{"pageNumber":"1905","pageRowStart":"47600","pageSize":"25","recordCount":184582,"records":[{"id":70148657,"text":"70148657 - 2010 - Development of standard weight equations for Caribbean and Gulf of Mexico amphidromous fishes","interactions":[],"lastModifiedDate":"2015-07-13T10:48:10","indexId":"70148657","displayToPublicDate":"2010-06-18T11:45:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2886,"text":"North American Journal of Fisheries Management","active":true,"publicationSubtype":{"id":10}},"title":"Development of standard weight equations for Caribbean and Gulf of Mexico amphidromous fishes","docAbstract":"<p>We collected and compiled length and weight information from four countries and one commonwealth to develop standard weight (W<sub>s</sub>) equations for three amphidromous fish species native to the Caribbean and Gulf of Mexico regions: mountain mullet <i>Agonostomus monticola</i> (N = 9,768 individuals, 52 populations), river goby <i>Awaous banana</i> (N = 1,847 individuals, 62 populations), and bigmouth sleeper <i>Gobiomorus dormitor</i> (N = 2,983 individuals, 53 populations). Linear and quadratic W<sub>s</sub> equations for three quartiles (25%, median, 75%) are presented for these three species. The length-weight relationship from eight lentic bigmouth sleeper populations was significantly different from that of lotic populations, reflecting higher weights of juvenile fish (&lt; 70 mm total length) in lentic environments. Thus, independent W(s) equations were developed for lotic populations of bigmouth sleepers. W(s) equations were not developed from lentic bigmouth sleeper populations alone due to the low number of applicable populations caused by life history constraints; the equation from combined lentic and lotic populations is suggested for application to lentic bigmouth sleeper populations. These morphometric relationships for amphidromous fishes may improve the ability to assess existing and potential sport fisheries and allow ecological assessment based on fish condition.</p>","language":"English","publisher":"American Fisheries Society","publisherLocation":"Lawrence, KS","doi":"10.1577/M10-058.1","usgsCitation":"Cooney, P.B., and Kwak, T.J., 2010, Development of standard weight equations for Caribbean and Gulf of Mexico amphidromous fishes: North American Journal of Fisheries Management, v. 30, no. 5, p. 1203-1209, https://doi.org/10.1577/M10-058.1.","productDescription":"7 p.","startPage":"1203","endPage":"1209","numberOfPages":"7","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-020809","costCenters":[{"id":198,"text":"Coop Res Unit Atlanta","active":true,"usgs":true}],"links":[{"id":305674,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"30","issue":"5","publishingServiceCenter":{"id":8,"text":"Raleigh PSC"},"noUsgsAuthors":false,"publicationDate":"2010-10-01","publicationStatus":"PW","scienceBaseUri":"55a4e13be4b0183d66e45391","contributors":{"authors":[{"text":"Cooney, Patrick B.","contributorId":141249,"corporation":false,"usgs":false,"family":"Cooney","given":"Patrick","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":564701,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kwak, Thomas J. 0000-0002-0616-137X tkwak@usgs.gov","orcid":"https://orcid.org/0000-0002-0616-137X","contributorId":834,"corporation":false,"usgs":true,"family":"Kwak","given":"Thomas","email":"tkwak@usgs.gov","middleInitial":"J.","affiliations":[{"id":198,"text":"Coop Res Unit Atlanta","active":true,"usgs":true}],"preferred":true,"id":548956,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70118904,"text":"70118904 - 2010 - Assessing conservation relevance of organism-environment relations using predicted changes in response variables","interactions":[],"lastModifiedDate":"2014-07-31T09:13:09","indexId":"70118904","displayToPublicDate":"2010-06-18T09:11:19","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2717,"text":"Methods in Ecology and Evolution","active":true,"publicationSubtype":{"id":10}},"title":"Assessing conservation relevance of organism-environment relations using predicted changes in response variables","docAbstract":"<p>1. Organism–environment models are used widely in conservation. The degree to which they are useful for informing conservation decisions – the conservation relevance of these relations – is important because lack of relevance may lead to misapplication of scarce conservation resources or failure to resolve important conservation dilemmas. Even when models perform well based on model fit and predictive ability, conservation relevance of associations may not be clear without also knowing the magnitude and variability of predicted changes in response variables.</p>\n<br/>\n<p>2. We introduce a method for evaluating the conservation relevance of organism–environment relations that employs confidence intervals for predicted changes in response variables. The confidence intervals are compared to a preselected magnitude of change that marks a threshold (trigger) for conservation action. To demonstrate the approach, we used a case study from the Chihuahuan Desert involving relations between avian richness and broad-scale patterns of shrubland. We considered relations for three winters and two spatial extents (1- and 2-km-radius areas) and compared predicted changes in richness to three thresholds (10%, 20% and 30% change). For each threshold, we examined 48 relations.</p>\n<br/>\n<p>3. The method identified seven, four and zero conservation-relevant changes in mean richness for the 10%, 20% and 30% thresholds respectively. These changes were associated with major (20%) changes in shrubland cover, mean patch size, the coefficient of variation for patch size, or edge density but not with major changes in shrubland patch density. The relative rarity of conservation-relevant changes indicated that, overall, the relations had little practical value for informing conservation decisions about avian richness.</p>\n<br/>\n<p>4. The approach we illustrate is appropriate for various response and predictor variables measured at any temporal or spatial scale. The method is broadly applicable across ecological environments, conservation objectives, types of statistical predictive models and levels of biological organization. By focusing on magnitudes of change that have practical significance, and by using the span of confidence intervals to incorporate uncertainty of predicted changes, the method can be used to help improve the effectiveness of conservation efforts.</p>","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Methods in Ecology and Evolution","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"British Ecological Society","publisherLocation":"Hoboken, NJ","doi":"10.1111/j.2041-210X.2010.00042.x","usgsCitation":"Gutzwiller, K.J., Barrow, W., White, J., Johnson-Randall, L., Cade, B.S., and Zygo, L.M., 2010, Assessing conservation relevance of organism-environment relations using predicted changes in response variables: Methods in Ecology and Evolution, v. 1, no. 4, p. 351-358, https://doi.org/10.1111/j.2041-210X.2010.00042.x.","productDescription":"8 p.","startPage":"351","endPage":"358","numberOfPages":"8","costCenters":[],"links":[{"id":475709,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1111/j.2041-210x.2010.00042.x","text":"Publisher Index Page"},{"id":291450,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":291449,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1111/j.2041-210X.2010.00042.x"}],"volume":"1","issue":"4","noUsgsAuthors":false,"publicationDate":"2010-06-18","publicationStatus":"PW","scienceBaseUri":"53db5841e4b0fba533fa3567","contributors":{"authors":[{"text":"Gutzwiller, Kevin J.","contributorId":101923,"corporation":false,"usgs":true,"family":"Gutzwiller","given":"Kevin","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":497384,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Barrow, Wylie C. 0000-0003-4671-2823 barroww@usgs.gov","orcid":"https://orcid.org/0000-0003-4671-2823","contributorId":1988,"corporation":false,"usgs":true,"family":"Barrow","given":"Wylie C.","email":"barroww@usgs.gov","affiliations":[{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true}],"preferred":false,"id":497380,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"White, Joseph D.","contributorId":56077,"corporation":false,"usgs":true,"family":"White","given":"Joseph D.","affiliations":[],"preferred":false,"id":497383,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Johnson-Randall, Lori 0000-0003-0100-994X","orcid":"https://orcid.org/0000-0003-0100-994X","contributorId":43604,"corporation":false,"usgs":true,"family":"Johnson-Randall","given":"Lori","affiliations":[{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"preferred":false,"id":497381,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Cade, Brian S. 0000-0001-9623-9849 cadeb@usgs.gov","orcid":"https://orcid.org/0000-0001-9623-9849","contributorId":1278,"corporation":false,"usgs":true,"family":"Cade","given":"Brian","email":"cadeb@usgs.gov","middleInitial":"S.","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":true,"id":497379,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Zygo, Lisa M.","contributorId":50456,"corporation":false,"usgs":true,"family":"Zygo","given":"Lisa","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":497382,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70202860,"text":"ofr20101125 - 2010 - Evidence of envronmental change in Rankin basin, Central Florida Bay, Everglades National Park","interactions":[],"lastModifiedDate":"2026-01-30T15:57:07.022726","indexId":"ofr20101125","displayToPublicDate":"2010-06-18T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2010-1125","displayTitle":"Evidence of Envronmental Change in Rankin Basin, Central Florida Bay, Everglades National Park","title":"Evidence of envronmental change in Rankin basin, Central Florida Bay, Everglades National Park","docAbstract":"<p>Analyses of core GLBW601 RL1 collected in Rankin Basin, Florida Bay, Everglades National Park, in June 2001 indicate that significant environmental changes occurred at the site over the last two centuries. The core was collected at a site of documented seagrass die-off in 1987-1988. The purpose of this study was to document the long-term sequences of events leading up to the die-off event. Analyses have been conducted to examine (1) faunal changes in the ostracodes and mollusks, (2) biochemistry of the ostracode shells, (3) floral changes in the pollen assemblages, and (4) geochemical and elemental changes in the sediment. The faunal assemblage analyses provide information on the salinity and benthic habitat at the site. The biochemical and geochemical data provide information about the water chemistry and sedimentation rates. The floral assemblage provides data about the nearby terrestrial environment and the first occurrence of pollen of the Australian pine, <i>Casuarina equisetifolia</i>, serves as a biostratigraphic marker for the beginning of the 20th century. These data provide clues to the cause and effect of the seagrass die-off and changes in salinity patterns and also illustrate decadal-scale patterns of change.</p><p>The analyses of GLBW601 RL1 show two important results. First, prior to 1900, Rankin Basin tended to be oligohaline to mesohaline on the basis of faunal data showing the assemblage to be similar to that of the lowest portions of a core from Taylor Creek. Second, prior to the documented seagrass die-off, the faunal assemblages indicate an increase in the amplitude of salinity fluctuations; a significant increase occurs in the mollusks <i>Brachidontes exustus</i> and <i>Anomalocardia auberiana</i>, two species that tolerate fluctuations in salinity.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20101125","usgsCitation":"Murray, J.B., Wingard, G.L., Cronin, T.M., Orem, W.H., Willard, D.A., Holmes, C.W., Reich, C., Shinn, E., Marot, M., Lerch, T., Trappe, C., and Landacre, B., 2010,  Evidence of envornmental change in Rankin Basin, central Florida Bay, Everglades National Park: U.S. Geological Survey Open-File Report 2010–1125, 49 p., https://doi.usgs.gov/10.3133/ofr20101125.","productDescription":"vi, 22 p.","costCenters":[{"id":27821,"text":"Caribbean-Florida Water Science Center","active":true,"usgs":true}],"links":[{"id":362628,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2010/1125/coverthb.jpg"},{"id":362629,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2010/1125/ofr20101125.pdf","text":"Report","size":"2.67 MB","linkFileType":{"id":1,"text":"pdf"},"description":"OFR 2010-1125"}],"country":"United States","state":"Florida","otherGeospatial":"Florida Bay","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -80.85311271484309,\n              25.132490788646592\n            ],\n            [\n              -80.85311271484309,\n              25.07697728453293\n            ],\n            [\n              -80.78943182632912,\n              25.07697728453293\n            ],\n            [\n              -80.78943182632912,\n              25.132490788646592\n            ],\n            [\n              -80.85311271484309,\n              25.132490788646592\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","contact":"<p><a href=\"https://www.usgs.gov/centers/car-fl-water\" data-mce-href=\"https://www.usgs.gov/centers/car-fl-water\">Caribbean-Florida Water Science Center</a><br>U.S. Geological Survey<br>3321 College Avenue<br>Davie, FL 33314</p><p><a href=\"../contact\" data-mce-href=\"../contact\">Contact Pubs Warehouse</a></p>","tableOfContents":"<ul><li>Acknowledgments</li><li>Introduction</li><li>Setting</li><li>Methods</li><li>Results</li><li>Discussiojn</li><li>References</li></ul>","publishedDate":"2010-06-18","noUsgsAuthors":false,"publicationDate":"2010-06-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Murray, James B. jbmurray@usgs.gov","contributorId":2065,"corporation":false,"usgs":true,"family":"Murray","given":"James","email":"jbmurray@usgs.gov","middleInitial":"B.","affiliations":[],"preferred":true,"id":760309,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cronin, Thomas M. 0000-0002-2643-0979 tcronin@usgs.gov","orcid":"https://orcid.org/0000-0002-2643-0979","contributorId":2579,"corporation":false,"usgs":true,"family":"Cronin","given":"Thomas","email":"tcronin@usgs.gov","middleInitial":"M.","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":760311,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wingard, G. Lynn","contributorId":44969,"corporation":false,"usgs":true,"family":"Wingard","given":"G. Lynn","affiliations":[],"preferred":false,"id":760321,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Orem, William H. 0000-0003-4990-0539 borem@usgs.gov","orcid":"https://orcid.org/0000-0003-4990-0539","contributorId":577,"corporation":false,"usgs":true,"family":"Orem","given":"William","email":"borem@usgs.gov","middleInitial":"H.","affiliations":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":760312,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Willard, Debra A. 0000-0003-4878-0942 dwillard@usgs.gov","orcid":"https://orcid.org/0000-0003-4878-0942","contributorId":2076,"corporation":false,"usgs":true,"family":"Willard","given":"Debra","email":"dwillard@usgs.gov","middleInitial":"A.","affiliations":[{"id":411,"text":"National Climate Change and Wildlife Science Center","active":true,"usgs":true},{"id":24693,"text":"Climate Research and Development","active":true,"usgs":true}],"preferred":true,"id":760313,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Holmes, Charles W.","contributorId":31071,"corporation":false,"usgs":true,"family":"Holmes","given":"Charles","email":"","middleInitial":"W.","affiliations":[{"id":218,"text":"Denver Federal Center","active":false,"usgs":true}],"preferred":false,"id":760314,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Reich, Christopher D. 0000-0002-2534-1456 creich@usgs.gov","orcid":"https://orcid.org/0000-0002-2534-1456","contributorId":900,"corporation":false,"usgs":true,"family":"Reich","given":"Christopher","email":"creich@usgs.gov","middleInitial":"D.","affiliations":[{"id":574,"text":"St. Petersburg Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":760315,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Shinn, Eugene","contributorId":201157,"corporation":false,"usgs":false,"family":"Shinn","given":"Eugene","affiliations":[],"preferred":false,"id":760316,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Marot, Marci E. 0000-0003-0504-315X mmarot@usgs.gov","orcid":"https://orcid.org/0000-0003-0504-315X","contributorId":2078,"corporation":false,"usgs":true,"family":"Marot","given":"Marci","email":"mmarot@usgs.gov","middleInitial":"E.","affiliations":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true},{"id":574,"text":"St. Petersburg Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":760317,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Lerch, Terry","contributorId":24040,"corporation":false,"usgs":true,"family":"Lerch","given":"Terry","email":"","affiliations":[],"preferred":false,"id":760318,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Trappe, Carleigh A.","contributorId":37782,"corporation":false,"usgs":true,"family":"Trappe","given":"Carleigh","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":760319,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Landacre, Bryan","contributorId":74468,"corporation":false,"usgs":true,"family":"Landacre","given":"Bryan","affiliations":[],"preferred":false,"id":760320,"contributorType":{"id":1,"text":"Authors"},"rank":12}]}}
,{"id":98460,"text":"fs20103031 - 2010 - Availability of Groundwater Data for California, Water Year 2009","interactions":[],"lastModifiedDate":"2012-03-08T17:16:13","indexId":"fs20103031","displayToPublicDate":"2010-06-18T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2010-3031","title":"Availability of Groundwater Data for California, Water Year 2009","docAbstract":"The U.S. Geological Survey, in cooperation with Federal, State, and local agencies, obtains a large amount of data pertaining to the groundwater resources of California each water year (October 1-September 30). These data constitute a valuable database for developing an improved understanding of the water resources of the State.\r\n\r\nThis Fact Sheet serves as an index to groundwater data for Water Year 2009. The 2 page report contains a map of California showing the number of wells (by county) with available water-level and water-quality data for Water Year 2009 (fig. 1) and instructions for obtaining this and other groundwater information contained in the databases of the U.S. Geological Survey, California Water Science Center.\r\n\r\nFrom 1985 to 1993, data were published in the annual report 'Water Resources Data for California, Volume 5. Ground-Water Data'; prior to 1985, the data were published in U.S. Geological Survey Water-Supply Papers.\r\n","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/fs20103031","usgsCitation":"Ray, M., 2010, Availability of Groundwater Data for California, Water Year 2009: U.S. Geological Survey Fact Sheet 2010-3031, 2 p., https://doi.org/10.3133/fs20103031.","productDescription":"2 p.","temporalStart":"2008-10-01","temporalEnd":"2009-09-30","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"links":[{"id":125914,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2010_3031.jpg"},{"id":13732,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2010/3031/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa9e4b07f02db667fa3","contributors":{"authors":[{"text":"Ray, Mary","contributorId":51704,"corporation":false,"usgs":true,"family":"Ray","given":"Mary","affiliations":[],"preferred":false,"id":305384,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":98461,"text":"ofr20101020 - 2010 - The power to detect trends in Missouri River fish populations within the Pallid Sturgeon Population Assessment Program","interactions":[],"lastModifiedDate":"2017-02-01T11:10:00","indexId":"ofr20101020","displayToPublicDate":"2010-06-18T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2010-1020","title":"The power to detect trends in Missouri River fish populations within the Pallid Sturgeon Population Assessment Program","docAbstract":"As with all large rivers in the United States, the Missouri River has been altered, with approximately 32.5 percent of the main stem length impounded and 32.5 percent channelized. These physical alterations to the environment have had effects on the fisheries, but studies examining the effects of alterations have been localized and for short periods of time. In response to the U.S. Fish and Wildlife Service biological opinion, the U.S. Army Corps of Engineers initiated monitoring of the fish community of the Missouri River in 2003. The goal of the Pallid Sturgeon Population Assessment Program is to provide information to detect changes in populations and habitat preferences with time for pallid sturgeon (Scaphirhynchus albus) and native target species in the Missouri River Basin. To determine statistical power of the Pallid Sturgeon Population Assessment Program, a power analysis was conducted using a normal linear mixed model with variance component estimates based on the first 3 years of data (2003 to 2005). In cases where 3 years of data were unavailable, estimates were obtained using those data. It was determined that at least 20 years of data, sampling 12 bends with 8 subsamples per bend, would be required to detect a 5 percent annual decline in most of the target fish populations. Power varied between Zones. Zone 1 (upstream from Lake Sakakawea) did not have any species/gear type combinations with adequate power, whereas Zone 3 (downstream from Gavins Point Dam) had 19 species/gear type combinations with adequate power. With a slight increase in the sampling effort to 12 subsamples per bend, the Pallid Sturgeon Population Assessment Program has adequate power to detect declines in shovelnose sturgeon (S. platorynchus) throughout the entire Missouri River because of large catch rates. The lowest level of non-occurrence (in other words, zero catches) at the bend level for pallid sturgeon was 0.58 using otter trawls in Zone 1. Consequently, the power of the pallid sturgeon models was not as high as other species at the current level of sampling, but an increase in the sampling effort to 16 subsamples for each of 24 bends for 20 years would generate adequate power for the pallid sturgeon in all Zones. Since gear types are selective in their species efficiency, the strength of the Pallid Sturgeon Population Assessment Program approach is using multiple gears that have statistical power to detect population trends at the same time in different fish species within the Missouri River. As often is the case with monitoring studies involving endangered species, the data used to conduct the analyses exhibit some departures from the parametric model assumptions; however, preliminary simulations indicate that the results of this study are appropriate.\r\n","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20101020","collaboration":"Prepared in cooperation with the U. S. Army Corp of Engineers","usgsCitation":"Bryan, J.L., Wildhaber, M.L., Gladish, D., Holan, S., and Ellerseick, M., 2010, The power to detect trends in Missouri River fish populations within the Pallid Sturgeon Population Assessment Program: U.S. Geological Survey Open-File Report 2010-1020, viii, 23 p.; Figures; Tables; Appendices, https://doi.org/10.3133/ofr20101020.","productDescription":"viii, 23 p.; Figures; Tables; Appendices","additionalOnlineFiles":"Y","costCenters":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"links":[{"id":125915,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr_2010_1020.jpg"},{"id":334531,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2010/1020/pdf/ofr2010_1020.pdf","size":"7 MB","linkFileType":{"id":1,"text":"pdf"}},{"id":334532,"rank":4,"type":{"id":3,"text":"Appendix"},"url":"https://pubs.usgs.gov/of/2010/1020/data/","text":"Appendixes"},{"id":13733,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2010/1020/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67ad81","contributors":{"authors":[{"text":"Bryan, Janice L.","contributorId":58589,"corporation":false,"usgs":true,"family":"Bryan","given":"Janice","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":305387,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wildhaber, Mark L. 0000-0002-6538-9083 mwildhaber@usgs.gov","orcid":"https://orcid.org/0000-0002-6538-9083","contributorId":1386,"corporation":false,"usgs":true,"family":"Wildhaber","given":"Mark","email":"mwildhaber@usgs.gov","middleInitial":"L.","affiliations":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"preferred":true,"id":305385,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gladish, Dan","contributorId":92217,"corporation":false,"usgs":true,"family":"Gladish","given":"Dan","email":"","affiliations":[],"preferred":false,"id":305389,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Holan, Scott","contributorId":52138,"corporation":false,"usgs":true,"family":"Holan","given":"Scott","email":"","affiliations":[],"preferred":false,"id":305386,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Ellerseick, Mark","contributorId":84323,"corporation":false,"usgs":true,"family":"Ellerseick","given":"Mark","email":"","affiliations":[],"preferred":false,"id":305388,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70037734,"text":"70037734 - 2010 - Controls on mangrove forest‐atmosphere carbon dioxide exchanges in western Everglades National Park","interactions":[],"lastModifiedDate":"2021-02-16T16:59:25.515513","indexId":"70037734","displayToPublicDate":"2010-06-17T15:27:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":7359,"text":"Journal of Geophysical Research Biogeosciences","active":true,"publicationSubtype":{"id":10}},"title":"Controls on mangrove forest‐atmosphere carbon dioxide exchanges in western Everglades National Park","docAbstract":"<p><span>We report on net ecosystem production (NEP) and key environmental controls on net ecosystem exchange (NEE) of carbon dioxide (CO</span><sub>2</sub><span>) between a mangrove forest and the atmosphere in the coastal Florida Everglades. An eddy covariance system deployed above the canopy was used to determine NEE during January 2004 through August 2005. Maximum daytime NEE ranged from −20 to −25&nbsp;</span><i>μ</i><span>mol (CO</span><sub>2</sub><span>) m</span><sup>−2</sup><span>&nbsp;s</span><sup>−1</sup><span>&nbsp;between March and May. Respiration (R</span><sub>d</sub><span>) was highly variable (2.81 ± 2.41&nbsp;</span><i>μ</i><span>mol (CO</span><sub>2</sub><span>) m</span><sup>−2</sup><span>&nbsp;s</span><sup>−1</sup><span>), reaching peak values during the summer wet season. During the winter dry season, forest CO</span><sub>2</sub><span>&nbsp;assimilation increased with the proportion of diffuse solar irradiance in response to greater radiative transfer in the forest canopy. Surface water salinity and tidal activity were also important controls on NEE. Daily light use efficiency was reduced at high (&gt;34 parts per thousand (ppt)) compared to low (&lt;17 ppt) salinity by 46%. Tidal inundation lowered daytime R</span><sub>d</sub><span>&nbsp;by ∼0.9&nbsp;</span><i>μ</i><span>mol (CO</span><sub>2</sub><span>) m</span><sup>−2</sup><span>&nbsp;s</span><sup>−1</sup><span>&nbsp;and nighttime R</span><sub>d</sub><span>&nbsp;by ∼0.5&nbsp;</span><i>μ</i><span>mol (CO</span><sub>2</sub><span>) m</span><sup>−2</sup><span>&nbsp;s</span><sup>−1</sup><span>. The forest was a sink for atmospheric CO</span><sub>2</sub><span>, with an annual NEP of 1170 ± 127 g C m</span><sup>−2</sup><span>&nbsp;during 2004. This unusually high NEP was attributed to year‐round productivity and low ecosystem respiration which reached a maximum of only 3 g C m</span><sup>−2</sup><span>&nbsp;d</span><sup>−1</sup><span>. Tidal export of dissolved inorganic carbon derived from belowground respiration likely lowered the estimates of mangrove forest respiration. These results suggest that carbon balance in mangrove coastal systems will change in response to variable salinity and inundation patterns, possibly resulting from secular sea level rise and climate change.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/2009JG001186","usgsCitation":"Barr, J.G., Engel, V., Fuentes, J.D., Zieman, J.C., O’Halloran, T.L., Smith, T.J., and Anderson, G.H., 2010, Controls on mangrove forest‐atmosphere carbon dioxide exchanges in western Everglades National Park: Journal of Geophysical Research Biogeosciences, v. 115, no. G2, 14 p., https://doi.org/10.1029/2009JG001186.","productDescription":"14 p.","costCenters":[{"id":275,"text":"Florida Integrated Science Center","active":false,"usgs":true},{"id":566,"text":"Southeast Ecological Science Center","active":true,"usgs":true}],"links":[{"id":475710,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1029/2009jg001186","text":"Publisher Index Page"},{"id":383288,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Florida","otherGeospatial":"Everglades National Park","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -81.8096923828125,\n              25.090573819461\n            ],\n            [\n              -79.7113037109375,\n              25.090573819461\n            ],\n            [\n              -79.7113037109375,\n              26.75051574561839\n            ],\n            [\n              -81.8096923828125,\n              26.75051574561839\n            ],\n            [\n              -81.8096923828125,\n              25.090573819461\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"115","issue":"G2","noUsgsAuthors":false,"publicationDate":"2010-06-17","publicationStatus":"PW","scienceBaseUri":"5059fbd1e4b0c8380cd4df9e","contributors":{"authors":[{"text":"Barr, Jordan G.","contributorId":85809,"corporation":false,"usgs":false,"family":"Barr","given":"Jordan","email":"","middleInitial":"G.","affiliations":[{"id":13531,"text":"South Florida Natural Resource Center, Everglades National Park","active":true,"usgs":false}],"preferred":false,"id":462536,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Engel, Vic 0000-0002-3858-7308","orcid":"https://orcid.org/0000-0002-3858-7308","contributorId":101790,"corporation":false,"usgs":true,"family":"Engel","given":"Vic","affiliations":[],"preferred":false,"id":462538,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fuentes, Jose D.","contributorId":97231,"corporation":false,"usgs":true,"family":"Fuentes","given":"Jose","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":462537,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Zieman, Joseph C.","contributorId":20806,"corporation":false,"usgs":true,"family":"Zieman","given":"Joseph","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":462534,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"O’Halloran, Thomas L.","contributorId":48838,"corporation":false,"usgs":true,"family":"O’Halloran","given":"Thomas","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":462535,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Smith, Thomas J. III tom_j_smith@usgs.gov","contributorId":1615,"corporation":false,"usgs":true,"family":"Smith","given":"Thomas","suffix":"III","email":"tom_j_smith@usgs.gov","middleInitial":"J.","affiliations":[{"id":566,"text":"Southeast Ecological Science Center","active":true,"usgs":true}],"preferred":false,"id":462532,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Anderson, Gordon H. 0000-0003-1675-8329 gordon_anderson@usgs.gov","orcid":"https://orcid.org/0000-0003-1675-8329","contributorId":2771,"corporation":false,"usgs":true,"family":"Anderson","given":"Gordon","email":"gordon_anderson@usgs.gov","middleInitial":"H.","affiliations":[{"id":566,"text":"Southeast Ecological Science Center","active":true,"usgs":true},{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"preferred":true,"id":462533,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70168801,"text":"70168801 - 2010 - The changing effects of Alaska’s boreal forests on the climate system","interactions":[],"lastModifiedDate":"2017-01-12T10:58:53","indexId":"70168801","displayToPublicDate":"2010-06-17T14:45:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1170,"text":"Canadian Journal of Forest Research","active":true,"publicationSubtype":{"id":10}},"title":"The changing effects of Alaska’s boreal forests on the climate system","docAbstract":"<p>In the boreal forests of Alaska, recent changes in climate have influenced the exchange of trace gases, water, and energy between these forests and the atmosphere. These changes in the structure and function of boreal forests can then feed back to impact regional and global climates. In this manuscript, we examine the type and magnitude of the climate feedbacks from boreal forests in Alaska. Research generally suggests that the net effect of a warming climate is a positive regional feedback to warming. Currently, the primary positive climate feedbacks are likely related to decreases in surface albedo due to decreases in snow cover. Fewer negative feedbacks have been identified, and they may not be large enough to counterbalance the large positive feedbacks. These positive feedbacks are most pronounced at the regional scale and reduce the resilience of the boreal vegetation &ndash; climate system by amplifying the rate of regional warming. Given the recent warming in this region, the large variety of associated mechanisms that can alter terrestrial ecosystems and influence the climate system, and a reduction in the boreal forest resilience, there is a strong need to continue to quantify and evaluate the feedback pathways.</p>","language":"English","publisher":"NRC Research Press","doi":"10.1139/X09-209","usgsCitation":"Euskirchen, E., McGuire, A.D., Chapin, F., and Rupp, T., 2010, The changing effects of Alaska’s boreal forests on the climate system: Canadian Journal of Forest Research, v. 40, no. 7, p. 1336-1346, https://doi.org/10.1139/X09-209.","productDescription":"11 p.","startPage":"1336","endPage":"1346","numberOfPages":"11","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-018388","costCenters":[{"id":199,"text":"Coop Res Unit Leetown","active":true,"usgs":true}],"links":[{"id":318565,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United 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,{"id":98459,"text":"ofr20101105 - 2010 - Hurricane Influences on Vegetation Community Change in Coastal Louisiana","interactions":[],"lastModifiedDate":"2019-03-27T13:45:00","indexId":"ofr20101105","displayToPublicDate":"2010-06-17T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2010-1105","title":"Hurricane Influences on Vegetation Community Change in Coastal Louisiana","docAbstract":"The impacts of Hurricanes Katrina and Rita in 2005 on wetland vegetation were investigated in Louisiana coastal marshes. Vegetation cover, pore-water salinity, and nutrients data from 100 marsh sites covering the entire Louisiana coast were sampled for two consecutive growing seasons after the storms. A mixed-model nested ANOVA with Tukey's HSD test for post-ANOVA multiple comparisons was used to analyze the data. Significantly (p<0.05) lower vegetation cover was observed within brackish and fresh marshes in the west as compared to the east and central regions throughout 2006, but considerable increase in vegetation cover was noticed in fall 2007 data. Marshes in the west were stressed by prolonged saltwater logging and increased sulfide content. High salinity levels persisted throughout the study period for all marsh types, especially in the west. The marshes of coastal Louisiana are still recovering after the hurricanes; however, changes in the species composition have increased in these marshes.\r\n","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20101105","usgsCitation":"Steyer, G.D., Cretini, K.F., Piazza, S.C., Sharp, L., Snedden, G., and Sapkota, S., 2010, Hurricane Influences on Vegetation Community Change in Coastal Louisiana: U.S. Geological Survey Open-File Report 2010-1105, vi, 21 p., https://doi.org/10.3133/ofr20101105.","productDescription":"vi, 21 p.","onlineOnly":"Y","costCenters":[{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true},{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"links":[{"id":125913,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr_2010_1105.jpg"},{"id":13731,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2010/1105/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db62a1a4","contributors":{"authors":[{"text":"Steyer, Gregory D. 0000-0001-7231-0110 steyerg@usgs.gov","orcid":"https://orcid.org/0000-0001-7231-0110","contributorId":2856,"corporation":false,"usgs":true,"family":"Steyer","given":"Gregory","email":"steyerg@usgs.gov","middleInitial":"D.","affiliations":[{"id":5062,"text":"Office of the Chief Scientist for Ecosystems","active":true,"usgs":true},{"id":5064,"text":"Southeast Regional Director's Office","active":true,"usgs":true},{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true},{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"preferred":true,"id":305379,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cretini, Kari Foster 0000-0003-0419-0748","orcid":"https://orcid.org/0000-0003-0419-0748","contributorId":40314,"corporation":false,"usgs":true,"family":"Cretini","given":"Kari","email":"","middleInitial":"Foster","affiliations":[],"preferred":false,"id":305382,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Piazza, Sarai C. 0000-0001-6962-9008 piazzas@usgs.gov","orcid":"https://orcid.org/0000-0001-6962-9008","contributorId":466,"corporation":false,"usgs":true,"family":"Piazza","given":"Sarai","email":"piazzas@usgs.gov","middleInitial":"C.","affiliations":[{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true}],"preferred":false,"id":305378,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Sharp, Leigh A.","contributorId":43879,"corporation":false,"usgs":true,"family":"Sharp","given":"Leigh A.","affiliations":[],"preferred":false,"id":305383,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Snedden, Gregg A. 0000-0001-7821-3709","orcid":"https://orcid.org/0000-0001-7821-3709","contributorId":17338,"corporation":false,"usgs":true,"family":"Snedden","given":"Gregg A.","affiliations":[{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"preferred":false,"id":305381,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Sapkota, Sijan sapkotas@usgs.gov","contributorId":2995,"corporation":false,"usgs":true,"family":"Sapkota","given":"Sijan","email":"sapkotas@usgs.gov","affiliations":[{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true}],"preferred":true,"id":305380,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":5224963,"text":"5224963 - 2010 - Uncovering a latent multinomial: Analysis of mark–recapture data with misidentification","interactions":[],"lastModifiedDate":"2021-02-23T12:40:04.048926","indexId":"5224963","displayToPublicDate":"2010-06-16T12:18:37","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1039,"text":"Biometrics","active":true,"publicationSubtype":{"id":10}},"title":"Uncovering a latent multinomial: Analysis of mark–recapture data with misidentification","docAbstract":"Natural tags based on DNA fingerprints or natural features of animals are now becoming very widely used in wildlife population biology.  However, classic capture-recapture models do not allow for misidentification of animals which is a potentially very serious problem with natural tags.  Statistical analysis of misidentification processes is extremely difficult using traditional likelihood methods but is easily handled using Bayesian methods.  We present a general framework for Bayesian analysis of categorical data arising from a latent multinomial distribution.  Although our work is motivated by a specific model for misidentification in closed population capture-recapture analyses, with crucial assumptions which may not always be appropriate, the methods we develop extend naturally to a variety of other models with similar structure.  Suppose that observed frequencies f are a known linear transformation f=A'x of a latent multinomial variable x with cell probability vector pi= pi(theta).  Given that full conditional distributions [theta | x] can be sampled, implementation of Gibbs sampling requires only that we can sample from the full conditional distribution [x | f, theta], which is made possible by knowledge of the null space of A'.  We illustrate the approach using two data sets with individual misidentification, one simulated, the other summarizing recapture data for salamanders based on natural marks.","language":"English","publisher":"Wiley","doi":"10.1111/j.1541-0420.2009.01244.x","usgsCitation":"Link, W., Yoshizaki, J., Bailey, L., and Pollock, K.H., 2010, Uncovering a latent multinomial: Analysis of mark–recapture data with misidentification: Biometrics, v. 66, no. 1, p. 178-185, https://doi.org/10.1111/j.1541-0420.2009.01244.x.","productDescription":"8 p.","startPage":"178","endPage":"185","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":475711,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1111/j.1541-0420.2009.01244.x","text":"Publisher Index Page"},{"id":383404,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"66","issue":"1","noUsgsAuthors":false,"publicationDate":"2010-03-17","publicationStatus":"PW","scienceBaseUri":"4f4e4a26e4b07f02db60f621","contributors":{"authors":[{"text":"Link, W.A. 0000-0002-9913-0256","orcid":"https://orcid.org/0000-0002-9913-0256","contributorId":8815,"corporation":false,"usgs":true,"family":"Link","given":"W.A.","affiliations":[],"preferred":false,"id":343306,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Yoshizaki, J.","contributorId":79596,"corporation":false,"usgs":true,"family":"Yoshizaki","given":"J.","email":"","affiliations":[],"preferred":false,"id":343309,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bailey, L.L. 0000-0002-5959-2018","orcid":"https://orcid.org/0000-0002-5959-2018","contributorId":61006,"corporation":false,"usgs":true,"family":"Bailey","given":"L.L.","affiliations":[],"preferred":false,"id":343307,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Pollock, K. H.","contributorId":65184,"corporation":false,"usgs":false,"family":"Pollock","given":"K.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":343308,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70230293,"text":"70230293 - 2010 - Immediate and long-term fire effects on total mercury in forests soils of northeastern Minnesota","interactions":[],"lastModifiedDate":"2022-04-06T15:37:32.320055","indexId":"70230293","displayToPublicDate":"2010-06-16T10:27:35","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5925,"text":"Environmental Science and Technology","active":true,"publicationSubtype":{"id":10}},"title":"Immediate and long-term fire effects on total mercury in forests soils of northeastern Minnesota","docAbstract":"<p><span>Within the Boundary Waters Canoe Area Wilderness in northeastern Minnesota, soils were collected from 116 sites in areas of primarily virgin forest with fire-origin stand years (year of last recognizable stand-killing wildfire) that range from the 1759 to 1976. Median concentrations for total mercury in soils for this span of 217 years range from 0.28 ± 0.088 ppm (1759) to 0.09 ± 0.047 ppm (1976) for A-horizon soils and from 0.23 ± 0.062 ppm (1759) to 0.09 ± 0.018 ppm (1976) for O-horizon soils. A separate study of soils collected from 30 sites within an area that burned in a 2004 wildfire at Voyageurs National Park, northern Minnesota, suggested that high soil burn severity resulted in significant mercury loss from both organic and mineral soils. Integrated data from these two studies and additional regional soil data demonstrate that older forests have progressively higher mercury concentrations in O-horizon soils (r</span><sup>2</sup><span>&nbsp;= 0.423) and A-horizon soils (r</span><sup>2</sup><span>&nbsp;= 0.456). These results support the hypotheses that an important factor for mercury concentrations in forest soils is time since stand-replacing fire and that high soil burn severity has the potential to reduce the concentration of mercury in burned soils for tens to hundreds of years.</span></p>","language":"English","publisher":"ACS Publications","doi":"10.1021/es100544d","usgsCitation":"Woodruff, L.G., and Cannon, W.F., 2010, Immediate and long-term fire effects on total mercury in forests soils of northeastern Minnesota: Environmental Science and Technology, v. 44, no. 14, p. 5371-5376, https://doi.org/10.1021/es100544d.","productDescription":"6 p.","startPage":"5371","endPage":"5376","costCenters":[{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"links":[{"id":398225,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Minnesota","otherGeospatial":"Boundary Waters Canoe Area Wilderness, Voyageurs National Park","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -89.9176025390625,\n              47.942106827553026\n            ],\n            [\n              -90.0494384765625,\n              48.111099041065366\n            ],\n            [\n              -90.5712890625,\n              48.10743118848039\n            ],\n            [\n              -90.7470703125,\n              48.10743118848039\n            ],\n            [\n              -90.86242675781249,\n              48.246625590713826\n            ],\n            [\n              -91.2799072265625,\n              48.09275716032736\n            ],\n            [\n              -91.56005859375,\n              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Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":839893,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70006211,"text":"70006211 - 2010 - Avipoxvirus","interactions":[],"lastModifiedDate":"2018-01-04T12:41:08","indexId":"70006211","displayToPublicDate":"2010-06-16T06:30:00","publicationYear":"2010","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Avipoxvirus","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Invasive Species Compendium","language":"English","publisher":"C.A.B. International","publisherLocation":"Wallingford, Oxfordshire","usgsCitation":"LaPointe, D., 2010, Avipoxvirus, chap. <i>of</i> Invasive Species Compendium, HTML Document.","productDescription":"HTML Document","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-022451","costCenters":[{"id":521,"text":"Pacific Island Ecosystems Research Center","active":false,"usgs":true}],"links":[{"id":326618,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":258013,"type":{"id":11,"text":"Document"},"url":"https://www.cabi.org/isc/datasheet/33990"}],"country":"UNITED STATES","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57b58abfe4b03bcb0104bb60","contributors":{"authors":[{"text":"LaPointe, Dennis dlapointe@usgs.gov","contributorId":2926,"corporation":false,"usgs":true,"family":"LaPointe","given":"Dennis","email":"dlapointe@usgs.gov","affiliations":[{"id":5049,"text":"Pacific Islands Ecosys Research Center","active":true,"usgs":true}],"preferred":false,"id":513532,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70156647,"text":"70156647 - 2010 - Assessing societal vulnerability of U.S. Pacific Northwest communities to storm-induced coastal change","interactions":[],"lastModifiedDate":"2021-11-09T16:04:05.742504","indexId":"70156647","displayToPublicDate":"2010-06-16T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Assessing societal vulnerability of U.S. Pacific Northwest communities to storm-induced coastal change","docAbstract":"<p><span>Progressive increases in storm intensities and extreme wave heights have been documented along the U.S. West Coast. Paired with global sea level rise and the potential for an increase in El Niño occurrences, these trends have substantial implications for the vulnerability of coastal communities to natural coastal hazards. Community vulnerability to hazards is characterized by the exposure, sensitivity, and adaptive capacity of human-environmental systems that influence potential impacts. To demonstrate how societal vulnerability to coastal hazards varies with both physical and social factors, we compared community exposure and sensitivity to storm-induced coastal change scenarios in Tillamook (Oregon) and Pacific (Washington) Counties. While both are backed by low-lying coastal dunes, communities in these two counties have experienced different shoreline change histories and have chosen to use the adjacent land in different ways. Therefore, community vulnerability varies significantly between the two counties. Identifying the reasons for this variability can help land-use managers make decisions to increase community resilience and reduce vulnerability in spite of a changing climate.</span></p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Shifting shorelines: Adapting to the future","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"Shifting Shorelines: Adapting to the Future, The 22nd International Conference of the Coastal Society","conferenceDate":"June 13-16 2010","conferenceLocation":"Wilmington, North Carolina","language":"English","publisher":"Coastal Society","usgsCitation":"Baron, H.M., Wood, N.J., Ruggerio, P., Allan, J., and Corcoran, P., 2010, Assessing societal vulnerability of U.S. Pacific Northwest communities to storm-induced coastal change, <i>in</i> Shifting shorelines: Adapting to the future, Wilmington, North Carolina, June 13-16 2010, 4 p.","productDescription":"4 p.","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-019447","costCenters":[{"id":657,"text":"Western Geographic Science Center","active":true,"usgs":true}],"links":[{"id":307431,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Oregon, Washington","county":"Pacific County, Tillamook County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -124.134521484375,\n              44.94924926661153\n            ],\n            [\n              -122.73376464843749,\n              44.94924926661153\n            ],\n            [\n              -122.73376464843749,\n              46.93526088057719\n            ],\n            [\n              -124.134521484375,\n              46.93526088057719\n            ],\n            [\n              -124.134521484375,\n              44.94924926661153\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"55dd91aee4b0518e354dd128","contributors":{"authors":[{"text":"Baron, Heather M.","contributorId":138585,"corporation":false,"usgs":false,"family":"Baron","given":"Heather","email":"","middleInitial":"M.","affiliations":[{"id":6680,"text":"Oregon State University","active":true,"usgs":false}],"preferred":false,"id":569790,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wood, Nathan J. 0000-0002-6060-9729 nwood@usgs.gov","orcid":"https://orcid.org/0000-0002-6060-9729","contributorId":3347,"corporation":false,"usgs":true,"family":"Wood","given":"Nathan","email":"nwood@usgs.gov","middleInitial":"J.","affiliations":[{"id":657,"text":"Western Geographic Science Center","active":true,"usgs":true}],"preferred":true,"id":569791,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ruggerio, Peter","contributorId":67403,"corporation":false,"usgs":true,"family":"Ruggerio","given":"Peter","email":"","affiliations":[],"preferred":false,"id":569792,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Allan, Jonathan","contributorId":46847,"corporation":false,"usgs":false,"family":"Allan","given":"Jonathan","affiliations":[{"id":7198,"text":"Oregon Department Geology and Mineral Industries","active":true,"usgs":false}],"preferred":false,"id":569793,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Corcoran, Patrick","contributorId":138588,"corporation":false,"usgs":false,"family":"Corcoran","given":"Patrick","email":"","affiliations":[{"id":12452,"text":"Oregon Sea Grant","active":true,"usgs":false}],"preferred":false,"id":569794,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70189133,"text":"70189133 - 2010 - Productivity, embryo and eggshell characteristics, and contaminants in bald eagles from the Great Lakes, USA, 1986 to 2000","interactions":[],"lastModifiedDate":"2018-10-17T15:58:45","indexId":"70189133","displayToPublicDate":"2010-06-16T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1571,"text":"Environmental Toxicology and Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"Productivity, embryo and eggshell characteristics, and contaminants in bald eagles from the Great Lakes, USA, 1986 to 2000","docAbstract":"<p><span>Chlorinated hydrocarbon concentrations in eggs of fish-eating birds from contaminated environments such as the Great Lakes of North America tend to be highly intercorrelated, making it difficult to elucidate mechanisms causing reproductive impairment, and to ascribe cause to specific chemicals. An information- theoretic approach was used on data from 197 salvaged bald eagle (</span><i>Haliaeetus leucocephalus</i><span>) eggs (159 clutches) that failed to hatch in Michigan and Ohio, USA (1986–2000). Contaminant levels declined over time while eggshell thickness increased, and by 2000 was at pre-1946 levels. The number of occupied territories and productivity increased during 1981 to 2004. For both the entire dataset and a subset of nests along the Great Lakes shoreline, polychlorinated biphenyls (ΣPCBs, fresh wet wt) were generally included in the most parsimonious models (lowest-Akaike's information criterion [AICs]) describing productivity, with significant declines in productivity observed above 26 µg/g ΣPCBs (fresh wet wt). Of 73 eggs with a visible embryo, eight (11%) were abnormal, including three with skewed bills, but they were not associated with known teratogens, including ΣPCBs. Eggs with visible embryos had greater concentrations of all measured contaminants than eggs without visible embryos; the most parsimonious models describing the presence of visible embryos incorporated dieldrin equivalents and dichlorodiphenyldichloroethylene (DDE). There were significant negative correlations between eggshell thickness and all contaminants, with ΣPCBs included in the most parsimonious models. There were, however, no relationships between productivity and eggshell thickness or Ratcliffe's index. The ΣPCBs and DDE were negatively associated with nest success of bald eagles in the Great Lakes watersheds, but the mechanism does not appear to be via shell quality effects, at least at current contaminant levels, while it is not clear what other mechanisms were involved.</span></p>","language":"English","publisher":"Society of Environmental Toxicology and Chemistry","doi":"10.1002/etc.195","usgsCitation":"Best, D.A., Elliott, K., Bowerman, W., Shieldcastle, M.C., Postupalsky, S., Kubiak, T.J., Tillitt, D.E., and Elliott, J., 2010, Productivity, embryo and eggshell characteristics, and contaminants in bald eagles from the Great Lakes, USA, 1986 to 2000: Environmental Toxicology and Chemistry, v. 29, no. 7, p. 1581-1592, https://doi.org/10.1002/etc.195.","productDescription":"12 p.","startPage":"1581","endPage":"1592","ipdsId":"IP-007522","costCenters":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true},{"id":34983,"text":"Contaminant Biology Program","active":true,"usgs":true}],"links":[{"id":475712,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1002/etc.195","text":"Publisher Index Page"},{"id":343242,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","otherGeospatial":"Great Lakes","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -90.65917968749999,\n              40.04443758460856\n            ],\n            [\n              -79.69482421875,\n              40.04443758460856\n            ],\n            [\n              -79.69482421875,\n              48.09275716032736\n            ],\n            [\n              -90.65917968749999,\n              48.09275716032736\n            ],\n            [\n              -90.65917968749999,\n              40.04443758460856\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"29","issue":"7","noUsgsAuthors":false,"publicationDate":"2010-04-05","publicationStatus":"PW","scienceBaseUri":"5957635ae4b0d1f9f051b6c3","contributors":{"authors":[{"text":"Best, David A.","contributorId":194063,"corporation":false,"usgs":false,"family":"Best","given":"David","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":703109,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Elliott, Kyle","contributorId":95347,"corporation":false,"usgs":true,"family":"Elliott","given":"Kyle","email":"","affiliations":[],"preferred":false,"id":703110,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bowerman, William","contributorId":175392,"corporation":false,"usgs":false,"family":"Bowerman","given":"William","affiliations":[],"preferred":false,"id":703111,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Shieldcastle, Mark C.","contributorId":189699,"corporation":false,"usgs":false,"family":"Shieldcastle","given":"Mark","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":703112,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Postupalsky, Sergej","contributorId":194064,"corporation":false,"usgs":false,"family":"Postupalsky","given":"Sergej","email":"","affiliations":[],"preferred":false,"id":703113,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Kubiak, Timothy J.","contributorId":74447,"corporation":false,"usgs":true,"family":"Kubiak","given":"Timothy","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":703114,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Tillitt, Donald E. 0000-0002-8278-3955 dtillitt@usgs.gov","orcid":"https://orcid.org/0000-0002-8278-3955","contributorId":1875,"corporation":false,"usgs":true,"family":"Tillitt","given":"Donald","email":"dtillitt@usgs.gov","middleInitial":"E.","affiliations":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"preferred":true,"id":703115,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Elliott, John E.","contributorId":169675,"corporation":false,"usgs":false,"family":"Elliott","given":"John E.","affiliations":[],"preferred":false,"id":703116,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":70188143,"text":"70188143 - 2010 - Shifting environmental foundations: The unprecedented and unpredictable future: Chapter 4","interactions":[],"lastModifiedDate":"2017-06-01T11:22:22","indexId":"70188143","displayToPublicDate":"2010-06-16T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Shifting environmental foundations: The unprecedented and unpredictable future: Chapter 4","docAbstract":"<p><span>As described in Chapter 2, protected area managers have been directed, through statutes and agency policy, to preserve natural conditions in parks and wilderness. Although preserving naturalness has always been a challenge for managers, there has never been much question about whether this is the right thing to do. But given what is known now about the pace and magnitude of ongoing global changes, the appropriateness of naturalness as a management goal must be reexamined. A host of anthropogenic environmental stressors are reshaping ecosystems, including those protected in parks and wilderness. Pollution is now ubiquitous worldwide, and invasive species are common in most landscapes. Habitats have become highly fragmented, and climatic changes are dramatically altering the abiotic conditions in which biota live. Given these changes, some attempts to restore and maintain naturalness may at best be ineffective; at worst, they could waste precious resources and even contribute to loss of some of the values that managers are trying to protect.</span></p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Beyond Naturalness: Rethinking Park and Wilderness Stewardship in an Era of Rapid Change","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Island Press","publisherLocation":"Washington, D.C.","usgsCitation":"Stephenson, N.L., Millar, C.I., and Cole, D., 2010, Shifting environmental foundations: The unprecedented and unpredictable future: Chapter 4, chap. <i>of</i> Beyond Naturalness: Rethinking Park and Wilderness Stewardship in an Era of Rapid Change, p. 50-66.","productDescription":"17 p.","startPage":"50","endPage":"66","ipdsId":"IP-013557","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":341990,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":341988,"type":{"id":15,"text":"Index Page"},"url":"https://www.nrs.fs.fed.us/pubs/34814"}],"publishingServiceCenter":{"id":1,"text":"Sacramento PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"593127b2e4b0e9bd0ea9ef1f","contributors":{"authors":[{"text":"Stephenson, Nathan L. 0000-0003-0208-7229 nstephenson@usgs.gov","orcid":"https://orcid.org/0000-0003-0208-7229","contributorId":2836,"corporation":false,"usgs":true,"family":"Stephenson","given":"Nathan","email":"nstephenson@usgs.gov","middleInitial":"L.","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":true,"id":696873,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Millar, Constance I.","contributorId":168554,"corporation":false,"usgs":false,"family":"Millar","given":"Constance","email":"","middleInitial":"I.","affiliations":[],"preferred":false,"id":696874,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cole, David","contributorId":172909,"corporation":false,"usgs":false,"family":"Cole","given":"David","affiliations":[],"preferred":false,"id":696875,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70188142,"text":"70188142 - 2010 - Responding to climate change: A toolbox of management strategies: Chapter 11","interactions":[],"lastModifiedDate":"2017-06-01T11:26:21","indexId":"70188142","displayToPublicDate":"2010-06-16T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Responding to climate change: A toolbox of management strategies: Chapter 11","docAbstract":"<p><span>Climate change and its effects are writ large across the landscape and in the natural and cultural heritage of parks and wilderness. They always have been and always will be. The sculpted walls of Yosemite National Park and the jagged scenery of the Sierra Nevada wilderness would not be as spectacular if periods of glaciation had not been followed by periods of deglaciation. High biodiversity in forests of the Great Smoky Mountains reflects a legacy of climate change, migrating species, and isolated climatic refugia. Fossils unearthed at Dinosaur National Monument reflect a time when the climate was very different than it is today, as do ruins left by peoples who practiced agriculture in places in the American Southwest where food production is not possible today. Over eons, climate change has molded the diversity of life and landscape in areas now protected as parks and wilderness.</span></p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Beyond Naturalness: Rethinking Park and Wilderness Stewardship in an Era of Rapid Change","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Island Press","publisherLocation":"Washington, D.C.","usgsCitation":"Cole, D., Stephenson, N.L., and Millar, C.I., 2010, Responding to climate change: A toolbox of management strategies: Chapter 11, chap. <i>of</i> Beyond Naturalness: Rethinking Park and Wilderness Stewardship in an Era of Rapid Change, p. 179-196.","productDescription":"18 p.","startPage":"179","endPage":"196","ipdsId":"IP-013585","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":341991,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":341987,"type":{"id":15,"text":"Index Page"},"url":"https://www.nrs.fs.fed.us/pubs/34815"}],"publishingServiceCenter":{"id":1,"text":"Sacramento PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"593127b2e4b0e9bd0ea9ef21","contributors":{"authors":[{"text":"Cole, David","contributorId":172909,"corporation":false,"usgs":false,"family":"Cole","given":"David","affiliations":[],"preferred":false,"id":696871,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stephenson, Nathan L. 0000-0003-0208-7229 nstephenson@usgs.gov","orcid":"https://orcid.org/0000-0003-0208-7229","contributorId":2836,"corporation":false,"usgs":true,"family":"Stephenson","given":"Nathan","email":"nstephenson@usgs.gov","middleInitial":"L.","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":true,"id":696870,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Millar, Constance I.","contributorId":168554,"corporation":false,"usgs":false,"family":"Millar","given":"Constance","email":"","middleInitial":"I.","affiliations":[],"preferred":false,"id":696872,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":98455,"text":"sir20105031 - 2010 - Estimated Withdrawals and Other Elements of Water Use in the Great Lakes Basin of the United States in 2005","interactions":[],"lastModifiedDate":"2012-03-08T17:16:30","indexId":"sir20105031","displayToPublicDate":"2010-06-16T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2010-5031","title":"Estimated Withdrawals and Other Elements of Water Use in the Great Lakes Basin of the United States in 2005","docAbstract":"Estimates of water withdrawals in the United States part of the Great Lakes Basin and 107 of its watersheds designated by the 8-digit hydrologic unit code (HUCs) indicate that about 30.3 billion gallons per day (Bgal/d) were withdrawn for practically all categories of use in 2005. Virtually all water withdrawn was freshwater. Surface-water withdrawals totaled 28.8 Bgal/d, or 95 percent of total withdrawals; about 24 Bgal/d was withdrawn from the Great Lakes or their connecting channels. Total withdrawals, and total surface-water withdrawals, decreased 7 percent from 1995 to 2005, generally following the withdrawal trends of industrial use and that of the largest use-thermoelectric power. Groundwater withdrawals increased 3 percent from 1995 to 2005 and 33 percent during 1985-2005. The substantial increase since 1985 results primarily from increases in irrigation and self-supplied domestic withdrawals. In 2005, withdrawals for public supply, domestic, and irrigation use accounted for 81 percent of groundwater withdrawals.\r\n\r\nAbout 21.9 Bgal/d, or 72 percent of total withdrawals for 2005, was used for thermoelectric power. Virtually all of this water was derived from surface water and used for once-through cooling at powerplants. As such, the reuse potential of this water in the basin is high, with the majority of the withdrawn water returned to its surface-water source.\r\n\r\nPublic-supply withdrawals were 3.81 Bgal/d (13 percent), with withdrawals declining by about 13 percent from 1995 to 2005. In 2005, about 77 percent of the population in the Great Lakes Basin obtained drinking water from public suppliers, compared to about 78 percent in 1995 and 83 percent in 1985. Surface water consistently provided about 88 percent of the total withdrawals for public supply since 1985.\r\n\r\nSelf-supplied industrial withdrawals in 2005 totaled 2.93 Bgal/d (10 percent), possibly as much as 30 percent less than in 1995. Surface water was the source for 95 percent of industrial withdrawals. Combined withdrawals for mining, irrigation, domestic, aquaculture, and livestock use (in order of decreasing rate) were 1.63 Bgal/d, or only 5 percent of total withdrawals; the withdrawals were distributed almost equally between surface-water and groundwater sources. Withdrawals for each of these uses, except livestock, increased almost continuously during 1985-2005. Withdrawals for mining increased 103 percent and for irrigation 94 percent during 1985-2005; livestock withdrawals decreased 25 percent from their peak in 1990. The number of irrigated acres increased 56 percent since 1985, totaling 750,000 acres in 2005. No use of reclaimed wastewater for industrial or irrigation applications was reported; however, sources of information regarding its use were sparse. \r\n\r\nWithin the basin, the Lake Michigan watershed accounted for 15.0 Bgal/d, or 49 percent, of total water withdrawals for 2005; an estimated 12.3 Bgal/d was withdrawn directly from Lake Michigan. The State of Michigan accounted for 38 percent of total water withdrawals, representing the largest surface-water withdrawals (primarily for thermoelectric power use) and groundwater withdrawals (primarily for public supply and self-supplied domestic use). A disproportionately large percentage of surface-water withdrawals (6 percent, 1.80 Bgal/d) were in Illinois, given this state represents less than 1 percent of the land area of the basin. Ninety percent of the Illinois population served by the water withdrawn from Lake Michigan for public supply resides outside the basin. Within land-based HUCs, the Lower Maumee (04100009) of Ohio accounted for the largest total withdrawal and total surface-water withdrawal (about 0.75 Bgal/d). The St. Joseph (04050001) of Michigan and Indiana accounted for the largest total groundwater withdrawal (0.25 Bgal/d). \r\n","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/sir20105031","collaboration":"National Water Availability and Use Pilot Program","usgsCitation":"Mills, P., and Sharpe, J.B., 2010, Estimated Withdrawals and Other Elements of Water Use in the Great Lakes Basin of the United States in 2005: U.S. Geological Survey Scientific Investigations Report 2010-5031, ix, 95 p., https://doi.org/10.3133/sir20105031.","productDescription":"ix, 95 p.","onlineOnly":"N","additionalOnlineFiles":"N","temporalStart":"2005-01-01","temporalEnd":"2005-12-31","costCenters":[{"id":344,"text":"Illinois Water Science Center","active":true,"usgs":true}],"links":[{"id":125911,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/sir_2010_5031.jpg"},{"id":13728,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2010/5031/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -95,40 ], [ -95,52 ], [ -72,52 ], [ -72,40 ], [ -95,40 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad8e4b07f02db68493f","contributors":{"authors":[{"text":"Mills, P.C. pcmills@usgs.gov","contributorId":3810,"corporation":false,"usgs":true,"family":"Mills","given":"P.C.","email":"pcmills@usgs.gov","affiliations":[{"id":344,"text":"Illinois Water Science Center","active":true,"usgs":true}],"preferred":true,"id":305357,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sharpe, Jennifer B. 0000-0002-5192-7848 jbsharpe@usgs.gov","orcid":"https://orcid.org/0000-0002-5192-7848","contributorId":2825,"corporation":false,"usgs":true,"family":"Sharpe","given":"Jennifer","email":"jbsharpe@usgs.gov","middleInitial":"B.","affiliations":[{"id":36532,"text":"Central Midwest Water Science Center","active":true,"usgs":true}],"preferred":true,"id":305356,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":98454,"text":"sir20105078 - 2010 - Surface-Water Quality Conditions and Long-Term Trends at Selected Sites within the Ambient Water-Quality Monitoring Network in Missouri, Water Years 1993-2008 ","interactions":[],"lastModifiedDate":"2012-03-08T17:16:29","indexId":"sir20105078","displayToPublicDate":"2010-06-16T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2010-5078","title":"Surface-Water Quality Conditions and Long-Term Trends at Selected Sites within the Ambient Water-Quality Monitoring Network in Missouri, Water Years 1993-2008 ","docAbstract":"The U.S. Geological Survey, in cooperation with the Missouri Department of Natural Resources, collects data pertaining to the surface-water resources of Missouri. These data are collected as part of the Missouri Ambient Water-Quality Monitoring Network and constitute a valuable source of reliable, impartial, and timely information for developing an improved understanding of water resources in the State.\r\n\r\nSix sites from the Ambient Water-Quality Monitoring Network, with data available from the 1993 through 2008 water years, were chosen to compare water-quality conditions and long-term trends of dissolved oxygen, selected physical properties, total suspended solids, dissolved nitrate plus nitrite as nitrogen, total phosphorous, fecal indicator bacteria, and selected trace elements. The six sites used in the study were classified in groups corresponding to the physiography, main land use, and drainage basin size, and represent most stream types in Missouri.\r\n\r\nLong-term trends in this study were analyzed using flow-adjusted and non-flow adjusted models. Highly censored datasets (greater than 5 percent but less than 50 percent censored values) were not flow-adjusted. Trends that were detected can possibly be related to changes in agriculture or urban development within the drainage basins. Trends in nutrients were the most prevalent. Upward flow-adjusted trends in dissolved nitrate plus nitrite (as nitrogen) concentrations were identified at the Elk River site, and in total phosphorus concentrations at the South Fabius and Grand River sites. A downward flow-adjusted trend was identified in total phosphorus concentrations from Wilson Creek, the only urban site in the study. The downward trend in phosphorus possibly was related to a phosphorus reduction system that began operation in 2001 at a wastewater treatment plant upstream from the sampling site. Total suspended solids concentrations indicated an upward non-flow adjusted trend at the two northern sites (South Fabius and Grand Rivers). The increase in total suspended solids concentrations could be because of soil erosion from land cultivated for row crops. Most trace element data examined in the study were highly censored and could not be used for flow-adjusted trend analyses.\r\n\r\nWater-quality conditions were assessed to explore relations between data from sites and to the State water-quality standards where applicable for selected constituents. Streamflow varied at each site because of drainage area, land use, and groundwater inputs. Dissolved oxygen and water temperature were similar at all sites except the urban site located on Wilson Creek. Specific conductance was similar between the most northern (South Fabius and Grand River sites) and the most southern sites (Current and Elk River sites). Total suspended solids concentrations were near the method reporting level at all sites, except the northern sites. Streams in northern Missouri are more turbid than streams in southern Missouri and are affected by large volumes of sediment deposition because of soil erosion from land cultivated for row crops.\r\n\r\nGeometric means of Escherichia coli were calculated from the recreational seasons within the study period. Only the Grand River site exceeded the whole-body-contact standard for frequently used waters. The South Fabius and Grand River sites and the Wilson Creek site had statistically larger densities of both fecal indicator bacteria types than the remaining sites.\r\n","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/sir20105078","collaboration":"Prepared in cooperation with Missouri Department of Natural Resources","usgsCitation":"Barr, M.N., and Davis, J., 2010, Surface-Water Quality Conditions and Long-Term Trends at Selected Sites within the Ambient Water-Quality Monitoring Network in Missouri, Water Years 1993-2008 : U.S. Geological Survey Scientific Investigations Report 2010-5078, v, 42 p. , https://doi.org/10.3133/sir20105078.","productDescription":"v, 42 p. ","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":396,"text":"Missouri Water Science Center","active":true,"usgs":true}],"links":[{"id":125909,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/sir_2010_5078.jpg"},{"id":13727,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2010/5078/","linkFileType":{"id":5,"text":"html"}}],"projection":"Universal Transverse Mercator","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -96,36 ], [ -96,42 ], [ -89,42 ], [ -89,36 ], [ -96,36 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae6e4b07f02db68b4d5","contributors":{"authors":[{"text":"Barr, Miya N. 0000-0002-9961-9190 mnbarr@usgs.gov","orcid":"https://orcid.org/0000-0002-9961-9190","contributorId":3686,"corporation":false,"usgs":true,"family":"Barr","given":"Miya","email":"mnbarr@usgs.gov","middleInitial":"N.","affiliations":[{"id":36532,"text":"Central Midwest Water Science Center","active":true,"usgs":true},{"id":396,"text":"Missouri Water Science Center","active":true,"usgs":true}],"preferred":true,"id":305355,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Davis, Jerri V. jdavis@usgs.gov","contributorId":2667,"corporation":false,"usgs":true,"family":"Davis","given":"Jerri V.","email":"jdavis@usgs.gov","affiliations":[{"id":396,"text":"Missouri Water Science Center","active":true,"usgs":true}],"preferred":false,"id":305354,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70189667,"text":"sir20105025D - 2010 - Biological pathways of exposure and ecotoxicity values for uranium and associated radionuclides: Chapter D in Hydrological, geological, and biological site characterization of breccia pipe uranium deposits in Northern Arizona","interactions":[{"subject":{"id":70189667,"text":"sir20105025D - 2010 - Biological pathways of exposure and ecotoxicity values for uranium and associated radionuclides: Chapter D in Hydrological, geological, and biological site characterization of breccia pipe uranium deposits in Northern Arizona","indexId":"sir20105025D","publicationYear":"2010","noYear":false,"chapter":"D","displayTitle":"Biological pathways of exposure and ecotoxicity values for uranium and associated radionuclides: Chapter D in <i>Hydrological, geological, and biological site characterization of breccia pipe uranium deposits in Northern Arizona</i>","title":"Biological pathways of exposure and ecotoxicity values for uranium and associated radionuclides: Chapter D in Hydrological, geological, and biological site characterization of breccia pipe uranium deposits in Northern Arizona"},"predicate":"IS_PART_OF","object":{"id":98205,"text":"sir20105025 - 2010 - Hydrological, geological, and biological site characterization of breccia pipe uranium deposits in Northern Arizona","indexId":"sir20105025","publicationYear":"2010","noYear":false,"title":"Hydrological, geological, and biological site characterization of breccia pipe uranium deposits in Northern Arizona"},"id":1}],"isPartOf":{"id":98205,"text":"sir20105025 - 2010 - Hydrological, geological, and biological site characterization of breccia pipe uranium deposits in Northern Arizona","indexId":"sir20105025","publicationYear":"2010","noYear":false,"title":"Hydrological, geological, and biological site characterization of breccia pipe uranium deposits in Northern Arizona"},"lastModifiedDate":"2020-02-21T13:26:40","indexId":"sir20105025D","displayToPublicDate":"2010-06-16T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2010-5025","chapter":"D","displayTitle":"Biological pathways of exposure and ecotoxicity values for uranium and associated radionuclides: Chapter D in <i>Hydrological, geological, and biological site characterization of breccia pipe uranium deposits in Northern Arizona</i>","title":"Biological pathways of exposure and ecotoxicity values for uranium and associated radionuclides: Chapter D in Hydrological, geological, and biological site characterization of breccia pipe uranium deposits in Northern Arizona","docAbstract":"<p>This chapter compiles available chemical and radiation toxicity information for plants and animals from the scientific literature on naturally occurring uranium and associated radionuclides. Specifically, chemical and radiation hazards associated with radionuclides in the uranium decay series including uranium, thallium, thorium, bismuth, radium, radon, protactinium, polonium, actinium, and francium were the focus of the literature compilation. In addition, exposure pathways and a food web specific to the segregation areas were developed. Major biological exposure pathways considered were ingestion, inhalation, absorption, and bioaccumulation, and biota categories included microbes, invertebrates, plants, fishes, amphibians, reptiles, birds, and mammals. These data were developed for incorporation into a risk assessment to be conducted as part of an environmental impact statement for the Bureau of Land Management, which would identify representative plants and animals and their relative sensitivities to exposure of uranium and associated radionuclides. This chapter provides pertinent information to aid in the development of such an ecological risk assessment but does not estimate or derive guidance thresholds for radionuclides associated with uranium. </p><p>Previous studies have not attempted to quantify the risks to biota caused directly by the chemical or radiation releases at uranium mining sites, although some information is available for uranium mill tailings and uranium mine closure activities. Research into the biological impacts of uranium exposure is strongly biased towards human health and exposure related to enriched or depleted uranium associated with the nuclear energy industry rather than naturally occurring uranium associated with uranium mining. Nevertheless, studies have reported that uranium and other radionuclides can affect the survival, growth, and reproduction of plants and animals. </p><p>Exposure to chemical and radiation hazards is influenced by a plant’s or an animal’s life history and surrounding environment. Various species of plants, invertebrates, fishes, amphibians, reptiles, birds, and mammals found in the segregation areas that are considered species of concern by State and Federal agencies were included in the development of the site-specific food web. The utilization of subterranean habitats (burrows in uranium-rich areas, burrows in waste rock piles or reclaimed mining areas, mine tunnels) in the seasonally variable but consistently hot, arid environment is of particular concern in the segregation areas. Certain species of reptiles, amphibians, birds, and mammals in the segregation areas spend significant amounts of time in burrows where they can inhale or ingest uranium and other radionuclides through digging, eating, preening, and hibernating. Herbivores may also be exposed though the ingestion of radionuclides that have been aerially deposited on vegetation. Measured tissues concentrations of uranium and other radionuclides are not available for any species of concern in the segregation areas. The sensitivity of these animals to uranium exposure is unknown based on the existing scientific literature, and species-specific uranium presumptive effects levels were only available for two endangered fish species known to inhabit the segregation areas. </p><p>Overall, the chemical toxicity data available for biological receptors of concern were limited, although chemical and radiation toxicity guidance values are available from several sources. However, caution should be used when directly applying these values to northern Arizona given the unique habitat and life history strategies of biological receptors in the segregation areas and the fact that some guidance values are based on models rather than empirical (laboratory or field) data. No chemical toxicity information based on empirical data is available for reptiles, birds, or wild mammals; therefore, the risks associated with uranium and other radionuclides are unknown for these biota.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Hydrological, geological, and biological site characterization of breccia pipe uranium deposits in Northern Arizona (Scientific Investigations Report 2010-5025)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20105025D","usgsCitation":"Hinck, J.E., Linder, G.L., Finger, S.E., Little, E.E., Tillitt, D.E., and Kuhne, W., 2010, Biological pathways of exposure and ecotoxicity values for uranium and associated radionuclides: Chapter D in Hydrological, geological, and biological site characterization of breccia pipe uranium deposits in Northern Arizona: U.S. Geological Survey Scientific Investigations Report 2010-5025, 69, https://doi.org/10.3133/sir20105025D.","productDescription":"69","startPage":"283","endPage":"351","costCenters":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"links":[{"id":344076,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":372514,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/sir/2010/5025/pdf/sir2010-5025_biology.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Arizona","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -114,\n              37.1\n            ],\n            [\n              -111.5,\n              37.1\n            ],\n            [\n              -111.5,\n              35.5\n            ],\n            [\n              -114,\n              35.5\n            ],\n            [\n              -114,\n              37.1\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"59706fdfe4b0d1f9f065ab0c","contributors":{"authors":[{"text":"Hinck, Jo Ellen 0000-0002-4912-5766 jhinck@usgs.gov","orcid":"https://orcid.org/0000-0002-4912-5766","contributorId":2743,"corporation":false,"usgs":true,"family":"Hinck","given":"Jo","email":"jhinck@usgs.gov","middleInitial":"Ellen","affiliations":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"preferred":true,"id":705694,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Linder, Greg L. linder2@usgs.gov","contributorId":1766,"corporation":false,"usgs":true,"family":"Linder","given":"Greg","email":"linder2@usgs.gov","middleInitial":"L.","affiliations":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"preferred":false,"id":705695,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Finger, Susan E. sfinger@usgs.gov","contributorId":1317,"corporation":false,"usgs":true,"family":"Finger","given":"Susan","email":"sfinger@usgs.gov","middleInitial":"E.","affiliations":[],"preferred":true,"id":705696,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Little, Edward E. 0000-0003-0034-3639 elittle@usgs.gov","orcid":"https://orcid.org/0000-0003-0034-3639","contributorId":1746,"corporation":false,"usgs":true,"family":"Little","given":"Edward","email":"elittle@usgs.gov","middleInitial":"E.","affiliations":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"preferred":true,"id":705697,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Tillitt, Donald E. 0000-0002-8278-3955 dtillitt@usgs.gov","orcid":"https://orcid.org/0000-0002-8278-3955","contributorId":1875,"corporation":false,"usgs":true,"family":"Tillitt","given":"Donald","email":"dtillitt@usgs.gov","middleInitial":"E.","affiliations":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"preferred":true,"id":705698,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Kuhne, Wendy","contributorId":194911,"corporation":false,"usgs":false,"family":"Kuhne","given":"Wendy","affiliations":[],"preferred":false,"id":705699,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70043883,"text":"70043883 - 2010 - Sequence analysis of the internal transcribed spacer (ITS) region reveals a novel clade of Ichthyophonus sp. from rainbow trout","interactions":[],"lastModifiedDate":"2016-12-27T11:22:56","indexId":"70043883","displayToPublicDate":"2010-06-16T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1396,"text":"Diseases of Aquatic Organisms","active":true,"publicationSubtype":{"id":10}},"title":"Sequence analysis of the internal transcribed spacer (ITS) region reveals a novel clade of Ichthyophonus sp. from rainbow trout","docAbstract":"The mesomycetozoean parasite Ichthyophonus hoferi is most commonly associated with marine fish hosts but also occurs in some components of the freshwater rainbow trout Oncorhynchus mykiss aquaculture industry in Idaho, USA. It is not certain how the parasite was introduced into rainbow trout culture, but it might have been associated with the historical practice of feeding raw, ground common carp Cyprinus carpio that were caught by commercial fisherman. Here, we report a major genetic division between west coast freshwater and marine isolates of Ichthyophonus hoferi. Sequence differences were not detected in 2 regions of the highly conserved small subunit (18S) rDNA gene; however, nucleotide variation was seen in internal transcribed spacer loci (ITS1 and ITS2), both within and among the isolates. Intra-isolate variation ranged from 2.4 to 7.6 nucleotides over a region consisting of ~740 bp. Majority consensus sequences from marine/anadromous hosts differed in only 0 to 3 nucleotides (99.6 to 100% nucleotide identity), while those derived from freshwater rainbow trout had no nucleotide substitutions relative to each other. However, the consensus sequences between isolates from freshwater rainbow trout and those from marine/anadromous hosts differed in 13 to 16 nucleotides (97.8 to 98.2% nucleotide identity).","language":"English","publisher":"Inter-Research Science Center","doi":"10.3354/dao02184","usgsCitation":"Rasmussen, C., Purcell, M.K., Gregg, J., LaPatra, S., Winton, J., and Hershberger, P., 2010, Sequence analysis of the internal transcribed spacer (ITS) region reveals a novel clade of Ichthyophonus sp. from rainbow trout: Diseases of Aquatic Organisms, v. 89, no. 2, p. 179-183, https://doi.org/10.3354/dao02184.","productDescription":"5 p.","startPage":"179","endPage":"183","numberOfPages":"5","ipdsId":"IP-015378","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":475713,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.3354/dao02184","text":"Publisher Index Page"},{"id":271652,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"89","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5180e7ebe4b0df838b924d9f","contributors":{"authors":[{"text":"Rasmussen, C.","contributorId":66392,"corporation":false,"usgs":true,"family":"Rasmussen","given":"C.","email":"","affiliations":[],"preferred":false,"id":474376,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Purcell, M. K.","contributorId":78464,"corporation":false,"usgs":true,"family":"Purcell","given":"M.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":474377,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gregg, J.L.","contributorId":78521,"corporation":false,"usgs":true,"family":"Gregg","given":"J.L.","email":"","affiliations":[],"preferred":false,"id":474378,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"LaPatra, S. E.","contributorId":55371,"corporation":false,"usgs":false,"family":"LaPatra","given":"S. E.","affiliations":[],"preferred":false,"id":474374,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Winton, J. R. 0000-0002-3505-5509","orcid":"https://orcid.org/0000-0002-3505-5509","contributorId":82441,"corporation":false,"usgs":true,"family":"Winton","given":"J. R.","affiliations":[],"preferred":false,"id":474379,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Hershberger, P.K. 0000-0002-2261-7760","orcid":"https://orcid.org/0000-0002-2261-7760","contributorId":58818,"corporation":false,"usgs":true,"family":"Hershberger","given":"P.K.","affiliations":[],"preferred":false,"id":474375,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70189940,"text":"70189940 - 2010 - Microbial oxidation of arsenite in a subarctic environment: diversity of arsenite oxidase genes and identification of a psychrotolerant arsenite oxidiser","interactions":[],"lastModifiedDate":"2018-10-10T16:41:36","indexId":"70189940","displayToPublicDate":"2010-06-16T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5472,"text":"BMC Microbiology","active":true,"publicationSubtype":{"id":10}},"title":"Microbial oxidation of arsenite in a subarctic environment: diversity of arsenite oxidase genes and identification of a psychrotolerant arsenite oxidiser","docAbstract":"<p>Arsenic is toxic to most living cells. The two soluble inorganic forms of arsenic are arsenite (+3) and arsenate (+5), with arsenite the more toxic. Prokaryotic metabolism of arsenic has been reported in both thermal and moderate environments and has been shown to be involved in the redox cycling of arsenic. No arsenic metabolism (either dissimilatory arsenate reduction or arsenite oxidation) has ever been reported in cold environments (i.e. &lt; 10°C).</p><p><strong>Results</strong>: Our study site is located 512 kilometres south of the Arctic Circle in the Northwest Territories, Canada in an inactive gold mine which contains mine waste water in excess of 50 mM arsenic. Several thousand tonnes of arsenic trioxide dust are stored in underground chambers and microbial biofilms grow on the chamber walls below seepage points rich in arsenite-containing solutions. We compared the arsenite oxidisers in two subsamples (which differed in arsenite concentration) collected from one biofilm. 'Species' (sequence) richness did not differ between subsamples, but the relative importance of the three identifiable clades did. An arsenite-oxidising bacterium (designated GM1) was isolated, and was shown to oxidise arsenite in the early exponential growth phase and to grow at a broad range of temperatures (4-25°C). Its arsenite oxidase was constitutively expressed and functioned over a broad temperature range.</p><p><strong>Conclusions</strong>: The diversity of arsenite oxidisers does not significantly differ from two subsamples of a microbial biofilm that vary in arsenite concentrations. GM1 is the first psychrotolerant arsenite oxidiser to be isolated with the ability to grow below 10°C. This ability to grow at low temperatures could be harnessed for arsenic bioremediation in moderate to cold climates.</p>","language":"English","publisher":"BioMed Central","doi":"10.1186/1471-2180-10-205","usgsCitation":"Osborne, T.H., Jamieson, H.E., Hudson-Edwards, K.A., Nordstrom, D.K., Walker, S.R., Ward, S.A., and Santini, J.M., 2010, Microbial oxidation of arsenite in a subarctic environment: diversity of arsenite oxidase genes and identification of a psychrotolerant arsenite oxidiser: BMC Microbiology, v. 10, no. 205, 8 p., https://doi.org/10.1186/1471-2180-10-205.","productDescription":"8 p.","ipdsId":"IP-017174","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true},{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"links":[{"id":475714,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1186/1471-2180-10-205","text":"Publisher Index Page"},{"id":344480,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"10","issue":"205","publishingServiceCenter":{"id":2,"text":"Denver PSC"},"noUsgsAuthors":false,"publicationDate":"2010-07-30","publicationStatus":"PW","scienceBaseUri":"59819317e4b0e2f5d463b7b3","contributors":{"authors":[{"text":"Osborne, Thomas H.","contributorId":195346,"corporation":false,"usgs":false,"family":"Osborne","given":"Thomas","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":706834,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jamieson, Heather E.","contributorId":150176,"corporation":false,"usgs":false,"family":"Jamieson","given":"Heather","email":"","middleInitial":"E.","affiliations":[{"id":7029,"text":"Queen's University, Kingston, Ontario, Canada","active":true,"usgs":false}],"preferred":false,"id":706830,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hudson-Edwards, Karen A.","contributorId":195345,"corporation":false,"usgs":false,"family":"Hudson-Edwards","given":"Karen","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":706832,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Nordstrom, D. Kirk 0000-0003-3283-5136 dkn@usgs.gov","orcid":"https://orcid.org/0000-0003-3283-5136","contributorId":749,"corporation":false,"usgs":true,"family":"Nordstrom","given":"D.","email":"dkn@usgs.gov","middleInitial":"Kirk","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":false,"id":706828,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Walker, Stephen R.","contributorId":195350,"corporation":false,"usgs":false,"family":"Walker","given":"Stephen","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":706833,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Ward, Seamus A.","contributorId":168896,"corporation":false,"usgs":false,"family":"Ward","given":"Seamus","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":706829,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Santini, Joanne M.","contributorId":168895,"corporation":false,"usgs":false,"family":"Santini","given":"Joanne","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":706831,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70118772,"text":"70118772 - 2010 - Population assessment of the Mariana fruit bat (Pteropus mariannus mariannus) on Anatahan, Sraigan, Guguan, Alamagan, Pagan, Agrihan, Asuncion, and Maug; 15 June - 10 July 2010","interactions":[],"lastModifiedDate":"2014-07-30T10:21:45","indexId":"70118772","displayToPublicDate":"2010-06-15T10:20:46","publicationYear":"2010","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":9,"text":"Other Report"},"seriesTitle":{"id":396,"text":"Annual Report","active":false,"publicationSubtype":{"id":9}},"title":"Population assessment of the Mariana fruit bat (Pteropus mariannus mariannus) on Anatahan, Sraigan, Guguan, Alamagan, Pagan, Agrihan, Asuncion, and Maug; 15 June - 10 July 2010","docAbstract":"No abstract available.","language":"English","publisher":"U. S. Geological Survey","publisherLocation":"Reston, VA","usgsCitation":"Valdez, E., 2010, Population assessment of the Mariana fruit bat (Pteropus mariannus mariannus) on Anatahan, Sraigan, Guguan, Alamagan, Pagan, Agrihan, Asuncion, and Maug; 15 June - 10 July 2010: Annual Report, 48 p.","productDescription":"48 p.","numberOfPages":"48","costCenters":[],"links":[{"id":291384,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57fe8262e4b0824b2d1485a9","contributors":{"authors":[{"text":"Valdez, Ernest","contributorId":36067,"corporation":false,"usgs":true,"family":"Valdez","given":"Ernest","affiliations":[],"preferred":false,"id":497198,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":98450,"text":"sir20105116 - 2010 - Chemical Constituents in Groundwater from Multiple Zones in the Eastern Snake River Plain Aquifer at the Idaho National Laboratory, Idaho, 2005-08","interactions":[],"lastModifiedDate":"2012-03-08T17:16:30","indexId":"sir20105116","displayToPublicDate":"2010-06-15T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2010-5116","title":"Chemical Constituents in Groundwater from Multiple Zones in the Eastern Snake River Plain Aquifer at the Idaho National Laboratory, Idaho, 2005-08","docAbstract":"From 2005 to 2008, the U.S. Geological Survey's Idaho National Laboratory (INL) Project office, in cooperation with the U.S. Department of Energy, collected water-quality samples from multiple water-bearing zones in the eastern Snake River Plain aquifer. Water samples were collected from six monitoring wells completed in about 350-700 feet of the upper part of the aquifer, and the samples were analyzed for major ions, selected trace elements, nutrients, selected radiochemical constituents, and selected stable isotopes. Each well was equipped with a multilevel monitoring system containing four to seven sampling ports that were each isolated by permanent packer systems. The sampling ports were installed in aquifer zones that were highly transmissive and that represented the water chemistry of the top four to five model layers of a steady-state and transient groundwater-flow model. The model's water chemistry and particle-tracking simulations are being used to better define movement of wastewater constituents in the aquifer.\r\n\r\nThe results of the water chemistry analyses indicated that, in each of four separate wells, one zone of water differed markedly from the other zones in the well. In four wells, one zone to as many as five zones contained radiochemical constituents that originated from wastewater disposal at selected laboratory facilities. The multilevel sampling systems are defining the vertical distribution of wastewater constituents in the eastern Snake River Plain aquifer and the concentrations of wastewater constituents in deeper zones in wells Middle 2051, USGS 132, and USGS 103 support the concept of groundwater flow deepening in the southwestern part of the INL.\r\n","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/sir20105116","collaboration":"Prepared in cooperation with the U.S. Department of Energy, DOE/ID-22211","usgsCitation":"Bartholomay, R.C., and Twining, B.V., 2010, Chemical Constituents in Groundwater from Multiple Zones in the Eastern Snake River Plain Aquifer at the Idaho National Laboratory, Idaho, 2005-08: U.S. Geological Survey Scientific Investigations Report 2010-5116, viii, 81 p., https://doi.org/10.3133/sir20105116.","productDescription":"viii, 81 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":125361,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/sir_2010_5116.jpg"},{"id":13717,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2010/5116/","linkFileType":{"id":5,"text":"html"}}],"scale":"24000","projection":"Universal Transverse Mercator","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114,43 ], [ -114,44.25 ], [ -112,44.25 ], [ -112,43 ], [ -114,43 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4bc7","contributors":{"authors":[{"text":"Bartholomay, Roy C. 0000-0002-4809-9287 rcbarth@usgs.gov","orcid":"https://orcid.org/0000-0002-4809-9287","contributorId":1131,"corporation":false,"usgs":true,"family":"Bartholomay","given":"Roy","email":"rcbarth@usgs.gov","middleInitial":"C.","affiliations":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"preferred":true,"id":305344,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Twining, Brian V. 0000-0003-1321-4721 btwining@usgs.gov","orcid":"https://orcid.org/0000-0003-1321-4721","contributorId":2387,"corporation":false,"usgs":true,"family":"Twining","given":"Brian","email":"btwining@usgs.gov","middleInitial":"V.","affiliations":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"preferred":true,"id":305345,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70189024,"text":"70189024 - 2010 - Mineralogy and stratigraphy of phyllosilicate-bearing and dark mantling units in the greater Mawrth Vallis/west Arabia Terra area: Constraints on geological origin","interactions":[],"lastModifiedDate":"2017-06-29T14:16:25","indexId":"70189024","displayToPublicDate":"2010-06-15T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2312,"text":"Journal of Geophysical Research","active":true,"publicationSubtype":{"id":10}},"title":"Mineralogy and stratigraphy of phyllosilicate-bearing and dark mantling units in the greater Mawrth Vallis/west Arabia Terra area: Constraints on geological origin","docAbstract":"<p><span>Analyses of MRO/CRISM images of the greater Mawrth Vallis region of Mars affirm the presence of two primary phyllosilicate assemblages throughout a region ∼1000 × 1000 km. These two units consist of an Fe/Mg-phyllosilicate assemblage overlain by an Al-phyllosilicate and hydrated silica assemblage. The lower unit contains Fe/Mg-smectites, sometimes combined with one or more of these other Fe/Mg-phyllosilicates: serpentine, chlorite, biotite, and/or vermiculite. It is more than 100 m thick and finely layered at meter scales. The upper unit includes Al-smectite, kaolin group minerals, and hydrated silica. It is tens of meters thick and finely layered as well. A common phyllosilicate stratigraphy and morphology is observed throughout the greater region wherever erosional windows are present. This suggests that the geologic processes forming these units must have occurred on at least a regional scale. Sinuous ridges (interpreted to be inverted channels) and narrow channels cut into the upper clay-bearing unit suggesting that aqueous processes were prevalent after, and possibly during, the deposition of the layered units. We propose that layered units may have been deposited at Mawrth Vallis and then subsequently altered to form the hydrated units. The Fe/Mg-phyllosilicate assemblage is consistent with hydrothermal alteration or pedogenesis of mafic to ultramafic rocks. The Al-phyllosilicate/hydrated silica unit may have formed through alteration of felsic material or via leaching of basaltic material through pedogenic alteration or a mildly acidic environment. These phyllosilicate-bearing units are overlain by a darker, relatively unaltered, and indurated material that has probably experienced a complex geological history.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/2009JE003351","usgsCitation":"Noe Dobrea, E., Bishop, J., McKeown, N., Fu, R., Rossi, C., Michalski, J., Heinlein, C., Hanus, V., Poulet, F., Mustard, R., Murchie, S., McEwen, A.S., Swayze, G., Bibring, J., Malaret, E., and Hash, C., 2010, Mineralogy and stratigraphy of phyllosilicate-bearing and dark mantling units in the greater Mawrth Vallis/west Arabia Terra area: Constraints on geological origin: Journal of Geophysical Research, v. 115, no. E7, Article E00D19: 27 p., https://doi.org/10.1029/2009JE003351.","productDescription":"Article E00D19: 27 p.","ipdsId":"IP-019901","costCenters":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"links":[{"id":343143,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Mars","volume":"115","issue":"E7","publishingServiceCenter":{"id":2,"text":"Denver PSC"},"noUsgsAuthors":false,"publicationDate":"2010-07-31","publicationStatus":"PW","scienceBaseUri":"595611c8e4b0d1f9f05067f4","contributors":{"authors":[{"text":"Noe Dobrea, E.Z.","contributorId":97316,"corporation":false,"usgs":true,"family":"Noe Dobrea","given":"E.Z.","email":"","affiliations":[],"preferred":false,"id":702463,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bishop, J.L.","contributorId":83244,"corporation":false,"usgs":true,"family":"Bishop","given":"J.L.","affiliations":[],"preferred":false,"id":702464,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McKeown, N.K.","contributorId":10529,"corporation":false,"usgs":true,"family":"McKeown","given":"N.K.","email":"","affiliations":[],"preferred":false,"id":702465,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Fu, R.","contributorId":193928,"corporation":false,"usgs":false,"family":"Fu","given":"R.","email":"","affiliations":[],"preferred":false,"id":702630,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Rossi, C.M.","contributorId":193929,"corporation":false,"usgs":false,"family":"Rossi","given":"C.M.","email":"","affiliations":[],"preferred":false,"id":702631,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Michalski, J.R.","contributorId":46202,"corporation":false,"usgs":true,"family":"Michalski","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":702632,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Heinlein, C.","contributorId":193930,"corporation":false,"usgs":false,"family":"Heinlein","given":"C.","email":"","affiliations":[],"preferred":false,"id":702633,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Hanus, V.","contributorId":193931,"corporation":false,"usgs":false,"family":"Hanus","given":"V.","email":"","affiliations":[],"preferred":false,"id":702634,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Poulet, F.","contributorId":61551,"corporation":false,"usgs":true,"family":"Poulet","given":"F.","email":"","affiliations":[],"preferred":false,"id":702725,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Mustard, R.J.F.","contributorId":193932,"corporation":false,"usgs":false,"family":"Mustard","given":"R.J.F.","email":"","affiliations":[],"preferred":false,"id":702726,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Murchie, S.","contributorId":16584,"corporation":false,"usgs":true,"family":"Murchie","given":"S.","email":"","affiliations":[],"preferred":false,"id":702727,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"McEwen, A. S.","contributorId":11317,"corporation":false,"usgs":true,"family":"McEwen","given":"A.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":702728,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Swayze, G. 0000-0002-1814-7823","orcid":"https://orcid.org/0000-0002-1814-7823","contributorId":55131,"corporation":false,"usgs":true,"family":"Swayze","given":"G.","affiliations":[],"preferred":false,"id":702729,"contributorType":{"id":1,"text":"Authors"},"rank":13},{"text":"Bibring, J.-P.","contributorId":86083,"corporation":false,"usgs":true,"family":"Bibring","given":"J.-P.","email":"","affiliations":[],"preferred":false,"id":702733,"contributorType":{"id":1,"text":"Authors"},"rank":14},{"text":"Malaret, E.","contributorId":84487,"corporation":false,"usgs":true,"family":"Malaret","given":"E.","email":"","affiliations":[],"preferred":false,"id":702734,"contributorType":{"id":1,"text":"Authors"},"rank":15},{"text":"Hash, C.","contributorId":59927,"corporation":false,"usgs":true,"family":"Hash","given":"C.","email":"","affiliations":[],"preferred":false,"id":702735,"contributorType":{"id":1,"text":"Authors"},"rank":16}]}}
,{"id":70154978,"text":"70154978 - 2010 - Climate change, cranes, and temperate floodplain ecosystems","interactions":[],"lastModifiedDate":"2017-05-30T11:29:31","indexId":"70154978","displayToPublicDate":"2010-06-15T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Climate change, cranes, and temperate floodplain ecosystems","docAbstract":"<p>Floodplain ecosystems provide important habitat to cranes globally. Lateral, longitudinal, vertical, and temporal hydrologic connectivity in rivers is essential to maintaining the functions and values of these systems. Agricultural development, flood control, water diversions, dams, and other anthropogenic activities have greatly affected hydrologic connectivity of river systems worldwide and altered the functional capacity of these systems. Although the specific effects of climate change in any given area are unknown, increased intensity and frequency of flooding and droughts and increased air and water temperatures are among many potential effects that can act synergistically with existing human modifications in these systems to create even greater challenges in maintaining ecosystem productivity. In this paper, I review basic hydrologic and geomorphic processes of river systems and use three North American rivers (Guadalupe, Platte, and Rio Grande) that are important to cranes as case studies to illustrate the challenges facing managers tasked with balancing the needs of cranes and people in the face of an uncertain climatic future. Each river system has unique natural and anthropogenic characteristics that will affect conservation strategies. Mitigating the effects of climate change on river systems necessitates an understanding of river/floodplain/landscape linkages, which include people and their laws as well as existing floodplain ecosystem conditions.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Cranes, agriculture, and climate change","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceDate":"May 28 - June 2, 2010","conferenceLocation":"Baraboo, WI","language":"English","publisher":"International Crane Foundation","usgsCitation":"King, S.L., 2010, Climate change, cranes, and temperate floodplain ecosystems, <i>in</i> Cranes, agriculture, and climate change, Baraboo, WI, May 28 - June 2, 2010, p. 28-34.","productDescription":"7 p.","startPage":"28","endPage":"34","ipdsId":"IP-022579","costCenters":[{"id":198,"text":"Coop Res Unit Atlanta","active":true,"usgs":true}],"links":[{"id":341834,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"publishingServiceCenter":{"id":8,"text":"Raleigh PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"592e84cae4b092b266f10ddf","contributors":{"authors":[{"text":"King, Sammy L. 0000-0002-5364-6361 sking@usgs.gov","orcid":"https://orcid.org/0000-0002-5364-6361","contributorId":557,"corporation":false,"usgs":true,"family":"King","given":"Sammy","email":"sking@usgs.gov","middleInitial":"L.","affiliations":[{"id":198,"text":"Coop Res Unit Atlanta","active":true,"usgs":true}],"preferred":true,"id":564457,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":98453,"text":"ofr20101110 - 2010 - Gas, oil, and water production from Grand Valley, Parachute, Rulison, and Mamm Creek fields in the Piceance Basin, Colorado","interactions":[],"lastModifiedDate":"2022-07-22T20:40:55.334098","indexId":"ofr20101110","displayToPublicDate":"2010-06-15T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2010-1110","title":"Gas, oil, and water production from Grand Valley, Parachute, Rulison, and Mamm Creek fields in the Piceance Basin, Colorado","docAbstract":"<p>Gas, oil, and water production data for tight gas reservoirs were compiled from selected wells in western Colorado. These reservoir rocks—the relatively shallow Paleogene Wasatch G sandstone interval in the Parachute and Rulison fields and fluvial sandstones in the deeper Upper Cretaceous Mesaverde Group in the Grand Valley, Parachute, Rulison, and Mamm Creek fields—are characterized by low permeability, low porosity, and the presence of clay minerals in pore space. Production from each well is represented by two samples spaced five years apart, the first sample typically taken two years after production commenced, which was generally in the 1990s. For each producing interval, summary diagrams of oil-versus-gas and water-versus-gas production show fluid production rates, the change in rates during five years, the water-gas and oil-gas ratios, and the fluid type. These diagrams permit well-to-well and field-to-field comparisons. Fields producing water at low rates (water dissolved in gas in the reservoir) can be distinguished from fields producing water at moderate or high rates, and the water-gas ratios are quantified.</p><p>Dry gas is produced from the Wasatch G interval and wet gas is produced from the Mesaverde Group. Production from the Wasatch G interval is also almost completely free of water, but water production commences with gas production in wells producing from the Mesaverde Group—all of these wells have water-gas ratios exceeding the amount that could exist dissolved in gas at reservoir temperature and pressure. The lack of produced water from the Wasatch G interval is attributed to expansion of the gas accumulation with uplift and erosion. The reported underpressure of the Wasatch G interval is here attributed to hydraulic connection to the atmosphere by outcrops in the Colorado River valley at an elevation lower than that of the gas fields.</p><p>The amount of reduction of gas production over the five-year time span between the first and second samples is roughly one-half, with median values of second-sample to first-sample gas-production ratios ranging from 0.40 for Rulison-Mesaverde to 0.63 for Rulison-Wasatch G. Commencing with the first sample, the logarithm-of-production rate appears to decline linearly with time in many wells. However, water production is much more erratic as a function of time from an individual well and also from one well to the next within a field. Water production can either decrease or increase with time (from the first to the second sample). In this study, slightly more than half the wells producing from the Mesaverde Group show decreases in water production with time. Plots of water decline versus gas decline show little relation between the two, with only the wells in Rulison field displaying some tendency for water and gas to decline proportionately.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20101110","usgsCitation":"Nelson, P.H., and Santus, S.L., 2010, Gas, oil, and water production from Grand Valley, Parachute, Rulison, and Mamm Creek fields in the Piceance Basin, Colorado: U.S. Geological Survey Open-File Report 2010-1110, v, 28 p.; 6 Plates: 24.00 × 16.00 inches; 6 Appendices; Downloads Directory, https://doi.org/10.3133/ofr20101110.","productDescription":"v, 28 p.; 6 Plates: 24.00 × 16.00 inches; 6 Appendices; Downloads Directory","onlineOnly":"Y","additionalOnlineFiles":"Y","costCenters":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"links":[{"id":125360,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr_2010_1110.jpg"},{"id":404392,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_93283.htm","linkFileType":{"id":5,"text":"html"}},{"id":13720,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2010/1110/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Colorado","otherGeospatial":"Grand Valley, Parachute, Rulison, and Mamm Creek fields, Piceance Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -108.5208,\n              39.1333\n            ],\n            [\n              -107.3333,\n              39.1333\n            ],\n            [\n              -107.3333,\n              39.75\n            ],\n            [\n              -108.5208,\n              39.75\n            ],\n            [\n              -108.5208,\n              39.1333\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b28e4b07f02db6b12fd","contributors":{"authors":[{"text":"Nelson, Philip H. pnelson@usgs.gov","contributorId":862,"corporation":false,"usgs":true,"family":"Nelson","given":"Philip","email":"pnelson@usgs.gov","middleInitial":"H.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":305352,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Santus, Stephen L. ssantus@usgs.gov","contributorId":4566,"corporation":false,"usgs":true,"family":"Santus","given":"Stephen","email":"ssantus@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":true,"id":305353,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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