{"pageNumber":"1703","pageRowStart":"42550","pageSize":"25","recordCount":184617,"records":[{"id":70003944,"text":"70003944 - 2011 - Intra-seasonal variation in foraging behavior among Adélie penguins (Pygocelis adeliae) breeding at Cape Hallett, Ross Sea, Antarctica","interactions":[],"lastModifiedDate":"2022-08-30T10:54:10.046989","indexId":"70003944","displayToPublicDate":"2012-05-23T11:26:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3093,"text":"Polar Biology","active":true,"publicationSubtype":{"id":10}},"title":"Intra-seasonal variation in foraging behavior among Adélie penguins (Pygocelis adeliae) breeding at Cape Hallett, Ross Sea, Antarctica","docAbstract":"We investigated intra-seasonal variation in foraging behavior of chick-rearing Ad&#233;lie penguins, <i>Pygoscelis adeliae</i>, during two consecutive summers at Cape Hallett, northwestern Ross Sea. Although foraging behavior of this species has been extensively studied throughout the broad continental shelf region of the Ross Sea, this is the first study to report foraging behaviors and habitat affiliations among birds occupying continental slope waters. Continental slope habitat supports the greatest abundances of this species throughout its range, but we lack information about how intra-specific competition for prey might affect foraging and at-sea distribution and how these attributes compare with previous Ross Sea studies. Foraging trips increased in both distance and duration as breeding advanced from guard to cr&#232;che stage, but foraging dive depth, dive rates, and vertical dive distances travelled per hour decreased. Consistent with previous studies within slope habitats elsewhere in Antarctic waters, Antarctic krill (<i>Euphausia superba</i>) dominated chick meal composition, but fish increased four-fold from guard to cr&#232;che stages. Foraging-, focal-, and core areas all doubled during the cr&#232;che stage as individuals shifted distribution in a southeasterly direction away from the coast while simultaneously becoming more widely dispersed (i.e., less spatial overlap among individuals). Intra-specific competition for prey among Ad&#233;lie penguins appears to influence foraging behavior of this species, even in food webs dominated by Antarctic krill.","language":"English","publisher":"Springer","publisherLocation":"Amsterdam, Netherlands","doi":"10.1007/s00300-010-0858-0","usgsCitation":"Lyver, P.O., MacLeod, C.J., Ballard, G., Karl, B.J., Barton, K.J., Adams, J., Ainley, D., and Wilson, P.R., 2011, Intra-seasonal variation in foraging behavior among Adélie penguins (Pygocelis adeliae) breeding at Cape Hallett, Ross Sea, Antarctica: Polar Biology, v. 34, no. 1, p. 49-67, https://doi.org/10.1007/s00300-010-0858-0.","productDescription":"19 p.","startPage":"49","endPage":"67","numberOfPages":"19","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":257094,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Antarctica, Cape Hallett, Ross Sea","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              168.5302734375,\n              -72.88087095711502\n            ],\n            [\n              174.111328125,\n              -72.88087095711502\n            ],\n            [\n              174.111328125,\n              -71.18775391813158\n            ],\n            [\n              168.5302734375,\n              -71.18775391813158\n            ],\n            [\n              168.5302734375,\n              -72.88087095711502\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"34","issue":"1","noUsgsAuthors":false,"publicationDate":"2010-07-15","publicationStatus":"PW","scienceBaseUri":"505a3dbde4b0c8380cd637e1","contributors":{"authors":[{"text":"Lyver, P. O. B.","contributorId":93714,"corporation":false,"usgs":false,"family":"Lyver","given":"P.","email":"","middleInitial":"O. B.","affiliations":[],"preferred":false,"id":349652,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"MacLeod, C. J.","contributorId":50333,"corporation":false,"usgs":false,"family":"MacLeod","given":"C.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":349648,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ballard, G.","contributorId":75314,"corporation":false,"usgs":false,"family":"Ballard","given":"G.","email":"","affiliations":[],"preferred":false,"id":349650,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Karl, B. J.","contributorId":43544,"corporation":false,"usgs":false,"family":"Karl","given":"B.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":349646,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Barton, K. J.","contributorId":66897,"corporation":false,"usgs":false,"family":"Barton","given":"K.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":349649,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Adams, J.","contributorId":45240,"corporation":false,"usgs":true,"family":"Adams","given":"J.","affiliations":[],"preferred":false,"id":349647,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Ainley, D. G.","contributorId":77870,"corporation":false,"usgs":false,"family":"Ainley","given":"D. G.","affiliations":[],"preferred":false,"id":349651,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Wilson, P. R.","contributorId":11388,"corporation":false,"usgs":false,"family":"Wilson","given":"P.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":349645,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":70005652,"text":"70005652 - 2011 - Interhemispheric ice-sheet synchronicity during the last glacial maximum","interactions":[],"lastModifiedDate":"2012-06-01T01:01:40","indexId":"70005652","displayToPublicDate":"2012-05-23T11:01:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Interhemispheric ice-sheet synchronicity during the last glacial maximum","docAbstract":"The timing of the last maximum extent of the Antarctic ice sheets relative to those in the Northern Hemisphere remains poorly understood. We develop a chronology for the Weddell Sea sector of the East Antarctic Ice Sheet that, combined with ages from other Antarctic ice-sheet sectors, indicates that the advance to and retreat from their maximum extent was within dating uncertainties synchronous with most sectors of Northern Hemisphere ice sheets. Surface climate forcing of Antarctic mass balance would probably cause an opposite response, whereby a warming climate would increase accumulation but not surface melting. Our new data support teleconnections involving sea-level forcing from Northern Hemisphere ice sheets and changes in North Atlantic deep-water formation and attendant heat flux to Antarctic grounding lines to synchronize the hemispheric ice sheets.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Science","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"American Association for the Advancement of Science","publisherLocation":"Washington, D.C.","doi":"10.1126/science.1209299","usgsCitation":"Weber, M.E., Clark, P., Ricken, W., Mitrovica, J.X., Hostetler, S.W., and Kuhn, G., 2011, Interhemispheric ice-sheet synchronicity during the last glacial maximum: Science, v. 334, no. 6060, p. 1265-1269, https://doi.org/10.1126/science.1209299.","productDescription":"5 p.","startPage":"1265","endPage":"1269","costCenters":[{"id":148,"text":"Branch of Regional Research-Western Region","active":false,"usgs":true}],"links":[{"id":257095,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":257083,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://dx.doi.org/10.1126/science.1209299","linkFileType":{"id":5,"text":"html"}}],"volume":"334","issue":"6060","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3d02e4b0c8380cd6321b","contributors":{"authors":[{"text":"Weber, Michael E.","contributorId":38818,"corporation":false,"usgs":true,"family":"Weber","given":"Michael","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":353011,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Clark, Peter U.","contributorId":68994,"corporation":false,"usgs":true,"family":"Clark","given":"Peter U.","affiliations":[],"preferred":false,"id":353012,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ricken, Werner","contributorId":102305,"corporation":false,"usgs":true,"family":"Ricken","given":"Werner","email":"","affiliations":[],"preferred":false,"id":353015,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Mitrovica, Jerry X.","contributorId":86200,"corporation":false,"usgs":true,"family":"Mitrovica","given":"Jerry","email":"","middleInitial":"X.","affiliations":[],"preferred":false,"id":353013,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Hostetler, Steven W. 0000-0003-2272-8302 swhostet@usgs.gov","orcid":"https://orcid.org/0000-0003-2272-8302","contributorId":3249,"corporation":false,"usgs":true,"family":"Hostetler","given":"Steven","email":"swhostet@usgs.gov","middleInitial":"W.","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true},{"id":200,"text":"Coop Res Unit Seattle","active":true,"usgs":true}],"preferred":true,"id":353010,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Kuhn, Gerhard","contributorId":102080,"corporation":false,"usgs":true,"family":"Kuhn","given":"Gerhard","email":"","affiliations":[],"preferred":false,"id":353014,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70004044,"text":"70004044 - 2011 - Interlaboratory comparison of measurements of acid-volatile sulfide and simultaneously extracted nickel in spiked sediments","interactions":[],"lastModifiedDate":"2020-01-28T15:43:59","indexId":"70004044","displayToPublicDate":"2012-05-23T09:31:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1571,"text":"Environmental Toxicology and Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"Interlaboratory comparison of measurements of acid-volatile sulfide and simultaneously extracted nickel in spiked sediments","docAbstract":"<p><span>An interlaboratory comparison of acid-volatile sulfide (AVS) and simultaneously extracted nickel (SEM_Ni) measurements of sediments was conducted among five independent laboratories. Relative standard deviations for the seven test samples ranged from 5.6 to 71% (mean = 25%) for AVS and from 5.5 to 15% (mean = 10%) for SEM_Ni. These results are in stark contrast to a recently published study that indicated AVS and SEM analyses were highly variable among laboratories.</span></p>","language":"English","publisher":"Society of Environmental Toxicology and Chemistry","doi":"10.1002/etc.506","usgsCitation":"Brumbaugh, W.G., Hammerschmidt, C.R., Zanella, L., Rogevich, E., Salata, G., and Bolek, R., 2011, Interlaboratory comparison of measurements of acid-volatile sulfide and simultaneously extracted nickel in spiked sediments: Environmental Toxicology and Chemistry, v. 30, no. 6, p. 1306-1309, https://doi.org/10.1002/etc.506.","productDescription":"4 p.","startPage":"1306","endPage":"1309","numberOfPages":"4","costCenters":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true},{"id":34983,"text":"Contaminant Biology Program","active":true,"usgs":true}],"links":[{"id":257074,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"30","issue":"6","noUsgsAuthors":false,"publicationDate":"2011-06-01","publicationStatus":"PW","scienceBaseUri":"505a3d21e4b0c8380cd6330c","contributors":{"authors":[{"text":"Brumbaugh, William G. 0000-0003-0081-375X bbrumbaugh@usgs.gov","orcid":"https://orcid.org/0000-0003-0081-375X","contributorId":493,"corporation":false,"usgs":true,"family":"Brumbaugh","given":"William","email":"bbrumbaugh@usgs.gov","middleInitial":"G.","affiliations":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"preferred":true,"id":350295,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hammerschmidt, Chad R.","contributorId":91458,"corporation":false,"usgs":true,"family":"Hammerschmidt","given":"Chad","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":350300,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Zanella, Luciana","contributorId":87798,"corporation":false,"usgs":true,"family":"Zanella","given":"Luciana","email":"","affiliations":[],"preferred":false,"id":350298,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Rogevich, Emily","contributorId":90150,"corporation":false,"usgs":true,"family":"Rogevich","given":"Emily","email":"","affiliations":[],"preferred":false,"id":350299,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Salata, Gregory","contributorId":29684,"corporation":false,"usgs":true,"family":"Salata","given":"Gregory","email":"","affiliations":[],"preferred":false,"id":350296,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Puchalka, Radoslaw","contributorId":31249,"corporation":false,"usgs":true,"family":"Puchalka","given":"Radoslaw","affiliations":[],"preferred":false,"id":350297,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70004028,"text":"70004028 - 2011 - Integration of paleoseismic data from multiple sites to develop an objective earthquake chronology: Application to the Weber segment of the Wasatch fault zone, Utah","interactions":[],"lastModifiedDate":"2012-06-01T01:01:40","indexId":"70004028","displayToPublicDate":"2012-05-23T08:56:00","publicationYear":"2011","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":"Integration of paleoseismic data from multiple sites to develop an objective earthquake chronology: Application to the Weber segment of the Wasatch fault zone, Utah","docAbstract":"We present a method to evaluate and integrate paleoseismic data from multiple sites into a single, objective measure of earthquake timing and recurrence on discrete segments of active faults. We apply this method to the Weber segment (WS) of the Wasatch fault zone using data from four fault-trench studies completed between 1981 and 2009. After systematically reevaluating the stratigraphic and chronologic data from each trench site, we constructed time-stratigraphic OxCal models that yield site probability density functions (PDFs) of the times of individual earthquakes. We next qualitatively correlated the site PDFs into a segment-wide earthquake chronology, which is supported by overlapping site PDFs, large per-event displacements, and prominent segment boundaries. For each segment-wide earthquake, we computed the product of the site PDF probabilities in common time bins, which emphasizes the overlap in the site earthquake times, and gives more weight to the narrowest, best-defined PDFs. The product method yields smaller earthquake-timing uncertainties compared to taking the mean of the site PDFs, but is best suited to earthquakes constrained by broad, overlapping site PDFs. We calculated segment-wide earthquake recurrence intervals and uncertainties using a Monte Carlo model. Five surface-faulting earthquakes occurred on the WS at about 5.9, 4.5, 3.1, 1.1, and 0.6 ka. With the exception of the 1.1-ka event, we used the product method to define the earthquake times. The revised WS chronology yields a mean recurrence interval of 1.3 kyr (0.7&ndash;1.9-kyr estimated two-sigma [2&delta;] range based on interevent recurrence). These data help clarify the paleoearthquake history of the WS, including the important question of the timing and rupture extent of the most recent earthquake, and are essential to the improvement of earthquake-probability assessments for the Wasatch Front region.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Bulletin of the Seismological Society of America","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"The Seismological Society of America","publisherLocation":"El Cerrito, CA","doi":"10.1785/0120110102","usgsCitation":"DuRoss, C., Personius, S.F., Crone, A.J., Olig, S.S., and Lund, W., 2011, Integration of paleoseismic data from multiple sites to develop an objective earthquake chronology: Application to the Weber segment of the Wasatch fault zone, Utah: Bulletin of the Seismological Society of America, v. 101, no. 6, p. 2765-2781, https://doi.org/10.1785/0120110102.","productDescription":"17 p.","startPage":"2765","endPage":"2781","temporalStart":"1981-01-01","temporalEnd":"2009-12-31","costCenters":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"links":[{"id":257077,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":257059,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://dx.doi.org/10.1785/0120110102","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Utah","otherGeospatial":"Wasatch Fault Zone","volume":"101","issue":"6","noUsgsAuthors":false,"publicationDate":"2011-12-08","publicationStatus":"PW","scienceBaseUri":"505a3c8de4b0c8380cd62e25","contributors":{"authors":[{"text":"DuRoss, Christopher B.","contributorId":66532,"corporation":false,"usgs":true,"family":"DuRoss","given":"Christopher B.","affiliations":[],"preferred":false,"id":350221,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Personius, Stephen F. personius@usgs.gov","contributorId":1214,"corporation":false,"usgs":true,"family":"Personius","given":"Stephen","email":"personius@usgs.gov","middleInitial":"F.","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":false,"id":350219,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Crone, Anthony J. 0000-0002-3006-406X crone@usgs.gov","orcid":"https://orcid.org/0000-0002-3006-406X","contributorId":790,"corporation":false,"usgs":true,"family":"Crone","given":"Anthony","email":"crone@usgs.gov","middleInitial":"J.","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":true,"id":350218,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Olig, Susan S.","contributorId":87640,"corporation":false,"usgs":true,"family":"Olig","given":"Susan","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":350222,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Lund, William R.","contributorId":48320,"corporation":false,"usgs":true,"family":"Lund","given":"William R.","affiliations":[],"preferred":false,"id":350220,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70038411,"text":"fs20113043 - 2011 - Streamflow of 2010--Water year summary","interactions":[],"lastModifiedDate":"2012-08-28T14:10:23","indexId":"fs20113043","displayToPublicDate":"2012-05-22T00:00:00","publicationYear":"2011","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":"2011-3043","title":"Streamflow of 2010--Water year summary","docAbstract":"The maps and graph in this summary describe streamflow conditions for water-year 2010 (October 1, 2009 to September 30, 2010) in the context of the 81-year period 1930-2010, unless otherwise noted. The illustrations are based on observed data from the U.S. Geological Survey's (USGS) National Streamflow Information Program. The period 1930-2010 was used because prior to 1930, the number of streamgages was too small to provide representative data for computing statistics for most regions of the country.\r\nIn the summary, reference is made to the term \"runoff,\" which is the depth to which a river basin, State, or other geographic area would be covered with water if all the streamflow within the area during a single year was uniformly distributed upon it. Runoff quantifies the magnitude of water flowing through the Nation's rivers and streams in measurement units that can be compared from one area to another.\r\nEach of the maps and graphs below can be expanded to a larger view by clicking on the image. In all the graphics, a rank of 1 indicates the highest flow of all years analyzed.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/fs20113043","usgsCitation":"Xiaodong, J., Wolock, D.M., Lins, H.F., and Brady, S., 2011, Streamflow of 2010--Water year summary: U.S. Geological Survey Fact Sheet 2011-3043, 8 p., https://doi.org/10.3133/fs20113043.","productDescription":"8 p.","numberOfPages":"8","onlineOnly":"Y","temporalStart":"2009-10-01","temporalEnd":"2010-09-30","costCenters":[{"id":502,"text":"Office of Surface Water","active":true,"usgs":true}],"links":[{"id":256944,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2011_3043.gif"},{"id":256939,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2011/3043/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b9b12e4b08c986b31cc75","contributors":{"authors":[{"text":"Xiaodong, Jian","contributorId":10260,"corporation":false,"usgs":true,"family":"Xiaodong","given":"Jian","email":"","affiliations":[],"preferred":false,"id":464062,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wolock, David M. 0000-0002-6209-938X dwolock@usgs.gov","orcid":"https://orcid.org/0000-0002-6209-938X","contributorId":540,"corporation":false,"usgs":true,"family":"Wolock","given":"David","email":"dwolock@usgs.gov","middleInitial":"M.","affiliations":[{"id":37778,"text":"WMA - Integrated Modeling and Prediction Division","active":true,"usgs":true},{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true},{"id":27111,"text":"National Water Quality Program","active":true,"usgs":true},{"id":503,"text":"Office of Water Quality","active":true,"usgs":true},{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"preferred":true,"id":464060,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lins, Harry F. 0000-0001-5385-9247 hlins@usgs.gov","orcid":"https://orcid.org/0000-0001-5385-9247","contributorId":1505,"corporation":false,"usgs":true,"family":"Lins","given":"Harry","email":"hlins@usgs.gov","middleInitial":"F.","affiliations":[{"id":502,"text":"Office of Surface Water","active":true,"usgs":true}],"preferred":true,"id":464061,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Brady, Steve","contributorId":108351,"corporation":false,"usgs":true,"family":"Brady","given":"Steve","email":"","affiliations":[],"preferred":false,"id":464063,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70006310,"text":"70006310 - 2011 - Innate immunity is not related to the sex of adult Tree Swallows during the nestling period","interactions":[],"lastModifiedDate":"2016-09-20T14:24:03","indexId":"70006310","displayToPublicDate":"2012-05-21T11:58:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3551,"text":"The Condor","active":true,"publicationSubtype":{"id":10}},"title":"Innate immunity is not related to the sex of adult Tree Swallows during the nestling period","docAbstract":"Evolutionary theory predicts that exposure to more diverse pathogens will result in the evolution of a more robust immune response. We predicted that during the breeding season the innate immune function of female Tree Swallows (<i>Tachycineta bicolor</i>) should be more effective than that of males because (1) the transmission of sexually transmitted microbes during copulation puts females at greater risk because ejaculates move from males to females, (2) females copulate with multiple males, exposing them to the potentially pathogenic microbes in semen, and (3) females spend more time in the nest than do males so may be more exposed to nest microbes and ectoparasites that can be vectors of bacterial and viral pathogens. In addition, elevated testosterone in males may suppress immune function. We tested our prediction during the 2009 breeding season with microbicidal assays in vitro to assess the ability of the innate immune system to kill <i>Escherichia coli</i>. The sexes did not differ in the ability of their whole blood to kill <i>E. coli</i>. We also found no significant relationships between the ability of whole blood to kill <i>E. coli</i> and the reproductive performance or the physical condition of males or females. These results indicate that during the nestling period there are no sexual differences in this component of the innate immune system. In addition, they suggest that there is little association between this component of innate immunity and the reproductive performance and physical condition during the nestling period of adult Tree Swallows.","language":"English","publisher":"Cooper Ornithological Society","publisherLocation":"Waco, TX","doi":"10.1525/cond.2011.100220","usgsCitation":"Houdek, B.J., Lombardo, M.P., Thorpe, P.A., and Hahn, D., 2011, Innate immunity is not related to the sex of adult Tree Swallows during the nestling period: The Condor, v. 113, no. 4, p. 853-859, https://doi.org/10.1525/cond.2011.100220.","productDescription":"7 p.","startPage":"853","endPage":"859","temporalStart":"2009-01-01","temporalEnd":"2009-12-31","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":474735,"rank":1,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1525/cond.2011.100220","text":"Publisher Index Page"},{"id":257022,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"113","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3bfbe4b0c8380cd6298f","contributors":{"authors":[{"text":"Houdek, Bradley J.","contributorId":20582,"corporation":false,"usgs":true,"family":"Houdek","given":"Bradley","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":354284,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lombardo, Michael P.","contributorId":9507,"corporation":false,"usgs":true,"family":"Lombardo","given":"Michael","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":354283,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Thorpe, Patrick A.","contributorId":45555,"corporation":false,"usgs":true,"family":"Thorpe","given":"Patrick","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":354286,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hahn, D. Caldwell 0000-0002-5242-2059","orcid":"https://orcid.org/0000-0002-5242-2059","contributorId":26055,"corporation":false,"usgs":true,"family":"Hahn","given":"D. Caldwell","affiliations":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"preferred":true,"id":354285,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70003530,"text":"70003530 - 2011 - Influence of throat configuration and fish density on escapement of channel catfish from hoop nets","interactions":[],"lastModifiedDate":"2015-06-05T11:15:06","indexId":"70003530","displayToPublicDate":"2012-05-21T11:34:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":718,"text":"American Fisheries Society Symposium","active":true,"publicationSubtype":{"id":10}},"title":"Influence of throat configuration and fish density on escapement of channel catfish from hoop nets","docAbstract":"<p>In recent years, several state agencies have adopted the use of baited, tandemset hoop nets to assess lentic channel catfish <i>Ictalurus punctatus</i> populations. Some level of escapement from the net is expected because an opening exists in each throat of the net, although factors influencing rates of escapement from hoop nets have not been quantified. We conducted experiments to quantify rates of escapement and to determine the influence of throat configuration and fish density within the net on escapement rates. An initial experiment to determine the rate of escapement from each net compartment utilized individually tagged channel catfish placed within the entrance (between the two throats) and cod (within the second throat) compartments of a single hoop net for overnight sets. From this experiment, the mean rate (&plusmn;SE) of channel catfish escaping was 4.2% (&plusmn;1.5) from the cod (cod throat was additionally restricted from the traditionally manufactured product), and 74% (&plusmn;4.2) from the entrance compartments. In a subsequent experiment, channel catfish were placed only in the cod compartment with different throat configurations (restricted or unrestricted) and at two densities (low [6 fish per net] and high [60 fish per net]) for overnight sets to determine the influence of fish density and throat configuration on escapement rates. Escapement rates between throat configurations were doubled at low fish density (13.3 &plusmn; 5.4% restricted versus 26.7 &plusmn; 5.6% unrestricted) and tripled at high fish density (14.3 &plusmn; 4.9% restricted versus 51.9 &plusmn; 5.0% unrestricted). These results suggest that retention efficiency is high from cod compartments with restricted throat entrances. However, managers and researchers need to be aware that modification to the cod throats (restrictions) is needed for hoop nets ordered from manufacturers. Managers need to be consistent in their use and reporting of cod end throat configurations when using this gear.</p>","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"American Fisheries Society Symposium","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"American Fisheries Society","publisherLocation":"Bethesda, MD","usgsCitation":"Porath, M.T., Pape, L.D., and Richters, L.K., 2011, Influence of throat configuration and fish density on escapement of channel catfish from hoop nets: American Fisheries Society Symposium, v. 77, p. 563-571.","productDescription":"9 p.","startPage":"563","endPage":"571","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":204,"text":"Cooperative Research Unit Seattle","active":false,"usgs":true}],"links":[{"id":257019,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":301046,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://fisheries.org/shop/54077C"}],"volume":"77","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3b8fe4b0c8380cd62644","contributors":{"authors":[{"text":"Porath, Mark T.","contributorId":28846,"corporation":false,"usgs":true,"family":"Porath","given":"Mark","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":347643,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pape, Larry D.","contributorId":102725,"corporation":false,"usgs":true,"family":"Pape","given":"Larry","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":347645,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Richters, Lindsey K.","contributorId":46345,"corporation":false,"usgs":true,"family":"Richters","given":"Lindsey","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":347644,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70005087,"text":"70005087 - 2011 - Influence of dissolved organic carbon on toxicity of copper to a unionid mussel (<i>Villosa iris</i>) and a cladoceran (<i>Ceriodaphnia dubia</i>) in acute and chronic water exposures","interactions":[],"lastModifiedDate":"2020-01-21T16:14:21","indexId":"70005087","displayToPublicDate":"2012-05-21T10:50:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1571,"text":"Environmental Toxicology and Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"Influence of dissolved organic carbon on toxicity of copper to a unionid mussel (<i>Villosa iris</i>) and a cladoceran (<i>Ceriodaphnia dubia</i>) in acute and chronic water exposures","docAbstract":"Acute and chronic toxicity of copper (Cu) to a unionid mussel (<i>Villosa iris</i>) and a cladoceran (<i>Ceriodaphnia dubia</i>) were determined in water exposures at four concentrations of dissolved organic carbon (DOC; nominally 0.5, 2.5, 5, and 10 mg/L as carbon [C]). Test waters with DOC concentrations of 2.5 to 10 mg C/L were prepared by mixing a concentrate of natural organic matter (Suwannee River, GA, USA) in diluted well water (hardness 100 mg/L as CaCO<sub>3</sub>, pH 8.3, DOC 0.5 mg C/L). Acute median effect concentrations (EC50s) for dissolved Cu increased approximately fivefold (15&ndash;72 &mu;g Cu/L) for mussel survival in 4-d exposures and increased about 11-fold (25&ndash;267 &mu;g Cu/L) for cladoceran survival in 2-d exposures across DOC concentrations from 0.5 to 10 mg C/L. Similarly, chronic 20% effect concentrations (EC20s) for the mussel in 28-d exposures increased about fivefold (13&ndash;61 &mu;g Cu/L for survival; 8.8&ndash;38 &mu;g Cu/L for biomass), and the EC20s for the cladoceran in 7-d exposures increased approximately 17-fold (13&ndash;215 &mu;g Cu/L) for survival or approximately fourfold (12&ndash;42 &mu;g Cu/L) for reproduction across DOC concentrations from 0.5 to 10 mg C/L. The acute and chronic values for the mussel were less than or approximately equal to the values for the cladoceran. Predictions from the biotic ligand model (BLM) used to derive the U.S. Environmental Protection Agency's ambient water quality criteria (AWQC) for Cu explained more than 90% of the variation in the acute and chronic endpoints for the two species, with the exception of the EC20 for cladoceran reproduction (only 46% of variation explained). The BLM-normalized acute EC50s and chronic EC20s for the mussel and BLM-normalized chronic EC20s for the cladoceran in waters with DOC concentrations of 2.5 to 10 mg C/L were equal to or less than the final acute value and final chronic value in the BLM-based AWQC for Cu, respectively, indicating that the Cu AWQC might not adequately protect the mussel from acute and chronic exposure, and the cladoceran from chronic exposure.","language":"English","publisher":"Society of Environmental Toxicology and Chemistry","doi":"10.1002/etc.596","usgsCitation":"Wang, N., Mebane, C.A., Kunz, J.L., Ingersoll, C.G., Brumbaugh, W.G., Santore, R.C., Gorsuch, J.W., and Arnold, W.R., 2011, Influence of dissolved organic carbon on toxicity of copper to a unionid mussel (<i>Villosa iris</i>) and a cladoceran (<i>Ceriodaphnia dubia</i>) in acute and chronic water exposures: Environmental Toxicology and Chemistry, v. 30, no. 9, p. 2115-2125, https://doi.org/10.1002/etc.596.","productDescription":"11 p.","startPage":"2115","endPage":"2125","numberOfPages":"11","costCenters":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true},{"id":34983,"text":"Contaminant Biology Program","active":true,"usgs":true}],"links":[{"id":257021,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"30","issue":"9","noUsgsAuthors":false,"publicationDate":"2011-09-01","publicationStatus":"PW","scienceBaseUri":"505a3b28e4b0c8380cd62295","contributors":{"authors":[{"text":"Wang, Ning 0000-0002-2846-3352 nwang@usgs.gov","orcid":"https://orcid.org/0000-0002-2846-3352","contributorId":2818,"corporation":false,"usgs":true,"family":"Wang","given":"Ning","email":"nwang@usgs.gov","affiliations":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"preferred":true,"id":351976,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mebane, Christopher A. 0000-0002-9089-0267 cmebane@usgs.gov","orcid":"https://orcid.org/0000-0002-9089-0267","contributorId":110,"corporation":false,"usgs":true,"family":"Mebane","given":"Christopher","email":"cmebane@usgs.gov","middleInitial":"A.","affiliations":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"preferred":true,"id":351973,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kunz, James L. 0000-0002-1027-158X jkunz@usgs.gov","orcid":"https://orcid.org/0000-0002-1027-158X","contributorId":3309,"corporation":false,"usgs":true,"family":"Kunz","given":"James","email":"jkunz@usgs.gov","middleInitial":"L.","affiliations":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"preferred":true,"id":351977,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ingersoll, Christopher G. 0000-0003-4531-5949 cingersoll@usgs.gov","orcid":"https://orcid.org/0000-0003-4531-5949","contributorId":2071,"corporation":false,"usgs":true,"family":"Ingersoll","given":"Christopher","email":"cingersoll@usgs.gov","middleInitial":"G.","affiliations":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"preferred":true,"id":351975,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Brumbaugh, William G. 0000-0003-0081-375X bbrumbaugh@usgs.gov","orcid":"https://orcid.org/0000-0003-0081-375X","contributorId":493,"corporation":false,"usgs":true,"family":"Brumbaugh","given":"William","email":"bbrumbaugh@usgs.gov","middleInitial":"G.","affiliations":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"preferred":true,"id":351974,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Santore, Robert C.","contributorId":53206,"corporation":false,"usgs":true,"family":"Santore","given":"Robert","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":351978,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Gorsuch, Joseph W.","contributorId":76975,"corporation":false,"usgs":true,"family":"Gorsuch","given":"Joseph","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":351979,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Arnold, W. Ray","contributorId":102721,"corporation":false,"usgs":true,"family":"Arnold","given":"W.","email":"","middleInitial":"Ray","affiliations":[],"preferred":false,"id":351980,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":70005572,"text":"70005572 - 2011 - Influence of body condition on influenza A virus infection in mallard ducks: Experimental infection data","interactions":[],"lastModifiedDate":"2023-10-16T19:03:49.696105","indexId":"70005572","displayToPublicDate":"2012-05-21T10:18:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2980,"text":"PLoS ONE","active":true,"publicationSubtype":{"id":10}},"title":"Influence of body condition on influenza A virus infection in mallard ducks: Experimental infection data","docAbstract":"<p>Migrating waterfowl are implicated in the global spread of influenza A viruses (IAVs), and mallards (<i>Anas platyrhynchos</i>) are considered a particularly important IAV reservoir. Prevalence of IAV infection in waterfowl peaks during autumn pre-migration staging and then declines as birds reach wintering areas. Migration is energetically costly and birds often experience declines in body condition that may suppress immune function. We assessed how body condition affects susceptibility to infection, viral shedding and antibody production in wild-caught and captive-bred juvenile mallards challenged with low pathogenic avian influenza virus (LPAIV) H5N9. Wild mallards (n = 30) were separated into three experimental groups; each manipulated through food availability to a different condition level (-20%, -10%, and normal &plusmn;5% original body condition), and captive-bred mallards (n = 10) were maintained at normal condition. We found that wild mallards in normal condition were more susceptible to LPAIV infection, shed higher peak viral loads and shed viral RNA more frequently compared to birds in poor condition. Antibody production did not differ according to condition. We found that wild mallards did not differ from captive-bred mallards in viral intensity and duration of infection, but they did exhibit lower antibody titers and greater variation in viral load. Our findings suggest that reduced body condition negatively influences waterfowl host competence to LPAIV infection. This observation is contradictory to the recently proposed condition-dependent hypothesis, according to which birds in reduced condition would be more susceptible to IAV infection. The mechanisms responsible for reducing host competency among birds in poor condition remain unknown. Our research indicates body condition may influence the maintenance and spread of LPAIV by migrating waterfowl.</p>","language":"English","publisher":"Public Library of Science","publisherLocation":"San Francisco, CA","doi":"10.1371/journal.pone.0022633","usgsCitation":"Arsnoe, D.M., Ip, S., and Owen, J.C., 2011, Influence of body condition on influenza A virus infection in mallard ducks: Experimental infection data: PLoS ONE, v. 6, no. 8, e22633, 9 p., https://doi.org/10.1371/journal.pone.0022633.","productDescription":"e22633, 9 p.","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-026665","costCenters":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"links":[{"id":474737,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1371/journal.pone.0022633","text":"Publisher Index Page"},{"id":257016,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Michigan","otherGeospatial":"Lower Peninsula","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -86.94580078125,\n              41.73852846935917\n            ],\n            [\n              -83.353271484375,\n              41.65649719441145\n            ],\n            [\n              -83.067626953125,\n              42.2366518803206\n            ],\n            [\n              -82.55126953124999,\n              42.593532625649935\n            ],\n            [\n              -82.529296875,\n              44.134913443750726\n            ],\n            [\n              -83.14453125,\n              44.24519901522129\n            ],\n            [\n              -83.232421875,\n              45.44471679159555\n            ],\n            [\n              -84.3310546875,\n              45.81348649679971\n            ],\n            [\n              -85.0341796875,\n              45.82879925192134\n            ],\n            [\n              -85.49560546875,\n              45.36758436884978\n            ],\n            [\n              -86.06689453125,\n              45.259422036351694\n            ],\n            [\n              -86.4404296875,\n              44.69989765840318\n            ],\n            [\n              -86.748046875,\n              43.992814500489914\n            ],\n            [\n              -86.5283203125,\n              43.26120612479979\n            ],\n            [\n              -86.396484375,\n              42.50450285299051\n            ],\n            [\n              -86.77001953125,\n              41.96765920367816\n            ],\n            [\n              -86.94580078125,\n              41.73852846935917\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"6","issue":"8","noUsgsAuthors":false,"publicationDate":"2011-08-16","publicationStatus":"PW","scienceBaseUri":"505a3b14e4b0c8380cd621ed","contributors":{"authors":[{"text":"Arsnoe, Dustin M.","contributorId":64521,"corporation":false,"usgs":true,"family":"Arsnoe","given":"Dustin","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":352844,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ip, S. 0000-0003-4844-7533 hip@usgs.gov","orcid":"https://orcid.org/0000-0003-4844-7533","contributorId":727,"corporation":false,"usgs":true,"family":"Ip","given":"S.","email":"hip@usgs.gov","affiliations":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"preferred":true,"id":352843,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Owen, Jennifer C.","contributorId":74255,"corporation":false,"usgs":true,"family":"Owen","given":"Jennifer","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":352845,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70005574,"text":"70005574 - 2011 - Indicators and protocols for monitoring impacts of formal and informal trails in protected areas","interactions":[],"lastModifiedDate":"2012-05-30T01:01:38","indexId":"70005574","displayToPublicDate":"2012-05-21T10:11:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2479,"text":"Journal of Tourism and Leisure Studies","active":true,"publicationSubtype":{"id":10}},"title":"Indicators and protocols for monitoring impacts of formal and informal trails in protected areas","docAbstract":"Trails are a common recreation infrastructure in protected areas and their conditions affect the quality of natural resources and visitor experiences. Various trail impact indicators and assessment protocols have been developed in support of monitoring programs, which are often used for management decision-making or as part of visitor capacity management frameworks. This paper reviews common indicators and assessment protocols for three types of trails, surfaced formal trails, unsurfaced formal trails, and informal (visitor-created) trails. Monitoring methods and selected data from three U.S. National Park Service units are presented to illustrate some common trail impact indicators and assessment options.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Tourism and Leisure Studies","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Marion, J.L., and Leung, Y., 2011, Indicators and protocols for monitoring impacts of formal and informal trails in protected areas: Journal of Tourism and Leisure Studies, v. 17, no. 2, p. 215-236.","productDescription":"22 p.","startPage":"215","endPage":"236","numberOfPages":"22","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":257018,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":257009,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://rpts.tamu.edu/files/2011/09/JTLS.pdf#page=128","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","volume":"17","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3a89e4b0c8380cd61d67","contributors":{"authors":[{"text":"Marion, Jeffrey L.","contributorId":56322,"corporation":false,"usgs":true,"family":"Marion","given":"Jeffrey","email":"","middleInitial":"L.","affiliations":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"preferred":false,"id":352850,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Leung, Yu-Fai","contributorId":95730,"corporation":false,"usgs":true,"family":"Leung","given":"Yu-Fai","affiliations":[],"preferred":false,"id":352851,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70007273,"text":"70007273 - 2011 - Impacts of climate change on the growing season in the United States","interactions":[],"lastModifiedDate":"2012-05-30T01:01:38","indexId":"70007273","displayToPublicDate":"2012-05-21T09:17:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1421,"text":"Earth Interactions","active":true,"publicationSubtype":{"id":10}},"title":"Impacts of climate change on the growing season in the United States","docAbstract":"Understanding the effects of climate change on the vegetative growing season is key to quantifying future hydrologic water budget conditions. The U.S. Geological Survey modeled changes in future growing season length at 14 basins across 11 states. Simulations for each basin were generated using five general circulation models with three emission scenarios as inputs to the Precipitation-Runoff Modeling System (PRMS). PRMS is a deterministic, distributed-parameter, watershed model developed to simulate the effects of various combinations of precipitation, climate, and land use on watershed response. PRMS was modified to include a growing season calculation in this study. The growing season was examined for trends in the total length (annual), as well as changes in the timing of onset (spring) and the end (fall) of the growing season. The results showed an increase in the annual growing season length in all 14 basins, averaging 27&ndash;47 days for the three emission scenarios. The change in the spring and fall growing season onset and end varied across the 14 basins, with larger increases in the total length of the growing season occurring in the mountainous regions and smaller increases occurring in the Midwest, Northeast, and Southeast regions. The Clear Creek basin, 1 of the 14 basins in this study, was evaluated to examine the growing season length determined by emission scenario, as compared to a growing season length fixed baseline condition. The Clear Creek basin showed substantial variation in hydrologic responses, including streamflow, as a result of growing season length determined by emission scenario.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Earth Interactions","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"American Meteorological Society","publisherLocation":"Boston, MA","doi":"10.1175/2011EI376.1","usgsCitation":"Markstrom, S., and Hay, L.E., 2011, Impacts of climate change on the growing season in the United States: Earth Interactions, v. 15, p. 1-17, https://doi.org/10.1175/2011EI376.1.","productDescription":"17 p.","startPage":"1","endPage":"17","costCenters":[{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true}],"links":[{"id":474739,"rank":101,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1175/2011ei376.1","text":"Publisher Index Page"},{"id":257007,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":256997,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://dx.doi.org/10.1175/2011EI376.1","linkFileType":{"id":5,"text":"html"}}],"country":"United States","volume":"15","noUsgsAuthors":false,"publicationDate":"2011-12-31","publicationStatus":"PW","scienceBaseUri":"505a38e7e4b0c8380cd61720","contributors":{"authors":[{"text":"Markstrom, Steven L. 0000-0001-7630-9547 markstro@usgs.gov","orcid":"https://orcid.org/0000-0001-7630-9547","contributorId":1986,"corporation":false,"usgs":true,"family":"Markstrom","given":"Steven L.","email":"markstro@usgs.gov","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":false,"id":356209,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hay, Lauren E. 0000-0003-3763-4595 lhay@usgs.gov","orcid":"https://orcid.org/0000-0003-3763-4595","contributorId":1287,"corporation":false,"usgs":true,"family":"Hay","given":"Lauren","email":"lhay@usgs.gov","middleInitial":"E.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":356208,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70006333,"text":"70006333 - 2011 - Habitat use and movement of the endangered Arroyo Toad (<i>Anaxyrus californicus</i>) in coastal southern California","interactions":[],"lastModifiedDate":"2012-05-30T01:01:38","indexId":"70006333","displayToPublicDate":"2012-05-21T09:02:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2334,"text":"Journal of Herpetology","active":true,"publicationSubtype":{"id":10}},"title":"Habitat use and movement of the endangered Arroyo Toad (<i>Anaxyrus californicus</i>) in coastal southern California","docAbstract":"Information on the habitat use and movement patterns of Arroyo Toads (<i>Anaxyrus californicus</i>) is limited. The temporal and spatial characteristics of terrestrial habitat use, especially as it relates to upland use in coastal areas of the species' range, are poorly understood. We present analyses of radiotelemetry data from 40 individual adult toads tracked at a single site in coastal southern California from March through November of 2004. We quantify adult Arroyo Toad habitat use and movements and interpret results in the context of their life history. We show concentrated activity by both male and female toads along stream terraces during and after breeding, and, although our fall sample size is low, the continued presence of adult toads in the floodplain through the late fall. Adult toads used open sandy flats with sparse vegetation. Home-range size and movement frequency varied as a function of body mass. Observed spatial patterns of movement and habitat use both during and outside of the breeding period as well as available climatological data suggest that overwintering of toads in floodplain habitats of near-coastal areas of southern California may be more common than previously considered. If adult toads are not migrating out of the floodplain at the close of the breeding season but instead overwinter on stream terraces in near-coastal areas, then current management practices that assume toad absence from floodplain habitats may be leaving adult toads over-wintering on stream terraces vulnerable to human disturbance during a time of year when Arroyo Toad mortality is potentially highest.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Herpetology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"The Society for the Study of Amphibians and Reptiles","doi":"10.1670/10-160.1","usgsCitation":"Gallegos, E., Lyren, L.M., Lovich, R., Mitrovich, M.J., and Fisher, R.N., 2011, Habitat use and movement of the endangered Arroyo Toad (<i>Anaxyrus californicus</i>) in coastal southern California: Journal of Herpetology, v. 45, no. 3, p. 319-328, https://doi.org/10.1670/10-160.1.","productDescription":"10 p.","startPage":"319","endPage":"328","numberOfPages":"10","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":257003,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":256996,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://dx.doi.org/10.1670/10-160.1","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"California","volume":"45","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a2f32e4b0c8380cd5cb8f","contributors":{"authors":[{"text":"Gallegos, Elizabeth 0000-0002-8402-2631 egallegos@usgs.gov","orcid":"https://orcid.org/0000-0002-8402-2631","contributorId":1528,"corporation":false,"usgs":true,"family":"Gallegos","given":"Elizabeth","email":"egallegos@usgs.gov","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":true,"id":354314,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lyren, Lisa M. llyren@usgs.gov","contributorId":2398,"corporation":false,"usgs":true,"family":"Lyren","given":"Lisa","email":"llyren@usgs.gov","middleInitial":"M.","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":true,"id":354316,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lovich, Robert E.","contributorId":73857,"corporation":false,"usgs":true,"family":"Lovich","given":"Robert E.","affiliations":[],"preferred":false,"id":354317,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Mitrovich, Milan J.","contributorId":88864,"corporation":false,"usgs":true,"family":"Mitrovich","given":"Milan","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":354318,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Fisher, Robert N. 0000-0002-2956-3240 rfisher@usgs.gov","orcid":"https://orcid.org/0000-0002-2956-3240","contributorId":1529,"corporation":false,"usgs":true,"family":"Fisher","given":"Robert","email":"rfisher@usgs.gov","middleInitial":"N.","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":true,"id":354315,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70006297,"text":"70006297 - 2011 - Formation of nanocolloidal metacinnabar in mercury-DOM-sulfide systems","interactions":[],"lastModifiedDate":"2020-01-11T10:15:47","indexId":"70006297","displayToPublicDate":"2012-05-21T08:44:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1565,"text":"Environmental Science & Technology","onlineIssn":"1520-5851","printIssn":"0013-936X","active":true,"publicationSubtype":{"id":10}},"title":"Formation of nanocolloidal metacinnabar in mercury-DOM-sulfide systems","docAbstract":"<p><span>Direct determination of mercury (Hg) speciation in sulfide-containing environments is confounded by low mercury concentrations and poor analytical sensitivity. Here we report the results of experiments designed to assess mercury speciation at environmentally relevant ratios of mercury to dissolved organic matter (DOM) (i.e., &lt;4 nmol Hg (mg DOM)</span><sup>−1</sup><span>) by combining solid phase extraction using C</span><sub>18</sub><span><span>&nbsp;</span>resin with extended X-ray absorption fine structure (EXAFS) spectroscopy. Aqueous Hg(II) and a DOM isolate were equilibrated in the presence and absence of 100 μM total sulfide. In the absence of sulfide, mercury adsorption to the resin increased as the Hg:DOM ratio decreased and as the strength of Hg-DOM binding increased. EXAFS analysis indicated that in the absence of sulfide, mercury bonds with an average of 2.4 ± 0.2 sulfur atoms with a bond length typical of mercury-organic thiol ligands (2.35 Å). In the presence of sulfide, mercury showed greater affinity for the C</span><sub>18</sub><span><span>&nbsp;</span>resin, and its chromatographic behavior was independent of Hg:DOM ratio. EXAFS analysis showed mercury–sulfur bonds with a longer interatomic distance (2.51–2.53 Å) similar to the mercury–sulfur bond distance in metacinnabar (2.53 Å) regardless of the Hg:DOM ratio. For all samples containing sulfide, the sulfur coordination number was below the ideal four-coordinate structure of metacinnabar. At a low Hg:DOM ratio where strong binding DOM sites may control mercury speciation (1.9 nmol mg</span><sup>–1</sup><span>) mercury was coordinated by 2.3 ± 0.2 sulfur atoms, and the coordination number rose with increasing Hg:DOM ratio. The less-than-ideal coordination numbers indicate metacinnabar-like species on the nanometer scale, and the positive correlation between Hg:DOM ratio and sulfur coordination number suggests progressively increasing particle size or crystalline order with increasing abundance of mercury with respect to DOM. In DOM-containing sulfidic systems nanocolloidal metacinnabar-like species may form, and these species need to be considered when addressing mercury biogeochemistry.</span></p>","language":"English","publisher":"ACS Publications","doi":"10.1021/es201837h","usgsCitation":"Gerbig, C., Kim, C., Stegemeier, J., Ryan, J.N., and Aiken, G.R., 2011, Formation of nanocolloidal metacinnabar in mercury-DOM-sulfide systems: Environmental Science & Technology, v. 45, no. 21, p. 9180-9187, https://doi.org/10.1021/es201837h.","productDescription":"8 p.","startPage":"9180","endPage":"9187","numberOfPages":"8","costCenters":[{"id":145,"text":"Branch of Regional Research-Central Region","active":false,"usgs":true},{"id":381,"text":"Mercury Research Laboratory","active":false,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":257001,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"45","issue":"21","noUsgsAuthors":false,"publicationDate":"2011-09-30","publicationStatus":"PW","scienceBaseUri":"505a1354e4b0c8380cd54603","contributors":{"authors":[{"text":"Gerbig, Chase A.","contributorId":63246,"corporation":false,"usgs":true,"family":"Gerbig","given":"Chase A.","affiliations":[],"preferred":false,"id":354254,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kim, Christopher S.","contributorId":69258,"corporation":false,"usgs":true,"family":"Kim","given":"Christopher S.","affiliations":[],"preferred":false,"id":354255,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stegemeier, John P.","contributorId":45151,"corporation":false,"usgs":true,"family":"Stegemeier","given":"John P.","affiliations":[],"preferred":false,"id":354252,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ryan, Joseph N.","contributorId":54290,"corporation":false,"usgs":false,"family":"Ryan","given":"Joseph","email":"","middleInitial":"N.","affiliations":[{"id":604,"text":"University of Colorado- Boulder","active":false,"usgs":true}],"preferred":false,"id":354253,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Aiken, George R. 0000-0001-8454-0984 graiken@usgs.gov","orcid":"https://orcid.org/0000-0001-8454-0984","contributorId":1322,"corporation":false,"usgs":true,"family":"Aiken","given":"George","email":"graiken@usgs.gov","middleInitial":"R.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true},{"id":191,"text":"Colorado Water Science Center","active":true,"usgs":true}],"preferred":true,"id":354251,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70003560,"text":"70003560 - 2011 - Exhumation history of the NW Indian Himalaya revealed by fission track and 40Ar/39Ar ages","interactions":[],"lastModifiedDate":"2021-03-24T12:39:28.440962","indexId":"70003560","displayToPublicDate":"2012-05-20T11:43:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2184,"text":"Journal of Asian Earth Sciences","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Exhumation history of the NW Indian Himalaya revealed by fission track and <sup>40</sup>Ar/<sup>39</sup>Ar ages","title":"Exhumation history of the NW Indian Himalaya revealed by fission track and 40Ar/39Ar ages","docAbstract":"<p>New fission track and Ar/Ar geochronological data provide time constraints on the exhumation history of the Himalayan nappes in the Mandi (Beas valley) &mdash; Tso Morari transect of the NW Indian Himalaya. Results from this and previous studies suggest that the SW-directed North Himalayan nappes were emplaced by detachment from the underthrusted upper Indian crust by 55 Ma and metamorphosed by ca. 48&ndash;40 Ma. The nappe stack was subsequently exhumed to shallow upper crustal depths (<10 km) by 40&ndash;30 Ma in the Tso Morari dome (northern section of the transect) and by 30&ndash;20 Ma close to frontal thrusts in the Baralacha La region. From the Oligocene to the present, exhumation continued slowly.</p>\n<p>Metamorphism started in the High Himalayan nappe prior to the Late Oligocene.</p>\n<p>High temperatures and anatexis of the subducting upper Indian crust engendered the buoyancy-driven ductile detachment and extrusion of the High Himalayan nappe in the zone of continental collision. Late extrusion of the High Himalayan nappe started about 26 Ma ago, accompanied by ductile extensional shearing in the Zanskar shear zone in its roof between 22 and 19 Ma concomitant with thrusting along the basal Main Central Thrust to the south. The northern part of the nappe was then rapidly exhumed to shallow depth (<10 km) between 20 and 6 Ma, while its southern front reached this depth at 10&ndash;5 Ma.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.jseaes.2010.06.008","usgsCitation":"Schlup, M., Steck, A., Carter, A., Cosca, M., Epard, J., and Hunziker, J., 2011, Exhumation history of the NW Indian Himalaya revealed by fission track and 40Ar/39Ar ages: Journal of Asian Earth Sciences, v. 40, no. 1, p. 334-350, https://doi.org/10.1016/j.jseaes.2010.06.008.","productDescription":"17 p.","startPage":"334","endPage":"350","numberOfPages":"17","costCenters":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true},{"id":35995,"text":"Geology, Geophysics, and Geochemistry Science Center","active":true,"usgs":true}],"links":[{"id":256988,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"India","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              69.43359375,\n              7.710991655433217\n            ],\n            [\n              89.82421875,\n              7.710991655433217\n            ],\n            [\n              89.82421875,\n              34.161818161230386\n            ],\n            [\n              69.43359375,\n              34.161818161230386\n            ],\n            [\n              69.43359375,\n              7.710991655433217\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"40","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0daee4b0c8380cd5313a","contributors":{"authors":[{"text":"Schlup, Micha","contributorId":15048,"corporation":false,"usgs":true,"family":"Schlup","given":"Micha","email":"","affiliations":[],"preferred":false,"id":347740,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Steck, Albrecht","contributorId":35162,"corporation":false,"usgs":true,"family":"Steck","given":"Albrecht","email":"","affiliations":[],"preferred":false,"id":347742,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Carter, Andrew","contributorId":52821,"corporation":false,"usgs":true,"family":"Carter","given":"Andrew","email":"","affiliations":[],"preferred":false,"id":347744,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Cosca, Michael 0000-0002-0600-7663","orcid":"https://orcid.org/0000-0002-0600-7663","contributorId":33043,"corporation":false,"usgs":true,"family":"Cosca","given":"Michael","affiliations":[{"id":35995,"text":"Geology, Geophysics, and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":347741,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Epard, Jean-Luc","contributorId":47620,"corporation":false,"usgs":true,"family":"Epard","given":"Jean-Luc","email":"","affiliations":[],"preferred":false,"id":347743,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Hunziker, Johannes","contributorId":103910,"corporation":false,"usgs":true,"family":"Hunziker","given":"Johannes","email":"","affiliations":[],"preferred":false,"id":347745,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70005855,"text":"70005855 - 2011 - Evaluating the potential for stock size to limit recruitment in largemouth bass","interactions":[],"lastModifiedDate":"2012-05-29T01:01:35","indexId":"70005855","displayToPublicDate":"2012-05-20T09:46:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3624,"text":"Transactions of the American Fisheries Society","active":true,"publicationSubtype":{"id":10}},"title":"Evaluating the potential for stock size to limit recruitment in largemouth bass","docAbstract":"Compensatory changes in juvenile survival allow fish stocks to maintain relatively constant recruitment across a wide range of stock sizes (and levels of fishing), but few studies have experimentally explored recruitment compensation in fish populations. We evaluated the potential for recruitment compensation in largemouth bass <i>Micropterus salmoides</i> by stocking six 0.4-ha hatchery ponds with adult densities ranging from 6 to 40 fish over 2 years. Ponds were drained in October each year, and the age-0 fish densities were used as a measure of recruitment. We found no relationship between stock abundance and recruitment; ponds with low adult densities produced nearly as many recruits as the higher-density ponds in some cases. Both prey abundance and the growth of age-0 largemouth bass declined with age-0 fish density. Recruit abundance was highly variable both within and among the adult density groups, and thus we were unable to identify a clear stock&ndash;recruit relationship for largemouth bass. Our results indicate that reducing the number of effective spawners via angling practices would not reduce recruitment over a relatively large range in stock size.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Transactions of the American Fisheries Society","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Taylor and Francis","publisherLocation":"Philadelphia, PA","doi":"10.1080/00028487.2011.599259","usgsCitation":"Allen, M.S., Rogers, M.W., Catalano, M.J., Gwinn, D.G., and Walsh, S.J., 2011, Evaluating the potential for stock size to limit recruitment in largemouth bass: Transactions of the American Fisheries Society, v. 140, no. 4, p. 1093-1100, https://doi.org/10.1080/00028487.2011.599259.","productDescription":"8 p.","startPage":"1093","endPage":"1100","costCenters":[{"id":566,"text":"Southeast Ecological Science Center","active":true,"usgs":true}],"links":[{"id":256981,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":256979,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://dx.doi.org/10.1080/00028487.2011.599259","linkFileType":{"id":5,"text":"html"}}],"volume":"140","issue":"4","noUsgsAuthors":false,"publicationDate":"2011-08-19","publicationStatus":"PW","scienceBaseUri":"505a0bfee4b0c8380cd529ad","contributors":{"authors":[{"text":"Allen, Michael S.","contributorId":67375,"corporation":false,"usgs":true,"family":"Allen","given":"Michael","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":353394,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rogers, Mark W. 0000-0001-7205-5623 mwrogers@usgs.gov","orcid":"https://orcid.org/0000-0001-7205-5623","contributorId":4590,"corporation":false,"usgs":true,"family":"Rogers","given":"Mark","email":"mwrogers@usgs.gov","middleInitial":"W.","affiliations":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true},{"id":198,"text":"Coop Res Unit Atlanta","active":true,"usgs":true}],"preferred":true,"id":353393,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Catalano, Mathew J.","contributorId":97780,"corporation":false,"usgs":true,"family":"Catalano","given":"Mathew","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":353396,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Gwinn, Daniel G.","contributorId":76607,"corporation":false,"usgs":true,"family":"Gwinn","given":"Daniel","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":353395,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Walsh, Stephen J. 0000-0002-1009-8537 swalsh@usgs.gov","orcid":"https://orcid.org/0000-0002-1009-8537","contributorId":1456,"corporation":false,"usgs":true,"family":"Walsh","given":"Stephen","email":"swalsh@usgs.gov","middleInitial":"J.","affiliations":[{"id":566,"text":"Southeast Ecological Science Center","active":true,"usgs":true},{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"preferred":true,"id":353392,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70005678,"text":"70005678 - 2011 - Evaluation of the horizontal-to-vertical spectral ratio (HVSR) seismic method to determine sediment thickness in the vicinity of the South Well Field, Franklin County, OH","interactions":[],"lastModifiedDate":"2013-03-17T16:16:00","indexId":"70005678","displayToPublicDate":"2012-05-20T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2938,"text":"Ohio Journal of Science","active":true,"publicationSubtype":{"id":10}},"title":"Evaluation of the horizontal-to-vertical spectral ratio (HVSR) seismic method to determine sediment thickness in the vicinity of the South Well Field, Franklin County, OH","docAbstract":"The horizontal-to-vertical spectral ratio (HVSR) seismic method involves analyzing measurements of ambient seismic noise in three dimensions to determine the fundamental site resonance frequency. Resonance is excited by the interaction of surface waves (Rayleigh and Love) and body waves (vertically incident shear) with the high-contrast aconstic impedance boundary at the bedrock-sediment interface. Measurements were made to determine the method's utility for estimating thickness of unconsolidated glacial sediments at 18 locations at the South Well Field, Franklin County, OH, and at six locations in Pickaway County where sediment thickness was already known. Measurements also were made near a high-capacity production well (with pumping on and off) and near a highway and a limestone quarry to examine changes in resonance frequencies over a 20-hour period. Although the regression relation for resonance frequency and sediment thickness had a relatively low [r.sup.2] (0.322), estimates of sediment thickness were, on average, within 14 percent of known thicknesses. Resonance frequencies for pumping on and pumping off were identical, although the amplitude of the peak was nearly double under pumping conditions. Resonance frequency for the 20-hour period did not change, but the amplitude of the peak changed considerably, with a maximum amplitude in the early afternoon and minimum in the very early morning hours. Clay layers within unconsolidated sediments may influence resonance frequency and the resulting regression equation, resulting in underestimation of sediment thickness; however, despite this and other complicating factors, hydrogeologists should consider this method when thickness data are needed for unconsolidated sediments.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Ohio Journal of Science","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Ohio Academy of Science","publisherLocation":"Reston, VA","usgsCitation":"Haefner, R.J., Sheets, R., and Andrews, R.E., 2011, Evaluation of the horizontal-to-vertical spectral ratio (HVSR) seismic method to determine sediment thickness in the vicinity of the South Well Field, Franklin County, OH: Ohio Journal of Science, v. 110, no. 4, p. 77-85.","productDescription":"9 p.","startPage":"77","endPage":"85","costCenters":[{"id":513,"text":"Ohio Water Science Center","active":true,"usgs":true}],"links":[{"id":256992,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":269504,"type":{"id":11,"text":"Document"},"url":"https://hdl.handle.net/1811/52793"}],"country":"United States","state":"Ohio","county":"Franklin","volume":"110","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0ce8e4b0c8380cd52d42","contributors":{"authors":[{"text":"Haefner, Ralph J. 0000-0002-4363-9010 rhaefner@usgs.gov","orcid":"https://orcid.org/0000-0002-4363-9010","contributorId":1793,"corporation":false,"usgs":true,"family":"Haefner","given":"Ralph","email":"rhaefner@usgs.gov","middleInitial":"J.","affiliations":[{"id":37947,"text":"Upper Midwest Water Science Center","active":true,"usgs":true}],"preferred":true,"id":353057,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sheets, Rodney A. rasheets@usgs.gov","contributorId":1848,"corporation":false,"usgs":true,"family":"Sheets","given":"Rodney A.","email":"rasheets@usgs.gov","affiliations":[{"id":35860,"text":"Ohio-Kentucky-Indiana Water Science Center","active":true,"usgs":true}],"preferred":true,"id":353058,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Andrews, Robert E.","contributorId":103126,"corporation":false,"usgs":true,"family":"Andrews","given":"Robert","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":353059,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70038359,"text":"ds613 - 2011 - Concentrations and loads of nutrients in the tributaries of the Lake Okeechobee watershed, south-central Florida, water years 2004-2008","interactions":[],"lastModifiedDate":"2012-05-15T01:01:40","indexId":"ds613","displayToPublicDate":"2012-05-14T00:00:00","publicationYear":"2011","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":"613","title":"Concentrations and loads of nutrients in the tributaries of the Lake Okeechobee watershed, south-central Florida, water years 2004-2008","docAbstract":"Lake Okeechobee in south-central Florida is the second largest freshwater lake in the contiguous United States. Excessive phosphorus loading, harmful high and low water levels, and rapid expansion of non-native vegetation have threatened the health of the lake in recent decades. A study was conducted to monitor discharge and nutrient concentrations from selected tributaries into Lake Okeechobee and to evaluate nutrient loads. The data analysis was performed at 16 monitoring stations from December 2003 to September 2008. Annual and seasonal discharge measured at monitoring stations is affected by rainfall. Hurricanes affected three wet years (2004, 2005, and the latter part of 2008) and resulted in substantially greater discharge than the drought years of 2006, 2007, and the early part of 2008. Rainfall supplies about 50 percent of the water to Lake Okeechobee, discharge from the Kissimmee River supplies about 25 percent, and discharge from tributaries and groundwater seepage along the lake perimeter collectively provide the remaining 25 percent. Annually, tributary discharge from basins located on the west side of the Kissimmee River is about 5 to 6 times greater than that from basins located on the east side. For the purposes of this study, the basins on the east side of the Kissimmee River are called \"priority basins\" because of elevated phosphorus concentrations, while those on the west side are called \"nonpriority\" basins. Total annual discharge in the non-priority basins ranged from 245,000 acre-feet (acre-ft) in 2007 to 1,322,000 acre-ft in 2005, while annual discharge from the priority basins ranged from 41,000 acre-ft in 2007 to 219,000 acre-ft in 2005. Mean total phosphorus concentrations ranged from 0.10 to 0.54 milligrams per liter (mg/L) at the 16 tributaries during 2004&ndash;2008. Mean concentrations were significantly higher at priority basin sites than at non-priority basin sites, particularly at Arbuckle Creek and C 41A Canal. Concentrations of organic nitrogen plus ammonia ranged from 1.27 to 2.96 mg/L at the 16 tributaries during 2004&ndash;2008. Mean concentrations were highest at Fisheating Creek at Lake Placid (a non-priority site), and lowest at Wolff Creek, Taylor Creek near Grassy Island, and Otter Creek (three priority basin sites), and at Arbuckle Creek (a non-priority basin site). Mean concentrations of nitrite plus nitrate ranged from 0.01 to 0.55 mg/L at the 16 tributaries during 2004&ndash;2008. Mean concentrations measured in priority basins were significantly higher than those measured in non-priority basins. Nutrient concentrations were substantially lower in the non-priority basins; however, total loads were substantially higher due to discharge that was 5 to 6 times greater than from the priority basins. Total phosphorus, organic nitrogen plus ammonia, and nitrite plus nitrate loads from the non-priority basins were 1.5, 4.5, and 3.5 times greater, respectively, than were loads from the priority basins. In the non-priority basins, total phosphorus loads ranged from 35 metric tons (MT) in 2007 to 247 MT in 2005. In the priority basins, the loads ranged from 18 MT in 2007 to 136 MT in 2005. In the non-priority basins, organic nitrogen plus ammonia loads ranged from 337 MT in 2007 to 2,817 MT in 2005. In the priority basins, organic nitrogen plus ammonia loads ranged from 85 MT in 2007 to 503 MT in 2005. In the non-priority basins, nitrite plus nitrate loads ranged from 34 MT in 2007 to 143 MT in 2005. In the priority basins, nitrite plus nitrate loads ranged from 4 MT in 2007 to 27 MT in 2005.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ds613","collaboration":"Prepared in cooperation with U.S. Army Corps of Engineers, South Florida Water Management District, and Florida Department of Agriculture and Consumer Services","usgsCitation":"Byrne, M., and Wood, M.S., 2011, Concentrations and loads of nutrients in the tributaries of the Lake Okeechobee watershed, south-central Florida, water years 2004-2008: U.S. Geological Survey Data Series 613, v, 22 p., https://doi.org/10.3133/ds613.","productDescription":"v, 22 p.","startPage":"i","endPage":"22","numberOfPages":"27","onlineOnly":"Y","additionalOnlineFiles":"N","temporalStart":"2003-12-01","temporalEnd":"2008-09-30","costCenters":[{"id":285,"text":"Florida Water Science Center","active":false,"usgs":true}],"links":[{"id":254771,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ds_613.jpg"},{"id":254761,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/ds/613/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Florida","otherGeospatial":"Lake Okeechobee Watershed","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f988e4b0c8380cd4d665","contributors":{"authors":[{"text":"Byrne, Michael J.","contributorId":8550,"corporation":false,"usgs":true,"family":"Byrne","given":"Michael J.","affiliations":[],"preferred":false,"id":463960,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wood, Molly S. 0000-0002-5184-8306 mswood@usgs.gov","orcid":"https://orcid.org/0000-0002-5184-8306","contributorId":788,"corporation":false,"usgs":true,"family":"Wood","given":"Molly","email":"mswood@usgs.gov","middleInitial":"S.","affiliations":[{"id":502,"text":"Office of Surface Water","active":true,"usgs":true},{"id":37786,"text":"WMA - Observing Systems Division","active":true,"usgs":true},{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"preferred":true,"id":463959,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70037782,"text":"70037782 - 2011 - Estimating water supply arsenic levels in the New England bladder cancer study","interactions":[],"lastModifiedDate":"2012-05-17T01:01:41","indexId":"70037782","displayToPublicDate":"2012-05-08T08:40:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1542,"text":"Environmental Health Perspectives","active":true,"publicationSubtype":{"id":10}},"title":"Estimating water supply arsenic levels in the New England bladder cancer study","docAbstract":"<p>Background: Ingestion of inorganic arsenic in drinking water is recognized as a cause of bladder cancer when levels are relatively high (&ge; 150 &mu;g/L). The epidemiologic evidence is less clear at the low-to-moderate concentrations typically observed in the United States. Accurate retrospective exposure assessment over a long time period is a major challenge in conducting epidemiologic studies of environmental factors and diseases with long latency, such as cancer.</p>\n<p>Objective: We estimated arsenic concentrations in the water supplies of 2,611 participants in a population-based case&ndash;control study in northern New England.</p>\n<p>Methods: Estimates covered the lifetimes of most study participants and were based on a combination of arsenic measurements at the homes of the participants and statistical modeling of arsenic concentrations in the water supply of both past and current homes. We assigned a residential water supply arsenic concentration for 165,138 (95%) of the total 173,361 lifetime exposure years (EYs) and a workplace water supply arsenic level for 85,195 EYs (86% of reported occupational years).</p>\n<p>Results: Three methods accounted for 93% of the residential estimates of arsenic concentration: direct measurement of water samples (27%; median, 0.3 &mu;g/L; range, 0.1&ndash;11.5), statistical models of water utility measurement data (49%; median, 0.4 &mu;g/L; range, 0.3&ndash;3.3), and statistical models of arsenic concentrations in wells using aquifers in New England (17%; median, 1.6 &mu;g/L; range, 0.6&ndash;22.4).</p>\n<p>Conclusions: We used a different validation procedure for each of the three methods, and found our estimated levels to be comparable with available measured concentrations. This methodology allowed us to calculate potential drinking water exposure over long periods.</p>","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Environmental Health Perspectives","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"National Institute of Environmental Health Sciences","publisherLocation":"Research Triangle Park, NC","doi":"10.1289/ehp.1002345","usgsCitation":"Nuckols, J.R., Beane Freeman, L.E., Lubin, J.H., Airola, M.S., Baris, D., Ayotte, J., Taylor, A., Paulu, C., Karagas, M.R., Colt, J., Ward, M.H., Huang, A., Bress, W., Cherala, S., Silverman, D.T., and Cantor, K.P., 2011, Estimating water supply arsenic levels in the New England bladder cancer study: Environmental Health Perspectives, v. 119, no. 9, p. 1279-1285, https://doi.org/10.1289/ehp.1002345.","productDescription":"7 p.","startPage":"1279","endPage":"1285","costCenters":[{"id":468,"text":"New Hampshire-Vermont Water Science Center","active":false,"usgs":true}],"links":[{"id":474741,"rank":101,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1289/ehp.1002345","text":"Publisher Index Page"},{"id":256866,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":256857,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://dx.doi.org/10.1289/ehp.1002345","linkFileType":{"id":5,"text":"html"}}],"country":"United States","volume":"119","issue":"9","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0b6de4b0c8380cd52704","contributors":{"authors":[{"text":"Nuckols, John R.","contributorId":87037,"corporation":false,"usgs":true,"family":"Nuckols","given":"John","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":462714,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Beane Freeman, Laura E.","contributorId":69852,"corporation":false,"usgs":true,"family":"Beane Freeman","given":"Laura","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":462711,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lubin, Jay H.","contributorId":47251,"corporation":false,"usgs":true,"family":"Lubin","given":"Jay","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":462707,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Airola, Matthew S.","contributorId":72668,"corporation":false,"usgs":true,"family":"Airola","given":"Matthew","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":462712,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Baris, Dalsu","contributorId":102344,"corporation":false,"usgs":true,"family":"Baris","given":"Dalsu","affiliations":[],"preferred":false,"id":462717,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Ayotte, Joseph D. jayotte@usgs.gov","contributorId":1802,"corporation":false,"usgs":true,"family":"Ayotte","given":"Joseph D.","email":"jayotte@usgs.gov","affiliations":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":false,"id":462703,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Taylor, Anne","contributorId":76194,"corporation":false,"usgs":true,"family":"Taylor","given":"Anne","affiliations":[],"preferred":false,"id":462713,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Paulu, Chris","contributorId":30105,"corporation":false,"usgs":true,"family":"Paulu","given":"Chris","email":"","affiliations":[],"preferred":false,"id":462705,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Karagas, Margaret R.","contributorId":53247,"corporation":false,"usgs":true,"family":"Karagas","given":"Margaret","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":462709,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Colt, Joanne","contributorId":36021,"corporation":false,"usgs":true,"family":"Colt","given":"Joanne","affiliations":[],"preferred":false,"id":462706,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Ward, Mary H.","contributorId":92550,"corporation":false,"usgs":true,"family":"Ward","given":"Mary","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":462715,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Huang, An-Tsun","contributorId":58902,"corporation":false,"usgs":true,"family":"Huang","given":"An-Tsun","email":"","affiliations":[],"preferred":false,"id":462710,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Bress, William","contributorId":21832,"corporation":false,"usgs":true,"family":"Bress","given":"William","email":"","affiliations":[],"preferred":false,"id":462704,"contributorType":{"id":1,"text":"Authors"},"rank":13},{"text":"Cherala, Sai","contributorId":94555,"corporation":false,"usgs":true,"family":"Cherala","given":"Sai","email":"","affiliations":[],"preferred":false,"id":462716,"contributorType":{"id":1,"text":"Authors"},"rank":14},{"text":"Silverman, Debra T.","contributorId":105607,"corporation":false,"usgs":true,"family":"Silverman","given":"Debra","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":462718,"contributorType":{"id":1,"text":"Authors"},"rank":15},{"text":"Cantor, Kenneth P.","contributorId":47252,"corporation":false,"usgs":true,"family":"Cantor","given":"Kenneth","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":462708,"contributorType":{"id":1,"text":"Authors"},"rank":16}]}}
,{"id":70038127,"text":"70038127 - 2011 - Understanding interaction effects of climate change and fire management on bird distributions through combined process and habitat models","interactions":[],"lastModifiedDate":"2019-03-25T10:51:18","indexId":"70038127","displayToPublicDate":"2012-05-07T21:12:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1321,"text":"Conservation Biology","active":true,"publicationSubtype":{"id":10}},"title":"Understanding interaction effects of climate change and fire management on bird distributions through combined process and habitat models","docAbstract":"Avian conservation efforts must account for changes in vegetation composition and structure associated with climate change. We modeled vegetation change and the probability of occurrence of birds to project changes in winter bird distributions associated with climate change and fire management in the northern Chihuahuan Desert (southwestern U.S.A.). We simulated vegetation change in a process-based model (Landscape and Fire Simulator) in which anticipated climate change was associated with doubling of current atmospheric carbon dioxide over the next 50 years. We estimated the relative probability of bird occurrence on the basis of statistical models derived from field observations of birds and data on vegetation type, topography, and roads. We selected 3 focal species, Scaled Quail (<i>Callipepla squamata</i>), Loggerhead Shrike (<i>Lanius ludovicianus</i>), and Rock Wren (<i>Salpinctes obsoletus</i>), that had a range of probabilities of occurrence for our study area. Our simulations projected increases in relative probability of bird occurrence in shrubland and decreases in grassland and Yucca spp. and ocotillo (<i>Fouquieria splendens</i>) vegetation. Generally, the relative probability of occurrence of all 3 species was highest in shrubland because leaf-area index values were lower in shrubland. This high probability of occurrence likely is related to the species' use of open vegetation for foraging. Fire suppression had little effect on projected vegetation composition because as climate changed there was less fuel and burned area. Our results show that if future water limits on plant type are considered, models that incorporate spatial data may suggest how and where different species of birds may respond to vegetation changes.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Conservation Biology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Society for Conservation Biology","publisherLocation":"Washington, D.C.","doi":"10.1111/j.1523-1739.2011.01684.x","usgsCitation":"White, J., Gutzwiller, K.J., Barrow, W., Johnson-Randall, L., Zygo, L., and Swint, P., 2011, Understanding interaction effects of climate change and fire management on bird distributions through combined process and habitat models: Conservation Biology, v. 25, no. 3, p. 536-546, https://doi.org/10.1111/j.1523-1739.2011.01684.x.","productDescription":"11 p.","startPage":"536","endPage":"546","numberOfPages":"10","costCenters":[{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true}],"links":[{"id":256855,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","otherGeospatial":"Chihuahuan Desert","volume":"25","issue":"3","noUsgsAuthors":false,"publicationDate":"2011-04-28","publicationStatus":"PW","scienceBaseUri":"505bbc55e4b08c986b328b83","contributors":{"authors":[{"text":"White, Joseph D.","contributorId":56077,"corporation":false,"usgs":true,"family":"White","given":"Joseph D.","affiliations":[],"preferred":false,"id":463470,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gutzwiller, Kevin J.","contributorId":101923,"corporation":false,"usgs":true,"family":"Gutzwiller","given":"Kevin","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":463471,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Barrow, Wylie C. 0000-0003-4671-2823 barroww@usgs.gov","orcid":"https://orcid.org/0000-0003-4671-2823","contributorId":1988,"corporation":false,"usgs":true,"family":"Barrow","given":"Wylie C.","email":"barroww@usgs.gov","affiliations":[{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true}],"preferred":false,"id":463466,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Johnson-Randall, Lori 0000-0003-0100-994X","orcid":"https://orcid.org/0000-0003-0100-994X","contributorId":43604,"corporation":false,"usgs":true,"family":"Johnson-Randall","given":"Lori","affiliations":[{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"preferred":false,"id":463469,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Zygo, Lisa","contributorId":9898,"corporation":false,"usgs":true,"family":"Zygo","given":"Lisa","affiliations":[],"preferred":false,"id":463467,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Swint, Pamela","contributorId":32765,"corporation":false,"usgs":true,"family":"Swint","given":"Pamela","email":"","affiliations":[],"preferred":false,"id":463468,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70038312,"text":"sir20115172 - 2011 - Comparison of load estimation techniques and trend analysis for nitrogen, phosphorus, and suspended sediment in the Eucha-Spavinaw Basin, northwestern Arkansas and northeastern Oklahoma, 2002-10","interactions":[],"lastModifiedDate":"2020-02-26T17:27:02","indexId":"sir20115172","displayToPublicDate":"2012-05-07T14:02:00","publicationYear":"2011","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":"2011-5172","title":"Comparison of load estimation techniques and trend analysis for nitrogen, phosphorus, and suspended sediment in the Eucha-Spavinaw Basin, northwestern Arkansas and northeastern Oklahoma, 2002-10","docAbstract":"<p>The City of Tulsa, Oklahoma, uses water from Lake Eucha and Spavinaw Lake in the Eucha-Spavinaw basin of northwestern Arkansas and northeastern Oklahoma for public water supply. Increases in algal biomass, which cause taste and odor problems in drinking water produced from the lakes, may be attributable to increases in nitrogen and phosphorus concentrations in the lakes and in streams discharging to the lakes. To evaluate transport of nitrogen, phosphorus, and suspended sediment in this basin, loads and temporal trends were evaluated for five streamflow-gaging stations in the Spavinaw and Beaty Creek basins.</p>\n<p>Two approaches were used to develop regression equations for estimation of loads and yields of nitrogen, phosphorus, and sediment. The first approach used regression equations referred to as daily mean load (DM<sub>L</sub>) regressions, developed from water-quality samples and daily mean streamflow data collected from 2002 through 2010 at five streamflow-gaging stations in the basin. This approach was updated to compare loading results with those used in previous investigations. The second approach used regression equations, referred to as instantaneous continuous (INST<sub>C</sub>) regressions, developed from continuous measurements of physical water-quality constituents (specific conductance, temperature, and turbidity, and streamflow data) obtained from 2004 through 2010 to estimate loads of nitrogen, phosphorus, and sediment at two of the streamflow-gaging stations, Spavinaw Creek near Colcord, Okla., and Beaty Creek near Jay, Okla. Daily, annual, and mean annual loads estimated from these two regression methods were compared for the period 2005&ndash;10.</p>\n<p>Based on estimates obtained using DM<sub>L</sub> regressions, mean annual loads of 1,640,000 pounds of nitrogen, 99,900 pounds of phosphorus, and 116,000,000 pounds of sediment were transported into Lake Eucha from the Spavinaw and Beaty Creek basins. Estimated annual loads of nitrogen and phosphorus delivered to Lake Eucha from the Spavinaw and Beaty Creek basins during 2002&ndash;10 were 2.5 to 7.8 percent less, respectively, than the loads of those constituents discharged to Lake Eucha from 2002&ndash;09, indicating that nitrogen and phosphorus loads in 2010 were less than loads typical for the period 2002&ndash;09.</p>\n<p>Daily, annual, and mean annual load estimates varied substantially, depending on streamflow conditions and the independent variables used to develop regressions. Daily and annual loads estimated from INST<sub>C</sub> regressions that included turbidity, streamflow, temperature, specific conductance, and seasonality fit better with the field data than loads estimated from DM<sub>L</sub> regressions that included streamflow, seasonality, and time. Loads estimated from the INST<sub>C</sub> regression generally were greater than those estimated from the DM<sub>L</sub> regression. Relative percent differences in the mean annual total nitrogen load estimated by the INST<sub>C</sub> and DM<sub>L</sub> regressions were within 2 percent for Spavinaw Creek near Colcord, and Beaty Creek near Jay, Okla. The relative percent difference between the two types of regressions for estimates of mean annual total phosphorus loads at the two streamflow-gaging stations was 27.7 for Spavinaw Creek near Colcord, Okla., and only -2.6 percent for Beaty Creek near Jay, Okla. The relative percent difference between mean annual suspended-sediment loads at the streamflow-gaging stations was -38.6 percent for Spavinaw Creek near Colcord, Okla., and -122.7 percent for Beaty Creek near Jay, Okla. The DM<sub>L</sub> regression may have substantially underestimated phosphorus load at the Spavinaw Creek near Colcord, Okla., streamflow-gaging station in wet years and overestimated sediment load at both streamflow-gaging stations in wet years.</p>\n<p>Temporal trends in flow-adjusted nitrate-nitrogen, nitrogen, phosphorus, and suspended-sediment concentrations were analyzed for the five streamflow-gaging stations for the period 2001&ndash;10. No significant trends were observed for nitrate plus nitrite-nitrogen or total nitrogen concentrations at any streamflow-gaging station. There were significant upward trends in phosphorus concentrations in water samples collected during base-flow conditions at the Spavinaw Creek near Maysville, Okla., streamflow-gaging station and during runoff conditions for the Beaty Creek near Jay, Okla., streamflow-gaging station (3.5 to 4.2 percent per year). There were significant downward trends in phosphorus concentrations in base-flow and runoff samples collected at the Spavinaw Creek near Cherokee City, Sycamore, and Colcord, Okla., streamflow-gaging stations (-4.9 to -12.9 percent per year). There were significant downward trends in suspended-sediment concentration at the Spavinaw Creek near Maysville, and Sycamore, Okla., and the Beaty Creek near Jay, Okla., streamflow-gaging stations (-1.5 to -1.8 percent per year). No significant trends were detected in suspended-sediment concentration for the Spavinaw Creek near Cherokee City, and Colcord, Okla., streamflow-gaging stations.</p>\n<p>Possible causes for downward trends in phosphorus concentrations include decreases in phosphorus discharges from a wastewater-treatment plant upstream from the Spavinaw Creek near Cherokee City, Okla., streamflow-gaging station, and implementation of best management practices in the basin. Downward trends in sediment concentrations may be related to effects of best management practices in the basin.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20115172","collaboration":"Prepared in cooperation with the City of Tulsa, Oklahoma","usgsCitation":"Esralew, R.A., Andrews, W.J., Allen, M.L., and Becker, C., 2011, Comparison of load estimation techniques and trend analysis for nitrogen, phosphorus, and suspended sediment in the Eucha-Spavinaw Basin, northwestern Arkansas and northeastern Oklahoma, 2002-10: U.S. Geological Survey Scientific Investigations Report 2011-5172, viii, 60 p., https://doi.org/10.3133/sir20115172.","productDescription":"viii, 60 p.","numberOfPages":"68","temporalStart":"2002-01-01","temporalEnd":"2010-12-31","costCenters":[{"id":516,"text":"Oklahoma Water Science Center","active":true,"usgs":true}],"links":[{"id":254701,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/sir_2011_5172.gif"},{"id":254694,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/sir/2011/5172/SIR11-5172.pdf"}],"country":"United States","state":"Arkansas, Oklahoma","otherGeospatial":"Eucha-Pavinaw Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -95.08333333333333,36.2 ], [ -95.08333333333333,36.5 ], [ -94.25,36.5 ], [ -94.25,36.2 ], [ -95.08333333333333,36.2 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f86fe4b0c8380cd4d0d8","contributors":{"authors":[{"text":"Esralew, Rachel A.","contributorId":104862,"corporation":false,"usgs":true,"family":"Esralew","given":"Rachel","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":463846,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Andrews, William J. 0000-0003-4780-8835 wandrews@usgs.gov","orcid":"https://orcid.org/0000-0003-4780-8835","contributorId":328,"corporation":false,"usgs":true,"family":"Andrews","given":"William","email":"wandrews@usgs.gov","middleInitial":"J.","affiliations":[{"id":516,"text":"Oklahoma Water Science Center","active":true,"usgs":true}],"preferred":true,"id":463843,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Allen, Monica L.","contributorId":43065,"corporation":false,"usgs":true,"family":"Allen","given":"Monica","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":463845,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Becker, Carol 0000-0001-6652-4542 cjbecker@usgs.gov","orcid":"https://orcid.org/0000-0001-6652-4542","contributorId":2489,"corporation":false,"usgs":true,"family":"Becker","given":"Carol","email":"cjbecker@usgs.gov","affiliations":[{"id":516,"text":"Oklahoma Water Science Center","active":true,"usgs":true}],"preferred":true,"id":463844,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70006313,"text":"70006313 - 2011 - Effects of biologically-active chemical mixtures on fish in a wastewater-impacted urban stream","interactions":[],"lastModifiedDate":"2020-01-14T10:05:37","indexId":"70006313","displayToPublicDate":"2012-05-06T19:55:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3352,"text":"Science of the Total Environment","active":true,"publicationSubtype":{"id":10}},"title":"Effects of biologically-active chemical mixtures on fish in a wastewater-impacted urban stream","docAbstract":"Stream flow in urban aquatic ecosystems often is maintained by water-reclamation plant (WRP) effluents that contain mixtures of natural and anthropogenic chemicals that persist through the treatment processes. In effluent-impactedstreams, aquatic organisms such as fish are continuously exposed to biologically-activechemicals throughout their life cycles. The North Shore Channel of the Chicago River (Chicago, Illinois) is part of an urban ecosystem in which > 80% of the annual flow consists of effluent from the North Side WRP. In this study, multiple samplings of the effluent and stream water were conducted and fish (largemouth bass and carp) were collected on 2 occasions from the North Shore Channel. Fish also were collected once from the Outer Chicago Harbor in Lake Michigan, a reference site not impacted by WRP discharges. Over 100 organic chemicals with differing behaviors and biological effects were measured, and 23 compounds were detected in all of the water samples analyzed. The most frequently detected and highest concentration (> 100 &mu;g/L) compounds were ethylenediaminetetraacetic acid and 4-nonylphenolmono-to-tetraethoxycarboxylic acids. Other biologically-activechemicals including bisphenol A, 4-nonylphenol, 4-nonylphenolmono-to-tetraethoxylates, 4-<i>tert</i>-octylphenol, and 4-<i>tert</i>-octylphenolmono-to-tetraethoxylates were detected at lower concentrations (< 5 &mu;g/L). The biogenic steroidal hormones 17&beta;-estradiol, estrone, testosterone, 4-androstene-3,17-dione, and <i>cis</i>-androsterone were detected at even lower concentrations (< 0.005 &mu;g/L). There were slight differences in concentrations between the North Side WRP effluent and the North Shore Channel, indicating minimal in-stream attenuation. Fish populations are continuously exposed to mixtures of biologically-activechemicals because of the relative persistency of the chemicals with respect to stream hydraulic residence time, and the lack of a fresh water source for dilution. The majority of male fish exhibited vitellogenin induction, a physiological response consistent with exposure to estrogenic compounds. Tissue-level signs of reproductive disruption, such as ovatestis, were not observed.","language":"English","publisher":"Elsevier","doi":"10.1016/j.scitotenv.2011.06.039","usgsCitation":"Barber, L.B., Brown, G., Nettesheim, T.G., Murphy, E.W., Bartell, S.E., and Schoenfuss, H.L., 2011, Effects of biologically-active chemical mixtures on fish in a wastewater-impacted urban stream: Science of the Total Environment, v. 409, no. 22, p. 4720-4728, https://doi.org/10.1016/j.scitotenv.2011.06.039.","productDescription":"9 p.","startPage":"4720","endPage":"4728","numberOfPages":"8","costCenters":[{"id":145,"text":"Branch of Regional Research-Central Region","active":false,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":254779,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Illinois","city":"Chicago","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -88.5223388671875,\n              41.52502957323801\n            ],\n            [\n              -87.5885009765625,\n              41.52502957323801\n            ],\n            [\n              -87.5885009765625,\n              42.49640294093705\n            ],\n            [\n              -88.5223388671875,\n              42.49640294093705\n            ],\n            [\n              -88.5223388671875,\n              41.52502957323801\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"409","issue":"22","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0698e4b0c8380cd5130e","contributors":{"authors":[{"text":"Barber, Larry B. 0000-0002-0561-0831 lbbarber@usgs.gov","orcid":"https://orcid.org/0000-0002-0561-0831","contributorId":921,"corporation":false,"usgs":true,"family":"Barber","given":"Larry","email":"lbbarber@usgs.gov","middleInitial":"B.","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true},{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":354299,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brown, Gregory K.","contributorId":8984,"corporation":false,"usgs":true,"family":"Brown","given":"Gregory K.","affiliations":[],"preferred":false,"id":354300,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Nettesheim, Todd G.","contributorId":85848,"corporation":false,"usgs":true,"family":"Nettesheim","given":"Todd","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":354304,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Murphy, Elizabeth W.","contributorId":78999,"corporation":false,"usgs":true,"family":"Murphy","given":"Elizabeth","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":354303,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Bartell, Stephen E.","contributorId":54445,"corporation":false,"usgs":false,"family":"Bartell","given":"Stephen","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":354301,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Schoenfuss, Heiko L.","contributorId":76409,"corporation":false,"usgs":false,"family":"Schoenfuss","given":"Heiko","email":"","middleInitial":"L.","affiliations":[{"id":13317,"text":"Saint Cloud State University","active":true,"usgs":false}],"preferred":false,"id":354302,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70038055,"text":"70038055 - 2011 - Selective uptake and biological consequences of environmentally relevant antidepressant pharmaceutical exposures on male fathead minnows","interactions":[],"lastModifiedDate":"2021-05-27T18:20:33.233002","indexId":"70038055","displayToPublicDate":"2012-05-06T19:43:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":874,"text":"Aquatic Toxicology","active":true,"publicationSubtype":{"id":10}},"title":"Selective uptake and biological consequences of environmentally relevant antidepressant pharmaceutical exposures on male fathead minnows","docAbstract":"Antidepressant pharmaceuticals have been reported in wastewater effluent at the nanogram to low microgram-per-liter range, and include bupropion (BUP), fluoxetine (FLX), sertraline (SER), and venlafaxine (VEN). To assess the effects of antidepressants on reproductive anatomy, physiology, and behavior, adult male fathead minnows (<i>Pimeplwles promelas</i>) were exposed for 21 days either to a single concentration of the antidepressants FLX, SER, VEN, or BUP, or to an antidepressant mixture. The data demonstrated that exposure to VEN (305 ng/L and 1104 ng/L) and SER (5.2 ng/L) resulted in mortality. Anatomical alterations were noted within the testes of fish exposed to SER and FLX, both modulators of the neurotransmitter serotonin. Additionally, FLX at 28 ng/L induced vitellogenin in male fish&mdash;a common endpoint for estrogenic endocrine disruption. Significant alterations in male secondary sex characteristics were noted with single exposures. Effects of single compound exposures neither carried over, nor became additive in the antidepressant mixtures, and reproductive behavior was not affected. Analysis of brain tissues from the exposed fish suggested increased uptake of FLX, SER and BUP and minimal uptake of VEN when compared to exposure water concentrations. Furthermore, the only metabolite detected consistently in the brain tissues was norfluoxetine. Similar trends of uptake by brain tissue were observed when fish were exposed to antidepressant mixtures. The present study demonstrates that anatomy and physiology, but not reproductive behavior, can be disrupted by exposure to environmental concentrations of some antidepressants. The observation that antidepressant uptake into fish tissues is selective may have consequences on assessing the mode-of-action and effects of these compounds in future studies.","language":"English","publisher":"Elsevier","doi":"10.1016/j.aquatox.2011.03.011","usgsCitation":"Schultz, M.M., Painter, M.M., Bartell, S.E., Logue, A., Furlong, E.T., Werner, S.L., and Schoenfuss, H.L., 2011, Selective uptake and biological consequences of environmentally relevant antidepressant pharmaceutical exposures on male fathead minnows: Aquatic Toxicology, v. 104, no. 1-2, p. 38-47, https://doi.org/10.1016/j.aquatox.2011.03.011.","productDescription":"10 p.","startPage":"38","endPage":"47","costCenters":[{"id":140,"text":"Branch of Analytical Serv (National Water Quality Laboratory)","active":false,"usgs":true},{"id":452,"text":"National Water Quality Laboratory","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":386010,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"104","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b8ce2e4b08c986b318197","contributors":{"authors":[{"text":"Schultz, Melissa M.","contributorId":52013,"corporation":false,"usgs":true,"family":"Schultz","given":"Melissa","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":463355,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Painter, Meghan M.","contributorId":68145,"corporation":false,"usgs":true,"family":"Painter","given":"Meghan","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":463357,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bartell, Stephen E.","contributorId":54445,"corporation":false,"usgs":false,"family":"Bartell","given":"Stephen","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":463356,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Logue, Amanda","contributorId":9504,"corporation":false,"usgs":true,"family":"Logue","given":"Amanda","email":"","affiliations":[],"preferred":false,"id":463354,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Furlong, Edward T. 0000-0002-7305-4603 efurlong@usgs.gov","orcid":"https://orcid.org/0000-0002-7305-4603","contributorId":740,"corporation":false,"usgs":true,"family":"Furlong","given":"Edward","email":"efurlong@usgs.gov","middleInitial":"T.","affiliations":[{"id":5046,"text":"Branch of Analytical Serv (NWQL)","active":true,"usgs":true},{"id":503,"text":"Office of Water Quality","active":true,"usgs":true},{"id":27111,"text":"National Water Quality Program","active":true,"usgs":true},{"id":191,"text":"Colorado Water Science Center","active":true,"usgs":true}],"preferred":true,"id":463352,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Werner, Stephen L. slwerner@usgs.gov","contributorId":1199,"corporation":false,"usgs":true,"family":"Werner","given":"Stephen","email":"slwerner@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":true,"id":463353,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Schoenfuss, Heiko L.","contributorId":76409,"corporation":false,"usgs":false,"family":"Schoenfuss","given":"Heiko","email":"","middleInitial":"L.","affiliations":[{"id":13317,"text":"Saint Cloud State University","active":true,"usgs":false}],"preferred":false,"id":463358,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70110397,"text":"70110397 - 2011 - Topographic mapping data semantics through data conversion and enhancement","interactions":[],"lastModifiedDate":"2022-12-29T16:31:53.591135","indexId":"70110397","displayToPublicDate":"2012-05-05T15:38:24","publicationYear":"2011","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"chapter":"7","title":"Topographic mapping data semantics through data conversion and enhancement","docAbstract":"<p><span>This paper presents research on the semantics of topographic data for triples and ontologies to blend the capabilities of the Semantic Web and&nbsp;</span><i>The National Map</i><span>&nbsp;of the U.S. Geological Survey. Automated conversion of relational topographic data of several geographic sample areas to the triple data model standard resulted in relatively poor semantic associations. Further research employed vocabularies of feature type and spatial relation terms. A user interface was designed to model the capture of non-standard terms relevant to public users and to map those terms to existing data models of&nbsp;</span><i>The National Map</i><span>&nbsp;through the use of ontology. Server access for the study area triple stores was made publicly available, illustrating how the development of linked data may transform institutional policies to open government data resources to the public. This paper presents these data conversion and research techniques that were tested as open linked data concepts leveraged through a user-centered interface and open USGS server access to the public.</span></p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Geospatial semantics and the semantic web","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Springer","doi":"10.1007/978-1-4419-9446-2_7","usgsCitation":"Varanka, D., Carter, J., Usery, E.L., and Shoberg, T., 2011, Topographic mapping data semantics through data conversion and enhancement, chap. 7 <i>of</i> Geospatial semantics and the semantic web, v. 12, p. 145-162, https://doi.org/10.1007/978-1-4419-9446-2_7.","productDescription":"18 p.","startPage":"145","endPage":"162","ipdsId":"IP-021600","costCenters":[{"id":161,"text":"Center of Excellence for Geospatial Information Science (CEGIS)","active":false,"usgs":true},{"id":423,"text":"National Geospatial Program","active":true,"usgs":true}],"links":[{"id":287898,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"12","noUsgsAuthors":false,"publicationDate":"2011-05-10","publicationStatus":"PW","scienceBaseUri":"53ae7876e4b0abf75cf2d652","contributors":{"editors":[{"text":"Ashish, Naveen","contributorId":112824,"corporation":false,"usgs":false,"family":"Ashish","given":"Naveen","email":"","affiliations":[],"preferred":false,"id":509852,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Sheth, Amit P.","contributorId":113340,"corporation":false,"usgs":true,"family":"Sheth","given":"Amit","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":509853,"contributorType":{"id":2,"text":"Editors"},"rank":2}],"authors":[{"text":"Varanka, Dalia","contributorId":99654,"corporation":false,"usgs":true,"family":"Varanka","given":"Dalia","affiliations":[],"preferred":false,"id":494062,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Carter, Jonathan","contributorId":58947,"corporation":false,"usgs":true,"family":"Carter","given":"Jonathan","affiliations":[],"preferred":false,"id":494061,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Usery, E. Lynn 0000-0002-2766-2173 usery@usgs.gov","orcid":"https://orcid.org/0000-0002-2766-2173","contributorId":231,"corporation":false,"usgs":true,"family":"Usery","given":"E.","email":"usery@usgs.gov","middleInitial":"Lynn","affiliations":[{"id":423,"text":"National Geospatial Program","active":true,"usgs":true}],"preferred":true,"id":494059,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Shoberg, Thomas","contributorId":46012,"corporation":false,"usgs":true,"family":"Shoberg","given":"Thomas","affiliations":[],"preferred":false,"id":494060,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70038193,"text":"ofr20111225 - 2011 - Geologic map of Detrital, Hualapai, and Sacramento Valleys and surrounding areas, northwest Arizona","interactions":[],"lastModifiedDate":"2012-04-30T16:43:34","indexId":"ofr20111225","displayToPublicDate":"2012-04-25T16:47:00","publicationYear":"2011","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":"2011-1225","title":"Geologic map of Detrital, Hualapai, and Sacramento Valleys and surrounding areas, northwest Arizona","docAbstract":"A 1:250,000-scale geologic map and report covering the Detrital, Hualapai, and Sacramento valleys in northwest Arizona is presented for the purpose of improving understanding of the geology and geohydrology of the basins beneath those valleys. The map was compiled from existing geologic mapping, augmented by digital photogeologic reconnaissance mapping. The most recent geologic map for the area, and the only digital one, is the 1:1,000,000-scale Geologic Map of Arizona. The larger scale map presented here includes significantly more detailed geology than the Geologic Map of Arizona in terms of accuracy of geologic unit contacts, number of faults, fault type, fault location, and details of Neogene and Quaternary deposits. Many sources were used to compile the geology; the accompanying geodatabase includes a source field in the polygon feature class that lists source references for polygon features. The citations for the source field are included in the reference section.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20111225","usgsCitation":"Beard, L.S., Kennedy, J., Truini, M., and Felger, T., 2011, Geologic map of Detrital, Hualapai, and Sacramento Valleys and surrounding areas, northwest Arizona: U.S. Geological Survey Open-File Report 2011-1225, ii, 35 p.; Figures; Table; Map: 34.00 x 44.01 inches; GIS Data Downloads, https://doi.org/10.3133/ofr20111225.","productDescription":"ii, 35 p.; Figures; Table; Map: 34.00 x 44.01 inches; GIS Data Downloads","additionalOnlineFiles":"Y","costCenters":[{"id":670,"text":"Western Region Geology and Geophysics Field Science Center-Flagstaff","active":false,"usgs":true}],"links":[{"id":254604,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr_2011_1225.gif"},{"id":254594,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2011/1225/","linkFileType":{"id":5,"text":"html"}}],"scale":"250000","projection":"UTM Zone 12","datum":"NAD83","country":"United States","state":"Arizona","otherGeospatial":"Detrital Valley;Hualapai Valley;Sacramento Valley","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114.75,34.333333333333336 ], [ -114.75,36.166666666666664 ], [ -113.66666666666667,36.166666666666664 ], [ -113.66666666666667,34.333333333333336 ], [ -114.75,34.333333333333336 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a1a29e4b0c8380cd55b89","contributors":{"authors":[{"text":"Beard, L. Sue","contributorId":87607,"corporation":false,"usgs":true,"family":"Beard","given":"L.","email":"","middleInitial":"Sue","affiliations":[],"preferred":false,"id":463633,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kennedy, Jeffrey 0000-0002-3365-6589","orcid":"https://orcid.org/0000-0002-3365-6589","contributorId":101124,"corporation":false,"usgs":true,"family":"Kennedy","given":"Jeffrey","affiliations":[],"preferred":false,"id":463634,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Truini, Margot mtruini@usgs.gov","contributorId":599,"corporation":false,"usgs":true,"family":"Truini","given":"Margot","email":"mtruini@usgs.gov","affiliations":[{"id":128,"text":"Arizona Water Science Center","active":true,"usgs":true}],"preferred":true,"id":463631,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Felger, Tracey","contributorId":34758,"corporation":false,"usgs":true,"family":"Felger","given":"Tracey","affiliations":[],"preferred":false,"id":463632,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70038168,"text":"sim3184 - 2011 - Bedrock geologic map of Vermont","interactions":[],"lastModifiedDate":"2025-05-14T16:35:14.218768","indexId":"sim3184","displayToPublicDate":"2012-04-23T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":333,"text":"Scientific Investigations Map","code":"SIM","onlineIssn":"2329-132X","printIssn":"2329-1311","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"3184","title":"Bedrock geologic map of Vermont","docAbstract":"The Bedrock Geologic Map of Vermont is the result of a cooperative agreement between the U.S. Geological Survey (USGS) and the State of Vermont. The State's complex geology spans 1.4 billion years of Earth's history. The new map comes 50 years after the most recent map of the State by Charles G. Doll and others in 1961 and a full 150 years since the publication of the first geologic map of Vermont by Edward Hitchcock and others in 1861. At a scale of 1:100,000, the map shows an uncommon level of detail for State geologic maps. Mapped rock units are primarily based on lithology, or rock type, to facilitate derivative studies in multiple disciplines. The 1961 map was compiled from 1:62,500-scale or smaller maps. The current map was created to integrate more detailed (1:12,000- to 1:24,000-scale) modern and older (1:62,500-scale) mapping with the theory of plate tectonics to provide a framework for geologic, tectonic, economic, hydrogeologic, and environmental characterization of the bedrock of Vermont. The printed map consists of three oversize sheets (52 x 76 inches). Sheets 1 and 2 show the southern and northern halves of Vermont, respectively, and can be trimmed and joined so that the entire State can be displayed as a single entity. These sheets also include 10 cross sections and a geologic structure map. Sheet 3 on the front consists of descriptions of 486 map units, a correlation of map units, and references cited. Sheet 3 on the back features a list of the 195 sources of geologic map data keyed to an index map of 7.5-minute quadrangles in Vermont, as well as a table identifying ages of rocks dated by uranium-lead zircon geochronology.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sim3184","collaboration":"Prepared in cooperation with the  State of Vermont, Vermont Agency of Natural Resources, Vermont Geological Survey","usgsCitation":"Ratcliffe, N.M., Stanley, R.S., Gale, M.H., Thompson, P.J., and Walsh, G.J., 2011, Bedrock geologic map of Vermont: U.S. Geological Survey Scientific Investigations Map 3184, 3 Sheets: 77.00 x 54.00 inches; Downloads Directory, https://doi.org/10.3133/sim3184.","productDescription":"3 Sheets: 77.00 x 54.00 inches; Downloads Directory","onlineOnly":"N","additionalOnlineFiles":"Y","costCenters":[{"id":595,"text":"U.S. Geological 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contributions by Norman L. Hatch Jr., Douglas W. Rankin, Barry L. Doolan, Jonathan Kim, Charlotte J. Mehrtens, John N. Aleinikoff, and J. Gregory McHone. Cartography by Linda M. 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