{"pageNumber":"2617","pageRowStart":"65400","pageSize":"25","recordCount":184605,"records":[{"id":85611,"text":"85611 - 2005 - Care and use of wildlife in field research","interactions":[],"lastModifiedDate":"2012-02-02T00:04:00","indexId":"85611","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Care and use of wildlife in field research","docAbstract":"Abstract not submitted to date","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Techniques for wildlife investigations and management","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","publisher":"The Wildlife Society","publisherLocation":"Bethesda, MD","usgsCitation":"Dein, F., Toweill, D.E., and Kenow, K., 2005, Care and use of wildlife in field research, chap. <i>of</i> Techniques for wildlife investigations and management, 185-196.","productDescription":"185-196","costCenters":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":127894,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f4e4b07f02db5f008c","contributors":{"editors":[{"text":"Braun, C.E.","contributorId":57421,"corporation":false,"usgs":true,"family":"Braun","given":"C.E.","email":"","affiliations":[],"preferred":false,"id":504563,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Dein, F. J.","contributorId":97030,"corporation":false,"usgs":true,"family":"Dein","given":"F. J.","affiliations":[],"preferred":false,"id":296121,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Toweill, D. E.","contributorId":81441,"corporation":false,"usgs":true,"family":"Toweill","given":"D.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":296120,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kenow, K.P.","contributorId":18302,"corporation":false,"usgs":true,"family":"Kenow","given":"K.P.","affiliations":[],"preferred":false,"id":296119,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70161789,"text":"70161789 - 2005 - Chronic boat strike and polycyctic kidneys in a free-ranging Florida manatee (<i>Trichechus manatus latirostris</i>)","interactions":[],"lastModifiedDate":"2016-01-06T10:01:52","indexId":"70161789","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Chronic boat strike and polycyctic kidneys in a free-ranging Florida manatee (<i>Trichechus manatus latirostris</i>)","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":24,"text":"Conference Paper"},"largerWorkTitle":"Proceedings of the 36th Annual Conference of the International Association for Aquatic Animal Medicine","largerWorkSubtype":{"id":19,"text":"Conference Paper"},"conferenceTitle":"36th Annual Conference of the International Association for Aquatic Animal Medicine","conferenceDate":"May 14-18, 2005","conferenceLocation":"Seward, AK","language":"English","publisher":"International Association for Aquatic Animal Medicine","usgsCitation":"Rember, R., Harr, K., Ginn, P.E., Lightsey, J., Keller, M., Bonde, R., and Reid, J., 2005, Chronic boat strike and polycyctic kidneys in a free-ranging Florida manatee (<i>Trichechus manatus latirostris</i>), <i>in</i> Proceedings of the 36th Annual Conference of the International Association for Aquatic Animal Medicine, v. 36, Seward, AK, May 14-18, 2005.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":566,"text":"Southeast Ecological Science Center","active":true,"usgs":true}],"links":[{"id":313907,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"36","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"568e48e9e4b0e7a44bc418b6","contributors":{"authors":[{"text":"Rember, Renee","contributorId":97633,"corporation":false,"usgs":true,"family":"Rember","given":"Renee","email":"","affiliations":[],"preferred":false,"id":587772,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Harr, K.","contributorId":84693,"corporation":false,"usgs":true,"family":"Harr","given":"K.","email":"","affiliations":[],"preferred":false,"id":587773,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ginn, Pamela E.","contributorId":13748,"corporation":false,"usgs":true,"family":"Ginn","given":"Pamela","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":587774,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lightsey, Jessica","contributorId":69709,"corporation":false,"usgs":true,"family":"Lightsey","given":"Jessica","email":"","affiliations":[],"preferred":false,"id":587775,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Keller, M.","contributorId":149251,"corporation":false,"usgs":false,"family":"Keller","given":"M.","email":"","affiliations":[],"preferred":false,"id":587776,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Bonde, R. 0000-0001-9179-4376","orcid":"https://orcid.org/0000-0001-9179-4376","contributorId":81042,"corporation":false,"usgs":true,"family":"Bonde","given":"R.","affiliations":[],"preferred":false,"id":587777,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Reid, J.","contributorId":42542,"corporation":false,"usgs":true,"family":"Reid","given":"J.","email":"","affiliations":[],"preferred":false,"id":587778,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70189665,"text":"70189665 - 2005 - Linkages between climate, growth, competition at sea and production of sockeye salmon populations in Bristol Bay, 1955-2000","interactions":[],"lastModifiedDate":"2017-07-19T15:06:11","indexId":"70189665","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Linkages between climate, growth, competition at sea and production of sockeye salmon populations in Bristol Bay, 1955-2000","docAbstract":"<p>Bristol Bay, Alaska, supports one of the largest and most valuable salmon fisheries in the world. Salmon abundance in Bristol Bay and other northern areas more than doubled after the 1976–77 marine climate shift. However, in 1997–98, a major El Niño event led to unusual oceanographic conditions and Bristol Bay sockeye salmon production was unexpectedly low. Nevertheless, the effect of climate on biological mechanisms leading to greater salmon survival and production are poorly understood. In order to test several hypotheses linking climate to salmon growth, interspecific and intraspecific competition, and salmon production, we measured annual marine and freshwater scale growth of Bristol Bay sockeye salmon, 1955 to 2000. </p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Proceedings of the open science meeting study of environmental Arctic change (SEARCH)","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"Open Science Meeting: Study of Environmental Arctic Change (SEARCH)","conferenceDate":"October 27-30, 2003","conferenceLocation":"Seattle, WA","language":"English","publisher":"Arctic Research Consortium of the U.S","usgsCitation":"Nielsen, J.L., and Ruggerone, G.T., 2005, Linkages between climate, growth, competition at sea and production of sockeye salmon populations in Bristol Bay, 1955-2000, <i>in</i> Proceedings of the open science meeting study of environmental Arctic change (SEARCH), Seattle, WA, October 27-30, 2003, p. 198-198.","productDescription":"1 p.","startPage":"198","endPage":"198","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":344073,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":344072,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.arcus.org/search-program/products"}],"country":"United States","state":"Alaska","otherGeospatial":"Bristol Bay","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"59706fdfe4b0d1f9f065ab1a","contributors":{"editors":[{"text":"Behr, Sarah","contributorId":20479,"corporation":false,"usgs":false,"family":"Behr","given":"Sarah","email":"","affiliations":[{"id":34108,"text":"Arctic Research Consortium of the U.S. (ARCUS)","active":true,"usgs":false}],"preferred":false,"id":705688,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Wiggins, Helen","contributorId":104416,"corporation":false,"usgs":false,"family":"Wiggins","given":"Helen","email":"","affiliations":[{"id":34108,"text":"Arctic Research Consortium of the U.S. (ARCUS)","active":true,"usgs":false}],"preferred":false,"id":705689,"contributorType":{"id":2,"text":"Editors"},"rank":2},{"text":"York, Alison","contributorId":99067,"corporation":false,"usgs":false,"family":"York","given":"Alison","email":"","affiliations":[{"id":34108,"text":"Arctic Research Consortium of the U.S. (ARCUS)","active":true,"usgs":false}],"preferred":false,"id":705693,"contributorType":{"id":2,"text":"Editors"},"rank":3}],"authors":[{"text":"Nielsen, Jennifer L.","contributorId":43722,"corporation":false,"usgs":true,"family":"Nielsen","given":"Jennifer","email":"","middleInitial":"L.","affiliations":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"preferred":true,"id":705680,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ruggerone, Gregory T.","contributorId":48068,"corporation":false,"usgs":true,"family":"Ruggerone","given":"Gregory","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":705681,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70161786,"text":"70161786 - 2005 - Prey vulnerability to peacock cichlids and largemouth bass based on predator gape and prey body depth","interactions":[],"lastModifiedDate":"2016-01-06T09:47:10","indexId":"70161786","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3896,"text":"Proceedings of the Southeastern Association of Fish and Wildlife Agencies","active":true,"publicationSubtype":{"id":10}},"title":"Prey vulnerability to peacock cichlids and largemouth bass based on predator gape and prey body depth","docAbstract":"<p><span>The interaction of prey fish body depth and predator gape size may produce prey assemblages dominated by invulnerable prey and excessive prey-to-predator biomass ratios. Peacock cichlids (Cichla ocellaris) were stocked into southeast Florida canals to consume excess prey fish biomass, particularly spotted tilapia (Tilapia mariae). The ecomorphologically similar largemouth bass (Micropterus salmoides) was already present in the canals. We present relations of length-specific gape size for peacock cichlids and largemouth bass. Both predators have broadly overlapping gape size, but largemouth bass ?126 mm total length have slightly larger gape sizes than peacock cichlids of the same length. Also, we experimentally tested the predictions of maximum prey size for peacock cichlids and determined that a simple method of measuring gape size used for largemouth bass also is appropriate for peacock cichlids. Lastly, we determined relations of body depth and length of prey species to investigate relative vulnerability. Using a simple predator-prey model and length frequencies of predators and bluegill (Lepomis macrochirus), redear sunfish (Lepomis microlophus), and spotted tilapia prey, we documented that much of the prey biomass in southeast Florida canals is unavailable for largemouth bass and peacock cichlid predation.</span></p>","language":"English","publisher":"Southeastern Association of Fish and Wildlife Agencies","usgsCitation":"Hill, J., Nico, L.G., Cichra, C.E., and Gilbert, C.R., 2005, Prey vulnerability to peacock cichlids and largemouth bass based on predator gape and prey body depth: Proceedings of the Southeastern Association of Fish and Wildlife Agencies, v. 58, p. 47-56.","productDescription":"10 p.","startPage":"47","endPage":"56","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":566,"text":"Southeast Ecological Science 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E.","contributorId":152065,"corporation":false,"usgs":false,"family":"Cichra","given":"Charles","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":587766,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Gilbert, Carter R.","contributorId":7667,"corporation":false,"usgs":true,"family":"Gilbert","given":"Carter","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":587767,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70029046,"text":"70029046 - 2005 - Dissolution of cinnabar (HgS) in the presence of natural organic matter","interactions":[],"lastModifiedDate":"2018-10-31T10:16:12","indexId":"70029046","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1759,"text":"Geochimica et Cosmochimica Acta","active":true,"publicationSubtype":{"id":10}},"title":"Dissolution of cinnabar (HgS) in the presence of natural organic matter","docAbstract":"<p><span>Cinnabar (HgS) dissolution rates were measured in the presence of 12 different natural dissolved organic matter (DOM) isolates including humic, fulvic, and hydrophobic acid fractions. Initial dissolution rates varied by 1.3 orders of magnitude, from 2.31 × 10</span><sup>−13</sup><span>&nbsp;to 7.16 × 10</span><sup>−12</sup><span>&nbsp;mol Hg (mg C)</span><sup>−1</sup><span>&nbsp;m</span><sup>−2</sup><span>s</span><sup>−1</sup><span>. Rates correlate positively with three DOM characteristics: specific ultraviolet absorbance (R</span><sup>2</sup><span>&nbsp;= 0.88), aromaticity (R</span><sup>2</sup><span>&nbsp;= 0.80), and molecular weight (R</span><sup>2</sup><span>= 0.76). Three experimental observations demonstrate that dissolution was controlled by the interaction of DOM with the cinnabar surface: (1) linear rates of Hg release with time, (2) significantly reduced rates when DOM was physically separated from the surface by dialysis membranes, and (3) rates that approached constant values at a specific ratio of DOM concentration to cinnabar surface area, suggesting a maximum surface coverage by dissolution-reactive DOM. Dissolution rates for the hydrophobic acid fractions correlate negatively with sorbed DOM concentrations, indicating the presence of a DOM component that reduced the surface area of cinnabar that can be dissolved. When two hydrophobic acid isolates that enhanced dissolution to different extents were mixed equally, a 20% reduction in rate occurred compared to the rate with the more dissolution-enhancing isolate alone. Rates in the presence of the more dissolution-enhancing isolate were reduced by as much as 60% when cinnabar was prereacted with the isolate that enhanced dissolution to a lesser extent. The data, taken together, imply that the property of DOM that enhances cinnabar dissolution is distinct from the property that causes it to sorb irreversibly to the cinnabar surface.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.gca.2004.09.029","issn":"00167037","usgsCitation":"Waples, J., Nagy, K.L., Aiken, G., and Ryan, J.N., 2005, Dissolution of cinnabar (HgS) in the presence of natural organic matter: Geochimica et Cosmochimica Acta, v. 69, no. 6, p. 1575-1588, https://doi.org/10.1016/j.gca.2004.09.029.","productDescription":"14 p.","startPage":"1575","endPage":"1588","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":209683,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.gca.2004.09.029"},{"id":236356,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"69","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a022fe4b0c8380cd4ff22","contributors":{"authors":[{"text":"Waples, J.S.","contributorId":107078,"corporation":false,"usgs":true,"family":"Waples","given":"J.S.","email":"","affiliations":[],"preferred":false,"id":421116,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nagy, K. L.","contributorId":56408,"corporation":false,"usgs":true,"family":"Nagy","given":"K.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":421114,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Aiken, G. R. 0000-0001-8454-0984","orcid":"https://orcid.org/0000-0001-8454-0984","contributorId":14452,"corporation":false,"usgs":true,"family":"Aiken","given":"G. R.","affiliations":[],"preferred":false,"id":421113,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ryan, J. N.","contributorId":102649,"corporation":false,"usgs":true,"family":"Ryan","given":"J.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":421115,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70194196,"text":"70194196 - 2005 - Environmental stresses and skeletal deformities in fish from the Willamette River, Oregon","interactions":[],"lastModifiedDate":"2017-11-17T10:38:29","indexId":"70194196","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1565,"text":"Environmental Science & Technology","onlineIssn":"1520-5851","printIssn":"0013-936X","active":true,"publicationSubtype":{"id":10}},"title":"Environmental stresses and skeletal deformities in fish from the Willamette River, Oregon","docAbstract":"<p>The Willamette River, one of 14 American Heritage Rivers, flows through the most densely populated and agriculturally productive region of Oregon. Previous biological monitoring of the Willamette River detected elevated frequencies of skeletal deformities in fish from certain areas of the lower (Newberg pool [NP], rivermile [RM] 26−55) and middle (Wheatland Ferry [WF], RM 72−74) river, relative to those in the upper river (Corvallis [CV], RM 125−138). The objective of this study was to determine the likely cause of these skeletal deformities. In 2002 and 2003, deformity loads in Willamette River fishes were 2−3 times greater at the NP and WF locations than at the CV location. There were some differences in water quality parameters between the NP and CV sites, but they did not readily explain the difference in deformity loads. Concentrations of bioavailable metals were below detection limits (0.6−1 μg/L). Concentrations of bioavailable polychlorinated biphenyls (PCBs) and chlorinated pesticides were generally below 0.25 ng/L. Concentrations of bioavailable polycyclic aromatic hydrocarbons were generally less than 5 ng/L. Concentrations of most persistent organic pollutants were below detection limits in ovary/oocyte tissue samples and sediments, and those that were detected were not significantly different among sites. Bioassay of Willamette River water extracts provided no evidence that unidentified compounds or the complex mixture of compounds present in the extracts could induce skeletal deformities in cyprinid fish. However, metacercariae of a digenean trematode were directly associated with a large percentage of deformities detected in two Willamette River fishes, and similar deformities were reproduced in laboratory fathead minnows exposed to cercariae extracted from Willamette River snails. Thus, the weight of evidence suggests that parasitic infection, not chemical contaminants, was the primary cause of skeletal deformities observed in Willamette River fish. </p>","language":"English","publisher":"ACS Publications","doi":"10.1021/es048570c","usgsCitation":"Villeneuve, D.L., Curtis, L.R., Jenkins, J., Warner, K.E., Tilton, F., Kent, M., Watral, V.G., Cunningham, M.E., Markle, D.F., Sethajintanin, D., Krissanakriangkrai, O., Johnson, E.R., and Grove, R., 2005, Environmental stresses and skeletal deformities in fish from the Willamette River, Oregon: Environmental Science & Technology, v. 39, no. 10, p. 3495-3506, https://doi.org/10.1021/es048570c.","productDescription":"12 p.","startPage":"3495","endPage":"3506","costCenters":[{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true}],"links":[{"id":349051,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Oregon","otherGeospatial":"Willamette River","volume":"39","issue":"10","noUsgsAuthors":false,"publicationDate":"2005-04-12","publicationStatus":"PW","scienceBaseUri":"5a611697e4b06e28e9c258ed","contributors":{"authors":[{"text":"Villeneuve, Daniel L.","contributorId":32091,"corporation":false,"usgs":false,"family":"Villeneuve","given":"Daniel","email":"","middleInitial":"L.","affiliations":[{"id":13485,"text":"U.S. Environmental Protection Agency, Duluth, MN","active":true,"usgs":false}],"preferred":false,"id":722605,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Curtis, Lawrence R.","contributorId":118469,"corporation":false,"usgs":false,"family":"Curtis","given":"Lawrence","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":722606,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Jenkins, Jeffrey J.","contributorId":98279,"corporation":false,"usgs":false,"family":"Jenkins","given":"Jeffrey J.","affiliations":[],"preferred":false,"id":722607,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Warner, Kara E.","contributorId":177381,"corporation":false,"usgs":false,"family":"Warner","given":"Kara","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":722608,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Tilton, Fred","contributorId":89534,"corporation":false,"usgs":false,"family":"Tilton","given":"Fred","email":"","affiliations":[],"preferred":false,"id":722609,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Kent, Michael L.","contributorId":108420,"corporation":false,"usgs":true,"family":"Kent","given":"Michael L.","affiliations":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"preferred":false,"id":722610,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Watral, Virginia G.","contributorId":55240,"corporation":false,"usgs":false,"family":"Watral","given":"Virginia","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":722611,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Cunningham, Michael E.","contributorId":61465,"corporation":false,"usgs":false,"family":"Cunningham","given":"Michael","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":722612,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Markle, Douglas F.","contributorId":14530,"corporation":false,"usgs":true,"family":"Markle","given":"Douglas","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":722613,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Sethajintanin, Doolalai","contributorId":77884,"corporation":false,"usgs":false,"family":"Sethajintanin","given":"Doolalai","email":"","affiliations":[],"preferred":false,"id":722614,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Krissanakriangkrai, Oraphin","contributorId":29267,"corporation":false,"usgs":false,"family":"Krissanakriangkrai","given":"Oraphin","email":"","affiliations":[],"preferred":false,"id":722615,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Johnson, Eugene R.","contributorId":54400,"corporation":false,"usgs":false,"family":"Johnson","given":"Eugene","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":722616,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Grove, Robert","contributorId":172512,"corporation":false,"usgs":true,"family":"Grove","given":"Robert","affiliations":[],"preferred":false,"id":722617,"contributorType":{"id":1,"text":"Authors"},"rank":13}]}}
,{"id":70029047,"text":"70029047 - 2005 - Cultural change in the songs of humpback whales (Megaptera novaeangliae) from Tonga","interactions":[],"lastModifiedDate":"2012-03-12T17:21:00","indexId":"70029047","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":986,"text":"Behaviour","active":true,"publicationSubtype":{"id":10}},"title":"Cultural change in the songs of humpback whales (Megaptera novaeangliae) from Tonga","docAbstract":"Some humpback whales migrate annually from Antarctic feeding grounds to the seas around the Tongan Islands to give birth and mate. The Tongan humpbacks are considered part of Southern Hemisphere Group V that splits during migration, some swimming to Eastern Australia and others to various Polynesian Islands. During this time long complex songs are produced. The song is thought to be a male breeding display and may serve either as an intra-sexual or an inter-sexual signal or both. It is in a constant state of change that occurs every season. Since these changes are directional they cannot be described by drift, and singers incorporate changes as they occur, thus song must be shared through cultural transmission. This investigation describes the cultural changes that occurred in 158 songs recorded from Tongan humpbacks through the 1990s. The rate of change differed within years, some themes were retained for as much as five years and others were lost after only two years. The farther apart the years the less similar are the songs, as in the humpback songs of the Northern Hemisphere. The largest number of changes seems to have occurred in the early 1990s where all themes seemed to have been lost and new ones originated. What initiates these changes remains speculative, but we assess some hypotheses in relation to humpback whale behaviour and cultural transmission in avian song. ?? Koninklijke Brill NV, 2005.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Behaviour","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1163/1568539053778283","issn":"00057959","usgsCitation":"Eriksen, N., Miller, L., Tougaard, J., and Helweg, D., 2005, Cultural change in the songs of humpback whales (Megaptera novaeangliae) from Tonga: Behaviour, v. 142, no. 3, p. 305-328, https://doi.org/10.1163/1568539053778283.","startPage":"305","endPage":"328","numberOfPages":"24","costCenters":[],"links":[{"id":236357,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":209684,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1163/1568539053778283"}],"volume":"142","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059fd05e4b0c8380cd4e5ba","contributors":{"authors":[{"text":"Eriksen, N.","contributorId":91289,"corporation":false,"usgs":true,"family":"Eriksen","given":"N.","email":"","affiliations":[],"preferred":false,"id":421118,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miller, L.A.","contributorId":39178,"corporation":false,"usgs":true,"family":"Miller","given":"L.A.","email":"","affiliations":[],"preferred":false,"id":421117,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Tougaard, J.","contributorId":92032,"corporation":false,"usgs":true,"family":"Tougaard","given":"J.","email":"","affiliations":[],"preferred":false,"id":421119,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Helweg, D.A.","contributorId":107072,"corporation":false,"usgs":true,"family":"Helweg","given":"D.A.","affiliations":[],"preferred":false,"id":421120,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70029612,"text":"70029612 - 2005 - Source mechanism of Vulcanian degassing at Popocatépetl Volcano, Mexico, determined from waveform inversions of very long period signals","interactions":[],"lastModifiedDate":"2019-05-01T10:37:26","indexId":"70029612","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2314,"text":"Journal of Geophysical Research B: Solid Earth","active":true,"publicationSubtype":{"id":10}},"title":"Source mechanism of Vulcanian degassing at Popocatépetl Volcano, Mexico, determined from waveform inversions of very long period signals","docAbstract":"<p><span>The source mechanism of very long period (VLP) signals accompanying volcanic degassing bursts at Popocat&eacute;petl is analyzed in the 15&ndash;70 s band by minimizing the residual error between data and synthetics calculated for a point source embedded in a homogeneous medium. The waveforms of two eruptions (23 April and 23 May 2000) representative of mild Vulcanian activity are well reproduced by our inversion, which takes into account volcano topography. The source centroid is positioned 1500 m below the western perimeter of the summit crater, and the modeled source is composed of a shallow dipping crack (sill with easterly dip of 10&deg;) intersecting a steeply dipping crack (northeast striking dike dipping 83&deg; northwest), whose surface extension bisects the vent. Both cracks undergo a similar sequence of inflation, deflation, and reinflation, reflecting a cycle of pressurization, depressurization, and repressurization within a time interval of 3&ndash;5 min. The largest moment release occurs in the sill, showing a maximum volume change of 500&ndash;1000 m</span><span>3</span><span>, pressure drop of 3&ndash;5 MPa, and amplitude of recovered pressure equal to 1.2 times the amplitude of the pressure drop. In contrast, the maximum volume change in the dike is less (200&ndash;300 m</span><span>3</span><span>), with a corresponding pressure drop of 1&ndash;2 MPa and pressure recovery equal to the pressure drop. Accompanying these volumetric sources are single-force components with magnitudes of 10</span><span>8</span><span>&nbsp;N, consistent with melt advection in response to pressure transients. The source time histories of the volumetric components of the source indicate that significant mass movement starts within the sill and triggers a mass movement response in the dike within a few seconds. Such source behavior is consistent with the opening of a pathway for escape of pent-up gases from slow pressurization of the sill driven by magma crystallization. The opening of this pathway and associated rapid evacuation of volcanic gases induces the pressure drop. Pressure recovery in the magma filling the sill is driven by diffusion of gases from the resulting supersaturated melt into bubbles. Assuming a penny-shaped crack at ambient pressure of 40 MPa, the observed pressure and volume variations can be modeled with the following attributes: crack radius (100 m), crack aperture (5 m), bubble number density (10</span><span>10</span><span>&ndash;10</span><span>12</span><span>&nbsp;m</span><span>&minus;3</span><span>), initial bubble radius (10</span><span>&minus;6</span><span>&nbsp;m), final bubble radius (&sim;10</span><span>&minus;5</span><span>&nbsp;m), and net decrease of gas concentration in the melt (0.01 wt %).</span></p>","language":"English","publisher":"AGU Publications","doi":"10.1029/2004JB003524","issn":"01480227","usgsCitation":"Chouet, B.A., Dawson, P.B., and Arciniega-Ceballos, A., 2005, Source mechanism of Vulcanian degassing at Popocatépetl Volcano, Mexico, determined from waveform inversions of very long period signals: Journal of Geophysical Research B: Solid Earth, v. 110, no. 7, p. 1-20, https://doi.org/10.1029/2004JB003524.","productDescription":"20 p.","startPage":"1","endPage":"20","numberOfPages":"20","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true}],"links":[{"id":477787,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1029/2004jb003524","text":"Publisher Index Page"},{"id":210799,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1029/2004JB003524"},{"id":237825,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Mexico","otherGeospatial":" Popocatépetl Volcano","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -98.8494873046875,\n              18.841313810317\n            ],\n            [\n              -98.41278076171875,\n              18.841313810317\n            ],\n            [\n              -98.41278076171875,\n              19.29299799768025\n            ],\n            [\n              -98.8494873046875,\n              19.29299799768025\n            ],\n            [\n              -98.8494873046875,\n              18.841313810317\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"110","issue":"7","noUsgsAuthors":false,"publicationDate":"2005-07-06","publicationStatus":"PW","scienceBaseUri":"505b932de4b08c986b31a33f","contributors":{"authors":[{"text":"Chouet, Bernard A. 0000-0001-5527-0532 chouet@usgs.gov","orcid":"https://orcid.org/0000-0001-5527-0532","contributorId":3304,"corporation":false,"usgs":true,"family":"Chouet","given":"Bernard","email":"chouet@usgs.gov","middleInitial":"A.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":423452,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dawson, Phillip B. dawson@usgs.gov","contributorId":2751,"corporation":false,"usgs":true,"family":"Dawson","given":"Phillip","email":"dawson@usgs.gov","middleInitial":"B.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":423451,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Arciniega-Ceballos, Alejandra","contributorId":57740,"corporation":false,"usgs":true,"family":"Arciniega-Ceballos","given":"Alejandra","affiliations":[],"preferred":false,"id":423450,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70029142,"text":"70029142 - 2005 - Population structure of Columbia spotted frogs (<i>Rana luteiventris</i>) is strongly affected by the landscape","interactions":[],"lastModifiedDate":"2015-12-14T10:16:49","indexId":"70029142","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2774,"text":"Molecular Ecology","active":true,"publicationSubtype":{"id":10}},"title":"Population structure of Columbia spotted frogs (<i>Rana luteiventris</i>) is strongly affected by the landscape","docAbstract":"<p>Landscape features such as mountains, rivers, and ecological gradients may strongly affect patterns of dispersal and gene flow among populations and thereby shape population dynamics and evolutionary trajectories. The landscape may have a particularly strong effect on patterns of dispersal and gene flow in amphibians because amphibians are thought to have poor dispersal abilities. We examined genetic variation at six microsatellite loci in Columbia spotted frogs (<i>Rana luteiventris</i>) from 28 breeding ponds in western Montana and Idaho, USA, in order to investigate the effects of landscape structure on patterns of gene flow. We were particularly interested in addressing three questions: (i) do ridges act as barriers to gene flow? (ii) is gene flow restricted between low and high elevation ponds? (iii) does a pond equal a 'randomly mating population' (a deme)? We found that mountain ridges and elevational differences were associated with increased genetic differentiation among sites, suggesting that gene flow is restricted by ridges and elevation in this species. We also found that populations of Columbia spotted frogs generally include more than a single pond except for very isolated ponds. There was also evidence for surprisingly high levels of gene flow among low elevation sites separated by large distances. Moreover, genetic variation within populations was strongly negatively correlated with elevation, suggesting effective population sizes are much smaller at high elevation than at low elevation. Our results show that landscape features have a profound effect on patterns of genetic variation in Columbia spotted frogs.</p>","language":"English","publisher":"Blackwell Science","publisherLocation":"Oxford","doi":"10.1111/j.1365-294X.2005.02426.x","issn":"09621083","usgsCitation":"Funk, W., Blouin, M., Corn, P., Maxell, B., Pilliod, D., Amish, S., and Allendorf, F., 2005, Population structure of Columbia spotted frogs (<i>Rana luteiventris</i>) is strongly affected by the landscape: Molecular Ecology, v. 14, no. 2, p. 483-496, https://doi.org/10.1111/j.1365-294X.2005.02426.x.","productDescription":"14 p.","startPage":"483","endPage":"496","numberOfPages":"14","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":481,"text":"Northern Rocky Mountain Science Center","active":true,"usgs":true}],"links":[{"id":477902,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1111/j.1365-294x.2005.02426.x","text":"Publisher Index Page"},{"id":237903,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":210857,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1111/j.1365-294X.2005.02426.x"}],"country":"United States","state":"Idaho, Montana","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-111.044156,43.020052],[-111.046689,42.001567],[-112.173352,41.996568],[-112.192976,42.001167],[-112.709375,42.000309],[-113.893261,41.988057],[-114.041723,41.99372],[-114.598267,41.994511],[-114.831077,42.002207],[-115.031783,41.996008],[-117.026222,42.000252],[-117.02678,43.829841],[-117.01077,43.862269],[-116.98294,43.86771],[-116.977332,43.905812],[-116.96247,43.928336],[-116.963666,43.952644],[-116.971835,43.962806],[-116.942944,43.987512],[-116.934485,44.021249],[-116.943361,44.035645],[-116.972504,44.048771],[-116.977351,44.085364],[-116.933704,44.100039],[-116.894309,44.158114],[-116.900103,44.176851],[-116.925392,44.191544],[-116.971675,44.197256],[-116.975905,44.242844],[-117.031862,44.248635],[-117.042283,44.242775],[-117.050057,44.22883],[-117.089503,44.258234],[-117.098531,44.275533],[-117.107673,44.280763],[-117.118018,44.278945],[-117.143394,44.258262],[-117.170342,44.25889],[-117.198147,44.273828],[-117.222647,44.297578],[-117.217843,44.30718],[-117.2055,44.311789],[-117.189842,44.335007],[-117.196149,44.346362],[-117.235117,44.373853],[-117.242675,44.396548],[-117.22698,44.405583],[-117.215072,44.427162],[-117.215573,44.453746],[-117.225076,44.482346],[-117.200237,44.492027],[-117.181583,44.52296],[-117.161033,44.525166],[-117.149242,44.536151],[-117.14293,44.557236],[-117.147934,44.562143],[-117.146032,44.568603],[-117.126009,44.581553],[-117.120522,44.614658],[-117.098221,44.640689],[-117.095868,44.664737],[-117.07912,44.692175],[-117.061799,44.706654],[-117.062273,44.727143],[-117.03827,44.748179],[-117.013802,44.756841],[-116.998903,44.756382],[-116.972902,44.772581],[-116.9368,44.782881],[-116.9308,44.790981],[-116.931099,44.804781],[-116.896249,44.84833],[-116.865338,44.870599],[-116.852427,44.887577],[-116.83199,44.933007],[-116.850737,44.958113],[-116.858313,44.978761],[-116.846103,44.999878],[-116.848037,45.021728],[-116.797329,45.060267],[-116.78371,45.076972],[-116.783537,45.093605],[-116.774847,45.105536],[-116.754643,45.113972],[-116.731216,45.139934],[-116.724205,45.171501],[-116.709536,45.203015],[-116.703607,45.239757],[-116.691388,45.263739],[-116.675587,45.274867],[-116.672733,45.283183],[-116.673793,45.321511],[-116.619057,45.39821],[-116.597447,45.41277],[-116.588195,45.44292],[-116.554829,45.46293],[-116.558803,45.480076],[-116.548676,45.510385],[-116.523638,45.54661],[-116.502756,45.566608],[-116.48297,45.577008],[-116.463635,45.602785],[-116.463504,45.615785],[-116.487894,45.649769],[-116.535396,45.691734],[-116.535698,45.734231],[-116.546643,45.750972],[-116.593004,45.778541],[-116.632032,45.784979],[-116.646342,45.779815],[-116.665344,45.781998],[-116.680139,45.79359],[-116.697192,45.820135],[-116.711822,45.826267],[-116.736268,45.826179],[-116.759787,45.816167],[-116.782676,45.825376],[-116.788329,45.831928],[-116.790151,45.849851],[-116.814142,45.877551],[-116.84355,45.892273],[-116.859795,45.907264],[-116.892935,45.974396],[-116.91868,45.999875],[-116.942656,46.061],[-116.957372,46.075449],[-116.978938,46.080007],[-116.981962,46.084915],[-116.978823,46.095731],[-116.955263,46.102237],[-116.950276,46.123464],[-116.922648,46.160744],[-116.923958,46.17092],[-116.965841,46.203417],[-116.955264,46.23088],[-116.966742,46.256923],[-116.991134,46.276342],[-116.986688,46.296662],[-117.020663,46.314793],[-117.027744,46.338751],[-117.051735,46.343833],[-117.06263,46.352522],[-117.062785,46.365287],[-117.046915,46.379577],[-117.034696,46.418318],[-117.039813,46.425425],[-117.042657,47.760857],[-117.032351,48.999188],[-104.048736,48.999877],[-104.041662,47.862282],[-104.046822,46.000199],[-104.040128,44.999987],[-105.913382,45.000941],[-105.928184,44.993647],[-106.263586,44.993788],[-107.351441,45.001407],[-109.08301,44.99961],[-109.103445,45.005904],[-110.110103,45.003905],[-110.199503,44.996188],[-110.362698,45.000593],[-110.402927,44.99381],[-110.552433,44.992237],[-110.705272,44.992324],[-110.785008,45.002952],[-111.055199,45.001321],[-111.044156,43.020052]]]},\"properties\":{\"name\":\"Idaho\",\"nation\":\"USA  \"}}]}","volume":"14","issue":"2","noUsgsAuthors":false,"publicationDate":"2005-01-10","publicationStatus":"PW","scienceBaseUri":"505a7d9ee4b0c8380cd7a068","contributors":{"authors":[{"text":"Funk, W.C.","contributorId":29934,"corporation":false,"usgs":true,"family":"Funk","given":"W.C.","email":"","affiliations":[],"preferred":false,"id":421496,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Blouin, M.S.","contributorId":77354,"corporation":false,"usgs":true,"family":"Blouin","given":"M.S.","email":"","affiliations":[],"preferred":false,"id":421499,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Corn, P.S.","contributorId":63751,"corporation":false,"usgs":true,"family":"Corn","given":"P.S.","affiliations":[],"preferred":false,"id":421498,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Maxell, B.A.","contributorId":29628,"corporation":false,"usgs":true,"family":"Maxell","given":"B.A.","email":"","affiliations":[],"preferred":false,"id":421495,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Pilliod, D. S.","contributorId":45259,"corporation":false,"usgs":false,"family":"Pilliod","given":"D. S.","affiliations":[],"preferred":false,"id":421497,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Amish, S.","contributorId":90927,"corporation":false,"usgs":true,"family":"Amish","given":"S.","affiliations":[],"preferred":false,"id":421500,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Allendorf, F.W.","contributorId":99937,"corporation":false,"usgs":true,"family":"Allendorf","given":"F.W.","affiliations":[],"preferred":false,"id":421501,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70029384,"text":"70029384 - 2005 - Epidemiology of fractures in people with severe and profound developmental disabilities","interactions":[],"lastModifiedDate":"2012-03-12T17:20:51","indexId":"70029384","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2969,"text":"Osteoporosis International","active":true,"publicationSubtype":{"id":10}},"title":"Epidemiology of fractures in people with severe and profound developmental disabilities","docAbstract":"Fractures are more prevalent among people with severe and profound developmental disabilities than in the general population. In order to characterize the tendency of these people to fracture, and to identify features that may guide the development of preventive strategies, we analyzed fracture epidemiology in people with severe and profound developmental disabilities who lived in a stable environment. Data from a 23-year longitudinal cohort registry of 1434 people with severe and profound developmental disabilities were analyzed to determine the effects of age, gender, mobility, bone fractured, month of fracture, and fracture history upon fracture rates. Eighty-five percent of all fractures involved the extremities. The overall fracture rate increased as mobility increased. In contrast, femoral shaft fracture risk was substantially higher in the least mobile [relative risk (RR), 10.36; 95% confidence interval (CI), 3.29-32.66] compared with the most mobile group. Although the overall fracture rate was not associated with age, the femoral shaft fractures decreased but hand/foot fractures increased with age. Overall fracture risk declined in August and September (RR, 0.70; 95% CI, 0.55-0.89), being especially prominent for tibial/fibular fractures (RR, 0.31; 95% CI, 0.13-0.70). Gender was not a factor in fracture risk. Two primary fracture mechanisms are apparent: one, largely associated with lack of weight-bearing in people with the least mobility, is exemplified by femoral fractures during non-traumatic events as simple as diapering or transfers; the other, probably due to movement- or fall-related trauma, is exemplified by hand/foot fractures in people who ambulate. The fracture experience of people with severe and profound developmental disabilities is unique and, because it differs qualitatively from postmenopausal osteoporosis, may require population-specific methods for assessing risk, for improving bone integrity, and for reduction of falls and accidents. ?? International Osteoporosis Foundation and National Osteoporosis Foundation 2004.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Osteoporosis International","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1007/s00198-004-1708-0","issn":"0937941X","usgsCitation":"Glick, N., Fischer, M., Heisey, D., Leverson, G., and Mann, D., 2005, Epidemiology of fractures in people with severe and profound developmental disabilities: Osteoporosis International, v. 16, no. 4, p. 389-396, https://doi.org/10.1007/s00198-004-1708-0.","startPage":"389","endPage":"396","numberOfPages":"8","costCenters":[],"links":[{"id":210645,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/s00198-004-1708-0"},{"id":237631,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"16","issue":"4","noUsgsAuthors":false,"publicationDate":"2004-08-07","publicationStatus":"PW","scienceBaseUri":"505a0a06e4b0c8380cd5216d","contributors":{"authors":[{"text":"Glick, N.R.","contributorId":10217,"corporation":false,"usgs":true,"family":"Glick","given":"N.R.","email":"","affiliations":[],"preferred":false,"id":422503,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fischer, M.H.","contributorId":54015,"corporation":false,"usgs":true,"family":"Fischer","given":"M.H.","email":"","affiliations":[],"preferred":false,"id":422506,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Heisey, D.M.","contributorId":77496,"corporation":false,"usgs":true,"family":"Heisey","given":"D.M.","email":"","affiliations":[],"preferred":false,"id":422507,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Leverson, G.E.","contributorId":23749,"corporation":false,"usgs":true,"family":"Leverson","given":"G.E.","email":"","affiliations":[],"preferred":false,"id":422505,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Mann, D.C.","contributorId":11403,"corporation":false,"usgs":true,"family":"Mann","given":"D.C.","email":"","affiliations":[],"preferred":false,"id":422504,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70029385,"text":"70029385 - 2005 - Magmatic effects of the Cobb hot spot on the Juan de Fuca Ridge","interactions":[],"lastModifiedDate":"2012-03-12T17:20:51","indexId":"70029385","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2314,"text":"Journal of Geophysical Research B: Solid Earth","active":true,"publicationSubtype":{"id":10}},"title":"Magmatic effects of the Cobb hot spot on the Juan de Fuca Ridge","docAbstract":"The interaction of the Juan de Fuca Ridge with the Cobb hot spot has had a considerable influence on the magmatism of the Axial Segment of the ridge, the second-order segment that overlies the hot spot. In addition to the construction of the large volcanic edifice of Axial Seamount, the Axial Segment has shallow bathymetry and a prevalence of constructional volcanic features along its 100-km length, suggesting that hot spot-derived magmas supplement and oversupply the ridge. Lavas are generally more primitive at Axial Seamount and more evolved in the Axial Segment rift zones, suggesting that fractional crystallization is enhanced with increasing distance from the hot spot because of a reduced magma supply and more rapid cooling. Although the Cobb hot spot is not an isotopically enriched plume, it produces lavas with some distinct geochemical characteristics relative to normal mid-ocean ridge basalt, such as enrichments in alkalis and highly incompatible trace elements, that can be used as tracers to identify the presence and prevalence of the hot spot influence along the ridge. These characteristics are most prominent at Axial Seamount and decline in gradients along the Axial Segment. The physical model that can best explain the geochemical observations is a scenario in which hot spot and mid-ocean ridge basalt (MORB) magmas mix to varying degrees, with the proportions controlled by the depth to the MORB source. Modeling of two-component mixing suggests that MORB is the dominant component in most Axial Segment basalts. Copyright 2005 by the American Geophysical Union.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Geophysical Research B: Solid Earth","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1029/2003JB002767","issn":"01480227","usgsCitation":"Chadwick, J., Perfit, M., Ridley, I., Jonasson, I., Kamenov, G., Chadwick, W., Embley, R., le, R., and Smith, M., 2005, Magmatic effects of the Cobb hot spot on the Juan de Fuca Ridge: Journal of Geophysical Research B: Solid Earth, v. 110, no. 3, p. 1-16, https://doi.org/10.1029/2003JB002767.","startPage":"1","endPage":"16","numberOfPages":"16","costCenters":[],"links":[{"id":210672,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1029/2003JB002767"},{"id":237667,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"110","issue":"3","noUsgsAuthors":false,"publicationDate":"2005-03-05","publicationStatus":"PW","scienceBaseUri":"505a4b43e4b0c8380cd693e6","contributors":{"authors":[{"text":"Chadwick, John","contributorId":13805,"corporation":false,"usgs":false,"family":"Chadwick","given":"John","email":"","affiliations":[],"preferred":false,"id":422508,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Perfit, M.","contributorId":32722,"corporation":false,"usgs":true,"family":"Perfit","given":"M.","email":"","affiliations":[],"preferred":false,"id":422511,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ridley, I.","contributorId":70339,"corporation":false,"usgs":true,"family":"Ridley","given":"I.","email":"","affiliations":[],"preferred":false,"id":422515,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Jonasson, I.","contributorId":25349,"corporation":false,"usgs":true,"family":"Jonasson","given":"I.","email":"","affiliations":[],"preferred":false,"id":422509,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Kamenov, G.","contributorId":42416,"corporation":false,"usgs":true,"family":"Kamenov","given":"G.","affiliations":[],"preferred":false,"id":422513,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Chadwick, W.","contributorId":36352,"corporation":false,"usgs":true,"family":"Chadwick","given":"W.","email":"","affiliations":[],"preferred":false,"id":422512,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Embley, R.","contributorId":43966,"corporation":false,"usgs":true,"family":"Embley","given":"R.","email":"","affiliations":[],"preferred":false,"id":422514,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"le, Roux P.","contributorId":104277,"corporation":false,"usgs":true,"family":"le","given":"Roux P.","affiliations":[],"preferred":false,"id":422516,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Smith, M.","contributorId":32658,"corporation":false,"usgs":false,"family":"Smith","given":"M.","affiliations":[],"preferred":false,"id":422510,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}}
,{"id":70029386,"text":"70029386 - 2005 - Behavior of a chlorinated ethene plume following source-area treatment with Fenton's reagent","interactions":[],"lastModifiedDate":"2018-10-31T09:11:06","indexId":"70029386","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1864,"text":"Ground Water Monitoring and Remediation","active":true,"publicationSubtype":{"id":10}},"title":"Behavior of a chlorinated ethene plume following source-area treatment with Fenton's reagent","docAbstract":"<p><span>Monitoring data collected over a 6‐year period show that a plume of chlorinated ethene–contaminated ground water has contracted significantly following treatment of the contaminant source area using in situ oxidation. Prior to treatment (1998), concentrations of perchloroethene (PCE) exceeded 4500 μg/L in a contaminant source area associated with a municipal landfill in Kings Bay, Georgia. The plume emanating from this source area was characterized by vinyl chloride (VC) concentrations exceeding 800 μg/L. In situ oxidation using Fenton's reagent lowered PCE concentrations in the source area below 100 μg/L, and PCE concentrations have not rebounded above this level since treatment. In the 6 years following treatment, VC concentrations in the plume have decreased significantly. These concentration declines can be attributed to the movement of Fenton's reagent–treated water downgradient through the system, the cessation of a previously installed pump‐and‐treat system, and the significant natural attenuation capacity of this anoxic aquifer. While in situ oxidation briefly decreased the abundance and activity of microorganisms in the source area, this activity rebounded in &lt;6 months. Nevertheless, the shift from sulfate‐reducing to Fe(III)‐reducing conditions induced by Fenton's treatment may have decreased the efficiency of reductive dechlorination in the injection zone. The results of this study indicate that source‐area removal actions, particularly when applied to ground water systems that have significant natural attenuation capacity, can be effective in decreasing the areal extent and contaminant concentrations of chlorinated ethene plumes.</span></p>","language":"English","publisher":"Wiley","doi":"10.1111/j.1745-6592.2005.0020.x","issn":"10693629","usgsCitation":"Chapelle, F.H., Bradley, P., and Casey, C., 2005, Behavior of a chlorinated ethene plume following source-area treatment with Fenton's reagent: Ground Water Monitoring and Remediation, v. 25, no. 2, p. 131-141, https://doi.org/10.1111/j.1745-6592.2005.0020.x.","productDescription":"11 p.","startPage":"131","endPage":"141","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":237668,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":210673,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1111/j.1745-6592.2005.0020.x"}],"volume":"25","issue":"2","noUsgsAuthors":false,"publicationDate":"2005-05-27","publicationStatus":"PW","scienceBaseUri":"5059f09fe4b0c8380cd4a7f9","contributors":{"authors":[{"text":"Chapelle, F. H.","contributorId":101697,"corporation":false,"usgs":true,"family":"Chapelle","given":"F.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":422519,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bradley, P. M. 0000-0001-7522-8606","orcid":"https://orcid.org/0000-0001-7522-8606","contributorId":29465,"corporation":false,"usgs":true,"family":"Bradley","given":"P. M.","affiliations":[],"preferred":false,"id":422518,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Casey, C.C.","contributorId":10206,"corporation":false,"usgs":true,"family":"Casey","given":"C.C.","email":"","affiliations":[],"preferred":false,"id":422517,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70029141,"text":"70029141 - 2005 - Spatial-temporal population dynamics across species range: From centre to margin","interactions":[],"lastModifiedDate":"2012-03-12T17:20:48","indexId":"70029141","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2939,"text":"Oikos","active":true,"publicationSubtype":{"id":10}},"title":"Spatial-temporal population dynamics across species range: From centre to margin","docAbstract":"Understanding the boundaries of species' ranges and the variations in population dynamics from the centre to margin of a species' range is critical. This study simulated spatial-temporal patterns of birth and death rates and migration across a species' range in different seasons. Our results demonstrated the importance of dispersal and migration in altering birth and death rates, balancing source and sink habitats, and governing expansion or contraction of species' ranges in changing environments. We also showed that the multiple equilibria of metapopulations across a species' range could be easily broken following climatic changes or physical disturbances either local or regional. Although we refer to our models as describing the population dynamics across whole species' range, they should also apply to small-scale habitats (metapopulations) in which species abundance follows a humped pattern or to any ecosystem or landscape where strong central-marginal (C-M) environmental gradients exist. Conservation of both central and marginal populations would therefore be equally important considerations in making management decisions.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Oikos","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1111/j.0030-1299.2005.13149.x","issn":"00301299","usgsCitation":"Guo, Q., Taper, M., Schoenberger, M., and Brandle, J., 2005, Spatial-temporal population dynamics across species range: From centre to margin: Oikos, v. 108, no. 1, p. 47-57, https://doi.org/10.1111/j.0030-1299.2005.13149.x.","startPage":"47","endPage":"57","numberOfPages":"11","costCenters":[],"links":[{"id":477883,"rank":10000,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://doi.org/10.1111/j.0030-1299.2005.13149.x","text":"External Repository"},{"id":210832,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1111/j.0030-1299.2005.13149.x"},{"id":237866,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"108","issue":"1","noUsgsAuthors":false,"publicationDate":"2004-12-07","publicationStatus":"PW","scienceBaseUri":"505b94c1e4b08c986b31ac2e","contributors":{"authors":[{"text":"Guo, Q.","contributorId":67039,"corporation":false,"usgs":true,"family":"Guo","given":"Q.","email":"","affiliations":[],"preferred":false,"id":421493,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Taper, M.","contributorId":20966,"corporation":false,"usgs":true,"family":"Taper","given":"M.","email":"","affiliations":[],"preferred":false,"id":421492,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Schoenberger, M.","contributorId":19515,"corporation":false,"usgs":true,"family":"Schoenberger","given":"M.","email":"","affiliations":[],"preferred":false,"id":421491,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Brandle, J.","contributorId":70575,"corporation":false,"usgs":true,"family":"Brandle","given":"J.","affiliations":[],"preferred":false,"id":421494,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70029396,"text":"70029396 - 2005 - Thiamine status in adult salmonines in the Great Lakes","interactions":[],"lastModifiedDate":"2017-01-31T15:01:49","indexId":"70029396","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2177,"text":"Journal of Aquatic Animal Health","active":true,"publicationSubtype":{"id":10}},"title":"Thiamine status in adult salmonines in the Great Lakes","docAbstract":"<p><span>In 1996 and again in 1999, hatchery personnel noted that some Lake Michigan coho salmon </span><i>Oncorhynchus kisutch</i><span> from fall spawning runs on the Platte River weir exhibited abnormal wiggling behavior that was similar to the behavior exhibited by thiamine-deficient Atlantic salmon </span><i>Salmo salar</i><span>, from the Baltic Sea. Samples of eggs or gonads, muscle, and liver from salmon and lake trout </span><i>Salvelinus namaycush</i><span> exhibiting abnormal behaviors were collected to determine the extent to which the behaviors were related to a thiamine deficiency. We compared these values with those found in normally behaving fish that produced offspring with high embryonic survival. In all adult fish exhibiting abnormal behavior, tissue residues of thiamine were among the lowest observed in the Great Lakes. Where embryonic survival was assessed, abnormal adult behavior was also associated with very high levels of offspring mortality due to early mortality syndrome. While the overall ecological significance remains to be determined, it appears that adult fish also exhibit neurological dysfunction and mortality associated with thiamine deficiency.</span></p>","language":"English","publisher":"Taylor & Francis","doi":"10.1577/H04-059.1","issn":"08997659","usgsCitation":"Brown, S., Honeyfield, D., Hnath, J., Wolgamood, M., Marcquenski, S., Fitzsimons, J., and Tillitt, D.E., 2005, Thiamine status in adult salmonines in the Great Lakes: Journal of Aquatic Animal Health, v. 17, no. 1, p. 59-64, https://doi.org/10.1577/H04-059.1.","productDescription":"6 p.","startPage":"59","endPage":"64","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"links":[{"id":237846,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":210814,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1577/H04-059.1"}],"volume":"17","issue":"1","noUsgsAuthors":false,"publicationDate":"2005-03-01","publicationStatus":"PW","scienceBaseUri":"505bb294e4b08c986b3258c9","contributors":{"authors":[{"text":"Brown, S.B.","contributorId":107636,"corporation":false,"usgs":true,"family":"Brown","given":"S.B.","email":"","affiliations":[],"preferred":false,"id":422562,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Honeyfield, D. C. 0000-0003-3034-2047","orcid":"https://orcid.org/0000-0003-3034-2047","contributorId":73136,"corporation":false,"usgs":true,"family":"Honeyfield","given":"D. C.","affiliations":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"preferred":false,"id":422560,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hnath, J.G.","contributorId":34852,"corporation":false,"usgs":true,"family":"Hnath","given":"J.G.","email":"","affiliations":[],"preferred":false,"id":422557,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Wolgamood, M.","contributorId":65790,"corporation":false,"usgs":true,"family":"Wolgamood","given":"M.","email":"","affiliations":[],"preferred":false,"id":422559,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Marcquenski, S.V.","contributorId":11984,"corporation":false,"usgs":true,"family":"Marcquenski","given":"S.V.","affiliations":[],"preferred":false,"id":422556,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Fitzsimons, J.D.","contributorId":50845,"corporation":false,"usgs":true,"family":"Fitzsimons","given":"J.D.","email":"","affiliations":[],"preferred":false,"id":422558,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Tillitt, D. E.","contributorId":83462,"corporation":false,"usgs":true,"family":"Tillitt","given":"D.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":422561,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70029138,"text":"70029138 - 2005 - TREMOR: A wireless MEMS accelerograph for dense arrays","interactions":[],"lastModifiedDate":"2012-03-12T17:20:48","indexId":"70029138","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1436,"text":"Earthquake Spectra","active":true,"publicationSubtype":{"id":10}},"title":"TREMOR: A wireless MEMS accelerograph for dense arrays","docAbstract":"The ability of a strong-motion network to resolve wavefields can be described on three axes: frequency, amplitude, and space. While the need for spatial resolution is apparent, for practical reasons that axis is often neglected. TREMOR is a MEMS-based accelerograph using wireless Internet to minimize lifecycle cost. TREMOR instruments can economically augment traditional ones, residing between them to improve spatial resolution. The TREMOR instrument described here has dynamic range of 96 dB between ??2 g, or 102 dB between ??4 g. It is linear to ???1% of full scale (FS), with a response function effectively shaped electronically. We developed an economical, very low noise, accurate (???1%FS) temperature compensation method. Displacement is easily recovered to 10-cm accuracy at full bandwidth, and better with care. We deployed prototype instruments in Oakland, California, beginning in 1998, with 13 now at mean spacing of ???3 km - one of the most densely instrumented urban centers in the United States. This array is among the quickest in returning (PGA, PGV, Sa) vectors to ShakeMap, ???75 to 100 s. Some 13 events have been recorded. A ShakeMap and an example of spatial variability are shown. Extensive tests of the prototypes for a commercial instrument are described here and in a companion paper. ?? 2005, Earthquake Engineering Research Institute.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Earthquake Spectra","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1193/1.1856534","issn":"87552930","usgsCitation":"Evans, J., Hamstra, R., Kundig, C., Camina, P., and Rogers, J.A., 2005, TREMOR: A wireless MEMS accelerograph for dense arrays: Earthquake Spectra, v. 21, no. 1, p. 91-124, https://doi.org/10.1193/1.1856534.","startPage":"91","endPage":"124","numberOfPages":"34","costCenters":[],"links":[{"id":210804,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1193/1.1856534"},{"id":237830,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"21","issue":"1","noUsgsAuthors":false,"publicationDate":"2005-02-01","publicationStatus":"PW","scienceBaseUri":"505ba392e4b08c986b31fd75","contributors":{"authors":[{"text":"Evans, J.R.","contributorId":50526,"corporation":false,"usgs":true,"family":"Evans","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":421483,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hamstra, R.H. Jr.","contributorId":6246,"corporation":false,"usgs":true,"family":"Hamstra","given":"R.H.","suffix":"Jr.","affiliations":[],"preferred":false,"id":421480,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kundig, C.","contributorId":37948,"corporation":false,"usgs":true,"family":"Kundig","given":"C.","affiliations":[],"preferred":false,"id":421481,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Camina, P.","contributorId":46755,"corporation":false,"usgs":true,"family":"Camina","given":"P.","affiliations":[],"preferred":false,"id":421482,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Rogers, J. A.","contributorId":90721,"corporation":false,"usgs":true,"family":"Rogers","given":"J.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":421484,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70029248,"text":"70029248 - 2005 - Investigating surface water-well interaction using stable isotope ratios of water","interactions":[],"lastModifiedDate":"2018-11-05T08:57:10","indexId":"70029248","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2342,"text":"Journal of Hydrology","active":true,"publicationSubtype":{"id":10}},"title":"Investigating surface water-well interaction using stable isotope ratios of water","docAbstract":"<p><span>Because surface water can be a source of undesirable water quality in a drinking&nbsp;<a title=\"Learn more about water well\" href=\"https://www.sciencedirect.com/topics/earth-and-planetary-sciences/water-well\" data-mce-href=\"https://www.sciencedirect.com/topics/earth-and-planetary-sciences/water-well\">water well</a>, an understanding of the amount of surface water and its travel time to the well is needed to assess a well's vulnerability. Stable&nbsp;<a title=\"Learn more about isotope ratios\" href=\"https://www.sciencedirect.com/topics/earth-and-planetary-sciences/isotope-ratios\" data-mce-href=\"https://www.sciencedirect.com/topics/earth-and-planetary-sciences/isotope-ratios\">isotope ratios</a>&nbsp;of oxygen in&nbsp;<a title=\"Learn more about river water\" href=\"https://www.sciencedirect.com/topics/earth-and-planetary-sciences/river-water\" data-mce-href=\"https://www.sciencedirect.com/topics/earth-and-planetary-sciences/river-water\">river water</a>&nbsp;at the City of La Crosse, Wisconsin, show peak-to-peak&nbsp;<a title=\"Learn more about seasonal variation\" href=\"https://www.sciencedirect.com/topics/earth-and-planetary-sciences/seasonal-variation\" data-mce-href=\"https://www.sciencedirect.com/topics/earth-and-planetary-sciences/seasonal-variation\">seasonal variation</a>&nbsp;greater than 4‰ in 2001 and 2002. This seasonal signal was identified in 7 of 13 city municipal wells, indicating that these 7 wells have appreciable surface water contributions and are potentially vulnerable to contaminants in the surface water. When looking at wells with more than 6 sampling events, a larger variation in&nbsp;</span><i>δ</i><sup>18</sup><span>O compositions correlated with a larger fraction of surface water, suggesting that samples collected for oxygen&nbsp;<a title=\"Learn more about isotopic composition\" href=\"https://www.sciencedirect.com/topics/earth-and-planetary-sciences/isotopic-composition\" data-mce-href=\"https://www.sciencedirect.com/topics/earth-and-planetary-sciences/isotopic-composition\">isotopic composition</a>&nbsp;over time may be useful for identifying the vulnerability to surface water influence even if a local&nbsp;<a title=\"Learn more about meteoric water\" href=\"https://www.sciencedirect.com/topics/earth-and-planetary-sciences/meteoric-water\" data-mce-href=\"https://www.sciencedirect.com/topics/earth-and-planetary-sciences/meteoric-water\">meteoric water</a>&nbsp;line is not available.</span></p><p>A time series of<span>&nbsp;</span><i>δ</i><sup>18</sup><span>O from one of the municipal wells and from a&nbsp;piezometerlocated between the river and the municipal well showed that the travel time of flood water to the municipal well was approximately 2 months; non-flood arrival times were on the order of 9 months. Four independent methods were also used to assess time of travel. Three methods (groundwater temperature arrival times at the intermediate piezometer, virus-culture results, and&nbsp;particle tracking&nbsp;using a numerical&nbsp;groundwater-flow&nbsp;model) yielded flood and non-flood travel times of less than 1 year for this site.&nbsp;Age dating&nbsp;of one groundwater sample using&nbsp;</span><sup>3</sup>H–<sup>3</sup>He methods estimated an age longer than 1 year, but was likely confounded by deviations from piston flow as noted by others. Chlorofluorocarbons and SF<sub>6</sub><span>analyses were not useful at this site due to degradation and contamination, respectively. This work illustrates the utility of stable hydrogen and&nbsp;oxygen isotope ratios&nbsp;of water to determine the contribution and travel time of surface water in groundwater, and demonstrates the importance of using multiple methods to improve estimates for time of travel of 1 year or less.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.jhydrol.2004.07.010","issn":"00221694","usgsCitation":"Hunt, R.J., Coplen, T., Haas, N., Saad, D.A., and Borchardt, M., 2005, Investigating surface water-well interaction using stable isotope ratios of water: Journal of Hydrology, v. 302, no. 1-4, p. 154-172, https://doi.org/10.1016/j.jhydrol.2004.07.010.","productDescription":"19 p.","startPage":"154","endPage":"172","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":237765,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":210748,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.jhydrol.2004.07.010"}],"volume":"302","issue":"1-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3e6ee4b0c8380cd63d99","contributors":{"authors":[{"text":"Hunt, R. J.","contributorId":40164,"corporation":false,"usgs":true,"family":"Hunt","given":"R.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":421909,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Coplen, T.B.","contributorId":34147,"corporation":false,"usgs":true,"family":"Coplen","given":"T.B.","affiliations":[],"preferred":false,"id":421908,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Haas, N.L.","contributorId":33496,"corporation":false,"usgs":true,"family":"Haas","given":"N.L.","email":"","affiliations":[],"preferred":false,"id":421907,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Saad, D. A.","contributorId":85212,"corporation":false,"usgs":true,"family":"Saad","given":"D.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":421911,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Borchardt, M. A.","contributorId":62804,"corporation":false,"usgs":true,"family":"Borchardt","given":"M. A.","affiliations":[],"preferred":false,"id":421910,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70029607,"text":"70029607 - 2005 - Role of reservoir engineering in the assessment of undiscovered oil and gas resources in the National Petroleum Reserve, Alaska","interactions":[],"lastModifiedDate":"2012-03-12T17:20:52","indexId":"70029607","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":701,"text":"American Association of Petroleum Geologists Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Role of reservoir engineering in the assessment of undiscovered oil and gas resources in the National Petroleum Reserve, Alaska","docAbstract":"The geology and reservoir-engineering data were integrated in the 2002 U.S. Geological Survey assessment of the National Petroleum Reserve in Alaska (NPRA). VVhereas geology defined the analog pools and fields and provided the basic information on sizes and numbers of hypothesized petroleum accumulations, reservoir engineering helped develop necessary equations and correlations, which allowed the determination of reservoir parameters for better quantification of in-place petroleum volumes and recoverable reserves. Seismic- and sequence-stratigraphic study of the NPRA resulted in identification of 24 plays. Depth ranges in these 24 plays, however, were typically greater than depth ranges of analog plays for which there were available data, necessitating the need for establishing correlations. The basic parameters required were pressure, temperature, oil and gas formation volume factors, liquid/gas ratios for the associated and nonassociated gas, and recovery factors. Finally, the re sults of U.S. Geological Survey deposit simulation were used in carrying out an economic evaluation, which has been separately published. Copyright ?? 2005. The American Association of Petroleum Geologists. All rights reserved.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"American Association of Petroleum Geologists Bulletin","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1306/04040504055","issn":"01491423","usgsCitation":"Verma, M., and Bird, K.J., 2005, Role of reservoir engineering in the assessment of undiscovered oil and gas resources in the National Petroleum Reserve, Alaska: American Association of Petroleum Geologists Bulletin, v. 89, no. 8, p. 1091-1111, https://doi.org/10.1306/04040504055.","startPage":"1091","endPage":"1111","numberOfPages":"21","costCenters":[],"links":[{"id":237718,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":210711,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1306/04040504055"}],"volume":"89","issue":"8","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505aae67e4b0c8380cd870bc","contributors":{"authors":[{"text":"Verma, M.K.","contributorId":90375,"corporation":false,"usgs":true,"family":"Verma","given":"M.K.","email":"","affiliations":[],"preferred":false,"id":423436,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bird, K. J.","contributorId":57824,"corporation":false,"usgs":false,"family":"Bird","given":"K.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":423435,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70029399,"text":"70029399 - 2005 - Structural evolution of fault zones in sandstone by multiple deformation mechanisms: Moab fault, southeast Utah","interactions":[],"lastModifiedDate":"2012-03-12T17:20:50","indexId":"70029399","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","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":"Structural evolution of fault zones in sandstone by multiple deformation mechanisms: Moab fault, southeast Utah","docAbstract":"Faults in sandstone are frequently composed of two classes of structures: (1) deformation bands and (2) joints and sheared joints. Whereas the former structures are associated with cataclastic deformation, the latter ones represent brittle fracturing, fragmentation, and brecciation. We investigated the distribution of these structures, their formation, and the underlying mechanical controls for their occurrence along the Moab normal fault in southeastern Utah through the use of structural mapping and numerical elastic boundary element modeling. We found that deformation bands occur everywhere along the fault, but with increased density in contractional relays. Joints and sheared joints only occur at intersections and extensional relays. In all locations , joints consistently overprint deformation bands. Localization of joints and sheared joints in extensional relays suggests that their distribution is controlled by local variations in stress state that are due to mechanical interaction between the fault segments. This interpretation is consistent with elastic boundary element models that predict a local reduction in mean stress and least compressive principal stress at intersections and extensional relays. The transition from deformation band to joint formation along these sections of the fault system likely resulted from the combined effects of changes in remote tectonic loading, burial depth, fluid pressure, and rock properties. In the case of the Moab fault, we conclude that the structural heterogeneity in the fault zone is systematically related to the geometric evolution of the fault, the local state of stress associated with fault slip , and the remote loading history. Because the type and distribution of structures affect fault permeability and strength, our results predict systematic variations in these parameters with fault evolution. ?? 2004 Geological Society of America.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Geological Society of America Bulletin","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1130/B25473.1","issn":"00167606","usgsCitation":"Davatzes, N., Eichhubl, P., and Aydin, A., 2005, Structural evolution of fault zones in sandstone by multiple deformation mechanisms: Moab fault, southeast Utah: Geological Society of America Bulletin, v. 117, no. 1-2, p. 135-148, https://doi.org/10.1130/B25473.1.","startPage":"135","endPage":"148","numberOfPages":"14","costCenters":[],"links":[{"id":210840,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1130/B25473.1"},{"id":237882,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"117","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b9be6e4b08c986b31d167","contributors":{"authors":[{"text":"Davatzes, N.C.","contributorId":59219,"corporation":false,"usgs":true,"family":"Davatzes","given":"N.C.","email":"","affiliations":[],"preferred":false,"id":422572,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Eichhubl, P.","contributorId":9060,"corporation":false,"usgs":true,"family":"Eichhubl","given":"P.","email":"","affiliations":[],"preferred":false,"id":422570,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Aydin, A.","contributorId":33898,"corporation":false,"usgs":true,"family":"Aydin","given":"A.","email":"","affiliations":[],"preferred":false,"id":422571,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70029066,"text":"70029066 - 2005 - Supergene destruction of a hydrothermal replacement alunite deposit at Big Rock Candy Mountain, Utah: Mineralogy, spectroscopic remote sensing, stable-isotope, and argon-age evidences","interactions":[],"lastModifiedDate":"2018-01-31T10:31:32","indexId":"70029066","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1213,"text":"Chemical Geology","active":true,"publicationSubtype":{"id":10}},"title":"Supergene destruction of a hydrothermal replacement alunite deposit at Big Rock Candy Mountain, Utah: Mineralogy, spectroscopic remote sensing, stable-isotope, and argon-age evidences","docAbstract":"<p><span>Big Rock Candy Mountain is a prominent center of variegated altered volcanic rocks in west-central Utah. It consists of the eroded remnants of a hypogene alunite deposit that, at ∼21 Ma, replaced intermediate-composition lava flows. The alunite formed in steam-heated conditions above the upwelling limb of a convection cell that was one of at least six spaced at 3- to 4-km intervals around the margin of a monzonite stock. Big Rock Candy Mountain is horizontally zoned outward from an alunite core to respective kaolinite, dickite, and propylite envelopes. The altered rocks are also vertically zoned from a lower pyrite–propylite assemblage upward through assemblages successively dominated by hypogene alunite, jarosite, and hematite, to a flooded silica cap. This hydrothermal assemblage is undergoing natural destruction in a steep canyon downcut by the Sevier River in Marysvale Canyon. Integrated geological, mineralogical, spectroscopic remote sensing using AVIRIS data, Ar radiometric, and stable isotopic studies trace the hypogene origin and supergene destruction of the deposit and permit distinction of primary (hydrothermal) and secondary (weathering) processes. This destruction has led to the formation of widespread supergene gypsum in cross-cutting fractures and as surficial crusts, and to natrojarosite, that gives the mountain its buff coloration along ridges facing the canyon. A small spring, Lemonade Spring, with a pH of 2.6 and containing Ca, Mg, Si, Al, Fe, Mn, Cl, and SO</span><sub>4</sub><span>, also occurs near the bottom of the canyon. The<span>&nbsp;</span></span><sup>40</sup><span>Ar/</span><sup>39</sup><span>Ar age (21.32±0.07 Ma) of the alunite is similar to that for other replacement alunites at Marysvale. However, the age spectrum contains evidence of a 6.6-Ma thermal event that can be related to the tectonic activity responsible for the uplift that led to the downcutting of Big Rock Candy Mountain by the Sevier River. This ∼6.6 Ma event also is present in the age spectrum of supergene natrojarosite forming today, and probably dates the beginning of supergene alteration at Big Rock Candy Mountain. The<span>&nbsp;</span></span><i>δ</i><sup>34</sup><span>S value (11.9‰) of alunite is similar to those for replacement alunite from other deposits in the Marysvale volcanic field. The<span>&nbsp;</span></span><i>δ</i><sup>34</sup><span>S values of natrojarosite (0.7‰ to −1.2‰) are similar to those for aqueous sulfate in Lemonade Spring, but are larger than those in pyrite (0.4‰ to −4.7‰). The<span>&nbsp;</span></span><i>δ</i><sup>34</sup><span>S and<span>&nbsp;</span></span><i>δ</i><sup>18</sup><span>O</span><sub>SO<sub>4</sub></sub><span><span>&nbsp;</span>values of gypsum show an excellent correlation, with values ranging from 15.2‰ to −5.2‰ and 7‰ to −8.2‰, respectively. The stable-isotope data indicate that the aqueous sulfate for gypsum is a mixture derived from the dissolution of hypogene gypsum and alunite, and from the supergene oxidation of pyrite. The aqueous sulfate for the natrojarosite, however, is derived largely from the supergene oxidation of pyrite, with a minor contribution from the dissolution of alunite and gypsum. The exceptional detailed spectral mapping capabilities of AVIRIS led to the recognition of a small amount of jarosite that is probably the top of the steam-heated system that produced the primary hypogene alteration at Big Rock Candy Mountain.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.chemgeo.2004.06.055","usgsCitation":"Cunningham, C.G., Rye, R.O., Rockwell, B.W., Kunk, M.J., and Councell, T.B., 2005, Supergene destruction of a hydrothermal replacement alunite deposit at Big Rock Candy Mountain, Utah: Mineralogy, spectroscopic remote sensing, stable-isotope, and argon-age evidences: Chemical Geology, v. 215, no. 1-4, p. 317-337, https://doi.org/10.1016/j.chemgeo.2004.06.055.","productDescription":"21 p.","startPage":"317","endPage":"337","costCenters":[],"links":[{"id":237788,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Utah","otherGeospatial":"Big Rock Candy Mountain","volume":"215","issue":"1-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b9f57e4b08c986b31e4eb","contributors":{"authors":[{"text":"Cunningham, Charles G.","contributorId":85940,"corporation":false,"usgs":true,"family":"Cunningham","given":"Charles","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":421200,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rye, Robert O. rrye@usgs.gov","contributorId":1486,"corporation":false,"usgs":true,"family":"Rye","given":"Robert","email":"rrye@usgs.gov","middleInitial":"O.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":421198,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rockwell, Barnaby W. 0000-0002-9549-0617 barnabyr@usgs.gov","orcid":"https://orcid.org/0000-0002-9549-0617","contributorId":2195,"corporation":false,"usgs":true,"family":"Rockwell","given":"Barnaby","email":"barnabyr@usgs.gov","middleInitial":"W.","affiliations":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":421199,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Kunk, Michael J. 0000-0003-4424-7825 mkunk@usgs.gov","orcid":"https://orcid.org/0000-0003-4424-7825","contributorId":200968,"corporation":false,"usgs":true,"family":"Kunk","given":"Michael","email":"mkunk@usgs.gov","middleInitial":"J.","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true},{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true}],"preferred":true,"id":421201,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Councell, Terry B.","contributorId":32301,"corporation":false,"usgs":true,"family":"Councell","given":"Terry","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":421197,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70029403,"text":"70029403 - 2005 - Sonoran pronghorn habitat use on landscapes disturbed by military activities","interactions":[],"lastModifiedDate":"2012-03-12T17:20:52","indexId":"70029403","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Sonoran pronghorn habitat use on landscapes disturbed by military activities","docAbstract":"The Sonoran pronghorn (Antilocapra americana sonoriensis) population in the United States declined to ???33 animals in January 2003. Low population numbers and unstable recruitment are concerns for biologists managing this subspecies. We examined habitat use by pronghorn from 1999 to 2002 on a portion of the Barry M. Goldwater Range (BMGR) used for military exercises. We overlaid locations of pronghorn (n= 1,203) on 377 1-km2 blocks within the North (NTAC) and South Tactical Ranges (STAC), BMGR; we classified vegetation associations and disturbance status (e.g., airfields, targets, roads) for each block. Locations of pronghorn were distributed in proportion to vegetation associations on NTAC and STAC. Sightings of pronghorns were biased toward disturbed blocks, with 73% of locations of pronghorn occurring in proximity to mock airfields, high-explosive hills (e.g., targets for live high-explosive bombs and rockets), other targets, and roads. Disturbed landscapes on the BMGR may attract Sonoran pronghorn by creating favorable forage. Habitat manipulations simulating the effects of military disturbances on the landscape (e.g., improved forage) may improve remaining Sonoran pronghorn habitat. Antilocapra americana sonoriensis, Barry M. Goldwater Air Force Range, disturbed habitat, habitat availability, habitat use, military activity, Sonoran pronghorn.","largerWorkTitle":"Wildlife Society Bulletin","language":"English","issn":"00917648","usgsCitation":"Krausman, P., Harris, L., Haas, S., Koenen, K.K., Devers, P., Bunting, D., and Barb, M., 2005, Sonoran pronghorn habitat use on landscapes disturbed by military activities, <i>in</i> Wildlife Society Bulletin, v. 33, no. 1, p. 16-23.","startPage":"16","endPage":"23","numberOfPages":"8","costCenters":[],"links":[{"id":237376,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"33","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b9306e4b08c986b31a239","contributors":{"authors":[{"text":"Krausman, P.R.","contributorId":35525,"corporation":false,"usgs":true,"family":"Krausman","given":"P.R.","affiliations":[],"preferred":false,"id":422609,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Harris, L.K.","contributorId":38351,"corporation":false,"usgs":true,"family":"Harris","given":"L.K.","email":"","affiliations":[],"preferred":false,"id":422610,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Haas, S.K.","contributorId":47966,"corporation":false,"usgs":true,"family":"Haas","given":"S.K.","email":"","affiliations":[],"preferred":false,"id":422612,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Koenen, Kiana K. G.","contributorId":34313,"corporation":false,"usgs":true,"family":"Koenen","given":"Kiana","email":"","middleInitial":"K. G.","affiliations":[],"preferred":false,"id":422608,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Devers, P.","contributorId":44344,"corporation":false,"usgs":true,"family":"Devers","given":"P.","email":"","affiliations":[],"preferred":false,"id":422611,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Bunting, D.","contributorId":53152,"corporation":false,"usgs":true,"family":"Bunting","given":"D.","email":"","affiliations":[],"preferred":false,"id":422613,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Barb, M.","contributorId":20535,"corporation":false,"usgs":true,"family":"Barb","given":"M.","email":"","affiliations":[],"preferred":false,"id":422607,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70029065,"text":"70029065 - 2005 - Timing and development of the Heise volcanic field, Snake River Plain, Idaho, western USA","interactions":[],"lastModifiedDate":"2012-03-12T17:20:47","indexId":"70029065","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","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":"Timing and development of the Heise volcanic field, Snake River Plain, Idaho, western USA","docAbstract":"The Snake River Plain (SRP) developed over the last 16 Ma as a bimodal volcanic province in response to the southwest movement of the North American plate over a fixed melting anomaly. Volcanism along the SRP is dominated by eruptions of explosive high-silica rhyolites and represents some of the largest eruptions known. Basaltic eruptions represent the final stages of volcanism, forming a thin cap above voluminous rhyolitic deposits. Volcanism progressed, generally from west to east, along the plain episodically in successive volcanic fields comprised of nested caldera complexes with major caldera-forming eruptions within a particular field separated by ca. 0.5-1 Ma, similar to, and in continuation with, the present-day Yellowstone Plateau volcanic field. Passage of the North American plate over the melting anomaly at a particular point in time and space was accompanied by uplift, regional tectonism, massive explosive eruptions, and caldera subsidence, and followed by basaltic volcanism and general subsidence. The Heise volcan ic field in the eastern SRP, Idaho, represents an adjacent and slightly older field immediately to the southwest of the Yellowstone Plateau volcanic field. Five large-volume (>0.5 km3) rhyolitic ignimbrites constitute a time-stratigraphic framework of late Miocene to early Pliocene volcanism for the study region. Field relations and high-precision 40Ar/39Ar age determinations establish that four of these regional ignimbrites were erupted from the Heise volcanic field and form the framework of the Heise Group. These are the Blacktail Creek Tuff (6.62 ?? 0.03 Ma), Walcott Tuff (6.27 ?? 0.04 Ma), Conant Creek Tuff (5.51 ?? 0.13 Ma), and Kilgore Tuff (4.45 ?? 0.05 Ma; all errors reported at ?? 2??). The fifth widespread ignimbrite in the regions is the Arbon Valley Tuff Member of the Starlight Formation (10.21 ?? 0.03 Ma), which erupted from a caldera source outside of the Heise volcanic field. These results establish the Conant Creek Tuff as a distinct and widespread ignimbrite in the Heise volcanic field, eliminating former confusion resulting from previous discordant K/Ar and fission-track dates. New 40Ar/39Ar determinations, when combined wi th geochemical, lithologic geophysical, and field data, define the volcanic and tectonic history of the Heise volcanic field and surrounding areas. Volcanic units erupted from the Heise volcanic field also provide temporal control for tectonic events associated with late Cenozoic extension in the Snake Range and with uplift of the Teton Range, Wyoming. In the Snake Range, movement of large (???0.10 km3) slide blocks of Mississippian limestone exposed 50 km to the east of the Heise field occurred between 6.3 and 5.5 Ma and may have been catastrophically triggered by the caldera eruption of the 5.51 ?? 0.13-Ma Conant Creek Tuff. This slide block movement of ???300 vertical meters indicates that the Snake Range had significant relief by at least 5.5 Ma. In Jackson Hole, the distribution of outflow facies of the 4.45 ?? 0.05-Ma Kilgore caldera in the Heise volcanic field on the eastern SRP indicates that the northern Teton Range was not a significant topographic feature at this time. ?? 2005 Geological Society of America.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Geological Society of America Bulletin","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1130/B25519.1","issn":"00167606","usgsCitation":"Morgan, L.A., and McIntosh, W.C., 2005, Timing and development of the Heise volcanic field, Snake River Plain, Idaho, western USA: Geological Society of America Bulletin, v. 117, no. 3-4, p. 288-306, https://doi.org/10.1130/B25519.1.","startPage":"288","endPage":"306","numberOfPages":"19","costCenters":[],"links":[{"id":210738,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1130/B25519.1"},{"id":237755,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"117","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb3e4e4b08c986b32604e","contributors":{"authors":[{"text":"Morgan, L. A.","contributorId":16350,"corporation":false,"usgs":true,"family":"Morgan","given":"L.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":421195,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McIntosh, W. C.","contributorId":68039,"corporation":false,"usgs":true,"family":"McIntosh","given":"W.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":421196,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70029525,"text":"70029525 - 2005 - Population structure of the African Clawed Frog (Xenopus laevis) in maize-growing areas with atrazine application versus non-maize-growing areas in South Africa","interactions":[],"lastModifiedDate":"2013-02-24T07:23:57","indexId":"70029525","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":671,"text":"African Journal of Herpetology","active":true,"publicationSubtype":{"id":10}},"title":"Population structure of the African Clawed Frog (Xenopus laevis) in maize-growing areas with atrazine application versus non-maize-growing areas in South Africa","docAbstract":"The herbicide atrazine has been suggested to cause gonadal deformities in frogs and could possibly impact on reproduction. Since the early 1960s, atrazine has been used in large amounts in maize production areas of South Africa. These areas overlap with populations of the African Clawed Frog (Xenopus laevis) that has a wide distribution in southern Africa and is found in most water-bodies including those where atrazine residues are detected. The aim of this study was to compare various attributes of individual- and population-level responses of X. laevis from maize-growing and non-maize-growing areas. Xenopus laevis were studied in three reference and five maize-growing sites. Sex ratio, snout-vent length, body-mass and age profiles were found to be similar for populations in maize-growing and non-maize-growing areas. Our mark-recapture data indicated that all sites had robust populations. There were no significant relationships between exposure to atrazine and any of the parameters investigated in populations of X. laevis.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"African Journal of Herpetology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1080/21564574.2005.9635518","issn":"04416651","usgsCitation":"Du Preez, L., Solomon, K., Carr, J., Giesy, J., Gross, T., Kendall, R., Smith, E., Van Der Kraak, G.L., and Weldon, C., 2005, Population structure of the African Clawed Frog (Xenopus laevis) in maize-growing areas with atrazine application versus non-maize-growing areas in South Africa: African Journal of Herpetology, v. 54, no. 1, p. 61-68, https://doi.org/10.1080/21564574.2005.9635518.","startPage":"61","endPage":"68","numberOfPages":"8","costCenters":[],"links":[{"id":268092,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1080/21564574.2005.9635518"},{"id":237567,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"54","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a7da1e4b0c8380cd7a07c","contributors":{"authors":[{"text":"Du Preez, L.H.","contributorId":88552,"corporation":false,"usgs":true,"family":"Du Preez","given":"L.H.","email":"","affiliations":[],"preferred":false,"id":423099,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Solomon, K.R.","contributorId":45432,"corporation":false,"usgs":true,"family":"Solomon","given":"K.R.","email":"","affiliations":[],"preferred":false,"id":423095,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Carr, J.A.","contributorId":106692,"corporation":false,"usgs":true,"family":"Carr","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":423102,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Giesy, J. P.","contributorId":60574,"corporation":false,"usgs":false,"family":"Giesy","given":"J. P.","affiliations":[],"preferred":false,"id":423097,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Gross, T. S.","contributorId":95828,"corporation":false,"usgs":true,"family":"Gross","given":"T. S.","affiliations":[],"preferred":false,"id":423101,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Kendall, R.J.","contributorId":38768,"corporation":false,"usgs":true,"family":"Kendall","given":"R.J.","email":"","affiliations":[],"preferred":false,"id":423094,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Smith, E.E.","contributorId":47154,"corporation":false,"usgs":true,"family":"Smith","given":"E.E.","email":"","affiliations":[],"preferred":false,"id":423096,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Van Der Kraak, G. L.","contributorId":62401,"corporation":false,"usgs":true,"family":"Van Der Kraak","given":"G.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":423098,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Weldon, C.","contributorId":93267,"corporation":false,"usgs":true,"family":"Weldon","given":"C.","email":"","affiliations":[],"preferred":false,"id":423100,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}}
,{"id":70029585,"text":"70029585 - 2005 - Drainage ditches facilitate frog movements in a hostile landscape","interactions":[],"lastModifiedDate":"2012-03-12T17:20:46","indexId":"70029585","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2602,"text":"Landscape Ecology","active":true,"publicationSubtype":{"id":10}},"title":"Drainage ditches facilitate frog movements in a hostile landscape","docAbstract":"Ditches are common in landscapes influenced by agricultural, forestry, and peat mining activities, and their value as corridors remains unassessed. Pond-breeding amphibians can encounter hostile environments when moving between breeding, summering, or hibernation sites, and are likely to benefit from the presence of ditches in the landscape. Within a system consisting of ditch networks in bogs mined for peat in eastern New Brunswick, Canada, I quantified the breeding, survival, and movements of green frogs (Rana clamitans melanota) in drainage ditches and also surveyed peat fields. Frogs rarely ventured on peat fields and most individuals frequented drainage ditches containing water, particularly in late summer. Though frogs did not breed in ditches, their survival rate in ditches was high (88%). Ditches did not hinder frog movements, as frogs moved independently of the current. Results indicate that drainage ditches containing water enable some movements between habitats isolated by peat mining, in contrast to peat surfaces, and suggest they function as amphibian movement corridors. Thus, such drainage ditches may mitigate the effects of peat extraction on amphibian populations. At the very least, these structures provide an alternative to hostile peat surfaces. This study highlights that small-scale corridors are potentially valuable in population dynamics. ?? Springer 2005.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Landscape Ecology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1007/s10980-004-3977-6","issn":"09212973","usgsCitation":"Mazerolle, M., 2005, Drainage ditches facilitate frog movements in a hostile landscape: Landscape Ecology, v. 20, no. 5, p. 579-590, https://doi.org/10.1007/s10980-004-3977-6.","startPage":"579","endPage":"590","numberOfPages":"12","costCenters":[],"links":[{"id":210876,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/s10980-004-3977-6"},{"id":237931,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"20","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a03cee4b0c8380cd50665","contributors":{"authors":[{"text":"Mazerolle, M. J. 0000-0002-0486-0310","orcid":"https://orcid.org/0000-0002-0486-0310","contributorId":12957,"corporation":false,"usgs":true,"family":"Mazerolle","given":"M. J.","affiliations":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"preferred":false,"id":423345,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70029482,"text":"70029482 - 2005 - River nutrient loads and catchment size","interactions":[],"lastModifiedDate":"2012-03-12T17:20:52","indexId":"70029482","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1007,"text":"Biogeochemistry","active":true,"publicationSubtype":{"id":10}},"title":"River nutrient loads and catchment size","docAbstract":"We have used a total of 496 sample sites to calibrate a simple regression model for calculating dissolved inorganic nutrient fluxes via runoff to the ocean. The regression uses the logarithms of runoff and human population as the independent variables and estimates the logarithms of dissolved inorganic nitrogen and phosphorus loading with R 2 values near 0.8. This predictive capability is about the same as has been derived for total nutrient loading with process-based models requiring more detailed information on independent variables. We conclude that population and runoff are robust proxies for the more detailed application, landscape modification, and in-stream processing estimated by more process-based models. The regression model has then been applied to a demonstration data set of 1353 river catchments draining to the sea from the North American continent south of the Canadian border. The geographic extents of these basins were extracted from a 1-km digital elevation model for North America, and both runoff and population were estimated for each basin. Most of the basins (72% of the total) are smaller than 103 km2, and both runoff and population density are higher and more variable among small basins than among larger ones.While total load to the ocean can probably be adequately estimated from large systems only, analysis of the geographic distribution of nutrient loading requires consideration of the small basins, which can exhibit significant hydrologic and demographic heterogeneity between systems over their range even within the same geographic region. High-resolution regional and local analysis is necessary for environmental assessment and management. ?? Springer 2005.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Biogeochemistry","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1007/s10533-004-6320-z","issn":"01682563","usgsCitation":"Smith, S.V., Swaney, D., Buddemeier, R., Scarsbrook, M., Weatherhead, M., Humborg, C., Eriksson, H., and Hannerz, F., 2005, River nutrient loads and catchment size: Biogeochemistry, v. 75, no. 1, p. 83-107, https://doi.org/10.1007/s10533-004-6320-z.","startPage":"83","endPage":"107","numberOfPages":"25","costCenters":[],"links":[{"id":210511,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/s10533-004-6320-z"},{"id":237451,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"75","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505aadb4e4b0c8380cd86f60","contributors":{"authors":[{"text":"Smith, S. V.","contributorId":89284,"corporation":false,"usgs":true,"family":"Smith","given":"S.","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":422926,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Swaney, D.P.","contributorId":68956,"corporation":false,"usgs":true,"family":"Swaney","given":"D.P.","email":"","affiliations":[],"preferred":false,"id":422924,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Buddemeier, R. W.","contributorId":86492,"corporation":false,"usgs":true,"family":"Buddemeier","given":"R. W.","affiliations":[],"preferred":false,"id":422925,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Scarsbrook, M.R.","contributorId":16212,"corporation":false,"usgs":true,"family":"Scarsbrook","given":"M.R.","email":"","affiliations":[],"preferred":false,"id":422919,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Weatherhead, M.A.","contributorId":55198,"corporation":false,"usgs":true,"family":"Weatherhead","given":"M.A.","email":"","affiliations":[],"preferred":false,"id":422922,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Humborg, Christoph","contributorId":43964,"corporation":false,"usgs":true,"family":"Humborg","given":"Christoph","email":"","affiliations":[],"preferred":false,"id":422920,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Eriksson, H.","contributorId":67280,"corporation":false,"usgs":true,"family":"Eriksson","given":"H.","email":"","affiliations":[],"preferred":false,"id":422923,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Hannerz, F.","contributorId":53154,"corporation":false,"usgs":true,"family":"Hannerz","given":"F.","email":"","affiliations":[],"preferred":false,"id":422921,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":70029404,"text":"70029404 - 2005 - Genomic variation of the fibropapilloma-associated marine turtle herpes virus across seven geographic areas and three host species","interactions":[],"lastModifiedDate":"2017-10-04T13:24:06","indexId":"70029404","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2497,"text":"Journal of Virology","active":true,"publicationSubtype":{"id":10}},"title":"Genomic variation of the fibropapilloma-associated marine turtle herpes virus across seven geographic areas and three host species","docAbstract":"<p>Fibropapillomatosis (FP) of marine turtles is an emerging neoplastic disease associated with infection by a novel turtle herpesvirus, fibropapilloma-associated turtle herpesvirus (FPTHV). This report presents 23 kb of the genome of an FPTHV infecting a Hawaiian green turtle (Chelonia mydas). By sequence homology, the open reading frames in this contig correspond to herpes simplex virus genes UL23 through UL36. The order, orientation, and homology of these putative genes indicate that FPTHV is a member of the Alphaherpesvirinae. The UL27-, UL30-, and UL34-homologous open reading frames from FPTHVs infecting nine FP-affected marine turtles from seven geographic areas and three turtle species (C. mydas, Caretta caretta, and Lepidochelys olivacea) were compared. A high degree of nucleotide sequence conservation was found among these virus variants. However, geographic variations were also found: the FPTHVs examined here form four groups, corresponding to the Atlantic Ocean, West pacific, mid-Pacific, and east Pacific. Our results indicate that FPTHV was established in marine turtle populations prior to the emergence of FP as it is currently known.</p>","language":"English","publisher":"American Society for Microbiology","doi":"10.1128/JVI.79.2.1125-1132.2005","issn":"0022538X","usgsCitation":"Greenblatt, R., Quackenbush, S., Casey, R., Rovnak, J., Balazs, G., Work, T.M., Casey, J., and Sutton, C., 2005, Genomic variation of the fibropapilloma-associated marine turtle herpes virus across seven geographic areas and three host species: Journal of Virology, v. 79, no. 2, p. 1125-1132, https://doi.org/10.1128/JVI.79.2.1125-1132.2005.","productDescription":"8 p.","startPage":"1125","endPage":"1132","numberOfPages":"8","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"links":[{"id":477811,"rank":10000,"type":{"id":41,"text":"Open Access External Repository 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