{"pageNumber":"1962","pageRowStart":"49025","pageSize":"25","recordCount":184617,"records":[{"id":70189023,"text":"70189023 - 2010 - Transient electromagnetic mapping of clay units in the San Luis Valley, Colorado","interactions":[],"lastModifiedDate":"2017-09-20T15:04:08","indexId":"70189023","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Transient electromagnetic mapping of clay units in the San Luis Valley, Colorado","docAbstract":"<p>Transient&nbsp;<span>electromagnetic soundings were used to obtain information needed to refine hydrologic models of the San Luis Valley, Colorado. The soundings were able to map an aquitard called the blue clay that separates an unconfined surface aquifer from a deeper confined aquifer. The blue clay forms a conductor with an average resistivity of 6.9 ohm‐m. Above the conductor are found a mixture of gray clay and sand. The gray clay has an average resistivity of 21 ohm‐m, while the sand has a resistivity of greater than 100 ohm‐m. The large difference in resistivity of these units makes mapping them with a surface geophysical method relatively easy. The blue clay was deposited at the bottom of Lake Alamosa which filled most of the San Luis Valley during the Pleistocene. The geometry of the blue clay is influenced by a graben on the eastern side of the valley. The depth to the blue clay is greater over the graben. Along the eastern edge of valley the blue clay appears to be truncated by faults.</span><br></p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Symposium on the Application of Geophysics to Engineering and Environmental Problems 2010","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"Symposium on the Application of Geophysics to Engineering and Environmental Problems 2010","language":"English","publisher":"Society of Exploration Geophysicists","doi":"10.4133/1.3445428","usgsCitation":"Fitterman, D.V., and Grauch, V.J., 2010, Transient electromagnetic mapping of clay units in the San Luis Valley, Colorado, <i>in</i> Symposium on the Application of Geophysics to Engineering and Environmental Problems 2010, p. 154-164, https://doi.org/10.4133/1.3445428.","productDescription":"11 p.","startPage":"154","endPage":"164","ipdsId":"IP-019459","costCenters":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"links":[{"id":343155,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Colorado","otherGeospatial":"San Luis Valley","publishingServiceCenter":{"id":2,"text":"Denver PSC"},"noUsgsAuthors":false,"publicationDate":"2010-05-17","publicationStatus":"PW","scienceBaseUri":"595611c9e4b0d1f9f0506802","contributors":{"authors":[{"text":"Fitterman, David V. dfitterman@usgs.gov","contributorId":1106,"corporation":false,"usgs":true,"family":"Fitterman","given":"David","email":"dfitterman@usgs.gov","middleInitial":"V.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":702461,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Grauch, V. J. S. 0000-0002-0761-3489 tien@usgs.gov","orcid":"https://orcid.org/0000-0002-0761-3489","contributorId":886,"corporation":false,"usgs":true,"family":"Grauch","given":"V.","email":"tien@usgs.gov","middleInitial":"J. S.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":702462,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70189025,"text":"70189025 - 2010 - Specular reflection on Titan: Liquids in Kraken Mare","interactions":[],"lastModifiedDate":"2017-06-29T14:02:00","indexId":"70189025","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1807,"text":"Geophysical Research Letters","active":true,"publicationSubtype":{"id":10}},"title":"Specular reflection on Titan: Liquids in Kraken Mare","docAbstract":"<p><span>After more than 50 close flybys of Titan by the Cassini spacecraft, it has become evident that features similar in morphology to terrestrial lakes and seas exist in Titan's polar regions. As Titan progresses into northern spring, the much more numerous and larger lakes and seas in the north-polar region suggested by Cassini RADAR data, are becoming directly illuminated for the first time since the arrival of the Cassini spacecraft. This allows the Cassini optical instruments to search for specular reflections to provide further confirmation that liquids are present in these evident lakes. On July 8, 2009 Cassini VIMS detected a specular reflection in the north-polar region of Titan associated with Kraken Mare, one of Titan's large, presumed seas, indicating the lake's surface is smooth and free of scatterers with respect to the wavelength of 5&nbsp;</span><i>μ</i><span>m, where VIMS detected the specular signal, strongly suggesting it is liquid.</span></p>","language":"English","publisher":"AGU","doi":"10.1029/2009GL042312","usgsCitation":"Stephan, K., Jaumann, R., Brown, R.H., Soderblom, J.M., Soderblom, L.A., Barnes, J.W., Sotin, C., Griffith, C.A., Kirk, R.L., Baines, K.H., Buratti, B.J., Clark, R.N., Lytle, D.M., Nelson, R.M., and Nicholson, P.D., 2010, Specular reflection on Titan: Liquids in Kraken Mare: Geophysical Research Letters, v. 37, no. 7, p. 1-5, https://doi.org/10.1029/2009GL042312.","productDescription":"Article L07104; 5 p.","startPage":"1","endPage":"5","ipdsId":"IP-020044","costCenters":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"links":[{"id":343137,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"37","issue":"7","publishingServiceCenter":{"id":2,"text":"Denver PSC"},"noUsgsAuthors":false,"publicationDate":"2010-04-07","publicationStatus":"PW","scienceBaseUri":"595611c9e4b0d1f9f0506800","contributors":{"authors":[{"text":"Stephan, Katrin","contributorId":147248,"corporation":false,"usgs":false,"family":"Stephan","given":"Katrin","email":"","affiliations":[],"preferred":false,"id":702610,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jaumann, Ralf","contributorId":147249,"corporation":false,"usgs":false,"family":"Jaumann","given":"Ralf","email":"","affiliations":[],"preferred":false,"id":702611,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brown, Robert H.","contributorId":147246,"corporation":false,"usgs":false,"family":"Brown","given":"Robert","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":702612,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Soderblom, Jason M.","contributorId":193866,"corporation":false,"usgs":false,"family":"Soderblom","given":"Jason","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":702613,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Soderblom, Laurence A. 0000-0002-0917-853X lsoderblom@usgs.gov","orcid":"https://orcid.org/0000-0002-0917-853X","contributorId":2721,"corporation":false,"usgs":true,"family":"Soderblom","given":"Laurence","email":"lsoderblom@usgs.gov","middleInitial":"A.","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":true,"id":702614,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Barnes, Jason W.","contributorId":147251,"corporation":false,"usgs":false,"family":"Barnes","given":"Jason","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":702615,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Sotin, Christophe","contributorId":53924,"corporation":false,"usgs":false,"family":"Sotin","given":"Christophe","email":"","affiliations":[],"preferred":false,"id":702616,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Griffith, Caitlin A.","contributorId":193921,"corporation":false,"usgs":false,"family":"Griffith","given":"Caitlin","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":702617,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Kirk, Randolph L. 0000-0003-0842-9226 rkirk@usgs.gov","orcid":"https://orcid.org/0000-0003-0842-9226","contributorId":2765,"corporation":false,"usgs":true,"family":"Kirk","given":"Randolph","email":"rkirk@usgs.gov","middleInitial":"L.","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":true,"id":702618,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Baines, Kevin H.","contributorId":193922,"corporation":false,"usgs":false,"family":"Baines","given":"Kevin","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":702619,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Buratti, Bonnie J.","contributorId":152192,"corporation":false,"usgs":false,"family":"Buratti","given":"Bonnie","email":"","middleInitial":"J.","affiliations":[{"id":18876,"text":"California Institute of Technology, Jet Propulsion Laboratory","active":true,"usgs":false}],"preferred":false,"id":702620,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Clark, Roger N. 0000-0002-7021-1220 rclark@usgs.gov","orcid":"https://orcid.org/0000-0002-7021-1220","contributorId":515,"corporation":false,"usgs":true,"family":"Clark","given":"Roger","email":"rclark@usgs.gov","middleInitial":"N.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":702621,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Lytle, Dyer M.","contributorId":193923,"corporation":false,"usgs":false,"family":"Lytle","given":"Dyer","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":702622,"contributorType":{"id":1,"text":"Authors"},"rank":13},{"text":"Nelson, Robert M.","contributorId":193924,"corporation":false,"usgs":false,"family":"Nelson","given":"Robert","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":702623,"contributorType":{"id":1,"text":"Authors"},"rank":14},{"text":"Nicholson, Philip D.","contributorId":193925,"corporation":false,"usgs":false,"family":"Nicholson","given":"Philip","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":702624,"contributorType":{"id":1,"text":"Authors"},"rank":15}]}}
,{"id":70189026,"text":"70189026 - 2010 - Are modern geothermal waters in northwest Nevada forming epithermal gold deposits?","interactions":[],"lastModifiedDate":"2017-06-29T14:53:05","indexId":"70189026","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Are modern geothermal waters in northwest Nevada forming epithermal gold deposits?","docAbstract":"<p>Hydrothermal systems currently are active near some gold deposits in northwestern Nevada. Possible links of these modern systems to gold mineralization were evaluated by chemically and isotopically analyzing water samples from the Brady, Dixie Valley, Humboldt House, San Emidio-Empire, Soda Lake, and Wabuska geothermal areas. In addition, quartz veins from Humboldt House and the adjacent Florida Canyon Mine were analyzed to compare ore and gangue phases with those predicted to form from proximal hydrothermal fluids.</p><p>Nearly all water samples are alkali-chloride-type. Total dissolved solids range from 800 to 3900 mg/L, and pH varies from 5.6 to 7.8. Geochemical modeling with SOLVEQ, WATCH, and CHILLER predict the precipitation of silica in all systems during cooling. Anhydrite, calcite, barite, pyrite, base-metal sulfides, and alumino-silicates are variably saturated at calculated reservoir temperatures and also precipitate during boiling/cooling of some fluids. Measured dissolved gold concentrations are low (&lt;0.2<span>μg/L), but are generally consistent with contents predicted by equilibrium of sampled solutions with elemental gold at reservoir temperatures. &nbsp;Although the modern geothermal waters can precipitate ore minerals, the low gold and other ore metal concentrations require very large fluid volumes to form a deposit of economic interest.</span></p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Geological Society of Nevada Symposium, Great Basin Evolution and Metallogeny 2010","largerWorkSubtype":{"id":12,"text":"Conference publication"},"language":"English","publisher":"Geological Society of Nevada","usgsCitation":"Breit, G.N., Hunt, A.G., Wolf, R.E., Koenig, A.E., Fifarek, R., and Coolbaugh, M.F., 2010, Are modern geothermal waters in northwest Nevada forming epithermal gold deposits?, <i>in</i> Geological Society of Nevada Symposium, Great Basin Evolution and Metallogeny 2010, p. 833-844.","productDescription":"12 p.","startPage":"833","endPage":"844","ipdsId":"IP-020129","costCenters":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"links":[{"id":343156,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"publishingServiceCenter":{"id":2,"text":"Denver PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"595611c9e4b0d1f9f05067fe","contributors":{"authors":[{"text":"Breit, George N. 0000-0003-2188-6798 gbreit@usgs.gov","orcid":"https://orcid.org/0000-0003-2188-6798","contributorId":1480,"corporation":false,"usgs":true,"family":"Breit","given":"George","email":"gbreit@usgs.gov","middleInitial":"N.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true},{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":702473,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hunt, Andrew G. 0000-0002-3810-8610 ahunt@usgs.gov","orcid":"https://orcid.org/0000-0002-3810-8610","contributorId":1582,"corporation":false,"usgs":true,"family":"Hunt","given":"Andrew","email":"ahunt@usgs.gov","middleInitial":"G.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":702471,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wolf, Ruth E. rwolf@usgs.gov","contributorId":903,"corporation":false,"usgs":true,"family":"Wolf","given":"Ruth","email":"rwolf@usgs.gov","middleInitial":"E.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":702474,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Koenig, Alan E. 0000-0002-5230-0924 akoenig@usgs.gov","orcid":"https://orcid.org/0000-0002-5230-0924","contributorId":1564,"corporation":false,"usgs":true,"family":"Koenig","given":"Alan","email":"akoenig@usgs.gov","middleInitial":"E.","affiliations":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":702472,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Fifarek, Richard","contributorId":193871,"corporation":false,"usgs":false,"family":"Fifarek","given":"Richard","email":"","affiliations":[],"preferred":false,"id":702476,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Coolbaugh, Mark F.","contributorId":193870,"corporation":false,"usgs":false,"family":"Coolbaugh","given":"Mark","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":702475,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70190465,"text":"70190465 - 2010 - The age of the Steens reversal and the Columbia River Basalt Group","interactions":[],"lastModifiedDate":"2017-08-31T15:48:25","indexId":"70190465","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1213,"text":"Chemical Geology","active":true,"publicationSubtype":{"id":10}},"title":"The age of the Steens reversal and the Columbia River Basalt Group","docAbstract":"<p><span>The Columbia River Basalt Group (CRBG) eruptions have a well-defined relative magnetostratigraphy but have not been definitively correlated to the geomagnetic polarity time scale.&nbsp;</span><sup>40</sup><span>Ar/</span><sup>39</sup><span>Ar ages are presented from lavas erupted in the<span>&nbsp;</span></span><i>R</i><sub>0</sub><span><span>&nbsp;</span>through<span>&nbsp;</span></span><i>N</i><sub>1</sub><span>magnetozones of the CRBG and in the transition between<span>&nbsp;</span></span><i>R</i><sub>0</sub><span><span>&nbsp;</span>and<span>&nbsp;</span></span><i>N</i><sub>0</sub><span>. Four ages from transitionally magnetized lava flows at Steens Mountain, Catlow Peak, and Poker Jim Ridge with a weighted mean age 16.58</span><span>&nbsp;</span><span>±</span><span>&nbsp;</span><span>0.10</span><span>&nbsp;</span><span>Ma</span><a class=\"workspace-trigger\" name=\"bfn1\" href=\"http://www.sciencedirect.com/science/article/pii/S0009254110001221?via%3Dihub#fn1\" data-mce-href=\"http://www.sciencedirect.com/science/article/pii/S0009254110001221?via%3Dihub#fn1\"><sup>1</sup></a><span><span>&nbsp;</span>and the more precise age 16.654</span><span>&nbsp;</span><span>±</span><span>&nbsp;</span><span>0.025</span><span>&nbsp;</span><span>Ma of the normally magnetized Oregon Canyon tuff at the top of the Catlow Peak section show that the oldest CRBG magnetozone (</span><i>R</i><sub>0</sub><span>) correlates with the C5Cr chron. Bayesian statistical analysis applied to data from four flows at Catlow Peak (using the mean age of the Steens reversal) gives a best and preferred age of the Steens reversal of 16.73</span><span>&nbsp;</span><span>+</span><span>&nbsp;</span><span>0.13/−0.08</span><span>&nbsp;</span><span>Ma (95% confidence). Depending on the geomagnetic polarity time scale model, the eruption rate from<span>&nbsp;</span></span><i>N</i><sub>0</sub><span><span>&nbsp;</span>through<span>&nbsp;</span></span><i>R</i><sub>2</sub><span><span>&nbsp;</span>(0.34–0.45</span><span>&nbsp;</span><span>Ma in the middle and the bulk of the CRBG emplacement) averaged 0.30–0.41</span><span>&nbsp;</span><span>km</span><sup>3</sup><span>/a and peaked at a rate 1 1/2 to 4 1/2 times higher during<span>&nbsp;</span></span><i>R</i><sub>2.</sub></p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.chemgeo.2010.04.001","usgsCitation":"Jarboe, N.A., Coe, R.S., Renne, P., and Glen, J.M., 2010, The age of the Steens reversal and the Columbia River Basalt Group: Chemical Geology, v. 274, no. 3-4, p. 158-168, https://doi.org/10.1016/j.chemgeo.2010.04.001.","productDescription":"11 p.","startPage":"158","endPage":"168","ipdsId":"IP-021994","costCenters":[{"id":309,"text":"Geology and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":345397,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"274","issue":"3-4","publishingServiceCenter":{"id":14,"text":"Menlo Park PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"59a92041e4b07e1a023ccdac","contributors":{"authors":[{"text":"Jarboe, Nicholas A.","contributorId":196084,"corporation":false,"usgs":false,"family":"Jarboe","given":"Nicholas","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":709296,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Coe, Robert S.","contributorId":20477,"corporation":false,"usgs":true,"family":"Coe","given":"Robert","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":709297,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Renne, Paul R.","contributorId":47680,"corporation":false,"usgs":false,"family":"Renne","given":"Paul R.","affiliations":[],"preferred":false,"id":709298,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Glen, Jonathan M. G. jglen@usgs.gov","contributorId":1753,"corporation":false,"usgs":true,"family":"Glen","given":"Jonathan","email":"jglen@usgs.gov","middleInitial":"M. G.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":false,"id":709299,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70187016,"text":"70187016 - 2010 - Interpreting canopy water balance and fog screen observations: separating cloud water from wind-blown rainfall at two contrasting forest sites in Hawai'i","interactions":[],"lastModifiedDate":"2017-04-19T10:02:29","indexId":"70187016","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Interpreting canopy water balance and fog screen observations: separating cloud water from wind-blown rainfall at two contrasting forest sites in Hawai'i","docAbstract":"<p>No abstract available.<br></p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Tropical montane cloud forests: science for conservation and management","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Cambridge University Press","usgsCitation":"Giambelluca, T.W., DeLay, J.K., Nullet, M., Scholl, M.A., and Gingerich, S.B., 2010, Interpreting canopy water balance and fog screen observations: separating cloud water from wind-blown rainfall at two contrasting forest sites in Hawai'i, chap. <i>of</i> Tropical montane cloud forests: science for conservation and management, p. 342-352.","productDescription":"11 p.","startPage":"342","endPage":"352","ipdsId":"IP-017121","costCenters":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"links":[{"id":339912,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":339911,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.cambridge.org/catalogue/catalogue.asp?isbn=9780521760355"}],"country":"United 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K.","contributorId":191118,"corporation":false,"usgs":false,"family":"DeLay","given":"J.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":691904,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Nullet, M.A.","contributorId":191119,"corporation":false,"usgs":false,"family":"Nullet","given":"M.A.","affiliations":[],"preferred":false,"id":691905,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Scholl, Martha A. 0000-0001-6994-4614 mascholl@usgs.gov","orcid":"https://orcid.org/0000-0001-6994-4614","contributorId":1920,"corporation":false,"usgs":true,"family":"Scholl","given":"Martha","email":"mascholl@usgs.gov","middleInitial":"A.","affiliations":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":true,"id":691903,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Gingerich, Stephen B. 0000-0002-4381-0746 sbginger@usgs.gov","orcid":"https://orcid.org/0000-0002-4381-0746","contributorId":1426,"corporation":false,"usgs":true,"family":"Gingerich","given":"Stephen","email":"sbginger@usgs.gov","middleInitial":"B.","affiliations":[{"id":525,"text":"Pacific Islands Water Science Center","active":true,"usgs":true},{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"preferred":true,"id":691906,"contributorType":{"id":1,"text":"Authors"},"rank":14}]}}
,{"id":70037717,"text":"70037717 - 2010 - New models for Paleoproterozoic orogenesis in the Cheyenne belt region: Evidence from the geology and U-Pb geochronology of the Big Creek Gneiss, southeastern Wyoming","interactions":[],"lastModifiedDate":"2012-04-30T16:43:36","indexId":"70037717","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1786,"text":"Geological Society of America Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"New models for Paleoproterozoic orogenesis in the Cheyenne belt region: Evidence from the geology and U-Pb geochronology of the Big Creek Gneiss, southeastern Wyoming","docAbstract":"The disputed age of the deep crust of the Colorado Province is central to hypotheses for Paleoproterozoic crustal growth in the region. We studied the high-grade Big Creek Gneiss, southeastern Wyoming, as a potential exposure of pre-1780 Ma basement rocks. New geologic mapping and U-Pb geochronological data indicate that the Big Creek Gneiss exposes a deeper, but coeval, level of the Green Mountain arc relative to the predominantly supracrustal section to the west. The Big Creek Gneiss is composed of: supracrustal rocks; a ca. 1780 Ma Green Mountain arc-correlative, bimodal intrusive suite; a ca. 1763 Ma extensional(?) bimodal intrusive suite; and widespread ca. 1630 Ma pegmatitic leucogranite. The mafic member of the younger bimodal suite is documented here for the first time. U-Pb zircon ages from migmatite leucosomes indicate penetrative deformation of the Big Creek Gneiss at ca. 1750 Ma. We find that the postarc intrusive suite is mantle-involved, implying a second period of crustal growth. Shortening postdates arc magmatism by ~20 m.y., implying that termination of arc magmatism and accretion were separate events. Finally, criteria previously used to constrain the polarity of subduction for the Green Mountain arc are not reliable. We propose two competing models: (1) southward-dipping Green Mountain arc subduction (present coordinates), with slab breakoff-related magmatism following arc accretion; or (2) northward-dipping subduction, with extensional postarc magmatism. In both models, high-temperature deformation coincides with accretion along the Cheyenne belt, and extensional magmatism is an important component of crustal growth. We prefer the northward-dipping subduction model because it can be better integrated with regional tectonic events and published isotopic compositions of the igneous rocks. ?? 2010 Geological Society of America.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Geological Society of America Bulletin","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1130/B30164.1","issn":"00167606","usgsCitation":"Jones, D., Snoke, A., Premo, W.R., and Chamberlain, K., 2010, New models for Paleoproterozoic orogenesis in the Cheyenne belt region: Evidence from the geology and U-Pb geochronology of the Big Creek Gneiss, southeastern Wyoming: Geological Society of America Bulletin, v. 122, no. 11-12, p. 1877-1898, https://doi.org/10.1130/B30164.1.","startPage":"1877","endPage":"1898","numberOfPages":"22","costCenters":[],"links":[{"id":217943,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1130/B30164.1"},{"id":245916,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"122","issue":"11-12","noUsgsAuthors":false,"publicationDate":"2010-08-11","publicationStatus":"PW","scienceBaseUri":"505a65eee4b0c8380cd72ca8","contributors":{"authors":[{"text":"Jones, D.S.","contributorId":48005,"corporation":false,"usgs":true,"family":"Jones","given":"D.S.","email":"","affiliations":[],"preferred":false,"id":462472,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Snoke, A.W.","contributorId":14899,"corporation":false,"usgs":true,"family":"Snoke","given":"A.W.","email":"","affiliations":[],"preferred":false,"id":462470,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Premo, W. R. 0000-0001-9904-4801","orcid":"https://orcid.org/0000-0001-9904-4801","contributorId":22782,"corporation":false,"usgs":true,"family":"Premo","given":"W.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":462471,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Chamberlain, K.R.","contributorId":49546,"corporation":false,"usgs":true,"family":"Chamberlain","given":"K.R.","email":"","affiliations":[],"preferred":false,"id":462473,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70193249,"text":"70193249 - 2010 - Migratory urge and gll Na+,K+-ATPase activity of hatchery-reared Atlantic salmon smolts from the Dennys and Penobscot River stocks, Maine","interactions":[],"lastModifiedDate":"2017-11-15T14:54:59","indexId":"70193249","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3624,"text":"Transactions of the American Fisheries Society","active":true,"publicationSubtype":{"id":10}},"title":"Migratory urge and gll Na+,K+-ATPase activity of hatchery-reared Atlantic salmon smolts from the Dennys and Penobscot River stocks, Maine","docAbstract":"<p><span>Hatchery-reared Atlantic salmon&nbsp;</span><i>Salmo salar</i><span><span>&nbsp;</span>smolts produced from captive-reared Dennys River and sea-run Penobscot River broodstock are released into their source rivers in Maine. The adult return rate of Dennys smolts is comparatively low, and disparity in smolt quality between stocks resulting from genetic or broodstock rearing effects is plausible. Smolt behavior and physiology were assessed during sequential 14-d trials conducted in seminatural annular tanks with circular flow. “Migratory urge” (downstream movement) was monitored remotely using passive integrated transponder tags, and gill Na</span><sup>+</sup><span>,K</span><sup>+</sup><span>-ATPase activity was measured at the beginning and end of the trials to provide an index of smolt development. The migratory urge of both stocks was low in early April, increased 20-fold through late May, and declined by the end of June. The frequency and seasonal distribution of downstream movement were independent of stock. In March and April, initial gill Na</span><sup>+</sup><span>,K</span><sup>+</sup><span>-ATPase activities of Penobscot River smolts were lower than those of Dennys River smolts. For these trials, however, Penobscot River smolts increased enzyme activity after exposure to the tank, whereas Dennys River smolts did not, resulting in similar activities between stocks at the end of all trials. There was no clear relationship between migratory urge and gill Na</span><sup>+</sup><span>,K</span><sup>+</sup><span>-ATPase activity. Gill Na</span><sup>+</sup><span>,K</span><sup>+</sup><span>-ATPase activity of both stocks increased in advance of migratory urge and then declined while migratory urge was increasing. Maximum movement was observed from 2 h after sunset through 1 h after sunrise but varied seasonally. Dennys River smolts were slightly more nocturnal than Penobscot River smolts. These data suggest that Dennys and Penobscot River stocks are not markedly different in either physiological or behavioral expression of smolting.</span></p>","language":"English","publisher":"Taylor & Francis","doi":"10.1577/T09-063.1","usgsCitation":"Spencer, R.C., Zydlewski, J.D., and Zydlewski, G., 2010, Migratory urge and gll Na+,K+-ATPase activity of hatchery-reared Atlantic salmon smolts from the Dennys and Penobscot River stocks, Maine: Transactions of the American Fisheries Society, v. 139, no. 4, p. 947-956, https://doi.org/10.1577/T09-063.1.","productDescription":"10 p.","startPage":"947","endPage":"956","ipdsId":"IP-012456","costCenters":[{"id":199,"text":"Coop Res Unit Leetown","active":true,"usgs":true}],"links":[{"id":348915,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Maine","volume":"139","issue":"4","publishingServiceCenter":{"id":9,"text":"Reston PSC"},"noUsgsAuthors":false,"publicationDate":"2011-01-09","publicationStatus":"PW","scienceBaseUri":"5a610acfe4b06e28e9c256f3","contributors":{"authors":[{"text":"Spencer, Randall C.","contributorId":200424,"corporation":false,"usgs":false,"family":"Spencer","given":"Randall","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":722268,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Zydlewski, Joseph D. 0000-0002-2255-2303 jzydlewski@usgs.gov","orcid":"https://orcid.org/0000-0002-2255-2303","contributorId":2004,"corporation":false,"usgs":true,"family":"Zydlewski","given":"Joseph","email":"jzydlewski@usgs.gov","middleInitial":"D.","affiliations":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true},{"id":199,"text":"Coop Res Unit Leetown","active":true,"usgs":true},{"id":198,"text":"Coop Res Unit Atlanta","active":true,"usgs":true}],"preferred":false,"id":718363,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Zydlewski, Gayle B.","contributorId":139211,"corporation":false,"usgs":false,"family":"Zydlewski","given":"Gayle B.","affiliations":[{"id":12606,"text":"University of Maine, Dept of Plant, Soil, & Envir Sciences","active":true,"usgs":false}],"preferred":false,"id":722269,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70176252,"text":"70176252 - 2010 - Biological community structure on patch reefs in Biscayne National Park, FL, USA","interactions":[],"lastModifiedDate":"2016-09-06T11:34:10","indexId":"70176252","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1552,"text":"Environmental Monitoring and Assessment","onlineIssn":"1573-2959","printIssn":"0167-6369","active":true,"publicationSubtype":{"id":10}},"title":"Biological community structure on patch reefs in Biscayne National Park, FL, USA","docAbstract":"<p><span>Coral reef ecosystem management benefits from continual quantitative assessment of the resources being managed, plus assessment of factors that affect distribution patterns of organisms in the ecosystem. In this study, we investigate the relationships among physical, benthic, and fish variables in an effort to help explain the distribution patterns of organisms on patch reefs within Biscayne National Park, FL, USA. We visited a total of 196 randomly selected sampling stations on 12 shallow (&lt;10&nbsp;m) patch reefs and measured physical variables (e.g., substratum rugosity, substratum type) and benthic and fish community variables. We also incorporated data on substratum rugosity collected remotely via airborne laser surveying (Experimental Advanced Airborne Research Lidar—EAARL). Across all stations, only weak relationships were found between physical, benthic cover, and fish assemblage variables. Much of the variance was attributable to a “reef effect,” meaning that community structure and organism abundances were more variable at stations among reefs than within reefs. However, when the reef effect was accounted for and removed statistically, patterns were detected. Within reefs, juvenile scarids were most abundant at stations with high coverage of the fleshy macroalgae </span><i class=\"EmphasisTypeItalic \">Dictyota</i><span> spp., and the calcified alga </span><i class=\"EmphasisTypeItalic \">Halimeda tuna</i><span> was most abundant at stations with low EAARL rugosity. Explanations for the overwhelming importance of “reef” in explaining variance in our dataset could include the stochastic arrangement of organisms on patch reefs related to variable larval recruitment in space and time and/or strong historical effects due to patchy disturbances (e.g., hurricanes, fishing), as well as legacy effects of prior residents (“priority” effects).</span></p>","language":"English","publisher":"Springer","doi":"10.1007/s10661-009-0910-0","usgsCitation":"Kuffner, I.B., Grober-Dunsmore, R., Brock, J., and Hickey, T.D., 2010, Biological community structure on patch reefs in Biscayne National Park, FL, USA: Environmental Monitoring and Assessment, v. 164, no. 1, p. 513-531, https://doi.org/10.1007/s10661-009-0910-0.","productDescription":"19 p.","startPage":"513","endPage":"531","costCenters":[{"id":574,"text":"St. Petersburg Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":489187,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1007/s10661-009-0910-0","text":"Publisher Index Page"},{"id":328239,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Florida","otherGeospatial":"Biscayne National Park","volume":"164","issue":"1","noUsgsAuthors":false,"publicationDate":"2009-04-28","publicationStatus":"PW","scienceBaseUri":"57cfe8b0e4b04836416a0d2b","contributors":{"authors":[{"text":"Kuffner, Ilsa B. 0000-0001-8804-7847 ikuffner@usgs.gov","orcid":"https://orcid.org/0000-0001-8804-7847","contributorId":3105,"corporation":false,"usgs":true,"family":"Kuffner","given":"Ilsa","email":"ikuffner@usgs.gov","middleInitial":"B.","affiliations":[{"id":574,"text":"St. Petersburg Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":648088,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Grober-Dunsmore, Rikki","contributorId":71292,"corporation":false,"usgs":true,"family":"Grober-Dunsmore","given":"Rikki","email":"","affiliations":[],"preferred":false,"id":648089,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brock, John 0000-0002-5289-9332 jbrock@usgs.gov","orcid":"https://orcid.org/0000-0002-5289-9332","contributorId":2261,"corporation":false,"usgs":true,"family":"Brock","given":"John","email":"jbrock@usgs.gov","affiliations":[{"id":5061,"text":"National Cooperative Geologic Mapping and Landslide Hazards","active":true,"usgs":true}],"preferred":true,"id":648090,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hickey, T. Don","contributorId":49066,"corporation":false,"usgs":true,"family":"Hickey","given":"T.","email":"","middleInitial":"Don","affiliations":[],"preferred":false,"id":648091,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70179316,"text":"70179316 - 2010 - Annual sex steroid and other physiological profiles of Pacific lampreys (<i>Entosphenus tridentatus</i>)","interactions":[],"lastModifiedDate":"2017-05-05T10:14:01","indexId":"70179316","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1289,"text":"Comparative Biochemistry and Physiology, Part A: Molecular & Integrative Physiology","active":true,"publicationSubtype":{"id":10}},"title":"Annual sex steroid and other physiological profiles of Pacific lampreys (<i>Entosphenus tridentatus</i>)","docAbstract":"<p>We documented changes in plasma levels of estradiol 17-β (E2), progesterone (P), 15α-hydroxytestosterone (15α-T), thyroxine (T4), triiodothyronine (T3), protein, triglycerides (TGs), and glucose in adult Pacific lampreys (<i>Entosphenus tridentatus</i>) held in the laboratory in two different years. Levels of E2 in both sexes ranged from 0.5 to 2&nbsp;ng/mL from September to March, peaked in late April (2–4&nbsp;ng/mL), and decreased in May, with levels higher in males than in females. Levels of P were low from September through April, but then increased substantially during May (2–4&nbsp;ng/mL), with levels again highest in males. Levels of 15α-T in males were around 0.75&nbsp;ng/mL through the winter before exceeding 1&nbsp;ng/mL in April and decreasing thereafter, whereas females showed a gradual increase from 0.25&nbsp;ng/mL in November to 0.5&nbsp;ng/mL in April before decreasing. Thyroxine concentrations differed between fish in each year, with most having levels ranging from 0.75 to 2.5&nbsp;ng/mL in the fall and winter, and only fish in 2003 showing distinct peaks (3–4&nbsp;ng/mL) in early April or May. Plasma T3 was undetectable from November through mid-March before surging dramatically in April (ca. 150&nbsp;ng/mL) and decreasing thereafter. Levels of protein, TGs, and glucose decreased or were stable during the fall and winter with TGs and glucose surging in late April to early May for some fish. Our study is the first to document long-term physiological changes in Pacific lampreys during overwintering and sexual maturation and increases our understanding of the life history of this unique fish.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.cbpa.2009.09.019","usgsCitation":"Mesa, M.G., Bayer, J.M., Bryan, M.B., and Sower, S.A., 2010, Annual sex steroid and other physiological profiles of Pacific lampreys (<i>Entosphenus tridentatus</i>): Comparative Biochemistry and Physiology, Part A: Molecular & Integrative Physiology, v. 155, no. 1, p. 56-63, https://doi.org/10.1016/j.cbpa.2009.09.019.","productDescription":"8 p. ","startPage":"56","endPage":"63","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":332585,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"155","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5864dd53e4b0cd2dabe7c1d7","contributors":{"authors":[{"text":"Mesa, Matthew G. mmesa@usgs.gov","contributorId":3423,"corporation":false,"usgs":true,"family":"Mesa","given":"Matthew","email":"mmesa@usgs.gov","middleInitial":"G.","affiliations":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"preferred":true,"id":656734,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bayer, Jennifer M. 0000-0001-9564-3110 jbayer@usgs.gov","orcid":"https://orcid.org/0000-0001-9564-3110","contributorId":3393,"corporation":false,"usgs":true,"family":"Bayer","given":"Jennifer","email":"jbayer@usgs.gov","middleInitial":"M.","affiliations":[{"id":5077,"text":"Northwest Regional Director's Office","active":true,"usgs":true},{"id":5067,"text":"Northeast Regional Director's Office","active":true,"usgs":true},{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"preferred":true,"id":656735,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bryan, Mara B.","contributorId":19863,"corporation":false,"usgs":true,"family":"Bryan","given":"Mara","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":656736,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Sower, Stacia A.","contributorId":25109,"corporation":false,"usgs":true,"family":"Sower","given":"Stacia","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":656737,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70179035,"text":"70179035 - 2010 - Management of bacterial kidney disease in Chinook Salmon hatcheries based on broodstock testing by enzyme-linked immunosorbent assay: A multiyear study","interactions":[],"lastModifiedDate":"2017-04-25T16:52:38","indexId":"70179035","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2886,"text":"North American Journal of Fisheries Management","active":true,"publicationSubtype":{"id":10}},"title":"Management of bacterial kidney disease in Chinook Salmon hatcheries based on broodstock testing by enzyme-linked immunosorbent assay: A multiyear study","docAbstract":"<p><span>From the mid-1980s through the early 1990s, outbreaks of bacterial kidney disease (BKD) caused by </span><i>Renibacterium salmoninarum</i><span> continued in Chinook salmon </span><i>Oncorhynchus tshawytscha</i><span> in Idaho Department of Fish and Game (IDFG) hatcheries despite the use of three control methods: (1) injection of returning adult fish with erythromycin to reduce prespawning BKD mortality and limit vertical transmission of </span><i>R. salmoninarum</i><span>, (2) topical disinfection of green eggs with iodophor, and (3) prophylactic treatments of juvenile fish with erythromycin-medicated feed. In addition, programs to manage BKD through measurement of </span><i>R. salmoninarum</i><span> antigen levels in kidney tissues from spawning female Chinook salmon by an enzyme-linked immunosorbent assay (ELISA) were tested over 13–15 brood years at three IDFG hatcheries. The ELISA results were used for either (1) segregated rearing of progeny from females with high ELISA optical density (OD) values (usually ≥0.25), which are indicative of high </span><i>R. salmoninarum</i><span> antigen levels, or (2) culling of eggs from females with high ELISA OD values. The ELISA-based culling program had the most profound positive effects on the study populations. Mortality of juvenile fish during rearing was significantly lower at each hatchery for brood years derived from culling compared with brood years for which culling was not practiced. The prevalence of </span><i>R. salmoninarum</i><span> in juvenile fish, as evidenced by detection of the bacterium in kidney smears by the direct fluorescent antibody test, also decreased significantly at each hatchery. In addition, the proportions of returning adult females with kidney ELISA OD values of 0.25 or more decreased 56–85% for fish reared in brood years during which culling was practiced, whereas the proportions of ELISA-negative adults increased 55–58%. This management strategy may allow IDFG Chinook salmon hatcheries to reduce or eliminate prophylactic erythromycin-medicated feed treatments. We recommend using ELISA-based management of BKD in Chinook salmon hatcheries where it is a concern.</span></p>","language":"English","publisher":"Taylor and Francis","doi":"10.1577/M09-044.1","usgsCitation":"Munson, A.D., Elliott, D.G., and Johnson, K., 2010, Management of bacterial kidney disease in Chinook Salmon hatcheries based on broodstock testing by enzyme-linked immunosorbent assay: A multiyear study: North American Journal of Fisheries Management, v. 30, no. 4, p. 940-955, https://doi.org/10.1577/M09-044.1.","productDescription":"16 p.","startPage":"940","endPage":"955","ipdsId":"IP-013578","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":332086,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"30","issue":"4","noUsgsAuthors":false,"publicationDate":"2010-08-01","publicationStatus":"PW","scienceBaseUri":"585116bce4b08138bf1abd5c","contributors":{"authors":[{"text":"Munson, A. Douglas","contributorId":177446,"corporation":false,"usgs":false,"family":"Munson","given":"A.","email":"","middleInitial":"Douglas","affiliations":[],"preferred":false,"id":655838,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Elliott, Diane G. 0000-0002-4809-6692 dgelliott@usgs.gov","orcid":"https://orcid.org/0000-0002-4809-6692","contributorId":2947,"corporation":false,"usgs":true,"family":"Elliott","given":"Diane","email":"dgelliott@usgs.gov","middleInitial":"G.","affiliations":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"preferred":true,"id":655839,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Johnson, Keith","contributorId":177448,"corporation":false,"usgs":false,"family":"Johnson","given":"Keith","email":"","affiliations":[],"preferred":false,"id":655840,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70037686,"text":"70037686 - 2010 - Sediment contamination of residential streams in the metropolitan Kansas City area, USA: Part II. whole-sediment toxicity to the amphipod hyalella azteca","interactions":[],"lastModifiedDate":"2018-10-22T10:21:49","indexId":"70037686","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":887,"text":"Archives of Environmental Contamination and Toxicology","active":true,"publicationSubtype":{"id":10}},"title":"Sediment contamination of residential streams in the metropolitan Kansas City area, USA: Part II. whole-sediment toxicity to the amphipod hyalella azteca","docAbstract":"<p>This is the second part of a study that evaluates the influence of nonpoint sources on the sediment quality of five adjacent streams within the metropolitan Kansas City area, central United States. Physical, chemical, and toxicity data (Hyalella azteca 28-day whole-sediment toxicity test) for 29 samples collected in 2003 were used for this evaluation, and the potential causes for the toxic effects were explored. The sediments exhibited a low to moderate toxicity, with five samples identified as toxic to H. azteca. Metals did not likely cause the toxicity based on low concentrations of metals in the pore water and elevated concentrations of acid volatile sulfide in the sediments. Although individual polycyclic aromatic hydrocarbons (PAHs) frequently exceeded effect-based sediment quality guidelines [probable effect concentrations (PECs)], only four of the samples had a PEC quotient (PEC-Q) for total PAHs over 1.0 and only one of these four samples was identified as toxic. For the mean PEC-Q for organochlorine compounds (chlordane, dieldrin, sum DDEs), 4 of the 12 samples with a mean PEC-Q above 1.0 were toxic and 4 of the 8 samples with a mean PEC-Q above 3.0 were toxic. Additionally, four of eight samples were toxic, with a mean PEC-Q above 1.0 based on metals, PAHs, polychlorinated biphenyls (PCBs), and organochlorine pesticides. The increase in the incidence of toxicity with the increase in the mean PEC-Q based on organochlorine pesticides or based on metals, PAHs, PCBs, and organochlorine pesticides suggests that organochlorine pesticides might have contributed to the observed toxicity and that the use of a mean PEC-Q, rather than PEC-Qs for individual compounds, might be more informative in predicting toxic effects. Our study shows that stream sediments subject to predominant nonpoint sources contamination can be toxic and that many factors, including analysis of a full suite of PAHs and pesticides of both past and present urban applications and the origins of these organic compounds, are important to identify the causes of toxicity.</p>","language":"English","publisher":"Springer","doi":"10.1007/s00244-010-9498-1","issn":"00904341","usgsCitation":"Tao, J., Ingersoll, C.G., Kemble, N.E., Dias, J., Murowchick, J., Welker, G., and Huggins, D., 2010, Sediment contamination of residential streams in the metropolitan Kansas City area, USA: Part II. whole-sediment toxicity to the amphipod hyalella azteca: Archives of Environmental Contamination and Toxicology, v. 59, no. 3, p. 370-381, https://doi.org/10.1007/s00244-010-9498-1.","productDescription":"12 p.","startPage":"370","endPage":"381","numberOfPages":"12","costCenters":[{"id":34983,"text":"Contaminant Biology Program","active":true,"usgs":true}],"links":[{"id":245926,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":217953,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/s00244-010-9498-1"}],"country":"United States","state":"Kansas, Missouri","city":"Kansas City","volume":"59","issue":"3","noUsgsAuthors":false,"publicationDate":"2010-04-16","publicationStatus":"PW","scienceBaseUri":"505b8967e4b08c986b316dc9","contributors":{"authors":[{"text":"Tao, J.","contributorId":56485,"corporation":false,"usgs":true,"family":"Tao","given":"J.","email":"","affiliations":[],"preferred":false,"id":462290,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ingersoll, Christopher G. 0000-0003-4531-5949 cingersoll@usgs.gov","orcid":"https://orcid.org/0000-0003-4531-5949","contributorId":2071,"corporation":false,"usgs":true,"family":"Ingersoll","given":"Christopher","email":"cingersoll@usgs.gov","middleInitial":"G.","affiliations":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"preferred":true,"id":462289,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kemble, Nile E. 0000-0002-3608-0538 nkemble@usgs.gov","orcid":"https://orcid.org/0000-0002-3608-0538","contributorId":2626,"corporation":false,"usgs":true,"family":"Kemble","given":"Nile","email":"nkemble@usgs.gov","middleInitial":"E.","affiliations":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"preferred":true,"id":462286,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Dias, J.R.","contributorId":97748,"corporation":false,"usgs":true,"family":"Dias","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":462291,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Murowchick, J.B.","contributorId":45058,"corporation":false,"usgs":true,"family":"Murowchick","given":"J.B.","email":"","affiliations":[],"preferred":false,"id":462288,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Welker, G.","contributorId":21390,"corporation":false,"usgs":true,"family":"Welker","given":"G.","email":"","affiliations":[],"preferred":false,"id":462285,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Huggins, D.","contributorId":29250,"corporation":false,"usgs":true,"family":"Huggins","given":"D.","email":"","affiliations":[],"preferred":false,"id":462287,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70009655,"text":"70009655 - 2010 - Regional estimates of ecological services derived from U.S. Department of Agriculture conservation programs in the Mississippi Alluvial Valley","interactions":[],"lastModifiedDate":"2014-12-16T13:22:17","indexId":"70009655","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesNumber":"143-013599","title":"Regional estimates of ecological services derived from U.S. Department of Agriculture conservation programs in the Mississippi Alluvial Valley","docAbstract":"<p>The Mississippi Alluvial Valley (MAV) is the Nation?s largest floodplain and this once predominantly forested ecosystem provided significant habitat for a diverse flora and fauna, sequestered carbon in trees and soil, and stored floodwater, sediments, and nutrients within the floodplain. This landscape has been substantially altered by the conversion of nearly 75% of the riparian forests, predominantly to agricultural cropland, with significant loss and degradation of important ecosystem services. Large-scale efforts have been employed to restore the forest and wetland resources and the U.S. Department of Agriculture (USDA) Wetlands Reserve Program (WRP) and Conservation Reserve Program (CRP) represent some of the most extensive restoration programs in the MAV. The objective of the WRP is to restore and protect the functions and values of wetlands in agricultural landscapes with an emphasis on habitat for migratory birds and wetland-dependent wildlife, protection and improvement of water quality, flood attenuation, ground water recharge, protection of native flora and fauna, and educational and scientific scholarship.</p>\n<p>&nbsp;</p>\n<p>The degree to which these conservation practices can restore ecosystem functions and services is not well known. This project was initiated to quantify existing ecological services derived from USDA conservation practices in the MAV as part of the USDA Conservation Effects Assessment Project, Wetlands Component (CEAP-Wetlands). The U.S. Geological Survey (USGS), in collaboration with the USDA Natural Resources Conservation Service, the USDA Farm Service Agency, the U.S. Fish and Wildlife Service, and Ducks Unlimited, collected data on soils, vegetation, nitrogen cycling, migratory birds, and amphibians from 88 different sites between 2006 and 2008. Results from restored WRP sites were compared to baseline data from active agricultural cropland (AG) to evaluate changes in ecosystem services.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"NRCS","largerWorkSubtype":{"id":1,"text":"Federal Government Series"},"language":"English","publisher":"U.S. Department of Agriculture Natural Resources Conservation Service","usgsCitation":"Faulkner, S.P., Baldwin, M., Barrow, W., Waddle, H., Keeland, B.D., Walls, S.C., James, D., and Moorman, T., 2010, Regional estimates of ecological services derived from U.S. Department of Agriculture conservation programs in the Mississippi Alluvial Valley, vi, 97 p.","productDescription":"vi, 97 p.","numberOfPages":"103","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-018884","costCenters":[{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true}],"links":[{"id":296719,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":296718,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://www.nrcs.usda.gov/Internet/FSE_DOCUMENTS/nrcs143_013599.pdf"}],"country":"United States","state":"Arkansas, Kentucky, Louisiana, Mississippi, Missouri, Tennessee","otherGeospatial":"Mississippi Alluvial River Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -92.30712890625,\n              29.132970130878636\n            ],\n            [\n              -92.30712890625,\n              38.08268954483802\n            ],\n            [\n              -87.82470703125,\n              38.08268954483802\n            ],\n            [\n              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J.","email":"baldwinm@usgs.gov","affiliations":[{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true}],"preferred":true,"id":536816,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Barrow, Wylie C. 0000-0003-4671-2823 barroww@usgs.gov","orcid":"https://orcid.org/0000-0003-4671-2823","contributorId":1988,"corporation":false,"usgs":true,"family":"Barrow","given":"Wylie C.","email":"barroww@usgs.gov","affiliations":[{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true}],"preferred":false,"id":536817,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Waddle, Hardin 0000-0003-1940-2133 waddleh@usgs.gov","orcid":"https://orcid.org/0000-0003-1940-2133","contributorId":2911,"corporation":false,"usgs":true,"family":"Waddle","given":"Hardin","email":"waddleh@usgs.gov","affiliations":[{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true}],"preferred":false,"id":536818,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Keeland, Bobby D.","contributorId":103506,"corporation":false,"usgs":true,"family":"Keeland","given":"Bobby","email":"","middleInitial":"D.","affiliations":[{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true},{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"preferred":true,"id":536819,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Walls, Susan C. 0000-0001-7391-9155 swalls@usgs.gov","orcid":"https://orcid.org/0000-0001-7391-9155","contributorId":2310,"corporation":false,"usgs":true,"family":"Walls","given":"Susan","email":"swalls@usgs.gov","middleInitial":"C.","affiliations":[{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true}],"preferred":false,"id":536820,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"James, Dale","contributorId":119281,"corporation":false,"usgs":false,"family":"James","given":"Dale","email":"","affiliations":[],"preferred":false,"id":513853,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Moorman, Tom","contributorId":118293,"corporation":false,"usgs":false,"family":"Moorman","given":"Tom","email":"","affiliations":[],"preferred":false,"id":513852,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":70037671,"text":"70037671 - 2010 - The effect of predation on stunted and nonstunted white perch","interactions":[],"lastModifiedDate":"2012-04-30T16:43:33","indexId":"70037671","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1471,"text":"Ecology of Freshwater Fish","active":true,"publicationSubtype":{"id":10}},"title":"The effect of predation on stunted and nonstunted white perch","docAbstract":"Predation is widely regarded as a means to prevent or minimise the establishment of a stunted (high density of slow growing individuals) population. We investigated the effect of predation on two different white perch Morone americana populations (stunted and nonstunted) by examining the stomach contents of piscivorous fishes. White perch and gizzard shad dominated piscivore diets in Branched Oak Lake, whereas white perch dominated piscivore diets in Pawnee Lake. White perch consumed in the stunted population (Branched Oak Lake) were larger and older than white perch consumed in the nonstunted population (Pawnee Lake). Many of the consumed white perch in the stunted population were sexually mature and had the opportunity to spawn at least once. In contrast, all of the consumed white perch in the nonstunted population were sexually immature. Predation may have reinforced the stunting of white perch in Branched Oak Lake through removal of the largest, oldest individuals. ?? 2010 John Wiley & Sons A/S.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Ecology of Freshwater Fish","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1111/j.1600-0633.2010.00423.x","issn":"09066691","usgsCitation":"Gosch, N., Pierce, L., and Pope, K., 2010, The effect of predation on stunted and nonstunted white perch: Ecology of Freshwater Fish, v. 19, no. 3, p. 401-407, https://doi.org/10.1111/j.1600-0633.2010.00423.x.","startPage":"401","endPage":"407","numberOfPages":"7","costCenters":[],"links":[{"id":218054,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1111/j.1600-0633.2010.00423.x"},{"id":246034,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"19","issue":"3","noUsgsAuthors":false,"publicationDate":"2010-08-15","publicationStatus":"PW","scienceBaseUri":"505bab3de4b08c986b322cfb","contributors":{"authors":[{"text":"Gosch, N.J.C.","contributorId":66513,"corporation":false,"usgs":true,"family":"Gosch","given":"N.J.C.","email":"","affiliations":[],"preferred":false,"id":462210,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pierce, L.L.","contributorId":27220,"corporation":false,"usgs":true,"family":"Pierce","given":"L.L.","email":"","affiliations":[],"preferred":false,"id":462209,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Pope, K.L.","contributorId":20454,"corporation":false,"usgs":true,"family":"Pope","given":"K.L.","email":"","affiliations":[],"preferred":false,"id":462208,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70037669,"text":"70037669 - 2010 - GIS-based spatial regression and prediction of water quality in river networks: A case study in Iowa","interactions":[],"lastModifiedDate":"2012-04-30T16:43:33","indexId":"70037669","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2258,"text":"Journal of Environmental Management","active":true,"publicationSubtype":{"id":10}},"title":"GIS-based spatial regression and prediction of water quality in river networks: A case study in Iowa","docAbstract":"Nonpoint source pollution is the leading cause of the U.S.'s water quality problems. One important component of nonpoint source pollution control is an understanding of what and how watershed-scale conditions influence ambient water quality. This paper investigated the use of spatial regression to evaluate the impacts of watershed characteristics on stream NO3NO2-N concentration in the Cedar River Watershed, Iowa. An Arc Hydro geodatabase was constructed to organize various datasets on the watershed. Spatial regression models were developed to evaluate the impacts of watershed characteristics on stream NO3NO2-N concentration and predict NO3NO2-N concentration at unmonitored locations. Unlike the traditional ordinary least square (OLS) method, the spatial regression method incorporates the potential spatial correlation among the observations in its coefficient estimation. Study results show that NO3NO2-N observations in the Cedar River Watershed are spatially correlated, and by ignoring the spatial correlation, the OLS method tends to over-estimate the impacts of watershed characteristics on stream NO3NO2-N concentration. In conjunction with kriging, the spatial regression method not only makes better stream NO3NO2-N concentration predictions than the OLS method, but also gives estimates of the uncertainty of the predictions, which provides useful information for optimizing the design of stream monitoring network. It is a promising tool for better managing and controlling nonpoint source pollution. ?? 2010 Elsevier Ltd.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Environmental Management","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.jenvman.2010.04.011","issn":"03014797","usgsCitation":"Yang, X., and Jin, W., 2010, GIS-based spatial regression and prediction of water quality in river networks: A case study in Iowa: Journal of Environmental Management, v. 91, no. 10, p. 1943-1951, https://doi.org/10.1016/j.jenvman.2010.04.011.","startPage":"1943","endPage":"1951","numberOfPages":"9","costCenters":[],"links":[{"id":218052,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.jenvman.2010.04.011"},{"id":246032,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"91","issue":"10","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a146ce4b0c8380cd54a1e","contributors":{"authors":[{"text":"Yang, X.","contributorId":66894,"corporation":false,"usgs":true,"family":"Yang","given":"X.","email":"","affiliations":[],"preferred":false,"id":462200,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jin, W.","contributorId":27682,"corporation":false,"usgs":true,"family":"Jin","given":"W.","email":"","affiliations":[],"preferred":false,"id":462199,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70037712,"text":"70037712 - 2010 - Dacite petrogenesis on mid-ocean ridges: Evidence for oceanic crustal melting and assimilation","interactions":[],"lastModifiedDate":"2012-04-30T16:43:34","indexId":"70037712","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","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":"Dacite petrogenesis on mid-ocean ridges: Evidence for oceanic crustal melting and assimilation","docAbstract":"Whereas the majority of eruptions at oceanic spreading centers produce lavas with relatively homogeneous mid-ocean ridge basalt (MORB) compositions, the formation of tholeiitic andesites and dacites at mid-ocean ridges (MORs) is a petrological enigma. Eruptions of MOR high-silica lavas are typically associated with ridge discontinuities and have produced regionally significant volumes of lava. Andesites and dacites have been observed and sampled at several locations along the global MOR system; these include propagating ridge tips at ridge-transform intersections on the Juan de Fuca Ridge and eastern Gal??pagos spreading center, and at the 9??N overlapping spreading center on the East Pacific Rise. Despite the formation of these lavas at various ridges, MOR dacites show remarkably similar major element trends and incompatible trace element enrichments, suggesting that similar processes are controlling their chemistry. Although most geochemical variability in MOR basalts is consistent with low-pressure fractional crystallization of various mantle-derived parental melts, our geochemical data for MOR dacitic glasses suggest that contamination from a seawater-altered component is important in their petrogenesis. MOR dacites are characterized by elevated U, Th, Zr, and Hf, low Nb and Ta concentrations relative to rare earth elements (REE), and Al2O3, K2O, and Cl concentrations that are higher than expected from low-pressure fractional crystallization alone. Petrological modeling of MOR dacites suggests that partial melting and assimilation are both integral to their petrogenesis. Extensive fractional crystallization of a MORB parent combined with partial melting and assimilation of amphibole-bearing altered crust produces a magma with a geochemical signature similar to a MOR dacite. This supports the hypothesis that crustal assimilation is an important process in the formation of highly evolved MOR lavas and may be significant in the generation of evolved MORB in general. Additionally, these processes are likely to be more common in regions of episodic magma supply and enhanced magma-crust interaction such as at the ends of ridge segments. ?? The Author 2010. Published by Oxford University Press. All rights reserved.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Petrology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1093/petrology/egq056","issn":"00223530","usgsCitation":"Wanless, V., Perfit, M., Ridley, W., and Klein, E., 2010, Dacite petrogenesis on mid-ocean ridges: Evidence for oceanic crustal melting and assimilation: Journal of Petrology, v. 51, no. 12, p. 2377-2410, https://doi.org/10.1093/petrology/egq056.","startPage":"2377","endPage":"2410","numberOfPages":"34","costCenters":[],"links":[{"id":475859,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1093/petrology/egq056","text":"Publisher Index Page"},{"id":245887,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":217914,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1093/petrology/egq056"}],"volume":"51","issue":"12","noUsgsAuthors":false,"publicationDate":"2010-12-02","publicationStatus":"PW","scienceBaseUri":"5059fd57e4b0c8380cd4e7ab","contributors":{"authors":[{"text":"Wanless, V.D.","contributorId":30487,"corporation":false,"usgs":true,"family":"Wanless","given":"V.D.","email":"","affiliations":[],"preferred":false,"id":462446,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Perfit, M.R.","contributorId":45467,"corporation":false,"usgs":true,"family":"Perfit","given":"M.R.","email":"","affiliations":[],"preferred":false,"id":462447,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ridley, W.I.","contributorId":72122,"corporation":false,"usgs":true,"family":"Ridley","given":"W.I.","email":"","affiliations":[],"preferred":false,"id":462448,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Klein, E.","contributorId":97356,"corporation":false,"usgs":true,"family":"Klein","given":"E.","email":"","affiliations":[],"preferred":false,"id":462449,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70034551,"text":"70034551 - 2010 - Modeling fire severity in black spruce stands in the Alaskan boreal forest using spectral and non-spectral geospatial data","interactions":[],"lastModifiedDate":"2017-11-22T11:30:36","indexId":"70034551","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3254,"text":"Remote Sensing of Environment","printIssn":"0034-4257","active":true,"publicationSubtype":{"id":10}},"title":"Modeling fire severity in black spruce stands in the Alaskan boreal forest using spectral and non-spectral geospatial data","docAbstract":"<p><span>Biomass burning in the Alaskan interior is already a major disturbance and source of carbon emissions, and is likely to increase in response to the warming and drying predicted for the future climate. In addition to quantifying changes to the spatial and temporal patterns of burned areas, observing variations in severity is the key to studying the impact of changes to the fire regime on carbon cycling, energy budgets, and post-fire succession. Remote sensing indices of fire severity have not consistently been well-correlated with in situ observations of important severity characteristics in Alaskan black spruce stands, including depth of burning of the surface organic layer. The incorporation of ancillary data such as in situ observations and GIS layers with spectral data from Landsat TM/ETM+ greatly improved efforts to map the reduction of the organic layer in burned black spruce stands. Using a regression tree approach, the R2 of the organic layer depth reduction models was 0.60 and 0.55 (pb0.01) for relative and absolute depth reduction, respectively. All of the independent variables used by the regression tree to estimate burn depth can be obtained independently of field observations. Implementation of a gradient boosting algorithm improved the R2 to 0.80 and 0.79 (pb0.01) for absolute and relative organic layer depth reduction, respectively. Independent variables used in the regression tree model of burn depth included topographic position, remote sensing indices related to soil and vegetation characteristics, timing of the fire event, and meteorological data. Post-fire organic layer depth characteristics are determined for a large (N200,000 ha) fire to identify areas that are potentially vulnerable to a shift in post-fire succession. This application showed that 12% of this fire event experienced fire severe enough to support a change in post-fire succession. We conclude that non-parametric models and ancillary data are useful in the modeling of the surface organic layer fire depth. Because quantitative differences in post-fire surface characteristics do not directly influence spectral properties, these modeling techniques provide better information than the use of remote sensing data alone.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.rse.2010.02.001","issn":"00344257","usgsCitation":"Barrett, K.M., Kasischke, E., McGuire, A., Turetsky, M., and Kane, E., 2010, Modeling fire severity in black spruce stands in the Alaskan boreal forest using spectral and non-spectral geospatial data: Remote Sensing of Environment, v. 114, no. 7, p. 1494-1503, https://doi.org/10.1016/j.rse.2010.02.001.","productDescription":"10 p.","startPage":"1494","endPage":"1503","numberOfPages":"10","ipdsId":"IP-018226","costCenters":[{"id":118,"text":"Alaska Science Center Geography","active":true,"usgs":true}],"links":[{"id":243722,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":215887,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.rse.2010.02.001"}],"volume":"114","issue":"7","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a5bf8e4b0c8380cd6f937","contributors":{"authors":[{"text":"Barrett, Kirsten M. kbarrett@usgs.gov","contributorId":2979,"corporation":false,"usgs":true,"family":"Barrett","given":"Kirsten","email":"kbarrett@usgs.gov","middleInitial":"M.","affiliations":[],"preferred":true,"id":446347,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kasischke, E.S.","contributorId":61201,"corporation":false,"usgs":true,"family":"Kasischke","given":"E.S.","email":"","affiliations":[],"preferred":false,"id":446349,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McGuire, A. D.","contributorId":16552,"corporation":false,"usgs":true,"family":"McGuire","given":"A. D.","affiliations":[],"preferred":false,"id":446346,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Turetsky, M.R.","contributorId":107470,"corporation":false,"usgs":true,"family":"Turetsky","given":"M.R.","email":"","affiliations":[],"preferred":false,"id":446350,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Kane, E.S.","contributorId":42275,"corporation":false,"usgs":true,"family":"Kane","given":"E.S.","email":"","affiliations":[],"preferred":false,"id":446348,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70037711,"text":"70037711 - 2010 - Diversity in destinations, routes and timing of small adult and sub-adult striped bass Morone saxatilis on their southward autumn migration","interactions":[],"lastModifiedDate":"2017-05-18T12:54:39","indexId":"70037711","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2285,"text":"Journal of Fish Biology","active":true,"publicationSubtype":{"id":10}},"title":"Diversity in destinations, routes and timing of small adult and sub-adult striped bass Morone saxatilis on their southward autumn migration","docAbstract":"<p><span>Almost three-quarters of the 46 young adult and sub-adult striped bass<span class=\"Apple-converted-space\">&nbsp;</span></span><i>Morone saxatilis</i><span><span class=\"Apple-converted-space\">&nbsp;</span>that were acoustically tagged in Plum Island Estuary, Massachusetts, U.S.A., in the summer of 2006 were detected in one or more southern coastal arrays during their autumn migration. On the basis of the trajectories along which these<span class=\"Apple-converted-space\">&nbsp;</span></span><i>M. saxatilis</i><span><span class=\"Apple-converted-space\">&nbsp;</span>moved from feeding to overwintering areas, three migratory groups emerged. After leaving Plum Island Estuary, about half of the fish were detected only in a mid-latitude array, Long Island Sound. The other half of the tagged fish were detected during autumn and winter in a more southern array, the Delaware Estuary. This latter group of fish may have used two routes. Some travelled to the Delaware Estuary through Long Island Sound while other fish may have taken a second, more direct, coastal route that did not include Long Island Sound. Consequently, a seemingly homogeneous group of fish tagged at the same time in the same non-natal feeding location exhibited a diversity of southward movement patterns that could affect population-level processes. These three groups that differed in overwintering location and migration route could be movement contingents with migratory connectivity.</span></p>","language":"English","publisher":"Wiley-Blackwell Publishing Ltd.","doi":"10.1111/j.1095-8649.2010.02811.x","issn":"00221112","usgsCitation":"Mather, M.E., Finn, J.T., Pautzke, S.M., Fox, D.A., Savoy, T., Brundage, H.M., Deegan, L.A., and Muth, R.M., 2010, Diversity in destinations, routes and timing of small adult and sub-adult striped bass Morone saxatilis on their southward autumn migration: Journal of Fish Biology, v. 77, no. 10, p. 2326-2337, https://doi.org/10.1111/j.1095-8649.2010.02811.x.","productDescription":"12 p.","startPage":"2326","endPage":"2337","numberOfPages":"12","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-013398","costCenters":[{"id":199,"text":"Coop Res Unit 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III","contributorId":69827,"corporation":false,"usgs":false,"family":"Brundage","given":"Harold","suffix":"III","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":462442,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Deegan, Linda A.","contributorId":34094,"corporation":false,"usgs":false,"family":"Deegan","given":"Linda","email":"","middleInitial":"A.","affiliations":[{"id":27818,"text":"The Ecosystems Center, Marine Biological Laboratory. Woods Hole, MA 02543.","active":true,"usgs":false}],"preferred":false,"id":462439,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Muth, Robert M.","contributorId":41682,"corporation":false,"usgs":true,"family":"Muth","given":"Robert","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":462440,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":70009680,"text":"70009680 - 2010 - Tidal freshwater wetland herbivory in Anacostia Park","interactions":[],"lastModifiedDate":"2016-10-19T13:42:29","indexId":"70009680","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":54,"text":"Natural Resource Technical Report","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"NPS/NCR/NCRO/NRTR2010/002","title":"Tidal freshwater wetland herbivory in Anacostia Park","docAbstract":"<p>Herbivory has played a major role in dictating vegetation abundance and species composition at Kingman Marsh in Anacostia Park, Washington, D.C., since restoration of this tidal freshwater wetland was initiated in 2000. In June 2009 an herbivory study was established to document the impacts of resident Canada goose (Branta canadensis maxima) herbivory to vegetation at Kingman Marsh. Sixteen modules consisting of paired exclosed plots and unfenced control plots were constructed. Eight of the modules were installed in vegetated portions of the restoration site that had been protected over time by fencing, while the remaining eight modules were placed in portions of the site that had not been protected over time and were basically unvegetated at the start of the experiment. Since the experiment was designed to determine the impacts of herbivory by resident Canada geese as opposed to other herbivores, exclosure fencing was elevated 0.2 m to permit access by herbivores such as fish and turtles while excluding mature Canada geese. Repeated measures analysis of variance (ANOVA) was used to analyze the differences between paired exclosure and control plots for a number of variables including total vegetative cover. Differences in total vegetative cover were not significant for the baseline data collected in June. By contrast, two months after the old protective fencing was removed from the initially-vegetated areas to allow Canada geese access to the control plots, total vegetative cover had declined dramatically in the initially-vegetated control plots, and differences between paired exclosed and control plots were significant (P = 0.0026). No herbivory by Canada geese or other herbivores such as fish or turtles was observed in the exclosures. These results show that Canada goose herbivory has inflicted significant damage to the native wetland vegetation in the portions of Kingman Marsh that had been refenced and replanted. Significant differences in total vegetative cover were limited to the eight modules installed in areas already vegetated by previous restoration efforts and protected until the start of the study, suggesting that areas of Kingman that are essentially devoid of vegetation would take longer than a growing season to show signs of improvement once goose herbivory impacts have been reduced. </p>","language":"English","publisher":"Department of Interior, National Park Service","publisherLocation":"Washington, D.C.","usgsCitation":"Krafft, C., Hatfield, J.S., and Hammerschlag, R.S., 2010, Tidal freshwater wetland herbivory in Anacostia Park: Natural Resource Technical Report NPS/NCR/NCRO/NRTR2010/002, vii, 28 p.","productDescription":"vii, 28 p.","numberOfPages":"38","ipdsId":"IP-035970","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":329751,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58088689e4b0f497e78e24df","contributors":{"authors":[{"text":"Krafft, Cairn ckrafft@usgs.gov","contributorId":3480,"corporation":false,"usgs":true,"family":"Krafft","given":"Cairn","email":"ckrafft@usgs.gov","affiliations":[],"preferred":true,"id":651406,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hatfield, Jeff S.","contributorId":95187,"corporation":false,"usgs":true,"family":"Hatfield","given":"Jeff","email":"","middleInitial":"S.","affiliations":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"preferred":false,"id":651407,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hammerschlag, Richard S.","contributorId":67206,"corporation":false,"usgs":true,"family":"Hammerschlag","given":"Richard","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":651408,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70179345,"text":"70179345 - 2010 - Juvenile salmonid survival, passage, and egress at McNary Dam during tests of temporary spillway weirs, 2008","interactions":[],"lastModifiedDate":"2016-12-29T11:34:41","indexId":"70179345","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"title":"Juvenile salmonid survival, passage, and egress at McNary Dam during tests of temporary spillway weirs, 2008","docAbstract":"<p>n/a&nbsp;</p>","language":"English","publisher":"U.S. Army Corps of Engineers","usgsCitation":"Adams, N., and Liedtke, T., 2010, Juvenile salmonid survival, passage, and egress at McNary Dam during tests of temporary spillway weirs, 2008.","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":332626,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58662f13e4b0cd2dabe7c4b7","contributors":{"authors":[{"text":"Adams, N.S.","contributorId":93175,"corporation":false,"usgs":true,"family":"Adams","given":"N.S.","affiliations":[],"preferred":false,"id":656857,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Liedtke, T.L.","contributorId":32800,"corporation":false,"usgs":true,"family":"Liedtke","given":"T.L.","email":"","affiliations":[],"preferred":false,"id":656858,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70043937,"text":"70043937 - 2010 - Guidelines for conducting Smolt survival studies in the Columbia River","interactions":[],"lastModifiedDate":"2016-12-28T11:38:07","indexId":"70043937","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"title":"Guidelines for conducting Smolt survival studies in the Columbia River","docAbstract":"For more than a decade, investigators from different research groups in the Pacific Northwest have been using electronic tags to estimate survival of salmonid smolts as they migrate seaward past hydroelectric dams and through impoundments on the Snake and Columbia Rivers. Over the years, they have refined both analytical and field methods associated with such studies. In this collaborative paper, they synthesize years of experience to formulate a set of guidelines that may assist others with the design and execution of survival studies involving smolts during their migratory phase.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":" Tagging, telemetry, and marking measures for monitoring fish populations","language":"English ","publisher":"PNAMP Report","publisherLocation":"Seattle, WA","usgsCitation":"Giorgi, A., Skalski, Pevin, C., Smith, S., Langeslay, M., Perry, R.W., Counihan, T.D., and Bickford, S., 2010, Guidelines for conducting Smolt survival studies in the Columbia River, 22 p.","productDescription":"22 p.","startPage":"47","endPage":"68","ipdsId":"IP-016411","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":332579,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5864dd54e4b0cd2dabe7c1db","contributors":{"authors":[{"text":"Giorgi, Albert Albert","contributorId":120911,"corporation":false,"usgs":true,"family":"Giorgi","given":"Albert","suffix":"Albert","email":"","affiliations":[],"preferred":false,"id":516962,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Skalski, John","contributorId":120021,"corporation":false,"usgs":true,"family":"Skalski","suffix":"John","affiliations":[],"preferred":false,"id":516961,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Pevin, Chuck Chuck","contributorId":119526,"corporation":false,"usgs":true,"family":"Pevin","given":"Chuck","suffix":"Chuck","email":"","affiliations":[],"preferred":false,"id":516960,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Smith, Steve Steve","contributorId":118431,"corporation":false,"usgs":true,"family":"Smith","given":"Steve","suffix":"Steve","email":"","affiliations":[],"preferred":false,"id":656710,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Langeslay, Mike Mike","contributorId":119200,"corporation":false,"usgs":true,"family":"Langeslay","given":"Mike","suffix":"Mike","email":"","affiliations":[],"preferred":false,"id":516959,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Counihan, Timothy D. 0000-0003-4967-6514 tcounihan@usgs.gov","orcid":"https://orcid.org/0000-0003-4967-6514","contributorId":4211,"corporation":false,"usgs":true,"family":"Counihan","given":"Timothy","email":"tcounihan@usgs.gov","middleInitial":"D.","affiliations":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"preferred":true,"id":656711,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Perry, Russell W. 0000-0003-4110-8619 rperry@usgs.gov","orcid":"https://orcid.org/0000-0003-4110-8619","contributorId":2820,"corporation":false,"usgs":true,"family":"Perry","given":"Russell","email":"rperry@usgs.gov","middleInitial":"W.","affiliations":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"preferred":true,"id":656712,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Bickford, Shane","contributorId":177698,"corporation":false,"usgs":false,"family":"Bickford","given":"Shane","email":"","affiliations":[],"preferred":false,"id":656713,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":70197093,"text":"70197093 - 2010 - Pre‐moult patterns of habitat use and moult site selection by Brent Geese Branta bernicla nigricans: Individuals prospect for moult sites ","interactions":[],"lastModifiedDate":"2018-05-17T10:03:15","indexId":"70197093","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1961,"text":"Ibis","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Pre‐moult patterns of habitat use and moult site selection by Brent Geese <i>Branta bernicla nigricans</i>: Individuals prospect for moult sites ","title":"Pre‐moult patterns of habitat use and moult site selection by Brent Geese Branta bernicla nigricans: Individuals prospect for moult sites ","docAbstract":"<p>In environments where habitat quality varies, the mechanism by which individuals assess and select habitats has significant consequences on their spatial distribution and ability to respond to environmental change. Each year, thousands of Black Brent Geese <i>Branta bernicla nigricans</i> migrate to the Teshekpuk Lake Special Area (TLSA), Alaska, to undergo a flightless wing‐moult. Over the last three decades, moulting Brent Geese have changed their distribution within the TLSA, redistributing from inland, freshwater wetlands towards coastal, brackish wetlands. To understand better the mechanism by which Brent Geese select a moult site, as well as reasons behind the long‐term shift of moulting distributions, we examined movements and habitat use of birds marked with GPS‐transmitters during the pre‐moult period. Brent Geese did not generally migrate directly to their moulting site during the pre‐moult period, defined as the time from arrival at the moulting grounds to the onset of flightlessness. Rather, individuals used an average of 3.7 ± 0.6 (se) wetland complexes and travelled a minimum of 95.14 ± 15.84 km during the pre‐moult period. Moreover, 69% of Brent Geese visited their final moult site only to leave and visit other sites before returning for the flightless moult. Brent Geese spent significant time in both inland freshwater and coastal estuarine habitats during the pre‐moult, irrespective of the habitat in which they ultimately moulted. Whereas previous research suggested that Brent Geese choose moult sites based largely upon the experience of previous years, our observations suggest a mechanism of moult site selection whereby Brent Geese ‘prospect’ for moult sites, visiting multiple potential moult sites across varied habitat types, presumably gathering information from each site and correspondingly using this information to choose an appropriate moult site. By allowing individuals to adjust their distributions in response to habitat quality cues that may change annually, such as forage type and availability, prospecting may have influenced the long‐term shift in moulting distributions of Brent Geese in the TLSA<span class=\"smallCaps\">.</span></p>","language":"English","publisher":"Wiley","doi":"10.1111/j.1474-919X.2010.01023.x","usgsCitation":"Lewis, T., Flint, P.L., Schmutz, J.A., and Derksen, D.V., 2010, Pre‐moult patterns of habitat use and moult site selection by Brent Geese Branta bernicla nigricans: Individuals prospect for moult sites : Ibis, v. 152, no. 3, p. 556-568, https://doi.org/10.1111/j.1474-919X.2010.01023.x.","productDescription":"13 p.","startPage":"556","endPage":"568","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":354235,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Teshekpuk Lake Special Area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -159.63134765625,\n              68.67254350285471\n            ],\n            [\n              -150.29296875,\n              68.67254350285471\n            ],\n            [\n              -150.29296875,\n              71.62906907439766\n            ],\n            [\n              -159.63134765625,\n              71.62906907439766\n            ],\n            [\n              -159.63134765625,\n              68.67254350285471\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"152","issue":"3","noUsgsAuthors":false,"publicationDate":"2010-06-15","publicationStatus":"PW","scienceBaseUri":"5afef89de4b0da30c1bfc9c2","contributors":{"authors":[{"text":"Lewis, Tyler 0000-0002-4998-3031 tlewis@usgs.gov","orcid":"https://orcid.org/0000-0002-4998-3031","contributorId":169307,"corporation":false,"usgs":true,"family":"Lewis","given":"Tyler","email":"tlewis@usgs.gov","affiliations":[{"id":117,"text":"Alaska Science Center Biology WTEB","active":true,"usgs":true},{"id":116,"text":"Alaska Science Center Biology MFEB","active":true,"usgs":true}],"preferred":true,"id":735567,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Flint, Paul L. 0000-0002-8758-6993 pflint@usgs.gov","orcid":"https://orcid.org/0000-0002-8758-6993","contributorId":3284,"corporation":false,"usgs":true,"family":"Flint","given":"Paul","email":"pflint@usgs.gov","middleInitial":"L.","affiliations":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":117,"text":"Alaska Science Center Biology WTEB","active":true,"usgs":true}],"preferred":true,"id":735568,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Schmutz, Joel A. 0000-0002-6516-0836 jschmutz@usgs.gov","orcid":"https://orcid.org/0000-0002-6516-0836","contributorId":1805,"corporation":false,"usgs":true,"family":"Schmutz","given":"Joel","email":"jschmutz@usgs.gov","middleInitial":"A.","affiliations":[{"id":117,"text":"Alaska Science Center Biology WTEB","active":true,"usgs":true},{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"preferred":true,"id":735569,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Derksen, Dirk V. dderksen@usgs.gov","contributorId":2269,"corporation":false,"usgs":true,"family":"Derksen","given":"Dirk","email":"dderksen@usgs.gov","middleInitial":"V.","affiliations":[{"id":117,"text":"Alaska Science Center Biology WTEB","active":true,"usgs":true}],"preferred":true,"id":735570,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70139963,"text":"70139963 - 2010 - Effectiveness of post-fire seeding in desert tortoise Critical Habitat following the 2005 Southern Nevada Fire Complex","interactions":[],"lastModifiedDate":"2016-09-09T14:09:18","indexId":"70139963","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"title":"Effectiveness of post-fire seeding in desert tortoise Critical Habitat following the 2005 Southern Nevada Fire Complex","docAbstract":"In June 2005, lightning strikes ignited multiple wildfires in southern Nevada. The Southern Nevada Fire Complex burned more than 32,000 acres of designated desert tortoise Critical Habitat and an additional 403,000 acres of Mojave Desert habitat characterized as potentially suitable for the tortoise. Mortalities of desert tortoises were observed after the fires, but altered habitat is likely to prolong and magnify the impacts of wildfire on desert tortoise populations. To accelerate the re-establishment of plants commonly used by tortoises for food and shelter, the Bureau of Land Management (BLM) distributed seeds of native annual and perennial species in burned areas within desert tortoise Critical Habitat. The U.S. Geological Survey (USGS) established monitoring plots to evaluate broadcast seeding as a means to restore habitat and tortoise activity compared with natural recovery. Within the standard three-year Emergency and Stabilization Response (ESR) monitoring timeline, seeding augmented perennial seed banks by four to six-fold within a year of seed applications compared with unseeded areas. By the end of the three-year monitoring period, seedling densities of seeded perennial species were 33% higher in seeded areas than in unseeded areas, particularly for the disturbance-adapted desert globemallow (Sphaeralcea ambigua) and desert marigold (Baileya multiradiata). Seeded annuals, in contrast, did not increase significantly in seed banks or biomass production, likely due to low seeding rates of these species. Production of non-native annuals that helped carry the fires was not reduced by seeding efforts but instead was strongly correlated with site-specific rainfall, as were native annual species. The short-term vegetation changes measured in seeded areas were not yet associated with a return of tortoise activity to unburned levels. By focusing on a combination of native species that can withstand disturbance conditions, including species that are found in adjacent unburned areas, and increasing seeding rates, broadcast seeding has strong potential to provide herbaceous plants for forage and long-term perennial plant cover to support tortoise recovery in burned habitats.","language":"English","publisher":"Bureau of Land Management","usgsCitation":"DeFalco, L., Drake, K.K., Scoles-Sciulla, S., and Bauer, K.L., 2010, Effectiveness of post-fire seeding in desert tortoise Critical Habitat following the 2005 Southern Nevada Fire Complex, 37 p. .","productDescription":"37 p. ","startPage":"43","endPage":"77","ipdsId":"IP-018386","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":328456,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":328452,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.werc.usgs.gov/ProductDetails.aspx?ID=4854"}],"country":"United States","state":"Nevada ","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -115.213623046875,\n              37.53150992479082\n            ],\n            [\n              -114.9664306640625,\n              36.88401445049676\n            ],\n            [\n              -114.92248535156249,\n              36.79169061907076\n            ],\n            [\n              -114.51599121093749,\n              36.66841891894786\n            ],\n            [\n              -114.0435791015625,\n              36.84006462037767\n            ],\n            [\n              -114.0765380859375,\n              37.67077737288316\n            ],\n            [\n              -115.0762939453125,\n              37.58376576718623\n            ],\n            [\n              -115.213623046875,\n              37.53150992479082\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","publishingServiceCenter":{"id":1,"text":"Sacramento PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57d3dd37e4b0571647d19a50","contributors":{"authors":[{"text":"DeFalco, Lesley ldefalco@usgs.gov","contributorId":139012,"corporation":false,"usgs":true,"family":"DeFalco","given":"Lesley","email":"ldefalco@usgs.gov","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":false,"id":539733,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Drake, K. Kristina 0000-0003-0711-7634 kdrake@usgs.gov","orcid":"https://orcid.org/0000-0003-0711-7634","contributorId":3799,"corporation":false,"usgs":true,"family":"Drake","given":"K.","email":"kdrake@usgs.gov","middleInitial":"Kristina","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":true,"id":539737,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Scoles-Sciulla, S. J.","contributorId":12274,"corporation":false,"usgs":true,"family":"Scoles-Sciulla","given":"S. J.","affiliations":[],"preferred":false,"id":539744,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bauer, Kyla L.","contributorId":139018,"corporation":false,"usgs":false,"family":"Bauer","given":"Kyla","email":"","middleInitial":"L.","affiliations":[{"id":12614,"text":"USGS, Western Ecological Research Center","active":true,"usgs":false}],"preferred":false,"id":539745,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70157176,"text":"70157176 - 2010 - The tectono-stratigraphic framework and evolution of southwestern Maine and southeastern New Hampshire","interactions":[],"lastModifiedDate":"2017-11-05T12:29:18","indexId":"70157176","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"The tectono-stratigraphic framework and evolution of southwestern Maine and southeastern New Hampshire","docAbstract":"<p><span>Five belts of metamorphosed sedimentary and volcanic rocks underlie southwestern Maine and southeastern New Hampshire: Middle Ordovician Falmouth-Brunswick sequence; Middle and Late Ordovician Casco Bay Group, and Late Ordovician to Early Silurian rocks of the Merribuckfred Basin; Late Ordovician to Early Silurian rocks of the East Harpswell Group; Silurian to Early Devonian rocks of the Central Maine Basin; and highly tectonized enigmatic rocks of the Rye complex of uncertain age. Stratigraphic reassessment and new U/Pb zircon ages support a model of east-directed Middle Ordovician subduction beneath Miramichi, a peri-Gondwanan block, and formation of the Falmouth-Brunswick&ndash;Casco Bay volcanic arc complex that is roughly correlative with arc activity on strike in New Brunswick. Passive Late Ordovician sedimentation in a reducing restricted backarc basin followed. Late Ordovician to Early Silurian volcanic rocks and volcanogenic sediments (East Harpswell Group) support west-directed subduction under the Miramichi block. Late Ordovician to Early Silurian turbidites accumulated in the Merribuckfred Basin between the Falmouth-Brunswick&ndash;Casco Bay arc and Ganderia to the east. The collision of Ganderia with the Falmouth Brunswick arc in Late Silurian time represents an early phase of the Acadian orogeny, during which the Merribuckfred rocks were deformed, metamorphosed, intruded, and uplifted. Simultaneously and inboard, the Central Maine Basin received sediment eroded mostly from Laurentia. Later, during the Late Silurian and Early Devonian, uplifted Merribuckfred basin rocks became the major source of sediments for the Central Maine Basin. A later phase of the Acadian orogeny resulted in Middle Devonian deformation, metamorphism, and intrusion of rocks of all six belts.</span></p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"From Rodinia to Pangea: the lithotectonic record of the Appalachian Region","language":"English","publisher":"Geological Society of America","publisherLocation":"Boulder, CO","doi":"10.1130/2010.1206(10)","usgsCitation":"Hussey, A.M., Bothner, W.A., and Alienikoff, J.N., 2010, The tectono-stratigraphic framework and evolution of southwestern Maine and southeastern New Hampshire, chap. <i>of</i> From Rodinia to Pangea: the lithotectonic record of the Appalachian Region, p. 205-230, https://doi.org/10.1130/2010.1206(10).","productDescription":"26 p.","startPage":"205","endPage":"230","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"links":[{"id":308079,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"560bb70ce4b058f706e53f29","contributors":{"editors":[{"text":"Tollo, Richard P.","contributorId":6465,"corporation":false,"usgs":true,"family":"Tollo","given":"Richard","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":572148,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Hussey, Arthur M. II.","contributorId":147611,"corporation":false,"usgs":false,"family":"Hussey","given":"Arthur","suffix":"II.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":572145,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bothner, Wallace A.","contributorId":80270,"corporation":false,"usgs":true,"family":"Bothner","given":"Wallace","email":"","middleInitial":"A.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":572146,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Alienikoff, John N.","contributorId":85078,"corporation":false,"usgs":true,"family":"Alienikoff","given":"John","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":572147,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70157415,"text":"70157415 - 2010 - Guidelines to indirectly measure and enhance detection efficiency of stationary PIT tag interrogation systems in streams","interactions":[],"lastModifiedDate":"2015-09-22T17:02:09","indexId":"70157415","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"seriesNumber":"2010-002","title":"Guidelines to indirectly measure and enhance detection efficiency of stationary PIT tag interrogation systems in streams","docAbstract":"<p><span>With increasing use of passive integrated transponder (PIT) tags and reliance on stationary PIT tag interrogation systems to monitor fish populations, guidelines are offered to inform users how best to use limited funding and human resources to create functional systems that maximize a desired level of detection and precision. The estimators of detection efficiency and their variability as described by Connolly et al. (2008) are explored over a span of likely performance metrics. These estimators were developed to estimate detection efficiency without relying on a known number of fish passing the system. I present graphical displays of the results derived from these estimators to show the potential efficiency and precision to be gained by adding an array or by increasing the number of PIT-tagged fish expected to move past an interrogation system.</span></p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"PNAMP Special Publication: Tagging, Telemetry and Marking Measures for Monitoring Fish Populations: A compendium of new and recent science for use in informing technique and decision modalities","language":"English","publisher":"Pacific Northwest Aquatic Monitoring Partnership","usgsCitation":"Connolly, P., 2010, Guidelines to indirectly measure and enhance detection efficiency of stationary PIT tag interrogation systems in streams, chap. <i>of</i> PNAMP Special Publication: Tagging, Telemetry and Marking Measures for Monitoring Fish Populations: A compendium of new and recent science for use in informing technique and decision modalities, p. 119-125.","productDescription":"7 p.","startPage":"119","endPage":"125","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":308403,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56027bd8e4b03bc34f544852","contributors":{"editors":[{"text":"Wolf, Keith","contributorId":147874,"corporation":false,"usgs":false,"family":"Wolf","given":"Keith","affiliations":[],"preferred":false,"id":573084,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"O’Neal, Jennifer S.","contributorId":147875,"corporation":false,"usgs":false,"family":"O’Neal","given":"Jennifer","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":573085,"contributorType":{"id":2,"text":"Editors"},"rank":2}],"authors":[{"text":"Connolly, Patrick J. 0000-0001-7365-7618 pconnolly@usgs.gov","orcid":"https://orcid.org/0000-0001-7365-7618","contributorId":2920,"corporation":false,"usgs":true,"family":"Connolly","given":"Patrick J.","email":"pconnolly@usgs.gov","affiliations":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"preferred":true,"id":573083,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70193305,"text":"70193305 - 2010 - Assessing the response of the Pamlico Sound, North Carolina, USA to human and climatic disturbances: Management implications","interactions":[],"lastModifiedDate":"2017-11-20T13:52:56","indexId":"70193305","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Assessing the response of the Pamlico Sound, North Carolina, USA to human and climatic disturbances: Management implications","docAbstract":"<p>The Pamlico Sound (PS) with its sub-estuaries is the largest lagoonal ecosystem in the United States. It exhibits periodically strong salinity stratification and an average freshwater residence time of 1 year for the sound proper. This relatively long residence time promotes effective use and cycling of nutrients, allowing the system to support high rates of primary and secondary production, and serve as a vitally important fisheries nursery. This hydrologic characteristic also makes the system highly sensitive to nutrient over-enrichment and eutrophication. The PS is experiencing ecological change in response to increasing human activity and climatic perturbations. Human impacts include a rise in nutrient, sediment, and other pollutant loads that accompany urbanization and agricultural and industrial growth in its watersheds and airsheds. Since the mid-1990s, the PS&nbsp;has witnessed a sudden rise in tropical storm and hurricane impacts, with eight hurricanes and four tropical storms having made landfall in the PS watershed during the 1996 to 2007 period. Each of these storms had unique hydrologic, nutrient, and other pollutant loading effects. In addition, since the early 2000s, the region has experienced record droughts, which are continuing. Variable freshwater discharges from storms and droughts have caused large oscillations in nutrient enrichment, reflected ultimately in differential phytoplankton production, biomass, and community compositional responses. Floodwaters from the two wettest hurricanes, Fran (1996) and Floyd (1999), and from Tropical Storm Ernesto (2006) exerted long-term (months) effects on hydrology, nutrient loads, and algal production. Windy but relatively dry hurricanes, like Irene (1999) and Isabel (2003), caused strong vertical mixing, storm surges, but relatively minor changes in river flow, flushing, and nutrient loads. These contrasting effects are accompanied by biogeochemical (hypoxia, nutrient cycling) and habitat alterations, and associated food web disturbances. Each storm type influenced algal growth and compositional dynamics; however, their respective ecological impacts differed substantially. Changes in hydrologic and wind forcing resulting from changes in frequency and intensity of storms and droughts strongly influence water and habitat quality. These changes must be integrated with nutrient loading/dilution effects when assessing and predicting ecological responses to nutrient and hydrologic variability on this and other large lagoonal ecosystems.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Coastal lagoons: Critical habitats of environmental change","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"CRC Press","isbn":" 978-1-4200-8830-4","usgsCitation":"Paerl, H., Peierls, B., Hall, N.S., Joyner, A.R., Christian, R., Bales, J.D., and Riggs, S., 2010, Assessing the response of the Pamlico Sound, North Carolina, USA to human and climatic disturbances: Management implications, chap. <i>of</i> Coastal lagoons: Critical habitats of environmental change, p. 17-42.","productDescription":"26 p.","startPage":"17","endPage":"42","ipdsId":"IP-004212","costCenters":[{"id":476,"text":"North Carolina Water Science Center","active":true,"usgs":true}],"links":[{"id":349142,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"North Carolina","otherGeospatial":"Pamlico Sound","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -76.59393310546875,\n              34.99625375979014\n            ],\n            [\n              -75.47882080078125,\n              34.99625375979014\n            ],\n            [\n              -75.47882080078125,\n              35.65060102359122\n            ],\n            [\n              -76.59393310546875,\n              35.65060102359122\n            ],\n            [\n              -76.59393310546875,\n              34.99625375979014\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","publishingServiceCenter":{"id":8,"text":"Raleigh PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5a610acee4b06e28e9c256eb","contributors":{"authors":[{"text":"Paerl, H.W.","contributorId":36893,"corporation":false,"usgs":true,"family":"Paerl","given":"H.W.","email":"","affiliations":[],"preferred":false,"id":722876,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Peierls, B.L.","contributorId":65332,"corporation":false,"usgs":true,"family":"Peierls","given":"B.L.","email":"","affiliations":[],"preferred":false,"id":722877,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hall, N. 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