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,{"id":70102386,"text":"ofr20141079 - 2014 - Temporal changes in lithology and radiochemistry from the back-barrier environments along the Chandeleur Islands, Louisiana: March 2012-July 2013","interactions":[],"lastModifiedDate":"2025-05-13T16:59:51.385661","indexId":"ofr20141079","displayToPublicDate":"2014-10-20T16:27:00","publicationYear":"2014","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2014-1079","title":"Temporal changes in lithology and radiochemistry from the back-barrier environments along the Chandeleur Islands, Louisiana: March 2012-July 2013","docAbstract":"<P>Scientists from the U.S. Geological Survey, St. Petersburg Coastal and Marine Science Center conducted a time-series collection of shallow sediment cores from the back-barrier environments along the Chandeleur Islands, Louisiana from March 2012 through July 2013. The sampling efforts were part of a larger USGS study to evaluate effects on the geomorphology of the Chandeleur Islands following the construction of an artificial sand berm to reduce oil transport onto federally managed lands. The objective of this study was to evaluate the response of the back-barrier tidal and wetland environments to the berm.</P>\n<br/>\n<P>This report serves as an archive for sedimentological, radiochemical, and microbiological data derived from the sediment cores. Data are available for a time-series of four sampling periods: March 2012; July 2012; September 2012; and July 2013. Downloadable data are available as Excel spreadsheets and as JPEG files. Additional files include: ArcGIS shapefiles of the sampling sites, detailed results of sediment grain size analyses, and formal Federal Geographic Data Committee metadata.</P>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20141079","usgsCitation":"Marot, M.E., Adams, C., Richwine, K.A., Smith, C.G., Osterman, L.E., and Bernier, J., 2014, Temporal changes in lithology and radiochemistry from the back-barrier environments along the Chandeleur Islands, Louisiana: March 2012-July 2013: U.S. Geological Survey Open-File Report 2014-1079, HTML Document, https://doi.org/10.3133/ofr20141079.","productDescription":"HTML Document","onlineOnly":"Y","temporalStart":"2012-03-01","temporalEnd":"2013-07-31","ipdsId":"IP-053261","costCenters":[{"id":574,"text":"St. Petersburg Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":295507,"rank":3,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr20141079.JPG"},{"id":295483,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2014/1079"},{"id":295506,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2014/1079/html/ofr2014-1079_abstract.html"}],"country":"United States","state":"Louisiana","otherGeospatial":"Chandeleur Islands","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5446160be4b0f888a81b7f05","contributors":{"authors":[{"text":"Marot, Marci E. 0000-0003-0504-315X mmarot@usgs.gov","orcid":"https://orcid.org/0000-0003-0504-315X","contributorId":2078,"corporation":false,"usgs":true,"family":"Marot","given":"Marci","email":"mmarot@usgs.gov","middleInitial":"E.","affiliations":[{"id":574,"text":"St. Petersburg Coastal and Marine Science Center","active":true,"usgs":true},{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"preferred":true,"id":492967,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Adams, C. 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,{"id":70124042,"text":"ds878 - 2014 - Pharmaceutical compounds in shallow groundwater in non-agricultural areas of Minnesota: study design, methods, and data, 2013","interactions":[],"lastModifiedDate":"2014-10-21T09:31:38","indexId":"ds878","displayToPublicDate":"2014-10-20T16:09:00","publicationYear":"2014","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":"878","title":"Pharmaceutical compounds in shallow groundwater in non-agricultural areas of Minnesota: study design, methods, and data, 2013","docAbstract":"The U.S. Geological Survey, in cooperation with the Minnesota Pollution Control Agency, completed a study on the occurrence of pharmaceutical compounds and other contaminants of emerging concern in shallow groundwater in non-agricultural areas of Minnesota during 2013. This report describes the study design and methods for the study on the occurrence of pharmaceuticals and other contaminants of emerging concern, and presents the data collected on pharmaceutical compounds. Samples were analyzed by the U.S. Geological Survey National Water Quality Laboratory for 110 pharmaceutical compounds using research method 9017. Samples from 21 of 45 wells had detectable concentrations of at least one of the 110 compounds analyzed. One sample contained detectable concentrations of nine compounds, which was the most detected in a single sample. Fewer than five compounds were detected in most samples. Among all samples, 27 of the 110 compounds were detected in groundwater from at least one well. Desmethyldiltiazem and nicotine were the most frequently detected compounds, each detected in 5 of 46 environmental samples (one well was sampled twice so a total of 46 environmental samples were collected from 45 wells). Caffeine had the highest detectable concentration of all the compounds at 2,060 nanograms per liter.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ds878","collaboration":"Prepared in cooperation with the Minnesota Pollution Control Agency","usgsCitation":"Elliott, S.M., and Erickson, M., 2014, Pharmaceutical compounds in shallow groundwater in non-agricultural areas of Minnesota: study design, methods, and data, 2013: U.S. Geological Survey Data Series 878, Report: v, 11 p.; Table 4, https://doi.org/10.3133/ds878.","productDescription":"Report: v, 11 p.; Table 4","numberOfPages":"22","onlineOnly":"Y","temporalStart":"2013-04-01","temporalEnd":"2013-06-30","ipdsId":"IP-057550","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":295505,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ds878.jpg"},{"id":295503,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/ds/0878/"},{"id":295509,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/ds/0878/downloads/table4.xls"},{"id":295508,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/ds/0878/pdf/ds878.pdf"}],"scale":"24000","projection":"Universal Transverse Mercator projection","country":"United States","state":"Minnesota","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"54461609e4b0f888a81b7f03","contributors":{"authors":[{"text":"Elliott, Sarah M. 0000-0002-1414-3024 selliott@usgs.gov","orcid":"https://orcid.org/0000-0002-1414-3024","contributorId":1472,"corporation":false,"usgs":true,"family":"Elliott","given":"Sarah","email":"selliott@usgs.gov","middleInitial":"M.","affiliations":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"preferred":true,"id":500578,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Erickson, Melinda L. 0000-0002-1117-2866 merickso@usgs.gov","orcid":"https://orcid.org/0000-0002-1117-2866","contributorId":3671,"corporation":false,"usgs":true,"family":"Erickson","given":"Melinda L.","email":"merickso@usgs.gov","affiliations":[{"id":37947,"text":"Upper Midwest Water Science Center","active":true,"usgs":true},{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"preferred":true,"id":500579,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70128323,"text":"fs20143103 - 2014 - Changing Arctic ecosystems: resilience of caribou to climatic shifts in the Arctic","interactions":[],"lastModifiedDate":"2018-07-14T13:42:47","indexId":"fs20143103","displayToPublicDate":"2014-10-20T15:53:00","publicationYear":"2014","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2014-3103","title":"Changing Arctic ecosystems: resilience of caribou to climatic shifts in the Arctic","docAbstract":"The U.S. Geological Survey (USGS) Changing Arctic Ecosystems (CAE) initiative strives to inform key resource management decisions for Arctic Alaska by providing scientific information and forecasts for current and future ecosystem response to a warming climate. Over the past 5 years, a focal area for the USGS CAE initiative has been the North Slope of Alaska. This region has experienced a warming trend over the past 60 years, yet the rate of change has been varied across the North Slope, leading scientists to question the future response and resilience of wildlife populations, such as caribou (<I>Rangifer tarandus</I>), that rely on tundra habitats for forage. Future changes in temperature and precipitation to coastal wet sedge and upland low shrub tundra are expected, with unknown consequences for caribou that rely on these plant communities for food. Understanding how future environmental change may affect caribou migration, nutrition, and reproduction is a focal question being addressed by the USGS CAE research. Results will inform management agencies in Alaska and people that rely on caribou for food.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/fs20143103","usgsCitation":"Gustine, D.D., Adams, L., Whalen, M.E., and Pearce, J.M., 2014, Changing Arctic ecosystems: resilience of caribou to climatic shifts in the Arctic: U.S. Geological Survey Fact Sheet 2014-3103, 2 p., https://doi.org/10.3133/fs20143103.","productDescription":"2 p.","numberOfPages":"2","onlineOnly":"Y","ipdsId":"IP-059331","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":295502,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs20143103.JPG"},{"id":295487,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2014/3103/"},{"id":295501,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/2014/3103/pdf/fs2014-3103.pdf"}],"country":"United States","state":"Alaska","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"54461606e4b0f888a81b7f01","contributors":{"authors":[{"text":"Gustine, David D. dgustine@usgs.gov","contributorId":3776,"corporation":false,"usgs":true,"family":"Gustine","given":"David","email":"dgustine@usgs.gov","middleInitial":"D.","affiliations":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":117,"text":"Alaska Science Center Biology WTEB","active":true,"usgs":true}],"preferred":true,"id":502877,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Adams, Layne G. 0000-0001-6212-2896 ladams@usgs.gov","orcid":"https://orcid.org/0000-0001-6212-2896","contributorId":2776,"corporation":false,"usgs":true,"family":"Adams","given":"Layne G.","email":"ladams@usgs.gov","affiliations":[{"id":117,"text":"Alaska Science Center Biology WTEB","active":true,"usgs":true}],"preferred":true,"id":502876,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Whalen, Mary E. 0000-0003-2820-5158 mwhalen@usgs.gov","orcid":"https://orcid.org/0000-0003-2820-5158","contributorId":203717,"corporation":false,"usgs":true,"family":"Whalen","given":"Mary","email":"mwhalen@usgs.gov","middleInitial":"E.","affiliations":[{"id":117,"text":"Alaska Science Center Biology WTEB","active":true,"usgs":true}],"preferred":true,"id":502875,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Pearce, John M. 0000-0002-8503-5485 jpearce@usgs.gov","orcid":"https://orcid.org/0000-0002-8503-5485","contributorId":181766,"corporation":false,"usgs":true,"family":"Pearce","given":"John","email":"jpearce@usgs.gov","middleInitial":"M.","affiliations":[{"id":117,"text":"Alaska Science Center Biology WTEB","active":true,"usgs":true},{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"preferred":true,"id":502878,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70129645,"text":"70129645 - 2014 - The story of invasive algae, arginine, and turtle tumors does not make sense","interactions":[],"lastModifiedDate":"2017-05-08T12:00:20","indexId":"70129645","displayToPublicDate":"2014-10-20T13:37:00","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5387,"text":"PeerJ Preprints","active":true,"publicationSubtype":{"id":10}},"title":"The story of invasive algae, arginine, and turtle tumors does not make sense","docAbstract":"<p>We are presenting a rebuttal letter to the following article that appeared recently on PeerJ: Van Houtan KS, Smith CM, Dailer ML, and Kawachi M. 2014. Eutrophication and the dietary promotion of sea turtle tumors. PeerJ 2:e602. This article is available at the following URL: https://peerj.com/articles/602/. We argue that the article lacks an inferential framework to answer the complex question regarding the drivers of the turtle tumor disease fibropapillomatosis in Hawaii. The article also contains procedural flaws and does not provide any compelling evidence of a link between algae, arginine, and turtle tumors.</p>","language":"English","publisher":"PeerJ","publisherLocation":"Corte Madera, CA","doi":"10.7287/peerj.preprints.539v1","usgsCitation":"Work, T.M., Ackermann, M., Casey, J., Chaloupka, M., Herbst, L., Lynch, J.M., and Stacy, B.A., 2014, The story of invasive algae, arginine, and turtle tumors does not make sense: PeerJ Preprints, Article 2:e539v1; 4 p., https://doi.org/10.7287/peerj.preprints.539v1.","productDescription":"Article 2:e539v1; 4 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"links":[{"id":472689,"rank":0,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://doi.org/10.7287/peerj.preprints.539v1","text":"External Repository"},{"id":295735,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Hawaii","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"544b6a32e4b03653c63fb1eb","contributors":{"authors":[{"text":"Work, Thierry M. 0000-0002-4426-9090 thierry_work@usgs.gov","orcid":"https://orcid.org/0000-0002-4426-9090","contributorId":1187,"corporation":false,"usgs":true,"family":"Work","given":"Thierry","email":"thierry_work@usgs.gov","middleInitial":"M.","affiliations":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"preferred":true,"id":503932,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ackermann, Mathias","contributorId":67030,"corporation":false,"usgs":true,"family":"Ackermann","given":"Mathias","affiliations":[],"preferred":false,"id":503935,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Casey, James W.","contributorId":103606,"corporation":false,"usgs":true,"family":"Casey","given":"James W.","affiliations":[],"preferred":false,"id":503938,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Chaloupka, Milani","contributorId":96617,"corporation":false,"usgs":true,"family":"Chaloupka","given":"Milani","email":"","affiliations":[],"preferred":false,"id":503937,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Herbst, Lawrence","contributorId":32856,"corporation":false,"usgs":true,"family":"Herbst","given":"Lawrence","email":"","affiliations":[],"preferred":false,"id":503933,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Lynch, Jennifer M.","contributorId":58212,"corporation":false,"usgs":true,"family":"Lynch","given":"Jennifer","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":503934,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Stacy, Brian A.","contributorId":74698,"corporation":false,"usgs":true,"family":"Stacy","given":"Brian","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":503936,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70131477,"text":"70131477 - 2014 - Hyporheic flow and transport processes: mechanisms, models, and biogeochemical implications","interactions":[],"lastModifiedDate":"2015-02-02T14:38:01","indexId":"70131477","displayToPublicDate":"2014-10-20T00:00:00","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3283,"text":"Reviews of Geophysics","active":true,"publicationSubtype":{"id":10}},"title":"Hyporheic flow and transport processes: mechanisms, models, and biogeochemical implications","docAbstract":"<p>Fifty years of hyporheic zone research have shown the important role played by the hyporheic zone as an interface between groundwater and surface waters. However, it is only in the last two decades that what began as an empirical science has become a mechanistic science devoted to modeling studies of the complex fluid dynamical and biogeochemical mechanisms occurring in the hyporheic zone. These efforts have led to the picture of surface-subsurface water interactions as regulators of the form and function of fluvial ecosystems. Rather than being isolated systems, surface water bodies continuously interact with the subsurface. Exploration of hyporheic zone processes has led to a new appreciation of their wide reaching consequences for water quality and stream ecology. Modern research aims toward a unified approach, in which processes occurring in the hyporheic zone are key elements for the appreciation, management, and restoration of the whole river environment. In this unifying context, this review summarizes results from modeling studies and field observations about flow and transport processes in the hyporheic zone and describes the theories proposed in hydrology and fluid dynamics developed to quantitatively model and predict the hyporheic transport of water, heat, and dissolved and suspended compounds from sediment grain scale up to the watershed scale. The implications of these processes for stream biogeochemistry and ecology are also discussed.\"</p>","language":"English","publisher":"Wiley","doi":"10.1002/2012RG000417","usgsCitation":"Boano, F., Harvey, J.W., Marion, A., Packman, A.I., Revelli, R., Ridolfi, L., and Anders, W., 2014, Hyporheic flow and transport processes: mechanisms, models, and biogeochemical implications: Reviews of Geophysics, v. 52, no. 4, p. 603-679, https://doi.org/10.1002/2012RG000417.","productDescription":"77 p.","startPage":"603","endPage":"679","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-055545","costCenters":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"links":[{"id":296110,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"52","issue":"4","noUsgsAuthors":false,"publicationDate":"2014-10-20","publicationStatus":"PW","scienceBaseUri":"546727b9e4b04d4b7dbde860","chorus":{"doi":"10.1002/2012rg000417","url":"http://dx.doi.org/10.1002/2012rg000417","publisher":"Wiley-Blackwell","authors":"Boano F., Harvey J. W., Marion A., Packman A. I., Revelli R., Ridolfi L., Wörman A.","journalName":"Reviews of Geophysics","publicationDate":"10/20/2014","auditedOn":"7/27/2015"},"contributors":{"authors":[{"text":"Boano, Fulvio","contributorId":124515,"corporation":false,"usgs":false,"family":"Boano","given":"Fulvio","email":"","affiliations":[{"id":5039,"text":"Department of Environment, Land, and Infrastructure Engineering, Politecnico di Torino, Torino, Italy","active":true,"usgs":false}],"preferred":false,"id":521224,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Harvey, Judson W. 0000-0002-2654-9873 jwharvey@usgs.gov","orcid":"https://orcid.org/0000-0002-2654-9873","contributorId":1796,"corporation":false,"usgs":true,"family":"Harvey","given":"Judson","email":"jwharvey@usgs.gov","middleInitial":"W.","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":521223,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Marion, Andrea","contributorId":124516,"corporation":false,"usgs":false,"family":"Marion","given":"Andrea","email":"","affiliations":[{"id":5040,"text":"Department of Industrial Engineering, University of Padua, Padova, Italy","active":true,"usgs":false}],"preferred":false,"id":521225,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Packman, Aaron I.","contributorId":124517,"corporation":false,"usgs":false,"family":"Packman","given":"Aaron","email":"","middleInitial":"I.","affiliations":[{"id":5041,"text":"Department of Civil and Environmental Engineering, Northwestern University, Evanston, Illinois, USA","active":true,"usgs":false}],"preferred":false,"id":521226,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Revelli, Roberto","contributorId":124518,"corporation":false,"usgs":false,"family":"Revelli","given":"Roberto","email":"","affiliations":[{"id":5039,"text":"Department of Environment, Land, and Infrastructure Engineering, Politecnico di Torino, Torino, Italy","active":true,"usgs":false}],"preferred":false,"id":521227,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Ridolfi, Luca","contributorId":124519,"corporation":false,"usgs":false,"family":"Ridolfi","given":"Luca","email":"","affiliations":[{"id":5039,"text":"Department of Environment, Land, and Infrastructure Engineering, Politecnico di Torino, Torino, Italy","active":true,"usgs":false}],"preferred":false,"id":521228,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Anders, Worman","contributorId":124520,"corporation":false,"usgs":false,"family":"Anders","given":"Worman","email":"","affiliations":[{"id":5042,"text":"Division of River Engineering, Institute of Land and Water Resources Engineering, Royal Institute of Technology, Stockholm, Sweden","active":true,"usgs":false}],"preferred":false,"id":521229,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70168351,"text":"70168351 - 2014 - Potential population and assemblage influences of non-native trout on native nongame fish in Nebraska headwater streams","interactions":[],"lastModifiedDate":"2016-02-16T15:56:56","indexId":"70168351","displayToPublicDate":"2014-10-20T00:00:00","publicationYear":"2014","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":"Potential population and assemblage influences of non-native trout on native nongame fish in Nebraska headwater streams","docAbstract":"<p><span>Non-native trout are currently stocked to support recreational fisheries in headwater streams throughout Nebraska. The influence of non-native trout introductions on native fish populations and their role in structuring fish assemblages in these systems is unknown. The objectives of this study were to determine (i) if the size structure or relative abundance of native fish differs in the presence and absence of non-native trout, (ii) if native fish-assemblage structure differs in the presence and absence of non-native trout and (iii) if native fish-assemblage structure differs across a gradient in abundances of non-native trout. Longnose dace&nbsp;</span><i>Rhinichthys cataractae</i><span>&nbsp;were larger in the presence of brown trout&nbsp;</span><i>Salmo trutta</i><span>&nbsp;and smaller in the presence of rainbow trout&nbsp;</span><i>Oncorhynchus mykiss</i><span>&nbsp;compared to sites without trout. There was also a greater proportion of larger white suckers&nbsp;</span><i>Catostomus commersonii</i><span>&nbsp;in the presence of brown trout. Creek chub&nbsp;</span><i>Semotilus atromaculatus</i><span>&nbsp;and fathead minnow&nbsp;</span><i>Pimephales promelas</i><span>&nbsp;size structures were similar in the presence and absence of trout. Relative abundances of longnose dace, white sucker, creek chub and fathead minnow were similar in the presence and absence of trout, but there was greater distinction in native fish-assemblage structure between sites with trout compared to sites without trout as trout abundances increased. These results suggest increased risk to native fish assemblages in sites with high abundances of trout. However, more research is needed to determine the role of non-native trout in structuring native fish assemblages in streams, and the mechanisms through which introduced trout may influence native fish populations.</span></p>","language":"English","publisher":"Munksgaard","publisherLocation":"Copenhagen, Denmark","doi":"10.1111/eff.12194","usgsCitation":"Turek, K.C., Pegg, M.A., Pope, K.L., and Schainost, S., 2014, Potential population and assemblage influences of non-native trout on native nongame fish in Nebraska headwater streams: Ecology of Freshwater Fish, v. 25, no. 1, p. 99-108, https://doi.org/10.1111/eff.12194.","productDescription":"10 p.","startPage":"99","endPage":"108","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-056720","costCenters":[{"id":200,"text":"Coop Res Unit Seattle","active":true,"usgs":true}],"links":[{"id":318086,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Nebraska","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -104.0625,\n              43.004647127794435\n            ],\n            [\n              -98.54736328125,\n              42.97250158602597\n            ],\n            [\n              -98.02001953125,\n              42.73087427928485\n            ],\n            [\n              -97.66845703124999,\n              42.71473218539458\n            ],\n            [\n              -97.1630859375,\n              42.69858589169842\n            ],\n            [\n              -96.74560546875,\n              42.52069952914966\n            ],\n            [\n              -96.416015625,\n              42.32606244456202\n            ],\n            [\n              -96.30615234375,\n              42.147114459221015\n            ],\n            [\n              -96.13037109375,\n              41.77131167976407\n            ],\n            [\n              -102.0849609375,\n              41.02964338716638\n            ],\n            [\n              -102.919921875,\n              41.21172151054787\n            ],\n            [\n              -104.04052734375,\n              41.64007838467894\n            ],\n            [\n              -104.0625,\n              43.004647127794435\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"25","issue":"1","publishingServiceCenter":{"id":12,"text":"Tacoma PSC"},"noUsgsAuthors":false,"publicationDate":"2014-10-20","publicationStatus":"PW","scienceBaseUri":"56c45653e4b0946c6521859e","chorus":{"doi":"10.1111/eff.12194","url":"http://dx.doi.org/10.1111/eff.12194","publisher":"Wiley-Blackwell","authors":"Turek Kelly C., Pegg Mark A., Pope Kevin L., Schainost Steve","journalName":"Ecology of Freshwater Fish","publicationDate":"10/20/2014"},"contributors":{"authors":[{"text":"Turek, Kelly C.","contributorId":7603,"corporation":false,"usgs":true,"family":"Turek","given":"Kelly","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":619791,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pegg, Mark A.","contributorId":45212,"corporation":false,"usgs":true,"family":"Pegg","given":"Mark","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":620589,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Pope, Kevin L. 0000-0003-1876-1687 kpope@usgs.gov","orcid":"https://orcid.org/0000-0003-1876-1687","contributorId":1574,"corporation":false,"usgs":true,"family":"Pope","given":"Kevin","email":"kpope@usgs.gov","middleInitial":"L.","affiliations":[{"id":200,"text":"Coop Res Unit Seattle","active":true,"usgs":true}],"preferred":true,"id":620590,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Schainost, Steve","contributorId":166965,"corporation":false,"usgs":false,"family":"Schainost","given":"Steve","email":"","affiliations":[{"id":17640,"text":"Nebraska Game and Parks Commission","active":true,"usgs":false}],"preferred":false,"id":620591,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70129169,"text":"70129169 - 2014 - Editors are editors, not oracles","interactions":[],"lastModifiedDate":"2018-04-02T16:44:19","indexId":"70129169","displayToPublicDate":"2014-10-17T15:41:00","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1121,"text":"Bulletin of the Ecological Society of America","active":true,"publicationSubtype":{"id":10}},"title":"Editors are editors, not oracles","docAbstract":"<p><span>Farji-Brener and Kitzberger (2014; hereafter FBK) resurrect the issues of Farji-Brener (2007) concerning manuscripts that are submitted to journals but that are not sent out for peer review: a process we call “reject following editorial review” (RFER). We thank FBK for reviving discussion about this important topic as new challenges, including new publication outlets, peer-review models, and an increasingly complex and voluminous scientific literature, are emerging across the publication</span> <span>landscape. While we disagree with FBK's perspective and conclusions, we recognize that this discussion can help to improve editorial and publication processes, and we welcome the opportunity to inform the ecological community about the current status of editorial practice at ESA journals.</span></p>","language":"English","publisher":"Ecological Society of America","doi":"10.1890/0012-9623-95.4.342","usgsCitation":"Schimel, D., Strong, D., Ellison, A., Peters, D.P., Silver, S., Johnson, E.A., Belnap, J., Classen, A.T., Essington, T.E., Finley, A.O., Inouye, B.D., and Stanley, E.H., 2014, Editors are editors, not oracles: Bulletin of the Ecological Society of America, v. 95, no. 4, p. 342-346, https://doi.org/10.1890/0012-9623-95.4.342.","productDescription":"5 p.","startPage":"342","endPage":"346","ipdsId":"IP-058838","costCenters":[{"id":200,"text":"Coop Res Unit Seattle","active":true,"usgs":true}],"links":[{"id":472690,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1890/0012-9623-95.4.342","text":"Publisher Index Page"},{"id":295472,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"95","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"54422185e4b0192a5a42f3bd","contributors":{"authors":[{"text":"Schimel, Dave","contributorId":34069,"corporation":false,"usgs":true,"family":"Schimel","given":"Dave","email":"","affiliations":[],"preferred":false,"id":503491,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Strong, Donald R.","contributorId":17933,"corporation":false,"usgs":true,"family":"Strong","given":"Donald R.","affiliations":[],"preferred":false,"id":503490,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ellison, Aaron M.","contributorId":94996,"corporation":false,"usgs":true,"family":"Ellison","given":"Aaron M.","affiliations":[],"preferred":false,"id":503498,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Peters, Debra P. C.","contributorId":42903,"corporation":false,"usgs":true,"family":"Peters","given":"Debra","email":"","middleInitial":"P. C.","affiliations":[],"preferred":false,"id":503494,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Silver, Sue","contributorId":40145,"corporation":false,"usgs":true,"family":"Silver","given":"Sue","email":"","affiliations":[],"preferred":false,"id":503493,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Johnson, Edward A. ejohnson@usgs.gov","contributorId":50836,"corporation":false,"usgs":true,"family":"Johnson","given":"Edward","email":"ejohnson@usgs.gov","middleInitial":"A.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":503495,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Belnap, Jayne 0000-0001-7471-2279 jayne_belnap@usgs.gov","orcid":"https://orcid.org/0000-0001-7471-2279","contributorId":1332,"corporation":false,"usgs":true,"family":"Belnap","given":"Jayne","email":"jayne_belnap@usgs.gov","affiliations":[{"id":568,"text":"Southwest Biological Science Center","active":true,"usgs":true}],"preferred":true,"id":503489,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Classen, Aimee T.","contributorId":55366,"corporation":false,"usgs":true,"family":"Classen","given":"Aimee","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":503496,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Essington, Timothy E.","contributorId":95826,"corporation":false,"usgs":false,"family":"Essington","given":"Timothy","email":"","middleInitial":"E.","affiliations":[{"id":13190,"text":"School of Aquatic and Fishery Sciences, University of Washington","active":true,"usgs":false}],"preferred":false,"id":503500,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Finley, Andrew O.","contributorId":39310,"corporation":false,"usgs":true,"family":"Finley","given":"Andrew","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":503492,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Inouye, Brian D.","contributorId":95409,"corporation":false,"usgs":true,"family":"Inouye","given":"Brian","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":503499,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Stanley, Emily H.","contributorId":55725,"corporation":false,"usgs":false,"family":"Stanley","given":"Emily","email":"","middleInitial":"H.","affiliations":[{"id":12951,"text":"Center for Limnology, University of Wisconsin Madison","active":true,"usgs":false}],"preferred":false,"id":503497,"contributorType":{"id":1,"text":"Authors"},"rank":12}]}}
,{"id":70129159,"text":"70129159 - 2014 - Formation of fine sediment deposit from a flash flood river in the Mediterranean Sea","interactions":[],"lastModifiedDate":"2014-10-17T13:44:20","indexId":"70129159","displayToPublicDate":"2014-10-17T13:39:00","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2321,"text":"Journal of Geophysical Research: Oceans","active":true,"publicationSubtype":{"id":10}},"title":"Formation of fine sediment deposit from a flash flood river in the Mediterranean Sea","docAbstract":"We identify the mechanisms controlling fine deposits on the inner-shelf in front of the Besòs River, in the northwestern Mediterranean Sea. This river is characterized by a flash flood regime discharging large amounts of water (more than 20 times the mean water discharge) and sediment in very short periods lasting from hours to few days. Numerical model output was compared with bottom sediment observations and used to characterize the multiple spatial and temporal scales involved in offshore sediment deposit formation. A high-resolution (50 m grid size) coupled hydrodynamic-wave-sediment transport model was applied to the initial stages of the sediment dispersal after a storm-related flood event. After the flood, sediment accumulation was predominantly confined to an area near the coastline as a result of preferential deposition during the final stage of the storm. Subsequent reworking occurred due to wave-induced bottom shear stress that resuspended fine materials, with seaward flow exporting them toward the midshelf. Wave characteristics, sediment availability, and shelf circulation determined the transport after the reworking and the final sediment deposition location. One year simulations of the regional area revealed a prevalent southwestward average flow with increased intensity downstream. The circulation pattern was consistent with the observed fine deposit depocenter being shifted southward from the river mouth. At the southern edge, bathymetry controlled the fine deposition by inducing near-bottom flow convergence enhancing bottom shear stress. According to the short-term and long-term analyses, a seasonal pattern in the fine deposit formation is expected.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Geophysical Research: Oceans","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"American Geophysical Union","doi":"10.1002/2014JC010187","usgsCitation":"Grifoll, M., Gracia, V., Aretxabaleta, A.L., Guillen, J., Espino, M., and Warner, J., 2014, Formation of fine sediment deposit from a flash flood river in the Mediterranean Sea: Journal of Geophysical Research: Oceans, v. 119, no. 9, p. 5837-5853, https://doi.org/10.1002/2014JC010187.","productDescription":"17 p.","startPage":"5837","endPage":"5853","numberOfPages":"17","ipdsId":"IP-058276","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":472691,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1002/2014jc010187","text":"Publisher Index Page"},{"id":295463,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":295462,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1002/2014JC010187"}],"otherGeospatial":"Besòs River, Mediterranean Sea","volume":"119","issue":"9","noUsgsAuthors":false,"publicationDate":"2014-09-09","publicationStatus":"PW","scienceBaseUri":"5442218ce4b0192a5a42f3c1","contributors":{"authors":[{"text":"Grifoll, Manel","contributorId":21884,"corporation":false,"usgs":true,"family":"Grifoll","given":"Manel","email":"","affiliations":[],"preferred":false,"id":503472,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gracia, Vicenc","contributorId":85107,"corporation":false,"usgs":true,"family":"Gracia","given":"Vicenc","email":"","affiliations":[],"preferred":false,"id":503475,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Aretxabaleta, Alfredo L. 0000-0002-9914-8018 aaretxabaleta@usgs.gov","orcid":"https://orcid.org/0000-0002-9914-8018","contributorId":5464,"corporation":false,"usgs":true,"family":"Aretxabaleta","given":"Alfredo","email":"aaretxabaleta@usgs.gov","middleInitial":"L.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":503471,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Guillen, Jorge","contributorId":76671,"corporation":false,"usgs":true,"family":"Guillen","given":"Jorge","email":"","affiliations":[],"preferred":false,"id":503474,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Espino, Manuel","contributorId":34843,"corporation":false,"usgs":true,"family":"Espino","given":"Manuel","email":"","affiliations":[],"preferred":false,"id":503473,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Warner, John C. 0000-0002-3734-8903 jcwarner@usgs.gov","orcid":"https://orcid.org/0000-0002-3734-8903","contributorId":2681,"corporation":false,"usgs":true,"family":"Warner","given":"John C.","email":"jcwarner@usgs.gov","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":503470,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70129160,"text":"70129160 - 2014 - Evidence for seasonal patterns in the relative abundance of avian influenza virus subtypes in blue-winged teal (Anas discors)","interactions":[],"lastModifiedDate":"2018-09-04T16:37:19","indexId":"70129160","displayToPublicDate":"2014-10-17T13:19:00","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2507,"text":"Journal of Wildlife Diseases","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Evidence for seasonal patterns in the relative abundance of avian influenza virus subtypes in blue-winged teal (<i>Anas discors</i>)","title":"Evidence for seasonal patterns in the relative abundance of avian influenza virus subtypes in blue-winged teal (Anas discors)","docAbstract":"Seasonal dynamics of influenza A viruses (IAVs) are driven by host density and population immunity. Through an analysis of subtypic data for IAVs isolated from Blue-winged Teal (<i>Anas discors</i>), we present evidence for seasonal patterns in the relative abundance of viral subtypes in spring and summer/autumn.","language":"English","publisher":"Wildlife Disease Association","publisherLocation":"Ames, IA","doi":"10.7589/2013-09-232","usgsCitation":"Ramey, A.M., Poulson, R.L., González-Reiche, A., Wilcox, B.R., Walther, P., Link, P., Carter, D.L., Newsome, G.M., Muller, M.L., Berghaus, R.D., Perez, D.R., Hall, J.S., and Stallknecht, D.E., 2014, Evidence for seasonal patterns in the relative abundance of avian influenza virus subtypes in blue-winged teal (Anas discors): Journal of Wildlife Diseases, v. 50, no. 4, p. 916-922, https://doi.org/10.7589/2013-09-232.","productDescription":"7 p.","startPage":"916","endPage":"922","numberOfPages":"7","ipdsId":"IP-050911","costCenters":[{"id":117,"text":"Alaska Science Center Biology WTEB","active":true,"usgs":true},{"id":456,"text":"National 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USA.","active":true,"usgs":false}],"preferred":false,"id":503478,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Walther, Patrick","contributorId":42153,"corporation":false,"usgs":true,"family":"Walther","given":"Patrick","affiliations":[],"preferred":false,"id":503482,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Link, Paul","contributorId":22707,"corporation":false,"usgs":true,"family":"Link","given":"Paul","affiliations":[],"preferred":false,"id":503480,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Carter, Deborah L.","contributorId":87473,"corporation":false,"usgs":true,"family":"Carter","given":"Deborah","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":503488,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Newsome, George M.","contributorId":47311,"corporation":false,"usgs":true,"family":"Newsome","given":"George","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":503483,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Muller, Maria L.","contributorId":71911,"corporation":false,"usgs":true,"family":"Muller","given":"Maria","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":503487,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Berghaus, Roy D.","contributorId":47312,"corporation":false,"usgs":true,"family":"Berghaus","given":"Roy","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":503484,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Perez, Daniel R.","contributorId":58208,"corporation":false,"usgs":true,"family":"Perez","given":"Daniel","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":503485,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Hall, Jeffrey S. 0000-0001-5599-2826 jshall@usgs.gov","orcid":"https://orcid.org/0000-0001-5599-2826","contributorId":2254,"corporation":false,"usgs":true,"family":"Hall","given":"Jeffrey","email":"jshall@usgs.gov","middleInitial":"S.","affiliations":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"preferred":true,"id":503476,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Stallknecht, David E.","contributorId":14323,"corporation":false,"usgs":false,"family":"Stallknecht","given":"David","email":"","middleInitial":"E.","affiliations":[{"id":7125,"text":"Southeastern Cooperative Wildlife Disease Study, College of Veterinary Medicine, University of Georgia, Athens, GA 30602, USA.","active":true,"usgs":false}],"preferred":false,"id":503477,"contributorType":{"id":1,"text":"Authors"},"rank":13}]}}
,{"id":70129111,"text":"70129111 - 2014 - Radiocarbon age-offsets in an arctic lake reveal the long-term response of permafrost carbon to climate change","interactions":[],"lastModifiedDate":"2014-10-17T11:42:59","indexId":"70129111","displayToPublicDate":"2014-10-17T11:33:00","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2320,"text":"Journal of Geophysical Research: Biogeosciences","active":true,"publicationSubtype":{"id":10}},"title":"Radiocarbon age-offsets in an arctic lake reveal the long-term response of permafrost carbon to climate change","docAbstract":"Continued warming of the Arctic may cause permafrost to thaw and speed the decomposition of large stores of soil organic carbon (OC), thereby accentuating global warming. However, it is unclear if recent warming has raised the current rates of permafrost OC release to anomalous levels or to what extent soil carbon release is sensitive to climate forcing. Here we use a time series of radiocarbon age-offsets (<sup>14</sup>C) between the bulk lake sediment and plant macrofossils deposited in an arctic lake as an archive for soil and permafrost OC release over the last 14,500 years. The lake traps and archives OC imported from the watershed and allows us to test whether prior warming events stimulated old carbon release and heightened age-offsets. Today, the age-offset (2 ka; thousand of calibrated years before A.D. 1950) and the depositional rate of ancient OC from the watershed into the lake are relatively low and similar to those during the Younger Dryas cold interval (occurring 12.9–11.7 ka). In contrast, age-offsets were higher (3.0–5.0 ka) when summer air temperatures were warmer than present during the Holocene Thermal Maximum (11.7–9.0 ka) and Bølling-Allerød periods (14.5–12.9 ka). During these warm times, permafrost thaw contributed to ancient OC depositional rates that were ~10 times greater than today. Although permafrost OC was vulnerable to climate warming in the past, we suggest surface soil organic horizons and peat are presently limiting summer thaw and carbon release. As a result, the temperature threshold to trigger widespread permafrost OC release is higher than during previous warming events.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Geophysical Research: Biogeosciences","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"American Geophysical Union","doi":"10.1002/2014JG002688","usgsCitation":"Gaglioti, B.V., Mann, D., Jones, B.M., Pohlman, J., Kunz, M.L., and Wooller, M.J., 2014, Radiocarbon age-offsets in an arctic lake reveal the long-term response of permafrost carbon to climate change: Journal of Geophysical Research: Biogeosciences, v. 119, no. 8, p. 1630-1651, https://doi.org/10.1002/2014JG002688.","productDescription":"22 p.","startPage":"1630","endPage":"1651","numberOfPages":"22","ipdsId":"IP-056287","costCenters":[{"id":118,"text":"Alaska Science Center Geography","active":true,"usgs":true}],"links":[{"id":472692,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1002/2014jg002688","text":"Publisher Index Page"},{"id":295454,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":295450,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1002/2014JG002688"}],"country":"United States","state":"Alaska","volume":"119","issue":"8","noUsgsAuthors":false,"publicationDate":"2014-08-22","publicationStatus":"PW","scienceBaseUri":"5442218ce4b0192a5a42f3c3","contributors":{"authors":[{"text":"Gaglioti, Benjamin V. 0000-0003-0591-5253 bgaglioti@usgs.gov","orcid":"https://orcid.org/0000-0003-0591-5253","contributorId":4521,"corporation":false,"usgs":true,"family":"Gaglioti","given":"Benjamin","email":"bgaglioti@usgs.gov","middleInitial":"V.","affiliations":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":118,"text":"Alaska Science Center Geography","active":true,"usgs":true}],"preferred":true,"id":503434,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mann, Daniel H.","contributorId":97441,"corporation":false,"usgs":true,"family":"Mann","given":"Daniel H.","affiliations":[],"preferred":false,"id":503438,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Jones, Benjamin M. 0000-0002-1517-4711 bjones@usgs.gov","orcid":"https://orcid.org/0000-0002-1517-4711","contributorId":2286,"corporation":false,"usgs":true,"family":"Jones","given":"Benjamin","email":"bjones@usgs.gov","middleInitial":"M.","affiliations":[{"id":118,"text":"Alaska Science Center Geography","active":true,"usgs":true},{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"preferred":true,"id":503433,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Pohlman, John W.","contributorId":7642,"corporation":false,"usgs":true,"family":"Pohlman","given":"John W.","affiliations":[],"preferred":false,"id":503435,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Kunz, Michael L.","contributorId":42157,"corporation":false,"usgs":true,"family":"Kunz","given":"Michael","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":503436,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Wooller, Matthew J.","contributorId":81039,"corporation":false,"usgs":true,"family":"Wooller","given":"Matthew","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":503437,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70129102,"text":"70129102 - 2014 - Spatio-temporal analysis of gyres in oriented lakes on the Arctic Coastal Plain of northern Alaska based on remotely sensed images","interactions":[],"lastModifiedDate":"2014-10-17T10:33:42","indexId":"70129102","displayToPublicDate":"2014-10-17T10:23:00","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3250,"text":"Remote Sensing","active":true,"publicationSubtype":{"id":10}},"title":"Spatio-temporal analysis of gyres in oriented lakes on the Arctic Coastal Plain of northern Alaska based on remotely sensed images","docAbstract":"The formation of oriented thermokarst lakes on the Arctic Coastal Plain of northern Alaska has been the subject of debate for more than half a century. The striking elongation of the lakes perpendicular to the prevailing wind direction has led to the development of a preferred wind-generated gyre hypothesis, while other hypotheses include a combination of sun angle, topographic aspect, and/or antecedent conditions. A spatio-temporal analysis of oriented thermokarst lake gyres with recent (Landsat 8) and historical (Landsat 4, 5, 7 and ASTER) satellite imagery of the Arctic Coastal Plain of northern Alaska indicates that wind-generated gyres are both frequent and regionally extensive. Gyres are most common in lakes located near the Arctic coast after several days of sustained winds from a single direction, typically the northeast, and decrease in number landward with decreasing wind energy. This analysis indicates that the conditions necessary for the Carson and Hussey (1962) wind-generated gyre for oriented thermokarst lake formation are common temporally and regionally and correspond spatially with the geographic distribution of oriented lakes on the Arctic Coastal Plain. Given an increase in the ice-free season for lakes as well as strengthening of the wind regime, the frequency and distribution of lake gyres may increase. This increase has implications for changes in northern high latitude aquatic ecosystems, particularly if wind-generated gyres promote permafrost degradation and thermokarst lake expansion.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Remote Sensing","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"MDPI AG","publisherLocation":"Basel, Switzerland","doi":"10.3390/rs6109170","usgsCitation":"Zhan, S., Beck, R.A., Hinkel, K., Liu, H., and Jones, B.M., 2014, Spatio-temporal analysis of gyres in oriented lakes on the Arctic Coastal Plain of northern Alaska based on remotely sensed images: Remote Sensing, v. 6, no. 10, p. 9170-9193, https://doi.org/10.3390/rs6109170.","productDescription":"24 p.","startPage":"9170","endPage":"9193","numberOfPages":"24","ipdsId":"IP-058095","costCenters":[{"id":118,"text":"Alaska Science Center Geography","active":true,"usgs":true}],"links":[{"id":472693,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.3390/rs6109170","text":"Publisher Index Page"},{"id":295445,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":295441,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.3390/rs6109170"}],"country":"United States","state":"Alaska","otherGeospatial":"Arctic Coastal Plain","volume":"6","issue":"10","noUsgsAuthors":false,"publicationDate":"2014-09-26","publicationStatus":"PW","scienceBaseUri":"5442218ce4b0192a5a42f3c5","contributors":{"authors":[{"text":"Zhan, Shengan","contributorId":83855,"corporation":false,"usgs":true,"family":"Zhan","given":"Shengan","email":"","affiliations":[],"preferred":false,"id":503432,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Beck, Richard A.","contributorId":70316,"corporation":false,"usgs":true,"family":"Beck","given":"Richard","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":503431,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hinkel, Kenneth M.","contributorId":64170,"corporation":false,"usgs":true,"family":"Hinkel","given":"Kenneth M.","affiliations":[],"preferred":false,"id":503430,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Liu, Hongxing","contributorId":38075,"corporation":false,"usgs":true,"family":"Liu","given":"Hongxing","email":"","affiliations":[],"preferred":false,"id":503429,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Jones, Benjamin M. 0000-0002-1517-4711 bjones@usgs.gov","orcid":"https://orcid.org/0000-0002-1517-4711","contributorId":2286,"corporation":false,"usgs":true,"family":"Jones","given":"Benjamin","email":"bjones@usgs.gov","middleInitial":"M.","affiliations":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":118,"text":"Alaska Science Center Geography","active":true,"usgs":true}],"preferred":true,"id":503428,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70126210,"text":"ds882 - 2014 - Water temperature differences by plant community and location in re-established wetlands in the Sacramento-San Joaquin Delta, California, July 2005 to February 2008","interactions":[],"lastModifiedDate":"2014-10-17T08:14:08","indexId":"ds882","displayToPublicDate":"2014-10-16T16:44:00","publicationYear":"2014","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":"882","title":"Water temperature differences by plant community and location in re-established wetlands in the Sacramento-San Joaquin Delta, California, July 2005 to February 2008","docAbstract":"<p>Rates of carbon storage in wetlands are determined by the balance of its inputs and losses, both of which are affected by environmental factors such as water temperature and depth. In the autumn of 1997, the U.S. Geological Survey re-established two wetlands with different shallow water depths—about 25 and 55 centimeters deep—to investigate the potential to reverse subsidence of delta islands by preserving and accumulating organic substrates derived from plant biomass inputs over time. Because cooler water temperatures can slow decomposition rates and increase accretion of plant biomass, water temperature was recorded from July 2005 to February 2008 in the deeper of the two wetlands, where areas of emergent and submerged vegetation persisted throughout the study, to assess differences in water temperature between the two vegetation types. Water temperature was compared at three depths in the water column between areas of emergent and submerged vegetation and between areas near the water inflow and in the wetland interior in both vegetation types. The latter comparison was a way of evaluating the effect of the length of time water had resided in the wetland on water temperatures.</p>\n<br/>\n<p>There were statistically significant differences in water temperature at all depths between the two vegetation types. Overall, in areas of emergent marsh vegetation, the mean water temperature at the surface was 1.4 degrees Celsius (°C) less than it was in areas of submerged vegetation; however, when analyses accounted for the changes in temperature due to seasonal and diurnal cycles, differences in the mean water temperature between the vegetation types were even greater than this. For example, in the spring, the mean temperatures in areas of emergent marsh vegetation at the surface, mid-point, and near the sediment in the water column were 2.0, 2.3, and 2.1 °C less, respectively, than water temperatures in areas of submerged vegetation. When diurnal changes in temperature were accounted for by comparing temperatures in mid-afternoon (at 3 p.m.), water-temperature differences were even greater than the seasonal means indicated. In areas of emergent vegetation, the mean temperatures were cooler than temperatures in areas of submerged vegetation at the surface, the mid-point, and near the sediment in the water column by 3.9, 3.6, and 2.3 °C, respectively. Furthermore, from July 2005 through December 2006, water temperatures at the surface in the interior of the wetland were significantly cooler than in areas near the inflow supplying water from the San Joaquin River by 1.0 °C in areas of submerged vegetation and by 1.1 °C in areas of emergent vegetation.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ds882","collaboration":"Prepared in cooperation with the California Department of Water Resources","usgsCitation":"Crepeau, K.L., and Miller, R., 2014, Water temperature differences by plant community and location in re-established wetlands in the Sacramento-San Joaquin Delta, California, July 2005 to February 2008: U.S. Geological Survey Data Series 882, Report: vi, 20 p.; 1 Appendix, https://doi.org/10.3133/ds882.","productDescription":"Report: vi, 20 p.; 1 Appendix","numberOfPages":"30","onlineOnly":"Y","temporalStart":"2005-07-01","temporalEnd":"2008-02-29","ipdsId":"IP-036902","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"links":[{"id":295440,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ds882.jpg"},{"id":295437,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/ds/0882/"},{"id":295438,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/ds/0882/pdf/ds882.pdf"},{"id":295439,"type":{"id":3,"text":"Appendix"},"url":"https://pubs.usgs.gov/ds/0882/downloads/ds882_appendix01.xlsx"}],"projection":"Albers Equal-Area Conic projection","datum":"North American Datum of 1983","country":"United States","state":"California","otherGeospatial":"Sacramento-San Joaquin Delta","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5440d007e4b0b0a643c7329c","contributors":{"authors":[{"text":"Crepeau, Kathryn L. kcrepeau@usgs.gov","contributorId":3943,"corporation":false,"usgs":true,"family":"Crepeau","given":"Kathryn","email":"kcrepeau@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":true,"id":501933,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miller, Robin L. romiller@usgs.gov","contributorId":887,"corporation":false,"usgs":true,"family":"Miller","given":"Robin L.","email":"romiller@usgs.gov","affiliations":[],"preferred":true,"id":501932,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70122402,"text":"sir20145155 - 2014 - Water chemistry, seepage investigation, streamflow, reservoir storage, and annual availability of water for the San Juan-Chama Project, northern New Mexico, 1942-2010","interactions":[],"lastModifiedDate":"2014-10-16T13:14:25","indexId":"sir20145155","displayToPublicDate":"2014-10-16T13:06:00","publicationYear":"2014","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2014-5155","title":"Water chemistry, seepage investigation, streamflow, reservoir storage, and annual availability of water for the San Juan-Chama Project, northern New Mexico, 1942-2010","docAbstract":"<p>The Albuquerque Bernalillo County Water Utility Authority supplements the municipal water supply for the Albuquerque metropolitan area, in central New Mexico, with surface water diverted from the Rio Grande. The U.S. Geological Survey, in cooperation with the Albuquerque Bernalillo County Water Utility Authority, undertook this study in which water-chemistry data and historical streamflow were compiled and new water-chemistry data were collected to characterize the water chemistry and streamflow of the San Juan-Chama Project (SJCP). Characterization of streamflow included analysis of the variability of annual streamflow and comparison of the theoretical amount of water that could have been diverted into the SJCP to the actual amount of water that was diverted for the SJCP. Additionally, a seepage investigation was conducted along the channel between Azotea Tunnel Outlet and the streamflow-gaging station at Willow Creek above Heron Reservoir to estimate the magnitude of the gain or loss in streamflow resulting from groundwater interaction over the approximately 10-mile reach.</p>\n<br/>\n<p>Generally, surface-water chemistry varied with streamflow throughout the year. Streamflow ranged from high flow to low flow on the basis of the quantity of water diverted from the Rio Blanco, Little Navajo River, and Navajo River for the SJCP. Vertical profiles of the water temperature over the depth of the water column at Heron Reservoir indicated that the reservoir is seasonally stratified. The results from the seepage investigations indicated a small amount of loss of streamflow along the channel.</p>\n<br/>\n<p>Annual variability in streamflow for the SJCP was an indication of the variation in the climate parameters that interact to contribute to streamflow in the Rio Blanco, Little Navajo River, Navajo River, and Willow Creek watersheds. For most years, streamflow at Azotea Tunnel Outlet started in March and continued for approximately 3 months until the middle of July. The majority of annual streamflow at Azotea Tunnel Outlet occurred from May through June, with a median duration of slightly longer than a month. Years with higher maximum daily streamflow generally are associated with higher annual streamflow than years with lower maximum daily streamflow. The amount of water that can be diverted for the SJCP is controlled by the availability of streamflow and is limited by several factors including legal limits for diversion, limits from the SJCP infrastructure including the size of the diversion dams and tunnels, the capacity of Heron Reservoir, and operational constraints that limit when water can be diverted. The average annual streamflow at Azotea Tunnel Outlet was 94,710 acre-feet, and the annual streamflow at Azotea Tunnel Outlet was approximately 75 percent of the annual streamflow available for the SJCP. The average annual percentage of available streamflow not diverted for the SJCP was 14 percent because of structural limitations of the capacity of infrastructure, 1 percent because of limitations of the reservoir storage capacity, and 29 percent because of the limitations from operations. For most years, the annual available streamflow not diverted for unknown reasons exceeded the sum of the water not diverted because of structural, capacity, and operational limitations.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20145155","collaboration":"Prepared in cooperation with Albuquerque Bernalillo County Water Utility Authority","usgsCitation":"McKean, S.E., and Anderholm, S.K., 2014, Water chemistry, seepage investigation, streamflow, reservoir storage, and annual availability of water for the San Juan-Chama Project, northern New Mexico, 1942-2010: U.S. Geological Survey Scientific Investigations Report 2014-5155, Report: viii, 52 p.; 1 Appendix, https://doi.org/10.3133/sir20145155.","productDescription":"Report: viii, 52 p.; 1 Appendix","numberOfPages":"63","ipdsId":"IP-045511","costCenters":[{"id":472,"text":"New Mexico Water Science Center","active":true,"usgs":true}],"links":[{"id":295409,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/sir20145155.jpg"},{"id":295407,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/sir/2014/5155/pdf/sir2014-5155.pdf"},{"id":295406,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2014/5155/"},{"id":295408,"type":{"id":3,"text":"Appendix"},"url":"https://pubs.usgs.gov/sir/2014/5155/downloads/sir2014-5155_appendix_1.xlsx"}],"datum":"North American Datum of 1983","country":"United States","state":"Colorado, New Mexico","otherGeospatial":"San Juan-Chama","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5440d006e4b0b0a643c7329a","contributors":{"authors":[{"text":"McKean, Sarah E.","contributorId":92604,"corporation":false,"usgs":true,"family":"McKean","given":"Sarah","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":499511,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Anderholm, Scott K.","contributorId":69912,"corporation":false,"usgs":true,"family":"Anderholm","given":"Scott","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":499510,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70128987,"text":"70128987 - 2014 - Using surface creep rate to infer fraction locked for sections of the San Andreas fault system in northern California from alignment array and GPS data","interactions":[],"lastModifiedDate":"2014-12-12T15:01:45","indexId":"70128987","displayToPublicDate":"2014-10-16T10:23:00","publicationYear":"2014","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":"Using surface creep rate to infer fraction locked for sections of the San Andreas fault system in northern California from alignment array and GPS data","docAbstract":"<p>Surface creep rate, observed along five branches of the dextral San Andreas fault system in northern California, varies considerably from one section to the next, indicating that so too may the depth at which the faults are locked. We model locking on 29 fault sections using each section&rsquo;s mean long‐term creep rate and the consensus values of fault width and geologic slip rate. Surface creep rate observations from 111 short‐range alignment and trilateration arrays and 48 near‐fault, Global Positioning System station pairs are used to estimate depth of creep, assuming an elastic half‐space model and adjusting depth of creep iteratively by trial and error to match the creep observations along fault sections. Fault sections are delineated either by geometric discontinuities between them or by distinctly different creeping behaviors. We remove transient rate changes associated with five large (M&ge;5.5) regional earthquakes. Estimates of fraction locked, the ratio of moment accumulation rate to loading rate, on each section of the fault system provide a uniform means to inform source parameters relevant to seismic‐hazard assessment. From its mean creep rates, we infer the main branch (the San Andreas fault) ranges from only 20%&plusmn;10% locked on its central creeping section to 99%&ndash;100% on the north coast. From mean accumulation rates, we infer that four urban faults appear to have accumulated enough seismic moment to produce major earthquakes: the northern Calaveras (M 6.8), Hayward (M 6.8), Rodgers Creek (M 7.1), and Green Valley (M 7.1). The latter three faults are nearing or past their mean recurrence interval.</p>","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Bulletin of the Seismological Society of America","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Seismological Society of America","doi":"10.1785/0120140117","usgsCitation":"Lienkaemper, J.J., McFarland, F.S., Simpson, R.W., and Caskey, S., 2014, Using surface creep rate to infer fraction locked for sections of the San Andreas fault system in northern California from alignment array and GPS data: Bulletin of the Seismological Society of America, v. 104, no. 6, p. 3094-3114, https://doi.org/10.1785/0120140117.","productDescription":"21 p.","startPage":"3094","endPage":"3114","numberOfPages":"21","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-056497","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"links":[{"id":295379,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":295344,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1785/0120140117"}],"country":"United States","state":"California","otherGeospatial":"San Andreas fault system","volume":"104","issue":"6","noUsgsAuthors":false,"publicationDate":"2014-10-14","publicationStatus":"PW","scienceBaseUri":"5440d005e4b0b0a643c73298","contributors":{"authors":[{"text":"Lienkaemper, James J. 0000-0002-7578-7042 jlienk@usgs.gov","orcid":"https://orcid.org/0000-0002-7578-7042","contributorId":1941,"corporation":false,"usgs":true,"family":"Lienkaemper","given":"James","email":"jlienk@usgs.gov","middleInitial":"J.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":503253,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McFarland, Forrest S.","contributorId":32104,"corporation":false,"usgs":true,"family":"McFarland","given":"Forrest","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":503255,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Simpson, Robert W. simpson@usgs.gov","contributorId":1053,"corporation":false,"usgs":true,"family":"Simpson","given":"Robert","email":"simpson@usgs.gov","middleInitial":"W.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":503252,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Caskey, S. John","contributorId":21483,"corporation":false,"usgs":true,"family":"Caskey","given":"S. John","affiliations":[],"preferred":false,"id":503254,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70129338,"text":"70129338 - 2014 - Florfenicol residues in Rainbow Trout after oral dosing in recirculating and flow-through culture systems","interactions":[],"lastModifiedDate":"2014-10-21T10:25:08","indexId":"70129338","displayToPublicDate":"2014-10-16T10:22:49","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2177,"text":"Journal of Aquatic Animal Health","active":true,"publicationSubtype":{"id":10}},"title":"Florfenicol residues in Rainbow Trout after oral dosing in recirculating and flow-through culture systems","docAbstract":"Aquaflor is a feed premix for fish containing the broad spectrum antibacterial agent florfenicol (FFC) incorporated at a ratio of 50% (w/w). To enhance the effectiveness of FFC for salmonids infected with certain isolates of <i>Flavobacterium psychrophilum</i> causing coldwater disease, the FFC dose must be increased from the standard 10 mg·kg<sup>−1</sup> body weight (BW)·d<sup>−1</sup> for 10 consecutive days. A residue depletion study was conducted to determine whether FFC residues remaining in the fillet tissue after treating fish at an increased dose would be safe for human consumption. Groups of Rainbow Trout <i>Oncorhynchus mykiss</i> (total n = 144; weight range, 126–617 g) were treated with FFC at 20 mg·kg<sup>−1</sup> BW·d<sup>−1</sup> for 10 d in a flow-through system (FTS) and a recirculating aquaculture system (RAS) each with a water temperature of ∼13°C. The two-tank RAS included a nontreated tank containing 77 fish. Fish were taken from each tank (treated tank, <i>n</i> = 16; nontreated tank, <i>n</i> = 8) at 6, 12, 24, 48, 72, 120, 240, 360, and 480 h posttreatment. Florfenicol amine (FFA) concentrations (the FFC marker residue) in skin-on fillets from treated fish were greatest at 12 h posttreatment (11.58 μg/g) in the RAS and were greatest at 6 h posttreatment (11.09 μg/g) in the FTS. The half-lives for FFA in skin-on fillets from the RAS and FTS were 20.3 and 19.7 h, respectively. Assimilation of FFC residues in the fillets of nontreated fish sharing the RAS with FFC-treated fish was minimal. Florfenicol water concentrations peaked in the RAS-treated tank and nontreated tanks at 10 h (453 μg/L) and 11 h (442 μg/L) posttreatment, respectively. Monitoring of nitrite concentrations throughout the study indicated the nitrogen oxidation efficiency of the RAS biofilter was minimally impacted by the FFC treatment.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Aquatic Animal Health","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"American Fisheries Society","publisherLocation":"Bethesda, MD","doi":"10.1080/08997659.2014.945046","usgsCitation":"Meinertz, J.R., Hess, K., Bernady, J.A., Gaikowski, M., Whitsel, M., and Endris, R.G., 2014, Florfenicol residues in Rainbow Trout after oral dosing in recirculating and flow-through culture systems: Journal of Aquatic Animal Health, v. 26, no. 4, p. 243-250, https://doi.org/10.1080/08997659.2014.945046.","productDescription":"8 p.","startPage":"243","endPage":"250","numberOfPages":"8","ipdsId":"IP-051937","costCenters":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":295529,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":295499,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1080/08997659.2014.945046"},{"id":295500,"type":{"id":15,"text":"Index Page"},"url":"https://www.tandfonline.com/doi/full/10.1080/08997659.2014.945046#.VEVreU0cS70"}],"volume":"26","issue":"4","noUsgsAuthors":false,"publicationDate":"2014-10-16","publicationStatus":"PW","scienceBaseUri":"544775aee4b0f888a81b8316","contributors":{"authors":[{"text":"Meinertz, Jeffery R. 0000-0002-8855-2648 jmeinertz@usgs.gov","orcid":"https://orcid.org/0000-0002-8855-2648","contributorId":2495,"corporation":false,"usgs":true,"family":"Meinertz","given":"Jeffery","email":"jmeinertz@usgs.gov","middleInitial":"R.","affiliations":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"preferred":true,"id":503594,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hess, Karina R.","contributorId":97838,"corporation":false,"usgs":true,"family":"Hess","given":"Karina R.","affiliations":[],"preferred":false,"id":503599,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bernady, Jeffry A.","contributorId":33250,"corporation":false,"usgs":true,"family":"Bernady","given":"Jeffry","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":503596,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Gaikowski, M. P.","contributorId":11975,"corporation":false,"usgs":true,"family":"Gaikowski","given":"M. P.","affiliations":[],"preferred":false,"id":503595,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Whitsel, Melissa","contributorId":59370,"corporation":false,"usgs":true,"family":"Whitsel","given":"Melissa","affiliations":[],"preferred":false,"id":503598,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Endris, R. G.","contributorId":43291,"corporation":false,"usgs":true,"family":"Endris","given":"R.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":503597,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70129011,"text":"70129011 - 2014 - Investigation of hurricane Ivan using the coupled ocean-atmosphere-wave-sediment transport (COAWST) model","interactions":[],"lastModifiedDate":"2014-10-23T09:39:27","indexId":"70129011","displayToPublicDate":"2014-10-16T10:17:00","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2923,"text":"Ocean Dynamics","active":true,"publicationSubtype":{"id":10}},"title":"Investigation of hurricane Ivan using the coupled ocean-atmosphere-wave-sediment transport (COAWST) model","docAbstract":"The coupled ocean–atmosphere–wave–sediment transport (COAWST) model is used to hindcast Hurricane Ivan (2004), an extremely intense tropical cyclone (TC) translating through the Gulf of Mexico. Sensitivity experiments with increasing complexity in ocean–atmosphere–wave coupled exchange processes are performed to assess the impacts of coupling on the predictions of the atmosphere, ocean, and wave environments during the occurrence of a TC. Modest improvement in track but significant improvement in intensity are found when using the fully atmosphere–ocean-wave coupled configuration versus uncoupled (e.g., standalone atmosphere, ocean, or wave) model simulations. Surface wave fields generated in the fully coupled configuration also demonstrates good agreement with in situ buoy measurements. Coupled and uncoupled model-simulated sea surface temperature (SST) fields are compared with both in situ and remote observations. Detailed heat budget analysis reveals that the mixed layer temperature cooling in the deep ocean (on the shelf) is caused primarily by advection (equally by advection and diffusion).","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Ocean Dynamics","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Springer","doi":"10.1007/s10236-014-0777-7","usgsCitation":"Zambon, J.B., He, R., and Warner, J., 2014, Investigation of hurricane Ivan using the coupled ocean-atmosphere-wave-sediment transport (COAWST) model: Ocean Dynamics, v. 64, no. 11, p. 1535-1554, https://doi.org/10.1007/s10236-014-0777-7.","productDescription":"20 p.","startPage":"1535","endPage":"1554","numberOfPages":"20","ipdsId":"IP-051462","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":295375,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":295370,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/s10236-014-0777-7"}],"volume":"64","issue":"11","noUsgsAuthors":false,"publicationDate":"2014-10-12","publicationStatus":"PW","scienceBaseUri":"5440d005e4b0b0a643c73296","contributors":{"authors":[{"text":"Zambon, Joseph B.","contributorId":73522,"corporation":false,"usgs":true,"family":"Zambon","given":"Joseph","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":503307,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"He, Ruoying","contributorId":58965,"corporation":false,"usgs":true,"family":"He","given":"Ruoying","affiliations":[],"preferred":false,"id":503306,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Warner, John C. 0000-0002-3734-8903 jcwarner@usgs.gov","orcid":"https://orcid.org/0000-0002-3734-8903","contributorId":2681,"corporation":false,"usgs":true,"family":"Warner","given":"John C.","email":"jcwarner@usgs.gov","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":503305,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70135670,"text":"70135670 - 2014 - Alpha-emitting isotopes and chromium in a coastal California aquifer","interactions":[],"lastModifiedDate":"2015-11-30T12:48:22","indexId":"70135670","displayToPublicDate":"2014-10-16T06:30:00","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":835,"text":"Applied Geochemistry","active":true,"publicationSubtype":{"id":10}},"title":"Alpha-emitting isotopes and chromium in a coastal California aquifer","docAbstract":"<p><span>The unadjusted 72-h gross alpha activities in water from two wells completed in marine and alluvial deposits in a coastal southern California aquifer 40&nbsp;km north of San Diego were 15 and 25&nbsp;picoCuries per liter (pCi/L). Although activities were below the Maximum Contaminant Level (MCL) of 15&nbsp;pCi/L, when adjusted for uranium activity; there is concern that new wells in the area may exceed MCLs, or that future regulations may limit water use from the wells. Coupled well-bore flow and depth-dependent water-quality data collected from the wells in 2011 (with analyses for isotopes within the uranium, actinium, and thorium decay-chains) show gross alpha activity in marine deposits is associated with decay of naturally-occurring&nbsp;</span><sup>238</sup><span>U and its daughter&nbsp;</span><sup>234</sup><span>U. Radon activities in marine deposits were as high as 2230&nbsp;pCi/L. In contrast, gross alpha activities in overlying alluvium within the Piedra de Lumbre watershed, eroded from the nearby San Onofre Hills, were associated with decay of&nbsp;</span><sup>232</sup><span>Th, including its daughter&nbsp;</span><sup>224</sup><span>Ra. Radon activities in alluvium from Piedra de Lumbre of 450&nbsp;pCi/L were lower than in marine deposits. Chromium VI concentrations in marine deposits were less than the California MCL of 10&nbsp;&mu;g/L (effective July 1, 2014) but &delta;</span><sup>53</sup><span>Cr compositions were near zero and within reported ranges for anthropogenic chromium. Alluvial deposits from the nearby Las Flores watershed, which drains a larger area having diverse geology, has low alpha activities and chromium as a result of geologic and geochemical conditions and may be more promising for future water-supply development.</span></p>","language":"English","publisher":"Pergamon Press","publisherLocation":"Oxford, UK","doi":"10.1016/j.apgeochem.2014.09.016","usgsCitation":"Densmore, J.N., Izbicki, J., Murtaugh, J.M., Swarzenski, P.W., and Bullen, T.D., 2014, Alpha-emitting isotopes and chromium in a coastal California aquifer: Applied Geochemistry, v. 51, p. 204-215, https://doi.org/10.1016/j.apgeochem.2014.09.016.","productDescription":"12 p.","startPage":"204","endPage":"215","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-044867","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"links":[{"id":472694,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1016/j.apgeochem.2014.09.016","text":"Publisher Index Page"},{"id":311750,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Camp Pendleton","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -117.69653320312499,\n              33.128351191631566\n            ],\n            [\n              -117.69653320312499,\n              33.486435450999885\n            ],\n            [\n              -117.21725463867186,\n              33.486435450999885\n            ],\n            [\n              -117.21725463867186,\n              33.128351191631566\n            ],\n            [\n              -117.69653320312499,\n              33.128351191631566\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"51","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"565d813ae4b071e7ea54345a","contributors":{"authors":[{"text":"Densmore, Jill N. 0000-0002-5345-6613 jidensmo@usgs.gov","orcid":"https://orcid.org/0000-0002-5345-6613","contributorId":1474,"corporation":false,"usgs":true,"family":"Densmore","given":"Jill","email":"jidensmo@usgs.gov","middleInitial":"N.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":false,"id":536721,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Izbicki, John A. 0000-0003-0816-4408 jaizbick@usgs.gov","orcid":"https://orcid.org/0000-0003-0816-4408","contributorId":1375,"corporation":false,"usgs":true,"family":"Izbicki","given":"John A.","email":"jaizbick@usgs.gov","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":536720,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Murtaugh, Joseph M.","contributorId":150070,"corporation":false,"usgs":false,"family":"Murtaugh","given":"Joseph","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":580624,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Swarzenski, Peter W. 0000-0003-0116-0578 pswarzen@usgs.gov","orcid":"https://orcid.org/0000-0003-0116-0578","contributorId":1070,"corporation":false,"usgs":true,"family":"Swarzenski","given":"Peter","email":"pswarzen@usgs.gov","middleInitial":"W.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":580625,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Bullen, Thomas D. 0000-0003-2281-1691 tdbullen@usgs.gov","orcid":"https://orcid.org/0000-0003-2281-1691","contributorId":1969,"corporation":false,"usgs":true,"family":"Bullen","given":"Thomas","email":"tdbullen@usgs.gov","middleInitial":"D.","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":536722,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70129358,"text":"70129358 - 2014 - Scaling up watershed model parameters--Flow and load simulations of the Edisto River Basin","interactions":[],"lastModifiedDate":"2016-11-30T14:36:50","indexId":"70129358","displayToPublicDate":"2014-10-16T00:00:00","publicationYear":"2014","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Scaling up watershed model parameters--Flow and load simulations of the Edisto River Basin","docAbstract":"<p>The Edisto River is the longest and largest river system completely contained in South Carolina and is one of the longest free flowing blackwater rivers in the United States. The Edisto River basin also has fish-tissue mercury concentrations that are some of the highest recorded in the United States. As part of an effort by the U.S. Geological Survey to expand the understanding of relations among hydrologic, geochemical, and ecological processes that affect fish-tissue mercury concentrations within the Edisto River basin, analyses and simulations of the hydrology of the Edisto River basin were made with the topography-based hydrological model (TOPMODEL). The potential for scaling up a previous application of TOPMODEL for the McTier Creek watershed, which is a small headwater catchment to the Edisto River basin, was assessed. Scaling up was done in a step-wise process beginning with applying the calibration parameters, meteorological data, and topographic wetness index data from the McTier Creek TOPMODEL to the Edisto River TOPMODEL. Additional changes were made with subsequent simulations culminating in the best simulation, which included meteorological and topographic wetness index data from the Edisto River basin and updated calibration parameters for some of the TOPMODEL calibration parameters. Comparison of goodness-of-fit statistics between measured and simulated daily mean streamflow for the two models showed that with calibration, the Edisto River TOPMODEL produced slightly better results than the McTier Creek model, despite the significant difference in the drainage-area size at the outlet locations for the two models (30.7 and 2,725 square miles, respectively). Along with the TOPMODEL hydrologic simulations, a visualization tool (the Edisto River Data Viewer) was developed to help assess trends and influencing variables in the stream ecosystem. Incorporated into the visualization tool were the water-quality load models TOPLOAD, TOPLOAD-H, and LOADEST. Because the focus of this investigation was on scaling up the models from McTier Creek, water-quality concentrations that were previously collected in the McTier Creek basin were used in the water-quality load models.</p>","largerWorkType":{"id":24,"text":"Conference Paper"},"largerWorkTitle":"Proceedings of the 2014 South Carolina Water Resources Conference","conferenceTitle":"2014 South Carolina Water Resources Conference","conferenceDate":"October 15-16, 2014","conferenceLocation":"Columbia, South Carolina","language":"English","usgsCitation":"Feaster, T., Benedict, S., Clark, J.M., Bradley, P.M., and Conrads, P., 2014, Scaling up watershed model parameters--Flow and load simulations of the Edisto River Basin, <i>in</i> Proceedings of the 2014 South Carolina Water Resources Conference, Columbia, South Carolina, October 15-16, 2014, 4 p.","productDescription":"4 p.","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-059324","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":311630,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"South Carolina","otherGeospatial":"Edisto River basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -80.45700073242188,\n              32.505129231918936\n            ],\n            [\n              -80.51742553710938,\n              32.986779893387755\n            ],\n            [\n              -81.54190063476562,\n              33.52536850360117\n            ],\n            [\n              -81.52130126953125,\n              33.74147082163694\n            ],\n            [\n              -81.474609375,\n              33.81452532651738\n            ],\n           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jmclark@usgs.gov","orcid":"https://orcid.org/0000-0002-3138-5738","contributorId":4773,"corporation":false,"usgs":true,"family":"Clark","given":"Jimmy","email":"jmclark@usgs.gov","middleInitial":"M.","affiliations":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true},{"id":559,"text":"South Carolina Water Science Center","active":true,"usgs":true}],"preferred":true,"id":519855,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bradley, Paul M. 0000-0001-7522-8606 pbradley@usgs.gov","orcid":"https://orcid.org/0000-0001-7522-8606","contributorId":361,"corporation":false,"usgs":true,"family":"Bradley","given":"Paul","email":"pbradley@usgs.gov","middleInitial":"M.","affiliations":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"preferred":true,"id":519851,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Conrads, Paul 0000-0003-0408-4208 pconrads@usgs.gov","orcid":"https://orcid.org/0000-0003-0408-4208","contributorId":764,"corporation":false,"usgs":true,"family":"Conrads","given":"Paul","email":"pconrads@usgs.gov","affiliations":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true},{"id":559,"text":"South Carolina Water Science Center","active":true,"usgs":true}],"preferred":false,"id":519852,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70126737,"text":"70126737 - 2014 - USGS National Wildlife Health Center quarterly wildlife mortality report","interactions":[],"lastModifiedDate":"2023-10-13T14:31:02.752658","indexId":"70126737","displayToPublicDate":"2014-10-15T12:00:00","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3769,"text":"Wildlife Disease Association Newsletter","active":true,"publicationSubtype":{"id":10}},"title":"USGS National Wildlife Health Center quarterly wildlife mortality report","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Wildlife Disease Association","usgsCitation":"Ballmann, A.E., Bodenstein, B.L., Dusek, R., and Chipault, J.G., 2014, USGS National Wildlife Health Center quarterly wildlife mortality report: Wildlife Disease Association Newsletter, no. October 2014, p. 8-9.","productDescription":"2 p.","startPage":"8","endPage":"9","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-059742","costCenters":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"links":[{"id":295338,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://www.wildlifedisease.org/PersonifyEbusiness/Resources/Publications/Newsletter/Archive"},{"id":295339,"rank":2,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -180.17578125,\n              17.14079039331665\n            ],\n            [\n              -180.17578125,\n              72.71190310803662\n            ],\n            [\n              -65.7421875,\n              72.71190310803662\n            ],\n            [\n              -65.7421875,\n              17.14079039331665\n            ],\n            [\n              -180.17578125,\n              17.14079039331665\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","issue":"October 2014","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"543f7e94e4b065f4ad22cf7d","contributors":{"authors":[{"text":"Ballmann, Anne E. 0000-0002-0380-056X aballmann@usgs.gov","orcid":"https://orcid.org/0000-0002-0380-056X","contributorId":1153,"corporation":false,"usgs":true,"family":"Ballmann","given":"Anne","email":"aballmann@usgs.gov","middleInitial":"E.","affiliations":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"preferred":false,"id":502142,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bodenstein, Barbara L. 0000-0001-7946-0103 bbodenstein@usgs.gov","orcid":"https://orcid.org/0000-0001-7946-0103","contributorId":4389,"corporation":false,"usgs":true,"family":"Bodenstein","given":"Barbara","email":"bbodenstein@usgs.gov","middleInitial":"L.","affiliations":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"preferred":true,"id":502140,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dusek, Robert J. 0000-0001-6177-7479 rdusek@usgs.gov","orcid":"https://orcid.org/0000-0001-6177-7479","contributorId":140066,"corporation":false,"usgs":true,"family":"Dusek","given":"Robert J.","email":"rdusek@usgs.gov","affiliations":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"preferred":false,"id":502141,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Chipault, Jennifer G. 0000-0002-1368-622X jchipault@usgs.gov","orcid":"https://orcid.org/0000-0002-1368-622X","contributorId":4765,"corporation":false,"usgs":true,"family":"Chipault","given":"Jennifer","email":"jchipault@usgs.gov","middleInitial":"G.","affiliations":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"preferred":false,"id":502143,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70128836,"text":"70128836 - 2014 - Evidence for large-magnitude, post-Eocene extension in the northern Shoshone Range, Nevada, and its implications for Carlin-type gold deposits in the lower plate of the Roberts Mountains allochthon","interactions":[],"lastModifiedDate":"2014-10-15T09:07:29","indexId":"70128836","displayToPublicDate":"2014-10-15T09:02:00","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"Evidence for large-magnitude, post-Eocene extension in the northern Shoshone Range, Nevada, and its implications for Carlin-type gold deposits in the lower plate of the Roberts Mountains allochthon","docAbstract":"<p>The northern Shoshone and Toiyabe Ranges in north-central Nevada expose numerous areas of mineralized Paleozoic rock, including major Carlin-type gold deposits at Pipeline and Cortez. Paleozoic rocks in these areas were previously interpreted to have undergone negligible postmineralization extension and tilting, but here we present new data that suggest major post-Eocene extension along west-dipping normal faults. Tertiary rocks in the northern Shoshone Range crop out in two W-NW–trending belts that locally overlie and intrude highly deformed Lower Paleozoic rocks of the Roberts Mountains allochthon. Tertiary exposures in the more extensive, northern belt were interpreted as subvertical breccia pipes (intrusions), but new field data indicate that these “pipes” consist of a 35.8 Ma densely welded dacitic ash flow tuff (informally named the tuff of Mount Lewis) interbedded with sandstones and coarse volcaniclastic deposits. Both tuff and sedimentary rocks strike N-S and dip 30° to 70° E; the steeply dipping compaction foliation in the tuffs was interpreted as subvertical flow foliation in breccia pipes. The southern belt along Mill Creek, previously mapped as undivided welded tuff, includes the tuff of Cove mine (34.4 Ma) and unit B of the Bates Mountain Tuff (30.6 Ma). These tuffs dip 30° to 50° east, suggesting that their west-dipping contacts with underlying Paleozoic rocks (previously mapped as depositional) are normal faults. Tertiary rocks in both belts were deposited on Paleozoic basement and none appear to be breccia pipes. We infer that their present east tilt is due to extension on west-dipping normal faults. Some of these faults may be the northern strands of middle Miocene (ca. 16 Ma) faults that cut and tilted the 34.0 Ma Caetano caldera ~40° east in the central Shoshone Range (<5 km south of Mill Creek), but further mapping is necessary to trace the faults through the highly deformed Paleozoic rocks that surround the isolated Tertiary outcrops. Significant post-Eocene extensional faulting in the northern Shoshone Range may have important implications for both the structure of the Roberts Mountains allochthon and the exposure of potentially mineralized rocks in its lower plate, both of which were likely east-tilted and repeated by west-dipping faults together with overlying Tertiary rocks.</p>","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Economic Geology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/econgeo.109.7.1843","usgsCitation":"Colgan, J.P., Henry, C., and John, D.A., 2014, Evidence for large-magnitude, post-Eocene extension in the northern Shoshone Range, Nevada, and its implications for Carlin-type gold deposits in the lower plate of the Roberts Mountains allochthon: Economic Geology, v. 109, no. 7, p. 1843-1862, https://doi.org/10.2113/econgeo.109.7.1843.","productDescription":"20 p.","startPage":"1843","endPage":"1862","ipdsId":"IP-044321","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":295332,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":295331,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.2113/econgeo.109.7.1843"}],"country":"United States","state":"Nevada","otherGeospatial":"Shoshone Rangebound","volume":"109","issue":"7","noUsgsAuthors":false,"publicationDate":"2014-08-27","publicationStatus":"PW","scienceBaseUri":"543f7e87e4b065f4ad22cf7b","contributors":{"authors":[{"text":"Colgan, Joseph P. 0000-0001-6671-1436 jcolgan@usgs.gov","orcid":"https://orcid.org/0000-0001-6671-1436","contributorId":1649,"corporation":false,"usgs":true,"family":"Colgan","given":"Joseph","email":"jcolgan@usgs.gov","middleInitial":"P.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true},{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":503232,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Henry, Christopher D.","contributorId":74320,"corporation":false,"usgs":true,"family":"Henry","given":"Christopher D.","affiliations":[],"preferred":false,"id":503234,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"John, David A. 0000-0001-7977-9106 djohn@usgs.gov","orcid":"https://orcid.org/0000-0001-7977-9106","contributorId":1748,"corporation":false,"usgs":true,"family":"John","given":"David","email":"djohn@usgs.gov","middleInitial":"A.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":503233,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70174119,"text":"70174119 - 2014 - Book review: Ecology of North American freshwater fishes","interactions":[],"lastModifiedDate":"2016-06-29T13:00:08","indexId":"70174119","displayToPublicDate":"2014-10-15T06:30:00","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2285,"text":"Journal of Fish Biology","active":true,"publicationSubtype":{"id":10}},"title":"Book review: Ecology of North American freshwater fishes","docAbstract":"<div class=\"t m0 x2 h4 yc ff2 fs3 fc0 sc0 ls7 ws0\">\n<p class=\"t m0 x5 h4 y2f ff2 fs3 fc0 sc0 ls7 ws0\">This book will be important in courses for upper undergraduates studying fish ecology or for graduate students. However, it will also be an excellent reference for the fishery manager who asks &lsquo;Why does this fish do that?&rsquo;. With the wealth of great information contained in Ross&rsquo; book, chances are an answer will be found.</p>\n</div>\n<p><span>Review info:</span><i>&nbsp;Ecology of North American freshwater fishes.</i><span>&nbsp;Edited by Stephen T. Ross, 2013. ISBN: 978-0520249455, 408&nbsp;pp.</span></p>","language":"English","publisher":"Academic Press","doi":"10.1111/jfb.12536","usgsCitation":"Bonar, S.A., 2014, Book review: Ecology of North American freshwater fishes: Journal of Fish Biology, v. 85, no. 5, p. 1799-1800, https://doi.org/10.1111/jfb.12536.","productDescription":"2 p.","startPage":"1799","endPage":"1800","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-059466","costCenters":[{"id":200,"text":"Coop Res Unit Seattle","active":true,"usgs":true}],"links":[{"id":324620,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"85","issue":"5","publishingServiceCenter":{"id":12,"text":"Tacoma PSC"},"noUsgsAuthors":false,"publicationDate":"2014-10-15","publicationStatus":"PW","scienceBaseUri":"5774f1ade4b07dd077c698f2","contributors":{"authors":[{"text":"Bonar, Scott A. 0000-0003-3532-4067 sbonar@usgs.gov","orcid":"https://orcid.org/0000-0003-3532-4067","contributorId":3712,"corporation":false,"usgs":true,"family":"Bonar","given":"Scott","email":"sbonar@usgs.gov","middleInitial":"A.","affiliations":[{"id":200,"text":"Coop Res Unit Seattle","active":true,"usgs":true}],"preferred":true,"id":640962,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70125697,"text":"70125697 - 2014 - A guidance manual for assessing scour potential using the South Carolina bridge-scour envelope curves","interactions":[],"lastModifiedDate":"2017-06-29T12:15:46","indexId":"70125697","displayToPublicDate":"2014-10-15T00:00:00","publicationYear":"2014","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"A guidance manual for assessing scour potential using the South Carolina bridge-scour envelope curves","docAbstract":"<p>The U.S. Geological Survey, in cooperation with the South Carolina Department of Transportation, conducted a series of three field investigations of bridge scour in order to better understand regional trends of scour within South Carolina. The studies collected historic-scour data at approximately 200 riverine bridges including measurements of clear-water abutment, contraction, and pier scour, as well as live-bed contraction and pier scour. These investigations provided valuable insights for regional scour trends and yielded bridge-scour envelope curves for assessing scour potential associated with all components of scour at riverine bridges in South Carolina. The application and limitations of these envelop cureves were documents in three reports, Each repoort addresses different components of bridge scour and this, there is a need to develop an integrated procedure for applying the South Carolina bridge-scour envelope curves. To address this need, the U.S. Geological Survey and the South Carolina Department of Transportation initiated a cooperative effort to develop an integrated procedure and document the method in a guidance manual. In addition to developing the integrated procedure, field data from other investigations outside of South Carolina were used to verify the South Carolina bridge-source envelope curves.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"S.C. Water Resources Conference 2014 Proceedings","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"S.C. Water Resources Conference 2014","conferenceDate":"October 15-16, 2014","conferenceLocation":"Columbia, SC","language":"English","publisher":"Clemson University Institute of Computational Technology","publisherLocation":"Clemson, SC","usgsCitation":"Benedict, S., Caldwell, A.W., and Feaster, T., 2014, A guidance manual for assessing scour potential using the South Carolina bridge-scour envelope curves, <i>in</i> S.C. Water Resources Conference 2014 Proceedings, Columbia, SC, October 15-16, 2014, 4 p.","productDescription":"4 p.","numberOfPages":"4","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-059120","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":296228,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://tigerprints.clemson.edu/scwrc/2014/2014basin/2/"},{"id":296229,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"South 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,{"id":70148006,"text":"70148006 - 2014 - Tsunamis: stochastic models of occurrence and generation mechanisms","interactions":[],"lastModifiedDate":"2016-10-11T16:45:31","indexId":"70148006","displayToPublicDate":"2014-10-15T00:00:00","publicationYear":"2014","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Tsunamis: stochastic models of occurrence and generation mechanisms","docAbstract":"<p>The devastating consequences of the 2004 Indian Ocean and 2011 Japan tsunamis have led to increased research into many different aspects of the tsunami phenomenon. In this entry, we review research related to the observed complexity and uncertainty associated with tsunami generation, propagation, and occurrence described and analyzed using a variety of stochastic methods. In each case, seismogenic tsunamis are primarily considered. Stochastic models are developed from the physical theories that govern tsunami evolution combined with empirical models fitted to seismic and tsunami observations, as well as tsunami catalogs. These stochastic methods are key to providing probabilistic forecasts and hazard assessments for tsunamis. The stochastic methods described here are similar to those described for earthquakes (Vere-Jones 2013) and volcanoes (Bebbington&nbsp;<span id=\"_mce_caret\" data-mce-bogus=\"true\"><i></i>2013</span>) in this encyclopedia.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Encyclopedia of complexity and systems science","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Springer New York","doi":"10.1007/978-3-642-27737-5_595-1","collaboration":"UC Riverside","usgsCitation":"Geist, E.L., and Oglesby, D.D., 2014, Tsunamis: stochastic models of occurrence and generation mechanisms, chap. <i>of</i> Encyclopedia of complexity and systems science, p. 1-29, https://doi.org/10.1007/978-3-642-27737-5_595-1.","productDescription":"29 p.","startPage":"1","endPage":"29","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-056422","costCenters":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":310876,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"publishingServiceCenter":{"id":14,"text":"Menlo Park PSC"},"noUsgsAuthors":false,"publicationDate":"2014-10-15","publicationStatus":"PW","scienceBaseUri":"563496b7e4b0480763480085","contributors":{"authors":[{"text":"Geist, Eric L. 0000-0003-0611-1150 egeist@usgs.gov","orcid":"https://orcid.org/0000-0003-0611-1150","contributorId":1956,"corporation":false,"usgs":true,"family":"Geist","given":"Eric","email":"egeist@usgs.gov","middleInitial":"L.","affiliations":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true},{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":546741,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Oglesby, David D.","contributorId":51637,"corporation":false,"usgs":true,"family":"Oglesby","given":"David","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":546742,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70125696,"text":"70125696 - 2014 - Assessment of the NCHRP abutment scour prediction equations with laboratory and field data","interactions":[],"lastModifiedDate":"2017-06-29T12:18:41","indexId":"70125696","displayToPublicDate":"2014-10-15T00:00:00","publicationYear":"2014","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Assessment of the NCHRP abutment scour prediction equations with laboratory and field data","docAbstract":"<p>The U.S. Geological Survey, in coopeation with nthe National Cooperative Highway Research Program (NCHRP) is assessing the performance of several abutment-scour predcition equations developed in NCHRP Project 24-15(2) and NCHRP Project 24-20. To accomplish this assssment, 516 laboratory and 329 fiels measurements of abutment scor were complied from selected sources and applied tto the new equations. Results will be used to identify stregths, weaknesses, and limitations of the NCHRP abutment scour equations, providing practical insights for applying the equations. This paper presents some prelimiray findings from the investigation.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"S.C. Water Resources Conference 2014 Proceedings","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"S.C. Water Resources Conference 2014","conferenceDate":"October 15-16, 2014","conferenceLocation":"Columbia, SC","language":"English","publisher":"Clemson University Institute of Computational Technology","publisherLocation":"Clemson, SC","usgsCitation":"Benedict, S., 2014, Assessment of the NCHRP abutment scour prediction equations with laboratory and field data, <i>in</i> S.C. Water Resources Conference 2014 Proceedings, Columbia, SC, October 15-16, 2014, 4 p.","productDescription":"4 p.","numberOfPages":"4","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-059119","costCenters":[{"id":559,"text":"South Carolina Water Science Center","active":true,"usgs":true}],"links":[{"id":296237,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":296236,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://tigerprints.clemson.edu/scwrc/2014/2014basin/3/"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"546f10e7e4b057be23d4a755","contributors":{"authors":[{"text":"Benedict, Stephen T. benedict@usgs.gov","contributorId":3198,"corporation":false,"usgs":true,"family":"Benedict","given":"Stephen T.","email":"benedict@usgs.gov","affiliations":[{"id":559,"text":"South Carolina Water Science Center","active":true,"usgs":true}],"preferred":false,"id":519524,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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