While many wildlife species are threatened, some populations have recovered from previous overexploitation, and data linking these population increases with disease dynamics are limited. We present data suggesting that free-ranging elk (Cervus elaphus) are a maintenance host for Brucella abortus in new areas of the Greater Yellowstone Ecosystem (GYE). Brucellosis seroprevalence in free-ranging elk increased from 0-7% in 1991-1992 to 8-20% in 2006-2007 in four of six herd units around the GYE. These levels of brucellosis are comparable to some herd units where elk are artificially aggregated on supplemental feeding grounds. There are several possible mechanisms for this increase that we evaluated using statistical and population modeling approaches. Simulations of an age-structured population model suggest that the observed levels of seroprevalence are unlikely to be sustained by dispersal from supplemental feeding areas with relatively high seroprevalence or an older age structure. Increases in brucellosis seroprevalence and the total elk population size in areas with feeding grounds have not been statistically detectable. Meanwhile, the rate of seroprevalence increase outside the feeding grounds was related to the population size and density of each herd unit. Therefore, the data suggest that enhanced elk-to-elk transmission in free-ranging populations may be occurring due to larger winter elk aggregations. Elk populations inside and outside of the GYE that traditionally did not maintain brucellosis may now be at risk due to recent population increases. In particular, some neighboring populations of Montana elk were 5-9 times larger in 2007 than in the 1970s, with some aggregations comparable to the Wyoming feeding-ground populations. Addressing the unintended consequences of these increasing populations is complicated by limited hunter access to private lands, which places many ungulate populations out of administrative control. Agency-landowner hunting access partnerships and the protection of large predators are two management strategies that may be used to target high ungulate densities in private refuges and reduce the current and future burden of disease.
","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Ecological Applications","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1890/08-2062.1","issn":"10510761","usgsCitation":"Cross, P.C., Cole, E., Dobson, A.P., Edwards, W., Hamlin, K., Luikart, G., Middleton, A., Scurlock, B., and White, P., 2010, Probable causes of increasing brucellosis in free-ranging elk of the Greater Yellowstone Ecosystem: Ecological Applications, v. 20, no. 1, p. 278-288, https://doi.org/10.1890/08-2062.1.","productDescription":"11 p.","startPage":"278","endPage":"288","numberOfPages":"11","costCenters":[{"id":34983,"text":"Contaminant Biology Program","active":true,"usgs":true}],"links":[{"id":498901,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1890/08-2062.1","text":"Publisher Index Page"},{"id":216863,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1890/08-2062.1"},{"id":244761,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","volume":"20","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a8cc0e4b0c8380cd7e881","contributors":{"authors":[{"text":"Cross, Paul C. 0000-0001-8045-5213 pcross@usgs.gov","orcid":"https://orcid.org/0000-0001-8045-5213","contributorId":2709,"corporation":false,"usgs":true,"family":"Cross","given":"Paul","email":"pcross@usgs.gov","middleInitial":"C.","affiliations":[{"id":481,"text":"Northern Rocky Mountain Science Center","active":true,"usgs":true}],"preferred":true,"id":443600,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cole, E.K.","contributorId":9087,"corporation":false,"usgs":true,"family":"Cole","given":"E.K.","email":"","affiliations":[],"preferred":false,"id":443594,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dobson, A. P.","contributorId":9992,"corporation":false,"usgs":false,"family":"Dobson","given":"A.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":443595,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Edwards, W.H.","contributorId":43718,"corporation":false,"usgs":true,"family":"Edwards","given":"W.H.","affiliations":[],"preferred":false,"id":443598,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Hamlin, K.L.","contributorId":37174,"corporation":false,"usgs":true,"family":"Hamlin","given":"K.L.","email":"","affiliations":[],"preferred":false,"id":443597,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Luikart, G.","contributorId":25515,"corporation":false,"usgs":true,"family":"Luikart","given":"G.","affiliations":[],"preferred":false,"id":443596,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Middleton, A.D.","contributorId":93730,"corporation":false,"usgs":true,"family":"Middleton","given":"A.D.","email":"","affiliations":[],"preferred":false,"id":443602,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Scurlock, B.M.","contributorId":44742,"corporation":false,"usgs":true,"family":"Scurlock","given":"B.M.","affiliations":[],"preferred":false,"id":443599,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"White, P.J.","contributorId":91436,"corporation":false,"usgs":true,"family":"White","given":"P.J.","affiliations":[],"preferred":false,"id":443601,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}} ,{"id":70037356,"text":"70037356 - 2010 - Mercury contamination in fish in midcontinent great rivers of the united states: Importance of species traits and environmental factors","interactions":[],"lastModifiedDate":"2012-03-12T17:22:11","indexId":"70037356","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":"Mercury contamination in fish in midcontinent great rivers of the united states: Importance of species traits and environmental factors","docAbstract":"We measured mercury (Hg) concentrations in whole fish from the Upper Mississippi, Missouri, and Ohio Rivers to characterize the extent and magnitude of Hg contamination and to identify environmental factors influencing Hg accumulation. Concentrations were generally lower (80% of values between 20?200 ng g1 wet weight) than those reported for other regions (e.g., upper Midwest and Northeast U.S.). Mercury exceeded the risk threshold for belted kingfisher (Ceryle alcyon, the most sensitive species considered) in 33?75% of river length and 1?7% of river length for humans. Concentrations were lower in the Missouri than in the Mississippi and Ohio Rivers, consistent with continental-scale patterns in atmospheric Hg deposition. Body size and trophic guild were the best predictors of Hg concentrations, which were highest in large-bodied top predators. Site geochemical and landscape properties were weakly related with fish Hg. Moreover, relationships often ran contrary to conventional wisdom, and the slopes of the relationships (positive or negative) were inconsistent among fish guilds and rivers. For example, sulfate is positively associated with fish Hg concentrations but was negatively correlated with Hg in five of six regression models of tissue concentrations. Variables such as pH, acid neutralizing capacity, and total phosphorus did not occur at levels associated with high fish Hg concentrations, partially explaining the relatively low Hg values we observed. ?? 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/es903754d","issn":"0013936X","usgsCitation":"Walters, D., Blocksom, K., Lazorchak, J., Jicha, T., Angradi, T., and Bolgrien, D., 2010, Mercury contamination in fish in midcontinent great rivers of the united states: Importance of species traits and environmental factors: Environmental Science & Technology, v. 44, no. 8, p. 2947-2953, https://doi.org/10.1021/es903754d.","startPage":"2947","endPage":"2953","numberOfPages":"7","costCenters":[],"links":[{"id":245354,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":217408,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1021/es903754d"}],"volume":"44","issue":"8","noUsgsAuthors":false,"publicationDate":"2010-03-18","publicationStatus":"PW","scienceBaseUri":"505a53f5e4b0c8380cd6ce37","contributors":{"authors":[{"text":"Walters, D.M.","contributorId":41507,"corporation":false,"usgs":true,"family":"Walters","given":"D.M.","email":"","affiliations":[],"preferred":false,"id":460629,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Blocksom, K.A.","contributorId":83766,"corporation":false,"usgs":true,"family":"Blocksom","given":"K.A.","affiliations":[],"preferred":false,"id":460632,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lazorchak, J.M.","contributorId":34620,"corporation":false,"usgs":true,"family":"Lazorchak","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":460628,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Jicha, T.","contributorId":47208,"corporation":false,"usgs":true,"family":"Jicha","given":"T.","email":"","affiliations":[],"preferred":false,"id":460630,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Angradi, T.R.","contributorId":57289,"corporation":false,"usgs":true,"family":"Angradi","given":"T.R.","email":"","affiliations":[],"preferred":false,"id":460631,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Bolgrien, D.W.","contributorId":8311,"corporation":false,"usgs":true,"family":"Bolgrien","given":"D.W.","affiliations":[],"preferred":false,"id":460627,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}} ,{"id":70037327,"text":"70037327 - 2010 - Analysis of solvent dyes in refined petroleum products by electrospray ionization mass spectrometry","interactions":[],"lastModifiedDate":"2018-10-09T10:41:44","indexId":"70037327","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1709,"text":"Fuel","active":true,"publicationSubtype":{"id":10}},"title":"Analysis of solvent dyes in refined petroleum products by electrospray ionization mass spectrometry","docAbstract":"Solvent dyes are used to color refined petroleum products to enable differentiation between gasoline, diesel, and jet fuels. Analysis for these dyes in the hydrocarbon product is difficult due to their very low concentrations in such a complex matrix. Flow injection analysis/electrospray ionization/mass spectrometry in both negative and positive mode was used to optimize ionization of ten typical solvent dyes. Samples of hydrocarbon product were analyzed under similar conditions. Positive electrospray ionization produced very complex spectra, which were not suitably specific for targeting only the dyes. Negative electrospray ionization produced simple spectra because aliphatic and aromatic moieties were not ionized. This enabled screening for a target dye in samples of hydrocarbon product from a spill.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Fuel","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.fuel.2009.09.011","issn":"00162361","usgsCitation":"Rostad, C.E., 2010, Analysis of solvent dyes in refined petroleum products by electrospray ionization mass spectrometry: Fuel, v. 89, no. 5, p. 997-1005, https://doi.org/10.1016/j.fuel.2009.09.011.","productDescription":"9p.","startPage":"997","endPage":"1005","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":244911,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":217002,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.fuel.2009.09.011"}],"volume":"89","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059eb31e4b0c8380cd48c97","contributors":{"authors":[{"text":"Rostad, Colleen E. cerostad@usgs.gov","contributorId":833,"corporation":false,"usgs":true,"family":"Rostad","given":"Colleen","email":"cerostad@usgs.gov","middleInitial":"E.","affiliations":[],"preferred":true,"id":460485,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70046632,"text":"ds587B - 2010 - National Land Cover Database 2001 (NLCD01) Imperviousness Layer Tile 2, Northeast United States: IMPV01_2","interactions":[],"lastModifiedDate":"2013-06-17T15:36:19","indexId":"ds587B","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":"587","chapter":"B","title":"National Land Cover Database 2001 (NLCD01) Imperviousness Layer Tile 2, Northeast United States: IMPV01_2","docAbstract":"This 30-meter resolution data set represents the imperviousness layer for the conterminous United States for the 2001 time period. The data have been arranged into four tiles to facilitate timely display and manipulation within a Geographic Information System, browse graphic: nlcd01-partition. The National Land Cover Data Set for 2001 was produced through a cooperative project conducted by the Multi-Resolution Land Characteristics (MRLC) Consortium. The MRLC Consortium is a partnership of Federal agencies (www.mrlc.gov), consisting of the U.S. Geological Survey (USGS), the National Oceanic and Atmospheric Administration (NOAA), the U.S. Environmental Protection Agency (USEPA), the U.S. Department of Agriculture (USDA), the U.S. Forest Service (USFS), the National Park Service (NPS), the U.S. Fish and Wildlife Service (USFWS), the Bureau of Land Management (BLM), and the USDA Natural Resources Conservation Service (NRCS). One of the primary goals of the project is to generate a current, consistent, seamless, and accurate National Land Cover Database (NLCD) circa 2001 for the United States at medium spatial resolution. For a detailed definition and discussion on MRLC and the NLCD 2001 products, refer to Homer and others (2004) and http://www.mrlc.gov/mrlc2k.asp.. The NLCD 2001 was created by partitioning the United States into mapping-zones. A total of 68 mapping-zones browse graphic: nlcd01-mappingzones.jpg were delineated within the conterminous United States based on ecoregion and geographical characteristics, edge-matching features, and the size requirement of Landsat mosaics. Mapping-zones encompass the whole or parts of several states. Questions about the NLCD mapping zones can be directed to the NLCD 2001 Land Cover Mapping Team at the USGS/EROS, Sioux Falls, SD (605) 594-6151 or mrlc@usgs.gov.","language":"English","publisher":"U.S. Geological Service","publisherLocation":"Reston, VA","doi":"10.3133/ds587B","usgsCitation":"LaMotte, A.E., and Wieczorek, M., 2010, National Land Cover Database 2001 (NLCD01) Imperviousness Layer Tile 2, Northeast United States: IMPV01_2 (Version 1): U.S. Geological Survey Data Series 587, Dataset, https://doi.org/10.3133/ds587B.","productDescription":"Dataset","onlineOnly":"Y","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":273859,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":273858,"type":{"id":16,"text":"Metadata"},"url":"https://water.usgs.gov/GIS/metadata/usgswrd/XML/impv01_2.xml"}],"country":"United States","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 98.612036,37.105324 ], [ 98.612036,51.857938 ], [ -65.143599,51.857938 ], [ -65.143599,37.105324 ], [ 98.612036,37.105324 ] ] ] } } ] }","edition":"Version 1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51c02ff2e4b0ee1529ed3d24","contributors":{"authors":[{"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":479907,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"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":479906,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70046761,"text":"dds49125 - 2010 - Attributes for MRB_E2RF1 Catchments by Major River Basins in the Conterminous United States: Surficial Geology","interactions":[],"lastModifiedDate":"2013-11-25T16:05:41","indexId":"dds49125","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":"491-25","title":"Attributes for MRB_E2RF1 Catchments by Major River Basins in the Conterminous United States: Surficial Geology","docAbstract":"This tabular data set represents the area of surficial geology types in square meters compiled for every MRB_E2RF1 catchment of selected Major River Basins (MRBs, Crawford and others, 2006). The source data set is the \"Digital data set describing surficial geology in the conterminous US\" (Clawges and Price, 1999).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, 2008). 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/dds49125","usgsCitation":"Wieczorek, M., and LaMotte, A.E., 2010, Attributes for MRB_E2RF1 Catchments by Major River Basins in the Conterminous United States: Surficial Geology: U.S. Geological Survey Data Series 491-25, Dataset, https://doi.org/10.3133/dds49125.","productDescription":"Dataset","onlineOnly":"Y","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":274422,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":274415,"type":{"id":16,"text":"Metadata"},"url":"https://water.usgs.gov/GIS/metadata/usgswrd/XML/mrb_e2rf1_sgeol.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":"51d3f663e4b09630fbdc5281","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":480179,"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":480180,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70037535,"text":"70037535 - 2010 - Numerical simulation of a low-lying barrier island's morphological response to Hurricane Katrina","interactions":[],"lastModifiedDate":"2012-03-12T17:22:05","indexId":"70037535","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1262,"text":"Coastal Engineering","active":true,"publicationSubtype":{"id":10}},"title":"Numerical simulation of a low-lying barrier island's morphological response to Hurricane Katrina","docAbstract":"Tropical cyclones that enter or form in the Gulf of Mexico generate storm surge and large waves that impact low-lying coastlines along the Gulf Coast. The Chandeleur Islands, located 161. km east of New Orleans, Louisiana, have endured numerous hurricanes that have passed nearby. Hurricane Katrina (landfall near Waveland MS, 29 Aug 2005) caused dramatic changes to the island elevation and shape. In this paper the predictability of hurricane-induced barrier island erosion and accretion is evaluated using a coupled hydrodynamic and morphodynamic model known as XBeach. Pre- and post-storm island topography was surveyed with an airborne lidar system. Numerical simulations utilized realistic surge and wave conditions determined from larger-scale hydrodynamic models. Simulations included model sensitivity tests with varying grid size and temporal resolutions. Model-predicted bathymetry/topography and post-storm survey data both showed similar patterns of island erosion, such as increased dissection by channels. However, the model under predicted the magnitude of erosion. Potential causes for under prediction include (1) errors in the initial conditions (the initial bathymetry/topography was measured three years prior to Katrina), (2) errors in the forcing conditions (a result of our omission of storms prior to Katrina and/or errors in Katrina storm conditions), and/or (3) physical processes that were omitted from the model (e.g., inclusion of sediment variations and bio-physical processes). ?? 2010.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Coastal Engineering","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.coastaleng.2010.06.004","issn":"03783839","usgsCitation":"Lindemer, C., Plant, N., Puleo, J., Thompson, D., and Wamsley, T., 2010, Numerical simulation of a low-lying barrier island's morphological response to Hurricane Katrina: Coastal Engineering, v. 57, no. 11-12, p. 985-995, https://doi.org/10.1016/j.coastaleng.2010.06.004.","startPage":"985","endPage":"995","numberOfPages":"11","costCenters":[],"links":[{"id":246008,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":218031,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.coastaleng.2010.06.004"}],"volume":"57","issue":"11-12","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a6906e4b0c8380cd73b1f","contributors":{"authors":[{"text":"Lindemer, C.A.","contributorId":11862,"corporation":false,"usgs":true,"family":"Lindemer","given":"C.A.","email":"","affiliations":[],"preferred":false,"id":461492,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Plant, N.G.","contributorId":94023,"corporation":false,"usgs":true,"family":"Plant","given":"N.G.","email":"","affiliations":[],"preferred":false,"id":461495,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Puleo, Jack A.","contributorId":108287,"corporation":false,"usgs":true,"family":"Puleo","given":"Jack A.","affiliations":[],"preferred":false,"id":461496,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Thompson, D.M.","contributorId":16570,"corporation":false,"usgs":true,"family":"Thompson","given":"D.M.","email":"","affiliations":[],"preferred":false,"id":461493,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Wamsley, T.V.","contributorId":60477,"corporation":false,"usgs":true,"family":"Wamsley","given":"T.V.","email":"","affiliations":[],"preferred":false,"id":461494,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":70037544,"text":"70037544 - 2010 - The Reimer Diatom Herbarium: An important resource for teaching and research","interactions":[],"lastModifiedDate":"2012-03-12T17:22:04","indexId":"70037544","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"The Reimer Diatom Herbarium: An important resource for teaching and research","docAbstract":"The Reimer Diatom Herbarium (ILH) at Iowa Lakeside Laboratory (ILL), a field station of Iowa's state universities, contains 3,280 permanent diatom slides of collections made from prairie potholes, alkaline fens, acid bogs, eutrophic lakes, saline lakes, Pleistocene paleolakes, and Miocene fossil deposits near ILL. The herbarium has a focus on collections made within Dickinson County, a region with an important legacy of study by students and visiting researchers from the US, Canada, and international institutions. The herbarium is well documented by taxon and location catalogues. The taxon card catalogue contains over 2,800 records referencing 67 genera, and the location card catalogue references collection sites from 51 counties in 16 North American states. Curated slides include over 300 species identifications made, or verified, by C.W. Reimer. Most curated slides have diatom specimens identified to species, circled with a diamond objective marker, and indicated on the slide label Six holotypes are included in the herbarium and we present the first light micrograph images of these type specimens. We present documentation of the contents and current condition of the herbarium and report that it is now available to researchers for scientific study. Many of the sites represented in the Reimer Diatom Herbarium are the same locations visited each year by students and visiting researchers at ILL, resulting in an important resource for monitoring environmental change, resolving taxonomic issues, and understanding species distributions in unique habitats.","largerWorkTitle":"Proceedings of the Academy of Natural Sciences of Philadelphia","language":"English","doi":"10.1635/053.160.0103","issn":"00973157","usgsCitation":"Rushforth, S., Edlund, M., Spaulding, S., and Stoermer, E.F., 2010, The Reimer Diatom Herbarium: An important resource for teaching and research, in Proceedings of the Academy of Natural Sciences of Philadelphia, v. 160, p. 13-20, https://doi.org/10.1635/053.160.0103.","startPage":"13","endPage":"20","numberOfPages":"8","costCenters":[],"links":[{"id":246067,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":218086,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1635/053.160.0103"}],"volume":"160","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505ba8b2e4b08c986b321dba","contributors":{"authors":[{"text":"Rushforth, S.J.","contributorId":20193,"corporation":false,"usgs":true,"family":"Rushforth","given":"S.J.","email":"","affiliations":[],"preferred":false,"id":461537,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Edlund, M.B.","contributorId":63644,"corporation":false,"usgs":true,"family":"Edlund","given":"M.B.","email":"","affiliations":[],"preferred":false,"id":461538,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Spaulding, S. 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This work was completed as part of the Master's thesis \"Turbidity Monitoring and LiDAR Imagery Indicate Landslides are Primary Source of Suspended-Sediment Load in the Little North Santiam River Basin, Oregon, Winter 2009-2010\" by Steven Sobieszczyk, Portland State University and U.S. Geological Survey. Data layers in this geodatabase include: landslide deposit boundaries (Deposits); field-verfied location imagery (Photos); head scarp or scarp flanks (Scarp_Flanks); and secondary scarp features (Scarps).The geodatabase template was developed by the Oregon Department of Geology and Mineral Industries (Burns and Madin, 2009).","language":"English","publisher":"U.S. Geological Service","publisherLocation":"Reston, VA","doi":"10.3133/70046643","usgsCitation":"Sobieszczyk, S., 2010, Top of head scarp and internal scarps for landslide deposits in the Little North Santiam River Basin, Oregon, Dataset, https://doi.org/10.3133/70046643.","productDescription":"Dataset","onlineOnly":"Y","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":273895,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":273894,"type":{"id":16,"text":"Metadata"},"url":"https://water.usgs.gov/GIS/metadata/usgswrd/XML/insantiam_LandslideInventory_Scarps.xml"}],"country":"United States","state":"Oregon","county":"Marion","otherGeospatial":"Little North Santiam River Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -122.582905,44.776225 ], [ -122.582905,44.894158 ], [ -122.135704,44.894158 ], [ -122.135704,44.776225 ], [ -122.582905,44.776225 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51c1816de4b0dd0e00d92219","contributors":{"authors":[{"text":"Sobieszczyk, Steven 0000-0002-0834-8437 ssobie@usgs.gov","orcid":"https://orcid.org/0000-0002-0834-8437","contributorId":885,"corporation":false,"usgs":true,"family":"Sobieszczyk","given":"Steven","email":"ssobie@usgs.gov","affiliations":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"preferred":true,"id":479922,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70034470,"text":"70034470 - 2010 - Arsenic in groundwater in the North Carolina Eastern slate belt (Esb): Nash and halifax counties, north carolina","interactions":[],"lastModifiedDate":"2016-11-30T11:27:36","indexId":"70034470","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3443,"text":"Southeastern Geology","active":true,"publicationSubtype":{"id":10}},"title":"Arsenic in groundwater in the North Carolina Eastern slate belt (Esb): Nash and halifax counties, north carolina","docAbstract":"Naturally occurring arsenic-contaminated groundwater is present within the Eastern Slate Belt (ESB) of North Carolina. Long-term, integrated geologic and geo-chemical investigations havedetermined the presence of arsenic by analyzing precipitates from first and second order streams under base flow conditions. When groundwater discharges into streams, arsenic and other metals are precipitated from solution, due to redox changes between the subsurface and surface environments. Analyses (As, base metals, Fe and Mn) were determined following chemical extraction ofnaturally occurring manganese-iron oxide-coatings, which had precipitated from solution onto stream-bed cobbles. Additionally, artificial redox fronts were produced by placing ceramic tilesin streambeds to collect and analyze oxide precipitates. Thermochemical plots from these data, as well as information from respective stream water measurements (pH and Eh), water sampling, and rock chemical analyses indicate mobile arsenic in predicted stability fields. Initial results show that naturally occurring arsenic-contaminated groundwater is present within the study area. However, the resulting oxidation and pre-cipitation within streams appreciably removes thiscontaminant from surface water solution.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Southeastern Geology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"00383678","usgsCitation":"Reid, J., Haven, W., Eudy, D., Milosh, R., and Stafford, E., 2010, Arsenic in groundwater in the North Carolina Eastern slate belt (Esb): Nash and halifax counties, north carolina: Southeastern Geology, v. 47, no. 3, p. 117-122.","startPage":"117","endPage":"122","numberOfPages":"6","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":244535,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"North Carolina","volume":"47","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059ed92e4b0c8380cd498b0","contributors":{"authors":[{"text":"Reid, J.C.","contributorId":61052,"corporation":false,"usgs":true,"family":"Reid","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":445974,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Haven, W.T.","contributorId":29668,"corporation":false,"usgs":true,"family":"Haven","given":"W.T.","affiliations":[],"preferred":false,"id":445972,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Eudy, D.D.","contributorId":28454,"corporation":false,"usgs":true,"family":"Eudy","given":"D.D.","email":"","affiliations":[],"preferred":false,"id":445971,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Milosh, R.M.","contributorId":100648,"corporation":false,"usgs":true,"family":"Milosh","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":445975,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Stafford, E.G.","contributorId":37172,"corporation":false,"usgs":true,"family":"Stafford","given":"E.G.","email":"","affiliations":[],"preferred":false,"id":445973,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":70046768,"text":"dds49128 - 2010 - Attributes for MRB_E2RF1 Catchments by Major River Basins in the Conterminous United States: Average Daily Maximum Temperature, 2002","interactions":[],"lastModifiedDate":"2013-11-25T16:06:07","indexId":"dds49128","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":"491-28","title":"Attributes for MRB_E2RF1 Catchments by Major River Basins in the Conterminous United States: Average Daily Maximum Temperature, 2002","docAbstract":"This tabular data set represents the average daily maximum temperature in Celsius multiplied by 100 for 2002, compiled for every MRB_E2RF1 catchment of selected Major River Basins (MRBs, Crawford and others, 2006). The source data were the Near-Real-Time High-Resolution Monthly Average Maximum/Minimum Temperature for the Conterminous United States for 2002 raster data set produced by the Spatial Climate Analysis Service at Oregon State University.\nThe MRB_E2RF1 catchments are based on a modified version of the 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, 2008). 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/dds49128","usgsCitation":"Wieczorek, M., and LaMotte, A.E., 2010, Attributes for MRB_E2RF1 Catchments by Major River Basins in the Conterminous United States: Average Daily Maximum Temperature, 2002: U.S. Geological Survey Data Series 491-28, Dataset, https://doi.org/10.3133/dds49128.","productDescription":"Dataset","onlineOnly":"Y","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":274437,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":274436,"type":{"id":16,"text":"Metadata"},"url":"https://water.usgs.gov/GIS/metadata/usgswrd/XML/mrb_e2rf1_tmax02.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":"51d3f662e4b09630fbdc5275","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":480195,"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":480196,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70046771,"text":"dds49131 - 2010 - Catchments by major river basins in the conterminous United States: 30-Year average daily minimum temperature, 1971-2000","interactions":[],"lastModifiedDate":"2024-09-25T17:02:12.262653","indexId":"dds49131","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":"491-31","title":"Catchments by major river basins in the conterminous United States: 30-Year average daily minimum temperature, 1971-2000","docAbstract":"This tabular data set represents thecatchment-average for the 30-year (1971-2000) average daily minimum temperature in Celsius multiplied by 100 compiled for every MRB_E2RF1 catchment of selected Major River Basins (MRBs, Crawford and others, 2006). The source data were the United States Average Monthly or Annual Minimum Temperature, 1971 - 2000 raster data set produced by the PRISM Group at Oregon State University. The MRB_E2RF1 catchments are based on a modified version of the 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/dds49131","usgsCitation":"Wieczorek, M., and LaMotte, A.E., 2010, Catchments by major river basins in the conterminous United States: 30-Year average daily minimum temperature, 1971-2000: U.S. Geological Survey Data Series 491-31, Dataset, https://doi.org/10.3133/dds49131.","productDescription":"Dataset","onlineOnly":"Y","additionalOnlineFiles":"N","costCenters":[{"id":374,"text":"Maryland Water Science 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]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51d3f663e4b09630fbdc5285","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":480201,"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":480202,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70046642,"text":"70046642 - 2010 - Location of photographs showing landslide features in the Little North Santiam River Basin, Oregon","interactions":[],"lastModifiedDate":"2013-06-18T09:00:14","indexId":"70046642","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Location of photographs showing landslide features in the Little North Santiam River Basin, Oregon","docAbstract":"Data points represent locations of photographs taken of landslides in the Little North Santiam River Basin, Oregon. Photos were taken in spring of 2010 during field verification of landslide locations (deposits previously mapped using LiDAR-derived imagery). The photographs depict various landslide features, such as scarps, pistol-butt trees, or colluvium deposits. This work was completed as part of the Master's thesis \"Turbidity Monitoring and LiDAR Imagery Indicate Landslides are Primary Source of Suspended-Sediment Load in the Little North Santiam River Basin, Oregon, Winter 2009-2010\" by Steven Sobieszczyk, Portland State University and U.S. Geological Survey. Data layers in this geodatabase include: landslide deposit boundaries (Deposits); field-verfied location imagery (Photos); head scarp or scarp flanks (Scarp_Flanks); and secondary scarp features (Scarps).The geodatabase template was developed by the Oregon Department of Geology and Mineral Industries (Burns and Madin, 2009).","language":"English","publisher":"U.S. Geological Service","publisherLocation":"Reston, VA","doi":"10.3133/70046642","usgsCitation":"Sobieszczyk, S., 2010, Location of photographs showing landslide features in the Little North Santiam River Basin, Oregon, Dataset, https://doi.org/10.3133/70046642.","productDescription":"Dataset","onlineOnly":"Y","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":273893,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":273891,"type":{"id":16,"text":"Metadata"},"url":"https://water.usgs.gov/GIS/metadata/usgswrd/XML/insantiam_LandslideInventory_Photos.xml"}],"country":"United States","state":"Oregon","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -122.561827,44.793310 ], [ -122.561827,44.866937 ], [ -122.233760,44.866937 ], [ -122.233760,44.793310 ], [ -122.561827,44.793310 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51c18169e4b0dd0e00d921e9","contributors":{"authors":[{"text":"Sobieszczyk, Steven 0000-0002-0834-8437 ssobie@usgs.gov","orcid":"https://orcid.org/0000-0002-0834-8437","contributorId":885,"corporation":false,"usgs":true,"family":"Sobieszczyk","given":"Steven","email":"ssobie@usgs.gov","affiliations":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"preferred":true,"id":479921,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70037468,"text":"70037468 - 2010 - Laboratory evaluation of a walleye (Sander vitreus) bioenergetics model","interactions":[],"lastModifiedDate":"2012-03-12T17:22:10","indexId":"70037468","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1651,"text":"Fish Physiology and Biochemistry","active":true,"publicationSubtype":{"id":10}},"title":"Laboratory evaluation of a walleye (Sander vitreus) bioenergetics model","docAbstract":"Walleye (Sander vitreus) is an important game fish throughout much of North America. We evaluated the performance of the Wisconsin bioenergetics model for walleye in the laboratory. Walleyes were fed rainbow smelt (Osmerus mordax) in four laboratory tanks during a 126-day experiment. Based on a statistical comparison of bioenergetics model predictions of monthly consumption with the observed monthly consumption, we concluded that the bioenergetics model significantly underestimated food consumption by walleye in the laboratory. The degree of underestimation appeared to depend on the feeding rate. For the tank with the lowest feeding rate (1.4% of walleye body weight per day), the agreement between the bioenergetics model prediction of cumulative consumption over the entire 126-day experiment and the observed cumulative consumption was remarkably close, as the prediction was within 0.1% of the observed cumulative consumption. Feeding rates in the other three tanks ranged from 1.6% to 1.7% of walleye body weight per day, and bioenergetics model predictions of cumulative consumption over the 126-day experiment ranged between 11 and 15% less than the observed cumulative consumption. ?? 2008 Springer Science+Business Media B.V.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Fish Physiology and Biochemistry","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1007/s10695-008-9278-2","issn":"09201742","usgsCitation":"Madenjian, C., Wang, C., O’Brien, T.P., Holuszko, M., Ogilvie, L., and Stickel, R., 2010, Laboratory evaluation of a walleye (Sander vitreus) bioenergetics model: Fish Physiology and Biochemistry, v. 36, no. 1, p. 45-53, https://doi.org/10.1007/s10695-008-9278-2.","startPage":"45","endPage":"53","numberOfPages":"9","costCenters":[],"links":[{"id":217036,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/s10695-008-9278-2"},{"id":244947,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"36","issue":"1","noUsgsAuthors":false,"publicationDate":"2008-11-02","publicationStatus":"PW","scienceBaseUri":"505a4109e4b0c8380cd65254","contributors":{"authors":[{"text":"Madenjian, C.P.","contributorId":64175,"corporation":false,"usgs":true,"family":"Madenjian","given":"C.P.","affiliations":[],"preferred":false,"id":461211,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wang, C.","contributorId":50689,"corporation":false,"usgs":true,"family":"Wang","given":"C.","email":"","affiliations":[],"preferred":false,"id":461209,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"O’Brien, T. P.","contributorId":22146,"corporation":false,"usgs":true,"family":"O’Brien","given":"T.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":461206,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Holuszko, M.J.","contributorId":35943,"corporation":false,"usgs":true,"family":"Holuszko","given":"M.J.","email":"","affiliations":[],"preferred":false,"id":461208,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Ogilvie, L.M.","contributorId":33682,"corporation":false,"usgs":true,"family":"Ogilvie","given":"L.M.","email":"","affiliations":[],"preferred":false,"id":461207,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Stickel, R.G.","contributorId":61229,"corporation":false,"usgs":true,"family":"Stickel","given":"R.G.","email":"","affiliations":[],"preferred":false,"id":461210,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}} ,{"id":70046639,"text":"70046639 - 2010 - Landslide deposit boundaries for the Little North Santiam River Basin, Oregon","interactions":[],"lastModifiedDate":"2013-06-18T08:29:34","indexId":"70046639","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Landslide deposit boundaries for the Little North Santiam River Basin, Oregon","docAbstract":"This layer is an inventory of existing landslides deposits in the Little North Santiam River Basin, Oregon (2009). Each landslide deposit shown on this map has been classified according to a number of specific characteristics identified at the time recorded in the GIS database. The classification scheme was developed by the Oregon Department of Geology and Mineral Industries (Burns and Madin, 2009). Several significant landslide characteristics recorded in the database are portrayed with symbology on this map. The specific characteristics shown for each landslide are the activity of landsliding, landslide features, deep or shallow failure, type of landslide movement, and confidence of landslide interpretation. These landslide characteristics are determined primarily on the basis of geomorphic features, or landforms, observed for each landslide. This work was completed as part of the Master's thesis \"Turbidity Monitoring and LiDAR Imagery Indicate Landslides are Primary Source of Suspended-Sediment Load in the Little North Santiam River Basin, Oregon, Winter 2009-2010\" by Steven Sobieszczyk, Portland State University and U.S. Geological Survey.Data layers in this geodatabase include: landslide deposit boundaries (Deposits); field-verfied location imagery (Photos); head scarp or scarp flanks (Scarp_Flanks); and secondary scarp features (Scarps).The geodatabase template was developed by the Oregon Department of Geology and Mineral Industries (Burns and Madin, 2009).","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70046639","usgsCitation":"Sobieszczyk, S., 2010, Landslide deposit boundaries for the Little North Santiam River Basin, Oregon, Dataset, https://doi.org/10.3133/70046639.","productDescription":"Dataset","onlineOnly":"Y","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":273886,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":273885,"type":{"id":16,"text":"Metadata"},"url":"https://water.usgs.gov/GIS/metadata/usgswrd/XML/insantiam_LandslideInventory_Deposits.xml"}],"country":"United States","state":"Oregon","county":"Marion","otherGeospatial":"Little North Santiam River Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -122.583361,44.776577 ], [ -122.583361,44.899782 ], [ -122.135924,44.899782 ], [ -122.135924,44.776577 ], [ -122.583361,44.776577 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51c18169e4b0dd0e00d921e5","contributors":{"authors":[{"text":"Sobieszczyk, Steven 0000-0002-0834-8437 ssobie@usgs.gov","orcid":"https://orcid.org/0000-0002-0834-8437","contributorId":885,"corporation":false,"usgs":true,"family":"Sobieszczyk","given":"Steven","email":"ssobie@usgs.gov","affiliations":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"preferred":true,"id":479917,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70037633,"text":"70037633 - 2010 - The Middle Jurassic basinal deposits of the Surmeh Formation in the Central Zagros Mountains, southwest Iran: Facies, sequence stratigraphy, and controls","interactions":[],"lastModifiedDate":"2012-03-12T17:22:06","indexId":"70037633","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1184,"text":"Carbonates and Evaporites","active":true,"publicationSubtype":{"id":10}},"title":"The Middle Jurassic basinal deposits of the Surmeh Formation in the Central Zagros Mountains, southwest Iran: Facies, sequence stratigraphy, and controls","docAbstract":"The lower part of the Lower to Upper Jurassic Surmeh Formation consists of a succession of shallow marine carbonates (Toarcian-Aalenian) overlain by a deep marine basinal succession (Aalenian-Bajocian) that grades upward to Middle to Upper Jurassic platform carbonates. The termination of shallow marine carbonate deposition of the lower part of the Surmeh Formation and the establishment of deep marine sedimentation indicate a change in the style of sedimentation in the Neotethys passive margin of southwest Iran during the Middle Jurassic. To evaluate the reasons for this change and to assess the basin configuration during the Middle Jurassic, this study focuses on facies analysis and sequence stratigraphy of the basinal deposits (pelagic and calciturbidite facies) of the Surmeh Formation, referred here as 'lower shaley unit' in the Central Zagros region. The upper Aalenian-Bajocian 'lower shaley unit' overlies, with an abrupt contact, the Toarcian-lower Aalenian platform carbonates. It consists of pelagic (calcareous shale and limestone) and calciturbidite facies grading to upper Bajocian-Bathonian platform carbonates. Calciturbidite deposits in the 'lower shaley unit' consist of various graded grainstone to lime mudstone facies containing mixed deep marine fauna and platform-derived material. These facies include quartz-bearing lithoclast/intraclast grainstone to lime mudstone, bioclast/ooid/peloid intraclast grainstone, ooid grainstone to packstone, and lime wackestone to mudstone. The calciturbidite layers are erosive-based and commonly exhibit graded bedding, incomplete Bouma turbidite sequence, flute casts, and load casts. They consist chiefly of platform-derived materials including ooids, intraclasts/lithoclasts, peloids, echinoderms, brachiopods, bivalves, and open-ocean biota, such as planktonic bivalves, crinoids, coccoliths, foraminifers, and sponge spicules. The 'lower shaley unit' constitutes the late transgressive and the main part of the highstand systems tract of a depositional sequence and grades upward to platform margin and platform interior facies as a result of late highstand basinward progradation. The sedimentary record of the 'lower shaley unit' in the Central Zagros region reveals the existence of a northwest-southeast trending platform margin during the Middle Jurassic that faced a deep basin, the 'Pars intrashelf basin' in the northeast. The thinning of calciturbidite layers towards the northeast and the widespread Middle Jurassic platform carbonates in the southern Persian Gulf states and in the Persian Gulf area support the existence of a southwest platform margin and platform interior source area. The platform margin was formed as a result of tectonic activity along the preexisting Mountain Front fault associated with Cimmerian continental rifting in northeast Gondwana. Flooding of the southwest platform margin during early to middle Bajocian resulted in the reestablishment of the carbonate sediment factory and overproduction of shallow marine carbonates associated with sea-level highstand, which led to vertical and lateral expansion of the platform and gradual infilling of the Pars intrashelf basin by late Bajocian time. ?? 2010 Springer-Verlag.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Carbonates and Evaporites","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1007/s13146-010-0032-3","issn":"08912556","usgsCitation":"Lasemi, Y., and Jalilian, A., 2010, The Middle Jurassic basinal deposits of the Surmeh Formation in the Central Zagros Mountains, southwest Iran: Facies, sequence stratigraphy, and controls: Carbonates and Evaporites, v. 25, no. 4, p. 283-295, https://doi.org/10.1007/s13146-010-0032-3.","startPage":"283","endPage":"295","numberOfPages":"13","costCenters":[],"links":[{"id":218037,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/s13146-010-0032-3"},{"id":246014,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"25","issue":"4","noUsgsAuthors":false,"publicationDate":"2010-09-14","publicationStatus":"PW","scienceBaseUri":"505ba7eee4b08c986b3218d0","contributors":{"authors":[{"text":"Lasemi, Y.","contributorId":70109,"corporation":false,"usgs":true,"family":"Lasemi","given":"Y.","email":"","affiliations":[],"preferred":false,"id":462015,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jalilian, A.H.","contributorId":92092,"corporation":false,"usgs":true,"family":"Jalilian","given":"A.H.","email":"","affiliations":[],"preferred":false,"id":462016,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70037287,"text":"70037287 - 2010 - Occurrence of avian Plasmodium and West Nile virus in culex species in Wisconsin","interactions":[],"lastModifiedDate":"2015-06-11T12:33:07","indexId":"70037287","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2522,"text":"Journal of the American Mosquito Control Association","active":true,"publicationSubtype":{"id":10}},"title":"Occurrence of avian Plasmodium and West Nile virus in culex species in Wisconsin","docAbstract":"The occurrence of multiple pathogens in mosquitoes and birds could affect the dynamics of disease transmission. We collected adult Culex pipiens and Cx. restuans (Cx. pipiens/restuans hereafter) from sites in Wisconsin and tested them for West Nile virus (WNV) and for avian malaria (Plasmodium). Gravid Cx. pipiens/restuans were tested for WNV using a commercial immunoassay, the RAMP?? WNV test, and positive results were verified by reverse transcriptasepolymerase chain reaction. There were 2 WNV-positive pools of Cx. pipiens/restuans in 2006 and 1 in 2007. Using a bias-corrected maximum likelihood estimation, the WNV infection rate for Cx. pipiens/restuans was 5.48/1,000 mosquitoes in 2006 and 1.08/1,000 mosquitoes in 2007. Gravid Cx. pipiens or Cx. restuans were tested individually for avian Plasmodium by a restriction enzymebased assay. Twelve mosquitoes were positive for avian Plasmodium (10.0), 2 were positive for Haemoproteus, and 3 were positive for Leucocytozoon. There were 4 mixed infections, with mosquitoes positive for >1 of the hemosporidian parasites. This work documents a high rate of hemosporidian infection in Culex spp. and illustrates the potential for co-infections with other arboviruses in bird-feeding mosquitoes and their avian hosts. In addition, hemosporidian infection rates may be a useful tool for investigating the ecological dynamics of Culex/avian interactions. ?? 2010 by The American Mosquito Control Association, Inc.
","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of the American Mosquito Control Association","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.2987/09-5893.1","issn":"8756971X","usgsCitation":"Hughes, T., Irwin, P., Hofmeister, E., and Paskewitz, S., 2010, Occurrence of avian Plasmodium and West Nile virus in culex species in Wisconsin: Journal of the American Mosquito Control Association, v. 26, no. 1, p. 24-31, https://doi.org/10.2987/09-5893.1.","startPage":"24","endPage":"31","numberOfPages":"8","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":245287,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":217343,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.2987/09-5893.1"}],"country":"United States","state":"Wisconsin","county":"Dane","city":"Madison","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"id\":\"3055\",\"properties\":{\"name\":\"Dane\",\"state\":\"WI\"},\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-89.0094,43.286],[-89.0084,43.2555],[-89.0094,43.2],[-89.01,43.1131],[-89.0109,43.0849],[-89.0107,43.0271],[-89.0132,42.9353],[-89.013,42.8762],[-89.0119,42.8471],[-89.132,42.8479],[-89.2488,42.8478],[-89.3689,42.8484],[-89.3688,42.8575],[-89.4832,42.858],[-89.6026,42.8575],[-89.7196,42.8587],[-89.8377,42.8598],[-89.8375,42.9471],[-89.8386,43.0317],[-89.8384,43.1181],[-89.8394,43.205],[-89.8325,43.2123],[-89.825,43.2187],[-89.8175,43.226],[-89.8125,43.2342],[-89.8088,43.2369],[-89.8012,43.2365],[-89.7874,43.2356],[-89.771,43.237],[-89.7579,43.2379],[-89.7529,43.2443],[-89.7485,43.2507],[-89.7391,43.2548],[-89.7259,43.2644],[-89.7171,43.2739],[-89.714,43.2821],[-89.7165,43.2867],[-89.7235,43.2935],[-89.7209,43.2935],[-89.6008,43.2932],[-89.4819,43.2942],[-89.3617,43.2954],[-89.3624,43.2832],[-89.246,43.2834],[-89.1271,43.2827],[-89.0094,43.286]]]}}]}","volume":"26","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a6bd2e4b0c8380cd748e7","contributors":{"authors":[{"text":"Hughes, T.","contributorId":64486,"corporation":false,"usgs":true,"family":"Hughes","given":"T.","email":"","affiliations":[],"preferred":false,"id":460284,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Irwin, P.","contributorId":94527,"corporation":false,"usgs":true,"family":"Irwin","given":"P.","email":"","affiliations":[],"preferred":false,"id":460286,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hofmeister, E.","contributorId":29556,"corporation":false,"usgs":true,"family":"Hofmeister","given":"E.","affiliations":[],"preferred":false,"id":460283,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Paskewitz, S.M.","contributorId":71802,"corporation":false,"usgs":true,"family":"Paskewitz","given":"S.M.","email":"","affiliations":[],"preferred":false,"id":460285,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70037348,"text":"70037348 - 2010 - Cassini spectra and photometry 0.25–5.1 μm of the small inner satellites of Saturn","interactions":[],"lastModifiedDate":"2015-03-23T13:21:43","indexId":"70037348","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1963,"text":"Icarus","active":true,"publicationSubtype":{"id":10}},"title":"Cassini spectra and photometry 0.25–5.1 μm of the small inner satellites of Saturn","docAbstract":"The nominal tour of the Cassini mission enabled the first spectra and solar phase curves of the small inner satellites of Saturn. We present spectra from the Visual Infrared Mapping Spectrometer (VIMS) and the Imaging Science Subsystem (ISS) that span the 0.25-5.1 ??m spectral range. The composition of Atlas, Pandora, Janus, Epimetheus, Calypso, and Telesto is primarily water ice, with a small amount (???5%) of contaminant, which most likely consists of hydrocarbons. The optical properties of the \"shepherd\" satellites and the coorbitals are tied to the A-ring, while those of the Tethys Lagrangians are tied to the E-ring of Saturn. The color of the satellites becomes progressively bluer with distance from Saturn, presumably from the increased influence of the E-ring; Telesto is as blue as Enceladus. Janus and Epimetheus have very similar spectra, although the latter appears to have a thicker coating of ring material. For at least four of the satellites, we find evidence for the spectral line at 0.68 ??m that Vilas et al. [Vilas, F., Larsen, S.M., Stockstill, K.R., Gaffley, M.J., 1996. Icarus 124, 262-267] attributed to hydrated iron minerals on Iapetus and Hyperion. However, it is difficult to produce a spectral mixing model that includes this component. We find no evidence for CO2 on any of the small satellites. There was a sufficient excursion in solar phase angle to create solar phase curves for Janus and Telesto. They bear a close similarity to the solar phase curves of the medium-sized inner icy satellites. Preliminary spectral modeling suggests that the contaminant on these bodies is not the same as the exogenously placed low-albedo material on Iapetus, but is rather a native material. The lack of CO2 on the small inner satellites also suggests that their low-albedo material is distinct from that on Iapetus, Phoebe, and Hyperion. ?? 2009 Elsevier Inc.","language":"English","publisher":"Elsevier","doi":"10.1016/j.icarus.2009.08.015","issn":"00191035","usgsCitation":"Buratti, B.J., Bauer, J., Hicks, M., Mosher, J.A., Filacchione, G., Momary, T., Baines, K.H., Brown, R.H., Clark, R.N., and Nicholson, P.D., 2010, Cassini spectra and photometry 0.25–5.1 μm of the small inner satellites of Saturn: Icarus, v. 206, no. 2, p. 524-536, https://doi.org/10.1016/j.icarus.2009.08.015.","productDescription":"13 p.","startPage":"524","endPage":"536","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":245227,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":217292,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.icarus.2009.08.015"}],"otherGeospatial":"Saturn","volume":"206","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f38fe4b0c8380cd4b8a5","contributors":{"authors":[{"text":"Buratti, B. J.","contributorId":69280,"corporation":false,"usgs":false,"family":"Buratti","given":"B.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":460574,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bauer, J.M.","contributorId":88543,"corporation":false,"usgs":true,"family":"Bauer","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":460575,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hicks, M.D.","contributorId":7045,"corporation":false,"usgs":true,"family":"Hicks","given":"M.D.","email":"","affiliations":[],"preferred":false,"id":460567,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Mosher, J. A.","contributorId":34605,"corporation":false,"usgs":false,"family":"Mosher","given":"J.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":460570,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Filacchione, G.","contributorId":48740,"corporation":false,"usgs":true,"family":"Filacchione","given":"G.","affiliations":[],"preferred":false,"id":460572,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Momary, T.","contributorId":17415,"corporation":false,"usgs":true,"family":"Momary","given":"T.","affiliations":[],"preferred":false,"id":460568,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Baines, K. H.","contributorId":37868,"corporation":false,"usgs":false,"family":"Baines","given":"K.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":460571,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Brown, R. H.","contributorId":19931,"corporation":false,"usgs":false,"family":"Brown","given":"R.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":460569,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Clark, R. N.","contributorId":6568,"corporation":false,"usgs":true,"family":"Clark","given":"R.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":460566,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Nicholson, P. D.","contributorId":54330,"corporation":false,"usgs":false,"family":"Nicholson","given":"P.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":460573,"contributorType":{"id":1,"text":"Authors"},"rank":10}]}} ,{"id":70037378,"text":"70037378 - 2010 - Repeated use of an abandoned vehicle by nesting Turkey vultures (Cathartes aura)","interactions":[],"lastModifiedDate":"2017-12-27T11:42:37","indexId":"70037378","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":"Repeated use of an abandoned vehicle by nesting Turkey vultures (Cathartes aura)","docAbstract":"Turkey Vultures (Cathartes aura) lay their eggs on an existing substrate in the dark recesses of a variety of natural sites (Kirk and Mossman 1998). Although an important requirement of Turkey Vulture nest-site selection is isolation from human disturbances (Kirk and Mossman 1998), their nests have been reported in abandoned buildings since at least the early 1800s (Nuttall 1832). Depopulation of rural areas in North America in recent decades has resulted in many abandoned buildings within the Turkey Vulture's breeding range (Peck 2003). Increased use of abandoned buildings by nesting Turkey Vultures has been implicated in the species' recent northward range expansion (Peck 2003, Nelson et al. 2005, Houston et al. 2007). Although abandoned or inoperative vehicles also are widespread in rural areas, we found no published literature documenting Turkey Vultures' use of these potential nest sites. Herein, we summarize the first documented incidence of a Turkey Vulture nesting in an abandoned vehicle.
","language":"English","publisher":"The Raptor Research Foundation","doi":"10.3356/JRR-09-02.1","issn":"08921016","usgsCitation":"Igl, L., and Peterson, S., 2010, Repeated use of an abandoned vehicle by nesting Turkey vultures (Cathartes aura): Journal of Raptor Research, v. 44, no. 1, p. 73-75, https://doi.org/10.3356/JRR-09-02.1.","productDescription":"3 p.","startPage":"73","endPage":"75","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":245196,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"South Dakota","county":"Butte County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-102.9587,45.2128],[-102.958,45.1251],[-102.9581,45.0388],[-102.9576,44.7781],[-102.9589,44.69],[-102.9653,44.6898],[-102.966,44.6036],[-103.1861,44.6039],[-103.2066,44.6039],[-103.3273,44.6042],[-103.4467,44.6053],[-103.5666,44.6044],[-103.8156,44.6048],[-103.8258,44.6023],[-103.8256,44.5982],[-103.8234,44.5937],[-103.8324,44.5939],[-103.8309,44.5889],[-103.8373,44.5888],[-103.8384,44.586],[-103.8417,44.5877],[-103.8464,44.5913],[-103.8533,44.5884],[-103.8567,44.5915],[-103.8641,44.5854],[-103.8702,44.5925],[-103.884,44.5985],[-103.8883,44.5952],[-103.8934,44.5942],[-103.8973,44.595],[-103.9018,44.5954],[-103.9061,44.5916],[-103.9053,44.5889],[-103.9105,44.5892],[-103.9144,44.59],[-103.9179,44.5849],[-103.9262,44.5838],[-103.9344,44.5799],[-103.9396,44.5812],[-103.9446,44.5783],[-103.9454,44.5819],[-103.9511,44.5808],[-103.9549,44.5789],[-103.9671,44.5791],[-103.9761,44.5811],[-103.9813,44.5814],[-103.983,44.5777],[-103.9997,44.5773],[-104.0183,44.5773],[-104.0229,44.5799],[-104.035,44.5782],[-104.0399,44.574],[-104.0457,44.5734],[-104.0564,44.5717],[-104.0571,44.9818],[-104.0571,44.9987],[-104.0397,44.9986],[-104.0399,45.0602],[-104.0402,45.1563],[-104.0403,45.169],[-104.0403,45.1774],[-104.0403,45.1832],[-104.0406,45.2143],[-104.0207,45.2144],[-103.9364,45.2133],[-103.8969,45.2134],[-103.8568,45.2135],[-103.8354,45.2136],[-103.814,45.2132],[-103.7751,45.2132],[-103.7545,45.2137],[-103.7117,45.2139],[-103.6916,45.2134],[-103.6709,45.2139],[-103.6515,45.2139],[-103.6301,45.2139],[-103.3257,45.2124],[-102.9587,45.2128]]]},\"properties\":{\"name\":\"Butte\",\"state\":\"SD\"}}]}","volume":"44","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505aa74de4b0c8380cd85335","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":460763,"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":460764,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70037573,"text":"70037573 - 2010 - Variations in coal characteristics and their possible implications for CO2 sequestration: Tanquary injection site, southeastern Illinois, USA","interactions":[],"lastModifiedDate":"2012-03-12T17:22:03","indexId":"70037573","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2033,"text":"International Journal of Coal Geology","active":true,"publicationSubtype":{"id":10}},"title":"Variations in coal characteristics and their possible implications for CO2 sequestration: Tanquary injection site, southeastern Illinois, USA","docAbstract":"As part of the U.S. Department of Energy's Regional Sequestration Partnership program, the potential for sequestering CO2 in the largest bituminous coal reserve in United States - the Illinois Basin - is being assessed at the Tanquary site in Wabash County, southeastern Illinois. To accomplish the main project objectives, which are to determine CO2 injection rates and storage capacity, we developed a detailed coal characterization program. The targeted Springfield Coal occurs at 274m (900ft) depth, is 2.1m (7ft) thick, and is of high volatile B bituminous rank, having an average vitrinite reflectance (Ro) of 0.63%. Desorbed Springfield Coal gas content in cores from four wells ~15 to ~30m (50 to 100ft) apart varies from 4.7-6.6cm3/g (150 to 210scf/ton, dmmf) and consists, generally, of >92% CH4 with lesser amounts of N2 and then CO2. Adsorption isotherms indicate that at least three molecules of CO2 can be stored for each displaced CH4 molecule. Whole seam petrographic composition, which affects sequestration potential, averages 76.5% vitrinite, 4.2% liptinite, 11.6% inertinite, and 7.7% mineral matter. Sulfur content averages 1.59%. Well-developed coal cleats with 1 to 2cm spacing contain partial calcite and/or kaolinite fillings that may decrease coal permeability. The shallow geophysical induction log curves show much higher resistivity in the lower part of the Springfield Coal than the medium or deep curves because of invasion by freshwater drilling fluid, possibly indicating higher permeability. Gamma-ray and bulk density vary, reflecting differences in maceral, ash, and pyrite content. Because coal properties vary across the basin, it is critical to characterize injection site coals to best predict the potential for CO2 injection and storage capacity. ?? 2010 Elsevier B.V.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"International Journal of Coal Geology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.coal.2010.08.001","issn":"01665162","usgsCitation":"Morse, D., Mastalerz, M., Drobniak, A., Rupp, J., and Harpalani, S., 2010, Variations in coal characteristics and their possible implications for CO2 sequestration: Tanquary injection site, southeastern Illinois, USA: International Journal of Coal Geology, v. 84, no. 1, p. 25-38, https://doi.org/10.1016/j.coal.2010.08.001.","startPage":"25","endPage":"38","numberOfPages":"14","costCenters":[],"links":[{"id":218047,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.coal.2010.08.001"},{"id":246027,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"84","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bc17be4b08c986b32a5c1","contributors":{"authors":[{"text":"Morse, D.G.","contributorId":45155,"corporation":false,"usgs":true,"family":"Morse","given":"D.G.","email":"","affiliations":[],"preferred":false,"id":461685,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mastalerz, Maria","contributorId":78065,"corporation":false,"usgs":true,"family":"Mastalerz","given":"Maria","affiliations":[],"preferred":false,"id":461686,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Drobniak, A.","contributorId":11748,"corporation":false,"usgs":true,"family":"Drobniak","given":"A.","affiliations":[],"preferred":false,"id":461683,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Rupp, J.A.","contributorId":30596,"corporation":false,"usgs":true,"family":"Rupp","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":461684,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Harpalani, S.","contributorId":10262,"corporation":false,"usgs":true,"family":"Harpalani","given":"S.","email":"","affiliations":[],"preferred":false,"id":461682,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":70037466,"text":"70037466 - 2010 - Control of one invasive plant species allows exotic grasses to become dominant in northern Great Plains grasslands","interactions":[],"lastModifiedDate":"2018-01-02T12:25:50","indexId":"70037466","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1015,"text":"Biological Conservation","active":true,"publicationSubtype":{"id":10}},"title":"Control of one invasive plant species allows exotic grasses to become dominant in northern Great Plains grasslands","docAbstract":"Decline of leafy spurge (Euphorbia esula) in the northern Great Plains of the US is generally viewed as a success story for biological control, but quality of the vegetation that survived the infestation is key to recovery of ecosystem function. In addition, effects of other invasive species, notably cool-season exotic grasses, must be taken into account. Objectives of this study were (1) to evaluate direction and significance of changes in biomass of native and exotic grasses, forbs, and leafy spurge and in plant species composition following control of leafy spurge by flea beetles and (2) to evaluate the relative effects of leafy spurge and exotic grasses on biomass of native grasses, biomass of forbs, and richness of native species. We monitored species composition (1998-2003 and 2008) and biomass (2000, 2002, 2003 and 2008) of these groups on spurge-infested and noninfested permanent plots at three sites with unbroken prairie sod in North Dakota, USA. We found little evidence, in terms of species richness or biomass of native grasses or forbs, that leafy spurge was being replaced by desirable native species, although desirable as well as weedy and exotic species were characteristic of 2008 vegetation at all three sites. Structural equation models revealed that leafy spurge had temporally intermittent negative effects on forb biomass and species richness, but no effects on native grasses. In contrast, exotic grass had consistently strong, negative effects on native grass biomass, as well as stronger negative effects than leafy spurge on native species richness. Although substantial native plant diversity remains at these sites, exotic grasses pose an important threat to these crucial building blocks of native prairie ecosystems. ?? 2010.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Biological Conservation","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.biocon.2010.04.045","issn":"00063207","usgsCitation":"Larson, D., and Larson, J., 2010, Control of one invasive plant species allows exotic grasses to become dominant in northern Great Plains grasslands: Biological Conservation, v. 143, no. 8, p. 1901-1910, https://doi.org/10.1016/j.biocon.2010.04.045.","productDescription":"10 p.","startPage":"1901","endPage":"1910","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":244919,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":217009,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.biocon.2010.04.045"}],"volume":"143","issue":"8","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059fb42e4b0c8380cd4ddac","contributors":{"authors":[{"text":"Larson, D.L. 0000-0001-5202-0634","orcid":"https://orcid.org/0000-0001-5202-0634","contributorId":69501,"corporation":false,"usgs":true,"family":"Larson","given":"D.L.","affiliations":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"preferred":false,"id":461204,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Larson, J.L.","contributorId":42549,"corporation":false,"usgs":true,"family":"Larson","given":"J.L.","email":"","affiliations":[],"preferred":false,"id":461203,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70037539,"text":"70037539 - 2010 - Fault-related clay authigenesis along the Moab Fault: Implications for calculations of fault rock composition and mechanical and hydrologic fault zone properties","interactions":[],"lastModifiedDate":"2012-03-12T17:22:05","indexId":"70037539","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2468,"text":"Journal of Structural Geology","active":true,"publicationSubtype":{"id":10}},"title":"Fault-related clay authigenesis along the Moab Fault: Implications for calculations of fault rock composition and mechanical and hydrologic fault zone properties","docAbstract":"The presence of clays in fault rocks influences both the mechanical and hydrologic properties of clay-bearing faults, and therefore it is critical to understand the origin of clays in fault rocks and their distributions is of great importance for defining fundamental properties of faults in the shallow crust. Field mapping shows that layers of clay gouge and shale smear are common along the Moab Fault, from exposures with throws ranging from 10 to ???1000 m. Elemental analyses of four locations along the Moab Fault show that fault rocks are enriched in clays at R191 and Bartlett Wash, but that this clay enrichment occurred at different times and was associated with different fluids. Fault rocks at Corral and Courthouse Canyons show little difference in elemental composition from adjacent protolith, suggesting that formation of fault rocks at those locations is governed by mechanical processes. Friction tests show that these authigenic clays result in fault zone weakening, and potentially influence the style of failure along the fault (seismogenic vs. aseismic) and potentially influence the amount of fluid loss associated with coseismic dilation. Scanning electron microscopy shows that authigenesis promotes that continuity of slip surfaces, thereby enhancing seal capacity. The occurrence of the authigenesis, and its influence on the sealing properties of faults, highlights the importance of determining the processes that control this phenomenon. ?? 2010 Elsevier Ltd.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Structural Geology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.jsg.2010.07.009","issn":"01918141","usgsCitation":"Solum, J., Davatzes, N., and Lockner, D., 2010, Fault-related clay authigenesis along the Moab Fault: Implications for calculations of fault rock composition and mechanical and hydrologic fault zone properties: Journal of Structural Geology, v. 32, no. 12, p. 1899-1911, https://doi.org/10.1016/j.jsg.2010.07.009.","startPage":"1899","endPage":"1911","numberOfPages":"13","costCenters":[],"links":[{"id":218059,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.jsg.2010.07.009"},{"id":246039,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"32","issue":"12","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0f20e4b0c8380cd537a5","contributors":{"authors":[{"text":"Solum, J.G.","contributorId":79280,"corporation":false,"usgs":true,"family":"Solum","given":"J.G.","email":"","affiliations":[],"preferred":false,"id":461508,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Davatzes, N.C.","contributorId":59219,"corporation":false,"usgs":true,"family":"Davatzes","given":"N.C.","email":"","affiliations":[],"preferred":false,"id":461507,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lockner, D.A. 0000-0001-8630-6833","orcid":"https://orcid.org/0000-0001-8630-6833","contributorId":85603,"corporation":false,"usgs":true,"family":"Lockner","given":"D.A.","affiliations":[],"preferred":false,"id":461509,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70046633,"text":"ds587C - 2010 - National Land Cover Database 2001 (NLCD01) Imperviousness Layer Tile 3, Southwest United States: IMPV01_3","interactions":[],"lastModifiedDate":"2013-06-17T15:45:18","indexId":"ds587C","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":"587","chapter":"C","title":"National Land Cover Database 2001 (NLCD01) Imperviousness Layer Tile 3, Southwest United States: IMPV01_3","docAbstract":"This 30-meter resolution data set represents the imperviousness layer for the conterminous United States for the 2001 time period. The data have been arranged into four tiles to facilitate timely display and manipulation within a Geographic Information System, browse graphic: nlcd01-partition. The National Land Cover Data Set for 2001 was produced through a cooperative project conducted by the Multi-Resolution Land Characteristics (MRLC) Consortium. The MRLC Consortium is a partnership of Federal agencies (www.mrlc.gov), consisting of the U.S. Geological Survey (USGS), the National Oceanic and Atmospheric Administration (NOAA), the U.S. Environmental Protection Agency (USEPA), the U.S. Department of Agriculture (USDA), the U.S. Forest Service (USFS), the National Park Service (NPS), the U.S. Fish and Wildlife Service (USFWS), the Bureau of Land Management (BLM), and the USDA Natural Resources Conservation Service (NRCS). One of the primary goals of the project is to generate a current, consistent, seamless, and accurate National Land Cover Database (NLCD) circa 2001 for the United States at medium spatial resolution. For a detailed definition and discussion on MRLC and the NLCD 2001 products, refer to Homer and others (2004) and http://www.mrlc.gov/mrlc2k.asp.. The NLCD 2001 was created by partitioning the United States into mapping-zones. A total of 68 mapping-zones browse graphic: nlcd01-mappingzones.jpg were delineated within the conterminous United States based on ecoregion and geographical characteristics, edge-matching features, and the size requirement of Landsat mosaics. Mapping-zones encompass the whole or parts of several states. 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