{"pageNumber":"1909","pageRowStart":"47700","pageSize":"25","recordCount":184605,"records":[{"id":70150455,"text":"70150455 - 2010 - Effects of visible implant elastomer mark colour on the predation of red shiners by largemouth bass","interactions":[],"lastModifiedDate":"2015-06-26T09:35:26","indexId":"70150455","displayToPublicDate":"2010-06-01T10:30:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1659,"text":"Fisheries Management and Ecology","active":true,"publicationSubtype":{"id":10}},"title":"Effects of visible implant elastomer mark colour on the predation of red shiners by largemouth bass","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Blackwell Science","publisherLocation":"Oxford, England","doi":"10.1111/j.1365-2400.2009.00720.x","usgsCitation":"Bouska, W.W., and Paukert, C.P., 2010, Effects of visible implant elastomer mark colour on the predation of red shiners by largemouth bass: Fisheries Management and Ecology, v. 17, no. 3, p. 294-296, https://doi.org/10.1111/j.1365-2400.2009.00720.x.","productDescription":"3 p.","startPage":"294","endPage":"296","numberOfPages":"3","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-011013","costCenters":[{"id":198,"text":"Coop Res Unit Atlanta","active":true,"usgs":true}],"links":[{"id":302359,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","issue":"3","publishingServiceCenter":{"id":8,"text":"Raleigh PSC"},"noUsgsAuthors":false,"publicationDate":"2010-05-07","publicationStatus":"PW","scienceBaseUri":"558e77b5e4b0b6d21dd65950","contributors":{"authors":[{"text":"Bouska, Wesley W.","contributorId":143724,"corporation":false,"usgs":false,"family":"Bouska","given":"Wesley","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":556938,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Paukert, Craig P. 0000-0002-9369-8545 cpaukert@usgs.gov","orcid":"https://orcid.org/0000-0002-9369-8545","contributorId":879,"corporation":false,"usgs":true,"family":"Paukert","given":"Craig","email":"cpaukert@usgs.gov","middleInitial":"P.","affiliations":[{"id":198,"text":"Coop Res Unit Atlanta","active":true,"usgs":true}],"preferred":true,"id":556906,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70227336,"text":"70227336 - 2010 - Lichen diversity changes along the Mississippi River in the Minneapolis-St. Paul urban area","interactions":[],"lastModifiedDate":"2022-01-10T16:08:34.480078","indexId":"70227336","displayToPublicDate":"2010-06-01T09:59:18","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1087,"text":"Bryologist","active":true,"publicationSubtype":{"id":10}},"title":"Lichen diversity changes along the Mississippi River in the Minneapolis-St. Paul urban area","docAbstract":"<p><span>Lichen diversity along the Mississippi River in the Minneapolis-St. Paul urban area was studied in 2008 by sampling 37 localities along the 110-kilometer river basin, resulting in 76 species, which are thought to represent 80% of the complete flora. A significant decrease in lichen diversity toward the urban part of the river basin, as well as the presence of only one cyanolichen suggests that urban factors, e.g. air pollutants and habitat destruction may be affecting lichen diversity. In addition, lichen diversity has significantly decreased from that of 112&nbsp;years ago, when a study by Fink reported 113 species, and a higher number of genera represented by a single species.</span></p>","language":"English","publisher":"American Bryological and Lichenological Society","doi":"10.1639/0007-2745-113.2.252","usgsCitation":"Bennett, J.P., and Wetmore, C.M., 2010, Lichen diversity changes along the Mississippi River in the Minneapolis-St. Paul urban area: Bryologist, v. 113, no. 2, p. 252-259, https://doi.org/10.1639/0007-2745-113.2.252.","productDescription":"8 p.","startPage":"252","endPage":"259","costCenters":[],"links":[{"id":394107,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Minnesota","city":"Minneapolis, St. Paul","otherGeospatial":"Mississippi River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -93.84796142578124,\n              44.60806814444478\n            ],\n            [\n              -92.63671875,\n              44.60806814444478\n            ],\n            [\n              -92.63671875,\n              45.41002023463975\n            ],\n            [\n              -93.84796142578124,\n              45.41002023463975\n            ],\n            [\n              -93.84796142578124,\n              44.60806814444478\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"113","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Bennett, James P.","contributorId":100323,"corporation":false,"usgs":true,"family":"Bennett","given":"James","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":830508,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wetmore, C. M.","contributorId":65036,"corporation":false,"usgs":false,"family":"Wetmore","given":"C.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":830509,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70227366,"text":"70227366 - 2010 - A chronicle of Miocene extension near the Colorado Plateau-Basin and Range boundary, southern White Hills, northwestern Arizona: Paleogeographic and tectonic implications","interactions":[],"lastModifiedDate":"2022-01-11T14:54:06.238118","indexId":"70227366","displayToPublicDate":"2010-06-01T08:43:05","publicationYear":"2010","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"A chronicle of Miocene extension near the Colorado Plateau-Basin and Range boundary, southern White Hills, northwestern Arizona: Paleogeographic and tectonic implications","docAbstract":"<p><span>In northwestern Arizona, the high-standing, relatively unextended Colorado Plateau abruptly gives way across a system of major west-dipping normal faults to a highly extended part of the Basin and Range province known as the northern Colorado River extensional corridor. The transition from unextended to highly extended upper crust is unusually sharp within this region, contrasting with a broad transition zone elsewhere. The southern White Hills lie near the eastern margin of the extensional corridor in northwestern Arizona and contain a large east-tilted half graben that chronicles Miocene extension and constrains the timing of structural demarcation between the Colorado Plateau and Basin and Range province during Neogene time. This growth-fault basin is bounded on the east by the west-dipping Cyclopic and Cerbat Mountains fault zones. Greater tilts in the hanging walls suggest that these faults have listric geometries. The stratigraphy in the half graben consists of Miocene vol canic rocks intercalated with an eastward-thickening wedge of synextensional fanglomerates. Tilts in the Miocene units decrease up section from ~75° to 5°. Recent&nbsp;</span><sup>40</sup><span>Ar/</span><sup>39</sup><span>Ar dating (11 new dates) of variably tilted volcanic rocks in the growth-fault basin and regional relations constrain the timing of east-west extension between ca. 16.6 and &lt;9 Ma, with peak extension from ca. 16.6 to 15.2 Ma. Capping 8.7 Ma basalts are tilted 5°–10° and record the waning stages of extension. Thus, the sharp boundary between the Colorado Plateau and Basin and Range began developing by ca. 16.5 Ma and has changed little since ca. 9 Ma. Major extension and basin development significantly lowered base level within the extensional corridor and induced headward erosion into the western margin of the Colorado Plateau, which ultimately facilitated development of the western Grand Canyon. Abundant clasts of 1.7 Ga megacrystic granite in the eastward-thickening fanglomerates within the growth-fault basin suggest a partial provenance from the Garnet Mountain area along or near the western margin of the Colorado Plateau beginning as early as ca. 16 Ma and continuing to ca. 9 Ma.</span></p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Miocene tectonics of the Lake Mead Region, central basin and range","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Geological Society of America","doi":"10.1130/2010.2463(05)","usgsCitation":"Faulds, J., Price, L.M., Snee, L.W., and Gans, P.B., 2010, A chronicle of Miocene extension near the Colorado Plateau-Basin and Range boundary, southern White Hills, northwestern Arizona: Paleogeographic and tectonic implications, chap. <i>of</i> Miocene tectonics of the Lake Mead Region, central basin and range, p. 87-119, https://doi.org/10.1130/2010.2463(05).","productDescription":"33 p.","startPage":"87","endPage":"119","costCenters":[],"links":[{"id":394182,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Arizona","otherGeospatial":"southern White HIlls","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -114.4830322265625,\n              35.65729624809628\n            ],\n            [\n              -113.8348388671875,\n              35.65729624809628\n            ],\n            [\n              -113.8348388671875,\n              35.93798832265393\n            ],\n            [\n              -114.4830322265625,\n              35.93798832265393\n            ],\n            [\n              -114.4830322265625,\n              35.65729624809628\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Faulds, James E.","contributorId":252834,"corporation":false,"usgs":false,"family":"Faulds","given":"James E.","affiliations":[{"id":50442,"text":"Great Basin Center for Geothermal Energy, Nevada Bureau of Mines and Geology, University of Nevada, Reno","active":true,"usgs":false}],"preferred":false,"id":830608,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Price, Linda M.","contributorId":271055,"corporation":false,"usgs":false,"family":"Price","given":"Linda","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":830609,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Snee, Lawrence W.","contributorId":199028,"corporation":false,"usgs":false,"family":"Snee","given":"Lawrence","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":830610,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Gans, Philip B.","contributorId":66791,"corporation":false,"usgs":false,"family":"Gans","given":"Philip","email":"","middleInitial":"B.","affiliations":[{"id":30783,"text":"Department of Earth Science, University of California, Santa Barbara, CA","active":true,"usgs":false}],"preferred":false,"id":830611,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70192478,"text":"70192478 - 2010 - Periodic, chaotic, and doubled earthquake recurrence intervals on the deep San Andreas Fault","interactions":[],"lastModifiedDate":"2017-10-26T14:57:50","indexId":"70192478","displayToPublicDate":"2010-06-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Periodic, chaotic, and doubled earthquake recurrence intervals on the deep San Andreas Fault","docAbstract":"<p><span>Earthquake recurrence histories may provide clues to the timing of future events, but long intervals between large events obscure full recurrence variability. In contrast, small earthquakes occur frequently, and recurrence intervals are quantifiable on a much shorter time scale. In this work, I examine an 8.5-year sequence of more than 900 recurring low-frequency earthquake bursts composing tremor beneath the San Andreas fault near Parkfield, California. These events exhibit tightly clustered recurrence intervals that, at times, oscillate between ~3 and ~6 days, but the patterns sometimes change abruptly. Although the environments of large and low-frequency earthquakes are different, these observations suggest that similar complexity might underlie sequences of large earthquakes.</span></p>","language":"English","publisher":"AAAS","doi":"10.1126/science.1189741","usgsCitation":"Shelly, D.R., 2010, Periodic, chaotic, and doubled earthquake recurrence intervals on the deep San Andreas Fault: Science, v. 328, no. 5984, p. 1385-1388, https://doi.org/10.1126/science.1189741.","productDescription":"4 p.","startPage":"1385","endPage":"1388","ipdsId":"IP-020851","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"links":[{"id":347501,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"San Andreas Fault","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -120.5,\n              35.5\n            ],\n            [\n              -120,\n              35.5\n            ],\n            [\n              -120,\n              36\n            ],\n            [\n              -120.5,\n              36\n            ],\n            [\n              -120.5,\n              35.5\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"328","issue":"5984","publishingServiceCenter":{"id":14,"text":"Menlo Park PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5a07f61ee4b09af898c8cded","contributors":{"authors":[{"text":"Shelly, David R. dshelly@usgs.gov","contributorId":2978,"corporation":false,"usgs":true,"family":"Shelly","given":"David","email":"dshelly@usgs.gov","middleInitial":"R.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true},{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"preferred":true,"id":716046,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70043809,"text":"70043809 - 2010 - Establishment and partial characterization of a cell line from burbot Lota lota maculosa: susceptibility to IHNV, IPNV and VHSV.","interactions":[],"lastModifiedDate":"2013-04-10T13:27:07","indexId":"70043809","displayToPublicDate":"2010-06-01T00:00:00","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":"Establishment and partial characterization of a cell line from burbot Lota lota maculosa: susceptibility to IHNV, IPNV and VHSV.","docAbstract":"This study describes the development and partial characterization of a continuous fibroblastic-like cell line (BEF-1) developed from late stage embryos of North American burbot Lota lota maculosa. This cell line has been maintained for over 5 yr and 100 passages in vitro. Cells were cultured using Eagle’s minimum essential medium with Earle’s salts (MEM) supplemented with GlutaMAX™, and 10% fetal bovine serum (FBS), pH 7.4. The addition of penicillin-streptomycin-neomycin (PSN) antibiotic mixture (0.05, 0.05, 0.1 mg ml–1, respectively) did not negatively influence cell replication; however, the antimycotic Fungizone™ (2.5 µg ml–1, amphotericin B) caused cell rounding and resulted in a severe decrease in cell proliferation. Optimal incubation temperature has been observed between 15 and 23°C, and at these temperatures cultures are routinely passed using standard trypsinization methods every 5 to 7 d at a split ratio of 1:3 or 1:4. The cell line was susceptible to isolates of the M and U North American genotypes of infectious hematopoietic necrosis virus (IHNV), and to isolates of genotypes I, IVa, and IVb of viral hemorrhagic septicemia virus (VHSV). In contrast, the cell line was refractory to infection by 2 North American isolates of infectious pancreatic necrosis virus (IPNV) from serotypes A1 and A9. This cell line provides a new laboratory tool, will allow further investigation into viral diseases of burbot and possibly other species, and is the first immortalized cell line reported from a species in the Gadidae (cod) family.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Diseases of Aquatic Organisms","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Inter-Research","publisherLocation":"Oldendorf/Luhe Germany","doi":"10.3354/dao02215","usgsCitation":"Batts, W.N., Polinski, M.P., Drennan, J.D., Ireland, S., and Cain, K.D., 2010, Establishment and partial characterization of a cell line from burbot Lota lota maculosa: susceptibility to IHNV, IPNV and VHSV.: Diseases of Aquatic Organisms, v. 90, no. 1, p. 15-23, https://doi.org/10.3354/dao02215.","startPage":"15","endPage":"23","numberOfPages":"9","ipdsId":"IP-020057","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":475720,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.3354/dao02215","text":"Publisher Index Page"},{"id":270777,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":270776,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.3354/dao02215"}],"country":"United States","volume":"90","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"516689e2e4b0bba30b388bd2","contributors":{"authors":[{"text":"Batts, William N. 0000-0002-6469-9004 bbatts@usgs.gov","orcid":"https://orcid.org/0000-0002-6469-9004","contributorId":3815,"corporation":false,"usgs":true,"family":"Batts","given":"William","email":"bbatts@usgs.gov","middleInitial":"N.","affiliations":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"preferred":true,"id":474259,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Polinski, Mark P.","contributorId":7980,"corporation":false,"usgs":true,"family":"Polinski","given":"Mark","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":474260,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Drennan, John D.","contributorId":43252,"corporation":false,"usgs":true,"family":"Drennan","given":"John","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":474262,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ireland, Susan C.","contributorId":18244,"corporation":false,"usgs":true,"family":"Ireland","given":"Susan C.","affiliations":[],"preferred":false,"id":474261,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Cain, Kenneth D.","contributorId":66146,"corporation":false,"usgs":true,"family":"Cain","given":"Kenneth","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":474263,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70186004,"text":"70186004 - 2010 - Diatomite, 2009","interactions":[],"lastModifiedDate":"2017-03-31T10:30:25","indexId":"70186004","displayToPublicDate":"2010-06-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2755,"text":"Mining Engineering","active":true,"publicationSubtype":{"id":10}},"title":"Diatomite, 2009","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"SME","usgsCitation":"Crangle, R., 2010, Diatomite, 2009: Mining Engineering, v. 62, no. 6, p. 39-39.","productDescription":"1 p.","startPage":"39","endPage":"39","ipdsId":"IP-012730","costCenters":[{"id":432,"text":"National Minerals Information Center","active":true,"usgs":true}],"links":[{"id":338935,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":338934,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://me.smenet.org/abstract.cfm?preview=1&articleID=391&page=39"}],"volume":"62","issue":"6","publishingServiceCenter":{"id":9,"text":"Reston PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58df6ac8e4b02ff32c6aea77","contributors":{"authors":[{"text":"Crangle, Robert Jr. 0000-0002-8120-3760 rcrangle@usgs.gov","orcid":"https://orcid.org/0000-0002-8120-3760","contributorId":141008,"corporation":false,"usgs":true,"family":"Crangle","given":"Robert","suffix":"Jr.","email":"rcrangle@usgs.gov","affiliations":[{"id":432,"text":"National Minerals Information Center","active":true,"usgs":true}],"preferred":true,"id":687328,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70188016,"text":"70188016 - 2010 - Soil quality assessment using weighted fuzzy association rules","interactions":[],"lastModifiedDate":"2017-05-26T13:38:04","indexId":"70188016","displayToPublicDate":"2010-06-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3025,"text":"Pedosphere","active":true,"publicationSubtype":{"id":10}},"title":"Soil quality assessment using weighted fuzzy association rules","docAbstract":"<p><span>Fuzzy association rules (FARs) can be powerful in assessing regional soil quality, a critical step prior to land planning and utilization; however, traditional FARs mined from soil quality database, ignoring the importance variability of the rules, can be redundant and far from optimal. In this study, we developed a method applying different weights to traditional FARs to improve accuracy of soil quality assessment. After the FARs for soil quality assessment were mined, redundant rules were eliminated according to whether the rules were significant or not in reducing the complexity of the soil quality assessment models and in improving the comprehensibility of FARs. The global weights, each representing the importance of a FAR in soil quality assessment, were then introduced and refined using a gradient descent optimization method. This method was applied to the assessment of soil resources conditions in Guangdong Province, China. The new approach had an accuracy of 87%, when 15 rules were mined, as compared with 76% from the traditional approach. The accuracy increased to 96% when 32 rules were mined, in contrast to 88% from the traditional approach. These results demonstrated an improved comprehensibility of FARs and a high accuracy of the proposed method.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/S1002-0160(10)60022-7","usgsCitation":"Xue, Y., Liu, S., Hu, Y., and Yang, J., 2010, Soil quality assessment using weighted fuzzy association rules: Pedosphere, v. 20, no. 3, p. 334-341, https://doi.org/10.1016/S1002-0160(10)60022-7.","productDescription":"8 p.","startPage":"334","endPage":"341","ipdsId":"IP-010167","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":341805,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"20","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"59293e9ae4b016f7a9407718","contributors":{"authors":[{"text":"Xue, Yue-Ju","contributorId":44346,"corporation":false,"usgs":true,"family":"Xue","given":"Yue-Ju","email":"","affiliations":[],"preferred":false,"id":696187,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Liu, Shu-Guang sliu@usgs.gov","contributorId":984,"corporation":false,"usgs":true,"family":"Liu","given":"Shu-Guang","email":"sliu@usgs.gov","affiliations":[{"id":223,"text":"Earth Resources Observation and Science (EROS) Center (Geography)","active":false,"usgs":true}],"preferred":false,"id":696188,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hu, Yue-Ming","contributorId":192310,"corporation":false,"usgs":false,"family":"Hu","given":"Yue-Ming","affiliations":[],"preferred":false,"id":696189,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Yang, Jing","contributorId":192311,"corporation":false,"usgs":false,"family":"Yang","given":"Jing","affiliations":[],"preferred":false,"id":696190,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70189349,"text":"70189349 - 2010 - Source and fate of inorganic solutes in the Gibbon River, Yellowstone National Park, Wyoming, USA: I. Low-flow discharge and major solute chemistry","interactions":[],"lastModifiedDate":"2018-10-10T13:17:22","indexId":"70189349","displayToPublicDate":"2010-06-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2499,"text":"Journal of Volcanology and Geothermal Research","active":true,"publicationSubtype":{"id":10}},"title":"Source and fate of inorganic solutes in the Gibbon River, Yellowstone National Park, Wyoming, USA: I. Low-flow discharge and major solute chemistry","docAbstract":"<p><span>The Gibbon River in Yellowstone National Park (YNP) is an important natural resource and habitat for fisheries and wildlife. However, the Gibbon River differs from most other mountain rivers because its chemistry is affected by several geothermal sources including Norris Geyser Basin, Chocolate Pots, Gibbon Geyser Basin, Beryl Spring, and Terrace Spring. Norris Geyser Basin is one of the most dynamic geothermal areas in YNP, and the water discharging from Norris is much more acidic (pH 3) than other geothermal basins in the upper-Madison drainage (Gibbon and Firehole Rivers). Water samples and discharge data were obtained from the Gibbon River and its major tributaries near Norris Geyser Basin under the low-flow conditions of September 2006. Surface inflows from Norris Geyser Basin were sampled to identify point sources and to quantify solute loading to the Gibbon River. The source and fate of the major solutes (Ca, Mg, Na, K, SiO</span><sub>2</sub><span>, Cl, F, HCO</span><sub>3</sub><span>, SO</span><sub>4</sub><span>, NO</span><sub>3</sub><span>, and NH</span><sub>4</sub><span>) in the Gibbon River were determined in this study and these results may provide an important link in understanding the health of the ecosystem and the behavior of many trace solutes. Norris Geyser Basin is the primary source of Na, K, Cl, SO</span><sub>4</sub><span>, and N loads (35–58%) in the Gibbon River. The largest source of HCO</span><sub>3</sub><span><span>&nbsp;</span>and F is in the lower Gibbon River reach. Most of the Ca and Mg originate in the Gibbon River upstream from Norris Geyser Basin. All the major solutes behave conservatively except for NH</span><sub>4</sub><span>, which decreased substantially downstream from Gibbon Geyser Basin, and SiO</span><sub>2</sub><span>, small amounts of which precipitated on mixing of thermal drainage with the river. As much as 9–14% of the river discharge at the gage is from thermal flows during this period.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.jvolgeores.2010.03.014","usgsCitation":"McCleskey, R.B., Nordstrom, D.K., Susong, D.D., Ball, J.W., and Holloway, J.M., 2010, Source and fate of inorganic solutes in the Gibbon River, Yellowstone National Park, Wyoming, USA: I. Low-flow discharge and major solute chemistry: Journal of Volcanology and Geothermal Research, v. 193, no. 34-4, p. 189-202, https://doi.org/10.1016/j.jvolgeores.2010.03.014.","productDescription":"14 p.","startPage":"189","endPage":"202","ipdsId":"IP-016033","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":343607,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Wyoming","otherGeospatial":"Yellowstone National Park","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -110.89324951171875,\n              44.6334823448553\n            ],\n            [\n              -110.65292358398438,\n              44.6334823448553\n            ],\n            [\n              -110.65292358398438,\n              44.75356026127114\n            ],\n            [\n              -110.89324951171875,\n              44.75356026127114\n            ],\n            [\n              -110.89324951171875,\n              44.6334823448553\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"193","issue":"34-4","publishingServiceCenter":{"id":2,"text":"Denver PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5965bff1e4b0d1f9f05b392d","contributors":{"authors":[{"text":"McCleskey, R. Blaine 0000-0002-2521-8052 rbmccles@usgs.gov","orcid":"https://orcid.org/0000-0002-2521-8052","contributorId":147399,"corporation":false,"usgs":true,"family":"McCleskey","given":"R.","email":"rbmccles@usgs.gov","middleInitial":"Blaine","affiliations":[{"id":503,"text":"Office of Water Quality","active":true,"usgs":true},{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true},{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":704320,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"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":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true},{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":false,"id":704318,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Susong, David D. ddsusong@usgs.gov","contributorId":1040,"corporation":false,"usgs":true,"family":"Susong","given":"David","email":"ddsusong@usgs.gov","middleInitial":"D.","affiliations":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"preferred":true,"id":704317,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ball, James W.","contributorId":38946,"corporation":false,"usgs":true,"family":"Ball","given":"James","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":704319,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Holloway, JoAnn M. 0000-0003-3603-7668 jholloway@usgs.gov","orcid":"https://orcid.org/0000-0003-3603-7668","contributorId":918,"corporation":false,"usgs":true,"family":"Holloway","given":"JoAnn","email":"jholloway@usgs.gov","middleInitial":"M.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":704321,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70176788,"text":"70176788 - 2010 - PCB exposure in sea otters and harlequin ducks in relation to history of contamination by the <i>Exxon Valdez</i> oil spill","interactions":[],"lastModifiedDate":"2018-05-13T11:58:40","indexId":"70176788","displayToPublicDate":"2010-06-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2676,"text":"Marine Pollution Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"PCB exposure in sea otters and harlequin ducks in relation to history of contamination by the <i>Exxon Valdez</i> oil spill","docAbstract":"<p><span>Exposure to contaminants other than petroleum hydrocarbons could confound interpretation of </span><i>Exxon Valdez</i><span> oil spill effects on biota at Prince William Sound, Alaska. Hence, we investigated polychlorinated biphenyls (PCBs) in blood of sea otters and harlequin ducks sampled during 1998. PCB concentrations characterized by lower chlorinated congeners were highest in sea otters from the unoiled area, whereas concentrations were similar among harlequin ducks from the oiled and unoiled area. Blood enzymes often elevated by xenobiotics were not related to PCB concentrations in sea otters. Only sea otters from the unoiled area had estimated risk from PCBs, and PCB composition or concentrations did not correspond to reported lower measures of population performance in sea otters or harlequin ducks from the oiled area. PCBs probably did not influence limited sea otter or harlequin duck recovery in the oiled area a decade after the spill.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.marpolbul.2010.01.005","usgsCitation":"Ricca, M.A., Miles, A.K., Ballachey, B.E., Bodkin, J.L., Esler, D., and Trust, K.A., 2010, PCB exposure in sea otters and harlequin ducks in relation to history of contamination by the <i>Exxon Valdez</i> oil spill: Marine Pollution Bulletin, v. 60, no. 6, p. 861-872, https://doi.org/10.1016/j.marpolbul.2010.01.005.","productDescription":"12 p.","startPage":"861","endPage":"872","ipdsId":"IP-016495","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":329350,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"60","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57fe8150e4b0824b2d1480aa","contributors":{"authors":[{"text":"Ricca, Mark A. mark_ricca@usgs.gov","contributorId":2400,"corporation":false,"usgs":true,"family":"Ricca","given":"Mark","email":"mark_ricca@usgs.gov","middleInitial":"A.","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":false,"id":650314,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miles, A. Keith 0000-0002-3108-808X keith_miles@usgs.gov","orcid":"https://orcid.org/0000-0002-3108-808X","contributorId":196,"corporation":false,"usgs":true,"family":"Miles","given":"A.","email":"keith_miles@usgs.gov","middleInitial":"Keith","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":true,"id":650315,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ballachey, Brenda E. 0000-0003-1855-9171 bballachey@usgs.gov","orcid":"https://orcid.org/0000-0003-1855-9171","contributorId":2966,"corporation":false,"usgs":true,"family":"Ballachey","given":"Brenda","email":"bballachey@usgs.gov","middleInitial":"E.","affiliations":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":116,"text":"Alaska Science Center Biology MFEB","active":true,"usgs":true}],"preferred":true,"id":650316,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bodkin, James L. 0000-0003-1641-4438 jbodkin@usgs.gov","orcid":"https://orcid.org/0000-0003-1641-4438","contributorId":748,"corporation":false,"usgs":true,"family":"Bodkin","given":"James","email":"jbodkin@usgs.gov","middleInitial":"L.","affiliations":[{"id":116,"text":"Alaska Science Center Biology MFEB","active":true,"usgs":true},{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"preferred":true,"id":650317,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Esler, Daniel 0000-0001-5501-4555 desler@usgs.gov","orcid":"https://orcid.org/0000-0001-5501-4555","contributorId":5465,"corporation":false,"usgs":true,"family":"Esler","given":"Daniel","email":"desler@usgs.gov","affiliations":[{"id":116,"text":"Alaska Science Center Biology MFEB","active":true,"usgs":true},{"id":12437,"text":"Simon Fraser University, Centre for Wildlife Ecology","active":true,"usgs":false},{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"preferred":true,"id":650318,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Trust, Kimberly A.","contributorId":42503,"corporation":false,"usgs":false,"family":"Trust","given":"Kimberly","email":"","middleInitial":"A.","affiliations":[{"id":6987,"text":"U.S. Fish and Wildlife Sevice","active":true,"usgs":false}],"preferred":false,"id":650319,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70176786,"text":"70176786 - 2010 - When parasites become prey: ecological and epidemiological significance of eating parasites","interactions":[],"lastModifiedDate":"2017-04-27T10:33:03","indexId":"70176786","displayToPublicDate":"2010-06-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3653,"text":"Trends in Ecology and Evolution","active":true,"publicationSubtype":{"id":10}},"title":"When parasites become prey: ecological and epidemiological significance of eating parasites","docAbstract":"<p><span>Recent efforts to include parasites in food webs have drawn attention to a previously ignored facet of foraging ecology: parasites commonly function as prey within ecosystems. Because of the high productivity of parasites, their unique nutritional composition and their pathogenicity in hosts, their consumption affects both food-web topology and disease risk in humans and wildlife. Here, we evaluate the ecological, evolutionary and epidemiological significance of feeding on parasites, including concomitant predation, grooming, predation on free-living stages and intraguild predation. Combining empirical data and theoretical models, we show that consumption of parasites is neither rare nor accidental, and that it can sharply affect parasite transmission and food web properties. Broader consideration of predation on parasites will enhance our understanding of disease control, food web structure and energy transfer, and the evolution of complex life cycles.</span></p>","language":"English","publisher":"Cell Press","doi":"10.1016/j.tree.2010.01.005","usgsCitation":"Johnson, P.T., Dobson, A.P., Lafferty, K.D., Marcogliese, D.J., Memmott, J., Orlofske, S.A., Poulin, R., and Thieltges, D.W., 2010, When parasites become prey: ecological and epidemiological significance of eating parasites: Trends in Ecology and Evolution, v. 25, no. 6, p. 362-371, https://doi.org/10.1016/j.tree.2010.01.005.","productDescription":"10 p.","startPage":"362","endPage":"371","ipdsId":"IP-016988","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":329348,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"25","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57fe8150e4b0824b2d1480ac","contributors":{"authors":[{"text":"Johnson, Pieter T.J.","contributorId":28508,"corporation":false,"usgs":true,"family":"Johnson","given":"Pieter","email":"","middleInitial":"T.J.","affiliations":[],"preferred":false,"id":650300,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dobson, Andrew P.","contributorId":63693,"corporation":false,"usgs":true,"family":"Dobson","given":"Andrew","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":650301,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lafferty, Kevin D. 0000-0001-7583-4593 klafferty@usgs.gov","orcid":"https://orcid.org/0000-0001-7583-4593","contributorId":1415,"corporation":false,"usgs":true,"family":"Lafferty","given":"Kevin","email":"klafferty@usgs.gov","middleInitial":"D.","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":true,"id":650302,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Marcogliese, David J.","contributorId":175161,"corporation":false,"usgs":false,"family":"Marcogliese","given":"David","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":650303,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Memmott, Jane","contributorId":175162,"corporation":false,"usgs":false,"family":"Memmott","given":"Jane","email":"","affiliations":[],"preferred":false,"id":650304,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Orlofske, Sarah A.","contributorId":175163,"corporation":false,"usgs":false,"family":"Orlofske","given":"Sarah","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":650305,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Poulin, Robert","contributorId":106813,"corporation":false,"usgs":true,"family":"Poulin","given":"Robert","email":"","affiliations":[],"preferred":false,"id":650306,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Thieltges, David W.","contributorId":56163,"corporation":false,"usgs":true,"family":"Thieltges","given":"David","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":650307,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":70148694,"text":"70148694 - 2010 - Conservation genetics of the alligator snapping turtle: cytonuclear evidence of range-wide bottleneck effects and unusually pronounced geographic structure","interactions":[],"lastModifiedDate":"2015-07-01T13:28:44","indexId":"70148694","displayToPublicDate":"2010-06-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1324,"text":"Conservation Genetics","active":true,"publicationSubtype":{"id":10}},"title":"Conservation genetics of the alligator snapping turtle: cytonuclear evidence of range-wide bottleneck effects and unusually pronounced geographic structure","docAbstract":"<p><span>A previous mtDNA study indicated that female-mediated gene flow was extremely rare among alligator snapping turtle populations in different drainages of the Gulf of Mexico. In this study, we used variation at seven microsatellite DNA loci to assess the possibility of male-mediated gene flow, we augmented the mtDNA survey with additional sampling of the large Mississippi River System, and we evaluated the hypothesis that the consistently low within-population mtDNA diversity reflects past population bottlenecks. The results show that dispersal between drainages of the Gulf of Mexico is rare (</span><i class=\"EmphasisTypeItalic\">F</i><span>&nbsp;</span><span>ST<i class=\"EmphasisTypeItalic\">msat</i>&nbsp;</span><span>&nbsp;=&nbsp;0.43, &Phi;</span><span>STmtDNA</span><span>&nbsp;=&nbsp;0.98). Past range-wide bottlenecks are indicated by several genetic signals, including low diversity for microsatellites (1.1&ndash;3.9 alleles/locus;&nbsp;</span><i class=\"EmphasisTypeItalic\">H</i><span>&nbsp;</span><span>e</span><span>&nbsp;=&nbsp;0.06&ndash;0.53) and mtDNA (</span><i class=\"EmphasisTypeItalic\">h</i><span>&nbsp;=&nbsp;0.00 for most drainages;&nbsp;</span><i class=\"EmphasisTypeItalic\">&pi;</i><span>&nbsp;=&nbsp;0.000&ndash;0.001). Microsatellite data reinforce the conclusion from mtDNA that the Suwannee River population might eventually be recognized as a distinct taxonomic unit. It was the only population showing fixation or near fixation for otherwise rare microsatellite alleles. Six evolutionarily significant units are recommended on the basis of reciprocal mtDNA monophyly and high levels of microsatellite DNA divergence.</span></p>","language":"English","publisher":"Springer","doi":"10.1007/s10592-009-9966-1","usgsCitation":"Echelle, A., Hackler, J., Lack, J., Ballard, S.R., Roman, J., Fox, S.F., Leslie, D.M., and Van Den Bussche, R.A., 2010, Conservation genetics of the alligator snapping turtle: cytonuclear evidence of range-wide bottleneck effects and unusually pronounced geographic structure: Conservation Genetics, v. 11, no. 4, p. 1375-1387, https://doi.org/10.1007/s10592-009-9966-1.","productDescription":"13 p.","startPage":"1375","endPage":"1387","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-013033","costCenters":[{"id":198,"text":"Coop Res Unit Atlanta","active":true,"usgs":true}],"links":[{"id":305542,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","otherGeospatial":"Gulf of Mexico","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -95.537109375,\n              28.613459424004414\n            ],\n            [\n              -95.537109375,\n              34.08906131584996\n            ],\n            [\n              -82.24365234375,\n              34.08906131584996\n            ],\n            [\n              -82.24365234375,\n              28.613459424004414\n            ],\n            [\n              -95.537109375,\n              28.613459424004414\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"11","issue":"4","publishingServiceCenter":{"id":8,"text":"Raleigh PSC"},"noUsgsAuthors":false,"publicationDate":"2009-08-04","publicationStatus":"PW","scienceBaseUri":"55950f2ee4b0b6d21dd6cbdb","contributors":{"authors":[{"text":"Echelle, A.A.","contributorId":61981,"corporation":false,"usgs":true,"family":"Echelle","given":"A.A.","affiliations":[],"preferred":false,"id":564060,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hackler, J.C.","contributorId":105835,"corporation":false,"usgs":true,"family":"Hackler","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":564061,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lack, Justin B.","contributorId":82038,"corporation":false,"usgs":true,"family":"Lack","given":"Justin B.","affiliations":[],"preferred":false,"id":564062,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ballard, S. R.","contributorId":145446,"corporation":false,"usgs":false,"family":"Ballard","given":"S.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":564063,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Roman, J.","contributorId":145447,"corporation":false,"usgs":false,"family":"Roman","given":"J.","email":"","affiliations":[],"preferred":false,"id":564064,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Fox, S. F.","contributorId":100984,"corporation":false,"usgs":true,"family":"Fox","given":"S.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":564065,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Leslie, David M. Jr. 0000-0002-3884-1484 cleslie@usgs.gov","orcid":"https://orcid.org/0000-0002-3884-1484","contributorId":2483,"corporation":false,"usgs":true,"family":"Leslie","given":"David","suffix":"Jr.","email":"cleslie@usgs.gov","middleInitial":"M.","affiliations":[{"id":198,"text":"Coop Res Unit Atlanta","active":true,"usgs":true}],"preferred":false,"id":549061,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Van Den Bussche, Ronald A.","contributorId":41121,"corporation":false,"usgs":true,"family":"Van Den Bussche","given":"Ronald","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":564066,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":70138811,"text":"70138811 - 2010 - A comparison of methods for estimating open-water evaporation in small wetlands","interactions":[],"lastModifiedDate":"2018-10-10T10:25:27","indexId":"70138811","displayToPublicDate":"2010-06-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3750,"text":"Wetlands","onlineIssn":"1943-6246","printIssn":"0277-5212","active":true,"publicationSubtype":{"id":10}},"title":"A comparison of methods for estimating open-water evaporation in small wetlands","docAbstract":"<p><span>We compared evaporation measurements from a floating pan, land pan, chamber, and the Priestley-Taylor (PT) equation. Floating pan, land pan, and meteorological data were collected from June 6 to July 21, 2005, at a small wetland in the Canadian River alluvium in central Oklahoma, USA. Evaporation measured with the floating pan compared favorably to 12&nbsp;h chamber measurements. Differences between chamber and floating pan rates ranged from &minus;0.2 to 0.3&nbsp;mm, mean of 0.1&nbsp;mm. The difference between chamber and land pan rates ranged from 0.8 to 2.0&nbsp;mm, mean of 1.5&nbsp;mm. The mean chamber-to-floating pan ratio was 0.97 and the mean chamber-to-land pan ratio was 0.73. The chamber-to-floating pan ratio of 0.97 indicates the use of a floating pan to measure evaporation in small limited-fetch water bodies is an appropriate and accurate method for the site investigated. One-sided Paired t-Tests indicate daily floating pan rates were significantly less than land pan and PT rates. A two-sided Paired t-Test indicated there was no significant difference between land pan and PT values. The PT equation tends to overestimate evaporation during times when the air is of low drying power and tends to underestimate as drying power increases.</span></p>","language":"English","publisher":"Springer","doi":"10.1007/s13157-010-0041-y","usgsCitation":"Masoner, J.R., and Stannard, D.I., 2010, A comparison of methods for estimating open-water evaporation in small wetlands: Wetlands, v. 30, no. 3, p. 513-524, https://doi.org/10.1007/s13157-010-0041-y.","productDescription":"12 p.","startPage":"513","endPage":"524","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-013356","costCenters":[{"id":516,"text":"Oklahoma Water Science Center","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":297518,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Oklahoma","otherGeospatial":"Canadian River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -102.919921875,\n              37.020098201368114\n            ],\n            [\n              -94.2626953125,\n              36.914764288955936\n            ],\n            [\n              -94.4384765625,\n              33.43144133557529\n            ],\n            [\n              -100.107421875,\n              34.415973384481866\n            ],\n            [\n              -102.919921875,\n              37.020098201368114\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"30","issue":"3","publishingServiceCenter":{"id":5,"text":"Lafayette PSC"},"noUsgsAuthors":false,"publicationDate":"2010-05-19","publicationStatus":"PW","scienceBaseUri":"54dd2b17e4b08de9379b3235","contributors":{"authors":[{"text":"Masoner, Jason R. 0000-0002-4829-6379 jmasoner@usgs.gov","orcid":"https://orcid.org/0000-0002-4829-6379","contributorId":3193,"corporation":false,"usgs":true,"family":"Masoner","given":"Jason","email":"jmasoner@usgs.gov","middleInitial":"R.","affiliations":[{"id":516,"text":"Oklahoma Water Science Center","active":true,"usgs":true},{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":538919,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stannard, David I. distanna@usgs.gov","contributorId":562,"corporation":false,"usgs":true,"family":"Stannard","given":"David","email":"distanna@usgs.gov","middleInitial":"I.","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":false,"id":538918,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70043952,"text":"70043952 - 2010 - Influence of a low intensity electric sea lion deterrence system on the migratory behavior of fishes in the upstream migrant tunnel (UMT) at Bonneville Dam.","interactions":[],"lastModifiedDate":"2016-12-28T12:00:09","indexId":"70043952","displayToPublicDate":"2010-06-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"title":"Influence of a low intensity electric sea lion deterrence system on the migratory behavior of fishes in the upstream migrant tunnel (UMT) at Bonneville Dam.","docAbstract":"Predation by pinnipeds, such as California sea lions (Zalophus alifornianus), Pacific harbor seals (Phoca vitulina), and Stellar sea lions (Eumetopias jubatus) on returning adult Pacific salmon (Oncorhynchus spp.) in the Columbia River basin has become an increasing concern for fishery managers trying to conserve and restore threatened and endangered runs of\nsalmonids. As a result, Smith-Root Incorporated (SRI; Vancouver, Washington) proposed a demonstration project to evaluate the potential of an electrical array to deter marine mammals (SRI 2007). The objective of their work was to develop, deploy, and evaluate a passive, integrated electric and sonar array that selectively inhibits upstream marine mammal movements and predation, without injuring pinnipeds or affecting anadromous fish migrations. However, before such a device could be placed in the field, concerns by regional fishery managers about the potential effects of such a device on the migratory behavior of or injury to Pacific salmon, steelhead (O. mykiss), Pacific lampreys (Entoshpenus tridentata), and white sturgeon (Acipenser transmontanus) needed to be addressed.","language":"English","publisher":"Bonneville Power Administration","publisherLocation":"Portland, OR","usgsCitation":"Mesa, M.G., and Dixon, C.J., 2010, Influence of a low intensity electric sea lion deterrence system on the migratory behavior of fishes in the upstream migrant tunnel (UMT) at Bonneville Dam., 18 p.","productDescription":"18 p.","ipdsId":"IP-022717","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":332584,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":332583,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pisces.bpa.gov/release/documents/documentviewer.aspx?doc=P119148"}],"country":"United States","state":"Oregon, Washington","otherGeospatial":"Bonneville Dam ","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -121.94480895996094,\n              45.65484809235974\n            ],\n            [\n              -121.90979003906249,\n              45.66564594502495\n            ],\n            [\n              -121.9197463989258,\n              45.67044432223406\n            ],\n            [\n              -121.90567016601562,\n              45.6819587493002\n            ],\n            [\n              -121.87683105468749,\n              45.67548217560647\n            ],\n            [\n              -121.92043304443361,\n              45.64020767854683\n            ],\n            [\n              -121.97845458984375,\n              45.62052109300635\n            ],\n            [\n              -121.97982788085938,\n              45.62940492064501\n            ],\n            [\n              -121.94480895996094,\n              45.65484809235974\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5864dd51e4b0cd2dabe7c1d3","contributors":{"authors":[{"text":"Mesa, Matthew G. mmesa@usgs.gov","contributorId":3423,"corporation":false,"usgs":true,"family":"Mesa","given":"Matthew","email":"mmesa@usgs.gov","middleInitial":"G.","affiliations":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"preferred":true,"id":656732,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dixon, Christopher J.","contributorId":42110,"corporation":false,"usgs":true,"family":"Dixon","given":"Christopher","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":656733,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70156473,"text":"70156473 - 2010 - Coalbed methane resources of the Appalachian Basin, eastern USA","interactions":[],"lastModifiedDate":"2022-11-08T19:49:11.743877","indexId":"70156473","displayToPublicDate":"2010-06-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2033,"text":"International Journal of Coal Geology","active":true,"publicationSubtype":{"id":10}},"title":"Coalbed methane resources of the Appalachian Basin, eastern USA","docAbstract":"<p><span>In 2002, the U.S. Geological Survey (USGS) assessed the technically recoverable, undiscovered coalbed-gas resources in the Appalachian basin and Black Warrior basin Assessment Provinces as about 15.5 trillion cubic feet. Although these resources are almost equally divided between the two areas, most of the production occurs within relatively small areas within these Provinces, where local geological and geochemical attributes have resulted in the generation and retention of large amounts of methane within the coal beds and have enhanced the producibility of the gas from the coal. In the Appalachian basin, coalbed methane (CBM) tests are commonly commercial where the cumulative coal thickness completed in wells is greater than three meters (10 ft), the depth of burial of the coal beds is greater than 100 m (350 ft), and the coal is in the thermogenic gas window. In addition to the ubiquitous cleating within the coal beds, commercial production may be enhanced by secondary fracture porosity related to supplemental fracture systems within the coal beds. In order to release the methane from microporus coal matrix, most wells are dewatered prior to commercial production of gas. Two Total Petroleum Systems (TPS) were defined by the USGS during the assessment: the Pottsville Coal-bed gas TPS in Alabama, and the Carboniferous Coal-bed Gas TPS in Pennsylvania, Ohio, West Virginia, eastern Kentucky, Virginia, Tennessee, and Alabama. These were divided into seven assessment units, of which three had sufficient data to be assessed. Production rates are higher in most horizontal wells drilled into relatively thick coal beds, than in vertical wells; recovery per unit area is greater, and potential adverse environmental impact is decreased.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.coal.2009.12.002","usgsCitation":"Milici, R.C., Hatch, J.R., and Pawlewicz, M.J., 2010, Coalbed methane resources of the Appalachian Basin, eastern USA: International Journal of Coal Geology, v. 82, no. 3-4, p. 160-174, https://doi.org/10.1016/j.coal.2009.12.002.","productDescription":"14 p.","startPage":"160","endPage":"174","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-014321","costCenters":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true}],"links":[{"id":307178,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alabama, Georgia, Kentucky, Maryland, North Carolina, Ohio, Pennsylvania, Tennessee, Virginia, West Virginia","otherGeospatial":"Appalachia basin, Black Warrior basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -86.1772349848587,\n              32.60617351765971\n            ],\n            [\n              -85.19488316523514,\n              33.00638865401339\n            ],\n            [\n              -84.13304691552142,\n              34.44850870017865\n            ],\n            [\n              -82.28585557789057,\n              35.655033116716126\n            ],\n            [\n              -81.79319852391995,\n              36.73030802315243\n            ],\n            [\n              -80.3761254402848,\n              37.44233148830088\n            ],\n            [\n              -79.68042218212922,\n              38.50698634259359\n            ],\n            [\n              -78.34080155565464,\n              40.02403541761586\n            ],\n            [\n              -76.83060794686116,\n              41.192717003786925\n            ],\n            [\n              -78.24409936484965,\n              41.25247290987559\n            ],\n            [\n              -80.23785620019234,\n              41.342335351640884\n            ],\n            [\n              -81.41805273922962,\n              40.76739882672112\n            ],\n            [\n              -82.47726615944153,\n              39.63755342984686\n            ],\n            [\n              -83.56715666160146,\n              38.15773576754589\n            ],\n            [\n              -84.22984964199225,\n              37.07700800351755\n            ],\n            [\n              -84.06720954251827,\n              36.37648676643913\n            ],\n            [\n              -84.17600881138497,\n              35.91346082996118\n            ],\n            [\n              -84.66790032633628,\n              35.832765049113746\n            ],\n            [\n              -86.02615909547431,\n              34.428290075469775\n            ],\n            [\n              -87.300130820564,\n              34.25491952298243\n            ],\n            [\n              -87.71813488405401,\n              33.49819489038315\n            ],\n            [\n              -87.31792649864902,\n              32.90952614970911\n            ],\n            [\n              -86.1772349848587,\n              32.60617351765971\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"82","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"55d84bb2e4b0518e3546efee","contributors":{"authors":[{"text":"Milici, Robert C. rmilici@usgs.gov","contributorId":563,"corporation":false,"usgs":true,"family":"Milici","given":"Robert","email":"rmilici@usgs.gov","middleInitial":"C.","affiliations":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":569269,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hatch, Joseph R. 0000-0001-9257-0278 jrhatch@usgs.gov","orcid":"https://orcid.org/0000-0001-9257-0278","contributorId":722,"corporation":false,"usgs":true,"family":"Hatch","given":"Joseph","email":"jrhatch@usgs.gov","middleInitial":"R.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":569270,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Pawlewicz, Mark J. pawlewicz@usgs.gov","contributorId":752,"corporation":false,"usgs":true,"family":"Pawlewicz","given":"Mark","email":"pawlewicz@usgs.gov","middleInitial":"J.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":569271,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70156643,"text":"70156643 - 2010 - Comparison of turbidity to multi-frequency sideways-looking acoustic-Doppler data and suspended-sediment data in the Colorado River in Grand Canyon","interactions":[],"lastModifiedDate":"2021-10-26T15:44:59.093627","indexId":"70156643","displayToPublicDate":"2010-06-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Comparison of turbidity to multi-frequency sideways-looking acoustic-Doppler data and suspended-sediment data in the Colorado River in Grand Canyon","docAbstract":"<p><span>Water clarity is important to biologists when studying fish and other fluvial fauna and flora. Turbidity is an indicator of the cloudiness of water, or reduced water clarity, and is commonly measured using nephelometric sensors that record the scattering and absorption of light by particles in the water. Unfortunately, nephelometric sensors only operate over a narrow range of the conditions typically encountered in rivers dominated by suspended-sediment transport. For example, sediment inputs into the Colorado River in Grand Canyon caused by tributary floods often result in turbidity levels that exceed the maximum recording level of nephelometric turbidity sensors. The limited range of these sensors is one reason why acoustic Doppler profiler instrument data, not turbidity, has been used as a surrogate for suspended sediment concentration and load of the Colorado River in Grand Canyon. However, in addition to being an important water-quality parameter to biologists, turbidity of the Colorado River in Grand Canyon has been used to strengthen the suspended-sediment record through the process of turbidity-threshold sampling; high turbidity values trigger a pump sampler to collect samples of the river at critical times for gathering suspended-sediment data. Turbidity depends on several characteristics of suspended sediment including concentration, particle size, particle shape, color, and the refractive index of particles. In this paper, turbidity is compared with other parameters coupled to suspended sediment, namely suspended-silt and clay concentration and multifrequency acoustic attenuation. These data have been collected since 2005 at four stations with different sediment-supply characteristics on the Colorado River in Grand Canyon. These comparisons reveal that acoustic attenuation is a particularly useful parameter, because it is strongly related to turbidity and it can be measured by instruments that experience minimal fouling and record over the entire range of turbidity encountered in the Colorado River in Grand Canyon. Relating turbidity to acoustic attenuation and suspended-silt and clay concentration provides an additional benefit in that data outliers are revealed that likely identify inflow events from anomalous sources with unusual sediment characteristics.</span></p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Proceedings of the Joint Federal Interagency Conference 2010: Hydrology and sedimentation for a changing future: existing and emerging issues","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"Joint Federal Interagency Conference 2010: Hydrology and sedimentation for a changing future: existing and emerging issues","conferenceDate":"June 27-July 1 2010","conferenceLocation":"Las Vegas, Nevada","language":"English","publisher":"Joint Federal Interagency Conference","usgsCitation":"Voichick, N., and Topping, D.J., 2010, Comparison of turbidity to multi-frequency sideways-looking acoustic-Doppler data and suspended-sediment data in the Colorado River in Grand Canyon, <i>in</i> Proceedings of the Joint Federal Interagency Conference 2010: Hydrology and sedimentation for a changing future: existing and emerging issues, Las Vegas, Nevada, June 27-July 1 2010, 10 p.","productDescription":"10 p.","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-019563","costCenters":[{"id":568,"text":"Southwest Biological Science Center","active":true,"usgs":true}],"links":[{"id":307422,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Arizona","otherGeospatial":"Colorado River, Grand Canyon","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -114.0380859375,\n              35.65729624809628\n            ],\n            [\n              -111.11572265625,\n              35.65729624809628\n            ],\n            [\n              -111.11572265625,\n              36.96744946416934\n            ],\n            [\n              -114.0380859375,\n              36.96744946416934\n            ],\n            [\n              -114.0380859375,\n              35.65729624809628\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"55dd91afe4b0518e354dd13d","contributors":{"authors":[{"text":"Voichick, Nicholas nvoichick@usgs.gov","contributorId":5015,"corporation":false,"usgs":true,"family":"Voichick","given":"Nicholas","email":"nvoichick@usgs.gov","affiliations":[{"id":568,"text":"Southwest Biological Science Center","active":true,"usgs":true}],"preferred":true,"id":569775,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Topping, David J. 0000-0002-2104-4577 dtopping@usgs.gov","orcid":"https://orcid.org/0000-0002-2104-4577","contributorId":715,"corporation":false,"usgs":true,"family":"Topping","given":"David","email":"dtopping@usgs.gov","middleInitial":"J.","affiliations":[{"id":568,"text":"Southwest Biological Science Center","active":true,"usgs":true}],"preferred":false,"id":569776,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70190459,"text":"70190459 - 2010 - Geologic map of Lake Mead and surrounding regions, southern Nevada, southwestern Utah, and northwestern Arizona","interactions":[],"lastModifiedDate":"2021-01-15T15:40:54.669083","indexId":"70190459","displayToPublicDate":"2010-06-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1727,"text":"GSA Special Papers","active":true,"publicationSubtype":{"id":10}},"title":"Geologic map of Lake Mead and surrounding regions, southern Nevada, southwestern Utah, and northwestern Arizona","docAbstract":"<p>Regional stratigraphic units and structural features of the Lake Mead region are presented as a 1:250,000 scale map, and as a Geographic Information System database. The map, which was compiled from existing geologic maps of various scales, depicts geologic units, bedding and foliation attitudes, faults and folds. Units and structural features were generalized to highlight the regional stratigraphic and tectonic aspects of the geology of the Lake Mead region. This map was prepared in support of the papers presented in this volume, Special Paper 463, as well as to facilitate future investigations in the region.</p><p>Stratigraphic units exposed within the area record 1800 million years of geologic history and include Proterozoic crystalline rocks, Paleozoic and Mesozoic sedimentary rocks, Mesozoic plutonic rocks, Cenozoic volcanic and intrusive rocks, sedimentary rocks and surficial deposits. Following passive margin sedimentation in the Paleozoic and Mesozoic, late Mesozoic (Sevier) thrusting and Late Cretaceous and early Tertiary compression produced major folding, reverse faulting, and thrust faulting in the Basin and Range, and resulted in regional uplift and monoclinal folding in the Colorado Plateau. Cenozoic extensional deformation, accompanied by sedimentation and volcanism, resulted in large-magnitude high- and low-angle normal faulting and strike-slip faulting in the Basin and Range; on the Colorado Plateau, extension produced north-trending high-angle normal faults. The latest history includes integration of the Colorado River system, dissection, development of alluvial fans, extensive pediment surfaces, and young faulting.</p><p>Stratigraphic units exposed within the area record 1800 million years of geologic history and include Proterozoic crystalline rocks, Paleozoic and Mesozoic sedimentary rocks, Mesozoic plutonic rocks, Cenozoic volcanic and intrusive rocks, sedimentary rocks and surfi cial deposits. Following passive margin sedimentation in the Paleozoic and Mesozoic, late Mesozoic (Sevier) thrusting and Late Cretaceous and early Tertiary compression produced major folding, reverse faulting, and thrust faulting in the Basin and Range, and resulted in regional uplift and monoclinal folding in the Colorado Plateau. Cenozoic extensional deformation, accompanied by sedimentation and volcanism, resulted in large-magnitude high- and low-angle normal faulting and strike-slip faulting in the Basin and Range; on the Colorado Plateau, extension produced north-trending high-angle normal faults. The latest history includes integration of the Colorado River system, dissection, development of alluvial fans, extensive pediment surfaces, and young faulting.</p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/2010.2463(02)","usgsCitation":"Felger, T.J., and Beard, S., 2010, Geologic map of Lake Mead and surrounding regions, southern Nevada, southwestern Utah, and northwestern Arizona: GSA Special Papers, v. 463, p. 29-39, https://doi.org/10.1130/2010.2463(02).","productDescription":"11 p.","startPage":"29","endPage":"39","ipdsId":"IP-013188","costCenters":[{"id":309,"text":"Geology and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":382222,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Arizona, Nevada, Utah","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -119.13574218749999,\n              34.361576287484176\n            ],\n            [\n              -111.005859375,\n              34.361576287484176\n            ],\n            [\n              -111.005859375,\n              39.21523130910491\n            ],\n            [\n              -119.13574218749999,\n              39.21523130910491\n            ],\n            [\n              -119.13574218749999,\n              34.361576287484176\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"463","publishingServiceCenter":{"id":14,"text":"Menlo Park PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"59afb7a0e4b0e9bde1351149","contributors":{"authors":[{"text":"Felger, Tracey J. 0000-0003-0841-4235 tfelger@usgs.gov","orcid":"https://orcid.org/0000-0003-0841-4235","contributorId":1117,"corporation":false,"usgs":true,"family":"Felger","given":"Tracey","email":"tfelger@usgs.gov","middleInitial":"J.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":709268,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Beard, Sue 0000-0001-9552-1893 sbeard@usgs.gov","orcid":"https://orcid.org/0000-0001-9552-1893","contributorId":167711,"corporation":false,"usgs":true,"family":"Beard","given":"Sue","email":"sbeard@usgs.gov","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":709267,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70173541,"text":"70173541 - 2010 - Patch dynamics and the timing of colonization-abandonment events by male Kirtland’s Warblers in an early succession habitat","interactions":[],"lastModifiedDate":"2021-03-31T15:00:34.272554","indexId":"70173541","displayToPublicDate":"2010-06-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1015,"text":"Biological Conservation","active":true,"publicationSubtype":{"id":10}},"title":"Patch dynamics and the timing of colonization-abandonment events by male Kirtland’s Warblers in an early succession habitat","docAbstract":"<p><span>Habitat colonization and abandonment affects the distribution of a species in space and time, ultimately influencing the duration of time habitat is used and the total area of habitat occupied in any given year. Both aspects have important implications to long-term conservation planning. The importance of patch isolation and area to colonization–extinction events is well studied, but little information exists on how changing regional landscape structure and population dynamics influences the variability in the timing of patch colonization and abandonment events. We used 26</span><span>&nbsp;</span><span>years of Kirtland’s Warbler (</span><i>Dendroica kirtlandii</i><span>) population data taken during a habitat restoration program (1979–2004) across its historical breeding range to examine the influence of patch attributes and temporal large-scale processes, specifically the rate of habitat turnover and fraction of occupied patches, on the year-to-year timing of patch colonization and abandonment since patch origin. We found the timing of patch colonization and abandonment was influenced by patch and large-scale regional factors. In this system, larger patches were typically colonized earlier (i.e., at a younger age) and abandoned later than smaller patches. Isolated patches (i.e., patches farther from another occupied patch) were generally colonized later and abandoned earlier. Patch habitat type affected colonization and abandonment; colonization occurred at similar patch ages between plantation and wildfire areas (9 and 8.5</span><span>&nbsp;</span><span>years, respectively), but plantations were abandoned at earlier ages (13.9</span><span>&nbsp;</span><span>years) than wildfire areas (16.4</span><span>&nbsp;</span><span>years) resulting in shorter use. As the fraction of occupied patches increased, patches were colonized and abandoned at earlier ages. Patches were abandoned at older ages when the influx of new habitat patches was at low and high rates. Our results provide empirical support for the temporal influence of patch dynamics (i.e., patch destruction, creation, and succession) on local colonization and extinction processes that help explain large-scale patterns of habitat occupancy. Results highlight the need for practitioners to consider the timing of habitat restoration as well as total amount and spatial arrangement of habitat to sustain populations.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.biocon.2010.02.023","usgsCitation":"Donner, D.M., Ribic, C., and Probst, J.R., 2010, Patch dynamics and the timing of colonization-abandonment events by male Kirtland’s Warblers in an early succession habitat: Biological Conservation, v. 143, no. 5, p. 1159-1167, https://doi.org/10.1016/j.biocon.2010.02.023.","productDescription":"9 p.","startPage":"1159","endPage":"1167","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-016822","costCenters":[{"id":199,"text":"Coop Res Unit Leetown","active":true,"usgs":true}],"links":[{"id":324008,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"143","issue":"5","publishingServiceCenter":{"id":9,"text":"Reston PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"576913e2e4b07657d19ff206","contributors":{"authors":[{"text":"Donner, Deahn M.","contributorId":171823,"corporation":false,"usgs":false,"family":"Donner","given":"Deahn","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":638797,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ribic, Christine 0000-0003-2583-1778 caribic@usgs.gov","orcid":"https://orcid.org/0000-0003-2583-1778","contributorId":147952,"corporation":false,"usgs":true,"family":"Ribic","given":"Christine","email":"caribic@usgs.gov","affiliations":[{"id":199,"text":"Coop Res Unit Leetown","active":true,"usgs":true},{"id":5068,"text":"Midwest Regional Director's Office","active":true,"usgs":true}],"preferred":true,"id":637280,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Probst, John R.","contributorId":171826,"corporation":false,"usgs":false,"family":"Probst","given":"John","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":638798,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70192601,"text":"70192601 - 2010 - Locations and magnitudes of historical earthquakes in the Sierra of Ecuador (1587–1996)","interactions":[],"lastModifiedDate":"2017-10-31T14:01:26","indexId":"70192601","displayToPublicDate":"2010-06-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1803,"text":"Geophysical Journal International","active":true,"publicationSubtype":{"id":10}},"title":"Locations and magnitudes of historical earthquakes in the Sierra of Ecuador (1587–1996)","docAbstract":"<p><span>The whole territory of Ecuador is exposed to seismic hazard. Great earthquakes can occur in the subduction zone (e.g. Esmeraldas, 1906,&nbsp;</span><i>M</i><sub>w</sub><span>8.8), whereas lower magnitude but shallower and potentially more destructive earthquakes can occur in the highlands. This study focuses on the historical crustal earthquakes of the Andean Cordillera. Several large cities are located in the Interandean Valley, among them Quito, the capital (∼2.5 millions inhabitants). A total population of ∼6 millions inhabitants currently live in the highlands, raising the seismic risk. At present, precise instrumental data for the Ecuadorian territory is not available for periods earlier than 1990 (beginning date of the revised instrumental Ecuadorian seismic catalogue); therefore historical data are of utmost importance for assessing seismic hazard. In this study, the Bakun &amp; Wentworth method is applied in order to determine magnitudes, locations, and associated uncertainties for historical earthquakes of the Sierra over the period 1587–1976. An intensity-magnitude equation is derived from the four most reliable instrumental earthquakes (</span><i>M</i><sub>w</sub><span>between 5.3 and 7.1). Intensity data available per historical earthquake vary between 10 (Quito, 1587, Intensity ≥VI) and 117 (Riobamba, 1797, Intensity ≥III). The bootstrap resampling technique is coupled to the B&amp;W method for deriving geographical confidence contours for the intensity centre depending on the data set of each earthquake, as well as confidence intervals for the magnitude. The extension of the area delineating the intensity centre location at the 67 per cent confidence level (±1σ) depends on the amount of intensity data, on their internal coherence, on the number of intensity degrees available, and on their spatial distribution. Special attention is dedicated to the few earthquakes described by intensities reaching IX, X and XI degrees. Twenty-five events are studied, and nineteen new epicentral locations are obtained, yielding equivalent moment magnitudes between 5.0 and 7.6. Large earthquakes seem to be related to strike slip faults between the North Andean Block and stable South America to the east, while moderate earthquakes (</span><i>M</i><sub>w</sub><span>≤ 6) seem to be associated with to thrust faults located on the western internal slopes of the Interandean Valley.</span></p>","language":"English","publisher":"Oxford Academic","doi":"10.1111/j.1365-246X.2010.04569.x","usgsCitation":"Beauval, C., Yepes, H., Bakun, W.H., Egred, J., Alvarado, A., and Singaucho, J., 2010, Locations and magnitudes of historical earthquakes in the Sierra of Ecuador (1587–1996): Geophysical Journal International, v. 181, no. 3, p. 1613-1633, https://doi.org/10.1111/j.1365-246X.2010.04569.x.","productDescription":"21 p.","startPage":"1613","endPage":"1633","ipdsId":"IP-016703","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"links":[{"id":475719,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1111/j.1365-246x.2010.04569.x","text":"Publisher Index Page"},{"id":347879,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Ecuador","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -79.65087890624999,\n              -2.7345569512697794\n            ],\n            [\n              -77.135009765625,\n              -2.7345569512697794\n            ],\n            [\n              -77.135009765625,\n              1.2962761196418218\n            ],\n            [\n              -79.65087890624999,\n              1.2962761196418218\n            ],\n            [\n              -79.65087890624999,\n              -2.7345569512697794\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"181","issue":"3","publishingServiceCenter":{"id":14,"text":"Menlo Park PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"59f98bc3e4b0531197afa096","contributors":{"authors":[{"text":"Beauval, Celine","contributorId":198594,"corporation":false,"usgs":false,"family":"Beauval","given":"Celine","email":"","affiliations":[],"preferred":false,"id":718627,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Yepes, Hugo","contributorId":54463,"corporation":false,"usgs":true,"family":"Yepes","given":"Hugo","affiliations":[],"preferred":false,"id":718628,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bakun, William H.","contributorId":39361,"corporation":false,"usgs":true,"family":"Bakun","given":"William","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":718629,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Egred, Jose","contributorId":198596,"corporation":false,"usgs":false,"family":"Egred","given":"Jose","email":"","affiliations":[],"preferred":false,"id":718630,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Alvarado, Alexandra","contributorId":21416,"corporation":false,"usgs":true,"family":"Alvarado","given":"Alexandra","email":"","affiliations":[],"preferred":false,"id":718631,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Singaucho, Juan-Carlos","contributorId":198597,"corporation":false,"usgs":false,"family":"Singaucho","given":"Juan-Carlos","email":"","affiliations":[],"preferred":false,"id":718632,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70147317,"text":"ds505 - 2010 - Chesapeake bay watershed land cover data series","interactions":[],"lastModifiedDate":"2021-07-02T14:06:36.853932","indexId":"ds505","displayToPublicDate":"2010-06-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":310,"text":"Data Series","code":"DS","onlineIssn":"2327-638X","printIssn":"2327-0271","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"505","title":"Chesapeake bay watershed land cover data series","docAbstract":"<p>To better understand how the land is changing and to relate those changes to water quality trends, the USGS EGSC funded the production of a Chesapeake Bay Watershed Land Cover Data Series (CBLCD) representing four dates: 1984, 1992, 2001, and 2006. EGSC will publish land change forecasts based on observed trends in the CBLCD over the coming year. They are in the process of interpreting and publishing statistics on the extent, type and patterns of land cover change for 1984-2006 in the Bay watershed, major tributaries and counties.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ds505","usgsCitation":"Irani, F., and Claggett, P.R., 2010, Chesapeake bay watershed land cover data series: U.S. Geological Survey Data Series 505, Report: PowerPoint, 4 p.; Data, https://doi.org/10.3133/ds505.","productDescription":"Report: PowerPoint, 4 p.; Data","numberOfPages":"4","onlineOnly":"Y","additionalOnlineFiles":"Y","temporalStart":"1984-01-01","temporalEnd":"2006-12-31","costCenters":[{"id":242,"text":"Eastern Geographic Science Center","active":true,"usgs":true}],"links":[{"id":299953,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":299952,"rank":4,"type":{"id":7,"text":"Companion 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Water Science Center","active":true,"usgs":true}],"preferred":true,"id":545751,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70175137,"text":"70175137 - 2010 - Taqman Real-Time PCR Detects <i>Avipoxvirus</i> DNA in Blood of Hawaìi `Amakihi (<i>Hemignathus virens</i>)","interactions":[],"lastModifiedDate":"2018-01-04T12:54:20","indexId":"70175137","displayToPublicDate":"2010-05-27T14:30:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2980,"text":"PLoS ONE","active":true,"publicationSubtype":{"id":10}},"title":"Taqman Real-Time PCR Detects <i>Avipoxvirus</i> DNA in Blood of Hawaìi `Amakihi (<i>Hemignathus virens</i>)","docAbstract":"<h3>Background</h3>\n<p><i>Avipoxvirus</i>&nbsp;sp. is a significant threat to endemic bird populations on several groups of islands worldwide, including Hawa&igrave;i, the Galapagos Islands, and the Canary Islands. Accurate identification and genotyping of&nbsp;<i>Avipoxvirus</i>&nbsp;is critical to the study of this disease and how it interacts with other pathogens, but currently available methods rely on invasive sampling of pox-like lesions and may be especially harmful in smaller birds.</p>\n<h3>Methodology/Principal Findings</h3>\n<p>Here, we present a nested TaqMan Real-Time PCR for the detection of the&nbsp;<i>Avipoxvirus</i>&nbsp;4b core protein gene in archived blood samples from Hawaiian birds. The method was successful in amplifying&nbsp;<i>Avipoxvirus</i>&nbsp;DNA from packed blood cells of one of seven Hawaiian honeycreepers with confirmed&nbsp;<i>Avipoxvirus</i>&nbsp;infections and 13 of 28 Hawa&igrave;i `amakihi (<i>Hemignathus virens</i>) with suspected&nbsp;<i>Avipoxvirus</i>&nbsp;infections based on the presence of pox-like lesions. Mixed genotype infections have not previously been documented in Hawa&igrave;i but were observed in two individuals in this study.</p>\n<h3>Conclusions/Significance</h3>\n<p>We anticipate that this method will be applicable to other closely related strains of&nbsp;<i>Avipoxvirus&nbsp;</i>and will become an important and useful tool in global studies of the epidemiology of&nbsp;<i>Avipoxvirus</i>.</p>","language":"English","publisher":"PLoS","doi":"10.1371/journal.pone.0010745","usgsCitation":"Farias, M.E., LaPointe, D., Atkinson, C.T., Czerwonka, C., Shrestha, R., and Jarvi, S.I., 2010, Taqman Real-Time PCR Detects <i>Avipoxvirus</i> DNA in Blood of Hawaìi `Amakihi (<i>Hemignathus virens</i>): PLoS ONE, v. 5, no. 5, p. 1-6, https://doi.org/10.1371/journal.pone.0010745.","productDescription":"6 p.","startPage":"1","endPage":"6","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-017575","costCenters":[{"id":521,"text":"Pacific Island Ecosystems Research Center","active":false,"usgs":true}],"links":[{"id":475721,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1371/journal.pone.0010745","text":"Publisher Index Page"},{"id":325858,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Ecuador, Spain, United States","state":"Hawaii","otherGeospatial":"Canary Islands, Galapagos Islands","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -154.51171875,\n              19.766703551716976\n            ],\n            [\n              -156.29150390625,\n              21.53484700204879\n            ],\n            [\n              -157.8955078125,\n              22.248428704383624\n            ],\n            [\n              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Center","active":true,"usgs":true}],"preferred":false,"id":644075,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Atkinson, C. T.","contributorId":24296,"corporation":false,"usgs":true,"family":"Atkinson","given":"C.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":644076,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Czerwonka, Christopher","contributorId":173284,"corporation":false,"usgs":false,"family":"Czerwonka","given":"Christopher","email":"","affiliations":[],"preferred":false,"id":644077,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Shrestha, Rajesh","contributorId":173288,"corporation":false,"usgs":false,"family":"Shrestha","given":"Rajesh","email":"","affiliations":[],"preferred":false,"id":644078,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Jarvi, Susan I.","contributorId":47748,"corporation":false,"usgs":true,"family":"Jarvi","given":"Susan","email":"","middleInitial":"I.","affiliations":[],"preferred":false,"id":644079,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70201010,"text":"70201010 - 2010 - The construction of Chasma Boreale on Mars","interactions":[],"lastModifiedDate":"2018-11-20T16:36:05","indexId":"70201010","displayToPublicDate":"2010-05-27T10:43:24","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2840,"text":"Nature","active":true,"publicationSubtype":{"id":10}},"title":"The construction of Chasma Boreale on Mars","docAbstract":"<p><span>The polar layered deposits of Mars contain the planet’s largest known reservoir of water ice</span><sup>1,2</sup><span>&nbsp;and the prospect of revealing a detailed Martian palaeoclimate record</span><sup>3,4</sup><span>, but the mechanisms responsible for the formation of the dominant features of the north polar layered deposits (NPLD) are unclear, despite decades of debate. Stratigraphic analyses of the exposed portions of Chasma Boreale—a large canyon 500 km long, up to 100 km wide, and nearly 2 km deep—have led most researchers to favour an erosional process for its formation following initial NPLD accumulation. Candidate mechanisms include the catastrophic outburst of water</span><sup>5</sup><span>, protracted basal melting</span><sup>6</sup><span>, erosional undercutting</span><sup>7</sup><span>, aeolian downcutting</span><sup>7,8,9</sup><span>&nbsp;and a combination of these processes</span><sup>10</sup><span>. Here we use new data from the Mars Reconnaissance Orbiter to show that Chasma Boreale is instead a long-lived, complex feature resulting primarily from non-uniform accumulation of the NPLD. The initial valley that later became Chasma Boreale was matched by a second, equally large valley that was completely filled in by subsequent deposition, leaving no evidence on the surface to indicate its former presence. We further demonstrate that topography existing before the NPLD began accumulating influenced successive episodes of deposition and erosion, resulting in most of the present-day topography. Long-term and large-scale patterns of mass balance achieved through sedimentary processes, rather than catastrophic events, ice flow or highly focused erosion, have produced the largest geomorphic anomaly in the north polar ice of Mars.</span></p>","language":"English","publisher":"Nature","doi":"10.1038/nature09050","usgsCitation":"Holt, J., Fishbaugh, K.E., Byrne, S., Christian, S., Tanaka, K.L., Russell, P., Herkenhoff, K.E., Safaeinili, A., Putzig, N.E., and Phillips, R., 2010, The construction of Chasma Boreale on Mars: Nature, v. 465, p. 446-449, https://doi.org/10.1038/nature09050.","productDescription":"4 p.","startPage":"446","endPage":"449","costCenters":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"links":[{"id":359599,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"465","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5bf52b6be4b045bfcae28022","contributors":{"authors":[{"text":"Holt, J.W.","contributorId":74121,"corporation":false,"usgs":true,"family":"Holt","given":"J.W.","email":"","affiliations":[],"preferred":false,"id":751684,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fishbaugh, Kathryn E.","contributorId":210540,"corporation":false,"usgs":false,"family":"Fishbaugh","given":"Kathryn","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":751685,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Byrne, S.","contributorId":105083,"corporation":false,"usgs":true,"family":"Byrne","given":"S.","email":"","affiliations":[],"preferred":false,"id":751686,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Christian, S.","contributorId":210753,"corporation":false,"usgs":false,"family":"Christian","given":"S.","email":"","affiliations":[{"id":13127,"text":"Jackson School of Geosciences, University of Texas, Austin","active":true,"usgs":false}],"preferred":false,"id":751687,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Tanaka, Kenneth L. ktanaka@usgs.gov","contributorId":610,"corporation":false,"usgs":true,"family":"Tanaka","given":"Kenneth","email":"ktanaka@usgs.gov","middleInitial":"L.","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":true,"id":751688,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Russell, P.S.","contributorId":100987,"corporation":false,"usgs":true,"family":"Russell","given":"P.S.","email":"","affiliations":[],"preferred":false,"id":751689,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Herkenhoff, Kenneth E. 0000-0002-3153-6663 kherkenhoff@usgs.gov","orcid":"https://orcid.org/0000-0002-3153-6663","contributorId":2275,"corporation":false,"usgs":true,"family":"Herkenhoff","given":"Kenneth","email":"kherkenhoff@usgs.gov","middleInitial":"E.","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":true,"id":751690,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Safaeinili, A.","contributorId":98025,"corporation":false,"usgs":true,"family":"Safaeinili","given":"A.","affiliations":[],"preferred":false,"id":751691,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Putzig, Nathaniel E. 0000-0003-4485-6321","orcid":"https://orcid.org/0000-0003-4485-6321","contributorId":208684,"corporation":false,"usgs":true,"family":"Putzig","given":"Nathaniel","email":"","middleInitial":"E.","affiliations":[{"id":13179,"text":"Planetary Science Institute","active":true,"usgs":false}],"preferred":false,"id":751692,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Phillips, R.J.","contributorId":93174,"corporation":false,"usgs":true,"family":"Phillips","given":"R.J.","email":"","affiliations":[],"preferred":false,"id":751693,"contributorType":{"id":1,"text":"Authors"},"rank":10}]}}
,{"id":70210254,"text":"70210254 - 2010 - Bayesian estimation of weak material dispersion: Theory and experiment","interactions":[],"lastModifiedDate":"2020-05-27T12:10:47.152531","indexId":"70210254","displayToPublicDate":"2010-05-26T14:37:47","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5953,"text":"Optics Express","active":true,"publicationSubtype":{"id":10}},"title":"Bayesian estimation of weak material dispersion: Theory and experiment","docAbstract":"<p>This work considers the estimation of dispersion in materials via an interferometric technique. At its core, the problem involves extracting the quadratic variation in phase over a range of wavelengths based on measured optical intensity. The estimation problem becomes extremely difficult for weakly dispersive materials where the quadratic nonlinearity is very small relative to the uncertainty inherent in experiment. This work provides a means of estimating dispersion in the face of such uncertainty. Specifically, we use a Markov Chain Monte Carlo implementation of Bayesian analysis to provide both the dispersion estimate and the associated confidence interval. The interplay between various system parameters and the size of the resulting confidence interval is discussed. The approach is then applied to several different experimental samples.</p>","language":"English","publisher":"Optical Society of America","doi":"10.1364/OE.18.002076","usgsCitation":"Nichols, J., Currie, M., Bucholtz, F., and Link, W.A., 2010, Bayesian estimation of weak material dispersion: Theory and experiment: Optics Express, v. 18, no. 3, p. 2076-2089, https://doi.org/10.1364/OE.18.002076.","productDescription":"14 p.","startPage":"2076","endPage":"2089","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":475722,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1364/oe.18.002076","text":"Publisher Index Page"},{"id":375040,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"18","issue":"3","noUsgsAuthors":false,"publicationDate":"2010-01-19","publicationStatus":"PW","contributors":{"authors":[{"text":"Nichols, J.M.","contributorId":18080,"corporation":false,"usgs":true,"family":"Nichols","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":789771,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Currie, M.","contributorId":224943,"corporation":false,"usgs":false,"family":"Currie","given":"M.","email":"","affiliations":[{"id":16692,"text":"Naval Research Laboratory","active":true,"usgs":false}],"preferred":false,"id":789772,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bucholtz, F.","contributorId":224944,"corporation":false,"usgs":false,"family":"Bucholtz","given":"F.","email":"","affiliations":[{"id":16692,"text":"Naval Research Laboratory","active":true,"usgs":false}],"preferred":false,"id":789773,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Link, William A. 0000-0002-9913-0256 wlink@usgs.gov","orcid":"https://orcid.org/0000-0002-9913-0256","contributorId":146920,"corporation":false,"usgs":true,"family":"Link","given":"William","email":"wlink@usgs.gov","middleInitial":"A.","affiliations":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"preferred":true,"id":789774,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70210253,"text":"70210253 - 2010 - Comparative analysis of Mourning Dove population change in North America","interactions":[],"lastModifiedDate":"2020-05-27T12:11:47.772599","indexId":"70210253","displayToPublicDate":"2010-05-26T14:00:55","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2508,"text":"Journal of Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"Comparative analysis of Mourning Dove population change in North America","docAbstract":"<p>Mourning doves (Zenaida macroura) are surveyed in North America with a Call-Count Survey (CCS) and the North American Breeding Bird Survey (BBS). Analyses in recent years have identified inconsistencies in results between surveys, and a need exists to analyze the surveys using modern methods and examine possible causes of differences in survey results. Call-Count Survey observers collect separate information on number of doves heard and number of doves seen during counting, whereas BBS observers record one index containing all doves observed. We used hierarchical log-linear models to estimate trend and annual indices of abundance for 1966–2007 from BBS data, CCS-heard data, and CCS-seen data. Trend estimates from analyses provided inconsistent results for several states and for eastern and central dovemanagement units. We examined differential effects of change in land use and noise-related disturbance on the CCS indices. Changes in noiserelated disturbance along CCS routes had a larger influence on the heard index than on the seen index, but association analyses among states of changes in temperature and of amounts of developed land suggest that CCS indices are differentially influenced by changes in these environmental features. Our hierarchical model should be used to estimate population change from dove surveys, because it provides an efficient framework for estimating population trends from dove indices while controlling for environmental features that differentially influence the indices.</p>","language":"English","publisher":"BioOne","doi":"10.2193/2008-459","usgsCitation":"Sauer, J.R., Link, W.A., Kendall, W.L., and Dolton, D., 2010, Comparative analysis of Mourning Dove population change in North America: Journal of Wildlife Management, v. 74, no. 5, p. 1059-1069, https://doi.org/10.2193/2008-459.","productDescription":"11 p.","startPage":"1059","endPage":"1069","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":375039,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"74","issue":"5","noUsgsAuthors":false,"publicationDate":"2010-12-13","publicationStatus":"PW","contributors":{"authors":[{"text":"Sauer, John R. 0000-0002-4557-3019 jrsauer@usgs.gov","orcid":"https://orcid.org/0000-0002-4557-3019","contributorId":146917,"corporation":false,"usgs":true,"family":"Sauer","given":"John","email":"jrsauer@usgs.gov","middleInitial":"R.","affiliations":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"preferred":true,"id":789767,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Link, William A. 0000-0002-9913-0256 wlink@usgs.gov","orcid":"https://orcid.org/0000-0002-9913-0256","contributorId":146920,"corporation":false,"usgs":true,"family":"Link","given":"William","email":"wlink@usgs.gov","middleInitial":"A.","affiliations":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"preferred":true,"id":789768,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kendall, William L. 0000-0003-0084-9891","orcid":"https://orcid.org/0000-0003-0084-9891","contributorId":204844,"corporation":false,"usgs":true,"family":"Kendall","given":"William","email":"","middleInitial":"L.","affiliations":[{"id":200,"text":"Coop Res Unit Seattle","active":true,"usgs":true}],"preferred":true,"id":789769,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Dolton, David D.","contributorId":100452,"corporation":false,"usgs":true,"family":"Dolton","given":"David D.","affiliations":[],"preferred":false,"id":789770,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":98414,"text":"ofr20081099 - 2010 - Gulf of Mexico dead zone - 1000 year record","interactions":[],"lastModifiedDate":"2014-04-10T15:11:02","indexId":"ofr20081099","displayToPublicDate":"2010-05-26T07:00:00","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":"2008-1099","title":"Gulf of Mexico dead zone - 1000 year record","docAbstract":"<p>An area of oxygen-depleted bottom- and subsurfacewater (hypoxia = dissolved oxygen < 2 mg per Liter) occurs seasonally on the Louisiana shelf near the Mississippi River. The area of hypoxia, also known as the 'dead zone,' forms when spring and early summer freshwater flow from the Mississippi River supplies a large amount of nutrients to the shelf while creating a freshwater lens, or cap, above the shelf water. The excess nutrients cause phytoplankton blooms in the shallow shelf water. After the bloom ceases, the organic material sinks in the water column and uses up oxygen during decomposition. Thus, the subsurface waters become oxygen depleted. The seasonal dead zone exists until a reduction in freshwater flow, or overturning by storms, allows mixing of the water column to restore normal oxygen conditions.</p>\n<br/>\n<p>Since systematic measurement of the extent of the dead zone was begun in 1985, the overall pattern indicates that the area of the dead zone is increasing. Several studies have concluded that the expansion of the Louisiana shelf dead zone is related to increased nutrients (primarily nitrogen, but possibly also phosphorous) in the Mississippi River drainage basin and is responsible for the degradation of Gulf of Mexico marine habitats. The goal of this research is to augment information on the recent expansion of Louisiana shelf hypoxia and to investigate the temporal and geographic extent of the lowoxygen bottom-water conditions prior to 1985 in sediment cores collected from the Louisiana shelf.</p>\n<br/>\n<p>We use a specific low-oxygen faunal proxy termed the PEB index based on the cumulative percentage of three foraminifers (= % Protononion atlanticum, + % Epistominella vitrea, + % Buliminella morgani) that has been shown statistically to represent the modern seasonal Louisiana hypoxia zone. Our hypothesis is that the increased relative abundance of PEB species in dated sediment cores accurately tracks past seasonal low-oxygen conditions on the Louisiana shelf.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20081099","usgsCitation":"Osterman, L., Poore, R., and Swarzenski, P., 2010, Gulf of Mexico dead zone - 1000 year record: U.S. Geological Survey Open-File Report 2008-1099, 2 p., https://doi.org/10.3133/ofr20081099.","productDescription":"2 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":118466,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr_2008_1099.jpg"},{"id":13666,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2008/1099/","linkFileType":{"id":5,"text":"html"}}],"country":"Mexico","otherGeospatial":"Gulf Of Mexico","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -93.5,28.5 ], [ -93.5,29.5 ], [ -89.5,29.5 ], [ -89.5,28.5 ], [ -93.5,28.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db64a242","contributors":{"authors":[{"text":"Osterman, L.E.","contributorId":53836,"corporation":false,"usgs":true,"family":"Osterman","given":"L.E.","email":"","affiliations":[],"preferred":false,"id":305239,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Poore, R.Z.","contributorId":35314,"corporation":false,"usgs":true,"family":"Poore","given":"R.Z.","email":"","affiliations":[],"preferred":false,"id":305238,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Swarzenski, P.W. 0000-0003-0116-0578","orcid":"https://orcid.org/0000-0003-0116-0578","contributorId":29487,"corporation":false,"usgs":true,"family":"Swarzenski","given":"P.W.","affiliations":[],"preferred":false,"id":305237,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":98413,"text":"ofr20071024 - 2010 - Biological, Physical and Chemical Data From Gulf of Mexico Gravity and Box Core MRD05-04","interactions":[],"lastModifiedDate":"2012-02-02T00:14:44","indexId":"ofr20071024","displayToPublicDate":"2010-05-26T00:00:00","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":"2007-1024","title":"Biological, Physical and Chemical Data From Gulf of Mexico Gravity and Box Core MRD05-04","docAbstract":"This paper presents the benthic foraminiferal census data, magnetic susceptibility measurements, vanadium and organic geochemistry (carbon isotope, sterols, and total organic carbon) data from the MRD05-04 gravity and box cores. The MRD05-04 cores were obtained from the Louisiana continental shelf in an on-going initiative to examine the geographic and temporal extent of hypoxia, low-oxygen bottom-water content, and geochemical transport. The development of low-oxygen bottom water conditions in coastal waters is dependent upon a new source of bio-available nutrients introduced into a well-stratified water column. A number of studies have concluded that the development of the current seasonal hypoxia (dissolved oxygen < 2 mg L-1) in subsurface waters of the northern Gulf of Mexico is related to increased transport of nutrients (primarily nitrogen, but possibly also phosphorous) by the Mississippi River. However, the development of earlier episodes of seasonal low-oxygen subsurface water on the Louisiana shelf may be related to Mississippi River discharge.\r\n","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20071024","usgsCitation":"Osterman, L.E., Campbell, P.L., Swarzenski, P.W., and Ricardo, J.P., 2010, Biological, Physical and Chemical Data From Gulf of Mexico Gravity and Box Core MRD05-04: U.S. Geological Survey Open-File Report 2007-1024, 18 p., https://doi.org/10.3133/ofr20071024.","productDescription":"18 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":118464,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr_2007_1024.jpg"},{"id":13665,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2007/1024/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a48e4b07f02db623379","contributors":{"authors":[{"text":"Osterman, Lisa E. osterman@usgs.gov","contributorId":3058,"corporation":false,"usgs":true,"family":"Osterman","given":"Lisa","email":"osterman@usgs.gov","middleInitial":"E.","affiliations":[{"id":574,"text":"St. Petersburg Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":305234,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Campbell, Pamela L.","contributorId":76719,"corporation":false,"usgs":true,"family":"Campbell","given":"Pamela","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":305236,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Swarzenski, Peter W. 0000-0003-0116-0578 pswarzen@usgs.gov","orcid":"https://orcid.org/0000-0003-0116-0578","contributorId":1070,"corporation":false,"usgs":true,"family":"Swarzenski","given":"Peter","email":"pswarzen@usgs.gov","middleInitial":"W.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":305233,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ricardo, John P.","contributorId":73307,"corporation":false,"usgs":true,"family":"Ricardo","given":"John","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":305235,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
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