{"pageNumber":"1802","pageRowStart":"45025","pageSize":"25","recordCount":184617,"records":[{"id":70032675,"text":"70032675 - 2011 - New collection records and range extension for the caddisfly Arctopora salmon (Smith, 1969) (Trichoptera: Limnephilidae)","interactions":[],"lastModifiedDate":"2013-03-04T12:59:04","indexId":"70032675","displayToPublicDate":"2011-01-01T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3007,"text":"Pan-Pacific Entomologist","printIssn":"0031-0603","active":true,"publicationSubtype":{"id":10}},"title":"New collection records and range extension for the caddisfly Arctopora salmon (Smith, 1969) (Trichoptera: Limnephilidae)","docAbstract":"[No abstract available]","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Pan-Pacific Entomologist","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Pacific Coast Entomological Society","publisherLocation":"San Francisco, CA","doi":"10.3956/2011-34.1","issn":"00310603","usgsCitation":"Hossack, B.R., Newell, R., and Ruiter, D.E., 2011, New collection records and range extension for the caddisfly Arctopora salmon (Smith, 1969) (Trichoptera: Limnephilidae): Pan-Pacific Entomologist, v. 87, no. 3, p. 206-208, https://doi.org/10.3956/2011-34.1.","productDescription":"3 p.","startPage":"206","endPage":"208","numberOfPages":"3","costCenters":[{"id":481,"text":"Northern Rocky Mountain Science Center","active":true,"usgs":true}],"links":[{"id":241765,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":214077,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.3956/2011-34.1"}],"country":"United States","state":"Idaho;Montana","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -117.07,41.93 ], [ -117.07,48.89 ], [ -103.93,48.89 ], [ -103.93,41.93 ], [ -117.07,41.93 ] ] ] } } ] }","volume":"87","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a6561e4b0c8380cd72b97","contributors":{"authors":[{"text":"Hossack, Blake R. 0000-0001-7456-9564 blake_hossack@usgs.gov","orcid":"https://orcid.org/0000-0001-7456-9564","contributorId":1177,"corporation":false,"usgs":true,"family":"Hossack","given":"Blake","email":"blake_hossack@usgs.gov","middleInitial":"R.","affiliations":[{"id":481,"text":"Northern Rocky Mountain Science Center","active":true,"usgs":true},{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":true,"id":437398,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Newell, Robert L.","contributorId":58109,"corporation":false,"usgs":true,"family":"Newell","given":"Robert L.","affiliations":[],"preferred":false,"id":437400,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ruiter, David E.","contributorId":37835,"corporation":false,"usgs":true,"family":"Ruiter","given":"David","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":437399,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70036729,"text":"70036729 - 2011 - A simple graphical approach to quantitative monitoring of rangelands","interactions":[],"lastModifiedDate":"2013-02-26T18:47:55","indexId":"70036729","displayToPublicDate":"2011-01-01T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3230,"text":"Rangelands","active":true,"publicationSubtype":{"id":10}},"title":"A simple graphical approach to quantitative monitoring of rangelands","docAbstract":"The article reviews graphical interpretation of the four monitoring methods that can be used to generate a variety of indicators of rangeland ecosystem function. Data for all four of the monitoring methods can be recorded on a single data sheet that is designed to be usable by somebody with minimal literacy. Indicators of plant and ground cover are central to most long-term monitoring systems. Plant and ground-cover data inform managers about forage availability, plant community composition and structure, and risk of runoff and erosion. The spatial arrangement of plants at a site in addition to the percent of the ground that is covered by plants is an important determinant of erosion potential. Vertical vegetation structure can be monitored by capturing data on maximum plant height at each stick location. Plant density method can provide an early indicator of future changes in plant cover, forage, quality, and habitat structure.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Rangelands","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Society for Range Management","publisherLocation":"Lawrence, KS","doi":"10.2111/1551-501X-33.4.6","issn":"01900528","usgsCitation":"Riginos, C., Herrick, J.E., Sundaresan, S., Farley, C., and Belnap, J., 2011, A simple graphical approach to quantitative monitoring of rangelands: Rangelands, v. 33, no. 4, p. 6-13, https://doi.org/10.2111/1551-501X-33.4.6.","productDescription":"8 p.","startPage":"6","endPage":"13","costCenters":[{"id":568,"text":"Southwest Biological Science Center","active":true,"usgs":true}],"links":[{"id":475300,"rank":10000,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"http://hdl.handle.net/10150/639818","text":"External Repository"},{"id":245458,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":217507,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.2111/1551-501X-33.4.6"}],"volume":"33","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e58ee4b0c8380cd46e0c","contributors":{"authors":[{"text":"Riginos, C.","contributorId":54437,"corporation":false,"usgs":true,"family":"Riginos","given":"C.","email":"","affiliations":[],"preferred":false,"id":457550,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Herrick, J. E.","contributorId":84709,"corporation":false,"usgs":true,"family":"Herrick","given":"J.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":457552,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sundaresan, S.R.","contributorId":95307,"corporation":false,"usgs":true,"family":"Sundaresan","given":"S.R.","affiliations":[],"preferred":false,"id":457553,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Farley, C.","contributorId":72622,"corporation":false,"usgs":true,"family":"Farley","given":"C.","email":"","affiliations":[],"preferred":false,"id":457551,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Belnap, J. 0000-0001-7471-2279","orcid":"https://orcid.org/0000-0001-7471-2279","contributorId":23872,"corporation":false,"usgs":true,"family":"Belnap","given":"J.","affiliations":[],"preferred":false,"id":457549,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70036640,"text":"70036640 - 2011 - Effects of intrusions on grades and contents of gold and other metals in volcanogenic massive sulfide deposits","interactions":[],"lastModifiedDate":"2017-08-31T15:56:43","indexId":"70036640","displayToPublicDate":"2011-01-01T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2954,"text":"Ore Geology Reviews","active":true,"publicationSubtype":{"id":10}},"title":"Effects of intrusions on grades and contents of gold and other metals in volcanogenic massive sulfide deposits","docAbstract":"<p id=\"sp0010\">The reason some VMS deposits contain more gold or other metals than others might be due to the influence of intrusions. A new approach examining this possibility is based on examining the information about many VMS deposits to test statistically if those with associated intrusions have significantly different grades or amounts of metals. A set of 632 VMS deposits with reported grades, tonnages, and information about the observed presence or absence of subvolcanic or plutonic intrusive bodies emplaced at or after VMS mineralization is statistically analyzed.</p><p id=\"sp0015\">Deposits with syn-mineralization or post-mineralization intrusions nearby have higher tonnages than deposits without reported intrusions, but the differences are not statistically significant. When both kinds of intrusions are reported, VMS deposit sizes are significantly higher than in the deposits without any intrusions. Gold, silver, zinc, lead, and copper average grades are not significantly different in the VMS deposits with nearby intrusions compared to deposits without regardless of relative age of intrusive. Only zinc and copper contents are significantly higher in VMS deposits with both kinds of intrusive reported. These differences in overall metal content are due to significantly larger deposit sizes of VMS deposits where both intrusive kinds are observed and reported, rather than any difference in metal grades.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.oregeorev.2010.12.003","issn":"01691368","usgsCitation":"Singer, D.A., Berger, V., and Mosier, D.L., 2011, Effects of intrusions on grades and contents of gold and other metals in volcanogenic massive sulfide deposits: Ore Geology Reviews, v. 39, no. 1-2, p. 116-118, https://doi.org/10.1016/j.oregeorev.2010.12.003.","productDescription":"3 p.","startPage":"116","endPage":"118","numberOfPages":"3","ipdsId":"IP-022140","costCenters":[{"id":662,"text":"Western Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"links":[{"id":475279,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1016/j.oregeorev.2010.12.003","text":"Publisher Index Page"},{"id":217560,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.oregeorev.2010.12.003"},{"id":245513,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"39","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a072ae4b0c8380cd515b7","contributors":{"authors":[{"text":"Singer, Donald A. dsinger@usgs.gov","contributorId":5601,"corporation":false,"usgs":true,"family":"Singer","given":"Donald","email":"dsinger@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":457119,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Berger, Vladimir vladimir@usgs.gov","contributorId":2795,"corporation":false,"usgs":true,"family":"Berger","given":"Vladimir","email":"vladimir@usgs.gov","affiliations":[],"preferred":true,"id":457118,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mosier, Dan L.","contributorId":42593,"corporation":false,"usgs":true,"family":"Mosier","given":"Dan","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":457117,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70036612,"text":"70036612 - 2011 - A buoyant plume adjacent to a headland-Observations of the Elwha River plume","interactions":[],"lastModifiedDate":"2020-12-29T18:14:42.641153","indexId":"70036612","displayToPublicDate":"2011-01-01T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1333,"text":"Continental Shelf Research","active":true,"publicationSubtype":{"id":10}},"title":"A buoyant plume adjacent to a headland-Observations of the Elwha River plume","docAbstract":"<p><span>Small rivers commonly discharge into coastal settings with topographic complexities – such as headlands and islands – but these settings are underrepresented in river plume studies compared to more simplified, straight coasts. The Elwha River provides a unique opportunity to study the effects of coastal topography on a buoyant plume, because it discharges into the Strait of Juan de Fuca on the western side of its deltaic headland. Here we show that this headland induces flow separation and transient eddies in the tidally dominated currents (O(100</span><span>&nbsp;</span><span>cm/s)), consistent with other headlands in oscillatory flow. These flow conditions are observed to strongly influence the buoyant river plume, as predicted by the “small-scale” or “narrow” dynamical classification using&nbsp;</span><a class=\"workspace-trigger\" name=\"bbib11\" href=\"https://www.sciencedirect.com/science/article/pii/S0278434310003584?via%3Dihub#bib11\" data-mce-href=\"https://www.sciencedirect.com/science/article/pii/S0278434310003584?via%3Dihub#bib11\">Garvine's (1995)</a><span>&nbsp;system. Because of the transient eddies and the location of the river mouth on the headland, flow immediately offshore of the river mouth is directed eastward twice as frequently as it is westward. This results in a buoyant plume that is much more frequently “bent over” toward the east than the west. During bent over plume conditions, the plume was attached to the eastern shoreline while having a distinct, cuspate front along its westernmost boundary. The location of the front was found to be related to the magnitude and direction of local flow during the preceding O(1</span><span>&nbsp;</span><span>h), and increases in alongshore flow resulted in deeper freshwater mixing, stronger baroclinic anomalies, and stronger hugging of the coast. During bent over plume conditions, we observed significant convergence of river plume water toward the frontal boundary within 1</span><span>&nbsp;</span><span>km of the river mouth. These results show how coastal topography can strongly influence buoyant plume behavior, and they should assist with understanding of initial coastal sediment dispersal pathways from the Elwha River during a pending dam removal project.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.csr.2010.11.007","issn":"02784343","usgsCitation":"Warrick, J.A., and Stevens, A.W., 2011, A buoyant plume adjacent to a headland-Observations of the Elwha River plume: Continental Shelf Research, v. 31, no. 2, p. 85-97, https://doi.org/10.1016/j.csr.2010.11.007.","productDescription":"13 p.","startPage":"85","endPage":"97","costCenters":[],"links":[{"id":245573,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":217616,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.csr.2010.11.007"}],"country":"United States","state":"Washington","otherGeospatial":"Elwha River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -123.68957519531251,\n              47.87214396888731\n            ],\n            [\n              -123.24462890625,\n              47.87214396888731\n            ],\n            [\n              -123.24462890625,\n              48.188063481211415\n            ],\n            [\n              -123.68957519531251,\n              48.188063481211415\n            ],\n            [\n              -123.68957519531251,\n              47.87214396888731\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"31","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e333e4b0c8380cd45e98","chorus":{"doi":"10.1016/j.csr.2010.11.007","url":"http://dx.doi.org/10.1016/j.csr.2010.11.007","publisher":"Elsevier BV","authors":"Warrick Jonathan A., Stevens Andrew W.","journalName":"Continental Shelf Research","publicationDate":"2/2011"},"contributors":{"authors":[{"text":"Warrick, Jonathan A. 0000-0002-0205-3814 jwarrick@usgs.gov","orcid":"https://orcid.org/0000-0002-0205-3814","contributorId":167736,"corporation":false,"usgs":true,"family":"Warrick","given":"Jonathan","email":"jwarrick@usgs.gov","middleInitial":"A.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":457003,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stevens, Andrew W. 0000-0003-2334-129X astevens@usgs.gov","orcid":"https://orcid.org/0000-0003-2334-129X","contributorId":139313,"corporation":false,"usgs":true,"family":"Stevens","given":"Andrew","email":"astevens@usgs.gov","middleInitial":"W.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true},{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"preferred":true,"id":457002,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70036534,"text":"70036534 - 2011 - Turtles and culverts, and alternative energy development: an unreported but potentially significant mortality threat to the desert tortoise (<i>Gopherus agassizii</i>)","interactions":[],"lastModifiedDate":"2012-12-27T11:13:29","indexId":"70036534","displayToPublicDate":"2011-01-01T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1210,"text":"Chelonian Conservation and Biology","active":true,"publicationSubtype":{"id":10}},"title":"Turtles and culverts, and alternative energy development: an unreported but potentially significant mortality threat to the desert tortoise (<i>Gopherus agassizii</i>)","docAbstract":"Culverts are often used to increase the permeability of roaded landscapes for wildlife, including turtles. Although the benefits of culverts as safe passages for turtles are well documented, under some conditions culverts can entrap them and cause mortality. Here we report a culvert-related mortality in the federally threatened desert tortoise (<i>Gopherus agassizii</i>) at a wind energy facility in California and offer simple recommendations to mitigate the negative effects of culverts for wildlife in general.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Chelonian Conservation and Biology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Chelonian Research Foundation","publisherLocation":"http://www.chelonian.org/","doi":"10.2744/CCB-0864.1","issn":"10718443","usgsCitation":"Lovich, J., Ennen, J., Madrak, S., and Grover, B., 2011, Turtles and culverts, and alternative energy development: an unreported but potentially significant mortality threat to the desert tortoise (<i>Gopherus agassizii</i>): Chelonian Conservation and Biology, v. 10, no. 1, p. 124-129, https://doi.org/10.2744/CCB-0864.1.","productDescription":"6 p.","startPage":"124","endPage":"129","costCenters":[{"id":568,"text":"Southwest Biological Science Center","active":true,"usgs":true}],"links":[{"id":495019,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.2744/ccb-0864.1","text":"Publisher Index Page"},{"id":217869,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.2744/CCB-0864.1"},{"id":245842,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"10","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb8fce4b08c986b327b52","contributors":{"authors":[{"text":"Lovich, J.E.","contributorId":102411,"corporation":false,"usgs":true,"family":"Lovich","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":456591,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ennen, J.R.","contributorId":108335,"corporation":false,"usgs":true,"family":"Ennen","given":"J.R.","affiliations":[],"preferred":false,"id":456592,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Madrak, S.","contributorId":50761,"corporation":false,"usgs":true,"family":"Madrak","given":"S.","affiliations":[],"preferred":false,"id":456589,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Grover, B.","contributorId":92895,"corporation":false,"usgs":true,"family":"Grover","given":"B.","email":"","affiliations":[],"preferred":false,"id":456590,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70035024,"text":"70035024 - 2011 - Demasculinization of male fish by wastewater treatment plant effluent","interactions":[],"lastModifiedDate":"2021-05-28T15:09:24.800561","indexId":"70035024","displayToPublicDate":"2011-01-01T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":874,"text":"Aquatic Toxicology","active":true,"publicationSubtype":{"id":10}},"title":"Demasculinization of male fish by wastewater treatment plant effluent","docAbstract":"<div id=\"abstracts\" class=\"Abstracts u-font-serif\"><div id=\"aep-abstract-id12\" class=\"abstract author\"><div id=\"aep-abstract-sec-id13\"><p id=\"spar0005\">Adult male fathead minnows (<i>Pimephales promelas</i>) were exposed to effluent from the City of Boulder, Colorado wastewater treatment plant (WWTP) under controlled conditions in the field to determine if the effluent induced reproductive disruption in fish. Gonadal intersex and other evidence of reproductive disruption were previously identified in white suckers (<i>Catostomus commersoni</i>) in Boulder Creek downstream from this WWTP effluent outfall. Fish were exposed within a mobile flow-through exposure laboratory in July 2005 and August 2006 to WWTP effluent (EFF), Boulder Creek water (REF), or mixtures of EFF and REF for up to 28 days. Primary (sperm abundance) and secondary (nuptial tubercles and dorsal fat pads) sex characteristics were demasculinized within 14 days of exposure to 50% and 100% EFF. Vitellogenin was maximally elevated in both 50% and 100% EFF treatments within 7 days and significantly elevated by 25% EFF within 14 days. The steroidal estrogens 17β-estradiol, estrone, estriol, and 17α-ethynylestradiol, as well as estrogenic alkylphenols and bisphenol A were identified within the EFF treatments and not in the REF treatment. These results support the hypothesis that the reproductive disruption observed in this watershed is due to endocrine-active chemicals in the WWTP effluent.</p></div></div></div>","language":"English","publisher":"Elsevier","doi":"10.1016/j.aquatox.2011.02.007","usgsCitation":"Vajda, A., Barber, L.B., Gray, J.L., Lopez, E., Bolden, A., Schoenfuss, H., and Norris, D., 2011, Demasculinization of male fish by wastewater treatment plant effluent: Aquatic Toxicology, v. 103, no. 3-4, p. 213-221, https://doi.org/10.1016/j.aquatox.2011.02.007.","productDescription":"9 p.","startPage":"213","endPage":"221","numberOfPages":"9","ipdsId":"IP-013216","costCenters":[{"id":452,"text":"National Water Quality Laboratory","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true},{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"links":[{"id":243345,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Colorado","city":"Boulder","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -105.2021598815918,\n              40.03839224384298\n            ],\n            [\n              -105.17572402954102,\n              40.03839224384298\n            ],\n            [\n              -105.17572402954102,\n              40.05692083088936\n            ],\n            [\n              -105.2021598815918,\n              40.05692083088936\n            ],\n            [\n              -105.2021598815918,\n              40.03839224384298\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"103","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059fe79e4b0c8380cd4ed49","contributors":{"authors":[{"text":"Vajda, A.M.","contributorId":35961,"corporation":false,"usgs":true,"family":"Vajda","given":"A.M.","affiliations":[],"preferred":false,"id":448930,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Barber, Larry B. 0000-0002-0561-0831 lbbarber@usgs.gov","orcid":"https://orcid.org/0000-0002-0561-0831","contributorId":921,"corporation":false,"usgs":true,"family":"Barber","given":"Larry","email":"lbbarber@usgs.gov","middleInitial":"B.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true},{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":779279,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gray, James L. 0000-0002-0807-5635 jlgray@usgs.gov","orcid":"https://orcid.org/0000-0002-0807-5635","contributorId":1253,"corporation":false,"usgs":true,"family":"Gray","given":"James","email":"jlgray@usgs.gov","middleInitial":"L.","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true},{"id":452,"text":"National Water Quality Laboratory","active":true,"usgs":true},{"id":5046,"text":"Branch of Analytical Serv (NWQL)","active":true,"usgs":true}],"preferred":true,"id":779280,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lopez, E.M.","contributorId":107520,"corporation":false,"usgs":true,"family":"Lopez","given":"E.M.","email":"","affiliations":[],"preferred":false,"id":448935,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Bolden, A.M.","contributorId":91707,"corporation":false,"usgs":true,"family":"Bolden","given":"A.M.","email":"","affiliations":[],"preferred":false,"id":448933,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Schoenfuss, H.L.","contributorId":103877,"corporation":false,"usgs":true,"family":"Schoenfuss","given":"H.L.","affiliations":[],"preferred":false,"id":448934,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Norris, D.O.","contributorId":58475,"corporation":false,"usgs":true,"family":"Norris","given":"D.O.","email":"","affiliations":[],"preferred":false,"id":448931,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70034967,"text":"70034967 - 2011 - Implementation of unmanned aircraft systems by the U.S. Geological Survey","interactions":[],"lastModifiedDate":"2012-03-12T17:21:42","indexId":"70034967","displayToPublicDate":"2011-01-01T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1753,"text":"Geocarto International","active":true,"publicationSubtype":{"id":10}},"title":"Implementation of unmanned aircraft systems by the U.S. Geological Survey","docAbstract":"The U.S. Geological Survey (USGS) Unmanned Aircraft Systems (UAS) Project Office is leading the implementation of UAS technology in anticipation of transforming the research methods and management techniques employed across the Department of the Interior. UAS technology is being made available to monitor environmental conditions, analyse the impacts of climate change, respond to natural hazards, understand landscape change rates and consequences, conduct wildlife inventories and support related land management missions. USGS is teaming with the Department of the Interior Aviation Management Directorate (AMD) to lead the safe and cost-effective adoption of UAS technology by the Department of the Interior Agencies and USGS scientists.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Geocarto International","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1080/10106049.2010.533199","issn":"10106049","usgsCitation":"Cress, J., Sloan, J., and Hutt, M., 2011, Implementation of unmanned aircraft systems by the U.S. Geological Survey: Geocarto International, v. 26, no. 2, p. 133-140, https://doi.org/10.1080/10106049.2010.533199.","startPage":"133","endPage":"140","numberOfPages":"8","costCenters":[],"links":[{"id":216034,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1080/10106049.2010.533199"},{"id":243873,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"26","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3911e4b0c8380cd617b8","contributors":{"authors":[{"text":"Cress, J.J.","contributorId":61669,"corporation":false,"usgs":true,"family":"Cress","given":"J.J.","email":"","affiliations":[],"preferred":false,"id":448626,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sloan, J.L.","contributorId":35977,"corporation":false,"usgs":true,"family":"Sloan","given":"J.L.","email":"","affiliations":[],"preferred":false,"id":448624,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hutt, M.E.","contributorId":43195,"corporation":false,"usgs":true,"family":"Hutt","given":"M.E.","email":"","affiliations":[],"preferred":false,"id":448625,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70036609,"text":"70036609 - 2011 - Regional long-term production modeling from a single well test, Mount Elbert Gas Hydrate Stratigraphic Test Well, Alaska North Slope","interactions":[],"lastModifiedDate":"2018-11-15T14:45:02","indexId":"70036609","displayToPublicDate":"2011-01-01T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2682,"text":"Marine and Petroleum Geology","active":true,"publicationSubtype":{"id":10}},"title":"Regional long-term production modeling from a single well test, Mount Elbert Gas Hydrate Stratigraphic Test Well, Alaska North Slope","docAbstract":"<p><span>Following the results from the open-hole formation pressure response test in the BPXA-DOE-USGS Mount Elbert Gas Hydrate Stratigraphic Test Well (Mount Elbert well) using Schlumberger's Modular Dynamics Formation Tester (MDT) wireline tool, the International Methane Hydrate Reservoir Simulator Code Comparison project performed long-term reservoir simulations on three different model reservoirs. These descriptions were based on 1) the Mount Elbert gas hydrate accumulation as delineated by an extensive history-matching exercise, 2) an estimation of the hydrate accumulation near the Prudhoe Bay L-pad, and 3) a reservoir that would be down-dip of the Prudhoe Bay L-pad and therefore warmer and deeper. All of these simulations were based, in part, on the results of the MDT results from the Mount Elbert Well. The comparison group's consensus value for the initial permeability of the hydrate-filled reservoir (</span><i>k</i><span>&nbsp;=&nbsp;0.12&nbsp;mD) and the permeability model based on the MDT history match were used as the basis for subsequent simulations on the three regional scenarios. The simulation results of the five different simulation codes, CMG STARS, HydrateResSim, MH-21 HYDRES, STOMP-HYD, and TOUGH+HYDRATE exhibit good qualitative agreement and the variability of potential methane production rates from gas hydrate reservoirs is illustrated. As expected, the predicted methane production rate increased with increasing&nbsp;</span><i>in situ</i><span>&nbsp;reservoir temperature; however, a significant delay in the onset of rapid hydrate dissociation is observed for a cold, homogeneous reservoir and it is found to be repeatable. The inclusion of reservoir heterogeneity in the description of this cold reservoir is shown to eliminate this delayed production. Overall, simulations utilized detailed information collected across the Mount Elbert reservoir either obtained or determined from geophysical well logs, including thickness (37&nbsp;ft), porosity (35%), hydrate saturation (65%), intrinsic permeability (1000&nbsp;mD), pore water salinity (5&nbsp;ppt), and formation temperature (3.3–3.9&nbsp;°C). This paper presents the approach and results of extrapolating regional forward production modeling from history-matching efforts on the results from a single well test.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.marpetgeo.2010.01.015","issn":"02648172","usgsCitation":"Anderson, B., Kurihara, M., White, M., Moridis, G.J., Wilson, S., Pooladi-Darvish, M., Gaddipati, M., Masuda, Y., Collett, T.S., Hunter, R., Narita, H., Rose, K., and Boswell, R., 2011, Regional long-term production modeling from a single well test, Mount Elbert Gas Hydrate Stratigraphic Test Well, Alaska North Slope: Marine and Petroleum Geology, v. 28, no. 2, p. 493-501, https://doi.org/10.1016/j.marpetgeo.2010.01.015.","productDescription":"9 p.","startPage":"493","endPage":"501","costCenters":[],"links":[{"id":245511,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":217558,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.marpetgeo.2010.01.015"}],"volume":"28","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50e4a537e4b0e8fec6cdbd8f","contributors":{"authors":[{"text":"Anderson, B.J.","contributorId":70914,"corporation":false,"usgs":true,"family":"Anderson","given":"B.J.","email":"","affiliations":[],"preferred":false,"id":456988,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kurihara, M.","contributorId":54823,"corporation":false,"usgs":true,"family":"Kurihara","given":"M.","email":"","affiliations":[],"preferred":false,"id":456985,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"White, M.D.","contributorId":58125,"corporation":false,"usgs":true,"family":"White","given":"M.D.","email":"","affiliations":[],"preferred":false,"id":456986,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Moridis, G. J.","contributorId":64863,"corporation":false,"usgs":false,"family":"Moridis","given":"G.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":456987,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Wilson, S.J.","contributorId":93734,"corporation":false,"usgs":true,"family":"Wilson","given":"S.J.","email":"","affiliations":[],"preferred":false,"id":456991,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Pooladi-Darvish, M.","contributorId":42455,"corporation":false,"usgs":false,"family":"Pooladi-Darvish","given":"M.","email":"","affiliations":[],"preferred":false,"id":456982,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Gaddipati, M.","contributorId":81346,"corporation":false,"usgs":true,"family":"Gaddipati","given":"M.","email":"","affiliations":[],"preferred":false,"id":456989,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Masuda, Y.","contributorId":46339,"corporation":false,"usgs":true,"family":"Masuda","given":"Y.","email":"","affiliations":[],"preferred":false,"id":456984,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Collett, Timothy S. 0000-0002-7598-4708 tcollett@usgs.gov","orcid":"https://orcid.org/0000-0002-7598-4708","contributorId":1698,"corporation":false,"usgs":true,"family":"Collett","given":"Timothy","email":"tcollett@usgs.gov","middleInitial":"S.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true},{"id":255,"text":"Energy Resources Program","active":true,"usgs":true},{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true},{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":456990,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Hunter, R.B.","contributorId":29538,"corporation":false,"usgs":true,"family":"Hunter","given":"R.B.","email":"","affiliations":[],"preferred":false,"id":456980,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Narita, H.","contributorId":105565,"corporation":false,"usgs":true,"family":"Narita","given":"H.","email":"","affiliations":[],"preferred":false,"id":456992,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Rose, K.","contributorId":43594,"corporation":false,"usgs":true,"family":"Rose","given":"K.","email":"","affiliations":[],"preferred":false,"id":456983,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Boswell, R.","contributorId":35121,"corporation":false,"usgs":true,"family":"Boswell","given":"R.","affiliations":[],"preferred":false,"id":456981,"contributorType":{"id":1,"text":"Authors"},"rank":13}]}}
,{"id":70036519,"text":"70036519 - 2011 - Mantle to surface degassing of alkalic magmas at Erebus volcano, Antarctica","interactions":[],"lastModifiedDate":"2021-01-07T17:16:07.029115","indexId":"70036519","displayToPublicDate":"2011-01-01T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1427,"text":"Earth and Planetary Science Letters","active":true,"publicationSubtype":{"id":10}},"title":"Mantle to surface degassing of alkalic magmas at Erebus volcano, Antarctica","docAbstract":"<p><span>Continental intraplate volcanoes, such as Erebus volcano, Antarctica, are associated with extensional tectonics, mantle upwelling and high heat flow. Typically, erupted magmas are alkaline and rich in volatiles (especially CO</span><sub>2</sub><span>), inherited from low degrees of partial melting of mantle sources. We examine the degassing of the magmatic system at Erebus volcano using melt inclusion data and high temporal resolution open-path Fourier transform infrared (FTIR) spectroscopic measurements of gas emissions from the active lava lake. Remarkably different gas signatures are associated with passive and explosive gas emissions, representative of volatile contents and redox conditions that reveal contrasting shallow and deep degassing sources. We show that this unexpected degassing signature provides a unique probe for magma differentiation and transfer of CO</span><sub>2</sub><span>-rich oxidised fluids from the mantle to the surface, and evaluate how these processes operate in time and space. Extensive crystallisation driven by CO</span><sub>2</sub><span>&nbsp;fluxing is responsible for isobaric fractionation of parental basanite magmas close to their source depth. Magma deeper than 4</span><span>&nbsp;</span><span>kbar equilibrates under vapour-buffered conditions. At shallower depths, CO</span><sub>2</sub><span>-rich fluids accumulate and are then released either via convection-driven, open-system gas loss or as closed-system slugs that ascend and result in Strombolian eruptions in the lava lake. The open-system gases have a reduced state (below the QFM buffer) whereas the closed-system gases preserve their deep oxidised signatures (close to the NNO buffer).</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.epsl.2011.04.005","issn":"0012821X","usgsCitation":"Oppenheimer, C., Moretti, R., Kyle, P., Eschenbacher, A., Lowenstern, J.B., Hervig, R., and Dunbar, N.W., 2011, Mantle to surface degassing of alkalic magmas at Erebus volcano, Antarctica: Earth and Planetary Science Letters, v. 306, no. 3-4, p. 261-271, https://doi.org/10.1016/j.epsl.2011.04.005.","productDescription":"11 p.","startPage":"261","endPage":"271","costCenters":[],"links":[{"id":475291,"rank":10000,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://insu.hal.science/insu-00707142","text":"External 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,{"id":70033828,"text":"70033828 - 2011 - The influence of stream channels on distributions of Larrea tridentata and Ambrosia dumosa in the Mojave Desert, CA, USA: Patterns, mechanisms and effects of stream redistribution","interactions":[],"lastModifiedDate":"2017-11-20T12:32:57","indexId":"70033828","displayToPublicDate":"2011-01-01T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1447,"text":"Ecohydrology","active":true,"publicationSubtype":{"id":10}},"title":"The influence of stream channels on distributions of Larrea tridentata and Ambrosia dumosa in the Mojave Desert, CA, USA: Patterns, mechanisms and effects of stream redistribution","docAbstract":"<p><span>Drainage channels are among the most conspicuous surficial features of deserts, but little quantitative analysis of their influence on plant distributions is available. We analysed the effects of desert stream channels (‘washes’) on&nbsp;</span><i>Larrea tridentata</i><span><span>&nbsp;</span>and<span>&nbsp;</span></span><i>Ambrosia dumosa</i><span><span>&nbsp;</span>density and cover on an alluvial piedmont in the Mojave Desert, based on a spatial analysis of transect data encompassing a total length of 2775 m surveyed in 5 cm increments. Significant deviations from average transect properties were identified by bootstrapping. Predictably, shrub cover and density were much reduced inside washes, and elevated above average levels adjacent to washes. Average<span>&nbsp;</span></span><i>Larrea</i><span><span>&nbsp;</span>and<span>&nbsp;</span></span><i>Ambrosia</i><span><span>&nbsp;</span>cover and density peaked 1·2–1·6 m and 0·5–1·0 m from wash edges, respectively. We compared wash effects in runon-depleted (−R) sections, where washes had been cut off from runon and were presumably inactive, with those in runon-supplemented (+R) sections downslope from railroad culverts to help identify mechanisms responsible for the facilitative effect of washes on adjacent shrubs. Shrub cover and density near washes peaked in both + R and − R sections, suggesting that improved water infiltration and storage alone can cause a facilitative effect on adjacent shrubs. However, washes of &lt; 2 m width in + R sections had larger than average effects on peak cover, suggesting that plants also benefit from occasional resource supplementation. The data suggest that channel networks significantly contribute to structuring plant communities in the Mojave Desert and their disruption has notable effects on geomorphic and ecological processes far beyond the original disturbance sites.<span>&nbsp;</span></span></p>","language":"English","publisher":"Wiley","doi":"10.1002/eco.116","issn":"19360584","usgsCitation":"Schwinning, S., Sandquist, D., Miller, D., Bedford, D.R., Phillips, S.L., and Belnap, J., 2011, The influence of stream channels on distributions of Larrea tridentata and Ambrosia dumosa in the Mojave Desert, CA, USA: Patterns, mechanisms and effects of stream redistribution: Ecohydrology, v. 4, no. 1, p. 12-25, https://doi.org/10.1002/eco.116.","productDescription":"14 p.","startPage":"12","endPage":"25","numberOfPages":"14","ipdsId":"IP-019949","costCenters":[{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true},{"id":309,"text":"Geology and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":241968,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":214263,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1002/eco.116"}],"country":"United States","state":"California","otherGeospatial":"Mojave Desert","volume":"4","issue":"1","noUsgsAuthors":false,"publicationDate":"2011-01-19","publicationStatus":"PW","scienceBaseUri":"505bad38e4b08c986b323a7b","contributors":{"authors":[{"text":"Schwinning, S.","contributorId":41207,"corporation":false,"usgs":true,"family":"Schwinning","given":"S.","email":"","affiliations":[],"preferred":false,"id":442729,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sandquist, D.R.","contributorId":37281,"corporation":false,"usgs":true,"family":"Sandquist","given":"D.R.","email":"","affiliations":[],"preferred":false,"id":442728,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Miller, D. M. 0000-0003-3711-0441","orcid":"https://orcid.org/0000-0003-3711-0441","contributorId":104422,"corporation":false,"usgs":true,"family":"Miller","given":"D. M.","affiliations":[],"preferred":false,"id":442731,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bedford, D. R.","contributorId":9734,"corporation":false,"usgs":true,"family":"Bedford","given":"D.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":442726,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Phillips, S. L.","contributorId":94460,"corporation":false,"usgs":true,"family":"Phillips","given":"S.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":442730,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Belnap, J. 0000-0001-7471-2279","orcid":"https://orcid.org/0000-0001-7471-2279","contributorId":23872,"corporation":false,"usgs":true,"family":"Belnap","given":"J.","affiliations":[],"preferred":false,"id":442727,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70035526,"text":"70035526 - 2011 - The Mairan domes: silicic volcanic constructs on the Moon","interactions":[],"lastModifiedDate":"2019-02-18T10:25:14","indexId":"70035526","displayToPublicDate":"2011-01-01T00:00:00","publicationYear":"2011","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":"The Mairan domes: silicic volcanic constructs on the Moon","docAbstract":"The Mairan domes are four features located in northern Oceanus Procellarum at ∼312.3E, 41.4N on the Moon. High resolution visible imagery, visible-to-mid-IR spectra, and Lunar Prospector Th abundance data all indicate that these four domes have a composition that is consistent with derivation from a Si-rich, highly evolved magma.","language":"English","publisher":"American Geophysical Union","doi":"10.1029/2011GL049548","issn":"00948276","usgsCitation":"Glotch, T.D., Hagerty, J., Lucey, P.G., Hawke, B.R., Giguere, T.A., Arnold, J.A., Williams, J., Jolliff, B.L., and Paige, D.A., 2011, The Mairan domes: silicic volcanic constructs on the Moon: Geophysical Research Letters, v. 38, no. 21, 5 p., https://doi.org/10.1029/2011GL049548.","productDescription":"5 p.","numberOfPages":"5","costCenters":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"links":[{"id":475186,"rank":1,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1029/2011gl049548","text":"Publisher Index Page"},{"id":244002,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Mairan domes; Moon","volume":"38","issue":"21","noUsgsAuthors":false,"publicationDate":"2011-11-15","publicationStatus":"PW","scienceBaseUri":"505ba7cee4b08c986b3217f2","contributors":{"authors":[{"text":"Glotch, Timothy D.","contributorId":10638,"corporation":false,"usgs":true,"family":"Glotch","given":"Timothy","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":451082,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hagerty, Justin 0000-0003-3800-7948 jhagerty@usgs.gov","orcid":"https://orcid.org/0000-0003-3800-7948","contributorId":911,"corporation":false,"usgs":true,"family":"Hagerty","given":"Justin","email":"jhagerty@usgs.gov","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":true,"id":451081,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lucey, Paul G.","contributorId":100218,"corporation":false,"usgs":true,"family":"Lucey","given":"Paul","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":451087,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hawke, B. Ray","contributorId":76570,"corporation":false,"usgs":true,"family":"Hawke","given":"B.","email":"","middleInitial":"Ray","affiliations":[],"preferred":false,"id":451085,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Giguere, Thomas A.","contributorId":11030,"corporation":false,"usgs":true,"family":"Giguere","given":"Thomas","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":451083,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Arnold, Jessica A.","contributorId":101485,"corporation":false,"usgs":true,"family":"Arnold","given":"Jessica","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":451088,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Williams, Jean-Pierre","contributorId":90507,"corporation":false,"usgs":true,"family":"Williams","given":"Jean-Pierre","email":"","affiliations":[],"preferred":false,"id":451086,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Jolliff, Bradley L.","contributorId":40040,"corporation":false,"usgs":true,"family":"Jolliff","given":"Bradley","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":451084,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Paige, David A.","contributorId":107891,"corporation":false,"usgs":true,"family":"Paige","given":"David","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":451089,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}}
,{"id":70034730,"text":"70034730 - 2011 - Engineering a future for amphibians under climate change","interactions":[],"lastModifiedDate":"2013-05-12T00:07:35","indexId":"70034730","displayToPublicDate":"2011-01-01T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2163,"text":"Journal of Applied Ecology","active":true,"publicationSubtype":{"id":10}},"title":"Engineering a future for amphibians under climate change","docAbstract":"1. Altered global climates in the 21st century pose serious threats for biological systems and practical actions are needed to mount a response for species at risk.\n\n2. We identify management actions from across the world and from diverse disciplines that are applicable to minimizing loss of amphibian biodiversity under climate change. Actions were grouped under three thematic areas of intervention: (i) installation of microclimate and microhabitat refuges; (ii) enhancement and restoration of breeding sites; and (iii) manipulation of hydroperiod or water levels at breeding sites.\n\n3. Synthesis and applications. There are currently few meaningful management actions that will tangibly impact the pervasive threat of climate change on amphibians. A host of potentially useful but poorly tested actions could be incorporated into local or regional management plans, programmes and activities for amphibians. Examples include: installation of irrigation sprayers to manipulate water potentials at breeding sites; retention or supplementation of natural and artificial shelters (e.g. logs, cover boards) to reduce desiccation and thermal stress; manipulation of canopy cover over ponds to reduce water temperature; and, creation of hydrologoically diverse wetland habitats capable of supporting larval development under variable rainfall regimes. We encourage researchers and managers to design, test and scale up new initiatives to respond to this emerging crisis.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Applied Ecology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Wiley","doi":"10.1111/j.1365-2664.2010.01942.x","issn":"00218901","usgsCitation":"Shoo, L., Olson, D., Mcmenamin, S., Murray, K., Van Sluys, M., Donnelly, M., Stratford, D., Terhivuo, J., Merino-Viteri, A., Herbert, S., Bishop, P., Corn, P., Dovey, L., Griffiths, R., Lowe, K., Mahony, M., McCallum, H., Shuker, J., Simpkins, C., Skerratt, L., Williams, S., and Hero, J., 2011, Engineering a future for amphibians under climate change: Journal of Applied Ecology, v. 48, no. 2, p. 487-492, https://doi.org/10.1111/j.1365-2664.2010.01942.x.","productDescription":"6 p.","startPage":"487","endPage":"492","costCenters":[{"id":527,"text":"Pacific Northwest Research Station","active":false,"usgs":true}],"links":[{"id":215726,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1111/j.1365-2664.2010.01942.x"},{"id":243548,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"48","issue":"2","noUsgsAuthors":false,"publicationDate":"2011-02-02","publicationStatus":"PW","scienceBaseUri":"505a0954e4b0c8380cd51e92","contributors":{"authors":[{"text":"Shoo, L.P.","contributorId":93295,"corporation":false,"usgs":true,"family":"Shoo","given":"L.P.","email":"","affiliations":[],"preferred":false,"id":447263,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Olson, D.H.","contributorId":85349,"corporation":false,"usgs":true,"family":"Olson","given":"D.H.","affiliations":[],"preferred":false,"id":447261,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mcmenamin, S.K.","contributorId":27699,"corporation":false,"usgs":true,"family":"Mcmenamin","given":"S.K.","email":"","affiliations":[],"preferred":false,"id":447250,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Murray, K.A.","contributorId":94880,"corporation":false,"usgs":true,"family":"Murray","given":"K.A.","email":"","affiliations":[],"preferred":false,"id":447264,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Van Sluys, M.","contributorId":61259,"corporation":false,"usgs":true,"family":"Van Sluys","given":"M.","email":"","affiliations":[],"preferred":false,"id":447253,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Donnelly, M.A.","contributorId":78845,"corporation":false,"usgs":true,"family":"Donnelly","given":"M.A.","email":"","affiliations":[],"preferred":false,"id":447258,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Stratford, D.","contributorId":89372,"corporation":false,"usgs":true,"family":"Stratford","given":"D.","email":"","affiliations":[],"preferred":false,"id":447262,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Terhivuo, J.","contributorId":7934,"corporation":false,"usgs":true,"family":"Terhivuo","given":"J.","email":"","affiliations":[],"preferred":false,"id":447246,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Merino-Viteri, A.","contributorId":103892,"corporation":false,"usgs":true,"family":"Merino-Viteri","given":"A.","email":"","affiliations":[],"preferred":false,"id":447267,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Herbert, S.M.","contributorId":16240,"corporation":false,"usgs":true,"family":"Herbert","given":"S.M.","email":"","affiliations":[],"preferred":false,"id":447247,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Bishop, P.J.","contributorId":96501,"corporation":false,"usgs":true,"family":"Bishop","given":"P.J.","email":"","affiliations":[],"preferred":false,"id":447265,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Corn, P.S.","contributorId":63751,"corporation":false,"usgs":true,"family":"Corn","given":"P.S.","affiliations":[],"preferred":false,"id":447254,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Dovey, L.","contributorId":59647,"corporation":false,"usgs":true,"family":"Dovey","given":"L.","email":"","affiliations":[],"preferred":false,"id":447252,"contributorType":{"id":1,"text":"Authors"},"rank":13},{"text":"Griffiths, R.A.","contributorId":24193,"corporation":false,"usgs":true,"family":"Griffiths","given":"R.A.","email":"","affiliations":[],"preferred":false,"id":447249,"contributorType":{"id":1,"text":"Authors"},"rank":14},{"text":"Lowe, K.","contributorId":70587,"corporation":false,"usgs":true,"family":"Lowe","given":"K.","email":"","affiliations":[],"preferred":false,"id":447256,"contributorType":{"id":1,"text":"Authors"},"rank":15},{"text":"Mahony, M.","contributorId":82553,"corporation":false,"usgs":true,"family":"Mahony","given":"M.","email":"","affiliations":[],"preferred":false,"id":447259,"contributorType":{"id":1,"text":"Authors"},"rank":16},{"text":"McCallum, H.","contributorId":70990,"corporation":false,"usgs":true,"family":"McCallum","given":"H.","email":"","affiliations":[],"preferred":false,"id":447257,"contributorType":{"id":1,"text":"Authors"},"rank":17},{"text":"Shuker, J.D.","contributorId":23354,"corporation":false,"usgs":true,"family":"Shuker","given":"J.D.","email":"","affiliations":[],"preferred":false,"id":447248,"contributorType":{"id":1,"text":"Authors"},"rank":18},{"text":"Simpkins, C.","contributorId":70207,"corporation":false,"usgs":true,"family":"Simpkins","given":"C.","email":"","affiliations":[],"preferred":false,"id":447255,"contributorType":{"id":1,"text":"Authors"},"rank":19},{"text":"Skerratt, L.F.","contributorId":85149,"corporation":false,"usgs":true,"family":"Skerratt","given":"L.F.","email":"","affiliations":[],"preferred":false,"id":447260,"contributorType":{"id":1,"text":"Authors"},"rank":20},{"text":"Williams, S.E.","contributorId":44002,"corporation":false,"usgs":true,"family":"Williams","given":"S.E.","email":"","affiliations":[],"preferred":false,"id":447251,"contributorType":{"id":1,"text":"Authors"},"rank":21},{"text":"Hero, J.-M.","contributorId":100999,"corporation":false,"usgs":true,"family":"Hero","given":"J.-M.","affiliations":[],"preferred":false,"id":447266,"contributorType":{"id":1,"text":"Authors"},"rank":22}]}}
,{"id":70193430,"text":"70193430 - 2011 - Walleye and sauger habitat","interactions":[],"lastModifiedDate":"2017-11-25T12:58:15","indexId":"70193430","displayToPublicDate":"2011-01-01T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"chapter":"5","title":"Walleye and sauger habitat","docAbstract":"<p>No abstract available.<br data-mce-bogus=\"1\"></p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Biology, management, and culture of walleye and sauger","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"American Fisheries Society","isbn":"978-1-934874-22-6","usgsCitation":"Bozek, M.A., Haxton, T.J., and Raabe, J.K., 2011, Walleye and sauger habitat, chap. 5 <i>of</i> Biology, management, and culture of walleye and sauger.","ipdsId":"IP-027474","costCenters":[{"id":199,"text":"Coop Res Unit Leetown","active":true,"usgs":true}],"links":[{"id":349312,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":349311,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://fisheries.org/bookstore/all-titles/professional-and-trade/55065p/"}],"publishingServiceCenter":{"id":9,"text":"Reston PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5a6107fce4b06e28e9c2562e","contributors":{"editors":[{"text":"Barton, Bruce A.","contributorId":177521,"corporation":false,"usgs":false,"family":"Barton","given":"Bruce","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":723406,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Bozek, Michael A.","contributorId":51030,"corporation":false,"usgs":true,"family":"Bozek","given":"Michael","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":719014,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Haxton, Timothy J.","contributorId":86368,"corporation":false,"usgs":false,"family":"Haxton","given":"Timothy","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":723404,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Raabe, Joshua K.","contributorId":140952,"corporation":false,"usgs":false,"family":"Raabe","given":"Joshua","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":723405,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70036901,"text":"70036901 - 2011 - Anthropogenic disturbance and landscape patterns affect diversity patterns of aquatic benthic macroinvertebrates","interactions":[],"lastModifiedDate":"2020-12-17T20:03:15.580005","indexId":"70036901","displayToPublicDate":"2011-01-01T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2564,"text":"Journal of the North American Benthological Society","onlineIssn":"1937-237X","printIssn":"0887-3593","active":true,"publicationSubtype":{"id":10}},"title":"Anthropogenic disturbance and landscape patterns affect diversity patterns of aquatic benthic macroinvertebrates","docAbstract":"<p><span>Measures of species diversity are valuable tools for assessing ecosystem health. However, most assessments have addressed individual sites or regional taxon pools, with few comparisons of differences in assemblage composition within or among regions. We examined the effects of anthropogenic disturbance on local richness (α diversity) and species turnover (β diversity) of benthic macroinvertebrates in small streams within and between 2 ecoregions (Northern Piedmont vs Southeastern Plains ecoregions) of the Patuxent River basin (Maryland, USA). Regional species pools did not differ between ecoregions (Piedmont  =  166 taxa, Plains  =  162 taxa); however, local richness was lower in the Plains (mean  =  17.4 taxa/stream) compared to the Piedmont (mean  =  22.2 taxa/stream). When streams were categorized into disturbance classes (low, medium, high), local richness did not differ among categories for either region. However, at the entire Patuxent scale, local richness tended to decrease with % impervious cover in a watershed. Variation in species composition, analyzed with nonmetric multidimensional scaling (nMDS), differed significantly between Piedmont and Plains streams, and Plains streams had higher β diversity than Piedmont streams. When partitioned by disturbance category and region, β diversity differed only between the low-disturbance sites (Plains &gt; Piedmont). Relationships between β diversity and environmental variables varied by region. β diversity was weakly negatively related to % row-crop cover in a watershed at the entire Patuxent scale. For the Piedmont region, β diversity tended to decrease with % forest, % pasture, and % row-crop cover in a watershed. Such negative relationships between β diversity and landuse variables indicate a possible homogenization of the assemblage. The incongruence between diversity measures and composition measures, together with differing effects of anthropogenic land use on β diversity in the 2 regions, emphasizes the need to incorporate both α and β diversity and regional environmental factors in conservation/land management studies.</span></p>","language":"English","publisher":"The University of Chicago Press Journals","doi":"10.1899/09-112.1","issn":"08873593","usgsCitation":"Maloney, K., Munguia, P., and Mitchell, R., 2011, Anthropogenic disturbance and landscape patterns affect diversity patterns of aquatic benthic macroinvertebrates: Journal of the North American Benthological Society, v. 30, no. 1, p. 284-295, https://doi.org/10.1899/09-112.1.","productDescription":"12 p.","startPage":"284","endPage":"295","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":245835,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":217863,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1899/09-112.1"}],"country":"United States","state":"Maryland","otherGeospatial":"Patuxent Watershed","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -76.35498046875,\n              38.11727165830543\n            ],\n            [\n              -76.2615966796875,\n              38.14751758025121\n            ],\n            [\n              -76.4044189453125,\n              38.406253794852674\n            ],\n            [\n              -76.6241455078125,\n              38.955137225429574\n            ],\n            [\n              -76.827392578125,\n              38.997841307500714\n            ],\n            [\n              -76.904296875,\n              38.8782049970615\n            ],\n            [\n              -76.8658447265625,\n              38.59540719940386\n            ],\n            [\n              -76.629638671875,\n              38.3287297527893\n            ],\n            [\n              -76.35498046875,\n              38.11727165830543\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"30","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059ec59e4b0c8380cd491f5","contributors":{"authors":[{"text":"Maloney, K.O. 0000-0003-2304-0745","orcid":"https://orcid.org/0000-0003-2304-0745","contributorId":105414,"corporation":false,"usgs":true,"family":"Maloney","given":"K.O.","affiliations":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"preferred":false,"id":458404,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Munguia, P.","contributorId":30855,"corporation":false,"usgs":true,"family":"Munguia","given":"P.","email":"","affiliations":[],"preferred":false,"id":458403,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mitchell, R.M.","contributorId":28721,"corporation":false,"usgs":true,"family":"Mitchell","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":458402,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70036701,"text":"70036701 - 2011 - Sea-level history of the past two interglacial periods: New evidence from U-series dating of reef corals from south Florida","interactions":[],"lastModifiedDate":"2020-12-23T18:39:54.574325","indexId":"70036701","displayToPublicDate":"2011-01-01T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3219,"text":"Quaternary Science Reviews","active":true,"publicationSubtype":{"id":10}},"title":"Sea-level history of the past two interglacial periods: New evidence from U-series dating of reef corals from south Florida","docAbstract":"<p><span>As a future warm-climate analog, much attention has been directed to studies of the Last Interglacial period or marine isotope substage (MIS) 5.5, which occurred ∼120,000 years ago. Nevertheless, there are still uncertainties with respect to its duration, warmth and magnitude of sea-level rise. Here we present new data from tectonically stable peninsular Florida and the Florida Keys that provide estimates of the timing and magnitude of sea-level rise during the Last Interglacial period. The Last Interglacial high sea stand in south Florida is recorded by the Key Largo Limestone, a fossil reef complex, and the Miami Limestone, an oolitic marine sediment. Thirty-five new, high-precision, uranium-series ages of fossil corals from the Key Largo Limestone indicate that sea level was significantly above present for at least 9000 years during the Last Interglacial period, and possibly longer. Ooids from the Miami Limestone show open-system histories with respect to U-series dating, but show a clear linear trend toward an age of ∼120&nbsp;ka, correlating this unit with the Last Interglacial corals of the Key Largo Limestone. Older fossil reefs at three localities in the Florida Keys have ages of ∼200&nbsp;ka and probably correlate to MIS 7. These reefs imply sea level near or slightly above present during the penultimate interglacial period. Elevation measurements of both the Key Largo Limestone and the Miami Limestone indicate that local (relative) sea level was at least 6.6&nbsp;m, and possibly as much as 8.3&nbsp;m higher than present during the Last Interglacial period.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.quascirev.2010.12.019","issn":"02773791","usgsCitation":"Muhs, D., Simmons, K., Schumann, R.R., and Halley, R.B., 2011, Sea-level history of the past two interglacial periods: New evidence from U-series dating of reef corals from south Florida: Quaternary Science Reviews, v. 30, no. 5-6, p. 570-590, https://doi.org/10.1016/j.quascirev.2010.12.019.","productDescription":"21 p.","startPage":"570","endPage":"590","numberOfPages":"21","costCenters":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"links":[{"id":245516,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":217563,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.quascirev.2010.12.019"}],"country":"United States","state":"Florida","otherGeospatial":"South Florida","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -82.08984375,\n              24.5271348225978\n            ],\n            [\n              -79.91455078125,\n              24.5271348225978\n            ],\n            [\n              -79.91455078125,\n              25.70093788144426\n            ],\n            [\n              -82.08984375,\n              25.70093788144426\n            ],\n            [\n              -82.08984375,\n              24.5271348225978\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"30","issue":"5-6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b8817e4b08c986b3167d5","contributors":{"authors":[{"text":"Muhs, Daniel R. 0000-0001-7449-251X dmuhs@usgs.gov","orcid":"https://orcid.org/0000-0001-7449-251X","contributorId":168575,"corporation":false,"usgs":true,"family":"Muhs","given":"Daniel R.","email":"dmuhs@usgs.gov","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":457429,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Simmons, Kathleen 0000-0002-7920-094X ksimmons@usgs.gov","orcid":"https://orcid.org/0000-0002-7920-094X","contributorId":200362,"corporation":false,"usgs":true,"family":"Simmons","given":"Kathleen","email":"ksimmons@usgs.gov","affiliations":[],"preferred":true,"id":457430,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Schumann, R. Randall 0000-0001-8158-6960 rschumann@usgs.gov","orcid":"https://orcid.org/0000-0001-8158-6960","contributorId":1569,"corporation":false,"usgs":true,"family":"Schumann","given":"R.","email":"rschumann@usgs.gov","middleInitial":"Randall","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":457428,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Halley, R. B.","contributorId":87941,"corporation":false,"usgs":true,"family":"Halley","given":"R.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":457431,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70036409,"text":"70036409 - 2011 - Volcanism on Io: New insights from global geologic mapping","interactions":[],"lastModifiedDate":"2018-11-09T14:48:49","indexId":"70036409","displayToPublicDate":"2011-01-01T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1963,"text":"Icarus","active":true,"publicationSubtype":{"id":10}},"title":"Volcanism on Io: New insights from global geologic mapping","docAbstract":"<p><span>We produced the first complete, 1:15</span><span>&nbsp;</span><span>M-scale global geologic map of Jupiter’s moon Io, based on a set of monochrome and color&nbsp;</span><i>Galileo</i><span>–</span><i>Voyager</i><span>&nbsp;image mosaics produced at a spatial resolution of 1</span><span>&nbsp;</span><span>km/pixel. The surface of Io was mapped into 19 units based on albedo, color and surface morphology, and is subdivided as follows: plains (65.8% of surface), lava flow fields (28.5%), mountains (3.2%), and patera floors (2.5%). Diffuse deposits (DD) that mantle the other units cover ∼18% of Io’s surface, and are distributed as follows: red (8.6% of surface), white (6.9%), yellow (2.1%), black (0.6%), and green (∼0.01%). Analyses of the geographical and areal distribution of these units yield a number of results, summarized below. (1) The distribution of plains units of different colors is generally geographically constrained: Red–brown plains occur &gt;±30° latitude, and are thought to result from enhanced alteration of other units induced by radiation coming in from the poles. White plains (possibly dominated by SO</span><sub>2</sub><span>&nbsp;</span><span>+</span><span>&nbsp;</span><span>contaminants) occur mostly in the equatorial antijovian region (±30°, 90–230°W), possibly indicative of a regional cold trap. Outliers of white, yellow, and red–brown plains in other regions may result from long-term accumulation of white, yellow, and red diffuse deposits, respectively. (2) Bright (possibly sulfur-rich) flow fields make up 30% more lava flow fields than dark (presumably silicate) flows (56.5% vs. 43.5%), and only 18% of bright flow fields occur within 10</span><span>&nbsp;</span><span>km of dark flow fields. These results suggest that secondary sulfurous volcanism (where a bright-dark association is expected) could be responsible for only a fraction of Io’s recent bright flows, and that primary sulfur-rich effusions could be an important component of Io’s recent volcanism. An unusual concentration of bright flows at ∼45–75°N, ∼60–120°W could be indicative of more extensive primary sulfurous volcanism in the recent past. However, it remains unclear whether most bright flows are bright because they are sulfur flows, or because they are cold&nbsp;<a title=\"Learn more about Silicates\" href=\"https://www.sciencedirect.com/topics/earth-and-planetary-sciences/silicates\" data-mce-href=\"https://www.sciencedirect.com/topics/earth-and-planetary-sciences/silicates\">silicate</a>&nbsp;flows covered in sulfur-rich particles from plume fallout. (3) We mapped 425 paterae (volcano-tectonic depressions), up from 417 previously identified by Radebaugh et al. (Radebaugh, J., Keszthelyi, L.P., McEwen, A.S., Turtle, E.P., Jaeger, W., Milazzo, M. [2001]. J. Geophys. Res. 106, 33005–33020). Although these features cover only 2.5% of Io’s surface, they correspond to 64% of all detected hot spots; 45% of all hot spots are associated with the freshest dark patera floors, reflecting the importance of active silicate volcanism to Io’s heat flow. (4) Mountains cover only ∼3% of the surface, although the transition from mountains to plains is gradational with the available imagery. 49% of all mountains are lineated and presumably layered, showing evidence of linear structures supportive of a tectonic origin. In contrast, only 6% of visible mountains are mottled (showing hummocks indicative of mass wasting) and 4% are tholi (domes or shields), consistent with a volcanic origin. (5) Initial analyses of the geographic distributions of map units show no significant longitudinal variation in the quantity of Io’s mountains or paterae, in contrast to earlier studies. This is because we use the area of mountain and patera materials as opposed to the number of structures, and our result suggests that the previously proposed anti-correlation of mountains and paterae (Schenk, P., Hargitai, H., Wilson, R., McEwen, A., Thomas, P. [2001]. J. Geophys. Res. 106, 33201–33222; Kirchoff, M.R., McKinnon, W.B., Schenk, P.M. [2011]. Earth Planet. Sci. Lett. 301, 22–30) is more complex than previously thought. There is also a slight decrease in surface area of lava flows toward the poles of Io, perhaps indicative of variations in volcanic activity. (6) The freshest bright and dark flows make up about 29% of all of Io’s flow fields, suggesting active emplacement is occurring in less than a third of Io’s visible lava fields. (7) About 47% of Io’s diffuse deposits (by area) are red, presumably deriving their color from condensed sulfur gas, and ∼38% are white, presumably dominated by condensed SO</span><sub>2</sub><span>. The much greater areal extent of gas-derived diffuse deposits (red</span><span>&nbsp;</span><span>+</span><span>&nbsp;</span><span>white, 85%) compared to presumably pyroclast-bearing diffuse deposits (dark (silicate tephra)</span><span>&nbsp;</span><span>+</span><span>&nbsp;</span><span>yellow (sulfur-rich tephra), 15%) indicates that there is effective separation between the transport of tephra and gas in many Ionian explosive eruptions. Future improvements in the geologic mapping of Io can be obtained via (a) investigating the relationships between different color/material units that are geographically and temporally associated, (b) better analysis of the temporal variations in the map units, and (c) additional high-resolution images (spatial resolutions ∼200</span><span>&nbsp;</span><span>m/pixel or better). These improvements would be greatly facilitated by new data, which could be obtained by future missions.</span></p>","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Icarus","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","doi":"10.1016/j.icarus.2011.05.007","issn":"00191035","usgsCitation":"Williams, D., Keszthelyi, L., Crown, D.A., Yff, J.A., Jaeger, W.L., Schenk, P.M., Geissler, P.E., and Becker, T.L., 2011, Volcanism on Io: New insights from global geologic mapping: Icarus, v. 214, no. 1, p. 91-112, https://doi.org/10.1016/j.icarus.2011.05.007.","productDescription":"22 p.","startPage":"91","endPage":"112","numberOfPages":"22","costCenters":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"links":[{"id":246160,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":218175,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.icarus.2011.05.007"}],"volume":"214","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bc322e4b08c986b32af90","contributors":{"authors":[{"text":"Williams, David A.","contributorId":84604,"corporation":false,"usgs":true,"family":"Williams","given":"David A.","affiliations":[],"preferred":false,"id":455991,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Keszthelyi, Laszlo P. 0000-0003-1879-4331 laz@usgs.gov","orcid":"https://orcid.org/0000-0003-1879-4331","contributorId":52802,"corporation":false,"usgs":true,"family":"Keszthelyi","given":"Laszlo P.","email":"laz@usgs.gov","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":true,"id":455986,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Crown, David A.","contributorId":196622,"corporation":false,"usgs":false,"family":"Crown","given":"David","email":"","middleInitial":"A.","affiliations":[{"id":24732,"text":"Planetary Science Institute, Tucson","active":true,"usgs":false}],"preferred":false,"id":455993,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Yff, Jessica A.","contributorId":9098,"corporation":false,"usgs":true,"family":"Yff","given":"Jessica","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":455992,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Jaeger, Windy L.","contributorId":61679,"corporation":false,"usgs":true,"family":"Jaeger","given":"Windy","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":455988,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Schenk, Paul M.","contributorId":196626,"corporation":false,"usgs":false,"family":"Schenk","given":"Paul","email":"","middleInitial":"M.","affiliations":[{"id":12445,"text":"Lunar and Planetary Institute","active":true,"usgs":false}],"preferred":false,"id":455987,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Geissler, Paul E. pgeissler@usgs.gov","contributorId":2811,"corporation":false,"usgs":true,"family":"Geissler","given":"Paul","email":"pgeissler@usgs.gov","middleInitial":"E.","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":true,"id":455989,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Becker, Tammy L. tbecker@usgs.gov","contributorId":4388,"corporation":false,"usgs":true,"family":"Becker","given":"Tammy","email":"tbecker@usgs.gov","middleInitial":"L.","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":true,"id":455990,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":70035617,"text":"70035617 - 2011 - Electronic tags and genetics explore variation in migrating steelhead kelts (oncorhynchus mykiss), Ninilchik river, Alaska","interactions":[],"lastModifiedDate":"2018-08-21T16:28:17","indexId":"70035617","displayToPublicDate":"2011-01-01T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1169,"text":"Canadian Journal of Fisheries and Aquatic Sciences","active":true,"publicationSubtype":{"id":10}},"title":"Electronic tags and genetics explore variation in migrating steelhead kelts (oncorhynchus mykiss), Ninilchik river, Alaska","docAbstract":"Acoustic and archival tags examined freshwater and marine migrations of postspawn steelhead kelts (Oncorhynchus mykiss) in the Ninilchik River, Alaska, USA. Postspawn steelhead were captured at a weir in 2002-2005. Scale analysis indicated multiple migratory life histories and spawning behaviors. Acoustic tags were implanted in 99 kelts (2002-2003), and an array of acoustic receivers calculated the average speed of outmigration, timing of saltwater entry, and duration of residency in the vicinity of the river mouth. Ocean migration data were recovered from two archival tags implanted in kelts in 2004 (one male and one female). Archival tags documented seasonal differences in maximum depth and behavior with both fish spending 97% of time at sea <6 m depth (day and night). All study fish were double tagged with passive integrated transponder (PIT) tags implanted in the body cavity. Less than 4% of PIT tags were retained in postspawn steelhead. Molecular genetics demonstrated no significant differences in genetic population structure across years or among spawning life history types, suggesting a genetically panmictic population with highly diverse life history characteristics in the Ninilchik River.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Canadian Journal of Fisheries and Aquatic Sciences","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1139/F10-124","issn":"0706652X","usgsCitation":"Nielsen, J., Turner, S., and Zimmerman, C.E., 2011, Electronic tags and genetics explore variation in migrating steelhead kelts (oncorhynchus mykiss), Ninilchik river, Alaska: Canadian Journal of Fisheries and Aquatic Sciences, v. 68, no. 1, p. 1-16, https://doi.org/10.1139/F10-124.","startPage":"1","endPage":"16","numberOfPages":"16","costCenters":[],"links":[{"id":244325,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":216454,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1139/F10-124"}],"volume":"68","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a08ace4b0c8380cd51c0e","contributors":{"authors":[{"text":"Nielsen, J.L.","contributorId":105665,"corporation":false,"usgs":true,"family":"Nielsen","given":"J.L.","email":"","affiliations":[],"preferred":false,"id":451482,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Turner, S.M.","contributorId":100220,"corporation":false,"usgs":true,"family":"Turner","given":"S.M.","email":"","affiliations":[],"preferred":false,"id":451481,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Zimmerman, Christian E. 0000-0002-3646-0688 czimmerman@usgs.gov","orcid":"https://orcid.org/0000-0002-3646-0688","contributorId":410,"corporation":false,"usgs":true,"family":"Zimmerman","given":"Christian","email":"czimmerman@usgs.gov","middleInitial":"E.","affiliations":[{"id":120,"text":"Alaska Science Center Water","active":true,"usgs":true},{"id":116,"text":"Alaska Science Center Biology MFEB","active":true,"usgs":true},{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"preferred":true,"id":451480,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70043452,"text":"70043452 - 2011 - Furunculosis and other aeromonad diseases","interactions":[],"lastModifiedDate":"2015-03-10T12:02:23","indexId":"70043452","displayToPublicDate":"2011-01-01T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Furunculosis and other aeromonad diseases","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Fish diseases and disorders: viral, bacterial and fungal, Volume 3: viral, bacterial and fungal infections","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"CAB International","usgsCitation":"Cipriano, R.C., and Austin, B., 2011, Furunculosis and other aeromonad diseases, chap. <i>of</i> Fish diseases and disorders: viral, bacterial and fungal, Volume 3: viral, bacterial and fungal infections, v. 3, p. 424-484.","productDescription":"61 p.","startPage":"424","endPage":"484","numberOfPages":"61","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-015535","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":272385,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"3","edition":"2nd","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5198a35de4b0eb382b44ac73","contributors":{"authors":[{"text":"Cipriano, Rocco C. rcipriano@usgs.gov","contributorId":2487,"corporation":false,"usgs":true,"family":"Cipriano","given":"Rocco","email":"rcipriano@usgs.gov","middleInitial":"C.","affiliations":[],"preferred":true,"id":473617,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Austin, Brian","contributorId":56541,"corporation":false,"usgs":true,"family":"Austin","given":"Brian","affiliations":[],"preferred":false,"id":473618,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70003449,"text":"70003449 - 2011 - Inference for occupancy and occupancy dynamics","interactions":[],"lastModifiedDate":"2016-09-26T09:57:52","indexId":"70003449","displayToPublicDate":"2011-01-01T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Inference for occupancy and occupancy dynamics","docAbstract":"<p><span>This chapter deals with the estimation of occupancy as a state variable to assess the status of, and track changes in, species distributions when sampling with camera traps. Much of the recent interest in occupancy estimation and modeling originated from the models developed by MacKenzie et al. (2002, 2003), although similar methods were developed independently (Azuma et al. 1990; Bayley and Petersen 2001; Nichols and Karanth, 2002; Tyre et al. 2003), all of which deal with species occurrence information and imperfect detection. Less than a decade after these publications, the modeling and estimation of species occurrence and occupancy dynamics have increased significantly. Special features of scientific journals have explored innovative uses of detection–nondetection data with occupancy models (Vojta 2005), and an entire volume has synthesized the use and application of occupancy estimation methods (MacKenzie et al. 2006). Reviews of the topical concepts, philosophical considerations, and various sampling designs that can be used for occupancy estimation are now readily available for a range of audiences (MacKenzie and Royle 2005; MacKenzie et al. 2006; Bailey et al. 2007; Royle and Dorazio 2008; Conroy and Carroll 2009; Kendall and White 2009; Hines et al. 2010; Link and Barker 2010). As a result, it would be pointless here to recast all that these publications have so eloquently articulated, but that said, a review of any scientific topic requires sufficient context and relevant background information, especially when relatively new methodologies and techniques such as occupancy estimation and camera traps are involved. This is especially critical in a digital age where new information is published at warp speed, making it increasingly difficult to stay abreast of theoretical advances and research developments.</span></p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Camera traps in animal ecology","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Springer","doi":"10.1007/978-4-431-99495-4_11","usgsCitation":"O’Connell, A.F., and Bailey, L., 2011, Inference for occupancy and occupancy dynamics, chap. <i>of</i> Camera traps in animal ecology, p. 191-204, https://doi.org/10.1007/978-4-431-99495-4_11.","productDescription":"14 p.","startPage":"191","endPage":"204","ipdsId":"IP-021692","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":328952,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"UNITED STATES","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57f7f5bae4b0bc0bec0a1814","contributors":{"editors":[{"text":"O’Connell, Allan F. 0000-0001-7032-7023 aoconnell@usgs.gov","orcid":"https://orcid.org/0000-0001-7032-7023","contributorId":471,"corporation":false,"usgs":true,"family":"O’Connell","given":"Allan","email":"aoconnell@usgs.gov","middleInitial":"F.","affiliations":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"preferred":true,"id":649603,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Nichols, James D. jnichols@usgs.gov","contributorId":139087,"corporation":false,"usgs":true,"family":"Nichols","given":"James D.","email":"jnichols@usgs.gov","affiliations":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"preferred":false,"id":649604,"contributorType":{"id":2,"text":"Editors"},"rank":2},{"text":"Karanth, K. Ullas","contributorId":6984,"corporation":false,"usgs":true,"family":"Karanth","given":"K.","email":"","middleInitial":"Ullas","affiliations":[],"preferred":false,"id":649605,"contributorType":{"id":2,"text":"Editors"},"rank":3}],"authors":[{"text":"O’Connell, Allan F. 0000-0001-7032-7023 aoconnell@usgs.gov","orcid":"https://orcid.org/0000-0001-7032-7023","contributorId":471,"corporation":false,"usgs":true,"family":"O’Connell","given":"Allan","email":"aoconnell@usgs.gov","middleInitial":"F.","affiliations":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"preferred":true,"id":649601,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bailey, Larissa L.","contributorId":93183,"corporation":false,"usgs":true,"family":"Bailey","given":"Larissa L.","affiliations":[],"preferred":false,"id":649602,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70036199,"text":"70036199 - 2011 - Redefinition and global estimation of basal ecosystem respiration rate","interactions":[],"lastModifiedDate":"2017-04-06T13:51:15","indexId":"70036199","displayToPublicDate":"2011-01-01T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1836,"text":"Global Biogeochemical Cycles","active":true,"publicationSubtype":{"id":10}},"title":"Redefinition and global estimation of basal ecosystem respiration rate","docAbstract":"<p><span>Basal ecosystem respiration rate (BR), the ecosystem respiration rate at a given temperature, is a common and important parameter in empirical models for quantifying ecosystem respiration (ER) globally. Numerous studies have indicated that BR varies in space. However, many empirical ER models still use a global constant BR largely due to the lack of a functional description for BR. In this study, we redefined BR to be ecosystem respiration rate at the mean annual temperature. To test the validity of this concept, we conducted a synthesis analysis using 276 site-years of eddy covariance data, from 79 research sites located at latitudes ranging from ∼3°S to ∼70°N. Results showed that mean annual ER rate closely matches ER rate at mean annual temperature. Incorporation of site-specific BR into global ER model substantially improved simulated ER compared to an invariant BR at all sites. These results confirm that ER at the mean annual temperature can be considered as BR in empirical models. A strong correlation was found between the mean annual ER and mean annual gross primary production (GPP). Consequently, GPP, which is typically more accurately modeled, can be used to estimate BR. A light use efficiency GPP model (i.e., EC-LUE) was applied to estimate global GPP, BR and ER with input data from MERRA (Modern Era Retrospective-Analysis for Research and Applications) and MODIS (Moderate resolution Imaging Spectroradiometer). The global ER was 103 Pg C yr </span><sup>−1</sup><span>, with the highest respiration rate over tropical forests and the lowest value in dry and high-latitude areas.</span></p>","language":"English","publisher":"AGU","doi":"10.1029/2011GB004150","issn":"08866236","usgsCitation":"Yuan, W., Luo, Y., Li, X., Liu, S., Yu, G., Zhou, T., Bahn, M., Black, A., Desai, A., Cescatti, A., Marcolla, B., Jacobs, C., Chen, J., Aurela, M., Bernhofer, C., Gielen, B., Bohrer, G., Cook, D., Dragoni, D., Dunn, A., Gianelle, D., Grnwald, T., Ibrom, A., Leclerc, M., Lindroth, A., Liu, H., Marchesini, L., Montagnani, L., Pita, G., Rodeghiero, M., Rodrigues, A., Starr, G., and Stoy, P., 2011, Redefinition and global estimation of basal ecosystem respiration rate: Global Biogeochemical Cycles, v. 25, no. 4, p. 1-14, https://doi.org/10.1029/2011GB004150.","productDescription":"Article GB4002; 14 p.","startPage":"1","endPage":"14","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":475325,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1029/2011gb004150","text":"Publisher Index Page"},{"id":246334,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":218335,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1029/2011GB004150"}],"volume":"25","issue":"4","noUsgsAuthors":false,"publicationDate":"2011-10-13","publicationStatus":"PW","scienceBaseUri":"50e4a3a7e4b0e8fec6cdb8fc","contributors":{"authors":[{"text":"Yuan, W.","contributorId":35955,"corporation":false,"usgs":true,"family":"Yuan","given":"W.","email":"","affiliations":[],"preferred":false,"id":454807,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Luo, Y.","contributorId":28417,"corporation":false,"usgs":true,"family":"Luo","given":"Y.","email":"","affiliations":[],"preferred":false,"id":454802,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Li, X.","contributorId":67635,"corporation":false,"usgs":true,"family":"Li","given":"X.","email":"","affiliations":[],"preferred":false,"id":454821,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Liu, S.","contributorId":93170,"corporation":false,"usgs":true,"family":"Liu","given":"S.","affiliations":[],"preferred":false,"id":454825,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Yu, G.","contributorId":61198,"corporation":false,"usgs":true,"family":"Yu","given":"G.","email":"","affiliations":[],"preferred":false,"id":454819,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Zhou, T.","contributorId":93248,"corporation":false,"usgs":true,"family":"Zhou","given":"T.","email":"","affiliations":[],"preferred":false,"id":454826,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Bahn, M.","contributorId":100668,"corporation":false,"usgs":true,"family":"Bahn","given":"M.","email":"","affiliations":[],"preferred":false,"id":454827,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Black, A.","contributorId":62870,"corporation":false,"usgs":true,"family":"Black","given":"A.","email":"","affiliations":[],"preferred":false,"id":454820,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Desai, A.R.","contributorId":28835,"corporation":false,"usgs":true,"family":"Desai","given":"A.R.","email":"","affiliations":[],"preferred":false,"id":454804,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Cescatti, A.","contributorId":25023,"corporation":false,"usgs":true,"family":"Cescatti","given":"A.","affiliations":[],"preferred":false,"id":454801,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Marcolla, B.","contributorId":105573,"corporation":false,"usgs":true,"family":"Marcolla","given":"B.","email":"","affiliations":[],"preferred":false,"id":454829,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Jacobs, C.","contributorId":55251,"corporation":false,"usgs":true,"family":"Jacobs","given":"C.","email":"","affiliations":[],"preferred":false,"id":454816,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Chen, J.","contributorId":104634,"corporation":false,"usgs":true,"family":"Chen","given":"J.","email":"","affiliations":[],"preferred":false,"id":454828,"contributorType":{"id":1,"text":"Authors"},"rank":13},{"text":"Aurela, M.","contributorId":85448,"corporation":false,"usgs":true,"family":"Aurela","given":"M.","affiliations":[],"preferred":false,"id":454823,"contributorType":{"id":1,"text":"Authors"},"rank":14},{"text":"Bernhofer, C.","contributorId":37964,"corporation":false,"usgs":true,"family":"Bernhofer","given":"C.","email":"","affiliations":[],"preferred":false,"id":454808,"contributorType":{"id":1,"text":"Authors"},"rank":15},{"text":"Gielen, B.","contributorId":28467,"corporation":false,"usgs":true,"family":"Gielen","given":"B.","email":"","affiliations":[],"preferred":false,"id":454803,"contributorType":{"id":1,"text":"Authors"},"rank":16},{"text":"Bohrer, G.","contributorId":60892,"corporation":false,"usgs":true,"family":"Bohrer","given":"G.","affiliations":[],"preferred":false,"id":454818,"contributorType":{"id":1,"text":"Authors"},"rank":17},{"text":"Cook, D.R.","contributorId":20585,"corporation":false,"usgs":true,"family":"Cook","given":"D.R.","email":"","affiliations":[],"preferred":false,"id":454799,"contributorType":{"id":1,"text":"Authors"},"rank":18},{"text":"Dragoni, D.","contributorId":30490,"corporation":false,"usgs":true,"family":"Dragoni","given":"D.","email":"","affiliations":[],"preferred":false,"id":454805,"contributorType":{"id":1,"text":"Authors"},"rank":19},{"text":"Dunn, A.L.","contributorId":87793,"corporation":false,"usgs":true,"family":"Dunn","given":"A.L.","email":"","affiliations":[],"preferred":false,"id":454824,"contributorType":{"id":1,"text":"Authors"},"rank":20},{"text":"Gianelle, D.","contributorId":47205,"corporation":false,"usgs":true,"family":"Gianelle","given":"D.","email":"","affiliations":[],"preferred":false,"id":454815,"contributorType":{"id":1,"text":"Authors"},"rank":21},{"text":"Grnwald, T.","contributorId":45160,"corporation":false,"usgs":true,"family":"Grnwald","given":"T.","email":"","affiliations":[],"preferred":false,"id":454812,"contributorType":{"id":1,"text":"Authors"},"rank":22},{"text":"Ibrom, A.","contributorId":46809,"corporation":false,"usgs":true,"family":"Ibrom","given":"A.","email":"","affiliations":[],"preferred":false,"id":454814,"contributorType":{"id":1,"text":"Authors"},"rank":23},{"text":"Leclerc, M.Y.","contributorId":78596,"corporation":false,"usgs":true,"family":"Leclerc","given":"M.Y.","email":"","affiliations":[],"preferred":false,"id":454822,"contributorType":{"id":1,"text":"Authors"},"rank":24},{"text":"Lindroth, A.","contributorId":24610,"corporation":false,"usgs":true,"family":"Lindroth","given":"A.","email":"","affiliations":[],"preferred":false,"id":454800,"contributorType":{"id":1,"text":"Authors"},"rank":25},{"text":"Liu, H.","contributorId":12222,"corporation":false,"usgs":true,"family":"Liu","given":"H.","affiliations":[],"preferred":false,"id":454798,"contributorType":{"id":1,"text":"Authors"},"rank":26},{"text":"Marchesini, L.B.","contributorId":38402,"corporation":false,"usgs":true,"family":"Marchesini","given":"L.B.","email":"","affiliations":[],"preferred":false,"id":454809,"contributorType":{"id":1,"text":"Authors"},"rank":27},{"text":"Montagnani, L.","contributorId":33157,"corporation":false,"usgs":true,"family":"Montagnani","given":"L.","email":"","affiliations":[],"preferred":false,"id":454806,"contributorType":{"id":1,"text":"Authors"},"rank":28},{"text":"Pita, G.","contributorId":42074,"corporation":false,"usgs":true,"family":"Pita","given":"G.","email":"","affiliations":[],"preferred":false,"id":454810,"contributorType":{"id":1,"text":"Authors"},"rank":29},{"text":"Rodeghiero, M.","contributorId":107547,"corporation":false,"usgs":true,"family":"Rodeghiero","given":"M.","email":"","affiliations":[],"preferred":false,"id":454830,"contributorType":{"id":1,"text":"Authors"},"rank":30},{"text":"Rodrigues, A.","contributorId":45161,"corporation":false,"usgs":true,"family":"Rodrigues","given":"A.","email":"","affiliations":[],"preferred":false,"id":454813,"contributorType":{"id":1,"text":"Authors"},"rank":31},{"text":"Starr, G.","contributorId":44776,"corporation":false,"usgs":true,"family":"Starr","given":"G.","email":"","affiliations":[],"preferred":false,"id":454811,"contributorType":{"id":1,"text":"Authors"},"rank":32},{"text":"Stoy, Paul C.","contributorId":60860,"corporation":false,"usgs":true,"family":"Stoy","given":"Paul C.","affiliations":[],"preferred":false,"id":454817,"contributorType":{"id":1,"text":"Authors"},"rank":33}]}}
,{"id":70035721,"text":"70035721 - 2011 - Distribution and seasonal dynamics of arsenic in a shallow lake in northwestern New Jersey, USA","interactions":[],"lastModifiedDate":"2019-10-21T09:58:09","indexId":"70035721","displayToPublicDate":"2011-01-01T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1538,"text":"Environmental Geochemistry and Health","active":true,"publicationSubtype":{"id":10}},"title":"Distribution and seasonal dynamics of arsenic in a shallow lake in northwestern New Jersey, USA","docAbstract":"<p><span>Elevated concentrations of arsenic (As) occurred during warm months in water from the outlet of Lake Mohawk in northwestern New Jersey. The shallow manmade lake is surrounded by residential development and used for recreation. Eutrophic conditions are addressed by alum and copper sulfate applications and aerators operating in the summer. In September 2005, arsenite was dominant in hypoxic to anoxic bottom water. Filterable As concentrations were about 1.6–2 times higher than those in the upper water column (23–25&nbsp;μg/L, mostly arsenate). Hypoxic/anoxic and near-neutral bottom conditions formed during the summer, but became more oxic and alkaline as winter approached. Acid-leachable As concentrations in lake-bed sediments ranged up to 694&nbsp;mg/kg in highly organic material from the tops of sediment cores but were &lt;15&nbsp;mg/kg in geologic substrate. During warm months, reduced As from the sediment diffuses into the water column and is oxidized; mixing by aerators, wind, and boat traffic spreads arsenate and metals, some in particulate form, throughout the water column. Similar levels of As in sediments of lakes treated with arsenic pesticides indicate that most of the As in Lake Mohawk probably derives from past use of arsenical pesticides, although records of applications are lacking. The annual loss of As at the lake outlet is only about 0.01% of the As calculated to be in the sediments, indicating that elevated levels of As in the lake will persist for decades.</span></p>","language":"English","publisher":"Springer","doi":"10.1007/s10653-010-9289-7","issn":"02694042","usgsCitation":"Barringer, J.L., Szabo, Z., Wilson, T., Bonin, J., Kratzer, T., Cenno, K., Romagna, T., Alebus, M., and Hirst, B., 2011, Distribution and seasonal dynamics of arsenic in a shallow lake in northwestern New Jersey, USA: Environmental Geochemistry and Health, v. 33, no. 1, p. 1-22, https://doi.org/10.1007/s10653-010-9289-7.","productDescription":"22 p.","startPage":"1","endPage":"22","numberOfPages":"22","costCenters":[{"id":470,"text":"New Jersey Water Science Center","active":true,"usgs":true}],"links":[{"id":243981,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New Jersey","otherGeospatial":"Lake Mohawk","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -74.65115547180176,\n              41.036765293038194\n            ],\n            [\n              -74.6645450592041,\n              41.0204485149169\n            ],\n            [\n              -74.65930938720703,\n              41.02031900050546\n            ],\n            [\n              -74.65948104858398,\n              41.0191533593421\n            ],\n            [\n              -74.67278480529785,\n              41.012482904826015\n            ],\n            [\n              -74.67347145080566,\n              41.014620114274955\n            ],\n            [\n              -74.6769905090332,\n              41.01403724584675\n            ],\n            [\n              -74.6854019165039,\n              41.007495813151536\n            ],\n            [\n              -74.68445777893066,\n              41.003220862709\n            ],\n            [\n              -74.67098236083984,\n              41.00600608917637\n            ],\n            [\n              -74.6561336517334,\n              41.01202954845378\n            ],\n            [\n              -74.63836669921874,\n              41.0313915626804\n            ],\n            [\n              -74.65115547180176,\n              41.036765293038194\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"33","issue":"1","noUsgsAuthors":false,"publicationDate":"2010-04-20","publicationStatus":"PW","scienceBaseUri":"505a029fe4b0c8380cd50128","contributors":{"authors":[{"text":"Barringer, J. L.","contributorId":13994,"corporation":false,"usgs":true,"family":"Barringer","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":452054,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Szabo, Z. 0000-0002-0760-9607","orcid":"https://orcid.org/0000-0002-0760-9607","contributorId":44302,"corporation":false,"usgs":true,"family":"Szabo","given":"Z.","affiliations":[],"preferred":false,"id":452056,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wilson, T.P. 0000-0003-1914-6344","orcid":"https://orcid.org/0000-0003-1914-6344","contributorId":99795,"corporation":false,"usgs":true,"family":"Wilson","given":"T.P.","affiliations":[],"preferred":false,"id":452061,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bonin, J.L. 0000-0002-5813-3549","orcid":"https://orcid.org/0000-0002-5813-3549","contributorId":55642,"corporation":false,"usgs":true,"family":"Bonin","given":"J.L.","email":"","affiliations":[],"preferred":false,"id":452057,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Kratzer, T.","contributorId":105532,"corporation":false,"usgs":true,"family":"Kratzer","given":"T.","email":"","affiliations":[],"preferred":false,"id":452062,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Cenno, K.","contributorId":66919,"corporation":false,"usgs":true,"family":"Cenno","given":"K.","email":"","affiliations":[],"preferred":false,"id":452058,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Romagna, T.","contributorId":37155,"corporation":false,"usgs":true,"family":"Romagna","given":"T.","email":"","affiliations":[],"preferred":false,"id":452055,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Alebus, M.","contributorId":84166,"corporation":false,"usgs":true,"family":"Alebus","given":"M.","affiliations":[],"preferred":false,"id":452060,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Hirst, B.","contributorId":78555,"corporation":false,"usgs":true,"family":"Hirst","given":"B.","email":"","affiliations":[],"preferred":false,"id":452059,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}}
,{"id":70035774,"text":"70035774 - 2011 - Ecology of invasive <i>Melilotus albus</i> on Alaskan glacial river floodplains","interactions":[],"lastModifiedDate":"2016-08-21T15:25:57","indexId":"70035774","displayToPublicDate":"2011-01-01T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":899,"text":"Arctic, Antarctic, and Alpine Research","active":true,"publicationSubtype":{"id":10}},"title":"Ecology of invasive <i>Melilotus albus</i> on Alaskan glacial river floodplains","docAbstract":"<p><i>Melilotus albus</i><span>&nbsp;(white sweetclover) has invaded Alaskan glacial river floodplains. We measured cover and density of plant species and environmental variables along transects perpendicular to the Nenana, Matanuska, and Stikine Rivers to study interactions between&nbsp;</span><i>M. albus</i><span>&nbsp;and other plant species and to characterize the environment where it establishes.&nbsp;</span><i>Melilotus albus</i><span>&nbsp;was a pioneer species on recently disturbed sites and did not persist into closed canopy forests. The relationships between&nbsp;</span><i>M. albus</i><span>&nbsp;cover and density and other species were site-specific.</span><i>Melilotus albus</i><span>&nbsp;was negatively correlated with native species&nbsp;</span><i>Elaeagnus commutata</i><span>&nbsp;at the Nenana River, but not at the Matanuska River.&nbsp;</span><i>Melilotus albus</i><span>&nbsp;was positively correlated with the exotic species&nbsp;</span><i>Crepis tectorum</i><span>and&nbsp;</span><i>Taraxacum officinale</i><span>&nbsp;at the Matanuska River and&nbsp;</span><i>T. officinale</i><span>&nbsp;on the upper Stikine River. However, the high density of&nbsp;</span><i>M. albus</i><span>&nbsp;at a lower Stikine River site was negatively correlated with&nbsp;</span><i>T. officinale</i><span>&nbsp;and several native species including&nbsp;</span><i>Lathyrus japonicus</i><span>&nbsp;var.&nbsp;</span><i>maritimus</i><span>&nbsp;and&nbsp;</span><i>Salix alaxensis</i><span>. Glacial river floodplains in Alaska are highly disturbed and are corridors for exotic plant species movement.&nbsp;</span><i>Melilotus albus</i><span>&nbsp;at moderate to low densities may facilitate establishment of exotic species, but at high densities can reduce the cover and density of both exotic and native species.</span></p>","largerWorkTitle":"Arctic, Antarctic, and Alpine Research","language":"English","publisher":"Institute of Arctic and Alpine Research","doi":"10.1657/1938-4246-43.3.343","issn":"15230430","usgsCitation":"Conn, J.S., Werdin-Pfisterer, N.R., Beattie, K.L., and Densmore, R.V., 2011, Ecology of invasive <i>Melilotus albus</i> on Alaskan glacial river floodplains: Arctic, Antarctic, and Alpine Research, v. 43, no. 3, p. 343-354, https://doi.org/10.1657/1938-4246-43.3.343.","productDescription":"12 p.","startPage":"343","endPage":"354","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":475188,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1657/1938-4246-43.3.343","text":"Publisher Index Page"},{"id":244242,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Matanuska River, Nenana River, Stikine River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -134.6923828125,\n              55.25407706707272\n            ],\n            [\n              -134.6923828125,\n              58.69977573144006\n            ],\n            [\n              -126.91406249999999,\n              58.69977573144006\n            ],\n            [\n              -126.91406249999999,\n              55.25407706707272\n            ],\n            [\n              -134.6923828125,\n              55.25407706707272\n            ]\n          ]\n        ]\n      }\n    },\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -149.996337890625,\n              61.19356635954457\n            ],\n            [\n              -149.996337890625,\n              61.91309898553723\n            ],\n            [\n              -148.194580078125,\n              61.91309898553723\n            ],\n            [\n              -148.194580078125,\n              61.19356635954457\n            ],\n            [\n              -149.996337890625,\n              61.19356635954457\n            ]\n          ]\n        ]\n      }\n    },\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -149.69970703125,\n              64.24698161075293\n            ],\n            [\n              -149.69970703125,\n              64.86760781632728\n            ],\n            [\n              -147.94189453125,\n              64.86760781632728\n            ],\n            [\n              -147.94189453125,\n              64.24698161075293\n            ],\n            [\n              -149.69970703125,\n              64.24698161075293\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"43","issue":"3","noUsgsAuthors":false,"publicationDate":"2018-01-17","publicationStatus":"PW","scienceBaseUri":"505a0575e4b0c8380cd50dea","contributors":{"authors":[{"text":"Conn, Jeff S.","contributorId":82962,"corporation":false,"usgs":true,"family":"Conn","given":"Jeff","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":452306,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Werdin-Pfisterer, Nancy R.","contributorId":19000,"corporation":false,"usgs":false,"family":"Werdin-Pfisterer","given":"Nancy","email":"","middleInitial":"R.","affiliations":[{"id":6752,"text":"University of Alaska Fairbanks","active":true,"usgs":false}],"preferred":false,"id":452304,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Beattie, Katherine L.","contributorId":23357,"corporation":false,"usgs":false,"family":"Beattie","given":"Katherine","email":"","middleInitial":"L.","affiliations":[{"id":7211,"text":"University of Alaska, Fairbanks","active":true,"usgs":false}],"preferred":false,"id":452305,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Densmore, Roseann V.","contributorId":24022,"corporation":false,"usgs":true,"family":"Densmore","given":"Roseann","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":452303,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70034112,"text":"70034112 - 2011 - Response to comment on \"pAHs underfoot: Contaminated dust from coal-tar sealcoated pavement is widespread in the U.S.\"","interactions":[],"lastModifiedDate":"2023-03-22T16:12:42.114022","indexId":"70034112","displayToPublicDate":"2011-01-01T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1565,"text":"Environmental Science & Technology","onlineIssn":"1520-5851","printIssn":"0013-936X","active":true,"publicationSubtype":{"id":10}},"title":"Response to comment on \"pAHs underfoot: Contaminated dust from coal-tar sealcoated pavement is widespread in the U.S.\"","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"ACS Publications","doi":"10.1021/es200481t","usgsCitation":"Van Metre, P.C., and Mahler, B., 2011, Response to comment on \"pAHs underfoot: Contaminated dust from coal-tar sealcoated pavement is widespread in the U.S.\": Environmental Science & Technology, v. 45, no. 7, p. 3187-3188, https://doi.org/10.1021/es200481t.","productDescription":"2 p.","startPage":"3187","endPage":"3188","numberOfPages":"2","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":475090,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1021/es200481t","text":"Publisher Index Page"},{"id":244422,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"45","issue":"7","noUsgsAuthors":false,"publicationDate":"2011-03-11","publicationStatus":"PW","scienceBaseUri":"505aaa89e4b0c8380cd863b3","contributors":{"authors":[{"text":"Van Metre, Peter C. 0000-0001-7564-9814","orcid":"https://orcid.org/0000-0001-7564-9814","contributorId":211144,"corporation":false,"usgs":true,"family":"Van Metre","given":"Peter","email":"","middleInitial":"C.","affiliations":[{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true},{"id":374,"text":"Maryland Water Science Center","active":true,"usgs":true},{"id":27111,"text":"National Water Quality Program","active":true,"usgs":true},{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":true,"id":444153,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mahler, Barbara 0000-0002-9150-9552 bjmahler@usgs.gov","orcid":"https://orcid.org/0000-0002-9150-9552","contributorId":1249,"corporation":false,"usgs":true,"family":"Mahler","given":"Barbara","email":"bjmahler@usgs.gov","affiliations":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true},{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"preferred":true,"id":444152,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70159146,"text":"70159146 - 2011 - Chapter 39 The Edwardsburg Formation and related rocks, Windermere Supergroup, central Idaho, USA","interactions":[],"lastModifiedDate":"2015-10-15T16:34:22","indexId":"70159146","displayToPublicDate":"2011-01-01T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2711,"text":"Memoir of the Geological Society of America","active":true,"publicationSubtype":{"id":10}},"title":"Chapter 39 The Edwardsburg Formation and related rocks, Windermere Supergroup, central Idaho, USA","docAbstract":"<p><span>In central Idaho, Neoproterozoic stratified rocks are engulfed by the Late Cretaceous Idaho batholith and by Eocene volcanic and plutonic rocks of the Challis event. Studied sections in the Gospel Peaks and Big Creek areas of west-central Idaho are in roof pendants of the Idaho batholith. A drill core section studied from near Challis, east-central Idaho, lies beneath the Challis Volcanic Group and is not exposed at the surface. Metamorphic and deformational overprinting, as well as widespread dismembering by the younger igneous rocks, conceals many primary details. Despite this, these rocks provide important links for regional correlations and have produced critical geochronological data for two Neoproterozoic glacial periods in the North American Cordillera. At the base of the section, the more than 700-m-thick Edwardsburg Formation (Fm.) contains interlayered diamictite and volcanic rocks. There are two diamictite-bearing members in the Edwardsburg Fm. that are closely related in time. Each of the diamictites is associated with intermediate composition tuff or flow rocks and the diamictites are separated by mafic volcanic rocks. SHRIMP U&ndash;Pb dating indicates that the lower diamictite is about 685&plusmn;7 Ma, whereas the upper diamictite is 684&plusmn;4 Ma. The diamictite units are part of a cycle of rocks from coarse clastic, to fine clastic, to carbonate rocks that, by correlation to better preserved sections, are thought to record an older Cryogenian glacial to interglacial period in the northern US Cordillera. The more than 75-m-thick diamictite of Daugherty Gulch is dated at 664&plusmn;6 Ma. This unit is preserved only in drill core and the palaeoenvironmental interpretation and local stratigraphic relations are non-unique. Thus, the date for this diamictite may provide a date for a newly recognized glaciogenic horizon or may be a minimum age for the diamictite in the Edwardsburg Fm. The c. 1000-m-thick Moores Lake Fm. is an amphibolite facies diamictite in which glacial features have not been observed. However, it is part of a sedimentary cycle from unsorted siliclastic deposits to mud and carbonate deposits. Using lithostratigraphy and available geochronology, the Moores Lake Fm. is correlated with a younger succession of Cryogenian glaciogenic rocks in southeastern Idaho. Traditional correlations of Neoproterozoic rocks in the Cordillera recognize two levels of Cryogenian diamictites. The Edwardsburg and Moores Lake diamictites along the middle Cordillera fit well into the scenario of two glacial events. Because of the correlations, dates that provide ages for the diamictites in central Idaho (and corroborated in southeastern Idaho, Link &amp; Fanning 2008) could constrain the age of correlated glaciogenic deposits elsewhere in the Cordillera. However, in the absence of dates for the glaciogenic diamictites in Canadian and southern US Cordilleran sections, the correlations are considered possible but uncertain.</span></p>","language":"English","publisher":"The Geological Society","usgsCitation":"Lund, K., Evans, K.V., and Alienikoff, J.N., 2011, Chapter 39 The Edwardsburg Formation and related rocks, Windermere Supergroup, central Idaho, USA: Memoir of the Geological Society of America, v. 36, p. 437-448.","productDescription":"12 p.","startPage":"437","endPage":"448","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":309968,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Idaho","otherGeospatial":"Central Idaho","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -116.98242187499999,\n              46.17983040759436\n            ],\n            [\n              -114.43359375,\n              46.10370875598026\n            ],\n            [\n              -112.8955078125,\n              44.402391829093915\n            ],\n            [\n              -113.02734374999999,\n              44.02442151965934\n            ],\n            [\n              -117.04833984375001,\n              43.78695837311561\n            ],\n            [\n              -116.96044921875,\n              44.18220395771566\n            ],\n            [\n              -117.20214843749999,\n              44.37098696297173\n            ],\n            [\n              -117.00439453125,\n              44.77793589631623\n            ],\n            [\n              -116.806640625,\n              45.24395342262324\n            ],\n            [\n              -116.78466796875,\n              45.521743896993634\n            ],\n            [\n              -117.04833984375001,\n              46.08847179577592\n            ],\n            [\n              -116.98242187499999,\n              46.17983040759436\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"36","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5620ce57e4b06217fc478acd","contributors":{"authors":[{"text":"Lund, Karen 0000-0002-4249-3582 klund@usgs.gov","orcid":"https://orcid.org/0000-0002-4249-3582","contributorId":1235,"corporation":false,"usgs":true,"family":"Lund","given":"Karen","email":"klund@usgs.gov","affiliations":[{"id":387,"text":"Mineral Resources Program","active":true,"usgs":true},{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":577699,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Evans, Karl V. kvevans@usgs.gov","contributorId":194,"corporation":false,"usgs":true,"family":"Evans","given":"Karl","email":"kvevans@usgs.gov","middleInitial":"V.","affiliations":[],"preferred":true,"id":577700,"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":577701,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70193259,"text":"70193259 - 2011 - Radiotelemetry to estimate stream life of adult chum salmon in the McNeil River, Alaska","interactions":[],"lastModifiedDate":"2017-11-15T14:50:33","indexId":"70193259","displayToPublicDate":"2011-01-01T00:00:00","publicationYear":"2011","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":"Radiotelemetry to estimate stream life of adult chum salmon in the McNeil River, Alaska","docAbstract":"<p><span>Estimating salmon escapement is one of the fundamental steps in managing salmon populations. The area-under-the-curve (AUC) method is commonly used to convert periodic aerial survey counts into annual salmon escapement indices. The AUC requires obtaining accurate estimates of stream life (SL) for target species. Traditional methods for estimating SL (e.g., mark–recapture) are not feasible for many populations. Our objective in this study was to determine the average SL of chum salmon&nbsp;</span><i>Oncorhynchus keta</i><span><span>&nbsp;</span>in the McNeil River, Alaska, through radiotelemetry. During the 2005 and 2006 runs, 155 chum salmon were fitted with mortality-indicating radio tags as they entered the McNeil River and tracked until they died. A combination of remote data loggers, aerial surveys, and foot surveys were used to determine the location of fish and provide an estimate of time of death. Higher predation resulted in tagged fish below McNeil Falls having a significantly shorter SL (12.6 d) than those above (21.9 d). The streamwide average SL (13.8 d) for chum salmon at the McNeil River was lower than the regionwide value (17.5 d) previously used to generate AUC indices of chum salmon escapement for the McNeil River. We conclude that radiotelemetry is an effective tool for estimating SL in rivers not well suited to other methods.</span></p>","language":"English","publisher":"Taylor & Francis","doi":"10.1080/02755947.2011.574080","usgsCitation":"Peirce, J., Otis, E.O., Wipfli, M.S., and Follmann, E., 2011, Radiotelemetry to estimate stream life of adult chum salmon in the McNeil River, Alaska: North American Journal of Fisheries Management, v. 31, no. 2, p. 315-322, https://doi.org/10.1080/02755947.2011.574080.","productDescription":"8 p.","startPage":"315","endPage":"322","ipdsId":"IP-013106","costCenters":[{"id":199,"text":"Coop Res Unit Leetown","active":true,"usgs":true}],"links":[{"id":348914,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"McNeil River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -154.2978286743164,\n              59.0957028026867\n            ],\n            [\n              -154.2037582397461,\n              59.0957028026867\n            ],\n            [\n              -154.2037582397461,\n              59.13843678215489\n            ],\n            [\n              -154.2978286743164,\n              59.13843678215489\n            ],\n            [\n              -154.2978286743164,\n              59.0957028026867\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"31","issue":"2","publishingServiceCenter":{"id":9,"text":"Reston PSC"},"noUsgsAuthors":false,"publicationDate":"2011-05-02","publicationStatus":"PW","scienceBaseUri":"5a6107fce4b06e28e9c25632","contributors":{"authors":[{"text":"Peirce, Joshua","contributorId":42510,"corporation":false,"usgs":true,"family":"Peirce","given":"Joshua","email":"","affiliations":[],"preferred":false,"id":722265,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Otis, Edward O.","contributorId":19065,"corporation":false,"usgs":true,"family":"Otis","given":"Edward","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":722266,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wipfli, Mark S. 0000-0002-4856-6068 mwipfli@usgs.gov","orcid":"https://orcid.org/0000-0002-4856-6068","contributorId":1425,"corporation":false,"usgs":true,"family":"Wipfli","given":"Mark","email":"mwipfli@usgs.gov","middleInitial":"S.","affiliations":[{"id":200,"text":"Coop Res Unit Seattle","active":true,"usgs":true}],"preferred":true,"id":718461,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Follmann, Erich H.","contributorId":75049,"corporation":false,"usgs":true,"family":"Follmann","given":"Erich H.","affiliations":[],"preferred":false,"id":722267,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
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