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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 Center","active":true,"usgs":true}],"links":[{"id":313903,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":313902,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.seafwa.org/html/proceedings/index.php?article=3822&key=2004&page=1#details"}],"country":"United 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 \"}}]}","volume":"58","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"568e4926e4b0e7a44bc41a3f","contributors":{"authors":[{"text":"Hill, Jeffrey E.","contributorId":36673,"corporation":false,"usgs":true,"family":"Hill","given":"Jeffrey E.","affiliations":[],"preferred":false,"id":587764,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nico, Leo G. 0000-0002-4488-7737 lnico@usgs.gov","orcid":"https://orcid.org/0000-0002-4488-7737","contributorId":2913,"corporation":false,"usgs":true,"family":"Nico","given":"Leo","email":"lnico@usgs.gov","middleInitial":"G.","affiliations":[{"id":566,"text":"Southeast Ecological Science Center","active":true,"usgs":true}],"preferred":false,"id":587765,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cichra, Charles 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":70156392,"text":"70156392 - 2005 - Global land cover mapping and characterization: present situation and future research priorities","interactions":[],"lastModifiedDate":"2015-08-20T14:57:12","indexId":"70156392","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1753,"text":"Geocarto International","active":true,"publicationSubtype":{"id":10}},"title":"Global land cover mapping and characterization: present situation and future research priorities","docAbstract":"<p><span>The availability and accessibility of global land cover data sets plays an important role in many global change studies. The importance of such science‐based information is also reflected in a number of international, regional, and national projects and programs. Recent developments in earth observing satellite technology, information technology, computer hardware and software, and infrastructure development have helped developed better quality land cover data sets. As a result, such data sets are increasingly becoming available, the user‐base is ever widening, application areas have been expanding, and the potential of many other applications are enormous. Yet, we are far from producing high quality global land cover data sets. This paper examines the progress in the development of digital global land cover data, their availability, and current applications. Problems and opportunities are also explained. The overview sets the stage for identifying future research priorities needed for operational land cover assessment and monitoring.</span></p>","language":"English","publisher":"Taylor & Francis","doi":"10.1080/10106040508542334","usgsCitation":"Giri, C., 2005, Global land cover mapping and characterization: present situation and future research priorities: Geocarto International, v. 20, no. 1, p. 35-42, https://doi.org/10.1080/10106040508542334.","productDescription":"8 p.","startPage":"35","endPage":"42","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":307052,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"20","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"55d6fa33e4b0518e3546bc44","contributors":{"authors":[{"text":"Giri, Chandra cgiri@usgs.gov","contributorId":2403,"corporation":false,"usgs":true,"family":"Giri","given":"Chandra","email":"cgiri@usgs.gov","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":569005,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70184385,"text":"70184385 - 2005 - Pacific volcanoes, mercury contaminated fish, and polynesian taboos","interactions":[],"lastModifiedDate":"2018-10-31T09:48:57","indexId":"70184385","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1257,"text":"Clinical Toxicology","active":true,"publicationSubtype":{"id":10}},"title":"Pacific volcanoes, mercury contaminated fish, and polynesian taboos","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"Taylor & Francis","doi":"10.1081/CLT-200068868","usgsCitation":"Dellinger, J., Hudson, J., Krabbenhoft, D., and Hinano Murphy, M., 2005, Pacific volcanoes, mercury contaminated fish, and polynesian taboos: Clinical Toxicology, v. 43, no. 6, p. 595-595, https://doi.org/10.1081/CLT-200068868.","productDescription":"2 p. ","startPage":"595","endPage":"595","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":477886,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1081/clt-200068868","text":"Publisher Index Page"},{"id":337059,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"43","issue":"6","noUsgsAuthors":false,"publicationDate":"2008-10-07","publicationStatus":"PW","scienceBaseUri":"58c12641e4b014cc3a3d34de","contributors":{"authors":[{"text":"Dellinger, John","contributorId":187671,"corporation":false,"usgs":false,"family":"Dellinger","given":"John","email":"","affiliations":[],"preferred":false,"id":681257,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hudson, Jean","contributorId":187672,"corporation":false,"usgs":false,"family":"Hudson","given":"Jean","email":"","affiliations":[],"preferred":false,"id":681258,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Krabbenhoft, David","contributorId":92538,"corporation":false,"usgs":true,"family":"Krabbenhoft","given":"David","affiliations":[],"preferred":false,"id":681259,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hinano Murphy, M.E.","contributorId":187670,"corporation":false,"usgs":false,"family":"Hinano Murphy","given":"M.E.","email":"","affiliations":[],"preferred":false,"id":681260,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70194195,"text":"70194195 - 2005 - Enhancing the value of the Breeding Bird Survey: Repy to Sauer et al (2005)","interactions":[],"lastModifiedDate":"2017-11-17T10:22:09","indexId":"70194195","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2508,"text":"Journal of Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"Enhancing the value of the Breeding Bird Survey: Repy to Sauer et al (2005)","docAbstract":"<p><a class=\"ref\" onclick=\"popRef2('i0022-541X-69-4-1327-Bart2','','','' ); return false;\">Bart et al (2004<i>a</i>)</a> proposed several approaches for enhancing the considerable value of the Breeding Bird Survey (BBS). <a class=\"ref\" onclick=\"popRef2('i0022-541X-69-4-1327-Sauer2','','','' ); return false;\">Sauer et al. (2005)</a> critiqued some of these approaches, and emphasized alternative goals for the survey. We agree with many of the suggestions of <a class=\"ref\" onclick=\"popRef2('i0022-541X-69-4-1327-Sauer2','','','' ); return false;\">Sauer et al. (2005)</a>; notably that multispecies, large-scale surveys such as the BBS are most valuable for bird conservation if they achieve multiple objectives. Nevertheless, we strongly assert that estimation of long-term trends is of fundamental importance for identifying important conservation issues and determining which species represent priorities for conservation efforts, as has been repeatedly demonstrated in the past. We are confident that our recommendations for enhancing the ability of the BBS to detect trends—reducing bias, explicitly recognizing that all bias cannot be eliminated, and increasing sample size in poorly covered areas—can only enhance, and not detract from, the value of the BBS for other purposes.</p>","language":"English","publisher":"The Wildlife Society","doi":"10.2193/0022-541X(2005)69[1327:ETVOTB]2.0.CO;2","usgsCitation":"Francis, C.M., Bart, J., Dunn, E.H., Burnham, K.P., and Ralph, C.J., 2005, Enhancing the value of the Breeding Bird Survey: Repy to Sauer et al (2005): Journal of Wildlife Management, v. 69, no. 4, p. 1327-1332, https://doi.org/10.2193/0022-541X(2005)69[1327:ETVOTB]2.0.CO;2.","startPage":"1327","endPage":"1332","costCenters":[{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true}],"links":[{"id":349048,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"69","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5a611697e4b06e28e9c258ef","contributors":{"authors":[{"text":"Francis, Charles M.","contributorId":195680,"corporation":false,"usgs":false,"family":"Francis","given":"Charles","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":722596,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bart, Jonathan jon_bart@usgs.gov","contributorId":57025,"corporation":false,"usgs":true,"family":"Bart","given":"Jonathan","email":"jon_bart@usgs.gov","affiliations":[{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true}],"preferred":false,"id":722597,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dunn, Erica H.","contributorId":35841,"corporation":false,"usgs":false,"family":"Dunn","given":"Erica","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":722598,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Burnham, Kenneth P.","contributorId":95025,"corporation":false,"usgs":true,"family":"Burnham","given":"Kenneth","email":"","middleInitial":"P.","affiliations":[{"id":189,"text":"Colorado Cooperative Fish and Wildlife Research Unit","active":false,"usgs":true}],"preferred":false,"id":722599,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Ralph, C. John","contributorId":71284,"corporation":false,"usgs":true,"family":"Ralph","given":"C.","email":"","middleInitial":"John","affiliations":[],"preferred":false,"id":722600,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70029341,"text":"70029341 - 2005 - Using chaotic forcing to detect damage in a structure","interactions":[],"lastModifiedDate":"2020-06-19T20:46:58.652525","indexId":"70029341","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1206,"text":"Chaos","active":true,"publicationSubtype":{"id":10}},"title":"Using chaotic forcing to detect damage in a structure","docAbstract":"In this work we develop a numerical test for Holder continuity and apply it and another test for continuity to the difficult problem of detecting damage in structures. We subject a thin metal plate with incremental damage to the plate changes, its filtering properties, and therefore the phase space trajectories of the response chaotic excitation of various bandwidths. Damage to the plate changes its filtering properties and therefore the phase space of the response. Because the data are multivariate (the plate is instrumented with multiple sensors) we use a singular value decomposition of the set of the output time series to reduce the embedding dimension of the response time series. We use two geometric tests to compare an attractor reconstructed from data from an undamaged structure to that reconstructed from data from a damaged structure. These two tests translate to testing for both generalized and differentiable synchronization between responses. We show loss of synchronization of responses with damage to the structure.","language":"English","publisher":"American Institute of Physics","publisherLocation":"Woodbury, N.Y.","doi":"10.1063/1.1903203","issn":"10541500","usgsCitation":"Moniz, L., Nichols, J., Trickey, S., Seaver, M., Pecora, D., and Pecora, L., 2005, Using chaotic forcing to detect damage in a structure: Chaos, v. 15, 023106, 10 p., https://doi.org/10.1063/1.1903203.","productDescription":"023106, 10 p.","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":237556,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"15","noUsgsAuthors":false,"publicationDate":"2005-05-11","publicationStatus":"PW","scienceBaseUri":"505bc03be4b08c986b329fdc","contributors":{"authors":[{"text":"Moniz, L.","contributorId":92783,"corporation":false,"usgs":true,"family":"Moniz","given":"L.","email":"","affiliations":[],"preferred":false,"id":422337,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nichols, J.","contributorId":105906,"corporation":false,"usgs":true,"family":"Nichols","given":"J.","email":"","affiliations":[],"preferred":false,"id":422338,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Trickey, S.","contributorId":6652,"corporation":false,"usgs":true,"family":"Trickey","given":"S.","email":"","affiliations":[],"preferred":false,"id":422333,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Seaver, M.","contributorId":73000,"corporation":false,"usgs":true,"family":"Seaver","given":"M.","email":"","affiliations":[],"preferred":false,"id":422336,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Pecora, D.","contributorId":22136,"corporation":false,"usgs":true,"family":"Pecora","given":"D.","email":"","affiliations":[],"preferred":false,"id":422334,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Pecora, L.","contributorId":49972,"corporation":false,"usgs":true,"family":"Pecora","given":"L.","email":"","affiliations":[],"preferred":false,"id":422335,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70027739,"text":"70027739 - 2005 - Part 1: Vadose-zone column studies of toluene (enhanced bioremediation) in a shallow unconfined aquifer","interactions":[],"lastModifiedDate":"2018-10-31T09:37:31","indexId":"70027739","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3728,"text":"Water, Air, & Soil Pollution","onlineIssn":"1573-2932","printIssn":"0049-6979","active":true,"publicationSubtype":{"id":10}},"title":"Part 1: Vadose-zone column studies of toluene (enhanced bioremediation) in a shallow unconfined aquifer","docAbstract":"<p class=\"Para\">The objectives of the laboratory study described in this paper were (1) to determine the effectiveness of four nutrient solutions and a control in stimulating the microbial degradation of toluene in the unsaturated zone as an alternative to bioremediation methodologies such as air sparging,<span>&nbsp;</span><i class=\"EmphasisTypeItalic \">in situ</i><span>&nbsp;</span>vitrification, or others (Part I), and (2) to compare the effectiveness of the addition of the most effective nutrient solution from Part I (modified Hoagland type, nitrate-rich) and hydrogen peroxide (H<sub>2</sub>O<sub>2</sub>) on microbial degradation of toluene for repeated, simulated spills in the unsaturated zone (Part II).</p><p class=\"Para\">For Part 1, fifteen columns (30-cm diameter by 150-cm height), packed with air-dried, 0.25-mm, medium-fine sand, were prepared to simulate shallow unconfined aquifer conditions. Toluene (10 mL) was added to the surface of each column, and soil solution and soil gas samples were collected from the columns every third day for 21 days. On day 21, a second application of toluene (10 mL) was made, and the experiment was run for another 21 days. Solution 4 was the most effective for microbial degradation in Part I. For Part II, three columns were designated nutrient-rich 3-day toluene columns and received toluene injections every 3 days; three columns were designated as nutrient-rich 7-day columns and received toluene injections every 7 days; and two columns were used as controls to which no nutrient was added.</p><p class=\"Para\">As measured by CO<sub>2</sub><span>&nbsp;</span>respiration, the initial benefits for aerobic organisms from the O<sub>2</sub>enhancement were sustained by the bacteria for only a short period of time (about 8 days). Degradation benefits from the nutrient solution were sustained throughout the experiment.</p><p class=\"Para\">The O<sub>2</sub><span>&nbsp;</span>and nutrient-enhanced columns degraded significantly more toluene than the control columns when simulating repeated spills onto the unsaturated zone, and demonstrated a potentially effective<span>&nbsp;</span><i class=\"EmphasisTypeItalic \">in situ</i><span>&nbsp;</span>bioremediation technology when used immediately or within days after a spill. The combined usage of H<sub>2</sub>O<sub>2</sub><span>&nbsp;</span>and nitrate-rich nutrients served to effectively maximize natural aerobic and anaerobic metabolic processes that biodegrade hydrocarbons in petroleum-contaminated media. Applications of this technology in the field may offer economical advantages to other, more intrusive abatement technologies.</p>","language":"English","publisher":"Springer","doi":"10.1007/s11270-005-1486-0","issn":"00496979","usgsCitation":"Tindall, J., Friedel, M., Szmajter, R., and Cuffin, S., 2005, Part 1: Vadose-zone column studies of toluene (enhanced bioremediation) in a shallow unconfined aquifer: Water, Air, & Soil Pollution, v. 168, no. 1-4, p. 325-357, https://doi.org/10.1007/s11270-005-1486-0.","productDescription":"33 p.","startPage":"325","endPage":"357","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":238312,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":211118,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/s11270-005-1486-0"}],"volume":"168","issue":"1-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a7518e4b0c8380cd779ae","contributors":{"authors":[{"text":"Tindall, J.A.","contributorId":25711,"corporation":false,"usgs":true,"family":"Tindall","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":415012,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Friedel, M.J.","contributorId":90823,"corporation":false,"usgs":true,"family":"Friedel","given":"M.J.","email":"","affiliations":[],"preferred":false,"id":415014,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Szmajter, R.J.","contributorId":87573,"corporation":false,"usgs":true,"family":"Szmajter","given":"R.J.","affiliations":[],"preferred":false,"id":415013,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Cuffin, S.M.","contributorId":6898,"corporation":false,"usgs":true,"family":"Cuffin","given":"S.M.","affiliations":[],"preferred":false,"id":415011,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70027909,"text":"70027909 - 2005 - Evidence for size-selective mortality after the first summer of ocean growth by pink salmon","interactions":[],"lastModifiedDate":"2012-03-12T17:20:46","indexId":"70027909","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3624,"text":"Transactions of the American Fisheries Society","active":true,"publicationSubtype":{"id":10}},"title":"Evidence for size-selective mortality after the first summer of ocean growth by pink salmon","docAbstract":"Pink salmon Onchorhynchus gorbuscha with identifiable thermal otolith marks from Prince William Sound hatchery release groups during 2001 were used to test the hypothesis that faster-growing fish during their first summer in the ocean had higher survival rates than slower-growing fish. Marked juvenile pink salmon were sampled monthly in Prince William Sound and the Gulf of Alaska, and adults that survived to maturity were recovered at hatchery release sites the following year. Surviving fish exhibited significantly wider circuli spacing on the region of the scale formed during early marine residence than did juveniles collected at sea during their first ocean summer, indicating that marine survival after the first growing season was related to increases in early marine growth. At the same circuli, a significantly larger average scale radius for returning adults than for juveniles from the same hatchery would suggest that larger, faster-growing juveniles had a higher survival rate and that significant size-selective mortality occurred after the juveniles were sampled. Growth patterns inferred from intercirculi spacing on scales varied among hatchery release groups, suggesting that density-dependent processes differed among release groups and occurred across Prince William Sound and the coastal Gulf of Alaska. These observations support other studies that have found that larger, faster-growing fish are more likely to survive until maturity. ?? Copyright by the American Fisheries Society 2005.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Transactions of the American Fisheries Society","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1577/T05-054.1","issn":"00028487","usgsCitation":"Moss, J., Beauchamp, D., Cross, A., Myers, K., Farley, E.V., Murphy, J., and Helle, J., 2005, Evidence for size-selective mortality after the first summer of ocean growth by pink salmon: Transactions of the American Fisheries Society, v. 134, no. 5, p. 1313-1322, https://doi.org/10.1577/T05-054.1.","startPage":"1313","endPage":"1322","numberOfPages":"10","costCenters":[],"links":[{"id":211079,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1577/T05-054.1"},{"id":238252,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"134","issue":"5","noUsgsAuthors":false,"publicationDate":"2011-01-09","publicationStatus":"PW","scienceBaseUri":"505a0d51e4b0c8380cd52f4b","contributors":{"authors":[{"text":"Moss, J.H.","contributorId":38772,"corporation":false,"usgs":true,"family":"Moss","given":"J.H.","email":"","affiliations":[],"preferred":false,"id":415752,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Beauchamp, D.A.","contributorId":54397,"corporation":false,"usgs":true,"family":"Beauchamp","given":"D.A.","email":"","affiliations":[],"preferred":false,"id":415753,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cross, A.D.","contributorId":71381,"corporation":false,"usgs":true,"family":"Cross","given":"A.D.","email":"","affiliations":[],"preferred":false,"id":415754,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Myers, K.W.","contributorId":36725,"corporation":false,"usgs":true,"family":"Myers","given":"K.W.","email":"","affiliations":[],"preferred":false,"id":415751,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Farley, Edward V. Jr.","contributorId":108313,"corporation":false,"usgs":true,"family":"Farley","given":"Edward","suffix":"Jr.","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":415756,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Murphy, J.M.","contributorId":84760,"corporation":false,"usgs":true,"family":"Murphy","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":415755,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Helle, J.H.","contributorId":33522,"corporation":false,"usgs":true,"family":"Helle","given":"J.H.","email":"","affiliations":[],"preferred":false,"id":415750,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70029338,"text":"70029338 - 2005 - Rapid differentiation of refined fuels using negative electrospray ionization/mass spectrometry","interactions":[],"lastModifiedDate":"2012-03-12T17:20:50","indexId":"70029338","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Rapid differentiation of refined fuels using negative electrospray ionization/mass spectrometry","docAbstract":"An application of electrospray ionization/mass spectrometry for identification of various commercially refined fuels using the unique signature of polar components, was investigated. The samples were analyzed by mass spectrometry using negative electrospray on an Agilent Series 1100 liquid chromatograph/mass spectrometer. These analysis were applied to hydrocarbon samples from a large, long-term fuel spill which were taken from the subsurface and different extent of biodegradation or weathering. The technique provided rapid identification of hydrocarbons released into the environment because these polar compounds are unique in different fuels.","largerWorkTitle":"American Chemical Society, Division of Petroleum Chemistry, Preprints","language":"English","issn":"05693799","usgsCitation":"Rostad, C., and Hostettler, F., 2005, Rapid differentiation of refined fuels using negative electrospray ionization/mass spectrometry, <i>in</i> American Chemical Society, Division of Petroleum Chemistry, Preprints, v. 50, no. 3, p. 286-287.","startPage":"286","endPage":"287","numberOfPages":"2","costCenters":[],"links":[{"id":237517,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"50","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a94d6e4b0c8380cd8164d","contributors":{"authors":[{"text":"Rostad, C.E.","contributorId":50939,"corporation":false,"usgs":true,"family":"Rostad","given":"C.E.","email":"","affiliations":[],"preferred":false,"id":422323,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hostettler, F. D.","contributorId":99563,"corporation":false,"usgs":true,"family":"Hostettler","given":"F. D.","affiliations":[],"preferred":false,"id":422324,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70027987,"text":"70027987 - 2005 - Hydratools, a MATLAB® based data processing package for Sontek Hydra data","interactions":[],"lastModifiedDate":"2015-05-04T11:14:38","indexId":"70027987","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Hydratools, a MATLAB® based data processing package for Sontek Hydra data","docAbstract":"<p><span>The U.S. Geological Survey (USGS) has developed a set of MATLAB tools to process and convert data collected by Sontek Hydra instruments to netCDF, which is a format used by the USGS to process and archive oceanographic time-series data. The USGS makes high-resolution current measurements within 1.5 meters of the bottom. These data are used in combination with other instrument data from sediment transport studies to develop sediment transport models. Instrument manufacturers provide software which outputs unique binary data formats. Multiple data formats are cumbersome. The USGS solution is to translate data streams into a common data format: netCDF. The Hydratools toolbox is written to create netCDF format files following EPIC conventions, complete with embedded metadata. Data are accepted from both the ADV and the PCADP. The toolbox will detect and remove bad data, substitute other sources of heading and tilt measurements if necessary, apply ambiguity corrections, calculate statistics, return information about data quality, and organize metadata. Standardized processing and archiving makes these data more easily and routinely accessible locally and over the Internet. In addition, documentation of the techniques used in the toolbox provides a baseline reference for others utilizing the data.</span></p>","largerWorkTitle":"Proceedings of the IEEE Working Conference on Current Measurement Technology","conferenceTitle":"IEEE/OES Eight working Conference on Current Measurement Technology: Experimental, Practical and Operational Current and Wave Monitoring Systems and Applications","conferenceDate":"28 June 2005 through 29 June 2005","conferenceLocation":"Southhampton","language":"English","doi":"10.1109/CCM.2005.1506360","usgsCitation":"Martini, M., Lightsom, F.L., Sherwood, C.R., Xu, J., Lacy, J., Ramsey, A., and Horwitz, R., 2005, Hydratools, a MATLAB® based data processing package for Sontek Hydra data, <i>in</i> Proceedings of the IEEE Working Conference on Current Measurement Technology, Southhampton, 28 June 2005 through 29 June 2005, p. 147-151, https://doi.org/10.1109/CCM.2005.1506360.","productDescription":"5 p.","startPage":"147","endPage":"151","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":237115,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a32cbe4b0c8380cd5eaa7","contributors":{"authors":[{"text":"Martini, M.","contributorId":24909,"corporation":false,"usgs":true,"family":"Martini","given":"M.","email":"","affiliations":[],"preferred":false,"id":416042,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lightsom, F. L.","contributorId":36610,"corporation":false,"usgs":true,"family":"Lightsom","given":"F.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":416044,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sherwood, C. R.","contributorId":48235,"corporation":false,"usgs":true,"family":"Sherwood","given":"C.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":416045,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Xu, J.","contributorId":25324,"corporation":false,"usgs":true,"family":"Xu","given":"J.","affiliations":[],"preferred":false,"id":416043,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Lacy, J.R.","contributorId":68508,"corporation":false,"usgs":true,"family":"Lacy","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":416048,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Ramsey, A.","contributorId":58077,"corporation":false,"usgs":true,"family":"Ramsey","given":"A.","email":"","affiliations":[],"preferred":false,"id":416046,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Horwitz, R.","contributorId":60008,"corporation":false,"usgs":true,"family":"Horwitz","given":"R.","email":"","affiliations":[],"preferred":false,"id":416047,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70029346,"text":"70029346 - 2005 - Stable-isotope geochemistry of the Pierina high-sulfidation Au-Ag deposit, Peru: Influence of hydrodynamics on SO42--H2S sulfur isotopic exchange in magmatic-steam and steam-heated environments","interactions":[],"lastModifiedDate":"2012-03-12T17:20:55","indexId":"70029346","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":"Stable-isotope geochemistry of the Pierina high-sulfidation Au-Ag deposit, Peru: Influence of hydrodynamics on SO42--H2S sulfur isotopic exchange in magmatic-steam and steam-heated environments","docAbstract":"The Pierina high-sulfidation Au-Ag deposit formed 14.5 my ago in rhyolite ash flow tuffs that overlie porphyritic andesite and dacite lavas and are adjacent to a crosscutting and interfingering dacite flow dome complex. The distribution of alteration zones indicates that fluid flow in the lavas was largely confined to structures but was dispersed laterally in the tuffs because of a high primary and alteration-induced permeability. The lithologically controlled hydrodynamics created unusual fluid, temperature, and pH conditions that led to complete SO42--H2S isotopic equilibration during the formation of some magmatic-steam and steam-heated alunite, a phenomenon not previously recognized in similar deposits. Isotopic data for early magmatic hydrothermal and main-stage alunite (??34S=8.5??? to 31.7???; ??18 OSO4=4.9??? to 16.5???; ??18 OOH=2.2??? to 14.4???; ??D=-97??? to -39???), sulfides (??34 S=-3.0??? to 4.3???), sulfur (??34S=-1.0??? to 1.1???), and clay minerals (??18O=4.3??? to 12.5???; ??D=-126??? to -81???) are typical of high-sulfidation epithermal deposits. The data imply the following genetic elements for Pierina alteration-mineralization: (1) fluid and vapor exsolution from an I-type magma, (2) wallrock buffering and cooling of slowing rising vapors to generate a reduced (H2S/SO4???6) highly acidic condensate that mixed with meteoric water but retained a magmatic ??34S???S signature of ???1???, (3) SO2 disproportionation to HSO4- and H2S between 320 and 180 ??C, and (4) progressive neutralization of laterally migrating acid fluids to form a vuggy quartz???alunite-quartz??clay???intermediate argillic???propylitic alteration zoning. Magmatic-steam alunite has higher ??34S (8.5??? to 23.2???) and generally lower ??18OSO4 (1.0 to 11.5???), ??18OOH (-3.4 to 5.9???), and ??D (-93 to -77???) values than predicted on the basis of data from similar occurrences. These data and supporting fluid-inclusion gas chemistry imply that the rate of vapor ascent for this environment was unusually slow, which provided sufficient time for the uptake of groundwater and partial to complete SO42--H2S isotopic exchange. The slow steam velocities were likely related to the dispersal of the steam column as it entered the tuffs and possibly to intermediate exsolution rates from magmatic brine. The low ??D values may also partly reflect continuous degassing of the mineralizing magma. Similarly, data for steam-heated alunite (??34S=12.3??? to 27.2???; ??18OSO4=11.7??? to 13.0???; ??18OOH=6.6??? to 9.4???; ??D=-59??? to -42???) are unusual and indicate a strong magmatic influence, relatively high temperatures (140 to 180 ??C, based on ??18 OSO4-OH fractionations), and partial to complete sulfur isotopic exchange between steam-heated sulfate and H2S. Restricted lithologically controlled fluid flow in the host tuffs allowed magmatic condensate to supplant meteoric groundwater at the water table and create the high-temperature low-pH conditions that permitted unusually rapid SO42--H2S isotopic equilibration (50-300 days) and (or) long sulfate residence times for this environment. Late void-filling barite (??34S=7.4??? to 29.7???; ??18OSO4=-0.4??? to 15.1???) and later void-filling goethite (??18O=-11.8??? to 0.2???) document a transition from magmatic condensate to dominantly meteoric water in steam-heated fluids during cooling and collapse of the hydrothermal system. These steam-heated fluids oxidized the top ???300 m of the deposit by leaching sulfides, redistributing metals, and precipitating barite??acanthite??gold and goethite-hematite ??gold. Steam-heated oxidation, rather than weathering, was critical to forming the orebody in that it not only released encapsulated gold but likely enriched the deposit to ore-grade Au concentrations. ?? 2004 Elsevier B.V. All rights reserved.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Chemical Geology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.chemgeo.2004.06.040","issn":"00092541","usgsCitation":"Fifarek, R., and Rye, R.O., 2005, Stable-isotope geochemistry of the Pierina high-sulfidation Au-Ag deposit, Peru: Influence of hydrodynamics on SO42--H2S sulfur isotopic exchange in magmatic-steam and steam-heated environments: Chemical Geology, v. 215, no. 1-4 SPEC. ISS., p. 253-279, https://doi.org/10.1016/j.chemgeo.2004.06.040.","startPage":"253","endPage":"279","numberOfPages":"27","costCenters":[],"links":[{"id":210642,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.chemgeo.2004.06.040"},{"id":237628,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"215","issue":"1-4 SPEC. ISS.","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b968ce4b08c986b31b59b","contributors":{"authors":[{"text":"Fifarek, R.H.","contributorId":50717,"corporation":false,"usgs":true,"family":"Fifarek","given":"R.H.","affiliations":[],"preferred":false,"id":422354,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rye, R. O.","contributorId":66208,"corporation":false,"usgs":true,"family":"Rye","given":"R.","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":422355,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70029335,"text":"70029335 - 2005 - The fundamental thermal niche of adult landlocked striped bass","interactions":[],"lastModifiedDate":"2012-03-12T17:20:50","indexId":"70029335","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3624,"text":"Transactions of the American Fisheries Society","active":true,"publicationSubtype":{"id":10}},"title":"The fundamental thermal niche of adult landlocked striped bass","docAbstract":"Researchers have described the temperatures selected by landlocked striped bass Morone saxatilis in different locales throughout the USA. However, seasonally low concentrations of dissolved oxygen (DO) in many systems prevented striped bass from using the cool waters (<22??C) they may have preferred. In Melton Hill Reservoir, a 92-km-long impoundment on the Clinch River in east Tennessee, 15 adult striped bass were tagged with temperature-sensing radio tags and tracked for an average of 418 d in 1999-2000. Cold, hypolimnetic discharges from an upstream dam and heated discharge from a steam-generating electric facility near the midpoint of this run-of-the-river reservoir provided a broad range of temperatures in most seasons, and hypoxic habitats were uncommon even during stratification. The mean temperature occupied by striped bass varied seasonally (repeated-measures analysis of variance, P < 0.0001) and was highest in summer (17.5??C), intermediate in spring and fall (15.4-16.9??C), and lowest in winter (13.0??C). The mean and modal temperatures occupied during the growing season (May-October 1999) were 17.5??C and 19.0??C, respectively; 30% of the observations were between 9??C and 15??C. These data indicate that the fundamental thermal niche of adult landlocked striped bass may be lower than literature estimates. These results also represent the first unbiased field estimates of the influence of season on the thermal ecology of adult striped bass. The thermal characteristics of habitats considered optimal in habitat suitability index models for adult landlocked striped bass (i.e., 18-24??C) should be revised to include cooler waters. ?? Copyright by the American Fisheries Society 2005.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Transactions of the American Fisheries Society","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1577/T03-204.1","issn":"00028487","usgsCitation":"Bettoli, P., 2005, The fundamental thermal niche of adult landlocked striped bass: Transactions of the American Fisheries Society, v. 134, no. 2, p. 305-314, https://doi.org/10.1577/T03-204.1.","startPage":"305","endPage":"314","numberOfPages":"10","costCenters":[],"links":[{"id":210532,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1577/T03-204.1"},{"id":237479,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"134","issue":"2","noUsgsAuthors":false,"publicationDate":"2011-01-09","publicationStatus":"PW","scienceBaseUri":"505bac2fe4b08c986b32331c","contributors":{"authors":[{"text":"Bettoli, P.W.","contributorId":80606,"corporation":false,"usgs":true,"family":"Bettoli","given":"P.W.","affiliations":[],"preferred":false,"id":422312,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70027910,"text":"70027910 - 2005 - Alternative life histories shape brain gene expression profiles in males of the same population","interactions":[],"lastModifiedDate":"2012-03-12T17:20:46","indexId":"70027910","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3174,"text":"Proceedings of the Royal Society B: Biological Sciences","active":true,"publicationSubtype":{"id":10}},"title":"Alternative life histories shape brain gene expression profiles in males of the same population","docAbstract":"Atlantic salmon (Salmo salar) undergo spectacular marine migrations before homing to spawn in natal rivers. However, males that grow fastest early in life can adopt an alternative 'sneaker' tactic by maturing earlier at greatly reduced size without leaving freshwater. While the ultimate evolutionary causes have been well studied, virtually nothing is known about the molecular bases of this developmental plasticity. We investigate the nature and extent of coordinated molecular changes that accompany such a fundamental transformation by comparing the brain transcription profiles of wild mature sneaker males to age-matched immature males (future large anadromous males) and immature females. Of the ca. 3000 genes surveyed, 15% are differentially expressed in the brains of the two male types. These genes are involved in a wide range of processes, including growth, reproduction and neural plasticity. Interestingly, despite the potential for wide variation in gene expression profiles among individuals sampled in nature, consistent patterns of gene expression were found for individuals of the same reproductive tactic. Notably, gene expression patterns in immature males were different both from immature females and sneakers, indicating that delayed maturation and sea migration by immature males, the 'default' life cycle, may actually result from an active inhibition of development into a sneaker. ?? 2005 The Royal Society.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Proceedings of the Royal Society B: Biological Sciences","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1098/rspb.2005.3125","issn":"09628436","usgsCitation":"Aubin-Horth, N., Landry, C., Letcher, B., and Hofmann, H., 2005, Alternative life histories shape brain gene expression profiles in males of the same population: Proceedings of the Royal Society B: Biological Sciences, v. 272, no. 1573, p. 1655-1662, https://doi.org/10.1098/rspb.2005.3125.","startPage":"1655","endPage":"1662","numberOfPages":"8","costCenters":[],"links":[{"id":477818,"rank":10000,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://www.ncbi.nlm.nih.gov/pmc/articles/1559854","text":"External Repository"},{"id":211080,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1098/rspb.2005.3125"},{"id":238253,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"272","issue":"1573","noUsgsAuthors":false,"publicationDate":"2005-07-14","publicationStatus":"PW","scienceBaseUri":"5059e97ee4b0c8380cd4830a","contributors":{"authors":[{"text":"Aubin-Horth, N.","contributorId":9850,"corporation":false,"usgs":true,"family":"Aubin-Horth","given":"N.","email":"","affiliations":[],"preferred":false,"id":415757,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Landry, C.R.","contributorId":80896,"corporation":false,"usgs":true,"family":"Landry","given":"C.R.","email":"","affiliations":[],"preferred":false,"id":415760,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Letcher, B. H. 0000-0003-0191-5678","orcid":"https://orcid.org/0000-0003-0191-5678","contributorId":48132,"corporation":false,"usgs":true,"family":"Letcher","given":"B.","middleInitial":"H.","affiliations":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"preferred":false,"id":415759,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hofmann, H.A.","contributorId":30432,"corporation":false,"usgs":true,"family":"Hofmann","given":"H.A.","email":"","affiliations":[],"preferred":false,"id":415758,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70027891,"text":"70027891 - 2005 - Helminth records from eleven species of Emoia (Sauria: Scincidae) from Oceania","interactions":[],"lastModifiedDate":"2013-03-20T15:35:46","indexId":"70027891","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2990,"text":"Pacific Science","active":true,"publicationSubtype":{"id":10}},"title":"Helminth records from eleven species of Emoia (Sauria: Scincidae) from Oceania","docAbstract":"As part of an ongoing study of the biogeography of helminth parasites of lizards from Oceania, 53 specimens of Emoia (11 species) were examined, as follows: E. atrocostata, E. boettgeri, E. caerulocauda, E. cyanogaster, E. cyanura, E. impar, E. nigra, E. nigromarginata, E. ponapea, E. sanfordi, E. trossula. One species of Digenea, Paradistomoides gregarium, and six species of Nematoda, Hedruris hanleyae, Maxvachonia chabaudi, Parapharyngodon maplestoni, Physalopteroides arnoensis, Spauligodon gehyrae, and Moaciria sp. indet., were found. These helminths have been reported previously from other lizard species. Seventeen new host records and eight new locality records are reported. ?? 2005 by University of Hawai'i Press All rights reserved.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Pacific Science","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1353/psc.2005.0043","issn":"00308870","usgsCitation":"Goldberg, S., Bursey, C., and Fisher, R., 2005, Helminth records from eleven species of Emoia (Sauria: Scincidae) from Oceania: Pacific Science, v. 59, no. 4, p. 609-614, https://doi.org/10.1353/psc.2005.0043.","startPage":"609","endPage":"614","numberOfPages":"6","costCenters":[],"links":[{"id":477714,"rank":1,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://doi.org/10.1353/psc.2005.0043","text":"External Repository"},{"id":238515,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":269781,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1353/psc.2005.0043"}],"volume":"59","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3048e4b0c8380cd5d4ec","contributors":{"authors":[{"text":"Goldberg, S.R.","contributorId":47975,"corporation":false,"usgs":true,"family":"Goldberg","given":"S.R.","email":"","affiliations":[],"preferred":false,"id":415688,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bursey, C.R.","contributorId":79698,"corporation":false,"usgs":true,"family":"Bursey","given":"C.R.","affiliations":[],"preferred":false,"id":415690,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fisher, Robert N. 0000-0002-2956-3240","orcid":"https://orcid.org/0000-0002-2956-3240","contributorId":51675,"corporation":false,"usgs":true,"family":"Fisher","given":"Robert N.","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":true,"id":415689,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70027809,"text":"70027809 - 2005 - Magmatic unrest beneath Mammoth Mountain, California","interactions":[],"lastModifiedDate":"2019-05-02T11:56:46","indexId":"70027809","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2499,"text":"Journal of Volcanology and Geothermal Research","active":true,"publicationSubtype":{"id":10}},"title":"Magmatic unrest beneath Mammoth Mountain, California","docAbstract":"<p><span>Mammoth Mountain, which stands on the southwest rim of Long Valley caldera in eastern California, last erupted ∼57,000 years BP. Episodic volcanic unrest detected beneath the mountain since late 1979, however, emphasizes that the underlying volcanic system is still active and capable of producing future volcanic eruptions. The unrest symptoms include swarms of small (</span><i>M</i><span>&nbsp;</span><span>≤</span><span>&nbsp;</span><span>3) earthquakes, spasmodic bursts (rapid-fire sequences of brittle-failure earthquakes with overlapping coda), long-period (LP) and very-long-period (VLP) volcanic earthquakes, ground deformation, diffuse emission of magmatic CO</span><sub>2</sub><span>, and fumarole gases with elevated&nbsp;</span><sup>3</sup><span>He/</span><sup>4</sup><span>He ratios. Spatial-temporal relations defined by the multi-parameter monitoring data together with earthquake source mechanisms suggest that this Mammoth Mountain unrest is driven by the episodic release of a volume of CO</span><sub>2</sub><span>-rich hydrous magmatic fluid derived from the upper reaches of a plexus of basaltic dikes and sills at mid-crustal depths (10–20 km). As the mobilized fluid ascends through the brittle–plastic transition zone and into overlying brittle crust, it triggers earthquake swarm activity and, in the case of the prolonged, 11-month-long earthquake swarm of 1989, crustal deformation and the onset of diffuse CO</span><sub>2&nbsp;</sub><span>emissions. Future volcanic activity from this system would most likely involve steam explosions or small-volume, basaltic, strombolian or Hawaiian style eruptions. The impact of such an event would depend critically on vent location and season.</span></p>","largerWorkTitle":"Journal of Volcanology and Geothermal Research","language":"English","doi":"10.1016/j.jvolgeores.2005.03.002","issn":"03770273","usgsCitation":"Hill, D., and Prejean, S., 2005, Magmatic unrest beneath Mammoth Mountain, California: Journal of Volcanology and Geothermal Research, v. 146, no. 4, p. 257-283, https://doi.org/10.1016/j.jvolgeores.2005.03.002.","productDescription":"27 p.","startPage":"257","endPage":"283","numberOfPages":"27","costCenters":[{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true}],"links":[{"id":211100,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.jvolgeores.2005.03.002"},{"id":238283,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Mammoth Mountain","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -119.0544605255127,\n              37.617494852086566\n            ],\n            [\n              -119.00570869445801,\n              37.617494852086566\n            ],\n            [\n              -119.00570869445801,\n              37.64366515163273\n            ],\n            [\n              -119.0544605255127,\n              37.64366515163273\n            ],\n            [\n              -119.0544605255127,\n              37.617494852086566\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"146","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a4b4fe4b0c8380cd69451","contributors":{"authors":[{"text":"Hill, D.P.","contributorId":27432,"corporation":false,"usgs":true,"family":"Hill","given":"D.P.","email":"","affiliations":[],"preferred":false,"id":415308,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Prejean, S.","contributorId":103442,"corporation":false,"usgs":true,"family":"Prejean","given":"S.","email":"","affiliations":[],"preferred":false,"id":415309,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70028820,"text":"70028820 - 2005 - Origin and development of plains-type folds in the mid-continent (United States) during the late Paleozoic","interactions":[],"lastModifiedDate":"2012-03-12T17:20:56","indexId":"70028820","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":"Origin and development of plains-type folds in the mid-continent (United States) during the late Paleozoic","docAbstract":"Plains-type folds are local, subtle anticlines formed in the thin sedimentary package overlying a shallow, crystalline basement on the craton. They are small in areal extent (usually less than 1-3 km 2 [0.4-1.2 mi2]), and their amplitude increases with depth (usually tens of meters), which is mainly the result of differential compaction of sediments (usually clastic units) over tilted, rigid, basement fault blocks. The development of these structural features by continuous but intermittent movement of the basement fault blocks in the late Paleozoic in the United States mid-continent is substantiated by a record of stratigraphic and sedimentological evidence. The recurrent structural movement, which reflects adjustment to external stresses, is expressed by the change in thickness of stratigraphic units over the crest of the fold compared to the flanks. By plotting the change in thickness for different stratigraphic units of anticlines on different fault blocks, it is possible to determine the timing of movement of the blocks that reflect structural adjustment. These readjustments are confirmed by sedimentological evidence, such as convolute, soft-sediment deformation features and small intraformational faults. The stratigraphic interval change in thickness for numerous structures in the Cherokee, Forest City, and Salina basins and on the Nemaha anticline of the mid-continent United States was determined and compared for location and timing of the adjustments. Most of the adjustment occurred during and after time of deposition of the Permian-Pennsylvanian clastic units, which, in turn, reflect tectonic disturbance in adjacent areas, and the largest amount of movement on the plains-type structures occurred on those nearest and semiparallel to major positive features, such as the Nemaha anticline. Depending on the time of origin and development of plains-type folds, they may control the entrapment and occurrence of oil and gas. 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":"10.1306/08050404013","issn":"01491423","usgsCitation":"Merriam, D.F., 2005, Origin and development of plains-type folds in the mid-continent (United States) during the late Paleozoic: American Association of Petroleum Geologists Bulletin, v. 89, no. 1, p. 101-118, https://doi.org/10.1306/08050404013.","startPage":"101","endPage":"118","numberOfPages":"18","costCenters":[],"links":[{"id":209798,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1306/08050404013"},{"id":236515,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"89","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a709ee4b0c8380cd7612e","contributors":{"authors":[{"text":"Merriam, D. F.","contributorId":63175,"corporation":false,"usgs":true,"family":"Merriam","given":"D.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":419881,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70027621,"text":"70027621 - 2005 - Coupled inverse modeling of vadose zone water, heat, and solute transport: Calibration constraints, parameter nonuniqueness, and predictive uncertainty","interactions":[],"lastModifiedDate":"2012-03-12T17:20:48","indexId":"70027621","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":"Coupled inverse modeling of vadose zone water, heat, and solute transport: Calibration constraints, parameter nonuniqueness, and predictive uncertainty","docAbstract":"In this study, an inverse methodology is presented and used to evaluate the effect that calibration of a synthetic artificial recharge model, constrained by different combinations of measurements (pressure head, temperature, and concentration), has on estimated vadose zone model parameter-value nonuniqueness and predictive water, heat, and solute transport uncertainty. Several findings are arrived at following model calibration and predictive analysis. First, composite scaled sensitivities revealed that all calibration measurement combinations contributed to the estimation of 30 water, heat, and solute transport parameters by inverting a set of vadose zone transport equations that were coupled explicitly through dependent variables and implicitly through parameters and fluid properties. Second, despite excellent model quality and perfect match of simulated-to-measured dependent field variables, the limitations in information content of field measurements used to constrain the calibration process promoted correlation among parameters; correlation among parameters promoted parameter nonuniqueness; and parameter nonuniqueness promoted predictive uncertainty. Consequently, simulations by transport models calibrated against field information represent a single realization associated with some quantifiable range of predictive uncertainty. Third, a primary reduction in uncertainty was achieved by increasing the number of calibration-constraint measurements, but reductions in uncertainty appeared restricted implying a practical limit to parameterization detail. Fourth, for a fixed number of measurements, a less prominent reduction in the range of predictive uncertainty could be realized through selective use of measurement types to constrain the calibration process. Therefore, field measurement types used to constrain the calibration process should be matched to target predictions. Fifth, because correlation among parameters contributes to predictive uncertainty, it may be possible to further reduce predictive uncertainty by estimating parameters that also minimize the largest eigenvalue in the normalized eigenvector matrix.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Hydrology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.jhydrol.2005.02.013","issn":"00221694","usgsCitation":"Friedel, M., 2005, Coupled inverse modeling of vadose zone water, heat, and solute transport: Calibration constraints, parameter nonuniqueness, and predictive uncertainty: Journal of Hydrology, v. 312, no. 1-4, p. 148-175, https://doi.org/10.1016/j.jhydrol.2005.02.013.","startPage":"148","endPage":"175","numberOfPages":"28","costCenters":[],"links":[{"id":211045,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.jhydrol.2005.02.013"},{"id":238200,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"312","issue":"1-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059fc89e4b0c8380cd4e2d9","contributors":{"authors":[{"text":"Friedel, M.J.","contributorId":90823,"corporation":false,"usgs":true,"family":"Friedel","given":"M.J.","email":"","affiliations":[],"preferred":false,"id":414401,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70027590,"text":"70027590 - 2005 - Monitoring eruptive activity at Mount St. Helens with TIR image data","interactions":[],"lastModifiedDate":"2019-05-14T08:39:44","indexId":"70027590","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1807,"text":"Geophysical Research Letters","active":true,"publicationSubtype":{"id":10}},"title":"Monitoring eruptive activity at Mount St. Helens with TIR image data","docAbstract":"<p><span>Thermal infrared (TIR) data from the MASTER airborne imaging spectrometer were acquired over Mount St. Helens in Sept and Oct, 2004, before and after the onset of recent eruptive activity. Pre‐eruption data showed no measurable increase in surface temperatures before the first phreatic eruption on Oct 1. MASTER data acquired during the initial eruptive episode on Oct 14 showed maximum temperatures of ∼330°C and TIR data acquired concurrently from a Forward Looking Infrared (FLIR) camera showed maximum temperatures ∼675°C, in narrow (∼1‐m) fractures of molten rock on a new resurgent dome. MASTER and FLIR thermal flux calculations indicated a radiative cooling rate of ∼714 J/m</span><sup>2</sup><span>/s over the new dome, corresponding to a radiant power of ∼24 MW. MASTER data indicated the new dome was dacitic in composition, and digital elevation data derived from LIDAR acquired concurrently with MASTER showed that the dome growth correlated with the areas of elevated temperatures. Low SO</span><sub>2</sub><span>&nbsp;concentrations in the plume combined with sub‐optimal viewing conditions prohibited quantitative measurement of plume SO</span><sub>2</sub><span>. The results demonstrate that airborne TIR data can provide information on the temperature of both the surface and plume and the composition of new lava during eruptive episodes. Given sufficient resources, the airborne instrumentation could be deployed rapidly to a newly‐awakening volcano and provide a means for remote volcano monitoring.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/2005GL024112","issn":"00948276","usgsCitation":"Vaughan, R., Hook, S., Ramsey, M., Realmuto, V., and Schneider, D., 2005, Monitoring eruptive activity at Mount St. Helens with TIR image data: Geophysical Research Letters, v. 32, no. 19, p. 1-4, https://doi.org/10.1029/2005GL024112.","productDescription":"4 p.","startPage":"1","endPage":"4","numberOfPages":"4","costCenters":[{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true}],"links":[{"id":477940,"rank":1,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1029/2005gl024112","text":"Publisher Index Page"},{"id":238236,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Washington","otherGeospatial":"Mount St. Helens","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -122.34649658203124,\n              46.12274903582433\n            ],\n            [\n              -121.98669433593749,\n              46.12274903582433\n            ],\n            [\n              -121.98669433593749,\n              46.337447097476925\n            ],\n            [\n              -122.34649658203124,\n              46.337447097476925\n            ],\n            [\n              -122.34649658203124,\n              46.12274903582433\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"32","issue":"19","noUsgsAuthors":false,"publicationDate":"2005-10-14","publicationStatus":"PW","scienceBaseUri":"505a5da5e4b0c8380cd704de","contributors":{"authors":[{"text":"Vaughan, R.G.","contributorId":44738,"corporation":false,"usgs":true,"family":"Vaughan","given":"R.G.","email":"","affiliations":[],"preferred":false,"id":414269,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hook, S.J.","contributorId":21711,"corporation":false,"usgs":true,"family":"Hook","given":"S.J.","email":"","affiliations":[],"preferred":false,"id":414268,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ramsey, M.S.","contributorId":66475,"corporation":false,"usgs":true,"family":"Ramsey","given":"M.S.","email":"","affiliations":[],"preferred":false,"id":414271,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Realmuto, V.J.","contributorId":60779,"corporation":false,"usgs":true,"family":"Realmuto","given":"V.J.","email":"","affiliations":[],"preferred":false,"id":414270,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Schneider, D.J.","contributorId":12997,"corporation":false,"usgs":true,"family":"Schneider","given":"D.J.","email":"","affiliations":[],"preferred":false,"id":414267,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70027677,"text":"70027677 - 2005 - Rainfall-runoff in the Albuquerque, New Mexico, area: Measurements, analyses and comparisons","interactions":[],"lastModifiedDate":"2012-03-12T17:21:17","indexId":"70027677","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Rainfall-runoff in the Albuquerque, New Mexico, area: Measurements, analyses and comparisons","docAbstract":"Albuquerque, New Mexico, has experienced significant growth over the last 20 years like many other cities in the Southwestern United States. While the US population grew by 37% between the 1970 and 2000 censuses, the growth for Albuquerque was 83%. More people mean more development and increased problems of managing runoff from urbanizing watersheds. The U.S. Geological Survey (USGS) in cooperation with the Albuquerque Arroyo Metropolitan Flood Control Authority (AMAFCA) and the City of Albuquerque has maintained a rainfall-runoff data collection program since 1976. The data from measured precipitation events can be used to verify hydrologic modeling. In this presentation, data from a representative gaged watershed is analyzed and discussed to set the overall framework for the rainfall-runoff process in the Albuquerque area. Of particular interest are the basic relationships between rainfall and watershed runoff response and an analysis of curve numbers as an indicator of runoff function. In urbanized areas, four land treatment types (natural, irrigated lawns, compacted soil, and impervious) are used to define surface infiltration conditions. Rainfall and runoff gage data are used to compare curve number (CN) and initial abstraction/uniform infiltration (IA/INF) techniques in an Albuquerque watershed. The IA/INF method appears to produce superior results over the CN method for the measured rainfall events.","largerWorkTitle":"Proceedings of the 2005 Watershed Management Conference - Managing Watersheds for Human and Natural Impacts: Engineering, Ecological, and Economic Challenges","conferenceTitle":"2005 Watershed Management Conference - Managing Watersheds for Human and Natural Impacts: Engineering, Ecological, and Economic Challenges","conferenceDate":"19 July 2005 through 22 July 2005","conferenceLocation":"Williamsburg, VA","language":"English","isbn":"0784407630","usgsCitation":"Anderson, C., Ward, T., and Kelly, T., 2005, Rainfall-runoff in the Albuquerque, New Mexico, area: Measurements, analyses and comparisons, <i>in</i> Proceedings of the 2005 Watershed Management Conference - Managing Watersheds for Human and Natural Impacts: Engineering, Ecological, and Economic Challenges, Williamsburg, VA, 19 July 2005 through 22 July 2005, p. 1787-1796.","startPage":"1787","endPage":"1796","numberOfPages":"10","costCenters":[],"links":[{"id":238502,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a947be4b0c8380cd8142c","contributors":{"editors":[{"text":"Moglen G.E.","contributorId":128404,"corporation":true,"usgs":false,"organization":"Moglen G.E.","id":536627,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Anderson, C.E.","contributorId":26511,"corporation":false,"usgs":true,"family":"Anderson","given":"C.E.","email":"","affiliations":[],"preferred":false,"id":414687,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ward, T.J.","contributorId":17039,"corporation":false,"usgs":true,"family":"Ward","given":"T.J.","email":"","affiliations":[],"preferred":false,"id":414686,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kelly, T.","contributorId":29993,"corporation":false,"usgs":true,"family":"Kelly","given":"T.","affiliations":[],"preferred":false,"id":414688,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70027674,"text":"70027674 - 2005 - Time-dependent seismic tomography of the Coso geothermal area, 1996-2004","interactions":[],"lastModifiedDate":"2012-03-12T17:21:17","indexId":"70027674","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Time-dependent seismic tomography of the Coso geothermal area, 1996-2004","docAbstract":"The permanent 18-station network of three-component digital seismometers at the seismically active Coso geothermal area, California, provides high-quality microearthquake (MEQ) data that are well suited to investigating temporal variations in structure related to processes within the geothermal reservoir. A preliminary study [Julian, et al., 2003; Julian, et al., 2004] comparing data from 1996 and 2003 found significant variations in the ratio of the seismic wave-speeds, Vp/Vs, at shallow depths over this time interval. This report describes results of a more detailed study of each year from 1996 through 2004.","largerWorkTitle":"Transactions - Geothermal Resources Council","conferenceTitle":"Geothermal Resources Council 2005 Annual Meeting","conferenceDate":"25 September 2005 through 28 September 2005","conferenceLocation":"Reno, NV","language":"English","issn":"01935933","usgsCitation":"Julian, B., and Foulger, G., 2005, Time-dependent seismic tomography of the Coso geothermal area, 1996-2004, <i>in</i> Transactions - Geothermal Resources Council, v. 29, Reno, NV, 25 September 2005 through 28 September 2005, p. 485-488.","startPage":"485","endPage":"488","numberOfPages":"4","costCenters":[],"links":[{"id":238462,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"29","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb3bde4b08c986b325f97","contributors":{"authors":[{"text":"Julian, B.R.","contributorId":101272,"corporation":false,"usgs":true,"family":"Julian","given":"B.R.","email":"","affiliations":[],"preferred":false,"id":414680,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Foulger, G.R.","contributorId":14439,"corporation":false,"usgs":false,"family":"Foulger","given":"G.R.","email":"","affiliations":[],"preferred":false,"id":414679,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70027584,"text":"70027584 - 2005 - Effects of coal-bed methane discharge waters on the vegetation and soil ecosystem in Powder River Basin, Wyoming","interactions":[],"lastModifiedDate":"2018-10-31T10:53:23","indexId":"70027584","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3728,"text":"Water, Air, & Soil Pollution","onlineIssn":"1573-2932","printIssn":"0049-6979","active":true,"publicationSubtype":{"id":10}},"title":"Effects of coal-bed methane discharge waters on the vegetation and soil ecosystem in Powder River Basin, Wyoming","docAbstract":"<p class=\"Para\">Coal-bed methane (CBM) co-produced discharge waters in the Powder River Basin of Wyoming, resulting from extraction of methane from coal seams, have become a priority for chemical, hydrological and biological research during the last few years. Soil and vegetation samples were taken from affected and reference sites (upland elevations and wetted gully) in Juniper Draw to investigate the effects of CBM discharge waters on soil physical and chemical properties and on native and introduced vegetation density and diversity. Results indicate an increase of salinity and sodicity within local soil ecosystems at sites directly exposed to CBM discharge waters. Elevated concentrations of sodium in the soil are correlated with consistent exposure to CBM waters. Clay-loam soils in the study area have a much larger specific surface area than the sandy soils and facilitate a greater sodium adsorption. However, there was no significant relation between increasing water sodium adsorption ratio (SAR) values and increasing sediment SAR values downstream; however, soils exposed to the CBM water ranged from the moderate to severe SAR hazard index. Native vegetation species density was highest at the reference (upland and gully) and CBM affected upland sites. The affected gully had the greatest percent composition of introduced vegetation species. Salt-tolerant species had the greatest richness at the affected gully, implying a potential threat of invasion and competition to established native vegetation. These findings suggest that CBM waters could affect agricultural production operations and long-term water quality.</p><div class=\"KeywordGroup\" lang=\"en\"><br data-mce-bogus=\"1\"></div>","language":"English","publisher":"Springer","doi":"10.1007/s11270-005-0588-z","issn":"00496979","usgsCitation":"Stearns, M., Tindall, J., Cronin, G., Friedel, M., and Bergquist, E., 2005, Effects of coal-bed methane discharge waters on the vegetation and soil ecosystem in Powder River Basin, Wyoming: Water, Air, & Soil Pollution, v. 168, no. 1-4, p. 33-57, https://doi.org/10.1007/s11270-005-0588-z.","productDescription":"25 p.","startPage":"33","endPage":"57","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":238166,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":211023,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/s11270-005-0588-z"}],"country":"United States","state":"Wyoming","otherGeospatial":"Powder River Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -108.87451171875,\n              44.99588261816546\n            ],\n            [\n              -108.43505859374999,\n              44.55916341529182\n            ],\n            [\n              -107.75390625,\n              44.22945656830167\n            ],\n            [\n              -107.60009765625,\n              43.96119063892024\n            ],\n            [\n              -107.46826171874999,\n              43.75522505306928\n            ],\n            [\n              -107.666015625,\n              43.40504748787035\n            ],\n            [\n              -108.25927734375,\n              42.71473218539458\n            ],\n            [\n              -104.56787109374999,\n              42.69858589169842\n            ],\n            [\n              -104.5458984375,\n              44.98034238084973\n            ],\n            [\n              -108.87451171875,\n              44.99588261816546\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"168","issue":"1-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a06b5e4b0c8380cd513a7","contributors":{"authors":[{"text":"Stearns, M.","contributorId":28061,"corporation":false,"usgs":true,"family":"Stearns","given":"M.","email":"","affiliations":[],"preferred":false,"id":414232,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tindall, J.A.","contributorId":25711,"corporation":false,"usgs":true,"family":"Tindall","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":414231,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cronin, G.","contributorId":92044,"corporation":false,"usgs":true,"family":"Cronin","given":"G.","email":"","affiliations":[],"preferred":false,"id":414235,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Friedel, M.J.","contributorId":90823,"corporation":false,"usgs":true,"family":"Friedel","given":"M.J.","email":"","affiliations":[],"preferred":false,"id":414234,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Bergquist, E.","contributorId":43969,"corporation":false,"usgs":true,"family":"Bergquist","given":"E.","email":"","affiliations":[],"preferred":false,"id":414233,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70027904,"text":"70027904 - 2005 - Ordovician conodonts and stratigraphy of the ST. Peter sandstone and glen wood shale, central United States","interactions":[],"lastModifiedDate":"2012-03-12T17:20:46","indexId":"70027904","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1142,"text":"Bulletins of American Paleontology","active":true,"publicationSubtype":{"id":10}},"title":"Ordovician conodonts and stratigraphy of the ST. Peter sandstone and glen wood shale, central United States","docAbstract":"The age of the St. Peter Sandstone in the central and northern Midcontinent has long been considered equivocal because of the general absence of biostratigraphically useful fossils. Conodonts recovered from the St. Peter Sandstone in Iowa, Minnesota, Nebraska, and Kansas for this study help place some age constraints on this renowned formation in its northern and western extent. Faunas from the lower St. Peter include Phragmodus flexuosus, Cahabagnathus sp., and Leptochirognathus sp., and a late Whiterockian (Chazyan) correlation is indicated. Juvenile or immature elements of P. flexuosus from these collections show morphologies trending toward P. cognitus and P. inflexus, and paedomorphic derivation of these latter species is proposed. Diverse assemblages of hyaline forms also occur in the St. Peter strata (Erismodus spp., Erraticodon sp., Curtognathus sp., Coleodus sp., Archeognathus sp., Stereoconus sp., others) along with various albid elements (Plectodina sp., Eoplacognathus sp., others). The overlying Glenwood Shale contains abundant conodonts dominated by Phragmodus cognitus, Erismodus sp., and Chirognathus duodactylus, and the fauna is interpreted as an early Mohawkian (Blackriveran) association. Certain thin shale units in the St. Peter-Glenwood succession represent condensed intervals, in part reflected by their exceptionally high conodont abundances. Some organic-rich phosphatic shale units in the lower St. Peter of western Iowa have produced equivalent yields of tens of thousands of conodonts per kilogram, and many Glenwood Shale samples yield thousands of conodonts per kilogram. Previous depositional models have proposed that the St. Peter is primarily a succession of littoral and nearshore facies forming a broadly diachronous transgressive sheet sand. However, broad-scale diachroneity cannot be demonstrated with available biostratigraphic control. The recognition of condensed marine shale units, phosphorites, ironstones, and pyritic hardgrounds in the western facies tract of the St. Peter Sandstone has necessitated a re-evaluation of previous regional models of St. Peter deposition. The St. Peter is interpreted to be a composite stratigraphic interval deposited during a succession of transgressive-regressive sedimentary cycles. Transgressive episodes in some cycles were marked by offshore sediment condensation or starvation within a stratified seaway.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Bulletins of American Paleontology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"00075779","usgsCitation":"Witzke, B., and Metzger, R., 2005, Ordovician conodonts and stratigraphy of the ST. Peter sandstone and glen wood shale, central United States: Bulletins of American Paleontology, v. 2005, no. 369, p. 53-91.","startPage":"53","endPage":"91","numberOfPages":"39","costCenters":[],"links":[{"id":238182,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"2005","issue":"369","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a6f5fe4b0c8380cd75a66","contributors":{"authors":[{"text":"Witzke, B.J.","contributorId":12976,"corporation":false,"usgs":true,"family":"Witzke","given":"B.J.","affiliations":[],"preferred":false,"id":415732,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Metzger, R.A.","contributorId":103825,"corporation":false,"usgs":true,"family":"Metzger","given":"R.A.","email":"","affiliations":[],"preferred":false,"id":415733,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70029332,"text":"70029332 - 2005 - Testing the generality of a trophic-cascade model for plague","interactions":[],"lastModifiedDate":"2012-03-12T17:20:51","indexId":"70029332","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1443,"text":"EcoHealth","active":true,"publicationSubtype":{"id":10}},"title":"Testing the generality of a trophic-cascade model for plague","docAbstract":"Climate may affect the dynamics of infectious diseases by shifting pathogen, vector, or host species abundance, population dynamics, or community interactions. Black-tailed prairie dogs (Cynomys ludovicianus) are highly susceptible to plague, yet little is known about factors that influence the dynamics of plague epizootics in prairie dogs. We investigated temporal patterns of plague occurrence in black-tailed prairie dogs to assess the generality of links between climate and plague occurrence found in previous analyses of human plague cases. We examined long-term data on climate and plague occurrence in prairie dog colonies within two study areas. Multiple regression analyses revealed that plague occurrence in prairie dogs was not associated with climatic variables in our Colorado study area. In contrast, plague occurrence was strongly associated with climatic variables in our Montana study area. The models with most support included a positive association with precipitation in April-July of the previous year, in addition to a positive association with the number of \"warm\" days and a negative association with the number of \"hot\" days in the same year as reported plague events. We conclude that the timing and magnitude of precipitation and temperature may affect plague occurrence in some geographic areas. The best climatic predictors of plague occurrence in prairie dogs within our Montana study area are quite similar to the best climatic predictors of human plague cases in the southwestern United States. This correspondence across regions and species suggests support for a (temperature-modulated) trophic-cascade model for plague, including climatic effects on rodent abundance, flea abundance, and pathogen transmission, at least in regions that experience strong climatic signals. ?? 2005 EcoHealth Journal Consortium.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"EcoHealth","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1007/s10393-005-3877-5","issn":"16129202","usgsCitation":"Collinge, S., Johnson, W., Ray, C., Matchett, R., Grensten, J., Cully, J., Gage, K., Kosoy, M., Loye, J., and Martin, A., 2005, Testing the generality of a trophic-cascade model for plague: EcoHealth, v. 2, no. 2, p. 102-112, https://doi.org/10.1007/s10393-005-3877-5.","startPage":"102","endPage":"112","numberOfPages":"11","costCenters":[],"links":[{"id":210478,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/s10393-005-3877-5"},{"id":237410,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"2","issue":"2","noUsgsAuthors":false,"publicationDate":"2005-05-05","publicationStatus":"PW","scienceBaseUri":"505ba5d4e4b08c986b320cee","contributors":{"authors":[{"text":"Collinge, S.K.","contributorId":58832,"corporation":false,"usgs":true,"family":"Collinge","given":"S.K.","email":"","affiliations":[],"preferred":false,"id":422298,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Johnson, W.C.","contributorId":68003,"corporation":false,"usgs":true,"family":"Johnson","given":"W.C.","email":"","affiliations":[],"preferred":false,"id":422299,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ray, C.","contributorId":40758,"corporation":false,"usgs":true,"family":"Ray","given":"C.","email":"","affiliations":[],"preferred":false,"id":422296,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Matchett, R.","contributorId":92482,"corporation":false,"usgs":true,"family":"Matchett","given":"R.","email":"","affiliations":[],"preferred":false,"id":422301,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Grensten, J.","contributorId":29196,"corporation":false,"usgs":true,"family":"Grensten","given":"J.","email":"","affiliations":[],"preferred":false,"id":422295,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Cully, J.F. Jr.","contributorId":51041,"corporation":false,"usgs":true,"family":"Cully","given":"J.F.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":422297,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Gage, K.L.","contributorId":107653,"corporation":false,"usgs":true,"family":"Gage","given":"K.L.","email":"","affiliations":[],"preferred":false,"id":422302,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Kosoy, M.Y.","contributorId":78283,"corporation":false,"usgs":true,"family":"Kosoy","given":"M.Y.","email":"","affiliations":[],"preferred":false,"id":422300,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Loye, J.E.","contributorId":9056,"corporation":false,"usgs":true,"family":"Loye","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":422293,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Martin, A.P.","contributorId":12257,"corporation":false,"usgs":true,"family":"Martin","given":"A.P.","email":"","affiliations":[],"preferred":false,"id":422294,"contributorType":{"id":1,"text":"Authors"},"rank":10}]}}
,{"id":70029331,"text":"70029331 - 2005 - Estimation of groundwater consumption by phreatophytes using diurnal water table fluctuations: A saturated‐unsaturated flow assessment","interactions":[],"lastModifiedDate":"2018-04-02T15:45:25","indexId":"70029331","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3722,"text":"Water Resources Research","onlineIssn":"1944-7973","printIssn":"0043-1397","active":true,"publicationSubtype":{"id":10}},"title":"Estimation of groundwater consumption by phreatophytes using diurnal water table fluctuations: A saturated‐unsaturated flow assessment","docAbstract":"<p><span>Groundwater consumption by phreatophytes is a difficult‐to‐measure but important component of the water budget in many arid and semiarid environments. Over the past 70 years the consumptive use of groundwater by phreatophytes has been estimated using a method that analyzes diurnal trends in hydrographs from wells that are screened across the water table (White, 1932). The reliability of estimates obtained with this approach has never been rigorously evaluated using saturated‐unsaturated flow simulation. We present such an evaluation for common flow geometries and a range of hydraulic properties. Results indicate that the major source of error in the White method is the uncertainty in the estimate of specific yield. Evapotranspirative consumption of groundwater will often be significantly overpredicted with the White method if the effects of drainage time and the depth to the water table on specific yield are ignored. We utilize the concept of readily available specific yield as the basis for estimation of the specific yield value appropriate for use with the White method. Guidelines are defined for estimating readily available specific yield based on sediment texture. Use of these guidelines with the White method should enable the evapotranspirative consumption of groundwater to be more accurately quantified.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/2005WR003942","usgsCitation":"Loheide, S.P., Butler, J.J., and Gorelick, S.M., 2005, Estimation of groundwater consumption by phreatophytes using diurnal water table fluctuations: A saturated‐unsaturated flow assessment: Water Resources Research, v. 41, no. 7, Article W07030; 14 p., https://doi.org/10.1029/2005WR003942.","productDescription":"Article W07030; 14 p.","costCenters":[],"links":[{"id":477898,"rank":1,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1029/2005wr003942","text":"Publisher Index Page"},{"id":237409,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"41","issue":"7","noUsgsAuthors":false,"publicationDate":"2005-07-27","publicationStatus":"PW","scienceBaseUri":"505a0b8fe4b0c8380cd52794","contributors":{"authors":[{"text":"Loheide, Steven P. II","contributorId":62377,"corporation":false,"usgs":false,"family":"Loheide","given":"Steven","suffix":"II","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":422292,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Butler, James J. Jr.","contributorId":199860,"corporation":false,"usgs":false,"family":"Butler","given":"James","suffix":"Jr.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":422290,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gorelick, Steven M.","contributorId":69295,"corporation":false,"usgs":true,"family":"Gorelick","given":"Steven","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":422291,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":81474,"text":"81474 - 2005 - Lake Michigan wetlands: classification, concerns, and management opportunities","interactions":[],"lastModifiedDate":"2012-02-02T00:04:01","indexId":"81474","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Lake Michigan wetlands: classification, concerns, and management opportunities","docAbstract":"The wetlands that border Lake Michigan are an extremely important component of the lake ecosystem.  In this paper, I will review the status of wetland classifications used for Lake Michigan and the other Great Lakes, as well as the major management concerns and opportunities presented by Lake Michigan wetlands.","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"State of Lake Michigan: Ecology, Health, and Management","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","publisher":"Aquatic Ecosystem Health and Management Society","publisherLocation":"New Delhi","isbn":"817898458X","usgsCitation":"Wilcox, D.A., 2005, Lake Michigan wetlands: classification, concerns, and management opportunities, chap. <i>of</i> State of Lake Michigan: Ecology, Health, and Management, p. 421-437.","productDescription":"p. 421-437","startPage":"421","endPage":"437","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":128024,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4822e4b07f02db4e1ff0","contributors":{"editors":[{"text":"Edsall, T.","contributorId":8792,"corporation":false,"usgs":true,"family":"Edsall","given":"T.","email":"","affiliations":[],"preferred":false,"id":504157,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Munawar, M.","contributorId":79835,"corporation":false,"usgs":true,"family":"Munawar","given":"M.","email":"","affiliations":[],"preferred":false,"id":504158,"contributorType":{"id":2,"text":"Editors"},"rank":2}],"authors":[{"text":"Wilcox, Douglas A.","contributorId":36880,"corporation":false,"usgs":true,"family":"Wilcox","given":"Douglas","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":295453,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70027845,"text":"70027845 - 2005 - Performance of juvenile steelhead trout (<i>Oncorhynchus mykiss</i>) produced from untreated and cryopreserved milt","interactions":[],"lastModifiedDate":"2017-01-04T13:53:19","indexId":"70027845","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":853,"text":"Aquaculture","active":true,"publicationSubtype":{"id":10}},"title":"Performance of juvenile steelhead trout (<i>Oncorhynchus mykiss</i>) produced from untreated and cryopreserved milt","docAbstract":"<p>Despite the expanding use of milt cryopreservation in aquaculture, the performance of fish produced from this technique has not been fully explored beyond initial rearing stages. We compared the performance of juvenile steelhead <i>Oncorhynchus mykiss</i> produced from untreated (UM) and cryopreserved milt (CM) and reared for 4&ndash;9 months. For the 1996 brood, CM alevins were heavier (&sim;&nbsp;1.7%, <i>P</i>&nbsp;&lt;&nbsp;0.01) than UM alevins and length was influenced by a significant milt-by-family interaction (<i>P</i>&nbsp;&lt;&nbsp;0.03) suggesting a greater treatment effect for some families. No significant differences were found in length or weight (<i>P</i>&nbsp;&gt;&nbsp;0.05) for 1997 brood alevins and percent yolk was similar for both broods (<i>P</i>&nbsp;&gt;&nbsp;0.34). In growth and survival experiment I (GSE-I, 1996), UM and CM juveniles reared in separate tanks and fed to satiation (130 days) showed no significant differences in survival, length or weight (<i>P</i>&nbsp;&gt;&nbsp;0.05) between milt groups. In contrast, for UM and CM siblings reared in the same tank for 210 days on a low food ration (GSE-II), survival was similar (<i>P</i>&nbsp;&gt;&nbsp;0.05), but length (UM 4%&nbsp;&gt;&nbsp;CM, <i>P</i>&nbsp;&lt;&nbsp;0.05) and possibly weight (UM 15%&nbsp;&gt;&nbsp;CM, <i>P</i>&nbsp;=&nbsp;0.08), were influenced by cryopreservation. Fish from the 1997 brood (GSE-III) were reared for 313 days in a repeat of GSE-II and no differences were found in survival (<i>P</i>&nbsp;=&nbsp;0.47), length (<i>P</i>&nbsp;=&nbsp;0.75) or weight (<i>P</i>&nbsp;=&nbsp;0.76) suggesting considerable heterogeneity between broods. Performance of the 1996 brood was also tested for response to stress and a disease challenge. Cortisol responses of juveniles exposed to acute stress were not significantly different (<i>P</i>&nbsp;=&nbsp;0.19), but mean cortisol was consistently and significantly greater (<i>P</i>&nbsp;&lt;&nbsp;0.01) for CM than UM fish exposed to a 48-h stress (increased density). After exposure to three dosages of the bacteria, <i>Listonella anguillarum</i>, we found similar mortality proportions (<i>P</i>&nbsp;=&nbsp;0.72) for UM and CM fish. Variable juvenile performance for the parameters tested indicated significant differences among broods and families and suggests a cautionary approach to the widespread use of cryopreservation for steelhead.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.aquaculture.2005.04.035","issn":"00448486","usgsCitation":"Hayes, M.C., Rubin, S.P., Hensleigh, J.E., Reisenbichler, R.R., and Wetzel, L.A., 2005, Performance of juvenile steelhead trout (<i>Oncorhynchus mykiss</i>) produced from untreated and cryopreserved milt: Aquaculture, v. 249, no. 1-4, p. 291-302, https://doi.org/10.1016/j.aquaculture.2005.04.035.","productDescription":"12 p.","startPage":"291","endPage":"302","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":238320,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"249","issue":"1-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a768be4b0c8380cd7818d","contributors":{"authors":[{"text":"Hayes, Michael C. 0000-0002-9060-0565 mhayes@usgs.gov","orcid":"https://orcid.org/0000-0002-9060-0565","contributorId":3017,"corporation":false,"usgs":true,"family":"Hayes","given":"Michael","email":"mhayes@usgs.gov","middleInitial":"C.","affiliations":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"preferred":true,"id":415524,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rubin, Stephen P. 0000-0003-3054-7173","orcid":"https://orcid.org/0000-0003-3054-7173","contributorId":38037,"corporation":false,"usgs":true,"family":"Rubin","given":"Stephen","email":"","middleInitial":"P.","affiliations":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"preferred":true,"id":415527,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hensleigh, Jay E.","contributorId":118799,"corporation":false,"usgs":true,"family":"Hensleigh","given":"Jay","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":415526,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Reisenbichler, Reginald R.","contributorId":20623,"corporation":false,"usgs":true,"family":"Reisenbichler","given":"Reginald","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":415525,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Wetzel, Lisa A. 0000-0003-3178-9940 lwetzel@usgs.gov","orcid":"https://orcid.org/0000-0003-3178-9940","contributorId":3016,"corporation":false,"usgs":true,"family":"Wetzel","given":"Lisa","email":"lwetzel@usgs.gov","middleInitial":"A.","affiliations":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"preferred":true,"id":415523,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
]}