{"pageNumber":"2849","pageRowStart":"71200","pageSize":"25","recordCount":184582,"records":[{"id":70025506,"text":"70025506 - 2003 - Bedload transport in alluvial channels","interactions":[],"lastModifiedDate":"2012-03-12T17:21:00","indexId":"70025506","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2338,"text":"Journal of Hydraulic Engineering","active":true,"publicationSubtype":{"id":10}},"title":"Bedload transport in alluvial channels","docAbstract":"Hydraulic, sediment, land-use, and rock-erosivity data of 22 alluvial streams were used to evaluate conditions of bedload transport and the performance of selected bedload-transport equations. Transport categories of transport-limited (TL), partially transport-limited (PTL), and supply-limited (SL) were identified by a semiquantitative approach that considers hydraulic constraints on sediment movement and the processes that control sediment availability at the basin scale. Equations by Parker et al. in 1982, Schoklitsch in 1962, and Meyer-Peter and Muller in 1948 adequately predicted sediment transport in channels with TL condition, whereas the equations of Bagnold in 1980, and Schoklitsch, in 1962, performed well for PTL and SL conditions. Overall, the equation of Schoklitsch predicted well the measured bedload data for eight of 22 streams, and the Bagnold equation predicted the measured data in seven streams.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Hydraulic Engineering","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1061/(ASCE)0733-9429(2003)129:10(783)","issn":"07339429","usgsCitation":"Bravo-Espinosa, M., Osterkamp, W.R., and Lopes, V., 2003, Bedload transport in alluvial channels: Journal of Hydraulic Engineering, v. 129, no. 10, p. 783-795, https://doi.org/10.1061/(ASCE)0733-9429(2003)129:10(783).","startPage":"783","endPage":"795","numberOfPages":"13","costCenters":[],"links":[{"id":209494,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1061/(ASCE)0733-9429(2003)129:10(783)"},{"id":236008,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"129","issue":"10","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f042e4b0c8380cd4a6a8","contributors":{"authors":[{"text":"Bravo-Espinosa, M.","contributorId":31561,"corporation":false,"usgs":true,"family":"Bravo-Espinosa","given":"M.","email":"","affiliations":[],"preferred":false,"id":405451,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Osterkamp, W. R.","contributorId":46044,"corporation":false,"usgs":true,"family":"Osterkamp","given":"W.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":405452,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lopes, V.L.","contributorId":84963,"corporation":false,"usgs":true,"family":"Lopes","given":"V.L.","email":"","affiliations":[],"preferred":false,"id":405453,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70025501,"text":"70025501 - 2003 - Molecular status of the dusky Canada goose (Branta canadensis occidentalis): A genetic assessment of a translocation effort","interactions":[],"lastModifiedDate":"2018-07-17T09:44:39","indexId":"70025501","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1324,"text":"Conservation Genetics","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Molecular status of the dusky Canada goose (<i>Branta canadensis occidentalis</i>): A genetic assessment of a translocation effort","title":"Molecular status of the dusky Canada goose (Branta canadensis occidentalis): A genetic assessment of a translocation effort","docAbstract":"<p><span>Until recently, the dusky Canada goose (</span><i class=\"EmphasisTypeItalic \">Branta canadensis occidentalis</i><span>) was managedas one breeding population from the CopperRiver Delta (CRD), Alaska. Population numberson the CRD have declined precipitously over thelast three decades, due in part to changes inhabitat. In 1981, a pair of Canada geese,presumably<span>&nbsp;</span></span><i class=\"EmphasisTypeItalic \">B.c. occidentalis</i><span>, wasreported nesting on Middleton Island (MID), inthe Gulf of Alaska. Numbers of Canada geese onthe island increased in the decade subsequentto a translocation of geese from CRD to MID,but it is unclear whether the increase isattributable to the translocation effort. Weused genetic data derived from three classes ofgenetic markers to clarify relationships ofCanada geese breeding in south-coastal Alaska. Geese were sampled from 5 populations: CRD,MID, Anchorage (ANC), Admiralty Island (ADM) insoutheastern Alaska, and Green Island (GRN) inPrince William Sound (PWS). Mitochondrial DNAanalyses demonstrate Canada geese from MID arenearly monomorphic for a unique haplotype fixedon GRN but not found in CRD or any otherbreeding population. Furthermore, nuclearmarkers consistently cluster MID with GRN tothe exclusion of CRD. We suggest the currentpopulation on MID is not derived from birdstranslocated from CRD, but rather that MID wasmost likely colonised by birds inhabiting otherisland habitats within the PWS. Furthermore,since geese from the CRD share mtDNA haplotypeswith geese from other breeding locales, theyapparently share recent common ancestry and/orgene flow with populations representing othersubspecies. Our genetic data raise questionsabout the validity of current management unitsof Canada geese.</span></p>","language":"English","publisher":"Springer","doi":"10.1023/A:1024041702616","issn":"15660621","usgsCitation":"Talbot, S.L., Pearce, J.M., Pierson, B.J., Derksen, D.V., and Scribner, K.T., 2003, Molecular status of the dusky Canada goose (Branta canadensis occidentalis): A genetic assessment of a translocation effort: Conservation Genetics, v. 4, no. 3, p. 367-381, https://doi.org/10.1023/A:1024041702616.","productDescription":"15 p.","startPage":"367","endPage":"381","costCenters":[],"links":[{"id":235936,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":209463,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1023/A:1024041702616"}],"volume":"4","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a5d13e4b0c8380cd7013a","contributors":{"authors":[{"text":"Talbot, Sandra L. 0000-0002-3312-7214 stalbot@usgs.gov","orcid":"https://orcid.org/0000-0002-3312-7214","contributorId":140512,"corporation":false,"usgs":true,"family":"Talbot","given":"Sandra","email":"stalbot@usgs.gov","middleInitial":"L.","affiliations":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":117,"text":"Alaska Science Center Biology WTEB","active":true,"usgs":true}],"preferred":true,"id":405436,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pearce, John M. 0000-0002-8503-5485 jpearce@usgs.gov","orcid":"https://orcid.org/0000-0002-8503-5485","contributorId":181766,"corporation":false,"usgs":true,"family":"Pearce","given":"John","email":"jpearce@usgs.gov","middleInitial":"M.","affiliations":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":117,"text":"Alaska Science Center Biology WTEB","active":true,"usgs":true}],"preferred":true,"id":405438,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Pierson, Barbara J. 0000-0001-8233-874X bpierson@usgs.gov","orcid":"https://orcid.org/0000-0001-8233-874X","contributorId":194939,"corporation":false,"usgs":true,"family":"Pierson","given":"Barbara","email":"bpierson@usgs.gov","middleInitial":"J.","affiliations":[{"id":117,"text":"Alaska Science Center Biology WTEB","active":true,"usgs":true},{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"preferred":true,"id":405434,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Derksen, Dirk V. dderksen@usgs.gov","contributorId":2269,"corporation":false,"usgs":true,"family":"Derksen","given":"Dirk","email":"dderksen@usgs.gov","middleInitial":"V.","affiliations":[{"id":117,"text":"Alaska Science Center Biology WTEB","active":true,"usgs":true}],"preferred":true,"id":405435,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Scribner, Kim T.","contributorId":146113,"corporation":false,"usgs":false,"family":"Scribner","given":"Kim","email":"","middleInitial":"T.","affiliations":[{"id":16582,"text":"Department of Fisheries and Wildlife and Department of Zoology, 480 Wilson Rd. 13 Natural Resources Building, Michigan State University, East Lansing, MI 48824","active":true,"usgs":false},{"id":135,"text":"Biological Resources Division","active":false,"usgs":true}],"preferred":false,"id":405437,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70026003,"text":"70026003 - 2003 - Model of the porphyry copper and polymetallic vein family of deposits - Applications in Slovakia, Hungary, and Romania","interactions":[],"lastModifiedDate":"2021-08-06T16:57:03.459603","indexId":"70026003","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2020,"text":"International Geology Review","active":true,"publicationSubtype":{"id":10}},"title":"Model of the porphyry copper and polymetallic vein family of deposits - Applications in Slovakia, Hungary, and Romania","docAbstract":"<p><span>A tectonic model useful in estimating the occurrence of undiscovered porphyry copper and polymetallic vein systems has been developed. This model is based on the manner in which magmatic and hydrothermal fluids flow and are trapped in fault systems as far-field stress is released in tectonic strain features above subducting plates (e.g. strike-slip fault systems). The structural traps include preferred locations for stock emplacement and tensional-shear fault meshes within the step-overs that localize porphyry- and vein-style deposits. The application of the model is illustrated for the porphyry copper and polymetallic vein deposits in the Central Slovakian Volcanic Field, Slovakia; the Mátra Mountains, Hungary; and the Apuseni Mountains, Romania.</span></p>","language":"English","publisher":"Taylor & Francis","doi":"10.2747/0020-6814.45.2.143","issn":"00206814","usgsCitation":"Drew, L., 2003, Model of the porphyry copper and polymetallic vein family of deposits - Applications in Slovakia, Hungary, and Romania: International Geology Review, v. 45, no. 2, p. 143-156, https://doi.org/10.2747/0020-6814.45.2.143.","productDescription":"14 p.","startPage":"143","endPage":"156","costCenters":[],"links":[{"id":387740,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"45","issue":"2","noUsgsAuthors":false,"publicationDate":"2010-07-14","publicationStatus":"PW","scienceBaseUri":"505a5bb0e4b0c8380cd6f72d","contributors":{"authors":[{"text":"Drew, L.J.","contributorId":69157,"corporation":false,"usgs":true,"family":"Drew","given":"L.J.","email":"","affiliations":[],"preferred":false,"id":407462,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":96241,"text":"96241 - 2003 - Evaluating the post-release success of rehabilitated manatees in Florida, 1973-2002","interactions":[],"lastModifiedDate":"2012-02-02T00:03:53","indexId":"96241","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":18,"text":"Abstract or summary"},"title":"Evaluating the post-release success of rehabilitated manatees in Florida, 1973-2002","docAbstract":"Abstract not supplied at this time","language":"English","usgsCitation":"Bonde, R., Keith, L., Ward, L., Reid, J., Pitchford, T., Deutsch, C., Ross, M., Valade, J., and Adimey, N., 2003, Evaluating the post-release success of rehabilitated manatees in Florida, 1973-2002.","costCenters":[{"id":275,"text":"Florida Integrated Science Center","active":false,"usgs":true}],"links":[{"id":127272,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db629783","contributors":{"authors":[{"text":"Bonde, R. 0000-0001-9179-4376","orcid":"https://orcid.org/0000-0001-9179-4376","contributorId":81042,"corporation":false,"usgs":true,"family":"Bonde","given":"R.","affiliations":[],"preferred":false,"id":299328,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Keith, L.","contributorId":77866,"corporation":false,"usgs":true,"family":"Keith","given":"L.","email":"","affiliations":[],"preferred":false,"id":299327,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ward, L.","contributorId":30934,"corporation":false,"usgs":true,"family":"Ward","given":"L.","affiliations":[],"preferred":false,"id":299324,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Reid, J.","contributorId":42542,"corporation":false,"usgs":true,"family":"Reid","given":"J.","email":"","affiliations":[],"preferred":false,"id":299325,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Pitchford, T.","contributorId":63338,"corporation":false,"usgs":true,"family":"Pitchford","given":"T.","email":"","affiliations":[],"preferred":false,"id":299326,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Deutsch, C.","contributorId":29343,"corporation":false,"usgs":true,"family":"Deutsch","given":"C.","affiliations":[],"preferred":false,"id":299323,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Ross, M.","contributorId":8026,"corporation":false,"usgs":true,"family":"Ross","given":"M.","email":"","affiliations":[],"preferred":false,"id":299321,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Valade, J.","contributorId":12802,"corporation":false,"usgs":true,"family":"Valade","given":"J.","email":"","affiliations":[],"preferred":false,"id":299322,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Adimey, N.","contributorId":5997,"corporation":false,"usgs":true,"family":"Adimey","given":"N.","affiliations":[],"preferred":false,"id":299320,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}}
,{"id":70024987,"text":"70024987 - 2003 - Influences of upland and riparian land use patterns on stream biotic integrity","interactions":[],"lastModifiedDate":"2012-03-12T17:20:12","indexId":"70024987","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2602,"text":"Landscape Ecology","active":true,"publicationSubtype":{"id":10}},"title":"Influences of upland and riparian land use patterns on stream biotic integrity","docAbstract":"We explored land use, fish assemblage structure, and stream habitat associations in 20 catchments in Opequon Creek watershed, West Virginia. The purpose was to determine the relative importance of urban and agriculture land use on stream biotic integrity, and to evaluate the spatial scale (i.e., whole-catchment vs riparian buffer) at which land use effects were most pronounced. We found that index of biological integrity (IBI) scores were strongly associated with extent of urban land use in individual catchments. Sites that received ratings of poor or very poor based on IBI scores had > 7% of urban land use in their respective catchments. Habitat correlations suggested that urban land use disrupted flow regime, reduced water quality, and altered stream channels. In contrast, we found no meaningful relationship between agricultural land use and IBI at either whole-catchment or riparian scales despite strong correlations between percent agriculture and several important stream habitat measures, including nitrate concentrations, proportion of fine sediments in riffles, and the abundance of fish cover. We also found that variation in gradient (channel slope) influenced responses of fish assemblages to land use. Urban land use was more disruptive to biological integrity in catchments with steeper channel slopes. Based on comparisons of our results in the topographically diverse Opequon Creek watershed with results from watersheds in flatter terrains, we hypothesize that the potential for riparian forests to mitigate effects of deleterious land uses in upland portions of the watershed is inversely related to gradient.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Landscape Ecology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1023/B:LAND.0000004178.41511.da","issn":"09212973","usgsCitation":"Snyder, C., Young, J., Villella, R., and Lemarie, D.P., 2003, Influences of upland and riparian land use patterns on stream biotic integrity: Landscape Ecology, v. 18, no. 7, p. 647-664, https://doi.org/10.1023/B:LAND.0000004178.41511.da.","startPage":"647","endPage":"664","numberOfPages":"18","costCenters":[],"links":[{"id":232795,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":207659,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1023/B:LAND.0000004178.41511.da"}],"volume":"18","issue":"7","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3bace4b0c8380cd6274f","contributors":{"authors":[{"text":"Snyder, C.D.","contributorId":73540,"corporation":false,"usgs":true,"family":"Snyder","given":"C.D.","email":"","affiliations":[],"preferred":false,"id":403353,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Young, J.A. 0000-0002-4500-3673","orcid":"https://orcid.org/0000-0002-4500-3673","contributorId":37674,"corporation":false,"usgs":true,"family":"Young","given":"J.A.","affiliations":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"preferred":false,"id":403352,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Villella, R.","contributorId":103627,"corporation":false,"usgs":true,"family":"Villella","given":"R.","email":"","affiliations":[],"preferred":false,"id":403354,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lemarie, D. P.","contributorId":23100,"corporation":false,"usgs":true,"family":"Lemarie","given":"D.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":403351,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70025932,"text":"70025932 - 2003 - Influence of eastern hemlock (Tsuga canadensis L.) on fish community structure and function in headwater streams of the Delaware River basin","interactions":[],"lastModifiedDate":"2012-03-12T17:20:24","indexId":"70025932","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1471,"text":"Ecology of Freshwater Fish","active":true,"publicationSubtype":{"id":10}},"title":"Influence of eastern hemlock (Tsuga canadensis L.) on fish community structure and function in headwater streams of the Delaware River basin","docAbstract":"Hemlock (Tsuga canadensis) forest of the eastern U.S. are in decline due to invasion by the exotic insect hemlock woolly adelgid (Adelges tsugae). Aquatic biodiversity in hemlock ecosystems has not been documented; thus the true impact of the infestation cannot be assessed. We compared ichthyofaunal assemblages and trophic structure of streams draining hemlock and hardwood forests by sampling first- and second-order streams draining 14 paired hemlock and hardwood stands during base flows in July 1997 at the Delaware Water Gap National Recreation Area of Pennsylvania and New Jersey. Over 1400 fish of 15 species and 7 families were collected, but hemlock and hardwood streams individually harbored only one to four species. Brook trout (Salvelinus fontinalis) and brown trout (Salmo trutta) were two to three times as prevalent in hemlock than hardwood streams. Insectivorous fishes occurred in significantly higher proportion in streams of hardwood (0.90) than hemlock (0.46) stands, while piscivores occurred more often in hemlock (0.85) than hardwood (0.54) stands. Functional (trophic) diversity of fishes in hemlock and second-order streams was numerically greater than that of hardwood and first-order streams. Species composition also differed by stream order and terrain type. Biodiversity is threatened at several levels within hemlock ecosystems at risk to the hemlock woolly adelgid in eastern U.S. forests.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Ecology of Freshwater Fish","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1034/j.1600-0633.2003.00006.x","issn":"09066691","usgsCitation":"Ross, R.M., Bennett, R.M., Snyder, C., Young, J., Smith, D., and Lemarie, D.P., 2003, Influence of eastern hemlock (Tsuga canadensis L.) on fish community structure and function in headwater streams of the Delaware River basin: Ecology of Freshwater Fish, v. 12, no. 1, p. 60-65, https://doi.org/10.1034/j.1600-0633.2003.00006.x.","startPage":"60","endPage":"65","numberOfPages":"6","costCenters":[],"links":[{"id":208752,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1034/j.1600-0633.2003.00006.x"},{"id":234720,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"12","issue":"1","noUsgsAuthors":false,"publicationDate":"2003-02-13","publicationStatus":"PW","scienceBaseUri":"505a3b2be4b0c8380cd622b9","contributors":{"authors":[{"text":"Ross, R. M.","contributorId":39311,"corporation":false,"usgs":true,"family":"Ross","given":"R.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":407146,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bennett, R. M.","contributorId":97852,"corporation":false,"usgs":true,"family":"Bennett","given":"R.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":407149,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Snyder, C.D.","contributorId":73540,"corporation":false,"usgs":true,"family":"Snyder","given":"C.D.","email":"","affiliations":[],"preferred":false,"id":407148,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Young, J.A. 0000-0002-4500-3673","orcid":"https://orcid.org/0000-0002-4500-3673","contributorId":37674,"corporation":false,"usgs":true,"family":"Young","given":"J.A.","affiliations":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"preferred":false,"id":407145,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Smith, D. R. 0000-0001-6074-9257","orcid":"https://orcid.org/0000-0001-6074-9257","contributorId":44108,"corporation":false,"usgs":true,"family":"Smith","given":"D. R.","affiliations":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"preferred":false,"id":407147,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Lemarie, D. P.","contributorId":23100,"corporation":false,"usgs":true,"family":"Lemarie","given":"D.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":407144,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70025952,"text":"70025952 - 2003 - Effects of Holocene climate change on mercury deposition in Elk Lake, Minnesota: The importance of eolain transport in the mercury cycle","interactions":[],"lastModifiedDate":"2021-08-10T11:53:47.047634","indexId":"70025952","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1796,"text":"Geology","active":true,"publicationSubtype":{"id":10}},"title":"Effects of Holocene climate change on mercury deposition in Elk Lake, Minnesota: The importance of eolain transport in the mercury cycle","docAbstract":"<p><span>Sediments&nbsp;</span>in<span>&nbsp;</span>Elk<span>&nbsp;</span>Lake<span>,&nbsp;</span>Minnesota<span>, consist of 10,400 varve layers that provide a precise chronology for&nbsp;</span>Holocene<span>&nbsp;fluctuations&nbsp;</span>in<span>&nbsp;</span>climate<span>&nbsp;and biota recorded&nbsp;</span>in<span>&nbsp;the strata. Progressively greater concentrations and accumulation rates of&nbsp;</span>mercury<span>&nbsp;since ca. A.D. 1875 reflect&nbsp;</span>deposition<span>&nbsp;of anthropogenic&nbsp;</span>mercury<span>&nbsp;additions to the atmosphere. Within the&nbsp;</span>Holocene<span>&nbsp;record are numerous short intervals&nbsp;</span>in<span>&nbsp;which&nbsp;</span>mercury<span>&nbsp;concentrations and accumulation rates exceed the modern values. The highest&nbsp;</span>mercury<span>&nbsp;concentrations formed ca. 8 ka, coincident with a rapid&nbsp;</span>change<span>&nbsp;from cool, moist conditions to warm, dry conditions. A related&nbsp;</span>change<span>&nbsp;</span>in<span>&nbsp;flora from pine forest to prairie caused destruction of organic forest soils and the release of&nbsp;</span>mercury<span>&nbsp;that had been sequestered&nbsp;</span>in<span>&nbsp;them, resulting&nbsp;</span>in<span>&nbsp;a short- lived pulse of&nbsp;</span>mercury<span>&nbsp;to the&nbsp;</span>lake<span>. Accumulation rates of&nbsp;</span>mercury<span>&nbsp;were highest during the 4 k.y. mid-</span>Holocene<span>&nbsp;dry interval and show a correlation with periods of rapid&nbsp;</span>deposition<span>&nbsp;of eolian dust. The&nbsp;</span>mercury<span>&nbsp;was probably bound to wind-borne mineral particles, which were derived from an unidentified&nbsp;</span>mercury<span>-rich source region west of&nbsp;</span>Elk<span>&nbsp;</span>Lake<span>.</span></p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0091-7613(2003)031<0187:EOHCCO>2.0.CO;2","issn":"00917613","usgsCitation":"Cannon, W., Dean, W., and Bullock, J., 2003, Effects of Holocene climate change on mercury deposition in Elk Lake, Minnesota: The importance of eolain transport in the mercury cycle: Geology, v. 31, no. 2, p. 187-190, https://doi.org/10.1130/0091-7613(2003)031<0187:EOHCCO>2.0.CO;2.","productDescription":"4 p.","startPage":"187","endPage":"190","costCenters":[],"links":[{"id":387691,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Minnesota","otherGeospatial":"Elk Lake","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -95.81734657287598,\n              45.853015907512436\n            ],\n            [\n              -95.77245712280273,\n              45.853015907512436\n            ],\n            [\n              -95.77245712280273,\n              45.87560860976356\n            ],\n            [\n              -95.81734657287598,\n              45.87560860976356\n            ],\n            [\n              -95.81734657287598,\n              45.853015907512436\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"31","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0654e4b0c8380cd511de","contributors":{"authors":[{"text":"Cannon, W.F. 0000-0002-2699-8118","orcid":"https://orcid.org/0000-0002-2699-8118","contributorId":70382,"corporation":false,"usgs":true,"family":"Cannon","given":"W.F.","affiliations":[],"preferred":false,"id":407228,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dean, W.E.","contributorId":97099,"corporation":false,"usgs":true,"family":"Dean","given":"W.E.","email":"","affiliations":[],"preferred":false,"id":407229,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bullock, J. H.","contributorId":57074,"corporation":false,"usgs":true,"family":"Bullock","given":"J. H.","affiliations":[],"preferred":false,"id":407227,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70026002,"text":"70026002 - 2003 - Morphometric and histopathological parameters of gonadal development in adult common carp from contaminated and reference sites in Lake Mead, Nevada","interactions":[],"lastModifiedDate":"2021-11-24T16:37:17.972046","indexId":"70026002","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2177,"text":"Journal of Aquatic Animal Health","active":true,"publicationSubtype":{"id":10}},"title":"Morphometric and histopathological parameters of gonadal development in adult common carp from contaminated and reference sites in Lake Mead, Nevada","docAbstract":"<p><span>This study examined the hypothesis that exposure to sublethal concentrations of contaminants alters the gonadal condition of feral common carp&nbsp;</span><i>Cyprinus carpio</i><span>. Adult common carp in Lake Mead, Nevada, were collected from a contaminated site (Las Vegas Bay) that receives municipal and industrial effluent and from a reference site (Overton Arm) with a relatively low level of contamination. Fish were sampled seven times over a 1-year period extending over two separate spawning seasons. Morphometric and histopathological parameters of gonadal and germ cell development were determined. In males, the pattern of seasonal changes in the gonadosomatic index (GSI) was similar between the sites and showed no clear association with site-specific seasonal temperature profiles. However, Las Vegas Bay males had consistently lower GSI values and, on one of the sampling dates, a lower proportion of sperm relative to other germ cell stages (determined histologically). Further, Las Vegas Bay males had a higher incidence of gonadal macrophage aggregates, which are putative tissue biomarkers of contaminant exposure in fishes. In females, seasonal GSI profiles, the frequency of fish with postovulatory follicles (an index of spawning activity), and the timing of new follicle recruitment all showed differences between sites, but these differences generally matched differences in water temperature profile. Also, the peak size-frequency of full-grown follicles did not differ between sites, and estimates of fecundity for the second spawning season indicated that females from the reference site unexpectedly produced a lower number of gametes. Overall, site differences in gonadal condition were observed in carp of both sexes but they seemed to be associated with site differences in contaminant levels only in males. The apparent lack of association between contaminant level and gonadal condition in female carp from mildly mesotrophic Lake Mead may indicate a lack of contaminant effects in females or a confounding effect of the higher nutrient loads in the Las Vegas Bay environment.</span></p>","language":"English","publisher":"Wiley","doi":"10.1577/1548-8667(2003)015<0055:MAHPOG>2.0.CO;2","issn":"08997659","usgsCitation":"Patino, R., Goodbred, S.L., Draugelis-Dale, R., Barry, C.E., Foott, J.S., Wainscott, M.R., Gross, T., and Covay, K., 2003, Morphometric and histopathological parameters of gonadal development in adult common carp from contaminated and reference sites in Lake Mead, Nevada: Journal of Aquatic Animal Health, v. 15, no. 1, p. 55-68, https://doi.org/10.1577/1548-8667(2003)015<0055:MAHPOG>2.0.CO;2.","productDescription":"14 p.","startPage":"55","endPage":"68","numberOfPages":"14","costCenters":[],"links":[{"id":234582,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Nevada","otherGeospatial":"Lake Mead","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -114.85931396484374,\n              36.07629718752892\n            ],\n            [\n              -114.76867675781249,\n              36.07629718752892\n            ],\n            [\n              -114.76867675781249,\n              36.132883744079486\n            ],\n            [\n              -114.85931396484374,\n              36.132883744079486\n            ],\n            [\n              -114.85931396484374,\n              36.07629718752892\n            ]\n          ]\n        ]\n      }\n    },\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -114.43153381347656,\n              36.42183496700228\n            ],\n            [\n              -114.30381774902344,\n              36.42183496700228\n            ],\n            [\n              -114.30381774902344,\n              36.53060536411363\n            ],\n            [\n              -114.43153381347656,\n              36.53060536411363\n            ],\n            [\n              -114.43153381347656,\n              36.42183496700228\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"15","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a5e60e4b0c8380cd709c8","contributors":{"authors":[{"text":"Patino, R.","contributorId":39915,"corporation":false,"usgs":true,"family":"Patino","given":"R.","email":"","affiliations":[],"preferred":false,"id":407455,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Goodbred, S. L.","contributorId":58232,"corporation":false,"usgs":true,"family":"Goodbred","given":"S.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":407459,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Draugelis-Dale, R. 0000-0001-8532-3287","orcid":"https://orcid.org/0000-0001-8532-3287","contributorId":86943,"corporation":false,"usgs":true,"family":"Draugelis-Dale","given":"R.","affiliations":[{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"preferred":false,"id":407460,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Barry, C. E.","contributorId":46275,"corporation":false,"usgs":true,"family":"Barry","given":"C.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":407457,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Foott, J. Scott","contributorId":28416,"corporation":false,"usgs":false,"family":"Foott","given":"J.","email":"","middleInitial":"Scott","affiliations":[],"preferred":false,"id":407454,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Wainscott, M. R.","contributorId":46276,"corporation":false,"usgs":false,"family":"Wainscott","given":"M.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":407458,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Gross, T. S.","contributorId":95828,"corporation":false,"usgs":true,"family":"Gross","given":"T. S.","affiliations":[],"preferred":false,"id":407461,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Covay, K.J.","contributorId":44948,"corporation":false,"usgs":true,"family":"Covay","given":"K.J.","affiliations":[],"preferred":false,"id":407456,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":70026001,"text":"70026001 - 2003 - Early neogene history of the central American arc from Bocas del Toro, western Panama","interactions":[],"lastModifiedDate":"2018-01-31T10:43:39","indexId":"70026001","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1786,"text":"Geological Society of America Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Early neogene history of the central American arc from Bocas del Toro, western Panama","docAbstract":"<p><span>A newly discovered sequence of lower to middle Miocene rocks from the eastern Bocas del Toro archipelago, western Panama, reveals the timing and environment of the earliest stages in the rise of the Isthmus of Panama in this region. Two new formations, the Punta Alegre Formation (lower Miocene, Aquitanian to Burdigalian) and the Valiente Formation (middle Miocene, Langhian to Serravallian), are here named and formally described. The Punta Alegre Formation contains a diagnostic microfauna of benthic and planktic foraminifera and calcareous nannofossils that indicate deposition in a 2000-m-deep pre-isthmian neotropical ocean from as old as 21.5–18.3 Ma. Its lithology varies from silty mudstone to muddy foraminiferal ooze with rare thin microturbidite layers near the top. The Valiente Formation, which ranges in age from 16.4 to ca. 12.0 Ma, lies with slight angular unconformity on the Punta Alegre Formation and consists of five lithofacies: (1) columnar basalt and flow breccia, (2) pyroclastic deposits, (3) coarse-grained volcaniclastic deposits, (4) coral-reef limestone with diverse large coral colonies, and (5) marine debris-flow deposits and microturbidites. These lithofacies are interpreted to indicate that after ca. 16 Ma a volcanic arc developed in the region of Bocas del Toro and that by ca. 12 Ma an extensively emergent archipelago of volcanic islands had formed.&nbsp;</span><sup>39</sup><span>Ar/</span><sup>40</sup><span>Ar dating of basalt flows associated with the fossiliferous sedimentary rocks in the upper part of the Valiente Formation strongly confirms the ages derived from planktic foraminifera and nannofossils. Paleobathymetric analysis of the two new formations in the Valiente Peninsula and Popa Island, in the Bocas del Toro archipelago, shows a general shallowing from lower- through upper-bathyal to upper-neritic and emergent laharic and fluviatile deposits from ca. 19 to 12 Ma. The overlying nonconformable Bocas del Toro Group contains a lower transgressive sequence ranging from basal nearshore sandstone to upper-bathyal mudstone (ca. 8.1–5.3 Ma) and an upper regressive sequence (5.3–3.5 Ma). A similar paleobathymetric pattern is observed from the Gatun to Chagres Formations (12–6 Ma) in the Panama Canal Basin area and in the Uscari, Rio Banana, Quebrada Chocolate, and Moin Formations (8–1.7 Ma) in the southern Limón Basin of Costa Rica.</span></p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(2003)115<0271:ENHOTC>2.0.CO;2","usgsCitation":"Coates, A.G., Aubry, M., Berggren, W.A., Collins, L.S., and Kunk, M.J., 2003, Early neogene history of the central American arc from Bocas del Toro, western Panama: Geological Society of America Bulletin, v. 115, no. 3, p. 271-287, https://doi.org/10.1130/0016-7606(2003)115<0271:ENHOTC>2.0.CO;2.","productDescription":"17 p.","startPage":"271","endPage":"287","costCenters":[],"links":[{"id":234548,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"115","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a048de4b0c8380cd50a58","contributors":{"authors":[{"text":"Coates, Anthony G.","contributorId":174335,"corporation":false,"usgs":false,"family":"Coates","given":"Anthony","email":"","middleInitial":"G.","affiliations":[{"id":27419,"text":"Smithsonian Tropical Research Institute, P.O. Box 0843-03092, Balboa, Republic of Panama","active":true,"usgs":false}],"preferred":false,"id":407450,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Aubry, Marie-Pierre","contributorId":174332,"corporation":false,"usgs":false,"family":"Aubry","given":"Marie-Pierre","email":"","affiliations":[{"id":27421,"text":"Department of Earth and Planetary Sciences Rutgers University 610 Taylor Road Piscataway NJ 08854-8066, USA","active":true,"usgs":false}],"preferred":false,"id":407453,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Berggren, William A.","contributorId":174333,"corporation":false,"usgs":false,"family":"Berggren","given":"William","email":"","middleInitial":"A.","affiliations":[{"id":27421,"text":"Department of Earth and Planetary Sciences Rutgers University 610 Taylor Road Piscataway NJ 08854-8066, USA","active":true,"usgs":false}],"preferred":false,"id":407449,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Collins, Laurel S.","contributorId":174336,"corporation":false,"usgs":false,"family":"Collins","given":"Laurel","email":"","middleInitial":"S.","affiliations":[{"id":27423,"text":"Department of Earth and Environment, and Department of Biological Sciences, Florida International University, Miami, Florida 33199, USA","active":true,"usgs":false}],"preferred":false,"id":407451,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Kunk, Michael J. 0000-0003-4424-7825 mkunk@usgs.gov","orcid":"https://orcid.org/0000-0003-4424-7825","contributorId":200968,"corporation":false,"usgs":true,"family":"Kunk","given":"Michael","email":"mkunk@usgs.gov","middleInitial":"J.","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true},{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true}],"preferred":true,"id":407452,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70024862,"text":"70024862 - 2003 - Growth and survival of <i>Escherichia coli</i> and enterococci populations in the macro-alga <i>Cladophora</i> (Chlorophyta)","interactions":[],"lastModifiedDate":"2016-05-19T11:51:06","indexId":"70024862","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1619,"text":"FEMS Microbiology Ecology","onlineIssn":"1574-6941","printIssn":"0168-6496","active":true,"publicationSubtype":{"id":10}},"title":"Growth and survival of <i>Escherichia coli</i> and enterococci populations in the macro-alga <i>Cladophora</i> (Chlorophyta)","docAbstract":"<p>The macro-alga <i>Cladophora glomerata</i> is found in streams and lakes worldwide. High concentrations of <i>Escherichia coli</i> and enterococci have been reported in <i>Cladophora</i> along the Lake Michigan shore. The objective of this study was to determine if <i>Cladophora</i> supported growth of these indicator bacteria. Algal leachate readily supported in vitro multiplication of <i>E. coli</i> and enterococci, suggesting that leachates contain necessary growth-promoting substances. Growth was directly related to the concentration of algal leachate. <i>E. coli</i> survived for over 6 months in dried <i>Cladophora</i> stored at 4&deg;C; residual <i>E. coli</i> grew after mat rehydration, reaching a carrying capacity of 8 log CFU g<sup>-1</sup> in 48 h. Results of this study also show that the <i>E. coli</i> strains associated with <i>Cladophora</i> are highly related; in most instances they are genetically different from each other, suggesting that the relationship between <i>E. coli</i> and <i>Cladophora</i> may be casual. These findings indicate that <i>Cladophora</i> provides a suitable environment for indicator bacteria to persist for extended periods and to grow under natural conditions.</p>","language":"English","publisher":"Oxford University Press","doi":"10.1016/S0168-6496(03)00214-9","issn":"01686496","usgsCitation":"Byappanahalli, M., Shively, D., Nevers, M., Sadowsky, M., and Whitman, R., 2003, Growth and survival of <i>Escherichia coli</i> and enterococci populations in the macro-alga <i>Cladophora</i> (Chlorophyta): FEMS Microbiology Ecology, v. 46, no. 2, p. 203-211, https://doi.org/10.1016/S0168-6496(03)00214-9.","productDescription":"9 p.","startPage":"203","endPage":"211","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":487426,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1016/s0168-6496(03)00214-9","text":"Publisher Index Page"},{"id":233212,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":207918,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/S0168-6496(03)00214-9"}],"volume":"46","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a2deee4b0c8380cd5c150","contributors":{"authors":[{"text":"Byappanahalli, M.N.","contributorId":11384,"corporation":false,"usgs":true,"family":"Byappanahalli","given":"M.N.","email":"","affiliations":[],"preferred":false,"id":402898,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Shively, D.A.","contributorId":78123,"corporation":false,"usgs":true,"family":"Shively","given":"D.A.","email":"","affiliations":[],"preferred":false,"id":402902,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Nevers, M.B.","contributorId":13787,"corporation":false,"usgs":true,"family":"Nevers","given":"M.B.","email":"","affiliations":[],"preferred":false,"id":402899,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Sadowsky, M.J.","contributorId":19337,"corporation":false,"usgs":true,"family":"Sadowsky","given":"M.J.","email":"","affiliations":[],"preferred":false,"id":402900,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Whitman, R.L.","contributorId":69750,"corporation":false,"usgs":true,"family":"Whitman","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":402901,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":96874,"text":"96874 - 2003 - Predator of nesting waterbirds in an urban environment. Final Report","interactions":[],"lastModifiedDate":"2012-02-02T00:03:50","indexId":"96874","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":9,"text":"Other Report"},"title":"Predator of nesting waterbirds in an urban environment. Final Report","docAbstract":"No abstract available at this time","language":"English","publisher":"NASA Ames Research Center, Moffett Federal Airfield","publisherLocation":"Mountainview, CA","usgsCitation":"Meckstroth, A., and Miles, A., 2003, Predator of nesting waterbirds in an urban environment. Final Report, 49 p.","productDescription":"49 p.","startPage":"49","numberOfPages":"49","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":126928,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67ebaf","contributors":{"authors":[{"text":"Meckstroth, A.","contributorId":36481,"corporation":false,"usgs":true,"family":"Meckstroth","given":"A.","email":"","affiliations":[],"preferred":false,"id":300458,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miles, A.K. 0000-0002-3108-808X","orcid":"https://orcid.org/0000-0002-3108-808X","contributorId":85902,"corporation":false,"usgs":true,"family":"Miles","given":"A.K.","affiliations":[],"preferred":false,"id":300459,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70025955,"text":"70025955 - 2003 - Interaction of lateral baroclinic forcing and turbulence in an estuary","interactions":[],"lastModifiedDate":"2018-09-19T09:22:04","indexId":"70025955","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2315,"text":"Journal of Geophysical Research C: Oceans","active":true,"publicationSubtype":{"id":10}},"title":"Interaction of lateral baroclinic forcing and turbulence in an estuary","docAbstract":"Observations of density and velocity in a channel in northern San Francisco Bay show that the onset of vertical density stratification during flood tides is controlled by the balance between the cross-channel baroclinic pressure gradient and vertical mixing due to turbulence. Profiles of velocity, salinity, temperature, and suspended sediment concentration were measured in transects across Suisun Cutoff, in northern San Francisco Bay, on two days over the 12.5-hour tidal cycle. During flood tides an axial density front developed between fresher water flowing from the shallows of Grizzly Bay into the northern side of Suisun Cutoff and saltier water flowing up the channel. North of the front, transverse currents were driven by the lateral salinity gradient, with a top-to-bottom velocity difference greater than 30 cm/s. South of the front, the secondary circulation was weak, and along-channel velocities were greater than to the north. The gradient Richardson number shows that stratification was stable north of the front, while the water column was turbulently mixed south of the front. Time-series measurements of velocity and salinity demonstrate that the front develops during each tidal cycle. In estuaries, longitudinal dynamics predict less stratification during flood than ebb tides. These data show that stratification can develop during flood tides due to a lateral baroclinic pressure gradient in estuaries with complex bathymetry.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Geophysical Research C: Oceans","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1029/2002JC001392","issn":"01480227","usgsCitation":"Lacy, J., Stacey, M., Burau, J., and Monismith, S., 2003, Interaction of lateral baroclinic forcing and turbulence in an estuary: Journal of Geophysical Research C: Oceans, v. 108, no. 3, p. 34-1, https://doi.org/10.1029/2002JC001392.","startPage":"34","endPage":"1","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"links":[{"id":235016,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":293139,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1029/2002JC001392"}],"volume":"108","issue":"3","noUsgsAuthors":false,"publicationDate":"2003-03-20","publicationStatus":"PW","scienceBaseUri":"505a3cb4e4b0c8380cd62f7c","contributors":{"authors":[{"text":"Lacy, J.R.","contributorId":68508,"corporation":false,"usgs":true,"family":"Lacy","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":407236,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stacey, M.T.","contributorId":82874,"corporation":false,"usgs":true,"family":"Stacey","given":"M.T.","email":"","affiliations":[],"preferred":false,"id":407237,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Burau, J.R. 0000-0002-5196-5035","orcid":"https://orcid.org/0000-0002-5196-5035","contributorId":7307,"corporation":false,"usgs":true,"family":"Burau","given":"J.R.","affiliations":[],"preferred":false,"id":407234,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Monismith, Stephen G.","contributorId":57228,"corporation":false,"usgs":true,"family":"Monismith","given":"Stephen G.","affiliations":[],"preferred":false,"id":407235,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70024870,"text":"70024870 - 2003 - The fate of wastewater-derived nitrate in the subsurface of the Florida Keys: Key Colony Beach, Florida","interactions":[],"lastModifiedDate":"2018-11-16T09:07:03","indexId":"70024870","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1587,"text":"Estuarine, Coastal and Shelf Science","active":true,"publicationSubtype":{"id":10}},"title":"The fate of wastewater-derived nitrate in the subsurface of the Florida Keys: Key Colony Beach, Florida","docAbstract":"<p>Shallow injection is the predominant mode of wastewater disposal for most tourist-oriented facilities and some residential communities in the US Florida Keys National Marine Sanctuary. Concern has been expressed that wastewater nutrients may be escaping from the saline groundwater system into canals and surrounding coastal waters and perhaps to the reef tract 10&nbsp;km offshore, promoting unwanted algal growth and degradation of water quality. We performed a field study of the fate of wastewater-derived nitrate in the subsurface of a Florida Keys residential community (Key Colony Beach, FL) that uses this disposal method, analyzing samples from 21 monitoring wells and two canal sites. The results indicate that wastewater injection at 18–27&nbsp;m depth into saline groundwater creates a large buoyant plume that flows quickly (within days) upward to a confining layer 6&nbsp;m below the surface, and then in a fast flow path toward a canal 200&nbsp;m to the east within a period of weeks to months. Low-salinity groundwaters along the fast flow path have nitrate concentrations that are not significantly reduced from that of the injected wastewaters (ranging from 400 to 600&nbsp;μmol&nbsp;kg<sup>−1</sup>). Portions of the low-salinity plume off the main axis of flow have relatively long residence times (&gt;2 months) and have had their nitrate concentrations strongly reduced by a combination of mixing and denitrification. These waters have dissolved N<sub>2</sub>&nbsp;concentrations up to 1.6 times air-saturation values with δ<sup>15</sup> N[N<sub>2</sub>]=0.5-5‰, δ<sup>15</sup>N[NO<sub>3</sub><sup>-</sup>]=16-26‰, and calculated isotope fractionation factors of about −12±4‰, consistent with denitrification as the predominant nitrate reduction reaction. Estimated rates of denitrification of wastewater in the aquifer are of the order of 4&nbsp;μmol&nbsp;kg<sup>-1</sup>&nbsp;N&nbsp;day<sup>-1</sup>&nbsp;or 0.008&nbsp;day<sup>-1</sup>. The data indicate that denitrification reduces the nitrate load of the injected wastewater substantially, but not completely, before it discharges to nearby canals.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/S0272-7714(03)00131-8","issn":"02727714","usgsCitation":"Griggs, E., Kump, L., and Böhlke, J., 2003, The fate of wastewater-derived nitrate in the subsurface of the Florida Keys: Key Colony Beach, Florida: Estuarine, Coastal and Shelf Science, v. 58, no. 3, p. 517-539, https://doi.org/10.1016/S0272-7714(03)00131-8.","productDescription":"23 p.","startPage":"517","endPage":"539","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":232788,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":207653,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/S0272-7714(03)00131-8"}],"country":"United States","state":"Florida","otherGeospatial":"Florida Keys","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -79.991455078125,\n              25.522614647623293\n            ],\n            [\n              -80.035400390625,\n              25.596948323286135\n            ],\n            [\n              -80.15625,\n              25.596948323286135\n            ],\n            [\n              -80.2716064453125,\n              25.54244147012483\n            ],\n            [\n              -80.3814697265625,\n              25.35891851754525\n            ],\n            [\n              -80.70556640625,\n              25.110471486223346\n            ],\n            [\n              -81.34277343749999,\n              24.886436490787712\n            ],\n            [\n              -81.9854736328125,\n              24.701924833689933\n            ],\n            [\n              -82.144775390625,\n              24.716895455859337\n            ],\n            [\n              -82.3590087890625,\n              24.632038149596895\n            ],\n            [\n              -82.3370361328125,\n              24.52213723599524\n            ],\n            [\n              -82.0404052734375,\n              24.427145340082046\n            ],\n            [\n              -81.45263671875,\n              24.48214938647425\n            ],\n            [\n              -81.10107421874999,\n              24.577099744289427\n            ],\n            [\n              -80.76599121093749,\n              24.716895455859337\n            ],\n            [\n              -80.4034423828125,\n              24.946219074360084\n            ],\n            [\n              -80.255126953125,\n              25.140311914680755\n            ],\n            [\n              -79.991455078125,\n              25.522614647623293\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"58","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505babf9e4b08c986b3231bb","contributors":{"authors":[{"text":"Griggs, E.M.","contributorId":33887,"corporation":false,"usgs":true,"family":"Griggs","given":"E.M.","email":"","affiliations":[],"preferred":false,"id":402938,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kump, L.R.","contributorId":80863,"corporation":false,"usgs":true,"family":"Kump","given":"L.R.","affiliations":[],"preferred":false,"id":402939,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Böhlke, J.K. 0000-0001-5693-6455","orcid":"https://orcid.org/0000-0001-5693-6455","contributorId":96696,"corporation":false,"usgs":true,"family":"Böhlke","given":"J.K.","affiliations":[],"preferred":false,"id":402940,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70025933,"text":"70025933 - 2003 - Community metabolism during early development of a restored wetland","interactions":[],"lastModifiedDate":"2016-05-20T10:36:41","indexId":"70025933","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3750,"text":"Wetlands","onlineIssn":"1943-6246","printIssn":"0277-5212","active":true,"publicationSubtype":{"id":10}},"title":"Community metabolism during early development of a restored wetland","docAbstract":"<p><span>Productivity is an important ecological function of any natural system and may be quite high in wetlands. Restoration of productive wetlands may play a key role in re-establishing ecological function to portions of the vast areas of wetlands (roughly 86%) drained and otherwise altered in the United States over the past two centuries. A restored wetland at the Montezuma National Wildlife Refuge (upstate New York, USA) was examined to determine if ecological function (i.e., productivity), as well as biotic structure, was restored. Physicochemical conditions and both aquatic and terrestrial productivity were measured at the restoration site and compared with rates and conditions in a reference wetland. Gross aquatic community production rates (based on diurnal oxygen curves) were similar at each site (1,679 and 2,311 g O</span><span>2</span><span>&nbsp;&middot; m</span><span>&minus;2</span><span>&nbsp;&middot; yr</span><span>&minus;1</span><span>) and within the range expected for the habitat. Terrestrial Net Aboveground Primary Production rates (measured by monthly biomass changes) (2,400 and 2,500 g dry wt. &middot; m</span><span>&minus;2</span><span>&nbsp;&middot; yr</span><span>&minus;1</span><span>) were also similar between sites when tree and herb production were combined. Aquatic respiration rates (3,704 and 4,552 g O</span><span>2</span><span>&nbsp;&middot; m</span><span>&minus;2</span><span>&middot; yr</span><span>&minus;1</span><span>) were also similar but high, typically more than twice as large as gross aquatic production. As a result, net aquatic production rates at both sites were usually negative, indicating that these small wetlands are organic matter sinks that satisfy aquatic respiration by consumption of both autochthonous aquatic production and imported terrestrial production. They enhance diversity of the local landscape by producing populations of aquatic consumers that cannot be supported by aquatic production alone. Typical wetland conditions and processes developed quickly after restoration, but differences in biotic community structure indicate that observed rates of production and respiration at both sites were maintained by flow through different foodweb pathways. Despite the relatively high process rates, and successional progress of the restoration site is expected to be slow.</span></p>","language":"English","publisher":"Springer","doi":"10.1672/0277-5212(2003)023[0035:CMDEDO]2.0.CO;2","issn":"02775212","usgsCitation":"McKenna, J., 2003, Community metabolism during early development of a restored wetland: Wetlands, v. 23, no. 1, p. 35-50, https://doi.org/10.1672/0277-5212(2003)023[0035:CMDEDO]2.0.CO;2.","productDescription":"16 p.","startPage":"35","endPage":"50","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":234721,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"23","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f809e4b0c8380cd4ce39","contributors":{"authors":[{"text":"McKenna, J.E. Jr.","contributorId":106065,"corporation":false,"usgs":true,"family":"McKenna","given":"J.E.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":407150,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70024982,"text":"70024982 - 2003 - Relative importance of early-successional forests and shrubland habitats to mammals in the northeastern United States","interactions":[],"lastModifiedDate":"2012-03-12T17:20:09","indexId":"70024982","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Relative importance of early-successional forests and shrubland habitats to mammals in the northeastern United States","docAbstract":"The majority of the 60 native terrestrial mammal species that reside in the northeastern United States (US) utilize resources from several habitats on a seasonal basis. However, as many as 20 species demonstrate some preference for early-successional forests, shrublands, or old-field habitats. A few of these (e.g. lagomorphs) can be considered obligate users of these habitats, and the specialist carnivores (e.g. felids) that prey on them may consequently also prefer such habitats. Other mammal species that prefer these habitats certainly depend on them to lesser and varying degrees; thus, the consequences of reducing or eliminating early-successional forests, shrublands, or old-field habitats across the landscape will likely have varying demographic consequences, and thus importance, to those species. ?? 2003 Elsevier B.V. All rights reserved.","largerWorkTitle":"Forest Ecology and Management","language":"English","doi":"10.1016/S0378-1127(03)00247-0","issn":"03781127","usgsCitation":"Fuller, T., and DeStefano, S., 2003, Relative importance of early-successional forests and shrubland habitats to mammals in the northeastern United States, <i>in</i> Forest Ecology and Management, v. 185, no. 1-2, p. 75-79, https://doi.org/10.1016/S0378-1127(03)00247-0.","startPage":"75","endPage":"79","numberOfPages":"5","costCenters":[],"links":[{"id":478496,"rank":10000,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.584.2786","text":"External Repository"},{"id":207968,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/S0378-1127(03)00247-0"},{"id":233294,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"185","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505aa683e4b0c8380cd84ec2","contributors":{"authors":[{"text":"Fuller, T.K.","contributorId":98252,"corporation":false,"usgs":true,"family":"Fuller","given":"T.K.","email":"","affiliations":[],"preferred":false,"id":403339,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"DeStefano, S.","contributorId":84309,"corporation":false,"usgs":true,"family":"DeStefano","given":"S.","email":"","affiliations":[],"preferred":false,"id":403338,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70194304,"text":"70194304 - 2003 - Estimates of global cyanobacterial biomass and its distribution","interactions":[],"lastModifiedDate":"2017-11-21T17:58:54","indexId":"70194304","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5560,"text":"Algological Studies","printIssn":"1864-1318","active":true,"publicationSubtype":{"id":10}},"title":"Estimates of global cyanobacterial biomass and its distribution","docAbstract":"<p>We estimated global cyanobacterial biomass in the main reservoirs of cyanobacteria on Earth: marine and freshwater plankton, arid land soil crusts, and endoliths. Estimates were based on typical population density values as measured during our research, or as obtained from literature surveys, which were then coupled with data on global geographical area coverage. Among the marine plankton, the global biomass of <i>Prochlorococcus</i> reaches 120 × 10<sup>12</sup> grams of carbon (g C), and that of <i>Synechoccus</i> some 43 × 10<sup>12</sup> g C. This makes <i>Prochlorococcus</i> and <i>Synechococcus</i>, in that order, the most abundant cyanobacteria on Earth. Tropical marine blooms of <i>Trichodesmium</i> account for an additional 10 × 10<sup>12</sup> g C worldwide. In terrestrial environments, the mass of cyanobacteria in arid land soil crusts is estimated to reach 54 × 10<sup>12</sup> g C and that of arid land endolithic communities an additional 14 × 10<sup>12</sup> g C. The global biomass of planktic cyanobacteria in lakes is estimated to be around 3 × 10<sup>12</sup> g C. Our conservative estimates, which did not include some potentially significant biomass reservoirs such as polar and subarctic areas, topsoils in subhumid climates, and shallow marine and freshwater benthos, indicate that the total global cyanobacterial biomass is in the order of 3 × 10<sup>14</sup> g C, surpassing a thousand million metric tons (10<sup>15</sup> g) of wet biomass. </p>","language":"English","publisher":"E. Schweizerbart'sche Verlagsbuchhandlung","doi":"10.1127/1864-1318/2003/0109-0213","usgsCitation":"Garcia-Pichel, F., Belnap, J., Neuer, S., and Schanz, F., 2003, Estimates of global cyanobacterial biomass and its distribution: Algological Studies, v. 109, no. 1, p. 213-227, https://doi.org/10.1127/1864-1318/2003/0109-0213.","productDescription":"15 p.","startPage":"213","endPage":"227","costCenters":[{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true}],"links":[{"id":349248,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"109","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5a611bc4e4b06e28e9c25a0f","contributors":{"authors":[{"text":"Garcia-Pichel, Ferran","contributorId":166779,"corporation":false,"usgs":false,"family":"Garcia-Pichel","given":"Ferran","email":"","affiliations":[{"id":24511,"text":"Arizona State University, Tempe AZ USA 85287","active":true,"usgs":false}],"preferred":false,"id":723186,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Belnap, Jayne 0000-0001-7471-2279 jayne_belnap@usgs.gov","orcid":"https://orcid.org/0000-0001-7471-2279","contributorId":1332,"corporation":false,"usgs":true,"family":"Belnap","given":"Jayne","email":"jayne_belnap@usgs.gov","affiliations":[{"id":568,"text":"Southwest Biological Science Center","active":true,"usgs":true}],"preferred":true,"id":723187,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Neuer, Susanne","contributorId":15377,"corporation":false,"usgs":false,"family":"Neuer","given":"Susanne","email":"","affiliations":[],"preferred":false,"id":723188,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Schanz, Ferdinand","contributorId":6586,"corporation":false,"usgs":false,"family":"Schanz","given":"Ferdinand","email":"","affiliations":[],"preferred":false,"id":723189,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70194362,"text":"70194362 - 2003 - Cooper's hawk (Accipter cooperii)","interactions":[{"subject":{"id":70194362,"text":"70194362 - 2003 - Cooper's hawk (Accipter cooperii)","indexId":"70194362","publicationYear":"2003","noYear":false,"displayTitle":"Cooper's hawk (<i>Accipter cooperii</i>)","title":"Cooper's hawk (Accipter cooperii)"},"predicate":"IS_PART_OF","object":{"id":70194356,"text":"70194356 - 2003 - Birds of Oregon: A general reference","indexId":"70194356","publicationYear":"2003","noYear":false,"title":"Birds of Oregon: A general reference"},"id":1}],"isPartOf":{"id":70194356,"text":"70194356 - 2003 - Birds of Oregon: A general reference","indexId":"70194356","publicationYear":"2003","noYear":false,"title":"Birds of Oregon: A general reference"},"lastModifiedDate":"2017-11-29T14:00:07","indexId":"70194362","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"displayTitle":"Cooper's hawk (<i>Accipter cooperii</i>)","title":"Cooper's hawk (Accipter cooperii)","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Birds of Oregon: A general reference","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Oregon State University Press","publisherLocation":"Corvallis, OR","isbn":"9780870714979","usgsCitation":"Henny, C.J., 2003, Cooper's hawk (Accipter cooperii), chap. <i>of</i> Birds of Oregon: A general reference, p. 148-151.","productDescription":"4 p.","startPage":"148","endPage":"151","costCenters":[{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true}],"links":[{"id":349338,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":349331,"rank":1,"type":{"id":15,"text":"Index 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P.M.","contributorId":29553,"corporation":false,"usgs":true,"family":"Sanzenbacher","given":"P.M.","affiliations":[],"preferred":false,"id":723458,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Haig, Susan M. 0000-0002-6616-7589 susan_haig@usgs.gov","orcid":"https://orcid.org/0000-0002-6616-7589","contributorId":719,"corporation":false,"usgs":true,"family":"Haig","given":"Susan","email":"susan_haig@usgs.gov","middleInitial":"M.","affiliations":[{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true},{"id":289,"text":"Forest and Rangeland Ecosys Science Center","active":true,"usgs":true}],"preferred":true,"id":723459,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1016601,"text":"1016601 - 2003 - [Book review] Prairie Wetland Ecology--The Contribution of the Marsh Ecology Research Program, edited by H. R. Murkin, A. G. van der Valk, and W. R. Clark","interactions":[],"lastModifiedDate":"2018-01-02T11:11:50","indexId":"1016601","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1859,"text":"Great Plains Research","active":true,"publicationSubtype":{"id":10}},"title":"[Book review] Prairie Wetland Ecology--The Contribution of the Marsh Ecology Research Program, edited by H. R. Murkin, A. G. van der Valk, and W. R. Clark","docAbstract":"Review of: Prairie Wetland Ecology: The Contribution of the Marsh Ecology Research Program by Henry R. Murkin, Arnold G. van der Valk, and William R. Clark, eds.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Great Plains Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Center for Great Plains Studies","publisherLocation":"Lincoln, NE","usgsCitation":"Krapu, G., 2003, [Book review] Prairie Wetland Ecology--The Contribution of the Marsh Ecology Research Program, edited by H. R. Murkin, A. G. van der Valk, and W. R. Clark: Great Plains Research, v. 13, no. 1, p. 162-163.","productDescription":"2 p.","startPage":"162","endPage":"163","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":132886,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":268122,"type":{"id":11,"text":"Document"},"url":"https://digitalcommons.unl.edu/greatplainsresearch/653/"}],"volume":"13","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad2e4b07f02db681c3e","contributors":{"authors":[{"text":"Krapu, Gary L.","contributorId":56994,"corporation":false,"usgs":true,"family":"Krapu","given":"Gary L.","affiliations":[],"preferred":false,"id":324476,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70024892,"text":"70024892 - 2003 - Planktonic marine diatom record of the past 18 m.y.: Appearances and extinctions in the Pacific and Southern Oceans","interactions":[],"lastModifiedDate":"2012-03-12T17:20:09","indexId":"70024892","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1388,"text":"Diatom Research","active":true,"publicationSubtype":{"id":10}},"title":"Planktonic marine diatom record of the past 18 m.y.: Appearances and extinctions in the Pacific and Southern Oceans","docAbstract":"Recently published diatom biochronologies provide accurate (to 0.1 m.y.) determination of the ages of appearances and disappearances of planktonic diatoms during the past 18 m.y. in the equatorial Pacific, North Pacific, and Southern Ocean. Comparisons of these records reveal the age of evolutionary appearance and extinction of species and their region of origin. Extinct planktonic diatom species have a mean longevity of 3.4 ?? 2.8 m.y. (SD, n = 53) in the equatorial Pacific, 2.5 ?? 2.1 m.y. (n = 52) in the North Pacific, and 2.9 ?? 2.3 m.y. (n = 38) in the Southern Ocean. The relatively large standard deviations are likely due to the inclusion of taxa that probably could be subdivided into two or more species. In the equatorial Pacific, evolutionary turnover of diatom species was relatively high between 18.0 and 6.0 Ma compared with the period after 6.0 Ma, presumably reflecting changing oceanic circulation and evolving water masses. In the North Pacific, evolutionary turnover peaked between 10.0 and 4.5 Ma, with increasing high-latitude cooling and enhanced provincialism. In the Southern Ocean, evolutionary turnover of endemic diatoms was greatest between 5.0 and 1.6 Ma, which provides evidence for the strong provincial character of Pliocene diatom assemblages. Taken as a whole, oceanic diatom assemblages became increasingly provincial in character during the late Miocene and Pliocene, as pole-to-equator thermal gradients increased and oceanic frontal systems were strengthened.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Diatom Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"0269249X","usgsCitation":"Barron, J., 2003, Planktonic marine diatom record of the past 18 m.y.: Appearances and extinctions in the Pacific and Southern Oceans: Diatom Research, v. 18, no. 2, p. 203-224.","startPage":"203","endPage":"224","numberOfPages":"22","costCenters":[],"links":[{"id":233111,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"18","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a7bcce4b0c8380cd79623","contributors":{"authors":[{"text":"Barron, J.A. 0000-0002-9309-1145","orcid":"https://orcid.org/0000-0002-9309-1145","contributorId":95461,"corporation":false,"usgs":true,"family":"Barron","given":"J.A.","affiliations":[],"preferred":false,"id":403032,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70024878,"text":"70024878 - 2003 - Use of input uncertainty and model sensitivity to guide site exploration","interactions":[],"lastModifiedDate":"2012-03-12T17:20:10","indexId":"70024878","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Use of input uncertainty and model sensitivity to guide site exploration","docAbstract":"Three Quantitatively Directed Exploration (QDE) methods to identify optimum field sampling locations based on model input covariance and model sensitivity are presented. The first method bases site exploration only on the spatial variation in the uncertainty of input properties. The second method uses only the spatial variation in model sensitivities. The third method uses a first-order second-moment (FOSM) method to estimate the spatial variation in the output covariance. The FOSM method estimates output uncertainty using the product of the input covariance and model sensitivity. The three methods are illustrated by means of a synthetic groundwater site simulated with MODFLOW-2000. The groundwater-flow model computes piezometric head and the sensitivity of head to changes in input values. The QDE methods are evaluated by comparing model results to the \"true\" head. For the synthetic site used in this study, the most effective QDE method was the FOSM method.","largerWorkTitle":"Groundwater Quality Modeling and Management Under Uncertinity","conferenceTitle":"Proceeding of the Symposium on Groundwater Management Under Uncertainty","conferenceDate":"23 June 2003 through 25 June 2003","conferenceLocation":"Philadelphia, PH","language":"English","isbn":"0784406960","usgsCitation":"Graettinger, A., Reeves, H.W., Lee, J., and Dethan, D., 2003, Use of input uncertainty and model sensitivity to guide site exploration, <i>in</i> Groundwater Quality Modeling and Management Under Uncertinity, Philadelphia, PH, 23 June 2003 through 25 June 2003, p. 215-225.","startPage":"215","endPage":"225","numberOfPages":"11","costCenters":[],"links":[{"id":232930,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bbf2de4b08c986b3299da","contributors":{"editors":[{"text":"Mishra S.Mishra S.","contributorId":128300,"corporation":true,"usgs":false,"organization":"Mishra S.Mishra S.","id":536538,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Graettinger, A.J.","contributorId":105884,"corporation":false,"usgs":true,"family":"Graettinger","given":"A.J.","email":"","affiliations":[],"preferred":false,"id":402985,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reeves, H. W.","contributorId":53739,"corporation":false,"usgs":true,"family":"Reeves","given":"H.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":402982,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lee, J.","contributorId":58596,"corporation":false,"usgs":true,"family":"Lee","given":"J.","affiliations":[],"preferred":false,"id":402983,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Dethan, D.","contributorId":99740,"corporation":false,"usgs":true,"family":"Dethan","given":"D.","email":"","affiliations":[],"preferred":false,"id":402984,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70024899,"text":"70024899 - 2003 - Rockfall hazard and risk assessment in the Yosemite Valley, California, USA","interactions":[],"lastModifiedDate":"2013-02-21T20:48:52","indexId":"70024899","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2824,"text":"Natural Hazards and Earth System Sciences","active":true,"publicationSubtype":{"id":10}},"title":"Rockfall hazard and risk assessment in the Yosemite Valley, California, USA","docAbstract":"Rock slides and rock falls are the most frequent types of slope movements in Yosemite National Park, California. In historical time (1857-2002) 392 rock falls and rock slides have been documented in the valley, and some of them have been mapped in detail. We present the results of an attempt to assess rock fall hazards in the Yosemite Valley. Spatial and temporal aspects of rock falls hazard are considered. A detailed inventory of slope movements covering the 145-year period from 1857 to 2002 is used to determine the frequency-volume statistics of rock falls and to estimate the annual frequency of rock falls, providing the temporal component of rock fall hazard. The extent of the areas potentially subject to rock fall hazards in the Yosemite Valley were obtained using STONE, a physically-based rock fall simulation computer program. The software computes 3-dimensional rock fall trajectories starting from a digital elevation model (DEM), the location of rock fall release points, and maps of the dynamic rolling friction coefficient and of the coefficients of normal and tangential energy restitution. For each DEM cell the software calculates the number of rock falls passing through the cell, the maximum rock fall velocity and the maximum flying height. For the Yosemite Valley, a DEM with a ground resolution of 10 ?? 10 m was prepared using topographic contour lines from the U.S. Geological Survey 1:24 000-scale maps. Rock fall release points were identified as DEM cells having a slope steeper than 60??, an assumption based on the location of historical rock falls. Maps of the normal and tangential energy restitution coefficients and of the rolling friction coefficient were produced from a surficial geologic map. The availability of historical rock falls mapped in detail allowed us to check the computer program performance and to calibrate the model parameters. Visual and statistical comparison of the model results with the mapped rock falls confirmed the accuracy of the model. The model results are compared with a previous map of rockfall talus and with a geomorphic assessment of rock fall hazard based on potential energy referred to as a shadow angle approach, recently completed for the Yosemite Valley. The model results are then used to identify the roads and trails more subject to rock fall hazard. Of the 166.5 km of roads and trails in the Yosemite Valley 31.2% were found to be potentially subject to rock fall hazard, of which 14% are subject to very high hazard. ?? European Geosciences Union 2003.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Natural Hazards and Earth System Science","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"European Geosciences Union","doi":"10.5194/nhess-3-491-2003","issn":"15618633","usgsCitation":"Guzzetti, F., Reichenbach, P., and Wieczorek, G.F., 2003, Rockfall hazard and risk assessment in the Yosemite Valley, California, USA: Natural Hazards and Earth System Sciences, v. 3, no. 6, p. 491-503, https://doi.org/10.5194/nhess-3-491-2003.","startPage":"491","endPage":"503","numberOfPages":"13","costCenters":[],"links":[{"id":478494,"rank":1,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.5194/nhess-3-491-2003","text":"Publisher Index Page"},{"id":233217,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":267922,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.5194/nhess-3-491-2003"}],"volume":"3","issue":"6","noUsgsAuthors":false,"publicationDate":"2003-12-31","publicationStatus":"PW","scienceBaseUri":"505aae0fe4b0c8380cd87005","contributors":{"authors":[{"text":"Guzzetti, F.","contributorId":46732,"corporation":false,"usgs":true,"family":"Guzzetti","given":"F.","email":"","affiliations":[],"preferred":false,"id":403048,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reichenbach, P.","contributorId":61988,"corporation":false,"usgs":true,"family":"Reichenbach","given":"P.","email":"","affiliations":[],"preferred":false,"id":403050,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wieczorek, G. F.","contributorId":50143,"corporation":false,"usgs":true,"family":"Wieczorek","given":"G.","middleInitial":"F.","affiliations":[],"preferred":false,"id":403049,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70175035,"text":"70175035 - 2003 - Seasonal and longitudinal homogeneity of suspended sediment in San Francisco Bay, California","interactions":[],"lastModifiedDate":"2016-07-27T13:58:58","indexId":"70175035","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Seasonal and longitudinal homogeneity of suspended sediment in San Francisco Bay, California","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Proceedings of the 17th Biennial Conference of the Estuarine Research Federation","largerWorkSubtype":{"id":12,"text":"Conference publication"},"language":"English","publisher":"Estuarine Research Federation","usgsCitation":"Schoellhamer, D., Ganju, N., Gartner, J.W., Murrell, M., and Wright, S., 2003, Seasonal and longitudinal homogeneity of suspended sediment in San Francisco Bay, California, <i>in</i> Proceedings of the 17th Biennial Conference of the Estuarine Research Federation, p. 119-119.","productDescription":"1 p.","startPage":"119","endPage":"119","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":552,"text":"San Francisco Bay-Delta","active":false,"usgs":true},{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true}],"links":[{"id":325717,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5799db70e4b0589fa1c7ea93","contributors":{"authors":[{"text":"Schoellhamer, D. H. 0000-0001-9488-7340","orcid":"https://orcid.org/0000-0001-9488-7340","contributorId":85624,"corporation":false,"usgs":true,"family":"Schoellhamer","given":"D. H.","affiliations":[],"preferred":false,"id":643670,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ganju, N. K. 0000-0002-1096-0465","orcid":"https://orcid.org/0000-0002-1096-0465","contributorId":64782,"corporation":false,"usgs":true,"family":"Ganju","given":"N. K.","affiliations":[],"preferred":false,"id":643671,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gartner, J. W.","contributorId":81903,"corporation":false,"usgs":false,"family":"Gartner","given":"J.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":643672,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Murrell, M.C.","contributorId":106308,"corporation":false,"usgs":true,"family":"Murrell","given":"M.C.","email":"","affiliations":[],"preferred":false,"id":643673,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Wright, S.A.","contributorId":90080,"corporation":false,"usgs":true,"family":"Wright","given":"S.A.","email":"","affiliations":[],"preferred":false,"id":643674,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70024900,"text":"70024900 - 2003 - Accumulation, release, and solubility of arsenic, molybdenum, and vanadium in wetland sediments","interactions":[],"lastModifiedDate":"2021-08-16T22:39:28.807699","indexId":"70024900","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2262,"text":"Journal of Environmental Quality","active":true,"publicationSubtype":{"id":10}},"title":"Accumulation, release, and solubility of arsenic, molybdenum, and vanadium in wetland sediments","docAbstract":"<p><span>This study was undertaken to determine the fate of As, Mo, and V (trace elements, TEs) in the sediments of a constructed wetland in use for the remediation of potentially toxic trace element–contaminated agricultural drainwater. After three years of wetland operation, sediment cores were collected to determine changes in TE concentrations as a function of depth and the effects of varying water column depth. All TE concentrations were highest in the top 2 to 4 cm and decreased with depth. Molybdenum accumulated in the wetland sediments, up to levels of 32.5 ± 4.6, 30.2 ± 8.9, and 59.3 ± 26.1 mg kg</span><sup>−1</sup><span>&nbsp;in the top 1 cm of sediment at water depths of 15, 30, and 60 cm, respectively. In the top 2 cm of sediment, As accumulated (28.2 ± 3.0 mg kg</span><sup>−1</sup><span>) only at the 60-cm water depth. Below 2 cm, as much as 10 mg kg</span><sup>−1</sup><span>&nbsp;of As was lost from the sediment at all water depths. In most cases, V concentrations decreased in the sediment. In this wetland system, the lowest redox potentials were found near the sediment surface and increased with depth. Thus, in general As, Mo, and V concentrations in the sediment were highest under more reducing conditions and lowest under more oxidizing conditions. Most of the accumulated Mo (73%) became water soluble on drying of samples. This has important implications for systems undergoing changes in redox status; for instance, if these wetland sediments are dried, potentially large amounts of Mo may be solubilized.</span></p>","language":"English","publisher":"American Society of Agronomy","doi":"10.2134/jeq2003.2428","issn":"00472425","usgsCitation":"Fox, P., and Doner, H., 2003, Accumulation, release, and solubility of arsenic, molybdenum, and vanadium in wetland sediments: Journal of Environmental Quality, v. 32, no. 6, p. 2428-2435, https://doi.org/10.2134/jeq2003.2428.","productDescription":"8 p.","startPage":"2428","endPage":"2435","costCenters":[],"links":[{"id":387956,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United  States","state":"California","otherGeospatial":"San Joaquin Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -123.06884765625,\n              40.713955826286046\n            ],\n            [\n              -122.56347656249999,\n              38.993572058209466\n            ],\n            [\n              -121.83837890625,\n              37.61423141542417\n            ],\n            [\n              -120.89355468749999,\n              36.63316209558658\n            ],\n            [\n              -120.12451171875,\n              35.44277092585766\n            ],\n            [\n              -118.69628906249999,\n              34.56085936708384\n            ],\n            [\n              -117.3779296875,\n              35.02999636902566\n            ],\n            [\n              -118.3447265625,\n              36.33282808737917\n            ],\n            [\n              -121.22314453124999,\n              39.605688178320804\n            ],\n            [\n              -123.06884765625,\n              40.713955826286046\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"32","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e685e4b0c8380cd47483","contributors":{"authors":[{"text":"Fox, P.M.","contributorId":47949,"corporation":false,"usgs":true,"family":"Fox","given":"P.M.","email":"","affiliations":[],"preferred":false,"id":403051,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Doner, H.E.","contributorId":103446,"corporation":false,"usgs":true,"family":"Doner","given":"H.E.","email":"","affiliations":[],"preferred":false,"id":403052,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
]}