{"pageNumber":"1955","pageRowStart":"48850","pageSize":"25","recordCount":184617,"records":[{"id":70037180,"text":"70037180 - 2010 - Influence of coal-tar sealcoat and other carbonaceous materials on polycyclic aromatic hydrocarbon loading in an urban watershed","interactions":[],"lastModifiedDate":"2012-03-12T17:22:11","indexId":"70037180","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":"Influence of coal-tar sealcoat and other carbonaceous materials on polycyclic aromatic hydrocarbon loading in an urban watershed","docAbstract":"Carbonaceous material (CM) particles are the principal vectors transporting polycyclic aromatic hydrocarbons (PAHs) into urban waters via runoff; however, characteristics of CM particles in urban watersheds and their relative contributions to PAH contamination remain unclear. Our objectives were to identify the sources and distribution of CM particles in an urban watershed and to determine the types of CMs that were the dominant sources of PAHs in the lake and stream sediments. Samples of soils, parking lot and street dust, and streambed and lake sediment were collected from the Lake Como watershed in Fort Worth, Texas. Characteristics of CM particles determined by organic petrography and a significant correlation between PAH concentrations and organic carbon in coal tar, asphalt, and soot indicate that these three CM particle types are the major sources and carriers of PAHs in the watershed. Estimates of the distribution of PAHs in CM particles indicate that coal-tar pitch, usedinsomepavementsealcoats, isadominant source of PAHs in the watershed, and contributes as much as 99% of the PAHs in sealed parking lot dust, 92% in unsealed parking lot dust, 88% in commercial area soil, 71% in streambed sediment, and 84% in surficial lake sediment. ?? 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/es902657h","issn":"0013936X","usgsCitation":"Yang, Y., Van Metre, P., Mahler, B., Wilson, J., Ligouis, B., Razzaque, M., Schaeffer, D., and Werth, C., 2010, Influence of coal-tar sealcoat and other carbonaceous materials on polycyclic aromatic hydrocarbon loading in an urban watershed: Environmental Science & Technology, v. 44, no. 4, p. 1217-1223, https://doi.org/10.1021/es902657h.","startPage":"1217","endPage":"1223","numberOfPages":"7","costCenters":[],"links":[{"id":217140,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1021/es902657h"},{"id":245059,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"44","issue":"4","noUsgsAuthors":false,"publicationDate":"2010-01-27","publicationStatus":"PW","scienceBaseUri":"505a3b1ae4b0c8380cd62223","contributors":{"authors":[{"text":"Yang, Y.","contributorId":105563,"corporation":false,"usgs":true,"family":"Yang","given":"Y.","email":"","affiliations":[],"preferred":false,"id":459779,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Van Metre, P. C.","contributorId":92999,"corporation":false,"usgs":true,"family":"Van Metre","given":"P. C.","affiliations":[],"preferred":false,"id":459777,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mahler, B.J.","contributorId":36888,"corporation":false,"usgs":true,"family":"Mahler","given":"B.J.","email":"","affiliations":[],"preferred":false,"id":459773,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Wilson, J.T.","contributorId":97489,"corporation":false,"usgs":true,"family":"Wilson","given":"J.T.","affiliations":[],"preferred":false,"id":459778,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Ligouis, B.","contributorId":59228,"corporation":false,"usgs":true,"family":"Ligouis","given":"B.","email":"","affiliations":[],"preferred":false,"id":459774,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Razzaque, M.","contributorId":74986,"corporation":false,"usgs":true,"family":"Razzaque","given":"M.","email":"","affiliations":[],"preferred":false,"id":459776,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Schaeffer, D.J.","contributorId":65038,"corporation":false,"usgs":true,"family":"Schaeffer","given":"D.J.","email":"","affiliations":[],"preferred":false,"id":459775,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Werth, C.J.","contributorId":26481,"corporation":false,"usgs":true,"family":"Werth","given":"C.J.","affiliations":[],"preferred":false,"id":459772,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":70037053,"text":"70037053 - 2010 - Common snapping turtle preys on an adult western grebe","interactions":[],"lastModifiedDate":"2017-12-27T11:42:09","indexId":"70037053","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3731,"text":"Waterbirds","onlineIssn":"19385390","printIssn":"15244695","active":true,"publicationSubtype":{"id":10}},"title":"Common snapping turtle preys on an adult western grebe","docAbstract":"The identification of predators of aquatic birds can be difficult. The Common Snapping Turtle (Chelydra serpentine) is considered a major predator of waterfowl and other aquatic birds, but the evidence for this reputation is based largely on circumstantial or indirect evidence rather than direct observations. Herein, the first documented observations of a snapping turtle attacking and killing an adult Western Grebe (Aechmophorus occidentalis) are described.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Waterbirds","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1675/063.033.0113","issn":"15244695","usgsCitation":"Igl, L., and Peterson, S., 2010, Common snapping turtle preys on an adult western grebe: Waterbirds, v. 33, p. 105-109, https://doi.org/10.1675/063.033.0113.","productDescription":"5 p.","startPage":"105","endPage":"109","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":245019,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":217102,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1675/063.033.0113"}],"volume":"33","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f801e4b0c8380cd4ce1a","contributors":{"authors":[{"text":"Igl, L.D. 0000-0003-0530-7266","orcid":"https://orcid.org/0000-0003-0530-7266","contributorId":13568,"corporation":false,"usgs":true,"family":"Igl","given":"L.D.","affiliations":[],"preferred":false,"id":459162,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Peterson, S.L.","contributorId":88981,"corporation":false,"usgs":true,"family":"Peterson","given":"S.L.","email":"","affiliations":[],"preferred":false,"id":459163,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70037326,"text":"70037326 - 2010 - Poroelastic stress-triggering of the 2005 M8.7 Nias earthquake by the 2004 M9.2 Sumatra-Andaman earthquake","interactions":[],"lastModifiedDate":"2020-05-04T15:50:57.831693","indexId":"70037326","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":"Poroelastic stress-triggering of the 2005 M8.7 Nias earthquake by the 2004 M9.2 Sumatra-Andaman earthquake","docAbstract":"<p>The M9.2 Sumatra-Andaman earthquake (SAE) occurred three months prior to the M8.7 Nias earthquake (NE). We propose that the NE was mechanically triggered by the SAE, and that poroelastic effects were a major component of this triggering. This study uses 3D finite element models (FEMs) of the Sumatra-Andaman subduction zone (SASZ) to predict the deformation, stress, and pore pressure fields of the SAE. The coseismic slip distribution for the SAE is calibrated to near-field GPS data using FEM-generated Green's Functions and linear inverse methods. The calibrated FEM is then used to predict the postseismic poroelastic contribution to stress-triggering along the rupture surface of the NE, which is adjacent to the southern margin of the SAE. The coseismic deformation of the SAE, combined with the rheologic configuration of the SASZ produces two transient fluid flow regimes having separate time constants. SAE coseismic pore pressures in the relatively shallow forearc and volcanic arc regions (within a few km depth) dissipate within one month after the SAE. However, pore pressures in the oceanic crust of the down-going slab persist several months after the SAE. Predictions suggest that the SAE initially induced MPa-scale negative pore pressure near the hypocenter of the NE. This pore pressure slowly recovered (increased) during the three-month interval separating the SAE and NE due to lateral migration of pore fluids, driven by coseismic pressure gradients, within the subducting oceanic crust. Because pore pressure is a fundamental component of Coulomb stress, the MPa-scale increase in pore pressure significantly decreased stability of the NE fault during the three-month interval after the SAE and prior to rupture of the NE. A complete analysis of stress-triggering due to the SAE must include a poroelastic component. Failure to include poroelastic mechanics will lead to an incomplete model that cannot account for the time interval between the SAE and NE. Our transient poroelastic model explains both the spatial and temporal characteristics of triggering of the NE by the SAE.&nbsp;</p>","largerWorkTitle":"","language":"English","publisher":"Elsevier","doi":"10.1016/j.epsl.2010.02.043","issn":"","usgsCitation":"Hughes, K., Masterlark, T., and Mooney, W.D., 2010, Poroelastic stress-triggering of the 2005 M8.7 Nias earthquake by the 2004 M9.2 Sumatra-Andaman earthquake: Earth and Planetary Science Letters, v. 293, no. 3-4, p. 289-299, https://doi.org/10.1016/j.epsl.2010.02.043.","productDescription":"11 p.","startPage":"289","endPage":"299","numberOfPages":"11","costCenters":[],"links":[{"id":244910,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Indian Ocean","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              24.2578125,\n              -39.6395375643667\n            ],\n            [\n              120.9375,\n              -39.6395375643667\n            ],\n            [\n              120.9375,\n              27.059125784374068\n            ],\n            [\n              24.2578125,\n              27.059125784374068\n            ],\n            [\n              24.2578125,\n              -39.6395375643667\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"293","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a7dd6e4b0c8380cd7a1be","contributors":{"authors":[{"text":"Hughes, K.L.H.","contributorId":96919,"corporation":false,"usgs":true,"family":"Hughes","given":"K.L.H.","email":"","affiliations":[],"preferred":false,"id":460484,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Masterlark, Timothy","contributorId":92829,"corporation":false,"usgs":false,"family":"Masterlark","given":"Timothy","email":"","affiliations":[{"id":35607,"text":"South Dakota School of Mines","active":true,"usgs":false}],"preferred":false,"id":460483,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mooney, Walter D. 0000-0002-5310-3631 mooney@usgs.gov","orcid":"https://orcid.org/0000-0002-5310-3631","contributorId":3194,"corporation":false,"usgs":true,"family":"Mooney","given":"Walter","email":"mooney@usgs.gov","middleInitial":"D.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":460482,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"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":70037354,"text":"70037354 - 2010 - Relationships between water temperatures and upstream migration, cold water refuge use, and spawning of adult bull trout from the Lostine River, Oregon, USA","interactions":[],"lastModifiedDate":"2017-11-17T16:02:42","indexId":"70037354","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1471,"text":"Ecology of Freshwater Fish","active":true,"publicationSubtype":{"id":10}},"title":"Relationships between water temperatures and upstream migration, cold water refuge use, and spawning of adult bull trout from the Lostine River, Oregon, USA","docAbstract":"Understanding thermal habitat use by migratory fish has been limited by difficulties in matching fish locations with water temperatures. To describe spatial and temporal patterns of thermal habitat use by migratory adult bull trout, Salvelinus confluentus, that spawn in the Lostine River, Oregon, we employed a combination of archival temperature tags, radio tags, and thermographs. We also compared temperatures of the tagged fish to ambient water temperatures to determine if the fish were using thermal refuges. The timing and temperatures at which fish moved upstream from overwintering areas to spawning locations varied considerably among individuals. The annual maximum 7-day average daily maximum (7DADM) temperatures of tagged fish were 16-18 ??C and potentially as high as 21 ??C. Maximum 7DADM ambient water temperatures within the range of tagged fish during summer were 18-25 ??C. However, there was no evidence of the tagged fish using localized cold water refuges. Tagged fish appeared to spawn at 7DADM temperatures of 7-14 ??C. Maximum 7DADM temperatures of tagged fish and ambient temperatures at the onset of the spawning period in late August were 11-18 ??C. Water temperatures in most of the upper Lostine River used for spawning and rearing appear to be largely natural since there has been little development, whereas downstream reaches used by migratory bull trout are heavily diverted for irrigation. Although the population effects of these temperatures are unknown, summer temperatures and the higher temperatures observed for spawning fish appear to be at or above the upper range of suitability reported for the species. Published 2009. This article is a US Governmentwork and is in the public domain in the USA.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Ecology of Freshwater Fish","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1111/j.1600-0633.2009.00393.x","issn":"09066691","usgsCitation":"Howell, P., Dunham, J., and Sankovich, P., 2010, Relationships between water temperatures and upstream migration, cold water refuge use, and spawning of adult bull trout from the Lostine River, Oregon, USA: Ecology of Freshwater Fish, v. 19, no. 1, p. 96-106, https://doi.org/10.1111/j.1600-0633.2009.00393.x.","startPage":"96","endPage":"106","numberOfPages":"11","costCenters":[{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true}],"links":[{"id":245323,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":217378,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1111/j.1600-0633.2009.00393.x"}],"volume":"19","issue":"1","noUsgsAuthors":false,"publicationDate":"2010-02-19","publicationStatus":"PW","scienceBaseUri":"505aa65ae4b0c8380cd84de9","contributors":{"authors":[{"text":"Howell, P.J.","contributorId":34361,"corporation":false,"usgs":true,"family":"Howell","given":"P.J.","email":"","affiliations":[],"preferred":false,"id":460620,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dunham, J. B. 0000-0002-6268-0633","orcid":"https://orcid.org/0000-0002-6268-0633","contributorId":96637,"corporation":false,"usgs":true,"family":"Dunham","given":"J. B.","affiliations":[],"preferred":false,"id":460622,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sankovich, P.M.","contributorId":64487,"corporation":false,"usgs":true,"family":"Sankovich","given":"P.M.","email":"","affiliations":[],"preferred":false,"id":460621,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70037324,"text":"70037324 - 2010 - Shear-rate-dependent strength control on the dynamics of rainfall-triggered landslides, Tokushima Prefecture, Japan","interactions":[],"lastModifiedDate":"2012-03-12T17:22:11","indexId":"70037324","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1425,"text":"Earth Surface Processes and Landforms","active":true,"publicationSubtype":{"id":10}},"title":"Shear-rate-dependent strength control on the dynamics of rainfall-triggered landslides, Tokushima Prefecture, Japan","docAbstract":"A typhoon (Typhoon No. 10) attacked Shikoku Island and the Tyugoku area of Japan in 2004. This typhoon produced a new daily precipitation record of 1317 mm on Shikoku Island and triggered hundreds of landslides in Tokushima Prefecture. One catastrophic landslide was triggered in the Shiraishi area of Kisawa village, and destroyed more than 10 houses while also leaving an unstable block high on the slope. The unstable block kept moving after the event, showing accelerating and decelerating movement during and after rainfall and reaching a displacement of several meters before countermeasures were put into place. To examine the mechanism for this landsliding characteristic, samples (weathered serpentinite) were taken from the field, and their shear behaviours examined using ring shear tests. The test results revealed that the residual shear strength of the samples is positively dependent on the shear rate, which may provide an explanation for the continuous acceleratingdecelerating process of the landsliding. The roughness of the shear surface and the microstructure of the shear zone were measured and observed by laser microscope and SEM techniques in an attempt to clarify the mechanism of shear rate effect on the residual shear strength. Copyright ?? 2010 John Wiley & Sons, Ltd.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Earth Surface Processes and Landforms","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1002/esp.1937","issn":"01979337","usgsCitation":"Wang, G., Suemine, A., and Schulz, W., 2010, Shear-rate-dependent strength control on the dynamics of rainfall-triggered landslides, Tokushima Prefecture, Japan: Earth Surface Processes and Landforms, v. 35, no. 4, p. 407-416, https://doi.org/10.1002/esp.1937.","startPage":"407","endPage":"416","numberOfPages":"10","costCenters":[],"links":[{"id":475932,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1002/esp.1937","text":"Publisher Index Page"},{"id":245383,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":217435,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1002/esp.1937"}],"volume":"35","issue":"4","noUsgsAuthors":false,"publicationDate":"2010-03-19","publicationStatus":"PW","scienceBaseUri":"505b8e5be4b08c986b3188b6","contributors":{"authors":[{"text":"Wang, G.","contributorId":11034,"corporation":false,"usgs":true,"family":"Wang","given":"G.","email":"","affiliations":[],"preferred":false,"id":460476,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Suemine, A.","contributorId":27722,"corporation":false,"usgs":true,"family":"Suemine","given":"A.","email":"","affiliations":[],"preferred":false,"id":460477,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Schulz, W.H.","contributorId":61225,"corporation":false,"usgs":true,"family":"Schulz","given":"W.H.","email":"","affiliations":[],"preferred":false,"id":460478,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70037353,"text":"70037353 - 2010 - Complete mitochondrial genome of a Pleistocene jawbone unveils the origin of polar bear","interactions":[],"lastModifiedDate":"2018-08-20T18:16:31","indexId":"70037353","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":"Complete mitochondrial genome of a Pleistocene jawbone unveils the origin of polar bear","docAbstract":"The polar bear has become the flagship species in the climate-change discussion. However, little is known about how past climate impacted its evolution and persistence, given an extremely poor fossil record. Although it is undisputed from analyses of mitochondrial (mt) DNA that polar bears constitute a lineage within the genetic diversity of brown bears, timing estimates of their divergence have differed considerably. Using next-generation sequencing technology, we have generated a complete, high-quality mt genome from a stratigraphically validated 130,000- to 110,000-year-old polar bear jawbone. In addition, six mt genomes were generated of extant polar bears from Alaska and brown bears from the Admiralty and Baranof islands of the Alexander Archipelago of southeastern Alaska and Kodiak Island. We show that the phylogenetic position of the ancient polar bear lies almost directly at the branching point between polar bears and brown bears, elucidating a unique morphologically and molecularly documented fossil link between living mammal species. Molecular dating and stable isotope analyses also show that by very early in their evolutionary history, polar bears were already inhabitants of the Artic sea ice and had adapted very rapidly to their current and unique ecology at the top of the Arctic marine food chain. As such, polar bears provide an excellent example of evolutionary opportunism within a widespread mammalian lineage.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"PNAS","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"National Academy of Sciences","publisherLocation":"Baltimore, MD","doi":"10.1073/pnas.0914266107","issn":"00278424","usgsCitation":"Lindqvist, C., Schuster, S.C., Sun, Y., Talbot, S.L., Qi, J., Ratan, A., Tomsho, L.P., Kasson, L., Zeyl, E., Aars, J., Miller, W., Ingolfsson, O., Bachmann, L., and Wiig, Ø., 2010, Complete mitochondrial genome of a Pleistocene jawbone unveils the origin of polar bear: PNAS, v. 107, no. 11, p. 5053-5057, https://doi.org/10.1073/pnas.0914266107.","productDescription":"5 p.","startPage":"5053","endPage":"5057","numberOfPages":"5","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":475866,"rank":10000,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://www.ncbi.nlm.nih.gov/pmc/articles/2841953","text":"External Repository"},{"id":217348,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1073/pnas.0914266107"},{"id":245292,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"107","issue":"11","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f90ae4b0c8380cd4d3c1","contributors":{"authors":[{"text":"Lindqvist, Charlotte","contributorId":35989,"corporation":false,"usgs":true,"family":"Lindqvist","given":"Charlotte","affiliations":[],"preferred":false,"id":460612,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schuster, Stephan 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,{"id":70037325,"text":"70037325 - 2010 - Determination of stress parameters for eight well-recorded earthquakes in eastern North America","interactions":[],"lastModifiedDate":"2012-12-19T14:44:57","indexId":"70037325","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":"Determination of stress parameters for eight well-recorded earthquakes in eastern North America","docAbstract":"We determined the stress parameter, <i>Δσ</i>, for the eight earthquakes studied by Atkinson and Boore (2006), using an updated dataset and a revised point-source stochastic model that captures the effect of a finite fault. We consider four geometrical-spreading functions, ranging from 1/<i>R</i> at all distances to two- or three-part functions. The <i>Δσ</i> values are sensitive to the rate of geometrical spreading at close distances, with 1/<i>R</i><sup>1.3</sup> spreading implying much higher <i>Δσ</i> than models with 1/<i>R</i> spreading. The important difference in ground motions of most engineering concern, however, arises not from whether the geometrical spreading is 1/<i>R</i><sup>1.3</sup> or 1/<i>R</i> at close distances, but from whether a region of flat or increasing geometrical spreading at intermediate distances is present, as long as <i>Δσ</i> is constrained by data that are largely at distances of 100 km–800 km. The simple 1/<i>R</i> model fits the sparse data for the eight events as well as do more complex models determined from larger datasets (where the larger datasets were used in our previous ground-motion prediction equations); this suggests that uncertainty in attenuation rates is an important component of epistemic uncertainty in ground-motion modeling. For the attenuation model used by Atkinson and Boore (2006), the average value of <i>Δσ</i> from the point-source model ranges from 180 bars to 250 bars, depending on whether or not the stress parameter from the 1988 Saguenay earthquake is included in the average. We also find that <i>Δσ</i> for a given earthquake is sensitive to its moment magnitude <b>M</b>, with a change of 0.1 magnitude units producing a factor of 1.3 change in the derived <i>Δσ</i>.","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","publisherLocation":"El Cerrito, CA","doi":"10.1785/0120090328","issn":"00371106","usgsCitation":"Boore, D., Campbell, K., and Atkinson, G.M., 2010, Determination of stress parameters for eight well-recorded earthquakes in eastern North America: Bulletin of the Seismological Society of America, v. 100, no. 4, p. 1632-1645, https://doi.org/10.1785/0120090328.","productDescription":"14 p.","startPage":"1632","endPage":"1645","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"links":[{"id":245384,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":217436,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1785/0120090328"}],"otherGeospatial":"North America","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 177.1,5.6 ], [ 177.1,85.4 ], [ -4.0,85.4 ], [ -4.0,5.6 ], [ 177.1,5.6 ] ] ] } } ] }","volume":"100","issue":"4","noUsgsAuthors":false,"publicationDate":"2010-07-27","publicationStatus":"PW","scienceBaseUri":"5059ffcae4b0c8380cd4f3d3","contributors":{"authors":[{"text":"Boore, D.M. 0000-0002-8605-9673","orcid":"https://orcid.org/0000-0002-8605-9673","contributorId":64226,"corporation":false,"usgs":true,"family":"Boore","given":"D.M.","affiliations":[],"preferred":false,"id":460480,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Campbell, K.W.","contributorId":26309,"corporation":false,"usgs":true,"family":"Campbell","given":"K.W.","email":"","affiliations":[],"preferred":false,"id":460479,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Atkinson, G. M.","contributorId":69283,"corporation":false,"usgs":true,"family":"Atkinson","given":"G.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":460481,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70037328,"text":"70037328 - 2010 - Uncertainties in slip-rate estimates for the Mission Creek strand of the southern San Andreas fault at Biskra Palms Oasis, southern California","interactions":[],"lastModifiedDate":"2020-09-24T17:37:40.49972","indexId":"70037328","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5935,"text":"Bulletin of the Geological Society of America","active":true,"publicationSubtype":{"id":10}},"title":"Uncertainties in slip-rate estimates for the Mission Creek strand of the southern San Andreas fault at Biskra Palms Oasis, southern California","docAbstract":"<p><span>This study focuses on uncertainties in estimates of the geologic slip rate along the Mission Creek strand of the southern San Andreas fault where it offsets an alluvial fan (T2) at Biskra Palms Oasis in southern California. We provide new estimates of the amount of fault offset of the T2 fan based on trench excavations and new cosmogenic&nbsp;</span><sup>10</sup><span>Be age determinations from the tops of 12 boulders on the fan surface. We present three alternative fan offset models: a minimum, a maximum, and a preferred offset of 660 m, 980 m, and 770 m, respectively. We assign an age of between 45 and 54 ka to the T2 fan from the&nbsp;</span><sup>10</sup><span>Be data, which is significantly older than previously reported but is consistent with both the degree of soil development associated with this surface, and with ages from U-series geochronology on pedogenic carbonate from T2, described in a companion paper by Fletcher et al. (this volume). These new constraints suggest a range of slip rates between ∼12 and 22 mm/yr with a preferred estimate of ∼14–17 mm/yr for the Mission Creek strand of the southern San Andreas fault. Previous studies suggested that the geologic and geodetic slip-rate estimates at Biskra Palms differed. We find, however, that considerable uncertainty affects both the geologic and geodetic slip-rate estimates, such that if a real discrepancy between these rates exists for the southern San Andreas fault at Biskra Palms, it cannot be demonstrated with available data.</span></p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/B30020.1","usgsCitation":"Behr, W.M., Rood, D.H., Fletcher, K.E., Guzman, N., Finkel, R., Hanks, T.C., Hudnut, K.W., Kendrick, K.J., Platt, J.P., Sharp, W.D., Weldon, R.J., and Yule, J.D., 2010, Uncertainties in slip-rate estimates for the Mission Creek strand of the southern San Andreas fault at Biskra Palms Oasis, southern California: Bulletin of the Geological Society of America, v. 122, no. 9-10, p. 1360-1377, https://doi.org/10.1130/B30020.1.","productDescription":"18 p.","startPage":"1360","endPage":"1377","numberOfPages":"18","costCenters":[],"links":[{"id":244941,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Biskra Palms Oasis","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -116.36306762695312,\n              33.76088200086917\n            ],\n            [\n              -116.15432739257811,\n              33.76088200086917\n            ],\n            [\n              -116.15432739257811,\n              33.84646707394075\n            ],\n            [\n              -116.36306762695312,\n              33.84646707394075\n            ],\n            [\n              -116.36306762695312,\n              33.76088200086917\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"122","issue":"9-10","noUsgsAuthors":false,"publicationDate":"2010-05-10","publicationStatus":"PW","scienceBaseUri":"505bbc15e4b08c986b328a10","contributors":{"authors":[{"text":"Behr, W. M.","contributorId":115625,"corporation":false,"usgs":true,"family":"Behr","given":"W.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":514044,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rood, D. H.","contributorId":117382,"corporation":false,"usgs":true,"family":"Rood","given":"D.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":514046,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fletcher, K. E.","contributorId":119067,"corporation":false,"usgs":true,"family":"Fletcher","given":"K.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":514048,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Guzman, N.","contributorId":77389,"corporation":false,"usgs":true,"family":"Guzman","given":"N.","email":"","affiliations":[],"preferred":false,"id":514042,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Finkel, R.","contributorId":103028,"corporation":false,"usgs":true,"family":"Finkel","given":"R.","email":"","affiliations":[],"preferred":false,"id":514043,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Hanks, T. C.","contributorId":119344,"corporation":false,"usgs":true,"family":"Hanks","given":"T.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":514050,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Hudnut, K. W.","contributorId":121269,"corporation":false,"usgs":true,"family":"Hudnut","given":"K.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":514052,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Kendrick, K. J.","contributorId":115663,"corporation":false,"usgs":true,"family":"Kendrick","given":"K.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":514045,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Platt, J. P.","contributorId":121418,"corporation":false,"usgs":true,"family":"Platt","given":"J.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":514053,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Sharp, W. D.","contributorId":119197,"corporation":false,"usgs":true,"family":"Sharp","given":"W.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":514049,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Weldon, R. J.","contributorId":120909,"corporation":false,"usgs":true,"family":"Weldon","given":"R.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":514051,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Yule, J. D.","contributorId":118164,"corporation":false,"usgs":true,"family":"Yule","given":"J.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":514047,"contributorType":{"id":1,"text":"Authors"},"rank":12}]}}
,{"id":70037411,"text":"70037411 - 2010 - Validation of a real-time reverse transcriptase-PCR assay for the detection of H7 avian influenza virus","interactions":[],"lastModifiedDate":"2013-04-30T09:36:19","indexId":"70037411","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":948,"text":"Avian Diseases","active":true,"publicationSubtype":{"id":10}},"title":"Validation of a real-time reverse transcriptase-PCR assay for the detection of H7 avian influenza virus","docAbstract":"This report describes the validation of an avian influenza virus (AIV) H7 subtype-specific real-time reverse transcriptasePCR (rRT-PCR) assay developed at the Southeast Poultry Research Laboratory (SEPRL) for the detection of H7 AI in North and South American wild aquatic birds and poultry. The validation was a collaborative effort by the SEPRL and the National Veterinary Services Laboratories. The 2008 H7 rRT-PCR assay detects 10<sup>1</sup> 50% embryo infectious doses per reaction, or 10<sup>3</sup>10<sup>4</sup> copies of transcribed H7 RNA. Diagnostic sensitivity and specificity were estimated to be 97.5% and 82.4%, respectively; the assay was shown to be specific for H7 AI when tested with &gt;270 wild birds and poultry viruses. Following validation, the 2008 H7 rRT-PCR procedure was adopted as an official U.S. Department of Agriculture procedure for the detection of H7 AIV. The 2008 H7 assay replaced the previously used (2002) assay, which does not detect H7 viruses currently circulating in wild birds in North and South America. ?? 2010 American Association of Avian Pathologists.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Avian Diseases","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"American Association of Avian Pathologists","doi":"10.1637/8911-043009-Reg.1","issn":"00052086","usgsCitation":"Pedersen, J., Killian, M., Hines, N., Senne, D., Panigrahy, B., Ip, H., and Spackman, E., 2010, Validation of a real-time reverse transcriptase-PCR assay for the detection of H7 avian influenza virus: Avian Diseases, v. 54, no. S1, p. 639-643, https://doi.org/10.1637/8911-043009-Reg.1.","productDescription":"5 p.","startPage":"639","endPage":"643","costCenters":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"links":[{"id":245106,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":217184,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1637/8911-043009-Reg.1"}],"volume":"54","issue":"S1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bc0fde4b08c986b32a3ef","contributors":{"authors":[{"text":"Pedersen, J.","contributorId":61269,"corporation":false,"usgs":true,"family":"Pedersen","given":"J.","affiliations":[],"preferred":false,"id":460931,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Killian, M.L.","contributorId":45116,"corporation":false,"usgs":true,"family":"Killian","given":"M.L.","email":"","affiliations":[],"preferred":false,"id":460930,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hines, N.","contributorId":84598,"corporation":false,"usgs":true,"family":"Hines","given":"N.","email":"","affiliations":[],"preferred":false,"id":460934,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Senne, D.","contributorId":61270,"corporation":false,"usgs":true,"family":"Senne","given":"D.","affiliations":[],"preferred":false,"id":460932,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Panigrahy, B.","contributorId":104739,"corporation":false,"usgs":true,"family":"Panigrahy","given":"B.","email":"","affiliations":[],"preferred":false,"id":460935,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Ip, Hon S. 0000-0003-4844-7533","orcid":"https://orcid.org/0000-0003-4844-7533","contributorId":15829,"corporation":false,"usgs":true,"family":"Ip","given":"Hon S.","affiliations":[],"preferred":false,"id":460929,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Spackman, Erica","contributorId":82126,"corporation":false,"usgs":false,"family":"Spackman","given":"Erica","affiliations":[{"id":6622,"text":"US Department of Agriculture","active":true,"usgs":false}],"preferred":false,"id":460933,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70037352,"text":"70037352 - 2010 - Organic intermediates in the anaerobic biodegradation of coal to methane under laboratory conditions","interactions":[],"lastModifiedDate":"2018-10-31T10:46:00","indexId":"70037352","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2958,"text":"Organic Geochemistry","active":true,"publicationSubtype":{"id":10}},"title":"Organic intermediates in the anaerobic biodegradation of coal to methane under laboratory conditions","docAbstract":"<p><span>Organic intermediates in coal fluids produced by anaerobic biodegradation of geopolymers in coal play a key role in the production of methane in natural gas reservoirs. Laboratory biodegradation experiments on sub-bituminous coal from Texas, USA, were conducted using bioreactors to examine the organic intermediates relevant to methane production. Production of methane in the bioreactors was linked to acetate accumulation in bioreactor fluid. Long chain fatty acids, alkanes (C</span><sub>19</sub><span>–C</span><sub>36</sub><span>) and various low molecular weight aromatics, including phenols, also accumulated in the bioreactor fluid and appear to be the primary intermediates in the biodegradation pathway from coal-derived geopolymers to acetate and methane.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.orggeochem.2010.03.005","usgsCitation":"Orem, W.H., Voytek, M.A., Jones, E., Lerch, H.E., Bates, A.L., Corum, M., Warwick, P.D., and Clark, A.C., 2010, Organic intermediates in the anaerobic biodegradation of coal to methane under laboratory conditions: Organic Geochemistry, v. 41, no. 9, p. 997-1000, https://doi.org/10.1016/j.orggeochem.2010.03.005.","productDescription":"4 p.","startPage":"997","endPage":"1000","costCenters":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":245291,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Texas","volume":"41","issue":"9","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a6fc3e4b0c8380cd75c5c","contributors":{"authors":[{"text":"Orem, William H. 0000-0003-4990-0539 borem@usgs.gov","orcid":"https://orcid.org/0000-0003-4990-0539","contributorId":577,"corporation":false,"usgs":true,"family":"Orem","given":"William","email":"borem@usgs.gov","middleInitial":"H.","affiliations":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":460603,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Voytek, Mary A.","contributorId":91943,"corporation":false,"usgs":true,"family":"Voytek","given":"Mary","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":460601,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Jones, Elizabeth J.","contributorId":96791,"corporation":false,"usgs":true,"family":"Jones","given":"Elizabeth J.","affiliations":[],"preferred":false,"id":460604,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lerch, Harry E. tlerch@usgs.gov","contributorId":600,"corporation":false,"usgs":true,"family":"Lerch","given":"Harry","email":"tlerch@usgs.gov","middleInitial":"E.","affiliations":[],"preferred":true,"id":460605,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Bates, Anne L. 0000-0002-4875-4675 abates@usgs.gov","orcid":"https://orcid.org/0000-0002-4875-4675","contributorId":2789,"corporation":false,"usgs":true,"family":"Bates","given":"Anne","email":"abates@usgs.gov","middleInitial":"L.","affiliations":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":460600,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Corum, M.D. 0000-0002-9038-3935 mcorum@usgs.gov","orcid":"https://orcid.org/0000-0002-9038-3935","contributorId":2249,"corporation":false,"usgs":true,"family":"Corum","given":"M.D.","email":"mcorum@usgs.gov","affiliations":[{"id":255,"text":"Energy Resources Program","active":true,"usgs":true},{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":460599,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Warwick, Peter D. 0000-0002-3152-7783 pwarwick@usgs.gov","orcid":"https://orcid.org/0000-0002-3152-7783","contributorId":762,"corporation":false,"usgs":true,"family":"Warwick","given":"Peter","email":"pwarwick@usgs.gov","middleInitial":"D.","affiliations":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true}],"preferred":false,"id":460602,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Clark, Arthur C. aclark@usgs.gov","contributorId":2320,"corporation":false,"usgs":true,"family":"Clark","given":"Arthur","email":"aclark@usgs.gov","middleInitial":"C.","affiliations":[],"preferred":true,"id":460598,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":70037315,"text":"70037315 - 2010 - Estimates of density, detection probability, and factors influencing detection of burrowing owls in the Mojave Desert","interactions":[],"lastModifiedDate":"2012-03-12T17:22:07","indexId":"70037315","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2442,"text":"Journal of Raptor Research","active":true,"publicationSubtype":{"id":10}},"title":"Estimates of density, detection probability, and factors influencing detection of burrowing owls in the Mojave Desert","docAbstract":"We estimated relative abundance and density of Western Burrowing Owls (Athene cunicularia hypugaea) at two sites in the Mojave Desert (200304). We made modifications to previously established Burrowing Owl survey techniques for use in desert shrublands and evaluated several factors that might influence the detection of owls. We tested the effectiveness of the call-broadcast technique for surveying this species, the efficiency of this technique at early and late breeding stages, and the effectiveness of various numbers of vocalization intervals during broadcasting sessions. Only 1 (3) of 31 initial (new) owl responses was detected during passive-listening sessions. We found that surveying early in the nesting season was more likely to produce new owl detections compared to surveying later in the nesting season. New owls detected during each of the three vocalization intervals (each consisting of 30 sec of vocalizations followed by 30 sec of silence) of our broadcasting session were similar (37, 40, and 23; n 30). We used a combination of detection trials (sighting probability) and double-observer method to estimate the components of detection probability, i.e., availability and perception. Availability for all sites and years, as determined by detection trials, ranged from 46.158.2. Relative abundance, measured as frequency of occurrence and defined as the proportion of surveys with at least one owl, ranged from 19.232.0 for both sites and years. Density at our eastern Mojave Desert site was estimated at 0.09 ?? 0.01 (SE) owl territories/km<sup>2</sup> and 0.16 ?? 0.02 (SE) owl territories/km<sup>2</sup> during 2003 and 2004, respectively. In our southern Mojave Desert site, density estimates were 0.09 ?? 0.02 (SE) owl territories/km<sup>2</sup> and 0.08 ?? 0.02 (SE) owl territories/km <sup>2</sup> during 2004 and 2005, respectively. ?? 2010 The Raptor Research Foundation, Inc.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Raptor Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.3356/JRR-08-40.1","issn":"08921016","usgsCitation":"Crowe, D., and Longshore, K., 2010, Estimates of density, detection probability, and factors influencing detection of burrowing owls in the Mojave Desert: Journal of Raptor Research, v. 44, no. 1, p. 1-11, https://doi.org/10.3356/JRR-08-40.1.","startPage":"1","endPage":"11","numberOfPages":"11","costCenters":[],"links":[{"id":475929,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.3356/jrr-08-40.1","text":"Publisher Index Page"},{"id":217319,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.3356/JRR-08-40.1"},{"id":245257,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"44","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0adce4b0c8380cd52483","contributors":{"authors":[{"text":"Crowe, D.E.","contributorId":43600,"corporation":false,"usgs":true,"family":"Crowe","given":"D.E.","email":"","affiliations":[],"preferred":false,"id":460436,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Longshore, K.M.","contributorId":70337,"corporation":false,"usgs":true,"family":"Longshore","given":"K.M.","email":"","affiliations":[],"preferred":false,"id":460437,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70037388,"text":"70037388 - 2010 - The quixotic search for a comprehensive understanding of hydrologic response at the surface: Horton, Dunne, Dunton, and the role of concept-development simulation","interactions":[],"lastModifiedDate":"2012-03-12T17:22:07","indexId":"70037388","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1924,"text":"Hydrological Processes","active":true,"publicationSubtype":{"id":10}},"title":"The quixotic search for a comprehensive understanding of hydrologic response at the surface: Horton, Dunne, Dunton, and the role of concept-development simulation","docAbstract":"[No abstract available]","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Hydrological Processes","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1002/hyp.7834","issn":"08856087","usgsCitation":"Loague, K., Heppner, C., Ebel, B., and VanderKwaak, J., 2010, The quixotic search for a comprehensive understanding of hydrologic response at the surface: Horton, Dunne, Dunton, and the role of concept-development simulation: Hydrological Processes, v. 24, no. 17, p. 2499-2505, https://doi.org/10.1002/hyp.7834.","startPage":"2499","endPage":"2505","numberOfPages":"7","costCenters":[],"links":[{"id":217411,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1002/hyp.7834"},{"id":245357,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"24","issue":"17","noUsgsAuthors":false,"publicationDate":"2010-07-20","publicationStatus":"PW","scienceBaseUri":"505baeede4b08c986b32442c","contributors":{"authors":[{"text":"Loague, K.","contributorId":77307,"corporation":false,"usgs":true,"family":"Loague","given":"K.","affiliations":[],"preferred":false,"id":460829,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Heppner, C.S.","contributorId":37147,"corporation":false,"usgs":true,"family":"Heppner","given":"C.S.","affiliations":[],"preferred":false,"id":460828,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ebel, B.A.","contributorId":87772,"corporation":false,"usgs":true,"family":"Ebel","given":"B.A.","email":"","affiliations":[],"preferred":false,"id":460830,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"VanderKwaak, J.E.","contributorId":103497,"corporation":false,"usgs":true,"family":"VanderKwaak","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":460831,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70037300,"text":"70037300 - 2010 - Active shoreline of Ontario Lacus, Titan: A morphological study of the lake and its surroundings","interactions":[],"lastModifiedDate":"2012-03-12T17:22:08","indexId":"70037300","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1807,"text":"Geophysical Research Letters","active":true,"publicationSubtype":{"id":10}},"title":"Active shoreline of Ontario Lacus, Titan: A morphological study of the lake and its surroundings","docAbstract":"Of more than 400 filled lakes now identified on Titan, the first and largest reported in the southern latitudes is Ontario Lacus, which is dark in both infrared and microwave. Here we describe recent observations including synthetic aperture radar (SAR) images by Cassini's radar instrument (??= 2 cm) and show morphological evidence for active material transport and erosion. Ontario Lacus lies in a shallow depression, with greater relief on the southwestern shore and a gently sloping, possibly wave-generated beach to the northeast. The lake has a closed internal drainage system fed by Earth-like rivers, deltas and alluvial fans. Evidence for active shoreline processes, including the wave-modified lakefront and deltaic deposition, indicates that Ontario is a dynamic feature undergoing typical terrestrial forms of littoral modification. Copyright ?? 2010 by the American Geophysical Union.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Geophysical Research Letters","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1029/2009GL041821","issn":"00948276","usgsCitation":"Wall, S., Hayes, A., Bristow, C., Lorenz, R., Stofan, E., Lunine, J., Le, G.A., Janssen, M., Lopes, R., Wye, L., Soderblom, L., Paillou, P., Aharonson, O., Zebker, H., Farr, T., Mitri, G., Kirk, R., Mitchell, K., Notarnicola, C., Casarano, D., and Ventura, B., 2010, Active shoreline of Ontario Lacus, Titan: A morphological study of the lake and its surroundings: Geophysical Research Letters, v. 37, no. 5, https://doi.org/10.1029/2009GL041821.","costCenters":[],"links":[{"id":475934,"rank":10000,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://hal.science/hal-00495897","text":"External 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C.","contributorId":81724,"corporation":false,"usgs":true,"family":"Bristow","given":"C.","email":"","affiliations":[],"preferred":false,"id":460341,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lorenz, R.","contributorId":49503,"corporation":false,"usgs":true,"family":"Lorenz","given":"R.","affiliations":[],"preferred":false,"id":460336,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Stofan, E.","contributorId":99268,"corporation":false,"usgs":true,"family":"Stofan","given":"E.","affiliations":[],"preferred":false,"id":460343,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Lunine, J.","contributorId":42335,"corporation":false,"usgs":true,"family":"Lunine","given":"J.","affiliations":[],"preferred":false,"id":460334,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Le, Gall A.","contributorId":36764,"corporation":false,"usgs":true,"family":"Le","given":"Gall","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":460332,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Janssen, M.","contributorId":22893,"corporation":false,"usgs":true,"family":"Janssen","given":"M.","email":"","affiliations":[],"preferred":false,"id":460327,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Lopes, R.","contributorId":61554,"corporation":false,"usgs":true,"family":"Lopes","given":"R.","affiliations":[],"preferred":false,"id":460337,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Wye, L.","contributorId":40333,"corporation":false,"usgs":true,"family":"Wye","given":"L.","affiliations":[],"preferred":false,"id":460333,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Soderblom, L.","contributorId":106244,"corporation":false,"usgs":true,"family":"Soderblom","given":"L.","affiliations":[],"preferred":false,"id":460346,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Paillou, P.","contributorId":45043,"corporation":false,"usgs":true,"family":"Paillou","given":"P.","affiliations":[],"preferred":false,"id":460335,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Aharonson, O.","contributorId":105030,"corporation":false,"usgs":false,"family":"Aharonson","given":"O.","affiliations":[],"preferred":false,"id":460345,"contributorType":{"id":1,"text":"Authors"},"rank":13},{"text":"Zebker, H.","contributorId":25276,"corporation":false,"usgs":false,"family":"Zebker","given":"H.","affiliations":[],"preferred":false,"id":460329,"contributorType":{"id":1,"text":"Authors"},"rank":14},{"text":"Farr, Tom","contributorId":24903,"corporation":false,"usgs":true,"family":"Farr","given":"Tom","affiliations":[],"preferred":false,"id":460328,"contributorType":{"id":1,"text":"Authors"},"rank":15},{"text":"Mitri, Giuseppe","contributorId":35052,"corporation":false,"usgs":false,"family":"Mitri","given":"Giuseppe","email":"","affiliations":[],"preferred":false,"id":460331,"contributorType":{"id":1,"text":"Authors"},"rank":16},{"text":"Kirk, R.","contributorId":66829,"corporation":false,"usgs":true,"family":"Kirk","given":"R.","affiliations":[],"preferred":false,"id":460338,"contributorType":{"id":1,"text":"Authors"},"rank":17},{"text":"Mitchell, Ken","contributorId":8211,"corporation":false,"usgs":true,"family":"Mitchell","given":"Ken","email":"","affiliations":[],"preferred":false,"id":460326,"contributorType":{"id":1,"text":"Authors"},"rank":18},{"text":"Notarnicola, C.","contributorId":82951,"corporation":false,"usgs":true,"family":"Notarnicola","given":"C.","email":"","affiliations":[],"preferred":false,"id":460342,"contributorType":{"id":1,"text":"Authors"},"rank":19},{"text":"Casarano, D.","contributorId":76162,"corporation":false,"usgs":true,"family":"Casarano","given":"D.","email":"","affiliations":[],"preferred":false,"id":460340,"contributorType":{"id":1,"text":"Authors"},"rank":20},{"text":"Ventura, B.","contributorId":67335,"corporation":false,"usgs":true,"family":"Ventura","given":"B.","email":"","affiliations":[],"preferred":false,"id":460339,"contributorType":{"id":1,"text":"Authors"},"rank":21}]}}
,{"id":70037137,"text":"70037137 - 2010 - Distribution of non-breeding great lakes piping plovers (Charadrius melodus) along Atlantic and Gulf of Mexico coastlines: Ten years of band sightings","interactions":[],"lastModifiedDate":"2017-09-11T15:54:51","indexId":"70037137","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3731,"text":"Waterbirds","onlineIssn":"19385390","printIssn":"15244695","active":true,"publicationSubtype":{"id":10}},"title":"Distribution of non-breeding great lakes piping plovers (Charadrius melodus) along Atlantic and Gulf of Mexico coastlines: Ten years of band sightings","docAbstract":"In 1993, a mark-recapture effort was initiated to band annually all Great Lakes Piping Plover nesting adults and offspring. With voluntary reporting by observers, >430 sightings of 154 individually-marked Great Lakes banded birds were documented on the wintering grounds during 19952005. This paper reports non-breeding distribution and site-fidelity and identifies Critical Habitat units used by this population during the winter. Information obtained through banded bird sightings indicates that the winter range of Great Lakes Piping Plovers extends from North Carolina to Texas, and the Bahamas, with the majority (75%) of reported individuals wintering in Georgia and Florida. About 95% of sightings were near or within federally-designated winter Critical Habitat for Piping Plovers. Within season (52%) and between-year (62%) site fidelity was documented for resightings within 3.5 km of initial sighting. Although breeding pairs do not winter in close association, there is some evidence to suggest that offspring winter closer to the male rather than the female parent (P-value = 0.03), and adult males and females appear to exhibit latitudinal segregation (P-value < 0.001). Females reach the winter grounds before males, arriving in July and staying through April (???9 months) or 75% of the annual cycle. The study is the first to identify winter distribution for the Great Lakes Piping Plover population. The significant proportion of the annual cycle spent on the wintering grounds emphasizes the importance of habitat protection during the non-breeding season for this federally-listed population.","language":"English","publisher":"The Waterbird Society","doi":"10.1675/063.033.0103","issn":"15244695","usgsCitation":"Stucker, J.H., Cuthbert, F., Winn, B., Noel, B., Maddock, S., Leary, P., Cordes, J., and Wemmer, L., 2010, Distribution of non-breeding great lakes piping plovers (Charadrius melodus) along Atlantic and Gulf of Mexico coastlines: Ten years of band sightings: Waterbirds, v. 33, no. 1, p. 22-32, https://doi.org/10.1675/063.033.0103.","productDescription":"11 p.","startPage":"22","endPage":"32","numberOfPages":"11","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":217395,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1675/063.033.0103"},{"id":245341,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"33","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a02eae4b0c8380cd50267","contributors":{"authors":[{"text":"Stucker, J. H.","contributorId":22595,"corporation":false,"usgs":true,"family":"Stucker","given":"J.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":459550,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cuthbert, F.J.","contributorId":45272,"corporation":false,"usgs":true,"family":"Cuthbert","given":"F.J.","email":"","affiliations":[],"preferred":false,"id":459551,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Winn, Brad","contributorId":90852,"corporation":false,"usgs":true,"family":"Winn","given":"Brad","email":"","affiliations":[],"preferred":false,"id":459554,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Noel, B.L.","contributorId":7537,"corporation":false,"usgs":true,"family":"Noel","given":"B.L.","email":"","affiliations":[],"preferred":false,"id":459548,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Maddock, S.B.","contributorId":48797,"corporation":false,"usgs":true,"family":"Maddock","given":"S.B.","email":"","affiliations":[],"preferred":false,"id":459552,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Leary, P.R.","contributorId":98148,"corporation":false,"usgs":true,"family":"Leary","given":"P.R.","email":"","affiliations":[],"preferred":false,"id":459555,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Cordes, J.","contributorId":88942,"corporation":false,"usgs":true,"family":"Cordes","given":"J.","email":"","affiliations":[],"preferred":false,"id":459553,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Wemmer, L.C.","contributorId":13592,"corporation":false,"usgs":true,"family":"Wemmer","given":"L.C.","email":"","affiliations":[],"preferred":false,"id":459549,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":70037232,"text":"70037232 - 2010 - Radar image and data fusion for natural hazards characterisation","interactions":[],"lastModifiedDate":"2017-04-05T16:38:44","indexId":"70037232","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2052,"text":"International Journal of Image and Data Fusion","active":true,"publicationSubtype":{"id":10}},"title":"Radar image and data fusion for natural hazards characterisation","docAbstract":"Fusion of synthetic aperture radar (SAR) images through interferometric, polarimetric and tomographic processing provides an all - weather imaging capability to characterise and monitor various natural hazards. This article outlines interferometric synthetic aperture radar (InSAR) processing and products and their utility for natural hazards characterisation, provides an overview of the techniques and applications related to fusion of SAR/InSAR images with optical and other images and highlights the emerging SAR fusion technologies. In addition to providing precise land - surface digital elevation maps, SAR - derived imaging products can map millimetre - scale elevation changes driven by volcanic, seismic and hydrogeologic processes, by landslides and wildfires and other natural hazards. With products derived from the fusion of SAR and other images, scientists can monitor the progress of flooding, estimate water storage changes in wetlands for improved hydrological modelling predictions and assessments of future flood impacts and map vegetation structure on a global scale and monitor its changes due to such processes as fire, volcanic eruption and deforestation. With the availability of SAR images in near real - time from multiple satellites in the near future, the fusion of SAR images with other images and data is playing an increasingly important role in understanding and forecasting natural hazards.","language":"English","publisher":"Taylor & Francis","doi":"10.1080/19479832.2010.499219","issn":"19479832","usgsCitation":"Lu, Z., Dzurisin, D., Jung, H., Zhang, J., and Zhang, Y., 2010, Radar image and data fusion for natural hazards characterisation: International Journal of Image and Data Fusion, v. 1, no. 3, p. 217-242, https://doi.org/10.1080/19479832.2010.499219.","productDescription":"26 p.","startPage":"217","endPage":"242","numberOfPages":"26","costCenters":[{"id":157,"text":"Cascades Volcano Observatory","active":false,"usgs":true},{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":245376,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":217429,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1080/19479832.2010.499219"}],"volume":"1","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a9383e4b0c8380cd80e78","contributors":{"authors":[{"text":"Lu, Zhong 0000-0001-9181-1818 lu@usgs.gov","orcid":"https://orcid.org/0000-0001-9181-1818","contributorId":901,"corporation":false,"usgs":true,"family":"Lu","given":"Zhong","email":"lu@usgs.gov","affiliations":[],"preferred":true,"id":459988,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dzurisin, Daniel 0000-0002-0138-5067 dzurisin@usgs.gov","orcid":"https://orcid.org/0000-0002-0138-5067","contributorId":538,"corporation":false,"usgs":true,"family":"Dzurisin","given":"Daniel","email":"dzurisin@usgs.gov","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":459987,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Jung, Hyung-Sup","contributorId":58382,"corporation":false,"usgs":true,"family":"Jung","given":"Hyung-Sup","email":"","affiliations":[],"preferred":false,"id":459990,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Zhang, Jixian","contributorId":36396,"corporation":false,"usgs":true,"family":"Zhang","given":"Jixian","affiliations":[],"preferred":false,"id":459989,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Zhang, Yonghong","contributorId":82563,"corporation":false,"usgs":true,"family":"Zhang","given":"Yonghong","email":"","affiliations":[],"preferred":false,"id":459991,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"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":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":70037206,"text":"70037206 - 2010 - Timing and duration of garnet granulite metamorphism in magmatic arc crust, Fiordland, New Zealand","interactions":[],"lastModifiedDate":"2012-03-12T17:22:07","indexId":"70037206","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":"Timing and duration of garnet granulite metamorphism in magmatic arc crust, Fiordland, New Zealand","docAbstract":"Pembroke Granulite from Fiordland, New Zealand provides a window into the mid- to lower crust of magmatic arcs. Garnet Sm-Nd and zircon U-Pb ages constrain the timing and duration of high-P partial melting that produced trondhjemitic high Sr/Y magma. Trace element zoning in large, euhedral garnet is compatible with little post growth modification and supports the interpretation that garnet Sm-Nd ages of 126.1??2.0 and 122.6??2.0. Ma date crystal growth. Integration of the garnet ages with U-Pb zircon ages elucidates a history of intrusion(?) and a protracted period of high-temperature metamorphism and partial melting. The oldest zircon ages of 163 to 150. Ma reflect inheritance or intrusion and a cluster of zircon ages ca. 134. Ma date orthopyroxene-bearing mineral assemblages that may be magmatic or metamorphic in origin. Zircon and garnet ages from unmelted gneiss and garnet reaction zones record garnet granulite facies metamorphism at 128 to 126. Ma. Peritectic garnet and additional zircon ages from trondhjemite veins and garnet reaction zones indicate that garnet growth and partial melting lasted until ca. 123. Ma. Two single fraction garnet ages and young zircon ages suggest continued high-temperature re-equilibration until ca. 95. Ma. Phase diagram sections constrain orthopyroxene assemblages to <0.6 GPa @ 650??C, peak garnet granulite facies metamorphic conditions to 680-815??C @ 1.1-1.4. GPa, and a P-T path with a P increase of???0.5. GPa. These sections are compatible with water contents???0.28wt.%, local dehydration during garnet granulite metamorphism, and <0.3. GPa P increases during garnet growth. Results demonstrate the utility of integrated U-Pb zircon and Sm-Nd garnet ages, and phase diagram sections for understanding the nature, duration, and conditions of deep crustal metamorphism and melting. Geochronologic and thermobarometric data for garnet granulite indicate that thickening of arc crust, which caused high-pressure metamorphism in northern Fiordland, must have occurred prior to 126. Ma, that loading occurred at a rate of ca. 0.06. GPa/m.y., and that garnet granulite metamorphism lasted 3-7m.y. Locally-derived partial melts formed and crystallized in considerably less than 10 and perhaps as little as 3m.y. ?? 2010 Elsevier B.V.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Chemical Geology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.chemgeo.2010.02.015","issn":"00092541","usgsCitation":"Stowell, H., Tulloch, A., Zuluaga, C., and Koenig, A., 2010, Timing and duration of garnet granulite metamorphism in magmatic arc crust, Fiordland, New Zealand: Chemical Geology, v. 273, no. 1-2, p. 91-110, https://doi.org/10.1016/j.chemgeo.2010.02.015.","startPage":"91","endPage":"110","numberOfPages":"20","costCenters":[],"links":[{"id":244964,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":217053,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.chemgeo.2010.02.015"}],"volume":"273","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb3e4e4b08c986b326051","contributors":{"authors":[{"text":"Stowell, H.","contributorId":19409,"corporation":false,"usgs":true,"family":"Stowell","given":"H.","email":"","affiliations":[],"preferred":false,"id":459899,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tulloch, A.","contributorId":10645,"corporation":false,"usgs":true,"family":"Tulloch","given":"A.","email":"","affiliations":[],"preferred":false,"id":459898,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Zuluaga, C.","contributorId":37177,"corporation":false,"usgs":true,"family":"Zuluaga","given":"C.","email":"","affiliations":[],"preferred":false,"id":459900,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Koenig, A. 0000-0002-5230-0924","orcid":"https://orcid.org/0000-0002-5230-0924","contributorId":64037,"corporation":false,"usgs":true,"family":"Koenig","given":"A.","affiliations":[],"preferred":false,"id":459901,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70037389,"text":"70037389 - 2010 - Spider-mediated flux of PCBs from contaminated sediments to terrestrial ecosystems and potential risks to arachnivorous birds","interactions":[],"lastModifiedDate":"2012-03-12T17:22:11","indexId":"70037389","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":"Spider-mediated flux of PCBs from contaminated sediments to terrestrial ecosystems and potential risks to arachnivorous birds","docAbstract":"We investigated aquatic insect utilization and PCB exposure in riparian spiders at the Lake Hartwell Superfund site (Clemson, SC). We sampled sediments, adult chironomids, terrestrial insects, riparian spiders (Tetragnathidae, Araneidae, and Mecynogea lemniscata), and upland spiders (Araneidae) along a sediment contamination gradient. Stable isotopes (?<sup>13</sup>C, ? <sup>15</sup>N) indicated that riparian spiders primarily consumed aquatic insects whereas upland spiders consumed terrestrial insects. PCBs in chironomids (mean 1240 ng/g among sites) were 2 orders of magnitude higher than terrestrial insects (15.2 ng/g), similar to differences between riparian (820?2012 ng/g) and upland spiders (30 ng/g). Riparian spider PCBs were positively correlated with sediment concentrations for all taxa (r<sup>2</sup> = 0.44?0.87). We calculated spider-based wildlife values (WVs, the minimum spider PCB concentrations causing physiologically significant doses in consumers) to assess exposure risks for arachnivorous birds. Spider concentrations exceeded WVs for most birds at heavily contaminated sites and were ?14-fold higher for the most sensitive species (chickadee nestlings, Poecile spp.). Spiders are abundant and ubiquitous in riparian habitats, where they depend on aquatic insect prey. These traits, along with the high degree of spatial correlation between spider and sediment concentrations we observed, suggest that they are model indicator species for monitoring contaminated sediment sites and assessing risks associated with contaminant flux into terrestrial ecosystems. ?? This article not subject to U.S. Copyright. Published 2009 by the American Chemical Society.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Environmental Science and Technology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1021/es9023139","issn":"0013936X","usgsCitation":"Walters, D., Mills, M., Fritz, K., and Raikow, D., 2010, Spider-mediated flux of PCBs from contaminated sediments to terrestrial ecosystems and potential risks to arachnivorous birds: Environmental Science & Technology, v. 44, no. 8, p. 2849-2856, https://doi.org/10.1021/es9023139.","startPage":"2849","endPage":"2856","numberOfPages":"8","costCenters":[],"links":[{"id":245386,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":217438,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1021/es9023139"}],"volume":"44","issue":"8","noUsgsAuthors":false,"publicationDate":"2009-12-21","publicationStatus":"PW","scienceBaseUri":"505b95c3e4b08c986b31b0eb","contributors":{"authors":[{"text":"Walters, D.M.","contributorId":41507,"corporation":false,"usgs":true,"family":"Walters","given":"D.M.","email":"","affiliations":[],"preferred":false,"id":460832,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mills, M.A.","contributorId":77764,"corporation":false,"usgs":true,"family":"Mills","given":"M.A.","email":"","affiliations":[],"preferred":false,"id":460833,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fritz, K.M.","contributorId":93300,"corporation":false,"usgs":true,"family":"Fritz","given":"K.M.","email":"","affiliations":[],"preferred":false,"id":460834,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Raikow, D.F.","contributorId":98972,"corporation":false,"usgs":true,"family":"Raikow","given":"D.F.","email":"","affiliations":[],"preferred":false,"id":460835,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70037078,"text":"70037078 - 2010 - Silica in a Mars analog environment: Ka u Desert, Kilauea Volcano, Hawaii","interactions":[],"lastModifiedDate":"2012-03-12T17:21:48","indexId":"70037078","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2317,"text":"Journal of Geophysical Research E: Planets","active":true,"publicationSubtype":{"id":10}},"title":"Silica in a Mars analog environment: Ka u Desert, Kilauea Volcano, Hawaii","docAbstract":"Airborne Visible/Near-Infrared Imaging Spectrometer (AVIRIS) data acquired over the Ka u Desert are atmospherically corrected to ground reflectance and used to identify the mineralogic components of relatively young basaltic materials, including 250-700 and 200-400 year old lava flows, 1971 and 1974 flows, ash deposits, and solfatara incrustations. To provide context, a geologic surface units map is constructed, verified with field observations, and supported by laboratory analyses. AVIRIS spectral endmembers are identified in the visible (0.4 to 1.2 ??m) and short wave infrared (2.0 to 2.5 ??m) wavelength ranges. Nearly all the spectral variability is controlled by the presence of ferrous and ferric iron in such minerals as pyroxene, olivine, hematite, goethite, and poorly crystalline iron oxides or glass. A broad, nearly ubiquitous absorption feature centered at 2.25 ??m is attributed to opaline (amorphous, hydrated) silica and is found to correlate spatially with mapped geologic surface units. Laboratory analyses show the silica to be consistently present as a deposited phase, including incrustations downwind from solfatara vents, cementing agent for ash duricrusts, and thin coatings on the youngest lava flow surfaces. A second, Ti-rich upper coating on young flows also influences spectral behavior. This study demonstrates that secondary silica is mobile in the Ka u Desert on a variety of time scales and spatial domains. The investigation from remote, field, and laboratory perspectives also mimics exploration of Mars using orbital and landed missions, with important implications for spectral characterization of coated basalts and formation of opaline silica in arid, acidic alteration environments. Copyright 2010 by the American Geophysical Union.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Geophysical Research E: Planets","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1029/2009JE003347","issn":"01480227","usgsCitation":"Seelos, K., Arvidson, R., Jolliff, B., Chemtob, S., Morris, R., Ming, D.W., and Swayze, G., 2010, Silica in a Mars analog environment: Ka u Desert, Kilauea Volcano, Hawaii: Journal of Geophysical Research E: Planets, v. 115, no. 4, https://doi.org/10.1029/2009JE003347.","costCenters":[],"links":[{"id":475821,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1029/2009je003347","text":"Publisher Index Page"},{"id":216990,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1029/2009JE003347"},{"id":244897,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"115","issue":"4","noUsgsAuthors":false,"publicationDate":"2010-04-08","publicationStatus":"PW","scienceBaseUri":"505b8f32e4b08c986b318da3","contributors":{"authors":[{"text":"Seelos, K.D.","contributorId":73849,"corporation":false,"usgs":true,"family":"Seelos","given":"K.D.","email":"","affiliations":[],"preferred":false,"id":459277,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Arvidson, R. E.","contributorId":46666,"corporation":false,"usgs":true,"family":"Arvidson","given":"R. E.","affiliations":[],"preferred":false,"id":459276,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Jolliff, B.L.","contributorId":21268,"corporation":false,"usgs":true,"family":"Jolliff","given":"B.L.","email":"","affiliations":[],"preferred":false,"id":459273,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Chemtob, S.M.","contributorId":38435,"corporation":false,"usgs":true,"family":"Chemtob","given":"S.M.","email":"","affiliations":[],"preferred":false,"id":459275,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Morris, R.V.","contributorId":6978,"corporation":false,"usgs":true,"family":"Morris","given":"R.V.","affiliations":[],"preferred":false,"id":459272,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Ming, D. W.","contributorId":96811,"corporation":false,"usgs":true,"family":"Ming","given":"D.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":459278,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Swayze, G.A. 0000-0002-1814-7823","orcid":"https://orcid.org/0000-0002-1814-7823","contributorId":21570,"corporation":false,"usgs":true,"family":"Swayze","given":"G.A.","affiliations":[],"preferred":false,"id":459274,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70037205,"text":"70037205 - 2010 - OMG earthquake! can twitter improve earthquake response?","interactions":[],"lastModifiedDate":"2012-03-12T17:22:07","indexId":"70037205","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3372,"text":"Seismological Research Letters","onlineIssn":"1938-2057","printIssn":"0895-0695","active":true,"publicationSubtype":{"id":10}},"title":"OMG earthquake! can twitter improve earthquake response?","docAbstract":"[No abstract available]","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Seismological Research Letters","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1785/gssrl.81.2.246","issn":"08950695","usgsCitation":"Earle, P., Guy, M., Buckmaster, R., Ostrum, C., Horvath, S., and Vaughan, A., 2010, OMG earthquake! can twitter improve earthquake response?: Seismological Research Letters, v. 81, no. 2, p. 246-251, https://doi.org/10.1785/gssrl.81.2.246.","startPage":"246","endPage":"251","numberOfPages":"6","costCenters":[],"links":[{"id":244963,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":217052,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1785/gssrl.81.2.246"}],"volume":"81","issue":"2","noUsgsAuthors":false,"publicationDate":"2010-03-09","publicationStatus":"PW","scienceBaseUri":"505a69e5e4b0c8380cd73f6e","contributors":{"authors":[{"text":"Earle, P.","contributorId":26860,"corporation":false,"usgs":true,"family":"Earle","given":"P.","email":"","affiliations":[],"preferred":false,"id":459893,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Guy, M.","contributorId":50014,"corporation":false,"usgs":true,"family":"Guy","given":"M.","email":"","affiliations":[],"preferred":false,"id":459894,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Buckmaster, R.","contributorId":100654,"corporation":false,"usgs":true,"family":"Buckmaster","given":"R.","email":"","affiliations":[],"preferred":false,"id":459896,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ostrum, C.","contributorId":96925,"corporation":false,"usgs":true,"family":"Ostrum","given":"C.","email":"","affiliations":[],"preferred":false,"id":459895,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Horvath, S.","contributorId":20575,"corporation":false,"usgs":true,"family":"Horvath","given":"S.","email":"","affiliations":[],"preferred":false,"id":459892,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Vaughan, A.","contributorId":108343,"corporation":false,"usgs":true,"family":"Vaughan","given":"A.","email":"","affiliations":[],"preferred":false,"id":459897,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70037260,"text":"70037260 - 2010 - Trace elements have limited utility for studying migratory connectivity in shorebirds that winter in Argentina","interactions":[],"lastModifiedDate":"2012-03-12T17:22:11","indexId":"70037260","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1318,"text":"Condor","active":true,"publicationSubtype":{"id":10}},"title":"Trace elements have limited utility for studying migratory connectivity in shorebirds that winter in Argentina","docAbstract":"Trace-element analysis has been suggested as a tool for the study of migratory connectivity because (1) trace-element abundance varies spatially in the environment, (2) trace elements are assimilated into animals' tissues through the diet, and (3) current technology permits the analysis of multiple trace elements in a small tissue sample, allowing the simultaneous exploration of several elements. We explored the potential of trace elements (B, Na, Mg, Al, Si, P, S, K, Ca, Ti, Cr, Mn, Ni, Cu, Zn, As, Sr, Cs, Hg, Tl, Pb, Bi, Th, and U) to clarify the migratory connectivity of shorebirds that breed in North America and winter in southern South America. We collected 66 recently replaced secondary feathers from Red Knots (Calidris canutus) at three sites in Patagonia and 76 from White-rumped Sandpipers (C. fuscicollis) at nine sites across Argentina. There were significant differences in trace-element abundance in shorebird feathers grown at different nonbreeding sites, and annual variability within a site was small compared to variability among sites. Across Argentina, there was no large-scale gradient in trace elements. The lack of such a gradient restricts the application of this technique to questions concerning the origin of shorebirds to a small number of discrete sites. Furthermore, our results including three additional species, the Pectoral Sandpiper (C. melanotos), Wilson's Phalarope (Phalaropus tricolor), and Collared Plover (Charadrius collaris), suggest that trace-element profiles change as feathers age. Temporal instability of trace-element values could undermine their application to the study of migratory connectivity in shorebirds. ?? The Cooper Ornithological Society 2010.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Condor","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1525/cond.2010.090166","issn":"00105422","usgsCitation":"Torres-Dowdall, J., Farmer, A., Abril, M., Bucher, E., and Ridley, I., 2010, Trace elements have limited utility for studying migratory connectivity in shorebirds that winter in Argentina: Condor, v. 112, no. 3, p. 490-498, https://doi.org/10.1525/cond.2010.090166.","startPage":"490","endPage":"498","numberOfPages":"9","costCenters":[],"links":[{"id":475962,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1525/cond.2010.090166","text":"Publisher Index Page"},{"id":245348,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":217402,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1525/cond.2010.090166"}],"volume":"112","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb649e4b08c986b326b94","contributors":{"authors":[{"text":"Torres-Dowdall, J.","contributorId":13433,"corporation":false,"usgs":true,"family":"Torres-Dowdall","given":"J.","email":"","affiliations":[],"preferred":false,"id":460130,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Farmer, A.H.","contributorId":79063,"corporation":false,"usgs":true,"family":"Farmer","given":"A.H.","email":"","affiliations":[],"preferred":false,"id":460134,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Abril, M.","contributorId":49751,"corporation":false,"usgs":true,"family":"Abril","given":"M.","email":"","affiliations":[],"preferred":false,"id":460131,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bucher, E.H.","contributorId":64054,"corporation":false,"usgs":true,"family":"Bucher","given":"E.H.","email":"","affiliations":[],"preferred":false,"id":460132,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Ridley, I.","contributorId":70339,"corporation":false,"usgs":true,"family":"Ridley","given":"I.","email":"","affiliations":[],"preferred":false,"id":460133,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70037055,"text":"70037055 - 2010 - Striped Bass, morone saxatilis, egg incubation in large volume jars","interactions":[],"lastModifiedDate":"2012-03-12T17:22:11","indexId":"70037055","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2574,"text":"Journal of the World Aquaculture Society","active":true,"publicationSubtype":{"id":10}},"title":"Striped Bass, morone saxatilis, egg incubation in large volume jars","docAbstract":"The standard McDonald jar was compared with a large volume jar for striped bass, Morone saxatilis, egg incubation. The McDonald jar measured 16 cm in diameter by 45 cm in height and had a volume of 6 L. The experimental jar measured 0.4 m in diameter by 1.3 m in height and had a volume of 200 L. The hypothesis is that there is no difference in percent survival of fry hatched in experimental jars compared with McDonald jars. Striped bass brood fish were collected from the Coosa River and spawned using the dry spawn method of fertilization. Four McDonald jars were stocked with approximately 150 g of eggs each. Post-hatch survival was estimated at 48, 96, and 144 h. Stocking rates resulted in an average egg loading rate (??1 SE) in McDonald jars of 21.9 ?? 0.03 eggs/mL and in experimental jars of 10.9 ?? 0.57 eggs/mL. The major finding of this study was that average fry survival was 37.3 ?? 4.49% for McDonald jars and 34.2 ?? 3.80% for experimental jars. Although survival in experimental jars was slightly less than in McDonald jars, the effect of container volume on survival to 48 h (F = 6.57; df = 1,5; P > 0.05), 96 h (F = 0.02; df = 1, 4; P > 0.89), and 144 h (F = 3.50; df = 1, 4; P > 0.13) was not statistically significant. Mean survival between replicates ranged from 14.7 to 60.1% in McDonald jars and from 10.1 to 54.4% in experimental jars. No effect of initial stocking rate on survival (t = 0.06; df = 10; P > 0.95) was detected. Experimental jars allowed for incubation of a greater number of eggs in less than half the floor space of McDonald jars. As hatchery production is often limited by space or water supply, experimental jars offer an alternative to extending spawning activities, thereby reducing labor and operations cost. As survival was similar to McDonald jars, the experimental jar is suitable for striped bass egg incubation. ?? Copyright by the World Aquaculture Society 2010.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of the World Aquaculture Society","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1111/j.1749-7345.2010.00404.x","issn":"08938849","usgsCitation":"Harper, C., Wrege, B., and Jeffery, I., 2010, Striped Bass, morone saxatilis, egg incubation in large volume jars: Journal of the World Aquaculture Society, v. 41, no. 4, p. 633-639, https://doi.org/10.1111/j.1749-7345.2010.00404.x.","startPage":"633","endPage":"639","numberOfPages":"7","costCenters":[],"links":[{"id":217133,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1111/j.1749-7345.2010.00404.x"},{"id":245052,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"41","issue":"4","noUsgsAuthors":false,"publicationDate":"2010-08-02","publicationStatus":"PW","scienceBaseUri":"505b9b73e4b08c986b31cec8","contributors":{"authors":[{"text":"Harper, C.J.","contributorId":107531,"corporation":false,"usgs":true,"family":"Harper","given":"C.J.","email":"","affiliations":[],"preferred":false,"id":459171,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wrege, B.M.","contributorId":100405,"corporation":false,"usgs":true,"family":"Wrege","given":"B.M.","affiliations":[],"preferred":false,"id":459170,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Jeffery, Isely J.","contributorId":15044,"corporation":false,"usgs":true,"family":"Jeffery","given":"Isely J.","affiliations":[],"preferred":false,"id":459169,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"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}]}}
]}