstone Ecosystem.
C1 [Saros, Jasmine E.] Univ Maine, Climate Change Inst, Orono, ME 04469 USA.
[Saros, Jasmine E.] Univ Maine, Sch Biol & Ecol, Orono, ME 04469 USA.
[Clow, David W.] US Geol Survey, Water Resources Discipline, Lakewood, CO 80225 USA.
[Blett, Tamara] Natl Pk Serv, Air Resources Div, Lakewood, CO 80225 USA.
[Wolfe, Alexander P.] Univ Alberta, Dept Earth & Atmospher Sci, Edmonton, AB, Canada.
RP Saros, JE (reprint author), Univ Maine, Climate Change Inst, Orono, ME 04469 USA.
EM jasmine.saros@maine.edu; dwclow@usgs.gov; tamara_blett@nps.gov;
awolfe@ualberta.ca
RI Wolfe, Alexander/G-6867-2011;
OI Clow, David/0000-0001-6183-4824
FU Air Resources Division of the National Park Service of the US; US
National Science Foundation [DEB-0089600, DEB-0734277]
FX We thank Dixon Landers for providing sediment samples from the GNP
lakes, and for sharing the age models for these cores. Courtney Wigdahl
counted the diatoms in the GNP and ESN cores, and assisted with core
collection in the eastern Sierras. Data from Mark Whiting, posted on the
Diatom Paleolimnology Data Cooperative
(http://diatom.acnatsci.org/dpdc/), were helpful in determining our
coring sites in the ESN. Leora Nanus provided information on
elevation-adjusted N deposition values for the GYE. Funding for this
project was provided by the Air Resources Division of the National Park
Service of the US, as well as the US National Science Foundation
(DEB-0089600 and DEB-0734277).
NR 37
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Z9 31
U1 0
U2 24
PU SPRINGER
PI DORDRECHT
PA VAN GODEWIJCKSTRAAT 30, 3311 GZ DORDRECHT, NETHERLANDS
SN 0049-6979
J9 WATER AIR SOIL POLL
JI Water Air Soil Pollut.
PD MAR
PY 2011
VL 216
IS 1-4
BP 193
EP 202
DI 10.1007/s11270-010-0526-6
PG 10
WC Environmental Sciences; Meteorology & Atmospheric Sciences; Water
Resources
SC Environmental Sciences & Ecology; Meteorology & Atmospheric Sciences;
Water Resources
GA 721CC
UT WOS:000287328000017
ER
PT J
AU Brown, HE
Yates, KF
Dietrich, G
MacMillan, K
Graham, CB
Reese, SM
Helterbrand, WS
Nicholson, WL
Blount, K
Mead, PS
Patrick, SL
Eisen, RJ
AF Brown, Heidi E.
Yates, Karen F.
Dietrich, Gabrielle
MacMillan, Katherine
Graham, Christine B.
Reese, Sara M.
Helterbrand, Wm Steve
Nicholson, William L.
Blount, Keith
Mead, Paul S.
Patrick, Sarah L.
Eisen, Rebecca J.
TI An Acarologic Survey and Amblyomma americanum Distribution Map with
Implications for Tularemia Risk in Missouri
SO AMERICAN JOURNAL OF TROPICAL MEDICINE AND HYGIENE
LA English
DT Article
ID WHITE-TAILED DEER; LONE STAR TICK; UNITED-STATES; LYME-DISEASE;
DERMACENTOR-VARIABILIS; FRANCISELLA-TULARENSIS; SEASONAL OCCURRENCE;
HOST ASSOCIATIONS; MENDOCINO COUNTY; DENSE WOODLANDS
AB In the United States, tickborne diseases occur focally. Missouri represents a major focus of several tickborne diseases that includes spotted fever rickettsiosis, tularemia, and ehrlichiosis. Our study sought to determine the potential risk of human exposure to human-biting vector ticks in this area. We collected ticks in 79 sites in southern Missouri during June 7-10, 2009, which yielded 1,047 adult and 3,585 nymphal Amblyomma americanum,5 adult Amblyomma maculatum, 19 adult Dermacentor variabilis, and 5 nymphal lxodes brunneus. Logistic regression analysis showed that areas posing an elevated risk of exposure to A. americanum nymphs or adults were more likely to be classified as forested than grassland, and the probability of being classified as elevated risk increased with increasing relative humidity during the month of June (30-year average). Overall accuracy of each of the two models was greater than 70% and showed that 20% and 30% of the state were classified as elevated risk for human exposure to nymphs and adults, respectively. We also found a significant positive association between heightened acarologic risk and counties reporting tularemia cases. Our study provides an updated distribution map for A. americanum in Missouri and suggests a wide-spread risk of human exposure to A. americanum and their associated pathogens in this region.
C1 [Brown, Heidi E.] Univ Arizona, Sch Geog & Dev, Tucson, AZ 85721 USA.
[Yates, Karen F.] Missouri Dept Hlth & Senior Serv, Vector Borne Dis Program, Jefferson City, MO USA.
Ctr Dis Control & Prevent, Div Vector Borne Dis, Bacterial Dis Branch, Ft Collins, CO USA.
Ctr Dis Control & Prevent, Div Vector Borne Dis, Epidemiol Branch, Ft Collins, CO USA.
[Dietrich, Gabrielle; MacMillan, Katherine; Graham, Christine B.; Mead, Paul S.; Eisen, Rebecca J.] Ctr Dis Control & Prevent, Natl Ctr Zoonot Vector Borne & Enter Dis, Div Vector Borne Infect Dis, Ft Collins, CO USA.
[Reese, Sara M.] Div Colorado Dept Publ Hlth & Environm, Hlth Facil & Emergency Med Serv, South Denver, CO USA.
Colorado Dept Publ Hlth & Environm, Patient Safety Program, Hlth Facil & Emergency Med Serv Div, South Denver, CO USA.
[Helterbrand, Wm Steve] US Geol Survey, Natl Geospatial Tech Operat Ctr, Ctr Excellence Geospatial Informat Sci, Rolla, MO USA.
US Geol Survey, Midcontinent Geog Sci Ctr, Rolla, MO USA.
[Nicholson, William L.] Ctr Dis Control & Prevent, Dis Assessment Team, Rickettsial Zoonoses Branch, Natl Ctr Zoonot Vector Borne & Enter Dis, Atlanta, GA USA.
[Blount, Keith] USAF Acad, Dept Biol, Colorado Springs, CO USA.
[Patrick, Sarah L.] Missouri Dept Hlth & Senior Serv, Sect Epidemiol & Publ Hlth Practice, Div Community & Publ Hlth, Jefferson City, MO USA.
USAF, Res Labs, Brooks City Base, TX USA.
RP Brown, HE (reprint author), Univ Arizona, Sch Geog & Dev, 1103 E 2nd St,Harvill Room 405, Tucson, AZ 85721 USA.
EM heidibrown@email.arizona.edu; karen.yates@dhss.mo.gov;
edietrich@cdc.gov; kmacmillan@cdc.gov; cgraham@cdc.gov;
sreese@smtpgate.dphe.state.co.us; vwhelterbrand@usgs.gov;
wnicholson@cdc.gov; keith.blount@us.af.mil; pfm0@cdc.gov;
sarah.patrick@dhss.mo.gov; rjeisen@cdc.gov
OI Brown, Heidi/0000-0001-8578-5510
FU National Center for Zoonotic, Vector-Borne; Enteric Diseases, Division
of Vector-Borne Diseases, CDC; U.S. Department of Energy; CDC; CDC
National Center for Environmental Health
FX This study was supported in part by the appointment of Heidi E. Brown to
the Research Participation Program at the National Center for Zoonotic,
Vector-Borne, and Enteric Diseases, Division of Vector-Borne Diseases,
CDC administered by the Oak Ridge Institute for Science and Education
through an interagency agreement between the U.S. Department of Energy
and CDC. Partial support for this project was provided through the
internal funding under the CDC National Center for Environmental Health.
NR 50
TC 17
Z9 17
U1 0
U2 23
PU AMER SOC TROP MED & HYGIENE
PI MCLEAN
PA 8000 WESTPARK DR, STE 130, MCLEAN, VA 22101 USA
SN 0002-9637
J9 AM J TROP MED HYG
JI Am. J. Trop. Med. Hyg.
PD MAR
PY 2011
VL 84
IS 3
BP 411
EP 419
DI 10.4269/ajtmh.2011.10-0593
PG 9
WC Public, Environmental & Occupational Health; Tropical Medicine
SC Public, Environmental & Occupational Health; Tropical Medicine
GA 730AK
UT WOS:000287995600010
PM 21363979
ER
PT J
AU Vrieze, LA
Bergstedt, RA
Sorensen, PW
AF Vrieze, Lance A.
Bergstedt, Roger A.
Sorensen, Peter W.
TI Olfactory-mediated stream-finding behavior of migratory adult sea
lamprey (Petromyzon marinus)
SO CANADIAN JOURNAL OF FISHERIES AND AQUATIC SCIENCES
LA English
DT Article
ID ULTRASONIC TELEMETRY; SPAWNING MIGRATION; ONCORHYNCHUS-NERKA; VERTICAL
MOVEMENTS; SOCKEYE-SALMON; BILE-ACIDS; PHEROMONE; RIVER; FISH;
ORIENTATION
AB Stream-finding behavior of adult sea lamprey (Petromyzon marinus), an anadromous fish that relies on pheromones to locate spawning streams, was documented in the vicinity of an important spawning river in the Great Lakes. Untreated and anosmic migrating sea lampreys were implanted with acoustic transmitters and then released outside the Ocqueoc River. Lampreys swam only at night and then actively. When outside of the river plume, lampreys pursued relatively straight bearings parallel to the shoreline while making frequent vertical excursions. In contrast, when within the plume, lampreys made large turns and exhibited a weak bias towards the river mouth, which one-third of them entered. The behavior of anosmic lampreys resembled that of untreated lampreys outside of the plume, except they pursued a more northerly compass bearing. To locate streams, sea lampreys appear to employ a three-phase odor-mediated strategy that involves an initial search along shorelines while casting vertically, followed by river-water-induced turning that brings them close to the river's mouth, which they then enter using rheotaxis. This novel strategy differs from that of salmonids and appears to offer this poor swimmer adaptive flexibility and suggests ways that pheromonal odors might be used to manage this invasive species.
C1 [Vrieze, Lance A.; Sorensen, Peter W.] Univ Minnesota, Dept Fisheries Wildlife & Conservat Biol, St Paul, MN 55108 USA.
[Bergstedt, Roger A.] US Geol Survey, Hammond Bay Biol Stn, Millersburg, MI 49759 USA.
RP Sorensen, PW (reprint author), Univ Minnesota, Dept Fisheries Wildlife & Conservat Biol, 1980 Folwell Ave, St Paul, MN 55108 USA.
EM soren003@umn.edu
FU Great Lakes Fisheries Commission; Minnesota Agriculture Experiment
Station
FX This project was supported by the Great Lakes Fisheries Commission and
the Minnesota Agriculture Experiment Station. Scott McKinley kindly
provided assistance with tag selection and lent us a fish swimming tube
to test performance. His students, Adam Cottrill and Kris Hunter,
provided instruction on surgeries and telemetry equipment. Sean Sisler
provided invaluable assistance during late-night tracking. Staff from
the Hammond Bay Biological Station, Marquette Biological Station, and
Sea Lamprey Control Centre (Sault Saint Marie) provided lampreys and
additional advice. Two anonymous reviewers and the editorial staff
provided many helpful comments.
NR 44
TC 29
Z9 30
U1 2
U2 30
PU CANADIAN SCIENCE PUBLISHING, NRC RESEARCH PRESS
PI OTTAWA
PA 1200 MONTREAL ROAD, BUILDING M-55, OTTAWA, ON K1A 0R6, CANADA
SN 0706-652X
J9 CAN J FISH AQUAT SCI
JI Can. J. Fish. Aquat. Sci.
PD MAR
PY 2011
VL 68
IS 3
BP 523
EP 533
DI 10.1139/F10-169
PG 11
WC Fisheries; Marine & Freshwater Biology
SC Fisheries; Marine & Freshwater Biology
GA 729VC
UT WOS:000287978500012
ER
PT J
AU Krauss, KW
Duberstein, JA
AF Krauss, Ken W.
Duberstein, Jamie A.
TI Sapflow and water use of freshwater wetland trees exposed to saltwater
incursion in a tidally influenced South Carolina watershed (vol 40, pg
525, 2010)
SO CANADIAN JOURNAL OF FOREST RESEARCH-REVUE CANADIENNE DE RECHERCHE
FORESTIERE
LA English
DT Correction
C1 [Krauss, Ken W.] US Geol Survey, Natl Wetlands Res Ctr, Lafayette, LA 70506 USA.
[Duberstein, Jamie A.] Clemson Univ, Baruch Inst Coastal Ecol & Forest Sci, Georgetown, SC 29442 USA.
RP Krauss, KW (reprint author), US Geol Survey, Natl Wetlands Res Ctr, 700 Cajundome Blvd, Lafayette, LA 70506 USA.
EM kkrauss@usgs.gov
NR 1
TC 0
Z9 0
U1 0
U2 3
PU CANADIAN SCIENCE PUBLISHING, NRC RESEARCH PRESS
PI OTTAWA
PA 1200 MONTREAL ROAD, BUILDING M-55, OTTAWA, ON K1A 0R6, CANADA
SN 0045-5067
J9 CAN J FOREST RES
JI Can. J. For. Res.-Rev. Can. Rech. For.
PD MAR
PY 2011
VL 41
IS 3
BP 660
EP 660
DI 10.1139/X10-249
PG 1
WC Forestry
SC Forestry
GA 730KN
UT WOS:000288032300023
ER
PT J
AU Storlazzi, CD
Field, ME
Bothner, MH
AF Storlazzi, C. D.
Field, M. E.
Bothner, M. H.
TI The use (and misuse) of sediment traps in coral reef environments:
theory, observations, and suggested protocols
SO CORAL REEFS
LA English
DT Article
DE Sediment trap; Coral reefs; Sedimentation; Waves; Currents; Shear stress
ID COLLECTION EFFICIENCY; FIELD ASSESSMENT; TURBULENT FLOWS; RESUSPENSION;
PARTICLES; MOLOKAI; HAWAII; BIASES; RATES; FLUX
AB Sediment traps are commonly used as standard tools for monitoring "sedimentation" in coral reef environments. In much of the literature where sediment traps were used to measure the effects of "sedimentation" on corals, it is clear from deployment descriptions and interpretations of the resulting data that information derived from sediment traps has frequently been misinterpreted or misapplied. Despite their widespread use in this setting, sediment traps do not provide quantitative information about "sedimentation" on coral surfaces. Traps can provide useful information about the relative magnitude of sediment dynamics if trap deployment standards are used. This conclusion is based first on a brief review of the state of knowledge of sediment trap dynamics, which has primarily focused on traps deployed high above the seabed in relatively deep water, followed by our understanding of near-bed sediment dynamics in shallow-water environments that characterize coral reefs. This overview is followed by the first synthesis of near-bed sediment trap data collected with concurrent hydrodynamic information in coral reef environments. This collective information is utilized to develop nine protocols for using sediment traps in coral reef environments, which focus on trap parameters that researchers can control such as trap height (H), trap mouth diameter (D), the height of the trap mouth above the substrate (z (o) ), and the spacing between traps. The hydrodynamic behavior of sediment traps and the limitations of data derived from these traps should be forefront when interpreting sediment trap data to infer sediment transport processes in coral reef environments.
C1 [Storlazzi, C. D.; Field, M. E.] US Geol Survey, Pacific Coastal & Marine Sci Ctr, Santa Cruz, CA 95060 USA.
[Bothner, M. H.] US Geol Survey, Woods Hole Sci Ctr, Woods Hole, MA 02543 USA.
RP Storlazzi, CD (reprint author), US Geol Survey, Pacific Coastal & Marine Sci Ctr, 400 Nat Bridges Dr, Santa Cruz, CA 95060 USA.
EM cstorlazzi@usgs.gov
OI Storlazzi, Curt/0000-0001-8057-4490
NR 51
TC 35
Z9 35
U1 1
U2 29
PU SPRINGER
PI NEW YORK
PA 233 SPRING ST, NEW YORK, NY 10013 USA
SN 0722-4028
EI 1432-0975
J9 CORAL REEFS
JI Coral Reefs
PD MAR
PY 2011
VL 30
IS 1
BP 23
EP 38
DI 10.1007/s00338-010-0705-3
PG 16
WC Marine & Freshwater Biology
SC Marine & Freshwater Biology
GA 716BV
UT WOS:000286940800004
ER
PT J
AU Yoshizaki, J
Brownie, C
Pollock, KH
Link, WA
AF Yoshizaki, Jun
Brownie, Cavell
Pollock, Kenneth H.
Link, William A.
TI Modeling misidentification errors that result from use of genetic tags
in capture-recapture studies
SO ENVIRONMENTAL AND ECOLOGICAL STATISTICS
LA English
DT Article
DE Closed population models; Genotype; Population size estimate; Natural
tags; Photographic identification; Misidentification
ID POPULATION-SIZE ESTIMATION; GENOTYPING ERRORS; DNA; ABUNDANCE; INFERENCE
AB Misidentification of animals is potentially important when naturally existing features (natural tags) such as DNA fingerprints (genetic tags) are used to identify individual animals. For example, when misidentification leads to multiple identities being assigned to an animal, traditional estimators tend to overestimate population size. Accounting for misidentification in capture-recapture models requires detailed understanding of the mechanism. Using genetic tags as an example, we outline a framework for modeling the effect of misidentification in closed population studies when individual identification is based on natural tags that are consistent over time (non-evolving natural tags). We first assume a single sample is obtained per animal for each capture event, and then generalize to the case where multiple samples (such as hair or scat samples) are collected per animal per capture occasion. We introduce methods for estimating population size and, using a simulation study, we show that our new estimators perform well for cases with moderately high capture probabilities or high misidentification rates. In contrast, conventional estimators can seriously overestimate population size when errors due to misidentification are ignored.
C1 [Yoshizaki, Jun] N Carolina State Univ, Biomath Grad Program, Raleigh, NC 27695 USA.
[Yoshizaki, Jun; Pollock, Kenneth H.] N Carolina State Univ, Dept Zool, Raleigh, NC 27695 USA.
[Brownie, Cavell] N Carolina State Univ, Dept Stat, Raleigh, NC 27695 USA.
[Link, William A.] USGS Patuxent Wildlife Res Ctr, Laurel, MD 20708 USA.
RP Yoshizaki, J (reprint author), N Carolina State Univ, Biomath Grad Program, Raleigh, NC 27695 USA.
EM jyoshiz@gmail.com
NR 19
TC 11
Z9 11
U1 0
U2 5
PU SPRINGER
PI DORDRECHT
PA VAN GODEWIJCKSTRAAT 30, 3311 GZ DORDRECHT, NETHERLANDS
SN 1352-8505
EI 1573-3009
J9 ENVIRON ECOL STAT
JI Environ. Ecol. Stat.
PD MAR
PY 2011
VL 18
IS 1
BP 27
EP 55
DI 10.1007/s10651-009-0116-1
PG 29
WC Environmental Sciences; Mathematics, Interdisciplinary Applications;
Statistics & Probability
SC Environmental Sciences & Ecology; Mathematics
GA 728EH
UT WOS:000287856600002
ER
PT J
AU Chang, FC
Simcik, MF
Capel, PD
AF Chang, Feng-Chih
Simcik, Matt F.
Capel, Paul D.
TI OCCURRENCE AND FATE OF THE HERBICIDE GLYPHOSATE AND ITS DEGRADATE
AMINOMETHYLPHOSPHONIC ACID IN THE ATMOSPHERE
SO ENVIRONMENTAL TOXICOLOGY AND CHEMISTRY
LA English
DT Article
DE Atmosphere; Glyphosate; Aminomethylphosphonic acid; Mass budget
ID ORGANOCHLORINE PESTICIDES; DEPOSITION; SOILS; AIR; MISSISSIPPI;
TRANSPORT; WATERS; REGION; AREAS; RAIN
AB This is the first report on the ambient levels of glyphosate, the most widely used herbicide in the United States, and its major degradation product, aminomethylphosphonic acid (AMPA), in air and rain. Concurrent, weekly integrated air particle and rain samples were collected during two growing seasons in agricultural areas in Mississippi and Iowa. Rain was also collected in Indiana in a preliminary phase of the study. The frequency of glyphosate detection ranged from 60 to 100% in both air and rain. The concentrations of glyphosate ranged from < 0.01 to 9.1 ng/m(3) and from < 0.1 to 2.5 mu g/L in air and rain samples, respectively. The frequency of detection and median and maximum concentrations of glyphosate in air were similar or greater to those of the other high-use herbicides observed in the Mississippi River basin, whereas its concentration in rain was greater than the other herbicides. It is not known what percentage of the applied glyphosate is introduced into the air, but it was estimated that up to 0.7% of application is removed from the air in rainfall. Glyphosate is efficiently removed from the air; it is estimated that an average of 97% of the glyphosate in the air is removed by a weekly rainfall >= 30 mm. Environ. Toxicol. Chem. 2011;30:548-555. (C) 2011 SETAC
C1 [Chang, Feng-Chih; Simcik, Matt F.] Univ Minnesota, Sch Publ Hlth, Minneapolis, MN 55455 USA.
[Capel, Paul D.] US Geol Survey, Minneapolis, MN USA.
RP Simcik, MF (reprint author), Univ Minnesota, Sch Publ Hlth, Minneapolis, MN 55455 USA.
EM msimcik@umn.edu
RI Simcik, Matt/K-9390-2015
FU U.S. Geological Survey
FX The authors thank the members of the U.S. Geological Survey offices in
Indiana, Iowa, Mississippi, and Kansas for their support in the field
and laboratory. This research was funded by the U.S. Geological Survey,
National Water-Quality Assessment (NAWQA) Program. Use of brand names in
this report is for identification purposes only and does not constitute
endorsement by the U.S. Geological Survey.
NR 37
TC 21
Z9 27
U1 4
U2 32
PU WILEY-BLACKWELL
PI MALDEN
PA COMMERCE PLACE, 350 MAIN ST, MALDEN 02148, MA USA
SN 0730-7268
J9 ENVIRON TOXICOL CHEM
JI Environ. Toxicol. Chem.
PD MAR
PY 2011
VL 30
IS 3
BP 548
EP 555
DI 10.1002/etc.431
PG 8
WC Environmental Sciences; Toxicology
SC Environmental Sciences & Ecology; Toxicology
GA 728UA
UT WOS:000287898800004
PM 21128261
ER
PT J
AU Lafrancois, BM
Riley, SC
Blehert, DS
Ballmann, AE
AF Lafrancois, Brenda Moraska
Riley, Stephen C.
Blehert, David S.
Ballmann, Anne E.
TI Links between type E botulism outbreaks, lake levels, and surface water
temperatures in Lake Michigan, 1963-2008
SO JOURNAL OF GREAT LAKES RESEARCH
LA English
DT Article
DE Botulism; Lake level; Water temperature; Lake Michigan; Avian mortality
ID LAURENTIAN GREAT-LAKES; CLOSTRIDIUM-BOTULINUM; AVIAN BOTULISM; DISEASE;
FISH; POPULATIONS; PREVALENCE; MORTALITY; CARCASSES; TOXICITY
AB Relationships between large-scale environmental factors and the incidence of type E avian botulism outbreaks in Lake Michigan were examined from 1963 to 2008. Avian botulism outbreaks most frequently occurred in years with low mean annual water levels, and lake levels were significantly lower in outbreak years than in non-outbreak years. Mean surface water temperatures in northern Lake Michigan during the period when type E outbreaks tend to occur (July through September) were significantly higher in outbreak years than in non-outbreak years. Trends in fish populations did not strongly correlate with botulism outbreaks, although botulism outbreaks in the 1960s coincided with high alewife abundance, and recent botulism outbreaks coincided with rapidly increasing round goby abundance. Botulism outbreaks occurred cyclically, and the frequency of outbreaks did not increase over the period of record. Climate change scenarios for the Great Lakes predict lower water levels and warmer water temperatures. As a consequence, the frequency and magnitude of type E botulism outbreaks in the Great lakes may increase. Published by Elsevier B.V. on behalf of International Association for Great lakes Research.
C1 [Riley, Stephen C.] US Geol Survey, Great Lakes Sci Ctr, Ann Arbor, MI 48105 USA.
[Lafrancois, Brenda Moraska] Natl Pk Serv, St Croix Watershed Res Stn, Marine St Croix, MN 55047 USA.
[Blehert, David S.; Ballmann, Anne E.] US Geol Survey, Natl Wildlife Hlth Ctr, Madison, WI 53711 USA.
RP Riley, SC (reprint author), US Geol Survey, Great Lakes Sci Ctr, 1451 Green Rd, Ann Arbor, MI 48105 USA.
EM brenda_moraska_lafrancois@nps.gov; sriley@usgs.gov; dblehert@usgs.gov;
aballmann@usgs.gov
NR 48
TC 16
Z9 17
U1 5
U2 55
PU ELSEVIER SCI LTD
PI OXFORD
PA THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, OXON, ENGLAND
SN 0380-1330
J9 J GREAT LAKES RES
JI J. Gt. Lakes Res.
PD MAR
PY 2011
VL 37
IS 1
BP 86
EP 91
DI 10.1016/j.jglr.2010.10.003
PG 6
WC Environmental Sciences; Limnology; Marine & Freshwater Biology
SC Environmental Sciences & Ecology; Marine & Freshwater Biology
GA 729KL
UT WOS:000287948400010
ER
PT J
AU Hondorp, DW
Pothoven, SA
Brandt, SB
AF Hondorp, Darryl W.
Pothoven, Steven A.
Brandt, Stephen B.
TI Feeding selectivity of slimy sculpin Cottus cognatus and deepwater
sculpin Myoxocephalus thompsonii in southeast Lake Michigan:
Implications for species coexistence
SO JOURNAL OF GREAT LAKES RESEARCH
LA English
DT Article
DE Sculpin; Prey selection; Community ecology; Lake Michigan
ID MYSIS-RELICTA; DEPTH DISTRIBUTION; AMPHIPOD DIPOREIA; DIET; ONTARIO;
PREY; COMMUNITY; FISHES; HURON; FOOD
AB Feeding selectivity was compared between slimy sculpin Cottus cognatus and deepwater sculpin Myoxocephalus thompsonii collected from southeast Lake Michigan during 1999-2002 to evaluate the hypothesis that differential prey selection contributes to long-term coexistence of these species. Study results indicated that slimy and deepwater sculpin select different prey types and sizes. Selection for the shrimp-like crustacean Mysis diluviana was consistently greater for deepwater sculpin than for slimy sculpin, whereas selection for the amphipod Diporeia spp. was higher for slimy sculpin than for deepwater sculpin when Mysis was the only other available prey type. Slimy sculpin also exhibited higher selectivity for chironomids (order Diptera, family Chironomidae) compared with deepwater sculpin. Patterns in food resource partitioning were consistent between sampling periods covering different locations, seasons and depths, as well as between locations with varying levels of Diporeia availability. This consistency suggests (1) that differences in food use by the two species are associated with intrinsic differences in food preferences or feeding behaviors and (2) that Diporeia declines had not fundamentally altered the resource partitioning dynamics of the two species as of 2002. The results also indicated that slimy and deepwater sculpin can partition food resources on the basis of prey size since deepwater sculpin tended to select larger Diporeia than slimy sculpin. Differences in prey selection may mediate competitive interactions between slimy and deepwater sculpin directly by reducing diet overlap in areas of sympatry or indirectly by causing these fish to select different depth habitats. Published by Elsevier B.V. on behalf of International Association for Great Lakes Research.
C1 [Hondorp, Darryl W.] Univ Michigan, Cooperat Inst Limnol & Ecosyst Res, Ann Arbor, MI 48108 USA.
[Hondorp, Darryl W.] NOAA GLERL, Ann Arbor, MI 48108 USA.
[Pothoven, Steven A.] NOAA GLERL, Lake Michigan Field Stn, Muskegon, MI 49441 USA.
[Brandt, Stephen B.] Oregon State Univ, Corvallis, OR 97331 USA.
RP Hondorp, DW (reprint author), US Geol Survey, Great Lakes Sci Ctr, 1451 Green Rd, Ann Arbor, MI 48105 USA.
EM dhondorp@usgs.gov; steve.pothoven@noaa.gov;
stephen.brandt@oregonstate.edu
OI Pothoven, Steven/0000-0002-7992-5422
FU Great Lakes Fishery Trust
FX Assistance in the field and laboratory provided by the crews of the RV
Shenehon and RV Laurentian, A. Neiman, C. Kingsbury, C. Hwang, H.
Gunder, B. Hice, and K. Downey. Funding was provided by the Great Lakes
Fishery Trust. This manuscript benefited from comments made by C.
Madenjian and K. Maloney. This is NOAA-GLERL contribution 1581.
NR 46
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U1 2
U2 23
PU ELSEVIER SCI LTD
PI OXFORD
PA THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, OXON, ENGLAND
SN 0380-1330
J9 J GREAT LAKES RES
JI J. Gt. Lakes Res.
PD MAR
PY 2011
VL 37
IS 1
BP 165
EP 172
DI 10.1016/j.jglr.2010.11.010
PG 8
WC Environmental Sciences; Limnology; Marine & Freshwater Biology
SC Environmental Sciences & Ecology; Marine & Freshwater Biology
GA 729KL
UT WOS:000287948400019
ER
PT J
AU Grobler, JP
Jones, JW
Johnson, NA
Neves, RJ
Hallerman, EM
AF Grobler, J. Paul
Jones, Jess W.
Johnson, Nathan A.
Neves, Richard J.
Hallerman, Eric M.
TI Homogeneity at Nuclear Microsatellite Loci Masks Mitochondrial Haplotype
Diversity in the Endangered Fanshell Pearlymussel (Cyprogenia stegaria)
SO JOURNAL OF HEREDITY
LA English
DT Article
DE Cyprogenia stegaria; endangered species; genetic structure;
microsatellites; mtDNA; Unionidae
ID FRESH-WATER MUSSEL; EVOLUTIONARILY-SIGNIFICANT-UNITS; BIOLOGICAL
DIVERSITY; GENETIC DIVERSITY; MOLECULAR SYSTEMATICS; CONSERVATION
GENETICS; POPULATION-STRUCTURE; ABERTI BIVALVIA; LIFE-HISTORY; UNIONIDAE
AB We report on multiple patterns of differentiation and connectivity in the fanshell pearlymussel (Cyprogenia stegaria), based on different markers. Knowledge of genetic variation and genetic connectivity among remaining populations of this federally endangered species is needed to initiate implementation of the species recovery plan. We collected tissue samples from 96 specimens from the Green, Rolling Fork, and Licking Rivers, tributaries to the Ohio River, and the Clinch River, a tributary to the Tennessee River, providing broad coverage of the current distributional range of the species. Results from 7 nuclear DNA microsatellite markers suggested minimal population-level differentiation, whereas a mitochondrial DNA (mtDNA) marker (ND1) exhibited significant differentiation between C. stegaria in the Clinch River and the Ohio River populations. The ND1 data also confirm the existence of 2 distinct mtDNA lineages in the genus that transcends species boundaries. Further analyses suggest that the disproportionally strong signal from 2 very divergent ND1 lineages possibly masks finer-grained structure in the Ohio River population, based on one of the mtDNA lineages only. We recommend further sampling to confirm the absence of one lineage from the upper Clinch River drainage and suggest that provisional management guidelines should limit reciprocal exchanges among C. stegaria populations from the Clinch River and those in the Ohio River system.
C1 [Grobler, J. Paul; Jones, Jess W.; Johnson, Nathan A.; Neves, Richard J.; Hallerman, Eric M.] Virginia Polytech Inst & State Univ, Dept Fisheries & Wildlife Sci, Blacksburg, VA 24061 USA.
[Grobler, J. Paul] Univ Orange Free State, Dept Genet, Bloemfontein, South Africa.
[Jones, Jess W.] US Fish & Wildlife Serv, Blacksburg, VA USA.
RP Grobler, JP (reprint author), Virginia Polytech Inst & State Univ, Dept Fisheries & Wildlife Sci, Blacksburg, VA 24061 USA.
EM groblerjp@ufs.ac.za
OI Johnson, Nathan/0000-0001-5167-1988
FU U.S. Geological Survey Biological Resources Division [00HQRU1573];
Virginia Tech Office of Sponsored Programs [432622]
FX U.S. Geological Survey Biological Resources Division (00HQRU1573, Work
Order 92); Virginia Tech Office of Sponsored Programs Project (432622).
NR 50
TC 2
Z9 2
U1 1
U2 8
PU OXFORD UNIV PRESS INC
PI CARY
PA JOURNALS DEPT, 2001 EVANS RD, CARY, NC 27513 USA
SN 0022-1503
J9 J HERED
JI J. Hered.
PD MAR-APR
PY 2011
VL 102
IS 2
BP 196
EP 206
DI 10.1093/jhered/esq120
PG 11
WC Evolutionary Biology; Genetics & Heredity
SC Evolutionary Biology; Genetics & Heredity
GA 723HF
UT WOS:000287496700006
PM 21273215
ER
PT J
AU Graves, R
Jordan, TH
Callaghan, S
Deelman, E
Field, E
Juve, G
Kesselman, C
Maechling, P
Mehta, G
Milner, K
Okaya, D
Small, P
Vahi, K
AF Graves, Robert
Jordan, Thomas H.
Callaghan, Scott
Deelman, Ewa
Field, Edward
Juve, Gideon
Kesselman, Carl
Maechling, Philip
Mehta, Gaurang
Milner, Kevin
Okaya, David
Small, Patrick
Vahi, Karan
TI CyberShake: A Physics-Based Seismic Hazard Model for Southern California
SO PURE AND APPLIED GEOPHYSICS
LA English
DT Article
DE Physics-based earthquake simulation; seismic hazard; rupture
directivity; 3D basin response
ID AVERAGE HORIZONTAL COMPONENT; GROUND-MOTION PREDICTION; RESPONSE
SPECTRA; EARTHQUAKE; FAULT; TOMOGRAPHY; PERIODS; PGV
AB CyberShake, as part of the Southern California Earthquake Center's (SCEC) Community Modeling Environment, is developing a methodology that explicitly incorporates deterministic source and wave propagation effects within seismic hazard calculations through the use of physics-based 3D ground motion simulations. To calculate a waveform-based seismic hazard estimate for a site of interest, we begin with Uniform California Earthquake Rupture Forecast, Version 2.0 (UCERF2.0) and identify all ruptures within 200 km of the site of interest. We convert the UCERF2.0 rupture definition into multiple rupture variations with differing hypocenter locations and slip distributions, resulting in about 415,000 rupture variations per site. Strain Green Tensors are calculated for the site of interest using the SCEC Community Velocity Model, Version 4 (CVM4), and then, using reciprocity, we calculate synthetic seismograms for each rupture variation. Peak intensity measures are then extracted from these synthetics and combined with the original rupture probabilities to produce probabilistic seismic hazard curves for the site. Being explicitly site-based, CyberShake directly samples the ground motion variability at that site over many earthquake cycles (i.e., rupture scenarios) and alleviates the need for the ergodic assumption that is implicitly included in traditional empirically based calculations. Thus far, we have simulated ruptures at over 200 sites in the Los Angeles region for ground shaking periods of 2 s and longer, providing the basis for the first generation CyberShake hazard maps. Our results indicate that the combination of rupture directivity and basin response effects can lead to an increase in the hazard level for some sites, relative to that given by a conventional Ground Motion Prediction Equation (GMPE). Additionally, and perhaps more importantly, we find that the physics-based hazard results are much more sensitive to the assumed magnitude-area relations and magnitude uncertainty estimates used in the definition of the ruptures than is found in the traditional GMPE approach. This reinforces the need for continued development of a better understanding of earthquake source characterization and the constitutive relations that govern the earthquake rupture process.
C1 [Graves, Robert] URS Corp, Los Angeles, CA USA.
[Jordan, Thomas H.; Callaghan, Scott; Juve, Gideon; Maechling, Philip; Mehta, Gaurang; Milner, Kevin; Okaya, David; Small, Patrick; Vahi, Karan] USC, Los Angeles, CA USA.
[Deelman, Ewa; Kesselman, Carl] USC ISI, Los Angeles, CA USA.
[Field, Edward] USGS, Golden, CO USA.
RP Graves, R (reprint author), URS Corp, Los Angeles, CA USA.
EM robert_graves@urscorp.com
RI Graves, Robert/B-2401-2013;
OI Kesselman, Carl/0000-0003-0917-1562
FU SCEC under NSF [EAR-0623704, OCI-0749313]
FX Funding for this work was provided by SCEC under NSF grants EAR-0623704
and OCI-0749313. Computational resources were provided by USC's Center
for High Performance Computing and Communications
(http://www.usc.edu/hpcc) and through NSF's TeraGrid Science Gateways
program (http://www.teragrid.org) using facilities at the National
Center for Supercomputing Applications (NCSA), the San Diego
Supercomputer Center (SDSC) and the Texas Advanced Computer Center
(TACC) under agreement with the SCEC CME project. This is SCEC
contribution 1426.
NR 38
TC 51
Z9 52
U1 1
U2 16
PU BIRKHAUSER VERLAG AG
PI BASEL
PA VIADUKSTRASSE 40-44, PO BOX 133, CH-4010 BASEL, SWITZERLAND
SN 0033-4553
J9 PURE APPL GEOPHYS
JI Pure Appl. Geophys.
PD MAR
PY 2011
VL 168
IS 3-4
BP 367
EP 381
DI 10.1007/s00024-010-0161-6
PG 15
WC Geochemistry & Geophysics
SC Geochemistry & Geophysics
GA 723JS
UT WOS:000287503400001
ER
PT J
AU Griffin, DW
Gonzalez, C
Teigell, N
Petrosky, T
Northup, DE
Lyles, M
AF Griffin, Dale W.
Gonzalez, Cristina
Teigell, Nuria
Petrosky, Terry
Northup, Diana E.
Lyles, Mark
TI Observations on the use of membrane filtration and liquid impingement to
collect airborne microorganisms in various atmospheric environments
SO AEROBIOLOGIA
LA English
DT Article
DE Bacteria; Fungi; Methods; Membrane filtration; Liquid impingement;
Aeromicrobiology; Microbiology
ID SAMPLING TIME; DESERT DUST; BACTERIA; ENUMERATION; AIR; TRANSPORT;
SURVIVAL; VIRUSES; FILTER; SPORES
AB The influence of sample-collection-time on the recovery of culturable airborne microorganisms using a low-flow-rate membrane-filtration unit and a high-flow-rate liquid impinger were investigated. Differences in recoveries were investigated in four different atmospheric environments, one mid-oceanic at an altitude of similar to 10.0 m, one on a mountain top at an altitude of similar to 3,000.0 m, one at similar to 1.0 m altitude in Tallahassee, Florida, and one at similar to 1.0 m above ground in a subterranean-cave. Regarding use of membrane filtration, a common trend was observed: the shorter the collection period, the higher the recovery of culturable bacteria and fungi. These data also demonstrated that lower culturable counts were common in the more remote mid-oceanic and mountain-top atmospheric environments with bacteria, fungi, and total numbers averaging (by sample time or method categories) < 3.0 colony-forming units (CFU) m(-3). At the Florida and subterranean sites, the lowest average count noted was 3.5 bacteria CFU m(-3), and the highest averaged 140.4 total CFU m(-3). When atmospheric temperature allowed use, the high-volume liquid impinger utilized in this study resulted in much higher recoveries, as much as 10x greater in a number of the categories (bacterial, fungal, and total CFU). Together, these data illustrated that (1) the high-volume liquid impinger is clearly superior to membrane filtration for aeromicrobiology studies if start-up costs are not an issue and temperature permits use; (2) although membrane filtration is more cost friendly and has a 'typically' wider operational range, its limits include loss of cell viability with increased sample time and issues with effectively extracting nucleic acids for community-based analyses; (3) the ability to recover culturable microorganisms is limited in 'extreme' atmospheric environments and thus the use of a 'limited' methodology in these environments must be taken into account; and (4) the atmosphere culls, i.e., everything is not everywhere.
C1 [Griffin, Dale W.] US Geol Survey, Geol Discipline, Tallahassee, FL 32303 USA.
[Gonzalez, Cristina; Teigell, Nuria] Univ La Laguna, Univ Inst Trop Dis & Publ Hlth, Tenerife, Canary Islands, Spain.
[Petrosky, Terry] US Geol Survey, Water Resources Discipline, Tallahassee, FL 32303 USA.
[Northup, Diana E.] Univ New Mexico, Albuquerque, NM 87131 USA.
[Lyles, Mark] USN, Res Program Integrat & Mission Dev, Bur Med & Surg, Washington, DC 20372 USA.
RP Griffin, DW (reprint author), US Geol Survey, Geol Discipline, 2639 N Monroe St,Suite A200, Tallahassee, FL 32303 USA.
EM dgriffin@usgs.gov
NR 36
TC 20
Z9 20
U1 7
U2 23
PU SPRINGER
PI DORDRECHT
PA VAN GODEWIJCKSTRAAT 30, 3311 GZ DORDRECHT, NETHERLANDS
SN 0393-5965
J9 AEROBIOLOGIA
JI Aerobiologia
PD MAR
PY 2011
VL 27
IS 1
BP 25
EP 35
DI 10.1007/s10453-010-9173-z
PG 11
WC Biology; Environmental Sciences
SC Life Sciences & Biomedicine - Other Topics; Environmental Sciences &
Ecology
GA 716AN
UT WOS:000286937300003
ER
PT J
AU Pothoven, SA
Hondorp, DW
Nalepa, TF
AF Pothoven, S. A.
Hondorp, D. W.
Nalepa, T. F.
TI Declines in deepwater sculpin Myoxocephalus thompsonii energy density
associated with the disappearance of Diporeia spp. in lakes Huron and
Michigan
SO ECOLOGY OF FRESHWATER FISH
LA English
DT Article
DE glacial relict; deepwater sculpin; Diporeia; Mysis; Great Lakes
ID WHITEFISH COREGONUS-CLUPEAFORMIS; NEARCTIC GLACIAL RELICT; LONG-TERM
TRENDS; DREISSENID MUSSELS; AMPHIPOD DIPOREIA; ONTARIO; FISH; COMMUNITY;
DIET; POPULATIONS
AB The deepwater sculpin Myoxocephalus thompsonii is a glacial relict in the Laurentian Great Lakes that primarily consumes two glacial relict crustaceans, Mysis relicta and Diporeia spp. Deepwater sculpin were collected in Lake Michigan off Little Sable Point (in 2001) and Muskegon, Michigan (in 2001 and 2009), and in Lake Huron off Harbor Beach, Michigan (in 2007) for energy density and diet analyses. These sites and years represented differences in available prey. In Lake Michigan, energy densities of deepwater sculpin in 2001 were similar to those reported in 1969-1971. In contrast, energy content declined at least 26% at Muskegon between 2001 and 2009. Overall, energy density was 31-34% higher at a site with abundant Diporeia spp. compared with two sites without Diporeia spp. Deepwater sculpin diets consisted primarily of M. relicta at all sites, but included 10-17% (dry mass) Diporeia spp. at sites where this crustacean was still abundant. Food biomass in stomachs was higher at sites with abundant Diporeia spp. than at those without Diporeia spp. Deepwater sculpin energy density and food biomass in stomachs were similar between two sites without Diporeia spp. despite differences in abundance of remaining prey, M. relicta. Declines in deepwater sculpin energy density suggest the potential for further effects on other species and changes in the flow of energy through the food web of the Great Lakes.
C1 [Pothoven, S. A.] NOAA, Great Lakes Environm Res Lab, Muskegon, MI 49441 USA.
[Hondorp, D. W.] US Geol Survey, Great Lakes Sci Ctr, Ann Arbor, MI USA.
[Nalepa, T. F.] NOAA, Great Lakes Environm Res Lab, Ann Arbor, MI 48105 USA.
RP Pothoven, SA (reprint author), NOAA, Great Lakes Environm Res Lab, 1431 Beach St, Muskegon, MI 49441 USA.
EM steve.pothoven@noaa.gov
OI Pothoven, Steven/0000-0002-7992-5422
NR 40
TC 11
Z9 11
U1 1
U2 18
PU WILEY-BLACKWELL
PI MALDEN
PA COMMERCE PLACE, 350 MAIN ST, MALDEN 02148, MA USA
SN 0906-6691
J9 ECOL FRESHW FISH
JI Ecol. Freshw. Fish
PD MAR
PY 2011
VL 20
IS 1
BP 14
EP 22
DI 10.1111/j.1600-0633.2010.00447.x
PG 9
WC Fisheries; Marine & Freshwater Biology
SC Fisheries; Marine & Freshwater Biology
GA 720VX
UT WOS:000287311900003
ER
PT J
AU Maloney, KO
Weller, DE
AF Maloney, Kelly O.
Weller, Donald E.
TI Anthropogenic disturbance and streams: land use and land-use change
affect stream ecosystems via multiple pathways
SO FRESHWATER BIOLOGY
LA English
DT Article
DE benthic macroinvertebrates; land use legacy; past land use; stream water
chemistry; structural equation modelling (SEM)
ID LARGE WOODY DEBRIS; COMMUNITY STRUCTURE; HEADWATER STREAMS; ECOLOGICAL
THEORY; CURRENT KNOWLEDGE; RIPARIAN BUFFERS; SOIL PROPERTIES;
UNITED-STATES; RIVER; CATCHMENT
AB 1. Ecosystems are strongly influenced by land use practices. However, identifying the mechanisms behind these influences is complicated by the many potential pathways (often indirect) between land use and ecosystems and by the long-lasting effects of past land use. To support ecosystem restoration and conservation efforts, we need to better understand these indirect and lasting effects.
2. We constructed structural equation models (SEM) to evaluate the direct and indirect effects of contemporary (2002) land use (agriculture and development) and change in land use from 1952 to 2002 on present-day streams (n = 190) in Maryland, U.S.A. Additional variables examined included site location, system size, altitude, per cent sand in soils, riparian condition, habitat quality, stream water NO(3)-N and benthic macroinvertebrate and fish measures of stream condition. Our first SEM (2002 Land Use) included the proportions of contemporary agriculture and development in catchments in the model. The second SEM (Land Use Change) included five measures of land use change (proportion agricultural in both times, developed in both times, agricultural in 1952 and developed in 2002, forested in 1952 and developed in 2002 and agricultural in 1952 and forested in 2002).
3. The data set fit both SEMs well. The 2002 Land Use model explained 71% of variation in NO(3)-N and 55%, 42% and 38% of variation in riffle quality, macroinvertebrate condition and fish condition, respectively. The Land Use Change model explained similar amounts of variation in NO(3)-N (R2 = 0.72), riffle quality (R2 = 0.57) and macroinvertebrate condition (R2 = 0.44) but slightly more variation in fish condition (R2 = 0.43).
4. Both models identified pathways through which landscape variables affect stream responses, including negative direct effects of latitude on macroinvertebrate and fish conditions and positive direct and indirect effects of altitude on NO(3)-N, riffle quality and macroinvertebrate and fish conditions. The 2002 Land Use model showed contemporary development and agriculture had positive total effects on NO(3)-N (both through direct pathways); contemporary development had negative effects on macroinvertebrate condition. The Land Use Change model showed that contemporary developed land that was forested in 1952 had no effects on NO(3)-N; current developed land that was developed or agricultural in 1952 showed positive effects on NO(3)-N. Forests that were agricultural in 1952 had negative effects on NO(3)-N, suggesting reduced NO(3)-N export with reforestation. The Land Use Change model also showed negative total effects of all types of contemporary developed land (developed, agricultural or forested in 1952) on benthic condition. Developed land that was forested in 1952 had negative effects on fish condition. Forest sites that were agricultural in 1952 had negative effects on fish and macroinvertebrate conditions, suggesting a long-term imprint of abandoned agriculture in stream communities.
5. Our analyses (i) identified multiple indirect effects of contemporary land use on streams, (ii) showed that current land uses with different land use histories can exhibit different effects on streams and (iii) demonstrated an imprint of land use lasting > 50 years. Knowledge of these indirect and long-term effects of land use will help to conserve and restore streams.
C1 [Maloney, Kelly O.; Weller, Donald E.] Smithsonian Environm Res Ctr, Edgewater, MD 21037 USA.
RP Maloney, KO (reprint author), US Geol Survey, Leetown Sci Ctr, No Appalachian Res Lab, 176 Straight Run Rd, Wellsboro, PA 16901 USA.
EM kmaloney@usgs.gov
OI Weller, Donald/0000-0002-7629-5437
FU Smithsonian Post-Doctoral Research Fellowship
FX We thank the Maryland Department of Natural Resources for providing the
MBSS data, the Maryland Department of Transportation for providing the
2002 land use data, Matt Baker for catchment boundaries and Eric Lind,
Darryl Hondorp, Lori Davias, John Parker, Ariana Sutton-Grier and two
anonymous reviewers for constructive comments on the manuscript. The
project was funded by a Smithsonian Post-Doctoral Research Fellowship
awarded to KOM.
NR 77
TC 25
Z9 26
U1 8
U2 94
PU WILEY-BLACKWELL
PI MALDEN
PA COMMERCE PLACE, 350 MAIN ST, MALDEN 02148, MA USA
SN 0046-5070
J9 FRESHWATER BIOL
JI Freshw. Biol.
PD MAR
PY 2011
VL 56
IS 3
BP 611
EP 626
DI 10.1111/j.1365-2427.2010.02522.x
PG 16
WC Marine & Freshwater Biology
SC Marine & Freshwater Biology
GA 718AV
UT WOS:000287092900016
ER
PT J
AU Banerjee, A
Person, M
Hofstra, A
Sweetkind, D
Cohen, D
Sabin, A
Unruh, J
Zyvoloski, G
Gable, CW
Crossey, L
Karlstrom, K
AF Banerjee, Amlan
Person, Mark
Hofstra, Albert
Sweetkind, Donald
Cohen, Denis
Sabin, Andrew
Unruh, Jeff
Zyvoloski, George
Gable, Carl W.
Crossey, Laura
Karlstrom, Karl
TI Deep permeable fault-controlled helium transport and limited mantle flux
in two extensional geothermal systems in the Great Basin, United States
SO GEOLOGY
LA English
DT Article
ID NEVADA; CALIFORNIA; TECTONICS; ISOTOPES; BEOWAWE; DEPOSIT; ORIGIN;
FLUIDS; AREA; FLOW
AB This study assesses the relative importance of deeply circulating meteoric water and direct mantle fluid inputs on near-surface He-3/He-4 anomalies reported at the Coso and Beowawe geothermal fields of the western United States. The depth of meteoric fluid circulation is a critical factor that controls the temperature, extent of fluid-rock isotope exchange, and mixing with deeply sourced fluids containing mantle volatiles. The influence of mantle fluid flux on the reported helium anomalies appears to be negligible in both systems. This study illustrates the importance of deeply penetrating permeable fault zones (10(-12) to 10(-15) m(2)) in focusing groundwater and mantle volatiles with high He-3/He-4 ratios to shallow crustal levels. These continental geothermal systems are driven by free convection.
C1 [Banerjee, Amlan; Person, Mark] New Mexico Inst Min & Technol, Dept Earth & Environm Sci, Socorro, NM 87801 USA.
[Hofstra, Albert; Sweetkind, Donald] US Geol Survey, Denver Fed Ctr, Denver, CO 80225 USA.
[Cohen, Denis] Iowa State Univ, Dept Geol & Atmospher Sci, Ames, IA 50011 USA.
[Sabin, Andrew] USN, Geothermal Program Off, China Lake, CA 93555 USA.
[Unruh, Jeff] William Lettis & Associates, Walnut Creek, CA 94596 USA.
[Zyvoloski, George; Gable, Carl W.] Los Alamos Natl Lab, Computat Earth Sci Grp, Los Alamos, NM 87545 USA.
[Crossey, Laura; Karlstrom, Karl] Univ New Mexico, Dept Earth & Planetary Sci, Albuquerque, NM 87131 USA.
RP Banerjee, A (reprint author), New Mexico Inst Min & Technol, Dept Earth & Environm Sci, Socorro, NM 87801 USA.
EM mperson@nmt.edu
RI Gable, Carl/B-4689-2011; Crossey, Laura/C-2033-2008; Cohen,
Denis/P-2015-2016; Banerjee, Amlan/P-9658-2016;
OI Gable, Carl/0000-0001-7063-0815; Crossey, Laura/0000-0001-6237-8023;
Cohen, Denis/0000-0002-8262-9798; Banerjee, Amlan/0000-0002-2065-1391;
Sweetkind, Donald/0000-0003-0892-4796
NR 21
TC 7
Z9 7
U1 0
U2 20
PU GEOLOGICAL SOC AMER, INC
PI BOULDER
PA PO BOX 9140, BOULDER, CO 80301-9140 USA
SN 0091-7613
J9 GEOLOGY
JI Geology
PD MAR
PY 2011
VL 39
IS 3
BP 195
EP 198
DI 10.1130/G31557.1
PG 4
WC Geology
SC Geology
GA 721SI
UT WOS:000287374900003
ER
PT J
AU Elders, WA
Frioleifsson, GO
Zierenberg, RA
Pope, EC
Mortensen, AK
Guomundsson, A
Lowenstern, JB
Marks, NE
Owens, L
Bird, DK
Reed, M
Olsen, NJ
Schiffman, P
AF Elders, Wilfred A.
Frioleifsson, Guomundur O.
Zierenberg, Robert A.
Pope, Emily C.
Mortensen, Anette K.
Guomundsson, Asgrimur
Lowenstern, Jacob B.
Marks, Naomi E.
Owens, Lara
Bird, Dennis K.
Reed, Mark
Olsen, Nellie J.
Schiffman, Peter
TI Origin of a rhyolite that intruded a geothermal well while drilling at
the Krafla volcano, Iceland
SO GEOLOGY
LA English
DT Article
ID ISOTOPE; BASALTS; YELLOWSTONE; CONSTRAINTS; REYKJANES; SYSTEMS; BENEATH;
FLUIDS; PLUME
AB Magma flowed into an exploratory geothermal well at 2.1 km depth being drilled in the Krafla central volcano in Iceland, creating a unique opportunity to study rhyolite magma in situ in a basaltic environment. The quenched magma is a partly vesicular, sparsely phyric, glass containing similar to 1.8% of dissolved volatiles. Based on calculated H2O-CO2 saturation pressures, it degassed at a pressure intermediate between hydrostatic and lithostatic, and geothermometry indicates that the crystals in the melt formed at similar to 900 degrees C. The glass shows no signs of hydrothermal alteration, but its hydrogen and oxygen isotopic ratios are much lower than those of typical mantle-derived magmas, indicating that this rhyolite originated by anhydrous mantle-derived magma assimilating partially melted hydrothermally altered basalts.
C1 [Elders, Wilfred A.] Univ Calif Riverside, Dept Earth Sci, Riverside, CA 92521 USA.
[Frioleifsson, Guomundur O.] HS Orka Hf, IS-260 Reykjanebaer, Iceland.
[Zierenberg, Robert A.; Marks, Naomi E.; Schiffman, Peter] Univ Calif Davis, Dept Geol, Davis, CA 95616 USA.
[Pope, Emily C.; Bird, Dennis K.; Olsen, Nellie J.] Stanford Univ, Dept Geol & Environm Sci, Stanford, CA 94305 USA.
[Mortensen, Anette K.] Iceland GeoSurvey ISOR, IS-108 Reykjavik, Iceland.
[Guomundsson, Asgrimur] Landsvirkjun Power, IS-103 Reykjavik, Iceland.
[Lowenstern, Jacob B.] US Geol Survey, Menlo Pk, CA 94025 USA.
[Owens, Lara] New Mexico Inst Min & Technol, Dept Earth & Environm Sci, Socorro, NM 87801 USA.
[Reed, Mark] Univ Oregon, Dept Geol Sci, Eugene, OR 97403 USA.
RP Elders, WA (reprint author), Univ Calif Riverside, Dept Earth Sci, Riverside, CA 92521 USA.
EM wilfred.elders@ucr.edu
RI Pope, Emily/A-6594-2013; Zierenberg, Robert/F-9329-2012;
OI Pope, Emily/0000-0001-8367-9351; Zierenberg, Robert/0000-0001-9384-7355;
Lowenstern, Jacob/0000-0003-0464-7779
FU International Continental Scientific Drilling Program; U.S. National
Science Foundation [EAR 0507625, EAR 0507518, EAR 0506882, EAR 0507181]
FX We are grateful to Landsvirkjun Power Company and to the Iceland Deep
Drilling Project (IDDP) consortium for making this study possible. John
Eichelberger and two anonymous reviewers provided insightful reviews of
an earlier version of this paper. Financial support came from the
International Continental Scientific Drilling Program and the U.S.
National Science Foundation (grant EAR 0507625 to Elders, EAR 0507518 to
Zierenberg and Schiffman, EAR 0506882 to Bird, and EAR 0507181 to Reed).
NR 29
TC 25
Z9 25
U1 2
U2 23
PU GEOLOGICAL SOC AMER, INC
PI BOULDER
PA PO BOX 9140, BOULDER, CO 80301-9140 USA
SN 0091-7613
J9 GEOLOGY
JI Geology
PD MAR
PY 2011
VL 39
IS 3
BP 231
EP 234
DI 10.1130/G31393.1
PG 4
WC Geology
SC Geology
GA 721SI
UT WOS:000287374900012
ER
PT J
AU Toke, NA
Arrowsmith, JR
Rymer, MJ
Landgraf, A
Haddad, DE
Busch, M
Coyan, J
Hannah, A
AF Toke, Nathan A.
Arrowsmith, J. Ramon
Rymer, Michael J.
Landgraf, Angela
Haddad, David E.
Busch, Melanie
Coyan, Joshua
Hannah, Alexander
TI Late Holocene slip rate of the San Andreas fault and its accommodation
by creep and moderate-magnitude earthquakes at Parkfield, California
SO GEOLOGY
LA English
DT Article
ID SURFACE SLIP; SEGMENT; SYSTEM; ARRAYS
AB Investigation of a right-laterally offset channel at the Miller's Field paleoseismic site yields a late Holocene slip rate of 26.2 +6.4/-4.3 mm/yr (1 sigma) for the main trace of the San Andreas fault at Parkfield, California. This is the first well-documented geologic slip rate between the Carrizo and creeping sections of the San Andreas fault. This rate is lower than Holocene measurements along the Carrizo Plain and rates implied by far-field geodetic measurements (similar to 35 mm/yr). However, the rate is consistent with historical slip rates, measured to the northwest, along the creeping section of the San Andreas fault (<30 mm/yr). The paleoseismic exposures at the Miller's Field site reveal a pervasive fabric of clay shear bands, oriented clockwise oblique to the San Andreas fault strike and extending into the uppermost stratigraphy. This fabric is consistent with dextral aseismic creep and observations of surface slip from the 28 September 2004 M6 Parkfield earthquake. Together, this slip rate and deformation fabric suggest that the historically observed San Andreas fault slip behavior along the Parkfield section has persisted for at least a millennium, and that significant slip is accommodated by structures in a zone beyond the main San Andreas fault trace.
C1 [Toke, Nathan A.; Arrowsmith, J. Ramon; Haddad, David E.; Busch, Melanie; Coyan, Joshua] Arizona State Univ, Sch Earth & Space Explorat, Tempe, AZ 85287 USA.
[Rymer, Michael J.] US Geol Survey, Menlo Pk, CA 94025 USA.
[Landgraf, Angela] Univ Potsdam, Inst Erd & Umweltwissensch, D-14476 Potsdam, Germany.
[Hannah, Alexander] Calif State Univ Northridge, Dept Geol Sci, Northridge, CA 91330 USA.
RP Toke, NA (reprint author), Arizona State Univ, Sch Earth & Space Explorat, Tempe, AZ 85287 USA.
FU National Earthquake Hazards Reduction Program [07HQGR0094]; Southern
California Earthquake Center (SCEC) [1452]; U.S. National Science
Foundation (NSF); U.S. Geological Survey (USGS); NSF [EAR-00310357, DGE
0504248]; German Academic Exchange Service [DAAD-D/07/42739]
FX We thank J. Tinsley, D. Ponti, and three anonymous reviewers for help
improving this manuscript. We thank J. Zechar for slip-rate probability
density discussion, and T. Fumal for visiting the site. The 2007
campaign was supported by National Earthquake Hazards Reduction Program
Grant 07HQGR0094 and the Southern California Earthquake Center (SCEC
Contribution 1452). The SCEC is funded by the U.S. National Science
Foundation (NSF) and the U.S. Geological Survey (USGS). Our 2004 work
was funded by NSF grant EAR-00310357. The NSF Integrative Graduate
Education and Research Traineeship (IGERT) in Urban Ecology grant DGE
0504248 also supported Toke. Landgraf's expertise was courtesy of German
Academic Exchange Service grant DAAD-D/07/42739. Measurement of offset
was enhanced by B4 Lidar (http://www.earthsciences.osu.edu/b4; Ohio
State University, USGS, National Center for Airborne Laser Mapping,
UNAVCO Inc., other volunteers) data, which were processed by
OpenTopography (http://www.opentopography.org.)
NR 19
TC 16
Z9 16
U1 0
U2 4
PU GEOLOGICAL SOC AMER, INC
PI BOULDER
PA PO BOX 9140, BOULDER, CO 80301-9140 USA
SN 0091-7613
J9 GEOLOGY
JI Geology
PD MAR
PY 2011
VL 39
IS 3
BP 243
EP 246
DI 10.1130/G31498.1
PG 4
WC Geology
SC Geology
GA 721SI
UT WOS:000287374900015
ER
PT J
AU Houghton, BF
Swanson, DA
Carey, RJ
Rausch, J
Sutton, AJ
AF Houghton, B. F.
Swanson, D. A.
Carey, R. J.
Rausch, J.
Sutton, A. J.
TI Pigeonholing pyroclasts: Insights from the 19 March 2008 explosive
eruption of Kilauea volcano
SO GEOLOGY
LA English
DT Article
ID NEW-ZEALAND; DEPOSITS; FRAGMENTATION; STROMBOLI; HAWAII; FALL
AB We think, conventionally, of volcanic explosive eruptions as being triggered in one of two ways: by release and expansion of volatiles dissolved in the ejected magma (magmatic explosions) or by transfer of heat from magma into an external source of water (phreatic or phreatomagmatic explosions). We document here an event where neither magma nor an external water source was involved in explosive activity at Kilauea. Instead, the eruption was powered by the expansion of decoupled magmatic volatiles released from deeper magma, which was not ejected by the eruption, and the trigger was a collapse of near-surface wall rocks that then momentarily blocked that volatile flux. Mapping of the advected fall deposit a day after this eruption has highlighted the difficulty of constraining deposit edges from unobserved or prehistoric eruptions of all magnitudes. Our results suggest that the dispersal area of advected fall deposits could be miscalculated by up to 30% of the total, raising issues for accurate hazard zoning and assessment. Eruptions of this type challenge existing classification schemes for pyroclastic deposits and explosive eruptions and, in the past, have probably been interpreted as phreatic explosions, where the eruptive mechanism has been assumed to involve flashing of groundwater to steam.
C1 [Houghton, B. F.; Carey, R. J.] Univ Hawaii, Dept Geol & Geophys, Honolulu, HI 96822 USA.
[Swanson, D. A.; Rausch, J.; Sutton, A. J.] US Geol Survey, Hawaiian Volcano Observ, Hawaii Natl Pk, HI 96718 USA.
RP Houghton, BF (reprint author), Univ Hawaii, Dept Geol & Geophys, Honolulu, HI 96822 USA.
EM bhought@soest.hawaii.edu
RI Houghton, Bruce/H-3363-2011; Carey, Rebecca/A-5381-2013
OI Carey, Rebecca/0000-0003-2015-6419
FU National Science Foundation [EAR-0810332]; U.S. Geological Survey
[SV-ARRA-0004]
FX We acknowledge contributions to this study by our colleagues Tamar
Elias, Jim Kauahikaua, Malin Klawonn, Tim Orr, Carolyn Parcheta, Matt
Patrick, Carl Thornber, and Kelly Wooten, and grain-size analyses by
Samantha Weaver and Lauren Swavely. The paper benefited greatly from
reviews by Sandra Wyld, Ray Cas, Richard Hanson, Matthew Patrick, and
Carl Thornber. The study was funded by two grants: National Science
Foundation grant EAR-0810332 and U.S. Geological Survey Grant
SV-ARRA-0004.
NR 24
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U1 0
U2 9
PU GEOLOGICAL SOC AMER, INC
PI BOULDER
PA PO BOX 9140, BOULDER, CO 80301-9140 USA
SN 0091-7613
J9 GEOLOGY
JI Geology
PD MAR
PY 2011
VL 39
IS 3
BP 263
EP 266
DI 10.1130/G31509.1
PG 4
WC Geology
SC Geology
GA 721SI
UT WOS:000287374900020
ER
PT J
AU Willard, D
Bernhardt, C
Brown, R
Landacre, B
Townsend, P
AF Willard, Debra
Bernhardt, Christopher
Brown, Roger
Landacre, Bryan
Townsend, Philip
TI Development and application of a pollen-based paleohydrologic
reconstruction from the Lower Roanoke River Basin, North Carolina, USA
SO HOLOCENE
LA English
DT Article
DE Atlantic Coastal Plain; floodplains; hydroperiod; paleohydrology;
pollen; vegetation
ID SOUTHEASTERN UNITED-STATES; ATLANTIC MULTIDECADAL OSCILLATION; HOLOCENE
CLIMATE VARIABILITY; LATE-QUATERNARY VEGETATION; COASTAL-PLAIN RIVERS;
MODERN ANALOGS; AMERICAN; HISTORY; PRECIPITATION; FLOODPLAIN
AB We used pollen assemblages to reconstruct late-Holocene paleohydrologic patterns in floodplain deposits from the lower Roanoke River basin (North Carolina, southeastern USA). Using 120 surface samples from 38 transects, we documented statistical relationships between pollen assemblages, vegetation, and landforms. Backswamp pollen assemblages (long hydroperiods) are dominated by Nyssa (tupelo) and Taxodium (cypress) and have high pollen concentrations. Sediments from elevated levees and seasonally flooded forests (shorter hydroperiods) are characterized by dominant Pinus (pine) pollen, variable abundance of hardwood taxa, and low pollen concentrations. We apply the calibration data set to interpret past vegetation and paleohydrology. Pollen from a radiocarbon-dated sediment core collected in a tupelo-cypress backswamp indicates centennial-scale fluctuations in forest composition during the last 2400 years. Backswamp vegetation has occupied the site since land clearance began similar to 300 years ago. Recent dam emplacement affected sedimentation rates, but vegetation changes are small compared with those caused by pre-Colonial climate variability. The occurrence of wetter conditions from similar to 2200 to 1800 cal.yr BP, similar to 1100 to 750 cal.yr BP, and similar to 400 to 250 cal.yr BP may indicate changes in cyclonic circulation patterns related to shifts in the position of the Bermuda High and jet stream.
C1 [Willard, Debra; Bernhardt, Christopher; Landacre, Bryan] US Geol Survey, Reston, VA 22092 USA.
[Bernhardt, Christopher] Univ Penn, Philadelphia, PA 19104 USA.
[Brown, Roger] Columbus State Univ, Columbus, GA 31907 USA.
[Townsend, Philip] Univ Wisconsin, Madison, WI 53706 USA.
RP Willard, D (reprint author), US Geol Survey, 959 Natl Ctr, Reston, VA 22092 USA.
EM dwillard@usgs.gov
RI Townsend, Philip/B-5741-2008
OI Townsend, Philip/0000-0001-7003-8774
FU US Geological Survey Earth Surface Dynamics Program; NSF [EAR GEO
0105929]
FX The authors gratefully acknowledge field and laboratory assistance
provided by many individuals, including Tom Sheehan, Randy Richardson,
Cliff Hupp, Michael Schening, Daniel Kroes, and Edward Schenk.
Assistance in site location and access was provided by Jeff Horton and
Sam Pearsall of The Nature Conservancy and Jean Richter of US Fish &
Wildlife Service. Robert Peet provided critical guidance on site
selection, ecological insights, and constructive suggestions throughout
the period of study. Radiocarbon dates were provided by Beta Analytic,
Inc., Miami, Florida. The research was supported by the US Geological
Survey Earth Surface Dynamics Program and NSF grant EAR GEO 0105929. We
greatly appreciate critical reviews of the manuscript by Thomas Cronin,
Cliff Hupp, and Robert Peet as well as two anonymous reviewers.
NR 67
TC 4
Z9 4
U1 2
U2 15
PU SAGE PUBLICATIONS LTD
PI LONDON
PA 1 OLIVERS YARD, 55 CITY ROAD, LONDON EC1Y 1SP, ENGLAND
SN 0959-6836
J9 HOLOCENE
JI Holocene
PD MAR
PY 2011
VL 21
IS 2
BP 305
EP 317
DI 10.1177/0959683610378876
PG 13
WC Geography, Physical; Geosciences, Multidisciplinary
SC Physical Geography; Geology
GA 725MI
UT WOS:000287648400009
ER
PT J
AU Lyons, DE
Roby, DD
AF Lyons, Donald E.
Roby, Daniel D.
TI Validating growth and development of a seabird as an indicator of food
availability: captive-reared Caspian Tern chicks fed ad libitum and
restricted diets
SO JOURNAL OF FIELD ORNITHOLOGY
LA English
DT Article
DE chick growth; corticosterone; food availability; food restriction;
Hydroprogne caspia; indicator species; seabirds
ID ADRENOCORTICAL-RESPONSE; STERNA-PARADISAEA; STRESS-RESPONSE; PUFFIN
CHICKS; GREAT TITS; ALLOCATION; ENERGETICS; SURVIVAL; MASS;
CORTICOSTERONE
AB For seabirds raising young under conditions of limited food availability, reducing chick provisioning and chick growth rates are the primary means available to avoid abandonment of a breeding effort. For most seabirds, however, baseline data characterizing chick growth and development under known feeding conditions are unavailable, so it is difficult to evaluate chick nutritional status as it relates to foraging conditions near breeding colonies. To address this need, we examined the growth and development of young Caspian Terns (Hydroprogne caspia), a cosmopolitan, generalist piscivore, reared in captivity and fed ad libitum and restricted (ca. one-third lower caloric intake) diets. Ad libitum-fed chicks grew at similar rates and achieved a similar size at fledging as previously documented for chicks in the wild and had energetic demands that closely matched allometric predictions. We identified three general characteristics of food-restricted Caspian Tern chicks compared to ad libitum chicks: (1) lower age-specific body mass, (2) lower age-specific skeletal and feather size, such as wing chord length, and (3) heightened levels of corticosterone in blood, both for baseline levels and in response to acute stress. Effects of diet restriction on feather growth (10-11% slower growth in diet-restricted chicks) were less pronounced than effects on structural growth (37-52% slower growth) and body mass (24% lower at fledging age), apparently due to preferential allocation of food resources to maintain plumage growth. Our results suggest that measurements of chick body mass and feather development (e.g., wing chord or primary length) or measurement of corticosterone levels in the blood would allow useful evaluation of the nutritional status of chicks reared in the wild and of food availability in the foraging range of adults. Such evaluations could also inform demography studies (e.g., predict future recruitment) and assist in evaluating designated piscivorous waterbird conservation (colony) sites.
C1 [Lyons, Donald E.; Roby, Daniel D.] Oregon State Univ, US Geol Survey, Oregon Cooperat Fish & Wildlife Res Unit, Corvallis, OR 97331 USA.
RP Lyons, DE (reprint author), Oregon State Univ, US Geol Survey, Oregon Cooperat Fish & Wildlife Res Unit, 104 Nash Hall, Corvallis, OR 97331 USA.
EM don.lyons@oregonstate.edu
FU Bonneville Power Administration
FX Funding for this research was provided by The Bonneville Power
Administration (COTR: D. Welch). C. Cardoni, G. Dorsey, K. Gorman, A. M.
Myers, S. McDougal, L. Sheffield, and S. Wright assisted with rearing
and laboratory analyses. E. Bridge, A. Hovey, R. Suryan, and B. Tarr
shared advice on chick-rearing protocol. W. Pearcy, K. Dugger, C.
Schreck, G. Ritchison, and three anonymous reviewers improved earlier
drafts of this manuscript with their suggestions. All procedures and
protocols involving live Caspian Terns were approved by the
Institutional Animal Care and Use Committee at Oregon State University.
Scientific collection permits were obtained for all procedures involving
handling or collection of terns from the U.S. Fish and Wildlife Service
(Migratory Birds and Habitats, Region 1, Portland, OR, USA) and the
Oregon Department of Fish and Wildlife (Salem, OR, USA).
NR 47
TC 10
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U1 1
U2 26
PU WILEY-BLACKWELL
PI HOBOKEN
PA 111 RIVER ST, HOBOKEN 07030-5774, NJ USA
SN 0273-8570
EI 1557-9263
J9 J FIELD ORNITHOL
JI J. Field Ornithol.
PD MAR
PY 2011
VL 82
IS 1
BP 88
EP 100
DI 10.1111/j.1557-9263.2010.00311.x
PG 13
WC Ornithology
SC Zoology
GA 725UD
UT WOS:000287670700010
ER
PT J
AU Strickland, A
Miller, EL
Wooden, JL
AF Strickland, Ariel
Miller, Elizabeth L.
Wooden, Joseph L.
TI The Timing of Tertiary Metamorphism and Deformation in the Albion-Raft
River-Grouse Creek Metamorphic Core Complex, Utah and Idaho
SO JOURNAL OF GEOLOGY
LA English
DT Article
ID WESTERN UNITED-STATES; RANGE SOUTHERN IDAHO; MANTLED GNEISS DOMES; PB
AGE DATA; CORDILLERAN OROGEN; NORTHWESTERN UTAH; CENTRAL AUSTRALIA;
BRITISH-COLUMBIA; CENTRAL NEVADA; NORMAL-FAULT
AB The Albion-Raft River-Grouse Creek metamorphic core complex of southern Idaho and northern Utah exposes 2.56-Ga orthogneisses and Neoproterozoic metasedimentary rocks that were intruded by 32-25-Ma granitic plutons. Pluton emplacement was contemporaneous with peak metamorphism, ductile thinning of the country rocks, and top-to-the-west, normal-sense shear along the Middle Mountain shear zone. Monazite and zircon from an attenuated stratigraphic section in the Middle Mountain were dated with U-Pb, using a SHRIMP-RG (reverse geometry) ion microprobe. Zircons from the deformed Archean gneiss preserve a crystallization age of 2532 +/- 33 Ma, while monazites range from 32.6 +/- 0.6 to 27.1 +/- 0.6 Ma. In the schist of the Upper Narrows, detrital zircons lack metamorphic overgrowths, and monazites produced discordant U-Pb ages that range from 52.8 +/- 0.6 to 37.5 +/- 0.3 Ma. From the structurally and stratigraphically highest unit sampled, the schist of Stevens Spring, narrow metamorphic rims on detrital zircons yield ages from 140-110 Ma, and monazite grains contained cores that yield an age of 141 +/- 2 Ma, whereas rims and some whole grains ranged from 35.5 +/- 0.5 to 30.0 +/- 0.4 Ma. A boudinaged pegmatite exposed in Basin Creek is deformed by the Middle Mountains shear zone and yields a monazite age of 27.6 +/- 0.2 Ma. We interpret these data to indicate two periods of monazite and metamorphic zircon growth: a poorly preserved Early Cretaceous period (similar to 140 Ma) that is strongly overprinted by Oligocene metamorphism (similar to 32-27 Ma) related to regional plutonism and extension.
C1 [Strickland, Ariel; Miller, Elizabeth L.] Stanford Univ, Dept Geol & Environm Sci, Stanford, CA 94305 USA.
[Wooden, Joseph L.] US Geol Survey, Menlo Pk, CA 94025 USA.
RP Strickland, A (reprint author), Univ Wisconsin, Dept Geosci, 1215 W Dayton St, Madison, WI 53706 USA.
EM stricklandariel@gmail.com
FU U.S. Geological Survey; National Science Foundation [EAR-0809226,
EAR-0229854]
FX The authors would like to thank Marty Grove for thoughtful discussions
and reviews of early manuscripts. The authors are also grateful for
constructive reviews by David Miller and Donna Whitney. The authors also
acknowledge support for this study from the U.S. Geological Survey and
partial funding from two National Science Foundation grants awarded to
Elizabeth Miller (EAR-0809226, EAR-0229854).
NR 76
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U1 0
U2 9
PU UNIV CHICAGO PRESS
PI CHICAGO
PA 1427 E 60TH ST, CHICAGO, IL 60637-2954 USA
SN 0022-1376
J9 J GEOL
JI J. Geol.
PD MAR
PY 2011
VL 119
IS 2
BP 185
EP 206
DI 10.1086/658294
PG 22
WC Geology
SC Geology
GA 726DB
UT WOS:000287697900005
ER
PT J
AU Purvis, OW
Bennett, JP
Spratt, J
AF Purvis, O. W.
Bennett, J. P.
Spratt, J.
TI 169Copper localization, elemental content, and thallus colour in the
copper hyperaccumulator lichen Lecanora sierrae from California
SO LICHENOLOGIST
LA English
DT Article
DE heavy metals; lichen chemistry; lichen pigments; selenium
ID CUPRIFEROUS SUBSTRATA; ASCOMYCOTINA; ACID
AB An unusual dark blue-green lichen, Lecanora sierrae, was discovered over 30 years ago by Czehura near copper mines in the Lights Creek District, Plumas County, Northern California. Using atomic absorption spectroscopy, Czehura found that dark green lichen samples from Warren Canyon contained 4% Cu in ash and suggested that its colour was due to copper accumulation in the cortex. The present study addressed the hypothesis that the green colour in similar material we sampled from Warren Canyon in 2008, is caused by copper localization in the thallus. Optical microscopy and electron microprobe analysis of specimens of L. sierrae confirmed that copper localization took place in the cortex. Elemental analyses of L. sierrae and three other species from the same localities showed high enrichments of copper and selenium, suggesting that copper selenates or selenites might occur in these lichens and be responsible for the unusual colour.
C1 [Purvis, O. W.; Spratt, J.] Nat Hist Museum, Dept Bot, London SW7 5BD, England.
[Purvis, O. W.; Spratt, J.] Nat Hist Museum, Dept Mineral, London SW7 5BD, England.
[Bennett, J. P.] US Geol Survey, Natl Wildlife Hlth Ctr, Madison, WI 53711 USA.
RP Purvis, OW (reprint author), Nat Hist Museum, Dept Bot, Cromwell Rd, London SW7 5BD, England.
EM w.purvis@nhm.ac.uk
FU UK Royal Society
FX We are grateful for support from a UK Royal Society Conference Grant for
OWP to attend IAL6 and particularly to Linda Geiser for her support, to
Norman Lamb for his interest, advice, and for granting access and
permissions, to Abigail Stephens, John Dilles, Robert Wetzel and Steve
Czehura for field assistance, Tony Wighton for sample preparation, Chris
Stanley and Gordon Cressey for assistance with reflected light
microscopy, Alex Ball and Lauren Howard with FESEM, Harry Taylor for
macrophotography (Fig. 1A), Juliet Brodie for helpful discussions, and
James McNeal for help on mineral colours. The mention of commercial
equipment or products does not imply endorsement by the U.S. Geological
Survey.
NR 27
TC 4
Z9 4
U1 2
U2 4
PU CAMBRIDGE UNIV PRESS
PI CAMBRIDGE
PA EDINBURGH BLDG, SHAFTESBURY RD, CB2 8RU CAMBRIDGE, ENGLAND
SN 0024-2829
J9 LICHENOLOGIST
JI Lichenologist
PD MAR
PY 2011
VL 43
BP 165
EP 173
DI 10.1017/S0024282910000770
PN 2
PG 9
WC Plant Sciences; Mycology
SC Plant Sciences; Mycology
GA 725DP
UT WOS:000287625700008
ER
PT J
AU Kraus, RT
Wells, RJD
Rooker, JR
AF Kraus, Richard T.
Wells, R. J. David
Rooker, Jay R.
TI Horizontal movements of Atlantic blue marlin (Makaira nigricans) in the
Gulf of Mexico
SO MARINE BIOLOGY
LA English
DT Article
ID SEA-SURFACE-TEMPERATURE; TUNA THUNNUS-THYNNUS; SAILFISH
ISTIOPHORUS-PLATYPTERUS; WESTERN BOUNDARY CURRENT; SATELLITE ARCHIVAL
TAGS; PELAGIC LONGLINE GEAR; VERTICAL HABITAT USE; WHITE MARLIN;
TETRAPTURUS-ALBIDUS; PARTIAL MIGRATION
AB We examined movements of Atlantic blue marlin (Makaira nigricans) from the Gulf of Mexico based upon 42 pop-up archival transmitting (PAT) tags. Long deployments (including one 334-day track) revealed diverse movement patterns within the Gulf of Mexico. North-south seasonal changes in blue marlin distribution showed strong correspondence with established seasonal patterns of sea surface temperature and primary production. During the summer spawning season, blue marlin utilized outer shelf and shelf edge waters in the northern Gulf of Mexico, and longer duration tracks indicated overwintering habitats in the Bay of Campeche. Egress occurred throughout the year and was difficult to determine because some tracks ended in the Straits of Florida (n = 3) while other tracks recorded movement through it or the Yucatan Channel (n = 4). Our results indicate that Atlantic blue marlin have a more restricted geographic range of habitats than previously recognized and that the Gulf of Mexico provides spatially dynamic suitable habitat that is utilized year-round through seasonal movements.
C1 [Kraus, Richard T.] George Mason Univ, Dept Environm Sci & Policy, Fairfax, VA 22030 USA.
[Wells, R. J. David; Rooker, Jay R.] Texas A&M Univ, Dept Marine Biol, Galveston, TX 77551 USA.
RP Kraus, RT (reprint author), US Geol Survey, Great Lakes Sci Ctr, Lake Erie Biol Stn, 6100 Columbus Ave, Sandusky, OH 44870 USA.
EM rkraus@usgs.gov
RI Rooker, Jay/M-3197-2013
OI Rooker, Jay/0000-0002-5934-7688
FU McDaniel Charitable Foundation; Texas Institute of Oceanography (TIO);
George Mason University
FX We are grateful for the participation of the captains and crew of the
sport fishing vessels in the tagging work, especially Bill Lyons, Mark
Lyons, John Cochrane, and Brett Falterman. In addition, we thank Anders
Nielsen and Tim Lam for their assistance with the state-space model
programs. We are also grateful for comments of an anonymous reviewer,
which greatly improved the manuscript. The tagging research was funded
by awards to J.R.R. from the McDaniel Charitable Foundation. R.J.D.W.
was supported in part by a Texas Institute of Oceanography (TIO)
post-doctoral research fellowship. R.T.K. was supported by a TIO
postdoctoral fellowship and a faculty development leave award from
George Mason University.
NR 79
TC 13
Z9 13
U1 1
U2 17
PU SPRINGER
PI NEW YORK
PA 233 SPRING ST, NEW YORK, NY 10013 USA
SN 0025-3162
J9 MAR BIOL
JI Mar. Biol.
PD MAR
PY 2011
VL 158
IS 3
BP 699
EP 713
DI 10.1007/s00227-010-1593-3
PG 15
WC Marine & Freshwater Biology
SC Marine & Freshwater Biology
GA 723RS
UT WOS:000287525100020
ER
PT J
AU Mulcahy, DM
AF Mulcahy, Daniel M.
TI Antibiotic use during the intracoelomic implantation of electronic tags
into fish
SO REVIEWS IN FISH BIOLOGY AND FISHERIES
LA English
DT Article
DE Antibiotics; Surgery; Implantation; Transmitter; Data logger; Fish
ID JUVENILE CHINOOK SALMON; CARP CYPRINUS-CARPIO; ONCORHYNCHUS-MYKISS
WALBAUM; ROCKFISH SEBASTES-INERMIS; MEKONG GIANT CATFISH; LOWER
CHESAPEAKE BAY; LOWER COLUMBIA RIVER; HYBRID STRIPED BASS; SOUTHERN
NEW-JERSEY; DATA-STORAGE TAGS
AB The use of antibiotics, in particular, the use of a single dose of antibiotics during electronic tag implantation is of unproven value, and carries with it the potential for the development of antibiotic resistance in bacteria and the alteration of the immune response of the fish. Antibiotic use during electronic tag implantation must conform to relevant drug laws and regulations in the country where work is being done, including the requirements for withdrawal times before human consumption is a possibility. Currently, the choice of antibiotics (most often tetracycline or oxytetracycline) and the use of a single dose of the drug are decisions made without knowledge of the basic need for antibiotic usage and of the bacteria involved in infections that occur following electronic tag implantation. Correct perioperative use of an antibiotic is to apply the drug to the animal before surgery begins, to assure serum and tissue levels of the drug are adequate before the incision is made. However, the most common perioperative application of antibiotics during implantation of an electronic tag is to delay the administration of the drug, injecting it into the coelom after the electronic tag is inserted, just prior to closure of the incision. There is little empirical evidence that the present application of antibiotics in fish being implanted with electronic tags is of value. Improvements should first be made to surgical techniques, especially the use of aseptic techniques and sterilized instruments and electronic tags, before resorting to antibiotics.
C1 US Geol Survey, Alaska Sci Ctr, Anchorage, AK 99508 USA.
RP Mulcahy, DM (reprint author), US Geol Survey, Alaska Sci Ctr, 4210 Univ Dr, Anchorage, AK 99508 USA.
EM daniel_mulcahy@usgs.gov
NR 150
TC 10
Z9 10
U1 2
U2 12
PU SPRINGER
PI DORDRECHT
PA VAN GODEWIJCKSTRAAT 30, 3311 GZ DORDRECHT, NETHERLANDS
SN 0960-3166
EI 1573-5184
J9 REV FISH BIOL FISHER
JI Rev. Fish. Biol. Fish.
PD MAR
PY 2011
VL 21
IS 1
SI SI
BP 83
EP 96
DI 10.1007/s11160-010-9190-6
PG 14
WC Fisheries; Marine & Freshwater Biology
SC Fisheries; Marine & Freshwater Biology
GA 726WG
UT WOS:000287756700009
ER
PT J
AU Plant, NG
Holland, KT
AF Plant, Nathaniel G.
Holland, K. Todd
TI Prediction and assimilation of surf-zone processes using a Bayesian
network Part II: Inverse models
SO COASTAL ENGINEERING
LA English
DT Article
DE Wave height; Bathymetry; Field data; Duck94; Parameter estimation
ID 3RD-GENERATION WAVE MODEL; COASTAL REGIONS; NEARSHORE; TRANSFORMATION;
VERIFICATION; DISSIPATION; BATHYMETRY; VALIDATION; FORECASTS; BEHAVIOR
AB A Bayesian network model has been developed to simulate a relatively simple problem of wave propagation in the surf zone (detailed in Part I). Here, we demonstrate that this Bayesian model can provide both inverse modeling and data-assimilation solutions for predicting offshore wave heights and depth estimates given limited wave-height and depth information from an onshore location. The inverse method is extended to allow data assimilation using observational inputs that are not compatible with deterministic solutions of the problem. These inputs include sand bar positions (instead of bathymetry) and estimates of the intensity of wave breaking (instead of wave-height observations). Our results indicate that wave breaking information is essential to reduce prediction errors. In many practical situations, this information could be provided from a shore-based observer or from remote-sensing systems. We show that various combinations of the assimilated inputs significantly reduce the uncertainty in the estimates of water depths and wave heights in the model domain. Application of the Bayesian network model to new field data demonstrated significant predictive skill (R(2) = 0.7) for the inverse estimate of a month-long time series of offshore wave heights. The Bayesian inverse results include uncertainty estimates that were shown to be most accurate when given uncertainty in the inputs (e.g., depth and tuning parameters). Furthermore, the inverse modeling was extended to directly estimate tuning parameters associated with the underlying wave-process model. The inverse estimates of the model parameters not only showed an offshore wave height dependence consistent with results of previous studies but the uncertainty estimates of the tuning parameters also explain previously reported variations in the model parameters. Published by Elsevier B.V.
C1 [Plant, Nathaniel G.] US Geol Survey, St Petersburg, FL 33701 USA.
[Holland, K. Todd] USN, Res Lab, Stennis Space Ctr, MS 39529 USA.
RP Plant, NG (reprint author), US Geol Survey, 600 4th St S, St Petersburg, FL 33701 USA.
EM nplant@usgs.gov; todd.holland@nrlssc.navy.mil
RI Holland, K. Todd/A-7673-2011;
OI Holland, K. Todd/0000-0002-4601-6097; Plant,
Nathaniel/0000-0002-5703-5672
FU USGS Coastal Marine Geology; Office of Naval Research [0602435N,
N0001409IP20080]; National Science Foundation
FX This work was supported by USGS Coastal Marine Geology (National
assessment of coastal change hazards project) and the Office of Naval
Research (PE Number: 0602435N for KTH and N0001409IP20080 for NGP). We
are indebted to the researchers at the Field Research Facility (FRF,
Duck, NC) who collected the long time series of bathymetry and wave
conditions used in our models. This debt is extended also to both the
FRF researchers and to Drs. Guza, Gallagher, Herbers, Raubenheimer, and
Elgar who collected the Duck94 field observation used to test our
predictions. That effort was supported by the Office of Naval Research
and the National Science Foundation. We appreciate the thoughtful and
constructive reviews provided by P. Howd, A. Reniers, and B. Lidz.
NR 24
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U1 0
U2 6
PU ELSEVIER SCIENCE BV
PI AMSTERDAM
PA PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS
SN 0378-3839
J9 COAST ENG
JI Coast. Eng.
PD MAR
PY 2011
VL 58
IS 3
BP 256
EP 266
DI 10.1016/j.coastaleng.2010.11.002
PG 11
WC Engineering, Civil; Engineering, Ocean
SC Engineering
GA 718GX
UT WOS:000287110200004
ER
PT J
AU Liu, WY
Wang, CY
Wang, TS
Fellers, GM
Lai, BC
Kam, YC
AF Liu, Wan-Yi
Wang, Ching-Yuh
Wang, Tsu-Shing
Fellers, Gary M.
Lai, Bo-Chi
Kam, Yeong-Choy
TI Impacts of the herbicide butachlor on the larvae of a paddy field
breeding frog (Fejervarya limnocharis) in subtropical Taiwan
SO ECOTOXICOLOGY
LA English
DT Article
DE Butachlor; LC(50); Fejervarya limnocharis; Paddy field; Genotoxicity;
Cholinesterase
ID GENOTOXICITY TEST DATA; GEL COMET ASSAY; DNA-DAMAGE; TADPOLES; WATER;
TOXICITY; ELECTROPHORESIS
AB Butachlor is the most commonly used herbicide on paddy fields in Taiwan and throughout Southeast Asia. Since paddy fields provide habitat for pond breeding amphibians, we examined growth, development, time to metamorphosis, and survival of alpine cricket frog tadpoles (Fejervarya limnocharis) exposed to environmentally realistic concentrations of butachlor. We documented negative impacts of butachlor on survival, development, and time to metamorphosis, but not on tadpole growth. The 96 h LC(50) for tadpoles was 0.87 mg/l, much lower than the 4.8 mg/l recommended dosage for application to paddy fields. Even given the rapid breakdown of butachlor, tadpoles would be exposed to concentrations in excess of their 96 h LC(50) for an estimated 126 h. We also documented DNA damage (genotoxicity) in tadpoles exposed to butachlor at concentrations an order of magnitude less than the 4.8 mg/l recommended application rate. We did not find that butachlor depressed cholinesterase activity of tadpoles, unlike most organophosphorus insecticides. We conclude that butachlor is likely to have widespread negative impacts on amphibians occupying paddy fields with traditional herbicide application.
C1 [Liu, Wan-Yi; Kam, Yeong-Choy] Tunghai Univ, Dept Life Sci, Taichung 407, Taiwan.
[Wang, Ching-Yuh] Natl Chung Hsing Univ, Dept Agron, Taichung 402, Taiwan.
[Wang, Tsu-Shing] Chung Shan Med Univ, Dept Biomed Sci, Taichung 402, Taiwan.
[Fellers, Gary M.] Point Reyes Natl Seashore, Western Ecol Res Ctr, US Geol Survey, Point Reyes Stn, CA 94956 USA.
[Lai, Bo-Chi] Dayeh Univ, Dept Bioresources, Dacun 51591, Changhua, Taiwan.
RP Kam, YC (reprint author), Tunghai Univ, Dept Life Sci, Taichung 407, Taiwan.
EM biyckam@thu.edu.tw
FU National Science Council [NSC 95-2311-B-029-006-MY3]
FX This study was supported by a National Science Council Grant (NSC
95-2311-B-029-006-MY3) to YCK. Joan Fellers, Patrick Kleeman, and Norm
Scott provided helpful comments on the manuscript. Any use of trade,
product, or firm names in this publication is for descriptive purposes
only and does not imply endorsement by the US Government. This is
contribution 417 of the US Geologic Survey, Amphibian Research and
Monitoring Initiative (ARMI).
NR 41
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U1 1
U2 25
PU SPRINGER
PI DORDRECHT
PA VAN GODEWIJCKSTRAAT 30, 3311 GZ DORDRECHT, NETHERLANDS
SN 0963-9292
J9 ECOTOXICOLOGY
JI Ecotoxicology
PD MAR
PY 2011
VL 20
IS 2
BP 377
EP 384
DI 10.1007/s10646-010-0589-6
PG 8
WC Ecology; Environmental Sciences; Toxicology
SC Environmental Sciences & Ecology; Toxicology
GA 719XO
UT WOS:000287245000008
PM 21210217
ER
PT J
AU du Bray, EA
Bacon, CR
John, DA
Wooden, JL
Mazdab, FK
AF du Bray, Edward A.
Bacon, Charles R.
John, David A.
Wooden, Joseph L.
Mazdab, Frank K.
TI Episodic intrusion, internal differentiation, and hydrothermal
alteration of the Miocene Tatoosh intrusive suite south of Mount
Rainier, Washington
SO GEOLOGICAL SOCIETY OF AMERICA BULLETIN
LA English
DT Article
ID CASCADE VOLCANIC ARC; GRANITIC-ROCKS; SIERRA-NEVADA; PLUTON
CONSTRUCTION; ELDORADO MOUNTAINS; PHYSICAL PROCESSES; MAGMA CHAMBER;
BISHOP TUFF; NEW-ZEALAND; ZIRCON
AB The Miocene Tatoosh intrusive suite south of Mount Rainier is composed of three broadly granodioritic plutons that are manifestations of ancestral Cascades arc magmatism. Tatoosh intrusive suite plutons have individually diagnostic characteristics, including texture, mineralogy, and geochemistry, and apparently lack internal contacts. New ionmicroprobe U-Pb zircon ages indicate crystallization of the Stevens pluton ca. 19.2 Ma, Reflection-Pyramid pluton ca. 18.5 Ma, and Nisqually pluton ca. 17.5 Ma. The Stevens pluton includes rare, statistically distinct ca. 20.1 Ma zircon antecrysts. Wide-ranging zircon rare earth element (REE), Hf, U, and Th concentrations suggest late crystallization from variably evolved residual liquids. Zircon Eu/Eu*-Hf covariation is distinct for each of the Reflection-Pyramid, Nisqually, and Stevens plutons. Although most Tatoosh intrusive suite rocks have been affected by weak hydrothermal alteration, and sparse mineralized veins cut some of these rocks, significant base or precious metal mineralization is absent.
At the time of shallow emplacement, each of these magma bodies was largely homogeneous in bulk composition and petrographic features, but, prior to final solidification, each of the Tatoosh intrusive suite plutons developed internal compositional variation. Geochemical and petrographic trends within each pluton are most consistent with differential loss of residual melt, possibly represented by late aplite dikes or erupted as rhyolite, from crystal-rich magma. Crystal-rich magma that formed each pluton evidently accumulated in reservoirs below the present level of exposure and then intruded to a shallow depth. Assembled by episodic intrusion, the Tatoosh intrusive suite may be representative of midsized composite plutonic complexes beneath arc volcanoes.
C1 [du Bray, Edward A.] US Geol Survey, Denver Fed Ctr, Lakewood, CO 80225 USA.
[Bacon, Charles R.; John, David A.] US Geol Survey, Menlo Pk, CA 94025 USA.
[Wooden, Joseph L.; Mazdab, Frank K.] US Geol Survey, Stanford USGS Ion Microprobe Lab, Stanford, CA 94305 USA.
RP du Bray, EA (reprint author), US Geol Survey, Denver Fed Ctr, MS 973,Box 25046, Lakewood, CO 80225 USA.
EM edubray@usgs.gov
RI Balsamo, Fabrizio/F-1674-2017;
OI Balsamo, Fabrizio/0000-0003-1931-466X; John, David/0000-0001-7977-9106
FU U.S. Geological Survey Mineral Resources Program; National Science
Foundation (NSF) [OCE-0648484, EAR-0635864]
FX We thank the National Park Service for permission to work within Mount
Rainier National Park and collect samples. Reviews by T.W. Sisson and
K.A. Howard improved an early version of this manuscript, and GSA
Bulletin reviewers J.M. Mattinson and G.A.R. Gualda, as well as
Associate Editor C.F. Miller, substantially sharpened the presentation
of our study. This work was funded by the U.S. Geological Survey Mineral
Resources Program. V.J.M. Salters generously provided radiogenic isotope
data through support from National Science Foundation (NSF) grants
OCE-0648484 and EAR-0635864.
NR 68
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U1 1
U2 6
PU GEOLOGICAL SOC AMER, INC
PI BOULDER
PA PO BOX 9140, BOULDER, CO 80301-9140 USA
SN 0016-7606
J9 GEOL SOC AM BULL
JI Geol. Soc. Am. Bull.
PD MAR-APR
PY 2011
VL 123
IS 3-4
BP 534
EP 561
DI 10.1130/B30095.1
PG 28
WC Geosciences, Multidisciplinary
SC Geology
GA 712KJ
UT WOS:000286665300009
ER
PT J
AU Lentz, EE
Hapke, CJ
AF Lentz, Erika E.
Hapke, Cheryl J.
TI Geologic framework influences on the geomorphology of an
anthropogenically modified barrier island: Assessment of dune/beach
changes at Fire Island, New York
SO GEOMORPHOLOGY
LA English
DT Article
DE Framework geology; Coastal geomorphology; Beach replenishment; LiDAR;
Volume change; Topography
ID INNER-CONTINENTAL-SHELF; SEDIMENT BUDGET; VOLUMETRIC CHANGE; SHORELINE
CHANGE; SOUTH-CAROLINA; NORTH-CAROLINA; AIRBORNE LIDAR; LONG-ISLAND;
COASTAL; BEACH
AB Antecedent geology plays a crucial role in determining the inner-shelf, nearshore, and onshore geomorphology observed in coastal systems. However, the influence of the geologic framework on a system is difficult to extract when evaluating responses to changes due to storms and anthropogenic modifications, and few studies have quantified the potential for these influences in dune/beach environments. This study evaluates topographic change to the dune/beach system at Fire Island, New York over a ten year period (1998-2008) at two sites representing eastern and western reaches of the island where morphology has been shown to vary. The sites are situated along swaths of coast eroding differentially and where the inner shelf geologic framework differs substantially. Fewer large storms occurred in the first half of the study period, compared with the later part of the study period which includes several severe and prolonged extratropical storms. Additionally, a major beach replenishment project was conducted at one of the study sites. Topographic data from LiDAR and RTK GPS surveys are used to construct high-resolution 3D surfaces, which are used to determine volumetric change and to extract 2D alongshore features and profiles for analysis. The study sites help to further characterize morphologic differences between eastern and western reaches of the island. The western site displays higher sand volumes, lower dunes, and a lower gradient profile slope when compared with the eastern site. In addition to these fundamental morphologic differences, the two sites also differ significantly in their response to coastal storms and in the fact that their replenishment histories are different. The replenished areas show reduced vulnerability to storms through minimal volume loss and shoreline accretion that should be considered when evaluating the response of replenished areas to episodic events. We propose that site-specific differences evident throughout the study period can be linked to alongshore variations in the framework geology of the system. Anthropogenic modifications may have intensified differences already inherent in the system. (C) 2010 Elsevier B.V. All rights reserved.
C1 [Lentz, Erika E.; Hapke, Cheryl J.] US Geol Survey, Woods Hole Coastal & Marine Sci Ctr, PWRC, Woods Hole, MA 02543 USA.
[Lentz, Erika E.] Univ Rhode Isl, Dept Geosci, Kingston, RI 02881 USA.
RP Lentz, EE (reprint author), US Geol Survey, Woods Hole Coastal & Marine Sci Ctr, PWRC, 384 Woods Hole Rd, Woods Hole, MA 02543 USA.
EM elentz@usgs.gov
OI Lentz, Erika/0000-0002-0621-8954
FU National Park Service; U.S. Geological Survey; University of Rhode
Island Coastal Institute; NSF IGERT [DGE-0504103]
FX Grant funding for this research and for graduate student support in this
project has been supplied by the National Park Service, the U.S.
Geological Survey, and the University of Rhode Island Coastal Institute
IGERT Project and in part by NSF IGERT grant DGE-0504103 to the
University of Rhode Island Coastal Institute. The slope change
methodology applied in this paper was developed by Meredith Kratzmann
with the U.S. Geological Survey. We are grateful to Rachel Hehre,
Michael Bradley, Meredith Kratzmann, and Fire Island NPS Staff for their
assistance in conducting field surveys, and also to Mike Bradley for his
work post-processing and generating RTK GPS surfaces. This paper was
also greatly enhanced by reviews from two U.S. Geological Survey
researchers, Jeffrey List and S. Jeffress Williams, and from two
anonymous reviewers.
NR 51
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U1 2
U2 14
PU ELSEVIER SCIENCE BV
PI AMSTERDAM
PA PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS
SN 0169-555X
J9 GEOMORPHOLOGY
JI Geomorphology
PD MAR 1
PY 2011
VL 126
IS 1-2
BP 82
EP 96
DI 10.1016/j.geomorph.2010.10.032
PG 15
WC Geography, Physical; Geosciences, Multidisciplinary
SC Physical Geography; Geology
GA 717NP
UT WOS:000287055000007
ER
PT J
AU Rodgers, PE
Celebi, M
AF Rodgers, Poise E.
Celebi, Mehmet
TI Method for detecting moment connection fracture using high-frequency
transients in recorded accelerations
SO JOURNAL OF CONSTRUCTIONAL STEEL RESEARCH
LA English
DT Article
DE Earthquake damage; Earthquake engineering; Instrumentation; Seismic
response; Steel frames; Structural dynamics
ID STRUCTURAL DAMAGE DETECTION; NEURAL-NETWORKS; ACOUSTIC-EMISSION; FRAMES;
IDENTIFICATION; EARTHQUAKE
AB The 1994 Northridge earthquake caused brittle fractures in steel moment frame building connections, despite causing little visible building damage in most cases. Future strong earthquakes are likely to cause similar damage to the many un-retrofitted pre-Northridge buildings in the western US and elsewhere. Without obvious permanent building deformation, costly intrusive inspections are currently the only way to determine if major fracture damage that compromises building safety has occurred. Building instrumentation has the potential to provide engineers and owners with timely information on fracture occurrence. Structural dynamics theory predicts and scale model experiments have demonstrated that sudden, large changes in structure properties caused by moment connection fractures will cause transient dynamic response. A method is proposed for detecting the building-wide level of connection fracture damage, based on observing high-frequency, fracture-induced transient dynamic responses in strong motion accelerograms. High-frequency transients are short (<1 s), sudden-onset waveforms with frequency content above 25 Hz that are visually apparent in recorded accelerations. Strong motion data and damage information from intrusive inspections collected from 24 sparsely instrumented buildings following the 1994 Northridge earthquake are used to evaluate the proposed method. The method's overall success rate for this data set is 67%, but this rate varies significantly with damage level. The method performs reasonably well in detecting significant fracture damage and in identifying cases with no damage, but fails in cases with few fractures. Combining the method with other damage indicators and removing records with excessive noise improves the ability to detect the level of damage. (C) 2010 Elsevier Ltd. All rights reserved.
C1 [Rodgers, Poise E.; Celebi, Mehmet] US Geol Survey, Menlo Pk, CA 94025 USA.
RP Rodgers, PE (reprint author), GeoHazards Int, 200 Town & Country Village, Palo Alto, CA 94577 USA.
EM rodgers@geohaz.org; celebi@usgs.gov
FU USGS
FX The authors gratefully acknowledge the financial support provided by
USGS to conduct this work. The findings and conclusions in this work are
those of the authors alone. Strong motion records, building information,
and information on data processing and instrument performance were
provided by Moh Huang, Vladimir Grazier, and their colleagues at the
California Strong Motion Instrumentation Program and Chris Stephens at
USGS. Information on instrument performance and impact response was
provided by Bill Rihn and Ian Standley of Kinemetrics, Inc. and Leroy
Foote, Ron Porcella, Chris Deitel and Roger Borcherdt of USGS. The
assistance of the following persons in gathering building damage
information is also greatly appreciated: Bruce Maison of East Bay
Municipal Utility District (retired), Tom Sabol of Englekirk and Sabot
Consulting Engineers, Kelvin Chang of the City of Burbank, Terrance
Paret and Kent Sasaki of Wiss, Janney, Elstner Associates, Inc., Gregg
Brandow and Peter Maranian of Brandow & Johnston Associates, Sea Fan of
Los Angeles Department of Building and Safety, Farzad Naeim of John A.
Martin & Associates, Brian Cochran of Brian L. Cochran & Associates,
Owen Hata of Nabih Youssef & Associates, Albert Chen of Black & Veatch,
Inc., and James Anderson of the University of Southern California.
Comments by the reviewers, which improved the manuscript, are also
greatly appreciated.
NR 59
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U2 5
PU ELSEVIER SCI LTD
PI OXFORD
PA THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, OXON, ENGLAND
SN 0143-974X
J9 J CONSTR STEEL RES
JI J. Constr. Steel. Res.
PD MAR
PY 2011
VL 67
IS 3
BP 293
EP 307
DI 10.1016/j.jcsr.2010.11.002
PG 15
WC Construction & Building Technology; Engineering, Civil
SC Construction & Building Technology; Engineering
GA 716HX
UT WOS:000286960800004
ER
PT J
AU Wimpey, J
Marion, JL
AF Wimpey, Jeremy
Marion, Jeffrey L.
TI A spatial exploration of informal trail networks within Great Falls
Park, VA
SO JOURNAL OF ENVIRONMENTAL MANAGEMENT
LA English
DT Article
DE Trail impacts; Informal trails; Landscape fragmentation; Recreation
impact
ID EFFECTIVE MESH SIZE; LANDSCAPE FRAGMENTATION; FOREST FRAGMENTATION;
MOUNTAINS; ROADS; USA; DEGRADATION; VEGETATION; IMPACTS; HIKING
AB Informal (visitor-created) trails represent a threat to the natural resources of protected natural areas around the globe. These trails can remove vegetation, displace wildlife, alter hydrology, alter habitat, spread invasive species, and fragment landscapes. This study examines informal and formal trails within Great Falls Park, VA, a sub-unit of the George Washington Memorial Parkway, managed by the U.S. National Park Service. This study sought to answer three specific questions: 1) Are the physical characteristics and topographic alignments of informal trails significantly different from formal trails, 2) Can landscape fragmentation metrics be used to summarize the relative impacts of formal and informal trail networks on a protected natural area? and 3) What can we learn from examining the spatial distribution of the informal trails within protected natural areas?
Statistical comparisons between formal and informal trails in this park indicate that informal trails have less sustainable topographic alignments than their formal counterparts. Spatial summaries of the lineal and areal extent and fragmentation associated with the trail networks by park management zones compare park management goals to the assessed attributes. Hot spot analyses highlight areas of high trail density within the park and findings provide insights regarding potential causes for development of dense informal trail networks. Published by Elsevier Ltd.
C1 [Marion, Jeffrey L.] Virginia Tech, Dept Forest Resources & Environm Conservat 0324, US Geol Survey, Virginia Tech Field Stn,USDI, Blacksburg, VA 24061 USA.
RP Marion, JL (reprint author), Virginia Tech, Dept Forest Resources & Environm Conservat 0324, US Geol Survey, Virginia Tech Field Stn,USDI, Blacksburg, VA 24061 USA.
EM wimpeyjf@vt.edu; jmarion@vt.edu
FU National Park Service
FX The authors would like to thank the National Park Service for sponsoring
this research and the following individuals for their assistance:; Ben
Helwig, NPS, for his assistance in creating providing several GIS
datasets.; Logan Park, Doctoral candidate, for his extensive fieldwork
assistance.; Laura Freeman, Virginia Tech Statistics Department, for her
helpful statistical consulting.
NR 76
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U1 4
U2 23
PU ACADEMIC PRESS LTD- ELSEVIER SCIENCE LTD
PI LONDON
PA 24-28 OVAL RD, LONDON NW1 7DX, ENGLAND
SN 0301-4797
EI 1095-8630
J9 J ENVIRON MANAGE
JI J. Environ. Manage.
PD MAR
PY 2011
VL 92
IS 3
BP 1012
EP 1022
DI 10.1016/j.jenvman.2010.11.015
PG 11
WC Environmental Sciences
SC Environmental Sciences & Ecology
GA 714BR
UT WOS:000286782400074
PM 21129844
ER
PT J
AU Zhou, X
Robinson, JL
Geraci, CJ
Parker, CR
Flint, OS
Etnier, DA
Ruiter, D
DeWalt, RE
Jacobus, LM
Hebert, PDN
AF Zhou, Xin
Robinson, Jason L.
Geraci, Christy J.
Parker, Charles R.
Flint, Oliver S., Jr.
Etnier, David A.
Ruiter, David
DeWalt, R. Edward
Jacobus, Luke M.
Hebert, Paul D. N.
TI Accelerated construction of a regional DNA-barcode reference library:
caddisflies (Trichoptera) in the Great Smoky Mountains National Park
SO JOURNAL OF THE NORTH AMERICAN BENTHOLOGICAL SOCIETY
LA English
DT Article
DE DNA barcoding; mitochondrial DNA; COI; aquatic insects; molecular
identification; biomonitoring; biodiversity; ATBI
ID PARASITOID FLIES DIPTERA; POPULATION-STRUCTURE; NORTHERN CALIFORNIA;
MITOCHONDRIAL-DNA; CRYPTIC DIVERSITY; GENETIC-STRUCTURE;
DRUSUS-DISCOLOR; EPHEMEROPTERA; GENUS; IDENTIFICATION
AB Deoxyribonucleic acid (DNA) barcoding is an effective tool for species identification and life-stage association in a wide range of animal taxa. We developed a strategy for rapid construction of a regional DNA-barcode reference library and used the caddisflies (Trichoptera) of the Great Smoky Mountains National Park (GSMNP) as a model. Nearly 1000 cytochrome c oxidase subunit I (COI) sequences, representing 209 caddisfly species previously recorded from GSMNP, were obtained from the global Trichoptera Barcode of Life campaign. Most of these sequences were collected from outside the GSMNP area. Another 645 COI sequences, representing 80 species, were obtained from specimens collected in a 3-d bioblitz (short-term, intense sampling program) in GSMNP. The joint collections provided barcode coverage for 212 species, 91% of the GSMNP fauna. Inclusion of samples from other localities greatly expedited construction of the regional DNA-barcode reference library. This strategy increased intraspecific divergence and decreased average distances to nearest neighboring species, but the DNA-barcode library was able to differentiate 93% of the GSMNP Trichoptera species examined. Global barcoding projects will aid construction of regional DNA-barcode libraries, but local surveys make crucial contributions to progress by contributing rare or endemic species and full-length barcodes generated from high-quality DNA. DNA taxonomy is not a goal of our present work, but the investigation of COI divergence patterns in caddisflies is providing new insights into broader biodiversity patterns in this group and has directed attention to various issues, ranging from the need to re-evaluate species taxonomy with integrated morphological and molecular evidence to the necessity of an appropriate interpretation of barcode analyses and its implications in understanding species diversity (in contrast to a simple claim for barcoding failure).
C1 [Zhou, Xin; Hebert, Paul D. N.] Univ Guelph, Biodivers Inst Ontario, Guelph, ON N1G 2W1, Canada.
[Robinson, Jason L.; Etnier, David A.] Univ Tennessee, Dept Ecol & Evolutionary Biol, Knoxville, TN 37996 USA.
[Geraci, Christy J.; Flint, Oliver S., Jr.] Smithsonian Inst, Natl Museum Nat Hist, Dept Entomol, Washington, DC 20013 USA.
[Parker, Charles R.] US Geol Survey, Biol Resources Discipline, Gatlinburg, TN 37738 USA.
[DeWalt, R. Edward] Illinois Nat Hist Survey, Champaign, IL 61820 USA.
[Jacobus, Luke M.] Indiana Univ, Dept Biol, Bloomington, IN 47405 USA.
RP Zhou, X (reprint author), Univ Guelph, Biodivers Inst Ontario, 50 Stone Rd E, Guelph, ON N1G 2W1, Canada.
EM xinzhou@uoguelph.ca; jrobin30@utk.edu; geracic@si.edu;
chuck_parker@usgs.gov; flinto@si.edu; dipnet@utk.edu; druiter@msn.com;
edewalt@inhs.uiuc.edu; luke.jacobus@gmail.com; phebert@uoguelph.ca
RI Zhou, Xin/D-4025-2009; Hebert, Paul/C-4161-2013
OI Zhou, Xin/0000-0002-1407-7952; Hebert, Paul/0000-0002-3081-6700
FU Discover Life in America [DLIA2007-08]; GSMNP; Natural Sciences and
Engineering Research Council of Canada; Genome Canada; US Geological
Survey; Environment Canada's Water Science and Technology program
FX The 2007 bioblitz was supported by Discover Life in America
(DLIA2007-08) and by the GSMNP. Sequencing costs and informatics support
were provided by grants from the Natural Sciences and Engineering
Research Council of Canada and by Genome Canada to PDNH. The US
Geological Survey provided funding from the Natural Resources Protection
Program to CRP. Funding from Environment Canada's Water Science and
Technology program enabled surveys in New Brunswick. Parks Canada
supported collecting efforts across Canada under permit number
NAP-2008-1636. We thank other members of the bioblitz team including Ian
Stocks, Lauren Harvey, Katy Hind, John Wilson, and Anne Timm, for aid
with collections and identifications. We thank the following
organizations for contributing crucial specimens to this study and
hosting voucher specimens: National Museum of Natural History,
University of Minnesota Insect Collection, Royal Ontario Museum, Florida
A&M University, Illinois Natural History Survey, Environment Canada, and
Rutgers University. Numerous collaborators have helped to collect
specimens, maintain vouchers, and provide taxonomic advice. We
particularly thank Ralph Holzenthal, Karl Kjer, Roger Blahnik, Donald
Baird, Kristie Heard, Boris Kondratieff, John Morse, Luke Myers, and
Andrew Rasmussen. Sheng Li of Peking University provided help in
generating the sample distribution map. Last, we thank colleagues at the
Canadian Centre for DNA Barcoding, and the Biodiversity Institute of
Ontario, for their assistance in the laboratory and field.
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PU NORTH AMER BENTHOLOGICAL SOC
PI LAWRENCE
PA 1041 NEW HAMSPHIRE STREET, LAWRENCE, KS 66044 USA
SN 0887-3593
J9 J N AM BENTHOL SOC
JI J. N. Am. Benthol. Soc.
PD MAR
PY 2011
VL 30
IS 1
BP 131
EP 162
DI 10.1899/10-010.1
PG 32
WC Ecology; Marine & Freshwater Biology
SC Environmental Sciences & Ecology; Marine & Freshwater Biology
GA 718IP
UT WOS:000287114800012
ER
PT J
AU Grant, EHC
AF Grant, Evan H. Campbell
TI Structural complexity, movement bias, and metapopulation extinction risk
in dendritic ecological networks
SO JOURNAL OF THE NORTH AMERICAN BENTHOLOGICAL SOCIETY
LA English
DT Article
DE dendritic ecological network; dendritic metapopulation; dispersal bias;
metapopulation persistence; network complexity
ID POPULATION-DYNAMICS; STREAM FISH; LANDSCAPE STRUCTURE; SPATIAL POSITION;
RIVER NETWORKS; DRIFT PARADOX; CONNECTIVITY; PATTERNS; HABITAT;
DISPERSAL
AB Spatial complexity in metacommunities can be separated into 3 main components: size (i.e., number of habitat patches), spatial arrangement of habitat patches (network topology), and diversity of habitat patch types. Much attention has been paid to lattice-type networks, such as patch-based metapopulations, but interest in understanding ecological networks of alternative geometries is building. Dendritic ecological networks (DENs) include some increasingly threatened ecological systems, such as caves and streams. The restrictive architecture of dendritic ecological networks might have overriding implications for species persistence. I used a modeling approach to investigate how number and spatial arrangement of habitat patches influence metapopulation extinction risk in 2 DENs of different size and topology. Metapopulation persistence was higher in larger networks, but this relationship was mediated by network topology and the dispersal pathways used to navigate the network. Larger networks, especially those with greater topological complexity, generally had lower extinction risk than smaller and less-complex networks, but dispersal bias and magnitude affected the shape of this relationship. Applying these general results to real systems will require empirical data on the movement behavior of organisms and will improve our understanding of the implications of network complexity on population and community patterns and processes.
C1 US Geol Survey, Patuxent Wildlife Res Ctr, Laurel, MD 20708 USA.
RP Grant, EHC (reprint author), US Geol Survey, Patuxent Wildlife Res Ctr, 12100 Beech Forest Rd, Laurel, MD 20708 USA.
EM ehgrant@usgs.gov
RI Grant, Evan/N-5160-2014
OI Grant, Evan/0000-0003-4401-6496
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PU NORTH AMER BENTHOLOGICAL SOC
PI LAWRENCE
PA 1041 NEW HAMSPHIRE STREET, LAWRENCE, KS 66044 USA
SN 0887-3593
J9 J N AM BENTHOL SOC
JI J. N. Am. Benthol. Soc.
PD MAR
PY 2011
VL 30
IS 1
BP 252
EP 258
DI 10.1899/09-120.1
PG 7
WC Ecology; Marine & Freshwater Biology
SC Environmental Sciences & Ecology; Marine & Freshwater Biology
GA 718IP
UT WOS:000287114800020
ER
PT J
AU Maloney, K
Munguia, P
Mitchell, RM
AF Maloney, Kelly O.
Munguia, Pablo
Mitchell, Richard M.
TI Anthropogenic disturbance and landscape patterns affect diversity
patterns of aquatic benthic macroinvertebrates
SO JOURNAL OF THE NORTH AMERICAN BENTHOLOGICAL SOCIETY
LA English
DT Article
DE beta diversity; alpha diversity; multivariate dispersion; nonmetric
multidimensional scaling; ecoregion; scale
ID BETA-DIVERSITY; SPECIES TRAITS; LAND-COVER; HEADWATER STREAMS; FISH
ASSEMBLAGES; HABITAT QUALITY; URBAN LANDSCAPE; UNITED-STATES;
HOMOGENIZATION; COMMUNITIES
AB Measures of species diversity are valuable tools for assessing ecosystem health. However, most assessments have addressed individual sites or regional taxon pools, with few comparisons of differences in assemblage composition within or among regions. We examined the effects of anthropogenic disturbance on local richness (alpha diversity) and species turnover (beta diversity) of benthic macroinvertebrates in small streams within and between 2 ecoregions (Northern Piedmont vs Southeastern Plains ecoregions) of the Patuxent River basin (Maryland, USA). Regional species pools did not differ between ecoregions (Piedmont = 166 taxa, Plains = 162 taxa); however, local richness was lower in the Plains (mean = 17.4 taxa/stream) compared to the Piedmont (mean = 22.2 taxa/stream). When streams were categorized into disturbance classes (low, medium, high), local richness did not differ among categories for either region. However, at the entire Patuxent scale, local richness tended to decrease with % impervious cover in a watershed. Variation in species composition, analyzed with nonmetric multidimensional scaling (nMDS), differed significantly between Piedmont and Plains streams, and Plains streams had higher beta diversity than Piedmont streams. When partitioned by disturbance category and region, beta diversity differed only between the low-disturbance sites (Plains > Piedmont). Relationships between beta diversity and environmental variables varied by region. beta diversity was weakly negatively related to % row-crop cover in a watershed at the entire Patuxent scale. For the Piedmont region, beta diversity tended to decrease with % forest, % pasture, and % row-crop cover in a watershed. Such negative relationships between beta diversity and landuse variables indicate a possible homogenization of the assemblage. The incongruence between diversity measures and composition measures, together with differing effects of anthropogenic land use on beta diversity in the 2 regions, emphasizes the need to incorporate both alpha and beta diversity and regional environmental factors in conservation/land management studies.
C1 [Maloney, Kelly O.] Smithsonian Environm Res Ctr, Edgewater, MD 21037 USA.
[Munguia, Pablo] Univ Texas Austin, Inst Marine Sci, Port Aransas, TX 78373 USA.
[Mitchell, Richard M.] Auburn Univ, Dept Biol Sci, Auburn, AL 36849 USA.
RP Maloney, K (reprint author), US Geol Survey, Leetown Sci Ctr, No Appalachian Res Lab, Wellsboro, PA 16901 USA.
EM kmaloney@usgs.gov; munguia@mail.utexas.edu; mitchrm@auburn.edu
RI Munguia, Pablo/D-8653-2012;
OI Munguia, Pablo/0000-0002-9900-2123
FU US Environmental Protection Agency National Center for Environmental
Research (NCER) [R831369]
FX We thank the Maryland Department of Natural Resources and Ryan King
(Baylor University) for providing data on benthic macroinvertebrates,
and Stephen Prince (University of Maryland) and Scott Goetz (Woods Hole
Research Center) for providing land-cover data. We also thank Kathy
Bailey-Boomer and Donald Weller of the Ecological Modeling lab at the
Smithsonian Environmental Research Center, Chris Swan, and 2 anonymous
referees for instructive comments on the manuscript. Funding for our
work was provided by the US Environmental Protection Agency National
Center for Environmental Research (NCER) Science to Achieve Results
(STAR) grant R831369. The research described in this article was funded
by the US Environmental Protection Agency, but it has not been subjected
to the Agency's required peer and policy review and, therefore, does not
necessarily reflect the views of the Agency, and no official endorsement
should be inferred.
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PI LAWRENCE
PA 1041 NEW HAMSPHIRE STREET, LAWRENCE, KS 66044 USA
SN 0887-3593
J9 J N AM BENTHOL SOC
JI J. N. Am. Benthol. Soc.
PD MAR
PY 2011
VL 30
IS 1
BP 284
EP 295
DI 10.1899/09-112.1
PG 12
WC Ecology; Marine & Freshwater Biology
SC Environmental Sciences & Ecology; Marine & Freshwater Biology
GA 718IP
UT WOS:000287114800023
ER
PT J
AU Hitt, NP
Angermeier, PL
AF Hitt, Nathaniel P.
Angermeier, Paul L.
TI Fish community and bioassessment responses to stream network position
SO JOURNAL OF THE NORTH AMERICAN BENTHOLOGICAL SOCIETY
LA English
DT Article
DE fish community; dispersal; stream network; bioassessment; metacommunity;
zoogeography
ID SPECIES-AREA RELATIONSHIP; ASSEMBLAGE STRUCTURE; BIOTIC INTEGRITY;
WEST-VIRGINIA; SPATIAL POSITION; RIVER; MOVEMENT; HABITAT;
CLASSIFICATION; CONNECTIVITY
AB If organisms move beyond the boundaries of local sampling units, regional metacommunity dynamics could undermine the ability of bioassessment studies to characterize local environmental quality. We tested the prediction that fish dispersal influences local fish community structure and bioassessment metrics as a function of site position within stream networks. We evaluated fish community data from the US Environmental Protection Agency's Regional Environmental Monitoring and Assessment Program in West Virginia, USA, to compare the influences of stream network position, ecoregion, basin, and stream size on local fish community composition. We assigned sites to 1 of 3 stream network positions: 1) main channels (MC, n = 12) encompassed streams with upstream catchment areas >200 km(2), 2) mainstem tributaries (MT, n = 43) flowed into MC-sized confluences within 15 fluvial km, 3) headwater tributaries (HT, n = 31) lacked such riverine confluences within 15 fluvial km. MT and HT sites had similar upstream catchment sizes and landuse gradients, but species richness was greater in MT sites than HT sites, whereas MT and MC sites were not different in this regard. Three bioassessment metrics were greater in MT sites than HT sites (intolerant species richness, cyprinid species richness, benthic species richness), but a multimetric index of biotic integrity did not differ among stream network positions. Ordinations revealed that fish community composition was organized primarily by zoogeographic basin (Monongahela River basin, New River basin, Ohio River basin), ecoregion (Central Appalachian Plateau, Western Appalachian Plateau, Ridge and Valley), and stream size. Riverine specialists were more abundant in MT than HT sites and were more abundant in basins connected to the Ohio River than in basins isolated from the Ohio River by a large waterfall (New River). Our results suggest that contemporary dispersal among streams influences fish community composition over small spatial scales (10(1) km), historical dispersal constrained by zoogeographic barriers influences community structure over larger areas (10(2) km), and contemporary dispersal by fishes influences certain metrics commonly used in bioassessment programs.
C1 [Hitt, Nathaniel P.] US Geol Survey, Leetown Sci Ctr, Aquat Ecol Branch, Kearneysville, WV 25430 USA.
[Angermeier, Paul L.] Virginia Polytech Inst & State Univ, Virginia Cooperat Fish & Wildlife Res Unit, US Geol Survey, Blacksburg, VA 24061 USA.
Virginia Polytech Inst & State Univ, Virginia Dept Game & Inland Fisheries, US Geol Survey, Blacksburg, VA 24061 USA.
Virginia Polytech Inst & State Univ, Wildlife Management Inst, US Geol Survey, Blacksburg, VA 24061 USA.
RP Hitt, NP (reprint author), US Geol Survey, Leetown Sci Ctr, Aquat Ecol Branch, Kearneysville, WV 25430 USA.
EM nhitt@usgs.gov; biota@vt.edu
FU US Geological Survey; Virginia Polytechnic Institute and State
University; Virginia Department of Game and Inland Fisheries; Wildlife
Management Institute; US EPA; US Geological Survey Leetown Science
Center
FX The Unit is jointly sponsored by the US Geological Survey, Virginia
Polytechnic Institute and State University, Virginia Department of Game
and Inland Fisheries, and Wildlife Management Institute.; This research
was supported by a US EPA grant (postdoctoral support for NPH at
Virginia Tech) and the US Geological Survey Leetown Science Center. We
thank D. Cincotta and L. Reynolds for providing raw data for this
analysis. We thank B. Brown and C. Swan for organizing this special
issue and M. Duncan, C. Snyder, B. Brown, J. Young, and M. Mandt for
providing helpful comments on previous drafts of this manuscript. Any
use of trade, product, or firm names does not imply endorsement by the
US government.
NR 52
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PU NORTH AMER BENTHOLOGICAL SOC
PI LAWRENCE
PA 1041 NEW HAMSPHIRE STREET, LAWRENCE, KS 66044 USA
SN 0887-3593
J9 J N AM BENTHOL SOC
JI J. N. Am. Benthol. Soc.
PD MAR
PY 2011
VL 30
IS 1
BP 296
EP 309
DI 10.1899/09-155.1
PG 14
WC Ecology; Marine & Freshwater Biology
SC Environmental Sciences & Ecology; Marine & Freshwater Biology
GA 718IP
UT WOS:000287114800024
ER
PT J
AU Brown, BL
Swan, CM
Auerbach, DA
Grant, EHC
Hitt, NP
Maloney, KO
Patrick, C
AF Brown, Bryan L.
Swan, Christopher M.
Auerbach, Daniel A.
Grant, Evan H. Campbell
Hitt, Nathaniel P.
Maloney, Kelly O.
Patrick, Christopher
TI Metacommunity theory as a multispecies, multiscale framework for
studying the influence of river network structure on riverine
communities and ecosystems
SO JOURNAL OF THE NORTH AMERICAN BENTHOLOGICAL SOCIETY
LA English
DT Article
DE biodiversity; dendritic ecological network; dispersal; drift;
metacommunity ecology; patch dynamics
ID LONG-DISTANCE DISPERSAL; LAND-USE; DIVERSITY PATTERNS; STREAM NETWORKS;
MACROINVERTEBRATE DIVERSITY; ECOLOGICAL COMMUNITIES;
ENVIRONMENTAL-FACTORS; POPULATION-DYNAMICS; RELATIVE IMPORTANCE; SPECIES
COMPOSITION
AB Explaining the mechanisms underlying patterns of species diversity and composition in riverine networks is challenging. Historically, community ecologists have conceived of communities as largely isolated entities and have focused on local environmental factors and interspecific interactions as the major forces determining species composition. However, stream ecologists have long embraced a multiscale approach to studying riverine ecosystems and have studied both local factors and larger-scale regional factors, such as dispersal and disturbance. River networks exhibit a dendritic spatial structure that can constrain aquatic organisms when their dispersal is influenced by or confined to the river network. We contend that the principles of metacommunity theory would help stream ecologists to understand how the complex spatial structure of river networks mediates the relative influences of local and regional control on species composition. From a basic ecological perspective, the concept is attractive because new evidence suggests that the importance of regional processes (dispersal) depends on spatial structure of habitat and on connection to the regional species pool. The role of local factors relative to regional factors will vary with spatial position in a river network. From an applied perspective, the long-standing view in ecology that local community composition is an indicator of habitat quality may not be uniformly applicable across a river network, but the strength of such bioassessment approaches probably will depend on spatial position in the network. The principles of metacommunity theory are broadly applicable across taxa and systems but seem of particular consequence to stream ecology given the unique spatial structure of riverine systems. By explicitly embracing processes at multiple spatial scales, metacommunity theory provides a foundation on which to build a richer understanding of stream communities.
C1 [Brown, Bryan L.] Clemson Univ, Dept Forestry & Nat Resources, Clemson, SC 29634 USA.
[Swan, Christopher M.] Univ Maryland, Dept Geog & Environm Syst, Baltimore, MD 21250 USA.
[Auerbach, Daniel A.] Colorado State Univ, Dept Biol, Ft Collins, CO 80523 USA.
[Grant, Evan H. Campbell] US Geol Survey, Patuxent Wildlife Ctr, NE Amphibian Res & Monitoring Initiat, Laurel, MD 20708 USA.
[Hitt, Nathaniel P.] US Geol Survey, Leetown Sci Ctr, Aquat Ecol Branch, Kearneysville, WV 25430 USA.
[Maloney, Kelly O.] US Geol Survey, Leetown Sci Ctr, No Appalachian Res Lab, Wellsboro, PA 16901 USA.
[Patrick, Christopher] Univ Notre Dame, Dept Biol Sci, Notre Dame, IN 46556 USA.
RP Brown, BL (reprint author), Clemson Univ, Dept Forestry & Nat Resources, Clemson, SC 29634 USA.
EM bbrown3@clemson.edu; cmswan@umbc.edu; auerbach.dan@gmail.com;
ehgrant@usgs.gov; nhitt@usgs.gov; kmaloney@usgs.gov; cjpaster@gmail.com
RI Brown, Bryan/D-9726-2014; Grant, Evan/N-5160-2014;
OI Grant, Evan/0000-0003-4401-6496; Swan, Christopher/0000-0002-9763-9630
FU NSF [DEB-1025958]
FX This contribution was the result of a special session on river networks
at the 2009 annual meeting of the North American Benthological Society
in Grand Rapids, Michigan, USA. We would like to thank the organizers of
the meeting for offering us that opportunity. We would especially like
to thank Pamela Silver, editor of J-NABS, for guiding us through the
editorial issues associated with putting together this special section
of J-NABS. In addition, LeRoy Poff advised and acted as guest editor for
several of the contributions. We also thank Jenna Stanek and James
Skelton who offered their opinions on early versions of the manuscript,
and Mathew Leibold who did not realize how closely his postdoc (BLB) was
listening to those metacommunity conversations when he was supposed to
be working on something else. We thank Laura E. Smith, the talented
artist who provided macroinvertebrate illustrations for Fig. 2. BLB and
CMS acknowledge funding assistance from NSF DEB-1025958. This manuscript
is contribution number 409 of the Amphibian Research and Monitoring
Initiative (ARMI) of the US Geological Survey.
NR 177
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U2 113
PU NORTH AMER BENTHOLOGICAL SOC
PI LAWRENCE
PA 1041 NEW HAMSPHIRE STREET, LAWRENCE, KS 66044 USA
SN 0887-3593
J9 J N AM BENTHOL SOC
JI J. N. Am. Benthol. Soc.
PD MAR
PY 2011
VL 30
IS 1
BP 310
EP 327
DI 10.1899/10-129.1
PG 18
WC Ecology; Marine & Freshwater Biology
SC Environmental Sciences & Ecology; Marine & Freshwater Biology
GA 718IP
UT WOS:000287114800025
ER
PT J
AU Brubaker, JL
Karouna-Renier, NK
Chen, Y
Jenko, K
Sprague, DT
Henry, PFP
AF Brubaker, Jessica L.
Karouna-Renier, Natalie K.
Chen, Yu
Jenko, Kathryn
Sprague, Daniel T.
Henry, Paula F. P.
TI A noninvasive, direct real-time PCR method for sex determination in
multiple avian species
SO MOLECULAR ECOLOGY RESOURCES
LA English
DT Article
DE birds; molecular sexing; noninvasive sampling; real-time PCR
ID NON-RATITE BIRDS
AB Polymerase chain reaction (PCR)-based methods to determine the sex of birds are well established and have seen few modifications since they were first introduced in the 1990s. Although these methods allowed for sex determination in species that were previously difficult to analyse, they were not conducive to high-throughput analysis because of the laboriousness of DNA extraction and gel electrophoresis. We developed a high-throughput real-time PCR-based method for analysis of sex in birds, which uses noninvasive sample collection and avoids DNA extraction and gel electrophoresis.
C1 [Brubaker, Jessica L.; Karouna-Renier, Natalie K.; Chen, Yu; Jenko, Kathryn; Sprague, Daniel T.; Henry, Paula F. P.] USGS, Patuxent Wildlife Res Ctr, Beltsville, MD 20705 USA.
[Chen, Yu] Virginia Tech, Dept Fisheries & Wildlife Sci, Blacksburg, VA 24061 USA.
RP Karouna-Renier, NK (reprint author), USGS, Patuxent Wildlife Res Ctr, BARC E Bldg 308,10300 Baltimore Ave, Beltsville, MD 20705 USA.
EM nkarouna@usgs.gov
OI Karouna-Renier, Natalie/0000-0001-7127-033X
FU US Environmental Protection Agency; US Geological Survey
FX Funding for the work was provided by the US Environmental Protection
Agency and the US Geological Survey. Use of product names does not imply
endorsement by the US Government.
NR 6
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U1 1
U2 13
PU WILEY-BLACKWELL
PI MALDEN
PA COMMERCE PLACE, 350 MAIN ST, MALDEN 02148, MA USA
SN 1755-098X
J9 MOL ECOL RESOUR
JI Mol. Ecol. Resour.
PD MAR
PY 2011
VL 11
IS 2
BP 415
EP 417
DI 10.1111/j.1755-0998.2010.02951.x
PG 3
WC Biochemistry & Molecular Biology; Ecology; Evolutionary Biology
SC Biochemistry & Molecular Biology; Environmental Sciences & Ecology;
Evolutionary Biology
GA 719JE
UT WOS:000287200200028
PM 21429156
ER
PT J
AU Pattison, RR
D'Antonio, CM
Dudley, TL
Allander, KK
Rice, B
AF Pattison, Robert R.
D'Antonio, Carla M.
Dudley, Tom L.
Allander, Kip K.
Rice, Benjamin
TI Early impacts of biological control on canopy cover and water use of the
invasive saltcedar tree (Tamarix spp.) in western Nevada, USA
SO OECOLOGIA
LA English
DT Article
DE Defoliation; Evapotranspiration; Herbivory; Sap flow
ID MOJAVE DESERT FLOODPLAIN; EDDY COVARIANCE; UNITED-STATES; LEAF BEETLE;
RIPARIAN RESTORATION; RAMOSISSIMA STANDS; SAP FLUX; EVAPOTRANSPIRATION;
TRANSPIRATION; DEFOLIATION
AB The success of biological control programs is rarely assessed beyond population level impacts on the target organism. The question of whether a biological control agent can either partially or completely restore ecosystem services independent of population level control is therefore still open to discussion. Using observational and experimental approaches, we investigated the ability of the saltcedar leaf beetle [Diorhabda carinulata (Brull,) (Coleoptera: Chrysomelidae)] to reduce the water use of saltcedar trees (Tamarix ramosissima Ledeb.) in two sites (Humboldt and Walker Rivers) in Nevada, USA. At these sites D. carinulata defoliated the majority of trees within 25 and 9 km, respectively, of the release location within 3 years. At the Humboldt site, D. carinulata reduced the canopy cover of trees adjacent to the release location by > 90%. At a location 4 km away during the first year of defoliation, D. carinulata reduced peak (August) stem water use by 50-70% and stand transpiration (July to late September) by 75% (P = 0.052). There was, however, no reduction in stem water use and stand transpiration during the second year of defoliation due to reduced beetle abundances at that location. At the Walker site, we measured stand evapotranspiration (ET) in the center of a large saltcedar stand and found that ET was highest immediately prior to D. carinulata arrival, dropped dramatically with defoliation, and remained low through the subsequent 2 years of the study. In contrast, near the perimeter of the stand, D. carinulata did not reduce sap flow, partly because of low rates of defoliation but also because of increased water use per unit leaf area in response to defoliation. Taken together, our results provide evidence that in the early stages of population expansion D. carinulata can lead to substantial declines in saltcedar water use. The extent of these declines varies spatially and temporally and is dependent on saltcedar compensatory responses along with D. carinulata population dynamics and patterns of dispersal.
C1 [Pattison, Robert R.; D'Antonio, Carla M.; Rice, Benjamin] USDA ARS, Exot & Invas Weed Res Unit, Reno, NV USA.
[Dudley, Tom L.] Univ Nevada, Dept Nat Resources & Environm Sci, Reno, NV 89557 USA.
[Allander, Kip K.] US Geol Survey, Reno, NV USA.
[Pattison, Robert R.] USDA FS, Anchorage Forestry Sci Lab, Anchorage, AK USA.
[Dudley, Tom L.] Univ Calif Santa Barbara, Inst Marine Sci, Santa Barbara, CA 93106 USA.
RP Pattison, RR (reprint author), USDA ARS, Exot & Invas Weed Res Unit, Reno, NV USA.
EM rrpattison@fs.fed.us
NR 40
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U1 4
U2 28
PU SPRINGER
PI NEW YORK
PA 233 SPRING ST, NEW YORK, NY 10013 USA
SN 0029-8549
J9 OECOLOGIA
JI Oecologia
PD MAR
PY 2011
VL 165
IS 3
BP 605
EP 616
DI 10.1007/s00442-010-1859-y
PG 12
WC Ecology
SC Environmental Sciences & Ecology
GA 721NL
UT WOS:000287361500007
PM 21153743
ER
PT J
AU Newton, TJ
Zigler, SJ
Rogala, JT
Gray, BR
Davis, M
AF Newton, Teresa J.
Zigler, Steven J.
Rogala, James T.
Gray, Brian R.
Davis, Mike
TI Population assessment and potential functional roles of native mussels
in the Upper Mississippi River
SO AQUATIC CONSERVATION-MARINE AND FRESHWATER ECOSYSTEMS
LA English
DT Article
DE native mussels; large rivers; population assessment; abundance;
ecosystem services
ID FRESH-WATER MUSSELS; LAKE ST-CLAIR; UNIONID MUSSELS; ASSEMBLAGE
STRUCTURE; NORTH-AMERICA; ZEBRA MUSSELS; HUDSON RIVER; BIVALVIA; STREAM;
ABUNDANCE
AB 1. Despite a heightened global concern for native mussels, fundamental research on mussel ecology in large rivers is lacking. These gaps in knowledge about where mussels occur, and why, are limiting habitat restoration activities.
2. Large-scale systematic surveys for native mussels in three reaches of the Upper Mississippi River documented mussel communities composed of 16-23 species and ranging from 2.9-4.5 live mussels m(-2) that were actively recruiting new cohorts into their populations (87-100% of the species were found as juveniles <= 5 years old). Estimates of mean tissue biomass and production in these reaches ranged from 2.1-3.1 g Cm-2 and 0.4-0.6 g Cm-2 year(-1), respectively.
3. Mussels filtered a significant amount of water (range, 0.05-0.07 m(3) m(-2) d(-1)) over a 480 km reach of the Upper Mississippi River - amounting to a filtration rate of 53.1 million m(3) day(-1). The filtration rate of mussels as a percentage of river discharge ranged from 0.5-1.4% at high flows (5% exceedance), from 1.5-4.4% at moderate flows (50% exceedance) and from 4.4-12.2% during low flows (95% exceedance).
4. Collectively, these data suggest that native mussels play an integral role in this ecosystem by sequestering suspended materials that can be used by other benthic organisms. Published in 2011 by John Wiley and Sons, Ltd.
C1 [Newton, Teresa J.; Zigler, Steven J.; Rogala, James T.; Gray, Brian R.] US Geol Survey, Upper Midwest Environm Sci Ctr, La Crosse, WI 54603 USA.
[Davis, Mike] MN Dept Nat Resources, Lake City, MN USA.
RP Newton, TJ (reprint author), US Geol Survey, Upper Midwest Environm Sci Ctr, 2630 Fanta Reed Rd, La Crosse, WI 54603 USA.
EM tnewton@usgs.gov
OI Zigler, Steven/0000-0002-4153-0652; Gray, Brian/0000-0001-7682-9550;
Newton, Teresa/0000-0001-9351-5852
FU US Army Corps of Engineers
FX This study was partially funded by the US Army Corps of Engineers. We
thank John Kern for survey design, Heidi Dunn and Dave Heath for
technical assistance, and Barry Johnson, Rita Villella, Wendell Haag,
Jon Duyvejonck, and David Strayer for useful discussions and comments on
the manuscript. Product names are provided for informational purposes
only and do not represent an endorsement by the US Geological Survey.
NR 55
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U1 2
U2 27
PU WILEY-BLACKWELL
PI MALDEN
PA COMMERCE PLACE, 350 MAIN ST, MALDEN 02148, MA USA
SN 1052-7613
J9 AQUAT CONSERV
JI Aquat. Conserv.-Mar. Freshw. Ecosyst.
PD MAR-APR
PY 2011
VL 21
IS 2
BP 122
EP 131
DI 10.1002/aqc.1170
PG 10
WC Environmental Sciences; Marine & Freshwater Biology; Water Resources
SC Environmental Sciences & Ecology; Marine & Freshwater Biology; Water
Resources
GA 737BT
UT WOS:000288543900003
ER
PT J
AU Crago, J
Corsi, SR
Weber, D
Bannerman, R
Klaper, R
AF Crago, Jordan
Corsi, Steven R.
Weber, Daniel
Bannerman, Roger
Klaper, Rebecca
TI Linking biomarkers to reproductive success of caged fathead minnows in
streams with increasing urbanization
SO CHEMOSPHERE
LA English
DT Article
DE Fathead minnow; Biomarker; Vitellogenin; GST; Urbanization; Reproduction
ID PIMEPHALES-PROMELAS; RISK-ASSESSMENT; FISH; EXPOSURE; IMPACT
AB Reproductive and oxidative stress biomarkers have been recommended as tools to assess the health of aquatic organisms. Though validated in the laboratory, there are few studies that tie a change in gene expression to adverse reproductive or population outcomes in the field. This paper looked at 17 streams with varying degrees of urbanization to assess the use of biomarkers associated with reproduction or stress in predicting reproductive success of fathead minnows. In addition, the relationship between biomarkers and water quality measures in streams with varying degrees of urbanization was examined. Liver vitellogenin mRNA was correlated with reproduction within a period of 11 d prior to sampling irrespective of habitat, but its correlation with egg output declined at 12 d and beyond indicating its usefulness as a short-term biomarker but its limits as a biomarker of total reproductive output. Stress biomarkers such as glutathione S-transferase may be better correlated with factors affecting reproduction over a longer term. There was a significant correlation between GST mRNA and a variety of anthropogenic pollutants. There was also an inverse correlation between glutathione S-transferase and the amount of the watershed designated as wetland. Egg production over the 21-d was negatively correlated with the amount of urbanization and positively correlated to wetland habitats. This study supports the development of multiple biomarkers linking oxidative stress and other non-reproductive endpoints to changes in aquatic habitats will be useful for predicting the health of fish populations and identifying the environmental factors that may need mitigation for sustainable population management. (C) 2010 Elsevier Ltd. All rights reserved.
C1 [Crago, Jordan; Klaper, Rebecca] Univ Wisconsin, Sch Freshwater Sci, Great Lakes WATER Inst, Milwaukee, WI 53204 USA.
[Corsi, Steven R.] US Geol Survey, Wisconsin Water Sci Ctr, Middleton, WI 53562 USA.
[Weber, Daniel] Univ Wisconsin, Childrens Environm Hlth Sci Ctr, Milwaukee, WI 53204 USA.
[Bannerman, Roger] Wisconsin Dept Nat Resources, Madison, WI 53703 USA.
RP Klaper, R (reprint author), Univ Wisconsin, Sch Freshwater Sci, Great Lakes WATER Inst, 600 E Greenfield Ave, Milwaukee, WI 53204 USA.
EM rklaper@uwm.edu
FU Wisconsin Department of Natural Resources; Greater Milwaukee Foundation
FX This study was financed by a grant from the Wisconsin Department of
Natural Resources and the Dorothy Shaw Fund through the Greater
Milwaukee Foundation.
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PU PERGAMON-ELSEVIER SCIENCE LTD
PI OXFORD
PA THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND
SN 0045-6535
J9 CHEMOSPHERE
JI Chemosphere
PD MAR
PY 2011
VL 82
IS 11
BP 1669
EP 1674
DI 10.1016/j.chemosphere.2010.11.011
PG 6
WC Environmental Sciences
SC Environmental Sciences & Ecology
GA 737SG
UT WOS:000288587900021
PM 21147497
ER
PT J
AU Paukert, CP
Pitts, KL
Whittier, JB
Olden, JD
AF Paukert, Craig P.
Pitts, Kristen L.
Whittier, Joanna B.
Olden, Julian D.
TI Development and assessment of a landscape-scale ecological threat index
for the Lower Colorado River Basin
SO ECOLOGICAL INDICATORS
LA English
DT Article
DE Anthropogenic threats; Ecological stressors; Freshwater conservation
planning; Lower Colorado River Basin
ID MULTIPLE SPATIAL SCALES; FISH ASSEMBLAGES; FRESH-WATER; LAND-USE;
SOUTHWESTERN FISHES; WISCONSIN STREAMS; BIOTIC INTEGRITY; ECOSYSTEMS;
GRADIENTS; HABITAT
AB Anthropogenic disturbances impact freshwater biota but are rarely incorporated into conservation planning due to the difficulties in quantifying threats. There is currently no widely accepted method to quantify disturbances, and determining how to measure threats to upstream catchments using disturbance metrics can be time consuming and subjective. We compared four watershed-scale ecological threat indices for the Lower Colorado River Basin (LCRB) using landscape-level threats of land use (e.g., agricultural and urban lands), waterway development and diversions (e.g., number of canals, dams), and human development (e.g., road and railroads density, pollution sites). The LCRB is an ideal region to assess ecological threat indices because of the increasing need for conservation to ensure the persistence of native fishes in highly altered habitat. Each threat was measured for severity (i.e., level of influence on the upstream watershed) and frequency throughout each watershed; both severity and frequency were measured using two different methods. Severity values were based either on peer-reviewed literature and weighted in accordance to their published ecological impact, or assumed equal severity across stressors. Threat frequency was calculated according to either the presence/absence of each stressor, or on the relative density of each stressor in the watershed. Each measure of severity was combined with a measure of frequency, creating four ecological threat indices, and transformed to a 0-100 scale. Threat indices were highly correlated (slopes of 0.94-1.63; R(2) of 0.82-0.98), and were highest for watersheds close to urban centers, including Phoenix, Tucson, and Flagstaff. Arizona, and Las Vegas, Nevada. Road crossings and density appeared to be the most influential stressors in the index, but the removal of any individual stressor only changed the index by <5.1 units. Our results indicate that a simpler index with less subjectivity (i.e., presence/absence of a stressor in a watershed) provides similar results to the more subjective measure of threats (i.e., peer-reviewed threat severity). Because these threats have been linked to ecological health, the development of the index should be a useful tool to identify regions of greatest potential threat to aquatic biota and can aid in conservation planning for the Lower Colorado River Basin. (C) 2010 Published by Elsevier Ltd.
C1 [Paukert, Craig P.] Kansas State Univ, US Geol Survey, Kansas Cooperat Fish & Wildlife Res Unit, Div Biol, Manhattan, KS 66506 USA.
[Olden, Julian D.] Univ Washington, Sch Aquat & Fishery Sci, Seattle, WA 98195 USA.
RP Paukert, CP (reprint author), Univ Missouri, US Geol Survey, Missouri Cooperat Fish & Wildlife Res Unit, Dept Fisheries & Wildlife Sci, 302 ABNR Bldg, Columbia, MO 65211 USA.
EM paukertc@missouri.edu; pitts.kris@gmail.com; whittierj@missouri.edu;
olden@u.washington.edu
RI Olden, Julian/A-8535-2010;
OI Olden, Julian/0000-0003-2143-1187; Bouska, Kristen/0000-0002-4115-2313
FU USGS; Kansas Department of Wildlife and Parks, Kansas State University;
U.S. Geological Survey; Wildlife Management Institute
FX We thank everyone who contributed data and knowledge to the Lower
Colorado River Basin Aquatic Gap Analysis Project. We thank Brad Schmidt
for database management, and Keith Gido and two anonymous reviewers for
comments on earlier manuscript drafts. Funding was provided by the USGS
Gap Analysis Program. The use of trade, product, industry names or
products does not constitute an endorsement by the U.S. Government, the
U.S. Geological Survey or other sponsoring or participating agencies.
The Kansas Cooperative Fish and Wildlife Research Unit is sponsored by
the Kansas Department of Wildlife and Parks, Kansas State University,
the U.S. Geological Survey, and the Wildlife Management Institute.
NR 38
TC 21
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U1 4
U2 40
PU ELSEVIER SCIENCE BV
PI AMSTERDAM
PA PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS
SN 1470-160X
J9 ECOL INDIC
JI Ecol. Indic.
PD MAR
PY 2011
VL 11
IS 2
BP 304
EP 310
DI 10.1016/j.ecolind.2010.05.008
PG 7
WC Biodiversity Conservation; Environmental Sciences
SC Biodiversity & Conservation; Environmental Sciences & Ecology
GA 690UW
UT WOS:000285035000010
ER
PT J
AU Firn, J
Moore, JL
MacDougall, AS
Borer, ET
Seabloom, EW
HilleRisLambers, J
Harpole, WS
Cleland, EE
Brown, CS
Knops, JMH
Prober, SM
Pyke, DA
Farrell, KA
Bakker, JD
O'Halloran, LR
Adler, PB
Collins, SL
D'Antonio, CM
Crawley, MJ
Wolkovich, EM
La Pierre, KJ
Melbourne, BA
Hautier, Y
Morgan, JW
Leakey, ADB
Kay, A
McCulley, R
Davies, KF
Stevens, CJ
Chu, CJ
Holl, KD
Klein, JA
Fay, PA
Hagenah, N
Kirkman, KP
Buckley, YM
AF Firn, Jennifer
Moore, Joslin L.
MacDougall, Andrew S.
Borer, Elizabeth T.
Seabloom, Eric W.
HilleRisLambers, Janneke
Harpole, W. Stanley
Cleland, Elsa E.
Brown, Cynthia S.
Knops, Johannes M. H.
Prober, Suzanne M.
Pyke, David A.
Farrell, Kelly A.
Bakker, John D.
O'Halloran, Lydia R.
Adler, Peter B.
Collins, Scott L.
D'Antonio, Carla M.
Crawley, Michael J.
Wolkovich, Elizabeth M.
La Pierre, Kimberly J.
Melbourne, Brett A.
Hautier, Yann
Morgan, John W.
Leakey, Andrew D. B.
Kay, Adam
McCulley, Rebecca
Davies, Kendi F.
Stevens, Carly J.
Chu, Cheng-Jin
Holl, Karen D.
Klein, Julia A.
Fay, Philip A.
Hagenah, Nicole
Kirkman, Kevin P.
Buckley, Yvonne M.
TI Abundance of introduced species at home predicts abundance away in
herbaceous communities
SO ECOLOGY LETTERS
LA English
DT Letter
DE Biogeography; biosecurity; disturbance; global meta-study;
homogenization of communities; invasion paradox; mechanisms of invasion;
Nutrient Network; plant invasion; propagule pressure
ID PLANT INVASIONS; CONSERVATION; HYPOTHESIS; INVASIVENESS; CONSEQUENCES;
PASSENGERS; INVADERS; PARADOX; DRIVERS; SUCCESS
AB P>Many ecosystems worldwide are dominated by introduced plant species, leading to loss of biodiversity and ecosystem function. A common but rarely tested assumption is that these plants are more abundant in introduced vs. native communities, because ecological or evolutionary-based shifts in populations underlie invasion success. Here, data for 26 herbaceous species at 39 sites, within eight countries, revealed that species abundances were similar at native (home) and introduced (away) sites - grass species were generally abundant home and away, while forbs were low in abundance, but more abundant at home. Sites with six or more of these species had similar community abundance hierarchies, suggesting that suites of introduced species are assembling similarly on different continents. Overall, we found that substantial changes to populations are not necessarily a pre-condition for invasion success and that increases in species abundance are unusual. Instead, abundance at home predicts abundance away, a potentially useful additional criterion for biosecurity programmes.
C1 [Firn, Jennifer; Buckley, Yvonne M.] CSIRO Ecosyst Sci, St Lucia, Qld 4067, Australia.
[Moore, Joslin L.] Univ Melbourne, Sch Bot, AEDA, Parkville, Vic 3010, Australia.
[MacDougall, Andrew S.] Univ Guelph, Dept Integrat Biol, Guelph, ON N1G 2W1, Canada.
[Borer, Elizabeth T.; Seabloom, Eric W.; O'Halloran, Lydia R.] Univ Minnesota, Dept Ecol Evolut & Behav, St Paul, MN 55108 USA.
[HilleRisLambers, Janneke] Univ Washington, Dept Biol, Seattle, WA 98195 USA.
[Harpole, W. Stanley] Iowa State Univ, Ames, IA 50011 USA.
[Cleland, Elsa E.] Univ Calif San Diego, Ecol Behav Evolut Sect, La Jolla, CA 92093 USA.
[Brown, Cynthia S.] Colorado State Univ, Dept Bioagr Sci & Pest Management, Ft Collins, CO 80523 USA.
[Knops, Johannes M. H.] Univ Nebraska, Sch Biol Sci, Lincoln, NE 68588 USA.
[Prober, Suzanne M.] CSIRO Ecosyst Sci, Wembley, WA 6913, Australia.
[Pyke, David A.] US Geol Survey Forest Rangeland Ecosys Sci Ctr, Corvallis, OR 97331 USA.
[Farrell, Kelly A.] Oregon State Univ, Dept Zool, Corvallis, OR 97331 USA.
[Bakker, John D.] Univ Washington, Sch Forest Resources, Seattle, WA 98195 USA.
[Adler, Peter B.] Utah State Univ, Dept Wildland Resources, Logan, UT 84322 USA.
[Adler, Peter B.] Utah State Univ, Ctr Ecol, Logan, UT 84322 USA.
[Collins, Scott L.] Univ New Mexico, Dept Biol, Albuquerque, NM 87131 USA.
[D'Antonio, Carla M.] Univ Calif Santa Barbara, Dept Ecol Evolut & Marine Biol, Santa Barbara, CA 93106 USA.
[Crawley, Michael J.] Imperial Coll London, Dept Biol, Ascot SL5 7PY, Berks, England.
[Wolkovich, Elizabeth M.] Natl Ctr Ecol Anal & Synth, Santa Barbara, CA 93101 USA.
[La Pierre, Kimberly J.; Hagenah, Nicole] Yale Univ, Dept Ecol Evolutionary Biol, New Haven, CT 06520 USA.
[Melbourne, Brett A.; Davies, Kendi F.] Univ Colorado, Dept Ecol & Evolutionary Biol, Boulder, CO 80309 USA.
[Hautier, Yann] Univ Zurich, Inst Evolutionary Biol Environm Studies, CH-8057 Zurich, Switzerland.
[Morgan, John W.] La Trobe Univ, Dept Bot, Bundoora, Vic 3086, Australia.
[Leakey, Andrew D. B.] Univ Illinois, Inst Genom Biol, Dept Plant Biol, Urbana, IL 61821 USA.
[Kay, Adam] Univ St Thomas, Dept Biol, St Paul, MN 55105 USA.
[McCulley, Rebecca] Univ Kentucky, Dept Plant Soil Sci, Lexington, KY 40546 USA.
[Stevens, Carly J.] Open Univ, Dept Life Sci, Milton Keynes MK7 6AA, Bucks, England.
[Chu, Cheng-Jin] Lanzhou Univ, MOE Key Lab Arid Grassland Ecol, Lanzhou 730000, Peoples R China.
[Holl, Karen D.] Univ Calif Santa Cruz, Dept Environm Studies, Santa Cruz, CA 95064 USA.
[Klein, Julia A.] Colorado State Univ, Nat Resource Ecol Lab, Ft Collins, CO 80523 USA.
[Fay, Philip A.] USDA ARS, Grassland Soil & Water Res Lab, Temple, TX 76502 USA.
[Hagenah, Nicole; Kirkman, Kevin P.] Univ KwaZulu Natal, Sch Biol Conservat Sci, ZA-3209 Pietermaritzburg, South Africa.
[Buckley, Yvonne M.] Univ Queensland, Sch Biol Sci, Brisbane, Qld 4072, Australia.
RP Firn, J (reprint author), Queensland Univ Technol, Sch Biogeosci, Brisbane, Qld 4001, Australia.
EM jennifer.firn@qut.edu.au
RI Prober, Suzanne/G-6465-2010; Adler, Peter/D-3781-2009; MacDougall,
Andrew/F-2037-2011; Moore, Joslin/C-5270-2009; Brown,
Cynthia/K-5814-2012; Harpole, William/C-2814-2013; Buckley,
Yvonne/B-1281-2008; Bakker, Jonathan/I-6960-2013; Holl,
Karen/D-8033-2014; Hautier, Yann/D-5426-2015; Collins,
Scott/P-7742-2014; Leakey, Andrew/Q-9889-2016
OI Firn, Jennifer/0000-0001-6026-8912; Seabloom, Eric/0000-0001-6780-9259;
Fay, Philip/0000-0002-8291-6316; Borer, Elizabeth/0000-0003-2259-5853;
La Pierre, Kimberly/0000-0001-7056-4547; Moore,
Joslin/0000-0001-9809-5092; Harpole, William/0000-0002-3404-9174;
Buckley, Yvonne/0000-0001-7599-3201; Holl, Karen/0000-0003-2893-6161;
Hautier, Yann/0000-0003-4347-7741; Collins, Scott/0000-0002-0193-2892;
Leakey, Andrew/0000-0001-6251-024X
NR 52
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Z9 38
U1 5
U2 94
PU WILEY-BLACKWELL
PI MALDEN
PA COMMERCE PLACE, 350 MAIN ST, MALDEN 02148, MA USA
SN 1461-023X
J9 ECOL LETT
JI Ecol. Lett.
PD MAR
PY 2011
VL 14
IS 3
BP 274
EP 281
DI 10.1111/j.1461-0248.2010.01584.x
PG 8
WC Ecology
SC Environmental Sciences & Ecology
GA 723SZ
UT WOS:000287528600009
PM 21281419
ER
PT J
AU Belovsky, GE
Stephens, D
Perschon, C
Birdsey, P
Paul, D
Naftz, D
Baskin, R
Larson, C
Mellison, C
Luft, J
Mosley, R
Mahon, H
Van Leeuwen, J
Allen, DV
AF Belovsky, Gary E.
Stephens, Doyle
Perschon, Clay
Birdsey, Paul
Paul, Don
Naftz, David
Baskin, Robert
Larson, Chad
Mellison, Chad
Luft, John
Mosley, Ryan
Mahon, Heidi
Van Leeuwen, James
Allen, David V.
TI The Great Salt Lake Ecosystem (Utah, USA): long term data and a
structural equation approach
SO ECOSPHERE
LA English
DT Article
DE Artemia franciscana; brine shrimp; food webs; Great Salt Lake; Utah;
hypersaline; phytoplankton; Podiceps nigricollis; terminal lake;
waterbirds
AB Great Salt Lake (Utah, USA) is one of the world's largest hypersaline lakes, supporting many of the western U.S.'s migratory waterbirds. This unique ecosystem is threatened, but it and other large hypersaline lakes are not well understood. The ecosystem consists of two weakly linked food webs: one phytoplankton-based, the other organic particle/benthic algae-based.
Seventeen years of data on the phytoplankton-based food web are presented: abundances of nutrients (N and P), phytoplankton (Chlorophyta, Bacillariophyta, Cyanophyta), brine shrimp (Artemia franciscana), corixids (Trichocorixa verticalis), and Eared Grebes (Podiceps nigricollis). Abundances of less common species, as well as brine fly larvae (Ephydra cinerea and hians) from the organic particle/benthic algae-based food web are also presented. Abiotic parameters were monitored: lake elevation, temperature, salinity, PAR, light penetration, and DO. We use these data to test hypotheses about the phytoplankton-based food web and its weak linkage with the organic particle/benthic algae-based food web via structural equation modeling.
Counter to common perceptions, the phytoplankton-based food web is not limited by high salinity, but principally through phytoplankton production, which is limited by N and grazing by brine shrimp. Annual N abundance is highly variable and depends on lake volume, complex mixing given thermo- and chemo-clines, and recycling by brine shrimp. Brine shrimp are food-limited, and predation by corixids and Eared Grebes does not depress their numbers. Eared Grebe numbers appear to be limited by brine shrimp abundance. Finally, there is little interaction of brine fly larvae with brine shrimp through competition, or with corixids or grebes through predation, indicating that the lake's two food webs are weakly connected.
Results are used to examine some general concepts regarding food web structure and dynamics, as well as the lake's future given expected anthropogenic impacts.
C1 [Belovsky, Gary E.; Larson, Chad; Mahon, Heidi] Univ Notre Dame, Environm Res Ctr, Notre Dame, IN 46556 USA.
[Stephens, Doyle; Naftz, David; Baskin, Robert; Allen, David V.] US Geol Survey, Salt Lake City, UT 84119 USA.
[Perschon, Clay; Birdsey, Paul; Paul, Don; Luft, John; Mosley, Ryan; Van Leeuwen, James] Utah Div Wildlife Resources, Salt Lake City, UT 84114 USA.
[Mellison, Chad] US Fish & Wildlife Serv, Reno, NV 89502 USA.
RP Belovsky, GE (reprint author), Univ Notre Dame, Environm Res Ctr, Notre Dame, IN 46556 USA.
EM belovsky.1@nd.edu
RI Belovsky, Gary/C-1255-2014
FU Utah Division of Wildlife Resources; National Science Foundation [DEB-
9322576]; U.S. Geological Survey
FX We wish to thank the Great Salt Lake Ecosystem Program, Utah Division of
Wildlife Resources (to GEB, DS, DN, RB), National Science Foundation (to
GEB, DEB- 9322576), and U.S. Geological Survey (to DS, DN, RB) for
funding. The Great Salt Lake Technical Advisory Group provided feedback.
S. Kilham, B. Marden and J. Butler provided discussion on data and
methods. We thank T. Crowl, J. Slade, J. Neill and W. Wurtsbaugh for
comments.
NR 150
TC 14
Z9 14
U1 4
U2 41
PU ECOLOGICAL SOC AMER
PI WASHINGTON
PA 1990 M STREET NW, STE 700, WASHINGTON, DC 20036 USA
SN 2150-8925
J9 ECOSPHERE
JI Ecosphere
PD MAR
PY 2011
VL 2
IS 3
AR UNSP 33
DI 10.1890/ES10-00091.1
PG 40
WC Ecology
SC Environmental Sciences & Ecology
GA V30IT
UT WOS:000208810400009
ER
PT J
AU Kurth, G
Phillips, FM
Reheis, MC
Redwine, JL
Paces, JB
AF Kurth, Gabrielle
Phillips, Fred M.
Reheis, Marith C.
Redwine, Joanna L.
Paces, James B.
TI Cosmogenic nuclide and uranium-series dating of old, high shorelines in
the western Great Basin, USA
SO GEOLOGICAL SOCIETY OF AMERICA BULLETIN
LA English
DT Article
ID LAKE LAHONTAN HIGHSTAND; BONNEVILLE-BASIN; SOIL DEVELOPMENT;
SIERRA-NEVADA; UNITED-STATES; OWENS LAKE; LATE PLEISTOCENE; VOLCANIC
FIELD; TUFA DEPOSITS; MOJAVE DESERT
AB Closed-basin pluvial lakes are sensitive recorders of effective moisture, and they provide a terrestrial signal of climate change that can be compared to marine and ice records of glacial-interglacial cycles. Although the most recent deep-lake cycle in the western Great Basin (at ca. 16 ka) has been studied intensively, comparatively little is known about the longer-term Quaternary lacustrine history of the region. Lacustrine features higher than those of the most recent highstand have been discovered in many locations throughout the western Great Basin. Qualitative geomorphic and soil studies of shoreline sequences above the latest Pleistocene level suggest that their ages increase as a function of increasing altitude.
The results of cosmogenic nuclide dating using chlorine-36 depth profiles from three sites in Nevada (Walker Lake, Columbus Salt Marsh, and Newark Valley), combined with uranium-series and radiocarbon ages, corroborate the geomorphic and soil evidence. The Cl-36 results are consistent with available C-14 ages and together indicate that the most recent highstands of all three lakes occurred ca. 20-15 ka, late in marine isotope stage (MIS) 2, as shown by previous ages. The Cl-36 ages indicate that older lakes in all three basins reached highstands between 100 and 50 ka, and most likely during MIS 4. Shorelines of this age are at about the same or higher altitudes as the younger, MIS 2 shorelines in those basins. The Cl-36 results combined with uranium-series ages and one tephra correlation obtained on shorelines higher in altitude than those of MIS 4 and 2 lakes suggest that there were also major lake highstands in the western Great Basin at ca. 100-200 ka, likely corresponding with MIS 6, and during at least two older periods. From these results, we conclude that the preserved shorelines show an apparent decrease in maximum levels with time, suggesting long-term drying of the region since the early middle Pleistocene.
C1 [Kurth, Gabrielle; Phillips, Fred M.] New Mexico Inst Min & Technol, Dept Earth & Environm Sci, Socorro, NM 87801 USA.
[Reheis, Marith C.; Paces, James B.] US Geol Survey, Denver Fed Ctr, Denver, CO 80225 USA.
[Redwine, Joanna L.] Desert Res Inst, Reno, NV 89512 USA.
RP Kurth, G (reprint author), OReilly Talbot & Okun Associates Inc, 293 Bridge St, Springfield, MA 01375 USA.
EM phillips@nmt.edu
FU National Science Foundation (NSF) [EAR-0001063]
FX This paper has had a long gestation time and we thank the National
Science Foundation (NSF grant EAR-0001063) and many other people who
have shown patience in waiting for the results. Eric Small (now at
University of Colorado) collaborated on the initial NSF proposal and
also assisted in field work. We thank Bud Burke and Ronna Bowers
(Humboldt State University) for help on field work in Newark Valley. We
appreciate the cooperation of Ron Tauchen and Michael Baskerville,
Bureau of Land Management, Carson City and Tonopah offices, in approving
the trench sites at Thorne Bar and Columbus Salt Marsh. Harland
Goldstein and Eric Fisher (U.S. Geological Survey-Denver) performed soil
laboratory analyses for the Thorne Bar and Columbus sites. Thorough
reviews and helpful suggestions by Michael Machette and Richard Briggs
(U.S. Geological Survey) greatly improved earlier versions of this
paper.
NR 100
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Z9 17
U1 0
U2 15
PU GEOLOGICAL SOC AMER, INC
PI BOULDER
PA PO BOX 9140, BOULDER, CO 80301-9140 USA
SN 0016-7606
EI 1943-2674
J9 GEOL SOC AM BULL
JI Geol. Soc. Am. Bull.
PD MAR-APR
PY 2011
VL 123
IS 3-4
BP 744
EP 768
DI 10.1130/B30010.1
PG 25
WC Geosciences, Multidisciplinary
SC Geology
GA 712KJ
UT WOS:000286665300020
ER
PT J
AU Anderson, L
AF Anderson, Lesleigh
TI Holocene record of precipitation seasonality from lake calcite delta
O-18 in the central Rocky Mountains, United States
SO GEOLOGY
LA English
DT Article
ID COLORADO RIVER-BASIN; CLIMATE-CHANGE; NORTH-AMERICA; EL-NINO; USA;
EVOLUTION; FLUCTUATIONS; CALIFORNIA; VARIABILITY; TIMESCALES
AB A context for recent hydroclimatic extremes and variability is provided by a similar to 10 k.y. sediment carbonate oxygen isotope (delta O-18) record at 5-100 yr resolution from Bison Lake, 3255 m above sea level, in northwestern Colorado (United States). Winter precipitation is the primary water source for the alpine headwater lake in the Upper Colorado River Basin and lake water delta O-18 measurements reflect seasonal variations in precipitation delta O-18. Holocene lake water delta O-18 variations are inferred from endogenic sedimentary calcite delta O-18 based on comparisons with historic watershed discharge records and tree-ring reconstructions. Drought periods (i.e., drier winters and/or a more rain-dominated seasonal precipitation balance) generally correspond with higher calcite delta O-18 values, and vice-versa. Early to middle Holocene delta O-18 values are higher, implying a rain-dominated seasonal precipitation balance. Lower, more variable delta O-18 values after ca. 3500 yr ago indicate a snow-dominated but more seasonally variable precipitation balance. The middle to late Holocene delta O-18 record corresponds with records of El Nino Southern Oscillation intensification that supports a teleconnection between Rocky Mountain climate and North Pacific sea-surface temperatures at decade to century time scales.
C1 US Geol Survey, Denver Fed Ctr, Denver, CO 80225 USA.
RP Anderson, L (reprint author), US Geol Survey, Denver Fed Ctr, Box 25046,MS-980, Denver, CO 80225 USA.
EM land@usgs.gov
FU U.S Geological Survey
FX The U.S Geological Survey Global Change Research and Development Program
supported this work. We thank Chris Eastoe, David Dettman and the
University of Arizona Environmental Isotope Laboratory, Chad Wolak, Jack
McGeehin, Joe Rosenbaum, Jeff Honke, Gary Skipp, Cheryl Mnich, Erik
Brown, Marian Kramer, Jen Morse, Andrew McFadden, Alisa Mast, and Carol
Ann Chapman for analytical and field assistance. Discussions with Bob
Thompson, John Barron, Connie Woodhouse, and Dan Muhs were helpful in
improvements of the manuscript. Any use of trade, product, or firm names
is for descriptive purposes only and does not imply endorsement by the
U.S. Government.
NR 34
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U1 1
U2 16
PU GEOLOGICAL SOC AMER, INC
PI BOULDER
PA PO BOX 9140, BOULDER, CO 80301-9140 USA
SN 0091-7613
J9 GEOLOGY
JI Geology
PD MAR
PY 2011
VL 39
IS 3
BP 211
EP 214
DI 10.1130/G31575.1
PG 4
WC Geology
SC Geology
GA 721SI
UT WOS:000287374900007
ER
PT J
AU O'Donnell, JA
Harden, JW
McGuire, AD
Kanevskiy, MZ
Jorgenson, MT
Xu, XM
AF O'Donnell, Jonathan A.
Harden, Jennifer W.
McGuire, A. David
Kanevskiy, Mikhail Z.
Jorgenson, M. Torre
Xu, Xiaomei
TI The effect of fire and permafrost interactions on soil carbon
accumulation in an upland black spruce ecosystem of interior Alaska:
implications for post-thaw carbon loss
SO GLOBAL CHANGE BIOLOGY
LA English
DT Article
DE boreal forest; climate change; permafrost; soil carbon; wildfire
ID ARCTIC TUNDRA SOILS; CLIMATE-CHANGE; ORGANIC-CARBON; BOREAL FOREST;
THAW; VULNERABILITY; TEMPERATURE; FEEDBACKS; STORAGE; CYCLE
AB High-latitude regions store large amounts of organic carbon (OC) in active-layer soils and permafrost, accounting for nearly half of the global belowground OC pool. In the boreal region, recent warming has promoted changes in the fire regime, which may exacerbate rates of permafrost thaw and alter soil OC dynamics in both organic and mineral soil. We examined how interactions between fire and permafrost govern rates of soil OC accumulation in organic horizons, mineral soil of the active layer, and near-surface permafrost in a black spruce ecosystem of interior Alaska. To estimate OC accumulation rates, we used chronosequence, radiocarbon, and modeling approaches. We also developed a simple model to track long-term changes in soil OC stocks over past fire cycles and to evaluate the response of OC stocks to future changes in the fire regime. Our chronosequence and radiocarbon data indicate that OC turnover varies with soil depth, with fastest turnover occurring in shallow organic horizons (similar to 60 years) and slowest turnover in near-surface permafrost (> 3000 years). Modeling analysis indicates that OC accumulation in organic horizons was strongly governed by carbon losses via combustion and burial of charred remains in deep organic horizons. OC accumulation in mineral soil was influenced by active layer depth, which determined the proportion of mineral OC in a thawed or frozen state and thus, determined loss rates via decomposition. Our model results suggest that future changes in fire regime will result in substantial reductions in OC stocks, largely from the deep organic horizon. Additional OC losses will result from fire-induced thawing of near-surface permafrost. From these findings, we conclude that the vulnerability of deep OC stocks to future warming is closely linked to the sensitivity of permafrost to wildfire disturbance.
C1 [O'Donnell, Jonathan A.] Univ Alaska Fairbanks, Dept Biol & Wildlife, Fairbanks, AK 99775 USA.
[Harden, Jennifer W.] US Geol Survey, Menlo Pk, CA 94025 USA.
[McGuire, A. David] Univ Alaska Fairbanks, US Geol Survey, Alaska Cooperat Fish & Wildlife Res Unit, Fairbanks, AK USA.
[Kanevskiy, Mikhail Z.] Univ Alaska Fairbanks, Inst No Engn, Fairbanks, AK USA.
[Jorgenson, M. Torre] Alaska Ecosci, Fairbanks, AK USA.
[Xu, Xiaomei] Univ Calif Irvine, Dept Earth Syst Sci, Irvine, CA USA.
RP O'Donnell, JA (reprint author), Univ Alaska Fairbanks, Dept Biol & Wildlife, Fairbanks, AK 99775 USA.
EM jaodonnell@alaska.edu
FU National Science Foundation [EAR-0630249, DEB-0423442]; Institute of
Northern Engineering at the University of Alaska Fairbanks; US
Geological Survey; USDA Forest Service (Pacific Northwest Research
Station) [PNW01-JV11261952-231]
FX The authors would like to thank Stephanie Ewing for her assistance in
the field and for sharing in many insightful discussions about
permafrost. Many thanks also go to Pedro Rodriguez for field/laboratory
assistance, Kristen Manies for assistance with data management, Yuri
Shur for initiating collaborations with AKDOT&PF, and Tom Douglas for
sharing laboratory space. Vladimir Romanovsky, Yuri Shur, Eran Hood, and
Evan Kane provided valuable comments on an earlier version of this
manuscript. Funding and support for J. O'Donnell was provided by the
National Science Foundation grant EAR-0630249 and the Institute of
Northern Engineering at the University of Alaska Fairbanks. The study
was also supported by grants from the US Geological Survey to Harden and
McGuire, and by the Bonanza Creek LTER (Long-Term Ecological Research)
Program, funded jointly by NSF (grant DEB-0423442) and the USDA Forest
Service (Pacific Northwest Research Station grant PNW01-JV11261952-231).
NR 77
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U1 3
U2 61
PU WILEY-BLACKWELL
PI HOBOKEN
PA 111 RIVER ST, HOBOKEN 07030-5774, NJ USA
SN 1354-1013
EI 1365-2486
J9 GLOBAL CHANGE BIOL
JI Glob. Change Biol.
PD MAR
PY 2011
VL 17
IS 3
BP 1461
EP 1474
DI 10.1111/j.1365-2486.2010.02358.x
PG 14
WC Biodiversity Conservation; Ecology; Environmental Sciences
SC Biodiversity & Conservation; Environmental Sciences & Ecology
GA 714VU
UT WOS:000286837900016
ER
PT J
AU Gallo, K
Hale, R
Tarpley, D
Yu, YY
AF Gallo, Kevin
Hale, Robert
Tarpley, Dan
Yu, Yunyue
TI Evaluation of the Relationship between Air and Land Surface Temperature
under Clear- and Cloudy-Sky Conditions
SO JOURNAL OF APPLIED METEOROLOGY AND CLIMATOLOGY
LA English
DT Article
ID SOLAR
AB Clear and cloudy daytime comparisons of land surface temperature (LST) and air temperature (Tair) were made for 14 stations included in the U. S. Climate Reference Network (USCRN) of stations from observations made from 2003 through 2008. Generally, LST was greater than Tair for both the clear and cloudy conditions; however, the differences between LST and Tair were significantly less for the cloudy-sky conditions. In addition, the relationships between LST and Tair displayed less variability under the cloudy-sky conditions than under clear-sky conditions. Wind speed, time of the observation of Tair and LST, season, the occurrence of precipitation at the time of observation, and normalized difference vegetation index values were all considered in the evaluation of the relationship between Tair and LST. Mean differences between LST and Tair of less than 2 degrees C were observed under cloudy conditions for the stations, as compared with a minimum difference of greater than 2 degrees C(and as great as 7+degrees C) for the clear-sky conditions. Under cloudy conditions, Tair alone explained over 94%-and as great as 98%-of the variance observed in LST for the stations included in this analysis, as compared with a range of 81%-93% for clear-sky conditions. Because of the relatively homogeneous land surface characteristics encouraged in the immediate vicinity of USCRN stations, and potential regional differences in surface features that might influence the observed relationships, additional analyses of the relationships between LST and Tair for additional regions and land surface conditions are recommended.
C1 [Gallo, Kevin; Yu, Yunyue] NOAA, NESDIS Ctr Satellite Applicat & Res, Camp Springs, MD USA.
[Hale, Robert] Colorado State Univ, Cooperat Inst Res Atmosphere, Ft Collins, CO 80523 USA.
[Tarpley, Dan] Short & Associates Inc, Chevy Chase, MD USA.
RP Gallo, K (reprint author), USGS EROS Ctr, 47914 252nd St, Sioux Falls, SD 57198 USA.
EM kevin.p.gallo@noaa.gov
RI Gallo, Kevin P./F-5588-2010; Yu, Yunyue/F-5636-2010
FU NOAA
FX This study was partially supported by the NOAA GOES-R Program. The
manuscript contents do not constitute a statement of policy, decision,
or position on behalf of NOAA or the U.S. government.
NR 23
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U1 3
U2 18
PU AMER METEOROLOGICAL SOC
PI BOSTON
PA 45 BEACON ST, BOSTON, MA 02108-3693 USA
SN 1558-8424
J9 J APPL METEOROL CLIM
JI J. Appl. Meteorol. Climatol.
PD MAR
PY 2011
VL 50
IS 3
BP 767
EP 775
DI 10.1175/2010JAMC2460.1
PG 9
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA 750PK
UT WOS:000289560300020
ER
PT J
AU Weems, RE
Edwards, LE
Osborne, JE
Alford, AA
AF Weems, Robert E.
Edwards, Lucy E.
Osborne, Jason E.
Alford, Aaron A.
TI AN OCCURRENCE OF THE PROTOCETID WHALE "EOCETUS" WARDII IN THE MIDDLE
EOCENE PINEY POINT FORMATION OF VIRGINIA
SO JOURNAL OF PALEONTOLOGY
LA English
DT Article
ID ARCHAEOCETE WHALE; MAMMALIA; CETACEA; CAROLINA
AB Two protocetid whale vertebrae, here referred to "Eocetus" wardii, have been recovered from the riverbed of the Pamunkey River in east-central Virginia. Neither bone was found in situ, but both were found with lumps of lithified matrix cemented to their surfaces. Most of this matrix was removed and processed for microfossils. Specimens of dinoflagellates were successfully recovered and this flora clearly demonstrates that both vertebrae came from the middle Eocene Piney Point Formation, which crops out above and below river level in the area where the bones were discovered. These vertebrae are the oldest whale remains reported from Virginia and are as old as any cetacean remains known from the western hemisphere.
C1 [Weems, Robert E.; Edwards, Lucy E.] US Geol Survey, Reston, VA 20192 USA.
[Osborne, Jason E.; Alford, Aaron A.] Paleo Quest, Gainesville, VA 20155 USA.
RP Weems, RE (reprint author), US Geol Survey, 926A Natl Ctr, Reston, VA 20192 USA.
EM rweems@usgs.gov; leedward@usgs.gov; osbornej@paleoquest.org;
alforda@paleoquest.org
OI Alford, Aaron/0000-0001-5910-6174
NR 53
TC 5
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U1 0
U2 1
PU CAMBRIDGE UNIV PRESS
PI NEW YORK
PA 32 AVENUE OF THE AMERICAS, NEW YORK, NY 10013-2473 USA
SN 0022-3360
EI 1937-2337
J9 J PALEONTOL
JI J. Paleontol.
PD MAR
PY 2011
VL 85
IS 2
BP 271
EP 278
DI 10.1666/10-083.1
PG 8
WC Paleontology
SC Paleontology
GA 791LO
UT WOS:000292666900007
ER
PT J
AU Robertson, DM
Rose, WJ
AF Robertson, Dale M.
Rose, William J.
TI Response in the trophic state of stratified lakes to changes in
hydrology and water level: potential effects of climate change
SO JOURNAL OF WATER AND CLIMATE CHANGE
LA English
DT Article
DE climate change; eutrophication; hydrology; productivity; water level
ID FLUCTUATIONS; QUALITY; BLOOMS
AB To determine how climate-induced changes in hydrology and water level may affect the trophic state (productivity) of stratified lakes, two relatively pristine dimictic temperate lakes in Wisconsin, USA, were examined. Both are closed-basin lakes that experience changes in water level and degradation in water quality during periods of high water. One, a seepage lake with no inlets or outlets, has a small drainage basin and hydrology dominated by precipitation and groundwater exchange causing small changes in water and phosphorus (P) loading, which resulted in small changes in water level, P concentrations, and productivity. The other, a terminal lake with inlets but no outlets, has a large drainage basin and hydrology dominated by runoff causing large changes in water and P loading, which resulted in large changes in water level, P concentrations, and productivity. Eutrophication models accurately predicted the effects of changes in hydrology, P loading, and water level on their trophic state. If climate changes, larger changes in hydrology and water levels than previously observed could occur. If this causes increased water and P loading, stratified (dimictic and monomictic) lakes are expected to experience higher water levels and become more eutrophic, especially those with large developed drainage basins.
C1 [Robertson, Dale M.; Rose, William J.] US Geol Survey, Middleton, WI USA.
RP Robertson, DM (reprint author), US Geol Survey, 8505 Res Way, Middleton, WI USA.
EM dzrobert@usgs.gov
OI Robertson, Dale/0000-0001-6799-0596
FU Wisconsin Department of Natural Resources; US Geological Survey
FX We thank Joe Schuler, Tom Popowski, Bernie Lenz, Fred and Sandy
Anderson, Vicki and David Van Ells, and David and Mary Lou Rossmeisl for
assistance with data collection. We also thank Tim Asplund and Randy
Hunt for suggestions and comments on this manuscript. Funds for this
work were provided through the Lake Protection Grant Program of the
Wisconsin Department of Natural Resources and the Cooperative Program of
the US Geological Survey.
NR 38
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U1 3
U2 17
PU IWA PUBLISHING
PI LONDON
PA ALLIANCE HOUSE, 12 CAXTON ST, LONDON SW1H0QS, ENGLAND
SN 2040-2244
J9 J WATER CLIM CHANGE
JI J. Water Clim. Chang.
PD MAR
PY 2011
VL 2
IS 1
BP 1
EP 18
DI 10.2166/wcc.2011.026
PG 18
WC Water Resources
SC Water Resources
GA 904QT
UT WOS:000301213700001
ER
PT J
AU Pearce, JM
Reeves, AB
Ramey, AM
Hupp, JW
Ip, HS
Bertram, M
Petrula, MJ
Scotton, BD
Trust, KA
Meixell, BW
Runstadler, JA
AF Pearce, John M.
Reeves, Andrew B.
Ramey, Andrew M.
Hupp, Jerry W.
Ip, Hon S.
Bertram, Mark
Petrula, Michael J.
Scotton, Bradley D.
Trust, Kimberly A.
Meixell, Brandt W.
Runstadler, Jonathan A.
TI Interspecific exchange of avian influenza virus genes in Alaska: the
influence of trans-hemispheric migratory tendency and breeding ground
sympatry
SO MOLECULAR ECOLOGY
LA English
DT Article
DE Anas platyrhynchos; avian influenza; migratory; reassortment;
transmission
ID PINTAIL ANAS-ACUTA; A VIRUS; NORTHERN PINTAILS; SATELLITE TELEMETRY;
SPRING MIGRATION; WILD DUCKS; RT-PCR; H5N1; EVOLUTION; BIRDS
AB The movement and transmission of avian influenza viral strains via wild migratory birds may vary by host species as a result of migratory tendency and sympatry with other infected individuals. To examine the roles of host migratory tendency and species sympatry on the movement of Eurasian low-pathogenic avian influenza (LPAI) genes into North America, we characterized migratory patterns and LPAI viral genomic variation in mallards (Anas platyrhynchos) of Alaska in comparison with LPAI diversity of northern pintails (Anas acuta). A 50-year band-recovery data set suggests that unlike northern pintails, mallards rarely make trans-hemispheric migrations between Alaska and Eurasia. Concordantly, fewer (14.5%) of 62 LPAI isolates from mallards contained Eurasian gene segments compared to those from 97 northern pintails (35%), a species with greater inter-continental migratory tendency. Aerial survey and banding data suggest that mallards and northern pintails are largely sympatric throughout Alaska during the breeding season, promoting opportunities for interspecific transmission. Comparisons of full-genome isolates confirmed near-complete genetic homology (> 99.5%) of seven viruses between mallards and northern pintails. This study found viral segments of Eurasian lineage at a higher frequency in mallards than previous studies, suggesting transmission from other avian species migrating inter-hemispherically or the common occurrence of endemic Alaskan viruses containing segments of Eurasian origin. We conclude that mallards are unlikely to transfer Asian-origin viruses directly to North America via Alaska but that they are likely infected with Asian-origin viruses via interspecific transfer from species with regular migrations to the Eastern Hemisphere.
C1 [Pearce, John M.; Reeves, Andrew B.; Ramey, Andrew M.; Hupp, Jerry W.] US Geol Survey, Alaska Sci Ctr, Anchorage, AK 99508 USA.
[Ip, Hon S.] US Geol Survey, Natl Wildlife Hlth Ctr, Madison, WI 53711 USA.
[Bertram, Mark] US Fish & Wildlife Serv, Fairbanks, AK 99701 USA.
[Petrula, Michael J.] Alaska Dept Fish & Game, Anchorage, AK 99518 USA.
[Scotton, Bradley D.] US Fish & Wildlife Serv, Galena, AK 99641 USA.
[Trust, Kimberly A.] US Fish & Wildlife Serv, Anchorage, AK 99503 USA.
[Meixell, Brandt W.] Univ Minnesota, Dept Fisheries Wildlife & Conservat, St Paul, MN 55108 USA.
[Runstadler, Jonathan A.] Univ Alaska, Dept Biol & Wildlife, Inst Arctic Biol, Fairbanks, AK 99775 USA.
RP Pearce, JM (reprint author), US Geol Survey, Alaska Sci Ctr, 4210 Univ Dr, Anchorage, AK 99508 USA.
EM jpearce@usgs.gov
OI Ramey, Andrew/0000-0002-3601-8400; Meixell, Brandt/0000-0002-6738-0349
FU US Geological Survey; US Fish and Wildlife Service; National Institute
of Allergy and Infectious Diseases [HHSN266200700009C,
HHSN266200700010C]; National Center for Research Resources (NCRR),
National Institutes of Health (NIH) [RR016466]
FX We are grateful to L. Allen, P. Bright, D. Derksen, T. DeGange, S.
Haseltine, R. Kearney (US Geological Survey) and D. Rocque (US Fish and
Wildlife Service) for financial and administrative support. D. Mauser
(Klamath Basin NWR), A. Dzubin (Canadian Wildlife Service), M. Wege, T.
Moran, C. Harwood (Yukon Delta NWR), E. Mallek, D. Marks and B. Eldridge
(US Fish and Wildlife Service, Alaska) provided unpublished banding
data. Numerous wildlife biologists assisted with virus sampling and
their efforts are appreciated. We thank past and current members of the
Diagnostic Virology Laboratory at the USGS National Wildlife Health
Center, including T. Egstad, K. Griffin, M. Houfe and R. Long. Y.
Gillies, J. Wiley (USGS Alaska Science Center), M. St. Peters (USFWS
Alaska Region), D. Goldberg and R. Zane (USGS National Wildlife Health
Center) coordinated distribution of sampling materials, receipt of
samples and data verification. J. Runstadler and B. Meixell and the work
to derive the mallard GenBank sequences were supported in part by
National Institute of Allergy and Infectious Diseases-funded Centers of
Excellence in Influenza Research and Surveillance (Contracts
HHSN266200700009C and HHSN266200700010C). We thank D. Spiro (J. Craig
Venter Institute) and G. Happ, F. Aldehoff, L. Gildehaus, J. Black, and
P. Gingrich and others at the University of Alaska, Fairbanks (UAF), for
their work to generate the viral strains and sequence information from
GenBank used in this study. Some analyses were run on the UAF Life
Science Informatics portal, a core research resource supported by Grant
Number RR016466 from the National Center for Research Resources (NCRR),
a component of the National Institutes of Health (NIH). D. Derksen, P.
Flint, K. McCracken and three anonymous reviewers provided comments that
improved the manuscript. None of the authors have any financial
interests or conflict of interest with this article. Any use of trade
names is for descriptive purposes only and does not imply endorsement by
the US Government.
NR 60
TC 23
Z9 23
U1 1
U2 10
PU WILEY-BLACKWELL PUBLISHING, INC
PI MALDEN
PA COMMERCE PLACE, 350 MAIN ST, MALDEN 02148, MA USA
SN 0962-1083
J9 MOL ECOL
JI Mol. Ecol.
PD MAR
PY 2011
VL 20
IS 5
BP 1015
EP 1025
DI 10.1111/j.1365-294X.2010.04908.x
PG 11
WC Biochemistry & Molecular Biology; Ecology; Evolutionary Biology
SC Biochemistry & Molecular Biology; Environmental Sciences & Ecology;
Evolutionary Biology
GA 721ZN
UT WOS:000287397600014
PM 21073586
ER
PT J
AU Bull, RAS
Cushman, SA
Mace, R
Chilton, T
Kendall, KC
Landguth, EL
Schwartz, MK
McKelvey, K
Allendorf, FW
Luikart, G
AF Bull, R. A. Short
Cushman, S. A.
Mace, R.
Chilton, T.
Kendall, K. C.
Landguth, E. L.
Schwartz, M. K.
McKelvey, K.
Allendorf, Fred W.
Luikart, G.
TI Why replication is important in landscape genetics: American black bear
in the Rocky Mountains
SO MOLECULAR ECOLOGY
LA English
DT Article
DE connectivity; gene flow; habitat fragmentation; landscape genetics;
landscape resistance modelling; noninvasive sampling; Ursus americanus
ID HABITAT FRAGMENTATION; POPULATION-STRUCTURE; NORTH-CAROLINA; DISPERSAL;
CORRIDOR; FEATURES; DIFFERENTIATION; CONNECTIVITY; WASHINGTON; CASCADES
AB We investigated how landscape features influence gene flow of black bears by testing the relative support for 36 alternative landscape resistance hypotheses, including isolation by distance (IBD) in each of 12 study areas in the north central U.S. Rocky Mountains. The study areas all contained the same basic elements, but differed in extent of forest fragmentation, altitude, variation in elevation and road coverage. In all but one of the study areas, isolation by landscape resistance was more supported than IBD suggesting gene flow is likely influenced by elevation, forest cover, and roads. However, the landscape features influencing gene flow varied among study areas. Using subsets of loci usually gave models with the very similar landscape features influencing gene flow as with all loci, suggesting the landscape features influencing gene flow were correctly identified. To test if the cause of the variability of supported landscape features in study areas resulted from landscape differences among study areas, we conducted a limiting factor analysis. We found that features were supported in landscape models only when the features were highly variable. This is perhaps not surprising but suggests an important cautionary note - that if landscape features are not found to influence gene flow, researchers should not automatically conclude that the features are unimportant to the species' movement and gene flow. Failure to investigate multiple study areas that have a range of variability in landscape features could cause misleading inferences about which landscape features generally limit gene flow. This could lead to potentially erroneous identification of corridors and barriers if models are transferred between areas with different landscape characteristics.
C1 [Bull, R. A. Short; Landguth, E. L.; Allendorf, Fred W.; Luikart, G.] Univ Montana, Div Biol Sci, Missoula, MT 59812 USA.
[Cushman, S. A.; Landguth, E. L.; Schwartz, M. K.; McKelvey, K.] US Forest Serv, USDA, Rocky Mt Res Stn, Missoula, MT 59801 USA.
[Mace, R.; Chilton, T.] Montana Dept Fish Wildlife & Pk, Kalispell, MT 59901 USA.
[Kendall, K. C.] US Geol Survey, No Rocky Mt Sci Ctr, Glacier Field Stn, Glacier Natl Pk, W Glacier, MT 59936 USA.
[Luikart, G.] Univ Porto, CIBIO, Ctr Invest Biodiversidade & Recursos Genet, P-4485661 Vairao, Portugal.
[Luikart, G.] Univ Montana, Flathead Lake Biol Stn, Polson, MT 59860 USA.
RP Bull, RAS (reprint author), Univ Montana, Div Biol Sci, Missoula, MT 59812 USA.
EM ruth.shortbull@umontana.edu
RI Schwartz, Michael/C-3184-2014;
OI Schwartz, Michael/0000-0003-3521-3367; Luikart,
Gordon/0000-0001-8697-0582
FU U.S. Geological Survey; United States Forest Service; U.S. National
Science Foundation [DEB 074218]; NSF [DEB-1067613]; Portuguese-American
Science Foundation; CIBIO-UP; Portuguese Science Foundation (FCT)
[PTDC/BIA-BDE/65625/2006]
FX We thank the Montana Fish, Wildlife and Parks, as well as the U.S.
Geological Survey for coordinating and collecting hair samples, which
also includes the hundreds of employees and volunteers. We also thank
the following agencies that provided other support: Blackfeet Nation;
Confederated Salish and Kootenai Tribes; Montana Department of Natural
Resources and Conservation; National Park Service; Northwest
Connections; United States Bureau of Land Management; United States Fish
and Wildlife Service; and Wildlife Genetics International. Financial
support was provided by the U.S. Geological Survey and United States
Forest Service. We also thank the bears that allowed this research to be
possible. F. W. A., G. L., and R. S. were partially supported by a grant
from the U.S. National Science Foundation Grant DEB 074218. G. L. also
was supported by an NSF grant (DEB-1067613) and the Portuguese-American
Science Foundation, CIBIO-UP, and research grant PTDC/BIA-BDE/65625/2006
from the Portuguese Science Foundation (FCT).
NR 65
TC 54
Z9 54
U1 10
U2 81
PU WILEY-BLACKWELL
PI HOBOKEN
PA 111 RIVER ST, HOBOKEN 07030-5774, NJ USA
SN 0962-1083
J9 MOL ECOL
JI Mol. Ecol.
PD MAR
PY 2011
VL 20
IS 6
BP 1092
EP 1107
DI 10.1111/j.1365-294X.2010.04944.x
PG 16
WC Biochemistry & Molecular Biology; Ecology; Evolutionary Biology
SC Biochemistry & Molecular Biology; Environmental Sciences & Ecology;
Evolutionary Biology
GA 730YX
UT WOS:000288074600004
PM 21261764
ER
PT J
AU Point, D
Sonke, JE
Day, RD
Roseneau, DG
Hobson, KA
Vander Pol, SS
Moors, AJ
Pugh, RS
Donard, OFX
Becker, PR
AF Point, D.
Sonke, J. E.
Day, R. D.
Roseneau, D. G.
Hobson, K. A.
Vander Pol, S. S.
Moors, A. J.
Pugh, R. S.
Donard, O. F. X.
Becker, P. R.
TI Methylmercury photodegradation influenced by sea-ice cover in Arctic
marine ecosystems
SO NATURE GEOSCIENCE
LA English
DT Article
ID MASS-INDEPENDENT FRACTIONATION; ISOTOPE FRACTIONATION; MERCURY ISOTOPES;
STABLE-ISOTOPES; TEMPORAL TRENDS; SURFACE WATERS; BELUGA WHALES;
DEPOSITION; EXPOSURE; HABITAT
AB Atmospheric deposition of mercury to remote areas has increased threefold since pre-industrial times. Mercury deposition is particularly pronounced in the Arctic. Following deposition to surface oceans and sea ice, mercury can be converted into methylmercury, a biologically accessible form of the toxin, which biomagnifies along the marine food chain. Mass-independent fractionation of mercury isotopes accompanies the photochemical breakdown of methylmercury to less bioavailable forms in surface waters. Here we examine the isotopic composition of mercury in seabird eggs collected from colonies in the North Pacific Ocean, the Bering Sea and the western Arctic Ocean, to determine geographical variations in methylmercury breakdown at northern latitudes. We find evidence for mass-independent fractionation of mercury isotopes. The degree of mass-independent fractionation declines with latitude. Foraging behaviour and geographic variations in mercury sources and solar radiation fluxes were unable to explain the latitudinal gradient. However, mass-independent fractionation was negatively correlated with sea-ice cover. We conclude that sea-ice cover impedes the photochemical breakdown of methylmercury in surface waters, and suggest that further loss of Arctic sea ice this century will accelerate sunlight-induced breakdown of methylmercury in northern surface waters.
C1 [Point, D.; Day, R. D.; Vander Pol, S. S.; Moors, A. J.; Pugh, R. S.; Becker, P. R.] Natl Inst Stand & Technol, Hollings Marine Lab, Charleston, SC 29412 USA.
[Point, D.; Sonke, J. E.] Univ Toulouse 3, CNRS, UMR 5563, Observ Midi Pyrenees,LMTG,UMR IRD 154, F-31400 Toulouse, France.
[Roseneau, D. G.] Alaska Maritime Natl Wildlife Refuge, US Fish & Wildlife Serv, Homer, AK 99603 USA.
[Hobson, K. A.] Environm Canada, Saskatoon, SK S7N 0X4, Canada.
[Donard, O. F. X.] CNRS, UMR 5254, Equipe Chim Analyt BioInorgan & Environm, Inst Pluridisciplinaire Rech Environm & Mat, F-64053 Pau, France.
RP Point, D (reprint author), Natl Inst Stand & Technol, Hollings Marine Lab, Charleston, SC 29412 USA.
EM david.point@lmtg.obs-mip.fr
OI Point, David/0000-0002-5218-7781
FU NIST; French Centre National de la Recherche Scientifique; French Agence
Nationale de Recherche [ANR-09-JCJC-0035-01]
FX The samples used in this study were obtained from the Marine
Environmental Specimen Bank (MESB) through the Seabird Tissue Archival
and Monitoring Project (STAMP), a long-term collaborative effort by the
Alaska Maritime National Wildlife Refuge (AMNWR), the National Institute
of Standards and Technology (NIST), the US Geological Survey Biological
Resources Division (USGS-BRD) and the Bureau of Indian Affairs Alaska
Region Subsistence Branch (BIA-ARSB). We thank AMNWR and University of
Alaska-Fairbanks (UAF) biologists, members of the St George Traditional
Council, the Native Village of Point Hope IRA Council and residents of
St George, Savoonga and Point Hope for collecting the eggs. We also
thank K. S. Simac (USGS-BRD) for processing the eggs, M. B. Ellisor
(NIST) for cryohomogenizing and banking the eggs and F. Poitrasson and
Y. Godderis for providing helpful comments on the manuscript. This work
is part of International Polar Year (IPY) Research Activity No. 439
'MERSAM' (MERcury Seabird Arctic Monitoring). Financial support for this
research was provided by NIST, the French Centre National de la
Recherche Scientifique, and Research Grant ANR-09-JCJC-0035-01 from the
French Agence Nationale de Recherche.
NR 49
TC 65
Z9 70
U1 3
U2 61
PU NATURE PUBLISHING GROUP
PI NEW YORK
PA 75 VARICK ST, 9TH FLR, NEW YORK, NY 10013-1917 USA
SN 1752-0894
J9 NAT GEOSCI
JI Nat. Geosci.
PD MAR
PY 2011
VL 4
IS 3
BP 188
EP 194
DI 10.1038/NGEO1049
PG 7
WC Geosciences, Multidisciplinary
SC Geology
GA 727LU
UT WOS:000287802300020
ER
PT J
AU van der Wegen, M
Dastgheib, A
Jaffe, BE
Roelvink, D
AF van der Wegen, Mick
Dastgheib, Ali
Jaffe, Bruce E.
Roelvink, Dano
TI Bed composition generation for morphodynamic modeling: case study of San
Pablo Bay in California, USA
SO OCEAN DYNAMICS
LA English
DT Article
DE Process-based model; Morphodynamic prediction; Bed composition;
Estuarine processes; San Pablo Bay; Data scarcity; Coastal geomorphology
ID SEDIMENT; VALIDATION
AB Applications of process-based morphodynamic models are often constrained by limited availability of data on bed composition, which may have a considerable impact on the modeled morphodynamic development. One may even distinguish a period of "morphodynamic spin-up" in which the model generates the bed level according to some ill-defined initial bed composition rather than describing the realistic behavior of the system. The present paper proposes a methodology to generate bed composition of multiple sand and/or mud fractions that can act as the initial condition for the process-based numerical model Delft3D. The bed composition generation (BCG) run does not include bed level changes, but does permit the redistribution of multiple sediment fractions over the modeled domain. The model applies the concept of an active layer that may differ in sediment composition above an underlayer with fixed composition. In the case of a BCG run, the bed level is kept constant, whereas the bed composition can change. The approach is applied to San Pablo Bay in California, USA. Model results show that the BCG run reallocates sand and mud fractions over the model domain. Initially, a major sediment reallocation takes place, but development rates decrease in the longer term. Runs that take the outcome of a BCG run as a starting point lead to more gradual morphodynamic development. Sensitivity analysis shows the impact of variations in the morphological factor, the active layer thickness, and wind waves. An important but difficult to characterize criterion for a successful application of a BCG run is that it should not lead to a bed composition that fixes the bed so that it dominates the "natural" morphodynamic development of the system. Future research will focus on a decadal morphodynamic hindcast and comparison with measured bathymetries in San Pablo Bay so that the proposed methodology can be tested and optimized.
C1 [van der Wegen, Mick; Dastgheib, Ali; Roelvink, Dano] UNESCO IHE, NL-2601 DA Delft, Netherlands.
[Jaffe, Bruce E.] USGS Pacific Sci Ctr, Santa Cruz, CA 95060 USA.
[Roelvink, Dano] Delft Univ Technol, NL-2600 GA Delft, Netherlands.
[Roelvink, Dano] Deltares, NL-2600 MH Delft, Netherlands.
RP van der Wegen, M (reprint author), UNESCO IHE, POB 3015, NL-2601 DA Delft, Netherlands.
EM m.vanderwegen@unesco-ihe.org; a.dastgheib@unesco-ihe.org;
bjaffe@usgs.gov; d.roelvink@unesco-ihe.org
RI Dastgheib, Ali/M-8982-2013; Jaffe, Bruce/A-9979-2012; van der Wegen,
Mick/C-6787-2009;
OI Dastgheib, Ali/0000-0002-5914-7213; Jaffe, Bruce/0000-0002-8816-5920;
van der Wegen, Mick/0000-0002-5227-2679; Roelvink,
Dano/0000-0002-5367-0003
FU USGS Priority Ecosystem Studies; CALFED; UNESCO-IHE
FX This research has been part of the USGS CASCaDE climate change project.
The authors wish to acknowledge USGS Priority Ecosystem Studies, CALFED,
as well as UNESCO-IHE research funding for making this research
possible.
NR 33
TC 25
Z9 25
U1 1
U2 5
PU SPRINGER HEIDELBERG
PI HEIDELBERG
PA TIERGARTENSTRASSE 17, D-69121 HEIDELBERG, GERMANY
SN 1616-7341
J9 OCEAN DYNAM
JI Ocean Dyn.
PD MAR
PY 2011
VL 61
IS 2-3
SI SI
BP 173
EP 186
DI 10.1007/s10236-010-0314-2
PG 14
WC Oceanography
SC Oceanography
GA 750EQ
UT WOS:000289528200003
ER
PT J
AU Martin, V
Pfeiffer, DU
Zhou, XY
Xiao, XM
Prosser, DJ
Guo, FS
Gilbert, M
AF Martin, Vincent
Pfeiffer, Dirk U.
Zhou, Xiaoyan
Xiao, Xiangming
Prosser, Diann J.
Guo, Fusheng
Gilbert, Marius
TI Spatial Distribution and Risk Factors of Highly Pathogenic Avian
Influenza (HPAI) H5N1 in China
SO PLOS PATHOGENS
LA English
DT Article
ID SOUTHERN CHINA; HONG-KONG; GENETIC-CHARACTERIZATION; SUBTYPE H5N1;
VIRUS; OUTBREAKS; DUCKS; ASIA; TRANSMISSION; EXPERIENCE
AB Highly pathogenic avian influenza (HPAI) H5N1 was first encountered in 1996 in Guangdong province (China) and started spreading throughout Asia and the western Palearctic in 2004-2006. Compared to several other countries where the HPAI H5N1 distribution has been studied in some detail, little is known about the environmental correlates of the HPAI H5N1 distribution in China. HPAI H5N1 clinical disease outbreaks, and HPAI virus (HPAIV) H5N1 isolated from active risk-based surveillance sampling of domestic poultry (referred to as HPAIV H5N1 surveillance positives in this manuscript) were modeled separately using seven risk variables: chicken, domestic waterfowl population density, proportion of land covered by rice or surface water, cropping intensity, elevation, and human population density. We used bootstrapped logistic regression and boosted regression trees (BRT) with cross-validation to identify the weight of each variable, to assess the predictive power of the models, and to map the distribution of HPAI H5N1 risk. HPAI H5N1 clinical disease outbreak occurrence in domestic poultry was mainly associated with chicken density, human population density, and elevation. In contrast, HPAIV H5N1 infection identified by risk-based surveillance was associated with domestic waterfowl density, human population density, and the proportion of land covered by surface water. Both models had a high explanatory power (mean AUC ranging from 0.864 to 0.967). The map of HPAIV H5N1 risk distribution based on active surveillance data emphasized areas south of the Yangtze River, while the distribution of reported outbreak risk extended further North, where the density of poultry and humans is higher. We quantified the statistical association between HPAI H5N1 outbreak, HPAIV distribution and post-vaccination levels of seropositivity (percentage of effective post-vaccination seroconversion in vaccinated birds) and found that provinces with either outbreaks or HPAIV H5N1 surveillance positives in 2007-2009 appeared to have had lower antibody response to vaccination. The distribution of HPAI H5N1 risk in China appears more limited geographically than previously assessed, offering prospects for better targeted surveillance and control interventions.
C1 [Martin, Vincent; Zhou, Xiaoyan; Guo, Fusheng] UN, FAO, Emergency Ctr Control Transboundary Anim Dis, Beijing, Peoples R China.
[Pfeiffer, Dirk U.] Univ London, Royal Vet Coll, Dept Vet Clin Sci, Vet Epidemiol & Publ Hlth Grp, London, England.
[Xiao, Xiangming] Univ Oklahoma, Dept Bot & Microbiol, Ctr Spatial Anal, Norman, OK 73019 USA.
[Prosser, Diann J.] USGS Patuxent Wildlife Res Ctr, Beltsville, MD USA.
[Prosser, Diann J.] Univ Maryland, College Pk, MD 20742 USA.
[Gilbert, Marius] Univ Libre Brussels, Brussels, Belgium.
[Gilbert, Marius] Fonds Natl Rech Sci, B-1050 Brussels, Belgium.
RP Martin, V (reprint author), UN, FAO, Emergency Ctr Control Transboundary Anim Dis, Beijing, Peoples R China.
EM mgilbert@ulb.ac.be
RI Pfeiffer, Dirk/C-5002-2009;
OI Pfeiffer, Dirk/0000-0001-7000-0530; Gilbert, Marius/0000-0003-3708-3359;
Prosser, Diann/0000-0002-5251-1799
FU Food and Agriculture Organization of the United Nations; United States
Agency for International Development (USAID) through the FAO Emergency
Center for Transboundary Animal Diseases (ECTAD) office in China;
National Institutes of Health Fogarty International Center through the
NSF/NIH [7R01TW007869-04]; China Ministry of Health [2008ZX10004-012];
China Ministry of Science and Technology
FX This study was supported by the Food and Agriculture Organization of the
United Nations and funded by the United States Agency for International
Development (USAID) through the FAO Emergency Center for Transboundary
Animal Diseases (ECTAD) office in China. The study was also supported by
the National Institutes of Health Fogarty International Center through
the NSF/NIH Ecology of Infectious Diseases program (7R01TW007869-04).
Dr. Xiao is also supported by the Chinese Special Program for Prevention
and Control of Infectious Diseases (No. 2008ZX10004-012) from the China
Ministry of Health and China Ministry of Science and Technology. The
funders had no role in study design, data collection and analysis,
decision to publish, or preparation of the manuscript.
NR 45
TC 68
Z9 70
U1 2
U2 35
PU PUBLIC LIBRARY SCIENCE
PI SAN FRANCISCO
PA 1160 BATTERY STREET, STE 100, SAN FRANCISCO, CA 94111 USA
SN 1553-7374
J9 PLOS PATHOG
JI PLoS Pathog.
PD MAR
PY 2011
VL 7
IS 3
AR e1001308
DI 10.1371/journal.ppat.1001308
PG 11
WC Microbiology; Parasitology; Virology
SC Microbiology; Parasitology; Virology
GA 743CQ
UT WOS:000288994900003
PM 21408202
ER
PT J
AU Brown, RS
Eppard, MB
Murchie, KJ
Nielsen, JL
Cooke, SJ
AF Brown, Richard S.
Eppard, M. Brad
Murchie, Karen J.
Nielsen, Jennifer L.
Cooke, Steven J.
TI An introduction to the practical and ethical perspectives on the need to
advance and standardize the intracoelomic surgical implantation of
electronic tags in fish
SO REVIEWS IN FISH BIOLOGY AND FISHERIES
LA English
DT Editorial Material
DE Surgery; Tagging; Transmitter; Telemetry
ID TELEMETRY TRANSMITTERS; BIOTELEMETRY; RESEARCHERS; RETENTION; OPINIONS;
BEHAVIOR; ECOLOGY; SALMON
AB The intracoelomic surgical implantation of electronic tags (including radio and acoustic telemetry transmitters, passive integrated transponders and archival biologgers) is frequently used for conducting studies on fish. Electronic tagging studies provide information on the spatial ecology, behavior and survival of fish in marine and freshwater systems. However, any surgical procedure, particularly one where a laparotomy is performed and the coelomic cavity is opened, has the potential to alter the survival, behavior or condition of the animal which can impair welfare and introduce bias. Given that management, regulatory and conservation decisions are based on the assumption that fish implanted with electronic tags have similar fates and behavior relative to untagged conspecifics, it is critical to ensure that best surgical practices are being used. Also, the current lack of standardized surgical procedures and reporting of specific methodological details precludes cross-study and cross-year analyses which would further progress the field of fisheries science. This compilation of papers seeks to identify the best practices for the entire intracoelomic tagging procedure including pre- and post-operative care, anesthesia, wound closure, and use of antibiotics. Although there is a particular focus on salmonid smolts given the large body of literature available on that group, other life-stages and species of fish are discussed where there is sufficient knowledge. Additional papers explore the role of the veterinarian in fish surgeries, the need for minimal standards in the training of fish surgeons, providing a call for more complete and transparent procedures, and identifying trends in procedures and research needs. Collectively, this body of knowledge should help to improve data quality (including comparability and repeatability), enhance management and conservation strategies, and maintain the welfare status of tagged fish.
C1 [Brown, Richard S.] Pacific NW Natl Lab, Ecol Grp, Richland, WA 99352 USA.
[Eppard, M. Brad] US Army Corps Engineers, Portland, OR 97208 USA.
[Murchie, Karen J.; Cooke, Steven J.] Carleton Univ, Dept Biol, Fish Ecol & Conservat Physiol Lab, Ottawa, ON K1S 5B6, Canada.
[Murchie, Karen J.; Cooke, Steven J.] Carleton Univ, Inst Environm Sci, Ottawa, ON K1S 5B6, Canada.
[Nielsen, Jennifer L.] US Geol Survey, Alaska Sci Ctr, Anchorage, AK 99508 USA.
RP Brown, RS (reprint author), Pacific NW Natl Lab, Ecol Grp, 902 Battelle Blvd,POB 999,MSIN K6-85, Richland, WA 99352 USA.
EM rich.brown@pnl.gov
RI Cooke, Steven/F-4193-2010
OI Cooke, Steven/0000-0002-5407-0659
NR 34
TC 10
Z9 10
U1 2
U2 30
PU SPRINGER
PI DORDRECHT
PA VAN GODEWIJCKSTRAAT 30, 3311 GZ DORDRECHT, NETHERLANDS
SN 0960-3166
EI 1573-5184
J9 REV FISH BIOL FISHER
JI Rev. Fish. Biol. Fish.
PD MAR
PY 2011
VL 21
IS 1
SI SI
BP 1
EP 9
DI 10.1007/s11160-010-9183-5
PG 9
WC Fisheries; Marine & Freshwater Biology
SC Fisheries; Marine & Freshwater Biology
GA 726WG
UT WOS:000287756700001
ER
PT J
AU Cooke, SJ
Woodley, CM
Eppard, MB
Brown, RS
Nielsen, JL
AF Cooke, Steven J.
Woodley, Christa M.
Eppard, M. Brad
Brown, Richard S.
Nielsen, Jennifer L.
TI Advancing the surgical implantation of electronic tags in fish: a gap
analysis and research agenda based on a review of trends in
intracoelomic tagging effects studies
SO REVIEWS IN FISH BIOLOGY AND FISHERIES
LA English
DT Review
DE Surgery; Biotelemetry; Behavior; Electronic tags
ID JUVENILE CHINOOK SALMON; PASSIVE INTEGRATED TRANSPONDERS; IMPLANTING
RADIO TRANSMITTERS; DUMMY ACOUSTIC TRANSMITTERS; ATLANTIC BLUEFIN TUNA;
CARP CYPRINUS-CARPIO; HYBRID STRIPED BASS; LONG-TERM RETENTION; SWIMMING
PERFORMANCE; RAINBOW-TROUT
AB Early approaches to surgical implantation of electronic tags in fish were often through trial and error, however, in recent years there has been an interest in using scientific research to identify techniques and procedures that improve the outcome of surgical procedures and determine the effects of tagging on individuals. Here we summarize the trends in 108 peer-reviewed electronic tagging effect studies focused on intracoleomic implantation to determine opportunities for future research. To date, almost all of the studies have been conducted in freshwater, typically in laboratory environments, and have focused on biotelemetry devices. The majority of studies have focused on salmonids, cyprinids, ictalurids and centrarchids, with a regional bias towards North America, Europe and Australia. Most studies have focused on determining whether there is a negative effect of tagging relative to control fish, with proportionally fewer that have contrasted different aspects of the surgical procedure (e.g., methods of sterilization, incision location, wound closure material) that could advance the discipline. Many of these studies included routine endpoints such as mortality, growth, healing and tag retention, with fewer addressing sublethal measures such as swimming ability, predator avoidance, physiological costs, or fitness. Continued research is needed to further elevate the practice of electronic tag implantation in fish in order to ensure that the data generated are relevant to untagged conspecifics (i.e., no long-term behavioural or physiological consequences) and the surgical procedure does not impair the health and welfare status of the tagged fish. To that end, we advocate for (1) rigorous controlled manipulations based on statistical designs that have adequate power, account for inter-individual variation, and include controls and shams, (2) studies that transcend the laboratory and the field with more studies in marine waters, (3) incorporation of knowledge and techniques emerging from the medical and veterinary disciplines, (4) addressing all components of the surgical event, (5) comparative studies that evaluate the same surgical techniques on multiple species and in different environments, (6) consideration of how biotic factors (e.g., sex, age, size) influence tagging outcomes, and (7) studies that cover a range of endpoints over ecologically relevant time periods.
C1 [Cooke, Steven J.] Carleton Univ, Dept Biol, Fish Ecol & Conservat Physiol Lab, Ottawa, ON K1S 5B6, Canada.
[Cooke, Steven J.] Carleton Univ, Inst Environm Sci, Ottawa, ON K1S 5B6, Canada.
[Woodley, Christa M.; Brown, Richard S.] Pacific NW Natl Lab, Ecol Grp, Richland, WA 99352 USA.
[Eppard, M. Brad] US Army Corps Engineers, Portland Dist Off, Portland, OR USA.
[Nielsen, Jennifer L.] US Geol Survey, Alaska Sci Ctr, Anchorage, AK 99508 USA.
RP Cooke, SJ (reprint author), Carleton Univ, Dept Biol, Fish Ecol & Conservat Physiol Lab, 1125 Colonel Dr, Ottawa, ON K1S 5B6, Canada.
EM Steven_Cooke@carleton.ca
RI Cooke, Steven/F-4193-2010
OI Cooke, Steven/0000-0002-5407-0659
FU United States Army Corps of Engineers, Portland District under Pacific
Northwest National Laboratory [DE-AC05-76RL01830]
FX Cooke was supported by the United States Army Corps of Engineers,
Portland District under contract from the Pacific Northwest National
Laboratory (Contract # DE-AC05-76RL01830). Additional support was
provided by Carleton University, the Canada Research Chairs Program, and
the Ocean Telemetry Network Canada. Chris Holbrook, Karen Murchie and an
anonymous referee kindly provided comments on the manuscript. Any
reference to trade names does not indicate endorsement by the US Federal
Government.
NR 134
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U1 2
U2 52
PU SPRINGER
PI DORDRECHT
PA VAN GODEWIJCKSTRAAT 30, 3311 GZ DORDRECHT, NETHERLANDS
SN 0960-3166
EI 1573-5184
J9 REV FISH BIOL FISHER
JI Rev. Fish. Biol. Fish.
PD MAR
PY 2011
VL 21
IS 1
SI SI
BP 127
EP 151
DI 10.1007/s11160-010-9193-3
PG 25
WC Fisheries; Marine & Freshwater Biology
SC Fisheries; Marine & Freshwater Biology
GA 726WG
UT WOS:000287756700012
ER
PT J
AU Twedt, DJ
AF Twedt, Daniel J.
TI Common Grackle Breeding on Bottomland Forest Restoration Sites
SO SOUTHEASTERN NATURALIST
LA English
DT Article
ID MISSISSIPPI ALLUVIAL VALLEY; QUISCALUS-QUISCULA; NEST SUCCESS; HABITAT;
BIRD; REPRODUCTION; CONSERVATION; BLACKBIRDS; VEGETATION; URBAN
AB Two of 36 forest restoration sites in the Mississippi Alluvial Valley surveyed from 2000-2002 harbored Quiscalus quiscula (Common Grackle). Occupied sites were in less-forested landscapes and had sparser understory vegetation due to flooding. Probability of daily nest survival (0.9077) of 169 Common Grackle nests was influenced by nest-placement, temporal, and landscape effects. Age of nest markedly affected nest survival, which increased from <0.89 during egg laying (age < 6 days) to >0.92 when nestlings were present (age > 18 days). Extrapolating daily nest survival to a 31-day nest period resulted in 5% nest success, far less then previously estimated for this species in more northern latitudes and likely less than required to sustain populations on these sites.
C1 US Geol Survey, Patuxent Wildlife Res Ctr, Vicksburg, MS 39180 USA.
RP Twedt, DJ (reprint author), US Geol Survey, Patuxent Wildlife Res Ctr, 2524 S Frontage Rd, Vicksburg, MS 39180 USA.
EM dtwedt@usgs.gov
OI Twedt, Daniel/0000-0003-1223-5045
FU US Geological Survey; US Fish and Wildlife Service; USDA Natural
Resources Conservation Service; University of Georgia
FX Support for this project was provided by the US Geological Survey, US
Fish and Wildlife Service, USDA Natural Resources Conservation Service,
and University of Georgia. I thank S. Somershoe, M. Huskey, and M. Hunt
for field assistance. US Fish and Wildlife Service, Mississippi
Department of Wildlife Fisheries and Parks, and private landowners
graciously allowed access to study sites.
NR 42
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U1 0
U2 10
PU HUMBOLDT FIELD RESEARCH INST
PI STEUBEN
PA PO BOX 9, STEUBEN, ME 04680-0009 USA
SN 1528-7092
EI 1938-5412
J9 SOUTHEAST NAT
JI Southeast. Nat.
PD MAR
PY 2011
VL 10
IS 1
BP 1
EP 10
DI 10.1656/058.010.0101
PG 10
WC Biodiversity Conservation; Ecology
SC Biodiversity & Conservation; Environmental Sciences & Ecology
GA 976RB
UT WOS:000306600900001
ER
PT J
AU Larson, ER
Magoulick, DD
AF Larson, Eric R.
Magoulick, Daniel D.
TI Life-History Notes on Cambarus hubbsi Creaser (Hubbs Crayfish) from the
South Fork Spring River, Arkansas
SO SOUTHEASTERN NATURALIST
LA English
DT Article
ID STREAM-DWELLING CRAYFISH; INVASIVE CRAYFISH; ORCONECTES-EUPUNCTUS; LOTIC
CRAYFISH; FRESH-WATER; HABITAT USE; MISSOURI; DRAINAGE; SIZE;
DISPLACEMENT
AB Many crayfish species native to the southeastern United States are imperiled due to small range sizes and anthropogenic impacts such as habitat loss and introduction of non-native species. Furthermore, effective management of crayfish is limited by the scarcity of life-history and ecological data for many of these species. We report results of the first life-history study of the crayfish Cambarus hubbsi (Hubbs Crayfish). We collected 466 Hubbs Crayfish from the South Fork Spring River, AR throughout 2006 and recorded carapace lengths, wet weights, indicators of reproductive activity, and number of eggs on ovigerous females. Using length-frequency distributions, we identified four Hubbs Crayfish age classes and evaluated growth rates by plotting size by season (winter, spring, summer, autumn). Male Hubbs Crayfish were more common than females in all seasons except autumn, and males weighed more at equivalent lengths than females. Reproductive activity in Hubbs Crayfish peaked in late winter and spring, and ovigerous females were collected in March, April, and June. Ovigerous females were age II or III and carried few eggs relative to co-occurring crayfish of the genus Orconectes. Compared to these Orconectes species, Hubbs Crayfish is comparatively slow growing, long lived, with low reproductive potential, and as a result may be categorized as a K life-history strategist. Based on this species' life-history strategy and previously documented habitat specificity and taxonomic distinctiveness, Hubbs Crayfish may require monitoring and management attention normally reserved for species with smaller ranges.
C1 [Larson, Eric R.] Univ Washington, Sch Aquat & Fishery Sci, Seattle, WA 98105 USA.
[Magoulick, Daniel D.] Univ Arkansas, US Geol Survey, Dept Biol Sci, Arkansas Cooperat Fish & Wildlife Res Unit, Fayetteville, AR 72701 USA.
RP Larson, ER (reprint author), Univ Washington, Sch Aquat & Fishery Sci, Seattle, WA 98105 USA.
EM lars9570@u.washington.edu
RI Larson, Eric/H-3528-2012; Larson, Eric/P-8253-2016
OI Larson, Eric/0000-0002-9232-5907
FU Arkansas Game and Fish Commission; University of Arkansas; US Geological
Survey; Wildlife Management Institute
FX This research was supported by a grant from the Arkansas Game and Fish
Commission. The Arkansas Cooperative Fish and Wildlife Research Unit is
supported by the Arkansas Game and Fish Commission, University of
Arkansas, US Geological Survey, and the Wildlife Management Institute.
We are grateful to the South Fork Resort, Saddle, AR for providing site
access. This manuscript was improved through comments and suggestions
from John Aho, Shawna Herleth-King, Jacob Westhoff, and two anonymous
reviewers.
NR 32
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U1 1
U2 15
PU HUMBOLDT FIELD RESEARCH INST
PI STEUBEN
PA PO BOX 9, STEUBEN, ME 04680-0009 USA
SN 1528-7092
J9 SOUTHEAST NAT
JI Southeast. Nat.
PD MAR
PY 2011
VL 10
IS 1
BP 121
EP 132
DI 10.1656/058.010.0110
PG 12
WC Biodiversity Conservation; Ecology
SC Biodiversity & Conservation; Environmental Sciences & Ecology
GA 976RB
UT WOS:000306600900010
ER
PT J
AU Bettoli, PW
Goldsworthy, C
AF Bettoli, Phillip W.
Goldsworthy, Cory
TI Larval Fish Dynamics in Spring Pools in Middle Tennessee
SO SOUTHEASTERN NATURALIST
LA English
DT Article
ID LIGHT-TRAP; GAMBUSIA-HOLBROOKI; MOSQUITOFISH; CHRONOLOGY; ABUNDANCE;
PATTERNS; RIVER; LAKE
AB We used lighted larval traps to assess reproduction by fishes inhabiting nine spring pools in the Barrens Plateau region of middle Tennessee between May and September 2004. The traps (n = 162 deployments) captured the larval or juvenile forms of Etheostoma crossopterum (Fringed Darter) (n = 188), Gambusia affinis (Western Mosquitofish) (n = 139), Hemitremia flammea (Flame Chub) (n = 55), the imperiled Fundulus julisia (Barrens Topminnow) (n = 10), and Forbesichthys agassizii (Spring Cavefish) (n = 1). The larval forms of four other species (Families Centrarchidae, Cyprinidae, and Cottidae) were not collected, despite the presence of adults. Larval Barrens Topminnow hatched over a protracted period (early June through late September); in contrast, hatching intervals were much shorter for Fringed Darter (mid-May through early June). Flame Chub hatching began before our first samples in early May and concluded by late-May. Juvenile Western Mosquitofish were collected between early June and late August. Our sampling revealed that at least two species (Flame Chub and Fringed Darter) were able to reproduce and recruit in habitats harboring the invasive Western Mosquitofish, while Barrens Topminnow could not.
C1 [Bettoli, Phillip W.] Tennessee Technol Univ, US Geol Survey, Tennessee Cooperat Fishery Res Unit, Cookeville, TN 38505 USA.
[Goldsworthy, Cory] Minnesota Dept Nat Resources, Duluth, MN 55804 USA.
RP Bettoli, PW (reprint author), Tennessee Technol Univ, US Geol Survey, Tennessee Cooperat Fishery Res Unit, Box 5114, Cookeville, TN 38505 USA.
EM pbettoli@tntech.edu
FU Tennessee Wildlife Resources Agency; US Fish and Wildlife Service;
Nature Conservancy of Tennessee; Center for the Management, Utilization,
and Protection of Water Resources at Tennessee Technological University;
US Geological Survey
FX Funding and support for this project was provided by the Tennessee
Wildlife Resources Agency, the US Fish and Wildlife Service, and The
Nature Conservancy of Tennessee. Additional support was provided by the
Center for the Management, Utilization, and Protection of Water
Resources at Tennessee Technological University, and the US Geological
Survey. This manuscript benefited from the constructive comments offered
by A. George, S. Chipps, G. Adams, and an anonymous reviewer.
NR 34
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U1 1
U2 9
PU HUMBOLDT FIELD RESEARCH INST
PI STEUBEN
PA PO BOX 9, STEUBEN, ME 04680-0009 USA
SN 1528-7092
J9 SOUTHEAST NAT
JI Southeast. Nat.
PD MAR
PY 2011
VL 10
IS 1
BP 145
EP 154
DI 10.1656/058.010.0112
PG 10
WC Biodiversity Conservation; Ecology
SC Biodiversity & Conservation; Environmental Sciences & Ecology
GA 976RB
UT WOS:000306600900012
ER
PT J
AU Berdeen, JB
Otis, DL
AF Berdeen, James B.
Otis, David L.
TI An Observation of a Partially Albinistic Zenaida macroura (Mourning
Dove)
SO SOUTHEASTERN NATURALIST
LA English
DT Article
ID AGE
AB Three of the 4 forms of albinism that occur in avifauna have been detected in Zenaida macroura (Mourning Dove). Albinism is rare in this species, and the incidence rate of each age and sex cohort is not well known. Consequently, we examined the pigmentation of Mourning Doves encountered in the Coastal Plain of South Carolina, and classified the age and sex of all individuals. One adult male Mourning Dove had unusually light coloration of some feathers and the upper mandible. This pigmentation is consistent with partial albinism. This was the only individual out of 10,749 examined that appeared to be albinistic. This low incidence rate of albinism supports the conclusion that this condition is relatively rare in Mourning Doves (Mirarchi 1993).
C1 [Berdeen, James B.] Clemson Univ, Dept Aquaculture Fisheries & Wildlife, Clemson, SC 29634 USA.
[Otis, David L.] Clemson Univ, US Geol Survey, S Carolina Cooperat Fish & Wildlife Res Unit, Clemson, SC 29634 USA.
RP Berdeen, JB (reprint author), Minnesota Dept Nat Resources, Wetland Wildlife Populat & Res Grp, 102 23rd St NE, Bemidji, MN 56601 USA.
EM james.berdeen@gmail.com
FU US Fish and Wildlife Service Webless Migratory Upland Game Bird Research
Fund; USGS - Biological Resources Division South Carolina Cooperative
Fish and Wildlife Research Unit; South Carolina Department of Natural
Resources (DNR); South Carolina Public Service Authority; Clemson
University; Safari Club International
FX Funding for this project was provided by the US Fish and Wildlife
Service Webless Migratory Upland Game Bird Research Fund, USGS -
Biological Resources Division South Carolina Cooperative Fish and
Wildlife Research Unit, South Carolina Department of Natural Resources
(DNR), South Carolina Public Service Authority (Santee Cooper), Clemson
University, and Safari Club International. Logistical support was
provided by Santee NWR and DNR personnel. Employees of the Clemson
University Godley-Snell Research Center provided digital photo images of
the albinistic Mourning Dove. We thank M. Anteau, J. Burnham III, L.
Cookman, C. Grondin, A. Hutchins, and K. Sughrue for assistance with
field research. D. Rave provided helpful comments on an earlier version
of this manuscript.
NR 14
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U1 0
U2 3
PU HUMBOLDT FIELD RESEARCH INST
PI STEUBEN
PA PO BOX 9, STEUBEN, ME 04680-0009 USA
SN 1528-7092
J9 SOUTHEAST NAT
JI Southeast. Nat.
PD MAR
PY 2011
VL 10
IS 1
BP 185
EP 188
DI 10.1656/058.010.0117
PG 4
WC Biodiversity Conservation; Ecology
SC Biodiversity & Conservation; Environmental Sciences & Ecology
GA 976RB
UT WOS:000306600900017
ER
PT J
AU Gumma, MK
Thenkabail, PS
Nelson, A
AF Gumma, Murali Krishna
Thenkabail, Prasad S.
Nelson, Andrew
TI Mapping Irrigated Areas Using MODIS 250 Meter Time-Series Data: A Study
on Krishna River Basin (India)
SO WATER
LA English
DT Article
DE ground water irrigated areas; MODIS; NDVI; irrigated areas; Krishna
Basin
ID AVHRR DATA; CLASSIFICATION; PRIORITIES
AB Mapping irrigated areas of a river basin is important in terms of assessing water use and food security. This paper describes an innovative remote sensing based vegetation phenological approach to map irrigated areas and then the differentiates the ground water irrigated areas from the surface water irrigated areas in the Krishna river basin (26,575,200 hectares) in India using MODIS 250 meter every 8-day near continuous time-series data for 2000-2001. Temporal variations in the Normalized Difference Vegetation Index (NDVI) pattern obtained in irrigated classes enabled demarcation between: (a) irrigated surface water double crop, (b) irrigated surface water continuous crop, and (c) irrigated ground water mixed crops. The NDVI patterns were found to be more consistent in areas irrigated with ground water due to the continuity of water supply. Surface water availability, on the other hand, was dependent on canal water release that affected time of crop sowing and growth stages, which was in turn reflected in the NDVI pattern. Double cropped and light irrigation have relatively late onset of greenness, because they use canal water from reservoirs that drain large catchments and take weeks to fill. Minor irrigation and ground water irrigated areas have early onset of greenness because they drain smaller catchments where aquifers and reservoirs fill more quickly. Vegetation phonologies of 9 distinct classes consisting of Irrigated, rainfed, and other land use classes were also derived using MODIS 250 meter near continuous time-series data that were tested and verified using groundtruth data, Google Earth very high resolution (sub-meter to 4 meter) imagery, and state-level census data. Fuzzy classification accuracies for most classes were around 80% with class mixing mainly between various irrigated classes. The areas estimated from MODIS were highly correlated with census data (R-squared value of 0.86).
C1 [Gumma, Murali Krishna; Nelson, Andrew] Int Rice Res Inst, Los Banos 7777, Philippines.
[Thenkabail, Prasad S.] US Geol Survey, SW Geog Sci Ctr, Flagstaff, AZ 86001 USA.
RP Gumma, MK (reprint author), Int Rice Res Inst, Los Banos 7777, Philippines.
EM m.gumma@irri.org; pthenkabail@usgs.gov; a.nelson@irri.org
RI Nelson, Andrew/G-3649-2012
OI Nelson, Andrew/0000-0002-7249-3778
FU International Water Management (IWMI); Australian Centre for
International Agriculture Research (ACIAR)
FX The authors would like to gratefully acknowledge the support of the
International Water Management (IWMI) and Australian Centre for
International Agriculture Research (ACIAR). We would like to also thank
Paul Pavelic, Senior Researcher, IWMI, and Hyderabad who was encouraging
during initial stage. The authors would like to thank Sreedhar Acharya
for providing census data. The MODIS data were provided through Earth
Observing system data and Information System (EOSDIS), so we would like
to thank them for this wonderful service. The paper is not internally
reviewed by the US Geological Survey (USGS), and the opinions expressed
in the paper are those of the authors and not those of USGS.
NR 20
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U1 1
U2 11
PU MDPI AG
PI BASEL
PA POSTFACH, CH-4005 BASEL, SWITZERLAND
SN 2073-4441
J9 WATER-SUI
JI Water
PD MAR
PY 2011
VL 3
IS 1
BP 113
EP 131
DI 10.3390/w3010113
PG 19
WC Water Resources
SC Water Resources
GA 053ES
UT WOS:000312254300006
ER
PT J
AU Mcroberts, JT
Butler, MJ
Ballard, WB
Wallace, MC
Whitlaw, HA
Haukos, DA
AF Mcroberts, Jon T.
Butler, Matthew J.
Ballard, Warren B.
Wallace, Mark C.
Whitlaw, Heather A.
Haukos, David A.
TI Response of Lesser Prairie-Chickens on Leks to Aerial Surveys
SO WILDLIFE SOCIETY BULLETIN
LA English
DT Article
DE aerial survey; behavior; disturbance; helicopter; lek; lesser
prairie-chicken; New Mexico; Texas; Tympanuchus pallidicinctus
AB Aerial surveys can be used to detect and monitor lesser prairie-chicken (Tympanuchus pallidicinctus) leks, but the need exists to understand the response of lesser prairie-chickens to survey aircraft. We conducted lek surveys in Texas and New Mexico, USA, using an R-22 Beta II helicopter and R-44 Raven II helicopter. We observed the behavior of lesser prairie-chickens at 44 leks during aerial lek surveys. We observed flush responses of 38.5% (20.2-59.4%; 95% CI) and 50.0% (26.0-74.0%) from the R-22 and R-44, respectively. We found no difference in flush response between helicopter types (P = 0.326). We used logistic regression models to predict lesser prairie-chicken flush response to aerial surveys. We found that distance from the transect was the most important flush response predictor during helicopter surveys. When flushed, lesser prairie-chickens returned to the lek and resumed predisturbance behavior in 7.0 +/- 2.6 min (mean +/- 95% CI). Our results suggest aerial surveys can be conducted without disruption to the lesser prairie-chicken lek dynamic. (C) 2011 The Wildlife Society.
C1 [Mcroberts, Jon T.; Butler, Matthew J.; Ballard, Warren B.; Wallace, Mark C.] Texas Tech Univ, Dept Nat Resources Management, Lubbock, TX 79409 USA.
[Whitlaw, Heather A.] Texas Parks & Wildlife Dept, Lubbock, TX 79409 USA.
[Haukos, David A.] US Fish & Wildlife Serv, Lubbock, TX 79409 USA.
RP Mcroberts, JT (reprint author), Texas Tech Univ, Dept Nat Resources Management, POB 42125, Lubbock, TX 79409 USA.
EM jon.mcroberts@ttu.edu
FU Federal Aid in Wildlife Restoration Act under Pittman-Robertson project
[W-126-R]; Dr. Donald and Sammie Bricker Foundation; Houston Safari Club
FX We thank J. Bonner, D. Lucia, D. Wright, and D. Holdstock, Texas Parks
and Wildlife Department (TPWD), for their commitment to the success of
this project. We also thank V. Bevill and R. Roegner, TPWD, for their
support in project funding by the Federal Aid in Wildlife Restoration
Act under Pittman-Robertson project W-126-R. J. Hughes, U.S. Fish and
Wildlife Service, P. McDaniel, The Nature Conservancy, and E. Jaquez and
T. Allen, U.S. Bureau of Land Management, were of great assistance in
logistical support during this study. We thank technicians E. Bruns and
L. (Rucker) Parks for their hard work, and thank R. Herbert, S. Rode,
and A. Teague for conducting ground observations. We are grateful to the
private landowners of Texas and New Mexico for allowing us to monitor
leks on their property. We also thank Texas Tech University Department
of Natural Resources Management graduate and undergraduate students for
volunteering for project field work. Financial support from the Dr.
Donald and Sammie Bricker Foundation and the Houston Safari Club was
greatly appreciated.
NR 29
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U1 2
U2 4
PU WILEY-BLACKWELL
PI HOBOKEN
PA 111 RIVER ST, HOBOKEN 07030-5774, NJ USA
SN 1938-5463
J9 WILDLIFE SOC B
JI Wildl. Soc. Bull.
PD MAR
PY 2011
VL 35
IS 1
BP 27
EP 31
DI 10.1002/wsb.1
PG 5
WC Biodiversity Conservation
SC Biodiversity & Conservation
GA V38GT
UT WOS:000209332600006
ER
PT J
AU McNutt, SR
AF McNutt, Stephen R.
TI EARTH SCIENCE Volcanic tremor wags on
SO NATURE
LA English
DT Editorial Material
ID SEISMICITY
C1 Univ Alaska Fairbanks, Inst Geophys, Alaska Volcano Observ, Fairbanks, AK 99775 USA.
RP McNutt, SR (reprint author), Univ Alaska Fairbanks, Inst Geophys, Alaska Volcano Observ, 903 Koyukuk Dr, Fairbanks, AK 99775 USA.
EM steve@giseis.alaska.edu
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U1 0
U2 4
PU NATURE PUBLISHING GROUP
PI LONDON
PA MACMILLAN BUILDING, 4 CRINAN ST, LONDON N1 9XW, ENGLAND
SN 0028-0836
J9 NATURE
JI Nature
PD FEB 24
PY 2011
VL 470
IS 7335
BP 471
EP 472
DI 10.1038/470471a
PG 2
WC Multidisciplinary Sciences
SC Science & Technology - Other Topics
GA 725NT
UT WOS:000287652900026
PM 21350475
ER
PT J
AU Fawcett, PJ
Werne, JP
Anderson, RS
Heikoop, JM
Brown, ET
Berke, MA
Smith, SJ
Goff, F
Donohoo-Hurley, L
Cisneros-Dozal, LM
Schouten, S
Damste, JSS
Huang, YS
Toney, J
Fessenden, J
WoldeGabriel, G
Atudorei, V
Geissman, JW
Allen, CD
AF Fawcett, Peter J.
Werne, Josef P.
Anderson, R. Scott
Heikoop, Jeffrey M.
Brown, Erik T.
Berke, Melissa A.
Smith, Susan J.
Goff, Fraser
Donohoo-Hurley, Linda
Cisneros-Dozal, Luz M.
Schouten, Stefan
Damste, Jaap S. Sinninghe
Huang, Yongsong
Toney, Jaime
Fessenden, Julianna
WoldeGabriel, Giday
Atudorei, Viorel
Geissman, John W.
Allen, Craig D.
TI Extended megadroughts in the southwestern United States during
Pleistocene interglacials
SO NATURE
LA English
DT Article
ID PAST 800,000 YEARS; CLIMATE VARIABILITY; NORTH-AMERICA; DROUGHT;
MONSOON; RECONSTRUCTIONS; TRANSITION; ATLANTIC; AFRICA; RECORD
AB The potential for increased drought frequency and severity linked to anthropogenic climate change in the semi-arid regions of the southwestern United States (US) is a serious concern(1). Multi-year droughts during the instrumental period(2) and decadal-length droughts of the past two millennia(1,3) were shorter and climatically different from the future permanent, 'dust-bowl-like' mega-drought conditions, lasting decades to a century, that are predicted as a consequence of warming(4). So far, it has been unclear whether or not such megadroughts occurred in the southwestern US, and, if so, with what regularity and intensity. Here we show that periods of aridity lasting centuries to millennia occurred in the southwestern US during mid-Pleistocene interglacials. Using molecular palaeo-temperature proxies(5) to reconstruct the mean annual temperature (MAT) in mid-Pleistocene lacustrine sediment from the Valles Caldera, New Mexico, we found that the driest conditions occurred during the warmest phases of interglacials, when the MAT was comparable to or higher than the modern MAT. A collapse of drought-tolerant C(4) plant communities during these warm, dry intervals indicates a significant reduction in summer precipitation, possibly in response to a poleward migration of the subtropical dry zone. Three MAT cycles similar to 2 degrees C in amplitude occurred within Marine Isotope Stage (MIS) 11 and seem to correspond to the muted precessional cycles within this interglacial. In comparison with MIS 11, MIS 13 experienced higher precessional-cycle amplitudes, larger variations in MAT (4-6 degrees C) and a longer period of extended warmth, suggesting that local insolation variations were important to interglacial climatic variability in the southwestern US. Comparison of the early MIS 11 climate record with the Holocene record shows many similarities and implies that, in the absence of anthropogenic forcing, the region should be entering a cooler and wetter phase.
C1 [Fawcett, Peter J.; Goff, Fraser; Donohoo-Hurley, Linda; Atudorei, Viorel; Geissman, John W.] Univ New Mexico, Dept Earth & Planetary Sci, Albuquerque, NM 87131 USA.
[Werne, Josef P.] Univ Minnesota, Dept Chem & Biochem, Duluth, MN 55812 USA.
[Werne, Josef P.; Brown, Erik T.; Berke, Melissa A.] Univ Minnesota, Large Lakes Observ, Duluth, MN 55812 USA.
[Brown, Erik T.; Berke, Melissa A.] Univ Minnesota, Dept Geol Sci, Duluth, MN 55812 USA.
[Werne, Josef P.] Univ Western Australia, Ctr Water Res, Crawley, WA 6009, Australia.
[Werne, Josef P.] Curtin Univ Technol, WA Organ & Isotope Geochem Ctr, Bentley, WA 6845, Australia.
[Anderson, R. Scott; Fessenden, Julianna; WoldeGabriel, Giday] Univ Arizona, Sch Earth Sci & Environm Sustainabil, Flagstaff, AZ 86011 USA.
[Anderson, R. Scott; Smith, Susan J.] Univ Arizona, Bilby Res Ctr, Lab Paleoecol, Flagstaff, AZ 86011 USA.
[Heikoop, Jeffrey M.; Cisneros-Dozal, Luz M.; Toney, Jaime] Los Alamos Natl Lab, Div Earth & Environm Sci, Los Alamos, NM 87545 USA.
[Schouten, Stefan; Damste, Jaap S. Sinninghe] NIOZ Royal Netherlands Inst Sea Res, Dept Marine Organ Biogeochem, NL-1790 AB Den Burg, Netherlands.
[Huang, Yongsong] Brown Univ, Dept Geol Sci, Providence, RI 02912 USA.
[Allen, Craig D.] USGS Ft Collins Sci Ctr, Jemez Mt Field Stn, Los Alamos, NM 87544 USA.
RP Fawcett, PJ (reprint author), Univ New Mexico, Dept Earth & Planetary Sci, Albuquerque, NM 87131 USA.
EM fawcett@unm.edu
RI Heikoop, Jeffrey/C-1163-2011; Toney, Jaime/I-5083-2012; Sinninghe
Damste, Jaap/F-6128-2011;
OI Toney, Jaime/0000-0003-3182-6887; Sinninghe Damste,
Jaap/0000-0002-8683-1854; Heikoop, Jeffrey/0000-0001-7648-3385
FU NSF; IGPP LANL; USGS Western Mountain Initiative; Gledden Fellowship
FX We thank A. Mets for analytical support, W. McIntosh for the Ar-Ar age
determination, T. Wawrzyniec and A. Ellwein for drilling help, and the
Valles Caldera Trust for permission to drill in the Valle Grande. Core
assistance was provided by LRC/LacCore. This work was supported by the
NSF Paleoclimate and P2C2 programs, IGPP LANL and the USGS Western
Mountain Initiative. Support from the Gledden Fellowship is
acknowledged. This work forms contribution 2399-JW at the Centre for
Water Research, The University of Western Australia and contribution 131
at the Laboratory of Paleoecology, Northern Arizona University.
NR 28
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U1 6
U2 114
PU NATURE PUBLISHING GROUP
PI LONDON
PA MACMILLAN BUILDING, 4 CRINAN ST, LONDON N1 9XW, ENGLAND
SN 0028-0836
J9 NATURE
JI Nature
PD FEB 24
PY 2011
VL 470
IS 7335
BP 518
EP 521
DI 10.1038/nature09839
PG 4
WC Multidisciplinary Sciences
SC Science & Technology - Other Topics
GA 725NT
UT WOS:000287652900038
PM 21350483
ER
PT J
AU Murcia, S
Kerans, BL
MacConnell, E
Koel, TM
AF Murcia, Silvia
Kerans, Billie L.
MacConnell, Elizabeth
Koel, Todd M.
TI Correlation of environmental attributes with histopathology of native
Yellowstone cutthroat trout naturally infected with Myxobolus cerebralis
SO DISEASES OF AQUATIC ORGANISMS
LA English
DT Article
DE Whirling disease; Pathogen; Invasion-environment synergism; Canonical
correlation; Yellowstone ecosystem
ID SALMONID WHIRLING-DISEASE; SNAKE RIVER CUTTHROAT; RAINBOW-TROUT;
ONCORHYNCHUS-MYKISS; MYXOSOMA-CEREBRALIS; PARASITE; HOST;
SUSCEPTIBILITY; EXPOSURE; SURVIVAL
AB Infection by the invasive parasite Myxobolus cerebralis (causing whirling disease in salmonids) is strongly influenced by a stream's physico-chemical characteristics, which might affect host pathology. We examined whether environmental variables of a M. cerebralis-positive tributary to Yellowstone Lake, Yellowstone National Park, USA, correlated with the histopathology of naturally infected native cutthroat trout Oncorhynchus clarkii bouvieri. Host inflammatory response and cranial cartilage lesions were the main correlates with whirling behavior. Canonical correlation analyses showed that the prevalence of trout with severe lesions in the cranial and jaw cartilages was highest in stream sites with a combination of high temperature and low specific conductivity. Our results reveal that environmental components can affect when and where a pathogen resides within the host, and manifestation of disease. Recognition of the synergism among environmental and histopathology factors most conducive to whirling disease will increase our prediction and detection abilities for M. cerebralis in salmonid hosts.
C1 [Murcia, Silvia; Kerans, Billie L.] Montana State Univ, Dept Ecol, Bozeman, MT 59717 USA.
[MacConnell, Elizabeth] US Fish & Wildlife Serv, Bozeman Fish Hlth Ctr, Bozeman, MT 59715 USA.
[Koel, Todd M.] Ctr Resources, Fisheries & Aquat Sci Sect, Yellowstone Natl Pk, WY 82190 USA.
RP Murcia, S (reprint author), Univ Magallanes, Inst Patagonia, Dept Sci & Nat Resources, Punta Arenas, Chilean Antarct, Chile.
EM silvia.murcia@umag.cl
FU Whirling Disease Initiative of the National Partnership on Management of
Wild and Native Cold Water Fisheries; Center for Resources-Yellowstone
National Park; Rocky Mountain Center for Ecosystems Studies Unit
(National Park Service); Montana State University-Bozeman; Chilean
National Commission for Research in Science and Technology (CONICYT)
[PDA-10]; Institute of Ecology and Biodiversity and its LTSER Network
FX This research was made possible by funding from the Whirling Disease
Initiative of the National Partnership on Management of Wild and Native
Cold Water Fisheries, the Center for Resources-Yellowstone National
Park, the Rocky Mountain Center for Ecosystems Studies Unit (National
Park Service), and a Graduate Assistantship from Montana State
University-Bozeman. The manuscript was improved by comments from 2
reviewers; part of its preparation was supported by a post-doctoral
contract to S. M. through funds from the Chilean National Commission for
Research in Science and Technology (CONICYT) Bicentennial Program (PBCT)
Project PDA-10 to A. Mansilla, University of Magallanes-Omora
Ethnobotanical Park (www.umag.cl/williams; www.omora.org), Institute of
Ecology and Biodiversity and its LTSER Network (www.ieb-chile.cl/ltser).
NR 56
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U1 2
U2 24
PU INTER-RESEARCH
PI OLDENDORF LUHE
PA NORDBUNTE 23, D-21385 OLDENDORF LUHE, GERMANY
SN 0177-5103
EI 1616-1580
J9 DIS AQUAT ORGAN
JI Dis. Aquat. Org.
PD FEB 22
PY 2011
VL 93
IS 3
BP 225
EP 234
DI 10.3354/dao02295
PG 10
WC Fisheries; Veterinary Sciences
SC Fisheries; Veterinary Sciences
GA 725TC
UT WOS:000287668000006
PM 21516975
ER
PT J
AU Gomez-Uchida, D
Seeb, JE
Smith, MJ
Habicht, C
Quinn, TP
Seeb, LW
AF Gomez-Uchida, Daniel
Seeb, James E.
Smith, Matt J.
Habicht, Christopher
Quinn, Thomas P.
Seeb, Lisa W.
TI Single nucleotide polymorphisms unravel hierarchical divergence and
signatures of selection among Alaskan sockeye salmon (Oncorhynchus
nerka) populations
SO BMC EVOLUTIONARY BIOLOGY
LA English
DT Article
ID MAJOR HISTOCOMPATIBILITY COMPLEX; ATLANTIC SALMON; PACIFIC SALMON;
GENETIC-VARIATION; CHINOOK SALMON; LOCAL ADAPTATION; NATURAL-SELECTION;
BRITISH-COLUMBIA; ALLELE FREQUENCY; KVICHAK RIVER
AB Background: Disentangling the roles of geography and ecology driving population divergence and distinguishing adaptive from neutral evolution at the molecular level have been common goals among evolutionary and conservation biologists. Using single nucleotide polymorphism (SNP) multilocus genotypes for 31 sockeye salmon (Oncorhynchus nerka) populations from the Kvichak River, Alaska, we assessed the relative roles of geography (discrete boundaries or continuous distance) and ecology (spawning habitat and timing) driving genetic divergence in this species at varying spatial scales within the drainage. We also evaluated two outlier detection methods to characterize candidate SNPs responding to environmental selection, emphasizing which mechanism(s) may maintain the genetic variation of outlier loci.
Results: For the entire drainage, Mantel tests suggested a greater role of geographic distance on population divergence than differences in spawn timing when each variable was correlated with pairwise genetic distances. Clustering and hierarchical analyses of molecular variance indicated that the largest genetic differentiation occurred between populations from distinct lakes or subdrainages. Within one population-rich lake, however, Mantel tests suggested a greater role of spawn timing than geographic distance on population divergence when each variable was correlated with pairwise genetic distances. Variable spawn timing among populations was linked to specific spawning habitats as revealed by principal coordinate analyses. We additionally identified two outlier SNPs located in the major histocompatibility complex (MHC) class II that appeared robust to violations of demographic assumptions from an initial pool of eight candidates for selection.
Conclusions: First, our results suggest that geography and ecology have influenced genetic divergence between Alaskan sockeye salmon populations in a hierarchical manner depending on the spatial scale. Second, we found consistent evidence for diversifying selection in two loci located in the MHC class II by means of outlier detection methods; yet, alternative scenarios for the evolution of these loci were also evaluated. Both conclusions argue that historical contingency and contemporary adaptation have likely driven differentiation between Kvichak River sockeye salmon populations, as revealed by a suite of SNPs. Our findings highlight the need for conservation of complex population structure, because it provides resilience in the face of environmental change, both natural and anthropogenic.
C1 [Gomez-Uchida, Daniel; Seeb, James E.; Smith, Matt J.; Quinn, Thomas P.; Seeb, Lisa W.] Sch Aquat & Fishery Sci, Seattle, WA 98195 USA.
[Smith, Matt J.] US Fish & Wildlife Serv, Abernathy Fish Technol Ctr, Longview, WA 98632 USA.
[Habicht, Christopher] Alaska Dept Fish & Game, Div Commercial Fisheries, Anchorage, AK 99518 USA.
RP Gomez-Uchida, D (reprint author), Sch Aquat & Fishery Sci, 1122 Boat St NE,Box 355020, Seattle, WA 98195 USA.
EM dgu@uw.edu
FU State of Alaska; Alaska Disaster Grant; National Park Service; US Fish
and Wildlife Service Office of Subsistence Management, North Pacific
Anadromous Fish Commission; North Pacific Research Board; National
Marine Fisheries Service; Bristol Bay Science and Research Institute;
Gordon and Betty Moore Foundation
FX Building the baseline for sockeye salmon in Bristol Bay has been ongoing
since the mid-1990s and has been financially supported through funding
from the State of Alaska, Alaska Disaster Grant, National Park Service,
US Fish and Wildlife Service Office of Subsistence Management, North
Pacific Anadromous Fish Commission, North Pacific Research Board,
National Marine Fisheries Service, and Bristol Bay Science and Research
Institute. We thank the many people who helped collect samples used in
the baseline, including S. Morstad and other staff from Alaska
Department of Fish and Game (ADF&G) King Salmon office; Gregory Buck and
Harry B. Rich, Jr. (University of Washington); C. A. Woody (U. S.
Geological Survey), D. Young (National Park Service); and K. Ramstad
(University of Montana). We thank the dedicated ADF&G laboratory staff
who processed the samples and I. Stewart for facilitating a matrix of
geographic distances between populations for the Kvichak subdrainage. We
also thank M. Ackerman, L. Creelman, J. Lin, M. McGlauflin, K. O'Malley,
and two anonymous reviewers for suggestions on earlier versions of the
manuscript. C. Pascal helped with the analysis of SNPs within MHC class
II genes. S. Kalinowski and T. Seamons stimulated discussions about the
methodological approaches used in the study. Funding for the analysis
and writing of this manuscript was provided by a grant to the University
of Washington from the Gordon and Betty Moore Foundation.
NR 97
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U1 1
U2 30
PU BIOMED CENTRAL LTD
PI LONDON
PA 236 GRAYS INN RD, FLOOR 6, LONDON WC1X 8HL, ENGLAND
SN 1471-2148
J9 BMC EVOL BIOL
JI BMC Evol. Biol.
PD FEB 18
PY 2011
VL 11
AR 48
DI 10.1186/1471-2148-11-48
PG 17
WC Evolutionary Biology; Genetics & Heredity
SC Evolutionary Biology; Genetics & Heredity
GA 748SN
UT WOS:000289411800002
PM 21332997
ER
PT J
AU Ruppert, NA
Prejean, S
Hansen, RA
AF Ruppert, Natalia A.
Prejean, Stephanie
Hansen, Roger A.
TI Seismic swarm associated with the 2008 eruption of Kasatochi Volcano,
Alaska: Earthquake locations and source parameters
SO JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH
LA English
DT Article
ID LONG VALLEY CALDERA; SATELLITE RADAR INTERFEROMETRY; FAULT PLANE
SOLUTIONS; VELOCITY STRUCTURE; CALIFORNIA; STRESS; RELOCATION;
DEFORMATION; MECHANISMS; ALGORITHM
AB An energetic seismic swarm accompanied an eruption of Kasatochi Volcano in the central Aleutian volcanic arc in August of 2008. In retrospect, the first earthquakes in the swarm were detected about 1 month prior to the eruption onset. Activity in the swarm quickly intensified less than 48 h prior to the first large explosion and subsequently subsided with decline of eruptive activity. The largest earthquake measured as moment magnitude 5.8, and a dozen additional earthquakes were larger than magnitude 4. The swarm exhibited both tectonic and volcanic characteristics. Its shear failure earthquake features were b value = 0.9, most earthquakes with impulsive P and S arrivals and higher-frequency content, and earthquake faulting parameters consistent with regional tectonic stresses. Its volcanic or fluid-influenced seismicity features were volcanic tremor, large CLVD components in moment tensor solutions, and increasing magnitudes with time. Earthquake location tests suggest that the earthquakes occurred in a distributed volume elongated in the NS direction either directly under the volcano or within 5-10 km south of it. Following the MW 5.8 event, earthquakes occurred in a new crustal volume slightly east and north of the previous earthquakes. The central Aleutian Arc is a tectonically active region with seismicity occurring in the crusts of the Pacific and North American plates in addition to interplate events. We postulate that the Kasatochi seismic swarm was a manifestation of the complex interaction of tectonic and magmatic processes in the Earth's crust. Although magmatic intrusion triggered the earthquakes in the swarm, the earthquakes failed in context of the regional stress field.
C1 [Ruppert, Natalia A.; Hansen, Roger A.] Univ Alaska Fairbanks, Alaska Earthquake Informat Ctr, Fairbanks, AK 99775 USA.
[Prejean, Stephanie] USGS, Alaska Volcano Observ, Anchorage, AK 99508 USA.
RP Ruppert, NA (reprint author), Univ Alaska Fairbanks, Alaska Earthquake Informat Ctr, Fairbanks, AK 99775 USA.
EM natasha@gi.alaska.edu
FU Geophysical Institute, University of Alaska Fairbanks; Office of the
Alaska State Seismologist
FX The authors thank the U. S. Fish and Wildlife service for providing felt
reports of seismicity on Kasatochi Island. We also thank anonymous
reviewers, Michelle Coombs, and John Power for constructive reviews.
Financial support in part was provided by the Geophysical Institute,
University of Alaska Fairbanks and Office of the Alaska State
Seismologist (N.A.R. and R.A.H.). Moment tensors were computed using the
tdmt-invc package developed by Douglas Dreger of the Berkeley
Seismological Laboratory, and Green's functions were computed using
FKRPROG software developed by Chandan Saikia with URS Granger, Woodward
Clyde Federal Services. MATLAB and GMT were used to make figures and
plots. AVO seismic stations used in this study were originally installed
with funding from the Federal Aviation Administration. Parametric
earthquake data is from the AEIC earthquake catalog. Waveform data was
recorded by AVO, AEIC and GSN stations in the central
NR 52
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U2 8
PU AMER GEOPHYSICAL UNION
PI WASHINGTON
PA 2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA
SN 2169-9313
EI 2169-9356
J9 J GEOPHYS RES-SOL EA
JI J. Geophys. Res.-Solid Earth
PD FEB 18
PY 2011
VL 116
AR B00B07
DI 10.1029/2010JB007435
PG 18
WC Geochemistry & Geophysics
SC Geochemistry & Geophysics
GA 723VL
UT WOS:000287535300001
ER
PT J
AU Aeby, GS
Williams, GJ
Franklin, EC
Haapkyla, J
Harvell, CD
Neale, S
Page, CA
Raymundo, L
Vargas-Angel, B
Willis, BL
Work, TM
Davy, SK
AF Aeby, Greta S.
Williams, Gareth J.
Franklin, Erik C.
Haapkyla, Jessica
Harvell, C. Drew
Neale, Stephen
Page, Cathie A.
Raymundo, Laurie
Vargas-Angel, Bernardo
Willis, Bette L.
Work, Thierry M.
Davy, Simon K.
TI Growth Anomalies on the Coral Genera Acropora and Porites Are Strongly
Associated with Host Density and Human Population Size across the
Indo-Pacific
SO PLOS ONE
LA English
DT Article
ID BLACK BAND DISEASE; GREAT-BARRIER-REEF; EMERGING INFECTIOUS-DISEASES;
NORTHERN FLORIDA-KEYS; CLIMATE-CHANGE; HAWAIIAN-ISLANDS; TRANSMISSION
DYNAMICS; METAGENOMIC ANALYSIS; NUTRIENT ENRICHMENT; MARINE ECOSYSTEMS
AB Growth anomalies (GAs) are common, tumor-like diseases that can cause significant morbidity and decreased fecundity in the major Indo-Pacific reef-building coral genera, Acropora and Porites. GAs are unusually tractable for testing hypotheses about drivers of coral disease because of their pan-Pacific distributions, relatively high occurrence, and unambiguous ease of identification. We modeled multiple disease-environment associations that may underlie the prevalence of Acropora growth anomalies (AGA) (n = 304 surveys) and Porites growth anomalies (PGA) (n = 602 surveys) from across the Indo-Pacific. Nine predictor variables were modeled, including coral host abundance, human population size, and sea surface temperature and ultra-violet radiation anomalies. Prevalence of both AGAs and PGAs were strongly host density-dependent. PGAs additionally showed strong positive associations with human population size. Although this association has been widely posited, this is one of the first broad-scale studies unambiguously linking a coral disease with human population size. These results emphasize that individual coral diseases can show relatively distinct patterns of association with environmental predictors, even in similar diseases (growth anomalies) found on different host genera (Acropora vs. Porites). As human densities and environmental degradation increase globally, the prevalence of coral diseases like PGAs could increase accordingly, halted only perhaps by declines in host density below thresholds required for disease establishment.
C1 [Aeby, Greta S.; Franklin, Erik C.] Hawaii Inst Marine Biol, Kaneohe, HI USA.
[Williams, Gareth J.; Davy, Simon K.] Victoria Univ Wellington, Sch Biol Sci, Wellington, New Zealand.
[Williams, Gareth J.] Univ Calif San Diego, Scripps Inst Oceanog, Ctr Marine Biodivers & Conservat, La Jolla, CA 92093 USA.
[Haapkyla, Jessica; Neale, Stephen; Page, Cathie A.; Willis, Bette L.] James Cook Univ, ARC Ctr Excellence Coral Reef Studies, Townsville, Qld 4811, Australia.
[Haapkyla, Jessica; Neale, Stephen; Page, Cathie A.; Willis, Bette L.] James Cook Univ, Sch Marine & Trop Biol, Townsville, Qld 4811, Australia.
[Harvell, C. Drew] Cornell Univ, Dept Ecol & Evolutionary Biol, Ithaca, NY USA.
[Harvell, C. Drew] Australian Inst Marine Sci, Townsville, Qld 4810, Australia.
[Raymundo, Laurie] Univ Guam, Marine Lab, Univ Guam UOG Stn, Mangilao, GU 96923 USA.
[Vargas-Angel, Bernardo] Univ Hawaii, Joint Inst Marine & Atmospher Res, Honolulu, HI 96822 USA.
[Work, Thierry M.] US Geol Survey, Natl Wildlife Hlth Ctr, Honolulu Field Stn, Honolulu, HI USA.
RP Aeby, GS (reprint author), Hawaii Inst Marine Biol, Kaneohe, HI USA.
EM greta@hawaii.edu; gareth@ucsd.edu
RI Work, Thierry/F-1550-2015
OI Work, Thierry/0000-0002-4426-9090
FU Center for International Earth Science Information Network (CIESIN),
Columbia University; United Nations Food and Agriculture Programme
(FAO); National Aeronautics and Space Administration [NAS5-03117];
Office of National Marine Sanctuaries (NWHICRER) [MOA-2005-008/6882];
Australian Research Council; Global Environment Fund (GEF)/World Bank
CRTR Program Coral Disease Working Group; NOAA; Pacific Islands
Fisheries Science Center's Coral Reef Ecosystem Division; Victoria
University of Wellington (VUW); New Zealand International Doctoral
Research Scholarship; National Geographic Society
FX Funding: Human population data was provided by the Center for
International Earth Science Information Network (CIESIN), Columbia
University; United Nations Food and Agriculture Programme (FAO); and
Centro Internacional de Agricultura Tropical (CIAT) with funding from
the National Aeronautics and Space Administration under Contract
NAS5-03117 for the Continued Operation of the Socioeconomic Data and
Applications Center (SEDAC). GA gratefully acknowledges funding from the
Office of National Marine Sanctuaries (NWHICRER MOA-2005-008/6882). BW
acknowledges funding from the Australian Research Council and the Global
Environment Fund (GEF)/World Bank CRTR Program Coral Disease Working
Group. BVA's work was supported by the NOAA Coral Reef Conservation
Program and the Pacific Islands Fisheries Science Center's Coral Reef
Ecosystem Division. GW was supported by a Victoria University of
Wellington (VUW) Vice-Chancellor's Strategic Research Scholarship and a
New Zealand International Doctoral Research Scholarship. GW was
additionally funded by grants from the National Geographic Society and
the VUW Research Fund awarded to SD. LR was supported by the GEF/CRTR
and the NOAA Coral Reef Initiative. The funders had no role in study
design, data collection and analysis, decision to publish, or
preparation of the manuscript.
NR 108
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U1 0
U2 30
PU PUBLIC LIBRARY SCIENCE
PI SAN FRANCISCO
PA 185 BERRY ST, STE 1300, SAN FRANCISCO, CA 94107 USA
SN 1932-6203
J9 PLOS ONE
JI PLoS One
PD FEB 18
PY 2011
VL 6
IS 2
AR e16887
DI 10.1371/journal.pone.0016887
PG 9
WC Multidisciplinary Sciences
SC Science & Technology - Other Topics
GA 723CC
UT WOS:000287482800020
PM 21365011
ER
PT J
AU Reppucci, J
Gardner, B
Lucherini, M
AF Reppucci, Juan
Gardner, Beth
Lucherini, Mauro
TI Estimating detection and density of the Andean cat in the high Andes
SO JOURNAL OF MAMMALOGY
LA English
DT Article
DE Argentina; camera trapping; felids; spatial capture-recapture
ID CAPTURE-RECAPTURE; MAXIMUM-LIKELIHOOD; LEOPARDUS-PARDALIS; ACTIVITY
PATTERNS; FIELD SIGNS; HABITAT USE; POPULATION; ABUNDANCE; CARNIVORES;
ARGENTINA
AB The Andean cat (Leopardus jacobita) is one of the most endangered, yet least known, felids. Although the Andean cat is considered at risk of extinction, rigorous quantitative population studies are lacking. Because physical observations of the Andean cat are difficult to make in the wild, we used a camera-trapping array to photo-capture individuals. The survey was conducted in northwestern Argentina at an elevation of approximately 4,200 m during October-December 2006 and April-June 2007. In each year we deployed 22 pairs of camera traps, which were strategically placed. To estimate detection probability and density we applied models for spatial capture-recapture using a Bayesian framework. Estimated densities were 0.07 and 0.12 individual/km(2) for 2006 and 2007, respectively. Mean baseline detection probability was estimated at 0.07. By comparison, densities of the Pampas cat (Leopardus colocolo), another poorly known fetid that shares its habitat with the Andean cat, were estimated at 0.74-0.79 individual/km(2) in the same study area for 2006 and 2007, and its detection probability was estimated at 0.02. Despite having greater detectability, the Andean cat is rarer in the study region than the Pampas cat. Properly accounting for the detection probability is important in making reliable estimates of density, a key parameter in conservation and management decisions for any species.
C1 [Gardner, Beth] US Geol Survey, Patuxent Wildlife Res Ctr, Laurel, MD 20708 USA.
[Reppucci, Juan; Lucherini, Mauro] Univ Nacl Sur, Dept Biol Bioquim & Farm, Grp Ecol Comportamental Mamiferos, RA-8000 Bahia Blanca, Buenos Aires, Argentina.
[Reppucci, Juan; Lucherini, Mauro] Consejo Nacl Invest Cient & Tecn, RA-8000 Bahia Blanca, Buenos Aires, Argentina.
RP Gardner, B (reprint author), US Geol Survey, Patuxent Wildlife Res Ctr, Laurel, MD 20708 USA.
EM beth_gardner@ncsu.edu
FU BP Conservation Programme; Wildlife Conservation Network; Darwin
Initiative; Whitley Fund for Nature; Wild About Cats; Cat Action
Treasury; Cleveland Zoological Society; Rufford Foundation;
International Society for Endangered Cats Canada; La Torbiera Zoological
Society; Patagonia; National Commission for Scientific and Technological
Research (CONICET); Sidney Byers Charitable Trust
FX We are grateful to P. Perovic, C. Sillero-Zubiri, J. A. Royle, S.
Wisely, 2 anonymous reviewers, and J. Nichols for advice and assistance.
We thank P. Cuello, C. Tellaeche, and all the volunteers and villagers
who contributed to data collection; E. Casanave for providing laboratory
facilities; and J. Sanderson for camera traps. Our project received
support from BP Conservation Programme, Wildlife Conservation Network,
Darwin Initiative, Whitley Fund for Nature, Wild About Cats, Cat Action
Treasury, Cleveland Zoological Society, Rufford Foundation,
International Society for Endangered Cats Canada, La Torbiera Zoological
Society, and Patagonia. We acknowledge the national and provincial
governmental institutions and DBByF of Universidad Nacional del Sur for
endorsing and authorizing the project. JR was supported by a doctoral
scholarship from the National Commission for Scientific and
Technological Research (CONICET) and a training scholarship from the
Sidney Byers Charitable Trust.
NR 53
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U1 1
U2 35
PU OXFORD UNIV PRESS INC
PI CARY
PA JOURNALS DEPT, 2001 EVANS RD, CARY, NC 27513 USA
SN 0022-2372
EI 1545-1542
J9 J MAMMAL
JI J. Mammal.
PD FEB 16
PY 2011
VL 92
IS 1
BP 140
EP 147
DI 10.1644/10-MAMM-A-053.1
PG 8
WC Zoology
SC Zoology
GA 728TZ
UT WOS:000287898700015
ER
PT J
AU Fram, MS
Belitz, K
AF Fram, Miranda S.
Belitz, Kenneth
TI Probability of Detecting Perchlorate under Natural Conditions in Deep
Groundwater in California and the Southwestern United States
SO ENVIRONMENTAL SCIENCE & TECHNOLOGY
LA English
DT Article
ID ISOTOPIC COMPOSITION; HIGH-PLAINS; NEW-MEXICO; NITRATE; DEPOSITION;
ORIGIN; DESERT; USA
AB We use data from 1626 groundwater samples collected in California, primarily from public drinking water supply wells, to investigate the distribution of perchlorate in deep groundwater under natural conditions. The wells were sampled for the California Groundwater Ambient Monitoring and Assessment Priority Basin Project. We develop a logistic regression model for predicting probabilities of detecting perchlorate at concentrations greater than multiple threshold concentrations as a function of climate (represented by an aridity index) and potential anthropogenic contributions of perchlorate (quantified as an anthropogenic score, AS). AS is a composite categorical variable including terms for nitrate, pesticides, and volatile organic compounds. Incorporating water-quality parameters in AS permits identification of perturbation of natural occurrence patterns by flushing of natural perchlorate salts from unsaturated zones by irrigation recharge as well as addition of perchlorate from industrial and agricultural sources. The data and model results indicate low concentrations (0.1-0.5 mu g/L) of perchlorate occur under natural conditions in groundwater across a wide range of climates, beyond the arid to semiarid climates in which they mostly have been previously reported. The probability of detecting perchlorate at concentrations greater than 0.1 mu g/L under natural conditions ranges from 50-70% in semiarid to arid regions of California and the Southwestern United States to 5-15% in the wettest regions sampled (the Northern California coast). The probability of concentrations above 1 mu g/L under natural conditions is low (generally <3%).
C1 [Fram, Miranda S.; Belitz, Kenneth] US Geol Survey, Sacramento, CA 95819 USA.
RP Fram, MS (reprint author), US Geol Survey, 6000 J St,Placer Hall, Sacramento, CA 95819 USA.
EM mfram@usgs.gov
OI Fram, Miranda/0000-0002-6337-059X
FU State bonds
FX We thank the approximately 1500 well owners and water purveyors who
graciously allowed the USGS to collect samples from their wells and
Barbara Dawson, Frank Moseanko, Steve Schmitt, and others who conducted
the field work. This study was funded by State bonds administered by the
California State Water Resources Control Board. This manuscript was
improved following technical reviews by six anonymous reviewers. The use
of brand names in this report is for identification purposes only and
does not imply endorsement by the U.S. Government.
NR 37
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U1 2
U2 12
PU AMER CHEMICAL SOC
PI WASHINGTON
PA 1155 16TH ST, NW, WASHINGTON, DC 20036 USA
SN 0013-936X
J9 ENVIRON SCI TECHNOL
JI Environ. Sci. Technol.
PD FEB 15
PY 2011
VL 45
IS 4
BP 1271
EP 1277
DI 10.1021/es103103p
PG 7
WC Engineering, Environmental; Environmental Sciences
SC Engineering; Environmental Sciences & Ecology
GA 718LI
UT WOS:000287122400018
PM 21247209
ER
PT J
AU Reeves, EP
Seewald, JS
Saccocia, P
Bach, W
Craddock, PR
Shanks, WC
Sylva, SP
Walsh, E
Pichler, T
Rosner, M
AF Reeves, Eoghan P.
Seewald, Jeffrey S.
Saccocia, Peter
Bach, Wolfgang
Craddock, Paul R.
Shanks, Wayne C.
Sylva, Sean P.
Walsh, Emily
Pichler, Thomas
Rosner, Martin
TI Geochemistry of hydrothermal fluids from the PACMANUS, Northeast Pual
and Vienna Woods hydrothermal fields, Manus Basin, Papua New Guinea
SO GEOCHIMICA ET COSMOCHIMICA ACTA
LA English
DT Article
ID BACK-ARC BASIN; DE-FUCA RIDGE; EAST PACIFIC RISE; MID-ATLANTIC RIDGE;
MODERN SEA-FLOOR; SEAWATER-BASALT INTERACTION; VENT FLUIDS;
STABLE-ISOTOPE; PHASE-SEPARATION; CHEMICAL-EXCHANGE
AB Processes controlling the composition of seafloor hydrothermal fluids in silicic back-arc or near-arc crustal settings remain poorly constrained despite growing evidence for extensive magmatic hydrothermal activity in such environments. We conducted a survey of vent fluid compositions from two contrasting sites in the Manus back-arc basin, Papua New Guinea, to examine the influence of variations in host rock composition and magmatic inputs (both a function of arc proximity) on hydrothermal fluid chemistry. Fluid samples were collected from felsic-hosted hydrothermal vent fields located on Pual Ridge (PACMANUS and Northeast (NE) Pual) near the active New Britain Arc and a basalt-hosted vent field (Vienna Woods) located farther from the arc on the Manus Spreading Center. Vienna Woods fluids were characterized by relatively uniform endmember temperatures (273-285 degrees C) and major element compositions, low dissolved CO2 concentrations (4.4 mmol/kg) and high measured pH (4.2-4.9 at 25 degrees C). Temperatures and compositions were highly variable at PACM-ANUS/NE Pual and a large, newly discovered vent area (Fenway) was observed to be vigorously venting boiling (358 degrees C) fluid. All PACMANUS fluids are characterized by negative delta D-H2O values, in contrast to positive values at Vienna Woods, suggesting substantial magmatic water input to circulating fluids at Pual Ridge. Low measured pH (25 degrees C) values (similar to 2.6-2.7), high endmember CO2 (up to 274 mmol/kg) and negative delta S-34(H2S) values (down to -2.7 parts per thousand) in some vent fluids are also consistent with degassing of acid-volatile species from evolved magma. Dissolved CO2 at PACMANUS is more enriched in C-13 (-4.1 parts per thousand to -2.3 parts per thousand) than Vienna Woods (-5.2 parts per thousand to -5.7 parts per thousand), suggesting a contribution of slab-derived carbon. The mobile elements (e.g. Li, K, Rb, Cs and B) are also greatly enriched in PACMANUS fluids reflecting increased abundances in the crust there relative to the Manus Spreading Center. Variations in alkali and dissolved gas abundances with Cl at PACMANUS and NE Pual suggest that phase separation has affected fluid chemistry despite the low temperatures of many vents. In further contrast to Vienna Woods, substantial modification of PACMANUS/NE Pual fluids has taken place as a result of seawater ingress into the upflow zone. Consistently high measured Mg concentrations as well as trends of increasingly non-conservative SO4 behavior, decreasing endmember Ca/Cl and Sr/Cl ratios with increased Mg indicate extensive subsurface anhydrite deposition is occurring as a result of subsurface seawater entrainment. Decreased pH and endmember Fe/Mn ratios in higher Mg fluids indicate that the associated mixing/cooling gives rise to sulfide deposition and secondary acidity production. Several low temperature (<= 80 degrees C) fluids at PACMANUS/NE Pual also show evidence for anhydrite dissolution and water rock interaction (fixation of B) subsequent to seawater entrainment. Hence, the evolution of fluid compositions at Pual Ridge reflects the cumulative effects of water/rock interaction, admixing and reaction of fluids exsolved from silicic magma, phase separation/segregation and seawater ingress into upflow zones. (C) 2010 Elsevier Ltd. All rights reserved.
C1 [Reeves, Eoghan P.; Bach, Wolfgang; Pichler, Thomas; Rosner, Martin] Univ Bremen, Dept Geosci, D-28359 Bremen, Germany.
[Reeves, Eoghan P.; Craddock, Paul R.] MIT WHOI Joint Program Oceanog, Woods Hole, MA 02543 USA.
[Reeves, Eoghan P.; Seewald, Jeffrey S.; Craddock, Paul R.; Sylva, Sean P.] Woods Hole Oceanog Inst, Dept Marine Chem & Geochem, Woods Hole, MA 02543 USA.
[Saccocia, Peter; Walsh, Emily] Bridgewater State Coll, Dept Earth Sci, Bridgewater, MA 02325 USA.
[Shanks, Wayne C.] US Geol Survey, Denver Fed Ctr 973, Denver, CO 80225 USA.
[Rosner, Martin] Free Univ Berlin, Fachbereich Geowissensch, D-12249 Berlin, Germany.
RP Reeves, EP (reprint author), Univ Bremen, Dept Geosci, 2 Klagenfurter Str, D-28359 Bremen, Germany.
EM ereeves@whoi.edu
RI Rosner, Martin/B-9264-2009; Sylva, Sean/D-4400-2014; Reeves,
Eoghan/M-3542-2013; Bach, Wolfgang/D-3713-2017;
OI Sylva, Sean/0000-0002-4727-440X; Reeves, Eoghan/0000-0003-0146-0714;
Bach, Wolfgang/0000-0002-3099-7142; Craddock, Paul/0000-0003-4702-0204
FU NSF [OCE-0327448]; WHOI Deep Ocean Exploration Institute; Ocean Drilling
Program Schlanger Fellowship
FX The authors are grateful to the crew of the R/V Melville and ROV Jason
II technical group for their expertise and assistance in completion of a
very successful dive program. We would also like to thank Maurice Tivey
and the Autonomous Benthic Explorer (ABE) technical group for providing
SM2000 bathymetric maps for our manuscript prior to publication. This
manuscript benefited greatly from numerous invaluable discussions with
Margaret K. Tivey. We would like to acknowledge helpful reviews by
Joseph Resing and two other anonymous reviewers, which greatly improved
the presentation and discussion of our research, in addition to helpful
comments from the Associate Editor, J.-I. Ishibashi. This study received
financial support from NSF Grant OCE-0327448, the WHOI Deep Ocean
Exploration Institute Graduate Fellowship (to E.P. Reeves) and the Ocean
Drilling Program Schlanger Fellowship (to P.R. Craddock).
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PI OXFORD
PA THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND
SN 0016-7037
EI 1872-9533
J9 GEOCHIM COSMOCHIM AC
JI Geochim. Cosmochim. Acta
PD FEB 15
PY 2011
VL 75
IS 4
BP 1088
EP 1123
DI 10.1016/j.gca.2010.11.008
PG 36
WC Geochemistry & Geophysics
SC Geochemistry & Geophysics
GA 716HT
UT WOS:000286960400009
ER
PT J
AU Lu, N
Kaya, BS
Godt, JW
AF Lu, Ning
Kaya, Basak Sener
Godt, Jonathan W.
TI Direction of unsaturated flow in a homogeneous and isotropic hillslope
SO WATER RESOURCES RESEARCH
LA English
DT Article
ID DRIVEN GROUNDWATER-FLOW; HYDRAULIC CONDUCTIVITY; SURFACE HYDROLOGY;
LATERAL FLOW; WATER-FLOW; SOIL; INFILTRATION; SLOPE; MOISTURE; STEEP
AB The distribution of soil moisture in a homogeneous and isotropic hillslope is a transient, variably saturated physical process controlled by rainfall characteristics, hillslope geometry, and the hydrological properties of the hillslope materials. The major driving mechanisms for moisture movement are gravity and gradients in matric potential. The latter is solely controlled by gradients of moisture content. In a homogeneous and isotropic saturated hillslope, absent a gradient in moisture content and under the driving force of gravity with a constant pressure boundary at the slope surface, flow is always in the lateral downslope direction, under either transient or steady state conditions. However, under variably saturated conditions, both gravity and moisture content gradients drive fluid motion, leading to complex flow patterns. In general, the flow field near the ground surface is variably saturated and transient, and the direction of flow could be laterally downslope, laterally upslope, or vertically downward. Previous work has suggested that prevailing rainfall conditions are sufficient to completely control these flow regimes. This work, however, shows that under time-varying rainfall conditions, vertical, downslope, and upslope lateral flow can concurrently occur at different depths and locations within the hillslope. More importantly, we show that the state of wetting or drying in a hillslope defines the temporal and spatial regimes of flow and when and where laterally downslope and/or laterally upslope flow occurs.
C1 [Lu, Ning; Kaya, Basak Sener] Colorado Sch Mines, Div Engn, Golden, CO 80401 USA.
[Godt, Jonathan W.] US Geol Survey, Lakewood, CO 80225 USA.
RP Lu, N (reprint author), Colorado Sch Mines, Div Engn, Golden, CO 80401 USA.
EM ninglu@mines.edu
FU National Science Foundation (NSF) [CMMI-0855783]; U.S. Geological Survey
(USGS) [G09AC00085]
FX The authors would like to thank Mark Reid, Brian Collins, the Associate
Editor Tetsu Tokunaga, four anonymous referees, and Charles Jackson for
their constructive comments. This research is partially supported by a
grant from the National Science Foundation (NSF CMMI-0855783) to N.L.
and J.W.G. and a grant from the U.S. Geological Survey (USGS G09AC00085)
to N.L.
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U2 15
PU AMER GEOPHYSICAL UNION
PI WASHINGTON
PA 2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA
SN 0043-1397
J9 WATER RESOUR RES
JI Water Resour. Res.
PD FEB 15
PY 2011
VL 47
AR W02519
DI 10.1029/2010WR010003
PG 15
WC Environmental Sciences; Limnology; Water Resources
SC Environmental Sciences & Ecology; Marine & Freshwater Biology; Water
Resources
GA 723VB
UT WOS:000287534300003
ER
PT J
AU Warrick, JA
Stevens, AW
AF Warrick, Jonathan A.
Stevens, Andrew W.
TI A buoyant plume adjacent to a headland-Observations of the Elwha River
plume
SO CONTINENTAL SHELF RESEARCH
LA English
DT Article
DE River plume; Coastal headland; Strait of Juan de Fuca; Elwha River; Dam
removal
ID COASTAL DISCHARGES; SEDIMENT; FRONT; CALIFORNIA; TRANSPORT; CURRENTS;
OCEAN; VARIABILITY; WASHINGTON; ECOSYSTEM
AB Small rivers commonly discharge into coastal settings with topographic complexities - such as headlands and islands - but these settings are underrepresented in river plume studies compared to more simplified, straight coasts. The Elwha River provides a unique opportunity to study the effects of coastal topography on a buoyant plume, because it discharges into the Strait of Juan de Fuca on the western side of its deltaic headland. Here we show that this headland induces flow separation and transient eddies in the tidally dominated currents (O(100 cm/s)), consistent with other headlands in oscillatory flow. These flow conditions are observed to strongly influence the buoyant river plume, as predicted by the "small-scale" or "narrow" dynamical classification using Garvine's (1995) system. Because of the transient eddies and the location of the river mouth on the headland, flow immediately offshore of the river mouth is directed eastward twice as frequently as it is westward. This results in a buoyant plume that is much more frequently "bent over" toward the east than the west. During bent over plume conditions, the plume was attached to the eastern shoreline while having a distinct, cuspate front along its westernmost boundary. The location of the front was found to be related to the magnitude and direction of local flow during the preceding O(1 h), and increases in alongshore flow resulted in deeper freshwater mixing, stronger baroclinic anomalies, and stronger hugging of the coast. During bent over plume conditions, we observed significant convergence of river plume water toward the frontal boundary within 1 km of the river mouth. These results show how coastal topography can strongly influence buoyant plume behavior, and they should assist with understanding of initial coastal sediment dispersal pathways from the Elwha River during a pending dam removal project. Published by Elsevier Ltd.
C1 [Warrick, Jonathan A.; Stevens, Andrew W.] US Geol Survey, Pacific Coastal & Marine Sci Ctr, Santa Cruz, CA 95062 USA.
RP Warrick, JA (reprint author), US Geol Survey, Pacific Coastal & Marine Sci Ctr, 400 Nat Bridges Dr, Santa Cruz, CA 95062 USA.
EM jwarrick@usgs.gov
FU USGS
FX We would like to thank Joanne Ferreira, Jamie Grover, Gerry Hatcher, Guy
Gelfenbaum, Hal Williams, Dave Gonzales, and Chris Curran for their
assistance with instrumentation and field activities. This paper was
improved substantially by comments from Amy Draut, Jessica Lacy and two
anonymous reviewers. This work was funded by the Coastal Habitats in
Puget Sound (CHIPS) project within the Coastal and Marine Geology
Program of the USGS.
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PI OXFORD
PA THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND
SN 0278-4343
J9 CONT SHELF RES
JI Cont. Shelf Res.
PD FEB 15
PY 2011
VL 31
IS 2
BP 85
EP 97
DI 10.1016/j.csr.2010.11.007
PG 13
WC Oceanography
SC Oceanography
GA 717QZ
UT WOS:000287063800001
ER
PT J
AU McGillis, WR
Langdon, C
Loose, B
Yates, KK
Corredor, J
AF McGillis, W. R.
Langdon, C.
Loose, B.
Yates, K. K.
Corredor, Jorge
TI Productivity of a coral reef using boundary layer and enclosure methods
SO GEOPHYSICAL RESEARCH LETTERS
LA English
DT Article
ID EDDY-CORRELATION TECHNIQUE; COMMUNITY METABOLISM; CARBON FLUXES; FLOW;
DYNAMICS; CALCIFICATION; ECOSYSTEM; FLAT; PH
AB The metabolism of Cayo Enrique Reef, Puerto Rico, was studied using in situ methods during March 2009. Benthic O-2 fluxes were used to calculate net community production using both the boundary layer gradient and enclosure techniques. The boundary layer O-2 gradient and the drag coefficients were used to calculate productivity ranging from -12.3 to 13.7 mmol O-2 m(-2) h(-1). Productivity measurements from the enclosure method ranged from -11.0 to 12.9 mmol O-2 m(-2) h(-1). During the study, the mean hourly difference between the methods was 0.65 mmol O-2 m(-2) h(-1) (r(2) = 0.92), resulting in well-reconciled estimates of net community production between the boundary layer (-33.1 mmol m(-2) d(-1)) and enclosure (-46.3 mmol m(-2) d(-1)) techniques. The results of these independent approaches corroborate quantified rates of metabolism at Cayo Enrique Reef. Close agreement between methods demonstrates that boundary layer measurements can provide near real-time assessments of coral reef health. Citation: McGillis, W. R., C. Langdon, B. Loose, K. K. Yates, and J. Corredor (2011), Productivity of a coral reef using boundary layer and enclosure methods, Geophys. Res. Lett., 38, L03611, doi:10.1029/2010GL046179.
C1 [McGillis, W. R.] Columbia Univ, Earth Inst, Lamont Doherty Earth Observ, Palisades, NY 10964 USA.
[Langdon, C.] Univ Miami, Rosenstiel Sch Marine & Atmospher Sci, Miami, FL 33149 USA.
[Loose, B.] Woods Hole Oceanog Inst, Woods Hole, MA 02543 USA.
[Yates, K. K.] US Geol Survey, St Petersburg, FL 33701 USA.
[Corredor, Jorge] Univ Puerto Rico, Dept Marine Sci, Mayaguez, PR 00681 USA.
RP McGillis, WR (reprint author), Columbia Univ, Earth Inst, Lamont Doherty Earth Observ, 61 Rte 9W, Palisades, NY 10964 USA.
EM wrm2102@columbia.edu
FU NOAA; University of Puerto Rico Marine Laboratory
FX The authors are grateful to the NOAA CORAL REEF Watch Program and the
University of Puerto Rico Marine Laboratory. We would like to thank Jon
Ware (WHOI) for the fabrication of CROSS. We would also like to extend
our gratitude to Luis Soler-Lopez and Pedro Diaz of the USGS in San
Juan, Puerto Rico; Nathan Smiley and Chris Dufore of the USGS in St.
Petersburg, Florida; and John MacAllister, Carol MacAllister, and Ismael
Ramos-Soler for their support and assistance with field deployments and
logistics.
NR 30
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PU AMER GEOPHYSICAL UNION
PI WASHINGTON
PA 2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA
SN 0094-8276
EI 1944-8007
J9 GEOPHYS RES LETT
JI Geophys. Res. Lett.
PD FEB 15
PY 2011
VL 38
AR L03611
DI 10.1029/2010GL046179
PG 5
WC Geosciences, Multidisciplinary
SC Geology
GA 723QI
UT WOS:000287521500001
ER
PT J
AU Merten, EC
Finlay, J
Johnson, L
Newman, R
Stefan, H
Vondracek, B
AF Merten, Eric Christopher
Finlay, Jacques
Johnson, Lucinda
Newman, Raymond
Stefan, Heinz
Vondracek, Bruce
TI Environmental controls of wood entrapment in upper Midwestern streams
SO HYDROLOGICAL PROCESSES
LA English
DT Article
DE wood movement; wood entrapment; wood transport
ID FISH HABITAT; FLUME EXPERIMENT; MOUNTAIN STREAM; LAKE-SUPERIOR; DEBRIS;
DYNAMICS; RIVER; TRANSPORT; WASHINGTON; STORAGE
AB Wood deposited in streams provides a wide variety of ecosystem functions, including enhancing habitat for key species in stream food webs, increasing geomorphic and hydraulic heterogeneity and retaining organic matter. Given the strong role that wood plays in streams, factors that influence wood inputs, retention and transport are critical to stream ecology. Wood entrapment, the process of wood coming to rest after being swept downstream at least 10 m, is poorly understood, yet important for predicting stream function and success of restoration efforts. Data on entrapment were collected for a wide range of natural wood pieces (n = 344), stream geomorphology and hydraulic conditions in nine streams along the north shore of Lake Superior in Minnesota. Locations of pieces were determined in summer 2007 and again following an overbank stormflow event in fall 2007. The ratio of piece length to effective stream width (length ratio) and the weight of the piece were important in a multiple logistic regression model that explained 25% of the variance in wood entrapment. Entrapment remains difficult to predict in natural streams, and often may simply occur wherever wood pieces are located when high water recedes. However, this study can inform stream modifications to discourage entrapment at road crossings or other infrastructure by applying the model formula to estimate the effective width required to pass particular wood pieces. Conversely, these results could also be used to determine conditions (e. g. pre-existing large, stable pieces) that encourage entrapment where wood is valued for ecological functions. Copyright (C) 2010 John Wiley & Sons, Ltd.
C1 [Merten, Eric Christopher; Newman, Raymond] Univ Minnesota, Dept Fisheries Wildlife & Conservat Biol, St Paul, MN 55108 USA.
[Stefan, Heinz] Univ Minnesota, Dept Civil Engn, Minneapolis, MN 55455 USA.
[Johnson, Lucinda] Univ Minnesota, Nat Resources Res Inst, Duluth, MN 55811 USA.
[Finlay, Jacques] Univ Minnesota, Dept Ecol Evolut & Behav, St Paul, MN 55108 USA.
[Vondracek, Bruce] Univ Minnesota, Minnesota Cooperat Fish & Wildlife Res Unit, US Geol Survey, St Paul, MN 55108 USA.
RP Merten, EC (reprint author), Univ Minnesota, Dept Fisheries Wildlife & Conservat Biol, 1980 Folwell Ave, St Paul, MN 55108 USA.
EM mert0042@umn.edu
RI Finlay, Jacques/B-6081-2011
OI Finlay, Jacques/0000-0002-7968-7030
FU Minnesota Department of Natural Resources; Minnesota Sea Grant; US
Geological Survey; University of Minnesota; Wildlife Management
Institute; US Fish and Wildlife Service
FX Wood and survey data were collected by Jo Fritz, Ryan Carlson, Dustin
Wilman, Nicole Rath, Levi Drevlow, Ryan Johnsen and April Bebault.
Rachael Stanze and Nathan Schroeder collected continuous discharge data
from six streams. Logistical support was provided by Tracy Close of
Minnesota Department of Natural Resources, Marty Rye of USDA Forest
Service, the Minnesota Cooperative Fish and Wildlife Research Unit and
the Natural Resources Research Institute. Mention of trade names or
commercial products does not imply endorsement by the US Government.
Funding was provided by the Minnesota Department of Natural Resources
and Minnesota Sea Grant. The Minnesota Cooperative Fish and Wildlife
Research Unit is jointly sponsored by the US Geological Survey, the
University of Minnesota, the Minnesota Department of Natural Resources,
the Wildlife Management Institute and the US Fish and Wildlife Service.
NR 44
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U2 11
PU WILEY-BLACKWELL
PI MALDEN
PA COMMERCE PLACE, 350 MAIN ST, MALDEN 02148, MA USA
SN 0885-6087
J9 HYDROL PROCESS
JI Hydrol. Process.
PD FEB 15
PY 2011
VL 25
IS 4
BP 593
EP 602
DI 10.1002/hyp.7846
PG 10
WC Water Resources
SC Water Resources
GA 721TD
UT WOS:000287377200006
ER
PT J
AU Wulder, MA
White, JC
Masek, JG
Dwyer, J
Roy, DP
AF Wulder, Michael A.
White, Joanne C.
Masek, Jeffrey G.
Dwyer, John
Roy, David P.
TI Continuity of Landsat observations: Short term considerations
SO REMOTE SENSING OF ENVIRONMENT
LA English
DT Article
DE Landsat; Monitoring; Operational; Research; Continuity; Global; Land
cover; Change detection
ID SPATIAL-RESOLUTION; SATELLITE DATA; FOREST COVER; MODIS; IMAGERY; TM;
CLASSIFICATION; REFLECTANCE; FUSION; PERFORMANCE
AB As of writing in mid-2010, both Landsat-5 and -7 continue to function, with sufficient fuel to enable data collection until the launch of the Landsat Data Continuity Mission (LDCM) scheduled for December of 2012. Failure of one or both of Landsat-5 or -7 may result in a lack of Landsat data for a period of time until the 2012 launch. Although the potential risk of a component failure increases the longer the sensor's design life is exceeded, the possible gap in Landsat data acquisition is reduced with each passing day and the risk of Landsat imagery being unavailable diminishes for all except a handful of applications that are particularly data demanding. Advances in Landsat data compositing and fusion are providing opportunities to address issues associated with Landsat-7 SLC-off imagery and to mitigate a potential acquisition gap through the integration of imagery from different sensors. The latter will likely also provide short-term, regional solutions to application-specific needs for the continuity of Landsat-like observations. Our goal in this communication is not to minimize the community's concerns regarding a gap in Landsat observations, but rather to clarify how the current situation has evolved and provide an up-to-date understanding of the circumstances, implications, and mitigation options related to a potential gap in the Landsat data record. Crown Copyright (C) 2010 Published by Elsevier Inc. All rights reserved.
C1 [Wulder, Michael A.; White, Joanne C.] Nat Resources Canada, Pacific Forestry Ctr, Canadian Forest Serv, Victoria, BC V8Z 1M5, Canada.
[Masek, Jeffrey G.] NASA, Goddard Space Flight Ctr, Biospher Sci Branch, Greenbelt, MD 20771 USA.
[Dwyer, John] US Geol Survey, Ctr Earth Resources Observat & Sci EROS, Sioux Falls, SD 57198 USA.
[Roy, David P.] S Dakota State Univ, Geog Informat Sci Ctr Excellence, Brookings, SD 57007 USA.
RP Wulder, MA (reprint author), Nat Resources Canada, Pacific Forestry Ctr, Canadian Forest Serv, Victoria, BC V8Z 1M5, Canada.
EM mwulder@nrcan.gc.ca
RI Masek, Jeffrey/D-7673-2012; Wulder, Michael/J-5597-2016;
OI Wulder, Michael/0000-0002-6942-1896; Dwyer, John/0000-0002-8281-0896;
White, Joanne/0000-0003-4674-0373
FU USGS; NASA
FX We gratefully acknowledge USGS and NASA leadership and support of the
Landsat Science Team.
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PU ELSEVIER SCIENCE INC
PI NEW YORK
PA 360 PARK AVE SOUTH, NEW YORK, NY 10010-1710 USA
SN 0034-4257
J9 REMOTE SENS ENVIRON
JI Remote Sens. Environ.
PD FEB 15
PY 2011
VL 115
IS 2
BP 747
EP 751
DI 10.1016/j.rse.2010.11.002
PG 5
WC Environmental Sciences; Remote Sensing; Imaging Science & Photographic
Technology
SC Environmental Sciences & Ecology; Remote Sensing; Imaging Science &
Photographic Technology
GA 714BS
UT WOS:000286782500041
ER
PT J
AU Liu, D
Dong, HL
Bishop, ME
Wang, HM
Agrawal, A
Tritschler, S
Eberl, DD
Xie, SC
AF Liu, Deng
Dong, Hailiang
Bishop, Michael E.
Wang, Hongmei
Agrawal, Abinash
Tritschler, Sarah
Eberl, Dennis D.
Xie, Shucheng
TI Reduction of structural Fe(III) in nontronite by methanogen
Methanosarcina barkeri
SO GEOCHIMICA ET COSMOCHIMICA ACTA
LA English
DT Article
ID EXTRACELLULAR ELECTRON-TRANSFER; MICROBIAL REDUCTION; HUMIC SUBSTANCES;
ILLITE REACTION; FERRIC IRON; QUANTITATIVE ASSAY; SMECTITE;
MICROORGANISMS; COMPETITION; INHIBITION
AB Clay minerals and methanogens are ubiquitous and co-exist in anoxic environments, yet it is unclear whether methanogens are able to reduce structural Fe(III) in clay minerals. In this study, the ability of methanogen Methanosarcina barkeri to reduce structural Fe(III) in iron-rich smectite (nontronite NAu-2) and the relationship between iron reduction and methanogenesis were investigated. Bioreduction experiments were conducted in growth medium using three types of substrate: H(2)/CO(2), methanol, and acetate. Time course methane production and hydrogen consumption were measured by gas chromatography. M. barkeri was able to reduce structural Fe(III) in NAu-2 with H(2)/CO(2) and methanol as substrate, but not with acetate. The extent of bioreduction, as measured by the 1,10-phenanthroline method, was 7-13% with H(2)/CO(2) as substrate, depending on nontronite concentration (5-10 g/L). The extent was higher when methanol was used as a substrate, reaching 25-33%. Methanogenesis was inhibited by Fe(III) reduction in the H(2)/CO(2) culture, but enhanced when methanol was used. High charge smectite and biogenic silica formed as a result of bioreduction. Our results suggest that methanogens may play an important role in biogeochemical cycling of iron in clay minerals and may have important implications for the global methane budget. (C) 2010 Elsevier Ltd. All rights reserved.
C1 [Liu, Deng; Dong, Hailiang; Wang, Hongmei; Xie, Shucheng] China Univ Geosci, Key Lab Biogeol & Environm Geol, Minist Educ, Wuhan 430074, Peoples R China.
[Dong, Hailiang] China Univ Geosci, Geomicrobiol Lab, State Key Lab Geol Proc & Mineral Resources, Beijing 100083, Peoples R China.
[Dong, Hailiang; Bishop, Michael E.] Miami Univ, Dept Geol, Oxford, OH 45056 USA.
[Agrawal, Abinash; Tritschler, Sarah] Wright State Univ, Dept Earth & Environm Sci, Dayton, OH 45435 USA.
[Eberl, Dennis D.] US Geol Survey, Boulder, CO 80303 USA.
[Xie, Shucheng] China Univ Geosci, State Key Lab Geol Proc & Mineral Resources, Wuhan 430074, Peoples R China.
RP Dong, HL (reprint author), China Univ Geosci, Key Lab Biogeol & Environm Geol, Minist Educ, Wuhan 430074, Peoples R China.
EM dongh@cug.edu.cn; wanghmei4@163.com
RI Xie, Shucheng/E-6713-2011; Agrawal, Abinash/B-8048-2013
FU National Basic Research Program of China [2011CB808800]; National
Science Foundation of China [41030211]; US Department of Energy
[DE-FG02-07ER64369]; US Department of Defense Strategic Environmental
Research and Development Program (SER-DP) [ER-1685]; 111 Project
[B07011, B08030]; CUG-Wuhan; Key Laboratory of Biogeology and
Environmental Geology of Ministry of Education [BGEGF200819]
FX We are grateful to Prof. Joseph A. Krzycki for providing the strain of
M. barkeri DSM800, Dr. John Morton for assisting the XRD and DCP
spectrometry analyses, and Charles A. Cravotta Ill for his help on
Phreeqc modeling. This work was supported by grants from the National
Basic Research Program of China (Grant No. 2011CB808800), National
Science Foundation of China (41030211), the US Department of Energy
(DE-FG02-07ER64369), the US Department of Defense Strategic
Environmental Research and Development Program (SER-DP) (ER-1685), the
111 Project (B07011 and B08030), Dong's startup funds from CUG-Wuhan,
and a grant from Key Laboratory of Biogeology and Environmental Geology
of Ministry of Education (BGEGF200819) to Deng Liu. We are grateful to
associate editor, Dr. Robert H. Byrne, and three anonymous reviewers
whose comments greatly improved the quality of this manuscript.
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PI OXFORD
PA THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND
SN 0016-7037
J9 GEOCHIM COSMOCHIM AC
JI Geochim. Cosmochim. Acta
PD FEB 15
PY 2011
VL 75
IS 4
BP 1057
EP 1071
DI 10.1016/j.gca.2010.11.009
PG 15
WC Geochemistry & Geophysics
SC Geochemistry & Geophysics
GA 716HT
UT WOS:000286960400007
ER
PT J
AU Slone, DH
AF Slone, D. H.
TI Increasing accuracy of dispersal kernels in grid-based population models
SO ECOLOGICAL MODELLING
LA English
DT Article
DE Map lattice; Spatial model; Invasion model; Numerical simulation;
Redistribution
ID INVADING ORGANISMS; LANDSCAPE; CONSERVATION; SPREAD; RESTORATION;
COEXISTENCE; EVERGLADES; MECHANISMS; INVASION; SPEED
AB Dispersal kernels in grid-based population models specify the proportion, distance and direction of movements within the model landscape. Spatial errors in dispersal kernels can have large compounding effects on model accuracy. Circular Gaussian and Laplacian dispersal kernels at a range of spatial resolutions were investigated, and methods for minimizing errors caused by the discretizing process were explored. Kernels of progressively smaller sizes relative to the landscape grid size were calculated using cell-integration and cell-center methods. These kernels were convolved repeatedly, and the final distribution was compared with a reference analytical solution. For large Gaussian kernels (sigma>10 cells), the total kernel error was <10(-11) compared to analytical results. Using an invasion model that tracked the time a population took to reach a defined goal, the discrete model results were comparable to the analytical reference. With Gaussian kernels that had sigma <= 0.12 using the cell integration method, or sigma <= 0.22 using the cell center method, the kernel error was greater than 10%, which resulted in invasion times that were orders of magnitude different than theoretical results. A goal-seeking routine was developed to adjust the kernels to minimize overall error. With this, corrections for small kernels were found that decreased overall kernel error to <10(-11) and invasion time error to <5%. Published by Elsevier B.V.
C1 USGS SE Ecol Sci Ctr, Gainesville, FL 32605 USA.
RP Slone, DH (reprint author), USGS SE Ecol Sci Ctr, 2201 NW 40th Terrace, Gainesville, FL 32605 USA.
EM dslone@usgs.gov
OI Slone, Daniel/0000-0002-9903-9727
NR 31
TC 9
Z9 9
U1 1
U2 17
PU ELSEVIER SCIENCE BV
PI AMSTERDAM
PA PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS
SN 0304-3800
J9 ECOL MODEL
JI Ecol. Model.
PD FEB 10
PY 2011
VL 222
IS 3
BP 573
EP 579
DI 10.1016/j.ecolmodel.2010.11.023
PG 7
WC Ecology
SC Environmental Sciences & Ecology
GA 714BP
UT WOS:000286782200020
ER
PT J
AU Piazza, BP
La Peyre, MK
AF Piazza, Bryan P.
La Peyre, Megan K.
TI Nekton community response to a large-scale Mississippi River discharge:
Examining spatial and temporal response to river management
SO ESTUARINE COASTAL AND SHELF SCIENCE
LA English
DT Article
DE freshwater diversion; nekton community assemblage; nekton indicators;
Louisiana
ID FRESH-WATER FLOW; SAN-FRANCISCO ESTUARY; BRETON SOUND; DELTAIC ESTUARY;
SOUTHERN-OSCILLATION; FISH ASSEMBLAGE; CLIMATE-CHANGE; HABITAT CHANGE;
LOUISIANA; USA
AB Freshwater flow is generally held to be one of the most influential factors affecting community structure and production in estuaries. In coastal Louisiana, the Caernarvon Freshwater Diversion (CFD) is managed to control freshwater discharge from the Mississippi River into Breton Sound basin. Operational since 1991, CFD has undergone several changes in management strategy including pulsed spring flooding, which was introduced in 2001. We used a 20-yr time series of fisheries-independent data to investigate how variation in freshwater inflow (i.e., pre- and post-CFD, and pre and post spring pulsing management) influences the downstream nekton community (abundance, diversity, and assemblage). Analyses of long-term data demonstrated that while there were effects from the CFD, they largely involved subtle changes in community structure. Spatially, effects were largely limited to the sites immediately downstream of the diversion and extended only occasionally to more down-estuary sites. Temporally, effects were 1) immediate (detected during spring diversion events) or 2) delayed (detected several months post-diversion). Analysis of river management found that pulsed spring-time inflow resulted in more significant changes in nekton assemblages, likely due to higher discharge rates that 1) increased marsh flooding, thus increasing marsh habitat accessibility for small resident marsh species, and 2) reduced salinity, possibly causing displacement of marine pelagic species down estuary. Published by Elsevier Ltd.
C1 [La Peyre, Megan K.] Louisiana State Univ, Sch Renewable Nat Resources, Louisiana Fish & Wildlife Cooperat Res Unit, US Geol Survey,AgCtr, Baton Rouge, LA 70803 USA.
[Piazza, Bryan P.] Louisiana State Univ, Sch Renewable Nat Resources, AgCtr, Baton Rouge, LA 70803 USA.
RP La Peyre, MK (reprint author), Louisiana State Univ, Sch Renewable Nat Resources, Louisiana Fish & Wildlife Cooperat Res Unit, US Geol Survey,AgCtr, Baton Rouge, LA 70803 USA.
EM mlapey@lsu.edu
FU Louisiana Department of Wildlife and Fisheries; U.S. Fish & Wildlife
Service [T-62-R]
FX Thanks to M. Fischer (USGS) who created the map figure and G. Snedden
(USGS) who provided historical Caernarvon discharge data. Thank you to
Sarai Piazza for comments that greatly improved the manuscript. This
work was funded by a grant from the Louisiana Department of Wildlife and
Fisheries and U.S. Fish & Wildlife Service, State Wildlife Grant,
T-62-R. Thanks to Drs Don Baltz and Brian Alford for comments that
significantly improved the manuscript. Any use of trade, product, or
firm names is for descriptive purposes only and does not imply
endorsement by the U.S. Government.
NR 55
TC 10
Z9 10
U1 3
U2 14
PU ACADEMIC PRESS LTD- ELSEVIER SCIENCE LTD
PI LONDON
PA 24-28 OVAL RD, LONDON NW1 7DX, ENGLAND
SN 0272-7714
J9 ESTUAR COAST SHELF S
JI Estuar. Coast. Shelf Sci.
PD FEB 10
PY 2011
VL 91
IS 3
BP 379
EP 387
DI 10.1016/j.ecss.2010.11.001
PG 9
WC Marine & Freshwater Biology; Oceanography
SC Marine & Freshwater Biology; Oceanography
GA 720OR
UT WOS:000287290500005
ER
PT J
AU Apotsos, A
Gelfenbaum, G
Jaffe, B
AF Apotsos, Alex
Gelfenbaum, Guy
Jaffe, Bruce
TI Process-based modeling of tsunami inundation and sediment transport
SO JOURNAL OF GEOPHYSICAL RESEARCH-EARTH SURFACE
LA English
DT Article
ID INDIAN-OCEAN-TSUNAMI; 26 DECEMBER 2004; BANDA ACEH SUMATRA; RUN-UP;
UNIFIED VIEW; FIELD SURVEY; SWASH ZONE; SRI-LANKA; NONCOHESIVE SEDIMENT;
SUSPENDED SEDIMENT
AB The infrequent and unpredictable nature of tsunamis precludes the use of field experiments to measure the hydrodynamic and sediment transport processes that occur. Instead, these processes are often approximated from laboratory, numerical, and theoretical studies or inferred from observations of the resultant sediment deposits. Here Delft3D, a three-dimensional numerical model, is used to simulate the inundation and sediment transport of a tsunami similar in magnitude to the 26 December 2004 Indian Ocean tsunami over one measured and three idealized morphologies. The model is first shown to match well the observations taken at Kuala Meurisi, Sumatra, and then used to examine in detail the processes that occur during the tsunami. The model predicts that at a given cross-shore location the onshore flow accelerates rapidly to a maximum as the wavefront passes, and then gradually decelerates before reversing direction and flowing offshore. The onshore flow does not tend to zero everywhere at maximum inundation, but instead flow reversal occurs near the shoreline even as the wavefront continues to inundate landward. While some sediment is eroded by the passing wavefront, the suspension of sandy sediment is dominated by the long-duration, high-velocity backwash that occurs along the beach face and offshore of the shoreline. Some of the sediment suspended during backwash is advected shoreward by the subsequent wave, creating large spatial gradients in the suspended sediment concentrations, which may not be in equilibrium with the local hydrodynamics. The inundation and transport of sediment during a tsunami can be affected by complexities in the morphological profile and interactions between multiple waves, and many of the hydrodynamic and sediment transport processes predicted here are similar to analogous processes previously observed in the swash zone.
C1 [Apotsos, Alex; Gelfenbaum, Guy] USGS, Coastal & Marine Geol Program, Menlo Pk, CA 94025 USA.
[Jaffe, Bruce] USGS, Pacific Sci Ctr, Santa Cruz, CA 95060 USA.
RP Apotsos, A (reprint author), USGS, Coastal & Marine Geol Program, 345 Middlefield Rd,MS 999, Menlo Pk, CA 94025 USA.
EM aapotsos@usgs.gov
RI Jaffe, Bruce/A-9979-2012
OI Jaffe, Bruce/0000-0002-8816-5920
FU USGS
FX This research was funded by a USGS Mendenhall Postdoctoral Fellowship
and the USGS Coastal and Marine Geology Program. Edwin Elias is thanked
for his help and guidance concerning the details of the numerical model.
Deepak Vatvani is thanked for providing the offshore water level time
series. Peter Ruggiero is thanked for helping collect the bathymetry at
Kuala Meurisi. Critical reviews from Britt Raubenheimer and Mark
Buckley, as well as three anonymous reviewers, significantly improved
this manuscript.
NR 83
TC 17
Z9 18
U1 0
U2 10
PU AMER GEOPHYSICAL UNION
PI WASHINGTON
PA 2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA
SN 2169-9003
EI 2169-9011
J9 J GEOPHYS RES-EARTH
JI J. Geophys. Res.-Earth Surf.
PD FEB 10
PY 2011
VL 116
AR F01006
DI 10.1029/2010JF001797
PG 20
WC Geosciences, Multidisciplinary
SC Geology
GA 721AI
UT WOS:000287323400002
ER
PT J
AU Carr, M
AF Carr, Michael
TI Geographies of Mars: Seeing and Knowing the Red Planet
SO NATURE
LA English
DT Book Review
C1 [Carr, Michael] US Geol Survey, Menlo Pk, CA 94025 USA.
RP Carr, M (reprint author), US Geol Survey, 345 Middlefield Rd, Menlo Pk, CA 94025 USA.
EM carr@usgs.gov
NR 1
TC 0
Z9 0
U1 0
U2 3
PU NATURE PUBLISHING GROUP
PI LONDON
PA MACMILLAN BUILDING, 4 CRINAN ST, LONDON N1 9XW, ENGLAND
SN 0028-0836
J9 NATURE
JI Nature
PD FEB 10
PY 2011
VL 470
IS 7333
BP 172
EP 173
DI 10.1038/470172a
PG 2
WC Multidisciplinary Sciences
SC Science & Technology - Other Topics
GA 718RQ
UT WOS:000287144200020
ER
PT J
AU Rodda, GH
Jarnevich, CS
Reed, RN
AF Rodda, Gordon H.
Jarnevich, Catherine S.
Reed, Robert N.
TI Challenges in Identifying Sites Climatically Matched to the Native
Ranges of Animal Invaders
SO PLOS ONE
LA English
DT Article
ID FUTURE BIOLOGICAL INVASIONS; SAMPLE SELECTION BIAS; PSEUDO-ABSENCE DATA;
SPECIES DISTRIBUTIONS; DISTRIBUTION MODELS; GEOGRAPHIC DISTRIBUTIONS;
SPATIAL AUTOCORRELATION; POTENTIAL DISTRIBUTION; CLIMATE-CHANGE; NICHE
SHIFT
AB Background: Species distribution models are often used to characterize a species' native range climate, so as to identify sites elsewhere in the world that may be climatically similar and therefore at risk of invasion by the species. This endeavor provoked intense public controversy over recent attempts to model areas at risk of invasion by the Indian Python (Python molurus). We evaluated a number of MaxEnt models on this species to assess MaxEnt's utility for vertebrate climate matching.
Methodology/Principal Findings: Overall, we found MaxEnt models to be very sensitive to modeling choices and selection of input localities and background regions. As used, MaxEnt invoked minimal protections against data dredging, multi-collinearity of explanatory axes, and overfitting. As used, MaxEnt endeavored to identify a single ideal climate, whereas different climatic considerations may determine range boundaries in different parts of the native range. MaxEnt was extremely sensitive to both the choice of background locations for the python, and to selection of presence points: inclusion of just four erroneous localities was responsible for Pyron et al.'s conclusion that no additional portions of the U. S. mainland were at risk of python invasion. When used with default settings, MaxEnt overfit the realized climate space, identifying models with about 60 parameters, about five times the number of parameters justifiable when optimized on the basis of Akaike's Information Criterion.
Conclusions/Significance: When used with default settings, MaxEnt may not be an appropriate vehicle for identifying all sites at risk of colonization. Model instability and dearth of protections against overfitting, multi-collinearity, and data dredging may combine with a failure to distinguish fundamental from realized climate envelopes to produce models of limited utility. A priori identification of biologically realistic model structure, combined with computational protections against these statistical problems, may produce more robust models of invasion risk.
C1 [Rodda, Gordon H.; Jarnevich, Catherine S.; Reed, Robert N.] US Geol Survey, Ft Collins Sci Ctr, Ft Collins, CO USA.
RP Rodda, GH (reprint author), US Geol Survey, Ft Collins Sci Ctr, Ft Collins, CO USA.
EM catherine_jarnevich@usgs.gov
FU U.S. government
FX This work was funded the U.S. government. The funders had no role in
study design, data collection and analysis, decision to publish, or
preparation of the manuscript, though the USGS did review the manuscript
to ensure conformance with USGS scientific standards.
NR 68
TC 41
Z9 42
U1 2
U2 30
PU PUBLIC LIBRARY SCIENCE
PI SAN FRANCISCO
PA 185 BERRY ST, STE 1300, SAN FRANCISCO, CA 94107 USA
SN 1932-6203
J9 PLOS ONE
JI PLoS One
PD FEB 9
PY 2011
VL 6
IS 2
AR e14670
DI 10.1371/journal.pone.0014670
PG 18
WC Multidisciplinary Sciences
SC Science & Technology - Other Topics
GA 721NN
UT WOS:000287361700004
PM 21347411
ER
PT J
AU Arvidson, RE
Ashley, JW
Bell, JF
Chojnacki, M
Cohen, J
Economou, TE
Farrand, WH
Fergason, R
Fleischer, I
Geissler, P
Gellert, R
Golombek, MP
Grotzinger, JP
Guinness, EA
Haberle, RM
Herkenhoff, KE
Herman, JA
Iagnemma, KD
Jolliff, BL
Johnson, JR
Klingelhofer, G
Knoll, AH
Knudson, AT
Li, R
McLennan, SM
Mittlefehldt, DW
Morris, RV
Parker, TJ
Rice, MS
Schroder, C
Soderblom, LA
Squyres, SW
Sullivan, RJ
Wolff, MJ
AF Arvidson, R. E.
Ashley, J. W.
Bell, J. F., III
Chojnacki, M.
Cohen, J.
Economou, T. E.
Farrand, W. H.
Fergason, R.
Fleischer, I.
Geissler, P.
Gellert, R.
Golombek, M. P.
Grotzinger, J. P.
Guinness, E. A.
Haberle, R. M.
Herkenhoff, K. E.
Herman, J. A.
Iagnemma, K. D.
Jolliff, B. L.
Johnson, J. R.
Klingelhoefer, G.
Knoll, A. H.
Knudson, A. T.
Li, R.
McLennan, S. M.
Mittlefehldt, D. W.
Morris, R. V.
Parker, T. J.
Rice, M. S.
Schroeder, C.
Soderblom, L. A.
Squyres, S. W.
Sullivan, R. J.
Wolff, M. J.
TI Opportunity Mars Rover mission: Overview and selected results from
Purgatory ripple to traverses to Endeavour crater
SO JOURNAL OF GEOPHYSICAL RESEARCH-PLANETS
LA English
DT Article
ID MERIDIANI-PLANUM; AEOLIAN PROCESSES; BURNS FORMATION; EREBUS CRATER;
LANDING SITE; EXPLORATION; MINERALOGY; CHEMISTRY; APHELION; DEPOSITS
AB Opportunity has been traversing the Meridiani plains since 25 January 2004 (sol 1), acquiring numerous observations of the atmosphere, soils, and rocks. This paper provides an overview of key discoveries between sols 511 and 2300, complementing earlier papers covering results from the initial phases of the mission. Key new results include (1) atmospheric argon measurements that demonstrate the importance of atmospheric transport to and from the winter carbon dioxide polar ice caps; (2) observations showing that aeolian ripples covering the plains were generated by easterly winds during an epoch with enhanced Hadley cell circulation; (3) the discovery and characterization of cobbles and boulders that include iron and stony-iron meteorites and Martian impact ejecta; (4) measurements of wall rock strata within Erebus and Victoria craters that provide compelling evidence of formation by aeolian sand deposition, with local reworking within ephemeral lakes; (5) determination that the stratigraphy exposed in the walls of Victoria and Endurance craters show an enrichment of chlorine and depletion of magnesium and sulfur with increasing depth. This result implies that regional-scale aqueous alteration took place before formation of these craters. Most recently, Opportunity has been traversing toward the ancient Endeavour crater. Orbital data show that clay minerals are exposed on its rim. Hydrated sulfate minerals are exposed in plains rocks adjacent to the rim, unlike the surfaces of plains outcrops observed thus far by Opportunity. With continued mechanical health, Opportunity will reach terrains on and around Endeavour's rim that will be markedly different from anything examined to date.
C1 [Arvidson, R. E.; Guinness, E. A.; Jolliff, B. L.] Washington Univ, Dept Earth & Planetary Sci, St Louis, MO 63130 USA.
[Ashley, J. W.] Arizona State Univ, Sch Earth & Space Explorat, Mars Space Flight Facil, Tempe, AZ 85287 USA.
[Bell, J. F., III; Rice, M. S.; Squyres, S. W.; Sullivan, R. J.] Cornell Univ, Dept Astron, Ithaca, NY 14853 USA.
[Chojnacki, M.] Univ Tennessee, Dept Earth & Planetary Sci, Planetary Geosci Inst, Knoxville, TN 37996 USA.
[Cohen, J.] Honeybee Robot Spacecraft Mech Corp, New York, NY 10001 USA.
[Economou, T. E.] Univ Chicago, Lab Astrophys & Space Res, Enrico Fermi Inst, Chicago, IL 60637 USA.
[Farrand, W. H.; Wolff, M. J.] Space Sci Inst, Boulder, CO 80301 USA.
[Fergason, R.; Geissler, P.; Herkenhoff, K. E.; Johnson, J. R.; Soderblom, L. A.] US Geol Survey, Flagstaff, AZ 86001 USA.
[Fleischer, I.; Klingelhoefer, G.] Johannes Gutenberg Univ Mainz, Inst Anorgan & Analyt Chem, D-55099 Mainz, Germany.
[Gellert, R.] Univ Guelph, Dept Phys, Guelph, ON N1G 2W1, Canada.
[Golombek, M. P.; Herman, J. A.; Parker, T. J.] CALTECH, Jet Prop Lab, Pasadena, CA 91109 USA.
[Haberle, R. M.] NASA, Ames Res Ctr, Moffett Field, CA 94035 USA.
[Iagnemma, K. D.] MIT, Dept Mech Engn, Cambridge, MA 02139 USA.
[Knoll, A. H.] Harvard Univ, Dept Organism & Evolutionary Biol, Cambridge, MA 02138 USA.
[Knudson, A. T.] Planetary Sci Inst, Tucson, AZ 85719 USA.
[Li, R.] Ohio State Univ, Dept Civil & Environm Engn, Columbus, OH 43210 USA.
[McLennan, S. M.] SUNY Stony Brook, Dept Geosci, Stony Brook, NY 11794 USA.
[Schroeder, C.] Univ Tubingen, Ctr Appl Geosci, D-72076 Tubingen, Germany.
[Schroeder, C.] Univ Bayreuth, Dept Hydrol, Bayreuth, Germany.
[Mittlefehldt, D. W.; Morris, R. V.] NASA, Lyndon B Johnson Space Ctr, Houston, TX 77058 USA.
RP Arvidson, RE (reprint author), Washington Univ, Dept Earth & Planetary Sci, St Louis, MO 63130 USA.
EM arvidson@rsmail.wustl.edu
RI Schroder, Christian/B-3870-2009; Chojnacki, Matthew/A-4245-2013;
Johnson, Jeffrey/F-3972-2015
OI Schroder, Christian/0000-0002-7935-6039; Chojnacki,
Matthew/0000-0001-8497-8994;
NR 61
TC 31
Z9 31
U1 1
U2 29
PU AMER GEOPHYSICAL UNION
PI WASHINGTON
PA 2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA
SN 2169-9097
EI 2169-9100
J9 J GEOPHYS RES-PLANET
JI J. Geophys. Res.-Planets
PD FEB 8
PY 2011
VL 116
AR E00F15
DI 10.1029/2010JE003746
PG 33
WC Geochemistry & Geophysics
SC Geochemistry & Geophysics
GA 721AS
UT WOS:000287324400001
ER
PT J
AU Cheek, LC
Pieters, CM
Boardman, JW
Clark, RN
Combe, JP
Head, JW
Isaacson, PJ
McCord, TB
Moriarty, D
Nettles, JW
Petro, NE
Sunshine, JM
Taylor, LA
AF Cheek, L. C.
Pieters, C. M.
Boardman, J. W.
Clark, R. N.
Combe, J. P.
Head, J. W.
Isaacson, P. J.
McCord, T. B.
Moriarty, D.
Nettles, J. W.
Petro, N. E.
Sunshine, J. M.
Taylor, L. A.
TI Goldschmidt crater and the Moon's north polar region: Results from the
Moon Mineralogy Mapper (M-3)
SO JOURNAL OF GEOPHYSICAL RESEARCH-PLANETS
LA English
DT Article
ID LUNAR MARE VOLCANISM; REFLECTANCE SPECTRA; SURFACE; SPECTROSCOPY;
PROSPECTOR
AB Soils within the impact crater Goldschmidt have been identified as spectrally distinct from the local highland material. High spatial and spectral resolution data from the Moon Mineralogy Mapper (M-3) on the Chandrayaan-1 orbiter are used to examine the character of Goldschmidt crater in detail. Spectral parameters applied to a north polar mosaic of M-3 data are used to discern large-scale compositional trends at the northern high latitudes, and spectra from three widely separated regions are compared to spectra from Goldschmidt. The results highlight the compositional diversity of the lunar nearside, in particular, where feldspathic soils with a low-Ca pyroxene component are pervasive, but exclusively feldspathic regions and small areas of basaltic composition are also observed. Additionally, we find that the relative strengths of the diagnostic OH/H2O absorption feature near 3000 nm are correlated with the mineralogy of the host material. On both global and local scales, the strongest hydrous absorptions occur on the more feldspathic surfaces. Thus, M-3 data suggest that while the feldspathic soils within Goldschmidt crater are enhanced in OH/H2O compared to the relatively mafic nearside polar highlands, their hydration signatures are similar to those observed in the feldspathic highlands on the farside.
C1 [Cheek, L. C.; Pieters, C. M.; Head, J. W.; Isaacson, P. J.; Moriarty, D.; Nettles, J. W.] Brown Univ, Dept Geol Sci, Providence, RI 02912 USA.
[Boardman, J. W.] Analyt Imaging & Geophys LLC, Boulder, CO 80305 USA.
[Clark, R. N.] US Geol Survey, Fed Ctr, Denver, CO 80225 USA.
[Combe, J. P.; McCord, T. B.] Bear Fight Inst, Winthrop, WA 98862 USA.
[Petro, N. E.] NASA, Goddard Space Flight Ctr, Greenbelt, MD 20771 USA.
[Sunshine, J. M.] Univ Maryland, Dept Astron, College Pk, MD 20742 USA.
[Taylor, L. A.] Univ Tennessee, Dept Earth & Planetary Sci, Knoxville, TN 37996 USA.
RP Cheek, LC (reprint author), Brown Univ, Dept Geol Sci, Box 1846, Providence, RI 02912 USA.
EM leah_cheek@brown.edu; boardman@aigllc.com; rclark@usgs.gov;
mccordtb@bearfightinstitute.com; noah.e.petro@mail.nasa.gov;
jess@astro.umd.edu; lataylor@utk.edu
RI Petro, Noah/F-5340-2013
FU NASA [NNM05AB26C]; NASA LSI at Brown University [NNA09DB34A]
FX The authors thank B. Ray Hawke and an anonymous reviewer for helpful
comments that improved that quality and clarity of the manuscript.
Support for this analysis was provided through the NASA Discovery
program. M3 science validation is supported through NASA
contract NNM05AB26C. Partial funding for this analysis has also been
provided through NASA LSI at Brown University under contract NNA09DB34A.
Thanks are extended to James Dickson for assistance in figure
preparation. The M3 team is grateful to ISRO for the
opportunity to fly as a guest instrument on Chandrayaan-1.
NR 44
TC 7
Z9 8
U1 0
U2 1
PU AMER GEOPHYSICAL UNION
PI WASHINGTON
PA 2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA
SN 0148-0227
J9 J GEOPHYS RES-PLANET
JI J. Geophys. Res.-Planets
PD FEB 4
PY 2011
VL 116
AR E00G02
DI 10.1029/2010JE003702
PG 15
WC Geochemistry & Geophysics
SC Geochemistry & Geophysics
GA 717HB
UT WOS:000287033200001
ER
PT J
AU Dawson, PB
Chouet, BA
Power, J
AF Dawson, Phillip B.
Chouet, Bernard A.
Power, John
TI Determining the seismic source mechanism and location for an explosive
eruption with limited observational data: Augustine Volcano, Alaska
SO GEOPHYSICAL RESEARCH LETTERS
LA English
DT Article
ID SIGNALS
AB Waveform inversions of the very-long-period components of the seismic wavefield produced by an explosive eruption that occurred on 11 January, 2006 at Augustine Volcano, Alaska constrain the seismic source location to near sea level beneath the summit of the volcano. The calculated moment tensors indicate the presence of a volumetric source mechanism. Systematic reconstruction of the source mechanism shows the source consists of a sill intersected by either a sub-vertical east-west trending dike or a sub-vertical pipe and a weak single force. The trend of the dike may be controlled by the east-west trending Augustine-Seldovia arch. The data from the network of broadband sensors is limited to fourteen seismic traces, and synthetic modeling confirms the ability of the network to recover the source mechanism. The synthetic modeling also provides a guide to the expected capability of a broadband network to resolve very-long-period source mechanisms, particularly when confronted with limited observational data. Citation: Dawson, P. B., B. A. Chouet, and J. Power (2011), Determining the seismic source mechanism and location for an explosive eruption with limited observational data: Augustine Volcano, Alaska, Geophys. Res. Lett., 38, L03302, doi:10.1029/2010GL045977.
C1 [Dawson, Phillip B.; Chouet, Bernard A.] US Geol Survey, Menlo Pk, CA 94025 USA.
[Power, John] US Geol Survey, Alaska Volcano Observ, Anchorage, AK 99508 USA.
RP Dawson, PB (reprint author), US Geol Survey, 345 Middlefield Rd,MS 910, Menlo Pk, CA 94025 USA.
EM dawson@usgs.gov; chouet@usgs.gov; jpower@usgs.gov
NR 11
TC 10
Z9 10
U1 0
U2 4
PU AMER GEOPHYSICAL UNION
PI WASHINGTON
PA 2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA
SN 0094-8276
J9 GEOPHYS RES LETT
JI Geophys. Res. Lett.
PD FEB 4
PY 2011
VL 38
AR L03302
DI 10.1029/2010GL045977
PG 5
WC Geosciences, Multidisciplinary
SC Geology
GA 717JC
UT WOS:000287038500002
ER
PT J
AU Hansen, CJ
Bourke, M
Bridges, NT
Byrne, S
Colon, C
Diniega, S
Dundas, C
Herkenhoff, K
McEwen, A
Mellon, M
Portyankina, G
Thomas, N
AF Hansen, C. J.
Bourke, M.
Bridges, N. T.
Byrne, S.
Colon, C.
Diniega, S.
Dundas, C.
Herkenhoff, K.
McEwen, A.
Mellon, M.
Portyankina, G.
Thomas, N.
TI Seasonal Erosion and Restoration of Mars' Northern Polar Dunes
SO SCIENCE
LA English
DT Article
ID SUBLIMATION-DRIVEN ACTIVITY; HIRISE OBSERVATIONS; DEPOSITS
AB Despite radically different environmental conditions, terrestrial and martian dunes bear a strong resemblance, indicating that the basic processes of saltation and grainfall (sand avalanching down the dune slipface) operate on both worlds. Here, we show that martian dunes are subject to an additional modification process not found on Earth: springtime sublimation of Mars' CO2 seasonal polar caps. Numerous dunes in Mars' north polar region have experienced morphological changes within a Mars year, detected in images acquired by the High-Resolution Imaging Science Experiment on the Mars Reconnaissance Orbiter. Dunes show new alcoves, gullies, and dune apron extension. This is followed by remobilization of the fresh deposits by the wind, forming ripples and erasing gullies. The widespread nature of these rapid changes, and the pristine appearance of most dunes in the area, implicates active sand transport in the vast polar erg in Mars' current climate.
C1 [Hansen, C. J.; Bourke, M.] Planetary Sci Inst, Tucson, AZ 85719 USA.
[Bourke, M.] Univ Oxford, Sch Geog & Environm, Oxford OX1 3QY, England.
[Bridges, N. T.] Johns Hopkins Univ, Appl Phys Lab, Laurel, MD 20723 USA.
[Byrne, S.; Dundas, C.; McEwen, A.] Univ Arizona, Lunar & Planetary Lab, Tucson, AZ 85721 USA.
[Colon, C.] Rutgers State Univ, Dept Earth & Environm Sci, Newark, NJ 07102 USA.
[Diniega, S.] CALTECH, Jet Prop Lab, Pasadena, CA 91109 USA.
[Herkenhoff, K.] US Geol Survey, Flagstaff, AZ 86001 USA.
[Mellon, M.] Univ Colorado, Lab Atmospher & Space Phys, Boulder, CO 80309 USA.
[Portyankina, G.; Thomas, N.] Univ Bern, Space Res & Planetol Div, CH-0132 Bern, Switzerland.
RP Hansen, CJ (reprint author), Planetary Sci Inst, Tucson, AZ 85719 USA.
EM cjhansen@psi.edu
RI Byrne, Shane/B-8104-2012; Bourke, Mary/I-4387-2012; Mellon,
Michael/C-3456-2016; Bridges, Nathan/D-6341-2016;
OI Bourke, Mary/0000-0002-0424-0322; Dundas, Colin/0000-0003-2343-7224
FU Jet Propulsion Laboratory, California Institute of Technology; NASA
FX This work was partially supported by the Jet Propulsion Laboratory,
California Institute of Technology, under a contract with NASA.
NR 32
TC 66
Z9 67
U1 6
U2 31
PU AMER ASSOC ADVANCEMENT SCIENCE
PI WASHINGTON
PA 1200 NEW YORK AVE, NW, WASHINGTON, DC 20005 USA
SN 0036-8075
J9 SCIENCE
JI Science
PD FEB 4
PY 2011
VL 331
IS 6017
BP 575
EP 578
DI 10.1126/science.1197636
PG 5
WC Multidisciplinary Sciences
SC Science & Technology - Other Topics
GA 715ZE
UT WOS:000286933600051
PM 21292976
ER
PT J
AU Katz, BG
Eberts, SM
Kauffman, LJ
AF Katz, Brian G.
Eberts, Sandra M.
Kauffman, Leon J.
TI Using Cl/Br ratios and other indicators to assess potential impacts on
groundwater quality from septic systems: A review and examples from
principal aquifers in the United States
SO JOURNAL OF HYDROLOGY
LA English
DT Review
DE Septic tanks; Groundwater quality; Chloride-bromide ratio; Aquifers;
United States
ID VOLATILE ORGANIC-COMPOUNDS; URBAN GROUNDWATER; NITRATE SOURCES;
CHLORIDE/BROMIDE RATIOS; SOURCE IDENTIFICATION; CHEMICAL INDICATORS;
SHALLOW GROUNDWATER; NATURAL-WATERS; WELLS; SEWAGE
AB A detailed review was made of chemical indicators used to identify impacts from septic tanks on groundwater quality. Potential impacts from septic tank leachate on groundwater quality were assessed using the mass ratio of chloride-bromide (Cl/Br), concentrations of selected chemical constituents, and ancillary information (land use, census data, well depth, soil characteristics) for wells in principal aquifers of the United States. Chemical data were evaluated from 1848 domestic wells in 19 aquifers, 121 public-supply wells in 6 aquifers, and associated monitoring wells in four aquifers and their overlying hydrogeologic units. Based on previously reported Cl/Br ratios, statistical comparisons between targeted wells (where Cl/Br ratios range from 400 to 1100 and Cl concentrations range from 20 to 100 mg/L) and non-targeted wells indicated that shallow targeted monitoring and domestic wells (<20 m depth below land surface) had a significantly (p <0.05) higher median percentage of houses with septic tanks (1990 census data) than non-targeted wells. Higher (p = 0.08) median nitrate-N concentration (3.1 mg/L) in oxic (dissolved oxygen concentrations >0.5 mg/L) shallow groundwater from target domestic wells, relative to non-target wells (1.5 mg/L), corresponded to significantly higher potassium, boron, chloride, dissolved organic carbon, and sulfate concentrations, which may also indicate the influence of septic-tank effluent. Impacts on groundwater quality from septic systems were most evident for the Eastern Glacial Deposits aquifer and the Northern High Plains aquifer that were associated with the number of housing units using septic tanks, high permeability of overlying sediments, mostly oxic conditions, and shallow wells. Overall, little or no influence from septic systems were found for water samples from the deeper public-supply wells.
The Cl/Br ratio is a useful first-level screening tool for assessing possible septic tank influence in water from shallow wells (<20 m) with the range of 400-1100. The use of this ratio would be enhanced with information on other chloride sources, temporal variability of chloride and bromide concentrations in shallow groundwater, knowledge of septic-system age and maintenance, and the use of multiple tracers (combination of additional chemical and microbiological indicators). Published by Elsevier B.V.
C1 [Katz, Brian G.] US Geol Survey, Tallahassee, FL 32303 USA.
[Eberts, Sandra M.] US Geol Survey, Columbus, OH 43229 USA.
[Kauffman, Leon J.] US Geol Survey, W Trenton, NJ 08628 USA.
RP Katz, BG (reprint author), US Geol Survey, 2639 N Monroe St, Tallahassee, FL 32303 USA.
EM bkatz@usgs.gov; smeberts@usgs.gov; lkauff@usgs.gov
OI Eberts, Sandra/0000-0001-5138-8293
NR 103
TC 45
Z9 45
U1 5
U2 60
PU ELSEVIER SCIENCE BV
PI AMSTERDAM
PA PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS
SN 0022-1694
J9 J HYDROL
JI J. Hydrol.
PD FEB 3
PY 2011
VL 397
IS 3-4
BP 151
EP 166
DI 10.1016/j.jhydrol.2010.11.017
PG 16
WC Engineering, Civil; Geosciences, Multidisciplinary; Water Resources
SC Engineering; Geology; Water Resources
GA 718IU
UT WOS:000287115300001
ER
PT J
AU Faunt, CC
Provost, AM
Hill, MC
Belcher, WR
AF Faunt, Claudia C.
Provost, Alden M.
Hill, Mary C.
Belcher, Wayne R.
TI Comment on "An unconfined groundwater model of the Death Valley Regional
Flow System and a comparison to its confined predecessor" by RWH
Carroll, GM Pohll and RL Hershey [Journal of Hydrology 373/3-4, pp.
316-328]
SO JOURNAL OF HYDROLOGY
LA English
DT Article
DE Groundwater; Numerical modeling; Death Valley; MODFLOW; Hydrogeology
ID VARIABLE-DENSITY FLOW; COASTAL AQUIFER; SIMULATION
AB Carroll et al. (2009) state that the United States Geological Survey (USGS) Death Valley Regional Flow System (DVRFS) model, which is based on MODFLOW, is "conceptually inaccurate in that it models an unconfined aquifer as a confined system and does not simulate unconfined drawdown in transient pumping simulations." Carroll et al. (2009) claim that "more realistic estimates of water availability" can be produced by a SURFACT-based model of the DVRFS that simulates unconfined groundwater flow and limits withdrawals from wells to avoid excessive drawdown. Differences in results from the original MODFLOW-based model and the SURFACT-based model stem primarily from application by Carroll et al. (2009) of head limits that can also be applied using the existing MODLOW model and not from any substantial difference in the accuracy with which the unconfined aquifer is represented in the two models. In a hypothetical 50-year predictive simulation presented by Carroll et al. (2009), large differences between the models are shown when simulating pumping from the lower clastic confining unit, where the transmissivity is nearly two orders of magnitude less than in an alluvial aquifer. Yet even for this extreme example, drawdowns and pumping rates from the MODFLOW and SURFACT models are similar when the head-limit capabilities of the MODFLOW MNW Package are applied. These similarities persist despite possible discrepancies between assigned hydraulic properties. The resulting comparison between the MODFLOW and SURFACT models of the DVRFS suggests that approximating the unconfined system in the DVRFS as a constant-saturated-thickness system (called a "confined system" by Carroll et al., 2009) performs very well. Published by Elsevier B.V.
C1 [Faunt, Claudia C.; Provost, Alden M.; Hill, Mary C.; Belcher, Wayne R.] US Geol Survey, Calif Water Sci Ctr, San Diego, CA 92101 USA.
RP Faunt, CC (reprint author), US Geol Survey, Calif Water Sci Ctr, 4165 Spruance Rd,Suite 200, San Diego, CA 92101 USA.
EM ccfaunt@usgs.gov
NR 25
TC 1
Z9 1
U1 1
U2 7
PU ELSEVIER SCIENCE BV
PI AMSTERDAM
PA PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS
SN 0022-1694
J9 J HYDROL
JI J. Hydrol.
PD FEB 3
PY 2011
VL 397
IS 3-4
BP 306
EP 309
DI 10.1016/j.jhydrol.2010.11.038
PG 4
WC Engineering, Civil; Geosciences, Multidisciplinary; Water Resources
SC Engineering; Geology; Water Resources
GA 718IU
UT WOS:000287115300013
ER
PT J
AU Frank, HJ
Mather, ME
Smith, JM
Muth, RM
Finn, JT
AF Frank, H. J.
Mather, M. E.
Smith, J. M.
Muth, R. M.
Finn, J. T.
TI Role of origin and release location in pre-spawning distribution and
movements of anadromous alewife
SO FISHERIES MANAGEMENT AND ECOLOGY
LA English
DT Article
DE alosine; native fish; restoration; stocking evaluation; telemetry; trap
and transfer
ID REARED ATLANTIC SALMON; ALOSA-PSEUDOHARENGUS; SPAWNING MIGRATION;
AMERICAN SHAD; FISH; RIVER; STOCKING; STRESS; COMMUNITY; RECOVERY
AB P>Capturing adult anadromous fish that are ready to spawn from a self sustaining population and transferring them into a depleted system is a common fisheries enhancement tool. The behaviour of these transplanted fish, however, has not been fully evaluated. The movements of stocked and native anadromous alewife, Alosa pseudoharengus (Wilson), were monitored in the Ipswich River, Massachusetts, USA, to provide a scientific basis for this management tool. Radiotelemetry was used to examine the effect of origin (native or stocked) and release location (upstream or downstream) on distribution and movement during the spawning migration. Native fish remained in the river longer than stocked fish regardless of release location. Release location and origin influenced where fish spent time and how they moved. The spatial mosaic of available habitats and the entire trajectory of freshwater movements should be considered to restore effectively spawners that traverse tens of kilometres within coastal rivers.
C1 [Mather, M. E.] Univ Massachusetts, Massachusetts Cooperat Fish & Wildlife Res Unit, Dept Nat Resources Conservat, US Geol Survey, Amherst, MA 01003 USA.
RP Mather, ME (reprint author), Univ Massachusetts, Massachusetts Cooperat Fish & Wildlife Res Unit, Dept Nat Resources Conservat, US Geol Survey, Amherst, MA 01003 USA.
EM mather@nrc.umass.edu
FU Massachusetts Division of Marine Fisheries; Ebsco Publishing; New
England BioLabs; Ipswich Bay Fly Fishing Derby; Northeast Utilities;
U.S. Fish and Wildlife Service
FX This project was administered through the Massachusetts Cooperative Fish
and Wildlife Research Unit, a cooperation among the University of
Massachusetts, the U.S. Geological Survey, the Massachusetts Division of
Marine Fisheries, the Massachusetts Division of Fisheries and Wildlife
and the Wildlife Management Institute. The Massachusetts Division of
Marine Fisheries, Ebsco Publishing, New England BioLabs, Ipswich Bay Fly
Fishing Derby, numerous alewife adopters, Northeast Utilities and the
U.S. Fish and Wildlife Service are acknowledged for support. A.
Silberzweig, S. Turner and M. Burak provided field assistance. Special
thanks to the Plum Island LTER (OCE 9726921) for generously providing
lodging. Use of brand names does not confer endorsement by the U.S.
government. Comments from Ken Sprankle, Joe Zydlewski, Mike Armstrong,
Donna Parrish, Alex Haro and three anonymous reviewers improved the
manuscript.
NR 45
TC 3
Z9 3
U1 1
U2 23
PU WILEY-BLACKWELL
PI HOBOKEN
PA 111 RIVER ST, HOBOKEN 07030-5774, NJ USA
SN 0969-997X
EI 1365-2400
J9 FISHERIES MANAG ECOL
JI Fisheries Manag. Ecol.
PD FEB
PY 2011
VL 18
IS 1
BP 12
EP 24
DI 10.1111/j.1365-2400.2010.00759.x
PG 13
WC Fisheries
SC Fisheries
GA 703RR
UT WOS:000285999500002
ER
PT J
AU Holzer, TL
Noce, TE
Bennett, MJ
AF Holzer, Thomas L.
Noce, Thomas E.
Bennett, Michael J.
TI Liquefaction Probability Curves for Surficial Geologic Deposits
SO ENVIRONMENTAL & ENGINEERING GEOSCIENCE
LA English
DT Article
DE Liquefaction; Earthquakes; Geologic Hazard Map; Engineering Geology;
Liquefaction Potential Index; Geotechnical
ID DETERMINISTIC ASSESSMENT; PENETRATION TEST; RESISTANCE; EARTHQUAKE;
SOILS; SUSCEPTIBILITY; CALIFORNIA; FAILURE; INDEX
AB Liquefaction probability curves that predict the probability of surface manifestations of earthquake-induced liquefaction are developed for 14 different types of surficial geologic units. The units consist of alluvial fan, beach ridge, river delta topset and foreset beds, eolian dune, point bar, flood basin, natural river and alluvial fan levees, abandoned river channel, deep-water lake, lagoonal, sandy artificial fill, and valley train deposits. Probability is conditioned on earthquake magnitude and peak ground acceleration. Curves are developed for water table depths of 1.5 and 5.0 m. Probabilities are derived from complementary cumulative frequency distributions of the liquefaction potential index (LPI) that were computed from 927 cone penetration tests. For natural deposits with a water table at 1.5 m and subjected to a M7.5 earthquake with peak ground acceleration (PGA) = 0.25g, probabilities range from <0.03 for alluvial fan and lacustrine deposits to >0.5 for beach ridge, point bar, and deltaic deposits. The curves also were used to assign ranges of liquefaction probabilities to the susceptibility categories proposed previously for different geologic deposits. For the earthquake described here, probabilities for susceptibility categories have ranges of 0-0.08 for low, 0.09-0.30 for moderate, 0.31-0.62 for high, and 0.63-1.00 for very high. Retrospective predictions of liquefaction during historical earthquakes based on the curves compare favorably to observations.
C1 [Holzer, Thomas L.; Noce, Thomas E.; Bennett, Michael J.] US Geol Survey, Menlo Pk, CA 94025 USA.
RP Holzer, TL (reprint author), US Geol Survey, 345 Middlefield Rd,MS977, Menlo Pk, CA 94025 USA.
RI noce, toshiaki/L-1739-2013
FU U.S. Nuclear Regulatory Commission [N6501]
FX This research was made possible by support from several institutions and
the generous assistance of many colleagues. This work was funded in part
by the U.S. Nuclear Regulatory Commission grant N6501, Central and
Eastern States Seismic Source Zones and Earthquake Characteristics.
These findings express the views of the authors and are not necessarily
those of the U. S. NRC. Other supporters include the U. S. Geological
Survey Earthquake Hazards Program and Central United States Earthquake
Consortium. Purchase of the CPT truck was enabled by the PG&E-SGS
Cooperative Research and Development Agreement. We are especially
grateful to the following individuals for discussions and help: John C.
Tinsley, III, Glenn J. Rix, David W. Moore, Scott C. Lundstrom, Todd A.
Thompson, Norman C. Hester, Coyn J. Criley, Eugene S. Schweig, Kathleen
B. Tucker, Rob E. Weems, Selcuk Toprak, Amy C. Padovani, and James
Wilkerson. We thank Ronald D. Andrus and John C. Tinsley, III, for
reviews of an early draft and the journal reviewers, Charles M.
Brankman, David Fenster, and Jeffrey R. Keaton.
NR 61
TC 10
Z9 10
U1 0
U2 5
PU GEOLOGICAL SOC AMER, INC
PI BOULDER
PA PO BOX 9140, BOULDER, CO 80301-9140 USA
SN 1078-7275
J9 ENVIRON ENG GEOSCI
JI Environ. Eng. Geosci.
PD FEB
PY 2011
VL 17
IS 1
BP 1
EP 21
DI 10.2113/gseegeosci.17.1.1
PG 21
WC Engineering, Environmental; Engineering, Geological; Geosciences,
Multidisciplinary
SC Engineering; Geology
GA 770MY
UT WOS:000291092000002
ER
PT J
AU Hart, KM
Crowder, LB
AF Hart, Kristen M.
Crowder, Larry B.
TI Mitigating By-Catch of Diamondback Terrapins in Crab Pots
SO JOURNAL OF WILDLIFE MANAGEMENT
LA English
DT Article
DE blue crab; by-catch; fisheries; North Carolina; terrapin; turtle
ID BYCATCH REDUCTION DEVICES; MALACLEMYS-TERRAPIN; MORTALITY; CAPTURE;
CONSERVATION; POPULATION; MANAGEMENT; FISHERIES; MATURITY; TURTLES
AB Chronic by-catch of diamondback terrapins (Malaclemys terrapin) in blue crab (Callinectes sapidus) pots is a concern for terrapin conservation along the United States Atlantic and Gulf of Mexico coasts. Despite the availability of by-catch reduction devices (BRDs) for crab pots, adoption of BRDs has not been mandated and by-catch of terrapins continues. We conducted experimental fishing studies in North Carolina's year-round blue crab fishery from 2000 to 2004 to evaluate the ability of various BRDs to reduce terrapin by-catch without a concomitant reduction in the catch of blue crabs. In 4,822 crab pot days fished, we recorded only 21 terrapin captures. Estimated capture rates were 0.003 terrapins/pot per day in hard crab experimental fishing and 0.008 terrapins/pot per day in peeler experimental fishing. All terrapin captures occurred from April to mid-May within 321.4 m of the shoreline. Longer soak times produced more dead terrapins, with 4 live and 4 dead during hard crab experimental fishing and 11 live and 2 dead during peeler experimental fishing. The 4.0-cm BRDs in fall and 4.5-cm and 5.0-cm BRDs in spring reduced the catch of legal-sized male hard crabs by 26.6%, 21.2%, and 5.7%, respectively. Only the 5.0-cm BRDs did not significantly affect the catch of legal-sized hard male crabs. However, BRDs had no measurable effect on catch of target crabs in the peeler crab fishery. Our results identify 3 complementary and economically feasible tools for blue crab fishery managers to exclude terrapins from commercially fished crab pots in North Carolina: 1) gear modifications (e.g., BRDs); 2) distance-to-shore restrictions; and 3) time-of-year regulations. These measures combined could provide a reduction in terrapin by-catch of up to 95% without a significant reduction in target crab catch. (C) 2011 The Wildlife Society.
C1 [Hart, Kristen M.] US Geol Survey, SE Ecol Sci Ctr, Davie, FL 33314 USA.
[Crowder, Larry B.] Duke Ctr Marine Conservat, Nicholas Sch, Environm Marine Lab, Beaufort, NC 28516 USA.
RP Hart, KM (reprint author), US Geol Survey, SE Ecol Sci Ctr, 3205 Coll Ave, Davie, FL 33314 USA.
EM kristen_hart@usgs.gov
FU North Carolina Sea Grant Fishery Resource Grant Program [00-FEG-23,
03-FEG-18]
FX Funding for experimental fishing studies was provided by the North
Carolina Sea Grant Fishery Resource Grant Program (00-FEG-23 and
03-FEG-18). Part of this work was completed as part of the doctoral work
of K. Hart at Duke University. We thank our fishing collaborators M.
Hooper and the Cahoon family and our Sea Grant Monitor B. Hines. We
acknowledge the field assistance of P. Gillikin, L. Thorne, E.
McLaughlin, and J. Kelley. We thank T. Ziegler and K. Craig for
assistance with statistical analysis, C. Good and J. Gannon for help
with calculations of distance to shore, L. Avens and Y. Escribano for
the map of our study site, and B. Boynton for crafting the crab pot
figure. J. Krebs, T. Smith, III, and E. Larrivee provided helpful
comments on an earlier draft of this manuscript. Use of trade or product
names does not imply endorsement by the United States Government.
NR 39
TC 19
Z9 20
U1 2
U2 21
PU WILEY-BLACKWELL
PI HOBOKEN
PA 111 RIVER ST, HOBOKEN 07030-5774, NJ USA
SN 0022-541X
J9 J WILDLIFE MANAGE
JI J. Wildl. Manage.
PD FEB
PY 2011
VL 75
IS 2
BP 264
EP 272
DI 10.1002/jwmg.49
PG 9
WC Ecology; Zoology
SC Environmental Sciences & Ecology; Zoology
GA 752EA
UT WOS:000289670800002
ER
PT J
AU Mccarthy, KP
Destefano, S
AF Mccarthy, Kyle P.
Destefano, Stephen
TI Effects of Spatial Disturbance on Common Loon Nest Site Selection and
Territory Success
SO JOURNAL OF WILDLIFE MANAGEMENT
LA English
DT Article
DE common loon; disturbance; eagle; Gavia immer; human; nest; Umbagog
National Wildlife Refuge
ID PRODUCTIVITY; PREDATION; GAVIA; IMMER
AB The common loon (Gavia immer) breeds during the summer on northern lakes and water bodies that are also often desirable areas for aquatic recreation and human habitation. In northern New England, we assessed how the spatial nature of disturbance affects common loon nest site selection and territory success. We found through classification and regression analysis that distance to and density of disturbance factors can be used to classify observed nest site locations versus random points, suggesting that these factors affect loon nest site selection (model 1: Correct classification = 75%, null = 50%, K = 0.507, P < 0.001; model 2: Correct classification = 78%, null 50%, K = 0.551, P < 0.001). However, in an exploratory analysis, we were unable to show a relation between spatial disturbance variables and breeding success (P = 0.595, R(2) = 0.436), possibly because breeding success was so low during the breeding seasons of 2007-2008. We suggest that by selecting nest site locations that avoid disturbance factors, loons thereby limit the effect that disturbance will have on their breeding success. Still, disturbance may force loons to use sub-optimal nesting habitat, limiting the available number of territories, and overall productivity. We advise that management efforts focus on limiting disturbance factors to allow breeding pairs access to the best nesting territories, relieving disturbance pressures that may force sub-optimal nest placement. (C) 2011 The Wildlife Society
C1 [Mccarthy, Kyle P.; Destefano, Stephen] Univ Massachusetts, Massachusetts Cooperat Fish & Wildlife Res Unit, US Geol Survey, Amherst, MA 01003 USA.
RP Mccarthy, KP (reprint author), Univ Massachusetts, Massachusetts Cooperat Fish & Wildlife Res Unit, US Geol Survey, 160 Holdsworth Way, Amherst, MA 01003 USA.
EM kyle.mccarthy@ufl.edu
FU United States Fish and Wildlife Service
FX Special thanks to J. Cooley and the Loon Preservation Committee of New
Hampshire, as well as the staff of Umbagog National Wildlife Refuge, for
allowing us to use data on loon reproductive success. Also, thanks to
our invaluable field assistants J. McCarthy and K. Rogers. Funding was
provided by the United States Fish and Wildlife Service.
NR 39
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U1 1
U2 24
PU WILEY-BLACKWELL
PI MALDEN
PA COMMERCE PLACE, 350 MAIN ST, MALDEN 02148, MA USA
SN 0022-541X
J9 J WILDLIFE MANAGE
JI J. Wildl. Manage.
PD FEB
PY 2011
VL 75
IS 2
BP 289
EP 296
DI 10.1002/jwmg.50
PG 8
WC Ecology; Zoology
SC Environmental Sciences & Ecology; Zoology
GA 752EA
UT WOS:000289670800005
ER
PT J
AU Drummer, TD
Corace, RG
Sjogren, SJ
AF Drummer, Thomas D.
Corace, R. Gregory, III
Sjogren, Stephen J.
TI Sharp-Tailed Grouse Lek Attendance and Fidelity in Upper Michigan
SO JOURNAL OF WILDLIFE MANAGEMENT
LA English
DT Article
DE lek attendance; lek fidelity; sharp-tailed grouse; upper Michigan
ID SAGE-GROUSE; PRAIRIE GROUSE; GREATER; PATTERNS; COLORADO
AB To assess and improve existing monitoring protocols for sharp-tailed grouse (Tympanuchus phasianellus) in the eastern Upper Peninsula of Michigan, we used data from 58 radio-collared grouse (46 M, 12 F) monitored within 3 openland landscape types: a xeric, conifer-dominated site, a wetland-dominated site, and a site dominated by low-intensity agriculture. We used lek counts and radio telemetry to determine lek attendance rates, factors affecting lek attendance rates, lek fidelity, and inter-sexual variation in these parameters. Our analysis indicated lek attendance varied with respect to sex of bird, day of year, time after sunrise, and wind speed. Peak male lek attendance rates exceeded those of females by up to 40%, and peak lekking activity for both males and females occurred during the second and third weeks of April. Male lekking activity occurred earlier and was sustained longer than that of females. Lekking activity was negatively related to time of day and wind speed. We observed strong lek fidelity as radio-collared birds attended a primary lek 94% of the time, indicating a low probability of multiple counting of individual birds. We also proposed a method to adjust lek count data for the probability that birds are on a lek during lek counts. Our proposed method can be used by researchers and managers to improve estimates of the number of birds attending a lek by reducing the negative bias associated with observed counts. (C) 2011 The Wildlife Society.
C1 [Drummer, Thomas D.] Michigan Technol Univ, Dept Math Sci, Houghton, MI 49931 USA.
[Corace, R. Gregory, III] US Fish & Wildlife Serv, Seney Natl Wildlife Refuge, Seney, MI 49883 USA.
[Sjogren, Stephen J.] US Forest Serv, St Ignace, MI 49781 USA.
RP Drummer, TD (reprint author), Michigan Technol Univ, Dept Math Sci, 1400 Townsend Dr, Houghton, MI 49931 USA.
EM tdrummer@mtu.edu
FU MDNRE; United States Forest Service Hiawatha National Forest; United
States Fish and Wildlife Service Seney National Wildlife Refuge; Seney
Natural History Association; UP Sustainable Forest and Wildlife Fund
FX This work was funded by the MDNRE, the United States Forest Service
Hiawatha National Forest, the United States Fish and Wildlife Service
Seney National Wildlife Refuge, the Seney Natural History Association,
and the UP Sustainable Forest and Wildlife Fund. Those who assisted with
data collection and assimilation include E. Brosnan, K. Henslee, B.
Johnson, D. McCormick, D. Munson, J. Patton, J. Patton, J. Polasik, J.
Reattoir, J. Reis, S. Rouser, W. Sterling, K. Traylor, and H. Whitman.
We thank the Michigan Sharp-tailed Grouse Association for their
enthusiasm and encouragement. We also thank the reviewers and Associate
Editor whose comments greatly improved this manuscript. The findings and
conclusions in this article are those of the author(s) and do not
necessarily represent the views of the United States Fish and Wildlife
Service or the United States Forest Service.
NR 34
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U1 6
U2 24
PU WILEY-BLACKWELL
PI MALDEN
PA COMMERCE PLACE, 350 MAIN ST, MALDEN 02148, MA USA
SN 0022-541X
J9 J WILDLIFE MANAGE
JI J. Wildl. Manage.
PD FEB
PY 2011
VL 75
IS 2
BP 311
EP 318
DI 10.1002/jwmg.42
PG 8
WC Ecology; Zoology
SC Environmental Sciences & Ecology; Zoology
GA 752EA
UT WOS:000289670800008
ER
PT J
AU Cummings, JL
Byrd, RW
Eddleman, WR
Engeman, RM
Tupper, SK
AF Cummings, John L.
Byrd, Robert W.
Eddleman, William R.
Engeman, Richard M.
Tupper, Shelagh K.
TI Effectiveness of AV-1011 (R) to Reduce Damage to Drill-Planted Rice From
Blackbirds
SO JOURNAL OF WILDLIFE MANAGEMENT
LA English
DT Article
DE Agelaius phoeniceus; anthraquinone; AV-1011 (R); birds; bird repellent;
blackbirds; rice; seedling damage; wildlife damage management
ID REGISTERED PESTICIDES; METHYL ANTHRANILATE; BIRDS; ANTHRAQUINONE;
REPELLENTS; METHIOCARB
AB We determined efficacy of AV-1011 (R) (a 50% anthraquinone product; Arkion (R) Life Sciences, New Castle, Delaware) on drill-planted rice seed to reduce blackbird damage and determine residue levels of anthraquinone (AQ) in rice seeds and seedlings and in the mature rice crop under field enclosures at the University of Missouri-Delta Center farm near Portageville, Missouri. Red-winged blackbird (Agelaius phoeniceus) damage was higher for untreated than AV-1011 (R) treated rice seedlings at assessment period 3, 15 days postplanting (F(1,141) = 15.81, P < 0.001), and at assessment period 4, 19 days postplanting (F(1,136) = 11.54, P = 0.001). Blackbird damage to AV-1011-treated seedling for assessment periods 3 and 4 was 8% and 7%, respectively, while blackbird damage to untreated seedlings during the same assessment periods was 52% and 44%. More blackbirds used untreated plots than AV-1011-treated plots during assessment periods 2-4 (F(1,17.8) = 20.02, P < 0.001). Overall concentrations of AQ on seeds averaged 5,993 mu g/g or 0.59% during the test period. Concentrations of AQ in mature rice seed and plant collected at harvest averaged 1.22 mu g/g and 0.10 mu g/g, respectively. AV-1011 offers promise for reducing bird depredations to newly planted rice, but additional testing should be conducted to evaluate this repellent in a large-scale field setting. (C) 2011 The Wildlife Society.
C1 [Cummings, John L.; Engeman, Richard M.; Tupper, Shelagh K.] US Fish & Wildlife Serv, Natl Wildlife Res Ctr, USDA, Anim & Plant Hlth Inspect Serv, Ft Collins, CO 80521 USA.
[Byrd, Robert W.] Wildlife Serv, USDA, Anim & Plant Hlth Inspect Serv, Portageville, MO 63873 USA.
[Eddleman, William R.] SE Missouri State Univ, Dept Biol, Cape Girardeau, MO 63701 USA.
RP Cummings, JL (reprint author), US Fish & Wildlife Serv, Natl Wildlife Res Ctr, USDA, Anim & Plant Hlth Inspect Serv, 4101 LaPorte Ave, Ft Collins, CO 80521 USA.
EM john.l.cummings@aphis.usda.gov
NR 16
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PU WILEY-BLACKWELL
PI MALDEN
PA COMMERCE PLACE, 350 MAIN ST, MALDEN 02148, MA USA
SN 0022-541X
J9 J WILDLIFE MANAGE
JI J. Wildl. Manage.
PD FEB
PY 2011
VL 75
IS 2
BP 353
EP 356
DI 10.1002/jwmg.65
PG 4
WC Ecology; Zoology
SC Environmental Sciences & Ecology; Zoology
GA 752EA
UT WOS:000289670800012
ER
PT J
AU Johnson, TL
Cully, JF
Collinge, SK
Ray, C
Frey, CM
Sandercock, BK
AF Johnson, Tammi L.
Cully, Jack F., Jr.
Collinge, Sharon K.
Ray, Chris
Frey, Christopher M.
Sandercock, Brett K.
TI Spread of Plague Among Black-Tailed Prairie Dogs Is Associated With
Colony Spatial Characteristics
SO JOURNAL OF WILDLIFE MANAGEMENT
LA English
DT Article
DE Cynomys ludovicianus; disease; epizootic; mark-recapture; multi-state;
Program MARK; Yersinia pestis
ID CAPTURE-RECAPTURE; CYNOMYS-LUDOVICIANUS; GENETIC-STRUCTURE; SYLVATIC
PLAGUE; TRANSMISSION; DYNAMICS; SURVIVAL; POPULATION; ENCOUNTER; RECORDS
AB Sylvatic plague (Yersinia pestis) is an exotic pathogen that is highly virulent in black-tailed prairie dogs (Cynomys ludovicianus) and causes widespread colony losses and individual mortality rates >95%. We investigated colony spatial characteristics that may influence inter-colony transmission of plague at 3 prairie dog colony complexes in the Great Plains. The 4 spatial characteristics we considered include: colony size, Euclidean distance to nearest neighboring colony, colony proximity index, and distance to nearest drainage (dispersal) corridor. We used multi-state mark-recapture models to determine the relationship between these colony characteristics and probability of plague transmission among prairie dog colonies. Annual mapping of colonies and mark-recapture analyses of disease dynamics in natural colonies led to 4 main results: 1) plague outbreaks exhibited high spatial and temporal variation, 2) the site of initiation of epizootic plague may have substantially influenced the subsequent inter-colony spread of plague, 3) the long-term effect of plague on individual colonies differed among sites because of how individuals and colonies were distributed, and 4) colony spatial characteristics were related to the probability of infection at all sites although the relative importance and direction of relationships varied among sites. Our findings suggest that conventional prairie dog conservation management strategies, including promoting large, highly connected colonies, may need to be altered in the presence of plague. (C) 2011 The Wildlife Society.
C1 [Johnson, Tammi L.] Univ Montana, Div Biol Sci, Missoula, MT 59812 USA.
[Cully, Jack F., Jr.] Kansas State Univ, Div Biol, USGS BRD Kansas Cooperat Fish & Wildlife Res Unit, Manhattan, KS 66506 USA.
[Collinge, Sharon K.] Univ Colorado, Dept Ecol & Evolutionary Biol, Environm Studies Program, Boulder, CO 80309 USA.
[Frey, Christopher M.] Stephen F Austin State Univ, Arthur Temple Coll Forestry & Agr, Nacogdoches, TX 75962 USA.
RP Johnson, TL (reprint author), Univ Montana, Div Biol Sci, Missoula, MT 59812 USA.
EM tammi.johnson@umontana.edu
RI Sandercock, Brett/L-1644-2016;
OI Sandercock, Brett/0000-0002-9240-0268; RAY, CHRIS/0000-0002-7963-9637
FU National Center for Environmental Research (NCER); United
States-Environmental Protection Agency (EPA) [R82909101-0]; National
Science Foundation [DEB-0224328]; National Institutes of Health
(NSF/NIH) [DEB-0224328]; United States Geological Survey; United States
Forest Service; Kansas Department of Wildlife and Parks; Division of
Biology at Kansas State University; Kansas Cooperative Fish and Wildlife
Research Unit
FX We thank D. Augustine and T. Peters (Comanche National Grassland), A.
Chappell, G. Mason, and J. Hartman (Cimarron National Grassland), D.
Garcia, and N. Walls (Kiowa-Rita Blanca National Grassland), and
especially the private landowners across our study areas for their
cooperation. We thank K. Gage and J. Montenieri, Centers for Disease
Control and Prevention, Division of Vector-borne Infectious Diseases
(CDC-NVBID), Ft. Collins, Colorado. We thank R. Marsh, J. Kraft, and J.
Kretzer for field assistance and B. Thiagarajan, J. Graham, and 2
anonymous reviewers of an earlier draft for their valuable comments.
Financial support for this research was provided by the National Center
for Environmental Research (NCER), Science to Achieve Results (STAR)
program of the United States-Environmental Protection Agency (EPA;
R82909101-0), the National Science Foundation and National Institutes of
Health (NSF/NIH) joint program in Ecology and Infectious Diseases
(DEB-0224328), United States Geological Survey, United States Forest
Service, Kansas Department of Wildlife and Parks, the Division of
Biology at Kansas State University, and the Kansas Cooperative Fish and
Wildlife Research Unit. Mention of trademarks or commercial products
does not imply endorsement by the U.S. government.
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PI HOBOKEN
PA 111 RIVER ST, HOBOKEN 07030-5774, NJ USA
SN 0022-541X
EI 1937-2817
J9 J WILDLIFE MANAGE
JI J. Wildl. Manage.
PD FEB
PY 2011
VL 75
IS 2
BP 357
EP 368
DI 10.1002/jwmg.40
PG 12
WC Ecology; Zoology
SC Environmental Sciences & Ecology; Zoology
GA 752EA
UT WOS:000289670800013
ER
PT J
AU Collins, WB
Dale, BW
Adams, LG
Mcelwain, DE
Joly, K
AF Collins, William B.
Dale, Bruce W.
Adams, Layne G.
Mcelwain, Darien E.
Joly, Kyle
TI Fire, Grazing History, Lichen Abundance, and Winter Distribution of
Caribou in Alaska's Taiga
SO JOURNAL OF WILDLIFE MANAGEMENT
LA English
DT Article
DE Alaska; caribou; fire; grazing history; lichen; range management;
Rangifer tarandus
ID SNOW
AB In the early 1990s the Nelchina Caribou (Rangifer tarandus) Herd (NCH) began a dramatic shift to its current winter range, migrating at least an additional 100 km beyond its historic range. We evaluated the impacts of fire and grazing history on lichen abundance and subsequent use and distribution by the NCH. Historic (prior to 1990) and current (2002) winter ranges of the NCH had similar vascular vegetation, lichen cover (P = 0.491), and fire histories (P = 0.535), but the former range had significantly less forage lichen biomass as a result of grazing by caribou. Biomass of forage lichens was twice as great overall (P = 0.031) and 4 times greater in caribou selected sites on the current range than in the historic range, greatly increasing availability to caribou. Caribou on the current range selected for stands with >20% lichen cover (P < 0.001), greater than 1,250 kg/ha (P < 0.001) forage lichen biomass and stands older than 80 yr postfire (P < 0.001). After fires, forage lichen cover and biomass seldom recovered sufficiently to attract caribou grazing until after >= 60 yr, and, as a group, primary forage lichen species did not reach maximum abundance until 180 yr postfire. Recovery following overgrazing can occur much more quickly because lichen cover, albeit mostly fragments, and organic substrates remain present. Our results provide benchmarks for wildlife managers assessing condition of caribou winter range and predicting effects of fires on lichen abundance and caribou distribution. Of our measurements of cover and biomass by species, densities and heights of trees, elevation, slope and aspect, only percentage cover by Cladonia amaurocraea, Cladina rangiferina, Flavocetraria cuculata, and lowbush cranberry (Vaccinium vitis-idaea) were necessary for predicting caribou use of winter range. (C) 2011 The Wildlife Society
C1 [Collins, William B.; Dale, Bruce W.] Alaska Dept Fish & Game, Div Wildlife Conservat, Palmer, AK 99645 USA.
[Adams, Layne G.] US Geol Survey, Alaska Sci Ctr, Anchorage, AK 99508 USA.
[Mcelwain, Darien E.] Univ Vermont, Dept Bot, Burlington, VT 05405 USA.
[Joly, Kyle] Gates Arctic Natl Pk & Preserve, Fairbanks, AK 99709 USA.
RP Collins, WB (reprint author), Alaska Dept Fish & Game, Div Wildlife Conservat, 1800 Glenn Hwy,Suite 4, Palmer, AK 99645 USA.
EM william.collins@alaska.gov
FU National Interagency Fire Center; United States Geological Survey-Alaska
Science Center; Alaska Department of Fish and Game
FX M. Collins, G. Roffler, and D. Spalinger assisted in collection of
vegetation data. A. Christ helped with statistical analysis. D. Morris
helped with graphics. Pilots J. Larivee and R. Swisher provided
efficient helicopter support and assisted in collection of vegetation
data. This paper greatly benefitted from comments by T. Jung, an
anonymous reviewer, and the editors. Funding was secured from a National
Interagency Fire Center grant, United States Geological Survey-Alaska
Science Center, and the Alaska Department of Fish and Game.
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PI MALDEN
PA COMMERCE PLACE, 350 MAIN ST, MALDEN 02148, MA USA
SN 0022-541X
J9 J WILDLIFE MANAGE
JI J. Wildl. Manage.
PD FEB
PY 2011
VL 75
IS 2
BP 369
EP 377
DI 10.1002/jwmg.39
PG 9
WC Ecology; Zoology
SC Environmental Sciences & Ecology; Zoology
GA 752EA
UT WOS:000289670800014
ER
PT J
AU Wilson, TL
Howe, FP
Edwards, TC
AF Wilson, Tammy L.
Howe, Frank P.
Edwards, Thomas C., Jr.
TI Effects of Sagebrush Treatments on Multi-Scale Resource Selection by
Pygmy Rabbits
SO JOURNAL OF WILDLIFE MANAGEMENT
LA English
DT Article
DE Brachylagus idahoensis; central-place forager; habitat selection; home
range; pygmy rabbit; sagebrush management; sagebrush restoration;
shrubsteppe; simulation; Utah
ID BRACHYLAGUS-IDAHOENSIS; SAGE-GROUSE; HABITAT; MANAGEMENT; WINTER; UTAH
AB The effects of widespread sagebrush removal treatments on pygmy rabbits (Brachylagus idahoensis) are not well understood. Due to reliance on sagebrush, pygmy rabbits are among the species for which these treatments may be detrimental. Our objectives were to evaluate the effects of experimental sagebrush treatment on 8 radio-collared pygmy rabbits between and within home range habitat selection using Monte Carlo simulation from null models. Pygmy rabbits were not extirpated from plots containing habitat treatments, and we found no evidence that treatments affected home range placement. The mean treatment distance of observed home range centers did not differ from repeated trials of random points. However, we found evidence of within home range selection against treatments from 2 of 8 rabbits located close to the treatments. The mean treatment distance of all observed locations for these 2 rabbits was greater than expected based on a null model. We also used snow tracking to show that pygmy rabbits entered treatments in 4 out of 21 trials, which was less often than expected by chance (G(2) = 8.662, P = 0.003). Conservatively, sagebrush removal treatments should not be conducted on active or recently active pygmy rabbit burrows. Elsewhere near known pygmy rabbit sites, treated patches should be small and connected by untreated corridors to prevent potentially limiting movement of rabbits among the untreated habitat. (C) 2011 The Wildlife Society.
C1 [Wilson, Tammy L.; Edwards, Thomas C., Jr.] Utah State Univ, Dept Wildland Resources, Cooperat Fish & Wildlife Res Unit, US Geol Survey, Logan, UT 84322 USA.
[Wilson, Tammy L.] Utah State Univ, Ctr Ecol, Logan, UT 84322 USA.
[Howe, Frank P.] Utah Div Wildlife Resources, Salt Lake City, UT 84114 USA.
RP Wilson, TL (reprint author), Utah State Univ, Dept Wildland Resources, Cooperat Fish & Wildlife Res Unit, US Geol Survey, Logan, UT 84322 USA.
EM t.w@aggiemail.usu.edu
FU Utah Division of Wildlife Resources; Bureau of Land Management; Natural
Resources Conservation Service; Rich County Coordinated Resource
Management Committee; United States Forest Service; Utah State
University Ecology Center
FX We thank R. Groll and the ranchers of the Rich County Grazing
Cooperative for access to private lands. The manuscript was improved by
presubmission reviews by F. Colchero, W. A. Estes-Zumpf, R. T. Larsen,
and D. M. Sanchez, further refined by 2 anonymous reviewers, and honed
by D. Hanseder and E. L. Duderino. We appreciate the dedication of our
technicians: C. Hiher, D. Lamereaux, T. B. Murphy, S. Ring, S.
Rowbottom, C. Simeon, E. Szilagyi, D. White. We also thank countless
volunteers, including A. J. Leffler, who helped with trapping and
telemetry. We extend thanks to W. A. Estes-Zumpf for instruction on the
capture and handling of pygmy rabbits. Utah Division of Wildlife
Resources, Bureau of Land Management, Natural Resources Conservation
Service, Rich County Coordinated Resource Management Committee, United
States Forest Service, and Utah State University Ecology Center all
provided funding or other support. Mention of any product does not
constitute endorsement by the United States Geological Survey.
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PI MALDEN
PA COMMERCE PLACE, 350 MAIN ST, MALDEN 02148, MA USA
SN 0022-541X
J9 J WILDLIFE MANAGE
JI J. Wildl. Manage.
PD FEB
PY 2011
VL 75
IS 2
BP 393
EP 398
DI 10.1002/jwmg.51
PG 6
WC Ecology; Zoology
SC Environmental Sciences & Ecology; Zoology
GA 752EA
UT WOS:000289670800017
ER
PT J
AU Langtimm, CA
Dorazio, RM
Stith, BM
Doyle, TJ
AF Langtimm, Catherine A.
Dorazio, Robert M.
Stith, Bradley M.
Doyle, Terry J.
TI New Aerial Survey and Hierarchical Model to Estimate Manatee Abundance
SO JOURNAL OF WILDLIFE MANAGEMENT
LA English
DT Article
DE abundance estimation; aerial surveys; dual-observer sampling; Everglades
restoration; Florida manatee; habitat covariates; hierarchical models;
removal sampling
ID DATA AUGMENTATION; ANIMAL ABUNDANCE; FLORIDA MANATEES; AGGREGATION SITE
AB Monitoring the response of endangered and protected species to hydrological restoration is a major component of the adaptive management framework of the Comprehensive Everglades Restoration Plan. The endangered Florida manatee (Trichechus manatus latirostris) lives at the marine-freshwater interface in southwest Florida and is likely to be affected by hydrologic restoration. To provide managers with prerestoration information on distribution and abundance for postrestoration comparison, we developed and implemented a new aerial survey design and hierarchical statistical model to estimate and map abundance of manatees as a function of patch-specific habitat characteristics, indicative of manatee requirements for offshore forage (seagrass), inland fresh drinking water, and warm-water winter refuge. We estimated the number of groups of manatees from dual-observer counts and estimated the number of individuals within groups by removal sampling. Our model is unique in that we jointly analyzed group and individual counts using assumptions that allow probabilities of group detection to depend on group size. Ours is the first analysis of manatee aerial surveys to model spatial and temporal abundance of manatees in association with habitat type while accounting for imperfect detection. We conducted the study in the Ten Thousand Islands area of southwestern Florida, USA, which was expected to be affected by the Picayune Strand Restoration Project to restore hydrology altered for a failed real-estate development. We conducted 11 surveys in 2006, spanning the cold, dry season and warm, wet season. To examine short-term and seasonal changes in distribution we flew paired surveys 1-2 days apart within a given month during the year. Manatees were sparsely distributed across the landscape in small groups. Probability of detection of a group increased with group size; the magnitude of the relationship between group size and detection probability varied among surveys. Probability of detection of individual manatees within a group also differed among surveys, ranging from a low of 0.27 on 11 January to a high of 0.73 on 8 August. During winter surveys, abundance was always higher inland at Port of the Islands (POI), a manatee warm-water aggregation site, than in the other habitat types. During warm-season surveys, highest abundances were estimated in offshore habitat where manatees forage on seagrass. Manatees continued to use POI in summer, but in lower numbers than in winter, possibly to drink freshwater. Abundance in other inland systems and inshore bays was low compared to POI in winter and summer, possibly because of low availability of freshwater. During cold weather, maps of patch abundance of paired surveys showed daily changes in manatee distribution associated with rapid changes in air and water temperature as manatees sought warm water with falling temperatures and seagrass areas with increasing temperatures. Within a habitat type, some patches had higher manatee abundance suggesting differences in quality, possibly due to freshwater flow. If hydrological restoration alters the location of quality habitat, postrestoration comparisons using our methods will document how manatees adjust to new resources, providing managers with information on spatial needs for further monitoring or management. Total abundance for the entire area was similar among survey dates. Credible intervals however were large on a few surveys, and may limit our ability to statistically detect trends in total abundance.
Additional modeling of abundance with time-and patch-secific covariates of salinity, water temperature, and seagrass abundance will directly link manatee abundance with physical and biological changes due to restoration and should decrease uncertainty of estimates. (C) 2011 The Wildlife Society.(dagger)
C1 [Langtimm, Catherine A.] US Geol Survey, SE Ecol Sci Ctr, Gainesville, FL 32605 USA.
[Dorazio, Robert M.] Univ Florida, US Geol Survey, SE Ecol Sci Ctr, Dept Stat, Gainesville, FL 32611 USA.
[Stith, Bradley M.] US Geol Survey, Jacobs Technol, Gainesville, FL 32605 USA.
[Doyle, Terry J.] US Fish & Wildlife Serv, Thousand Isl Natl Wildlife Refuge 10, Naples, FL 34114 USA.
RP Langtimm, CA (reprint author), US Geol Survey, SE Ecol Sci Ctr, 2201 NW 40th Terrace, Gainesville, FL 32605 USA.
EM clangtimm@usgs.gov
FU USFWS; USGS Priority Ecosystem Studies; ENP Critical Ecosystem Studies
Initiative
FX Funding was provided by the USFWS, the USGS Priority Ecosystem Studies,
and ENP Critical Ecosystem Studies Initiative. This study would not have
been possible without the able assistance of observers S. M. Bertone and
D. G. Suitor. We appreciate the abilities of pilots L. Jonas and D.
Moruzzi to fly us safely during the flights. We thank J. D. Nichols for
his excellent advice on survey designs. This manuscript was improved
with the help of the anonymous reviewers. The findings and conclusions
in this article are those of the authors and do not necessarily
represent the views of the USFWS. Any use of trade, product, or firm
names is for descriptive purposes only and does not imply endorsement by
the United States Government.
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PA 111 RIVER ST, HOBOKEN 07030-5774, NJ USA
SN 0022-541X
EI 1937-2817
J9 J WILDLIFE MANAGE
JI J. Wildl. Manage.
PD FEB
PY 2011
VL 75
IS 2
BP 399
EP 412
DI 10.1002/jwmg.41
PG 14
WC Ecology; Zoology
SC Environmental Sciences & Ecology; Zoology
GA 752EA
UT WOS:000289670800018
ER
PT J
AU Williams, BL
Holtfreter, RW
Ditchkoff, SS
Grand, JB
AF Williams, Brian L.
Holtfreter, Robert W.
Ditchkoff, Stephen S.
Grand, James B.
TI Trap Style Influences Wild Pig Behavior and Trapping Success
SO JOURNAL OF WILDLIFE MANAGEMENT
LA English
DT Article
DE box traps; corral traps; Fort Benning; Sus scrofa; trapping efficiency;
wild pigs
ID FERAL PIGS; SUS-SCROFA; ERADICATION; POPULATION
AB Despite the efforts of many natural resource professionals, wild pig (Sus scrofa) populations are expanding in many areas of the world. Although many creative techniques for controlling pig populations are being explored, trapping has been and still is the most commonly used method of population control for many public and private land managers. We conducted an observational study to examine the efficiency of 2 frequently used trap styles: a small, portable box-style trap and a larger, semi-permanent, corral-style trap. We used game cameras to examine patterns of trap entry by wild pigs around each style of trap, and we conducted a trapping session to compare trapping success between trap styles. Adult female and juvenile wild pigs entered both styles of trap more readily than did adult males, and adult males seemed particularly averse to entering box traps. Less than 10% of adult male visits to box traps resulted in entries, easily the least percentage of any class at any style of trap. Adult females entered corral traps approximately 2.2 times more often per visit than box traps and re-entered corral traps >2 times more frequently. Juveniles entered and re-entered both box and corral traps at similar rates. Overall (all-class) entry-per-visit rates at corral traps (0.71) were nearly double that of box traps (0.37). Subsequent trapping data supported these preliminary entry data; the capture rate for corral traps was >4 times that of box traps. Our data suggest that corral traps are temporally and economically superior to box traps with respect to efficiency; that is, corral traps effectively trap more pigs per trap night at a lower cost per pig than do box traps. (C) 2011 The Wildlife Society.
C1 [Williams, Brian L.; Holtfreter, Robert W.; Ditchkoff, Stephen S.] Auburn Univ, Sch Forestry & Wildlife Sci, Auburn, AL 36849 USA.
[Grand, James B.] Auburn Univ, US Geol Survey, Alabama Cooperat Fish & Wildlife Res Unit, Auburn, AL 36849 USA.
RP Williams, BL (reprint author), Auburn Univ, Sch Forestry & Wildlife Sci, Auburn, AL 36849 USA.
EM graycal6pb@aol.com
FU United States Department of Defense, Fort Benning Military Reservation;
School of Forestry and Wildlife Sciences and Center for Forest
Sustainability, Auburn University; Alabama Cooperative Fish and Wildlife
Research Unit
FX We thank G. Brooks, S. Abrams, and T. Hess for their invaluable
assistance collecting data. Funding for this research was provided by
the United States Department of Defense, Fort Benning Military
Reservation. Additional support was provided by the School of Forestry
and Wildlife Sciences and Center for Forest Sustainability, Auburn
University, and the Alabama Cooperative Fish and Wildlife Research Unit.
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PI MALDEN
PA COMMERCE PLACE, 350 MAIN ST, MALDEN 02148, MA USA
SN 0022-541X
J9 J WILDLIFE MANAGE
JI J. Wildl. Manage.
PD FEB
PY 2011
VL 75
IS 2
BP 432
EP 436
DI 10.1002/jwmg.64
PG 5
WC Ecology; Zoology
SC Environmental Sciences & Ecology; Zoology
GA 752EA
UT WOS:000289670800021
ER
PT J
AU Halstead, BJ
Wylie, GD
Coates, PS
Casazza, ML
AF Halstead, Brian J.
Wylie, Glenn D.
Coates, Peter S.
Casazza, Michael L.
TI Bayesian Adaptive Survey Protocols for Resource Management
SO JOURNAL OF WILDLIFE MANAGEMENT
LA English
DT Article
DE Bayesian inference; California; decision analysis; giant gartersnake;
occurrence; survey design; Thamnophis gigas; uncertainty
ID DETECTION PROBABILITIES; CONSERVATION; OCCUPANCY; DETECTABILITY;
INFERENCE; MODELS
AB Transparency in resource management decisions requires a proper accounting of uncertainty at multiple stages of the decision-making process. As information becomes available, periodic review and updating of resource management protocols reduces uncertainty and improves management decisions. One of the most basic steps to mitigating anthropogenic effects on populations is determining if a population of a species occurs in an area that will be affected by human activity. Species are rarely detected with certainty, however, and falsely declaring a species absent can cause improper conservation decisions or even extirpation of populations. We propose a method to design survey protocols for imperfectly detected species that accounts for multiple sources of uncertainty in the detection process, is capable of quantitatively incorporating expert opinion into the decision-making process, allows periodic updates to the protocol, and permits resource managers to weigh the severity of consequences if the species is falsely declared absent. We developed our method using the giant gartersnake (Thamnophis gigas), a threatened species precinctive to the Central Valley of California, as a case study. Survey date was negatively related to the probability of detecting the giant gartersnake, and water temperature was positively related to the probability of detecting the giant gartersnake at a sampled location. Reporting sampling effort, timing and duration of surveys, and water temperatures would allow resource managers to evaluate the probability that the giant gartersnake occurs at sampled sites where it is not detected. This information would also allow periodic updates and quantitative evaluation of changes to the giant gartersnake survey protocol. Because it naturally allows multiple sources of information and is predicated upon the idea of updating information, Bayesian analysis is well-suited to solving the problem of developing efficient sampling protocols for species of conservation concern. (C) 2011 The Wildlife Society.
C1 [Halstead, Brian J.; Wylie, Glenn D.; Coates, Peter S.; Casazza, Michael L.] US Geol Survey, Western Ecol Res Ctr, Dixon Field Stn, Dixon, CA 95620 USA.
RP Halstead, BJ (reprint author), US Geol Survey, Western Ecol Res Ctr, Dixon Field Stn, 6924 Tremont Rd, Dixon, CA 95620 USA.
EM bhalstead@usgs.gov
OI casazza, Mike/0000-0002-5636-735X
FU Calfed; California Waterfowl Association; Natomas Basin Conservancy;
United States Army Corps of Engineers; USFWS
FX We thank the USFWS for initiating our interest in developing a survey
protocol for the giant gartersnake. J. Yee provided statistical guidance
and stimulating discussion of Bayesian methods in addition to review of
an early version of this manuscript. K. Nussear also provided valuable
comments on an early version of this manuscript. P. Gore provided
administrative support. We thank the numerous biological technicians who
collected data. Support was provided by grants from Calfed, the
California Waterfowl Association, the Natomas Basin Conservancy, the
United States Army Corps of Engineers, and the USFWS. Any use of trade
names is for descriptive purposes only and does not imply endorsement by
the United States Government.
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PI HOBOKEN
PA 111 RIVER ST, HOBOKEN 07030-5774, NJ USA
SN 0022-541X
EI 1937-2817
J9 J WILDLIFE MANAGE
JI J. Wildl. Manage.
PD FEB
PY 2011
VL 75
IS 2
BP 450
EP 457
DI 10.1002/jwmg.55
PG 8
WC Ecology; Zoology
SC Environmental Sciences & Ecology; Zoology
GA 752EA
UT WOS:000289670800023
ER
PT J
AU Henley, RW
Berger, BR
AF Henley, Richard W.
Berger, Byron R.
TI Magmatic-vapor expansion and the formation of high-sulfidation gold
deposits: Chemical controls on alteration and mineralization
SO ORE GEOLOGY REVIEWS
LA English
DT Review
DE High-sulfidation; Gold; Magmatic vapor; Enargite; Silica-alunite;
Sulfosalt melt; Tennantite; Solfatara
ID STABLE-ISOTOPE GEOCHEMISTRY; ACID-SULFATE ALTERATION; CU-AU DEPOSITS;
EPITHERMAL TRANSITION; HYDROTHERMAL SYSTEMS; FLUID-INCLUSION; KUDRYAVY
VOLCANO; COLIMA VOLCANO; ORE-DEPOSITS; CRATER LAKE
AB Large bulk-tonnage high-sulfidation gold deposits, such as Yanacocha. Peru, are the surface expression of structurally-controlled lode gold deposits, such as El Indio, Chile. Both formed in active andesite-dacite volcanic terranes. Fluid inclusion, stable isotope and geologic data show that lode deposits formed within 1500 m of the paleo-surface as a consequence of the expansion of low-salinity, low-density magmatic vapor with very limited, if any, groundwater mixing. They are characterized by an initial 'Sulfate' Stage of advanced argillic wallrock alteration +/- alunite commonly with intense silicification followed by a 'Sulfide' Stage - a succession of discrete sulfide-sulfosalt veins that may be ore grade in gold and silver. Fluid inclusions in quartz formed during wallrock alteration have homogenization temperatures between 100 and over 500 degrees C and preserve a record of a vapor-rich environment.
Recent data for El Indio and similar deposits show that at the commencement of the Sulfide Stage, 'condensation' of Cu-As-S sulfosalt melts with trace concentrations of Sb, Te, Bi, Ag and Au occurred at >600 degrees C following pyrite deposition. Euhedral quartz crystals were simultaneously deposited from the vapor phase during crystallization of the vapor-saturated melt occurs to Fe-tennantite with progressive non-equilibrium fractionation of heavy metals between melt-vapor and solid. Vugs containing a range of sulfides, sulfosalts and gold record the changing composition of the vapor.
Published fluid inclusion and mineralogical data are reviewed in the context of geological relationships to establish boundary conditions through which to trace the expansion of magmatic vapor from source to surface and consequent alteration and mineralization. Initially heat loss from the vapor is high resulting in the formation of acid condensate permeating through the wallrock. This Sulfate Stage alteration effectively isolates the expansion of magmatic vapor in subsurface fracture arrays from any external contemporary hydrothermal activity. Subsequent fracturing is localized by the embrittled wallrock to provide high-permeability fracture arrays that constrain vapor expansion with minimization of heat loss. The Sulfide Stage vein sequence is then a consequence of destabilization of metal-vapor species in response to depressurization and decrease in vapor density.
The geology, mineralogy, fluid inclusion and stable isotope data and geothermometry for high-sulfidation, bulk-tonnage and lode deposits are quite different from those for epithermal gold-silver deposits such as McLaughlin. California that formed near-surface in groundwater-dominated hydrothermal systems where magmatic fluid has been diluted to less than about 30%. High sulfidation gold deposits are better termed 'Solfataric Gold Deposits' to emphasize this distinction. The magmatic-vapor expansion hypothesis also applies to the phenomenology of acidic geothermal systems in active volcanic systems and equivalent magmatic-vapor discharges on the flanks of submarine volcanoes. Published by Elsevier B.V.
C1 [Berger, Byron R.] US Geol Survey, Fed Ctr MS 964, Denver, CO 80225 USA.
[Henley, Richard W.] Australian Natl Univ, Res Sch Earth Sci, Canberra, ACT, Australia.
RP Berger, BR (reprint author), US Geol Survey, Fed Ctr MS 964, Denver, CO 80225 USA.
EM bberger@usgs.gov
NR 104
TC 21
Z9 21
U1 4
U2 47
PU ELSEVIER SCIENCE BV
PI AMSTERDAM
PA PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS
SN 0169-1368
J9 ORE GEOL REV
JI Ore Geol. Rev.
PD FEB
PY 2011
VL 39
IS 1-2
BP 63
EP 74
DI 10.1016/j.oregeorev.2010.11.003
PG 12
WC Geology; Mineralogy; Mining & Mineral Processing
SC Geology; Mineralogy; Mining & Mineral Processing
GA 753IY
UT WOS:000289766700004
ER
PT J
AU Berger, BR
Henley, RW
AF Berger, Byron R.
Henley, Richard W.
TI Magmatic-vapor expansion and the formation of high-sulfidation gold
deposits: Structural controls on hydrothermal alteration and ore
mineralization
SO ORE GEOLOGY REVIEWS
LA English
DT Review
DE High-sulfidation deposits; Advanced argillic alteration; Magmatic vapor;
Structural geology; Enargite; Gold; Solfatara
ID CU-AU DEPOSITS; ISOTOPE GEOCHEMISTRY; FLUID INCLUSIONS; COLLISION BELT;
AG DEPOSIT; FAULT; PHILIPPINES; EVOLUTION; DEFORMATION; LEPANTO
AB High-sulfidation copper-gold lode deposits such as Chinkuashih, Taiwan, Lepanto, Philippines, and Goldfield, Nevada, formed within 1500 m of the paleosurface in volcanic terranes. All underwent an early stage of extensive advanced argillic silica-alunite alteration followed by an abrupt change to spatially much more restricted stages of fracture-controlled sulfide-sulfosalt mineral assemblages and gold-silver mineralization. The alteration as well as ore mineralization stages of these deposits were controlled by the dynamics and history of syn-hydrothermal faulting.
At the Sulfate Stage, aggressive advanced argillic alteration and silicification were consequent on the in situ formation of acidic condensate from magmatic vapor as it expanded through secondary fracture networks alongside active faults. The reduction of permeability at this stage due to alteration decreased fluid flow to the surface, and progressively developed a barrier between magmatic-vapor expansion constrained by the active faults and peripheral hydrothermal activity dominated by hot-water flow. In conjunction with the increased rock strength resulting from alteration, subsequent fault-slip inversion in response to an increase in compressional stress generated new, highly permeable fractures localized by the embrittled, altered rock. The new fractures focused magmatic-vapor expansion with much lower heat loss so that condensation occurred. Sulfide Stage sulfosalt, sulfide, and gold-silver deposition then resulted from destabilization of vapor phase metal species due to vapor decompression through the new fracture array. The switch from sulfate to sulfide assemblages is, therefore, a logical consequence of changes in structural permeability due to the coupling of alteration and fracture dynamics rather than to changes in the chemistry of the fluid phase at its magmatic source. Published by Elsevier B.V.
C1 [Berger, Byron R.] US Geol Survey, Fed Ctr MS 964, Denver, CO 80225 USA.
[Henley, Richard W.] Australian Natl Univ, Res Sch Earth Sci, Canberra, ACT, Australia.
RP Berger, BR (reprint author), US Geol Survey, Fed Ctr MS 964, Denver, CO 80225 USA.
EM bberger@usgs.gov
NR 70
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Z9 16
U1 4
U2 26
PU ELSEVIER SCIENCE BV
PI AMSTERDAM
PA PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS
SN 0169-1368
J9 ORE GEOL REV
JI Ore Geol. Rev.
PD FEB
PY 2011
VL 39
IS 1-2
BP 75
EP 90
DI 10.1016/j.oregeorev.2010.11.004
PG 16
WC Geology; Mineralogy; Mining & Mineral Processing
SC Geology; Mineralogy; Mining & Mineral Processing
GA 753IY
UT WOS:000289766700005
ER
PT J
AU Singer, DA
Berger, VI
Mosier, DL
AF Singer, Donald A.
Berger, Vladimir I.
Mosier, Dan L.
TI Effects of intrusions on grades and contents of gold and other metals in
volcanogenic massive sulfide deposits
SO ORE GEOLOGY REVIEWS
LA English
DT Review
DE Exploration; Mineral assessment; VMS
ID ORE; EXPLORATION
AB The reason some VMS deposits contain more gold or other metals than others might be due to the influence of intrusions. A new approach examining this possibility is based on examining the information about many VMS deposits to test statistically if those with associated intrusions have significantly different grades or amounts of metals. A set of 632 VMS deposits with reported grades, tonnages, and information about the observed presence or absence of subvolcanic or plutonic intrusive bodies emplaced at or after VMS mineralization is statistically analyzed.
Deposits with syn-mineralization or post-mineralization intrusions nearby have higher tonnages than deposits without reported intrusions, but the differences are not statistically significant. When both kinds of intrusions are reported, VMS deposit sizes are significantly higher than in the deposits without any intrusions. Gold, silver, zinc, lead, and copper average grades are not significantly different in the VMS deposits with nearby intrusions compared to deposits without regardless of relative age of intrusive. Only zinc and copper contents are significantly higher in VMS deposits with both kinds of intrusive reported. These differences in overall metal content are due to significantly larger deposit sizes of VMS deposits where both intrusive kinds are observed and reported, rather than any difference in metal grades. Published by Elsevier BM.
C1 [Singer, Donald A.; Berger, Vladimir I.; Mosier, Dan L.] US Geol Survey, Menlo Pk, CA 94025 USA.
RP Singer, DA (reprint author), US Geol Survey, MS 901,345 Middlefield Rd, Menlo Pk, CA 94025 USA.
EM singer@usgs.gov
NR 15
TC 2
Z9 2
U1 1
U2 8
PU ELSEVIER SCIENCE BV
PI AMSTERDAM
PA PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS
SN 0169-1368
J9 ORE GEOL REV
JI Ore Geol. Rev.
PD FEB
PY 2011
VL 39
IS 1-2
BP 116
EP 118
DI 10.1016/j.oregeorev.2010.12.003
PG 3
WC Geology; Mineralogy; Mining & Mineral Processing
SC Geology; Mineralogy; Mining & Mineral Processing
GA 753IY
UT WOS:000289766700008
ER
PT J
AU Krapu, GL
Brandt, DA
Jones, KL
Johnson, DH
AF Krapu, Gary L.
Brandt, David A.
Jones, Kenneth L.
Johnson, Douglas H.
TI Geographic Distribution of the Mid-Continent Population of Sandhill
Cranes and Related Management Applications
SO WILDLIFE MONOGRAPHS
LA English
DT Article
DE breeding affiliation; Central Flyway; Grus canadensis; harvest;
Mid-continent Population (MCP); sandhill crane; satellite telemetry;
fall staging areas; subspecies; wintering grounds
ID SATELLITE TELEMETRY; LOCATION ACCURACY; SPRING MIGRATION;
GRUS-CANADENSIS; FALL MIGRATION; NORTH-DAKOTA; HABITAT USE; SNOW GEESE;
ABUNDANCE; NEBRASKA
AB The Mid-continent Population (MCP) of sandhill cranes (Grus canadensis) is widely hunted in North America and is separated into the Gulf Coast Subpopulation and Western Subpopulation for management purposes. Effective harvest management of the MCP requires detailed knowledge of breeding distribution of subspecies and subpopulations, chronology of their use of fall staging areas and wintering grounds, and exposure to and harvest from hunting. To address these information needs, we tagged 153 sandhill cranes with Platform Transmitting Terminals (PTTs) during 22 February-12 April 1998-2003 in the Central and North Platte River valleys of south-central Nebraska. We monitored PTT-tagged sandhill cranes, hereafter tagged cranes, from their arrival to departure from breeding grounds, during their fall migration, and throughout winter using the Argos satellite tracking system. The tracking effort yielded 74,041 useable locations over 49,350 tag days; median duration of tracking of individual cranes was 352 days and 73 cranes were tracked > 12 months. Genetic sequencing of mitochondrial DNA (mtDNA) from blood samples taken from each of our random sample of tagged cranes indicated 64% were G. c. canadensis and 34% were Grus canadensis tabida. Tagged cranes during the breeding season settled in northern temperate, subarctic, and arctic North America (U. S. [23%, n = 35], Canada [57%, n = 87]) and arctic regions of northeast Asia (Russia [20%, n = 31]). Distribution of tagged cranes by breeding affiliation was as follows: Western Alaska-Siberia (WA-S, 42 +/- 4% [SE]), northern Canada-Nunavut (NC-N, 21 +/- 4%), West-central Canada-Alaska (WC-A, 23 +/- 4%) and East-central Canada-Minnesota (EC-M, 14 +/- 3%). All tagged cranes returned to the same breeding affiliation used during the previous year with a median distance of 1.60 km (range: 0.08-7.7 km, n - 53) separating sites used in year 1 and year 2. Fall staging occurred primarily in central and western Saskatchewan (69%), North Dakota (16%), southwestern Manitoba (10%), and northwestern Minnesota (3%). Space-use sharing indices showed that except for NC-N and WC-A birds, probability of finding a crane from one breeding affiliation within the home range of another breeding affiliation was low during fall staging. Tagged cranes from WC-A and EC-M breeding affiliations, on average, spent 25 and 20 days, respectively, longer on fall staging areas in the northern plains than did WA-S and NC-N birds. Cranes in the NC-N, WA-S, and WC-A affiliations spent 99%, 74%, and 64%, respectively, of winter in western Texas in Hunting Zone A; EC-M cranes spent 83% of winter along the Texas Gulf Coast in Hunting Zone C. Tagged cranes that settled within the breeding range of the Gulf Coast Subpopulation spent 28% and 42% of fall staging and winter within the range of the Western Subpopulation, indicating sufficient exchange of birds to potentially limit effectiveness of MCP harvest management. Harvests of EC-M and WC-A cranes during 1998-2003 were disproportionately high to their estimated numbers in the MCP, suggesting more conservative harvest strategies may be required for these subpopulations in the future, and for sandhill cranes to occupy major parts of their historical breeding range in the Prairie Pothole Region.
Exceptionally high philopatry of MCP cranes of all 4 subpopulations to breeding sites coupled with strong linkages between crane breeding distribution, and fall staging areas and wintering grounds, provide managers guidance for targeting MCP crane harvest to meet management goas. Sufficient temporal or spatial separation exists among the 4 subpopulations on fall staging areas and wintering grounds to allow harvest to be targeted at the subpopulation level in all states and provinces (and most hunting zones within states and provinces) when conditions warrant. Knowledge gained from our study provides decision-makers in the United States, Canada, Mexico, and Russia with improved guidance for developing sound harvest regulations, focusing conservation efforts, and generating collaborative efforts among these nations on sandhill crane research and management to meet mutually important goals. (c) 2011 The Wildlife Society.
C1 [Krapu, Gary L.; Brandt, David A.; Johnson, Douglas H.] US Geol Survey, No Prairie Wildlife Res Ctr, Jamestown, ND 58401 USA.
[Jones, Kenneth L.] Univ Illinois, Dept Biol Sci MC 066, Chicago, IL 60607 USA.
RP Krapu, GL (reprint author), US Geol Survey, No Prairie Wildlife Res Ctr, 8711 37th St SE, Jamestown, ND 58401 USA.
EM gkrapu@usgs.gov
FU U.S. Geological Survey; Northern Prairie Wildlife Research Center; U.S.
Fish and Wildlife Service; North Dakota Game and Fish Department; Texas
Game and Parks Commission; Oklahoma Department of Wildlife Conservation;
Nebraska Game and Parks Commission; Kansas Department of Wildlife and
Parks; New Mexico Department of Game and Fish; South Dakota Game, Fish
and Parks Department; Wyoming Game and Fish Department; Montana
Department of Fish, Wildlife and Parks; International Crane Foundation;
Platte River Whooping Crane Maintenance Trust; Playa Lakes Joint Venture
FX This research was conducted by the Central Platte River Priority
Ecosystem Study, Biological Resources Discipline, USGS. We thank D.
Douglas for providing technical and Argos program support. We thank D.
Sharp, J. Dubovsky, J. Roberson, M. O'Meilia, T. Mitchusson, J. Hansen,
M. Syzmanski, M. Johnson, J. Gammonley, H. Hands, S. Kohn, D. Nieman, M.
Vrtiska, S. Taylor, S. Vaa, V. Bevill, R. George, L. Roberts, J.
Solberg, D. Dolton, the late J. Gabig, D. Benning, R. Parker, S.
Anschutz, P. Kinzel, J. Cornely, M. Forsberg, and P. Tebbel for their
help in facilitating various aspects of the study. We thank the late P.
Currier and F. Chavez-Ramirez, Directors of the Whooping Crane Habitat
Maintenance Trust, for allowing use of their facilities near Wood River,
Nebraska, when trapping and tagging sandhill cranes in the Platte River
Valley and North Platte River Valley. We thank R. Kirby, J. Hestbeck,
and J. Powell, Directors, and D. Jorde, Deputy Director, at the Northern
Prairie Wildlife Research Center for their support. We thank D.
Fronczak, A. Olson, A. Stonsifer, J. Drahota, W. Jones, T. Buhl, F.
Sargeant, J. Fiest, L. Wood, S. Hawks, D. Grandmaison, M. Westbrock, K.
Seginak, B. Hanson, C. Mettenbrink, R. Knopik, C. Graue, V. Carter, B.
Geaumont, J. McCabe, D. Smith, L. Potter, J. Thibault, B. Toay, M.
Stoley, M. Heiser, and M. Pieron for field assistance. We are grateful
for comments by R. Drewien, D. Sharp, and G. Ivey, which improved
earlier drafts of this manuscript and Ingrid Barcelo, Audrey
Desmarteaux-Houle, and Galina Revina for translating the abstract into
Spanish, French, and Russian. We thank the many private landowners in
Nebraska that allowed access to their lands to trap and tag cranes. Any
mention of trade, product, or firm names is for descriptive purposes
only and does not imply endorsement by the U.S. Government. This study
was supported by U.S. Geological Survey, Northern Prairie Wildlife
Research Center, U.S. Fish and Wildlife Service, North Dakota Game and
Fish Department, Texas Game and Parks Commission, Oklahoma Department of
Wildlife Conservation, Nebraska Game and Parks Commission, Kansas
Department of Wildlife and Parks, New Mexico Department of Game and
Fish, South Dakota Game, Fish and Parks Department, Wyoming Game and
Fish Department, Montana Department of Fish, Wildlife and Parks,
International Crane Foundation, Platte River Whooping Crane Maintenance
Trust, and Playa Lakes Joint Venture. Publication costs were provided by
United States Geological Survey, Science Support Program.
NR 94
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U1 8
U2 53
PU WILEY-BLACKWELL
PI HOBOKEN
PA 111 RIVER ST, HOBOKEN 07030-5774, NJ USA
SN 0084-0173
EI 1938-5455
J9 WILDLIFE MONOGR
JI Wildl. Monogr.
PD FEB
PY 2011
IS 175
BP 1
EP 38
DI 10.1002/wmon.1
PG 38
WC Ecology; Zoology
SC Environmental Sciences & Ecology; Zoology
GA 752ZU
UT WOS:000289734800001
ER
PT J
AU Small, GE
Pringle, CM
Pyron, M
Duff, JH
AF Small, Gaston E.
Pringle, Catherine M.
Pyron, Mark
Duff, John H.
TI Role of the fish Astyanax aeneus (Characidae) as a keystone nutrient
recycler in low-nutrient Neotropical streams
SO ECOLOGY
LA English
DT Article
DE Astyanax aeneus; Atherinidae; Characidae; Cichlidae; ecological
stoichiometry; fish; La Selva Biological Station, Costa Rica; nutrient
cycling; phosphorus; Poecilidae; streams
ID COSTA-RICA; PHOSPHORUS-LIMITATION; ECOSYSTEM PROCESSES; FRESH-WATER;
STOICHIOMETRY; NITROGEN; LANDSCAPE; COMMUNITY; DYNAMICS; CONSEQUENCES
AB Nutrient recycling by animals is a potentially important biogeochemical process in both terrestrial and aquatic ecosystems. Stoichiometric traits of individual species may result in some taxa playing disproportionately important roles in the recycling of nutrients relative to their biomass, acting as keystone nutrient recyclers. We examined factors controlling the relative contribution of 12 Neotropical fish species to nutrient recycling in four streams spanning a range of phosphorus (P) levels. In high-P conditions (135 mu g/L soluble reactive phosphorus, SRP), most species fed on P-enriched diets and P excretion rates were high across species. In low-P conditions (3 mu g/L SRP), aquatic food resources were depleted in P, and species with higher body P content showed low rates of P recycling. However, fishes that were subsidized by terrestrial inputs were decoupled from aquatic P availability and therefore excreted P at disproportionately high rates. One of these species, Astyanax aeneus (Characidae), represented 12% of the total population and 18% of the total biomass of the fish assemblage in our focal low-P study stream but had P excretion rates >10-fold higher than other abundant fishes. As a result, we estimated that P excretion by A. aeneus accounted for 90% of the P recycled by this fish assemblage and also supplied similar to 90% of the stream P demand in this P-limited ecosystem. Nitrogen excretion rates showed little variation among species, and the contribution of a given species to ecosystem N recycling was largely dependent upon the total biomass of that species. Because of the high variability in P excretion rates among fish species, ecosystem-level P recycling could be particularly sensitive to changes in fish community structure in P-limited systems.
C1 [Small, Gaston E.] Univ Minnesota, Dept Ecol Evolut & Behav, St Paul, MN 55108 USA.
[Pringle, Catherine M.] Univ Georgia, Odum Sch Ecol, Athens, GA 30602 USA.
[Pyron, Mark] Ball State Univ, Aquat Biol & Fisheries Ctr, Dept Biol, Muncie, IN 47306 USA.
[Duff, John H.] US Geol Survey, Div Water Resources, Menlo Pk, CA 94025 USA.
RP Small, GE (reprint author), Univ Minnesota, Dept Ecol Evolut & Behav, St Paul, MN 55108 USA.
EM gesmall@umn.edu
RI Pringle, Catherine/I-1841-2012; Pyron, Mark/D-4572-2011;
OI Pyron, Mark/0000-0003-0451-7827; Small, Gaston/0000-0002-9018-7555
FU National Science Foundation [DEB 0545463]; United States Environmental
Protection Agency (EPA)
FX We are grateful to M. Hidalgo, M. Snyder, P. Torres, M. Lettrich, J.
Frisch, and L. Schweizer for help with fieldwork. T. Maddox and L. Dean
contributed to laboratory analyses. Suggestions from the Pringle and
Rosemond laboratories, J. Benstead, S. Thomas, T. Short, and two
anonymous reviewers improved the manuscript. J. Reeves contributed
advice on statistical models. Research funding was provided by the
National Science Foundation (DEB 0545463 to C. M. Pringle, F. J. Triska,
and A. Ramirez). G. Small is supported in part by the United States
Environmental Protection Agency (EPA) under the Science to Achieve
Results (STAR) Graduate Fellowship Program. EPA has not officially
endorsed this publication, and the views expressed herein may not
reflect the views of the EPA.
NR 41
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U1 5
U2 48
PU ECOLOGICAL SOC AMER
PI WASHINGTON
PA 1990 M STREET NW, STE 700, WASHINGTON, DC 20036 USA
SN 0012-9658
J9 ECOLOGY
JI Ecology
PD FEB
PY 2011
VL 92
IS 2
BP 386
EP 397
DI 10.1890/10-0081.1
PG 12
WC Ecology
SC Environmental Sciences & Ecology
GA 750NC
UT WOS:000289553600014
PM 21618918
ER
PT J
AU Stueve, KM
Isaacs, RE
Tyrrell, LE
Densmore, RV
AF Stueve, Kirk M.
Isaacs, Rachel E.
Tyrrell, Lucy E.
Densmore, Roseann V.
TI Spatial variability of biotic and abiotic tree establishment constraints
across a treeline ecotone in the Alaska Range
SO ECOLOGY
LA English
DT Article
DE Denali National Park and Preserve, Alaska, USA; equilibrium assumption;
facilitation; hierarchical partitioning; landscape ecology; permafrost;
Picea glauca; seed dispersal; timberline; topography
ID ARCTIC ALPINE TREELINE; WHITE SPRUCE; INTERIOR ALASKA; SWEDISH SCANDES;
TUNDRA ECOTONE; CLIMATE-CHANGE; LINE DYNAMICS; VEGETATION; MODEL;
PERSPECTIVE
AB Throughout interior Alaska (USA), a gradual warming trend in mean monthly temperatures occurred over the last few decades (similar to 2-4 degrees C). The accompanying increases in woody vegetation at many alpine treeline (hereafter treeline) locations provided an opportunity to examine how biotic and abiotic local site conditions interact to control tree establishment patterns during warming. We devised a landscape ecological approach to investigate these relationships at an undisturbed treeline in the Alaska Range. We identified treeline changes between 1953 (aerial photography) and 2005 (satellite imagery) in a geographic information system (GIS) and linked them with corresponding local site conditions derived from digital terrain data, ancillary climate data, and distance to 1953 trees. Logistic regressions enabled us to rank the importance of local site conditions in controlling tree establishment.
We discovered a spatial transition in the importance of tree establishment controls. The biotic variable (proximity to 1953 trees) was the most important tree establishment predictor below the upper tree limit, providing evidence of response lags with the abiotic setting and suggesting that tree establishment is rarely in equilibrium with the physical environment or responding directly to warming. Elevation and winter sun exposure were important predictors of tree establishment at the upper tree limit, but proximity to trees persisted as an important tertiary predictor, indicating that tree establishment may achieve equilibrium with the physical environment. However, even here, influences from the biotic variable may obscure unequivocal correlations with the abiotic setting (including temperature). Future treeline expansion will likely be patchy and challenging to predict without considering the spatial variability of influences from biotic and abiotic local site conditions.
C1 [Stueve, Kirk M.] Texas A&M Univ, Coll Geosci, Dept Geog, College Stn, TX 77843 USA.
[Isaacs, Rachel E.] KR Biogeog Res, Shafer, MN 55075 USA.
[Tyrrell, Lucy E.] Denali Natl Pk & Preserve, Natl Pk Serv, Denali Natl Pk, AK 99755 USA.
[Densmore, Roseann V.] US Geol Survey, Alaska Sci Ctr, Anchorage, AK 99508 USA.
RP Stueve, KM (reprint author), USDA, No Res Stn, Forest Serv, St Paul, MN 55108 USA.
FU Discover Denali Fellowship Program; Murie Science and Learning Center;
Denali Education Center; Texas A&M Department of Geography
FX We dedicate this research to the memory of Les Viereck, who devoted much
of his life to studying the vegetation of Alaska. The Discover Denali
Fellowship Program, Murie Science and Learning Center, Denali Education
Center, and Texas A&M Department of Geography generously provided
funding, equipment use, and laboratory resources. We thank David Tomeo
for supporting fieldwork logistics and Jon Paynter for distributing
spatial data. We thank the National Park Service for help with the
research and collecting permit and with park logistics. Carl Roland and
Martin Wilmking made invaluable contributions to facilitate the
selection of the study site. Aaron Moody provided exceptional
suggestions during the formative stages of our landscape ecological
approach. We appreciate constructive criticisms given by two anonymous
referees.
NR 48
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U1 0
U2 53
PU ECOLOGICAL SOC AMER
PI WASHINGTON
PA 1990 M STREET NW, STE 700, WASHINGTON, DC 20036 USA
SN 0012-9658
J9 ECOLOGY
JI Ecology
PD FEB
PY 2011
VL 92
IS 2
BP 496
EP 506
DI 10.1890/09-1725.1
PG 11
WC Ecology
SC Environmental Sciences & Ecology
GA 750NC
UT WOS:000289553600024
PM 21618928
ER
PT J
AU Valente, JJ
King, SL
Wilson, RR
AF Valente, Jonathon J.
King, Sammy L.
Wilson, R. Randy
TI Distribution and Habitat Associations of Breeding Secretive Marsh Birds
in Louisiana's Mississippi Alluvial Valley
SO WETLANDS
LA English
DT Article
DE Bittern; Rail; Wetland
ID SITE-OCCUPANCY; SOUTHWESTERN LOUISIANA; COMMON MOORHEN; YELLOW RAILS;
KING RAILS; NEW-YORK; RIVER; CONSERVATION; WATERBIRDS; ABUNDANCE
AB Populations of many North American secretive marsh birds (SMBs) have declined in recent decades, partially as a function of wetland loss. Protecting and restoring appropriate habitat for these species is contingent upon understanding the habitat features they utilize. We investigated breeding distributions of SMBs in northeast Louisiana at 118 wetlands in 2007 and 2008 and modeled species occupancy (psi) as a function of habitat variables measured at local (<= 100 m) and landscape (<= 1 km) scales. Common Moorhens (Gallinula chloropus), Least Bitterns (Ixobrychus exilis), and Purple Gallinules (Porphyrula martinica) were the most commonly detected species, whereas breeding King Rails (Rallus elegans) and American Coots (Fulica americana) were rare. Local habitat features consistently played a greater role in predicting psi than landscape features for the three most common species. The proportion of local wetland area dominated by robust emergent vegetation (i.e., Typha spp. and Zizaniopsis miliacea) positively influenced psi for all species, while other wetland vegetation types tended to have a minimal or negative effect. Our results suggest the habitat characteristics preferred by breeding SMBs differ from those used by migrating shorebirds and wintering waterfowl and management and restoration objectives for those species may be inadequate for enhancing SMB habitat.
C1 [Valente, Jonathon J.] Louisiana State Univ, Sch Renewable Nat Resources, Baton Rouge, LA 70803 USA.
[King, Sammy L.] Louisiana State Univ, US Geol Survey, Louisiana Cooperat Fish & Wildlife Res Unit, Sch Renewable Nat Resources 124, Baton Rouge, LA 70803 USA.
[Wilson, R. Randy] US Fish & Wildlife Serv, Jackson, MS 39213 USA.
RP Valente, JJ (reprint author), USA, Environm Lab, Engn Res & Dev Ctr, Louisville, KY 40204 USA.
EM Jonathon.J.Valente@gmail.com
FU U.S. Fish & Wildlife Service State Wildlife [T-41-R]
FX This project was funded by U.S. Fish & Wildlife Service State Wildlife
Grant T-41-R which was administered by the Louisiana Department of
Wildlife and Fisheries. The use of trade, product, or industry firm
names or products is for informative purposes only and does not
constitute an endorsement by the U.S. Government or the U.S. Geological
Survey. We thank J. A. Nyman, P. Stouffer, K. McCarter, B. Strader, M.
Kaller, S. Pierluissi, T. Cooper and the late R. Helm for their
intellectual contributions. We also thank C. Duplechain, D. Crawford, E.
DeLeon, T. Gancos, E. Hunter, J. Unger, J. Keiser, M. Osinskie, J.
Russell, R. Villani, H. Gee, B. Pickens, P. Newell, S. R. Kang, for
their logistical assistance. Lastly, this research would not have been
possible without the support and resources provided by numerous
individuals working for the Louisiana Department of Wildlife and
Fisheries, U.S. Fish and Wildlife Service, and Natural Resources
Conservation Service.
NR 51
TC 9
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U1 5
U2 33
PU SPRINGER
PI DORDRECHT
PA VAN GODEWIJCKSTRAAT 30, 3311 GZ DORDRECHT, NETHERLANDS
SN 0277-5212
EI 1943-6246
J9 WETLANDS
JI Wetlands
PD FEB
PY 2011
VL 31
IS 1
BP 1
EP 10
DI 10.1007/s13157-010-0138-3
PG 10
WC Ecology; Environmental Sciences
SC Environmental Sciences & Ecology
GA 741ZO
UT WOS:000288907700001
ER
PT J
AU Cariveau, AB
Pavlacky, DC
Bishop, AA
LaGrange, TG
AF Cariveau, Alison B.
Pavlacky, David C., Jr.
Bishop, Andrew A.
LaGrange, Theodore G.
TI Effects of Surrounding Land use on Playa Inundation following Intense
Rainfall
SO WETLANDS
LA English
DT Article
DE Conservation Reserve Program; Herbaceous buffer; Hydrology;
Infiltration; Nebraska; Runoff; Sedimentation
ID CONSERVATION RESERVE PROGRAM; PRAIRIE POTHOLE REGION; SOUTHERN
HIGH-PLAINS; WETLANDS; SEDIMENT; WATER; MIGRATION; WILDLIFE; HABITAT;
IMPACT
AB Many isolated wetlands that fill by rainfall, such as playas, have been affected by sedimentation in heavily modified agricultural landscapes. Conservation plantings and buffers reduce sedimentation in wetlands but also may reduce the frequency of inundation. We studied the effects of surrounding landcover on the responses of playas in southwestern Nebraska to heavy rain events using aerial photography, ground surveys, and GIS landscape analyses. Using a generalized linear mixed model, we found that playas in rangeland were more likely to become inundated than playas in cropland, and both were more likely to become inundated than playas in fields enrolled in USDA's Conservation Reserve Program (CRP), typified by tall, dense grasses. Inundation was also positively related to rainfall amount and playa size. Our results highlight the significance of maintaining playas in native prairie and underscore the importance of planting and managing appropriate mixes of native shortgrass and/or mixed-grass prairie species surrounding playas to mimic the vegetative structure of native prairie. In light of historic wetland losses, a reduction in the probability of flooding for individual playas in CRP must be weighed against the protection from sedimentation that buffers afford wetlands in cropland and other beneficial influences of CRP in the landscape.
C1 [Cariveau, Alison B.; Pavlacky, David C., Jr.] Rocky Mt Bird Observ, Brighton, CO 80603 USA.
[Bishop, Andrew A.] US Fish & Wildlife Serv, Grand Isl, NE 68801 USA.
[LaGrange, Theodore G.] Nebraska Game & Pk Commiss, Lincoln, NE 68503 USA.
RP Cariveau, AB (reprint author), Rocky Mt Bird Observ, 14500 Lark Bunting Lane,POB 1232, Brighton, CO 80603 USA.
EM Alison.Cariveau@gmail.com
FU Nebraska Game and Parks Commission (NGPC); PLJV
FX The Nebraska Game and Parks Commission (NGPC) and the PLJV funded this
project from the USFWS State Wildlife Grant Program and Conoco-Phillips,
respectively. We thank NGPC biologists Douglas Ekberg, Mike Fritz, Tim
Hermansen, Emily Munter, and Sarah Rehme; Kelsi Niederklein of Pheasants
Forever; and RMBO staff Crystal Bechaver, Jennifer Blakesley, Luke
Caldwell, Cliff Cordy, Derek Hill, Lacrecia Johnson, Marie-Melissa
Kalamaras, Sarah Manor, Christopher Nicholson, Larry Snyder, Rob Sparks,
Emily Steel, and Eric Sytsma for their hard work on this project. We
thank Jacob Erdman at the USFWS Great Plains GIS Partnership and Megan
McLachlan at PLJV for their assistance with aerial photography
interpretation and GIS data analysis. We thank Nadine Bishop and Claudia
Stevenson of the NRCS for hand-delineating playa water-sheds and
supporting a field surveyor, respectively. We thank Joel Jorgensen, Mike
Gilbert, Tim McCoy, Ritch Nelson, and Mark Vrtiska for comments on
drafts of this manuscript.
NR 51
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U1 3
U2 20
PU SPRINGER
PI DORDRECHT
PA VAN GODEWIJCKSTRAAT 30, 3311 GZ DORDRECHT, NETHERLANDS
SN 0277-5212
EI 1943-6246
J9 WETLANDS
JI Wetlands
PD FEB
PY 2011
VL 31
IS 1
BP 65
EP 73
DI 10.1007/s13157-010-0129-4
PG 9
WC Ecology; Environmental Sciences
SC Environmental Sciences & Ecology
GA 741ZO
UT WOS:000288907700007
ER
PT J
AU Heimann, DC
Krempa, HM
AF Heimann, David C.
Krempa, Heather M.
TI Cumulative Effects of Impoundments on the Hydrology of Riparian Wetlands
along the Marmaton River, West-Central Missouri, USA
SO WETLANDS
LA English
DT Article
DE Numerical modeling; Streamflow regulation; Water budget; Wetland
hydrology
ID GOODNESS-OF-FIT; UNITED-STATES; ECOSYSTEMS; IMPACTS; REGIME; MODEL; DAMS
AB The effects of proposed impoundments and resulting streamflow regulation on riparian wetlands in the Marmaton River Basin, Missouri, USA were determined using measurements and numerical simulations of wetland water budgets. Calibrated and validated Soil-Plant-Air-Water (SPAW) models were used to simulate daily water depths of four riparian wetlands for Current (model scenario of existing impoundments) and Proposed (model scenario of existing and proposed impoundments) impoundment conditions. The simulated frequency of flooding decreased 19-65% at the wetlands following the additions of proposed impoundments. The reduced flooding resulted in decreases in wetland water depths at all sites during the 10 simulated growing seasons under Proposed conditions with an average duration of continuous water-depth declines of 289 days at the upstream (most regulated) site. Downstream wetlands within the zone of least regulation had an average duration of water level decreases of about 20 days. Decreased water levels under Proposed conditions resulted in a range of 65-365 additional dry days at the study wetlands during the simulated 10-year period of Proposed conditions. The areas of the four wetlands meeting the hydrologic criteria of a formal jurisdictional wetland definition decreased ranging from zero to 31% under Proposed impoundment conditions.
C1 [Heimann, David C.] 401 US Geol Survey, Water Resources Discipline, Lees Summit, MO 64086 USA.
[Krempa, Heather M.] Univ Cent Missouri, Dept Biol & Earth Sci, Warrensburg, MO 64093 USA.
RP Heimann, DC (reprint author), 401 US Geol Survey, Water Resources Discipline, NW Capital Dr, Lees Summit, MO 64086 USA.
EM dheimann@usgs.gov
FU U.S. Environmental Protection Agency [CD 98779501]; Missouri Department
of Conservation
FX Partial support for this project was made possible through a U.S.
Environmental Protection Agency wetlands program development grant
(grant number CD 98779501). Additional support and assistance was
provided by the Missouri Department of Conservation.
NR 43
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U2 8
PU SPRINGER
PI DORDRECHT
PA VAN GODEWIJCKSTRAAT 30, 3311 GZ DORDRECHT, NETHERLANDS
SN 0277-5212
EI 1943-6246
J9 WETLANDS
JI Wetlands
PD FEB
PY 2011
VL 31
IS 1
BP 135
EP 146
DI 10.1007/s13157-010-0121-z
PG 12
WC Ecology; Environmental Sciences
SC Environmental Sciences & Ecology
GA 741ZO
UT WOS:000288907700013
ER
PT J
AU Fujisaki, I
Mazzotti, FJ
Dorazio, RM
Rice, KG
Cherkiss, M
Jeffery, B
AF Fujisaki, Ikuko
Mazzotti, Frank J.
Dorazio, Robert M.
Rice, Kenneth G.
Cherkiss, Michael
Jeffery, Brian
TI Estimating Trends in Alligator Populations from Nightlight Survey Data
SO WETLANDS
LA English
DT Article
DE Alligator mississippiensis; Crocodilian; Everglades; Detection
probability; Hierarchical model; Monitoring
ID CROCODYLUS-POROSUS; CROCODILE ABUNDANCE; SPOTLIGHT COUNTS;
MARK-RECAPTURE; RESTORATION; INDICATORS; MODELS
AB Nightlight surveys are commonly used to evaluate status and trends of crocodilian populations, but imperfect detection caused by survey- and location-specific factors makes it difficult to draw population inferences accurately from uncorrected data. We used a two-stage hierarchical model comprising population abundance and detection probability to examine recent abundance trends of American alligators (Alligator mississippiensis) in subareas of Everglades wetlands in Florida using nightlight survey data. During 2001-2008, there were declining trends in abundance of small and/or medium sized animals in a majority of subareas, whereas abundance of large sized animals had either demonstrated an increased or unclear trend. For small and large sized class animals, estimated detection probability declined as water depth increased. Detection probability of small animals was much lower than for larger size classes. The declining trend of smaller alligators may reflect a natural population response to the fluctuating environment of Everglades wetlands under modified hydrology. It may have negative implications for the future of alligator populations in this region, particularly if habitat conditions do not favor recruitment of offspring in the near term. Our study provides a foundation to improve inferences made from nightlight surveys of other crocodilian populations.
C1 [Fujisaki, Ikuko; Mazzotti, Frank J.; Cherkiss, Michael; Jeffery, Brian] Univ Florida, Ft Lauderdale Res & Educ Ctr, Davie, FL 33314 USA.
[Dorazio, Robert M.] Univ Florida, Dept Stat, Gainesville, FL 32611 USA.
[Dorazio, Robert M.; Rice, Kenneth G.] US Geol Survey, SE Ecol Sci Ctr, Gainesville, FL 32653 USA.
RP Fujisaki, I (reprint author), Univ Florida, Ft Lauderdale Res & Educ Ctr, 3205 Coll Ave, Davie, FL 33314 USA.
EM ikuko@ufl.edu
FU U.S. Army; U.S. Geological Survey Priority Ecosystems Sciences program;
U.S. National Park Service Critical Ecosystem Science Initiative
FX This study was funded by the U.S. Army Corps of Engineers Comprehensive
Everglades Restoration Plan Monitoring and Assessment Program, the U.S.
Geological Survey Priority Ecosystems Sciences program, and the U.S.
National Park Service Critical Ecosystem Science Initiative. We thank
our many technicians for conducting nightlight surveys, two anonymous
reviewers of the U. S. Geological Survey, Rebecca Harvey and Sara
Williams for providing editorial assistance, and two anonymous reviewers
for helping to clarify and contextualize the manuscript. Use of trade,
product, or firm names does not imply endorsement by the U.S.
Government.
NR 43
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U1 2
U2 23
PU SPRINGER
PI DORDRECHT
PA VAN GODEWIJCKSTRAAT 30, 3311 GZ DORDRECHT, NETHERLANDS
SN 0277-5212
EI 1943-6246
J9 WETLANDS
JI Wetlands
PD FEB
PY 2011
VL 31
IS 1
BP 147
EP 155
DI 10.1007/s13157-010-0120-0
PG 9
WC Ecology; Environmental Sciences
SC Environmental Sciences & Ecology
GA 741ZO
UT WOS:000288907700014
ER
PT J
AU Blanco, JM
Long, JA
Gee, G
Wildt, DE
Donoghue, AM
AF Blanco, Juan M.
Long, Julie A.
Gee, George
Wildt, David E.
Donoghue, Ann M.
TI Comparative cryopreservation of avian spermatozoa: Benefits of
non-permeating osmoprotectants and ATP on turkey and crane sperm
cryosurvival
SO ANIMAL REPRODUCTION SCIENCE
LA English
DT Article
DE Poultry sperm; DMA; Trehalose; Sucrose; Betaine hydrochloride
ID EXTRACELLULAR ADENOSINE 5'-TRIPHOSPHATE; COTURNIX-JAPONICA SPERMATOZOA;
FERTILIZING ABILITY; GLYCINE BETAINE; FOWL SPERMATOZOA; RAM SPERMATOZOA;
COOLING RATE; BULL SPERM; TREHALOSE; MOTILITY
AB A comparative approach was used to evaluate the cryosurvival of turkey and crane sperm frozen in a dimethylacetamide (DMA) cryodiluent supplemented with osmoprotectants and ATP. A range (6-26%) of DMA concentrations was used alone or in combination with ATP (30,60 or 118 mM) or one of the following osmoprotectants: (1) sucrose (turkey, 8.0%; crane, 5.0%); (2) 5.0% sucrose and 5.0% trehalose; or (3) betaine hydrochloride (0.1, 0.2 or 0.4 mM). The viability of thawed sperm was assessed using the nigrosin-eosin stain and sperm motility was determined using the hanging-drop technique. For semen frozen only with DMA, post-thaw sperm motility was greatest (P < 0.05) for the 6.0%, 10.0% and 18% concentrations, regardless of species. Turkey sperm frozen with the sucrose/trehalose combination had greater (P < 0.05) post-thaw motility for all DMA treatments compared to DMA alone. The lowest concentration of the osmoprotectant betaine hydrochloride substantially improved turkey sperm viability post-thaw in all treatments compared to DMA alone (P < 0.05). The post-thaw motility of crane sperm was improved (P< 0.05) with a combination of 18.0%, 24.0% or 26.0% DMA and 30 mM ATP. Moreover, in the presence of osmoprotectants, crane sperm motility decreased as the osmoprotectant concentration increased. The lowest concentration of ATP also improved crane sperm viability post-thaw, especially for DMA concentrations 18% or greater. The combination of sucrose and trehalose improved (P < 0.05) crane sperm viability only with 6% and 10% DMA. These data affirm that there are avian-specific differences in sperm survival after cryopreservation and suggest that post-thaw survival can be enhanced by including species-based osmoprotectant/ATP combinations in a cryodiluent where DMA is the cryoprotectant. Published by Elsevier B.V.
C1 [Blanco, Juan M.; Long, Julie A.] ARS, USDA, ANRI, ABBL, Beltsville, MD 20705 USA.
[Blanco, Juan M.] Aquila Fdn, Toledo, Spain.
[Blanco, Juan M.] CERI, Ctr Studies Iberian Raptors, Toledo, Spain.
[Gee, George] US Fish & Wildlife Serv, Patuxent Wildlife Res Ctr, Laurel, MD 20708 USA.
[Wildt, David E.] Smithsonians Natl Zool Pk, Conservat & Res Ctr, Ctr Species Survival, Front Royal, VA 22630 USA.
[Donoghue, Ann M.] ARS, USDA, PPPSRU, Fayetteville, AR 72701 USA.
RP Long, JA (reprint author), ARS, USDA, ANRI, ABBL, Beltsville, MD 20705 USA.
EM julie.long@ars.usda.gov
RI Wilkinson, Stuart/C-2802-2013
FU USDA [SP 33]; Patuxent Wildlife Research Center, USGS; Junta de
Comunidades de Castilla-La Mancha; Smithsonian Institution/British
Airways partnership; Smithsonian Women's Committee; Aquila Foundation
FX This study was supported by the USDA Foreign Agricultural Services
Project #SP 33; The Patuxent Wildlife Research Center, USGS; The Junta
de Comunidades de Castilla-La Mancha, the Smithsonian
Institution/British Airways partnership; The Smithsonian Women's
Committee; and the Aquila Foundation.
NR 48
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U1 0
U2 11
PU ELSEVIER SCIENCE BV
PI AMSTERDAM
PA PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS
SN 0378-4320
J9 ANIM REPROD SCI
JI Anim. Reprod. Sci.
PD FEB
PY 2011
VL 123
IS 3-4
BP 242
EP 248
DI 10.1016/j.anireprosci.2010.12.005
PG 7
WC Agriculture, Dairy & Animal Science; Reproductive Biology
SC Agriculture; Reproductive Biology
GA 738GG
UT WOS:000288627700015
PM 21277718
ER
PT J
AU Oppel, S
Powell, AN
Butler, MG
AF Oppel, Steffen
Powell, Abby N.
Butler, Malcolm G.
TI KING EIDER FORAGING EFFORT DURING THE PRE-BREEDING PERIOD IN ALASKA
SO CONDOR
LA English
DT Article
DE behavior; chironomid; foraging; intake rate; King Eider; sea duck;
Somateria spectabilis
ID WINTERING COMMON-EIDERS; SOMATERIA-MOLLISSIMA; EGG-PRODUCTION; SNOW
GEESE; FUNCTIONAL-RESPONSE; INCOME DICHOTOMY; CAPITAL BREEDERS; ACTIVITY
BUDGETS; NORTHERN ALASKA; BODY-MASS
AB For reproduction, many arctic-nesting migratory birds rely on nutrients obtained on the breeding grounds, so they devote sufficient time to foraging immediately prior to nesting. However, little is known about the increase in foraging effort necessary to meet the energetic requirements of reproduction. In early June 2006 and 2008, we quantified the proportion of time spent foraging before breeding by a large sea duck, the King Eider (Somateria spectabilis), on its breeding grounds in northern Alaska. During > 235 hours of behavioral observations, both male and female King Eiders spent > 50% of the day loafing (resting, sleeping, comfort behavior, or being alert). Females foraged on average 30% of the time (mean 7.2 hr day(-1), 95% CI 6.0-8.4 hr day(-1)), three times as much as males (9%; 2.3 hr day(-1), 95% CI 1.5-2.8 hr day(-1)). The most common prey in ponds where the eiders foraged were chironomid larvae and worms ranging in length from 1 to 30 mm. If the King Eider's daily energy expenditure on its breeding grounds is similar to values published for related species, it would need to ingest only 0.2-0.6 g dry mass of invertebrates per minute of foraging to meet its energetic requirements. Males did not lose body mass before breeding, and we assume that their foraging effort was sufficient for energy balance. Therefore, female King Eiders appear to triple their foraging effort over maintenance requirements to meet the energetic challenges of egg formation.
C1 [Oppel, Steffen; Powell, Abby N.] Univ Alaska, Dept Biol & Wildlife, Fairbanks, AK 99775 USA.
[Powell, Abby N.] Univ Alaska, US Geol Survey, Alaska Cooperat Fish & Wildlife Res Unit, Fairbanks, AK 99775 USA.
[Powell, Abby N.] Univ Alaska, Inst Arctic Biol, Fairbanks, AK 99775 USA.
[Butler, Malcolm G.] N Dakota State Univ, Dept Biol Sci, Fargo, ND 58108 USA.
RP Oppel, S (reprint author), Royal Soc Protect Birds, Sandy SG19 2DL, Beds, England.
EM abby.powell@alaska.edu
OI Powell, Abby/0000-0002-9783-134X; Oppel, Steffen/0000-0002-8220-3789
FU U.S. Geological Survey; U.S. National Fish and Wildlife Foundation
FX This study was funded by the U.S. Geological Survey's Outer Continental
Shelf Program. The Alaska Fish and Wildlife Fund, through the U.S.
National Fish and Wildlife Foundation, supported the sampling of
invertebrates in 2009. We thank the North Slope Borough and R. Suydam
for logistical support during field work. P. Petterson Sartz, E.
Goldsmith, J. Heathcote, J. Rogalla, and J. Lambrecht assisted in
behavioral observations. We appreciate the comments of J. Lovvorn, P.
Barboza, D.L. Dickson, E.C. Murphy, R. Elner, and two anonymous
reviewers on an earlier draft of the manuscript. Mention of trade names
or commercial products is for descriptive purposes only and does not
imply endorsement by the U.S. government.
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PU COOPER ORNITHOLOGICAL SOC
PI LAWRENCE
PA ORNITHOLOGICAL SOC NORTH AMER PO BOX 1897, LAWRENCE, KS 66044-8897 USA
SN 0010-5422
J9 CONDOR
JI Condor
PD FEB
PY 2011
VL 113
IS 1
BP 52
EP 60
DI 10.1525/cond.2011.100077
PG 9
WC Ornithology
SC Zoology
GA 739RT
UT WOS:000288736400006
ER
PT J
AU Kochert, MN
Fuller, MR
Schueck, LS
Bond, L
Bechard, MJ
Woodbridge, B
Holroyd, GL
Martell, MS
Banasch, U
AF Kochert, Michael N.
Fuller, Mark R.
Schueck, Linda S.
Bond, Laura
Bechard, Marc J.
Woodbridge, Brian
Holroyd, Geoff L.
Martell, Mark S.
Banasch, Ursula
TI MIGRATION PATTERNS, USE OF STOPOVER AREAS, AND AUSTRAL SUMMER MOVEMENTS
OF SWAINSON'S HAWKS
SO CONDOR
LA English
DT Article
DE Buteo swainsoni; migration; migratory behavior; movements; stopovers;
Argentina; austral summer; connectivity; Swainson's Hawk
ID OSPREYS PANDION-HALIAETUS; FALCONS FALCO-PEREGRINUS; SATELLITE TRACKING;
WINTERING GROUNDS; AUTUMN MIGRATION; MASS MORTALITY; ARGENTINA; HABITAT;
ROUTES; AFRICA
AB From 1995 to 1998, we tracked movements of adult Swainson's Hawks (Buteo swainsoni), using satellite telemetry to characterize migration, important stopover areas, and movements in the austral summer. We tagged 46 hawks from July to September on their nesting grounds in seven U.S. states and two Canadian provinces. Swainson's Hawks followed three basic routes south on a broad front, converged along the east coast of central Mexico, and followed a concentrated corridor to a communal area in central Argentina for the austral summer. North of 20 degrees N, southward and northward tracks differed little for individuals from east of the continental divide but differed greatly (up to 1700 km) for individuals from west of the continental divide. Hawks left the breeding grounds mid-August to mid-October; departure dates did not differ by location, year, or sex. Southbound migration lasted 42 to 98 days, northbound migration 51 to 82 days. Southbound, 36% of the Swainson's Hawks departed the nesting grounds nearly 3 weeks earlier than the other radio-marked hawks and made stopovers 9.0-26.0 days long in seven separate areas, mainly in the southern Great Plains, southern Arizona and New Mexico, and north-central Mexico. The birds stayed in their nonbreeding range for 76 to 128 days. All used a core area in central Argentina within 23% of the 738 800-km(2) austral summer range, where they frequently moved long distances (up to 1600 km). Conservation of Swainson's Hawks must be an international effort that considers habitats used during nesting and non-nesting seasons, including migration stopovers.
C1 [Kochert, Michael N.; Fuller, Mark R.; Schueck, Linda S.] US Geol Survey, Forest & Rangeland Ecosyt Sci Ctr, Snake River Field Stn, Boise, ID 83706 USA.
[Bond, Laura] Boise State Univ, Dept Biol, Boise, ID 83725 USA.
[Bechard, Marc J.; Woodbridge, Brian] Boise State Univ, Raptor Res Ctr, Boise, ID 83725 USA.
US Fish & Wildlife Serv, Yreka Fish & Wildlife Off, Yreka, CA 96097 USA.
[Holroyd, Geoff L.; Banasch, Ursula] Environm Canada, Edmonton, AB T6B 2X3, Canada.
[Martell, Mark S.] Univ Minnesota, Raptor Ctr, St Paul, MN 55125 USA.
RP Kochert, MN (reprint author), US Geol Survey, Forest & Rangeland Ecosyt Sci Ctr, Snake River Field Stn, Boise, ID 83706 USA.
EM mkochert@usgs.gov
FU U.S. Forest Service; U.S. Fish and Wildlife Service; U.S. Department of
the Army; U.S. Geological Survey; National Biological Service; Canadian
Wildlife Service; Boise State University; Arizona Department of Game and
Fish; Minnesota Department of Natural Resources; Oregon Department of
Fish and Wildlife; Novartis Pesticide Division; American Cyanamid;
American Bird Conservancy; National Fish and Wildlife Foundation
FX This paper is a contribution of the U.S. Geological Survey, Forest and
Rangeland Ecosystem Science Center. Major funding came from U.S. Forest
Service, U.S. Fish and Wildlife Service, U.S. Department of the Army,
U.S. Geological Survey, National Biological Service, Canadian Wildlife
Service, Boise State University, Arizona Department of Game and Fish,
Minnesota Department of Natural Resources, Oregon Department of Fish and
Wildlife, Novartis Pesticide Division, and American Cyanamid. The
American Bird Conservancy and National Fish and Wildlife Foundation also
provided support. J. McKinley, S. Houston, D. Matiatos, R. Glinski, T.
Maechtle, and Hawkwatch International staff trapped and instrumented
most of the Swainson's Hawks. R. Glinski, M. Henjem, S. Houston, and D.
Matiatos coordinated field activities. M. Leu advised and assisted on
some statistical analyses, and K. Steenhof, D. Douglas, J. Erickson, P.
Kochert, C. McIntyre, and an anonymous reviewer provided comments and
suggestions that greatly improved the manuscript. Any use of trade,
product, or firm names is for descriptive purposes only and does not
imply endorsement by the U.S. government.
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PU COOPER ORNITHOLOGICAL SOC
PI LAWRENCE
PA ORNITHOLOGICAL SOC NORTH AMER PO BOX 1897, LAWRENCE, KS 66044-8897 USA
SN 0010-5422
EI 1938-5129
J9 CONDOR
JI Condor
PD FEB
PY 2011
VL 113
IS 1
BP 89
EP 106
DI 10.1525/cond.2011.090243
PG 18
WC Ornithology
SC Zoology
GA 739RT
UT WOS:000288736400010
PM 26380528
ER
PT J
AU Hamilton, CD
Golightly, RT
Takekawa, JY
AF Hamilton, Christine D.
Golightly, Richard T.
Takekawa, John Y.
TI RELATIONSHIPS BETWEEN BREEDING STATUS, SOCIAL-CONGREGATION ATTENDANCE,
AND FORAGING DISTANCE OF XANTUS'S MURRELETS
SO CONDOR
LA English
DT Article
DE California Channel Islands; foraging; radio telemetry; Synthliboramphus
hypoleucus; Xantus's Murrrelet
ID AUKLETS PTYCHORAMPHUS-ALEUTICUS; SOUTHERN CALIFORNIA BIGHT;
CHANNEL-ISLANDS; HOME-RANGE; SEA; DIET
AB At night during the breeding season, Xantus's Murrelets (Synthliboramphus hypoleucus) congregate on the water adjacent to nesting colonies. We examined relationships of attendance at these nocturnal congregations, breeding status, and daytime foraging locations of radio-marked Xantus's Murrelets from Anacapa Island (33 in 2002, 44 in 2003) and Santa Barbara Island (35 in 2002) in the California Channel Islands. Murrelets that spent more nights attending congregations were located closer to the island during the day, so regular attendance at the congregations may have constrained daytime traveling distances to foraging locations. In mid-May 2003 home-range sizes increased while congregation attendance decreased, likely indicating the end of colony attendance and declining availability of prey near Anacapa Island. In both years, incubating murrelets foraged farther from the colony than did nonbreeding murrelets, suggesting that breeding and nonbreeding murrelets use different foraging strategies to meet their energetic requirements.
C1 [Hamilton, Christine D.] HT Harvey & Associates, Arcata, CA 95521 USA.
[Golightly, Richard T.] Humboldt State Univ, Dept Wildlife, Arcata, CA 95521 USA.
[Takekawa, John Y.] US Geol Survey, Western Ecol Res Ctr, San Francisco Bay Estuary Field Stn, Vallejo, CA 94592 USA.
RP Hamilton, CD (reprint author), HT Harvey & Associates, 1125 16th St,Suite 209, Arcata, CA 95521 USA.
EM chamilton@harveyecology.com
FU U.S. Geological Survey Western Ecological Research Center (Dixon and San
Francisco Bay Estuary Field Station); Minerals Management Service
(Pacific Outer Shelf Region); U.S. Navy (Naval Air Station, Point Mugu);
Humboldt State University (HSU); California Department of Fish and Game
(CDFG; Habitat Conservation Planning Branch); CHINP vessel Pacific
Ranger
FX We thank J. Ackerman, H. Carter, M. Colwell, D. Goley, W. McIver, D.
Whitworth, K. Phillips, and R. Kirby for providing valuable comments and
editorial assistance on the manuscript. We especially thank H. Carter
for his advice and involvement in developing the project. Funding and
in-kind support were provided by the U.S. Geological Survey Western
Ecological Research Center (Dixon and San Francisco Bay Estuary Field
Station), Minerals Management Service (Pacific Outer Shelf Region), U.S.
Navy (Naval Air Station, Point Mugu, Legacy Resources Management
Program), Humboldt State University (HSU), and California Department of
Fish and Game (CDFG; Habitat Conservation Planning Branch). Aircraft
were provided by CDFG Air Services (J. Veal and T. Evans) and Aspen
Helicopters. Logistical support was provided by Channel Islands National
Park (CHINP; T. Hofstra, P. Martin, and K. Faulkner). Capture of
murrelets was supported by CHINP vessel Pacific Ranger (captain B.
Wilson). Biologists assisting with field research included J. Ackerman,
J. Adams, H. Carter, E. Craig, E. Creel, G. Howald, J. Mason, W. McIver,
S. Newman, D. Orthmeyer, C. Short, R. Young, and D. Whitworth. Research
was conducted with permits from HSU (Institutional Animal Care and Use
Committee protocol 01/02.W.106.A), U.S. Geological Survey (banding
permit 22911), CHINP (research permit CHIS-2003-SCI-0005), and CDFG
(scientific collecting permit 000392). Any use of trade, product, or
firm names in this publication is for descriptive purposes only and does
not imply endorsement by the U.S. government.
NR 42
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PU COOPER ORNITHOLOGICAL SOC
PI LAWRENCE
PA ORNITHOLOGICAL SOC NORTH AMER PO BOX 1897, LAWRENCE, KS 66044-8897 USA
SN 0010-5422
EI 1938-5129
J9 CONDOR
JI Condor
PD FEB
PY 2011
VL 113
IS 1
BP 140
EP 149
DI 10.1525/cond.2011.100040
PG 10
WC Ornithology
SC Zoology
GA 739RT
UT WOS:000288736400014
ER
PT J
AU Glenn, EM
Anthony, RG
Forsman, ED
Olson, GS
AF Glenn, Elizabeth M.
Anthony, Robert G.
Forsman, Eric D.
Olson, Gail S.
TI LOCAL WEATHER, REGIONAL CLIMATE, AND ANNUAL SURVIVAL OF THE NORTHERN
SPOTTED OWL
SO CONDOR
LA English
DT Article
DE Strix occidentalis caurina; weather; climate; annual survival; Spotted
Owl
ID REPRODUCTIVE SUCCESS; DEMOGRAPHIC PERFORMANCE; POPULATION-DYNAMICS;
TEMPORAL VARIATION; VOLE POPULATIONS; ADULT SURVIVAL; WESTERN OREGON;
HABITAT; IMPACT; OCCIDENTALIS
AB We used an information-theoretical approach and Cormack-Jolly-Seber models for open populations in program MARK to examine relationships between survival rates of Northern Spotted Owls and a variety of local weather variables and long-term climate variables. In four of the six populations examined, survival was positively associated with wetter than normal conditions during the growing season or high summer temperatures. At the three study areas located at the highest elevations, survival was positively associated with winter temperature but also had a negative or quadratic relation with the number of storms and winter precipitation. A meta-analysis of all six areas combined indicated that annual survival was most strongly associated with phase shifts in the Southern Oscillation and Pacific Decadal Oscillation, which reflect large-scale temperature and precipitation patterns in this region. Climate accounted for a variable amount (1-41%) of the total process variation in annual survival but for more year-to-year variation (3-66%) than did spatial variation among owl territories (0-7%). Negative associations between survival and cold, wet winters and nesting seasons were similar to those found in other studies of the Spotted Owl. The relationships between survival and growing-season precipitation and regional climate patterns, however, had not been reported for this species previously. Climate-change models for the first half of the 21st century predict warmer, wetter winters and hotter, drier summers for the Pacific Northwest. Our results indicate that these conditions could decrease Spotted Owl survival in some areas.
C1 [Glenn, Elizabeth M.; Olson, Gail S.] Oregon State Univ, Dept Fisheries & Wildlife, Corvallis, OR 97331 USA.
[Anthony, Robert G.] Oregon State Univ, Dept Fisheries & Wildlife, Oregon Cooperat Wildlife Res Unit, US Geol Survey, Corvallis, OR 97331 USA.
[Forsman, Eric D.] US Forest Serv, USDA, Pacific NW Res Stn, Forestry Sci Lab, Corvallis, OR 97330 USA.
RP Glenn, EM (reprint author), US Fish & Wildlife Serv, 2600 SE 98th Ave,Suite 100, Portland, OR 97266 USA.
EM betsy_glenn@fws.gov
FU Forest Service of the U.S. Department of Agriculture; Bureau of Land
Management, National Park Service; Fish and Wildlife Service of the U.S.
Department of the Interior; National Science Foundation
FX Our research was funded by the Forest Service of the U.S. Department of
Agriculture, the Bureau of Land Management, National Park Service, and
Fish and Wildlife Service of the U.S. Department of the Interior, and a
pre-doctoral fellowship to Glenn from the National Science Foundation.
We are especially indebted to the many crew leaders and field biologists
who collected the demographic data. Review comments from C. Periera and
G. Taylor of Oregon State University helped us to improve the manuscript
greatly.
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U2 39
PU COOPER ORNITHOLOGICAL SOC
PI LAWRENCE
PA ORNITHOLOGICAL SOC NORTH AMER PO BOX 1897, LAWRENCE, KS 66044-8897 USA
SN 0010-5422
J9 CONDOR
JI Condor
PD FEB
PY 2011
VL 113
IS 1
BP 159
EP 176
DI 10.1525/cond.2011.100118
PG 18
WC Ornithology
SC Zoology
GA 739RT
UT WOS:000288736400016
ER
PT J
AU Bhattacharya, T
Beach, T
Wahl, D
AF Bhattacharya, Tripti
Beach, Timothy
Wahl, David
TI An analysis of modern pollen rain from the Maya lowlands of northern
Belize
SO REVIEW OF PALAEOBOTANY AND PALYNOLOGY
LA English
DT Article
DE Maya lowlands; modern pollen; vegetation; Belize; Neotropics
ID CLIMATE-CHANGE; FOREST; GUATEMALA; HOLOCENE; PETEN; REPRESENTATION;
CIVILIZATION; COMMUNITIES; PLEISTOCENE; SPECTRA
AB In the lowland Maya area, pollen records provide important insights into the impact of past human populations and climate change on tropical ecosystems. Despite a long history of regional paleoecological research, few studies have characterized the palynological signatures of lowland ecosystems, a fact which lowers confidence in ecological inferences made from palynological data. We sought to verify whether we could use pollen spectra to reliably distinguish modern ecosystem types in the Maya lowlands of Central America. We collected 23 soil and sediment samples from eight ecosystem types, including upland, riparian, secondary, and swamp (bajo) forests; pine savanna; and three distinct wetland communities. We analyzed pollen spectra with non-metric multidimensional scaling (NMDS), and found significant compositional differences in ecosystem types' pollen spectra. Forested sites had spectra dominated by Moraceae/Urticaceae pollen, while non-forested sites had significant portions of Poaceae, Asteraceae, and Amaranthaceae pollen. Upland, bajo, and riparian forest differed in representation of Cyperaceae, Bactris-type, and Combretaceae/Melastomataceae pollen. High percentages of pine (Pinus), oak (Quercus), and the presence of Byrsonima characterized pine savanna. Despite its limited sample size, this study provides one of the first statistical analyses of modem pollen rain in the Maya lowlands. Our results show that pollen assemblages can accurately reflect differences between ecosystem types, which may help refine interpretations of pollen records from the Maya area. (C) 2010 Elsevier B.V. All rights reserved.
C1 [Bhattacharya, Tripti; Beach, Timothy] Georgetown Univ, Washington, DC 20057 USA.
[Wahl, David] US Geol Survey, Menlo Pk, CA 94025 USA.
RP Bhattacharya, T (reprint author), Univ Calif Berkeley, Dept Geog, 107 McCone Hall, Berkeley, CA 94720 USA.
EM tripti@berkeley.edu
OI Wahl, David/0000-0002-0451-3554; Bhattacharya,
Tripti/0000-0002-5528-3760
FU Georgetown University
FX We thank Deb Willard, Christopher Bernhardt, Tom Sheehan (U.S.
Geological Survey), and Roger Byrne (U.C. Berkeley) for their help with
pollen identification and laboratory techniques. Gina Wimp (Georgetown
University) provided invaluable statistical advice, and Sheryl
Luzzadder-Beach (George Mason University) provided field support and
help revising this manuscript. We thank Nick Brokaw (University of
Puerto Rico) for his insights on the region's ecology and forest
composition, and Darin Jensen (UC Berkeley) for his cartographic
insights. Caitlin Karniski and Grayson Badgley provided field
assistance. We also thank the Maya Research Program, the Programme for
Belize, and the communities of Blue Creek and San Felipe for their
continued support of our fieldwork. This research was funded by the
Georgetown University Research Opportunities Program. We thank Henry
Hooghiemstra, A.F. Lotter, and an anonymous reviewer for comments that
greatly improved this manuscript.
NR 77
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PU ELSEVIER SCIENCE BV
PI AMSTERDAM
PA PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS
SN 0034-6667
EI 1879-0615
J9 REV PALAEOBOT PALYNO
JI Rev. Palaeobot. Palynology
PD FEB
PY 2011
VL 164
IS 1-2
BP 109
EP 120
DI 10.1016/j.revpalbo.2010.11.010
PG 12
WC Plant Sciences; Paleontology
SC Plant Sciences; Paleontology
GA 736EA
UT WOS:000288472200009
ER
PT J
AU Sleeter, BM
Wilson, TS
Soulard, CE
Liu, JX
AF Sleeter, Benjamin M.
Wilson, Tamara S.
Soulard, Christopher E.
Liu, Jinxun
TI Estimation of late twentieth century land-cover change in California
SO ENVIRONMENTAL MONITORING AND ASSESSMENT
LA English
DT Article
DE Land cover; Land use; California; Change; Trends
ID CONTERMINOUS UNITED-STATES; CARBON; ECOREGIONS; TRENDS; PERSPECTIVES;
DYNAMICS; CLIMATE
AB We present the first comprehensive multi-temporal analysis of land-cover change for California across its major ecological regions and primary land-cover types. Recently completed satellite-based estimates of land-cover and land-use change information for large portions of the United States allow for consistent measurement and comparison across heterogeneous landscapes. Landsat data were employed within a pure-panel stratified one-stage cluster sample to estimate and characterize land-cover change for 1973-2000. Results indicate anthropogenic and natural disturbances, such as forest cutting and fire, were the dominant changes, followed by large fluctuations between agriculture and rangelands. Contrary to common perception, agriculture remained relatively stable over the 27-year period with an estimated loss of 1.0% of agricultural land. The largest net declines occurred in the grasslands/shrubs class at 5,131 km(2) and forest class at 4,722 km2. Developed lands increased by 37.6%, composing an estimated 4.2% of the state's land cover by 2000.
C1 [Sleeter, Benjamin M.; Wilson, Tamara S.; Soulard, Christopher E.] US Geol Survey, Western Geog Sci Ctr, Menlo Pk, CA 94025 USA.
[Liu, Jinxun] Stinger Ghallarian Technol SGT Inc, US Geol Survey, Earth Resources Observat & Sci EROS Ctr, Sioux Falls, SD 57198 USA.
RP Sleeter, BM (reprint author), US Geol Survey, Western Geog Sci Ctr, Menlo Pk, CA 94025 USA.
EM bsleeter@usgs.gov; tswilson@usgs.gov; csoulard@usgs.gov; jxliu@usgs.gov
OI Soulard, Christopher/0000-0002-5777-9516
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PU SPRINGER
PI DORDRECHT
PA VAN GODEWIJCKSTRAAT 30, 3311 GZ DORDRECHT, NETHERLANDS
SN 0167-6369
J9 ENVIRON MONIT ASSESS
JI Environ. Monit. Assess.
PD FEB
PY 2011
VL 173
IS 1-4
BP 251
EP 266
DI 10.1007/s10661-010-1385-8
PG 16
WC Environmental Sciences
SC Environmental Sciences & Ecology
GA 729VY
UT WOS:000287982000021
PM 20217217
ER
PT J
AU Walter, WD
Walsh, DP
Farnsworth, ML
Winkelman, DL
Miller, MW
AF Walter, W. David
Walsh, Daniel P.
Farnsworth, Matthew L.
Winkelman, Dana L.
Miller, Michael W.
TI Soil clay content underlies prion infection odds
SO NATURE COMMUNICATIONS
LA English
DT Article
ID CHRONIC WASTING DISEASE; MULE DEER; SCRAPIE; EPIDEMIOLOGY; TRANSMISSION;
SHEEP; CONVERGENCE; PROTEIN; ENVIRONMENT; INGESTION
AB Environmental factors-especially soil properties-have been suggested as potentially important in the transmission of infectious prion diseases. Because binding to montmorillonite (an aluminosilicate clay mineral) or clay-enriched soils had been shown to enhance experimental prion transmissibility, we hypothesized that prion transmission among mule deer might also be enhanced in ranges with relatively high soil clay content. In this study, we report apparent influences of soil clay content on the odds of prion infection in free-ranging deer. Analysis of data from prion-infected deer herds in northern Colorado, USA, revealed that a 1% increase in the clay-sized particle content in soils within the approximate home range of an individual deer increased its odds of infection by up to 8.9%. Our findings suggest that soil clay content and related environmental properties deserve greater attention in assessing risks of prion disease outbreaks and prospects for their control in both natural and production settings.
C1 [Walsh, Daniel P.; Miller, Michael W.] Colorado Div Wildlife, Wildlife Res Ctr, Ft Collins, CO 80526 USA.
[Walter, W. David; Winkelman, Dana L.] US Geol Survey, US Dept Interior, Colorado Cooperat Fish & Wildlife Res Unit, Ft Collins, CO 80523 USA.
[Farnsworth, Matthew L.] Vet Serv, USDA, Anim & Plant Hlth Inspect Serv, Ctr Epidemiol & Anim Hlth, Ft Collins, CO 80526 USA.
RP Miller, MW (reprint author), Colorado Div Wildlife, Wildlife Res Ctr, Ft Collins, CO 80526 USA.
EM mike.miller@state.co.us
RI Ducey, Thomas/A-6493-2011;
OI Walsh, Daniel/0000-0002-7772-2445
FU Colorado Division of Wildlife; US Geological Survey; US Department of
Agriculture (USDA) Animal and Plant Health Inspection Service-Veterinary
Services (APHIS-VS); State Agricultural Experiment Station; Cooperative
State Research, Education and Extension Service under USDA
FX We thank the Colorado Division of Wildlife, US Geological Survey, US
Department of Agriculture (USDA) Animal and Plant Health Inspection
Service-Veterinary Services (APHIS-VS) and the State Agricultural
Experiment Station in partnership with the Cooperative State Research,
Education and Extension Service under the USDA for providing funding and
support for this research. We thank the many hunters, volunteers and
staff who helped to gather deer samples and data, and also thank R.
Miller, L. Creekmore and others for access to USDA data layers, and D.
Noe for consulting on Colorado soil clay geology and mineralogy.
Thumbnail image by D. W. Miller.
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PU NATURE PUBLISHING GROUP
PI LONDON
PA MACMILLAN BUILDING, 4 CRINAN ST, LONDON N1 9XW, ENGLAND
SN 2041-1723
J9 NAT COMMUN
JI Nat. Commun.
PD FEB
PY 2011
VL 2
AR 200
DI 10.1038/ncomms1203
PG 6
WC Multidisciplinary Sciences
SC Science & Technology - Other Topics
GA 732YP
UT WOS:000288225900029
ER
PT J
AU Moridis, GJ
Collett, TS
Pooladi-Darvish, M
Hancock, S
Santamarina, C
Boswell, R
Kneafsey, T
Rutqvist, J
Kowalsky, MB
Reagan, MT
Sloan, ED
Sum, AK
Koh, CA
AF Moridis, G. J.
Collett, T. S.
Pooladi-Darvish, M.
Hancock, S.
Santamarina, C.
Boswell, R.
Kneafsey, T.
Rutqvist, J.
Kowalsky, M. B.
Reagan, M. T.
Sloan, E. D.
Sum, A. K.
Koh, C. A.
TI Challenges, Uncertainties, and Issues Facing Gas Production From
Gas-Hydrate Deposits
SO SPE RESERVOIR EVALUATION & ENGINEERING
LA English
DT Article
ID GULF-OF-MEXICO; METHANE HYDRATE; THERMAL-CONDUCTIVITY; POROUS-MEDIA;
BEARING SEDIMENTS; MARINE-SEDIMENTS; DISSOCIATION CHARACTERISTICS;
MACKENZIE DELTA; WAVE VELOCITIES; WATER
AB The current paper complements the Moridis et al. (2009) review of the status of the effort toward commercial gas production from hydrates. We aim to describe the concept of the gas-hydrate (GH) petroleum system; to discuss advances, requirements, and suggested practices in GH prospecting and GH deposit characterization; and to review the associated technical, economic, and environmental challenges and uncertainties, which include the following: accurate assessment of producible fractions of the GH resource; development of methods for identifying suitable production targets; sampling of hydrate-bearing sediments (HBS) and sample analysis; analysis and interpretation of geophysical surveys of GH reservoirs; well-testing methods; interpretation of well-testing results; geomechanical and reservoir/well stability concerns; well design, operation, and installation; field operations and extending production beyond sand-dominated GH reservoirs; monitoring production and geomechanical stability; laboratory investigations; fundamental knowledge of hydrate behavior; the economics of commercial gas production from hydrates; and associated environmental concerns.
C1 [Moridis, G. J.; Kowalsky, M. B.] Lawrence Berkeley Natl Lab, Div Earth Sci, Hydrologeol Dept, Berkeley, CA USA.
[Collett, T. S.] US Geol Survey, Geol Div, Menlo Pk, CA USA.
[Pooladi-Darvish, M.] Fekete Associates, Calgary, AB, Canada.
[Pooladi-Darvish, M.] Univ Calgary, Calgary, AB T2N 1N4, Canada.
[Hancock, S.] RPS Grp, Menlo Pk, CA USA.
[Santamarina, C.] Georgia Inst Technol, Sch Civil & Environm Engn, Atlanta, GA 30332 USA.
[Boswell, R.] US DOE, GH Res Program, Natl Energy Technol Lab, Morgantown, WV USA.
[Sloan, E. D.] Colorado Sch Mines, Ctr Hydrate Res, Golden, CO 80401 USA.
[Sum, A. K.; Koh, C. A.] Colorado Sch Mines, Dept Chem Engn, Golden, CO 80401 USA.
RP Moridis, GJ (reprint author), Lawrence Berkeley Natl Lab, Div Earth Sci, Hydrologeol Dept, Berkeley, CA USA.
EM mpooladi-darvish@fekete.com; jcs@gatech.edu; Ray.Boswell@NETL.DOE.GOV;
JRutqvist@lbl.gov; mtreagan@lbl.gov; asum@mines.edu; ckoh@mines.edu
RI Kneafsey, Timothy/H-7412-2014; Rutqvist, Jonny/F-4957-2015; Reagan,
Matthew/D-1129-2015
OI Kneafsey, Timothy/0000-0002-3926-8587; Rutqvist,
Jonny/0000-0002-7949-9785; Reagan, Matthew/0000-0001-6225-4928
FU Assistant Secretary for Fossil Energy, Office of Natural Gas and
Petroleum Technology, through the National Energy Technology Laboratory,
under the US DOE [DE-AC02-05CH11231]
FX The contributions of G.J. Moridis, T. Kneafsey, J. Rutqvist, M.B.
Kowalsky, and M.T. Reagan were supported by the Assistant Secretary for
Fossil Energy, Office of Natural Gas and Petroleum Technology, through
the National Energy Technology Laboratory, under the US DOE, Contract
No. DE-AC02-05CH11231. The authors are indebted to Stefan Finsterle,
John Apps, and Dan Hawkes for their insightful comments.
NR 233
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PU SOC PETROLEUM ENG
PI RICHARDSON
PA 222 PALISADES CREEK DR,, RICHARDSON, TX 75080 USA
SN 1094-6470
EI 1930-0212
J9 SPE RESERV EVAL ENG
JI SPE Reserv. Eval. Eng.
PD FEB
PY 2011
VL 14
IS 1
BP 76
EP 112
PG 37
WC Energy & Fuels; Engineering, Petroleum; Geosciences, Multidisciplinary
SC Energy & Fuels; Engineering; Geology
GA 727HX
UT WOS:000287790300006
ER
PT J
AU McGowan, CP
Ryan, MR
Runge, MC
Millspaugh, JJ
Cochrane, JF
AF McGowan, Conor P.
Ryan, Mark R.
Runge, Michael C.
Millspaugh, Joshua J.
Cochrane, Jean Fitts
TI The role of demographic compensation theory in incidental take
assessments for endangered species
SO BIOLOGICAL CONSERVATION
LA English
DT Article
DE Endangered species; Compensation; Piping plover; Charadrius melodus;
Population modeling
ID PIPING PLOVERS; WATERFOWL POPULATIONS; DENSITY-DEPENDENCE; GREAT-PLAINS;
SURVIVAL; MORTALITY; VIABILITY; UNCERTAINTY; MANAGEMENT; SIMULATION
AB Many endangered species laws provide exceptions to legislated prohibitions through incidental take provisions as long as take is the result of unintended consequences of an otherwise legal activity. These allowances presumably invoke the theory of demographic compensation, commonly applied to harvested species, by allowing limited harm as long as the probability of the species' survival or recovery is not reduced appreciably. Demographic compensation requires some density-dependent limits on survival or reproduction in a species' annual cycle that can be alleviated through incidental take. Using a population model for piping plovers in the Great Plains, we found that when the population is in rapid decline or when there is no density dependence, the probability of quasi-extinction increased linearly with increasing take. However, when the population is near stability and subject to density-dependent survival, there was no relationship between quasi-extinction probability and take rates. We note however, that a brief examination of piping plover demography and annual cycles suggests little room for compensatory capacity. We argue that a population's capacity for demographic compensation of incidental take should be evaluated when considering incidental allowances because compensation is the only mechanism whereby a population can absorb the negative effects of take without incurring a reduction in the probability of survival in the wild. With many endangered species there is probably little known about density dependence and compensatory capacity. Under these circumstances, using multiple system models (with and without compensation) to predict the population's response to incidental take and implementing follow-up monitoring to assess species response may be valuable in increasing knowledge and improving future decision making. Published by Elsevier Ltd.
C1 [McGowan, Conor P.; Ryan, Mark R.; Millspaugh, Joshua J.] Univ Missouri, Dept Fisheries & Wildlife Sci, Columbia, MO 65211 USA.
[McGowan, Conor P.; Runge, Michael C.; Cochrane, Jean Fitts] USGS Patuxent Wildlife Res Ctr, Laurel, MD 20708 USA.
RP McGowan, CP (reprint author), Auburn Univ, US Geol Survey, Alabama Cooperat Fish & Wildlife Res Unit, Sch Forestry & Wildlife Sci, Auburn, AL 36849 USA.
EM cmcgowan@usgs.gov
RI Runge, Michael/E-7331-2011
OI Runge, Michael/0000-0002-8081-536X
FU USFWS; USGS
FX We thank: The USFWS and the USGS for supporting this work financially;
B. Gardner for assistance with R code; M. Larson, J.E. Lyons, S. Rikoon,
F.R. Thompson III, and E. Zipkin for reviewing and helping to improve
earlier versions of this manuscript; The editors and anonymous reviewers
of this paper for their constructive input and efforts to improve this
paper. Use of product or firm names does not imply endorsement by the US
Government.
NR 54
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PU ELSEVIER SCI LTD
PI OXFORD
PA THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, OXON, ENGLAND
SN 0006-3207
J9 BIOL CONSERV
JI Biol. Conserv.
PD FEB
PY 2011
VL 144
IS 2
BP 730
EP 737
DI 10.1016/j.biocon.2010.10.020
PG 8
WC Biodiversity Conservation; Ecology; Environmental Sciences
SC Biodiversity & Conservation; Environmental Sciences & Ecology
GA 728TJ
UT WOS:000287897100012
ER
PT J
AU Zeller, KA
Nijhawan, S
Salom-Perez, R
Potosme, SH
Hines, JE
AF Zeller, Katherine A.
Nijhawan, Sahil
Salom-Perez, Roberto
Potosme, Sandra H.
Hines, James E.
TI Integrating occupancy modeling and interview data for corridor
identification: A case study for jaguars in Nicaragua
SO BIOLOGICAL CONSERVATION
LA English
DT Article
DE Panthera onca; Connectivity; Conservation planning;
Detection/non-detection; Detection probability; Interviews
ID ESTIMATING SITE OCCUPANCY; PANTHERA-ONCA; SPECIES OCCURRENCE; MULTIPLE
STATES; HABITAT USE; CONSERVATION; INDIA; UNCERTAINTY; PECCARIES;
ABUNDANCE
AB Corridors are critical elements in the long-term conservation of wide-ranging species like the jaguar (Pantheta onca). Jaguar corridors across the range of the species were initially identified using a GIS-based least-cost corridor model. However, due to inherent errors in remotely sensed data and model uncertainties, these corridors warrant field verification before conservation efforts can begin. We developed a novel corridor assessment protocol based on interview data and site occupancy modeling. We divided our pilot study area, in southeastern Nicaragua, into 71, 6 x 6 km sampling units and conducted 160 structured interviews with local residents. Interviews were designed to collect data on jaguar and seven prey species so that detection/non-detection matrices could be constructed for each sampling unit. Jaguars were reportedly detected in 57% of the sampling units and had a detection probability of 28%. With the exception of white-lipped peccary, prey species were reportedly detected in 82-100% of the sampling units. Though the use of interview data may violate some assumptions of the occupancy modeling approach for determining 'proportion of area occupied', we countered these shortcomings through study design and interpreting the occupancy parameter, psi, as 'probability of habitat used'. Probability of habitat use was modeled for each target species using single state or multistate models. A combination of the estimated probabilities of habitat use for jaguar and prey was selected to identify the final jaguar corridor. This protocol provides an efficient field methodology for identifying corridors for easily-identifiable species, across large study areas comprised of unprotected, private lands. (c) 2010 Elsevier Ltd. All rights reserved.
C1 [Zeller, Katherine A.; Nijhawan, Sahil; Salom-Perez, Roberto; Potosme, Sandra H.] Panthera, New York, NY 10018 USA.
[Hines, James E.] USGS Patuxent Wildlife Res Ctr, Laurel, MD 20708 USA.
RP Zeller, KA (reprint author), Panthera, 8 W 40th St, New York, NY 10018 USA.
EM kzeller@panthera.org
FU Wildlife Conservation Society; Liz Claiborne and Art Ortenberg
Foundation; Environmental Systems Research Institute, Inc.; United
States Department of State; T. Kaplan and Panthera
FX We are grateful to the Wildlife Conservation Society, the Liz Claiborne
and Art Ortenberg Foundation, Environmental Systems Research Institute,
Inc., the United States Department of State, and T. Kaplan and Panthera
for funding and support of this work. We would also like to thank J.D.
Nichols for his input in the protocol development, and J. Smith, L
Hunter, H. Quigley, M. Linkie and the journal reviewers for critical
review of this manuscript. We are indebted to A. Rabinowitz for his
jaguar corridor vision and encouragement, J. Polisar for valuable input
during the early stages of this work, and F. Diaz and L. Maffei for
their assistance in the field.
NR 57
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PU ELSEVIER SCI LTD
PI OXFORD
PA THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, OXON, ENGLAND
SN 0006-3207
J9 BIOL CONSERV
JI Biol. Conserv.
PD FEB
PY 2011
VL 144
IS 2
BP 892
EP 901
DI 10.1016/j.biocon.2010.12.003
PG 10
WC Biodiversity Conservation; Ecology; Environmental Sciences
SC Biodiversity & Conservation; Environmental Sciences & Ecology
GA 728TJ
UT WOS:000287897100030
ER
PT J
AU Varian-Ramos, CW
Condon, AM
Hallinger, KK
Carlson-Drexler, KA
Cristol, DA
AF Varian-Ramos, Claire W.
Condon, Anne M.
Hallinger, Kelly K.
Carlson-Drexler, Kjarstin A.
Cristol, Daniel A.
TI Stability of Mercury Concentrations in Frozen Avian Blood Samples
SO BULLETIN OF ENVIRONMENTAL CONTAMINATION AND TOXICOLOGY
LA English
DT Article
DE Avian blood; Temporal stability; Mercury; Tissue storage
ID BIOLOGICAL-MATERIALS; WHOLE-BLOOD; STORAGE; METHYLMERCURY; LEVEL
AB It is unclear whether mercury concentration in wildlife tissues changes appreciably after lengthy frozen storage. To test whether such freezer-archived samples are stable, small (similar to 10-50 mu L) avian blood samples stored in capped glass capillary tubes were analyzed for total mercury concentration, and then reanalyzed after being frozen for up to 3 years. Mercury concentrations increased 6% on average over the 3 year period, but time spent frozen explained only 11% of the variation between measurements. This small amount of change suggests that archived blood samples remain useful for at least several years.
C1 [Varian-Ramos, Claire W.; Hallinger, Kelly K.; Carlson-Drexler, Kjarstin A.; Cristol, Daniel A.] Coll William & Mary, Dept Biol, Williamsburg, VA 23187 USA.
[Condon, Anne M.] US Fish & Wildlife Serv, Gloucester, VA 23061 USA.
RP Varian-Ramos, CW (reprint author), Coll William & Mary, Dept Biol, POB 8795, Williamsburg, VA 23187 USA.
EM cwramos@wm.edu
FU E. I. DuPont de Nemours and Company; Office of Vice Provost for Research
at the College of William and Mary; National Science Foundation [UBM
0436318]; Howard Hughes Medical Institute
FX We thank the South River Science Team. Funding was provided by E. I.
DuPont de Nemours and Company, The Office of Vice Provost for Research
at the College of William and Mary, National Science Foundation Grant
UBM 0436318, and the William and Mary Undergraduate Science Education
and Research Program sponsored by the Howard Hughes Medical Institute.
NR 13
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PU SPRINGER
PI NEW YORK
PA 233 SPRING ST, NEW YORK, NY 10013 USA
SN 0007-4861
J9 B ENVIRON CONTAM TOX
JI Bull. Environ. Contam. Toxicol.
PD FEB
PY 2011
VL 86
IS 2
BP 159
EP 162
DI 10.1007/s00128-010-0164-0
PG 4
WC Environmental Sciences; Toxicology
SC Environmental Sciences & Ecology; Toxicology
GA 715ZM
UT WOS:000286934500004
PM 21132490
ER
PT J
AU Hayer, CA
Chipps, SR
Stone, JJ
AF Hayer, Cari-Ann
Chipps, Steven R.
Stone, James J.
TI Influence of Physiochemical and Watershed Characteristics on Mercury
Concentration in Walleye, Sander vitreus, M.
SO BULLETIN OF ENVIRONMENTAL CONTAMINATION AND TOXICOLOGY
LA English
DT Article
DE Bioaccumulation; Walleye; Sander vitreus; Mercury; Watershed;
Physiochemical
ID FISH; LAKES; RESERVOIRS; CHEMISTRY
AB Elevated mercury concentration has been documented in a variety of fish and is a growing concern for human consumption. Here, we explore the influence of physiochemical and watershed attributes on mercury concentration in walleye (Sander vitreus, M.) from natural, glacial lakes in South Dakota. Regression analysis showed that water quality attributes were poor predictors of walleye mercury concentration (R-2 = 0.57, p = 0.13). In contrast, models based on watershed features (e.g., lake level changes, watershed slope, agricultural land, wetlands) and local habitat features (i.e., substrate composition, maximum lake depth) explained 81% (p = 0.001) and 80% (p = 0.002) of the variation in walleye mercury concentration. Using an information theoretic approach we evaluated hypotheses related to water quality, physical habitat and watershed features. The best model explaining variation in walleye mercury concentration included local habitat features (W-i = 0.991). These results show that physical habitat and watershed features were better predictors of walleye mercury concentration than water chemistry in glacial lakes of the Northern Great Plains.
C1 [Hayer, Cari-Ann; Chipps, Steven R.] S Dakota State Univ, Dept Wildlife & Fisheries Sci, S Dakota Cooperat Fish & Wildlife Res Unit, US Geol Survey, Brookings, SD 57007 USA.
[Stone, James J.] S Dakota Sch Mines & Technol, Dept Civil & Environm Engn, Rapid City, SD 57701 USA.
RP Hayer, CA (reprint author), S Dakota State Univ, Dept Wildlife & Fisheries Sci, S Dakota Cooperat Fish & Wildlife Res Unit, US Geol Survey, Box 2140B, Brookings, SD 57007 USA.
EM cari-ann.hayer@sdstate.edu
RI Stone, James/E-1524-2013; Hayer, Cari-Ann/C-1319-2009
FU South Dakota Department of Environment and Natural Resources; US
Environmental Protection Agency
FX This research was supported by grants from the South Dakota Department
of Environment and Natural Resources and the US Environmental Protection
Agency (Region 8). We thank Pat Snyder and Shannon Minerich from the SD
DENR for providing data on fish mercury concentration and water quality.
Sam Stukel and Trevor Selch provided information on physical habitat for
the study lakes. We thank Robert Hanten and Jacob Krause for comments on
an earlier draft that greatly improved the manuscript. Any use of trade
names is for descriptive purposes only and does not imply endorsement by
the US Government.
NR 21
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U1 1
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PU SPRINGER
PI NEW YORK
PA 233 SPRING ST, NEW YORK, NY 10013 USA
SN 0007-4861
J9 B ENVIRON CONTAM TOX
JI Bull. Environ. Contam. Toxicol.
PD FEB
PY 2011
VL 86
IS 2
BP 163
EP 167
DI 10.1007/s00128-010-0166-y
PG 5
WC Environmental Sciences; Toxicology
SC Environmental Sciences & Ecology; Toxicology
GA 715ZM
UT WOS:000286934500005
PM 21152888
ER
PT J
AU Tucker, RD
Roig, JY
Delor, C
Amelin, Y
Goncalves, P
Rabarimanana, MH
Ralison, AV
Belcher, RW
AF Tucker, R. D.
Roig, J. -Y.
Delor, C.
Amelin, Y.
Goncalves, P.
Rabarimanana, M. H.
Ralison, A. V.
Belcher, R. W.
TI Neoproterozoic extension in the Greater Dharwar Craton: a reevaluation
of the "Betsimisaraka suture" in Madagascar
SO CANADIAN JOURNAL OF EARTH SCIENCES
LA English
DT Article
ID NORTH-CENTRAL MADAGASCAR; EAST-AFRICAN OROGEN; U-PB AGE; WEST-CENTRAL
MADAGASCAR; SOUTHERN INDIA; ZIRCON GEOCHRONOLOGY; TECTONIC EVOLUTION;
DETRITAL ZIRCON; ID-TIMS; KARNATAKA CRATON
AB The Precambrian shield of Madagascar is reevaluated with recently compiled geological data and new U-Pb sensitive high-resolution ion microprobe (SHRIMP) geochronology. Two Archean domains are recognized: the eastern Antongil-Masora domain and the central Antananarivo domain, the latter with distinctive belts of metamafic gneiss and schist (Tsaratanana Complex). In the eastern domain, the period of early crust formation is extended to the Paleo-Mesoarchean (3.32-3.15 Ga) and a supracrustal sequence (Fenerivo Group), deposited at 3.18 Ga and metamorphosed at 2.55 Ga, is identified. In the central domain, a Neoarchean period of high-grade metamorphism and anatexis that affected both felsic (Betsiboka Suite) and mafic gneisses (Tsaratanana Complex) is documented. We propose, therefore, that the Antananarivo domain was amalgamated within the Greater Dharwar Craton (India + Madagascar) by a Neoarchean accretion event (2.55-2.48 Ga), involving emplacement of juvenile igneous rocks, high-grade metamorphism, and the juxtaposition of disparate belts of mafic gneiss and schist (metagreenstones). The concept of the "Betsimisaraka suture'' is dispelled and the zone is redefined as a domain of Neoproterozoic metasedimentary (Manampotsy Group) and metaigneous rocks (Itsindro-Imorona Suite) formed during a period of continental extension and intrusive igneous activity between 840 and 760 Ma. Younger orogenic convergence (560-520 Ma) resulted in east-directed overthrusting throughout south Madagascar and steepening with local inversion of the domain in central Madagascar. Along part of its length, the Manampotsy Group covers the boundary between the eastern and central Archean domains and is overprinted by the Angavo-Ifanadiana high-strain zone that served as a zone of crustal weakness throughout Cretaceous to Recent times.
C1 [Tucker, R. D.] US Geol Survey, Natl Ctr, Reston, VA 20192 USA.
[Roig, J. -Y.; Delor, C.] Bur Rech Geol & Minieres, F-45060 Orleans 2, France.
[Amelin, Y.] Australian Natl Univ, Res Sch Earth Sci, Canberra, ACT 0200, Australia.
[Goncalves, P.] Univ Franche Comte, UMR 6249, F-25030 Besancon, France.
[Rabarimanana, M. H.; Ralison, A. V.] Project Gouvernance Ressources Minerales, Antananarivo 101, Madagascar.
[Belcher, R. W.] RWB Explorat Ltd, Stockport SK6 2SN, Cheshire, England.
RP Tucker, RD (reprint author), US Geol Survey, Natl Ctr, MS 926A,12201 Sunrise Valley Dr, Reston, VA 20192 USA.
EM rtucker@usgs.gov
RI Goncalves, Philippe/J-8643-2013
OI Goncalves, Philippe/0000-0001-8069-7976
FU Australian National University, Canberra, Australia; National Science
Foundation [EAR-0125957]
FX We gratefully acknowledge the contributions from scientists of the
national consortiums and the supervisory group who contributed ideas and
constructive suggestions to the authors. We acknowledge, in particular,
the Project de Gouvernance des Ressources Minerales (Madagascar) and
Drs. Ortega, Moine, and Rakotomanana, who granted us permission to cite
the Report of the Consultants, and who financed our field work and U-Pb
geochronology (performed at The Australian National University,
Canberra, Australia). Some of our samples were acquired during field
work supported by a National Science Foundation grant, EAR-0125957, to
R. D. T. We also appreciate the comments of reviewers P. Cawood, B.
Moine, J-L Paquette, N. Ratcliffe, and J. Rogers, and Associate Editor
Bill Davis, that substantially improved this manuscript. The ideas in
this article owe their origin to many discussions over the years with
colleagues at the Jack Satterly Laboratory, Royal Ontario Museum,
Toronto, Ontario, who shared openly their insight into the Archean
tectonics of the Superior Craton. Foremost among them was Tom Krogh, our
friend and mentor, who was a source of inspiration to R. D. T. and Y.A.
during their formative years as young scientists. This small
contribution is dedicated to the memory of Tom Krogh and the institution
of scholarly achievement he built in Toronto, Canada.
NR 74
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PU CANADIAN SCIENCE PUBLISHING, NRC RESEARCH PRESS
PI OTTAWA
PA 1200 MONTREAL ROAD, BUILDING M-55, OTTAWA, ON K1A 0R6, CANADA
SN 0008-4077
J9 CAN J EARTH SCI
JI Can. J. Earth Sci.
PD FEB
PY 2011
VL 48
IS 2
BP 389
EP 417
DI 10.1139/E10-034
PG 29
WC Geosciences, Multidisciplinary
SC Geology
GA 726YQ
UT WOS:000287763800016
ER
PT J
AU Allibon, J
Ovtcharova, M
Bussy, F
Cosca, M
Schaltegger, U
Bussien, D
Lewin, E
AF Allibon, James
Ovtcharova, Maria
Bussy, Francois
Cosca, Michael
Schaltegger, Urs
Bussien, Denise
Lewin, Eric
TI Lifetime of an ocean island volcano feeder zone: constraints from U-Pb
dating on coexisting zircon and baddeleyite, and Ar-40/Ar-39 age
determinations, Fuerteventura, Canary Islands
SO CANADIAN JOURNAL OF EARTH SCIENCES
LA English
DT Article
ID SHALLOW-LEVEL MIGMATIZATION; OXYGEN-ISOTOPE RATIOS; TRACE-ELEMENT; BASAL
COMPLEX; K-AR; ID-TIMS; METAMORPHIC ROCKS; HYDROGEN ISOTOPE; CENTRAL
ATLANTIC; RESIDENCE TIMES
AB High-precision isotope dilution - thermal ionization mass spectrometry (ID-TIMS) U-Pb zircon and baddeleyite ages from the PX1 vertically layered mafic intrusion Fuerteventura, Canary Islands, indicate initiation of magma crystallization at 22.10 +/- 0.07 Ma. The magmatic activity lasted a minimum of 0.52 Ma. Ar-40/Ar-39 amphibole dating yielded ages from 21.9 +/- 0.6 to 21.8 +/- 0.3, identical within errors to the U-Pb ages, despite the expected 1% theoretical bias between Ar-40/Ar-39 and U-Pb dates. This overlap could result from (i) rapid cooling of the intrusion (i. e., less than the 0.3 to 0.6 Ma 40Ar/39Ar age uncertainties) from closure temperatures (T-c) of zircon (699-988 degrees C) to amphibole (500-600 degrees C); (ii) lead loss affecting the youngest zircons; or (iii) excess argon shifting the plateau ages towards older values. The combination of the Ar-40/Ar-39 and U/Pb datasets implies that the maximum amount of time PX1 intrusion took to cool below amphibole T-c is 0.8 Ma, suggesting PX1 lifetime of 520 000 to 800 000 Ma. Age disparities among coexisting baddeleyite and zircon (22.10 +/- 0.07/0.08/0.15 Ma and 21.58 +/- 0.15/0.16/0.31 Ma) in a gabbro sample from the pluton margin suggest complex genetic relationships between phases. Baddeleyite is found preserved in plagioclase cores and crystallized early from low silica activity magma. Zircon crystallized later in a higher silica activity environment and is found in secondary scapolite and is found close to calcite veins, in secondary scapolite that recrystallised from plagioclase. close to calcite veins. Oxygen isotope delta O-18 values of altered plagioclase are high (+7.7), indicating interaction with fluids derived from host-rock carbonatites. The coexistence of baddeleyite and zircon is ascribed to interaction of the PX1 gabbro with CO2-rich carbonatite-derived fluids released during contact metamorphism.
C1 [Allibon, James; Bussy, Francois; Bussien, Denise] Univ Lausanne, Inst Mineral & Geochem, CH-1015 Lausanne, Switzerland.
[Allibon, James; Lewin, Eric] Lab Geodynam Chaines Alpines, UMR 5025, F-38000 Grenoble, France.
[Ovtcharova, Maria; Schaltegger, Urs] Univ Geneva, Sect Earth & Environm Sci, CH-1205 Geneva, Switzerland.
[Cosca, Michael] US Geol Survey, Denver Fed Ctr, Denver, CO 80225 USA.
RP Allibon, J (reprint author), Univ Lausanne, Inst Mineral & Geochem, Batiment Anthropole, CH-1015 Lausanne, Switzerland.
EM james.allibon@unil.ch
RI LEWIN, Eric/F-1451-2017
FU Institut de Mineralogie et de Geochimie of the University of Lausanne;
"bourse d'aide a la mobilite" of the Rhone Alpes region (France)
FX With this contribution the authors commemorate the late Tom Krogh, who
taught the senior authors Francois Bussy and Urs Schaltegger how to date
zircon. The authors would like to express their gratitude to Benita
Putlitz, Alexei Ulianov, Mathias Dessimoz, and Laurent Nicod for their
valuable technical support in preparing samples and acquiring data on
the laser ablation - inductively coupled plasma mass spectrometry
(LA-ICP-MS) at the University of Lausanne. The authors are grateful for
the help of Honza Catchpole in acquiring the Raman spectra and to
Rossana Martini for technical support using the SEM at the University of
Geneva. The authors also thank the Cabildo Insular de Fuerteventura for
granting permission to sample in the studied area. This ongoing study
was funded by the Institut de Mineralogie et de Geochimie of the
University of Lausanne and by the "bourse d'aide a la mobilite" of the
Rhone Alpes region (France). This manuscript was greatly improved thanks
to the constructive reviews of R. Mundil and J. Lissenberg as well as W.
Davis, a CJES associate editor.
NR 136
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U1 1
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PU CANADIAN SCIENCE PUBLISHING, NRC RESEARCH PRESS
PI OTTAWA
PA 1200 MONTREAL ROAD, BUILDING M-55, OTTAWA, ON K1A 0R6, CANADA
SN 0008-4077
J9 CAN J EARTH SCI
JI Can. J. Earth Sci.
PD FEB
PY 2011
VL 48
IS 2
BP 567
EP 592
DI 10.1139/E10-032
PG 26
WC Geosciences, Multidisciplinary
SC Geology
GA 726YQ
UT WOS:000287763800024
ER
PT J
AU Duffy, EJ
Beauchamp, DA
AF Duffy, Elisabeth J.
Beauchamp, David A.
TI Rapid growth in the early marine period improves the marine survival of
Chinook salmon (Oncorhynchus tshawytscha) in Puget Sound, Washington
SO CANADIAN JOURNAL OF FISHERIES AND AQUATIC SCIENCES
LA English
DT Article
ID SIZE-SELECTIVE MORTALITY; JUVENILE PACIFIC SALMON; PINK SALMON; COHO
SALMON; BRITISH-COLUMBIA; SMOLT SIZE; ATLANTIC SALMON; SOCKEYE-SALMON;
RIVER; KISUTCH
AB We examined the effect of early marine entry timing and body size on the marine (smolt-to-adult) survival of Puget Sound Chinook salmon ( Oncorhynchus tshawytscha). We used data from coded wire tag release groups of hatchery Chinook salmon to test whether hatchery release date, release size, and size in offshore waters in July and September influenced marine survival. Marine survival was most strongly related to the average body size in July, with larger sizes associated with higher survivals. This relationship was consistent over multiple years (1997-2002), suggesting that mortality after July is strongly size-dependent. Release size and date only slightly improved this relationship, whereas size in September showed little relationship to marine survival. Specifically, fish that experienced the highest marine survivals were released before 25 May and were larger than 17 g ( or 120 mm fork length) by July. Our findings highlight the importance of local conditions in Puget Sound ( Washington, USA) during the spring and summer, and suggest that declines in marine survival since the 1980s may have been caused by reductions in the quality of feeding and growing conditions during early marine life.
C1 [Duffy, Elisabeth J.] Univ Washington, Sch Aquat & Fisheries Sci, Seattle, WA 98195 USA.
[Beauchamp, David A.] Univ Washington, US Geol Survey, Washington Cooperat Fish & Wildlife Res Unit, Sch Aquat & Fisheries Sci, Seattle, WA 98195 USA.
RP Duffy, EJ (reprint author), Univ Washington, Sch Aquat & Fisheries Sci, Box 355020, Seattle, WA 98195 USA.
EM ejduffy@u.washington.edu
FU Pacific Salmon Commission (PSC); University of Washington; Washington
Department of Fish and Wildlife (WDFW); Washington Sea Grant; Washington
Cooperative Fish and Wildlife Research Unit (WACFWRU); US Geological
Survey, University of Washington; Washington State University; state of
Washington Department of Fish and Wildlife; state of Washington
Department of Ecology; state of Washington Department of Natural
Resources; US Fish and Wildlife Service
FX This study was made possible by funding from the Pacific Salmon
Commission (PSC), the University of Washington's H. Mason Keeler
fellowship, Washington Department of Fish and Wildlife (WDFW),
Washington Sea Grant, and Washington Cooperative Fish and Wildlife
Research Unit (WACFWRU). The midwater trawl sampling was made possible
by the Department of Fisheries and Oceans Canada. Thanks to the many
people that helped with the field work, especially Rusty Sweeting, Carol
Cooper, and Krista Lange. We are also grateful to the crew of the RV
"Ricker", FV "Viking Storm", and FV "Frosti" for their enthusiasm and
hard work. The US Geological Survey, Washington Cooperative Fish and
Wildlife Research Unit, is jointly sponsored by US Geological Survey,
University of Washington, Washington State University, the state of
Washington Departments of Fish and Wildlife, Ecology, and Natural
Resources, and the US Fish and Wildlife Service. The use of trade,
product, or firm names in this publication is for descriptive purposes
only and does not imply endorsement by the US Government.
NR 44
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U1 0
U2 36
PU CANADIAN SCIENCE PUBLISHING, NRC RESEARCH PRESS
PI OTTAWA
PA 1200 MONTREAL ROAD, BUILDING M-55, OTTAWA, ON K1A 0R6, CANADA
SN 0706-652X
J9 CAN J FISH AQUAT SCI
JI Can. J. Fish. Aquat. Sci.
PD FEB
PY 2011
VL 68
IS 2
BP 232
EP 240
DI 10.1139/F10-144
PG 9
WC Fisheries; Marine & Freshwater Biology
SC Fisheries; Marine & Freshwater Biology
GA 731IE
UT WOS:000288098700005
ER
PT J
AU Scott, JM
Rachlow, JL
AF Scott, J. Michael
Rachlow, Janet L.
TI Refocusing the Debate about Advocacy
SO CONSERVATION BIOLOGY
LA English
DT Editorial Material
ID CONSERVATION BIOLOGY; POLICY ADVOCACY; SCIENCE; SCIENTISTS
C1 [Scott, J. Michael] Univ Idaho, US Geol Survey, Idaho Cooperat Fish & Wildlife Res Unit, Moscow, ID 83844 USA.
[Rachlow, Janet L.] Univ Idaho, Dept Fish & Wildlife Resources, Moscow, ID 83844 USA.
RP Scott, JM (reprint author), Univ Idaho, US Geol Survey, Idaho Cooperat Fish & Wildlife Res Unit, Moscow, ID 83844 USA.
EM mscott@uidaho.edu
NR 15
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U1 2
U2 13
PU WILEY-BLACKWELL
PI HOBOKEN
PA 111 RIVER ST, HOBOKEN 07030-5774, NJ USA
SN 0888-8892
EI 1523-1739
J9 CONSERV BIOL
JI Conserv. Biol.
PD FEB
PY 2011
VL 25
IS 1
BP 1
EP 3
DI 10.1111/j.1523-1739.2010.01629.x
PG 3
WC Biodiversity Conservation; Ecology; Environmental Sciences
SC Biodiversity & Conservation; Environmental Sciences & Ecology
GA 708QX
UT WOS:000286380500001
PM 21251070
ER
PT J
AU Skagen, SK
Adams, AAY
AF Skagen, Susan K.
Adams, Amy A. Yackel
TI Potential Misuse of Avian Density as a Conservation Metric
SO CONSERVATION BIOLOGY
LA English
DT Article
DE avian density; density dependence; habitat quality; per capita
fecundity; population growth rate
ID IDEAL FREE DISTRIBUTION; REPRODUCTIVE SUCCESS; POPULATION-DYNAMICS;
ECOLOGICAL TRAPS; HABITAT QUALITY; PUBLIC INFORMATION; NEST PREDATION;
BIRDS; EVOLUTION; COLONIALITY
AB Effective conservation metrics are needed to evaluate the success of management in a rapidly changing world. Reproductive rates and densities of breeding birds (as a surrogate for reproductive rate) have been used to indicate the quality of avian breeding habitat, but the underlying assumptions of these metrics rarely have been examined. When birds are attracted to breeding areas in part by the presence of conspecifics and when breeding in groups influences predation rates, the effectiveness of density and reproductive rate as indicators of habitat quality is reduced. It is beneficial to clearly distinguish between individual- and population-level processes when evaluating habitat quality. We use the term reproductive rate to refer to both levels and further distinguish among levels by using the terms per capita fecundity (number of female offspring per female per year, individual level) and population growth rate (the product of density and per capita fecundity, population level). We predicted how density and reproductive rate interact over time under density-independent and density-dependent scenarios, assuming the ideal free distribution model of how birds settle in breeding habitats. We predicted population density of small populations would be correlated positively with both per capita fecundity and population growth rate due to the Allee effect. For populations in the density-dependent growth phase, we predicted no relation between density and per capita fecundity (because individuals in all patches will equilibrate to the same success rate) and a positive relation between density and population growth rate. Several ecological theories collectively suggest that positive correlations between density and per capita fecundity would be difficult to detect. We constructed a decision tree to guide interpretation of positive, neutral, nonlinear, and negative relations between density and reproductive rates at individual and population levels.
C1 [Skagen, Susan K.; Adams, Amy A. Yackel] US Geol Survey, Ft Collins Sci Ctr, Ft Collins, CO 80526 USA.
RP Skagen, SK (reprint author), US Geol Survey, Ft Collins Sci Ctr, 2150 Ctr Ave,Bldg C, Ft Collins, CO 80526 USA.
EM skagens@usgs.gov
FU U.S. Geological Survey
FX We thank B.S. Cade, J.F. Kelly for invigorating discussions, and J.W.
Shoemaker for graphics. This work was funded by the U.S. Geological
Survey.
NR 60
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U1 1
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PU WILEY-BLACKWELL
PI MALDEN
PA COMMERCE PLACE, 350 MAIN ST, MALDEN 02148, MA USA
SN 0888-8892
J9 CONSERV BIOL
JI Conserv. Biol.
PD FEB
PY 2011
VL 25
IS 1
BP 48
EP 55
DI 10.1111/j.1523-1739.2010.01571.x
PG 8
WC Biodiversity Conservation; Ecology; Environmental Sciences
SC Biodiversity & Conservation; Environmental Sciences & Ecology
GA 708QX
UT WOS:000286380500007
PM 20825446
ER
PT J
AU Lautze, NC
Sisson, TW
Mangan, MT
Grove, TL
AF Lautze, Nicole C.
Sisson, Thomas W.
Mangan, Margaret T.
Grove, Timothy L.
TI Segregating gas from melt: an experimental study of the Ostwald ripening
of vapor bubbles in magmas (vol 161, pg 331, 2011)
SO CONTRIBUTIONS TO MINERALOGY AND PETROLOGY
LA English
DT Correction
C1 [Lautze, Nicole C.] Ist Nazl Geofis & Volcanol Roma, Rome, Italy.
[Lautze, Nicole C.; Sisson, Thomas W.; Mangan, Margaret T.] US Geol Survey, Volcano Hazards Team, Menlo Pk, CA 94025 USA.
[Grove, Timothy L.] MIT, Cambridge, MA 02139 USA.
RP Lautze, NC (reprint author), Ist Nazl Geofis & Volcanol Roma, Rome, Italy.
EM nicole.lautze@ingv.it
RI Grove, Timothy/M-9638-2013
OI Grove, Timothy/0000-0003-0628-1969
NR 1
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U1 1
U2 7
PU SPRINGER
PI NEW YORK
PA 233 SPRING ST, NEW YORK, NY 10013 USA
SN 0010-7999
J9 CONTRIB MINERAL PETR
JI Contrib. Mineral. Petrol.
PD FEB
PY 2011
VL 161
IS 2
BP 349
EP 349
DI 10.1007/s00410-010-0563-6
PG 1
WC Geochemistry & Geophysics; Mineralogy
SC Geochemistry & Geophysics; Mineralogy
GA 705GQ
UT WOS:000286117300012
ER
PT J
AU Criales, MM
Robblee, MB
Browder, JA
Cardenas, H
Jackson, TL
AF Criales, Maria M.
Robblee, Michael B.
Browder, Joan A.
Cardenas, Hernando
Jackson, Thomas L.
TI FIELD OBSERVATIONS ON SELECTIVE TIDAL-STREAM TRANSPORT FOR POSTLARVAL
AND JUVENILE PINK SHRIMP IN FLORIDA BAY
SO JOURNAL OF CRUSTACEAN BIOLOGY
LA English
DT Article
DE Florida Bay; pink shrimp; selective tidal stream transport
ID CRAB CALLINECTES-SAPIDUS; EVERGLADES-NATIONAL-PARK; CROSS-SHELF
TRANSPORT; BLUE-CRAB; BEHAVIORAL-RESPONSES; PENAEUS-DUORARUM; LARVAE;
SALINITY; ABUNDANCE; VARIABILITY
AB Post larvae and juveniles of pink shrimp were collected in the summers of 2005 and 2006 at three stations in northwestern Florida Bay. the main nursery ground of this species in South Florida. Collections were made at one- or two-hour intervals during three full moon nights and two new moon nights at depth intervals in the water column. Results of the five collections were consistent with the assumption that postlarvae use a flood-tide transport (FTT) to advance into the estuary by ascending in the water column during the dark-flood tide and resting near the bottom during the ebb tide. Evidence of a FTT were higher numbers of postlarvae per hour collected during the flood tide vs. ebb tide and the large number of postlarvae collected with highest velocity flood tide currents. ANOVA indicated significant differences in the number of postlarvae collected between tidal stages and moon phases, but not among depths. Post larvae were more abundant during new moon than full moon. We also found different patterns of postlarval distribution between the new and full moon. During the new moon, a large peak of postlarvae occurred coincident with highest current speeds, whereas, with one exception, during the full moon postlarvae were more abundant in the second half of the flood period near the slack tide. In contrast, juveniles exhibited a behavior and migratory pattern opposite to that of postlarvae. ANOVA indicated significant differences between the number of juveniles captured between tidal stages and among depths, but not between moon phases. Juveniles were found almost exclusively near the surface on the ebb tide. Significantly larger juveniles were captured on the dark-ebb rather than on the dark-flood tide during both moon phases, suggesting that older juveniles were leaving the Bay on the ebb tide.
C1 [Criales, Maria M.; Cardenas, Hernando] Univ Miami, Rosenstiel Sch Marine & Atmospher Sci, Miami, FL 33149 USA.
[Robblee, Michael B.] US Geol Survey, Florida Caribbean Sci Ctr, Gainesville, FL 32653 USA.
[Browder, Joan A.; Jackson, Thomas L.] NOAA Fisheries, SE Fisheries Sci Ctr, Miami, FL 33149 USA.
RP Criales, MM (reprint author), Univ Miami, Rosenstiel Sch Marine & Atmospher Sci, 4600 Rickenbacker Causeway, Miami, FL 33149 USA.
EM mcriales@rsmas.miami.edu; mike_robblee@usgs.gov; joan.browder@noaa.gov;
hcardenas@rsmas.miami.edu; tom.jackson@noaa.gov
FU NOAA; Habitat Program at NOAA Fisheries
FX We thank the NOAA South Florida Ecosystem Restoration and Modeling
Program and the Habitat Program at NOAA Fisheries for funding this
research. We thank Jeremy Hall, Destiny Hazra, Joe Contillo, Joe
Tomoleoni, Eric Buck, Andre Daniels, Randee Esteve, and other NOAA and
USGS personnel for assistance with field sampling.
NR 42
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U1 3
U2 8
PU CRUSTACEAN SOC
PI SAN ANTONIO
PA 840 EAST MULBERRY, SAN ANTONIO, TX 78212 USA
SN 0278-0372
J9 J CRUSTACEAN BIOL
JI J. Crustac. Biol.
PD FEB
PY 2011
VL 31
IS 1
BP 26
EP 33
DI 10.1651/10-3291.1
PG 8
WC Marine & Freshwater Biology
SC Marine & Freshwater Biology
GA 722JA
UT WOS:000287427300003
ER
PT J
AU Luo, AX
Ge, ZF
Fan, YJ
Luo, AS
Chun, Z
He, XJ
AF Luo, Aoxue
Ge, Zhongfu
Fan, Yijun
Luo, Aoshuang
Chun, Ze
He, XingJin
TI In Vitro and In Vivo Antioxidant Activity of a Water-Soluble
Polysaccharide from Dendrobium denneanum
SO MOLECULES
LA English
DT Article
DE Dendrobium denneanum; polysaccharide; antioxidant activity
ID STRUCTURAL-CHARACTERIZATION; OXIDATIVE STRESS; MUTANT STRAIN; NOBILE
LINDL; IDENTIFICATION; PURIFICATION; EXTRACTS; FRACTION; FEATURES;
SUGARS
AB The water-soluble crude polysaccharide (DDP) obtained from the aqueous extracts of the stem of Dendrobium denneanum through hot water extraction followed by ethanol precipitation, was found to have an average molecular weight (Mw) of about 484.7 kDa. Monosaccharide analysis revealed that DDP was composed of arabinose, xylose, mannose, glucose and galactose in a molar ratio of 1.00:2.66:8.92:34.20:10.16. The investigation of antioxidant activity both in vitro and in vivo showed that DDP is a potential antioxidant.
C1 [Luo, Aoxue; Fan, Yijun] Sichuan Agr Univ, Dept Landscape Plants, Chengdu 611130, Peoples R China.
[Ge, Zhongfu] US Geol Survey, Lake Michigan Ecol Res Stn, Porter, IN 46304 USA.
[Luo, Aoshuang; Chun, Ze] Chinese Acad Sci, Chengdu Inst Biol, Chengdu 610041, Peoples R China.
[He, XingJin] Sichuan Univ, Coll Life Sci, Chengdu 610064, Peoples R China.
RP Fan, YJ (reprint author), Sichuan Agr Univ, Dept Landscape Plants, Chengdu Campus, Chengdu 611130, Peoples R China.
EM Yijfan@yahoo.com.cn
FU Education Department Foundation of Sichuan Province of China [08ZA074]
FX This study was supported by the Education Department Foundation of
Sichuan Province of China (08ZA074).
NR 46
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U1 4
U2 40
PU MDPI AG
PI BASEL
PA KANDERERSTRASSE 25, CH-4057 BASEL, SWITZERLAND
SN 1420-3049
J9 MOLECULES
JI Molecules
PD FEB
PY 2011
VL 16
IS 2
BP 1579
EP 1592
DI 10.3390/molecules16021579
PG 14
WC Chemistry, Organic
SC Chemistry
GA 726SC
UT WOS:000287745400038
PM 21321529
ER
PT J
AU Schmitt, AK
Perfit, MR
Rubin, KH
Stockli, DF
Smith, MC
Cotsonika, LA
Zellmer, GF
Ridley, WI
Lovera, OM
AF Schmitt, Axel K.
Perfit, Michael R.
Rubin, Kenneth H.
Stockli, Daniel F.
Smith, Matthew C.
Cotsonika, Laurie A.
Zellmer, Georg F.
Ridley, W. Ian
Lovera, Oscar M.
TI Rapid cooling rates at an active mid-ocean ridge from zircon
thermochronology
SO EARTH AND PLANETARY SCIENCE LETTERS
LA English
DT Article
DE uranium series; (U-Th)/He dating; axial magma chamber; fractional
crystallization; mid-ocean ridge volcanism
ID JUAN-DE-FUCA; LOWER OCEANIC-CRUST; GALAPAGOS SPREADING CENTER; ION
MICROPROBE ANALYSIS; SOUTHWEST INDIAN RIDGE; EAST PACIFIC RISE;
TI-IN-ZIRCON; OMAN OPHIOLITE; ABYSSAL LAVAS; TH-230 DISEQUILIBRIUM
AB Oceanic spreading ridges are Earth's most productive crust generating environment, but mechanisms and rates of crustal accretion and heat loss are debated. Existing observations on cooling rates are ambiguous regarding the prevalence of conductive vs. convective cooling of lower oceanic crust. Here, we report the discovery and dating of zircon in mid-ocean ridge dacite lavas that constrain magmatic differentiation and cooling rates at an active spreading center. Dacitic lavas erupted on the southern Cleft segment of the Juan de Fuca ridge, an intermediate-rate spreading center, near the intersection with the Blanco transform fault. Their U-Th zircon crystallization ages (29.3(-4.6)(+4.8)ka; 1 sigma standard error se.) overlap with the (U-Th)/He zircon eruption age (32.7 +/- 1.6 ka) within uncertainty. Based on similar U-238-Th-230 disequilibria between southern Cleft dacite glass separates and young mid-ocean ridge basalt (MORB) erupted nearby, differentiation must have occurred rapidly, within similar to 10-20 ka at most. Ti-in-zircon thermometry indicates crystallization at 850-900 degrees C and pressures > 70-150 MPa are calculated from H2O solubility models. These time-temperature constraints translate into a magma cooling rate of similar to 2 x 10(-2) degrees C/a. This rate is at least one order-of-magnitude faster than those calculated for zircon-bearing plutonic rocks from slow spreading ridges. Such short intervals for differentiation and cooling can only be resolved through uranium-series (U-238-Th-230) decay in young lavas, and are best explained by dissipating heat convectively at high crustal permeability. (c) 2010 Elsevier B.V. All rights reserved.
C1 [Perfit, Michael R.; Smith, Matthew C.; Cotsonika, Laurie A.] Univ Florida, Dept Geol Sci, Gainesville, FL 32611 USA.
[Rubin, Kenneth H.; Zellmer, Georg F.] Univ Hawaii, Dept Geol & Geophys SOEST, Honolulu, HI 96822 USA.
[Stockli, Daniel F.] Univ Kansas, Dept Geol, Lawrence, KS 66045 USA.
[Stockli, Daniel F.] Univ Kansas, Dept Geol, Lawrence, KS 66045 USA.
[Zellmer, Georg F.] Acad Sinica, Inst Earth Sci, Taipei 11529, Taiwan.
[Ridley, W. Ian] US Geol Survey, Cent Reg Mineral Resources Team, Denver Fed Ctr, Lakewood, CO 80225 USA.
RP Schmitt, AK (reprint author), Univ Calif Los Angeles, Dept Earth & Space Sci, 595 Charles Young Dr E, Los Angeles, CA 90095 USA.
EM axel@oro.ess.ucla.edu
RI Rubin, Kenneth/B-3685-2008; Zellmer, Georg/M-6258-2014; Stockli,
Daniel/N-8868-2015; UCLA, SIMS/A-1459-2011;
OI Rubin, Kenneth/0000-0002-8554-1337; Zellmer, Georg/0000-0001-5450-9353;
Stockli, Daniel/0000-0001-7652-2129; Schmitt, Axel/0000-0002-9029-4211
FU Division of Earth Sciences, National Science Foundation; Ocean Sciences
Division of the NSF [OCE-0221541, OCE-0933884]
FX Debra S. Stakes, the crew of the R/V Western Flyer, and the pilots of
the ROV Tiburon are acknowledged for support during the sampling cruise.
Janet C. Harvey is thanked for processing bathymetry data. We thank
reviewers Joshua Schwartz and Michel Condomines, as well as editor
Richard Carlson. The ion microprobe facility at UCLA is partly supported
by a grant from the Instrumentation and Facilities Program, Division of
Earth Sciences, National Science Foundation. MRP, KHR, MCS and LAC were
supported by grants from the Ocean Sciences Division of the NSF
(OCE-0221541, Perfit; OCE-0933884, Rubin). WIR publishes with the
permission of the US Geologic Survey.
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U1 1
U2 21
PU ELSEVIER SCIENCE BV
PI AMSTERDAM
PA PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS
SN 0012-821X
J9 EARTH PLANET SC LETT
JI Earth Planet. Sci. Lett.
PD FEB 1
PY 2011
VL 302
IS 3-4
BP 349
EP 358
DI 10.1016/j.epsl.2010.12.022
PG 10
WC Geochemistry & Geophysics
SC Geochemistry & Geophysics
GA 724ZL
UT WOS:000287614900009
ER
PT J
AU McKinney, MA
Letcher, RJ
Aars, J
Born, EW
Branigan, M
Dietz, R
Evans, TJ
Gabrielsen, GW
Peacock, E
Sonne, C
AF McKinney, Melissa A.
Letcher, Robert J.
Aars, Jon
Born, Erik W.
Branigan, Marsha
Dietz, Rune
Evans, Thomas J.
Gabrielsen, Geir W.
Peacock, Elizabeth
Sonne, Christian
TI Flame retardants and legacy contaminants in polar bears from Alaska,
Canada, East Greenland and Svalbard, 2005-2008
SO ENVIRONMENT INTERNATIONAL
LA English
DT Article
DE Polar bear (Ursus maritimus); PCB; Brominated flame retardant;
Organochlorine; Spatial trends; Temporal trends
ID CHLORINATED-HYDROCARBON CONTAMINANTS; POLYBROMINATED DIPHENYL ETHERS;
ARCTIC MARINE MAMMALS; METHYL SULFONE PCB; URSUS-MARITIMUS; TEMPORAL
TRENDS; GULL EGGS; ORGANOCHLORINES; METABOLITES; FATE
AB Flame retardants and legacy contaminants were analyzed in adipose tissue from 11 circumpolar polar bear (Ursus maritimus) subpopulations in 2005-2008 spanning Alaska east to Svalbard. Although 37 polybrominated diphenyl ethers (PBDEs), total-(alpha)-hexabromocyclododecane (HBCD), 2 polybrominated biphenyls (PBBs), pentabromotoluene, pentabromoethylbenzene, hexabromobenzene, 1,2-bis (2,4,6-tribromophenoxy(ethane) and decabromodiphenyl ethane were screened, only 4 PBDEs, total-(alpha-) HBCD and BB153 were consistently found. Geometric mean Sigma PBDE (4.6-78.4 ng/g lipid weight (lw)) and BB153 (2.5-81.1 ng/g lw) levels were highest in East Greenland (43.2 and 39.2 ng/g lipid weight (lw), respectively), Svalbard (44.4 and 20.9 ng/g lw) and western (38.6 and 30.1 ng/g lw) and southern Hudson Bay (78.4 and 81.1 ng/g lw). Total-(alpha)-HBCD levels (<0.3-41.1 ng/g lw) were lower than Sigma PBDE levels in all subpopulations except in Svalbard, consistent with greater European HBCD use versus North American pentaBDE product use. Sigma PCB levels were high relative to flame retardants as well as other legacy contaminants and increased from west to east (1797-10,537 ng/g lw). Sigma CHL levels were highest among legacy organochlorine pesticides and relatively spatially uniform (765-3477 ng/g lw). Sigma DDT levels were relatively low and spatially variable (31.5-206 ng/g lw). However, elevated proportions of p,p'-DDT to Sigma DDT in Alaska and Beaufort Sea relative to other subpopulations suggested fresh inputs from vector control use in Asia and/or Africa. Comparing earlier circumpolar polar bear studies, Sigma PBDE, total-(alpha)-HBCD, p,p'-DDE and Sigma CHL levels consistently declined, whereas levels of other legacy contaminants did not. International regulations have clearly been effective in reducing levels of several legacy contaminants in polar bears relative to historical levels. However, slow or stalling declines of certain historic pollutants like PCBs and a complex mixture of "new" chemicals continue to be of concern to polar bear health and that of their arctic marine ecosystems. (c) 2010 Elsevier Ltd. All rights reserved.
C1 [McKinney, Melissa A.] Carleton Univ, Natl Wildlife Res Ctr, Ecotoxicol & Wildlife Hlth Div, Environm Canada,Sci & Technol Branch, Ottawa, ON K1A 0H3, Canada.
[McKinney, Melissa A.; Letcher, Robert J.] Carleton Univ, Dept Chem, Ottawa, ON K1S 5B6, Canada.
[Aars, Jon; Gabrielsen, Geir W.] Norwegian Polar Res Inst, NO-9296 Tromso, Norway.
[Born, Erik W.] Greenland Inst Nat Resources, DK-3900 Nuuk, Greenland, Denmark.
[Branigan, Marsha] Govt NW Terr, Dept Environm & Nat Resources, Inuvik, NT X0E 0T0, Canada.
[Dietz, Rune; Sonne, Christian] Aarhus Univ, Natl Environm Res Inst, Dept Arctic Environm, DK-4000 Roskilde, Denmark.
[Evans, Thomas J.] US Fish & Wildlife Serv, Anchorage, AK 99503 USA.
[Peacock, Elizabeth] Govt Nunavut, Dept Environm, Igloolik, NU X0A 0L0, Canada.
RP McKinney, MA (reprint author), Carleton Univ, Natl Wildlife Res Ctr, Ecotoxicol & Wildlife Hlth Div, Environm Canada,Sci & Technol Branch, Raven Rd, Ottawa, ON K1A 0H3, Canada.
EM melissaamckinney@gmail.com; robert.letcher@ec.gc.ca
RI Sonne, Christian/I-7532-2013; Dietz, Rune/L-4640-2013; Dietz,
Rune/F-9154-2015;
OI Sonne, Christian/0000-0001-5723-5263; McKinney,
Melissa/0000-0002-8171-7534
FU Department of Indian and Northern Affairs Canada; Canadian International
Polar Year Secretariat; Molson Foundation; Natural Sciences and
Engineering Research Council of Canada (NSERC); KVUG; DANCEA; Prince
Albert Foundation; US Fish and Wildlife Service Marine Mammals
Management
FX For Canadian sampling and assistance, we thank Nunavut Hunters and
Trappers Organizations, Nunavut Department of Environment conservation
officers and lab technicians (A. Coxon, F. Piugattuk, A. Niptanatiak, D.
Fredlund, J. Ashevak, J. Savikataaq, J. Qaunaq, A. Williams, P.
Prefontaine, K. Nogier, A. Nakashuk, L Kudluk, N. Nakoolik, E. Qaggutaq,
T. Palluq, N. Amarualik, T. Mullin, B. J. Hainnu, G. Koonoo, T. Palluq,
J. Coutu-Autut) and Environment Canada's National Wildlife Specimen Bank
at NWRC. Thanks to R. Pugh (Hollings Marine Laboratory, NIST) for
assistance with the Alaskan samples. For Svalbard sampling, we thank M.
Andersen. For East Greenland sampling and assistance, we thank local
hunters, J. Bronlund, M. Kierkegaard, S. Joensen and L Bruun. In Canada,
this study was funded by the Northern Contaminants Program (Department
of Indian and Northern Affairs Canada) (R.J.L.), the Canadian
International Polar Year Secretariat (E.P., R.J.L), the Molson
Foundation (R.J.L.) and the Natural Sciences and Engineering Research
Council of Canada (NSERC) by a Discovery Grant (R.J.L.) and an NSERC
Canada Graduate Scholarship (M.A.M.). Greenland program funding was from
the IPY program "BearHealth" by KVUG, DANCEA and the Prince Albert
Foundation and the US Fish and Wildlife Service Marine Mammals
Management contributed to Alaskan funding.
NR 47
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PU PERGAMON-ELSEVIER SCIENCE LTD
PI OXFORD
PA THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND
SN 0160-4120
J9 ENVIRON INT
JI Environ. Int.
PD FEB
PY 2011
VL 37
IS 2
BP 365
EP 374
DI 10.1016/j.envint.2010.10.008
PG 10
WC Environmental Sciences
SC Environmental Sciences & Ecology
GA 725BL
UT WOS:000287620100009
PM 21131049
ER
PT J
AU Barringer, JL
Szabo, Z
Wilson, TP
Bonin, JL
Kratzer, T
Cenno, K
Romagna, T
Alebus, M
Hirst, B
AF Barringer, Julia L.
Szabo, Zoltan
Wilson, Timothy P.
Bonin, Jennifer L.
Kratzer, Todd
Cenno, Kimberly
Romagna, Terri
Alebus, Marzooq
Hirst, Barbara
TI Distribution and seasonal dynamics of arsenic in a shallow lake in
northwestern New Jersey, USA
SO ENVIRONMENTAL GEOCHEMISTRY AND HEALTH
LA English
DT Article
DE Arsenic; Lake water; Lake sediments; Redox; Metals
ID CCA-TREATED WOOD; OXIDE MINERALS; SEDIMENTS; SPECIATION; ELEMENTS;
WATER; PHOSPHATE; RESERVOIR; MOBILITY; ACCUMULATION
AB Elevated concentrations of arsenic (As) occurred during warm months in water from the outlet of Lake Mohawk in northwestern New Jersey. The shallow manmade lake is surrounded by residential development and used for recreation. Eutrophic conditions are addressed by alum and copper sulfate applications and aerators operating in the summer. In September 2005, arsenite was dominant in hypoxic to anoxic bottom water. Filterable As concentrations were about 1.6-2 times higher than those in the upper water column (23-25 mu g/L, mostly arsenate). Hypoxic/anoxic and near-neutral bottom conditions formed during the summer, but became more oxic and alkaline as winter approached. Acid-leachable As concentrations in lake-bed sediments ranged up to 694 mg/kg in highly organic material from the tops of sediment cores but were < 15 mg/kg in geologic substrate. During warm months, reduced As from the sediment diffuses into the water column and is oxidized; mixing by aerators, wind, and boat traffic spreads arsenate and metals, some in particulate form, throughout the water column. Similar levels of As in sediments of lakes treated with arsenic pesticides indicate that most of the As in Lake Mohawk probably derives from past use of arsenical pesticides, although records of applications are lacking. The annual loss of As at the lake outlet is only about 0.01% of the As calculated to be in the sediments, indicating that elevated levels of As in the lake will persist for decades.
C1 [Barringer, Julia L.; Szabo, Zoltan; Wilson, Timothy P.; Bonin, Jennifer L.] US Geol Survey, New Jersey Water Res Ctr, W Trenton, NJ 08628 USA.
[Kratzer, Todd] New Jersey Water Supply Author, Somerville, NJ 08876 USA.
[Cenno, Kimberly; Romagna, Terri; Alebus, Marzooq; Hirst, Barbara] New Jersey Dept Environm Protect, Trenton, NJ 08625 USA.
RP Barringer, JL (reprint author), US Geol Survey, New Jersey Water Res Ctr, 810 Bear Tavern Rd, W Trenton, NJ 08628 USA.
EM jbarring@usgs.gov
FU New Jersey Department of Environmental Protection
FX Funding for the study was provided by the New Jersey Department of
Environmental Protection. The authors are grateful to Frances Smith of
the LMCC for permission to sample Lake Mohawk, for operational help
during the sampling campaign, and for information about the lake. Ernest
Hofer of the Sussex County MUA and Dr. Stephen J. Souza of Princeton
Hydro provided us with maps, data, and information about the lake's
history and ecology. Steve Glasson supplied and piloted the boat that
was our sampling platform. We thank USGS colleagues Peter Van Metre for
supplying the coring equipment, and MaryLynn Musgrove and Faith
Fitzpatrick for insightful comments on drafts of this manuscript. We are
grateful for anonymous reviewer comments that greatly improved the
clarity of the paper. Use of brand or trade names is for identification
purposes only and does not imply endorsement by the US Government.
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PU SPRINGER
PI DORDRECHT
PA VAN GODEWIJCKSTRAAT 30, 3311 GZ DORDRECHT, NETHERLANDS
SN 0269-4042
J9 ENVIRON GEOCHEM HLTH
JI Environ. Geochem. Health
PD FEB
PY 2011
VL 33
IS 1
BP 1
EP 22
DI 10.1007/s10653-010-9289-7
PG 22
WC Engineering, Environmental; Environmental Sciences; Public,
Environmental & Occupational Health; Water Resources
SC Engineering; Environmental Sciences & Ecology; Public, Environmental &
Occupational Health; Water Resources
GA 723MH
UT WOS:000287510200001
PM 20405171
ER
PT J
AU Singh, A
Hines, TC
Hostetler, JA
Percival, HF
Oli, MK
AF Singh, Aditya
Hines, Tommy C.
Hostetler, Jeffery A.
Percival, H. Franklin
Oli, Madan K.
TI Patterns of space and habitat use by northern bobwhites in South
Florida, USA
SO EUROPEAN JOURNAL OF WILDLIFE RESEARCH
LA English
DT Article
DE Colinus virginianus; Game bird; Habitat selection; Habitat management;
Habitat preference; Home range; Space use
ID IMPORTED FIRE ANTS; HOME-RANGE SIZE; CLASSIFICATION-BASED ANALYSES;
COLINUS-VIRGINIANUS; RESOURCE SELECTION; SUPPLEMENTAL FOOD; BLACK BEARS;
POPULATIONS; SURVIVAL; TEXAS
AB The manner by which animals use space and select resources can have important management consequences. We studied patterns of habitat selection by northern bobwhites (Colinus virginianus) on Babcock-Webb Wildlife Management Area, Charlotte County, Florida and evaluated factors influencing the sizes of their home ranges. A total of 1,245 radio-tagged bobwhites were monitored for 19,467 radio days during 2002-2007. The mean ( +/- 1 SE) annual home range size, estimated using the Kernel density method, was 88.43 ( +/- 6.16) ha and did not differ between genders. Winter home ranges of bobwhites (69.27 +/- 4.92 ha) were generally larger than summer home ranges (53.90 +/- 4.93 ha). Annual and winter home ranges were smaller for bobwhites whose ranges contained food plots compared to those that did not; however, the presence of food plots did not influence summer home ranges. We used distance-based methods to investigate habitat selection by bobwhites at two scales: selection of home ranges within the study site (second-order selection) and selection of habitats within home ranges (third-order selection). Across both scales, bobwhites generally preferred food plots and dry prairie habitat and avoided wet prairies and roads. This pattern was generally consistent between genders and across years. Our data indicate that management practices aimed at increasing and maintaining a matrix of food plots and dry prairie habitat would provide the most favorable environment for bobwhites.
C1 [Singh, Aditya; Hostetler, Jeffery A.; Oli, Madan K.] Univ Florida, Dept Wildlife Ecol & Conservat, Gainesville, FL 32611 USA.
[Hines, Tommy C.] Florida Fish & Wildlife Conservat Commiss, Small Game Program, Newberry, FL 32669 USA.
[Percival, H. Franklin] Univ Florida, Dept Wildlife Ecol & Conservat, Florida Cooperat Fish & Wildlife Res Unit, US Geol Survey, Gainesville, FL 32611 USA.
RP Oli, MK (reprint author), Univ Florida, Dept Wildlife Ecol & Conservat, 110 Newins Ziegler Hall, Gainesville, FL 32611 USA.
EM olim@ufl.edu
RI Hostetler, Jeffrey/A-3345-2011; Singh, Aditya/I-3628-2013
OI Hostetler, Jeffrey/0000-0003-3669-1758; Singh,
Aditya/0000-0001-5559-9151
FU Florida Fish and Wildlife Conservation Commission; Department of
Wildlife Ecology and Conservation; School of Natural Resources and the
Environment, University of Florida
FX We thank Ralph W. Dimmick and Stephen Brinkley for leading the field
data collection efforts; this work would not have been possible without
their dedicated work. We thank M. Kemmerer and C. Pope for providing
information on the history and management of the WMA, for assistance
with equipment maintenance, and for general counsel and advice as the
study progressed. A. Brinkley, G. Coker, C. McKelvy, D. Caudill, S.
Dimmick, D. Holt, J. McGrady, J. Sloane, J. Scott, and L. Taylor
assisted with data collection. T. O'Meara provided valuable advice
throughout the study. R. Dimmick and W. Palmer and V. Rolland provided
many helpful comments on the manuscript. We are grateful to the many
volunteers from the Southwest Florida Chapter of Quail Unlimited who
aided the research in many ways. Research was funded by the Florida Fish
and Wildlife Conservation Commission, and the Department of Wildlife
Ecology and Conservation and School of Natural Resources and the
Environment, University of Florida. We thank two anonymous reviewers for
many helpful comments and suggestions.
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PI NEW YORK
PA 233 SPRING ST, NEW YORK, NY 10013 USA
SN 1612-4642
EI 1439-0574
J9 EUR J WILDLIFE RES
JI Eur. J. Wildl. Res.
PD FEB
PY 2011
VL 57
IS 1
BP 15
EP 26
DI 10.1007/s10344-010-0393-x
PG 12
WC Ecology; Zoology
SC Environmental Sciences & Ecology; Zoology
GA 711ZG
UT WOS:000286630300002
ER
PT J
AU Palacios, V
Mech, LD
AF Palacios, Vicente
Mech, L. David
TI Problems with studying wolf predation on small prey in summer via global
positioning system collars
SO EUROPEAN JOURNAL OF WILDLIFE RESEARCH
LA English
DT Article
DE Canis lupus; Global positioning system (GPS) collars; Predation;
Telemetry; White-tailed deer; Wolf
ID WHITE-TAILED DEER; DIFFERENTIAL CORRECTION; NORTHEASTERN MINNESOTA; KILL
RATES; ACCURACY; ECOSYSTEMS; LOCATIONS; TELEMETRY; WOLVES; FAWNS
AB We attempted to study predation on various-sized prey by a male and female wolf (Canis lupus) with global positioning system (GPS) collars programmed to acquire locations every 10 min in the Superior National Forest of Minnesota. During May to August 2007, we investigated 147 clusters of locations (31% of the total) and found evidence of predation on a white-tailed deer (Odocoileus virginianus) fawn and yearling, a beaver (Castor canadensis), ruffed grouse (Bonasa umbellus), and fisher (Martes pennanti) and scavenging on a road-killed deer and other carrion. However, we missed finding many prey items and discuss the problems associated with trying to conduct such a study.
C1 [Palacios, Vicente] Univ Valencia, Inst Cavanilles Biodiversidad & Biol Evolut, Valencia 46071, Spain.
[Mech, L. David] US Geol Survey, No Prairie Wildlife Res Ctr, Jamestown, ND 58401 USA.
RP Palacios, V (reprint author), Univ Valencia, Inst Cavanilles Biodiversidad & Biol Evolut, Apdo 22085, Valencia 46071, Spain.
EM v_palacios_s@hotmail.com
FU Biological Resources Division, United States Geological Survey; United
Sates Department of Agriculture NorthCentral Research Station
FX This study was supported by the Biological Resources Division, United
States Geological Survey, and the United Sates Department of Agriculture
NorthCentral Research Station. We thank M. E. Nelson, D. Thompson, and
A. Bennett for field assistance, and especially M. Clark for special
devotion to this project, and D. J. Demma and S. M. Barber-Meyer for
reviewing the manuscript and offering helpful suggestions for
improvement.
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PU SPRINGER
PI NEW YORK
PA 233 SPRING ST, NEW YORK, NY 10013 USA
SN 1612-4642
J9 EUR J WILDLIFE RES
JI Eur. J. Wildl. Res.
PD FEB
PY 2011
VL 57
IS 1
BP 149
EP 156
DI 10.1007/s10344-010-0408-7
PG 8
WC Ecology; Zoology
SC Environmental Sciences & Ecology; Zoology
GA 711ZG
UT WOS:000286630300015
ER
PT J
AU McDermott, ME
Wood, PB
Miller, GW
Simpson, BT
AF McDermott, Molly E.
Wood, Petra Bohall
Miller, Gary W.
Simpson, Brian T.
TI Predicting breeding bird occurrence by stand- and microhabitat-scale
features in even-aged stands in the Central Appalachians
SO FOREST ECOLOGY AND MANAGEMENT
LA English
DT Article
DE Bird-habitat modeling; Early successional birds; Even-age; Forest birds;
Multiscale; West Virginia
ID MULTIPLE SCALES; AVIAN HABITAT; FOREST; LANDSCAPE; DISTURBANCE; USA;
CLASSIFICATION; CONSERVATION; COMMUNITIES; MANAGEMENT
AB Spatial scale is an important consideration when managing forest wildlife habitat, and models can be used to improve our understanding of these habitats at relevant scales. Our objectives were to determine whether stand- or microhabitat-scale variables better predicted bird metrics (diversity, species presence, and abundance) and to examine breeding bird response to clearcut size and age in a highly forested landscape. In 2004-2007, vegetation data were collected from 62 even-aged stands that were 3.6-34.6 ha in size and harvested in 1963-1990 on the Monongahela National Forest, WV, USA. In 2005-2007, we also surveyed birds at vegetation plots. We used classification and regression trees to model breeding bird habitat use with a suite of stand and microhabitat variables. Among stand variables, elevation, stand age, and stand size were most commonly retained as important variables in guild and species models. Among microhabitat variables, medium-sized tree density and tree species diversity most commonly predicted bird presence or abundance. Early successional and generalist bird presence, abundance, and diversity were better predicted by microhabitat variables than stand variables. Thus, more intensive field sampling may be required to predict habitat use for these species, and management may be needed at a finer scale. Conversely, stand-level variables had greater utility in predicting late-successional species occurrence and abundance; thus management decisions and modeling at this scale may be suitable in areas with a uniform landscape, such as our study area. Our study suggests that late-successional breeding bird diversity can be maximized long-term by including harvests >10 ha in size into our study area and by increasing tree diversity. Some harvesting will need to be incorporated regularly, because after 15 years, the study stands did not provide habitat for most early successional breeding specialists. (C) 2010 Elsevier B.V. All rights reserved.
C1 [McDermott, Molly E.] W Virginia Univ, W Virginia Cooperat Fish & Wildlife Res Unit, Div Forestry & Nat Resources, Morgantown, WV 26506 USA.
[Wood, Petra Bohall] W Virginia Univ, US Geol Survey, W Virginia Cooperat Fish & Wildlife Res Unit, Morgantown, WV 26506 USA.
[Miller, Gary W.; Simpson, Brian T.] US Forest Serv, USDA, No Res Stn, Forestry Sci Lab, Morgantown, WV 26505 USA.
RP McDermott, ME (reprint author), Ohio State Univ, Sch Environm & Nat Resources, 2021 Coffey Rd, Columbus, OH 43210 USA.
EM mollyemcdermott@gmail.com; pbwood@wvu.edu; gwmiller@fs.fed.us;
bsimpson@fs.fed.us
RI Liu, Yi-Chun/H-5463-2012
FU USDA Forest Service, Monongahela National Forest
FX This work was funded by the USDA Forest Service, Monongahela National
Forest. The U.S. Geological Survey, West Virginia Cooperative Fish and
Wildlife Research Unit provided field vehicles, equipment access, and
logistical support. West Virginia University and USDA Forest Service
also provided logistical support. We thank USDA Forest Service for
access to sites on the Monongahela National Forest. Thanks to D. Feicht
and J. Juracko, USDA Forest Service, Northern Research Station for
collecting woody vegetation data. We are grateful to R. Gauza, D.
Hinnebusch, L. Koerner, M. Shumar, J. Walker, and T. Weidman for help
with bird surveys. G. George, S. Stoleson, and two anonymous reviewers
provided comments on an earlier version of this manuscript. Use of
tradenames in this manuscript does not imply endorsement by the Federal
government.
NR 53
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U1 3
U2 21
PU ELSEVIER SCIENCE BV
PI AMSTERDAM
PA PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS
SN 0378-1127
J9 FOREST ECOL MANAG
JI For. Ecol. Manage.
PD FEB 1
PY 2011
VL 261
IS 3
BP 373
EP 380
DI 10.1016/j.foreco.2010.10.020
PG 8
WC Forestry
SC Forestry
GA 721DO
UT WOS:000287333000006
ER
PT J
AU Bekins, BA
Matmon, D
Screaton, EJ
Brown, KM
AF Bekins, B. A.
Matmon, D.
Screaton, E. J.
Brown, K. M.
TI Reanalysis of in situ permeability measurements in the Barbados
decollement
SO GEOFLUIDS
LA English
DT Article
DE borehole observatory; CORK; decollement; ODP; permeability
ID ACCRETIONARY COMPLEX; FLUID MIGRATION; FAULT; FLOW; INITIATION; STRESS;
ZONE
AB A cased and sealed borehole in the Northern Barbados accretionary complex was the site of the first attempts to measure permeability in situ along a plate boundary decollement. Three separate efforts at Hole 949C yielded permeability estimates for the decollement spanning four orders of magnitude. An analysis of problems encountered during installation of the casing and seals provides insights into how the borehole conditions may have led to the wide range of results. During the installation, sediments from the surrounding formation repeatedly intruded into the borehole and casing. Stress analysis shows that the weak sediments were deforming plastically and the radial and tangential stresses around the borehole were significantly lower than lithostatic. This perturbed stress state may explain why the test pressure records showed indications of hydrofracture at pressures below lithostatic, and permeabilities rose rapidly as the estimated effective stress dropped below 0.8 MPa. Even after the borehole was sealed, the plastic deformation of the formation and relatively large gap of the wire wrapped screen allowed sediment to flow into the casing. Force equilibrium calculations predict sediment would have filled the borehole to 10 cm above the top of the screen by the time slug tests were conducted 1.5 years after the borehole was sealed. Reanalysis of the slug test results with these conditions yields several orders of magnitude higher permeability estimates than the original analysis which assumed an open casing. Overall the results based on only the tests with no sign of hydrofracture yield a permeability range of 10-14-10-15 m2 and a rate of increase in permeability with decreasing effective stress consistent with laboratory tests on samples from the decollement zone.
C1 [Bekins, B. A.] US Geol Survey, Menlo Pk, CA 94025 USA.
[Matmon, D.] TAHAL Consulting Engn Ltd, Tel Aviv, Israel.
[Screaton, E. J.] Univ Florida, Dept Geol Sci, Gainesville, FL USA.
[Brown, K. M.] Univ Calif San Diego, Scripps Inst Oceanog, La Jolla, CA 92093 USA.
RP Bekins, BA (reprint author), US Geol Survey, 345 Middlefield Rd, Menlo Pk, CA 94025 USA.
EM babekins@usgs.gov
FU NSF [OCE-0623358, OCE-0326749]
FX This research used samples and/or data provided by the Ocean Drilling
Program (ODP). NSF funding was provided for Screaton by OCE-0623358 and
for Matmon by OCE-0326749. We are also grateful for valuable comments on
the manuscript by Chris Neuzil, Paul Hsieh, David Lockner, and one
anonymous reviewer. Feedback on a presentation at the annual Hubbert
Quorum was also invaluable.
NR 42
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Z9 5
U1 0
U2 4
PU WILEY-BLACKWELL PUBLISHING, INC
PI MALDEN
PA COMMERCE PLACE, 350 MAIN ST, MALDEN 02148, MA USA
SN 1468-8115
J9 GEOFLUIDS
JI Geofluids
PD FEB
PY 2011
VL 11
IS 1
BP 57
EP 70
DI 10.1111/j.1468-8123.2010.00310.x
PG 14
WC Geochemistry & Geophysics; Geology
SC Geochemistry & Geophysics; Geology
GA 714WM
UT WOS:000286839700007
ER
PT J
AU Feng, ZL
Qiu, ZP
Liu, RS
DeAngelis, DL
AF Feng, Zhilan
Qiu, Zhipeng
Liu, Rongsong
DeAngelis, Donald L.
TI Dynamics of a plant-herbivore-predator system with plant-toxicity
SO MATHEMATICAL BIOSCIENCES
LA English
DT Article
DE Plant-herbivore interactions; Tritrophic chain; Plant toxicity; Boreal
ecosystem; Stability conditions
ID FUNCTIONAL-RESPONSE; MOOSE; SYMBIOSIS; COMMUNITIES; VERTEBRATES;
DIVERSITY; MODELS
AB A system of ordinary differential equations is considered that models the interactions of two plant species populations, an herbivore population, and a predator population. We use a toxin-determined functional response to describe the interactions between plant species and herbivores and use a Holling Type II functional response to model the interactions between herbivores and predators. In order to study how the predators impact the succession of vegetation, we derive invasion conditions under which a plant species can invade into an environment in which another plant species is co-existing with a herbivore population with or without a predator population. These conditions provide threshold quantities for several parameters that may play a key role in the dynamics of the system. Numerical simulations are conducted to reinforce the analytical results. This model can be applied to a boreal ecosystem trophic chain to examine the possible cascading effects of predator-control actions when plant species differ in their levels of toxic defense. Published by Elsevier Inc.
C1 [DeAngelis, Donald L.] Univ Miami, Dept Biol, Coral Gables, FL 33124 USA.
[DeAngelis, Donald L.] US Geol Survey, Florida Integrated Sci Ctr, Coral Gables, FL 33124 USA.
[Feng, Zhilan] Purdue Univ, Dept Math, W Lafayette, IN 47907 USA.
[Qiu, Zhipeng] Nanjing Univ Sci & Technol, Dept Appl Math, Nanjing 210094, Peoples R China.
[Liu, Rongsong] Univ Wyoming, Dept Math, Laramie, WY 82071 USA.
RP DeAngelis, DL (reprint author), Univ Miami, Dept Biol, POB 249118, Coral Gables, FL 33124 USA.
EM ddeangelis@bio.miami.edu
FU NSF [DMS-0920828]; NSF of China [10801074]; Qinglan Project of Jiangsu
Province; U.S. Geological Survey's Florida Integrated Science Center
FX We thank the reviewer for helpful comments that improved the manuscript.
This research is partially supported by NSF grant DMS-0920828. Z. Qiu
was supported by the NSF of China grant (10801074) and by the Qinglan
Project of Jiangsu Province. D.L. DeAngelis was supported by the U.S.
Geological Survey's Florida Integrated Science Center.
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U1 3
U2 20
PU ELSEVIER SCIENCE INC
PI NEW YORK
PA 360 PARK AVE SOUTH, NEW YORK, NY 10010-1710 USA
SN 0025-5564
J9 MATH BIOSCI
JI Math. Biosci.
PD FEB
PY 2011
VL 229
IS 2
BP 190
EP 204
DI 10.1016/j.mbs.2010.12.005
PG 15
WC Biology; Mathematical & Computational Biology
SC Life Sciences & Biomedicine - Other Topics; Mathematical & Computational
Biology
GA 724ZK
UT WOS:000287614800006
PM 21195093
ER
PT J
AU Hawkes, AD
Horton, BP
Nelson, AR
Vane, CH
Sawai, Y
AF Hawkes, A. D.
Horton, B. P.
Nelson, A. R.
Vane, C. H.
Sawai, Y.
TI Coastal subsidence in Oregon, USA, during the giant Cascadia earthquake
of AD 1700
SO QUATERNARY SCIENCE REVIEWS
LA English
DT Article
DE Cascadia subduction zone; Earthquake; Coseismic subsidence; Foraminifera
ID SEA-LEVEL INDICATORS; TIDAL MARSH STRATIGRAPHY; LATE HOLOCENE
EARTHQUAKE; PAST 2000 YEARS; SUBDUCTION-ZONE; COSEISMIC SUBSIDENCE;
GREAT EARTHQUAKES; VANCOUVER-ISLAND; BRITISH-COLUMBIA; NORTHERN OREGON
AB Quantitative estimates of land-level change during the giant AD 1700 Cascadia earthquake along the Oregon coast are inferred from relative sea-level changes reconstructed from fossil foraminiferal assemblages preserved within the stratigraphic record. A transfer function, based upon a regional training set of modern sediment samples from Oregon estuaries, is calibrated to fossil assemblages in sequences of samples across buried peat-mud and peat-sand contacts marking the AD 1700 earthquake. Reconstructions of sample elevations with sample-specific errors estimate the amount of coastal subsidence during the earthquake at six sites along 400 km of coast. The elevation estimates are supported by lithological, carbon isotope, and faunal tidal zonation data. Coseismic subsidence at Nehalem River, Nestucca River, Salmon River, Alsea Bay, Siuslaw River and South Slough varies between 0.18 m and 0.85 m with errors between 0.18 m and 0.32 m. These subsidence estimates are more precise, consistent, and generally lower than previous semi-quantitative estimates. Following earlier comparisons of semi-quantitative subsidence estimates with elastic dislocation models of megathrust rupture during great earthquakes, our lower estimates for central and northern Oregon are consistent with modeled rates of strain accumulation and amounts of slip on the subduction megathrust, and thus, with a magnitude of 9 for the AD 1700 earthquake. (C) 2010 Elsevier Ltd. All rights reserved.
C1 [Hawkes, A. D.] Woods Hole Oceanog Inst, Dept Geol & Geophys, Woods Hole, MA 02543 USA.
[Horton, B. P.] Univ Penn, Dept Earth & Environm Sci, Philadelphia, PA 19104 USA.
[Horton, B. P.] Nanyang Technol Univ, Earth Observ Singapore, Singapore 639798, Singapore.
[Nelson, A. R.] US Geol Survey, Lakewood, CO 80225 USA.
[Vane, C. H.] British Geol Survey, Keyworth NG12 5GG, Notts, England.
[Sawai, Y.] Natl Inst Adv Ind Sci & Technol, Geol Survey Japan, Act Fault & Earthquake Res Ctr, Tsukub, Ibaraki 3058567, Japan.
RP Hawkes, AD (reprint author), Woods Hole Oceanog Inst, Dept Geol & Geophys, Woods Hole, MA 02543 USA.
EM ahawkes@whoi.edu
RI Vane, Christopher/A-8814-2008; Sawai, Yuki /D-3216-2013
OI Vane, Christopher/0000-0002-8150-3640; Sawai, Yuki /0000-0001-7015-4361
FU National Science Foundation [EAR-0842728]; United States Geological
Survey, Society of Sedimentary Geology (SEPM); University of
Pennsylvania; National Oceanographic Science Accelerator Mass
Spectrometer; Earthquake Hazards Program of the United States Geological
Survey
FX This research was supported by National Science Foundation award
(EAR-0842728). Hawkes thanks other supporting agencies; United States
Geological Survey, Society of Sedimentary Geology (SEPM - Sanders
Student Research Fund), the University of Pennsylvania paleo-stipend,
and National Oceanographic Science Accelerator Mass Spectrometer for
radiocarbon dating. We acknowledge partial support from the Earthquake
Hazards Program of the United States Geological Survey. Vane publishes
with permission of the Director of the British Geological Survey. Sawai
was supported by the Japan Society for the Promotion of Science (JSPS)
Postdoctoral Fellowship for Research Abroad. Rob Witter, Andrew Kemp,
Simon Engelhardt and Candace GrandPre contributed to field sampling. EOS
publication #19. We are grateful for reviews by Chris Bernhardt and Rob
Thieler. This paper is a contribution to IGCP 588 "Preparing for coastal
change: A detailed process-response framework for coastal change at
different timescale".
NR 80
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U1 1
U2 24
PU PERGAMON-ELSEVIER SCIENCE LTD
PI OXFORD
PA THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND
SN 0277-3791
J9 QUATERNARY SCI REV
JI Quat. Sci. Rev.
PD FEB
PY 2011
VL 30
IS 3-4
BP 364
EP 376
DI 10.1016/j.quascirev.2010.11.017
PG 13
WC Geography, Physical; Geosciences, Multidisciplinary
SC Physical Geography; Geology
GA 722LP
UT WOS:000287434000009
ER
PT J
AU Sundberg, MD
DeAngelis, P
Havens, K
Holsinger, K
Kennedy, K
Kramer, AT
Muir, R
Olwell, P
Schierenbeck, K
Stritch, L
Zorn-Arnold, B
AF Sundberg, Marshall D.
DeAngelis, Patricia
Havens, Kayri
Holsinger, Kent
Kennedy, Kathryn
Kramer, Andrea T.
Muir, Rachel
Olwell, Peggy
Schierenbeck, Kristina
Stritch, Larry
Zorn-Arnold, Barbara
TI Perceptions of Strengths and Deficiencies: Disconnects between Graduate
Students and Prospective Employers
SO BIOSCIENCE
LA English
DT Article
DE botanical capacity; student perceptions; employer expectations; skill
sets; education
ID SYSTEMATICS; PIPELINE; SCIENCE
AB The US Botanical Capacity Assessment Project (BCAP) was initiated as a first step to gauge the nation's collective ability to meet the environmental challenges of the 21st century The project, in which the authors of this article are involved, specifically aimed to identify multisector contributions to and gaps in botanical capacity in order to develop growth opportunities to address research and management problems. One of the primary gaps revealed by the BCAP surveys was that the skills graduate students identified as their greatest strengths closely matched the areas future employers (government and private sectors) identified as needing greatest improvement. Although our survey focused on only one discipline (botany), we suspect that the results are applicable throughout the science, technology, engineering, and mathematics disciplines. We suggest that it is critical for university faculty and administrators to team with professionals from government, nonprofit, and for-profit organizations to identify critical and desired knowledge and skill sets and implement the necessary curriculum changes to provide graduates with the tools they need.
C1 [Sundberg, Marshall D.] Emporia State Univ, Dept Biol Sci, Emporia, KS 66801 USA.
[DeAngelis, Patricia] US Fish & Wildlife Serv, Div Sci Author, Arlington, VA USA.
[Havens, Kayri; Zorn-Arnold, Barbara] Chicago Bot Garden, Div Plant Sci & Conservat, Glencoe, IL USA.
[Kramer, Andrea T.] Chicago Bot Garden, Bot Gardens Conservat Int, Glencoe, IL USA.
[Holsinger, Kent] Univ Connecticut, Dept Ecol & Evolutionary Biol, Storrs, CT 06269 USA.
[Kennedy, Kathryn] Missouri Bot Garden, Ctr Plant Conservat, St Louis, MO USA.
[Muir, Rachel] US Geol Survey, Off Reg Execut NE, Reston, VA 22092 USA.
[Olwell, Peggy] Div Fish Wildlife & Plant Conservat, Bur Land Management, Washington, DC USA.
[Schierenbeck, Kristina] Calif State Univ Chico, Dept Biol Sci, Chico, CA 95929 USA.
[Stritch, Larry] US Forest Serv, Washington Off Range Staff, Washington, DC 20250 USA.
RP Sundberg, MD (reprint author), Emporia State Univ, Dept Biol Sci, Emporia, KS 66801 USA.
EM msundber@emporia.edu
OI Holsinger, Kent/0000-0003-4312-3804
FU Chicago Botanic Garden, Botanic Gardens Conservation International (US);
National Fish and Wildlife Foundation
FX The Botanical Capacity Assessment Project (BCAP) is supported by the
Chicago Botanic Garden, Botanic Gardens Conservation International (US),
and a grant from the National Fish and Wildlife Foundation. The authors
are members of the BCAP advisory board. We thank Jean Schulenberg,
graduate students Jennifer Ison and Rebecca Tonietto, and three
anonymous reviewers for their critical reviews of the manuscript.
NR 20
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U1 0
U2 10
PU AMER INST BIOLOGICAL SCI
PI WASHINGTON
PA 1444 EYE ST, NW, STE 200, WASHINGTON, DC 20005 USA
SN 0006-3568
J9 BIOSCIENCE
JI Bioscience
PD FEB
PY 2011
VL 61
IS 2
BP 133
EP 138
DI 10.1525/bio.2011.61.2.8
PG 6
WC Biology
SC Life Sciences & Biomedicine - Other Topics
GA 720FY
UT WOS:000287267200012
ER
PT J
AU Day, JW
Kemp, GP
Reed, DJ
Cahoon, DR
Boumans, RM
Suhayda, JM
Gambrell, R
AF Day, John W.
Kemp, G. Paul
Reed, Denise J.
Cahoon, Donald R.
Boumans, Roelof M.
Suhayda, Joseph M.
Gambrell, Robert
TI Vegetation death and rapid loss of surface elevation in two contrasting
Mississippi delta salt marshes: The role of sedimentation,
autocompaction and sea-level rise
SO ECOLOGICAL ENGINEERING
LA English
DT Article
DE Peat collapse; Wetland loss; Subsidence; Compaction; Soil strength;
Mississippi delta
ID SUBMERGING COASTAL MARSH; SPARTINA-ALTERNIFLORA; TERREBONNE BAY; WETLAND
LOSS; RIVER DELTA; LAND LOSS; LOUISIANA; PLAIN; ACCRETION; WATER
AB From 1990 to 2004, we carried out a study on accretionary dynamics and wetland loss in salt marshes surrounding two small ponds in the Mississippi delta; Old Oyster Bayou (OB), a sediment-rich area near the mouth of the Atchafalaya River and Bayou Chitigue (BC), a sediment-poor area about 70 km to the east. The OB site was stable, while most of the marsh at BC disappeared within a few years. Measurements were made of short-term sedimentation, vertical accretion, change in marsh surface elevation, pond wave activity, and marsh soil characteristics. The OB marsh was about 10 cm higher than BC; the extremes of the elevation range for Spartina alterniflora in Louisiana. Vertical accretion and short-term sedimentation were about twice as high at BC than at OB, but the OB marsh captured nearly all sediments deposited, while the BC marsh captured <30%. The OB and BC sites flooded about 15% and 85% of the time, respectively. Marsh loss at BC was not due to wave erosion. The mineral content of deposited sediments was higher at OB. Exposure and desiccation of the marsh surface at OB increased the efficiency that deposited sediments were incorporated into the marsh soil, and displaced the marsh surface upward by biological processes like root growth, while also reducing shallow compaction. Once vegetation dies, there is a loss of soil volume clue to loss of root turgor and oxidation of root organic matter, which leads to elevation collapse. Revegetation cannot occur because of the low elevation and weak soil strength. The changes in elevation at both marsh sites are punctuated, occurring in steps that can either increase or decrease elevation. When a marsh is low as at BC, a step down can result in an irreversible change. At this point, the option is not restoration but creating a new marsh with massive sediment input either from the river or via dredging. (C) 2010 Elsevier B.V. All rights reserved.
C1 [Day, John W.; Gambrell, Robert] Louisiana State Univ, Dept Oceanog & Coastal Sci, Baton Rouge, LA 70803 USA.
[Kemp, G. Paul] Natl Audubon Soc, Baton Rouge, LA 70808 USA.
[Reed, Denise J.] Univ New Orleans, Dept Geol, New Orleans, LA 70148 USA.
[Cahoon, Donald R.] USGS Patuxent Wildlife Res Ctr, Beltsville, MD 20705 USA.
[Boumans, Roelof M.] Univ Vermont, Gund Inst Ecol Econ, Burlington, VT 05405 USA.
[Suhayda, Joseph M.] Louisiana State Univ, Hurricane Ctr, Baton Rouge, LA 70803 USA.
RP Day, JW (reprint author), Louisiana State Univ, Dept Oceanog & Coastal Sci, Baton Rouge, LA 70803 USA.
EM johnday@lsu.edu
FU United States Geological Survey [14-08-0001-23411, 04ERAG0068]
FX Funding for this study was provided by the United States Geological
Survey (grants number 14-08-0001-23411 and 04ERAG0068). Additional
funding came from the Louisiana Sea Grant Program. Assistance in the
project was provided by Robert Lane, Numair Latif, David Rogues, Nina de
Luca, Derral Dupre, Wendy Morrison, Laura Dancer, and Jill Rooth.
NR 70
TC 54
Z9 54
U1 11
U2 96
PU ELSEVIER SCIENCE BV
PI AMSTERDAM
PA PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS
SN 0925-8574
J9 ECOL ENG
JI Ecol. Eng.
PD FEB
PY 2011
VL 37
IS 2
BP 229
EP 240
DI 10.1016/j.ecoleng.2010.11.021
PG 12
WC Ecology; Engineering, Environmental; Environmental Sciences
SC Environmental Sciences & Ecology; Engineering
GA 721VX
UT WOS:000287387000015
ER
PT J
AU Gannon, JL
Love, JJ
AF Gannon, J. L.
Love, J. J.
TI USGS 1-min Dst index
SO JOURNAL OF ATMOSPHERIC AND SOLAR-TERRESTRIAL PHYSICS
LA English
DT Article
DE Magnetosphere; Ring current; Dst; Disturbance index
ID RESOLUTION; STORM
AB We produce a 1-min time resolution storm-time disturbance index, the USGS Dst, called Dst(8507-45M). This index is based on minute resolution horizontal magnetic field intensity from low-latitude observatories in Honolulu, Kakioka, San Juan and Hermanus, for the years 1985-2007. The method used to produce the index uses a combination of time- and frequency-domain techniques, which more clearly identifies and excises solar-quiet variation from the horizontal intensity time series of an individual station than the strictly time-domain method used in the Kyoto Dst index. The USGS 1-min Dst is compared against the Kyoto Dst, Kyoto Sym-H, and the USGS 1-h Dst (Dst(5807-4SH)). In a time series comparison, Sym-H is found to produce more extreme values during both sudden impulses and main phase maximum deviation, possibly due to the latitude of its contributing observatories. Both Kyoto indices are shown to have a peak in their distributions below zero, while the USGS indices have a peak near zero. The USGS 1-min Dst is shown to have the higher time resolution benefits of Sym-H, while using the more typical low-latitude observatories of Kyoto Dst. Published by Elsevier Ltd.
C1 [Gannon, J. L.; Love, J. J.] USGS Geomagnetism Program, Denver, CO USA.
RP Gannon, JL (reprint author), USGS Geomagnetism Program, Denver, CO USA.
EM jgannon@usgs.gov
RI Love, Jeffrey/N-7593-2013
OI Love, Jeffrey/0000-0002-3324-0348
FU USGS
FX We thank the Japan Meteorological Agency and the South African National
Research Foundation for their commitment to the long-term operation,
respectively, of the Kakioka and Hermanus magnetic observatories. We
acknowledge Intermagnet (www.intermagnet.org) for its role in promoting
high standards of magnetic-observatory practice. We thank the former
World Data Center at Copenhagen, and the present World Data Centers at
Kyoto and Edinburgh. We thank J.C. Green, C.A. Finn and T. White for
reviewing a draft manuscript. We thank two anonymous referees for their
reviews of the submitted draft manuscript. We thank E.A. McWhirter Jr.
for help with data format conversion. This work and the present
operation of the Honolulu and San Juan observatories are supported by
the USGS Geomagnetism Program.
NR 20
TC 15
Z9 16
U1 0
U2 3
PU PERGAMON-ELSEVIER SCIENCE LTD
PI OXFORD
PA THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND
SN 1364-6826
J9 J ATMOS SOL-TERR PHY
JI J. Atmos. Sol.-Terr. Phys.
PD FEB
PY 2011
VL 73
IS 2-3
SI SI
BP 323
EP 334
DI 10.1016/j.jastp.2010.02.013
PG 12
WC Geochemistry & Geophysics; Meteorology & Atmospheric Sciences
SC Geochemistry & Geophysics; Meteorology & Atmospheric Sciences
GA 717NS
UT WOS:000287055300020
ER
PT J
AU Kaven, JO
Maerten, F
Pollard, DD
AF Kaven, J. O.
Maerten, F.
Pollard, D. D.
TI Mechanical analysis of fault slip data: Implications for paleostress
analysis
SO JOURNAL OF STRUCTURAL GEOLOGY
LA English
DT Article
DE Fault slip data; Paleostress; Stress inversion; Mechanical interaction
ID TRIANGULAR DISLOCATION ELEMENTS; INTERSECTING NORMAL FAULTS; STRESS
INVERSION PROCEDURE; CHI TAIWAN EARTHQUAKE; SAN-ANDREAS FAULT; FOCAL
MECHANISMS; FIELD DATA; DATA SETS; TENSOR INVERSION; SURFACE RUPTURE
AB Stress inversions are a useful and popular tool for structural geologist and seismologist alike. These methods were first introduced by Wallace (1951) and Bott (1959) and subsequent studies continue to be based on their assumptions: the remote stress tensor is spatially uniform for the rock mass containing the faults and temporally constant over the history of faulting in that region, and the slip on each fault surface has the same direction and sense as the maximum shear stress resolved on that surface from the remote stress tensor. Furthermore, successful implementation requires that slip accumulates on faults of diverse orientation. Many studies employ these methods on isolated faults or on fault systems with limited ranges of orientations, which can lead to erroneous results. We propose a new method that incorporates the effects of mechanical interaction of the entire fault or fault system, and solves the complete mechanical problem rather than employing empirical relationships between slip and stress or strain (or strain rate). The method requires knowledge of the fault geometry and information on at least one slip vector component along portions of the known fault geometry. For example, if throw is known, the strike-slip component can be solved for. We test the method using a single synthetic fault with anisotropic roughness similar to that measured at fault outcrops. While the orientation of remote stress may be determined precisely, the lack of diverse fault orientations introduces a systematic error in the remote stress ratio. We further test the effect of diversity of fault orientations and find that Wallace Bott type inversions do not perform as well for limited ranges of orientations when compared to the proposed method. Finally, we use published data from the 1999 Chi-Chi, Taiwan, earthquake, and find that the method using surface data only, and surface data with subsurface focal mechanisms, produce similar results. The resulting stress orientations are in good agreement with results from Wallace Bott inversions. Furthermore, the slip distribution is in general agreement with kinematic slip inversions using coseismic surface deformation. Stress inversion methods using fault slip data can thus be improved upon, significantly in some cases, by solving a mechanical boundary value problem that takes into account the geometry of faults or fault systems. As a bonus, the solution provides the stress, strain, and displacement fields throughout the region and the slip distributions on the faults. (C) 2010 Elsevier Ltd. All rights reserved.
C1 [Maerten, F.] IGEOSS, F-34790 Grabels, France.
[Pollard, D. D.] Stanford Univ, Dept Geol & Environm Sci, Stanford, CA 94305 USA.
RP Kaven, JO (reprint author), USGS Menlo Pk, Menlo Pk, CA 94025 USA.
EM okaven@usgs.gov; fmaerten@igeoss.com; dpollard@standard.edu
FU Stanford Rock Fracture Project
FX Financial support for this project was provided by the Stanford Rock
Fracture Project. We appreciate thorough reviews by R.J. Lisle and an
anonymous reviewer that improved the manuscript. Careful reviews by and
interesting discussions with Paul Segall helped improve the manuscript.
Thanks to the Igeoss consortium members for supporting the development
of Poly3D. We thank Kaj Johnson for providing the coordinates of the
Chelungpu fault trace. We also thank Lei Zhang for providing the results
of his slip inversion.
NR 110
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U1 1
U2 10
PU PERGAMON-ELSEVIER SCIENCE LTD
PI OXFORD
PA THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND
SN 0191-8141
J9 J STRUCT GEOL
JI J. Struct. Geol.
PD FEB
PY 2011
VL 33
IS 2
BP 78
EP 91
DI 10.1016/j.jsg.2010.12.004
PG 14
WC Geosciences, Multidisciplinary
SC Geology
GA 717NV
UT WOS:000287055600003
ER
PT J
AU Hunter, RB
Collett, TS
Boswell, R
Anderson, BJ
Digert, SA
Pospisil, G
Baker, R
Weeks, M
AF Hunter, Robert B.
Collett, Timothy S.
Boswell, Ray
Anderson, Brian J.
Digert, Scott A.
Pospisil, Gordon
Baker, Richard
Weeks, Micaela
TI Mount Elbert Gas Hydrate Stratigraphic Test Well, Alaska North Slope:
Overview of scientific and technical program
SO MARINE AND PETROLEUM GEOLOGY
LA English
DT Editorial Material
DE Gas hydrate; Prudhoe Bay; Mount Elbert test well; Milne Point;
Production test
ID PHYSICAL-PROPERTIES; SEDIMENTS; UNCERTAINTIES; GEOCHEMISTRY; PROSPECT;
HISTORY; LOG
AB The Mount Elbert Gas Hydrate Stratigraphic Test Well was drilled within the Alaska North Slope (ANS) Milne Point Unit (MPU) from February 3 to 19, 2007. The well was conducted as part of a Cooperative Research Agreement (CRA) project co-sponsored since 2001 by BP Exploration (Alaska), Inc. (BPXA) and the U.S. Department of Energy (DOE) in collaboration with the U.S. Geological Survey (USGS) to help determine whether ANS gas hydrate can become a technically and commercially viable gas resource. Early in the effort, regional reservoir characterization and reservoir simulation modeling studies indicated that up to 0.34 trillion cubic meters (tcm; 12 trillion cubic feet, tcf) gas may be technically recoverable from 0.92 tcm (33 tcf) gas-in-place within the Eileen gas hydrate accumulation near industry infrastructure within ANS MPU, Prudhoe Bay Unit (PBU), and Kuparuk River Unit (KRU) areas. To further constrain these estimates and to enable the selection of a test site for further data acquisition. the USGS reprocessed and interpreted MPU 3D seismic data provided by BPXA to delineate 14 prospects containing significant highly-saturated gas hydrate-bearing sand reservoirs. The "Mount Elbert" site was selected to drill a stratigraphic test well to acquire a full suite of wireline log, core, and formation pressure test data. Drilling results and data interpretation confirmed pre-drill predictions and thus increased confidence in both the prospect interpretation methods and in the wider ANS gas hydrate resource estimates. The interpreted data from the Mount Elbert well provide insight into and reduce uncertainty of key gas hydrate-bearing reservoir properties, enable further refinement and validation of the numerical simulation of the production potential of both MPU and broader ANS gas hydrate resources, and help determine viability of potential field sites for future extended term production testing. Drilling and data acquisition operations demonstrated that gas hydrate scientific research programs can be safely, effectively, and efficiently conducted within ANS infrastructure. The program success resulted in a technical team recommendation to project management to drill and complete a long-term production test within the area of existing ANS infrastructure. If approved by stakeholders, this long-term test would build on prior arctic research efforts to better constrain the potential gas rates and volumes that could be produced from gas hydrate-bearing sand reservoirs. (C) 2010 Elsevier Ltd. All rights reserved.
C1 [Hunter, Robert B.] ASRC Energy Serv, Anchorage, AK 99503 USA.
[Collett, Timothy S.] US Geol Survey, Denver Fed Ctr, Denver, CO 80225 USA.
[Boswell, Ray; Anderson, Brian J.; Baker, Richard] Natl Energy Technol Lab, Morgantown, WV 26507 USA.
[Anderson, Brian J.] W Virginia Univ, Dept Chem Engn, Morgantown, WV 26506 USA.
[Digert, Scott A.; Pospisil, Gordon; Weeks, Micaela] BP Explorat Alaska Inc, Anchorage, AK 99518 USA.
RP Hunter, RB (reprint author), ASRC Energy Serv, 3900 C St,Suite 702, Anchorage, AK 99503 USA.
EM robert.hunter@asrcenergy.com
OI Boswell, Ray/0000-0002-3824-2967
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PA THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, OXON, ENGLAND
SN 0264-8172
J9 MAR PETROL GEOL
JI Mar. Pet. Geol.
PD FEB
PY 2011
VL 28
IS 2
BP 295
EP 310
DI 10.1016/j.marpetgeo.2010.02.015
PG 16
WC Geosciences, Multidisciplinary
SC Geology
GA 724AM
UT WOS:000287548500002
ER
PT J
AU Torres, ME
Collett, TS
Rose, KK
Sample, JC
Agena, WF
Rosenbaum, EJ
AF Torres, M. E.
Collett, T. S.
Rose, K. K.
Sample, J. C.
Agena, W. F.
Rosenbaum, E. J.
TI Pore fluid geochemistry from the Mount Elbert Gas Hydrate Stratigraphic
Test Well, Alaska North Slope
SO MARINE AND PETROLEUM GEOLOGY
LA English
DT Article
DE Gas hydrate; Mt Elbert Well; Pore water; Water isotopes; Permafrost
ID ARCTIC-OCEAN; ISOTOPIC FRACTIONATION; WATER; CASCADIA; RIDGE; FLOW; ICE
AB The BPXA-DOE-USGS Mount Elbert Gas Hydrate Stratigraphic Test Well was drilled and cored from 606.5 to 760.1 m on the North Slope of Alaska, to evaluate the occurrence, distribution and formation of gas hydrate in sediments below the base of the ice-bearing permafrost. Both the dissolved chloride and the isotopic composition of the water co-vary in the gas hydrate-bearing zones, consistent with gas hydrate dissociation during core recovery, and they provide independent indicators to constrain the zone of gas hydrate occurrence. Analyses of chloride and water isotope data indicate that an observed increase in salinity towards the top of the cored section reflects the presence of residual fluids from ion exclusion during ice formation at the base of the permafrost layer. These salinity changes are the main factor controlling major and minor ion distributions in the Mount Elbert Well. The resulting background chloride can be simulated with a one-dimensional diffusion model, and the results suggest that the ion exclusion at the top of the cored section reflects deepening of the permafrost layer following the last glaciation (similar to 100 kyr), consistent with published thermal models. Gas hydrate saturation values estimated from dissolved chloride agree with estimates based on logging data when the gas hydrate occupies more than 20% of the pore space; the correlation is less robust at lower saturation values. The highest gas hydrate concentrations at the Mount Elbert Well are clearly associated with coarse-grained sedimentary sections, as expected from theoretical calculations and field observations in marine and other arctic sediment cores. (C) 2009 Elsevier Ltd. All rights reserved.
C1 [Torres, M. E.] Oregon State Univ, Corvallis, OR 97331 USA.
[Collett, T. S.; Agena, W. F.] US Geol Survey, Denver Fed Ctr, Denver, CO 80225 USA.
[Rose, K. K.; Rosenbaum, E. J.] US DOE, Natl Energy Technol Lab, Morgantown, WV 26507 USA.
[Sample, J. C.] No Arizona Univ, Dept Geol, Flagstaff, AZ 86011 USA.
RP Torres, ME (reprint author), Oregon State Univ, 104 COAS Adm Bldg, Corvallis, OR 97331 USA.
EM mtorres@coas.oregonstate.edu
RI Sample, Jane/H-4459-2014; Sample, James/A-9622-2015
OI Sample, Jane/0000-0002-8783-3229;
FU US Department of Energy (DOE); BP Exploration (Alaska) Inc (BPXA)
FX The pore water geochemistry work was funded by a cooperative agreement
between the US Department of Energy (DOE) and BP Exploration (Alaska)
Inc (BPXA), via a contract to M. Torres. We want to acknowledge the US
Geological Survey for additional support, field work planning and
background resources. We thank the drillers and staff at the well site
for their efforts in obtaining high quality cores and providing
logistical support during the field program. Bobbi Conard and Margaret
Sparrow are thanked for their analytical contributions. The manuscript
benefited from helpful reviews by Jerry Dickens and George Claypool, and
from editorial handling by Ray Boswell.
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SN 0264-8172
J9 MAR PETROL GEOL
JI Mar. Pet. Geol.
PD FEB
PY 2011
VL 28
IS 2
BP 332
EP 342
DI 10.1016/j.marpetgeo.2009.10.001
PG 11
WC Geosciences, Multidisciplinary
SC Geology
GA 724AM
UT WOS:000287548500004
ER
PT J
AU Lorenson, TD
Collett, TS
Hunter, RB
AF Lorenson, Thomas D.
Collett, Timothy S.
Hunter, Robert B.
TI Gas geochemistry of the Mount Elbert Gas Hydrate Stratigraphic Test
Well, Alaska North Slope: Implications for gas hydrate exploration in
the Arctic
SO MARINE AND PETROLEUM GEOLOGY
LA English
DT Article
DE Gas hydrate; Arctic; Alaska; North slope; Gas geochemistry;
Hydrocarbons; Isotopes; Biodegraded oil
ID DEEP SUBSURFACE; PRUDHOE BAY; OIL; BIODEGRADATION; PROSPECT; KUPARUK;
MARINE; CO2
AB Gases were analyzed from well cuttings, core, gas hydrate, and formation tests at the BPXA-DOE-USGS Mount Elbert Gas Hydrate Stratigraphic Test Well, drilled within the Milne Point Unit, Alaska North Slope. The well penetrated a portion of the Eileen gas hydrate deposit, which overlies the more deeply buried Prudhoe Bay, Milne Point, West Sak, and Kuparuk River oil fields. Gas sources in the upper 200 m are predominantly from microbial sources (C-1 isotopic compositions ranging from -86.4 to -80.6 parts per thousand). The C-1 isotopic composition becomes progressively enriched from 200 m to the top of the gas hydrate-bearing sands at 600 m. The tested gas hydrates occur in two primary intervals, units D and C, between 614.0 m and 664.7 m, containing a total of 29.3 m of gas hydrate-bearing sands. The hydrocarbon gases in cuttings and core samples from 604 to 914 m are composed of methane with very little ethane. The isotopic composition of the methane carbon ranges from -50.1 to -43.9 parts per thousand with several outliers, generally decreasing with depth. Gas samples collected by the Modular Formation Dynamics Testing (MDT) tool in the hydrate-bearing units were similarly composed mainly of methane, with up to 284 ppm ethane. The methane isotopic composition ranged from -48.2 to -48.0 parts per thousand in the C sand and from -48.4 to -46.6 parts per thousand in the D sand. Methane hydrogen isotopic composition ranged from 238 to -230 parts per thousand with slightly more depleted values in the deeper C sand. These results are consistent with the concept that the Eileen gas hydrates contain a mixture of deep-sourced, microbially biodegraded thermogenic gas, with lesser amounts of thermogenic oil-associated gas, and coal gas. Thermal gases are likely sourced from existing oil and gas accumulations that have migrated up-dip and/or up-fault and formed gas hydrate in response to climate cooling with permafrost formation. Published by Elsevier Ltd.
C1 [Lorenson, Thomas D.] US Geol Survey, Menlo Pk, CA 94025 USA.
[Collett, Timothy S.] US Geol Survey, Denver Fed Ctr, Denver, CO 80225 USA.
[Hunter, Robert B.] ASRC Energy Serv, Anchorage, AK 99503 USA.
RP Lorenson, TD (reprint author), US Geol Survey, 345 Middlefield Rd,MS 999, Menlo Pk, CA 94025 USA.
EM tlorenson@usgs.gov
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SN 0264-8172
J9 MAR PETROL GEOL
JI Mar. Pet. Geol.
PD FEB
PY 2011
VL 28
IS 2
BP 343
EP 360
DI 10.1016/j.marpetgeo.2010.02.007
PG 18
WC Geosciences, Multidisciplinary
SC Geology
GA 724AM
UT WOS:000287548500005
ER
PT J
AU Kneafsey, TJ
Lu, HL
Winters, W
Boswell, R
Hunter, R
Collett, TS
AF Kneafsey, Timothy J.
Lu, Hailong
Winters, William
Boswell, Ray
Hunter, Robert
Collett, Timothy S.
TI Examination of core samples from the Mount Elbert Gas Hydrate
Stratigraphic Test Well, Alaska North Slope: Effects of retrieval and
preservation
SO MARINE AND PETROLEUM GEOLOGY
LA English
DT Article
DE Gas hydrate; Core handling; Core disturbance; Dissociation; Thermal
processes
ID METHANE HYDRATE; GEOCHEMISTRY; SEDIMENT
AB Collecting and preserving undamaged core samples containing gas hydrates from depth is difficult because of the pressure and temperature changes encountered upon retrieval. Hydrate-bearing core samples were collected at the BPXA-DOE-USGS Mount Elbert Gas Hydrate Stratigraphic Test Well in February 2007. Coring was performed while using a custom oil-based drilling mud, and the cores were retrieved by a wireline. The samples were characterized and subsampled at the surface under ambient winter arctic conditions. Samples thought to be hydrate bearing were preserved either by immersion in liquid nitrogen (LN), or by storage under methane pressure at ambient arctic conditions, and later depressurized and immersed in LN. Eleven core samples from hydrate-bearing zones were scanned using x-ray computed tomography to examine core structure and homogeneity. Features observed include radial fractures, spalling-type fractures, and reduced density near the periphery. These features were induced during sample collection, handling, and preservation. Isotopic analysis of the methane from hydrate in an initially LN-preserved core and a pressure-preserved core indicate that secondary hydrate formation occurred throughout the pressurized core, whereas none occurred in the LN-preserved core, however no hydrate was found near the periphery of the LN-preserved core. To replicate some aspects of the preservation methods, natural and laboratory-made saturated porous media samples were frozen in a variety of ways, with radial fractures observed in some LN-frozen sands, and needle-like ice crystals forming in slowly frozen clay-rich sediments. Suggestions for hydrate-bearing core preservation are presented. (C) 2009 Elsevier Ltd. All rights reserved.
C1 [Kneafsey, Timothy J.] Univ Calif Berkeley, Lawrence Berkeley Lab, Berkeley, CA 94720 USA.
[Lu, Hailong] Natl Res Council Canada, Steacie Inst Mol Sci, Ottawa, ON, Canada.
[Winters, William] US Geol Survey, Woods Hole, MA 02543 USA.
[Boswell, Ray] US DOE, Natl Energy Technol Lab, Morgantown, WV USA.
[Collett, Timothy S.] US Geol Survey, Denver Fed Ctr, Denver, CO 80225 USA.
RP Kneafsey, TJ (reprint author), Univ Calif Berkeley, Lawrence Berkeley Lab, 1 Cyclotron Rd, Berkeley, CA 94720 USA.
EM tjkneafsey@lbl.gov
RI Kneafsey, Timothy/H-7412-2014;
OI Kneafsey, Timothy/0000-0002-3926-8587; Boswell, Ray/0000-0002-3824-2967
FU Office of Natural Gas and Petroleum Technology, through the National
Energy Technology Laboratory, under the U.S. DOE [DE-AC02-05CH11231]
FX The authors wish first to acknowledge the many people whose diligent
efforts made it possible to collect the samples discussed in this paper.
A portion of this work was supported by the Assistant Secretary for
Fossil Energy, Office of Natural Gas and Petroleum Technology, through
the National Energy Technology Laboratory, under the U.S. DOE Contract
No. DE-AC02-05CH11231.
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SN 0264-8172
J9 MAR PETROL GEOL
JI Mar. Pet. Geol.
PD FEB
PY 2011
VL 28
IS 2
BP 381
EP 393
DI 10.1016/j.marpetgeo.2009.10.009
PG 13
WC Geosciences, Multidisciplinary
SC Geology
GA 724AM
UT WOS:000287548500007
ER
PT J
AU Lee, MW
Collett, TS
AF Lee, M. W.
Collett, T. S.
TI In-situ gas hydrate hydrate saturation estimated from various well logs
at the Mount Elbert Gas Hydrate Stratigraphic Test Well, Alaska North
Slope
SO MARINE AND PETROLEUM GEOLOGY
LA English
DT Article
DE Gas hydrate; Saturation; Mount Elbert; Well logs; Rock physics model
ID NATURAL-GAS; BEARING SEDIMENTS; VELOCITIES
AB In 2006, the U.S. Geological Survey (USGS) completed detailed analysis and interpretation of available 2-D and 3-D seismic data and proposed a viable method for identifying sub-permafrost gas hydrate prospects within the gas hydrate stability zone in the Milne Point area of northern Alaska. To validate the predictions of the USGS and to acquire critical reservoir data needed to develop a long-term production testing program, a well was drilled at the Mount Elbert prospect in February, 2007. Numerous well log data and cores were acquired to estimate in-situ gas hydrate saturations and reservoir properties.
Gas hydrate saturations were estimated from various well logs such as nuclear magnetic resonance (NMR), P- and S-wave velocity, and electrical resistivity logs along with pore-water salinity. Gas hydrate saturations from the NMR log agree well with those estimated from P- and S-wave velocity data. Because of the low salinity of the connate water and the low formation temperature, the resistivity of connate water is comparable to that of shale. Therefore, the effect of clay should be accounted for to accurately estimate gas hydrate saturations from the resistivity data. Two highly gas hydrate-saturated intervals are identified - an upper similar to 43 ft zone with an average gas hydrate saturation of 54% and a lower similar to 53 ft zone with an average gas hydrate saturation of 50%; both zones reach a maximum of about 75% saturation. Published by Elsevier Ltd.
C1 [Lee, M. W.; Collett, T. S.] US Geol Survey, Denver, CO 80225 USA.
RP Lee, MW (reprint author), US Geol Survey, Box 25046,MS 939 Denver Fed Ctr, Denver, CO 80225 USA.
EM mlee@usgs.gov
FU U. S. Geological Survey; U. S. Department of Energy [DE-AI21-92MC29214];
U. S. Bureau of Land Management [LAI-02-0015]
FX We thank the Mount Elbert Science Team for the successful logging and
coring program, and we appreciate Warren Agena and Tanya Inks for their
many helpful comments and suggestions. This contribution was funded by
the U. S. Geological Survey Energy Resources Program, the U. S.
Department of Energy (under Interagency Agreement No.
DE-AI21-92MC29214), and the U. S. Bureau of Land Management (under
Interagency Agreement No. LAI-02-0015).
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SN 0264-8172
J9 MAR PETROL GEOL
JI Mar. Pet. Geol.
PD FEB
PY 2011
VL 28
IS 2
BP 439
EP 449
DI 10.1016/j.marpetgeo.2009.06.007
PG 11
WC Geosciences, Multidisciplinary
SC Geology
GA 724AM
UT WOS:000287548500013
ER
PT J
AU Sun, Y
Goldberg, D
Collett, T
Hunter, R
AF Sun, Y.
Goldberg, D.
Collett, T.
Hunter, R.
TI High-resolution well-log derived dielectric properties of
gas-hydrate-bearing sediments, Mount Elbert Gas Hydrate Stratigraphic
Test Well, Alaska North Slope
SO MARINE AND PETROLEUM GEOLOGY
LA English
DT Article
DE Gas hydrates; Saturation; Dielectric property
ID METHANE HYDRATE; RESERVOIR
AB A dielectric logging tool, electromagnetic propagation tool (EPT), was deployed in 2007 in the BPXA-DOE-USGS Mount Elbert Gas Hydrate Stratigraphic Test Well (Mount Elbert Well), North Slope, Alaska. The measured dielectric properties in the Mount Elbert well, combined with density log measurements, result in a vertical high-resolution (cm-scale) estimate of gas hydrate saturation. Two hydrate-bearing sand reservoirs about 20 m thick were identified using the EPT log and exhibited gas-hydrate saturation estimates ranging from 45% to 85%. In hydrate-bearing zones where variation of hole size and oil-based mud invasion are minimal, EPT-based gas hydrate saturation estimates on average agree well with lower vertical resolution estimates from the nuclear magnetic resonance logs; however, saturation and porosity estimates based on EPT logs are not reliable in intervals with substantial variations in borehole diameter and oil-based invasion.
EPT log interpretation reveals many thin-bedded layers at various depths, both above and below the thick continuous hydrate occurrences, which range from 30-cm to about 1-m thick. Such thin layers are not indicated in other well logs, or from the visual observation of core, with the exception of the image log recorded by the oil-base microimager. We also observe that EPT dielectric measurements can be used to accurately detect fine-scale changes in lithology and pore fluid properties of hydrate-bearing sediments where variation of hole size is minimal. EPT measurements may thus provide high-resolution in-situ hydrate saturation estimates for comparison and calibration with laboratory analysis. (C) 2010 Elsevier Ltd. All rights reserved.
C1 [Sun, Y.] Texas A&M Univ, Dept Geol & Geophys, College Stn, TX 77843 USA.
[Goldberg, D.] Columbia Univ, Lamont Doherty Earth Observ, Palisades, NY USA.
[Collett, T.] US Geol Survey, Denver, CO 80225 USA.
[Hunter, R.] ASRC Energy Serv, Anchorage, AK USA.
RP Sun, Y (reprint author), Texas A&M Univ, Dept Geol & Geophys, College Stn, TX 77843 USA.
EM sun@geo.tamu.edu
FU U.S. Department of Energy; BP Exploration (Alaska) Inc.
FX We thank the U.S. Department of Energy and the BP Exploration (Alaska)
Inc. for supporting this research. Constructive comments and critical
reviews by the anonymous reviewer and R.L. Kleinberg greatly improved
the manuscript.
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SN 0264-8172
J9 MAR PETROL GEOL
JI Mar. Pet. Geol.
PD FEB
PY 2011
VL 28
IS 2
BP 450
EP 459
DI 10.1016/j.marpetgeo.2010.03.001
PG 10
WC Geosciences, Multidisciplinary
SC Geology
GA 724AM
UT WOS:000287548500014
ER
PT J
AU Anderson, B
Hancock, S
Wilson, S
Enger, C
Collett, T
Boswell, R
Hunter, R
AF Anderson, Brian
Hancock, Steve
Wilson, Scott
Enger, Christopher
Collett, Timothy
Boswell, Ray
Hunter, Robert
TI Formation pressure testing at the Mount Elbert Gas Hydrate Stratigraphic
Test Well, Alaska North Slope: Operational summary, history matching,
and interpretations
SO MARINE AND PETROLEUM GEOLOGY
LA English
DT Article
DE Gas hydrates; Reservoir simulations; Production modeling; Porous media;
Modular dynamics testing
AB In February 2007, the U.S. Department of Energy, BP Exploration (Alaska), and the U.S. Geological Survey, collected open-hole pressure-response data, as well as gas and water sample collection, in a gas hydrate reservoir (the BPXA-DOE-USGS Mount Elbert Gas Hydrate Stratigraphic Test Well) using Schlumberger's Modular Dynamics Formation Tester (MDT) wireline tool. Four such MDT tests, ranging from six to twelve hours duration, and including a series of flow, sampling, and shut-in periods of various durations, were conducted. Locations for the testing were selected based on NMR and other log data to assure sufficient isolation from reservoir boundaries and zones of excess free water. Test stages in which pressure was reduced sufficiently to mobilize free water in the formation (yet not cause gas hydrate dissociation) produced readily interpretable pressure build-up profiles. Build-ups following larger drawdowns consistently showed gas-hydrate dissociation and gas release (as confirmed by optical fluid analyzer data), as well as progressive dampening of reservoir pressure build-up during sequential tests at a given MDT test station.
History matches of one multi-stage, 12-h test (the C2 test) were accomplished using five different reservoir simulators: CMG-STARS, HydrateResSim, MH21-HYDRES, STOMP-HYD, and TOUGH + HYDRATE. Simulations utilized detailed information collected across the reservoir either obtained or determined from geophysical well logs, including thickness (11.3 m, 37 ft.), porosity (35%), hydrate saturation (65%), both mobile and immobile water saturations, intrinsic permeability (1000 mD), pore water salinity (5 ppt), and formation temperature (3.3-3.9 degrees C). This paper will present the approach and preliminary results of the history-matching efforts, including estimates of initial formation permeability and analyses of the various unique features exhibited by the MDT results. (C) 2010 Elsevier Ltd. All rights reserved.
C1 [Anderson, Brian] W Virginia Univ, Dept Chem Engn, Morgantown, WV 26506 USA.
[Anderson, Brian; Boswell, Ray] Natl Energy Technol Lab, Morgantown, WV 26507 USA.
[Hancock, Steve] RPS Energy Canada, Calgary, AB T2P 3T6, Canada.
[Wilson, Scott] Ryder Scott Co, Petr Consultants, Denver, CO 80293 USA.
[Enger, Christopher] Colorado Sch Mines, Rock Mech Lab, Golden, CO 80401 USA.
[Collett, Timothy] US Geol Survey, Denver Fed Ctr, Denver, CO 80225 USA.
[Hunter, Robert] ASRC Energy Serv, Anchorage, AK 99503 USA.
RP Anderson, B (reprint author), W Virginia Univ, Dept Chem Engn, Morgantown, WV 26506 USA.
EM brian.anderson@mail.wvu.edu
OI Boswell, Ray/0000-0002-3824-2967
FU National Energy Technology Laboratory of the U.S. Department of Energy;
U.S. Geological Survey; Japan MH-21 project; BP Exploration (Alaska)
FX The authors would like to thank the National Energy Technology
Laboratory of the U.S. Department of Energy, the U.S. Geological Survey,
the Japan MH-21 project, and BP Exploration (Alaska) for supporting this
effort. We would also like to acknowledge the Mount Elbert science party
for sharing the data obtained at Mount Elbert for use in our
history-matching and production simulations. Finally, the authors would
like to thank Michael Batzle for his supervision of the experimental
simulation and Marisa Rydzy for the original experimental apparatus.
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J9 MAR PETROL GEOL
JI Mar. Pet. Geol.
PD FEB
PY 2011
VL 28
IS 2
BP 478
EP 492
DI 10.1016/j.marpetgeo.2010.02.012
PG 15
WC Geosciences, Multidisciplinary
SC Geology
GA 724AM
UT WOS:000287548500016
ER
PT J
AU Collett, TS
Lewis, RE
Winters, WJ
Lee, MW
Rose, KK
Boswell, RM
AF Collett, T. S.
Lewis, R. E.
Winters, W. J.
Lee, M. W.
Rose, K. K.
Boswell, R. M.
TI Downhole well log and core montages from the Mount Elbert Gas Hydrate
Stratigraphic Test Well, Alaska North Slope
SO MARINE AND PETROLEUM GEOLOGY
LA English
DT Article
DE Gas hydrate; Alaska; Resources; Logs; Core; North Slope; Drilling
ID BEARING SEDIMENTS; GEOCHEMISTRY
AB The BPXA-DOE-USGS Mount Elbert Gas Hydrate Stratigraphic Test Well was an integral part of an ongoing project to determine the future energy resource potential of gas hydrates on the Alaska North Slope. As part of this effort, the Mount Elbert well included an advanced downhole geophysical logging program. Because gas hydrate is unstable at ground surface pressure and temperature conditions, a major emphasis was placed on the downhole-logging program to determine the occurrence of gas hydrates and the in-situ physical properties of the sediments. In support of this effort, well-log and core data montages have been compiled which include downhole log and core-data obtained from the gas-hydrate-bearing sedimentary section in the Mount Elbert well. Also shown are numerous reservoir parameters, including gas-hydrate saturation and sediment porosity log traces calculated from available downhole well log and core data. Published by Elsevier Ltd.
C1 [Collett, T. S.; Lee, M. W.] US Geol Survey, Denver Fed Ctr, Denver, CO 80225 USA.
[Lewis, R. E.] Schlumberger, Oklahoma City, OK 73114 USA.
[Winters, W. J.] US Geol Survey, Woods Hole, MA 02543 USA.
[Rose, K. K.; Boswell, R. M.] US DOE, Natl Energy Technol Lab, Morgantown, WV 26507 USA.
RP Collett, TS (reprint author), US Geol Survey, Denver Fed Ctr, MS 939,Box 25046, Denver, CO 80225 USA.
EM tcollett@usgs.gov
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SN 0264-8172
J9 MAR PETROL GEOL
JI Mar. Pet. Geol.
PD FEB
PY 2011
VL 28
IS 2
BP 561
EP 577
DI 10.1016/j.marpetgeo.2010.03.016
PG 17
WC Geosciences, Multidisciplinary
SC Geology
GA 724AM
UT WOS:000287548500022
ER
PT J
AU Boswell, R
Rose, K
Collett, TS
Lee, M
Winters, W
Lewis, KA
Agena, W
AF Boswell, Ray
Rose, Kelly
Collett, Timothy S.
Lee, Myung
Winters, William
Lewis, Kristen A.
Agena, Warren
TI Geologic controls on gas hydrate occurrence in the Mount Elbert
prospect, Alaska North Slope
SO MARINE AND PETROLEUM GEOLOGY
LA English
DT Article
DE Mount Elbert well; Gas hydrate; Alaska North Slope; Milne Point;
Sagavanirktok formation
ID METHANE HYDRATE
AB Data acquired at the BPXA-DOE-USGS Mount Elbert Gas Hydrate Stratigraphic Test Well, drilled in the Milne Point area of the Alaska North Slope in February, 2007, indicates two zones of high gas hydrate saturation within the Eocene Sagavanirktok Formation. Gas hydrate is observed in two separate sand reservoirs (the D and C units), in the stratigraphically highest portions of those sands, and is not detected in non-sand lithologies. In the younger D unit, gas hydrate appears to fill much of the available reservoir space at the top of the unit. The degree of vertical fill with the D unit is closely related to the unit reservoir quality. A thick, low-permeability clay-dominated unit serves as an upper seal, whereas a subtle transition to more clay-rich, and interbedded sand, silt, and clay units is associated with the base of gas hydrate occurrence. In the underlying C unit, the reservoir is similarly capped by a clay-dominated section, with gas hydrate filling the relatively lower-quality sands at the top of the unit leaving an underlying thick section of high-reservoir quality sands devoid of gas hydrate. Evaluation of well log, core, and seismic data indicate that the gas hydrate occurs within complex combination stratigraphic/structural traps. Structural trapping is provided by a four-way fold closure augmented by a large western bounding fault. Lithologic variation is also a likely strong control on lateral extent of the reservoirs, particularly in the D unit accumulation, where gas hydrate appears to extend beyond the limits of the structural closure. Porous and permeable zones within the C unit sand are only partially charged due most likely to limited structural trapping in the reservoir lithofacies during the period of primary charging. The occurrence of the gas hydrate within the sands in the upper portions of both the C and D units and along the crest of the fold is consistent with an interpretation that these deposits are converted free gas accumulations formed prior to the imposition of gas hydrate stability conditions. Published by Elsevier Ltd.
C1 [Boswell, Ray; Rose, Kelly] US DOE, Natl Energy Technol Lab, Morgantown, WV 26507 USA.
[Collett, Timothy S.; Lee, Myung; Lewis, Kristen A.; Agena, Warren] US Geol Survey, Denver, CO 80225 USA.
[Winters, William] US Geol Survey, Woods Hole, MA 02543 USA.
RP Boswell, R (reprint author), US DOE, Natl Energy Technol Lab, Morgantown, WV 26507 USA.
EM ray.boswell@netl.doe.gov
OI Boswell, Ray/0000-0002-3824-2967
NR 44
TC 23
Z9 27
U1 1
U2 14
PU ELSEVIER SCI LTD
PI OXFORD
PA THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, OXON, ENGLAND
SN 0264-8172
J9 MAR PETROL GEOL
JI Mar. Pet. Geol.
PD FEB
PY 2011
VL 28
IS 2
BP 589
EP 607
DI 10.1016/j.marpetgeo.2009.12.004
PG 19
WC Geosciences, Multidisciplinary
SC Geology
GA 724AM
UT WOS:000287548500024
ER
PT J
AU Philibosian, B
Fumal, T
Weldon, R
AF Philibosian, Belle
Fumal, Thomas
Weldon, Ray
TI San Andreas Fault Earthquake Chronology and Lake Cahuilla History at
Coachella, California
SO BULLETIN OF THE SEISMOLOGICAL SOCIETY OF AMERICA
LA English
DT Article
ID MISSION CREEK STRAND; SOUTHERN-CALIFORNIA; HECTOR MINE; SLIP-RATE;
PALEOSEISMIC SITE; IMPERIAL-VALLEY; PALMS OASIS; WRIGHTWOOD; ZONE;
PALEOEARTHQUAKES
AB The southernmost similar to 100 km of the San Andreas fault has not ruptured historically. It is imperative to determine its rupture history to better predict its future behavior. This paleoseismic investigation in Coachella, California, establishes a chronology of at least five and up to seven major earthquakes during the past similar to 1100 yr. This chronology yields a range of average recurrence intervals between 116 and 221 yr, depending on assumptions, with a best-estimate average recurrence interval of 180 yr. The most recent earthquake occurred c. 1690, more than 300 yr ago, suggesting that this stretch of the fault has accumulated a large amount of tectonic stress and is likely to rupture in the near future, assuming the fault follows a stress renewal model. This study also establishes the timing of the past 5-6 highstands of ancient Lake Cahuilla since A. D. 800. We found that earthquakes do not tend to occur at any particular stage in the lake cycle.
C1 [Philibosian, Belle] CALTECH, Div Geol & Planetary Sci, Pasadena, CA 91125 USA.
[Fumal, Thomas] US Geol Survey, Menlo Pk, CA 94025 USA.
[Weldon, Ray] Univ Oregon, Dept Geol Sci, Eugene, OR 97403 USA.
RP Philibosian, B (reprint author), CALTECH, Div Geol & Planetary Sci, M-C 100-23, Pasadena, CA 91125 USA.
EM belle@gps.caltech.edu; tfumal@usgs.gov
OI Philibosian, Belle/0000-0003-3138-4716
FU USGS [07HQGR0019, 06HQAG0143]; University of Oregon; National Science
Foundation
FX This research was funded by USGS NEHRP grant #07HQGR0019, USGS grant
#06HQAG0143, and internal funding from the University of Oregon. Belle
Philibosian was supported by a National Science Foundation Graduate
Research Fellowship. We are extremely grateful to Rilington Communities
for granting access to their property and to Matt Cohrt and Doug Cook of
Sladden Engineering for accommodating our study. We would like to thank
Katherine Kendrick, Kate Scharer, Sean Bemis, Reed Burgette, Beth
Wisely, Nissa Morton, and Mike O'Bleness for their invaluable assistance
in the field; Malcolm Britton, Lorna Crider, Tyler Claycomb, and Sarah
Hunt for assistance with image processing; and Ken Hudnut of USGS for
assistance with funding acquisition and LiDAR data. For assistance with
carbon dating, we thank Michaele Kashgarian and Paula Zermeno of the
Center for Acceleration Mass Spectrometry at Lawrence Livermore National
Laboratory, Douglas Kennett and Brian Culleton of the Coastal
Archaeology and Human Ecology Laboratory at the University of Oregon,
and John Southon of the Keck Carbon Cycle Accelerator Mass Spectrometry
Laboratory at the University of California, Irvine. This paper was
greatly improved thanks to thoughtful reviews by Katherine Kendrick, Rob
Langridge, Tom Rockwell, and Pat Williams.
NR 53
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U1 0
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PU SEISMOLOGICAL SOC AMER
PI EL CERRITO
PA PLAZA PROFESSIONAL BLDG, SUITE 201, EL CERRITO, CA 94530 USA
SN 0037-1106
J9 B SEISMOL SOC AM
JI Bull. Seismol. Soc. Amer.
PD FEB
PY 2011
VL 101
IS 1
BP 13
EP 38
DI 10.1785/0120100050
PG 26
WC Geochemistry & Geophysics
SC Geochemistry & Geophysics
GA 711WY
UT WOS:000286623300002
ER
PT J
AU Field, EH
Page, MT
AF Field, Edward H.
Page, Morgan T.
TI Estimating Earthquake-Rupture Rates on a Fault or Fault System
SO BULLETIN OF THE SEISMOLOGICAL SOCIETY OF AMERICA
LA English
DT Article
ID 2004 PARKFIELD EARTHQUAKE; FREQUENCY-DISTRIBUTION; PREDICTION; SLIP
AB Previous approaches used to determine the rates of different earthquakes on a fault have made assumptions regarding segmentation, have been difficult to document and reproduce, and have lacked the ability to satisfy all available data constraints. We present a relatively objective and reproducible inverse methodology for determining the rate of different ruptures on a fault or fault system. The data used in the inversion include slip rate, event rate, and other constraints such as an optional a priori magnitude-frequency distribution. We demonstrate our methodology by solving for the long-term rate of ruptures on the southern San Andreas fault. Our results imply that a Gutenberg-Richter distribution is consistent with the data available for this fault; however, more work is needed to test the robustness of this assertion. More importantly, the methodology is extensible to an entire fault system (thereby including multifault ruptures) and can be used to quantify the relative benefits of collecting additional paleoseismic data at different sites.
C1 [Field, Edward H.] US Geol Survey, Denver, CO 80225 USA.
[Page, Morgan T.] US Geol Survey, Pasadena, CA 91106 USA.
RP Field, EH (reprint author), US Geol Survey, POB 25046,Mail Stop 966, Denver, CO 80225 USA.
NR 28
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U1 0
U2 1
PU SEISMOLOGICAL SOC AMER
PI ALBANY
PA 400 EVELYN AVE, SUITE 201, ALBANY, CA 94706-1375 USA
SN 0037-1106
EI 1943-3573
J9 B SEISMOL SOC AM
JI Bull. Seismol. Soc. Amer.
PD FEB
PY 2011
VL 101
IS 1
BP 79
EP 92
DI 10.1785/0120100004
PG 14
WC Geochemistry & Geophysics
SC Geochemistry & Geophysics
GA 711WY
UT WOS:000286623300005
ER
PT J
AU Rubinstein, JL
AF Rubinstein, Justin L.
TI Nonlinear Site Response in Medium Magnitude Earthquakes near Parkfield,
California
SO BULLETIN OF THE SEISMOLOGICAL SOCIETY OF AMERICA
LA English
DT Article
ID STRONG GROUND MOTION; LOMA-PRIETA EARTHQUAKE; DENSE SEISMOGRAPH ARRAY;
TEMPORAL-CHANGES; DOWNHOLE ARRAY; VELOCITY; WAVES; UPSAR; FAULT; ROCK
AB Careful analysis of strong-motion recordings of 13 medium magnitude earthquakes (3.7 <= M <= 6.5) in the Parkfield, California, area shows that very modest levels of shaking (approximately 3.5% of the acceleration of gravity) can produce observable changes in site response. Specifically, I observe a drop and subsequent recovery of the resonant frequency at sites that are part of the USGS Parkfield dense seismograph array (UPSAR) and Turkey Flat array. While further work is necessary to fully eliminate other models, given that these frequency shifts correlate with the strength of shaking at the Turkey Flat array and only appear for the strongest shaking levels at UPSAR, the most plausible explanation for them is that they are a result of nonlinear site response. Assuming this to be true, the observation of nonlinear site response in small (M < 5) earthquakes implies that nonlinear site response can occur at much lower levels of shaking than previously believed. Below I present observations of a resonant frequency shift during five M <= 5 earthquakes near Parkfield, California, strongly contrasting with previous studies that have only identified nonlinear site effects for much larger events. In addition to the nonlinear effects seen for the smaller events, nonlinear site response is also observed for two largest earthquakes in the region during the study period (the 2003 M 6.5 San Simeon earthquake and the 2004 M 6 Parkfield earthquake).
C1 US Geol Survey, Menlo Pk, CA 94025 USA.
RP Rubinstein, JL (reprint author), US Geol Survey, 345 Middlefield Rd,MS-977, Menlo Pk, CA 94025 USA.
EM jrubinstein@usgs.gov
OI Rubinstein, Justin/0000-0003-1274-6785
NR 41
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U1 0
U2 2
PU SEISMOLOGICAL SOC AMER
PI ALBANY
PA 400 EVELYN AVE, SUITE 201, ALBANY, CA 94706-1375 USA
SN 0037-1106
EI 1943-3573
J9 B SEISMOL SOC AM
JI Bull. Seismol. Soc. Amer.
PD FEB
PY 2011
VL 101
IS 1
BP 275
EP 286
DI 10.1785/0120090396
PG 12
WC Geochemistry & Geophysics
SC Geochemistry & Geophysics
GA 711WY
UT WOS:000286623300018
ER
PT J
AU Klein, ES
Berg, EE
Dial, R
AF Klein, Eric S.
Berg, Edward E.
Dial, Roman
TI Reply to comment by Gracz on "Wetland drying and succession across the
Kenai Peninsula Lowlands, south-central Alaska"
SO CANADIAN JOURNAL OF FOREST RESEARCH-REVUE CANADIENNE DE RECHERCHE
FORESTIERE
LA English
DT Editorial Material
ID PEAT; TUNDRA; FIELD
AB Gracz (2011, Can. J. For. Res. 41: 425-428) proposes that the Good Friday earthquake of 1964 caused falling lake levels and drying wetlands on Alaska's Northern Kenai Lowlands (NKL). His hypothesis states that the earthquake increased hydraulic conductivity by fracturing a leaky confining layer, accelerating drainage of surface water into regional aquifers. We counter that a single model of draining does not apply across the heterogeneity of geomorphology and soils on the NKL. In particular, the NKL's glacial history precludes uniform application of a subsurface hydrologic model for lake draining and the nature of peat-based wetlands precludes its application to wetland drying. Instead, small, yet cumulative, climatic reductions in moisture surplus explain both observed lake level declines and vegetation changes. Moreover, and unlike a climatic hypothesis, a seismic hypothesis fails to explain lake drying elsewhere in Alaska. Although it is likely that the earthquake influenced some hydrologic features in the NKL, it is unlikely that a single hydrologic model based on a simple mechanical cause, e. g., downward drainage, adequately explains the changes observed across the whole NKL. Conversely, we maintain that the uniformity of the vegetation response seen across different landscapes, including wetlands, forests, and alpine areas, throughout the state of Alaska strongly supports a climatic hypothesis.
C1 [Klein, Eric S.] Lehigh Univ, Earth & Environm Sci Dept, Bethlehem, PA 18015 USA.
[Berg, Edward E.] US Fish & Wildlife Serv, Soldotna, AK 99669 USA.
[Dial, Roman] Alaska Pacific Univ, Dept Environm Sci, Anchorage, AK 99508 USA.
RP Klein, ES (reprint author), Lehigh Univ, Earth & Environm Sci Dept, 1 W Packer Ave, Bethlehem, PA 18015 USA.
EM esk209@lehigh.edu
NR 25
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U1 1
U2 7
PU CANADIAN SCIENCE PUBLISHING, NRC RESEARCH PRESS
PI OTTAWA
PA 1200 MONTREAL ROAD, BUILDING M-55, OTTAWA, ON K1A 0R6, CANADA
SN 0045-5067
J9 CAN J FOREST RES
JI Can. J. For. Res.-Rev. Can. Rech. For.
PD FEB
PY 2011
VL 41
IS 2
BP 429
EP 433
DI 10.1139/X10-216
PG 5
WC Forestry
SC Forestry
GA 709XW
UT WOS:000286475700022
ER
PT J
AU Olsen, JB
Crane, PA
Flannery, BG
Dunmall, K
Templin, WD
Wenburg, JK
AF Olsen, Jeffrey B.
Crane, Penelope A.
Flannery, Blair G.
Dunmall, Karen
Templin, William D.
Wenburg, John K.
TI Comparative landscape genetic analysis of three Pacific salmon species
from subarctic North America
SO CONSERVATION GENETICS
LA English
DT Article
DE Landscape genetics; Pacific salmon; Population structure; Subarctic
ID POPULATION-STRUCTURE; ATLANTIC SALMON; CHINOOK SALMON; CHUM SALMON;
ENVIRONMENTAL-FACTORS; WESTERN ALASKA; DISTANCE; RIVER; SOFTWARE;
PATTERNS
AB We examined the assumption that landscape heterogeneity similarly influences the spatial distribution of genetic diversity in closely related and geographically overlapping species. Accordingly, we evaluated the influence of watershed affiliation and nine habitat variables from four categories (spatial isolation, habitat size, climate, and ecology) on population divergence in three species of Pacific salmon (Oncorhynchus tshawytscha, O. kisutch, and O. keta) from three contiguous watersheds in subarctic North America. By incorporating spatial data we found that the three watersheds did not form the first level of hierarchical population structure as predicted. Instead, each species exhibited a broadly similar spatial pattern: a single coastal group with populations from all watersheds and one or more inland groups primarily in the largest watershed. These results imply that the spatial scale of conservation should extend across watersheds rather than at the watershed level which is the scale for fishery management. Three independent methods of multivariate analysis identified two variables as having influence on population divergence across all watersheds: precipitation in all species and subbasin area (SBA) in Chinook. Although we found general broad-scale congruence in the spatial patterns of population divergence and evidence that precipitation may influence population divergence in each species, we also found differences in the level of population divergence (coho > Chinook and chum) and evidence that SBA may influence population divergence only in Chinook. These differences among species support a species-specific approach to evaluating and planning for the influence of broad-scale impacts such as climate change.
C1 [Olsen, Jeffrey B.; Crane, Penelope A.; Flannery, Blair G.; Wenburg, John K.] US Fish & Wildlife Serv, Conservat Genet Lab, Anchorage, AK 99503 USA.
[Dunmall, Karen] Kawerak Inc, Dept Fisheries, Nome, AK 99762 USA.
[Templin, William D.] Alaska Dept Fish & Game, Div Commercial Fisheries, Gene Conservat Lab, Anchorage, AK 99518 USA.
RP Olsen, JB (reprint author), US Fish & Wildlife Serv, Conservat Genet Lab, 1011 E Tudor Rd, Anchorage, AK 99503 USA.
EM jeffrey_olsen@fws.gov
FU Arctic Yukon Kuskokwim Sustainable Salmon Initiative [45490]; US Fish
and Wildlife Service (US-FWS) Alaska Region Conservation Genetics
Laboratory
FX Funding for this study was provided by the Arctic Yukon Kuskokwim
Sustainable Salmon Initiative through project number 45490, and the US
Fish and Wildlife Service (US-FWS) Alaska Region Conservation Genetics
Laboratory. Tyler Grossheusch developed the ArcGIS version 9.2 data
layers for each species. Doug Molyneaux (Alaska Department of Fish and
Game) organized sample collections from the Kuskokwim River. The data
layers used in this study can be downloaded from a companion web map at
http://alaska.fws.gov/fisheries/genetics/CGL_googlemap.html. The
findings and conclusions in this article are those of the authors and do
not necessarily represent the views of the USFWS.
NR 57
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U1 0
U2 25
PU SPRINGER
PI DORDRECHT
PA VAN GODEWIJCKSTRAAT 30, 3311 GZ DORDRECHT, NETHERLANDS
SN 1566-0621
J9 CONSERV GENET
JI Conserv. Genet.
PD FEB
PY 2011
VL 12
IS 1
BP 223
EP 241
DI 10.1007/s10592-010-0135-3
PG 19
WC Biodiversity Conservation; Genetics & Heredity
SC Biodiversity & Conservation; Genetics & Heredity
GA 703IP
UT WOS:000285971900020
ER
PT J
AU Ransler, FA
Quinn, TW
Oyler-McCance, SJ
AF Ransler, Findley A.
Quinn, Thomas W.
Oyler-McCance, Sara J.
TI Genetic consequences of trumpeter swan (Cygnus buccinator)
reintroductions
SO CONSERVATION GENETICS
LA English
DT Article
DE Translocation; Reintroduction; Trumpeter swan; Microsatellite;
Conservation genetics; Genetic diversity
ID MULTILOCUS GENOTYPE DATA; POPULATION-STRUCTURE; CONSERVATION;
TRANSLOCATION; VARIABILITY; DIVERSITY; MANAGEMENT; INFERENCE; WILDLIFE;
UNITS
AB Relocation programs are often initiated to restore threatened species to previously occupied portions of their range. A primary challenge of restoration efforts is to translocate individuals in a way that prevents loss of genetic diversity and decreases differentiation relative to source populations-a challenge that becomes increasingly difficult when remnant populations of the species are already genetically depauperate. Trumpeter swans were previously extirpated in the entire eastern half of their range. Physical translocations of birds over the last 70 years have restored the species to portions of its historical range. Despite the long history of management, there has been little monitoring of the genetic outcomes of these restoration attempts. We assessed the consequences of this reintroduction program by comparing patterns of genetic variation at 17 microsatellite loci across four restoration flocks (three wild-released, one captive) and their source populations. We found that a wild-released population established from a single source displayed a trend toward reduced genetic diversity relative to and significant genetic differentiation from its source population, though small founder population effects may also explain this pattern. Wild-released flocks restored from multiple populations maintained source levels of genetic variation and lacked significant differentiation from at least one of their sources. Further, the flock originating from a single source revealed significantly lower levels of genetic variation than those established from multiple sources. The distribution of genetic variation in the captive flock was similar to its source. While the case of trumpeter swans provides evidence that restorations from multiple versus single source populations may better preserve natural levels of genetic diversity, more studies are needed to understand the general applicability of this management strategy.
C1 [Ransler, Findley A.; Quinn, Thomas W.; Oyler-McCance, Sara J.] Univ Denver, Dept Biol Sci, Rocky Mt Ctr Conservat Genet & Systemat, Denver, CO 80208 USA.
[Ransler, Findley A.] Cornell Univ, Dept Ecol & Evolutionary Biol, Ithaca, NY 14850 USA.
[Oyler-McCance, Sara J.] US Geol Survey, Ft Collins Sci Ctr, Ft Collins, CO 80526 USA.
RP Ransler, FA (reprint author), Univ Denver, Dept Biol Sci, Rocky Mt Ctr Conservat Genet & Systemat, Denver, CO 80208 USA.
EM far25@cornell.edu
FU U.S. Fish and Wildlife Service; U.S. Geological Survey
FX We would like to thank the volunteers and staff from many state and
federal agencies who helped collect both natural and reintroduced
trumpeter swan samples with special thanks to W. Long, from the Wildlife
Wetlands Society, and the late J. Johnson, from the Kellogg Bird
Sanctuary. We thank J. St. John, J. Cornely, J. Dubovsky, P. Llambias,
G. Ransler, P. Stevens, and the Harrison lab at Cornell for thoughtful
comments on the manuscript. J. St. John also provided invaluable lab
expertise. A. Coulon and R. Vallender gave helpful advice with some of
the analysis programs. Funding for this project was provided by the U.S.
Fish and Wildlife Service Migratory Bird Program and the U.S. Geological
Survey through its Science Support Program. Any use of trade, product,
or firm names is for descriptive purposes only and does not imply
endorsement by the U.S. Government.
NR 49
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U1 3
U2 28
PU SPRINGER
PI DORDRECHT
PA VAN GODEWIJCKSTRAAT 30, 3311 GZ DORDRECHT, NETHERLANDS
SN 1566-0621
J9 CONSERV GENET
JI Conserv. Genet.
PD FEB
PY 2011
VL 12
IS 1
BP 257
EP 268
DI 10.1007/s10592-010-0137-1
PG 12
WC Biodiversity Conservation; Genetics & Heredity
SC Biodiversity & Conservation; Genetics & Heredity
GA 703IP
UT WOS:000285971900022
ER
PT J
AU Lind, AJ
Spinks, PQ
Fellers, GM
Shaffer, HB
AF Lind, Amy J.
Spinks, Phillip Q.
Fellers, Gary M.
Shaffer, H. Bradley
TI Rangewide phylogeography and landscape genetics of the Western U.S.
endemic frog Rana boylii (Ranidae): implications for the conservation of
frogs and rivers
SO CONSERVATION GENETICS
LA English
DT Article
DE Declining amphibian; California; River basins; Foothill yellow-legged
frog; Conservation genetics
ID CALIFORNIA FLORISTIC PROVINCE; SOUTHEASTERN UNITED-STATES; YELLOW-LEGGED
FROG; NORTH-AMERICA; SOUTHERN CALIFORNIA; CRYPTIC VARIATION;
EMYS-MARMORATA; SPOTTED FROGS; POND TURTLE; SALAMANDER
AB Genetic data are increasingly being used in conservation planning for declining species. We sampled both the ecological and distributional limits of the foothill yellow-legged frog, Rana boylii to characterize mitochondrial DNA (mtDNA) variation in this declining, riverine amphibian. We evaluated 1525 base pairs (bp) of cytochrome b and ND2 fragments for 77 individuals from 34 localities using phylogenetic and population genetic analyses. We constructed gene trees using maximum likelihood and Bayesian inference, and quantified genetic variance (using AMOVA and partial Mantel tests) within and among hydrologic regions and river basins. Several moderately supported, geographically-cohesive mtDNA clades were recovered for R. boylii. While genetic variation was low among populations in the largest, most inclusive clade, samples from localities at the edges of the geographic range demonstrated substantial genetic divergence from each other and from more central populations. Hydrologic regions and river basins, which represent likely dispersal corridors for R. boylii, accounted for significant levels of genetic variation. These results suggest that both rivers and larger hydrologic and geographic regions should be used in conservation planning for R. boylii.
C1 [Lind, Amy J.] USDA Forest Serv, Pacific SW Res Stn, Sierra Nevada Res Ctr, Davis, CA 95618 USA.
[Lind, Amy J.; Spinks, Phillip Q.; Shaffer, H. Bradley] Univ Calif Davis, Dept Ecol & Evolut, Davis, CA 95616 USA.
[Fellers, Gary M.] US Geol Survey, Western Ecol Res Ctr, Point Reyes Natl Seashore, Point Reyes Stn, CA 94956 USA.
[Shaffer, H. Bradley] Univ Calif Davis, Ctr Populat Biol, Davis, CA 95616 USA.
RP Lind, AJ (reprint author), USDA Forest Serv, Pacific SW Res Stn, Sierra Nevada Res Ctr, 1735 Res Pk Dr, Davis, CA 95618 USA.
EM alind@fs.fed.us
FU U.C. Davis Graduate Group in Ecology; U.C. Davis Center for
Biosystematics; CALFED Bay-Delta Program; UC Davis Agricultural
Experimental Station; NSF [0817042]
FX We are indebted to M. Fujita, T. Engstrom, T. Near, D. Starkey, and J.
Abramyan for their help with laboratory techniques and analyses, and the
Shaffer Lab (University of California, Davis) for discussion and input
on data analysis. L. Clark, D. Chester, A. Fesnock, K. Freel, P.
Johnson, P. Kleeman, T. Murphey, G. Rotta, T. Sutfin, T. Tharalson, J.
Uyehara, M. van Hattem, and S. Yarnell provided information on sampling
localities and/or accompanied AJL in the field and helped with
collecting. A. Borisenko, C. Rombough, M. Stephens, R. Grasso, K.
Mathews, and L. Vance contributed tissue samples. Funding was provided
by U.C. Davis Graduate Group in Ecology and U.C. Davis Center for
Biosystematics (to AJL) and CALFED Bay-Delta Program, UC Davis
Agricultural Experimental Station, and the NSF (#0817042) (to HBS). T.
Beebee, S. Greco, and P. Moyle provided reviews and guidance on earlier
drafts of this manuscript. Any use of trade, product, or firm names in
this publication is for descriptive purposes only and does not imply
endorsement by the U.S. government.
NR 72
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U2 29
PU SPRINGER
PI DORDRECHT
PA VAN GODEWIJCKSTRAAT 30, 3311 GZ DORDRECHT, NETHERLANDS
SN 1566-0621
EI 1572-9737
J9 CONSERV GENET
JI Conserv. Genet.
PD FEB
PY 2011
VL 12
IS 1
BP 269
EP 284
DI 10.1007/s10592-010-0138-0
PG 16
WC Biodiversity Conservation; Genetics & Heredity
SC Biodiversity & Conservation; Genetics & Heredity
GA 703IP
UT WOS:000285971900023
ER
PT J
AU Cope, WG
Holliman, FM
Kwak, TJ
Oakley, NC
Lazaro, PR
Shea, D
Augspurger, T
Law, JM
Henne, JP
Ware, KM
AF Cope, W. G.
Holliman, F. M.
Kwak, T. J.
Oakley, N. C.
Lazaro, P. R.
Shea, D.
Augspurger, T.
Law, J. M.
Henne, J. P.
Ware, K. M.
TI Assessing water quality suitability for shortnose sturgeon in the
Roanoke River, North Carolina, USA with an in situ bioassay approach
SO JOURNAL OF APPLIED ICHTHYOLOGY
LA English
DT Article
ID TROUT ONCORHYNCHUS-MYKISS; ASSESSING CONTAMINANT SENSITIVITY; SOURCED
ORGANIC-CHEMICALS; SOUTH-CAROLINA; ACIPENSER-TRANSMONTANUS; ACUTE
TOXICITY; HABITAT USE; PAPER-MILL; RETENE; SEDIMENTS
AB P>The aim of this study was to determine the suitability of water quality in the Roanoke River of North Carolina for supporting shortnose sturgeon Acipenser brevirostrum, an endangered species in the United States. Fathead minnows Pimephales promelas were also evaluated alongside the sturgeon as a comparative species to measure potential differences in fish survival, growth, contaminant accumulation, and histopathology in a 28-day in situ toxicity test. Captively propagated juvenile shortnose sturgeon (total length 49 +/- 8 mm, mean +/- SD) and fathead minnows (total length 39 +/- 3 mm, mean +/- SD) were used in the test and their outcomes were compared to simultaneous measurements of water quality (temperature, dissolved oxygen, pH, conductivity, total ammonia nitrogen, hardness, alkalinity, turbidity) and contaminant chemistry (metals, polycyclic aromatic hydrocarbons, organochlorine pesticides, current use pesticides, polychlorinated biphenyls) in river water and sediment. In the in situ test, there were three non-riverine control sites and eight riverine test sites with three replicate cages (25 x 15-cm (OD) clear plexiglass with 200-mu m tear-resistant Nitex (R) screen over each end) of 20 shortnose sturgeon per cage at each site. There was a single cage of fathead minnows also deployed at each site alongside the sturgeon cages. Survival of caged shortnose sturgeon among the riverine sites averaged 9% (range 1.7-25%) on day 22 of the 28-day study, whereas sturgeon survival at the non-riverine control sites averaged 64% (range 33-98%). In contrast to sturgeon, only one riverine deployed fathead minnow died (average 99.4% survival) over the 28-day test period and none of the control fathead minnows died. Although chemical analyses revealed the presence of retene (7-isopropyl-1-methylphenanthrene), a pulp and paper mill derived compound with known dioxin-like toxicity to early life stages of fish, in significant quantities in the water (251-603 ng L-1) and sediment (up to 5000 ng g-1 dry weight) at several river sites, no correlation was detected of adverse water quality conditions or measured contaminant concentrations to the poor survival of sturgeon among riverine test sites. Histopathology analysis determined that the mortality of the river deployed shortnose sturgeon was likely due to liver and kidney lesions from an unknown agent(s). Given the poor survival of shortnose sturgeon (9%) and high survival of fathead minnows (99.4%) at the riverine test sites, our study indicates that conditions in the Roanoke River are incongruous with the needs of juvenile shortnose sturgeon and that fathead minnows, commonly used standard toxicity test organisms, do not adequately predict the sensitivity of shortnose sturgeon. Therefore, additional research is needed to help identify specific limiting factors and management actions for the enhancement and recovery of this imperiled fish species.
C1 [Cope, W. G.; Lazaro, P. R.; Shea, D.] N Carolina State Univ, Dept Environm & Mol Toxicol, Raleigh, NC 27695 USA.
[Holliman, F. M.] Smith Root Inc, Vancouver, WA USA.
[Kwak, T. J.] N Carolina State Univ, US Geol Survey, N Carolina Cooperat Fish & Wildlife Res Unit, Dept Biol, Raleigh, NC 27695 USA.
[Oakley, N. C.] N Carolina Wildlife Resources Commiss, Mebane, NC USA.
[Augspurger, T.] US Fish & Wildlife Serv, Raleigh Field Off, Raleigh, NC USA.
[Law, J. M.] N Carolina State Univ, Coll Vet Med, Raleigh, NC 27695 USA.
[Henne, J. P.; Ware, K. M.] US Fish & Wildlife Serv, Wadmalaw Isl, SC USA.
RP Cope, WG (reprint author), N Carolina State Univ, Dept Environm & Mol Toxicol, Campus Box 7633, Raleigh, NC 27695 USA.
EM greg_cope@ncsu.edu
FU US Fish and Wildlife Service [200040001]
FX Funding for this research was provided by the US Fish and Wildlife
Service, Environmental Contaminants Program (Study ID Number 200040001)
through a grant to WGC and TJK. We thank the many state and federal
agency staff who provided information, guidance, and technical
assistance throughout the duration of this project, especially Glenn
Green and Ronnie Smith of the US Fish and Wildlife Service, Edenton
National Fish Hatchery. Charles Rudder and John Barr provided assistance
in the field and laboratory. Any use of trade, product, or firm names is
for descriptive purposes only and does not imply endorsement by the US
Government.
NR 43
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U1 3
U2 28
PU WILEY-BLACKWELL PUBLISHING, INC
PI MALDEN
PA COMMERCE PLACE, 350 MAIN ST, MALDEN 02148, MA USA
SN 0175-8659
J9 J APPL ICHTHYOL
JI J. Appl. Ichthyol.
PD FEB
PY 2011
VL 27
IS 1
BP 1
EP 12
DI 10.1111/j.1439-0426.2010.01570.x
PG 12
WC Fisheries; Marine & Freshwater Biology
SC Fisheries; Marine & Freshwater Biology
GA 709YV
UT WOS:000286478200001
ER
PT J
AU Hagerty, BE
Nussear, KE
Esque, TC
Tracy, CR
AF Hagerty, Bridgette E.
Nussear, Kenneth E.
Esque, Todd C.
Tracy, C. Richard
TI Making molehills out of mountains: landscape genetics of the Mojave
desert tortoise
SO LANDSCAPE ECOLOGY
LA English
DT Article
DE Landscape genetics; Desert tortoise; Gopherus agassizii; Mojave desert;
Least-cost-path; Isolation-by-resistance; Habitat suitability model
ID PARTIAL MANTEL TESTS; GOPHERUS-AGASSIZII; HABITAT FRAGMENTATION;
FUNCTIONAL CONNECTIVITY; POPULATION-STRUCTURE; MICROSATELLITE LOCI;
SPATIAL PREDICTION; CIRCUIT-THEORY; FLOW; DISTANCE
AB Heterogeneity in habitat often influences how organisms traverse the landscape matrix that connects populations. Understanding landscape connectivity is important to determine the ecological processes that influence those movements, which lead to evolutionary change due to gene flow. Here, we used landscape genetics and statistical models to evaluate hypotheses that could explain isolation among locations of the threatened Mojave desert tortoise (Gopherus agassizii). Within a causal modeling framework, we investigated three factors that can influence landscape connectivity: geographic distance, barriers to dispersal, and landscape friction. A statistical model of habitat suitability for the Mojave desert tortoise, based on topography, vegetation, and climate variables, was used as a proxy for landscape friction and barriers to dispersal. We quantified landscape friction with least-cost distances and with resistance distances among sampling locations. A set of diagnostic partial Mantel tests statistically separated the hypotheses of potential causes of genetic isolation. The best-supported model varied depending upon how landscape friction was quantified. Patterns of genetic structure were related to a combination of geographic distance and barriers as defined by least-cost distances, suggesting that mountain ranges and extremely low-elevation valleys influence connectivity at the regional scale beyond the tortoises' ability to disperse. However, geographic distance was the only influence detected using resistance distances, which we attributed to fundamental differences between the two ways of quantifying friction. Landscape friction, as we measured it, did not influence the observed patterns of genetic distances using either quantification. Barriers and distance may be more valuable predictors of observed population structure for species like the desert tortoise, which has high dispersal capability and a long generation time.
C1 [Hagerty, Bridgette E.; Tracy, C. Richard] Univ Nevada, Dept Biol, Program Ecol Evolut & Conservat Biol, Reno, NV 89557 USA.
[Nussear, Kenneth E.; Esque, Todd C.] US Geol Survey, Western Ecol Res Ctr, Las Vegas Field Stn, Henderson, NV 89074 USA.
RP Hagerty, BE (reprint author), Univ Nevada, Dept Biol, Program Ecol Evolut & Conservat Biol, Reno, NV 89557 USA.
EM bridgetteh@unr.edu
FU Clark County Multi-Species Habitat Conservation Plan; U.S. Fish and
Wildlife Service; NIH [P20 RR016463]
FX The Clark County Multi-Species Habitat Conservation Plan and the U.S.
Fish and Wildlife Service supported this research. Sample collection was
permitted by the USFWS (TE-076710), NDOW (S 24403), CADFG (SC-007374),
UDWR (5BAND6646), and the UNR IACUC (A03/04-12, A05/06-23). We thank F.
Sandmeier and technicians from the University of Nevada, Reno, the
Student Conservation Association, and Kiva Biological for helping with
sample collection. We thank V. Kirchoff and the Nevada Genomics Center
(NIH Grant P20 RR016463) for helping to genotype individuals. BH McRae
provided helpful technical support and advice on the connectivity
modeling. Members of the FWS Desert Tortoise Recovery Office were
helpful sounding boards for ideas, and facilitated research that
provided data for this study. We thank G Hoelzer, MM Peacock, LC
Zimmerman, H Wagner and two anonymous reviewers for helpful comments on
previous drafts of this manuscript. Any use of trade, product, or firm
names in this publication is for descriptive purposes only and does not
imply endorsement by the U.S. government.
NR 82
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U1 5
U2 54
PU SPRINGER
PI DORDRECHT
PA VAN GODEWIJCKSTRAAT 30, 3311 GZ DORDRECHT, NETHERLANDS
SN 0921-2973
J9 LANDSCAPE ECOL
JI Landsc. Ecol.
PD FEB
PY 2011
VL 26
IS 2
BP 267
EP 280
DI 10.1007/s10980-010-9550-6
PG 14
WC Ecology; Geography, Physical; Geosciences, Multidisciplinary
SC Environmental Sciences & Ecology; Physical Geography; Geology
GA 709XO
UT WOS:000286474900009
ER
PT J
AU Olea, RA
Pardo-Iguzquiza, E
AF Olea, Ricardo A.
Pardo-Iguzquiza, Eulogio
TI Generalized Bootstrap Method for Assessment of Uncertainty in
Semivariogram Inference
SO MATHEMATICAL GEOSCIENCES
LA English
DT Article
DE Bootstrap; Geostatistical simulation; Resampling; Semivariogram model;
Percentile confidence interval
ID SPATIAL COVARIANCE PARAMETERS; CONDITIONAL SIMULATIONS; VARIOGRAM
UNCERTAINTY; FORTRAN-77 PROGRAM; MAXIMUM-LIKELIHOOD; COMPUTER-PROGRAM;
LEAST-SQUARES; MATRIX; DECOMPOSITION; MODELS
AB The semivariogram and its related function, the covariance, play a central role in classical geostatistics for modeling the average continuity of spatially correlated attributes. Whereas all methods are formulated in terms of the true semivariogram, in practice what can be used are estimated semivariograms and models based on samples. A generalized form of the bootstrap method to properly model spatially correlated data is used to advance knowledge about the reliability of empirical semivariograms and semivariogram models based on a single sample. Among several methods available to generate spatially correlated resamples, we selected a method based on the LU decomposition and used several examples to illustrate the approach. The first one is a synthetic, isotropic, exhaustive sample following a normal distribution, the second example is also a synthetic but following a non-Gaussian random field, and a third empirical sample consists of actual raingauge measurements. Results show wider confidence intervals than those found previously by others with inadequate application of the bootstrap. Also, even for the Gaussian example, distributions for estimated semivariogram values and model parameters are positively skewed. In this sense, bootstrap percentile confidence intervals, which are not centered around the empirical semivariogram and do not require distributional assumptions for its construction, provide an achieved coverage similar to the nominal coverage. The latter cannot be achieved by symmetrical confidence intervals based on the standard error, regardless if the standard error is estimated from a parametric equation or from bootstrap.
C1 [Olea, Ricardo A.] US Geol Survey, Reston, VA 20192 USA.
[Pardo-Iguzquiza, Eulogio] IGME, Madrid 28003, Spain.
RP Olea, RA (reprint author), US Geol Survey, 12201 Sunrise Valley Dr,MS 956, Reston, VA 20192 USA.
EM rolea@usgs.gov
RI Pardo-Iguzquiza, Eulogio/A-6324-2013
OI Pardo-Iguzquiza, Eulogio/0000-0002-3865-8639
NR 27
TC 7
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U1 0
U2 6
PU SPRINGER HEIDELBERG
PI HEIDELBERG
PA TIERGARTENSTRASSE 17, D-69121 HEIDELBERG, GERMANY
SN 1874-8961
EI 1874-8953
J9 MATH GEOSCI
JI Math Geosci.
PD FEB
PY 2011
VL 43
IS 2
BP 203
EP 228
DI 10.1007/s11004-010-9269-6
PG 26
WC Geosciences, Multidisciplinary; Mathematics, Interdisciplinary
Applications
SC Geology; Mathematics
GA 709UY
UT WOS:000286468100004
ER
PT J
AU Sanford, WE
Aeschbach-Hertig, W
Herczeg, AL
AF Sanford, Ward E.
Aeschbach-Hertig, Werner
Herczeg, Andrew L.
TI Preface: Insights from environmental tracers in groundwater systems
SO HYDROGEOLOGY JOURNAL
LA English
DT Editorial Material
C1 [Sanford, Ward E.] US Geol Survey, Reston, VA 20192 USA.
[Aeschbach-Hertig, Werner] Univ Heidelberg, Inst Environm Phys, D-69120 Heidelberg, Germany.
[Herczeg, Andrew L.] CSIRO, Glen Osmond, SA 5064, Australia.
RP Sanford, WE (reprint author), US Geol Survey, MS 431,12201 Sunrise Valley Dr, Reston, VA 20192 USA.
EM wsanford@usgs.gov
RI Herczeg, Andrew/B-8323-2011;
OI Herczeg, Andrew/0000-0002-3788-2743; Aeschbach,
Werner/0000-0003-0917-1239
NR 19
TC 10
Z9 11
U1 0
U2 10
PU SPRINGER
PI NEW YORK
PA 233 SPRING ST, NEW YORK, NY 10013 USA
SN 1431-2174
J9 HYDROGEOL J
JI Hydrogeol. J.
PD FEB
PY 2011
VL 19
IS 1
BP 1
EP 3
DI 10.1007/s10040-010-0687-9
PG 3
WC Geosciences, Multidisciplinary; Water Resources
SC Geology; Water Resources
GA 706HT
UT WOS:000286209700001
ER
PT J
AU Shapiro, AM
AF Shapiro, Allen M.
TI The challenge of interpreting environmental tracer concentrations in
fractured rock and carbonate aquifers
SO HYDROGEOLOGY JOURNAL
LA English
DT Article
DE Fractured rocks; Carbonate rocks; Groundwater flow; Chemical transport;
Environmental tracer
ID GROUNDWATER-FLOW; MATRIX DIFFUSION; SOLUTE TRANSPORT; AGE; SIMULATION;
MEDIA; MODEL
C1 US Geol Survey, Reston, VA 20192 USA.
RP Shapiro, AM (reprint author), US Geol Survey, 12201 Sunrise Valley Dr,Mail Stop 431, Reston, VA 20192 USA.
EM ashapiro@usgs.gov
NR 16
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U1 1
U2 5
PU SPRINGER
PI NEW YORK
PA 233 SPRING ST, NEW YORK, NY 10013 USA
SN 1431-2174
J9 HYDROGEOL J
JI Hydrogeol. J.
PD FEB
PY 2011
VL 19
IS 1
BP 9
EP 12
DI 10.1007/s10040-010-0678-x
PG 4
WC Geosciences, Multidisciplinary; Water Resources
SC Geology; Water Resources
GA 706HT
UT WOS:000286209700003
ER
PT J
AU Sanford, W
AF Sanford, Ward
TI Calibration of models using groundwater age
SO HYDROGEOLOGY JOURNAL
LA English
DT Article
DE Groundwater age; Inverse modeling
ID TRANSIT-TIME DISTRIBUTIONS; DIRECT SIMULATION; RESERVOIR THEORY;
DISPERSION; DIFFUSION; WATER; USA
C1 USGS, Reston, VA 20192 USA.
RP Sanford, W (reprint author), USGS, MS 431, Reston, VA 20192 USA.
EM wsanford@usgs.gov
NR 24
TC 38
Z9 38
U1 0
U2 18
PU SPRINGER
PI NEW YORK
PA 233 SPRING ST, NEW YORK, NY 10013 USA
SN 1431-2174
J9 HYDROGEOL J
JI Hydrogeol. J.
PD FEB
PY 2011
VL 19
IS 1
BP 13
EP 16
DI 10.1007/s10040-010-0637-6
PG 4
WC Geosciences, Multidisciplinary; Water Resources
SC Geology; Water Resources
GA 706HT
UT WOS:000286209700004
ER
PT J
AU Park, JW
Moon, CH
Harmache, A
Wargo, AR
Purcell, MK
Bremont, M
Kurath, G
AF Park, J. W.
Moon, C. H.
Harmache, A.
Wargo, A. R.
Purcell, M. K.
Bremont, M.
Kurath, G.
TI Restricted growth of U-type infectious haematopoietic necrosis virus
(IHNV) in rainbow trout cells may be linked to casein kinase II activity
SO JOURNAL OF FISH DISEASES
LA English
DT Article
DE casein kinase II; IHNV; RTG-2 cells; U-type growth
ID VESICULAR STOMATITIS-VIRUS; HEMORRHAGIC SEPTICEMIA VIRUS; DEPENDENT
PROTEIN-KINASE; ONCORHYNCHUS-MYKISS; VIRULENCE MECHANISMS;
PHOSPHOPROTEIN-P; SOCKEYE-SALMON; RNA-POLYMERASE; RABIES VIRUS;
MAP-KINASE
AB Previously, we demonstrated that a representative M genogroup type strain of infectious haematopoietic necrosis virus (IHNV) from rainbow trout grows well in rainbow trout-derived RTG-2 cells, but a U genogroup type strain from sockeye salmon has restricted growth, associated with reduced genome replication and mRNA transcription. Here, we analysed further the mechanisms for this growth restriction of U-type IHNV in RTG-2 cells, using strategies that assessed differences in viral genes, host immune regulation and phosphorylation. To determine whether the viral glycoprotein (G) or non-virion (NV) protein was responsible for the growth restriction, four recombinant IHNV viruses were generated in which the G gene of an infectious IHNV clone was replaced by the G gene of U- or M-type IHNV and the NV gene was replaced by NV of U- or M-type IHNV. There was no significant difference in the growth of these recombinants in RTG-2 cells, indicating that G and NV proteins are not major factors responsible for the differential growth of the U- and M-type strains. Poly I:C pretreatment of RTG-2 cells suppressed the growth of both U- and M-type IHNV, although the M virus continued to replicate at a reduced level. Both viruses induced type 1 interferon (IFN1) and the IFN1 stimulated gene Mx1, but the expression levels in M-infected cells were significantly higher than in U-infected cells and an inhibitor of the IFN1-inducible protein kinase PKR, 2-aminopurine (2-AP), did not affect the growth of U- or M-type IHNV in RTG-2 cells. These data did not indicate a role for the IFN1 system in the restricted growth of U-type IHNV in RTG-2 cells. Prediction of kinase-specific phosphorylation sites in the viral phosphoprotein (P) using the NetPhosK program revealed differences between U- and M-type P genes at five phosphorylation sites. Pretreatment of RTG-2 cells with a PKC inhibitor or a p38MAPK inhibitor did not affect the growth of the U- and M-type viruses. However, 100 mu m of the casein kinase II (CKII) inhibitor, 5,6-dichloro-1-beta-d-ribofuranosylbenzimidazole (DRB), reduced the titre of the U type 8.3-fold at 24 h post-infection. In contrast, 100 mu m of the CKII inhibitor reduced the titre of the M type only 1.3-fold at 48 h post-infection. Our data suggest that the different growth of U- and M-type IHNV in RTG-2 cells may be linked to a differential requirement for cellular protein kinases such as CKII for their growth.
C1 [Park, J. W.; Moon, C. H.; Wargo, A. R.; Purcell, M. K.; Kurath, G.] US Geol Survey, Western Fisheries Res Ctr, Seattle, WA USA.
[Park, J. W.] Univ Ulsan, Dept Biol Sci, Ulsan, South Korea.
[Harmache, A.; Bremont, M.] INRA CRJ, Unite Virol & Immunol Mol, Jouy En Josas, France.
RP Kurath, G (reprint author), US Geol Survey, Western Fisheries Res Ctr, Seattle, WA USA.
EM gkurath@usgs.gov
RI HARMACHE, ABDALLAH/E-7274-2011; Perez , Claudio Alejandro/F-8310-2010;
OI Perez , Claudio Alejandro/0000-0001-9688-184X; harmache,
abdallah/0000-0002-7377-7641; Purcell, Maureen/0000-0003-0154-8433
FU U. S. Geological Survey; National Research Initiative of the USDA
Cooperative State Research, Education and Extension Service
[2006-35204-17393]; Korean government (MEST) [2009-0060042]; Korean
Government (MOEHRD) [KRF-2007-357-F00030]; University of Ulsan
[2008-0063]
FX The authors thank Bill Batts for providing nucleotide sequences of the P
genes of U-type and M-type IHNV. This project was supported by: the U.
S. Geological Survey; National Research Initiative of the USDA
Cooperative State Research, Education and Extension Service, grant
number 2006-35204-17393; Korea Science and Engineering Foundation
(KOSEF) grant funded by the Korean government (MEST) (grant code:
2009-0060042); Korea Research Foundation Grant funded by the Korean
Government (MOEHRD, Basic Research Promotion Fund)
(KRF-2007-357-F00030); and the Research Fund of the University of Ulsan
(2008-0063). The use of trade, firm or corporation names in this
publication is for the information and convenience of the reader. Such
use does not constitute an official endorsement or approval by the U. S.
Department of Interior or the U. S. Geological Survey of any product or
service to the exclusion of others that may be suitable.
NR 53
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U1 0
U2 5
PU WILEY-BLACKWELL PUBLISHING, INC
PI MALDEN
PA COMMERCE PLACE, 350 MAIN ST, MALDEN 02148, MA USA
SN 0140-7775
J9 J FISH DIS
JI J. Fish Dis.
PD FEB
PY 2011
VL 34
IS 2
BP 115
EP 129
DI 10.1111/j.1365-2761.2010.01225.x
PG 15
WC Fisheries; Marine & Freshwater Biology; Veterinary Sciences
SC Fisheries; Marine & Freshwater Biology; Veterinary Sciences
GA 706NW
UT WOS:000286226100003
PM 21241319
ER
PT J
AU Simoes, FJM
AF Simoes, Francisco J. M.
TI Finite Volume Model for Two-Dimensional Shallow Environmental Flow
SO JOURNAL OF HYDRAULIC ENGINEERING
LA English
DT Article
DE Shallow water equations; Godunov methods; Unstructured grids; Flooding;
Wetting and drying; Upwind finite volume
ID HYPERBOLIC CONSERVATION-LAWS; WATER FLOW; EULER EQUATIONS; SIMULATION;
TOPOGRAPHY; STABILITY; SCHEMES; RUNUP
AB This paper presents the development of a two-dimensional, depth integrated, unsteady, free-surface model based on the shallow water equations. The development was motivated by the desire of balancing computational efficiency and accuracy by selective and conjunctive use of different numerical techniques. The base framework of the discrete model uses Godunov methods on unstructured triangular grids, but the solution technique emphasizes the use of a high-resolution Riemann solver where needed, switching to a simpler and computationally more efficient upwind finite volume technique in the smooth regions of the flow. Explicit time marching is accomplished with strong stability preserving Runge-Kutta methods, with additional acceleration techniques for steady-state computations. A simplified mass-preserving algorithm is used to deal with wet/dry fronts. Application of the model is made to several benchmark cases that show the interplay of the diverse solution techniques.
C1 USGS, Geomorphol & Sediment Transport Lab, Golden, CO 80403 USA.
RP Simoes, FJM (reprint author), USGS, Geomorphol & Sediment Transport Lab, 4620 Technol Dr, Golden, CO 80403 USA.
EM frsimoes@usgs.gov
NR 30
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U1 0
U2 5
PU ASCE-AMER SOC CIVIL ENGINEERS
PI RESTON
PA 1801 ALEXANDER BELL DR, RESTON, VA 20191-4400 USA
SN 0733-9429
EI 1943-7900
J9 J HYDRAUL ENG
JI J. Hydraul. Eng.-ASCE
PD FEB
PY 2011
VL 137
IS 2
BP 173
EP 182
DI 10.1061/(ASCE)HY.1943-7900.0000292
PG 10
WC Engineering, Civil; Engineering, Mechanical; Water Resources
SC Engineering; Water Resources
GA 706LB
UT WOS:000286218800004
ER
PT J
AU Senay, GB
Budde, ME
Verdin, JP
AF Senay, G. B.
Budde, M. E.
Verdin, J. P.
TI Enhancing the Simplified Surface Energy Balance (SSEB) approach for
estimating landscape ET: Validation with the METRIC model
SO AGRICULTURAL WATER MANAGEMENT
LA English
DT Article
DE Evapotranspiration; Energy balance; Surface temperature; NDVI; METRIC
ID SATELLITE DATA; MAPPING EVAPOTRANSPIRATION; TEMPERATURE; EVAPORATION;
TOPOGRAPHY; MANAGEMENT; MOISTURE; CLIMATE; CONTEXT; IMAGERY
AB Evapotranspiration (ET) can be derived from satellite data using surface energy balance principles. METRIC (Mapping EvapoTranspiration at high Resolution with Internalized Calibration) is one of the most widely used models available in the literature to estimate ET from satellite imagery. The Simplified Surface Energy Balance (SSEB) model is much easier and less expensive to implement. The main purpose of this research was to present an enhanced version of the Simplified Surface Energy Balance (SSEB) model and to evaluate its performance using the established METRIC model. In this study, SSEB and METRIC Er fractions were compared using 7 Landsat images acquired for south central Idaho during the 2003 growing season. The enhanced SSEB model compared well with the METRIC model output exhibiting an r(2) improvement from 0.83 to 0.90 in less complex topography (elevation less than 2000 m) and with an improvement of r(2) from 0.27 to 0.38 in more complex (mountain) areas with elevation greater than 2000 m. Independent evaluation showed that both models exhibited higher variation in complex topographic regions, although more with SSEB than with METRIC. The higher Er fraction variation in the complex mountainous regions highlighted the difficulty of capturing the radiation and heat transfer physics on steep slopes having variable aspect with the simple index model, and the need to conduct more research. However, the temporal consistency of the results suggests that the SSEB model can be used on a wide range of elevation (more successfully up 2000 m) to detect anomalies in space and time for water resources management and monitoring such as for drought early warning systems in data scarce regions. SSEB has a potential for operational agro-hydrologic applications to estimate ET with inputs of surface temperature, NDVI, DEM and reference ET. Published by Elsevier B.V.
C1 [Senay, G. B.; Budde, M. E.; Verdin, J. P.] US Geol Survey, Earth Resources Observat & Sci EROS Ctr, Sioux Falls, SD 57198 USA.
RP Senay, GB (reprint author), US Geol Survey, Earth Resources Observat & Sci EROS Ctr, 47914 252nd St, Sioux Falls, SD 57198 USA.
EM senay@usgs.gov; mbudde@usgs.gov; verdin@usgs.gov
FU USGS/EROS
FX Funding was provided through the USGS/EROS support for the Geographic
Science Center of Excellence (GIScCE), South Dakota State University. We
acknowledge the use of METRIC-based data sets made available by Dr.
Richard Allen and his research team at the University of Idaho. We also
thank Dr. Allen for a variety of suggestions made during comparisons
between SSEB and METRIC and during preparation of this manuscript. We
are also grateful to Dr. Susan Moran for her important comments and
suggestions. We thank our colleagues at EROS, Lei Ji, Guleid Artan and
Mike Crane for their valuable technical comments and edits.
NR 43
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U1 4
U2 19
PU ELSEVIER SCIENCE BV
PI AMSTERDAM
PA PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS
SN 0378-3774
EI 1873-2283
J9 AGR WATER MANAGE
JI Agric. Water Manage.
PD FEB
PY 2011
VL 98
IS 4
BP 606
EP 618
DI 10.1016/j.agwat.2010.10.014
PG 13
WC Agronomy; Water Resources
SC Agriculture; Water Resources
GA 722LE
UT WOS:000287432900014
ER
PT J
AU Donovan, JJ
Lowers, HA
Rusk, BG
AF Donovan, John J.
Lowers, Heather A.
Rusk, Brian G.
TI Improved electron probe microanalysis of trace elements in quartz
SO AMERICAN MINERALOGIST
LA English
DT Article
DE Electron microprobe; trace elements; quartz; detection limit; accuracy;
background artifacts; blank correction; aggregate intensities
ID PORPHYRY COPPER-DEPOSIT; HYDROTHERMAL QUARTZ; VEIN QUARTZ;
CATHODOLUMINESCENCE; TEXTURES; MONTANA; COMPLEX; SYSTEM; BUTTE
AB Quartz occurs in a wide range of geologic environments throughout the Earth's crust. The concentration and distribution of trace elements in quartz provide information such as temperature and other physical conditions of formation. Trace element analyses with modern electron-probe microanalysis (EPMA) instruments can achieve 99% confidence detection of similar to 100 ppm with fairly minimal effort for many elements in samples of low to moderate average atomic number such as many common oxides and silicates. However, trace element measurements below 100 ppm in many materials are limited, not only by the precision of the background measurement, but also by the accuracy with which background levels are determined. A new "blank" correction algorithm has been developed and tested on both Cameca and JEOL instruments, which applies a quantitative correction to the emitted X-ray intensities during the iteration of the sample matrix correction based on a zero level (or known trace) abundance calibration standard. This iterated blank correction, when combined with improved background fit models, and an "aggregate" intensity calculation utilizing multiple spectrometer intensities in software for greater geometric efficiency, yields a detection limit of 2 to 3 ppm for Ti and 6 to 7 ppm for Al in quartz at 99% t-test confidence with similar levels for absolute accuracy.
C1 [Donovan, John J.] Univ Oregon, CAMCOR, Eugene, OR 97403 USA.
[Lowers, Heather A.] US Geol Survey, Denver, CO 80225 USA.
[Rusk, Brian G.] James Cook Univ, Sch Earth & Environm Sci, Townsville, Qld 4811, Australia.
RP Donovan, JJ (reprint author), Univ Oregon, CAMCOR, Eugene, OR 97403 USA.
EM donovan@uoregon.edu
FU USGS
FX The authors acknowledge Paul Carpenter, John Fournelle, and Dale Newbury
for their excellent comments on this manuscript, and thanks to Celeste
Mercer for work on Figure 2. Alan Koenig, Paul Lamothe, Ruth Wolf, and
Monique Adams of the U.S. Geological Survey for their ICP-MS data on the
quartz standard. Brian Rusk acknowledges the USGS Mendenhall Fellowship.
NR 26
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U2 39
PU MINERALOGICAL SOC AMER
PI CHANTILLY
PA 3635 CONCORDE PKWY STE 500, CHANTILLY, VA 20151-1125 USA
SN 0003-004X
J9 AM MINERAL
JI Am. Miner.
PD FEB-MAR
PY 2011
VL 96
IS 2-3
BP 274
EP 282
DI 10.2138/am.2011.3631
PG 9
WC Geochemistry & Geophysics; Mineralogy
SC Geochemistry & Geophysics; Mineralogy
GA 721EK
UT WOS:000287336200006
ER
PT J
AU Mazzola, MB
Chambers, JC
Blank, RR
Pyke, DA
Schupp, EW
Allcock, KG
Doescher, PS
Nowak, RS
AF Mazzola, Monica B.
Chambers, Jeanne C.
Blank, Robert R.
Pyke, David A.
Schupp, Eugene W.
Allcock, Kimberly G.
Doescher, Paul S.
Nowak, Robert S.
TI Effects of resource availability and propagule supply on native species
recruitment in sagebrush ecosystems invaded by Bromus tectorum
SO BIOLOGICAL INVASIONS
LA English
DT Article
DE Bromus tectorum (cheatgrass); Invasion; Sagebrush-steppe; Resource
availability; Propagule supply; Seedling establishment; Sucrose addition
ID GREAT-BASIN; COMMUNITY INVASIBILITY; NITROGEN AVAILABILITY; ECOLOGICAL
RESISTANCE; SECONDARY SUCCESSION; PERENNIAL GRASS; EXOTIC ANNUALS;
SOIL-NITROGEN; PLANT; INVASION
AB Resource availability and propagule supply are major factors influencing establishment and persistence of both native and invasive species. Increased soil nitrogen (N) availability and high propagule inputs contribute to the ability of annual invasive grasses to dominate disturbed ecosystems. Nitrogen reduction through carbon (C) additions can potentially immobilize soil N and reduce the competitiveness of annual invasive grasses. Native perennial species are more tolerant of resource limiting conditions and may benefit if N reduction decreases the competitive advantage of annual invaders and if sufficient propagules are available for their establishment. Bromus tectorum, an exotic annual grass in the sagebrush steppe of western North America, is rapidly displacing native plant species and causing widespread changes in ecosystem processes. We tested whether nitrogen reduction would negatively affect B. tectorum while creating an opportunity for establishment of native perennial species. A C source, sucrose, was added to the soil, and then plots were seeded with different densities of both B. tectorum (0, 150, 300, 600, and 1,200 viable seeds m(-2)) and native species (0, 150, 300, and 600 viable seeds m(-2)). Adding sucrose had short-term (1 year) negative effects on available nitrogen and B. tectorum density, biomass and seed numbers, but did not increase establishment of native species. Increasing propagule availability increased both B. tectorum and native species establishment. Effects of B. tectorum on native species were density dependent and native establishment increased as B. tectorum propagule availability decreased. Survival of native seedlings was low indicating that recruitment is governed by the seedling stage.
C1 [Chambers, Jeanne C.] US Forest Serv, USDA, Rocky Mt Res Stn, Reno, NV 89512 USA.
[Mazzola, Monica B.] Univ Nevada Reno, Dept Nat Resources & Environm Sci, Reno, NV 89557 USA.
[Mazzola, Monica B.] Univ Nacl La Pampa, Fac Ciencias Exactas & Nat, RA-6300 Santa Rosa, La Pampa, Argentina.
[Blank, Robert R.] ARS, USDA, Exot & Invas Weeds Unit, Reno, NV 89512 USA.
[Pyke, David A.] US Geol Survey, Forest & Rangeland Ecosyst Sci Ctr, Corvallis, OR 97331 USA.
[Schupp, Eugene W.] Utah State Univ, Dept Wildland Resources, Logan, UT 84322 USA.
[Allcock, Kimberly G.; Nowak, Robert S.] Univ Nevada Reno, Dept Nat Resources & Environm Sci, Reno, NV 89557 USA.
[Doescher, Paul S.] Oregon State Univ, Dept Forest Resources, Corvallis, OR 97331 USA.
RP Chambers, JC (reprint author), US Forest Serv, USDA, Rocky Mt Res Stn, Reno, NV 89512 USA.
EM jchambers@fs.fed.us
RI Schupp, Eugene/F-1834-2010
FU USDA Initiative for Future Agricultural and Food Systems
[2001-52103-11322]; USDA Forest Service; Rocky Mountain Research
Station; Nevada Agricultural Experiment Station; USDI Bureau of Land
Management
FX We thank Carlos Wilson, Jacob Landmesser, Kendra Moseley, Lisa Ellsworth
and Tye Morgan for technical assistance. George Fernandez, Dave Turner
and Dave Board provided statistical advice, and Thomas A. Jones, Thomas
Monaco, Dan Ogle and Loren St. Jones helped with study implementation.
Comments from Carla D'Antonio, Dale Johnson, Tara Forbis and anonymous
reviewers improved the manuscript. Research was funded by the USDA
Initiative for Future Agricultural and Food Systems (CREES Agreement
2001-52103-11322) with additional support from the USDA Forest Service,
Rocky Mountain Research Station, the Nevada Agricultural Experiment
Station, and the USDI Bureau of Land Management. Any use of trade names
is for descriptive purposes only and does not imply endorsement by U.S.
government.
NR 62
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U1 3
U2 34
PU SPRINGER
PI DORDRECHT
PA VAN GODEWIJCKSTRAAT 30, 3311 GZ DORDRECHT, NETHERLANDS
SN 1387-3547
J9 BIOL INVASIONS
JI Biol. Invasions
PD FEB
PY 2011
VL 13
IS 2
BP 513
EP 526
DI 10.1007/s10530-010-9846-0
PG 14
WC Biodiversity Conservation; Ecology
SC Biodiversity & Conservation; Environmental Sciences & Ecology
GA 703RJ
UT WOS:000285998700024
ER
PT J
AU Hurteau, MD
Brooks, ML
AF Hurteau, Matthew D.
Brooks, Matthew L.
TI Short- and Long-term Effects of Fire on Carbon in US Dry Temperate
Forest Systems
SO BIOSCIENCE
LA English
DT Article
DE carbon stability; climate change; fire severity; forest management;
fuels management
ID PONDEROSA PINE FORESTS; MIXED-CONIFER FOREST; WESTERN UNITED-STATES;
CLIMATE-CHANGE; PRESCRIBED FIRE; TREE MORTALITY; SIERRA-NEVADA;
WILDFIRE; CALIFORNIA; SEVERITY
AB Forests sequester carbon from the atmosphere, and in so doing can mitigate the effects of climate change. Fire is a natural disturbance process in many forest systems that releases carbon back to the atmosphere. In dry temperate forests, fires historically burned with greater frequency and lower severity than they do today Frequent fires consumed fuels on the forest floor and maintained open stand structures. Fire suppression has resulted in increased understory fluel loads and tree density; a change in structure that has caused a shift from low- to high-severity fires. More severe fires, resulting in greater tree mortality have caused a decrease in forest carbon stability. Fire management actions can mitigate the risk of high-severity fires, but these actions often require a trade-off between maximizing carbon stocks and carbon stability. We discuss the effects of fire on forest carbon stocks and recommend that managing forests on the basis of their specific ecologies should be the foremost goal, with carbon sequestration being an ancillary benefit.
C1 [Hurteau, Matthew D.] No Arizona Univ, Flagstaff, AZ 86011 USA.
[Brooks, Matthew L.] US Geol Survey, Western Ecol Res Ctr, Yosemite Field Stn, Reston, VA USA.
RP Hurteau, MD (reprint author), No Arizona Univ, Flagstaff, AZ 86011 USA.
EM matthew.hurteau@nau.edu
RI Hurteau, Matthew/D-2301-2009
OI Hurteau, Matthew/0000-0001-8457-8974
FU US Department of Agriculture Forest Service Pacific Southwest Research
Station [08-CA-11272170-102]; Bureau of Land Management; US Geological
Survey Terrestrial, Freshwater; Marine Ecosystems Program; National Park
Service Fire and Aviation Management Program [F8803090011]; Climate
Change Response Program [F8803100033]
FX The authors thank Karen Phillips, Nathan Stephenson, Leland Tarnay, and
four anonymous reviewers for helpful comments on previous versions of
this manuscript. MDH acknowledges support from Cooperative Agreement
08-CA-11272170-102 with the US Department of Agriculture Forest Service
Pacific Southwest Research Station, using funds provided by the Bureau
of Land Management through the sale of public lands as authorized by the
Southern Nevada Public Land Management Act. MLB acknowledges support
from the US Geological Survey Terrestrial, Freshwater, and Marine
Ecosystems Program, and the National Park Service Fire and Aviation
Management Program (Interagency Agreement F8803090011) and Climate
Change Response Program (Interagency Agreement F8803100033).
NR 59
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U1 7
U2 55
PU AMER INST BIOLOGICAL SCI
PI WASHINGTON
PA 1444 EYE ST, NW, STE 200, WASHINGTON, DC 20005 USA
SN 0006-3568
J9 BIOSCIENCE
JI Bioscience
PD FEB
PY 2011
VL 61
IS 2
BP 139
EP 146
DI 10.1525/bio.2011.61.2.9
PG 8
WC Biology
SC Life Sciences & Biomedicine - Other Topics
GA 720FY
UT WOS:000287267200013
ER
PT J
AU Burns, SP
Sun, J
Lenschow, DH
Oncley, SP
Stephens, BB
Yi, CX
Anderson, DE
Hu, J
Monson, RK
AF Burns, Sean P.
Sun, Jielun
Lenschow, Donald H.
Oncley, Steven P.
Stephens, Britton B.
Yi, Chuixiang
Anderson, Dean E.
Hu, Jia
Monson, Russell K.
TI Atmospheric Stability Effects on Wind Fields and Scalar Mixing Within
and Just Above a Subalpine Forest in Sloping Terrain
SO BOUNDARY-LAYER METEOROLOGY
LA English
DT Article
DE Canopy-layer turbulence; Carbon in the Mountains Experiment (CME04);
Complex terrain; Richardson number; Scalar mixing; Wind fields
ID TURBULENT FLUX MEASUREMENTS; NOCTURNAL BOUNDARY-LAYER; HIGH-ELEVATION;
COMPLEX TERRAIN; PART I; ROUGHNESS SUBLAYER; MOMENTUM-TRANSFER; SOIL
RESPIRATION; HILLY TERRAIN; VEGETATION CANOPIES
AB Air temperature T (a) , specific humidity q, CO2 mole fraction chi (c) , and three-dimensional winds were measured in mountainous terrain from five tall towers within a 1 km region encompassing a wide range of canopy densities. The measurements were sorted by a bulk Richardson number Ri (b) . For stable conditions, we found vertical scalar differences developed over a "transition" region between 0.05 < Ri (b) < 0.5. For strongly stable conditions (Ri (b) > 1), the vertical scalar differences reached a maximum and remained fairly constant with increasing stability. The relationships q and chi (c) have with Ri (b) are explained by considering their sources and sinks. For winds, the strong momentum absorption in the upper canopy allows the canopy sublayer to be influenced by pressure gradient forces and terrain effects that lead to complex subcanopy flow patterns. At the dense-canopy sites, soil respiration coupled with wind-sheltering resulted in CO2 near the ground being 5-7 mu mol mol(-1) larger than aloft, even with strong above-canopy winds (near-neutral conditions). We found Ri (b) -binning to be a useful tool for evaluating vertical scalar mixing; however, additional information (e.g., pressure gradients, detailed vegetation/topography, etc.) is needed to fully explain the subcanopy wind patterns. Implications of our results for CO2 advection over heterogenous, complex terrain are discussed.
C1 [Burns, Sean P.; Sun, Jielun; Lenschow, Donald H.; Oncley, Steven P.; Stephens, Britton B.] Natl Ctr Atmospher Res, Boulder, CO 80307 USA.
[Yi, Chuixiang] Queens Coll, Sch Earth & Environm Sci, Flushing, NY USA.
[Anderson, Dean E.] US Geol Survey, Denver, CO 80225 USA.
[Burns, Sean P.; Hu, Jia; Monson, Russell K.] Univ Colorado, Dept Ecol & Evolutionary Biol, Boulder, CO 80309 USA.
RP Burns, SP (reprint author), Natl Ctr Atmospher Res, POB 3000, Boulder, CO 80307 USA.
EM sean@ucar.edu
RI Burns, Sean/A-9352-2008; Yi, Chuixiang/A-1388-2013; Stephens,
Britton/B-7962-2008; Sun, Jielun/H-6576-2015;
OI Burns, Sean/0000-0002-6258-1838; Stephens, Britton/0000-0002-1966-6182;
Sun, Jielun/0000-0003-3271-7914; LENSCHOW, DONALD/0000-0003-4353-0098
FU South Central Section of the National Institute for Global Environmental
Change (NIGEC) through the US Department of Energy [DE-FC03-90ER61010];
NCAR; National Science Foundation [EAR-0321918]
FX Tony Delany created TGaMS and oversaw its operation during CME04. Andy
Watt helped construct, deploy and maintain the AIRCOA systems. Steve
Semmer, Gordon Maclean, Kurt Knudsen, Chris Golubieski, and many others
at NCAR/ISFF deployed, instrumented, and dismantled the EOL Towers. We
thank Dave Bowling for constructive comments on an early version of the
manuscript. We also thank two anonymous reviewers for their insightful
comments. The NWT tower is supported by a grant from the South Central
Section of the National Institute for Global Environmental Change
(NIGEC) through the US Department of Energy (BER Program, Cooperative
Agreement No. DE-FC03-90ER61010). CME04 was supported by the NCAR
Director Opportunity Fund and NSF grant EAR-0321918. The National Center
for Atmospheric Research (NCAR) is sponsored by the National Science
Foundation.
NR 89
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U1 0
U2 16
PU SPRINGER
PI DORDRECHT
PA VAN GODEWIJCKSTRAAT 30, 3311 GZ DORDRECHT, NETHERLANDS
SN 0006-8314
EI 1573-1472
J9 BOUND-LAY METEOROL
JI Bound.-Layer Meteor.
PD FEB
PY 2011
VL 138
IS 2
BP 231
EP 262
DI 10.1007/s10546-010-9560-6
PG 32
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA 705AT
UT WOS:000286100800004
ER
PT J
AU Trumbull, RB
Slack, JF
Krienitz, MS
Belkin, HE
Wiedenbeck, M
AF Trumbull, Robert B.
Slack, John F.
Krienitz, Marc-Sebastian
Belkin, Harvey E.
Wiedenbeck, Michael
TI FLUID SOURCES AND METALLOGENESIS IN THE BLACKBIRD Co-Cu-Au-Bi-Y-REE
DISTRICT, IDAHO, USA: INSIGHTS FROM MAJOR-ELEMENT AND BORON ISOTOPIC
COMPOSITIONS OF TOURMALINE
SO CANADIAN MINERALOGIST
LA English
DT Article
DE Blackbird; Idaho; cobalt-enriched belt; stratabound sulfides;
tourmaline; chemical composition; boron isotopes; SIMS; fluid sources;
metallogeny
ID MASSIVE SULFIDE DEPOSITS; COBALT BELT; HYDROTHERMAL TOURMALINES;
CONTINENTAL-CRUST; ION MICROPROBE; GOLD DEPOSITS; RICH ROCKS; EVOLUTION;
ZONE; MINERALIZATION
AB Tourmaline is a widespread mineral in the Mesoproterozoic Blackbird Co-Cu-Au-Bi-Y-REE district, Idaho, where it occurs in both mineralized zones and wallrocks. We report here major-element and B-isotope compositions of tourmaline from stratabound sulfide deposits and their metasedimentary wallrocks, from mineralized and barren pipes of tourmaline breccia, from late barren quartz veins, and from Mesoproterozoic granite. The tourmalines are aluminous, intermediate in the schorl-dravite series, with Fe/(Fe + Mg) values of 0.30 to 0.85, and 10 to 50% X-site vacancies. Compositional zoning is prominent only in tourmaline from breccias and quartz veins; crystal rims are enriched in Mg, Ca and Ti, and depleted in Fe and Al relative to cores. The chemical composition of tourmaline does not correlate with the presence or absence of mineralization. The delta(11)B values fall into two groups. Isotopically light tourmaline (-21.7 to -7.6%) occurs in unmineralized samples from wallrocks, late quartz veins and Mesoproterozoic granite, whereas heavy tourmaline (-6.9 to +3.2%) is spatially associated with mineralization (stratabound and breccia-hosted), and is also found in barren breccia. At an inferred temperature of 300 degrees C, boron in the hydrothermal fluid associated with mineralization had delta(11)B values of -3 to + 7%. The high end of this range indicates a marine source of the boron. A likely scenario involves leaching of boron principally from marine carbonate beds or B-bearing evaporites in Mesoproterozoic strata of the region. The delta(11)B values of the isotopically light tourmaline in the sulfide deposits are attributed to recrystallization during Cretaceous metamorphism, superimposed on a light boron component derived from footwall siliciclastic sediments (e.g., marine clays) during Mesoproterozoic mineralization, and possibly a minor component of light boron from a magmatic-hydrothermal fluid. The metal association of Bi-Be-Y-REE in the Blackbird ores suggests some magmatic input, but involvement of granite-derived fluids cannot be conclusively established from the present database.
C1 [Trumbull, Robert B.; Krienitz, Marc-Sebastian; Wiedenbeck, Michael] GFZ German Res Ctr Geosci, D-14473 Potsdam, Germany.
[Slack, John F.; Belkin, Harvey E.] US Geol Survey, Natl Ctr, Reston, VA 20192 USA.
RP Trumbull, RB (reprint author), GFZ German Res Ctr Geosci, D-14473 Potsdam, Germany.
EM robert.trumbull@gfz-potsdam.de
OI Belkin, Harvey/0000-0001-7879-6529
NR 69
TC 18
Z9 19
U1 1
U2 9
PU MINERALOGICAL ASSOC CANADA
PI OTTAWA
PA PO BOX 78087, MERILINE POSTAL OUTLET, 1460 MERIVALE RD, OTTAWA, ONTARIO
K2E 1B1, CANADA
SN 0008-4476
J9 CAN MINERAL
JI Can. Mineral.
PD FEB
PY 2011
VL 49
IS 1
BP 225
EP 244
DI 10.3749/canmin.49.1.225
PG 20
WC Mineralogy
SC Mineralogy
GA 733DF
UT WOS:000288240400016
ER
PT J
AU Archinal, BA
A'Hearn, MF
Bowell, E
Conrad, A
Consolmagno, GJ
Courtin, R
Fukushima, T
Hestroffer, D
Hilton, JL
Krasinsky, GA
Neumann, G
Oberst, J
Seidelmann, PK
Stooke, P
Tholen, DJ
Thomas, PC
Williams, IP
AF Archinal, B. A.
A'Hearn, M. F.
Bowell, E.
Conrad, A.
Consolmagno, G. J.
Courtin, R.
Fukushima, T.
Hestroffer, D.
Hilton, J. L.
Krasinsky, G. A.
Neumann, G.
Oberst, J.
Seidelmann, P. K.
Stooke, P.
Tholen, D. J.
Thomas, P. C.
Williams, I. P.
TI Report of the IAU Working Group on Cartographic Coordinates and
Rotational Elements: 2009
SO CELESTIAL MECHANICS & DYNAMICAL ASTRONOMY
LA English
DT Article
DE Cartographic coordinates; Longitude; Latitude; Rotation axes; Rotation
periods; Sizes; Shapes; Planets; Satellites; Dwarf planets; Minor
planets; Comets
ID CASSINI-ISS IMAGES; INTERIOR STRUCTURE; GLOBAL SHAPE; SATELLITES;
PLANETS; GRAVITY; TOPOGRAPHY; PERIOD; CERES; STATE
AB Every three years the IAU Working Group on Cartographic Coordinates and Rotational Elements revises tables giving the directions of the poles of rotation and the prime meridians of the planets, satellites, minor planets, and comets. This report takes into account the IAU Working Group for Planetary System Nomenclature (WGPSN) and the IAU Committee on Small Body Nomenclature (CSBN) definition of dwarf planets, introduces improved values for the pole and rotation rate of Mercury, returns the rotation rate of Jupiter to a previous value, introduces improved values for the rotation of five satellites of Saturn, and adds the equatorial radius of the Sun for comparison. It also adds or updates size and shape information for the Earth, Mars' satellites Deimos and Phobos, the four Galilean satellites of Jupiter, and 22 satellites of Saturn. Pole, rotation, and size information has been added for the asteroids (21) Lutetia, (511) Davida, and (2867) teins. Pole and rotation information has been added for (2) Pallas and (21) Lutetia. Pole and rotation and mean radius information has been added for (1) Ceres. Pole information has been updated for (4) Vesta. The high precision realization for the pole and rotation rate of the Moon is updated. Alternative orientation models for Mars, Jupiter, and Saturn are noted. The Working Group also reaffirms that once an observable feature at a defined longitude is chosen, a longitude definition origin should not change except under unusual circumstances. It is also noted that alternative coordinate systems may exist for various (e.g. dynamical) purposes, but specific cartographic coordinate system information continues to be recommended for each body. The Working Group elaborates on its purpose, and also announces its plans to occasionally provide limited updates to its recommendations via its website, in order to address community needs for some updates more often than every 3 years. Brief recommendations are also made to the general planetary community regarding the need for controlled products, and improved or consensus rotation models for Mars, Jupiter, and Saturn.
C1 [Archinal, B. A.] US Geol Survey, Flagstaff, AZ 86001 USA.
[A'Hearn, M. F.] Univ Maryland, College Pk, MD 20742 USA.
[Bowell, E.] Lowell Observ, Flagstaff, AZ 86001 USA.
[Conrad, A.] WM Keck Observ, Kamuela, HI USA.
[Consolmagno, G. J.] Vatican Observ, Vatican City, Vatican.
[Courtin, R.] Observ Paris, CNRS, LESIA, F-75014 Paris, France.
[Fukushima, T.] Natl Astron Observ Japan, Tokyo, Japan.
[Hestroffer, D.] Observ Paris, CNRS, IMCCE, F-75014 Paris, France.
[Hilton, J. L.] US Naval Observ, Washington, DC USA.
[Krasinsky, G. A.] Inst Appl Astron, St Petersburg, Russia.
[Neumann, G.] NASA, Goddard Space Flight Ctr, Greenbelt, MD 20771 USA.
[Oberst, J.] DLR Berlin Adlershof, Berlin, Germany.
[Seidelmann, P. K.] Univ Virginia, Charlottesville, VA USA.
[Stooke, P.] Univ Western Ontario, London, ON, Canada.
[Tholen, D. J.] Univ Hawaii, Honolulu, HI 96822 USA.
[Thomas, P. C.] Cornell Univ, Ithaca, NY USA.
[Williams, I. P.] Queen Mary Univ London, London, England.
RP Archinal, BA (reprint author), US Geol Survey, Flagstaff, AZ 86001 USA.
EM barchinal@usgs.gov
RI Neumann, Gregory/I-5591-2013;
OI Neumann, Gregory/0000-0003-0644-9944; Williams, Iwan
Prys/0000-0002-8069-1344
NR 74
TC 106
Z9 116
U1 0
U2 12
PU SPRINGER
PI DORDRECHT
PA VAN GODEWIJCKSTRAAT 30, 3311 GZ DORDRECHT, NETHERLANDS
SN 0923-2958
J9 CELEST MECH DYN ASTR
JI Celest. Mech. Dyn. Astron.
PD FEB
PY 2011
VL 109
IS 2
BP 101
EP 135
DI 10.1007/s10569-010-9320-4
PG 35
WC Astronomy & Astrophysics; Mathematics, Interdisciplinary Applications
SC Astronomy & Astrophysics; Mathematics
GA 712JH
UT WOS:000286662300001
ER
PT J
AU Jaisi, DP
Eberl, DD
Dong, HL
Kim, J
AF Jaisi, Deb P.
Eberl, Dennis D.
Dong, Hailiang
Kim, Jinwook
TI THE FORMATION OF ILLITE FROM NONTRONITE BY MESOPHILIC AND THERMOPHILIC
BACTERIAL REACTION
SO CLAYS AND CLAY MINERALS
LA English
DT Article
DE Illite-smectite Reaction; Microbial Fe(III) Reduction; NAu-2; Shewanella
putrefaciens CN32; Thermos scotoductus SA-01
ID TRANSMISSION ELECTRON-MICROSCOPY; GULF-OF-MEXICO; MICROBIAL REDUCTION;
SMECTITE DIAGENESIS; CLAY-MINERALS; HYDROCARBON ACCUMULATION;
DISSIMILATORY REDUCTION; THERMUS-SCOTODUCTUS; STRUCTURAL FE(III); BURIAL
DIAGENESIS
AB The formation of illite through the smectite-to-illite (S-I) reaction is considered to be one of the most important mineral reactions occurring during diagenesis. In biologically catalyzed systems, however, this transformation has been suggested to be rapid and to bypass the high temperature and long time requirements. To understand the factors that promote the S-I reaction, the present study focused on the effects of pH, temperature, solution chemistry, and aging on the S-I reaction in microbially mediated systems. Fe(III)-reduction experiments were performed in both growth and non-growth media with two types of bacteria: mesophilic (Shewanella putrefaciens CN32) and thermophilic (Thermos scotoductus SA-01). Reductive dissolution of NAu-2 was observed and the formation of illite in treatment with thermophilic SA-01 was indicated by X-ray diffraction (XRD) and high-resolution transmission electron microscopy (HRTEM). A basic pH (8.4) and high temperature (65 degrees C) were the most favorable conditions for the formation of illite. A long incubation time was also found to enhance the formation of illite. K-nontronite (non-permanent fixation of K) was also detected and differentiated from the discrete illite in the XRD profiles. These results collectively suggested that the formation of illite associated with the biologically catalyzed smectite-to-illite reaction pathway may bypass the prolonged time and high temperature required for the S-I reaction in the absence of microbial activity.
C1 [Kim, Jinwook] Yonsei Univ, Dept Earth Syst Sci, Seoul 120749, South Korea.
[Jaisi, Deb P.; Dong, Hailiang] Miami Univ, Dept Geol, Oxford, OH 45056 USA.
[Jaisi, Deb P.] Univ Delaware, Dept Plant & Soil Sci, Newark, DE 19716 USA.
[Eberl, Dennis D.] US Geol Survey, Boulder, CO 80303 USA.
RP Kim, J (reprint author), Yonsei Univ, Dept Earth Syst Sci, Seoul 120749, South Korea.
EM Jinwook@yonsei.ac.kr
FU Ministry of Education, Science and Technology [20090085989]; National
Science Foundation [EAR-0345307]; The Clay Minerals Society; AAPG
FX The present research was supported by the Basic Science Research Program
through the National Research Foundation of Korea (NRF) funded by the
Ministry of Education, Science and Technology (20090085989) to JWK, a
grant from the National Science Foundation (EAR-0345307) to HD, and by
student grants from The Clay Minerals Society (2004, 2006) and the AAPG
(John Teagle Memorial Grant, 2004) to DPJ. The authors are grateful to
three anonymous reviewers and the Associate Editor whose comments
greatly improved the quality of the manuscript.
NR 79
TC 21
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U1 1
U2 21
PU CLAY MINERALS SOC
PI CHANTILLY
PA 3635 CONCORDE PKWY, STE 500, CHANTILLY, VA 20151-1125 USA
SN 0009-8604
EI 1552-8367
J9 CLAY CLAY MINER
JI Clay Clay Min.
PD FEB
PY 2011
VL 59
IS 1
BP 21
EP 33
DI 10.1346/CCMN.2011.0590105
PG 13
WC Chemistry, Physical; Geosciences, Multidisciplinary; Mineralogy; Soil
Science
SC Chemistry; Geology; Mineralogy; Agriculture
GA 754TV
UT WOS:000289881200005
ER
PT J
AU Kotzerka, J
Hatch, SA
Garthe, S
AF Kotzerka, Jana
Hatch, Scott A.
Garthe, Stefan
TI EVIDENCE FOR FORAGING-SITE FIDELITY AND INDIVIDUAL FORAGING BEHAVIOR OF
PELAGIC CORMORANTS REARING CHICKS IN THE GULF OF ALASKA
SO CONDOR
LA English
DT Article
DE Alaska; diving activity; foraging behavior; GPS dataloggers; Pelagic
Cormorant; Phalacrocorax pelagicus; site fidelity
ID SHAGS PHALACROCORAX-ARISTOTELIS; INTRA-SPECIFIC COMPETITION; FEEDING
LOCATIONS; DIVING BEHAVIOR; MARINE PREDATOR; AREA FIDELITY; SEABIRDS;
PERFORMANCE; PREY; VARIABILITY
AB The Pelagic Cormorant (Phalacrocorax pelagicus) is the most widespread cormorant in the North Pacific, but little is known about its foraging and diving behavior. However, knowledge of seabirds' foraging behavior is important to understanding their function in the marine environment. In 2006, using GPS dataloggers, we studied the foraging behavior of 14 male Pelagic Cormorants rearing chicks on Middleton Island, Alaska. For foraging, the birds had high fidelity to a small area 8 km north of the colony. Within that area, the cormorants' diving activity was of two distinct kinds-near-surface dives (1-6 m) and benthic dives (28-33 m). Individuals were consistent in the depths of their dives, either mostly shallow or mostly deep. Few showed no depth preference. Dive duration, time at maximum depth, and pauses at the water surface between consecutive dives were shorter for shallow dives than for deep dives. The cormorants made dives of both types throughout the day, but the frequency of deep dives increased toward evening. Maximum foraging range was 9 km; maximum total distance traveled per trip was 43.4 km. Trip durations ranged from 0.3 to 7.7 hr. Maximum depth of a dive was 42.2 m, and duration of dives ranged from 4 to 120 sec. We found that Pelagic Cormorants at Middleton Island were faithful to one particular foraging area and individuals dived in distinct patterns. Distinct, specialized foraging behavior may be advantageous in reducing intra- and interspecific competition but may also render the species vulnerable to changing environmental conditions.
C1 [Kotzerka, Jana; Garthe, Stefan] Univ Kiel, Res & Technol Ctr Westcoast Buesum, D-25761 Buesum, Germany.
[Hatch, Scott A.] US Geol Survey, Alaska Sci Ctr, Anchorage, AK 99508 USA.
RP Kotzerka, J (reprint author), Univ Kiel, Res & Technol Ctr Westcoast Buesum, Hafentoern 1, D-25761 Buesum, Germany.
EM kotzerka@ftz-west.uni-kiel.de
FU German Science Foundation (DFG) [GA 617/5-1]
FX This project was funded by the German Science Foundation (DFG GA
617/5-1). We thank all those who helped with the field work on Middleton
Island. Special thanks to Thomas Mattern, who provided a Matlab script
for analysis of dive data. Henriette Dries, Joel White, and two
anonymous reviewers made useful comments on an earlier draft of the
manuscript. The study was approved and carried out under permits issued
by the state of Alaska and U.S. Fish and Wildlife Service. Mention of
trade names is for descriptive purposes only and does not imply
endorsement by the U.S. government.
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PU COOPER ORNITHOLOGICAL SOC
PI LAWRENCE
PA ORNITHOLOGICAL SOC NORTH AMER PO BOX 1897, LAWRENCE, KS 66044-8897 USA
SN 0010-5422
J9 CONDOR
JI Condor
PD FEB
PY 2011
VL 113
IS 1
BP 80
EP 88
DI 10.1525/cond.2011.090158
PG 9
WC Ornithology
SC Zoology
GA 739RT
UT WOS:000288736400009
ER
PT J
AU Lindstrom, A
Gill, RE
Jamieson, SE
McCaffery, B
Wennerberg, L
Wikelski, M
Klaassen, M
AF Lindstrom, Ake
Gill, Robert E., Jr.
Jamieson, Sarah E.
McCaffery, Brian
Wennerberg, Liv
Wikelski, Martin
Klaassen, Marcel
TI A PUZZLING MIGRATORY DETOUR: ARE FUELING CONDITIONS IN ALASKA DRIVING
THE MOVEMENT OF JUVENILE SHARP-TAILED SANDPIPERS?
SO CONDOR
LA English
DT Article
DE Calidris acuminata; migration; waders; body mass; fat stores; predation;
age-segregated migration; Alaska
ID DUNLINS CALIDRIS-ALPINA; WESTERN SANDPIPERS; AUTUMN MIGRATION; STOPOVER
SITE; BIRDS; PREDATION; MASS; FAT; ECOLOGY; FLIGHTS
AB Making a detour can be advantageous to a migrating bird if fuel-deposition rates at stopover sites along the detour are considerably higher than at stopover sites along a more direct route. One example of an extensive migratory detour is that of the Sharp-tailed Sandpiper (Calidris acuminata), of which large numbers of juveniles are found during fall migration in western Alaska. These birds take a detour of 1500-3400 km from the most direct route between their natal range in northeastern Siberia and nonbreeding areas in Australia. We studied the autumnal fueling rates and fuel loads of 357 Sharp-tailed Sandpipers captured in western Alaska. In early September the birds increased in mass at a rate of only 0.5% of lean body mass day(-1). Later in September, the rate of mass increase was about 6% of lean body mass day(-1), among the highest values found among similar-sized shorebirds around the world. Some individuals more than doubled their body mass because of fuel deposition, allowing non-stop flight of between 7100 and 9800 km, presumably including a trans-oceanic flight to the southern hemisphere. Our observations indicated that predator attacks were rare in our study area, adding another potential benefit of the detour. We conclude that the most likely reason for the Alaskan detour is that it allows juvenile Sharp-tailed Sand-pipers to put on large fuel stores at exceptionally high rates.
C1 [Lindstrom, Ake] Lund Univ, Dept Biol, S-22362 Lund, Sweden.
[Gill, Robert E., Jr.] US Geol Survey, Alaska Sci Ctr, Anchorage, AK 99508 USA.
[Jamieson, Sarah E.] Simon Fraser Univ, Ctr Wildlife Ecol, Burnaby, BC V5A 1S6, Canada.
[McCaffery, Brian] US Fish & Wildlife Serv, Bethel, AK 99559 USA.
[Wennerberg, Liv] Univ Oslo, Nat Hist Museum, NO-0318 Oslo, Norway.
[Wikelski, Martin] Max Planck Inst Ornithol, Dept Migrat & Immunoecol, D-78315 Radolfzell am Bodensee, Germany.
[Klaassen, Marcel] NIOO KNAW, Netherlands Inst Ecol, NL-3631 AC Nieuwersluis, Netherlands.
[Klaassen, Marcel] Deakin Univ, Ctr Integrat Ecol, Geelong, Vic 3217, Australia.
RP Lindstrom, A (reprint author), Lund Univ, Dept Biol, Ecol Bldg, S-22362 Lund, Sweden.
EM marcel.klaassen@deakin.edu.au
RI Klaassen, Marcel/B-4325-2008
OI Klaassen, Marcel/0000-0003-3907-9599
FU U.S. Geological Survey; Alaska Science Center, Anchorage; Dutch Science
Foundation (NWO-NAP); Royal Physiographic Society in Lund; Environment
Canada
FX This project was part of the "Beringia 2005" expedition organized by the
Swedish Polar Research Secretariat, to which we are most grateful. We
thank Mike Rearden of the U.S. Fish and Wildlife Service in Bethel and
his personnel for their superb logistic and moral support. Additional
logistic and financial support was kindly provided by the U.S.
Geological Survey, Alaska Science Center, Anchorage, the Dutch Science
Foundation (NWO-NAP), the Royal Physiographic Society in Lund, and
Environment Canada. Several people helped substantially in the field,
including Martin Green, Phil Battley, Nils Warnock, Jesse Conklin,
Patrick Lemons, David Melville, James Luown, Ty Donnelly, and Anders
Wirdheim. George Walters, Robert Sundown, Mike Rearden, Fred Broerman,
and Isaac Bedingfield assisted in aerial radio telemetry, John Terenzi
helped with wing-area estimates, and Raymond Klaassen assisted with
flight-distance calculations. We thank Staffan Bensch, Martin Green, and
two anonymous reviewers for comments on earlier versions of the
manuscript. Any use of trade, product, or firm names in this publication
is for descriptive purposes only and does not imply endorsement by any
author's affiliation. This is publication 4926 of the Netherlands
Institute of Ecology.
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PU COOPER ORNITHOLOGICAL SOC
PI LAWRENCE
PA ORNITHOLOGICAL SOC NORTH AMER PO BOX 1897, LAWRENCE, KS 66044-8897 USA
SN 0010-5422
J9 CONDOR
JI Condor
PD FEB
PY 2011
VL 113
IS 1
BP 129
EP 139
DI 10.1525/cond.2011.090171
PG 11
WC Ornithology
SC Zoology
GA 739RT
UT WOS:000288736400013
ER
PT J
AU Lautze, NC
Sisson, TW
Mangan, MT
Grove, TL
AF Lautze, Nicole C.
Sisson, Thomas W.
Mangan, Margaret T.
Grove, Timothy L.
TI Segregating gas from melt: an experimental study of the Ostwald ripening
of vapor bubbles in magmas
SO CONTRIBUTIONS TO MINERALOGY AND PETROLOGY
LA English
DT Article
DE Ostwald; Ripening; Coarsening; Bubble; Magma; Transient
ID SIZE DISTRIBUTIONS; EMPIRICAL-MODEL; H2O; SOLUBILITY; DIFFUSION; GROWTH;
CONSTRAINTS; DYNAMICS; RHYOLITE
AB Diffusive coarsening (Ostwald ripening) of H2O and H2O-CO2 bubbles in rhyolite and basaltic andesite melts was studied with elevated temperature-pressure experiments to investigate the rates and time spans over which vapor bubbles may enlarge and attain sufficient buoyancy to segregate in magmatic systems. Bubble growth and segregation are also considered in terms of classical steady-state and transient (non-steady-state) ripening theory. Experimental results are consistent with diffusive coarsening as the dominant mechanism of bubble growth. Ripening is faster in experiments saturated with pure H2O than in those with a CO2-rich mixed vapor probably due to faster diffusion of H2O than CO2 through the melt. None of the experimental series followed the time(1/3) increase in mean bubble radius and time(-1) decrease in bubble number density predicted by classical steady-state ripening theory. Instead, products are interpreted as resulting from transient regime ripening. Application of transient regime theory suggests that bubbly magmas may require from days to 100 years to reach steady-state ripening conditions. Experimental results, as well as theory for steady-state ripening of bubbles that are immobile or undergoing buoyant ascent, indicate that diffusive coarsening efficiently eliminates micron-sized bubbles and would produce mm-sized bubbles in 10(2)-10(4) years in crustal magma bodies. Once bubbles attain mm-sizes, their calculated ascent rates are sufficient that they could transit multiple kilometers over hundreds to thousands of years through mafic and silicic melt, respectively. These results show that diffusive coarsening can facilitate transfer of volatiles through, and from, magmatic systems by creating bubbles sufficiently large for rapid ascent.
C1 [Lautze, Nicole C.] Ist Nazl Geofis & Volcanol Roma, Rome, Italy.
[Lautze, Nicole C.; Sisson, Thomas W.; Mangan, Margaret T.] US Geol Survey, Volcano Hazards Team, Menlo Pk, CA 94025 USA.
[Grove, Timothy L.] MIT, Cambridge, MA 02139 USA.
RP Lautze, NC (reprint author), Ist Nazl Geofis & Volcanol Roma, Rome, Italy.
EM nicole.lautze@ingv.it
RI Grove, Timothy/M-9638-2013
OI Grove, Timothy/0000-0003-0628-1969
FU NSF; INGV-Roma
FX The authors are highly grateful to Ben Hankins for his skillful guidance
in the USGS Magma Dynamics Laboratory, and to Shaul Hurwitz, Larry
Mastin, and two anonymous reviewers for constructive suggestions. Lautze
acknowledges the USGS Mendenhall Postdoctoral Program and Volcano
Hazards Team for the generous support that enabled this study, and
support from the NSF International Research Fellowship Program and
INGV-Roma during the review process.
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PU SPRINGER
PI NEW YORK
PA 233 SPRING ST, NEW YORK, NY 10013 USA
SN 0010-7999
J9 CONTRIB MINERAL PETR
JI Contrib. Mineral. Petrol.
PD FEB
PY 2011
VL 161
IS 2
BP 331
EP 347
DI 10.1007/s00410-010-0535-x
PG 17
WC Geochemistry & Geophysics; Mineralogy
SC Geochemistry & Geophysics; Mineralogy
GA 705GQ
UT WOS:000286117300011
ER
PT J
AU Chelgren, ND
Adams, MJ
Bailey, LL
Bury, RB
AF Chelgren, Nathan D.
Adams, Michael J.
Bailey, Larissa L.
Bury, R. Bruce
TI Using multilevel spatial models to understand salamander site occupancy
patterns after wildfire
SO ECOLOGY
LA English
DT Article
DE Bayesian; capture probability; detection probability; generalized linear
mixed models; independence; late seral stage; mixed models; N-mixture
model; Plethodontidae; presence-absence; spatial autocorrelation;
wildland fire
ID RED-BACKED SALAMANDER; LINEAR MIXED MODELS; SPECIES DISTRIBUTIONS;
PLETHODONTID SALAMANDERS; DETECTION PROBABILITY; HIERARCHICAL-MODELS;
TERRESTRIAL SALAMANDERS; VARIANCE PARAMETERS; MAXIMUM-LIKELIHOOD;
HARDWOOD FORESTS
AB Studies of the distribution of elusive forest wildlife have suffered from the confounding of true presence with the uncertainty of detection. Occupancy modeling, which incorporates probabilities of species detection conditional on presence, is an emerging approach for reducing observation bias. However, the current likelihood modeling framework is restrictive for handling unexplained sources of variation in the response that may occur when there are dependence structures such as smaller sampling units that are nested within larger sampling units. We used multilevel Bayesian occupancy modeling to handle dependence structures and to partition sources of variation in occupancy of sites by terrestrial salamanders (family Plethodontidae) within and surrounding an earlier wildfire in western Oregon, USA. Comparison of model fit favored a spatial N-mixture model that accounted for variation in salamander abundance over models that were based on binary detection/non-detection data. Though catch per unit effort was higher in burned areas than unburned, there was strong support that this pattern was due to a higher probability of capture for individuals in burned plots. Within the burn, the odds of capturing an individual given it was present were 2.06 times the odds outside the burn, reflecting reduced complexity of ground cover in the burn. There was weak support that true occupancy was lower within the burned area. While the odds of occupancy in the burn were 0.49 times the odds outside the burn among the five species, the magnitude of variation attributed to the burn was small in comparison to variation attributed to other landscape variables and to unexplained, spatially autocorrelated random variation. While ordinary occupancy models may separate the biological pattern of interest from variation in detection probability when all sources of variation are known, the addition of random effects structures for unexplained sources of variation in occupancy and detection probability may often more appropriately represent levels of uncertainty.
C1 [Chelgren, Nathan D.; Adams, Michael J.; Bury, R. Bruce] US Geol Survey, Forest & Rangeland Ecosyst Sci Ctr, Corvallis, OR 97331 USA.
[Bailey, Larissa L.] US Geol Survey, Patuxent Wildlife Res Ctr, Laurel, MD 20708 USA.
RP Chelgren, ND (reprint author), US Geol Survey, Forest & Rangeland Ecosyst Sci Ctr, Corvallis, OR 97331 USA.
EM nathan_chelgren@usgs.gov
RI Bailey, Larissa/A-2565-2009
FU U.S. Geological Survey's Amphibian Research and Monitoring Initiative
FX This research was funded by the U.S. Geological Survey's Amphibian
Research and Monitoring Initiative. We are grateful to S. Anderson, L.
Frady, B. McCreary, E. Meyer, and T. Smith for field assistance, and to
the U. S. Forest Service, Willamette National Forest for providing
logistical support. D. DeGross and E. Hyde contributed helpful
discussion regarding study design. J. A. Royle, J. Nichols, R. Steidl,
and two anonymous reviewers provided helpful comments on an earlier
draft of the manuscript.
NR 83
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PU ECOLOGICAL SOC AMER
PI WASHINGTON
PA 1990 M STREET NW, STE 700, WASHINGTON, DC 20036 USA
SN 0012-9658
J9 ECOLOGY
JI Ecology
PD FEB
PY 2011
VL 92
IS 2
BP 408
EP 421
PG 14
WC Ecology
SC Environmental Sciences & Ecology
GA 750NC
UT WOS:000289553600016
PM 21618920
ER
PT J
AU Marques, TA
Thomas, L
Royle, JA
AF Marques, Tiago A.
Thomas, Len
Royle, J. Andrew
TI A hierarchical model for spatial capture-recapture data: comment
SO ECOLOGY
LA English
DT Editorial Material
C1 [Marques, Tiago A.; Thomas, Len] Univ St Andrews, Ctr Res Ecol & Environm Modelling, St Andrews KY16 9LZ, Fife, Scotland.
[Marques, Tiago A.; Thomas, Len] Univ St Andrews, Res Unit Wildlife Populat Assessment, St Andrews KY16 9LZ, Fife, Scotland.
[Marques, Tiago A.] Univ Lisbon, Ctr Estat & Aplicacoes, P-1749016 Lisbon, Portugal.
[Royle, J. Andrew] US Geol Survey, Patuxent Wildlife Res Ctr, Laurel, MD 20708 USA.
RP Marques, TA (reprint author), Univ St Andrews, Ctr Res Ecol & Environm Modelling, St Andrews KY16 9LZ, Fife, Scotland.
EM tiago@mcs.st-and.ac.uk
RI Marques, Tiago/A-5530-2010;
OI Marques, Tiago/0000-0002-2581-1972; Royle, Jeffrey/0000-0003-3135-2167
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PU ECOLOGICAL SOC AMER
PI WASHINGTON
PA 1990 M STREET NW, STE 700, WASHINGTON, DC 20036 USA
SN 0012-9658
J9 ECOLOGY
JI Ecology
PD FEB
PY 2011
VL 92
IS 2
BP 526
EP 528
DI 10.1890/10-1440.1
PG 3
WC Ecology
SC Environmental Sciences & Ecology
GA 750NC
UT WOS:000289553600027
PM 21618931
ER
PT J
AU Pereira, P
Ubeda, X
Martin, D
Mataix-Solera, J
Guerrero, C
AF Pereira, Paulo
Ubeda, Xavier
Martin, Deborah
Mataix-Solera, Jorge
Guerrero, Cesar
TI Effects of a low severity prescribed fire on water-soluble elements in
ash from a cork oak (Quercus suber) forest located in the northeast of
the Iberian Peninsula
SO ENVIRONMENTAL RESEARCH
LA English
DT Article; Proceedings Paper
CT International Meeting on Fire Effects on Soil Properties
CY FEB 11-15, 2009
CL Marmaris, TURKEY
SP Hacettepe Univ, Dept Biol, Ankara Univ, Dept Soil Sci
DE Prescribed fire; Ash; Quercus suber; Iberian Peninsula; Quercus robur
ID SOIL-SOLUTION CHEMISTRY; ACID-MINE DRAINAGE; WOOD-ASH; ORGANIC-MATTER;
HEAVY-METALS; PINE FOREST; CHEMICAL-PROPERTIES; PLANT ASH; NITROGEN
TRANSFORMATIONS; SEQUENTIAL EXTRACTION
AB Wildfire is the major disturbance in Mediterranean forests. Prescribed fire can be an alternative to reduce the amount of fuel and hence decrease the wildfire risk. However the effects of prescribed fire must be studied, especially on ash properties, because ash is an important nutrient source for ecosystem recovery. The aim of this study is to determine the effects of a low severity prescribed fire on water-soluble elements in ash including pH, electrical conductivity (EC), calcium (Ca), magnesium (Mg), sodium (Na), potassium (K), aluminum (Al), manganese (Mn), iron (Fe), zinc (Zn), silica (SiO2) and total sulphur (TS). A prescribed fire was conducted in a cork oak (Quercus suber) (Q.S) forest located in the northeast part of the Iberian Peninsula. Samples were collected from a flat plot of 40 x 70 m mainly composed of Q.S and Quercus robur (Q.R) trees. In order to understand the effects of the prescribed fire on the soluble elements in ash, we conducted our data analysis on three data groups: all samples, only Q.S samples and only Q.R samples. All three sample groups exhibited a significant increase in pH, EC (p < 0.001), water-soluble Ca, Mg, Na, SiO2 and IS and a decrease in water-soluble Mn, Fe and Zn. Differences were identified between oak species for water-soluble K, Al and Fe. In Q.S samples we registered a significant increase in the first two elements p < 0.001 and p < 0.01, respectively, and a non-significant impact in the third, at p < 0.05. In Q.R data we identified a non-significant impact on water-soluble K and Al and a significant decrease in water-soluble Fe (p < 0.05). These differences are probably due to vegetation characteristics and burn severity. The fire induced a higher variability in the ash soluble elements, especially in Q.S samples, that at some points burned with higher severity. The increase of pH, EC, Ca, Mg, Na and K will improve soil fertility, mainly in the study area where soils are acidic. The application of this low severity prescribed fire will improve soil nutrient status without causing soil degradation and thus is considered to be a good management strategy. (C) 2010 Elsevier Inc. All rights reserved.
C1 [Pereira, Paulo; Ubeda, Xavier] Univ Barcelona, Dept Phys Geog & Reg Geog Anal, GRAM Mediterranean Environm Res Grp, Catalunya 0800, Spain.
[Pereira, Paulo] Mykolas Romeris Univ, Dept Environm Policy & Management, LT-08303 Vilnius, Lithuania.
[Pereira, Paulo] Vilnius Gedminas Tech Univ, Environm Protect Dept, LT-01108 Vilnius, Lithuania.
[Martin, Deborah] US Geol Survey, Boulder, CO 80303 USA.
[Mataix-Solera, Jorge; Guerrero, Cesar] Univ Miguel Hernandez, Dept Agrochem & Environm, Environm Soil Sci Grp, Alicante 03202, Spain.
RP Pereira, P (reprint author), Univ Barcelona, Dept Phys Geog & Reg Geog Anal, GRAM Mediterranean Environm Res Grp, C Montalegre 6, Catalunya 0800, Spain.
EM pereiraub@gmail.com; xubeda@gmail.com; damartin@usgs.gov;
jorge.mataix@umh.es; cesar.guerrero@umh.es
RI Guerrero, Cesar/A-3550-2008; Mataix-Solera, Jorge/A-3520-2008; Pereira,
Paulo/O-1845-2016
OI Guerrero, Cesar/0000-0002-3960-9724; Mataix-Solera,
Jorge/0000-0003-2789-9936; Pereira, Paulo/0000-0003-0227-2010
NR 139
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U2 33
PU ACADEMIC PRESS INC ELSEVIER SCIENCE
PI SAN DIEGO
PA 525 B ST, STE 1900, SAN DIEGO, CA 92101-4495 USA
SN 0013-9351
J9 ENVIRON RES
JI Environ. Res.
PD FEB
PY 2011
VL 111
IS 2
BP 237
EP 247
DI 10.1016/j.envres.2010.09.002
PG 11
WC Environmental Sciences; Public, Environmental & Occupational Health
SC Environmental Sciences & Ecology; Public, Environmental & Occupational
Health
GA 719DF
UT WOS:000287179200007
PM 20869047
ER
PT J
AU Puckett, LJ
Tesoriero, AJ
Dubrovsky, NM
AF Puckett, Larry J.
Tesoriero, Anthony J.
Dubrovsky, Neil M.
TI Nitrogen Contamination of Surficial Aquifers-A Growing Legacy
SO ENVIRONMENTAL SCIENCE & TECHNOLOGY
LA English
DT Article
ID UNITED-STATES; NITRATE POLLUTION; GROUND WATER; DENITRIFICATION;
AGROECOSYSTEMS
C1 [Tesoriero, Anthony J.] US Geol Survey, NAWQA Program, Portland, OR USA.
[Puckett, Larry J.] US Geol Survey, NAWQA Program, Reston, VA 22092 USA.
[Dubrovsky, Neil M.] US Geol Survey, Sacramento, CA USA.
RP Tesoriero, AJ (reprint author), US Geol Survey, NAWQA Program, Portland, OR USA.
EM tesorier@usgs.gov
NR 32
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U1 1
U2 27
PU AMER CHEMICAL SOC
PI WASHINGTON
PA 1155 16TH ST, NW, WASHINGTON, DC 20036 USA
SN 0013-936X
J9 ENVIRON SCI TECHNOL
JI Environ. Sci. Technol.
PD FEB 1
PY 2011
VL 45
IS 3
BP 839
EP 844
DI 10.1021/es1038358
PG 6
WC Engineering, Environmental; Environmental Sciences
SC Engineering; Environmental Sciences & Ecology
GA 711HG
UT WOS:000286577100003
PM 21171622
ER
PT J
AU McKinney, MA
Letcher, RJ
Aars, J
Born, EW
Branigan, M
Dietz, R
Evans, TJ
Gabrielsen, GW
Muir, DCG
Peacock, E
Sonne, C
AF McKinney, Melissa A.
Letcher, Robert J.
Aars, Jon
Born, Erik W.
Branigan, Marsha
Dietz, Rune
Evans, Thomas J.
Gabrielsen, Geir W.
Muir, Derek C. G.
Peacock, Elizabeth
Sonne, Christian
TI Regional Contamination versus Regional Dietary Differences:
Understanding Geographic Variation in Brominated and Chlorinated
Contaminant Levels in Polar Bears
SO ENVIRONMENTAL SCIENCE & TECHNOLOGY
LA English
DT Article
ID STABLE-ISOTOPE ANALYSIS; FATTY-ACID-COMPOSITION; MARINE FOOD-WEB; FISH
POPULATIONS; TROPHIC TRANSFER; HUDSON-BAY; SEALS; SVALBARD; GREENLAND;
CHUKCHI
AB The relative contribution of regional contamination versus dietary differences to geographic variation in polar bear (Ursus maritimus) contaminant levels is unknown. Dietary variation between Alaska, Canada, East Greenland, and Svalbard subpopulations was assessed by muscle nitrogen and carbon stable isotope (delta(15)N, (delta(2)C) and adipose fatty acid (FA) signatures relative to their main prey (ringed seals). Western and southern Hudson Bay signatures were characterized by depleted delta(15)N and (delta(13)C, lower proportions of C(20) and C(22) monounsaturated FAs and higher proportions of C(18) and longer chain polyunsaturated FAs. East Greenland and Svalbard signatures were reversed relative to Hudson Bay. Alaskan and Canadian Arctic signatures were intermediate. Betweensubpopulation dietary differences predominated over interannual, seasonal, sex, or age variation. Among various brominated and chlorinated contaminants, diet signatures significantly explained variation in adipose levels of polybrominated diphenyl ether (PBDE) flame retardants (14-15%) and legacy PCBs (18-21%). However, dietary influence was contaminant class-specific, since only low or nonsignificant proportions of variation in organochlorine pesticide (e.g., chlordane) levels were explained by diet Hudson Bay diet signatures were associated with lower PCB and PBDE levels, whereas East Greenland and Svalbard signatures were associated with higher levels. Understanding diet/food web factors is important to accurately interpret contaminant trends, particularly in a changing Arctic.
C1 [McKinney, Melissa A.; Letcher, Robert J.] Environm Canada, Ecotoxicol & Wildlife Hlth Div, Sci & Technol Branch, Ottawa, ON K1A 0H3, Canada.
[McKinney, Melissa A.; Letcher, Robert J.] Carleton Univ, Dept Chem, Ottawa, ON K1S 5B6, Canada.
[Aars, Jon; Gabrielsen, Geir W.] Norwegian Polar Res Inst, NO-9296 Tromso, Norway.
[Born, Erik W.] Greenland Inst Nat Resources, Nuuk 3900, Greenland.
[Branigan, Marsha] Govt NW Terr, Dept Environm & Nat Resources, Inuvik, NT X0E 0T0, Canada.
[Dietz, Rune; Sonne, Christian] Aarhus Univ, Natl Environm Res Inst, Dept Arctic Environm, DK-4000 Roskilde, Denmark.
[Evans, Thomas J.] US Fish & Wildlife Serv, Anchorage, AK 99503 USA.
[Muir, Derek C. G.] Environm Canada, Natl Water Res Inst, Burlington, ON L7R 4A6, Canada.
[Peacock, Elizabeth] Govt Nunavut, Dept Environm, Igloolik, NU X0A 0L0, Canada.
RP McKinney, MA (reprint author), Environm Canada, Ecotoxicol & Wildlife Hlth Div, Sci & Technol Branch, Ottawa, ON K1A 0H3, Canada.
EM melissaamckinney@gmail.com; robert.letcher@ec.gc.ca
RI Daniel, Emily/A-7387-2012; Sonne, Christian/I-7532-2013; Dietz,
Rune/L-4640-2013; Dietz, Rune/F-9154-2015;
OI Sonne, Christian/0000-0001-5723-5263; Muir, Derek/0000-0001-6631-9776;
McKinney, Melissa/0000-0002-8171-7534
FU Indian and Northern Affairs Canada; Canadian International Polar Year
Secretariat; Molson Foundation; Natural Sciences and Engineering
Research Council of Canada; Canada Graduate Scholarship
FX We thank Nunavut Hunters and Trappers Organizations and Nunavut
Department of Environment staff (A. Coxon, F. Piugattuk) and
conservation officers (A. Niptanatiak, D. Fredlund, J. Ashevak, J.
Savikataaq, J. Qaunaq, A. Williams, P. Prefontaine, K. Nogier, A.
Nakashuk, L. Kudluk, N. Nakoolik, E. Qaggutaq, T. Palluq, N. Amarualik,
T. Mullin, B. J. Hainnu, G. Koonoo, T. Palluq, J. Coutu-Autut), Alaska
Native subsistence hunters and wildlife technicians, U.S. Fish and
Wildlife Service (USFWS) Marine Mammals Management biologists, NIST
National Marine Mammal Tissue Bank (R. Pugh, Hollings Marine
Laboratory), M. Andersen (Norwegian Polar Institute), local Greenland
hunters, J. Bronlund, M. Kierkegaard, S. Joensen, L. Bruun, F. Riget, H.
Tuborg and B. Sandell for sample collection and assistance. Thanks to A.
Coxon for Nunavut bear tooth aging. We thank Environment Canada staff at
NWRC (Ottawa), University of Waterloo EIL (W. Mark) for SI analysis and
K. Hobson for discussions on application and interpretation of
ecological tracers. Funding came from the Northern Contaminants Program
(Indian and Northern Affairs Canada) (R.J.L.), Canadian International
Polar Year Secretariat (E.P., R.J.L.), Molson Foundation (R.J.L.), a
Natural Sciences and Engineering Research Council of Canada Discovery
Grant (R.J.L.) and Canada Graduate Scholarship (M.A.M.), and for
Greenland, Alaska, and Svalbard sampling from the IPY program
"BearHealth" by KVUG, DANCEA and the Prince Albert Foundation (R.D.,
C.S.), the USFWS Marine Mammals Management (T.E.), and the Norwegian
Polar Institute (G.W.G.), respectively.
NR 34
TC 21
Z9 21
U1 2
U2 44
PU AMER CHEMICAL SOC
PI WASHINGTON
PA 1155 16TH ST, NW, WASHINGTON, DC 20036 USA
SN 0013-936X
J9 ENVIRON SCI TECHNOL
JI Environ. Sci. Technol.
PD FEB 1
PY 2011
VL 45
IS 3
BP 896
EP 902
DI 10.1021/es102781b
PG 7
WC Engineering, Environmental; Environmental Sciences
SC Engineering; Environmental Sciences & Ecology
GA 711HG
UT WOS:000286577100010
PM 21166451
ER
PT J
AU Hung, HW
Lin, TF
Chiou, CT
AF Hung, Hsu-Wen
Lin, Tsair-Fuh
Chiou, Cary T.
TI Reply to Comment on "Partition Coefficients of Organic Contaminants with
Carbohydrates"
SO ENVIRONMENTAL SCIENCE & TECHNOLOGY
LA English
DT Letter
ID MATTER
C1 [Hung, Hsu-Wen; Lin, Tsair-Fuh; Chiou, Cary T.] Natl Cheng Kung Univ, Dept Environm Engn, Tainan 70101, Taiwan.
[Hung, Hsu-Wen; Lin, Tsair-Fuh; Chiou, Cary T.] Natl Cheng Kung Univ, Sustainable Environm Res Ctr, Tainan 70101, Taiwan.
[Chiou, Cary T.] US Geol Survey, Denver Fed Ctr, Denver, CO 80225 USA.
RP Chiou, CT (reprint author), Natl Cheng Kung Univ, Dept Environm Engn, Tainan 70101, Taiwan.
EM carychio@mail.ncku.edu.tw
RI Lin, Tsair-Fuh/C-4056-2008; Chiou, Cary/C-3203-2013
OI Lin, Tsair-Fuh/0000-0002-2439-9090;
NR 7
TC 0
Z9 0
U1 3
U2 22
PU AMER CHEMICAL SOC
PI WASHINGTON
PA 1155 16TH ST, NW, WASHINGTON, DC 20036 USA
SN 0013-936X
J9 ENVIRON SCI TECHNOL
JI Environ. Sci. Technol.
PD FEB 1
PY 2011
VL 45
IS 3
BP 1159
EP 1159
DI 10.1021/es103898s
PG 1
WC Engineering, Environmental; Environmental Sciences
SC Engineering; Environmental Sciences & Ecology
GA 711HG
UT WOS:000286577100050
ER
PT J
AU Sanchez, BC
Ralston-Hooper, K
Sepulveda, MS
AF Sanchez, Brian C.
Ralston-Hooper, Kimberly
Sepulveda, Maria S.
TI REVIEW OF RECENT PROTEOMIC APPLICATIONS IN AQUATIC TOXICOLOGY
SO ENVIRONMENTAL TOXICOLOGY AND CHEMISTRY
LA English
DT Article; Proceedings Paper
CT 30th Annual Meeting of SETAC-North -America
CY NOV 19-23, 2009
CL New Orleans, LA
SP SETAC N Amer
DE Proteomics; Aquatic toxicology; Fish; Aquatic invertebrates
ID MUSSEL MYTILUS-EDULIS; PROTEIN EXPRESSION SIGNATURES; OXIDATIVE-STRESS;
MASS-SPECTROMETRY; 2-DIMENSIONAL ELECTROPHORESIS; BIOMARKER DISCOVERY;
MICROCYSTIN-LR; SELDI-TOF; RUDITAPES-DECUSSATUS; CADMIUM TOXICITY
AB Over the last decade, the environmental sciences have witnessed an incredible movement towards the utilization of high-throughput molecular tools that are capable of detecting simultaneous changes of hundreds, and even thousands, of molecules and molecular components after exposure of organisms to different environmental stressors. These techniques have received a great deal of attention because they not only offer the potential to unravel novel mechanisms of physiological and toxic action but are also amenable to the discovery of biomarkers of exposure and effects. In this article, we review the state of knowledge of one of these tools in ecotoxicological research: proteomics. We summarize the state of proteomics research in fish, and follow with studies conducted with aquatic invertebrates. A brief discussion on proteomic methods is also presented. We conclude with some ideas for future proteomic studies with fish and aquatic invertebrates. Environ. Toxicol. Chem. 2011;30:274-282. (C) 2010 SETAC
C1 [Sepulveda, Maria S.] Purdue Univ, W Lafayette, IN 47907 USA.
[Sanchez, Brian C.] US Fish & Wildlife Serv, Lakewood, CO USA.
[Ralston-Hooper, Kimberly] US EPA, Ecosyst Res Div, Athens, GA USA.
RP Sepulveda, MS (reprint author), Purdue Univ, W Lafayette, IN 47907 USA.
EM mssepulv@purdue.edu
RI Sepulveda, Maria/P-3598-2014
NR 79
TC 45
Z9 47
U1 6
U2 46
PU WILEY-BLACKWELL
PI MALDEN
PA COMMERCE PLACE, 350 MAIN ST, MALDEN 02148, MA USA
SN 0730-7268
J9 ENVIRON TOXICOL CHEM
JI Environ. Toxicol. Chem.
PD FEB
PY 2011
VL 30
IS 2
BP 274
EP 282
DI 10.1002/etc.402
PG 9
WC Environmental Sciences; Toxicology
SC Environmental Sciences & Ecology; Toxicology
GA 710DB
UT WOS:000286490000003
PM 21072841
ER
PT J
AU Richter, CA
Garcia-Reyero, N
Martyniuk, C
Knoebl, I
Pope, M
Wright-Osment, MK
Denslow, ND
Tillitt, DE
AF Richter, Catherine A.
Garcia-Reyero, Natalia
Martyniuk, Chris
Knoebl, Iris
Pope, Marie
Wright-Osment, Maureen K.
Denslow, Nancy D.
Tillitt, Donald E.
TI GENE EXPRESSION CHANGES IN FEMALE ZEBRAFISH (DANIO RERIO) BRAIN IN
RESPONSE TO ACUTE EXPOSURE TO METHYLMERCURY
SO ENVIRONMENTAL TOXICOLOGY AND CHEMISTRY
LA English
DT Article; Proceedings Paper
CT 30th Annual Meeting of SETAC-North -America
CY NOV 19-23, 2009
CL New Orleans, LA
SP SETAC N Amer
DE Mercury; Fish; Neurotoxicity; Molecular Biology; Toxicity Mechanisms
ID MINNOWS PIMEPHALES-PROMELAS; TROUT ONCORHYNCHUS-MYKISS; DIETARY
METHYLMERCURY; FATHEAD MINNOWS; TRANSCRIPTIONAL RESPONSE;
MERCURIC-CHLORIDE; OXIDATIVE STRESS; NEUROTOXICITY; BEHAVIOR; SYSTEM
AB Methylmercury (MeHg) is a potent neurotoxicant and endocrine disruptor that accumulates in aquatic systems. Previous studies have shown suppression of hormone levels in both male and female fish, suggesting effects on gonadotropin regulation in the brain. The gene expression profile in adult female zebrafish whole brain induced by acute (96 h) MeHg exposure was investigated. Fish were exposed by injection to 0 or 0.5 mu g MeHg/g. Gene expression changes in the brain were examined using a 22,000-feature zebrafish microarray. At a significance level of p < 0.01, 79 genes were up-regulated and 76 genes were down-regulated in response to MeHg exposure. Individual genes exhibiting altered expression in response to MeHg exposure implicate effects on glutathione metabolism in the mechanism of MeHg neurotoxicity. Gene ontology (GO) terms significantly enriched among altered genes included protein folding, cell redox homeostasis, and steroid biosynthetic process. The most affected biological functions were related to nervous system development and function, as well as lipid metabolism and molecular transport. These results support the involvement of oxidative stress and effects on protein structure in the mechanism of action of MeHg in the female brain. Future studies will compare the gene expression profile induced in response to MeHg with that induced by other toxicants and will investigate responsive genes as potential biomarkers of MeHg exposure. Environ. Toxicol. Chem. 2011;30:301-308. (C) 2010 SETAC
C1 [Richter, Catherine A.; Pope, Marie; Wright-Osment, Maureen K.; Tillitt, Donald E.] US Geol Survey, Columbia, MO USA.
[Garcia-Reyero, Natalia; Martyniuk, Chris; Knoebl, Iris; Denslow, Nancy D.] Univ Florida, Gainesville, FL USA.
RP Richter, CA (reprint author), US Geol Survey, Columbia, MO USA.
EM CRichter@usgs.gov
OI Richter, Catherine/0000-0001-7322-4206
FU NCRR NIH HHS [P40 RR012546, P40 RR012546-13]
NR 40
TC 20
Z9 20
U1 4
U2 22
PU WILEY-BLACKWELL
PI HOBOKEN
PA 111 RIVER ST, HOBOKEN 07030-5774, NJ USA
SN 0730-7268
J9 ENVIRON TOXICOL CHEM
JI Environ. Toxicol. Chem.
PD FEB
PY 2011
VL 30
IS 2
BP 301
EP 308
DI 10.1002/etc.409
PG 8
WC Environmental Sciences; Toxicology
SC Environmental Sciences & Ecology; Toxicology
GA 710DB
UT WOS:000286490000006
PM 21082716
ER
PT J
AU Gehrke, GE
Blum, JD
Marvin-DiPasquale, M
AF Gehrke, Gretchen E.
Blum, Joel D.
Marvin-DiPasquale, Mark
TI Sources of mercury to San Francisco Bay surface sediment as revealed by
mercury stable isotopes
SO GEOCHIMICA ET COSMOCHIMICA ACTA
LA English
DT Article
ID MASS-INDEPENDENT FRACTIONATION; SACRAMENTO RIVER-BASIN; MINING DISTRICT;
LAKE-SEDIMENTS; METHYL MERCURY; PABLO BAY; CALIFORNIA; ESTUARY; HG;
SPECIATION
AB Mercury (Hg) concentrations and isotopic compositions were examined in shallow-water surface sediment (0-2 cm) from San Francisco (SF) Bay to determine the extent to which historic Hg mining contributes to current Hg contamination in. SF Bay, and to assess the use of Hg isotopes to trace sources of contamination in estuaries. Inter-tidal and wetland sediment had total Hg (Hg-T) concentrations ranging from 161 to 1529 ng/g with no simple gradients of spatial variation. In contrast, inter-tidal and wetland sediment displayed a geographic gradient of delta Hg-202 values, ranging from -0.30 parts per thousand in the southern-most part of SF Bay (draining the New Almaden Hg District) to -0.99 parts per thousand in the northern-most part of SF Bay near the Sacramento-San Joaquin River Delta. Similar to SF Bay inter-tidal sediment, surface sediment from the Alviso Slough channel draining into South SF Bay had a delta Hg-202 value of -2.29 parts per thousand, while surface sediment from the Cosumnes River and Sacramento-San Joaquin River Delta draining into north SF Bay had lower average delta Hg-202 values of -0.90 parts per thousand and -0.75 parts per thousand, respectively. This isotopic trend suggests that Hg-contaminated sediment from the New Almaden Hg District mixes with Hg-contaminated sediment from a low delta He-202 source north of SF Bay. Tailings and thermally decomposed ore (calcine) from the New idria Hg mine in the California Coast Range had average delta Hg-202 values of -0.37 and +0.03 parts per thousand, respectively, showing that Hg calcination fractionates Hg isotopes resulting in Hg contamination from Hg(II) mine waste products with higher delta Hg-202 values than metallic Hg(0) produced from Hg mines. Thus, there is evidence for at least two distinct isotopic signals for Hg contamination in SF Bay: Hg associated with calcine waste materials at Hg mines in the Coast Range, such as New Almaden and New Idria; and Hg(0) produced from these mines and used in placer gold mines and/or in other industrial processes in the Sierra Nevada region and SF Bay area. (C) 2010 Elsevier Ltd. All rights reserved.
C1 [Gehrke, Gretchen E.; Blum, Joel D.] Univ Michigan, Dept Geol Sci, Ann Arbor, MI 48109 USA.
[Marvin-DiPasquale, Mark] US Geol Survey, Menlo Pk, CA 94025 USA.
RP Gehrke, GE (reprint author), Univ Michigan, Dept Geol Sci, 1100 N Univ Ave, Ann Arbor, MI 48109 USA.
EM gegehrke@umich.edu
FU Regional Monitoring Program (RMP) for Water Quality in the San Francisco
Bay; United States Environmental Protection Agency (USEPA)
FX The authors would like to acknowledge funding provided by the Regional
Monitoring Program (RMP) for Water Quality in the San Francisco Bay. The
RMP is administered by the San Francisco Estuary Institute under a
memorandum of understanding with the Regional Water Quality Control
Board. The research described in this paper also was partially funded by
the United States Environmental Protection Agency (USEPA) under the
Science to Achieve Results (STAR) Graduate Fellowship Program. EPA has
not officially endorsed this publication and the views expressed herein
may not reflect the views of the EPA. The authors thank Darell Slotton,
Shaun Ayers, Ben Greenfield, Katie Harrold, and other staff at the San
Francisco Estuary Institute for study design and sample collection. We
also thank Marcus Johnson for skillful maintenance and operation of the
MC-ICP-MS. The manuscript benefited from helpful reviews by Dave
Krabbenhoft, Ben Greenfield and two anonymous reviewers.
NR 72
TC 55
Z9 60
U1 6
U2 69
PU PERGAMON-ELSEVIER SCIENCE LTD
PI OXFORD
PA THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND
SN 0016-7037
J9 GEOCHIM COSMOCHIM AC
JI Geochim. Cosmochim. Acta
PD FEB 1
PY 2011
VL 75
IS 3
BP 691
EP 705
DI 10.1016/j.gca.2010.11.012
PG 15
WC Geochemistry & Geophysics
SC Geochemistry & Geophysics
GA 708NG
UT WOS:000286367900001
ER
PT J
AU Mars, JC
Rowan, LC
AF Mars, John C.
Rowan, Lawrence C.
TI ASTER spectral analysis and lithologic mapping of the Khanneshin
carbonatite volcano, Afghanistan
SO GEOSPHERE
LA English
DT Article
ID SPACEBORNE THERMAL EMISSION; REFLECTION RADIOMETER ASTER; ALTERED ROCKS;
AVIRIS DATA; IRON-HILL; COMPLEX; AUSTRALIA; ALGORITHM; MINERALS;
COLORADO
AB Advanced Spaceborne Thermal and Reflection Radiometer (ASTER) data of the early Quaternary Khanneshin carbonatite volcano located in southern Afghanistan were used to identify carbonate rocks within the volcano and to distinguish them from Neogene ferruginous polymict sandstone and argillite. The carbonatitic rocks are characterized by diagnostic CO(3) absorption near 11.2 mu m and 2.31-2.33 mu m, whereas the sandstone, argillite, and adjacent alluvial deposits exhibit intense Si-O absorption near 8.7 mu m caused mainly by quartz and Al-OH absorption near 2.20 mu m due to muscovite and illite.
Calcitic carbonatite was distinguished from ankeritic carbonatite in the short wave infrared (SWIR) region of the ASTER data due to a slight shift of the CO(3) absorption feature toward 2.26 mu m (ASTER band 7) in the ankeritic carbonatite spectra. Spectral assessment using ASTER SWIR data suggests that the area is covered by extensive carbonatite flows that contain calcite, ankerite, and muscovite, though some areas mapped as ankeritic carbonatite on a preexisting geologic map were not identified in the ASTER data. A contact aureole shown on the geologic map was defined using an ASTER false color composite image (R = 6, G = 3, B = 1) and a logical operator byte image. The contact aureole rocks exhibit Fe(2+), Al-OH, and Fe, Mg-OH spectral absorption features at 1.65, 2.2, and 2.33 mu m, respectively, which suggest that the contact aureole rocks contain muscovite, epidote, and chlorite. The contact aureole rocks were mapped using an Interactive Data Language (IDL) logical operator.
A visible through short wave infrared (VNIR-SWIR) mineral and rock-type map based on matched filter, band ratio, and logical operator analysis illustrates: (1) laterally extensive calcitic carbonatite that covers most of the crater and areas northeast of the crater; (2) ankeritic carbonatite located southeast and north of the crater and some small deposits located within the crater; (3) agglomerate that primarily covers the inside rim of the crater and a small area west of the crater; (4) a crater rim that consists mostly of epidote-chlorite-muscovite-rich metamorphosed argillite and sandstone; and (5) iron (Fe(3+)) and muscovite-illite-rich rocks and iron-rich eolian sands surrounding the western part of the volcano. The thermal infrared (TIR) rock-type map illustrates laterally extensive carbonatitic and mafic rocks surrounded by quartz-rich eolian and fluvial reworked sediments. In addition, the combination of VNIR, SWIR, and TIR data complement one another in that the TIR data illustrate more laterally extensive rock types and the VNIR-SWIR data distinguish more specific varieties of rocks and mineral mixtures.
C1 [Mars, John C.; Rowan, Lawrence C.] US Geol Survey, Reston, VA 20192 USA.
RP Mars, JC (reprint author), US Geol Survey, MS 954, Reston, VA 20192 USA.
EM jmars@usgs.gov
NR 36
TC 16
Z9 17
U1 1
U2 14
PU GEOLOGICAL SOC AMER, INC
PI BOULDER
PA PO BOX 9140, BOULDER, CO 80301-9140 USA
SN 1553-040X
J9 GEOSPHERE
JI Geosphere
PD FEB
PY 2011
VL 7
IS 1
BP 276
EP 289
DI 10.1130/GES00630.1
PG 14
WC Geosciences, Multidisciplinary
SC Geology
GA 713IT
UT WOS:000286732100020
ER
PT J
AU Goulden, ML
McMillan, AMS
Winston, GC
Rocha, AV
Manies, KL
Harden, JW
Bond-Lamberty, BP
AF Goulden, M. L.
McMillan, A. M. S.
Winston, G. C.
Rocha, A. V.
Manies, K. L.
Harden, J. W.
Bond-Lamberty, B. P.
TI Patterns of NPP, GPP, respiration, and NEP during boreal forest
succession
SO GLOBAL CHANGE BIOLOGY
LA English
DT Article
DE black spruce; chronosequence; fire; gross primary production; net
ecosystem production; net primary production; Picea mariana; secondary
succession
ID SPRUCE FIRE CHRONOSEQUENCE; GROSS PRIMARY PRODUCTION; ECOSYSTEM CO2
EXCHANGE; CARBON USE EFFICIENCY; PONDEROSA PINE; CONSTANT FRACTION;
INTERIOR ALASKA; EDDY COVARIANCE; WOODY DEBRIS; AGE
AB We combined year-round eddy covariance with biometry and biomass harvests along a chronosequence of boreal forest stands that were 1, 6, 15, 23, 40, similar to 74, and similar to 154 years old to understand how ecosystem production and carbon stocks change during recovery from stand-replacing crown fire. Live biomass (C(live)) was low in the 1- and 6-year-old stands, and increased following a logistic pattern to high levels in the 74- and 154-year-old stands. Carbon stocks in the forest floor (C(forest floor)) and coarse woody debris (C(CWD)) were comparatively high in the 1-year-old stand, reduced in the 6- through 40-year-old stands, and highest in the 74- and 154-year-old stands. Total net primary production (TNPP) was reduced in the 1- and 6-year-old stands, highest in the 23- through 74-year-old stands and somewhat reduced in the 154-year-old stand. The NPP decline at the 154-year-old stand was related to increased autotrophic respiration rather than decreased gross primary production (GPP). Net ecosystem production (NEP), calculated by integrated eddy covariance, indicated the 1- and 6-year-old stands were losing carbon, the 15-year-old stand was gaining a small amount of carbon, the 23- and 74-year-old stands were gaining considerable carbon, and the 40- and 154-year-old stands were gaining modest amounts of carbon. The recovery from fire was rapid; a linear fit through the NEP observations at the 6- and 15-year-old stands indicated the transition from carbon source to sink occurred within 11-12 years. The NEP decline at the 154-year-old stand appears related to increased losses from C(live) by tree mortality and possibly from C(forest floor) by decomposition. Our findings support the idea that NPP, carbon production efficiency (NPP/GPP), NEP, and carbon storage efficiency (NEP/TNPP) all decrease in old boreal stands.
C1 [Goulden, M. L.; McMillan, A. M. S.; Winston, G. C.; Rocha, A. V.] Univ Calif Irvine, Dept Earth Syst Sci, Irvine, CA 92697 USA.
[Manies, K. L.; Harden, J. W.] US Geol Survey, Menlo Pk, CA 94025 USA.
[Bond-Lamberty, B. P.] Univ Maryland, Pacific NW Natl Lab, Joint Global Change Res Inst, College Pk, MD 20740 USA.
RP Goulden, ML (reprint author), Univ Calif Irvine, Dept Earth Syst Sci, Irvine, CA 92697 USA.
EM mgoulden@uci.edu
RI Goulden, Michael/B-9934-2008; Bond-Lamberty, Ben/C-6058-2008; Rocha,
Adrian/B-6504-2013
OI Bond-Lamberty, Ben/0000-0001-9525-4633;
FU Custom Storage; Northern Lights Bed and Breakfast; Churchill River
Lodge; Brad and Tara Ritchey; National Science Foundation; Department of
Energy; Comer Foundation
FX We thank Scott Miller, Marcy Litvak, Steve Beaupre, Sami Rifai, Anders
Holmberg, Aaron Fellows, Kelsey McDuffee, Ruth Errington, and Lee Pruett
for help in the lab or field. We thank Thompson Technologies, the NASA
Terrestrial Ecology program, and the BOREAS science and support teams
for setting up and operating NOBS. We thank Custom Storage, the Northern
Lights Bed and Breakfast, the Churchill River Lodge, and Brad and Tara
Ritchey for support, space and friendship. We thank Sue Trumbore, Steve
Wofsy, Ali Dunn, Tom Gower, Brian Amiro, Marcy Litvak, and especially
Hugo Veldhuis for sharing their understanding of the boreal forest. We
thank Nisichawayasihk Cree Nation and the Canadian Government for
permission to use their land. This work was supported by grants from the
National Science Foundation, the Department of Energy, and the Comer
Foundation.
NR 62
TC 132
Z9 142
U1 19
U2 171
PU WILEY-BLACKWELL PUBLISHING, INC
PI MALDEN
PA COMMERCE PLACE, 350 MAIN ST, MALDEN 02148, MA USA
SN 1354-1013
J9 GLOBAL CHANGE BIOL
JI Glob. Change Biol.
PD FEB
PY 2011
VL 17
IS 2
BP 855
EP 871
DI 10.1111/j.1365-2486.2010.02274.x
PG 17
WC Biodiversity Conservation; Ecology; Environmental Sciences
SC Biodiversity & Conservation; Environmental Sciences & Ecology
GA 702ES
UT WOS:000285878000016
ER
PT J
AU Stapanian, MA
AF Stapanian, Martin A.
TI QuickBird satellite imagery as a tool for restoration and rehabilitation
of Lake Sevan, Armenia
SO HYDROBIOLOGIA
LA English
DT Article
C1 US Geol Survey, Lake Erie Biol Stn, Sandusky, OH 44870 USA.
RP Stapanian, MA (reprint author), US Geol Survey, Lake Erie Biol Stn, 6100 Columbus Ave, Sandusky, OH 44870 USA.
EM mstapanian@usgs.gov
OI Stapanian, Martin/0000-0001-8173-4273
NR 8
TC 0
Z9 0
U1 1
U2 6
PU SPRINGER
PI DORDRECHT
PA VAN GODEWIJCKSTRAAT 30, 3311 GZ DORDRECHT, NETHERLANDS
SN 0018-8158
J9 HYDROBIOLOGIA
JI Hydrobiologia
PD FEB
PY 2011
VL 661
IS 1
BP 81
EP 83
DI 10.1007/s10750-010-0513-3
PG 3
WC Marine & Freshwater Biology
SC Marine & Freshwater Biology
GA 691FE
UT WOS:000285064900007
ER
PT J
AU Landis, AMG
Lapointe, NWR
Angermeier, PL
AF Landis, Andrew M. Gascho
Lapointe, Nicolas W. R.
Angermeier, Paul L.
TI Individual growth and reproductive behavior in a newly established
population of northern snakehead (Channa argus), Potomac River, USA
SO HYDROBIOLOGIA
LA English
DT Article
DE Channa argus; Gonadosomatic index; Virginia; von Bertalanffy
ID LIFE-HISTORY; FISH; DYNAMICS; SYSTEM; BASS
AB Northern snakehead (Channa argus) were first found in the Potomac River in 2004. In 2007, we documented feeding and reproductive behavior to better understand how this species is performing in this novel environment. From April to October, we used electrofishing surveys to collect data on growth, condition, and gonad weight of adult fish. Growth rates of young were measured on a daily basis for several weeks. Mean length-at-age for Potomac River northern snakehead was lower than for fish from China, Russia, and Uzbekistan. Fish condition was above average during spring and fall, but below average in summer. Below-average condition corresponded to periods of high spawning activity. Gonadosomatic index indicated that females began spawning at the end of April and continued through August. Peak spawning occurred at the beginning of June when average temperatures reached 26A degrees C. Larval fish growth rate, after the transition to exogenous feeding, was 2.3 (SD +/- A 0.7) mm (total length, TL) per day. Although Potomac River northern snakehead exhibited lower overall growth rates when compared to other populations, these fish demonstrated plasticity in timing of reproduction and rapid larval growth rates. Such life history characteristics likely contribute to the success of northern snakehead in its new environment and limit managers' options for significant control of its invasion.
C1 [Landis, Andrew M. Gascho; Lapointe, Nicolas W. R.; Angermeier, Paul L.] Virginia Polytech Inst & State Univ, Dept Fisheries & Wildlife Sci, Blacksburg, VA 24061 USA.
[Angermeier, Paul L.] US Geol Survey, Virginia Cooperat Fish & Wildlife Res Unit, Blacksburg, VA 24061 USA.
RP Landis, AMG (reprint author), Auburn Univ, Dept Fisheries & Allied Aquaculture, 203 Swingle Hall, Auburn, AL 36849 USA.
EM andrewmgl@gmail.com; nlapointe@gmail.com
FU U.S. Geological Survey, Virginia Polytechnic Institute and State
University; Virginia Department of Game and Inland Fisheries; Wildlife
Management Institute
FX We are grateful to John Odenkirk and VDGIF for sharing their northern
snakehead data. We appreciate help in the field and lab from Ryan
Saylor, Eric Tobin, David Belkosky, Lluis Benejam Vidal, and Filipa
Filipe. Eric Yu translated the Chinese literature. Ryan Hunter provided
helpful comments. Fort Belvoir marina allowed convenient access to our
study sites. Northern snakehead were collected under a Virginia Tech
IACUC permit (06-198, 08-048) and a Virginia Department of Game and
Inland Fisheries collection permit: (30241 [2006, 2007], 34045 [2008]).
Use of trade names or commercial products does not imply endorsement by
the U.S. government. The Virginia Cooperative Fish and Wildlife Research
Unit is jointly sponsored by U.S. Geological Survey, Virginia
Polytechnic Institute and State University, Virginia Department of Game
and Inland Fisheries, and Wildlife Management Institute.
NR 28
TC 9
Z9 9
U1 6
U2 68
PU SPRINGER
PI DORDRECHT
PA VAN GODEWIJCKSTRAAT 30, 3311 GZ DORDRECHT, NETHERLANDS
SN 0018-8158
J9 HYDROBIOLOGIA
JI Hydrobiologia
PD FEB
PY 2011
VL 661
IS 1
BP 123
EP 131
DI 10.1007/s10750-010-0509-z
PG 9
WC Marine & Freshwater Biology
SC Marine & Freshwater Biology
GA 691FE
UT WOS:000285064900011
ER
PT J
AU Albright, TP
Ode, DJ
AF Albright, Thomas P.
Ode, David J.
TI Monitoring the dynamics of an invasive emergent macrophyte community
using operational remote sensing data
SO HYDROBIOLOGIA
LA English
DT Article
DE Curly pondweed; Remote sensing; Landsat; AWiFS; South Dakota;
Macrophytes; Monitoring; Potamogeton crispus
ID RIVER; VEGETATION; ACCURACY
AB Potamogeton crispus L. (curly pondweed) is a cosmopolitan aquatic macrophyte considered invasive in North America and elsewhere. Its range is expanding and, on individual water bodies, its coverage can be dynamic both within and among years. In this study, we evaluate the use of free and low-cost satellite remote sensing data to monitor a problematic emergent macrophyte community dominated by P. crispus. Between 2000 and 2006, we acquired eight satellite images of 24,000-ha Lake Sharpe, South Dakota (USA). During one of the dates for which satellite imagery was acquired, we sampled the lake for P. crispus and other emergent macrophytes using GPS and photography for documentation. We used cluster analysis to assist in classification of the satellite imagery and independently validated results using the field data. Resulting estimates of emergent macrophyte coverage ranged from less than 20 ha in 2002 to 245 ha in 2004. Accuracy assessment indicated 82% of image pixels were correctly classified, with errors being primarily due to failure to identify emergent macrophytes. These results emphasize the dynamic nature of P. crispus-dominated macrophyte communities and show how they can be effectively monitored over large areas using low-cost remote sensing imagery. While results may vary in other systems depending on water quality and local flora, such an approach could be applied elsewhere and for a variety of macrophyte communities.
C1 [Albright, Thomas P.] SAIC, Sioux Falls, SD USA.
[Albright, Thomas P.] USGS Ctr Earth Resources Observat & Sci, Sioux Falls, SD USA.
[Ode, David J.] S Dakota Dept Game Fish & Pk, Pierre, SD USA.
RP Albright, TP (reprint author), Univ Nevada, Dept Geog, MS0154, Reno, NV 89557 USA.
EM talbright@unr.edu
NR 18
TC 4
Z9 4
U1 3
U2 16
PU SPRINGER
PI DORDRECHT
PA VAN GODEWIJCKSTRAAT 30, 3311 GZ DORDRECHT, NETHERLANDS
SN 0018-8158
J9 HYDROBIOLOGIA
JI Hydrobiologia
PD FEB
PY 2011
VL 661
IS 1
BP 469
EP 474
DI 10.1007/s10750-010-0537-8
PG 6
WC Marine & Freshwater Biology
SC Marine & Freshwater Biology
GA 691FE
UT WOS:000285064900037
ER
PT J
AU Mordecai, RS
Mattsson, BJ
Tzilkowski, CJ
Cooper, RJ
AF Mordecai, Rua S.
Mattsson, Brady J.
Tzilkowski, Caleb J.
Cooper, Robert J.
TI Addressing challenges when studying mobile or episodic species:
hierarchical Bayes estimation of occupancy and use
SO JOURNAL OF APPLIED ECOLOGY
LA English
DT Article
DE detection probability; Louisiana waterthrush; Markov chain Monte Carlo;
monitoring; multi-scale occupancy; Seiurus motacilla; spatiotemporal
distribution; state-space modelling; WinBUGS
ID ESTIMATING SITE OCCUPANCY; POINT-COUNT SURVEYS; DETECTION PROBABILITIES;
HABITAT DISTURBANCE; IMPERFECT DETECTION; SEIURUS-MOTACILLA; BREEDING
BIRDS; LAND-COVER; HOME-RANGE; MODELS
AB P>1. Understanding the distribution and ecology of episodic or mobile species requires us to address multiple potential biases, including spatial clustering of survey locations, imperfect detectability and partial availability for detection. These challenges have been addressed individually by previous modelling approaches, but there is currently no extension of the occupancy modelling framework that accounts for all three problems while estimating occupancy (Sigma), availability for detection (i.e. use; theta) and detectability (P).
2. We describe a hierarchical Bayes multi-scale occupancy model that simultaneously estimates site occupancy, use, and detectability, while accounting for spatial dependence through a state-space approach based on repeated samples at multiple spatial or temporal scales. As an example application, we analyse the spatiotemporal distribution of the Louisiana waterthrush Seiurus motacilla with respect to catchment size and availability of potential prey based on data collected along Appalachian streams of southern West Virginia, USA. In spring 2009, single observers recorded detections of Louisiana waterthrush (henceforth, waterthrush) within 75 m of point-count stations (i.e. sites) during four 5-min surveys per site, with each survey broken into 1-min intervals.
3. Waterthrushes were widely distributed (Sigma range: 0 center dot 6-1 center dot 0) and were regularly using (theta range: 0 center dot 4-0 center dot 6) count circles along forested mountain streams. While accounting for detection biases and spatial dependence among nearby sampling sites, waterthrushes became more common as catchment area increased, and they became more available for detection as the per cent of the benthic macroinvertebrates that were of the orders Ephemeroptera, Plecoptera or Trichoptera (EPT) increased. These results lend some support to the hypothesis that waterthrushes are influenced by instream conditions as mediated by watershed size and benthic macroinvertebrate community composition.
4. Synthesis and applications. Although several available modelling techniques provide estimates of occupancy at one scale, hierarchical Bayes multi-scale occupancy modelling provides estimates of distribution at two scales simultaneously while accounting for detection biases and spatial dependencies. Hierarchical Bayes multi-scale occupancy models therefore hold significant potential for addressing complex conservation threats that operate at a landscape scale (e.g. climate change) and probably influence species distributions over multiple scales.
C1 [Mordecai, Rua S.; Mattsson, Brady J.; Cooper, Robert J.] Univ Georgia, Warnell Sch Forestry & Nat Resources, Athens, GA 30602 USA.
[Tzilkowski, Caleb J.] Natl Pk Serv, Eastern Rivers & Mt Network, University Pk, PA 16802 USA.
RP Mattsson, BJ (reprint author), US Geol Survey, Patuxent Wildlife Res Ctr, Laurel, MD 20708 USA.
EM bmattsson@usgs.gov
RI Mattsson, Brady/K-1688-2015
OI Mattsson, Brady/0000-0002-3182-9538
NR 78
TC 35
Z9 36
U1 3
U2 56
PU WILEY-BLACKWELL
PI HOBOKEN
PA 111 RIVER ST, HOBOKEN 07030-5774, NJ USA
SN 0021-8901
EI 1365-2664
J9 J APPL ECOL
JI J. Appl. Ecol.
PD FEB
PY 2011
VL 48
IS 1
BP 56
EP 66
DI 10.1111/j.1365-2664.2010.01921.x
PG 11
WC Biodiversity Conservation; Ecology
SC Biodiversity & Conservation; Environmental Sciences & Ecology
GA 703RX
UT WOS:000286000100008
ER
PT J
AU Yamaura, Y
Royle, JA
Kuboi, K
Tada, T
Ikeno, S
Makino, S
AF Yamaura, Yuichi
Royle, J. Andrew
Kuboi, Kouji
Tada, Tsuneo
Ikeno, Susumu
Makino, Shun'ichi
TI Modelling community dynamics based on species-level abundance models
from detection/nondetection data
SO JOURNAL OF APPLIED ECOLOGY
LA English
DT Article
DE data augmentation; detection; nondetection data; detectability;
functional group; hierarchical Bayesian modelling; monitoring; presence;
absence data
ID BINOMIAL MIXTURE-MODELS; PRESENCE-ABSENCE; BIOLOGICAL DIVERSITY; BIRD
ABUNDANCE; RICHNESS; DETECTABILITY; CONSERVATION; OCCUPANCY; HABITATS;
COUNTS
AB P>1. In large-scale field surveys, a binary recording of each species' detection or nondetection has been increasingly adopted for its simplicity and low cost. Because of the importance of abundance in many studies, it is desirable to obtain inferences about abundance at species-, functional group-, and community-levels from such binary data.
2. We developed a novel hierarchical multi-species abundance model based on species-level detection/nondetection data. The model accounts for the existence of undetected species, and variability in abundance and detectability among species. Species-level detection/nondetection is linked to species-level abundance via a detection model that accommodates the expectation that probability of detection (at least one individuals is detected) increases with local abundance of the species. We applied this model to a 9-year dataset composed of the detection/nondetection of forest birds, at a single post-fire site (from 7 to 15 years after fire) in a montane area of central Japan. The model allocated undetected species into one of the predefined functional groups by assuming a prior distribution on individual group membership.
3. The results suggest that 15-20 species were missed in each year, and that species richness of communities and functional groups did not change with post-fire forest succession. Overall abundance of birds and abundance of functional groups tended to increase over time, although only in the winter, while decreases in detectabilities were observed in several species.
4. Synthesis and applications. Understanding and prediction of large-scale biodiversity dynamics partly hinge on how we can use data effectively. Our hierarchical model for detection/nondetection data estimates abundance in space/time at species-, functional group-, and community-levels while accounting for undetected individuals and species. It also permits comparison of multiple communities by many types of abundance-based diversity and similarity measures under imperfect detection.
C1 [Yamaura, Yuichi; Makino, Shun'ichi] Forestry & Forest Prod Res Inst, Dept Forest Entomol, Tsukuba, Ibaraki 3058687, Japan.
[Royle, J. Andrew] US Geol Survey, Patuxent Wildlife Res Ctr, Laurel, MD 20708 USA.
[Kuboi, Kouji; Tada, Tsuneo] NPO Sch Enjoying Nat Forests, Hitachi, Ibaraki 3160032, Japan.
[Ikeno, Susumu] Wild Bird Soc Japan, Ibaraki Branch, Mito, Ibaraki 3100002, Japan.
RP Yamaura, Y (reprint author), Hokkaido Univ, Grad Sch Agr, Div Environm Resources, Kita Ku, Nishi 9,Kita 9, Sapporo, Hokkaido 0608589, Japan.
EM yamaura@for.agr.hokudai.ac.jp
RI Yamaura, Yuichi/A-3638-2012
OI Yamaura, Yuichi/0000-0001-9355-4413
FU Forestry and Forest Products Research Institute [200802]; JSPS [21-7033]
FX Suggestions from two anonymous reviewers and the editor greatly improved
our manuscript. We are grateful to M. Kery, R. Russell, and E. F. Zipkin
for their helpful reviews of a draft of this manuscript. We also thanks
for T. Amano, K. Matsumoto, Y. Mitsuda, H. Taki, K. Okabe, and S.
Sugiura for useful suggestions for this study. Y. Yamaura was supported
by Research grant No. 200802 of the Forestry and Forest Products
Research Institute, and JSPS KAKENHI (Grand-in-Aid for JSPS Fellows No.
21-7033).
NR 60
TC 20
Z9 21
U1 1
U2 44
PU WILEY-BLACKWELL
PI HOBOKEN
PA 111 RIVER ST, HOBOKEN 07030-5774, NJ USA
SN 0021-8901
EI 1365-2664
J9 J APPL ECOL
JI J. Appl. Ecol.
PD FEB
PY 2011
VL 48
IS 1
BP 67
EP 75
DI 10.1111/j.1365-2664.2010.01922.x
PG 9
WC Biodiversity Conservation; Ecology
SC Biodiversity & Conservation; Environmental Sciences & Ecology
GA 703RX
UT WOS:000286000100009
ER
PT J
AU Meier, ES
Edwards, TC
Kienast, F
Dobbertin, M
Zimmermann, NE
AF Meier, Eliane S.
Edwards, Thomas C., Jr.
Kienast, Felix
Dobbertin, Matthias
Zimmermann, Niklaus E.
TI Co-occurrence patterns of trees along macro-climatic gradients and their
potential influence on the present and future distribution of Fagus
sylvatica L.
SO JOURNAL OF BIOGEOGRAPHY
LA English
DT Article
DE Climate change; environmental gradients; Europe; forest; generalized
additive models; relative abundance; species distribution model; species
interactions; stress-gradient hypothesis
ID BIOTIC INTERACTIONS; SPECIES DISTRIBUTIONS; POSITIVE INTERACTIONS;
DISTRIBUTION MODELS; EUROPEAN BEECH; COMMUNITIES; COMPETITION;
MORPHOLOGY; GROWTH; RANGE
AB Aim
During recent and future climate change, shifts in large-scale species ranges are expected due to the hypothesized major role of climatic factors in regulating species distributions. The stress-gradient hypothesis suggests that biotic interactions may act as major constraints on species distributions under more favourable growing conditions, while climatic constraints may dominate under unfavourable conditions. We tested this hypothesis for one focal tree species having three major competitors using broad-scale environmental data. We evaluated the variation of species co-occurrence patterns in climate space and estimated the influence of these patterns on the distribution of the focal species for current and projected future climates.
Location
Europe.
Methods
We used ICP Forest Level 1 data as well as climatic, topographic and edaphic variables. First, correlations between the relative abundance of European beech (Fagus sylvatica) and three major competitor species (Picea abies, Pinus sylvestris and Quercus robur) were analysed in environmental space, and then projected to geographic space. Second, a sensitivity analysis was performed using generalized additive models (GAM) to evaluate where and how much the predicted F. sylvatica distribution varied under current and future climates if potential competitor species were included or excluded. We evaluated if these areas coincide with current species co-occurrence patterns.
Results
Correlation analyses supported the stress-gradient hypothesis: towards favourable growing conditions of F. sylvatica, its abundance was strongly linked to the abundance of its competitors, while this link weakened towards unfavourable growing conditions, with stronger correlations in the south and at low elevations than in the north and at high elevations. The sensitivity analysis showed a potential spatial segregation of species with changing climate and a pronounced shift of zones where co-occurrence patterns may play a major role.
Main conclusions
Our results demonstrate the importance of species co-occurrence patterns for calibrating improved species distribution models for use in projections of climate effects. The correlation approach is able to localize European areas where inclusion of biotic predictors is effective. The climate-induced spatial segregation of the major tree species could have ecological and economic consequences.
C1 [Meier, Eliane S.; Kienast, Felix; Dobbertin, Matthias; Zimmermann, Niklaus E.] Swiss Fed Res Inst WSL, CH-8903 Birmensdorf, Switzerland.
[Edwards, Thomas C., Jr.] Utah State Univ, US Geol Survey, Utah Cooperat Fish & Wildlife Res Unit, Logan, UT 84322 USA.
RP Meier, ES (reprint author), Swiss Fed Res Inst WSL, Zuercherstr 111, CH-8903 Birmensdorf, Switzerland.
EM eliane.meier@wsl.ch
RI Kienast, Felix/L-3536-2013; Zimmermann, Niklaus/A-4276-2008; Meier,
Eliane/D-5214-2012
OI Zimmermann, Niklaus/0000-0003-3099-9604; Meier,
Eliane/0000-0002-9545-1167
FU 6th & 7th European Framework Programme [GOCE-CT-2007-036866,
ENV-CT-2009-226544]
FX The evaluations were carried out with data submitted under the joint
EU/ICP Forests monitoring programme (http://www.icp-forests.org).
Specifically, data were used from the current member states of the EU
(excluding Cyprus), Andorra, Norway, Switzerland, Croatia, Serbia and
Republic of Belarus. This research was conducted as part of the 6th &
7th European Framework Programme Grants GOCE-CT-2007-036866 (ECOCHANGE)
and ENV-CT-2009-226544 (MOTIVE). Use of any particular product in this
research does not constitute endorsement by the US Geological Survey.
NR 56
TC 47
Z9 47
U1 4
U2 49
PU WILEY-BLACKWELL PUBLISHING, INC
PI MALDEN
PA COMMERCE PLACE, 350 MAIN ST, MALDEN 02148, MA USA
SN 0305-0270
J9 J BIOGEOGR
JI J. Biogeogr.
PD FEB
PY 2011
VL 38
IS 2
BP 371
EP 382
DI 10.1111/j.1365-2699.2010.02405.x
PG 12
WC Ecology; Geography, Physical
SC Environmental Sciences & Ecology; Physical Geography
GA 707YT
UT WOS:000286328200012
ER
PT J
AU McCleskey, RB
AF McCleskey, R. Blaine
TI Electrical Conductivity of Electrolytes Found In Natural Waters from (5
to 90) degrees C
SO JOURNAL OF CHEMICAL AND ENGINEERING DATA
LA English
DT Article
ID POTASSIUM-CHLORIDE SOLUTIONS; TOTAL DISSOLVED SOLIDS; LIMITING
EQUIVALENT CONDUCTANCES; SODIUM-HYDROXIDE SOLUTIONS; ALKALINE-EARTH
CHLORIDES; AQUEOUS-SOLUTIONS; HYDROCHLORIC-ACID; HIGH-TEMPERATURES;
CONDUCTIMETRIC DETERMINATION; CONCENTRATED SOLUTIONS
AB The electrical conductivities of 34 electrolyte solutions found in natural waters ranging from (10(-4) to 1) mol.kg(-1) in concentration and from (5 to 90) degrees C have been determined. High-quality electrical conductivity data for numerous electrolytes exist in the scientific literature, but the data do not span the concentration or temperature ranges of many electrolytes in natural waters. Methods for calculating the electrical conductivities of natural waters have incorporated these data from the literature, and as a result these methods cannot be used to reliably calculate the electrical conductivity over a large enough range of temperature and concentration. For the single-electrolyte solutions, empirical equations were developed that relate electrical conductivity to temperature and molality. For the 942 molar conductivity determinations for single electrolytes from this study, the mean relative difference between the calculated and measured values was 0.1 %. The calculated molar conductivity was compared to literature data, and the mean relative difference for 1978 measurements was 0.2 %. These data provide an improved basis for calculating electrical conductivity for most natural waters.
C1 US Geol Survey, Boulder, CO 80303 USA.
RP McCleskey, RB (reprint author), US Geol Survey, 3215 Marine St, Boulder, CO 80303 USA.
OI McCleskey, Richard/0000-0002-2521-8052
FU USGS
FX I would like to thank Kirk Nordstrom of the USGS for his assistance on
many occasions during this study and manuscript preparation. I also
would like to thank Jim Ball and Joe Ryan for their constructive
comments and reviews. This study would not have been possible without
the support of the National Research Program of the USGS. The use of
trade, product, industry, or firm names is for descriptive purposes only
and does not imply endorsement by the U.S. Government.
NR 125
TC 25
Z9 25
U1 1
U2 20
PU AMER CHEMICAL SOC
PI WASHINGTON
PA 1155 16TH ST, NW, WASHINGTON, DC 20036 USA
SN 0021-9568
J9 J CHEM ENG DATA
JI J. Chem. Eng. Data
PD FEB
PY 2011
VL 56
IS 2
BP 317
EP 327
DI 10.1021/je101012n
PG 11
WC Thermodynamics; Chemistry, Multidisciplinary; Engineering, Chemical
SC Thermodynamics; Chemistry; Engineering
GA 717SE
UT WOS:000287066900020
ER
PT J
AU Lieb, DA
Bouchard, RW
Canine, RF
AF Lieb, David A.
Bouchard, Raymond W.
Canine, Robert F.
TI CRAYFISH FAUNA OF SOUTHEASTERN PENNSYLVANIA: DISTRIBUTIONS, ECOLOGY, AND
CHANGES OVER THE LAST CENTURY
SO JOURNAL OF CRUSTACEAN BIOLOGY
LA English
DT Article
DE Cambarus acuminatus complex; Cambarus bartonii; conservation; exotic
species; Orconectes limosus; Orconectes obscurus; Orconectes rusticus;
Orconectes virilis; Procambarus acutus; Procambarus clarkii; range
shifts
ID ORCONECTES-RUSTICUS GIRARD; AUSTROPOTAMOBIUS-PALLIPES;
PROCAMBARUS-CLARKII; SCHUYLKILL RIVER; UNITED-STATES; VALLEY CREEK;
DECAPODA CAMBARIDAE; CONSERVATION STATUS; SOUTHWESTERN OHIO; HEADWATER
STREAMS
AB We describe the current distributions and relative abundances of southeastern Pennsylvania's crayfish; changes in the region's crayfish fauna over the last century; and, where pertinent, the relationship of the current fauna to site-specific characteristics, basin-wide attributes, and exotic crayfish. The crayfish fauna currently inhabiting the region bears little resemblance to the historical assemblage. Whereas historical surveys yielded Orconectes limosus and Cambarus bartonii, both native species, recent collections produced eight species including five exotics. Many areas occupied by exotic Orconectes no longer support O. limosus. Cambarus bartonii was found in a number of invaded systems, but was typically a minor component of the crayfish community and may not be able to persist in those systems indefinitely. The distribution of Cambarus (Puncticambarus) sp., an undescribed member of the Cambarus acuminatus complex, was extremely limited, with populations only found in four streams, all of which are threatened by urbanization and exotic crayfish. Exotic species collections include the first published records for Procambarus clarkii in Pennsylvania and extend the ranges of Orconectes virilis and Orconectes obscurus in the state by > 150 km. These results indicate the need for conservation and management initiatives aimed at preserving the native crayfish that remain in southeastern Pennsylvania.
C1 [Lieb, David A.] Penn State Univ, Intercoll Grad Degree Program Ecol, University Pk, PA 16802 USA.
[Bouchard, Raymond W.] Acad Nat Sci, Patrick Ctr Environm Res, Philadelphia, PA 19106 USA.
[Canine, Robert F.] Penn State Univ, Penn Cooperat Fish & Wildlife Res Unit, USGS Biol Resources Div, University Pk, PA 16802 USA.
RP Lieb, DA (reprint author), Penn State Univ, Intercoll Grad Degree Program Ecol, 435 Forest Resources Bldg, University Pk, PA 16802 USA.
EM dal105@psu.edu; rwbouchard@verizon.net; f7u@psu.edu
FU Pennsylvania Department of Conservation and Natural Resources
[AG050523]; National Park Service [H4560030064]; Pennsylvania State
[PFBC050305.01]
FX We thank Nellie Bhattarai, Hannah M. Ingram, and Jeremy Harper for their
substantial contributions. The Wild Resources Conservation Fund,
Pennsylvania Department of Conservation and Natural Resources (Project
Number AG050523); the National Park Service (Grant Agreement
H4560030064); and a Pennsylvania State Wildlife Grant (number
PFBC050305.01) provided financial support. Christopher A. Urban, Matt R.
Marshall, and Sarah Nichols administered grants and provided
encouragement. Marybeth Lieb, John E. Cooper, and an anonymous reviewer
provided helpful critiques of the paper and Erin Greb assisted with
figure preparation. Drew Reif, Mike Bilger, Rafael Lemaitre, and
especially Richard J. Horwitz and Paul F. Overbeck provided museum
records or crayfish specimens. The Stroud Water Research Center granted
access to White Clay Creek.
NR 96
TC 4
Z9 5
U1 0
U2 19
PU CRUSTACEAN SOC
PI SAN ANTONIO
PA 840 EAST MULBERRY, SAN ANTONIO, TX 78212 USA
SN 0278-0372
J9 J CRUSTACEAN BIOL
JI J. Crustac. Biol.
PD FEB
PY 2011
VL 31
IS 1
BP 166
EP 178
DI 10.1651/10-3287.1
PG 13
WC Marine & Freshwater Biology
SC Marine & Freshwater Biology
GA 722JA
UT WOS:000287427300018
ER
PT J
AU Obaza, A
DeAngelis, DL
Trexler, JC
AF Obaza, A.
DeAngelis, D. L.
Trexler, J. C.
TI Using data from an encounter sampler to model fish dispersal
SO JOURNAL OF FISH BIOLOGY
LA English
DT Article
DE Everglades; sampling bias; stratified movement model
ID UNDERWATER VIDEO; GILL NETS; SWIMMING PERFORMANCE; COMMUNITY STRUCTURE;
MINNOW TRAPS; MOVEMENT; POPULATION; BEHAVIOR; DENSITY; RIVER
AB A method to estimate speed of free-ranging fishes using a passive sampling device is described and illustrated with data from the Everglades, U.S.A. Catch per unit effort (CPUE) from minnow traps embedded in drift fences was treated as an encounter rate and used to estimate speed, when combined with an independent estimate of density obtained by use of throw traps that enclose 1 m2 of marsh habitat. Underwater video was used to evaluate capture efficiency and species-specific bias of minnow traps and two sampling studies were used to estimate trap saturation and diel-movement patterns; these results were used to optimize sampling and derive correction factors to adjust species-specific encounter rates for bias and capture efficiency. Sailfin mollies Poecilia latipinna displayed a high frequency of escape from traps, whereas eastern mosquitofish Gambusia holbrooki were most likely to avoid a trap once they encountered it; dollar sunfish Lepomis marginatus were least likely to avoid the trap once they encountered it or to escape once they were captured. Length of sampling and time of day affected CPUE; fishes generally had a very low retention rate over a 24 h sample time and only the Everglades pygmy sunfish Elassoma evergladei were commonly captured at night. Dispersal speed of fishes in the Florida Everglades, U.S.A., was shown to vary seasonally and among species, ranging from 0 center dot 05 to 0 center dot 15 m s-1 for small poeciliids and fundulids to 0 center dot 1 to 1 center dot 8 m s-1 for L. marginatus. Speed was generally highest late in the wet season and lowest in the dry season, possibly tied to dispersal behaviours linked to finding and remaining in dry-season refuges. These speed estimates can be used to estimate the diffusive movement rate, which is commonly employed in spatial ecological models.
C1 [Obaza, A.; Trexler, J. C.] Florida Int Univ, Dept Biol, N Miami, FL 33181 USA.
[DeAngelis, D. L.] US Geol Survey, Florida Integrated Sci Ctr, Ft Lauderdale, FL 33315 USA.
[DeAngelis, D. L.] Univ Miami, Dept Biol, Coral Gables, FL 33124 USA.
RP Trexler, JC (reprint author), Florida Int Univ, Dept Biol, 3000 NE 151st St, N Miami, FL 33181 USA.
EM trexlerj@fiu.edu
FU Everglades National Park [H5000060104, J5284060023]; National Science
Foundation [DEB-9910514]
FX The authors wish to thank J. Kline and members of the Trexler laboratory
for help with field work; W. Loftus and M. Heithaus assisted with this
effort and provided helpful comments on the manuscript. Financial
support for this project was provided by Cooperative Agreement
H5000060104 Task Agreement Number J5284060023 from Everglades National
Park to Florida International University. This material was developed in
collaboration with the Florida Coastal Everglades Long-Term Ecological
Research programme under National Science Foundation Grant No.
DEB-9910514. This paper is number 187 from the Tropical Biology Program
at Florida International University and publication number 492 from the
South East Research Center.
NR 58
TC 15
Z9 15
U1 1
U2 12
PU WILEY-BLACKWELL
PI MALDEN
PA COMMERCE PLACE, 350 MAIN ST, MALDEN 02148, MA USA
SN 0022-1112
J9 J FISH BIOL
JI J. Fish Biol.
PD FEB
PY 2011
VL 78
IS 2
BP 495
EP 513
DI 10.1111/j.1095-8649.2010.02867.x
PG 19
WC Fisheries; Marine & Freshwater Biology
SC Fisheries; Marine & Freshwater Biology
GA 715MH
UT WOS:000286888100007
PM 21284631
ER
PT J
AU Williams, GJ
Work, TM
Aeby, GS
Knapp, IS
Davy, SK
AF Williams, Gareth J.
Work, Thierry M.
Aeby, Greta S.
Knapp, Ingrid S.
Davy, Simon K.
TI Gross and microscopic morphology of lesions in Cnidaria from Palmyra
Atoll, Central Pacific
SO JOURNAL OF INVERTEBRATE PATHOLOGY
LA English
DT Article
DE Coral disease; Coral lesion; Growth anomaly; Tissue loss; Discoloration;
Hyperplasia; Necrosis; Fungi; Scleractinian coral; Soft coral; Zoanthid
ID CARIBBEAN SCLERACTINIAN CORALS; INDO-PACIFIC; BAND DISEASE; REEF;
CRYPTOCHIRIDAE; BRACHYURA
AB We conducted gross and microscopic characterizations of lesions in Cnidaria from Palmyra Atoll, Central Pacific. We found growth anomalies (GA) to be the most commonly encountered lesion. Cases of discoloration and tissue loss were rare. GAs had a focal or multi-focal distribution and were predominantly nodular, exophytic, and umbonate. In scleractinians, the majority of GAs manifested as hyperplasia of the basal body wall (52% of cases), with an associated absence or reduction of polyp structure (mesenteries and filaments, actinopharynx and tentacles), and depletion of zooxanthellae in the gastrodermis of the upper body wall. In the soft corals Sinularia sp. and Lobophytum sp., GAs exclusively manifested as prominent hyperplasia of the coenenchyme with an increased density of solenia. In contrast to scleractinians, soft coral GAs displayed an inflammatory and necrotizing component with marked edema of the mesoglea, accompanied by infiltrates of variably-sized granular amoebocytes. Fungi, algae, sponges, and Crustacea were present in some scleractinian GAs, but absent in soft coral GAs. Fragmentation of tissues was a common finding in Acropora acuminata and Montipora cf. dilatata colonies with tissue loss, although no obvious causative agents were seen. Discoloration in the zoanthid, Palythoa tuberculosa, was found to be the result of necrosis, while in Lobophytum sp. discoloration was the result of zooxanthellar depletion (bleaching). Soft corals with discoloration or tissue loss showed a marked inflammatory response, however no obvious causative organisms were seen. Lesions that appeared similar at the gross level were revealed to be distinct by microscopy, emphasizing the importance of histopathology. (C) 2010 Elsevier Inc. All rights reserved.
C1 [Williams, Gareth J.; Knapp, Ingrid S.; Davy, Simon K.] Victoria Univ Wellington, Sch Biol Sci, Wellington, New Zealand.
[Williams, Gareth J.; Knapp, Ingrid S.; Davy, Simon K.] Victoria Univ Wellington, Ctr Marine Environm & Econ Res, Wellington, New Zealand.
[Work, Thierry M.] US Geol Survey, Natl Wildlife Hlth Ctr, Honolulu Field Stn, Honolulu, HI 96850 USA.
[Aeby, Greta S.] Hawaii Inst Marine Biol, Kaneohe, HI 96744 USA.
RP Davy, SK (reprint author), Victoria Univ Wellington, Sch Biol Sci, POB 600, Wellington, New Zealand.
EM simon.davy@vuw.ac.nz
RI Work, Thierry/F-1550-2015
OI Work, Thierry/0000-0002-4426-9090
FU National Geographic Society; Victoria University of Wellington; New
Zealand International Doctoral Research Scholarship
FX We thank the US Fish and Wildlife Service and The Nature Conservancy for
granting access to the refuge and logistical support. Thanks also to Jim
Maragos for assistance with cnidarian taxonomy, and Scott Godwin for
assistance with gall crab taxonomy.Lastly, we thank two anonymous
referees who critically reviewed the manuscript. This work was funded,
in part, by a Grant from the National Geographic Society awarded to SKD.
GJW was supported by a Victoria University of Wellington
Vice-Chancellor's Strategic Research Scholarship and a New Zealand
International Doctoral Research Scholarship. Victoria University of
Wellington and USGS are members of the Palmyra Atoll Research Consortium
(PARC). The majority of this work was conducted under the special use
permit 12533-09015 granted by the United States Department of the
Interior Fish and Wildlife Service.
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PU ACADEMIC PRESS INC ELSEVIER SCIENCE
PI SAN DIEGO
PA 525 B ST, STE 1900, SAN DIEGO, CA 92101-4495 USA
SN 0022-2011
J9 J INVERTEBR PATHOL
JI J. Invertebr. Pathol.
PD FEB
PY 2011
VL 106
IS 2
BP 165
EP 173
DI 10.1016/j.jip.2010.08.002
PG 9
WC Zoology
SC Zoology
GA 712YG
UT WOS:000286701600001
PM 20709072
ER
PT J
AU Putirka, K
Ryerson, FJ
Perfit, M
Ridley, WI
AF Putirka, Keith
Ryerson, F. J.
Perfit, Michael
Ridley, W. Ian
TI Mineralogy and Composition of the Oceanic Mantle
SO JOURNAL OF PETROLOGY
LA English
DT Article
DE mineralogy; mantle composition; partial melting; Hawaii; Siqueiros
ID SCIENTIFIC DRILLING PROJECT; MIDOCEAN RIDGE BASALTS; EAST PACIFIC RISE;
MAUNA-KEA VOLCANO; TRACE-ELEMENT; HAWAIIAN PLUME; BENEATH HAWAII; ISLAND
BASALTS; KOOLAU VOLCANO; ORTHO-PYROXENE
AB The mineralogy of the oceanic basalt source region is examined by testing whether a peridotite mineralogy can yield observed whole-rock and olivine compositions from (1) the Hawaiian Islands, our type example of a mantle plume, and (2) the Siqueiros Transform, which provides primitive samples of normal mid-ocean ridge basalt. New olivine compositional data from phase 2 of the Hawaii Scientific Drilling Project (HSDP2) show that higher Ni-in-olivine at the Hawaiian Islands is due to higher temperatures (T) of melt generation and processing (by c. 300 degrees C) related to the Hawaiian mantle plume. Pm is low at high T, so parental Hawaiian basalts are enriched in NiO. When Hawaiian (picritic) parental magmas are transported to shallow depths, olivine precipitation occurs at lower temperatures, where D-Ni is high, leading to high Ni-in-olivine. Similarly, variations in Mn and Fe/Mn ratios in olivines are explained by contrasts in the temperatures of magma processing. Using the most mafic rocks to delimit Siqueiros and Hawaiian Co and Ni contents in parental magmas and mantle source compositions also shows that both suites can be derived from natural peridotites, but are inconsistent with partial melting of natural pyroxenites. Whole-rock compositions at Hawaii and Siqueiros are also matched by partial melting experiments conducted on peridotite bulk compositions. Hawaiian whole-rocks have elevated FeO contents compared with Siqueiros, which can be explained if Hawaiian parental magmas are generated from peridotite at 4-5 GPa, in contrast to pressures of slightly greater than 1 GPa for melt generation at Siqueiros; these pressures are consistent with olivine thermometry, as described in an earlier paper. SiO2-enriched Koolau compositions are reproduced if high-Fe Hawaiian parental magmas re-equilibrate at 1-1.5 GPa. Peridotite partial melts from experimental studies also reproduce the CaO and Al2O3 contents of Hawaiian (and Siqueiros) whole-rocks. Hawaiian magmas have TiO2 contents, however, that are enriched compared with melts from natural peridotites and magmas derived from the Siqueiros depleted mantle, and consequently may require an enriched source. TiO2 is not the only element that is enriched relative to melts of natural peridotites. Moderately incompatible elements, such as Ti, Zr, Hf, Gamma, and Eu, and compatible elements, such as Gamma b and Lu, are all enriched at the Hawaiian Islands. Such enrichments can be explained by adding 5-10% mid-ocean ridge basalt (crust) to depleted mantle; when the major element composition of such a mixture is recast into mineral components, the result is a fertile peridotite mineralogy.
C1 [Putirka, Keith] Calif State Univ Fresno, Dept Earth & Environm Sci, Fresno, CA 93740 USA.
[Ryerson, F. J.] Lawrence Livermore Natl Lab, Inst Geophys & Planetary Phys, Livermore, CA 94550 USA.
[Perfit, Michael] Univ Florida, Dept Geol Sci, Gainesville, FL 32611 USA.
[Ridley, W. Ian] US Geol Survey, Denver Fed Ctr, Denver, CO 80225 USA.
RP Putirka, K (reprint author), Calif State Univ Fresno, Dept Earth & Environm Sci, 2576 E San Ramon Ave,MS ST25, Fresno, CA 93740 USA.
EM kputirka@csufresno.edu
FU National Science Foundation [NSF-EAR 0337345, OCE-90-19154]
FX This work was supported by the National Science Foundation grants to
K.P. (NSF-EAR 0337345) and M.P. (OCE-90-19154). W.I.R. publishes with
the permission of the Director of the US Geological Survey
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PU OXFORD UNIV PRESS
PI OXFORD
PA GREAT CLARENDON ST, OXFORD OX2 6DP, ENGLAND
SN 0022-3530
J9 J PETROL
JI J. Petrol.
PD FEB
PY 2011
VL 52
IS 2
BP 279
EP 313
DI 10.1093/petrology/egq080
PG 35
WC Geochemistry & Geophysics
SC Geochemistry & Geophysics
GA 721EY
UT WOS:000287337600003
ER
PT J
AU DeMaso, SJ
Grant, WE
Hernandez, F
Brennan, LA
Silvy, NJ
Wu, XB
Bryant, FC
AF DeMaso, Stephen J.
Grant, William E.
Hernandez, Fidel
Brennan, Leonard A.
Silvy, Nova J.
Wu, X. Ben
Bryant, Fred C.
TI A Population Model to Simulate Northern Bobwhite Population Dynamics in
Southern Texas
SO JOURNAL OF WILDLIFE MANAGEMENT
LA English
DT Article
DE Colinus virginianus; model; northern bobwhite; population; simulation;
south Texas; stochastic
ID SURVIVAL; QUAIL; GROWTH; RATES; PRECIPITATION; ABUNDANCE; HARVEST; SEX
AB Models are important tools that can help managers and researchers understand the population dynamics of a species and how different habitat or population management scenarios impact that species. We used radio-telemetry data from northern bobwhites (Colinus virginianus) in southern Texas from 2000 to 2005 to develop a stochastic simulation model for bobwhite populations. Our model is based on difference equations, with stochastic variables drawn from normal and Weibull distributions. We simulated bobwhite populations to 100 yr and evaluated our model by comparing results with independent estimates of 4 population parameters (spring and fall density, finite rate of increase in the fall population [lambda], and winter juv:ad age ratios). Using a quasi-extinction criterion of <= 40 birds (density <= 0.05 birds/ha), probability of persistence to 100 yr was 88.3% (106 of 120 simulations) for the spring population and 96.7% (116 of 120 simulations) for the fall population. Using a less restrictive quasi-extinction criteria (<= 14 birds), probability of persistence was 93.3% (112 of 120 simulations) for the spring population and 98.3% (118 of 120 simulations) for the fall population. Simulated population parameters were similar to independent estimates for 4 of 4 population parameters. Winter age ratios differed between our model ((x) over bar = 4.98 juv:ad, n = 120, SE = 0.32) and empirical age ratios from harvested bobwhites on our study area ((x) over bar = 2.85 juv:ad, n = 25, SE = 0.24). However, when we corrected harvest age ratios for bias in juvenile harvest ((x) over bar = 3.85 juv:ad, n = 25, SE = 0.32) simulated and empirical estimates were similar. Our model appears to be a reliable predictor of bobwhite populations in the southern Texas. Our simulation results indicate that bobwhite hunters and managers can expect excellent bobwhite hunting (fall populations >= 2.2 birds per ha) in about one of 10 yr. (C) 2011 The Wildlife Society.
C1 [DeMaso, Stephen J.; Hernandez, Fidel; Brennan, Leonard A.; Bryant, Fred C.] Texas A&M Univ, Caesar Kleberg Wildlife Res Inst, Kingsville, TX 78363 USA.
[Grant, William E.; Silvy, Nova J.] Texas A&M Univ, Dept Wildlife & Fisheries Sci, College Stn, TX 77843 USA.
[Wu, X. Ben] Texas A&M Univ, Dept Ecosyst Sci & Management, College Stn, TX 77843 USA.
RP DeMaso, SJ (reprint author), US Fish & Wildlife Serv, 700 Cajundome Blvd, Lafayette, LA 70506 USA.
EM fidel.hernandez@tamuk.edu
RI Wu, X. Ben/E-3772-2010
OI Wu, X. Ben/0000-0001-5947-3118
FU Caesar Kleberg Wildlife Research Institute; Texas AM University; Texas
State Council, South Texas, Houston, East Texas, and Alamo chapters of
Quail Unlimited; George and Mary Josephine Hamman Foundation; Robert J.
Kleberg, Jr. and Helen C. Kleberg Foundation; Amy Shelton McNutt
Charitable Trust; Amy Shelton McNutt Memorial Fund; Bob and Vivian Smith
Foundation; William A. and Madeline Welder Smith Foundation
FX We thank the Caesar Kleberg Wildlife Research Institute and Texas A&M
University for providing financial and logistical support. Cooperative
funding was provided by the Texas State Council, South Texas, Houston,
East Texas, and Alamo chapters of Quail Unlimited; George and Mary
Josephine Hamman Foundation; Robert J. Kleberg, Jr. and Helen C. Kleberg
Foundation; Amy Shelton McNutt Charitable Trust; Amy Shelton McNutt
Memorial Fund; Bob and Vivian Smith Foundation; and The William A. and
Madeline Welder Smith Foundation. We thank F. S. Guthery, T. L. Hiller,
and T. M. Terhune for providing helpful comments on earlier versions of
this manuscript. This manuscript is Caesar Kleberg Wildlife Research
Institute publication number 10-116.
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PU WILEY-BLACKWELL
PI MALDEN
PA COMMERCE PLACE, 350 MAIN ST, MALDEN 02148, MA USA
SN 0022-541X
J9 J WILDLIFE MANAGE
JI J. Wildl. Manage.
PD FEB
PY 2011
VL 75
IS 2
BP 319
EP 332
DI 10.1002/jwmg.52
PG 14
WC Ecology; Zoology
SC Environmental Sciences & Ecology; Zoology
GA 752EA
UT WOS:000289670800009
ER
PT J
AU Haramis, GM
White, TS
AF Haramis, G. Michael
White, Timothy S.
TI A beaded collar for dual micro GPS/VHF transmitter attachment to nutria
SO MAMMALIA
LA English
DT Article
DE GPS collar; Myocastor coypus; nutria; radio telemetry; wildlife tracking
ID WHITE-TAILED DEER; KETAMINE-HYDROCHLORIDE; XYLAZINE HYDROCHLORIDE;
MYOCASTOR-COYPUS; IMMOBILIZATION; RATES; TELEMETRY
AB We report on the development of an approximately 85-g beaded collar for dual micro GPS/VHF transmitter attachment to semi-aquatic nutria (Myocastor coypus). Prototype collars were tested on captive nutria and refined during field trials. Central to the design was novel use of the VHF transmitter antenna as a collar. A circular collar was formed by passing the 44-cm antenna cable through a pre-made hole in the transmitter, leaving an approximately 16-cm upright antenna. GPS units were mounted separately via a hole in the base of each unit. For good satellite contact, GPS units (similar to 28 g) were maintained at the nape of the neck by counterbalance of the heavier VHF transmitters (similar to 50 g) positioned under the neck. To reduce friction, we lined the collar with alternate-sized plastic and, later, more durable nylon beads. The final collar configuration was worn for approximately 1 month deployments with only minor neck abrasion; one collar was worn successfully for 5 months. Foot entanglement remained the greatest risk of injury from the collar. By fitting collars tightly, we reduced the incidence of foot entanglement to 2 of 33 deployments (6%). Successful GPS tracks were acquired on 29 of 33 deployments (88%).
C1 [Haramis, G. Michael] USGS Patuxent Wildlife Res Ctr, Beltsville, MD 20705 USA.
[White, Timothy S.] USDA APHIS Wildlife Serv, Cambridge, MD 21613 USA.
RP Haramis, GM (reprint author), USGS Patuxent Wildlife Res Ctr, C-O BARC E Bldg 308,Rm 225,10300 Baltimore Ave, Beltsville, MD 20705 USA.
EM mharamis@usgs.gov
FU U.S. Fish and Wildlife Service
FX Special thanks are extended to the U.S. Fish and Wildlife Service for
financial support and to S. Kendrot and trapping personnel of the
USDA-APHIS Maryland Nutria Eradication Project for assistance in
recovering collared nutria in Maryland marshes. Additional thanks are
extended to B. Freske and J. Fringeli of the U. S. Fish and Wildlife
Service and C. Olfenbuttel of North Carolina Wildlife Resources
Commission for supporting our work with nutria at Mattamuskeet National
Wildlife Refuge. P. Brennand, J. Jones, J. Miller, and T. Wilson
provided additional valuable field assistance. G. Heinz and M. Perry
made helpful editorial comments on an earlier draft of the manuscript.
NR 17
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U1 1
U2 12
PU WALTER DE GRUYTER & CO
PI BERLIN
PA GENTHINER STRASSE 13, D-10785 BERLIN, GERMANY
SN 0025-1461
J9 MAMMALIA
JI Mammalia
PD FEB
PY 2011
VL 75
IS 1
BP 79
EP 82
DI 10.1515/MAMM.2010.070
PG 4
WC Zoology
SC Zoology
GA 780TO
UT WOS:000291882300010
ER
PT J
AU Collett, TS
Lee, MW
Agena, WF
Miller, JJ
Lewis, KA
Zyrianova, MV
Boswell, R
Inks, TL
AF Collett, Timothy S.
Lee, Myung W.
Agena, Warren F.
Miller, John J.
Lewis, Kristen A.
Zyrianova, Margarita V.
Boswell, Ray
Inks, Tanya L.
TI Permafrost-associated natural gas hydrate occurrences on the Alaska
North Slope
SO MARINE AND PETROLEUM GEOLOGY
LA English
DT Editorial Material
DE Gas hydrates; Gas; Alaska; Resources; Exploration; Petroleum system;
Drilling; Coring; Seismic analysis
ID STRATIGRAPHIC TEST WELL; METHANE HYDRATE; SEDIMENTS; PROSPECT
AB In the 1960s Russian scientists made what was then a bold assertion that gas hydrates should occur in abundance in nature. Since this early start, the scientific foundation has been built for the realization that gas hydrates are a global phenomenon, occurring in permafrost regions of the arctic and in deep water portions of most continental margins worldwide. In 1995, the U.S. Geological Survey made the first systematic assessment of the in-place natural gas hydrate resources of the United States. That study suggested that the amount of gas in the gas hydrate accumulations of northern Alaska probably exceeds the volume of known conventional gas resources on the North Slope. Researchers have long speculated that gas hydrates could eventually become a producible energy resource, yet technical and economic hurdles have historically made gas hydrate development a distant goal. This view began to change in recent years with the realization that this unconventional resource could be developed with existing conventional oil and gas production technology. One of the most significant developments was the completion of the BPXA-DOE-USGS Mount Elbert Gas Hydrate Stratigraphic Test Well on the Alaska North Slope, which along with the Mallik project in Canada, have for the first time allowed the rational assessment of gas hydrate production technology and concepts. Almost 40 years of gas hydrate research in northern Alaska has confirmed the occurrence of at least two large gas hydrate accumulations on the North Slope. We have also seen in Alaska the first ever assessment of how much gas could be technically recovered from gas hydrates. However, significant technical concerns need to be further resolved in order to assess the ultimate impact of gas hydrate energy resource development in northern Alaska. (C) 2009 Elsevier Ltd. All rights reserved.
C1 [Collett, Timothy S.; Lee, Myung W.; Agena, Warren F.; Miller, John J.; Lewis, Kristen A.; Zyrianova, Margarita V.] US Geol Survey, Energy Resources Program, Denver Fed Ctr, Denver, CO 80225 USA.
[Boswell, Ray] US DOE, Natl Energy Technol Lab, Morgantown, WV 26507 USA.
[Inks, Tanya L.] IS Interpretat Serv Inc, Denver, CO 80202 USA.
RP Collett, TS (reprint author), US Geol Survey, Energy Resources Program, Denver Fed Ctr, MS 939,Box 25046, Denver, CO 80225 USA.
EM tcollett@usgs.gov
OI Boswell, Ray/0000-0002-3824-2967
NR 58
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PU ELSEVIER SCI LTD
PI OXFORD
PA THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, OXON, ENGLAND
SN 0264-8172
J9 MAR PETROL GEOL
JI Mar. Pet. Geol.
PD FEB
PY 2011
VL 28
IS 2
BP 279
EP 294
DI 10.1016/j.marpetgeo.2009.12.001
PG 16
WC Geosciences, Multidisciplinary
SC Geology
GA 724AM
UT WOS:000287548500001
ER
PT J
AU Rose, K
Boswell, R
Collett, T
AF Rose, Kelly
Boswell, Ray
Collett, Timothy
TI Mount Elbert Gas Hydrate Stratigraphic Test Well, Alaska North Slope:
Coring operations, core sedimentology, and lithostratigraphy
SO MARINE AND PETROLEUM GEOLOGY
LA English
DT Article
DE Methane hydrates; Mount Elbert; Coring operations; Sedimentology;
Lithostratigraphy
ID ARCTIC-OCEAN; PHYSICAL-PROPERTIES; GEOCHEMISTRY; PROSPECT; TERMS; SIZE
AB In February 2007, BP Exploration (Alaska), the U.S. Department of Energy, and the U.S. Geological Survey completed the BPXA-DOE-USGS Mount Elbert Gas Hydrate Stratigraphic Test Well (Mount Elbert well) in the Milne Point Unit on the Alaska North Slope. The program achieved its primary goals of validating the pre-drill estimates of gas hydrate occurrence and thickness based on 3-D seismic interpretations and wireline log correlations and collecting a comprehensive suite of logging, coring, and pressure testing data. The upper section of the Mount Elbert well was drilled through the base of ice-bearing permafrost to a casing point of 594 m (1950 ft), approximately 15 m (50 ft) above the top of the targeted reservoir interval. The lower portion of the well was continuously cored from 606 m (1987 ft) to 760 m (2494 ft) and drilled to a total depth of 914 m. Ice-bearing permafrost extends to a depth of roughly 536 m and the base of gas hydrate stability is interpreted to extend to a depth of 870 m. Coring through the targeted gas hydrate bearing reservoirs was completed using a wireline-retrievable system. The coring program achieved 85% recovery of 7.6 cm (3 in) diameter core through 154 m (504 ft) of the hole. An onsite team processed the cores, collecting and preserving approximately 250 sub-samples for analyses of pore water geochemistry, microbiology, gas chemistry, petrophysical analysis, and thermal and physical properties. Eleven samples were immediately transferred to either methane-charged pressure vessels or liquid nitrogen for future study of the preserved gas hydrate. Additional offsite sampling, analyses, and detailed description of the cores were also conducted. Based on this work, one lithostratigraphic unit with eight subunits was identified across the cored interval. Subunits II and Va comprise :he majority of the reservoir facies and are dominantly very fine to fine, moderately sorted, quartz, feldspar, and lithic fragment-bearing to -rich sands. Lithostratigraphic and palynologic data indicate that this section is most likely early Eocene to late Paleocene in age. The examined units contain evidence for both marine and non-marine lithofacies, and indications that the depositional environment for the reservoir facies may have been shallower marine than originally interpreted based on pre-drill wireline log interpretations. There is also evidence of reduced salinity marine conditions during deposition that may be related to the paleo-climate and depositional conditions during the early Eocene. Published by Elsevier Ltd.
C1 [Rose, Kelly; Boswell, Ray] US DOE, Natl Energy Technol Lab, Morgantown, WV 26507 USA.
[Collett, Timothy] US Geol Survey, Denver Fed Ctr, Denver, CO 80225 USA.
RP Rose, K (reprint author), US DOE, Natl Energy Technol Lab, 3610 Collins Ferry Rd, Morgantown, WV 26507 USA.
EM Kelly.Rose@NETL.DOE.GOV
OI Boswell, Ray/0000-0002-3824-2967
NR 61
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PU ELSEVIER SCI LTD
PI OXFORD
PA THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, OXON, ENGLAND
SN 0264-8172
J9 MAR PETROL GEOL
JI Mar. Pet. Geol.
PD FEB
PY 2011
VL 28
IS 2
BP 311
EP 331
DI 10.1016/j.marpetgeo.2010.02.001
PG 21
WC Geosciences, Multidisciplinary
SC Geology
GA 724AM
UT WOS:000287548500003
ER
PT J
AU Winters, W
Walker, M
Hunter, R
Collett, T
Boswell, R
Rose, K
Waite, W
Torres, M
Patil, S
Dandekar, A
AF Winters, William
Walker, Michael
Hunter, Robert
Collett, Timothy
Boswell, Ray
Rose, Kelly
Waite, William
Torres, Marta
Patil, Shirish
Dandekar, Abhijit
TI Physical properties of sediment from the Mount Elbert Gas Hydrate
Stratigraphic Test Well, Alaska North Slope
SO MARINE AND PETROLEUM GEOLOGY
LA English
DT Article
DE Gas hydrate; Sagavanirktok Formation; Milne Point; Physical properties;
Grain size; Mineralogy; Porosity; Permeability
AB This study characterizes cored and logged sedimentary strata from the February 2007 BP Exploration Alaska, Department of Energy, U.S. Geological Survey (BPXA-DOE-USGS) Mount Elbert Gas Hydrate Stratigraphic Test Well on the Alaska North Slope (ANS). The physical-properties program analyzed core samples recovered from the well, and in conjunction with downhole geophysical logs, produced an extensive dataset including grain size, water content, porosity, grain density, bulk density, permeability, X-ray diffraction (XRD) mineralogy, nuclear magnetic resonance (NMR), and petrography.
This study documents the physical property interrelationships in the well and demonstrates their correlation with the occurrence of gas hydrate. Gas hydrate (GH) occurs in three unconsolidated, coarse silt to fine sand intervals within the Paleocene and Eocene beds of the Sagavanirktok Formation: Unit D-GH (614.4 m-627.9 m); unit C-GH1 (649.8 m-660.8 m); and unit C-GH2 (663.2 m-666.3 m). These intervals are overlain by fine to coarse silt intervals with greater clay content. A deeper interval (unit B) is similar lithologically to the gas-hydrate-bearing strata; however, it is water-saturated and contains no hydrate.
In this system it appears that high sediment permeability (k) is critical to the formation of concentrated hydrate deposits. Intervals D-GH and C-GH1 have average "plug" intrinsic permeability to nitrogen values of 1700 mD and 675 mD, respectively. These values are in strong contrast with those of the overlying, gas-hydrate-free sediments, which have k values of 5.7 mD and 49 mD, respectively, and thus would have provided effective seals to trap free gas. The relation between permeability and porosity critically influences the occurrence of GH. For example, an average increase of 4% in porosity increases permeability by an order of magnitude, but the presence of a second fluid (e.g., methane from dissociating gas hydrate) in the reservoir reduces permeability by more than an order of magnitude. Published by Elsevier Ltd.
C1 [Winters, William; Waite, William] US Geol Survey, Woods Hole, MA 02543 USA.
[Walker, Michael] Weatherford Labs, Houston, TX 77064 USA.
[Hunter, Robert] ASRC Energy Serv, Anchorage, AK 99503 USA.
[Collett, Timothy] US Geol Survey, Denver, CO 80225 USA.
[Boswell, Ray; Rose, Kelly] US DOE, Natl Energy Technol Lab, Morgantown, WV 26507 USA.
[Torres, Marta] Oregon State Univ, Corvallis, OR 97331 USA.
[Patil, Shirish; Dandekar, Abhijit] Univ Alaska, Fairbanks, AK 99775 USA.
RP Winters, W (reprint author), US Geol Survey, 384 Woods Hole Rd, Woods Hole, MA 02543 USA.
EM bwinters@usgs.gov
OI Waite, William/0000-0002-9436-4109; Boswell, Ray/0000-0002-3824-2967
FU U.S. Department of Energy
FX Melanie Holland, Peter Schultheiss, and Walter Barnhardt provided
helpful reviews of the manuscript. Aditya Deshpande, University of
Alaska at Fairbanks, assisted with minipermeameter measurements. BP was
the designated operator for fieldwork. The drillers and staff at the
well site are thanked for obtaining cores, performing logging runs, and
providing logistical support under adverse conditions. This work was
supported by the Coastal and Marine Geology, and Energy Programs of the
U.S. Geological Survey and funding was provided by the Gas Hydrate
Program of the U.S. Department of Energy.
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PI OXFORD
PA THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, OXON, ENGLAND
SN 0264-8172
J9 MAR PETROL GEOL
JI Mar. Pet. Geol.
PD FEB
PY 2011
VL 28
IS 2
BP 361
EP 380
DI 10.1016/j.marpetgeo.2010.01.008
PG 20
WC Geosciences, Multidisciplinary
SC Geology
GA 724AM
UT WOS:000287548500006
ER
PT J
AU Stern, LA
Lorenson, TD
Pinkston, JC
AF Stern, Laura A.
Lorenson, Thomas D.
Pinkston, John C.
TI Gas hydrate characterization and grain-scale imaging of recovered cores
from the Mount Elbert Gas Hydrate Stratigraphic Test Well, Alaska North
Slope
SO MARINE AND PETROLEUM GEOLOGY
LA English
DT Article
DE Gas hydrate; Mount Elbert; Electron microscopy; Gas chromatography;
X-ray diffraction
ID METHANE CLATHRATE HYDRATE; NATURAL-GAS; ICE
AB Using cryogenic scanning electron microscopy (CSEM), powder X-ray diffraction, and gas chromatography methods, we investigated the physical states, grain characteristics, gas composition, and methane isotopic composition of two gas-hydrate-bearing sections of core recovered from the BPXA-DOE-USGS Mount Elbert Gas Hydrate Stratigraphic Test Well situated on the Alaska North Slope. The well was continuously cored from 606.5 m to 760.1 m depth, and sections investigated here were retrieved from 619.9 m and 661.0 m depth. X-ray analysis and imaging of the sediment phase in both sections shows it consists of a predominantly fine-grained and well-sorted quartz sand with lesser amounts of feldspar, muscovite, and minor clays. Cryogenic SEM shows the gas-hydrate phase forming primarily as a pore-filling material between the sediment grains at approximately 70-75% saturation, and more sporadically as thin veins typically several tens of microns in diameter. Pore throat diameters vary, but commonly range 20-120 microns. Gas chromatography analyses of the hydrate-forming gas show that it is comprised of mainly methane (>99.9%), indicating that the gas hydrate is structure I. Here we report on the distribution and articulation of the gas-hydrate phase within the cores, the grain morphology of the hydrate, the composition of the sediment host, and the composition of the hydrate-forming gas. (C) 2009 Published by Elsevier Ltd.
C1 [Stern, Laura A.; Lorenson, Thomas D.; Pinkston, John C.] US Geol Survey, Menlo Pk, CA 94025 USA.
RP Stern, LA (reprint author), US Geol Survey, 345 Middlefield Rd, Menlo Pk, CA 94025 USA.
EM lstern@usgs.gov
FU U.S. Department of Energy
FX This work was supported by the USGS Gas Hydrate Project and partially
funded by the U.S. Department of Energy. We thank the Mount Elbert
scientific parties and field crews for providing us with the cored
sections investigated in this study. We thank T. Kneafsey of Lawrence
Berkeley Laboratory for providing preliminary CT X-ray scans of the core
sections, R. Oscarson of the USGS for technical assistance, and D. Moore
of the USGS for helpful discussions regarding clay identification.
Careful reviews of the manuscript were provided by S. Kirby and W.
Winters of the USGS and two anonymous referees. Use of product and/or
trade names is for descriptive purposes only and does not imply
endorsement by the U.S. Government.
NR 33
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PU ELSEVIER SCI LTD
PI OXFORD
PA THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, OXON, ENGLAND
SN 0264-8172
J9 MAR PETROL GEOL
JI Mar. Pet. Geol.
PD FEB
PY 2011
VL 28
IS 2
BP 394
EP 403
DI 10.1016/j.marpetgeo.2009.08.003
PG 10
WC Geosciences, Multidisciplinary
SC Geology
GA 724AM
UT WOS:000287548500008
ER
PT J
AU Lu, HL
Lorenson, TD
Moudrakovski, IL
Ripmeester, JA
Collett, TS
Hunter, RB
Ratcliffe, CI
AF Lu, Hailong
Lorenson, Thomas D.
Moudrakovski, Igor L.
Ripmeester, John A.
Collett, Timothy S.
Hunter, Robert B.
Ratcliffe, Chris I.
TI The characteristics of gas hydrates recovered from the Mount Elbert Gas
Hydrate Stratigraphic Test Well, Alaska North Slope
SO MARINE AND PETROLEUM GEOLOGY
LA English
DT Article
DE Gas hydrate; Crystal structure; Hydration number; Isotope; Geochemistry;
Alaska; North Slope
ID DISSOCIATION
AB Systematic analyses have been carried out on two gas hydrate-bearing sediment core samples, HYPV4, which was preserved by CH4 gas pressurization, and HYLN7, which was preserved in liquid-nitrogen, recovered from the BPXA-DOE-USGS Mount Elbert Stratigraphic Test Well. Gas hydrate in the studied core samples was found by observation to have developed in sediment pores, and the distribution of hydrate saturation in the cores imply that gas hydrate had experienced stepwise dissociation before it was stabilized by either liquid nitrogen or pressurizing gas. The gas hydrates were determined to be structure Type I hydrate with hydration numbers of approximately 6.1 by instrumentation methods such as powder X-ray diffraction, Raman spectroscopy and solid state C-13 NMR. The hydrate gas composition was predominantly methane, and isotopic analysis showed that the methane was of thermogenic origin (mean delta C-13 = 48.6 parts per thousand and delta(D) = 248 parts per thousand for sample HYLN7). Isotopic analysis of methane from sample HYPV4 revealed secondary hydrate formation from the pressurizing methane gas during storage. (C) 2010 Elsevier Ltd. All rights reserved.
C1 [Lu, Hailong; Moudrakovski, Igor L.; Ripmeester, John A.; Ratcliffe, Chris I.] Natl Res Council Canada, Steacie Inst Mol Sci, Ottawa, ON J9J 2R8, Canada.
[Lorenson, Thomas D.] US Geol Survey, Menlo Pk, CA 94025 USA.
[Collett, Timothy S.] US Geol Survey, Denver, CO 80225 USA.
RP Lu, HL (reprint author), Natl Res Council Canada, Steacie Inst Mol Sci, Ottawa, ON J9J 2R8, Canada.
EM hailong.lu@nrc-cnrc.gc.ca
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SN 0264-8172
J9 MAR PETROL GEOL
JI Mar. Pet. Geol.
PD FEB
PY 2011
VL 28
IS 2
BP 411
EP 418
DI 10.1016/j.marpetgeo.2010.01.002
PG 8
WC Geosciences, Multidisciplinary
SC Geology
GA 724AM
UT WOS:000287548500010
ER
PT J
AU Wilson, SJ
Hunter, RB
Collett, TS
Hancock, S
Boswell, R
Anderson, BJ
AF Wilson, Scott J.
Hunter, Robert B.
Collett, Timothy S.
Hancock, Steve
Boswell, Ray
Anderson, Brian J.
TI Alaska North Slope regional gas hydrate production modeling forecasts
SO MARINE AND PETROLEUM GEOLOGY
LA English
DT Article
DE Gas hydrates; Alaska North Slope; Resource development modeling;
Production forecasting
AB A series of gas hydrate development scenarios were created to assess the range of outcomes predicted for the possible development of the "Eileen" gas hydrate accumulation, North Slope, Alaska. Production forecasts for the "reference case" were built using the 2002 Mallik production tests, mechanistic simulation, and geologic studies conducted by the US Geological Survey. Three additional scenarios were considered: A "downside-scenario" which fails to identify viable production, an "upside-scenario" describes results that are better than expected. To capture the full range of possible outcomes and balance the downside case, an "extreme upside scenario" assumes each well is exceptionally productive.
Starting with a representative type-well simulation forecasts, field development timing is applied and the sum of individual well forecasts creating the field-wide production forecast. This technique is commonly used to schedule large-scale resource plays where drilling schedules are complex and production forecasts must account for many changing parameters. The complementary forecasts of rig count, capital investment, and cash flow can be used in a pre-appraisal assessment of potential commercial viability.
Since no significant gas sales are currently possible on the North Slope of Alaska, typical parameters were used to create downside, reference, and upside case forecasts that predict from 0 to 71 BM3 (2.5 tcf) of gas may be produced in 20 years and nearly 283 BM3 (10 tcf) ultimate recovery after 100 years.
Outlining a range of possible outcomes enables decision makers to visualize the pace and milestones that will be required to evaluate gas hydrate resource development in the Eileen accumulation. Critical values of peak production rate, time to meaningful production volumes, and investments required to rule out a downside case are provided. Upside cases identify potential if both depressurization and thermal stimulation yield positive results. An "extreme upside" case captures the full potential of unconstrained development with widely spaced wells. The results of this study indicate that recoverable gas hydrate resources may exist in the Eileen accumulation and that it represents a good opportunity for continued research. (C) 2010 Elsevier Ltd. All rights reserved.
C1 [Wilson, Scott J.] Ryder Scott Co LP, Denver, CO 80293 USA.
[Hunter, Robert B.] ASRC Energy Serv, Anchorage, AK 99503 USA.
[Collett, Timothy S.] US Geol Survey, Denver Fed Ctr, Denver, CO 80225 USA.
[Hancock, Steve] RPS Energy Canada, Calgary, AB T2P 3T6, Canada.
[Boswell, Ray; Anderson, Brian J.] Natl Energy Technol Lab, Morgantown, WV 26507 USA.
[Anderson, Brian J.] W Virginia Univ, Dept Chem Engn, Morgantown, WV 26506 USA.
RP Wilson, SJ (reprint author), Ryder Scott Co LP, 621 17th St,Suite 1550, Denver, CO 80293 USA.
EM scott.wilson@ryderscott.com
OI Boswell, Ray/0000-0002-3824-2967
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SN 0264-8172
J9 MAR PETROL GEOL
JI Mar. Pet. Geol.
PD FEB
PY 2011
VL 28
IS 2
BP 460
EP 477
DI 10.1016/j.marpetgeo.2010.03.007
PG 18
WC Geosciences, Multidisciplinary
SC Geology
GA 724AM
UT WOS:000287548500015
ER
PT J
AU Anderson, BJ
Kurihara, M
White, MD
Moridis, GJ
Wilson, SJ
Pooladi-Darvish, M
Gaddipati, M
Masuda, Y
Collett, TS
Hunter, RB
Narita, H
Rose, K
Boswell, R
AF Anderson, Brian J.
Kurihara, Masanori
White, Mark D.
Moridis, George J.
Wilson, Scott J.
Pooladi-Darvish, Mehran
Gaddipati, Manohar
Masuda, Yoshihiro
Collett, Timothy S.
Hunter, Robert B.
Narita, Hideo
Rose, Kelly
Boswell, Ray
TI Regional long-term production modeling from a single well test, Mount
Elbert Gas Hydrate Stratigraphic Test Well, Alaska North Slope
SO MARINE AND PETROLEUM GEOLOGY
LA English
DT Article
DE Gas hydrates; Reservoir simulations; Production modeling; Porous media
AB Following the results from the open-hole formation pressure response test in the BPXA-DOE-USGS Mount Elbert Gas Hydrate Stratigraphic Test Well (Mount Elbert well) using Schluinberger's Modular Dynamics Formation Tester (MDT) wireline tool, the International Methane Hydrate Reservoir Simulator Code Comparison project performed long-term reservoir simulations on three different model reservoirs. These descriptions were based on 1) the Mount Elbert gas hydrate accumulation as delineated by an extensive history-matching exercise, 2) an estimation of the hydrate accumulation near the Prudhoe Bay L-pad, and 3) a reservoir that would be down-dip of the Prudhoe Bay L-pad and therefore warmer and deeper. All of these simulations were based, in part, on the results of the MDT results from the Mount Elbert Well. The comparison group's consensus value for the initial permeability of the hydrate-filled reservoir (k = 0.12 mD) and the permeability model based on the MDT history match were used as the basis for subsequent simulations on the three regional scenarios. The simulation results of the five different simulation codes, CMG STARS, HydrateResSirn, MH-21 HYDRES, STOMP-HYD, and TOUGH+HYDRATE exhibit good qualitative agreement and the variability of potential methane production rates from gas hydrate reservoirs is illustrated. As expected, the predicted methane production rate increased with increasing in situ reservoir temperature; however, a significant delay in the onset of rapid hydrate dissociation is observed for a cold, homogeneous reservoir and it is found to be repeatable. The inclusion of reservoir heterogeneity in the description of this cold reservoir is shown to eliminate this delayed production. Overall, simulations utilized detailed information collected across the Mount Elbert reservoir either obtained or determined from geophysical well logs, including thickness (37 ft), porosity (35%), hydrate saturation (65%), intrinsic permeability (1000 mD), pore water salinity (5 ppt), and formation temperature (3.3-3.9 degrees C). This paper presents the approach and results of extrapolating regional forward production modeling from history-matching efforts on the results from a single well test. (C) 2010 Elsevier Ltd. All rights reserved.
C1 [Anderson, Brian J.; Gaddipati, Manohar] W Virginia Univ, Dept Chem Engn, NETL IAES, Morgantown, WV 26506 USA.
[Anderson, Brian J.; Gaddipati, Manohar; Rose, Kelly; Boswell, Ray] Natl Energy Technol Lab, Morgantown, WV 26507 USA.
[Kurihara, Masanori] Japan Oil Engn Co Ltd, Chuo Ku, Tokyo 1040054, Japan.
[White, Mark D.] Pacific NW Natl Lab, Hydrol Grp, Richland, WA 99352 USA.
[Moridis, George J.] Univ Calif Berkeley, Lawrence Berkeley Lab, Div Earth Sci, Berkeley, CA 94720 USA.
[Wilson, Scott J.] Ryder Scott Co LP, Denver, CO 80120 USA.
[Pooladi-Darvish, Mehran] Fekete Associates Inc, Calgary, AB T2P 0M2, Canada.
[Masuda, Yoshihiro] Univ Tokyo, Dept Geosyst Engn, Tokyo 1138654, Japan.
[Collett, Timothy S.] US Geol Survey, Denver Fed Ctr, Denver, CO 80225 USA.
[Hunter, Robert B.] ASRC Energy Serv, Anchorage, AK 99503 USA.
[Narita, Hideo] Natl Inst Adv Ind Sci & Technol, Methane Hydrate Res Lab, Sapporo, Hokkaido 0628517, Japan.
RP Anderson, BJ (reprint author), W Virginia Univ, Dept Chem Engn, NETL IAES, POB 6102, Morgantown, WV 26506 USA.
EM brian.anderson@mail.wvu.edu
OI Boswell, Ray/0000-0002-3824-2967
FU National Energy Technology Laboratory of the U.S. Department of Energy;
U.S. Geological Survey; Japan MH-21 project; BP Exploration (Alaska)
FX The authors would like to thank the National Energy Technology
Laboratory of the U.S. Department of Energy, the U.S. Geological Survey,
the Japan MH-21 project, and BP Exploration (Alaska) for supporting this
effort. We would also like to acknowledge the Mount Elbert science party
for sharing the data obtained at Mount Elbert for use in our
history-matching and production simulations.
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SN 0264-8172
J9 MAR PETROL GEOL
JI Mar. Pet. Geol.
PD FEB
PY 2011
VL 28
IS 2
BP 493
EP 501
DI 10.1016/j.marpetgeo.2010.01.015
PG 9
WC Geosciences, Multidisciplinary
SC Geology
GA 724AM
UT WOS:000287548500017
ER
PT J
AU Moridis, GJ
Silpngarmlert, S
Reagan, MT
Collett, T
Zhang, K
AF Moridis, G. J.
Silpngarmlert, S.
Reagan, M. T.
Collett, T.
Zhang, K.
TI Gas production from a cold, stratigraphically-bounded gas hydrate
deposit at the Mount Elbert Gas Hydrate Stratigraphic Test Well, Alaska
North Slope: Implications of uncertainties
SO MARINE AND PETROLEUM GEOLOGY
LA English
DT Article
DE Hydrates; Permafrost; Methane; Gas production
ID DECOMPOSITION; RESERVOIRS; SEDIMENTS
AB As part of an effort to identify suitable targets for a planned long-term field test, we investigate by means of numerical simulation the gas production potential from unit D, a stratigraphically bounded (Class 3) permafrost-associated hydrate occurrence penetrated in the BPXA-DOE-USGS Mount Elbert Gas Hydrate Stratigraphic Test Well on North Slope, Alaska. This shallow, low-pressure deposit has high porosities (phi = 0.4), high intrinsic permeabilities (k = 10(-12) m(2)) and high hydrate saturations (S-H = 0.65). It has a low temperature (T = 2.3-2.6 degrees C) because of its proximity to the overlying permafrost. The simulation results indicate that vertical wells operating at a constant bottomhole pressure would produce at very low rates for a very long period. Horizontal wells increase gas production by almost two orders of magnitude, but production remains low. Sensitivity analysis indicates that the initial deposit temperature is by the far the most important factor determining production performance (and the most effective criterion for target selection) because it controls the sensible heat available to fuel dissociation. Thus, a 1 degrees C increase in temperature is sufficient to increase the production rate by a factor of almost 8. Production also increases with a decreasing hydrate saturation (because of a larger effective permeability for a given k), and is favored (to a lesser extent) by anisotropy. Published by Elsevier Ltd.
C1 [Moridis, G. J.; Reagan, M. T.; Zhang, K.] Univ Calif Berkeley, Lawrence Berkeley Lab, Berkeley, CA 94720 USA.
[Silpngarmlert, S.] Conoco Phillips, Houston, TX 77252 USA.
[Collett, T.] US Geol Survey, Denver Fed Ctr, Denver, CO 80225 USA.
RP Reagan, MT (reprint author), Univ Calif Berkeley, Lawrence Berkeley Lab, 1 Cyclotron Rd, Berkeley, CA 94720 USA.
EM mtreagan@lbl.gov
RI Reagan, Matthew/D-1129-2015
OI Reagan, Matthew/0000-0001-6225-4928
FU Office of Natural Gas and Petroleum Technology, through the National
Energy Technology Laboratory, under the U.S. Department of Energy
[DE-AC02-05CH11231]
FX This work was supported by the Assistant Secretary for Fossil Energy,
Office of Natural Gas and Petroleum Technology, through the National
Energy Technology Laboratory, under the U.S. Department of Energy,
Contract No. DE-AC02-05CH11231. The authors are indebted to John Apps
and Dan Hawkes for their careful review.
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SN 0264-8172
J9 MAR PETROL GEOL
JI Mar. Pet. Geol.
PD FEB
PY 2011
VL 28
IS 2
BP 517
EP 534
DI 10.1016/j.marpetgeo.2010.01.005
PG 18
WC Geosciences, Multidisciplinary
SC Geology
GA 724AM
UT WOS:000287548500019
ER
PT J
AU Lee, MW
Agena, WF
Collett, TS
Inks, TL
AF Lee, M. W.
Agena, W. F.
Collett, T. S.
Inks, T. L.
TI Pre- and post-drill comparison of the Mount Elbert gas hydrate prospect,
Alaska North Slope
SO MARINE AND PETROLEUM GEOLOGY
LA English
DT Article
DE Gas hydrate; Mount Elbert; Prospecting; Thin-bed analysis; Estimation
AB In 2006, the United States Geological Survey (USGS) completed a detailed analysis and interpretation of available 2-D and 3-D seismic data, along with seismic modeling and correlation with specially processed downhole well log data for identifying potential gas hydrate accumulations on the North Slope of Alaska. A methodology was developed for identifying sub-permafrost gas hydrate prospects within the gas hydrate stability zone in the Milne Point area. The study revealed a total of 14 gas hydrate prospects in this area.
In order to validate the gas hydrate prospecting protocol of the USGS and to acquire critical reservoir data needed to develop a longer-term production testing program, a stratigraphic test well was drilled at the Mount Elbert prospect in the Milne Point area in early 2007. The drilling confirmed the presence of two prominent gas-hydrate-bearing units in the Mount Elbert prospect, and high quality well logs and core data were acquired. The post-drill results indicate pre-drill predictions of the reservoir thickness and the gas-hydrate saturations based on seismic and existing well data were 90% accurate for the upper unit (hydrate unit D) and 70% accurate for the lower unit (hydrate unit C), confirming the validity of the USGS approach to gas hydrate prospecting. The Mount Elbert prospect is the first gas hydrate accumulation on the North Slope of Alaska identified primarily on the basis of seismic attribute analysis and specially processed downhole log data. Post-drill well log data enabled a better constraint of the elastic model and the development of an improved approach to the gas hydrate prospecting using seismic attributes. Published by Elsevier Ltd.
C1 [Lee, M. W.; Agena, W. F.; Collett, T. S.] US Geol Survey, Denver Fed Ctr, Cent Energy Team, Denver, CO 80225 USA.
[Inks, T. L.] IS Interpretat Serv Inc, Denver, CO 80202 USA.
RP Lee, MW (reprint author), US Geol Survey, Denver Fed Ctr, Cent Energy Team, MS 939,Box 25046, Denver, CO 80225 USA.
EM mlee@usgs.gov
FU U.S. Geological Survey; U.S. Department of Energy [DE-AI21-92MC29214];
U.S. Bureau of Land Management [LAI-02-0015]
FX We thank the Mount Elbert Science Team for the successful logging and
coring program at the Mount Elbert well under adverse weather
conditions. We also thank Kristen Lewis and Kelly Rose for their many
helpful comments and suggestions for the paper. This contribution was
funded by the U.S. Geological Survey Energy Resources Program, the U.S.
Department of Energy under Interagency Agreement No. DE-AI21-92MC29214,
and the U.S. Bureau of Land Management under Interagency Agreement No.
LAI-02-0015.
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SN 0264-8172
J9 MAR PETROL GEOL
JI Mar. Pet. Geol.
PD FEB
PY 2011
VL 28
IS 2
BP 578
EP 588
DI 10.1016/j.marpetgeo.2009.08.007
PG 11
WC Geosciences, Multidisciplinary
SC Geology
GA 724AM
UT WOS:000287548500023
ER
PT J
AU Bromaghin, JF
Nielson, RM
Hard, JJ
AF Bromaghin, Jeffrey F.
Nielson, Ryan M.
Hard, Jeffrey J.
TI A MODEL OF CHINOOK SALMON POPULATION DYNAMICS INCORPORATING
SIZE-SELECTIVE EXPLOITATION AND INHERITANCE OF POLYGENIC CORRELATED
TRAITS
SO NATURAL RESOURCE MODELING
LA English
DT Article
DE Fishery-induced evolution; fishery-induced adaptation; selective
fisheries; Oncorhynchus tshawytscha; fishery management; fishery
conservation; individual-based model; age-structured model; Yukon River
ID FISHERIES-INDUCED EVOLUTION; INDIVIDUAL-BASED MODEL; EVOLVING FISH
STOCKS; PACIFIC SALMON; ONCORHYNCHUS-TSHAWYTSCHA; ARTIFICIAL SELECTION;
MARINE FISHERIES; TIME SCALES; MATE CHOICE; AGE
AB P>Concern regarding the potential for selective fisheries to degrade desirable characteristics of exploited fish populations is growing worldwide. Although the occurrence of fishery-induced evolution in a wild population has not been irrefutably documented, considerable theoretical and empirical evidence for that possibility exists. Environmental conditions influence survival and growth in many species and may mask comparatively subtle trends induced by selective exploitation, especially given the evolutionarily short time series of data available from many fisheries. Modeling may be the most efficient investigative tool under such conditions. Motivated by public concern that large-mesh gillnet fisheries may be altering Chinook salmon in western Alaska, we constructed a stochastic model of the population dynamics of Chinook salmon. The model contained several individually based components and incorporated size-selective exploitation, assortative mating, size-dependent female fecundity, density-dependent survival, and the heritability of size and age. Substantial reductions in mean size and age were observed under all scenarios. Concurrently reducing directional selection and increasing spawning abundance was most effective in stimulating population recovery. Use of this model has potential to improve our ability to investigate the consequences of selective exploitation and aid development of improved management strategies to more effectively sustain fish and fisheries into the future.
C1 [Bromaghin, Jeffrey F.] US Fish & Wildlife Serv, Fisheries & Ecol Serv, Anchorage, AK 99503 USA.
[Nielson, Ryan M.] Western EcoSyst Technol Inc, Laramie, WY 82070 USA.
[Hard, Jeffrey J.] NOAA, Natl Marine Fisheries Serv, NW Fisheries Sci Ctr, Conservat Biol Div, Seattle, WA 98112 USA.
RP Bromaghin, JF (reprint author), US Geol Survey, Alaska Sci Ctr, 4210 Univ Dr, Anchorage, AK 99508 USA.
EM jbromaghin@usgs.gov; rnielson@west-inc.com; jeff.hard@noaa.gov
RI Hard, Jeffrey/C-7229-2009; Bromaghin, Jeffrey/B-5058-2009
OI Bromaghin, Jeffrey/0000-0002-7209-9500
FU National Oceanic and Atmospheric Administration, U.S. Department of
Commerce [NA16FP2993]
FX We thank Danielle Evenson and Toshihide Hamazaki (Alaska Department of
Fish and Game, Commercial Fisheries Division, Anchorage Alaska) for
providing data on Yukon River Chinook salmon. David Patterson and
Michael Bradford (Department of Fisheries and Oceans, Cooperative
Resource Management Institute, School of Resource and Environmental
Management, Simon Fraser University, Burnaby, British Columbia) provided
assistance via discussions of the reproductive behavior and survival of
salmon. We thank Lyman McDonald (West Inc., Laramie, Wyoming) for
helpful comments and review of the proposed models during model
development. David Hankin (Department of Fisheries Biology, Humboldt
State University, Arcata, California) and Brian Riddell (Department of
Fisheries and Oceans, Pacific Biological Station, Nanaimo, British
Columbia) provided insightful technical reviews of a draft agency report
that were extremely helpful in improving the contents and presentation
of the manuscript. This work was partially funded under award NA16FP2993
from the National Oceanic and Atmospheric Administration, U.S.
Department of Commerce, as authorized by the Arctic Yukon Kuskokwim
Sustainable Salmon Initiative (www.aykssi.org). The statements,
findings, conclusions, and recommendations are those of the authors and
do not necessarily reflect the views of the National Oceanic and
Atmospheric Administration, the Department of Commerce, the Arctic Yukon
Kuskokwim Sustainable Salmon Initiative, or the U. S. Fish and Wildlife
Service. Karen Gillis (Arctic Yukon Kuskokwim Sustainable Salmon
Initiative and Bering Sea Fishermen's Association, Anchorage, Alaska)
provided invaluable administrative support throughout the duration of
this investigation. The editor and two anonymous reviewers provided
valuable suggestions for improving the manuscript.
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SN 0890-8575
EI 1939-7445
J9 NAT RESOUR MODEL
JI Nat. Resour. Model.
PD FEB
PY 2011
VL 24
IS 1
BP 1
EP 47
DI 10.1111/j.1939-7445.2010.00077.x
PG 47
WC Environmental Sciences; Mathematics, Interdisciplinary Applications
SC Environmental Sciences & Ecology; Mathematics
GA 714WJ
UT WOS:000286839400001
ER
PT J
AU McGowan, CP
Smith, DR
Sweka, JA
Martin, J
Nichols, JD
Wong, R
Lyons, JE
Niles, LJ
Kalasz, K
Brust, J
AF McGowan, Conor P.
Smith, David R.
Sweka, John A.
Martin, Julien
Nichols, James D.
Wong, Richard
Lyons, James E.
Niles, Lawrence J.
Kalasz, Kevin
Brust, Jeffrey
TI MULTISPECIES MODELING FOR ADAPTIVE MANAGEMENT OF HORSESHOE CRABS AND RED
KNOTS IN THE DELAWARE BAY
SO NATURAL RESOURCE MODELING
LA English
DT Article
DE Calidris canutus rufa; Limulus polyphemus; population modeling;
structured decision making; two species model; two sex model
ID LIMULUS-POLYPHEMUS; NEW-JERSEY; POPULATION; SHOREBIRDS; ABUNDANCE;
HARVEST; EGGS; AVAILABILITY; RECAPTURE; OPTIMIZATION
AB P>Adaptive management requires that predictive models be explicit and transparent to improve decisions by comparing management actions, directing further research and monitoring, and facilitating learning. The rufa subspecies of red knots (Calidris canutus rufa), which has recently exhibited steep population declines, relies on horseshoe crab (Limulus polyphemus) eggs as their primary food source during stopover in Delaware Bay during spring migration. We present a model with two different parameterizations for use in the adaptive management of horseshoe crab harvests in the Delaware Bay that links red knot mass gain, annual survival, and fecundity to horseshoe crab dynamics. The models reflect prevailing hypotheses regarding ecological links between these two species. When reported crab harvest from 1998 to 2008 was applied, projections corresponded to the observed red knot population abundances depending on strengths of the demographic relationship between these species. We compared different simulated horseshoe crab harvest strategies to evaluate whether, given this model, horseshoe crab harvest management can affect red knot conservation and found that restricting harvest can benefit red knot populations. Our model is the first to explicitly and quantitatively link these two species and will be used within an adaptive management framework to manage the Delaware Bay system and learn more about the specific nature of the linkage between the two species.
C1 [McGowan, Conor P.; Martin, Julien; Nichols, James D.] USGS, Patuxent Wildlife Res Ctr, Laurel, MD 20708 USA.
[McGowan, Conor P.] N Carolina State Univ, Dept Biol, Raleigh, NC 27695 USA.
[Smith, David R.] USGS, Leetown Sci Ctr, Kearneysville, WV 25430 USA.
[Sweka, John A.] US Fish & Wildlife Serv, NE Fishery Ctr, Lamar, PA 16848 USA.
[Martin, Julien] Fish & Wildlife Res Inst, Florida Fish & Wildlife Conservat Commiss, St Petersburg, FL 33701 USA.
[Wong, Richard; Kalasz, Kevin] Delaware Div Fish & Wildlife, Smyrna, DE 19977 USA.
[Lyons, James E.] US Fish & Wildlife Serv, Div Migratory Birds, Laurel, MD 20708 USA.
[Niles, Lawrence J.] Conserve Wildlife Fdn New Jersey, Bordenton, NJ 08505 USA.
[Brust, Jeffrey] Div Fish & Wildlife, New Jersey Dept Environm Protect, Port Republic, NJ 08241 USA.
RP McGowan, CP (reprint author), Auburn Univ, Sch Forestry & Wildlife Sci, USGS Alabama Cooperat Fish & Wildlife Res Unit, 602 Duncan Dr, Auburn, AL 36849 USA.
EM cmcgowan@usgs.gov; drsmith@usgs.gov; John_Sweka@fws.gov;
Julienm@ufl.edu; jnichols@usgs.gov; Richard.wong@de.state.us;
James_Lyons@fws.gov; larry.niles@gmail.com; Kevin.Kalasz@state.de.us;
Jeffrey.Brust@dep.state.nj.us
FU National Fish and Wildlife Foundation; U.S. Geological Survey Science
FX The authors thank the National Fish and Wildlife Foundation and U.S.
Geological Survey Science Support Program for funding this work. We also
thank A. J. Baker, N. A. Clark, and the Joint Horseshoe Crab and
Shorebird Technical Committee of the Atlantic State Marine Fisheries
Commission for discussions on our modeling approach. The findings and
conclusions in this article are those of the authors and do not
necessarily represent the views of the U.S. Fish and Wildlife Service.
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SN 0890-8575
EI 1939-7445
J9 NAT RESOUR MODEL
JI Nat. Resour. Model.
PD FEB
PY 2011
VL 24
IS 1
BP 117
EP 156
DI 10.1111/j.1939-7445.2010.00085.x
PG 40
WC Environmental Sciences; Mathematics, Interdisciplinary Applications
SC Environmental Sciences & Ecology; Mathematics
GA 714WJ
UT WOS:000286839400005
ER
PT J
AU Iverson, RM
Reid, ME
Logan, M
LaHusen, RG
Godt, JW
Griswold, JP
AF Iverson, Richard M.
Reid, Mark E.
Logan, Matthew
LaHusen, Richard G.
Godt, Jonathan W.
Griswold, Julia P.
TI Positive feedback and momentum growth during debris-flow entrainment of
wet bed sediment
SO NATURE GEOSCIENCE
LA English
DT Article
ID MASS; MOBILIZATION; LANDSLIDES; AVALANCHES; FRICTION; EROSION; RUNOUT;
RANGE; MODEL
AB Debris flows typically occur when intense rainfall or snowmelt triggers landslides or extensive erosion on steep, debris-mantled slopes. The flows can then grow dramatically in size and speed as they entrain material from their beds and banks, but the mechanism of this growth is unclear. Indeed, momentum conservation implies that entrainment of static material should retard the motion of the flows if friction remains unchanged. Here we use data from large-scale experiments to assess the entrainment of bed material by debris flows. We find that entrainment is accompanied by increased flow momentum and speed only if large positive pore pressures develop in wet bed sediments as the sediments are overridden by debris flows. The increased pore pressure facilitates progressive scour of the bed, reduces basal friction and instigates positive feedback that causes flow speed, mass and momentum to increase. If dryer bed sediment is entrained, however, the feedback becomes negative and flow momentum declines. We infer that analogous feedbacks could operate in other types of gravity-driven mass flow that interact with erodible beds.
C1 [Iverson, Richard M.; Logan, Matthew; LaHusen, Richard G.; Griswold, Julia P.] US Geol Survey, Vancouver, WA 98683 USA.
[Reid, Mark E.] US Geol Survey, Menlo Pk, CA 94025 USA.
[Godt, Jonathan W.] US Geol Survey, Denver, CO 80225 USA.
RP Iverson, RM (reprint author), US Geol Survey, Vancouver, WA 98683 USA.
EM riverson@usgs.gov
NR 45
TC 95
Z9 97
U1 5
U2 37
PU NATURE PUBLISHING GROUP
PI NEW YORK
PA 75 VARICK ST, 9TH FLR, NEW YORK, NY 10013-1917 USA
SN 1752-0894
EI 1752-0908
J9 NAT GEOSCI
JI Nat. Geosci.
PD FEB
PY 2011
VL 4
IS 2
BP 116
EP 121
DI 10.1038/NGEO1040
PG 6
WC Geosciences, Multidisciplinary
SC Geology
GA 713GN
UT WOS:000286723300018
ER
PT J
AU Cole, JJ
Carpenter, SR
Kitchell, J
Pace, ML
Solomon, CT
Weidel, B
AF Cole, Jonathan J.
Carpenter, Stephen R.
Kitchell, Jim
Pace, Michael L.
Solomon, Christopher T.
Weidel, Brian
TI Strong evidence for terrestrial support of zooplankton in small lakes
based on stable isotopes of carbon, nitrogen, and hydrogen
SO PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF
AMERICA
LA English
DT Article
DE allochthony; terrestrial subsidy
ID DISSOLVED ORGANIC-CARBON; AQUATIC FOOD WEBS; ALLOCHTHONOUS CARBON; C-13
ADDITION; BENTHIC INVERTEBRATES; TROPHIC POSITION; NORTHERN SWEDEN;
STREAM; RESOURCES; MATTER
AB Cross-ecosystem subsidies to food webs can alter metabolic balances in the receiving (subsidized) system and free the food web, or particular consumers, from the energetic constraints of local primary production. Although cross-ecosystem subsidies between terrestrial and aquatic systems have been well recognized for benthic organisms in streams, rivers, and the littoral zones of lakes, terrestrial subsidies to pelagic consumers are more difficult to demonstrate and remain controversial. Here, we adopt a unique approach by using stable isotopes of H, C, and N to estimate terrestrial support to zooplankton in two contrasting lakes. Zooplankton (Holopedium, Daphnia, and Leptodiaptomus) are comprised of approximate to 20-40% of organic material of terrestrial origin. These estimates are as high as, or higher than, prior measures obtained by experimentally manipulating the inorganic C-13 content of these lakes to augment the small, natural contrast in C-13 between terrestrial and algal photosynthesis. Our study gives credence to a growing literature, which we review here, suggesting that significant terrestrial support of pelagic crustaceans (zooplankton) is widespread.
C1 [Cole, Jonathan J.] Cary Inst Ecosyst Studies, Millbrook, NY 12545 USA.
[Carpenter, Stephen R.; Kitchell, Jim] Univ Wisconsin, Ctr Limnol, Madison, WI 53706 USA.
[Pace, Michael L.] Univ Virginia, Dept Environm Sci, Charlottesville, VA 22904 USA.
[Solomon, Christopher T.] McGill Univ, Dept Nat Resource Sci, Ste Anne De Bellevue, PQ H9X 3V9, Canada.
[Weidel, Brian] US Geol Survey, Lake Ontario Biol Stn, Oswego, NY 13126 USA.
RP Cole, JJ (reprint author), Cary Inst Ecosyst Studies, Millbrook, NY 12545 USA.
EM colej@caryinstitute.org
RI Solomon, Chris/E-6284-2014;
OI Solomon, Chris/0000-0002-2850-4257; Pace, Michael/0000-0001-5945-6131
FU National Science Foundation
FX We thank Jim Coloso and Laura Smith who collected much of the data shown
here and Jim Hodgson, Jon Frum for inspiration in writing this paper.
The work took place at the University of Notre Dame Environmental
Research Center, and we are grateful for the assistance from Dr. Gary
Belovsky and his staff. We thank the National Science Foundation for
funding.
NR 66
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U1 12
U2 168
PU NATL ACAD SCIENCES
PI WASHINGTON
PA 2101 CONSTITUTION AVE NW, WASHINGTON, DC 20418 USA
SN 0027-8424
J9 P NATL ACAD SCI USA
JI Proc. Natl. Acad. Sci. U. S. A.
PD FEB 1
PY 2011
VL 108
IS 5
BP 1975
EP 1980
DI 10.1073/pnas.1012807108
PG 6
WC Multidisciplinary Sciences
SC Science & Technology - Other Topics
GA 714JA
UT WOS:000286804700044
PM 21245299
ER
PT J
AU Wieser, ME
Coplen, TB
AF Wieser, Michael E.
Coplen, Tyler B.
TI Atomic weights of the elements 2009 (IUPAC Technical Report)
SO PURE AND APPLIED CHEMISTRY
LA English
DT Article; Proceedings Paper
CT 2nd Regional Symposium on Electrochemistry
CY JUN 06-10, 2010
CL Belgrade, SERBIA
DE atomic-weight interval; atomic-weight range; conventional atomic-weight
values; boron; carbon; chlorine; germanium; half-lives; hydrogen; IUPAC
Inorganic Chemistry Division; lithium; nitrogen; oxygen; silicon;
sulfur; thallium
ID ABSOLUTE ISOTOPIC COMPOSITION; REFERENCE SAMPLE; ABUNDANCE RATIOS;
SINGLE CRYSTALS; SILICON; SEDIMENTS; NITROGEN; GEOCHEMISTRY; GERMANIUM;
THALLIUM
AB The biennial review of atomic-weight determinations and other cognate data has resulted in changes for the standard atomic weights of 11 elements. Many atomic weights are not constants of nature, but depend upon the physical, chemical, and nuclear history of the material. The standard atomic weights of 10 elements having two or more stable isotopes have been changed to reflect this variability of atomic-weight values in natural terrestrial materials. To emphasize the fact that these standard atomic weights are not constants of nature, each atomic-weight value is expressed as an interval. The interval is used together with the symbol [a; b] to denote the set of atomic-weight values, A(r)(E), of element E in normal materials for which a <= A(r)(E) <= b. The symbols a and b denote the bounds of the interval [a; b]. The revised atomic weight of hydrogen, Ar(H), is [1.00784; 1.008 11] from 1.00794(7); lithium, A(r)(Li), is [6.938; 6.997] from 6.941(2); boron, A(r)(B), is [10.806; 10.821] from 10.811(7); carbon, A(r)(C), is [12.0096; 12.0116] from 12.0107(8); nitrogen, A(r)(N), is [14.00643; 14.00728] from 14.0067(2); oxygen, A(r)(O), is [15.99903; 15.99977] from 15.9994(3); silicon, A(r)(Si), is [28.084; 28.086] from 28.0855(3); sulfur, A(r)(S), is [32.059; 32.076] from 32.065(2); chlorine, A(r)(Cl), is [35.446; 35.457] from 35.453(2); and thallium. A(r)(Tl), is [204.382; 204.385] from 204.3833(2). This fundamental change in the presentation of the atomic weights represents an important advance in our knowledge of the natural world and underscores the significance and contributions of chemistry to the well-being of humankind in the International Year of Chemistry 2011. The standard atomic weight of germanium, A(r)(Ge), was also changed to 72.63(1) from 72.64(1).
C1 [Wieser, Michael E.] Univ Calgary, Dept Phys & Astron, Calgary, AB T2N 1N4, Canada.
[Coplen, Tyler B.] US Geol Survey, Reston, VA 22092 USA.
RP Wieser, ME (reprint author), Univ Calgary, Dept Phys & Astron, Calgary, AB T2N 1N4, Canada.
EM mwieser@ucalgary.ca
FU U.S. Geological Survey National Research Program
FX The support of the U.S. Geological Survey National Research Program made
this report possible.
NR 69
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Z9 152
U1 5
U2 39
PU WALTER DE GRUYTER GMBH
PI BERLIN
PA GENTHINER STRASSE 13, D-10785 BERLIN, GERMANY
SN 0033-4545
EI 1365-3075
J9 PURE APPL CHEM
JI Pure Appl. Chem.
PD FEB
PY 2011
VL 83
IS 2
BP 359
EP 396
DI 10.1351/PAC-REP-10-09-14
PG 38
WC Chemistry, Multidisciplinary
SC Chemistry
GA 720FD
UT WOS:000287265000010
ER
PT J
AU Tsukamoto, S
Duller, GAT
Wintle, AG
Muhs, D
AF Tsukamoto, S.
Duller, G. A. T.
Wintle, A. G.
Muhs, D.
TI Assessing the potential for luminescence dating of basalts
SO QUATERNARY GEOCHRONOLOGY
LA English
DT Article
DE Luminescence dating; IRSL; Cima volcanic field; Mars analogue; Basalt;
Plagioclase
ID OPTICALLY STIMULATED LUMINESCENCE; MARTIAN ANALOG MATERIALS; LANDSCAPE
EVOLUTION; MOJAVE DESERT; DOSE-RATE; FELDSPARS; SEDIMENTS; SIGNALS;
CALIFORNIA; SAMPLES
AB The possibility of dating basalt using luminescence was tested on four samples with independent age control from Cima volcanic field, California, with the ultimate aim of assessing whether the technique could be used to date sediments on the surface of Mars. Previous analysis of these samples had demonstrated that the infrared stimulated luminescence (IRSL) signal is most suitable for dating as it showed the lowest fading rate among various luminescence signals. In this study, changes in equivalent dose as a function of preheat are described. The ages for the two youngest Cima samples agree with the independent ages based on cosmogenic nuclide measurements (12.0 +/- 0.8 ka). In the two older samples (dated to 320 and 580 ka by K-Ar), the luminescence behaviour is more complex and the form of the IRSL decay curve is seen to vary with dose. Mathematical fitting is used to isolate two components and their intensities are used to produce dose response curves. The slower component yields a larger equivalent dose. However, even using this component and after correction for fading, the ages obtained for the older samples are younger than the K-Ar ages. (c) 2010 Elsevier B.V. All rights reserved.
C1 [Tsukamoto, S.] Leibniz Inst Appl Geophys, D-30655 Hannover, Germany.
[Tsukamoto, S.; Duller, G. A. T.; Wintle, A. G.] Aberystwyth Univ, Inst Geog & Earth Sci, Ceredigion SY23 3DB, Wales.
[Muhs, D.] US Geol Survey, Fed Ctr, Denver, CO 80225 USA.
RP Tsukamoto, S (reprint author), Leibniz Inst Appl Geophys, Stilleweg 2, D-30655 Hannover, Germany.
EM sumiko.tsukamoto@liag-hannover.de
RI Duller, Geoffrey/D-5110-2015
OI Duller, Geoffrey/0000-0002-2694-4590
FU ESA ESTEC [18581/04/04/NL/HB, 21506/08/NL/IA]
FX This work was partially supported by ESA ESTEC contracts
18581/04/04/NL/HB and 21506/08/NL/IA. Detlev Klosa is thanked for the
EPMA analysis. Jeff Pigati and Kathleen Simmons of the USGS are thanked
for their helpful comments, and Sebastien Huot and Regina De Witt are
thanked for their constructive referees' comments which helped to
improve the paper. Any use of trade, product, or firm names is for
descriptive purposes only and does not imply endorsement by the U.S.
Government.
NR 30
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U1 0
U2 5
PU ELSEVIER SCI LTD
PI OXFORD
PA THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, OXON, ENGLAND
SN 1871-1014
J9 QUAT GEOCHRONOL
JI Quat. Geochronol.
PD FEB
PY 2011
VL 6
IS 1
BP 61
EP 70
DI 10.1016/j.quageo.2010.04.002
PG 10
WC Geography, Physical; Geosciences, Multidisciplinary
SC Physical Geography; Geology
GA 696HU
UT WOS:000285433300007
ER
PT J
AU Pinter, N
Fiedel, S
Keeley, JE
AF Pinter, Nicholas
Fiedel, Stuart
Keeley, Jon E.
TI Fire and vegetation shifts in the Americas at the vanguard of
Paleoindian migration
SO QUATERNARY SCIENCE REVIEWS
LA English
DT Article
DE Fire; Fire regime; Vegetation; Vegetation change; Climate; Climate
change; Megafauna; Anthropogenic effects; Anthropocene
ID SOUTHERN SOUTH-AMERICA; LATE QUATERNARY; HUMAN OCCUPATION;
CLIMATE-CHANGE; NORTH-AMERICA; HUMAN IMPACT; NEW-ZEALAND; PLEISTOCENE;
EXTINCTION; AUSTRALIA
AB Across North and South America, the final millennia of the Pleistocene saw dramatic changes in climate, vegetation, fauna, fire regime, and other local and regional paleo-environmental characteristics. Rapid climate shifts following the Last Glacial Maximum (LGM) exerted a first-order influence, but abrupt post-glacial shifts in vegetation composition, vegetation structure, and fire regime also coincided with human arrival and transformative faunal extinctions in the Americas. We propose a model of post-glacial vegetation change in response to climatic drivers, punctuated by local fire regime shifts in response to megaherbivore-driven fuel changes and anthropogenic ignitions. The abrupt appearance of humans, disappearance of megaherbivores, and resulting changes in New World fire systems were transformative events that should not be dismissed in favor of climate-only interpretations of post-glacial paleo-environmental shifts in the Americas. Fire is a mechanism by which small human populations can have broad impacts, and growing evidence suggests that early anthropogenic influences on regional, even global, paleo-environments should be tested alongside other potential causal mechanisms. (C) 2010 Elsevier Ltd. All rights reserved.
C1 [Pinter, Nicholas] So Illinois Univ, Dept Geol, Carbondale, IL 62901 USA.
[Fiedel, Stuart] Louis Berger Grp, Richmond, VA 23219 USA.
[Keeley, Jon E.] US Geol Survey, Western Ecol Res Ctr, Three Rivers, CA 93271 USA.
[Keeley, Jon E.] Univ Calif Los Angeles, Dept Ecol & Evolutionary Biol, Los Angeles, CA 90095 USA.
RP Pinter, N (reprint author), So Illinois Univ, Dept Geol, Carbondale, IL 62901 USA.
EM npinter@geo.siu.edu
NR 53
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U2 38
PU PERGAMON-ELSEVIER SCIENCE LTD
PI OXFORD
PA THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND
SN 0277-3791
J9 QUATERNARY SCI REV
JI Quat. Sci. Rev.
PD FEB
PY 2011
VL 30
IS 3-4
BP 269
EP 272
DI 10.1016/j.quascirev.2010.12.010
PG 4
WC Geography, Physical; Geosciences, Multidisciplinary
SC Physical Geography; Geology
GA 722LP
UT WOS:000287434000001
ER
PT J
AU Westbrook, CJ
Cooper, DJ
Baker, BW
AF Westbrook, C. J.
Cooper, D. J.
Baker, B. W.
TI BEAVER ASSISTED RIVER VALLEY FORMATION
SO RIVER RESEARCH AND APPLICATIONS
LA English
DT Article
DE beaver meadow; Castor canadensis; ecosystem engineering; floodplain;
habitat heterogeneity; river valley formation; Rocky Mountain National
Park; terrace
ID NATIONAL-PARK; NUTRIENT AVAILABILITY; SPATIAL VARIABILITY;
CASTOR-CANADENSIS; FLOODPLAIN; DYNAMICS; WILLOW; ECOSYSTEM; NITROGEN;
FOREST
AB We examined how beaver dams affect key ecosystem processes, including pattern and process of sediment deposition, the composition and spatial pattern of vegetation, and nutrient loading and processing. We provide new evidence for the formation of heterogeneous beaver meadows on riverine system floodplains and terraces where dynamic flows are capable of breaching in-channel beaver dams. Our data show a 1.7-m high beaver dam triggered overbank flooding that drowned vegetation in areas deeply flooded, deposited nutrient-rich sediment in a spatially heterogeneous pattern on the floodplain and terrace, and scoured soils in other areas. The site quickly de-watered following the dam breach by high stream flows, protecting the deposited sediment from future re-mobilization by overbank floods. Bare sediment either exposed by scouring or deposited by the beaver flood was quickly colonized by a spatially heterogeneous plant community, forming a beaver meadow. Many willow and some aspen seedlings established in the more heavily disturbed areas, suggesting the site may succeed to a willow carr plant community suitable for future beaver re-occupation. We expand existing theory beyond the beaver pond to include terraces within valleys. This more fully explains how beavers can help drive the formation of alluvial valleys and their complex vegetation patterns as was first postulated by Ruedemann and Schoonmaker in 1938. Copyright (C) 2010 John Wiley & Sons, Ltd.
C1 [Westbrook, C. J.] Univ Saskatchewan, Dept Geog & Planning, Ctr Hydrol, Saskatoon, SK S7N 5C8, Canada.
[Cooper, D. J.] Colorado State Univ, Grad Degree Program Ecol, Ft Collins, CO 80523 USA.
[Baker, B. W.] US Geol Survey, Ft Collins Sci Ctr, Ft Collins, CO USA.
RP Westbrook, CJ (reprint author), Univ Saskatchewan, Dept Geog & Planning, Ctr Hydrol, 117 Sci Pl, Saskatoon, SK S7N 5C8, Canada.
EM cherie.westbrook@usask.ca
FU U.S. Geological Survey; Rocky Mountain National Park
FX This work was supported by grants from U.S. Geological Survey and Rocky
Mountain National Park. The authors thank David Fetter, Jen Greco and
Angie Welch for help with field collections and laboratory analyses.
Jordan Clayton graciously provided the sediment corer. They thank Kevin
Devito, Jill Johnstone and two anonymous reviewers for their comments on
an earlier draft of this paper. Any use of trade, product or firm names
is for descriptive processes only and does not imply endorsement by the
U.S. Government.
NR 59
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U2 57
PU WILEY-BLACKWELL
PI HOBOKEN
PA 111 RIVER ST, HOBOKEN 07030-5774, NJ USA
SN 1535-1459
EI 1535-1467
J9 RIVER RES APPL
JI River Res. Appl.
PD FEB
PY 2011
VL 27
IS 2
DI 10.1002/rra.1359
PG 10
WC Environmental Sciences; Water Resources
SC Environmental Sciences & Ecology; Water Resources
GA 724TT
UT WOS:000287599800010
ER
PT J
AU Nevers, MB
Whitman, RL
AF Nevers, Meredith B.
Whitman, Richard L.
TI Efficacy of monitoring and empirical predictive modeling at improving
public health protection at Chicago beaches
SO WATER RESEARCH
LA English
DT Article
DE E. coli; Fecal indicator bacteria; Recreational water quality; Lake
Michigan; Swimming; Risk
ID SOUTHERN LAKE-MICHIGAN; ESCHERICHIA-COLI CONCENTRATIONS; FECAL INDICATOR
BACTERIA; WATER-QUALITY; RECREATIONAL BEACHES; CALIFORNIA BEACHES;
HUNTINGTON-BEACH; NEARSHORE WATER; COASTAL WATERS; ENTEROCOCCI
AB Efforts to improve public health protection in recreational swimming waters have focused on obtaining real-time estimates of water quality. Current monitoring techniques rely on the time-intensive culturing of fecal indicator bacteria (FIB) from water samples, but rapidly changing FIB concentrations result in management errors that lead to the public being exposed to high FIB concentrations (type II error) or beaches being closed despite acceptable water quality (type I error). Empirical predictive models may provide a rapid solution, but their effectiveness at improving health protection has not been adequately assessed. We sought to determine if emerging monitoring approaches could effectively reduce risk of illness exposure by minimizing management errors. We examined four monitoring approaches (inactive, current protocol, a single predictive model for all beaches, and individual models for each beach) with increasing refinement at 14 Chicago beaches using historical monitoring and hydrometeorological data and compared management outcomes using different standards for decision-making. Predictability (R(2)) of FIB concentration improved with model refinement at all beaches but one. Predictive models did not always reduce the number of management errors and therefore the overall illness burden. Use of a Chicago-specific single-sample standard-rather than the default 235 E. cob CFU/100 ml widely used-together with predictive modeling resulted in the greatest number of open beach days without any increase in public health risk. These results emphasize that emerging monitoring approaches such as empirical models are not equally applicable at all beaches, and combining monitoring approaches may expand beach access. Published by Elsevier Ltd.
C1 [Nevers, Meredith B.; Whitman, Richard L.] US Geol Survey, Great Lakes Sci Ctr, Lake Michigan Ecol Res Stn, Porter, IN 46304 USA.
RP Nevers, MB (reprint author), US Geol Survey, Great Lakes Sci Ctr, Lake Michigan Ecol Res Stn, 1100 N Mineral Springs Rd, Porter, IN 46304 USA.
EM mnevers@usgs.gov
RI Guan, Xiaokang/A-6675-2012;
OI Nevers, Meredith/0000-0001-6963-6734
FU US Ocean Action Plan: USGS Ocean Research Priorities Plan; Great Lakes
Restoration Initiative
FX We thank Murulee Byappanahalli (USGS) for his careful review. Research
was funded in part by the US Ocean Action Plan: USGS Ocean Research
Priorities Plan and by the Great Lakes Restoration Initiative. Any use
of trade, product, or firm names is for descriptive purposes only and
does not imply endorsement by the U.S. Government. This article is
Contribution 1627 of the USGS Great Lakes Science Center.
NR 40
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U2 20
PU PERGAMON-ELSEVIER SCIENCE LTD
PI OXFORD
PA THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND
SN 0043-1354
J9 WATER RES
JI Water Res.
PD FEB
PY 2011
VL 45
IS 4
BP 1659
EP 1668
DI 10.1016/j.watres.2010.12.010
PG 10
WC Engineering, Environmental; Environmental Sciences; Water Resources
SC Engineering; Environmental Sciences & Ecology; Water Resources
GA 716SY
UT WOS:000286995000015
PM 21195447
ER
PT J
AU Flores, C
Bounds, DL
Ruby, DE
AF Flores, Conception
Bounds, Dixie L.
Ruby, Douglas E.
TI Does Prescribed Fire Benefit Wetland Vegetation?
SO WETLANDS
LA English
DT Article
DE Biomass; Distichlis spicata; Marsh; Schoenoplectus americanus; Spartina
alterniflora; Spartina patens; Stem density
ID PLANT COMMUNITY; BIOMASS; MARSH; MANAGEMENT; HERBIVORY; TEXAS
AB The effects of fire on wetland vegetation in the mid-Atlantic region of the United States are poorly known, despite the historical use of fire by federal, state, and private landowners in the Chesapeake Bay Region. Prescribed fire is widely used by land managers to promote vegetation that is beneficial to migratory waterfowl, muskrats, and other native wildlife and to reduce competition from less desirable plant species. We compared vegetative response to two fire rotations, annual burns and 3-year burns, and two control sites, Control 1 and Control 2. We tested the effects of fire within six tidal marsh wetlands at Blackwater National Wildlife Refuge and Fishing Bay Wildlife Management Area in Maryland. We examined changes in total live biomass (all species), total stem density, litter, and changes in live biomass and stem density of four dominant wetland plant species (11 variables). Our results suggest that annual prescribed fires will decrease the accumulation of litter, increase the biomass and stem densities of some wetland plants generally considered less desirable for wildlife, and have little or no effect on other wetland plants previously thought to benefit from fire.
C1 [Flores, Conception; Bounds, Dixie L.] Univ Maryland Eastern Shore, US Geol Survey, Biol Resources Div, Maryland Cooperat Fish & Wildlife Res Unit, Princess Anne, MD 21853 USA.
[Ruby, Douglas E.] Univ Maryland Eastern Shore, Dept Nat Sci, Princess Anne, MD 21853 USA.
RP Flores, C (reprint author), USN, Facil Engn Command SW, 1220 Pacific Highway, San Diego, CA 92132 USA.
EM conception.flores@navy.mil; dixie_birch@fws.gov; deruby@umes.edu
FU U. S. Fish and Wildlife Service
FX We thank the U. S. Fish and Wildlife Service for funding the project. We
are grateful to Bjorn Burgeson, Katherine Thorington, Fred Adams, and
Alice Brown for assistance in biomass collection. Thanks to the
Blackwater NWR staff, especially, Glenn Carowan, Bill Giese, Keith
Morris, Roger Stone, and the Blackwater Fire Crew. Statistical
assistance and support was provided by Jeff S. Hatfield, USGS Patuxent
Wildlife Research Center; Dr. Mary Christman, University of Maryland
College Park; Dr. Patricia Jones, University of Arizona; Dr. David
Turner, USFS Rocky Mountain Research Station; and Dawn Lawson and Toni
Mizerek, Naval Facilities Engineering Command Southwest. The findings
and conclusions in this article are those of the author(s) and do not
necessarily represent the views of the U.S. Fish and Wildlife Service.
NR 46
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PU SPRINGER
PI DORDRECHT
PA VAN GODEWIJCKSTRAAT 30, 3311 GZ DORDRECHT, NETHERLANDS
SN 0277-5212
EI 1943-6246
J9 WETLANDS
JI Wetlands
PD FEB
PY 2011
VL 31
IS 1
BP 35
EP 44
DI 10.1007/s13157-010-0131-x
PG 10
WC Ecology; Environmental Sciences
SC Environmental Sciences & Ecology
GA 741ZO
UT WOS:000288907700004
ER
PT J
AU Liu, SG
Tan, ZX
Li, ZP
Zhao, SQ
Yuan, WP
AF Liu, Shuguang
Tan, Zhengxi
Li, Zhengpeng
Zhao, Shuqing
Yuan, Wenping
TI Are soils of Iowa USA currently a carbon sink or source? Simulated
changes in SOC stock from 1972 to 2007
SO AGRICULTURE ECOSYSTEMS & ENVIRONMENT
LA English
DT Article
DE Biogeochemical modeling; Land use change; Soil organic carbon; Tile
drainage; Western Corn Belt
ID CLIMATE-CHANGE; LAND-USE; GLOBAL CLIMATE; ORGANIC-MATTER; TILE DRAINAGE;
UNITED-STATES; CROP YIELDS; SEQUESTRATION; TILLAGE; MANAGEMENT
AB Upscaling the spatial and temporal changes in carbon (C) stocks and fluxes from sites to regions is a critical and challenging step toward improving our understanding of the dynamics of C sources and sinks over large areas. This study simulated soil organic C (SOC) dynamics within 0-100 cm depth of soils across the state of Iowa in the USA from 1972 to 2007 using the General Ensemble biogeochemical Modeling System (GEMS). The model outputs with variation coefficient were analyzed and assembled from simulation unit to the state scale based upon major land use types at annual step. Results from this study indicate that soils (within a depth of 0-100 cm) in Iowa had been a SOC source at a rate of 190 +/- 380 kg C ha(-1) yr(-1). This was likely caused by the installation of a massive drainage system which led to the release of SOC from deep soil layers previously protected under poor drainage conditions. The annual crop rotation was another major force driving SOC variation and resulted in spatial variability of annual budgets in all croplands. Annual rate of change of SOC stocks in all land types depended significantly on the baseline SOC levels; soils with higher SOC levels tended to be C sources, and those with lower levels tended to be C sinks. Management practices (e.g., conservation tillage and residue management practices) slowed down the C emissions from Iowa soils, but could not reverse the general trend of net SOC loss in view of the entire state due mainly to a high level of baseline SOC stocks. (C) 2010 Elsevier B.V. All rights reserved.
C1 [Tan, Zhengxi; Li, Zhengpeng] US Geol Survey, Earth Resources Observat & Sci EROS Ctr, ARTS, Sioux Falls, SD 57198 USA.
[Zhao, Shuqing] Peking Univ, Coll Urban & Environm Sci, Beijing 100871, Peoples R China.
[Yuan, Wenping] Beijing Normal Univ, Coll Global Change & Earth Syst Sci, Beijing 100875, Peoples R China.
RP Tan, ZX (reprint author), US Geol Survey, Earth Resources Observat & Sci EROS Ctr, ARTS, Sioux Falls, SD 57198 USA.
EM ztan@usgs.gov
OI Tan, Zhengxi/0000-0002-4136-0921
FU US Geological Survey; USGS [08HQCN0007]
FX The research was funded by the Geographic Analysis and Monitoring (GAM)
Program and the Global Change Research and Development Program (R&D) of
the US Geological Survey. We would like to express our thanks to Sandra
Poppenga for providing CTI data and Md Shahriar Pervez for sharing
irrigation information with us. We thank Mr. Craig Walters and Dr.
Jinxun Liu for their internal review. We also really appreciate the
valuable comments from two anonymous peer reviewers. Work of Zhengxi Tan
and Zhengpeng Li was performed under USGS contract 08HQCN0007.
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U2 36
PU ELSEVIER SCIENCE BV
PI AMSTERDAM
PA PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS
SN 0167-8809
J9 AGR ECOSYST ENVIRON
JI Agric. Ecosyst. Environ.
PD JAN 30
PY 2011
VL 140
IS 1-2
BP 106
EP 112
DI 10.1016/j.agee.2010.11.017
PG 7
WC Agriculture, Multidisciplinary; Ecology; Environmental Sciences
SC Agriculture; Environmental Sciences & Ecology
GA 728RO
UT WOS:000287892400013
ER
PT J
AU Landwehr, JM
Meier-Augenstein, W
Kemp, HF
AF Landwehr, Jurate M.
Meier-Augenstein, Wolfram
Kemp, Helen F.
TI A counter-intuitive approach to calculating non-exchangeable H-2
isotopic composition of hair: treating the molar exchange fraction f(E)
as a process-related rather than compound-specific variable
SO RAPID COMMUNICATIONS IN MASS SPECTROMETRY
LA English
DT Article
ID RATIO MASS-SPECTROMETRY; STABLE-HYDROGEN; HUMAN IDENTIFICATION; ORGANIC
MATERIALS; OXYGEN; ORIGINS; NAILS
AB Hair is a keratinous tissue that incorporates hydrogen from material that an animal consumes but it is metabolically inert following synthesis. The stable hydrogen isotope composition of hair has been used in ecological studies to track migrations of mammals as well as for forensic and archaeological purposes to determine the provenance of human remains or the recent geographic life trajectory of living people. Measurement of the total hydrogen isotopic composition of a hair sample yields a composite value comprised of both metabolically informative, non-exchangeable hydrogen and exchangeable hydrogen, with the latter reflecting ambient or sample preparation conditions. Neither of these attributes is directly measurable, and the non-exchangeable hydrogen composition is obtained by estimation using a commonly applied mathematical expression incorporating sample measurements obtained from two distinct equilibration procedures. This commonly used approach treats the fraction of exchangeable hydrogen as a mixing ratio, with a minimal procedural fractionation factor assumed to be close or equal to 1. Instead, we propose to use full molar ratios to derive an expression for the non-exchangeable hydrogen composition explicitly as a function of both the procedural fractionation factor a and the molar hydrogen exchange fraction f(E). We apply these derivations in a longitudinal study of a hair sample and demonstrate that the molar hydrogen exchange fraction f(E) should, like the procedural fractionation factor alpha, be treated as a process-dependent parameter, i.e. a reaction-specific constant. This is a counter-intuitive notion given that maximum theoretical values for the molar hydrogen exchange fraction f(E) can be calculated that are arguably protein-type specific and, as such, f(E) could be regarded as a compound-specific constant. We also make some additional suggestions for future approaches to determine the non-exchangeable hydrogen composition of hair and the use of standards. Copyright (C) 2010 John Wiley & Sons, Ltd.
C1 [Landwehr, Jurate M.] US Geol Survey, Natl Ctr MS431, Reston, VA 20192 USA.
[Meier-Augenstein, Wolfram] Univ Dundee, Ctr Anat & Human Identificat, Dundee DD1 5EH, Scotland.
[Meier-Augenstein, Wolfram; Kemp, Helen F.] Scottish Crop Res Inst, Dundee DD2 5DA, Scotland.
RP Landwehr, JM (reprint author), US Geol Survey, Natl Ctr MS431, Reston, VA 20192 USA.
EM jmlandwe@usgs.gov
RI Meier-Augenstein, Wolfram/F-1895-2011
OI Meier-Augenstein, Wolfram/0000-0002-9498-5837
FU USGS; Scottish Government Rural and Environment Research and Analysis
Directorate (RERAD)
FX J. M. Landwehr gratefully acknowledges the support of the USGS National
Research Program. SCRI gratefully acknowledges financial support from
the Scottish Government Rural and Environment Research and Analysis
Directorate (RERAD). Any use of trade, product, or firm names is for
descriptive purposes only and does not imply endorsement by the U.S.
Government.
NR 15
TC 10
Z9 10
U1 1
U2 8
PU WILEY-BLACKWELL
PI MALDEN
PA COMMERCE PLACE, 350 MAIN ST, MALDEN 02148, MA USA
SN 0951-4198
J9 RAPID COMMUN MASS SP
JI Rapid Commun. Mass Spectrom.
PD JAN 30
PY 2011
VL 25
IS 2
BP 301
EP 306
DI 10.1002/rcm.4854
PG 6
WC Biochemical Research Methods; Chemistry, Analytical; Spectroscopy
SC Biochemistry & Molecular Biology; Chemistry; Spectroscopy
GA 701UL
UT WOS:000285848800006
PM 21192025
ER
PT J
AU Scholl, M
Eugster, W
Burkard, R
AF Scholl, Martha
Eugster, Werner
Burkard, Reto
TI Understanding the role of fog in forest hydrology: stable isotopes as
tools for determining input and partitioning of cloud water in montane
forests
SO HYDROLOGICAL PROCESSES
LA English
DT Article
DE stable isotopes; cloud water; fog; oxygen-18; deuterium; cloud forest
ID POINT-REYES PENINSULA; SOIL-WATER; RAIN-FOREST; REDWOOD FOREST; AMAZON
BASIN; DRY SOILS; PRECIPITATION; O-18; GROUNDWATER; CALIFORNIA
AB Understanding the hydrology of tropical montane cloud forests (TMCF) has become essential as deforestation of mountain areas proceeds at an increased rate worldwide. Passive and active cloud-water collectors, throughfall and stemflow collectors, visibility or droplet size measurements, and micrometeorological sensors are typically used to measure the fog water inputs to ecosystems. In addition, stable isotopes may be used as a natural tracer for fog and rain. Previous studies have shown that the isotopic signature of fog tends to be more enriched in the heavier isotopes (2)H and (18)O than that of rain, due to differences in condensation temperature and history. Differences between fog and rain isotopes are largest when rain is from synoptic-scale storms, and fog or orographic cloud water is generated locally. Smaller isotopic differences have been observed between rain and fog on mountains with orographic clouds, but only a few studies have been conducted. Quantifying fog deposition using isotope methods is more difficult in forests receiving mixed precipitation, because of limitations in the ability of sampling equipment to separate fog from rain, and because fog and rain may, under some conditions, have similar isotopic composition. This article describes the various types of fog most relevant to montane cloud forests and the importance of fog water deposition in the hydrologic budget. A brief overview of isotope hydrology provides the background needed to understand isotope applications in cloud forests. A summary of previous work explains isotopic differences between rain and fog in different environments, and how monitoring the isotopic signature of surface water, soil water and tree xylem water can yield estimates of the contribution of fog water to streamflow, groundwater recharge and transpiration. Next, instrumentation to measure fog and rain, and methods to determine isotopic concentrations in plant and soil water are discussed. The article concludes with the identification of some of the more pressing research questions in this field and offers various suggestions for future research. Published in 2010 by John Wiley & Sons, Ltd.
C1 [Scholl, Martha] US Geol Survey, Reston, VA USA.
[Eugster, Werner] Swiss Fed Inst Technol, Inst Plant Anim & Agroecosyst Sci, Zurich, Switzerland.
[Burkard, Reto] Univ Bern, Inst Geog, Bern, Switzerland.
RP Scholl, M (reprint author), US Geol Survey, Reston, VA USA.
EM mascholl@usgs.gov
RI Eugster, Werner/E-5116-2010;
OI Eugster, Werner/0000-0001-6067-0741; Scholl, Martha/0000-0001-6994-4614
NR 93
TC 24
Z9 25
U1 5
U2 67
PU WILEY-BLACKWELL
PI MALDEN
PA COMMERCE PLACE, 350 MAIN ST, MALDEN 02148, MA USA
SN 0885-6087
J9 HYDROL PROCESS
JI Hydrol. Process.
PD JAN 30
PY 2011
VL 25
IS 3
SI SI
BP 353
EP 366
DI 10.1002/hyp.7762
PG 14
WC Water Resources
SC Water Resources
GA 721TC
UT WOS:000287377100004
ER
PT J
AU Giambelluca, TW
Delay, JK
Nullet, MA
Scholl, MA
Gingerich, SB
AF Giambelluca, Thomas W.
DeLay, John K.
Nullet, Michael A.
Scholl, Martha A.
Gingerich, Stephen B.
TI Canopy water balance of windward and leeward Hawaiian cloud forests on
Haleakala, Maui, Hawai'i
SO HYDROLOGICAL PROCESSES
LA English
DT Article
DE tropical montane cloud forest; cloud water interception; fog
ID STANDARD FOG COLLECTOR; HIGH-ELEVATION REGIONS; DEPOSITION
AB The contribution of intercepted cloud water to precipitation at windward and leeward cloud forest sites on the slopes of Haleakala, Maui was assessed using two approaches. Canopy water balance estimates based on meteorological monitoring were compared with interpretations of fog screen measurements collected over a 2-year period at each location. The annual incident rainfall was 973 mm at the leeward site (Auwahi) and 2550 mm at the windward site (Waikamoi). At the leeward, dry forest site, throughfall was less than rainfall (87%), and, at the windward, wet forest site, throughfall exceeded rainfall (122%). Cloud water interception estimated from canopy water balance was 166 mm year(-1) at Auwahi and 1212 mm year(-1) at Waikamoi. Annual fog screen measurements of cloud water flux, corrected for wind-blown rainfall, were 132 and 3017 mm for the dry and wet sites respectively. Event totals of cloud water flux based on fog screen measurements were poorly correlated with event cloud water interception totals derived from the canopy water balance. Hence, the use of fixed planar fog screens to estimate cloud water interception is not recommended. At the wet windward site, cloud water interception made up 32% of the total precipitation, adding to the already substantial amount of rainfall. At the leeward dry site, cloud water interception was 15% of the total precipitation. Vegetation at the dry site, where trees are more exposed and isolated, was more efficient at intercepting the available cloud water than at the rainy site, but events were less frequent, shorter in duration and lower in intensity. A large proportion of intercepted cloud water, 74% and 83%, respectively for the two sites, was estimated to become throughfall, thus adding significantly to soil water at both sites. Published in 2010 by John Wiley & Sons, Ltd.
C1 [Giambelluca, Thomas W.; DeLay, John K.; Nullet, Michael A.] Univ Hawaii Manoa, Honolulu, HI 96822 USA.
[Scholl, Martha A.] US Geol Survey, Reston, VA 22092 USA.
[Gingerich, Stephen B.] US Geol Survey, Honolulu, HI USA.
RP Giambelluca, TW (reprint author), Univ Hawaii Manoa, Honolulu, HI 96822 USA.
EM thomas@hawaii.edu
OI Gingerich, Stephen/0000-0002-4381-0746; Scholl,
Martha/0000-0001-6994-4614; Giambelluca, Thomas/0000-0002-6798-3780
FU US Geological Survey, Water Resources Discipline; US National Science
Foundation [EAR-0309731]; US Geological Survey, Biological Resources
Discipline
FX The work presented in this paper was supported by the US Geological
Survey, Water Resources Discipline, Venture Capital Fund, the US
National Science Foundation under Grant No. EAR-0309731 and by the US
Geological Survey, Biological Resources Discipline, Global Change
Program. Any use of trade, product or firm names is for descriptive
purposes only and does not imply endorsement by the US Government. The
authors thank Veronica Hutton and Corina Niemand for contributions to
early stages of the data analysis, and the editors of Tropical Montane
Cloud Forests: Science for Conservation and Management, (Cambridge
University Press), especially Sampurno Bruijnzeel, for their many
helpful suggestions on an earlier version of this paper. We also thank
Sumner Erdman and the staff of Ulupalakua Ranch, for their kind
assistance and for the use of their land for the Auwahi measurement
site, and The Nature Conservancy for logistical support and access to
the Waikamoi Preserve.
NR 33
TC 17
Z9 17
U1 2
U2 27
PU WILEY-BLACKWELL
PI MALDEN
PA COMMERCE PLACE, 350 MAIN ST, MALDEN 02148, MA USA
SN 0885-6087
J9 HYDROL PROCESS
JI Hydrol. Process.
PD JAN 30
PY 2011
VL 25
IS 3
SI SI
BP 438
EP 447
DI 10.1002/hyp.7738
PG 10
WC Water Resources
SC Water Resources
GA 721TC
UT WOS:000287377100013
ER
PT J
AU Splinter, KD
Holman, RA
Plant, NG
AF Splinter, Kristen D.
Holman, Robert A.
Plant, Nathaniel G.
TI A behavior-oriented dynamic model for sandbar migration and 2DH
evolution
SO JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS
LA English
DT Article
ID SEDIMENT TRANSPORT; BAR MORPHOLOGY; EMBAYED BEACH; SURF ZONES;
NEARSHORE; QUANTIFICATION; VARIABILITY; CURRENTS
AB A nonlinear model is developed to study the time-dependent relationship between the alongshore variability of a sandbar, a(t), and alongshore-averaged sandbar position, x(c)(t). Sediment transport equations are derived from energetics-based formulations. A link between this continuous physical representation and a parametric form describing the migration of sandbars of constant shape is established through a simple transformation of variables. The model is driven by offshore wave conditions. The parametric equations are dynamically coupled such that changes in one term (i.e., x(c)) drive changes in the other (i.e., a(t)). The model is tested on 566 days of data from Palm Beach, New South Wales, Australia. Using weighted nonlinear least squares to estimate best fit model coefficients, the model explained 49% and 41% of the variance in measured x(c) and a(t), respectively. Comparisons against a 1-D horizontal (1DH) version of the model showed significant improvements when the 2DH terms were included (1DH and 2DH Brier skill scores were -0.12 and 0.42, respectively). Onshore bar migration was not predicted in the 1DH model, while the 2DH model correctly predicted onshore migration in the presence of 2DH morphology and allowed the bar to remain closer to shore for a given amount of breaking, providing an important hysteresis to the system. The model is consistent with observations that active bar migration occurs under breaking waves with onshore migration occurring at timescales of days to weeks and increasing 2DH morphology, while offshore migration occurs rapidly under high waves and coincides with a reduction in 2DH morphology.
C1 [Splinter, Kristen D.; Holman, Robert A.] Oregon State Univ, Coll Ocean & Atmospher Sci, Corvallis, OR 97331 USA.
[Plant, Nathaniel G.] US Geol Survey, Florida Integrated Sci Ctr, St Petersburg, FL 33701 USA.
RP Splinter, KD (reprint author), Griffith Univ, Griffith Ctr Coastal Management, Gold Coast Campus, Southport, Qld 4222, Australia.
EM k.splinter@griffith.edu.au; holman@coas.oregonstate.edu; nplant@usgs.gov
OI Plant, Nathaniel/0000-0002-5703-5672; Splinter,
Kristen/0000-0002-0082-8444
FU ONR SECNAV/CNO Chair of Oceanography [N00014-03-1-0973]; Coastal
Geosciences Program [N00014-07-1-0490]
FX This research was made possible with the help and data provided by many
people. T. Lippmann provided cross-shore wave heights, profiles, and
wave breaking data from Duck94. Daily RMS wave heights and angles for
Palm Beach were provided by G. Symonds. The authors also extend their
appreciation to J. Stanley for always knowing where the data are and for
his unending patience and technical savvy for all things Argus database
related; H. T. Ozkan-Haller, J. Long, M. Palmsten, and G. Wilson for
their insight into the problem; and A. Bowen, an eternal mentor. The
authors also extend their sincere appreciation to the reviewers of this
manuscript whose extensive comments greatly improved the quality of this
paper. This research was generously funded by ONR SECNAV/CNO Chair of
Oceanography (N00014-03-1-0973) and the Coastal Geosciences Program
(N00014-07-1-0490).
NR 53
TC 16
Z9 16
U1 1
U2 8
PU AMER GEOPHYSICAL UNION
PI WASHINGTON
PA 2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA
SN 2169-9275
EI 2169-9291
J9 J GEOPHYS RES-OCEANS
JI J. Geophys. Res.-Oceans
PD JAN 29
PY 2011
VL 116
AR C01020
DI 10.1029/2010JC006382
PG 21
WC Oceanography
SC Oceanography
GA 713UU
UT WOS:000286763700002
ER
PT J
AU Rice, MS
Bell, JF
Cloutis, EA
Wray, JJ
Herkenhoff, KE
Sullivan, R
Johnson, JR
Anderson, RB
AF Rice, M. S.
Bell, J. F., III
Cloutis, E. A.
Wray, J. J.
Herkenhoff, K. E.
Sullivan, R.
Johnson, J. R.
Anderson, R. B.
TI Temporal observations of bright soil exposures at Gusev crater, Mars
SO JOURNAL OF GEOPHYSICAL RESEARCH-PLANETS
LA English
DT Article
ID SCIENCE EXPERIMENT HIRISE
AB The Mars Exploration Rover Spirit has discovered bright soil deposits in its wheel tracks that previously have been confirmed to contain ferric sulfates and/or opaline silica. Repeated Pancam multispectral observations have been acquired at four of these deposits to monitor spectral and textural changes over time during exposure to Martian surface conditions. Previous studies suggested that temporal spectral changes occur because of mineralogic changes (e. g., phase transitions accompanying dehydration). In this study, we present a multispectral and temporal analysis of eight Pancam image sequences at the Tyrone exposure, three at the Gertrude Weise exposure, two at the Kit Carson exposure, and ten at the Ulysses exposure that have been acquired as of sol 2132 (1 January 2010). We compare observed variations in Pancam data to spectral changes predicted by laboratory experiments for the dehydration of ferric sulfates. We also present a spectral analysis of repeated Mars Reconnaissance Orbiter HiRISE observations spanning 32 sols and a textural analysis of Spirit Microscopic Imager observations of Ulysses spanning 102 sols. At all bright soil exposures, we observe no statistically significant spectral changes with time that are uniquely diagnostic of dehydration and/or mineralogic phase changes. However, at Kit Carson and Ulysses, we observe significant textural changes, including slumping within the wheel trench, movement of individual grains, disappearance of fines, and dispersal of soil clods. All observed textural changes are consistent with aeolian sorting and/or minor amounts of air fall dust deposition.
C1 [Rice, M. S.; Bell, J. F., III; Wray, J. J.; Sullivan, R.; Anderson, R. B.] Cornell Univ, Dept Astron, Ithaca, NY 14853 USA.
[Cloutis, E. A.] Univ Winnipeg, Dept Geog, Winnipeg, MB R3B 2E9, Canada.
[Herkenhoff, K. E.; Johnson, J. R.] US Geol Survey, Astrogeol Sci Ctr, Flagstaff, AZ 86001 USA.
RP Rice, MS (reprint author), Cornell Univ, Dept Astron, Ithaca, NY 14853 USA.
EM mrice@astro.cornell.edu
RI Wray, James/B-8457-2008; Johnson, Jeffrey/F-3972-2015
OI Wray, James/0000-0001-5559-2179;
FU NASA; Mars Data Analysis Program (Cornell); National Science Foundation;
CSA; NSERC; CFI; MRIF; University of Winnipeg; NSF; Fannie and John
Hertz Foundation
FX We gratefully acknowledge our colleagues on the Mars Exploration Rover
and MRO HiRISE teams at the Jet Propulsion Laboratory, Cornell
University, USGS/Flagstaff, University of Arizona, and other partner
institutions for enabling us to study the surface of Mars from
microscopic to orbital scales. We thank Jonathan Joseph for his help in
the calibration of Pancam images, Stan Mertzman for the compositional
analysis of the ferric sulfate samples, Richard Morris for insightful
suggestions that strengthened this work, Anya Portyankina and M.
Vincendon for providing dust-corrected HiRISE images, and Alicia Vaughan
and Jennifer Herman for their help with the presentation of Spirit's
array energy. Leah Roach and an anonymous reviewer provided thoughtful
comments that improved the quality of this work. This work is supported
by grants and contracts from the NASA Mars Exploration Program (JPL) and
the Mars Data Analysis Program (Cornell). M. S. R. was supported by a
National Science Foundation Graduate Research Fellowship. E. A. C. and
his lab facility are supported by grants from CSA, NSERC, CFI, MRIF, and
the University of Winnipeg. J.J.W. thanks the NSF and the Fannie and
John Hertz Foundation for support.
NR 45
TC 11
Z9 11
U1 0
U2 4
PU AMER GEOPHYSICAL UNION
PI WASHINGTON
PA 2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA
SN 2169-9097
EI 2169-9100
J9 J GEOPHYS RES-PLANET
JI J. Geophys. Res.-Planets
PD JAN 27
PY 2011
VL 116
AR E00F14
DI 10.1029/2010JE003683
PG 28
WC Geochemistry & Geophysics
SC Geochemistry & Geophysics
GA 713VA
UT WOS:000286764300001
ER
PT J
AU Prejean, SG
Brodsky, EE
AF Prejean, Stephanie G.
Brodsky, Emily E.
TI Volcanic plume height measured by seismic waves based on a mechanical
model
SO JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH
LA English
DT Article
ID MOUNT ST-HELENS; STROMBOLI VOLCANO; PYROCLASTIC FLOWS; SOURCE
PARAMETERS; FORM INVERSIONS; ERUPTION; DYNAMICS; SIGNALS; JAPAN;
CONSTRAINTS
AB In August 2008 an unmonitored, largely unstudied Aleutian volcano, Kasatochi, erupted catastrophically. Here we use seismic data to infer the height of large eruptive columns such as those of Kasatochi based on a combination of existing fluid and solid mechanical models. In so doing, we propose a connection between a common, observable, short-period seismic wave amplitude to the physics of an eruptive column. To construct a combined model, we estimate the mass ejection rate of material from the vent on the basis of the plume height, assuming that the height is controlled by thermal buoyancy for a continuous plume. Using the estimated mass ejection rate, we then derive the equivalent vertical force on the Earth through a momentum balance. Finally, we calculate the far-field surface waves resulting from the vertical force. The model performs well for recent eruptions of Kasatochi and Augustine volcanoes if v, the velocity of material exiting the vent, is 120-230 m s(-1). The consistency between the seismically inferred and measured plume heights indicates that in these cases the far-field similar to 1 s seismic energy radiated by fluctuating flow in the volcanic jet during the eruption is a useful indicator of overall mass ejection rates. Thus, use of the model holds promise for characterizing eruptions and evaluating ash hazards to aircraft in real time on the basis of far-field short-period seismic data. This study emphasizes the need for better measurements of eruptive plume heights and a more detailed understanding of the full spectrum of seismic energy radiated coeruptively.
C1 [Prejean, Stephanie G.] US Geol Survey, Alaska Volcano Observ, Anchorage, AK 99508 USA.
[Brodsky, Emily E.] Univ Calif Santa Cruz, Dept Earth & Planetary Sci, Santa Cruz, CA 95064 USA.
RP Prejean, SG (reprint author), US Geol Survey, Alaska Volcano Observ, 4210 Univ Ave, Anchorage, AK 99508 USA.
EM sprejean@usgs.gov
RI Brodsky, Emily/B-9139-2014;
OI Brodsky, Emily/0000-0002-6855-6860
FU Federal Aviation Administration
FX Reviews by Larry Mastin, Darcy Ogden, David Schneider, David Hill, David
Fee, and two anonymous reviewers significantly improved this manuscript.
Seismic stations used in this study were originally installed with
funding from the Federal Aviation Administration and are maintained by
the Alaska Volcano Observatory, the Alaska Earthquake Information
Center, and the Alaska Tsunami Warning Center.
NR 56
TC 9
Z9 9
U1 0
U2 10
PU AMER GEOPHYSICAL UNION
PI WASHINGTON
PA 2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA
SN 2169-9313
EI 2169-9356
J9 J GEOPHYS RES-SOL EA
JI J. Geophys. Res.-Solid Earth
PD JAN 26
PY 2011
VL 116
AR B01306
DI 10.1029/2010JB007620
PG 13
WC Geochemistry & Geophysics
SC Geochemistry & Geophysics
GA 713TZ
UT WOS:000286761600005
ER
PT J
AU Waller, RG
Scanlon, KM
Robinson, LF
AF Waller, Rhian G.
Scanlon, Kathryn M.
Robinson, Laura F.
TI Cold-Water Coral Distributions in the Drake Passage Area from Towed
Camera Observations - Initial Interpretations
SO PLOS ONE
LA English
DT Article
ID BIOLOGY; DEEP; REGION; REEFS
AB Seamounts are unique deep-sea features that create habitats thought to have high levels of endemic fauna, productive fisheries and benthic communities vulnerable to anthropogenic impacts. Many seamounts are isolated features, occurring in the high seas, where access is limited and thus biological data scarce. There are numerous seamounts within the Drake Passage (Southern Ocean), yet high winds, frequent storms and strong currents make seafloor sampling particularly difficult. As a result, few attempts to collect biological data have been made, leading to a paucity of information on benthic habitats or fauna in this area, particularly those on primarily hard-bottom seamounts and ridges. During a research cruise in 2008 six locations were examined (two on the Antarctic margin, one on the Shackleton Fracture Zone, and three on seamounts within the Drake Passage), using a towed camera with onboard instruments to measure conductivity, temperature, depth and turbidity. Dominant fauna and bottom type were categorized from 200 randomized photos from each location. Cold-water corals were present in high numbers in habitats both on the Antarctic margin and on the current swept seamounts of the Drake Passage, though the diversity of orders varied. Though the Scleractinia (hard corals) were abundant on the sedimented margin, they were poorly represented in the primarily hard-bottom areas of the central Drake Passage. The two seamount sites and the Shackleton Fracture Zone showed high numbers of stylasterid (lace) and alcyonacean (soft) corals, as well as large numbers of sponges. Though data are preliminary, the geological and environmental variability (particularly in temperature) between sample sites may be influencing cold-water coral biogeography in this region. Each area observed also showed little similarity in faunal diversity with other sites examined for this study within all phyla counted. This manuscript highlights how little is understood of these isolated features, particularly in Polar regions.
C1 [Waller, Rhian G.] Univ Hawaii Manoa, Sch Ocean & Earth Sci & Technol, Honolulu, HI 96822 USA.
[Scanlon, Kathryn M.] US Geol Survey, Woods Hole, MA 02543 USA.
[Robinson, Laura F.] Woods Hole Oceanog Inst, Marine Chem & Geochem Dept, Woods Hole, MA 02543 USA.
RP Waller, RG (reprint author), Univ Maine, Darling Marine Ctr, Sch Marine Sci, Walpole, ME 04573 USA.
EM rhian.waller@maine.edu
OI Robinson, Laura/0000-0001-6811-0140
FU National Science Foundation [ANT0636787]; CenSeam; University of Hawaii
at Manoa
FX This work was funded by the National Science Foundation's Antarctic
Earth Sciences Program (ANT0636787 awarded to LFR and RGW) and a CenSeam
minigrant (awarded to RGW), and RGW is supported by a SOEST Young
Investigator Fellowship from the University of Hawaii at Manoa. The
funders had no role in study design, data collection and analysis,
decision to publish, or preparation of the manuscript.
NR 26
TC 14
Z9 14
U1 2
U2 16
PU PUBLIC LIBRARY SCIENCE
PI SAN FRANCISCO
PA 1160 BATTERY STREET, STE 100, SAN FRANCISCO, CA 94111 USA
SN 1932-6203
J9 PLOS ONE
JI PLoS One
PD JAN 25
PY 2011
VL 6
IS 1
AR e16153
DI 10.1371/journal.pone.0016153
PG 9
WC Multidisciplinary Sciences
SC Science & Technology - Other Topics
GA 712IZ
UT WOS:000286661400030
PM 21283585
ER
PT J
AU Foster, AL
Ashley, RP
Rytuba, JJ
AF Foster, Andrea L.
Ashley, Roger P.
Rytuba, James J.
TI Arsenic species in weathering mine tailings and biogenic solids at the
Lava Cap Mine Superfund Site, Nevada City, CA
SO GEOCHEMICAL TRANSACTIONS
LA English
DT Article
ID X-RAY-ABSORPTION; LODE GOLD DISTRICT; QUANTITATIVE SPECIATION;
OXIDATION-KINETICS; SURFACE-CHEMISTRY; SYNTHETIC PYRITE; NI IMPURITIES;
HEAVY-METALS; SPECTROSCOPY; FERRIHYDRITE
AB Background: A realistic estimation of the health risk of human exposure to solid-phase arsenic (As) derived from historic mining operations is a major challenge to redevelopment of California's famed "Mother Lode" region. Arsenic, a known carcinogen, occurs in multiple solid forms that vary in bioaccessibility. X-ray absorption fine-structure spectroscopy (XAFS) was used to identify and quantify the forms of As in mine wastes and biogenic solids at the Lava Cap Mine Superfund (LCMS) site, a historic "Mother Lode" gold mine. Principal component analysis (PCA) was used to assess variance within water chemistry, solids chemistry, and XAFS spectral datasets. Linear combination, least-squares fits constrained in part by PCA results were then used to quantify arsenic speciation in XAFS spectra of tailings and biogenic solids.
Results: The highest dissolved arsenic concentrations were found in Lost Lake porewater and in a groundwater-fed pond in the tailings deposition area. Iron, dissolved oxygen, alkalinity, specific conductivity, and As were the major variables in the water chemistry PCA. Arsenic was, on average, 14 times more concentrated in biologically-produced iron (hydr)oxide than in mine tailings. Phosphorous, manganese, calcium, aluminum, and As were the major variables in the solids chemistry PCA. Linear combination fits to XAFS spectra indicate that arsenopyrite (FeAsS), the dominant form of As in ore material, remains abundant (average: 65%) in minimally-weathered ore samples and water-saturated tailings at the bottom of Lost Lake. However, tailings that underwent drying and wetting cycles contain an average of only 30% arsenopyrite. The predominant products of arsenopyrite weathering were identified by XAFS to be As-bearing Fe (hydr)oxide and arseniosiderite (Ca(2)Fe(AsO(4))(3)O(3)center dot 3H(2)O). Existence of the former species is not in question, but the presence of the latter species was not confirmed by additional measurements, so its identification is less certain. The linear combination, least-squares fits totals of several samples deviate by more than +/- 20% from 100%, suggesting that additional phases may be present that were not identified or evaluated in this study.
Conclusions: Sub-to anoxic conditions minimize dissolution of arsenopyrite at the LCMS site, but may accelerate the dissolution of As-bearing secondary iron phases such as Fe(3+)-oxyhydroxides and arseniosiderite, if sufficient organic matter is present to spur anaerobic microbial activity. Oxidizing, dry conditions favor the stabilization of secondary phases, while promoting oxidative breakdown of the primary sulfides. The stability of both primary and secondary As phases is likely to be at a minimum under cyclic wet-dry conditions. Biogenic iron (hydr)oxide flocs can sequester significant amounts of arsenic; this property may be useful for treatment of perpetual sources of As such as mine adit water, but the fate of As associated with natural accumulations of floc material needs to be assessed.
C1 [Foster, Andrea L.; Ashley, Roger P.; Rytuba, James J.] US Geol Survey, Menlo Pk, CA 94025 USA.
RP Foster, AL (reprint author), US Geol Survey, 345 Middlefield Rd,MS 901, Menlo Pk, CA 94025 USA.
EM afoster@usgs.gov
FU Geoenvironmental Impacts of Mercury
FX ALF assisted in collection of water samples, and collected/analyzed
about half of the solid samples. XAFS data collection and interpretation
was performed by ALF. ALF was the primary author of all but the
background sections of this manuscript. RPA led the collection and
analysis of water samples, was responsible for the chemical analysis of
about 1/2 of the solid samples, and was the primary author of the
initial draft of the background section of the manuscript. JJR provided
guidance and oversight as chief of the USGS-funded project
Geoenvironmental Impacts of Mercury and As, which provided financial
support for this work. All authors have read and approved the final
manuscript.
NR 58
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U1 6
U2 35
PU BIOMED CENTRAL LTD
PI LONDON
PA 236 GRAYS INN RD, FLOOR 6, LONDON WC1X 8HL, ENGLAND
SN 1467-4866
J9 GEOCHEM T
JI Geochem. Trans.
PD JAN 24
PY 2011
VL 12
AR 1
DI 10.1186/1467-4866-12-1
PG 21
WC Geochemistry & Geophysics
SC Geochemistry & Geophysics
GA 720CG
UT WOS:000287257200001
PM 21261983
ER
PT J
AU Hart, LM
Traxler, GS
Garver, KA
Richard, J
Gregg, JL
Grady, CA
Kurath, G
Hershberger, PK
AF Hart, Lucas M.
Traxler, Garth S.
Garver, Kyle A.
Richard, Jon
Gregg, Jacob L.
Grady, Courtney A.
Kurath, Gael
Hershberger, Paul K.
TI Larval and juvenile Pacific herring Clupea pallasii are not susceptible
to infectious hematopoietic necrosis under laboratory conditions
SO DISEASES OF AQUATIC ORGANISMS
LA English
DT Article
DE IHN; Infectious hematopoietic necrosis; Pacific herring; Clupea pallasii
ID SALMON ONCORHYNCHUS-NERKA; VIRAL HEMORRHAGIC SEPTICEMIA; SOCKEYE-SALMON;
BRITISH-COLUMBIA; ATLANTIC SALMON; VIRUS; TRANSMISSION; CANADA; FISH;
WALBAUM
AB Infectious hematopoietic necrosis (IHN) leads to periodic epidemics among certain wild and farmed fish species of the Northeast (NE) Pacific. The source of the IHN virus (IHNV) that initiates these outbreaks remains unknown; however, a leading hypothesis involves viral persistence in marine host species such as Pacific herring Clupea pallasii. Under laboratory conditions we exposed specific pathogen-free (SPF) larval and juvenile Pacific herring to 10(3) to 10(4) plaque-forming units (pfu) of IHNV ml(-1) by waterborne immersion. Cumulative mortalities among exposed groups were not significantly different from those of negative control groups. After waterborne exposure, IHNV was transiently recovered from the tissues of larvae but absent in tissues of juveniles. Additionally, no evidence of viral shedding was detected in the tank water containing exposed juveniles. After intraperitoneal (IP) injection of IHNV in juvenile herring with 10(3) pfu, IHNV was recovered from the tissues of sub-sampled individuals for only the first 5 d post-exposure. The lack of susceptibility to overt disease and transient levels of IHNV in the tissues of exposed fish indicate that Pacific herring do not likely serve a major epizootiological role in perpetuation of IHNV among free-ranging sock-eye salmon Oncorhynchus nerka and farmed Atlantic salmon Salmo salar in the NE Pacific.
C1 [Hart, Lucas M.; Gregg, Jacob L.; Grady, Courtney A.; Hershberger, Paul K.] US Geol Survey, Marrowstone Marine Field Stn, WFRC, Nordland, WA 98358 USA.
[Traxler, Garth S.; Garver, Kyle A.; Richard, Jon] Fisheries & Oceans Canada, Pacific Biol Stn, Nanaimo, BC V9T 6N7, Canada.
[Kurath, Gael] US Geol Survey, WFRC, Seattle, WA 98115 USA.
RP Hart, LM (reprint author), US Geol Survey, Marrowstone Marine Field Stn, WFRC, Nordland, WA 98358 USA.
EM lhart@usgs.gov
FU Exxon Valdez Oil Spill Trustee Council [070819]; Fisheries and Oceans
Canada; US Geological Survey
FX Funding was provided by the Exxon Valdez Oil Spill Trustee Council,
Project # 070819, Fisheries and Oceans Canada, and US Geological Survey
Fisheries and Aquatic Resources Program. The use of trade, firm, or
corporation names in this publication is for the information and
convenience of the reader. Such use does not constitute an official
endorsement or approval by the US Department of Interior or the US
Geological Survey of any product or service to the exclusion of others
that may be suitable.
NR 28
TC 0
Z9 0
U1 0
U2 2
PU INTER-RESEARCH
PI OLDENDORF LUHE
PA NORDBUNTE 23, D-21385 OLDENDORF LUHE, GERMANY
SN 0177-5103
J9 DIS AQUAT ORGAN
JI Dis. Aquat. Org.
PD JAN 21
PY 2011
VL 93
IS 2
BP 105
EP 110
DI 10.3354/dao02294
PG 6
WC Fisheries; Veterinary Sciences
SC Fisheries; Veterinary Sciences
GA 711SF
UT WOS:000286611000002
PM 21381516
ER
PT J
AU Gleeson, T
Smith, L
Moosdorf, N
Hartmann, J
Durr, HH
Manning, AH
van Beek, LPH
Jellinek, AM
AF Gleeson, Tom
Smith, Leslie
Moosdorf, Nils
Hartmann, Jens
Durr, Hans H.
Manning, Andrew H.
van Beek, Ludovicus P. H.
Jellinek, A. M.
TI Mapping permeability over the surface of the Earth
SO GEOPHYSICAL RESEARCH LETTERS
LA English
DT Article
ID HYDRAULIC CONDUCTIVITY; CONTINENTAL-CRUST; GROUNDWATER; FLOW; DYNAMICS;
MODELS
AB Permeability, the ease of fluid flow through porous rocks and soils, is a fundamental but often poorly quantified component in the analysis of regional-scale water fluxes. Permeability is difficult to quantify because it varies over more than 13 orders of magnitude and is heterogeneous and dependent on flow direction. Indeed, at the regional scale, maps of permeability only exist for soil to depths of 1-2 m. Here we use an extensive compilation of results from hydrogeologic models to show that regional-scale (>5 km) permeability of consolidated and unconsolidated geologic units below soil horizons (hydrolithologies) can be characterized in a statistically meaningful way. The representative permeabilities of these hydrolithologies are used to map the distribution of near-surface (on the order of 100 m depth) permeability globally and over North America. The distribution of each hydrolithology is generally scale independent. The near-surface mean permeability is of the order of similar to 5 x 10(-14) m(2). The results provide the first global picture of near-surface permeability and will be of particular value for evaluating global water resources and modeling the influence of climate-surface-subsurface interactions on global climate change. Citation: Gleeson, T., L. Smith, N. Moosdorf, J. Hartmann, H. H. Durr, A. H. Manning, L. P. H. van Beek, and A. M. Jellinek (2011), Mapping permeability over the surface of the Earth, Geophys. Res. Lett., 38, L02401, doi: 10.1029/2010GL045565.
C1 [Gleeson, Tom; Smith, Leslie; Jellinek, A. M.] Univ British Columbia, Dept Earth & Ocean Sci, Vancouver, BC V6T 1Z4, Canada.
[Durr, Hans H.; van Beek, Ludovicus P. H.] Univ Utrecht, Dept Phys Geog, Fac Geosci, NL-3508 TC Utrecht, Netherlands.
[Moosdorf, Nils; Hartmann, Jens] Univ Hamburg, Inst Biogeochem & Marine Chem, D-20146 Hamburg, Germany.
[Manning, Andrew H.] US Geol Survey, Denver, CO 80225 USA.
RP Gleeson, T (reprint author), Univ British Columbia, Dept Earth & Ocean Sci, 6339 Stores Rd, Vancouver, BC V6T 1Z4, Canada.
EM tgleeson@eos.ubc.ca
RI Moosdorf, Nils/B-3851-2009; Durr, Hans/F-6370-2010; Hartmann,
Jens/A-6306-2008; Gleeson, Tom/F-2552-2011; van Beek, Rens/B-4904-2014;
OI Moosdorf, Nils/0000-0003-2822-8261; Durr, Hans/0000-0001-5787-3994;
Hartmann, Jens/0000-0003-1878-9321; Gleeson, Tom/0000-0001-9493-7707;
van Beek, Rens/0000-0002-4758-108X; Manning, Andrew/0000-0002-6404-1237
FU NSERC; German Science Foundation (DFG) [HA 4472/6-1, EXC177]; Utrecht
University; EU [036993]
FX TG is supported by a NSERC postdoctoral grant. JH and NM are supported
through the German Science Foundation (DFG-project HA 4472/6-1 and the
Cluster of Excellence 'CliSAP' (EXC177), University of Hamburg). We
thank numerous hydrogeologists including L. Bentley, B. Jaworska-Szulc,
C. Neuzil, A. Reeves, R. Rojas-Mujica and W. Sanford for providing
information for the compilation. N. Sihota completed the normality
tests. J. Caine (USGS), K. Christie (University of Alaska-Fairbanks), H.
Peterson (UBC) and D. Sweetkind (USGS) and two anonymous reviewers
greatly improved this paper. Please contact TG to contribute to the
ongoing permeability compilation or for high-resolution versions of the
permeability map. HHD has been funded by Utrecht University (High
Potential Project G-NUX) and the EU FP6 project CARBO-North (project
number 036993).
NR 34
TC 78
Z9 78
U1 11
U2 51
PU AMER GEOPHYSICAL UNION
PI WASHINGTON
PA 2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA
SN 0094-8276
J9 GEOPHYS RES LETT
JI Geophys. Res. Lett.
PD JAN 21
PY 2011
VL 38
AR L02401
DI 10.1029/2010GL045565
PG 6
WC Geosciences, Multidisciplinary
SC Geology
GA 710MY
UT WOS:000286517100003
ER
PT J
AU Zhang, L
Wylie, BK
Ji, L
Gilmanov, TG
Tieszen, LL
Howard, DM
AF Zhang, Li
Wylie, Bruce K.
Ji, Lei
Gilmanov, Tagir G.
Tieszen, Larry L.
Howard, Daniel M.
TI Upscaling carbon fluxes over the Great Plains grasslands: Sinks and
sources
SO JOURNAL OF GEOPHYSICAL RESEARCH-BIOGEOSCIENCES
LA English
DT Article
ID CONTERMINOUS UNITED-STATES; GROSS PRIMARY PRODUCTION; NET ECOSYSTEM
EXCHANGE; CO2 EXCHANGE; DIOXIDE EXCHANGE; INTERANNUAL VARIABILITY;
PRIMARY PRODUCTIVITY; TEMPERATE GRASSLAND; EUROPEAN FORESTS; COMBINING
MODIS
AB Previous studies suggested that the grasslands may be carbon sinks or near equilibrium, and they often shift between carbon sources in drought years and carbon sinks in other years. It is important to understand the responses of net ecosystem production (NEP) to various climatic conditions across the U. S. Great Plains grasslands. Based on 15 grassland flux towers, we developed a piecewise regression model and mapped the grassland NEP at 250 m spatial resolution over the Great Plains from 2000 to 2008. The results showed that the Great Plains was a net sink with an averaged annual NEP of 24 +/- 14 g C m(-2) yr(-1), ranging from a low value of 0.3 g C m(-2) yr(-1) in 2002 to a high value of 47.7 g C m(-2) yr-1 in 2005. The regional averaged NEP for the entire Great Plains grasslands was estimated to be 336 Tg C yr(-1) from 2000 to 2008. In the 9 year period including 4 dry years, the annual NEP was very variable in both space and time. It appeared that the carbon gains for the Great Plains were more sensitive to droughts in the west than the east. The droughts in 2000, 2002, 2006, and 2008 resulted in increased carbon losses over drought-affected areas, and the Great Plains grasslands turned into a relatively low sink with NEP values of 15.8, 0.3, 20.1, and 10.2 g C m(-2) yr(-1) for the 4 years, respectively.
C1 [Zhang, Li] Chinese Acad Sci, Key Lab Digital Earth, Ctr Earth Observat & Digital Earth, Beijing 100101, Peoples R China.
[Gilmanov, Tagir G.] S Dakota State Univ, Dept Biol & Microbiol, Brookings, SD 57007 USA.
[Ji, Lei] ASRC Res & Technol Solut, USGS EROS Ctr, Sioux Falls, SD 57198 USA.
[Wylie, Bruce K.; Tieszen, Larry L.] US Geol Survey, Earth Resources Observat & Sci Ctr, Sioux Falls, SD 57198 USA.
[Zhang, Li] Beijing Normal Univ, Acad Disaster Reduct & Emergency Management, State Key Lab Earth Surface Proc & Resource Ecol, Beijing 100875, Peoples R China.
[Howard, Daniel M.] Stinger Ghaffarian Technol, USGS EROS Ctr, Sioux Falls, SD 57198 USA.
RP Zhang, L (reprint author), Chinese Acad Sci, Key Lab Digital Earth, Ctr Earth Observat & Digital Earth, Beijing 100101, Peoples R China.
EM lizhang@ceode.ac.cn; wylie@usgs.gov; lji@usgs.gov;
tagir.gilmanov@sdstate.edu; tieszen@usgs.gov; dhoward@usgs.gov
RI li, dongsheng/B-2285-2012; Wylie, Bruce/H-3182-2014;
OI Wylie, Bruce/0000-0002-7374-1083; Howard, Daniel/0000-0002-7563-7538
FU USGS [08HQCN0005]; National Basic Research Program of China (973)
[2009CB723906]
FX The study was supported by the USGS Geographic Analysis and Monitoring
Program and the National Basic Research Program of China (973) under
grant 2009CB723906. Any use of trade, product, or firm names is for
description purposes only and does not imply endorsement by the U. S.
Government. The work by Lei Ji was performed under USGS contract
08HQCN0007, and the work by Daniel Howard was performed under USGS
contract 08HQCN0005. We are grateful for the flux tower data provided by
AmeriFlux network, USDA Agriflux network, and other flux tower
investigators.
NR 60
TC 20
Z9 21
U1 2
U2 36
PU AMER GEOPHYSICAL UNION
PI WASHINGTON
PA 2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA
SN 2169-8953
EI 2169-8961
J9 J GEOPHYS RES-BIOGEO
JI J. Geophys. Res.-Biogeosci.
PD JAN 20
PY 2011
VL 116
AR G00J03
DI 10.1029/2010JG001504
PG 13
WC Environmental Sciences; Geosciences, Multidisciplinary
SC Environmental Sciences & Ecology; Geology
GA 710OG
UT WOS:000286520500002
ER
PT J
AU Anteau, MJ
Afton, AD
AF Anteau, Michael J.
Afton, Alan D.
TI Lipid Catabolism of Invertebrate Predator Indicates Widespread Wetland
Ecosystem Degradation
SO PLOS ONE
LA English
DT Article
ID SPRING CONDITION HYPOTHESIS; SCAUP AYTHYA-AFFINIS; LESSER SCAUP;
MISSISSIPPI-RIVER; UPPER-MIDWEST; WESTERN SANDPIPERS; MIGRATION;
METABOLITES; CONSISTENT; RESERVES
AB Animals frequently undergo periods when they accumulate lipid reserves for subsequent energetically expensive activities, such as migration or breeding. During such periods, daily lipid-reserve dynamics (DLD) of sentinel species can quantify how landscape modifications affect function, health, and resilience of ecosystems. Aythya affinis (Eyton 1838; lesser scaup; diving duck) are macroinvertebrate predators; they migrate through an agriculturally dominated landscape in spring where they select wetlands with the greatest food density to refuel and accumulate lipid reserves for subsequent reproduction. We index DLD by measuring plasma-lipid metabolites of female scaup (n = 459) that were refueling at 75 spring migration stopover areas distributed across the upper Midwest, USA. We also indexed DLD for females (n = 44) refueling on a riverine site (Pool 19) south of our upper Midwest study area. We found that mean DLD estimates were significantly (P < 0.05) less than zero in all ecophysiographic regions of the upper Midwest, and the greatest negative value was in the Iowa Prairie Pothole region (-31.6). Mean DLD was 16.8 at Pool 19 and was markedly greater than in any region of the upper Midwest. Our results indicate that females catabolized rather than stored lipid reserves throughout the upper Midwest. Moreover, levels of lipid catabolism are alarming, because scaup use the best quality wetlands available within a given stopover area. Accordingly, these results provide evidence of wetland ecosystem degradation across this large agricultural landscape and document affects that are carried-up through several trophic levels. Interestingly, storing of lipids by scaup at Pool 19 likely reflects similar ecosystem perturbations as observed in the upper Midwest because wetland drainage and agricultural runoff nutrifies the riverine habitat that scaup use at Pool 19. Finally, our results underscore how using this novel technique to monitor DLD, of a carefully selected sentinel species, can index ecosystem health at a landscape scale.
C1 [Anteau, Michael J.] Louisiana State Univ, Sch Renewable Nat Resources, Baton Rouge, LA 70803 USA.
[Afton, Alan D.] Louisiana State Univ, Louisiana Cooperat Fish & Wildlife Res Unit, US Geol Survey, Baton Rouge, LA 70803 USA.
RP Anteau, MJ (reprint author), US Geol Survey, No Prairie Wildlife Res Ctr, Jamestown, ND USA.
EM manteau@usgs.gov
FU Ducks Unlimited Inc. USA; Federal and Winchester Cartridge Companies;
Iowa Department of Natural Resources; IWWR of Ducks Unlimited Canada;
Graduate School and the School of Renewable Natural Resources at
Louisiana State University; Louisiana Department of Wildlife and
Fisheries, Louisiana State University; Minnesota Department of Natural
Resources; Minnesota Waterfowl Association; North Dakota Game and Fish
Department; Prairie Pothole Joint Venture; Upper Mississippi River and
Great Lakes Region Joint Venture; USFWS Regions 3 and 6 HAPET offices;
USGS-Louisiana Cooperative Fish and Wildlife Research Unit;
USGS-National Wetlands Research Center
FX The following organizations provided financial or in-kind support: Ducks
Unlimited Inc. USA, Federal and Winchester Cartridge Companies, Iowa
Department of Natural Resources, IWWR of Ducks Unlimited Canada, IWWR of
Ducks Unlimited Canada through the Bonnycastle Fellowship, the Graduate
School and the School of Renewable Natural Resources at Louisiana State
University, Louisiana Department of Wildlife and Fisheries, Louisiana
State University through the Bosch Fellowship, Minnesota Department of
Natural Resources, Minnesota Waterfowl Association, North Dakota Game
and Fish Department, Prairie Pothole Joint Venture, Upper Mississippi
River and Great Lakes Region Joint Venture, USFWS Regions 3 and 6 HAPET
offices, USGS-Louisiana Cooperative Fish and Wildlife Research Unit, and
USGS-National Wetlands Research Center. The funders had no role in study
design, data collection and analysis, decision to publish, or
preparation of the manuscript.
NR 44
TC 7
Z9 8
U1 0
U2 15
PU PUBLIC LIBRARY SCIENCE
PI SAN FRANCISCO
PA 185 BERRY ST, STE 1300, SAN FRANCISCO, CA 94107 USA
SN 1932-6203
J9 PLOS ONE
JI PLoS One
PD JAN 19
PY 2011
VL 6
IS 1
AR e16029
DI 10.1371/journal.pone.0016029
PG 6
WC Multidisciplinary Sciences
SC Science & Technology - Other Topics
GA 710OH
UT WOS:000286520600020
PM 21283806
ER
PT J
AU Ellis, BK
Stanford, JA
Goodman, D
Stafford, CP
Gustafson, DL
Beauchamp, DA
Chess, DW
Craft, JA
Deleray, MA
Hansen, BS
AF Ellis, Bonnie K.
Stanford, Jack A.
Goodman, Daniel
Stafford, Craig P.
Gustafson, Daniel L.
Beauchamp, David A.
Chess, Dale W.
Craft, James A.
Deleray, Mark A.
Hansen, Barry S.
TI Long-term effects of a trophic cascade in a large lake ecosystem
SO PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF
AMERICA
LA English
DT Article
DE invasive species; top predators; food web; Mysis diluviana; lake trout
ID OLIGOTROPHIC LAKE; FLATHEAD LAKE; ZOOPLANKTON; PRODUCTIVITY;
PHYTOPLANKTON; NUTRIENTS; STOCKING; COLLAPSE; MONTANA; USA
AB Introductions or invasions of nonnative organisms can mediate major changes in the trophic structure of aquatic ecosystems. Here we document multitrophic level impacts in a spatially extensive system that played out over more than a century. Positive interactions among exotic vertebrate and invertebrate predators caused a substantial and abrupt shift in community composition resulting in a trophic cascade that extended to primary producers and to a nonaquatic species, the bald eagle. The opossum shrimp, Mysis diluviana, invaded Flathead Lake, Montana, the largest freshwater lake in the western United States. Lake trout had been introduced 80 y prior but remained at low densities until nonnative Mysis became established. The bottom-dwelling mysids eliminated a recruitment bottleneck for lake trout by providing a deep water source of food where little was available previously. Lake trout subsequently flourished on mysids and this voracious piscivore now dominates the lake fishery; formerly abundant kokanee were extirpated, and native bull and westslope cutthroat trout are imperiled. Predation by Mysis shifted zooplankton and phytoplankton community size structure. Bayesian change point analysis of primary productivity (27-y time series) showed a significant step increase of 55 mg C m(-2) d(-1) (i.e., 21% rise) concurrent with the mysid invasion, but little trend before or after despite increasing nutrient loading. Mysis facilitated predation by lake trout and indirectly caused the collapse of kokanee, redirecting energy flow through the ecosystem that would otherwise have been available to other top predators (bald eagles).
C1 [Ellis, Bonnie K.; Stanford, Jack A.; Craft, James A.] Univ Montana, Flathead Lake Biol Stn, Polson, MT 59860 USA.
[Goodman, Daniel; Gustafson, Daniel L.] Montana State Univ, Dept Ecol, Environm Stat Grp, Bozeman, MT 59717 USA.
[Ellis, Bonnie K.; Stanford, Jack A.; Stafford, Craig P.] Univ Montana, Div Biol Sci, Missoula, MT 59812 USA.
[Beauchamp, David A.] Univ Washington, Sch Aquat & Fisheries Sci, Washington Cooperat Fish & Wildlife Res Unit, US Geol Survey, Seattle, WA 98105 USA.
[Chess, Dale W.] Coeur Alene Tribe, Plummer, ID 83851 USA.
[Deleray, Mark A.] Montana Fish, Wildlife & Pk, Kalispell, MT 59901 USA.
[Hansen, Barry S.] Confederated Salish & Kootenai Tribes, Pablo, MT 59855 USA.
RP Ellis, BK (reprint author), Univ Montana, Flathead Lake Biol Stn, Polson, MT 59860 USA.
EM bonnie.ellis@umontana.edu
NR 40
TC 62
Z9 63
U1 21
U2 151
PU NATL ACAD SCIENCES
PI WASHINGTON
PA 2101 CONSTITUTION AVE NW, WASHINGTON, DC 20418 USA
SN 0027-8424
J9 P NATL ACAD SCI USA
JI Proc. Natl. Acad. Sci. U. S. A.
PD JAN 18
PY 2011
VL 108
IS 3
BP 1070
EP 1075
DI 10.1073/pnas.1013006108
PG 6
WC Multidisciplinary Sciences
SC Science & Technology - Other Topics
GA 707TF
UT WOS:000286310300036
PM 21199944
ER
PT J
AU Riedel, M
Collett, TS
Shankar, U
AF Riedel, M.
Collett, T. S.
Shankar, U.
TI Documenting channel features associated with gas hydrates in the
Krishna-Godavari Basin, offshore India
SO MARINE GEOLOGY
LA English
DT Article
DE gas hydrates; channel systems; levee deposits; East Coast of India
ID EAST-COAST; STRATIGRAPHY
AB During the India National Gas Hydrate Program (NGHP) Expedition 01 in 2006 significant sand and gas hydrate were recovered at Site NGHP-01-15 within the Krishna-Godavari Basin, East Coast off India. At the drill site NGHP-01-15, a 5-8 m thick interval was found that is characterized by higher sand content than anywhere else at the site and within the KG Basin. Gas hydrate concentrations were determined to be 20-40% of the pore volume using wire-line electrical resistivity data as well as core-derived pore-fluid freshening trends. The gas hydrate-bearing interval was linked to a prominent seismic reflection observed in the 3D seismic data. This reflection event, mapped for about 1 km(2) south of the drill site, is bound by a fault at its northern limit that may act as migration conduit for free gas to enter the gas hydrate stability zone (GHSZ) and subsequently charge the sand-rich layer. On 3D and additional regional 2D seismic data a prominent channel system was imaged mainly by using the seismic instantaneous amplitude attribute. The channel can be clearly identified by changes in the seismic character of the channel fill (sand-rich) and pronounced levees (less sand content than in the fill, but higher than in surrounding mud-dominated sediments). The entire channel sequence (channel fill and levees) has been subsequently covered and back-filled with a more mud-prone sediment sequence. Where the levees intersect the base of the GHSZ, their reflection strengths are significantly increased to 5- to 6-times the surrounding reflection amplitudes. Using the 3D seismic data these high-amplitude reflection edges where linked to the gas hydrate-bearing layer at Site NGHP-01-15. Further south along the channel the same reflection elements representing the levees do not show similarly large reflection amplitudes. However, the channel system is still characterized by several high-amplitude reflection events (a few hundred meters wide and up to similar to 1 km in extent) interpreted as gas hydrate-bearing sand intervals along the length of the channel. Crown Copyright (C) 2010 Published by Elsevier B.V. All rights reserved.
C1 [Riedel, M.] Geol Survey Canada, Pacific Geosci Ctr, Nat Resources Canada, Sidney, BC V8L 4B2, Canada.
[Collett, T. S.] US Geol Survey, Denver Fed Ctr, Lakewood, CO 80225 USA.
[Shankar, U.] Natl Geophys Res Inst, Hyderabad 500606, Andhra Pradesh, India.
[Shankar, U.] CSIR, New Delhi, India.
RP Riedel, M (reprint author), Geol Survey Canada, Pacific Geosci Ctr, Nat Resources Canada, 9860 W Saanich Rd, Sidney, BC V8L 4B2, Canada.
EM mriedel@nrcan.gc.ca; tcollett@usgs.gov; umashankar_ngri@yahoo.com
NR 32
TC 20
Z9 23
U1 3
U2 11
PU ELSEVIER SCIENCE BV
PI AMSTERDAM
PA PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS
SN 0025-3227
J9 MAR GEOL
JI Mar. Geol.
PD JAN 15
PY 2011
VL 279
IS 1-4
BP 1
EP 11
DI 10.1016/j.margeo.2010.10.008
PG 11
WC Geosciences, Multidisciplinary; Oceanography
SC Geology; Oceanography
GA 717OR
UT WOS:000287057800001
ER
PT J
AU Gamage, K
Screaton, E
Bekins, B
Aiello, I
AF Gamage, Kusali
Screaton, Elizabeth
Bekins, Barbara
Aiello, Ivano
TI Permeability-porosity relationships of subduction zone sediments
SO MARINE GEOLOGY
LA English
DT Article
DE permeability; porosity; subduction zone; marine sediment; grain size;
smectite
ID FLUID-FLOW; ACCRETIONARY COMPLEX; ANISOTROPIC PERMEABILITY;
MARINE-SEDIMENTS; HEAT-FLOW; DIAGENESIS; SMECTITE; MARGIN; CLAYS;
GEOCHEMISTRY
AB Permeability porosity relationships for sediments from the northern Barbados, Costa Rica, Nankai, and Peru subduction zones were examined based on sediment type, grain size distribution, and general mechanical and chemical compaction history. Greater correlation was observed between permeability and porosity in siliciclastic sediments, diatom oozes, and nannofossil chalks than in nannofossil oozes. For siliciclastic sediments, grouping of sediments by percentage of clay-sized material yields relationships that are generally consistent with results from other marine settings and suggests decreasing permeability as percentage of clay-sized material increases. Correction of measured porosities for smectite content improved the correlation of permeability porosity relationships for siliciclastic sediments and diatom oozes. The relationship between permeability and porosity for diatom oozes is very similar to the relationship in siliciclastic sediments, and permeabilities of both sediment types are related to the amount of clay-size particles. In contrast, nannofossil oozes have higher permeability values by 1.5 orders of magnitude than siliciclastic sediments of the same porosity and show poor correlation between permeability and porosity. More indurated calcareous sediments, nannofossil chalks, overlap siliciclastic permeabilities at the lower end of their measured permeability range, suggesting similar consolidation patterns at depth. Thus, the lack of correlation between permeability and porosity for nannofossil oozes is likely related to variations in mechanical and chemical compaction at shallow depths. This study provides the foundation for a much-needed global database with fundamental properties that relate to permeability in marine settings. Further progress in delineating controls on permeability requires additional carefully documented permeability measurements on well-characterized samples. (C) 2010 Elsevier B.V. All rights reserved.
C1 [Gamage, Kusali; Screaton, Elizabeth] Univ Florida, Dept Geol Sci, Gainesville, FL 32611 USA.
[Bekins, Barbara] US Geol Survey, Menlo Pk, CA 94025 USA.
[Aiello, Ivano] Moss Landing Marine Labs, Moss Landing, CA 95039 USA.
RP Gamage, K (reprint author), Texas A&M Univ, Integrated Ocean Drilling Program, 1000 Discovery Dr, College Stn, TX 77845 USA.
EM kusali@ufl.edu
FU U.S. National Science Foundation (NSF); JOI/United States Science
Support Program (USSSP); NSF [OCE-0751497]
FX This research used samples and data provided by the Ocean Drilling
Program (ODP). ODP was sponsored by the U.S. National Science Foundation
(NSF) and participating countries under the management of Joint
Oceanographic Institutions (JOI), Inc. We especially want to thank Mike
Underwood and Dawn Cardace for use of their data. This manuscript has
benefited greatly from valuable and thorough reviews by the Editor David
Piper, Chris Neuzil, Steve Ingebritsen, Angelo Camerlenghi, and two
anonymous reviewers. Funding for this research was provided by
JOI/United States Science Support Program (USSSP) postcruise grants to
E. Screaton and B. Bekins and by the NSF through grant OCE-0751497 to E.
Screaton.
NR 71
TC 24
Z9 24
U1 0
U2 21
PU ELSEVIER SCIENCE BV
PI AMSTERDAM
PA PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS
SN 0025-3227
EI 1872-6151
J9 MAR GEOL
JI Mar. Geol.
PD JAN 15
PY 2011
VL 279
IS 1-4
BP 19
EP 36
DI 10.1016/j.margeo.2010.10.010
PG 18
WC Geosciences, Multidisciplinary; Oceanography
SC Geology; Oceanography
GA 717OR
UT WOS:000287057800003
ER
PT J
AU Moore, DE
Lockner, DA
AF Moore, Diane E.
Lockner, David A.
TI Frictional strengths of talc-serpentine and talc-quartz mixtures
SO JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH
LA English
DT Article
ID SLAB-MANTLE INTERFACE; SUBDUCTION ZONES; FAULT GOUGE; STABILITY;
MINERALS; BEHAVIOR; ROCKS; WATER
AB Talc is a constituent of faults in a variety of settings, and it may be an effective weakening agent depending on its abundance and distribution within a fault. We conducted frictional strength experiments under hydrothermal conditions to determine the effect of talc on the strengths of synthetic gouges of lizardite and antigorite serpentinites and of quartz. Small amounts of talc weaken serpentinite gouges substantially more than predicted by simple weight averaging. In comparison, mixtures of quartz and talc show a linear trend of strength reduction at talc concentrations <= 15 wt % and enhanced weakening at higher concentrations. All of the strength data are fit by a modified version of the Reuss mixing law that allows for the dominance of one mineral over the other. The difference in the behavior of serpentinite-talc and quartz-talc mixtures at low talc concentrations is a reflection of their different textures. Lizardite, antigorite, and talc all have platy habits, and displacement within gouges composed of these minerals is localized to narrow shears along which the platy grains have rotated into alignment with the shear surfaces. The shears in the mixed phyllosilicate gouges maximize the proportion of the weaker mineral within them. When mixed with a strong, rounded mineral such as quartz, some minimum concentration of talc is needed to form connected pathways that enhance strength reductions. The typical development of talc by the reaction of Si-rich fluids with serpentinite or dolomite would tend to localize its occurrence in a natural fault and result in enhanced weakening.
C1 [Moore, Diane E.; Lockner, David A.] US Geol Survey, Menlo Pk, CA 94025 USA.
RP Moore, DE (reprint author), US Geol Survey, 345 Middlefield Rd,MS977, Menlo Pk, CA 94025 USA.
EM dmoore@usgs.gov
NR 33
TC 27
Z9 27
U1 2
U2 9
PU AMER GEOPHYSICAL UNION
PI WASHINGTON
PA 2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA
SN 2169-9313
EI 2169-9356
J9 J GEOPHYS RES-SOL EA
JI J. Geophys. Res.-Solid Earth
PD JAN 15
PY 2011
VL 116
AR B01403
DI 10.1029/2010JB007881
PG 17
WC Geochemistry & Geophysics
SC Geochemistry & Geophysics
GA 707YL
UT WOS:000286327300001
ER
PT J
AU Rasmussen, C
Brantley, S
Richter, DD
Blum, A
Dixon, J
White, AF
AF Rasmussen, C.
Brantley, S.
Richter, D. deB.
Blum, A.
Dixon, J.
White, A. F.
TI Strong climate and tectonic control on plagioclase weathering in
granitic terrain
SO EARTH AND PLANETARY SCIENCE LETTERS
LA English
DT Article
DE denudation; chemical weathering; physical erosion; granite; regolith;
climate
ID LONG-TERM; LUQUILLO MOUNTAINS; PHYSICAL EROSION; MASS-BALANCE;
PUERTO-RICO; FIELD-MEASUREMENTS; SILICATE MINERALS; DENUDATION RATES;
ATMOSPHERIC CO2; VOLCANIC SOILS
AB Investigations to understand linkages among climate, erosion and weathering are central to quantifying landscape evolution. We approach these linkages through synthesis of regolith data for granitic terrain compiled with respect to climate, geochemistry, and denudation rates for low sloping upland profiles. Focusing on Na as a proxy for plagioclase weathering, we quantified regolith Na depletion, Na mass loss, and the relative partitioning of denudation to physical and chemical contributions. The depth and magnitude of regolith Na depletion increased continuously with increasing water availability, except for locations with mean annual temperature <5 degrees C that exhibited little Na depletion, and locations with physical erosion rates <20 g m(-2) yr(-1) that exhibited deep and complete regolith Na depletion. Surface Na depletion also tended to decrease with increasing physical erosion. Depth-integrated Na mass loss and regolith depth were both three orders of magnitude greater in the fully depleted, low erosion rate sites relative to other locations. These locations exhibited strong erosion-limitation of Na chemical weathering rates based on correlation of Na chemical weathering rate to total Na denudation. Sodium weathering rates in cool locations with positive annual water balance were strongly correlated to total Na denudation and precipitation, and exhibited an average apparent activation energy (Ea) of 69 kJ mol(-1) Na. The remaining water-limited locations exhibited kinetic limitation of Na weathering rates with an Ea of 136 kJ mol(-1) Na, roughly equivalent to the sum of laboratory measures of Ea and dissolution reaction enthalpy for albite. Water availability is suggested as the dominant factor limiting rate kinetics in the water-limited systems. Together, these data demonstrate marked transitions and nonlinearity in how climate and tectonics correlate to plagioclase chemical weathering and Na mass loss. (C) 2010 Elsevier B.V. All rights reserved.
C1 [Rasmussen, C.] Univ Arizona, Dept Soil Water & Environm Sci, Tucson, AZ 85721 USA.
[Brantley, S.] Penn State Univ, Earth & Environm Syst Inst, University Pk, PA 16802 USA.
[Richter, D. deB.] Duke Univ, Nicholas Sch Environm, Durham, NC 27708 USA.
[Blum, A.] US Geol Survey, Boulder, CO 80303 USA.
[Dixon, J.] Arizona State Univ, Sch Earth & Space Explorat, Tempe, AZ 85287 USA.
[White, A. F.] US Geol Survey, Menlo Pk, CA 94025 USA.
RP Rasmussen, C (reprint author), Univ Arizona, Dept Soil Water & Environm Sci, Tucson, AZ 85721 USA.
EM crasmuss@cals.arizona.edu
RI Dixon, Jean/B-2099-2012
OI Dixon, Jean/0000-0002-7763-4939
FU Critical Zone Exploration Network; NSF [EAR-0632516, EAR-0724958,
EAR-0722476, DEB-0543130]
FX This work was coordinated and supported through the Critical Zone
Exploration Network and NSF grants EAR-0632516, EAR-0724958, EAR-0722476
and DEB-0543130. The manuscript benefitted from discussions with Cliff
Riebe, Oliver Chadwick, Anthony Hartshorn, Marina Lebedeva and Jennifer
Williams, and comments from three anonymous reviewers.
NR 88
TC 41
Z9 41
U1 4
U2 62
PU ELSEVIER SCIENCE BV
PI AMSTERDAM
PA PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS
SN 0012-821X
J9 EARTH PLANET SC LETT
JI Earth Planet. Sci. Lett.
PD JAN 15
PY 2011
VL 301
IS 3-4
BP 521
EP 530
DI 10.1016/j.epsl.2010.11.037
PG 10
WC Geochemistry & Geophysics
SC Geochemistry & Geophysics
GA 717TL
UT WOS:000287070200011
ER
PT J
AU Jew, AD
Kim, CS
Rytuba, JJ
Gustin, MS
Brown, GE
AF Jew, Adam D.
Kim, Christopher S.
Rytuba, James J.
Gustin, Mae S.
Brown, Gordon E., Jr.
TI New Technique for Quantification of Elemental Hg in Mine Wastes and Its
Implications for Mercury Evasion Into the Atmosphere
SO ENVIRONMENTAL SCIENCE & TECHNOLOGY
LA English
DT Article
ID MULTIPLE-SCATTERING; EXAFS SPECTROSCOPY; ORGANIC-MATTER; SPECIATION;
SOILS; EXTRACTIONS; SEDIMENTS; EMISSION; TAILINGS; PYROLYSIS
AB Mercury in the environment is of prime concern to both ecosystem and human health. Determination of the molecular-level speciation of Hg in soils and mine wastes is important for understanding its sequestration, mobility, and availability for methylation. Extended X-ray absorption fine structure (EXAFS) spectroscopy carried out under ambient P-T conditions has been used in a number of past studies to determine Hg speciation in complex mine wastes and associated soils. However, this approach cannot detect elemental (liquid) mercury in Hg-polluted soils and sediments due to the significant structural disorder of liquid Hg at ambient-temperature. A new sample preparation protocol involving slow cooling through the crystallization temperature of Hg(0) (234 K) results in its transformation to crystalline alpha-Hg(0). The presence and proportion of Hg(0), relative to other crystalline Hg-bearing phases, in samples prepared in this way can be quantified by low-temperature (77 K) EXAFS spectroscopy. Using this approach, we have determined the relative concentrations of liquid Hg(0) in Hg mine wastes from several sites in the California Coast Range and have found that they correlate well with measured fluxes of gaseous Hg released during light and dark exposure of the same samples, with higher evasion ratios from samples containing higher concentrations of liquid Hg(0). Two different linear relationships are observed in plots of the ratio of Hg emission under light and dark conditions vs % Hg(0), corresponding to silica-carbonate- and hot springs-type Hg deposits, with the hot springs-type samples exhibiting higher evasion fluxes than silica-carbonate type samples at similar Hg(0) concentrations. Our findings help explain significant differences in Hg evasion data for different mine sites in the California Coast Range.
C1 [Jew, Adam D.; Brown, Gordon E., Jr.] Stanford Univ, Dept Geol & Environm Sci, Surface & Aqueous Geochem Grp, Stanford, CA 94305 USA.
[Kim, Christopher S.] Chapman Univ, Dept Chem, Environm Geochem Lab, Orange, CA 92866 USA.
[Rytuba, James J.] US Geol Survey, USGS Mineral Resources Program, Menlo Pk, CA 94025 USA.
[Gustin, Mae S.] Univ Nevada, Dept Nat Resources & Environm Sci, Reno, NV 89557 USA.
[Brown, Gordon E., Jr.] SLAC Natl Accelerator Lab, Dept Photon Sci & Stanford Synchrotron Radiat Lig, Menlo Pk, CA 94025 USA.
RP Jew, AD (reprint author), Stanford Univ, Dept Geol & Environm Sci, Surface & Aqueous Geochem Grp, Stanford, CA 94305 USA.
EM adamjew@stanford.edu
FU Stanford Environmental Molecular Science Institute through NSF
[CHE-0431425]
FX We wish to thank Joe Rogers and John Bargar of the Stanford Synchrotron
Radiation Lightsource for help with data collection on beamline 11-2.
The LN2 cryostat used in the low-temperature work was
designed and built by Steve Conradson of Los Alamos National Laboratory.
G.E.B. thanks George Parks (Stanford University) for helpful discussions
over a number of years about the environmental chemistry of mercury.
Funding for this research comes from the Stanford Environmental
Molecular Science Institute through NSF Grant CHE-0431425. Portions of
this research were carried out at the Stanford Synchrotron Radiation
Lightsource, a National user facility operated by Stanford University on
behalf of the U.S. Department of Energy, Office of Basic Energy Science,
with additional support from the National Institute of Health.
NR 41
TC 23
Z9 23
U1 1
U2 24
PU AMER CHEMICAL SOC
PI WASHINGTON
PA 1155 16TH ST, NW, WASHINGTON, DC 20036 USA
SN 0013-936X
J9 ENVIRON SCI TECHNOL
JI Environ. Sci. Technol.
PD JAN 15
PY 2011
VL 45
IS 2
BP 412
EP 417
DI 10.1021/es1023527
PG 6
WC Engineering, Environmental; Environmental Sciences
SC Engineering; Environmental Sciences & Ecology
GA 704YB
UT WOS:000286090500014
PM 21121657
ER
PT J
AU Bjornsson, BT
Stefansson, SO
McCormick, SD
AF Bjornsson, Bjorn Thrandur
Stefansson, Sigurd O.
McCormick, Stephen D.
TI Environmental endocrinology of salmon smoltification
SO GENERAL AND COMPARATIVE ENDOCRINOLOGY
LA English
DT Article
DE Salmon; Trout; Parr; Smolt; Post-smolt; Smoltification; Cortisol;
Thyroid hormones; Growth hormone; Insulin-like-growth factor I;
Prolactin; Environmental cues
ID PARR-SMOLT TRANSFORMATION; JUVENILE COHO SALMON; GROWTH-HORMONE
ENDOCRINOLOGY; ATLANTIC SALMON; ONCORHYNCHUS-KISUTCH; SEAWATER
ADAPTATION; THYROID-HORMONES; BROWN TROUT; POST-SMOLTS; SALAR L
AB Smolting is a hormone-driven developmental process that is adaptive for downstream migration and ocean survival and growth in anadromous salmonids. Smolting includes increased salinity tolerance, increased metabolism, downstream migratory and schooling behavior, silvering and darkened fin margins, and olfactory imprinting. These changes are promoted by growth hormone, insulin-like growth factor I, cortisol, thyroid hormones, whereas prolactin is inhibitory. Photoperiod and temperature are critical environmental cues for smolt development, and their relative importance will be critical in determining responses to future climate change. Most of our knowledge of the environmental control and endocrine mediation of smolting is based on laboratory and hatchery studies, yet there is emerging information on fish in the wild that indicates substantial differences. Such differences may arise from differences in environmental stimuli in artificial rearing environments, and may be critical to ocean survival and population sustainability. Endocrine disruptors, acidification and other contaminants can perturb smolt development, resulting in poor survival after seawater entry. Published by Elsevier Inc.
C1 [McCormick, Stephen D.] Conte Anadromous Fish Res Ctr, USGS, Turners Falls, MA 01376 USA.
[Bjornsson, Bjorn Thrandur] Univ Gothenburg, Dept Zool Zoophysiol, Fish Endocrinol Lab, SE-40530 Gothenburg, Sweden.
[Stefansson, Sigurd O.] Univ Bergen, Dept Biol, Bergen High Technol Ctr, N-5020 Bergen, Norway.
RP McCormick, SD (reprint author), Conte Anadromous Fish Res Ctr, USGS, 1 Migratory Way,POB 796, Turners Falls, MA 01376 USA.
EM mccormick@umext.umass.edu
RI Bjornsson, Bjorn/B-9161-2008
OI Bjornsson, Bjorn/0000-0002-1310-9756
FU University of Gothenburg Platform on Integrative Physiology (GRIP)
FX This paper has been partly supported by the University of Gothenburg
Platform on Integrative Physiology (GRIP).
NR 118
TC 56
Z9 59
U1 13
U2 140
PU ACADEMIC PRESS INC ELSEVIER SCIENCE
PI SAN DIEGO
PA 525 B ST, STE 1900, SAN DIEGO, CA 92101-4495 USA
SN 0016-6480
EI 1095-6840
J9 GEN COMP ENDOCR
JI Gen. Comp. Endocrinol.
PD JAN 15
PY 2011
VL 170
IS 2
SI SI
BP 290
EP 298
DI 10.1016/j.ygcen.2010.07.003
PG 9
WC Endocrinology & Metabolism
SC Endocrinology & Metabolism
GA 708ND
UT WOS:000286367600009
PM 20627104
ER
PT J
AU Carr, JA
Patino, R
AF Carr, James A.
Patino, Reynaldo
TI The hypothalamus-pituitary-thyroid axis in teleosts and amphibians:
Endocrine disruption and its consequences to natural populations
SO GENERAL AND COMPARATIVE ENDOCRINOLOGY
LA English
DT Article
DE Thyroid; Pituitary; Hypothalamus; Reproduction; Development; Amphibians;
Fishes
ID POLYBROMINATED DIPHENYL ETHERS; ENVIRONMENTALLY RELEVANT CONCENTRATIONS;
TROUT ONCORHYNCHUS-MYKISS; WASTE-WATER CONTAMINANTS; SUCKER
CATOSTOMUS-COMMERSONI; DEPENDENT GENE-EXPRESSION; CATFISH
CLARIAS-BATRACHUS; DEVELOPING XENOPUS-LAEVIS; ZEBRAFISH DANIO-RERIO;
NORTHERN LEOPARD FROG
AB Teleosts and pond-breeding amphibians may be exposed to a wide variety of anthropogenic, waterborne contaminants that affect the hypothalamus-pituitary-thyroid (HPT) axis. Because thyroid hormone is required for their normal development and reproduction, the potential impact of HPT-disrupting contaminants on natural teleost and amphibian populations raises special concern. There is laboratory evidence indicating that persistent organic pollutants, heavy metals, pharmaceutical and personal care products, agricultural chemicals, and aerospace products may alter HPT activity, development, and reproduction in teleosts and amphibians. However, at present there is no evidence to clearly link contaminant-induced HPT alterations to impairments in teleost or amphibian population health in the field. Also, with the exception of perchlorate for which laboratory studies have shown a direct link between HPT disruption and adverse impacts on development and reproductive physiology, little is known about if or how other HPT-disrupting contaminants affect organismal performance. Future field studies should focus on establishing temporal associations between the presence of HPT-disrupting chemicals, the occurrence of HPT alterations, and adverse effects on development and reproduction in natural populations; as well as determining how complex mixtures of HPT contaminants affect organismal and population health. (C) 2010 Elsevier Inc. All rights reserved.
C1 [Carr, James A.] Texas Tech Univ, Dept Biol Sci, Lubbock, TX 79409 USA.
[Patino, Reynaldo] Texas Tech Univ, US Geol Survey, Texas Cooperat Fish & Wildlife Res Unit, Lubbock, TX 79409 USA.
[Patino, Reynaldo] Texas Tech Univ, Dept Nat Resources Management, Lubbock, TX 79409 USA.
[Patino, Reynaldo] Texas Tech Univ, Dept Biol Sci, Lubbock, TX 79409 USA.
RP Carr, JA (reprint author), Texas Tech Univ, Dept Biol Sci, Box 4-3131, Lubbock, TX 79409 USA.
EM james.carr@ttu.edu
FU Texas Tech University; Texas Parks and Wildlife Department; U.S.
Geological Survey; Wildlife Management Institute; U.S. Fish and Wildlife
Service
FX The Texas Cooperative Fish and Wildlife Research Unit is jointly
supported by Texas Tech University, Texas Parks and Wildlife Department,
U.S. Geological Survey, Wildlife Management Institute, and U.S. Fish and
Wildlife Service. We thank Drs. Nathan Collie, Sandeep Mukhi, Phil
Smith, Ernest Smith, and Christopher Theodorakis for reading earlier
drafts of this manuscript.
NR 159
TC 61
Z9 61
U1 5
U2 65
PU ACADEMIC PRESS INC ELSEVIER SCIENCE
PI SAN DIEGO
PA 525 B ST, STE 1900, SAN DIEGO, CA 92101-4495 USA
SN 0016-6480
EI 1095-6840
J9 GEN COMP ENDOCR
JI Gen. Comp. Endocrinol.
PD JAN 15
PY 2011
VL 170
IS 2
SI SI
BP 299
EP 312
DI 10.1016/j.ygcen.2010.06.001
PG 14
WC Endocrinology & Metabolism
SC Endocrinology & Metabolism
GA 708ND
UT WOS:000286367600010
PM 20566362
ER
PT J
AU Schelker, J
Burns, DA
Weiler, M
Laudon, H
AF Schelker, J.
Burns, D. A.
Weiler, M.
Laudon, H.
TI Hydrological mobilization of mercury and dissolved organic carbon in a
snow-dominated, forested watershed: Conceptualization and modeling
SO JOURNAL OF GEOPHYSICAL RESEARCH-BIOGEOSCIENCES
LA English
DT Article
ID NET METHYLMERCURY PRODUCTION; ADIRONDACK LAKES; ULTRAVIOLET ABSORBENCY;
CANADIAN SHIELD; DEPOSITION; CATCHMENT; PEATLANDS; TRANSPORT; DYNAMICS;
TOPMODEL
AB The mobilization of mercury and dissolved organic carbon (DOC) during snowmelt often accounts for a major fraction of the annual loads. We studied the role of hydrological connectivity of riparian wetlands and upland/wetland transition zones to surface waters on the mobilization of Hg and DOC in Fishing Brook, a headwater of the Adirondack Mountains, New York. Stream water total mercury (THg) concentrations varied strongly (mean = 2.25 +/- 0.5 ng L (1)), and the two snowmelt seasons contributed 40% (2007) and 48% (2008) of the annual load. Methyl mercury (MeHg) concentrations ranged up to 0.26 ng L (1), and showed an inverse log relationship with discharge. TOPMODEL-simulated saturated area corresponded well with wetland areas, and the application of a flow algorithm based elevation-above-creek approach suggests that most wetlands become well connected during high flow. The dynamics of simulated saturated area and soil storage deficit were able to explain a large part of the variation of THg concentrations (r(2) = 0.53 to 0.72). In contrast, the simulations were not able to explain DOC variations and DOC and THg concentrations were not correlated. These results indicate that all three constituents, THg, MeHg, and DOC, follow different patterns at the outlet: (1) the mobilization of THg is primarily controlled by the saturation state of the catchment, (2) the dilution of MeHg suggests flushing from a supply limited pool, and (3) DOC dynamics follow a pattern different from THg dynamics, which likely results from differing gain and/or loss processes for THg and/or DOC within the Fishing Brook catchment.
C1 [Schelker, J.; Laudon, H.] Swedish Univ Agr Sci, Dept Forest Ecol & Management, SE-90183 Umea, Sweden.
[Burns, D. A.] US Geol Survey, Watersheds Res Sect, Troy, NY 12180 USA.
[Weiler, M.] Univ Freiburg, Inst Hydrol, D-79085 Freiburg, Germany.
RP Schelker, J (reprint author), Swedish Univ Agr Sci, Dept Forest Ecol & Management, SE-90183 Umea, Sweden.
EM jakob.schelker@slu.se
RI Weiler, Markus/F-5584-2011; Burns, Douglas/A-7507-2009; Laudon,
Hjalmar/J-3074-2013
OI Weiler, Markus/0000-0001-6245-6917; Laudon, Hjalmar/0000-0001-6058-1466
FU U.S. Geological Survey
FX Funding for the research was provided by the U.S. Geological Survey
National Water Quality Assessment Program (NAWQA). A particular thanks
to John Byrnes (USGS) for excellent support in the field and Christoph
Kulls for additional lab analysis at the University of Freiburg,
Germany. Additional logistical support was provided by the Adirondack
Ecological Center operated by SUNY-ESF. Further we thank Jamie Shanley,
Mark Brigham, and David Wolock for useful comments on an earlier version
of this manuscript.
NR 72
TC 24
Z9 25
U1 3
U2 28
PU AMER GEOPHYSICAL UNION
PI WASHINGTON
PA 2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA
SN 0148-0227
J9 J GEOPHYS RES-BIOGEO
JI J. Geophys. Res.-Biogeosci.
PD JAN 12
PY 2011
VL 116
AR G01002
DI 10.1029/2010JG001330
PG 17
WC Environmental Sciences; Geosciences, Multidisciplinary
SC Environmental Sciences & Ecology; Geology
GA 707XB
UT WOS:000286323400001
ER
PT J
AU Close, DA
Yun, SS
McCormick, SD
AF Close, David A.
Yun, Sang-Seon
McCormick, Stephen D.
TI Reply to Thornton and Carroll: Lamprey possess a highly specific
corticosteroid signaling system
SO PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF
AMERICA
LA English
DT Letter
ID HORMONE; MECHANISM; RECEPTOR; BINDING
C1 [Close, David A.] Univ British Columbia, Fisheries Ctr, Vancouver, BC V6T 1Z4, Canada.
[Close, David A.] Univ British Columbia, Dept Zool, Vancouver, BC V6T 1Z4, Canada.
[Yun, Sang-Seon] Kunsan Natl Univ, Dept Marine Biotechnol, Gunsan 573701, Jeonbuk, South Korea.
[McCormick, Stephen D.] US Geol Survey, Conte Anadromous Fish Res Ctr, Turners Falls, MA 01376 USA.
RP Close, DA (reprint author), Univ British Columbia, Fisheries Ctr, Vancouver, BC V6T 1Z4, Canada.
EM d.close@fisheries.ubc.ca
NR 6
TC 1
Z9 1
U1 1
U2 6
PU NATL ACAD SCIENCES
PI WASHINGTON
PA 2101 CONSTITUTION AVE NW, WASHINGTON, DC 20418 USA
SN 0027-8424
J9 P NATL ACAD SCI USA
JI Proc. Natl. Acad. Sci. U. S. A.
PD JAN 11
PY 2011
VL 108
IS 2
BP E6
EP E6
DI 10.1073/pnas.1015112108
PG 1
WC Multidisciplinary Sciences
SC Science & Technology - Other Topics
GA 704ZU
UT WOS:000286097700002
ER
PT J
AU Perkins, KS
Nimmo, JR
Rose, CE
Coupe, RH
AF Perkins, Kim S.
Nimmo, John R.
Rose, Claire E.
Coupe, Richard H.
TI Field tracer investigation of unsaturated zone flow paths and mechanisms
in agricultural soils of northwestern Mississippi, USA
SO JOURNAL OF HYDROLOGY
LA English
DT Article
DE Unsaturated zone; Infiltration; Preferential flow; Aquifer recharge;
Solute transport; Bromide tracer
ID PREFERENTIAL FLOW; WATER; BREAKTHROUGH; CONDUCTIVITY; GROUNDWATER
AB In many farmed areas, intensive application of agricultural chemicals and withdrawal of groundwater for irrigation have led to water quality and supply issues. Unsaturated-zone processes, including preferential flow, play a major role in these effects but are not well understood. In the Bogue Phalia basin, an intensely agricultural area in the Delta region of northwestern Mississippi, the fine-textured soils often exhibit surface ponding and runoff after irrigation and rainfall as well as extensive surface cracking during prolonged dry periods. Fields are typically land-formed to promote surface flow into drainage ditches and streams that feed into larger river ecosystems. Downward flow of water below the root zone is considered minimal; regional groundwater models predict only 5% or less of precipitation recharges the heavily used alluvial aquifer. In this study transport mechanisms within and below the root zone of a fallow soybean field were assessed by performing a 2-m ring infiltration test with tracers and subsurface monitoring instruments. Seven months after tracer application, 48 continuous cores were collected for tracer extraction to define the extent of water movement and quantify preferential flow using a mass-balance approach. Vertical water movement was rapid below the pond indicating the importance of vertical preferential flow paths in the shallow unsaturated zone, especially to depths where agricultural disturbance occurs. Lateral flow of water at shallow depths was extensive and spatially non-uniform, reaching up to 10 m from the pond within 2 months. Within 1 month, the wetting front reached a textural boundary at 4-5 m between the fine-textured soil and sandy alluvium, now a potential capillary barrier which, prior to extensive irrigation withdrawals, was below the water table. Within 10 weeks, tracer was detectable at the water table which is presently about 12 m below land surface. Results indicate that 43% of percolation may be through preferential flow paths and that any water breaking through the capillary barrier (as potential recharge) likely does so in fingers which are difficult to detect with coring methods. In other areas where water levels have declined and soils have similar properties, the potential for transport of agricultural chemicals to the aquifer may be greater than previously assumed. Published by Elsevier B.V.
C1 [Perkins, Kim S.; Nimmo, John R.] US Geol Survey, Menlo Pk, CA 94025 USA.
[Rose, Claire E.; Coupe, Richard H.] US Geol Survey, Pearl, MS 39208 USA.
RP Perkins, KS (reprint author), US Geol Survey, 345 Middlefield Rd, Menlo Pk, CA 94025 USA.
EM kperkins@usgs.gov
FU USGS
FX The authors would like to acknowledge the hard work of many who made
this study possible: Patrick Mills, Michael Manning, Allen Roberts,
Heather Welch, Bobby Richards, Hunter Berch, Jared Smith, Tammy
McKaskle, Trent Snellings, and Rick Healy. The authors are grateful for
the thoughtful reviews provided by Randall Bayless and Patrick Mills.
Funding for this work was provided by the USGS National Water Quality
Assessment Program.
NR 26
TC 12
Z9 12
U1 0
U2 27
PU ELSEVIER SCIENCE BV
PI AMSTERDAM
PA PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS
SN 0022-1694
J9 J HYDROL
JI J. Hydrol.
PD JAN 5
PY 2011
VL 396
IS 1-2
BP 1
EP 11
DI 10.1016/j.jhydrol.2010.09.009
PG 11
WC Engineering, Civil; Geosciences, Multidisciplinary; Water Resources
SC Engineering; Geology; Water Resources
GA 710TR
UT WOS:000286540400001
ER
PT J
AU Wray, JJ
Milliken, RE
Dundas, CM
Swayze, GA
Andrews-Hanna, JC
Baldridge, AM
Chojnacki, M
Bishop, JL
Ehlmann, BL
Murchie, SL
Clark, RN
Seelos, FP
Tornabene, LL
Squyres, SW
AF Wray, J. J.
Milliken, R. E.
Dundas, C. M.
Swayze, G. A.
Andrews-Hanna, J. C.
Baldridge, A. M.
Chojnacki, M.
Bishop, J. L.
Ehlmann, B. L.
Murchie, S. L.
Clark, R. N.
Seelos, F. P.
Tornabene, L. L.
Squyres, S. W.
TI Columbus crater and other possible groundwater-fed paleolakes of Terra
Sirenum, Mars
SO JOURNAL OF GEOPHYSICAL RESEARCH-PLANETS
LA English
DT Article
ID THERMAL EMISSION SPECTROMETER; YELLOWSTONE-NATIONAL-PARK; SCIENCE
EXPERIMENT HIRISE; MERIDIANI-PLANUM; CLAY-MINERALS; REFLECTANCE
SPECTROSCOPY; OMEGA/MARS EXPRESS; MARTIAN HIGHLANDS;
INFRARED-SPECTROSCOPY; SOUTHERN HIGHLANDS
AB Columbus crater in the Terra Sirenum region of the Martian southern highlands contains light-toned layered deposits with interbedded sulfate and phyllosilicate minerals, a rare occurrence on Mars. Here we investigate in detail the morphology, thermophysical properties, mineralogy, and stratigraphy of these deposits; explore their regional context; and interpret the crater's aqueous history. Hydrated mineral-bearing deposits occupy a discrete ring around the walls of Columbus crater and are also exposed beneath younger materials, possibly lava flows, on its floor. Widespread minerals identified in the crater include gypsum, polyhydrated and monohydrated Mg/Fe-sulfates, and kaolinite; localized deposits consistent with montmorillonite, Fe/Mg-phyllosilicates, jarosite, alunite, and crystalline ferric oxide or hydroxide are also detected. Thermal emission spectra suggest abundances of these minerals in the tens of percent range. Other craters in northwest Terra Sirenum also contain layered deposits and Al/Fe/Mg-phyllosilicates, but sulfates have so far been found only in Columbus and Cross craters. The region's intercrater plains contain scattered exposures of Al-phyllosilicates and one isolated mound with opaline silica, in addition to more common Fe/Mg-phyllosilicates with chlorides. A Late Noachian age is estimated for the aqueous deposits in Columbus, coinciding with a period of inferred groundwater upwelling and evaporation, which (according to model results reported here) could have formed evaporites in Columbus and other craters in Terra Sirenum. Hypotheses for the origin of these deposits include groundwater cementation of crater-filling sediments and/or direct precipitation from subaerial springs or in a deep (similar to 900 m) paleolake. Especially under the deep lake scenario, which we prefer, chemical gradients in Columbus crater may have created a habitable environment at this location on early Mars. Citation: Wray, J. J., et al. (2011), Columbus crater and other possible groundwater-fed paleolakes of Terra Sirenum, Mars, J. Geophys. Res., 116, E01001, doi:10.1029/2010JE003694.
C1 [Wray, J. J.; Squyres, S. W.] Cornell Univ, Dept Astron, Ithaca, NY 14853 USA.
[Milliken, R. E.] Univ Notre Dame, Dept Civil Engn & Geol Sci, Notre Dame, IN 46556 USA.
[Dundas, C. M.] Univ Arizona, Lunar & Planetary Lab, Tucson, AZ 85721 USA.
[Swayze, G. A.; Clark, R. N.] US Geol Survey, Denver, CO 80225 USA.
[Andrews-Hanna, J. C.] Colorado Sch Mines, Dept Geophys, Golden, CO 80401 USA.
[Baldridge, A. M.] CALTECH, Jet Prop Lab, Pasadena, CA 91109 USA.
[Chojnacki, M.] Univ Tennessee, Dept Earth & Planetary Sci, Knoxville, TN 37996 USA.
[Bishop, J. L.] SETI Inst, Mountain View, CA 94043 USA.
[Ehlmann, B. L.] Univ Paris 11, Inst Astrophys Spatiale, F-91405 Orsay, France.
[Murchie, S. L.; Seelos, F. P.] Johns Hopkins Univ, Appl Phys Lab, Laurel, MD 20723 USA.
[Tornabene, L. L.] Smithsonian Inst, Natl Air & Space Museum, Ctr Earth & Planetary Studies, Washington, DC 20024 USA.
RP Wray, JJ (reprint author), Cornell Univ, Dept Astron, Ithaca, NY 14853 USA.
EM jwray@astro.cornell.edu
RI Wray, James/B-8457-2008; Chojnacki, Matthew/A-4245-2013; Murchie,
Scott/E-8030-2015; Seelos, Frank/C-7875-2016
OI Wray, James/0000-0001-5559-2179; Dundas, Colin/0000-0003-2343-7224;
Chojnacki, Matthew/0000-0001-8497-8994; Murchie,
Scott/0000-0002-1616-8751; Seelos, Frank/0000-0001-9721-941X
FU Fannie & John Hertz Foundation; NSF
FX We thank S. Mattson and A. Dumke for their efforts producing HiRISE and
HRSC DEMs, respectively. Early reviews by J. K. Crowley, G. A.
Desborough, and S. A. Wilson Purdy as well as discussions with J. F.
Mustard, M. P. Golombek, N. A. Cabrol, J. A. Grant, D. J. Des Marais, V.
F. Chevrier, T. S. Altheide, and S. Karunatillake improved the paper. We
thank R. P. Irwin III and an anonymous reviewer for their thorough
attention to the manuscript. J.J.W. thanks the Fannie & John Hertz
Foundation and the NSF Graduate Research Fellowship for support. We
thank the HiRISE and CRISM science and operations teams for acquiring
the data most critical to our observations and interpretations.
NR 223
TC 69
Z9 69
U1 5
U2 31
PU AMER GEOPHYSICAL UNION
PI WASHINGTON
PA 2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA
SN 2169-9097
EI 2169-9100
J9 J GEOPHYS RES-PLANET
JI J. Geophys. Res.-Planets
PD JAN 5
PY 2011
VL 116
AR E01001
DI 10.1029/2010JE003694
PG 41
WC Geochemistry & Geophysics
SC Geochemistry & Geophysics
GA 704NI
UT WOS:000286059300001
ER
PT J
AU Schlup, M
Steck, A
Carter, A
Cosca, M
Epard, JL
Hunziker, J
AF Schlup, Micha
Steck, Albrecht
Carter, Andrew
Cosca, Michael
Epard, Jean-Luc
Hunziker, Johannes
TI Exhumation history of the NW Indian Himalaya revealed by fission track
and Ar-40/Ar-39 ages
SO JOURNAL OF ASIAN EARTH SCIENCES
LA English
DT Article
DE Himalaya; Geochronology; Nappe tectonics; Ar-Ar ages; Fission track ages
ID ZANSKAR SHEAR ZONE; HIGH-PRESSURE METAMORPHISM; SHIKAR-BEH-NAPPE;
TSO-MORARI; LADAKH HIMALAYA; SE ZANSKAR; NORTHWESTERN HIMALAYA;
CONTINENTAL COLLISION; WESTERN HIMALAYA; EASTERN LADAKH
AB New fission track and Ar/Ar geochronological data provide time constraints on the exhumation history of the Himalayan nappes in the Mandi (Beas valley) - Tso Monad transect of the NW Indian Himalaya. Results from this and previous studies suggest that the SW-directed North Himalayan nappes were emplaced by detachment from the underthrusted upper Indian crust by 55 Ma and metamorphosed by ca. 48-40 Ma. The nappe stack was subsequently exhumed to shallow upper crustal depths (<10 km) by 40-30 Ma in the Tso Monad dome (northern section of the transect) and by 30-20 Ma close to frontal thrusts in the Baralacha La region. From the Oligocene to the present, exhumation continued slowly.
Metamorphism started in the High Himalayan nappe prior to the Late Oligocene.
High temperatures and anatexis of the subducting upper Indian crust engendered the buoyancy-driven ductile detachment and extrusion of the High Himalayan nappe in the zone of continental collision. Late extrusion of the High Himalayan nappe started about 26 Ma ago, accompanied by ductile extensional shearing in the Zanskar shear zone in its roof between 22 and 19 Ma concomitant with thrusting along the basal Main Central Thrust to the south. The northern part of the nappe was then rapidly exhumed to shallow depth (<10 km) between 20 and 6 Ma, while its southern front reached this depth at 10-5 Ma. (C) 2010 Elsevier Ltd. All rights reserved.
C1 [Schlup, Micha; Steck, Albrecht; Cosca, Michael; Hunziker, Johannes] Univ Lausanne, Inst Mineral & Geochim, CH-1015 Lausanne, Switzerland.
[Carter, Andrew] Univ London, Sch Earth Sci, Birkbeck Coll, London WC1E 7HX, England.
[Cosca, Michael] US Geol Survey, Denver Fed Ctr, Lakewood, CO 80225 USA.
[Epard, Jean-Luc] Univ Lausanne, Inst Geol & Paleontol, CH-1015 Lausanne, Switzerland.
RP Steck, A (reprint author), Univ Lausanne, Inst Mineral & Geochim, CH-1015 Lausanne, Switzerland.
EM Albrecht.Steck@unil.ch
RI Carter, Andrew/C-1371-2008; Epard, Jean-Luc/C-8082-2013
OI Carter, Andrew/0000-0002-0090-5868; Epard, Jean-Luc/0000-0003-2319-9967
FU Georgine Claraz Foundation; Herbette Foundation of the University of
Lausanne; Swiss National Science Foundation [20-37470.93, 20-38917.93,
20-58777.99]
FX This study was financed by the Georgine Claraz Foundation, Herbette
Foundation of the University of Lausanne and by the Swiss National
Science Foundation (20-37470.93, 20-38917.93 and 20-58777.99). Marc
Jolivet and an anonymous reviewer are thanked for their critical reading
of the manuscript.
NR 115
TC 9
Z9 9
U1 0
U2 6
PU PERGAMON-ELSEVIER SCIENCE LTD
PI OXFORD
PA THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND
SN 1367-9120
EI 1878-5786
J9 J ASIAN EARTH SCI
JI J. Asian Earth Sci.
PD JAN 4
PY 2011
VL 40
IS 1
BP 334
EP 350
DI 10.1016/j.jseaes.2010.06.008
PG 17
WC Geosciences, Multidisciplinary
SC Geology
GA 696JI
UT WOS:000285437300025
ER
PT J
AU Gold, RD
Cowgill, E
AF Gold, Ryan D.
Cowgill, Eric
TI Deriving fault-slip histories to test for secular variation in slip,
with examples from the Kunlun and Awatere faults
SO EARTH AND PLANETARY SCIENCE LETTERS
LA English
DT Article
DE slip rate; fault-slip history; secular variation in slip;
morphochronology; Kunlun fault; Awatere fault; Monte Carlo
ID SAN-ANDREAS FAULT; ALTYN TAGH FAULT; TRANSIENT STRAIN ACCUMULATION;
CURRENT PLATE MOTIONS; NEW-ZEALAND; SOUTH ISLAND; EASTERN CALIFORNIA;
LARGE EARTHQUAKES; QUATERNARY SLIP; DISPLACEMENT RATES
AB Although offset and age data from displaced landforms are essential for identifying earthquake clusters and thus testing whether faults slip at uniform or secularly varying rates, it is not clear how the uncertainties in such measurements should be propagated so as to yield a robust fault-slip history (i.e., record of fault displacement over time). Here we develop a Monte Carlo approach for estimating the distribution of geologically reasonable fault-slip histories that fit the offset and age data from a population of dated and displaced landforms. The model assumes that the landforms share common faulting histories, the offset and age constraints are correct, and the fault has not reversed shear sense. Analysis of the model results yields both a precise average slip rate, in the case where a linear fit is applied to the data, and a best-fit fault-slip history, in the case where the linear constraint is removed. The method can be used to test for secular variation in slip because the uncertainty on this best-fit history is quantified. By applying the method to previously published morphochronologic data from faulted late Quaternary terrace risers along the Kunlun fault in China and the Awatere fault in New Zealand, we have assessed the extent to which our modeled average slip rates match previously reported values and the data support previous interpretations of uniform slip rate. The Kunlun data set yields average slip rates of 8.7 + 3.6/-2.1 mm/yr and 5.1 + 1.6/-12 mm/yr (68.27% confidence), for the central and eastern reaches of the fault, respectively, both of which match previously published slip rates. Our analysis further indicates that these fault reaches have both slipped uniformly over the latest Quaternary. In contrast, analysis of data from the Saxton River site along the Awatere fault reveals a mid-Holocene deceleration in slip rate from 62 + 1.6/-1.4 mm/yr to 2.8 + 1.0/-0.6 mm/yr. This result contradicts previous interpretations of uniform slip along the Awatere fault. The Monte Carlo method we present here for quantifying fault-slip histories using the offset and age data from a population of faulted landforms provides an important tool for distinguishing temporally uniform from secularly varying fault slip. Published by Elsevier B.V.
C1 [Gold, Ryan D.; Cowgill, Eric] Univ Calif Davis, Dept Geol, Davis, CA 95616 USA.
RP Gold, RD (reprint author), US Geol Survey, Geol Hazards Sci Ctr, Golden, CO 80401 USA.
EM rgold@usgs.gov
RI Gold, Ryan/I-3287-2012
OI Gold, Ryan/0000-0002-4464-6394
FU NSF Office of International Science and Engineering [EAR-0610107]
FX This work was supported by NSF grant EAR-0610107 from the Tectonics
Program and the East Asia and Pacific Program in the NSF Office of
International Science and Engineering. We thank J. D. Zechar, P. Bird,
and R. Weldon for comments that significantly improved the paper. We are
grateful for the computer programming assistance provided by S. Andrews
and N. Conjeepuram and also for statistical consultation provided by N.
Willits of the UC Davis Statistical Laboratory. Conversations with D.
Perkins, E. Burkett, and A. Forte contributed to the development of this
analysis. An early version of the manuscript benefited from reviews from
P. Gold and A. Reuther.
NR 91
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Z9 15
U1 3
U2 12
PU ELSEVIER SCIENCE BV
PI AMSTERDAM
PA PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS
SN 0012-821X
EI 1385-013X
J9 EARTH PLANET SC LETT
JI Earth Planet. Sci. Lett.
PD JAN 3
PY 2011
VL 301
IS 1-2
BP 52
EP 64
DI 10.1016/j.epsl.2010.10.011
PG 13
WC Geochemistry & Geophysics
SC Geochemistry & Geophysics
GA 712CM
UT WOS:000286640400006
ER
PT J
AU Takekawa, JY
De La Cruz, SW
Wilson, MT
Palm, EC
Yee, J
Nysewander, DR
Evenson, JR
Eadie, JM
Esler, D
Boyd, WS
Ward, DH
AF Takekawa, John Y.
De La Cruz, Susan W.
Wilson, Matthew T.
Palm, Eric C.
Yee, Julie
Nysewander, David R.
Evenson, Joseph R.
Eadie, John M.
Esler, Daniel
Boyd, W. Sean
Ward, David H.
BE Wells, JV
TI Breeding Distribution and Ecology of Pacific Coast Surf Scoters
SO BOREAL BIRDS OF NORTH AMERICA: A HEMISPHERIC VIEW OF THEIR CONSERVATION
LINKS AND SIGNIFICANCE
SE Studies in Avian Biology
LA English
DT Article; Book Chapter
DE Baja California; boreal forest; breeding; Melanitta perspicillata;
migratory connectivity; nearest neighbor; Northwest Territories; Puget
Sound; San Francisco Bay; San Quintin Bay; site fidelity; Strait of
Georgia; Surf Scoter
ID WHITE-WINGED SCOTERS; BOREAL FOREST; CLIMATE-CHANGE; HABITAT SELECTION;
POTAMOCORBULA-AMURENSIS; NEAREST-NEIGHBORS; SPRING MIGRATION; FRONTED
GEESE; NEST SUCCESS; BLACK BRANT
AB Recent declines in sea duck populations have highlighted the need for additional basic research across the life cycle of these long-distance migratory birds. A lack of basic ecological information on Surf Scoters (Melanitta perspicillata), including the linkage between wintering and breeding areas and description of their nesting areas, is a major impediment to determining factors contributing to their decline. We marked 415 Surf Scoters with radio and satellite transmitters at four wintering areas along the Pacific coast to describe their breeding synchrony, sympatry, philopatry, and nesting areas selection in the northern boreal forest (NBF). Their primary breeding region was located in the western NBF centered on the Great Slave and Great Bear Lakes in the Northwest Territories, Canada, and their mean settling date (31 May) was remarkably synchronous (+/- 0.9 d). We developed a nearest-neighbor statistic C to examine nesting areas of individuals from different wintering areas and found that they were not clustered (C = 0.031, P = 0.15), but nests of eight individuals found in successive years were highly philopatric and within 1.2 +/- 0.2 km of their previous locations. Finally, we compared nesting areas and random locations with step-wise selection in a second-order Akaike Information Criterion (AIC(c)) analysis to identify the best models. Key landscape features included distance to snowline, elevation gradient, numbers of lakes, distance to treeline, and latitude. A nonparametric classification and regression tree (CART) showed that nesting areas were in an arc of habitat near snowline (<218 km), in lower elevation gradients (<14 m/km), and in areas with 3-6 lakes within 2 X 2 km. Climate change is predicted to have the greatest effects on more northern ecosystems, and NBF species like Surf Scoters with relatively inflexible breeding ecology may be adversely affected if they are unable to adapt quickly to rapidly changing conditions.
C1 [Takekawa, John Y.; De La Cruz, Susan W.; Palm, Eric C.] US Geol Survey, Western Ecol Res Ctr, San Francisco Bay Estuary Field Stn, Vallejo, CA 94592 USA.
[Ward, David H.] US Geol Survey, Alaska Sci Ctr, Anchorage, AK USA.
[Wilson, Matthew T.; Eadie, John M.] Dept Fisheries Wildlife & Conservat Biol, Avian Sci Grad Grp, Davis, CA 95616 USA.
[Yee, Julie] Western Ecol Res Ctr, Sacramento, CA 95819 USA.
[Nysewander, David R.] Washington Dept Fish & Wildlife, Olympia, WA 98501 USA.
[Esler, Daniel; Boyd, W. Sean] Canadian Wildlife Serv, Delta, BC V4K 3N2, Canada.
[Evenson, Joseph R.] Washington Dept Fish & Wildlife, Lakewood, WA 98498 USA.
[De La Cruz, Susan W.] Univ Calif Davis, Grad Grp Ecol, Davis, CA 95616 USA.
RP Takekawa, JY (reprint author), US Geol Survey, Western Ecol Res Ctr, San Francisco Bay Estuary Field Stn, 505 Azuar Dr, Vallejo, CA 94592 USA.
EM john_takekawa@usgs.gov; susan_delacruz@usgs.gov; matt_wilson@fws.gov;
epalm@sfu.ca; julie_yee@usgs.gov; drn2inoly@comcast.net;
evensjre@dfw.wa.gov; jmeadie@ucdavis.edu; desler@sfu.ca;
sean.boyd@ec.gc.ca; david_ward@usgs.gov
RI Eadie, John/E-4820-2011
NR 103
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Z9 6
U1 2
U2 14
PU UNIV CALIFORNIA PRESS
PI BERKELEY
PA 2120 BERKELEY WAY, BERKELEY, CA 94720 USA
BN 978-0-520-95058-0
J9 STUD AVIAN BIOL
JI Stud. Avian Biol.
PY 2011
IS 41
BP 41
EP 63
PG 23
WC Ornithology
SC Zoology
GA BXG81
UT WOS:000296090000005
ER
PT J
AU Greenberg, R
Demarest, DW
Matsuoka, SM
Mettke-Hofmann, C
Evers, D
Hamel, PB
Luscier, J
Powell, LL
Shaw, D
Avery, ML
Hobson, KA
Blancher, PJ
Niven, DK
AF Greenberg, Russell
Demarest, Dean W.
Matsuoka, Steven M.
Mettke-Hofmann, Claudia
Evers, David
Hamel, Paul B.
Luscier, Jason
Powell, Luke L.
Shaw, David
Avery, Michael L.
Hobson, Keith A.
Blancher, Peter J.
Niven, Daniel K.
BE Wells, JV
TI Understanding Declines in Rusty Blackbirds
SO BOREAL BIRDS OF NORTH AMERICA: A HEMISPHERIC VIEW OF THEIR CONSERVATION
LINKS AND SIGNIFICANCE
SE Studies in Avian Biology
LA English
DT Article; Book Chapter
DE contaminants; Euphagus carolinus; habitat use; limiting factors;
population decline; population movements; Rusty Blackbird
ID ESTIMATING SITE OCCUPANCY; ALLUVIAL VALLEY; UNITED-STATES; COMMON LOONS;
FOREST; MERCURY; CONSERVATION; CONTAMINATION; ECOSYSTEMS; RESPONSES
AB The Rusty Blackbird (Euphagus carolinus), a formerly common breeding species of boreal wetlands, has exhibited the most marked decline of any North American landbird. North American Breeding Bird Survey (BBS) trends in abundance are estimated to be -12.5%/yr over the last 40 years, which is tantamount to a >95% cumulative decline. Trends in abundance calculated from Christmas Bird Counts (CBC) for a similar period indicate a range-wide decline of -5.6%/yr. Qualitative analyses of ornithological accounts suggest the species has been declining for over a century. Several studies document range retraction in the southern boreal forest, whereas limited data suggest that abundance may be more stable in more northerly areas. The major hypotheses for the decline include degradation of boreal habitats from logging and agricultural development, mercury contamination, and wetland desiccation resulting from global warming. Other likely reasons for decline include loss or degradation of wooded wetlands of the southeastern U. S and mortality associated with abatement efforts targeting nuisance blackbirds. In addition, the patchy breeding distribution of this species may inhibit population consolidation, causing local populations to crash when reduced to low levels. Progress in understanding the causes and mechanisms for observed declines has remained limited until recently. Here we present initial attempts to understand the habitat requirements of Rusty Blackbirds and offer specific predictions associated with each of the hypotheses for decline as a way of guiding future research.
C1 [Greenberg, Russell] Smithsonian Inst, Natl Zool Pk, Smithsonian Migratory Bird Ctr, Washington, DC 20008 USA.
[Evers, David] BioDivers Res Inst, Gorham, ME 04038 USA.
[Hamel, Paul B.] US Forest Serv, USDA, So Hardwoods Lab, Stoneville, MS 38776 USA.
[Hobson, Keith A.] Canada Canadian Wildlife Serv, Saskatoon, SK S7N 0X4, Canada.
[Luscier, Jason] Univ Arkansas, Dept Biol Sci, Fayetteville, AR 72701 USA.
[Matsuoka, Steven M.] US Fish & Wildlife Serv, Anchorage, AK 99503 USA.
[Mettke-Hofmann, Claudia] Liverpool John Moores Univ, Sch Nat Sci & Psychol, Liverpool L3 3AF, Merseyside, England.
[Powell, Luke L.] Univ Maine, Dept Biol Sci, Orono, ME 04469 USA.
[Shaw, David] Alaska Bird Observ, Fairbanks, AK 99701 USA.
[Niven, Daniel K.] Natl Audubon Soc, Illinois Nat Hist Survey, Champaign, IL 61820 USA.
[Avery, Michael L.] Natl Wildlife Res Ctr, Wildlife Serv, Gainesville, FL 32641 USA.
[Blancher, Peter J.] Environm Canada, Natl Wildlife Res Ctr, Ottawa, ON K1A 0H3, Canada.
[Demarest, Dean W.] US Fish & Wildlife Serv, Atlanta, GA 30345 USA.
RP Greenberg, R (reprint author), Smithsonian Inst, Natl Zool Pk, Smithsonian Migratory Bird Ctr, Washington, DC 20008 USA.
EM greenbergr@si.edu; dean_demarest@fws.gov; steve_matsuoka@fws.gov;
mettke@erl.orn.mpg.de; david.evers@briloon.org; phamel@fs.fed.us;
jluscie@uark.edu; luke.l.powell@gmail.com; dshaw@alaskabird.org;
michael.l.avery@aphis.usda.gov; keith.hobson@ec.gc.ca;
peter.blancher@ec.gc.ca; dniven@audubon.org
NR 91
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Z9 7
U1 4
U2 18
PU UNIV CALIFORNIA PRESS
PI BERKELEY
PA 2120 BERKELEY WAY, BERKELEY, CA 94720 USA
BN 978-0-520-95058-0
J9 STUD AVIAN BIOL
JI Stud. Avian Biol.
PY 2011
IS 41
BP 107
EP 125
PG 19
WC Ornithology
SC Zoology
GA BXG81
UT WOS:000296090000010
ER
PT J
AU Kaczor, NW
Jensen, KC
Klaver, RW
Rumble, MA
Herman-Brunson, KM
Swanson, CC
AF Kaczor, Nicholas W.
Jensen, Kent C.
Klaver, Robert W.
Rumble, Mark A.
Herman-Brunson, Katie M.
Swanson, Christopher C.
BE Sandercock, BK
Martin, K
Segelbacher, G
TI Nesting Success and Resource Selection of Greater Sage-Grouse
SO ECOLOGY, CONSERVATION, AND MANAGEMENT OF GROUSE
SE Studies in Avian Biology
LA English
DT Article; Book Chapter
DE Centrocercus urophasianus; Greater Sage-Grouse; nest initiation; nest
success; renesting; resource selection; sagebrush; South Dakota
ID CENTROCERCUS-UROPHASIANUS; VISUAL OBSTRUCTION; SOUTHEASTERN IDAHO;
CENTRAL WASHINGTON; SURVIVAL; HABITATS; POPULATIONS; ECOSYSTEMS;
VEGETATION; COVER
AB Declines of Greater Sage-Grouse (Centrocercus urophasianus) in South Dakota are a concern because further population declines may lead to isolation from populations in Wyoming and Montana. Furthermore, little information exists about reproductive ecology and resource selection of sage grouse on the eastern edge of their distribution. We investigated Greater Sage-Grouse nesting success and resource selection in South Dakota during 2006-2007. Radio-marked females were tracked to estimate nesting rates, nest success, and habitat resources selected for nesting. Nest initiation was 98.0%, with a maximum likelihood estimate of nest success of 45.6 +/- 5.3%. Females selected nest sites that had greater sagebrush canopy cover and visual obstruction of the nest bowl compared to random sites. Nest survival models indicated that taller grass surrounding nests increased nest survival. Tall grass may supplement the low sagebrush cover in this area in providing suitable nest sites for Greater Sage-Grouse. Land managers on the eastern edge of Greater Sage-Grouse range could focus on increasing sagebrush density while maintaining tall grass by developing range management practices that accomplish this goal. To achieve nest survival rates similar to other populations, predictions from our models suggest 26 cm grass height would result in approximately 50% nest survival. Optimal conditions could be accomplished by adjusting livestock grazing systems and stocking rates.
C1 [Kaczor, Nicholas W.; Jensen, Kent C.; Herman-Brunson, Katie M.; Swanson, Christopher C.] S Dakota State Univ, Dept Wildlife & Fisheries Sci, Brookings, SD 57007 USA.
[Klaver, Robert W.] US Geol Survey, Earth Resources Observat & Sci Ctr, Sioux Falls, SD 57198 USA.
[Rumble, Mark A.] US Forest Serv Rocky Mt, Forest & Grassland Res Lab, Res Stn, Rapid City, SD 57702 USA.
RP Kaczor, NW (reprint author), US Fish & Wildlife Serv, Div Refuge Planning, Lakewood, CO 80228 USA.
EM nick_kaczor@fws.gov; kent.jensen@sdstate.edu; bklaver@usgs.gov;
mrumble@fs.fed.us; kbrunson@ccsd.k12.wy.us; chris_swanson@fws.gov
NR 57
TC 8
Z9 8
U1 2
U2 17
PU UNIV CALIFORNIA PRESS
PI BERKELEY
PA 2120 BERKELEY WAY, BERKELEY, CA 94720 USA
BN 978-0-520-95057-3
J9 STUD AVIAN BIOL
JI Stud. Avian Biol.
PY 2011
IS 39
BP 107
EP 118
PG 12
WC Ornithology
SC Zoology
GA BZU73
UT WOS:000303012700009
ER
PT J
AU Casazza, ML
Coates, PS
Overton, CT
AF Casazza, Michael L.
Coates, Peter S.
Overton, Cory T.
BE Sandercock, BK
Martin, K
Segelbacher, G
TI Linking Habitat Selection and Brood Success in Greater Sage-Grouse
SO ECOLOGY, CONSERVATION, AND MANAGEMENT OF GROUSE
SE Studies in Avian Biology
LA English
DT Article; Book Chapter
DE brood success; Centrocercus urophasianus; forb; Greater Sage-Grouse;
habitat; juniper; pinyon; selection; spatial scale; meadow
ID CROSS-SCALE CORRELATIONS; RESOURCE SELECTION; REARING HABITAT; CHICKS;
PRODUCTIVITY; POPULATION; PATTERNS; SURVIVAL; VEGETATION; ECOLOGY
AB Examining links between the fitness of individual organisms and their habitat-based decisions is useful to identify key resources for conservation and management of a species, especially at multiple spatial scales because selection of habitat attributes may vary with spatial scale. Decisions of habitat use by brood-rearing Greater Sage-Grouse (Centrocercus urophasianus) may influence the survival of chicks. We conducted radiotelemetry on 38 sage grouse broods within Mono County, California, during 2003-2005. At relocation and random sites, we measured habitat characteristics at three spatial scales using field procedures (scale, 0.03 ha) and Geographical Information System tools (scales, 7.9 ha and 226.8 ha). We then conducted three data analyses using an information-theoretic modeling approach. The purpose of these analyses was to: (1) identify habitat factors that were selected (defined as use disproportionate to availability) by sage grouse broods; (2) identify habitat factors associated with brood success (defined as >= 1 live chick at 50 days post-hatch; 24 were successful, 14 unsuccessful); and (3) evaluate brood success as a function of habitat selection indices for brood-rearing sage grouse. At the smallest spatial scale (0.03 ha), grouse with broods selected areas with greater perennial forbs and higher richness of plant species. At larger scales (7.9 ha and 226.8 ha), areas with Utah juniper (Juniperus osteosperma) and singleleaf pinyon pine (Pinus monophylla) encroachment were avoided by grouse. Most importantly, the probability of fledging a brood increased as sage grouse females selected habitats with greater densities of perennial forbs (0.03 ha) and higher meadow edge (perimeter to edge ratio; 7.9 ha), perhaps because these areas provided a balance of food and protective cover for chicks. These results suggest that managers should discourage tree encroachment and preserve and enhance sagebrush stands interspersed with perennial forbs and a mixture of small upland meadows.
C1 [Casazza, Michael L.; Coates, Peter S.; Overton, Cory T.] US Geol Survey, Western Ecol Res Ctr, Dixon Field Stn, Dixon, CA 95620 USA.
RP Casazza, ML (reprint author), US Geol Survey, Western Ecol Res Ctr, Dixon Field Stn, 6924 Tremont Rd, Dixon, CA 95620 USA.
EM mike_casazza@usgs.gov; pcoates@usgs.gov; coverton@usgs.gov
NR 84
TC 24
Z9 25
U1 1
U2 11
PU UNIV CALIFORNIA PRESS
PI BERKELEY
PA 2120 BERKELEY WAY, BERKELEY, CA 94720 USA
BN 978-0-520-95057-3
J9 STUD AVIAN BIOL
JI Stud. Avian Biol.
PY 2011
IS 39
BP 151
EP 167
PG 17
WC Ornithology
SC Zoology
GA BZU73
UT WOS:000303012700012
ER
PT J
AU Oyler-McCance, SJ
Stricker, CA
St John, J
Braun, CE
Wann, GT
O'Donnell, MS
Aldridge, CL
AF Oyler-McCance, Sara J.
Stricker, Craig A.
St John, Judy
Braun, Clait E.
Wann, Gregory T.
O'Donnell, Michael S.
Aldridge, Cameron L.
BE Sandercock, BK
Martin, K
Segelbacher, G
TI Effects of Climate Change on Nutrition and Genetics of White-tailed
Ptarmigan
SO ECOLOGY, CONSERVATION, AND MANAGEMENT OF GROUSE
SE Studies in Avian Biology
LA English
DT Article; Book Chapter
DE climate change; genetics; Lagopus leucura; stable isotopes; temporal
variation
ID GUNNISON SAGE-GROUSE; COLORADO FRONT RANGE; NITROGEN DEPOSITION;
ROCKY-MOUNTAINS; POPULATION BOTTLENECK; MICROSATELLITE LOCI; ECOLOGY;
USA; RESPONSES; ISOTOPES
AB White-tailed Ptarmigan (Lagopus leucura) are well suited as a focal species for the study of climate change because they are adapted to cool, alpine environments that are expected to undergo unusually rapid climate change. We compared samples collected in the late 1930s, the late 1960s, and the late 2000s using molecular genetic and stable isotope methods in an effort to determine whether White-tailed Ptarmigan on Mt. Evans, Colorado, have experienced recent environmental changes resulting in shifts in genetic diversity, gene frequency, and nutritional ecology. We genotyped 115 individuals spanning the three time periods, using nine polymorphic microsatellite loci in our genetic analysis. These samples were also analyzed for stable carbon and nitrogen isotopic composition. We found a slight trend of lower heterozygosity through time, and allelic richness values were lower in more recent times, but not significantly using an alpha of 0.05 (P < 0.1). We found no changes in allele frequencies across time periods, suggesting that population sizes have not changed dramatically. Feather delta C-13 and delta N-15 values decreased significantly across time periods, whereas the range in isotope values increased consistently from the late 1930s to the later time periods. Inferred changes in the nutritional ecology of White-tailed Ptarmigan on Mt. Evans relate primarily to increased atmospheric deposition of nutrients that likely influenced foraging habits and tundra plant composition and nutritional quality. Future work seeks to integrate genetic and isotopic data with long-term demographics to develop a detailed understanding of the interaction among environmental stressors on the long-term viability of ptarmigan populations.
C1 [Oyler-McCance, Sara J.; O'Donnell, Michael S.] US Geol Survey, Ft Collins Sci Ctr, ASRC Management Serv, Ft Collins, CO 80526 USA.
[Stricker, Craig A.] US Geol Survey, Ft Collins Sci Ctr, Denver Fed Ctr, Denver, CO 80225 USA.
[St John, Judy] Univ Denver, Dept Biol Sci, Rocky Mt Ctr Conservat Genet & Systemat, Denver, CO 80208 USA.
[Braun, Clait E.] Grouse Inc, Tucson, AZ 85750 USA.
[Wann, Gregory T.; Aldridge, Cameron L.] Colorado State Univ, Nat Resource Ecol Lab, Ft Collins, CO 80526 USA.
RP Oyler-McCance, SJ (reprint author), US Geol Survey, Ft Collins Sci Ctr, ASRC Management Serv, 2150 Ctr Ave,Bldg C, Ft Collins, CO 80526 USA.
EM sara_oyler-mccance@usgs.gov; cstricker@usgs.gov; stjohn.judy@gmail.com;
sg-wtp@juno.com; gtw248@gmail.com; odonnellm@usgs.gov;
aldridgec@usgs.gov
RI Sidorenko, Aleksandr /F-2724-2016
OI Sidorenko, Aleksandr /0000-0001-5478-0688
NR 55
TC 2
Z9 2
U1 2
U2 5
PU UNIV CALIFORNIA PRESS
PI BERKELEY
PA 2120 BERKELEY WAY, BERKELEY, CA 94720 USA
BN 978-0-520-95057-3
J9 STUD AVIAN BIOL
JI Stud. Avian Biol.
PY 2011
IS 39
BP 283
EP 294
PG 12
WC Ornithology
SC Zoology
GA BZU73
UT WOS:000303012700022
ER
PT S
AU Varanka, D
Carter, J
Usery, EL
Shoberg, T
AF Varanka, Dalia
Carter, Jonathan
Usery, E. Lynn
Shoberg, Thomas
BE Ashish, N
Sheth, AP
TI Topographic Mapping Data Semantics Through Data Conversion and
Enhancement
SO GEOSPATIAL SEMANTICS AND THE SEMANIC WEB: FOUNDATIONS, ALGORITHMS, AND
APPLICATIONS
SE Semantic Web and Beyond-Computing for Human Experience
LA English
DT Article; Book Chapter
ID PRINCIPLES
AB This paper presents research on the semantics of topographic data for triples and ontologies to blend the capabilities of the Semantic Web and The National Map of the U.S. Geological Survey. Automated conversion of relational topographic data of several geographic sample areas to the triple data model standard resulted in relatively poor semantic associations. Further research employed vocabularies of feature type and spatial relation terms. A user interface was designed to model the capture of non-standard terms relevant to public users and to map those terms to existing data models of The National Map through the use of ontology. Server access for the study area triple stores was made publicly available, illustrating how the development of linked data may transform institutional policies to open government data resources to the public. This paper presents these data conversion and research techniques that were tested as open linked data concepts leveraged through a user-centered interface and open USGS server access to the public.
C1 [Varanka, Dalia; Carter, Jonathan; Usery, E. Lynn; Shoberg, Thomas] US Geol Survey, Rolla, MO USA.
RP Varanka, D (reprint author), US Geol Survey, Rolla, MO USA.
EM dvaranka@usgs.gov; jjcarter@usgs.gov; usery@usgs.gov; tshoberg@usgs.gov
NR 37
TC 0
Z9 0
U1 1
U2 1
PU SPRINGER
PI NEW YORK
PA 233 SPRING STREET, NEW YORK, NY 10013, UNITED STATES
SN 1559-7474
BN 978-1-4419-9445-5
J9 SEMAT WEB BEYOND-COM
PY 2011
VL 12
BP 145
EP 162
DI 10.1007/978-1-4419-9446-2_7
D2 10.1007/978-1-4419-9446-2
PG 18
WC Computer Science, Artificial Intelligence; Computer Science, Information
Systems; Computer Science, Theory & Methods
SC Computer Science
GA BVX98
UT WOS:000293120600007
ER
PT S
AU Jones, BF
Conko, KM
AF Jones, Blair F.
Conko, Kathryn M.
BE Galan, E
Singer, A
TI Environmental Influences on the Occurrences of Sepiolite and
Palygorskite: A Brief Review
SO DEVELOPMENTS IN PALYGORSKITE-SEPIOLITE RESEARCH: A NEW OUTLOOK ON THESE
NANOMATERIALS
SE Developments in Clay Science
LA English
DT Article; Book Chapter
ID LACUSTRINE SEDIMENTS; CENTRAL ANATOLIA; CLAY-MINERALS; JBEL RHASSOUL;
HIGH-PLAINS; SW TURKEY; ORIGIN; BASIN; DEPOSITS; GENESIS
C1 [Jones, Blair F.; Conko, Kathryn M.] US Geol Survey, Natl Res Program, Reston, VA 22092 USA.
RP Jones, BF (reprint author), US Geol Survey, Natl Res Program, 959 Natl Ctr, Reston, VA 22092 USA.
NR 41
TC 7
Z9 7
U1 0
U2 0
PU ELSEVIER SCIENCE BV
PI AMSTERDAM
PA SARA BURGERHARTSTRAAT 25, PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS
SN 1572-4352
BN 978-0-44-453608-2
J9 DEV CLAY SCI
PY 2011
VL 3
BP 69
EP 83
DI 10.1016/B978-0-444-53607-5.00003-7
PG 15
WC Nanoscience & Nanotechnology
SC Science & Technology - Other Topics
GA BCS18
UT WOS:000311243300005
ER
PT J
AU Schuenemeyer, JH
Drew, LJ
AF Schuenemeyer, John H.
Drew, Lawrence J.
BA Schuenemeyer, JH
Drew, LJ
BF Schuenemeyer, JH
Drew, LJ
TI Role of Statistics and Data Analysis
SO STATISTICS FOR EARTH AND ENVIRONMENTAL SCIENTISTS
LA English
DT Article; Book Chapter
C1 [Schuenemeyer, John H.] SW Stat Consulting LLC, Cortez, CO USA.
[Drew, Lawrence J.] US Geol Survey, Reston, VA 22092 USA.
RP Schuenemeyer, JH (reprint author), SW Stat Consulting LLC, Cortez, CO USA.
NR 0
TC 0
Z9 0
U1 0
U2 0
PU BLACKWELL SCIENCE PUBL
PI OXFORD
PA OSNEY MEAD, OXFORD OX2 0EL, ENGLAND
BN 978-0-470-65070-7
PY 2011
BP 1
EP 35
PG 35
WC Geology; Mathematics, Applied; Statistics & Probability
SC Geology; Mathematics
GA BCJ07
UT WOS:000310271300002
ER
PT J
AU Schuenemeyer, JH
Drew, LJ
AF Schuenemeyer, John H.
Drew, Lawrence J.
BA Schuenemeyer, JH
Drew, LJ
BF Schuenemeyer, JH
Drew, LJ
TI STATISTICS FOR EARTH AND ENVIRONMENTAL SCIENTISTS PREFACE
SO STATISTICS FOR EARTH AND ENVIRONMENTAL SCIENTISTS
LA English
DT Editorial Material; Book Chapter
C1 [Schuenemeyer, John H.] SW Stat Consulting LLC, Cortez, CO USA.
[Drew, Lawrence J.] US Geol Survey, Reston, VA 22092 USA.
RP Schuenemeyer, JH (reprint author), SW Stat Consulting LLC, Cortez, CO USA.
NR 0
TC 0
Z9 0
U1 0
U2 0
PU BLACKWELL SCIENCE PUBL
PI OXFORD
PA OSNEY MEAD, OXFORD OX2 0EL, ENGLAND
BN 978-0-470-65070-7
PY 2011
BP IX
EP +
PG 11
WC Geology; Mathematics, Applied; Statistics & Probability
SC Geology; Mathematics
GA BCJ07
UT WOS:000310271300001
ER
PT J
AU Schuenemeyer, JH
Drew, LJ
AF Schuenemeyer, John H.
Drew, Lawrence J.
BA Schuenemeyer, JH
Drew, LJ
BF Schuenemeyer, JH
Drew, LJ
TI Modeling Concepts
SO STATISTICS FOR EARTH AND ENVIRONMENTAL SCIENTISTS
LA English
DT Article; Book Chapter
C1 [Schuenemeyer, John H.] SW Stat Consulting LLC, Cortez, CO USA.
[Drew, Lawrence J.] US Geol Survey, Reston, VA 22092 USA.
RP Schuenemeyer, JH (reprint author), SW Stat Consulting LLC, Cortez, CO USA.
NR 0
TC 0
Z9 0
U1 0
U2 0
PU BLACKWELL SCIENCE PUBL
PI OXFORD
PA OSNEY MEAD, OXFORD OX2 0EL, ENGLAND
BN 978-0-470-65070-7
PY 2011
BP 37
EP 50
PG 14
WC Geology; Mathematics, Applied; Statistics & Probability
SC Geology; Mathematics
GA BCJ07
UT WOS:000310271300003
ER
PT J
AU Schuenemeyer, JH
Drew, LJ
AF Schuenemeyer, John H.
Drew, Lawrence J.
BA Schuenemeyer, JH
Drew, LJ
BF Schuenemeyer, JH
Drew, LJ
TI Estimation and Hypothesis Testing on Means and Other Statistics
SO STATISTICS FOR EARTH AND ENVIRONMENTAL SCIENTISTS
LA English
DT Article; Book Chapter
C1 [Schuenemeyer, John H.] SW Stat Consulting LLC, Cortez, CO USA.
[Drew, Lawrence J.] US Geol Survey, Reston, VA 22092 USA.
RP Schuenemeyer, JH (reprint author), SW Stat Consulting LLC, Cortez, CO USA.
NR 0
TC 0
Z9 0
U1 0
U2 0
PU BLACKWELL SCIENCE PUBL
PI OXFORD
PA OSNEY MEAD, OXFORD OX2 0EL, ENGLAND
BN 978-0-470-65070-7
PY 2011
BP 51
EP 98
PG 48
WC Geology; Mathematics, Applied; Statistics & Probability
SC Geology; Mathematics
GA BCJ07
UT WOS:000310271300004
ER
PT J
AU Schuenemeyer, JH
Drew, LJ
AF Schuenemeyer, John H.
Drew, Lawrence J.
BA Schuenemeyer, JH
Drew, LJ
BF Schuenemeyer, JH
Drew, LJ
TI Regression
SO STATISTICS FOR EARTH AND ENVIRONMENTAL SCIENTISTS
LA English
DT Article; Book Chapter
C1 [Schuenemeyer, John H.] SW Stat Consulting LLC, Cortez, CO USA.
[Drew, Lawrence J.] US Geol Survey, Reston, VA 22092 USA.
RP Schuenemeyer, JH (reprint author), SW Stat Consulting LLC, Cortez, CO USA.
NR 0
TC 0
Z9 0
U1 0
U2 0
PU BLACKWELL SCIENCE PUBL
PI OXFORD
PA OSNEY MEAD, OXFORD OX2 0EL, ENGLAND
BN 978-0-470-65070-7
PY 2011
BP 99
EP 149
PG 51
WC Geology; Mathematics, Applied; Statistics & Probability
SC Geology; Mathematics
GA BCJ07
UT WOS:000310271300005
ER
PT J
AU Schuenemeyer, JH
Drew, LJ
AF Schuenemeyer, John H.
Drew, Lawrence J.
BA Schuenemeyer, JH
Drew, LJ
BF Schuenemeyer, JH
Drew, LJ
TI Time Series
SO STATISTICS FOR EARTH AND ENVIRONMENTAL SCIENTISTS
LA English
DT Article; Book Chapter
C1 [Schuenemeyer, John H.] SW Stat Consulting LLC, Cortez, CO USA.
[Drew, Lawrence J.] US Geol Survey, Reston, VA 22092 USA.
RP Schuenemeyer, JH (reprint author), SW Stat Consulting LLC, Cortez, CO USA.
NR 0
TC 1
Z9 1
U1 0
U2 0
PU BLACKWELL SCIENCE PUBL
PI OXFORD
PA OSNEY MEAD, OXFORD OX2 0EL, ENGLAND
BN 978-0-470-65070-7
PY 2011
BP 151
EP 192
PG 42
WC Geology; Mathematics, Applied; Statistics & Probability
SC Geology; Mathematics
GA BCJ07
UT WOS:000310271300006
ER
PT J
AU Schuenemeyer, JH
Drew, LJ
AF Schuenemeyer, John H.
Drew, Lawrence J.
BA Schuenemeyer, JH
Drew, LJ
BF Schuenemeyer, JH
Drew, LJ
TI Spatial Statistics
SO STATISTICS FOR EARTH AND ENVIRONMENTAL SCIENTISTS
LA English
DT Article; Book Chapter
C1 [Schuenemeyer, John H.] SW Stat Consulting LLC, Cortez, CO USA.
[Drew, Lawrence J.] US Geol Survey, Reston, VA 22092 USA.
RP Schuenemeyer, JH (reprint author), SW Stat Consulting LLC, Cortez, CO USA.
NR 0
TC 0
Z9 0
U1 0
U2 0
PU BLACKWELL SCIENCE PUBL
PI OXFORD
PA OSNEY MEAD, OXFORD OX2 0EL, ENGLAND
BN 978-0-470-65070-7
PY 2011
BP 193
EP 241
PG 49
WC Geology; Mathematics, Applied; Statistics & Probability
SC Geology; Mathematics
GA BCJ07
UT WOS:000310271300007
ER
PT J
AU Schuenemeyer, JH
Drew, LJ
AF Schuenemeyer, John H.
Drew, Lawrence J.
BA Schuenemeyer, JH
Drew, LJ
BF Schuenemeyer, JH
Drew, LJ
TI Multivariate Analysis
SO STATISTICS FOR EARTH AND ENVIRONMENTAL SCIENTISTS
LA English
DT Article; Book Chapter
C1 [Schuenemeyer, John H.] SW Stat Consulting LLC, Cortez, CO USA.
[Drew, Lawrence J.] US Geol Survey, Reston, VA 22092 USA.
RP Schuenemeyer, JH (reprint author), SW Stat Consulting LLC, Cortez, CO USA.
NR 0
TC 0
Z9 0
U1 0
U2 0
PU BLACKWELL SCIENCE PUBL
PI OXFORD
PA OSNEY MEAD, OXFORD OX2 0EL, ENGLAND
BN 978-0-470-65070-7
PY 2011
BP 243
EP 291
PG 49
WC Geology; Mathematics, Applied; Statistics & Probability
SC Geology; Mathematics
GA BCJ07
UT WOS:000310271300008
ER
PT J
AU Schuenemeyer, JH
Drew, LJ
AF Schuenemeyer, John H.
Drew, Lawrence J.
BA Schuenemeyer, JH
Drew, LJ
BF Schuenemeyer, JH
Drew, LJ
TI Discrete Data Analysis and Point Processes
SO STATISTICS FOR EARTH AND ENVIRONMENTAL SCIENTISTS
LA English
DT Article; Book Chapter
C1 [Schuenemeyer, John H.] SW Stat Consulting LLC, Cortez, CO USA.
[Drew, Lawrence J.] US Geol Survey, Reston, VA 22092 USA.
RP Schuenemeyer, JH (reprint author), SW Stat Consulting LLC, Cortez, CO USA.
NR 0
TC 0
Z9 0
U1 0
U2 0
PU BLACKWELL SCIENCE PUBL
PI OXFORD
PA OSNEY MEAD, OXFORD OX2 0EL, ENGLAND
BN 978-0-470-65070-7
PY 2011
BP 293
EP 333
PG 41
WC Geology; Mathematics, Applied; Statistics & Probability
SC Geology; Mathematics
GA BCJ07
UT WOS:000310271300009
ER
PT J
AU Schuenemeyer, JH
Drew, LJ
AF Schuenemeyer, John H.
Drew, Lawrence J.
BA Schuenemeyer, JH
Drew, LJ
BF Schuenemeyer, JH
Drew, LJ
TI Design of Experiments
SO STATISTICS FOR EARTH AND ENVIRONMENTAL SCIENTISTS
LA English
DT Article; Book Chapter
C1 [Schuenemeyer, John H.] SW Stat Consulting LLC, Cortez, CO USA.
[Drew, Lawrence J.] US Geol Survey, Reston, VA 22092 USA.
RP Schuenemeyer, JH (reprint author), SW Stat Consulting LLC, Cortez, CO USA.
NR 0
TC 0
Z9 0
U1 0
U2 0
PU BLACKWELL SCIENCE PUBL
PI OXFORD
PA OSNEY MEAD, OXFORD OX2 0EL, ENGLAND
BN 978-0-470-65070-7
PY 2011
BP 335
EP 370
PG 36
WC Geology; Mathematics, Applied; Statistics & Probability
SC Geology; Mathematics
GA BCJ07
UT WOS:000310271300010
ER
PT J
AU Schuenemeyer, JH
Drew, LJ
AF Schuenemeyer, John H.
Drew, Lawrence J.
BA Schuenemeyer, JH
Drew, LJ
BF Schuenemeyer, JH
Drew, LJ
TI Directional Data
SO STATISTICS FOR EARTH AND ENVIRONMENTAL SCIENTISTS
LA English
DT Article; Book Chapter
C1 [Schuenemeyer, John H.] SW Stat Consulting LLC, Cortez, CO USA.
[Drew, Lawrence J.] US Geol Survey, Reston, VA 22092 USA.
RP Schuenemeyer, JH (reprint author), SW Stat Consulting LLC, Cortez, CO USA.
NR 0
TC 0
Z9 0
U1 0
U2 0
PU BLACKWELL SCIENCE PUBL
PI OXFORD
PA OSNEY MEAD, OXFORD OX2 0EL, ENGLAND
BN 978-0-470-65070-7
PY 2011
BP 371
EP 388
PG 18
WC Geology; Mathematics, Applied; Statistics & Probability
SC Geology; Mathematics
GA BCJ07
UT WOS:000310271300011
ER
PT S
AU Key, RM
Pitfield, PEJ
Thomas, RJ
Goodenough, KM
De Waele, B
Schofield, DI
Bauer, W
Horstwood, MSA
Styles, MT
Conrad, J
Encarnacion, J
Lidke, DJ
O'Connor, EA
Potter, C
Smith, RA
Walsh, GJ
Ralison, AV
Randriamananjara, T
Rafahatelo, JM
Rabarimanana, M
AF Key, R. M.
Pitfield, P. E. J.
Thomas, R. J.
Goodenough, K. M.
De Waele, B.
Schofield, D. I.
Bauer, W.
Horstwood, M. S. A.
Styles, M. T.
Conrad, J.
Encarnacion, J.
Lidke, D. J.
O'Connor, E. A.
Potter, C.
Smith, R. A.
Walsh, G. J.
Ralison, A. V.
Randriamananjara, T.
Rafahatelo, J-M
Rabarimanana, M.
BE VanHinsbergen, DJJ
Buiter, SJH
Torsvik, TH
Gaina, C
Webb, SJ
TI Polyphase Neoproterozoic orogenesis within the East Africa-Antarctica
Orogenic Belt in central and northern Madagascar
SO FORMATION AND EVOLUTION OF AFRICA: A SYNOPSIS OF 3.8 GA OF EARTH HISTORY
SE Geological Society Special Publication
LA English
DT Article; Book Chapter
ID U-PB GEOCHRONOLOGY; WEST-CENTRAL MADAGASCAR; DRONNING MAUD LAND;
GONDWANA CONNECTIONS; TECTONIC EVOLUTION; MOZAMBIQUE BELT; DHARWAR
CRATON; CONGO CRATON; ITREMO-GROUP; ZIRCON AGES
AB Our recent geological survey of the basement of central and northern Madagascar allowed us to re-evaluate the evolution of this part of the East Africa-Antarctica Orogen (EAAO). Five crustal domains are recognized, characterized by distinctive lithologies and histories of sedimentation, magmatism, deformation and metamorphism, and separated by tectonic and/or unconformable contacts. Four consist largely of Archaean metamorphic rocks (Antongil, Masora and Antananarivo Cratons, Tsaratanana Complex). The fifth (Bemarivo Belt) comprises Proterozoic meta-igneous rocks. The older rocks were intruded by plutonic suites at c. 1000 Ma, 820-760 Ma, 630-595 Ma and 560-520 Ma. The evolution of the four Archaean domains and their boundaries remains contentious, with two end-member interpretations evaluated: (1) all five crustal domains are separate tectonic elements, juxtaposed along Neoproterozoic sutures and (2) the four Archaean domains are segments of an older Archaean craton, which was sutured against the Bemarivo Belt in the Neoproterozoic. Rodinia fragmented during the early Neoproterozoic with intracratonic rifts that sometimes developed into oceanic basins. Subsequent Mid-Neoproterozoic collision of smaller cratonic blocks was followed by renewed extension and magmatism. The global 'Terminal Pan-African' event (560-490 Ma) finally stitched together the Mid-Neoproterozoic cratons to form Gondwana.
C1 [Key, R. M.; Goodenough, K. M.; Bauer, W.; Smith, R. A.] BGS, Edinburgh EH9 3LA, Midlothian, Scotland.
[Pitfield, P. E. J.; Thomas, R. J.; Schofield, D. I.; Styles, M. T.; O'Connor, E. A.] BGS, Keyworth NG12 5GG, Notts, England.
[De Waele, B.] SRK Consulting, Perth, WA 6005, Australia.
[Horstwood, M. S. A.] NIGL, Keyworth NG12 5GG, Notts, England.
[Conrad, J.; Encarnacion, J.; Lidke, D. J.; Potter, C.; Walsh, G. J.] USGS, Reston, VA 20192 USA.
[Ralison, A. V.; Randriamananjara, T.; Rafahatelo, J-M; Rabarimanana, M.] Projet Gouvernance Ressources Minieres, Antananarivo, Madagascar.
RP Key, RM (reprint author), BGS, W Mains Rd, Edinburgh EH9 3LA, Midlothian, Scotland.
EM rmk@bgs.ac.uk
OI Schofield, David/0000-0002-2669-5627; Horstwood,
Matthew/0000-0003-4200-8193
NR 74
TC 18
Z9 18
U1 0
U2 1
PU GEOLOGICAL SOC PUBLISHING HOUSE
PI BATH
PA UNIT 7, BRASSMILL ENTERPRISE CTR, BRASSMILL LANE, BATH BA1 3JN, AVON,
ENGLAND
SN 0305-8719
BN 978-1-86239-335-6
J9 GEOL SOC SPEC PUBL
JI Geol. Soc. Spec. Publ.
PY 2011
VL 357
BP 49
EP 68
DI 10.1144/SP357.4
D2 10.1144/SP357.0
PG 20
WC Geology
SC Geology
GA BBN14
UT WOS:000307461300004
ER
PT S
AU Dubiel, RF
Hasiotis, ST
AF Dubiel, Russell F.
Hasiotis, Stephen T.
BE Davidson, SK
Leleu, S
North, CP
TI DEPOSYSTEMS, PALEOSOLS, AND CLIMATIC VARIABILITY IN A CONTINENTAL
SYSTEM: THE UPPER TRIASSIC CHINLE FORMATION, COLORADO PLATEAU, USA
SO FROM RIVER TO ROCK RECORD: THE PRESERVATION OF FLUVIAL SEDIMENTS AND
THEIR SUBSEQUENT INTERPRETATION
SE Society for Sedimentary Geology Special Publication
LA English
DT Proceedings Paper
CT 1st River to Rock Record Conference
CY JAN 12-14, 2009
CL Univ Aberdeen, Geol Dept, Aberdeen, SCOTLAND
SP Areva SA, BP Explorat Plc, Brit Soc Geomorphol, Canadian Nat Resources Ltd, Geol Survey Norway, Shell Explorat & Product Ltd, Talisman energy UK Ltd, Total E&P UKk Ltd, Tullow Oil Plc, Univ Nebraska Lincoln, Univ Padova, US Geol Survey
HO Univ Aberdeen, Geol Dept
DE sequence stratigraphy; climate; ichnofossils; fluvial-lacustrine
ID WESTERN UNITED-STATES; NORTHERN NEW-MEXICO; SEQUENCE STRATIGRAPHY;
CORNERS REGION; BIGHORN BASIN; NATIONAL-PARK; PALEOCLIMATE; ARIZONA;
BURROWS; EXAMPLE
AB The Upper Triassic Chinle Formation of the Colorado Plateau in the western United States was deposited as a continental fluvial-floodplain-lacustrine-eolian depositional system near the west coast of Pangea just north of the paleoequator. The deposystem evolved in response to regional tectonics and long-term climate change. Clastic and volcanic sediment was supplied by uplifted highlands and arc magmatism on the margins of the basin. Climate changed from a Pangean megamonsoon regime in the early Late Triassic to an arid climate setting at the close of the Triassic. Chinle fluvial discharge and sediment load varied through time in response to climate, producing degradational and aggradational cycles. Degradation eroded paleovalleys, and aggradation filled them with both meandering and braided fluvial systems, as well as varying amounts of floodplain mudstones. Paleosols developed on paleovalley fills, interfluves, and floodplain siltstones and mudstones, all of which combine to define several scales of degradational and aggradational cycles. An upward stratigraphic trend in Chinle paleosols from Oxisols and Gleysols, to Alfisols (Argillisols) and Vertisols, culminating in Inceptisols (Prototsols) and Aridisols (Calcisols), supports previous interpretations that climate evolved from monsoonal or humid conditions at the beginning of Chinle deposition to progressively more arid climate conditions at the end of deposition.
C1 [Dubiel, Russell F.] US Geol Survey, Denver, CO 80225 USA.
RP Dubiel, RF (reprint author), US Geol Survey, MS 939,Box 25046 DFC, Denver, CO 80225 USA.
NR 140
TC 8
Z9 8
U1 0
U2 4
PU S E P M - SOC SEDIMENTARY GEOLOGY
PI TULSA
PA PO BOX 4756 1731 E 71ST ST, TULSA, OK 74159-0756 USA
SN 1060-071X
BN 978-1-56576-305-0
J9 SOC SEDIMENT GEOL SP
PY 2011
IS 97
BP 393
EP 421
PG 29
WC Geology
SC Geology
GA BCC23
UT WOS:000309690900020
ER
PT J
AU Lipman, PW
McIntosh, WC
AF Lipman, Peter W.
McIntosh, William C.
BE Blair, R
Bracksieck, G
TI Tertiary Volcanism in the Eastern San Juan Mountains
SO EASTERN SAN JUAN MOUNTAINS: THEIR GEOLOGY, ECOLOGY, AND HUMAN HISTORY
LA English
DT Article; Book Chapter
ID COLORADO; FIELD; ERUPTION; EVOLUTION; CALDERAS
C1 [Lipman, Peter W.] US Geol Survey, Menlo Pk, CA 94025 USA.
[McIntosh, William C.] New Mexico Bur Geol & Mineral Resources, Socorro, NM USA.
RP Lipman, PW (reprint author), US Geol Survey, 345 Middlefield Rd, Menlo Pk, CA 94025 USA.
NR 19
TC 0
Z9 0
U1 0
U2 1
PU UNIV PRESS COLORADO
PI BOULDER
PA 5589 ARAPAHOE AVE, STE 206C, BOULDER, CO 80303 USA
BN 978-1-60732-084-5
PY 2011
BP 17
EP 37
PG 21
WC Geography; Geography, Physical
SC Geography; Physical Geography
GA BZB47
UT WOS:000301001400004
ER
PT J
AU Bethke, PM
AF Bethke, Philip M.
BE Blair, R
Bracksieck, G
TI Mineralization in the Eastern San Juan Mountains
SO EASTERN SAN JUAN MOUNTAINS: THEIR GEOLOGY, ECOLOGY, AND HUMAN HISTORY
LA English
DT Article; Book Chapter
ID CREEDE MINING DISTRICT; AMETHYST VEIN SYSTEM; ACID-SULFATE;
FLUID-INCLUSION; ORE DEPOSITION; COLORADO; SUMMITVILLE; ENVIRONMENT;
MINERALOGY; EVOLUTION
C1 US Geol Survey, Reston, VA 22092 USA.
RP Bethke, PM (reprint author), US Geol Survey, 959 Natl Ctr, Reston, VA 22092 USA.
NR 47
TC 0
Z9 0
U1 0
U2 0
PU UNIV PRESS COLORADO
PI BOULDER
PA 5589 ARAPAHOE AVE, STE 206C, BOULDER, CO 80303 USA
BN 978-1-60732-084-5
PY 2011
BP 39
EP 60
PG 22
WC Geography; Geography, Physical
SC Geography; Physical Geography
GA BZB47
UT WOS:000301001400005
ER
PT J
AU Caine, JS
Wilson, AB
AF Caine, Jonathan Saul
Wilson, Anna B.
BE Blair, R
Bracksieck, G
TI The Hydrogeology of the San Juan Mountains
SO EASTERN SAN JUAN MOUNTAINS: THEIR GEOLOGY, ECOLOGY, AND HUMAN HISTORY
LA English
DT Article; Book Chapter
ID FRONT RANGE; COLORADO; PERMEABILITY; AQUIFER; SYSTEM; WATER; USA
C1 [Caine, Jonathan Saul; Wilson, Anna B.] US Geol Survey, Denver, CO 80225 USA.
RP Caine, JS (reprint author), US Geol Survey, Box 25046, Denver, CO 80225 USA.
OI Caine, Jonathan/0000-0002-7269-6989
NR 34
TC 0
Z9 0
U1 0
U2 1
PU UNIV PRESS COLORADO
PI BOULDER
PA 5589 ARAPAHOE AVE, STE 206C, BOULDER, CO 80303 USA
BN 978-1-60732-084-5
PY 2011
BP 79
EP +
PG 52
WC Geography; Geography, Physical
SC Geography; Physical Geography
GA BZB47
UT WOS:000301001400007
ER
PT J
AU Griffiths, JM
King, DW
AF Griffiths, Jose-Marie
King, Donald W.
BE Baker, D
Evans, W
TI The future of librarians in the workforce: a US perspective
SO LIBRARIES AND SOCIETY: ROLE, RESPONSIBILITY AND FUTURE IN AN AGE OF
CHANGE
SE Chandos Information Professional Series
LA English
DT Article; Book Chapter
C1 [Griffiths, Jose-Marie; King, Donald W.] Bryant Univ, Smithfield, RI 02917 USA.
[Griffiths, Jose-Marie] Natl Sci Board, Arlington, VA USA.
[Griffiths, Jose-Marie] Presidents Informat Technol Advisory Comm, Arlington, VA USA.
[Griffiths, Jose-Marie] US Natl Commiss Lib & Informat Sci, Washington, DC USA.
[Griffiths, Jose-Marie] Natl Acad Sci, Washington, DC USA.
[Griffiths, Jose-Marie] NASA, Washington, DC USA.
[Griffiths, Jose-Marie] US DOE, Washington, DC 20560 USA.
[Griffiths, Jose-Marie] US Dept Commerce, Washington, DC 20230 USA.
[Griffiths, Jose-Marie] US Geol Survey, Reston, VA USA.
[Griffiths, Jose-Marie] USN, Washington, DC USA.
[Griffiths, Jose-Marie] Amer Assoc Advancement Sci, Washington, DC USA.
[King, Donald W.] Westat Corp, Gaithersburg, MD USA.
[King, Donald W.] Amer Stat Assoc, Alexandria, VA 22314 USA.
RP Griffiths, JM (reprint author), Bryant Univ, Smithfield, RI 02917 USA.
NR 28
TC 0
Z9 0
U1 0
U2 1
PU CHANDOS PUBL
PI SAWSTON
PA 80 HIGH ST, SAWSTON, CAMBRIDGE CB22 3HJ, ENGLAND
BN 978-1-84334-131-4
J9 CHANDOS INF PROF SER
PY 2011
BP 279
EP 302
D2 10.1533/9781780632636
PG 24
WC Information Science & Library Science
SC Information Science & Library Science
GA BYR59
UT WOS:000299894500021
ER
PT J
AU Rykhus, R
Lu, Z
AF Rykhus, Russell
Lu, Zhong
TI Monitoring a boreal wildfire using multi-temporal Radarsat-1 intensity
and coherence images
SO GEOMATICS NATURAL HAZARDS & RISK
LA English
DT Article
ID CONTERMINOUS UNITED-STATES; POSTFIRE TREE RECRUITMENT; SURFACE
SOIL-MOISTURE; LAND-COVER DATABASE; INTERIOR ALASKA; CLIMATE-CHANGE;
BURN SEVERITY; FORESTS; INTERFEROMETRY; PATTERNS
AB Twenty-five C-band Radarsat-1 synthetic aperture radar (SAR) images acquired from the summer of 2002 to the summer of 2005 are used to map a 2003 boreal wildfire (B346) in the Yukon Flats National Wildlife Refuge, Alaska under conditions of near-persistent cloud cover. Our analysis is primarily based on the 15 SAR scenes acquired during arctic growing seasons. The Radarsat-1 intensity data are used to map the onset and progression of the fire, and interferometric coherence images are used to qualify burn severity and monitor post-fire recovery. We base our analysis of the fire on three test sites, two from within the fire and one unburned site. The B346 fire increased backscattered intensity values for the two burn study sites by approximately 5-6 dB and substantially reduced coherence from background levels of approximately 0.8 in unburned background forested areas to approximately 0.2 in the burned area. Using ancillary vegetation information from the National Land Cover Database (NLCD) and information on burn severity from Normalized Burn Ratio (NBR) data, we conclude that burn site 2 was more severely burned than burn site 1 and that C-band interferometric coherence data are useful for mapping landscape changes due to fire. Differences in burn severity and topography are determined to be the likely reasons for the observed differences in post-fire intensity and coherence trends between burn sites.
C1 [Rykhus, Russell] SGT, Sioux Falls, SD 57198 USA.
[Rykhus, Russell] USGS, Earth Resources Observat & Sci EROS Ctr, Sioux Falls, SD 57198 USA.
[Lu, Zhong] USGS, Cascades Volcano Observ, Vancouver, WA 98683 USA.
[Lu, Zhong] USGS, EROS Ctr, Vancouver, WA 98683 USA.
RP Rykhus, R (reprint author), SGT, 47914 252nd St, Sioux Falls, SD 57198 USA.
EM rykhus@usgs.gov
FU USGS [08HQCN0005]; USGS Land Remote Sensing Program
FX This work was made possible by funding under USGS contract 08HQCN0005
and the USGS Land Remote Sensing Program. Original Radarsat-1 SAR raw
data are copyrighted by the Canadian Space Agency 2002-2005 TM and were
provided by the Alaska Satellite Facility. The authors wish to thank the
anonymous reviewers for their thorough reviews. The use of trade names
does not constitute endorsement by the US Geological Survey or the US
Government.
NR 40
TC 4
Z9 4
U1 0
U2 11
PU TAYLOR & FRANCIS LTD
PI ABINGDON
PA 2-4 PARK SQUARE, MILTON PARK, ABINGDON OR14 4RN, OXON, ENGLAND
SN 1947-5705
EI 1947-5713
J9 GEOMAT NAT HAZ RISK
JI Geomat. Nat. Hazards Risk
PY 2011
VL 2
IS 1
BP 15
EP 32
DI 10.1080/19475705.2010.532971
PG 18
WC Geosciences, Multidisciplinary; Meteorology & Atmospheric Sciences;
Water Resources
SC Geology; Meteorology & Atmospheric Sciences; Water Resources
GA 982QI
UT WOS:000307060100002
ER
PT B
AU Bullen, TD
AF Bullen, Thomas D.
BE Baskaran, M
TI Stable Isotopes of Transition and Post-Transition Metals as Tracers in
Environmental Studies
SO HANDBOOK OF ENVIRONMENTAL ISOTOPE GEOCHEMISTRY, VOLS 1 AND 2
SE Advances in Isotope Geochemisty
LA English
DT Article; Book Chapter
ID IONIZATION MASS-SPECTROMETRY; FE ISOTOPE; CHROMIUM ISOTOPES;
HIGHER-PLANTS; NONTRADITIONAL ISOTOPES; PRECISE DETERMINATION;
ATMOSPHERIC MERCURY; NORTHEASTERN FRANCE; AQUEOUS-SOLUTIONS; CR(VI)
REDUCTION
AB The transition and post-transition metals, which include the elements in Groups 3-12 of the Periodic Table, have a broad range of geological and biological roles as well as industrial applications and thus are widespread in the environment. Interdisciplinary research over the past decade has resulted in a broad understanding of the isotope systematics of this important group of elements and revealed largely unexpected variability in isotope composition for natural materials. Significant kinetic and equilibrium isotope fractionation has been observed for redox sensitive metals such as iron, chromium, copper, molybdenum and mercury, and for metals that are not redox sensitive in nature such as cadmium and zinc. In the environmental sciences, the isotopes are increasingly being used to understand important issues such as tracing of metal contaminant sources and fates, unraveling metal redox cycles, deciphering metal nutrient pathways and cycles, and developing isotope biosignatures that can indicate the role of biological activity in ancient and modern planetary systems.
C1 US Geol Survey, Menlo Pk, CA 94025 USA.
RP Bullen, TD (reprint author), US Geol Survey, MS 420,345 Middlefield Rd,Menlo Pk, Menlo Pk, CA 94025 USA.
EM tbullen@usgs.gov
NR 114
TC 6
Z9 6
U1 0
U2 10
PU SPRINGER-VERLAG BERLIN
PI BERLIN
PA HEIDELBERGER PLATZ 3, D-14197 BERLIN, GERMANY
BN 978-3-642-10636-1
J9 ADV ISOTOP GEOCHEM
PY 2011
BP 177
EP 203
DI 10.1007/978-3-642-10637-8_10
D2 10.1007/978-3-642-10637-8
PG 27
WC Geochemistry & Geophysics
SC Geochemistry & Geophysics
GA BZC58
UT WOS:000301099200010
ER
PT B
AU Kulongoski, JT
Hilton, DR
AF Kulongoski, J. T.
Hilton, D. R.
BE Baskaran, M
TI Applications of Groundwater Helium
SO HANDBOOK OF ENVIRONMENTAL ISOTOPE GEOCHEMISTRY, VOLS 1 AND 2
SE Advances in Isotope Geochemisty
LA English
DT Article; Book Chapter
ID QUADRUPOLE MASS-SPECTROMETER; GREAT ARTESIAN BASIN; NOBLE-GASES;
ISOTOPIC COMPOSITION; SHALLOW GROUNDWATER; RADIOGENIC HELIUM;
TRITIOGENIC HE-3; PANNONIAN BASIN; ISLAND BASALTS; MANTLE FLUIDS
AB Helium abundance and isotope variations have widespread application in groundwater-related studies. This stems from the inert nature of this noble gas and the fact that its two isotopes - helium-3 and helium-4 - have distinct origins and vary widely in different terrestrial reservoirs. These attributes allow He concentrations and He-3/He-4 isotope ratios to be used to recognize and quantify the influence of a number of potential contributors to the total He budget of a groundwater sample. These are atmospheric components, such as air-equilibrated and air-entrained He, as well as terrigenic components, including in situ (aquifer) He, deep crustal and/or mantle He and tritiogenic He-3. Each of these components can be exploited to reveal information on a number of topics, from groundwater chronology, through degassing of the Earth's crust to the role of faults in the transfer of mantle-derived volatiles to the surface. In this review, we present a guide to how groundwater He is collected from aquifer systems and quantitatively measured in the laboratory. We then illustrate the approach of resolving the measured He characteristics into its component structures using assumptions of endmember compositions. This is followed by a discussion of the application of groundwater He to the types of topics mentioned above using case studies from aquifers in California and Australia. Finally, we present possible future research directions involving dissolved He in groundwater.
C1 [Kulongoski, J. T.] US Geol Survey, Calif Water Sci Ctr, San Diego, CA 92101 USA.
[Hilton, D. R.] Univ Calif San Diego, Scripps Inst Oceanog, La Jolla, CA 92093 USA.
RP Kulongoski, JT (reprint author), US Geol Survey, Calif Water Sci Ctr, San Diego, CA 92101 USA.
EM kulongos@usgs.gov; drhilton@ucsd.edu
NR 95
TC 10
Z9 10
U1 1
U2 3
PU SPRINGER-VERLAG BERLIN
PI BERLIN
PA HEIDELBERGER PLATZ 3, D-14197 BERLIN, GERMANY
BN 978-3-642-10636-1
J9 ADV ISOTOP GEOCHEM
PY 2011
BP 285
EP 304
DI 10.1007/978-3-642-10637-8_15
D2 10.1007/978-3-642-10637-8
PG 20
WC Geochemistry & Geophysics
SC Geochemistry & Geophysics
GA BZC58
UT WOS:000301099200015
ER
PT B
AU Zhang, L
Zhang, J
Swarzenski, PW
Liu, Z
AF Zhang, L.
Zhang, J.
Swarzenski, P. W.
Liu, Z.
BE Baskaran, M
TI Radium Isotope Tracers to Evaluate Coastal Ocean Mixing and Residence
Times
SO HANDBOOK OF ENVIRONMENTAL ISOTOPE GEOCHEMISTRY, VOLS 1 AND 2
SE Advances in Isotope Geochemisty
LA English
DT Article; Book Chapter
ID SUBMARINE GROUNDWATER DISCHARGE; EAST-CHINA-SEA; OPTIMUM MULTIPARAMETER
ANALYSIS; BRAZIL-MALVINAS CONFLUENCE; WATER MASS COMPOSITION;
SURFACE-WATER; RIVER ESTUARY; YELLOW SEAS; RA-226; ZONE
AB The identification and provenance of unique coastal water masses is essential in near-shore biogeochemical studies. Water mass mixing and residence times impact water quality and can play a role in the evolution of algal blooms. Such information is thus critical for resource managers who have an interest in understanding the source and fate of contaminants and their eventual fate in the coastal ocean. If mixing is important for quantitatively assessing the amount of exchange, the water residence time or water age is important to assess the rate of this exchange. An understanding of water mass residence times is useful to examine time scales of contaminant discharge and to evaluate transport phenomena.
This review summarizes the scientific significance, measurement approaches, and models to evaluate coastal water mixing and residence times using radium isotopes. Each method or model described here is valid, although each has its own advantages and disadvantages. Examples of mixing among different end-members are given as case studies. All approaches presented here demonstrate the utility of radium isotopes for the evaluation of water mass mixing and residence times.
C1 [Zhang, L.; Zhang, J.] E China Normal Univ, State Key Lab Estuarine & Coastal Res, Shanghai 200062, Peoples R China.
[Swarzenski, P. W.] US Geol Survey, Santa Cruz, CA 95060 USA.
[Liu, Z.] Ocean Univ China, Key Lab Marine Environm & Ecol, Minist Educ, Qingdao 266003, Peoples R China.
RP Zhang, L (reprint author), E China Normal Univ, State Key Lab Estuarine & Coastal Res, 3663 Zhongshan Rd N, Shanghai 200062, Peoples R China.
EM 1979_zhanglei@163.com; jzhang@sklec.ecnu.edu.cn; pswarzen@usgs.gov;
liuzhe_ecnu@yahoo.com.cn
NR 65
TC 3
Z9 3
U1 0
U2 0
PU SPRINGER-VERLAG BERLIN
PI BERLIN
PA HEIDELBERGER PLATZ 3, D-14197 BERLIN, GERMANY
BN 978-3-642-10636-1
J9 ADV ISOTOP GEOCHEM
PY 2011
BP 331
EP 343
DI 10.1007/978-3-642-10637-8_17
D2 10.1007/978-3-642-10637-8
PG 13
WC Geochemistry & Geophysics
SC Geochemistry & Geophysics
GA BZC58
UT WOS:000301099200017
ER
PT B
AU Smith, CG
Swarzenski, PW
Dimova, NT
Zhang, J
AF Smith, C. G.
Swarzenski, P. W.
Dimova, N. T.
Zhang, J.
BE Baskaran, M
TI Natural Radium and Radon Tracers to Quantify Water Exchange and Movement
in Reservoirs
SO HANDBOOK OF ENVIRONMENTAL ISOTOPE GEOCHEMISTRY, VOLS 1 AND 2
SE Advances in Isotope Geochemisty
LA English
DT Article; Book Chapter
ID SUBMARINE GROUNDWATER DISCHARGE; SEA GAS-EXCHANGE; IONIZATION
MASS-SPECTROMETRY; DELAYED COINCIDENCE COUNTER; IN-AIR MONITOR;
SEDIMENT-WATER; COASTAL ZONE; PACIFIC-OCEAN; ENVIRONMENTAL-SAMPLES;
MINERAL COMPONENTS
AB Radon and radium isotopes are routinely used to quantify exchange rates between different hydrologic reservoirs. Since their recognition as oceanic tracers in the 1960s, both radon and radium have been used to examine processes such as air-sea exchange, deep oceanic mixing, benthic inputs, and many others. Recently, the application of radon-222 and the radium-quartet (Ra-223,Ra-224,Ra-226,Ra-228) as coastal tracers has seen a revelation with the growing interest in coastal groundwater dynamics. The enrichment of these isotopes in benthic fluids including groundwater makes both radium and radon ideal tracers of coastal benthic processes (e.g. submarine groundwater discharge). In this chapter we review traditional and recent advances in the application of radon and radium isotopes to understand mixing and exchange between various hydrologic reservoirs, specifically: (1) atmosphere and ocean, (2) deep and shallow oceanic water masses, (3) coastal groundwater/benthic pore waters and surface ocean, and (4) aquifer-lakes. While the isotopes themselves and their distribution in the environment provide qualitative information about the exchange processes, it is mixing/exchange and transport models for these isotopes that provide specific quantitative information about these processes. Brief introductions of these models and mixing parameters are provided for both historical and more recent studies.
C1 [Smith, C. G.] US Geol Survey, St Petersburg, FL 33701 USA.
[Swarzenski, P. W.; Dimova, N. T.] US Geol Survey, UC Santa Cruz, Santa Cruz, CA USA.
[Zhang, J.] E China Normal Univ, State Key Lab Estuarine & Coastal Res, Shanghai 2000062, Peoples R China.
RP Smith, CG (reprint author), US Geol Survey, 600 4th St S, St Petersburg, FL 33701 USA.
EM cgsmith@usgs.gov; pswarzen@usgs.gov; ndimova@usgs.gov;
jzhang@sklec.ecnu.edu.cn
NR 157
TC 5
Z9 5
U1 0
U2 1
PU SPRINGER-VERLAG BERLIN
PI BERLIN
PA HEIDELBERGER PLATZ 3, D-14197 BERLIN, GERMANY
BN 978-3-642-10636-1
J9 ADV ISOTOP GEOCHEM
PY 2011
BP 345
EP 365
DI 10.1007/978-3-642-10637-8_18
D2 10.1007/978-3-642-10637-8
PG 21
WC Geochemistry & Geophysics
SC Geochemistry & Geophysics
GA BZC58
UT WOS:000301099200018
ER
PT B
AU Sturchio, NC
Bohlke, JK
Gu, BH
Hatzinger, PB
Jackson, WA
AF Sturchio, Neil C.
Boehlke, John Karl
Gu, Baohua
Hatzinger, Paul B.
Jackson, W. Andrew
BE Baskaran, M
TI Isotopic Tracing of Perchlorate in the Environment
SO HANDBOOK OF ENVIRONMENTAL ISOTOPE GEOCHEMISTRY, VOLS 1 AND 2
SE Advances in Isotope Geochemisty
LA English
DT Article; Book Chapter
ID UNITED-STATES; NATURAL PERCHLORATE; ATACAMA DESERT; NITRATE DEPOSITS;
OZONE OXIDATION; NORTH-AMERICA; HIGH-PLAINS; NEW-MEXICO; CHLORINE;
FRACTIONATION
AB Isotopic measurements can be used for tracing the sources and behavior of environmental contaminants. Perchlorate (ClO4-) has been detected widely in groundwater, soils, fertilizers, plants, milk, and human urine since 1997, when improved analytical methods for analyzing ClO4- concentration became available for routine use. Perchlorate ingestion poses a risk to human health because of its interference with thyroidal hormone production. Consequently, methods for isotopic analysis of ClO4- have been developed and applied to assist evaluation of the origin and migration of this common contaminant. Isotopic data are now available for stable isotopes of oxygen and chlorine, as well as Cl-36 isotopic abundances, in ClO4- samples from a variety of natural and synthetic sources. These isotopic data provide a basis for distinguishing sources of ClO4- found in the environment, and for understanding the origin of natural ClO4-. In addition, the isotope effects of microbial ClO4- reduction have been measured in laboratory and field experiments, providing a tool for assessing ClO4- attenuation in the environment. Isotopic data have been used successfully in some areas for identifying major sources of ClO4- contamination in drinking water supplies. Questions about the origin and global biogeochemical cycle of natural ClO4- remain to be addressed; such work would benefit from the development of methods for preparation and isotopic analysis of ClO4- in samples with low concentrations and complex matrices.
C1 [Sturchio, Neil C.] Univ Illinois, Chicago, IL 60607 USA.
[Boehlke, John Karl] US Geol Survey, Reston, VA 20192 USA.
[Gu, Baohua] Oak Ridge Natl Lab, Oak Ridge, TN 37831 USA.
[Hatzinger, Paul B.] Shaw Environm Inc, Lawrenceville, NJ 08648 USA.
[Jackson, W. Andrew] Texas Tech Univ, Lubbock, TX 79409 USA.
RP Sturchio, NC (reprint author), Univ Illinois, Chicago, IL 60607 USA.
EM sturchio@uic.edu; jkbohlke@usgs.gov
NR 73
TC 4
Z9 5
U1 3
U2 5
PU SPRINGER-VERLAG BERLIN
PI BERLIN
PA HEIDELBERGER PLATZ 3, D-14197 BERLIN, GERMANY
BN 978-3-642-10636-1
J9 ADV ISOTOP GEOCHEM
PY 2011
BP 437
EP 452
DI 10.1007/978-3-642-10637-8_22
D2 10.1007/978-3-642-10637-8
PG 16
WC Geochemistry & Geophysics
SC Geochemistry & Geophysics
GA BZC58
UT WOS:000301099200022
ER
PT S
AU Ellsworth, WL
Malin, PE
AF Ellsworth, William L.
Malin, Peter E.
BE Fagereng, A
Toy, VG
Rowland, JV
TI Deep rock damage in the San Andreas Fault revealed by P- and S-type
fault-zone-guided waves
SO GEOLOGY OF THE EARTHQUAKE SOURCE: A VOLUME IN HONOUR OF RICK SIBSON
SE Geological Society Special Publication
LA English
DT Article; Book Chapter
ID 2004 PARKFIELD EARTHQUAKE; TRAPPING STRUCTURE; CENTRAL CALIFORNIA;
SEISMIC-WAVES; SLIP; SAFOD; SYSTEM; ATTENUATION; VELOCITY; LANDERS
AB Damage to fault-zone rocks during fault slip results in the formation of a channel of low seismic-wave velocities. Within such channels guided seismic waves, denoted by F-g, can propagate. Here we show with core samples, well logs and F-g-waves that such a channel is crossed by the SAFOD (San Andreas Fault Observatory at Depth) borehole at a depth of 2.7 km near Parkfield, California, USA. This laterally extensive channel extends downwards to at least half way through the seismogenic crust, more than about 7 km. The channel supports not only the previously recognized Love-type- (F-L) and Rayleigh-type- (F-R) guided waves, but also a new fault-guided wave, which we name F-Phi. As recorded 2.7 km underground, F-Phi is normally dispersed, ends in an Airy phase, and arrives between the P- and S-waves. Modelling shows that F-Phi travels as a leaky mode within the core of the fault zone. Combined with the drill core samples, well logs and the two other types of guided waves, F-Phi at SAFOD reveals a zone of profound, deep, rock damage. Originating from damage accumulated over the recent history of fault movement, we suggest it is maintained either by fracturing near the slip surface of earthquakes, such as the 1857 Fort Tejon M 7.9, or is an unexplained part of the fault-creep process known to be active at this site.
C1 [Ellsworth, William L.] US Geol Survey, Menlo Pk, CA 94025 USA.
[Malin, Peter E.] Univ Auckland, Inst Earth Sci & Engn, Auckland 1142, New Zealand.
RP Ellsworth, WL (reprint author), US Geol Survey, 345 Middlefield Rd,MS-977, Menlo Pk, CA 94025 USA.
EM ellsworth@usgs.gov
NR 55
TC 12
Z9 12
U1 0
U2 1
PU GEOLOGICAL SOC PUBLISHING HOUSE
PI BATH
PA UNIT 7, BRASSMILL ENTERPRISE CTR, BRASSMILL LANE, BATH BA1 3JN, AVON,
ENGLAND
SN 0305-8719
BN 978-1-86239-337-0
J9 GEOL SOC SPEC PUBL
JI Geol. Soc. Spec. Publ.
PY 2011
VL 359
BP 39
EP 53
DI 10.1144/SP359.3
PG 15
WC Geology
SC Geology
GA BAP81
UT WOS:000305142000004
ER
PT B
AU Moniz, LJ
Nichols, JD
Nichols, JM
Cooch, EG
Pecora, LM
AF Moniz, L. J.
Nichols, J. D.
Nichols, J. M.
Cooch, E. G.
Pecora, L. M.
BE Dehmer, M
EmmertStreib, F
Mehler, A
TI Inferences About Coupling from Ecological Surveillance Monitoring:
Approaches Based on Nonlinear Dynamics and Information Theory
SO TOWARDS AN INFORMATION THEORY OF COMPLEX NETWORKS: STATISTICAL METHODS
AND APPLICATIONS
LA English
DT Article; Book Chapter
DE 37M10 Time-Series Analysis; 37M99 Computational Methods; 37N99
Application of Dynamical Systems; 92D40 Ecology
ID RECURRENCE QUANTIFICATION ANALYSIS; TIME-SERIES ANALYSIS;
POPULATION-DYNAMICS; SPATIOTEMPORAL SYSTEMS; STRANGE ATTRACTORS; MUTUAL
PREDICTION; DELAY EMBEDDINGS; FORCED SYSTEMS; NOISY WORLD; MODELS
AB Some monitoring programs for ecological resources are developed as components of larger science or management programs and are thus guided by a priori hypotheses. More commonly, ecological monitoring programs are initiated for the purpose of surveillance with no a priori hypotheses in mind. No conceptual framework currently exists to guide the development of surveillance monitoring programs, resulting in substantial debate about program design. We view surveillance monitoring programs as providing information about system dynamics and focus on methods for extracting such information from time series of monitoring data. We briefly describe methods from the general field of nonlinear dynamics that we believe may be useful in extracting information about system dynamics. In looking at the system as a network of locations or components, we emphasize methods for assessing coupling between system components for use in understanding system dynamics and interactions and in detecting changes in system dynamics. More specifically, these methods hold promise for such ecological problems as identifying indicator species, developing informative spatial monitoring designs, detecting ecosystem change and damage, and investigating such topics as population synchrony, species interactions, and environmental drivers. We believe that these ideas and methods provide a useful conceptual framework for surveillance monitoring and can be used with model systems to draw inferences about the design of surveillance monitoring programs. In addition, some of the current methods should be useful with some actual ecological monitoring data, and methodological extensions and modifications should increase the applicability of these approaches to additional sources of actual ecological data.
C1 [Moniz, L. J.] Johns Hopkins Univ, Appl Phys Lab, Laurel, MD 20723 USA.
[Nichols, J. D.] US Geol Survey, Patuxent Wildlife Res Ctr, Laurel, MD 20708 USA.
[Nichols, J. M.] USN, Res Lab, Div Opt Sci, Washington, DC 20375 USA.
[Cooch, E. G.] Cornell Univ, Dept Nat Resources, Ithaca, NY 14853 USA.
RP Moniz, LJ (reprint author), Johns Hopkins Univ, Appl Phys Lab, 11100 Johns Hopkins Rd, Laurel, MD 20723 USA.
EM Linda.Moniz@jhuapl.edu; jnichols@usgs.gov;
jonathan.nichols@nrl.navy.mil; evan.cooch@cornell.edu;
pecora@anvil.nrl.navy.mil
NR 105
TC 0
Z9 0
U1 0
U2 5
PU BIRKHAUSER BOSTON
PI CAMBRIDGE
PA 675 MASSACHUSETTS AVE, CAMBRIDGE, MA 02139-2333 USA
BN 978-0-8176-4903-6
PY 2011
BP 169
EP 198
DI 10.1007/978-0-8176-4904-3_8
D2 10.1007/978-0-8176-4904-3
PG 30
WC Computer Science, Theory & Methods; Statistics & Probability
SC Computer Science; Mathematics
GA BYL98
UT WOS:000299298200008
ER
PT B
AU Kassen, M
Williams, JE
AF Kassen, Melinda
Williams, Jack E.
BE Kenney, DS
Wilkinson, R
TI Energy, water and the natural environment
SO WATER-ENERGY NEXUS IN THE AMERICAN WEST
LA English
DT Editorial Material; Book Chapter
ID WESTSLOPE CUTTHROAT TROUT; CONSERVATION STATUS; FRESH-WATER;
UNITED-STATES; FLOW REGIME; FISH; INVASION; CANADA
C1 [Williams, Jack E.] So Oregon Univ, Ashland, OR USA.
[Williams, Jack E.] Boise Natl Forest, Boise, ID USA.
[Williams, Jack E.] Univ Calif Davis, US Fish & Wildlife Serv, Davis, CA USA.
NR 36
TC 0
Z9 0
U1 0
U2 0
PU EDWARD ELGAR PUBLISHING LTD
PI CHELTENHAM
PA GLENSANDA HOUSE, MONTPELLIER PARADE, CHELTENHAM GL50 1UA, GLOS, ENGLAND
BN 978-1-84980-936-8
PY 2011
BP 18
EP 30
PG 13
WC Geosciences, Multidisciplinary; Water Resources
SC Geology; Water Resources
GA BYH99
UT WOS:000298876200003
ER
PT S
AU Conway, SJ
Balme, MR
Murray, JB
Towner, MC
Okubo, CH
Grindrod, PM
AF Conway, Susan J.
Balme, Matthew R.
Murray, John B.
Towner, Martin C.
Okubo, Chris H.
Grindrod, Peter M.
BE Balme, MR
Bargery, AS
Gallagher, CJ
Gupta, S
TI The indication of Martian gully formation processes by slope-area
analysis
SO MARTIAN GEOMORPHOLOGY
SE Geological Society Special Publication
LA English
DT Article; Book Chapter
ID DIGITAL ELEVATION MODELS; POTENTIAL FORMATION MECHANISMS; SURFACE GROUND
ICE; DEBRIS FLOWS; LIQUID WATER; TOPOGRAPHIC SIGNATURE; HILLSLOPE
PROCESSES; CHANNEL INITIATION; LANDSCAPE RESPONSE; MARS IMPLICATIONS
AB The formation process of recent gullies on Mars is currently under debate. This study aims to discriminate between the proposed formation processes - pure water flow, debris flow and dry mass wasting - through the application of geomorphological indices commonly used in terrestrial geomorphology. High-resolution digital elevation models (DEMs) of Earth and Mars were used to evaluate the drainage characteristics of small slope sections. Data from Earth were used to validate the hillslope, debris-flow and alluvial process domains previously found for large fluvial catchments on Earth, and these domains were applied to gullied and ungullied slopes on Mars. In accordance with other studies, our results indicate that debris flow is one of the main processes forming the Martian gullies that were being examined. The source of the water is predominantly distributed surface melting, not an underground aquifer. Evidence is also presented indicating that other processes may have shaped Martian crater slopes, such as ice-assisted creep and solifluction, in agreement with the proposed recent Martian glacial and periglacial climate. Our results suggest that, within impact craters, different processes are acting on differently oriented slopes, but further work is needed to investigate the potential link between these observations and changes in Martian climate.
C1 [Conway, Susan J.; Balme, Matthew R.; Murray, John B.] Open Univ, Milton Keynes MK7 6AA, Bucks, England.
[Towner, Martin C.] Univ London Imperial Coll Sci Technol & Med, Dept Earth Sci & Engn, Impacts & Astromat Res Ctr, London SW7 2AZ, England.
[Okubo, Chris H.] US Geol Survey, Astrogeol Sci Ctr, Flagstaff, AZ 86001 USA.
[Grindrod, Peter M.] UCL, Dept Earth Sci, London WC1E 6BT, England.
RP Conway, SJ (reprint author), Univ Nantes, CNRS UMR 6112, Lab Planetol & Geodynam, 2 Rue Houssiniere,BP 92208, F-44322 Nantes, France.
EM susan.conway@univ-nantes.fr
RI Grindrod, Peter/F-5819-2011;
OI Grindrod, Peter/0000-0002-0934-5131; Conway, Susan/0000-0002-0577-2312;
Balme, Matthew/0000-0001-5871-7475
NR 98
TC 21
Z9 21
U1 0
U2 7
PU GEOLOGICAL SOC PUBLISHING HOUSE
PI BATH
PA UNIT 7, BRASSMILL ENTERPRISE CTR, BRASSMILL LANE, BATH BA1 3JN, AVON,
ENGLAND
SN 0305-8719
BN 978-1-86239-330-1
J9 GEOL SOC SPEC PUBL
JI Geol. Soc. Spec. Publ.
PY 2011
VL 356
BP 171
EP 201
DI 10.1144/SP356.10
D2 10.1144/SP356.0
PG 31
WC Geology
SC Geology
GA BAD27
UT WOS:000303838600011
ER
PT J
AU Menghini, RP
Coelho, C
Rovai, AS
Cunha-Lignon, M
Schaeffer-Novelli, Y
Cintron, G
AF Menghini, R. P.
Coelho-, C., Jr.
Rovai, A. S.
Cunha-Lignon, M.
Schaeffer-Novelli, Y.
Cintron, G.
TI Massive mortality of mangrove forests in Southeast Brazil (Baixada
Santista, State of Sao Paulo) as a result of harboring activities
SO JOURNAL OF COASTAL RESEARCH
LA English
DT Article; Proceedings Paper
CT 11th International Coastal Symposium (ICS)
CY MAY 09-13, 2011
CL Szczecin, POLAND
SP Univ Szczecin, Inst Marine & Coastal Sci, Coastal Educ & Res Fdn, Univ Szczecinski (US), Cztowiek Nauka Srodowisko (CNS), ZMGM, Reg Dyrekcja Ochrony Srodowiska, Esri, Springer, Lotos, GA2 Syst, World Sci, Helmholtz-Zentrum Geesthacht, Nfosigm, Urzad Marszalkowski Wojewodztwa Zachodniopomorskiego, Wojewodzki Fundusz Ochrony Srodowiska I Gospodarki Wodnej W Gdansku
DE Anthropogenic impact; Natural recovery; Structural characterization
ID WORLD
AB R. P. Menghini, C. Coelho-Jr, A. S. Rovai, M. Cunha-Lignon, Y. Schaeffer-Novelli and G. Cintron, 2011. Massive mortality of mangrove forests in Southeast Brazil (Barnabe Island, Baixada Santista, State of Silo Paulo) as a result of harboring activities. Journal of Coastal Research, SI 64 (Proceedings of the 11th International Coastal Symposium), 1793 - 1797. Szczecin, Poland, ISBN 0749-0208.
Since the fifties the Baixada Santista's landscape has been intensively modified by spreading unplanned and illegal human settlements, mainly by industrial and harboring activities. On 3rd September 1998, a portion of the mangrove forests that surround the Barnabe Island, Santos, State of Silo Paulo, Brazil (23 degrees 55'23"S; 46 degrees 19'28"W) was affected by a fire due to the accidental spillage of a flammable chemical substance called dicyclopentadiene (DCPD). The goals of the current study were to determine the impacts as well as to assess the initial natural recovery of this mangrove forest. Six permanent plots, were established. Three of them were used to gather data from the adult individuals that survived after spillage (M1, M2 and M3) and the others to investigate the recruitments presents in the natural recovery (RN1, RN2 e RN3) using standardized methodology. Among the adult individuals, Laguncularia racemosa was the dominant species. The densities of dead stems for these quadrants, especially for M1 and M3, were very high reaching 65.39% and 48.97%, respectively. The RN1 and RN2 plots were also dominated by L. racemosa with 100% of the stems alive. RN3 was dominated by Avicennia schaueriana but showed a decrease in the proportion of alive stems (89.09%). The magnitude of the accident is evidenced considering half (M3) or more (M1) out of the total number of stems were found dead. Yet simple and inexpensive, the methodology applied in the current study showed to be an effective tool to evaluate impacts over mangrove stands. Finally, we recommend that Baixada Santista's integrated coastal management process must incorporate long-term mangrove monitoring.
C1 [Menghini, R. P.; Coelho-, C., Jr.; Rovai, A. S.; Cunha-Lignon, M.; Schaeffer-Novelli, Y.] Inst BiomaBrasil IBB, BR-05434060 Sao Paulo, Brazil.
[Menghini, R. P.] Univ Paulista UNIP, BR-01533000 Sao Paulo, Brazil.
[Coelho-, C., Jr.] Univ Pernambuco UPE, BR-52041050 Recife, PE, Brazil.
[Rovai, A. S.] Univ Fed Santa Catarina UFSC, BR-88040900 Florianopolis, SC, Brazil.
[Cunha-Lignon, M.] Natl Inst Space Res INPE, BR-12227010 Sao Jose Dos Campos, SP, Brazil.
[Cunha-Lignon, M.] Univ Libre Bruxelles ULB Brussels, B-1050 Brussels, Belgium.
[Cintron, G.] US Fish & Wildlife Serv, Arlington, VA 22203 USA.
RP Menghini, RP (reprint author), Inst BiomaBrasil IBB, Rua Laboriosa 80, BR-05434060 Sao Paulo, Brazil.
EM ricardo.menghini@biomabrasil.org; clemente.coelhojr@biomabrasil.org;
rovai@ccb.ufsc.br; marilia.cunha@biomabrasil.org;
yara.novelli@biomabrasil.org; gil_cintron@fws.gov
RI Cunha Lignon, Marilia/B-8953-2012
FU Conselho Nacional de Desenvolvimento Cientifico e Tecnologico - CNPq -
Brazil [140090/2005-3]
FX We would like to thank Mr. Luis Oshiro, manager of the Odfjell Terminals
facility, and their staff for providing assistance during the mangrove
surveys conducted in the Santos Estuary (Brazil). This study was
undertaken with the financial supports of the Conselho Nacional de
Desenvolvimento Cientifico e Tecnologico - CNPq - Brazil (Process
140090/2005-3).
NR 19
TC 2
Z9 2
U1 2
U2 10
PU COASTAL EDUCATION & RESEARCH FOUNDATION
PI LAWRENCE
PA 810 EAST 10TH STREET, LAWRENCE, KS 66044 USA
SN 0749-0208
EI 1551-5036
J9 J COASTAL RES
JI J. Coast. Res.
PY 2011
SI 64
BP 1793
EP 1797
PN 2
PG 5
WC Environmental Sciences; Geography, Physical; Geosciences,
Multidisciplinary
SC Environmental Sciences & Ecology; Physical Geography; Geology
GA 926IR
UT WOS:000302825000155
ER
PT J
AU Cunha-Lignon, M
Kampel, M
Menghini, RP
Schaeffer-Novelli, Y
Cintron, G
Dahdouh-Guebas, F
AF Cunha-Lignon, M.
Kampel, M.
Menghini, R. P.
Schaeffer-Novelli, Y.
Cintron, G.
Dahdouh-Guebas, F.
TI Mangrove Forests Submitted to Depositional Processes and Salinity
Variation Investigated using satellite images and vegetation structure
surveys
SO JOURNAL OF COASTAL RESEARCH
LA English
DT Article; Proceedings Paper
CT 11th International Coastal Symposium (ICS)
CY MAY 09-13, 2011
CL Szczecin, POLAND
SP Univ Szczecin, Inst Marine & Coastal Sci, Coastal Educ & Res Fdn, Univ Szczecinski (US), Cztowiek Nauka Srodowisko (CNS), ZMGM, Reg Dyrekcja Ochrony Srodowiska, Esri, Springer, Lotos, GA2 Syst, World Sci, Helmholtz-Zentrum Geesthacht, Nfosigm, Urzad Marszalkowski Wojewodztwa Zachodniopomorskiego, Wojewodzki Fundusz Ochrony Srodowiska I Gospodarki Wodnej W Gdansku
DE monitoring; remote sensing; permanent plots
ID CLIMATE-CHANGE; THREATS
AB Cunha-Lignon, M., Kampel, M., Menghini, R.P., Schaeffer-Novelli, Y., Cintron, G. and Dandouh-Guebas, F. 2011. Mangrove Forests Submitted to Depositional Processes and Salinity Variation Investigated using satellite images and vegetation structure surveys. Journal of Coastal Research, SI 64 (Proceedings of the 11th International Coastal Symposium), 344 - 348. Szczecin, Poland, ISSN 0749-0208.
The current paper examines the growth and spatio-temporal variation of mangrove forests in response to depositional processes and different salinity conditions. Data from mangrove vegetation structure collected at permanent plots and satellite images were used. In the northern sector important environmental changes occurred due to an artificial channel producing modifications in salinity. The southern sector is considered the best conserved mangrove area along the coast of Sao Paulo State, Brazil. Landsat TM5 images from 1997 and 2010 were processed using Geographical Information Systems. Supervised classifications complemented by visual interpretations and ground truth were used to map mangrove areas in both periods. In each permanent plot, all plants were identified and tree diameter, height, and incidence of associated species were recorded. Mean height, basal area dominance, and stem density were also assessed. In the southern sector of the study area, digital image analysis revealed shoreline progradation and mangrove establishment. These sites have demonstrated both vegetation growth and extension. In the northern sector, the satellite image analysis revealed an increase of depositional areas. An important number of associated freshwater plants were observed, inhibiting the establishment of mangrove seedlings or growth of saplings. Despite the high sedimentation rate, which enables mangrove colonization, the low salinity exerts indirect negative influence on mangrove development, considering that it creates good conditions to macrophytes reproduction. Coastal planning requires that the spatial differences be recognized as unique sub-systems due to the hydrodynamic complexity. Both on-the-ground monitoring of the vegetation structure and space-borne remote sensing are important tools to support coastal zone management.
C1 [Cunha-Lignon, M.; Kampel, M.] Natl Inst Space Res INPE, BR-12227010 Sao Jose Dos Campos, SP, Brazil.
[Cunha-Lignon, M.; Menghini, R. P.; Schaeffer-Novelli, Y.] Inst BiomaBrasil IBB, BR-05434060 Sao Paulo, Brazil.
[Cunha-Lignon, M.; Dahdouh-Guebas, F.] Univ Libre Bruxelles, B-1050 Brussels, Belgium.
[Menghini, R. P.] Univ Paulista UNIP, BR-05347020 Sao Paulo, Brazil.
[Cintron, G.] US Fish & Wildlife Serv, Arlington, VA 22203 USA.
[Dahdouh-Guebas, F.] Vrije Univ Brussels, B-1050 Brussels, Belgium.
RP Cunha-Lignon, M (reprint author), Natl Inst Space Res INPE, BR-12227010 Sao Jose Dos Campos, SP, Brazil.
EM marilia@dsr.inpe.br; ricardo.menghini@biomabrasil.org;
yara.novelli@biomabrasil.org; gil_cintron@fws.gov; fdandouh@ulb.ac.be
RI Cunha Lignon, Marilia/B-8953-2012
NR 14
TC 8
Z9 8
U1 2
U2 14
PU COASTAL EDUCATION & RESEARCH FOUNDATION
PI LAWRENCE
PA 810 EAST 10TH STREET, LAWRENCE, KS 66044 USA
SN 0749-0208
EI 1551-5036
J9 J COASTAL RES
JI J. Coast. Res.
PY 2011
SI 64
BP 344
EP 348
PN 1
PG 5
WC Environmental Sciences; Geography, Physical; Geosciences,
Multidisciplinary
SC Environmental Sciences & Ecology; Physical Geography; Geology
GA 926IQ
UT WOS:000302824900071
ER
PT J
AU Cunha-Lignon, M
Coelho, C
Almeida, R
Menghini, RP
Schaeffer-Novelli, Y
Cintron, G
Dahdouh-Guebas, F
AF Cunha-Lignon, M.
Coelho, C., Jr.
Almeida, R.
Menghini, R. P.
Schaeffer-Novelli, Y.
Cintron, G.
Dahdouh-Guebas, F.
TI Characterisation of mangrove forest types in view of conservation and
management: a review of mangals at the Cananeia region, Sao Paulo State,
Brazil
SO JOURNAL OF COASTAL RESEARCH
LA English
DT Article; Proceedings Paper
CT 11th International Coastal Symposium (ICS)
CY MAY 09-13, 2011
CL Szczecin, POLAND
SP Univ Szczecin, Inst Marine & Coastal Sci, Coastal Educ & Res Fdn, Univ Szczecinski (US), Cztowiek Nauka Srodowisko (CNS), ZMGM, Reg Dyrekcja Ochrony Srodowiska, Esri, Springer, Lotos, GA2 Syst, World Sci, Helmholtz-Zentrum Geesthacht, Nfosigm, Urzad Marszalkowski Wojewodztwa Zachodniopomorskiego, Wojewodzki Fundusz Ochrony Srodowiska I Gospodarki Wodnej W Gdansku
DE dynamics; self-organisation; management
ID VARIABILITY; COAST
AB M. Cunha-Lignon, C. Coelho Jr., R. Almeida, R.P. Menghini, Y. Schaeffer-Novelli, G. Cintron and F. Dahdouh-Guebas, 2011. Characterisation of mangrove forest types in view of conservation and management: a review of mangals at the Canandia region, Sao Paulo State, Brazil. Journal of Coastal Research, SE 64 (Proceedings of the 11th International Coastal Symposium), 349 - 353. Szczecin, Poland, ISSN 0749-0208.
Wetlands, including mangroves, perform diverse functions, besides the production of goods and services on an ecosystem and landscape scale. The combination of functions, goods and ecological services has a fundamental importance for society. The study of physiographic types is intended to help in dealing with and understanding the function of a complex system. Complex systems are those that share four attributes: diversity of constituents, interdependence between parts, connectedness and adaptation. This study was carried out in the Cananeia region, located in the southern coast of the Sao Paulo State (25 S), Brazil. Data from the 1980's to 2009 on the structural development of mangrove forests of two physiographic types, fringe and basin, were analyzed to discern patterns of spatial and structural organization. The fringe forests studied in the region presented a predominance of Rhizophora mangle and high structural development due to the high inundation frequency in depositionally stable sites. Fringe forests, located in progradation areas with low tidal energy, were dominated by Laguncularia racemosa with low structural development. The basin forests are dominated by R. mangle or L. racemosa, presenting reduced structural development in function of the lower inundation frequency, a predominantly sandy substrate and low salinity. But some basin forests dominated by Avicennia schaueriana were better developed reflecting the growth characteristic of this species. The results shown here highlight the large variations in the quality and intensity of forcing functions and the structural and functional diversity allowed by the plasticity of the species involved and their capacity to interact and adjust to the environment in which they develop.
C1 [Cunha-Lignon, M.] Natl Inst Space Res INPE, BR-12227010 Sao Jose Dos Campos, SP, Brazil.
[Cunha-Lignon, M.; Coelho, C., Jr.; Almeida, R.; Menghini, R. P.; Schaeffer-Novelli, Y.] Inst BiomaBrasil IBB, BR-52041050 Recife, PE, Brazil.
[Cunha-Lignon, M.] Univ Libre Brussels, B-1050 Brussels, Belgium.
[Coelho, C., Jr.] Univ Pernambuco UPE, BR-52041050 Recife, PE, Brazil.
[Almeida, R.] UFRB, BR-44380000 Cruz Das Almas, BA, Brazil.
[Menghini, R. P.] Univ Paulista UNIP, BR-05347020 Sao Paulo, Brazil.
[Cintron, G.] US Fish & Wildlife Serv, Arlington, VA 22203 USA.
[Dahdouh-Guebas, F.] Vrije Univ Brussel, B-1050 Brussels, Belgium.
RP Cunha-Lignon, M (reprint author), Natl Inst Space Res INPE, BR-12227010 Sao Jose Dos Campos, SP, Brazil.
EM marilia@dsr.inpe.br; clemente.coelhojr@biomabrasil.org;
renato.almeida@biomabrasil.org; ricardo.menghini@biomabrasil.org;
yara.novelli@biomabrasil.org; gil_cintron@fws.gov; fdandouh@ulb.ac.be
RI Cunha Lignon, Marilia/B-8953-2012
NR 25
TC 8
Z9 8
U1 2
U2 23
PU COASTAL EDUCATION & RESEARCH FOUNDATION
PI LAWRENCE
PA 810 EAST 10TH STREET, LAWRENCE, KS 66044 USA
SN 0749-0208
J9 J COASTAL RES
JI J. Coast. Res.
PY 2011
SI 64
BP 349
EP 353
PN 1
PG 5
WC Environmental Sciences; Geography, Physical; Geosciences,
Multidisciplinary
SC Environmental Sciences & Ecology; Physical Geography; Geology
GA 926IQ
UT WOS:000302824900072
ER
PT J
AU Brumback, WE
Cairns, S
Sperduto, MB
Fyler, CW
AF Brumback, William E.
Cairns, Sara
Sperduto, Molly B.
Fyler, Carol W.
TI Response of an Isotria medeoloides Population to Canopy Thinning
SO NORTHEASTERN NATURALIST
LA English
DT Article
AB Isotria medeoloides (Small Whorled Pogonia) is a globally rare woodland orchid. Observed population declines in this species may be related to decreased light availability resulting from forest maturation. In East Alton, NH, a population of Small Whorled Pogonia was partitioned into two groups, with one left as a control and the other subjected to canopy-reduction management. The removal of all shrubs and 25% of the tree basal area approximately doubled light transmission to the managed group. The number of stems and seed capsules significantly increased in this group relative to tie control group. While this was not a replicated experiment, our observations suggest that canopy thinning may help promote the long-term conservation of this federally threatened species.
C1 [Sperduto, Molly B.] US Fish & Wildlife Serv, Concord, NH 03301 USA.
[Brumback, William E.; Fyler, Carol W.] New England Wild Flower Soc, Framingham, MA 01701 USA.
[Cairns, Sara] DRED, New Hampshire Nat Heritage Bur, Concord, NH 03302 USA.
RP Sperduto, MB (reprint author), US Fish & Wildlife Serv, 70 Commercial St,Suite 300, Concord, NH 03301 USA.
EM molly_sperduto@fws.gov
FU Harold Whitworth Pierce Charitable Trust; US Fish and Wildlife Service;
New England Wild Flower Society; New Hampshire Natural Heritage Bureau
FX Many thanks to Peter Farrell, New England Forestry Consultants, Inc. for
tree removal, and to Tom Hoopes and the Town of Alton, NH for granting
permission for the project. We thank Charles D. Canham and Lynn Schnurr,
Cary Institute of Ecosystem Studies, for their analyses of hemispherical
photography. We also thank Susi von Oettingen, Jessica Korecki, Danielle
Ogurcak, and Chris Mattrick for their help, guidance, and support.
Support for this project came from the Harold Whitworth Pierce
Charitable Trust, the US Fish and Wildlife Service, the New England Wild
Flower Society, and the New Hampshire Natural Heritage Bureau.
NR 9
TC 3
Z9 3
U1 0
U2 8
PU HUMBOLDT FIELD RESEARCH INST
PI STEUBEN
PA PO BOX 9, STEUBEN, ME 04680-0009 USA
SN 1092-6194
J9 NORTHEAST NAT
JI Northeast. Nat
PY 2011
VL 18
IS 2
BP 185
EP 196
PG 12
WC Biodiversity Conservation; Ecology
SC Biodiversity & Conservation; Environmental Sciences & Ecology
GA 926KJ
UT WOS:000302829600005
ER
PT J
AU McCarthy, KP
DeStefano, S
AF McCarthy, Kyle P.
DeStefano, Stephen
TI Common Loon Nest Defense Against an American Mink
SO NORTHEASTERN NATURALIST
LA English
DT Article
AB We describe a successful nest defense strategy of an adult Gavia immer (Common Loon) during an attempted predation event by a Nevison vison (American Mink) at Umbagog National Wildlife Refuge, NH. It is suspected that mink occasionally depredate loon nests, but defense strategies have not been described previously.
C1 [McCarthy, Kyle P.; DeStefano, Stephen] Univ Massachusetts, Massachusetts Cooperat Fish & Wildlife Res Unit, US Geol Survey, Amherst, MA 01003 USA.
RP McCarthy, KP (reprint author), Univ Massachusetts, Massachusetts Cooperat Fish & Wildlife Res Unit, US Geol Survey, 160 Holdsworth Way, Amherst, MA 01003 USA.
EM mccarthy@udel.edu
FU US Fish and Wildlife Service; Umbagog National Wild life Refuge
FX We thank the US Fish and Wildlife Service and Umbagog National Wild life
Refuge for their funding and support. We also thank our field
assistants, Jennifer McCarthy and Kevin Rogers, who made it possible to
record this rarely described event. Useful comments and suggestions were
received from two anonymous reviewers and manuscript editor Thomas J.
Maier.
NR 13
TC 1
Z9 1
U1 2
U2 7
PU HUMBOLDT FIELD RESEARCH INST
PI STEUBEN
PA PO BOX 9, STEUBEN, ME 04680-0009 USA
SN 1092-6194
J9 NORTHEAST NAT
JI Northeast. Nat
PY 2011
VL 18
IS 2
BP 247
EP 249
PG 3
WC Biodiversity Conservation; Ecology
SC Biodiversity & Conservation; Environmental Sciences & Ecology
GA 926KJ
UT WOS:000302829600012
ER
PT J
AU Mech, LD
AF Mech, L. David
TI Minnesota Wolf Ear Lengths as Possible Indicators of Taxonomic
Differences
SO NORTHEASTERN NATURALIST
LA English
DT Article
ID GREAT-LAKES REGION; MITOCHONDRIAL-DNA; GRAY WOLF; BODY-MASS; WOLVES;
POPULATIONS; HISTORY
AB Genetic findings suggest that 2 types of wolves, Canis. lupus (Gray Wolf) and C. lycaon (Eastern Wolf), and/or their hybrids occupy Minnesota (MN), and this study examines adult wolf ear lengths as a possible distinguisher between these two. Photographic evidence suggested that the Eastern Wolf possesses proportionately longer ears than Gray Wolves. Ear lengths from 22 northwestern MN wolves from the early 1970s and 22 Alaskan wolves were used to represent Gray Wolves, and the greatest length of the sample (12.8 cm) was used as the least length to demarcate Eastern Wolf from Gray Wolf influence in the samples. Twenty-three percent of 112 adult wolves from Algonquin Park in eastern Ontario and 30% of 106 recent adult wolves in northeastern MN possessed ears >12.8 cm. The northeastern MN sample differed significantly from that of current and past northwestern MN wolves. Ear-lengths of wolves in the eastern half of the northeastern MN wolf population were significantly longer than those in the western half of that study area, even though the mean distance between the 2 areas was only 40 km, and the mean length of my 2004-2009 sample was significantly longer than that of 1999-2003. These findings support the hypothesis that Eastern Wolves tend to possess longer ears than do Gray Wolves and suggest a dynamic hybridization process is still underway in MN.
C1 [Mech, L. David] Prairie & No Wildlife Res Ctr, US Geol Survey, Jamestown, ND 58401 USA.
RP Mech, LD (reprint author), Univ Minnesota, US Geol Survey, Raptor Ctr, 1920 Fitch Ave, St Paul, MN 55108 USA.
EM mechx002@umn.edu
FU US Geological Survey; US Forest Service North Central Research Station
FX This study was supported by the US Geological Survey and the US Forest
Service North Central Research Station. I thank J. Hart and L.G. Butler
for collecting ear-lengths from western MN and Alaskan wolves,
respectively; J.B. and M.T. Theberge, V. Van Ballenberghe, and S.H.
Fritts for use of their unpublished data: and T. Wheeldon, J. Hart, and
reviewers and editor B. Patterson for offering helpful suggestions for
improvement.
NR 30
TC 1
Z9 1
U1 0
U2 6
PU HUMBOLDT FIELD RESEARCH INST
PI STEUBEN
PA PO BOX 9, STEUBEN, ME 04680-0009 USA
SN 1092-6194
J9 NORTHEAST NAT
JI Northeast. Nat
PY 2011
VL 18
IS 3
BP 265
EP 274
PG 10
WC Biodiversity Conservation; Ecology
SC Biodiversity & Conservation; Environmental Sciences & Ecology
GA 926JZ
UT WOS:000302828600002
ER
PT J
AU Buhlmann, KA
Osborn, CP
AF Buhlmann, Kurt A.
Osborn, Colin P.
TI Use of an Artificial Nesting Mound by Wood Turtles (Glyptemys
insculpta): A Tool for Turtle Conservation
SO NORTHEASTERN NATURALIST
LA English
DT Article
ID CLEMMYS-INSCULPTA; EMYDOIDEA-BLANDINGII; NORTHERN LIMIT; NEW-JERSEY;
ECOLOGY; MANAGEMENT; MOVEMENTS; RANGE; POPULATION; SELECTION
AB We constructed an artificial nesting mound for Glyptemys insculpta (Wood Turtle) in the Great Swamp National Wildlife Refuge, NJ. The original nesting site was impacted by development and invasive plants. The new nesting mound was constructed from similar soil and was 100 in distant from the original site. The new mound was 50 m from stream habitat and in an old field where it received full sun for the entire day. The mound was 18 m long, 8 in wide, and had a maximum height of 1.5 m, with gently sloping sides. We encountered nest-searching female Wood Turtles on the impacted site during late May to early June for four years, 2007-2010. We carefully hand-carried females to the new nesting area and allowed them to choose whether or not to nest on the mound. We protected all nests from predators. Seventeen of 18 nests that were deposited and left on the nesting mound produced live hatchlings. Six clutches had 100% hatching success, with only one failing completely. At least nine different female Wood Turtles nested on the mound. One female returned on her own in three subsequent years, another returned on her own in one subsequent year, several were re-shown the mound in subsequent years, and one turtle found the mound and nested on it on her own. The nesting mound has produced 142 hatchling Wood Turtles over the four years. We suggest that it is possible to entice female turtles to nest in a new area and that when nesting resources are limited, construction and protection of nesting areas can be a useful conservation action.
C1 [Buhlmann, Kurt A.] Univ Georgia, Savannah River Ecol Lab, Aiken, SC 29802 USA.
[Osborn, Colin P.] US Fish & Wildlife Serv, Basking Ridge, NJ 07920 USA.
RP Buhlmann, KA (reprint author), Univ Georgia, Savannah River Ecol Lab, Aiken, SC 29802 USA.
EM kbuhlmann@earthlink.net
FU US Department of Energy [DE-FC-09-075R22506]; Buhlmann Ecological
Research, LLC
FX We thank Michael Home for constructing the nest mound for us with the
backhoe and Susi Ponce for thoughts on the initial nesting-cage design.
We also thank Len Soucy and technicians of the New Jersey Raptor Trust
for X-radiographing turtles, Rich Seigel and Jackie Record for providing
historical information about Great Swamp Wood Turtles, and William Koch,
Refuge Manager, for his support of this project. We thank the following
individuals who helped to track and locate Wood Turtles in the field:
Heather Barrett, George Cevera, Kean Clifford, Tom Clifford, Greg
Cooper, Charlie Cotton, Ray Farrell, Andrew Ferreira, Bridget Goldsmith,
Anthony Henehan, Steve Henry, Chris Hernandez, Peter Hrinewski, Georgina
Jacquez, Helen Johnson, Marilyn Kitchell, Scott Kuhn, Marnie
Miller-Keas, Dave Moskowitz, Laura Newgard, Adam Osborn, Hanina Osborn,
Joe Pignatelli, Harry, Harriet, and Harley Spaven, Tim and Marcia
Stevens, Kelly Triece, Tracey Tuberville, Peter Warny, Bob Zappalorti,
and Brian Zarate. We thank Tony Cullen and Dave Miller for mowing the
old field each winter. We thank Brett DeGregorio and three anonymous
reviewers for greatly improving earlier drafts of the manuscript.
Manuscript preparation was supported by the US Department of Energy
under Award Number DE-FC-09-075R22506 to the Savannah River Ecology
Laboratory, and by Buhlmann Ecological Research, LLC.
NR 43
TC 8
Z9 8
U1 12
U2 34
PU HUMBOLDT FIELD RESEARCH INST
PI STEUBEN
PA PO BOX 9, STEUBEN, ME 04680-0009 USA
SN 1092-6194
J9 NORTHEAST NAT
JI Northeast. Nat
PY 2011
VL 18
IS 3
BP 315
EP 334
PG 20
WC Biodiversity Conservation; Ecology
SC Biodiversity & Conservation; Environmental Sciences & Ecology
GA 926JZ
UT WOS:000302828600005
ER
PT J
AU Wilson, PU
Longcore, JR
AF Wilson, Paul U.
Longcore, Jerry R.
TI Least Bittern Nesting Record in Maine
SO NORTHEASTERN NATURALIST
LA English
DT Article
AB In June 2001, we located an active Ixobrychus exilis (Least Bittern) nest in Bass Harbor marsh on Mount Desert Island, Hancock County, ME. Only 2 other descriptions of Least Bittern nests exist for Maine, although based on other breeding evidence, the species is known to breed elsewhere in the state. We found the nest in a 0.7-ha Typha sp. (cattail)-dominated area within a larger (3.5 ha) freshwater wetland located approximate to 120 m from an 88-ha estuary. During the breeding season, most Least Bitterns in Maine and elsewhere are found in wetlands of greater size, usually >10 ha.
C1 [Wilson, Paul U.] Natl Pk Serv, Bar Harbor, ME 04609 USA.
[Longcore, Jerry R.] US Geol Survey, Patuxent Wildlife Res Ctr, Orono, ME 04469 USA.
RP Wilson, PU (reprint author), Antioch Univ New England, 40 Avon St, Keene, NH 03431 USA.
EM pwilson1@antioch.edu
FU National Park Service [IA4520-1-05]; US Geological Survey, Patuxent
Wildlife Research Center, Orono, ME
FX We thank T. Hodgman (Maine Department of Inland Fish and Wildlife) and
J. Despres (Maine Bird Notes) for helpful information about status and
distribution of Least Bitterns in Maine. Scott Melvin and Peter Vickery
reviewed an early draft of the manuscript. D. Manski, B. Connery, and K.
Anderson provided logistical and technical support at Acadia National
Park. Research funds were provided by the National Park Service through
an Interagency Agreement (# IA4520-1-05) with the US Geological Survey,
Patuxent Wildlife Research Center, Orono, ME.
NR 14
TC 0
Z9 0
U1 0
U2 3
PU HUMBOLDT FIELD RESEARCH INST
PI STEUBEN
PA PO BOX 9, STEUBEN, ME 04680-0009 USA
SN 1092-6194
J9 NORTHEAST NAT
JI Northeast. Nat
PY 2011
VL 18
IS 3
BP 382
EP 385
PG 4
WC Biodiversity Conservation; Ecology
SC Biodiversity & Conservation; Environmental Sciences & Ecology
GA 926JZ
UT WOS:000302828600011
ER
PT J
AU Mech, LD
AF Mech, L. David
TI Non-genetic Data Supporting Genetic Evidence for the Eastern Wolf
SO NORTHEASTERN NATURALIST
LA English
DT Article
ID MOUNTAIN-NATIONAL-PARK; MITOCHONDRIAL-DNA; CANIS-LUPUS; GRAY WOLF;
WOLVES; COYOTE; HYBRIDIZATION; MANITOBA; LATRANS; ONTARIO
AB Two schools of thought dominate the molecular-genetics literature on Canis spp. (wolves) in the western Great Lakes region of the US and Canada: (1) they are hybrids between Canis lupus (Gray Wolf) and Canis latrans (Coyote), or (2) they are hybrids between the Gray Wolf and Canis lycaon (Eastern Wolf). This article presents 3 types of non-genetic evidence that bears on the controversy and concludes that all 3 support the second interpretation.
C1 [Mech, L. David] US Geol Survey, No Prairie Wildlife Res Ctr, Jamestown, ND 58401 USA.
RP Mech, LD (reprint author), Univ Minnesota, US Geol Survey, Raptor Ctr, 1920 Fitch Ave, St Paul, MN 55108 USA.
EM mechx002@umn.edu
FU US Geological Survey
FX This study was supported by the US Geological Survey. I thank T.
Wheeldon and S.R. Fain for critiquing an earlier draft and making
helpful suggestions for improving it.
NR 40
TC 7
Z9 9
U1 0
U2 10
PU HUMBOLDT FIELD RESEARCH INST
PI STEUBEN
PA PO BOX 9, STEUBEN, ME 04680-0009 USA
SN 1092-6194
J9 NORTHEAST NAT
JI Northeast. Nat
PY 2011
VL 18
IS 4
BP 521
EP 526
PG 6
WC Biodiversity Conservation; Ecology
SC Biodiversity & Conservation; Environmental Sciences & Ecology
GA 926KB
UT WOS:000302828800009
ER
PT S
AU North, EW
Adams, EE
Schlag, Z
Sherwood, CR
He, RY
Hyun, KH
Socololskys, SA
AF North, Elizabeth W.
Adams, E. Eric
Schlag, Zachary
Sherwood, Christopher R.
He, Ruoying
Hyun, Kyung Hoon
Socololskys, Scott A.
BE Liu, Y
MacFadyen, A
Ji, ZG
Weisberg, RH
TI Simulating Oil Droplet Dispersal From the Deepwater Horizon Spill With a
Lagrangian Approach
SO MONITORING AND MODELING THE DEEPWATER HORIZON OIL SPILL: A
RECORD-BREAKING ENTERPRISE
SE Geophysical Monograph Series
LA English
DT Article; Book Chapter
ID STRATIFIED MULTIPHASE PLUMES; RANDOM-WALK MODELS; TRANSPORT; BEHAVIOR;
TRACKING; VELOCITY
AB An analytical multiphase plume model, combined with time-varying flow and hydrographic fields generated by the 3-D South Atlantic Bight and Gulf of Mexico model (SABGOM) hydrodynamic model, were used as input to a Lagrangian transport model (LTRANS), to simulate transport of oil droplets dispersed at depth from the recent Deepwater Horizon MC 252 oil spill. The plume model predicts a stratification-dominated near field, in which small oil droplets detrain from the central plume containing faster rising large oil droplets and gas bubbles and become trapped by density stratification. Simulated intrusion (trap) heights of similar to 310-370 m agree well with the midrange of conductivity-temperature-depth observations, though the simulated variation in trap height was lower than observed, presumably in part due to unresolved variability in source composition (percentage oil versus gas) and location (multiple leaks during first half of spill). Simulated droplet trajectories by the SABGOM-LTRANS modeling system showed that droplets with diameters between 10 and 50 mu m formed a distinct subsurface plume, which was transported horizontally and remained in the subsurface for >1 month. In contrast, droplets with diameters >= 90 mu m rose rapidly to the surface. Simulated trajectories of droplets <= 50 mu m in diameter were found to be consistent with field observations of a southwest-tending subsurface plume in late June 2010 reported by Camilli et al. [2010]. Model results suggest that the subsurface plume looped around to the east, with potential subsurface oil transport to the northeast and southeast. Ongoing work is focusing on adding degradation processes to the model to constrain droplet dispersal.
C1 [North, Elizabeth W.; Schlag, Zachary] Univ Maryland, Horn Point Lab, Ctr Environm Sci, Cambridge, MD 21613 USA.
[Adams, E. Eric] MIT, Dept Civil & Environm Engn, Cambridge, MA 02139 USA.
[He, Ruoying; Hyun, Kyung Hoon] N Carolina State Univ, Dept Marine Earth & Atmospher Sci, Raleigh, NC 27695 USA.
[Sherwood, Christopher R.] US Geol Survey, Woods Hole, MA 02543 USA.
[Socololskys, Scott A.] Texas A&M Univ, Zachry Dept Civil Engn, Coastal & Ocean Engn Div, College Stn, TX 77843 USA.
RP North, EW (reprint author), Univ Maryland, Horn Point Lab, Ctr Environm Sci, 2020 Horns Point Rd, Cambridge, MD 21613 USA.
EM enorth@umces.edu
NR 29
TC 36
Z9 38
U1 1
U2 6
PU AMER GEOPHYSICAL UNION
PI WASHINGTON
PA 2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA
SN 0065-8448
BN 978-0-87590-485-6
J9 GEOPHYS MONOGR SER
PY 2011
VL 195
BP 217
EP 226
DI 10.1029/2011GM001102
PG 10
WC Geochemistry & Geophysics; Environmental Sciences
SC Geochemistry & Geophysics; Environmental Sciences & Ecology
GA BYW60
UT WOS:000300646700019
ER
PT J
AU Jimenez, JE
White, TH
AF Jimenez, Jaime E.
White, Thomas H., Jr.
TI USE OF TREE CAVITIES FOR NESTING BY SPECKLED TEAL (ANAS FLAVIROSTRIS) IN
SOUTHERN CHILE: POTENTIAL COMPETITION WITH THE SLENDER-BILLED PARAKEET
(ENICOGNATHUS LEPTORHYNCHUS)
SO ORNITOLOGIA NEOTROPICAL
LA English
DT Article
DE Speckled Teal; Anas flavirostris; Slender-billed Parakeet; Enicognathus
leptorhynchus; Nothofagus; nesting; cavities; competition; Chile
ID EASTERN AUSTRALIA; FOREST; BIRDS; FRAGMENTATION; PARROT
C1 [Jimenez, Jaime E.] Univ Lagos, Lab Vida Silvestre, Osorno, Chile.
[White, Thomas H., Jr.] US Fish & Wildlife Serv, Puerto Rican Parrot Recovery Program, Rio Grande, PR 00745 USA.
RP Jimenez, JE (reprint author), Univ N Texas, Dept Biol Sci, Subantarctic Biocultural Conservat Program, 1155 Union Circle 305220, Denton, TX 76203 USA.
EM jaime.jimenez@unt.edu; thomas_white@fws.gov
FU United States Fish and Wildlife Service; Parrots International; Amigos
de Las Ayes; Canadian Parrot Society; International Conure Association
FX We are grateful to the United States Fish and Wildlife Service - Puerto
Rican Parrot Recovery Program, Parrots International, Amigos de Las
Ayes, Canadian Parrot Society, International Conure Association, and
Tony Pittman for funding and technical assistance with all aspects of
this study. Several students and volunteers also helped with nest
inspections, especially Ana Bertoldi, Gemma Ffrench, Samuel Aylwin, and
Magdelena Contreras. In particular, we thank the brothers Mauricio and
Nelson Ojeda for their invaluable advice and assistance with locating
nests and tree climbing. We also thank the administration of
INIA-Remehue and the numerous private landowners who kindly provided us
access to their properties. Jaime Collazo, Tatiana Saco, Andre Weller,
and an anonymous reviewer provided helpful comments that improved the
manuscript.
NR 21
TC 3
Z9 3
U1 0
U2 3
PU NEOTROPICAL ORNITHOLOGICAL SOC, USGS PATUXENT WILDLIFE RESEARCH CTR
PI ATHENS
PA UNIV GEORGIA, WARNELL SCH FOREST RESOURCES, ATHENS, GA 30602-2152 USA
SN 1075-4377
J9 ORNITOL NEOTROP
JI ORNITOL. NEOTROP.
PY 2011
VL 22
IS 3
BP 465
EP 469
PG 5
WC Ornithology
SC Zoology
GA 918UC
UT WOS:000302275600015
ER
PT S
AU Custer, CM
AF Custer, Christine M.
BE Elliott, JE
Bishop, CA
Morrissey, CA
TI Swallows as a Sentinel Species for Contaminant Exposure and Effect
Studies
SO WILDLIFE ECOTOXICOLOGY: FORENSIC APPROACHES
SE Emerging Topics in Ecotoxicology
LA English
DT Article; Book Chapter
ID NESTLING TREE SWALLOWS; RIVER SUPERFUND SITE; POLYCHLORINATED BIPHENYL
CONTAMINATION; POLYBROMINATED DIPHENYL ETHERS; SPRAYED APPLE ORCHARDS;
POLYCYCLIC AROMATIC-HYDROCARBONS; CORTICOSTERONE STRESS-RESPONSE;
STARLINGS STURNUS-VULGARIS; UPPER MISSISSIPPI RIVER; THYROID-HORMONE
LEVELS
AB Tree swallows are an important model species to study the effects of contaminants in wild bird populations and have been used extensively in studies across North America. The advantages of swallows compared to other avian species are detailed. Three case histories are provided where swallows have been successfully used in Natural Resource Damage and Ecological Risk Assessments. The final two sections of this chapter are for individuals who want more in-depth information and include a summary of the chemical classes for which there are swallow data, including effect levels when known. Information provided in this section can be used to put exposure to most classes of contaminants into context with other sites across North America. Finally, commonly used endpoints, ranging from population-level down to cellular and genetic endpoints, are discussed including considerations and pitfalls, and when further work is needed to more fully understand the role of environmental and biological variation in interpreting these endpoints.
C1 US Geol Survey, Upper Midw Environm Sci Ctr, La Crosse, WI 54603 USA.
RP Custer, CM (reprint author), US Geol Survey, Upper Midw Environm Sci Ctr, 2630 Fanta Reed Rd, La Crosse, WI 54603 USA.
EM ccuster@usgs.gov
NR 147
TC 18
Z9 18
U1 0
U2 14
PU SPRINGER
PI NEW YORK
PA 233 SPRING STREET, NEW YORK, NY 10013, UNITED STATES
SN 1868-1344
BN 978-0-387-89431-7
J9 EMERG TOP ECOTOXICOL
JI Emrg. Top. Ecotox.
PY 2011
VL 3
BP 45
EP 91
DI 10.1007/978-0-387-89432-4_3
D2 10.1007/978-0-387-89432-4
PG 47
WC Ecology; Environmental Sciences; Toxicology
SC Environmental Sciences & Ecology; Toxicology
GA BYV31
UT WOS:000300582100004
ER
PT S
AU Woodward, AR
Percival, HF
Rauschenberger, RH
Gross, TS
Rice, KG
Conrow, R
AF Woodward, Allan R.
Percival, H. Franklin
Rauschenberger, R. Heath
Gross, Timothy S.
Rice, Kenneth G.
Conrow, Roxanne
BE Elliott, JE
Bishop, CA
Morrissey, CA
TI Abnormal Alligators and Organochlorine Pesticides in Lake Apopka,
Florida
SO WILDLIFE ECOTOXICOLOGY: FORENSIC APPROACHES
SE Emerging Topics in Ecotoxicology
LA English
DT Article; Book Chapter
ID LIFE-STAGE MORTALITY; AMERICAN ALLIGATOR; THIAMINE-DEFICIENCY;
REPRODUCTIVE-CYCLE; GREAT-LAKES; FATTY-ACIDS; ENVIRONMENTAL
CONTAMINANTS; JUVENILE ALLIGATORS; REARED ALLIGATORS; CLUTCH VIABILITY
AB Lake Apopka is a 12,400-ha hypereutrophic lake in central Florida that was the recipient of nutrient and pesticide pollution from adjacent agricultural operations for 50 years. The abnormal American alligator (Alligator mississsippiensis) population in Lake Apopka has been the object of a number of studies including investigations of a population crash, the epidemiology of egg failure, and anomalous endocrine function. Several hypotheses of the causes of these abnormalities have been proposed and examined by multiple research organizations over the past three decades. Initially, organochlorine pesticide (OCP) contamination was considered the most likely factor causing poor reproductive success. DDE concentrations in alligator eggs sampled in 1984-1985 were approximately 4 mg/kg and toxaphene concentrations were approximately 2.5 mg/kg. These levels were known to cause reproductive failure in certain birds. However, transmissible diseases, population age and density, cyanotoxins, nutritional deficiencies, and combinations thereof, were also investigated for their contribution to poor alligator reproductive success. Investigations of an alligator mortality and reproductive failure event on Lake Griffin, a lake similar to Lake Apopka but with lower OCP levels, revealed analogous reproductive abnormalities that were associated with a dietary thiamine deficiency. Thiamine deficiency appeared to be associated with a diet of almost exclusively gizzard shad, which contain thiaminase, an enzyme that breaks down thiamine. OCP contaminants may contribute to these maladies, perhaps through endocrine disruption and increased stress. The findings of the past 30 years of work at Lake Apopka have affected local management decisions as well as policy at the national level.
C1 [Woodward, Allan R.] Florida Fish & Wildlife Conservat Commiss, Fish & Wildlife Res Inst, Gainesville, FL 32601 USA.
[Conrow, Roxanne] St Johns River Water Management Dist, Palatka, FL 32178 USA.
[Gross, Timothy S.] Univ Florida, Environm Resource Consultants, Gainesville, FL 32611 USA.
[Percival, H. Franklin] Univ Florida, Florida Cooperat Fish & Wildlife Res Unit, US Geol Survey, Gainesville, FL 32611 USA.
[Rauschenberger, R. Heath] US Fish & Wildlife Serv, N Florida Ecol Serv Field Off, Jacksonville, FL 32256 USA.
[Rice, Kenneth G.] US Geol Survey, SE Ecol Sci Ctr, Gainesville, FL 32653 USA.
RP Woodward, AR (reprint author), Florida Fish & Wildlife Conservat Commiss, Fish & Wildlife Res Inst, 1105 SW Williston Rd, Gainesville, FL 32601 USA.
EM allan.woodward@myfwc.com; percivaf@ufl.edu;
Heath_Rauschenberger@fws.gov; tsgross@cox.ne; krice@usgs.gov;
rconrow@sjrwmd.com
NR 108
TC 5
Z9 5
U1 1
U2 17
PU SPRINGER
PI NEW YORK
PA 233 SPRING STREET, NEW YORK, NY 10013, UNITED STATES
SN 1868-1344
BN 978-0-387-89431-7
J9 EMERG TOP ECOTOXICOL
JI Emrg. Top. Ecotox.
PY 2011
VL 3
BP 153
EP 187
DI 10.1007/978-0-387-89432-4_5
D2 10.1007/978-0-387-89432-4
PG 35
WC Ecology; Environmental Sciences; Toxicology
SC Environmental Sciences & Ecology; Toxicology
GA BYV31
UT WOS:000300582100006
ER
PT J
AU West, D
Corbett, DG
Lefevre, C
AF West, Dixie
Corbett, Debra G.
Lefevre, Christine
TI Petroglyphs from Gillon Point, Agattu Island, Aleutian Islands, Alaska
SO ARCTIC ANTHROPOLOGY
LA English
DT Article
AB In 2002, biologists with the National Marine Fisheries Service recorded petroglyphs while counting sea lions at the rookery near Gillon Point on Agattu Island, Aleutian Islands. This is the first well-documented rock art in the Aleutian archipelago. The images, individually and in groups, appear to represent female genitalia, rectangles and straight lines, and an anthropomorphic figure. The Agattu petroglyphs either represent art that arose in situ or motifs imported from elsewhere. The engravings do not reveal evidence of contact with human groups living to the west or south.
C1 [West, Dixie] Univ Kansas, Nat Hist Museum, Lawrence, KS 66045 USA.
[West, Dixie] Univ Kansas, Biodivers Res Ctr, Lawrence, KS 66045 USA.
[Corbett, Debra G.] US Fish & Wildlife Serv, Anchorage, AK 99503 USA.
[Lefevre, Christine] Museum Natl Hist Nat, F-75005 Paris, France.
[Lefevre, Christine] CNRS, UMR 7209, F-75005 Paris, France.
RP West, D (reprint author), Univ Kansas, Nat Hist Museum, Dyche Hall,1345 Jayhawk Blvd, Lawrence, KS 66045 USA.
NR 21
TC 0
Z9 0
U1 0
U2 2
PU UNIV WISCONSIN PRESS
PI MADISON
PA JOURNAL DIVISION, 1930 MONROE ST, 3RD FL, MADISON, WI 53711 USA
SN 0066-6939
J9 ARCTIC ANTHROPOL
JI Arct. Anthropol.
PY 2011
VL 48
IS 2
BP 17
EP 24
PG 8
WC Anthropology
SC Anthropology
GA 905TU
UT WOS:000301298700003
ER
PT J
AU Lefevre, C
West, D
Corbett, DG
AF Lefevre, Christine
West, Dixie
Corbett, Debra G.
TI Zooarchaeological Analysis at ADK-011, Adak Island, Central Aleutian
Islands, Alaska
SO ARCTIC ANTHROPOLOGY
LA English
DT Article
ID WESTERN ALEUTIANS; BULDIR ISLAND; BERING-SEA
AB Although William Dall explored the Central Aleutians nearly 140 years ago, surprisingly little archaeological research has occurred in this area since then. During 1999 the Western Aleutians Archaeological and Paleobiological Project excavated archaeological sites on north Adak Island, Alaska. Faunal remains from two excavation pits at ADK-011 are analyzed here. This is the first analysis of faunal remains from this particular island. Our research reveals that late prehistoric Aleuts depended on marine mammals, birds, fish, and invertebrates. Although whale remains were recovered, it is currently impossible to tell if these represent hunted or stranded animals. Birds were hunted for their valuable bones as well as for their meat. Aleuts captured both pelagic and near-shore fish. Invertebrate remains indicate that prehistoric Aleuts depended on nearby high energy reefs as well as the calmer waters of Clam Lagoon for subsistence. Additionally, the marine reservoir effect must be considered when understanding radiocarbon dates from Aleutian archaeological sites.
C1 [Lefevre, Christine] Museum Natl Hist Nat, F-75005 Paris, France.
[Lefevre, Christine] CNRS, Dept Ecol & Gest Biodiversite, UMR 7209, F-75005 Paris, France.
[West, Dixie] Univ Kansas, Biodivers Res Ctr, Lawrence, KS 66045 USA.
[Corbett, Debra G.] US Fish & Wildlife Serv, Anchorage, AK 99503 USA.
RP Lefevre, C (reprint author), Museum Natl Hist Nat, 55 Rue Buffon, F-75005 Paris, France.
NR 37
TC 2
Z9 2
U1 0
U2 4
PU UNIV WISCONSIN PRESS
PI MADISON
PA JOURNAL DIVISION, 1930 MONROE ST, 3RD FL, MADISON, WI 53711 USA
SN 0066-6939
J9 ARCTIC ANTHROPOL
JI Arct. Anthropol.
PY 2011
VL 48
IS 2
BP 69
EP 82
PG 14
WC Anthropology
SC Anthropology
GA 905TU
UT WOS:000301298700006
ER
PT S
AU Bird, KJ
Houseknecht, DW
AF Bird, Kenneth J.
Houseknecht, David W.
BE Spencer, AM
Embry, AF
Gautier, DL
Stoupakova, AV
Sorensen, K
TI Geology and petroleum potential of the Arctic Alaska petroleum province
SO ARCTIC PETROLEUM GEOLOGY
SE Geological Society Memoirs
LA English
DT Proceedings Paper
CT 33rd International Geological Congress (IGC)
CY AUG 06-14, 2008
CL Oslo, NORWAY
SP Int Marine Minerals Soc, petr ind
ID WESTERN BROOKS RANGE; PRUDHOE BAY FIELD; NORTH SLOPE; SEQUENCE
STRATIGRAPHY; SHUBLIK FORMATION; SCHIST BELT; RESERVOIR; EVOLUTION;
ORIGIN; BASIN
AB The Arctic Alaska petroleum province encompasses all lands and adjacent continental shelf areas north of the Brooks Range-Herald Arch orogenic belt and south of the northern (outboard) margin of the Beaufort Rift shoulder. Even though only a small part is thoroughly explored, it is one of the most prolific petroleum provinces in North America with total known resources (cumulative production plus proved reserves) of c. 28 BBOE. The province constitutes a significant part of a displaced continental fragment, the Arctic Alaska microplate, that was probably rifted from the Canadian Arctic margin during formation of the Canada Basin. Petroleum prospective rocks in the province, mostly Mississippian and younger, record a sequential geological evolution through passive margin, rift and foreland basin tectonic stages. Significant petroleum source and reservoir rocks were formed during each tectonic stage but it was the foreland basin stage that provided the necessary burial heating to generate petroleum from the source rocks. The lion's share of known petroleum resources in the province occur in combination structural-stratigraphic traps formed as a consequence of rifting and located along the rift shoulder. Since the discovery of the super-giant Prudhoe Bay accumulation in one of these traps in the late 1960s, exploration activity preferentially focused on these types of traps. More recent activity, however, has emphasized the potential for stratigraphic traps and the prospect of a natural gas pipeline in this region has spurred renewed interest in structural traps. For assessment purposes, the province is divided into a Platform assessment unit (AU), comprising the Beaufort Rift shoulder and its relatively undeformed flanks, and a Fold-and-Thrust Belt AU, comprising the deformed area north of the Brooks Range and Herald Arch tectonic belt. Mean estimates of undiscovered, technically recoverable resources include nearly 28 billion barrels of oil (BBO) and 122 trillion cubic feet (TCF) of nonassociated gas in the Platform AU and 2 BBO and 59 TCF of nonassociated gas in the Fold-and-Thrust Belt AU.
C1 [Bird, Kenneth J.] US Geol Survey, Menlo Pk, CA 94025 USA.
RP Bird, KJ (reprint author), US Geol Survey, 345 Middlefield Rd, Menlo Pk, CA 94025 USA.
EM kbird@usgs.gov
NR 80
TC 8
Z9 10
U1 0
U2 28
PU GEOLOGICAL SOC PUBLISHING HOUSE
PI BATH
PA UNIT 7, BRASSMILL ENTERPRISE CTR, BRASSMILL LANE, BATH BA1 3JN, AVON,
ENGLAND
SN 0435-4052
BN 978-1-86239-328-8
J9 GEOL SOC MEM
PY 2011
VL 35
DI 10.1144/M35.32
PG 15
WC Geology
SC Geology
GA BYY32
UT WOS:000300715800032
ER
PT S
AU Charpentier, RR
Gautier, DL
AF Charpentier, Ronald R.
Gautier, Donald L.
BE Spencer, AM
Embry, AF
Gautier, DL
Stoupakova, AV
Sorensen, K
TI US Geological Survey Circum-Arctic Resource Appraisal (CARA):
introduction and summary of organization and methods
SO ARCTIC PETROLEUM GEOLOGY
SE Geological Society Memoirs
LA English
DT Proceedings Paper
CT 33rd International Geological Congress (IGC)
CY AUG 06-14, 2008
CL Oslo, NORWAY
SP Int Marine Minerals Soc, petr ind
AB The USGS has assessed undiscovered petroleum resources in the Arctic through geological mapping, basin analysis and quantitative assessment. The new map compilation provided the base from which geologists subdivided the Arctic for burial history modelling and quantitative assessment. The CARA was a probabilistic, geologically based study that used existing USGS methodology, modified somewhat for the circumstances of the Arctic. The assessment relied heavily on analogue modelling, with numerical input as lognormal distributions of sizes and numbers of undiscovered accumulations. Probabilistic results for individual assessment units were statistically aggregated taking geological dependencies into account. Fourteen papers in this Geological Society volume present summaries of various aspects of the CARA.
C1 [Gautier, Donald L.] US Geol Survey, Menlo Pk, CA 94025 USA.
RP Gautier, DL (reprint author), US Geol Survey, 345 Middlefield Rd, Menlo Pk, CA 94025 USA.
EM gautier@usgs.gov; gautier@usgs.gov
NR 22
TC 11
Z9 12
U1 1
U2 4
PU GEOLOGICAL SOC PUBLISHING HOUSE
PI BATH
PA UNIT 7, BRASSMILL ENTERPRISE CTR, BRASSMILL LANE, BATH BA1 3JN, AVON,
ENGLAND
SN 0435-4052
BN 978-1-86239-328-8
J9 GEOL SOC MEM
PY 2011
VL 35
DI 10.1144/M35.8
PG 6
WC Geology
SC Geology
GA BYY32
UT WOS:000300715800008
ER
PT S
AU Gautier, DL
Stemmerik, L
Christiansen, FG
Sorensen, K
Bidstrup, T
Bojesen-Koefoed, JA
Bird, KJ
Charpentier, RR
Houseknecht, DW
Klett, TR
Schenk, CJ
Tennyson, ME
AF Gautier, Donald L.
Stemmerik, Lars
Christiansen, Flemming G.
Sorensen, Kai
Bidstrup, Torben
Bojesen-Koefoed, Jorgen A.
Bird, Kenneth J.
Charpentier, Ronald R.
Houseknecht, David W.
Klett, T. R.
Schenk, Christopher J.
Tennyson, Marilyn E.
BE Spencer, AM
Embry, AF
Gautier, DL
Stoupakova, AV
Sorensen, K
TI Assessment of NE Greenland: prototype for development of Circum-Arctic
Resource Appraisal methodology
SO ARCTIC PETROLEUM GEOLOGY
SE Geological Society Memoirs
LA English
DT Proceedings Paper
CT 33rd International Geological Congress (IGC)
CY AUG 06-14, 2008
CL Oslo, NORWAY
SP Int Marine Minerals Soc, petr ind
ID EAST GREENLAND; ORGANIC GEOCHEMISTRY; LACUSTRINE SHALES; NORTH-ATLANTIC;
MARGIN; BASIN; SEA
AB Geological features of NE Greenland suggest large petroleum potential, as well as high uncertainty and risk. The area was the prototype for development of methodology used in the US Geological Survey (USGS) Circum-Arctic Resource Appraisal (CARA), and was the first area evaluated. In collaboration with the Geological Survey of Denmark and Greenland (GEUS), eight 'assessment units' (AU) were defined, six of which were probabilistically assessed. The most prospective areas are offshore in the Danmarkshavn Basin. This study supersedes a previous USGS assessment, from which it differs in several important respects: oil estimates are reduced and natural gas estimates are increased to reflect revised understanding of offshore geology. Despite the reduced estimates, the CARA indicates that NE Greenland may be an important future petroleum province.
C1 [Gautier, Donald L.; Bird, Kenneth J.] US Geol Survey, Menlo Pk, CA 94025 USA.
RP Gautier, DL (reprint author), US Geol Survey, 345 Middlefield Rd, Menlo Pk, CA 94025 USA.
EM gautier@usgs.gov; gautier@usgs.gov
NR 35
TC 4
Z9 4
U1 0
U2 3
PU GEOLOGICAL SOC PUBLISHING HOUSE
PI BATH
PA UNIT 7, BRASSMILL ENTERPRISE CTR, BRASSMILL LANE, BATH BA1 3JN, AVON,
ENGLAND
SN 0435-4052
BN 978-1-86239-328-8
J9 GEOL SOC MEM
PY 2011
VL 35
DI 10.1144/M35.43
PG 10
WC Geology
SC Geology
GA BYY32
UT WOS:000300715800043
ER
PT S
AU Gautier, DL
Bird, KJ
Charpentier, RR
Grantz, A
Houseknecht, DW
Klett, TR
Moore, TE
Pitman, JK
Schenk, CJ
Schuenemeyer, JH
Sorensen, K
Tennyson, ME
Valin, ZC
Wandrey, CJ
AF Gautier, Donald L.
Bird, Kenneth J.
Charpentier, Ronald R.
Grantz, Arthur
Houseknecht, David W.
Klett, Timothy R.
Moore, Thomas E.
Pitman, Janet K.
Schenk, Christopher J.
Schuenemeyer, John H.
Sorensen, Kai
Tennyson, Marilyn E.
Valin, Zenon C.
Wandrey, Craig J.
BE Spencer, AM
Embry, AF
Gautier, DL
Stoupakova, AV
Sorensen, K
TI Oil and gas resource potential north of the Arctic Circle
SO ARCTIC PETROLEUM GEOLOGY
SE Geological Society Memoirs
LA English
DT Proceedings Paper
CT 33rd International Geological Congress (IGC)
CY AUG 06-14, 2008
CL Oslo, NORWAY
SP Int Marine Minerals Soc, petr ind
AB The US Geological Survey recently assessed the potential for undiscovered conventional petroleum in the Arctic. Using a new map compilation of sedimentary elements, the area north of the Arctic Circle was subdivided into 70 assessment units, 48 of which were quantitatively assessed. The Circum-Arctic Resource Appraisal (CARA) was a geologically based, probabilistic study that relied mainly on burial history analysis and analogue modelling to estimate sizes and numbers of undiscovered oil and gas accumulations. The results of the CARA suggest the Arctic is gas-prone with an estimated 770-2990 trillion cubic feet of undiscovered conventional natural gas, most of which is in Russian territory. On an energy-equivalent basis, the quantity of natural gas is more than three times the quantity of oil and the largest undiscovered gas field is expected to be about 10 times the size of the largest undiscovered oil field. In addition to gas, the gas accumulations may contain an estimated 39 billion barrels of liquids. The South Kara Sea is the most prospective gas assessment unit, but giant gas fields containing more than 6 trillion cubic feet of recoverable gas are possible at a 50% chance in 10 assessment units. Sixty per cent of the estimated undiscovered oil resource is in just six assessment units, of which the Alaska Platform, with 31% of the resource, is the most prospective. Overall, the Arctic is estimated to contain between 44 and 157 billion barrels of recoverable oil. Billion barrel oil fields are possible at a 50% chance in seven assessment units. Undiscovered oil resources could be significant to the Arctic nations, but are probably not sufficient to shift the world oil balance away from the Middle East.
C1 [Gautier, Donald L.; Bird, Kenneth J.; Moore, Thomas E.; Valin, Zenon C.] US Geol Survey, Menlo Pk, CA 94025 USA.
RP Gautier, DL (reprint author), US Geol Survey, 345 Middlefield Rd, Menlo Pk, CA 94025 USA.
EM gautier@usgs.gov; gautier@usgs.gov
NR 17
TC 14
Z9 14
U1 10
U2 26
PU GEOLOGICAL SOC PUBLISHING HOUSE
PI BATH
PA UNIT 7, BRASSMILL ENTERPRISE CTR, BRASSMILL LANE, BATH BA1 3JN, AVON,
ENGLAND
SN 0435-4052
BN 978-1-86239-328-8
J9 GEOL SOC MEM
PY 2011
VL 35
DI 10.1144/M35.9
PG 11
WC Geology
SC Geology
GA BYY32
UT WOS:000300715800009
ER
PT S
AU Grantz, A
Hart, PE
Childers, VA
AF Grantz, Arthur
Hart, Patrick E.
Childers, Vicki A.
BE Spencer, AM
Embry, AF
Gautier, DL
Stoupakova, AV
Sorensen, K
TI Geology and tectonic development of the Amerasia and Canada Basins,
Arctic Ocean
SO ARCTIC PETROLEUM GEOLOGY
SE Geological Society Memoirs
LA English
DT Proceedings Paper
CT 33rd International Geological Congress (IGC)
CY AUG 06-14, 2008
CL Oslo, NORWAY
SP Int Marine Minerals Soc, petr ind
ID BEAUFORT-MACKENZIE BASIN; QUEEN-ELIZABETH-ISLANDS; IBERIA ABYSSAL-PLAIN;
CONTINENTAL-MARGIN; ALPHA-RIDGE; LOMONOSOV RIDGE; CRUSTAL STRUCTURE;
REFRACTION PROFILES; MAGNETIC-ANOMALIES; NORTHWIND RIDGE
AB Amerasia Basin is the product of two phases of counterclockwise rotational opening about a pole in the lower Mackenzie Valley of NW Canada. Phase 1 opening brought ocean-continent transition crust (serpentinized peridotite?) to near the seafloor of the proto-Amerasia Basin, created detachment on the Eskimo Lakes Fault Zone of the Canadian Arctic margin and thinned the continental crust between the fault zone and the proto-Amerasia Basin to the west, beginning about 195 Ma and ending prior to perhaps about 160 Ma. The symmetry of the proto-Amerasia Basin was disrupted by clockwise rotation of the Chukchi Microcontinent into the basin from an original position along the Eurasia margin about a pole near 72 degrees N, 165 W about 145.5-140 Ma. Phase 2 opening enlarged the proto-Amerasia Basin by intrusion of mid-ocean ridge basalt along its axis between about 131 and 127.5 Ma. Following intrusion of the Phase 2 crust an oceanic volcanic plateau, the Alpha-Mendeleev Ridge LIP (large igneous province), was extruded over the northern Amerasia Basin from about 127 to 89-75 Ma. Emplacement of the LIP halved the area of the Amerasia Basin, and the area lying south of the LIP became the Canada Basin.
C1 [Grantz, Arthur] US Geol Survey, Menlo Pk, CA 94025 USA.
RP Grantz, A (reprint author), US Geol Survey, 345 Middlefield Rd,MS 969, Menlo Pk, CA 94025 USA.
EM agrantz@pacbell.net
NR 117
TC 50
Z9 50
U1 2
U2 5
PU GEOLOGICAL SOC PUBLISHING HOUSE
PI BATH
PA UNIT 7, BRASSMILL ENTERPRISE CTR, BRASSMILL LANE, BATH BA1 3JN, AVON,
ENGLAND
SN 0435-4052
BN 978-1-86239-328-8
J9 GEOL SOC MEM
PY 2011
VL 35
DI 10.1144/M35.50
PG 31
WC Geology
SC Geology
GA BYY32
UT WOS:000300715800050
ER
PT S
AU Grantz, A
Scott, RA
Drachev, SS
Moore, TE
Valin, ZC
AF Grantz, Arthur
Scott, Robert A.
Drachev, Sergey S.
Moore, Thomas E.
Valin, Zenon C.
BE Spencer, AM
Embry, AF
Gautier, DL
Stoupakova, AV
Sorensen, K
TI Sedimentary successions of the Arctic Region (58-64 degrees to 90
degrees N) that may be prospective for hydrocarbons
SO ARCTIC PETROLEUM GEOLOGY
SE Geological Society Memoirs
LA English
DT Proceedings Paper
CT 33rd International Geological Congress (IGC)
CY AUG 06-14, 2008
CL Oslo, NORWAY
SP Int Marine Minerals Soc, petr ind
ID NORWEGIAN-GREENLAND SEA; WESTERN BARENTS SEA; CONTINENT-OCEAN
TRANSITION; BEAUFORT-MACKENZIE BASIN; SEISMIC-REFLECTION DATA;
POTENTIAL-FIELD DATA; NORTHERN BAFFIN-BAY; EAST SIBERIAN SEA; LOMONOSOV
RIDGE; CRUSTAL STRUCTURE
AB A total of 143 sedimentary successions that contain, or may be prospective for, hydrocarbons were identified in the Arctic Region north of 58-64 degrees N and mapped in four quadrants at a scale of 1: 11 000 000. Eighteen of these successions (12.6%) occur in the Arctic Ocean Basin, 25 (17.5%) in the passive and sheared continental margins of the Arctic Basin and 100 (70.0%) on the Circum-Arctic continents of which one (<1%) lies in the active margin of the Pacific Rim. Each succession was assigned to one of 13 tectono-stratigraphic and morphologic classes and coloured accordingly on the map. The thickness of each succession and that of any underlying sedimentary section down to economic basement, where known, are shown on the map by isopachs. Major structural or tectonic features associated with the creation of the successions, or with the enhancement or degradation of their hydrocarbon potential, are also shown. Forty-four (30.8%) of the successions are known to contain hydrocarbon accumulations, 64 (44.8%) are sufficiently thick to have generated hydrocarbons and 35 (24.5%) may be too thin to be prospective.
C1 [Grantz, Arthur] US Geol Survey, Menlo Pk, CA 94025 USA.
RP Grantz, A (reprint author), US Geol Survey, 345 Middlefield Rd,MS 969, Menlo Pk, CA 94025 USA.
EM agrantz@pacbell.net
NR 273
TC 8
Z9 10
U1 0
U2 2
PU GEOLOGICAL SOC PUBLISHING HOUSE
PI BATH
PA UNIT 7, BRASSMILL ENTERPRISE CTR, BRASSMILL LANE, BATH BA1 3JN, AVON,
ENGLAND
SN 0435-4052
BN 978-1-86239-328-8
J9 GEOL SOC MEM
PY 2011
VL 35
DI 10.1144/M35.2
PG 23
WC Geology
SC Geology
GA BYY32
UT WOS:000300715800002
ER
PT S
AU Houseknecht, DW
Bird, KJ
AF Houseknecht, David W.
Bird, Kenneth J.
BE Spencer, AM
Embry, AF
Gautier, DL
Stoupakova, AV
Sorensen, K
TI Geology and petroleum potential of the rifted margins of the Canada
Basin
SO ARCTIC PETROLEUM GEOLOGY
SE Geological Society Memoirs
LA English
DT Proceedings Paper
CT 33rd International Geological Congress (IGC)
CY AUG 06-14, 2008
CL Oslo, NORWAY
SP Int Marine Minerals Soc, petr ind
ID BEAUFORT-MACKENZIE BASIN; BIOLOGICAL MARKER GEOCHEMISTRY; ARCTIC CANADA;
NORTH SLOPE; SOURCE-ROCK; CRUSTAL STRUCTURE; SVERDRUP BASIN; STRUCTURAL
EVOLUTION; AMERASIA BASIN; POLAR MARGIN
AB Three sides of the Canada Basin are bordered by high-standing, conjugate rift shoulders of the Chukchi Borderland, Alaska and Canada. The Alaska and Canada margins are mantled with thick, growth-faulted sediment prisms, and the Chukchi Borderland contains only a thin veneer of sediment. The rift-margin strata of Alaska and Canada reflect the tectonics and sediment dispersal systems of adjacent continental regions whereas the Chukchi Borderland was tectonically isolated from these sediment dispersal systems. Along the eastern Alaska-southern Canada margin, termed herein the 'Canning-Mackenzie deformed margin', the rifted margin is deformed by ongoing Brooks Range tectonism. Additional contractional structures occur in a gravity fold belt that may be present along the entire Alaska and Canada margins of the Canada Basin. Source-rock data inboard of the rift shoulders and regional palaeogeographic reconstructions suggest three potential source-rock intervals: Lower Cretaceous (Hauterivian-Albian), Upper Cretaceous (mostly Turonian) and Lower Palaeogene. Burial history modelling indicates favourable timing for generation from all three intervals beneath the Alaska and Canada passive margins, and an active petroleum system has been documented in the Canning-Mackenzie deformed margin. Assessment of undiscovered petroleum resources indicates the greatest potential in the Canning-Mackenzie deformed margin and significant potential in the Canada and Alaska passive margins.
C1 [Houseknecht, David W.] US Geol Survey, Reston, VA 20192 USA.
RP Houseknecht, DW (reprint author), US Geol Survey, Reston, VA 20192 USA.
EM dhouse@usgs.gov
NR 97
TC 15
Z9 16
U1 1
U2 11
PU GEOLOGICAL SOC PUBLISHING HOUSE
PI BATH
PA UNIT 7, BRASSMILL ENTERPRISE CTR, BRASSMILL LANE, BATH BA1 3JN, AVON,
ENGLAND
SN 0435-4052
BN 978-1-86239-328-8
J9 GEOL SOC MEM
PY 2011
VL 35
DI 10.1144/M35.34
PG 18
WC Geology
SC Geology
GA BYY32
UT WOS:000300715800034
ER
PT S
AU Klett, TR
Wandrey, CJ
Pitman, JK
AF Klett, T. R.
Wandrey, C. J.
Pitman, J. K.
BE Spencer, AM
Embry, AF
Gautier, DL
Stoupakova, AV
Sorensen, K
TI Geology and petroleum potential of the north and east margins of the
Siberian Craton, north of the Arctic Circle
SO ARCTIC PETROLEUM GEOLOGY
SE Geological Society Memoirs
LA English
DT Proceedings Paper
CT 33rd International Geological Congress (IGC)
CY AUG 06-14, 2008
CL Oslo, NORWAY
SP Int Marine Minerals Soc, petr ind
ID FOLD BELT; RUSSIA; EVOLUTION; BASIN
AB The Siberian Craton consists of crystalline rocks and superimposed Precambrian sedimentary rocks deposited in rift basins. Palaeozoic rocks, mainly carbonates, were deposited along the margins of the craton to form an outwardly younger concentric pattern that underlies an outward-thickening Mesozoic sedimentary section. The north and east margins of the Siberian Craton subsequently became foreland basins created by compressional deformation during collision with other tectonic plates. The Tunguska Basin developed as a Palaeozoic rift/sag basin over Proterozoic rifts. The geological provinces along the north and east margins of the Siberian Craton are immature with respect to exploration, so exploration-history analysis alone cannot be used for assessing undiscovered petroleum resources. Therefore, other areas from around the world having greater petroleum exploration maturity and similar geological characteristics, and which have been previously assessed, were used as analogues to aid in this assessment. The analogues included those of foreland basins and rift/sag basins that were later subjected to compression. The US Geological Survey estimated the mean undiscovered, technically recoverable conventional petroleum resources to be approximately 28 billion barrels of oil equivalent, including approximately 8 billion barrels of crude oil, 103 trillion cubic feet of natural gas and 3 billion barrels of natural gas liquids.
C1 [Klett, T. R.; Wandrey, C. J.; Pitman, J. K.] US Geol Survey, Denver Fed Ctr, Denver, CO 80225 USA.
RP Klett, TR (reprint author), US Geol Survey, Denver Fed Ctr, MS 939,Box 25046, Denver, CO 80225 USA.
EM tklett@usgs.gov
NR 83
TC 1
Z9 1
U1 0
U2 1
PU GEOLOGICAL SOC PUBLISHING HOUSE
PI BATH
PA UNIT 7, BRASSMILL ENTERPRISE CTR, BRASSMILL LANE, BATH BA1 3JN, AVON,
ENGLAND
SN 0435-4052
BN 978-1-86239-328-8
J9 GEOL SOC MEM
PY 2011
VL 35
DI 10.1144/M35.27
PG 19
WC Geology
SC Geology
GA BYY32
UT WOS:000300715800027
ER
PT S
AU Moore, TE
Grantz, A
Pitman, JK
Brown, PJ
AF Moore, Thomas E.
Grantz, Arthur
Pitman, Janet K.
Brown, Philip J.
BE Spencer, AM
Embry, AF
Gautier, DL
Stoupakova, AV
Sorensen, K
TI A first look at the petroleum geology of the Lomonosov Ridge
microcontinent, Arctic Ocean
SO ARCTIC PETROLEUM GEOLOGY
SE Geological Society Memoirs
LA English
DT Proceedings Paper
CT 33rd International Geological Congress (IGC)
CY AUG 06-14, 2008
CL Oslo, NORWAY
SP Int Marine Minerals Soc, petr ind
ID ALPHA-RIDGE; CRUSTAL STRUCTURE; SEDIMENTARY STRUCTURE;
CONTINENTAL-MARGIN; SEISMIC-REFRACTION; TECTONIC EVOLUTION; NORTHERN
RUSSIA; EURASIA BASIN; SEA; CONSTRAINTS
AB The Lomonosov microcontinent is an elongated continental fragment that transects the Arctic Ocean between North America and Siberia via the North Pole. Although it lies beneath polar pack ice, the geological framework of the microcontinent is inferred from sparse seismic reflection data, a few cores, potential field data and the geology of its conjugate margin in the Barents-Kara Shelf. Petroleum systems inferred to be potentially active are comparable to those sourced by condensed Triassic and Jurassic marine shale of the Barents Platform and by condensed Jurassic and (or) Cretaceous shale probably present in the adjacent Amerasia Basin. Cenozoic deposits are known to contain rich petroleum source rocks but are too thermally immature to have generated petroleum. For the 2008 USGS Circum Arctic Resource Appraisal (CARA), the microcontinent was divided into shelf and slope assessment units (AUs) at the tectonic hinge line along the Amerasia Basin margin. A low to moderate probability of accumulation in the slope AU yielded fully risked mean estimates of 123 MMBO oil and 740 BCF gas. For the shelf AU, no quantitative assessment was made because the probability of petroleum accumulations of the 50 MMBOE minimum size was estimated to be less than 10% owing to rift-related uplift, erosion and faulting.
C1 [Moore, Thomas E.] US Geol Survey, Menlo Pk, CA 94025 USA.
RP Moore, TE (reprint author), US Geol Survey, 345 Middlefield Rd, Menlo Pk, CA 94025 USA.
EM tmoore@usgs.gov
NR 94
TC 2
Z9 2
U1 0
U2 1
PU GEOLOGICAL SOC PUBLISHING HOUSE
PI BATH
PA UNIT 7, BRASSMILL ENTERPRISE CTR, BRASSMILL LANE, BATH BA1 3JN, AVON,
ENGLAND
SN 0435-4052
BN 978-1-86239-328-8
J9 GEOL SOC MEM
PY 2011
VL 35
DI 10.1144/M35.49
PG 19
WC Geology
SC Geology
GA BYY32
UT WOS:000300715800049
ER
PT S
AU Schenk, CJ
AF Schenk, Christopher J.
BE Spencer, AM
Embry, AF
Gautier, DL
Stoupakova, AV
Sorensen, K
TI Geology and petroleum potential of the West Greenland-East Canada
Province
SO ARCTIC PETROLEUM GEOLOGY
SE Geological Society Memoirs
LA English
DT Proceedings Paper
CT 33rd International Geological Congress (IGC)
CY AUG 06-14, 2008
CL Oslo, NORWAY
SP Int Marine Minerals Soc, petr ind
ID NORTHERN BAFFIN-BAY; LABRADOR SEA; NUUSSUAQ BASIN; ELLESMERE-ISLAND;
SEISMIC-REFRACTION; TECTONIC EVOLUTION; VOLCANIC MARGINS; EUREKAN
OROGENY; ATANE FORMATION; NEOGENE UPLIFT
AB The US Geological Survey (USGS) assessed the potential for undiscovered oil and gas resources of the West Greenland-East Canada Province as part of the USGS Circum-Arctic Resource Appraisal programme. The province lies in the offshore area between western Greenland and eastern Canada and includes Baffin Bay, Davis Strait, Lancaster Sound and Nares Strait west of and including part of Kane Basin. A series of major tectonic events led to the formation of several distinct structural domains that are the geological basis for defining five assessment units (AU) in the province, all of which are within the Mesozoic-Cenozoic Composite Petroleum System. Potential petroleum source rocks include strata of Ordovician, Lower and Upper Cretaceous, and Palaeogene ages. The five AUs defined for this study - the Eurekan Structures AU, NW Greenland Rifted Margin AU, NE Canada Rifted Margin AU, Baffin Bay Basin AU and the Greater Ungava Fault Zone AU - encompass the entire province and were assessed for undiscovered technically recoverable resources. The mean volumes of undiscovered resources for the West Greenland-East Canada Province are 10.7 x 10(9) barrels of oil, 75 x 10(12) cubic feet of gas, and 1.7 x 10(9) barrels of natural gas liquids. For the part of the province that is north of the Arctic Circle, the estimated mean volumes of these undiscovered resources are 7.3 x 10 9 barrels of oil, 52 x 10(12) cubic feet of natural gas, and 1.1 x 10(9) barrels of natural gas liquids.
C1 [Schenk, Christopher J.] US Geol Survey, Denver, CO 80225 USA.
RP Schenk, CJ (reprint author), US Geol Survey, MS 939,Box 25046, Denver, CO 80225 USA.
EM schenk@usgs.gov
NR 82
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PU GEOLOGICAL SOC PUBLISHING HOUSE
PI BATH
PA UNIT 7, BRASSMILL ENTERPRISE CTR, BRASSMILL LANE, BATH BA1 3JN, AVON,
ENGLAND
SN 0435-4052
BN 978-1-86239-328-8
J9 GEOL SOC MEM
PY 2011
VL 35
DI 10.1144/M35.41
PG 19
WC Geology
SC Geology
GA BYY32
UT WOS:000300715800041
ER
PT S
AU Schenk, CJ
AF Schenk, Christopher J.
BE Spencer, AM
Embry, AF
Gautier, DL
Stoupakova, AV
Sorensen, K
TI Geology and petroleum potential of the Timan-Pechora Basin Province,
Russia
SO ARCTIC PETROLEUM GEOLOGY
SE Geological Society Memoirs
LA English
DT Proceedings Paper
CT 33rd International Geological Congress (IGC)
CY AUG 06-14, 2008
CL Oslo, NORWAY
SP Int Marine Minerals Soc, petr ind
ID EVOLUTION; OILS
AB The Timan-Pechora Basin Province represents the northeastern-most cratonic block of Eastern European Russia. More than 16 billion barrels of oil (BBO) and 40 trillion cubic feet of gas (TCFG) have been discovered in this basin. Three geological assessment units (AU) were defined for assessing the potential for undiscovered oil and gas resources. The NW Izhma Depression AU encompasses all potential structures and reservoirs in the northwestern part of the Izhma-Pechora Depression, but this part of the basin contains little source and reservoir rocks and so was not assessed quantitatively. The Main Basin Platform AU includes all structures and reservoirs that developed in the central part of the basin where the tectonic evolution and development of petroleum systems were complex. The Foredeep Basins AU includes all potential reservoirs within the thick sedimentary section of the foredeep basins developed during the Permo-Triassic Uralian Orogeny. For the Timan-Pechora Basin Province, the estimated means of undiscovered resources are 3.3 BBO, 17 TCFG and 0.3 billion barrels of natural gas liquids (BBNGL). For the areas of the AUs north of the Arctic Circle in the Timan-Pechora Basin Province, the estimated means of undiscovered resources are 1.7 BBO, 9.0 TCFG and 0.2 BBNGL. The Pechora Sea was assessed with the South Barents Sea Province and is not included in this assessment.
C1 US Geol Survey, Denver, CO 80225 USA.
RP Schenk, CJ (reprint author), US Geol Survey, MS 939,Box 25046, Denver, CO 80225 USA.
EM schenk@usgs.gov
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PU GEOLOGICAL SOC PUBLISHING HOUSE
PI BATH
PA UNIT 7, BRASSMILL ENTERPRISE CTR, BRASSMILL LANE, BATH BA1 3JN, AVON,
ENGLAND
SN 0435-4052
BN 978-1-86239-328-8
J9 GEOL SOC MEM
PY 2011
VL 35
DI 10.1144/M35.18
PG 12
WC Geology
SC Geology
GA BYY32
UT WOS:000300715800018
ER
PT J
AU Spice, EK
Whitesel, TA
McFarlane, CT
Docker, MF
AF Spice, E. K.
Whitesel, T. A.
McFarlane, C. T.
Docker, M. F.
TI Characterization of 12 microsatellite loci for the Pacific lamprey,
Entosphenus tridentatus (Petromyzontidae), and cross-amplification in
five other lamprey species
SO GENETICS AND MOLECULAR RESEARCH
LA English
DT Article
DE Entosphenus; Lampetra richardsoni; Microsatellite; Pacific lamprey;
Petromyzontidae; Western brook lamprey
AB The Pacific lamprey (Entosphenus tridentatus) is an anadromous fish that is of conservation concern in North America and Asia. Data on Pacific lamprey population structure are scarce and conflicting, impeding conservation efforts. We optimized 12 polymorphic microsatellite loci for the Pacific lamprey. Three to 13 alleles per locus were observed in a sample of 51 fish collected from the West Fork Illinois River, Oregon. Observed heterozygosity ranged from 0.235 to 0.902 and expected heterozygosity ranged from 0.214 to 0.750. Cross-species amplification produced 8 to 12 polymorphic loci in four other Entosphenus species and in the western brook lamprey (Lampetra richardsoni). Two loci appear to be diagnostic for distinguishing Entosphenus from Lampetra. These markers will be valuable for evaluating population structure and making conservation decisions for E. tridentatus and other lamprey species.
C1 [Spice, E. K.; McFarlane, C. T.; Docker, M. F.] Univ Manitoba, Dept Biol Sci, Winnipeg, MB, Canada.
[Whitesel, T. A.] US Fish & Wildlife Serv, Columbia River Fisheries Program Off, Vancouver, WA USA.
RP Docker, MF (reprint author), Univ Manitoba, Dept Biol Sci, Winnipeg, MB, Canada.
EM dockerm@cc.umanitoba.ca
FU United States Fish and Wildlife Service (USFWS)
FX We thank Damon Goodman, Les Harris, Christina Luzier, Stewart Reid, Greg
Silver, and Eric B. Taylor for providing samples and intellectual
support, and the United States Fish and Wildlife Service (USFWS) for
financial support. Mention of trade names does not imply endorsement by
the USFWS. The findings and conclusions in this manuscript are those of
the authors and do not necessarily represent the views of the USFWS.
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PU FUNPEC-EDITORA
PI RIBEIRAO PRETO
PA RUA HUDSON 655, JARDIM CANADA, RIBEIRAO PRETO, SP, BRAZIL
SN 1676-5680
J9 GENET MOL RES
JI Genet. Mol. Res.
PY 2011
VL 10
IS 4
BP 3246
EP 3250
DI 10.4238/2011.December.22.2
PG 5
WC Biochemistry & Molecular Biology; Genetics & Heredity
SC Biochemistry & Molecular Biology; Genetics & Heredity
GA 897CA
UT WOS:000300617600099
PM 22194188
ER
PT J
AU Harris, JE
Hightower, JE
AF Harris, Julianne E.
Hightower, Joseph E.
TI Identification of American Shad Spawning Sites and Habitat Use in the
Pee Dee River, North Carolina and South Carolina
SO NORTH AMERICAN JOURNAL OF FISHERIES MANAGEMENT
LA English
DT Article
ID LOW-HEAD DAM; ALOSA-SAPIDISSIMA; ROANOKE RIVER; FISH PASSAGE; JAMES
RIVER; VIRGINIA; MIGRATION; UPSTREAM; MOVEMENT
AB We examined spawning site selection and habitat use by American shad Alosa sapidissima in the Pee Dee River, North Carolina and South Carolina, to inform future management in this flow-regulated river. American shad eggs were collected in plankton tows, and the origin (spawning site) of each egg was estimated; relocations of radio-tagged adults on spawning grounds illustrated habitat use and movement in relation to changes in water discharge rates. Most spawning was estimated to occur in the Piedmont physiographic region within a 25-river-kilometer (rkm) section just below the lowermost dam in the system; however, some spawning also occurred downstream in the Coastal Plain. The Piedmont region has a higher gradient and is predicted to have slightly higher current velocities and shallower depths, on average, than the Coastal Plain. The Piedmont region is dominated by large substrates (e. g., boulders and gravel), whereas the Coastal Plain is dominated by sand. Sampling at night (the primary spawning period) resulted in the collection of young eggs (<= 1.5 h old) that more precisely identified the spawning sites. In the Piedmont region, most radio-tagged American shad remained in discrete areas (average linear range = 3.6 rkm) during the spawning season and generally occupied water velocities between 0.20 and 0.69 m/s, depths between 1.0 and 2.9 m, and substrates dominated by boulder or bedrock and gravel. Tagged adults made only small-scale movements with changes in water discharge rates. Our results demonstrate that the upstream extent of migration and an area of concentrated spawning occur just below the lowermost dam. If upstream areas have similar habitat, facilitating upstream access for American shad could increase the spawning habitat available and increase the population's size.
C1 [Harris, Julianne E.; Hightower, Joseph E.] N Carolina State Univ, Dept Biol, N Carolina Cooperat Fish & Wildlife Res Unit, US Geol Survey, Raleigh, NC 27695 USA.
RP Harris, JE (reprint author), N Carolina State Univ, Dept Biol, N Carolina Cooperat Fish & Wildlife Res Unit, US Geol Survey, 127 David Clark Labs,Campus Box 7617, Raleigh, NC 27695 USA.
EM jeharris@ncsu.edu
FU National Marine Fisheries Service (National Oceanic and Atmospheric
Administration); North Carolina State University; North Carolina
Wildlife Resources Commission; U.S. Geological Survey; U.S. Fish and
Wildlife Service; Wildlife Management Institute
FX We thank Jason Brown, Prescott Brownell, Patrick Cooney, John
Crutchfield, Lindsey Garner, Ryan Heise, Brena Jones, Fritz Rohde, and
Mike Swing for help with study design and fieldwork. We are grateful to
Michael Fisk for contributing his expertise on the Pee Dee River, for
helping with field research, and for reviewing an earlier draft of this
document. We also thank Jay Holder for his comments on an earlier draft.
This study was funded by the National Marine Fisheries Service (National
Oceanic and Atmospheric Administration). The Cooperative Fish and
Wildlife Research Unit is jointly supported by North Carolina State
University, North Carolina Wildlife Resources Commission, U.S.
Geological Survey, U.S. Fish and Wildlife Service, and Wildlife
Management Institute. Any use of trade, product, or firm names is for
descriptive purposes only and does not imply endorsement by the U.S.
Government.
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PI PHILADELPHIA
PA 325 CHESTNUT ST, SUITE 800, PHILADELPHIA, PA 19106 USA
SN 0275-5947
J9 N AM J FISH MANAGE
JI North Am. J. Fish Manage.
PY 2011
VL 31
IS 6
BP 1019
EP 1033
DI 10.1080/02755947.2011.633686
PG 15
WC Fisheries
SC Fisheries
GA 902NJ
UT WOS:000301044900003
ER
PT J
AU Yuen, H
Conrad, R
AF Yuen, Henry
Conrad, Robert
TI Bias in the Estimation of Impacts of Simultaneous Mark-Selective and
Nonselective Fisheries on Ocean Salmon
SO NORTH AMERICAN JOURNAL OF FISHERIES MANAGEMENT
LA English
DT Article
AB The management models currently used in the Pacific Fishery Management Council's preseason planning process to project mortalities during proposed fisheries for coho salmon Oncorhynchus kisutch and Chinook salmon O. tshawytscha produce biased estimates of the mortalities in mark-selective fisheries and concurrent nonselective fisheries. The bias is caused by (1) unmarked fish encountering fishing gear more than once because of the required release of all unmarked fish and (2) the change in the unmarked-marked ratio resulting from the selective removal of marked salmon by the mark-selective fishery. Biased estimates of mortalities in nonselective fisheries operating during the same time and area as mark-selective fisheries occur because of the increasing unmarked-marked ratio in the common pool of salmon being fished. This bias is an increasing function of the stock exploitation rate on marked fish. The expected exploitation rates must also take into account mark-recognition errors whereby marked fish are released by mistake and unmarked fish are landed by mistake. The adjustment for mark-recognition error is a function of the unmarked-marked ratio.
C1 [Yuen, Henry] US Fish & Wildlife Serv, Vancouver, WA 98683 USA.
[Conrad, Robert] NW Indian Fisheries Commiss, Olympia, WA 98516 USA.
RP Yuen, H (reprint author), US Fish & Wildlife Serv, 1211 SE Cardinal Court,Suite 100, Vancouver, WA 98683 USA.
EM henry_yuen@fws.gov
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PI PHILADELPHIA
PA 325 CHESTNUT ST, SUITE 800, PHILADELPHIA, PA 19106 USA
SN 0275-5947
J9 N AM J FISH MANAGE
JI North Am. J. Fish Manage.
PY 2011
VL 31
IS 6
BP 1043
EP 1051
DI 10.1080/02755947.2011.635780
PG 9
WC Fisheries
SC Fisheries
GA 902NJ
UT WOS:000301044900005
ER
PT J
AU Riley, SC
Rinchard, J
Honeyfield, DC
Evans, AN
Begnoche, L
AF Riley, Stephen C.
Rinchard, Jacques
Honeyfield, Dale C.
Evans, Allison N.
Begnoche, Linda
TI Increasing Thiamine Concentrations in Lake Trout Eggs from Lakes Huron
and Michigan Coincide with Low Alewife Abundance
SO NORTH AMERICAN JOURNAL OF FISHERIES MANAGEMENT
LA English
DT Article
ID EARLY MORTALITY SYNDROME; GREAT-LAKES; SALVELINUS-NAMAYCUSH;
ALOSA-PSEUDOHARENGUS; RELATIVE ABUNDANCE; DEPTH DISTRIBUTION; ATLANTIC
SALMON; FATTY-ACIDS; COHO SALMON; BALTIC SEA
AB Lake trout Salvelinus namaycush in the Laurentian Great Lakes suffer from thiamine deficiency as a result of adult lake trout consuming prey containing thiaminase, a thiamine-degrading enzyme. Sufficiently low egg thiamine concentrations result in direct mortality of or sublethal effects on newly hatched lake trout fry. To determine the prevalence and severity of low thiamine in lake trout eggs, we monitored thiamine concentrations in lake trout eggs from 15 sites in Lakes Huron and Michigan from 2001 to 2009. Lake trout egg thiamine concentrations at most sites in both lakes were initially low and increased over time at 11 of 15 sites, and the proportion of females with egg thiamine concentrations lower than the recommended management objective of 4 nmol/g decreased over time at eight sites. Egg thiamine concentrations at five of six sites in Lakes Huron and Michigan were significantly inversely related to site-specific estimates of mean abundance of alewives Alosa pseudoharengus, and successful natural reproduction of lake trout has been observed in Lake Huron since the alewife population crashed. These results support the hypothesis that low egg thiamine in Great Lakes lake trout is associated with increased alewife abundance and that low alewife abundance may currently be a prerequisite for successful reproduction by lake trout in the Great Lakes.
C1 [Riley, Stephen C.; Rinchard, Jacques; Begnoche, Linda] US Geol Survey, Great Lakes Sci Ctr, Ann Arbor, MI 48105 USA.
[Honeyfield, Dale C.] US Geol Survey, No Appalachian Res Lab, Wellsboro, PA 16901 USA.
[Evans, Allison N.] Oregon State Univ, Dept Fisheries & Wildlife, Corvallis, OR 97330 USA.
RP Riley, SC (reprint author), US Geol Survey, Great Lakes Sci Ctr, 1451 Green Rd, Ann Arbor, MI 48105 USA.
EM sriley@usgs.gov
RI Mensinger, Allen/B-7349-2013
FU USGS-GLSC [1638]; USGS Leetown Science Center; Great Lakes Fishery
Commission; Great Lakes Fishery Trust
FX We thank the many individuals that collected eggs for thiamine
monitoring, including Steve Robillard and Dan Makauskas (Illinois DNR);
Brian Breidert and Randy Brindza (Indiana DNR); Tom Burzynski and
Bradley Eggold (Wisconsin DNR); Steve Lenart (Little Traverse Bay Band
of Ottawa Indians); Erik Olsen (Grand Traverse Bay Band of Ottawa and
Chippewa Indians); Archie Martell (Little River Band of Ottawa Indians);
Sergiusz Czesny (Illinois Natural History Survey); Dale Hanson, Mark
Holey, Scott Koproski, Adam Kowalski, and Aaron Woldt (U.S. Fish and
Wildlife Service); Ji He and James Johnson (Michigan DNR); Mark Ebener,
Amanda Handziak, and Greg Wright (Chippewa Ottawa Resource Authority);
and Adam Cottrill, David Reid, and Jeff Speers (Ontario Ministry of
Natural Resources). Courtenay Vining, Michael Gabor, Kimberly Smith,
Christina Accardi, Blake Snyder, and Robert Gerroux provided technical
assistance during sample analysis. Clifford Kraft, Don Tillitt, David
Warner, and two anonymous reviewers provided comments that improved the
manuscript. John Van Sickle (U.S. Environmental Protection Agency,
Corvallis, Oregon) provided helpful statistical advice. D. Bunnell
provided alewife abundance data for Lake Michigan.This work was funded
by the USGS-GLSC, the USGS Leetown Science Center, the Great Lakes
Fishery Commission's Fishery Research Program, and the Great Lakes
Fishery Trust. This is Contribution 1638 of the USGS-GLSC. Reference to
trade names does not imply endorsement by the U.S. Government.
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PU TAYLOR & FRANCIS INC
PI PHILADELPHIA
PA 530 WALNUT STREET, STE 850, PHILADELPHIA, PA 19106 USA
SN 0275-5947
EI 1548-8675
J9 N AM J FISH MANAGE
JI North Am. J. Fish Manage.
PY 2011
VL 31
IS 6
BP 1052
EP 1064
DI 10.1080/02755947.2011.641066
PG 13
WC Fisheries
SC Fisheries
GA 902NJ
UT WOS:000301044900006
ER
PT J
AU Burdick, SM
AF Burdick, Summer M.
TI Tag Loss and Short-Term Mortality Associated with Passive Integrated
Transponder Tagging of Juvenile Lost River Suckers
SO NORTH AMERICAN JOURNAL OF FISHERIES MANAGEMENT
LA English
DT Article
ID SURGICAL IMPLANTATION; PIT TAGS; RETENTION; GROWTH; SURVIVAL; FISH;
TRANSMITTERS; POPULATIONS; RECAPTURE; SALMON
AB Passive integrated transponder (PIT) tags are commonly used to mark small catostomids, but tag loss and the effect of tagging on mortality have not been assessed for juveniles of the endangered Lost River sucker Deltistes luxatus. I evaluated tag loss and short-term (34-d) mortality associated with the PIT tagging of juvenile Lost River suckers in the laboratory by using a completely randomized design and three treatment groups (PIT tagged, positive control, and control). An empty needle was inserted into each positive control fish, whereas control fish were handled but not tagged. Only one fish expelled its PIT tag. Mortality rate averaged 9.8 +/- 3.4% (mean +/- SD) for tagged fish; mortality was 0% for control and positive control fish. All tagging mortalities occurred in fish with standard lengths of 71 mm or less, and most of the mortalities occurred within 48 h of tagging. My results indicate that 12.45 x 2.02-mm PIT tags provide a viable method of marking juvenile Lost River suckers that are 72 mm or larger.
C1 US Geol Survey, Western Fisheries Res Ctr, Klamath Falls Field Stn, Klamath Falls, OR 97603 USA.
RP Burdick, SM (reprint author), US Geol Survey, Western Fisheries Res Ctr, Klamath Falls Field Stn, 2795 Anderson Ave, Klamath Falls, OR 97603 USA.
EM smburdick@usgs.gov
OI Burdick, Summer/0000-0002-3480-5793
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PI PHILADELPHIA
PA 530 WALNUT STREET, STE 850, PHILADELPHIA, PA 19106 USA
SN 0275-5947
EI 1548-8675
J9 N AM J FISH MANAGE
JI North Am. J. Fish Manage.
PY 2011
VL 31
IS 6
BP 1088
EP 1092
DI 10.1080/02755947.2011.641067
PG 5
WC Fisheries
SC Fisheries
GA 902NJ
UT WOS:000301044900009
ER
PT J
AU Herbst, SJ
Marsden, JE
Smith, SJ
AF Herbst, Seth J.
Marsden, J. Ellen
Smith, Stephen J.
TI Lake Whitefish in Lake Champlain after Commercial Fishery Closure and
Ecosystem Changes
SO NORTH AMERICAN JOURNAL OF FISHERIES MANAGEMENT
LA English
DT Article
ID LAMPREY PETROMYZON-MARINUS; COREGONUS-CLUPEAFORMIS;
SALVELINUS-NAMAYCUSH; MICHIGAN; POPULATIONS; SUPERIOR; HABITAT; GROWTH;
HURON; TROUT
AB Lake whitefish Coregonus clupeaformis were commercially fished in Lake Champlain until the 1913 fishery closure in U.S. waters. The only study of lake whitefish in the lake had been done in the 1930s. Our goals were to compare current biological parameters with historical information and to determine distribution and spatial differences in larval densities, with an emphasis on locating current spawning grounds, to gain insight on the current population in Lake Champlain. Adult lake whitefish (N = 545) were collected from 2006 to 2010 by using gill nets and trawls focused in the Main Lake. Larvae were collected extensively lakewide and intensively at Wilcox Cove and Rockwell Bay with an ichthyoplankton net. Population attributes (size, age, and sex composition; and growth, condition, and mortality) were typical of unexploited populations, as there was a wide range of length-classes (126-638 mm total length) and age-classes (1-26 years). Lake whitefish from the Main Lake had a high condition factor, and growth parameters were comparable with those of fish collected in the 1930s. Lake Champlain lake whitefish had greater asymptotic lengths than generally documented for the species. Larvae were found at sites throughout the Main Lake, and larval densities were among the highest recorded for the species (maximum = 2,558 larvae/1,000 m(3)); however, no lake whitefish were collected on the two historically documented spawning grounds. Lake whitefish in the Main Lake demonstrate characteristics of an unexploited population; however, evidence of spawning is absent or rare in portions of their historic range where habitat has been altered.
C1 [Herbst, Seth J.; Marsden, J. Ellen] Univ Vermont, Rubenstein Sch Environm & Nat Resources, Burlington, VT 05405 USA.
[Smith, Stephen J.] US Fish & Wildlife Serv, Lake Champlain Fish & Wildlife Resources Off, Essex Jct, VT 05452 USA.
RP Marsden, JE (reprint author), Univ Vermont, Rubenstein Sch Environm & Nat Resources, 81 Carrigan Dr, Burlington, VT 05405 USA.
EM ellen.marsden@uvm.edu
FU National Oceanic and Atmospheric Administration
FX We thank Shawn Good (VTFWD) for access to laboratory equipment. We also
thank Elias Rosenblatt, Neil Thompson, Josh Ashline, Kevin Osantowski,
Lindsay Schwarting, and Joanna Hatt for assistance in the field and
laboratory, and Richard Furbush, Joe Bartlett, and Rebecca Gorney for
assistance with fish collection. We especially thank the National
Oceanic and Atmospheric Administration for funding this project.
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PI PHILADELPHIA
PA 325 CHESTNUT ST, SUITE 800, PHILADELPHIA, PA 19106 USA
SN 0275-5947
J9 N AM J FISH MANAGE
JI North Am. J. Fish Manage.
PY 2011
VL 31
IS 6
BP 1106
EP 1115
DI 10.1080/02755947.2011.641068
PG 10
WC Fisheries
SC Fisheries
GA 902NJ
UT WOS:000301044900012
ER
PT J
AU Brown, PJ
Johnson, H
Zale, AV
AF Brown, Peter J.
Johnson, Heather
Zale, Alexander V.
TI Effect of Rainbow Trout Size on Response to Rotenone and Antimycin
SO NORTH AMERICAN JOURNAL OF FISHERIES MANAGEMENT
LA English
DT Article
ID ISOLATED-PERFUSED GILLS; ONCORHYNCHUS-MYKISS; ORGANIC-CHEMICALS;
TOXICITY; FISH
AB The piscicides rotenone and antimycin are commonly used to eradicate unwanted fish populations. However, the relationships (if present) between their toxicities and fish sizes are unknown and could be especially important when bioassay fish are used to detect piscicide presence and effectiveness. Size-mediated toxicity could lead to either excessive or inadequate piscicide applications if bioassay fish are larger or smaller than the fish being eradicated. The relationships between time to death and weight of rainbow trout Oncorhynchus mykiss (0.7-574.0 g) at an antimycin concentration of 7.5 mu g/L and a rotenone concentration of 12.5 mu g/L were determined. Antimycin took significantly longer than rotenone to kill rainbow trout at concentrations typically used in eradication projects. Significant positive relationships existed between fish size and time to death for rotenone and antimycin exposures and were probably caused by size-mediated differences in metabolic rate; however, these relationships accounted for less than 21% of the variation in time to death. Smaller fish appeared to be affected by the chemicals more quickly, but their deaths did not consistently occur before the deaths of larger fish.
C1 [Brown, Peter J.; Zale, Alexander V.] Montana State Univ, Dept Ecol, Montana Cooperat Fishery Res Unit, US Geol Survey, Bozeman, MT 59717 USA.
RP Brown, PJ (reprint author), Montana State Univ, Dept Ecol, Montana Cooperat Fishery Res Unit, US Geol Survey, Lewis Hall,POB 173460, Bozeman, MT 59717 USA.
EM peterbrown406@gmail.com
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PI PHILADELPHIA
PA 325 CHESTNUT ST, SUITE 800, PHILADELPHIA, PA 19106 USA
SN 0275-5947
EI 1548-8675
J9 N AM J FISH MANAGE
JI North Am. J. Fish Manage.
PY 2011
VL 31
IS 6
BP 1146
EP 1152
DI 10.1080/02755947.2011.646456
PG 7
WC Fisheries
SC Fisheries
GA 902NJ
UT WOS:000301044900016
ER
PT J
AU Neville, HM
Dunham, JB
AF Neville, Helen M.
Dunham, Jason B.
TI Patterns of Hybridization of Nonnative Cutthroat Trout and Hatchery
Rainbow Trout with Native Redband Trout in the Boise River, Idaho
SO NORTH AMERICAN JOURNAL OF FISHERIES MANAGEMENT
LA English
DT Article
ID ONCORHYNCHUS-CLARKII-LEWISI; ENDANGERED SPECIES ACT; SOUTHEASTERN
BRITISH-COLUMBIA; FISH INTRODUCTIONS; BROWN TROUT; SALMO-TRUTTA; BULL
TROUT; INTROGRESSIVE HYBRIDIZATION; SALVELINUS-FONTINALIS;
ENVIRONMENTAL-FACTORS
AB Hybridization is one of the greatest threats to native fishes. Threats from hybridization are particularly important for native trout species as stocking of nonnative trout has been widespread within the ranges of native species, thus increasing the potential for hybridization. While many studies have documented hybridization between native cutthroat trout Oncorhynchus clarkii and nonnative rainbow trout O. mykiss, fewer have focused on this issue in native rainbow trout despite widespread threats from introductions of both nonnative cutthroat trout and hatchery rainbow trout. Here, we describe the current genetic (i.e., hybridization) status of native redband trout O. mykiss gairdneri populations in the upper Boise River, Idaho. Interspecific hybridization was widespread (detected at 14 of the 41 sampled locations), but high levels of hybridization between nonnative cutthroat trout and redband trout were detected in only a few streams. Intraspecific hybridization was considerably more widespread (almost 40% of sampled locations), and several local populations of native redband trout have been almost completely replaced with hatchery coastal rainbow trout O. mykiss irideus; other populations exist as hybrid swarms, some are in the process of being actively invaded, and some are maintaining genetic characteristics of native populations. The persistence of some redband trout populations with high genetic integrity provides some opportunity to conserve native genomes, but our findings also highlight the complex decisions facing managers today. Effective management strategies in this system may include analysis of the specific attributes of each site and population to evaluate the relative risks posed by isolation versus maintaining connectivity, identifying potential sites for control or eradication of nonnative trout, and long-term monitoring of the genetic integrity of remaining redband trout populations to track changes in their status.
C1 [Neville, Helen M.] Trout Unlimited, Boise, ID 83702 USA.
[Dunham, Jason B.] US Geol Survey, Forest & Rangeland Ecosyst Sci Ctr, Corvallis, OR 97331 USA.
RP Neville, HM (reprint author), Trout Unlimited, 910 W Main St,Suite 342, Boise, ID 83702 USA.
EM hneville@tu.org
FU Trout Unlimited (TU); Embrace-A-Stream grant; U.S. Geological Survey's
Forest and Rangeland Ecosystem Science Center; Boise National Forest;
National Fire Plan, U.S. Forest Service Rocky Mountain Research Station,
U.S. Forest Service regions 1 and 4; Rangeland Ecosystem Science Center
FX This study was funded by Trout Unlimited (TU) through salary support to
H.M.N. and an Embrace-A-Stream grant to the Ted Trueblood Chapter of TU.
We thank the many members of the Ted Trueblood Chapter and the Boise
Valley Fly Fishermen; Mike Kellet (Boise National Forest); and Jeff
Dillon, Lance Hebdon, Sharon Clark, Liz Mamer, Chris Kozfkay, and Stacey
Dauwalter (IDFG) for their assistance in sample collection and providing
stocking information. We are grateful to Veronica Kirchoff and Mary
Peacock (University of Nevada) for performing the laboratory work and to
Matt Mayfield and Sabrina Beus (TU) for help with figures. This
manuscript was greatly improved by comments from Chris Kozfkay, Jeff
Dillon, Dan Dauwalter, Jack Williams, Stephen Bennett, and four
anonymous reviewers. The previous study was funded by the National Fire
Plan, U.S. Forest Service Rocky Mountain Research Station, U.S. Forest
Service regions 1 and 4, the U.S. Geological Survey's Forest and
Rangeland Ecosystem Science Center, and the Boise National Forest. For
acknowledgment of the many additional people who helped with this study,
please see Neville et al. (2009). Reference to trade names does not
imply endorsement by the U.S. Government.
NR 65
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U1 0
U2 23
PU TAYLOR & FRANCIS INC
PI PHILADELPHIA
PA 325 CHESTNUT ST, SUITE 800, PHILADELPHIA, PA 19106 USA
SN 0275-5947
J9 N AM J FISH MANAGE
JI North Am. J. Fish Manage.
PY 2011
VL 31
IS 6
BP 1163
EP 1176
DI 10.1080/02755947.2011.647252
PG 14
WC Fisheries
SC Fisheries
GA 902NJ
UT WOS:000301044900018
ER
PT S
AU Kokaly, RF
King, TVV
Hoefen, TM
AF Kokaly, Raymond F.
King, Trude V. V.
Hoefen, Todd M.
GP IEEE
TI MAPPING THE DISTRIBUTION OF MATERIALS IN HYPERSPECTRAL DATA USING THE
USGS MATERIAL IDENTIFICATION AND CHARACTERIZATION ALGORITHM (MICA)
SO 2011 IEEE INTERNATIONAL GEOSCIENCE AND REMOTE SENSING SYMPOSIUM (IGARSS)
SE IEEE International Symposium on Geoscience and Remote Sensing IGARSS
LA English
DT Proceedings Paper
CT IEEE International Geoscience and Remote Sensing Symposium (IGARSS)
CY JUL 24-29, 2011
CL Vancouver, CANADA
SP IEEE, Inst Elect & Elect Engineers Geosci & Remote Sensing Soc (IEEE GRSS)
C1 [Kokaly, Raymond F.; King, Trude V. V.; Hoefen, Todd M.] US Geol Survey, Reston, VA 20191 USA.
RP Kokaly, RF (reprint author), US Geol Survey, Reston, VA 20191 USA.
RI Kokaly, Raymond/A-6817-2017
OI Kokaly, Raymond/0000-0003-0276-7101
NR 3
TC 0
Z9 0
U1 0
U2 3
PU IEEE
PI NEW YORK
PA 345 E 47TH ST, NEW YORK, NY 10017 USA
SN 2153-6996
BN 978-1-4577-1005-6
J9 INT GEOSCI REMOTE SE
PY 2011
BP 1569
EP 1572
DI 10.1109/IGARSS.2011.6049370
PG 4
WC Engineering, Electrical & Electronic; Geosciences, Multidisciplinary;
Remote Sensing
SC Engineering; Geology; Remote Sensing
GA BXX72
UT WOS:000297496301157
ER
PT S
AU Jones, C
Bawden, G
Deverel, S
Dudas, J
Hensley, S
AF Jones, Cathleen
Bawden, Gerald
Deverel, Steven
Dudas, Joel
Hensley, Scott
GP IEEE
TI CHARACTERIZING LAND SURFACE CHANGE AND LEVEE STABILITY IN THE
SACRAMENTO-SAN JOAQUIN DELTA USING UAVSAR RADAR IMAGERY
SO 2011 IEEE INTERNATIONAL GEOSCIENCE AND REMOTE SENSING SYMPOSIUM (IGARSS)
SE IEEE International Symposium on Geoscience and Remote Sensing IGARSS
LA English
DT Proceedings Paper
CT IEEE International Geoscience and Remote Sensing Symposium (IGARSS)
CY JUL 24-29, 2011
CL Vancouver, CANADA
SP IEEE, Inst Elect & Elect Engineers Geosci & Remote Sensing Soc (IEEE GRSS)
AB The islands of the Sacramento-San Joaquin Delta have been subject to subsidence since they were first reclaimed from the estuary marshlands starting over 100 years ago, with most of the land currently lying below mean sea level. This area, which is the primary water resource of the state of California, is under constant threat of inundation from levee failure. Since July 2009, we have been imaging the area using the quad-polarimetric UAVSAR L-band radar, with eighteen data sets collected as of April 2011. Here we report results of our polarimetric and differential interferometric analysis of the data for levee deformation and land surface change.
C1 [Jones, Cathleen; Hensley, Scott] CALTECH, Jet Prop Lab, Pasadena, CA 91125 USA.
[Bawden, Gerald] USGS, California Water Sci Ctr, Sacramento, CA USA.
[Deverel, Steven] Hydrofocus Inc, Davis, CA USA.
[Hensley, Scott] Delta Suisun Marsh Off, California Dept Water Resources, Davis, CA USA.
RP Jones, C (reprint author), CALTECH, Jet Prop Lab, Pasadena, CA 91125 USA.
NR 2
TC 4
Z9 4
U1 0
U2 7
PU IEEE
PI NEW YORK
PA 345 E 47TH ST, NEW YORK, NY 10017 USA
SN 2153-6996
BN 978-1-4577-1005-6
J9 INT GEOSCI REMOTE SE
PY 2011
BP 1638
EP 1641
DI 10.1109/IGARSS.2011.6049546
PG 4
WC Engineering, Electrical & Electronic; Geosciences, Multidisciplinary;
Remote Sensing
SC Engineering; Geology; Remote Sensing
GA BXX72
UT WOS:000297496301175
ER
PT J
AU Wiles, GJ
O'Shea, TJ
Worthington, DJ
Esselstyn, JA
Valdez, EW
AF Wiles, Gary J.
O'Shea, Thomas J.
Worthington, David J.
Esselstyn, Jacob A.
Valdez, Ernest W.
TI Status and natural history of Emballonura semicaudata rotensis on
Aguiguan, Mariana Islands
SO ACTA CHIROPTEROLOGICA
LA English
DT Article
ID TEMPERATURE REGULATION; BATS; VERTEBRATES; METABOLISM; GUAM
AB Pacific sheath-tailed bats (Emballonura semicaudata rotensis) in the Mariana Islands declined greatly in abundance and distribution during the 20th century. The small island of Aguiguan now supports the only persisting population. We studied abundance and natural history of this population from 1995-2008. There was a likely population increase during the study, with 359-466 (minimum and maximum) bats counted at caves in 2008. Bats roosted only in caves, primarily those of relatively larger size. Bats were detected in only seven of 95 caves; three caves were always occupied when surveyed. One cave consistently had the largest colony ((x) over bar +/- SD +/- 333 33.6 in 2008). Others held 1-64 bats. Cave environments showed no complexities in temperature or humidity. Preliminary observations indicate a litter size of one and the possibility of birthing timed to coincide with the transitional period leading into the rainy season (June July). We review potential threats to E. s. rotensis on Aguiguan and make suggestions for conservation.
C1 [O'Shea, Thomas J.] US Geol Survey, Ft Collins Sci Ctr, Ft Collins, CO 80526 USA.
[Worthington, David J.; Esselstyn, Jacob A.] Div Fish & Wildlife, Rota, CM 96951 USA.
[Valdez, Ernest W.] US Geol Survey, Ft Collins Sci Ctr, Dept Biol, Albuquerque, NM 87131 USA.
[Wiles, Gary J.] Div Aquat & Wildlife Resources, Mangilao, GU 96913 USA.
RP Wiles, GJ (reprint author), Washington Dept Fish & Wildlife, 600 Capitol Way N, Olympia, WA 98501 USA.
EM wilesharkey@yahoo.com
FU U.S. Fish and Wildlife Service; Ecological Services office in Honolulu,
Hawaii; U.S. Navy
FX Funding was provided by the U.S. Fish and Wildlife Service's Federal Aid
to Wildlife Restoration Projects in the CNMI and Guam, and its
Ecological Services office in Honolulu, Hawaii, and from the U.S. Navy
through an interagency agreement with the U.S. Fish and Wildlife Service
and U.S. Geological Survey. Any use of trade, product, or firm names in
this publication is for descriptive purposes only and does not imply
endorsement by the U.S. Government. We thank A. Marshall and C. Kessler
for organizing the 1995 and 2008 surveys, respectively. For assistance
with fieldwork and logistics, we are grateful to E. Masga, E. Taisacan,
V. Camacho, M. Gorresen, R. Ulloa, D. Reyes, J. Omar, E. Campbell, A.
Marshall, H. King, F. Muna, G. Camacho, M. Palacios, R. Camacho, D.
Evangelista, J. Salas, T. Castro, J. Camacho, F. Bonaccorso, and D.
Grout. Many other CNMI Division of Fish and Wildlife (DFW) staff
participated in trips to the island since 1983 and we acknowledge their
contributions. S. Igisomar of the DFW facilitated work in 2008, carried
out under CNMI Scientific Research Permit 01048-08. We thank M. Gorresen
for preparing the figure, and J. de Cruz, K. Stafford, and F. Amidon for
supplying additional information. Helpful comments on the manuscript
were provided by P. Cryan, M. Neubaum, and D. Neubaum.
NR 59
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U1 3
U2 10
PU MUSEUM & INST ZOOLOGY PAS-POLISH ACAD SCIENCES
PI WARSAW
PA WILCZA STREET 64, 00-679 WARSAW, POLAND
SN 1508-1109
J9 ACTA CHIROPTEROL
JI Acta Chiropt.
PY 2011
VL 13
IS 2
BP 299
EP 309
DI 10.3161/150811011X624785
PG 11
WC Zoology
SC Zoology
GA 901ZJ
UT WOS:000301008100006
ER
PT J
AU Johnson, JB
Edwards, JW
Ford, WM
AF Johnson, Joshua B.
Edwards, John W.
Ford, W. Mark
TI Nocturnal activity patterns of northern myotis (Myotis septentrionalis)
during the maternity season in West Virginia (USA)
SO ACTA CHIROPTEROLOGICA
LA English
DT Article
DE Anabat; bats; Myotis septentrionalis; night-roosting; northern myotis;
West Virginia
ID FEMALE HOARY BATS; LONG-EARED BATS; BROWN BAT; LASIURUS-CINEREUS;
ROOSTING ECOLOGY; LUCIFUGUS; FOREST; SELECTION; BEHAVIOR; INDIANA
AB Nocturnal activity patterns of northern myotis (Myotis septentrionalis) at diurnal roost trees remain largely uninvestigated. For example, the influence of reproductive status, weather, and roost tree and surrounding habitat characteristics on timing of emergence, intra-night activity, and entrance at their roost trees is poorly known. We examined nocturnal activity patterns of northern myotis maternity colonies during pregnancy and lactation at diurnal roost trees situated in areas that were and were not subjected to recent prescribed fires at the Fernow Experimental Forest, West Virginia from 2007 to 2009. According to exit counts and acoustic data, northern myotis colony sizes were similar between reproductive periods and roost tree settings. However, intra-night activity patterns differed slightly between reproductive periods and roost trees in burned and non-burned areas. Weather variables poorly explained variation in activity patterns during pregnancy, but precipitation and temperature were negatively associated with activity patterns during lactation.
C1 [Johnson, Joshua B.; Edwards, John W.] W Virginia Univ, Div Forestry & Nat Resources, Morgantown, WV 26506 USA.
[Ford, W. Mark] Virginia Polytech Inst & State Univ, Virginia Cooperat Fish & Wildlife Res Unit, US Geol Survey, Blacksburg, VA 24061 USA.
RP Johnson, JB (reprint author), W Virginia Univ, Div Forestry & Nat Resources, Box 6125, Morgantown, WV 26506 USA.
EM j-johnson3@juno.com
FU U.S. Forest Service Northern Research Station [06-JV-11242300-140,
06-CO-112331-034]
FX The USDA Forest Service Northern Research Station Joint Venture
Agreement 06-JV-11242300-140 provided primary funding for our study from
the National Fire Plan to West Virginia University, Division of Forestry
and Natural Resources. Funding for prescribed burning was provided by a
grant from Florida Power and Light and BHE Environmental to the U.S.
Forest Service Northern Research Station through Collection Agreement
06-CO-112331-034. We thank the staff of the USDA Forest Service
Monongahela National Forest and the USDA Forest Service Northern
Research Station Timber and Watershed Laboratory for conducting the
prescribed burns. J. Rodrigue graciously provided field assistance. We
thank F. Wood for providing weather data.
NR 44
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U1 4
U2 33
PU MUSEUM & INST ZOOLOGY PAS-POLISH ACAD SCIENCES
PI WARSAW
PA WILCZA STREET 64, 00-679 WARSAW, POLAND
SN 1508-1109
J9 ACTA CHIROPTEROL
JI Acta Chiropt.
PY 2011
VL 13
IS 2
BP 391
EP 397
DI 10.3161/150811011X624866
PG 7
WC Zoology
SC Zoology
GA 901ZJ
UT WOS:000301008100014
ER
PT J
AU Arrott, M
Alexander, C
Graybeal, J
Mueller, C
Signell, R
de La Beaujardiere, J
Taylor, A
Wilkin, J
Powell, B
Orcutt, J
AF Arrott, Matthew
Alexander, Charles
Graybeal, John
Mueller, Christopher
Signell, Richard
de La Beaujardiere, Jeff
Taylor, Arthur
Wilkin, John
Powell, Brian
Orcutt, John
GP IEEE
TI Building transparent data access for ocean observatories: Coordination
of US IOOS DMAC with NSF's OOI Cyberinfrastructure
SO OCEANS 2011
LA English
DT Proceedings Paper
CT MTS/IEEE OCEANS Conference
CY SEP 19-22, 2011
CL Kona, HI
SP Marine Technol Soc (MTS), IEEE, OES
DE data access; ocean observatories; US IOOS; OOI; cyberinfrastructure;
coastal modelers; DMAC
AB The NOAA-led U. S. Integrated Ocean Observing System (IOOS) and the National Science Foundation's Ocean Observatories Initiative (OOI) have been collaborating since 2007 on advanced tools and technologies that ensure open access to ocean observations and models. Initial collaboration focused on serving ocean data via cloud computing - a key component of the OOI cyberinfrastructure (CI) architecture. As the OOI transitioned from planning to execution in the Fall of 2009, an OOI/IOOS team developed a customer-based "use case" to align more closely with the emerging objectives of OOI-CI team's first software release scheduled for Summer 2011 and provide a quantitative capacity for stress-testing these tools and protocols. A requirements process was initiated with coastal modelers, focusing on improved workflows to deliver ocean observation data. Accomplishments to date include the documentation and assessment of scientific workflows for two "early adopter" modeling teams from IOOS Regional partners (Rutgers - the State University of New Jersey and University of Hawaii's School of Ocean and Earth Science and Technology) to enable full understanding of data sources and needs; generation of all-inclusive lists of the data sets required and those obtainable through IOOS; a more complete understanding of areas where IOOS can expand data access capabilities to better serve the needs of the modeling community; and development of "data set agents" (software) to facilitate data acquisition from numerous data providers and conversions of the data format to the OOI-CI canonical form.
C1 [Arrott, Matthew; Graybeal, John] Univ Calif San Diego, Calit2, La Jolla, CA 92093 USA.
[Alexander, Charles; de La Beaujardiere, Jeff] NOAA, US IOOS Program Off, Silver Spring, MD 20910 USA.
[Mueller, Christopher] Appl Sci Assoc Inc, S Kingstown, RI USA.
[Signell, Richard] USGS, Woods Hole Coastal & Marine Sci Ctr, Woods Hole, MA 02543 USA.
[Taylor, Arthur] NOAA, Natl Weather Serv, Meteorolog Dev Lab, Silver Spring, MD 20910 USA.
[Wilkin, John] Rutgers State Univ, Inst Marine & Coastal Sci, New Brunswick, NJ 08901 USA.
[Powell, Brian] Univ HI, Sch Oceanog & Earth Sci & Technol, Honolulu, HI 96822 USA.
[Orcutt, John] UCSD, Scripps Inst Oceanog, La Jolla, CA 92093 USA.
RP Arrott, M (reprint author), Univ Calif San Diego, Calit2, La Jolla, CA 92093 USA.
FU JOI [JSA7-11]; NSF [OCE-0418967]; Consortium for Ocean Leadership, Inc.;
NOAA [NA17RJ1231]; Scripps Institution of Oceanography University of
California, San Diego
FX The OOI Cyberinfrastructure effort described in this paper is funded
through the JOI Subaward, JSA7-11, which in turn is funded by the NSF
contract OCE-0418967 with the Consortium for Ocean Leadership, Inc. The
intial OOI- IOOS collaboration described in this paper was funded
through the NOAA cooperative agreement # NA17RJ1231, with the Scripps
Institution of Oceanography University of California, San Diego.
NR 10
TC 0
Z9 0
U1 0
U2 3
PU IEEE
PI NEW YORK
PA 345 E 47TH ST, NEW YORK, NY 10017 USA
BN 978-0-933957-39-8
PY 2011
PG 9
WC Engineering, Multidisciplinary; Engineering, Electrical & Electronic
SC Engineering
GA BYJ22
UT WOS:000299005800089
ER
PT J
AU Wei, Y
Titov, VV
Newman, A
Hayes, G
Tang, LJ
Chamberlin, C
AF Wei, Yong
Titov, Vasily V.
Newman, Andrew
Hayes, Gavin
Tang, Liujuan
Chamberlin, Chris
GP IEEE
TI Near-Field Hazard Assessment of March 11, 2011 JapanTsunami Sources
Inferred from Different Methods
SO OCEANS 2011
LA English
DT Proceedings Paper
CT MTS/IEEE OCEANS Conference
CY SEP 19-22, 2011
CL Kona, HI
SP Marine Technol Soc (MTS), IEEE, OES
DE tsunameter; GPS; finite-fault solution; tsunami; tsunami forecast;
runup; inundation; near field
ID TOHOKU-OKI EARTHQUAKE; INDIAN-OCEAN TSUNAMI; MEGATHRUST; INVERSION;
MODELS; FAULT; GPS
AB Tsunami source is the origin of the subsequent transoceanic water waves, and thus the most critical component in modern tsunami forecast methodology. Although impractical to be quantified directly, a tsunami source can be estimated by different methods based on a variety of measurements provided by deep-ocean tsunameters, seismometers, GPS, and other advanced instruments, some in real time, some in post real-time. Here we assess these different sources of the devastating March 11, 2011 Japan tsunami by model-data comparison for generation, propagation and inundation in the near field of Japan. This study provides a comparative study to further understand the advantages and shortcomings of different methods that may be potentially used in real-time warning and forecast of tsunami hazards, especially in the near field. The model study also highlights the critical role of deep-ocean tsunami measurements for high-quality tsunami forecast, and its combination with land GPS measurements may lead to better understanding of both the earthquake mechanisms and tsunami generation process.
C1 [Wei, Yong; Tang, Liujuan; Chamberlin, Chris] Univ Washington, Joint Inst Study Ocean & Atmosphere, Seattle, WA 98195 USA.
[Wei, Yong; Titov, Vasily V.; Tang, Liujuan; Chamberlin, Chris] NOAA, Ctrtsunami Res, Pacific Marine Environm Lab, Seattle, WA 98164 USA.
[Tang, Liujuan] Sch Earth & Atmospher Sci, Georgia Inst Technol, Atlanta, GA 30334 USA.
[Hayes, Gavin] Natl Informat Ctr Earthquake, US Geolog Survey, Denver, CO 80225 USA.
RP Wei, Y (reprint author), Univ Washington, Joint Inst Study Ocean & Atmosphere, Seattle, WA 98195 USA.
RI Newman, Andrew/E-7682-2012; Wei, Yong/I-3462-2015
OI Newman, Andrew/0000-0001-7414-1197; Wei, Yong/0000-0002-6908-1342
NR 32
TC 0
Z9 0
U1 0
U2 6
PU IEEE
PI NEW YORK
PA 345 E 47TH ST, NEW YORK, NY 10017 USA
BN 978-0-933957-39-8
PY 2011
PG 9
WC Engineering, Multidisciplinary; Engineering, Electrical & Electronic
SC Engineering
GA BYJ22
UT WOS:000299005801195
ER
PT J
AU Wynn, J
Urquhart, S
Williamson, M
Fleming, J
AF Wynn, Jeff
Urquhart, Scott
Williamson, Mike
Fleming, John
GP IEEE
TI An Open-Water Electrical Geophysical Tool for Mapping Sub-Seafloor Heavy
Placer Minerals in 3D and Migrating Hydrocarbon Plumes in 4D
SO OCEANS 2011
LA English
DT Proceedings Paper
CT MTS/IEEE OCEANS Conference
CY SEP 19-22, 2011
CL Kona, HI
SP Marine Technol Soc (MTS), IEEE, OES
DE tracking hydrocarbon plumes; seafloor minerals; induced polarization;
sub-seafloor mapping; electrical geophysical tool; heavy placer
minerals; hydrocarbons in seawater
AB A towed-streamer technology has been developed for mapping placer heavy minerals and dispersed hydrocarbon plumes in the open ocean. The approach uses induced polarization (IP), an electrical measurement that encompasses several different surface-reactive capacitive and electrochemical phenomena, and thus is ideally suited for mapping dispersed or disseminated targets. The application is operated at sea by towing active electrical geophysical streamers behind a ship; a wide area can be covered in three dimensions by folding towpaths over each other in lawn-mower fashion. This technology has already been proven in laboratory and ocean settings to detect IP-reactive titanium-and rare-earth (REE) minerals such as ilmenite and monazite. By extension, minerals that weather and accumulate/concentrate by a similar mechanism, including gold, platinum, and diamonds, may be rapidly detected and mapped indirectly-- even when dispersed and covered with thick, inert sediment. IP is also highly reactive to metal structures such as pipelines and cables.
Currently, the only means for mapping an oil-spill plume is to park a large ship in the ocean and drop a sampling string over the side, requiring hours of time per sampling point. The samples must then be chemically analyzed, adding additional time and expense. We believe that an extension of the marine IP technology could also apply to rapidly mapping both seafloor-blanket and disseminated hydrocarbon plumes in the open ocean, as hydrocarbon droplets in conductive seawater are topologically equivalent to a metal-plates-and-dielectric capacitor. Because the effective capacitance would be frequency-dependent on droplet size, the approach we advocate holds the potential to not only map, but also to characterize the evolution and degradation of such a plume over time. In areas where offshore oil field development has been practiced for extended periods, making IP measurements from a towed streamer may be useful for locating buried and exposed pipelines, as well as pipeline leaks. We believe this technique will be a more cost-effective method than drop-sampling to map and monitor hydrocarbon plumes in open ocean settings.
A marine induced polarization system was used successfully to map a 15 km x 45 km swath of the ocean floor off eastern South Africa with 3-meter sampling along 200-meter-separated profiles.The survey detected titanium-bearing sands up to 15 meters below the seafloor. From preliminary laboratory work it is apparent that we can extend this technology to monitor significant environmental problems including anthropogenic and industrial waste washed into sensitive estuaries and sounds during storm-water runoff episodes, and also to map and characterize dispersed oil plumes in the seawater column in three dimensions, as well as movement and dispersal of both over time.
C1 [Wynn, Jeff] US Geol Survey, Vancouver, WA USA.
[Williamson, Mike] Wilson & Assoc, Seattle, WA 98101 USA.
[Urquhart, Scott; Fleming, John] Zonge Internat, Tucson, AZ 85716 USA.
RP Wynn, J (reprint author), US Geol Survey, Vancouver, WA USA.
EM jwynn@usgs.gov; scottu@zonge.us; mikew@wassoc.com; johnf@zonge.us
NR 16
TC 0
Z9 0
U1 0
U2 3
PU IEEE
PI NEW YORK
PA 345 E 47TH ST, NEW YORK, NY 10017 USA
BN 978-0-933957-39-8
PY 2011
PG 6
WC Engineering, Multidisciplinary; Engineering, Electrical & Electronic
SC Engineering
GA BYJ22
UT WOS:000299005801187
ER
PT J
AU Stolz, JF
Oremland, RS
AF Stolz, John F.
Oremland, Ronald S.
BE Stolz, JF
Oremland, RS
TI Microbial Metal and Metalloid Metabolism ADVANCES AND APPLICATIONS
PREFACE
SO MICROBIAL METAL AND METALLOID METABOLISM: ADVANCES AND APPLICATIONS
LA English
DT Editorial Material; Book Chapter
C1 [Stolz, John F.] Duquesne Univ, Dept Biol Sci, Pittsburgh, PA 15282 USA.
[Oremland, Ronald S.] US Geol Survey, Div Water Resources, Menlo Pk, CA 94025 USA.
RP Stolz, JF (reprint author), Duquesne Univ, Dept Biol Sci, Pittsburgh, PA 15282 USA.
NR 3
TC 0
Z9 0
U1 0
U2 2
PU AMER SOC MICROBIOLOGY
PI WASHINGTON
PA 1752 N STREET NW, WASHINGTON, DC 20036-2904 USA
BN 978-1-55581-719-0
PY 2011
BP XIII
EP +
PG 4
WC Biotechnology & Applied Microbiology; Environmental Sciences;
Microbiology
SC Biotechnology & Applied Microbiology; Environmental Sciences & Ecology;
Microbiology
GA BYN80
UT WOS:000299464700001
ER
PT J
AU Pearce, CI
Baesman, SM
Blum, JS
Fellowes, JW
Oremland, RS
AF Pearce, Carolyn I.
Baesman, Shaun M.
Blum, Jodi Switzer
Fellowes, Jonathan W.
Oremland, Ronald S.
BE Stolz, JF
Oremland, RS
TI NANOPARTICLES FORMED FROM MICROBIAL OXYANION REDUCTION OF TOXIC GROUP 15
AND GROUP 16 METALLOIDS
SO MICROBIAL METAL AND METALLOID METABOLISM: ADVANCES AND APPLICATIONS
LA English
DT Article; Book Chapter
ID ENTEROBACTER-CLOACAE SLD1A-1; REDUCING BACTERIAL BIOFILMS; ELEMENTAL
SELENIUM; SP NOV.; MONO LAKE; RESPIRING BACTERIA; SELENATE REDUCTION;
THAUERA-SELENATIS; DISSIMILATORY REDUCTION; RHODOBACTER-SPHAEROIDES
C1 [Pearce, Carolyn I.] Pacific NW Natl Lab, Richland, WA 99352 USA.
[Baesman, Shaun M.; Blum, Jodi Switzer; Oremland, Ronald S.] US Geol Survey, Div Water Resources, Menlo Pk, CA 94025 USA.
[Fellowes, Jonathan W.] Univ Manchester, Sch Earth Atmospher & Environm Sci, Manchester M13 9PL, Lancs, England.
RP Pearce, CI (reprint author), Pacific NW Natl Lab, Richland, WA 99352 USA.
NR 99
TC 3
Z9 3
U1 0
U2 6
PU AMER SOC MICROBIOLOGY
PI WASHINGTON
PA 1752 N STREET NW, WASHINGTON, DC 20036-2904 USA
BN 978-1-55581-719-0
PY 2011
BP 297
EP +
PG 25
WC Biotechnology & Applied Microbiology; Environmental Sciences;
Microbiology
SC Biotechnology & Applied Microbiology; Environmental Sciences & Ecology;
Microbiology
GA BYN80
UT WOS:000299464700017
ER
PT J
AU Toda, S
Lin, J
Stein, RS
AF Toda, Shinji
Lin, Jian
Stein, Ross S.
TI Using the 2011 M-w 9.0 off the Pacific coast of Tohoku Earthquake to
test the Coulomb stress triggering hypothesis and to calculate faults
brought closer to failure
SO EARTH PLANETS AND SPACE
LA English
DT Article
DE Coulomb stress change; Tohoku Earthquake; stress triggering; remote
aftershocks
ID SEISMICITY; SHADOWS; SLIP
AB The 11 March 2011 Tohoku Earthquake provides an unprecedented test of the extent to which Coulomb stress transfer governs the triggering of aftershocks. During 11-31 March, there were 177 aftershocks with focal mechanisms, and so the Coulomb stress change imparted by the rupture can be resolved on the aftershock nodal planes to learn whether they were brought closer to failure. Numerous source models for the mainshock have been inverted from seismic, geodetic, and tsunami observations. Here, we show that, among six tested source models, there is a mean 47% gain in positively-stressed aftershock mechanisms over that for the background (1997-10 March 2011) earthquakes, which serve as the control group. An aftershock fault friction of 0.4 is found to fit the data better than 0.0 or 0.8, and among all the tested models, Wei and Sladen (2011) produced the largest gain, 63%. We also calculate that at least 5 of the seven large, exotic, or remote aftershocks were brought >= 0.3 bars closer to failure. With these tests as confirmation, we calculate that large sections of the Japan trench megathrust, the outer trench slope normal faults, the Kanto fragment beneath Tokyo, and the Itoigawa-Shizuoka Tectonic Line, were also brought >= 0.3 bars closer to failure.
C1 [Toda, Shinji] Kyoto Univ, Disaster Prevent Res Inst, Kyoto 6068501, Japan.
[Lin, Jian] Woods Hole Oceanog Inst, Woods Hole, MA 02543 USA.
[Stein, Ross S.] US Geol Survey, Menlo Pk, CA 94025 USA.
RP Toda, S (reprint author), Kyoto Univ, Disaster Prevent Res Inst, Kyoto 6068501, Japan.
EM toda@rcep.dpri.kyoto-u.ac.jp
NR 20
TC 57
Z9 62
U1 1
U2 22
PU TERRA SCIENTIFIC PUBL CO
PI TOKYO
PA 2003 SANSEI JIYUGAOKA HAIMU, 5-27-19 OKUSAWA, SETAGAYA-KU, TOKYO,
158-0083, JAPAN
SN 1343-8832
J9 EARTH PLANETS SPACE
JI Earth Planets Space
PY 2011
VL 63
IS 7
BP 725
EP 730
DI 10.5047/eps.2011.05.010
PG 6
WC Geosciences, Multidisciplinary
SC Geology
GA 854TC
UT WOS:000297516400040
ER
PT J
AU Knick, ST
Connelly, JW
AF Knick, Steven T.
Connelly, John W.
BE Knick, ST
Connelly, JW
TI GREATER SAGE-GROUSE AND SAGEBRUSH An Introduction to the Landscape
SO GREATER SAGE-GROUSE: ECOLOGY AND CONSERVATION OF A LANDSCAPE SPECIES AND
ITS HABITATS
SE Studies in Avian Biology
LA English
DT Editorial Material; Book Chapter
C1 [Knick, Steven T.] US Geol Survey, Forest & Rangeland Ecosyst Sci Ctr, Boise, ID 83706 USA.
[Connelly, John W.] Idaho Dept Fish & Game, Pocatello, ID 83204 USA.
RP Knick, ST (reprint author), US Geol Survey, Forest & Rangeland Ecosyst Sci Ctr, 970 Lusk St, Boise, ID 83706 USA.
EM steve_knick@usgs.gov; jcsagegrouse@aol.com; steve_knick@usgs.gov;
jcsagegrouse@aol.com
NR 0
TC 16
Z9 16
U1 0
U2 10
PU UNIV CALIFORNIA PRESS
PI BERKELEY
PA 2120 BERKELEY WAY, BERKELEY, CA 94720 USA
BN 978-0-520-94868-6
J9 STUD AVIAN BIOL
JI Stud. Avian Biol.
PY 2011
IS 38
BP 1
EP 9
PG 9
WC Biodiversity Conservation; Ecology; Ornithology
SC Biodiversity & Conservation; Environmental Sciences & Ecology; Zoology
GA BXE42
UT WOS:000295869900003
ER
PT J
AU Knick, ST
AF Knick, Steven T.
BE Knick, ST
Connelly, JW
TI Historical Development, Principal Federal Legislation, and Current
Management of Sagebrush Habitats IMPLICATIONS FOR CONSERVATION
SO GREATER SAGE-GROUSE: ECOLOGY AND CONSERVATION OF A LANDSCAPE SPECIES AND
ITS HABITATS
SE Studies in Avian Biology
LA English
DT Article; Book Chapter
DE federal government agencies; legislation; public land management;
sagebrush
AB The historical disposition and development of sagebrush (Artemisia spp.) landscapes have resulted in land ownership mosaics and differences in environmental qualities among land managers that influence today's conservation planning. Early land-use policies following major land acquisitions from 1776 to 1867 in the western United States were designed to transfer the vast public resources to private ownership. Federal legislation enacted during the late 1800s and early 1900s encouraged development of arable regions, facilitated livestock grazing, created transportation corridors, and provided for access to minerals, coal, and petroleum. Productive lands characterized by deeper soils and access to water were transferred to private entities and converted from native habitats to agriculture. Privately owned lands are a major constituent of sagebrush landscapes in the Great Plains and Columbia Basin and are intermixed with public lands in other Sage-Grouse (Centrocercus spp.) Management Zones. The public still retains large areas and 70% of current sagebrush habitats. The Bureau of Land Management has responsibility for almost half of the sagebrush habitat in the United States; however, those lands are relatively unproductive and characterized by xeric environments and shallow soils. More recent legislation reflects changing public values to maintain or restore natural components, such as plants and wildlife, and minimize the impact of land uses in sagebrush landscapes. Multiple use dominates the management policy of most sagebrush habitat on public land; very little of the lands used by Greater Sage-Grouse (Centrocercus urophasianus) has protected status in national parks or reserves. Conserving sagebrush landscapes required by Greater Sage-Grouse and other wildlife will depend on engaging the mosaic of public agencies and private ownerships in management programs, understanding the broad diversity of habitat characteristics, and recognizing the limitations of environments supporting the majority of sagebrush habitat on public lands.
C1 US Geol Survey, Forest & Rangeland Ecosyst Sci Ctr, Boise, ID 83706 USA.
RP Knick, ST (reprint author), US Geol Survey, Forest & Rangeland Ecosyst Sci Ctr, 970 Lusk St, Boise, ID 83706 USA.
EM steve_knick@usgs.gov; steve_knick@usgs.gov
NR 0
TC 5
Z9 5
U1 0
U2 9
PU UNIV CALIFORNIA PRESS
PI BERKELEY
PA 2120 BERKELEY WAY, BERKELEY, CA 94720 USA
BN 978-0-520-94868-6
J9 STUD AVIAN BIOL
JI Stud. Avian Biol.
PY 2011
IS 38
BP 13
EP 31
PG 19
WC Biodiversity Conservation; Ecology; Ornithology
SC Biodiversity & Conservation; Environmental Sciences & Ecology; Zoology
GA BXE42
UT WOS:000295869900004
ER
PT J
AU Oyler-McCance, SJ
Quinn, TW
AF Oyler-McCance, Sara J.
Quinn, Thomas W.
BE Knick, ST
Connelly, JW
TI Molecular Insights into the Biology of Greater Sage-Grouse
SO GREATER SAGE-GROUSE: ECOLOGY AND CONSERVATION OF A LANDSCAPE SPECIES AND
ITS HABITATS
SE Studies in Avian Biology
LA English
DT Article; Book Chapter
DE Centrocercus urophasianus; genetics; lek evolution; mating system;
population genetics; taxonomic boundaries
AB Recent research on Greater Sage-Grouse (Centrocercus urophasianus) genetics has revealed some important findings. First, multiple paternity in broods is more prevalent than previously thought, and leks do not comprise kin groups. Second, the Greater Sage-Grouse is genetically distinct from the congeneric Gunnison Sage-Grouse (C. minimus). Third, the Lyon-Mono population in the Mono Basin, spanning the border between Nevada and California, has unique genetic characteristics. Fourth, the previous delineation of western (C. u. phaios) and eastern Greater Sage-Grouse (C. u. urophasianus) is not supported genetically. Fifth, two isolated populations in Washington show indications that genetic diversity has been lost due to population declines and isolation.
C1 [Oyler-McCance, Sara J.] US Geol Survey, Ft Collins Sci Ctr, Ft Collins, CO 80526 USA.
[Quinn, Thomas W.] Univ Denver, Dept Biol Sci, Rocky Mt Ctr Conservat Genet & Systemat, Denver, CO 80208 USA.
RP Oyler-McCance, SJ (reprint author), US Geol Survey, Ft Collins Sci Ctr, 2150 Ctr Ave,Bldg C, Ft Collins, CO 80526 USA.
EM sara_oyler-mccance@usgs.gov; tquinn@du.edu
NR 0
TC 2
Z9 2
U1 1
U2 9
PU UNIV CALIFORNIA PRESS
PI BERKELEY
PA 2120 BERKELEY WAY, BERKELEY, CA 94720 USA
BN 978-0-520-94868-6
J9 STUD AVIAN BIOL
JI Stud. Avian Biol.
PY 2011
IS 38
BP 85
EP 94
PG 10
WC Biodiversity Conservation; Ecology; Ornithology
SC Biodiversity & Conservation; Environmental Sciences & Ecology; Zoology
GA BXE42
UT WOS:000295869900008
ER
PT J
AU Miller, RF
Knick, ST
Pyke, DA
Meinke, CW
Hanser, SE
Wisdom, MJ
Hild, AL
AF Miller, Richard F.
Knick, Steven T.
Pyke, David A.
Meinke, Cara W.
Hanser, Steven E.
Wisdom, Michael J.
Hild, Ann L.
BE Knick, ST
Connelly, JW
TI Characteristics of Sagebrush Habitats and Limitations to Long-Term
Conservation
SO GREATER SAGE-GROUSE: ECOLOGY AND CONSERVATION OF A LANDSCAPE SPECIES AND
ITS HABITATS
SE Studies in Avian Biology
LA English
DT Article; Book Chapter
DE Artemisia; Bromus tectorum; climate change; community dynamics; drought;
exotic plant species; juniper; pinyon; sagebrush; weather; wildfire
AB The distribution of sagebrush (Artemisia spp.) within the Sage-Grouse Conservation Area (SGCA, the historical distribution of sage-grouse buffered by 50 km) stretches from British Columbia and Saskatchewan in the north, to northern Arizona and New Mexico in the south, and from the eastern slopes of the Sierra Nevada and Cascade mountains to western South Dakota. The dominant sagebrush (sub) species as well as the composition and proportion of shrubs, grasses, and forbs varies across different ecological sites as a function of precipitation, temperature, soils, topographic position, elevation, and disturbance history. Most important to Greater Sage-Grouse (Centrocercus urophasianus) are three subspecies of big sagebrush (Artemisia tridentata)(basin big sagebrush [A. t. ssp. tridentata], Wyoming big sagebrush [A. t. ssp. wyomingensis], and mountain big sagebrush [A. t. ssp. vaseyana]); two low or dwarf forms (little sagebrush [A. arbuscula] and black sagebrush [A. nova]); and silver sagebrush (A. cana), which occurs primarily in the northeast portion of the sage-grouse range. Invasive plant species, wildfires, and weather and climate change are major influences on sagebrush habitats and present significant challenges to their long-term conservation. Each factor is spatially pervasive across the Greater Sage-Grouse Conservation Area and has significant potential to influence processes within sagebrush communities. Cheatgrass (Bromus tectorum), the most widespread exotic annual grass, has invaded much of the lower-elevation, more xeric sagebrush landscapes across the western portion of the Greater Sage-Grouse Conservation Area. A large proportion of existing sagebrush communities are at moderate to high risk of invasion by cheatgrass. Juniper (Juniperus spp.) and pinyon (Pinus spp.) woodlands have expanded into sagebrush habitats at higher elevations creating an elevational squeeze on the sagebrush ecosystem from both extremes. Number of fires and total area burned have increased since 1980 throughout the SGCA except in the Snake River Plain, which has a long-term history of high fire disturbance. Climate change scenarios for the sagebrush region predict increasing trends in temperature, atmospheric carbon dioxide, and frequency of severe weather events that favor cheatgrass expansion and in creased fire disturbance resulting in a decline in sagebrush. Approximately 12% of the current distribution of sagebrush is predicted to be replaced by expansion of other woody vegetation for each 1 degrees C increase in temperature. Periodic drought regularly influences sagebrush ecosystems; drought duration and severity have increased throughout the 20th century in much of the interior western United States. Synergistic feedbacks among invasive plant species, fire, and climate change, coupled with current trajectories of habitat changes and rates of disturbance (natural and humancaused), will continue to change sagebrush communities and create challenges for future conservation and management.
C1 [Miller, Richard F.] Oregon State Univ, Eastern Oregon Agr Res Ctr, Strand Agr Res Ctr 202, Corvallis, OR 97331 USA.
[Knick, Steven T.; Meinke, Cara W.; Hanser, Steven E.] US Geol Survey, Forest & Rangeland Ecosyst Sci Ctr, Boise, ID 83706 USA.
[Hild, Ann L.] Univ Wyoming, Dept Renewable Resources, Laramie, WY 82009 USA.
[Wisdom, Michael J.] US Forest Serv, USDA, Pacific NW Res Stn, La Grande, OR 97850 USA.
[Pyke, David A.] US Geol Survey, Forest & Rangeland Ecosyst Sci Ctr, Corvallis, OR 97331 USA.
RP Miller, RF (reprint author), Oregon State Univ, Eastern Oregon Agr Res Ctr, Strand Agr Res Ctr 202, Corvallis, OR 97331 USA.
EM richard.miller@oregonstate.edu; steve_knick@usgs.gov;
david_pyke@usgs.gov; cara.meinke@stantec.com; shanser@usgs.gov;
mwisdom@fs.fed.us; annhild@uwyo.edu; steve_knick@usgs.gov
NR 0
TC 75
Z9 75
U1 2
U2 37
PU UNIV CALIFORNIA PRESS
PI BERKELEY
PA 2120 BERKELEY WAY, BERKELEY, CA 94720 USA
BN 978-0-520-94868-6
J9 STUD AVIAN BIOL
JI Stud. Avian Biol.
PY 2011
IS 38
BP 145
EP 184
PG 40
WC Biodiversity Conservation; Ecology; Ornithology
SC Biodiversity & Conservation; Environmental Sciences & Ecology; Zoology
GA BXE42
UT WOS:000295869900013
ER
PT J
AU Knick, ST
Hanser, SE
Miller, RF
Pyke, DA
Wisdom, MJ
Finn, SP
Rinkes, ET
Henny, CJ
AF Knick, Steven T.
Hanser, Steven E.
Miller, Richard F.
Pyke, David A.
Wisdom, Michael J.
Finn, Sean P.
Rinkes, E. Thomas
Henny, Charles J.
BE Knick, ST
Connelly, JW
TI Ecological Influence and Pathways of Land Use in Sagebrush
SO GREATER SAGE-GROUSE: ECOLOGY AND CONSERVATION OF A LANDSCAPE SPECIES AND
ITS HABITATS
SE Studies in Avian Biology
LA English
DT Article; Book Chapter
DE agriculture; Conservation Reserve Program; energy development; land use;
livestock grazing; off-highway vehicle; prescribed fire; sagebrush;
sage-grouse; urbanization
AB Land use in sagebrush (Artemisia spp.) landscapes influences all sage-grouse (Centrocercus spp.) populations in western North America. Croplands and the network of irrigation canals cover 230,000 km(2) and indirectly influence up to 77% of the Sage-Grouse Conservation Area and 73% of sagebrush land cover by subsidizing synanthropic predators on sage-grouse. Urbanization and the demands of human population growth have created an extensive network of connecting infrastructure that is expanding its influence on sagebrush landscapes. Over 2,500 km(2) are now covered by interstate highways and paved roads; when secondary roads are included, 15% of the Sage-Grouse Conservation Area and 5% of existing sagebrush habitats are >2.5 km from roads. Density of secondary roads often exceeds 5 km/km(2), resulting in widespread motorized access for recreation, creating extensive travel corridors for management actions and resource development, subsidizing predators adapted to human presence, and facilitating spread of exotic or invasive plants. Sagebrush lands also are being used for their wilderness and recreation values, including off-highway vehicle use. Approximately 12,000,000 animal use months (AUM = amount of forage to support one livestock unit per month) are permitted for grazing livestock on public lands in the western states. Direct effects of grazing on sage-grouse populations or sagebrush landscapes are not possible to assess from current data. However, management of lands grazed by livestock has influenced sagebrush ecosystems by vegetation treatments to increase forage and reduce sagebrush and other plant species unpalatable to livestock. Fences (>2 km/km(2) in some regions), roads, and water developments to manage livestock movements further modify the landscape. Oil and gas development influences 8% of the sagebrush habitats with the highest intensities occurring in the eastern range of sage-grouse; >20% of the sagebrush distribution is indirectly influenced in the Great Plains, Wyoming Basin, and Colorado Plateau SMZs. Energy development physically removes habitat to construct well pads, roads, power lines, and pipelines; indirect effects include habitat fragmentation, soil disturbance, and facilitation of exotic plant and animal spread. More recent development of alternative energy, such as wind and geothermal, creates infrastructure in new regions of the sage-grouse distribution. Land use will continue to be a dominant stressor on sagebrush systems; its individual and cumulative effects will challenge long-term conservation of sage-grouse populations.
C1 [Knick, Steven T.; Hanser, Steven E.; Finn, Sean P.] US Geol Survey, Forest & Rangeland Ecosyst Sci Ctr, Boise, ID 83706 USA.
[Miller, Richard F.] Oregon State Univ, Eastern Oregon Agr Res Ctr, Strand Agr Res Ctr 202, Corvallis, OR 97331 USA.
[Pyke, David A.; Henny, Charles J.] US Geol Survey, Forest & Rangeland Ecosyst Sci Ctr, Corvallis, OR 97331 USA.
[Rinkes, E. Thomas] US Bur Land Management, Boise, ID 83709 USA.
[Wisdom, Michael J.] US Forest Serv, USDA, Pacific NW Res Stn, La Grande, OR 97850 USA.
RP Knick, ST (reprint author), US Geol Survey, Forest & Rangeland Ecosyst Sci Ctr, 970 Lusk St, Boise, ID 83706 USA.
EM steve_knick@usgs.gov; shanser@usgs.gov; richard.miller@oregonstate.edu;
david_pyke@usgs.gov; mwisdom@fs.fed.us; sfinn@usgs.gov;
tom_rinkes@blm.gov; hennyc@usgs.gov; steve_knick@usgs.gov
NR 0
TC 20
Z9 20
U1 0
U2 20
PU UNIV CALIFORNIA PRESS
PI BERKELEY
PA 2120 BERKELEY WAY, BERKELEY, CA 94720 USA
BN 978-0-520-94868-6
J9 STUD AVIAN BIOL
JI Stud. Avian Biol.
PY 2011
IS 38
BP 203
EP 251
PG 49
WC Biodiversity Conservation; Ecology; Ornithology
SC Biodiversity & Conservation; Environmental Sciences & Ecology; Zoology
GA BXE42
UT WOS:000295869900015
ER
PT J
AU Leu, M
Hanser, SE
AF Leu, Matthias
Hanser, Steven E.
BE Knick, ST
Connelly, JW
TI Influences of the Human Footprint on Sagebrush Landscape Patterns
IMPLICATIONS FOR SAGE-GROUSE CONSERVATION
SO GREATER SAGE-GROUSE: ECOLOGY AND CONSERVATION OF A LANDSCAPE SPECIES AND
ITS HABITATS
SE Studies in Avian Biology
LA English
DT Article; Book Chapter
DE Artemisia; Centrocercus spp.; fragmentation; Greater Sage-Grouse;
Gunnison Sage-Grouse; human footprint; lacunarity; sagebrush
AB Sagebrush (Artemisia spp.) ecosystems in the western United States have changed in quantity and configuration from a variety of causes including agriculture and human population growth since Euro-American settlement. Activities sustaining human society can decrease or fragment land cover and alter ecological processes within sagebrush systems. The extent of these activities, cumulatively called the human footprint, within the range of sage-grouse (Greater Sage-Grouse [Centrocercus urophasianus] and Gunnison Sage-Grouse [C. minimus]) has not been evaluated. Using a recent human-footprint model of the western United States, we evaluated human-footprint intensity: (1) across the sage-grouse range within seven Sage-Grouse Management Zones (SMZs), (2) across five sagebrush land-cover classes and a nonsagebrush land-cover class within SMZ, and (3) on landscape pattern of sagebrush land cover in relation to three scenarios differing in human-footprint effect area. Based on four criteria, we ranked SMZs from most to least human-footprint influence as follows: Columbia Basin, Colorado Plateau, Wyoming Basin, Great Plains, Snake River Plain, Southern Great Basin, and Northern Great Basin. Range-wide, black (Artemisia nova) and little (A. arbuscula) sagebrush land covers were least affected by the human footprint. Increasing human-footprint effect area decreased sagebrush land cover in the landscape between 33.5% and 97.0% and reduced mean patch size by 18.7% to 60.5%. A landscape-pattern analysis, using a lacunarity index, or measure of sagebrush patchiness, revealed sagebrush landscapes to be multiscaled, with dispersed sagebrush patches at small and clumped distributions at large scales, and organized at a scale between 4.5 and 9.0 km. This scale overlaps with published sage-grouse average dispersal and movement patterns. Our study supports growing evidence that sage-grouse respond to environmental factors at larger scales than those currently applied in management.
C1 [Leu, Matthias] US Geol Survey, Forest & Rangeland Ecosyst Res Ctr, Snake River Field Stn, Boise, ID 83706 USA.
RP Leu, M (reprint author), Coll William & Mary, Dept Biol, Integrated Sci Ctr, POB 8795,540 Landrum Dr,RM 2129, Williamsburg, VA 23185 USA.
EM mleu@wm.edu; shanser@usgs.gov
NR 0
TC 3
Z9 3
U1 0
U2 15
PU UNIV CALIFORNIA PRESS
PI BERKELEY
PA 2120 BERKELEY WAY, BERKELEY, CA 94720 USA
BN 978-0-520-94868-6
J9 STUD AVIAN BIOL
JI Stud. Avian Biol.
PY 2011
IS 38
BP 253
EP 271
PG 19
WC Biodiversity Conservation; Ecology; Ornithology
SC Biodiversity & Conservation; Environmental Sciences & Ecology; Zoology
GA BXE42
UT WOS:000295869900016
ER
PT J
AU Beever, EA
Aldridge, CL
AF Beever, Erik A.
Aldridge, Cameron L.
BE Knick, ST
Connelly, JW
TI Influences of Free-Roaming Equids on Sagebrush Ecosystems, with a Focus
on Greater Sage-Grouse
SO GREATER SAGE-GROUSE: ECOLOGY AND CONSERVATION OF A LANDSCAPE SPECIES AND
ITS HABITATS
SE Studies in Avian Biology
LA English
DT Article; Book Chapter
DE burros; Centrocercus urophasianus; direct and indirect effects; Equus
asinus; Equus caballus; grazing; horses; sagebrush; sage-grouse
AB Free-roaming equids (horses [Equus caballus] and burros [E. asinus]) in the United States were introduced to North America at the end of the 15th century, and have unique management status among ungulates. Legislation demands that these animals are neither hunted nor actively managed with fences and rotation among pastures, but instead constitute an integral part of the natural system of the public lands. Past research has elaborated that free-roaming horses can exert notable direct influences in sagebrush (Artemisia spp.) communities on structure and composition of vegetation and soils, as well as indirect influences on numerous animal groups whose abundance collectively may indicate the ecological integrity of such communities. Alterations to vegetation attributes and invertebrates can most directly affect fitness of Greater Sage-Grouse (Centrocercus urophasianus) and other sagebrush-obligate species; alterations of soils and other ecosystem properties may also indirectly affect these species. Across 3.03 million ha of the western Great Basin, horse-occupied sites exhibited lower grass, shrub, and overall plant cover; higher cover of unpalatable forbs and abundance of cheatgrass; 2.2-10.0 times lower densities of ant mounds; and 2.9-17.4 times greater penetration resistance in soil surfaces, compared to sites from which horses had been removed for 10-14 years. As is true for all herbivores, equid effects on ecosystems vary markedly with elevation, stocking density, and season and duration of use. However, they may be especially pronounced in periods of drought, which are forecasted to occur with increasing frequency in the southwestern United States under climate change, and when they interact synergistically with livestock-grazing effects. Equids' use of sagebrush landscapes will have different ecological consequences than will livestock grazing, at both local and landscape scales. Spatially, the addition of horses to sagebrush landscapes means more of the landscape receives use by nonnative grazers than if domestic cattle alone were present. In spite of recent advances in ecological understanding of equid synecology, much remains to be learned. Life-history characteristics of Greater Sage-Grouse and other sagebrush-obligate species suggest the great value in evaluating equid effects more broadly than through a horsesvs.-livestock perspective, and in monitoring ecosystem components such as soil-surface hardness and ant-mound density that have ecological and management relevance yet for which data are relatively inexpensive to collect.
C1 [Beever, Erik A.] US Geol Survey, Forest & Rangeland Ecosyst Sci Ctr, Corvallis, OR 97331 USA.
[Aldridge, Cameron L.] Colorado State Univ, Nat Resource Ecol Lab, Ft Collins, CO 80526 USA.
[Aldridge, Cameron L.] US Geol Survey, Ft Collins, CO 80526 USA.
RP Beever, EA (reprint author), US Geol Survey, No Rocky Mt Sci Ctr, 2327 Univ Way,Suite 2, Bozeman, MT 59715 USA.
EM ebeever@usgs.gov; cameron_aldridge@usgs.gov
NR 0
TC 2
Z9 3
U1 2
U2 8
PU UNIV CALIFORNIA PRESS
PI BERKELEY
PA 2120 BERKELEY WAY, BERKELEY, CA 94720 USA
BN 978-0-520-94868-6
J9 STUD AVIAN BIOL
JI Stud. Avian Biol.
PY 2011
IS 38
BP 273
EP 290
PG 18
WC Biodiversity Conservation; Ecology; Ornithology
SC Biodiversity & Conservation; Environmental Sciences & Ecology; Zoology
GA BXE42
UT WOS:000295869900017
ER
PT J
AU Knick, ST
Hanser, SE
AF Knick, Steven T.
Hanser, Steven E.
BE Knick, ST
Connelly, JW
TI Connecting Pattern and Process in Greater Sage-Grouse Populations and
Sagebrush Landscapes
SO GREATER SAGE-GROUSE: ECOLOGY AND CONSERVATION OF A LANDSCAPE SPECIES AND
ITS HABITATS
SE Studies in Avian Biology
LA English
DT Article; Book Chapter
DE Artemisia; Centrocercus urophasianus; connectivity; graph analysis;
Greater Sage-Grouse; landscape configuration; sagebrush
AB Spatial patterns influence the processes that maintain Greater Sage-Grouse (Centrocercus urophasianus) populations and sagebrush (Artemisia spp.) landscapes on which they depend. We used connectivity analyses to: (1) delineate the dominant pattern of sagebrush landscapes; (2) identify regions of the current range-wide distribution of Greater Sage-Grouse important for conservation; (3) estimate distance thresholds that potentially isolate populations; and (4) understand how landscape pattern, environmental disturbance, or location within the spatial network influenced lek persistence during a population decline. Long-term viability of sagebrush, assessed from its dominance in relatively unfragmented landscapes, likely is greatest in south-central Oregon and northwest Nevada; the Owyhee region of southeast Oregon, southwest Idaho, and northern Nevada; southwest Wyoming; and south-central Wyoming. The most important leks (breeding locations) for maintaining connectivity, characterized by higher counts of sage-grouse and connections with other leks, were within the core regions of the sage-grouse range. Sage-grouse populations presently have the highest levels of connectivity in the Wyoming Basin and lowest in the Columbia Basin Sage-Grouse management zones (SMZs). Leks separated by distances >13-18 km could be isolated due to decreased probability of dispersals from neighboring leks. The range-wide distribution of sage-grouse was clustered into 209 separate components (units in which leks were interconnected within but not among) when dispersal was limited to distances <18 km. The most important components for maintaining connectivity were distributed across the central and eastern regions of the range-wide distribution. Connectivity among sage-grouse populations was lost during population declines from 1965-1979 to 1998-2007, most dramatically in the Columbia Basin SMZ. Leks that persisted during this period were larger in size, were more highly connected, and had lower levels of broad-scale fire and human disturbance. Protecting core regions and maintaining connectivity with more isolated sage-grouse populations may help reverse or stabilize the processes of range contraction and isolation that have resulted in long-term population declines.
C1 [Knick, Steven T.; Hanser, Steven E.] US Geol Survey, Forest & Rangeland Ecosyst Sci Ctr, Boise, ID 83706 USA.
RP Knick, ST (reprint author), US Geol Survey, Forest & Rangeland Ecosyst Sci Ctr, 970 Lusk St, Boise, ID 83706 USA.
EM steve_knick@usgs.gov; shanser@usgs.gov; steve_knick@usgs.gov
NR 0
TC 13
Z9 13
U1 1
U2 11
PU UNIV CALIFORNIA PRESS
PI BERKELEY
PA 2120 BERKELEY WAY, BERKELEY, CA 94720 USA
BN 978-0-520-94868-6
J9 STUD AVIAN BIOL
JI Stud. Avian Biol.
PY 2011
IS 38
BP 383
EP 405
PG 23
WC Biodiversity Conservation; Ecology; Ornithology
SC Biodiversity & Conservation; Environmental Sciences & Ecology; Zoology
GA BXE42
UT WOS:000295869900019
ER
PT J
AU Johnson, DH
Holloran, MJ
Connelly, JW
Hanser, SE
Amundson, CL
Knick, ST
AF Johnson, Douglas H.
Holloran, Matthew J.
Connelly, John W.
Hanser, Steven E.
Amundson, Courtney L.
Knick, Steven T.
BE Knick, ST
Connelly, JW
TI Influences of Environmental and Anthropogenic Features on Greater
Sage-Grouse Populations, 1997-2007
SO GREATER SAGE-GROUSE: ECOLOGY AND CONSERVATION OF A LANDSCAPE SPECIES AND
ITS HABITATS
SE Studies in Avian Biology
LA English
DT Article; Book Chapter
DE Centrocercus urophasianus; communication towers; Greater Sage-Grouse;
lek; oil and gas wells; population; roads; sagebrush
AB The Greater Sage-Grouse (Centrocercus urophasianus), endemic to western North America, is of great conservation interest. Its populations are tracked by spring counts of males at lek sites. We explored the relations between trends of Greater Sage-Grouse lek counts from 1997 to 2007 and a variety of natural and anthropogenic features. We found that trends were correlated with several habitat features, but not always similarly throughout the range. Lek trends were positively associated with proportion of sagebrush (Artemisia spp.) cover, within 5 km and 18 km. Lek trends had negative associations with the coverage of agriculture and exotic plant species. Trends also tended to be lower for leks where a greater proportion of their surrounding landscape had been burned. Few leks were located within 5 km of developed land and trends were lower for those leks with more developed land within 5 km or 18 km. Lek trends were reduced where communication towers were nearby, whereas no effect of power lines was detected. Active oil or natural gas wells and highways, but not secondary roads, were associated with lower trends. Effects of some anthropogenic features may have already been manifested before our study period and thus not have been detected in this analysis. Results of this range-wide analysis complement those from more intensive studies on smaller areas. Our findings are important for identifying features that could threaten Greater Sage-Grouse populations.
C1 [Johnson, Douglas H.] US Geol Survey, No Prairie Wildlife Res Ctr, St Paul, MN 55108 USA.
[Holloran, Matthew J.] Wyoming Wildlife Consultants LLC, Laramie, WY 82072 USA.
[Hanser, Steven E.; Knick, Steven T.] US Geol Survey, Forest & Rangeland Ecosyst Sci Ctr, Boise, ID 83706 USA.
[Amundson, Courtney L.] Univ Minnesota, Dept Fisheries Wildlife & Conservat Biol, St Paul, MN 55108 USA.
[Connelly, John W.] Idaho Dept Fish & Game, Pocatello, ID 83204 USA.
RP Johnson, DH (reprint author), US Geol Survey, No Prairie Wildlife Res Ctr, 204 Hodson Hall,1980 Folwell Ave, St Paul, MN 55108 USA.
EM douglas_h_johnson@usgs.gov; matth@wyowildlife.com; jcsagegrouse@aol.com;
shanser@usgs.gov; amun0113@umn.edu; steve_knick@usgs.gov;
steve_knick@usgs.gov; jcsagegrouse@aol.com
NR 0
TC 12
Z9 12
U1 0
U2 8
PU UNIV CALIFORNIA PRESS
PI BERKELEY
PA 2120 BERKELEY WAY, BERKELEY, CA 94720 USA
BN 978-0-520-94868-6
J9 STUD AVIAN BIOL
JI Stud. Avian Biol.
PY 2011
IS 38
BP 407
EP 450
PG 44
WC Biodiversity Conservation; Ecology; Ornithology
SC Biodiversity & Conservation; Environmental Sciences & Ecology; Zoology
GA BXE42
UT WOS:000295869900020
ER
PT J
AU Wisdom, MJ
Meinke, CW
Knick, ST
Schroeder, MA
AF Wisdom, Michael J.
Meinke, Cara W.
Knick, Steven T.
Schroeder, Michael A.
BE Knick, ST
Connelly, JW
TI Factors Associated with Extirpation of Sage-Grouse
SO GREATER SAGE-GROUSE: ECOLOGY AND CONSERVATION OF A LANDSCAPE SPECIES AND
ITS HABITATS
SE Studies in Avian Biology
LA English
DT Article; Book Chapter
DE Centrocercus minimus; Centrocercus urophasianus; extirpated range;
extirpation; Greater Sage-Grouse; Gunnison Sage-Grouse; range
contraction; sagebrush
AB Geographic ranges of Greater Sage-Grouse (Centrocercus urophasianus) and Gunnison Sage-Grouse (C. minimus) have contracted across large areas in response to habitat loss and detrimental land uses. However, quantitative analyses of the environmental factors most closely associated with range contraction have been lacking, results of which could be highly relevant to conservation planning. Consequently, we analyzed differences in 22 environmental variables between areas of former range (extirpated range), and areas still occupied by the two species (occupied range). Fifteen of the 22 variables, representing a broad spectrum of biotic, abiotic, and anthropogenic conditions, had mean values that were significantly different between extirpated and occupied ranges. Best discrimination between extirpated and occupied ranges, using discriminant function analysis (DFA), was provided by five of these variables: sagebrush area (Artemisia spp.); elevation; distance to transmission lines; distance to cellular towers; and land ownership. A DFA model containing these five variables correctly classified >80% of sage-grouse historical locations to extirpated and occupied ranges. We used this model to estimate the similarity between areas of occupied range with areas where extirpation has occurred. Areas currently occupied by sage-grouse, but with high similarity to extirpated range, may not support persistent populations. Model estimates showed that areas of highest similarity were concentrated in the smallest, disjunct portions of occupied range and along range peripheries. Large areas in the eastern portion of occupied range also had high similarity with extirpated range. By contrast, areas of lowest similarity with extirpated range were concentrated in the largest, most contiguous portions of occupied range that dominate Oregon, Idaho, Nevada, and western Wyoming. Our results have direct relevance to conservation planning. We describe how results can be used to identify strongholds and spatial priorities for effective landscape management of sage-grouse.
C1 [Wisdom, Michael J.] US Forest Serv, USDA, Pacific NW Res Stn, La Grande, OR 97850 USA.
[Schroeder, Michael A.] Washington Dept Fish & Wildlife, Bridgeport, WA 98813 USA.
[Meinke, Cara W.; Knick, Steven T.] US Geol Survey, Forest & Rangeland Ecosyst Sci Ctr, Boise, ID 83706 USA.
RP Wisdom, MJ (reprint author), US Forest Serv, USDA, Pacific NW Res Stn, 1401 Gekeler Lane, La Grande, OR 97850 USA.
EM mwisdom@fs.fed.us; cara.meinke@stantec.com; steve_knick@usgs.gov;
michael.schroeder@dfw.wa.gov; steve_knick@usgs.gov
NR 0
TC 23
Z9 23
U1 0
U2 4
PU UNIV CALIFORNIA PRESS
PI BERKELEY
PA 2120 BERKELEY WAY, BERKELEY, CA 94720 USA
BN 978-0-520-94868-6
J9 STUD AVIAN BIOL
JI Stud. Avian Biol.
PY 2011
IS 38
BP 451
EP 472
PG 22
WC Biodiversity Conservation; Ecology; Ornithology
SC Biodiversity & Conservation; Environmental Sciences & Ecology; Zoology
GA BXE42
UT WOS:000295869900021
ER
PT J
AU Hanser, SE
Knick, ST
AF Hanser, Steven E.
Knick, Steven T.
BE Knick, ST
Connelly, JW
TI Greater Sage-Grouse as an Umbrella Species for Shrubland Passerine Birds
A MULTISCALE ASSESSMENT
SO GREATER SAGE-GROUSE: ECOLOGY AND CONSERVATION OF A LANDSCAPE SPECIES AND
ITS HABITATS
SE Studies in Avian Biology
LA English
DT Article; Book Chapter
DE canonical correspondence analysis; Centrocercus urophasianus; Greater
Sage-Grouse; habitat management; passerine birds; sagebrush ecosystem;
umbrella species
AB Working groups and government agencies are planning and conducting land actions in sagebrush (Artemisia spp.) habitats to benefit Greater Sage-Grouse (Centrocercus urophasianus) populations. Managers have adopted an umbrella concept, creating habitat characteristics specific to sage-grouse requirements, in the belief that other wildlife species dependent on sagebrush will benefit. We tested the efficacy of this approach by first identifying the primary environmental gradients underlying sagebrush steppe bird communities (including Greater Sage-Grouse). We integrated field sampling for birds and vegetation with geographic information system (GIS) data to characterize 305 sites sampled throughout the current range of Greater Sage-Grouse in the Intermountain West, United States. The primary environmental axis defining the bird community represented a gradient from local-scale Wyoming/basin big sagebrush (A. t. ssp. wyomingensis/A. t. ssp. tridentata), and bare ground cover to local and regional grassland cover; the second axis represented a transition from low-elevation Wyoming/basin big sagebrush and bare ground to mountain big sagebrush (A. t. ssp. vaseyana) and habitat edge. We identified the relative overlap of sage-grouse with 13 species of passerine birds along the multiscale gradients and estimated the width of the umbrella when applying management guidelines specific to sage-grouse. Passerine birds associated with sagebrush steppe habitats had high levels of overlap with Greater Sage-Grouse along the multiscale environmental gradients. However, the overlap of the umbrella was primarily a function of the broad range of sagebrush habitats used by sage-grouse. Management that focuses on creating a narrow set of plot-scale conditions will likely be less effective than restoration efforts that recognize landscape scale heterogeneity and multiscale organization of habitats. These multiscale efforts may improve some sage-grouse habitats and strengthen the management umbrella for shrub steppe passerine birds.
C1 [Hanser, Steven E.; Knick, Steven T.] US Geol Survey, Forest & Rangeland Ecosyst Sci Ctr, Boise, ID 83706 USA.
RP Hanser, SE (reprint author), US Geol Survey, Forest & Rangeland Ecosyst Sci Ctr, 970 Lusk St, Boise, ID 83706 USA.
EM shanser@usgs.gov; steve_knick@usgs.gov; steve_knick@usgs.gov
NR 0
TC 13
Z9 13
U1 0
U2 20
PU UNIV CALIFORNIA PRESS
PI BERKELEY
PA 2120 BERKELEY WAY, BERKELEY, CA 94720 USA
BN 978-0-520-94868-6
J9 STUD AVIAN BIOL
JI Stud. Avian Biol.
PY 2011
IS 38
BP 475
EP 487
PG 13
WC Biodiversity Conservation; Ecology; Ornithology
SC Biodiversity & Conservation; Environmental Sciences & Ecology; Zoology
GA BXE42
UT WOS:000295869900022
ER
PT J
AU Doherty, KE
Naugle, DE
Copeland, HE
Pocewicz, A
Kiesecker, JM
AF Doherty, Kevin E.
Naugle, David E.
Copeland, Holly E.
Pocewicz, Amy
Kiesecker, Joseph M.
BE Knick, ST
Connelly, JW
TI Energy Development and Conservation Tradeoffs SYSTEMATIC PLANNING FOR
GREATER SAGE-GROUSE IN THEIR EASTERN RANGE
SO GREATER SAGE-GROUSE: ECOLOGY AND CONSERVATION OF A LANDSCAPE SPECIES AND
ITS HABITATS
SE Studies in Avian Biology
LA English
DT Article; Book Chapter
DE Centrocercus urophasianus; conservation planning; core regions; energy
development; lek counts; prioritization; risk assessment; sage-grouse;
Wyoming
AB We developed a framework for conservation planning to evaluate options for reducing development impacts on Greater Sage-Grouse (Centrocercus urophasianus) in Wyoming, Montana, Colorado, Utah, North Dakota, and South Dakota that contained some of the largest populations and highest risk of energy development. We used lek-count data (N = 2,336 leks) to delineate high-abundance population centers, which we termed core regions, that contained 25%, 50%, 75%, and 100% of the known breeding population. We assessed vulnerability of these areas by examining risk of future land transforming uses from energy development. Sage-grouse abundance varied by state. Core regions contain a disproportionately large segment of the breeding population, and core regions vary dramatically by risk of future energy development. Wyoming contains 64% of the known sage-grouse population and more active leks than all the other states combined within our study area. Conservation success in Wyoming will depend on leasing and permitting policy decisions because this state has the highest risk of development. Montana contains fewer sage-grouse (24%) than Wyoming, but actions that reduce sagebrush (Artemisia spp.) tillage by providing private landowners incentives to maintain sagebrush-dominated landscapes would provide lasting benefits because core regions in Montana are at comparatively low development risk. Habitat restoration in areas with low risk of development but containing fewer sage-grouse fit into the overall conservation strategy by targeting populations that promote connectivity of core regions. This vulnerability assessment illustrates the trade-offs between conservation and energy development, and provides a framework for maintaining populations across the species' eastern range.
C1 [Doherty, Kevin E.; Naugle, David E.] Univ Montana, Wildlife Biol Program, Missoula, MT 59812 USA.
[Copeland, Holly E.; Pocewicz, Amy] Nature Conservancy, Wyoming State Off, Lander, WY 82520 USA.
[Kiesecker, Joseph M.] Nature Conservancy, Rocky Mt Conservat Reg, Ft Collins, CO 80524 USA.
RP Doherty, KE (reprint author), US Fish & Wildlife Serv, 3425 Miriam Ave, Bismarck, ND 58501 USA.
EM kevin_doherty@fws.gov; david.naugle@umontana.edu; hcopeland@tnc.org;
apocewicz@tnc.org; jkiesecker@tnc.org
NR 0
TC 25
Z9 25
U1 1
U2 4
PU UNIV CALIFORNIA PRESS
PI BERKELEY
PA 2120 BERKELEY WAY, BERKELEY, CA 94720 USA
BN 978-0-520-94868-6
J9 STUD AVIAN BIOL
JI Stud. Avian Biol.
PY 2011
IS 38
BP 505
EP 516
PG 12
WC Biodiversity Conservation; Ecology; Ornithology
SC Biodiversity & Conservation; Environmental Sciences & Ecology; Zoology
GA BXE42
UT WOS:000295869900024
ER
PT J
AU Connelly, JW
Knick, ST
Braun, CE
Baker, WL
Beever, EA
Christiansen, T
Doherty, KE
Garton, EO
Hanser, SE
Johnson, DH
Leu, M
Miller, RF
Naugle, DE
Oyler-McCance, SJ
Pyke, DA
Reese, KP
Schroeder, MA
Stiver, SJ
Walker, BL
Wisdom, MJ
AF Connelly, J. W.
Knick, S. T.
Braun, C. E.
Baker, W. L.
Beever, E. A.
Christiansen, T.
Doherty, K. E.
Garton, E. O.
Hanser, S. E.
Johnson, D. H.
Leu, M.
Miller, R. F.
Naugle, D. E.
Oyler-McCance, S. J.
Pyke, D. A.
Reese, K. P.
Schroeder, M. A.
Stiver, S. J.
Walker, B. L.
Wisdom, M. J.
BE Knick, ST
Connelly, JW
TI Conservation of Greater Sage-Grouse A SYNTHESIS OF CURRENT TRENDS AND
FUTURE MANAGEMENT
SO GREATER SAGE-GROUSE: ECOLOGY AND CONSERVATION OF A LANDSCAPE SPECIES AND
ITS HABITATS
SE Studies in Avian Biology
LA English
DT Article; Book Chapter
DE Centrocercus urophasianus; Greater Sage-Grouse; habitats; management;
populations; restoration; sagebrush
AB Recent analyses of Greater Sage-Grouse (Centrocercus urophasianus) populations indicate substantial declines in many areas but relatively stable populations in other portions of the species' range. Sagebrush (Artemisia spp.) habitats necessary to support sage-grouse are being burned by large wildfires, invaded by nonnative plants, and developed for energy resources (gas, oil, and wind). Management on public lands, which contain 70% of sagebrush habitats, has changed over the last 30 years from large sagebrush control projects directed at enhancing livestock grazing to a greater emphasis on projects that often attempt to improve or restore ecological integrity. Nevertheless, the mandate to manage public lands to provide traditional consumptive uses as well as recreation and wilderness values is not likely to change in the near future. Consequently, demand and use of resources contained in sagebrush landscapes plus the associated infrastructure to support increasing human populations in the western United States will continue to challenge efforts to conserve Greater Sage-Grouse. The continued widespread distribution of sage-grouse, albeit at very low densities in some areas, coupled with large areas of important sagebrush habitat that are relatively unaffected by the human footprint, suggest that Greater Sage-Grouse populations may be able to persist into the future. We summarize the status of sage-grouse populations and habitats, provide a synthesis of major threats and challenges to conservation of sage-grouse, and suggest a roadmap to attaining conservation goals.
C1 [Connelly, J. W.] Idaho Dept Fish & Game, Pocatello, ID 83204 USA.
[Knick, S. T.; Hanser, S. E.; Leu, M.] US Geol Survey, Forest & Rangeland Ecosyst Sci Ctr, Snake River Field Stn, Boise, ID 83706 USA.
[Braun, C. E.] Grouse Inc, Tucson, AZ 85750 USA.
[Baker, W. L.] Univ Wyoming, Ecol Program, Laramie, WY 82071 USA.
[Baker, W. L.] Univ Wyoming, Dept Geog, Laramie, WY 82071 USA.
[Beever, E. A.; Pyke, D. A.] US Geol Survey, Forest & Rangeland Ecosyst Sci Ctr, Corvallis, OR 97331 USA.
[Christiansen, T.] Wyoming Game & Fish Dept, Green River, WY 82935 USA.
[Doherty, K. E.; Naugle, D. E.; Walker, B. L.] Univ Montana, Wildlife Biol Program, Missoula, MT 59812 USA.
[Garton, E. O.; Reese, K. P.] Univ Idaho, Dept Fish & Wildlife Resources, Moscow, ID 83844 USA.
[Johnson, D. H.] US Geol Survey, No Prairie Wildlife Res Ctr, St Paul, MN 55108 USA.
[Miller, R. F.] Oregon State Univ, Eastern Oregon Agr Res Ctr, Corvallis, OR 97331 USA.
[Oyler-McCance, S. J.] US Geol Survey, Ft Collins Sci Ctr, Ft Collins, CO 80526 USA.
[Schroeder, M. A.] Washington Dept Fish & Wildlife, Bridgeport, WA 98813 USA.
[Stiver, S. J.] Western Assoc Fish & Wildlife Agencies, Prescott, AZ 86301 USA.
[Wisdom, M. J.] US Forest Serv, USDA, Pacific NW Res Stn, La Grande, OR 97850 USA.
RP Connelly, JW (reprint author), Idaho Dept Fish & Game, 1345 Barton Rd, Pocatello, ID 83204 USA.
EM jcsagegrouse@aol.com; sg-wtp@juno.com; bakerwl@uwyo.edu;
ebeever@usgs.gov; tom_christiansen@wgf.state.wy.us;
kevin_doherty@fws.gov; ogarton@uidaho.edu; shanser@usgs.gov;
douglas_h_johnson@usgs.gov; mleu@wm.edu; richard.miller@oregonstate.edu;
david.naugle@umontana.edu; sara_oyler-mccance@usgs.gov;
david_pyke@usgs.gov; kreese@uidaho.edu; michael.schroeder@dfw.wa.gov;
stiver@cableone.net; brett.walker@state.co.us; mwisdom@fs.fed.us;
jcsagegrouse@aol.com
NR 0
TC 18
Z9 19
U1 0
U2 17
PU UNIV CALIFORNIA PRESS
PI BERKELEY
PA 2120 BERKELEY WAY, BERKELEY, CA 94720 USA
BN 978-0-520-94868-6
J9 STUD AVIAN BIOL
JI Stud. Avian Biol.
PY 2011
IS 38
BP 549
EP 563
PG 15
WC Biodiversity Conservation; Ecology; Ornithology
SC Biodiversity & Conservation; Environmental Sciences & Ecology; Zoology
GA BXE42
UT WOS:000295869900027
ER
PT J
AU Lantry, BF
O'Gorman, R
Strang, TG
Lantry, JR
Connerton, MJ
Schaner, T
AF Lantry, B. F.
O'Gorman, R.
Strang, T. G.
Lantry, J. R.
Connerton, M. J.
Schaner, T.
TI Evaluation of Offshore Stocking of Lake Trout in Lake Ontario
SO NORTH AMERICAN JOURNAL OF FISHERIES MANAGEMENT
LA English
DT Article
ID FOOD-WEB; STRAINS; DISTRIBUTIONS; SURVIVAL; MICHIGAN; ALEWIVES;
SOUTHERN; GROWTH; FISH
AB Restoration stocking of hatchery-reared lake trout Salvelinus namaycush has occurred in Lake Ontario since 1973. In U. S. waters, fish stocked through 1990 survived well and built a large adult population. Survival of yearlings stocked from shore declined during 1990-1995, and adult numbers fell during 1998-2005. Offshore stocking of lake trout was initiated in the late 1990s in response to its successful mitigation of predation losses to double-crested cormorants Phalacrocorax auritus and the results of earlier studies that suggested it would enhance survival in some cases. The current study was designed to test the relative effectiveness of three stocking methods at a time when poststocking survival for lake trout was quite low and losses due to fish predators was a suspected factor. The stocking methods tested during 2000-2002 included May offshore, May onshore, and June onshore. Visual observations during nearshore stockings and hydroacoustic observations of offshore stockings indicated that release methods were not a direct cause of fish mortality. Experimental stockings were replicated for 3 years at one site in the southwest and for 2 years at one site in the southeast. Offshore releases used a landing craft to transport hatchery trucks from 3 to 6 km offshore out to 55-60-m-deep water. For the southwest site, offshore stocking significantly enhanced poststocking survival. Among the three methods, survival ratios were 1.74 : 1.00 : 1.02 (May offshore : May onshore : June onshore). Although not statistically significant owing to the small samples, the trends were similar for the southeast site, with survival ratios of 1.67 : 1.00 : 0.72. Consistent trends across years and sites indicated that offshore stocking of yearling lake trout during 2000-2002 provided nearly a twofold enhancement in survival; however, this increase does not appear to be great enough to achieve the 12-fold enhancement necessary to return population abundance to restoration targets.
C1 [Lantry, B. F.; O'Gorman, R.; Strang, T. G.] US Geol Survey, Lake Ontario Biol Stn, Oswego, NY 13126 USA.
[Lantry, J. R.; Connerton, M. J.] New York State Dept Environm Conservat, Cape Vincent Fisheries Stn, Cape Vincent, NY 13618 USA.
[Schaner, T.] Ontario Minist Nat Resources, Glenora Res Stn, Picton, ON KOK 2TO, Canada.
RP Lantry, BF (reprint author), US Geol Survey, Lake Ontario Biol Stn, 17 Lake St, Oswego, NY 13126 USA.
EM bflantry@usgs.gov
NR 41
TC 2
Z9 2
U1 0
U2 4
PU TAYLOR & FRANCIS INC
PI PHILADELPHIA
PA 325 CHESTNUT ST, SUITE 800, PHILADELPHIA, PA 19106 USA
SN 0275-5947
J9 N AM J FISH MANAGE
JI North Am. J. Fish Manage.
PY 2011
VL 31
IS 4
BP 671
EP 682
DI 10.1080/02755947.2011.608613
PG 12
WC Fisheries
SC Fisheries
GA 836VC
UT WOS:000296141400009
ER
PT J
AU Tabor, RA
Fresh, KL
Piaskowski, RM
Gearns, HA
Hayes, DB
AF Tabor, Roger A.
Fresh, Kurt L.
Piaskowski, Richard M.
Gearns, Howard A.
Hayes, Daniel B.
TI Habitat Use by Juvenile Chinook Salmon in the Nearshore Areas of Lake
Washington: Effects of Depth, Lakeshore Development, Substrate, and
Vegetation
SO NORTH AMERICAN JOURNAL OF FISHERIES MANAGEMENT
LA English
DT Article
ID TROUT SALVELINUS-FONTINALIS; NORTH TEMPERATE LAKES;
ONCORHYNCHUS-TSHAWYTSCHA; RESIDENTIAL DEVELOPMENT; ATLANTIC SALMON;
PREDATION RISK; RAINBOW-TROUT; BROOK TROUT; PUGET-SOUND; MICROHABITAT
SELECTION
AB Juvenile Chinook salmon Oncorhynchus tshawytscha in nearshore areas of Lake Washington, Washington, were studied to determine their depth distribution, substrate associations, and use of overhanging vegetation (OHV) and shoreline armoring. From March to May, juvenile Chinook salmon progressively shifted to deeper waters as they increased in size. At night, they were associated with small substrates, whereas no association with a particular substrate type was detected during daytime. Juveniles were commonly found in open areas or within 5 m of overwater structures (e. g., piers and docks) but were rarely found directly under such structures. The number of juveniles associated with armored shorelines was lower than expected given the availability of this habitat type. Large numbers of small juveniles often used OHV during the day; however, at night they moved away from cover and occupied open areas with no structure. Larger juveniles did not show a strong affinity to overhead cover. Our results suggest that continued development of the Lake Washington shoreline has the potential to restrict the amount of habitat that is useable by the Chinook salmon. They used shallow shoreline areas with fine substrates (sands and gravels), including both open beaches and areas with riparian vegetation for providing woody debris and OHV. These types of habitat features tend to be reduced as a result of lakeshore development. We hypothesize that habitat use by juvenile Chinook salmon was most likely being driven by predation risk. Habitat changes resulting from shoreline development could therefore potentially increase their vulnerability to predators.
C1 [Tabor, Roger A.] US Fish & Wildlife Serv, Washington Fish & Wildlife Off, Lacey, WA 98503 USA.
[Fresh, Kurt L.] Natl Marine Fisheries Serv, NW Fisheries Sci Ctr, Seattle, WA 98112 USA.
[Piaskowski, Richard M.; Gearns, Howard A.] US Fish & Wildlife Serv, Washington Fish & Wildlife Off, Lacey, WA 98503 USA.
[Hayes, Daniel B.] Michigan State Univ, Dept Fisheries & Wildlife, E Lansing, MI 48824 USA.
RP Tabor, RA (reprint author), US Fish & Wildlife Serv, Washington Fish & Wildlife Off, 510 Desmond Dr SE,Suite 102, Lacey, WA 98503 USA.
EM roger_tabor@fws.gov
FU Seattle Public Utilities
FX Sean Rubey, Chuck McCoy, Sergio Camacho, David Low, and Heather
Tschaekofske (USFWS) assisted with field sampling. Personnel of the City
of Renton, Washington, provided logistic support for field sampling.
Steve Dilley and Scott Sanders (USFWS) assisted with the figures. Kelly
Kiyohara (Washington Department of Fish and Wildlife) provided
information on Chinook salmon emigration. The study was financially
supported by Seattle Public Utilities and administered by Keith Kurko
and Julie Hall. Comments provided by Julie Hall (Seattle Public
Utilities), Michele Koehler (Seattle Public Utilities), Ken Tiffan, Jim
Johnson, and an anonymous reviewer greatly improved earlier versions of
the manuscript. The findings and conclusions in this article are those
of the authors and do not necessarily represent the views of USFWS.
NR 69
TC 5
Z9 5
U1 2
U2 20
PU TAYLOR & FRANCIS INC
PI PHILADELPHIA
PA 325 CHESTNUT ST, SUITE 800, PHILADELPHIA, PA 19106 USA
SN 0275-5947
J9 N AM J FISH MANAGE
JI North Am. J. Fish Manage.
PY 2011
VL 31
IS 4
BP 700
EP 713
DI 10.1080/02755947.2011.611424
PG 14
WC Fisheries
SC Fisheries
GA 836VC
UT WOS:000296141400012
ER
PT J
AU McKenna, JE
Johnson, JH
AF McKenna, James E., Jr.
Johnson, James H.
TI Landscape Models of Brook Trout Abundance and Distribution in Lotic
Habitat with Field Validation
SO NORTH AMERICAN JOURNAL OF FISHERIES MANAGEMENT
LA English
DT Article
ID ARTIFICIAL NEURAL-NETWORKS; MICHIGANS LOWER PENINSULA; NEW-YORK;
SALVELINUS-FONTINALIS; RAINBOW-TROUT; LAKE-ONTARIO; POSTGLACIAL
DISPERSAL; ATLANTIC SALMON; UNITED-STATES; STREAM FISH
AB Brook trout Salvelinus fontinalis are native fish in decline owing to environmental changes. Predictions of their potential distribution and a better understanding of their relationship to habitat conditions would enhance the management and conservation of this valuable species. We used over 7,800 brook trout observations throughout New York State and georeferenced, multiscale landscape condition data to develop four regionally specific artificial neural network models to predict brook trout abundance in rivers and streams. Land cover data provided a general signature of human activity, but other habitat variables were resistant to anthropogenic changes (i.e., changing on a geological time scale). The resulting models predict the potential for any stream to support brook trout. The models were validated by holding 20% of the data out as a test set and by comparison with additional field collections from a variety of habitat types. The models performed well, explaining more than 90% of data variability. Errors were often associated with small spatial displacements of predicted values. When compared with the additional field collections (39 sites), 92% of the predictions were off by only a single class from the field-observed abundances. Among "least-disturbed" field collection sites, all predictions were correct or off by a single abundance class, except for one where brown trout Salmo trutta were present. Other degrading factors were evident at most sites where brook trout were absent or less abundant than predicted. The most important habitat variables included landscape slope, stream and drainage network sizes, water temperature, and extent of forest cover. Predicted brook trout abundances were applied to all New York streams, providing a synoptic map of the distribution of brook trout habitat potential. These fish models set benchmarks of best potential for streams to support brook trout under broad-scale human influences and can assist with planning and identification of protection or rehabilitation sites.
C1 [McKenna, James E., Jr.; Johnson, James H.] US Geol Survey, Great Lakes Sci Ctr, Tunison Lab Aquat Sci, Cortland, NY 13045 USA.
RP McKenna, JE (reprint author), US Geol Survey, Great Lakes Sci Ctr, Tunison Lab Aquat Sci, 3075 Gracie Rd, Cortland, NY 13045 USA.
EM jemckenna@usgs.gov
FU New York Department of Environmental Conservation; National Gap Analysis
Program
FX We are grateful to J. D. McKenna, M. Bowker, and other volunteers for
assistance with field collections. Thanks go to M. Chalupnicki, M.
Slattery, and M. Henry for field and geographical information systems
assistance. We are indebted to the New York Department of Environmental
Conservation for data and support, particularly C. Festa and S. Hurst.
We appreciate all of the thoughtful effort and suggestions provided by
the department's fishery biologists and manuscript reviewers. This
project was supported by funding from the National Gap Analysis Program
and is contribution 1628 of the U. S. Geological Survey, Great Lakes
Science Center.
NR 68
TC 19
Z9 19
U1 2
U2 20
PU TAYLOR & FRANCIS INC
PI PHILADELPHIA
PA 325 CHESTNUT ST, SUITE 800, PHILADELPHIA, PA 19106 USA
SN 0275-5947
J9 N AM J FISH MANAGE
JI North Am. J. Fish Manage.
PY 2011
VL 31
IS 4
BP 742
EP 756
DI 10.1080/02755947.2011.593940
PG 15
WC Fisheries
SC Fisheries
GA 836VC
UT WOS:000296141400017
ER
PT J
AU Schwinning, S
Sandquist, DR
Miller, DM
Bedford, DR
Phillips, SL
Belnap, J
AF Schwinning, S.
Sandquist, D. R.
Miller, D. M.
Bedford, D. R.
Phillips, S. L.
Belnap, J.
TI The influence of stream channels on distributions of Larrea tridentata
and Ambrosia dumosa in the Mojave Desert, CA, USA: patterns, mechanisms
and effects of stream redistribution
SO ECOHYDROLOGY
LA English
DT Article
DE shrub cover and density; wash; alluvial fan; disturbance
ID VEGETATION PATTERNS; CHIHUAHUAN DESERT; SOIL-MOISTURE; ROOT GROWTH;
SHRUBS; DYNAMICS; COMMUNITIES; LANDSCAPE; VARIABILITY; HISTORY
AB Drainage channels are among the most conspicuous surficial features of deserts, but little quantitative analysis of their influence on plant distributions is available. We analysed the effects of desert stream channels ('washes') on Larrea tridentata and Ambrosia dumosa density and cover on an alluvial piedmont in the Mojave Desert, based on a spatial analysis of transect data encompassing a total length of 2775 m surveyed in 5 cm increments. Significant deviations from average transect properties were identified by bootstrapping. Predictably, shrub cover and density were much reduced inside washes, and elevated above average levels adjacent to washes. Average Larrea and Ambrosia cover and density peaked 1.2-1.6 m and 0.5-1.0 m from wash edges, respectively. We compared wash effects in runon-depleted (-R) sections, where washes had been cut off from runon and were presumably inactive, with those in runon-supplemented (+R) sections downslope from railroad culverts to help identify mechanisms responsible for the facilitative effect of washes on adjacent shrubs. Shrub cover and density near washes peaked in both +R and -R sections, suggesting that improved water infiltration and storage alone can cause a facilitative effect on adjacent shrubs. However, washes of <2 m width in +R sections had larger than average effects on peak cover, suggesting that plants also benefit from occasional resource supplementation. The data suggest that channel networks significantly contribute to structuring plant communities in the Mojave Desert and their disruption has notable effects on geomorphic and ecological processes far beyond the original disturbance sites. Copyright (C) 2010 John Wiley & Sons, Ltd.
C1 [Schwinning, S.] Texas State Univ, Dept Biol, San Marcos, TX 78666 USA.
[Sandquist, D. R.] Calif State Univ Fullerton, Dept Biol Sci, Fullerton, CA 92834 USA.
[Miller, D. M.; Bedford, D. R.] US Geol Survey, Menlo Pk, CA 94025 USA.
[Phillips, S. L.; Belnap, J.] USGS SW Biol Sci Ctr, Moab, UT 84532 USA.
RP Schwinning, S (reprint author), Texas State Univ, Dept Biol, San Marcos, TX 78666 USA.
EM schwinn@txstate.edu
RI Schwinning, Susanne/G-6412-2015;
OI Schwinning, Susanne/0000-0002-9740-0291; Bedford,
David/0000-0001-9706-928X
FU U.S. Geological Survey
FX This research was supported by the U.S. Geological Survey, Priority
Ecosystems Program. We are grateful to Sasha Reed and Kristin H. Berry,
as well as one anonymous reviewer for providing many thoughtful
suggestions that helped improve the original manuscript.
NR 38
TC 8
Z9 9
U1 0
U2 24
PU WILEY-BLACKWELL
PI MALDEN
PA COMMERCE PLACE, 350 MAIN ST, MALDEN 02148, MA USA
SN 1936-0584
J9 ECOHYDROLOGY
JI Ecohydrology
PD JAN
PY 2011
VL 4
IS 1
BP 12
EP 25
DI 10.1002/eco.116
PG 14
WC Ecology; Environmental Sciences; Water Resources
SC Environmental Sciences & Ecology; Water Resources
GA 718VM
UT WOS:000287154500002
ER
PT J
AU Valentine-Darby, PL
Darby, PC
Percival, HF
AF Valentine-Darby, Patricia L.
Darby, Philip C.
Percival, H. Franklin
TI GENDER-BASED DIFFERENCES IN FLORIDAAPPLE SNAIL (POMACEA PALUDOSA)
MOVEMENTS
SO MALACOLOGIA
LA English
DT Article
DE Pomacea paludosa; reproduction; movements; Florida; apple snail
ID APPLE-SNAIL; WETLAND HABITATS; SEX-PHEROMONE; CHEMICAL CUES; PEDAL
MUCUS; POPULATION; BEHAVIOR; SAY; CANALICULATA; AMPULLARIIDAE
AB Gastropod movements have been studied in the context of habitat selection, finding food and mates, and avoiding predation. Many of these studies were conducted in the laboratory, where constraints on spatial scale influence behavior. We conducted a field study of Florida apple snail (Pomacea paludosa) movements using telemetry. We hypothesized that Florida apple snail movements were driven by reproductive activity, and that gender differences would be evident. We documented male and female directions and distances traveled. We also conducted a trapping study that included conspecific bait to test if the presence of females attracted more males as measured by M:F ratios in traps. The greatest distances traveled were by males, and males were more likely to maintain a consistent bearing compared to females. Male distances peaked in what typically corresponds to peak breeding season. M:F ratios in traps were positively associated with reproductive activity in the study population as measured by egg cluster counts. Conspecific bait had no effect on the number of males or females captured. However, if a female crawled into the trap, we observed greater numbers of males compared to those with no trapped females. Males may have tracked females to increase mating encounters, following slime trails, as seen in other aquatic (including other Pomacea) snails. The capacity for mate finding has implications for reproductive success in the relatively low density populations often seen for Pomacea paludosa.
C1 [Darby, Philip C.] Univ W Florida, Dept Biol, Pensacola, FL 32514 USA.
[Valentine-Darby, Patricia L.] Pomacea Project, Pensacola, FL 32514 USA.
[Percival, H. Franklin] Univ Florida, Florida Cooperat Fish & Wildlife Res Unit, US Geol Survey, Gainesville, FL 32611 USA.
RP Darby, PC (reprint author), Univ W Florida, Dept Biol, 11000 Univ Pkwy, Pensacola, FL 32514 USA.
EM pdarby@uwf.edu
FU South Florida Water Management District (West Palm Beach, Florida); St.
Johns River Water Management District (Palatka, Florida) through a
contract with the Florida Cooperative Fish and Wildlife Research Unit
(Gainesville, Florida); Department of Biology and College of Arts and
Sciences at the University of West Florida (Pensacola, Florida)
FX The field project was funded by the South Florida Water Management
District (West Palm Beach, Florida) and the St. Johns River Water
Management District (Palatka, Florida) through a contract with the
Florida Cooperative Fish and Wildlife Research Unit (Gainesville,
Florida). Research support was also provided to PCD by the Department of
Biology and College of Arts and Sciences at the University of West
Florida (Pensacola, Florida). Bethany Wight (UWF) provided valuable
assistance in manuscript preparation. We thank lkuko Fujisaki
(University of Florida) for help with statistical analyses. We thank
Chris Cattau (UF), Charles D'Asaro (UWF), and three anonymous reviewers
for helpful comments on drafts of this manuscript.
NR 50
TC 2
Z9 2
U1 1
U2 5
PU INST MALACOL
PI ANN ARBOR
PA 2415 SOUTH CIRCLE DR, ANN ARBOR, MI 48103 USA
SN 0076-2997
J9 MALACOLOGIA
JI Malacologia
PY 2011
VL 54
IS 1-2
BP 109
EP 118
PG 10
WC Zoology
SC Zoology
GA 837NU
UT WOS:000296211300005
ER
PT J
AU Bowker, JD
Carty, D
Smith, CE
Bergen, SR
AF Bowker, James D.
Carty, Daniel
Smith, Charlie E.
Bergen, Silas R.
TI Chloramine-T Margin-of-Safety Estimates for Fry, Fingerling, and
Juvenile Rainbow Trout
SO NORTH AMERICAN JOURNAL OF AQUACULTURE
LA English
DT Article
ID BACTERIAL GILL DISEASE; HYDROGEN-PEROXIDE; ONCORHYNCHUS-MYKISS; ATLANTIC
SALMON; CHANNEL CATFISH; FRESH-WATER; CONTROL MORTALITY; ACID-BASE;
EXPOSURE; FISH
AB Chloramine-T (CLT) is a candidate for approval for use in U.S. aquaculture to control mortality in freshwater-reared salmonids caused by bacterial gill disease (causative agent, Flavobacterium branchiophilum). The proposed treatment regimen is to administer CLT at 12-20 mg/L in a static or flow-through bath for 60 min/d on three alternate or consecutive days. To estimate a CLT margin of safety, defined as the highest dosing regimen above the proposed maximum therapeutic regimen at which no adverse effects are observed, we conducted seven experiments with fry, fingerling, and juvenile rainbow trout Oncorhynchus mykiss that examined mortality and an eighth experiment that examined mortality, gross pathology, and histopathology after CLT exposure. In each experiment, triplicate groups of fish were exposed to a range of CLT concentrations representing 0, 1, 1.5, 2, 2.5, 3, 3.5, 4, or 5 x the highest proposed dose (20 mg/L) for 3 x the proposed treatment duration (60 min) on three alternate or consecutive days at 8 degrees C or 14 degrees C. The survival of fry and fingerlings was unaffected by exposure to CLT concentrations as high as 100 and 60 mg/L, respectively (survival = 97.3-100%). Although the survival of juvenile fish was unaffected by exposure to 20 mg/L, exposure to higher CLT concentrations significantly reduced survival (<= 10.0% at 100 mg/L). Across experiments, 92% of all mortalities occurred within 20 h of the first exposure to CLT. The histopathological changes of most concern were associated with gill tissues, but these were evident only in moribund fish exposed to doses of 60 mg/L or higher. Based on analysis of the survival data, the margin-of-safety estimates were approximately 100 mg/L for rainbow trout fry, at least 60 mg/L for fingerlings, and 50-60 mg/L for juveniles. Tissue responses to CLT at these concentrations were minor and did not warrant decreasing these estimates.
C1 [Bowker, James D.; Carty, Daniel] US Fish & Wildlife Serv, Aquat Anim Drug Approval Partnership Program, Bozeman, MT 59715 USA.
[Smith, Charlie E.] US Fish & Wildlife Serv, College Place, WA 99324 USA.
[Bergen, Silas R.] Winona State Univ, Winona, MN 55987 USA.
RP Bowker, JD (reprint author), US Fish & Wildlife Serv, Aquat Anim Drug Approval Partnership Program, 4050 Bridger Canyon Rd, Bozeman, MT 59715 USA.
EM jim_bowker@fws.gov
NR 44
TC 3
Z9 3
U1 1
U2 10
PU TAYLOR & FRANCIS INC
PI PHILADELPHIA
PA 325 CHESTNUT ST, SUITE 800, PHILADELPHIA, PA 19106 USA
SN 1522-2055
J9 N AM J AQUACULT
JI N. Am. J. Aqualcult.
PY 2011
VL 73
IS 3
BP 259
EP 269
DI 10.1080/15222055.2011.588918
PG 11
WC Fisheries
SC Fisheries
GA 836UT
UT WOS:000296139800002
ER
PT J
AU Leicht-Young, SA
Latimer, AM
Silander, JA
AF Leicht-Young, Stacey A.
Latimer, Andrew M.
Silander, John A., Jr.
TI Lianas escape self-thinning: Experimental evidence of positive density
dependence in temperate lianas Celastrus orbiculatus and C. scandens
SO PERSPECTIVES IN PLANT ECOLOGY EVOLUTION AND SYSTEMATICS
LA English
DT Article
DE Competition; Facilitation; Lianas; Invasive species; Temperate forests;
Vines
ID HOST LIQUIDAMBAR-STYRACIFLUA; BELOW-GROUND COMPETITION; TROPICAL FOREST;
UNITED-STATES; ASYMMETRIC COMPETITION; TREE REGENERATION; PLANT
COMPETITION; LONICERA-JAPONICA; GROWTH; LIGHT
AB The neighborhood density of plants strongly affects their growth, reproduction, and survival. In most cases, high density increases competition and negatively affects a focal plant in predictable ways, leading to the self-thinning law. There are, however, situations in which high densities of plants facilitate focal plant performance, resulting in positive density dependence. Despite their importance in forest gap dynamics and distinctive growth form, there have been very few studies of the effect of density on lianas or vines. We grew an invasive (Celastrus orbiculatus)and a native (Celastrus scandens) liana species together in three different density treatments, while also manipulating the light and support availability. We found that across treatment conditions, C. orbiculatus always out-performed C. scandens, showing greater relative growth rate in height and diameter, greater biomass and higher survival. Both species responded similarly to the density treatments: with plants in high density not showing a decrease in relative height growth rate compared to medium density. Aboveground biomass for C. scandens was not affected by density, while for C. orbiculatus, the most massive plants were growing in medium density without support. More surprisingly, survival analysis indicated that the two species both had significantly lower mortality rates in the highest density treatment: this trend held true across the other treatments of light and supports. More generally, this study demonstrates that these lianas can escape the consequences of high density and thus the self-thinning law that affects self-supporting plants. This suggests a broader hypothesis about lianas in general: their greater flexibility in allocating growth resources allows them to grow taller and thinner without collapsing and thereby potentially escape shading and mortality even at high densities. Published by Elsevier GmbH.
C1 [Leicht-Young, Stacey A.] US Geol Survey, Lake Michigan Ecol Res Stn, Porter, IN 46304 USA.
[Latimer, Andrew M.] Univ Calif Davis, Dept Plant Sci, Davis, CA 95616 USA.
[Silander, John A., Jr.] Univ Connecticut, Dept Ecol & Evolutionary Biol, Storrs, CT 06269 USA.
RP Leicht-Young, SA (reprint author), US Geol Survey, Lake Michigan Ecol Res Stn, 1100N Mineral Springs Rd, Porter, IN 46304 USA.
EM slyoung@usgs.gov
FU USDA [2001-52103-11320]; University of Connecticut Department of Ecology
and Evolutionary Biology Ronald Bamford Endowment
FX We would like to thank Robin Chazdon, Cynthia Jones, and Zoe Cardon for
their assistance in many stages of this study. Susan Letcher, Martha
Carlson Mazur, Johannes Kollmann, and two anonymous reviewers provided
helpful comments on earlier drafts of this manuscript. We would also
like to thank the many undergraduate technicians without whom data
collection would not have been possible. We greatly appreciated the use
of the University of Connecticut's Plant Science Research Farm and the
help of Stephen Olsen and the farm crew. Research support was provided
by the USDA grant 2001-52103-11320 for the Invasive Plant Atlas of New
England (IPANE) and the University of Connecticut Department of Ecology
and Evolutionary Biology Ronald Bamford Endowment. This article is
contribution No. 1633 of the USGS Great Lakes Science Center. Use of
trade, product, or firm names does not imply endorsement by the U. S.
Government.
NR 91
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U1 5
U2 39
PU ELSEVIER GMBH, URBAN & FISCHER VERLAG
PI JENA
PA OFFICE JENA, P O BOX 100537, 07705 JENA, GERMANY
SN 1433-8319
J9 PERSPECT PLANT ECOL
JI Perspect. Plant Ecol. Evol. Syst.
PY 2011
VL 13
IS 3
BP 163
EP 172
DI 10.1016/j.ppees.2011.04.002
PG 10
WC Plant Sciences; Ecology
SC Plant Sciences; Environmental Sciences & Ecology
GA 834YL
UT WOS:000296000300001
ER
PT J
AU Voulgaris, G
Kumar, N
Gurgel, KW
Warner, JC
List, JH
AF Voulgaris, George
Kumar, Nirnimesh
Gurgel, Klaus-Werner
Warner, John C.
List, Jeffrey H.
GP IEEE
TI 2 2-D Inner-Shelf Current Observations from a Single VHF WEllen RAdar
(WERA) Station
SO 2011 IEEE/OES/CWTM TENTH WORKING CONFERENCE ON CURRENT, WAVES AND
TURBULENCE MEASUREMENT (CWTM)
LA English
DT Proceedings Paper
CT IEEE/OES/CWTM 10th Working Conference on Current, Waves and Turbulence
Measurement (CWTM)
CY MAR 20-23, 2011
CL Monterey, CA
SP Inst Elect Elect Engn (IEEE), IEEE Ocean Engn Soc (OES), Current, Waves & Turbulence Measurement Comm (CWTMC)
DE WERA; VHF Radar; radial currents; surface ocean currents; remote
sensing; nearshore; current accuracy
ID HF RADAR; SURFACE CURRENTS
AB The majority of High Frequency (HF) radars used worldwide operate at medium to high frequencies (8 to 30 MHz) providing spatial resolutions ranging from 3 to 1.5 km and ranges from 150 to 50 km. This paper presents results from the deployment of a single Very High Frequency (VHF, 48 MHz) WEllen RAdar (WERA) radar with spatial resolution of 150 m and range 10-15 km, used in the nearshore off Cape Hatteras, NC, USA. It consisted of a linear array of 12 antennas operating in beam forming mode. Radial velocities were estimated from radar backscatter for a variety of wind and nearshore wave conditions. A methodology similar to that used for converting acoustically derived beam velocities to an orthogonal system is presented for obtaining 2-D current fields from a single station. The accuracy of the VHF radar-derived radial velocities is examined using a new statistical technique that evaluates the system over the range of measured velocities. The VHF radar velocities showed a bias of 3 to 7 cm/s over the experimental period explainable by the differences in radar penetration and in-situ measurement height. The 2-D current field shows good agreement with the in-situ measurements. Deviations and inaccuracies are well explained by the geometric dilution analysis.
C1 [Voulgaris, George; Kumar, Nirnimesh] Univ S Carolina, Dept Earth & Ocean Sci, Columbia, SC 29205 USA.
[Gurgel, Klaus-Werner] Univ Hamburg, Inst Oceanog, D-20146 Hamburg, Germany.
[Warner, John C.; List, Jeffrey H.] US Geol Survey, Coastal & Marine Geol, Woods Hole, MA 02543 USA.
RP Voulgaris, G (reprint author), Univ S Carolina, Dept Earth & Ocean Sci, Columbia, SC 29205 USA.
EM gvoulgaris@geol.sc.edu; gurgel@ifm.uni-hamburg.de
FU US Geological Survey as part of the Carolinas Coastal Change Project
through a cooperative agreement with the University of South Carolina;
National Science Foundation [OCE-0451989, OCE-0535893]; German Academic
Exchange Service (DAAD)
FX Funding for the data collection was provided by the US Geological Survey
as part of the Carolinas Coastal Change Project through a cooperative
agreement with the University of South Carolina. Additional funding
during the data analysis was provided by the National Science Foundation
(Awards: OCE-0451989 and OCE -0535893). This manuscript was prepared
during a research visit of G. Voulgaris to the University of Hamburg,
Institute of Oceanography funded by a grant from the German Academic
Exchange Service (DAAD).
NR 15
TC 0
Z9 0
U1 0
U2 1
PU IEEE
PI NEW YORK
PA 345 E 47TH ST, NEW YORK, NY 10017 USA
BN 978-1-4577-0022-4
PY 2011
BP 56
EP 64
PG 9
WC Engineering, Electrical & Electronic
SC Engineering
GA BXB44
UT WOS:000295584600010
ER
PT B
AU Billington, N
Wilson, CC
Sloss, BL
AF Billington, Neil
Wilson, Chris C.
Sloss, Brian L.
BE Barton, BA
TI Distribution and Population Genetics of Walleye and Sauger
SO BIOLOGY, MANAGEMENT, AND CULTURE OF WALLEYE AND SAUGER
LA English
DT Article; Book Chapter
ID STIZOSTEDION-VITREUM-VITREUM; MITOCHONDRIAL-DNA VARIATION; MIXED-STOCK
ANALYSIS; FRESH-WATER FISHES; MAJOR HISTOCOMPATIBILITY COMPLEX;
CROSS-SPECIES AMPLIFICATION; PERCH PERCA-FLAVESCENS; EASTERN LAKE-ERIE;
SANDER-VITREUS; MALATE DEHYDROGENASE
C1 [Billington, Neil] Troy Univ, Dept Biol & Environm Sci, Troy, AL 36082 USA.
[Sloss, Brian L.] Univ Wisconsin, US Geol Survey, Wisconsin Cooperat Fishery Res Unit, Coll Nat Resources, Stevens Point, WI 54481 USA.
[Wilson, Chris C.] Trent Univ, Ontario Minist Nat Resources, Aquat Res & Dev Sect, Peterborough, ON K9J 7B8, Canada.
RP Billington, N (reprint author), Troy Univ, Dept Biol & Environm Sci, Troy, AL 36082 USA.
NR 134
TC 5
Z9 5
U1 1
U2 5
PU AMER FISHERIES SOC
PI BETHESDA
PA 5410 GROSVENOR LANE, STE 110, BETHESDA, MD 20814-2199 USA
BN 978-1-934874-22-6
PY 2011
BP 105
EP 132
PG 28
WC Fisheries; Zoology
SC Fisheries; Zoology
GA BVR93
UT WOS:000292616800004
ER
PT B
AU Bozek, MA
Haxton, TJ
Raabe, JK
AF Bozek, Michael A.
Haxton, Timothy J.
Raabe, Joshua K.
BE Barton, BA
TI Walleye and Sauger Habitat
SO BIOLOGY, MANAGEMENT, AND CULTURE OF WALLEYE AND SAUGER
LA English
DT Article; Book Chapter
ID STIZOSTEDION-VITREUM-VITREUM; WESTERN LAKE-ERIE; NORTHERN WISCONSIN
LAKES; JOHN-DAY-RESERVOIR; FISH-COMMUNITY STRUCTURE; UPPER MISSISSIPPI
RIVER; PERCH PERCA-FLAVESCENS; ALTERED FLOW REGIMES; LIFE-HISTORY
STAGES; MID-COLUMBIA RIVER
C1 [Bozek, Michael A.] Univ Wisconsin, US Geol Survey, Wisconsin Cooperat Fishery Res Unit, Coll Nat Resources, Stevens Point, WI 54481 USA.
[Haxton, Timothy J.] Ontario Minist Nat Resources, Sci & Informat Branch, Peterborough, ON K9J 8M5, Canada.
[Raabe, Joshua K.] N Carolina State Univ, N Carolina Cooperat Fish & Wildlife Res Unit, Dept Biol, Raleigh, NC 27695 USA.
RP Bozek, MA (reprint author), Univ Wisconsin, US Geol Survey, Wisconsin Cooperat Fishery Res Unit, Coll Nat Resources, 800 Reserve St, Stevens Point, WI 54481 USA.
NR 359
TC 14
Z9 14
U1 0
U2 11
PU AMER FISHERIES SOC
PI BETHESDA
PA 5410 GROSVENOR LANE, STE 110, BETHESDA, MD 20814-2199 USA
BN 978-1-934874-22-6
PY 2011
BP 133
EP 197
PG 65
WC Fisheries; Zoology
SC Fisheries; Zoology
GA BVR93
UT WOS:000292616800005
ER
PT B
AU Bozek, MA
Baccante, DA
Lester, NP
AF Bozek, Michael A.
Baccante, Dominic A.
Lester, Nigel P.
BE Barton, BA
TI Walleye and Sauger Life History
SO BIOLOGY, MANAGEMENT, AND CULTURE OF WALLEYE AND SAUGER
LA English
DT Article; Book Chapter
ID STIZOSTEDION-VITREUM-VITREUM; WESTERN LAKE-ERIE; NORTHERN WISCONSIN
LAKES; TROUT SALVELINUS-NAMAYCUSH; GREAT-PLAINS RESERVOIR; SEXUAL SIZE
DIMORPHISM; GROWING DEGREE-DAY; SANDER-VITREUS; ONEIDA-LAKE; JUVENILE
WALLEYES
C1 [Bozek, Michael A.] Univ Wisconsin, US Geol Survey, Wisconsin Cooperat Fishery Res Unit, Coll Nat Resources, Stevens Point, WI 54481 USA.
[Baccante, Dominic A.] British Columbia Minist Environm, Fish & Wildlife Sect, Ft St John, BC V1J 6M7, Canada.
[Lester, Nigel P.] Trent Univ, Ontario Minist Nat Resources, Aquat Res & Dev Sect, Peterborough, ON K9J 7B8, Canada.
RP Bozek, MA (reprint author), Univ Wisconsin, US Geol Survey, Wisconsin Cooperat Fishery Res Unit, Coll Nat Resources, 800 Reserve St, Stevens Point, WI 54481 USA.
NR 294
TC 15
Z9 16
U1 0
U2 11
PU AMER FISHERIES SOC
PI BETHESDA
PA 5410 GROSVENOR LANE, STE 110, BETHESDA, MD 20814-2199 USA
BN 978-1-934874-22-6
PY 2011
BP 233
EP 301
PG 69
WC Fisheries; Zoology
SC Fisheries; Zoology
GA BVR93
UT WOS:000292616800007
ER
PT B
AU Chipps, SR
Graeb, BDS
AF Chipps, Steven R.
Graeb, Brian D. S.
BE Barton, BA
TI Feeding Ecology and Energetics
SO BIOLOGY, MANAGEMENT, AND CULTURE OF WALLEYE AND SAUGER
LA English
DT Article; Book Chapter
ID STIZOSTEDION-VITREUM-VITREUM; FISH BIOENERGETICS MODELS; MISSOURI RIVER
RESERVOIR; PERCH PERCA-FLAVESCENS; INDIVIDUAL-BASED MODEL; WESTERN LAKE
ERIE; OF-YEAR WALLEYES; THE-YEAR WALLEYE; FOOD-CONSUMPTION; YELLOW PERCH
C1 [Chipps, Steven R.] S Dakota State Univ, US Geol Survey, S Dakota Cooperat Fish & Wildlife Res Unit, Dept Wildlife & Fisheries Sci, Brookings, SD 57007 USA.
RP Chipps, SR (reprint author), S Dakota State Univ, US Geol Survey, S Dakota Cooperat Fish & Wildlife Res Unit, Dept Wildlife & Fisheries Sci, SNP 138,Box 2140B, Brookings, SD 57007 USA.
NR 84
TC 2
Z9 3
U1 1
U2 4
PU AMER FISHERIES SOC
PI BETHESDA
PA 5410 GROSVENOR LANE, STE 110, BETHESDA, MD 20814-2199 USA
BN 978-1-934874-22-6
PY 2011
BP 303
EP 319
PG 17
WC Fisheries; Zoology
SC Fisheries; Zoology
GA BVR93
UT WOS:000292616800008
ER
PT J
AU Rolland, V
Hostetler, JA
Hines, TC
Johnson, FA
Percival, HF
Oli, MK
AF Rolland, Virginie
Hostetler, Jeffrey A.
Hines, Tommy C.
Johnson, Fred A.
Percival, H. Franklin
Oli, Madan K.
TI Effects of harvest and climate on population dynamics of northern
bobwhites in south Florida
SO WILDLIFE RESEARCH
LA English
DT Article
DE elasticity analysis; harvest management; LTRE analysis; management
scenarios; stochastic demography; weather conditions
ID CAUSE-SPECIFIC MORTALITY; SENSITIVITY-ANALYSIS; COMPENSATORY MORTALITY;
RELATIVE IMPORTANCE; GROWTH-RATE; SURVIVAL; HISTORY; IMPACT;
CONSEQUENCES; FLUCTUATIONS
AB Context. Hunting-related (hereafter harvest) mortality is assumed to be compensatory in many exploited species. However, when harvest mortality is additive, hunting can lead to population declines, especially on public land where hunting pressure can be intense. Recent studies indicate that excessive hunting may have contributed to the decline of a northern bobwhite (Colinus virginianus) population in south Florida.
Aims. This study aimed to estimate population growth rates to determine potential and actual contribution of vital rates to annual changes in population growth rates, and to evaluate the role of harvest and climatic variables on bobwhite population decline.
Methods. We used demographic parameters estimated from a six-year study to parameterise population matrix models and conduct prospective and retrospective perturbation analyses.
Key results. The stochastic population growth rate (lambda(S) = 0.144) was proportionally more sensitive to adult winter survival and survival of fledglings, nests and broods from first nesting attempts; the same variables were primarily responsible for annual changes in population growth rate. Demographic parameters associated with second nesting attempts made virtually no contribution to population growth rate. All harvest scenarios consistently revealed a substantial impact of harvest on bobwhite population dynamics. If the lowest harvest level recorded in the study period (i.e. 0.08 birds harvested per day per km(2) in 2008) was applied, lS would increase by 32.1%. Winter temperatures and precipitation negatively affected winter survival, and precipitation acted synergistically with harvest in affecting winter survival.
Conclusions. Our results suggest that reduction in winter survival due to overharvest has been an important cause of the decline in our study population, but that climatic factors might have also played a role. Thus, for management actions to be effective, assessing the contribution of primary (e. g. harvesting) but also secondary factors (e.g. climate) to population decline may be necessary.
Implications. Reducing hunting pressure would be necessary for the recovery of the bobwhite population at our study site. In addition, an adaptive harvest management strategy that considers weather conditions in setting harvest quota would help reverse the population decline further.
C1 [Rolland, Virginie; Hostetler, Jeffrey A.; Oli, Madan K.] Univ Florida, Dept Wildlife & Ecol Conservat, Gainesville, FL 32611 USA.
[Johnson, Fred A.; Percival, H. Franklin] Univ Florida, US Geol Survey, Florida Cooperat Fish & Wildlife Res Unit, Gainesville, FL 32611 USA.
RP Rolland, V (reprint author), Arkansas State Univ, Dept Biol Sci, State Univ, AR 72467 USA.
EM vrolland@astate.edu
RI Hostetler, Jeffrey/A-3345-2011
OI Hostetler, Jeffrey/0000-0003-3669-1758
FU Florida Fish and Wildlife Conservation Commission; Department of
Wildlife Ecology and Conservation, University of Florida
FX We thank R. Dimmick for leading field data collection efforts, and S.
and A. Brinkley, G. Coker, D. Caudill, D. Holt, J. McGrady, J. Sloane
and J. Scott for their significant contribution to data collection. We
are grateful to the many volunteers from the Southwest Florida Chapter
of Quail Unlimited who aided the research in many ways. Research was
funded by the Florida Fish and Wildlife Conservation Commission, and the
Department of Wildlife Ecology and Conservation, University of Florida.
Any use of trade, product or firm names is for descriptive purposes only
and does not imply endorsement by the USA Government.
NR 56
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U1 1
U2 29
PU CSIRO PUBLISHING
PI COLLINGWOOD
PA 150 OXFORD ST, PO BOX 1139, COLLINGWOOD, VICTORIA 3066, AUSTRALIA
SN 1035-3712
J9 WILDLIFE RES
JI Wildl. Res.
PY 2011
VL 38
IS 5
BP 396
EP 407
DI 10.1071/WR10239
PG 12
WC Ecology; Zoology
SC Environmental Sciences & Ecology; Zoology
GA 832IQ
UT WOS:000295798500005
ER
PT S
AU Janecke, SU
Dorsey, RJ
Forand, D
Steely, AN
Kirby, SM
Lutz, AT
Housen, BA
Belgarde, B
Langenheim, VE
Rittenour, TM
AF Janecke, Susanne U.
Dorsey, Rebecca J.
Forand, David
Steely, Alexander N.
Kirby, Stefan M.
Lutz, Andrew T.
Housen, Bernard A.
Belgarde, Benjamin
Langenheim, Victoria E.
Rittenour, Tammy M.
TI High Geologic Slip Rates Since Early Pleistocene Initiation of the San
Jacinto and San Felipe Fault Zones in the San Andreas Fault System:
Southern California, USA
SO HIGH GEOLOGIC SLIP RATES SINCE EARLY PLEISTOCENE INITIATION OF THE SAN
JACINTO AND SAN FELIPE FAULT ZONES IN THE SAN ANDREAS FAULT SYSTEM:
SOUTHERN CALIFORNIA, USA
SE Geological Society of America Special Papers
LA English
DT Article; Book
ID 1992 LANDERS EARTHQUAKE; GULF-OF-CALIFORNIA; LOS-ANGELES BASIN;
SALTON-TROUGH; STRIKE-SLIP; PENINSULAR RANGES; IMPERIAL-VALLEY;
STRUCTURAL EVOLUTION; STRAIN ACCUMULATION; TECTONIC EVOLUTION
C1 [Janecke, Susanne U.; Forand, David; Steely, Alexander N.; Kirby, Stefan M.; Belgarde, Benjamin; Rittenour, Tammy M.] Utah State Univ, Dept Geol, Logan, UT 84322 USA.
[Dorsey, Rebecca J.] 1272 Univ Oregon, Dept Geol Sci, Eugene, OR 97403 USA.
[Forand, David] Chevron USA Inc, Midland, TX 79705 USA.
[Kirby, Stefan M.] Utah Geol & Min Survey, Salt Lake City, UT 84114 USA.
[Lutz, Andrew T.] Fugro William Lettis & Associates Inc, Walnut Creek, CA 94596 USA.
[Housen, Bernard A.] Western Washington Univ, Dept Geol, Bellingham, WA 98225 USA.
[Belgarde, Benjamin] ExxonMobil, Houston, TX 77060 USA.
[Langenheim, Victoria E.] US Geol Survey, Menlo Pk, CA 94025 USA.
RP Janecke, SU (reprint author), Utah State Univ, Dept Geol, 4505 Old Main Hill, Logan, UT 84322 USA.
EM susanne.janecke@usu.edu
NR 167
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Z9 5
U1 1
U2 1
PU GEOLOGICAL SOC AMER INC
PI BOULDER
PA 3300 PENROSE PL, PO BOX 9140, BOULDER, CO 80301 USA
SN 0072-1077
BN 978-0-8137-2475-1
J9 GEOL SOC AM SPEC PAP
PY 2011
VL 475
BP 1
EP 48
DI 10.1130/2010.2475
PG 48
WC Geology
SC Geology
GA BWQ24
UT WOS:000294461400001
ER
PT J
AU Fegyveresi, JM
Alley, RB
Spencer, MK
Fitzpatrick, JJ
Steig, EJ
White, JWC
McConnell, JR
Taylor, KC
AF Fegyveresi, J. M.
Alley, R. B.
Spencer, M. K.
Fitzpatrick, J. J.
Steig, E. J.
White, J. W. C.
McConnell, J. R.
Taylor, K. C.
TI Late-Holocene climate evolution at the WAIS Divide site, West
Antarctica: bubble number-density estimates
SO JOURNAL OF GLACIOLOGY
LA English
DT Article
ID ICE-SHEET SURFACE; POLAR ICE; CORE; AIR; GREENLAND; LAYERS; FIRN
AB A surface cooling of similar to 1.7 degrees C occurred over the similar to two millennia prior to similar to 1700 CE at the West Antarctic ice sheet (WAIS) Divide site, based on trends in observed bubble number-density of samples from the WDC06A ice core, and on an independently constructed accumulation-rate history using annual-layer dating corrected for density variations and thinning from ice flow. Density increase and grain growth in polar firn are both controlled by temperature and accumulation rate, and the integrated effects are recorded in the number-density of bubbles as the firn changes to ice. Number-density is conserved in bubbly ice following pore close-off, allowing reconstruction of either paleotemperature or paleo-accumulation rate if the other is known. A quantitative late-Holocene paleoclimate reconstruction is presented for West Antarctica using data obtained from the WAIS Divide WDC06A ice core and a steady-state bubble number-density model. The resultant temperature history agrees closely with independent reconstructions based on stable-isotopic ratios of ice. The similar to 1.7 degrees C cooling trend observed is consistent with a decrease in Antarctic summer duration from changing orbital obliquity, although it remains possible that elevation change at the site contributed part of the signal. Accumulation rate and temperature dropped together, broadly consistent with control by saturation vapor pressure.
C1 [Fegyveresi, J. M.; Alley, R. B.] Penn State Univ, Dept Geosci, University Pk, PA 16802 USA.
[Fegyveresi, J. M.; Alley, R. B.] Earth & Environm Syst Inst, University Pk, PA 16802 USA.
[Spencer, M. K.] Lake Super State Univ, Dept Geol & Phys, Sault Ste Marie, MI 49783 USA.
[Fitzpatrick, J. J.] US Geol Survey, Geol & Environm Change Sci Ctr, Denver, CO 80225 USA.
[Steig, E. J.] Univ Washington, Dept Earth & Space Sci, Seattle, WA 98195 USA.
[Steig, E. J.] Univ Washington, Quaternary Res Ctr, Seattle, WA 98195 USA.
[White, J. W. C.] Univ Colorado, Inst Arctic & Alpine Res, UCB 450, Boulder, CO 80309 USA.
[McConnell, J. R.; Taylor, K. C.] Desert Res Inst, Reno, NV 89512 USA.
RP Fegyveresi, JM (reprint author), Penn State Univ, Dept Geosci, University Pk, PA 16802 USA.
EM jmf439@psu.edu
RI White, James/A-7845-2009; Steig, Eric/G-9088-2015; Taylor,
Kendrick/A-3469-2016
OI White, James/0000-0001-6041-4684; Steig, Eric/0000-0002-8191-5549;
Taylor, Kendrick/0000-0001-8535-1261
FU US National Science Foundation (NSF) [0539578, 0539232]; NSF [0440817,
0230396, 0944348, 0537930, 0839093, 0538427, 0739780, 0944191]
FX This work was supported by US National Science Foundation (NSF) grants
0539578 and 0539232. K. Walsh and N. Reed assisted with bubble
number-density measurements. The WAIS Divide Science Coordination Office
at the Desert Research Institute of Reno, Nevada, was responsible for
the collection and distribution of the WAIS Divide ice core and related
tasks under NSF grants 0440817, 0230396 and 0944348. delta18O
isotope data were obtained at the University of Washington under NSF
grant 0537930. The depth-age scale and accumulation-rate data were
determined at the Desert Research Institute under NSF grants 0839093,
0538427, 0739780 and 0944191. The NSF Office of Polar Programs also
funds the Ice Drilling Program Office and Ice Drilling Design and
Operations group for coring activities. The US National Ice Core
Laboratory, which curated the core and performed core processing, is
funded by the NSF. Raytheon Polar Services provided logistics support,
and the 109th New York Air National Guard provided airlift support in
Antarctica. We thank the hardworking people at all of these
organizations. Lastly, we thank T. Sowers and D. Pollard for unpublished
results, the US Geological Survey (USGS) Earth Surface Dynamics Program,
and the Delta*IsoLab at the University of Washington for assistance with
the isotope measurements.
NR 44
TC 9
Z9 9
U1 1
U2 17
PU INT GLACIOL SOC
PI CAMBRIDGE
PA LENSFIELD RD, CAMBRIDGE CB2 1ER, ENGLAND
SN 0022-1430
J9 J GLACIOL
JI J. Glaciol.
PY 2011
VL 57
IS 204
BP 629
EP 638
PG 10
WC Geography, Physical; Geosciences, Multidisciplinary
SC Physical Geography; Geology
GA 822BT
UT WOS:000295019400005
ER
PT J
AU Storey, JC
AF Storey, James C.
BE LeMoigne, J
Netanyahu, NS
Eastman, RD
TI Landsat image geocorrection and registration
SO IMAGE REGISTRATION FOR REMOTE SENSING
LA English
DT Article; Book Chapter
ID ORBIT GEOMETRIC CALIBRATION; PERFORMANCE
AB As the primary archive for the data acquired by the Landsat series of spacecraft, the U. S. Geological Survey Center for Earth Resources Observation and Science (EROS) is responsible for the processing systems that capture, correct, and distribute Landsat image data products. The Landsat ground system includes product generation components that apply the radiometric and geometric processing necessary to convert the digital detector samples acquired by the sensor to top-of-atmosphere radiance measurements referenced to an Earth-fixed coordinate system. These product generation systems implement geometric correction algorithms that use the instrument and spacecraft support data, provided in the Landsat data stream, to construct a model of the geometric relationship between the acquired image data samples and an Earth-fixed ground reference system. These support data include onboard measurements of instrument timing, spacecraft attitude (orientation) and jitter, and estimates of the spacecraft position and velocity derived from ground tracking data. The accuracy of the basic systematic geometric registration model is limited by uncertainties in these supporting data. In particular, the spacecraft position and attitude data typically contain residual biases on the order of tens to hundreds of meters. Fortunately, these errors are usually slowly varying, allowing for the registration of multiple Landsat images using simple, low-order techniques. When higher-accuracy products are required, additional capabilities of the Landsat ground system are employed to perform more precise geometric correction. This higher-level processing requires ancillary data sources, such as ground control points, to remove the residual pointing and position biases, and digital elevation data, to correct for the effects of terrain height on the Landsat viewing geometry. These ancillary data are used to derive corrections to the systematic geometric model that yield image products registered to a ground reference system to subpixel accuracy.
C1 USGS Ctr Earth Resources Observat & Sci EROS, Sioux Falls, SD USA.
RP Storey, JC (reprint author), USGS Ctr Earth Resources Observat & Sci EROS, Sioux Falls, SD USA.
NR 13
TC 1
Z9 1
U1 0
U2 0
PU CAMBRIDGE UNIV PRESS
PI CAMBRIDGE
PA THE PITT BUILDING, TRUMPINGTON ST, CAMBRIDGE CB2 1RP, CAMBS, ENGLAND
BN 978-0-52151-611-2
PY 2011
BP 400
EP 414
PG 15
WC Computer Science, Interdisciplinary Applications; Remote Sensing
SC Computer Science; Remote Sensing
GA BWC01
UT WOS:000293386100019
ER
PT J
AU Syphard, AD
Keeley, JE
Brennan, TJ
AF Syphard, Alexandra D.
Keeley, Jon E.
Brennan, Teresa J.
TI Factors affecting fuel break effectiveness in the control of large fires
on the Los Padres National Forest, California
SO INTERNATIONAL JOURNAL OF WILDLAND FIRE
LA English
DT Article
DE chaparral; firefighter; mapping; pre-fire fuel treatment; southern
California; strategic location; structural equation model; suppression;
wildland-urban interface
ID WILDLAND-URBAN INTERFACE; WESTERN UNITED-STATES; SIERRA-NEVADA;
LANDSCAPE; MODELS; MANAGEMENT; WILDFIRE; CLIMATE; REGIMES; ECOSYSTEMS
AB As wildfires have increased in frequency and extent, so have the number of homes developed in the wildland-urban interface. In California, the predominant approach to mitigating fire risk is construction of fuel breaks, but there has been little empirical study of their role in controlling large fires. We constructed a spatial database of fuel breaks on the Los Padres National Forest in southern California to better understand characteristics of fuel breaks that affect the behaviour of large fires and to map where fires and fuel breaks most commonly intersect. We evaluated whether fires stopped or crossed over fuel breaks over a 28-year period and compared the outcomes with physical characteristics of the sites, weather and firefighting activities during the fire event. Many fuel breaks never intersected fires, but others intersected several, primarily in historically fire-prone areas. Fires stopped at fuel breaks 46% of the time, almost invariably owing to fire suppression activities. Firefighter access to treatments, smaller fires and longer fuel breaks were significant direct influences, and younger vegetation and fuel break maintenance indirectly improved the outcome by facilitating firefighter access. This study illustrates the importance of strategic location of fuel breaks because they have been most effective where they provided access for firefighting activities.
C1 [Syphard, Alexandra D.] Conservat Biol Inst, La Mesa, CA 91941 USA.
[Keeley, Jon E.; Brennan, Teresa J.] US Geol Survey, Western Ecol Res Ctr, Sequoia Kings Canyon Field Stn, Three Rivers, CA 93271 USA.
[Keeley, Jon E.] Univ Calif Los Angeles, Dept Ecol & Evolutionary Biol, Los Angeles, CA 90095 USA.
RP Syphard, AD (reprint author), Conservat Biol Inst, 10423 Sierra Vista Ave, La Mesa, CA 91941 USA.
EM asyphard@consbio.org
FU US Geological Survey
FX Funding for this research was provided by the US Geological Survey
Multi-Hazards Demonstration Project. We thank John Abatzoglou and Tim
Brown for providing weather data, Jim Grace for providing guidance on
structural equation modelling and Steve Davis for providing expert
knowledge about firefighting on the Los Padres National Forest. Thanks
also to Erik C. Berg, Richard Halsey, Brian Halstead and Hugh Safford
for reviewing the manuscript and offering many valuable suggestions. Any
use of trade, product or firm names in this publication is for
descriptive purposes only and does not imply endorsement by the US
government.
NR 67
TC 16
Z9 17
U1 1
U2 26
PU CSIRO PUBLISHING
PI COLLINGWOOD
PA 150 OXFORD ST, PO BOX 1139, COLLINGWOOD, VICTORIA 3066, AUSTRALIA
SN 1049-8001
J9 INT J WILDLAND FIRE
JI Int. J. Wildland Fire
PY 2011
VL 20
IS 6
BP 764
EP 775
DI 10.1071/WF10065
PG 12
WC Forestry
SC Forestry
GA 821EJ
UT WOS:000294957400004
ER
PT J
AU Cipriano, RC
Austin, B
AF Cipriano, Rocco C.
Austin, Brian
BE Woo, PTK
Bruno, DW
TI Furunculosis and Other Aeromonad Diseases
SO FISH DISEASES AND DISORDERS, VOL 3: VIRAL, BACTERIAL AND FUNGAL
INFECTIONS, 2ND EDITION
LA English
DT Article; Book Chapter
ID SALMONICIDA SUBSP SALMONICIDA; SALMO-SALAR L; TROUT ONCORHYNCHUS-MYKISS;
POLYMERASE-CHAIN-REACTION; ICTALURUS-PUNCTATUS RAFINESQUE;
CYPRINUS-CARPIO L; LINKED-IMMUNOSORBENT-ASSAY; GOLDFISH
CARASSIUS-AURATUS; BACTERIAL FISH PATHOGENS; III SECRETION SYSTEM
C1 [Cipriano, Rocco C.] US Geol Survey, Natl Fish Hlth Res Lab, Kearneysville, WV 25430 USA.
[Austin, Brian] Univ Stirling, Inst Aquaculture, Stirling FK9 4LA, Scotland.
RP Cipriano, RC (reprint author), US Geol Survey, Natl Fish Hlth Res Lab, 11649 Leetown Rd, Kearneysville, WV 25430 USA.
NR 492
TC 6
Z9 6
U1 0
U2 3
PU CABI PUBLISHING-C A B INT
PI WALLINGFORD
PA CABI PUBLISHING, WALLINGFORD 0X10 8DE, OXON, ENGLAND
BN 978-1-84593-554-2
PY 2011
BP 424
EP 483
DI 10.1079/9781845935542.0424
D2 10.1079/9781845935542.0000
PG 60
WC Fisheries
SC Fisheries
GA BVY86
UT WOS:000293175200014
ER
PT B
AU Hofstra, AH
Christiansen, WD
Zohar, PB
Tousignant, G
AF Hofstra, Albert H.
Christiansen, William D.
Zohar, Pamela B.
Tousignant, Gilles
BE Steininger, R
Pennell, B
TI Lithogeochemistry of the Devonian Popovich Formation in the Northern
Carlin Trend, Nevada
SO GREAT BASIN EVOLUTION AND METALLOGENY, VOLS I AND II
LA English
DT Proceedings Paper
CT 6th Geological Society of Nevada on Great Basin Evolution and
Metallogeny
CY MAY 14-22, 2010
CL Nevada Bur Mines & Geol, Reno, NV
SP Soc Econom Geologists, Us Geolog Survey, Utah Geolog Assoc, Arizona Geolog Soc, Barrick Gold Exploration Inc, Haywood Securities, Newmont Mining Corp, Agnico Eagle US Ltd, Goldcorp, ALS Chemex, Boart Longyear, Evolving Gold Corp, Int Royal Corp, KinRoss Gold Corp, Nevada Div Minerals, Newcrest Mining Ltd, GIS Land Serv, Gold Fields Ltd, Hecla Mining Co, Kappes, Cassidy & Assoc, Floren Analyt Serv, Mine Dev Assoc, Allied Nevada Gold Corp, Amec, AuEx Inc, Centerra Gold, Geotemps Inc, Romarco Minerals US Inc, Nevada Mining Assoc, Carrington Consultants, Century Gold, Coeur, Drift Explorat Drilling Inc, Entree Gold Inc, Enviroscientists Inc, Fronteer Dev Inc, Fugro Airborne Surveys, Gold Summit Corp, Golden Predator Royal & Dev Corp, Jipangu Holdings Inc, Klondex Mines, Legend Inc, MGC Resources Inc, Miranda Gold Corp, Queensgate Resources Corp, Royal Gold Inc, Ruen Drilling Inc, Redstar Gold Corp, Rye Patch Gold Corp, Teck, Timberline Drilling, Timberline Resources Corp, US Gold Corp, Victoria Gold Corp, Western Energy Dev Corp, Western Lithium
HO Nevada Bur Mines & Geol
DE Screamer; Carlin; Nevada; gold; Popovich; Devonian; geochemistry; factor
analysis; oxygen; carbon; sulfur; isotope
ID GOLD DEPOSITS; EPITHERMAL TRANSITION; EVOLUTION; ORE; VAPOR;
MINERALIZATION; SULFIDATION; SOLUBILITY; DIAGENESIS; DISTRICT
AB The Devonian Popovich Formation is the major host for Carlin-type gold deposits in the northern Carlin trend, which contains >2800 t (90 Moz) of Au. The chemical and isotopic composition of barren and mineralized intervals of the Popovich Formation were determined in the Screamer sector of the Betze-Post deposit where there are numerous through-going, dike-filled, mineral-controlling structures. The stratigraphy sampled extends through the Wispy, Planar, Soft Sediment Deformation and Upper Mud units. The 332, 5-foot core samples analyzed are from 5 holes separated by as much as 600 m that are outside the zone of metamorphic recrystallization around the Jurassic Goldstrike Stock and below the level of supergene weathering and oxidation.
Core from barren intervals has <= 0.001 opt Au, whereas core from mineralized intervals has up to 0.64 opt Au. R-mode factor analysis revealed 4 element associations: CO(2)-(-Si)-Ca-Mn-Mg-Sr-(-Sb), Al-Nd-La-Ti-K-Sc-Co-Nb-Na-Ce-Ga, Ni-Cu-V-Zn-Cd-Organic C-Mo-Y-Cr, and Au-As-Mn-Fe-S-Li. The first three associations reflect the original carbonate, terrigenous detrital, and organic components of the Popovich Formation. The first association also reflects the occurrence of stibnite in jasperoid. The third association is typical of metalliferous black shales deposited under euxinic conditions and is best developed in the Upper Mud unit and an interval in the Planar unit and upper part of the Wispy unit. The fourth association is indicative of epigenetic Carlin-type Au mineralization and is best developed in the lower part of the Wispy unit. Though the association of Mn and Li with classic Carlin-type elements is unusual, Li is high in argillized rocks with low K(2)O/Al(2)O(3) and Mn is high in sulfidized rocks with low Fe(2)O(3)/Al(2)O(3).
Barren core has delta(18)O(carbonate) and delta(13)C(carbonate) values of 19 to 27 parts per thousand and -2.0 to 1.8 parts per thousand, respectively, which are typical of marine limestone. The lowest delta(13)C(carbonate) values are in carbonaceous strata of the Upper Mud unit. Some of the mineralized core is shifted to delta(18)O(carbonate) values as low as 8.6 parts per thousand with delta(13)C(carbonate) values near 0.5 parts per thousand and is high in Mn. Other core, with Au grades up to 0.39 opt, is not shifted significantly from its original isotopic composition. The negative 16 parts per thousand delta(18)O shift from that of typical marine limestone towards the meteoric water line in some of the mineralized core is indicative of alteration by hot meteoric water. Conversely, the mineralized core without such shifts apparently did not react with hot meteoric water. Likewise, the absence of a negative shift in delta(13)C towards the carbonatite box in all of the mineralized samples precludes a substantial input of magmatic CO(2).
Barren core has a wide range of delta(34)S(sulfide) values, from -16 to +16 parts per thousand, and a mean near 0 parts per thousand. There is a distinct stratigraphic interval of high delta(34)S(sulfide) values (>10 parts per thousand) in the Wispy and Planar units that is bound by overlying and underlying strata with low delta(34)S(sulfide) values (<5 parts per thousand). The interval with high delta(34)S(sulfide) values is indicative of bacterial reduction of a sulfate limited marine reservoir and has high concentrations of organic C and other elements indicative of euxinia. The strata with low delta(34)S(sulfide) values are characteristic of the kinetic fractionations associated with bacterial reduction of marine sulfate in an open marine environment. In mineralized core, as Au concentrations, Au/As, As/S, S/Al(2)0(3) and Fe(2)O(3)/Al(2)0(3) ratios, and DOS increase, delta(34)Ss(ulfide) values converge from the initial wide range of values towards a value near 0 parts per thousand. This result suggests that ore stage pyrite with delta(34)S near 0 parts per thousand formed by sulfidation of host rock Fe and Fe in a contrasting fluid. While the 0 parts per thousand S may be evidence that Au was introduced by magmatic H(2)S, the negative correlation between Au, Cu and Te does not support such a model. Considering that ore pyrite in the heart of the Betze-Post deposit has delta(34)S values near 9 parts per thousand, the mean delta(34)S(sulfide) value of the Popovich Formation is near 0%, the preferred host in the Wispy unit has low delta(34)S(sulfide) values, and Screamer is on the periphery of Betze-Post, it is perhaps more likely that the 0 parts per thousand S in Screamer reflects changes in fluid composition associated with wall rock reactions and lateral flow away from central high grade conduits along the Post fault system (i.e. zoning).
While these results permit multiple interpretations they suggest that a minor proportion of the ore formed without meteoric or magmatic fluid inputs or typical Carlin-type processes. Such ore could be evidence of an earlier event (sedex?). Additional work is needed to unambiguously ascertain the age(s) and source(s) of ore fluid components in each ore type. Further chemical and isotopic characterization of ore pyrite in each ore body along the entire Carlin trend may define the loci of fluid upwelling and the directions of fluid movement.
C1 [Hofstra, Albert H.; Christiansen, William D.] US Geol Survey, Denver, CO 80225 USA.
RP Hofstra, AH (reprint author), US Geol Survey, MS 973,Box 25046, Denver, CO 80225 USA.
EM ahofstra@usgs.gov
NR 45
TC 0
Z9 0
U1 0
U2 5
PU DESTECH PUBLICATIONS, INC
PI LANCASTER
PA 439 DUKE STREET, LANCASTER, PA 17602-4967 USA
BN 978-1-60595-040-2
PY 2011
BP 63
EP 96
PG 34
WC Geology; Metallurgy & Metallurgical Engineering
SC Geology; Metallurgy & Metallurgical Engineering
GA BWF52
UT WOS:000293810500004
ER
PT B
AU Howard, KA
AF Howard, Keith A.
BE Steininger, R
Pennell, B
TI The upper crust on its side-steeply tilted slabs in the Basin and Range
SO GREAT BASIN EVOLUTION AND METALLOGENY, VOLS I AND II
LA English
DT Proceedings Paper
CT 6th Geological Society of Nevada on Great Basin Evolution and
Metallogeny
CY MAY 14-22, 2010
CL Nevada Bur Mines & Geol, Reno, NV
SP Soc Econom Geologists, Us Geolog Survey, Utah Geolog Assoc, Arizona Geolog Soc, Barrick Gold Exploration Inc, Haywood Securities, Newmont Mining Corp, Agnico Eagle US Ltd, Goldcorp, ALS Chemex, Boart Longyear, Evolving Gold Corp, Int Royal Corp, KinRoss Gold Corp, Nevada Div Minerals, Newcrest Mining Ltd, GIS Land Serv, Gold Fields Ltd, Hecla Mining Co, Kappes, Cassidy & Assoc, Floren Analyt Serv, Mine Dev Assoc, Allied Nevada Gold Corp, Amec, AuEx Inc, Centerra Gold, Geotemps Inc, Romarco Minerals US Inc, Nevada Mining Assoc, Carrington Consultants, Century Gold, Coeur, Drift Explorat Drilling Inc, Entree Gold Inc, Enviroscientists Inc, Fronteer Dev Inc, Fugro Airborne Surveys, Gold Summit Corp, Golden Predator Royal & Dev Corp, Jipangu Holdings Inc, Klondex Mines, Legend Inc, MGC Resources Inc, Miranda Gold Corp, Queensgate Resources Corp, Royal Gold Inc, Ruen Drilling Inc, Redstar Gold Corp, Rye Patch Gold Corp, Teck, Timberline Drilling, Timberline Resources Corp, US Gold Corp, Victoria Gold Corp, Western Energy Dev Corp, Western Lithium
HO Nevada Bur Mines & Geol
DE Cenozoic; Basin and Range; Ruby Mountains; homoclines; core complex
ID METAMORPHIC CORE COMPLEX; APATITE (U-TH)/HE THERMOCHRONOMETRY; SOUTH
VIRGIN MOUNTAINS; EXPOSED CROSS-SECTION; EXTENSIONAL OROGEN; NORTHEAST
NEVADA; COLORADO PLATEAU; PEQUOP-MOUNTAINS; TERTIARY ROCKS;
UNITED-STATES
AB Tilted slabs that expose as much as 8-15 km of the upper crust in the Basin and Range province allow analysis of pre-tilt depth variations in igneous systems and thermal structure. Before tilting the slabs were panels between moderately to steeply dipping Tertiary normal faults. The slabs and their bounding normal faults were tilted to piggyback positions on deeper footwalls that warped up isostatically beneath them during crustal stretching and tectonic unloading. Stratal dips within some slabs are now vertical or even slightly overturned, especially in the southern Basin and Range, where thick sections of basement granite and gneiss are tilted homoclinally as determined from both stratified cover and intrusive-sheet proxies of original horizontality. Some tilted slabs of basement rock display faults that splay upwards into overlying cover sequences, folding them to shallower dips, so stratified rocks are not always the best indicators of slab tilt. The 12-15-km maximum exposed paleodepth for the slabs matches the depth of the modern base of the seismogenic zone of normal-fault earthquakes in the Basin and Range, and so this depth is inferred to represent the pre-tilt base of the brittle part of the extending crust. Many highly tilted slabs are upper-plates to metamorphic core complexes, but not all core complexes expose thick recumbent upper-plate slabs. Paleozoic stratal sequences in thin upper-plate fault slices commonly are dragged or sheared subparallel to the faults, thereby obscuring the original fault-bedding cutoff angles and maximum block tilt. The Ruby Mountains core complex, for example, preserves only scraps of upper-plate rocks as domed-up extensional klippen uneven in stratal dips, and most of the thick crustal section that originally overlay the uplifted metamorphic core now must reside at depth to the west. In contrast, large intact tilted fault-bounded slabs of plutonic and metamorphic basement rock near core complexes in the Colorado River extensional corridor and the San Pedro Trough expose 8-15 km paleodepths that originally roofed the metamorphic cores; the exposed paleodepths imply that deeper core-complex footwalls rolled up beneath such slabs.
C1 US Geol Survey, Menlo Pk, CA 94025 USA.
RP Howard, KA (reprint author), US Geol Survey, MS 973, Menlo Pk, CA 94025 USA.
EM khoward@usgs.gov
NR 70
TC 0
Z9 0
U1 0
U2 2
PU DESTECH PUBLICATIONS, INC
PI LANCASTER
PA 439 DUKE STREET, LANCASTER, PA 17602-4967 USA
BN 978-1-60595-040-2
PY 2011
BP 289
EP 297
PG 9
WC Geology; Metallurgy & Metallurgical Engineering
SC Geology; Metallurgy & Metallurgical Engineering
GA BWF52
UT WOS:000293810500016
ER
PT B
AU Vikre, PG
Henry, CD
AF Vikre, Peter G.
Henry, Christopher D.
BE Steininger, R
Pennell, B
TI Quartz-alunite alteration cells in the southern segment of the Ancestral
Cascades Magmatic Arc
SO GREAT BASIN EVOLUTION AND METALLOGENY, VOLS I AND II
LA English
DT Proceedings Paper
CT 6th Geological Society of Nevada on Great Basin Evolution and
Metallogeny
CY MAY 14-22, 2010
CL Nevada Bur Mines & Geol, Reno, NV
SP Soc Econom Geologists, Us Geolog Survey, Utah Geolog Assoc, Arizona Geolog Soc, Barrick Gold Exploration Inc, Haywood Securities, Newmont Mining Corp, Agnico Eagle US Ltd, Goldcorp, ALS Chemex, Boart Longyear, Evolving Gold Corp, Int Royal Corp, KinRoss Gold Corp, Nevada Div Minerals, Newcrest Mining Ltd, GIS Land Serv, Gold Fields Ltd, Hecla Mining Co, Kappes, Cassidy & Assoc, Floren Analyt Serv, Mine Dev Assoc, Allied Nevada Gold Corp, Amec, AuEx Inc, Centerra Gold, Geotemps Inc, Romarco Minerals US Inc, Nevada Mining Assoc, Carrington Consultants, Century Gold, Coeur, Drift Explorat Drilling Inc, Entree Gold Inc, Enviroscientists Inc, Fronteer Dev Inc, Fugro Airborne Surveys, Gold Summit Corp, Golden Predator Royal & Dev Corp, Jipangu Holdings Inc, Klondex Mines, Legend Inc, MGC Resources Inc, Miranda Gold Corp, Queensgate Resources Corp, Royal Gold Inc, Ruen Drilling Inc, Redstar Gold Corp, Rye Patch Gold Corp, Teck, Timberline Drilling, Timberline Resources Corp, US Gold Corp, Victoria Gold Corp, Western Energy Dev Corp, Western Lithium
HO Nevada Bur Mines & Geol
DE quartz-alunite; alteration; southern Cascades; magmatic arc; Au-Ag-Cu
deposits; S deposits; geochronology; isotopes
ID WESTERN UNITED-STATES; PRECIOUS-METAL MINERALIZATION; STABLE-ISOTOPE
GEOCHEMISTRY; NEVADA VOLCANIC FIELD; NORTHERN GREAT-BASIN; ASH-FLOW
TUFFS; SIERRA-NEVADA; GOLD DEPOSITS; HYDROTHERMAL SYSTEMS; VIRGINIA
RANGE
AB At least 40 alteration cells characterized by hydrothermal quartz and alunite occur in the southern segment of the ancestral Cascades magmatic arc from Portola, CA to Goldfield, NV. Significant amounts of Au, Ag, Cu and S degrees (elemental sulfur) were produced from 6 cells (Goldfield, Paradise Peak, Borealis, and Ramsey, NV; Masonic and Monitor, CA), 3 cells contain Au, Ag, and S degrees resources (Isabella-Pearl, NV; Golden Dome and Cinnabar Canyon, CA), and minor amounts of Au, Ag, Cu, and Hg have been produced from several cells, but no appreciable metal concentrations have been identified in most cells. Cell exposures vary from similar to 70 km(2) (Goldfield) to hundreds of m(2) (Mystic, CA), and have known vertical dimensions of hundreds of meters. Cells range in age from about 22 Ma (Goldfield and Pyramid, NV) to 4 Ma (Painted Rock, CA). Most cells formed in andesite and dacite flows and subvolcanic intrusions immediately after their eruption and/or emplacement, and are confined to these slightly older (0 to 2 Ma) volcanic rocks, although several cells (Goldfield; Masonic; Golden Dome) partly formed in Mesozoic and Paleozoic rocks.
In addition to quartz and alunite, hydrothermal minerals common to cells are kaolinite, K-mica, pyrite, and clay minerals. In cells in which fluids circulated through permeable high-angle faults and tensional fissures, alteration minerals are zoned with lenticular zones of vuggy silica enclosed by keel-shaped to sub-horizontal masses of fine-grained silica minerals +/- alunite +/- pyrite, and flanked by proximal selvages composed of clay minerals (kaolinite; dickite), pyrite and K-mica, and distal selvages containing illite-montomorillonite, chlorite, and calcite. These alteration assemblages formed by dissolution and alteration by low pH fluids of feldspars and mafic minerals in host rocks and breccias clasts, and by redistribution of silica at temperatures of 250 +/- 50 degrees C, based on T degrees C(delta 34S) (sulfide-sulfate). Dimensions of alteration zones are meters to tens of meters laterally, and tens to hundreds of meters vertically; in large cells with numerous structural conduits, alteration zones commonly coalesce. Cells that appear to have formed from a single magmatic-hydrothermal event are indistinctly zoned, and planar fluid conduits are absent or uncommon.
Enargite-luzonite, famatinite, tennantite, gold, and numerous Cu-As-Sb-Au-Ag-Pb-Zn-Te-Se-S minerals in complex parageneses characterize mineralized cells. These minerals, along with quartz, pyrite, and minor sulfate minerals were deposited by hydrothermal fluids also at 250 +/- 50 degrees C (as indicated by T degrees C(delta 34S) (sulfide-sulfate) and fluid inclusion microthermometry); fluids circulated through fractures and breccias in previously silicified structures that were ruptured by tectonic and hydraulic processes. S degrees in stratiform deposits was sublimated by partial oxidation of H(2)S in voids and fractures in volcaniclastic rocks and enclosing flows that were leached and silicified similarly to structures that contain metal deposits, but were subsequently dewatered by regional depression of groundwater saturation, or by boiling. Sulfur in alteration zones and deposits was derived from disproportionation of magmatic SO(2) which acidified and heated groundwater in saturated eruptive rocks.
Mid- to late Cenozoic magmatism that generated the quartz-alunite alteration cells was part of the ancestral Cascade arc that developed as magmatism swept southwestward through Nevada during rollback of the shallow Farallon slab following Laramide flat-slab subduction. Intermediate composition magmatism typical of continental volcanic arcs began similar to 32 Ma in western Nevada and was contemporaneous with the ignimbrite flare-up (caldera formation) in central Nevada. A sharp boundary along what is now the northeastern edge of the Walker Lane separates the region of the ignimbrite flare-up from a region of intermediate composition volcanism with no documented calderas. At least by similar to 20 Ma, an intermediate volcanic arc (the ancestral Cascades arc) extended from the latitude of Goldfield northward along the Nevada California border.
Cell formation required arc magmatism as a source of heat and volatiles, but numerous questions remain as to the specific sources of metals and volatiles, why cells are associated with certain volcanic centers, and why cells are restricted to the western Nevada-eastern California arc segment. Answers to those questions probably include some combination of crustal and lithospheric characteristics, tectonic setting (e.g., presence or absence of contemporaneous extension or transtension), and magmatic emplacement and degassing processes.
C1 [Vikre, Peter G.] Univ Nevada, US Geol Survey, Mackay Sch Earth Sci & Engn, Reno, NV 89557 USA.
RP Vikre, PG (reprint author), Univ Nevada, US Geol Survey, Mackay Sch Earth Sci & Engn, MS 176, Reno, NV 89557 USA.
EM pvikre@usgs.gov
NR 136
TC 8
Z9 8
U1 0
U2 3
PU DESTECH PUBLICATIONS, INC
PI LANCASTER
PA 439 DUKE STREET, LANCASTER, PA 17602-4967 USA
BN 978-1-60595-040-2
PY 2011
BP 701
EP 745
PG 45
WC Geology; Metallurgy & Metallurgical Engineering
SC Geology; Metallurgy & Metallurgical Engineering
GA BWF52
UT WOS:000293810500038
ER
PT B
AU Breit, GN
Hunt, AG
Wolf, RE
Koenig, AE
Fifarek, RH
Coolbaugh, MF
AF Breit, George N.
Hunt, Andrew G.
Wolf, Ruth E.
Koenig, Alan E.
Fifarek, Richard H.
Coolbaugh, Mark F.
BE Steininger, R
Pennell, B
TI Are modern geothermal waters in northwest Nevada forming epithermal gold
deposits?
SO GREAT BASIN EVOLUTION AND METALLOGENY, VOLS I AND II
LA English
DT Proceedings Paper
CT 6th Geological Society of Nevada on Great Basin Evolution and
Metallogeny
CY MAY 14-22, 2010
CL Nevada Bur Mines & Geol, Reno, NV
SP Soc Econom Geologists, Us Geolog Survey, Utah Geolog Assoc, Arizona Geolog Soc, Barrick Gold Exploration Inc, Haywood Securities, Newmont Mining Corp, Agnico Eagle US Ltd, Goldcorp, ALS Chemex, Boart Longyear, Evolving Gold Corp, Int Royal Corp, KinRoss Gold Corp, Nevada Div Minerals, Newcrest Mining Ltd, GIS Land Serv, Gold Fields Ltd, Hecla Mining Co, Kappes, Cassidy & Assoc, Floren Analyt Serv, Mine Dev Assoc, Allied Nevada Gold Corp, Amec, AuEx Inc, Centerra Gold, Geotemps Inc, Romarco Minerals US Inc, Nevada Mining Assoc, Carrington Consultants, Century Gold, Coeur, Drift Explorat Drilling Inc, Entree Gold Inc, Enviroscientists Inc, Fronteer Dev Inc, Fugro Airborne Surveys, Gold Summit Corp, Golden Predator Royal & Dev Corp, Jipangu Holdings Inc, Klondex Mines, Legend Inc, MGC Resources Inc, Miranda Gold Corp, Queensgate Resources Corp, Royal Gold Inc, Ruen Drilling Inc, Redstar Gold Corp, Rye Patch Gold Corp, Teck, Timberline Drilling, Timberline Resources Corp, US Gold Corp, Victoria Gold Corp, Western Energy Dev Corp, Western Lithium
HO Nevada Bur Mines & Geol
DE epithermal gold; geochemistry; geothermal fluids
ID UNITED-STATES; GREAT-BASIN; NEW-ZEALAND; METALS; EVOLUTION; ICELAND;
SYSTEMS; FLUIDS
AB Hydrothermal systems currently are active near some gold deposits in northwestern Nevada. Possible links of these modern systems to gold mineralization were evaluated by chemically and isotopically analyzing water samples from the Brady, Dixie Valley, Humboldt House, San Emidio-Empire, Soda Lake, and Wabuska geothermal areas. In addition, quartz veins from Humboldt House and the adjacent Florida Canyon Mine were analyzed to compare ore and gangue phases with those predicted to form from proximal hydrothermal fluids.
Nearly all water samples are alkali-chloride-type. Total dissolved solids range from 800 to 3900 mg/L, and pH varies from 5.6 to 7.8. Geochemical modeling with SOLVEQ, WATCH, and CHILLER predict the precipitation of silica in all systems during cooling. Anhydrite, calcite, barite, pyrite, base-metal sulfides, and alumino-silicates are variably saturated at calculated reservoir temperatures and also precipitate during boiling/cooling of some fluids. Measured dissolved gold concentrations are low (<0.2 mu g/L), but are generally consistent with contents predicted by equilibrium of sampled solutions with elemental gold at reservoir temperatures. Although the modern geothermal waters can precipitate ore minerals, the low gold and other ore metal concentrations require very large fluid volumes to form a deposit of economic interest.
C1 [Breit, George N.; Hunt, Andrew G.; Wolf, Ruth E.; Koenig, Alan E.] US Geol Survey, Denver, CO 80225 USA.
RP Breit, GN (reprint author), US Geol Survey, Box 25046, Denver, CO 80225 USA.
EM gbreit@usgs.gov
NR 34
TC 2
Z9 2
U1 2
U2 5
PU DESTECH PUBLICATIONS, INC
PI LANCASTER
PA 439 DUKE STREET, LANCASTER, PA 17602-4967 USA
BN 978-1-60595-040-2
PY 2011
BP 833
EP 844
PG 12
WC Geology; Metallurgy & Metallurgical Engineering
SC Geology; Metallurgy & Metallurgical Engineering
GA BWF52
UT WOS:000293810500045
ER
PT B
AU Hunt, AG
Landis, GP
Breit, G
Wolf, R
Bergfeld, D
Rytuba, JJ
AF Hunt, Andrew G.
Landis, Gary P.
Breit, George
Wolf, Ruth
Bergfeld, Deborah
Rytuba, James J.
BE Steininger, R
Pennell, B
TI Identifying magmatic versus amagmatic sources for modern geothermal
systems associated with epithermal mineralization using noble gas
geochemistry
SO GREAT BASIN EVOLUTION AND METALLOGENY, VOLS I AND II
LA English
DT Proceedings Paper
CT 6th Geological Society of Nevada on Great Basin Evolution and
Metallogeny
CY MAY 14-22, 2010
CL Nevada Bur Mines & Geol, Reno, NV
SP Soc Econom Geologists, Us Geolog Survey, Utah Geolog Assoc, Arizona Geolog Soc, Barrick Gold Exploration Inc, Haywood Securities, Newmont Mining Corp, Agnico Eagle US Ltd, Goldcorp, ALS Chemex, Boart Longyear, Evolving Gold Corp, Int Royal Corp, KinRoss Gold Corp, Nevada Div Minerals, Newcrest Mining Ltd, GIS Land Serv, Gold Fields Ltd, Hecla Mining Co, Kappes, Cassidy & Assoc, Floren Analyt Serv, Mine Dev Assoc, Allied Nevada Gold Corp, Amec, AuEx Inc, Centerra Gold, Geotemps Inc, Romarco Minerals US Inc, Nevada Mining Assoc, Carrington Consultants, Century Gold, Coeur, Drift Explorat Drilling Inc, Entree Gold Inc, Enviroscientists Inc, Fronteer Dev Inc, Fugro Airborne Surveys, Gold Summit Corp, Golden Predator Royal & Dev Corp, Jipangu Holdings Inc, Klondex Mines, Legend Inc, MGC Resources Inc, Miranda Gold Corp, Queensgate Resources Corp, Royal Gold Inc, Ruen Drilling Inc, Redstar Gold Corp, Rye Patch Gold Corp, Teck, Timberline Drilling, Timberline Resources Corp, US Gold Corp, Victoria Gold Corp, Western Energy Dev Corp, Western Lithium
HO Nevada Bur Mines & Geol
DE Helium; Noble Gas; the Great Basin; Geothermal; Clear Lake; Lassen
Volcanic National Park; Gold
ID CALIFORNIA; ORIGIN
AB Modern geothermal systems in the Great Basin of California and Nevada typically are characterized as the result of a focused and identifiable magmatic heat source or of a regionally dispersed amagmatic heat flux. Young (< 7Ma), economically viable epithermal Au deposits are closely associated with some modern, presumably amagmatic geothermal systems. This close spatial association of the Au deposits to the modern geothermal systems has led to speculation of an amagmatic origin for the deposits and that the modern geothermal systems could be actively precipitating Au in the subsurface. In an effort to clarify the possible role of amagmatic geothermal systems as the source of young to modern epithermal Au mineralization, noble gas and fluid chemistry samples were collected from active, amagmatic geothermal systems in Nevada (Wabuska, San Emidio, Brady Hot Springs, Humboldt House [Florida Canyon], and Soda Lake) as well as modern magmatic geothermal systems in California (Clear Lake, Wilber Springs, Lassen Volcanic National Park and Mammoth Mountain). Calculated silica geothermometery on the fluids from the Nevada geothermal systems agrees well with the measured down-hole temperatures from the reservoirs. The calculated reservoir temperatures of these systems span the range of 150 to 210 degrees C, except Wabuska which yields a temperature of 135 degrees C. Noble gas compositions from both magmatic or amagmatic systems are characterized by atmospherically derived components that have mixed with deeper non-atmospheric sources. Helium isotopic data, after correction for atmospheric components (excess He), shows a dominance of crustal helium (87 to 97 percent of the excess He component) supporting an amagmatic origin, except in the case of the Soda Lake, where almost 54 to 59 percent of the excess He is mantle derived. Comparison of the He data with Au concentrations in fluid samples shows a positive correlation between gold and the mantle helium content in both the magmatic and amagmatic systems. This relationship is at odds with current theories that the modern, amagmatic geothermal systems are responsible for substantial Au transport that resulted in the spatially associated young epithermal deposits. This postulate is further supported from noble and bulk gas compositions from fluid inclusions in silica precipitates from Florida Canyon and Dixie Valley.
C1 [Hunt, Andrew G.; Landis, Gary P.; Breit, George; Wolf, Ruth] US Geol Survey, Denver Fed Ctr, Lakewood, CO 80225 USA.
RP Hunt, AG (reprint author), US Geol Survey, Denver Fed Ctr, MS 963,Bld 21, Lakewood, CO 80225 USA.
EM AHUNT@usgs.gov
NR 27
TC 0
Z9 0
U1 1
U2 4
PU DESTECH PUBLICATIONS, INC
PI LANCASTER
PA 439 DUKE STREET, LANCASTER, PA 17602-4967 USA
BN 978-1-60595-040-2
PY 2011
BP 899
EP 908
PG 10
WC Geology; Metallurgy & Metallurgical Engineering
SC Geology; Metallurgy & Metallurgical Engineering
GA BWF52
UT WOS:000293810500049
ER
PT B
AU du Bray, EA
Nash, JT
Meeker, GP
Adam, D
Wright, WA
AF du Bray, Edward A.
Nash, J. Thomas
Meeker, Gregory P.
Adam, David
Wright, William A.
BE Steininger, R
Pennell, B
TI Petrology and hydrothermal alteration of Jurassic intrusive rocks
associated with gold deposits in the Bald Mountain mining district,
White Pine County, Nevada
SO GREAT BASIN EVOLUTION AND METALLOGENY, VOLS I AND II
LA English
DT Proceedings Paper
CT 6th Geological Society of Nevada on Great Basin Evolution and
Metallogeny
CY MAY 14-22, 2010
CL Nevada Bur Mines & Geol, Reno, NV
SP Soc Econom Geologists, Us Geolog Survey, Utah Geolog Assoc, Arizona Geolog Soc, Barrick Gold Exploration Inc, Haywood Securities, Newmont Mining Corp, Agnico Eagle US Ltd, Goldcorp, ALS Chemex, Boart Longyear, Evolving Gold Corp, Int Royal Corp, KinRoss Gold Corp, Nevada Div Minerals, Newcrest Mining Ltd, GIS Land Serv, Gold Fields Ltd, Hecla Mining Co, Kappes, Cassidy & Assoc, Floren Analyt Serv, Mine Dev Assoc, Allied Nevada Gold Corp, Amec, AuEx Inc, Centerra Gold, Geotemps Inc, Romarco Minerals US Inc, Nevada Mining Assoc, Carrington Consultants, Century Gold, Coeur, Drift Explorat Drilling Inc, Entree Gold Inc, Enviroscientists Inc, Fronteer Dev Inc, Fugro Airborne Surveys, Gold Summit Corp, Golden Predator Royal & Dev Corp, Jipangu Holdings Inc, Klondex Mines, Legend Inc, MGC Resources Inc, Miranda Gold Corp, Queensgate Resources Corp, Royal Gold Inc, Ruen Drilling Inc, Redstar Gold Corp, Rye Patch Gold Corp, Teck, Timberline Drilling, Timberline Resources Corp, US Gold Corp, Victoria Gold Corp, Western Energy Dev Corp, Western Lithium
HO Nevada Bur Mines & Geol
DE Bald Mountain; Nevada; reduced intrusions; Jurassic; gold; geochemistry;
petrography; alteration; petrogenesis; mineral chemistry; volatiles
ID NORTHERN GREAT-BASIN; RARE-EARTH ELEMENT; GRANITIC-ROCKS; EPITHERMAL
DEPOSITS; IGNEOUS SYSTEMS; UNITED-STATES; CARLIN TREND; EVOLUTION;
ORIGIN; SERIES
AB Late Jurassic intrusive rocks in the Bald Mountain mining district of northern Nevada are spatially and genetically associated with significant coeval gold deposits. A volumetrically dominant monzogranite, the 159 Ma Bald Mountain pluton, is petro-graphically distinct but geochemically similar to other northern Nevada intrusive rocks. The monzogranite has features typical of reduced intrusions, including a very low abundance of opaque oxide minerals, the virtual absence of magnetite, and practically no aeromagnetic expression. The monzogranite contains distinctive 1-cm-long K-feldspar, plagioclase, and round quartz phenocrysts, as well as biotite, surrounded by a fine-grained groundmass. A set of quartz-feldspar porphyry dikes, compositionally indistinguishable from the monzogranite, and a set of basaltic andesite dikes intrude, but are essentially coeval with, the monzogranite pluton. The porphyry dikes contain phenocrysts that are identical in composition to those of the monzogranite, though less abundant, in an aphanitic groundmass. The porphyritic basaltic andesite dikes intrude mineralized rock and consist of an intersertal inter-growth of plagioclase, hornblende, and/or biotite, also in an aphanitic groundmass. Jurassic lamprophyre dikes and aplite sills are minor components of the igneous rock suite in the Bald Mountain district. Geochemical data suggest that the Bald Mountain monzogranite, quartz-feldspar porphyry dikes, and basaltic andesite dikes are petrogenetically related and associated with back-arc, subduction-related processes along the west margin of Jurassic North America. Petrographic features, geochemical data and limited geochronology suggest that the aplite sills are unrelated to other intrusive rocks and mineral deposits in the district. The petrogenesis of the lamprophyre dikes, as indicated by their petrographic and geochemical features, is unrelated to that of other intrusive rocks in the district, although the associated magma reservoir may have contributed volatile constituents to mineralizing processes.
In the Bald Mountain district, gold deposition was accompanied by hypogene phyllic alteration and silicification, whereas superimposed supergene argillic alteration evolved principally as a consequence of oxidative pyrite weathering. Together, these alteration processes obscure primary petrographic features of all Bald Mountain intrusive rocks and render protolith identification difficult. However, relative abundances of immobile trace elements, especially Ta, Yb, Ni, Cr, in the unaltered igneous rocks are diagnostic for each of the five rock types and facilitate identification of their altered equivalents. Alteration processes caused volatile element concentrations to increase significantly, probably in response to groundmass silicification and growth of volatile-rich minerals such as kaolinite, sericite, calcite, and pyrite as well as iron oxide minerals. In contrast, the alkali elements are markedly depleted, probably as a consequence of feldspar and biotite destruction.
Geologic relations suggest that the parent magma which formed the Bald Mountain monzogranite pluton was reduced by assimilation of carbonaceous Paleozoic sedimentary rocks that host the intrusion. Reducing conditions favored speciation of sulfur in the exsolved volatile phase as hydrogen sulfide; fluids of this type preferentially transport gold relative to base metals. Globally, reduced intrusions are associated with gold deposits that are also enriched in Bi, W, Sn, and Mo, but not base metals. Relations among reduced intrusions, their exsolved fluids, and the relative abundance of gold versus base metals are in accord with empirical evidence that relatively reduced, ilmenite-series, back-arc igneous rocks, such as those exposed in the Bald Mountain district, are associated with Au, W, Sn, and Mo deposits and Bi enrichments. In contrast, relatively oxidized, magnetite series, magmatic arc rocks are associated with Cu, Cu-Mo, and Cu-Au porphyry deposits, such as those that occur elsewhere in northern Nevada.
C1 [du Bray, Edward A.; Nash, J. Thomas; Meeker, Gregory P.; Adam, David] US Geol Survey, Washington, DC 20242 USA.
RP du Bray, EA (reprint author), US Geol Survey, Washington, DC 20242 USA.
EM edubray@usgs.gov
NR 60
TC 1
Z9 1
U1 0
U2 3
PU DESTECH PUBLICATIONS, INC
PI LANCASTER
PA 439 DUKE STREET, LANCASTER, PA 17602-4967 USA
BN 978-1-60595-040-2
PY 2011
BP 1019
EP 1038
PG 20
WC Geology; Metallurgy & Metallurgical Engineering
SC Geology; Metallurgy & Metallurgical Engineering
GA BWF52
UT WOS:000293810500055
ER
PT B
AU Holm-Denoma, CS
Hofstra, AH
Noble, PJ
Leslie, SA
AF Holm-Denoma, Christopher S.
Hofstra, Albert H.
Noble, Paula J.
Leslie, Stephen A.
BE Steininger, R
Pennell, B
TI Paleozoic stratigraphy and kinematics of the Roberts Mountains
allochthon in the Independence Mountains, northern Nevada
SO GREAT BASIN EVOLUTION AND METALLOGENY, VOLS I AND II
LA English
DT Proceedings Paper
CT 6th Geological Society of Nevada on Great Basin Evolution and
Metallogeny
CY MAY 14-22, 2010
CL Nevada Bur Mines & Geol, Reno, NV
SP Soc Econom Geologists, Us Geolog Survey, Utah Geolog Assoc, Arizona Geolog Soc, Barrick Gold Exploration Inc, Haywood Securities, Newmont Mining Corp, Agnico Eagle US Ltd, Goldcorp, ALS Chemex, Boart Longyear, Evolving Gold Corp, Int Royal Corp, KinRoss Gold Corp, Nevada Div Minerals, Newcrest Mining Ltd, GIS Land Serv, Gold Fields Ltd, Hecla Mining Co, Kappes, Cassidy & Assoc, Floren Analyt Serv, Mine Dev Assoc, Allied Nevada Gold Corp, Amec, AuEx Inc, Centerra Gold, Geotemps Inc, Romarco Minerals US Inc, Nevada Mining Assoc, Carrington Consultants, Century Gold, Coeur, Drift Explorat Drilling Inc, Entree Gold Inc, Enviroscientists Inc, Fronteer Dev Inc, Fugro Airborne Surveys, Gold Summit Corp, Golden Predator Royal & Dev Corp, Jipangu Holdings Inc, Klondex Mines, Legend Inc, MGC Resources Inc, Miranda Gold Corp, Queensgate Resources Corp, Royal Gold Inc, Ruen Drilling Inc, Redstar Gold Corp, Rye Patch Gold Corp, Teck, Timberline Drilling, Timberline Resources Corp, US Gold Corp, Victoria Gold Corp, Western Energy Dev Corp, Western Lithium
HO Nevada Bur Mines & Geol
DE Roberts Mountains allochthon; Independence Mountains; Paleozoic;
structure; stratigraphy; biostratigraphy; Snow Canyon Formation; Vinini
Formation; Elder Sandstone; Slaven Chert; McAfee Quartzite; Vainly
Formation; Antler orogeny; Carlin-type gold deposits
ID WESTERN UNITED-STATES; GOLD DEPOSITS; CRUSTAL STRUCTURE; JERRITT CANYON;
GREAT-BASIN; RANGE; MARGIN; ROCKS; CONSTRAINTS; RADIOLARIAN
AB New biostratigraphic, stratigraphic, and structural data from deformed lower Paleozoic sedimentary units of the Roberts Mountains allochthon (RMA), Independence Mountains, Nevada, have enabled the identification of stratigraphic units within the allochthon that range in age from Late Cambrian through Late Devonian. The McAfee thrust fault emplaced a relatively thick (>200 m) sheet of Ordovician Valmy quartzite (locally termed the McAfee Quartzite) on complexly deformed units of the RMA (locally termed the Snow Canyon Formation) comprised of the Vinini Formation, Elder Sandstone, and Slaven Chert. The rocks were affected by multiple phases of deformation during and after the Devonian-Mississippian Antler orogeny, including: emplacement of the Roberts Mountains allochthon with south-vergent folding and faulting of the upper and lower plate rocks to the Roberts Mountains thrust; emplacement of Upper Mississippian (324 Ma) basalt dikes that cross-cut the upper (allochthonous) and lower (para-autochthonous) plate rocks and south-vergent folds; emplacement of the McAfee Quartzite; and upright north-trending folding after the deposition of Antler overlap rocks. Recognition of this history is required to determine the internal structure and thickness of the allochthon and location of high-angle structures within it that, respectively, may conceal and localize Carlin-type gold deposits in underlying carbonate rocks.
C1 [Holm-Denoma, Christopher S.; Hofstra, Albert H.] US Geol Survey, Denver, CO 80225 USA.
RP Holm-Denoma, CS (reprint author), US Geol Survey, Box 25046, Denver, CO 80225 USA.
EM cholm-denoma@usgs.gov
NR 67
TC 2
Z9 2
U1 1
U2 2
PU DESTECH PUBLICATIONS, INC
PI LANCASTER
PA 439 DUKE STREET, LANCASTER, PA 17602-4967 USA
BN 978-1-60595-040-2
PY 2011
BP 1039
EP 1054
PG 16
WC Geology; Metallurgy & Metallurgical Engineering
SC Geology; Metallurgy & Metallurgical Engineering
GA BWF52
UT WOS:000293810500056
ER
PT B
AU John, DA
Rockwell, BW
Henry, CD
Colgan, JP
AF John, David A.
Rockwell, Barnaby W.
Henry, Christopher D.
Colgan, Joseph P.
BE Steininger, R
Pennell, B
TI Hydrothermal alteration of the late Eocene Caetano ash-flow caldera,
north-central Nevada: A field and ASTER remote sensing study
SO GREAT BASIN EVOLUTION AND METALLOGENY, VOLS I AND II
LA English
DT Proceedings Paper
CT 6th Geological Society of Nevada on Great Basin Evolution and
Metallogeny
CY MAY 14-22, 2010
CL Nevada Bur Mines & Geol, Reno, NV
SP Soc Econom Geologists, Us Geolog Survey, Utah Geolog Assoc, Arizona Geolog Soc, Barrick Gold Exploration Inc, Haywood Securities, Newmont Mining Corp, Agnico Eagle US Ltd, Goldcorp, ALS Chemex, Boart Longyear, Evolving Gold Corp, Int Royal Corp, KinRoss Gold Corp, Nevada Div Minerals, Newcrest Mining Ltd, GIS Land Serv, Gold Fields Ltd, Hecla Mining Co, Kappes, Cassidy & Assoc, Floren Analyt Serv, Mine Dev Assoc, Allied Nevada Gold Corp, Amec, AuEx Inc, Centerra Gold, Geotemps Inc, Romarco Minerals US Inc, Nevada Mining Assoc, Carrington Consultants, Century Gold, Coeur, Drift Explorat Drilling Inc, Entree Gold Inc, Enviroscientists Inc, Fronteer Dev Inc, Fugro Airborne Surveys, Gold Summit Corp, Golden Predator Royal & Dev Corp, Jipangu Holdings Inc, Klondex Mines, Legend Inc, MGC Resources Inc, Miranda Gold Corp, Queensgate Resources Corp, Royal Gold Inc, Ruen Drilling Inc, Redstar Gold Corp, Rye Patch Gold Corp, Teck, Timberline Drilling, Timberline Resources Corp, US Gold Corp, Victoria Gold Corp, Western Energy Dev Corp, Western Lithium
HO Nevada Bur Mines & Geol
DE Caetano caldera; hydrothermal system; hydrothermal alteration; ASTER;
Carlin-type gold deposits
ID EXTENSION
AB Geologic mapping and analysis of ASTER remote sensing data were used to define the effects of a large hydrothermal system in the 12-18 by 22 km Caetano caldera. The caldera formed at similar to 33.8 Ma during eruption of >1100 km(3) of the rhyolitic Caetano Tuff that left a 1 km deep basin which was partly filled by a lake. Magma resurgence resulted in shallow (<1 km) emplacement of the Redrock Canyon granite porphyry intrusion into caldera fill in the southwestern part of the caldera. Field and petrographic studies indicate that heat from the pluton or from deeper residual Caetano magma caused a large hydrothermal system to form that altered both the pluton and intracaldera Caetano Tuff throughout the western half of the caldera. ASTER-based mineral mapping shows that the most intense alteration, including local alunite, developed primarily along the southwestern and western caldera margins. Alteration was most intense in the Redrock Canyon intrusion itself and in the upper unit of the Caetano Tuff, which is a sequence of thin ash flows interlayered with finely bedded sedimentary rocks and mesobreccia. Hydrothermally altered intracaldera tuff was domed and crosscut by the unaltered 33.78 +/- 0.05 Ma Carico Lake pluton, indicating that caldera formation, magma resurgence, pluton emplacement, and hydrothermal activity all occurred in less than about 100 ka.
Two major forms of hydrothermal alteration are present: (1) early pervasive pyrite-bearing intermediate argillic, advanced argillic, and residual quartz alteration, and (2) later cross-cutting, structurally controlled hematite +/- barite alteration. Three major assemblages are recognized in early alteration: areally widespread (1) advanced argillic and (2) intermediate argillic, and areally restricted (3) residual (vuggy) quartz. In residual quartz alteration, both plagioclase and sanidine phenocrysts were leached leaving prominent voids and the groundmass was replaced by fine-grained quartz and minor fine-grained pyrite. Residual quartz alteration transitions into advanced argillic alteration that mostly consists of a quartz-kaolinite-pyrite assemblage in which both plagioclase and sanidine phenocrysts were replaced by kaolinite. Alunite is present locally as replacement of feldspar phenocrysts and as breccia matrix, although ASTER data suggest that alunite is more abundant than was detected in hand samples. Advanced argillic alteration transitions into intermediate argillic alteration in which fine-grained kaolinite and (or) montmorillonite replaced plagioclase phenocrysts, whereas sanidine phenocrysts were not altered. Early pervasive alteration is cross cut by narrow (<= 2 cm wide), locally sheeted or stockwork specular hematite +/- barite veins and hydrothermal breccias that are widely distributed, especially in zones of advanced argillic alteration. Similar hematite-rich veins are present in Paleozoic rocks along the caldera margins near Horse Mountain and Stone Cabin Basin; these areas are recent exploration targets for Carlin-type gold deposits. Sedimentary beds in the upper unit of Caetano Tuff were locally silicified (+/- pyrite, barite) and scattered narrow quartz or chalcedony +/- pyrite veins are present, but no major zones of quartz-veined or silicified rocks were recognized. Coarse-grained barite filling narrow veins and voids and forming breccia matrix is common especially in the southern part of the caldera on both sides of Carico Lake Valley.
Chemical analyses of similar to 75 samples show (1) enrichment in Li, Sb, W, and Zn in early argillic and advanced argillic altered rocks relative to unaltered Caetano caldera rocks; (2) locally highly anomalous concentrations of As, Ba, Hg, Li, Mn, Mo, Pb, Sb, W, and Zn with scattered anomalous Au in hematite +/- barite veins and breccias; and (3) anomalous Hg, Mo, Sb, and W concentrations in narrow quartz/chalcedony veins. Gold and silver contents are generally below detection (<5 ppb and <1 ppm, respectively) with maximum values of 683 ppb Au and 3 ppm Ag.
Widespread advanced argillic alteration, such as in the Caetano caldera, is uncommon in ash-flow calderas. We attribute the abundance of advanced argillic alteration in the Caetano caldera to mixing of lake water with acid-generating gases released from crystallizing residual Caetano magma underlying the caldera. Upflow of hot magmatic gases into the lake produced a large convective hydrothermal system that mostly flowed through permeable, interbedded poorly welded tuff and sedimentary rocks of the upper unit of Caetano Tuff. Early acidic fluids that formed pyrite-bearing advanced argillic alteration assemblages represent relatively high fluxes of magmatic heat and gas. Decreased fluxes of magmatic gas and heat led to cooling and collapse of the hydrothermal system, downward flow of cool, oxidized fluids, and formation of widespread hematite +/- barite veins and breccias that crosscut the advanced argillic alteration.
Mineralogy, geochemistry, and paragenesis of the Caetano hydrothermal system are fundamentally different than Carlin-type hydrothermal systems making it unlikely Carlin-type disseminated gold mineralization exists in Paleozoic rocks along the south caldera wall.
C1 [John, David A.; Colgan, Joseph P.] US Geol Survey, Menlo Pk, CA 94025 USA.
RP John, DA (reprint author), US Geol Survey, MS-901,345 Middlefield Rd, Menlo Pk, CA 94025 USA.
EM djohn@usgs.gov
NR 21
TC 5
Z9 5
U1 0
U2 3
PU DESTECH PUBLICATIONS, INC
PI LANCASTER
PA 439 DUKE STREET, LANCASTER, PA 17602-4967 USA
BN 978-1-60595-040-2
PY 2011
BP 1055
EP 1083
PG 29
WC Geology; Metallurgy & Metallurgical Engineering
SC Geology; Metallurgy & Metallurgical Engineering
GA BWF52
UT WOS:000293810500057
ER
PT J
AU Singh, RK
Irmak, A
AF Singh, Ramesh K.
Irmak, Ayse
TI Treatment of anchor pixels in the METRIC model for improved estimation
of sensible and latent heat fluxes
SO HYDROLOGICAL SCIENCES JOURNAL-JOURNAL DES SCIENCES HYDROLOGIQUES
LA English
DT Article
DE energy balance; evapotranspiration; Landsat; Priestley-Taylor equation;
remote sensing; wMETRIC model
ID PRIESTLEY-TAYLOR PARAMETER; ENERGY-BALANCE; MAPPING EVAPOTRANSPIRATION;
SURFACE-TEMPERATURE; SEMIARID RANGELAND; EVAPORATION; VEGETATION; LAND;
EQUILIBRIUM; COEFFICIENT
AB Reliable estimation of sensible heat flux (H) is important in energy balance models for quantifying evapotranspiration (ET). This study was conducted to evaluate the value of adding the Priestley-Taylor (PT) equation to the METRIC (Mapping Evapotranspiration at high Resolution with Internalized Calibration) model. METRIC was used to estimate energy fluxes for 10 Landsat images from the 2005, 2006 and 2007 crop growing seasons in south-central Nebraska, USA, where each image owing to recent rainfall exhibited high residual moisture content even at the hot pixel. The METRIC model performed satisfactorily for net radiation (R-n) and soil heat flux (G) estimation with a root mean square error (RMSE) of 52 and 24 W m(-2), respectively. A RMSE of 122 W m(-2) for H indicated the limitation of the METRIC model in estimating H for high residual moisture content of the hot pixel (Alfalfa reference ET fraction, ETrT > 0.15). The modified METRIC model (wet METRIC or wMETRIC) incorporating the PT equation was applied to calculate H at the anchor pixels (hot and cold) for high residual moisture content of the hot pixel. The alpha coefficient of the PT equation was locally calibrated using hourly meteorological data from an automatic weather station and R-n and G data from a Bowen ratio flux tower. The mean alpha coefficient value was 1.14. The wMETRIC model reduced the RMSE of H from 122 to 64 W m(-2) and that of latent heat flux, LE, from 163 to 106 W m(-2). The RMSE of daily ET decreased from 1.7 to 1.1 mm d(-1) with wMETRIC. The results indicate that treatment of anchor pixels for high residual moisture content with the PT approach gives improved estimation of H, LE and daily ET. It is recommended that the wMETRIC model be used for estimating ET if the hot pixel has high residual moisture (i.e. reference ET fraction > 0.15).
C1 [Singh, Ramesh K.] US Geol Survey, ARTS Contractor, Earth Resources Observat & Sci EROS Ctr, Sioux Falls, SD 57198 USA.
[Irmak, Ayse] Univ Nebraska, Sch Nat Resources, Lincoln, NE 68583 USA.
RP Singh, RK (reprint author), US Geol Survey, ARTS Contractor, Earth Resources Observat & Sci EROS Ctr, Sioux Falls, SD 57198 USA.
EM rsingh@usgs.gov
OI Singh, Ramesh/0000-0002-8164-3483
NR 42
TC 15
Z9 15
U1 1
U2 11
PU TAYLOR & FRANCIS LTD
PI ABINGDON
PA 2-4 PARK SQUARE, MILTON PARK, ABINGDON OR14 4RN, OXON, ENGLAND
SN 0262-6667
EI 2150-3435
J9 HYDROLOG SCI J
JI Hydrol. Sci. J.-J. Sci. Hydrol.
PY 2011
VL 56
IS 5
BP 895
EP 906
DI 10.1080/02626667.2011.587424
PG 12
WC Water Resources
SC Water Resources
GA 817CS
UT WOS:000294649000012
ER
PT J
AU Chapman, EW
Hofmann, EE
Patterson, DL
Ribic, CA
Fraser, WR
AF Chapman, Erik W.
Hofmann, Eileen E.
Patterson, Donna L.
Ribic, Christine A.
Fraser, William R.
TI Marine and terrestrial factors affecting Adelie penguin Pygoscelis
adeliae chick growth and recruitment off the western Antarctic Peninsula
SO MARINE ECOLOGY PROGRESS SERIES
LA English
DT Article
DE Adelie penguin; Climate change; Chick growth; Antarctic Peninsula
ID KRILL EUPHAUSIA-SUPERBA; LAST 50 YEARS; PLEURAGRAMMA-ANTARCTICUM; ANIMAL
COATS; BREEDING SUCCESS; FORAGING EFFORT; DIFFERENT PREY;
CLIMATE-CHANGE; ICE CONDITIONS; HEAT-LOSS
AB An individual-based bioenergetics model that simulates the growth of an Adelie penguin Pygoscelis adeliae chick from hatching to fledging was used to assess marine and terrestrial factors that affect chick growth and fledging mass off the western Antarctic Peninsula. Simulations considered the effects on Adelie penguin fledging mass of (1) modification of chick diet through the addition of Antarctic silverfish Pleuragramma antarcticum to an all-Antarctic krill Euphausia superba diet, (2) reduction of provisioning rate which may occur as a result of an environmental stress such as reduced prey availability, and (3) increased thermoregulatory costs due to wetting of chicks which may result from increased precipitation or snow-melt in colonies. Addition of 17% Antarctic silverfish of Age-Class 3 yr (AC3) to a penguin chick diet composed of Antarctic krill increased chick fledging mass by 5%. Environmental stress that results in > 4% reduction in provisioning rate or wetting of just 10% of the chick's surface area decreased fledging mass enough to reduce the chick's probability of successful recruitment. The negative effects of reduced provisioning and wetting on chick growth can be compensated for by inclusion of Antarctic silverfish of AC3 and older in the chick diet. Results provide insight into climate-driven processes that influence chick growth and highlight a need for field research designed to investigate factors that determine the availability of AC3 and older Antarctic silverfish to foraging Adelie penguins and the influence of snowfall on chick wetting, thermoregulation and adult provisioning rate.
C1 [Chapman, Erik W.; Hofmann, Eileen E.] Old Dominion Univ, Ctr Coastal Phys Oceanog, Norfolk, VA 23529 USA.
[Patterson, Donna L.; Fraser, William R.] Polar Oceans Res Grp, Sheridan, MT 59749 USA.
[Ribic, Christine A.] Univ Wisconsin, US Geol Survey, Wisconsin Cooperat Wildlife Res Unit, Dept Forest & Wildlife Ecol, Madison, WI 53706 USA.
RP Chapman, EW (reprint author), Univ New Hampshire Cooperat Extens, 131 Main St, Durham, NH 03824 USA.
EM erik.chapman@unh.edu
FU National Science Foundation [ANT-0323254, OPP-9011927, OPP-9605596,
OPP-0130525, OPP-0217282, OPP-0224727, OPP-052361, ANT-0523254]
FX We thank B. Salihoglu for providing the original framework for the chick
growth model. We also thank the Palmer Station support staff for
facilitating our long-term data collection efforts. Furthermore, we are
grateful for the assistance provided by many field team members who have
helped with data collection over the years. We thank David Ainley and 4
anonymous reviewers for their comments which greatly improved the
present paper. This research was funded through National Science
Foundation Grants ANT-0323254, OPP-9011927, OPP-9605596, OPP-0130525,
OPP-0217282, OPP-0224727, and OPP-052361. The development of the penguin
chick growth model was supported by National Science Foundation Grant
ANT-0523254 and is part of the U.S. Southern Ocean Global Oceans
Ecosystem Dynamics synthesis and integration phase.
NR 69
TC 16
Z9 16
U1 2
U2 27
PU INTER-RESEARCH
PI OLDENDORF LUHE
PA NORDBUNTE 23, D-21385 OLDENDORF LUHE, GERMANY
SN 0171-8630
J9 MAR ECOL PROG SER
JI Mar. Ecol.-Prog. Ser.
PY 2011
VL 436
BP 273
EP 289
DI 10.3354/meps09242
PG 17
WC Ecology; Marine & Freshwater Biology; Oceanography
SC Environmental Sciences & Ecology; Marine & Freshwater Biology;
Oceanography
GA 816RM
UT WOS:000294619800020
ER
PT J
AU Mantilla, R
Gupta, VK
Troutman, BM
AF Mantilla, R.
Gupta, V. K.
Troutman, B. M.
TI Scaling of peak flows with constant flow velocity in random self-similar
networks
SO NONLINEAR PROCESSES IN GEOPHYSICS
LA English
DT Article
ID FRACTAL CHANNEL NETWORKS; SIMILAR RIVER NETWORKS; DISCHARGE POWER LAWS;
STREAM NUMBERS; RAINFALL; RUNOFF; VARIABILITY; FRAMEWORK; EXPONENTS;
MODEL
AB A methodology is presented to understand the role of the statistical self-similar topology of real river networks on scaling, or power law, in peak flows for rainfall-runoff events. We created Monte Carlo generated sets of ensembles of 1000 random self-similar networks (RSNs) with geometrically distributed interior and exterior generators having parameters pi and p(e), respectively. The parameter values were chosen to replicate the observed topology of real river networks. We calculated flow hydrographs in each of these networks by numerically solving the link-based mass and momentum conservation equation under the assumption of constant flow velocity. From these simulated RSNs and hydrographs, the scaling exponents beta and phi characterizing power laws with respect to drainage area, and corresponding to the width functions and flow hydrographs respectively, were estimated. We found that, in general, phi > beta, which supports a similar finding first reported for simulations in the river network of the Walnut Gulch basin, Arizona. Theoretical estimation of beta and phi in RSNs is a complex open problem. Therefore, using results for a simpler problem associated with the expected width function and expected hydrograph for an ensemble of RSNs, we give heuristic arguments for theoretical derivations of the scaling exponents beta(E) and phi(E) that depend on the Horton ratios for stream lengths and areas. These ratios in turn have a known dependence on the parameters of the geometric distributions of RSN generators. Good agreement was found between the analytically conjectured values of beta((E)) and phi((E)) and the values estimated by the simulated ensembles of RSNs and hydrographs. The independence of the scaling exponents phi((E)) and phi with respect to the value of flow velocity and runoff intensity implies an interesting connection between unit hydrograph theory and flow dynamics. Our results provide a reference framework to study scaling exponents under more complex scenarios of flow dynamics and runoff generation processes using ensembles of RSNs.
C1 [Mantilla, R.] Univ Iowa, IIHR Hydrosci & Engn, Iowa City, IA 52242 USA.
[Gupta, V. K.] Univ Colorado, Cooperat Inst Res Environm Sci, Dept Civil Environm & Architectural Engn, Boulder, CO 80309 USA.
[Troutman, B. M.] US Geol Survey, Denver Fed Ctr, Lakewood, CO 80225 USA.
RP Mantilla, R (reprint author), Univ Iowa, IIHR Hydrosci & Engn, Iowa City, IA 52242 USA.
EM ricardo-mantilla@uiowa.edu
RI Mantilla, Ricardo/B-9658-2008
OI Mantilla, Ricardo/0000-0002-2957-6252
FU National Science Foundation
FX This research was partially supported by grants from the National
Science Foundation to the University of Colorado and the University of
Iowa. This support is gratefully acknowledged. Our thanks to the
reviewers of this manuscript for providing insightful comments that
helped improve the presentation of the ideas. We also thank John Moody
and Lauren Hay of the USGS for helpful reviews, which improved the
manuscript.
NR 31
TC 6
Z9 6
U1 1
U2 5
PU COPERNICUS GESELLSCHAFT MBH
PI GOTTINGEN
PA BAHNHOFSALLEE 1E, GOTTINGEN, 37081, GERMANY
SN 1023-5809
J9 NONLINEAR PROC GEOPH
JI Nonlinear Process Geophys.
PY 2011
VL 18
IS 4
BP 489
EP 502
DI 10.5194/npg-18-489-2011
PG 14
WC Geochemistry & Geophysics; Meteorology & Atmospheric Sciences
SC Geochemistry & Geophysics; Meteorology & Atmospheric Sciences
GA 814GT
UT WOS:000294437200005
ER
PT B
AU Boore, DM
AF Boore, D. M.
BE Akkar, S
Gulkan, P
VanEck, T
TI Ground-Motion Prediction Equations (GMPEs) from a Global Dataset: The
PEER NGA Equations
SO EARTHQUAKE DATA IN ENGINEERING SEISMOLOGY: PREDICTIVE MODELS, DATA
MANAGEMENT AND NETWORKS
SE Geotechnical Geological and Earthquake Engineering
LA English
DT Article; Book Chapter
ID APPLICABILITY; PROJECT; REGION; MODELS
AB The PEER NGA ground-motion prediction equations (GMPEs) were derived by five developer teams over several years, resulting in five sets of GMPEs. The teams used various subsets of a global database of ground motions and metadata from shallow earthquakes in tectonically active regions in the development of the equations. Since their publication, the predicted motions from these GMPEs have been compared with data from various parts of the world data that largely were not used in the development of the GMPEs. The comparisons suggest that the NGA GMPEs are applicable globally for shallow earthquakes in tectonically active regions.
C1 US Geol Survey, Menlo Pk, CA 94025 USA.
RP Boore, DM (reprint author), US Geol Survey, MS977, Menlo Pk, CA 94025 USA.
EM boore@usgs.gov
NR 14
TC 2
Z9 2
U1 0
U2 1
PU SPRINGER
PI DORDRECHT
PA PO BOX 17, 3300 AA DORDRECHT, NETHERLANDS
BN 978-94-007-0151-9
J9 GEOTECH GEOL EARTHQ
PY 2011
VL 14
BP 3
EP 15
DI 10.1007/978-94-007-0152-6_1
D2 10.1007/978-94-007-0152-6
PG 13
WC Engineering, Civil; Engineering, Geological; Geosciences,
Multidisciplinary
SC Engineering; Geology
GA BTH81
UT WOS:000286948900001
ER
PT J
AU Witmer, GW
Fuller, PL
AF Witmer, Gary W.
Fuller, Pam L.
TI Vertebrate species introductions in the United States and its
territories
SO CURRENT ZOOLOGY
LA English
DT Article
DE Eradication; Introductions; Invasive species; Management; United States
ID ISLANDS; ERADICATION
AB At least 1,065 introduced vertebrate species have been introduced in the United States and its territories, including at least 86 mammalian, 127 avian, 179 reptilian/amphibian, and 673 fish species. Examples in each major taxonomic group include domestic cat, small Indian mongoose, red fox, goat, pig, rabbit, rats, house mouse, gray squirrel, nutria, starling, Indian common myna, red-vented bulbul, brown treesnake, red-eared slider, brown trout, tilapia, and grass carp. We briefly review some of these species and the types of damage they cause. We then review the basic types of methods used for control or eradication of each taxonomic group, including physical, chemical, biological, and cultural methods. We discuss some of the challenges in managing these species, including issues with the use of toxicants, land access, public attitudes, and monitoring difficulties. Finally, we list some ongoing research and future research needs, including improved detection methods, improved attractants, improved barriers, improved capture methods, fertility control, and risk assessment methods [Current Zoology 57 (5): 559-567, 2011].
C1 [Witmer, Gary W.] USDA, APHIS, WS Natl Wildlife Res Ctr, Ft Collins, CO 80521 USA.
[Fuller, Pam L.] USGS, BRD, SE Ecol Sci Ctr, Gainesville, FL 32653 USA.
RP Witmer, GW (reprint author), USDA, APHIS, WS Natl Wildlife Res Ctr, 4101 Laporte Ave, Ft Collins, CO 80521 USA.
EM gary.w.witmer@aphis.usda.gov
NR 52
TC 3
Z9 4
U1 4
U2 43
PU CURRENT ZOOLOGY
PI BEIJING
PA CHINESE ACAD SCIENCES, INST ZOOLOGY, BEICHEN XILU, CHAOYANG DISTRICT,
BEIJING, 100101, PEOPLES R CHINA
SN 1674-5507
J9 CURR ZOOL
JI Curr. Zool.
PY 2011
VL 57
IS 5
BP 559
EP 567
PG 9
WC Zoology
SC Zoology
GA 800EX
UT WOS:000293343700002
ER
PT J
AU Stohlgren, TJ
Jarnevich, CS
Esaias, WE
Morisette, JT
AF Stohlgren, Thomas J.
Jarnevich, Catherine S.
Esaias, Wayne E.
Morisette, Jeffrey T.
TI Bounding species distribution models
SO CURRENT ZOOLOGY
LA English
DT Article
DE Niche models; Geographic information systems; Extrapolation; Clamping
ID GEOGRAPHIC DISTRIBUTIONS; PREDICTION
AB Species distribution models are increasing in popularity for mapping suitable habitat for species of management concern. Many investigators now recognize that extrapolations of these models with geographic information systems (GIS) might be sensitive to the environmental bounds of the data used in their development, yet there is no recommended best practice for "clamping" model extrapolations. We relied on two commonly used modeling approaches: classification and regression tree (CART) and maximum entropy (Maxent) models, and we tested a simple alteration of the model extrapolations, bounding extrapolations to the maximum and minimum values of primary environmental predictors, to provide a more realistic map of suitable habitat of hybridized Africanized honey bees in the southwestern United States. Findings suggest that multiple models of bounding, and the most conservative bounding of species distribution models, like those presented here, should probably replace the unbounded or loosely bounded techniques currently used [Current Zoology 57 (5): 642-647, 2011].
C1 [Stohlgren, Thomas J.; Jarnevich, Catherine S.; Morisette, Jeffrey T.] US Geol Survey, Ft Collins Sci Ctr, Ft Collins, CO 80526 USA.
[Esaias, Wayne E.] NASA, Goddard Space Flight Ctr, Code 614 5, Greenbelt, MD 20771 USA.
RP Stohlgren, TJ (reprint author), US Geol Survey, Ft Collins Sci Ctr, 2150 Ctr Ave, Ft Collins, CO 80526 USA.
EM stohlgrent@USGS.gov
FU Natural Resource Ecology Laboratory at Colorado State University; U.S.
Geological Survey Invasive Species Program; USGS; USDA [CSREES/NRI
2008-35615-04666]; [NoNNH08AI02I]
FX We thank NASA grant NoNNH08AI02I for funding, and the Natural Resource
Ecology Laboratory at Colorado State University, and USGS Fort Collins
Science Center for logistical support. We thank Pete Ma and Elizabeth
Sellers for helpful review comments on an earlier draft. Any use of
trade, product, or firm names is for descriptive purposes only and does
not imply endorsement by the US Government. TJS contribution supported
by U.S. Geological Survey Invasive Species Program, USGS Fort Collins
Science Program, and USDA CSREES/NRI 2008-35615-04666.
NR 20
TC 9
Z9 9
U1 0
U2 10
PU CURRENT ZOOLOGY
PI BEIJING
PA CHINESE ACAD SCIENCES, INST ZOOLOGY, BEICHEN XILU, CHAOYANG DISTRICT,
BEIJING, 100101, PEOPLES R CHINA
SN 1674-5507
J9 CURR ZOOL
JI Curr. Zool.
PY 2011
VL 57
IS 5
BP 642
EP 647
PG 6
WC Zoology
SC Zoology
GA 800EX
UT WOS:000293343700009
ER
PT J
AU Gumma, MK
Thenkabail, PS
Muralikrishna, IV
Velpuri, MN
Gangadhararao, PT
Dheeravath, V
Biradar, CM
Nalan, SA
Gaur, A
AF Gumma, Murali Krishna
Thenkabail, Prasad S.
Muralikrishna, I. V.
Velpuri, Manohar N.
Gangadhararao, Parthasarathi T.
Dheeravath, Venkateswarlu
Biradar, Chandrasekhar M.
Nalan, Sreedhar Acharya
Gaur, Anju
TI Changes in agricultural cropland areas between a water-surplus year and
a water-deficit year impacting food security, determined using MODIS 250
m time-series data and spectral matching techniques, in the Krishna
River basin (India)
SO INTERNATIONAL JOURNAL OF REMOTE SENSING
LA English
DT Article
ID USE/LAND-COVER LULC; AVHRR DATA; LAND; CLASSIFICATION; IMAGERY;
VEGETATION; NDVI
AB The objective of this study was to investigate the changes in cropland areas as a result of water availability using Moderate Resolution Imaging Spectroradiometer (MODIS) 250 m time-series data and spectral matching techniques (SMTs). The study was conducted in the Krishna River basin in India, a very large river basin with an area of 265 752 km 2 (26 575 200 ha), comparing a water-surplus year (2000-2001) and a water-deficit year (2002-2003). The MODIS 250 m time-series data and SMTs were found ideal for agricultural cropland change detection over large areas and provided fuzzy classification accuracies of 61-100% for various land-use classes and 61-81% for the rain-fed and irrigated classes. The most mixing change occurred between rain-fed cropland areas and informally irrigated (e. g. groundwater and small reservoir) areas. Hence separation of these two classes was the most difficult. The MODIS 250 m-derived irrigated cropland areas for the districts were highly correlated with the Indian Bureau of Statistics data, with R-2-values between 0.82 and 0.86.
The change in the net area irrigated was modest, with an irrigated area of 8 669 881 ha during the water-surplus year, as compared with 7 718 900 ha during the water-deficit year. However, this is quite misleading as most of the major changes occurred in cropping intensity, such as changing from higher intensity to lower intensity (e.g. from double crop to single crop). The changes in cropping intensity of the agricultural cropland areas that took place in the water-deficit year (2002-2003) when compared with the water-surplus year (2000-2001) in the Krishna basin were: (a) 1 078 564 ha changed from double crop to single crop, (b) 1 461 177 ha changed from continuous crop to single crop, (c) 704 172 ha changed from irrigated single crop to fallow and (d) 1 314 522 ha changed from minor irrigation (e.g. tanks, small reservoirs) to rain-fed. These are highly significant changes that will have strong impact on food security. Such changes may be expected all over the world in a changing climate.
C1 [Gumma, Murali Krishna] Int Rice Res Inst, Los Banos, Philippines.
[Thenkabail, Prasad S.] US Geol Survey, SW Geog Sci Ctr, Flagstaff, AZ 86001 USA.
[Muralikrishna, I. V.] Asian Inst Technol, Bangkok 10501, Thailand.
[Velpuri, Manohar N.] S Dakota State Univ, Geog Informat Sci Ctr Excellence, Brookings, SD 57007 USA.
[Gangadhararao, Parthasarathi T.; Nalan, Sreedhar Acharya] Int Crops Res Inst Semi Arid Trop, Int Water Management Inst, Hyderabad, Andhra Pradesh, India.
[Dheeravath, Venkateswarlu] United Nations Joint Logist Ctr, Juba, Sudan.
[Biradar, Chandrasekhar M.] Univ Oklahoma, Dept Bot & Microbiol, Norman, OK 73019 USA.
[Gaur, Anju] World Bank, New Delhi, India.
RP Gumma, MK (reprint author), Int Rice Res Inst, Los Banos, Philippines.
EM m.gumma@cgiar.org
RI Velpuri, Naga Manohar/A-5193-2013
OI Velpuri, Naga Manohar/0000-0002-6370-1926
NR 33
TC 16
Z9 16
U1 0
U2 19
PU TAYLOR & FRANCIS LTD
PI ABINGDON
PA 4 PARK SQUARE, MILTON PARK, ABINGDON OX14 4RN, OXON, ENGLAND
SN 0143-1161
J9 INT J REMOTE SENS
JI Int. J. Remote Sens.
PY 2011
VL 32
IS 12
BP 3495
EP 3520
DI 10.1080/01431161003749485
PG 26
WC Remote Sensing; Imaging Science & Photographic Technology
SC Remote Sensing; Imaging Science & Photographic Technology
GA 798QK
UT WOS:000293226100014
ER
PT J
AU Ruleman, CA
AF Ruleman, C. A.
TI Neotectonic inversion of the Hindu Kush-Pamir Mountain Region
SO HIMALAYAN GEOLOGY
LA English
DT Article
DE Hindu Kush; Pamir Mountains; Neotectonics; Afghanistan; Pakistan;
Himalaya; active tectonics
ID CRUSTAL DEFORMATION; PLATE
AB The Hindu Kush-Pamir region of southern Asia is one of Earth's most rapidly deforming regions and it is poorly understood. This study develops a kinematic model based on active faulting in this part of the Trans-Himalayan orogenic belt. Previous studies have described north-verging thrust faults and some strike-slip faults, reflected in the northward-convex geomorphologic and structural grain of the Pamir Mountains. However, this structural analysis suggests that contemporary tectonics are changing the style of deformation from north-verging thrusts formed during the initial contraction of the Himalayan orogeny to south-verging thrusts and a series of northwest-trending, dextral strike-slip faults in the modern transpressional regime. These northwest-trending fault zones are linked to the major right-lateral Karakoram fault, located to the east, as synthetic, conjugate shears that form a right-stepping en echelon pattern. Northwest-trending lineaments with dextral displacements extend continuously westward across the Hindu Kush-Pamir region indicating a pattern of systematic shearing of multiple blocks to the northwest as the deformation effects from Indian plate collision expands to the north-northwest. Locally, east-northeast- and northwest-trending faults display sinistral and dextral displacement, respectively, yielding conjugate shear pairs developed in a northwest-southeast compressional stress field. Geodetic measurements and focal mechanisms from historical seismicity support these surficial, tectono-morphic observations. The conjugate shear pairs may be structurally linked subsidiary faults and co-seismically slip during single large magnitude (> M7) earthquakes that occur on major south-verging thrust faults. This kinematic model provides a potential context for prehistoric, historic, and future patterns of faulting and earthquakes.
C1 US Geol Survey, Denver Fed Ctr, Denver, CO 80225 USA.
RP Ruleman, CA (reprint author), US Geol Survey, Denver Fed Ctr, POB 25046,MS 980, Denver, CO 80225 USA.
EM cruleman@usgs.gov
FU United States Agency for International Development; United States
Geological Survey (U.S.G.S.)
FX This work was funded in part by the United States Agency for
International Development and the United States Geological Survey
(U.S.G.S.). I thank my colleagues Michael Machette, Tony Crone, and
Kathy Haller (U.S.G.S.) for their accompanying mapping and insightful
collaboration. Ken Rukstales (U.S.G.S.) provided necessary GIS support
to create the database from which the kinematic model was derived.
NR 25
TC 0
Z9 0
U1 0
U2 5
PU WADIA INST HIMALAYAN GEOLOGY
PI DEHRA DUN
PA 33 GENERAL MAHADEO SINGH RD, DEHRA DUN, 248 001, INDIA
SN 0971-8966
J9 HIMAL GEOL
JI Himal. Geol.
PY 2011
VL 32
IS 2
BP 95
EP 111
PG 17
WC Geology
SC Geology
GA 792ZD
UT WOS:000292788000001
ER
PT B
AU Watanabe, H
Bailey, B
Duda, K
Kannari, Y
Miura, A
Ramachandran, B
AF Watanabe, Hiroshi
Bailey, Bryan
Duda, Kenneth
Kannari, Yoshiaki
Miura, Akira
Ramachandran, Bhaskar
BE Ramachandran, B
Justice, CO
Abrams, MJ
TI The ASTER Data System: An Overview of the Data Products in Japan and in
the United States
SO LAND REMOTE SENSING AND GLOBAL ENVIRONMENTAL CHANGE: NASA'S EARTH
OBSERVING SYSTEM AND THE SCIENCE OF ASTER AND MODIS
SE Remote Sensing and Digital Image Processing
LA English
DT Article; Book Chapter
ID PERFORMANCE
AB The Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) data system is a cooperative system, which is operated jointly by Japan's Ministry of Economy, Trade, and Industry (METI) through its Earth Remote Sensing Data Analysis Center (ERSDAC), and by the National Aeronautics and Space Administration (NASA) primarily through its Goddard Space Flight Center (GSFC) and Land Processes (LP) Distributed Active Archive Center (DAAC). ASTER is a moderate-resolution land remote sensing system onboard the Earth Observing System (EOS) Terra spacecraft. ASTER-acquired data are received at the White Sands, New Mexico, ground receiving station, and then transmitted via land network to the EOS Data and Operations System (EDOS) within the Goddard DAAC, located at the GSFC. EDOS pre-processes raw ASTER data to Level-0 (L0) data, and sends them via the high-speed Asia-Pacific Advanced Network (APAN) to the ASTER Ground Data System (GDS) in Japan. ASTER GDS processes the L0 data to level-1 (L1) datasets; they distribute these data to users, and also use them to generate higher-level products for their user community. ASTER GDS sends a copy of all L1A data they produce to NASA's LP DAAC, located at the U.S. Geological Survey's Center for Earth Resources Observation and Science (EROS) near Sioux Falls, South Dakota. All L1 data received from Japan are ingested, archived, and available for users at LP DAAC. The LP DAAC also generates and distributes higher-level products from L1 data based on requests from users. To meet time-critical needs related to sensor health and performance, natural disasters, national emergencies, and certain field campaigns, the ASTER Expedited Data System (EDS) was developed, and is operated jointly by U.S. and Japanese partners.
C1 [Watanabe, Hiroshi] Natl Inst Environm Studies, Tsukuba, Ibaraki 3058506, Japan.
[Duda, Kenneth; Ramachandran, Bhaskar] USGS Ctr Earth Resources Observat & Sci, NASA LP DAAC, Sioux Falls, SD 57198 USA.
[Kannari, Yoshiaki; Miura, Akira] Earth Remote Sensing Data Anal Ctr, Chuo Ku, Tokyo 1040054, Japan.
RP Watanabe, H (reprint author), Natl Inst Environm Studies, 16-2 Onogawa, Tsukuba, Ibaraki 3058506, Japan.
EM watanabe.hiroshi@nies.go.jp
NR 8
TC 2
Z9 2
U1 0
U2 3
PU SPRINGER
PI DORDRECHT
PA PO BOX 17, 3300 AA DORDRECHT, NETHERLANDS
BN 978-1-4419-6748-0
J9 REMOTE SENS DIGIT IM
PY 2011
VL 11
BP 233
EP 244
DI 10.1007/978-1-4419-6749-7_11
D2 10.1007/978-1-4419-6749-7
PG 12
WC Astronomy & Astrophysics; Geochemistry & Geophysics; Geosciences,
Multidisciplinary; Remote Sensing; Imaging Science & Photographic
Technology
SC Astronomy & Astrophysics; Geochemistry & Geophysics; Geology; Remote
Sensing; Imaging Science & Photographic Technology
GA BSG06
UT WOS:000284351600011
ER
PT B
AU Townshend, J
Latham, J
Justice, CO
Janetos, A
Conant, R
Arino, O
Balstad, R
Belward, A
Feuquay, J
Liu, JY
Ojima, D
Schmullius, C
Singh, A
Tschirley, J
AF Townshend, John
Latham, John
Justice, Christopher O.
Janetos, Anthony
Conant, Richard
Arino, Olivier
Balstad, Roberta
Belward, Alan
Feuquay, Jay
Liu, Jiyuan
Ojima, Dennis
Schmullius, Christiana
Singh, Ashbindu
Tschirley, Jeff
BE Ramachandran, B
Justice, CO
Abrams, MJ
TI International Coordination of Satellite Land Observations: Integrated
Observations of the Land
SO LAND REMOTE SENSING AND GLOBAL ENVIRONMENTAL CHANGE: NASA'S EARTH
OBSERVING SYSTEM AND THE SCIENCE OF ASTER AND MODIS
SE Remote Sensing and Digital Image Processing
LA English
DT Article; Book Chapter
ID MODIS; DATABASE
C1 [Townshend, John; Justice, Christopher O.] Univ Maryland, Dept Geog, College Pk, MD 20742 USA.
[Balstad, Roberta] Columbia Univ, CIESIN, Earth Inst, Palisades, NY 10964 USA.
[Belward, Alan] Joint Res Ctr, Inst Environm & Sustainabil, I-21027 Ispra, VA, Italy.
[Conant, Richard] Colorado State Univ, Nat Resource Ecol Lab, Ft Collins, CO 80523 USA.
[Feuquay, Jay] US Geol Survey, Reston, VA 22092 USA.
[Janetos, Anthony] Joint Global Change Res Inst, Univ Res Court 5825, College Pk, MD 20740 USA.
[Latham, John] Environm & Nat Resources Serv SDRN, Food & Agr Org United Nations FAO, I-00153 Rome, Italy.
[Liu, Jiyuan] Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, Beijing 100101, Peoples R China.
[Ojima, Dennis] H John Heinz III Ctr Sci Econ & Environm, Washington, DC 20006 USA.
[Schmullius, Christiana] Univ Jena, Inst Geog, Abt Fernerkundung, D-07743 Jena, Germany.
[Singh, Ashbindu] United Nations Environm Programme UNEP, Div Early Warning & Assessment N Amer, Washington, DC 20006 USA.
[Tschirley, Jeff] Environm & Nat Resources Serv SDRN, Food & Agr Org United Nations, I-00153 Rome, Italy.
RP Townshend, J (reprint author), Univ Maryland, Dept Geog, College Pk, MD 20742 USA.
EM jtownshend@bsos.umd.edu
NR 53
TC 6
Z9 6
U1 0
U2 1
PU SPRINGER
PI DORDRECHT
PA PO BOX 17, 3300 AA DORDRECHT, NETHERLANDS
BN 978-1-4419-6748-0
J9 REMOTE SENS DIGIT IM
PY 2011
VL 11
BP 835
EP 856
DI 10.1007/978-1-4419-6749-7_36
D2 10.1007/978-1-4419-6749-7
PG 22
WC Astronomy & Astrophysics; Geochemistry & Geophysics; Geosciences,
Multidisciplinary; Remote Sensing; Imaging Science & Photographic
Technology
SC Astronomy & Astrophysics; Geochemistry & Geophysics; Geology; Remote
Sensing; Imaging Science & Photographic Technology
GA BSG06
UT WOS:000284351600036
ER
PT J
AU Adams, AAY
Stanford, JW
Wiewel, AS
Rodda, GH
AF Adams, Amy A. Yackel
Stanford, James W.
Wiewel, Andrew S.
Rodda, Gordon H.
TI Modelling detectability of kiore (Rattus exulans) on Aguiguan, Mariana
Islands, to inform possible eradication and monitoring efforts
SO NEW ZEALAND JOURNAL OF ECOLOGY
LA English
DT Article
DE absolute density; capture probability; detection probability;
mark-recapture; neophobia
ID CAPTURE EXPERIMENTS; POPULATION ECOLOGY; NORVEGICUS; WILDLIFE; BEHAVIOR;
MAMMALS
AB Estimating the detection probability of introduced organisms during the pre-monitoring phase of an eradication effort can be extremely helpful in informing eradication and post-eradication monitoring efforts, but this step is rarely taken. We used data collected during 11 nights of mark-recapture sampling on Aguiguan, Mariana Islands, to estimate introduced kiore (Rattus exulans Peale) density and detection probability, and evaluated factors affecting detectability to help inform possible eradication efforts. Modelling of 62 captures of 48 individuals resulted in a model-averaged density estimate of 55 kiore/ha. Kiore detection probability was best explained by a model allowing neophobia to diminish linearly (i.e. capture probability increased linearly) until occasion 7, with additive effects of sex and cumulative rainfall over the prior 48 hours. Detection probability increased with increasing rainfall and females ware up to three times more likely than males to be trapped. In this paper, we illustrate the type of information that can be obtained by modelling mark-recapture data collected during pre-eradication monitoring and discuss the potential of using these data to inform eradication and post-eradication monitoring efforts.
C1 [Adams, Amy A. Yackel] Ft Collins Sci Ctr, ASRC Management Serv, Ft Collins, CO 80526 USA.
[Stanford, James W.] USGS Brown Treesnake Lab, Dededo, GU 96912 USA.
[Rodda, Gordon H.] USGS Ft Collins Sci Ctr, Ft Collins, CO 80526 USA.
RP Adams, AAY (reprint author), Ft Collins Sci Ctr, ASRC Management Serv, 2150 Ctr Ave,Bldg C, Ft Collins, CO 80526 USA.
EM yackela@usgs.gov
FU U.S. Fish and Wildlife Service
FX The rather difficult challenge of getting safely to Aguiguan was a
bureaucratic and logistic burden of the first magnitude, ably carried
out on our behalf by Earl Campbell, Karl Buermeyer, Curt Kessler, Nate
Hawley, Elvin Masga, Ton Castro, Peter Dunlevy, and especially Jess
Omar. We are extremely grateful to all. Nate Hawley assisted with
permitting. Field work assistance was provided by Allen Hambrick.
Funding was provided by the U.S. Navy (Scott Vogt) through the U.S. Fish
and Wildlife Service (Earl Campbell). Lea' Bonewell assisted with
stateside logistics. Thomas Stanley and Shane Siers provided helpful
reviews of earlier drafts. Michael Fall provided valuable insight into
our understanding of the population dynamics of rats. Any use of trade,
product, or firm names is for descriptive purposes only and does not
imply endorsement by the U.S. Government.
NR 45
TC 1
Z9 1
U1 1
U2 10
PU NEW ZEALAND ECOL SOC
PI CHRISTCHURCH
PA PO BOX 25178, CHRISTCHURCH, NEW ZEALAND
SN 0110-6465
J9 NEW ZEAL J ECOL
JI N. Z. J. Ecol.
PY 2011
VL 35
IS 2
SI SI
BP 145
EP 152
PG 8
WC Ecology
SC Environmental Sciences & Ecology
GA 787WB
UT WOS:000292406300003
ER
PT J
AU Savidge, JA
Stanford, JW
Reed, RN
Haddock, GR
Adams, AAY
AF Savidge, Julie A.
Stanford, James W.
Reed, Robert N.
Haddock, Ginger R.
Adams, Amy A. Yackel
TI Canine detection of free-ranging brown treesnakes on Guam
SO NEW ZEALAND JOURNAL OF ECOLOGY
LA English
DT Article
DE Boiga irregularis; brown treesnake; canine detection; detector dogs;
invasive species
ID SCAT DETECTION DOGS; GOPHERUS-AGASSIZII; ISLAND; MANAGEMENT; ABILITY;
SNAKES; ODOR
AB We investigated canine teams (dogs and their handlers) on Guam as a potential tool for finding invasive brown treesnakes (Boiga irregularis) in the wild. Canine teams searched a 40 x 40 m forested area for a snake that had consumed a dead mouse containing a radio-transmitter. To avoid tainting the target or target area with human scent, no snake was handled or closely approached prior to searches. Trials were conducted during the morning when these nocturnal snakes were usually hidden in refugia. A radiotracker knew the snake's location, but dog handlers and search navigators did not. Of 85 trials conducted over four months, the two canine teams had an average success rate of 35% of correctly defining an area <= 5 x 5 m that contained the transmittered snake; the team with more experience prior to the trials had a success rate of 44% compared with 26% for the less experienced team. Canine teams also found 11 shed skins from wild snakes. Although dogs alerted outside the vicinity of transmittered snakes, only one wild, non-transmittered snake was found during the trials, possibly reflecting the difficulty humans have in locating non-transmittered brown treesnakes in refugia. We evaluated success at finding snakes as a function of canine team, number of prior trials (i.e. experience gained during the trials), recent canine success at finding a target snake, various environmental conditions, snake perch height, and snake characteristics (snout-vent length and sex). Success rate increased over the course of the trials. Canine team success also increased with increasing average humidity and decreased with increasing average wind speed. Our results suggest dogs could be useful at detecting brown treesnakes in refugia, particularly when compared to daytime visual searches by humans, but techniques are needed to help humans find and extract snakes once a dog has alerted.
C1 [Savidge, Julie A.] Colorado State Univ, Dept Fish Wildlife & Conservat Biol, Ft Collins, CO 80523 USA.
[Stanford, James W.; Reed, Robert N.] US Geol Survey, Ft Collins Sci Ctr, Ft Collins, CO 80526 USA.
[Haddock, Ginger R.; Adams, Amy A. Yackel] Ft Collins Sci Ctr, ASRC Management Serv, Ft Collins, CO 80526 USA.
RP Savidge, JA (reprint author), Colorado State Univ, Dept Fish Wildlife & Conservat Biol, Ft Collins, CO 80523 USA.
EM jsavidge@cnr.colostate.edu
FU US Office of Insular Affairs; USGS
FX We sincerely thank Rebecca Stafford for handling dog Sam and Aimee Hurt
and Megan Parker (Working Dogs for Conservation) and Marielle Schmitz
(Dog Werks) for training both dog teams and offering suggestions
throughout the research. Brett Silk of the Dog Training Squad provided
additional obedience training. Other professional dog trainers and
handlers from various organizations and agencies provided helpful
insight and comments during the course of this research including but
not limited to staff from USDA Wildlife Services, Hawaii Department of
Agriculture, US Department of Defense, and the Division of Fish and
Wildlife Northern Marianas Islands. Gordon Rodda provided valuable input
at various stages of our research and helpful suggestions on the
manuscript. Many people were instrumental in project management or field
assistance, and we particularly thank Lea' Bonewell, Michelle Christy,
Jason Hackman, Allen Hambrick, Tom Hinkle, Bjorn Lardner, Pete Reynolds,
Dan Scott, Shane Siers, Arron Tuggle, and Kristin Winford. We also thank
Erin Muths, Christina Romagosa, James Russell and an anonymous reviewer
for comments on the manuscript and Thomas Stanley for statistical
assistance. We are grateful to the private citizens that allowed access
to their land and to the US Office of Insular Affairs and USGS Invasive
Species Program for funding. Any use of trade, product or firm names is
for descriptive purposes only and does not imply endorsement by the US
Government. Research was conducted under Colorado State University ACUC
protocol no. 06-212A-01.
NR 38
TC 6
Z9 7
U1 5
U2 32
PU NEW ZEALAND ECOL SOC
PI CHRISTCHURCH
PA PO BOX 25178, CHRISTCHURCH, NEW ZEALAND
SN 0110-6465
EI 1177-7788
J9 NEW ZEAL J ECOL
JI N. Z. J. Ecol.
PY 2011
VL 35
IS 2
SI SI
BP 174
EP 181
PG 8
WC Ecology
SC Environmental Sciences & Ecology
GA 787WB
UT WOS:000292406300006
ER
PT B
AU Weil, E
Rogers, CS
AF Weil, Ernesto
Rogers, Caroline S.
BE Dubinsky, Z
Stambler, N
TI Coral Reef Diseases in the Atlantic-Caribbean
SO CORAL REEFS: AN ECOSYSTEM IN TRANSITION
LA English
DT Article; Book Chapter
ID BLACK-BAND DISEASE; US VIRGIN-ISLANDS; GREAT-BARRIER-REEF; INDO-PACIFIC
REEFS; DARK SPOTS DISEASE; LONG-TERM DECLINE; SANTA-MARTA AREA; PLAGUE
TYPE-II; MASS MORTALITY; DIADEMA-ANTILLARUM
C1 [Weil, Ernesto] Univ Puerto Rico, Dept Marine Sci, Mayaguez, PR 00680 USA.
[Rogers, Caroline S.] USGS Caribbean Field Stn, St John, VI 00830 USA.
RP Weil, E (reprint author), Univ Puerto Rico, Dept Marine Sci, POB 9000, Mayaguez, PR 00680 USA.
EM eweil@caribe.net
NR 206
TC 40
Z9 42
U1 0
U2 13
PU SPRINGER
PI DORDRECHT
PA PO BOX 17, 3300 AA DORDRECHT, NETHERLANDS
BN 978-94-007-0113-7
PY 2011
BP 465
EP 491
DI 10.1007/978-94-007-0114-4_27
D2 10.1007/978-94-007-0114-4
PG 27
WC Biodiversity Conservation; Marine & Freshwater Biology
SC Biodiversity & Conservation; Marine & Freshwater Biology
GA BSW81
UT WOS:000285982500027
ER
PT B
AU Hayes, DJ
McGuire, AD
Kicklighter, DW
Burnside, TJ
Melillo, JM
AF Hayes, Daniel J.
McGuire, A. David
Kicklighter, David W.
Burnside, Todd J.
Melillo, Jerry M.
BE Gutman, G
Reissel, A
TI The Effects of Land Cover and Land Use Change on the Contemporary Carbon
Balance of the Arctic and Boreal Terrestrial Ecosystems of Northern
Eurasia
SO EURASIAN ARCTIC LAND COVER AND LAND USE IN A CHANGING CLIMATE
LA English
DT Article; Book Chapter
ID NET PRIMARY PRODUCTION; SOIL THERMAL DYNAMICS; CLIMATE-CHANGE;
ATMOSPHERIC TRANSPORT; EQUILIBRIUM RESPONSES; NITROGEN INTERACTIONS;
AMAZONIAN ECOSYSTEMS; TUNDRA ECOSYSTEMS; PROJECTED CLIMATE;
UNITED-STATES
AB Recent changes in climate, disturbance regimes and land use and management systems in Northern Eurasia have the potential to disrupt the terrestrial sink of atmospheric CO2 in a way that accelerates global climate change. To determine the recent trends in the carbon balance of the arctic and boreal ecosystems of this region, we performed a retrospective analysis of terrestrial carbon dynamics across northern Eurasia over a recent 10-year period using a terrestrial biogeochemical process model. The results of the simulations suggest a shift in direction of the net flux from the terrestrial sink of earlier decades to a net source on the order of 45 Tg C year(-1) between 1997 and 2006. The simulation framework and subsequent analyses presented in this study attribute this shift to a large loss of carbon from boreal forest ecosystems, which experienced a trend of decreasing precipitation and a large area burned during this time period.
C1 [Hayes, Daniel J.; Burnside, Todd J.] Univ Alaska Fairbanks, Inst Arctic Biol, Fairbanks, AK 99775 USA.
[McGuire, A. David] Univ Alaska Fairbanks, US Geol Survey, Alaska Cooperat Fish & Wildlife Res Unit, Fairbanks, AK 99775 USA.
[Kicklighter, David W.; Melillo, Jerry M.] Marine Biol Lab, Ctr Ecosyst, Woods Hole, MA 02543 USA.
RP Hayes, DJ (reprint author), Univ Alaska Fairbanks, Inst Arctic Biol, Fairbanks, AK 99775 USA.
EM Daniel.Hayes@alaska.edu; admcguire@alaska.edu; dkicklighter@mbl.edu;
canoebum@gmail.com; jmelillo@mbl.edu
NR 86
TC 3
Z9 3
U1 1
U2 6
PU SPRINGER
PI NEW YORK
PA 233 SPRING STREET, NEW YORK, NY 10013, UNITED STATES
BN 978-90-481-9117-8
PY 2011
BP 109
EP 136
DI 10.1007/978-90-481-9118-5_6
D2 10.1007/978-90-481-9118-5
PG 28
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA BSD75
UT WOS:000284236100006
ER
PT B
AU Byappanahalli, MN
Ishii, S
AF Byappanahalli, Muruleedhara N.
Ishii, Satoshi
BE Sadowsky, MJ
Whitman, RL
TI ENVIRONMENTAL SOURCES OF FECAL BACTERIA
SO FECAL BACTERIA
LA English
DT Article; Book Chapter
ID RECREATIONAL WATER-QUALITY; ESCHERICHIA-COLI O157-H7; SOUTHERN
LAKE-MICHIGAN; TROPICAL RAIN-FOREST; RNA GENETIC-MARKERS; LONG-TERM
SURVIVAL; INDICATOR BACTERIA; FRESH-WATER; NEARSHORE WATER;
SOURCE-TRACKING
C1 [Byappanahalli, Muruleedhara N.] US Geol Survey, Great Lakes Sci Ctr, Lake Michigan Ecol Res Stn, Porter, IN 46304 USA.
[Ishii, Satoshi] Univ Tokyo, Grad Sch Agr & Life Sci, Dept Appl Biol Chem, Tokyo 1138657, Japan.
RP Byappanahalli, MN (reprint author), US Geol Survey, Great Lakes Sci Ctr, Lake Michigan Ecol Res Stn, Porter, IN 46304 USA.
RI Sadowsky, Michael/J-2507-2016
OI Sadowsky, Michael/0000-0001-8779-2781
NR 142
TC 5
Z9 5
U1 0
U2 5
PU AMER SOC MICROBIOLOGY
PI WASHINGTON
PA 1752 N STREET NW, WASHINGTON, DC 20036-2904 USA
BN 978-1-55581-608-7
PY 2011
BP 93
EP 110
PG 18
WC Microbiology
SC Microbiology
GA BSR24
UT WOS:000285533600005
ER
PT B
AU Nevers, MB
Boehm, AB
AF Nevers, Meredith B.
Boehm, Alexandria B.
BE Sadowsky, MJ
Whitman, RL
TI MODELING FATE AND TRANSPORT OF FECAL BACTERIA IN SURFACE WATER
SO FECAL BACTERIA
LA English
DT Article; Book Chapter
ID ESCHERICHIA-COLI CONCENTRATIONS; MARINE RECREATIONAL BEACHES; SIMULATED
SOLAR-RADIATION; UNSATURATED POROUS-MEDIA; SOUTHERN LAKE-MICHIGAN; NEUSE
RIVER ESTUARY; INDICATOR BACTERIA; HUNTINGTON-BEACH; REGRESSION-MODELS;
NEARSHORE WATER
C1 [Nevers, Meredith B.] US Geol Survey, Great Lakes Sci Ctr, Lake Michigan Ecol Res Stn, Porter, IN 46304 USA.
[Boehm, Alexandria B.] Dept Civil & Environm Engn, Stanford, CA 94305 USA.
RP Nevers, MB (reprint author), US Geol Survey, Great Lakes Sci Ctr, Lake Michigan Ecol Res Stn, Porter, IN 46304 USA.
RI Sadowsky, Michael/J-2507-2016
OI Sadowsky, Michael/0000-0001-8779-2781
NR 111
TC 4
Z9 4
U1 1
U2 4
PU AMER SOC MICROBIOLOGY
PI WASHINGTON
PA 1752 N STREET NW, WASHINGTON, DC 20036-2904 USA
BN 978-1-55581-608-7
PY 2011
BP 165
EP 188
PG 24
WC Microbiology
SC Microbiology
GA BSR24
UT WOS:000285533600008
ER
PT B
AU Hooten, MB
AF Hooten, Mevin B.
BE Drew, CA
Wiersma, YF
Huettmann, F
TI The State of Spatial and Spatio-Temporal Statistical Modeling
SO PREDICTIVE SPECIES AND HABITAT MODELING IN LANDSCAPE ECOLOOGY: CONCEPTS
AND APPLICATIONS
LA English
DT Article; Book Chapter
ID SAMPLING DESIGN; PREDICTION; ABUNDANCE; ECOLOGY
C1 Colorado State Univ, USGS Colorado Cooperat Fish & Wildlife Res Unit, Dept Fish Wildlife & Conservat Biol, Ft Collins, CO 80523 USA.
RP Hooten, MB (reprint author), Colorado State Univ, USGS Colorado Cooperat Fish & Wildlife Res Unit, Dept Fish Wildlife & Conservat Biol, 201 JVK Wagar Bldg,1484 Campus Delivery, Ft Collins, CO 80523 USA.
EM mevin.hooten@colostate.edu
NR 50
TC 2
Z9 2
U1 0
U2 1
PU SPRINGER
PI NEW YORK
PA 233 SPRING STREET, NEW YORK, NY 10013, UNITED STATES
BN 978-1-4419-7389-4
PY 2011
BP 29
EP 41
DI 10.1007/978-1-4419-7390-0_3
D2 10.1007/978-1-4419-7390-0
PG 13
WC Ecology
SC Environmental Sciences & Ecology
GA BSR07
UT WOS:000285525000003
ER
PT S
AU Wood, WW
Eckardt, FD
Kraemer, TF
Eng, K
AF Wood, Warren W.
Eckardt, Frank D.
Kraemer, Thomas F.
Eng, Ken
BE Ozturk, M
Boer, B
Barth, HJ
Breckle, SW
ClusenerGodt, M
Khan, MA
TI Quantitative Eolian Transport of Evaporite Salts from the Makgadikgadi
Depression (Ntwetwe and Sua Pans) in Northeastern Botswana: Implications
for Regional Ground-Water Quality
SO SABKHA ECOSYSTEMS: AFRICA AND SOUTHERN EUROPE, VOL III
SE Tasks for Vegetation Science
LA English
DT Article; Book Chapter
ID DEPOSITION; SULFATE; WATER
AB Eolian salts from the evaporite-covered Makgadikgadi Depression in Botswana were observed in the soil as far as 150 km downwind from the depression. Over three million metric tons of chloride, sodium, and bicarbonate are transported each year from the basin to the adjacent land. Infiltering soil water mobilizes and transports these soluble salts to the ground water, where they degrade the water quality. A relation between the size of the evaporative floor area and the length of the downwind salt "footprint" on the soil was established. This permits use of readily available topographic maps to estimate the area and length of potential degradation of ground water without extensive field sampling. Significant mass of naturally-occurring radioactive 226-radium is present in the eolian-transported salts that may have deleterious health consequences for individuals residing in the downwind area.
C1 [Wood, Warren W.] Michigan State Univ, Dept Geol Sci, E Lansing, MI 48824 USA.
[Eckardt, Frank D.] Univ Cape Town, Dept Environm & Geog Sci, ZA-7701 Rondebosch, South Africa.
[Kraemer, Thomas F.; Eng, Ken] US Geol Survey, Reston, VA 20192 USA.
RP Wood, WW (reprint author), Michigan State Univ, Dept Geol Sci, Room 206,Nat Sci Bldg, E Lansing, MI 48824 USA.
EM wwwood@msu.edu
NR 21
TC 1
Z9 1
U1 0
U2 1
PU SPRINGER
PI DORDRECHT
PA PO BOX 17, 3300 AA DORDRECHT, NETHERLANDS
SN 0167-9406
BN 978-90-481-9672-2
J9 TASKS VEG SCI
JI Tasks Veg. Sci.
PY 2011
VL 46
BP 27
EP 37
DI 10.1007/978-90-481-9673-9_4
PG 11
WC Plant Sciences; Ecology
SC Plant Sciences; Environmental Sciences & Ecology
GA BSZ42
UT WOS:000286165300004
ER
PT S
AU Allison, SD
Weintraub, MN
Gartner, TB
Waldrop, MP
AF Allison, Steven D.
Weintraub, Michael N.
Gartner, Tracy B.
Waldrop, Mark P.
BE Shukla, G
Varma, A
TI Evolutionary-Economic Principles as Regulators of Soil Enzyme Production
and Ecosystem Function
SO SOIL ENZYMOLOGY
SE Soil Biology
LA English
DT Article; Book Chapter
ID N-P STOICHIOMETRY; SIMULATED NITROGEN DEPOSITION; MICROBIAL BIOMASS;
ORGANIC-MATTER; ELEVATED CO2; EXTRACELLULAR ENZYMES; TERRESTRIAL
ECOSYSTEMS; BACILLUS-LICHENIFORMIS; PHOSPHATASE-ACTIVITIES;
THEORETICAL-MODEL
C1 [Allison, Steven D.] Univ Calif Irvine, Irvine, CA 92697 USA.
[Weintraub, Michael N.] Univ Toledo, Dept Environm Sci, Toledo, OH 43606 USA.
[Gartner, Tracy B.] Carthage Coll, Dept Biol, Kenosha, WI 53140 USA.
[Gartner, Tracy B.] Carthage Coll, Environm Sci Program, Kenosha, WI 53140 USA.
[Waldrop, Mark P.] US Geol Survey, Menlo Pk, CA 94025 USA.
RP Allison, SD (reprint author), Univ Calif Irvine, 321 Steinhaus, Irvine, CA 92697 USA.
EM allisons@uci.edu; michael.weintraub@utoledo.edu; tgartner@carthage.edu;
mwaldrop@usgs.eov
RI Allison, Steven/E-2978-2010
OI Allison, Steven/0000-0003-4629-7842
NR 74
TC 55
Z9 61
U1 2
U2 18
PU SPRINGER-VERLAG BERLIN
PI BERLIN
PA HEIDELBERGER PLATZ 3, D-14197 BERLIN, GERMANY
SN 1613-3382
BN 978-3-642-14224-6
J9 SOIL BIOL
JI Soil Biol.
PY 2011
VL 22
BP 229
EP 243
DI 10.1007/978-3-642-14225-3_12
D2 10.1007/978-3-642-14225-3
PG 15
WC Soil Science
SC Agriculture
GA BRN72
UT WOS:000283198600012
ER
PT J
AU Jordan, NR
Larson, DL
Huerd, SC
AF Jordan, Nicholas R.
Larson, Diane L.
Huerd, Sheri C.
TI Evidence of Qualitative Differences between Soil-Occupancy Effects of
Invasive vs. Native Grassland Plant Species
SO INVASIVE PLANT SCIENCE AND MANAGEMENT
LA English
DT Article
DE Plant-soil feedback; biofuel; nurse plants; arbuscular mycorrhizal
fungi; invasion ecology; soil legacy; invasive plants
ID ARBUSCULAR-MYCORRHIZAL FUNGI; MICROBIAL COMMUNITY; POSITIVE
INTERACTIONS; BROMUS-TECTORUM; HIGH-DIVERSITY; RESTORATION; DYNAMICS;
VEGETATION; FEEDBACK; ECOLOGY
AB Diversified grasslands that contain native plant species are being recognized as important elements of agricultural landscapes and for production of biofuel feedstocks as well as a variety of other ecosystem services. Unfortunately, establishment of such grasslands is often difficult, unpredictable, and highly vulnerable to interference and invasion by weeds. Evidence suggests that soil-microbial "legacies" of invasive perennial species can inhibit growth of native grassland species. However, previous assessments of legacy effects of soil occupancy by invasive species that invade grasslands have focused on single invasive species and on responses to invasive soil occupancy in only a few species. In this study, we tested the hypothesis that legacy effects of invasive species differ qualitatively from those of native grassland species. In a glasshouse, three invasive and three native grassland perennials and a native perennial mixture were grown separately through three cycles of growth and soil conditioning in soils with and without arbuscular mycorrhizal fungi (AM F), after which we assessed seedling growth in these soils. Native species differed categorically from invasives in their response to soil conditioning by native or invasive species, but these differences depended on the presence of AMF. When AMF were present, native species largely had facilitative effects on invasive species, relative to effects of invasives on other invasives. Invasive species did not facilitate native growth; neutral effects were predominant, but strong soil-mediated inhibitory effects on certain native species occurred. Our results support the hypothesis that successful plant invaders create biological legacies in soil that inhibit native growth, but suggest also this mechanism of invasion will have nuanced effects on community dynamics, as some natives may be unaffected by such legacies. Such native species may be valuable as nurse plants that provide cost-effective restoration of soil conditions needed for efficient establishment of diversified grasslands.
C1 [Jordan, Nicholas R.; Huerd, Sheri C.] Univ Minnesota, Agron & Plant Genet Dept, St Paul, MN 55108 USA.
[Larson, Diane L.] US Geol Survey, No Prairie Wildlife Res Ctr, St Paul, MN 55108 USA.
RP Jordan, NR (reprint author), Univ Minnesota, Agron & Plant Genet Dept, 1991 Buford Circle, St Paul, MN 55108 USA.
EM jorda020@umn.edu
OI Larson, Diane/0000-0001-5202-0634
FU Minnesota Agricultural Experiment Station
FX We thank our field and laboratory assistants, D. Buhl and W. Newton, for
statistical advice; several colleagues for manuscript review; and the
Minnesota Agricultural Experiment Station for its support. Any use of
trade, product, or firm names is for descriptive purposes only and does
not imply endorsement by the U.S. government.
NR 71
TC 10
Z9 12
U1 5
U2 58
PU WEED SCI SOC AMER
PI LAWRENCE
PA 810 EAST 10TH ST, LAWRENCE, KS 66044-8897 USA
SN 1939-7291
J9 INVAS PLANT SCI MANA
JI Invasive Plant Sci. Manag.
PD JAN-MAR
PY 2011
VL 4
IS 1
BP 11
EP 21
DI 10.1614/IPSM-D-10-00004.1
PG 11
WC Plant Sciences
SC Plant Sciences
GA 778MH
UT WOS:000291707900002
ER
PT J
AU Gerig, B
Moerke, A
Greil, R
Koproski, S
AF Gerig, Brandon
Moerke, Ashley
Greil, Roger
Koproski, Scott
TI Movement patterns and habitat characteristics of Lake Sturgeon
(Acipenser fulvescens) in the St. Marys River, Michigan, 2007-2008
SO JOURNAL OF GREAT LAKES RESEARCH
LA English
DT Article
DE Lake sturgeon; St. Marys River; Telemetry; Acipenser fulvescens
ID POPULATION; SYSTEM; QUEBEC; USA
AB Historically, the St. Marys River (SMR), Michigan, provided suitable habitat for lake sturgeon (Acipenser fulvescens) but their population declined dramatically during the past century due to overharvest and habitat alteration. Since 2000, the Lake Superior State University Aquatic Research lab has monitored a remnant population of lake sturgeon in the SMR. During 2007 and 2008, lake sturgeon were implanted with sonic transponders to determine spatial extent, movement patterns, and habitat use in the SMR. Telemetry observations indicated that lake sturgeon inhabit a 40 km river reach, representing approximately one-third of the total area of the SMR. Lake sturgeon movement in the SMR was confined to an area between the North Channel of Sugar Island to the southern end of East Neebish Island, with the majority centered around the north end of Lake George. Additionally, lake sturgeon were not observed in the main shipping channel which suggests that they may actively avoid areas with high shipping traffic. During this study, individual weekly movement rates of lake sturgeon varied from under 100 m to over 25 km. Lake sturgeon used transition areas between lotic and lentic waters extensively. These areas create depositional habitats that may be essential foraging areas for lake sturgeon in the SMR. Telemetry results to date have not confirmed the spawning location of lake sturgeon within the SMR. However, two females with partially mature eggs were tagged in 2007 and may spawn within the next 2 years. Their movements could lead to the positive identification of the spawning location which would provide essential information for fisheries managers in the SMR. (C) 2010 International Association for Great lakes Research. Published by Elsevier B.V. All rights reserved.
C1 [Gerig, Brandon; Moerke, Ashley; Greil, Roger] Lake Super State Univ, Aquat Res Lab, Sault Ste Marie, MI 49783 USA.
[Koproski, Scott] US Fish & Wildlife Serv, Alpena Natl Fish & Wildlife Conservat Off, Alpena, MI 49707 USA.
RP Moerke, A (reprint author), Lake Super State Univ, Aquat Res Lab, 650 W Easterday Ave, Sault Ste Marie, MI 49783 USA.
EM bsgerig@ufl.edu; amoerke@lssu.edu; rgreil@lssu.edu;
scott_koproski@fws.gov
RI Greil, Richard/C-7673-2017
OI Greil, Richard/0000-0002-4462-3694
FU Bay Mills Indian Community for setline bait; National Fish and Wildlife
Foundation
FX We are grateful to the Lake Superior State University Aquatic Research
Lab summer staff (Scott Collins, Jesse Comben, Joe Menghini, Dan
Operhall, Ben Turshack, and Frank Zomer) for their valuable assistance
conducting all field work and processing habitat samples, the Bay Mills
Indian Community for setline bait and the National Fish and Wildlife
Foundation for funding. Additional thanks goes to two anonymous
reviewers for comments and constructive critiques.
NR 27
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U1 3
U2 29
PU ELSEVIER SCI LTD
PI OXFORD
PA THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, OXON, ENGLAND
SN 0380-1330
J9 J GREAT LAKES RES
JI J. Gt. Lakes Res.
PY 2011
VL 37
SU 2
SI SI
BP 54
EP 60
DI 10.1016/j.jglr.2010.09.007
PG 7
WC Environmental Sciences; Limnology; Marine & Freshwater Biology
SC Environmental Sciences & Ecology; Marine & Freshwater Biology
GA 778OC
UT WOS:000291713000009
ER
PT J
AU Schaeffer, JS
Fielder, DG
Godby, N
Bowen, A
O'Connor, L
Parrish, J
Greenwood, S
Chong, S
Wright, G
AF Schaeffer, Jeffrey S.
Fielder, David G.
Godby, Neal
Bowen, Anjanette
O'Connor, Lisa
Parrish, Josh
Greenwood, Susan
Chong, Stephen
Wright, Greg
TI Long-term trends in the St. Marys River open water fish community
SO JOURNAL OF GREAT LAKES RESEARCH
LA English
DT Article
DE St. Marys River; Walleye; Yellow perch; Northern pike; Cisco
ID LAKE-HURON; FISHERIES; COLLAPSE
AB We examined trends in species composition and abundance of the St. Marys River fish community. Abundance data were available approximately once every six years from 1975 through 2006, and size and age data were available from 1995 through 2006. We also compared survey data in 2006 with results of a concurrent creel survey that year, as well as data from prior surveys spanning a 69 year time frame. The St. Marys River fish community was best characterized as a coolwater fish community with apparent little variation in species composition, and only slight variation in overall fish abundance since 1975. However, we did find recent trends in abundance among target species sought by anglers: centrarchids increased, percids appeared stable, and both northern pike Esox lucius and cisco Coregonus artedii declined. Survey results suggested that walleye (Sander vitreus) and yellow perch (Perca flavescens) experienced moderate exploitation but benefited from recent strong recruitment and faster growth. Mechanisms underlying declines of northern pike and cisco were not clear: reduced abundance could have resulted from high exploitation, variation in recruitment, or a combination of both factors. Despite these challenges, the St. Marys River fish community appears remarkably stable. We suggest that managers insure that creel surveys occur simultaneously with assessments, but periodic gill net surveys may no longer provide adequate data in support of recent, more complex management objectives. While additional surveys would add costs, more frequent data might ensure sustainability of a unique fish community that supports a large proportion of angler effort on Lake Huron. (C) 2011 International Association for Great Lakes Research. Published by Elsevier B.V. All rights reserved.
C1 [Schaeffer, Jeffrey S.] US Geol Survey, Great Lakes Sci Ctr, Ann Arbor, MI 48105 USA.
[Fielder, David G.] Michigan Dept Nat Resources & Environm, Alpena Fisheries Res Stn, Alpena, MI 49707 USA.
[Godby, Neal] Michigan Dept Nat Resources & Environm, No Lake Huron Management Unit, Gaylord, MI 49735 USA.
[Bowen, Anjanette] US Fish & Wildlife Serv, Alpena Fisheries Resource Off, Alpena, MI 49707 USA.
[O'Connor, Lisa] Fisheries & Oceans Canada, Great Lakes Lab Fisheries & Aquat Sci, Sault Ste Marie, ON P6A 6W4, Canada.
[Parrish, Josh] Bay Mills Indian Community, Brimley, MI 49715 USA.
[Greenwood, Susan; Chong, Stephen] Ontario Minist Nat Resources, Sault Ste Marie, ON P6A 2E5, Canada.
[Wright, Greg] Chippewa Ottawa Resource Author, Sault Ste Marie, MI 49783 USA.
RP Schaeffer, JS (reprint author), US Geol Survey, Great Lakes Sci Ctr, 1451 Green Rd, Ann Arbor, MI 48105 USA.
EM jschaeffer@usgs.gov
NR 29
TC 7
Z9 7
U1 1
U2 8
PU ELSEVIER SCI LTD
PI OXFORD
PA THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, OXON, ENGLAND
SN 0380-1330
J9 J GREAT LAKES RES
JI J. Gt. Lakes Res.
PY 2011
VL 37
SU 2
SI SI
BP 70
EP 79
DI 10.1016/j.jglr.2011.02.002
PG 10
WC Environmental Sciences; Limnology; Marine & Freshwater Biology
SC Environmental Sciences & Ecology; Marine & Freshwater Biology
GA 778OC
UT WOS:000291713000011
ER
PT J
AU Soranno, PA
Wagner, T
Martin, SL
McLean, C
Novitski, LN
Provence, CD
Rober, AR
AF Soranno, Patricia A.
Wagner, Tyler
Martin, Sherry L.
McLean, Colleen
Novitski, Linda N.
Provence, Cole D.
Rober, Allison R.
TI Quantifying regional reference conditions for freshwater ecosystem
management: A comparison of approaches and future research needs
SO LAKE AND RESERVOIR MANAGEMENT
LA English
DT Article
DE freshwater assessment; paleolimnology; predictive classification models;
regional reference conditions; regionalization
ID MULTIPLE TAXONOMIC GROUPS; BIOTIC INTEGRITY; BENTHIC MACROINVERTEBRATES;
GREAT-LAKES; NUTRIENT CRITERIA; NORTHERN LAKES; BIOLOGICAL ASSESSMENT;
ECOLOGICAL CONDITION; RESOURCE MANAGEMENT; FORESTS ECOREGION
AB Accurate and robust approaches for quantifying regional reference conditions are critical to the management and restoration of freshwater resources. We considered approaches developed for streams, lakes, or wetlands and for either biological or chemical waterbody features to review 4 common approaches for quantifying regional reference conditions: multimetric, multivariate, landscape-context statistical modeling, and paleolimnology. We focused on the major steps in the decision-making process that led to the most appropriate approach. Based on this synthesis, we argue that there is a need to (1) more explicitly quantify the spatial scale of waterbody variation within and across regions, (2) develop and use predictive classification models in a more explicit fashion to more effectively model this local and regional variation, (3) consider additional metrics with a focus on lakes and wetland responses to both individual and multiple anthropogenic stressors, and (4) continue to develop quantitative approaches to explicitly account for uncertainties in regional reference condition predictions.
C1 [Soranno, Patricia A.; Martin, Sherry L.; Provence, Cole D.] Michigan State Univ, Dept Fisheries & Wildlife, E Lansing, MI 48824 USA.
[Wagner, Tyler] Penn State Univ, US Geol Survey, Penn Cooperat Fish & Wildlife Res Unit, University Pk, PA 16802 USA.
[McLean, Colleen] Michigan State Univ, Dept Geol Sci, E Lansing, MI 48824 USA.
[Novitski, Linda N.; Rober, Allison R.] Michigan State Univ, Dept Zool, E Lansing, MI 48824 USA.
RP Soranno, PA (reprint author), Michigan State Univ, Dept Fisheries & Wildlife, 13 Nat Resources Bldg, E Lansing, MI 48824 USA.
EM soranno@msu.edu
NR 81
TC 13
Z9 13
U1 7
U2 47
PU NORTH AMER LAKE MANAGEMENT SOC
PI MADISON
PA PO BOX 5443, MADISON, WI 53705-5443 USA
SN 1040-2381
J9 LAKE RESERV MANAGE
JI Lake Reserv. Manag.
PY 2011
VL 27
IS 2
BP 138
EP 148
AR PII 937257204
DI 10.1080/07438141.2011.573614
PG 11
WC Limnology; Marine & Freshwater Biology; Water Resources
SC Marine & Freshwater Biology; Water Resources
GA 780KE
UT WOS:000291853900004
ER
PT J
AU Brown, ME
Crosier, A
Lynch, W
Converse, SJ
Chandler, J
Olsen, G
French, J
Wildt, DE
Songsasen, N
AF Brown, M. E.
Crosier, A.
Lynch, W.
Converse, S. J.
Chandler, J.
Olsen, G.
French, J.
Wildt, D. E.
Songsasen, N.
TI SEMINAL QUALITY IN WHOOPING CRANE (GRUS AMERICANA) IS AFFECTED BY STAGE
OF BREEDING SEASON BUT NOT BY AGE OF INDIVIDUAL
SO REPRODUCTION FERTILITY AND DEVELOPMENT
LA English
DT Meeting Abstract
C1 [Brown, M. E.; Crosier, A.; Lynch, W.; Wildt, D. E.; Songsasen, N.] Smithsonian Conservat Biol Inst, Front Royal, VA USA.
[Converse, S. J.; Chandler, J.; Olsen, G.; French, J.] US Fish & Wildlife Serv, Patuxent Wildlife Res Ctr, Laurel, MD 20708 USA.
NR 0
TC 0
Z9 0
U1 0
U2 6
PU CSIRO PUBLISHING
PI COLLINGWOOD
PA 150 OXFORD ST, PO BOX 1139, COLLINGWOOD, VICTORIA 3066, AUSTRALIA
SN 1031-3613
J9 REPROD FERT DEVELOP
JI Reprod. Fertil. Dev.
PY 2011
VL 23
IS 1
MA 231
BP 214
EP 214
PG 1
WC Developmental Biology; Reproductive Biology; Zoology
SC Developmental Biology; Reproductive Biology; Zoology
GA 690MF
UT WOS:000285008200241
ER
PT J
AU Milly, PCD
Dunne, KA
AF Milly, P. C. D.
Dunne, Krista A.
TI On the Hydrologic Adjustment of Climate-Model Projections: The Potential
Pitfall of Potential Evapotranspiration
SO EARTH INTERACTIONS
LA English
DT Article
DE Hydrologic model; Climate change; Potential evapotranspiration
ID DATASET
AB Hydrologic models often are applied to adjust projections of hydroclimatic change that come from climate models. Such adjustment includes climate-bias correction, spatial refinement ("downscaling"), and consideration of the roles of hydrologic processes that were neglected in the climate model. Described herein is a quantitative analysis of the effects of hydrologic adjustment on the projections of runoff change associated with projected twenty-first-century climate change. In a case study including three climate models and 10 river basins in the contiguous United States, the authors find that relative (i.e., fractional or percentage) runoff change computed with hydrologic adjustment more often than not was less positive (or, equivalently, more negative) than what was projected by the climate models. The dominant contributor to this decrease in runoff was a ubiquitous change in runoff (median - 11%) caused by the hydrologic model's apparent amplification of the climate-model-implied growth in potential evapotranspiration. Analysis suggests that the hydrologic model, on the basis of the empirical, temperature-based modified Jensen-Haise formula, calculates a change in potential evapotranspiration that is typically 3 times the change implied by the climate models, which explicitly track surface energy budgets. In comparison with the amplification of potential evapotranspiration, central tendencies of other contributions from hydrologic adjustment (spatial refinement, climate-bias adjustment, and process refinement) were relatively small. The authors' findings highlight the need for caution when projecting changes in potential evapotranspiration for use in hydrologic models or drought indices to evaluate climate-change impacts on water.
C1 [Milly, P. C. D.; Dunne, Krista A.] US Geol Survey, Princeton, NJ USA.
RP Milly, PCD (reprint author), NOAA, Geophys Fluid Dynam Lab, 201 Forrestal Rd, Princeton, NJ 08540 USA.
EM cmilly@usgs.gov
NR 10
TC 43
Z9 43
U1 4
U2 27
PU AMER METEOROLOGICAL SOC
PI BOSTON
PA 45 BEACON ST, BOSTON, MA 02108-3693 USA
SN 1087-3562
J9 EARTH INTERACT
JI Earth Interact.
PD JAN
PY 2011
VL 15
AR 1
DI 10.1175/2010EI363.1
PG 14
WC Geosciences, Multidisciplinary
SC Geology
GA 771GM
UT WOS:000291145200001
ER
PT J
AU Harris, JE
Hightower, JE
AF Harris, Julianne E.
Hightower, Joseph E.
TI Movement Patterns of American Shad Transported Upstream of Dams on the
Roanoke River, North Carolina and Virginia
SO NORTH AMERICAN JOURNAL OF FISHERIES MANAGEMENT
LA English
DT Article
ID LOW-HEAD DAM; CONNECTICUT RIVER; ALOSA-SAPIDISSIMA; FISH PASSAGE; JAMES
RIVER; YORK RIVER; ADULT; RESTORATION; POPULATION; MIGRATION
AB American shad Alosa sapidissima are in decline throughout much of their native range as a result of overfishing, pollution, and habitat alteration in coastal rivers where they spawn. One approach to restoration in regulated rivers is to provide access to historical spawning habitat above dams through a trap-and-transport program. We examined the initial survival, movement patterns, spawning, and downstream passage of sonic-tagged adult American shad transported to reservoir and riverine habitats upstream of hydroelectric dams on the Roanoke River, North Carolina and Virginia, during 2007-2009. Average survival to release in 2007-2008 was 85%, but survival decreased with increasing water temperature. Some tagged fish released in reservoirs migrated upstream to rivers; however, most meandered back and forth within the reservoir. A higher percentage of fish migrated through a smaller (8,215-ha) than a larger (20,234-ha) reservoir, suggesting that the population-level effects of transport may depend on upper basin characteristics. Transported American shad spent little time in upper basin rivers but were there when temperatures were appropriate for spawning. No American shad eggs were collected during weekly plankton sampling in upper basin rivers. The estimated initial survival of sonic-tagged American shad after downstream passage through each dam was 71-100%; however, only 1% of the detected fish migrated downstream through all three dams and many were relocated just upstream of a dam late in the season. Although adult American shad were successfully transported to upstream habitats in the Roanoke River basin, under present conditions transported individuals may have reduced effective fecundity and postspawning survival compared with nontransported fish that spawn in the lower Roanoke River.
C1 [Harris, Julianne E.; Hightower, Joseph E.] N Carolina State Univ, Dept Biol, N Carolina Cooperat Fish & Wildlife Res Unit, US Geol Survey, Raleigh, NC 27695 USA.
RP Harris, JE (reprint author), N Carolina State Univ, Dept Biol, N Carolina Cooperat Fish & Wildlife Res Unit, US Geol Survey, 127 David Clark Labs,Campus Box 7617, Raleigh, NC 27695 USA.
EM jeharris@ncsu.edu
FU Dominion/North Carolina Power; North Carolina Wildlife Resources
Commission; North Carolina State University; U.S. Geological Survey;
U.S. Fish and Wildlife Service; Wildlife Management Institute
FX We thank Nicole Antaya, Jeffery Buckel, Chad Coley, Patrick Cooney,
Kevin Dockendorf, Robert Graham, Thomas Kwak, Kenneth Pollock, and Kyle
Ward for help with design, field work, and analysis of this study. We
appreciate Fritz Rohde and Troy Tuckey for reviewing an earlier draft of
this manuscript. This work was funded by Dominion/North Carolina Power
and the North Carolina Wildlife Resources Commission. The North Carolina
Cooperative Fish and Wildlife Research Unit is jointly supported by
North Carolina State University, North Carolina Wildlife Resources
Commission, U.S. Geological Survey, U.S. Fish and Wildlife Service, and
Wildlife Management Institute. Any use of trade, product, or firm names
is for descriptive purposes only and does not imply endorsement by the
U.S. government.
NR 60
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U1 3
U2 27
PU TAYLOR & FRANCIS INC
PI PHILADELPHIA
PA 530 WALNUT STREET, STE 850, PHILADELPHIA, PA 19106 USA
SN 0275-5947
EI 1548-8675
J9 N AM J FISH MANAGE
JI North Am. J. Fish Manage.
PY 2011
VL 31
IS 2
BP 240
EP 256
DI 10.1080/02755947.2011.572806
PG 17
WC Fisheries
SC Fisheries
GA 761VJ
UT WOS:000290428800007
ER
PT J
AU Sykes, CL
Caldwell, CA
Gould, WR
AF Sykes, Catherine L.
Caldwell, Colleen A.
Gould, William R.
TI Physiological Effects of Potassium Chloride, Formalin, and Handling
Stress on Bonytail
SO NORTH AMERICAN JOURNAL OF FISHERIES MANAGEMENT
LA English
DT Article
ID JUVENILE CHINOOK SALMON; PLASMA-CORTISOL; ZEBRA MUSSELS; AQUACULTURE
ACTIVITIES; DREISSENA-POLYMORPHA; OFFSHORE WATERS; FISH HATCHERY;
RESPONSES; TRANSPORT; CONFINEMENT
AB We characterized the sublethal physiological changes in bonytail Gila elegans subjected to consecutive 750-mg/L potassium chloride (KCl) and 25-mg/L formalin treatments for the removal of zebra mussel Dreissena polymorpha and quagga mussel D. bugensis veligers. Plasma cortisol, glucose, and osmolality were measured over 24 h and at 14 d posthandling after exposing bonytail to KCl and one net stressor (capture with a net), KCl plus formalin and two net stressors, and one or two net stressors without chemicals. Elevated plasma cortisol (322-440 ng/mL) and glucose (254-399 mg/dL) concentrations were observed in all treatments compared with the concentrations in control fish (plasma cortisol, 56 ng/mL; glucose, 43 mg/dL). While there were no detectable differences in plasma osmolality among the treatment and control fish, a difference was observed between fish that were handled once versus twice. Chemical effects of stress were not observed in any of the physiological responses when the KCl treatment was compared with the one-net stressor treatment or when the KCl plus formalin treatment was compared with the two-net stressor treatment. Cumulative responses, however, were observed between one net stressor and two net stressors for plasma glucose and osmolality but not for plasma cortisol. Plasma cortisol and glucose levels remained elevated at 24 h posthandling, indicating that bonytail had not completely recovered from the handling stressors and would benefit from a recovery period in protected refugia before being released.
C1 [Sykes, Catherine L.] US Fish & Wildlife Serv, Dexter Natl Fish Hatchery & Technol Ctr, Dexter, NM 88230 USA.
[Caldwell, Colleen A.] New Mexico State Univ, New Mexico Cooperat Fish & Wildlife Res Unit, US Geol Survey, Dept Fish Wildlife & Conservat Ecol, Las Cruces, NM 88003 USA.
[Gould, William R.] New Mexico State Univ, Univ Stat Ctr, Las Cruces, NM 88003 USA.
RP Sykes, CL (reprint author), US Fish & Wildlife Serv, Dexter Natl Fish Hatchery & Technol Ctr, POB 219, Dexter, NM 88230 USA.
EM catherine_sykes@fws.gov
FU U.S. Fish and Wildlife Service; Dexter National Fish Hatchery and
Technology Center
FX Funding for this research was provided by the U.S. Fish and Wildlife
Service, Dexter National Fish Hatchery and Technology Center. Additional
support was provided by U.S. Geological Survey, Cooperative Research
Units and New Mexico State University, Agricultural Experiment Station.
The authors are grateful to Manuel Ulibarri, William Knight, Jason
Nachtmann, Bill Williams, Renee Martin, and Michael Shoemaker for their
tireless help throughout the project. We also thank Wade Wilson and
Connie Keeler-Foster for invaluable comments during the preparation of
this manuscript. The work was conducted under the U.S. Fish and Wildlife
Service Federal Endangered Species permit number TE676811-2. The
findings and conclusions in this article are those of the authors and do
not necessarily represent the views of the U.S. Fish and Wildlife
Service. Mention of trade names or commercial products does not
constitute endorsement or recommendation for use by the U.S. Government.
NR 34
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U1 2
U2 13
PU TAYLOR & FRANCIS INC
PI PHILADELPHIA
PA 325 CHESTNUT ST, SUITE 800, PHILADELPHIA, PA 19106 USA
SN 0275-5947
J9 N AM J FISH MANAGE
JI North Am. J. Fish Manage.
PY 2011
VL 31
IS 2
BP 291
EP 298
DI 10.1080/02755947.2011.576201
PG 8
WC Fisheries
SC Fisheries
GA 761VJ
UT WOS:000290428800011
ER
PT J
AU Quinn, JW
Kwak, TJ
AF Quinn, Jeffrey W.
Kwak, Thomas J.
TI Movement and Survival of Brown Trout and Rainbow Trout in an Ozark
Tailwater River
SO NORTH AMERICAN JOURNAL OF FISHERIES MANAGEMENT
LA English
DT Editorial Material
ID SEASONAL MOVEMENT; TENNESSEE; MICHIGAN; PATTERNS; HABITAT; STREAM
AB We evaluated the movement of adult brown trout Salmo trutta and rainbow trout Oncorhynchus mykiss in relation to a catch-and-release area in the White River downstream from Beaver Dam, Arkansas. Nine fish of each species were implanted with radio transmitters and monitored from July 1996 to July 1997. The 1.5-km river length of a catch-and-release area (closed to angler harvest) was greater than the total linear range of 72% of the trout (13 of 18 fish), but it did not include two brown trout spawning riffles, suggesting that it effectively protects resident fish within the catch-and-release area except during spawning. The total detected linear range of movement varied from 172 to 3,559 m for brown trout and from 205 to 3,023 m for rainbow trout. The movements of both species appeared to be generally similar to that in unregulated river systems. The annual apparent survival of both trout species was less than 0.40, and exploitation was 44%. Management to protect fish on spawning riffles may be considered if management for wild brown trout becomes a priority.
C1 [Quinn, Jeffrey W.] Arkansas Game & Fish Commiss, Little Rock, AR 72205 USA.
[Kwak, Thomas J.] N Carolina State Univ, Dept Biol, N Carolina Cooperat Fish & Wildlife Res Unit, US Geol Survey, Raleigh, NC 27695 USA.
RP Quinn, JW (reprint author), Arkansas Game & Fish Commiss, 2 Nat Resources Dr, Little Rock, AR 72205 USA.
EM jwquinn@agfc.state.ar.us
NR 26
TC 1
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U1 1
U2 13
PU TAYLOR & FRANCIS INC
PI PHILADELPHIA
PA 325 CHESTNUT ST, SUITE 800, PHILADELPHIA, PA 19106 USA
SN 0275-5947
J9 N AM J FISH MANAGE
JI North Am. J. Fish Manage.
PY 2011
VL 31
IS 2
BP 299
EP 304
DI 10.1080/02755947.2011.576204
PG 6
WC Fisheries
SC Fisheries
GA 761VJ
UT WOS:000290428800012
ER
PT J
AU Peirce, JM
Otis, EO
Wipfli, MS
Follmann, EH
AF Peirce, Joshua M.
Otis, Edward O.
Wipfli, Mark S.
Follmann, Erich H.
TI Radiotelemetry to Estimate Stream Life of Adult Chum Salmon in the
McNeil River, Alaska
SO NORTH AMERICAN JOURNAL OF FISHERIES MANAGEMENT
LA English
DT Editorial Material
ID UNDER-THE-CURVE; SPAWNING SALMON; SOCKEYE-SALMON; PACIFIC SALMON;
ESCAPEMENT ESTIMATION; RESIDENCE TIME; AERIAL COUNTS; ONCORHYNCHUS;
EFFICIENCY; TELEMETRY
AB Estimating salmon escapement is one of the fundamental steps in managing salmon populations. The area-under-the-curve (AUC) method is commonly used to convert periodic aerial survey counts into annual salmon escapement indices. The AUC requires obtaining accurate estimates of stream life (SL) for target species. Traditional methods for estimating SL (e.g., mark-recapture) are not feasible for many populations. Our objective in this study was to determine the average SL of chum salmon Oncorhynchus keta in the McNeil River, Alaska, through radiotelemetry. During the 2005 and 2006 runs, 155 chum salmon were fitted with mortality-indicating radio tags as they entered the McNeil River and tracked until they died. A combination of remote data loggers, aerial surveys, and foot surveys were used to determine the location of fish and provide an estimate of time of death. Higher predation resulted in tagged fish below McNeil Falls having a significantly shorter SL (12.6 d) than those above (21.9 d). The streamwide average SL (13.8 d) for chum salmon at the McNeil River was lower than the regionwide value (17.5 d) previously used to generate AUC indices of chum salmon escapement for the McNeil River. We conclude that radiotelemetry is an effective tool for estimating SL in rivers not well suited to other methods.
C1 [Peirce, Joshua M.] Alaska Dept Fish & Game, Div Wildlife Conservat, Fairbanks, AK 99701 USA.
[Otis, Edward O.] Alaska Dept Fish & Game, Div Commercial Fisheries, Homer, AK 99603 USA.
[Wipfli, Mark S.] Univ Alaska Fairbanks, Inst Arctic Biol, Alaska Cooperat Fish & Wildlife Res Unit, US Geol Survey, Fairbanks, AK 99775 USA.
RP Peirce, JM (reprint author), Alaska Dept Fish & Game, Div Wildlife Conservat, 1300 Coll Rd, Fairbanks, AK 99701 USA.
EM joshua.peirce@alaska.gov
NR 31
TC 1
Z9 1
U1 1
U2 5
PU TAYLOR & FRANCIS INC
PI PHILADELPHIA
PA 325 CHESTNUT ST, SUITE 800, PHILADELPHIA, PA 19106 USA
SN 0275-5947
J9 N AM J FISH MANAGE
JI North Am. J. Fish Manage.
PY 2011
VL 31
IS 2
BP 315
EP 322
DI 10.1080/02755947.2011.574080
PG 8
WC Fisheries
SC Fisheries
GA 761VJ
UT WOS:000290428800014
ER
PT J
AU Hudson, JM
Johnson, JR
Kynard, B
AF Hudson, J. Michael
Johnson, Jeffrey R.
Kynard, Boyd
TI A Portable Electronarcosis System for Anesthetizing Salmonids and Other
Fish
SO NORTH AMERICAN JOURNAL OF FISHERIES MANAGEMENT
LA English
DT Editorial Material
ID ELECTRICAL ANESTHESIA; RAINBOW-TROUT; IMMOBILIZATION; ELECTROSHOCK;
PIMELODIDAE; MIGRATION; GAIRDNERI; BEHAVIOR; MS-222; BRAZIL
AB The physiological responses of fish to continuous (nonpulsed) direct current were first described in the 1960s. One of these responses, electronarcosis (anesthesia, accompanied by muscle relaxation, through electrical inhibition), has been used in fisheries research and management as an anesthetic since the 1970s. We provide details on the assembly and operation of a portable electronarcosis unit for fish anesthesia and describe its performance with respect to two species of salmonids. The portability and effectiveness of this approach make electronarcosis a viable alternative to existing anesthetics that can be used for a number of applications.
C1 [Hudson, J. Michael; Johnson, Jeffrey R.] US Fish & Wildlife Serv, Columbia River Fisheries Program Off, Vancouver, WA 98683 USA.
[Kynard, Boyd] BK Riverfish LLC, Amherst, MA 01002 USA.
RP Hudson, JM (reprint author), US Fish & Wildlife Serv, Columbia River Fisheries Program Off, 1211 SE Cardinal Court,Suite 100, Vancouver, WA 98683 USA.
EM michael_hudson@fws.gov
NR 26
TC 9
Z9 10
U1 2
U2 8
PU TAYLOR & FRANCIS INC
PI PHILADELPHIA
PA 325 CHESTNUT ST, SUITE 800, PHILADELPHIA, PA 19106 USA
SN 0275-5947
J9 N AM J FISH MANAGE
JI North Am. J. Fish Manage.
PY 2011
VL 31
IS 2
BP 335
EP 339
DI 10.1080/02755947.2011.578524
PG 5
WC Fisheries
SC Fisheries
GA 761VJ
UT WOS:000290428800016
ER
PT J
AU Wagner, T
Sweka, JA
AF Wagner, Tyler
Sweka, John A.
TI Evaluation of Hypotheses for Describing Temporal Trends in Atlantic
Salmon Parr Densities in Northeast US Rivers
SO NORTH AMERICAN JOURNAL OF FISHERIES MANAGEMENT
LA English
DT Article
ID GENERALIZED ADDITIVE-MODELS; SALAR FRY; SURVIVAL; MORTALITY; RECOVERY;
GROWTH; SIZE
AB Atlantic salmon Salmo salar in the USA have declined dramatically and their persistence is heavily dependent on stocking juvenile fish, predominantly fry. The success of stocking hatchery fry is evaluated annually throughout New England by electrofishing surveys targeting age-1 parr. The objective of this study was to examine temporal trends in Atlantic salmon parr densities throughout New England and determine how trends vary among river basins. We fit generalized additive mixed models to investigate potential linear and nonlinear temporal trends in parr density. Akaike's information criterion was used to evaluate competing hypotheses about how temporal trends vary regionally. The top-ranked model suggested two types of trends. The first type (the Penobscot River) showed a nonlinear trend in which parr densities increased until the 1990s and then rapidly decreased through 2008. The second type (all other rivers) showed a linear decrease throughout the time series. Parr density trends reflected trends in spawning escapement for each river group. We conclude that fry stocking has not been able to overcome the decrease in spawning escapement in altered stream ecosystems in New England and that additional management strategies should be considered.
C1 [Wagner, Tyler] Penn State Univ, Penn Cooperat Fish & Wildlife Res Unit, US Geol Survey, University Pk, PA 16802 USA.
[Sweka, John A.] US Fish & Wildlife Serv, NE Fishery Ctr, Lamar, PA 16848 USA.
RP Wagner, T (reprint author), Penn State Univ, Penn Cooperat Fish & Wildlife Res Unit, US Geol Survey, 402 Forest Resources Bldg, University Pk, PA 16802 USA.
EM txw19@psu.edu
NR 42
TC 2
Z9 2
U1 0
U2 1
PU TAYLOR & FRANCIS INC
PI PHILADELPHIA
PA 325 CHESTNUT ST, SUITE 800, PHILADELPHIA, PA 19106 USA
SN 0275-5947
J9 N AM J FISH MANAGE
JI North Am. J. Fish Manage.
PY 2011
VL 31
IS 2
BP 340
EP 351
DI 10.1080/02755947.2011.574081
PG 12
WC Fisheries
SC Fisheries
GA 761VJ
UT WOS:000290428800017
ER
PT J
AU Rech, JA
Pigati, JS
Lehmann, SB
McGimpsey, CN
Grimley, DA
Nekola, JC
AF Rech, Jason A.
Pigati, Jeffrey S.
Lehmann, Sophie B.
McGimpsey, Chelsea N.
Grimley, David A.
Nekola, Jeffrey C.
TI ASSESSING OPEN-SYSTEM BEHAVIOR OF C-14 IN TERRESTRIAL GASTROPOD SHELLS
SO RADIOCARBON
LA English
DT Article
ID RADIOCARBON AGE ANOMALIES; SNAIL SHELLS; LAND SNAILS; CARBONATE;
SAMPLES; VALIDITY; DEPOSITS; ARIZONA; BASIN; DATES
AB In order to assess open-system behavior of radiocarbon in fossil gastropod shells, we measured the C-14 activity on 10 aliquots of shell material recovered from Illinoian (similar to 190-130 ka) and pre-Illinoian (similar to 800 ka) loess and lacustrine deposits in the Midwestern USA. Eight of the 10 aliquots yielded measurable C-14 activities that ranged from 0.25 to 0.53 percent modern carbon (pMC), corresponding to apparent C-14 ages between 48.2 and 42.1 ka. This small level of open-system behavior is common in many materials that are used for C-14 dating (e.g. charcoal), and typically sets the upper practical limit of the technique. Two aliquots of gastropod shells from the Illinoian-aged Petersburg Silt (Petersburg Section) in central Illinois, USA, however, yielded elevated C-14 activities of 1.26 and 1.71 pMC, which correspond to apparent C-14 ages of 35.1 and 32.7 ka. Together, these results suggest that while many fossil gastropods shells may not suffer from major (>1%) open-system problems, this is not always the case. We then examined the mineralogy, trace element chemistry, and physical characteristics of a suite of fossil and modern gastropod shells to identify the source of contamination in the Petersburg shells and assess the effectiveness of these screening techniques at identifying samples suitable for C-14 dating. Mineralogical (XRD) and trace element analyses were inconclusive, which suggests that these techniques are not suitable for assessing open-system behavior in terrestrial gastropod shells. Analysis with scanning electron microscopy (SEM), however, identified secondary mineralization (calcium carbonate) primarily within the inner whorls of the Petersburg shells. This indicates that SEM examination, or possibly standard microscope examination, of the interior of gastropod shells should be used when selecting fossil gastropod shells for C-14 dating.
C1 [Rech, Jason A.; Lehmann, Sophie B.; McGimpsey, Chelsea N.] Miami Univ, Dept Geol, Oxford, OH 45056 USA.
[Pigati, Jeffrey S.] US Geol Survey, Denver Fed Ctr, Denver, CO 80225 USA.
[Grimley, David A.] Univ Illinois, Illinois State Geol Survey, Champaign, IL 61820 USA.
[Nekola, Jeffrey C.] Univ New Mexico, Dept Biol, Albuquerque, NM 87131 USA.
RP Rech, JA (reprint author), Miami Univ, Dept Geol, Oxford, OH 45056 USA.
EM rechja@muohio.edu
FU National Science Foundation [NSF EAR 0614647]; Sedimentary Geology and
Paleontology program
FX This research was funded by National Science Foundation research grant
NSF EAR 0614647 to JSP, JAR, and JCN from the Sedimentary Geology and
Paleontology program.
NR 31
TC 8
Z9 8
U1 1
U2 12
PU UNIV ARIZONA DEPT GEOSCIENCES
PI TUCSON
PA RADIOCARBON 4717 E FORT LOWELL RD, TUCSON, AZ 85712 USA
SN 0033-8222
EI 1945-5755
J9 RADIOCARBON
JI Radiocarbon
PY 2011
VL 53
IS 2
BP 325
EP 335
PG 11
WC Geochemistry & Geophysics
SC Geochemistry & Geophysics
GA 770NK
UT WOS:000291093400009
ER
PT J
AU O'Donnell, JA
Harden, JW
McGuire, AD
Romanovsky, VE
AF O'Donnell, J. A.
Harden, J. W.
McGuire, A. D.
Romanovsky, V. E.
TI Exploring the sensitivity of soil carbon dynamics to climate change,
fire disturbance and permafrost thaw in a black spruce ecosystem
SO BIOGEOSCIENCES
LA English
DT Article
ID ORGANIC-MATTER DECOMPOSITION; INTERIOR ALASKA; BOREAL FOREST;
TEMPERATURE SENSITIVITY; THERMAL DYNAMICS; ACTIVE LAYER; SNOW COVER;
RESPIRATION; TUNDRA; MODEL
AB In the boreal region, soil organic carbon (OC) dynamics are strongly governed by the interaction between wildfire and permafrost. Using a combination of field measurements, numerical modeling of soil thermal dynamics, and mass-balance modeling of OC dynamics, we tested the sensitivity of soil OC storage to a suite of individual climate factors (air temperature, soil moisture, and snow depth) and fire severity. We also conducted sensitivity analyses to explore the combined effects of fire-soil moisture interactions and snow seasonality on OC storage. OC losses were calculated as the difference in OC stocks after three fire cycles (similar to 500 yr) following a prescribed step-change in climate and/or fire. Across single-factor scenarios, our findings indicate that warmer air temperatures resulted in the largest relative soil OC losses (similar to 5.3 kg C m(-2)), whereas dry soil conditions alone (in the absence of wildfire) resulted in the smallest carbon losses (similar to 0.1 kg C m(-2)). Increased fire severity resulted in carbon loss of similar to 3.3 kg C m(-2), whereas changes in snow depth resulted in smaller OC losses (2.1-2.2 kg C m(-2)). Across multiple climate factors, we observed larger OC losses than for single-factor scenarios. For instance, high fire severity regime associated with warmer and drier conditions resulted in OC losses of similar to 6.1 kg C m(-2), whereas a low fire severity regime associated with warmer and wetter conditions resulted in OC losses of similar to 5.6 kg C m(-2). A longer snow-free season associated with future warming resulted in OC losses of similar to 5.4 kg C m(-2). Soil climate was the dominant control on soil OC loss, governing the sensitivity of microbial decomposers to fluctuations in temperature and soil moisture; this control, in turn, is governed by interannual changes in active layer depth. Transitional responses of the active layer depth to fire regimes also contributed to OC losses, primarily by determining the proportion of OC into frozen and unfrozen soil layers.
C1 [O'Donnell, J. A.] Univ Alaska Fairbanks, Dept Biol & Wildlife, Fairbanks, AK USA.
[Harden, J. W.] US Geol Survey, Menlo Pk, CA 94025 USA.
[McGuire, A. D.] Univ Alaska, Alaska Cooperat Fish & Wildlife Res Unit, US Geol Survey, Fairbanks, AK 99701 USA.
[Romanovsky, V. E.] Univ Alaska Fairbanks, Inst Geophys, Fairbanks, AK 99775 USA.
RP O'Donnell, JA (reprint author), Univ Alaska Fairbanks, Dept Biol & Wildlife, Fairbanks, AK USA.
EM jodonnell@usgs.gov
FU National Science Foundation [EAR-0630249, DEB-0423442]; Institute of
Northern Engineering at the University of Alaska Fairbanks; US
Geological Survey; Bonanza Creek LTER; USDA Forest Service
[PNW01-JV11261952-231]
FX Funding and support for J. O'Donnell was provided by the National
Science Foundation grant EAR-0630249 and the Institute of Northern
Engineering at the University of Alaska Fairbanks. We thank Eran Hood
and two anonymous reviewers for providing valuable comments on an
earlier version of this manuscript. The study was also supported by
grants from the US Geological Survey to Harden and McGuire, and by the
Bonanza Creek LTER (Long-Term Ecological Research) Program, funded
jointly by NSF (grant DEB-0423442) and the USDA Forest Service (Pacific
Northwest Research Station grant PNW01-JV11261952-231).
NR 75
TC 18
Z9 19
U1 0
U2 55
PU COPERNICUS GESELLSCHAFT MBH
PI GOTTINGEN
PA BAHNHOFSALLEE 1E, GOTTINGEN, 37081, GERMANY
SN 1726-4170
EI 1726-4189
J9 BIOGEOSCIENCES
JI Biogeosciences
PY 2011
VL 8
IS 5
BP 1367
EP 1382
DI 10.5194/bg-8-1367-2011
PG 16
WC Ecology; Geosciences, Multidisciplinary
SC Environmental Sciences & Ecology; Geology
GA 769HK
UT WOS:000291003200023
ER
PT J
AU Schofield, PJ
Peterson, MS
Lowe, MR
Brown-Peterson, NJ
Slack, WT
AF Schofield, Pamela J.
Peterson, Mark S.
Lowe, Michael R.
Brown-Peterson, Nancy J.
Slack, William T.
TI Survival, growth and reproduction of non-indigenous Nile tilapia,
Oreochromis niloticus (Linnaeus 1758). I. Physiological capabilities in
various temperatures and salinities
SO MARINE AND FRESHWATER RESEARCH
LA English
DT Article
DE dispersal; estuary; invasive species; osmoregulation; salinity
ID MAN-MADE LAKES; FRESH-WATER FAUNAS; CLIMATE-CHANGE; COTE-DIVOIRE; NATIVE
BIODIVERSITY; COASTAL MISSISSIPPI; COLD TOLERANCE; FISH; HOMOGENIZATION;
SIZE
AB The physiological tolerances of non-native fishes is an integral component of assessing potential invasive risk. Salinity and temperature are environmental variables that limit the spread of many non-native fishes. We hypothesised that combinations of temperature and salinity will interact to affect survival, growth, and reproduction of Nile tilapia, Oreochromis niloticus, introduced into Mississippi, USA. Tilapia withstood acute transfer from fresh water up to a salinity of 20 and survived gradual transfer up to 60 at typical summertime (30 degrees C) temperatures. However, cold temperature (14 degrees C) reduced survival of fish in saline waters >= 10 and increased the incidence of disease in freshwater controls. Although fish were able to equilibrate to saline waters in warm temperatures, reproductive parameters were reduced at salinities >= 30. These integrated responses suggest that Nile tilapia can invade coastal areas beyond their point of introduction. However, successful invasion is subject to two caveats: (1) wintertime survival depends on finding thermal refugia, and (2) reproduction is hampered in regions where salinities are >= 30. These data are vital to predicting the invasion of non-native fishes into coastal watersheds. This is particularly important given the predicted changes in coastal landscapes due to global climate change and sea-level rise.
C1 [Schofield, Pamela J.] US Geol Survey, SE Ecol Sci Ctr, Gainesville, FL 32653 USA.
[Peterson, Mark S.; Lowe, Michael R.; Brown-Peterson, Nancy J.] Univ So Mississippi, Dept Coastal Sci, Ocean Springs, MS 39564 USA.
[Slack, William T.] USA, ERDC, Waterways Expt Stn EE A, Vicksburg, MS 39180 USA.
RP Schofield, PJ (reprint author), US Geol Survey, SE Ecol Sci Ctr, 7920 NW 71st St, Gainesville, FL 32653 USA.
EM pschofield@usgs.gov
FU US Fish and Wildlife Service (Region 4); USA Geological Survey Invasive
Species Program
FX Funding for this project provided by US Fish and Wildlife Service
(Region 4) and the USA Geological Survey Invasive Species Program.
Thanks to M. E. Brown, D. R. Gregoire and J. N. Langston for their
assistance in the laboratory. Denise Petty and T. Crosby provided
veterinary care and fish-disease diagnoses. Shane Ruessler and B. Lewis
provided technical assistance in the laboratory. Bill Loftus kindly
edited the manuscript for us. We thank two anonymous reviewers for their
comments on an earlier version of the manuscript. Methods for this study
followed 'Guidelines for the Use of Fishes in Research' published by the
American Society of Icthyologists and Herpetologists
(http://www.asih.org/files/fish%20guidelines.doc). This study was
conducted under Institutional Animal Care and Use Committee permit
number USGS/FISC 2007-01. Specimens were collected under an
administrative scientific collecting permit issued to W. T. Slack by
Mississippi Department of Wildlife, Fisheries and Parks - Mississippi
Museum of Natural Science. Any use of trade, product, or firm names is
for descriptive purposes only and does not imply endorsement by the US
Government. Permission to publish was granted by the Chief of Engineers,
US Army Corps of Engineers.
NR 76
TC 13
Z9 14
U1 6
U2 30
PU CSIRO PUBLISHING
PI CLAYTON
PA UNIPARK, BLDG 1, LEVEL 1, 195 WELLINGTON RD, LOCKED BAG 10, CLAYTON, VIC
3168, AUSTRALIA
SN 1323-1650
EI 1448-6059
J9 MAR FRESHWATER RES
JI Mar. Freshw. Res.
PY 2011
VL 62
IS 5
BP 439
EP 449
DI 10.1071/MF10207
PG 11
WC Fisheries; Limnology; Marine & Freshwater Biology; Oceanography
SC Fisheries; Marine & Freshwater Biology; Oceanography
GA 768VC
UT WOS:000290965500003
ER
PT J
AU King, TL
Johnson, RL
AF King, T. L.
Johnson, R. L.
TI Novel tetra-nucleotide microsatellite DNA markers for assessing the
evolutionary genetics and demographics of Northern Snakehead (Channa
argus) invading North America
SO CONSERVATION GENETICS RESOURCES
LA English
DT Article
DE Snakehead; Channa argus; Invasive; Population; Demographics;
Microsatellite; Mutation-drift equilibrium
ID ZAPUS-HUDSONIUS-PREBLEI; ALLELE FREQUENCY DATA; POPULATION BOTTLENECKS;
POTOMAC RIVER; IDENTIFICATION; TESTS; LOCI
AB We document the isolation and characterization of 19 tetra-nucleotide microsatellite DNA markers in northern snakehead (Channa argus) fish that recently colonized Meadow Lake, New York City, New York. These markers displayed moderate levels of allelic diversity (averaging 6.8 alleles/locus) and heterozygosity (averaging 74.2%). Demographic analyses suggested that the Meadow Lake collection has not achieved mutation-drift equilibrium. These results were consistent with instances of deviations from Hardy-Weinberg equilibrium and the presence of some linkage disequilibrium. A comparison of individual pair-wise distances suggested the presence of multiple differentiated groups of related individuals. Results of all analyses are consistent with a pattern of multiple, recent introductions. The microsatellite markers developed for C. argus yielded sufficient genetic diversity to potentially: (1) delineate kinship; (2) elucidate fine-scale population structure; (3) define management (eradication) units; (4) estimate dispersal rates; (5) estimate population sizes; and (6) provide unique demographic perspectives of control or eradication effectiveness.
C1 [King, T. L.; Johnson, R. L.] US Geol Survey, Biol Resources Div, Aquat Ecol Branch, Leetown Sci Ctr, Kearneysville, WV 25430 USA.
RP King, TL (reprint author), US Geol Survey, Biol Resources Div, Aquat Ecol Branch, Leetown Sci Ctr, 11649 Leetown Rd, Kearneysville, WV 25430 USA.
EM tlking@usgs.gov
FU U.S. Geological Survey's (USGS) Leetown Science Center; USGS
FX This research was funded by the U.S. Geological Survey's (USGS) Leetown
Science Center and the USGS Invasive Species Program. The authors wish
to thank Sharon Gross (USGS, Invasive Species Program Coordinator,
Reston, Virginia) for supporting this project. The following scientists
provided tissue samples for marker development: Steve Minkkinen, U.S.
Fish and Wildlife Service, Annapolis, Maryland; John Odenkirk, Virginia
Department of Game and Inland Fisheries, Fredericksburg, Virginia; and
Christine Densmore, USGS, National Fish Health Research Laboratory,
Kearneysville, West Virginia. We are extremely grateful to Melissa
Cohen, New York State Department of Environmental Conservation, New York
City, New York for provided the sample from Meadow Lake.
NR 14
TC 6
Z9 7
U1 1
U2 19
PU SPRINGER
PI DORDRECHT
PA VAN GODEWIJCKSTRAAT 30, 3311 GZ DORDRECHT, NETHERLANDS
SN 1877-7252
J9 CONSERV GENET RESOUR
JI Conserv. Genet. Resour.
PD JAN
PY 2011
VL 3
IS 1
BP 1
EP 4
DI 10.1007/s12686-010-9256-8
PG 4
WC Biodiversity Conservation; Genetics & Heredity
SC Biodiversity & Conservation; Genetics & Heredity
GA 761YE
UT WOS:000290438500001
ER
PT J
AU Galbraith, HS
Wozney, KM
Smith, CM
Zanatta, DT
Wilson, C
AF Galbraith, Heather S.
Wozney, Kristyne M.
Smith, Caleigh M.
Zanatta, David T.
Wilson, Chris
TI Isolation and characterization of microsatellite loci in the freshwater
mussel Lasmigona costata (Bivalvia: Unionoida)
SO CONSERVATION GENETICS RESOURCES
LA English
DT Article
DE Lasmigona costata; Flutedshell mussel; Ontario; Microsatellite;
Population genetics
AB Eleven microsatellite loci for the freshwater mussel Lasmigona costata were isolated and characterized. Genetic screening of individuals from four rivers in southern Ontario confirmed that all loci were highly polymorphic. These loci should prove useful in a range of studies from fine- and coarse-scale population structure and gene flow to reproductive success of individuals.
C1 [Wozney, Kristyne M.; Smith, Caleigh M.; Wilson, Chris] Trent Univ, Ontario Minist Nat Resources, Aquat Res Sect, Peterborough, ON K9J 7B8, Canada.
[Zanatta, David T.] Cent Michigan Univ, Dept Biol, Mt Pleasant, MI 48859 USA.
[Galbraith, Heather S.] Trent Univ, Dept Biol, Peterborough, ON K9J 7B8, Canada.
RP Galbraith, HS (reprint author), US Geol Survey, No Appalachian Res Lab, Wellsboro, PA 16901 USA.
EM hsgspooner@gmail.com
RI Wilson, Chris/J-4851-2012
OI Wilson, Chris/0000-0002-9528-0652
FU Endangered Species Recovery Fund of World Wildlife Fund Canada,
Fisheries and Oceans Canada; Ontario Ministry of Natural Resources
FX This work was made possible through funding from the Endangered Species
Recovery Fund of World Wildlife Fund Canada, Fisheries and Oceans
Canada, and Ontario Ministry of Natural Resources. Friedrich Fischer and
Ryan and Kirsty Hill provided valuable assistance with field sampling.
NR 9
TC 2
Z9 2
U1 1
U2 10
PU SPRINGER
PI DORDRECHT
PA VAN GODEWIJCKSTRAAT 30, 3311 GZ DORDRECHT, NETHERLANDS
SN 1877-7252
J9 CONSERV GENET RESOUR
JI Conserv. Genet. Resour.
PD JAN
PY 2011
VL 3
IS 1
BP 9
EP 11
DI 10.1007/s12686-010-9261-y
PG 3
WC Biodiversity Conservation; Genetics & Heredity
SC Biodiversity & Conservation; Genetics & Heredity
GA 761YE
UT WOS:000290438500003
ER
PT J
AU Inoue, K
Moyer, GR
Williams, A
Monroe, EM
Berg, DJ
AF Inoue, Kentaro
Moyer, Gregory R.
Williams, Ashantye
Monroe, Emy M.
Berg, David J.
TI Isolation and characterization of 17 polymorphic microsatellite loci in
the spectaclecase, Cumberlandia monodonta (Bivalvia: Margaritiferidae)
SO CONSERVATION GENETICS RESOURCES
LA English
DT Article
DE Cumberlandia monodonta; Spectaclecase; Margaritiferidae; Microsatellite
primers
ID AMPLIFICATION; UNIONIDAE; SOFTWARE
AB We isolated 29 microsatellite loci from Cumberlandia monodonta, a freshwater mussel species that has experienced population declines throughout its range. Seventeen loci were polymorphic, with 3-13 alleles, observed heterozygosity values of 0.375-1.00, and 38% of alleles found in more than one population. These loci should be useful for describing population genetic diversity, which will facilitate ongoing conservation efforts for C. monodonta.
C1 [Inoue, Kentaro] Miami Univ, Dept Zool, Oxford, OH 45056 USA.
[Moyer, Gregory R.; Williams, Ashantye] US Fish & Wildlife Serv, Conservat Genet Lab, Warm Springs, GA 31830 USA.
[Monroe, Emy M.] Univ S Dakota, Dept Biol, Vermillion, SD 57069 USA.
[Berg, David J.] Miami Univ, Dept Zool, Hamilton, OH 45011 USA.
RP Inoue, K (reprint author), Miami Univ, Dept Zool, Oxford, OH 45056 USA.
EM inouek@muohio.edu
OI Inoue, Kentaro/0000-0001-6087-3290
NR 16
TC 2
Z9 2
U1 1
U2 8
PU SPRINGER
PI DORDRECHT
PA VAN GODEWIJCKSTRAAT 30, 3311 GZ DORDRECHT, NETHERLANDS
SN 1877-7252
J9 CONSERV GENET RESOUR
JI Conserv. Genet. Resour.
PD JAN
PY 2011
VL 3
IS 1
BP 57
EP 60
DI 10.1007/s12686-010-9289-z
PG 4
WC Biodiversity Conservation; Genetics & Heredity
SC Biodiversity & Conservation; Genetics & Heredity
GA 761YE
UT WOS:000290438500015
ER
PT J
AU Pavlovic, NB
Leicht-Young, SA
AF Pavlovic, Noel B.
Leicht-Young, Stacey A.
TI Are temperate mature forests buffered from invasive lianas?
SO JOURNAL OF THE TORREY BOTANICAL SOCIETY
LA English
DT Article
DE Celastrus orbiculatus; Celastrus scandens; deciduous forests; invasive
plants; Lake Michigan; lianas
ID CELASTRUS-ORBICULATUS; HARDWOOD FOREST; TROPICAL FOREST; DECIDUOUS
FORESTS; TREE REGENERATION; PLANT INVASION; UNITED-STATES; DIVERSITY;
DYNAMICS; ABUNDANCE
AB PAVLOVIC, N. B. AND S. A. LEICHT-YOUNG (U.S. Geological Survey, 1100 N. Mineral Springs Rd., Porter, IN 46304). Are temperate mature forests buffered from invasive lianas? J. Toekev Bur. Soc. 138: 85-92. 2011.-Mature and old-growth forests are often thought to be buffered against invasive species due to low levels of light and infrequent disturbance. Lianas (woody vines) and other climbing plants are also known to exhibit lower densities in older forests. As part of a larger survey of the lianas of the southern Lake Michigan region in mature and old-growth forests, the level of infestation by invasive lianas was evaluated. The only invasive liana detected in these surveys was Celastrus orbiculatus Thunb. (Celastraceae). Although this species had only attached to trees and reached the canopy in a few instances, it was present in 30% of transects surveyed, mostly as a component of the ground layer. Transects with C orbiculatus had higher levels of soil potassium and higher liana richness than transects without. In contrast, transects with the native scandens had higher pH, sand content, and soil magnesium and lower organic matter compared to transects where it was absent. Celastrus orbiculatus appears to be a generalist liana since it often occurs with native lianas. Celastrus orbiculatus poses a substantial threat to mature forests as it will persist in the understory until a canopy gap or other disturbance provides the light and supports necessary for it to ascend to the canopy and damage tree species. As a result, these forests should be monitored by land managers so that C orbiculatus eradication can occur while invasions are at low densities and restricted to the ground layer.
C1 [Pavlovic, Noel B.; Leicht-Young, Stacey A.] US Geol Survey, Great Lakes Sci Ctr, Porter, IN 46304 USA.
RP Pavlovic, NB (reprint author), US Geol Survey, Great Lakes Sci Ctr, 1100 N Mineral Springs Rd, Porter, IN 46304 USA.
EM npavlovic@usgs.gov
NR 51
TC 12
Z9 12
U1 8
U2 33
PU TORREY BOTANICAL SOC
PI LAWRENCE
PA 810 E 10TH ST, LAWRENCE, KS 66044 USA
SN 1095-5674
J9 J TORREY BOT SOC
JI J. Torrey Bot. Soc.
PD JAN-MAR
PY 2011
VL 138
IS 1
BP 85
EP 92
PG 8
WC Plant Sciences
SC Plant Sciences
GA 765IX
UT WOS:000290700000010
ER
PT J
AU Sierra, CA
Harmon, ME
Thomann, E
Perakis, SS
Loescher, HW
AF Sierra, C. A.
Harmon, M. E.
Thomann, E.
Perakis, S. S.
Loescher, H. W.
TI Amplification and dampening of soil respiration by changes in
temperature variability
SO BIOGEOSCIENCES
LA English
DT Article
ID CLIMATE-CHANGE; TERRESTRIAL ECOSYSTEMS; JENSENS INEQUALITY; CARBON;
FLUXES; DECOMPOSITION; DEPENDENCE; FEEDBACKS; RESPONSES; STORAGE
AB Accelerated release of carbon from soils is one of the most important feedbacks related to anthropogenically induced climate change. Studies addressing the mechanisms for soil carbon release through organic matter decomposition have focused on the effect of changes in the average temperature, with little attention to changes in temperature variability. Anthropogenic activities are likely to modify both the average state and the variability of the climatic system; therefore, the effects of future warming on decomposition should not only focus on trends in the average temperature, but also variability expressed as a change of the probability distribution of temperature. Using analytical and numerical analyses we tested common relationships between temperature and respiration and found that the variability of temperature plays an important role determining respiration rates of soil organic matter. Changes in temperature variability, without changes in the average temperature, can affect the amount of carbon released through respiration over the long-term. Furthermore, simultaneous changes in the average and variance of temperature can either amplify or dampen the release of carbon through soil respiration as climate regimes change. These effects depend on the degree of convexity of the relationship between temperature and respiration and the magnitude of the change in temperature variance. A potential consequence of this effect of variability would be higher respiration in regions where both the mean and variance of temperature are expected to increase, such as in some low latitude regions; and lower amounts of respiration where the average temperature is expected to increase and the variance to decrease, such as in northern high latitudes.
C1 [Thomann, E.] Oregon State Univ, Dept Math, Corvallis, OR 97333 USA.
[Perakis, S. S.] US Geol Survey, Forest & Rangeland Ecosyst Sci Ctr, Corvallis, OR 97333 USA.
[Sierra, C. A.] Oregon State Univ, Dept Forest Ecosyst & Soc, Corvallis, OR 97333 USA.
[Loescher, H. W.] Natl Ecol Observ Network, Boulder, CO 80301 USA.
RP Sierra, CA (reprint author), Max Planck Inst Biogeochem, D-07745 Jena, Germany.
EM csierra@bgc-jena.mpg.de
RI Sierra, Carlos/A-5694-2009
OI Sierra, Carlos/0000-0003-0009-4169
FU Eduardo Ruiz Landa Fellowship; Kay and Ward Richardson endowment; NSF
FX Financial support was provided by the Eduardo Ruiz Landa Fellowship and
the Kay and Ward Richardson endowment. Data used in this research was
also supported by funding from the NSF Long-term Ecological Research
(LTER) Program to the H. J. Andrews and Toolik Lake LTER sites. We would
like to thank Claire Phillips and Michael Unsworth for important
comments on previous versions of this manuscript.
NR 35
TC 15
Z9 15
U1 0
U2 11
PU COPERNICUS GESELLSCHAFT MBH
PI GOTTINGEN
PA BAHNHOFSALLEE 1E, GOTTINGEN, 37081, GERMANY
SN 1726-4170
J9 BIOGEOSCIENCES
JI Biogeosciences
PY 2011
VL 8
IS 4
BP 951
EP 961
DI 10.5194/bg-8-951-2011
PG 11
WC Ecology; Geosciences, Multidisciplinary
SC Environmental Sciences & Ecology; Geology
GA 756MV
UT WOS:000290017000010
ER
PT J
AU Twibell, RG
Gannam, AL
Ostrand, SL
Holmes, JSA
Poole, JB
AF Twibell, Ronald G.
Gannam, Ann L.
Ostrand, Susan L.
Holmes, John S. A.
Poole, Jeff B.
TI Altered Growth Rates, Carcass Fatty Acid Concentrations, and Tissue
Histology in First-Feeding Steelhead Fed a Fish-Meal- and Fish-Oil-Free
Diet
SO NORTH AMERICAN JOURNAL OF AQUACULTURE
LA English
DT Article
ID TROUT ONCORHYNCHUS-MYKISS; SALMON SALMO-SALAR; RAINBOW-TROUT;
LIPID-COMPOSITION; PRODUCT QUALITY; VEGETABLE-OILS; SPARUS-AURATA;
REPLACEMENT; PERFORMANCE; DIGESTIBILITY
AB A 12-week feeding trial was conducted to evaluate a fish-meal-free, fish-oil-free diet for use with first-feeding steelhead Oncorhynchus mykiss. The marine-based control diet (marine diet) contained sardine (Sardinops spp.) meal and pollock (Pollachius virens) liver oil as the primary sources of protein and lipid, respectively. The experimental diet (terrestrial diet) contained only terrestrial sources of protein (poultry by-product meal, blood meal, canola, corn gluten, and wheat gluten) and lipid (canola oil and flaxseed oil). Each diet was administered to five replicate groups of first-feeding fry. At the conclusion of the feeding trial, fish that were fed the marine diet exhibited significantly higher weight gain and feed efficiency than fish that were given the terrestrial diet. Survival was not significantly affected by dietary treatment. However, fish that received the terrestrial diet exhibited significantly lower hemoglobin concentration and percent packed cell volume. Histological examination indicated that in comparison with control fish, steelhead that were fed the terrestrial diet exhibited a lesser degree of vacuolation in hepatocytes, mild hypertrophy and hyperplasia of the nephron tubular epithelium, and intracellular vacuolation in epithelium of the pyloric caeca. Carcass crude protein concentration was significantly higher in fish that were fed the marine diet than in fish that were fed the terrestrial diet. After 2 weeks of feeding, steelhead that received the marine diet exhibited significantly higher carcass concentrations of 14:0, 16:0, 16:1, 20:1, 20:5(n-3), 22:5(n-3), and 22:6(n-3) fatty acids but significantly lower carcass concentrations of 18:1, 18:2(n-6), 18:3(n-6), 18:3(n-3), and 20:4(n-6) relative to fish that were given the terrestrial diet. These differences in carcass fatty acid concentrations persisted throughout the feeding trial. Results of this study indicate that the current terrestrial-based diet is not a satisfactory replacement for the standard marine-based diet used with first-feeding steelhead.
C1 [Twibell, Ronald G.; Gannam, Ann L.; Ostrand, Susan L.; Holmes, John S. A.; Poole, Jeff B.] US Fish & Wildlife Serv, Abernathy Fish Technol Ctr, Longview, WA 98632 USA.
RP Twibell, RG (reprint author), US Fish & Wildlife Serv, Abernathy Fish Technol Ctr, 1440 Abernathy Creek Rd, Longview, WA 98632 USA.
EM ronald_twibell@fws.gov
FU Bonneville Power Administration [016522]
FX We thank Joy Evered (U.S. Fish and Wildlife Service [US-FWS], Olympia
Fish Health Center), Sonia Mumford (USFWS, Olympia Fish Health Center),
and John Morrison (USFWS, retired) for conducting the plasma chemistry
analyses and histological work. The findings and conclusions in this
paper are those of the authors and do not necessarily represent the
views of the USFWS. Partial funding for this project was provided by the
Bonneville Power Administration (Contract Number 016522). The use of
trade names does not imply endorsement by the U.S. Government.
NR 42
TC 3
Z9 3
U1 1
U2 10
PU TAYLOR & FRANCIS INC
PI PHILADELPHIA
PA 325 CHESTNUT ST, SUITE 800, PHILADELPHIA, PA 19106 USA
SN 1522-2055
J9 N AM J AQUACULT
JI N. Am. J. Aqualcult.
PY 2011
VL 73
IS 2
BP 230
EP 238
AR PII 937269309
DI 10.1080/15222055.2011.579028
PG 9
WC Fisheries
SC Fisheries
GA 761OS
UT WOS:000290407900007
ER
PT J
AU Wedding, LM
Lepczyk, CA
Pittman, SJ
Friedlander, AM
Jorgensen, S
AF Wedding, Lisa M.
Lepczyk, Christopher A.
Pittman, Simon J.
Friedlander, Alan M.
Jorgensen, Stacy
TI Quantifying seascape structure: extending terrestrial spatial pattern
metrics to the marine realm
SO MARINE ECOLOGY PROGRESS SERIES
LA English
DT Article
DE Seascape ecology; Landscape indices; Landscape metrics; Seascape
structure; Spatial pattern metrics; Spatial scale
ID FISH SPECIES RICHNESS; ROCKY BENTHIC COMMUNITIES; BOOSTED REGRESSION
TREES; REMOTE-SENSING DATA; LANDSCAPE ECOLOGY; REEF FISH; SEAGRASS
LANDSCAPES; ENVIRONMENT; DIVERSITY; DYNAMICS
AB Spatial pattern metrics have routinely been applied to characterize and quantify structural features of terrestrial landscapes and have demonstrated great utility in landscape ecology and conservation planning. The important role of spatial structure in ecology and management is now commonly recognized, and recent advances in marine remote sensing technology have facilitated the application of spatial pattern metrics to the marine environment. However, it is not yet clear whether concepts, metrics, and statistical techniques developed for terrestrial ecosystems are relevant for marine species and seascapes. To address this gap in our knowledge, we reviewed, synthesized, and evaluated the utility and application of spatial pattern metrics in the marine science literature over the past 30 yr (1980 to 2010). In total, 23 studies characterized seascape structure, of which 17 quantified spatial patterns using a 2-dimensional patch-mosaic model and 5 used a continuously varying 3-dimensional surface model. Most seascape studies followed terrestrial-based studies in their search for ecological patterns and applied or modified existing metrics. Only 1 truly unique metric was found (hydrodynamic aperture applied to Pacific atolls). While there are still relatively few studies using spatial pattern metrics in the marine environment, they have suffered from similar misuse as reported for terrestrial studies, such as the lack of a priori considerations or the problem of collinearity between metrics. Spatial pattern metrics offer great potential for ecological research and environmental management in marine systems, and future studies should focus on (1) the dynamic boundary between the land and sea; (2) quantifying 3-dimensional spatial patterns; and (3) assessing and monitoring seascape change.
C1 [Wedding, Lisa M.; Jorgensen, Stacy] Univ Hawaii Manoa, Dept Geog, Honolulu, HI 96822 USA.
[Wedding, Lisa M.; Pittman, Simon J.] Natl Ocean & Atmospher Adm Biogeog Branch, Silver Spring, MD 20910 USA.
[Lepczyk, Christopher A.] Univ Hawaii Manoa, Dept Nat Resources & Environm Management, Honolulu, HI 96822 USA.
[Pittman, Simon J.] Univ Virgin Isl, Ctr Marine Sci, St Thomas, VI 00802 USA.
[Friedlander, Alan M.] US Geol Survey, Hawaii Cooperat Fisheries Res Unit, Honolulu, HI 96822 USA.
RP Wedding, LM (reprint author), Univ Hawaii Manoa, Dept Geog, Saunders Hall 445, Honolulu, HI 96822 USA.
EM wedding@hawaii.edu
FU National Science Foundation [BCS-1003871]; NOAA's Biogeography Branch;
Coral Reef Conservation Program
FX This research was supported by a National Science Foundation
Dissertation Improvement Grant BCS-1003871, NOAA's Biogeography Branch,
and the Coral Reef Conservation Program.
NR 86
TC 33
Z9 33
U1 7
U2 54
PU INTER-RESEARCH
PI OLDENDORF LUHE
PA NORDBUNTE 23, D-21385 OLDENDORF LUHE, GERMANY
SN 0171-8630
J9 MAR ECOL PROG SER
JI Mar. Ecol.-Prog. Ser.
PY 2011
VL 427
BP 219
EP 232
DI 10.3354/meps09119
PG 14
WC Ecology; Marine & Freshwater Biology; Oceanography
SC Environmental Sciences & Ecology; Marine & Freshwater Biology;
Oceanography
GA 749SM
UT WOS:000289489800017
ER
PT J
AU Splinter, DK
Dauwalter, DC
Marston, RA
Fisher, WL
AF Splinter, Dale K.
Dauwalter, Daniel C.
Marston, Richard A.
Fisher, William L.
TI Watershed Morphology of Highland and Mountain Ecoregions in Eastern
Oklahoma
SO PROFESSIONAL GEOGRAPHER
LA English
DT Article
DE ecoregions; Oklahoma; streams; watershed morphology
ID STREAM HABITAT; FISH ASSEMBLAGES; CLASSIFICATION SCHEMES; DRAINAGE
SYSTEMS; GEOMORPHOLOGY; MORPHOMETRY; PATTERNS; TIME; USA
AB The fluvial system represents a nested hierarchy that reflects the relationship among different spatial and temporal scales. Within the hierarchy, larger scale variables influence the characteristics of the next lower nested scale. Ecoregions represent one of the largest scales in the fluvial hierarchy and are defined by recurring patterns of geology, climate, land use, soils, and potential natural vegetation. Watersheds, the next largest scale, are often nested into a single ecoregion and therefore have properties that are indicative of a given ecoregion. Differences in watershed morphology (relief, drainage density, circularity ratio, relief ratio, and ruggedness number) were evaluated among three ecoregions in eastern Oklahoma: Ozark Highlands, Boston Mountains, and Ouachita Mountains. These ecoregions were selected because of their high-quality stream resources and diverse aquatic communities and are of special management interest to the Oklahoma Department of Wildlife Conservation. One hundred thirty-four watersheds in first-through fourth-order streams were compared. Using a nonparametric, two-factor analysis of variance (alpha = 0.05) we concluded that the relief, drainage density, relief ratio, and ruggedness number all changed among ecoregion and stream order, whereas circularity ratio only changed with stream order. Our study shows that ecoregions can be used as a broad-scale framework for watershed management.
C1 [Splinter, Dale K.] Univ Wisconsin, Dept Geog & Geol, Whitewater, WI 53190 USA.
[Dauwalter, Daniel C.; Fisher, William L.] US Geol Survey, Oklahoma Cooperat Fish & Wildlife Res Unit, Stillwater, OK 74078 USA.
[Marston, Richard A.] Kansas State Univ, Dept Geog, Manhattan, KS 66506 USA.
RP Splinter, DK (reprint author), Univ Wisconsin, Dept Geog & Geol, Whitewater, WI 53190 USA.
EM splinted@uww.edu; DDauwalter@tu.org; rmarston@ksu.edu; wlf9@cornell.edu
NR 57
TC 3
Z9 3
U1 0
U2 15
PU ROUTLEDGE JOURNALS, TAYLOR & FRANCIS LTD
PI ABINGDON
PA 4 PARK SQUARE, MILTON PARK, ABINGDON OX14 4RN, OXFORDSHIRE, ENGLAND
SN 0033-0124
EI 1467-9272
J9 PROF GEOGR
JI Prof. Geogr.
PY 2011
VL 63
IS 1
BP 131
EP 143
DI 10.1080/00330124.2010.533575
PG 13
WC Geography
SC Geography
GA 742RF
UT WOS:000288961500008
ER
PT J
AU Sanders, TG
Biddanda, BA
Stricker, CA
Nold, SC
AF Sanders, T. Garrison, Jr.
Biddanda, Bopaiah A.
Stricker, Craig A.
Nold, Stephen C.
TI Benthic macroinvertebrate and fish communities in Lake Huron are linked
to submerged groundwater vents
SO AQUATIC BIOLOGY
LA English
DT Article
DE Stable isotopes; Submerged sinkholes; Groundwater; Food web; Lake Huron
ID DISSOLVED INORGANIC CARBON; ORGANIC-MATTER FLOW; STABLE-ISOTOPE;
FOOD-WEB; ECOLOGICAL SIGNIFICANCE; COASTAL WATERS; SULFUR; NITROGEN;
DELTA-C-13; DISCHARGE
AB Groundwater can be an important source of nutrients and energy to aquatic ecosystems, but quantifying the inputs and biogeochemical importance remains challenging. A series of submerged groundwater vents in northern Lake Huron were examined to determine the linkage between groundwater nutrients and aquatic food webs. We collected samples of key food-web components from groundwater vent and reference habitats and analyzed them for C-13, N-15, and S-34 isotopes. Dissolved inorganic carbon (DIC) in the groundwater was depleted in C-13, while aqueous sulfate was enriched in S-34 (mean differences between groundwater and reference sites were -3.9% and + 12.0%, respectively). Benthic primary producers, macroinvertebrates, and benthivorous fish had significantly lower delta C-13 values in groundwater environments, and benthivorous fish were somewhat depleted (-2.5%) in delta S-34 at groundwater sites compared to reference sites. However, delta N-15 values were not different between groundwater and reference sites, and pelagic components of the ecosystems (plankton and planktivorous and piscivorous fish) were similar in both delta C-13 and delta N-15. These data suggest benthic metazoan communities surrounding groundwater vents are partially linked to groundwater-derived benthic primary production, while planktivorous and piscivorous communities not directly associated with the benthos do not rely on groundwater nutrients.
C1 [Sanders, T. Garrison, Jr.; Biddanda, Bopaiah A.] Grand Valley State Univ, Annis Water Resources Inst, Muskegon, MI 49441 USA.
[Stricker, Craig A.] US Geol Survey, Stable Isotope Lab, DFC, Denver, CO 80225 USA.
[Nold, Stephen C.] Univ Wisconsin Stout, Dept Biol, Menomonie, WI 54751 USA.
RP Sanders, TG (reprint author), Crooked River Watershed Council, 498 SE Lynn Blvd, Prineville, OR 97754 USA.
EM garrysanders@gmail.com
FU National Science Foundation [NSF-MCB 0603944]; Grand Valley State
University; Michigan Space Grant Consortium
FX This work was funded by the National Science Foundation (NSF-MCB 0603944
to B.A.B.), Grand Valley State University, and the Michigan Space Grant
Consortium (to T.G.S.). We are grateful to S. Kendall, E. Strickler, S.
Ruberg, and R. Green, and the dive staff of the NOAA Thunder Bay
National Marine Sanctuary for field assistance. Thanks are also due to
L. Clyburn and the staff and sea cadets on board Noble Odyssey
Foundation's 'Pride of Michigan' for help with field sampling and dive
operations. D. Fielder of the Michigan Department of Natural Resources
assisted with sampling advice for fish. N. Ostrom, P. Ostrom, H. Gandhi,
and C. Cook provided valuable insight into stable isotope analyses.
Peer-review of earlier versions of this manuscript by graduate students
(K. Thomas, J. DeBoer), faculty (N. MacDonald, R. Rediske, and M.
Luttenton) and anonymous Aquatic Biology reviewers helped in making
improvements. The use of any trade, product, or firm names is for
descriptive purposes only and does not imply endorsement by the US
government.
NR 63
TC 10
Z9 10
U1 2
U2 15
PU INTER-RESEARCH
PI OLDENDORF LUHE
PA NORDBUNTE 23, D-21385 OLDENDORF LUHE, GERMANY
SN 1864-7790
EI 1864-7782
J9 AQUAT BIOL
JI Aquat. Biol.
PY 2011
VL 12
IS 1
BP 1
EP 11
DI 10.3354/ab00318
PG 11
WC Marine & Freshwater Biology
SC Marine & Freshwater Biology
GA 746OB
UT WOS:000289255500001
ER
PT J
AU Gaidet, N
Cappelle, J
Takekawa, JY
Iverson, SA
Perry, WM
Douglas, DC
Prosser, DJ
Mundkur, T
Newman, SH
AF Gaidet, Nicolas
Cappelle, Julien
Takekawa, John Y.
Iverson, Samuel A.
Perry, William M.
Douglas, David C.
Prosser, Diann J.
Mundkur, Taej
Newman, Scott H.
TI Potential Spread of Highly Pathogenic Avian Influenza H5N1 by Wildfowl:
Dispersal Ranges and Rates Determined from Large-scale Satellite
Telemetry
SO ECOHEALTH
LA English
DT Meeting Abstract
C1 [Gaidet, Nicolas; Cappelle, Julien] CIRAD, Anim & Integrated Risk Management Unit Agirs, Herault, France.
[Takekawa, John Y.; Iverson, Samuel A.; Perry, William M.] USGS, Western Ecol Res Ctr, Reston, VA 20192 USA.
[Douglas, David C.] USGS Alaska Sci Ctr, Anchorage, AK USA.
[Prosser, Diann J.] USGS, Patuxent Wildlife Res Ctr, Denver, CO USA.
[Mundkur, Taej] Anim Hlth Serv, Infect Dis Grp EMPRES, Wetlands Int, Rome, Italy.
[Mundkur, Taej; Newman, Scott H.] Anim Hlth Serv, Infect Dis Grp EMPRES, FAO, Rome, Italy.
RI Gaidet, Niccolas/H-8122-2013
NR 0
TC 1
Z9 1
U1 0
U2 9
PU SPRINGER
PI NEW YORK
PA 233 SPRING ST, NEW YORK, NY 10013 USA
SN 1612-9202
J9 ECOHEALTH
JI EcoHealth
PY 2011
VL 7
SU 1
BP S35
EP S35
PG 1
WC Biodiversity Conservation; Ecology; Environmental Sciences
SC Biodiversity & Conservation; Environmental Sciences & Ecology
GA 728VB
UT WOS:000287901500054
ER
PT J
AU Alder, JR
Hostetler, SW
Pollard, D
Schmittner, A
AF Alder, J. R.
Hostetler, S. W.
Pollard, D.
Schmittner, A.
TI Evaluation of a present-day climate simulation with a new coupled
atmosphere-ocean model GENMOM
SO GEOSCIENTIFIC MODEL DEVELOPMENT
LA English
DT Article
ID LAST GLACIAL MAXIMUM; ATLANTIC THERMOHALINE CIRCULATION; INTERCOMPARISON
PROJECT PMIP; TRANSFER SCHEME LSX; STOMATAL-RESISTANCE; CARBON-DIOXIDE;
SEA-ICE; SENSITIVITY; GENESIS; CO2
AB We present a new, non-flux corrected AOGCM, GENMOM, that combines the GENESIS version 3 atmospheric GCM (Global Environmental and Ecological Simulation of Interactive Systems) and MOM2 (Modular Ocean Model version 2) nominally at T31 resolution. We evaluate GENMOM by comparison with reanalysis products (e. g., NCEP2) and three models used in the IPCC AR4 assessment. GENMOM produces a global temperature bias of 0.6 degrees C. Atmospheric features such as the jet stream structure and major semi-permanent sea level pressure centers are well simulated as is the mean planetary-scale wind structure that is needed to produce the correct position of stormtracks. Most ocean surface currents are reproduced except where they are not resolvable at T31 resolution. Overall, GENMOM captures reasonably well the observed gradients and spatial distributions of annual surface temperature and precipitation and the simulations are on par with other AOGCMs. Deficiencies in the GENMOM simulations include a warm bias in the surface temperature over the southern oceans, a split in the ITCZ and weaker-than-observed overturning circulation.
C1 [Alder, J. R.; Hostetler, S. W.] Oregon State Univ, Dept Geosci, US Geol Survey, Corvallis, OR 97331 USA.
[Pollard, D.] Penn State Univ, EMS Earth & Environm Syst, University Pk, PA 16802 USA.
[Schmittner, A.] Oregon State Univ, Coll Ocean & Atmospher Sci, Corvallis, OR 97331 USA.
RP Alder, JR (reprint author), Oregon State Univ, Dept Geosci, US Geol Survey, Corvallis, OR 97331 USA.
EM jay.alder@geo.oregonstate.edu
RI Schmittner, Andreas/O-9647-2015;
OI Schmittner, Andreas/0000-0002-8376-0843; Alder, Jay/0000-0003-2378-2853
NR 65
TC 18
Z9 18
U1 0
U2 7
PU COPERNICUS GESELLSCHAFT MBH
PI GOTTINGEN
PA BAHNHOFSALLEE 1E, GOTTINGEN, 37081, GERMANY
SN 1991-959X
J9 GEOSCI MODEL DEV
JI Geosci. Model Dev.
PY 2011
VL 4
IS 1
BP 69
EP 83
DI 10.5194/gmd-4-69-2011
PG 15
WC Geosciences, Multidisciplinary
SC Geology
GA 742AO
UT WOS:000288910700005
ER
PT J
AU Thode, AE
van Wagtendonk, JW
Miller, JD
Quinn, JF
AF Thode, Andrea E.
van Wagtendonk, Jan W.
Miller, Jay D.
Quinn, James F.
TI Quantifying the fire regime distributions for severity in Yosemite
National Park, California, USA
SO INTERNATIONAL JOURNAL OF WILDLAND FIRE
LA English
DT Article
DE burn severity; dNBR; Landsat; RdNBR; Sierra Nevada
ID KLAMATH MOUNTAINS; FOREST STRUCTURE; BURN SEVERITY; LANDSCAPE; PATTERNS;
HISTORY; MANAGEMENT; WILDFIRE; CLIMATE
AB This paper quantifies current fire severity distributions for 19 different fire-regime types in Yosemite National Park, California, USA. Landsat Thematic Mapper remote sensing data are used to map burn severity for 99 fires (cumulatively over 97 000 ha) that burned in Yosemite over a 20-year period. These maps are used to quantify the frequency distributions of fire severity by fire-regime type. A classification is created for the resultant distributions and they are discussed within the context of four vegetation zones: the foothill shrub and woodland zone; the lower montane forest zone; the upper montane forest zone and the subalpine forest zone. The severity distributions can form a building block from which to discuss current fire regimes across the Sierra Nevada in California. This work establishes a framework for comparing the effects of current fires on our landscapes with our notions of how fires historically burned, and how current fire severity distributions differ from our desired future conditions. As this process is refined, a new set of information will be available to researchers and land managers to help understand how fire regimes have changed from the past and how we might attempt to manage them in the future.
C1 [Thode, Andrea E.] No Arizona Univ, Sch Forestry, Flagstaff, AZ 86011 USA.
[van Wagtendonk, Jan W.] US Geol Survey, Western Ecol Res Ctr, Yosemite Field Stn, El Portal, CA 95318 USA.
[Miller, Jay D.] US Forest Serv, Mcclellan, CA 95652 USA.
[Thode, Andrea E.; Quinn, James F.] Univ Calif Davis, Dept Environm Sci & Policy, Davis, CA 95616 USA.
RP Thode, AE (reprint author), No Arizona Univ, Sch Forestry, POB 15018, Flagstaff, AZ 86011 USA.
EM andi.thode@nau.edu
FU Forest Service Pacific Southwest Region; Switzer Foundation
FX This work was funded through the Forest Service Pacific Southwest Region
Fire and Aviation Management Program, and through a fellowship from the
Switzer Foundation. The US Geological Survey-National Park Service Burn
Severity Program was a cooperator and provided the imagery used in this
study. Field data collection would not have been possible without the
help of our field crew members: Emily Kachorek, Aaron Petty, Brian
Strand, Genvieve Belley, Jeremy Frank, Rachel Brush, Glenda Yenni,
Daniel Sweet, Patrick Huber, Tasha Halevi and Jonathan Wooley. A special
thanks goes to Brianna Collins for her field and office efforts in this
work. We thank Mark Schwartz for his review of this work and his advice
in the analysis. Discussions with Neil Sugihara were invaluable in the
development of this study. Any use of trade, product, or firm names in
this publication is for descriptive purposes only and does not imply
endorsement by the US government.
NR 58
TC 25
Z9 25
U1 1
U2 26
PU CSIRO PUBLISHING
PI COLLINGWOOD
PA 150 OXFORD ST, PO BOX 1139, COLLINGWOOD, VICTORIA 3066, AUSTRALIA
SN 1049-8001
J9 INT J WILDLAND FIRE
JI Int. J. Wildland Fire
PY 2011
VL 20
IS 2
BP 223
EP 239
DI 10.1071/WF09060
PG 17
WC Forestry
SC Forestry
GA 741XP
UT WOS:000288900600006
ER
PT J
AU Beeler, NM
Tullis, TE
AF Beeler, N. M.
Tullis, T. E.
TI A Barnes-Hut scheme for simulating fault slip
SO NONLINEAR PROCESSES IN GEOPHYSICS
LA English
DT Article
ID SYNTHETIC SEISMICITY MODELS; AFTERSHOCK SEQUENCES; PHYSICAL MODEL;
EARTHQUAKE NUCLEATION; RECURRENCE INTERVALS; STATIC FATIGUE; TENSILE
FAULTS; HALF-SPACE; FRICTION; STRESS
AB To account for natural spatial and temporal complexity, large-scale, long-duration calculations are required for simulations of seismicity in fault zones that host large earthquakes. Without advances in computational methods, the rate of progress in "earthquake simulator" models and associated earthquake forecasts is limited by the rates at which computer speed and storage increase. To explore improvements in computational efficiency we develop the first implementation of the Barnes-Hut algorithm (Barnes and Hut, 1986) to calculate elastic interactions in a fault model. The Barnes-Hut method is an efficient, numerical scheme that treats local forces exactly and distant forces approximately. The approach is illustrated in example simulations of nonlinear fault strength in plane strain. Rudimentary error analysis indicates that efficient calculations, where execution time scales with number of grid points (N) as N log N, can be conducted routinely with errors on the order of 0.1%. We expect the Barnes-Hut method to be well suited for conducting initial exploration of parameter space for fault simulations with non-linear constitutive equations, and for efficient calculations of stress interaction in complex fault systems.
C1 [Beeler, N. M.] US Geol Survey, Cascades Observ, Vancouver, WA 98683 USA.
[Tullis, T. E.] Brown Univ, Providence, RI 02912 USA.
RP Beeler, NM (reprint author), US Geol Survey, Cascades Observ, Vancouver, WA 98683 USA.
EM nbeeler@usgs.gov
FU Southern California Earthquake Center; NASA; US Geological Survey
Venture Capital Fund
FX This study was supported by Southern California Earthquake Center and
NASA Earth Science program through grants to Terry Tullis of Brown
University, and by the US Geological Survey Venture Capital Fund.
Calculations used USGS and NASA computing facilities with technical
advice and programming assistance from Larry Baker (USGS/EHZ) and Art
Lanzanoff (NASA Ames). Thanks to Andrea Donnellean of NASA/JPL for
support. This study followed from a collaboration by the authors with
John Salmon. The wavenumber domain plane strain program used to verify
errors in the BH solutions was written by Allan Rubin. Conversations
with Allan provided insights on nucleation and recurrence that informed
the example simulations. This paper was greatly improved in response to
reviews by Ruth Harris, Steve Schilling, Mike Poland, Brad Aagaard,
Keith Richards-Dinger, Gregor Hillers and the NPG editor Bruce Malamud.
NR 63
TC 0
Z9 0
U1 1
U2 5
PU COPERNICUS GESELLSCHAFT MBH
PI GOTTINGEN
PA BAHNHOFSALLEE 1E, GOTTINGEN, 37081, GERMANY
SN 1023-5809
J9 NONLINEAR PROC GEOPH
JI Nonlinear Process Geophys.
PY 2011
VL 18
IS 2
BP 133
EP 146
DI 10.5194/npg-18-133-2011
PG 14
WC Geochemistry & Geophysics; Meteorology & Atmospheric Sciences
SC Geochemistry & Geophysics; Meteorology & Atmospheric Sciences
GA 742AV
UT WOS:000288911400001
ER
PT J
AU Duffy, WG
Bjorkstedt, EP
Ellings, CS
AF Duffy, Walter G.
Bjorkstedt, Eric P.
Ellings, Christopher S.
TI Predation on Juvenile Pacific Salmon Oncorhynchus spp. in Downstream
Migrant Traps in Prairie Creek, California
SO NORTH AMERICAN JOURNAL OF FISHERIES MANAGEMENT
LA English
DT Article
ID MARK-RECAPTURE ESTIMATION; COHO SALMON; CUTTHROAT TROUT; SMOLT
POPULATION; ATLANTIC SALMON; LIFE-HISTORY; SURVIVAL; KISUTCH;
WASHINGTON; HABITAT
AB Downstream migrant traps are a widely applied fishery management tool for sampling anadromous Pacific salmon Oncorhynchus spp. and steelhead O. mykiss smolts along the West Coast of North America and elsewhere, yet predation on juvenile salmonids in traps has not been studied quantitatively. We assessed the frequency of occurrence and abundance of juvenile salmonids in the stomachs of coastal cutthroat trout O. clarkii clarkii, coho salmon O. kisutch, steelhead, and prickly sculpin Cottus asper (> 70 mm fork length) captured in traps and in nearby stream habitats. All four predator species took juvenile salmonids with much greater frequency in traps than in stream habitats. Among free-swimming predators, only coastal cutthroat trout were observed with salmonid fry in their stomachs, but they took fewer salmonid prey and appeared to rely more heavily on insect prey than did coastal cutthroat trout captured in traps. Predators consumed up to 25% of the available prey over a broad range of prey abundances. Over the course of the study, predators consumed 2.5% of all salmonid fry captured in traps, but this fraction ranged from less than 1% to more than 10% in any given year. The number of prey taken in traps increased with predator length and with prey abundance in traps, and predation in traps peaked during the period of most intense downstream migration by salmon fry. In contrast, live-box design and trap location had little or no effect on the total number of prey taken by individual predators. We estimated that the predation mortality of juvenile salmon increased by 0.5-1.0% due to in-trap predation (i.e., a 9-10% relative increase over natural predation rates). We found no evidence that predators selected for prey on the basis of species. These results should motivate additional research on methods that reduce or eliminate predation in trap live-boxes and protocols for efficiently measuring predation associated with the trapping of downstream migrants.
C1 [Duffy, Walter G.] Humboldt State Univ, US Geol Survey, Calif Cooperat Fish Res Unit, Arcata, CA 95521 USA.
[Bjorkstedt, Eric P.] Humboldt State Univ, Natl Ocean & Atmospher Adm Fisheries, Fisheries Ecol Div, SW Fisheries Sci Ctr, Arcata, CA 95521 USA.
[Bjorkstedt, Eric P.] Humboldt State Univ, Dept Fisheries Biol, Arcata, CA 95521 USA.
[Ellings, Christopher S.] Nisqually Indian Tribe, Nat Resources, Olympia, WA 98513 USA.
RP Duffy, WG (reprint author), Humboldt State Univ, US Geol Survey, Calif Cooperat Fish Res Unit, 1 Harpst St, Arcata, CA 95521 USA.
EM walter.duffy@humboldt.edu
FU Fisheries Ecology Division (National Oceanic and Atmospheric
Administration, National Marine Fisheries Service, Southwest Fisheries
Science Center); California Department of Fish and Game
FX We thank Bethany Reisburger for help with field data collection and
Rosemary Records for assistance with Figure 1. Barry Collins, Michael
Sparkman, Brian Spence, Tommy Williams, and several anonymous reviewers
provided comments that greatly improved the manuscript. Partial funding
for this research was provided by the Fisheries Ecology Division
(National Oceanic and Atmospheric Administration, National Marine
Fisheries Service, Southwest Fisheries Science Center) and by the
California Department of Fish and Game. The use of trade or firm names
in this paper is for reader information only and does not imply
endorsement by the U.S. Government of any product or service. This is
Contribution Number 1028 of the Fisheries Ecology Division of the
National Marine Fisheries Service, Southwest Fisheries Science Center.
NR 41
TC 0
Z9 0
U1 1
U2 6
PU TAYLOR & FRANCIS INC
PI PHILADELPHIA
PA 530 WALNUT STREET, STE 850, PHILADELPHIA, PA 19106 USA
SN 0275-5947
EI 1548-8675
J9 N AM J FISH MANAGE
JI North Am. J. Fish Manage.
PY 2011
VL 31
IS 1
BP 151
EP 164
DI 10.1080/02755947.2011.562752
PG 14
WC Fisheries
SC Fisheries
GA 742QR
UT WOS:000288960000003
ER
PT J
AU Chalupnicki, MA
Ketola, HG
Starliper, CE
Gallagher, D
AF Chalupnicki, Marc A.
Ketola, H. George
Starliper, Clifford E.
Gallagher, Dennis
TI Efficacy and Toxicity of Iodine Disinfection of Atlantic Salmon Eggs
SO NORTH AMERICAN JOURNAL OF AQUACULTURE
LA English
DT Article
ID FALL CHINOOK SALMON; FLOW TRAY INCUBATORS; RAINBOW-TROUT EGGS; 2
IODOPHORS; BACTERIAL-POPULATIONS; SURFACE DISINFECTION; AEROMONAS;
IDENTIFICATION; GAIRDNERI; FORMALIN
AB Recent interest in the restoration of Atlantic salmon Salmo salar in the Great Lakes has given rise to new culture techniques and management programs designed to reduce pathogen transmission while stabilizing and enhancing wild populations. We examined the toxicity of iodine to Atlantic salmon eggs and its effectiveness as a disinfectant against bacteria on egg surfaces. We spawned and fertilized eight gravid Atlantic salmon from Cayuga Lake, New York, and exposed their eggs to 10 concentrations of iodine (5, 10, 50, 75, 100, 500, 750, 1,000, 5,000, and 7,500 mg/L) for 30 min during water hardening. An additional subsample of unfertilized eggs was also exposed to some of the same concentrations of iodine (5, 10, 50, 75, and 100 mg/L) to determine the efficiency of disinfection. Viable eggs were only obtained from four females. Survival of eggs to the eyed stage and hatch tended to be reduced at iodine concentrations of 50 and 75 mg/L and was significantly reduced at concentrations of 100 mg/L iodine or more. We calculated the concentrations of iodine that killed 50% of the Atlantic salmon eggs at eye-up and hatch to be 175 and 85 mg/L, respectively. Aeromonas veronii, A. schubertii, A. hydrophila, A. caviae, Plesiomonas shiggeloides, and Citrobacter spp. were the predominant bacteria present on the surface of green eggs and were significantly reduced by an iodine immersion. The use of iodine as a disinfectant on Atlantic salmon eggs was effective at low concentrations (50-75 mg/L), for which toxicity to Atlantic salmon was minimal.
C1 [Chalupnicki, Marc A.; Ketola, H. George] US Geol Survey, Great Lakes Sci Ctr, Tunison Lab Aquat Sci, Cortland, NY 13045 USA.
[Starliper, Clifford E.] US Geol Survey, Natl Fish Hlth Res Lab, Leetown Sci Ctr, Kearneysville, WV 25430 USA.
[Gallagher, Dennis] Cortland High Sch, Cortland, NY 13045 USA.
RP Chalupnicki, MA (reprint author), US Geol Survey, Great Lakes Sci Ctr, Tunison Lab Aquat Sci, 3075 Gracie Rd, Cortland, NY 13045 USA.
EM mchalupnicki@usgs.go
NR 44
TC 3
Z9 3
U1 0
U2 7
PU TAYLOR & FRANCIS INC
PI PHILADELPHIA
PA 325 CHESTNUT ST, SUITE 800, PHILADELPHIA, PA 19106 USA
SN 1522-2055
J9 N AM J AQUACULT
JI N. Am. J. Aqualcult.
PY 2011
VL 73
IS 2
BP 124
EP 128
AR PII 934642508
DI 10.1080/15222055.2011.559865
PG 5
WC Fisheries
SC Fisheries
GA 734LS
UT WOS:000288336200006
ER
PT J
AU Honeyfield, DC
Kindschi, GA
Bell, TA
Mohler, JW
AF Honeyfield, Dale C.
Kindschi, Greg A.
Bell, Thomas A.
Mohler, Jerre W.
TI Dietary Calcein Marking of Shovelnose Sturgeon and the Effect of
Sunlight on Mark Retention
SO NORTH AMERICAN JOURNAL OF AQUACULTURE
LA English
DT Article
ID ALIZARIN RED-S; ATLANTIC SALMON; OSMOTIC INDUCTION; YELLOW PERCH; MASS
MARKING; OXYTETRACYCLINE; SCALES; TROUT; FRY
AB Calcein, a fluorochrome dye, is a potential fish-marking agent that has not been evaluated in sturgeon. Shovelnose sturgeon Scaphirhynchus platorynchus (average weight, 9.7 g) were fed calcein, immersed in a calcein bath, or left unmarked to determine calcein mark intensity. In the first study, six treatments were evaluated in a two-by-three factorial arrangement. Feed was formulated with 2.0 g of SE-MARK/kg either as powder or in an encapsulated form. Sturgeon were fed the test diets for 5, 10, or 15 d. They readily ate feed containing powdered or encapsulated calcein. Sturgeon fed powdered calcein had more brilliant marks than those fed encapsulated calcein (8.27 versus 4.66 lm; P 0.03) 6 months postexposure. Fish fed calcein for 15 d (11.26 lm) were more brilliant (P 0.002) than fish fed for either 5 d (3.02 lm) or 10 d (5.11 lm). Post hoc comparison of the three treatment groups showed that sturgeon fed powdered calcein for 15 d (14.06 lm) were brighter (P 0.01) than fish fed encapsulated calcein (8.46 lm) or fish immersed in calcein (9.68 lm). In the second study, previously marked sturgeon were exposed to sunlight for 14 months to determine their retention of calcein marks. Dorsal marks were no longer visible on fish exposed to 100% sunlight after 8 weeks. Most but not all fish exposed to 20% sunlight had no discernable dorsal marks after 8 weeks, but ventral marks at the pectoral fin girdle were present on all fish in the 0% and 20% sunlight exposure treatments. Feeding calcein for 15 d appears to have excellent potential for practical application, such as distinguishing hatchery-reared from wild fish. Ventral calcein marks remained visible after 14 months of exposure to 20% sunlight when sturgeon were reared in clear water.
C1 [Honeyfield, Dale C.] US Geol Survey, No Appalachian Res Lab, Wellsboro, PA 16901 USA.
[Bell, Thomas A.] US Fish & Wildlife Serv, Aquat Anim Drug Approval Partnership Program, Bozeman, MT 59715 USA.
[Mohler, Jerre W.] US Fish & Wildlife Serv, Lamar Fish Technol Ctr, NE Fishery Ctr, Lamar, PA 16848 USA.
RP Kindschi, GA (reprint author), 505 N Valley Dr, Bozeman, MT 59718 USA.
EM gandckindschi@msn.com
FU SE-MARK calcein; Bozeman Fish Technology Center
FX We would like to thank a number of people for their support in
conducting these studies: Frederic Barrows, Linda Beck, John Borkowski,
James Bowker, Molly Bowman, and the Aquatic Animal Drug Approval
Partnership. We would also like to thank Daniel Carty, Miranda Dotson,
Dave Erdahl, John W. Fletcher, William C. Fraser, Jason Frost, Jason
Ilgen, Kevin Kappenman, Tom Kehler, Wesley Orr, Ron and LeAnn Secor,
Matthew Toner, and Aquatic Life Sciences, Inc., for technical assistance
and donation of SE-MARK calcein and the Bozeman Fish Technology Center
for their staff and facility support. Any use of trade, product, or firm
names is for descriptive purposes only and does not imply endorsement by
the U.S. government.
NR 21
TC 3
Z9 3
U1 0
U2 9
PU TAYLOR & FRANCIS INC
PI PHILADELPHIA
PA 325 CHESTNUT ST, SUITE 800, PHILADELPHIA, PA 19106 USA
SN 1522-2055
J9 N AM J AQUACULT
JI N. Am. J. Aqualcult.
PY 2011
VL 73
IS 2
BP 129
EP 134
AR PII 934636189
DI 10.1080/15222055.2011.559869
PG 6
WC Fisheries
SC Fisheries
GA 734LS
UT WOS:000288336200007
ER
PT J
AU Dicataldo, G
Johnson, WP
Naftz, DL
Hayes, DF
Moellmer, WO
Miller, T
AF Dicataldo, Gennaro
Johnson, William P.
Naftz, David L.
Hayes, Donald F.
Moellmer, William O.
Miller, Theron
TI Diel variation of selenium and arsenic in a wetland of the Great Salt
Lake, Utah
SO APPLIED GEOCHEMISTRY
LA English
DT Article
ID USA; MONTANA; ADSORPTION; MERCURY; SYSTEM; STREAM; FRACTIONATION;
DESORPTION; SPECIATION; CHEMISTRY
AB Diel (24-h) changes in Se and As concentrations in a freshwater wetland pond bordering the Great Salt Lake (GSL) were examined. Selenium concentrations (filtered and unfiltered) changed on a diel basis, i.e., were depleted during early morning and enriched during daytime over August 17-18. During the May 24-25, 2006 and September 29-30 diel studies, no significant 24-h trends were observed in Se concentrations compared to August, which showed daily maximums up to 59% greater than the daily minimum. Both filtered and unfiltered As concentrations also varied on a diel cycle, with increased concentrations during early morning and decreased concentrations during daytime. Filtered As concentrations increased 110% during the May 24-25, 2006 diel study. Selenium varied in phase with pH, dissolved O(2) (DO), and water temperature (T(w)) whereas As varied opposite to Se, pH, DO and T(w). Changes in pH. DO and T(w) showed a direct linear correlation (r = 0.74, 0.75, and 0.55, respectively) to filtered Se. Also pH, DO and T(w) were inversely correlated to filtered As concentration (r = -0.88, -0.87, and -0.84, respectively). Equilibrium geochemical speciation and sorption models were used to examine the potential oxidation state changes in Se and As, and sorption and desorption reactions corresponding to the observed 24-h variations in pe and pH. In this wetland it was postulated that diel Se variation was driven by sorption and desorption due to photosynthesis-induced changes in pH and redox conditions. Diel variations of As were hypothesized to be linked to pH-driven sorption and desorption as well as co-precipitation and co-dissolution with mineral phases of Mn. (C) 2010 Elsevier Ltd. All rights reserved.
C1 [Johnson, William P.] Univ Utah, Dept Geol & Geophys, Salt Lake City, UT 84112 USA.
[Dicataldo, Gennaro] Ward Engn Grp, Salt Lake City, UT 84101 USA.
[Naftz, David L.] US Geol Survey, Salt Lake City, UT 84119 USA.
[Hayes, Donald F.] Univ Louisiana Lafayette, Dept Civil Engn, Lafayette, LA 70504 USA.
[Moellmer, William O.] Moellmer & Associate, Kearns, UT 84118 USA.
[Miller, Theron] Jordan River Farmington Bay Water Qual Council, W Bountiful, UT 84087 USA.
RP Johnson, WP (reprint author), Univ Utah, Dept Geol & Geophys, 135 S 1460 E, Salt Lake City, UT 84112 USA.
EM william.johnson@utah.edu
RI Johnson, William/G-7733-2011
FU Utah Division of Water Quality; US EPA
FX The authors thank the Utah Division of Water Quality, and the US EPA for
the funds and equipment. Thanks to the UPH and Central Davis Sewer
District, for the use of the laboratories, and equipment, and the ADC
for providing the study site.
NR 43
TC 7
Z9 7
U1 1
U2 12
PU PERGAMON-ELSEVIER SCIENCE LTD
PI OXFORD
PA THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND
SN 0883-2927
J9 APPL GEOCHEM
JI Appl. Geochem.
PD JAN
PY 2011
VL 26
IS 1
BP 28
EP 36
DI 10.1016/j.apgeochem.2010.10.011
PG 9
WC Geochemistry & Geophysics
SC Geochemistry & Geophysics
GA 717NM
UT WOS:000287054700003
ER
PT J
AU Sauer, JR
Link, WA
AF Sauer, John R.
Link, William A.
TI ANALYSIS OF THE NORTH AMERICAN BREEDING BIRD SURVEY USING HIERARCHICAL
MODELS
SO AUK
LA English
DT Article
DE birds; hierarchical model; indices; North American Breeding Bird Survey;
population trend
ID POPULATION-CHANGE; CERULEAN WARBLERS; DECLINES
AB We analyzed population change for 420 bird species from the North American Breeding Bird Survey (BBS) using a hierarchical log-linear model and compared the results with those obtained through route-regression analysis. Survey-wide trend estimates based on the hierarchical model were generally more precise than estimates from the earlier analysis. No consistent pattern of differences existed in the magnitude of trends between the analysis methods. Survey-wide trend estimates changed substantially for 15 species between route-regression and hierarchical-model analyses. We compared regional estimates for states, provinces, and Bird Conservation Regions; differences observed in these regional analyses are likely a consequence of the route-regression procedure's inadequate accommodation of temporal differences in survey effort. We used species-specific hierarchical-model results to estimate composite change for groups of birds associated with major habitats and migration types. Grassland, aridland, and eastern-forest-obligate bird species declined, whereas urban-suburban species increased over the interval 1968-2008. No migration status group experienced significant changes, although Nearctic-Neotropical migrant species showed intervals of decline and permanent resident species increased almost 20% during the interval. Hierarchical-model results better portrayed patterns of population change over time than route-regression results. We recommend use of hierarchical models for BBS analyses. Received 2 November 2009, accepted 10 September 2010.
C1 [Sauer, John R.; Link, William A.] US Geol Survey, Patuxent Wildlife Res Ctr, Laurel, MD 20708 USA.
RP Sauer, JR (reprint author), US Geol Survey, Patuxent Wildlife Res Ctr, 12100 Beech Forest Rd, Laurel, MD 20708 USA.
EM jrsauer@usgs.gov
NR 26
TC 76
Z9 79
U1 6
U2 96
PU AMER ORNITHOLOGISTS UNION
PI LAWRENCE
PA ORNITHOLOGICAL SOC NORTH AMER PO BOX 1897, LAWRENCE, KS 66044-8897 USA
SN 0004-8038
EI 1938-4254
J9 AUK
JI AUK
PD JAN
PY 2011
VL 128
IS 1
BP 87
EP 98
DI 10.1525/auk.2010.09220
PG 12
WC Ornithology
SC Zoology
GA 733CJ
UT WOS:000288237700010
ER
PT J
AU Hart, PJ
Woodworth, BL
Camp, RJ
Turner, K
McClure, K
Goodall, K
Henneman, C
Spiegel, C
LeBrun, J
Tweed, E
Samuel, M
AF Hart, Patrick J.
Woodworth, Bethany L.
Camp, Richard J.
Turner, Kathryn
McClure, Katherine
Goodall, Katherine
Henneman, Carlene
Spiegel, Caleb
LeBrun, Jaymi
Tweed, Erik
Samuel, Michael
TI TEMPORAL VARIATION IN BIRD AND RESOURCE ABUNDANCE ACROSS AN ELEVATIONAL
GRADIENT IN HAWAII
SO AUK
LA English
DT Article
DE bird density; ecological trap; flower density; flower phenology;
Hawaiian Honeycreeper; Metrosideros polymorpha; nectarivore
ID COSTA-RICA; ECOLOGICAL TRAPS; AVIAN MALARIA; FORESTS; AVAILABILITY;
CONSEQUENCES; CONSERVATION; MOVEMENTS; MIGRATION; DYNAMICS
AB We documented patterns of nectar availability and nectarivorous bird abundance over similar to 3 years at nine study sites across an 1,800-m elevational gradient on Hawaii Island to investigate the relationship between resource variation and bird abundance. Flower density (flowers ha(-1)) and nectar energy content were measured across the gradient for the monodominant 'Ohi'a (Metrosideros polymorpha). Four nectarivorous bird species were captured monthly in mist nets and surveyed quarterly with point-transect distance sampling at each site to examine patterns of density and relative abundance. Flowering peaks were associated with season but not rainfall or elevation. Bird densities peaked in the winter and spring of each year at high elevations, but patterns were less clear at middle and low elevations. Variability in bird abundance was generally best modeled as a function of elevation, season, and flower density, but the strength of the latter effect varied with species. The low elevations had the greatest density of flowers but contained far fewer individuals of the two most strongly nectarivorous species. There is little evidence of large-scale altitudinal movement of birds in response to 'Ohi'a flowering peaks. The loose relationship between nectar and bird abundance may be explained by a number of potential mechanisms, including (1) demographic constraints to movement; (2) nonlimiting nectar resources; and (3) the presence of an "ecological trap," whereby birds are attracted by the high resource abundance of, but suffer increased mortality at, middle and low elevations as a result of disease. Received 10 February 2010, accepted 21 October 2010.
C1 [Hart, Patrick J.; Camp, Richard J.; Turner, Kathryn; McClure, Katherine; Goodall, Katherine; Henneman, Carlene; Spiegel, Caleb; LeBrun, Jaymi; Tweed, Erik] Univ Hawaii Hilo, Hawaii Cooperat Studies Llnit, Hilo, HI 96718 USA.
[Samuel, Michael] US Geol Survey, Biol Resources Discipline, Wisconsin Cooperat Wildlife Res Llnit, Madison, WI 53706 USA.
RP Hart, PJ (reprint author), Univ Hawaii, Dept Biol, 200 W Kawili St, Hilo, HI 96720 USA.
EM pjhart@hawaii.edu
OI Camp, Richard/0000-0001-7008-923X
FU National Science Foundation [DEB 0083944]; U.S. Geological Survey
FX We thank Kamehameha Schools, Hawai'i Volcanoes National Park, and
Hawai'i Division of Forestry and Wildlife for permission to work on
their properties. We thank our colleagues on the Biocomplexity of
Introduced Avian Diseases in Hawai'i research group, particularly J.
Ahumada, D. LaPointe, C. Atkinson, S. Jarvi, P. Banko, and D. Duffy, for
critical insight and collaboration, and W. Steiner and D. Helweg for
support. This work would not have been possible without the help of many
volunteer field assistants, and we are grateful for their hard work,
patience, and ability to work long hours in the field under sometimes
adverse conditions (including sharp lava, dense mosquitoes, tropical
storms, deep earth cracks, and vandals). This study was supported by
National Science Foundation Grant DEB 0083944 and by the U.S. Geological
Survey Invasive Species and Wildlife and Terrestrial Resources programs.
NR 51
TC 11
Z9 11
U1 2
U2 44
PU AMER ORNITHOLOGISTS UNION
PI LAWRENCE
PA ORNITHOLOGICAL SOC NORTH AMER PO BOX 1897, LAWRENCE, KS 66044-8897 USA
SN 0004-8038
EI 1938-4254
J9 AUK
JI AUK
PD JAN
PY 2011
VL 128
IS 1
BP 113
EP 126
DI 10.1525/auk.2011.10031
PG 14
WC Ornithology
SC Zoology
GA 733CJ
UT WOS:000288237700012
ER
PT J
AU Limburg, KE
Hughes, RM
Jackson, DC
Czech, B
AF Limburg, Karin E.
Hughes, Robert M.
Jackson, Donald C.
Czech, Brian
TI Human Population Increase, Economic Growth, and Fish Conservation:
Collision Course or Savvy Stewardship?
SO FISHERIES
LA English
DT Editorial Material
ID WESTERN US STREAMS; BIOTIC INTEGRITY; UNITED-STATES; DIADROMOUS FISHES;
FRESH-WATER; BIODIVERSITY; MARINE; POLICY; RIVERS; ECOSYSTEMS
AB Globally, fishes and fisheries are in severe decline, driven in large part by economic and human population growth. Despite progress in environmental philosophies, legislation, and protection, conflicts between economic/human population growth and fish conservation remain and are intensifying at continental and global scales. The growth of the human enterprise ad infinitum is impossible because of dependence on finite resources; hence policies should leave a margin of error when dealing with the biophysical environment. We suggest a re-definition of Earth stewardship to serve as a conceptual bridge between ecology and economics, recognizing the hubris behind most economic models, which assume that the biosphere is a subset of the economy or else an externality, when in fact Homo sapiens is a species operating within the biosphere. Additional indicators that focus on a different suite of values (e.g., social justice, corporate responsibility, and ethics) would underscore the complexity of economic and human population growth effects on societies and ecosystems, and could help guide us away from unsustainable actions toward those that are osavviero in terms of co-existence with the resources upon which we depend.
C1 [Limburg, Karin E.] SUNY Syracuse, Coll Environm Sci & Forestry, Syracuse, NY USA.
[Hughes, Robert M.] Oregon State Univ, Dept Fisheries & Wildlife, Corvallis, OR 97331 USA.
[Hughes, Robert M.] Univ Fed Lavras, Lab Fish Biol, Lavras, MG, Brazil.
[Jackson, Donald C.] Mississippi State Univ, Dept Wildlife & Fisheries, Mississippi State, MS 39762 USA.
[Czech, Brian] US Fish & Wildlife Serv, Arlington, VA USA.
RP Limburg, KE (reprint author), SUNY Syracuse, Coll Environm Sci & Forestry, Syracuse, NY USA.
EM klimburg@esf.edu
RI Limburg, Karin/M-8380-2013
NR 69
TC 22
Z9 22
U1 2
U2 34
PU AMER FISHERIES SOC
PI BETHESDA
PA 5410 GROSVENOR LANE SUITE 110, BETHESDA, MD 20814-2199 USA
SN 0363-2415
J9 FISHERIES
JI Fisheries
PD JAN
PY 2011
VL 36
IS 1
BP 27
EP 34
AR PII 933540106
DI 10.1577/03632415.2011.10389053
PG 8
WC Fisheries
SC Fisheries
GA 733LT
UT WOS:000288264900004
ER
PT J
AU Bury, RB
AF Bury, R. Bruce
TI Modifications of Traps to Reduce Bycatch of Freshwater Turtles
SO JOURNAL OF WILDLIFE MANAGEMENT
LA English
DT Article
DE bycatch; flotation devices; fyke traps; hoop traps; mortality; turtles
ID DIAMONDBACK TERRAPIN; MALACLEMYS-TERRAPIN; CRAB POTS; POPULATIONS;
MORTALITY; CAPTURE; DEVICES; AMPHIBIANS; REPTILES; HABITAT
AB Mortality of freshwater turtles varies among types and deployments of traps. There are few or no losses in hoop or fyke traps set where turtles may reach air, including placement in shallows, addition of floats on traps, and tying traps securely to a stake or to shore. Turtle mortality occurs when traps are set deep, traps are checked at intervals >1 day, and when turtles are captured as bycatch. Devices are available that exclude turtles from traps set for crab or game fish harvest. Slotted gates in front of the trap mouth reduce turtle entry, but small individuals still may be trapped. Incidental take of turtles is preventable by integrating several designs into aquatic traps, such as adding floats to the top of traps so turtles may reach air or an extension tube (chimney, ramp) that creates an escape route. (C) 2011 The Wildlife Society.
C1 US Geol Survey, Forest & Rangeland Ecosyst Sci Ctr, Corvallis, OR 97331 USA.
RP Bury, RB (reprint author), US Geol Survey, Forest & Rangeland Ecosyst Sci Ctr, 3200 SW Jefferson Way, Corvallis, OR 97331 USA.
EM buryb@usgs.gov
NR 42
TC 12
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U1 2
U2 14
PU WILEY-BLACKWELL
PI MALDEN
PA COMMERCE PLACE, 350 MAIN ST, MALDEN 02148, MA USA
SN 0022-541X
J9 J WILDLIFE MANAGE
JI J. Wildl. Manage.
PD JAN
PY 2011
VL 75
IS 1
BP 3
EP 5
DI 10.1002/jwmg.31
PG 3
WC Ecology; Zoology
SC Environmental Sciences & Ecology; Zoology
GA 729GR
UT WOS:000287937200002
ER
PT J
AU Adams, MJ
Pearl, CA
Galvan, S
McCreary, B
AF Adams, Michael J.
Pearl, Christopher A.
Galvan, Stephanie
McCreary, Brome
TI Non-Native Species Impacts on Pond Occupancy by an Anuran
SO JOURNAL OF WILDLIFE MANAGEMENT
LA English
DT Article
DE bullfrogs; colonization; fish; local extinction; non-native species;
northern red-legged frog; occupancy; Rana aurora; wetlands
ID BULLFROGS RANA-CATESBEIANA; ESTIMATING SITE OCCUPANCY; RED-LEGGED FROGS;
INTRODUCED BULLFROGS; AMPHIBIAN OCCURRENCE; DECLINE; OREGON; MITIGATION;
WASHINGTON; INVASION
AB Non-native fish and bullfrogs (Lithobates catesbeianus) are frequently cited as contributing to the decline of ranid frogs in the western United States, so we hypothesized that non-native species, habitat, or a combination of these relate to the probability of local extinction for northern red-legged frogs (Rana aurora) in Oregon, USA. We also hypothesized that the probability of colonization relates to land use, wetland size, or riparian forest. In a 5-yr study, we found no support for an effect of non-native species on northern red-legged frogs. Instead, probability of local extinction decreased with the extent of emergent vegetation and riparian forest. This finding suggests that managers consider the role of habitat when confronting non-native species problems. (C) 2011 The Wildlife Society.
C1 [Adams, Michael J.; Pearl, Christopher A.; Galvan, Stephanie; McCreary, Brome] US Geol Survey, Forest & Rangeland Ecosyst Sci Ctr, Corvallis, OR 97331 USA.
RP Adams, MJ (reprint author), US Geol Survey, Forest & Rangeland Ecosyst Sci Ctr, 3200 SW Jefferson Way, Corvallis, OR 97331 USA.
EM michael_adams@usgs.gov
FU Amphibian Research and Monitoring Initiative
FX Our study was funded by the Amphibian Research and Monitoring
Initiative. We thank N. Chelgren for guidance throughout this study and
J. Beall for help with logistics and site access. P. Corn and L. Bailey
provided helpful comments on this manuscript. Any use of trade, product,
or firm names is for descriptive purposes only and does not imply
endorsement by the United States Government.
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U1 2
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PU WILEY-BLACKWELL
PI HOBOKEN
PA 111 RIVER ST, HOBOKEN 07030-5774, NJ USA
SN 0022-541X
EI 1937-2817
J9 J WILDLIFE MANAGE
JI J. Wildl. Manage.
PD JAN
PY 2011
VL 75
IS 1
BP 30
EP 35
DI 10.1002/jwmg.29
PG 6
WC Ecology; Zoology
SC Environmental Sciences & Ecology; Zoology
GA 729GR
UT WOS:000287937200005
ER
PT J
AU Potter, LM
Otis, DL
Bogenschutz, TR
AF Potter, Lisa M.
Otis, David L.
Bogenschutz, Todd R.
TI Nest Success of Northern Bobwhite on Managed and Unmanaged Landscapes in
Southeast Iowa
SO JOURNAL OF WILDLIFE MANAGEMENT
LA English
DT Article
DE Colinus virginianus; habitat management; Iowa; landscape composition;
nest success; northern bobwhite; predation; reproduction
ID MICROHABITAT SELECTION; SURVIVAL; POPULATIONS; KANSAS; REPRODUCTION;
VEGETATION; CHICKS
AB Range-wide declines in northern bobwhite populations (Colinus virginianus) have been attributed to concomitant loss of breeding habitat. Bobwhite management efforts to restore this habitat resource can be informed by empirical studies of associations between breeding success and multi-scale habitat attributes. We compared bobwhite nest success in 2 southern Iowa landscapes as a function of microhabitat and landscape composition. Lake Sugema Fish and Wildlife Area (LSWA) was managed to promote bobwhite recruitment, and Harrisburg Township (HT) was an adjacent landscape dominated by private agricultural production. Survival rate modeling based on telemetry data provided evidence for age-specific daily nest survival rate. Daily survival rates decreased as nest age increased, but the decline was more severe at HT. Nest survival at LSWA (S = 0.495, SE = 0.103) was nearly twice that on HT (S = 0.277, SE = 0.072). We found no evidence that habitat composition or spatial attributes within 210 m of a nest site significantly influenced nest success. Forb canopy at the nest site had a positive influence on nest success at HT but not at LSWA. We suggest nesting habitat with greater forb canopy cover will increase the opportunity for nesting success in landscapes with limited nesting habitat. (C) 2011 The Wildlife Society.
C1 [Potter, Lisa M.] Iowa State Univ, Dept Nat Resource Ecol & Management, Ames, IA 50011 USA.
[Otis, David L.] Iowa State Univ, Iowa Cooperat Fish & Wildlife Res Unit, US Geol Survey, Ames, IA 50011 USA.
[Bogenschutz, Todd R.] Iowa Dept Nat Resources, Boone, IA 50036 USA.
RP Potter, LM (reprint author), MDC, Parkade Plaza,Suite 250,601 Business Loop,70W, Columbia, MO 65203 USA.
EM dotis@iastate.edu
FU IDNR [W-115-R]; United States Geological Survey Iowa Cooperative Fish
and Wildlife Research Unit (Unit) at Iowa State University; United
States Geological Survey; Iowa State University; Wildlife Management
Institute
FX Our study was supported by the IDNR Federal Aid in Wildlife Restoration
Project W-115-R (T. W. Little, Research Supervisor) and the United
States Geological Survey Iowa Cooperative Fish and Wildlife Research
Unit (Unit) at Iowa State University. We gratefully acknowledge the
field assistance provided by IDNR staff. We thank T. Dailey, C. Steffen,
and S. Taylor for review of earlier versions of this manuscript. The
Unit is supported by a cooperative agreement between the United States
Geological Survey, IDNR, Iowa State University, and the Wildlife
Management Institute.
NR 42
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U1 1
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PU WILEY-BLACKWELL
PI HOBOKEN
PA 111 RIVER ST, HOBOKEN 07030-5774, NJ USA
SN 0022-541X
EI 1937-2817
J9 J WILDLIFE MANAGE
JI J. Wildl. Manage.
PD JAN
PY 2011
VL 75
IS 1
BP 46
EP 51
DI 10.1002/jwmg.18
PG 6
WC Ecology; Zoology
SC Environmental Sciences & Ecology; Zoology
GA 729GR
UT WOS:000287937200007
ER
PT J
AU Ely, CR
Raveling, DG
AF Ely, Craig R.
Raveling, Dennis G.
TI Seasonal Variation in Nutritional Characteristics of the Diet of Greater
White-Fronted Geese
SO JOURNAL OF WILDLIFE MANAGEMENT
LA English
DT Article
DE Anser albifrons; California; diet; distribution; food habits; greater
white-fronted geese; habitat; nutrition; winter ecology
ID LESSER SNOW GEESE; ANSER-ALBIFRONS-FLAVIROSTRIS; HABITAT USE; CANADA
GEESE; BODY-COMPOSITION; CENTRAL VALLEY; RESOURCE USE; FOOD-HABITS;
WINTER; WATERFOWL
AB We studied diet and habitat use of greater white-fronted geese )(Anser albifrons) from autumn through spring on their primary staging and wintering areas in the Pacific Flyway, 1979-1982. There have been few previous studies of resource use and forage quality of wintering greater white-fronted geese in North America, and as a consequence there has been little empirical support for management practices pertaining to habitat conservation of this broadly distributed species. Observations of >2,500 flocks of geese and collections of foraging birds revealed seasonal and geographic variation in resource use reflective of changes in habitat availability, selection, and fluctuating physiological demands. Autumn migrants from Alaska arrived first in the Klamath Basin of California and southern Oregon, where they fed on barley, oats, wheat, and potatoes. Geese migrated from the Klamath Basin into the Central Valley of California in late autumn where they exploited agricultural crops rich in soluble carbohydrates, with geese in the Sacramento Valley feeding almost exclusively on rice and birds on the Sacramento-San Joaquin Delta primarily utilizing corn. White-fronted geese began their northward migration in late winter, and by early spring most had returned to the Klamath Basin where 37% of flocks were found in fields of new growth cultivated and wild grasses. Cereal grains and potatoes ingested by geese were low in protein )(7-14%) and high in soluble nutrients )(17-47% neutral detergent fiber [NDF]), whereas grasses were low in available energy )(47-49% NDF) but high in protein )(26-42%). Greater white-fronted geese are generalist herbivores and can exploit a variety of carbohydrate-rich cultivated crops, likely making these geese less susceptible to winter food shortages than prior to the agriculturalization of the North American landscape. However, agricultural landscapes can be extremely dynamic and may be less predictable in the long-term than the historic environments to which geese are adapted. Thus far greater white-fronted geese have proved resilient to changes in land cover in the Pacific Flyway and by altering their migration regime have even been able to adapt to changes in the availability of suitable forage crops. (C) 2011 The Wildlife Society.
C1 [Ely, Craig R.; Raveling, Dennis G.] Univ Calif Davis, Dept Wildlife Fish & Conservat Biol, Davis, CA 95616 USA.
RP Ely, CR (reprint author), US Geol Survey, Alaska Sci Ctr, 4210 Univ Dr, Anchorage, AK 99508 USA.
EM cely@usgs.gov
FU University of California, Davis (UCD)
FX This project would not have been possible without the participation of
the California Department of Fish and Game (CDFG), USFWS, and the
University of California, Davis (UCD). The University provided financial
assistance, laboratory equipment, and computer facilities. D. P.
Connelly (CDFG) provided extensive logistical support, and W. C.
Rienecker, B. Deuel, H. Romero, and S. Castillo helped with field work.
E. H. McCollum, E. J. O'Neill, and R. Fields (USFWS) provided useful
information and assisted with work in the Klamath Basin, and E. Collins
and J. B. Helvie (USFWS) granted us access to refuges in the Sacramento
Valley. D. Mauser (USFWS) provided unpublished refuge reports and
insights into long-term changes in habitat in the Klamath Basin. A. Ely
assisted with collections, and D. V. Derksen (USFWS) and G. Dickison
(Alaska Department Natural Resources) provided computer facilities. B.
Crampton (UCD) assisted with plant identification, and J. Gammonley, and
J. McDowel assisted with laboratory analysis of food items. S. Howlin
assisted with statistical analysis of habitat use in the Klamath Basin.
J. Hupp, D. Derksen, D. Ward, and J. Fischer kindly reviewed earlier
drafts of this manuscript. Suggestions by 2 anonymous reviewers and the
Associate Editor were helpful in improving the manuscript. Mention of
trade names or commercial products does not constitute endorsement or
recommendation for use.
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PI MALDEN
PA COMMERCE PLACE, 350 MAIN ST, MALDEN 02148, MA USA
SN 0022-541X
J9 J WILDLIFE MANAGE
JI J. Wildl. Manage.
PD JAN
PY 2011
VL 75
IS 1
BP 78
EP 91
DI 10.1002/jwmg.13
PG 14
WC Ecology; Zoology
SC Environmental Sciences & Ecology; Zoology
GA 729GR
UT WOS:000287937200011
ER
PT J
AU Lok, EK
Esler, D
Takekawa, JY
De La Cruz, SW
Boyd, WS
Nysewander, DR
Evenson, JR
Ward, DH
AF Lok, Erika K.
Esler, Daniel
Takekawa, John Y.
De La Cruz, Susan W.
Boyd, W. Sean
Nysewander, David R.
Evenson, Joseph R.
Ward, David H.
TI Stopover Habitats of Spring Migrating Surf Scoters in Southeast Alaska
SO JOURNAL OF WILDLIFE MANAGEMENT
LA English
DT Article
DE habitat; Melanitta perspicillata; satellite telemetry; southeast Alaska;
spring migration; stopover; surf scoter
ID WHITE-WINGED SCOTERS; BRITISH-COLUMBIA; HARLEQUIN DUCKS; CLUPEA-PALLASI;
REPRODUCTIVE-PERFORMANCE; NUTRIENT RESERVES; WINTERING SURF; BERING-SEA;
SPAWN; SANDPIPERS
AB Habitat conditions and nutrient reserve levels during spring migration have been suggested as important factors affecting population declines in waterfowl, emphasizing the need to identify key sites used during spring and understand habitat features and resource availability at stopover sites. We used satellite telemetry to identify stopover sites used by surf scoters migrating through southeast Alaska during spring. We then contrasted habitat features of these sites to those of random sites to determine habitat attributes corresponding to use by migrating scoters. We identified 14 stopover sites based on use by satellite tagged surf scoters from several wintering sites. We identified Lynn Canal as a particularly important stopover site for surf scoters originating throughout the Pacific winter range; approximately half of tagged coastally migrating surf scoters used this site, many for extended periods. Stopover sites were farther from the mainland coast and closer to herring spawn sites than random sites, whereas physical shoreline habitat attributes were generally poor predictors of site use. The geography and resource availability within southeast Alaska provides unique and potentially critical stopover habitat for spring migrating surf scoters. Our work identifies specific sites and habitat resources that deserve conservation and management consideration. Aggregations of birds are vulnerable to human activity impacts such as contaminant spills and resource management decisions. This information is of value to agencies and organizations responsible for emergency response planning, herring fisheries management, and bird and ecosystem conservation. (C) 2011 The Wildlife Society.
C1 [Lok, Erika K.] Simon Fraser Univ, Ctr Wildlife Ecol, Burnaby, BC V5A 1S6, Canada.
[Esler, Daniel] Simon Fraser Univ, Ctr Wildlife Ecol, Delta, BC V4K 3N2, Canada.
[Takekawa, John Y.; De La Cruz, Susan W.] US Geol Survey, Western Ecol Res Ctr, San Francisco Bay Estuary Field Stn, Vallejo, CA 94592 USA.
[Boyd, W. Sean] Canadian Wildlife Serv, Delta, BC V4K 3N2, Canada.
[Nysewander, David R.; Evenson, Joseph R.] Washington Dept Fish & Wildlife, Olympia, WA 98501 USA.
[Ward, David H.] US Geol Survey, Alaska Sci Ctr, Anchorage, AK 99508 USA.
RP Lok, EK (reprint author), Simon Fraser Univ, Ctr Wildlife Ecol, 8888 Univ Dr, Burnaby, BC V5A 1S6, Canada.
EM eklok@alumni.sfu.ca
FU Sea Duck Joint Venture; Environment Canada-Canadian Wildlife Service
Pacific and Yukon Region; Environment Canada's Georgia Basin Action
Plan; Washington Department of Fish and Wildlife; USGS-Alaska Science
Center; USGS Western Ecological Research Center Coastal Ecosystems
Program; Calfed Ecosystem Restoration Program
FX Funding was provided by the Sea Duck Joint Venture, Environment
Canada-Canadian Wildlife Service Pacific and Yukon Region, Environment
Canada's Georgia Basin Action Plan, Washington Department of Fish and
Wildlife, USGS-Alaska Science Center, USGS Western Ecological Research
Center Coastal Ecosystems Program with support from the Calfed Ecosystem
Restoration Program. Special thanks to K. Brodhead, E. Carrera, S.
Herzka, and E. Mellink for their support in Mexico. We also thank the
biologists and veterinarians who assisted with captures and marking of
scoters. The use of trade, product, or firm names in this publication is
for descriptive purposes only and does not imply endorsement.
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PI MALDEN
PA COMMERCE PLACE, 350 MAIN ST, MALDEN 02148, MA USA
SN 0022-541X
J9 J WILDLIFE MANAGE
JI J. Wildl. Manage.
PD JAN
PY 2011
VL 75
IS 1
BP 92
EP 100
DI 10.1002/jwmg.5
PG 9
WC Ecology; Zoology
SC Environmental Sciences & Ecology; Zoology
GA 729GR
UT WOS:000287937200012
ER
PT J
AU Fondell, TF
Flint, PL
Sedinger, JS
Nicolai, CA
Schamber, JL
AF Fondell, Thomas F.
Flint, Paul L.
Sedinger, James S.
Nicolai, Christopher A.
Schamber, Jason L.
TI Intercolony Variation in Growth of Black Brant Goslings on the
Yukon-Kuskokwim Delta, Alaska
SO JOURNAL OF WILDLIFE MANAGEMENT
LA English
DT Article
DE black brant; Branta bernicla nigricans; gosling growth; intercolony
variation; population limitation; Yukon-Kuskokwim Delta
ID GEESE CHEN-CANAGICA; LESSER SNOW GEESE; EMPEROR GEESE; HATCH DATE;
BODY-SIZE; ENVIRONMENTAL-CHANGE; BREEDING POPULATION;
DENSITY-DEPENDENCE; BERNICLA-NIGRICANS; SURVIVAL
AB Recent declines in black brant (Branta bernicla nigricans) are likely the result of low recruitment. In geese, recruitment is strongly affected by habitat conditions experienced by broods because gosling growth rates are indicative of forage conditions during brood rearing and strongly influence future survival and productivity. In 2006-2008, we studied gosling growth at 3 of the 4 major colonies on the Yukon-Kuskokwim Delta, Alaska. Estimates of age-adjusted gosling mass at the 2 southern colonies (approx. 30% of the world population of breeding black brant) was low (gosling mass at 30.5 days ranged 346.7 +/- 42.5 g to 627.1 +/- 15.9 g) in comparison to a third colony (gosling mass at 30.5 days ranged 640.0 +/- 8.3 g to 821.6 +/- 13.6 g) and to most previous estimates of age-adjusted mass of brant goslings. Thus, our results are consistent with the hypothesis that poor gosling growth is negatively influencing the brant population. There are 2 non-mutually exclusive explanations for the apparent growth rates we observed. First, the population decline may have been caused by density-independent factors and habitat capacity has declined along with the population as a consequence of the unique foraging feedback between brant and their grazing habitats. Alternatively, a reduction in habitat capacity, as a result of changes to the grazing system, may have negatively influenced gosling growth, which is contributing to the overall long-term population decline. We found support for both explanations. For colonies over habitat capacity we recommend management to enhance foraging habitat, whereas for colonies below habitat capacity we recommend management to increase nesting productivity. (C) 2011 The Wildlife Society.
C1 [Fondell, Thomas F.; Flint, Paul L.; Schamber, Jason L.] US Geol Survey, Alaska Sci Ctr, Anchorage, AK 99508 USA.
[Sedinger, James S.; Nicolai, Christopher A.] Univ Nevada, Dept Nat Resources & Environm Sci, Reno, NV 89512 USA.
RP Fondell, TF (reprint author), US Geol Survey, Alaska Sci Ctr, 4210 Univ Dr, Anchorage, AK 99508 USA.
EM tfondell@usgs.gov
OI Flint, Paul/0000-0002-8758-6993
FU USGS, Alaska Science Center; Migratory Bird Management, Region 7, USFWS;
Ducks Unlimited, Inc.; National Science Foundation [OPP 0196406, DEB
0743152]; Morro Bay Black Brant Group; Phil Jebbia
FX Funding for work at the Baird and Kigigak colonies was provided by the
USGS, Alaska Science Center avian influenza monitoring program. Work at
Tutakoke River was supported by Migratory Bird Management, Region 7,
USFWS; Ducks Unlimited, Inc.; National Science Foundation (OPP 0196406,
DEB 0743152); the Morro Bay Black Brant Group; and Phil Jebbia. We thank
D. Baldassarre, A. Cheney, T. Donnelly, B. Heindl, M. Rieck, N. Saake,
J. Seyfried, E. Smith, C., and J. Steffen, S. Stortz, M. Walker and D.
Ward for field assistance; R. Cone and R. King who piloted us safely;
and the staff of the Yukon-Delta National Wildlife Refuge for
hospitality and logistical assistance, especially B. Lake and M. Wege,
who graciously allowed us to work from their field camps. D. Derksen
provided advice in project planning. Comments from G. Gauthier, J.
Schmutz, M. Wege improved the quality of this manuscript. Any use of
trade names is for descriptive purposes only and does not imply
endorsement by the United States Government.
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U1 2
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PI HOBOKEN
PA 111 RIVER ST, HOBOKEN 07030-5774, NJ USA
SN 0022-541X
EI 1937-2817
J9 J WILDLIFE MANAGE
JI J. Wildl. Manage.
PD JAN
PY 2011
VL 75
IS 1
BP 101
EP 108
DI 10.1002/jwmg.24
PG 8
WC Ecology; Zoology
SC Environmental Sciences & Ecology; Zoology
GA 729GR
UT WOS:000287937200013
ER
PT J
AU Blank, PJ
Dively, GP
Gill, DE
Rewa, CA
AF Blank, Peter J.
Dively, Galen P.
Gill, Douglas E.
Rewa, Charles A.
TI Bird Community Response to Filter Strips in Maryland
SO JOURNAL OF WILDLIFE MANAGEMENT
LA English
DT Article
DE agriculture; birds; buffer; Conservation Reserve Enhancement Program
(CREP); filter strip; Maryland
ID CONSERVATION RESERVE PROGRAM; EASTERN NORTH-AMERICA; GRASSLAND BIRDS;
HABITAT QUALITY; FIELDS; VEGETATION; MANAGEMENT; SHRUBLAND; MISSOURI;
PARTNERS
AB Filter strips are strips of herbaceous vegetation planted along agricultural field margins adjacent to streams or wetlands and are designed to intercept sediment, nutrients, and agrichemicals. Roughly 16,000 ha of filter strips have been established in Maryland through the United States Department of Agriculture's Conservation Reserve Enhancement Program. Filter strips often represent the only uncultivated herbaceous areas on farmland in Maryland and therefore may be important habitat for early-successional bird species. Most filter strips in Maryland are planted to either native warm-season grasses or cool-season grasses and range in width from 10.7 m to 91.4 m. From 2004 to 2007 we studied the breeding and wintering bird communities in filter strips adjacent to wooded edges and non-buffered field edges and the effect that grass type and width of filter strips had on bird community composition. We used 5 bird community metrics (total bird density, species richness, scrub-shrub bird density, grassland bird density, and total avian conservation value), species-specific densities, nest densities, and nest survival estimates to assess the habitat value of filter strips for birds. Breeding and wintering bird community metrics were greater in filter strips than in non-buffered field edges but did not differ between cool-season and warm-season grass filter strips. Most breeding bird community metrics were negatively related to the percent cover of orchardgrass (Dactylis glomerata) in >= 1 yr. Breeding bird density was greater in narrow (<30 m) compared to wide (>60 m) filter strips. Our results suggest that narrow filter strips adjacent to wooded edges can provide habitat for many bird species but that wide filter strips provide better habitat for grassland birds, particularly obligate grassland species. If bird conservation is an objective, avoid planting orchardgrass in filter strips and reduce or eliminate orchardgrass from filter strips through management practices. (C) 2011 The Wildlife Society
C1 [Blank, Peter J.] Univ Maryland, Marine Estuarine Environm Sci Program, College Pk, MD 20742 USA.
[Dively, Galen P.] Univ Maryland, Dept Entomol, College Pk, MD 20742 USA.
[Gill, Douglas E.] Univ Maryland, Dept Biol, College Pk, MD 20742 USA.
[Rewa, Charles A.] Nat Resources Conservat Serv, Beltsville, MD 20705 USA.
RP Blank, PJ (reprint author), USGS Patuxent Wildlife Res Ctr, 12100 Beech Forest Rd, Laurel, MD 20708 USA.
EM blankpj@gmail.com
FU NRCS Agricultural Wildlife Conservation Center; Maryland Department of
Natural Resources
FX We thank M. Gimpel, J. Guerard, L. Kelly, B. Olsen, J. Parks, Z. Parks,
and D. Small for their help in the field. We appreciate L. Adams, P.
Marra, and G. Brewer for their help with the study design. B. Momen, M.
Runge, T. Shaffer, E. Grant, S. Sillett, C. Che-castaldo, and L.
Douglass assisted with statistical analysis. We thank the farm owners
that allowed us to work on their properties. The NRCS and the Farm
Service Agency staff in Caroline, Kent, Queen Anne's, and Talbot
counties helped with locating CREP filter strips and with technical
information. P. Engler, A. Lynn, and S. Strano at NRCS, Maryland, helped
with study design and technical resources. N. Gerber and the staff at
the Chesapeake Wildlife Heritage provided technical information and
advice. Funding was provided by the NRCS Agricultural Wildlife
Conservation Center and the Maryland Department of Natural Resources.
NR 43
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U1 1
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PU WILEY-BLACKWELL
PI HOBOKEN
PA 111 RIVER ST, HOBOKEN 07030-5774, NJ USA
SN 0022-541X
EI 1937-2817
J9 J WILDLIFE MANAGE
JI J. Wildl. Manage.
PD JAN
PY 2011
VL 75
IS 1
BP 116
EP 125
DI 10.1002/jwmg.3
PG 10
WC Ecology; Zoology
SC Environmental Sciences & Ecology; Zoology
GA 729GR
UT WOS:000287937200015
ER
PT J
AU Sargeant, GA
Weber, DC
Roddy, DE
AF Sargeant, Glen A.
Weber, Duane C.
Roddy, Daniel E.
TI Implications of Chronic Wasting Disease, Cougar Predation, and Reduced
Recruitment for Elk Management
SO JOURNAL OF WILDLIFE MANAGEMENT
LA English
DT Article
DE Cervus elaphus; chronic wasting disease; cougar; elk; population
dynamics; Puma concolor; reproduction; South Dakota; survival; Wind Cave
National Park
ID POPULATION-DYNAMICS; MULE DEER; TEMPORAL VARIATION; LARGE HERBIVORES;
CALF SURVIVAL; FEMALE ELK; HARVEST; CERVIDS; GROWTH; MODELS
AB Emerging diseases and expanding carnivore populations may have profound implications for ungulate harvest management and population regulation. To better understand effects of chronic wasting disease (CWD) and cougar (Puma concolor) predation, we studied mortality and recruitment of elk (Cervus elaphus) at Wind Cave National Park (WICA) during 2005-2009. We marked 202 elk (83 subadult M and 119 subadult and ad F) with Global Positioning System (GPS) collars, observed 28 deaths during 74,220 days of monitoring, and investigated 42 additional deaths of unmarked elk found dead. Survival rates were similar for males and females and averaged 0.863 (SE = 0.025) annually. Leading causes of mortality included hunting (0.065, SE = 0.019), CWD (0.034, SE = 0.012), and cougar predation (0.029, SE = 0.012). Marked elk killed by hunters and cougars typically were in good physical condition and not infected with CWD. Effects of mortality on population growth were exacerbated by low rates of pregnancy (subadults = 9.5%, SE = 6.6%; ad = 76.9%, SE = 4.2%) and perinatal survival (0.49, SE = 0.085 from 1 Feb to 1 Sep). Chronic wasting disease, increased predation, and reduced recruitment reduced the rate of increase for elk at WICA to approximately lambda = 1.00 (SE = 0.027) during the past decade. Lower rates of increase are mitigating effects of elk on park vegetation, other wildlife, and neighboring lands and will facilitate population control, but may reduce opportunities for elk hunting outside the park. (C) 2011 The Wildlife Society.
C1 [Sargeant, Glen A.] US Geol Survey, No Prairie Wildlife Res Ctr, Jamestown, ND 58401 USA.
[Weber, Duane C.; Roddy, Daniel E.] Natl Pk Serv, Hot Springs, SD 57747 USA.
RP Sargeant, GA (reprint author), US Geol Survey, No Prairie Wildlife Res Ctr, 8711 37th St SE, Jamestown, ND 58401 USA.
EM gsargeant@usgs.gov
FU NPS Natural Resources Preservation Program; USGS; NPS Biological
Resources Management Division; NPS WICA
FX Project funding was provided by the NPS Natural Resources Preservation
Program, USGS, NPS Biological Resources Management Division, and NPS
WICA. We are especially grateful to NPS staff who assisted with elk
captures and to J. G. Powers and M. A. Wild, who provided veterinary
support. S. Griffin provided information about hunter-killed elk. C. L.
Sexton prepared Figure 1. J. A. Jenks, D. H. Johnson, M. W. Oehler, and
J. G. Powers reviewed early drafts of our manuscript. Use of trade,
product, and firm names is for descriptive purposes only and does not
imply endorsement by the United States Government.
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U2 25
PU WILEY-BLACKWELL
PI MALDEN
PA COMMERCE PLACE, 350 MAIN ST, MALDEN 02148, MA USA
SN 0022-541X
J9 J WILDLIFE MANAGE
JI J. Wildl. Manage.
PD JAN
PY 2011
VL 75
IS 1
BP 171
EP 177
DI 10.1002/jwmg.27
PG 7
WC Ecology; Zoology
SC Environmental Sciences & Ecology; Zoology
GA 729GR
UT WOS:000287937200022
ER
PT J
AU Gustine, DD
Barboza, PS
Adams, LG
Farnell, RG
Parker, KL
AF Gustine, David D.
Barboza, Perry S.
Adams, Layne G.
Farnell, Richard G.
Parker, Katherine L.
TI An Isotopic Approach to Measuring Nitrogen Balance in Caribou
SO JOURNAL OF WILDLIFE MANAGEMENT
LA English
DT Article
DE caribou; Chisana; isotopes; nitrogen; nutrition; protein status;
Rangifer
ID REINDEER RANGIFER-TARANDUS; WHITE-TAILED DEER; MUSKOXEN
OVIBOS-MOSCHATUS; BODY-COMPOSITION; FEMALE CARIBOU; SEASONAL-CHANGES;
STABLE-ISOTOPES; ALASKAN CARIBOU; MILK-PRODUCTION; WILD REINDEER
AB Nutritional restrictions in winter may reduce the availability of protein for reproduction and survival in northern ungulates. We refined a technique that uses recently voided excreta on snow to assess protein status in wild caribou (Rangifer tarandus) in late winter. Our study was the first application of this non-invasive, isotopic approach to assess protein status of wild caribou by determining dietary and endogenous contributions of nitrogen (N) to urinary urea. We used isotopic ratios of N (delta N-15) in urine and fecal samples to estimate the proportion of urea N derived from body N (p-UN) in pregnant, adult females of the Chisana Herd, a small population that ranged across the Alaska-Yukon border. We took advantage of a predator-exclosure project to examine N status of penned caribou in April 2006. Lichens were the primary forage (>40%) consumed by caribou in the pen and delta N-15 of fiber tracked the major forages in their diets. The delta N-15 of urinary urea for females in the pen was depleted relative (-1.3 +/- 1.0 parts per thousand [parts per thousand], (x) over bar +/- SD) to the delta N-15 of body N (2.7 +/- 0.7 parts per thousand). A similar proportion of animals in the exclosure lost core body mass (excluding estimates of fetal and uterine tissues; 55%) and body protein (estimated by isotope ratios; 54%). This non-invasive technique could be applied at various spatial and temporal scales to assess trends in protein status of free-ranging populations of northern ungulates. Intra- and inter-annual estimates of protein status could help managers monitor effects of foraging conditions on nutritional constraints in ungulates, increase the efficiency and efficacy of management actions, and help prepare stakeholders for potential changes in population trends. (C) 2011 The Wildlife Society.
C1 [Gustine, David D.; Barboza, Perry S.] Univ Alaska, Dept Biol & Wildlife, Inst Arctic Biol, Fairbanks, AK 99775 USA.
[Adams, Layne G.] US Geol Survey, Alaska Sci Ctr, Anchorage, AK 99508 USA.
[Farnell, Richard G.] Yukon Dept Environm Retired, Whitehorse, YT Y1A 2C6, Canada.
[Parker, Katherine L.] Univ No British Columbia, Nat Resources & Environm Studies Inst, Prince George, BC V2N 4Z9, Canada.
RP Gustine, DD (reprint author), Univ Alaska, Dept Biol & Wildlife, Inst Arctic Biol, Fairbanks, AK 99775 USA.
EM dgustine@usgs.gov
OI Barboza, Perry/0000-0002-1489-6448
FU Cooperative Institute for Arctic Research [CIPY-10]; National Oceanic
and Atmospheric Administration [NA17RJ1224]; UAF; USGS; UAF Graduate
School; Department of Biology and Wildlife at UAF; Canadian Wildlife
Service
FX Funding for D. Gustine was provided by a Cooperative Institute for
Arctic Research (Project CIPY-10) with funds from the National Oceanic
and Atmospheric Administration under a cooperative agreement
(NA17RJ1224) with the UAF, USGS, the UAF Graduate School, and the
Department of Biology and Wildlife at UAF. Financial support for
collection and processing of samples was provided by the USGS and the
Canadian Wildlife Service. Use of any trade names in this manuscript
does not imply endorsement by the United States government. Many people
assisted in collecting samples and we particularly thank L. Larocque, G.
Lortie, J. McLelland, and G. Roffler. J. Addison, N. Gustine, K. Moon,
and R. Parsley assisted with laboratory work; N. Haubenstock, T. Howe,
L. Oliver, and M. Otter conducted the isotopic analysis; and B. Davitt
did the microhistology work. M. Gillingham provided guidance on the
structure of the simulation model. This manuscript was greatly improved
by comments from S. Cote, J. Lawler, and 2 anonymous reviewers.
NR 87
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U1 0
U2 39
PU WILEY-BLACKWELL
PI HOBOKEN
PA 111 RIVER ST, HOBOKEN 07030-5774, NJ USA
SN 0022-541X
EI 1937-2817
J9 J WILDLIFE MANAGE
JI J. Wildl. Manage.
PD JAN
PY 2011
VL 75
IS 1
BP 178
EP 188
DI 10.1002/jwmg.11
PG 11
WC Ecology; Zoology
SC Environmental Sciences & Ecology; Zoology
GA 729GR
UT WOS:000287937200023
ER
PT J
AU Grovenburg, TW
Swanson, CC
Jacques, CN
Klaver, RW
Brinkman, TJ
Burris, BM
Deperno, CS
Jenks, JA
AF Grovenburg, Troy W.
Swanson, Christopher C.
Jacques, Christopher N.
Klaver, Robert W.
Brinkman, Todd J.
Burris, Benjamin M.
Deperno, Christopher S.
Jenks, Jonathan A.
TI Survival of White-Tailed Deer Neonates in Minnesota and South Dakota
SO JOURNAL OF WILDLIFE MANAGEMENT
LA English
DT Article
DE habitat; landscape; Minnesota; mortality; neonate; Odocoileus
virginianus; predation; South Dakota; survival
ID CAUSE-SPECIFIC MORTALITY; CONTERMINOUS UNITED-STATES; NORTH-CENTRAL
MINNESOTA; NORTHEASTERN MINNESOTA; COYOTE PREDATION; NEW-BRUNSWICK; DOE
BEHAVIOR; FAWNS; LANDSCAPE; ILLINOIS
AB Understanding the influence of intrinsic (e. g., age, birth mass, and sex) and habitat factors on survival of neonate white-tailed deer improves understanding of population ecology. During 2002-2004, we captured and radiocollared 78 neonates in eastern South Dakota and southwestern Minnesota, of which 16 died before 1 September. Predation accounted for 80% of mortality; the remaining 20% was attributed to starvation. Canids (coyotes [Canis latrans], domestic dogs) accounted for 100% of predation on neonates. We used known fate analysis in Program MARK to estimate survival rates and investigate the influence of intrinsic and habitat variables on survival. We developed 2 a priori model sets, including intrinsic variables (model set 1) and habitat variables (model set 2; forested cover, wetlands, grasslands, and croplands). For model set 1, model {S(age-interval)} had the lowest AIC(c) (Akaike's information criterion for small sample size) value, indicating that age at mortality (3-stage age-interval: 0-2 weeks, 2-8 weeks, and > 8 weeks) best explained survival. Model set 2 indicated that habitat variables did not further influence survival in the study area; beta-estimates and 95% confidence intervals for habitat variables in competing models encompassed zero; thus, we excluded these models from consideration. Overall survival rate using model {S(age-interval)} was 0.87 (95% CI - 0.83-0.91); 61% of mortalities occurred at 0-2 weeks of age, 26% at 2-8 weeks of age, and 13% at > 8 weeks of age. Our results indicate that variables influencing survival may be area specific. Region-specific data are needed to determine influences of intrinsic and habitat variables on neonate survival before wildlife managers can determine which habitat management activities influence neonate populations. (C) 2011 The Wildlife Society.
C1 [Grovenburg, Troy W.; Swanson, Christopher C.; Burris, Benjamin M.; Jenks, Jonathan A.] S Dakota State Univ, Dept Wildlife & Fisheries Sci, Brookings, SD 57007 USA.
[Jacques, Christopher N.] Bur Sci Serv, Wisconsin Dept Nat Resources, Madison, WI 53716 USA.
[Klaver, Robert W.] US Geol Survey, Ctr Earth Resources Observat & Sci EROS, Sioux Falls, SD 57198 USA.
[Brinkman, Todd J.] Univ Alaska Fairbanks, Dept Biol & Wildlife, Inst Arctic Biol, Fairbanks, AK 99775 USA.
[Deperno, Christopher S.] N Carolina State Univ, Dept Forestry & Environm Resources, Fisheries & Wildlife Sci Program, Raleigh, NC 27695 USA.
RP Grovenburg, TW (reprint author), S Dakota State Univ, Dept Wildlife & Fisheries Sci, Brookings, SD 57007 USA.
EM troy.grovenburg@sdstate.edu
RI Jenks, Jonathan/B-7321-2009; Brinkman, Todd/B-3578-2013; Grovenburg,
Troy/K-3346-2012
FU Federal Aid to Wildlife Restoration; South Dakota State University; Bend
of the River Chapter of Minnesota Deer Hunters Association; Bluffland
Whitetails Association; Cottonwood County Game and Fish League; Des
Moines Valley Chapter of Minnesota Deer Hunters Association; Minnesota
Bowhunters, Inc.; Minnesota Deer Hunters Association; Minnesota State
Archery Association I; North Country Bowhunters Chapter of Safari Club
International; Rum River Chapter of Minnesota Deer Hunters Association;
South Metro Chapter of Minnesota Deer Hunters Association; Whitetail
Institute of North America; Minnesota Department of Natural Resources
FX Funding for this study was provided by Federal Aid to Wildlife
Restoration administered by South Dakota Department of Game, Fish and
Parks and the Minnesota Department of Natural Resources. Funding also
was provided by South Dakota State University, Bend of the River Chapter
of Minnesota Deer Hunters Association, Bluffland Whitetails Association,
Cottonwood County Game and Fish League, Des Moines Valley Chapter of
Minnesota Deer Hunters Association, Minnesota Bowhunters, Inc.,
Minnesota Deer Hunters Association, Minnesota State Archery Association
I, North Country Bowhunters Chapter of Safari Club International, Rum
River Chapter of Minnesota Deer Hunters Association, South Metro Chapter
of Minnesota Deer Hunters Association, and Whitetail Institute of North
America. Additionally, many volunteers and technicians (J. Smith, C.
Schultz) greatly contributed to the success of this study. We thank R.
Auch and D. Ohlen for reviewing this manuscript. We are grateful to the
many landowners who granted us permission to conduct our study on their
property. Any mention of trade, product, or firm names is for
descriptive purposes only and does not imply endorsement by the United
States Government.
NR 60
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U1 2
U2 35
PU WILEY-BLACKWELL
PI MALDEN
PA COMMERCE PLACE, 350 MAIN ST, MALDEN 02148, MA USA
SN 0022-541X
J9 J WILDLIFE MANAGE
JI J. Wildl. Manage.
PD JAN
PY 2011
VL 75
IS 1
BP 213
EP 220
DI 10.1002/jwmg.20
PG 8
WC Ecology; Zoology
SC Environmental Sciences & Ecology; Zoology
GA 729GR
UT WOS:000287937200027
ER
PT J
AU Prouty, NG
Roark, EB
Buster, NA
Ross, SW
AF Prouty, N. G.
Roark, E. B.
Buster, N. A.
Ross, S. W.
TI Growth rate and age distribution of deep-sea black corals in the Gulf of
Mexico
SO MARINE ECOLOGY PROGRESS SERIES
LA English
DT Article
DE Black corals; Radiocarbon age; Growth rates; Gulf of Mexico; Oil
ID RADIOCARBON-BASED AGES; PRIMNOA-RESEDAEFORMIS; SKELETON COELENTERATA;
WATER ANTIPATHARIANS; RECORDS; C-14; POPULATIONS; CALIBRATION; PATTERNS;
FJORDS
AB Black corals (order Antipatharia) are important long-lived, habitat-forming, sessile, benthic suspension feeders that are found in all oceans and are usually found in water depths greater than 30 m. Deep-water black corals are some of the slowest-growing, longest-lived deep-sea corals known. Previous age dating of a limited number of black coral samples in the Gulf of Mexico focused on extrapolated ages and growth rates based on skeletal Pb-210 dating. Our results greatly expand the age and growth rate data of black corals from the Gulf of Mexico. Radiocarbon analysis of the oldest Leiopathes sp. specimen from the upper De Soto Slope at 300 m water depth indicates that these animals have been growing continuously for at least the last 2 millennia, with growth rates ranging from 8 to 22 mu m yr(-1). Visual growth ring counts based on scanning electron microscopy images were in good agreement with the C-14-derived ages, suggestive of annual ring formation. The presence of bomb-derived C-14 in the outermost samples confirms sinking particulate organic matter as the dominant carbon source and suggests a link between the deep-sea and surface ocean. There was a high degree of reproducibility found between multiple discs cut from the base of each specimen, as well as within duplicate subsamples. Robust C-14-derived chronologies and known surface ocean C-14 reservoir age constraints in the Gulf of Mexico provided reliable calendar ages with future application to the development of proxy records.
C1 [Prouty, N. G.] US Geol Survey, Santa Cruz, CA 95060 USA.
[Roark, E. B.] Texas A&M Univ, Dept Geog, College Stn, TX 77843 USA.
[Buster, N. A.] US Geol Survey, St Petersburg, FL 33701 USA.
[Ross, S. W.] Univ N Carolina, Ctr Marine Sci, Wilmington, NC 28409 USA.
RP Prouty, NG (reprint author), US Geol Survey, 400 Nat Bridges Dr, Santa Cruz, CA 95060 USA.
EM nprouty@usgs.gov
RI Roark, Erin/D-4124-2013
OI Roark, Erin/0000-0002-1742-9642
FU USGS
FX The USGS Outer Continental Shelf Ecosystem Program and USGS Coastal and
Marine Geology Program supported this work. We thank S. Griffin and E.
Druffel (University of California, Irvine) and T. Guilderson (Lawrence
Livermore National Laboratory) for assistance with radiocarbon analysis,
and K. Sulak (USGS) and S. Cairns (Smithsonian Institution National
Museum of Natural History) for donating samples, D. Opresko for species
identification of some samples, and C. Holmes (USGS) for providing
supplementary radiocarbon data. We also thank the entire USGS Diversity
Systematic, and Connectivity of Valuable Reef Ecosystems (DISCOVRE) team
for their support and collaboration. In addition, we are grateful to K.
Sulak and T. Lorenson (USGS) for providing valuable editorial input as
well as to several anonymous reviewers for their constructive comments
and suggestions.
NR 61
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U1 0
U2 19
PU INTER-RESEARCH
PI OLDENDORF LUHE
PA NORDBUNTE 23, D-21385 OLDENDORF LUHE, GERMANY
SN 0171-8630
EI 1616-1599
J9 MAR ECOL PROG SER
JI Mar. Ecol.-Prog. Ser.
PY 2011
VL 423
BP 101
EP U121
DI 10.3354/meps08953
PG 21
WC Ecology; Marine & Freshwater Biology; Oceanography
SC Environmental Sciences & Ecology; Marine & Freshwater Biology;
Oceanography
GA 729QO
UT WOS:000287965900010
ER
PT J
AU Parsley, MJ
Popoff, ND
Romine, JG
AF Parsley, Michael J.
Popoff, Nicholas D.
Romine, Jason G.
TI Short-Term Response of Subadult White Sturgeon to Hopper Dredge Disposal
Operations
SO NORTH AMERICAN JOURNAL OF FISHERIES MANAGEMENT
LA English
DT Article
ID LOWER COLUMBIA-RIVER; ATLANTIC STURGEON; HABITAT USE; MOVEMENTS;
BEHAVIOR; IMPACTS; FISH; SITE; TOOL
AB The effect of dredged-material disposal operations on the behavior of seven white sturgeon Acipenser transmontanus (50-101 cm fork length) was examined by analysis of the movements and depth use of these fish before, during, and after a series of hopper dredge disposal operations in the lower Columbia River. Analyses of fish locations showed that 12 flow-lane disposal operations within a 24-h period had minimal effect on subadult white sturgeon behavior; six of the seven fish showed slight attraction to the disposal area during disposals, and one fish increased its distance from the disposal area. The core area for all fish combined shifted toward the disposal area during disposals. In the 24 h after completion of the disposal operations the fish core areas shifted back toward those areas occupied before the disposals. The rates of movement, depths used, and diel movement patterns of the white sturgeon showed little change over all periods, suggesting that natural behaviors were not altered during and immediately after hopper dredge disposal operations.
C1 [Parsley, Michael J.; Popoff, Nicholas D.; Romine, Jason G.] US Geol Survey, Western Fisheries Res Ctr, Columbia River Res Lab, Cook, WA 98605 USA.
RP Parsley, MJ (reprint author), US Geol Survey, Western Fisheries Res Ctr, Columbia River Res Lab, 5501A Cook Underwood Rd, Cook, WA 98605 USA.
EM mparsley@usgs.gov
FU U.S. Army Corps of Engineers (USACE), Portland District [W66QKZ11169068,
W66QKZ23243684, W66QKZ31126479, W66QKZ33455609]
FX We acknowledge the contributions of field technicians from Johnson
Controls International whose efforts enabled the collection of most of
these data: Bjorn van der Leeuw, Corey Wright, Ken Bennett, Matt
Sholtis, and Brian Bonath. We appreciate the efforts of Eric (Pete)
Kofoot and Joe Warren from the U.S. Geological Survey (USGS) and Brad
Cady of the Washington Department of Fish and Wildlife for their
assistance with capturing fish. Tom Batt (USGS) provided extensive GIS
support by postprocessing field coordinates and creating compatible
imagery used during data collection. James Hatten (USGS) provided advice
and assistance on spatial analyses. Corey Wright and Bjorn van der Leeuw
did much of the data manipulation and quality assurance and quality
control work before analysis. Special thanks are extended to the crew
and captain of the hopper dredge Essayons. The U.S. Army Corps of
Engineers (USACE), Portland District, funded this work under MIPR
numbers W66QKZ11169068, W66QKZ23243684, W66QKZ31126479, and
W66QKZ33455609. Kim Larson was the USACE technical representative. Any
use of trade, product, or firm names is for descriptive purposes only
and does not imply endorsement by the U. S. Government.
NR 30
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U1 2
U2 6
PU AMER FISHERIES SOC
PI BETHESDA
PA 5410 GROSVENOR LANE SUITE 110, BETHESDA, MD 20814-2199 USA
SN 0275-5947
J9 N AM J FISH MANAGE
JI North Am. J. Fish Manage.
PY 2011
VL 31
IS 1
BP 1
EP 11
AR PII 933116997
DI 10.1080/02755947.2010.549033
PG 11
WC Fisheries
SC Fisheries
GA 733RF
UT WOS:000288279800001
ER
PT J
AU Evans, AF
Roby, DD
Collis, K
Cramer, BM
Sheggeby, JA
Adrean, LJ
Battaglia, DS
Lyons, DE
AF Evans, Allen F.
Roby, Daniel D.
Collis, Ken
Cramer, Bradley M.
Sheggeby, John A.
Adrean, Lindsay J.
Battaglia, Daniel S.
Lyons, Donald E.
TI Recovery of Coded Wire Tags at a Caspian Tern Colony in San Francisco
Bay: A Technique to Evaluate Impacts of Avian Predation on Juvenile
Salmonids
SO NORTH AMERICAN JOURNAL OF FISHERIES MANAGEMENT
LA English
DT Article
ID COLUMBIA RIVER ESTUARY; PASSIVE INTEGRATED TRANSPONDERS; DOUBLE-CRESTED
CORMORANTS; CHINOOK SALMON; HUMAN DISTURBANCE; VULNERABILITY;
TRANSMITTERS; SURVIVAL; SIZE; DAM
AB We recovered coded wire tags (CWTs) from a colony of Caspian terns Hydroprogne caspia on Brooks Island in San Francisco Bay, California, to evaluate predation on juvenile salmonids originating from the Sacramento and San Joaquin rivers. Subsamples of colony substrate representing 11.7% of the nesting habitat used by the terns yielded 2,079 salmonid CWTs from fish released and subsequently consumed by terns in 2008. The estimated number of CWTs deposited on the entire tern colony was 40,143 (ranging from 26,763 to 80,288), once adjustments were made to account for tag loss and the total amount of nesting habitat used by terns. Tags ingested by terns and then egested on the colony were undamaged, and the tags' complete numeric codes were still identifiable. The CWTs found on the tern colony indicated that hatchery Chinook salmon Oncorhynchus tshawytscha trucked to and released in San Pablo Bay were significantly more likely to be consumed by Caspian terns than Chinook salmon that migrated in-river to the bay; 99.7% of all tags recovered were from bay-released Chinook salmon. Of the CWTs recovered on the tern colony, 98.0% were from fall-run Chinook salmon, indicating a higher susceptibility to tern predation than for the spring run type. None of the approximately 518,000 wild Chinook salmon that were coded-wire-tagged and released in the basin were recovered on the tern colony, suggesting that the impacts on wild, U.S. Endangered Species Act-listed Chinook salmon populations were minimal in 2008. Overall, we estimate that 0.3% of the approximately 12.3 million coded-wire-tagged Chinook salmon released in the basin in 2008 were subsequently consumed by Caspian terns from the Brooks Island colony. These results indicate that CWTs implanted in juvenile salmon can be recovered from a piscivorous waterbird colony and used to evaluate smolt losses for runs that are tagged.
C1 [Evans, Allen F.; Collis, Ken; Cramer, Bradley M.; Sheggeby, John A.] Real Time Res Inc, Bend, OR 97702 USA.
[Roby, Daniel D.; Adrean, Lindsay J.; Battaglia, Daniel S.; Lyons, Donald E.] Oregon State Univ, US Geol Survey, Oregon Cooperat Fish & Wildlife Res Unit, Dept Fisheries & Wildlife, Corvallis, OR 97331 USA.
RP Evans, AF (reprint author), Real Time Res Inc, 52 SW Roosevelt Ave, Bend, OR 97702 USA.
EM allen@realtimeresearch.com
FU U.S. Army Corps of Engineers (USACE), Portland District
FX This project was funded by the U.S. Army Corps of Engineers (USACE),
Portland District. We especially want to thank Paul Schmidt and Geoff
Dorsey (USACE) for their assistance and support during the study. We
thank Kevin Neimela and Patricia Brandes from the U.S. Fish and Wildlife
Service, Armando Quinones and Clint Garman from the California
Department of Fish and Game, and Kari Burr from the Fisheries Foundation
of California for providing support and information on CWT releases. We
thank Gary Shugart of the University of Puget Sound for providing some
initial guidance on ways to recover CWTs from tern nesting material. We
are grateful to Steve Bobzien of East Bay Regional Parks District for
granting access to Brooks Island and for his long-standing support of
our research. A special thanks to Tim Marcella, Jarvi Kononen, and
Angela Whitney for their assistance in recovering CWTs as part of this
study.
NR 35
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Z9 9
U1 1
U2 8
PU AMER FISHERIES SOC
PI BETHESDA
PA 5410 GROSVENOR LANE SUITE 110, BETHESDA, MD 20814-2199 USA
SN 0275-5947
J9 N AM J FISH MANAGE
JI North Am. J. Fish Manage.
PY 2011
VL 31
IS 1
BP 79
EP 87
AR PII 934657111
DI 10.1080/02755947.2011.562429
PG 9
WC Fisheries
SC Fisheries
GA 733RF
UT WOS:000288279800009
ER
PT J
AU Dunham, J
Gallo, K
Shively, D
Allen, C
Goehring, B
AF Dunham, Jason
Gallo, Kirsten
Shively, Dan
Allen, Chris
Goehring, Brad
TI Assessing the Feasibility of Native Fish Reintroductions: A Framework
Applied to Threatened Bull Trout
SO NORTH AMERICAN JOURNAL OF FISHERIES MANAGEMENT
LA English
DT Editorial Material
ID METAPOPULATION STRUCTURE; SALVELINUS-CONFLUENTUS; RIVER SYSTEM; HABITAT
USE; CONSERVATION; TRANSLOCATION; POPULATIONS; MONTANA; BIOLOGY; SIZE
AB Translocations to recover native fishes have resulted in mixed success. One reason for the failure of these actions is inadequate assessments of their feasibility prior to implementation. Here, we provide a framework developed to assess the feasibility of one type of translocation-reintroduction. The framework was founded on two simple components of feasibility: the potential for recipient habitats to support a reintroduction and the potential of available donor populations to support a reintroduction. Within each component, we developed a series of key questions. The final assessment was based on a scoring system that incorporated consideration of uncertainty in available information. The result was a simple yet transparent system for assessing reintroduction feasibility that can be rapidly applied in practice. We applied this assessment framework to the potential reintroduction of threatened bull trout Salvelinus confluentus into the Clackamas River, Oregon. In this case, the assessment suggested that the degree of feasibility for reintroduction was high based on the potential of recipient habitats and available donor populations. The assessment did not provide a comprehensive treatment of all possible factors that would drive an actual decision to implement a reintroduction, but it did provide a fundamental level of feasibility assessment that is often lacking in practice.
C1 [Dunham, Jason] US Geol Survey, Forest & Rangeland Ecosyst Sci Ctr, Corvallis, OR 97331 USA.
[Gallo, Kirsten] US Forest Serv, USDA, Corvallis, OR 97333 USA.
[Shively, Dan] US Forest Serv, USDA, Sandy, OR 97055 USA.
[Allen, Chris; Goehring, Brad] US Fish & Wildlife Serv, Oregon Fish & Wildlife Off, Portland, OR 97266 USA.
RP Dunham, J (reprint author), US Geol Survey, Forest & Rangeland Ecosyst Sci Ctr, 3200 SW Jefferson Way, Corvallis, OR 97331 USA.
EM jdunham@usgs.gov
NR 34
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U1 3
U2 26
PU AMER FISHERIES SOC
PI BETHESDA
PA 5410 GROSVENOR LANE SUITE 110, BETHESDA, MD 20814-2199 USA
SN 0275-5947
J9 N AM J FISH MANAGE
JI North Am. J. Fish Manage.
PY 2011
VL 31
IS 1
BP 106
EP 115
DI 10.1080/02755947.2011.559830
PG 10
WC Fisheries
SC Fisheries
GA 733RF
UT WOS:000288279800012
ER
PT J
AU Bowen, MW
Juracek, KE
AF Bowen, Mark W.
Juracek, Kyle E.
TI ASSESSMENT OF THE GEOMORPHIC EFFECTS OF LARGE FLOODS USING STREAMGAGE
DATA: THE 1951 FLOODS IN EASTERN KANSAS, USA
SO PHYSICAL GEOGRAPHY
LA English
DT Article
DE geomorphic effect; 1951 floods; streamgage; channel-bed elevation;
channel width; channel change; channel recovery; Kansas
ID GAUGE INFORMATION
AB Data from 23 U.S. Geological Survey (USGS) streamgages were analyzed to assess the geomorphic effects (short-term change and subsequent recovery) of the record 1951 floods on streams in eastern Kansas. Flood-related, channel-bed elevation change was indicated for 17 gage sites, with substantial deposition at five sites and substantial erosion at two sites. An assessment of post-flood bed elevation recovery was possible for several sites. While recovery to pre-flood channel-bed elevation occurred over a period of months to years at some sites, at other sites recovery was incomplete or absent. Flood-related channel widening with partial recovery was indicated for one site and possible channel widening was indicated for two sites. It was demonstrated that an analysis of streamgage data is a potentially useful technique for assessing the geomorphic effects of a large flood at a site, provided that the gage has a long period of record and is located on an alluvial channel. In the absence of other lines of evidence, streamgage data can provide an estimate of the direction and magnitude (net) of geomorphic change that otherwise might not be available or attainable.
C1 [Bowen, Mark W.] Univ Kansas, Dept Geog, Lawrence, KS 66045 USA.
[Juracek, Kyle E.] US Geol Survey, Lawrence, KS 66049 USA.
RP Bowen, MW (reprint author), Univ Kansas, Dept Geog, Lawrence, KS 66045 USA.
NR 38
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U1 1
U2 5
PU BELLWETHER PUBL LTD
PI COLUMBIA
PA 8640 GUILFORD RD, STE 200, COLUMBIA, MD 21046 USA
SN 0272-3646
J9 PHYS GEOGR
JI Phys. Geogr.
PD JAN-FEB
PY 2011
VL 32
IS 1
BP 52
EP 77
DI 10.2747/0272-3646.32.1.52
PG 26
WC Environmental Sciences; Geography, Physical; Geosciences,
Multidisciplinary; Meteorology & Atmospheric Sciences
SC Environmental Sciences & Ecology; Physical Geography; Geology;
Meteorology & Atmospheric Sciences
GA 732JQ
UT WOS:000288181200003
ER
PT J
AU Irmak, A
Singh, RK
Walter-Shea, EA
Verma, SB
Suyker, AE
AF Irmak, A.
Singh, R. K.
Walter-Shea, E. A.
Verma, S. B.
Suyker, A. E.
TI COMPARISON AND ANALYSIS OF EMPIRICAL EQUATIONS FOR SOIL HEAT FLUX FOR
DIFFERENT CROPPING SYSTEMS AND IRRIGATION METHODS
SO TRANSACTIONS OF THE ASABE
LA English
DT Article
DE Energy balance; Maize; Remote sensing; Soybeans
ID SURFACE-ENERGY BALANCE; REFERENCE-REFLECTANCE PANELS; NET-RADIATION;
STOMATAL-RESISTANCE; MAIZE; MODEL; EVAPOTRANSPIRATION; COEFFICIENTS;
VARIABILITY; CALIBRATION
AB We evaluated the performance of four models for estimating soil heat flux density (G) in maize (Zea mays L.) and soybean (Glycine max L.) fields under different irrigation methods (center-pivot irrigated fields at Mead, Nebraska, and subsurface drip irrigated field at Clay Center, Nebraska) and rainfed conditions at Mead. The model estimates were compared against measurements made during growing seasons of 2003, 2004, and 2005 at Mead and during 2005, 2006, and 2007 at Clay Center. We observed a strong relationship between the G and net radiation (R(n)) ratio (G/R(n)) and the normalized difference vegetation index (NDVI). When a significant portion of the ground was bare soil, G/R(n) ranged from 0.15 to 0.30 and decreased with increasing NDVI. In contrast to the NDVI progression, the G/R(n) ratio decreased with crop growth and development. The G/R(n) ratio for subsurface drip irrigated crops was smaller than for the center-pivot irrigated crops. The seasonal average G was 13.1%, 15.2%, 10.9%, and 12.8% of R(n) for irrigated maize, rainfed maize, irrigated soybean, and rainfed soybean, respectively. Statistical analyses of the performance of the four models showed a wide range of variation in G estimation. The root mean square error (RMSE) of predictions ranged from 15 to 81.3 W m(-2). Based on the wide range of RMSE, it is recommended that local calibration of the models should be carried out for remote estimation of soil heat flux.
C1 [Irmak, A.] Univ Nebraska, Dept Civil Engn, Lincoln, NE 68583 USA.
[Irmak, A.] Univ Nebraska, Sch Nat Resources, Ctr Adv Land Management Informat Technol CALMIT, Lincoln, NE 68583 USA.
[Singh, R. K.] USGS, Earth Resources Observat & Sci EROS Ctr, Sioux Falls, SD USA.
[Walter-Shea, E. A.; Verma, S. B.; Suyker, A. E.] Univ Nebraska, Sch Nat Resources, Lincoln, NE 68583 USA.
RP Irmak, A (reprint author), Univ Nebraska, Dept Civil Engn, 311 Hardin Hall, Lincoln, NE 68583 USA.
EM airmak2@unl.edu
OI Singh, Ramesh/0000-0002-8164-3483
NR 41
TC 2
Z9 2
U1 0
U2 11
PU AMER SOC AGRICULTURAL & BIOLOGICAL ENGINEERS
PI ST JOSEPH
PA 2950 NILES RD, ST JOSEPH, MI 49085-9659 USA
SN 0001-2351
J9 T ASABE
JI Trans. ASABE
PD JAN-FEB
PY 2011
VL 54
IS 1
BP 67
EP 80
PG 14
WC Agricultural Engineering
SC Agriculture
GA 733AU
UT WOS:000288233600008
ER
PT J
AU Jain, AA
Koford, RR
Hancock, AW
Zenner, GG
AF Jain, Aaftab A.
Koford, Rolf R.
Hancock, Alan W.
Zenner, Guy G.
TI Bat Mortality and Activity at a Northern Iowa Wind Resource Area
SO AMERICAN MIDLAND NATURALIST
LA English
DT Article
ID COLLISION MORTALITY; ENERGY FACILITIES; POWER DEVELOPMENT; BUFFALO
RIDGE; FATALITIES; MINNESOTA; MIGRATION; LASIURUS; BEHAVIOR; TURBINES
AB We examined bat collision mortality, activity and species composition at an 89-turbine wind resource area in farmland of north-central Iowa from mid-Apr. to mid-Dec., 2003 and mid-Mar, to mid-Dec., 2004. We found 30 bats beneath turbines on cleared ground and gravel access areas in 2003 and 45 bats in 2004. After adjusting for search probability, search efficiency and scavenging rate, we estimated total bat mortality at 396 +/- 72 (95% ci) in 2003 and 636 +/- 112 (95% ci) in 2004. Although carcasses were mostly migratory tree bats, we found a considerable proportion of little brown bats (Myotis lucifugus). We recorded 1465 bat echolocation call files at turbine sites (x = 34.88 call files/detector-night) and 1536 bat call files at adjacent non-turbine sites (x = 36.57 call files/detector-night). Bat activity did not differ significantly between turbine and non-turbine sites. A large proportion of recorded call files were made by Myotis sp. but this may be because we detected activity at ground level only. There was no relationship between types of turbine lights and either collision mortality or echolocation activity. The highest levels of bat echolocation activity and collision mortality were recorded during Jul. and Aug. during the autumn dispersal and migration period. The fatality rates for bats in general and little brown bats in particular were higher at the Top of Iowa Wind Resource Area than at other, comparable studies in the region. Future efforts to study behavior of bats in flight around turbines as well as cumulative impact studies should not ignore non-tree dwelling bats, generally regarded as minimally affected.
C1 [Jain, Aaftab A.] Iowa State Univ, Iowa Cooperat Fish & Wildlife Res Unit, Dept Nat Resource Ecol & Management, Ames, IA 50011 USA.
[Koford, Rolf R.] Iowa State Univ, US Geol Survey, Iowa Cooperat Fish & Wildlife Res Unit, Ames, IA 50011 USA.
[Hancock, Alan W.; Zenner, Guy G.] Iowa Dept Nat Resources, Clear Lake, IA 50428 USA.
RP Jain, AA (reprint author), 302 Bryn Mawr Dr SE, Albuquerque, NM 87106 USA.
EM aaftabj@hotmail.com
FU Iowa Cooperative Fish and Wildlife Research Unit; Northern Iowa
Windpower LLC; U.S. Fish and Wildlife Service State Wildlife through
Iowa Department of Natural Resources
FX We thank P. Cryan, P. Dixon, T. Kunz and J. Miller for critical comments
on earlier drafts of this manuscript, as well as the two anonymous
reviewers who provided constructive comments on later drafts. Funding
for this study was provided by the Iowa Cooperative Fish and Wildlife
Research Unit, Northern Iowa Windpower LLC and by a U.S. Fish and
Wildlife Service State Wildlife Grant, through the Iowa Department of
Natural Resources. We thank J. Bockenstedt, P. Brandon, B. Carter, I.
Foster, D. Goshorn, K. Kuennen, J. Makosky, R. Miller and M. Piorkowski
for their hard work in the field and laboratory. R. Benedict, D. Howell
and A. Slattery identified bat species. We thank I. Ramler and P. Dixon
for statistical support, and M. Yeager for necropsy work. This research
was conducted under a protocol approved by the Iowa State University
(COAC # 9-03-5524-Q). Mention of trade names or commercial products does
not imply endorsement by the U.S. Government.
NR 46
TC 5
Z9 8
U1 4
U2 30
PU AMER MIDLAND NATURALIST
PI NOTRE DAME
PA UNIV NOTRE DAME, BOX 369, ROOM 295 GLSC, NOTRE DAME, IN 46556 USA
SN 0003-0031
J9 AM MIDL NAT
JI Am. Midl. Nat.
PD JAN
PY 2011
VL 165
IS 1
BP 185
EP 200
DI 10.1674/0003-0031-165.1.185
PG 16
WC Biodiversity Conservation; Ecology
SC Biodiversity & Conservation; Environmental Sciences & Ecology
GA 716KH
UT WOS:000286967000016
ER
PT J
AU Love, JJ
AF Love, J. J.
TI Secular trends in storm-level geomagnetic activity
SO ANNALES GEOPHYSICAE
LA English
DT Article
DE Magnetospheric physics; Solar wind-magnetosphere interactions
ID INTERPLANETARY MAGNETIC-FIELD; GROUP SUNSPOT NUMBERS; LONG-TERM CHANGE;
SOLAR-WIND; TIME-SERIES; AA INDEX; CLIMATE; KP; RECONSTRUCTION;
20TH-CENTURY
AB Analysis is made of K-index data from groups of ground-based geomagnetic observatories in Germany, Britain, and Australia, 1868.0-2009.0, solar cycles 11-23. Methods include nonparametric measures of trends and statistical significance used by the hydrological and climatological research communities. Among the three observatory groups, GermanK data systematically record the highest disturbance levels, followed by the British and, then, the Australian data. Signals consistently seen in K data from all three observatory groups can be reasonably interpreted as physically meaninginful: (1) geomagnetic activity has generally increased over the past 141 years. However, the detailed secular evolution of geomagnetic activity is not well characterized by either a linear trend nor, even, a monotonic trend. Therefore, simple, phenomenological extrapolations of past trends in solar and geomagnetic activity levels are unlikely to be useful for making quantitative predictions of future trends lasting longer than a solar cycle or so. (2) The well-known tendency for magnetic storms to occur during the declining phase of a sunspot-solar cycles is clearly seen for cycles 14-23; it is not, however, clearly seen for cycles 11-13. Therefore, in addition to an increase in geomagnetic activity, the nature of solar-terrestrial interaction has also apparently changed over the past 141 years.
C1 US Geol Survey, Geomagnetism Program, Denver, CO 80225 USA.
RP Love, JJ (reprint author), US Geol Survey, Geomagnetism Program, Box 25046, Denver, CO 80225 USA.
EM jlove@usgs.gov
RI Love, Jeffrey/N-7593-2013
OI Love, Jeffrey/0000-0002-3324-0348
NR 66
TC 11
Z9 11
U1 0
U2 4
PU COPERNICUS GESELLSCHAFT MBH
PI GOTTINGEN
PA BAHNHOFSALLEE 1E, GOTTINGEN, 37081, GERMANY
SN 0992-7689
EI 1432-0576
J9 ANN GEOPHYS-GERMANY
JI Ann. Geophys.
PY 2011
VL 29
IS 2
BP 251
EP 262
DI 10.5194/angeo-29-251-2011
PG 12
WC Astronomy & Astrophysics; Geosciences, Multidisciplinary; Meteorology &
Atmospheric Sciences
SC Astronomy & Astrophysics; Geology; Meteorology & Atmospheric Sciences
GA 727LG
UT WOS:000287800700004
ER
PT J
AU Stith, BM
Reid, JP
Langtimm, CA
Swain, ED
Doyle, TJ
Slone, DH
Decker, JD
Soderqvist, LE
AF Stith, Bradley M.
Reid, James P.
Langtimm, Catherine A.
Swain, Eric D.
Doyle, Terry J.
Slone, Daniel H.
Decker, Jeremy D.
Soderqvist, Lars E.
TI Temperature Inverted Haloclines Provide Winter Warm-Water Refugia for
Manatees in Southwest Florida
SO ESTUARIES AND COASTS
LA English
DT Article
DE Thermal inversion; Halocline; Stratification; Passive thermal refugia;
Picayune Strand restoration; Everglades restoration; Aerial survey;
Satellite telemetry; Climate change; Aquatic species
ID SWAN RIVER ESTUARY; NUTRIENT DISCHARGE; THERMAL REFUGIA; SURFACE-WATER;
GROUNDWATER; SALINITY; CANALS; SITE
AB Florida manatees (Trichechus manatus latirostris) overwintering in the Ten Thousand Islands and western Everglades have no access to power plants or major artesian springs that provide warm-water refugia in other parts of Florida. Instead, hundreds of manatees aggregate at artificial canals, basins, and natural deep water sites that act as passive thermal refugia (PTR). Monitoring at two canal sites revealed temperature inverted haloclines, which provided warm salty bottom layers that generally remained above temperatures considered adverse for manatees. At the largest PTR, the warmer bottom layer disappeared unless significant salt stratification was maintained by upstream freshwater inflow over a persistent tidal wedge. A detailed three-dimensional hydrology model showed that salinity stratification inhibited vertical convection induced by atmospheric cooling. Management or creation of temperature inverted haloclines may be a feasible and desirable option for resource managers to provide passive thermal refugia for manatees and other temperature sensitive aquatic species.
C1 [Stith, Bradley M.; Reid, James P.; Langtimm, Catherine A.; Slone, Daniel H.] US Geol Survey, SE Ecol Sci Ctr, Gainesville, FL 32605 USA.
[Swain, Eric D.; Decker, Jeremy D.] US Geol Survey, Florida Water Sci Ctr, Ft Lauderdale, FL 33315 USA.
[Doyle, Terry J.] US Fish & Wildlife Serv, Arlington, VA 22203 USA.
[Soderqvist, Lars E.] US Geol Survey, Florida Water Sci Ctr Ft Myers, Ft Myers, FL 33901 USA.
RP Stith, BM (reprint author), US Geol Survey, SE Ecol Sci Ctr, 2201 NW 40th Terrace, Gainesville, FL 32605 USA.
EM bstith@usgs.gov
OI Slone, Daniel/0000-0002-9903-9727; Reid, James/0000-0002-8497-1132
FU USGS
FX We wish to thank the following agencies for hydrology or environmental
data: South Florida Water Management District, Rookery Bay National
Estuarine Research Reserve, National Oceanic and Atmospheric
Administration, Everglades National Park, Big Cypress National Preserve,
Ten Thousand Islands National Wildlife Refuge, Florida Automated Weather
Network of the University of Florida Institute of Food and Agriculture
Extension, and United States Geological Survey. We thank the Fish and
Wildlife Research Institute division of the Florida Fish and Wildlife
Conservation Commission for synoptic aerial survey data. We thank Susan
Butler and Dean Easton for their help with data acquisition and Andrea
Bowling for manuscript proofing. Partial funding was provided by the
following USGS programs: Place-Based Studies (PBS), Priority Ecosystems
Science (PES), and Critical Ecosystem Studies Initiative (CESI). Use of
trade or product names does not imply endorsement by the U.S.
Government. The findings and conclusions in this article are those of
the authors and do not necessarily represent the views of the U.S. Fish
and Wildlife Service.
NR 54
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Z9 8
U1 4
U2 23
PU SPRINGER
PI NEW YORK
PA 233 SPRING ST, NEW YORK, NY 10013 USA
SN 1559-2723
J9 ESTUAR COAST
JI Estuaries Coasts
PD JAN
PY 2011
VL 34
IS 1
BP 106
EP 119
DI 10.1007/s12237-010-9286-1
PG 14
WC Environmental Sciences; Marine & Freshwater Biology
SC Environmental Sciences & Ecology; Marine & Freshwater Biology
GA 718VY
UT WOS:000287155800009
ER
PT J
AU Feyrer, F
Newman, K
Nobriga, M
Sommer, T
AF Feyrer, Frederick
Newman, Ken
Nobriga, Matthew
Sommer, Ted
TI Modeling the Effects of Future Outflow on the Abiotic Habitat of an
Imperiled Estuarine Fish
SO ESTUARIES AND COASTS
LA English
DT Article
DE Delta smelt; Native fish; Annual species; Sacramento-San Joaquin Delta;
San Francisco Estuary; Climate change; Abiotic habitat; Future
development; Generalized additive model
ID SAN-FRANCISCO ESTUARY; FRESH-WATER FLOW; CLIMATE-CHANGE; CALIFORNIA;
RESTORATION; COLLAPSE; IMPACTS; SALMON
AB Future development and climate change pose potentially serious threats to estuarine fish populations around the world. We examined how habitat suitability for delta smelt (Hypomesus transpacificus), a state and federally protected species, might be affected by changes in outflow in the San Francisco Estuary due to future development and climate change. Forty years of sampling data collected during fall from 1967 to 2008 were examined to define abiotic habitat suitability for delta smelt as a function of salinity and water transparency, and to describe long-term trends in habitat conditions. The annual habitat index we developed, which incorporated both quantity and quality of habitat, decreased by 78% over the study period. Future habitat index values under seven different development and climate change scenarios, representing a range of drier and wetter possibilities, were predicted using a model which related estuarine outflow to the habitat index. The results suggested that each of the scenarios would generally lead to further declines in delta smelt habitat across all water year types. Recovery targets for delta smelt will be difficult to attain if the modeled habitat conditions are realized.
C1 [Feyrer, Frederick] US Bur Reclamat, Appl Sci Branch, Sacramento, CA 95825 USA.
[Newman, Ken] US Fish & Wildlife Serv, Stockton, CA 95205 USA.
[Nobriga, Matthew] US Fish & Wildlife Serv, Bay Delta Fish & Wildlife Off, Sacramento, CA 95814 USA.
RP Feyrer, F (reprint author), US Bur Reclamat, Appl Sci Branch, 2800 Cottage Way, Sacramento, CA 95825 USA.
EM ffeyrer@usbr.gov
NR 37
TC 19
Z9 19
U1 3
U2 21
PU SPRINGER
PI NEW YORK
PA 233 SPRING ST, NEW YORK, NY 10013 USA
SN 1559-2723
J9 ESTUAR COAST
JI Estuaries Coasts
PD JAN
PY 2011
VL 34
IS 1
BP 120
EP 128
DI 10.1007/s12237-010-9343-9
PG 9
WC Environmental Sciences; Marine & Freshwater Biology
SC Environmental Sciences & Ecology; Marine & Freshwater Biology
GA 718VY
UT WOS:000287155800010
ER
PT J
AU Llewellyn, C
La Peyre, M
AF Llewellyn, Chris
La Peyre, Megan
TI Evaluating Ecological Equivalence of Created Marshes: Comparing
Structural Indicators with Stable Isotope Indicators of Blue Crab
Trophic Support
SO ESTUARIES AND COASTS
LA English
DT Article
DE Blue crab; Louisiana; Ecological equivalence; Dredged marsh;
Restoration; Stable isotopes
ID COMMUNITY-WIDE MEASURES; SALT-MARSH; RATIOS PROVIDE; DIET; RESTORATION;
ECOSYSTEM; HABITATS; ANIMALS; CARBON; DELTA-N-15
AB This study sought to examine ecological equivalence of created marshes of different ages using traditional structural measures of equivalence, and tested a relatively novel approach using stable isotopes as a measure of functional equivalence. We compared soil properties, vegetation, nekton communities, and delta(13)C and delta(15)N isotope values of blue crab muscle and hepatopancreas tissue and primary producers at created (5-24 years old) and paired reference marshes in SW Louisiana. Paired contrasts indicated that created and reference marshes supported equivalent plant and nekton communities, but differed in soil characteristics. Stable isotope indicators examining blue crab food web support found that the older marshes (8 years+) were characterized by comparable trophic diversity and breadth compared to their reference marshes. Interpretation of results for the youngest site was confounded by the fact that the paired reference, which represented the desired end goal of restoration, contained a greater diversity of basal resources. Stable isotope techniques may give coastal managers an additional tool to assess functional equivalency of created marshes, as measured by trophic support, but may be limited to comparisons of marshes with similar vegetative communities and basal resources, or require the development of robust standardization techniques.
C1 [La Peyre, Megan] Louisiana State Univ AgCtr, Sch Renewable Nat Resources, Louisiana Fish & Wildlife Cooperat Res Unit, USGS, Baton Rouge, LA 70803 USA.
RP La Peyre, M (reprint author), Louisiana State Univ AgCtr, Sch Renewable Nat Resources, Louisiana Fish & Wildlife Cooperat Res Unit, USGS, Baton Rouge, LA 70803 USA.
EM mlapey@lsu.edu
FU Louisiana Department of Wildlife and Fisheries
FX This project could not have been completed without the help of Whitney
Gayle, Bryan Gossman, Katie Llewellyn, Bryan Piazza, and Mason Piehler
who worked tirelessly in the lab and field. Raw data for this work are
available in the electronic thesis by C. Llewellyn
(http://etd.lsu.edu/docs/available/etd-10282008-094243/unrestricted/llew
ellynthesis.pdf). Thanks to Dr. Jerome La Peyre for use of the wetlab
space. Dr. Brian Fry provided invaluable insight and help with the
stable isotope analyses and extremely helpful comments on various
versions of this manuscript. Dr. Ken Brown provided valuable comments
that improved the manuscript. Dr. Heather Haas provided significant
comments that greatly improved the manuscript. This project was funded
by the Louisiana Department of Wildlife and Fisheries. Mention of trade
names does not imply endorsement from the U. S. government.
NR 39
TC 1
Z9 1
U1 3
U2 35
PU SPRINGER
PI NEW YORK
PA 233 SPRING ST, NEW YORK, NY 10013 USA
SN 1559-2723
J9 ESTUAR COAST
JI Estuaries Coasts
PD JAN
PY 2011
VL 34
IS 1
BP 172
EP 184
DI 10.1007/s12237-010-9297-y
PG 13
WC Environmental Sciences; Marine & Freshwater Biology
SC Environmental Sciences & Ecology; Marine & Freshwater Biology
GA 718VY
UT WOS:000287155800014
ER
PT J
AU La Peyre, MK
Gossman, B
Piazza, BP
AF La Peyre, Megan K.
Gossman, Bryan
Piazza, Bryan P.
TI Short- and Long-Term Response of Deteriorating Brackish Marshes and
Open-Water Ponds to Sediment Enhancement by Thin-Layer Dredge Disposal
(vol 32, pg 390, 2010)
SO ESTUARIES AND COASTS
LA English
DT Correction
C1 [La Peyre, Megan K.] Louisiana State Univ, Ctr Agr, Louisiana Fish & Wildlife Cooperat Res Unit, Sch Renewable Nat Resources,US Geol Survey, Baton Rouge, LA 70803 USA.
RP La Peyre, MK (reprint author), Louisiana State Univ, Ctr Agr, Louisiana Fish & Wildlife Cooperat Res Unit, Sch Renewable Nat Resources,US Geol Survey, Baton Rouge, LA 70803 USA.
EM mlapey@lsu.edu
NR 1
TC 0
Z9 0
U1 0
U2 5
PU SPRINGER
PI NEW YORK
PA 233 SPRING ST, NEW YORK, NY 10013 USA
SN 1559-2723
J9 ESTUAR COAST
JI Estuaries Coasts
PD JAN
PY 2011
VL 34
IS 1
BP 185
EP 186
DI 10.1007/s12237-010-9339-5
PG 2
WC Environmental Sciences; Marine & Freshwater Biology
SC Environmental Sciences & Ecology; Marine & Freshwater Biology
GA 718VY
UT WOS:000287155800015
ER
PT J
AU Vos, SM
Ribic, CA
AF Vos, Susan M.
Ribic, Christine A.
TI Grassland Bird Use of Oak Barrens and Dry Prairies in Wisconsin
SO NATURAL AREAS JOURNAL
LA English
DT Article
DE dry sand prairie; grassland birds; oak barrens; patch size
ID POPULATION TRENDS; NORTH-AMERICA; HABITAT; COMMUNITIES; VEGETATION;
LANDSCAPE; SPARROWS; FIELDS; AREA
AB Grassland bird populations have declined more than any other group of birds in North America and are of conservation concern to state and federal agencies. We determined relative abundances of grassland birds in oak barrens and dry sand prairies native habitat types rare in the state of Wisconsin. We also investigated the association of relative abundance, patch size, and patch vegetation. Our study was conducted May-July 2000-2002 on Fort McCoy Military Installation in Monroe County, Wisconsin. Fourteen grassland bird species were found in native habitat patches. Vesper sparrow (Pooecetes gramineus), grasshopper sparrow (Ammodramus savannarum), and field sparrow (Spizella pusilla) were the most abundant grassland bird species; all are species of management concern in Wisconsin. Of the most abundant species, only grasshopper sparrow relative abundance increased as patch size increased; vesper sparrow and field sparrow relative abundances decreased as patch size increased. Though found at lower relative abundances, horned larks (Erephila alpestris), savannah sparrows (Passerculus sandwichensis), and upland sandpipers (Bartramia longicauda) were found at higher relative abundances as patch size increased. Patch vegetation was important for some species. Vesper sparrows were found at higher abundances in patches with shorter, less dense vegetation and higher woody cover, eastern meadowlark (Sturnella magna) relative abundances were higher in patches with higher proportions of grass, and dickcissel (Spiza americana) relative abundances were higher in patches with taller, denser vegetation and lower proportions of litter. Native habitats are important for grassland bird species of management concern and large patches are particularly important for some of them.
C1 [Ribic, Christine A.] Univ Wisconsin, US Geol Survey, Wisconsin Cooperat Wildlife Res Unit, Dept Forest & Wildlife Ecol, Madison, WI 53706 USA.
RP Ribic, CA (reprint author), Univ Wisconsin, US Geol Survey, Wisconsin Cooperat Wildlife Res Unit, Dept Forest & Wildlife Ecol, Madison, WI 53706 USA.
EM caribic@wisc.edu
FU U.S. Department of Defense; University of Tennessee; Wisconsin
Department of Natural Resources; U.S. Geological Survey, Wisconsin
Cooperative Wildlife Research Unit
FX We thank the staff biologists at Fort McCoy Military Installation for
their invaluable help: K. Mello, D. Beckmann, B. Friedl, and T. Wilder.
We thank the radio staff in Range Control and the schedulers, M.
Stelzner (Ranger) and D. Wetuski (Ski), for coordinating with the field
team and providing invaluable guidance while conducting research on the
Installation. In addition, we thank the technicians involved in the
study: M. Guzy, T. Backus, A. Weber, J. Cianciolo, D. Williams, M.
Weindant, K. Ruekheim, K. Sash, K. Repyack, L. Braggs, and D. Jones. We
thank D. Sample for his help in establishing this project. We thank two
anonymous reviewers for their comments. This work was supported by the
U.S. Department of Defense Legacy Project as a subcontract with the
University of Tennessee; additional funding was provided by the
Wisconsin Department of Natural Resources and the U.S. Geological
Survey, Wisconsin Cooperative Wildlife Research Unit. We thank The
Department of Forest and Wildlife Ecology, University of Wisconsin,
Madison, for assistance with publication expenses. Mention of trade
names or commercial products does not imply endorsement by the U.S.
government.
NR 35
TC 1
Z9 2
U1 2
U2 13
PU NATURAL AREAS ASSOC
PI ROCKFORD
PA 320 SOUTH THIRD ST, ROCKFORD, IL 61104 USA
SN 0885-8608
EI 2162-4399
J9 NAT AREA J
JI Nat. Areas J.
PD JAN
PY 2011
VL 31
IS 1
BP 26
EP 33
PG 8
WC Ecology; Forestry
SC Environmental Sciences & Ecology; Forestry
GA 716TZ
UT WOS:000286997700004
ER
PT J
AU Duncan, WW
Goodloe, RB
Meyer, JL
Prowell, ES
AF Duncan, William W.
Goodloe, Robin B.
Meyer, Judy L.
Prowell, Eric S.
TI Does Channel Incision Affect In-stream Habitat? Examining the Effects of
Multiple Geomorphic Variables on Fish Habitat
SO RESTORATION ECOLOGY
LA English
DT Article
DE bed mobility; entrenchment; incision; macrophyte; Podostemum
ceratophyllum; Rosgen Classification of Natural Rivers
ID SOUTHERN APPALACHIAN RIVER; ASSEMBLAGE STRUCTURE; PIEDMONT RIVER; USA;
HOMOGENIZATION; URBANIZATION; REGIME; BASIN
AB Incised river channels are dynamic components of fluvial systems, represent geomorphic degradation, and are encountered worldwide. Ecological effects of incision can be far-reaching, affecting habitat availability and channel processes. Although incision can reflect habitat degradation, some studies suggest that important in-stream habitats do not differ with the degree of incision. Therefore, we tested whether in-stream habitat variables that are important to imperiled fishes differ in river reaches with varying degrees of incision. Because incision (measured using entrenchment ratio) had no discernable effect on in-stream habitat characteristics (i.e., proportion fines, gravel, cobble, and macrophyte occurrence and length), we expanded our analysis to assess the effects of 29 additional geomorphic variables on in-stream habitat. These analyses indicated that bank height, bed mobility, D(84), cross-sectional area, bankfull width, and wetted perimeter accounted for 42% of macrophyte occurrence and 64% of macrophyte length variance. Postflood surveys indicated that macrophyte occurrence on cobble declined as bank height and bed mobility increased, and sediment size decreased, suggesting that sediment size and bed mobility have a stronger influence on in-stream habitat than incision. Although channel incision often indicates environmental degradation, important aspects of habitat are not described by this measurement. Strategies that depend on incision to identify restoration sites may have limited habitat benefits in Southeastern Piedmont streams and rivers. Instead, landscape or shoal-scale restoration approaches that increase coarse sediment proportions may increase macrophyte occurrence, length, and persistence. Sediment budgets that identify coarse and fine sediment sources and transport may be useful to prioritize restoration approaches.
C1 [Duncan, William W.; Meyer, Judy L.] Univ Georgia, Odum Sch Ecol, Athens, GA 30602 USA.
[Goodloe, Robin B.; Prowell, Eric S.] US Fish & Wildlife Serv, Ecol Serv, Athens, GA 30605 USA.
RP Duncan, WW (reprint author), Univ Georgia, Odum Sch Ecol, Athens, GA 30602 USA.
EM wduncan1701@gmail.com
NR 41
TC 3
Z9 4
U1 4
U2 18
PU WILEY-BLACKWELL
PI MALDEN
PA COMMERCE PLACE, 350 MAIN ST, MALDEN 02148, MA USA
SN 1061-2971
J9 RESTOR ECOL
JI Restor. Ecol.
PD JAN
PY 2011
VL 19
IS 1
BP 64
EP 73
DI 10.1111/j.1526-100X.2009.00534.x
PG 10
WC Ecology
SC Environmental Sciences & Ecology
GA 704AV
UT WOS:000286024400008
ER
PT J
AU Jackson, JC
Horton, JW
Chou, IM
Belkin, HE
AF Jackson, John C.
Horton, J. Wright, Jr.
Chou, I-Ming
Belkin, Harvey E.
TI Monoclinic tridymite in clast-rich impact melt rock from the Chesapeake
Bay impact structure
SO AMERICAN MINERALOGIST
LA English
DT Article
DE Monoclinic tridymite; quartz paramorph after tridymite; cristobalite;
Chesapeake Bay impact structure
ID X-RAY; ORTHORHOMBIC MODIFICATION; HIGHER TEMPERATURE; CRISTOBALITE;
SUPERSTRUCTURE; SILICA; PHASE; RAMAN; CRYSTALLIZATION; TRANSFORMATION
AB X-ray diffraction and Raman spectroscopy confirm a rare terrestrial occurrence of monoclinic tridymite in clast-rich impact melt rock from the Eyreville B drill core in the Chesapeake Bay impact structure. The monoclinic tridymite occurs with quartz paramorphs after tridymite and K-feldspar in a microcrystalline groundmass of devitrified glass and Fe-rich smectite. Electron-microprobe analyses revealed that the tridymite and quartz paramorphs after tridymite contain different amounts of chemical impurities. Inspection by SEM showed that the tridymite crystal surfaces are smooth, whereas the quartz paramorphs contain irregular tabular voids. These voids may represent microporosity formed by volume decrease in the presence of fluid during transformation from tridymite to quartz, or skeletal growth in the original tridymite. Cristobalite locally rims spherulites within the same drill core interval. The occurrences of tridymite and cristobalite appear to be restricted to the thickest clast-rich impact melt body in the core at 1402.02-1407.49 m depth. Their formation and preservation in an alkali-rich, high-silica melt rock suggest initially high temperatures followed by rapid cooling.
C1 [Jackson, John C.; Horton, J. Wright, Jr.; Chou, I-Ming; Belkin, Harvey E.] US Geol Survey, Natl Ctr, Reston, VA 20192 USA.
RP Jackson, JC (reprint author), US Geol Survey, Natl Ctr, Reston, VA 20192 USA.
EM jjackson@usgs.gov
OI Belkin, Harvey/0000-0001-7879-6529
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PU MINERALOGICAL SOC AMER
PI CHANTILLY
PA 3635 CONCORDE PKWY STE 500, CHANTILLY, VA 20151-1125 USA
SN 0003-004X
J9 AM MINERAL
JI Am. Miner.
PD JAN
PY 2011
VL 96
IS 1
BP 81
EP 88
DI 10.2138/am.2011.3589
PG 8
WC Geochemistry & Geophysics; Mineralogy
SC Geochemistry & Geophysics; Mineralogy
GA 703OP
UT WOS:000285988400010
ER
PT J
AU Vogel, JR
Linard, JI
AF Vogel, J. R.
Linard, J. I.
TI AGRICULTURAL HERBICIDE TRANSPORT IN A FIRST-ORDER INTERMITTENT STREAM,
NEBRASKA, USA
SO APPLIED ENGINEERING IN AGRICULTURE
LA English
DT Article
DE Herbicides; Contaminant transport; Degradates; Mass load
ID ORGANIC-MATTER; SURFACE WATERS; GLYPHOSATE; SOILS; ADSORPTION; ATRAZINE;
SCALE; PESTICIDES; PHOSPHATE; BEHAVIOR
AB The behavior of herbicides in surface waters is a function of many variables, including scale of the watershed, physical and chemical properties of the herbicide, physical and chemical properties of the soil, rainfall intensity, and time of year. In this study, the transport of 6 herbicides and 12 herbicide degradates was examined during the 2004 growing season in an intermediate-scale agricultural watershed (146 ha) that is drained by a first-order intermittent stream, and the mass load for each herbicide in the stream was estimated. The herbicide load during the first week of storm events after application ranged from 17% of annual load for trifluralin to 84% of annual load for acetochlor. The maximum weekly herbicide load in the stream was generally within the first 3 weeks after application for those compounds that were applied within the watershed during 2004, and later for herbicides not applied within the watershed during 2004 but still detected in the stream. The apparent dominant mode of herbicide transport in the stream-determined by analysis amongst herbicide and conservative ion concentrations at different points in the hydrograph and in base flow samples-was either overland runoff or shallow subsurface flow, depending on the elapsed time after application and type of herbicide. The load as a percentage of use (LAPU) for the parent compounds in this study was similar to literature values for those compounds applied by the farmer within the watershed, but smaller for those herbicides that had rainfall as their only source within the watershed.
C1 [Vogel, J. R.] Oklahoma State Univ, Biosyst & Agr Engn Dept, Stillwater, OK 74078 USA.
[Linard, J. I.] US Geol Survey, Colorado Water Sci Ctr, Grand Junction, CO USA.
RP Vogel, JR (reprint author), Oklahoma State Univ, Biosyst & Agr Engn Dept, 218 Ag Hall, Stillwater, OK 74078 USA.
EM jason.vogel@okstate.edu
FU U.S. Geological Survey (USGS)
FX This research was supported by the U.S. Geological Survey (USGS)
National Water-Quality Assessment (NAWQA) Program. The authors would
like to express their thanks for the interpretative guidance provided by
Paul Capel (USGS), Joseph Domagalski (USGS), and Ronald Zelt (USGS).
Numerous USGS colleagues assisted with installation, sample collection,
and data management, and their involvement in the successful completion
of the project was invaluable. Finally, we would like to thank the
landowners in the watershed for their cooperation during this project.
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PU AMER SOC AGRICULTURAL & BIOLOGICAL ENGINEERS
PI ST JOSEPH
PA 2950 NILES RD, ST JOSEPH, MI 49085-9659 USA
SN 0883-8542
J9 APPL ENG AGRIC
JI Appl. Eng. Agric.
PD JAN
PY 2011
VL 27
IS 1
BP 63
EP 74
PG 12
WC Agricultural Engineering
SC Agriculture
GA 727CG
UT WOS:000287774500007
ER
PT J
AU Jones, JW
Neves, RJ
AF Jones, Jess W.
Neves, Richard J.
TI Influence of life-history variation on demographic responses of three
freshwater mussel species (Bivalvia: Unionidae) in the Clinch River, USA
SO AQUATIC CONSERVATION-MARINE AND FRESHWATER ECOSYSTEMS
LA English
DT Article
DE Clinch River; freshwater mussels; Epioblasma brevidens; Epioblasma
capsaeformis; Lampsilis fasciola; life history and demographic
variation; age; shell growth; population size; recruitment
ID FLORENTINA-WALKERI BIVALVIA; POPULATION REGULATION; K-SELECTION;
R-SELECTION; GROWTH; PEARLYMUSSEL; VIRGINIA; ASSEMBLAGES; PROPAGATION;
RECRUITMENT
AB 1. Variation in age, shell growth, and demographic responses of two endangered mussel species, Epioblasma brevidens and Epioblasma capsaeformis, and a third non-listed species, Lampsilis fasciola, were studied from 2004-2008 in a 32-km reach of the Clinch River, TN.
2. Observed maximum age and length of E. brevidens was 28 yr and 71.5 mm for males and 15 yr and 56.6 mm for females; of E. capsaeformis, 12 yr and 54.6 mm for males and 9 yr and 48.6 mm for females; and of L. fasciola, 45 yr and 91.3 mm for males and 24 yr and 79.8 mm for females.
3. Estimated population size was similar to 46 000 individuals for E. brevidens, similar to 862 000 individuals for E. capsaeformis, and similar to 33 000 individuals for L. fasciola.
4. Mean recruitment per year of 1 yr-olds ranged from 12.0% to 24.0% for E. brevidens, 4.2% to 56.6% for E. capsaeformis, and 10.0% to 38.5% for L. fasciola, and mean annual population growth rate was 21.0%, 31.3%, and -24.3%, respectively.
5. Juveniles were detectable but temporally and spatially variable in occurrence, and a significant proportion of the age-class structure of each species. Recruitment was exceptionally high for E. capsaeformis during years when discharge was low in spring and summer.
6. Population size, growth, recruitment, and mortality rates of the shorter-lived E. capsaeformis were correspondingly higher than those of E. brevidens and L. fasciola.
7. The federal recovery plan for E. brevidens and E. capsaeformis identifies quantification of demographic variables as a critical step toward meeting the recovery needs of each species. The data collected in this study begin to meet these needs and can be used to monitor and evaluate population performance of each species. Published in 2011 by John Wiley & Sons, Ltd.
C1 [Jones, Jess W.] Virginia Polytech Inst & State Univ, Dept Fisheries & Wildlife Sci, US Fish & Wildlife Serv, Blacksburg, VA 24061 USA.
RP Jones, JW (reprint author), Virginia Polytech Inst & State Univ, Dept Fisheries & Wildlife Sci, US Fish & Wildlife Serv, Blacksburg, VA 24061 USA.
EM Jess_Jones@fws.gov
FU US Fish and Wildlife Service (USFWS); Tennessee Wildlife Resources
Agency (TWRA)
FX Financial support for this project was provided by the US Fish and
Wildlife Service (USFWS) and the Tennessee Wildlife Resources Agency
(TWRA). Special thanks are owed to the many people who helped us conduct
the field work for this project, to include: Steve Ahlstedt, US
Geological Survey (Retired); Don Hubbs, TWRA; Braven Beaty, The Nature
Conservancy; Robert Butler, Geoff Call, Brian Evans, Shane Hanlon,
Matthew Patterson, and Brian Tompkins, USFWS; Craig Walker, Office of
Surface Mining; Nathan Eckert, Joe Ferraro, Mike Pinder, Melanie Stein,
and Brian Watson, Virginia Department of Game and Inland Fisheries;
Richard Davis, Virginia Department of Mines, Minerals and Energy; Amy
Bush, Dan Hua and her son Kenneth, Jay McGhee, Nathan Johnson, Matt
Johnson, Nick King, Missy Petty, Brett Ostby, James Vance, and Meghann
Vincie, Virginia Tech University; and Chris Isaac, Travis Lowe and
Quentin Tolliver, Appalachian Technical Services. The views expressed in
this publication are those of the authors and do not necessarily
represent the views of the USFWS.
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PU JOHN WILEY & SONS LTD
PI CHICHESTER
PA THE ATRIUM, SOUTHERN GATE, CHICHESTER PO19 8SQ, W SUSSEX, ENGLAND
SN 1052-7613
J9 AQUAT CONSERV
JI Aquat. Conserv.-Mar. Freshw. Ecosyst.
PD JAN-FEB
PY 2011
VL 21
IS 1
BP 57
EP 73
DI 10.1002/aqc.1161
PG 17
WC Environmental Sciences; Marine & Freshwater Biology; Water Resources
SC Environmental Sciences & Ecology; Marine & Freshwater Biology; Water
Resources
GA 718ZD
UT WOS:000287164300007
ER
PT J
AU Nielsen, JL
Turner, SM
Zimmerman, CE
AF Nielsen, Jennifer L.
Turner, Sara M.
Zimmerman, Christian E.
TI Electronic tags and genetics explore variation in migrating steelhead
kelts (Oncorhynchus mykiss), Ninilchik River, Alaska
SO CANADIAN JOURNAL OF FISHERIES AND AQUATIC SCIENCES
LA English
DT Article
ID IMPLANTED DUMMY TRANSMITTERS; JUVENILE ATLANTIC SALMON; DATA-STORAGE
TAGS; BRITISH-COLUMBIA; PACIFIC SALMON; RAINBOW-TROUT; LIFE-HISTORY;
WILD STEELHEAD; CHINOOK SALMON; BROWN TROUT
AB Acoustic and archival tags examined freshwater and marine migrations of postspawn steelhead kelts (Oncorhynchus mykiss) in the Ninilchik River, Alaska, USA. Postspawn steelhead were captured at a weir in 2002-2005. Scale analysis indicated multiple migratory life histories and spawning behaviors. Acoustic tags were implanted in 99 kelts (2002-2003), and an array of acoustic receivers calculated the average speed of outmigration, timing of saltwater entry, and duration of residency in the vicinity of the river mouth. Ocean migration data were recovered from two archival tags implanted in kelts in 2004 (one male and one female). Archival tags documented seasonal differences in maximum depth and behavior with both fish spending 97% of time at sea <6 m depth (day and night). All study fish were double tagged with passive integrated transponder (PIT) tags implanted in the body cavity. Less than 4% of PIT tags were retained in postspawn steelhead. Molecular genetics demonstrated no significant differences in genetic population structure across years or among spawning life history types, suggesting a genetically panmictic population with highly diverse life history characteristics in the Ninilchik River.
C1 [Nielsen, Jennifer L.; Turner, Sara M.; Zimmerman, Christian E.] US Geol Survey, Alaska Sci Ctr, Anchorage, AK 99508 USA.
RP Nielsen, JL (reprint author), US Geol Survey, Alaska Sci Ctr, 4210 Univ Dr, Anchorage, AK 99508 USA.
EM jlnielsen@usgs.gov
OI Zimmerman, Christian/0000-0002-3646-0688
FU Census of Marine Life; USGS Alaska Science Center; Pacific Ocean Shelf
Tracking Project
FX The authors thank Derek Wilson, Sara Graziano, Phil Richards, Julie
Carter, Mike Booz, and Thor Tingey for assistance in the field and
laboratory. Permits from the Ninilchik Native Association facilitated
weir operations. Assistance by several Alaska Fish and Game biologists
was critical to successful weir construction and operation. Use of
original beta-archival tags for salmon was done under a memorandum of
understanding between USGS and Lotek Wireless, Inc. Dan Mulcahy provided
training for surgical implantation of transmitters and assisted with
sterilization of surgical gear and tags. This work was partially funded
by the Census of Marine Life, Pacific Ocean Shelf Tracking Project, and
the USGS Alaska Science Center. Comments and suggestions by Trey Walker
and Erika Ammann greatly improved the manuscript. Mention of trade names
does not imply US Government endorsement.
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PU CANADIAN SCIENCE PUBLISHING, NRC RESEARCH PRESS
PI OTTAWA
PA 65 AURIGA DR, SUITE 203, OTTAWA, ON K2E 7W6, CANADA
SN 0706-652X
EI 1205-7533
J9 CAN J FISH AQUAT SCI
JI Can. J. Fish. Aquat. Sci.
PD JAN
PY 2011
VL 68
IS 1
BP 1
EP 16
DI 10.1139/F10-124
PG 16
WC Fisheries; Marine & Freshwater Biology
SC Fisheries; Marine & Freshwater Biology
GA 718SK
UT WOS:000287146300001
ER
PT J
AU Reddy, KR
Best, GR
Sklar, F
AF Reddy, K. R.
Best, G. R.
Sklar, F.
TI Biogeochemistry and Water Quality of the Everglades: Symposium Overview
SO CRITICAL REVIEWS IN ENVIRONMENTAL SCIENCE AND TECHNOLOGY
LA English
DT Editorial Material
C1 [Reddy, K. R.] Univ Florida, Gainesville, FL 32610 USA.
[Best, G. R.] US Geol Survey, Ft Lauderdale, FL USA.
[Sklar, F.] S Florida Water Management Dist, W Palm Beach, FL USA.
RP Reddy, KR (reprint author), Univ Florida, Gainesville, FL 32610 USA.
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PI PHILADELPHIA
PA 325 CHESTNUT ST, SUITE 800, PHILADELPHIA, PA 19106 USA
SN 1064-3389
J9 CRIT REV ENV SCI TEC
JI Crit. Rev. Environ. Sci. Technol.
PY 2011
VL 41
SU 1
BP 1
EP 3
AR PII 933736937
DI 10.1080/10643389.2010.530920
PG 3
WC Environmental Sciences
SC Environmental Sciences & Ecology
GA 723GG
UT WOS:000287494000001
ER
PT J
AU McCormick, PV
Harvey, JW
Crawford, ES
AF McCormick, Paul V.
Harvey, Judson W.
Crawford, Eric S.
TI Influence of Changing Water Sources and Mineral Chemistry on the
Everglades Ecosystem
SO CRITICAL REVIEWS IN ENVIRONMENTAL SCIENCE AND TECHNOLOGY
LA English
DT Review
DE conductivity; Everglades; hydrology; minerotrophy; peatlands;
periphyton; vegetation; wetlands
ID LOST RIVER PEATLAND; NORTHERN MINNESOTA; FLORIDA EVERGLADES; EUROPEAN
MIRES; SURFACE-WATER; SEED BANKS; VEGETATION; FENS; PHOSPHORUS;
GRADIENTS
AB Human influences during the previous century increased mineral inputs to the Florida Everglades by changing the sources and chemistry of surface inflows. Biogeochemical responses to this enrichment include changes in the availability of key limiting nutrients such as P, the potential for increased turnover of nutrient pools due to accelerated plant decomposition, and increased rates of mercury methylation associated with sulfate enrichment. Mineral enrichment has also been linked to the loss of sensitive macrophyte species, although dominant Everglades species appear tolerant of a broad range of mineral chemistry. Shifts in periphyton community composition and function provide an especially sensitive indicator of mineral enrichment. Understanding the influence of mineral chemistry on Everglades processes and biota may improve predictions of ecosystem responses to ongoing hydrologic restoration efforts and provide guidelines for protecting remaining mineral-poor areas of this peatland.
C1 [McCormick, Paul V.; Crawford, Eric S.] S Florida Water Management Dist, Restorat Sci Dept, W Palm Beach, FL 33406 USA.
[McCormick, Paul V.; Crawford, Eric S.] US Geol Survey, Leetown Sci Ctr, Kearneysville, WV USA.
[Harvey, Judson W.] US Geol Survey, Natl Ctr, Reston, VA 22092 USA.
RP McCormick, PV (reprint author), S Florida Water Management Dist, Restorat Sci Dept, 3301 Gun Club Rd, W Palm Beach, FL 33406 USA.
EM pmccormi@sfwmd.gov
RI Harvey, Judson/L-2047-2013
OI Harvey, Judson/0000-0002-2654-9873
FU USGS
FX This document was produced with support from the USGS Greater Everglades
Priority Ecosystem Science Program. Leslie MacGregor (A.R.M. Loxahatchee
National Wildlife Refuge) provided GIS and graphics support. Nick Aumen
(Everglades National Park), Laura Brandt (A.R.M. Loxahatchee National
Wildlife Refuge), and Joel Trexler (Florida International University)
reviewed an earlier draft of the document. A later draft was reviewed by
Joffre Castro (Everglades National Park), Paul Glaser (University of
Minnesota), Christopher McVoy (SFWMD), Martha Nungesser (SFWMD), Edward
Pendleton (USGS), Bruce Taggart (USGS), and Michael Waldon (A.R.M.
Loxahatchee National Wildlife Refuge). The final version was improved
with comments from two anonymous reviewers.
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PI PHILADELPHIA
PA 325 CHESTNUT ST, SUITE 800, PHILADELPHIA, PA 19106 USA
SN 1064-3389
J9 CRIT REV ENV SCI TEC
JI Crit. Rev. Environ. Sci. Technol.
PY 2011
VL 41
SU 1
BP 28
EP 63
AR PII 933735772
DI 10.1080/10643389.2010.530921
PG 36
WC Environmental Sciences
SC Environmental Sciences & Ecology
GA 723GG
UT WOS:000287494000003
ER
PT J
AU Jones, JW
AF Jones, John W.
TI Remote Sensing of Vegetation Pattern and Condition to Monitor Changes in
Everglades Biogeochemistry
SO CRITICAL REVIEWS IN ENVIRONMENTAL SCIENCE AND TECHNOLOGY
LA English
DT Review
DE biogeochemistry; remote sensing; vegetation pattern
ID ECOSYSTEM; FLORIDA
AB Ground-based studies of biogeochemistry and vegetation patterning yield process understanding, but the amount of information gained by ground-based studies can be greatly enhanced by efficient, synoptic, and temporally resolute monitoring afforded by remote sensing. The variety of presently available Everglades vegetation maps reflects both the wide range of application requirements and the need to balance cost and capability. More effort needs to be applied to documenting and understanding vegetation distribution and condition as indicators of biogeochemistry and contamination. Ground-based and remote sensing studies should be modified to maximize their synergy and utility for adaptive management.
C1 US Geol Survey, Eastern Geog Sci Ctr, Reston, VA 20192 USA.
RP Jones, JW (reprint author), US Geol Survey, Eastern Geog Sci Ctr, 521 Natl Ctr, Reston, VA 20192 USA.
EM jwjones@usgs.gov
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PI PHILADELPHIA
PA 325 CHESTNUT ST, SUITE 800, PHILADELPHIA, PA 19106 USA
SN 1064-3389
J9 CRIT REV ENV SCI TEC
JI Crit. Rev. Environ. Sci. Technol.
PY 2011
VL 41
SU 1
BP 64
EP 91
AR PII 933738372
DI 10.1080/10643389.2010.530924
PG 28
WC Environmental Sciences
SC Environmental Sciences & Ecology
GA 723GG
UT WOS:000287494000004
ER
PT J
AU Orem, W
Gilmour, C
Axelrad, D
Krabbenhoft, D
Scheidt, D
Kalla, P
McCormick, P
Gabriel, M
Aiken, G
AF Orem, William
Gilmour, Cynthia
Axelrad, Donald
Krabbenhoft, David
Scheidt, Daniel
Kalla, Peter
McCormick, Paul
Gabriel, Mark
Aiken, George
TI Sulfur in the South Florida Ecosystem: Distribution, Sources,
Biogeochemistry, Impacts, and Management for Restoration
SO CRITICAL REVIEWS IN ENVIRONMENTAL SCIENCE AND TECHNOLOGY
LA English
DT Review
DE Everglades; methylmercury; sulfate; sulfur; water quality
ID CLADIUM-JAMAICENSE CYPERACEAE; FERTILIZER-DERIVED URANIUM; FRESH-WATER
WETLANDS; NEW-JERSEY PINELANDS; TYPHA-DOMINGENSIS; EVERGLADES
RESTORATION; NORTHERN EVERGLADES; HYDROGEN SULFIDE; TROPHIC GRADIENT;
SULFATE
AB Sulfur is broadly recognized as a water quality issue of significance for the freshwater Florida Everglades. Roughly 60% of the remnant Everglades has surface water sulfate concentrations above 1 mg l-1, a restoration performance measure based on present sulfate levels in unenriched areas. Highly enriched marshes in the northern Everglades have average sulfate levels of 60 mg l-1. Sulfate loading to the Everglades is principally a result of land and water management in South Florida. The highest concentrations of sulfate (average 60-70 mg l-1) in the ecosystem are in canal water in the Everglades Agricultural Area (EAA). Potential sulfur sourcesin the watershed are many, but geochemical data and a preliminary sulfur mass balance for the EAA are consistent with sulfur presently used in agricultural, and sulfur released by oxidation of organic EAA soils (including legacy agricultural applications and natural sulfur) as the primary sources of sulfate enrichment in the EAA canals. Sulfate loading to the Everglades increases microbial sulfate reduction in soils, leading to more reducing conditions, greater cycling of nutrients in soils, production of toxic sulfide, and enhanced methylmercury (MeHg) production and bioaccumulation. Wetlands are zones of naturally high MeHg production, but the combination of high atmospheric mercury deposition rates in South Florida and elevated sulfate loading leads to increased MeHg production and MeHg risk to Everglades wildlife and human consumers. Sulfate from the EAA drainage canals penetrates deep into the Everglades Water Conservation Areas, and may extend into Everglades National Park. Present plans to restore sheet flow and to deliver more water to the Everglades may increase overall sulfur loads to the ecosystem, and move sulfate-enriched water further south. However, water management practices that minimize soil drying and rewetting cycles can mitigate sulfate release during soil oxidation. A comprehensive Everglades restoration strategy should include reduction of sulfur loads as a goal because of the many detrimental impacts of sulfate on the ecosystem. Monitoring data show that the ecosystem response to changes in sulfate levels is rapid, and strategies for reducing sulfate loading may be effective in the near term. A multifaceted approach employing best management practices for sulfur in agriculture, agricultural practices that minimize soil oxidation, and changes to stormwater treatment areas that increase sulfate retention could help achieve reduced sulfate loads to the Everglades, with resulting benefits.
C1 [Orem, William] US Geol Survey, Reston, VA 20192 USA.
[Gilmour, Cynthia] Smithsonian Environm Res Ctr, Edgewater, MD 21037 USA.
[Axelrad, Donald] Florida Dept Environm Protect, Tallahassee, FL USA.
[Krabbenhoft, David] US Geol Survey, Middleton, WI USA.
[Scheidt, Daniel; Kalla, Peter] US EPA, Athens, GA USA.
[McCormick, Paul; Gabriel, Mark] S Florida Water Management Dist, W Palm Beach, FL USA.
[Aiken, George] US Geol Survey, Boulder, CO USA.
RP Orem, W (reprint author), US Geol Survey, 959 Natl Ctr, Reston, VA 20192 USA.
EM borem@usgs.gov
RI Gilmour, Cynthia/G-1784-2010
OI Gilmour, Cynthia/0000-0002-1720-9498
FU U.S. Geological Survey; U.S. Environmental Protection Agency; National
Park Service; Army Corps of Engineers; South Florida Water Management
District; Florida Department of Environmental Protection
FX The research described in this report was supported by funding from a
number of Federal and State agencies: the U.S. Geological Survey
(Priority Ecosystems Studies for South Florida-G. Ronnie Best, Program
Executive), the U.S. Environmental Protection Agency, the National Park
Service, the Army Corps of Engineers, the South Florida Water Management
District, and the Florida Department of Environmental Protection. The
authors thank Alan Kolker and Mark Engle from the USGS, Samira Daroub of
the University of Florida, Garth Redfield (South Florida Water
Management District), and one anonymous reviewer for their helpful
comments on the manuscript.
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PI PHILADELPHIA
PA 325 CHESTNUT ST, SUITE 800, PHILADELPHIA, PA 19106 USA
SN 1064-3389
J9 CRIT REV ENV SCI TEC
JI Crit. Rev. Environ. Sci. Technol.
PY 2011
VL 41
SU 1
BP 249
EP 288
AR PII 933735549
DI 10.1080/10643389.2010.531201
PG 40
WC Environmental Sciences
SC Environmental Sciences & Ecology
GA 723GG
UT WOS:000287494000010
ER
PT J
AU Obeysekera, J
Kuebler, L
Ahmed, S
Chang, ML
Engel, V
Langevin, C
Swain, E
Wan, YS
AF Obeysekera, Jayantha
Kuebler, Laura
Ahmed, Shabbir
Chang, Miao-Li
Engel, Vic
Langevin, Christian
Swain, Eric
Wan, Yongshan
TI Use of Hydrologic and Hydrodynamic Modeling for Ecosystem Restoration
SO CRITICAL REVIEWS IN ENVIRONMENTAL SCIENCE AND TECHNOLOGY
LA English
DT Review
DE hydrology; hydrodynamic; modeling; Everglades; restoration
ID WATER FLOW; SIMULATION; DISCHARGE; ESTUARY; WETLAND
AB Planning and implementation of unprecedented projects for restoring the greater Everglades ecosystem are underway and the hydrologic and hydrodynamic modeling of restoration alternatives has become essential for success of restoration efforts. In view of the complex nature of the South Florida water resources system, regional-scale (system-wide) hydrologic models have been developed and used extensively for the development of the Comprehensive Everglades Restoration Plan. In addition, numerous subregional-scale hydrologic and hydrodynamic models have been developed and are being used for evaluating project-scale water management plans associated with urban, agricultural, and inland costal ecosystems. The authors provide a comprehensive summary of models of all scales, as well as the next generation models under development to meet the future needs of ecosystem restoration efforts in South Florida. The multiagency efforts to develop and apply models have allowed the agencies to understand the complex hydrologic interactions, quantify appropriate performance measures, and use new technologies in simulation algorithms, software development, and GIS/database techniques to meet the future modeling needs of the ecosystem restoration programs.
C1 [Obeysekera, Jayantha; Kuebler, Laura; Chang, Miao-Li; Wan, Yongshan] S Florida Water Management Dist, W Palm Beach, FL 33406 USA.
[Ahmed, Shabbir] US Army Corps Engineers, Jacksonville, FL USA.
[Langevin, Christian; Swain, Eric] US Geol Survey, Reston, VA 22092 USA.
US Geol Survey, Ft Lauderdale, FL USA.
RP Obeysekera, J (reprint author), S Florida Water Management Dist, 3301 Gun Club Rd,MSC 750, W Palm Beach, FL 33406 USA.
EM jobey@sfwmd.gov
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PI PHILADELPHIA
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SN 1064-3389
J9 CRIT REV ENV SCI TEC
JI Crit. Rev. Environ. Sci. Technol.
PY 2011
VL 41
SU 1
BP 447
EP 488
AR PII 933740050
DI 10.1080/10643389.2010.531226
PG 42
WC Environmental Sciences
SC Environmental Sciences & Ecology
GA 723GG
UT WOS:000287494000017
ER
PT J
AU Wetzel, PR
Sklar, FH
Coronado, CA
Troxler, TG
Krupa, SL
Sullivan, PL
Ewe, S
Price, RM
Newman, S
Orem, WH
AF Wetzel, Paul R.
Sklar, Fred H.
Coronado, Carlos A.
Troxler, Tiffany G.
Krupa, Steven L.
Sullivan, Pamela L.
Ewe, Sharon
Price, Rene M.
Newman, Susan
Orem, William H.
TI Biogeochemical Processes on Tree Islands in the Greater Everglades:
Initiating a New Paradigm
SO CRITICAL REVIEWS IN ENVIRONMENTAL SCIENCE AND TECHNOLOGY
LA English
DT Review
DE Everglades restoration; Focused Nutrient Redistribution model; Florida
Everglades; groundwater flows; landscape modulation; nitrogen;
phosphorus; sap flow; tree patches; tree transpiration; zone of
confluence
ID WATER CONSERVATION AREA-3; FLORIDA EVERGLADES; OKAVANGO DELTA;
PHOSPHORUS ENRICHMENT; GROUNDWATER DISCHARGE; SPATIAL-DISTRIBUTION;
SOUTHERN EVERGLADES; NORTHERN EVERGLADES; ECOSYSTEM STRUCTURE; SOIL
PROPERTIES
AB Scientists' understanding of the role of tree islands in the Everglades has evolved from a plant community of minor biogeochemical importance to a plant community recognized as the driving force for localized phosphorus accumulation within the landscape. Results from this review suggest that tree transpiration, nutrient infiltration from the soil surface, and groundwater flow create a soil zone of confluence where nutrients and salts accumulate under the head of a tree island during dry periods. Results also suggest accumulated salts and nutrients are flushed downstream by regional water flows during wet periods. That trees modulate their environment to create biogeochemical hot spots and strong nutrient gradients is a significant ecological paradigm shift in the understanding of the biogeochemical processes in the Everglades. In terms of island sustainability, this new paradigm suggests the need for distinct dry-wet cycles as well as a hydrologic regime that supports tree survival. Restoration of historic tree islands needs further investigation but the creation of functional tree islands is promising.
C1 [Wetzel, Paul R.] Smith Coll, Dept Biol Sci, Northampton, MA 01063 USA.
[Sklar, Fred H.; Coronado, Carlos A.; Krupa, Steven L.; Newman, Susan] S Florida Water Management Dist, Everglades Div, W Palm Beach, FL USA.
[Troxler, Tiffany G.; Price, Rene M.] Florida Int Univ, SE Environm Res Ctr, Miami, FL 33199 USA.
[Sullivan, Pamela L.; Price, Rene M.] Florida Int Univ, Dept Earth & Environm, Miami, FL 33199 USA.
[Ewe, Sharon] Ecol & Environm, W Palm Beach, FL USA.
[Orem, William H.] US Geol Survey, Reston, VA 22092 USA.
RP Wetzel, PR (reprint author), Smith Coll, Dept Biol Sci, 44 Coll Lane, Northampton, MA 01063 USA.
EM pwetzel@smith.edu
FU South Florida Water Management District; National Science Foundation
[DBI-0620409]
FX Research on tree islands in the Everglades requires the efforts of many
people and the authors express their appreciation for the hard work of
their colleagues. The water chemistry analysis was improved with the
comments of Robert Newton. The authors also appreciate the comments of
three anonymous reviewers. Work at the Loxahatchee Impoundment Landscape
Assessment described in this paper was funded by the South Florida Water
Management District. The authors are grateful for the help of Eric Cline
and Ryan Desilu at LILA. A portion of R.M. Price's contribution to this
research was supported by the National Science Foundation under Grant
No. DBI-0620409. This paper is contribution No. 506 of the Southeast
Environmental Research Center (SERC).
NR 86
TC 16
Z9 16
U1 0
U2 26
PU TAYLOR & FRANCIS INC
PI PHILADELPHIA
PA 530 WALNUT STREET, STE 850, PHILADELPHIA, PA 19106 USA
SN 1064-3389
EI 1547-6537
J9 CRIT REV ENV SCI TEC
JI Crit. Rev. Environ. Sci. Technol.
PY 2011
VL 41
SU 1
BP 670
EP 701
AR PII 933741979
DI 10.1080/10643389.2010.530908
PG 32
WC Environmental Sciences
SC Environmental Sciences & Ecology
GA 723GG
UT WOS:000287494000024
ER
PT J
AU Cui, P
Hou, YS
Tang, MJ
Zhang, HT
Zhou, YC
Yin, ZH
Li, TX
Guo, S
Xing, Z
He, YB
Prosser, DJ
Newman, SH
Takekawa, JY
Yan, BP
Lei, FM
AF Cui, Peng
Hou, Yuansheng
Tang, Mingjie
Zhang, Haiting
Zhou, Yuanchun
Yin, Zuohua
Li, Tianxian
Guo, Shan
Xing, Zhi
He, Yubang
Prosser, Diann J.
Newman, Scott H.
Takekawa, John Y.
Yan, Baoping
Lei, Fumin
TI Movement patterns of Bar-headed Geese Anser indicus during breeding and
post-breeding periods at Qinghai Lake, China
SO JOURNAL OF ORNITHOLOGY
LA English
DT Article
DE GPS satellite tracking; Bar-headed Goose; Breeding; Post-breeding; Moult
migration
ID H5N1 INFLUENZA-VIRUS; STELLERS EIDERS; SATELLITE TELEMETRY; MIGRATORY
WATERFOWL; AVIAN INFLUENZA; MOLT MIGRATION; EMPEROR GEESE; ALASKA;
SURVEILLANCE; CALIFORNIA
AB The highly pathogenic avian influenza (HPAI) H5N1 outbreak at Qinghai Lake, China, in 2005 caused the death of over 6,000 migratory birds, half of which were Bar-headed Geese Anser indicus. Understanding the movements of this species may inform monitoring of outbreak risks for HPAI viruses; thus, we investigated the movement patterns of 29 Bar-headed Geese at Qinghai Lake, China during 2007 and 2008 by using high resolution GPS satellite telemetry. We described the movements and distribution of marked Bar-headed Geese during the pre-nesting, nesting, and moulting periods. Of 21 Bar-headed Geese with complete transmission records, 3 moved to other areas during the nesting period: 2 to Jianghe wetland (50 km northwest of Qinghai Lake) and 1 to Cuolongka Lake (220 km northwest of Qinghai Lake) during the nesting period. We identified nesting attempts of 7 of the marked geese at Qinghai Lake. Four completed successful nesting attempts according to our rules of judgment for the breeding status, and 2 geese lost broods soon after hatching (hereafter referred to as unsuccessful breeders). Of 18 geese present at Qinghai Lake during the nesting period, 9 (6 non-breeders, 2 successful breeders and 1 unsuccessful breeder) remained at Qinghai Lake during the moulting period; and 9 (5 non-breeders, 4 unsuccessful breeders) left Qinghai Lake for moulting. Kuhai Lake, Donggeicuona Lake, Alake Lake, Zhaling-Eling Lake area and Huangheyuan wetland area were used as moulting sites. Geese that moulted at Qinghai Lake, Cuolongka Lake, Kuhai Lake, Donggeicuona Lake and Alake Lake also moved to Zhaling-Eling Lake area or Huangheyuan wetland area and stayed there for several days prior to autumn migration. Mean home range and core area estimates did not differ significantly by sex, year and between breeders and non-breeders.
C1 [Cui, Peng; Yin, Zuohua; Lei, Fumin] Chinese Acad Sci, Inst Zool, Key Lab Zool Systemat & Evolut, Beijing 100101, Peoples R China.
[Cui, Peng] Chinese Acad Sci, Grad Sch, Beijing 100049, Peoples R China.
[Hou, Yuansheng; Xing, Zhi; He, Yubang] Qinghai Lake Natl Nat Reserve, Xining 810003, Peoples R China.
[Li, Tianxian] Chinese Acad Sci, Wuhan Inst Virol, Wuhan 430071, Peoples R China.
[Guo, Shan] Chinese Acad Sci, Inst Remote Sensing Applicat, Beijing 100101, Peoples R China.
[Prosser, Diann J.] USGS Patuxent Wildlife Res Ctr, Beltsville, MD 20705 USA.
[Prosser, Diann J.] Univ Maryland, College Pk, MD 20742 USA.
[Newman, Scott H.] Food & Agr Org United Nations, Anim Prod & Hlth Div, Emergency Ctr Transboundary Anim Dis, EMPRES Wildlife Unit, I-00153 Rome, Italy.
[Takekawa, John Y.] USGS Western Ecol Res Ctr, Vallejo, CA 94592 USA.
[Tang, Mingjie; Zhang, Haiting; Zhou, Yuanchun; Yan, Baoping] Chinese Acad Sci, Comp Network Informat Ctr, Beijing 100080, Peoples R China.
RP Lei, FM (reprint author), Chinese Acad Sci, Inst Zool, Key Lab Zool Systemat & Evolut, Beijing 100101, Peoples R China.
EM leifm@ioz.ac.cn
OI Prosser, Diann/0000-0002-5251-1799
FU CAS [KSCX2-YW-N-063]; NSFC, China [30925008, J0930004]; MOST
[2006BAD06A01]; E-Science Program [INFO-115-D02]; IDRC; NIH; USDA;
Government of Sweden; USGS; United States National Science Foundation
[0713027]; United Nations Food and Agriculture Organization
FX We thank the staff of Qinghai Lake National Nature Reserve for field and
logistical support. We thank Yanhua Qu (Institute of Zoology, CAS) for
helpful comments on earlier version of this manuscript. We thank Steve
Schwarzbach (Western Ecological Research Center, WERC) and Judd Howell
(Patuxent Wildlife Research Center), United States Geological Survey
(USGS) for supporting this project. We thank David Douglas for decoding
and managing data from the satellite system and William Perry for
webpage maintenance. The research was supported by CAS Innovation
Program (KSCX2-YW-N-063), NSFC (30925008), China MOST Program
(2006BAD06A01), and E-Science Program (INFO-115-D02). The research was
also supported by IDRC, NIH and USDA to Lei F. M., and NSFC Program
J0930004 to Cui P.). Funding was also provided by the Government of
Sweden, USGS, United States National Science Foundation (No. 0713027)
and the United Nations Food and Agriculture Organization-EMPRES Wildlife
Program in the Animal Health Service.
NR 38
TC 8
Z9 10
U1 4
U2 33
PU SPRINGER
PI NEW YORK
PA 233 SPRING ST, NEW YORK, NY 10013 USA
SN 0021-8375
J9 J ORNITHOL
JI J. Ornithol.
PD JAN
PY 2011
VL 152
IS 1
BP 83
EP 92
DI 10.1007/s10336-010-0552-6
PG 10
WC Ornithology
SC Zoology
GA 700ZK
UT WOS:000285783900010
ER
PT J
AU Zipfel, J
Schroder, C
Jolliff, BL
Gellert, R
Herkenhoff, KE
Rieder, R
Anderson, R
Bell, JF
Bruckner, J
Crisp, JA
Christensen, PR
Clark, BC
de Souza, PA
Dreibus, G
d'Uston, C
Economou, T
Gorevan, SP
Hahn, BC
Klingelhofer, G
McCoy, TJ
McSween, HY
Ming, DW
Morris, RV
Rodionov, DS
Squyres, SW
Wanke, H
Wright, SP
Wyatt, MB
Yen, AS
AF Zipfel, Jutta
Schroeder, Christian
Jolliff, Bradley L.
Gellert, Ralf
Herkenhoff, Kenneth E.
Rieder, Rudolf
Anderson, Robert
Bell, James F., III
Brueckner, Johannes
Crisp, Joy A.
Christensen, Philip R.
Clark, Benton C.
de Souza, Paulo A., Jr.
Dreibus, Gerlind
d'Uston, Claude
Economou, Thanasis
Gorevan, Steven P.
Hahn, Brian C.
Klingelhoefer, Goestar
McCoy, Timothy J.
McSween, Harry Y., Jr.
Ming, Douglas W.
Morris, Richard V.
Rodionov, Daniel S.
Squyres, Steven W.
Waenke, Heinrich
Wright, Shawn P.
Wyatt, Michael B.
Yen, Albert S.
TI Bounce Rock-A shergottite-like basalt encountered at Meridiani Planum,
Mars
SO METEORITICS & PLANETARY SCIENCE
LA English
DT Article
ID X-RAY SPECTROMETER; FE-BEARING CLINOPYROXENES; MARTIAN METEORITES;
OPPORTUNITY ROVER; GUSEV CRATER; MOSSBAUER SPECTROMETER;
TEMPERATURE-DEPENDENCE; HYPERFINE PARAMETERS; CA-RICH; CHEMISTRY
AB The Opportunity rover of the Mars Exploration Rover mission encountered an isolated rock fragment with textural, mineralogical, and chemical properties similar to basaltic shergottites. This finding was confirmed by all rover instruments, and a comprehensive study of these results is reported here. Spectra from the miniature thermal emission spectrometer and the Panoramic Camera reveal a pyroxene-rich mineralogy, which is also evident in Mossbauer spectra and in normative mineralogy derived from bulk chemistry measured by the alpha particle X-ray spectrometer. The correspondence of Bounce Rock's chemical composition with the composition of certain basaltic shergottites, especially Elephant Moraine (EET) 79001 lithology B and Queen Alexandra Range (QUE) 94201, is very close, with only Cl, Fe, and Ti exhibiting deviations. Chemical analyses further demonstrate characteristics typical of Mars such as the Fe/Mn ratio and P concentrations. Possible shock features support the idea that Bounce Rock was ejected from an impact crater, most likely in the Meridiani Planum region. Bopolu crater, 19.3 km in diameter, located 75 km to the southwest could be the source crater. To date, no other rocks of this composition have been encountered by any of the rovers on Mars. The finding of Bounce Rock by the Opportunity rover provides further direct evidence for an origin of basaltic shergottite meteorites from Mars.
C1 [Zipfel, Jutta] Senckenberg Forschungsinst, Sekt Meteoritenforsch, D-60325 Frankfurt, Germany.
[Zipfel, Jutta] Nat Museum Frankfurt, D-60325 Frankfurt, Germany.
[Schroeder, Christian; Klingelhoefer, Goestar; Rodionov, Daniel S.] Johannes Gutenberg Univ Mainz, Inst Anorgan Chem & Analyt Chem, D-55128 Mainz, Germany.
[Jolliff, Bradley L.] Washington Univ, Dept Earth & Planetary Sci, St Louis, MO 63130 USA.
[Gellert, Ralf] Univ Guelph, Dept Phys, Guelph, ON N1G 2W1, Canada.
[Herkenhoff, Kenneth E.] US Geol Survey, Astrogeol Sci Ctr, Flagstaff, AZ 86001 USA.
[Rieder, Rudolf; Brueckner, Johannes; Dreibus, Gerlind; Waenke, Heinrich] Max Planck Inst Chem, Abt Geochem, D-55020 Mainz, Germany.
[Anderson, Robert; Crisp, Joy A.; Yen, Albert S.] CALTECH, Jet Prop Lab, Pasadena, CA 91109 USA.
[Bell, James F., III; Squyres, Steven W.] Cornell Univ, Dept Astron, Ithaca, NY 14853 USA.
[Christensen, Philip R.] Arizona State Univ, Sch Earth & Space Explorat, Tempe, AZ 85287 USA.
[Clark, Benton C.] Lockheed Martin Corp, Littleton, CO 80127 USA.
[de Souza, Paulo A., Jr.] CSIRO, Tasmanian ICT Ctr, Hobart, Tas 7001, Australia.
[d'Uston, Claude] Ctr Etud Spatiale Rayonnements, F-31028 Toulouse, France.
[Economou, Thanasis] Univ Chicago, Enrico Fermi Inst, Lab Atmospher & Space Res, Chicago, IL 60637 USA.
[Gorevan, Steven P.] Honeybee Robot, New York, NY 10012 USA.
[Hahn, Brian C.] SUNY Stony Brook, Dept Geosci, Stony Brook, NY 11794 USA.
[McCoy, Timothy J.] Smithsonian Inst, Natl Museum Nat Hist, Dept Mineral Sci, Washington, DC 20560 USA.
[McSween, Harry Y., Jr.] Univ Tennessee, Dept Earth & Planetary Sci, Knoxville, TN 37996 USA.
[Ming, Douglas W.; Morris, Richard V.] NASA, Lyndon B Johnson Space Ctr, Houston, TX 77058 USA.
[Wright, Shawn P.] Univ New Mexico, Inst Meteorit, Albuquerque, NM 87131 USA.
[Wyatt, Michael B.] Brown Univ, Dept Geol Sci, Providence, RI 02912 USA.
RP Zipfel, J (reprint author), Senckenberg Forschungsinst, Sekt Meteoritenforsch, Senckenberganlage 25, D-60325 Frankfurt, Germany.
EM jzipfel@senckenberg.de
RI de Souza, Paulo/B-8961-2008; Centre, TasICT/D-1212-2011; Schroder,
Christian/B-3870-2009; Crisp, Joy/H-8287-2016
OI de Souza, Paulo/0000-0002-0091-8925; Schroder,
Christian/0000-0002-7935-6039; Crisp, Joy/0000-0002-3202-4416
FU National Aeronautics and Space Administration
FX The authors thank the Meteorite Working Group and the curator for
Antarctic meteorites, Kevin Righter, for loan of an unpolished butt of
EETA79001. Some of this research was carried out at and for the Jet
Propulsion Laboratory, California Institute of Technology, sponsored by
the National Aeronautics and Space Administration. This article has
benefitted greatly from reviews of an earlier version of the manuscript
by Phil Bland, Cyrena Goodrich, Takashi Mikouchi, Deon van Niekerk, and
Larry Nittler. We also thank M. Schmidt, E. Walton, and Alan Treiman for
their reviews.
NR 72
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U1 1
U2 6
PU WILEY-BLACKWELL
PI HOBOKEN
PA 111 RIVER ST, HOBOKEN 07030-5774, NJ USA
SN 1086-9379
EI 1945-5100
J9 METEORIT PLANET SCI
JI Meteorit. Planet. Sci.
PD JAN
PY 2011
VL 46
IS 1
BP 1
EP 20
DI 10.1111/j.1945-5100.2010.01127.x
PG 20
WC Geochemistry & Geophysics
SC Geochemistry & Geophysics
GA 719YR
UT WOS:000287247900001
ER
PT J
AU Gilchrist, S
Gates, A
Elzinga, E
Gorring, M
Szabo, Z
AF Gilchrist, Sivajini
Gates, Alexander
Elzinga, Evert
Gorring, Matthew
Szabo, Zoltan
TI Source and Fate of Inorganic Soil Contamination Around the Abandoned
Phillips Sulfide Mine, Hudson Highlands, New York
SO SOIL & SEDIMENT CONTAMINATION
LA English
DT Article
DE mine tailings; metal contamination; goethite; jarosite; -SXRF
ID ACID; OXIDATION; DRAINAGE; SORPTION; SPECTROSCOPY; ADSORPTION; CHROMIUM;
QUALITY; METALS; WATERS
AB The abandoned Phillips sulfide mine in the critical Highlands watershed in New York has been shown to produce strongly acidic mine drainage (AMD) with anomalous metal contaminants in first-order streams that exceeded local water standards by up to several orders of magnitude (Gilchrist et al., 2009). The metal-sulfide-rich tailings also produce contaminated soils with pH 4, organic matter 2.5% and trace metals sequestered in soil oxides. A geochemical transect to test worst-case soil contamination showed that Cr, Co and Ni correlated positively with Mn, (r= 0.72, r= 0.89, r= 0.80, respectively), suggesting Mn-oxide sequestration and that Cu and Pb correlated with Fe (r= 0.76, r= 0.83, respectively), suggesting sequestration in goethite. Ubiquitous, yellow coating on the mine wastes, including jarosite and goethite, is a carrier of the metals. Geochemical and -SXRF analyses determined Cu to be the major soil contaminant. -SXRF also demonstrated that the heterogeneous nature of the soil chemistry at the micro-meter scale is self-similar to those in the bulk soil samples. Generally metals decreased, with some fluctuations, rapidly downslope through suspension of fines and dissolution in AMD leaving the area of substantial contamination 0.5 km from the source.
C1 [Gilchrist, Sivajini] Rutgers State Univ, Dept Earth & Environm Sci, Newark, NJ 07102 USA.
[Gorring, Matthew] Montclair State Univ, Montclair, NJ USA.
[Szabo, Zoltan] US Geol Survey, New Jersey Water Sci Ctr, Trenton, NJ USA.
RP Gilchrist, S (reprint author), Rutgers State Univ, Dept Earth & Environm Sci, Smith Hall,Rm 137,101 Warren St, Newark, NJ 07102 USA.
EM sivajini@pegasus.rutgers.edu
FU Dorr Foundation; J.M. Kaplan Fund
FX This study benefitted greatly from the suggestions of two anonymous
reviewers. The authors gratefully acknowledge laboratory assistance by
Fara Lindsay, Rutgers New Brunswick, and Dr. Charles Mandeville,
American Museum of Natural History; SEM-EDS support by Dr. Marian
Lupulescu, New York State Museum, and Dr. David Bailey, Hamilton
College. The authors also thank the staff at NSLS beamline X-27A for
assistance with mu-SXRF data collection. The Dorr Foundation and the
J.M. Kaplan Fund grants to Dr. Alexander Gates provided financial
support for this work.
NR 40
TC 1
Z9 1
U1 4
U2 11
PU TAYLOR & FRANCIS INC
PI PHILADELPHIA
PA 325 CHESTNUT ST, SUITE 800, PHILADELPHIA, PA 19106 USA
SN 1532-0383
J9 SOIL SEDIMENT CONTAM
JI Soil. Sediment. Contam.
PY 2011
VL 20
IS 1
BP 54
EP 74
AR PII 931552174
DI 10.1080/15320383.2011.528712
PG 21
WC Environmental Sciences
SC Environmental Sciences & Ecology
GA 714OC
UT WOS:000286817900004
ER
PT J
AU Hoagstrom, CW
Brooks, JE
Davenport, SR
AF Hoagstrom, Christopher W.
Brooks, James E.
Davenport, Stephen R.
TI A large-scale conservation perspective considering endemic fishes of the
North American plains
SO BIOLOGICAL CONSERVATION
LA English
DT Review
DE Climatic refugia; Regional endemics; Extinction debt; Great Plains;
Osage Plains
ID RED-RIVER PUPFISH; NOTROPIS-SIMUS-PECOSENSIS; FRESH-WATER FISHES; LOWER
YELLOWSTONE RIVERS; CLIMATE-CHANGE IMPACTS; GREAT-PLAINS; THREATENED
FISHES; PRAIRIE STREAM; DIONDA-DIABOLI; CYPRINODON-RUBROFLUVIATILIS
AB Regions with unique habitats often harbor endemic taxa associated with temporally stable habitats. We identified such habitats that sustain endemic fishes in the plains of North America. We also summarized threats to their conservation and identified remnant habitats that still harbor endemic fishes (refuges) based on post-1989 surveys. Major springs, smaller, spring-fed streams, larger rivers, and euryhaline habitats were associated with a total of 49 endemics. Endemism was attributable to climatic refugia associated with each habitat type and dispersal limitation among major river drainages and springs. Forty-one endemic fishes (84%) were declining or extinct. Dewatering, habitat fragmentation, and habitat degradation were main causes of declines, often present together. Pollution and non-native species were also threats in many cases. Evidence for 53 existing refuges was found. We considered 34 refuges to be "high-quality" because they harbored three or more endemics. Twenty of these (those with available data) maintained consistent streamflow regimes for at least 50 years up to 2009. Case studies suggest high stream length, more natural flow regimes, and fewer direct human impacts are features of high-quality refuges, but extinction thresholds are unquantified and extinction debts of refuges are unknown. Limited information on past extinctions suggests drought, a natural feature of the plains, combines with other threats to eliminate remnant endemic populations. Long-term conservation planning requires identification, protection, and restoration of high-quality refuges to reduce extinction risk, especially during future drought periods. Planning should be integrated with regional water resource planning, given scarcity of water in the region. (C) 2010 Elsevier Ltd. All rights reserved.
C1 [Hoagstrom, Christopher W.] Weber State Univ, Dept Zool, Ogden, UT 84408 USA.
[Brooks, James E.; Davenport, Stephen R.] US Fish & Wildlife Serv, New Mexico Fish & Wildlife Conservat Off, Albuquerque, NM 87109 USA.
RP Hoagstrom, CW (reprint author), Weber State Univ, Dept Zool, 2505 Univ Circle, Ogden, UT 84408 USA.
EM ChristopherHoagstrom@weber.edu; Jim_Brooks@fws.gov;
Stephen_Davenport@fws.gov
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U2 46
PU ELSEVIER SCI LTD
PI OXFORD
PA THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, OXON, ENGLAND
SN 0006-3207
EI 1873-2917
J9 BIOL CONSERV
JI Biol. Conserv.
PD JAN
PY 2011
VL 144
IS 1
BP 21
EP 34
DI 10.1016/j.biocon.2010.07.015
PG 14
WC Biodiversity Conservation; Ecology; Environmental Sciences
SC Biodiversity & Conservation; Environmental Sciences & Ecology
GA 719AA
UT WOS:000287168100003
ER
PT J
AU Converse, SJ
Shelley, KJ
Morey, S
Chan, J
LaTier, A
Scafidi, C
Crouse, DT
Runge, MC
AF Converse, Sarah J.
Shelley, Kevin J.
Morey, Steve
Chan, Jeffrey
LaTier, Andrea
Scafidi, Carolyn
Crouse, Deborah T.
Runge, Michael C.
TI A decision-analytic approach to the optimal allocation of resources for
endangered species consultation
SO BIOLOGICAL CONSERVATION
LA English
DT Article
DE Bull trout; Expert elicitation; Puget Sound; Salvelinus confluentus;
Structured decision-making; US Fish and Wildlife Service; Workload
allocation
ID BULL TROUT; CONSERVATION; UNCERTAINTY; INVESTMENT; MANAGEMENT
AB The resources available to support conservation work, whether time or money, are limited. Decision makers need methods to help them identify the optimal allocation of limited resources to meet conservation goals, and decision analysis is uniquely suited to assist with the development of such methods. In recent years, a number of case studies have been described that examine optimal conservation decisions under fiscal constraints; here we develop methods to look at other types of constraints, including limited staff and regulatory deadlines. In the US, Section Seven consultation, an important component of protection under the federal Endangered Species Act, requires that federal agencies overseeing projects consult with federal biologists to avoid jeopardizing species. A benefit of consultation is negotiation of project modifications that lessen impacts on species, so staff time allocated to consultation supports conservation. However, some offices have experienced declining staff, potentially reducing the efficacy of consultation. This is true of the US Fish and Wildlife Service's Washington Fish and Wildlife Office (WFWO) and its consultation work on federally-threatened bull trout (Salvelinus confluentus). To improve effectiveness, WFWO managers needed a tool to help allocate this work to maximize conservation benefits. We used a decision-analytic approach to score projects based on the value of staff time investment, and then identified an optimal decision rule for how scored projects would be allocated across bins, where projects in different bins received different time investments. We found that, given current staff, the optimal decision rule placed 80% of informal consultations (those where expected effects are beneficial, insignificant, or discountable) in a short bin where they would be completed without negotiating changes. The remaining 20% would be placed in a long bin, warranting an investment of seven days, including time for negotiation. For formal consultations (those where expected effects are significant), 82% of projects would be placed in a long bin, with an average time investment of 15 days. The WFWO is using this decision-support tool to help allocate staff time. Because workload allocation decisions are iterative, we describe a monitoring plan designed to increase the tool's efficacy over time. This work has general application beyond Section Seven consultation, in that it provides a framework for efficient investment of staff time in conservation when such time is limited and when regulatory deadlines prevent an unconstrained approach. Published by Elsevier Ltd.
C1 [Converse, Sarah J.; Runge, Michael C.] US Geol Survey, Patuxent Wildlife Res Ctr, Laurel, MD 20708 USA.
[Shelley, Kevin J.; Chan, Jeffrey; LaTier, Andrea; Scafidi, Carolyn] US Fish & Wildlife Serv, Lacey, WA 98503 USA.
[Morey, Steve] US Fish & Wildlife Serv, Portland, OR 97232 USA.
[Crouse, Deborah T.] US Fish & Wildlife Serv, Arlington, VA 22203 USA.
RP Converse, SJ (reprint author), US Geol Survey, Patuxent Wildlife Res Ctr, 12100 Beech Forest Rd, Laurel, MD 20708 USA.
EM sconverse@usgs.gov; kevin_shelley@fws.gov; steven_morey@fws.gov;
jeffrey_chan@fws.gov; andrea_latier@fws.gov; carolyn_scafidi@fws.gov;
debbby_crouse@fws.gov; mrunge@usgs.gov
RI Runge, Michael/E-7331-2011;
OI Runge, Michael/0000-0002-8081-536X; Converse, Sarah
J/0000-0002-3719-5441
FU USGS Patuxent Wildlife Research Center; USFWS Region 1 office
FX Our thanks go to the WFWO, especially K. Berg and J. Grettenberger, and
to the National Conservation Training Center, especially D. Brewer and
A. Starfield, for facilitating our collaboration. We offer our
appreciation to M. Eaton, B. Gardner, J. Lyons, J. Martin, and C. Moore
for helpful reviews and discussions. We also thank M Post van der Burg
and three anonymous reviewers who provided helpful suggestions for
improving drafts of the manuscript. Finally, we thank our expert panel,
R. Baker, N. Brennan-Dubbs, V. Harke, J. Muck, and E. Teachout, for
their irreplaceable contributions. USGS Patuxent Wildlife Research
Center supported SJC's and MCR's and the USFWS Region 1 office supported
SM's work on this project. Use of trade or product names does not imply
endorsement by the US Government.
NR 35
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U1 1
U2 31
PU ELSEVIER SCI LTD
PI OXFORD
PA THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, OXON, ENGLAND
SN 0006-3207
J9 BIOL CONSERV
JI Biol. Conserv.
PD JAN
PY 2011
VL 144
IS 1
BP 319
EP 329
DI 10.1016/j.biocon.2010.09.009
PG 11
WC Biodiversity Conservation; Ecology; Environmental Sciences
SC Biodiversity & Conservation; Environmental Sciences & Ecology
GA 719AA
UT WOS:000287168100034
ER
PT J
AU Roberts, SL
van Wagtendonk, JW
Miles, AK
Kelt, DA
AF Roberts, Susan L.
van Wagtendonk, Jan W.
Miles, A. Keith
Kelt, Douglas A.
TI Effects of fire on spotted owl site occupancy in a late-successional
forest
SO BIOLOGICAL CONSERVATION
LA English
DT Article
DE Fire; Late-successional forest species; Occupancy model; Population
density; Spotted owl; Yosemite National Park
ID NORTHERN FLYING SQUIRRELS; CENTRAL SIERRA-NEVADA; REPRODUCTIVE SUCCESS;
CASCADE MOUNTAINS; PACIFIC-NORTHWEST; FORAGING HABITAT; BARRED OWLS;
CALIFORNIA; SELECTION; ASSOCIATIONS
AB The spotted owl (Strix occidentalis) is a late-successional forest dependent species that is sensitive to forest management practices throughout its range. An increase in the frequency and spatial extent of stand-replacing fires in western North America has prompted concern for the persistence of spotted owls and other sensitive late-successional forest associated species. However, there is sparse information on the effects of fire on spotted owls to guide conservation policies. In 2004-2005, we surveyed for California spotted owls during the breeding season at 32 random sites (16 burned, 16 unburned) throughout late-successional montane forest in Yosemite National Park, California. Our burned areas burned at all severities, but predominately involved low to moderate fire severity. Based on an information theoretic approach, spotted owl detection and occupancy rates were similar between burned and unburned sites. Nest and roost site occupancy was best explained by a model that combined total tree basal area (positive effect) with cover by coarse woody debris (negative effect). The density estimates of California spotted owl pairs were similar in burned and unburned forests, and the overall mean density estimate for Yosemite was higher than previously reported for montane forests. Our results indicate that low to moderate severity fires, historically common within montane forests of the Sierra Nevada, California, maintain habitat characteristics essential for spotted owl site occupancy. These results suggest that managed fires that emulate the historic fire regime of these forests may maintain spotted owl habitat and protect this species from the effects of future catastrophic fires. Published by Elsevier Ltd.
C1 [Roberts, Susan L.; van Wagtendonk, Jan W.] US Geol Survey, Western Ecol Res Ctr, Yosemite Field Stn, El Portal, CA 95318 USA.
[Miles, A. Keith] Univ Calif Davis, Western Ecol Res Ctr, Davis Field Stn, US Geol Survey, Davis, CA 95616 USA.
RP Roberts, SL (reprint author), US Geol Survey, Western Ecol Res Ctr, Yosemite Field Stn, El Portal, CA 95318 USA.
EM susan_roberts@usgs.gov; jan_van_wagntendonk@usgs.gov;
keith_miles@usgs.gov; dakelt@ucdavis.edu
FU Yosemite National Park
FX We thank M. Meyer for his invaluable advice and field support, E. Berlow
and University of California, Merced, for housing and office support,
and Yosemite National Park Fee Program for funding this research. S.
Thompson was critical for obtaining the funding and providing logistical
support. K. van Wagtendonk performed the GIS analysis necessary for plot
selection. We are grateful for the advice and thorough reviews of J.
Yee, R. Anthony, E. Forsman, G. Smith, and two anonymous reviewers who
greatly improved this work. The project would not have been possible
without the incredibly dedicated efforts of the field crews: S. Evans,
S. Eyes, A. Farris, J. Felis, D. Giordano, C. Gratten, Z. Hambleton, N.
Hatch, L. Illingworth, M. Kaufman, E. Kolden, J. Lane, R. Lechalk, M.
Masten, M. McDonald, C. Morcos, G. Palmer, K. Schlimme, P. Segre, E.
Williams, and of course, Mus musculus. Any use of trade, product, or
firm names is for descriptive purposes only and does not imply
endorsement by the US Government.
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PA THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, OXON, ENGLAND
SN 0006-3207
J9 BIOL CONSERV
JI Biol. Conserv.
PD JAN
PY 2011
VL 144
IS 1
BP 610
EP 619
DI 10.1016/j.biocon.2010.11.002
PG 10
WC Biodiversity Conservation; Ecology; Environmental Sciences
SC Biodiversity & Conservation; Environmental Sciences & Ecology
GA 719AA
UT WOS:000287168100066
ER
PT J
AU Kappes, PJ
McChesney, GJ
Parker, MW
Carter, HR
Kress, SW
Golightly, RT
AF Kappes, Peter J.
McChesney, Gerard J.
Parker, Michael W.
Carter, Harry R.
Kress, Stephen W.
Golightly, Richard T.
TI Use of time-activity budgets to measure early progress of a social
attraction restoration project
SO BIOLOGICAL CONSERVATION
LA English
DT Article
DE Social attraction; Time-activity budgets; Common murre; Restoration;
Social environment; Uria aalge
ID MURRES URIA-AALGE; CENTRAL CALIFORNIA; CONSPECIFIC ATTRACTION; COMMON
MURRE; CONSERVATION; BEHAVIOR; COLONY; TRANSITION; SONGBIRDS; PATTERNS
AB Social attraction is a useful technique for re-establishing or relocating waterbird colonies and other species groups. However, little information exists regarding how newly attending individuals behave when the social environment is influenced predominantly by artificial stimuli. To help assess early progress of colony re-establishment, we compared time-activity budgets of common murres (Uria aalge) at a social attraction site (Devil's Slide Rock; DSR) in central California with two nearby reference colonies during the first 3 years (1996-1998) of efforts. Murres at all colonies spent over 95% of their time engaged in resting, comfort, courtship, and alert activities during the pre-breeding period and over 88% of their time in similar activities during the breeding period. Although patterns were similar overall, comparisons of pooled and year-specific time budget data revealed significant differences between all three colonies, especially during pre-breeding. Murres at DSR typically engaged in comfort behaviors less frequently and in alert and courtship behaviors more frequently than reference colonies. Differences likely were due to recent re-establishment, including lower bird densities and higher proportions of non-breeders and first-time breeders at DSR, along with other factors such as disturbance. Results indicate that newly attracted birds at DSR behaved "normally" even though the social environment was influenced predominantly by artificial stimuli. Furthermore, re-established breeding in the first year of efforts, subsequent colony growth, and high productivity reflected successful restoration efforts. Thus, time-activity budgets can provide important measures of early progress of social attraction efforts and as such can be used to inform adaptive management decisions. Published by Elsevier Ltd.
C1 [Kappes, Peter J.; McChesney, Gerard J.; Parker, Michael W.] US Fish & Wildlife Serv, Newark, CA 94560 USA.
[Carter, Harry R.; Golightly, Richard T.] Humboldt State Univ, Dept Wildlife, Arcata, CA 95521 USA.
[Kress, Stephen W.] Natl Audubon Soc, Ithaca, NY 14850 USA.
RP McChesney, GJ (reprint author), US Fish & Wildlife Serv, San Francisco Bay Natl Wildlife Refuge Complex,95, Newark, CA 94560 USA.
EM olostriver@gmail.com; Gerry_McChesney@fws.-gov; mparker1500@gmail.com;
carterhr@shaw.ca; skress@audubon.org; rtg1@humboldt.edu
OI Kappes, Peter/0000-0001-6029-5355
FU Apex Houston Trustee Council
FX Funding and other support for this project was provided by the Apex
Houston Trustee Council that has been comprised of: D. Welsh, J. Buffa
and J. Whitlock (U.S. Fish and Wildlife Service); E. Ueber, M. Brown,
and J. Boyce (National Oceanic and Atmospheric Administration); and D.
Lollock, P. Kelly, and S. Hampton (California Department of Fish and
Game). We thank the numerous project staff in 1996-98 for their
assistance collecting time-activity budget data, including E. McLaren,
S. Schubel, J. Boyce, P. Capitol, M. Ortwerth, V. Collins, D.
Nothhelfer, R. Young, E. Craig, and H. Gellerman. J. Yee (U.S.
Geological Survey-Western Ecological Research Center) and M. Kappes
provided statistical assistance. We also appreciate the efforts and
support of M. Kolar, G.M. Stewart, A. Hutzel, G. Moore, S. Allen, R.
Helm, B. Foster, B. Drollman, and the hundreds of local elementary
students and teachers that helped repaint our decoys. Observations of
DSR were conducted under California Department of Transportation permit
0496-NSV0373. Observations at PR were conducted under National Park
Service permit 95-10. This paper benefited from reviews by M. Kappes and
three anonymous reviewers.
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PA THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, OXON, ENGLAND
SN 0006-3207
J9 BIOL CONSERV
JI Biol. Conserv.
PD JAN
PY 2011
VL 144
IS 1
BP 620
EP 626
DI 10.1016/j.biocon.2010.11.003
PG 7
WC Biodiversity Conservation; Ecology; Environmental Sciences
SC Biodiversity & Conservation; Environmental Sciences & Ecology
GA 719AA
UT WOS:000287168100067
ER
PT J
AU Brand, LA
Stromberg, JC
Goodrich, DC
Dixon, MD
Lansey, K
Kang, D
Brookshire, DS
Cerasale, DJ
AF Brand, L. Arriana
Stromberg, Juliet C.
Goodrich, David C.
Dixon, Mark D.
Lansey, Kevin
Kang, Doosun
Brookshire, David S.
Cerasale, David J.
TI Projecting avian response to linked changes in groundwater and riparian
floodplain vegetation along a dryland river: a scenario analysis
SO ECOHYDROLOGY
LA English
DT Article
DE avian abundance; Populus; ecohydrology; dryland river; groundwater;
riparian; Tamarix; scenario modelling; space-for-time substitution
ID SAN-PEDRO RIVER; NATURAL FLOW REGIME; SPECIES RICHNESS; BREEDING BIRDS;
COLORADO RIVER; NORTH-AMERICA; UNITED-STATES; FRESH-WATER; ARIZONA;
RESTORATION
AB Groundwater is a key driver of riparian condition on dryland rivers but is in high demand for municipal, industrial, and agricultural uses. Approaches are needed to guide decisions that balance human water needs while conserving riparian ecosystems. We developed a space-for-time substitution model that links groundwater change scenarios implemented within a Decision Support System (DSS) with proportions of floodplain vegetation types and abundances of breeding and migratory birds along the upper San Pedro River, AZ, USA. We investigated nine scenarios ranging from groundwater depletion to recharge. In groundwater decline scenarios, relative proportions of tall-canopied obligate phreatophytes (Populus/Salix, cottonwood/willow) on the floodplain progressively decline, and shrubbier species less dependent on permanent water sources (e. g. Tamarix spp., saltcedar) increase. These scenarios result in broad shifts in the composition of the breeding bird community, with canopy-nesting and water-obligate birds declining but midstory nesting birds increasing in abundance as groundwater declines. For the most extreme draw-down scenario where all reaches undergo groundwater declines, models project that only 10% of the upper San Pedro floodplain would be comprised of cottonwood/willow (73% saltcedar and 18% mesquite), and abundances of canopy-nesting, water-obligate, and spring migrant birds would decline 48%, 72%, and 40%, respectively. Groundwater recharge scenarios were associated with increases in canopy-nesting birds particularly given the extreme recharge scenario (all reaches regain shallow water tables and perennial streamflow). Model outputs serve to assess the sensitivity of biotic groups to potential changes in groundwater and thus to rank scenarios based on their expected ecological impacts. Copyright (C) 2010 John Wiley & Sons, Ltd.
C1 [Brand, L. Arriana] Univ Arizona, Dept Hydrol & Water Resources, SAHRA Ctr, Tucson, AZ 85721 USA.
[Stromberg, Juliet C.] Arizona State Univ, Sch Life Sci, Tempe, AZ 85287 USA.
[Goodrich, David C.] ARS, USDA, Tucson, AZ 85719 USA.
[Dixon, Mark D.] Univ S Dakota, Dept Biol, Vermillion, SD 57069 USA.
[Lansey, Kevin; Kang, Doosun] Univ Arizona, Dept Civil Engn & Engn Mech, Tucson, AZ 85721 USA.
[Brookshire, David S.] Univ New Mexico, Dept Econ, Albuquerque, NM 87131 USA.
[Cerasale, David J.] Cornell Univ, Dept Ecol & Evolutionary Biol, Ithaca, NY 14853 USA.
RP Brand, LA (reprint author), US Geol Survey, Western Ecol Res Ctr, San Francisco Bay Estuary Field Stn, 505 Azuar Dr, Vallejo, CA 94592 USA.
EM arriana_brand@usgs.gov
RI Dixon, Mark/F-2641-2011; Goodrich, David/B-1763-2009
OI Dixon, Mark/0000-0002-0345-5655; Goodrich, David/0000-0001-7735-1448
FU Strategic Environment Research and Development (SERDP) Project
[CS-1100]; National Science Foundation [EAR-9876800]; US Environmental
Protection Agency [2003-STAR-G2]
FX Avian data collection for this research was funded by the Strategic
Environment Research and Development (SERDP) Project CS-1100. Analysis
and writing portions for L. A. B. were supported by Sustainability of
semi-Arid Hydrology and Riparian Areas (SAHRA) under the STC Program of
the National Science Foundation, Agreement No. EAR-9876800, and the US
Environmental Protection Agency 'Integrated Modelling and Ecological
Valuation' EPA STAR grant Program #2003-STAR-G2. The Bureau of Land
Management, San Pedro Project Office, provided access to the San Pedro
National Conservation Area as well as housing for the data collection
effort. We appreciate discussions with S. Lite, K. Benedict, J. Thacher,
C. Broadbent, S. Stewart, and M. McIntosh that contributed to this
manuscript. We also greatly appreciate the field staff who helped in
collecting data.
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PI HOBOKEN
PA 111 RIVER ST, HOBOKEN, NJ 07030 USA
SN 1936-0584
J9 ECOHYDROLOGY
JI Ecohydrology
PD JAN
PY 2011
VL 4
IS 1
BP 130
EP 142
DI 10.1002/eco.143
PG 13
WC Ecology; Environmental Sciences; Water Resources
SC Environmental Sciences & Ecology; Water Resources
GA 718VM
UT WOS:000287154500012
ER
PT J
AU Olea, RA
Luppens, JA
Tewalt, SJ
AF Olea, Ricardo A.
Luppens, James A.
Tewalt, Susan J.
TI Methodology for quantifying uncertainty in coal assessments with an
application to a Texas lignite deposit
SO INTERNATIONAL JOURNAL OF COAL GEOLOGY
LA English
DT Article
DE Coal resources; Bed thickness; Geographical distance; Spatial
correlation; Probability distribution; Stochastic simulation
AB A common practice for characterizing uncertainty in coal resource assessments has been the itemization of tonnage at the mining unit level and the classification of such units according to distance to drilling holes. Distance criteria, such as those used in U.S. Geological Survey Circular 891, are still widely used for public disclosure. A major deficiency of distance methods is that they do not provide a quantitative measure of uncertainty. Additionally, relying on distance between data points alone does not take into consideration other factors known to have an influence on uncertainty, such as spatial correlation, type of probability distribution followed by the data, geological discontinuities, and boundary of the deposit. Several geostatistical methods have been combined to formulate a quantitative characterization for appraising uncertainty. Drill hole datasets ranging from widespread exploration drilling to detailed development drilling from a lignite deposit in Texas were used to illustrate the modeling. The results show that distance to the nearest drill hole is almost completely unrelated to uncertainty, which confirms the inadequacy of characterizing uncertainty based solely on a simple classification of resources by distance classes. The more complex statistical methods used in this study quantify uncertainty and show good agreement between confidence intervals in the uncertainty predictions and data from additional drilling. Published by Elsevier B.V.
C1 [Olea, Ricardo A.; Luppens, James A.; Tewalt, Susan J.] US Geol Survey, Reston, VA 20192 USA.
RP Olea, RA (reprint author), US Geol Survey, 12201 Sunrise Valley Dr,Mail Stop 956, Reston, VA 20192 USA.
EM olea@usgs.gov
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PU ELSEVIER SCIENCE BV
PI AMSTERDAM
PA PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS
SN 0166-5162
J9 INT J COAL GEOL
JI Int. J. Coal Geol.
PD JAN 1
PY 2011
VL 85
IS 1
BP 78
EP 90
DI 10.1016/j.coal.2010.10.001
PG 13
WC Energy & Fuels; Geosciences, Multidisciplinary
SC Energy & Fuels; Geology
GA 712ZK
UT WOS:000286704600009
ER
PT J
AU Lyver, PO
MacLeod, CJ
Ballard, G
Karl, BJ
Barton, KJ
Adams, J
Ainley, DG
Wilson, PR
AF Lyver, P. O'B.
MacLeod, C. J.
Ballard, G.
Karl, B. J.
Barton, K. J.
Adams, J.
Ainley, D. G.
Wilson, P. R.
TI Intra-seasonal variation in foraging behavior among Ad,lie penguins
(Pygocelis adeliae) breeding at Cape Hallett, Ross Sea, Antarctica
SO POLAR BIOLOGY
LA English
DT Article
DE Adelie penguin; Foraging; Intra-seasonal competition; Pack ice;
Antarctic krill; Antarctic silverfish
ID BLACK-LEGGED KITTIWAKES; LUTZOW-HOLM BAY; PYGOSCELIS-ADELIAE; NORTH-SEA;
ICE CONDITIONS; RECORDING DEVICES; EUPHAUSIA-SUPERBA; TROPHIC STRUCTURE;
RISSA-TRIDACTYLA; DIVING BEHAVIOR
AB We investigated intra-seasonal variation in foraging behavior of chick-rearing Ad,lie penguins, Pygoscelis adeliae, during two consecutive summers at Cape Hallett, northwestern Ross Sea. Although foraging behavior of this species has been extensively studied throughout the broad continental shelf region of the Ross Sea, this is the first study to report foraging behaviors and habitat affiliations among birds occupying continental slope waters. Continental slope habitat supports the greatest abundances of this species throughout its range, but we lack information about how intra-specific competition for prey might affect foraging and at-sea distribution and how these attributes compare with previous Ross Sea studies. Foraging trips increased in both distance and duration as breeding advanced from guard to crSche stage, but foraging dive depth, dive rates, and vertical dive distances travelled per hour decreased. Consistent with previous studies within slope habitats elsewhere in Antarctic waters, Antarctic krill (Euphausia superba) dominated chick meal composition, but fish increased four-fold from guard to crSche stages. Foraging-, focal-, and core areas all doubled during the crSche stage as individuals shifted distribution in a southeasterly direction away from the coast while simultaneously becoming more widely dispersed (i.e., less spatial overlap among individuals). Intra-specific competition for prey among Ad,lie penguins appears to influence foraging behavior of this species, even in food webs dominated by Antarctic krill.
C1 [Lyver, P. O'B.; Karl, B. J.] Landcare Res, Lincoln 7640, New Zealand.
[MacLeod, C. J.] Landcare Res, Dunedin 9054, New Zealand.
[Ballard, G.] PRBO Conservat Sci, Petaluma, CA 94954 USA.
[Ballard, G.] Univ Auckland, Sch Biol Sci, Auckland 1, New Zealand.
[Barton, K. J.] Landcare Res, Nelson Mail Ctr, Nelson 7042, New Zealand.
[Adams, J.] US Geol Survey, Western Ecol Res Ctr, Pacific Sci Ctr, Santa Cruz, CA 95060 USA.
[Ainley, D. G.] HT Harvey & Associates, Los Gatos, CA 95032 USA.
RP Lyver, PO (reprint author), Landcare Res, POB 40, Lincoln 7640, New Zealand.
EM lyverp@landcareresearch.co.nz
FU US Adelie Penguin Program [B031]; New Zealand Foundation for Research,
Science and Technology [C09X0510]; Office of Polar Programs, National
Science Foundation [OPP 0125608, 0440643]
FX We thank the following persons for planning and field assistance: Peter
Dilks, Shulamit Gordon, Rachel Brown and Gus McAlister. Antarctica New
Zealand provided extensive logistic support for the NZ Adelie Penguin
Program (K122b) through their Latitudinal Gradient Program, while the US
Antarctic Program supported members from the US Adelie Penguin Program
(B031). This project was funded by the New Zealand Foundation for
Research, Science and Technology (C09X0510) and Office of Polar
Programs, National Science Foundation (OPP 0125608, 0440643). Draft
manuscripts received valuable review from the editor and three anonymous
referees. Reference to trade names does not imply endorsement of these
products.
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PU SPRINGER
PI NEW YORK
PA 233 SPRING ST, NEW YORK, NY 10013 USA
SN 0722-4060
J9 POLAR BIOL
JI Polar Biol.
PD JAN
PY 2011
VL 34
IS 1
BP 49
EP 67
DI 10.1007/s00300-010-0858-0
PG 19
WC Biodiversity Conservation; Ecology
SC Biodiversity & Conservation; Environmental Sciences & Ecology
GA 709WH
UT WOS:000286471600006
ER
PT J
AU Pfeiffer, TJ
Summerfelt, ST
Watten, BJ
AF Pfeiffer, Timothy J.
Summerfelt, Steven T.
Watten, Barnaby J.
TI Comparative performance of CO2 measuring methods: Marine aquaculture
recirculation system application
SO AQUACULTURAL ENGINEERING
LA English
DT Article
DE Dissolved carbon dioxide; Recirculating aquaculture systems; Head space
unit; Non-dispersive infra-red absorption
ID TROUT SALMO-GAIRDNERI; CARBON-DIOXIDE; PARTIAL PRESSURES; PH; WATER
AB Many methods are available for the measurement of dissolved carbon dioxide in an aqueous environment. Standard titration is the typical field method for measuring dissolved CO2 in aquaculture systems. However, titrimetric determination of dissolved CO2 in marine water aquaculture systems is unsuitable because of the high dissolved solids, silicates, and other dissolved minerals that interfere with the determination. Other methods used to measure dissolved carbon dioxide in an aquaculture water included use of a wetted CO2 probe analyzer, standard nomographic methods, and calculation by direct measurements of the water's pH, temperature, and alkalinity. The determination of dissolved CO2 in saltwater based on partial pressure measurements and non-dispersive infra-red (NDIR) techniques with a CO2 gas analyzer are widely employed for oceanic surveys of surface ocean CO2 flux and are similar to the techniques employed with the head space unit (HSU) in this study. Dissolved carbon dioxide (DC) determination with the HSU using a infra-red gas analyzer (IRGA) was compared with titrimetric, nomographic, calculated, and probe measurements of CO2 in freshwater and in saltwater with a salinity ranging from 5.0 to 30 ppt, and a CO2 range from 8 to 50 mg/L. Differences in CO2 measurements between duplicate HSUs (0.1-0.2 mg/L) were not statistically significant different. The coefficient of variation for the HSU readings averaged 1.85% which was better than the CO2 probe (4.09%) and that for the titrimetric method (5.84%). In all low, medium and high salinity level trials HSU precision was good, averaging 3.39%. Differences existed between comparison testing of the CO2 probe and HSU measurements with the CO2 probe readings, on average, providing DC estimates that were higher than HSU estimates. Differences between HSU and titration based estimates of DC increased with salinity and reached a maximum at 32.2 ppt. These differences were statistically significant (P < 0.05) at all salinity levels greater than 0.3 ppt. Results indicated reliable replicated results from the head space unit with varying salinity and dissolved carbon dioxide concentrations. Published by Elsevier B.V.
C1 [Pfeiffer, Timothy J.] USDA ARS, Ft Pierce, FL 34946 USA.
[Summerfelt, Steven T.] Inst Freshwater, Conservat Funds, Shepherdstown, WV 25443 USA.
[Watten, Barnaby J.] USGS Leetown Sci Ctr, Kearneysville, WV 25430 USA.
RP Pfeiffer, TJ (reprint author), USDA ARS, 5600 US Hwy 1 N, Ft Pierce, FL 34946 USA.
EM timothy.pfeiffer@ars.usda.gov; s.summerfelt@freshwaterinstitute.org;
bwatten@usgs.gov
FU USDA Agricultural Research Service [6225-63000-007-00]
FX This work was supported by the USDA Agricultural Research Service under
the National Aquaculture Program under Project no. 6225-63000-007-00,
titled Engineering and Production Strategies for Sustainable Marine
Aquaculture. The authors thank Michael Gearheart, Environmental Chemist
for the Freshwater Institute and Todd Lenger, Engineering Technician for
the USDA Agricultural Research Service for assistance in experimental
data collection. Mention of trade names or commercial products in this
manuscript publication is solely for the purpose of providing specific
information and does not imply recommendation or endorsement by the
Agricultural Research Service of the U.S.D.A.
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PA THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, OXON, ENGLAND
SN 0144-8609
J9 AQUACULT ENG
JI Aquac. Eng.
PD JAN
PY 2011
VL 44
IS 1
BP 1
EP 9
DI 10.1016/j.aquaeng.2010.10.001
PG 9
WC Agricultural Engineering; Fisheries
SC Agriculture; Fisheries
GA 712ZB
UT WOS:000286703700001
ER
PT J
AU Cross, A
Perakis, SS
AF Cross, Alison
Perakis, Steven S.
TI Tree species and soil nutrient profiles in old-growth forests of the
Oregon Coast Range
SO CANADIAN JOURNAL OF FOREST RESEARCH-REVUE CANADIENNE DE RECHERCHE
FORESTIERE
LA English
DT Article
ID DOUGLAS-FIR FORESTS; RED ALDER; TEMPERATE FORESTS; WESTERN REDCEDAR;
BRITISH-COLUMBIA; CANOPY TREE; NITROGEN; CHEMISTRY; CONIFER; CALCIUM
AB Old-growth forests of the Pacific Northwest provide a unique opportunity to examine tree species - soil relationships in ecosystems that have developed without significant human disturbance. We characterized foliage, forest floor, and mineral soil nutrients associated with four canopy tree species (Douglas-fir (Pseudotsuga menziesii (Mirbel) Franco), western hemlock (Tsuga heterophylla (Raf.) Sarg.), western redcedar (Thuja plicata Donn ex D. Don), and bigleaf maple (Acer macrophyllum Pursh)) in eight old-growth forests of the Oregon Coast Range. The greatest forest floor accumulations of C, N, P, Ca, Mg, and K occurred under Douglas-fir, primarily due to greater forest floor mass. In mineral soil, western hemlock exhibited significantly lower Ca concentration and sum of cations (Ca + Mg + K) than bigleaf maple, with intermediate values for Douglas-fir and western redcedar. Bigleaf maple explained most species-based differences in foliar nutrients, displaying high concentrations of N, P, Ca, Mg, and K. Foliar P and N: P variations largely reflected soil P variation across sites. The four tree species that we examined exhibited a number of individualistic effects on soil nutrient levels that contribute to biogeochemical heterogeneity in these ecosystems. Where fire suppression and long-term succession favor dominance by highly shade-tolerant western hemlock, our results suggest a potential for declines in both soil Ca availability and soil biogeochemical heterogeneity in old-growth forests.
C1 [Perakis, Steven S.] US Geol Survey, Forest & Rangeland Ecosyst Sci Ctr, Corvallis, OR 97331 USA.
[Cross, Alison] Oregon State Univ, Dept Forest Sci, Corvallis, OR 97331 USA.
RP Perakis, SS (reprint author), US Geol Survey, Forest & Rangeland Ecosyst Sci Ctr, Corvallis, OR 97331 USA.
EM steven.perakis@oregonstate.edu
FU U.S. Geological Survey Forest and Rangeland Ecosystem Science Center;
Oregon Department of Forestry
FX The authors thank Chris Catricala and crew for field and laboratory
assistance, Lisa Ganio for statistical consulting, Patti Haggerty for
map illustration, and Kermit Cromack, David Hibbs, David Myrold, and
three anonymous reviewers for comments. This research was produced
through the Cooperative Forest Ecosystem Research Program, with funding
provided by the U.S. Geological Survey Forest and Rangeland Ecosystem
Science Center and the Oregon Department of Forestry. Any use of trade
names is for descriptive purposes only and does not imply endorsement by
the U.S. Government.
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PI OTTAWA
PA 1200 MONTREAL ROAD, BUILDING M-55, OTTAWA, ON K1A 0R6, CANADA
SN 0045-5067
J9 CAN J FOREST RES
JI Can. J. For. Res.-Rev. Can. Rech. For.
PD JAN
PY 2011
VL 41
IS 1
BP 195
EP 210
DI 10.1139/X10-199
PG 16
WC Forestry
SC Forestry
GA 709YE
UT WOS:000286476500016
ER
PT J
AU Plant, NG
Holland, KT
AF Plant, Nathaniel G.
Holland, K. Todd
TI Prediction and assimilation of surf-zone processes using a Bayesian
network Part I: Forward models
SO COASTAL ENGINEERING
LA English
DT Article
DE Wave height; Bathymetry; Field data; Duck94
ID 3RD-GENERATION WAVE MODEL; SANDBAR MIGRATION; COASTAL REGIONS;
NEARSHORE; EVOLUTION; BEHAVIOR; BEACHES; SCALE; TRANSFORMATION;
VERIFICATION
AB Prediction of coastal processes, including waves, currents, and sediment transport, can be obtained from a variety of detailed geophysical-process models with many simulations showing significant skill. This capability supports a wide range of research and applied efforts that can benefit from accurate numerical predictions. However, the predictions are only as accurate as the data used to drive the models and, given the large temporal and spatial variability of the surf zone, inaccuracies in data are unavoidable such that useful predictions require corresponding estimates of uncertainty. We demonstrate how a Bayesian-network model can be used to provide accurate predictions of wave-height evolution in the surf zone given very sparse and/or inaccurate boundary-condition data. The approach is based on a formal treatment of a data-assimilation problem that takes advantage of significant reduction of the dimensionality of the model system. We demonstrate that predictions of a detailed geophysical model of the wave evolution are reproduced accurately using a Bayesian approach. In this surf-zone application, forward prediction skill was 83%, and uncertainties in the model inputs were accurately transferred to uncertainty in output variables. We also demonstrate that if modeling uncertainties were not conveyed to the Bayesian network (i.e., perfect data or model were assumed), then overly optimistic prediction uncertainties were computed. More consistent predictions and uncertainties were obtained by including model-parameter errors as a source of input uncertainty. Improved predictions (skill of 90%) were achieved because the Bayesian network simultaneously estimated optimal parameters while predicting wave heights. Published by Elsevier B.V.
C1 [Plant, Nathaniel G.] US Geol Survey, St Petersburg, FL 33701 USA.
[Holland, K. Todd] USN, Res Lab, Stennis Space Ctr, MS 39529 USA.
RP Plant, NG (reprint author), US Geol Survey, 600 4th St S, St Petersburg, FL 33701 USA.
EM nplant@usgs.gov; todd.holland@nrlssc.navy.mil
RI Holland, K. Todd/A-7673-2011;
OI Holland, K. Todd/0000-0002-4601-6097; Plant,
Nathaniel/0000-0002-5703-5672
FU Office of Naval Research [0602435N, N0001409IP20080]; National Science
Foundation
FX This work was supported by the Office of Naval Research (PE Number:
0602435N for KTH and N0001409IP20080 for NGP). We are indebted to the
researchers at the Field Research Facility (Duck, NC) who collected the
long time series of bathymetry and wave conditions used in our models.
This debt is extended again to the FRF researchers and to Drs. Guza,
Gallagher, Herbers, Raubenheimer, and Elgar who collected the Duck94
field observation used to test our predictions. That effort was
supported by the Office of Naval Research and the National Science
Foundation. Also, we are grateful to Sarah Rennie and Alan Brandt, who
introduced us to Bayesian networks and worked with us for several years
to develop and understand the potential applications of this approach.
Comments from reviews by Drs. P. Howd and A. Reniers led to substantial
improvements of this work. Barbara Lidz provided numerous comments that
improved the manuscript's clarity.
NR 35
TC 25
Z9 26
U1 0
U2 7
PU ELSEVIER SCIENCE BV
PI AMSTERDAM
PA PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS
SN 0378-3839
J9 COAST ENG
JI Coast. Eng.
PD JAN
PY 2011
VL 58
IS 1
BP 119
EP 130
DI 10.1016/j.coastaleng.2010.09.003
PG 12
WC Engineering, Civil; Engineering, Ocean
SC Engineering
GA 699IQ
UT WOS:000285657500009
ER
PT J
AU Pierson, TC
Pringle, PT
Cameron, KA
AF Pierson, Thomas C.
Pringle, Patrick T.
Cameron, Kenneth A.
TI Magnitude and timing of downstream channel aggradation and degradation
in response to a dome-building eruption at Mount Hood, Oregon
SO GEOLOGICAL SOCIETY OF AMERICA BULLETIN
LA English
DT Article
ID FLUVIAL SEDIMENT TRANSPORT; SOUFRIERE HILLS VOLCANO; NEW-ZEALAND;
ST-HELENS; BRITISH-COLUMBIA; FLUME EXPERIMENT; UNZEN VOLCANO; REDWOOD
CREEK; OYABU CREEK; LAVA DOME
AB A dome-building eruption at Mount Hood, Oregon, starting in A. D. 1781 and lasting until ca. 1793, produced dome-collapse lithic pyroclastic flows that triggered lahars and intermittently fed 10(8) m(3) of coarse volcaniclastic sediment to sediment reservoirs in headwater canyons of the Sandy River. Mobilization of dominantly sandy sediment from these reservoirs by lahars and seasonal floods initiated downstream migration of a sediment wave that resulted in a profound cycle of aggradation and degradation in the lowermost reach of the river (depositional reach), 61-87 km from the source. Stratigraphic and sedimentologic relations in the alluvial fill, together with dendrochronologic dating of degradation terraces, demonstrate that (1) channel aggradation in response to sediment loading in the headwater canyons raised the river bed in this reach at least 23 m in a decade or less; (2) the transition from aggradation to degradation in the upper part of this reach roughly coincided with the end of the dome-building eruption; (3) fluvial sediment transport and deposition, augmented by one lahar, achieved a minimum average aggradation rate of similar to 2 m/yr; (4) the degradation phase of the cycle was more prolonged than the aggradation phase, requiring more than half a century for the river to reach its present bed elevation; and (5) the present longitudinal profile of the Sandy River in this reach is at least 3 m above the pre-eruption profile. The pattern and rate of channel response and recovery in the Sandy River following heavy sediment loading resemble those of other rivers similarly subjected to very large sediment inputs.
The magnitude of channel aggradation in the lower Sandy River, greater than that achieved at other volcanoes following much larger eruptions, was likely enhanced by lateral confinement of the channel within a narrow incised valley. A combination of at least one lahar and winter floods from frequent moderate-magnitude rainstorms and infrequent very large storms was responsible for flushing large volumes of sediment to the depositional reach. These conditions permitted a sedimentation response in the Sandy River that approached the magnitude of channel aggradation resulting elsewhere from large explosive eruptions and high-intensity rainfall regimes, despite the fact that the Sandy River aggradation was in response to an unremarkable dome-building eruption in a climate dominated by low to moderate rainfall intensities.
C1 [Pierson, Thomas C.] US Geol Survey, Cascades Volcano Observ, Vancouver, WA 98683 USA.
[Pringle, Patrick T.] Centralia Coll, Dept Sci, Centralia, WA 98531 USA.
[Cameron, Kenneth A.] Oregon Dept Environm Qual, Portland, OR 97204 USA.
RP Pierson, TC (reprint author), US Geol Survey, Cascades Volcano Observ, Vancouver, WA 98683 USA.
EM tpierson@usgs.gov
NR 98
TC 20
Z9 21
U1 1
U2 18
PU GEOLOGICAL SOC AMER, INC
PI BOULDER
PA PO BOX 9140, BOULDER, CO 80301-9140 USA
SN 0016-7606
J9 GEOL SOC AM BULL
JI Geol. Soc. Am. Bull.
PD JAN
PY 2011
VL 123
IS 1-2
BP 3
EP 20
DI 10.1130/B30127.1
PG 18
WC Geosciences, Multidisciplinary
SC Geology
GA 699XL
UT WOS:000285696100001
ER
PT J
AU Wainwright, AJ
Tosdal, RM
Forster, CN
Kirwin, DJ
Lewis, PD
Wooden, JL
AF Wainwright, Alan J.
Tosdal, Richard M.
Forster, Charles N.
Kirwin, Douglas J.
Lewis, Peter D.
Wooden, Joseph L.
TI Devonian and Carboniferous arcs of the Oyu Tolgoi porphyry Cu-Au
district, South Gobi region, Mongolia
SO GEOLOGICAL SOCIETY OF AMERICA BULLETIN
LA English
DT Article
ID ASIAN OROGENIC BELT; COPPER-GOLD DEPOSITS; PB ZIRCON AGES; U-PB; CRUSTAL
GROWTH; CONTINENTAL GROWTH; EVOLUTION; ACCRETION; GEOCHRONOLOGY;
COLLISION
AB The Central Asian orogenic belt consists of microcontinental blocks and mobile belts positioned between the Siberian craton and the Tarim and North China cratons. Extending across Asia for 5000 km, the belt consists of terranes that decrease in age southward away from the Siberian craton. A time-stratigraphic-structural sequence for the rocks is critical to defining the tectonic evolution of the belt. In the Oyu Tolgoi area of the South Gobi Desert (Mongolia), Devonian and Carboniferous rocks record the construction of multiple arcs, formation of a giant porphyry Cu-Au system, exhumation, and polyphase deformation. The oldest rocks are basaltic volcanic and subvolcanic rocks of the Devonian Alagbayan Group intruded by Late Devonian quartz monzodiorite stocks and dikes, which host giant porphyry Cu-Au deposits. The rocks were exhumed, overlain by pyroclastic rocks, and then tectonically buried by marine mafic supracrustal rocks prior to the youngest Devonian granodiorite intrusions. The postmineral Carboniferous Gurvankharaat Group unconformably overlying the deformed terrane consists of effusive, pyroclastic, subvolcanic and volcaniclastic rocks, as well as sedimentary units. The supracrustal rocks underwent polyphase shortening after 330 Ma and prior to 290 Ma. Variations in stratigraphic sequences suggest that the region is underlain by a submarine arc that became emergent during the Upper Devonian and remained subaerial to shallow subaqueous through much of the Carboniferous. Xenocrystic zircons in igneous rocks suggest that the offshore arcs were sufficiently close to ancient crust to have interacted with detritus shed into marine basins, most likely from the Siberian craton and fringing early Paleozoic terranes.
C1 [Wainwright, Alan J.; Tosdal, Richard M.] Univ British Columbia, Mineral Deposit Res Unit, Dept Earth & Ocean Sci, Vancouver, BC V6T 1Z4, Canada.
[Kirwin, Douglas J.] Ivanhoe Mines, Bangkok 12000, Thailand.
[Wooden, Joseph L.] US Geol Survey, Menlo Pk, CA 94025 USA.
RP Wainwright, AJ (reprint author), Univ British Columbia, Mineral Deposit Res Unit, Dept Earth & Ocean Sci, 6339 Stores Rd, Vancouver, BC V6T 1Z4, Canada.
EM rtosdal@gmail.com
NR 57
TC 16
Z9 17
U1 2
U2 19
PU GEOLOGICAL SOC AMER, INC
PI BOULDER
PA PO BOX 9140, BOULDER, CO 80301-9140 USA
SN 0016-7606
J9 GEOL SOC AM BULL
JI Geol. Soc. Am. Bull.
PD JAN
PY 2011
VL 123
IS 1-2
BP 306
EP 328
DI 10.1130/B30137.1
PG 23
WC Geosciences, Multidisciplinary
SC Geology
GA 699XL
UT WOS:000285696100019
ER
PT J
AU Asch, TH
Sweetkind, DS
AF Asch, Theodore H.
Sweetkind, Donald S.
TI Audiomagnetotelluric characterization of range-front faults, Snake
Range, Nevada
SO GEOPHYSICS
LA English
DT Article
ID EAST-CENTRAL NEVADA; MAGNETOTELLURICS; DECOLLEMENT
AB Two controlled-source audio-magnetotelluric (CSAMT) profiles were collected on the eastern flank of the Snake Range in eastern Nevada across geologically complex terrain to investigate the suspected presence of faults along the range front. The location of the range-bounding faults is not easily determined on geologic grounds because of the presence of extensive young sedimentary cover and overall geologic complexity. Characterization of the presence, location, and structural style of the range-front faults is critical to assessment of connectivity of groundwater aquifers near the mountain front and in adjacent alluvial basins. A total of 48 CSAMT soundings were recorded along two lines that were chosen to maximize subsurface geologic information. Two generations of faults were interpreted based on the CSAMT data: an older, low-angle fault that is cut by a younger, more steeply dipping fault. Lack of deep boreholes in the region required that the subsurface interpretation rely on analogy from surface outcrops within and adjacent to the study area. The success of the CSAMT method as applied in this study hinged on near-ideal collection conditions, the relatively high contrast in electrical resistivity provided by the rock types involved, and well-developed geologic conceptual models of the region.
C1 [Asch, Theodore H.] US Geol Survey, Crustal Geophys & Geochem Sci Ctr, UXO MEC Invest, Denver, CO 80225 USA.
RP Asch, TH (reprint author), US Geol Survey, Crustal Geophys & Geochem Sci Ctr, UXO MEC Invest, Box 25046, Denver, CO 80225 USA.
EM tasch@usgs.gov; dsweetkind@usgs.gov
OI Sweetkind, Donald/0000-0003-0892-4796
NR 27
TC 4
Z9 5
U1 0
U2 4
PU SOC EXPLORATION GEOPHYSICISTS
PI TULSA
PA 8801 S YALE ST, TULSA, OK 74137 USA
SN 0016-8033
J9 GEOPHYSICS
JI Geophysics
PD JAN-FEB
PY 2011
VL 76
IS 1
BP B1
EP B7
DI 10.1190/1.3511358
PG 7
WC Geochemistry & Geophysics
SC Geochemistry & Geophysics
GA 711VW
UT WOS:000286620500003
ER
PT J
AU Okubo, CH
Tornabene, LL
Lanza, NL
AF Okubo, Chris H.
Tornabene, Livio L.
Lanza, Nina L.
TI Constraints on mechanisms for the growth of gully alcoves in Gasa
crater, Mars, from two-dimensional stability assessments of rock slopes
SO ICARUS
LA English
DT Article
DE Mars, Surface; Geological processes; Tectonics
ID POTENTIAL FORMATION MECHANISMS; WHITE ISLAND VOLCANO; MARTIAN GULLIES;
LIQUID WATER; ENGINEERING GEOLOGY; BRITISH-COLUMBIA; VALLES-MARINERIS;
MASS STRENGTH; DEBRIS FLOWS; LANDSLIDE
AB The value of slope stability analyses for gaining insight into the geologic conditions that would facilitate the growth of gully alcoves on Mars is demonstrated in Gasa crater. Two-dimensional limit equilibrium methods are used in conjunction with high-resolution topography derived from stereo High Resolution Imaging Science Experiment (HiRISE) imagery. These analyses reveal three conditions that may produce observed alcove morphologies through slope failure: (1) a ca. >10 m thick surface layer that is either saturated with H2O ground ice or contains no groundwater/ice at all, above a zone of melting H2O ice or groundwater and under dynamic loading (i.e., seismicity), (2) a 1-10 m thick surface layer that is saturated with either melting H2O ice or groundwater and under dynamic loading, or (3) a >100 m thick surface layer that is saturated with either melting H2O ice or groundwater and under static loading. This finding of three plausible scenarios for slope failure demonstrates how the triggering mechanisms and characteristics of future alcove growth would be affected by prevailing environmental conditions. HiRISE images also reveal normal faults and other fractures tangential to the crowns of some gully alcoves that are interpreted to be the result of slope instability, which may facilitate future slope movement. Stability analyses show that the most failure-prone slopes in this area are found in alcoves that are adjacent to crown fractures. Accordingly, crown fractures appear to be a useful indicator of those alcoves that should be monitored for future landslide activity. Published by Elsevier Inc.
C1 [Okubo, Chris H.] US Geol Survey, Astrogeol Sci Ctr, Flagstaff, AZ 86001 USA.
[Tornabene, Livio L.] Univ Arizona, Lunar & Planetary Lab, Tucson, AZ 85721 USA.
[Lanza, Nina L.] Univ New Mexico, Inst Meteorit, Albuquerque, NM 87131 USA.
RP Okubo, CH (reprint author), US Geol Survey, Astrogeol Sci Ctr, Flagstaff, AZ 86001 USA.
EM cokubo@usgs.gov
FU HiRISE
FX Constructive discussions and reviews were provided by Nathan Bridges,
Kelly Kolb, Alfred McEwen and James Wray during the development of this
paper. Comments by Jay Dickson and an anonymous reviewer helped to focus
and clarify the discussion herein. Robin Fergason and Greg Vaughan
assisted with the USGS internal review of this paper (IP-018258). The
HiRISE DEM used in this study was constructed by C. Okubo at the HiRISE
Operations Center, University of Arizona. This work is supported by the
HiRISE project.
NR 87
TC 10
Z9 10
U1 0
U2 5
PU ACADEMIC PRESS INC ELSEVIER SCIENCE
PI SAN DIEGO
PA 525 B ST, STE 1900, SAN DIEGO, CA 92101-4495 USA
SN 0019-1035
J9 ICARUS
JI Icarus
PD JAN
PY 2011
VL 211
IS 1
BP 207
EP 221
DI 10.1016/j.icarus.2010.09.025
PG 15
WC Astronomy & Astrophysics
SC Astronomy & Astrophysics
GA 709MK
UT WOS:000286443600017
ER
PT J
AU Radebaugh, J
Lorenz, RD
Wall, SD
Kirk, RL
Wood, CA
Lunine, JI
Stofan, ER
Lopes, RMC
Valora, P
Farr, TG
Hayes, A
Stiles, B
Mitri, G
Zebker, H
Janssen, M
Wye, L
LeGall, A
Mitchell, KL
Paganelli, F
West, RD
Schaller, EL
AF Radebaugh, J.
Lorenz, R. D.
Wall, S. D.
Kirk, R. L.
Wood, C. A.
Lunine, J. I.
Stofan, E. R.
Lopes, R. M. C.
Valora, P.
Farr, T. G.
Hayes, A.
Stiles, B.
Mitri, G.
Zebker, H.
Janssen, M.
Wye, L.
LeGall, A.
Mitchell, K. L.
Paganelli, F.
West, R. D.
Schaller, E. L.
CA Cassini Radar Team
TI Regional geomorphology and history of Titan's Xanadu province
SO ICARUS
LA English
DT Article
DE Titan; Satellites, Surfaces; Saturn, Satellites
ID CASSINI RADAR OBSERVATIONS; MIDLATITUDE CLOUDS; SURFACE; IMAGES;
WAVELENGTH; TOPOGRAPHY; ROTATION; AMMONIA; DRIZZLE; DUNES
AB Titan's enigmatic Xanadu province has been seen in some detail with instruments from the Cassini spacecraft. The region contains some of the most rugged, mountainous terrain on Titan, with relief over 2000 m. Xanadu contains evolved and integrated river channels, impact craters, and dry basins filled with smooth, radar-dark material, perhaps sediments from past lake beds. Arcuate and aligned mountain chains give evidence of compressional tectonism, yet the overall elevation of Xanadu is puzzlingly low compared to surrounding sand seas. Lineations associated with mountain fronts and valley floors give evidence of extension that probably contributed to this regional lowering. Several locations on Xanadu's western and southern margins contain flow-like features that may be cryovolcanic in origin, perhaps ascended from lithospheric faults related to regional downdropping late in its history. Radiometry and scatterometry observations are consistent with a water-ice or water-ammonia-ice composition to its exposed, eroded, fractured bedrock; both microwave and visible to near-infrared (v-nIR) data indicate a thin overcoating of organics, likely derived from the atmosphere. We suggest Xanadu is one of the oldest terrains on Titan and that its origin and evolution have been controlled and shaped by compressional and then extensional tectonism in the icy crust and ongoing erosion by methane rainfall. (C) 2010 Elsevier Inc. All rights reserved.
C1 [Radebaugh, J.; Valora, P.] Brigham Young Univ, Dept Geol Sci, Provo, UT 84602 USA.
[Lorenz, R. D.] Johns Hopkins Appl Phys Lab, Laurel, MD 20723 USA.
[Wall, S. D.; Lopes, R. M. C.; Farr, T. G.; Stiles, B.; Mitri, G.; Janssen, M.; LeGall, A.; Mitchell, K. L.; West, R. D.] CALTECH, Jet Prop Lab, Pasadena, CA 91109 USA.
[Kirk, R. L.] US Geol Survey, Branch Astrogeol, Flagstaff, AZ 86001 USA.
[Wood, C. A.] Wheeling Jesuit Univ, Wheeling, WV 26003 USA.
[Lunine, J. I.] Univ Roma Tor Vergata, Dept Phys, I-00133 Rome, Italy.
[Stofan, E. R.; Paganelli, F.] Proxemy Res, Rectortown, VA 20140 USA.
[Hayes, A.] CALTECH, Dept Geol Sci, Pasadena, CA 91125 USA.
[Zebker, H.; Wye, L.] Stanford Univ, Dept Elect Engn, Stanford, CA 94305 USA.
[Schaller, E. L.] Univ Arizona, Lunar & Planetary Lab, Tucson, AZ 85721 USA.
RP Radebaugh, J (reprint author), Brigham Young Univ, Dept Geol Sci, S-389 ESC, Provo, UT 84602 USA.
EM jani.radebaugh@byu.edu
RI Hayes, Alexander/P-2024-2014; Lorenz, Ralph/B-8759-2016; Lopes,
Rosaly/D-1608-2016
OI Farr, Thomas/0000-0001-5406-2096; Hayes, Alexander/0000-0001-6397-2630;
Lorenz, Ralph/0000-0001-8528-4644; Lopes, Rosaly/0000-0002-7928-3167
FU Jet Propulsion Laboratory, California Institute of Technology; NASA;
program "Incentivazione alla mobilita' di studiosi straineri e italiani
residenti all'estero"
FX The authors acknowledge the NASA Cassini Project and all those who
designed and operate the remarkable Cassini spacecraft. Portions of this
work were supported by the Jet Propulsion Laboratory, California
Institute of Technology, under a contract with NASA. JIL acknowledges
support from the program "Incentivazione alla mobilita' di studiosi
straineri e italiani residenti all'estero." The authors also acknowledge
the thorough and helpful reviews from Geoffrey Collins and Devon Burr.
NR 70
TC 28
Z9 28
U1 0
U2 9
PU ACADEMIC PRESS INC ELSEVIER SCIENCE
PI SAN DIEGO
PA 525 B ST, STE 1900, SAN DIEGO, CA 92101-4495 USA
SN 0019-1035
EI 1090-2643
J9 ICARUS
JI Icarus
PD JAN
PY 2011
VL 211
IS 1
BP 672
EP 685
DI 10.1016/j.icarus.2010.07.022
PG 14
WC Astronomy & Astrophysics
SC Astronomy & Astrophysics
GA 709MK
UT WOS:000286443600050
ER
PT J
AU Heilweil, VM
Watt, DE
AF Heilweil, Victor M.
Watt, Dennis E.
TI Trench infiltration for managed aquifer recharge to permeable bedrock
SO HYDROLOGICAL PROCESSES
LA English
DT Article
DE trench infiltration; managed aquifer recharge; fractured sandstone;
trapped gas; seasonal viscosity variation
ID ARTIFICIAL RECHARGE; HYDRAULIC CONDUCTIVITY; BANK FILTRATION; SATURATED
SOILS; ENTRAPPED AIR; WATER; BASINS; GAS; PEAT; FLOW
AB Managed aquifer recharge to permeable bedrock is increasingly being utilized to enhance resources and maintain sustainable groundwater development practices. One such target is the Navajo Sandstone, an extensive regional aquifer located throughout the Colorado Plateau of the western United States. Spreading-basin and bank-filtration projects along the sandstone outcrop's western edge in southwestern Utah have recently been implemented to meet growth-related water demands. This paper reports on a new cost-effective surface-infiltration technique utilizing trenches for enhancing managed aquifer recharge to permeable bedrock. A 48-day infiltration trench experiment on outcropping Navajo Sandstone was conducted to evaluate this alternative surface-spreading artificial recharge method. Final infiltration rates through the bottom of the trench were about 0.5 m/day. These infiltration rates were an order of magnitude higher than rates from a previous surface-spreading experiment at the same site. The higher rates were likely caused by a combination of factors including the removal of lower permeability soil and surficial caliche deposits, access to open vertical sandstone fractures, a reduction in physical clogging associated with silt and biofilm layers, minimizing viscosity effects by maintaining isothermal conditions, minimizing chemical clogging caused by carbonate mineral precipitation associated with algal photosynthesis, and diminished gas clogging associated with trapped air and biogenic gases. This pilot study illustrates the viability of trench infiltration for enhancing surface spreading of managed aquifer recharge to permeable bedrock. Published in 2010 by John Wiley & Sons, Ltd.
C1 [Heilweil, Victor M.] US Geol Survey, Salt Lake City, UT 84119 USA.
[Watt, Dennis E.] US Bur Reclamat, Lower Colorado Reg Off, Boulder City, NV 89006 USA.
RP Heilweil, VM (reprint author), US Geol Survey, 2329 Orton Circle, Salt Lake City, UT 84119 USA.
EM heilweil@usgs.gov
FU Washington County Water Conservancy District; U.S. Geological Survey
FX This study was funded by the Washington County Water Conservancy
District in cooperation with the U.S. Geological Survey. Publication is
authorized by the Director of the U.S. Geological Survey. The authors
thank Joel Hubbell and Buck Sisson, Idaho National Laboratory, for their
technical assistance with installing the advanced tensiometers; and
Kevin Ellett, U.S. Geological Survey, for his technical assistance
calibrating and installing the heat dissipation probes.
NR 54
TC 4
Z9 4
U1 1
U2 23
PU JOHN WILEY & SONS LTD
PI CHICHESTER
PA THE ATRIUM, SOUTHERN GATE, CHICHESTER PO19 8SQ, W SUSSEX, ENGLAND
SN 0885-6087
J9 HYDROL PROCESS
JI Hydrol. Process.
PD JAN 1
PY 2011
VL 25
IS 1
BP 141
EP 151
DI 10.1002/hyp.7833
PG 11
WC Water Resources
SC Water Resources
GA 707JM
UT WOS:000286282300012
ER
PT J
AU Jung, HS
Lu, Z
Won, JS
Poland, MP
Miklius, A
AF Jung, H. S.
Lu, Z.
Won, J. S.
Poland, M. P.
Miklius, A.
TI Mapping Three-Dimensional Surface Deformation by Combining
Multiple-Aperture Interferometry and Conventional Interferometry:
Application to the June 2007 Eruption of Kilauea Volcano, Hawaii
SO IEEE GEOSCIENCE AND REMOTE SENSING LETTERS
LA English
DT Article
DE Interferometric synthetic aperture radar (SAR) (InSAR);
multiple-aperture interferometry (MAI); SAR; 3-D surface deformation
measurement
ID INSAR
AB Surface deformation caused by an intrusion and small eruption during June 17-19, 2007, along the East Rift Zone of Kilauea Volcano, Hawaii, was three-dimensionally reconstructed from radar interferograms acquired by the Advanced Land Observing Satellite (ALOS) phased-array type L-band synthetic aperture radar (SAR) (PALSAR) instrument. To retrieve the 3-D surface deformation, a method that combines multiple-aperture interferometry (MAI) and conventional interferometric SAR (InSAR) techniques was applied to one ascending and one descending ALOS PALSAR interferometric pair. The maximum displacements as a result of the intrusion and eruption are about 0.8, 2, and 0.7 m in the east, north, and up components, respectively. The radar-measured 3-D surface deformation agrees with GPS data from 24 sites on the volcano, and the root-mean-square errors in the east, north, and up components of the displacement are 1.6, 3.6, and 2.1 cm, respectively. Since a horizontal deformation of more than 1 m was dominantly in the north-northwest-south-southeast direction, a significant improvement of the north-south component measurement was achieved by the inclusion of MAI measurements that can reach a standard deviation of 3.6 cm. A 3-D deformation reconstruction through the combination of conventional InSAR and MAI will allow for better modeling, and hence, a more comprehensive understanding, of the source geometry associated with volcanic, seismic, and other processes that are manifested by surface deformation.
C1 [Jung, H. S.] Univ Seoul, Dept Geoinfomat, Seoul 130743, South Korea.
[Lu, Z.] US Geol Survey, EROS Ctr, Vancouver, WA 98683 USA.
[Lu, Z.] Cascades Volcano Observ, Vancouver, WA 98683 USA.
[Won, J. S.] Yonsei Univ, Dept Earth Syst Sci, Seoul 120749, South Korea.
[Poland, M. P.; Miklius, A.] US Geol Survey, Hawaiian Volcano Observ, Hawaii Natl Pk, HI 96718 USA.
RP Jung, HS (reprint author), Univ Seoul, Dept Geoinfomat, Seoul 130743, South Korea.
OI Poland, Michael/0000-0001-5240-6123; Jung, Hyung-Sup/0000-0003-2335-8438
FU Ministry of Education, Science and Technology
[M105DA000004-08D0100-0011A]; NASA [2005-0021]; USGS
FX Manuscript received July 22, 2009; revised November 25, 2009, January
30, 2010, and March 22, 2010; accepted May 24, 2010. Date of publication
July 8, 2010; date of current version December 27, 2010. This work was
supported in part by the National Space Lab Program through the Korea
Science and Engineering Foundation funded by the Ministry of Education,
Science and Technology (M105DA000004-08D0100-0011A), by the NASA Earth
Surface and Interior Program (2005-0021), by the USGS Volcano Hazards
Program, and by the USGS Land Remote Sensing Program.
NR 12
TC 42
Z9 46
U1 1
U2 20
PU IEEE-INST ELECTRICAL ELECTRONICS ENGINEERS INC
PI PISCATAWAY
PA 445 HOES LANE, PISCATAWAY, NJ 08855-4141 USA
SN 1545-598X
EI 1558-0571
J9 IEEE GEOSCI REMOTE S
JI IEEE Geosci. Remote Sens. Lett.
PD JAN
PY 2011
VL 8
IS 1
BP 34
EP 38
DI 10.1109/LGRS.2010.2051793
PG 5
WC Geochemistry & Geophysics; Engineering, Electrical & Electronic; Remote
Sensing; Imaging Science & Photographic Technology
SC Geochemistry & Geophysics; Engineering; Remote Sensing; Imaging Science
& Photographic Technology
GA 701SP
UT WOS:000285844000008
ER
PT J
AU McNutt, M
AF McNutt, Marcia
TI USGS Science in the Gulf Oil Spill: Novel Science Applications in a
Crisis
SO SEA TECHNOLOGY
LA English
DT Editorial Material
C1 US Geol Survey, Reston, VA 22092 USA.
RP McNutt, M (reprint author), US Geol Survey, 959 Natl Ctr, Reston, VA 22092 USA.
NR 0
TC 0
Z9 0
U1 0
U2 1
PU COMPASS PUBLICATIONS, INC
PI ARLINGTON
PA 1501 WILSON BLVD., STE 1001, ARLINGTON, VA 22209-2403 USA
SN 0093-3651
J9 SEA TECHNOL
JI Sea Technol.
PD JAN
PY 2011
VL 52
IS 1
BP 13
EP 14
PG 2
WC Engineering, Ocean
SC Engineering
GA 715FK
UT WOS:000286865800003
ER
PT S
AU Apps, JA
Zheng, LG
Spycher, N
Birkholzer, JT
Kharaka, Y
Thordsen, J
Kakouros, E
Trautz, R
AF Apps, John A.
Zheng, Liange
Spycher, Nicolas
Birkholzer, Jens T.
Kharaka, Yousif
Thordsen, James
Kakouros, Evangelos
Trautz, Robert
BE Gale, J
Hendriks, C
Turkenberg, W
TI TRANSIENT CHANGES IN SHALLOW GROUNDWATER CHEMISTRY DURING THE MSU ZERT
CO2 INJECTION EXPERIMENT
SO 10TH INTERNATIONAL CONFERENCE ON GREENHOUSE GAS CONTROL TECHNOLOGIES
SE Energy Procedia
LA English
DT Proceedings Paper
CT 10th International Conference on Greenhouse Gas Control Technologies
CY SEP 19-23, 2010
CL Amsterdam, NETHERLANDS
DE CO2; Release; Groundwater; Impact; Geochemistry
ID CATION-EXCHANGE; SEQUESTRATION; MONTMORILLONITE; ADSORPTION; TRANSPORT;
MEDIA; SITE
AB Food-grade CO2 was injected into a shallow aquifer through a perforated pipe placed horizontally 1-2 m below the water table at the Montana State University Zero Emission Research and Technology (MSU-ZERT) field site at Bozeman, Montana. The possible impact of elevated CO2 levels on groundwater quality was investigated by analyzing 80 water samples taken before, during, and following CO2 injection. Field determinations and laboratory analyses showed rapid and systematic changes in pH, alkalinity, and conductance, as well as increases in the aqueous concentrations of trace element species. The geochemical data were first evaluated using principal component analysis (PCA) in order to identify correlations between aqueous species. The PCA findings were then used in formulating a geochemical model to simulate the processes likely to be responsible for the observed increases in the concentrations of dissolved constituents. Modeling was conducted taking into account aqueous and surface complexation, cation exchange, and mineral precipitation and dissolution. Reasonable matches between measured data and model results suggest that: (1) CO2 dissolution in the groundwater causes calcite to dissolve. (2) Observed increases in the concentration of dissolved trace metals result likely from Ca+2-driven ion exchange with clays (smectites) and sorption/desorption reactions likely involving Fe (hydr)oxides. (3) Bicarbonate from CO2 dissolution appears to compete for sorption with anionic species such as HAsO4-2, potentially increasing dissolved As levels in groundwater. (C) 2011 Published by Elsevier Ltd.
C1 [Apps, John A.; Zheng, Liange; Spycher, Nicolas; Birkholzer, Jens T.] Univ Calif Berkeley, Lawrence Berkeley Natl Lab, Berkeley, CA 94720 USA.
[Kharaka, Yousif; Thordsen, James; Kakouros, Evangelos] US Geolog Survey, Berkeley, CA 94720 USA.
[Trautz, Robert] EPRI, Palo Alto, CA 94304 USA.
RP Apps, JA (reprint author), Univ Calif Berkeley, Lawrence Berkeley Natl Lab, Berkeley, CA 94720 USA.
RI Birkholzer, Jens/C-6783-2011
OI Birkholzer, Jens/0000-0002-7989-1912
NR 19
TC 12
Z9 12
U1 1
U2 8
PU ELSEVIER SCIENCE BV
PI AMSTERDAM
PA SARA BURGERHARTSTRAAT 25, PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS
SN 1876-6102
J9 ENRGY PROCED
PY 2011
VL 4
BP 3231
EP 3238
DI 10.1016/j.egypro.2011.02.241
PG 8
WC Energy & Fuels; Environmental Sciences
SC Energy & Fuels; Environmental Sciences & Ecology
GA BYE96
UT WOS:000298299703078
ER
PT S
AU Hovorka, SD
Meckel, TA
Trevino, RH
Lu, JM
Nicot, JP
Choi, JW
Freeman, D
Cook, P
Daley, TM
Ajo-Franklin, JB
Freifeild, BM
Doughty, C
Carrigan, CR
La Brecque, D
Kharaka, YK
Thordsen, JJ
Phelps, TJ
Yang, CB
Romanak, KD
Zhang, TW
Holt, RM
Lindler, JS
Butsch, RJ
AF Hovorka, Susan D.
Meckel, Timothy A.
Trevino, Ramon H.
Lu, Jiemin
Nicot, Jean-Philippe
Choi, Jong-Won
Freeman, David
Cook, Paul
Daley, Thomas M.
Ajo-Franklin, Jonathan B.
Freifeild, Barry M.
Doughty, Christine
Carrigan, Charles R.
La Brecque, Doug
Kharaka, Yousif K.
Thordsen, James J.
Phelps, Tommy J.
Yang, Changbing
Romanak, Katherine D.
Zhang, Tongwei
Holt, Robert M.
Lindler, Jeffery S.
Butsch, Robert J.
BE Gale, J
Hendriks, C
Turkenberg, W
TI Monitoring a large volume CO2 injection: Year two results from SECARB
project at Denbury's Cranfield, Mississippi, USA
SO 10TH INTERNATIONAL CONFERENCE ON GREENHOUSE GAS CONTROL TECHNOLOGIES
SE Energy Procedia
LA English
DT Proceedings Paper
CT 10th International Conference on Greenhouse Gas Control Technologies
CY SEP 19-23, 2010
CL Amsterdam, NETHERLANDS
DE Carbon Sequestration; Field Test; Monitoring
AB The Southeast Regional Carbon Sequestration Partnership (SECARB) early project in western Mississippi has been testing monitoring tools and approaches to document storage efficiency and storage permanence under conditions of CO2 EOR as well as downdip injection into brine. Denbury Onshore LLC is host for the study and has brought a depleted oil and gas reservoir, Cranfield Field, under CO2 flood. Injection was started in July 2008 and has now achieved injection rates greater than 1.2 million tons/year though 23 wells, with cumulative mass injected as of August, 2010 of 2.2 million metric tons. Injection is into coarse grained fluvial deposits of the Cretaceous lower Tuscaloosa Formation in a gentle anticline at depths of 3300 m. A team of researchers from 10 institutions has collected data from five study areas, each with a different goal and different spatial and temporal scale.
The Phase 2 study began at the start of injection and has been using pressure and temperature as a tool for assessing permanence mostly in the oil productive interval. Real-time read-out shows high sensitivity to distant changes in injection rate and confirms the geologic model of reservoir compartmentalization. Above-zone pressure monitoring similar to 120 m above the injection interval is used to test the sensitivity of this approach for documentation of integrity of the confining system in an area of numerous well completions as pressure increase is induced in the reservoir by more than 70 bar.
Monitoring of the High Volume Injection Test (HiVIT) area includes repeat measurements of aqueous geochemistry in the injection zone. Rock-water-CO2 interactions in the reservoir as CO2 dissolves are minimized by mineral "armoring" by abundant chlorite cement in high permeability reservoir sandstone. Geochemical monitoring of confined freshwater aquifers at depths of 70-100 m is underway. Groundwater analysis focuses on assessment of the sensitivity of this method to detect leakage above background variability.
A repeat seismic survey of the HiVIT is planned for late 2010 to assess saturation change especially in downdip brine-only areas. A study focused on feasibility of monitoring the shallow subsurface to separate leakage from normal complex surface fluxes is underway at an monitoring array installed in October 2009 to assess the interactions of recharge, soil gas, and shallow groundwater aquifers. Recent well re-entry and tracer injection will provide further information to interpret observed elevated deep-sourced methane.
The Detailed Area Study (DAS) is collecting dense time-lapse data from closely-spaced three well array of an injector and two observation wells. The observation wells were completed with fiberglass casing to facilitate electrical resistance tomography (ERT) measurements, and a diverse array of instrumentation was both cemented behind casing and suspended on tubing. Injection started at the DAS December 1, 2009. We have measured pulsed neutron and resistivity via wireline, downhole and above-zone pressure, distributed temperature, and fluid chemistry including introduced pulses of perfluorocarbons, noble gases, and SF6 as tracers. Between wells, time-lapse cross-well seismic and electrical resistance tomography (ERT) are used to measure saturation change. The goals are to measure changes as fluids evolve from single phase (brine) to two phase (CO2-brine) in order to document linkages between pressure and sweep efficiency. A time-lapse VSP survey bridges the vertical resolution and areal coverage between cross-well and surface seismic. The repeat surveys for many tools are scheduled for September, 2010.
Reservoir characterization based on cores, historic and new wireline log data, production history, hydrologic tests, fluid analysis, and a three-D seismic survey have been used in multiple numerical models to predict reservoir response in order to design effective monitoring strategies and optimize deployment. History matching of observed response to predicted response is used to interpret results and improve confidence in conceptual models and numerical approaches. Probabilistic methods have been used to assess the significant uncertainties resulting from reservoir heterogeneity.
C1 [Hovorka, Susan D.; Meckel, Timothy A.; Trevino, Ramon H.; Lu, Jiemin; Nicot, Jean-Philippe; Choi, Jong-Won; Yang, Changbing; Romanak, Katherine D.; Zhang, Tongwei] Univ Texas Austin, Gulf Coast Carbon Ctr, Bur Econ Geol, Jackson Sch Geosci, Austin, TX 78713 USA.
[Freeman, David] Sandia Technol LLC, Houston, TX 77041 USA.
[Cook, Paul; Daley, Thomas M.; Ajo-Franklin, Jonathan B.; Freifeild, Barry M.; Doughty, Christine] Lawrence Berkeley Natl Lab, Berkeley, CA 94720 USA.
[Carrigan, Charles R.] Lawrence Livermore Natl Lab, Livermore, CA 94551 USA.
[La Brecque, Doug] LLC, Multi Phase Technol, Sparks, NV 89431 USA.
[Kharaka, Yousif K.; Thordsen, James J.] US Geol Survey, Menlo Pk, CA 94025 USA.
[Phelps, Tommy J.] Oak Ridge Natl Lab, Oak Ridge, TN 37831 USA.
[Holt, Robert M.] Univ Mississippi, Oxford, MS 38677 USA.
[Lindler, Jeffery S.] Mississippi State Univ, Inst Clean Energy Technol, Mississippi State, MS 39762 USA.
[Butsch, Robert J.] Schlumberger Carbon Serv, Houston, TX 77056 USA.
RP Hovorka, SD (reprint author), Univ Texas Austin, Gulf Coast Carbon Ctr, Bur Econ Geol, Jackson Sch Geosci, Austin, TX 78713 USA.
RI Nicot, Jean-Philippe/A-3954-2009; Romanak, Katherine/M-5841-2013; Zhang,
Tongwei/M-8000-2014; Lu, Jiemin/H-3581-2011; yang,
changbing/A-3097-2009; Daley, Thomas/G-3274-2015; Ajo-Franklin,
Jonathan/G-7169-2015;
OI Romanak, Katherine/0000-0002-8763-7818; Lu, Jiemin/0000-0001-6783-5510;
yang, changbing/0000-0002-2442-2270; Daley, Thomas/0000-0001-9445-0843;
Ajo-Franklin, Jonathan/0000-0002-6666-4702
FU US Department of Energy, National Energy Technology Laboratory, Regional
Carbon Sequestration Partnerships program [DE-FC26-05NT42590]
FX This study is funded by the US Department of Energy, National Energy
Technology Laboratory as part of the Regional Carbon Sequestration
Partnerships program under contract number DE-FC26-05NT42590. SECARB is
led by Southern States Energy Board (www.sseb.org).
NR 9
TC 51
Z9 51
U1 1
U2 48
PU ELSEVIER SCIENCE BV
PI AMSTERDAM
PA SARA BURGERHARTSTRAAT 25, PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS
SN 1876-6102
J9 ENRGY PROCED
PY 2011
VL 4
BP 3478
EP 3485
DI 10.1016/j.egypro.2011.02.274
PG 8
WC Energy & Fuels; Environmental Sciences
SC Energy & Fuels; Environmental Sciences & Ecology
GA BYE96
UT WOS:000298299703111
ER
PT S
AU Garcia, S
Rosenbauer, RJ
Palandri, J
Maroto-Valer, MM
AF Garcia, Susana
Rosenbauer, Robert J.
Palandri, James
Maroto-Valer, M. Mercedes
BE Gale, J
Hendriks, C
Turkenberg, W
TI Experimental and simulation studies of iron oxides for geochemical
fixation of CO2-SO2 gas mixtures
SO 10TH INTERNATIONAL CONFERENCE ON GREENHOUSE GAS CONTROL TECHNOLOGIES
SE Energy Procedia
LA English
DT Proceedings Paper
CT 10th International Conference on Greenhouse Gas Control Technologies
CY SEP 19-23, 2010
CL Amsterdam, NETHERLANDS
DE saline aquifers; CO2-SO2 gas mixtures; CO2 storage
ID DEEP-SALINE AQUIFERS; CARBON-DIOXIDE; CO2 SEQUESTRATION; MINERAL TRAP;
FERRIC IRON; IN-SITU; SEDIMENTS; HEMATITE; STORAGE
AB Iron-bearing minerals are reactive phases of the subsurface environment and could potentially trap CO2-SO2 gas mixtures derived from fossil fuel combustion processes by their conversion to siderite (FeCO3) and dissolved sulfate. Changes in fluid and mineral compositions resulting from reactions, involving the co-injection of SO2 with CO2 were observed both theoretically and experimentally. Experiments were conducted with a natural hematite (alpha-Fe2O3) sample. A high pressure-high temperature apparatus was used to simulate conditions in geologic formations deeper than 800 m, where CO2 is in the supercritical state. Solid samples were allowed to react with a NaCl-NaOH brine and SO2-bearing CO2-dominated gas mixtures. The predicted equilibrium mineral assemblage at 100 degrees C and 250bar became hematite, dawsonite (NaAl(OH)(2)CO3), siderite (FeCO3) and quartz (SiO2). Experimentally, siderite and dawsonite, derived from the presence of kaolinite (Al2Si2O5(OH)(4)) in the parent material, were present in residual solids at longer reaction time intervals, which agreed well with results from the modelling work. (C) 2011 Published by Elsevier Ltd.
C1 [Garcia, Susana; Maroto-Valer, M. Mercedes] Univ Nottingham, CICCS, Energy & Sustainabil Res Div, Fac Engn, Univ Pk, Nottingham NG7 2RD, England.
[Rosenbauer, Robert J.] US Geol Survey, Menlo Pk, CA 94025 USA.
[Palandri, James] Univ Oregon, Dept Geol Sci, Eugene, OR 97403 USA.
RP Maroto-Valer, MM (reprint author), Univ Nottingham, CICCS, Energy & Sustainabil Res Div, Fac Engn, Univ Pk, Nottingham NG7 2RD, England.
EM Mercedes.maroto-valer@nottingham.ac.uk
RI Maroto-Valer, Mercedes/F-5016-2014
OI Maroto-Valer, Mercedes/0000-0003-1643-2863
FU Centre for Innovation in Carbon Capture and Storage (CICCS) through the
Engineering and Physical Sciences Research Council, EPSRC
[EP/F012098/1]; University of Nottingham Business-Engineering and
Science Travel Scholarships (BESTS) Programme
FX The financial support of the Centre for Innovation in Carbon Capture and
Storage (CICCS) through the Engineering and Physical Sciences Research
Council, EPSRC (EP/F012098/1), and the University of Nottingham
Business-Engineering and Science Travel Scholarships (BESTS) Programme
is gratefully acknowledged.
NR 19
TC 3
Z9 3
U1 1
U2 9
PU ELSEVIER SCIENCE BV
PI AMSTERDAM
PA SARA BURGERHARTSTRAAT 25, PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS
SN 1876-6102
J9 ENRGY PROCED
PY 2011
VL 4
BP 5108
EP 5113
DI 10.1016/j.egypro.2011.02.486
PG 6
WC Energy & Fuels; Environmental Sciences
SC Energy & Fuels; Environmental Sciences & Ecology
GA BYE96
UT WOS:000298299705090
ER
EF