{"pageNumber":"2461","pageRowStart":"61500","pageSize":"25","recordCount":184660,"records":[{"id":70029293,"text":"70029293 - 2006 - Active dust devils in Gusev crater, Mars: Observations from the Mars Exploration Rover Spirit","interactions":[],"lastModifiedDate":"2012-03-12T17:20:51","indexId":"70029293","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2317,"text":"Journal of Geophysical Research E: Planets","active":true,"publicationSubtype":{"id":10}},"title":"Active dust devils in Gusev crater, Mars: Observations from the Mars Exploration Rover Spirit","docAbstract":"A full dust devil \"season\" was observed from Spirit from 10 March 2005 (sol 421, first active dust devil observed) to 12 December 2005 (sol 691, last dust devil seen); this corresponds to the period Ls 173.2?? to 339.5??, or the southern spring and summer on Mars. Thermal Emission Spectrometer data suggest a correlation between high surface temperatures and a positive thermal gradient with active dust devils in Gusev and that Spirit landed in the waning stages of a dust devil season as temperatures decreased. 533 active dust devils were observed, enabling new characterizations; they ranged in diameter from 2 to 276 m, with most in the range of 10-20 m in diameter, and occurred from about 0930 to 1630 hours local true solar time (with the maximum forming around 1300 hours) and a peak occurrence in southern late spring (Ls ??? 250??). Horizontal speeds of the dust devils ranged from <1 to 21 m/s, while vertical wind speeds within the dust devils ranged from 0.2 to 8.8 m/s. These data, when combined with estimates of the dust content within the dust devils, yield dust fluxes of 3.95 ?? 10-9 to 4.59-4 kg/m2/s. Analysis of the dust devil frequency distribution over the inferred dust devil zone within Gusev crater yields ???50 active dust devils/km2/sol, suggesting a dust loading into the atmosphere of ???19 kg/km2/sol. This value is less than one tenth the estimates by Cantor et al. (2001) for regional dust storms on Mars. Copyright 2006 by the American Geophysical Union.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Geophysical Research E: Planets","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1029/2006JE002743","issn":"01480227","usgsCitation":"Greeley, R., Whelley, P., Arvidson, R., Cabrol, N., Foley, D., Franklin, B., Geissler, P., Golombek, M., Kuzmin, R., Landis, G.A., Lemmon, M., Neakrase, L., Squyres, S.W., and Thompson, S., 2006, Active dust devils in Gusev crater, Mars: Observations from the Mars Exploration Rover Spirit: Journal of Geophysical Research E: Planets, v. 111, no. 12, https://doi.org/10.1029/2006JE002743.","costCenters":[],"links":[{"id":477357,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1029/2006je002743","text":"Publisher Index Page"},{"id":237370,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":210449,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1029/2006JE002743"}],"volume":"111","issue":"12","noUsgsAuthors":false,"publicationDate":"2006-12-07","publicationStatus":"PW","scienceBaseUri":"5059e6aae4b0c8380cd47587","contributors":{"authors":[{"text":"Greeley, R.","contributorId":6538,"corporation":false,"usgs":true,"family":"Greeley","given":"R.","email":"","affiliations":[],"preferred":false,"id":422111,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Whelley, P.L.","contributorId":29555,"corporation":false,"usgs":true,"family":"Whelley","given":"P.L.","email":"","affiliations":[],"preferred":false,"id":422114,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Arvidson, R. E.","contributorId":46666,"corporation":false,"usgs":true,"family":"Arvidson","given":"R. E.","affiliations":[],"preferred":false,"id":422118,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Cabrol, N.A.","contributorId":65208,"corporation":false,"usgs":true,"family":"Cabrol","given":"N.A.","email":"","affiliations":[],"preferred":false,"id":422122,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Foley, D.J.","contributorId":83646,"corporation":false,"usgs":true,"family":"Foley","given":"D.J.","email":"","affiliations":[],"preferred":false,"id":422124,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Franklin, B.J.","contributorId":48358,"corporation":false,"usgs":true,"family":"Franklin","given":"B.J.","email":"","affiliations":[],"preferred":false,"id":422119,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Geissler, P.G.","contributorId":41644,"corporation":false,"usgs":true,"family":"Geissler","given":"P.G.","email":"","affiliations":[],"preferred":false,"id":422117,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Golombek, M.P.","contributorId":52696,"corporation":false,"usgs":true,"family":"Golombek","given":"M.P.","email":"","affiliations":[],"preferred":false,"id":422120,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Kuzmin, R.O.","contributorId":14932,"corporation":false,"usgs":true,"family":"Kuzmin","given":"R.O.","email":"","affiliations":[],"preferred":false,"id":422113,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Landis, G. A.","contributorId":76536,"corporation":false,"usgs":true,"family":"Landis","given":"G.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":422123,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Lemmon, M.T.","contributorId":7032,"corporation":false,"usgs":true,"family":"Lemmon","given":"M.T.","email":"","affiliations":[],"preferred":false,"id":422112,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Neakrase, L.D.V.","contributorId":38690,"corporation":false,"usgs":true,"family":"Neakrase","given":"L.D.V.","affiliations":[],"preferred":false,"id":422116,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Squyres, S. W.","contributorId":31836,"corporation":false,"usgs":true,"family":"Squyres","given":"S.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":422115,"contributorType":{"id":1,"text":"Authors"},"rank":13},{"text":"Thompson, S.D.","contributorId":63511,"corporation":false,"usgs":true,"family":"Thompson","given":"S.D.","email":"","affiliations":[],"preferred":false,"id":422121,"contributorType":{"id":1,"text":"Authors"},"rank":14}]}}
,{"id":70029285,"text":"70029285 - 2006 - Real-time seismic monitoring of the integrated cape girardeau bridge array and recorded earthquake response","interactions":[],"lastModifiedDate":"2012-03-12T17:20:49","indexId":"70029285","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Real-time seismic monitoring of the integrated cape girardeau bridge array and recorded earthquake response","docAbstract":"This paper introduces the state of the art, real-time and broad-band seismic monitoring network implemented for the 1206 m [3956 ft] long, cable-stayed Bill Emerson Memorial Bridge in Cape Girardeau (MO), a new Mississippi River crossing, approximately 80 km from the epicentral region of the 1811-1812 New Madrid earthquakes. The bridge was designed for a strong earthquake (magnitude 7.5 or greater) during the design life of the bridge. The monitoring network comprises a total of 84 channels of accelerometers deployed on the superstructure, pier foundations and at surface and downhole free-field arrays of the bridge. The paper also presents the high quality response data obtained from the network. Such data is aimed to be used by the owner, researchers and engineers to assess the performance of the bridge, to check design parameters, including the comparison of dynamic characteristics with actual response, and to better design future similar bridges. Preliminary analyses of ambient and low amplitude small earthquake data reveal specific response characteristics of the bridge and the free-field. There is evidence of coherent tower, cable, deck interaction that sometimes results in amplified ambient motions. Motions at the lowest tri-axial downhole accelerometers on both MO and IL sides are practically free from any feedback from the bridge. Motions at the mid-level and surface downhole accelerometers are influenced significantly by feedback due to amplified ambient motions of the bridge. Copyright ASCE 2006.","largerWorkTitle":"Proceedings of the Structures Congress and Exposition","conferenceTitle":"Structures Congress 2006","conferenceDate":"18 May 2006 through 21 May 2006","conferenceLocation":"St. Louis, MO","language":"English","doi":"10.1061/40889(201)169","usgsCitation":"Çelebi, M., 2006, Real-time seismic monitoring of the integrated cape girardeau bridge array and recorded earthquake response, <i>in</i> Proceedings of the Structures Congress and Exposition, v. 2006, St. Louis, MO, 18 May 2006 through 21 May 2006, https://doi.org/10.1061/40889(201)169.","startPage":"169","costCenters":[],"links":[{"id":210778,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1061/40889(201)169"},{"id":237803,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"2006","noUsgsAuthors":false,"publicationDate":"2012-06-20","publicationStatus":"PW","scienceBaseUri":"505a95b0e4b0c8380cd81b93","contributors":{"authors":[{"text":"Çelebi, M.","contributorId":36946,"corporation":false,"usgs":true,"family":"Çelebi","given":"M.","affiliations":[],"preferred":false,"id":422072,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70194226,"text":"70194226 - 2006 - Taricha granulosa (Rough-skinned newt). Summer habitat and aggregation.","interactions":[],"lastModifiedDate":"2017-11-18T13:22:15","indexId":"70194226","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1898,"text":"Herpetological Review","active":true,"publicationSubtype":{"id":10}},"displayTitle":"<i>Taricha granulosa</i> (Rough-skinned newt). Summer habitat and aggregation.","title":"Taricha granulosa (Rough-skinned newt). Summer habitat and aggregation.","docAbstract":"<p>Terrestrial behavior and habitat associations of post-metamorphic <i>Taricha granulosa </i>are poorly understood (Oliver and McCurdy 1974. Can. J. Zool. 52:541-545; Pimentel 1960. Amer. Midl. Nat. 63:470-496). Chandler (1918. Oregon Agric. Coll. Exper. Sta. Bull. 152:6) referenced Fall T <i>granulosa </i>aggregations in \"cavities under stumps, logs, and stones,\" but does not present specific data. Pimentel <i>(op. cit.) </i>reported that T <i>granulosa </i>constructed burrows in a terrarium and 1-3 adults of both sexes shared burrows for up to three months. Here, I describe two summer aggregations of T <i>granulosa </i>from the Willow Creek Natural Area (WCNA) in the southern Willamette Valley, Oregon, USA. The WCNA includes wetlands (primarily seasonal), prairies, riparian forests of willow <i>(Salix </i>spp.), black cottonwood <i>(Populus trichocarpa), </i>and Oregon ash <i>(Fraxinus latifolia), </i>and patches of upland forest of Oregon white oak <i>(Quercus garryana), </i>California black oak <i>(Quercus kelloggii), </i>and Douglas fir <i>(Pseudotsuga menziesii). Taricha granulosa </i>commonly breed in old stock ponds and beaver impoundments on the site.</p>","language":"English","publisher":"Society for the Study of Reptiles and Amphibians","usgsCitation":"Pearl, C., 2006, Taricha granulosa (Rough-skinned newt). Summer habitat and aggregation.: Herpetological Review, v. 37, no. 1, p. 71-72.","productDescription":"2 p.","startPage":"71","endPage":"72","costCenters":[{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true}],"links":[{"id":349096,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":349095,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://ssarherps.org/herpetological-review-pdfs/"}],"volume":"37","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5a61142de4b06e28e9c25874","contributors":{"authors":[{"text":"Pearl, Christopher A. christopher_pearl@usgs.gov","contributorId":145515,"corporation":false,"usgs":true,"family":"Pearl","given":"Christopher A.","email":"christopher_pearl@usgs.gov","affiliations":[{"id":289,"text":"Forest and Rangeland Ecosys Science Center","active":true,"usgs":true}],"preferred":false,"id":722775,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70179487,"text":"70179487 - 2006 - Distribution of Tui Chub in Cow Head Lake watershed system, Nevada and California","interactions":[],"lastModifiedDate":"2017-01-03T15:45:42","indexId":"70179487","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5250,"text":"California Department of Fish and Game","active":true,"publicationSubtype":{"id":2}},"title":"Distribution of Tui Chub in Cow Head Lake watershed system, Nevada and California","docAbstract":"<p>n/a</p>","language":"English","publisher":"California Department of Fish and Game","usgsCitation":"Scoppettone, G., and Rissler, P., 2006, Distribution of Tui Chub in Cow Head Lake watershed system, Nevada and California: California Department of Fish and Game, v. 92, 7 p. .","productDescription":"7 p. 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,{"id":70194222,"text":"70194222 - 2006 - Trachemys scripta elegans (Red-eared Slider). Reproduction","interactions":[],"lastModifiedDate":"2017-11-18T09:26:07","indexId":"70194222","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1898,"text":"Herpetological Review","active":true,"publicationSubtype":{"id":10}},"displayTitle":"<i>Trachemys scripta elegans</i> (Red-eared Slider). Reproduction","title":"Trachemys scripta elegans (Red-eared Slider). Reproduction","docAbstract":"<p>The natural range of <i>Trachemys scripta elegans</i> is centered in the south-central United States, from Illinois to the Gulf of Mexico. Because of its prominence in the international pet trade, the species now can be found over much of the United States, and its introduction has been documented throughout the world (Ernst et al. 1994. Turtles of the United States and Canada. Smithsonian Institution Press, Washington. 578 pp.). There has been speculation as to whether and where introduced Red-eared Sliders can reproduce in the wild in California (Bury and Luckenbach 1976. Biol. Conserv. 10:1-14). Successful nesting or presumed breeding (i.e., gravid females) in northern California were reported by Bury and Luckenbach (<i>op. cit</i>.) at Clear Lake, by Spinks et al. (2003. Biol. Cons. 113:257-267) at the University of California, Davis, and by Fidenci (2006. Herpetol. Rev. 37:80) in the Mount Tamalpais Watershed, Mann Co. Here, we report additional evidence of reproduction in <i>T. s. elegans</i> in the wild in northern California.</p>","language":"English","publisher":"Society for the Study of Amphibians and Reptiles","usgsCitation":"Bettelheim, M.P., Bury, R.B., Patterson, L.C., and Lubcke, G.M., 2006, Trachemys scripta elegans (Red-eared Slider). Reproduction: Herpetological Review, v. 37, no. 4, p. 459-460.","productDescription":"2 p.","startPage":"459","endPage":"460","costCenters":[{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true}],"links":[{"id":349092,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":349091,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://ssarherps.org/herpetological-review-pdfs/"}],"country":"United States","state":"California","volume":"37","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5a61142de4b06e28e9c25876","contributors":{"authors":[{"text":"Bettelheim, Matthew P.","contributorId":12391,"corporation":false,"usgs":false,"family":"Bettelheim","given":"Matthew","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":722758,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bury, R. Bruce buryb@usgs.gov","contributorId":3660,"corporation":false,"usgs":true,"family":"Bury","given":"R.","email":"buryb@usgs.gov","middleInitial":"Bruce","affiliations":[{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true}],"preferred":false,"id":722759,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Patterson, Laura C.","contributorId":146300,"corporation":false,"usgs":false,"family":"Patterson","given":"Laura","email":"","middleInitial":"C.","affiliations":[{"id":6952,"text":"California Department of Fish and Wildlife","active":true,"usgs":false}],"preferred":false,"id":722760,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lubcke, Glen M.","contributorId":197413,"corporation":false,"usgs":false,"family":"Lubcke","given":"Glen","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":722761,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70045419,"text":"70045419 - 2006 - Michigan Water Year 2005","interactions":[],"lastModifiedDate":"2013-07-09T10:51:50","indexId":"70045419","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":389,"text":"Water Resources Data","active":false,"publicationSubtype":{"id":6}},"seriesNumber":"MI-05-1","title":"Michigan Water Year 2005","docAbstract":"This volume of the annual hydrologic data report of Michigan is one of a series of annual reports that document hydrologic data gathered from the U.S. Geological Survey's surface- and ground-water data-collection networks in each state, Puerto Rico, and the Trust Territories. These records of streamflow, ground-water levels, and quality of water provide the hydrologic information needed by State, local, and Federal agencies, and the private sector for developing and managing our Nation's land and water resources.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Lansing, MI","doi":"10.3133/70045419","collaboration":"Prepared in cooperation with the State of Michigan and with other agencies","usgsCitation":"Blumer, S.P., Whited, C., Ellis, J., Minnerick, R., and LeuVoy, R., 2006, Michigan Water Year 2005: Water Resources Data MI-05-1, xviii, 554 p., https://doi.org/10.3133/70045419.","productDescription":"xviii, 554 p.","numberOfPages":"594","additionalOnlineFiles":"N","temporalStart":"2004-10-01","temporalEnd":"2005-09-30","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":270942,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70045417/report-thumb.jpg"},{"id":272727,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70045417/report.pdf"}],"country":"United States","state":"Michigan","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -90.516667,41.683333 ], [ -90.516667,48.250000 ], [ -82.433333,48.250000 ], [ -82.433333,41.683333 ], [ -90.516667,41.683333 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"516d216ce4b0411d430a8a2d","contributors":{"authors":[{"text":"Blumer, S. P.","contributorId":23938,"corporation":false,"usgs":true,"family":"Blumer","given":"S.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":477471,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Whited, C.R.","contributorId":49387,"corporation":false,"usgs":true,"family":"Whited","given":"C.R.","email":"","affiliations":[],"preferred":false,"id":477473,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ellis, J.M.","contributorId":29502,"corporation":false,"usgs":true,"family":"Ellis","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":477472,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Minnerick, R. J.","contributorId":52255,"corporation":false,"usgs":true,"family":"Minnerick","given":"R. J.","affiliations":[],"preferred":false,"id":477474,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"LeuVoy, R.L.","contributorId":56706,"corporation":false,"usgs":true,"family":"LeuVoy","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":477475,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70194214,"text":"70194214 - 2006 - Emerging concepts for management of river ecosystems and challenges to applied integration of physical and biological sciences in the Pacific Northwest, USA","interactions":[],"lastModifiedDate":"2017-11-17T16:49:19","indexId":"70194214","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3876,"text":"International Journal of River Basin Management","active":true,"publicationSubtype":{"id":10}},"title":"Emerging concepts for management of river ecosystems and challenges to applied integration of physical and biological sciences in the Pacific Northwest, USA","docAbstract":"<p>Integration of biological and physical concepts is necessary to understand and conserve the ecological integrity of river systems. Past attempts at integration have often focused at relatively small scales and on mechanistic models that may not capture the complexity of natural systems leaving substantial uncertainty about ecological responses to management actions. Two solutions have been proposed to guide management in the face of that uncertainty: the use of “natural variability” in key environmental patterns, processes, or disturbance as a reference; and the retention of some areas as essentially unmanaged reserves to conserve and represent as much biological diversity as possible. Both concepts are scale dependent because dominant processes or patterns that might be referenced will change with scale. Context and linkages across scales may be as important in structuring biological systems as conditions within habitats used by individual organisms. Both ideas view the physical environment as a template for expression, maintenance, and evolution of ecological diversity. To conserve or restore a diverse physical template it will be important to recognize the ecologically important differences in physical characteristics and processes among streams or watersheds that we might attempt to mimic in management or represent in conservation or restoration reserves.</p>","language":"English","publisher":"Taylor & Francis","doi":"10.1080/15715124.2006.9635279","usgsCitation":"Rieman, B., Dunham, J.B., and Clayton, J., 2006, Emerging concepts for management of river ecosystems and challenges to applied integration of physical and biological sciences in the Pacific Northwest, USA: International Journal of River Basin Management, v. 4, no. 2, p. 85-97, https://doi.org/10.1080/15715124.2006.9635279.","productDescription":"13 p.","startPage":"85","endPage":"97","costCenters":[{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true}],"links":[{"id":349083,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"4","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5a61142de4b06e28e9c2587c","contributors":{"authors":[{"text":"Rieman, Bruce","contributorId":101140,"corporation":false,"usgs":true,"family":"Rieman","given":"Bruce","affiliations":[],"preferred":false,"id":722719,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dunham, Jason B. 0000-0002-6268-0633 jdunham@usgs.gov","orcid":"https://orcid.org/0000-0002-6268-0633","contributorId":147808,"corporation":false,"usgs":true,"family":"Dunham","given":"Jason","email":"jdunham@usgs.gov","middleInitial":"B.","affiliations":[{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true},{"id":289,"text":"Forest and Rangeland Ecosys Science Center","active":true,"usgs":true},{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"preferred":true,"id":722720,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Clayton, James","contributorId":92879,"corporation":false,"usgs":false,"family":"Clayton","given":"James","email":"","affiliations":[],"preferred":false,"id":722721,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70029299,"text":"70029299 - 2006 - Erosion rates at the Mars Exploration Rover landing sites and long-term climate change on Mars","interactions":[],"lastModifiedDate":"2012-03-12T17:20:51","indexId":"70029299","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2317,"text":"Journal of Geophysical Research E: Planets","active":true,"publicationSubtype":{"id":10}},"title":"Erosion rates at the Mars Exploration Rover landing sites and long-term climate change on Mars","docAbstract":"Erosion rates derived from the Gusev cratered plains and the erosion of weak sulfates by saltating sand at Meridiani Planum are so slow that they argue that the present dry and desiccating environment has persisted since the Early Hesperian. In contrast, sedimentary rocks at Meridiani formed in the presence of groundwater and occasional surface water, and many Columbia Hills rocks at Gusev underwent aqueous alteration during the Late Noachian, approximately coeval with a wide variety of geomorphic indicators that indicate a wetter and likely warmer environment. Two-toned rocks, elevated ventifacts, and perched and undercut rocks indicate localized deflation of the Gusev plains and deposition of an equivalent amount of sediment into craters to form hollows, suggesting average erosion rates of ???0.03 nm/yr. Erosion of Hesperian craters, modification of Late Amazonian craters, and the concentration of hematite concretions in the soils of Meridiani yield slightly higher average erosion rates of 1-10 nm/yr in the Amazonian. These erosion rates are 2-5 orders of magnitude lower than the slowest continental denudation rates on Earth, indicating that liquid water was not an active erosional agent. Erosion rates for Meridiani just before deposition of the sulfate-rich sediments and other eroded Noachian areas are comparable with slow denudation rates on Earth that are dominated by liquid water. Available data suggest the climate change at the landing sites from wet and likely warm to dry and desiccating occurred sometime between the Late Noachian and the beginning of the Late Hesperian (3.7-3.5 Ga). Copyright 2006 by the American Geophysical Union.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Geophysical Research E: Planets","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1029/2006JE002754","issn":"01480227","usgsCitation":"Golombek, M., Grant, J.A., Crumpler, L., Greeley, R., Arvidson, R., Bell, J., Weitz, C., Sullivan, R., Christensen, P.R., Soderblom, L., and Squyres, S.W., 2006, Erosion rates at the Mars Exploration Rover landing sites and long-term climate change on Mars: Journal of Geophysical Research E: Planets, v. 111, no. 12, https://doi.org/10.1029/2006JE002754.","costCenters":[],"links":[{"id":477528,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1029/2006je002754","text":"Publisher Index Page"},{"id":210504,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1029/2006JE002754"},{"id":237442,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"111","issue":"12","noUsgsAuthors":false,"publicationDate":"2006-12-08","publicationStatus":"PW","scienceBaseUri":"505a0a3ee4b0c8380cd5227a","contributors":{"authors":[{"text":"Golombek, M.P.","contributorId":52696,"corporation":false,"usgs":true,"family":"Golombek","given":"M.P.","email":"","affiliations":[],"preferred":false,"id":422145,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Grant, J. A.","contributorId":28334,"corporation":false,"usgs":true,"family":"Grant","given":"J.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":422142,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Crumpler, L.S.","contributorId":81575,"corporation":false,"usgs":true,"family":"Crumpler","given":"L.S.","email":"","affiliations":[],"preferred":false,"id":422146,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Greeley, R.","contributorId":6538,"corporation":false,"usgs":true,"family":"Greeley","given":"R.","email":"","affiliations":[],"preferred":false,"id":422138,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Arvidson, R. E.","contributorId":46666,"corporation":false,"usgs":true,"family":"Arvidson","given":"R. E.","affiliations":[],"preferred":false,"id":422144,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Bell, J.F. III","contributorId":97612,"corporation":false,"usgs":true,"family":"Bell","given":"J.F.","suffix":"III","email":"","affiliations":[],"preferred":false,"id":422147,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Weitz, C.M.","contributorId":8649,"corporation":false,"usgs":true,"family":"Weitz","given":"C.M.","email":"","affiliations":[],"preferred":false,"id":422140,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Sullivan, R.J.","contributorId":21302,"corporation":false,"usgs":true,"family":"Sullivan","given":"R.J.","email":"","affiliations":[],"preferred":false,"id":422141,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Christensen, P. R.","contributorId":7819,"corporation":false,"usgs":false,"family":"Christensen","given":"P.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":422139,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Soderblom, L.A. 0000-0002-0917-853X","orcid":"https://orcid.org/0000-0002-0917-853X","contributorId":6139,"corporation":false,"usgs":true,"family":"Soderblom","given":"L.A.","affiliations":[],"preferred":false,"id":422137,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Squyres, S. W.","contributorId":31836,"corporation":false,"usgs":true,"family":"Squyres","given":"S.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":422143,"contributorType":{"id":1,"text":"Authors"},"rank":11}]}}
,{"id":70194221,"text":"70194221 - 2006 - Dawning of Herpetological Conservation and Biology: A special welcome to your new journal","interactions":[],"lastModifiedDate":"2017-11-18T09:00:47","indexId":"70194221","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1894,"text":"Herpetological Conservation and Biology","onlineIssn":"2151-0733","printIssn":"1931-7603","active":true,"publicationSubtype":{"id":10}},"title":"Dawning of Herpetological Conservation and Biology: A special welcome to your new journal","docAbstract":"<p>Inception of a new journal in herpetology is a rare event. The first discussion of developing a journal with an emphasis on natural history and conservation occurred among a subset of us (McCallum, others), while at the 2005 joint annual meeting of the SSAR/HL/ASIH in Tampa, Florida. Some of the initial questions we posed for a new herpetological journal were as follows: (1) is there a need; (2) audience; and (3) support? If any one of these did not exist, then the concept should be abandoned or modified. We critically examined these questions through discussions with many individuals and informal surveys performed on the Partners in Amphibian and Reptile Conservation (PARC) listserver (parc@listserv.uga.edu) and other forums. Early on, it was obvious to us that there was strong demand for an outlet serving natural history, field ecology and conservation studies, especially descriptive investigations and management case studies that appeared to lack a home in other journals. The road traveled since those discussions has been fast paced, culminating in this 2006 launch of Herpetological Conservation and Biology (HCB).</p>","language":"English","publisher":"Herpetological Conservation & Biology","usgsCitation":"Bury, R.B., McCallum, M.L., Trauth, S.E., and Saumure, R.A., 2006, Dawning of Herpetological Conservation and Biology: A special welcome to your new journal: Herpetological Conservation and Biology, v. 1, no. 1, p. i-iii.","productDescription":"3 p.","startPage":"i","endPage":"iii","costCenters":[{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true}],"links":[{"id":349090,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":349089,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.herpconbio.org/contents_vol1_issue1.html"}],"volume":"1","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5a61142de4b06e28e9c25878","contributors":{"authors":[{"text":"Bury, R. Bruce buryb@usgs.gov","contributorId":3660,"corporation":false,"usgs":true,"family":"Bury","given":"R.","email":"buryb@usgs.gov","middleInitial":"Bruce","affiliations":[{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true}],"preferred":false,"id":722754,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McCallum, Malcolm L.","contributorId":75808,"corporation":false,"usgs":false,"family":"McCallum","given":"Malcolm","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":722755,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Trauth, Stanley E.","contributorId":93406,"corporation":false,"usgs":true,"family":"Trauth","given":"Stanley","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":722756,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Saumure, Raymond A.","contributorId":71375,"corporation":false,"usgs":false,"family":"Saumure","given":"Raymond","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":722757,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70175551,"text":"70175551 - 2006 - Implications of mitochondrial DNA polyphyly in two ecologically undifferentiated but morphologically distinct migratory birds, the masked and white-browed woodswallows <i>Artamus</i> spp. of inland Australia","interactions":[],"lastModifiedDate":"2016-08-16T14:58:00","indexId":"70175551","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2190,"text":"Journal of Avian Biology","active":true,"publicationSubtype":{"id":10}},"title":"Implications of mitochondrial DNA polyphyly in two ecologically undifferentiated but morphologically distinct migratory birds, the masked and white-browed woodswallows <i>Artamus</i> spp. of inland Australia","docAbstract":"<p><span>The white-browed woodswallow&nbsp;</span><i>Artamus superciliosus</i><span>&nbsp;and masked woodswallow&nbsp;</span><i>A. personatus</i><span>(Passeriformes: Artamidae) are members of Australia's diverse arid- and semi-arid zone avifauna. Widely sympatric and among Australia's relatively few obligate long-distance temperate-tropical migrants, the two are well differentiated morphologically but not ecologically and vocally. They are pair breeders unlike other&nbsp;</span><i>Artamus</i><span>&nbsp;species, which are at least facultative cooperative breeders. For these reasons they are an excellent case in which to use molecular data in integrative study of their evolution from ecological and biogeographical perspectives. We used mitochondrial DNA (mtDNA) to test whether they are each other's closest relatives, whether they evolved migration independently, whether they have molecular signatures of population expansions like some other Australian arid zone birds, and to estimate the timing of any inferred population expansions. Their mtDNAs are monophyletic with respect to other species of&nbsp;</span><i>Artamus</i><span>but polyphyletic with respect to each other. The two species appear not to have evolved migration independently of each other but their morphological and mtDNA evolution have been strongly decoupled. Some level of hybridization and introgression cannot be dismissed outright as being involved in their mtDNA polyphyly but incomplete sorting of their most recent common ancestor's mtDNA is a simpler explanation consistent with their ecology. Bayesian phylogenetic inference and analyses of diversity within the two species (n=77) with conventional diversity statistics, statistical parsimony, and tests for population expansion&nbsp;</span><i>vs</i><span>&nbsp;stability (Tajima's&nbsp;</span><i>D</i><span>, Fu's&nbsp;</span><i>Fs</i><span>and Ramos-Onsin and Rozas's&nbsp;</span><i>R</i><span>2</span><span>) all favour recent population increases. However, a non-starlike network suggests expansion(s) relatively early in the Pleistocene. Repeated population bottlenecks corresponding with multiple peaks of Pleistocene aridity could explain our findings, which add a new dimension to accruing data on the effects of Pleistocene aridity on the Australian biota.</span></p>","language":"English","publisher":"Wiley","doi":"10.1111/j.0908-8857.2006.03767.x","usgsCitation":"Joseph, L., Wilke, T., Ten Have, J., and Chesser, R., 2006, Implications of mitochondrial DNA polyphyly in two ecologically undifferentiated but morphologically distinct migratory birds, the masked and white-browed woodswallows <i>Artamus</i> spp. of inland Australia: Journal of Avian Biology, v. 37, no. 6, p. 625-636, https://doi.org/10.1111/j.0908-8857.2006.03767.x.","productDescription":"12 p.","startPage":"625","endPage":"636","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":326587,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"37","issue":"6","noUsgsAuthors":false,"publicationDate":"2006-11-02","publicationStatus":"PW","scienceBaseUri":"57b43952e4b03bcb01039ffe","contributors":{"authors":[{"text":"Joseph, Leo","contributorId":173726,"corporation":false,"usgs":false,"family":"Joseph","given":"Leo","affiliations":[],"preferred":false,"id":645653,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wilke, Thomas","contributorId":173727,"corporation":false,"usgs":false,"family":"Wilke","given":"Thomas","email":"","affiliations":[],"preferred":false,"id":645654,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ten Have, Jose","contributorId":173728,"corporation":false,"usgs":false,"family":"Ten Have","given":"Jose","email":"","affiliations":[],"preferred":false,"id":645655,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Chesser, R. Terry 0000-0003-4389-7092 tchesser@usgs.gov","orcid":"https://orcid.org/0000-0003-4389-7092","contributorId":894,"corporation":false,"usgs":true,"family":"Chesser","given":"R. Terry","email":"tchesser@usgs.gov","affiliations":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"preferred":false,"id":645656,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70179499,"text":"70179499 - 2006 -  Lower Methow tributaries intensive effectiveness monitoring study. 2005 progress report","interactions":[],"lastModifiedDate":"2017-01-03T16:04:11","indexId":"70179499","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"title":" Lower Methow tributaries intensive effectiveness monitoring study. 2005 progress report","docAbstract":"<p>n/a</p>","language":"English","publisher":"U.S. Bureau of Reclamation","usgsCitation":"Connolly, P., Martens, K., Ruttenberg, D., and Clayton, S., 2006,  Lower Methow tributaries intensive effectiveness monitoring study. 2005 progress report.","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":332802,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Washington","otherGeospatial":"Lower Meadow tributaries ","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -120.17669677734374,\n              48.66557095325139\n            ],\n            [\n              -120.55297851562499,\n              48.60204136700653\n            ],\n            [\n              -120.54336547851562,\n              48.469279317167164\n            ],\n            [\n              -120.421142578125,\n              48.31882083063846\n            ],\n            [\n              -120.03799438476561,\n              48.27679550566659\n            ],\n            [\n              -119.90753173828125,\n              48.36446129786668\n            ],\n            [\n              -120.07095336914061,\n              48.66557095325139\n            ],\n            [\n              -120.17669677734374,\n              48.66557095325139\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"586cc6b9e4b0f5ce109fa997","contributors":{"authors":[{"text":"Connolly, P.J.","contributorId":70141,"corporation":false,"usgs":true,"family":"Connolly","given":"P.J.","email":"","affiliations":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"preferred":false,"id":657453,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Martens, K.","contributorId":47221,"corporation":false,"usgs":true,"family":"Martens","given":"K.","email":"","affiliations":[],"preferred":false,"id":657454,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ruttenberg, D.","contributorId":177898,"corporation":false,"usgs":false,"family":"Ruttenberg","given":"D.","email":"","affiliations":[],"preferred":false,"id":657455,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Clayton, S.","contributorId":177899,"corporation":false,"usgs":false,"family":"Clayton","given":"S.","email":"","affiliations":[],"preferred":false,"id":657456,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70030987,"text":"70030987 - 2006 - Explosion source strong ground motions in the Mississippi embayment","interactions":[],"lastModifiedDate":"2020-04-28T15:20:52.91803","indexId":"70030987","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1135,"text":"Bulletin of the Seismological Society of America","onlineIssn":"1943-3573","printIssn":"0037-1106","active":true,"publicationSubtype":{"id":10}},"title":"Explosion source strong ground motions in the Mississippi embayment","docAbstract":"Two strong-motion arrays were deployed for the October 2002 Embayment Seismic Excitation Experiment to study the spatial variation of strong ground motions in the deep, unconsolidated sediments of the Mississippi embayment because there are no comparable strong-motion data from natural earthquakes in the area. Each linear array consisted of eight three-component K2 accelerographs spaced 15 m apart situated 1.2 and 2.5 kin from 2268-kg and 1134-kg borehole explosion sources, respectively. The array data show distinct body-wave and surface-wave arrivals that propagate within the thick, unconsolidated sedimentary column, the high-velocity basement rocks, and small-scale structure near the surface. Time-domain coherence of body-wave and surface-wave arrivals is computed for acceleration, velocity, and displacement time windows. Coherence is high for relatively low-frequency verticalcomponent Rayleigh waves and high-frequency P waves propagating across the array. Prominent high-frequency PS conversions seen on radial components, a proxy for the direct S wave from earthquake sources, lose coherence quickly over the 105-m length of the array. Transverse component signals are least coherent for any ground motion and appear to be highly scattered. Horizontal phase velocity is computed by using the ratio of particle velocity to estimates of the strain based on a plane-wave-propagation model. The resulting time-dependent phase-velocity map is a useful way to infer the propagation mechanisms of individual seismic phases and time windows of three-component waveforms. Displacement gradient analysis is a complementary technique for processing general spatial-array data to obtain horizontal slowness information.","largerWorkTitle":"","language":"English","publisher":"Geological Society of America","doi":"10.1785/0120050105","issn":"00371106","usgsCitation":"Langston, C., Bodin, P., Powell, C., Withers, M., Horton, S., and Mooney, W.D., 2006, Explosion source strong ground motions in the Mississippi embayment: Bulletin of the Seismological Society of America, v. 96, no. 3, p. 1038-1054, https://doi.org/10.1785/0120050105.","productDescription":"17 p.","startPage":"1038","endPage":"1054","numberOfPages":"17","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"links":[{"id":239038,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Arkansas, Missouri, Tennessee ","otherGeospatial":"Mississippi River embayment","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -90.98876953125,\n              34.75966612466248\n            ],\n            [\n              -88.74755859375,\n              34.75966612466248\n            ],\n            [\n              -88.74755859375,\n              36.756490329505176\n            ],\n            [\n              -90.98876953125,\n              36.756490329505176\n            ],\n            [\n              -90.98876953125,\n              34.75966612466248\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"96","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0e29e4b0c8380cd53314","contributors":{"authors":[{"text":"Langston, C.A.","contributorId":84882,"corporation":false,"usgs":true,"family":"Langston","given":"C.A.","email":"","affiliations":[],"preferred":false,"id":429523,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bodin, P.","contributorId":29554,"corporation":false,"usgs":true,"family":"Bodin","given":"P.","email":"","affiliations":[],"preferred":false,"id":429520,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Powell, C.","contributorId":56849,"corporation":false,"usgs":true,"family":"Powell","given":"C.","email":"","affiliations":[],"preferred":false,"id":429522,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Withers, M.","contributorId":27667,"corporation":false,"usgs":true,"family":"Withers","given":"M.","email":"","affiliations":[],"preferred":false,"id":429519,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Horton, S.","contributorId":20146,"corporation":false,"usgs":true,"family":"Horton","given":"S.","email":"","affiliations":[],"preferred":false,"id":429518,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Mooney, Walter D. 0000-0002-5310-3631 mooney@usgs.gov","orcid":"https://orcid.org/0000-0002-5310-3631","contributorId":3194,"corporation":false,"usgs":true,"family":"Mooney","given":"Walter","email":"mooney@usgs.gov","middleInitial":"D.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":429521,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70030642,"text":"70030642 - 2006 - Biofouling and the continuous monitoring of underwater light from a seagrass perspective","interactions":[],"lastModifiedDate":"2019-11-27T14:59:08","indexId":"70030642","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1584,"text":"Estuaries and Coasts","active":true,"publicationSubtype":{"id":10}},"title":"Biofouling and the continuous monitoring of underwater light from a seagrass perspective","docAbstract":"<p><span>For more than a decade, inexpensive electronic instruments have made continuous underwater light monitoring an integral part of many seagrass studies. Although biofouling, if not controlled, compromises the utility of the record. A year-long assessment of the time course of sensor fouling, in the Laguna Madre of Texas established that light transmitted through the fouling layer after 2 wk of exposure exceeded 90% except for a 6–8 wk period in May and June. On that basis, a 2-wk interval was chosen for routine servicing. Subsequent monitoring proved this choice to be grossly in error. The period of sub-90% transmittance after 2 wk extended to 4–6 mo annually over the next 3 yr. Fouling was strongly correlated with temperature, ambient light, and year. Since an algal bloom of 7-yr duration finally waned during this study, increased ambient light seemed most likely to explain increased fouling later in the study. The explanatory value of light was less than temperature or year in multiple regression, requiring some other explanation of the date effect than change in ambient light. Allelopathic and suspension-feeding depressant effects of the brown tide are offered as the most likely cause of unusually low fouling in the first year. Biofouling was so unpredictable and rapid in this study that at least weekly maintenance would be required to assure reliability of the light monitoring record.</span></p>","language":"English","publisher":"Springer","doi":"10.1007/BF02784998","issn":"15592723","usgsCitation":"Onuf, C., 2006, Biofouling and the continuous monitoring of underwater light from a seagrass perspective: Estuaries and Coasts, v. 29, no. 3, p. 511-518, https://doi.org/10.1007/BF02784998.","productDescription":"8 p.","startPage":"511","endPage":"518","numberOfPages":"8","costCenters":[{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true},{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"links":[{"id":239463,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Texas","otherGeospatial":"Upper Laguna Madre","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -97.27775573730469,\n              27.662852655417325\n            ],\n            [\n              -97.30110168457031,\n              27.609321622948173\n            ],\n            [\n              -97.294921875,\n              27.591066424185087\n            ],\n            [\n              -97.32170104980469,\n              27.569156172901426\n            ],\n            [\n              -97.35671997070311,\n              27.485126363846202\n            ],\n            [\n              -97.37045288085938,\n              27.41931914228741\n            ],\n            [\n              -97.415771484375,\n              27.319924711806493\n            ],\n            [\n              -97.41302490234375,\n              27.285146100246426\n            ],\n            [\n              -97.3773193359375,\n              27.28087429152069\n            ],\n            [\n              -97.35671997070311,\n              27.31138360632011\n            ],\n            [\n              -97.36358642578125,\n              27.34859361222366\n            ],\n            [\n              -97.33200073242188,\n              27.42053815128712\n            ],\n            [\n              -97.32994079589844,\n              27.436384043710643\n            ],\n            [\n              -97.26676940917969,\n              27.545415129939936\n            ],\n            [\n              -97.25372314453125,\n              27.579503225827125\n            ],\n            [\n              -97.22831726074219,\n              27.629398828704613\n            ],\n            [\n              -97.27775573730469,\n              27.662852655417325\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"29","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f14de4b0c8380cd4ab90","contributors":{"authors":[{"text":"Onuf, C.P.","contributorId":80837,"corporation":false,"usgs":true,"family":"Onuf","given":"C.P.","affiliations":[],"preferred":false,"id":428003,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70185645,"text":"70185645 - 2006 - Arsenic and selenium in microbial metabolism","interactions":[],"lastModifiedDate":"2018-10-26T08:08:11","indexId":"70185645","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5335,"text":"Annual Review of Microbiology","active":true,"publicationSubtype":{"id":10}},"title":"Arsenic and selenium in microbial metabolism","docAbstract":"<p><span>Arsenic and selenium are readily metabolized by prokaryotes, participating in a full range of metabolic functions including assimilation, methylation, detoxification, and anaerobic respiration. Arsenic speciation and mobility is affected by microbes through oxidation/reduction reactions as part of resistance and respiratory processes. A robust arsenic cycle has been demonstrated in diverse environments. Respiratory arsenate reductases, arsenic methyltransferases, and new components in arsenic resistance have been recently described. The requirement for selenium stems primarily from its incorporation into selenocysteine and its function in selenoenzymes. Selenium oxyanions can serve as an electron acceptor in anaerobic respiration, forming distinct nanoparticles of elemental selenium that may be enriched in (76)Se. The biogenesis of selenoproteins has been elucidated, and selenium methyltransferases and a respiratory selenate reductase have also been described. This review highlights recent advances in ecology, biochemistry, and molecular biology and provides a prelude to the impact of genomics studies.</span></p>","language":"English","publisher":"Annual Review","doi":"10.1146/annurev.micro.60.080805.142053","usgsCitation":"Stolz, J.F., Basu, P., Santini, J.M., and Oremland, R.S., 2006, Arsenic and selenium in microbial metabolism: Annual Review of Microbiology, v. 60, p. 107-130, https://doi.org/10.1146/annurev.micro.60.080805.142053.","productDescription":"24 p. ","startPage":"107","endPage":"130","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":338345,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"60","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58da251be4b0543bf7fda800","contributors":{"authors":[{"text":"Stolz, John F.","contributorId":179305,"corporation":false,"usgs":false,"family":"Stolz","given":"John","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":686203,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Basu, Partha","contributorId":189834,"corporation":false,"usgs":false,"family":"Basu","given":"Partha","email":"","affiliations":[],"preferred":false,"id":686204,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Santini, Joanne M.","contributorId":168895,"corporation":false,"usgs":false,"family":"Santini","given":"Joanne","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":686205,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Oremland, Ronald S. 0000-0001-7382-0147 roremlan@usgs.gov","orcid":"https://orcid.org/0000-0001-7382-0147","contributorId":931,"corporation":false,"usgs":true,"family":"Oremland","given":"Ronald","email":"roremlan@usgs.gov","middleInitial":"S.","affiliations":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true},{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":686206,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70028593,"text":"70028593 - 2006 - The diamondback terrapin: The biology, ecology, cultural history, and conservation status of an obligate estuarine turtle","interactions":[],"lastModifiedDate":"2012-03-12T17:20:55","indexId":"70028593","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3489,"text":"Studies in Avian Biology","active":true,"publicationSubtype":{"id":10}},"title":"The diamondback terrapin: The biology, ecology, cultural history, and conservation status of an obligate estuarine turtle","docAbstract":"Ranging from Cape Cod to nearly the Texas-Mexico border, the diamondback terrapin (Malaclemys terrapin) is the only species of North American turtle restricted to estuarine systems. Despite this extensive distribution, its zone of occurrence is very linear, and in places fragmented, resulting in a relatively small total area of occupancy. On a global scale, excluding marine species, few turtles even venture into brackish water on a regular basis, and only two Asian species approach the North American terrapin's dependency on estuarine habitats. Here we describe some of the biological and behavioral adaptations of terrapins that allow them to live in the rather harsh estuarine environment. In this chapter we review the natural and cultural history of this turtle, discuss conservation issues, and provide information on the types of research needed to make sound management decisions for terrapin populations in peril.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Studies in Avian Biology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"01979922","isbn":"0943610702; 9780943610702","usgsCitation":"Hart, K., and Lee, D., 2006, The diamondback terrapin: The biology, ecology, cultural history, and conservation status of an obligate estuarine turtle: Studies in Avian Biology, no. 32, p. 206-213.","startPage":"206","endPage":"213","numberOfPages":"8","costCenters":[],"links":[{"id":236364,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"issue":"32","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505baaabe4b08c986b32290c","contributors":{"editors":[{"text":"Greenberg R.Maldonado J.E.Droege S.McDonald M.V.","contributorId":128314,"corporation":true,"usgs":false,"organization":"Greenberg R.Maldonado J.E.Droege S.McDonald M.V.","id":536638,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Hart, K.M. 0000-0002-5257-7974","orcid":"https://orcid.org/0000-0002-5257-7974","contributorId":7483,"corporation":false,"usgs":true,"family":"Hart","given":"K.M.","affiliations":[],"preferred":false,"id":418755,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lee, D.S.","contributorId":50330,"corporation":false,"usgs":true,"family":"Lee","given":"D.S.","email":"","affiliations":[],"preferred":false,"id":418756,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70190530,"text":"70190530 - 2006 - A mid-holocene fauna from Bear Den Cave, Sequoia National Park, California","interactions":[],"lastModifiedDate":"2017-09-06T14:02:26","indexId":"70190530","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1092,"text":"Bulletin, Southern California Academy of Sciences","active":true,"publicationSubtype":{"id":10}},"title":"A mid-holocene fauna from Bear Den Cave, Sequoia National Park, California","docAbstract":"<p><span>Test excavation of floor fill deposits in the first room in Bear Den Cave, Sequoia National Park, produced fossiliferous sediments down to at least 40 cm depth. Radiocarbon analysis of charcoal from this layer indicates an early-middle Holocene age of 7220 CAL BP. The fossil accumulation represents prey recovered from generations of ringtail (</span><i>Bassariscus astutus</i><span>) dung. Microvertebrate remains include salamanders, lizards, snakes, and mammals. The recovery of<span>&nbsp;</span></span><i>Aneides ferreus</i><span>/</span><i>vagrans</i><span>from early-middle Holocene deposits in Bear Den Cave is a first for this species group. Equally interesting is the recovery of<span>&nbsp;</span></span><i>Plethodon</i><span><span>&nbsp;</span>sp. Neither taxa live in the Sierra Nevada today. The fossil-rich deposits of Bear Den Cave indicate that future paleoecological studies will be productive in Sequoia National Park.</span></p>","language":"English","publisher":"Southern California Academy of Sciences","doi":"10.3160/0038-3872(2006)105[43:AMFFBD]2.0.CO;2","usgsCitation":"Mead, J.I., McGinnis, T.W., and Keeley, J.E., 2006, A mid-holocene fauna from Bear Den Cave, Sequoia National Park, California: Bulletin, Southern California Academy of Sciences, v. 105, no. 2, p. 43-58, https://doi.org/10.3160/0038-3872(2006)105[43:AMFFBD]2.0.CO;2.","productDescription":"16 p.","startPage":"43","endPage":"58","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":477612,"rank":0,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://doi.org/10.3160/0038-3872(2006)105[43:amffbd]2.0.co;2","text":"External Repository"},{"id":345502,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Bear Den Cave, Sequoia National Park","volume":"105","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"59b10936e4b020cdf7d8da0a","contributors":{"authors":[{"text":"Mead, Jim I.","contributorId":87067,"corporation":false,"usgs":true,"family":"Mead","given":"Jim","email":"","middleInitial":"I.","affiliations":[],"preferred":false,"id":709652,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McGinnis, Thomas W.","contributorId":87272,"corporation":false,"usgs":true,"family":"McGinnis","given":"Thomas","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":709653,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Keeley, Jon E. 0000-0002-4564-6521 jon_keeley@usgs.gov","orcid":"https://orcid.org/0000-0002-4564-6521","contributorId":1268,"corporation":false,"usgs":true,"family":"Keeley","given":"Jon","email":"jon_keeley@usgs.gov","middleInitial":"E.","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":true,"id":709654,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70028379,"text":"70028379 - 2006 - Seeing the elephant: Importance of spatial and temporal coverage in a large-scale volunteer-based program to monitor horseshoe crabs","interactions":[],"lastModifiedDate":"2012-03-12T17:20:53","indexId":"70028379","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1657,"text":"Fisheries","onlineIssn":"1548-8446","printIssn":"0363-2415","active":true,"publicationSubtype":{"id":10}},"title":"Seeing the elephant: Importance of spatial and temporal coverage in a large-scale volunteer-based program to monitor horseshoe crabs","docAbstract":"As in John Godfrey Saxe's poem about six blind men and an elephant, conclusions drawn from a monitoring program depend critically on where and when observations are made. We examined results from the Delaware Bay horseshoe crab (Limulus polyphemus) spawning survey to evaluate the effect of spatial and temporal coverage on conclusions about spawning activity. Declines due to previously unregulated harvest triggered an increase in monitoring. Although we detected no apparent trend in bay-wide spawning activity for 1999-2005, conclusions would have differed depending on where and when observations were made. For example, spawning activity in May during the shorebird stopover was a poor predictor of spawning activity over the whole season. Observations made only during peak spawning incorrectly suggested that spawning activity increased during 2001-2005. Trends at one place in the bay were not indicative of trends for the whole bay. Many natural resource issues begin like the blind men and the elephant with dispute partially caused by an incomplete picture of the resource. As sufficient time and funds are directed to gathering necessary data using effective sampling designs, a more complete picture can emerge.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Fisheries","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1577/1548-8446(2006)31[485:STE]2.0.CO;2","issn":"03632415","usgsCitation":"Smith, D., and Michels, S., 2006, Seeing the elephant: Importance of spatial and temporal coverage in a large-scale volunteer-based program to monitor horseshoe crabs: Fisheries, v. 31, no. 10, p. 485-491, https://doi.org/10.1577/1548-8446(2006)31[485:STE]2.0.CO;2.","startPage":"485","endPage":"491","numberOfPages":"7","costCenters":[],"links":[{"id":210434,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1577/1548-8446(2006)31[485:STE]2.0.CO;2"},{"id":237347,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"31","issue":"10","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b8acce4b08c986b3173b4","contributors":{"authors":[{"text":"Smith, D. R. 0000-0001-6074-9257","orcid":"https://orcid.org/0000-0001-6074-9257","contributorId":44108,"corporation":false,"usgs":true,"family":"Smith","given":"D. R.","affiliations":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"preferred":false,"id":417799,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Michels, S.F.","contributorId":34867,"corporation":false,"usgs":true,"family":"Michels","given":"S.F.","email":"","affiliations":[],"preferred":false,"id":417798,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70028754,"text":"70028754 - 2006 - Extreme U-Th disequilibrium in rift-related basalts, rhyolites and granophyric granite and the timescale of rhyolite generation, intrusion and crystallization at Alid volcanic center, Eritrea","interactions":[],"lastModifiedDate":"2019-04-08T10:59:36","indexId":"70028754","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2420,"text":"Journal of Petrology","active":true,"publicationSubtype":{"id":10}},"title":"Extreme U-Th disequilibrium in rift-related basalts, rhyolites and granophyric granite and the timescale of rhyolite generation, intrusion and crystallization at Alid volcanic center, Eritrea","docAbstract":"<div id=\"abstract-1\" class=\"section abstract\"><p id=\"p-1\">Rhyolite pumices and co-erupted granophyric (granite) xenoliths yield evidence for rapid magma generation and crystallization prior to their eruption at 15·2 ± 2·9 ka at the Alid volcanic center in the Danikil Depression, Eritrea. Whole-rock U and Th isotopic analyses show <sup>230</sup>Th excesses up to 50% in basalts &lt;10 000 years old from the surrounding Oss lava fields. The 15 ka rhyolites also have 30–40% <sup>230</sup>Th excesses. Similarity in U–Th disequilibrium, and in Sr, Nd, and Pb isotopic values, implies that the rhyolites are mostly differentiated from the local basaltic magma. Given the (<sup>230</sup>Th/<sup>232</sup>Th) ratio of the young basalts, and presumably the underlying mantle, the (<sup>230</sup>Th/<sup>232</sup>Th) ratio of the rhyolites upon eruption could be generated by in situ decay in about 50 000 years. Limited (∼5%) assimilation of old crust would hasten the lowering of (<sup>230</sup>Th/<sup>232</sup>Th) and allow the process to take place in as little as 30 000 years. Final crystallization of the Alid granophyre occurred rapidly and at shallow depths at ∼20–25 ka, as confirmed by analyses of mineral separates and ion microprobe data on individual zircons. Evidently, 30 000–50 000 years were required for extraction of basalt from its mantle source region, subsequent crystallization and melt extraction to form silicic magmas, and final crystallization of the shallow intrusion. The granophyre was then ejected during eruption of the comagmatic rhyolites.</p></div>","largerWorkTitle":"Journal of Petrology","language":"English","publisher":"University Press","doi":"10.1093/petrology/egl038","issn":"00223530","usgsCitation":"Lowenstern, J.B., Charlier, B.L., Clynne, M., and Wooden, J.L., 2006, Extreme U-Th disequilibrium in rift-related basalts, rhyolites and granophyric granite and the timescale of rhyolite generation, intrusion and crystallization at Alid volcanic center, Eritrea: Journal of Petrology, v. 47, no. 11, p. 2105-2122, https://doi.org/10.1093/petrology/egl038.","productDescription":"18 p.","startPage":"2105","endPage":"2122","numberOfPages":"18","costCenters":[{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true}],"links":[{"id":477482,"rank":1,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1093/petrology/egl038","text":"Publisher Index Page"},{"id":236645,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"47","issue":"11","noUsgsAuthors":false,"publicationDate":"2006-08-02","publicationStatus":"PW","scienceBaseUri":"505a0e66e4b0c8380cd5342e","contributors":{"authors":[{"text":"Lowenstern, J. B.","contributorId":7737,"corporation":false,"usgs":true,"family":"Lowenstern","given":"J.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":419616,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Charlier, B. L. A.","contributorId":45090,"corporation":false,"usgs":false,"family":"Charlier","given":"B.","email":"","middleInitial":"L. A.","affiliations":[],"preferred":false,"id":419617,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Clynne, M.A.","contributorId":90722,"corporation":false,"usgs":true,"family":"Clynne","given":"M.A.","affiliations":[],"preferred":false,"id":419619,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Wooden, J. L.","contributorId":58678,"corporation":false,"usgs":true,"family":"Wooden","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":419618,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70028838,"text":"70028838 - 2006 - Cross-calibration of MODIS with ETM+ and ALI sensors for long-term monitoring of land surface processes","interactions":[],"lastModifiedDate":"2022-05-17T15:53:59.766539","indexId":"70028838","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Cross-calibration of MODIS with ETM+ and ALI sensors for long-term monitoring of land surface processes","docAbstract":"Increasingly, data from multiple sensors are used to gain a more complete understanding of land surface processes at a variety of scales. Although higher-level products (e.g., vegetation cover, albedo, surface temperature) derived from different sensors can be validated independently, the degree to which these sensors and their products can be compared to one another is vastly improved if their relative spectroradiometric responses are known. Most often, sensors are directly calibrated to diffuse solar irradiation or vicariously to ground targets. However, space-based targets are not traceable to metrological standards, and vicarious calibrations are expensive and provide a poor sampling of a sensor's full dynamic range. Crosscalibration of two sensors can augment these methods if certain conditions can be met: (1) the spectral responses are similar, (2) the observations are reasonably concurrent (similar atmospheric & solar illumination conditions), (3) errors due to misregistrations of inhomogeneous surfaces can be minimized (including scale differences), and (4) the viewing geometry is similar (or, some reasonable knowledge of surface bi-directional reflectance distribution functions is available). This study explores the impacts of cross-calibrating sensors when such conditions are met to some degree but not perfectly. In order to constrain the range of conditions at some level, the analysis is limited to sensors where cross-calibration studies have been conducted (Enhanced Thematic Mapper Plus (ETM+) on Landsat-7 (L7), Advance Land Imager (ALI) and Hyperion on Earth Observer-1 (EO-1)) and including systems having somewhat dissimilar geometry, spatial resolution & spectral response characteristics but are still part of the so-called \"A.M. constellation\" (Moderate Resolution Imaging Spectrometer (MODIS) aboard the Terra platform). Measures for spectral response differences and methods for cross calibrating such sensors are provided in this study. These instruments are cross calibrated using the Railroad Valley playa in Nevada. Best fit linear coefficients (slope and offset) are provided for ALI-to-MODIS and ETM+-to-MODIS cross calibrations, and root-mean-squared errors (RMSEs) and correlation coefficients are provided to quantify the uncertainty in these relationships. In theory, the linear fits and uncertainties can be used to compare radiance and reflectance products derived from each instrument.","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Proceedings of SPIE - The International Society for Optical Engineering","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"Earth Observing Systems XI","conferenceDate":"Aug 14-16, 2006","conferenceLocation":"San Diego, CA","language":"English","publisher":"SPIE","doi":"10.1117/12.683567","usgsCitation":"Meyer, D., and Chander, G., 2006, Cross-calibration of MODIS with ETM+ and ALI sensors for long-term monitoring of land surface processes, <i>in</i> Proceedings of SPIE - The International Society for Optical Engineering, v. 6296, San Diego, CA, Aug 14-16, 2006, 62960H, https://doi.org/10.1117/12.683567.","productDescription":"62960H","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":236759,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"6296","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059fcc1e4b0c8380cd4e3fa","contributors":{"authors":[{"text":"Meyer, D.","contributorId":31131,"corporation":false,"usgs":true,"family":"Meyer","given":"D.","affiliations":[],"preferred":false,"id":419938,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Chander, G.","contributorId":51449,"corporation":false,"usgs":true,"family":"Chander","given":"G.","affiliations":[],"preferred":false,"id":419939,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70028369,"text":"70028369 - 2006 - Dietary exposure of mink (<i>Mustela vison</i>) to fish from the Housatonic River, Berkshire County, Massachusetts, USA: Effects on reproduction, kit growth, and survival","interactions":[],"lastModifiedDate":"2016-11-14T14:16:27","indexId":"70028369","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1571,"text":"Environmental Toxicology and Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"Dietary exposure of mink (<i>Mustela vison</i>) to fish from the Housatonic River, Berkshire County, Massachusetts, USA: Effects on reproduction, kit growth, and survival","docAbstract":"We evaluated the effects of feeding farm-raised mink (Mustela vison) diets containing polychlorinated biphenyl (PCB)-contaminated fish from the Housatonic River (HR; Berkshire County, MA, USA) on adult reproductive performance and kit growth and survival. Diets contained 0.22-3.54% HR fish, providing 0.34-3.7 ??g total PCBs (TPCB)/g feed wet wt (3.5-68.5 pg toxic equivalence [TEQ]/g). Female mink were fed diets before breeding through weaning of kits. Twelve kits from each treatment were maintained on their respective diets for an additional 180 d. Dietary PCBs had no effect on the number of offspring produced, gestation period, or other measures of adult reproductive performance. Mink kits exposed to 3.7 ??g TPCB/g feed (68.5 pg TEQ/g) in utero and during lactation had reduced survivability between three and six weeks of age. The lethal concentrations to 10 and 20% of the population (LC10 and LC20, respectively) were estimated to be 0.231 and 0.984 ??g TPCB/g feed, respectively. Because inclusion of PCB-contaminated fish that composed approximately 1% of the diet would reduce mink kit survival by 20% or more, it is likely that consumption of up to 30-fold that quantity of HR fish, as could be expected for wild mink, would have an adverse effect on wild mink populations. ?? 2006 SETAC.","language":"English","publisher":"Wiley","doi":"10.1897/05-406R.1","issn":"07307268","usgsCitation":"Bursian, S., Sharma, C., Aulerich, R., Yamini, B., Mitchell, R., Orazio, C., Moore, D., Svirsky, S., and Tillitt, D.E., 2006, Dietary exposure of mink (<i>Mustela vison</i>) to fish from the Housatonic River, Berkshire County, Massachusetts, USA: Effects on reproduction, kit growth, and survival: Environmental Toxicology and Chemistry, v. 25, no. 6, p. 1533-1540, https://doi.org/10.1897/05-406R.1.","productDescription":"8 p.","startPage":"1533","endPage":"1540","numberOfPages":"8","costCenters":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"links":[{"id":237173,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":210295,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1897/05-406R.1"}],"volume":"25","issue":"6","noUsgsAuthors":false,"publicationDate":"2006-06-01","publicationStatus":"PW","scienceBaseUri":"505a00dfe4b0c8380cd4f97b","contributors":{"authors":[{"text":"Bursian, S.J.","contributorId":16127,"corporation":false,"usgs":true,"family":"Bursian","given":"S.J.","email":"","affiliations":[],"preferred":false,"id":417763,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sharma, C.","contributorId":22134,"corporation":false,"usgs":true,"family":"Sharma","given":"C.","email":"","affiliations":[],"preferred":false,"id":417764,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Aulerich, R.J.","contributorId":39904,"corporation":false,"usgs":true,"family":"Aulerich","given":"R.J.","email":"","affiliations":[],"preferred":false,"id":417765,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Yamini, B.","contributorId":59612,"corporation":false,"usgs":true,"family":"Yamini","given":"B.","affiliations":[],"preferred":false,"id":417766,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Mitchell, R.R.","contributorId":8665,"corporation":false,"usgs":true,"family":"Mitchell","given":"R.R.","email":"","affiliations":[],"preferred":false,"id":417761,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Orazio, C.E.","contributorId":68440,"corporation":false,"usgs":true,"family":"Orazio","given":"C.E.","email":"","affiliations":[],"preferred":false,"id":417767,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Moore, D.R.J.","contributorId":74188,"corporation":false,"usgs":true,"family":"Moore","given":"D.R.J.","email":"","affiliations":[],"preferred":false,"id":417768,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Svirsky, S.","contributorId":11821,"corporation":false,"usgs":true,"family":"Svirsky","given":"S.","email":"","affiliations":[],"preferred":false,"id":417762,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Tillitt, D. E.","contributorId":83462,"corporation":false,"usgs":true,"family":"Tillitt","given":"D.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":417769,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}}
,{"id":70028752,"text":"70028752 - 2006 - Community maturity, species saturation and the variant diversity- productivity relationships in grasslands","interactions":[],"lastModifiedDate":"2018-11-07T12:25:14","indexId":"70028752","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1466,"text":"Ecology Letters","active":true,"publicationSubtype":{"id":10}},"title":"Community maturity, species saturation and the variant diversity- productivity relationships in grasslands","docAbstract":"Detailed knowledge of the relationship between plant diversity and productivity is critical for advancing our understanding of ecosystem functioning and for achieving success in habitat restoration efforts. However, effects and interactions of diversity, succession and biotic invasions on productivity remain elusive. We studied newly established communities in relation to preexisting homogeneous vegetation invaded by exotic plants in the northern Great Plains, USA, at four study sites for 3 years. We observed variant diversity-productivity relationships for the seeded communities (generally positive monotonic at three sites and non-monotonic at the other site) but no relationships for the resident community or the seeded and resident communities combined at all sites and all years. Community richness was enhanced by seeding additional species but productivity was not. The optimal diversity (as indicated by maximum productivity) changed among sites and as the community developed. The findings shed new light on ecosystem functioning of biodiversity under different conditions and have important implications for restoration. ?? 2006 Blackwell Publishing Ltd/CNRS.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Ecology Letters","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1111/j.1461-0248.2006.00980.x","issn":"1461023X","usgsCitation":"Guo, Q., Shaffer, T., and Buhl, T., 2006, Community maturity, species saturation and the variant diversity- productivity relationships in grasslands: Ecology Letters, v. 9, no. 12, p. 1284-1292, https://doi.org/10.1111/j.1461-0248.2006.00980.x.","productDescription":"9 p.","startPage":"1284","endPage":"1292","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":236612,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":209870,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1111/j.1461-0248.2006.00980.x"}],"volume":"9","issue":"12","noUsgsAuthors":false,"publicationDate":"2006-10-18","publicationStatus":"PW","scienceBaseUri":"5059f808e4b0c8380cd4ce36","contributors":{"authors":[{"text":"Guo, Q.","contributorId":67039,"corporation":false,"usgs":true,"family":"Guo","given":"Q.","email":"","affiliations":[],"preferred":false,"id":419611,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Shaffer, T.","contributorId":71749,"corporation":false,"usgs":true,"family":"Shaffer","given":"T.","email":"","affiliations":[],"preferred":false,"id":419612,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Buhl, T. 0000-0001-9909-3419","orcid":"https://orcid.org/0000-0001-9909-3419","contributorId":44342,"corporation":false,"usgs":true,"family":"Buhl","given":"T.","affiliations":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"preferred":false,"id":419610,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70028310,"text":"70028310 - 2006 - Electrical resistance sensors record spring flow timing, Grand Canyon, Arizona","interactions":[],"lastModifiedDate":"2012-03-12T17:20:52","indexId":"70028310","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1861,"text":"Ground Water","active":true,"publicationSubtype":{"id":10}},"title":"Electrical resistance sensors record spring flow timing, Grand Canyon, Arizona","docAbstract":"Springs along the south rim of the Grand Canyon, Arizona, are important ecological and cultural resources in Grand Canyon National Park and are discharge points for regional and local aquifers of the Coconino Plateau. This study evaluated the applicability of electrical resistance (ER) sensors for measuring diffuse, low-stage (<1.0 cm) intermittent and ephemeral flow in the steep, rocky spring-fed tributaries of the south rim. ER sensors were used to conduct a baseline survey of spring flow timing at eight sites in three spring-fed tributaries in Grand Canyon. Sensors were attached to a nearly vertical rock wall at a spring outlet and were installed in alluvial and bedrock channels. Spring flow timing data inferred by the ER sensors were consistent with observations during site visits, with flow events recorded with collocated streamflow gauging stations and with local precipitation gauges. ER sensors were able to distinguish the presence of flow along nearly vertical rock surfaces with flow depths between 0.3 and 1.0 cm. Laboratory experiments confirmed the ability of the sensors to monitor the timing of diffuse flow on impervious surfaces. A comparison of flow patterns along the stream reaches and at springs identified the timing and location of perennial and intermittent flow, and periods of increased evapotranspiration.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Ground Water","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1111/j.1745-6584.2006.00223.x","issn":"0017467X","usgsCitation":"Adams, E., Monroe, S.A., Springer, A.E., Blasch, K., and Bills, D.J., 2006, Electrical resistance sensors record spring flow timing, Grand Canyon, Arizona: Ground Water, v. 44, no. 5, p. 630-641, https://doi.org/10.1111/j.1745-6584.2006.00223.x.","startPage":"630","endPage":"641","numberOfPages":"12","costCenters":[],"links":[{"id":210429,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1111/j.1745-6584.2006.00223.x"},{"id":237342,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"44","issue":"5","noUsgsAuthors":false,"publicationDate":"2006-05-15","publicationStatus":"PW","scienceBaseUri":"505a0894e4b0c8380cd51b9a","contributors":{"authors":[{"text":"Adams, E.A.","contributorId":42411,"corporation":false,"usgs":true,"family":"Adams","given":"E.A.","email":"","affiliations":[],"preferred":false,"id":417488,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Monroe, S. A.","contributorId":90346,"corporation":false,"usgs":true,"family":"Monroe","given":"S.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":417490,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Springer, Abraham E.","contributorId":76278,"corporation":false,"usgs":true,"family":"Springer","given":"Abraham","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":417489,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Blasch, K.W.","contributorId":29877,"corporation":false,"usgs":true,"family":"Blasch","given":"K.W.","affiliations":[],"preferred":false,"id":417487,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Bills, D. J.","contributorId":17610,"corporation":false,"usgs":true,"family":"Bills","given":"D.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":417486,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70028749,"text":"70028749 - 2006 - Damped regional-scale stress inversions: Methodology and examples for southern California and the Coalinga aftershock sequence","interactions":[],"lastModifiedDate":"2012-03-12T17:21:00","indexId":"70028749","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2314,"text":"Journal of Geophysical Research B: Solid Earth","active":true,"publicationSubtype":{"id":10}},"title":"Damped regional-scale stress inversions: Methodology and examples for southern California and the Coalinga aftershock sequence","docAbstract":"We present a new focal mechanism stress inversion technique to produce regional-scale models of stress orientation containing the minimum complexity necessary to fit the data. Current practice is to divide a region into small subareas and to independently fit a stress tensor to the focal mechanisms of each subarea. This procedure may lead to apparent spatial variability that is actually an artifact of overfitting noisy data or nonuniquely fitting data that does not completely constrain the stress tensor. To remove these artifacts while retaining any stress variations that are strongly required by the data, we devise a damped inversion method to simultaneously invert for stress in all subareas while minimizing the difference in stress between adjacent subareas. This method is conceptually similar to other geophysical inverse techniques that incorporate damping, such as seismic tomography. In checkerboard tests, the damped inversion removes the stress rotation artifacts exhibited by an undamped inversion, while resolving sharper true stress rotations than a simple smoothed model or a moving-window inversion. We show an example of a spatially damped stress field for southern California. The methodology can also be used to study temporal stress changes, and an example for the Coalinga, California, aftershock sequence is shown. We recommend use of the damped inversion technique for any study examining spatial or temporal variations in the stress field.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Geophysical Research B: Solid Earth","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1029/2005JB004144","issn":"01480227","usgsCitation":"Hardebeck, J., and Michael, A., 2006, Damped regional-scale stress inversions: Methodology and examples for southern California and the Coalinga aftershock sequence: Journal of Geophysical Research B: Solid Earth, v. 111, no. 11, https://doi.org/10.1029/2005JB004144.","costCenters":[],"links":[{"id":236545,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":209819,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1029/2005JB004144"}],"volume":"111","issue":"11","noUsgsAuthors":false,"publicationDate":"2006-11-29","publicationStatus":"PW","scienceBaseUri":"5059fd60e4b0c8380cd4e7e1","contributors":{"authors":[{"text":"Hardebeck, J.L.","contributorId":98862,"corporation":false,"usgs":true,"family":"Hardebeck","given":"J.L.","email":"","affiliations":[],"preferred":false,"id":419602,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Michael, A.J. 0000-0002-2403-5019","orcid":"https://orcid.org/0000-0002-2403-5019","contributorId":52192,"corporation":false,"usgs":true,"family":"Michael","given":"A.J.","affiliations":[],"preferred":false,"id":419601,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70028374,"text":"70028374 - 2006 - Incised valley fill interpretation for Mississippian Black Hand Sandstone, Appalachian Basin, USA: Implications for glacial eustasy at Kinderhookian-Osagean (Tn2-Tn3) boundary","interactions":[],"lastModifiedDate":"2012-03-12T17:20:53","indexId":"70028374","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3368,"text":"Sedimentary Geology","active":true,"publicationSubtype":{"id":10}},"title":"Incised valley fill interpretation for Mississippian Black Hand Sandstone, Appalachian Basin, USA: Implications for glacial eustasy at Kinderhookian-Osagean (Tn2-Tn3) boundary","docAbstract":"Lower Mississippian strata of east-central Ohio are predominantly fine-grained marine deposits of the Cuyahoga and Logan formations. Within these sediments is the Black Hand Sandstone of the Cuyahoga Formation. The Black Hand Sandstone is a multistory, crossbedded, coarse-grained conglomeratic sandstone. The contact between the Black Hand Sandstone and the subjacent Cuyahoga Formation is sharp and scoured, with intraclasts of the Cuyahoga Formation incorporated into the basal Black Hand Sandstone. The Black Hand Sandstone was previously thought to represent a distributary channel deposit; however, the combination of lithofacies and architectural elements indicates deposition in a braided stream setting. The Cuyahoga Formation was deposited in a shallow marine setting. The erosional basal contact of the Black Hand Sandstone and the juxtaposition of fluvial and marine sediments suggests a sequence boundary. The geographic distribution of the Black Hand Sandstone combined with the evidence for a sequence boundary suggests deposition in an incised valley. The age of the Black Hand Sandstone is key to inferring the causes of valley incision. The Black Hand Sandstone is nearly devoid of body fossils, necessitating a biostratigraphic analysis of the surrounding Cuyahoga and Logan formations. Analysis indicates the Logan Formation is early Osagean age. Data from the Cuyahoga Formation suggest a Kinderhookian age with a possible transition to the Osagean in the uppermost Cuyahoga Formation. This constrains the age of the Black Hand Sandstone to the transition at the Kinderhookian-Osagean boundary. Recent reports indicate late Kinderhookian (Tournaisian, Tn2) Gondwanan glaciation based upon tillites and sharp excursions in stable-isotope curves. A glacio-eustatic fall in sea level is inferred to have caused incision of the Cuyahoga Formation, followed by deposition of the Black Hand Sandstone and Logan Formation during the subsequent sea level rise. The associated unconformity correlates to the sequence boundary at the Kinderhookian-Osagean boundary in the stratotype area of North America, and the correlative Tn2-Tn3 boundary worldwide, supporting the hypothesis of a global eustatic event at this time. ?? 2006 Elsevier B.V. All rights reserved.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Sedimentary Geology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.sedgeo.2006.02.002","issn":"00370738","usgsCitation":"Matchen, D., and Kammer, T.W., 2006, Incised valley fill interpretation for Mississippian Black Hand Sandstone, Appalachian Basin, USA: Implications for glacial eustasy at Kinderhookian-Osagean (Tn2-Tn3) boundary: Sedimentary Geology, v. 191, no. 1-2, p. 89-113, https://doi.org/10.1016/j.sedgeo.2006.02.002.","startPage":"89","endPage":"113","numberOfPages":"25","costCenters":[],"links":[{"id":210379,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.sedgeo.2006.02.002"},{"id":237277,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"191","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a39dfe4b0c8380cd61a7e","contributors":{"authors":[{"text":"Matchen, D.L.","contributorId":44733,"corporation":false,"usgs":true,"family":"Matchen","given":"D.L.","email":"","affiliations":[],"preferred":false,"id":417783,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kammer, T. W.","contributorId":9208,"corporation":false,"usgs":true,"family":"Kammer","given":"T.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":417782,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70028380,"text":"70028380 - 2006 - Spatial patterns of fish communities along two estuarine gradients in southern Florida","interactions":[],"lastModifiedDate":"2014-10-24T15:31:43","indexId":"70028380","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1919,"text":"Hydrobiologia","onlineIssn":"1573-5117","printIssn":"0018-8158","active":true,"publicationSubtype":{"id":10}},"title":"Spatial patterns of fish communities along two estuarine gradients in southern Florida","docAbstract":"In tropical and subtropical estuaries, gradients of primary productivity and salinity are generally invoked to explain patterns in community structure and standing crops of fishes. We documented spatial and temporal patterns in fish community structure and standing crops along salinity and nutrient gradients in two subtropical drainages of Everglades National Park, USA. The Shark River drains into the Gulf of Mexico and experiences diurnal tides carrying relatively nutrient enriched waters, while Taylor River is more hydrologically isolated by the oligohaline Florida Bay and experiences no discernable lunar tides. We hypothesized that the more nutrient enriched system would support higher standing crops of fishes in its mangrove zone. We collected 50 species of fish from January 2000 to April 2004 at six sampling sites spanning fresh to brackish salinities in both the Shark and Taylor River drainages. Contrary to expectations, we observed lower standing crops and density of fishes in the more nutrient rich tidal mangrove forest of the Shark River than in the less nutrient rich mangrove habitats bordering the Taylor River. Tidal mangrove habitats in the Shark River were dominated by salt-tolerant fish and displayed lower species richness than mangrove communities in the Taylor River, which included more freshwater taxa and yielded relatively higher richness. These differences were maintained even after controlling for salinity at the time of sampling. Small-scale topographic relief differs between these two systems, possibly created by tidal action in the Shark River. We propose that this difference in topography limits movement of fishes from upstream marshes into the fringing mangrove forest in the Shark River system, but not the Taylor River system. Understanding the influence of habitat structure, including connectivity, on aquatic communities is important to anticipate effects of construction and operational alternatives associated with restoration of the Everglades ecosystem.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Hydrobiologia","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Springer","doi":"10.1007/s10750-006-0144-x","issn":"00188158","usgsCitation":"Green, D., Trexler, J., Lorenz, J., McIvor, C., and Philippi, T., 2006, Spatial patterns of fish communities along two estuarine gradients in southern Florida: Hydrobiologia, v. 569, no. 1, p. 387-399, https://doi.org/10.1007/s10750-006-0144-x.","productDescription":"13 p.","startPage":"387","endPage":"399","numberOfPages":"13","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"links":[{"id":236822,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":210027,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/s10750-006-0144-x"}],"country":"United States","state":"Florida","otherGeospatial":"Everglades National Park","volume":"569","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b949de4b08c986b31abaa","contributors":{"authors":[{"text":"Green, D.P.J.","contributorId":20963,"corporation":false,"usgs":true,"family":"Green","given":"D.P.J.","email":"","affiliations":[],"preferred":false,"id":417800,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Trexler, J.C.","contributorId":23108,"corporation":false,"usgs":true,"family":"Trexler","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":417801,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lorenz, J.J.","contributorId":67058,"corporation":false,"usgs":true,"family":"Lorenz","given":"J.J.","email":"","affiliations":[],"preferred":false,"id":417803,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"McIvor, C.C.","contributorId":38104,"corporation":false,"usgs":true,"family":"McIvor","given":"C.C.","email":"","affiliations":[],"preferred":false,"id":417802,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Philippi, T.","contributorId":78142,"corporation":false,"usgs":true,"family":"Philippi","given":"T.","affiliations":[],"preferred":false,"id":417804,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
]}