{"pageNumber":"2848","pageRowStart":"71175","pageSize":"25","recordCount":184569,"records":[{"id":70179823,"text":"70179823 - 2003 - IHN virus traffic in the Columbia River basin","interactions":[],"lastModifiedDate":"2017-01-18T14:39:18","indexId":"70179823","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"IHN virus traffic in the Columbia River basin","docAbstract":"<p>Abstract not available&nbsp;</p>","largerWorkType":{"id":24,"text":"Conference Paper"},"largerWorkTitle":"Proceedings of the american fisheries society symposium on propagated fish in resource management","conferenceTitle":"American fisheries society symposium on propagated fish in resource management","conferenceLocation":"Boise, ID","language":"English","usgsCitation":"Kurath, G., Garver, K., and Troyer, R., 2003, IHN virus traffic in the Columbia River basin, <i>in</i> Proceedings of the american fisheries society symposium on propagated fish in resource management, Boise, ID.","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":333375,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58808d9ae4b01dfadfff15b3","contributors":{"authors":[{"text":"Kurath, G.","contributorId":152437,"corporation":false,"usgs":true,"family":"Kurath","given":"G.","affiliations":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"preferred":false,"id":658840,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Garver, K.A.","contributorId":42766,"corporation":false,"usgs":true,"family":"Garver","given":"K.A.","email":"","affiliations":[],"preferred":false,"id":658841,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Troyer, R.M.","contributorId":63592,"corporation":false,"usgs":true,"family":"Troyer","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":658842,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70025125,"text":"70025125 - 2003 - Diel cycles in dissolved metal concentrations in streams: Occurrence and possible causes","interactions":[],"lastModifiedDate":"2018-11-16T08:36:39","indexId":"70025125","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3722,"text":"Water Resources Research","onlineIssn":"1944-7973","printIssn":"0043-1397","active":true,"publicationSubtype":{"id":10}},"title":"Diel cycles in dissolved metal concentrations in streams: Occurrence and possible causes","docAbstract":"<p><span>Substantial diel (24‐hour) cycles in dissolved (0.1‐μm filtration) metal concentrations were observed during low flow for 18 sampling episodes at 14 sites on 12 neutral and alkaline streams draining historical mining areas in Montana and Idaho. At some sites, concentrations of Cd, Mn, Ni, and Zn increased as much as 119, 306, 167, and 500%, respectively, from afternoon minimum values to maximum values shortly after sunrise. Arsenic concentrations exhibited the inverse temporal pattern with increases of up to 54%. Variations in Cu concentrations were small and inconsistent. Diel metal cycles are widespread and persistent, occur over a wide range of metal concentrations, and likely are caused primarily by instream geochemical processes. Adsorption is the only process that can explain the inverse temporal patterns of As and the divalent metals. Diel metal cycles have important implications for many types of water‐quality studies and for understanding trace‐metal mobility.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/2002WR001571","usgsCitation":"Nimick, D.A., Gammons, C.H., Cleasby, T., Madison, J.P., Skaar, D., and Brick, C.M., 2003, Diel cycles in dissolved metal concentrations in streams: Occurrence and possible causes: Water Resources Research, v. 39, no. 9, p. 2-1-2-17, https://doi.org/10.1029/2002WR001571.","productDescription":"Article 1247; 17 p.","startPage":"2-1","endPage":"2-17","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":478497,"rank":1,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1029/2002wr001571","text":"Publisher Index Page"},{"id":235878,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"39","issue":"9","noUsgsAuthors":false,"publicationDate":"2003-09-17","publicationStatus":"PW","scienceBaseUri":"505a00c0e4b0c8380cd4f8cc","contributors":{"authors":[{"text":"Nimick, David A. dnimick@usgs.gov","contributorId":421,"corporation":false,"usgs":true,"family":"Nimick","given":"David","email":"dnimick@usgs.gov","middleInitial":"A.","affiliations":[{"id":573,"text":"Special Applications Science Center","active":true,"usgs":true},{"id":5050,"text":"WY-MT Water Science Center","active":true,"usgs":true}],"preferred":true,"id":403907,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gammons, Chris","contributorId":140801,"corporation":false,"usgs":false,"family":"Gammons","given":"Chris","affiliations":[{"id":13574,"text":"Montana Tech of the University of Montana, Butte, MT","active":true,"usgs":false}],"preferred":false,"id":403904,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cleasby, Tom 0000-0003-0694-1541 tcleasby@usgs.gov","orcid":"https://orcid.org/0000-0003-0694-1541","contributorId":1137,"corporation":false,"usgs":true,"family":"Cleasby","given":"Tom","email":"tcleasby@usgs.gov","affiliations":[{"id":5050,"text":"WY-MT Water Science Center","active":true,"usgs":true}],"preferred":false,"id":403908,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Madison, James P.","contributorId":171749,"corporation":false,"usgs":false,"family":"Madison","given":"James","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":403903,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Skaar, Don","contributorId":9171,"corporation":false,"usgs":true,"family":"Skaar","given":"Don","email":"","affiliations":[],"preferred":false,"id":403905,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Brick, Christine M.","contributorId":99481,"corporation":false,"usgs":false,"family":"Brick","given":"Christine","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":403906,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70025335,"text":"70025335 - 2003 - Pumping‐induced leakage in a bounded aquifer: An example of a scale‐invariant phenomenon","interactions":[],"lastModifiedDate":"2018-04-02T12:41:04","indexId":"70025335","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3722,"text":"Water Resources Research","onlineIssn":"1944-7973","printIssn":"0043-1397","active":true,"publicationSubtype":{"id":10}},"title":"Pumping‐induced leakage in a bounded aquifer: An example of a scale‐invariant phenomenon","docAbstract":"<p><span>A new approach is presented for calculation of the volume of pumping‐induced leakage entering an aquifer as a function of time. This approach simplifies the total leakage calculation by extending analytical‐based methods developed for infinite systems to bounded aquifers of any size. The simplification is possible because of the relationship between drawdown and leakage in aquifers laterally bounded by impermeable formations. This relationship produces a scale‐invariant total leakage; i.e., the volume of leakage as a function of time does not change with the size of the aquifer or with the location of the pumping well. Two examples and image well theory are used to demonstrate and prove, respectively, the generality of this interesting phenomenon.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/2002WR001484","usgsCitation":"Butler, J.J., and Tsou, M., 2003, Pumping‐induced leakage in a bounded aquifer: An example of a scale‐invariant phenomenon: Water Resources Research, v. 39, no. 12, p. 2-1-2-8, https://doi.org/10.1029/2002WR001484.","productDescription":"Article 1344; 8 p.","startPage":"2-1","endPage":"2-8","costCenters":[],"links":[{"id":478489,"rank":1,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1029/2002wr001484","text":"Publisher Index Page"},{"id":235697,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"39","issue":"12","noUsgsAuthors":false,"publicationDate":"2003-12-05","publicationStatus":"PW","scienceBaseUri":"505a9039e4b0c8380cd7fbe7","contributors":{"authors":[{"text":"Butler, James J. Jr.","contributorId":199860,"corporation":false,"usgs":false,"family":"Butler","given":"James","suffix":"Jr.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":404797,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tsou, Ming-shu","contributorId":20507,"corporation":false,"usgs":false,"family":"Tsou","given":"Ming-shu","email":"","affiliations":[],"preferred":false,"id":404798,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70025260,"text":"70025260 - 2003 - Post-breeding distribution of Long-tailed Ducks Clangula hyemalis from the Yukon-Kuskokwim Delta, Alaska","interactions":[],"lastModifiedDate":"2022-08-16T15:08:59.701556","indexId":"70025260","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3764,"text":"Wildfowl","onlineIssn":"2052-6458","printIssn":"0954-6324","active":true,"publicationSubtype":{"id":10}},"title":"Post-breeding distribution of Long-tailed Ducks Clangula hyemalis from the Yukon-Kuskokwim Delta, Alaska","docAbstract":"<p>Breeding populations of Long-tailed Ducks <i>Clangula hyemalis</i> have declined in western Alaska, particularly on the Yukon-Kuskokwim (Y-K) Delta, and the species is currently considered a species of particular concern by the U.S. Fish &amp; Wildlife Service in Alaska. Potential factors that may have contributed to this decline that occurred away from the breeding grounds could not be considered since moulting and wintering areas for this population were unknown. A study was conducted in 1998 and 1999 to locate the moulting and wintering areas of the Y-K Delta breeding population. VHF and satellite transmitters were deployed to identify areas used by moulting birds. Based on the locations identified by satellite telemetry, aerial surveys were flown to locate birds marked with VHF transmitters, then low-level aerial surveys were designed and conducted to determine the number of birds using these and adjacent areas. Moulting locations of 54 marked female Long-tailed Ducks were identified: 13 marked females were found in wetlands and large lakes on the Y-K Delta, 11 in coastal lagoons at St Lawrence Island, Alaska, and two along the coast of the Chukotka Peninsula, Russia. A autumn staging area was identified along the east coast of the Chukotka Peninsula which was used by seven of 10 birds with satellite transmitters providing locations during that period. Birds wintered in coastal waters of the North Pacific Ocean north of 50°N and between 150°E and 130°W. The wide distribution of birds in winter suggests little probability of a single factor in winter contributing to the decline.</p>","language":"English","publisher":"Wildfowl & Wetlands Trust","usgsCitation":"Petersen, M.R., McCaffery, B.J., and Flint, P.L., 2003, Post-breeding distribution of Long-tailed Ducks Clangula hyemalis from the Yukon-Kuskokwim Delta, Alaska: Wildfowl, v. 54, p. 103-113.","productDescription":"11 p.","startPage":"103","endPage":"113","numberOfPages":"11","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":235774,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":405183,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://wildfowl.wwt.org.uk/index.php/wildfowl/article/view/1161","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Alaska","otherGeospatial":"Yukon-Kuskokwim Delta","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -166.39892578125,\n              60.3812902796077\n            ],\n            [\n              -163.4765625,\n              60.3812902796077\n            ],\n            [\n              -163.4765625,\n              63.40136142059639\n            ],\n            [\n              -166.39892578125,\n              63.40136142059639\n            ],\n            [\n              -166.39892578125,\n              60.3812902796077\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"54","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a7e57e4b0c8380cd7a49f","contributors":{"authors":[{"text":"Petersen, Margaret R. 0000-0001-6082-3189 mrpetersen@usgs.gov","orcid":"https://orcid.org/0000-0001-6082-3189","contributorId":167729,"corporation":false,"usgs":true,"family":"Petersen","given":"Margaret","email":"mrpetersen@usgs.gov","middleInitial":"R.","affiliations":[{"id":117,"text":"Alaska Science Center Biology WTEB","active":true,"usgs":true}],"preferred":true,"id":404492,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McCaffery, B. J.","contributorId":99355,"corporation":false,"usgs":false,"family":"McCaffery","given":"B.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":404493,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Flint, Paul L. 0000-0002-8758-6993 pflint@usgs.gov","orcid":"https://orcid.org/0000-0002-8758-6993","contributorId":3284,"corporation":false,"usgs":true,"family":"Flint","given":"Paul","email":"pflint@usgs.gov","middleInitial":"L.","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":404491,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70026138,"text":"70026138 - 2003 - Initial river test of a monostatic RiverSonde streamflow measurement system","interactions":[],"lastModifiedDate":"2023-03-10T18:39:27.205922","indexId":"70026138","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Initial river test of a monostatic RiverSonde streamflow measurement system","docAbstract":"A field experiment was conducted on May 7-8, 2002 using a CODAR RiverSonde UHF radar system at Vernalis, California on the San Joaquin River. The monostatic radar configuration on one bank of the river, with the antennas looking both upriver and downriver, provided very high-quality data. Estimates of both along-river and cross-river surface current were generated using several models, including one based on normal-mode analysis. Along-river surface velocities ranged from about 0.6 m/s at the river banks to about 1.0 m/s near the middle of the river. Average cross-river surface velocities were 0.02 m/s or less.","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Proceedings of the IEEE Working Conference on Current Measurement","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"Proceedings of the IEEE Seventh Working Conference on Current Measurement; Current and Wave Monitoring and Emerging Technologies","conferenceDate":"March 13-15, 2003","conferenceLocation":"San Diego, California, United States","language":"English","doi":"10.1109/CCM.2003.1194281","usgsCitation":"Teague, C., Barrick, D., Lilleboe, P., and Cheng, R.T., 2003, Initial river test of a monostatic RiverSonde streamflow measurement system, <i>in</i> Proceedings of the IEEE Working Conference on Current Measurement, San Diego, California, United States, March 13-15, 2003, p. 46-50, https://doi.org/10.1109/CCM.2003.1194281.","productDescription":"5 p.","startPage":"46","endPage":"50","costCenters":[],"links":[{"id":234522,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","city":"Vernalis","otherGeospatial":"San Joaquin River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -121.34306105965155,\n              37.70722574782812\n            ],\n            [\n              -121.34306105965155,\n              37.564761014880446\n            ],\n            [\n              -121.14427718513983,\n              37.564761014880446\n            ],\n            [\n              -121.14427718513983,\n              37.70722574782812\n            ],\n            [\n              -121.34306105965155,\n              37.70722574782812\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3beae4b0c8380cd62927","contributors":{"editors":[{"text":"Rizoli J.A.","contributorId":128304,"corporation":true,"usgs":false,"organization":"Rizoli J.A.","id":536577,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Teague, C.C.","contributorId":17758,"corporation":false,"usgs":true,"family":"Teague","given":"C.C.","email":"","affiliations":[],"preferred":false,"id":408071,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Barrick, D.E.","contributorId":86483,"corporation":false,"usgs":true,"family":"Barrick","given":"D.E.","email":"","affiliations":[],"preferred":false,"id":408074,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lilleboe, P.M.","contributorId":25284,"corporation":false,"usgs":true,"family":"Lilleboe","given":"P.M.","email":"","affiliations":[],"preferred":false,"id":408073,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Cheng, R. T.","contributorId":23138,"corporation":false,"usgs":false,"family":"Cheng","given":"R.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":408072,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70025055,"text":"70025055 - 2003 - High precision earthquake locations reveal seismogenic structure beneath Mammoth Mountain, California","interactions":[],"lastModifiedDate":"2017-02-27T14:51:53","indexId":"70025055","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2003","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":"High precision earthquake locations reveal seismogenic structure beneath Mammoth Mountain, California","docAbstract":"<p><span>In 1989, an unusual earthquake swarm occurred beneath Mammoth Mountain that was probably associated with magmatic intrusion. To improve our understanding of this swarm, we relocated Mammoth Mountain earthquakes using a double difference algorithm. Relocated hypocenters reveal that most earthquakes occurred on two structures, a near-vertical plane at 7–9 km depth that has been interpreted as an intruding dike, and a circular ring-like structure at ∼5.5 km depth, above the northern end of the inferred dike. Earthquakes on this newly discovered ring structure form a conical section that dips outward away from the aseismic interior. Fault-plane solutions indicate that in 1989 the seismicity ring was slipping as a ring-normal fault as the center of the mountain rose with respect to the surrounding crust. Seismicity migrated around the ring, away from the underlying dike at a rate of ∼0.4 km/month, suggesting that fluid movement triggered seismicity on the ring fault.</span></p>","language":"English","publisher":"Wiley","doi":"10.1029/2003GL018334","issn":"00948276","usgsCitation":"Prejean, S.G., Stork, A., Ellsworth, W.L., Hill, D., and Julian, B.R., 2003, High precision earthquake locations reveal seismogenic structure beneath Mammoth Mountain, California: Geophysical Research Letters, v. 30, no. 24, 4 p.; 2247, https://doi.org/10.1029/2003GL018334.","productDescription":"4 p.; 2247","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":478583,"rank":1,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1029/2003gl018334","text":"Publisher Index Page"},{"id":236092,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Long Valley Caldera, Mammoth Mountain","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -119.15359497070312,\n              37.40725549559874\n            ],\n            [\n              -118.54385375976564,\n              37.40725549559874\n            ],\n            [\n              -118.54385375976564,\n              37.83907230547641\n            ],\n            [\n              -119.15359497070312,\n              37.83907230547641\n            ],\n            [\n              -119.15359497070312,\n              37.40725549559874\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"30","issue":"24","noUsgsAuthors":false,"publicationDate":"2003-12-18","publicationStatus":"PW","scienceBaseUri":"505a30c3e4b0c8380cd5d919","contributors":{"authors":[{"text":"Prejean, Stephanie G. sprejean@usgs.gov","contributorId":2602,"corporation":false,"usgs":true,"family":"Prejean","given":"Stephanie","email":"sprejean@usgs.gov","middleInitial":"G.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":false,"id":403626,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stork, Anna","contributorId":100171,"corporation":false,"usgs":false,"family":"Stork","given":"Anna","email":"","affiliations":[],"preferred":false,"id":403625,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ellsworth, William L. ellsworth@usgs.gov","contributorId":787,"corporation":false,"usgs":true,"family":"Ellsworth","given":"William","email":"ellsworth@usgs.gov","middleInitial":"L.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":403624,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hill, David","contributorId":10500,"corporation":false,"usgs":true,"family":"Hill","given":"David","affiliations":[],"preferred":false,"id":403623,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Julian, Bruce R.","contributorId":50063,"corporation":false,"usgs":true,"family":"Julian","given":"Bruce","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":403622,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70026175,"text":"70026175 - 2003 - Stratigraphy, geochronology, and accretionary terrane settings of two Bronson Hill arc sequences, northern New England","interactions":[],"lastModifiedDate":"2020-08-31T14:43:19.418946","indexId":"70026175","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3067,"text":"Physics and Chemistry of the Earth","active":true,"publicationSubtype":{"id":10}},"title":"Stratigraphy, geochronology, and accretionary terrane settings of two Bronson Hill arc sequences, northern New England","docAbstract":"<p>The Ammonoosuc Volcanics, Partridge Formation, and the Oliverian and Highlandcroft Plutonic Suites of the Bronson Hill anticlinorium (BHA) in axial New England are widely accepted as a single Middle to Late Ordovician magmatic arc that was active during closure of Iapetus. Mapping and U–Pb dating indicate, however, that the BHA contains two volcano-sedimentary-intrusive sequences of probable opposite subduction polarity, here termed the Ammonoosuc and Quimby sequences.</p><p>The Ammonoosuc sequence is defined by the Middle Ordovician Ammonoosuc Volcanics near Littleton, NH, the type area, northeast to Milan, NH, and Oquossoc, ME; it also includes black slate of the Partridge Formation (<i>C. bicornis</i>––zone graptolites, ∼457 Ma). Related metamorphosed intrusives are the tonalitic Joslin Turn pluton (469&nbsp;±&nbsp;2 Ma), the Cambridge Black granitic pluton (468&nbsp;±&nbsp;3 Ma), and gabbro, tonalite (467&nbsp;±&nbsp;4 Ma), and sheeted diabase of the Chickwolnepy intrusions. These intrusives cut lowermost Ammonoosuc (therefore &gt;469 Ma). Probable uppermost Ammonoosuc is dated at 465&nbsp;±&nbsp;6 and 461&nbsp;±&nbsp;8 Ma. Successively below the Ammonoosuc are the Dead River and Hurricane Mountain Formations (flysch and melange), and the Jim Pond Formation (484&nbsp;±&nbsp;5 Ma) and Boil Mountain Complex (both ophiolite), which are structurally underlain by the Neoproterozoic(?) Chain Lakes massif.</p><p>The Quimby sequence is defined by the Lower Silurian(?) to Upper Ordovician Quimby Formation, composed of bimodal volcanics (443&nbsp;±&nbsp;4 Ma) and sulfidic shale and graywacke that lie conformably to unconformably above the Ammmonoosuc Volcanics and Partridge Formation. Also in the Quimby sequence are several granitic to sparsely gabbroic plutons of the Highlandcroft (441–452 Ma) and Oliverian (435–456 Ma) Plutonic Suites, which intrude the Dead River, Ammonoouc and Partridge, but not the Quimby Formation.</p><p>Based on faunal, paleolatitude, and isotopic data, the Ammonoosuc sequence and its correlatives and underlying sequences formed off the southern Laurentian margin, but northwest of the principal Iapetan suture, or Red Indian line. The Boil Mountain-Jim Pond-Hurricane Mountain sequence was ramped northwestward over the Chain Lakes massif at ∼475 Ma, on the basal Boil Mountain surface. This obduction probably occurred slightly before obduction on the Baie Vert-Brompton surface (BBL), farther NW, over the Laurentian margin, and was followed by Dead River flysch sedimentation, which ended with the abrupt onset of Ammonoosuc-sequence arc magmatism at ∼470 Ma. Ammonoosuc eruptions probably ended at ∼460 Ma, when Iapetus closed along the Red Indian line.</p><p>During a following magmatic hiatus of ∼3–5 m.y., now represented by portions of the Partridge Formation that overlie the Ammonoosuc Volcanics, subduction polarity reversed, and subduction resumed below the northwest-dipping Brunswick subduction complex (BSC) of New Brunswick, Canada. Quimby-sequence magmatism (∼456–435 Ma) on the newly accreted Laurentian margin occurred above the BSC, whose footwall is now buried to the southeast by mainly Silurian clastic sediments of the Merrimack-Fredericton trough, deposited in the “Fredericton Sea”. In Silurian to Early Devonian time, the NW-dipping BSC footwall was paired with a SE-dipping subduction zone that produced arc magmas of the Coastal Volcanic belt, built on the composite Avalon and adjacent peri-Avalonian terranes. Orogen-normal extension produced by rapid rollback of both subduction zones narrowed the Fredericton Sea, produced the Central Maine and Connecticut Valley-Gaspé basins, and culminated in the Acadian orogeny when the sea completely closed in Early Devonian time.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/S1474-7065(03)00012-3","issn":"14747065","usgsCitation":"Moench, R.H., and Aleinikoff, J.N., 2003, Stratigraphy, geochronology, and accretionary terrane settings of two Bronson Hill arc sequences, northern New England: Physics and Chemistry of the Earth, v. 28, no. 1-3, p. 113-160, https://doi.org/10.1016/S1474-7065(03)00012-3.","productDescription":"48 p.","startPage":"113","endPage":"160","numberOfPages":"48","costCenters":[],"links":[{"id":234593,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Maine, New Hampshire","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -72.24609375,\n              43.100982876188546\n            ],\n            [\n              -72.0703125,\n              42.71473218539458\n            ],\n            [\n              -70.8837890625,\n              42.87596410238256\n            ],\n            [\n              -69.2578125,\n              43.739352079154706\n            ],\n            [\n              -66.8408203125,\n              44.68427737181225\n            ],\n            [\n              -67.0166015625,\n              44.933696389694674\n            ],\n            [\n              -67.763671875,\n              45.767522962149876\n            ],\n            [\n              -68.203125,\n              46.34692761055676\n            ],\n            [\n              -69.169921875,\n              46.01222384063236\n            ],\n            [\n              -72.24609375,\n              43.100982876188546\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"28","issue":"1-3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b9a46e4b08c986b31c852","contributors":{"authors":[{"text":"Moench, R. H.","contributorId":8853,"corporation":false,"usgs":true,"family":"Moench","given":"R.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":408262,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Aleinikoff, J. N. 0000-0003-3494-6841","orcid":"https://orcid.org/0000-0003-3494-6841","contributorId":75132,"corporation":false,"usgs":true,"family":"Aleinikoff","given":"J.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":408263,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70025258,"text":"70025258 - 2003 - Searching for a life history approach to salmon escapement management","interactions":[],"lastModifiedDate":"2012-03-12T17:20:29","indexId":"70025258","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":718,"text":"American Fisheries Society Symposium","active":true,"publicationSubtype":{"id":10}},"title":"Searching for a life history approach to salmon escapement management","docAbstract":"A number of Pacific salmon populations have already been lost and many others throughout the range are in various states of decline. Recent research has documented that Pacific salmon carcasses serve as a key delivery vector of marine-derived nutrients into the freshwater portions of their ecosystems. This nutrient supply plays a critical biological feedback role in salmon sustainability by supporting juvenile salmon production. We first demonstrate how nutrient feedback potential to juvenile production may be unaccounted for in spawner-recruit models of populations under long-term exploitation. We then present a heuristic, life history-based, spreadsheet survival model that incorporates salmon carcass-driven nutrient feedback to the freshwater components of the salmon ecosystem. The productivity of a hypothetical coho salmon population was simulated using rates from the literature for survival from spawner to egg, egg to fry, fry to smolt, and smolt to adult. The effects of climate variation and nutrient feedback on survival were incorporated, as were density-dependent effects of the numbers of spawners and fry on freshwater survival of eggs and juveniles. The unexploited equilibrium population was subjected to 100 years of 20, 40, 60, and 80% harvest. Each harvest scenario greater than 20% brought the population to a reduced steady state, regardless of generous compensatory survival at low population sizes. Increasing harvest reduced the positive effects of nutrient contributions to population growth. Salmon researchers should further explore this modeling approach for establishing escapement goals. Given the importance of nutrient feedback, managers should strive for generous escapements that support nutrient rebuilding, as well as egg deposition, to ensure strong future salmon production.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"American Fisheries Society Symposium","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"08922284","usgsCitation":"Knudsen, E., Symmes, E., and Margraf, F., 2003, Searching for a life history approach to salmon escapement management: American Fisheries Society Symposium, v. 2003, no. 34, p. 261-276.","startPage":"261","endPage":"276","numberOfPages":"16","costCenters":[],"links":[{"id":235733,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"2003","issue":"34","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b8853e4b08c986b3168f7","contributors":{"authors":[{"text":"Knudsen, E.E.","contributorId":26116,"corporation":false,"usgs":true,"family":"Knudsen","given":"E.E.","email":"","affiliations":[],"preferred":false,"id":404486,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Symmes, E.W.","contributorId":45095,"corporation":false,"usgs":true,"family":"Symmes","given":"E.W.","email":"","affiliations":[],"preferred":false,"id":404487,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Margraf, F.J.","contributorId":47738,"corporation":false,"usgs":true,"family":"Margraf","given":"F.J.","email":"","affiliations":[],"preferred":false,"id":404488,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70025132,"text":"70025132 - 2003 - The Mendocino crustal conveyor: Making and breaking the California crust","interactions":[],"lastModifiedDate":"2021-08-06T21:12:50.243944","indexId":"70025132","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2020,"text":"International Geology Review","active":true,"publicationSubtype":{"id":10}},"title":"The Mendocino crustal conveyor: Making and breaking the California crust","docAbstract":"<p><span>The northward migration of the Mendocino triple junction has resulted in a fundamental modification of the crust of coastal California. As a consequence of viscous coupling between the southern edge of the Gorda slab and the base of the North American crust beneath the Coast Ranges of central and northern California, the crust of coastal California was first thickened and then thinned. This viscous coupling and ephemeral crustal thickening has produced a distinctive pattern of uplift that allows us to map the three-dimensional extent of crustal modification. This pattern of crustal deformation has combined with the strain field of the developing San Andreas fault system to produce the observed pattern of near-surface deformation. The rapid rise in heat flow south of the triple junction observed in the northern Coast Ranges is a direct consequence of development and removal of the crustal welt that migrated with the triple junction.</span></p>","language":"English","publisher":"Taylor & Francis","doi":"10.2747/0020-6814.45.9.767","issn":"00206814","usgsCitation":"Furlong, K., Lock, J., Guzofski, C., Whitlock, J., and Benz, H., 2003, The Mendocino crustal conveyor: Making and breaking the California crust: International Geology Review, v. 45, no. 9, p. 767-779, https://doi.org/10.2747/0020-6814.45.9.767.","productDescription":"13 p.","startPage":"767","endPage":"779","costCenters":[],"links":[{"id":387743,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Mendocino Triple Junction","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -125.5078125,\n              39.26628442213066\n            ],\n            [\n              -123.11279296875001,\n              39.26628442213066\n            ],\n            [\n              -123.11279296875001,\n              41.52502957323801\n            ],\n            [\n              -125.5078125,\n              41.52502957323801\n            ],\n            [\n              -125.5078125,\n              39.26628442213066\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"45","issue":"9","noUsgsAuthors":false,"publicationDate":"2010-07-14","publicationStatus":"PW","scienceBaseUri":"505ba7e0e4b08c986b321868","contributors":{"authors":[{"text":"Furlong, K.P.","contributorId":35490,"corporation":false,"usgs":true,"family":"Furlong","given":"K.P.","email":"","affiliations":[],"preferred":false,"id":403945,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lock, J.","contributorId":40784,"corporation":false,"usgs":true,"family":"Lock","given":"J.","email":"","affiliations":[],"preferred":false,"id":403947,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Guzofski, C.","contributorId":18950,"corporation":false,"usgs":true,"family":"Guzofski","given":"C.","affiliations":[],"preferred":false,"id":403944,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Whitlock, J.","contributorId":36732,"corporation":false,"usgs":true,"family":"Whitlock","given":"J.","email":"","affiliations":[],"preferred":false,"id":403946,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Benz, H.","contributorId":61953,"corporation":false,"usgs":true,"family":"Benz","given":"H.","email":"","affiliations":[],"preferred":false,"id":403948,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70026137,"text":"70026137 - 2003 - Managing troubled data: Coastal data partnerships smooth data integration","interactions":[],"lastModifiedDate":"2018-08-10T15:08:56","indexId":"70026137","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1552,"text":"Environmental Monitoring and Assessment","onlineIssn":"1573-2959","printIssn":"0167-6369","active":true,"publicationSubtype":{"id":10}},"title":"Managing troubled data: Coastal data partnerships smooth data integration","docAbstract":"Understanding the ecology, condition, and changes of coastal areas requires data from many sources. Broad-scale and long-term ecological questions, such as global climate change, biodiversity, and cumulative impacts of human activities, must be addressed with databases that integrate data from several different research and monitoring programs. Various barriers, including widely differing data formats, codes, directories, systems, and metadata used by individual programs, make such integration troublesome. Coastal data partnerships, by helping overcome technical, social, and organizational barriers, can lead to a better understanding of environmental issues, and may enable better management decisions. Characteristics of successful data partnerships include a common need for shared data, strong collaborative leadership, committed partners willing to invest in the partnership, and clear agreements on data standards and data policy. Emerging data and metadata standards that become widely accepted are crucial. New information technology is making it easier to exchange and integrate data. Data partnerships allow us to create broader databases than would be possible for any one organization to create by itself.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Environmental Monitoring and Assessment","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1023/A:1021372923589","issn":"01676369","usgsCitation":"Hale, S., Hale, M.A., Bradley, M., Belton, T., Cooper, L., Frame, M., Friel, C., Harwell, L., King, R., Michener, W., Nicolson, D., and Peterjohn, B., 2003, Managing troubled data: Coastal data partnerships smooth data integration: Environmental Monitoring and Assessment, v. 81, no. 1-3, p. 133-148, https://doi.org/10.1023/A:1021372923589.","startPage":"133","endPage":"148","numberOfPages":"16","costCenters":[{"id":37226,"text":"Core Science Analytics, Synthesis, and Libraries","active":true,"usgs":true}],"links":[{"id":234521,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":208640,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1023/A:1021372923589"}],"volume":"81","issue":"1-3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a4c99e4b0c8380cd69d7e","contributors":{"authors":[{"text":"Hale, S.S.","contributorId":64001,"corporation":false,"usgs":true,"family":"Hale","given":"S.S.","email":"","affiliations":[],"preferred":false,"id":408067,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hale, Miglarese A.","contributorId":49152,"corporation":false,"usgs":true,"family":"Hale","given":"Miglarese","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":408063,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bradley, M.P.","contributorId":20122,"corporation":false,"usgs":true,"family":"Bradley","given":"M.P.","email":"","affiliations":[],"preferred":false,"id":408060,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Belton, T.J.","contributorId":75730,"corporation":false,"usgs":true,"family":"Belton","given":"T.J.","email":"","affiliations":[],"preferred":false,"id":408069,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Cooper, L.D.","contributorId":94468,"corporation":false,"usgs":true,"family":"Cooper","given":"L.D.","email":"","affiliations":[],"preferred":false,"id":408070,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Frame, M.T.","contributorId":6618,"corporation":false,"usgs":true,"family":"Frame","given":"M.T.","email":"","affiliations":[],"preferred":false,"id":408059,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Friel, C.A.","contributorId":74551,"corporation":false,"usgs":true,"family":"Friel","given":"C.A.","email":"","affiliations":[],"preferred":false,"id":408068,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Harwell, L.M.","contributorId":51506,"corporation":false,"usgs":true,"family":"Harwell","given":"L.M.","email":"","affiliations":[],"preferred":false,"id":408064,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"King, R.E.","contributorId":53998,"corporation":false,"usgs":true,"family":"King","given":"R.E.","email":"","affiliations":[],"preferred":false,"id":408065,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Michener, W.K.","contributorId":59139,"corporation":false,"usgs":true,"family":"Michener","given":"W.K.","email":"","affiliations":[],"preferred":false,"id":408066,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Nicolson, D.T.","contributorId":42763,"corporation":false,"usgs":true,"family":"Nicolson","given":"D.T.","affiliations":[],"preferred":false,"id":408062,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Peterjohn, B.G.","contributorId":25255,"corporation":false,"usgs":true,"family":"Peterjohn","given":"B.G.","email":"","affiliations":[],"preferred":false,"id":408061,"contributorType":{"id":1,"text":"Authors"},"rank":12}]}}
,{"id":70026136,"text":"70026136 - 2003 - Individual variation in prey selection by sea otters: Patterns, causes and implications","interactions":[],"lastModifiedDate":"2012-03-12T17:20:34","indexId":"70026136","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2158,"text":"Journal of Animal Ecology","active":true,"publicationSubtype":{"id":10}},"title":"Individual variation in prey selection by sea otters: Patterns, causes and implications","docAbstract":"1. Longitudinal records of prey selection by 10 adult female sea otters on the Monterey Peninsula, California, from 1983 to 1990 demonstrate extreme inter-individual variation in diet. Variation in prey availability cannot explain these differences as the data were obtained from a common spatial-temporal area. 2. Individual dietary patterns persisted throughout our study, thus indicating that they are life-long characteristics. 3. Individual dietary patterns in sea otters appear to be transmitted along matrilines, probably by way of learning during the period of mother-young association. 4. Efficient utilization of different prey types probably requires radically different sensory/motor skills, each of which is difficult to acquire and all of which may exceed the learning and performance capacities of any single individual. This would explain the absence of generalists and inertia against switching, but not the existence of alternative specialists. 5. Such individual variation might arise in a constant environment from frequency-dependent effects, whereby the relative benefit of a given prey specialization depends on the number of other individuals utilizing that prey. Additionally, many of the sea otter's prey fluctuate substantially in abundance through time. This temporal variation, in conjunction with matrilineal transmission of foraging skills, may act to mediate the temporal dynamics of prey specializations. 6. Regardless of the exact cause, such extreme individual variation in diet has broad ramifications for population and community ecology. 7. The published literature indicates that similar patterns occur in many other species.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Animal Ecology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1046/j.1365-2656.2003.00690.x","issn":"00218790","usgsCitation":"Estes, J.A., Riedman, M.L., Staedler, M., Tinker, M.T., and Lyon, B., 2003, Individual variation in prey selection by sea otters: Patterns, causes and implications: Journal of Animal Ecology, v. 72, no. 1, p. 144-155, https://doi.org/10.1046/j.1365-2656.2003.00690.x.","startPage":"144","endPage":"155","numberOfPages":"12","costCenters":[],"links":[{"id":478481,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1046/j.1365-2656.2003.00690.x","text":"Publisher Index Page"},{"id":208942,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1046/j.1365-2656.2003.00690.x"},{"id":235064,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"72","issue":"1","noUsgsAuthors":false,"publicationDate":"2003-02-10","publicationStatus":"PW","scienceBaseUri":"505a3aa1e4b0c8380cd61e35","contributors":{"authors":[{"text":"Estes, J. A.","contributorId":53319,"corporation":false,"usgs":true,"family":"Estes","given":"J.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":408055,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Riedman, Marianne L.","contributorId":89079,"corporation":false,"usgs":true,"family":"Riedman","given":"Marianne","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":408057,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Staedler, M. M.","contributorId":101603,"corporation":false,"usgs":false,"family":"Staedler","given":"M. M.","affiliations":[],"preferred":false,"id":408058,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Tinker, M. T. 0000-0002-3314-839X","orcid":"https://orcid.org/0000-0002-3314-839X","contributorId":54152,"corporation":false,"usgs":false,"family":"Tinker","given":"M.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":408056,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Lyon, B.E.","contributorId":49159,"corporation":false,"usgs":true,"family":"Lyon","given":"B.E.","email":"","affiliations":[],"preferred":false,"id":408054,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70025209,"text":"70025209 - 2003 - Differential mortality of male spectacled eiders (<i>Somateria fischeri</i>) and king eiders (<i>Somateria spectabilis</i>) subsequent to anesthesia with propofol, bupivacaine, and ketoprofen","interactions":[],"lastModifiedDate":"2017-02-28T11:29:46","indexId":"70025209","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2191,"text":"Journal of Avian Medicine and Surgery","active":true,"publicationSubtype":{"id":10}},"title":"Differential mortality of male spectacled eiders (<i>Somateria fischeri</i>) and king eiders (<i>Somateria spectabilis</i>) subsequent to anesthesia with propofol, bupivacaine, and ketoprofen","docAbstract":"<p>Twenty free-ranging spectacled eiders (<i>Somateria fischeri</i>; 10 male, 10 female), 11 free-ranging king eiders (<i>Somateria spectabilis</i>; 6 male, 5 female), and 20 female common eiders (<i>Somateria mollissima</i>) were anesthetized with propofol, bupivacaine, and ketoprofen for the surgical implantation of satellite transmitters. Propofol was given to induce and maintain anesthesia (mean total dose, 26.2-45.6 mg/kg IV), bupivacaine (2-10 mg/kg SC) was infused into the incision site for local analgesia, and ketoprofen (2-5 mg/kg IM) was given at the time of surgery for postoperative analgesia. Four of 10 male spectacled eiders and 5 of 6 male king eiders died within 1-4 days after surgery. None of the female spectacled or common eiders and only 1 of the 5 female king eiders died during the same postoperative period. Histopathologic findings in 2 dead male king eiders were severe renal tubular necrosis, acute rhabdomyolysis, and mild visceral gout. Necropsy findings in 3 other dead male king eiders were consistent with visceral gout. We suspect that the perioperative use of ketoprofen caused lethal renal damage in the male eiders. Male eiders may be more susceptible to renal damage than females because of behavioral differences during their short stay on land in mating season. The combination of propofol, bupivacaine, and ketoprofen should not be used to anesthetize free-ranging male eiders, and nonsteroidal anti-inflammatory drugs should not be used perioperatively in any bird that may be predisposed to renal insufficiency.</p>","language":"English","publisher":"Association of Avian Veterinarians","doi":"10.1647/2001-024","issn":"10826742","usgsCitation":"Mulcahy, D.M., Tuomi, P.A., and Larsen, R.S., 2003, Differential mortality of male spectacled eiders (<i>Somateria fischeri</i>) and king eiders (<i>Somateria spectabilis</i>) subsequent to anesthesia with propofol, bupivacaine, and ketoprofen: Journal of Avian Medicine and Surgery, v. 17, no. 3, p. 117-123, https://doi.org/10.1647/2001-024.","productDescription":"7 p.","startPage":"117","endPage":"123","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":116,"text":"Alaska Science Center Biology MFEB","active":true,"usgs":true}],"links":[{"id":236063,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a00f4e4b0c8380cd4f9ed","contributors":{"authors":[{"text":"Mulcahy, Daniel M. dmulcahy@usgs.gov","contributorId":3102,"corporation":false,"usgs":true,"family":"Mulcahy","given":"Daniel","email":"dmulcahy@usgs.gov","middleInitial":"M.","affiliations":[{"id":116,"text":"Alaska Science Center Biology MFEB","active":true,"usgs":true}],"preferred":true,"id":404243,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tuomi, Pamela A.","contributorId":66900,"corporation":false,"usgs":false,"family":"Tuomi","given":"Pamela","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":404244,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Larsen, R. S.","contributorId":81473,"corporation":false,"usgs":false,"family":"Larsen","given":"R.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":404245,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70025318,"text":"70025318 - 2003 - Life history dependent morphometric variation in stream-dwelling Atlantic salmon","interactions":[],"lastModifiedDate":"2012-03-12T17:20:58","indexId":"70025318","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2932,"text":"Oecologia","active":true,"publicationSubtype":{"id":10}},"title":"Life history dependent morphometric variation in stream-dwelling Atlantic salmon","docAbstract":"The time course of morphometric variation among life histories for stream-dwelling Atlantic salmon (Salmo salar L.) parr (age-0+ to age-2+) was analyzed. Possible life histories were combinations of parr maturity status in the autumn (mature or immature) and age at outmigration (smolt at age-2+ or later age). Actual life histories expressed with enough fish for analysis in the 1997 cohort were immature/age-2+ smolt, mature/age-2 +smolt, and mature/age-2+ non-smolt. Tagged fish were assigned to one of the three life histories and digital pictures from the field were analyzed using landmark-based geometric morphometrics. Results indicated that successful grouping of fish according to life history varied with fish age, but that fish could be grouped before the actual expression of the life histories. By March (age-1+), fish were successfully grouped using a descriptive discriminant function and successful assignment ranged from 84 to 97% for the remainder of stream residence. A jackknife of the discriminant function revealed an average life history prediction success of 67% from age-1+ summer to smolting. Low sample numbers for one of the life histories may have limited prediction success. A MANOVA on the shape descriptors (relative warps) also indicated significant differences in shape among life histories from age-1+ summer through to smolting. Across all samples, shape varied significantly with size. Within samples, shape did not vary significantly with size for samples from December (age-0+) to May (age-1+). During the age-1+ summer however, shape varied significantly with size, but the relationship between shape and size was not different among life histories. In the autumn (age-1+) and winter (age-2+), life history differences explained a significant portion of the change in shape with size. Life history dependent morphometric variation may be useful to indicate the timing of early expressions of life history variation and as a tool to explore temporal and spatial variation in life history expression.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Oecologia","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1007/s00442-003-1387-0","issn":"00298549","usgsCitation":"Letcher, B., 2003, Life history dependent morphometric variation in stream-dwelling Atlantic salmon: Oecologia, v. 137, no. 4, p. 533-540, https://doi.org/10.1007/s00442-003-1387-0.","startPage":"533","endPage":"540","numberOfPages":"8","costCenters":[],"links":[{"id":209520,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/s00442-003-1387-0"},{"id":236071,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"137","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a475ce4b0c8380cd6783d","contributors":{"authors":[{"text":"Letcher, B. H. 0000-0003-0191-5678","orcid":"https://orcid.org/0000-0003-0191-5678","contributorId":48132,"corporation":false,"usgs":true,"family":"Letcher","given":"B.","middleInitial":"H.","affiliations":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"preferred":false,"id":404740,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70025134,"text":"70025134 - 2003 - Evaluation of specific ultraviolet absorbance as an indicator of the chemical composition and reactivity of dissolved organic carbon","interactions":[],"lastModifiedDate":"2020-01-04T13:25:57","indexId":"70025134","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1565,"text":"Environmental Science & Technology","onlineIssn":"1520-5851","printIssn":"0013-936X","active":true,"publicationSubtype":{"id":10}},"title":"Evaluation of specific ultraviolet absorbance as an indicator of the chemical composition and reactivity of dissolved organic carbon","docAbstract":"Specific UV absorbance (SUVA) is defined as the UV absorbance of a water sample at a given wavelength normalized for dissolved organic carbon (DOC) concentration. Our data indicate that SUVA, determined at 254 nm, is strongly correlated with percent aromaticity as determined by 13C NMR for 13 organic matter isolates obtained from a variety of aquatic environments. SUVA, therefore, is shown to be a useful parameter for estimating the dissolved aromatic carbon content in aquatic systems. Experiments involving the reactivity of DOC with chlorine and tetramethylammonium hydroxide (TMAH), however, show a wide range of reactivity for samples with similar SUVA values. These results indicate that, while SUVA measurements are good predictors of general chemical characteristics of DOC, they do not provide information about reactivity of DOC derived from different types of source materials. Sample pH, nitrate, and iron were found to influence SUVA measurements.","language":"English","publisher":"ACS","doi":"10.1021/es030360x","issn":"0013936X","usgsCitation":"Weishaar, J., Aiken, G.R., Bergamaschi, B., Fram, M.S., Fujii, R., and Mopper, K., 2003, Evaluation of specific ultraviolet absorbance as an indicator of the chemical composition and reactivity of dissolved organic carbon: Environmental Science & Technology, v. 37, no. 20, p. 4702-4708, https://doi.org/10.1021/es030360x.","productDescription":"7 p.","startPage":"4702","endPage":"4708","numberOfPages":"7","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":438876,"rank":1,"type":{"id":30,"text":"Data Release"},"url":"https://doi.org/10.5066/P9SBK2DZ","text":"USGS data release","linkHelpText":"Stream and River Chemistry in Watersheds of Northwestern Alaska, 2015-2019"},{"id":235988,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"37","issue":"20","noUsgsAuthors":false,"publicationDate":"2003-09-17","publicationStatus":"PW","scienceBaseUri":"505a0cc5e4b0c8380cd52cb9","contributors":{"authors":[{"text":"Weishaar, J.L.","contributorId":99754,"corporation":false,"usgs":true,"family":"Weishaar","given":"J.L.","email":"","affiliations":[],"preferred":false,"id":403956,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Aiken, George R. 0000-0001-8454-0984 graiken@usgs.gov","orcid":"https://orcid.org/0000-0001-8454-0984","contributorId":1322,"corporation":false,"usgs":true,"family":"Aiken","given":"George","email":"graiken@usgs.gov","middleInitial":"R.","affiliations":[{"id":191,"text":"Colorado Water Science Center","active":true,"usgs":true},{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":403951,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bergamaschi, Brian A. 0000-0002-9610-5581 bbergama@usgs.gov","orcid":"https://orcid.org/0000-0002-9610-5581","contributorId":1448,"corporation":false,"usgs":true,"family":"Bergamaschi","given":"Brian A.","email":"bbergama@usgs.gov","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":false,"id":403952,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Fram, Miranda S. 0000-0002-6337-059X mfram@usgs.gov","orcid":"https://orcid.org/0000-0002-6337-059X","contributorId":1156,"corporation":false,"usgs":true,"family":"Fram","given":"Miranda","email":"mfram@usgs.gov","middleInitial":"S.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":403955,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Fujii, Roger rfujii@usgs.gov","contributorId":553,"corporation":false,"usgs":true,"family":"Fujii","given":"Roger","email":"rfujii@usgs.gov","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":403953,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Mopper, K.","contributorId":63211,"corporation":false,"usgs":true,"family":"Mopper","given":"K.","email":"","affiliations":[],"preferred":false,"id":403954,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70025135,"text":"70025135 - 2003 - Relations between seismicity and deformation during unrest in Long Valley Caldera, California, from 1995 through 1999","interactions":[],"lastModifiedDate":"2012-03-12T17:20:57","indexId":"70025135","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2499,"text":"Journal of Volcanology and Geothermal Research","active":true,"publicationSubtype":{"id":10}},"title":"Relations between seismicity and deformation during unrest in Long Valley Caldera, California, from 1995 through 1999","docAbstract":"Unrest in Long Valley Caldera and the adjacent Sierra Nevada from 1995 through 2000 was dominated by three major episodes: (1) the March-April 1996 earthquake swarm in the east lobe of the south moat; (2) the July 1997-January 1998 caldera-wide unrest; and (3) a sequence of three M>5 earthquakes (9 June 1998, 13 July 1998, and 15 May 1999 UT) located in the Sierra Nevada block immediately south of the caldera. These three unrest episodes each had distinct characteristics with distinct implications for associated hazards. Seismicity developed as earthquake swarms for the 1996 and 1997-98 episodes, both of which were within the caldera. In contrast, the series of three M>5 earthquakes south of the caldera in 1998-99 each developed as a mainshock-aftershock sequence. Marginal deformation within the caldera associated with the 1996 swarm and the 1998-99 M>5 earthquakes is consistent with the cumulative seismic moments for the respective sequences. Deformation associated with the 1997-98 episode, however, was roughly five times larger than can be accounted for by the cumulative seismic moment of the associated earthquake swarm. We conclude that the 1997-98 episode was associated with mass transport (local intrusion of magma or magmatic brine) and that the associated earthquake swarm activity, which had a relatively high b -value of 1.2, was largely driven by the intrusive process. In contrast, the 1996 earthquake swarm and the 1998-99 M>5 mainshock-aftershock sequences, both with 'normal' b -values of ???0.9, represent brittle relaxation to previously accumulated stresses associated with little or no mass transport. These relations emphasize the importance of simultaneous, real-time monitoring of both seismicity and deformation as a basis for judging whether an evolving unrest episode has the potential for culminating in a volcanic eruption. ?? 2003 Elsevier B.V. All rights reserved.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Volcanology and Geothermal Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/S0377-0273(03)00169-0","issn":"03770273","usgsCitation":"Hill, D., Langbein, J.O., and Prejean, S., 2003, Relations between seismicity and deformation during unrest in Long Valley Caldera, California, from 1995 through 1999: Journal of Volcanology and Geothermal Research, v. 127, no. 3-4, p. 175-193, https://doi.org/10.1016/S0377-0273(03)00169-0.","startPage":"175","endPage":"193","numberOfPages":"19","costCenters":[],"links":[{"id":209498,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/S0377-0273(03)00169-0"},{"id":236024,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"127","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50e4a700e4b0e8fec6cdc333","contributors":{"authors":[{"text":"Hill, D.P.","contributorId":27432,"corporation":false,"usgs":true,"family":"Hill","given":"D.P.","email":"","affiliations":[],"preferred":false,"id":403957,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Langbein, J. O.","contributorId":39404,"corporation":false,"usgs":true,"family":"Langbein","given":"J.","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":403958,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Prejean, S.","contributorId":103442,"corporation":false,"usgs":true,"family":"Prejean","given":"S.","email":"","affiliations":[],"preferred":false,"id":403959,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70025206,"text":"70025206 - 2003 - Sediment-starved sand ridges on a mixed carbonate/siliciclastic inner shelf off west-central Florida","interactions":[],"lastModifiedDate":"2018-04-09T13:19:58","indexId":"70025206","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2667,"text":"Marine Geology","active":true,"publicationSubtype":{"id":10}},"title":"Sediment-starved sand ridges on a mixed carbonate/siliciclastic inner shelf off west-central Florida","docAbstract":"High-resolution side-scan mosaics, sediment analyses, and physical process data have revealed that the mixed carbonate/siliciclastic, inner shelf of west-central Florida supports a highly complex field of active sand ridges mantled by a hierarchy of bedforms. The sand ridges, mostly oriented obliquely to the shoreline trend, extend from 2 km to over 25 km offshore. They show many similarities to their well-known counterparts situated along the US Atlantic margin in that both increase in relief with increasing water depth, both are oriented obliquely to the coast, and both respond to modern shelf dynamics. There are significant differences in that the sand ridges on the west-central Florida shelf are smaller in all dimensions, have a relatively high carbonate content, and are separated by exposed rock surfaces. They are also shoreface-detached and are sediment-starved, thus stunting their development. Morphological details are highly distinctive and apparent in side-scan imagery due to the high acoustic contrast. The seafloor is active and not a relict system as indicated by: (1) relatively young AMS 14C dates (< 1600 yr BP) from forams in the shallow subsurface (1.6 meters below seafloor), (2) apparent shifts in sharply distinctive grayscale boundaries seen in time-series side-scan mosaics, (3) maintenance of these sharp acoustic boundaries and development of small bedforms in an area of constant and extensive bioturbation, (4) sediment textural asymmetry indicative of selective transport across bedform topography, (5) morphological asymmetry of sand ridges and 2D dunes, and (6) current-meter data indicating that the critical threshold velocity for sediment transport is frequently exceeded. Although larger sand ridges are found along other portions of the west-central Florida inner shelf, these smaller sand ridges are best developed seaward of a major coastal headland, suggesting some genetic relationship. The headland may focus and accelerate the N-S reversing currents. An elevated rock terrace extending from the headland supports these ridges in a shallower water environment than the surrounding shelf, allowing them to be more easily influenced by currents and surface gravity waves. Tidal currents, storm-generated flows, and seasonally developed flows are shore-parallel and oriented obliquely to the NW-SE trending ridges, indicating that they have developed as described by the Huthnance model. Although inner shelf sand ridges have been extensively examined elsewhere, this study is the first to describe them in a low-energy, sediment-starved, dominantly mixed siliciclastic/carbonate sedimentary environment situated on a former limestone platform. ?? 2003 Elsevier B.V. All rights reserved.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Marine Geology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/S0025-3227(03)00182-8","issn":"00253227","usgsCitation":"Harrison, S.E., Locker, S., Hine, A.C., Edwards, J., Naar, D., Twichell, D., and Mallinson, D.J., 2003, Sediment-starved sand ridges on a mixed carbonate/siliciclastic inner shelf off west-central Florida: Marine Geology, v. 200, no. 1-4, p. 171-194, https://doi.org/10.1016/S0025-3227(03)00182-8.","productDescription":"24 p.","startPage":"171","endPage":"194","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":235992,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Florida","otherGeospatial":"Tampa Bay","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -84,\n              26.85\n            ],\n            [\n              -82,\n              26.85\n            ],\n            [\n              -82,\n              28.5\n            ],\n            [\n              -84,\n              28.5\n            ],\n            [\n              -84,\n              26.85\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"200","issue":"1-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b8a09e4b08c986b316fc7","contributors":{"authors":[{"text":"Harrison, S. E.","contributorId":87976,"corporation":false,"usgs":true,"family":"Harrison","given":"S.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":404234,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Locker, S. D.","contributorId":81532,"corporation":false,"usgs":true,"family":"Locker","given":"S. D.","affiliations":[],"preferred":false,"id":404232,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hine, A. C.","contributorId":21197,"corporation":false,"usgs":true,"family":"Hine","given":"A.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":404229,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Edwards, J.H.","contributorId":96467,"corporation":false,"usgs":true,"family":"Edwards","given":"J.H.","email":"","affiliations":[],"preferred":false,"id":404235,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Naar, D. F.","contributorId":80434,"corporation":false,"usgs":true,"family":"Naar","given":"D. F.","affiliations":[],"preferred":false,"id":404231,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Twichell, D.C.","contributorId":84304,"corporation":false,"usgs":true,"family":"Twichell","given":"D.C.","affiliations":[],"preferred":false,"id":404233,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Mallinson, D. J.","contributorId":71745,"corporation":false,"usgs":true,"family":"Mallinson","given":"D.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":404230,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70025315,"text":"70025315 - 2003 - Characterization of yield reduction in Ethiopia using a GIS-based crop water balance model","interactions":[],"lastModifiedDate":"2015-08-27T14:19:25","indexId":"70025315","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1175,"text":"Canadian Journal of Remote Sensing","active":true,"publicationSubtype":{"id":10}},"title":"Characterization of yield reduction in Ethiopia using a GIS-based crop water balance model","docAbstract":"<p>In many parts of sub-Saharan Africa, subsistence agriculture is characterized by significant fluctuations in yield and production due to variations in moisture availability to staple crops. Widespread drought can lead to crop failures, with associated deterioration in food security. Ground data collection networks are sparse, so methods using geospatial rainfall estimates derived from satellite and gauge observations, where available, have been developed to calculate seasonal crop water balances. Using conventional crop production data for 4 years in Ethiopia (1996-1999), it was found that water-limited and water-unlimited growing regions can be distinguished. Furthermore, maize growing conditions are also indicative of conditions for sorghum. However, another major staple, teff, was found to behave sufficiently differently from maize to warrant studies of its own.</p>","language":"English","publisher":"Taylor & Francis","doi":"10.5589/m03-039","issn":"07038992","usgsCitation":"Senay, G., and Verdin, J., 2003, Characterization of yield reduction in Ethiopia using a GIS-based crop water balance model: Canadian Journal of Remote Sensing, v. 29, no. 6, p. 687-692, https://doi.org/10.5589/m03-039.","productDescription":"6 p.","startPage":"687","endPage":"692","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":236035,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"29","issue":"6","noUsgsAuthors":false,"publicationDate":"2014-06-02","publicationStatus":"PW","scienceBaseUri":"5059f4ece4b0c8380cd4bfdd","contributors":{"authors":[{"text":"Senay, G.B. 0000-0002-8810-8539","orcid":"https://orcid.org/0000-0002-8810-8539","contributorId":17741,"corporation":false,"usgs":true,"family":"Senay","given":"G.B.","affiliations":[],"preferred":false,"id":404728,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Verdin, J. 0000-0003-0238-9657","orcid":"https://orcid.org/0000-0003-0238-9657","contributorId":26112,"corporation":false,"usgs":true,"family":"Verdin","given":"J.","affiliations":[],"preferred":false,"id":404729,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70026135,"text":"70026135 - 2003 - Benefits and costs of increased levels of corticosterone in seabird chicks","interactions":[],"lastModifiedDate":"2017-11-18T09:29:55","indexId":"70026135","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1907,"text":"Hormones and Behavior","active":true,"publicationSubtype":{"id":10}},"title":"Benefits and costs of increased levels of corticosterone in seabird chicks","docAbstract":"Seabird chicks respond to food shortages by increasing corticosterone (cort) secretion, which is probably associated with fitness benefits and costs. To examine this, we experimentally increased levels of circulating cort in captive black-legged kittiwake chicks fed ad libitum. We found that cort-implanted chicks begged more frequently and were more aggressive compared to controls. These behavioral modifications must be beneficial to chicks as they facilitate acquisition of food from the parents and might trigger brood reduction and reduced competition for food. Cort-implanted chicks also increased food intake; however, their growth rates were similar to controls. To examine the costs of chronically increased circulating levels of cort, we removed cort implants and, after a 10-day recovery period, tested cognitive abilities of young kittiwakes. We found that the ability of kittiwakes to associate a visual cue with the presence of food in a choice situation was compromised by the experimental elevation of cort during development. To examine the long-term costs of increased levels of cort, 8 months later we tested the performance of the same individuals in a spatial task requiring them to make a detour around a barrier in order to escape from an enclosure. Individuals treated with cort during development took significantly more time to solve this task compared to controls. The results of this study suggest that the adrenocortical response of a developing bird to environmental stressors is associated with both benefits (increased food intake, foraging behavior, and aggression) and costs (low growth efficiency and compromised cognitive abilities later in life). This provides an evolutionary framework for relating juvenile physiological traits to fitness of birds in subsequent life-history stages. ?? 2003 Elsevier Science (USA). All rights reserved.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Hormones and Behavior","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/S0018-506X(02)00030-2","issn":"0018506X","usgsCitation":"Kitaysky, A., Kitaiskaia, E., Piatt, J.F., and Wingfield, J., 2003, Benefits and costs of increased levels of corticosterone in seabird chicks: Hormones and Behavior, v. 43, no. 1, p. 140-149, https://doi.org/10.1016/S0018-506X(02)00030-2.","startPage":"140","endPage":"149","numberOfPages":"10","costCenters":[],"links":[{"id":235063,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":208941,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/S0018-506X(02)00030-2"}],"volume":"43","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f0afe4b0c8380cd4a86d","contributors":{"authors":[{"text":"Kitaysky, A.S.","contributorId":104239,"corporation":false,"usgs":true,"family":"Kitaysky","given":"A.S.","email":"","affiliations":[],"preferred":false,"id":408053,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kitaiskaia, E.V.","contributorId":102668,"corporation":false,"usgs":true,"family":"Kitaiskaia","given":"E.V.","email":"","affiliations":[],"preferred":false,"id":408052,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Piatt, John F. 0000-0002-4417-5748 jpiatt@usgs.gov","orcid":"https://orcid.org/0000-0002-4417-5748","contributorId":3025,"corporation":false,"usgs":true,"family":"Piatt","given":"John","email":"jpiatt@usgs.gov","middleInitial":"F.","affiliations":[{"id":117,"text":"Alaska Science Center Biology WTEB","active":true,"usgs":true},{"id":116,"text":"Alaska Science Center Biology MFEB","active":true,"usgs":true},{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"preferred":true,"id":408051,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Wingfield, J.C.","contributorId":22929,"corporation":false,"usgs":true,"family":"Wingfield","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":408050,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70025013,"text":"70025013 - 2003 - Selection of the Mars Exploration Rover landing sites","interactions":[],"lastModifiedDate":"2018-12-12T08:36:51","indexId":"70025013","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2317,"text":"Journal of Geophysical Research E: Planets","active":true,"publicationSubtype":{"id":10}},"title":"Selection of the Mars Exploration Rover landing sites","docAbstract":"<p><span>The selection of Meridiani Planum and Gusev crater as the Mars Exploration Rover landing sites took over 2 years, involved broad participation of the science community via four open workshops, and narrowed an initial ∼155 potential sites (80–300 × 30 km) to four finalists based on science and safety. Engineering constraints important to the selection included (1) latitude (10°N–15°S) for maximum solar power, (2) elevation (less than −1.3 km) for sufficient atmosphere to slow the lander, (3) low horizontal winds, shear, and turbulence in the last few kilometers to minimize horizontal velocity, (4) low 10‐m‐scale slopes to reduce airbag spin‐up and bounce, (5) moderate rock abundance to reduce abrasion or strokeout of the airbags, and (6) a radar‐reflective, load‐bearing, and trafficable surface safe for landing and roving that is not dominated by fine‐grained dust. The evaluation of sites utilized existing as well as targeted orbital information acquired from the Mars Global Surveyor and Mars Odyssey. Three of the final four landing sites show strong evidence for surface processes involving water and appear capable of addressing the science objectives of the missions, which are to determine the aqueous, climatic, and geologic history of sites on Mars where conditions may have been favorable to the preservation of evidence of possible prebiotic or biotic processes. The evaluation of science criteria placed Meridiani and Gusev as the highest‐priority sites. The evaluation of the three most critical safety criteria (10‐m‐scale slopes, rocks, and winds) and landing simulation results indicated that Meridiani and Elysium Planitia are the safest sites, followed by Gusev and Isidis Planitia.</span></p>","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Geophysical Research E: Planets","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"American Geophysical Union","publisherLocation":"Washington, D.C.","doi":"10.1029/2003JE002074","issn":"01480227","usgsCitation":"Golombek, M., Grant, J.A., Parker, T.J., Kass, D., Crisp, J., Squyres, S.W., Haldemann, A.F., Adler, M., Lee, W., Bridges, N., Arvidson, R., Carr, M.H., Kirk, R.L., Knocke, P., Roncoli, R., Weitz, C., Schofield, J.T., Zurek, R., Christensen, P.R., Fergason, R., Anderson, F., and Rice, J.W., 2003, Selection of the Mars Exploration Rover landing sites: Journal of Geophysical Research E: Planets, v. 108, no. E12, 48 p., https://doi.org/10.1029/2003JE002074.","productDescription":"48 p.","costCenters":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"links":[{"id":233154,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Gusev Crater; Mars; Meridiani Planum","volume":"108","issue":"E12","noUsgsAuthors":false,"publicationDate":"2003-12-10","publicationStatus":"PW","scienceBaseUri":"505b8cd5e4b08c986b318166","contributors":{"authors":[{"text":"Golombek, M.P.","contributorId":52696,"corporation":false,"usgs":true,"family":"Golombek","given":"M.P.","email":"","affiliations":[],"preferred":false,"id":403443,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Grant, J. A.","contributorId":28334,"corporation":false,"usgs":true,"family":"Grant","given":"J.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":403436,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Parker, T. J.","contributorId":30776,"corporation":false,"usgs":false,"family":"Parker","given":"T.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":403437,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Kass, D.M.","contributorId":35513,"corporation":false,"usgs":true,"family":"Kass","given":"D.M.","email":"","affiliations":[],"preferred":false,"id":403440,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Crisp, J.A.","contributorId":36327,"corporation":false,"usgs":true,"family":"Crisp","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":403441,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Squyres, S. W.","contributorId":31836,"corporation":false,"usgs":true,"family":"Squyres","given":"S.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":403438,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Haldemann, A. F. C.","contributorId":33437,"corporation":false,"usgs":false,"family":"Haldemann","given":"A.","email":"","middleInitial":"F. C.","affiliations":[],"preferred":false,"id":403439,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Adler, M.","contributorId":56832,"corporation":false,"usgs":true,"family":"Adler","given":"M.","email":"","affiliations":[],"preferred":false,"id":403445,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Lee, W.J.","contributorId":76511,"corporation":false,"usgs":true,"family":"Lee","given":"W.J.","email":"","affiliations":[],"preferred":false,"id":403448,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Bridges, N.T.","contributorId":23673,"corporation":false,"usgs":true,"family":"Bridges","given":"N.T.","email":"","affiliations":[],"preferred":false,"id":403434,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Arvidson, R. E.","contributorId":46666,"corporation":false,"usgs":true,"family":"Arvidson","given":"R. E.","affiliations":[],"preferred":false,"id":403442,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Carr, M. H.","contributorId":84727,"corporation":false,"usgs":true,"family":"Carr","given":"M.","email":"","middleInitial":"H.","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":false,"id":403449,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Kirk, Randolph L. 0000-0003-0842-9226 rkirk@usgs.gov","orcid":"https://orcid.org/0000-0003-0842-9226","contributorId":2765,"corporation":false,"usgs":true,"family":"Kirk","given":"Randolph","email":"rkirk@usgs.gov","middleInitial":"L.","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":true,"id":403450,"contributorType":{"id":1,"text":"Authors"},"rank":13},{"text":"Knocke, P.C.","contributorId":20945,"corporation":false,"usgs":true,"family":"Knocke","given":"P.C.","email":"","affiliations":[],"preferred":false,"id":403433,"contributorType":{"id":1,"text":"Authors"},"rank":14},{"text":"Roncoli, R.B.","contributorId":65639,"corporation":false,"usgs":true,"family":"Roncoli","given":"R.B.","email":"","affiliations":[],"preferred":false,"id":403446,"contributorType":{"id":1,"text":"Authors"},"rank":15},{"text":"Weitz, C.M.","contributorId":8649,"corporation":false,"usgs":true,"family":"Weitz","given":"C.M.","email":"","affiliations":[],"preferred":false,"id":403430,"contributorType":{"id":1,"text":"Authors"},"rank":16},{"text":"Schofield, J. T.","contributorId":26099,"corporation":false,"usgs":false,"family":"Schofield","given":"J.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":403435,"contributorType":{"id":1,"text":"Authors"},"rank":17},{"text":"Zurek, R.W.","contributorId":71305,"corporation":false,"usgs":true,"family":"Zurek","given":"R.W.","email":"","affiliations":[],"preferred":false,"id":403447,"contributorType":{"id":1,"text":"Authors"},"rank":18},{"text":"Christensen, P. R.","contributorId":7819,"corporation":false,"usgs":false,"family":"Christensen","given":"P.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":403429,"contributorType":{"id":1,"text":"Authors"},"rank":19},{"text":"Fergason, R.L.","contributorId":13786,"corporation":false,"usgs":true,"family":"Fergason","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":403432,"contributorType":{"id":1,"text":"Authors"},"rank":20},{"text":"Anderson, F.S.","contributorId":8650,"corporation":false,"usgs":true,"family":"Anderson","given":"F.S.","email":"","affiliations":[],"preferred":false,"id":403431,"contributorType":{"id":1,"text":"Authors"},"rank":21},{"text":"Rice, J. W. Jr.","contributorId":53040,"corporation":false,"usgs":true,"family":"Rice","given":"J.","suffix":"Jr.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":403444,"contributorType":{"id":1,"text":"Authors"},"rank":22}]}}
,{"id":70026187,"text":"70026187 - 2003 - Temperature, pressure, and compositional effects on anomalous or \"self\" preservation of gas hydrates","interactions":[],"lastModifiedDate":"2012-03-12T17:20:21","indexId":"70026187","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1173,"text":"Canadian Journal of Physics","active":true,"publicationSubtype":{"id":10}},"title":"Temperature, pressure, and compositional effects on anomalous or \"self\" preservation of gas hydrates","docAbstract":"We previously reported on a thermal regime where pure, polycrystalline methane hydrate is preserved metastably in bulk at up to 75 K above its nominal temperature stability limit of 193 K at 0.1 MPa, following rapid release of the sample pore pressure. Large fractions (>50 vol.%) of methane hydrate can be preserved for 2-3 weeks by this method, reflecting the greatly suppressed rates of dissociation that characterize this \"anomalous preservation\" regime. This behavior contrasts that exhibited by methane hydrate at both colder (193-240 K) and warmer (272-290 K) isothermal test conditions, where dissociation rates increase monotonically with increasing temperature. Here, we report on recent experiments that further investigate the effects of temperature, pressure, and composition on anomalous preservation behavior. All tests conducted on sI methane hydrate yielded self-consistent results that confirm the highly temperature-sensitive but reproducible nature of anomalous preservation behavior. Temperature-stepping experiments conducted between 250 and 268 K corroborate the relative rates measured previously in isothermal preservation tests, and elevated pore-pressure tests showed that, as expected, dissociation rates are further reduced with increasing pressure. Surprisingly, sII methane-ethane hydrate was found to exhibit no comparable preservation effect when rapidly depressurized at 268 K, even though it is thermodynamically stable at higher temperatures and lower pressures than sI methane hydrate. These results, coupled with SEM imaging of quenched sample material from a variety of dissociation tests, strongly support our earlier arguments that ice-\"shielding\" effects provided by partial dissociation along hydrate grain surfaces do not serve as the primary mechanism for anomalous preservation. The underlying physical-chemistry mechanism(s) of anomalous preservation remains elusive, but appears to be based more on textural or morphological changes within the hydrate material itself, rather than on compositional zoning or ice-rind development.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Canadian Journal of Physics","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1139/p03-018","issn":"00084204","usgsCitation":"Stern, L., Circone, S., Kirby, S.H., and Durham, W., 2003, Temperature, pressure, and compositional effects on anomalous or \"self\" preservation of gas hydrates: Canadian Journal of Physics, v. 81, no. 1-2, p. 271-283, https://doi.org/10.1139/p03-018.","startPage":"271","endPage":"283","numberOfPages":"13","costCenters":[],"links":[{"id":234775,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":208782,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1139/p03-018"}],"volume":"81","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505ba4d0e4b08c986b3205dd","contributors":{"authors":[{"text":"Stern, L.A.","contributorId":38293,"corporation":false,"usgs":true,"family":"Stern","given":"L.A.","email":"","affiliations":[],"preferred":false,"id":408365,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Circone, S.","contributorId":35901,"corporation":false,"usgs":true,"family":"Circone","given":"S.","email":"","affiliations":[],"preferred":false,"id":408364,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kirby, S. H.","contributorId":51721,"corporation":false,"usgs":true,"family":"Kirby","given":"S.","middleInitial":"H.","affiliations":[],"preferred":false,"id":408366,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Durham, W.B.","contributorId":72135,"corporation":false,"usgs":true,"family":"Durham","given":"W.B.","email":"","affiliations":[],"preferred":false,"id":408367,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70025319,"text":"70025319 - 2003 - Copepod communities from surface and ground waters in the everglades, south Florida","interactions":[],"lastModifiedDate":"2021-08-22T19:30:47.088586","indexId":"70025319","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3444,"text":"Southeastern Naturalist","active":true,"publicationSubtype":{"id":10}},"title":"Copepod communities from surface and ground waters in the everglades, south Florida","docAbstract":"We studied species composition and individual abundance of copepods in the surficial aquifer northeast of Everglades National Park. We identified the spatial distribution of subsurface habitats by assessing the depth of the high porosity layers in the limestone along a canal system, and we used copepods to assess the exchange between surface water and ground water along canal banks, at levels in the wells where high porosity connections to the canals exist. Surface- and ground-water taxa were defined, and species composition was related to areal position, sampling depth, and time. Subsurface copepod communities were dominated by surface copepods that disperse into the aquifer following the groundwater seepage along canal L-31N. The similarities in species composition between wells along canal reaches, suggest that copepods mainly enter ground water horizontally along canals via active and passive dispersal. Thus, the copepod populations indicate continuous connections between surface- and ground waters. The most abundant species were Orthocyclops modestus, Arctodiaptomus floridanus, Mesocyclops edax, and Thermocyclops parvus, all known in literature from surface habitats; however, these species have been collected in ground water in ENP. Only two stygophiles were collected: Diacylcops nearcticus and Diacyclops crassicaudis brachycercus. Restoration of the Everglades ecosystem requires a mosaic of data to reveal a complete picture of this complex system. The use of copepods as indicators of seepage could be a tool in helping to assess the direction and the duration of surface and ground water exchange.","language":"English","publisher":"BioOne","doi":"10.1656/1528-7092(2003)002[0523:CCFSAG]2.0.CO;2","issn":"15287092","usgsCitation":"Bruno, M., Cunningham, K., and Perry, S., 2003, Copepod communities from surface and ground waters in the everglades, south Florida: Southeastern Naturalist, v. 2, no. 4, p. 523-546, https://doi.org/10.1656/1528-7092(2003)002[0523:CCFSAG]2.0.CO;2.","productDescription":"24 p.","startPage":"523","endPage":"546","costCenters":[],"links":[{"id":388335,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United  States","state":"Florida","otherGeospatial":"south Florida","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -83.14453125,\n              24.44714958973082\n            ],\n            [\n              -79.27734374999999,\n              24.44714958973082\n            ],\n            [\n              -79.27734374999999,\n              29.152161283318915\n            ],\n            [\n              -83.14453125,\n              29.152161283318915\n            ],\n            [\n              -83.14453125,\n              24.44714958973082\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"2","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059fbf2e4b0c8380cd4e04d","contributors":{"authors":[{"text":"Bruno, M.C.","contributorId":17402,"corporation":false,"usgs":true,"family":"Bruno","given":"M.C.","email":"","affiliations":[],"preferred":false,"id":404741,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cunningham, K.J.","contributorId":39852,"corporation":false,"usgs":true,"family":"Cunningham","given":"K.J.","email":"","affiliations":[],"preferred":false,"id":404742,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Perry, S.A.","contributorId":50113,"corporation":false,"usgs":true,"family":"Perry","given":"S.A.","email":"","affiliations":[],"preferred":false,"id":404743,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70185190,"text":"70185190 - 2003 - [Book Review] Biology of marine birds","interactions":[],"lastModifiedDate":"2017-05-08T18:42:15","indexId":"70185190","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3544,"text":"The Auk","onlineIssn":"1938-4254","printIssn":"0004-8038","active":true,"publicationSubtype":{"id":10}},"title":"[Book Review] Biology of marine birds","docAbstract":"<p>A text devoted to the biology and ecology of marine birds has not been published in the last 15 years. Although a number of more taxa-specific texts have been produced during that period, there has not been a single publication that attempted to review our knowledge of all the major seabird orders since the works of Nelson (1979), Croxall (1987), and Furness and Monaghan (1987). Following the publication of those works, a large and impressive body of literature has been produced. Given the rapid expansion of the field in the last two decades, the time was ripe for production of an extensive compendium on the biology, ecology, and conservation of the world's seabirds.</p><p>E. A. Schreiber and J. Burger are editors of this CRC publication, <i>Biology of Marine Birds</i>. The book consists of 19 chapters that vary in length from 15 to 51 pages. There are also two extensive appendices: (1) a list of seabird species (restricted to the orders Sphenisciformes, Procellariiformes, Pelecaniformes, and Charadriiformes, the latter limited to Stercorariidae, Laridae, Rhynchopidae, and Alcidae) and their IUCN status, and (2) a very useful table of species-specific life-history traits. The 19 chapters were prepared by 26 authors, among them some of the most respected and published seabird scientists in the world. A brief preface introduces the book, its objective (to provide an examination and summary of the research on seabirds), its audience (researchers, conservationists, managers, and policy-makers), and the taxa covered. The editors coauthored the introductory chapter, Seabirds in the Marine Environment. The authors describe distinctive characteristics of seabird life-histories in comparison to other taxa, hypotheses for why those lifestyles evolved and the potential role of energy limitation in the evolution of seabird life-histories. Along with a discussion of other common seabird traits, such as a propensity for colonial breeding, the authors also suggest directions for future research in seabird ecology.</p>","language":"English","publisher":"American Ornithological Society","doi":"10.1642/0004-8038(2003)120[0240:BOMB]2.0.CO;2","usgsCitation":"Jodice, P.G., Roby, D.D., Antolos, M., Lyons, D., Rizzolo, D., Wright, S.K., Anderson, C.D., Anderson, S.K., Nelson, S.K., Gall, A.E., and Wennerberg, L., 2003, [Book Review] Biology of marine birds: The Auk, v. 120, no. 1, p. 240-245, https://doi.org/10.1642/0004-8038(2003)120[0240:BOMB]2.0.CO;2.","productDescription":"6 p.","startPage":"240","endPage":"245","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":337705,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"120","issue":"1","publicComments":"Review of: <i>Biology of marine birds.  E. A. Schreiber and J. Burger, Eds. 2002. CRC Press, Boca Raton, Florida. xxii + 722 pp. ISBN 0-8493-9882-7. </i>","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58cba41de4b0849ce97dc75e","contributors":{"authors":[{"text":"Jodice, Patrick G.R. 0000-0001-8716-120X pjodice@usgs.gov","orcid":"https://orcid.org/0000-0001-8716-120X","contributorId":1119,"corporation":false,"usgs":true,"family":"Jodice","given":"Patrick","email":"pjodice@usgs.gov","middleInitial":"G.R.","affiliations":[{"id":198,"text":"Coop Res Unit Atlanta","active":true,"usgs":true}],"preferred":false,"id":684677,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Roby, Daniel D. 0000-0001-9844-0992 droby@usgs.gov","orcid":"https://orcid.org/0000-0001-9844-0992","contributorId":3702,"corporation":false,"usgs":true,"family":"Roby","given":"Daniel","email":"droby@usgs.gov","middleInitial":"D.","affiliations":[{"id":200,"text":"Coop Res Unit Seattle","active":true,"usgs":true}],"preferred":true,"id":684678,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Antolos, Michelle 0000-0003-0626-6021","orcid":"https://orcid.org/0000-0003-0626-6021","contributorId":64873,"corporation":false,"usgs":false,"family":"Antolos","given":"Michelle","email":"","affiliations":[],"preferred":false,"id":684679,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lyons, Donald E.","contributorId":20119,"corporation":false,"usgs":true,"family":"Lyons","given":"Donald E.","affiliations":[],"preferred":false,"id":684680,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Rizzolo, Daniel drizzolo@usgs.gov","contributorId":5631,"corporation":false,"usgs":true,"family":"Rizzolo","given":"Daniel","email":"drizzolo@usgs.gov","affiliations":[{"id":117,"text":"Alaska Science Center Biology WTEB","active":true,"usgs":true}],"preferred":true,"id":684681,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Wright, Sadie K.","contributorId":63223,"corporation":false,"usgs":false,"family":"Wright","given":"Sadie","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":684682,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Anderson, Cynthia D.","contributorId":189391,"corporation":false,"usgs":false,"family":"Anderson","given":"Cynthia","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":684683,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Anderson, Scott K.","contributorId":71748,"corporation":false,"usgs":false,"family":"Anderson","given":"Scott","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":684684,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Nelson, S. Kim","contributorId":86680,"corporation":false,"usgs":false,"family":"Nelson","given":"S.","email":"","middleInitial":"Kim","affiliations":[{"id":6680,"text":"Oregon State University","active":true,"usgs":false}],"preferred":false,"id":684685,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Gall, Adrian E.","contributorId":54396,"corporation":false,"usgs":false,"family":"Gall","given":"Adrian","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":684696,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Wennerberg, Liv","contributorId":63360,"corporation":false,"usgs":false,"family":"Wennerberg","given":"Liv","affiliations":[],"preferred":false,"id":684697,"contributorType":{"id":1,"text":"Authors"},"rank":11}]}}
,{"id":70026188,"text":"70026188 - 2003 - Removal of dissolved textile dyes from wastewater by a compost sorbent","interactions":[],"lastModifiedDate":"2012-03-12T17:20:31","indexId":"70026188","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1275,"text":"Coloration Technology","active":true,"publicationSubtype":{"id":10}},"title":"Removal of dissolved textile dyes from wastewater by a compost sorbent","docAbstract":"The objective of this study was to evaluate the potential for treating dye-contaminated waste streams by sorption using compost as a low-cost sorbent. A mature, thermophilic compost sample was used to sorb CI Acid Black 24, CI Acid Orange 74, CI Basic Blue 9, CI Basic Green 4, CI Direct Blue 71, CI Direct Orange 39, CI Reactive Orange 16 and CI Reactive Red 2 from solution using a batch-sorption method. With the exception of the two reactive dyes, the sorption kinetics were favourable for a continuous-flow treatment process with the compost-dye mixtures reaching a steady state within 3-5 h. Based on limited comparisons, the affinity of the compost for each dye appeared to be competitive with other non-activated carbon sorbents. The results suggest that additional research on using compost as a sorbent for dye-contaminated solutions is warranted.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Coloration Technology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"14723581","usgsCitation":"Tsui, L., Roy, W.R., and Cole, M., 2003, Removal of dissolved textile dyes from wastewater by a compost sorbent: Coloration Technology, v. 119, no. 1, p. 14-18.","startPage":"14","endPage":"18","numberOfPages":"5","costCenters":[],"links":[{"id":234809,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"119","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505aa72be4b0c8380cd85279","contributors":{"authors":[{"text":"Tsui, L.S.","contributorId":61998,"corporation":false,"usgs":true,"family":"Tsui","given":"L.S.","email":"","affiliations":[],"preferred":false,"id":408369,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Roy, William R.","contributorId":45454,"corporation":false,"usgs":true,"family":"Roy","given":"William","middleInitial":"R.","affiliations":[],"preferred":false,"id":408368,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cole, M.A.","contributorId":77262,"corporation":false,"usgs":true,"family":"Cole","given":"M.A.","email":"","affiliations":[],"preferred":false,"id":408370,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70026189,"text":"70026189 - 2003 - Field evaluation of boat-mounted acoustic Doppler instruments used to measure streamflow","interactions":[],"lastModifiedDate":"2012-03-12T17:20:31","indexId":"70026189","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Field evaluation of boat-mounted acoustic Doppler instruments used to measure streamflow","docAbstract":"The use of instruments based on the Doppler principle for measuring water velocity and computing discharge is common within the U.S. Geological Survey (USGS). The instruments and software have changed appreciably during the last 5 years; therefore, the USGS has begun field validation of the instruments used to make discharge measurements from a moving boat. Instruments manufactured by SonTek/YSI and RD Instruments, Inc. were used to collect discharge data at five different sites. One or more traditional discharge measurements were made using a Price AA current meter and standard USGS procedures concurrent with the acoustic instruments at each site. Discharges measured with the acoustic instruments were compared with discharges measured with Price AA current meters and the USGS stage-discharge rating for each site. The mean discharges measured by each acoustic instrument were within 5 percent of the Price AA-based measurement and (or) discharge from the stage-discharge rating.","largerWorkTitle":"Proceedings of the IEEE Working Conference on Current Measurement","conferenceTitle":"Proceedings of the IEEE Seventh Working Conference on Current Measurement; Current and Wave Monitoring and Emerging Technologies","conferenceDate":"13 March 2003 through 15 March 2003","conferenceLocation":"San Diego, CA","language":"English","usgsCitation":"Mueller, D.S., 2003, Field evaluation of boat-mounted acoustic Doppler instruments used to measure streamflow, <i>in</i> Proceedings of the IEEE Working Conference on Current Measurement, San Diego, CA, 13 March 2003 through 15 March 2003, p. 30-34.","startPage":"30","endPage":"34","numberOfPages":"5","costCenters":[],"links":[{"id":234810,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0fb3e4b0c8380cd539ae","contributors":{"editors":[{"text":"Rizoli J.A.","contributorId":128304,"corporation":true,"usgs":false,"organization":"Rizoli J.A.","id":536583,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Mueller, D. S.","contributorId":51338,"corporation":false,"usgs":true,"family":"Mueller","given":"D.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":408371,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70025081,"text":"70025081 - 2003 - Athena Mars rover science investigation","interactions":[],"lastModifiedDate":"2012-03-12T17:20:27","indexId":"70025081","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2317,"text":"Journal of Geophysical Research E: Planets","active":true,"publicationSubtype":{"id":10}},"title":"Athena Mars rover science investigation","docAbstract":"Each Mars Exploration Rover carries an integrated suite of scientific instruments and tools called the Athena science payload. The primary objective of the Athena science investigation is to explore two sites on the Martian surface where water may once have been present, and to assess past environmental conditions at those sites and their suitability for life. The remote sensing portion of the payload uses a mast called the Pancam Mast Assembly (PMA) that provides pointing for two instruments: the Panoramic Camera (Pancam), and the Miniature Thermal Emission Spectrometer (Mini-TES). Pancam provides high-resolution, color, stereo imaging, while Mini-TES provides spectral cubes at mid-infrared wavelengths. For in-situ study, a five degree-of-freedom arm called the Instrument Deployment Device (IDD) carries four more tools: a Microscopic Imager (MI) for close-up imaging, an Alpha Particle X-Ray Spectrometer (APXS) for elemental chemistry, a Mo??ssbauer Spectrometer (MB) for the mineralogy of Fe-bearing materials, and a Rock Abrasion Tool (RAT) for removing dusty and weathered surfaces and exposing fresh rock underneath. The payload also includes magnets that allow the instruments to study the composition of magnetic Martian materials. All of the Athena instruments have undergone extensive calibration, both individually and using a set of geologic reference materials that are being measured with all the instruments. Using a MER-like rover and payload in a number of field settings, we have devised operations processes that will enable us to use the MER rovers to formulate and test scientific hypotheses concerning past environmental conditions and habitability at the landing sites. Copyright 2003 by the American Geophysical Union.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Geophysical Research E: Planets","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"01480227","usgsCitation":"Squyres, S.W., Arvidson, R., Baumgartner, E., Bell, J., Christensen, P.R., Gorevan, S., Herkenhoff, K.E., Klingelhofer, G., Madsen, M., Morris, R., Rieder, R., and Romero, R., 2003, Athena Mars rover science investigation: Journal of Geophysical Research E: Planets, v. 108, no. 12.","costCenters":[],"links":[{"id":235837,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"108","issue":"12","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059ee9ee4b0c8380cd49e84","contributors":{"authors":[{"text":"Squyres, S. W.","contributorId":31836,"corporation":false,"usgs":true,"family":"Squyres","given":"S.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":403738,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Arvidson, R. E.","contributorId":46666,"corporation":false,"usgs":true,"family":"Arvidson","given":"R. E.","affiliations":[],"preferred":false,"id":403739,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Baumgartner, E.T.","contributorId":48057,"corporation":false,"usgs":true,"family":"Baumgartner","given":"E.T.","email":"","affiliations":[],"preferred":false,"id":403740,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bell, J.F. III","contributorId":97612,"corporation":false,"usgs":true,"family":"Bell","given":"J.F.","suffix":"III","email":"","affiliations":[],"preferred":false,"id":403745,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Christensen, P. R.","contributorId":7819,"corporation":false,"usgs":false,"family":"Christensen","given":"P.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":403735,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Gorevan, S.","contributorId":7886,"corporation":false,"usgs":true,"family":"Gorevan","given":"S.","email":"","affiliations":[],"preferred":false,"id":403736,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Herkenhoff, K. E.","contributorId":57959,"corporation":false,"usgs":true,"family":"Herkenhoff","given":"K.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":403742,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Klingelhofer, G.","contributorId":57195,"corporation":false,"usgs":true,"family":"Klingelhofer","given":"G.","email":"","affiliations":[],"preferred":false,"id":403741,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Madsen, M.B.","contributorId":97291,"corporation":false,"usgs":true,"family":"Madsen","given":"M.B.","affiliations":[],"preferred":false,"id":403744,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Morris, R.V.","contributorId":6978,"corporation":false,"usgs":true,"family":"Morris","given":"R.V.","affiliations":[],"preferred":false,"id":403734,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Rieder, R.","contributorId":28046,"corporation":false,"usgs":true,"family":"Rieder","given":"R.","email":"","affiliations":[],"preferred":false,"id":403737,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Romero, R.A.","contributorId":68612,"corporation":false,"usgs":true,"family":"Romero","given":"R.A.","email":"","affiliations":[],"preferred":false,"id":403743,"contributorType":{"id":1,"text":"Authors"},"rank":12}]}}
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