{"pageNumber":"1978","pageRowStart":"49425","pageSize":"25","recordCount":184633,"records":[{"id":70003634,"text":"70003634 - 2009 - The golden rule of reviewing","interactions":[],"lastModifiedDate":"2013-02-23T21:22:44","indexId":"70003634","displayToPublicDate":"2012-01-01T00:00:00","publicationYear":"2009","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":740,"text":"American Naturalist","active":true,"publicationSubtype":{"id":10}},"title":"The golden rule of reviewing","docAbstract":"A major bottleneck in the time required to publish a scientific or scholarly paper is the speed with which reviews by peers are returned to journals. Peer review is a reciprocal altruistic system in which each individual may perform every task—editors, reviewers, and authors—at different times. Journals have no way to coerce reviewers to return their critiques faster. To greatly shorten the time to publication, all actors in this altruistic network should abide by the Golden Rule of Reviewing: review for others as you would have others review for you. Say yes to reviewing whenever your duties and schedule allow; provide a thorough, fair, and constructive critique of the work; and do it at your first opportunity regardless of the deadline.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"American Naturalist","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"The American Society of Naturalists","publisherLocation":"Chicago, IL","doi":"10.1086/598847","usgsCitation":"McPeek, M.A., DeAngelis, D., Shaw, R.G., Moore, A.J., Rausher, M.D., Strong, D.R., Ellison, A.M., Barrett, L., Rieseberg, L., Breed, M.D., Sullivan, J., Osenberg, C.W., Holyoak, M., and Elgar, M.A., 2009, The golden rule of reviewing: American Naturalist, v. 173, no. 5, p. E155-E158, https://doi.org/10.1086/598847.","productDescription":"4 p.","startPage":"E155","endPage":"E158","costCenters":[{"id":566,"text":"Southeast Ecological Science Center","active":true,"usgs":true}],"links":[{"id":268050,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1086/598847"},{"id":204475,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"173","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bac92e4b08c986b3235b5","contributors":{"authors":[{"text":"McPeek, Mark A.","contributorId":75818,"corporation":false,"usgs":true,"family":"McPeek","given":"Mark","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":348055,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"DeAngelis, Donald L. 0000-0002-1570-4057","orcid":"https://orcid.org/0000-0002-1570-4057","contributorId":88015,"corporation":false,"usgs":true,"family":"DeAngelis","given":"Donald L.","affiliations":[],"preferred":false,"id":348057,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Shaw, Ruth G.","contributorId":70656,"corporation":false,"usgs":true,"family":"Shaw","given":"Ruth","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":348052,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Moore, Allen J.","contributorId":73069,"corporation":false,"usgs":true,"family":"Moore","given":"Allen","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":348053,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Rausher, Mark D.","contributorId":61716,"corporation":false,"usgs":true,"family":"Rausher","given":"Mark","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":348051,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Strong, Donald R.","contributorId":73882,"corporation":false,"usgs":true,"family":"Strong","given":"Donald","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":348054,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Ellison, Aaron M.","contributorId":37058,"corporation":false,"usgs":true,"family":"Ellison","given":"Aaron","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":348047,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Barrett, Louise","contributorId":31635,"corporation":false,"usgs":true,"family":"Barrett","given":"Louise","email":"","affiliations":[],"preferred":false,"id":348046,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Rieseberg, Loren","contributorId":80552,"corporation":false,"usgs":true,"family":"Rieseberg","given":"Loren","affiliations":[],"preferred":false,"id":348056,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Breed, Michael D.","contributorId":90601,"corporation":false,"usgs":true,"family":"Breed","given":"Michael","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":348058,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Sullivan, Jack","contributorId":53660,"corporation":false,"usgs":true,"family":"Sullivan","given":"Jack","email":"","affiliations":[],"preferred":false,"id":348048,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Osenberg, Craig W.","contributorId":58899,"corporation":false,"usgs":true,"family":"Osenberg","given":"Craig","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":348049,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Holyoak, Marcel","contributorId":15076,"corporation":false,"usgs":false,"family":"Holyoak","given":"Marcel","email":"","affiliations":[{"id":7082,"text":"University of California - Davis","active":true,"usgs":false}],"preferred":false,"id":348045,"contributorType":{"id":1,"text":"Authors"},"rank":13},{"text":"Elgar, Mark A.","contributorId":59684,"corporation":false,"usgs":true,"family":"Elgar","given":"Mark","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":348050,"contributorType":{"id":1,"text":"Authors"},"rank":14}]}}
,{"id":70041338,"text":"70041338 - 2009 - Laguna del Maule volcanic field: Eruptive history of a Quaternary basalt-to-rhyolite distributed volcanic field on the Andean rangecrest in central Chile","interactions":[],"lastModifiedDate":"2022-04-12T15:55:35.292816","indexId":"70041338","displayToPublicDate":"2012-01-01T00:00:00","publicationYear":"2009","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":3,"text":"Organization Series"},"seriesTitle":{"id":162,"text":"Bulletin","active":false,"publicationSubtype":{"id":3}},"seriesNumber":"63","title":"Laguna del Maule volcanic field: Eruptive history of a Quaternary basalt-to-rhyolite distributed volcanic field on the Andean rangecrest in central Chile","docAbstract":"The Laguna del Maule (LdM) volcanic field, which surrounds the 54-km<sup>2</sup> lake of that name, covers ~500 km<sup>2</sup> of rugged glaciated terrain with Quaternary lavas and tuffs that extend for 40 km westward from the Argentine frontier and 30 km north-south from the Rio Campanario to Laguna Fea. The distributed rear-arc volcanic field is contiguous with the Tatara-San Pedro stratovolcano complex on the volcanic front of the Quaternary Andean arc. The LdM field has had few large edifices but at least 130 separate vents have been identified, from which >350 km<sup>3</sup> of products have erupted since 1.5 Ma. Products of 14 ice-ravaged (early and middle Pleistocene) stratocones and shields, and of ~115 monogenetic cones, domes, and lava flows, were mapped on foot, studied petrographically, and chemically analyzed. More than 70 radiometric ages were determined to calibrate the eruptive sequence. A large welded ignimbrite erupted at 1.5 Ma and was followed by another at ~950 ka, producing a 12 x 8 km-wide caldera that underlies the north half or the lake basin and rugged highlands north of it; outside the caldera, the south half of the basin is an erosional feature cut on Tertiary andesites and dacites.","language":"English","publisher":"Servicio Nacional de Geología y Minería","publisherLocation":"Santiago, Chile","usgsCitation":"Hildreth, W., Godoy, E., Fierstein, J., and Singer, B., 2009, Laguna del Maule volcanic field: Eruptive history of a Quaternary basalt-to-rhyolite distributed volcanic field on the Andean rangecrest in central Chile: Bulletin 63, 145 p.","productDescription":"145 p.","startPage":"1","endPage":"145","ipdsId":"IP-017560","costCenters":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"links":[{"id":398547,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Chile","otherGeospatial":"Andes Mountains, Laguna del Maule","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -70.50888061523438,\n              -36.15672664526234\n            ],\n            [\n              -70.49652099609375,\n              -36.18111652966561\n            ],\n            [\n              -70.46630859375,\n              -36.17224835899679\n            ],\n            [\n              -70.45120239257811,\n              -36.17335693522159\n            ],\n            [\n              -70.4388427734375,\n              -36.170031159499516\n            ],\n            [\n              -70.41824340820312,\n              -36.15118243124802\n            ],\n            [\n              -70.41961669921875,\n              -36.14341987311765\n            ],\n            [\n              -70.41275024414061,\n              -36.13565654678543\n            ],\n            [\n              -70.41549682617188,\n              -36.12567399853602\n            ],\n            [\n              -70.411376953125,\n              -36.110143066608224\n            ],\n            [\n              -70.42373657226562,\n              -36.09571873655536\n            ],\n            [\n              -70.4168701171875,\n              -36.08684090951099\n            ],\n            [\n              -70.4058837890625,\n              -36.05354012833974\n            ],\n            [\n              -70.38940429687499,\n              -36.05465038150425\n            ],\n            [\n              -70.36880493164062,\n              -36.04021586880111\n            ],\n            [\n              -70.37704467773438,\n              -36.02244668175845\n            ],\n            [\n              -70.38116455078124,\n              -36.00467348670187\n            ],\n            [\n              -70.37567138671875,\n              -35.99356320483023\n            ],\n            [\n              -70.38803100585938,\n              -35.98134008706755\n            ],\n            [\n              -70.40725708007812,\n              -35.98134008706755\n            ],\n            [\n              -70.41961669921875,\n              -35.97244935753682\n            ],\n            [\n              -70.41412353515625,\n              -35.96022296929668\n            ],\n            [\n              -70.38665771484375,\n              -35.936876426075145\n            ],\n            [\n              -70.60226440429688,\n              -35.94799468798151\n            ],\n            [\n              -70.67779541015624,\n              -36.052429859513424\n            ],\n            [\n              -70.57205200195312,\n              -36.12900165569651\n            ],\n            [\n              -70.50888061523438,\n              -36.15672664526234\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Hildreth, Wes","contributorId":15996,"corporation":false,"usgs":true,"family":"Hildreth","given":"Wes","email":"","affiliations":[],"preferred":false,"id":515440,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Godoy, Estanislao","contributorId":116368,"corporation":false,"usgs":true,"family":"Godoy","given":"Estanislao","email":"","affiliations":[],"preferred":false,"id":515442,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fierstein, Judy","contributorId":88337,"corporation":false,"usgs":true,"family":"Fierstein","given":"Judy","email":"","affiliations":[],"preferred":false,"id":515441,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Singer, Brad","contributorId":121387,"corporation":false,"usgs":true,"family":"Singer","given":"Brad","affiliations":[],"preferred":false,"id":515443,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70042162,"text":"70042162 - 2009 - National Wildlife Health Center's quarterly wildlife mortality report","interactions":[],"lastModifiedDate":"2023-10-13T16:58:57.057395","indexId":"70042162","displayToPublicDate":"2012-01-01T00:00:00","publicationYear":"2009","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3769,"text":"Wildlife Disease Association Newsletter","active":true,"publicationSubtype":{"id":10}},"title":"National Wildlife Health Center's quarterly wildlife mortality report","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Wildlife Disease Association","publisherLocation":"Lawrence, KS","usgsCitation":"Ballmann, A., Schuler, K., and Hoeh, J., 2009, National Wildlife Health Center's quarterly wildlife mortality report: Wildlife Disease Association Newsletter, no. April 2009, p. 8-14.","productDescription":"7 p.","startPage":"8","endPage":"14","ipdsId":"IP-013035","costCenters":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"links":[{"id":264853,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.wildlifedisease.org/PersonifyEbusiness/Resources/Publications/Newsletter/Archive","linkFileType":{"id":5,"text":"html"}},{"id":264854,"rank":2,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.er.usgs.gov/thumbnails/outside_thumb.jpg"}],"issue":"April 2009","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50e08cc5e4b0fec3206ee2a3","contributors":{"authors":[{"text":"Ballmann, Anne 0000-0002-0380-056X","orcid":"https://orcid.org/0000-0002-0380-056X","contributorId":104631,"corporation":false,"usgs":true,"family":"Ballmann","given":"Anne","affiliations":[],"preferred":false,"id":470874,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schuler, Krysten","contributorId":53735,"corporation":false,"usgs":true,"family":"Schuler","given":"Krysten","affiliations":[],"preferred":false,"id":470873,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hoeh, Julia","contributorId":8353,"corporation":false,"usgs":true,"family":"Hoeh","given":"Julia","affiliations":[],"preferred":false,"id":470872,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70041525,"text":"70041525 - 2009 - Geophysical setting of western Utah and eastern Nevada between latitudes 37°45′ and 40°N","interactions":[],"lastModifiedDate":"2012-12-14T11:20:13","indexId":"70041525","displayToPublicDate":"2012-01-01T00:00:00","publicationYear":"2009","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Geophysical setting of western Utah and eastern Nevada between latitudes 37°45′ and 40°N","docAbstract":"Gravity and aeromagnetic data refine the structural setting for the region of western Utah and eastern Nevada between Snake and Hamlin Valleys on the west and Tule Valley on the east. These data are used here as part of a regional analysis. An isostatic gravity map shows large areas underlain by gravity lows, the most prominent of which is a large semi-circular low associated with the Indian Peak caldera complex in the southwestern part of the study area. Another low underlies the Thomas caldera in the northeast, and linear lows elsewhere indicate low-density basin-fill in all major north-trending graben valleys. Gravity highs reflect pre-Cenozoic rocks mostly exposed in the mountain ranges. In the Confusion Range, however, the gravity high extends about 15 km east of the range front to Coyote Knolls, indicating a broad pediment cut on upper Paleozoic rocks and covered by a thin veneer of alluvium. Aeromagnetic highs sharply delineate Oligocene and Miocene volcanic rocks and intracaldera plutons associated with the Indian Peak caldera complex and the Pioche–Marysvale igneous belt. Jurassic to Eocene plutons and volcanic rocks elsewhere in the study area, however, have much more modest magnetic signatures. Some relatively small magnetic highs in the region are associated with outcrops of volcanic rock, and the continuation of those anomalies indicates that the rocks are probably extensive in the subsurface. A gravity inversion method separating the isostatic gravity anomaly into fields representing pre-Cenozoic basement rocks and Cenozoic basin deposits was used to calculate depth to basement and estimate maximum amounts of alluvial and volcanic fill within the valleys. Maximum depths within the Indian Peak caldera complex average about 2.5 km, locally reaching 3 km. North of the caldera complex, thickness of valley fill in most graben valleys ranges from 1.5 to 3 km thick, with Hamlin and Pine Valleys averaging ~3 km. The main basin beneath Tule Valley is relatively shallow (~0.6 km), reaching a maximum depth of ~1 km over a small area northeast of Coyote Knolls. Maximum horizontal gradients were calculated for both long-wavelength gravity and magnetic-potential data, and these were used to constrain major density and magnetic lineaments. These lineaments help delineate deep-seated crustal structures that separate major tectonic domains, potentially localizing Cenozoic tectonic features that may control regional ground-water flow.","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Geology and Geologic Resources and Issues of Western Utah, UGA-38","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","publisher":"Utah Geological Association","publisherLocation":"http://www.utahgeology.org","collaboration":"This book is available in CD-ROM format at <a href=\"http://www.mapstore.utah.gov/uga38.html/\" target=\"_blank\">http://www.mapstore.utah.gov/uga38.html/</a>","usgsCitation":"Mankinen, E.A., and McKee, E.H., 2009, Geophysical setting of western Utah and eastern Nevada between latitudes 37°45′ and 40°N, chap. <i>of</i> Geology and Geologic Resources and Issues of Western Utah, UGA-38, p. 271-286.","productDescription":"16 p.; CD-ROM Chapter","startPage":"271","endPage":"286","ipdsId":"IP-012963","costCenters":[{"id":309,"text":"Geology and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":264041,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":264040,"type":{"id":15,"text":"Index Page"},"url":"https://archives.datapages.com/data/uga/data/081/081001/271_ugs810271.htm"}],"country":"United States","state":"Nevada;Utah","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -120.01,40.0 ], [ -120.01,37.75 ], [ -109.04,37.75 ], [ -109.04,40.0 ], [ -120.01,40.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50cc58d2e4b00ab7c548c697","contributors":{"editors":[{"text":"Tripp, Bryce","contributorId":113835,"corporation":false,"usgs":true,"family":"Tripp","given":"Bryce","email":"","affiliations":[],"preferred":false,"id":509108,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Krahulec, Ken","contributorId":113293,"corporation":false,"usgs":true,"family":"Krahulec","given":"Ken","email":"","affiliations":[],"preferred":false,"id":509107,"contributorType":{"id":2,"text":"Editors"},"rank":2},{"text":"Jordan, Lucy","contributorId":111392,"corporation":false,"usgs":true,"family":"Jordan","given":"Lucy","email":"","affiliations":[],"preferred":false,"id":509106,"contributorType":{"id":2,"text":"Editors"},"rank":3}],"authors":[{"text":"Mankinen, Edward A. 0000-0001-7496-2681 emank@usgs.gov","orcid":"https://orcid.org/0000-0001-7496-2681","contributorId":1054,"corporation":false,"usgs":true,"family":"Mankinen","given":"Edward","email":"emank@usgs.gov","middleInitial":"A.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":469901,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McKee, Edwin H. mckee@usgs.gov","contributorId":3728,"corporation":false,"usgs":true,"family":"McKee","given":"Edwin","email":"mckee@usgs.gov","middleInitial":"H.","affiliations":[],"preferred":true,"id":469902,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70043081,"text":"pp17138 - 2009 - Petroleum systems used to determine the assessment units in the San Joaquin Basin Province, California","interactions":[{"subject":{"id":70043081,"text":"pp17138 - 2009 - Petroleum systems used to determine the assessment units in the San Joaquin Basin Province, California","indexId":"pp17138","publicationYear":"2009","noYear":false,"title":"Petroleum systems used to determine the assessment units in the San Joaquin Basin Province, California"},"predicate":"IS_PART_OF","object":{"id":80526,"text":"pp1713 - 2007 - Petroleum Systems and Geologic Assessment of Oil and Gas in the San Joaquin Basin Province, California","indexId":"pp1713","publicationYear":"2007","noYear":false,"title":"Petroleum Systems and Geologic Assessment of Oil and Gas in the San Joaquin Basin Province, California"},"id":1}],"isPartOf":{"id":80526,"text":"pp1713 - 2007 - Petroleum Systems and Geologic Assessment of Oil and Gas in the San Joaquin Basin Province, California","indexId":"pp1713","publicationYear":"2007","noYear":false,"title":"Petroleum Systems and Geologic Assessment of Oil and Gas in the San Joaquin Basin Province, California"},"lastModifiedDate":"2022-06-07T18:33:27.713194","indexId":"pp17138","displayToPublicDate":"2012-01-01T00:00:00","publicationYear":"2009","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1713-8","title":"Petroleum systems used to determine the assessment units in the San Joaquin Basin Province, California","docAbstract":"For the San Joaquin Basin Province in California (fig. 8.1), six petroleum systems were identified, mapped, and described to provide the basis for the five total petroleum systems (TPS) and ten related assessment units (AU) used in the 2003 U.S. Geological Survey (USGS) National Oil and Gas Assessment (table 8.1; Gautier and others, 2004; Hosford Scheirer, 2007). The petroleum pools in the province were allocated to each petroleum system on the basis of (1) geochemical composition as described by Lillis and Magoon (this volume, chapter 9) and Lillis and others (this volume, chapter 10), (2) reservoir rock nomenclature (fig 8.2; appendix 8.1 and appendix 8.2) as described by Hosford Scheirer and Magoon (this volume, chapter 5), and (3) the volume of oil and gas discovered for each petroleum system by system, flank, and trap type (tables 8.2, 8.3 and 8.4). For this assessment, each petroleum system was determined, followed by the TPS from one or more petroleum systems. For example, the Miocene TPS includes two petroleum systems, the McLure-Tulare(!) and Antelope-Stevens(!) (notation described in Petroleum System Name section, below). Magoon and Schmoker (2000) describe how the TPS is used in this and the USGS world assessments. This chapter describes the six petroleum systems used to make five total petroleum systems in this San Joaquin Basin Province assessment.\nThe figures and tables for each petroleum system and TPS are as follows: (1) the San Joaquin(?) petroleum system or the Neogene Nonassociated Gas TPS is a natural gas system in the southeast part of the province (figs. 8.3 through 8.8; table 8.5; this volume, chapter 22); (2) the Miocene TPS (this volume, chapters 13, 14, 15, 16, and 17) includes the McLure-Tulare(!) petroleum system north of the Bakersfield Arch (figs. 8.9 through 8.13; table 8.6), and the Antelope-Stevens(!) petroleum system south of the arch (figs. 8.14 through 8.18; table 8.7), and is summarized in figure 8.19; (3) the Eocene TPS (this volume, chapters 18 and 19) combines two petroleum systems, the Tumey-Temblor(.) covering much of the province (figs. 8.20 through 8.24; table 8.8) and the underlying Kreyenhagen-Temblor(!) (figs. 8.25 through 8.29: table 8.9), and is summarized in figure 8.30; (4) the Eocene-Miocene Composite TPS, formed by combining the Miocene and Eocene TPS (this volume, chapter 20); and (5) the Moreno-Nortonville(.) is both a petroleum system and a TPS consisting mainly of natural gas in the northern part of the province (figs. 8.31 through 8.36: table 8.10; this volume, chapter 21). Oil samples with geochemistry from surface seeps and wells used to map these petroleum systems are listed in table 8.11. Finally, the volume of oil and gas expelled by each pod of active source rock was calculated and compared with the discovered hydrocarbons in each petroleum system (figs. 8.37 through 8.39; tables 8.12 and 8.13).","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Petroleum systems and geologic assessment of oil and gas in the San Joaquin Basin Province, California (Professional Paper 1713)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/pp17138","usgsCitation":"Magoon, L.B., Lillis, P.G., and Peters, K., 2009, Petroleum systems used to determine the assessment units in the San Joaquin Basin Province, California: U.S. Geological Survey Professional Paper 1713-8, 65 p., https://doi.org/10.3133/pp17138.","productDescription":"65 p.","additionalOnlineFiles":"Y","costCenters":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true},{"id":255,"text":"Energy Resources Program","active":true,"usgs":true}],"links":[{"id":266951,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/pp_1713_8.jpg"},{"id":401863,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_87072.htm"},{"id":266950,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/pp1713/08/pp1713_ch08.pdf"},{"id":266949,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/pp/pp1713/"}],"country":"United States","state":"California","otherGeospatial":"San Joaquin Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -121.4,\n              34.9\n            ],\n            [\n              -118.625,\n              34.9\n            ],\n            [\n              -118.625,\n              37.8167\n            ],\n            [\n              -121.4,\n              37.8167\n            ],\n            [\n              -121.4,\n              34.9\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","publicComments":"This report is Chapter 8 in <i>Petroleum systems and geologic assessment of oil and gas in the San Joaquin Basin Province, California</i>.  Please see <a href=\"http://pubs.er.usgs.gov/publication/pp1713\" target=\"_blank\">Professional Paper 1713</a> for other chapters.","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5110e6a2e4b0361176563965","contributors":{"authors":[{"text":"Magoon, Leslie B. lmagoon@usgs.gov","contributorId":2383,"corporation":false,"usgs":true,"family":"Magoon","given":"Leslie","email":"lmagoon@usgs.gov","middleInitial":"B.","affiliations":[],"preferred":true,"id":472924,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lillis, Paul G. 0000-0002-7508-1699 plillis@usgs.gov","orcid":"https://orcid.org/0000-0002-7508-1699","contributorId":1817,"corporation":false,"usgs":true,"family":"Lillis","given":"Paul","email":"plillis@usgs.gov","middleInitial":"G.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":472923,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Peters, Kenneth E.","contributorId":10897,"corporation":false,"usgs":true,"family":"Peters","given":"Kenneth E.","affiliations":[],"preferred":false,"id":472925,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70041337,"text":"70041337 - 2009 - Simulations of cataclysmic outburst floods from Pleistocene Glacial Lake Missoula","interactions":[],"lastModifiedDate":"2013-03-30T07:51:52","indexId":"70041337","displayToPublicDate":"2012-01-01T00:00:00","publicationYear":"2009","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1786,"text":"Geological Society of America Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Simulations of cataclysmic outburst floods from Pleistocene Glacial Lake Missoula","docAbstract":"Using a flow domain that we constructed from 30 m digital-elevation model data of western United States and Canada and a two-dimensional numerical model for shallow-water flow over rugged terrain, we simulated outburst floods from Pleistocene Glacial Lake Missoula. We modeled a large, but not the largest, flood, using initial lake elevation at 1250 m instead of 1285 m. Rupture of the ice dam, centered on modern Lake Pend Oreille, catastrophically floods eastern Washington and rapidly fills the broad Pasco, Yakima, and Umatilla Basins. Maximum flood stage is reached in Pasco and Yakima Basins 38 h after the dam break, whereas maximum flood stage in Umatilla Basin occurs 17 h later. Drainage of these basins through narrow Columbia gorge takes an additional 445 h. For this modeled flood, peak discharges in eastern Washington range from 10 to 20 × 10<sup>6</sup> m<sup>3</sup>/s. However, constrictions in Columbia gorge limit peak discharges to <6 × 10<sup>6</sup> m<sup>3</sup>/s and greatly extend the duration of flooding. We compare these model results with field observations of scabland distribution and high-water indicators. Our model predictions of the locations of maximum scour (product of bed shear stress and average flow velocity) match the distribution of existing scablands. We compare model peak stages to high-water indicators from the Rathdrum-Spokane valley, Walulla Gap, and along Columbia gorge. Though peak stages from this less-than-maximal flood model attain or exceed peak-stage indicators along Rathdrum-Spokane valley and along Columbia gorge, simulated peak stages near Walulla Gap are 10–40 m below observed peak-stage indicators. Despite this discrepancy, our match to field observations in most of the region indicates that additional sources of water other than Glacial Lake Missoula are not required to explain the Missoula floods.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Geological Society of America Bulletin","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"The Geological Society of America","publisherLocation":"Boulder, CO","doi":"10.1130/B26454.1","usgsCitation":"Denlinger, R.P., and O’Connell, D.R., 2009, Simulations of cataclysmic outburst floods from Pleistocene Glacial Lake Missoula: Geological Society of America Bulletin, v. 122, no. 5-6, p. 678-689, https://doi.org/10.1130/B26454.1.","productDescription":"12 p.","startPage":"678","endPage":"689","ipdsId":"IP-007425","costCenters":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"links":[{"id":263715,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":263714,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1130/B26454.1"}],"country":"United States","state":"Montana","city":"Missoula","otherGeospatial":"Pasco Basin;Pleistocene Glacial Lake Missoula;Umatilla Basin;Walulla Gap;Yakima Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -116.0,44.1 ], [ -116.0,49.0 ], [ -108.0,49.0 ], [ -108.0,44.1 ], [ -116.0,44.1 ] ] ] } } ] }","volume":"122","issue":"5-6","noUsgsAuthors":false,"publicationDate":"2009-12-30","publicationStatus":"PW","scienceBaseUri":"50bfbdcee4b01744973f782f","contributors":{"authors":[{"text":"Denlinger, Roger P. 0000-0003-0930-0635 roger@usgs.gov","orcid":"https://orcid.org/0000-0003-0930-0635","contributorId":2679,"corporation":false,"usgs":true,"family":"Denlinger","given":"Roger","email":"roger@usgs.gov","middleInitial":"P.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true},{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true}],"preferred":true,"id":469553,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"O’Connell, D. R. H.","contributorId":53606,"corporation":false,"usgs":true,"family":"O’Connell","given":"D.","email":"","middleInitial":"R. H.","affiliations":[],"preferred":false,"id":469554,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70003358,"text":"70003358 - 2009 - The Portland Basin: A (big) river runs through it","interactions":[],"lastModifiedDate":"2018-03-15T10:47:16","indexId":"70003358","displayToPublicDate":"2011-12-25T15:02:00","publicationYear":"2009","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1728,"text":"GSA Today","active":true,"publicationSubtype":{"id":10}},"title":"The Portland Basin: A (big) river runs through it","docAbstract":"Metropolitan Portland, Oregon, USA, lies within a small Neogene to Holocene basin in the forearc of the Cascadia subduction system. Although the basin owes its existence and structural development to its convergent-margin tectonic setting, the stratigraphic architecture of basin-fill deposits chiefly reflects its physiographic position along the lower reaches of the continental-scale Columbia River system. As a result of this globally unique setting, the basin preserves a complex record of aggradation and incision in response to distant as well as local tectonic, volcanic, and climatic events. Voluminous flood basalts, continental and locally derived sediment and volcanic debris, and catastrophic flood deposits all accumulated in an area influenced by contemporaneous tectonic deformation and variations in regional and local base level.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"GSA Today","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"The Geological Society of America","publisherLocation":"Boulder, CO","usgsCitation":"Evarts, R.C., O'Connor, J., Wells, R., and Madin, I.P., 2009, The Portland Basin: A (big) river runs through it: GSA Today, v. 19, no. 9, p. 4-10.","productDescription":"7 p.","startPage":"4","endPage":"10","costCenters":[{"id":309,"text":"Geology and Geophysics Science Center","active":true,"usgs":true},{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":204291,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":112418,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://www.geosociety.org/gsatoday/archive/19/9/pdf/i1052-5173-19-9-4.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Oregon","city":"Portland","volume":"19","issue":"9","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505ba894e4b08c986b321d06","contributors":{"authors":[{"text":"Evarts, Russell C. revarts@usgs.gov","contributorId":1974,"corporation":false,"usgs":true,"family":"Evarts","given":"Russell","email":"revarts@usgs.gov","middleInitial":"C.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":347005,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"O'Connor, Jim E. 0000-0002-7928-5883 oconnor@usgs.gov","orcid":"https://orcid.org/0000-0002-7928-5883","contributorId":140771,"corporation":false,"usgs":true,"family":"O'Connor","given":"Jim E.","email":"oconnor@usgs.gov","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true},{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"preferred":false,"id":347007,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wells, Ray E. 0000-0002-7796-0160 rwells@usgs.gov","orcid":"https://orcid.org/0000-0002-7796-0160","contributorId":2692,"corporation":false,"usgs":true,"family":"Wells","given":"Ray E.","email":"rwells@usgs.gov","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":false,"id":347006,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Madin, Ian P.","contributorId":66404,"corporation":false,"usgs":true,"family":"Madin","given":"Ian","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":347008,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70003510,"text":"70003510 - 2009 - Eruption of Alaska volcano breaks historic pattern","interactions":[],"lastModifiedDate":"2019-04-16T11:10:51","indexId":"70003510","displayToPublicDate":"2011-12-22T00:00:00","publicationYear":"2009","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Eruption of Alaska volcano breaks historic pattern","docAbstract":"In the late morning of 12 July 2008, the Alaska Volcano Observatory (AVO) received an unexpected call from the U.S. Coast Guard, reporting an explosive volcanic eruption in the central Aleutians in the vicinity of Okmok volcano, a relatively young (~2000-year-old) caldera. The Coast Guard had received an emergency call requesting assistance from a family living at a cattle ranch on the flanks of the volcano, who reported loud \"thunder,\" lightning, and noontime darkness due to ashfall. AVO staff immediately confirmed the report by observing a strong eruption signal recorded on the Okmok seismic network and the presence of a large dark ash cloud above Okmok in satellite imagery. Within 5 minutes of the call, AVO declared the volcano at aviation code red, signifying that a highly explosive, ash-rich eruption was under way.","language":"English","publisher":"American Geophysical Union","doi":"10.1029/2009EO200001","usgsCitation":"Larsen, J., Neal, C.A., Webley, P., Freymueller, J., Haney, M., McNutt, S., Schneider, D., Prejean, S., Schaefer, J., and Wessels, R.L., 2009, Eruption of Alaska volcano breaks historic pattern: Eos, Transactions, American Geophysical Union, v. 90, no. 20, p. 173-174, https://doi.org/10.1029/2009EO200001.","productDescription":"2 p.","startPage":"173","endPage":"174","numberOfPages":"2","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true},{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"links":[{"id":475987,"rank":301,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1029/2009eo200001","text":"Publisher Index Page"},{"id":204220,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":269263,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1029/2009EO200001"},{"id":112407,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://smtp.subduction.net/Storage%20for%20Journal%20Articles/Alaska%20Volcano%20Breaks%20Pattern,%20EOS,%20May%202009.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Alaska","otherGeospatial":"Okmok Volcano","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -168.563232421875,\n              53.28163740806336\n            ],\n            [\n              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tneal@usgs.gov","orcid":"https://orcid.org/0000-0002-7697-7825","contributorId":639,"corporation":false,"usgs":true,"family":"Neal","given":"Christina","email":"tneal@usgs.gov","middleInitial":"A.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":false,"id":347579,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Webley, Peter","contributorId":34783,"corporation":false,"usgs":true,"family":"Webley","given":"Peter","affiliations":[],"preferred":false,"id":347582,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Freymueller, Jeff","contributorId":82190,"corporation":false,"usgs":true,"family":"Freymueller","given":"Jeff","affiliations":[],"preferred":false,"id":347587,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Haney, Matthew","contributorId":80555,"corporation":false,"usgs":true,"family":"Haney","given":"Matthew","affiliations":[],"preferred":false,"id":347586,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"McNutt, Stephen","contributorId":26196,"corporation":false,"usgs":true,"family":"McNutt","given":"Stephen","affiliations":[],"preferred":false,"id":347581,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Schneider, David","contributorId":78204,"corporation":false,"usgs":true,"family":"Schneider","given":"David","affiliations":[],"preferred":false,"id":347585,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Prejean, Stephanie","contributorId":61916,"corporation":false,"usgs":true,"family":"Prejean","given":"Stephanie","affiliations":[],"preferred":false,"id":347583,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Schaefer, Janet","contributorId":8131,"corporation":false,"usgs":true,"family":"Schaefer","given":"Janet","affiliations":[],"preferred":false,"id":347580,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Wessels, Rick L. rwessels@usgs.gov","contributorId":566,"corporation":false,"usgs":true,"family":"Wessels","given":"Rick","email":"rwessels@usgs.gov","middleInitial":"L.","affiliations":[{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":false,"id":347578,"contributorType":{"id":1,"text":"Authors"},"rank":10}]}}
,{"id":70003838,"text":"70003838 - 2009 - Temporal and maternal effects on reproductive ecology of the giant gartersnake (<i>Thamnophis gigas</i>)","interactions":[],"lastModifiedDate":"2017-09-06T09:50:09","indexId":"70003838","displayToPublicDate":"2011-12-18T15:07:00","publicationYear":"2009","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3451,"text":"Southwestern Naturalist","active":true,"publicationSubtype":{"id":10}},"title":"Temporal and maternal effects on reproductive ecology of the giant gartersnake (<i>Thamnophis gigas</i>)","docAbstract":"We used mixed-effects models to examine relationships of reproductive characteristics of the giant gartersnake (<i>Thamnophis gigas</i>) to improve population modeling and conservation planning for this species. Neonates from larger litters had lower mass, and mass of neonates also was affected by random variation among mothers. Length of mother did not affect relative mass of litters; however, our data suggest that longer mothers expended less reproductive effort per offspring than shorter mothers. We detected random variation in length of neonates among mothers, but these lengths were not related to length of mother or size of litter. Mean size of litter varied among years, but little evidence existed for a relationship between size of litter or mass of litter and length of mother. Sex ratios of neonates did not differ from 1:1.","language":"English","publisher":"Southwestern Association of Naturalists","doi":"10.1894/GC-205.1","usgsCitation":"Halstead, B., Wylie, G.D., Casazza, M.L., and Coates, P.S., 2009, Temporal and maternal effects on reproductive ecology of the giant gartersnake (<i>Thamnophis gigas</i>): Southwestern Naturalist, v. 56, no. 1, p. 29-34, https://doi.org/10.1894/GC-205.1.","productDescription":"6 p.","startPage":"29","endPage":"34","ipdsId":"IP-012262","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":204426,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"56","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505ba4eae4b08c986b320681","contributors":{"authors":[{"text":"Halstead, Brian J. 0000-0002-5535-6528 bhalstead@usgs.gov","orcid":"https://orcid.org/0000-0002-5535-6528","contributorId":3051,"corporation":false,"usgs":true,"family":"Halstead","given":"Brian J.","email":"bhalstead@usgs.gov","affiliations":[{"id":200,"text":"Coop Res Unit Seattle","active":true,"usgs":true},{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":true,"id":349117,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wylie, Glenn D. 0000-0002-7061-6658 glenn_wylie@usgs.gov","orcid":"https://orcid.org/0000-0002-7061-6658","contributorId":3052,"corporation":false,"usgs":true,"family":"Wylie","given":"Glenn","email":"glenn_wylie@usgs.gov","middleInitial":"D.","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":true,"id":349118,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Casazza, Michael L. 0000-0002-5636-735X mike_casazza@usgs.gov","orcid":"https://orcid.org/0000-0002-5636-735X","contributorId":2091,"corporation":false,"usgs":true,"family":"Casazza","given":"Michael","email":"mike_casazza@usgs.gov","middleInitial":"L.","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":true,"id":349116,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Coates, Peter S. 0000-0003-2672-9994 pcoates@usgs.gov","orcid":"https://orcid.org/0000-0003-2672-9994","contributorId":3263,"corporation":false,"usgs":true,"family":"Coates","given":"Peter","email":"pcoates@usgs.gov","middleInitial":"S.","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":true,"id":349119,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70003457,"text":"70003457 - 2009 - Stratigraphy and conodont biostratigraphy of the uppermost Carboniferous and Lower Permian from the North American Midcontinent","interactions":[],"lastModifiedDate":"2012-02-02T00:16:01","indexId":"70003457","displayToPublicDate":"2011-12-06T16:05:00","publicationYear":"2009","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2579,"text":"Kansas Geological Survey Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Stratigraphy and conodont biostratigraphy of the uppermost Carboniferous and Lower Permian from the North American Midcontinent","docAbstract":"<p><b>Part A</b> The uppermost Wabaunsee, Admire, Council Grove, and lower Chase Groups of Kansas, Oklahoma, and Nebraska are placed into three third-order depositional sequences: a Gzhelian late-highstand sequence set, a Council Grove transgressive and highstand sequence set, and a Chase transgressive sequence set. Sequences are defined by bounding maximum-exposure surfaces and are placed within the zone of exposure surfaces (typically, stacked paleosols). Conodonts are abundant in open-marine deposits and most marine units have a differing and characteristic faunal make-up. Eleven species are described as new: <i>Streptognathodus binodosus</i>, <i>S. denticulatus</i>, <i>S. elongianus</i>, <i>S. florensis</i>, <i>S. lineatus</i>, <i>S. nevaensis</i>, <i>S. postconstrictus</i>, <i>S. postelongatus</i>, <i>S. robustus</i>, <i>S. translinearis</i>, and <i>S. trimilus</i>.</p> <p><b>Part B</b> Maximum-marine flooding levels and marine-condensed sections from uppermost Carboniferous and Lower Permian fourth-order (0.1-1 m.y.) depositional sequences of the North American midcontinent reveal a rich stratigraphic succession of species of <i>Streptognathodus</i> and <i>Sweetognathus conodonts</i> that permits high-precision correlation of the Carboniferous-Permian boundary as well as the Asselian-Sakmarian and Sakmarian-Artinskian boundaries. Eleven new species of <i>Streptognathodus</i> are described: <i>Streptognathodus binodosus</i>, <i>S. denticulatus</i>, <i>S. elongianus</i>, <i>S. florensis</i>, <i>S. lineatus</i>, <i>S. nevaensis</i>, <i>S. postconstrictus</i>, <i>S. postelongatus</i>, <i>S. robustus</i>, <i>S. translinearis</i>, and <i>S. trimilus</i>. Seventeen species are redescribed and clarified and include <i>Streptognathodus alius</i>, <i>S. barskovi</i>, <i>S. bellus</i>, <i>S. brownvillensis</i>, <i>S. conjunctus</i>, <i>S. constrictus</i>, <i>S. elongatus</i>, <i>S. farmeri</i>, <i>S. flexuosus</i>, <i>S. fuchengensis</i>, <i>S. fusus</i>, <i>S. invaginatus</i>, <i>S. isolatus</i>, <i>S. longissimus</i>, <i>S. minacutus</i>, <i>S. nodulinearis</i>, and <i>S. wabaunsensis</i>.</p> <p>The correlated level of the Carboniferous-Permian boundary is recognized in the lower part of the Red Eagle Depositional Sequence based on the introduction of <i>Streptognathodus isolatus</i> Chernykh, Ritter, and Wardlaw; <i>Streptognathodus minacutus</i> Barskov and Reimers; <i>Streptognathodus invaginatus</i> Reshetkova and Chernykh; <i>Streptognathodus fuchengensis</i> Zhao; and <i>Streptognathodus nodulinearis</i> Reshetkova and Chernykh. The correlated Carboniferous-Permian boundary occurs in the depositional sequence that represents the maximum-marine highstand of the Council Grove Composite Third Order Sequence. This level represents a significant marine-flooding event that should be correlatable in numerous shelfal sections throughout the world.</p> <p>Although the Asselian-Sakmarian boundary has not been rigorously defined, <i>Sweetognathus merrilli</i> has been informally utilized as a Sakmarian indicator. Due to the ecologically controlled distribution of species of <i>Sweetognathus</i>, we prefer to use a species of <i>Streptognathodus</i> as a defining species. We propose that <i>Streptognathodus barskovi</i> (Kozur) Reshetkova be considered as a potentially defining or ancillary defining species for the Sakmarian Stage. In the North American midcontinent, <i>Streptognathodus barskovi</i> appears in the same depositional sequence with <i>Sweetognathus merrilli</i> in the Eiss (Lower Bader) Depositional Sequence. Historically, <i>Sweetognathus whitei</i> has been used to mark the Sakmarian-Artinskian boundary. In our succession <i>Sweetognathus whitei</i> and <i>Streptognathodus florensis</i> appear in the basal part of the Barneston Depositional Sequence. We suggest that <i>Streptognathodus florensis</i> be further investigated as a possible defining or ancillary defining taxon for the base of the Artinskian Stage. This depositional sequence also forms the maximum-marine highstand of the Chase Third-Order Composite Depositional Sequence suggesting that this level is a significant marine-flooding event that should be widely traceable in numerous shelfal sections.</p>","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Kansas Geological Survey Bulletin","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"The University of Kansas","publisherLocation":"Lawrence, KS","usgsCitation":"Boardman, D.R., Wardlaw, B.R., and Nestell, M.K., 2009, Stratigraphy and conodont biostratigraphy of the uppermost Carboniferous and Lower Permian from the North American Midcontinent: Kansas Geological Survey Bulletin, v. 255, x, 145 p.; Appendices.","productDescription":"x, 145 p.; Appendices","costCenters":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"links":[{"id":204483,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":111144,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://www.kgs.ku.edu/Publications/Bulletins/255/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Kansas;Nebraska;Oklahoma","volume":"255","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b9981e4b08c986b31c46f","contributors":{"authors":[{"text":"Boardman, Darwin R. II","contributorId":41295,"corporation":false,"usgs":true,"family":"Boardman","given":"Darwin","suffix":"II","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":347346,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wardlaw, Bruce R. bwardlaw@usgs.gov","contributorId":266,"corporation":false,"usgs":true,"family":"Wardlaw","given":"Bruce","email":"bwardlaw@usgs.gov","middleInitial":"R.","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"preferred":true,"id":347345,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Nestell, Merlynd K.","contributorId":68603,"corporation":false,"usgs":false,"family":"Nestell","given":"Merlynd","email":"","middleInitial":"K.","affiliations":[{"id":12734,"text":"University of Texas at Arlington","active":true,"usgs":false}],"preferred":false,"id":347347,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70003927,"text":"70003927 - 2009 - Spring migration routes and chronology of surf scoters (Melanitta perspicillata): A synthesis of Pacific coast studies","interactions":[],"lastModifiedDate":"2018-08-21T15:41:33","indexId":"70003927","displayToPublicDate":"2011-12-06T12:29:00","publicationYear":"2009","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1176,"text":"Canadian Journal of Zoology","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Spring migration routes and chronology of surf scoters (<i>Melanitta perspicillata</i>): A synthesis of Pacific coast studies","title":"Spring migration routes and chronology of surf scoters (Melanitta perspicillata): A synthesis of Pacific coast studies","docAbstract":"Understanding interconnectivity among wintering, stopover, and breeding areas of migratory birds is pivotal to discerning how events occurring in each might have a cross-seasonal effect on another. Such information can guide the location and timing of conservation efforts. Thus, we examined spring migration routes, chronology, and stopover use of 85 surf scoters (<i>Melanitta perspicillata</i> (L., 1758)) marked with satellite transmitters at four Pacific Flyway wintering sites: San Quintin Bay, Baja California; San Francisco Bay, California; Puget Sound, Washington; and Strait of Georgia, British Columbia. Eighty-three percent of marked scoters followed two main routes to the breeding area: a Southern Inland route involving staging in Puget Sound and Strait of Georgia and protracted inland migration, or a Northern Coastal route characterized by short movements along the Pacific coast of British Columbia and southeast Alaska with inland migration initiating from Lynn Canal and surrounding areas. Route choice was related to nesting site latitude in the Canadian Northern Boreal Forest. Data from birds tracked over 2 years indicated strong migration route fidelity, but altered chronology and stopover locations between years. Departure date varied by wintering site, but arrival and apparent settling dates were synchronous, suggesting individuals adjusted migration timing to meet an optimized reproductive schedule.","language":"English","publisher":"Canadian Science Publishing","publisherLocation":"Ottawa, Ontario","doi":"10.1139/Z09-099","usgsCitation":"De La Cruz, S.E., Takekawa, J.Y., Wilson, M.T., Nysewander, D., Evenson, J., Esler, D., Boyd, W.S., and Ward, D.H., 2009, Spring migration routes and chronology of surf scoters (Melanitta perspicillata): A synthesis of Pacific coast studies: Canadian Journal of Zoology, v. 87, no. 11, p. 1069-1086, https://doi.org/10.1139/Z09-099.","productDescription":"18 p.","startPage":"1069","endPage":"1086","numberOfPages":"18","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":486669,"rank":1,"type":{"id":30,"text":"Data Release"},"url":"https://doi.org/10.5066/P9LUFGEF","text":"USGS data release","linkHelpText":"Tracking Data for Surf Scoters (Melanitta perspicillata)"},{"id":204209,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Canada, United States","state":"British Columbia, California, Washington","volume":"87","issue":"11","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b9620e4b08c986b31b2ea","contributors":{"authors":[{"text":"De La Cruz, Susan E.W. 0000-0001-6315-0864 sdelacruz@usgs.gov","orcid":"https://orcid.org/0000-0001-6315-0864","contributorId":3248,"corporation":false,"usgs":true,"family":"De La Cruz","given":"Susan","email":"sdelacruz@usgs.gov","middleInitial":"E.W.","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":true,"id":349548,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Takekawa, John Y. 0000-0003-0217-5907 john_takekawa@usgs.gov","orcid":"https://orcid.org/0000-0003-0217-5907","contributorId":176168,"corporation":false,"usgs":true,"family":"Takekawa","given":"John","email":"john_takekawa@usgs.gov","middleInitial":"Y.","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":false,"id":349546,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wilson, M. T.","contributorId":102116,"corporation":false,"usgs":true,"family":"Wilson","given":"M.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":349549,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Nysewander, D.R.","contributorId":90946,"corporation":false,"usgs":true,"family":"Nysewander","given":"D.R.","affiliations":[],"preferred":false,"id":349547,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Evenson, J.R.","contributorId":105927,"corporation":false,"usgs":true,"family":"Evenson","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":349550,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Esler, Daniel 0000-0001-5501-4555 desler@usgs.gov","orcid":"https://orcid.org/0000-0001-5501-4555","contributorId":5465,"corporation":false,"usgs":true,"family":"Esler","given":"Daniel","email":"desler@usgs.gov","affiliations":[{"id":12437,"text":"Simon Fraser University, Centre for Wildlife Ecology","active":true,"usgs":false},{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":116,"text":"Alaska Science Center Biology MFEB","active":true,"usgs":true}],"preferred":true,"id":349543,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Boyd, W. S.","contributorId":49051,"corporation":false,"usgs":true,"family":"Boyd","given":"W.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":349545,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Ward, David H. 0000-0002-5242-2526 dward@usgs.gov","orcid":"https://orcid.org/0000-0002-5242-2526","contributorId":3247,"corporation":false,"usgs":true,"family":"Ward","given":"David","email":"dward@usgs.gov","middleInitial":"H.","affiliations":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":117,"text":"Alaska Science Center Biology WTEB","active":true,"usgs":true}],"preferred":true,"id":349544,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":70003754,"text":"70003754 - 2009 - Structural development of high-temperature mylonites in the Archean Wyoming province, northwestern Madison Range, Montana","interactions":[],"lastModifiedDate":"2020-09-08T14:27:14.408808","indexId":"70003754","displayToPublicDate":"2011-12-06T00:00:00","publicationYear":"2009","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3310,"text":"Rocky Mountain Geology","active":true,"publicationSubtype":{"id":10}},"title":"Structural development of high-temperature mylonites in the Archean Wyoming province, northwestern Madison Range, Montana","docAbstract":"<p>The Crooked Creek mylonite, in the northwestern Madison Range, southwestern Montana, is defined by several curved lenses of high non-coaxial strain exposed over a 7-km-wide, northeast-trending strip. The country rocks, part of the Archean Wyoming province, are dominantly trondhjemitic to granitic orthogneiss with subordinate amphibolite, quartzite, aluminous gneiss, and sills of metabasite (mafic granulite). Data presented here support an interpretation that the mylonite formed during a period of rapid, heterogeneous strain at near-peak metamorphic conditions during an early deformational event (D<sub>1</sub>) caused by northwest–southeast-directed transpression. The mylonite has a well-developed L-S tectonite fabric and a fine-grained, recrystallized (granoblastic) texture. The strong linear fabric, interpreted as the stretching direction, is defined by elongate compositional “fish,” fold axes, aligned elongate minerals, and mullion axes. The margins of the mylonitic zones are concordant with and grade into regions of unmylonitized gneiss. A second deformational event (D<sub>2</sub>) has folded the mylonite surface to produce meter- to kilometer-scale, tight-to-isoclinal, gently plunging folds in both the mylonite and country rock, and represents a northwest–southeast shortening event. Planar or linear fabrics associated with D<sub>2</sub><span>&nbsp;</span>are remarkably absent. A third regional deformational event (D<sub>3</sub>) produced open, kilometer-scale folds generally with gently north-plunging fold axes.</p><p>Thermobarometric measurements presented here indicate that metamorphic conditions during D<sub>1</sub><span>&nbsp;</span>were the same in both the mylonite and the country gneiss, reaching upper amphibolite- to lower granulite-facies conditions: 700 ± 50° C and 8.5 ± 0.5 kb. Previous geochronological studies of mylonitic and cross-cutting rocks in the Jerome Rock Lake area, east of the Crooked Creek mylonite, bracket the timing of this high-grade metamorphism and mylonitization between 2.78 and 2.56 Ga, nearly a billion years before the 1.78-Ga Big Sky orogeny, which overprinted the basement rocks exposed in adjacent ranges of the Wyoming province.</p>","language":"English","publisher":"University of Wyoming","publisherLocation":"Laramie, WY","doi":"10.2113/gsrocky.44.2.85","usgsCitation":"Kellogg, K., and Mogk, D.W., 2009, Structural development of high-temperature mylonites in the Archean Wyoming province, northwestern Madison Range, Montana: Rocky Mountain Geology, v. 44, no. 2, p. 85-102, https://doi.org/10.2113/gsrocky.44.2.85.","productDescription":"18 p.","startPage":"85","endPage":"102","costCenters":[{"id":308,"text":"Geology and Environmental Change Science Center","active":false,"usgs":true}],"links":[{"id":204513,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Montana","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -112.06054687499999,\n              44.99588261816546\n            ],\n            [\n              -110.74218749999999,\n              44.99588261816546\n            ],\n            [\n              -110.74218749999999,\n              45.644768217751924\n            ],\n            [\n              -112.06054687499999,\n              45.644768217751924\n            ],\n            [\n              -112.06054687499999,\n              44.99588261816546\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"44","issue":"2","noUsgsAuthors":false,"publicationDate":"2009-11-24","publicationStatus":"PW","scienceBaseUri":"505b9be0e4b08c986b31d141","contributors":{"authors":[{"text":"Kellogg, Karl S.","contributorId":89896,"corporation":false,"usgs":true,"family":"Kellogg","given":"Karl S.","affiliations":[],"preferred":false,"id":348712,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mogk, David W.","contributorId":99687,"corporation":false,"usgs":true,"family":"Mogk","given":"David","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":348713,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70003352,"text":"70003352 - 2009 - Software for inference of dynamic ground strains and rotations and their errors from short baseline array observations of ground motions","interactions":[],"lastModifiedDate":"2023-10-17T00:52:28.713108","indexId":"70003352","displayToPublicDate":"2011-12-01T15:30:00","publicationYear":"2009","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1135,"text":"Bulletin of the Seismological Society of America","onlineIssn":"1943-3573","printIssn":"0037-1106","active":true,"publicationSubtype":{"id":10}},"title":"Software for inference of dynamic ground strains and rotations and their errors from short baseline array observations of ground motions","docAbstract":"In two previous articles we presented a formulation for inferring the strains and rotations of the ground beneath a seismic array having a finite footprint. In this article we derive expressions for the error covariance matrices of the inferred strains and rotations, and we present software for the calculation of ground strains, rotations, and their variances from short baseline array ground-motion data.","language":"English","publisher":"Seismological Society of America","doi":"10.1785/0120080230","usgsCitation":"Spudich, P., and Fletcher, J.B., 2009, Software for inference of dynamic ground strains and rotations and their errors from short baseline array observations of ground motions: Bulletin of the Seismological Society of America, v. 99, no. 2B, p. 1480-1482, https://doi.org/10.1785/0120080230.","productDescription":"3 p.","startPage":"1480","endPage":"1482","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"links":[{"id":204468,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.er.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"99","issue":"2B","noUsgsAuthors":false,"publicationDate":"2009-05-01","publicationStatus":"PW","scienceBaseUri":"505b91dae4b08c986b319b49","contributors":{"authors":[{"text":"Spudich, Paul","contributorId":54579,"corporation":false,"usgs":true,"family":"Spudich","given":"Paul","affiliations":[],"preferred":false,"id":346989,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fletcher, Jon B.","contributorId":65614,"corporation":false,"usgs":true,"family":"Fletcher","given":"Jon","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":346990,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70003641,"text":"70003641 - 2009 - Size and shape of Saturn's moon Titan","interactions":[],"lastModifiedDate":"2021-03-09T16:38:28.735592","indexId":"70003641","displayToPublicDate":"2011-12-01T15:09:00","publicationYear":"2009","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Size and shape of Saturn's moon Titan","docAbstract":"<p><span>Cassini observations show that Saturn’s moon Titan is slightly oblate. A fourth-order spherical harmonic expansion yields north polar, south polar, and mean equatorial radii of 2574.32 ± 0.05 kilometers (km), 2574.36 ± 0.03 km, and 2574.91 ± 0.11 km, respectively; its mean radius is 2574.73 ± 0.09 km. Titan’s shape approximates a hydrostatic, synchronously rotating triaxial ellipsoid but is best fit by such a body orbiting closer to Saturn than Titan presently does. Titan’s lack of high relief implies that most—but not all—of the surface features observed with the Cassini imaging subsystem and synthetic aperture radar are uncorrelated with topography and elevation. Titan’s depressed polar radii suggest that a constant geopotential hydrocarbon table could explain the confinement of the hydrocarbon lakes to high latitudes.</span></p>","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.1168905","usgsCitation":"Zebker, H.A., Stiles, B., Hensley, S., Lorenz, R., Kirk, R.L., and Lunine, J., 2009, Size and shape of Saturn's moon Titan: Science, v. 324, no. 5929, p. 921-923, https://doi.org/10.1126/science.1168905.","productDescription":"3 p.","startPage":"921","endPage":"923","costCenters":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"links":[{"id":204324,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":111020,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://www.sciencemag.org/content/324/5929/921.short","linkFileType":{"id":5,"text":"html"}}],"otherGeospatial":"Saturn's Moon Titan","volume":"324","issue":"5929","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b9115e4b08c986b31975c","contributors":{"authors":[{"text":"Zebker, Howard A.","contributorId":80401,"corporation":false,"usgs":true,"family":"Zebker","given":"Howard","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":348118,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stiles, Bryan","contributorId":37053,"corporation":false,"usgs":true,"family":"Stiles","given":"Bryan","affiliations":[],"preferred":false,"id":348116,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hensley, Scott","contributorId":85313,"corporation":false,"usgs":true,"family":"Hensley","given":"Scott","email":"","affiliations":[],"preferred":false,"id":348119,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lorenz, Ralph","contributorId":53933,"corporation":false,"usgs":true,"family":"Lorenz","given":"Ralph","affiliations":[],"preferred":false,"id":348117,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Kirk, Randolph L. 0000-0003-0842-9226 rkirk@usgs.gov","orcid":"https://orcid.org/0000-0003-0842-9226","contributorId":2765,"corporation":false,"usgs":true,"family":"Kirk","given":"Randolph","email":"rkirk@usgs.gov","middleInitial":"L.","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":true,"id":348114,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Lunine, Jonathan","contributorId":29560,"corporation":false,"usgs":true,"family":"Lunine","given":"Jonathan","email":"","affiliations":[],"preferred":false,"id":348115,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70009653,"text":"ofr20091256 - 2009 - Aeromagnetic survey of Howard Pass quadrangle and the East half of Misheguk Mountain quadrangle, Alaska&mdash;a Web site for the distribution of data","interactions":[],"lastModifiedDate":"2012-04-15T17:28:15","indexId":"ofr20091256","displayToPublicDate":"2011-12-01T12:56:39","publicationYear":"2009","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2009-1256","title":"Aeromagnetic survey of Howard Pass quadrangle and the East half of Misheguk Mountain quadrangle, Alaska&mdash;a Web site for the distribution of data","docAbstract":"U.S. Geological Survey Open-File-Report 2009-1256 is for the preliminary release of magnetic data (and associated contractor reports) for an airborne survey in the Brooks Range, northwest of Bettles, Alaska.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20091256","usgsCitation":"Brown, P., 2009, Aeromagnetic survey of Howard Pass quadrangle and the East half of Misheguk Mountain quadrangle, Alaska&mdash;a Web site for the distribution of data: U.S. Geological Survey Open-File Report 2009-1256, iii, 15 p.; Appendices; HTML View of Location Map; Downloads of Associated Files, https://doi.org/10.3133/ofr20091256.","productDescription":"iii, 15 p.; Appendices; HTML View of Location Map; Downloads of Associated Files","startPage":"i","endPage":"29","numberOfPages":"32","onlineOnly":"Y","additionalOnlineFiles":"Y","costCenters":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"links":[{"id":204836,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2009/1256/","linkFileType":{"id":5,"text":"html"}},{"id":204837,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr_2009_1256.gif"}],"country":"United States","state":"Alaska","otherGeospatial":"Howard Pass;Misheguk Mountain","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -161,68 ], [ -161,69 ], [ -156,69 ], [ -156,68 ], [ -161,68 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e8a9e4b0c8380cd47e19","contributors":{"authors":[{"text":"Brown, Philip J.","contributorId":70483,"corporation":false,"usgs":true,"family":"Brown","given":"Philip J.","affiliations":[],"preferred":false,"id":356812,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70003391,"text":"70003391 - 2009 - Modeling co-occurrence of northern spotted and barred owls: accounting for detection probability differences","interactions":[],"lastModifiedDate":"2012-02-02T00:16:01","indexId":"70003391","displayToPublicDate":"2011-12-01T12:52:56","publicationYear":"2009","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1015,"text":"Biological Conservation","active":true,"publicationSubtype":{"id":10}},"title":"Modeling co-occurrence of northern spotted and barred owls: accounting for detection probability differences","docAbstract":"Barred owls (Strix varia) have recently expanded their range and now encompass the entire range of the northern spotted owl (Strix occidentalis caurina). This expansion has led to two important issues of concern for management of northern spotted owls: (1) possible competitive interactions between the two species that could contribute to population declines of northern spotted owls, and (2) possible changes in vocalization behavior and detection probabilities of northern spotted owls induced by presence of barred owls. We used a two-species occupancy model to investigate whether there was evidence of competitive exclusion between the two species at study locations in Oregon, USA. We simultaneously estimated detection probabilities for both species and determined if the presence of one species influenced the detection of the other species. Model selection results and associated parameter estimates provided no evidence that barred owls excluded spotted owls from territories. We found strong evidence that detection probabilities differed for the two species, with higher probabilities for northern spotted owls that are the object of current surveys. Non-detection of barred owls is very common in surveys for northern spotted owls, and detection of both owl species was negatively influenced by the presence of the congeneric species. Our results suggest that analyses directed at hypotheses of barred owl effects on demographic or occupancy vital rates of northern spotted owls need to deal adequately with imperfect and variable detection probabilities for both species.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Biological Conservation","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","publisherLocation":"Amsterdam, Netherlands","doi":"10.1016/j.biocon.2009.07.028","usgsCitation":"Bailey, L., Reid, J.A., Forsman, E.D., and Nichols, J., 2009, Modeling co-occurrence of northern spotted and barred owls: accounting for detection probability differences: Biological Conservation, v. 142, no. 12, p. 2983-2989, https://doi.org/10.1016/j.biocon.2009.07.028.","productDescription":"7 p.","startPage":"2983","endPage":"2989","numberOfPages":"7","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":204476,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":21671,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.biocon.2009.07.028","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Oregon","volume":"142","issue":"12","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a5be8e4b0c8380cd6f8ba","contributors":{"authors":[{"text":"Bailey, Larissa L.","contributorId":93183,"corporation":false,"usgs":true,"family":"Bailey","given":"Larissa L.","affiliations":[],"preferred":false,"id":347100,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reid, Janice A.","contributorId":98034,"corporation":false,"usgs":true,"family":"Reid","given":"Janice","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":347102,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Forsman, Eric D.","contributorId":96792,"corporation":false,"usgs":false,"family":"Forsman","given":"Eric","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":347101,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Nichols, James D. 0000-0002-7631-2890 jnichols@usgs.gov","orcid":"https://orcid.org/0000-0002-7631-2890","contributorId":405,"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":347099,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70006102,"text":"fs20093043 - 2009 - Taste and odor occurrence in Lake William C. Bowen and Municipal Reservoir #1, Spartanburg County, South Carolina","interactions":[],"lastModifiedDate":"2016-12-07T10:02:24","indexId":"fs20093043","displayToPublicDate":"2011-11-30T00:00:00","publicationYear":"2009","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2009-3043","title":"Taste and odor occurrence in Lake William C. Bowen and Municipal Reservoir #1, Spartanburg County, South Carolina","docAbstract":"The U.S. Geological Survey and Spartanburg Water are working cooperatively on an ongoing study of Lake Bowen and Reservoir #1 to identify environmental factors that enhance or influence the production of geosmin in the source-water reservoirs. Spartanburg Water is using information from this study to develop management strategies to reduce (short-term solution) and prevent (long-term solution) geosmin occurrence.  Spartanburg Water utility treats and distributes drinking water to the Spartanburg area of South Carolina. The drinking water sources for the area are Lake William C. Bowen (Lake Bowen) and Municipal Reservoir #1 (Reservoir #1), located north of Spartanburg. These reservoirs, which were formed by the impoundment of the South Pacolet River, were assessed in 2006 by the South Carolina Department of Health and Environmental Control (SCDHEC) as being fully supportive of all uses based on established criteria. Nonetheless, Spartanburg Water had noted periodic taste and odor problems due to the presence of geosmin, a naturally occurring compound in the source water. Geosmin is not harmful, but its presence in drinking water is aesthetically unpleasant.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/fs20093043","collaboration":"Prepared in Cooperation with Spartanburg Water","usgsCitation":"Journey, C., and Arrington, J.M., 2009, Taste and odor occurrence in Lake William C. Bowen and Municipal Reservoir #1, Spartanburg County, South Carolina: U.S. Geological Survey Fact Sheet 2009-3043, 2 p., https://doi.org/10.3133/fs20093043.","productDescription":"2 p.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":110954,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2009/3043/","linkFileType":{"id":5,"text":"html"}},{"id":116665,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2009_3043.jpg"}],"country":"United States","state":"South Carolina","county":"Spartanburg","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -82.1942138671875,\n              35.05922870088872\n            ],\n            [\n              -82.1942138671875,\n              35.1614594458557\n            ],\n            [\n              -81.91783905029297,\n              35.1614594458557\n            ],\n            [\n              -81.91783905029297,\n              35.05922870088872\n            ],\n            [\n              -82.1942138671875,\n              35.05922870088872\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adce4b07f02db686341","contributors":{"authors":[{"text":"Journey, Celeste","contributorId":93585,"corporation":false,"usgs":true,"family":"Journey","given":"Celeste","affiliations":[],"preferred":false,"id":353840,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Arrington, Jane M.","contributorId":65975,"corporation":false,"usgs":true,"family":"Arrington","given":"Jane","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":353839,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70006104,"text":"ofr20091002 - 2009 - Digital seismic-reflection data from western Rhode Island Sound, 1980","interactions":[],"lastModifiedDate":"2012-02-10T00:12:00","indexId":"ofr20091002","displayToPublicDate":"2011-11-30T00:00:00","publicationYear":"2009","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2009-1002","title":"Digital seismic-reflection data from western Rhode Island Sound, 1980","docAbstract":"During 1980, the U.S. Geological Survey (USGS) conducted a seismic-reflection survey in western Rhode Island Sound aboard the Research Vessel Neecho. Data from this survey were recorded in analog form and archived at the USGS Woods Hole Science Center's Data Library. Due to recent interest in the geology of Rhode Island Sound and in an effort to make the data more readily accessible while preserving the original paper records, the seismic data from this cruise were scanned and converted to Tagged Image File Format (TIFF) images and SEG-Y data files. Navigation data were converted from U.S. Coast Guard Long Range Aids to Navigation (LORAN-C) time delays to latitudes and longitudes, which are available in Environmental Systems Research Institute, Inc. (ESRI) shapefile format and as eastings and northings in space-delimited text format.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20091002","usgsCitation":"McMullen, K., Poppe, L., and Soderberg, N., 2009, Digital seismic-reflection data from western Rhode Island Sound, 1980: U.S. Geological Survey Open-File Report 2009-1002, HTML Document, https://doi.org/10.3133/ofr20091002.","productDescription":"HTML Document","additionalOnlineFiles":"Y","temporalStart":"1980-01-01","temporalEnd":"1980-12-31","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":116661,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr_2009_1002.png"},{"id":110956,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2009/1002/index.html","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Rhode Island","geographicExtents":"{\"crs\": {\"type\": \"name\", \"properties\": {\"name\": \"urn:ogc:def:crs:OGC:1.3:CRS84\"}}, \"geometry\": {\"type\": \"Polygon\", \"coordinates\": [[[-71.41096878051758, 41.20311164855963], [-71.47355461120607, 41.19138145446782], [-71.53353118896484, 41.25826835632323], [-71.56668090820314, 41.314348220825316], [-71.56702232360838, 41.354669570922844], [-71.43700722642183, 41.40092751856604], [-71.45225320048858, 41.43205471561894], [-71.4178638458252, 41.45497703552252], [-71.40476962657254, 41.4462231268984], [-71.37142120309039, 41.45290428086218], [-71.3640254382043, 41.4404771516156], [-71.29193956647572, 41.458237438853125], [-71.29568381910639, 41.468077805435875], [-71.20956802368164, 41.485330581665046], [-71.14755249023438, 41.339784622192376], [-71.13011169433594, 41.260560989379975], [-71.41096878051758, 41.20311164855963]]]}, \"properties\": {\"extentType\": \"Custom\", \"code\": \"\", \"name\": \"\", \"notes\": \"\", \"promotedForReuse\": false, \"abbreviation\": \"\", \"shortName\": \"\", \"description\": \"\"}, \"bbox\": [-71.5692081451416, 41.19138145446782, -71.13011169433594, 41.485330581665046], \"type\": \"Feature\", \"id\": \"3091905\"}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0185e4b0c8380cd4fc37","contributors":{"authors":[{"text":"McMullen, K.Y.","contributorId":51857,"corporation":false,"usgs":true,"family":"McMullen","given":"K.Y.","email":"","affiliations":[],"preferred":false,"id":353843,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Poppe, L.J.","contributorId":72782,"corporation":false,"usgs":true,"family":"Poppe","given":"L.J.","affiliations":[],"preferred":false,"id":353844,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Soderberg, N.K.","contributorId":34138,"corporation":false,"usgs":true,"family":"Soderberg","given":"N.K.","email":"","affiliations":[],"preferred":false,"id":353842,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70006109,"text":"ofr20091298 - 2009 - Digital Mapping Techniques '08: Workshop Proceedings, Moscow, Idaho, May 18-21, 2008","interactions":[],"lastModifiedDate":"2019-04-01T08:40:01","indexId":"ofr20091298","displayToPublicDate":"2011-11-30T00:00:00","publicationYear":"2009","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2009-1298","title":"Digital Mapping Techniques '08: Workshop Proceedings, Moscow, Idaho, May 18-21, 2008","docAbstract":"The Digital Mapping Techniques '08 (DMT'08) workshop was attended by more than 100 technical experts from 40 agencies, universities, and private companies, including representatives from 24 State geological surveys. This year's meeting, the twelfth in the annual series, was hosted by the Idaho Geological Survey, from May 18-21, 2008, on the University of Idaho campus in Moscow, Idaho. Each DMT workshop has been coordinated by the U.S. Geological Survey's National Geologic Map Database Project and the Association of American State Geologists (AASG). As in previous years' meetings, the objective was to foster informal discussion and exchange of technical information, principally in order to develop more efficient methods for digital mapping, cartography, GIS analysis, and information management. At this meeting, oral and poster presentations and special discussion sessions emphasized (1) methods for creating and publishing map products (here, \"publishing\" includes Web-based release); (2) field data capture software and techniques, including the use of LiDAR; (3) digital cartographic techniques; (4) migration of digital maps into ArcGIS Geodatabase format; (5) analytical GIS techniques; and (6) continued development of the National Geologic Map Database.","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Digital Mapping Techniques '08: Workshop Proceedings, Moscow, Idaho, May 18-21, 2008","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"Digital Mapping Techniques '08 Workshop","conferenceDate":"May 18-21, 2009","conferenceLocation":"Moscow, Idaho","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20091298","usgsCitation":"Soller, D.R., 2009, Digital Mapping Techniques '08: Workshop Proceedings, Moscow, Idaho, May 18-21, 2008: U.S. Geological Survey Open-File Report 2009-1298, iv, 216 p.; PDF Downloads of Chapters, https://doi.org/10.3133/ofr20091298.","productDescription":"iv, 216 p.; PDF Downloads of Chapters","startPage":"i","endPage":"216","numberOfPages":"220","additionalOnlineFiles":"Y","costCenters":[{"id":420,"text":"National Geologic Map Database","active":false,"usgs":true}],"links":[{"id":116664,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr_2009_1298.jpg"},{"id":110961,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2009/1298/","linkFileType":{"id":5,"text":"html"}},{"id":362521,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2009/1298/pdf/usgs_of2009-1298.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0123e4b0c8380cd4faec","contributors":{"authors":[{"text":"Soller, David R. 0000-0001-6177-8332 drsoller@usgs.gov","orcid":"https://orcid.org/0000-0001-6177-8332","contributorId":2700,"corporation":false,"usgs":true,"family":"Soller","given":"David","email":"drsoller@usgs.gov","middleInitial":"R.","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true},{"id":5061,"text":"National Cooperative Geologic Mapping and Landslide Hazards","active":true,"usgs":true}],"preferred":true,"id":353858,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70006110,"text":"sir20095163 - 2009 - Estimated use of water in Alabama in 2005","interactions":[],"lastModifiedDate":"2012-02-03T00:10:05","indexId":"sir20095163","displayToPublicDate":"2011-11-30T00:00:00","publicationYear":"2009","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2009-5163","title":"Estimated use of water in Alabama in 2005","docAbstract":"Water use in Alabama was about 9,958 million gallons per day (Mgal/d) during 2005. Estimates of withdrawals by source indicate that total surface-water withdrawals were about 9,467 Mgal/d (95 percent of the total withdrawals) and the remaining 491 Mgal/d (5 percent) were from ground water. More surface water than ground water was withdrawn for all categories except aquaculture, mining, and self-supplied residential. During 2005, estimated withdrawals by category and in descending order were: thermoelectric power, 8,274 Mgal/d; public supply, 802 Mgal/d; self-supplied industrial, 550 Mgal/d; irrigation, 161 Mgal/d; aquaculture, 75 Mgal/d; self-supplied residential, 39 Mgal/d; livestock, 28 Mgal/d; and mining, 28 Mgal/d.\nDuring 2005, about 83 percent of the water used in Alabama was for thermoelectric power to generate about 114,144 net gigawatt-hours of energy. Almost all of the thermoelectric-power water use (about 8,274 Mgal/d) was from surface water; nearly all of the water (98 percent) was used for once-through cooling, and most of that water was returned to a surface-water source.\nPublic-supply and self-supplied residential withdrawals were about 8 percent of total water withdrawals and about 50 percent of total water withdrawals for all categories excluding thermoelectric power. The combined public-supply and self-supplied residential ground-water withdrawals were about 64 percent of total ground-water withdrawals for Alabama. Public-supply deliveries to residential customers were 41 percent of total public-supply withdrawals, or about 326 Mgal/d; combined industrial and commercial deliveries were 44 percent, or about 355 Mgal/d; and public use and losses accounted for the remaining 15 percent, or about 120 Mgal/d.\nSelf-supplied industrial (550 Mgal/d) and mining (28 Mgal/d) withdrawals were about 6 percent of total water withdrawals and about 33 percent of total water withdrawals for all categories excluding thermoelectric power. Paper and allied products accounted for the largest self-supplied industrial surface-water withdrawals (301 Mgal/d), and chemical and allied products (12 Mgal/d) accounted for the largest ground-water withdrawals.\nWater withdrawals for the agricultural sector-irrigation (161 Mgal/d), aquaculture (75 Mgal/d), and livestock (28 Mgal/d)-were about 3 percent of total withdrawals and about 16 percent of total withdrawals for all categories excluding thermoelectric power. About 135,800 acres of crops, nursery stock, sod, and golf courses were irrigated in 2005. About 97 percent of these acres were irrigated with sprinkler irrigation systems. The statewide average application rate was 1.33 acre-feet per acre per year. The highest application rate, 3.74 acre-feet per acre per year, was for nursery stock.\nThe largest total water withdrawals by county occurred in Limestone, Jackson, Colbert, and Mobile Counties, and were 60 percent of the total; these withdrawals primarily were used to meet the cooling needs at thermoelectric-power plants. Excluding thermoelectric power, the largest withdrawals by county were in Morgan, Mobile, Jefferson, Talladega, and Madison Counties.\nWater use was estimated at the hydrologic subbasin level for all categories except aquaculture, mining, and self-supplied residential. The Middle Tennessee-Elk subregion accounted for about 53 percent (5,185 Mgal/d) of the estimated total withdrawals by subbasin of 9,816 Mgal/d. About 92 percent of the water use in the Middle Tennessee-Elk subregion was for thermoelectric power, and more than 99 percent of the water was from surface water.\nGross per capita use for all offstream uses was 2,185 gallons per day (gal/d) for the estimated 4.56 million Alabama residents in 2005. Public-supply per capita use was 199 gal/d for the estimated 4.04 million residents served by a public supplier; public-supplied residential per capita use was 81 gal/d. Self-supplied residential per capita use was 75 gal/d for the estimated 0.52 million self-supplied residential population. Average residential per capita use was 80 gal/d.\nTotal water withdrawals decreased less than 1 percent from 9,990 Mgal/d in 2000 to 9,958 Mgal/d in 2005. Surface-water withdrawals decreased less than 5 percent from 9,950 Mgal/d in 2000 to 9,467 Mgal/d in 2005. In contrast, ground-water withdrawals increased about 12 percent from 440 Mgal/d in 2000 to 491 Mgal/d in 2005. By category, increases in irrigation (118 Mgal/d, about 274 percent), thermoelectric power (84 Mgal/d, about 1 percent), and aquaculture (65 Mgal/d, 620 percent) were offset by declines in self-supplied industrial (283 Mgal/d, about 34 percent), self-supplied residential (40 Mgal/d, about 50 percent); and public supply (32 Mgal/d, about 4 percent) from 2000 to 2005. Water use for livestock and mining was not estimated in 2000.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20095163","collaboration":"Prepared in cooperation with the Alabama Department of Economic and Community Affairs Office of Water Resources","usgsCitation":"Hutson, S.S., Littlepage, T.M., Harper, M.J., and Tinney, J.O., 2009, Estimated use of water in Alabama in 2005: U.S. Geological Survey Scientific Investigations Report 2009-5163, x, 102 p.; Appendices, https://doi.org/10.3133/sir20095163.","productDescription":"x, 102 p.; Appendices","costCenters":[{"id":101,"text":"AUM TechnaCenter","active":false,"usgs":true},{"id":105,"text":"Alabama Water Science Center","active":true,"usgs":true}],"links":[{"id":116666,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/sir_2009_5163.jpg"},{"id":110962,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2009/5163/","linkFileType":{"id":5,"text":"html"}}],"state":"Alabama","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4779e4b07f02db47f0a9","contributors":{"authors":[{"text":"Hutson, Susan S. sshutson@usgs.gov","contributorId":2040,"corporation":false,"usgs":true,"family":"Hutson","given":"Susan","email":"sshutson@usgs.gov","middleInitial":"S.","affiliations":[{"id":374,"text":"Maryland Water Science Center","active":true,"usgs":true}],"preferred":true,"id":353859,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Littlepage, Thomas M.","contributorId":55542,"corporation":false,"usgs":true,"family":"Littlepage","given":"Thomas","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":353860,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Harper, Michael J.","contributorId":63904,"corporation":false,"usgs":true,"family":"Harper","given":"Michael","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":353861,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Tinney, James O.","contributorId":104175,"corporation":false,"usgs":true,"family":"Tinney","given":"James","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":353862,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70006106,"text":"ofr20091171 - 2009 - Low-flow frequency and flow duration of selected South Carolina streams in the Pee Dee River basin through March 2007","interactions":[],"lastModifiedDate":"2016-12-08T12:38:47","indexId":"ofr20091171","displayToPublicDate":"2011-11-30T00:00:00","publicationYear":"2009","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2009-1171","title":"Low-flow frequency and flow duration of selected South Carolina streams in the Pee Dee River basin through March 2007","docAbstract":"Part of the mission of the South Carolina Department of Health and Environmental Control and the South Carolina Department of Natural Resources is to protect and preserve South Carolina's water resources. Doing so requires an ongoing understanding of streamflow characteristics of the rivers and streams in South Carolina. A particular need is information concerning the low-flow characteristics of streams; this information is especially important for effectively managing the State's water resources during critical flow periods such as the severe drought that occurred between 1998 and 2002 and the most recent drought that occurred between 2006 and 2009. In 2008, the U.S. Geological Survey, in cooperation with the South Carolina Department of Health and Environmental Control, initiated a study to update low-flow statistics at continuous-record streamgaging stations operated by the U.S. Geological Survey in South Carolina. Under this agreement, the low-flow characteristics at continuous-record streamgaging stations will be updated in a systematic manner during the monitoring and assessment of the eight major basins in South Carolina as defined and grouped according to the South Carolina Department of Health and Environmental Control's Watershed Water Quality Management Strategy. Depending on the length of record available at the continuous-record streamgaging stations, low-flow frequency characteristics are estimated for annual minimum 1-, 3-, 7-, 14-, 30-, 60-, and 90-day average flows with recurrence intervals of 2, 5, 10, 20, 30, and 50 years. Low-flow statistics are presented for 18 streamgaging stations in the Pee Dee River basin. In addition, daily flow durations for the 5-, 10-, 25-, 50-, 75-, 90-, and 95-percent probability of exceedance also are presented for the stations. The low-flow characteristics were computed from records available through March 31, 2007. The last systematic update of low-flow characteristics in South Carolina occurred more than 20 years ago and included data through March 1987. Of the 17 streamgaging stations included in this study, 15 had low-flow characteristics that were published in previous U.S. Geological Survey reports. A comparison of the low-flow characteristic for the minimum average flow for a 7-consecutive-day period with a 10-year recurrence interval from this study with the most recently published values indicated that 10 of the 15 streamgaging stations had values that were within &plusmn;25 percent of each other. Nine of the 15 streamgaging stations had negative percentage differences indicating the low-flow statistic had decreased since the previous study, 4 streamgaging stations had positive percent differences indicating that the low-flow statistic had increased since the previous study, and 2 streamgaging stations had a zero percent difference indicating no change since the previous study. The low-flow characteristics are influenced by length of record, hydrologic regime under which the record was collected, techniques used to do the analysis, and other changes that may have occurred in the watershed.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20091171","collaboration":"Prepared in cooperation with the South Carolina Department of Health and Environmental Control","usgsCitation":"Feaster, T., and Guimaraes, W.B., 2009, Low-flow frequency and flow duration of selected South Carolina streams in the Pee Dee River basin through March 2007 (Version 2.0: June 22, 2010): U.S. Geological Survey Open-File Report 2009-1171, vi, 19 p.; Tables, https://doi.org/10.3133/ofr20091171.","productDescription":"vi, 19 p.; Tables","startPage":"i","endPage":"39","numberOfPages":"45","additionalOnlineFiles":"N","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":116659,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr_2009_1171.jpg"},{"id":110958,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2009/1171/","linkFileType":{"id":5,"text":"html"}}],"projection":"Albers Equal Area","datum":"NAD 83","country":"United States","state":"North Carolina, South Carolina","otherGeospatial":"Pee Dee River 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Carolina\",\"nation\":\"USA  \"}}]}","edition":"Version 2.0: June 22, 2010","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7fe4b07f02db64873b","contributors":{"authors":[{"text":"Feaster, Toby D. 0000-0002-5626-5011 tfeaster@usgs.gov","orcid":"https://orcid.org/0000-0002-5626-5011","contributorId":1109,"corporation":false,"usgs":true,"family":"Feaster","given":"Toby D.","email":"tfeaster@usgs.gov","affiliations":[{"id":559,"text":"South Carolina Water Science Center","active":true,"usgs":true}],"preferred":false,"id":353852,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Guimaraes, Wladmir B. wbguimar@usgs.gov","contributorId":3818,"corporation":false,"usgs":true,"family":"Guimaraes","given":"Wladmir","email":"wbguimar@usgs.gov","middleInitial":"B.","affiliations":[{"id":559,"text":"South Carolina Water Science Center","active":true,"usgs":true}],"preferred":true,"id":353853,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70003945,"text":"70003945 - 2009 - Mine spoil prairies expand critical habitat for endangered and threatened amphibian and reptile species","interactions":[],"lastModifiedDate":"2012-02-02T00:16:01","indexId":"70003945","displayToPublicDate":"2011-11-28T00:00:00","publicationYear":"2009","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1398,"text":"Diversity","active":true,"publicationSubtype":{"id":10}},"title":"Mine spoil prairies expand critical habitat for endangered and threatened amphibian and reptile species","docAbstract":"Coal extraction has been occurring in the Midwestern United States for over a century. Despite the pre-mining history of the landscape as woodlands, spent surface coalfields are often reclaimed to grasslands. We assessed amphibian and reptile species on a large tract of coal spoil prairie and found 13 species of amphibians (nine frog and four salamander species) and 19 species of reptiles (one lizard, five turtle, and 13 snake species). Two state-endangered and three state species of special concern were documented. The amphibian diversity at our study site was comparable to the diversity found at a large restored prairie situated 175 km north, within the historic prairie peninsula.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Diversity","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Multidisciplinary Digital Publishing Institute","publisherLocation":"Basel, Switzerland","usgsCitation":"Lannoo, M.J., Kinney, V.C., Heemeyer, J.L., Engbrecht, N.J., Gallant, A.L., and Klaver, R.W., 2009, Mine spoil prairies expand critical habitat for endangered and threatened amphibian and reptile species: Diversity, v. 1, no. 2, p. 118-132.","productDescription":"15 p.","startPage":"118","endPage":"132","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":110929,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://www.mdpi.com/1424-2818/1/2/118/","linkFileType":{"id":5,"text":"html"}},{"id":204343,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","volume":"1","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a60e4b07f02db635695","contributors":{"authors":[{"text":"Lannoo, Michael J.","contributorId":46482,"corporation":false,"usgs":true,"family":"Lannoo","given":"Michael","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":349656,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kinney, Vanessa C.","contributorId":99690,"corporation":false,"usgs":true,"family":"Kinney","given":"Vanessa","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":349657,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Heemeyer, Jennifer L.","contributorId":14943,"corporation":false,"usgs":true,"family":"Heemeyer","given":"Jennifer","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":349655,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Engbrecht, Nathan J.","contributorId":103785,"corporation":false,"usgs":true,"family":"Engbrecht","given":"Nathan","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":349658,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Gallant, Alisa L. 0000-0002-3029-6637 gallant@usgs.gov","orcid":"https://orcid.org/0000-0002-3029-6637","contributorId":2940,"corporation":false,"usgs":true,"family":"Gallant","given":"Alisa","email":"gallant@usgs.gov","middleInitial":"L.","affiliations":[{"id":223,"text":"Earth Resources Observation and Science (EROS) Center (Geography)","active":false,"usgs":true},{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"preferred":true,"id":349653,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Klaver, Robert W. 0000-0002-3263-9701 bklaver@usgs.gov","orcid":"https://orcid.org/0000-0002-3263-9701","contributorId":3285,"corporation":false,"usgs":true,"family":"Klaver","given":"Robert","email":"bklaver@usgs.gov","middleInitial":"W.","affiliations":[{"id":199,"text":"Coop Res Unit Leetown","active":true,"usgs":true},{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"preferred":true,"id":349654,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70006007,"text":"70006007 - 2009 - Occurrence and removal of pharmaceutically active compounds in sewage treatment plants with different technologies","interactions":[],"lastModifiedDate":"2018-10-05T08:30:17","indexId":"70006007","displayToPublicDate":"2011-11-25T00:00:00","publicationYear":"2009","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2259,"text":"Journal of Environmental Monitoring","active":true,"publicationSubtype":{"id":10}},"title":"Occurrence and removal of pharmaceutically active compounds in sewage treatment plants with different technologies","docAbstract":"Occurrence of eight selected pharmaceutically active compounds (PhACs; caffeine, carbamazepine, triclosan, gemfibrozil, diclofenac, ibuprofen, ketoprofen and naproxen) were investigated in effluents from fifteen sewage treatment plants (STPs) across South Australia. In addition, a detailed investigation into the removal of these compounds was also carried out in four STPs with different technologies (Plant A: conventional activated sludge; plant B: two oxidation ditches; plant C: three bioreactors; and plant D: ten lagoons in series). The concentrations of these compounds in the effluents from the fifteen STPs showed substantial variations among the STPs, with their median concentrations ranging from 26 ng/L for caffeine to 710 ng/L for carbamazepine. Risk assessment based on the \"worst case scenario\" of the monitoring data from the present study suggested potential toxic risks to aquatic organisms posed by carbamazepine, triclosan and diclofenac associated with such effluent discharge. With the exception of carbamazepine and gemfibrozil, significant concentration decreases between influent and effluent were observed in the four STPs studied in more detail. Biodegradation was found to be the main mechanism for removing concentrations from the liquid waste stream for the PhACs within the four STPs, while adsorption onto sludge appeared to be a minor process for all target PhACs except for triclosan. Some compounds (<i>e.g.</i> gemfibrozil) exhibited variable removal efficiencies within the four STPs. Plant D (10 lagoons in series) was least efficient in the removal of the target PhACs; significant biodegradation of these compounds only occurred from the sixth or seventh lagoon.","language":"English","publisher":"Royal Society of Chemistry Publishing","doi":"10.1039/b904548a","usgsCitation":"Ying, G., Kookana, R., and Kolpin, D.W., 2009, Occurrence and removal of pharmaceutically active compounds in sewage treatment plants with different technologies: Journal of Environmental Monitoring, v. 11, no. 8, p. 1498-1505, https://doi.org/10.1039/b904548a.","productDescription":"8 p.","startPage":"1498","endPage":"1505","costCenters":[{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":204362,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":110917,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://www.sklog.labs.gov.cn/atticle/A09/A09040.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"Australia","volume":"11","issue":"8","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afbe4b07f02db696123","contributors":{"authors":[{"text":"Ying, Guang-Guo","contributorId":6576,"corporation":false,"usgs":true,"family":"Ying","given":"Guang-Guo","affiliations":[],"preferred":false,"id":353638,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kookana, Rai S.","contributorId":100518,"corporation":false,"usgs":true,"family":"Kookana","given":"Rai S.","affiliations":[],"preferred":false,"id":353639,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kolpin, Dana W. 0000-0002-3529-6505 dwkolpin@usgs.gov","orcid":"https://orcid.org/0000-0002-3529-6505","contributorId":1239,"corporation":false,"usgs":true,"family":"Kolpin","given":"Dana","email":"dwkolpin@usgs.gov","middleInitial":"W.","affiliations":[{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true}],"preferred":true,"id":353637,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70003532,"text":"70003532 - 2009 - Revisions to the stratigraphic nomenclature of the Abiquiu Formation, Abiquiu and contiguous areas, north-central New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:16:00","indexId":"70003532","displayToPublicDate":"2011-11-25T00:00:00","publicationYear":"2009","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2860,"text":"New Mexico Geology","active":true,"publicationSubtype":{"id":10}},"title":"Revisions to the stratigraphic nomenclature of the Abiquiu Formation, Abiquiu and contiguous areas, north-central New Mexico","docAbstract":"Stratigraphic studies and geologic mapping on the Abiquiu 7.5-min quadrangle have led to revision of the stratigraphic nomenclature for the Oligocene to Miocene Abiquiu Formation in north-central New Mexico. The Abiquiu Formation had previously been defined to include informal upper, middle (Pedernal chert member), and lower members. The basement-derived conglomeratic lower member in the northern Jemez Mountains and Abiquiu embayment is here redefined. We propose removing the \"lower member\" from the Abiquiu Formation because provenance of these coarse sediments is dramatically different than the volcaniclastic strata of the \"upper member.\" Furthermore, we propose that the term \"lower member of the Abiquiu Formation\" be replaced with an existing unit name, the Ritito Conglomerate of Barker (1958), and that the name Abiquiu Formation be restricted to the volcaniclastic succession. The lower part of the Ritito Conglomerate in Arroyo del Cobre on the Abiquiu quadrangle is 47 m (155 ft) thick and is composed of arkosic conglomeratic beds interbedded with arkosic sands and siltstones. Clasts include, in descending order of abundance, Proterozoic quartzite, granite, metavolcanic rocks, quartz, schist, and gneiss and a trace of Mesozoic sandstone and Paleozoic chert. Clasts are predominantly of pebble and cobble size but range from granule to boulder size. Paleocurrent data collected in the Arroyo del Cobre area indicate that the Ritito Conglomerate was deposited by a south-flowing river system during the Oligocene, eroding Laramide highlands such as the Tusas Mountains to the northeast, which contain predominantly Proterozoic rocks. This depositional setting has also been suggested by previous workers. The middle member or Pedernal chert member is present both at the top of the Ritito Conglomerate and as lenses within the lower part of the Abiquiu Formation. This post-depositional diagenetic chert remains an informal unit called the Pedernal chert.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"New Mexico Geology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"New Mexico Bureau of Geology & Mineral Resources","publisherLocation":"Socorro, NM","usgsCitation":"Maldonado, F., and Kelley, S.A., 2009, Revisions to the stratigraphic nomenclature of the Abiquiu Formation, Abiquiu and contiguous areas, north-central New Mexico: New Mexico Geology, v. 31, no. 1, p. 3-8.","productDescription":"6 p.","startPage":"3","endPage":"8","costCenters":[{"id":308,"text":"Geology and Environmental Change Science Center","active":false,"usgs":true}],"links":[{"id":204340,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":110912,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://geoinfo.nmt.edu/publications/periodicals/nmg/downloads/31/n1/nmg_v31_n1_p3.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"New Mexico","volume":"31","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db602902","contributors":{"authors":[{"text":"Maldonado, Florian fmaldona@usgs.gov","contributorId":805,"corporation":false,"usgs":true,"family":"Maldonado","given":"Florian","email":"fmaldona@usgs.gov","affiliations":[],"preferred":true,"id":347651,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kelley, Shari A.","contributorId":25606,"corporation":false,"usgs":true,"family":"Kelley","given":"Shari","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":347652,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70003394,"text":"70003394 - 2009 - Response to the <i>Point of View</i> of Gregory B. Pauly, David M. Hillis, and David C. Cannatella, by the Anuran Subcommittee of the SSAR/HL/ASIH Scientific and Standard English Names List","interactions":[],"lastModifiedDate":"2012-02-02T00:16:00","indexId":"70003394","displayToPublicDate":"2011-11-23T00:00:00","publicationYear":"2009","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1892,"text":"Herpetologica","active":true,"publicationSubtype":{"id":10}},"title":"Response to the <i>Point of View</i> of Gregory B. Pauly, David M. Hillis, and David C. Cannatella, by the Anuran Subcommittee of the SSAR/HL/ASIH Scientific and Standard English Names List","docAbstract":"The <i>Point of View</i> by Gregory Pauly, David Hillis, and David Cannatella misrepresents the motives and activities of the anuran subcommittee of the Scientific and Standard English Names Committee, contains a number of misleading statements, omits evidence and references to critical literature that have already rejected or superseded their positions, and cloaks the limitations of their nomenclatural approach in ambiguous language. Their <i>Point of View</i> is not about promoting transparency in the process of constructing the English Names list, assuring that its taxonomy is adequately reviewed, or promoting nomenclatural stability in any global sense. Rather, their <i>Point of View</i> focuses in large part on a single publication, <i>The Amphibian Tree of Life</i>, which is formally unrelated to the <i>Standard English Names List</i>, and promotes an approach to nomenclature mistakenly asserted by them to be compatible with both the <i>International Code of Zoological Nomenclature</i> and one of its competitors, the <i>PhyloCode</i>.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Herpetologica","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"The Herpetologists' League","publisherLocation":"Lawrence, KS","usgsCitation":"Frost, D., McDiarmid, R.W., and Mendelson, J.R., 2009, Response to the <i>Point of View</i> of Gregory B. Pauly, David M. Hillis, and David C. Cannatella, by the Anuran Subcommittee of the SSAR/HL/ASIH Scientific and Standard English Names List: Herpetologica, v. 65, no. 2, p. 136-153.","productDescription":"18 p.","startPage":"136","endPage":"153","numberOfPages":"18","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":204497,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":21673,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://si-pddr.si.edu/jspui/bitstream/10088/11419/1/vz_2009_Response_to_Point_of_View_Herpetologica_65_136-153.pdf","linkFileType":{"id":1,"text":"pdf"}}],"volume":"65","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ee4b07f02db628306","contributors":{"authors":[{"text":"Frost, Darrel R.","contributorId":69851,"corporation":false,"usgs":true,"family":"Frost","given":"Darrel R.","affiliations":[],"preferred":false,"id":347112,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McDiarmid, Roy W. 0000-0002-7649-1796 rmcdiarmid@usgs.gov","orcid":"https://orcid.org/0000-0002-7649-1796","contributorId":3603,"corporation":false,"usgs":true,"family":"McDiarmid","given":"Roy","email":"rmcdiarmid@usgs.gov","middleInitial":"W.","affiliations":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"preferred":true,"id":347110,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mendelson, Joseph R. III","contributorId":46834,"corporation":false,"usgs":true,"family":"Mendelson","given":"Joseph","suffix":"III","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":347111,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
]}