{"pageNumber":"1969","pageRowStart":"49200","pageSize":"25","recordCount":184617,"records":[{"id":70037121,"text":"70037121 - 2010 - Holocene coastal dune fields used as indicators of net littoral transport: West Coast, USA","interactions":[],"lastModifiedDate":"2012-03-12T17:22:11","indexId":"70037121","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1801,"text":"Geomorphology","active":true,"publicationSubtype":{"id":10}},"title":"Holocene coastal dune fields used as indicators of net littoral transport: West Coast, USA","docAbstract":"Between Point Grenville, Washington, and Point Conception, California (1500 km distance) 21 dune fields record longshore transport in 20 littoral cells during the late Holocene. The direction of predominant littoral transport is established by relative positions of dune fields (north, central, or south) in 17 representative littoral cells. Dune field position is north of cell midpoints in northernmost Oregon and Washington, but is south of cell midpoints in southern Oregon and California. Downdrift sand trapping occurs at significant changes in shoreline angle and/or at bounding headlands that project at least 2.5 km seaward from the general coastal trend. Sand bypassing occurs around small headlands of less than 0.5 km in projection distance. A northward shift of the winter low-pressure center in the northeast Pacific Ocean is modeled from 11 ka to 0 ka. Nearshore current forcing in southern Oregon and northern California switched from northward in earliest Holocene time to southward in late Holocene time. The late Holocene (5-0 ka) is generally characterized by net northward littoral drift in northernmost Oregon and Washington and by net southward littoral drift in southernmost Oregon and California. A regional divergence of net transport direction in central Oregon, i.e. no net drift, is consistent with modeled wind and wave forcing at the present time (0 ka). ?? 2009 Elsevier B.V.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Geomorphology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.geomorph.2009.10.013","issn":"0169555X","usgsCitation":"Peterson, C., Stock, E., Hart, R., Percy, D., Hostetler, S.W., and Knott, J., 2010, Holocene coastal dune fields used as indicators of net littoral transport: West Coast, USA: Geomorphology, v. 116, no. 1-2, p. 115-134, https://doi.org/10.1016/j.geomorph.2009.10.013.","startPage":"115","endPage":"134","numberOfPages":"20","costCenters":[],"links":[{"id":217163,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.geomorph.2009.10.013"},{"id":245084,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"116","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a31dae4b0c8380cd5e2b3","contributors":{"authors":[{"text":"Peterson, C. D.","contributorId":79897,"corporation":false,"usgs":true,"family":"Peterson","given":"C. D.","affiliations":[],"preferred":false,"id":459487,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stock, E.","contributorId":13438,"corporation":false,"usgs":true,"family":"Stock","given":"E.","email":"","affiliations":[],"preferred":false,"id":459482,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hart, R.","contributorId":52793,"corporation":false,"usgs":true,"family":"Hart","given":"R.","affiliations":[],"preferred":false,"id":459485,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Percy, D.","contributorId":70913,"corporation":false,"usgs":true,"family":"Percy","given":"D.","email":"","affiliations":[],"preferred":false,"id":459486,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Hostetler, S. W. 0000-0003-2272-8302","orcid":"https://orcid.org/0000-0003-2272-8302","contributorId":42911,"corporation":false,"usgs":true,"family":"Hostetler","given":"S.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":459484,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Knott, J.R.","contributorId":26847,"corporation":false,"usgs":true,"family":"Knott","given":"J.R.","affiliations":[],"preferred":false,"id":459483,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70037233,"text":"70037233 - 2010 - The 2009 Samoa-Tonga great earthquake triggered doublet","interactions":[],"lastModifiedDate":"2012-03-12T17:22:10","indexId":"70037233","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2840,"text":"Nature","active":true,"publicationSubtype":{"id":10}},"title":"The 2009 Samoa-Tonga great earthquake triggered doublet","docAbstract":"Great earthquakes (having seismic magnitudes of at least 8) usually involve abrupt sliding of rock masses at a boundary between tectonic plates. Such interplate ruptures produce dynamic and static stress changes that can activate nearby intraplate aftershocks, as is commonly observed in the trench-slope region seaward of a great subduction zone thrust event1-4. The earthquake sequence addressed here involves a rare instance in which a great trench-slope intraplate earthquake triggered extensive interplate faulting, reversing the typical pattern and broadly expanding the seismic and tsunami hazard. On 29 September 2009, within two minutes of the initiation of a normal faulting event with moment magnitude 8.1 in the outer trench-slope at the northern end of the Tonga subduction zone, two major interplate underthrusting subevents (both with moment magnitude 7.8), with total moment equal to a second great earthquake of moment magnitude 8.0, ruptured the nearby subduction zone megathrust. The collective faulting produced tsunami waves with localized regions of about 12metres run-up that claimed 192 lives in Samoa, American Samoa and Tonga. Overlap of the seismic signals obscured the fact that distinct faults separated by more than 50km had ruptured with different geometries, with the triggered thrust faulting only being revealed by detailed seismic wave analyses. Extensive interplate and intraplate aftershock activity was activated over a large region of the northern Tonga subduction zone. ?? 2010 Macmillan Publishers Limited. All rights reserved.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Nature","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1038/nature09214","issn":"00280836","usgsCitation":"Lay, T., Ammon, C., Kanamori, H., Rivera, L., Koper, K., and Hutko, A.R., 2010, The 2009 Samoa-Tonga great earthquake triggered doublet: Nature, v. 466, no. 7309, p. 964-968, https://doi.org/10.1038/nature09214.","startPage":"964","endPage":"968","numberOfPages":"5","costCenters":[],"links":[{"id":475886,"rank":10000,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://resolver.caltech.edu/CaltechAUTHORS:20100830-105911579","text":"External Repository"},{"id":217430,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1038/nature09214"},{"id":245377,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"466","issue":"7309","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505ba64de4b08c986b32102e","contributors":{"authors":[{"text":"Lay, T.","contributorId":49909,"corporation":false,"usgs":true,"family":"Lay","given":"T.","email":"","affiliations":[],"preferred":false,"id":459994,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ammon, C.J.","contributorId":28389,"corporation":false,"usgs":true,"family":"Ammon","given":"C.J.","email":"","affiliations":[],"preferred":false,"id":459992,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kanamori, H.","contributorId":55438,"corporation":false,"usgs":true,"family":"Kanamori","given":"H.","affiliations":[],"preferred":false,"id":459995,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Rivera, L.","contributorId":39535,"corporation":false,"usgs":true,"family":"Rivera","given":"L.","email":"","affiliations":[],"preferred":false,"id":459993,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Koper, K.D.","contributorId":69798,"corporation":false,"usgs":true,"family":"Koper","given":"K.D.","email":"","affiliations":[],"preferred":false,"id":459996,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Hutko, Alexander R.","contributorId":101788,"corporation":false,"usgs":true,"family":"Hutko","given":"Alexander","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":459997,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70037222,"text":"70037222 - 2010 - Influence of sulfur-bearing polyatomic species on high precision measurements of Cu isotopic composition","interactions":[],"lastModifiedDate":"2012-03-12T17:22:11","indexId":"70037222","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1213,"text":"Chemical Geology","active":true,"publicationSubtype":{"id":10}},"title":"Influence of sulfur-bearing polyatomic species on high precision measurements of Cu isotopic composition","docAbstract":"An increased interest in high precision Cu isotope ratio measurements using multi-collector inductively coupled plasma mass spectrometry (MC-ICP-MS) has developed recently for various natural geologic systems and environmental applications, these typically contain high concentrations of sulfur, particularly in the form of sulfate (SO<sub>4</sub><sup>2-</sup>) and sulfide (S). For example, Cu, Fe, and Zn concentrations in acid mine drainage (AMD) can range from 100??g/L to greater than 50mg/L with sulfur species concentrations reaching greater than 1000mg/L. Routine separation of Cu, Fe and Zn from AMD, Cu-sulfide minerals and other geological matrices usually incorporates single anion exchange resin column chromatography for metal separation. During chromatographic separation, variable breakthrough of SO<sub>4</sub><sup>2-</sup> during anion exchange resin column chromatography into the Cu fractions was observed as a function of the initial sulfur to Cu ratio, column properties, and the sample matrix. SO<sub>4</sub><sup>2-</sup> present in the Cu fraction can form a polyatomic <sup>32</sup>S-<sup>14</sup>N-<sup>16</sup>O-<sup>1</sup>H species causing a direct mass interference with <sup>63</sup>Cu and producing artificially light ??<sup>65</sup>Cu values. Here we report the extent of the mass interference caused by SO<sub>4</sub><sup>2-</sup> breakthrough when measuring ??<sup>65</sup>Cu on natural samples and NIST SRM 976 Cu isotope spiked with SO<sub>4</sub><sup>2-</sup> after both single anion column chromatography and double anion column chromatography. A set of five 100??g/L Cu SRM 976 samples spiked with 500mg/L SO<sub>4</sub><sup>2-</sup> resulted in an average ??<sup>65</sup>Cu of -3.50?????5.42??? following single anion column separation with variable SO<sub>4</sub><sup>2-</sup> breakthrough but an average concentration of 770??g/L. Following double anion column separation, the average SO<sub>4</sub><sup>2-</sup>concentration of 13??g/L resulted in better precision and accuracy for the measured ??<sup>65</sup>Cu value of 0.01?????0.02??? relative to the expected 0??? for SRM 976. We conclude that attention to SO<sub>4</sub><sup>2-</sup> breakthrough on sulfur-rich samples is necessary for accurate and precise measurements of ??<sup>65</sup>Cu and may require the use of a double ion exchange column procedure. ?? 2010.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Chemical Geology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.chemgeo.2010.02.003","issn":"00092541","usgsCitation":"Pribil, M., Wanty, R., Ridley, W., and Borrok, D., 2010, Influence of sulfur-bearing polyatomic species on high precision measurements of Cu isotopic composition: Chemical Geology, v. 272, no. 1-4, p. 49-54, https://doi.org/10.1016/j.chemgeo.2010.02.003.","startPage":"49","endPage":"54","numberOfPages":"6","costCenters":[],"links":[{"id":245218,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":217283,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.chemgeo.2010.02.003"}],"volume":"272","issue":"1-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3b82e4b0c8380cd625c6","contributors":{"authors":[{"text":"Pribil, M.J.","contributorId":86481,"corporation":false,"usgs":true,"family":"Pribil","given":"M.J.","email":"","affiliations":[],"preferred":false,"id":459959,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wanty, R. B. 0000-0002-2063-6423","orcid":"https://orcid.org/0000-0002-2063-6423","contributorId":66704,"corporation":false,"usgs":true,"family":"Wanty","given":"R. B.","affiliations":[],"preferred":false,"id":459957,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ridley, W.I.","contributorId":72122,"corporation":false,"usgs":true,"family":"Ridley","given":"W.I.","email":"","affiliations":[],"preferred":false,"id":459958,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Borrok, D.M.","contributorId":38775,"corporation":false,"usgs":true,"family":"Borrok","given":"D.M.","email":"","affiliations":[],"preferred":false,"id":459956,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70037223,"text":"70037223 - 2010 - Localized surface disruptions observed by InSAR during strong earthquakes in Java and Hawai'i","interactions":[],"lastModifiedDate":"2018-10-30T10:00:30","indexId":"70037223","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1135,"text":"Bulletin of the Seismological Society of America","onlineIssn":"1943-3573","printIssn":"0037-1106","active":true,"publicationSubtype":{"id":10}},"title":"Localized surface disruptions observed by InSAR during strong earthquakes in Java and Hawai'i","docAbstract":"Interferometric Synthetic Aperture Radar data spanning strong earthquakes on the islands of Java and Hawai‘i in 2006 reveal patches of subsidence and incoherence indicative of localized ground failure. Interferograms spanning the 26 May 2006 Java earthquake suggest an area of about 7.5 km<sup>2</sup> of subsidence (~2 cm) and incoherence south of the city of Yogyakarta that correlates with significant damage to housing, high modeled peak ground accelerations, and poorly consolidated geologic deposits. The subsidence and incoherence is inferred to be a result of intense shaking and/or damage. At least five subsidence patches on the west side of the Island of Hawai‘i, ranging 0.3–2.2 km<sup>2</sup> in area and 3–8 cm in magnitude, occurred as a result of a pair of strong earthquakes on 15 October 2006. Although no felt reports or seismic data are available from the areas in Hawai‘i, the Java example suggests that the subsidence patches indicate areas of amplified earthquake shaking. Surprisingly, all subsidence areas in Hawai‘i were limited to recent, and supposedly stable, lava flows and may reflect geological conditions not detectable at the surface. In addition, two ‘a‘ā lava flows in Hawai‘i were partially incoherent in interferograms spanning the earthquakes, indicating surface disruption as a result of the earthquake shaking. Coearthquake incoherence of rubbly deposits, like ‘a‘ā flows, should be explored as a potential indicator of earthquake intensity and past strong seismic activity.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Bulletin of the Seismological Society of America","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Seismological Society of America","doi":"10.1785/0120090175","issn":"00371106","usgsCitation":"Poland, M.P., 2010, Localized surface disruptions observed by InSAR during strong earthquakes in Java and Hawai'i: Bulletin of the Seismological Society of America, v. 100, no. 2, p. 532-540, https://doi.org/10.1785/0120090175.","productDescription":"9 p.","startPage":"532","endPage":"540","costCenters":[{"id":336,"text":"Hawaiian Volcano Observatory","active":false,"usgs":true}],"links":[{"id":217284,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1785/0120090175"},{"id":245219,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"100","issue":"2","noUsgsAuthors":false,"publicationDate":"2010-03-15","publicationStatus":"PW","scienceBaseUri":"505a48f6e4b0c8380cd68270","contributors":{"authors":[{"text":"Poland, Michael P. 0000-0001-5240-6123 mpoland@usgs.gov","orcid":"https://orcid.org/0000-0001-5240-6123","contributorId":146118,"corporation":false,"usgs":true,"family":"Poland","given":"Michael","email":"mpoland@usgs.gov","middleInitial":"P.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":459960,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70037201,"text":"70037201 - 2010 - Evaluation of the use of performance reference compounds in an oasis-HLB adsorbent based passive sampler for improving water concentration estimates of polar herbicides in freshwater","interactions":[],"lastModifiedDate":"2012-03-12T17:21:44","indexId":"70037201","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1565,"text":"Environmental Science & Technology","onlineIssn":"1520-5851","printIssn":"0013-936X","active":true,"publicationSubtype":{"id":10}},"title":"Evaluation of the use of performance reference compounds in an oasis-HLB adsorbent based passive sampler for improving water concentration estimates of polar herbicides in freshwater","docAbstract":"Passive samplers such as the Polar Organic Chemical Integrative Sampler (POCIS) are useful tools for monitoring trace levels of polar organic chemicals in aquatic environments. The use of performance reference compounds (PRC) spiked into the POCIS adsorbent for in situ calibration may improve the semiquantitative nature of water concentration estimates based on this type of sampler. In this work, deuterium labeled atrazine-desisopropyl (DIA-d5) was chosen as PRC because of its relatively high fugacity from Oasis HLB (the POCIS adsorbent used) and our earlier evidence of its isotropic exchange. In situ calibration of POCIS spiked with DIA-d5was performed, and the resulting time-weighted average concentration estimates were compared with similar values from an automatic sampler equipped with Oasis HLB cartridges. Before PRC correction, water concentration estimates based on POCIS data sampling ratesfrom a laboratory calibration exposure were systematically lower than the reference concentrations obtained with the automatic sampler. Use of the DIA-d5 PRC data to correct POCIS sampling rates narrowed differences between corresponding values derived from the two methods. Application of PRCs for in situ calibration seems promising for improving POCIS-derived concentration estimates of polar pesticides. However, careful attention must be paid to the minimization of matrix effects when the quantification is performed by HPLC-ESI-MS/MS. ?? 2010 American Chemical Society.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Environmental Science and Technology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1021/es902256m","issn":"0013936X","usgsCitation":"Mazzella, N., Lissalde, S., Moreira, S., Delmas, F., Mazellier, P., and Huckins, J., 2010, Evaluation of the use of performance reference compounds in an oasis-HLB adsorbent based passive sampler for improving water concentration estimates of polar herbicides in freshwater: Environmental Science & Technology, v. 44, no. 5, p. 1713-1719, https://doi.org/10.1021/es902256m.","startPage":"1713","endPage":"1719","numberOfPages":"7","costCenters":[],"links":[{"id":216995,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1021/es902256m"},{"id":244902,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"44","issue":"5","noUsgsAuthors":false,"publicationDate":"2010-01-28","publicationStatus":"PW","scienceBaseUri":"505a0cf8e4b0c8380cd52d82","contributors":{"authors":[{"text":"Mazzella, N.","contributorId":63244,"corporation":false,"usgs":true,"family":"Mazzella","given":"N.","email":"","affiliations":[],"preferred":false,"id":459871,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lissalde, S.","contributorId":21789,"corporation":false,"usgs":true,"family":"Lissalde","given":"S.","email":"","affiliations":[],"preferred":false,"id":459867,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Moreira, S.","contributorId":60473,"corporation":false,"usgs":true,"family":"Moreira","given":"S.","email":"","affiliations":[],"preferred":false,"id":459869,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Delmas, F.","contributorId":74984,"corporation":false,"usgs":true,"family":"Delmas","given":"F.","email":"","affiliations":[],"preferred":false,"id":459872,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Mazellier, P.","contributorId":46797,"corporation":false,"usgs":true,"family":"Mazellier","given":"P.","email":"","affiliations":[],"preferred":false,"id":459868,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Huckins, J.N.","contributorId":62553,"corporation":false,"usgs":true,"family":"Huckins","given":"J.N.","email":"","affiliations":[],"preferred":false,"id":459870,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70037056,"text":"70037056 - 2010 - Population dynamics of American horseshoe crabs-historic climatic events and recent anthropogenic pressures","interactions":[],"lastModifiedDate":"2012-03-12T17:22:10","indexId":"70037056","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2774,"text":"Molecular Ecology","active":true,"publicationSubtype":{"id":10}},"title":"Population dynamics of American horseshoe crabs-historic climatic events and recent anthropogenic pressures","docAbstract":"Populations of the American horseshoe crab, Limulus polyphemus, have declined, but neither the causes nor the magnitude are fully understood. In order to evaluate historic demography, variation at 12 microsatellite DNA loci surveyed in 1218 L. polyphemus sampled from 28 localities was analysed with Bayesian coalescent-based methods. The analysis showed strong declines in population sizes throughout the species' distribution except in the geographically isolated southern-most population in Mexico, where a strong increase in population size was inferred. Analyses suggested that demographic changes in the core of the distribution occurred in association with the recolonization after the Ice Age and also by anthropogenic effects, such as the past overharvest of the species for fertilizer or the current use of the animals as bait for American eel (Anguilla rostrata) and whelk (Busycon spp.) fisheries. This study highlights the importance of considering both climatic changes and anthropogenic effects in efforts to understand population dynamics-a topic which is highly relevant in the ongoing assessments of the effects of climate change and overharvest. ?? 2010 Blackwell Publishing Ltd.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Molecular Ecology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1111/j.1365-294X.2010.04732.x","issn":"09621083","usgsCitation":"Faurby, S., King, T., Obst, M., Hallerman, E., Pertoldi, C., and Funch, P., 2010, Population dynamics of American horseshoe crabs-historic climatic events and recent anthropogenic pressures: Molecular Ecology, v. 19, no. 15, p. 3088-3100, https://doi.org/10.1111/j.1365-294X.2010.04732.x.","startPage":"3088","endPage":"3100","numberOfPages":"13","costCenters":[],"links":[{"id":217158,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1111/j.1365-294X.2010.04732.x"},{"id":245079,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"19","issue":"15","noUsgsAuthors":false,"publicationDate":"2010-06-25","publicationStatus":"PW","scienceBaseUri":"505a7d46e4b0c8380cd79e51","contributors":{"authors":[{"text":"Faurby, S.","contributorId":95291,"corporation":false,"usgs":true,"family":"Faurby","given":"S.","email":"","affiliations":[],"preferred":false,"id":459177,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"King, T.L.","contributorId":93416,"corporation":false,"usgs":true,"family":"King","given":"T.L.","email":"","affiliations":[],"preferred":false,"id":459176,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Obst, M.","contributorId":24596,"corporation":false,"usgs":true,"family":"Obst","given":"M.","email":"","affiliations":[],"preferred":false,"id":459174,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hallerman, E.M.","contributorId":23671,"corporation":false,"usgs":true,"family":"Hallerman","given":"E.M.","email":"","affiliations":[],"preferred":false,"id":459173,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Pertoldi, C.","contributorId":21378,"corporation":false,"usgs":true,"family":"Pertoldi","given":"C.","email":"","affiliations":[],"preferred":false,"id":459172,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Funch, P.","contributorId":91335,"corporation":false,"usgs":true,"family":"Funch","given":"P.","email":"","affiliations":[],"preferred":false,"id":459175,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70037204,"text":"70037204 - 2010 - Abundance and sexual size dimorphism of the giant gartersnake (Thamnophis gigas) in the Sacramento valley of California","interactions":[],"lastModifiedDate":"2017-11-18T12:45:23","indexId":"70037204","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2334,"text":"Journal of Herpetology","active":true,"publicationSubtype":{"id":10}},"title":"Abundance and sexual size dimorphism of the giant gartersnake (Thamnophis gigas) in the Sacramento valley of California","docAbstract":"The Giant Gartersnake (Thamnophis gigas) is restricted to wetlands of the Central Valley of California. Because of wetland loss in this region, the Giant Gartersnake is both federally and state listed as threatened. We conducted markrecapture studies of four populations of the Giant Gartersnake in the Sacramento Valley (northern Central Valley), California, to obtain baseline data on abundance and density to assist in recovery planning for this species. We sampled habitats that ranged from natural, unmanaged marsh to constructed managed marshes and habitats associated with rice agriculture. Giant Gartersnake density in a natural wetland (1.90 individuals/ha) was an order of magnitude greater than in a managed wetland subject to active season drying (0.17 individuals/ha). Sex ratios at all sites were not different from 1 1, and females were longer and heavier than males. Females had greater body condition than males, and individuals at the least disturbed sites had significantly greater body condition than individuals at the managed wetland. The few remaining natural wetlands in the Central Valley are important, productive habitat for the Giant Gartersnake, and should be conserved and protected. Wetlands constructed and restored for the Giant Gartersnake should be modeled after the permanent, shallow wetlands representative of historic Giant Gartersnake habitat. ?? 2010 Society for the Study of Amphibians and Reptiles.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Herpetology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1670/08-337.1","issn":"00221511","usgsCitation":"Wylie, G., Casazza, M.L., Gregory, C., and Halstead, B., 2010, Abundance and sexual size dimorphism of the giant gartersnake (Thamnophis gigas) in the Sacramento valley of California: Journal of Herpetology, v. 44, no. 1, p. 94-103, https://doi.org/10.1670/08-337.1.","startPage":"94","endPage":"103","numberOfPages":"10","costCenters":[],"links":[{"id":475808,"rank":10000,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://doi.org/10.1670/08-337.1","text":"External Repository"},{"id":244934,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":217024,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1670/08-337.1"}],"volume":"44","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e65ce4b0c8380cd47376","contributors":{"authors":[{"text":"Wylie, G.D.","contributorId":68238,"corporation":false,"usgs":true,"family":"Wylie","given":"G.D.","email":"","affiliations":[],"preferred":false,"id":459891,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Casazza, Michael L. 0000-0002-5636-735X mike_casazza@usgs.gov","orcid":"https://orcid.org/0000-0002-5636-735X","contributorId":2091,"corporation":false,"usgs":true,"family":"Casazza","given":"Michael","email":"mike_casazza@usgs.gov","middleInitial":"L.","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":true,"id":459888,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gregory, C.J.","contributorId":32487,"corporation":false,"usgs":true,"family":"Gregory","given":"C.J.","email":"","affiliations":[],"preferred":false,"id":459889,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Halstead, B.J.","contributorId":42045,"corporation":false,"usgs":true,"family":"Halstead","given":"B.J.","email":"","affiliations":[],"preferred":false,"id":459890,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70046693,"text":"dds49101 - 2010 - Attributes for MRB_E2RF1 Catchments by Major River Basins in the Conterminous United States: Artificial Drainage (1992) and Irrigation (1997)","interactions":[],"lastModifiedDate":"2013-11-25T16:05:21","indexId":"dds49101","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":310,"text":"Data Series","code":"DS","onlineIssn":"2327-638X","printIssn":"2327-0271","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"491-01","title":"Attributes for MRB_E2RF1 Catchments by Major River Basins in the Conterminous United States: Artificial Drainage (1992) and Irrigation (1997)","docAbstract":"This tabular data set represents the estimated area of artifical drainage for the year 1992 and irrigation types for the year 1997 compiled for every MRB_E2RF1 catchment of  Major River Basins (MRBs, Crawford and others, 2006). The source data sets were derived from tabular National Resource Inventory (NRI) data sets created by the National Resources Conservation Service (NRCS, U.S. Department of Agriculture, 1995, 2000).  Artificial drainage is defined as subsurface drains and ditches.  Irrigation types are defined as gravity and pressure.  Subsurface drains are described as conduits, such as corrugated plastic tubing, tile, or pipe, installed beneath the ground surface to collect and/or convey drainage. Surface drainage field ditches are described as graded ditches for collecting excess water.  Gravity irrigation source is described as irrigation delivered to the farm and/or field by canals or pipelines open to the atmosphere; and water is distributed by the force of gravity down the field by: (1) A surface irrigation system (border, basin, furrow, corrugation, wild flooding, etc.) or (2) Sub-surface irrigation pipelines or ditches. Pressure irrigation source is described as irrigation delivered to the farm and/or field in pump or elevation-induced pressure pipelines, and water is distributed across the field by: (1) Sprinkle irrigation (center pivot, linear move, traveling gun, side roll, hand move, big gun, or fixed set sprinklers), or (2) Micro irrigation (drip emitters, continuous tube bubblers, micro spray or micro sprinklers). NRI data do not include Federal lands and are thus excluded from this dataset.  The tabular data for drainage were spatially apportioned to the National Land Cover Dataset (NLCD, Kerie Hitt, U.S. Geological Survey, written commun., 2005) and the tabular data for irrigation were spatially apportioned to an enhanced version of the National Land Cover Dataset (NLCDe, Nakagaki and others, 2007). The MRB_E2RF1 catchments are based on a modified version of the U.S. Environmental Protection Agency's (USEPA) ERF1_2 and include enhancements to support national and regional-scale surface-water quality modeling (Nolan and others, 2002; Brakebill and others, 2011). Data were compiled for every MRB_E2RF1 catchment for the conterminous United States covering New England and Mid-Atlantic (MRB1), South Atlantic-Gulf and Tennessee (MRB2), the Great Lakes, Ohio, Upper Mississippi, and Souris-Red-Rainy (MRB3), the Missouri (MRB4), the Lower Mississippi, Arkansas-White-Red, and Texas-Gulf (MRB5), the Rio Grande, Colorado, and the Great basin (MRB6), the Pacific Northwest (MRB7) river basins, and California (MRB8).","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/dds49101","usgsCitation":"Wieczorek, M., and LaMotte, A.E., 2010, Attributes for MRB_E2RF1 Catchments by Major River Basins in the Conterminous United States: Artificial Drainage (1992) and Irrigation (1997): U.S. Geological Survey Data Series 491-01, Dataset, https://doi.org/10.3133/dds49101.","productDescription":"Dataset","onlineOnly":"Y","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":274189,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":274186,"type":{"id":16,"text":"Metadata"},"url":"https://water.usgs.gov/GIS/metadata/usgswrd/XML/mrb_e2rf1_adrain.xml"}],"country":"United States","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -127.910792,23.243486 ], [ -127.910792,51.657387 ], [ -65.327751,51.657387 ], [ -65.327751,23.243486 ], [ -127.910792,23.243486 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51cabbdfe4b0d298e5434c24","contributors":{"authors":[{"text":"Wieczorek, Michael mewieczo@usgs.gov","contributorId":2309,"corporation":false,"usgs":true,"family":"Wieczorek","given":"Michael","email":"mewieczo@usgs.gov","affiliations":[{"id":374,"text":"Maryland Water Science Center","active":true,"usgs":true}],"preferred":false,"id":480024,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"LaMotte, Andrew E. 0000-0002-1434-6518 alamotte@usgs.gov","orcid":"https://orcid.org/0000-0002-1434-6518","contributorId":2842,"corporation":false,"usgs":true,"family":"LaMotte","given":"Andrew","email":"alamotte@usgs.gov","middleInitial":"E.","affiliations":[{"id":374,"text":"Maryland Water Science Center","active":true,"usgs":true}],"preferred":true,"id":480025,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70194875,"text":"70194875 - 2010 - Controls on biochemical oxygen demand in the upper Klamath River, Oregon","interactions":[],"lastModifiedDate":"2018-01-26T09:56:42","indexId":"70194875","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1213,"text":"Chemical Geology","active":true,"publicationSubtype":{"id":10}},"title":"Controls on biochemical oxygen demand in the upper Klamath River, Oregon","docAbstract":"<p><span>A series of 30-day biochemical oxygen demand (BOD) experiments were conducted on water column samples from a reach of the upper Klamath River that experiences hypoxia and anoxia in summer. Samples were incubated with added nitrification inhibitor to measure carbonaceous BOD (CBOD), untreated to measure total BOD, which included demand from nitrogenous BOD (NBOD), and coarse-filtered to examine the effect of removing large particulate matter. All BOD data were fit well with a two-group model, so named because it considered contributions from both labile and refractory pools of carbon:&nbsp;</span><i>BOD</i><sub><i>t</i></sub><span>&nbsp;</span><span>=</span><span>&nbsp;</span><i>a</i><sub>1</sub><span>(1</span><span>&nbsp;</span><span>−</span><span>&nbsp;</span><i>e</i><sup>−&nbsp;<i>a</i><sub>0</sub><i>t</i></sup><span>)</span><span>&nbsp;</span><span>+</span><span>&nbsp;</span><i>a</i><sub>2</sub><i>t</i><span>. Site-average labile first-order decay rates<span>&nbsp;</span></span><i>a</i><sub>0</sub><span><span>&nbsp;</span>ranged from 0.15 to 0.22/day for CBOD and 0.11 to 0.29/day for BOD. Site-average values of refractory zero-order decay rates<span>&nbsp;</span></span><i>a</i><sub>2</sub><span><span>&nbsp;</span>ranged from 0.13 to 0.25</span><span>&nbsp;</span><span>mg/L/day for CBOD and 0.01 to 0.45</span><span>&nbsp;</span><span>mg/L/day for BOD; the zero-order CBOD decay rate increased from early- to mid-summer. Values of ultimate CBOD for the labile component<span>&nbsp;</span></span><i>a</i><sub>1</sub><span><span>&nbsp;</span>ranged from 5.5 to 28.8</span><span>&nbsp;</span><span>mg/L for CBOD, and 7.6 to 30.8</span><span>&nbsp;</span><span>mg/L for BOD. Two upstream sites had higher CBOD compared to those downstream. Maximum measured total BOD</span><sub>5</sub><span><span>&nbsp;</span>and BOD</span><sub>30</sub><span><span>&nbsp;</span>during the study were 26.5 and 55.4</span><span>&nbsp;</span><span>mg/L; minimums were 4.2 and 13.6</span><span>&nbsp;</span><span>mg/L. For most samples, the oxygen demand from the three components considered here were: labile CBOD</span><span>&nbsp;</span><span>&gt;</span><span>&nbsp;</span><span>NBOD</span><span>&nbsp;</span><span>&gt;</span><span>&nbsp;</span><span>refractory CBOD, though the relative importance of refractory CBOD to oxygen demand increased over time. Coarse-filtering reduced CBOD for samples with high particulate carbon and high biovolumes of<span>&nbsp;</span></span><i>Aphanizomenon flos-aquae</i><span>. There was a strong positive correlation between BOD, CBOD, and the labile component of CBOD to particulate C and N, with weaker positive correlation to field pH, field dissolved oxygen, and total N. The refractory component of CBOD was not correlated to particulate matter, instead showing weak but statistically significant correlation to dissolved organic carbon, UV absorbance at 254</span><span>&nbsp;</span><span>nm, and total N. Particulate organic matter, especially the alga<span>&nbsp;</span></span><i>A.</i><i>flos-aquae</i><span>, is an important component of oxygen demand in this reach of the Klamath River, though refractory dissolved organic matter would continue to exert an oxygen demand over longer time periods and as water travels downstream.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.chemgeo.2009.08.007","usgsCitation":"Sullivan, A., Snyder, D.M., and Rounds, S.A., 2010, Controls on biochemical oxygen demand in the upper Klamath River, Oregon: Chemical Geology, v. 269, no. 1-2, p. 12-21, https://doi.org/10.1016/j.chemgeo.2009.08.007.","productDescription":"10 p.","startPage":"12","endPage":"21","ipdsId":"IP-013602","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":350636,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Oregon","otherGeospatial":"Klamath River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -121.99150085449219,\n              42.0518419954737\n            ],\n            [\n              -121.73538208007811,\n              42.0518419954737\n            ],\n            [\n              -121.73538208007811,\n              42.288992779814045\n            ],\n            [\n              -121.99150085449219,\n              42.288992779814045\n            ],\n            [\n              -121.99150085449219,\n              42.0518419954737\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"269","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5a6c4c99e4b06e28e9cabb24","contributors":{"authors":[{"text":"Sullivan, Annett B. 0000-0001-7783-3906 annett@usgs.gov","orcid":"https://orcid.org/0000-0001-7783-3906","contributorId":79821,"corporation":false,"usgs":true,"family":"Sullivan","given":"Annett B.","email":"annett@usgs.gov","affiliations":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"preferred":false,"id":725841,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Snyder, Dean M.","contributorId":201484,"corporation":false,"usgs":false,"family":"Snyder","given":"Dean","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":725842,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rounds, Stewart A. 0000-0002-8540-2206 sarounds@usgs.gov","orcid":"https://orcid.org/0000-0002-8540-2206","contributorId":905,"corporation":false,"usgs":true,"family":"Rounds","given":"Stewart","email":"sarounds@usgs.gov","middleInitial":"A.","affiliations":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"preferred":true,"id":725843,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70037436,"text":"70037436 - 2010 - Geochronology and paleoclimatic implications of the last deglaciation of the Mauna Kea Ice Cap, Hawaii","interactions":[],"lastModifiedDate":"2012-03-12T17:22:09","indexId":"70037436","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1427,"text":"Earth and Planetary Science Letters","active":true,"publicationSubtype":{"id":10}},"title":"Geochronology and paleoclimatic implications of the last deglaciation of the Mauna Kea Ice Cap, Hawaii","docAbstract":"We present new 3He surface exposure ages on moraines and bedrock near the summit of Mauna Kea, Hawaii, which refine the age of the Mauna Kea Ice Cap during the Local Last Glacial Maximum (LLGM) and identify a subsequent fluctuation of the ice margin. The 3He ages, when combined with those reported previously, indicate that the local ice-cap margin began to retreat from its LLGM extent at 20.5??2.5ka, in agreement with the age of deglaciation determined from LLGM moraines elsewhere in the tropics. The ice-cap margin receded to a position at least 3km upslope for ~4.5-5.0kyr before readvancing nearly to its LLGM extent. The timing of this readvance at ~15.4ka corresponds to a large reduction of the Atlantic meridional overturning circulation (AMOC) following Heinrich Event 1. Subsequent ice-margin retreat began at 14.6??1.9ka, corresponding to a rapid resumption of the AMOC and onset of the B??lling warm interval, with the ice cap melting rapidly to complete deglaciation. Additional 3He ages obtained from a flood deposit date the catastrophic outburst of a moraine-dammed lake roughly coeval with the Younger Dryas cold interval, suggesting a more active hydrological cycle on Mauna Kea at this time. A coupled mass balance and ice dynamics model is used to constrain the climate required to generate ice caps of LLGM and readvance sizes. The depression of the LLGM equilibrium line altitude requires atmospheric cooling of 4.5??1??C, whereas the mass balance modeling indicates an accompanying increase in precipitation of as much as three times that of present. We hypothesize (1) that the LLGM temperature depression was associated with global cooling, (2) that the temperature depression that contributed to the readvance occurred in response to an atmospheric teleconnection to the North Atlantic, and (3) that the precipitation enhancement associated with both events occurred in response to a southward shift in the position of the inter-tropical convergence zone (ITCZ). Such a shift in the ITCZ would have allowed midlatitude cyclones to reach Mauna Kea more frequently which would have increased precipitation at high elevations and caused additional cooling. ?? 2010 Elsevier B.V.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Earth and Planetary Science Letters","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.epsl.2010.06.025","issn":"0012821X","usgsCitation":"Anslow, F.S., Clark, P., Kurz, M., and Hostetler, S.W., 2010, Geochronology and paleoclimatic implications of the last deglaciation of the Mauna Kea Ice Cap, Hawaii: Earth and Planetary Science Letters, v. 297, no. 1-2, p. 234-248, https://doi.org/10.1016/j.epsl.2010.06.025.","startPage":"234","endPage":"248","numberOfPages":"15","costCenters":[],"links":[{"id":245235,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":217300,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.epsl.2010.06.025"}],"volume":"297","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a1732e4b0c8380cd55409","contributors":{"authors":[{"text":"Anslow, Faron S.","contributorId":35442,"corporation":false,"usgs":true,"family":"Anslow","given":"Faron","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":461056,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Clark, P.U.","contributorId":78449,"corporation":false,"usgs":true,"family":"Clark","given":"P.U.","email":"","affiliations":[],"preferred":false,"id":461059,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kurz, M.D.","contributorId":66845,"corporation":false,"usgs":true,"family":"Kurz","given":"M.D.","email":"","affiliations":[],"preferred":false,"id":461058,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hostetler, S. W. 0000-0003-2272-8302","orcid":"https://orcid.org/0000-0003-2272-8302","contributorId":42911,"corporation":false,"usgs":true,"family":"Hostetler","given":"S.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":461057,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70037355,"text":"70037355 - 2010 - Predicting mercury concentrations in mallard eggs from mercury in the diet or blood of adult females and from duckling down feathers","interactions":[],"lastModifiedDate":"2018-10-17T16:50:41","indexId":"70037355","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1571,"text":"Environmental Toxicology and Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"Predicting mercury concentrations in mallard eggs from mercury in the diet or blood of adult females and from duckling down feathers","docAbstract":"Measurements of Hg concentrations in avian eggs can be used to predict possible harm to reproduction, but it is not always possible to sample eggs. When eggs cannot be sampled, some substitute tissue, such as female blood, the diet of the breeding female, or down feathers of hatchlings, must be used. When female mallards (Anas platyrhynchos) were fed diets containing methylmercury chloride, the concentration of Hg in a sample of their blood was closely correlated with the concentration of Hg in the egg they laid the day they were bled (r<sup>2</sup>=0.88; p&lt;0.001). Even when the blood sample was taken more than two weeks after an egg was laid, there was a strong correlation between Hg concentrations in female blood and eggs (r<sup>2</sup>=0.67; p&lt;0.0002). When we plotted the dietary concentrations of Hg we fed to the egg-laying females against the concentrations of Hg in their eggs, the r<sup>2</sup> value was 0.96 (p&lt;0.0001). When the concentrations of Hg in the down feathers of newly hatched ducklings were plotted against Hg in the whole ducklings, the r <sup>2</sup> value was 0.99 ( p&lt;0.0003). Although measuring Hg in eggs may be the most direct way of predicting possible embryotoxicity, our findings demonstrate that measuring Hg in the diet of breeding birds, in the blood of egg-laying females, or in down feathers of hatchlings all can be used to estimate what concentration of Hg may have been in the egg.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Environmental Toxicology and Chemistry","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1002/etc.50","issn":"07307268","usgsCitation":"Heinz, G.H., Hoffman, D.J., Klimstra, J.D., and Stebbins, K.R., 2010, Predicting mercury concentrations in mallard eggs from mercury in the diet or blood of adult females and from duckling down feathers: Environmental Toxicology and Chemistry, v. 29, no. 2, p. 389-392, https://doi.org/10.1002/etc.50.","productDescription":"4 p.","startPage":"389","endPage":"392","numberOfPages":"4","costCenters":[{"id":34983,"text":"Contaminant Biology Program","active":true,"usgs":true}],"links":[{"id":475840,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1002/etc.50","text":"Publisher Index Page"},{"id":245324,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":217379,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1002/etc.50"}],"volume":"29","issue":"2","noUsgsAuthors":false,"publicationDate":"2009-10-16","publicationStatus":"PW","scienceBaseUri":"505a81bbe4b0c8380cd7b6d1","contributors":{"authors":[{"text":"Heinz, Gary H.","contributorId":85698,"corporation":false,"usgs":true,"family":"Heinz","given":"Gary","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":460626,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hoffman, David J.","contributorId":86075,"corporation":false,"usgs":true,"family":"Hoffman","given":"David","email":"","middleInitial":"J.","affiliations":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"preferred":false,"id":460623,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Klimstra, Jon D.","contributorId":6985,"corporation":false,"usgs":false,"family":"Klimstra","given":"Jon","email":"","middleInitial":"D.","affiliations":[{"id":6661,"text":"US Fish and Wildlife Service","active":true,"usgs":false}],"preferred":false,"id":460625,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Stebbins, Katherine R.","contributorId":94012,"corporation":false,"usgs":true,"family":"Stebbins","given":"Katherine","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":460624,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70037678,"text":"70037678 - 2010 - Tree-ring 14C links seismic swarm to CO2 spike at Yellowstone, USA","interactions":[],"lastModifiedDate":"2012-04-30T16:43:33","indexId":"70037678","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1796,"text":"Geology","active":true,"publicationSubtype":{"id":10}},"title":"Tree-ring 14C links seismic swarm to CO2 spike at Yellowstone, USA","docAbstract":"Mechanisms to explain swarms of shallow seismicity and inflation-deflation cycles at Yellowstone caldera (western United States) commonly invoke episodic escape of magma-derived brines or gases from the ductile zone, but no correlative changes in the surface efflux of magmatic constituents have ever been documented. Our analysis of individual growth rings in a tree core from the Mud Volcano thermal area within the caldera links a sharp ~25% drop in 14C to a local seismic swarm in 1978. The implied fivefold increase in CO2 emissions clearly associates swarm seismicity with upflow of magma-derived fluid and shows that pulses of magmatic CO2 can rapidly traverse the 5-kmthick brittle zone, even through Yellowstone's enormous hydrothermal reservoir. The 1978 event predates annual deformation surveys, but recognized connections between subsequent seismic swarms and changes in deformation suggest that CO2 might drive both processes. ?? 2010 Geological Society of America.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Geology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1130/G31345.1","issn":"00917613","usgsCitation":"Evans, W.C., Bergfeld, D., McGeehin, J., King, J., and Heasler, H., 2010, Tree-ring 14C links seismic swarm to CO2 spike at Yellowstone, USA: Geology, v. 38, no. 12, p. 1075-1078, https://doi.org/10.1130/G31345.1.","startPage":"1075","endPage":"1078","numberOfPages":"4","costCenters":[],"links":[{"id":218105,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1130/G31345.1"},{"id":246087,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"38","issue":"12","noUsgsAuthors":false,"publicationDate":"2010-11-12","publicationStatus":"PW","scienceBaseUri":"505bb7a3e4b08c986b3273c3","contributors":{"authors":[{"text":"Evans, William C.","contributorId":104903,"corporation":false,"usgs":true,"family":"Evans","given":"William","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":462253,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bergfeld, D.","contributorId":58053,"corporation":false,"usgs":true,"family":"Bergfeld","given":"D.","email":"","affiliations":[],"preferred":false,"id":462251,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McGeehin, J. P. 0000-0002-5320-6091","orcid":"https://orcid.org/0000-0002-5320-6091","contributorId":48593,"corporation":false,"usgs":true,"family":"McGeehin","given":"J. P.","affiliations":[],"preferred":false,"id":462250,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"King, J.C.","contributorId":85811,"corporation":false,"usgs":true,"family":"King","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":462252,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Heasler, H.","contributorId":7818,"corporation":false,"usgs":true,"family":"Heasler","given":"H.","email":"","affiliations":[],"preferred":false,"id":462249,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70037677,"text":"70037677 - 2010 - Forest responses to increasing aridity and warmth in the southwestern United States","interactions":[],"lastModifiedDate":"2018-01-23T12:30:17","indexId":"70037677","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2982,"text":"PNAS","active":true,"publicationSubtype":{"id":10}},"title":"Forest responses to increasing aridity and warmth in the southwestern United States","docAbstract":"<p>In recent decades, intense droughts, insect outbreaks, and wildfires have led to decreasing tree growth and increasing mortality in many temperate forests. We compared annual tree-ring width data from 1,097 populations in the coterminous United States to climate data and evaluated site-specific tree responses to climate variations throughout the 20th century. For each population, we developed a climate-driven growth equation by using climate records to predict annual ring widths. Forests within the southwestern United States appear particularly sensitive to drought and warmth. We input 21st century climate projections to the equations to predict growth responses. Our results suggest that if temperature and aridity rise as they are projected to, southwestern trees will experience substantially reduced growth during this century. As tree growth declines, mortality rates may increase at many sites. Increases in wildfires and bark-beetle outbreaks in the most recent decade are likely related to extreme drought and high temperatures during this period. Using satellite imagery and aerial survey data, we conservatively calculate that ≈2.7% of southwestern forest and woodland area experienced substantial mortality due to wildfires from 1984 to 2006, and ≈7.6% experienced mortality associated with bark beetles from 1997 to 2008. We estimate that up to ≈18% of southwestern forest area (excluding woodlands) experienced mortality due to bark beetles or wildfire during this period. Expected climatic changes will alter future forest productivity, disturbance regimes, and species ranges throughout the Southwest. Emerging knowledge of these impending transitions informs efforts to adaptively manage southwestern forests. </p>","language":"English","publisher":"National Academy of Sciences of the United States of America","doi":"10.1073/pnas.0914211107","usgsCitation":"Williams, A., Allen, C.D., Millar, C.I., Swetnam, T., Michaelsen, J., Still, C., and Leavitt, S.W., 2010, Forest responses to increasing aridity and warmth in the southwestern United States: PNAS, v. 107, no. 50, p. 21289-21294, https://doi.org/10.1073/pnas.0914211107.","productDescription":"6 p.","startPage":"21289","endPage":"21294","costCenters":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"links":[{"id":475789,"rank":1,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://europepmc.org/articles/pmc3003095","text":"External Repository"},{"id":246075,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"107","issue":"50","noUsgsAuthors":false,"publicationDate":"2010-12-13","publicationStatus":"PW","scienceBaseUri":"505a1336e4b0c8380cd54577","contributors":{"authors":[{"text":"Williams, A.P.","contributorId":70226,"corporation":false,"usgs":true,"family":"Williams","given":"A.P.","email":"","affiliations":[],"preferred":false,"id":462246,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Allen, Craig D. 0000-0002-8777-5989 craig_allen@usgs.gov","orcid":"https://orcid.org/0000-0002-8777-5989","contributorId":2597,"corporation":false,"usgs":true,"family":"Allen","given":"Craig","email":"craig_allen@usgs.gov","middleInitial":"D.","affiliations":[{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true},{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":true,"id":462243,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Millar, C. I.","contributorId":47165,"corporation":false,"usgs":true,"family":"Millar","given":"C.","email":"","middleInitial":"I.","affiliations":[],"preferred":false,"id":462244,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Swetnam, T.W.","contributorId":95433,"corporation":false,"usgs":true,"family":"Swetnam","given":"T.W.","email":"","affiliations":[],"preferred":false,"id":462248,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Michaelsen, J.","contributorId":12288,"corporation":false,"usgs":true,"family":"Michaelsen","given":"J.","affiliations":[],"preferred":false,"id":462242,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Still, C.J.","contributorId":61277,"corporation":false,"usgs":true,"family":"Still","given":"C.J.","email":"","affiliations":[],"preferred":false,"id":462245,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Leavitt, Steven W.","contributorId":77312,"corporation":false,"usgs":true,"family":"Leavitt","given":"Steven","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":462247,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70037534,"text":"70037534 - 2010 - Direct and indirect responses of tallgrass prairie butterflies to prescribed burning","interactions":[],"lastModifiedDate":"2012-03-12T17:22:05","indexId":"70037534","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2356,"text":"Journal of Insect Conservation","active":true,"publicationSubtype":{"id":10}},"title":"Direct and indirect responses of tallgrass prairie butterflies to prescribed burning","docAbstract":"Fire is an important tool in the conservation and restoration of tallgrass prairie ecosystems. We investigated how both the vegetation composition and butterfly community of tallgrass prairie remnants changed in relation to the elapsed time (in months) since prescribed fire. Butterfly richness and butterfly abundance were positively correlated with the time since burn. Habitat-specialist butterfly richness recovery time was greater than 70 months post-fire and habitat-specialist butterfly abundance recovery time was approximately 50 months post-fire. Thus, recovery times for butterfly populations after prescribed fires in our study were potentially longer than those previously reported. We used Path Analysis to evaluate the relative contributions of the direct effect of time since fire and the indirect effects of time since fire through changes in vegetation composition on butterfly abundance. Path models highlighted the importance of the indirect effects of fire on habitat features, such as increases in the cover of bare ground. Because fire return intervals on managed prairie remnants are often less than 5 years, information on recovery times for habitat-specialist insect species are of great importance. ?? 2010 Springer Science+Business Media B.V.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Insect Conservation","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1007/s10841-010-9295-1","issn":"1366638X","usgsCitation":"Vogel, J.A., Koford, R.R., and Debinski, D.M., 2010, Direct and indirect responses of tallgrass prairie butterflies to prescribed burning: Journal of Insect Conservation, v. 14, no. 6, p. 663-677, https://doi.org/10.1007/s10841-010-9295-1.","startPage":"663","endPage":"677","numberOfPages":"15","costCenters":[],"links":[{"id":246007,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":218030,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/s10841-010-9295-1"}],"volume":"14","issue":"6","noUsgsAuthors":false,"publicationDate":"2010-05-30","publicationStatus":"PW","scienceBaseUri":"505a01abe4b0c8380cd4fcd4","contributors":{"authors":[{"text":"Vogel, Jennifer A.","contributorId":9463,"corporation":false,"usgs":true,"family":"Vogel","given":"Jennifer","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":461489,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Koford, Rolf R.","contributorId":16347,"corporation":false,"usgs":true,"family":"Koford","given":"Rolf","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":461490,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Debinski, Diane M.","contributorId":25361,"corporation":false,"usgs":true,"family":"Debinski","given":"Diane","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":461491,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70037685,"text":"70037685 - 2010 - Algal blooms and \"Marine snow\": Mechanisms that enhance preservation of organic carbon in ancient fine-grained sediments","interactions":[],"lastModifiedDate":"2017-09-01T10:54:49","indexId":"70037685","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2451,"text":"Journal of Sedimentary Research","onlineIssn":"1938-3681","printIssn":"1527-1404","active":true,"publicationSubtype":{"id":10}},"title":"Algal blooms and \"Marine snow\": Mechanisms that enhance preservation of organic carbon in ancient fine-grained sediments","docAbstract":"<p id=\"p-1\">Combined petrographic and geochemical methods are used to investigate the microfabrics present in thin sections prepared from representative organic carbon-rich mudstones collected from three successions (the Kimmeridge Clay Formation, the Jet Rock Member of the Whitby Mudstone Formation, and the pebble shale and Hue Shale). This study was initiated to determine how organic carbon-rich materials were being delivered to the sediment–water interface, and what happened to them after deposition, prior to deep burial.</p><p id=\"p-2\">Analyses of the fabrics present shows that they exhibit many common attributes. In particular they are all: (1) highly heterogeneous on the scale of a thin section, (2) organized into thin beds (&lt; 10 mm thick) composed mainly of mineral mixtures of fine-grained siliciclastic detritus and carbonate materials, and (3) contain significant concentrations of organic carbon, much of which is organized into laminasets that contain abundant organomineralic aggregates and pellets. In addition, framboidal pyrite (range of sizes from &lt; 20 μm to &lt; 1 μm) and abundant agglutinated foraminifers are present in some units. The individual beds are commonly sharp-based and overlain by thin, silt lags. The tops of many of the beds have been homogenized and some regions of the pelleted laminasets contain small horizontal burrows.</p><p id=\"p-3\">The organomineralic aggregates present in these mudstones are interpreted to be ancient examples of marine snow. This marine snow likely formed in the water column, particularly during phytoplankton blooms, and was then transported rapidly to the seafloor. The existence of the thin beds with homogenized tops and an<span>&nbsp;</span><i>in-situ</i><span>&nbsp;</span>infauna indicates that between blooms there was sufficient oxygen and time for a mixed layer to develop as a result of sediment colonization by diminutive organisms using either aerobic or dysaerobic metabolic pathways. These textures suggest that the constituents of these mudstones were delivered neither as a continuous rain of sediment nor were the bottom waters persistently anoxic. In addition, the presence of thin lags and sharp-based beds suggests that the seafloor was being episodically reworked during deposition. These fabrics indicate that conditions in the water columns and at the seafloors while these rocks were being deposited were very dynamic, and episodic fluxes of high concentrations of organic carbon to the seafloor, during phytoplankton blooms, likely enhanced preservation of organic carbon.</p>","language":"English","publisher":"Society for Sedimentary Geology","doi":"10.2110/jsr.2010.085","issn":"15271404","usgsCitation":"Macquaker, J.H., Keller, M.A., and Davies, S., 2010, Algal blooms and \"Marine snow\": Mechanisms that enhance preservation of organic carbon in ancient fine-grained sediments: Journal of Sedimentary Research, v. 80, no. 11, p. 934-942, https://doi.org/10.2110/jsr.2010.085.","productDescription":"9 p.","startPage":"934","endPage":"942","numberOfPages":"9","ipdsId":"IP-023206","costCenters":[{"id":309,"text":"Geology and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":500620,"rank":10000,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"http://hdl.handle.net/2381/27012","text":"External Repository"},{"id":245914,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":217941,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.2110/jsr.2010.085"}],"volume":"80","issue":"11","noUsgsAuthors":false,"publicationDate":"2010-11-04","publicationStatus":"PW","scienceBaseUri":"5059e95de4b0c8380cd4821b","contributors":{"authors":[{"text":"Macquaker, Joe H.S.","contributorId":143669,"corporation":false,"usgs":false,"family":"Macquaker","given":"Joe","email":"","middleInitial":"H.S.","affiliations":[{"id":15294,"text":"Univ. of Newfoundland","active":true,"usgs":false}],"preferred":false,"id":462283,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Keller, Margaret A. mkeller@usgs.gov","contributorId":1017,"corporation":false,"usgs":true,"family":"Keller","given":"Margaret","email":"mkeller@usgs.gov","middleInitial":"A.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":462282,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Davies, Sarah J.","contributorId":140794,"corporation":false,"usgs":false,"family":"Davies","given":"Sarah J.","affiliations":[{"id":13568,"text":"Department Geography, Aberystwyth University, Aberystwyth SY21 3DB, UK","active":true,"usgs":false}],"preferred":false,"id":462284,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70037676,"text":"70037676 - 2010 - Unifying quantitative life-history theory and field endocrinology to assess prudent parenthood in a long-lived seabird","interactions":[],"lastModifiedDate":"2020-11-03T15:27:59.920349","indexId":"70037676","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1604,"text":"Evolutionary Ecology Research","active":true,"publicationSubtype":{"id":10}},"title":"Unifying quantitative life-history theory and field endocrinology to assess prudent parenthood in a long-lived seabird","docAbstract":"<p><strong>Question:</strong><span>&nbsp;</span>Can field measurements of stress hormones help us to assess the prudent parent hypothesis in a long-lived seabird?</p><p><strong>Organism:</strong><span>&nbsp;</span>Black-legged kittiwake,<span>&nbsp;</span><i>Rissa tridactyla</i>.</p><p><strong>Location:</strong><span>&nbsp;</span>Duck and Gull Islands, Cook Inlet, Alaska, USA.</p><p><strong>Methods:</strong><span>&nbsp;</span>We examined the statistical relationship between the stress hormone corticosterone and mortality in black-legged kittiwakes. We built a demographic model of the kittiwake life cycle to determine whether the mortality rates associated with persisting in a breeding attempt despite high corticosterone caused the birds to sacrifice more lifetime reproductive output than they gain from one year’s breeding.</p><p><strong>Results:</strong><span>&nbsp;</span>The probability of apparent mortality increased with corticosterone, suggesting some birds incurred increased mortality risk for the sake of breeding. For Duck Island (low reproductive success), it appears birds sacrificed more lifetime reproductive success than a prudent parent would. On Gull Island, it appears most but possibly not all birds were behaving in ways consistent with theory, although definitive statements require larger samples of highly stressed birds.</p>","language":"English","publisher":"Evolutionary Ecology Ltd.","usgsCitation":"Satterthwaite, W., Kitaysky, A., Hatch, S.A., Piatt, J.F., and Mangel, M., 2010, Unifying quantitative life-history theory and field endocrinology to assess prudent parenthood in a long-lived seabird: Evolutionary Ecology Research, v. 12, no. 6, p. 779-792.","productDescription":"14 p.","startPage":"779","endPage":"792","numberOfPages":"14","costCenters":[{"id":116,"text":"Alaska Science Center Biology MFEB","active":true,"usgs":true}],"links":[{"id":246074,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":380079,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://www.evolutionary-ecology.com/abstracts/v12/2602.html"}],"country":"United States","state":"Alaska","otherGeospatial":"Duck Island, Gull Island","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -152.5554656982422,\n              60.145179450123415\n            ],\n            [\n              -152.54465103149414,\n              60.145179450123415\n            ],\n            [\n              -152.54465103149414,\n              60.15056259396778\n            ],\n            [\n              -152.5554656982422,\n              60.15056259396778\n            ],\n            [\n              -152.5554656982422,\n              60.145179450123415\n            ]\n          ]\n        ]\n      }\n    },\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -148.370361328125,\n              70.36466302872434\n            ],\n            [\n              -148.36280822753906,\n              70.36466302872434\n            ],\n            [\n              -148.36280822753906,\n              70.36627811144407\n            ],\n            [\n              -148.370361328125,\n              70.36627811144407\n            ],\n            [\n              -148.370361328125,\n              70.36466302872434\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"12","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bbc83e4b08c986b328c8d","contributors":{"authors":[{"text":"Satterthwaite, W.H.","contributorId":107839,"corporation":false,"usgs":true,"family":"Satterthwaite","given":"W.H.","email":"","affiliations":[],"preferred":false,"id":462241,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kitaysky, A.S.","contributorId":104239,"corporation":false,"usgs":true,"family":"Kitaysky","given":"A.S.","email":"","affiliations":[],"preferred":false,"id":462240,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hatch, Scott A. 0000-0002-0064-8187 shatch@usgs.gov","orcid":"https://orcid.org/0000-0002-0064-8187","contributorId":2625,"corporation":false,"usgs":true,"family":"Hatch","given":"Scott","email":"shatch@usgs.gov","middleInitial":"A.","affiliations":[{"id":116,"text":"Alaska Science Center Biology MFEB","active":true,"usgs":true}],"preferred":true,"id":462238,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Piatt, John F. 0000-0002-4417-5748 jpiatt@usgs.gov","orcid":"https://orcid.org/0000-0002-4417-5748","contributorId":3025,"corporation":false,"usgs":true,"family":"Piatt","given":"John","email":"jpiatt@usgs.gov","middleInitial":"F.","affiliations":[{"id":116,"text":"Alaska Science Center Biology MFEB","active":true,"usgs":true},{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":117,"text":"Alaska Science Center Biology WTEB","active":true,"usgs":true}],"preferred":true,"id":462239,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Mangel, M.","contributorId":8309,"corporation":false,"usgs":true,"family":"Mangel","given":"M.","email":"","affiliations":[],"preferred":false,"id":462237,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70037478,"text":"70037478 - 2010 - Landscape influences on genetic differentiation among bull trout populations in a stream-lake network","interactions":[],"lastModifiedDate":"2012-03-12T17:22:10","indexId":"70037478","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2774,"text":"Molecular Ecology","active":true,"publicationSubtype":{"id":10}},"title":"Landscape influences on genetic differentiation among bull trout populations in a stream-lake network","docAbstract":"This study examined the influence of landscape heterogeneity on genetic differentiation between migratory bull trout (Salvelinus confluentus) populations in Glacier National Park, Montana. An information-theoretic approach was used to compare different conceptual models of dispersal associated with barriers, different models of isolation by distance, and the combined effects of barriers, waterway distance, patch size, and intra- and inter-drainage distribution of populations on genetic differentiation between bull trout populations. The effect of distance between populations on genetic differentiation was best explained by partitioning the effects of mainstem and tributary stream sections. Models that categorized barriers as having a one-way effect (i.e. allowed downstream dispersal) or a two-way effect were best supported. Additionally, patch size and the distribution of populations among drainages influenced genetic differentiation. Genetic differentiation between bull trout populations in Glacier National Park is linked to landscape features that restrict dispersal. However, this analysis illustrates that modelling variability within landscape features, such as dispersal corridors, will benefit landscape genetic analyses. Additionally, the framework used for evaluating the effects of barriers must consider not just barrier presence, but also potential asymmetries in barrier effects with respect to the organism under investigation.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Molecular Ecology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1111/j.1365-294X.2010.04655.x","issn":"09621083","usgsCitation":"Meeuwig, M., Guy, C., Kalinowski, S., and Fredenberg, W., 2010, Landscape influences on genetic differentiation among bull trout populations in a stream-lake network: Molecular Ecology, v. 19, no. 17, p. 3620-3633, https://doi.org/10.1111/j.1365-294X.2010.04655.x.","startPage":"3620","endPage":"3633","numberOfPages":"14","costCenters":[],"links":[{"id":217097,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1111/j.1365-294X.2010.04655.x"},{"id":245013,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"19","issue":"17","noUsgsAuthors":false,"publicationDate":"2010-08-13","publicationStatus":"PW","scienceBaseUri":"505a4414e4b0c8380cd6682b","contributors":{"authors":[{"text":"Meeuwig, M.H.","contributorId":24741,"corporation":false,"usgs":true,"family":"Meeuwig","given":"M.H.","affiliations":[],"preferred":false,"id":461248,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Guy, C.S.","contributorId":59160,"corporation":false,"usgs":true,"family":"Guy","given":"C.S.","email":"","affiliations":[],"preferred":false,"id":461251,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kalinowski, S.T.","contributorId":26899,"corporation":false,"usgs":true,"family":"Kalinowski","given":"S.T.","affiliations":[],"preferred":false,"id":461249,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Fredenberg, W.A.","contributorId":53196,"corporation":false,"usgs":true,"family":"Fredenberg","given":"W.A.","email":"","affiliations":[],"preferred":false,"id":461250,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70037675,"text":"70037675 - 2010 - Sediment contamination of residential streams in the metropolitan Kansas City area, USA: Part I. distribution of polycyclic aromatic hydrocarbon and pesticide-related compounds","interactions":[],"lastModifiedDate":"2018-10-22T10:21:14","indexId":"70037675","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":887,"text":"Archives of Environmental Contamination and Toxicology","active":true,"publicationSubtype":{"id":10}},"title":"Sediment contamination of residential streams in the metropolitan Kansas City area, USA: Part I. distribution of polycyclic aromatic hydrocarbon and pesticide-related compounds","docAbstract":"<p><span>This is the first part of a study that evaluates the influence of nonpoint-source contaminants on the sediment quality of five streams within the metropolitan Kansas City area, central United States. Surficial sediment was collected in 2003 from 29 sites along five streams with watersheds that extend from the core of the metropolitan area to its development fringe. Sediment was analyzed for 16 polycyclic aromatic hydrocarbons (PAHs), 3 common polychlorinated biphenyl mixtures (Aroclors), and 25 pesticide-related compounds of eight chemical classes. Multiple PAHs were detected at more than 50% of the sites, and concentrations of total PAHs ranged from 290 to 82,150&nbsp;μg/kg (dry weight). The concentration and frequency of detection of PAHs increased with increasing urbanization of the residential watersheds. Four- and five-ring PAH compounds predominated the PAH composition (73–100%), especially fluoranthene and pyrene. The PAH composition profiles along with the diagnostic isomer ratios [e.g., anthracene/(anthracene&nbsp;+&nbsp;phenanthrene), 0.16&nbsp;±&nbsp;0.03; fluoranthene/(fluoranthene&nbsp;+&nbsp;pyrene), 0.55&nbsp;±&nbsp;0.01)] indicate that pyrogenic sources (i.e., coal-tar-related operations or materials and traffic-related particles) may be common PAH contributors to these residential streams. Historical-use organochlorine insecticides and their degradates dominated the occurrences of pesticide-related compounds, with chlordane and dieldrin detected in over or nearly 50% of the samples. The occurrence of these historical organic compounds was associated with past urban applications, which may continue to be nonpoint sources replenishing local streams. Concentrations of low molecular weight (LMW; two or three rings) and high molecular weight (HMW; four to six rings) PAHs covaried along individual streams but showed dissimilar distribution patterns between the streams, while the historical pesticide-related compounds generally increased in concentration downstream. Correlations were noted between LMW and HMW PAHs for most of the streams and between historical-use organochlorine compounds and total organic carbon and clay content of sediments for one of the streams (Brush Creek). Stormwater runoff transport modes are proposed to describe how the two groups of contaminants migrated and distributed in the streambed.</span></p>","language":"English","publisher":"Springer","doi":"10.1007/s00244-010-9497-2","issn":"00904341","usgsCitation":"Tao, J., Huggins, D., Welker, G., Dias, J., Ingersoll, C.G., and Murowchick, J., 2010, Sediment contamination of residential streams in the metropolitan Kansas City area, USA: Part I. distribution of polycyclic aromatic hydrocarbon and pesticide-related compounds: Archives of Environmental Contamination and Toxicology, v. 59, no. 3, p. 352-369, https://doi.org/10.1007/s00244-010-9497-2.","productDescription":"18 p.","startPage":"352","endPage":"369","numberOfPages":"18","costCenters":[{"id":34983,"text":"Contaminant Biology Program","active":true,"usgs":true}],"links":[{"id":218081,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/s00244-010-9497-2"},{"id":246062,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Kansas, Missouri","city":"Kansas City","volume":"59","issue":"3","noUsgsAuthors":false,"publicationDate":"2010-04-14","publicationStatus":"PW","scienceBaseUri":"505b8966e4b08c986b316dc6","contributors":{"authors":[{"text":"Tao, J.","contributorId":56485,"corporation":false,"usgs":true,"family":"Tao","given":"J.","email":"","affiliations":[],"preferred":false,"id":462235,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Huggins, D.","contributorId":29250,"corporation":false,"usgs":true,"family":"Huggins","given":"D.","email":"","affiliations":[],"preferred":false,"id":462232,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Welker, G.","contributorId":21390,"corporation":false,"usgs":true,"family":"Welker","given":"G.","email":"","affiliations":[],"preferred":false,"id":462231,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Dias, J.R.","contributorId":97748,"corporation":false,"usgs":true,"family":"Dias","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":462236,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Ingersoll, Christopher G. 0000-0003-4531-5949 cingersoll@usgs.gov","orcid":"https://orcid.org/0000-0003-4531-5949","contributorId":2071,"corporation":false,"usgs":true,"family":"Ingersoll","given":"Christopher","email":"cingersoll@usgs.gov","middleInitial":"G.","affiliations":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"preferred":true,"id":462234,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Murowchick, J.B.","contributorId":45058,"corporation":false,"usgs":true,"family":"Murowchick","given":"J.B.","email":"","affiliations":[],"preferred":false,"id":462233,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70156846,"text":"70156846 - 2010 - Managing undesired and invading fishes","interactions":[],"lastModifiedDate":"2021-11-09T16:18:44.837849","indexId":"70156846","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Managing undesired and invading fishes","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Inland fisheries management in North America","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"American Fisheries Society","publisherLocation":"Bethesda, Md.","doi":"10.47886/9781934874165.ch8","usgsCitation":"Kolar, C.S., Courtenay, W.R., and Nico, L.G., 2010, Managing undesired and invading fishes, chap. <i>of</i> Inland fisheries management in North America, p. 213-259, https://doi.org/10.47886/9781934874165.ch8.","productDescription":"47 p.","startPage":"213","endPage":"259","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-012119","costCenters":[{"id":566,"text":"Southeast Ecological Science Center","active":true,"usgs":true}],"links":[{"id":307748,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"edition":"3rd","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"560bb6c6e4b058f706e53d4d","contributors":{"editors":[{"text":"Hubert, Wayne A.","contributorId":9325,"corporation":false,"usgs":true,"family":"Hubert","given":"Wayne","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":570823,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Quist, Michael C. mquist@usgs.gov","contributorId":4042,"corporation":false,"usgs":true,"family":"Quist","given":"Michael","email":"mquist@usgs.gov","middleInitial":"C.","affiliations":[{"id":350,"text":"Iowa Cooperative Fish and Wildlife Research Unit","active":false,"usgs":true}],"preferred":false,"id":570824,"contributorType":{"id":2,"text":"Editors"},"rank":2}],"authors":[{"text":"Kolar, Cindy S.","contributorId":82413,"corporation":false,"usgs":true,"family":"Kolar","given":"Cindy","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":570820,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Courtenay, Walter R. Jr.","contributorId":8930,"corporation":false,"usgs":true,"family":"Courtenay","given":"Walter","suffix":"Jr.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":570821,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Nico, Leo G. 0000-0002-4488-7737 lnico@usgs.gov","orcid":"https://orcid.org/0000-0002-4488-7737","contributorId":2913,"corporation":false,"usgs":true,"family":"Nico","given":"Leo","email":"lnico@usgs.gov","middleInitial":"G.","affiliations":[{"id":566,"text":"Southeast Ecological Science Center","active":true,"usgs":true}],"preferred":false,"id":570822,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70037673,"text":"70037673 - 2010 - Long generation time delays the genetic response to habitat fragmentation in the threatened florida sand skink","interactions":[],"lastModifiedDate":"2012-04-30T16:43:34","indexId":"70037673","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Long generation time delays the genetic response to habitat fragmentation in the threatened florida sand skink","docAbstract":"A recent study showed that populations of the threatened Florida Sand Skink had limited loss of genetic diversity over the past 60 yr as a consequence of anthropogenic fragmentation. This study assumed that 60 yr represents 3037 generations for the Florida Sand Skink, but a new evaluation of markrecapture data shows that 60 yr represents only about 15 generations. This result suggests that too little time may have passed to observe the full genetic consequences of contemporary anthropogenic fragmentation in the Florida Sand Skink and reinforces similar results from other species. We suggest that snapshots of existing genetic variability in fragmented populations are limited in their ability to predict the evolutionary fate of a species unless life-history attributes of the organism are taken into account. Copyright 2010 Society for the Study of Amphibians and Reptiles.","largerWorkTitle":"Journal of Herpetology","language":"English","doi":"10.1670/09-089.1","issn":"00221511","usgsCitation":"McCoy, E., Richmond, J., Mushinsky, H., Britt, E., and Godley, J., 2010, Long generation time delays the genetic response to habitat fragmentation in the threatened florida sand skink, <i>in</i> Journal of Herpetology, v. 44, no. 4, p. 641-644, https://doi.org/10.1670/09-089.1.","startPage":"641","endPage":"644","numberOfPages":"4","costCenters":[],"links":[{"id":218068,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1670/09-089.1"},{"id":246048,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"44","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a4962e4b0c8380cd68577","contributors":{"authors":[{"text":"McCoy, E.D.","contributorId":15022,"corporation":false,"usgs":true,"family":"McCoy","given":"E.D.","email":"","affiliations":[],"preferred":false,"id":462215,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Richmond, J.Q.","contributorId":17080,"corporation":false,"usgs":true,"family":"Richmond","given":"J.Q.","email":"","affiliations":[],"preferred":false,"id":462217,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mushinsky, H.R.","contributorId":54416,"corporation":false,"usgs":true,"family":"Mushinsky","given":"H.R.","email":"","affiliations":[],"preferred":false,"id":462219,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Britt, E.J.","contributorId":27728,"corporation":false,"usgs":true,"family":"Britt","given":"E.J.","email":"","affiliations":[],"preferred":false,"id":462218,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Godley, J.S.","contributorId":15731,"corporation":false,"usgs":true,"family":"Godley","given":"J.S.","email":"","affiliations":[],"preferred":false,"id":462216,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70037672,"text":"70037672 - 2010 - Holocene variations in mineral and grain-size composition along the East Greenland glaciated margin (ca 67°–70°N): local versus long-distance sediment transport","interactions":[],"lastModifiedDate":"2015-03-23T11:30:04","indexId":"70037672","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3219,"text":"Quaternary Science Reviews","active":true,"publicationSubtype":{"id":10}},"title":"Holocene variations in mineral and grain-size composition along the East Greenland glaciated margin (ca 67°–70°N): local versus long-distance sediment transport","docAbstract":"Quantitative X-Ray Diffraction (qXRD) analysis of the <2 mm sediment fraction from surface (sea floor) samples, and marine sediment cores that span the last 10-12 cal ka BP, are used to describe spatial and temporal variations in non-clay mineral compositions for an area between Kangerlussuaq Trough and Scoresby Sund (???67??-70??N), East Greenland. Bedrock consists primarily of an early Tertiary alkaline complex with high weight% of pyroxene and plagioclase. Farther inland and to the north, the bedrock is dominantly felsic with a high fraction of quartz and potassium feldspars. Principal Component (PC) analysis of the non-clay sediment compositions indicates the importance of quartz and pyroxene as compositional end members, with an abrupt shift from quartz and k-feldspar dominated sediments north of Scoresby Sund to sediments rich in pyroxene and plagioclase feldspars offshore from the early Tertiary basaltic outcrop. Coarse (<2 mm or <1 mm) ice-rafted sediments are largely absent from the trough sediments between ???8 and 5 cal ka BP, but then increase in the last 4 cal ka BP. Compositional unmixing of the sediments in Grivel Basin and Kangerlussuaq Trough indicate the dominance of local over long distance sediment sources, with pulses of sediment from tidewater glaciers in Kangerlussuaq and Nansen fjords reaching the inner shelf during the Neoglaciation. The change in IRD is more dramatic in the sediment grain-size proxies than in the quartz wt%. Forty to seventy percent of the variance in the quartz records from either side of Denmark Strait is explained by low frequency trends, but the data from the Grivel Basin, East Greenland, are distinctly different, with an approximate 2500 yr periodicity. ?? 2010 Elsevier Ltd.","language":"English","publisher":"Elsevier","doi":"10.1016/j.quascirev.2010.06.001","issn":"02773791","usgsCitation":"Andrews, J.T., Jennings, A.E., Coleman, G.C., and Eberl, D.D., 2010, Holocene variations in mineral and grain-size composition along the East Greenland glaciated margin (ca 67°–70°N): local versus long-distance sediment transport: Quaternary Science Reviews, v. 29, no. 19-20, p. 2619-2632, https://doi.org/10.1016/j.quascirev.2010.06.001.","productDescription":"14 p.","startPage":"2619","endPage":"2632","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":246047,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":218067,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.quascirev.2010.06.001"}],"country":"Greenland","volume":"29","issue":"19-20","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a31f9e4b0c8380cd5e3eb","contributors":{"authors":[{"text":"Andrews, John T.","contributorId":19886,"corporation":false,"usgs":true,"family":"Andrews","given":"John","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":462214,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jennings, Anne E.","contributorId":38876,"corporation":false,"usgs":true,"family":"Jennings","given":"Anne","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":462212,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Coleman, George C.","contributorId":76582,"corporation":false,"usgs":true,"family":"Coleman","given":"George","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":462213,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Eberl, Dennis D.","contributorId":68388,"corporation":false,"usgs":true,"family":"Eberl","given":"Dennis","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":462211,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70037670,"text":"70037670 - 2010 - Transmission and reassortment of avian influenza viruses at the Asian-North American interface","interactions":[],"lastModifiedDate":"2019-12-10T10:30:27","indexId":"70037670","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3696,"text":"Virology","active":true,"publicationSubtype":{"id":10}},"title":"Transmission and reassortment of avian influenza viruses at the Asian-North American interface","docAbstract":"<p>Twenty avian influenza viruses were isolated from seven wild migratory bird species sampled at St. Lawrence Island, Alaska. We tested predictions based on previous phylogenetic analyses of avian influenza viruses that support spatially dependent trans-hemispheric gene flow and frequent interspecies transmission at a location situated at the Asian&ndash;North American interface. Through the application of phylogenetic and genotypic approaches, our data support functional dilution by distance of trans-hemispheric reassortants and interspecific virus transmission. Our study confirms infection of divergent avian taxa with nearly identical avian influenza strains in the wild. Findings also suggest that H16N3 viruses may contain gene segments with unique phylogenetic positions and that further investigation of how host specificity may impact transmission of H13 and H16 viruses is warranted.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.virol.2010.07.031","issn":"00426822","usgsCitation":"Ramey, A.M., Pearce, J.M., Ely, C.R., Guy, L.M., Irons, D.B., Derksen, D.V., and Ip, S., 2010, Transmission and reassortment of avian influenza viruses at the Asian-North American interface: Virology, v. 406, no. 2, p. 352-359, https://doi.org/10.1016/j.virol.2010.07.031.","productDescription":"8 p.","startPage":"352","endPage":"359","numberOfPages":"8","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"links":[{"id":475871,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1016/j.virol.2010.07.031","text":"Publisher Index Page"},{"id":246033,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":218053,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.virol.2010.07.031"}],"country":"United States","state":"Alaska","otherGeospatial":"St Lawrence Island","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -171.7822265625,\n              63.704722429433225\n            ],\n            [\n              -171.38671874999997,\n              63.213829705155625\n            ],\n            [\n              -169.013671875,\n              62.75472592723178\n            ],\n            [\n              -168.22265625,\n              63.27318217465046\n            ],\n            [\n              -170.595703125,\n              63.78248603116502\n            ],\n            [\n              -171.7822265625,\n              63.704722429433225\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"406","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb725e4b08c986b3270a8","contributors":{"authors":[{"text":"Ramey, Andrew M. 0000-0002-3601-8400 aramey@usgs.gov","orcid":"https://orcid.org/0000-0002-3601-8400","contributorId":1872,"corporation":false,"usgs":true,"family":"Ramey","given":"Andrew","email":"aramey@usgs.gov","middleInitial":"M.","affiliations":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":117,"text":"Alaska Science Center Biology WTEB","active":true,"usgs":true}],"preferred":true,"id":462206,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pearce, John M. 0000-0002-8503-5485 jpearce@usgs.gov","orcid":"https://orcid.org/0000-0002-8503-5485","contributorId":181766,"corporation":false,"usgs":true,"family":"Pearce","given":"John","email":"jpearce@usgs.gov","middleInitial":"M.","affiliations":[{"id":117,"text":"Alaska Science Center Biology WTEB","active":true,"usgs":true},{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"preferred":true,"id":462202,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ely, Craig R. 0000-0003-4262-0892 cely@usgs.gov","orcid":"https://orcid.org/0000-0003-4262-0892","contributorId":3214,"corporation":false,"usgs":true,"family":"Ely","given":"Craig","email":"cely@usgs.gov","middleInitial":"R.","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true},{"id":117,"text":"Alaska Science Center Biology WTEB","active":true,"usgs":true}],"preferred":true,"id":462204,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Guy, Lisa M. Sheffield","contributorId":14234,"corporation":false,"usgs":true,"family":"Guy","given":"Lisa","email":"","middleInitial":"M. Sheffield","affiliations":[],"preferred":false,"id":462205,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Irons, David B.","contributorId":63658,"corporation":false,"usgs":true,"family":"Irons","given":"David","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":462207,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Derksen, Dirk V. dderksen@usgs.gov","contributorId":2269,"corporation":false,"usgs":true,"family":"Derksen","given":"Dirk","email":"dderksen@usgs.gov","middleInitial":"V.","affiliations":[{"id":117,"text":"Alaska Science Center Biology WTEB","active":true,"usgs":true}],"preferred":true,"id":462203,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Ip, S. 0000-0003-4844-7533 hip@usgs.gov","orcid":"https://orcid.org/0000-0003-4844-7533","contributorId":727,"corporation":false,"usgs":true,"family":"Ip","given":"S.","email":"hip@usgs.gov","affiliations":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"preferred":true,"id":462201,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70037357,"text":"70037357 - 2010 - Transformation of chiral polychlorinated biphenyls (PCBs) in a stream food web","interactions":[],"lastModifiedDate":"2012-03-12T17:22:07","indexId":"70037357","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1565,"text":"Environmental Science & Technology","onlineIssn":"1520-5851","printIssn":"0013-936X","active":true,"publicationSubtype":{"id":10}},"title":"Transformation of chiral polychlorinated biphenyls (PCBs) in a stream food web","docAbstract":"The enantiomeric composition of chiral PCB congeners was determined in Twelvemile Creek (Clemson, SC) to examine potential mechanisms of biotransformation in a stream food web. We measured enantiomeric fractions (EFs) of six PCB atropisomers (PCBs 84, 91, 95, 136, 149, and 174) in surface sediment, fine benthic organic matter (FBOM), coarse particulate organic matter (CPOM), periphyton, Asian clam, mayflies, yellowfin shiner, and semipermeable membrane devices (SPMDs) using gas chromatography (GC-ECD). Nonracemic EFs of PCBs 91, 95, 136, and 149 were measured in almost all samples. Enantiomeric compositions of PCBs 84 and 174 were infrequently detected with racemic EFs measured in samples except for a nonracemic EF of PCB 84 in clams. Nonracemic EFs of PCBs 91, 136, and 149 in SPMDs may be due to desorption of nonracemic residues from FBOM. EFs for some atropisomers were significantly different among FBOM, CPOM, and periphyton, suggesting that their microbial communities have different biotransformation processes. Nonracemic EFs in clams and fish suggest both in vivo biotransformation and uptake of nonracemic residues from their food sources. Longitudinal variability in EFs was generally low among congeners observed in matrices. ?? 2010 American Chemical Society.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Environmental Science and Technology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1021/es902227a","issn":"0013936X","usgsCitation":"Dang, V., Walters, D., and Lee, C., 2010, Transformation of chiral polychlorinated biphenyls (PCBs) in a stream food web: Environmental Science & Technology, v. 44, no. 8, p. 2836-2841, https://doi.org/10.1021/es902227a.","startPage":"2836","endPage":"2841","numberOfPages":"6","costCenters":[],"links":[{"id":217409,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1021/es902227a"},{"id":245355,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"44","issue":"8","noUsgsAuthors":false,"publicationDate":"2010-01-08","publicationStatus":"PW","scienceBaseUri":"505bb6d2e4b08c986b326ecf","contributors":{"authors":[{"text":"Dang, V.D.","contributorId":33558,"corporation":false,"usgs":true,"family":"Dang","given":"V.D.","email":"","affiliations":[],"preferred":false,"id":460633,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Walters, D.M.","contributorId":41507,"corporation":false,"usgs":true,"family":"Walters","given":"D.M.","email":"","affiliations":[],"preferred":false,"id":460635,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lee, C.M.","contributorId":40031,"corporation":false,"usgs":true,"family":"Lee","given":"C.M.","email":"","affiliations":[],"preferred":false,"id":460634,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70037668,"text":"70037668 - 2010 - Comparison of thiaminase activity in fish using the radiometric and 4-nitrothiophenol colorimetric methods","interactions":[],"lastModifiedDate":"2022-07-29T19:19:02.5516","indexId":"70037668","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2330,"text":"Journal of Great Lakes Research","active":true,"publicationSubtype":{"id":10}},"title":"Comparison of thiaminase activity in fish using the radiometric and 4-nitrothiophenol colorimetric methods","docAbstract":"<h1>Notice</h1><p><strong>This publication has been retracted. See the <a data-mce-href=\"https://doi.org/10.1016/j.jglr.2022.05.005\" href=\"https://doi.org/10.1016/j.jglr.2022.05.005\">retraction notice</a>.</strong></p>","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Great Lakes Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.jglr.2010.07.005","issn":"03801330","usgsCitation":"Honeyfield, D., Hanes, J., Brown, L., Kraft, C., and Begley, T., 2010, Comparison of thiaminase activity in fish using the radiometric and 4-nitrothiophenol colorimetric methods: Journal of Great Lakes Research, v. 36, no. 4, p. 641-645, https://doi.org/10.1016/j.jglr.2010.07.005.","productDescription":"5 p.","startPage":"641","endPage":"645","numberOfPages":"5","costCenters":[],"links":[{"id":475884,"rank":1,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://www.ncbi.nlm.nih.gov/pmc/articles/6042866","text":"Publisher Index Page"},{"id":246017,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"36","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f8b1e4b0c8380cd4d22b","contributors":{"authors":[{"text":"Honeyfield, D. C. 0000-0003-3034-2047","orcid":"https://orcid.org/0000-0003-3034-2047","contributorId":73136,"corporation":false,"usgs":true,"family":"Honeyfield","given":"D. C.","affiliations":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"preferred":false,"id":462197,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hanes, J.W.","contributorId":62867,"corporation":false,"usgs":true,"family":"Hanes","given":"J.W.","email":"","affiliations":[],"preferred":false,"id":462196,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brown, L. 0000-0001-6702-4531","orcid":"https://orcid.org/0000-0001-6702-4531","contributorId":56995,"corporation":false,"usgs":true,"family":"Brown","given":"L.","affiliations":[],"preferred":false,"id":462195,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Kraft, C.E.","contributorId":80610,"corporation":false,"usgs":true,"family":"Kraft","given":"C.E.","email":"","affiliations":[],"preferred":false,"id":462198,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Begley, T.P.","contributorId":17078,"corporation":false,"usgs":true,"family":"Begley","given":"T.P.","email":"","affiliations":[],"preferred":false,"id":462194,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70037666,"text":"70037666 - 2010 - Solute and heat transport model of the Henry and Hilleke laboratory experiment","interactions":[],"lastModifiedDate":"2012-04-30T16:43:35","indexId":"70037666","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1861,"text":"Ground Water","active":true,"publicationSubtype":{"id":10}},"title":"Solute and heat transport model of the Henry and Hilleke laboratory experiment","docAbstract":"SEAWAT is a coupled version of MODFLOW and MT3DMS designed to simulate variable-density ground water flow and solute transport. The most recent version of SEAWAT, called SEAWAT Version 4, includes new capabilities to represent simultaneous multispecies solute and heat transport. To test the new features in SEAWAT, the laboratory experiment of Henry and Hilleke (1972) was simulated. Henry and Hilleke used warm fresh water to recharge a large sand-filled glass tank. A cold salt water boundary was represented on one side. Adjustable heating pads were used to heat the bottom and left sides of the tank. In the laboratory experiment, Henry and Hilleke observed both salt water and fresh water flow systems separated by a narrow transition zone. After minor tuning of several input parameters with a parameter estimation program, results from the SEAWAT simulation show good agreement with the experiment. SEAWAT results suggest that heat loss to the room was more than expected by Henry and Hilleke, and that multiple thermal convection cells are the likely cause of the widened transition zone near the hot end of the tank. Other computer programs with similar capabilities may benefit from benchmark testing with the Henry and Hilleke laboratory experiment. Journal Compilation ?? 2009 National Ground Water Association.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Ground Water","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1111/j.1745-6584.2009.00596.x","issn":"0017467X","usgsCitation":"Langevin, C., Dausman, A., and Sukop, M., 2010, Solute and heat transport model of the Henry and Hilleke laboratory experiment: Ground Water, v. 48, no. 5, p. 757-770, https://doi.org/10.1111/j.1745-6584.2009.00596.x.","startPage":"757","endPage":"770","numberOfPages":"14","costCenters":[],"links":[{"id":246002,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":218025,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1111/j.1745-6584.2009.00596.x"}],"volume":"48","issue":"5","noUsgsAuthors":false,"publicationDate":"2010-08-19","publicationStatus":"PW","scienceBaseUri":"505b924ee4b08c986b319e1f","contributors":{"authors":[{"text":"Langevin, C.D.","contributorId":25976,"corporation":false,"usgs":true,"family":"Langevin","given":"C.D.","email":"","affiliations":[],"preferred":false,"id":462185,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dausman, A.M.","contributorId":99373,"corporation":false,"usgs":true,"family":"Dausman","given":"A.M.","affiliations":[],"preferred":false,"id":462187,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sukop, M.C.","contributorId":88468,"corporation":false,"usgs":true,"family":"Sukop","given":"M.C.","affiliations":[],"preferred":false,"id":462186,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
]}