{"pageNumber":"2612","pageRowStart":"65275","pageSize":"25","recordCount":184582,"records":[{"id":70029054,"text":"70029054 - 2005 - Mid-Pliocene deep-sea bottom-water temperatures based on ostracode Mg/Ca ratios","interactions":[],"lastModifiedDate":"2017-05-10T16:16:48","indexId":"70029054","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2673,"text":"Marine Micropaleontology","active":true,"publicationSubtype":{"id":10}},"title":"Mid-Pliocene deep-sea bottom-water temperatures based on ostracode Mg/Ca ratios","docAbstract":"We studied magnesium:calcium (Mg/Ca) ratios in shells of the deep-sea ostracode genus Krithe from a short interval in the middle Pliocene between 3.29 and 2.97 Ma using deep-sea drilling sites in the North and South Atlantic in order to estimate bottom water temperatures (BWT) during a period of climatic warmth. Results from DSDP and ODP Sites 552A, 610A, 607, 658A, 659A, 661A and 704 for the period Ma reveal both depth and latitudinal gradients of mean Mg/Ca values. Shallower sites (552A, 610A and 607) have higher mean Mg/Ca ratios (10.3, 9.7, 10.1 mmol/mol) than deeper sites (661A, 6.3 mmol/mol), and high latitude North Atlantic sites (552A, 610A, 607) have higher Mg/Ca ratios than low latitude (658A: 9.8 mmol/mol, 659A: 7.7 mmol/mol, 661A: 6.3 mmol/mol) and Southern Ocean (704: 8.0 mmol/mol) sites. Converting Mg/Ca ratios into estimated temperatures using the calibration of Dwyer et al. (1995) [Dwyer, G.S., Cronin, T.M., Baker, P.A., Raymo, M.E., Buzas, J.S., Corre??ge, T., 1995. North Atlantic deepwater temperature change during late Pliocene and late Quaternary climatic cycles. Science 270, 1347-1351] suggests that mean middle Pliocene bottom water temperatures at the study sites in the deep Atlantic were about the same as modern temperatures. However, brief pulses of elevated BWT occurred several times between 3.29 and 2.97 Ma in both the North and South Atlantic Ocean suggesting short-term changes in deep ocean circulation.","language":"English","publisher":"Elsevier","doi":"10.1016/j.marmicro.2004.12.003","issn":"03778398","usgsCitation":"Cronin, T.M., Dowsett, H., Dwyer, G., Baker, P., and Chandler, M., 2005, Mid-Pliocene deep-sea bottom-water temperatures based on ostracode Mg/Ca ratios: Marine Micropaleontology, v. 54, no. 3-4, p. 249-261, https://doi.org/10.1016/j.marmicro.2004.12.003.","productDescription":"13","startPage":"249","endPage":"261","costCenters":[],"links":[{"id":487540,"rank":1,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"http://hdl.handle.net/10161/7000","text":"External Repository"},{"id":237577,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"54","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a56bfe4b0c8380cd6d7ce","contributors":{"authors":[{"text":"Cronin, T. M. 0000-0002-2643-0979","orcid":"https://orcid.org/0000-0002-2643-0979","contributorId":42613,"corporation":false,"usgs":true,"family":"Cronin","given":"T.","email":"","middleInitial":"M.","affiliations":[{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true}],"preferred":false,"id":421153,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dowsett, H.J. 0000-0003-1983-7524","orcid":"https://orcid.org/0000-0003-1983-7524","contributorId":87924,"corporation":false,"usgs":true,"family":"Dowsett","given":"H.J.","affiliations":[],"preferred":false,"id":421155,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dwyer, Gary S.","contributorId":67642,"corporation":false,"usgs":true,"family":"Dwyer","given":"Gary S.","affiliations":[],"preferred":false,"id":421152,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Baker, P.A.","contributorId":55148,"corporation":false,"usgs":true,"family":"Baker","given":"P.A.","email":"","affiliations":[],"preferred":false,"id":421154,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Chandler, M.A.","contributorId":26874,"corporation":false,"usgs":true,"family":"Chandler","given":"M.A.","email":"","affiliations":[],"preferred":false,"id":421151,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70029052,"text":"70029052 - 2005 - The effect of thiamine injection on upstream migration, survival, and thiamine status of putative thiamine-deficient coho salmon","interactions":[],"lastModifiedDate":"2012-03-12T17:20:53","indexId":"70029052","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2177,"text":"Journal of Aquatic Animal Health","active":true,"publicationSubtype":{"id":10}},"title":"The effect of thiamine injection on upstream migration, survival, and thiamine status of putative thiamine-deficient coho salmon","docAbstract":"A diet containing a high proportion of alewives Alosa pseudoharengus results in a thiamine deficiency that has been associated with high larval salmonid mortality, known as early mortality syndrome (EMS), but relatively little is known about the effects of the deficiency on adults. Using thiamine injection (50 mg thiamine/kg body weight) of ascending adult female coho salmon Oncorhynchus kisutch on the Platte River, Michigan, we investigated the effects of thiamine supplementation on migration, adult survival, and thiamine status. The thiamine concentrations of eggs, muscle (red and white), spleen, kidney (head and trunk), and liver and the transketolase activity of the liver, head kidney, and trunk kidney of fish injected with thiamine dissolved in physiological saline (PST) or physiological saline only (PS) were compared with those of uninjected fish. The injection did not affect the number of fish making the 15-km upstream migration to a collection weir but did affect survival once fish reached the upstream weir, where survival of PST-injected fish was almost twice that of controls. The egg and liver thiamine concentrations in PS fish sampled after their upstream migration were significantly lower than those of uninjected fish collected at the downstream weir, but the white muscle thiamine concentration did not differ between the two groups. At the upper weir, thiamine levels in the liver, spleen, head kidney, and trunk kidney of PS fish were indistinguishable from those of uninjected fish (called \"wigglers\") suffering from a severe deficiency and exhibiting reduced equilibrium, a stage that precedes total loss of equilibrium and death. For PST fish collected at the upstream weir, total thiamine levels in all tissues were significantly elevated over those of PS fish. Based on the limited number of tissues examined, thiamine status was indicated better by tissue thiamine concentration than by transketolase activity. The adult injection method we used appears to be a more effective means of increasing egg thiamine levels than immersion of eggs in a thiamine solution. ?? Copyright by the American Fisheries Society 2005.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Aquatic Animal Health","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1577/H04-003.1","issn":"08997659","usgsCitation":"Fitzsimons, J., Williston, B., Amcoff, P., Balk, L., Pecor, C., Ketola, H.G., Hinterkopf, J.P., and Honeyfield, D., 2005, The effect of thiamine injection on upstream migration, survival, and thiamine status of putative thiamine-deficient coho salmon: Journal of Aquatic Animal Health, v. 17, no. 1, p. 48-58, https://doi.org/10.1577/H04-003.1.","startPage":"48","endPage":"58","numberOfPages":"11","costCenters":[],"links":[{"id":210601,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1577/H04-003.1"},{"id":237575,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","issue":"1","noUsgsAuthors":false,"publicationDate":"2005-03-01","publicationStatus":"PW","scienceBaseUri":"505bab5be4b08c986b322db5","contributors":{"authors":[{"text":"Fitzsimons, J.D.","contributorId":50845,"corporation":false,"usgs":true,"family":"Fitzsimons","given":"J.D.","email":"","affiliations":[],"preferred":false,"id":421141,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Williston, B.","contributorId":49176,"corporation":false,"usgs":true,"family":"Williston","given":"B.","email":"","affiliations":[],"preferred":false,"id":421140,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Amcoff, P.","contributorId":51087,"corporation":false,"usgs":true,"family":"Amcoff","given":"P.","email":"","affiliations":[],"preferred":false,"id":421142,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Balk, L.","contributorId":42415,"corporation":false,"usgs":true,"family":"Balk","given":"L.","email":"","affiliations":[],"preferred":false,"id":421139,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Pecor, C.","contributorId":73152,"corporation":false,"usgs":true,"family":"Pecor","given":"C.","email":"","affiliations":[],"preferred":false,"id":421145,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Ketola, H. G.","contributorId":60976,"corporation":false,"usgs":true,"family":"Ketola","given":"H.","middleInitial":"G.","affiliations":[],"preferred":false,"id":421143,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Hinterkopf, J. P.","contributorId":11145,"corporation":false,"usgs":true,"family":"Hinterkopf","given":"J.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":421138,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Honeyfield, D. C. 0000-0003-3034-2047","orcid":"https://orcid.org/0000-0003-3034-2047","contributorId":73136,"corporation":false,"usgs":true,"family":"Honeyfield","given":"D. C.","affiliations":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"preferred":false,"id":421144,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":70029119,"text":"70029119 - 2005 - Effects of iron on arsenic speciation and redox chemistry in acid mine water","interactions":[],"lastModifiedDate":"2012-03-12T17:20:53","indexId":"70029119","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2302,"text":"Journal of Geochemical Exploration","active":true,"publicationSubtype":{"id":10}},"title":"Effects of iron on arsenic speciation and redox chemistry in acid mine water","docAbstract":"Concern about arsenic is increasing throughout the world, including areas of the United States. Elevated levels of arsenic above current drinking-water regulations in ground and surface water can be the result of purely natural phenomena, but often are due to anthropogenic activities, such as mining and agriculture. The current study correlates arsenic speciation in acid mine drainage and mining-influenced water with the important water-chemistry properties Eh, pH, and iron(III) concentration. The results show that arsenic speciation is generally in equilibrium with iron chemistry in low pH AMD, which is often not the case in other natural-water matrices. High pH mine waters and groundwater do not always hold to the redox predictions as well as low pH AMD samples. The oxidation and precipitation of oxyhydroxides deplete iron from some systems, and also affect arsenite and arsenate concentrations through sorption processes. ?? 2004 Elsevier B.V. All rights reserved.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Geochemical Exploration","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.gexplo.2004.10.001","issn":"03756742","usgsCitation":"Bednar, A., Garbarino, J., Ranville, J., and Wildeman, T., 2005, Effects of iron on arsenic speciation and redox chemistry in acid mine water: Journal of Geochemical Exploration, v. 85, no. 2, p. 55-62, https://doi.org/10.1016/j.gexplo.2004.10.001.","startPage":"55","endPage":"62","numberOfPages":"8","costCenters":[],"links":[{"id":210548,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.gexplo.2004.10.001"},{"id":237503,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"85","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a072de4b0c8380cd515c6","contributors":{"authors":[{"text":"Bednar, A.J.","contributorId":67247,"corporation":false,"usgs":true,"family":"Bednar","given":"A.J.","email":"","affiliations":[],"preferred":false,"id":421391,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Garbarino, J.R.","contributorId":76326,"corporation":false,"usgs":true,"family":"Garbarino","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":421392,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ranville, J. F.","contributorId":54245,"corporation":false,"usgs":true,"family":"Ranville","given":"J. F.","affiliations":[],"preferred":false,"id":421390,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Wildeman, T.R.","contributorId":30248,"corporation":false,"usgs":true,"family":"Wildeman","given":"T.R.","email":"","affiliations":[],"preferred":false,"id":421389,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70029118,"text":"70029118 - 2005 - Interferometric synthetic aperture radar study of Okmok volcano, Alaska, 1992-2003: Magma supply dynamics and postemplacement lava flow deformation","interactions":[],"lastModifiedDate":"2019-05-06T11:20:58","indexId":"70029118","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2314,"text":"Journal of Geophysical Research B: Solid Earth","active":true,"publicationSubtype":{"id":10}},"title":"Interferometric synthetic aperture radar study of Okmok volcano, Alaska, 1992-2003: Magma supply dynamics and postemplacement lava flow deformation","docAbstract":"<p><span>Okmok volcano, located in the central Aleutian arc, Alaska, is a dominantly basaltic complex topped with a 10-km-wide caldera that formed circa 2.05 ka. Okmok erupted several times during the 20th century, most recently in 1997; eruptions in 1945, 1958, and 1997 produced lava flows within the caldera. We used 80 interferometric synthetic aperture radar (InSAR) images (interferograms) to study transient deformation of the volcano before, during, and after the 1997 eruption. Point source models suggest that a magma reservoir at a depth of 3.2 km below sea level, located beneath the center of the caldera and about 5 km northeast of the 1997 vent, is responsible for observed volcano-wide deformation. The preeruption uplift rate decreased from about 10 cm yr</span><sup>−1</sup><span> during 1992–1993 to 2 ∼ 3 cm yr</span><sup>−1</sup><span> during 1993–1995 and then to about −1 ∼ −2 cm yr</span><sup>−1</sup><span> during 1995–1996. The posteruption inflation rate generally decreased with time during 1997–2001, but increased significantly during 2001–2003. By the summer of 2003, 30 ∼ 60% of the magma volume lost from the reservoir in the 1997 eruption had been replenished. Interferograms for periods before the 1997 eruption indicate consistent subsidence of the surface of the 1958 lava flows, most likely due to thermal contraction. Interferograms for periods after the eruption suggest at least four distinct deformation processes: (1) volcano-wide inflation due to replenishment of the shallow magma reservoir, (2) subsidence of the 1997 lava flows, most likely due to thermal contraction, (3) deformation of the 1958 lava flows due to loading by the 1997 flows, and (4) continuing subsidence of 1958 lava flows buried beneath 1997 flows. Our results provide insights into the postemplacement behavior of lava flows and have cautionary implications for the interpretation of inflation patterns at active volcanoes.</span></p>","language":"English","publisher":"AGU","doi":"10.1029/2004JB003148","issn":"01480227","usgsCitation":"Lu, Z., Masterlark, T., and Dzurisin, D., 2005, Interferometric synthetic aperture radar study of Okmok volcano, Alaska, 1992-2003: Magma supply dynamics and postemplacement lava flow deformation: Journal of Geophysical Research B: Solid Earth, v. 110, no. B2, p. 1-18, https://doi.org/10.1029/2004JB003148.","productDescription":"18 p.","startPage":"1","endPage":"18","numberOfPages":"18","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true},{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true}],"links":[{"id":477915,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1029/2004jb003148","text":"Publisher Index Page"},{"id":237465,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":210522,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1029/2004JB003148"}],"country":"United States","state":"Alaska","otherGeospatial":"Okmok volcano","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -168.2281494140625,\n              53.34399288223422\n            ],\n            [\n              -167.9754638671875,\n              53.34399288223422\n            ],\n            [\n              -167.9754638671875,\n              53.48477702972815\n            ],\n            [\n              -168.2281494140625,\n              53.48477702972815\n            ],\n            [\n              -168.2281494140625,\n              53.34399288223422\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"110","issue":"B2","noUsgsAuthors":false,"publicationDate":"2005-02-23","publicationStatus":"PW","scienceBaseUri":"505a3d00e4b0c8380cd63206","contributors":{"authors":[{"text":"Lu, Z.","contributorId":106241,"corporation":false,"usgs":true,"family":"Lu","given":"Z.","affiliations":[],"preferred":false,"id":421388,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Masterlark, Timothy","contributorId":92829,"corporation":false,"usgs":false,"family":"Masterlark","given":"Timothy","email":"","affiliations":[{"id":35607,"text":"South Dakota School of Mines","active":true,"usgs":false}],"preferred":false,"id":421387,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dzurisin, Daniel 0000-0002-0138-5067 dzurisin@usgs.gov","orcid":"https://orcid.org/0000-0002-0138-5067","contributorId":538,"corporation":false,"usgs":true,"family":"Dzurisin","given":"Daniel","email":"dzurisin@usgs.gov","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":421386,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70029161,"text":"70029161 - 2005 - Geometry and kinematics of Late Cretaceous inversion structures in the Jiuquan Basin, western China","interactions":[],"lastModifiedDate":"2012-03-12T17:20:53","indexId":"70029161","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1344,"text":"Cretaceous Research","active":true,"publicationSubtype":{"id":10}},"title":"Geometry and kinematics of Late Cretaceous inversion structures in the Jiuquan Basin, western China","docAbstract":"Late Cretaceous inversion structures, which are significant for oil and gas accumulation, are widely distributed throughout the Jiuquan Basin. These structures are primarily made up of inverted faults and fault-related folds. Most of the axial planes of folds are parallel to inverted faults trending north-east, indicating that the principal stress direction was north-west - south-east in the Late Cretaceous. The average inversion ratios of faults in the four sags that were investigated are 0.39, 0.29, 0.38, 0.32. The average inversion ratio in the Jiuquan Basin is 0.34 and the degree of inversion is moderate to strong. As moderate inversion is suitable for forming excellent hydrocarbon traps, there is considered to be significant potential in the basin for the presence of structural traps. ?? 2005 Elsevier Ltd. All rights reserved.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Cretaceous Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.cretres.2005.01.005","issn":"01956671","usgsCitation":"Wang, B., Hao, C., Yang, S., Xiao, A., Cheng, X., and Rupp, J., 2005, Geometry and kinematics of Late Cretaceous inversion structures in the Jiuquan Basin, western China: Cretaceous Research, v. 26, no. 2, p. 319-327, https://doi.org/10.1016/j.cretres.2005.01.005.","startPage":"319","endPage":"327","numberOfPages":"9","costCenters":[],"links":[{"id":210609,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.cretres.2005.01.005"},{"id":237583,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"26","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a2769e4b0c8380cd59878","contributors":{"authors":[{"text":"Wang, B.","contributorId":29011,"corporation":false,"usgs":true,"family":"Wang","given":"B.","email":"","affiliations":[],"preferred":false,"id":421585,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hao, Chen","contributorId":89306,"corporation":false,"usgs":true,"family":"Hao","given":"Chen","email":"","affiliations":[],"preferred":false,"id":421587,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Yang, S.","contributorId":13588,"corporation":false,"usgs":true,"family":"Yang","given":"S.","email":"","affiliations":[],"preferred":false,"id":421583,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Xiao, A.","contributorId":97779,"corporation":false,"usgs":true,"family":"Xiao","given":"A.","email":"","affiliations":[],"preferred":false,"id":421588,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Cheng, X.","contributorId":23027,"corporation":false,"usgs":true,"family":"Cheng","given":"X.","email":"","affiliations":[],"preferred":false,"id":421584,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Rupp, J.A.","contributorId":30596,"corporation":false,"usgs":true,"family":"Rupp","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":421586,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70029163,"text":"70029163 - 2005 - A new Sunwaptan (Late Cambrian) trilobite fauna from the Upper Mississippi Valley","interactions":[],"lastModifiedDate":"2022-05-24T15:55:50.396125","indexId":"70029163","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2412,"text":"Journal of Paleontology","active":true,"publicationSubtype":{"id":10}},"title":"A new Sunwaptan (Late Cambrian) trilobite fauna from the Upper Mississippi Valley","docAbstract":"A single bed at the base of the Jordan Sandstone in a road cut at Arcadia, Wisconsin, yielded an undescribed Late Sunwaptan (Saukia Zone) trilobite fauna that includes at least four species from the families Dikelocephalidae Miller, 1889 and Eurekiidae Hupe??, 1953. Arcadiaspis bispinata n. gen. and sp. is a distinctive eurekiid that is characterized by paired occipital and thoracic axial spines, long genal spines, and a nonspinose pygidial margin. Other genera present are the dikelocephalids, Dikelocephalus Owen, 1852 and Calvinella Walcott, 1914, and the eurekiid, Eurekia Walcott, 1916. Type material of Calvinella spiniger (Hall, 1863) is illustrated photographically for the first time. A new eurekiid species, Corbinia burkhalteri from the Fort Sill Formation, Oklahoma, is also described.","language":"English","publisher":"Society of Economic Paleontologists and Mineralogists","doi":"10.1666/0022-3360(2005)079%3C0072:ANSLCT%3E2.0.CO;2","usgsCitation":"Westrop, S.R., Palmer, A.R., and Runkel, A., 2005, A new Sunwaptan (Late Cambrian) trilobite fauna from the Upper Mississippi Valley: Journal of Paleontology, v. 79, no. 1, p. 72-88, https://doi.org/10.1666/0022-3360(2005)079%3C0072:ANSLCT%3E2.0.CO;2.","productDescription":"17 p.","startPage":"72","endPage":"88","numberOfPages":"17","costCenters":[],"links":[{"id":237616,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"79","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e499e4b0c8380cd4675e","contributors":{"authors":[{"text":"Westrop, S. R.","contributorId":69727,"corporation":false,"usgs":false,"family":"Westrop","given":"S.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":421593,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Palmer, Allison R.","contributorId":24343,"corporation":false,"usgs":true,"family":"Palmer","given":"Allison","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":421592,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Runkel, Anthony","contributorId":87023,"corporation":false,"usgs":true,"family":"Runkel","given":"Anthony","affiliations":[],"preferred":false,"id":421594,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70031489,"text":"70031489 - 2005 - Changes in productivity and contaminants in bald eagles nesting along the lower Columbia River, USA","interactions":[],"lastModifiedDate":"2016-08-18T16:51:27","indexId":"70031489","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1571,"text":"Environmental Toxicology and Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"Changes in productivity and contaminants in bald eagles nesting along the lower Columbia River, USA","docAbstract":"<p>Previous studies documented poor productivity of bald eagles (Haliaeetus leucocephalus) in the lower Columbia River (LCR), USA, and elevated p,p???-dichlorodiphenyldichloroethylene (DDE), polychlorinated biphenyls (PCBs), dioxins, and furans in eagle eggs. From 1994 to 1995, we collected partially incubated eggs at 19 of 43 occupied territories along the LCR and compared productivity and egg contaminants to values obtained in the mid-1980s. We found higher productivity at new nesting sites along the river, yet productivity at 23 older breeding territories remained low and was not different (p = 0.713) between studies. Eggshell thickness at older territories had not improved (p = 0.404), and eggshells averaged 11% thinner than shells measured before dichlorodiphenyltrichloroethane use. Decreases in DDE (p = 0.022) and total PCBs (p = 0.0004) in eggs from older breeding areas occurred between study periods. Productivity was not correlated to contaminants, but DDE, PCBs, and dioxin-like chemicals exceeded estimated no-effect values. Some dioxin-like contaminants in eggs were correlated to nest location, with highest concentrations occurring toward the river's mouth where productivity was lowest. Although total productivity increased due to the success of new nesting pairs in the region, egg contaminants remain high enough to impair reproduction at older territories and, over time, may alter productivity of new pairs nesting near the river's mouth. ?? 2005 SETAC.</p>","language":"English","publisher":"Wiley","doi":"10.1897/03-621.1","issn":"07307268","usgsCitation":"Buck, J., Anthony, R., Schuler, C., Isaacs, F., and Tillitt, D.E., 2005, Changes in productivity and contaminants in bald eagles nesting along the lower Columbia River, USA: Environmental Toxicology and Chemistry, v. 24, no. 7, p. 1779-1792, https://doi.org/10.1897/03-621.1.","productDescription":"14 p.","startPage":"1779","endPage":"1792","numberOfPages":"14","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"links":[{"id":239995,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":212502,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1897/03-621.1"}],"country":"United States","state":"Oregon, Washington","otherGeospatial":"Lower Columbia River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -124.06311035156249,\n              46.320378031062354\n            ],\n            [\n              -123.96972656249999,\n              46.32986150334176\n            ],\n            [\n              -123.87634277343749,\n              46.25774588045683\n            ],\n            [\n              -123.74999999999999,\n              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C.A.","contributorId":42627,"corporation":false,"usgs":true,"family":"Schuler","given":"C.A.","email":"","affiliations":[],"preferred":false,"id":431767,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Isaacs, F.B.","contributorId":39733,"corporation":false,"usgs":true,"family":"Isaacs","given":"F.B.","email":"","affiliations":[],"preferred":false,"id":431766,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Tillitt, D. E.","contributorId":83462,"corporation":false,"usgs":true,"family":"Tillitt","given":"D.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":431768,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70029146,"text":"70029146 - 2005 - Influence of the Atchafalaya River on recent evolution of the chenier-plain inner continental shelf, northern Gulf of Mexico","interactions":[],"lastModifiedDate":"2012-03-12T17:20:55","indexId":"70029146","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1333,"text":"Continental Shelf Research","active":true,"publicationSubtype":{"id":10}},"title":"Influence of the Atchafalaya River on recent evolution of the chenier-plain inner continental shelf, northern Gulf of Mexico","docAbstract":"This study examines the influence of the Atchafalaya River, a major distributary of the Mississippi River, on stratigraphic evolution of the inner continental shelf in the northern Gulf of Mexico. Sedimentary, geochemical, and shallow acoustic data are used to identify the western limit of the distal Atchafalaya subaqueous delta, and to estimate the proportion of the Atchafalaya River's sediment load that accumulates on the inner shelf seaward of Louisiana's chenier-plain coast. The results demonstrate a link between sedimentary facies distribution on the inner shelf and patterns of shoreline accretion and retreat on the chenier plain. Mudflat progradation on the eastern chenier-plain coast corresponds to the location of deltaic mud accumulation on the inner shelf. On the central chenier-plain shelf, west of the subaqueous delta, relict sediment is exposed that was originally deposited between ???1200 and 600 years BP during activity of the Lafourche lobe of the Mississippi Delta complex. Mass-balance calculations indicate that the eastern chenier-plain inner shelf and coastal zone form a sink for 7??2% of the sediment load carried by the Atchafalaya River. ?? 2004 Elsevier Ltd. All rights reserved.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Continental Shelf Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.csr.2004.09.002","issn":"02784343","usgsCitation":"Draut, A., Kineke, G., Velasco, D., Allison, M.A., and Prime, R., 2005, Influence of the Atchafalaya River on recent evolution of the chenier-plain inner continental shelf, northern Gulf of Mexico: Continental Shelf Research, v. 25, no. 1, p. 91-112, https://doi.org/10.1016/j.csr.2004.09.002.","startPage":"91","endPage":"112","numberOfPages":"22","costCenters":[],"links":[{"id":210470,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.csr.2004.09.002"},{"id":237396,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"25","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3b85e4b0c8380cd625e6","contributors":{"authors":[{"text":"Draut, A.E.","contributorId":50273,"corporation":false,"usgs":true,"family":"Draut","given":"A.E.","affiliations":[],"preferred":false,"id":421517,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kineke, G.C.","contributorId":12214,"corporation":false,"usgs":true,"family":"Kineke","given":"G.C.","email":"","affiliations":[],"preferred":false,"id":421515,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Velasco, D.W.","contributorId":51972,"corporation":false,"usgs":true,"family":"Velasco","given":"D.W.","email":"","affiliations":[],"preferred":false,"id":421518,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Allison, M. A.","contributorId":49834,"corporation":false,"usgs":true,"family":"Allison","given":"M.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":421516,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Prime, R.J.","contributorId":88140,"corporation":false,"usgs":true,"family":"Prime","given":"R.J.","email":"","affiliations":[],"preferred":false,"id":421519,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70029117,"text":"70029117 - 2005 - Forearc structure beneath southwestern British Columbia: A three-dimensional tomographic velocity model","interactions":[],"lastModifiedDate":"2012-03-12T17:20:54","indexId":"70029117","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2314,"text":"Journal of Geophysical Research B: Solid Earth","active":true,"publicationSubtype":{"id":10}},"title":"Forearc structure beneath southwestern British Columbia: A three-dimensional tomographic velocity model","docAbstract":"This paper presents a three-dimensional compressional wave velocity model of the forearc crust and upper mantle and the subducting Juan de Fuca plate beneath southwestern British Columbia and the adjoining straits of Georgia and Juan de Fuca. The velocity model was constructed through joint tomographic inversion of 50,000 first-arrival times from earthquakes and active seismic sources. Wrangellia rocks of the accreted Paleozoic and Mesozoic island arc assemblage underlying southern Vancouver Island in the Cascadia forearc are imaged at some locations with higher than average lower crustal velocities of 6.5-7.2 km/s, similar to observations at other island arc terranes. The mafic Eocene Crescent terrane, thrust landward beneath southern Vancouver Island, exhibits crustal velocities in the range of 6.0-6.7 km/s and is inferred to extend to a depth of more than 20 km. The Cenozoic Olympic Subduction Complex, an accretionary prism thrust beneath the Crescent terrane in the Olympic Peninsula, is imaged as a low-velocity wedge to depths of at least 20 km. Three zones with velocities of 7.0-7.5 km/s, inferred to be mafic and/or ultramafic units, lie above the subducting Juan de Fuca plate at depths of 25-35 km. The forearc upper mantle wedge beneath southeastern Vancouver Island and the Strait of Georgia exhibits low velocities of 7.2-7.5 km/s, inferred to correspond to ???20% serpentinization of mantle peridotites, and consistent with similar observations in other warm subduction zones. Estimated dip of the Juan de Fuca plate beneath southern Vancouver Island is ???11??, 16??, and 27?? at depths of 30, 40, and 50 km, respectively. Copyright 2005 by the American Geophysical Union.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Geophysical Research B: Solid Earth","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1029/2004JB003258","issn":"01480227","usgsCitation":"Ramachandran, K., Dosso, S., Spence, G., Hyndman, R., and Brocher, T., 2005, Forearc structure beneath southwestern British Columbia: A three-dimensional tomographic velocity model: Journal of Geophysical Research B: Solid Earth, v. 110, no. 2, p. 1-17, https://doi.org/10.1029/2004JB003258.","startPage":"1","endPage":"17","numberOfPages":"17","costCenters":[],"links":[{"id":477908,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1029/2004jb003258","text":"Publisher Index Page"},{"id":210521,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1029/2004JB003258"},{"id":237464,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"110","issue":"2","noUsgsAuthors":false,"publicationDate":"2005-02-24","publicationStatus":"PW","scienceBaseUri":"505a130ee4b0c8380cd544de","contributors":{"authors":[{"text":"Ramachandran, K.","contributorId":71735,"corporation":false,"usgs":true,"family":"Ramachandran","given":"K.","email":"","affiliations":[],"preferred":false,"id":421384,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dosso, S.E.","contributorId":45085,"corporation":false,"usgs":true,"family":"Dosso","given":"S.E.","email":"","affiliations":[],"preferred":false,"id":421381,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Spence, G.D.","contributorId":85750,"corporation":false,"usgs":true,"family":"Spence","given":"G.D.","email":"","affiliations":[],"preferred":false,"id":421385,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hyndman, R.D.","contributorId":45831,"corporation":false,"usgs":true,"family":"Hyndman","given":"R.D.","email":"","affiliations":[],"preferred":false,"id":421382,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Brocher, T.M. 0000-0002-9740-839X","orcid":"https://orcid.org/0000-0002-9740-839X","contributorId":69994,"corporation":false,"usgs":true,"family":"Brocher","given":"T.M.","affiliations":[],"preferred":false,"id":421383,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70031679,"text":"70031679 - 2005 - Colorado Late Cenozoic Fault and Fold Database and Internet Map Server: User-friendly technology for complex information","interactions":[],"lastModifiedDate":"2012-03-12T17:21:13","indexId":"70031679","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1574,"text":"Environmental & Engineering Geoscience","printIssn":"1078-7275","active":true,"publicationSubtype":{"id":10}},"title":"Colorado Late Cenozoic Fault and Fold Database and Internet Map Server: User-friendly technology for complex information","docAbstract":"Internet mapping applications for geologic data allow simultaneous data delivery and collection, enabling quick data modification while efficiently supplying the end user with information. Utilizing Web-based technologies, the Colorado Geological Survey's Colorado Late Cenozoic Fault and Fold Database was transformed from a monothematic, nonspatial Microsoft Access database into a complex information set incorporating multiple data sources. The resulting user-friendly format supports easy analysis and browsing. The core of the application is the Microsoft Access database, which contains information compiled from available literature about faults and folds that are known or suspected to have moved during the late Cenozoic. The database contains nonspatial fields such as structure type, age, and rate of movement. Geographic locations of the fault and fold traces were compiled from previous studies at 1:250,000 scale to form a spatial database containing information such as length and strike. Integration of the two databases allowed both spatial and nonspatial information to be presented on the Internet as a single dataset (http://geosurvey.state.co.us/pubs/ceno/). The user-friendly interface enables users to view and query the data in an integrated manner, thus providing multiple ways to locate desired information. Retaining the digital data format also allows continuous data updating and quick delivery of newly acquired information. This dataset is a valuable resource to anyone interested in earthquake hazards and the activity of faults and folds in Colorado. Additional geologic hazard layers and imagery may aid in decision support and hazard evaluation. The up-to-date and customizable maps are invaluable tools for researchers or the public.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Environmental and Engineering Geoscience","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.2113/11.2.155","issn":"10787275","usgsCitation":"Morgan, K., Pattyn, G., and Morgan, M., 2005, Colorado Late Cenozoic Fault and Fold Database and Internet Map Server: User-friendly technology for complex information: Environmental & Engineering Geoscience, v. 11, no. 2, p. 155-162, https://doi.org/10.2113/11.2.155.","startPage":"155","endPage":"162","numberOfPages":"8","costCenters":[],"links":[{"id":212276,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.2113/11.2.155"},{"id":239738,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"11","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f7c0e4b0c8380cd4ccb1","contributors":{"authors":[{"text":"Morgan, K.S.","contributorId":60438,"corporation":false,"usgs":true,"family":"Morgan","given":"K.S.","email":"","affiliations":[],"preferred":false,"id":432643,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pattyn, G.J.","contributorId":73009,"corporation":false,"usgs":true,"family":"Pattyn","given":"G.J.","email":"","affiliations":[],"preferred":false,"id":432644,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Morgan, M.L.","contributorId":59245,"corporation":false,"usgs":true,"family":"Morgan","given":"M.L.","email":"","affiliations":[],"preferred":false,"id":432642,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70031495,"text":"70031495 - 2005 - Vertical motions of the Puerto Rico Trench and Puerto Rico and their cause","interactions":[],"lastModifiedDate":"2017-11-18T10:05:23","indexId":"70031495","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2314,"text":"Journal of Geophysical Research B: Solid Earth","active":true,"publicationSubtype":{"id":10}},"title":"Vertical motions of the Puerto Rico Trench and Puerto Rico and their cause","docAbstract":"The Puerto Rico trench exhibits great water depth, an extremely low gravity anomaly, and a tilted carbonate platform between (reconstructed) elevations of +1300 m and -4000 m. I argue that these features are manifestations of large vertical movements of a segment of the Puerto Rico trench, its forearc, and the island of Puerto Rico that took place 3.3 m.y. ago over a time period as short as 14-40 kyr. I explain these vertical movements by a sudden increase in the slab's descent angle that caused the trench to subside and the island to rise. The increased dip could have been caused by shearing or even by a complete tear of the descending North American slab, although the exact nature of this deformation is unknown. The rapid (14-40 kyr) and uniform tilt along a 250 km long section of the trench is compatible with scales of mantle flow and plate bending. The proposed shear zone or tear is inferred from seismic, morphological, and gravity observations to start at the trench at 64.5??W and trend southwestwardly toward eastern Puerto Rico. The tensile stresses necessary to deform or tear the slab could have been generated by increased curvature of the trench following a counterclockwise rotation of the upper plate and by the subduction of a large seamount.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Geophysical Research B: Solid Earth","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1029/2004JB003459","issn":"01480227","usgsCitation":"ten Brink, U., 2005, Vertical motions of the Puerto Rico Trench and Puerto Rico and their cause: Journal of Geophysical Research B: Solid Earth, v. 110, no. 6, p. 1-16, https://doi.org/10.1029/2004JB003459.","startPage":"1","endPage":"16","numberOfPages":"16","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":487016,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1029/2004jb003459","text":"Publisher Index Page"},{"id":212597,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1029/2004JB003459"},{"id":240103,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"110","issue":"6","noUsgsAuthors":false,"publicationDate":"2005-06-22","publicationStatus":"PW","scienceBaseUri":"505bc23ee4b08c986b32a9f5","contributors":{"authors":[{"text":"ten Brink, Uri S. 0000-0001-6858-3001 utenbrink@usgs.gov","orcid":"https://orcid.org/0000-0001-6858-3001","contributorId":127560,"corporation":false,"usgs":true,"family":"ten Brink","given":"Uri S.","email":"utenbrink@usgs.gov","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true},{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"preferred":false,"id":431794,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70028999,"text":"70028999 - 2005 - Observer variability in pinniped counts: Ground-based enumeration of walruses at haul-out sites","interactions":[],"lastModifiedDate":"2018-08-20T20:05:41","indexId":"70028999","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2671,"text":"Marine Mammal Science","active":true,"publicationSubtype":{"id":10}},"title":"Observer variability in pinniped counts: Ground-based enumeration of walruses at haul-out sites","docAbstract":"<p>Pinnipeds are often monitored by counting individuals at haul-out sites, but the often large numbers of densely packed individuals at these sites are difficult to enumerate accurately. Errors in enumeration can induce bias and reduce precision in estimates of population size and trend. We used data from paired observers monitoring walrus haul-outs in Bristol Bay, Alaska, to quantify observer variability and assess its relative importance. The probability of a pair of observers making identical counts was 50 individuals. Mean count differences ranged up to 25% for the largest counts, depending on beach and observers. In at least some cases, there was a clear tendency for counts of one observer to be consistently greater than counts of the other observer in a pair, indicating that counts of at least one of the observers were biased. These results suggest that efforts to improve accuracy of counts will be worthwhile. However, we also found that variation among observers was relatively small compared to variation among visits to a beach so that efforts to account for other sources of variation will be more important.</p>","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Marine Mammal Science","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1111/j.1748-7692.2005.tb01211.x","issn":"08240469","usgsCitation":"Udevitz, M.S., Jay, C., and Cody, M., 2005, Observer variability in pinniped counts: Ground-based enumeration of walruses at haul-out sites: Marine Mammal Science, v. 21, no. 1, p. 108-120, https://doi.org/10.1111/j.1748-7692.2005.tb01211.x.","productDescription":"13 p.","startPage":"108","endPage":"120","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":236734,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"21","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a6af8e4b0c8380cd7444d","contributors":{"authors":[{"text":"Udevitz, Mark S. 0000-0003-4659-138X mudevitz@usgs.gov","orcid":"https://orcid.org/0000-0003-4659-138X","contributorId":3189,"corporation":false,"usgs":true,"family":"Udevitz","given":"Mark","email":"mudevitz@usgs.gov","middleInitial":"S.","affiliations":[{"id":116,"text":"Alaska Science Center Biology MFEB","active":true,"usgs":true}],"preferred":true,"id":420888,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jay, C.V. 0000-0002-9559-2189","orcid":"https://orcid.org/0000-0002-9559-2189","contributorId":67827,"corporation":false,"usgs":true,"family":"Jay","given":"C.V.","affiliations":[],"preferred":false,"id":420887,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cody, M.B.","contributorId":43154,"corporation":false,"usgs":true,"family":"Cody","given":"M.B.","email":"","affiliations":[],"preferred":false,"id":420886,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70029043,"text":"70029043 - 2005 - Cassini Visual and Infrared Mapping Spectrometer observations of Iapetus: Detection of CO2","interactions":[],"lastModifiedDate":"2012-03-12T17:20:59","indexId":"70029043","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":917,"text":"Astrophysical Journal","active":true,"publicationSubtype":{"id":10}},"title":"Cassini Visual and Infrared Mapping Spectrometer observations of Iapetus: Detection of CO2","docAbstract":"The Visual and Infrared Mapping Spectrometer (VIMS) instrument aboard the Cassini spacecraft obtained its first spectral map of the satellite lapetus in which new absorption bands are seen in the spectra of both the low-albedo hemisphere and the H2O ice-rich hemisphere. Carbon dioxide is identified in the low-albedo material, probably as a photochemically produced molecule that is trapped in H2O ice or in some mineral or complex organic solid. Other absorption bands are unidentified. The spectrum of the low-albedo hemisphere is satisfactorily modeled with a combination of organic tholin, poly-HCN, and small amounts of H2O ice and Fe 2O3. The high-albedo hemisphere is modeled with H 2O ice slightly darkened with tholin. The detection of CO2 in the low-albedo material on the leading hemisphere supports the contention that it is carbon-bearing material from an external source that has been swept up by the satellite's orbital motion. ?? 2005. The American Astronomical Society. All rights reserved.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Astrophysical Journal","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1086/429800","issn":"0004637X","usgsCitation":"Buratti, B.J., Cruikshank, D.P., Brown, R.H., Clark, R.N., Bauer, J., Jaumann, R., McCord, T.B., Simonelli, D., Hibbitts, C.A., Hansen, G.B., Owen, T., Baines, K.H., Bellucci, G., Bibring, J., Capaccioni, F., Cerroni, P., Coradini, A., Drossart, P., Formisano, V., Langevin, Y., Matson, D.L., Mennella, V., Nelson, R., Nicholson, P.D., Sicardy, B., Sotin, C., Roush, T.L., Soderlund, K., and Muradyan, A., 2005, Cassini Visual and Infrared Mapping Spectrometer observations of Iapetus: Detection of CO2: Astrophysical Journal, v. 622, no. 2 II, https://doi.org/10.1086/429800.","costCenters":[],"links":[{"id":477952,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1086/429800","text":"Publisher Index Page"},{"id":236353,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":209680,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1086/429800"}],"volume":"622","issue":"2 II","noUsgsAuthors":false,"publicationDate":"2005-03-08","publicationStatus":"PW","scienceBaseUri":"5059f38ee4b0c8380cd4b899","contributors":{"authors":[{"text":"Buratti, B. J.","contributorId":69280,"corporation":false,"usgs":false,"family":"Buratti","given":"B.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":421093,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cruikshank, D. P.","contributorId":51434,"corporation":false,"usgs":false,"family":"Cruikshank","given":"D.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":421086,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brown, R. H.","contributorId":19931,"corporation":false,"usgs":false,"family":"Brown","given":"R.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":421076,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Clark, R. N.","contributorId":6568,"corporation":false,"usgs":true,"family":"Clark","given":"R.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":421074,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Bauer, J.M.","contributorId":88543,"corporation":false,"usgs":true,"family":"Bauer","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":421100,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Jaumann, R.","contributorId":81232,"corporation":false,"usgs":false,"family":"Jaumann","given":"R.","email":"","affiliations":[],"preferred":false,"id":421097,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"McCord, T. B.","contributorId":69695,"corporation":false,"usgs":false,"family":"McCord","given":"T.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":421094,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Simonelli, D.P.","contributorId":42373,"corporation":false,"usgs":true,"family":"Simonelli","given":"D.P.","email":"","affiliations":[],"preferred":false,"id":421083,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Hibbitts, C. A.","contributorId":21703,"corporation":false,"usgs":false,"family":"Hibbitts","given":"C.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":421077,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Hansen, G. B.","contributorId":98478,"corporation":false,"usgs":false,"family":"Hansen","given":"G.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":421102,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Owen, T.C.","contributorId":62603,"corporation":false,"usgs":true,"family":"Owen","given":"T.C.","email":"","affiliations":[],"preferred":false,"id":421092,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Baines, K. H.","contributorId":37868,"corporation":false,"usgs":false,"family":"Baines","given":"K.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":421081,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Bellucci, G.","contributorId":46256,"corporation":false,"usgs":true,"family":"Bellucci","given":"G.","email":"","affiliations":[],"preferred":false,"id":421085,"contributorType":{"id":1,"text":"Authors"},"rank":13},{"text":"Bibring, J.-P.","contributorId":86083,"corporation":false,"usgs":true,"family":"Bibring","given":"J.-P.","email":"","affiliations":[],"preferred":false,"id":421098,"contributorType":{"id":1,"text":"Authors"},"rank":14},{"text":"Capaccioni, F.","contributorId":90900,"corporation":false,"usgs":true,"family":"Capaccioni","given":"F.","email":"","affiliations":[],"preferred":false,"id":421101,"contributorType":{"id":1,"text":"Authors"},"rank":15},{"text":"Cerroni, P.","contributorId":7869,"corporation":false,"usgs":true,"family":"Cerroni","given":"P.","affiliations":[],"preferred":false,"id":421075,"contributorType":{"id":1,"text":"Authors"},"rank":16},{"text":"Coradini, A.","contributorId":34679,"corporation":false,"usgs":true,"family":"Coradini","given":"A.","affiliations":[],"preferred":false,"id":421080,"contributorType":{"id":1,"text":"Authors"},"rank":17},{"text":"Drossart, P.","contributorId":29574,"corporation":false,"usgs":true,"family":"Drossart","given":"P.","affiliations":[],"preferred":false,"id":421079,"contributorType":{"id":1,"text":"Authors"},"rank":18},{"text":"Formisano, V.","contributorId":44694,"corporation":false,"usgs":true,"family":"Formisano","given":"V.","email":"","affiliations":[],"preferred":false,"id":421084,"contributorType":{"id":1,"text":"Authors"},"rank":19},{"text":"Langevin, Y.","contributorId":24900,"corporation":false,"usgs":true,"family":"Langevin","given":"Y.","email":"","affiliations":[],"preferred":false,"id":421078,"contributorType":{"id":1,"text":"Authors"},"rank":20},{"text":"Matson, D. L.","contributorId":59940,"corporation":false,"usgs":false,"family":"Matson","given":"D.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":421091,"contributorType":{"id":1,"text":"Authors"},"rank":21},{"text":"Mennella, V.","contributorId":88522,"corporation":false,"usgs":true,"family":"Mennella","given":"V.","affiliations":[],"preferred":false,"id":421099,"contributorType":{"id":1,"text":"Authors"},"rank":22},{"text":"Nelson, R.M.","contributorId":38316,"corporation":false,"usgs":true,"family":"Nelson","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":421082,"contributorType":{"id":1,"text":"Authors"},"rank":23},{"text":"Nicholson, P. D.","contributorId":54330,"corporation":false,"usgs":false,"family":"Nicholson","given":"P.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":421089,"contributorType":{"id":1,"text":"Authors"},"rank":24},{"text":"Sicardy, B.","contributorId":57622,"corporation":false,"usgs":true,"family":"Sicardy","given":"B.","affiliations":[],"preferred":false,"id":421090,"contributorType":{"id":1,"text":"Authors"},"rank":25},{"text":"Sotin, Christophe","contributorId":53924,"corporation":false,"usgs":false,"family":"Sotin","given":"Christophe","email":"","affiliations":[],"preferred":false,"id":421088,"contributorType":{"id":1,"text":"Authors"},"rank":26},{"text":"Roush, T. L.","contributorId":77661,"corporation":false,"usgs":false,"family":"Roush","given":"T.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":421095,"contributorType":{"id":1,"text":"Authors"},"rank":27},{"text":"Soderlund, K.","contributorId":80883,"corporation":false,"usgs":true,"family":"Soderlund","given":"K.","email":"","affiliations":[],"preferred":false,"id":421096,"contributorType":{"id":1,"text":"Authors"},"rank":28},{"text":"Muradyan, A.","contributorId":52380,"corporation":false,"usgs":true,"family":"Muradyan","given":"A.","email":"","affiliations":[],"preferred":false,"id":421087,"contributorType":{"id":1,"text":"Authors"},"rank":29}]}}
,{"id":70029184,"text":"70029184 - 2005 - Generation and validation of characteristic spectra from EO1 Hyperion image data for detecting the occurrence of the invasive species, Chinese tallow","interactions":[],"lastModifiedDate":"2012-03-12T17:20:48","indexId":"70029184","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2068,"text":"International Journal of Remote Sensing","active":true,"publicationSubtype":{"id":10}},"title":"Generation and validation of characteristic spectra from EO1 Hyperion image data for detecting the occurrence of the invasive species, Chinese tallow","docAbstract":"Chinese tallow (Triadica sebifera) is an invasive tree that is spreading throughout the south-eastern United States and now into the west, and in many places causing extensive change to native habitat and associated wildlife. Detecting and mapping the relative distribution of this species is important to its control and eradication. To map the relative distribution of Chinese tallow within a southwestern Louisiana coastal wetland to upland environment, Earth Observing 1 (EO1) satellite Hyperion sensor hyperspectral image data were combined with a subpixel extraction method that modelled characteristic spectra from the image data without requiring a priori characteristic spectra. Because of the low percentage occurrences of Chinese tallow and high spectral covariation in the environment, unique validation and verification methods were implemented, relying on simultaneous collection of field canopy reflectance spectra and subsequent classification of canopy compositions. The subpixel extraction method produced five characteristic spectra, which we further refined to four that adequately represented the field spectra, as well as the Hyperion imaged canopy reflectance datasets. Characteristic spectra were designated as senescing foliage, cypress-tupelo trees, and trees without leaves; shadows and green vegetation; senescing Chinese tallow with yellow leaves and yellowing foliage; and senescing Chinese tallow with red leaves ('red tallow'). About 81% (n=34) of the field and 78% (n=33) of the Hyperion imaged characteristic spectra associated with 'red tallow' were explained by the compositions generated in the field slide classifications. ?? 2005 US Government.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"International Journal of Remote Sensing","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1080/01431160512331326710","issn":"01431161","usgsCitation":"Ramsey, E., Rangoonwala, A., Nelson, G., Ehrlich, R., and Martella, K., 2005, Generation and validation of characteristic spectra from EO1 Hyperion image data for detecting the occurrence of the invasive species, Chinese tallow: International Journal of Remote Sensing, v. 26, no. 8, p. 1611-1636, https://doi.org/10.1080/01431160512331326710.","startPage":"1611","endPage":"1636","numberOfPages":"26","costCenters":[],"links":[{"id":210859,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1080/01431160512331326710"},{"id":237906,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"26","issue":"8","noUsgsAuthors":false,"publicationDate":"2007-02-22","publicationStatus":"PW","scienceBaseUri":"505a1550e4b0c8380cd54d54","contributors":{"authors":[{"text":"Ramsey, Elijah W. III 0000-0002-4518-5796","orcid":"https://orcid.org/0000-0002-4518-5796","contributorId":72769,"corporation":false,"usgs":true,"family":"Ramsey","given":"Elijah W.","suffix":"III","affiliations":[{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"preferred":false,"id":421663,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rangoonwala, A. 0000-0002-0556-0598","orcid":"https://orcid.org/0000-0002-0556-0598","contributorId":95248,"corporation":false,"usgs":true,"family":"Rangoonwala","given":"A.","affiliations":[{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"preferred":false,"id":421664,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Nelson, G.","contributorId":101072,"corporation":false,"usgs":true,"family":"Nelson","given":"G.","affiliations":[],"preferred":false,"id":421665,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ehrlich, R.","contributorId":72192,"corporation":false,"usgs":true,"family":"Ehrlich","given":"R.","email":"","affiliations":[],"preferred":false,"id":421662,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Martella, K.","contributorId":42417,"corporation":false,"usgs":true,"family":"Martella","given":"K.","affiliations":[],"preferred":false,"id":421661,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70029094,"text":"70029094 - 2005 - Rupture dynamics with energy loss outside the slip zone","interactions":[],"lastModifiedDate":"2012-03-12T17:20:53","indexId":"70029094","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2314,"text":"Journal of Geophysical Research B: Solid Earth","active":true,"publicationSubtype":{"id":10}},"title":"Rupture dynamics with energy loss outside the slip zone","docAbstract":"Energy loss in a fault damage zone, outside the slip zone, contributes to the fracture energy that determines rupture velocity of an earthquake. A nonelastic two-dimensional dynamic calculation is done in which the slip zone is modeled as a fault plane and material off the fault is subject to a Coulomb yield condition. In a mode 2 crack-like solution in which an abrupt uniform drop of shear traction on the fault spreads from a point, Coulomb yielding occurs on the extensional side of the fault. Plastic strain is distributed with uniform magnitude along the fault, and it has a thickness normal to the fault proportional to propagation distance. Energy loss off the fault is also proportional to propagation distance, and it can become much larger than energy loss on the fault specified by the fault constitutive relation. The slip velocity function could be produced in an equivalent elastic problem by a slip-weakening friction law with breakdown slip Dc increasing with distance. Fracture energy G and equivalent Dc will be different in ruptures with different initiation points and stress drops, so they are not constitutive properties; they are determined by the dynamic solution that arrives at a particular point. Peak slip velocity is, however, a property of a fault location. Nonelastic response can be mimicked by imposing a limit on slip velocity on a fault in an elastic medium.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Geophysical Research B: Solid Earth","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1029/2004JB003191","issn":"01480227","usgsCitation":"Andrews, D., 2005, Rupture dynamics with energy loss outside the slip zone: Journal of Geophysical Research B: Solid Earth, v. 110, no. 1, p. 1-14, https://doi.org/10.1029/2004JB003191.","startPage":"1","endPage":"14","numberOfPages":"14","costCenters":[],"links":[{"id":478009,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1029/2004jb003191","text":"Publisher Index Page"},{"id":210658,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1029/2004JB003191"},{"id":237650,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"110","issue":"1","noUsgsAuthors":false,"publicationDate":"2005-01-20","publicationStatus":"PW","scienceBaseUri":"505aaecee4b0c8380cd87225","contributors":{"authors":[{"text":"Andrews, D.J.","contributorId":7416,"corporation":false,"usgs":true,"family":"Andrews","given":"D.J.","email":"","affiliations":[],"preferred":false,"id":421303,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70031333,"text":"70031333 - 2005 - A simulation of the hydrothermal response to the Chesapeake Bay bolide impact","interactions":[],"lastModifiedDate":"2012-03-12T17:21:15","indexId":"70031333","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1765,"text":"Geofluids","active":true,"publicationSubtype":{"id":10}},"title":"A simulation of the hydrothermal response to the Chesapeake Bay bolide impact","docAbstract":"Groundwater more saline than seawater has been discovered in the tsunami breccia of the Chesapeake Bay impact Crater. One hypothesis for the origin of this brine is that it may be a liquid residual following steam separation in a hydrothermal system that evolved following the impact. Initial scoping calculations have demonstrated that it is feasible such a residual brine could have remained in the crater for the 35 million years since impact. Numerical simulations have been conducted using the code HYDROTHERM to test whether or not conditions were suitable in the millennia following the impact for the development of a steam phase in the hydrothermal system. Hydraulic and thermal parameters were estimated for the bedrock underlying the crater and the tsunami breccia that fills the crater. Simulations at three different breccia permeabilities suggest that the type of hydrothermal system that might have developed would have been very sensitive to the permeability. A relatively low breccia permeability (1 ?? 10-16 m2) results in a system partitioned into a shallow water phase and a deeper superheated steam phase. A moderate breccia permeability (1 ?? 10-15 m2 ) results in a system with regionally extensive multiphase conditions. A relatively high breccia permeability (1 ?? 10-14 m2 ) results in a system dominated by warm-water convection cells. The permeability of the crater breccia could have had any of these values at given depths and times during the hydrothermal system evolution as the sediments compacted. The simulations were not able to take into account transient permeability conditions, or equations of state that account for the salt content of seawater. Results suggest, however, that it is likely that steam conditions existed at some time in the system following impact, providing additional evidence that is consistent with a hydrothermal origin for the crater brine. ?? Blackwell Publishing Ltd.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Geofluids","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1111/j.1468-8123.2005.00110.x","issn":"14688115","usgsCitation":"Sanford, W., 2005, A simulation of the hydrothermal response to the Chesapeake Bay bolide impact: Geofluids, v. 5, no. 3, p. 185-201, https://doi.org/10.1111/j.1468-8123.2005.00110.x.","startPage":"185","endPage":"201","numberOfPages":"17","costCenters":[],"links":[{"id":212257,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1111/j.1468-8123.2005.00110.x"},{"id":239718,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"5","issue":"3","noUsgsAuthors":false,"publicationDate":"2005-07-14","publicationStatus":"PW","scienceBaseUri":"5059e596e4b0c8380cd46e58","contributors":{"authors":[{"text":"Sanford, W. E. 0000-0002-6624-0280","orcid":"https://orcid.org/0000-0002-6624-0280","contributorId":102112,"corporation":false,"usgs":true,"family":"Sanford","given":"W. E.","affiliations":[],"preferred":false,"id":431087,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70031332,"text":"70031332 - 2005 - Cryopreservation of sperm of red abalone (Haliotis rufescens)","interactions":[],"lastModifiedDate":"2019-10-02T16:39:42","indexId":"70031332","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2455,"text":"Journal of Shellfish Research","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Cryopreservation of sperm of red abalone (<i>Haliotis rufescens</i>)","title":"Cryopreservation of sperm of red abalone (Haliotis rufescens)","docAbstract":"<p><span>Abalone culture, a developing industry in Baja California, Mexico, would benefit from genetic improvement and controlled breeding. The use of cryopreserved sperm would allow germplasm availability, and this study was designed to develop sperm cryopreservation protocols for red abalone&nbsp;</span><span class=\"genus-species\">Haliotis rufescens</span><span>. The acute toxic effects of the cryoprotectants dimethyl sulfoxide (DMSO), propylene glycol (PG), and glycerol (GLY) were assessed after suspending sperm in different concentrations, whereby cryoprotectant treatments of 10% DMSO and 10% GLY equilibrated for 10 min yielded the highest range of motile sperm in preliminary freezing trials and were used for cryopreservation studies. To determine effective cooling rates, three freezing chambers were tested. Replicate samples of sperm from 4 males were placed in 0.5-mL French straws and frozen using a commercial freezing chamber (CFC) used for bull sperm, a programmable rate chamber (PRC), and a manually controlled styrofoam chamber (MCC). For the CFC, the cooling rate was 16°C/min, from 4°C to −140°C. For the PRC and MCC, it was 1°C/min, from −20°C to −30°C. The samples were held at −30°C for 5 min before being plunged into liquid nitrogen (−196°C) for storage, and each sample was thawed in a water bath at 45°C for 8 s. The quality of thawed sperm was determined by estimating percent motility, evaluating membrane integrity using a dual-staining technique and flow cytometry, and estimating fertilization rate. Statistical analyses were performed using 2-way ANOVA where chamber and treatment were the independent variables. Sperm quality parameters were independent. For motilities, a significant interaction was noted between the cryoprotective treatment and the chamber type, whereby motilities for DMSO and GLY were higher (</span><i>P</i><span>&nbsp;= 0.0055) using MCC. Membrane integrities were significantly lower after using the PRC than the CFC or the MCC (</span><i>P</i><span>&nbsp;= 0.0167). The highest post-thaw motility (48 ± 7%) was found using sperm suspended in 10% glycerol and frozen in the MCC. The highest percent of intact membranes (56 ± 11%) was for sperm suspended in 10% glycerol and frozen in the CFC. The highest fertilization rate (29 ± 10%) was with samples frozen with 10% glycerol in the CFC. The use of cryopreserved sperm from red abalone provides an alternative breeding option for culture and the protocols delineated are the first developed for this species.</span></p>","language":"English","publisher":"BioOne","doi":"10.2983/0730-8000(2005)24[415:COSORA]2.0.CO;2","issn":"07308000","usgsCitation":"Salinas-Flores, L., Paniagua-Chavez, C.G., Jenkins, J., and Tiersch, T., 2005, Cryopreservation of sperm of red abalone (Haliotis rufescens): Journal of Shellfish Research, v. 24, no. 2, p. 415-420, https://doi.org/10.2983/0730-8000(2005)24[415:COSORA]2.0.CO;2.","productDescription":"6 p.","startPage":"415","endPage":"420","numberOfPages":"6","costCenters":[{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true}],"links":[{"id":239685,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Mexico","state":"Baja California","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -117.59765625,\n              28.07198030177986\n            ],\n            [\n              -112.87353515625,\n              28.07198030177986\n            ],\n            [\n              -112.87353515625,\n              32.676372772089834\n            ],\n            [\n              -117.59765625,\n              32.676372772089834\n            ],\n            [\n              -117.59765625,\n              28.07198030177986\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"24","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059fcf4e4b0c8380cd4e53d","contributors":{"authors":[{"text":"Salinas-Flores, L.","contributorId":82127,"corporation":false,"usgs":true,"family":"Salinas-Flores","given":"L.","email":"","affiliations":[],"preferred":false,"id":431086,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Paniagua-Chavez, C. G.","contributorId":9842,"corporation":false,"usgs":true,"family":"Paniagua-Chavez","given":"C.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":431083,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Jenkins, J.A. 0000-0002-5087-0894","orcid":"https://orcid.org/0000-0002-5087-0894","contributorId":51703,"corporation":false,"usgs":true,"family":"Jenkins","given":"J.A.","affiliations":[{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"preferred":false,"id":431084,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Tiersch, T.R.","contributorId":76051,"corporation":false,"usgs":true,"family":"Tiersch","given":"T.R.","affiliations":[],"preferred":false,"id":431085,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70031331,"text":"70031331 - 2005 - Metamorphosis of two amphibian species after chronic cadmium exposure in outdoor aquatic mesocosms","interactions":[],"lastModifiedDate":"2017-05-24T12:25:46","indexId":"70031331","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1571,"text":"Environmental Toxicology and Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"Metamorphosis of two amphibian species after chronic cadmium exposure in outdoor aquatic mesocosms","docAbstract":"<p><span>Amphibian larvae at contaminated sites may experience an alteration of metamorphic traits and survival compared to amphibians in uncontaminated conditions. Effects of chronic cadmium (Cd) exposure on the metamorphosis of American toads (</span><i>Bufo americanus</i><span>) and southern leopard frogs (</span><i>Rana sphenocephala</i><span>) were determined. The two species were reared separately from shortly after hatching through metamorphosis in outdoor mesocosms (1,325-L polyethylene cattle tanks) that simulated natural ponds and enhanced environmental realism relative to the laboratory. Both species exhibited a decrease in survival with increasing initial nominal aqueous Cd concentration. Cadmium treatment did not influence mass at metamorphosis for either species when survival was included as a covariate, but increased the age at metamorphosis for the American toads. The whole body Cd content of metamorphs increased with aqueous Cd treatment level for both species, and the American toads tended to possess more elevated residues. Cadmium quickly partitioned out of the water column and accumulated in and altered the abundance of the tadpoles' diet. Cadmium-contaminated sites may produce fewer metamorphs, and those that survive will metamorphose later and contain Cd. Interspecific differences in the response variables illustrate the importance of testing multiple species when assessing risk.</span></p>","language":"English","publisher":"Wiley","doi":"10.1897/04-568R.1","issn":"07307268","usgsCitation":"James, S., Little, E.E., and Semlitsch, R.D., 2005, Metamorphosis of two amphibian species after chronic cadmium exposure in outdoor aquatic mesocosms: Environmental Toxicology and Chemistry, v. 24, no. 8, p. 1994-2001, https://doi.org/10.1897/04-568R.1.","productDescription":"8 p.","startPage":"1994","endPage":"2001","numberOfPages":"8","costCenters":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"links":[{"id":239684,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":212228,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1897/04-568R.1"}],"volume":"24","issue":"8","noUsgsAuthors":false,"publicationDate":"2005-08-01","publicationStatus":"PW","scienceBaseUri":"505a5508e4b0c8380cd6d0de","contributors":{"authors":[{"text":"James, S.M.","contributorId":8267,"corporation":false,"usgs":true,"family":"James","given":"S.M.","email":"","affiliations":[],"preferred":false,"id":431080,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Little, E. E.","contributorId":13187,"corporation":false,"usgs":true,"family":"Little","given":"E.","email":"","middleInitial":"E.","affiliations":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"preferred":false,"id":431081,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Semlitsch, R. D.","contributorId":22522,"corporation":false,"usgs":true,"family":"Semlitsch","given":"R.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":431082,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70029136,"text":"70029136 - 2005 - Host population persistence in the face of introduced vector-borne diseases: Hawaii amakihi and avian malaria","interactions":[],"lastModifiedDate":"2018-06-20T20:10:18","indexId":"70029136","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3165,"text":"Proceedings of the National Academy of Sciences of the United States of America","active":true,"publicationSubtype":{"id":10}},"title":"Host population persistence in the face of introduced vector-borne diseases: Hawaii amakihi and avian malaria","docAbstract":"The past quarter century has seen an unprecedented increase in the number of new and emerging infectious diseases throughout the world, with serious implications for human and wildlife populations. We examined host persistence in the face of introduced vector-borne diseases in Hawaii, where introduced avian malaria and introduced vectors have had a negative impact on most populations of Hawaiian forest birds for nearly a century. We studied birds, parasites, and vectors in nine study areas from 0 to 1,800 m on Mauna Loa Volcano, Hawaii from January to October, 2002. Contrary to predictions of prior work, we found that Hawaii amakihi (Hemignathus virens), a native species susceptible to malaria, comprised from 24.5% to 51.9% of the avian community at three low-elevation forests (55-270 m). Amakihi were more abundant at low elevations than at disease-free high elevations, and were resident and breeding there. Infection rates were 24-40% by microscopy and 55-83% by serology, with most infected individuals experiencing low-intensity, chronic infections. Mosquito trapping and diagnostics provided strong evidence for year-round local transmission. Moreover, we present evidence that Hawaii amakihi have increased in low elevation habitats on south-eastern Hawaii Island over the past decade. The recent emergent phenomenon of recovering amakihi populations at low elevations, despite extremely high prevalence of avian malaria, suggests that ecological or evolutionary processes acting on hosts or parasites have allowed this species to recolonize low-elevation habitats. A better understanding of the mechanisms allowing coexistence of hosts and parasites may ultimately lead to tools for mitigating disease impacts on wildlife and human populations.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Proceedings of the National Academy of Sciences of the United States of America","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1073/pnas.0409454102","issn":"00278424","usgsCitation":"Woodworth, B., Atkinson, C., Lapointe, D., Hart, P., Spiegel, C., Tweed, E., Henneman, C., LeBrun, J., Denette, T., DeMots, R., Kozar, K., Triglia, D., Lease, D., Gregor, A., Smith, T., and Duffy, D., 2005, Host population persistence in the face of introduced vector-borne diseases: Hawaii amakihi and avian malaria: Proceedings of the National Academy of Sciences of the United States of America, v. 102, no. 5, p. 1531-1536, https://doi.org/10.1073/pnas.0409454102.","startPage":"1531","endPage":"1536","numberOfPages":"6","costCenters":[],"links":[{"id":477914,"rank":10000,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://doi.org/10.1073/pnas.0409454102","text":"External Repository"},{"id":237792,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":210770,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1073/pnas.0409454102"}],"volume":"102","issue":"5","noUsgsAuthors":false,"publicationDate":"2005-01-24","publicationStatus":"PW","scienceBaseUri":"505a3230e4b0c8380cd5e5ba","contributors":{"authors":[{"text":"Woodworth, B.L.","contributorId":88538,"corporation":false,"usgs":true,"family":"Woodworth","given":"B.L.","email":"","affiliations":[],"preferred":false,"id":421472,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Atkinson, C. T.","contributorId":29349,"corporation":false,"usgs":false,"family":"Atkinson","given":"C. T.","affiliations":[],"preferred":false,"id":421464,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lapointe, D.A.","contributorId":69691,"corporation":false,"usgs":true,"family":"Lapointe","given":"D.A.","email":"","affiliations":[],"preferred":false,"id":421469,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hart, P.J.","contributorId":104260,"corporation":false,"usgs":true,"family":"Hart","given":"P.J.","email":"","affiliations":[],"preferred":false,"id":421474,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Spiegel, C.S.","contributorId":29198,"corporation":false,"usgs":true,"family":"Spiegel","given":"C.S.","email":"","affiliations":[],"preferred":false,"id":421463,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Tweed, E.J.","contributorId":35518,"corporation":false,"usgs":true,"family":"Tweed","given":"E.J.","email":"","affiliations":[],"preferred":false,"id":421465,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Henneman, C.","contributorId":64879,"corporation":false,"usgs":true,"family":"Henneman","given":"C.","affiliations":[],"preferred":false,"id":421467,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"LeBrun, J.","contributorId":67716,"corporation":false,"usgs":true,"family":"LeBrun","given":"J.","email":"","affiliations":[],"preferred":false,"id":421468,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Denette, T.","contributorId":73402,"corporation":false,"usgs":true,"family":"Denette","given":"T.","email":"","affiliations":[],"preferred":false,"id":421470,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"DeMots, R.","contributorId":42018,"corporation":false,"usgs":true,"family":"DeMots","given":"R.","email":"","affiliations":[],"preferred":false,"id":421466,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Kozar, K.L.","contributorId":14631,"corporation":false,"usgs":true,"family":"Kozar","given":"K.L.","email":"","affiliations":[],"preferred":false,"id":421461,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Triglia, D.","contributorId":80481,"corporation":false,"usgs":true,"family":"Triglia","given":"D.","affiliations":[],"preferred":false,"id":421471,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Lease, Dan","contributorId":105907,"corporation":false,"usgs":false,"family":"Lease","given":"Dan","email":"","affiliations":[],"preferred":false,"id":421476,"contributorType":{"id":1,"text":"Authors"},"rank":13},{"text":"Gregor, A.","contributorId":96892,"corporation":false,"usgs":true,"family":"Gregor","given":"A.","email":"","affiliations":[],"preferred":false,"id":421473,"contributorType":{"id":1,"text":"Authors"},"rank":14},{"text":"Smith, T.","contributorId":28032,"corporation":false,"usgs":true,"family":"Smith","given":"T.","affiliations":[],"preferred":false,"id":421462,"contributorType":{"id":1,"text":"Authors"},"rank":15},{"text":"Duffy, D.","contributorId":105519,"corporation":false,"usgs":true,"family":"Duffy","given":"D.","email":"","affiliations":[],"preferred":false,"id":421475,"contributorType":{"id":1,"text":"Authors"},"rank":16}]}}
,{"id":70029103,"text":"70029103 - 2005 - Consequences of harvesting for genetic diversity in American ginseng (Panax quinquefolius L.): A simulation study","interactions":[],"lastModifiedDate":"2012-03-12T17:20:48","indexId":"70029103","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1006,"text":"Biodiversity and Conservation","active":true,"publicationSubtype":{"id":10}},"title":"Consequences of harvesting for genetic diversity in American ginseng (Panax quinquefolius L.): A simulation study","docAbstract":"American ginseng, Panax quinquefolius L., is one of the most heavily traded medicinal plants in North America. The effect of harvest on genetic diversity in ginseng was measured with a single generation culling simulation program. Culling scenarios included random harvest at varying levels, legal limit random harvest and legal limit mature plant harvest. The legal limit was determined by the proportion of legally harvestable plants per population (% mature plants per population). Random harvest at varying levels resulted in significant loss of genetic diversity, especially allelic richness. Relative to initial levels, average within-population genetic diversity (H e) was significantly lower when plants were culled randomly at the legal limit (Mann-Whitney U = 430, p < 0.001) or when only mature plants were culled (Mann-Whitney U = 394, p < 0.01). Within-population genetic diversity was significantly higher with legal limit mature plant harvest (H e = 0.068) than when plants were culled randomly at the legal limit (H e = 0.064; U = 202, p < 0.01). Based on these simulations of harvest over one generation, we recommend that harvesting fewer than the proportion of mature plants could reduce the negative genetic effects of harvest on ginseng populations. ?? Springer 2005.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Biodiversity and Conservation","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1007/s10531-004-7308-7","issn":"09603115","usgsCitation":"Cruse-Sanders, J., Hamrick, J., and Ahumada, J., 2005, Consequences of harvesting for genetic diversity in American ginseng (Panax quinquefolius L.): A simulation study: Biodiversity and Conservation, v. 14, no. 2, p. 493-504, https://doi.org/10.1007/s10531-004-7308-7.","startPage":"493","endPage":"504","numberOfPages":"12","costCenters":[],"links":[{"id":237791,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":210769,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/s10531-004-7308-7"}],"volume":"14","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f9d5e4b0c8380cd4d7e0","contributors":{"authors":[{"text":"Cruse-Sanders, J. M.","contributorId":8281,"corporation":false,"usgs":true,"family":"Cruse-Sanders","given":"J. M.","affiliations":[],"preferred":false,"id":421336,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hamrick, J.L.","contributorId":70991,"corporation":false,"usgs":true,"family":"Hamrick","given":"J.L.","email":"","affiliations":[],"preferred":false,"id":421338,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ahumada, J.A.","contributorId":51710,"corporation":false,"usgs":true,"family":"Ahumada","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":421337,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70031303,"text":"70031303 - 2005 - Experimental and geochemical evidence for derivation of the El Capitan Granite, California, by partial melting of hydrous gabbroic lower crust","interactions":[],"lastModifiedDate":"2019-05-10T08:40:11","indexId":"70031303","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1336,"text":"Contributions to Mineralogy and Petrology","active":true,"publicationSubtype":{"id":10}},"title":"Experimental and geochemical evidence for derivation of the El Capitan Granite, California, by partial melting of hydrous gabbroic lower crust","docAbstract":"<p><span>Partial melting of mafic intrusions recently emplaced into the lower crust can produce voluminous silicic magmas with isotopic ratios similar to their mafic sources. Low-temperature (825 and 850°C) partial melts synthesized at 700&nbsp;MPa in biotite-hornblende gabbros from the central Sierra Nevada batholith (Sisson et al. in Contrib Mineral Petrol 148:635–661, 2005) have major-element and modeled trace-element (REE, Rb, Ba, Sr, Th, U) compositions matching those of the Cretaceous El Capitan Granite, a prominent granite and silicic granodiorite pluton in the central part of the Sierra Nevada batholith (Yosemite, CA, USA) locally mingled with coeval, isotopically similar quartz diorite through gabbro intrusions (Ratajeski et al. in Geol Soc Am Bull 113:1486–1502, 2001). These results are evidence that the El Capitan Granite, and perhaps similar intrusions in the Sierra Nevada batholith with lithospheric-mantle-like isotopic values, were extracted from LILE-enriched, hydrous (hornblende-bearing) gabbroic rocks in the Sierran lower crust. Granitic partial melts derived by this process may also be silicic end members for mixing events leading to large-volume intermediate composition Sierran plutons such as the Cretaceous Lamarck Granodiorite. Voluminous gabbroic residues of partial melting may be lost to the mantle by their conversion to garnet-pyroxene assemblages during batholithic magmatic crustal thickening.</span></p>","language":"English","doi":"10.1007/s00410-005-0677-4","issn":"00107999","usgsCitation":"Ratajeski, K., Sisson, T.W., and Glazner, A.F., 2005, Experimental and geochemical evidence for derivation of the El Capitan Granite, California, by partial melting of hydrous gabbroic lower crust: Contributions to Mineralogy and Petrology, v. 149, no. 6, p. 713-734, https://doi.org/10.1007/s00410-005-0677-4.","productDescription":"22 p.","startPage":"713","endPage":"734","numberOfPages":"22","costCenters":[{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true}],"links":[{"id":239815,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":212344,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/s00410-005-0677-4"}],"volume":"149","issue":"6","noUsgsAuthors":false,"publicationDate":"2005-05-26","publicationStatus":"PW","scienceBaseUri":"505a0dc0e4b0c8380cd53192","contributors":{"authors":[{"text":"Ratajeski, K.","contributorId":58799,"corporation":false,"usgs":true,"family":"Ratajeski","given":"K.","email":"","affiliations":[],"preferred":false,"id":430964,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sisson, T. W.","contributorId":108120,"corporation":false,"usgs":true,"family":"Sisson","given":"T.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":430966,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Glazner, A. F.","contributorId":91639,"corporation":false,"usgs":false,"family":"Glazner","given":"A.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":430965,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70031301,"text":"70031301 - 2005 - Comment on \"Coral reef calcification and climate change: The effect of ocean warming\"","interactions":[],"lastModifiedDate":"2012-03-12T17:21:13","indexId":"70031301","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":"Comment on \"Coral reef calcification and climate change: The effect of ocean warming\"","docAbstract":"McNeil et al. [2004] attempt to address an important question about the interactions of temperature and carbonate chemistry on calcification, but their projected values of reef calcification are based on assumptions that ignore critical observational and experimental literature. Certainly, more research is needed to better understand how changing temperatures and carbonate chemistry will affect not only coral reef calcification, but coral survival. As discussed above, the McNeil et al. [2004] analysis is based on assumptions that exclude potentially important factors and therefore needs to be viewed with caution. Copyright 2005 by the American Geophysical Union.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Geophysical Research Letters","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1029/2004GL022329","issn":"00948276","usgsCitation":"Kleypas, J., Buddemeier, R., Eakin, C., Gattuso, J., Guinotte, J., Hoegh-Guldberg, O., Iglesias-Prieto, R., Jokiel, P., Langdon, C., Skirving, W., and Strong, A., 2005, Comment on \"Coral reef calcification and climate change: The effect of ocean warming\": Geophysical Research Letters, v. 32, no. 8, p. 1-3, https://doi.org/10.1029/2004GL022329.","startPage":"1","endPage":"3","numberOfPages":"3","costCenters":[],"links":[{"id":477736,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1029/2004gl022329","text":"Publisher Index Page"},{"id":212342,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1029/2004GL022329"},{"id":239813,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"32","issue":"8","noUsgsAuthors":false,"publicationDate":"2005-04-20","publicationStatus":"PW","scienceBaseUri":"5059f7e5e4b0c8380cd4cd72","contributors":{"authors":[{"text":"Kleypas, J.A.","contributorId":13221,"corporation":false,"usgs":true,"family":"Kleypas","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":430950,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Buddemeier, R. W.","contributorId":86492,"corporation":false,"usgs":true,"family":"Buddemeier","given":"R. W.","affiliations":[],"preferred":false,"id":430957,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Eakin, C.M.","contributorId":62020,"corporation":false,"usgs":true,"family":"Eakin","given":"C.M.","email":"","affiliations":[],"preferred":false,"id":430953,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Gattuso, J.-P.","contributorId":61194,"corporation":false,"usgs":true,"family":"Gattuso","given":"J.-P.","email":"","affiliations":[],"preferred":false,"id":430952,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Guinotte, J.","contributorId":17831,"corporation":false,"usgs":true,"family":"Guinotte","given":"J.","email":"","affiliations":[],"preferred":false,"id":430951,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Hoegh-Guldberg, O.","contributorId":104706,"corporation":false,"usgs":true,"family":"Hoegh-Guldberg","given":"O.","affiliations":[],"preferred":false,"id":430958,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Iglesias-Prieto, R.","contributorId":79296,"corporation":false,"usgs":true,"family":"Iglesias-Prieto","given":"R.","email":"","affiliations":[],"preferred":false,"id":430955,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Jokiel, P. L.","contributorId":80367,"corporation":false,"usgs":true,"family":"Jokiel","given":"P. L.","affiliations":[],"preferred":false,"id":430956,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Langdon, C.","contributorId":65597,"corporation":false,"usgs":true,"family":"Langdon","given":"C.","email":"","affiliations":[],"preferred":false,"id":430954,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Skirving, W.","contributorId":105914,"corporation":false,"usgs":true,"family":"Skirving","given":"W.","email":"","affiliations":[],"preferred":false,"id":430959,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Strong, A.E.","contributorId":105915,"corporation":false,"usgs":true,"family":"Strong","given":"A.E.","email":"","affiliations":[],"preferred":false,"id":430960,"contributorType":{"id":1,"text":"Authors"},"rank":11}]}}
,{"id":70029029,"text":"70029029 - 2005 - Efficacy of hydrogen peroxide versus formalin treatments to control mortality associated with saprolegniasis on lake trout eggs","interactions":[],"lastModifiedDate":"2012-03-12T17:21:00","indexId":"70029029","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2885,"text":"North American Journal of Aquaculture","active":true,"publicationSubtype":{"id":10}},"title":"Efficacy of hydrogen peroxide versus formalin treatments to control mortality associated with saprolegniasis on lake trout eggs","docAbstract":"We compared the efficacy of hydrogen peroxide versus formalin treatments to control fungal infections on eggs of lake trout Salvelinus namaycush incubated at a hatchery in Wisconsin. Four strains of lake trout eggs were incubated in six vertical-flow Heath incubators; three replicate incubators for each chemical. Each incubator had 13 trays containing approximately 25,000-30,000 eggs/tray. Formalin (1,667 mg/L) or hydrogen peroxide (1,000 mg/L) treatments were administered once daily for 15 min up to the development of visible eye spots in the eggs (eyed egg stage). Eyed and dead eggs were separated using a photoelectric egg sorter, and the number of live and dead eggs was determined volumetrically. In the hydrogen peroxide test group, the bottom trays of each incubator had fungus present on the eggs, whereas no fungus was observed on eggs treated with formalin. The mean percentage of eyed eggs for an incubator treated with formalin (75%) was significantly greater than an incubator treated with hydrogen peroxide (70%). Formalin was the most efficacious therapeutant; however, both therapeutants were effective in increasing lake trout egg survival up to the eyed egg stage. ?? Copyright by the American Fisheries Society 2005.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"North American Journal of Aquaculture","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1577/A04-062.1","issn":"15222055","usgsCitation":"Rach, J., Redman, S., Bast, D., and Gaikowski, M., 2005, Efficacy of hydrogen peroxide versus formalin treatments to control mortality associated with saprolegniasis on lake trout eggs: North American Journal of Aquaculture, v. 67, no. 2, p. 148-154, https://doi.org/10.1577/A04-062.1.","startPage":"148","endPage":"154","numberOfPages":"7","costCenters":[],"links":[{"id":209651,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1577/A04-062.1"},{"id":236318,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"67","issue":"2","noUsgsAuthors":false,"publicationDate":"2005-04-01","publicationStatus":"PW","scienceBaseUri":"505a085fe4b0c8380cd51abd","contributors":{"authors":[{"text":"Rach, J.J.","contributorId":73948,"corporation":false,"usgs":true,"family":"Rach","given":"J.J.","email":"","affiliations":[],"preferred":false,"id":421019,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Redman, S.","contributorId":90094,"corporation":false,"usgs":true,"family":"Redman","given":"S.","email":"","affiliations":[],"preferred":false,"id":421020,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bast, D.","contributorId":101860,"corporation":false,"usgs":true,"family":"Bast","given":"D.","email":"","affiliations":[],"preferred":false,"id":421021,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Gaikowski, M.P. 0000-0002-6507-9341","orcid":"https://orcid.org/0000-0002-6507-9341","contributorId":51685,"corporation":false,"usgs":true,"family":"Gaikowski","given":"M.P.","affiliations":[],"preferred":false,"id":421018,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70029137,"text":"70029137 - 2005 - Relationships between recapture rates from different gears for estimating walleye abundance in northern Wisconsin lakes","interactions":[],"lastModifiedDate":"2012-03-12T17:20:48","indexId":"70029137","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2886,"text":"North American Journal of Fisheries Management","active":true,"publicationSubtype":{"id":10}},"title":"Relationships between recapture rates from different gears for estimating walleye abundance in northern Wisconsin lakes","docAbstract":"Maximizing sampling efficiency and reducing sampling costs are desirable goals for fisheries management agencies. Expensive and labor-intensive methods (such as mark-recapture) are commonly used to estimate the population abundance of walleye Sander vitreus, but more efficient methods may be available. We compared recapture rates from surveys and harvests to evaluate the efficiency of currently used recapture gears and the potential for using gears that require less effort. To evaluate the usefulness of walleye harvest as mark-recapture samples, we used errors-in-variables models to determine whether recapture rates differed between fyke-netting and spearing, electrofishing and spearing, and electrofishing and angling. We found no significant differences between fyke-netting and adult walleye electrofishing recapture rates or between spearing and adult walleye electrofishing recapture rates. In contrast, we found that recapture rates from angling and electrofishing differed significantly in lakes with and without minimum length limits. We concluded that the lack of significant differences between the slopes of some harvest and survey recapture rates may allow the use of harvest recapture rates to estimate walleye abundance, but the biases associated with each gear should be considered. We also concluded that more attention should be given to understanding the biases of recapture gears. ?? Copyright by the American Fisheries Society 2005.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"North American Journal of Fisheries Management","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1577/M03-171.1","issn":"02755947","usgsCitation":"Rogers, M., Hansen, M., and Beard, T., 2005, Relationships between recapture rates from different gears for estimating walleye abundance in northern Wisconsin lakes: North American Journal of Fisheries Management, v. 25, no. 1, p. 195-202, https://doi.org/10.1577/M03-171.1.","startPage":"195","endPage":"202","numberOfPages":"8","costCenters":[],"links":[{"id":477873,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1577/m03-171.1","text":"Publisher Index Page"},{"id":237793,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":210771,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1577/M03-171.1"}],"volume":"25","issue":"1","noUsgsAuthors":false,"publicationDate":"2005-02-01","publicationStatus":"PW","scienceBaseUri":"505aa64ae4b0c8380cd84da3","contributors":{"authors":[{"text":"Rogers, M.W.","contributorId":68929,"corporation":false,"usgs":true,"family":"Rogers","given":"M.W.","email":"","affiliations":[],"preferred":false,"id":421478,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hansen, M.J.","contributorId":39166,"corporation":false,"usgs":true,"family":"Hansen","given":"M.J.","email":"","affiliations":[],"preferred":false,"id":421477,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Beard, T.D. Jr.","contributorId":100160,"corporation":false,"usgs":true,"family":"Beard","given":"T.D.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":421479,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70031675,"text":"70031675 - 2005 - North American Brant: Effects of changes in habitat and climate on population dynamics","interactions":[],"lastModifiedDate":"2016-06-29T16:02:06","indexId":"70031675","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1837,"text":"Global Change Biology","active":true,"publicationSubtype":{"id":10}},"title":"North American Brant: Effects of changes in habitat and climate on population dynamics","docAbstract":"<p>We describe the importance of key habitats used by four nesting populations of nearctic brant (Branta bernicla) and discuss the potential relationship between changes in these habitats and population dynamics of brant. Nearctic brant, in contrast to most geese, rely on marine habitats and native intertidal plants during the non-breeding season, particularly the seagrass, Zostera, and the macroalgae, Ulva. Atlantic and Eastern High Arctic brant have experienced the greatest degradation of their winter habitats (northeastern United States and Ireland, respectively) and have also shown the most plasticity in feeding behavior. Black and Western High Arctic brant of the Pacific Flyway are the most dependent on Zostera, and are undergoing a shift in winter distribution that is likely related to climate change and its associated effects on Zostera dynamics. Variation in breeding propensity of Black Brant associated with winter location and climate strongly suggests that food abundance on the wintering grounds directly affects reproductive performance in these geese. In summer, salt marshes, especially those containing Carex and Puccinellia, are key habitats for raising young, while lake shorelines with fine freshwater grasses and sedges are important for molting birds. Availability and abundance of salt marshes has a direct effect on growth and recruitment of goslings and ultimately, plays an important role in regulating size of local brant populations. ?? 2005 Blackwell Publishing Ltd.</p>","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Global Change Biology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1111/j.1365-2486.2005.00942.x","issn":"13541013","usgsCitation":"Ward, D.H., Reed, A., Sedinger, J.S., Black, J.M., Derksen, D.V., and Castelli, P.M., 2005, North American Brant: Effects of changes in habitat and climate on population dynamics: Global Change Biology, v. 11, no. 6, p. 869-880, https://doi.org/10.1111/j.1365-2486.2005.00942.x.","productDescription":"12 p.","startPage":"869","endPage":"880","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":212219,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1111/j.1365-2486.2005.00942.x"},{"id":239673,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"11","issue":"6","noUsgsAuthors":false,"publicationDate":"2005-05-13","publicationStatus":"PW","scienceBaseUri":"505a67d8e4b0c8380cd734e3","contributors":{"authors":[{"text":"Ward, David H. 0000-0002-5242-2526 dward@usgs.gov","orcid":"https://orcid.org/0000-0002-5242-2526","contributorId":3247,"corporation":false,"usgs":true,"family":"Ward","given":"David","email":"dward@usgs.gov","middleInitial":"H.","affiliations":[{"id":117,"text":"Alaska Science Center Biology WTEB","active":true,"usgs":true},{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"preferred":true,"id":432624,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reed, Austin","contributorId":18833,"corporation":false,"usgs":true,"family":"Reed","given":"Austin","email":"","affiliations":[],"preferred":false,"id":432626,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sedinger, James S.","contributorId":84861,"corporation":false,"usgs":false,"family":"Sedinger","given":"James","email":"","middleInitial":"S.","affiliations":[{"id":12742,"text":"University of Nevada Reno","active":true,"usgs":false}],"preferred":false,"id":432625,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Black, Jeffrey M.","contributorId":77822,"corporation":false,"usgs":true,"family":"Black","given":"Jeffrey","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":432627,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Derksen, Dirk V. dderksen@usgs.gov","contributorId":2269,"corporation":false,"usgs":true,"family":"Derksen","given":"Dirk","email":"dderksen@usgs.gov","middleInitial":"V.","affiliations":[{"id":117,"text":"Alaska Science Center Biology WTEB","active":true,"usgs":true}],"preferred":true,"id":432623,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Castelli, Paul M.","contributorId":107931,"corporation":false,"usgs":true,"family":"Castelli","given":"Paul","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":432628,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
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