{"pageNumber":"260","pageRowStart":"6475","pageSize":"25","recordCount":10462,"records":[{"id":70029392,"text":"70029392 - 2005 - Home range and space use patterns of flathead catfish during the summer-fall period in two Missouri streams","interactions":[],"lastModifiedDate":"2016-08-21T17:16:01","indexId":"70029392","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3624,"text":"Transactions of the American Fisheries Society","active":true,"publicationSubtype":{"id":10}},"title":"Home range and space use patterns of flathead catfish during the summer-fall period in two Missouri streams","docAbstract":"<p class=\"p1\"><span class=\"s1\">Flathead catfish <i>Pylodictis olivaris</i> were radio-tracked in the Grand River and Cuivre River, Missouri, from late July until they moved to overwintering habitats in late October. Fish moved within a definable area, and although occasional long-distance movements occurred, the fish typically returned to the previously occupied area. Seasonal home range was calculated with the use of kernel density estimation, which can be interpreted as a probabilistic utilization distribution that documents the internal structure of the estimate by delineating portions of the range that was used a specified percentage of the time. A traditional linear range also was reported. Most flathead catfish (89%) had one 50% kernel-estimated core area, whereas 11% of the fish split their time between two core areas. Core areas were typically in the middle of the 90% kernel-estimated home range (58%), although several had core areas in upstream (26%) and downstream (16%) portions of the home range. Home-range size did not differ based on river, sex, or size and was highly variable among individuals. The median 95% kernel estimate was 1,085 m (range, 70&ndash; 69,090 m) for all fish. The median 50% kernel-estimated core area was 135 m (10&ndash;2,260 m). The median linear range was 3,510 m (150&ndash;50,400 m). Fish pairs with core areas in the same and neighboring pools had static joint space use values of up to 49% (area of intersection index), indicating substantial overlap and use of the same area. However, all fish pairs had low dynamic joint space use values (&lt;0.07; coefficient of association), indicating that fish pairs were temporally segregated, rarely occurring in the same location at the same time.</span></p>","language":"English","publisher":"American Fisheries Society","doi":"10.1577/T04-064.1","issn":"00028487","usgsCitation":"Vokoun, J.C., and Rabeni, C.F., 2005, Home range and space use patterns of flathead catfish during the summer-fall period in two Missouri streams: Transactions of the American Fisheries Society, v. 134, no. 2, p. 509-517, https://doi.org/10.1577/T04-064.1.","productDescription":"9 p.","startPage":"509","endPage":"517","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":237772,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Missouri","otherGeospatial":"Cuivre River, Grand River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -93.2958984375,\n              39.28860847419942\n            ],\n            [\n              -93.2958984375,\n              39.51781418588603\n            ],\n            [\n              -92.98278808593749,\n              39.51781418588603\n            ],\n            [\n              -92.98278808593749,\n              39.28860847419942\n            ],\n            [\n              -93.2958984375,\n              39.28860847419942\n            ]\n          ]\n        ]\n      }\n    },\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -91.10412597656249,\n              38.70694605159386\n            ],\n            [\n              -91.10412597656249,\n              39.07037913108751\n            ],\n            [\n              -90.55755615234375,\n              39.07037913108751\n            ],\n            [\n              -90.55755615234375,\n              38.70694605159386\n            ],\n            [\n              -91.10412597656249,\n              38.70694605159386\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"134","issue":"2","noUsgsAuthors":false,"publicationDate":"2011-01-09","publicationStatus":"PW","scienceBaseUri":"505a3202e4b0c8380cd5e44c","contributors":{"authors":[{"text":"Vokoun, Jason C.","contributorId":173912,"corporation":false,"usgs":false,"family":"Vokoun","given":"Jason","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":422535,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rabeni, Charles F.","contributorId":34804,"corporation":false,"usgs":true,"family":"Rabeni","given":"Charles","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":422534,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70029692,"text":"70029692 - 2005 - Relation of organic contaminant equilibrium sorption and kinetic uptake in plants","interactions":[],"lastModifiedDate":"2012-03-12T17:21:07","indexId":"70029692","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1565,"text":"Environmental Science & Technology","onlineIssn":"1520-5851","printIssn":"0013-936X","active":true,"publicationSubtype":{"id":10}},"title":"Relation of organic contaminant equilibrium sorption and kinetic uptake in plants","docAbstract":"Plant uptake is one of the environmental processes that influence contaminant fate. Understanding the magnitude and rate of plant uptake is critical to assessing potential crop contamination and the development of phytoremediation technologies. We determined (1) the partition-dominated equilibrium sorption of lindane (LDN) and hexachlorobenzene (HCB) by roots and shoots of wheat seedlings, (2) the kinetic uptake of LDN and HCB by roots and shoots of wheat seedlings, (3) the kinetic uptake of HCB, tetrachloroethylene (PCE), and trichloroethylene (TCE) by roots and shoots of ryegrass seedlings, and (4) the lipid, carbohydrate, and water contents of the plants. Although the determined sorption and the plant composition together suggest the predominant role of plant lipids for the sorption of LDN and HCB, the predicted partition with lipids of LDN and HCB using the octanol-water partition coefficients is notably lower than the measured sorption, due presumably to underestimation of the plant lipid contents and to the fact that octanol is less effective as a partition medium than plant lipids. The equilibrium sorption or the estimated partition can be viewed as the kinetic uptake limits. The uptakes of LDN, PCE, and TCE from water at fixed concentrations increased with exposure time in approach to steady states. The uptake of HCB did not reach a plateau within the tested time because of its exceptionally high partition coefficient. In all of the cases, the observed uptakes were lower than their respective limits, due presumably to contaminant dissipation in and limited water transpiration by the plants. ?? 2005 American Chemical Society.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Environmental Science and Technology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1021/es050424z","issn":"0013936X","usgsCitation":"Li, H., Sheng, G., Chiou, C.T., and Xu, O., 2005, Relation of organic contaminant equilibrium sorption and kinetic uptake in plants: Environmental Science & Technology, v. 39, no. 13, p. 4864-4870, https://doi.org/10.1021/es050424z.","startPage":"4864","endPage":"4870","numberOfPages":"7","costCenters":[],"links":[{"id":212707,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1021/es050424z"},{"id":240234,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"39","issue":"13","noUsgsAuthors":false,"publicationDate":"2005-05-19","publicationStatus":"PW","scienceBaseUri":"50e4a69be4b0e8fec6cdc225","contributors":{"authors":[{"text":"Li, H.","contributorId":44338,"corporation":false,"usgs":true,"family":"Li","given":"H.","email":"","affiliations":[],"preferred":false,"id":423839,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sheng, G.","contributorId":70961,"corporation":false,"usgs":true,"family":"Sheng","given":"G.","email":"","affiliations":[],"preferred":false,"id":423840,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Chiou, C. T.","contributorId":97080,"corporation":false,"usgs":true,"family":"Chiou","given":"C.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":423841,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Xu, O.","contributorId":8678,"corporation":false,"usgs":true,"family":"Xu","given":"O.","email":"","affiliations":[],"preferred":false,"id":423838,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70029660,"text":"70029660 - 2005 - Widespread detection of N, N-diethyl-m-toluamide in U.S. streams: Comparison with concentrations of pesticides, personal care products, and other organic wastewater compounds","interactions":[],"lastModifiedDate":"2021-05-27T14:46:10.989349","indexId":"70029660","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1571,"text":"Environmental Toxicology and Chemistry","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Widespread detection of <i>N</i>,<i>N</i>-diethyl-<i>m</i>-toluamide in U.S. streams: Comparison with concentrations of pesticides, personal care products, and other organic wastewater compounds","title":"Widespread detection of N, N-diethyl-m-toluamide in U.S. streams: Comparison with concentrations of pesticides, personal care products, and other organic wastewater compounds","docAbstract":"<p>One of the most frequently detected organic chemicals in a nationwide study concerning the effects of wastewater on stream water quality conducted in the year 2000 was the widely used insect repellant <i>N</i>,<i>N</i>-diethyl-<i>m</i>-toluamide (DEET). It was detected at levels of 0.02 &mu;g/L or greater in 73% of the stream sites sampled, with the selection of sampling sites being biased toward streams thought to be subject to wastewater contamination (i.e., downstream from intense urbanization and livestock production). Although DEET frequently was detected at all sites, the median concentration was low (0.05 &mu;g/L). The highest concentrations of DEET were found in streams from the urban areas (maximum concentration, 1.1 &mu;g/L). The results of the present study suggest that the movement of DEET to streams through wastewater-treatment systems is an important mechanism that might lead to the exposure of aquatic organisms to this chemical.</p>","language":"English","publisher":"Elsevier","doi":"10.1897/04-297R.1","usgsCitation":"Sandstrom, M.W., Kolpin, D., Thurman, E., and Zaugg, S., 2005, Widespread detection of N, N-diethyl-m-toluamide in U.S. streams: Comparison with concentrations of pesticides, personal care products, and other organic wastewater compounds: Environmental Toxicology and Chemistry, v. 24, no. 5, p. 1029-1034, https://doi.org/10.1897/04-297R.1.","productDescription":"6 p.","startPage":"1029","endPage":"1034","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":452,"text":"National Water Quality Laboratory","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":240267,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -123.04687499999999,\n              49.03786794532644\n            ],\n            [\n              -123.04687499999999,\n              48.04870994288686\n            ],\n            [\n              -124.892578125,\n              48.40003249610685\n            ],\n            [\n              -124.01367187499999,\n              46.6795944656402\n            ],\n            [\n              -124.71679687499999,\n              43.004647127794435\n            ],\n            [\n              -124.541015625,\n              41.64007838467894\n            ],\n            [\n              -125.068359375,\n              40.38002840251183\n            ],\n            [\n              -123.837890625,\n              38.34165619279593\n            ],\n            [\n              -121.81640624999999,\n              36.4566360115962\n            ],\n            [\n              -120.84960937499999,\n              34.59704151614417\n            ],\n            [\n              -118.828125,\n              33.94335994657882\n            ],\n            [\n              -117.0703125,\n              32.62087018318113\n            ],\n            [\n              -115.04882812499999,\n              32.62087018318113\n            ],\n            [\n              -110.56640625,\n              31.27855085894653\n            ],\n            [\n              -108.017578125,\n              31.353636941500987\n            ],\n            [\n              -108.017578125,\n              31.653381399664\n            ],\n            [\n              -106.5234375,\n              31.653381399664\n            ],\n            [\n              -105.29296874999999,\n              30.675715404167743\n            ],\n            [\n              -104.32617187499999,\n              29.38217507514529\n            ],\n            [\n              -103.0078125,\n              28.998531814051795\n            ],\n            [\n              -102.12890625,\n              29.76437737516313\n            ],\n            [\n              -101.07421875,\n              29.22889003019423\n            ],\n            [\n              -99.931640625,\n              27.371767300523047\n            ],\n            [\n              -99.404296875,\n              26.43122806450644\n            ],\n            [\n              -97.20703125,\n              25.720735134412106\n            ],\n            [\n              -97.20703125,\n              27.449790329784214\n            ],\n            [\n              -96.240234375,\n              28.69058765425071\n            ],\n            [\n              -93.779296875,\n              29.611670115197377\n            ],\n            [\n              -89.20898437499999,\n              29.152161283318915\n            ],\n            [\n              -89.56054687499999,\n              30.14512718337613\n            ],\n            [\n              -87.978515625,\n              30.372875188118016\n            ],\n            [\n              -86.396484375,\n              30.221101852485987\n            ],\n            [\n              -84.814453125,\n              29.458731185355344\n            ],\n            [\n              -84.0234375,\n              29.916852233070173\n            ],\n            [\n              -82.79296874999999,\n              28.767659105691255\n            ],\n            [\n              -82.880859375,\n              27.761329874505233\n            ],\n            [\n              -81.123046875,\n              25.085598897064777\n            ],\n            [\n              -80.244140625,\n              25.16517336866393\n            ],\n            [\n              -79.98046875,\n              27.371767300523047\n            ],\n            [\n              -81.2109375,\n              29.152161283318915\n            ],\n            [\n              -81.298828125,\n              31.12819929911196\n            ],\n            [\n              -79.8046875,\n              32.694865977875075\n            ],\n            [\n              -78.046875,\n              33.87041555094183\n            ],\n            [\n              -76.201171875,\n              35.02999636902566\n            ],\n            [\n              -75.673828125,\n              35.67514743608467\n            ],\n            [\n              -75.849609375,\n              37.020098201368114\n            ],\n            [\n              -73.564453125,\n              40.17887331434696\n            ],\n            [\n              -73.47656249999999,\n              40.51379915504413\n            ],\n            [\n              -69.697265625,\n              41.64007838467894\n            ],\n            [\n              -70.751953125,\n              42.48830197960227\n            ],\n            [\n              -70.13671875,\n              43.51668853502909\n            ],\n            [\n              -67.1484375,\n              44.33956524809713\n            ],\n            [\n              -67.1484375,\n              45.27488643704894\n            ],\n            [\n              -67.763671875,\n              45.9511496866914\n            ],\n            [\n              -67.8515625,\n              47.27922900257082\n            ],\n            [\n              -68.90625,\n              47.45780853075031\n            ],\n            [\n              -70.048828125,\n              46.98025235521883\n            ],\n            [\n              -70.751953125,\n              45.706179285330855\n            ],\n            [\n              -71.455078125,\n              45.089035564831036\n            ],\n            [\n              -74.970703125,\n              44.96479793033104\n            ],\n            [\n              -77.16796875,\n              43.58039085560786\n            ],\n            [\n              -79.27734374999999,\n              43.58039085560786\n            ],\n            [\n              -78.837890625,\n              42.81152174509788\n            ],\n            [\n              -81.298828125,\n              41.77131167976407\n            ],\n            [\n              -83.056640625,\n              41.77131167976407\n            ],\n            [\n              -82.529296875,\n              43.389081939117496\n            ],\n            [\n              -82.44140625,\n              44.08758502824518\n            ],\n            [\n              -83.84765625,\n              43.58039085560786\n            ],\n            [\n              -83.3203125,\n              44.715513732021336\n            ],\n            [\n              -83.671875,\n              45.460130637921004\n            ],\n            [\n              -84.990234375,\n              45.644768217751924\n            ],\n            [\n              -86.572265625,\n              44.653024159812\n            ],\n            [\n              -86.30859375,\n              42.87596410238254\n            ],\n            [\n              -86.572265625,\n              42.09822241118974\n            ],\n            [\n              -87.978515625,\n              43.004647127794435\n            ],\n            [\n              -86.923828125,\n              45.213003555993964\n            ],\n            [\n              -85.78125,\n              45.82879925192134\n            ],\n            [\n              -83.583984375,\n              45.767522962149904\n            ],\n            [\n              -84.990234375,\n              46.86019101567027\n            ],\n            [\n              -87.275390625,\n              46.6795944656402\n            ],\n            [\n              -88.154296875,\n              47.040182144806664\n            ],\n            [\n              -87.978515625,\n              47.635783590864854\n            ],\n            [\n              -89.47265625,\n              46.98025235521883\n            ],\n            [\n              -90.87890625,\n              46.619261036171515\n            ],\n            [\n              -91.23046875,\n              46.800059446787316\n            ],\n            [\n              -89.20898437499999,\n              48.22467264956519\n            ],\n            [\n              -91.669921875,\n              48.22467264956519\n            ],\n            [\n              -93.07617187499999,\n              48.69096039092549\n            ],\n            [\n              -94.306640625,\n              48.748945343432936\n            ],\n            [\n              -95.185546875,\n              49.26780455063753\n            ],\n            [\n              -95.712890625,\n              48.980216985374994\n            ],\n            [\n              -123.04687499999999,\n              49.03786794532644\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"24","issue":"5","noUsgsAuthors":false,"publicationDate":"2005-05-01","publicationStatus":"PW","scienceBaseUri":"505bd0b0e4b08c986b32efda","contributors":{"authors":[{"text":"Sandstrom, Mark W. 0000-0003-0006-5675 sandstro@usgs.gov","orcid":"https://orcid.org/0000-0003-0006-5675","contributorId":706,"corporation":false,"usgs":true,"family":"Sandstrom","given":"Mark","email":"sandstro@usgs.gov","middleInitial":"W.","affiliations":[{"id":452,"text":"National Water Quality Laboratory","active":true,"usgs":true},{"id":503,"text":"Office of Water Quality","active":true,"usgs":true},{"id":37464,"text":"WMA - Laboratory & Analytical Services Division","active":true,"usgs":true},{"id":5046,"text":"Branch of Analytical Serv (NWQL)","active":true,"usgs":true}],"preferred":true,"id":423682,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kolpin, D.W.","contributorId":87565,"corporation":false,"usgs":true,"family":"Kolpin","given":"D.W.","email":"","affiliations":[],"preferred":false,"id":423684,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Thurman, E.M.","contributorId":102864,"corporation":false,"usgs":true,"family":"Thurman","given":"E.M.","affiliations":[],"preferred":false,"id":423685,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Zaugg, S.D.","contributorId":82811,"corporation":false,"usgs":true,"family":"Zaugg","given":"S.D.","email":"","affiliations":[],"preferred":false,"id":423683,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70029624,"text":"70029624 - 2005 - The evolution of vertebrate Toll-like receptors","interactions":[],"lastModifiedDate":"2012-03-12T17:20:54","indexId":"70029624","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3165,"text":"Proceedings of the National Academy of Sciences of the United States of America","active":true,"publicationSubtype":{"id":10}},"title":"The evolution of vertebrate Toll-like receptors","docAbstract":"The complete sequences of Takifugu Toll-like receptor (TLR) loci and gene predictions from many draft genomes enable comprehensive molecular phylogenetic analysis. Strong selective pressure for recognition of and response to pathogen-associated molecular patterns has maintained a largely unchanging TLR recognition in all vertebrates. There are six major families of vertebrate TLRs. This repertoire is distinct from that of invertebrates. TLRs within a family recognize a general class of pathogen-associated molecular patterns. Most vertebrates have exactly one gene ortholog for each TLR family. The family including TLR1 has more species-specific adaptations than other families. A major family including TLR11 is represented in humans only by a pseudogene. Coincidental evolution plays a minor role in TLR evolution. The sequencing phase of this study produced finished genomic sequences for the 12 Takifugu rubripes TLRs. In addition, we have produced > 70 gene models, including sequences from the opossum, chicken, frog, dog, sea urchin, and sea squirt. ?? 2005 by The National Academy of Sciences of the USA.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Proceedings of the National Academy of Sciences of the United States of America","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1073/pnas.0502272102","issn":"00278424","usgsCitation":"Roach, J., Glusman, G., Rowen, L., Kaur, A., Purcell, M.K., Smith, K., Hood, L., and Aderem, A., 2005, The evolution of vertebrate Toll-like receptors: Proceedings of the National Academy of Sciences of the United States of America, v. 102, no. 27, p. 9577-9582, https://doi.org/10.1073/pnas.0502272102.","startPage":"9577","endPage":"9582","numberOfPages":"6","costCenters":[],"links":[{"id":477796,"rank":10000,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://www.ncbi.nlm.nih.gov/pmc/articles/1172252","text":"External Repository"},{"id":210492,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1073/pnas.0502272102"},{"id":237427,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"102","issue":"27","noUsgsAuthors":false,"publicationDate":"2005-06-23","publicationStatus":"PW","scienceBaseUri":"505babe8e4b08c986b323164","contributors":{"authors":[{"text":"Roach, J.C.","contributorId":19362,"corporation":false,"usgs":true,"family":"Roach","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":423499,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Glusman, G.","contributorId":82519,"corporation":false,"usgs":true,"family":"Glusman","given":"G.","email":"","affiliations":[],"preferred":false,"id":423505,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rowen, L.","contributorId":82915,"corporation":false,"usgs":true,"family":"Rowen","given":"L.","email":"","affiliations":[],"preferred":false,"id":423506,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Kaur, A.","contributorId":35532,"corporation":false,"usgs":true,"family":"Kaur","given":"A.","email":"","affiliations":[],"preferred":false,"id":423501,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Purcell, M. K.","contributorId":78464,"corporation":false,"usgs":true,"family":"Purcell","given":"M.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":423504,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Smith, K.D.","contributorId":64003,"corporation":false,"usgs":true,"family":"Smith","given":"K.D.","email":"","affiliations":[],"preferred":false,"id":423503,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Hood, L.E.","contributorId":30026,"corporation":false,"usgs":true,"family":"Hood","given":"L.E.","email":"","affiliations":[],"preferred":false,"id":423500,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Aderem, A.","contributorId":41645,"corporation":false,"usgs":true,"family":"Aderem","given":"A.","email":"","affiliations":[],"preferred":false,"id":423502,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":70029569,"text":"70029569 - 2005 - Atmospheric dry deposition in the vicinity of the Salton Sea, California - I: Air pollution and deposition in a desert environment","interactions":[],"lastModifiedDate":"2012-03-12T17:20:52","indexId":"70029569","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":924,"text":"Atmospheric Environment","active":true,"publicationSubtype":{"id":10}},"title":"Atmospheric dry deposition in the vicinity of the Salton Sea, California - I: Air pollution and deposition in a desert environment","docAbstract":"Air pollutant concentrations and atmospheric dry deposition were monitored seasonally at the Salton Sea, southern California. Measurements of ozone (O 3), nitric acid vapor (HNO3), ammonia (NH3), nitric oxide (NO), nitrogen dioxide (NO2) and sulfur dioxide (SO 2) were performed using passive samplers. Deposition rates of NO 3-, NH4+, Cl-, SO 42-, Na+, K+ and Ca2+ to creosote bush branches and nylon filters as surrogate surfaces were determined for one-week long exposure periods. Maximum O3 values were recorded in spring with 24-h average values of 108.8 ??g m-3. Concentrations of NO and NO2 were low and within ranges of the non-urban areas in California (0.4-5.6 and 3.3-16.2 ??g m-3 ranges, respectively). Concentrations of HNO3 (2.0-6.7 ??g m-3) and NH 3 (6.4-15.7 ??g m-3) were elevated and above the levels typical for remote locations in California. Deposition rates of Cl-, SO42-, Na+, K+ and Ca2+ were related to the influence of sea spray or to suspended soil particles, and no strong enrichments caused by ions originated by human activities were detected. Dry deposition rates of NO3- and NH4+ were similar to values registered in areas where symptoms of nitrogen saturation and changes in species composition have been described. Deposition of nitrogenous compounds might be contributing to eutrophication processes at the Salton Sea. ?? 2005 Elsevier Ltd. All rights reserved.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Atmospheric Environment","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.atmosenv.2005.04.016","issn":"13522310","usgsCitation":"Alonso, R., Bytnerowicz, A., and Boarman, W., 2005, Atmospheric dry deposition in the vicinity of the Salton Sea, California - I: Air pollution and deposition in a desert environment: Atmospheric Environment, v. 39, no. 26, p. 4671-4679, https://doi.org/10.1016/j.atmosenv.2005.04.016.","startPage":"4671","endPage":"4679","numberOfPages":"9","costCenters":[],"links":[{"id":210684,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.atmosenv.2005.04.016"},{"id":237679,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"39","issue":"26","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059eec1e4b0c8380cd49f21","contributors":{"authors":[{"text":"Alonso, R.","contributorId":74190,"corporation":false,"usgs":true,"family":"Alonso","given":"R.","email":"","affiliations":[],"preferred":false,"id":423305,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bytnerowicz, A.","contributorId":30027,"corporation":false,"usgs":true,"family":"Bytnerowicz","given":"A.","email":"","affiliations":[],"preferred":false,"id":423303,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Boarman, W.I.","contributorId":73523,"corporation":false,"usgs":true,"family":"Boarman","given":"W.I.","email":"","affiliations":[],"preferred":false,"id":423304,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70029557,"text":"70029557 - 2005 - Catch rates relative to angler party size with implications for monitoring angler success","interactions":[],"lastModifiedDate":"2012-03-12T17:20:53","indexId":"70029557","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3624,"text":"Transactions of the American Fisheries Society","active":true,"publicationSubtype":{"id":10}},"title":"Catch rates relative to angler party size with implications for monitoring angler success","docAbstract":"Angler catch rates often are used to monitor angler success, assess the need for additional management actions, and evaluate the effectiveness of management practices. Potential linkages between catch rate and angler party size were examined to assess how party size might affect the use of catch rate as an index of angler success in recreational fisheries. Data representing 22,355 completed interviews conducted at access points in lakes and reservoirs throughout Mississippi during 1987-2003 were analyzed. Total party catch was not proportional to total party effort; thus, catch rate decreased as party size increased. Depending on the taxa targeted, the average catch rate per angler decreased 40-50% between parties of one and parties of two, although subsequent decreases were less substantial. Because party size accounted for a considerable portion of the variability in catch rate over time and space, failure to remove this variability weakens the manager's ability to detect differences or changes in catch rates. Therefore, the use of catch rates to monitor fisheries may be inappropriate unless party size is taken into account. Party size may influence the angler's ability to catch fish through a variety of processes, including partitioning a limited number of catchable fish among members of a party and party composition. When catch rates are used to estimate total catch rather than to index angler success, party size is not a concern.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Transactions of the American Fisheries Society","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1577/T04-171.1","issn":"00028487","usgsCitation":"Miranda, L., 2005, Catch rates relative to angler party size with implications for monitoring angler success: Transactions of the American Fisheries Society, v. 134, no. 4, p. 1005-1010, https://doi.org/10.1577/T04-171.1.","startPage":"1005","endPage":"1010","numberOfPages":"6","costCenters":[],"links":[{"id":237533,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":210570,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1577/T04-171.1"}],"volume":"134","issue":"4","noUsgsAuthors":false,"publicationDate":"2011-01-09","publicationStatus":"PW","scienceBaseUri":"5059f3cbe4b0c8380cd4b979","contributors":{"authors":[{"text":"Miranda, L.E.","contributorId":58406,"corporation":false,"usgs":true,"family":"Miranda","given":"L.E.","affiliations":[],"preferred":false,"id":423268,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70029522,"text":"70029522 - 2005 - Response of seismicity to Coulomb stress triggers and shadows of the 1999 Mw=7.6 Chi-Chi, Taiwan, earthquake","interactions":[],"lastModifiedDate":"2012-03-12T17:20:52","indexId":"70029522","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2314,"text":"Journal of Geophysical Research B: Solid Earth","active":true,"publicationSubtype":{"id":10}},"title":"Response of seismicity to Coulomb stress triggers and shadows of the 1999 Mw=7.6 Chi-Chi, Taiwan, earthquake","docAbstract":"The correlation between static Coulomb stress increases and aftershocks has thus far provided the strongest evidence that stress changes promote seismicity, a correlation that the Chi-Chi earthquake well exhibits. Several studies have deepened the argument by resolving stress changes on aftershock focal mechanisms, which removes the assumption that the aftershocks are optimally oriented for failure. Here one compares the percentage of planes on which failure is promoted after the main shock relative to the percentage beforehand. For Chi-Chi we find a 28% increase for thrust and an 18% increase for strike-slip mechanisms, commensurate with increases reported for other large main shocks. However, perhaps the chief criticism of static stress triggering is the difficulty in observing predicted seismicity rate decreases in the stress shadows, or sites of Coulomb stress decrease. Detection of sustained drops in seismicity rate demands a long catalog with a low magnitude of completeness and a high seismicity rate, conditions that are met at Chi-Chi. We find four lobes with statistically significant seismicity rate declines of 40-90% for 50 months, and they coincide with the stress shadows calculated for strike-slip faults, the dominant faulting mechanism. The rate drops are evident in uniform cell calculations, 100-month time series, and by visual inspection of the M ??? 3 seismicity. An additional reason why detection of such declines has proven so rare emerges from this study: there is a widespread increase in seismicity rate during the first 3 months after Chi-Chi, and perhaps many other main shocks, that might be associated with a different mechanism. Copyright 2005 by the American Geophysical Union.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Geophysical Research B: Solid Earth","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1029/2004JB003389","issn":"01480227","usgsCitation":"Ma, K., Chan, C., and Stein, R., 2005, Response of seismicity to Coulomb stress triggers and shadows of the 1999 Mw=7.6 Chi-Chi, Taiwan, earthquake: Journal of Geophysical Research B: Solid Earth, v. 110, no. 5, p. 1-16, https://doi.org/10.1029/2004JB003389.","startPage":"1","endPage":"16","numberOfPages":"16","costCenters":[],"links":[{"id":237529,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":210566,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1029/2004JB003389"}],"volume":"110","issue":"5","noUsgsAuthors":false,"publicationDate":"2005-05-28","publicationStatus":"PW","scienceBaseUri":"505aaa67e4b0c8380cd862f0","contributors":{"authors":[{"text":"Ma, K.-F.","contributorId":85371,"corporation":false,"usgs":false,"family":"Ma","given":"K.-F.","email":"","affiliations":[],"preferred":false,"id":423089,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Chan, C.-H.","contributorId":18565,"corporation":false,"usgs":true,"family":"Chan","given":"C.-H.","email":"","affiliations":[],"preferred":false,"id":423088,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stein, R.S.","contributorId":8875,"corporation":false,"usgs":true,"family":"Stein","given":"R.S.","email":"","affiliations":[],"preferred":false,"id":423087,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70029369,"text":"70029369 - 2005 - Evolution of the magmatic-hydrothermal acid-sulfate system at Summitville, Colorado: Integration of geological, stable-isotope, and fluid-inclusion evidence","interactions":[],"lastModifiedDate":"2012-03-12T17:20:52","indexId":"70029369","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1213,"text":"Chemical Geology","active":true,"publicationSubtype":{"id":10}},"title":"Evolution of the magmatic-hydrothermal acid-sulfate system at Summitville, Colorado: Integration of geological, stable-isotope, and fluid-inclusion evidence","docAbstract":"The Summitville Au-Ag-Cu deposit is a classic volcanic dome-hosted high-sulfidation deposit. It occurs in the Quartz Latite of South Mountain, a composite volcanic dome that was emplaced along the coincident margins of the Platoro and Summitville calderas at 22.5??0.5 Ma, penecontemporaneous with alteration and mineralization. A penecontemporaneous quartz monzonite porphyry intrusion underlies the district and is cut and overlain by pyrite-quartz stockwork veins with traces of chalcopyrite and molybdenite. Alteration and mineralization proceeded through three hypogene stages and a supergene stage, punctuated by at least three periods of hydrothermal brecciation. Intense acid leaching along fractures in the quartz latite produced irregular pipes and lenticular pods of vuggy silica enclosed sequentially by alteration zones of quartz-alunite, quartz-kaolinite, and clay. The acid-sulfate-altered rocks host subsequent covellite+enargite/luzonite+chalcopyrite mineralization accompanied by kaolinite, and later barite-base-metal veins, some containing high Au values and kaolinite. The presence of both liquid- and vapor-rich fluid inclusions indicates the episodic presence of a low-density fluid at all levels of the system. In the mineralized zone, liquid-rich fluid inclusions in healed fractures in quartz phenocrysts and in quartz associated with mineralization homogenize to temperatures between 160 and 390 ??C (90% between 190 and 310 ??C), consistent with the range (200-250 ??C) estimated from the fractionation of sulfur isotopes between coexisting alunite and pyrite. A deep alunite-pyrite pair yielded a sulfur-isotope temperature of 390 ??C, marking a transition from hydrostatic to lithostatic pressure at a depth of about 1.5 km. Two salinity populations dominate the liquid-rich fluid inclusions. One has salinities between 0 and 5 wt.% NaCl equivalent; the other has salinities of up to 43 wt.% NaCl equivalent. The occurrence of high-salinity fluid inclusions in vein quartz associated with mineralization, as well as in the deep stockwork veins, suggests that brines originating deep in the system transported the metals. The ??34S values of sulfides in magnetite (-2.3???) and of sulfate in apatite (5.4???) in unaltered quartz latite indicate that ??34S???S was near 0???. The ??34S values of coexisting alteration alunite and pyrite are 18.2??? to 24.5??? and -8.1??? to -2.2???, respectively. Deep in the system, most of the change in ??34S values occurs in the sulfates, indicating that the fluids were initially H2S-dominant, their redox state buffered at depth by equilibration with igneous rocks. However, in the main alteration zone, most of the change in ??34S values occurs in pyrite, indicating that the fluids moved off the rock buffer and became SO42- -dominant as pyrite precipitated and SO2 disproportionation produced the sulfuric acid requisite for acid leaching. The ??34S values of the late-stage barite and sulfides indicate that the system returned to high H2S/SO42- ratios typical of the original rock-buffered fluid. The ??DH2O of alunite parent fluids was near -45??? and their ??18O ranged from 7??? to -1???, depending on the degree of exchange in the alteration zone at low water-rock ratio, or mixing with unexchanged meteoric water. The low ??D values of some alunite samples are interpreted to result from postdepositional exchange with later ore fluids. Fluid exsolved fr om the magma at depth had ??DH2O and ??18OH2O values near -70??? and 10???, respectively. During and following migration to the top of the magma chamber, the fluid underwent isotopic exchange with the partially crystallized magma and its solid and cooler, but still plastic, carapace just below the transition from a lithostatic to hydrostatic pressure regime. These evolved magmatic fluids had ??DH2O and ??18OH2O values close to -40??? and 5???, respectively, prior to release into the superjacent hydrostatically pressured fracture zone, wherein the fluids separat","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Chemical Geology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.chemgeo.2004.06.041","issn":"00092541","usgsCitation":"Bethke, P.M., Rye, R.O., Stoffregen, R., and Vikre, P., 2005, Evolution of the magmatic-hydrothermal acid-sulfate system at Summitville, Colorado: Integration of geological, stable-isotope, and fluid-inclusion evidence: Chemical Geology, v. 215, no. 1-4 SPEC. ISS., p. 281-315, https://doi.org/10.1016/j.chemgeo.2004.06.041.","startPage":"281","endPage":"315","numberOfPages":"35","costCenters":[],"links":[{"id":210454,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.chemgeo.2004.06.041"},{"id":237375,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"215","issue":"1-4 SPEC. ISS.","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0d8ce4b0c8380cd5309f","contributors":{"authors":[{"text":"Bethke, P. M.","contributorId":32921,"corporation":false,"usgs":true,"family":"Bethke","given":"P.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":422441,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rye, R. O.","contributorId":66208,"corporation":false,"usgs":true,"family":"Rye","given":"R.","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":422442,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stoffregen, R.E.","contributorId":70417,"corporation":false,"usgs":true,"family":"Stoffregen","given":"R.E.","affiliations":[],"preferred":false,"id":422443,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Vikre, P.G.","contributorId":76930,"corporation":false,"usgs":true,"family":"Vikre","given":"P.G.","affiliations":[],"preferred":false,"id":422444,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70029345,"text":"70029345 - 2005 - Cambro-ordovician sea-level fluctuations and sequence boundaries: The missing record and the evolution of new taxa","interactions":[],"lastModifiedDate":"2012-03-12T17:20:50","indexId":"70029345","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3460,"text":"Special Papers in Palaeontology","active":true,"publicationSubtype":{"id":10}},"title":"Cambro-ordovician sea-level fluctuations and sequence boundaries: The missing record and the evolution of new taxa","docAbstract":"The evolution of early Palaeozoic conodont faunas shows a clear connection to sea-level changes. One way that this connection manifests itself is that thick successions of carbonates are missing beneath major sequence boundaries due to karstification and erosion. From this observation arises the question of how many taxa have been lost from different conodont lineages in these incomplete successions. Although many taxa suffered extinction due to the environmental stresses associated with falling sea-levels, some must have survived in these extreme conditions. The number of taxa missing in the early Palaeozoic tropics always will be unclear, but it will be even more difficult to evaluate the missing record in detrital successions of higher latitudes. A common pattern in the evolution of Cambrian-Ordovician conodont lineages is appearances of new species at sea-level rises and disappearances at sea-level drops. This simple picture can be complicated by intervals that consistently have no representatives of a particular lineage, even after extensive sampling of the most complete sections. Presumably the lineages survived in undocumented refugia. In this paper, we give examples of evolution in Cambrian-Ordovician shallowmarine conodont faunas and highlight problems of undiscovered or truly missing segments of lineages. ?? The Palaeontological Association.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Special Papers in Palaeontology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"00386804","usgsCitation":"Lehnert, O., Miller, J., Leslie, S.A., Repetski, J., and Ethington, R.L., 2005, Cambro-ordovician sea-level fluctuations and sequence boundaries: The missing record and the evolution of new taxa: Special Papers in Palaeontology, no. 73, p. 117-134.","startPage":"117","endPage":"134","numberOfPages":"18","costCenters":[],"links":[{"id":237595,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"issue":"73","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f32de4b0c8380cd4b642","contributors":{"authors":[{"text":"Lehnert, O.","contributorId":39143,"corporation":false,"usgs":true,"family":"Lehnert","given":"O.","email":"","affiliations":[],"preferred":false,"id":422352,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miller, J.F.","contributorId":29830,"corporation":false,"usgs":true,"family":"Miller","given":"J.F.","email":"","affiliations":[],"preferred":false,"id":422350,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Leslie, Stephen A.","contributorId":25750,"corporation":false,"usgs":false,"family":"Leslie","given":"Stephen","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":422349,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Repetski, J.E.","contributorId":38579,"corporation":false,"usgs":true,"family":"Repetski","given":"J.E.","affiliations":[],"preferred":false,"id":422351,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Ethington, Raymond L.","contributorId":93507,"corporation":false,"usgs":false,"family":"Ethington","given":"Raymond","email":"","middleInitial":"L.","affiliations":[{"id":6754,"text":"University of Missouri","active":true,"usgs":false}],"preferred":false,"id":422353,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70029333,"text":"70029333 - 2005 - Hydrologic regime controls soil phosphorus fluxes in restoration and undisturbed wetlands","interactions":[],"lastModifiedDate":"2012-03-12T17:20:51","indexId":"70029333","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3271,"text":"Restoration Ecology","active":true,"publicationSubtype":{"id":10}},"title":"Hydrologic regime controls soil phosphorus fluxes in restoration and undisturbed wetlands","docAbstract":"Many wetland restoration projects occur on former agricultural soils that have a history of disturbance and fertilization, making them prone to phosphorus (P) release upon flooding. To study the relationship between P release and hydrologic regime, we collected soil cores from three restoration wetlands and three undisturbed wetlands around Upper Klamath Lake in southern Oregon, U.S.A. Soil cores were subjected to one of three hydrologic regimes - flooded, moist, and dry - for 7.5 weeks, and P fluxes were measured upon reflooding. Soils from restoration wetlands released P upon reflooding regardless of the hydrologic regime, with the greatest releases coming from soils that had been flooded or dried. Undisturbed wetland soils released P only after drying. Patterns in P release can be explained by a combination of physical and biological processes, including the release of iron-bound P due to anoxia in the flooded treatment and the mineralization of organic P under aerobic conditions in the dry treatment. Higher rates of soil P release from restoration wetland soils, particularly under flooded conditions, were associated with higher total P concentrations compared with undisturbed wetland soils. We conclude that maintaining moist soil is the means to minimize P release from recently flooded wetland soils. Alternatively, prolonged flooding provides a means of liberating excess labile P from former agricultural soils while minimizing continued organic P mineralization and soil subsidence. ?? 2005 Society for Ecological Restoration International.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Restoration Ecology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1111/j.1526-100X.2005.00043.x","issn":"10612971","usgsCitation":"Aldous, A., McCormick, P., Ferguson, C., Graham, S., and Craft, C., 2005, Hydrologic regime controls soil phosphorus fluxes in restoration and undisturbed wetlands: Restoration Ecology, v. 13, no. 2, p. 341-347, https://doi.org/10.1111/j.1526-100X.2005.00043.x.","startPage":"341","endPage":"347","numberOfPages":"7","costCenters":[],"links":[{"id":477899,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1111/j.1526-100x.2005.00043.x","text":"Publisher Index Page"},{"id":237443,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":210505,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1111/j.1526-100X.2005.00043.x"}],"volume":"13","issue":"2","noUsgsAuthors":false,"publicationDate":"2005-05-24","publicationStatus":"PW","scienceBaseUri":"505a367fe4b0c8380cd6076d","contributors":{"authors":[{"text":"Aldous, A.","contributorId":105517,"corporation":false,"usgs":true,"family":"Aldous","given":"A.","email":"","affiliations":[],"preferred":false,"id":422307,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McCormick, P.","contributorId":30022,"corporation":false,"usgs":true,"family":"McCormick","given":"P.","email":"","affiliations":[],"preferred":false,"id":422304,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ferguson, C.","contributorId":18960,"corporation":false,"usgs":true,"family":"Ferguson","given":"C.","email":"","affiliations":[],"preferred":false,"id":422303,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Graham, S.","contributorId":70988,"corporation":false,"usgs":true,"family":"Graham","given":"S.","affiliations":[],"preferred":false,"id":422306,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Craft, C.","contributorId":67712,"corporation":false,"usgs":true,"family":"Craft","given":"C.","email":"","affiliations":[],"preferred":false,"id":422305,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70029316,"text":"70029316 - 2005 - Temporal variations and scaling of streamflow and baseflow and their nitrate-nitrogen concentrations and loads","interactions":[],"lastModifiedDate":"2012-03-12T17:20:55","indexId":"70029316","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":664,"text":"Advances in Water Resources","active":true,"publicationSubtype":{"id":10}},"title":"Temporal variations and scaling of streamflow and baseflow and their nitrate-nitrogen concentrations and loads","docAbstract":"The patterns of temporal variations of precipitation (P), streamflow (SF) and baseflow (BF) as well as their nitrate-nitrogen (nitrate) concentrations (C) and loads (L) from a long-term record (28 years) in the Raccoon River, Iowa, were analyzed using variogram and spectral analyses. The daily P is random but scaling may exist in the daily SF and BF with a possible break point in the scaling at about 18 days and 45 days, respectively. The nitrate concentrations and loads are shown to have a half-year cycle while daily P, SF, and BF have a one-year cycle. Furthermore, there may be a low-frequency cycle of 6-8 years in C. The power spectra of C and L in both SF and BF exhibit fractal 1/f scaling with two characteristic frequencies of half-year and one-year, and are fitted well with the spectrum of the gamma distribution. The nitrate input to SF and BF at the Raccoon watershed seems likely to be a white noise process superimposed on another process with a half-year and one-year cycle. ?? 2005 Elsevier Ltd. All rights reserved.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Advances in Water Resources","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.advwatres.2004.12.014","issn":"03091708","usgsCitation":"Zhang, Y., and Schilling, K., 2005, Temporal variations and scaling of streamflow and baseflow and their nitrate-nitrogen concentrations and loads: Advances in Water Resources, v. 28, no. 7, p. 701-710, https://doi.org/10.1016/j.advwatres.2004.12.014.","startPage":"701","endPage":"710","numberOfPages":"10","costCenters":[],"links":[{"id":210724,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.advwatres.2004.12.014"},{"id":237737,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"28","issue":"7","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505ba52ae4b08c986b32086c","contributors":{"authors":[{"text":"Zhang, Y.-K.","contributorId":44309,"corporation":false,"usgs":true,"family":"Zhang","given":"Y.-K.","email":"","affiliations":[],"preferred":false,"id":422236,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schilling, K.","contributorId":101423,"corporation":false,"usgs":true,"family":"Schilling","given":"K.","affiliations":[],"preferred":false,"id":422237,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70029252,"text":"70029252 - 2005 - Seasonal to interannual morphodynamics along a high-energy dissipative littoral cell","interactions":[],"lastModifiedDate":"2012-03-12T17:20:49","indexId":"70029252","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2220,"text":"Journal of Coastal Research","active":true,"publicationSubtype":{"id":10}},"title":"Seasonal to interannual morphodynamics along a high-energy dissipative littoral cell","docAbstract":"A beach morphology monitoring program was initiated during summer 1997 along the Columbia River littoral cell (CRLC) on the coasts of northwest Oregon and southwest Washington, USA. This field program documents the seasonal through interannual morphological variability of these high-energy dissipative beaches over a variety of spatial scales. Following the installation of a dense network of geodetic control monuments, a nested sampling scheme consisting of cross-shore topographic beach profiles, three-dimensional topographic beach surface maps, nearshore bathymetric surveys, and sediment size distribution analyses was initiated. Beach monitoring is being conducted with state-of-the-art real-time kinematic differential global positioning system survey methods that combine both high accuracy and speed of measurement. Sampling methods resolve variability in beach morphology at alongshore length scales of approximately 10 meters to approximately 100 kilometers and cross-shore length scales of approximately 1 meter to approximately 2 kilometers. During the winter of 1997/1998, coastal change in the US Pacific Northwest was greatly influenced by one of the strongest El Nin??o events on record. Steeper than typical southerly wave angles resulted in alongshore sediment transport gradients and shoreline reorientation on a regional scale. The La Nin??a of 1998/1999, dominated by cross-shore processes associated with the largest recorded wave year in the region, resulted in net beach erosion along much of the littoral cell. The monitoring program successfully documented the morphological response to these interannual forcing anomalies as well as the subsequent beach recovery associated with three consecutive moderate wave years. These morphological observations within the CRLC can be generalized to explain overall system patterns; however, distinct differences in large-scale coastal behavior (e.g., foredune ridge morphology, sandbar morphometrics, and nearshore beach slopes) are not readily explained or understood.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Coastal Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.2112/03-0029.1","issn":"07490208","usgsCitation":"Ruggiero, P., Kaminsky, G.M., Gelfenbaum, G., and Voigt, B., 2005, Seasonal to interannual morphodynamics along a high-energy dissipative littoral cell: Journal of Coastal Research, v. 21, no. 3, p. 553-578, https://doi.org/10.2112/03-0029.1.","startPage":"553","endPage":"578","numberOfPages":"26","costCenters":[],"links":[{"id":210808,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.2112/03-0029.1"},{"id":237837,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"21","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b88dfe4b08c986b316bf4","contributors":{"authors":[{"text":"Ruggiero, P.","contributorId":25995,"corporation":false,"usgs":true,"family":"Ruggiero","given":"P.","affiliations":[],"preferred":false,"id":421927,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kaminsky, G. M.","contributorId":50586,"corporation":false,"usgs":true,"family":"Kaminsky","given":"G.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":421928,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gelfenbaum, G.","contributorId":72429,"corporation":false,"usgs":true,"family":"Gelfenbaum","given":"G.","email":"","affiliations":[],"preferred":false,"id":421929,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Voigt, B.","contributorId":21755,"corporation":false,"usgs":true,"family":"Voigt","given":"B.","email":"","affiliations":[],"preferred":false,"id":421926,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70029248,"text":"70029248 - 2005 - Investigating surface water-well interaction using stable isotope ratios of water","interactions":[],"lastModifiedDate":"2018-11-05T08:57:10","indexId":"70029248","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2342,"text":"Journal of Hydrology","active":true,"publicationSubtype":{"id":10}},"title":"Investigating surface water-well interaction using stable isotope ratios of water","docAbstract":"<p><span>Because surface water can be a source of undesirable water quality in a drinking&nbsp;<a title=\"Learn more about water well\" href=\"https://www.sciencedirect.com/topics/earth-and-planetary-sciences/water-well\" data-mce-href=\"https://www.sciencedirect.com/topics/earth-and-planetary-sciences/water-well\">water well</a>, an understanding of the amount of surface water and its travel time to the well is needed to assess a well's vulnerability. Stable&nbsp;<a title=\"Learn more about isotope ratios\" href=\"https://www.sciencedirect.com/topics/earth-and-planetary-sciences/isotope-ratios\" data-mce-href=\"https://www.sciencedirect.com/topics/earth-and-planetary-sciences/isotope-ratios\">isotope ratios</a>&nbsp;of oxygen in&nbsp;<a title=\"Learn more about river water\" href=\"https://www.sciencedirect.com/topics/earth-and-planetary-sciences/river-water\" data-mce-href=\"https://www.sciencedirect.com/topics/earth-and-planetary-sciences/river-water\">river water</a>&nbsp;at the City of La Crosse, Wisconsin, show peak-to-peak&nbsp;<a title=\"Learn more about seasonal variation\" href=\"https://www.sciencedirect.com/topics/earth-and-planetary-sciences/seasonal-variation\" data-mce-href=\"https://www.sciencedirect.com/topics/earth-and-planetary-sciences/seasonal-variation\">seasonal variation</a>&nbsp;greater than 4‰ in 2001 and 2002. This seasonal signal was identified in 7 of 13 city municipal wells, indicating that these 7 wells have appreciable surface water contributions and are potentially vulnerable to contaminants in the surface water. When looking at wells with more than 6 sampling events, a larger variation in&nbsp;</span><i>δ</i><sup>18</sup><span>O compositions correlated with a larger fraction of surface water, suggesting that samples collected for oxygen&nbsp;<a title=\"Learn more about isotopic composition\" href=\"https://www.sciencedirect.com/topics/earth-and-planetary-sciences/isotopic-composition\" data-mce-href=\"https://www.sciencedirect.com/topics/earth-and-planetary-sciences/isotopic-composition\">isotopic composition</a>&nbsp;over time may be useful for identifying the vulnerability to surface water influence even if a local&nbsp;<a title=\"Learn more about meteoric water\" href=\"https://www.sciencedirect.com/topics/earth-and-planetary-sciences/meteoric-water\" data-mce-href=\"https://www.sciencedirect.com/topics/earth-and-planetary-sciences/meteoric-water\">meteoric water</a>&nbsp;line is not available.</span></p><p>A time series of<span>&nbsp;</span><i>δ</i><sup>18</sup><span>O from one of the municipal wells and from a&nbsp;piezometerlocated between the river and the municipal well showed that the travel time of flood water to the municipal well was approximately 2 months; non-flood arrival times were on the order of 9 months. Four independent methods were also used to assess time of travel. Three methods (groundwater temperature arrival times at the intermediate piezometer, virus-culture results, and&nbsp;particle tracking&nbsp;using a numerical&nbsp;groundwater-flow&nbsp;model) yielded flood and non-flood travel times of less than 1 year for this site.&nbsp;Age dating&nbsp;of one groundwater sample using&nbsp;</span><sup>3</sup>H–<sup>3</sup>He methods estimated an age longer than 1 year, but was likely confounded by deviations from piston flow as noted by others. Chlorofluorocarbons and SF<sub>6</sub><span>analyses were not useful at this site due to degradation and contamination, respectively. This work illustrates the utility of stable hydrogen and&nbsp;oxygen isotope ratios&nbsp;of water to determine the contribution and travel time of surface water in groundwater, and demonstrates the importance of using multiple methods to improve estimates for time of travel of 1 year or less.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.jhydrol.2004.07.010","issn":"00221694","usgsCitation":"Hunt, R.J., Coplen, T., Haas, N., Saad, D.A., and Borchardt, M., 2005, Investigating surface water-well interaction using stable isotope ratios of water: Journal of Hydrology, v. 302, no. 1-4, p. 154-172, https://doi.org/10.1016/j.jhydrol.2004.07.010.","productDescription":"19 p.","startPage":"154","endPage":"172","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":237765,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":210748,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.jhydrol.2004.07.010"}],"volume":"302","issue":"1-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3e6ee4b0c8380cd63d99","contributors":{"authors":[{"text":"Hunt, R. J.","contributorId":40164,"corporation":false,"usgs":true,"family":"Hunt","given":"R.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":421909,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Coplen, T.B.","contributorId":34147,"corporation":false,"usgs":true,"family":"Coplen","given":"T.B.","affiliations":[],"preferred":false,"id":421908,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Haas, N.L.","contributorId":33496,"corporation":false,"usgs":true,"family":"Haas","given":"N.L.","email":"","affiliations":[],"preferred":false,"id":421907,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Saad, D. A.","contributorId":85212,"corporation":false,"usgs":true,"family":"Saad","given":"D.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":421911,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Borchardt, M. A.","contributorId":62804,"corporation":false,"usgs":true,"family":"Borchardt","given":"M. A.","affiliations":[],"preferred":false,"id":421910,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70029244,"text":"70029244 - 2005 - Survival of captive-reared Puerto Rican Parrots released in the Caribbean National Forest","interactions":[],"lastModifiedDate":"2022-06-07T15:13:30.947557","indexId":"70029244","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1318,"text":"Condor","active":true,"publicationSubtype":{"id":10}},"title":"Survival of captive-reared Puerto Rican Parrots released in the Caribbean National Forest","docAbstract":"<p><span>We report first-year survival for 34 captive-reared Puerto Rican Parrots (</span><i>Amazona vittata</i><span>) released in the Caribbean National Forest, Puerto Rico between 2000 and 2002. The purpose of the releases were to increase population size and the potential number of breeding individuals of the sole extant wild population, and to refine release protocols for eventual reintroduction of a second wild population elsewhere on the island. After extensive prerelease training, we released 10 parrots in 2000, 16 parrots in 2001, and eight parrots in 2002 ranging in age from 1–4 years old. All birds were equipped with radio-transmitters to monitor survival. The overall first-year survival estimate for the 34 parrots was 41% (CI = 22%–61%). Only one parrot died within the first week postrelease, with most (94%) surviving for at least eight weeks after release. Most (54%) documented mortalities were due to raptor predation, which claimed 21% of all released parrots. A captive-reared bird (male, age one), released in 2001, paired with a wild female and fledged two young in 2004. We also calculated survival based on 0% and 50% of observed predation losses and found hypothetical survival rates of 72% and 54%, respectively. Rigorous prerelease training and acclimation was believed to have improved initial postrelease parrot survival, and releasing mixed age-class groups suggests the potential for shortening the time to recruitment.</span></p>","language":"English","publisher":"Oxford Academic","doi":"10.1093/condor/107.2.424","usgsCitation":"White, T.H., Collazo, J.A., and Vilella, F., 2005, Survival of captive-reared Puerto Rican Parrots released in the Caribbean National Forest: Condor, v. 107, no. 2, p. 424-432, https://doi.org/10.1093/condor/107.2.424.","productDescription":"9 p.","startPage":"424","endPage":"432","numberOfPages":"9","costCenters":[{"id":200,"text":"Coop Res Unit Seattle","active":true,"usgs":true}],"links":[{"id":488182,"rank":1,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1093/condor/107.2.424","text":"Publisher Index Page"},{"id":237694,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Puerto Rico","otherGeospatial":"Caribbean National Forest","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -65.85823059082031,\n              18.254132567888902\n            ],\n            [\n              -65.80673217773438,\n              18.25021997706561\n            ],\n            [\n              -65.731201171875,\n              18.2515241837971\n            ],\n            [\n              -65.70236206054688,\n              18.317373879896916\n            ],\n            [\n              -65.77995300292969,\n              18.352570378258942\n            ],\n            [\n              -65.830078125,\n              18.34540130240112\n            ],\n            [\n              -65.8575439453125,\n              18.291949733550336\n            ],\n            [\n              -65.85823059082031,\n              18.254132567888902\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"107","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505ba2cae4b08c986b31f974","contributors":{"authors":[{"text":"White, Thomas H. Jr.","contributorId":201474,"corporation":false,"usgs":false,"family":"White","given":"Thomas","suffix":"Jr.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":421899,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Collazo, Jaime A. 0000-0002-1816-7744","orcid":"https://orcid.org/0000-0002-1816-7744","contributorId":217287,"corporation":false,"usgs":true,"family":"Collazo","given":"Jaime","email":"","middleInitial":"A.","affiliations":[{"id":198,"text":"Coop Res Unit Atlanta","active":true,"usgs":true}],"preferred":true,"id":421898,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Vilella, Francisco 0000-0003-1552-9989 fvilella@usgs.gov","orcid":"https://orcid.org/0000-0003-1552-9989","contributorId":171363,"corporation":false,"usgs":true,"family":"Vilella","given":"Francisco","email":"fvilella@usgs.gov","affiliations":[{"id":198,"text":"Coop Res Unit Atlanta","active":true,"usgs":true}],"preferred":true,"id":421900,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70029221,"text":"70029221 - 2005 - Upstream migration of Pacific lampreys in the John Day River, Oregon: Behavior, timing, and habitat use","interactions":[],"lastModifiedDate":"2016-05-12T15:10:28","indexId":"70029221","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2900,"text":"Northwest Science","onlineIssn":"2161-9859","printIssn":"0029-344X","active":true,"publicationSubtype":{"id":10}},"title":"Upstream migration of Pacific lampreys in the John Day River, Oregon: Behavior, timing, and habitat use","docAbstract":"<p>Adult Pacific lamprey migration and habitat preferences for over-winter holding and spawning, and larval rearing in tributaries to the Columbia River are not well understood. The John Day River is one such tributary where larval and adult stages of this species have been documented, and its free-flowing character provided the opportunity to study migration of Pacific lampreys unimpeded by passage constraints. Forty-two adult Pacific lampreys were captured in the John Day River near its mouth during their upstream migration. Pacific lampreys were surgically implanted with radio transmitters and released onsite, and tracked by fixed-site, aerial, and terrestrial telemetry methods for nearly one year. Adults moved upstream exclusively at night, with a mean rate of 11.1 ?? 6.3 km/day. They halted upstream migration by September, and held a single position for approximately six months in the lateral margins of riffles and glides, using boulders for cover. More than half of Pacific lampreys resumed migration in March before ending movement in early May. Pacific lampreys that resumed migration in spring completed a median of 87% of their upstream migration before over-winter holding. Upon completing migration. Pacific lampreys briefly held position before beginning downstream movement at the end of May. Though not directly observed, halting migration and movement downstream were likely the result of spawning and death. Gains in adult Pacific lamprey passage through the Columbia River hydrosystem and tributaries may be made by improvements that would expedite migration during spring and summer and increase the quantity and variety of cover and refuge opportunities. ?? 2005 by the Northwest Scientific Association. All rights reserved.</p>","language":"English","issn":"0029344X","usgsCitation":"Robinson, T.C., and Bayer, J., 2005, Upstream migration of Pacific lampreys in the John Day River, Oregon: Behavior, timing, and habitat use: Northwest Science, v. 79, no. 2-3, p. 106-119.","productDescription":"14 p.","startPage":"106","endPage":"119","numberOfPages":"14","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":237365,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Oregon","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -120.69305419921874,\n              45.69275137290873\n            ],\n            [\n              -120.67657470703124,\n              45.515970517182474\n            ],\n            [\n              -120.68206787109375,\n              45.10454630976873\n            ],\n            [\n              -120.51177978515625,\n              44.735027899515465\n            ],\n            [\n              -119.79217529296876,\n              44.623708968901205\n            ],\n            [\n              -119.55047607421875,\n              44.482789890501586\n            ],\n            [\n              -118.927001953125,\n              44.37098696297173\n            ],\n            [\n              -118.62213134765626,\n              45.08321794926837\n            ],\n            [\n              -118.71551513671876,\n              45.29421101337773\n            ],\n            [\n              -119.56146240234375,\n              45.160737441973495\n            ],\n            [\n              -119.90203857421875,\n              44.96285457777543\n            ],\n            [\n              -120.19317626953124,\n              44.824708282300236\n            ],\n            [\n              -120.311279296875,\n              44.96479793033104\n            ],\n            [\n              -120.2947998046875,\n              45.52751668442124\n            ],\n            [\n              -120.58593749999999,\n              45.73685954736049\n            ],\n            [\n              -120.69305419921874,\n              45.69275137290873\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"79","issue":"2-3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bbd6fe4b08c986b329012","contributors":{"authors":[{"text":"Robinson, T. Craig","contributorId":93266,"corporation":false,"usgs":true,"family":"Robinson","given":"T.","email":"","middleInitial":"Craig","affiliations":[],"preferred":false,"id":421811,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bayer, J.M.","contributorId":47945,"corporation":false,"usgs":true,"family":"Bayer","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":421810,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70029170,"text":"70029170 - 2005 - Mineralogical and geochemical consequences of the long-term presence of CO2 in natural reservoirs: An example from the Springerville-St. Johns Field, Arizona, and New Mexico, U.S.A","interactions":[],"lastModifiedDate":"2012-03-12T17:20:54","indexId":"70029170","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1213,"text":"Chemical Geology","active":true,"publicationSubtype":{"id":10}},"title":"Mineralogical and geochemical consequences of the long-term presence of CO2 in natural reservoirs: An example from the Springerville-St. Johns Field, Arizona, and New Mexico, U.S.A","docAbstract":"The Springerville-St. Johns CO2 field in eastern Arizona and western New Mexico is one of more than a dozen gas fields developed within the Colorado Plateau and Southern Rocky Mountain region. Extensive travertine (CaCO3) deposits record a long history of CO2 migration and leakage to the atmosphere. The oldest travertine deposits may have formed during the initial filling of the CO2 reservoir when groundwaters exsolved CO2 upon reaching the surface. The youngest travertine deposits are associated with springs on the floor of the Little Colorado River valley, but travertine deposition appears to be insignificant today. Older deposits occur up to 325 m above the valley floor. Geologic relationships suggest travertine deposition began in the late Pleistocene after volcanic activity ended at ???0.3 Ma. Most of the CaCO3 could have been derived from dissolution of the underlying limestones and dolomites. Interactions between the reservoir fluids and rocks were observed in core samples from one of the intervals that produced dry gas. These reactions resulted in the dissolution of carbonate cements and detrital feldspars and the formation of dawsonite and kaolinite. Geochemical simulations suggest that the dawsonite could have been deposited when the CO2 fugacity reached 20 bars and that the kaolinite formed as the CO2 fugacity decreased. Corrosion of drill pipe by acidic waters and a pronounced HCO3 anomaly above the CO2 reservoir provide evidence of a continuing flux of CO2 from depth. CO2 storage occurs primarily as dissolved carbonate species and as gas accumulations. Only a small percentage of the CO2 was sequestered in secondary minerals. ?? 2005 Elsevier B.V. All rights reserved.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Chemical Geology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.chemgeo.2004.12.019","issn":"00092541","usgsCitation":"Moore, J., Adams, M., Allis, R., Lutz, S., and Rauzi, S., 2005, Mineralogical and geochemical consequences of the long-term presence of CO2 in natural reservoirs: An example from the Springerville-St. Johns Field, Arizona, and New Mexico, U.S.A: Chemical Geology, v. 217, no. 3-4 SPEC. ISS., p. 365-385, https://doi.org/10.1016/j.chemgeo.2004.12.019.","startPage":"365","endPage":"385","numberOfPages":"21","costCenters":[],"links":[{"id":210693,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.chemgeo.2004.12.019"},{"id":237690,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"217","issue":"3-4 SPEC. ISS.","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a5a92e4b0c8380cd6ef91","contributors":{"authors":[{"text":"Moore, Jeff","contributorId":49059,"corporation":false,"usgs":true,"family":"Moore","given":"Jeff","email":"","affiliations":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"preferred":false,"id":421611,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Adams, M.","contributorId":81176,"corporation":false,"usgs":true,"family":"Adams","given":"M.","email":"","affiliations":[],"preferred":false,"id":421613,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Allis, R.","contributorId":14606,"corporation":false,"usgs":true,"family":"Allis","given":"R.","affiliations":[],"preferred":false,"id":421609,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lutz, S.","contributorId":40005,"corporation":false,"usgs":true,"family":"Lutz","given":"S.","email":"","affiliations":[],"preferred":false,"id":421610,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Rauzi, S.","contributorId":70179,"corporation":false,"usgs":true,"family":"Rauzi","given":"S.","affiliations":[],"preferred":false,"id":421612,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70029138,"text":"70029138 - 2005 - TREMOR: A wireless MEMS accelerograph for dense arrays","interactions":[],"lastModifiedDate":"2012-03-12T17:20:48","indexId":"70029138","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1436,"text":"Earthquake Spectra","active":true,"publicationSubtype":{"id":10}},"title":"TREMOR: A wireless MEMS accelerograph for dense arrays","docAbstract":"The ability of a strong-motion network to resolve wavefields can be described on three axes: frequency, amplitude, and space. While the need for spatial resolution is apparent, for practical reasons that axis is often neglected. TREMOR is a MEMS-based accelerograph using wireless Internet to minimize lifecycle cost. TREMOR instruments can economically augment traditional ones, residing between them to improve spatial resolution. The TREMOR instrument described here has dynamic range of 96 dB between ??2 g, or 102 dB between ??4 g. It is linear to ???1% of full scale (FS), with a response function effectively shaped electronically. We developed an economical, very low noise, accurate (???1%FS) temperature compensation method. Displacement is easily recovered to 10-cm accuracy at full bandwidth, and better with care. We deployed prototype instruments in Oakland, California, beginning in 1998, with 13 now at mean spacing of ???3 km - one of the most densely instrumented urban centers in the United States. This array is among the quickest in returning (PGA, PGV, Sa) vectors to ShakeMap, ???75 to 100 s. Some 13 events have been recorded. A ShakeMap and an example of spatial variability are shown. Extensive tests of the prototypes for a commercial instrument are described here and in a companion paper. ?? 2005, Earthquake Engineering Research Institute.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Earthquake Spectra","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1193/1.1856534","issn":"87552930","usgsCitation":"Evans, J., Hamstra, R., Kundig, C., Camina, P., and Rogers, J.A., 2005, TREMOR: A wireless MEMS accelerograph for dense arrays: Earthquake Spectra, v. 21, no. 1, p. 91-124, https://doi.org/10.1193/1.1856534.","startPage":"91","endPage":"124","numberOfPages":"34","costCenters":[],"links":[{"id":210804,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1193/1.1856534"},{"id":237830,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"21","issue":"1","noUsgsAuthors":false,"publicationDate":"2005-02-01","publicationStatus":"PW","scienceBaseUri":"505ba392e4b08c986b31fd75","contributors":{"authors":[{"text":"Evans, J.R.","contributorId":50526,"corporation":false,"usgs":true,"family":"Evans","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":421483,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hamstra, R.H. Jr.","contributorId":6246,"corporation":false,"usgs":true,"family":"Hamstra","given":"R.H.","suffix":"Jr.","affiliations":[],"preferred":false,"id":421480,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kundig, C.","contributorId":37948,"corporation":false,"usgs":true,"family":"Kundig","given":"C.","affiliations":[],"preferred":false,"id":421481,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Camina, P.","contributorId":46755,"corporation":false,"usgs":true,"family":"Camina","given":"P.","affiliations":[],"preferred":false,"id":421482,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Rogers, J. A.","contributorId":90721,"corporation":false,"usgs":true,"family":"Rogers","given":"J.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":421484,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70029082,"text":"70029082 - 2005 - Invertebrate eggs can fly: Evidence of waterfowl-mediated gene flow in aquatic invertebrates","interactions":[],"lastModifiedDate":"2012-03-12T17:20:53","indexId":"70029082","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":740,"text":"American Naturalist","active":true,"publicationSubtype":{"id":10}},"title":"Invertebrate eggs can fly: Evidence of waterfowl-mediated gene flow in aquatic invertebrates","docAbstract":"Waterfowl often have been assumed to disperse freshwater aquatic organisms between isolated wetlands, but no one has analyzed the impact of this transport on the population structure of aquatic organisms. For three cladocerans (Daphnia ambigua, Daphnia laevis, and Sida crystallina) and one bryozoan (Cristatella mucedo), we estimated the genetic distances between populations across North America using sequences of several mitochondrial DNA genes and genotypic frequencies at allozyme and microsatellite loci. Waterfowl movements across North America (estimated from band recovery data) explained a significant proportion of the gene flow occurring between populations across the continent for three of the four species, even after controlling for geographic distances between localities. The fourth species, S. crystallina, has propagules less likely to survive desiccation or ingestion by birds. Differences in the capacity to exploit bird-mediated transport are likely to have important consequences for the ecology of aquatic communities and the spread of invasive species.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"American Naturalist","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1086/427092","issn":"00030147","usgsCitation":"Figuerola, J., Green, A., and Michot, T., 2005, Invertebrate eggs can fly: Evidence of waterfowl-mediated gene flow in aquatic invertebrates: American Naturalist, v. 165, no. 2, p. 274-280, https://doi.org/10.1086/427092.","startPage":"274","endPage":"280","numberOfPages":"7","costCenters":[],"links":[{"id":477798,"rank":10000,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"http://hdl.handle.net/10261/40921","text":"External Repository"},{"id":210519,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1086/427092"},{"id":237462,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"165","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3e5ee4b0c8380cd63d06","contributors":{"authors":[{"text":"Figuerola, J.","contributorId":65277,"corporation":false,"usgs":true,"family":"Figuerola","given":"J.","email":"","affiliations":[],"preferred":false,"id":421267,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Green, A.J.","contributorId":51529,"corporation":false,"usgs":true,"family":"Green","given":"A.J.","email":"","affiliations":[],"preferred":false,"id":421266,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Michot, T.C. 0000-0002-7044-987X","orcid":"https://orcid.org/0000-0002-7044-987X","contributorId":43426,"corporation":false,"usgs":true,"family":"Michot","given":"T.C.","affiliations":[],"preferred":false,"id":421265,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70029081,"text":"70029081 - 2005 - The role of shoreland development and commercial cranberry farming in a lake in Wisconsin, USA","interactions":[],"lastModifiedDate":"2012-03-12T17:20:54","indexId":"70029081","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2411,"text":"Journal of Paleolimnology","active":true,"publicationSubtype":{"id":10}},"title":"The role of shoreland development and commercial cranberry farming in a lake in Wisconsin, USA","docAbstract":"Musky Bay in Lac Courte Oreilles, Wisconsin, USA, is currently eutrophic. This large, shallow bay of an oligotrophic lake possesses the densest aquatic plant growth and a floating algal mat. Paleoecological reconstructions encompassing the last 130 years, were based on multiproxy analyses of sediment cores from three coring sites, two within the bay and one in the lake itself. These data were compared to historical records of the construction and expansion of two commercial cranberry bogs and shoreline residential homes to identify temporal and causal relations of eutrophication. The proxies investigated included: minor and trace elements; biogenic silica; and the diatom community. Post-depositional diagenesis of organic carbon, nitrogen, and phosphorus in the upper 30 cm of the core obscured records of historical ambient nutrient concentrations in the bay obviating their usefulness for this purpose. In contrast, calcium, magnesium, and potassium concentration profiles appeared to reflect runoff of soil amendments applied to the cranberry bogs and aerial fertilizer spraying over the eastern bog adjacent to Musky Bay. The increase in aluminum content since about 1930 coincided with the historical trend in shoreland development and construction of the original commercial cranberry farm. The biogenic silica profile recorded a steady increase of nutrients to Musky Bay over the last several decades. Stratigraphic changes in the diatom community indicated that nutrient input began to increase in the 1940s and accelerated in the mid-1990s with the onset of a noxious floating algal mat. The diatom community indicates the bay has possessed a significant macrophyte community for at least the last 200 years, but increased nutrient input was manifested by a change in the composition, and an increase in the density of the epiphytic diatom community. Cranberry farming appeared to be the major source of nutrients because the diatom community changes occurred prior to the significant increase in residential housing.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Paleolimnology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1007/s10933-004-3990-4","issn":"09212728","usgsCitation":"Garrison, P., and Fitzgerald, S., 2005, The role of shoreland development and commercial cranberry farming in a lake in Wisconsin, USA: Journal of Paleolimnology, v. 33, no. 2, p. 169-188, https://doi.org/10.1007/s10933-004-3990-4.","startPage":"169","endPage":"188","numberOfPages":"20","costCenters":[],"links":[{"id":210493,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/s10933-004-3990-4"},{"id":237429,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"33","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505baf97e4b08c986b3248e8","contributors":{"authors":[{"text":"Garrison, P.J.","contributorId":86072,"corporation":false,"usgs":true,"family":"Garrison","given":"P.J.","email":"","affiliations":[],"preferred":false,"id":421263,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fitzgerald, S.A.","contributorId":94348,"corporation":false,"usgs":true,"family":"Fitzgerald","given":"S.A.","email":"","affiliations":[],"preferred":false,"id":421264,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70029079,"text":"70029079 - 2005 - Three decades of Martian surface changes","interactions":[],"lastModifiedDate":"2012-03-12T17:20:54","indexId":"70029079","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","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":"Three decades of Martian surface changes","docAbstract":"The surface of Mars has changed dramatically during the three decades spanned by spacecraft exploration. Comparisons of Mars Global Surveyor images with Viking and Mariner 9 pictures suggest that more than one third of Mars' surface area has brightened or darkened by at least 10%. Such albedo changes could produce significant effects on solar heating and the global circulation of winds across the planet. All of the major changes took place in areas of moderate to high thermal inertia and rock abundance, consistent with burial of rocky surfaces by thin dust layers deposited during dust storms and subsequent exposure of the rocky surfaces by aeolian erosion. Several distinct mechanisms contribute to aeolian erosion on Mars. Prevailing winds dominate erosion at low latitudes, producing diffuse albedo boundaries and elongated wind streaks generally oriented in the direction of southern summer winds. Dust devils darken the mid to high latitudes from 45 to 70 degrees during the summer seasons, forming irregular albedo patterns consisting of dark linear tracks. Dust storms produce regional albedo variations with distinct but irregular margins. Dark sand duties in southern high latitudes appear to be associated with regional darkening that displays diffuse albedo boundaries. No surface changes were observed to repeat regularly on an annual basis, but many of the changes took place in areas that alternate episodically between high- and low-albedo states as thin mantles of dust are deposited and later stripped off. Hence the face of Mars remains recognizable after a century of telescopic observations, in spite of the enormous extent of alteration that has taken place during the era of spacecraft exploration.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Geophysical Research E: Planets","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1029/2004JE002345","issn":"01480227","usgsCitation":"Geissler, P., 2005, Three decades of Martian surface changes: Journal of Geophysical Research E: Planets, v. 110, no. 2, p. 1-23, https://doi.org/10.1029/2004JE002345.","startPage":"1","endPage":"23","numberOfPages":"23","costCenters":[],"links":[{"id":210468,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1029/2004JE002345"},{"id":237393,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"110","issue":"2","noUsgsAuthors":false,"publicationDate":"2005-02-03","publicationStatus":"PW","scienceBaseUri":"505bb306e4b08c986b325b2e","contributors":{"authors":[{"text":"Geissler, P.E.","contributorId":67636,"corporation":false,"usgs":true,"family":"Geissler","given":"P.E.","email":"","affiliations":[],"preferred":false,"id":421260,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70029042,"text":"70029042 - 2005 - Limiting similarity and functional diversity along environmental gradients","interactions":[],"lastModifiedDate":"2012-03-12T17:20:59","indexId":"70029042","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1466,"text":"Ecology Letters","active":true,"publicationSubtype":{"id":10}},"title":"Limiting similarity and functional diversity along environmental gradients","docAbstract":"Recent developments in community models emphasize the importance of incorporating stochastic processes (e.g. ecological drift) in models of niche-structured community assembly. We constructed a finite, spatially explicit, lottery model to simulate the distribution of species in a one-dimensional landscape with an underlying gradient in environmental conditions. Our framework combines the potential for ecological drift with environmentally-mediated competition for space in a heterogeneous environment. We examined the influence of niche breadth, dispersal distances, community size (total number of individuals) and the breadth of the environmental gradient on levels of species and functional trait diversity (i.e. differences in niche optima). Three novel results emerge from this model: (1) niche differences between adjacent species (e.g. limiting similarity) increase in smaller communities, because of the interaction of competitive effects and finite population sizes; (2) immigration from a regional species pool, stochasticity and niche-assembly generate a bimodal distribution of species residence times ('transient' and 'resident') under a heterogeneous environment; and (3) the magnitude of environmental heterogeneity has a U-shaped effect on diversity, because of shifts in species richness of resident vs. transient species. These predictions illustrate the potential importance of stochastic (although not necessarily neutral) processes in community assembly. ??2005 Blackwell Publishing Ltd/CNRS.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Ecology Letters","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1111/j.1461-0248.2004.00720.x","issn":"1461023X","usgsCitation":"Schwilk, D., and Ackerly, D., 2005, Limiting similarity and functional diversity along environmental gradients: Ecology Letters, v. 8, no. 3, p. 272-281, https://doi.org/10.1111/j.1461-0248.2004.00720.x.","startPage":"272","endPage":"281","numberOfPages":"10","costCenters":[],"links":[{"id":236352,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":209679,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1111/j.1461-0248.2004.00720.x"}],"volume":"8","issue":"3","noUsgsAuthors":false,"publicationDate":"2005-01-20","publicationStatus":"PW","scienceBaseUri":"505a4794e4b0c8380cd678df","contributors":{"authors":[{"text":"Schwilk, D.W.","contributorId":29770,"corporation":false,"usgs":true,"family":"Schwilk","given":"D.W.","affiliations":[],"preferred":false,"id":421072,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ackerly, D. D.","contributorId":94077,"corporation":false,"usgs":false,"family":"Ackerly","given":"D. D.","affiliations":[],"preferred":false,"id":421073,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70029039,"text":"70029039 - 2005 - Calculation of broadband time histories of ground motion, Part II: Kinematic and dynamic modeling using theoretical Green's functions and comparison with the 1994 northridge earthquake","interactions":[],"lastModifiedDate":"2016-01-27T13:48:35","indexId":"70029039","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1135,"text":"Bulletin of the Seismological Society of America","onlineIssn":"1943-3573","printIssn":"0037-1106","active":true,"publicationSubtype":{"id":10}},"title":"Calculation of broadband time histories of ground motion, Part II: Kinematic and dynamic modeling using theoretical Green's functions and comparison with the 1994 northridge earthquake","docAbstract":"<p>In the evolution of methods for calculating synthetic time histories of ground motion for postulated earthquakes, kinematic source models have dominated to date because of their ease of application. Dynamic models, however, which incorporate a physical relationship between important faulting parameters of stress drop, slip, rupture velocity, and rise time, are becoming more accessible. This article compares a class of kinematic models based on the summation of a fractal distribution of subevent sizes with a dynamic model based on the slip-weakening friction law. Kinematic modeling is done for the frequency band 0.2 to 10.0. Hz, dynamic models are calculated from 0.2 to 2.0. Hz. The strong motion data set for the 1994 Northridge earthquake is used to evaluate and compare the synthetic time histories. Source models are propagated to the far field by convolution with 1D and 3D theoretical Green&rsquo;s functions. In addition, the kinematic model is used to evaluate the importance of propagation path effects: velocity structure, scattering, and nonlinearity. At present, the kinematic model gives a better broadband fit to the Northridge ground motion than the simple slip-weakening dynamic model. In general, the dynamic model overpredicts rise times and produces insufficient shorter-period energy. Within the context of the slip-weakening model, the Northridge ground motion requires a short slip-weakening distance, on the order of 0.15 m or less. A more complex dynamic model including rate weakening or one that allows shorter rise times near the hypocenter may fit the data better.</p>","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Bulletin of the Seismological Society of America","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Seismological Society of America","publisherLocation":"Stanford","doi":"10.1785/0120040136","issn":"00371106","usgsCitation":"Hartzell, S., Guatteri, M., Mai, P., Liu, P., and Fisk, M.R., 2005, Calculation of broadband time histories of ground motion, Part II: Kinematic and dynamic modeling using theoretical Green's functions and comparison with the 1994 northridge earthquake: Bulletin of the Seismological Society of America, v. 95, no. 2, p. 614-645, https://doi.org/10.1785/0120040136.","productDescription":"32 p.","startPage":"614","endPage":"645","numberOfPages":"32","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":236419,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":209724,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1785/0120040136"}],"volume":"95","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f301e4b0c8380cd4b53f","contributors":{"authors":[{"text":"Hartzell, S.","contributorId":12603,"corporation":false,"usgs":true,"family":"Hartzell","given":"S.","email":"","affiliations":[],"preferred":false,"id":421059,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Guatteri, Mariagiovanna","contributorId":29979,"corporation":false,"usgs":true,"family":"Guatteri","given":"Mariagiovanna","email":"","affiliations":[],"preferred":false,"id":421062,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mai, P.M.","contributorId":32712,"corporation":false,"usgs":true,"family":"Mai","given":"P.M.","email":"","affiliations":[],"preferred":false,"id":421063,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Liu, P.-C.","contributorId":25339,"corporation":false,"usgs":true,"family":"Liu","given":"P.-C.","email":"","affiliations":[],"preferred":false,"id":421061,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Fisk, M. R.","contributorId":17031,"corporation":false,"usgs":false,"family":"Fisk","given":"M.","email":"","middleInitial":"R.","affiliations":[{"id":6680,"text":"Oregon State University","active":true,"usgs":false}],"preferred":false,"id":421060,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70028867,"text":"70028867 - 2005 - Offshore marine observation of Willow Ptarmigan, including water landings, Kuskokwim Bay, Alaska","interactions":[],"lastModifiedDate":"2017-03-21T17:40:17","indexId":"70028867","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3783,"text":"The Wilson Bulletin","printIssn":"0043-5643","active":true,"publicationSubtype":{"id":10}},"title":"Offshore marine observation of Willow Ptarmigan, including water landings, Kuskokwim Bay, Alaska","docAbstract":"<p>We report an observation of Willow Ptarmigan (<i>Lagopus lagopus</i>) encountered 8 to 17 km from the nearest shoreline on Kuskokwim Bay, Alaska, on 30 August 2003. The ptarmigan were observed flying, landing on our research vessel, and landing and taking off from the water surface. We also report on one other observation of ptarmigan sitting on the water surface and other marine observations of ptarmigan from the North Pacific Pelagic Seabird Database. These observations provide evidence that Willow Ptarmigan are capable of dispersing across large bodies of water and landing and taking off from the water surface.</p>","language":"English","publisher":"Wilson Ornithological Society","doi":"10.1676/04-074","issn":"00435643","usgsCitation":"Zimmerman, C.E., Hillgruber, N., Burril, S., St. Peters, M.A., and Wetzel, J.D., 2005, Offshore marine observation of Willow Ptarmigan, including water landings, Kuskokwim Bay, Alaska: The Wilson Bulletin, v. 117, no. 1, p. 12-14, https://doi.org/10.1676/04-074.","productDescription":"3 p.","startPage":"12","endPage":"14","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":477823,"rank":1,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://doi.org/10.1676/04-074","text":"External Repository"},{"id":236654,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Kuskokwim Bay","volume":"117","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a6cb8e4b0c8380cd74da6","contributors":{"authors":[{"text":"Zimmerman, Christian E. 0000-0002-3646-0688 czimmerman@usgs.gov","orcid":"https://orcid.org/0000-0002-3646-0688","contributorId":410,"corporation":false,"usgs":true,"family":"Zimmerman","given":"Christian","email":"czimmerman@usgs.gov","middleInitial":"E.","affiliations":[{"id":120,"text":"Alaska Science Center Water","active":true,"usgs":true},{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":116,"text":"Alaska Science Center Biology MFEB","active":true,"usgs":true}],"preferred":true,"id":420100,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hillgruber, Nicola","contributorId":138856,"corporation":false,"usgs":false,"family":"Hillgruber","given":"Nicola","email":"","affiliations":[{"id":12548,"text":"University of Alaska Fairbanks, School of Fisheries and Ocean Sciences","active":true,"usgs":false}],"preferred":false,"id":420102,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Burril, Sean E.","contributorId":56183,"corporation":false,"usgs":true,"family":"Burril","given":"Sean E.","affiliations":[],"preferred":false,"id":420101,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"St. Peters, Michelle A.","contributorId":25744,"corporation":false,"usgs":false,"family":"St. Peters","given":"Michelle","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":420099,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Wetzel, Jennifer D.","contributorId":92861,"corporation":false,"usgs":false,"family":"Wetzel","given":"Jennifer","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":420103,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70029510,"text":"70029510 - 2005 - Identifying spawning behavior in Pacific halibut (<i>Hippoglossus stenolepis</i>) using electronic tags","interactions":[],"lastModifiedDate":"2016-06-20T09:58:58","indexId":"70029510","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1528,"text":"Environmental Biology of Fishes","active":true,"publicationSubtype":{"id":10}},"title":"Identifying spawning behavior in Pacific halibut (<i>Hippoglossus stenolepis</i>) using electronic tags","docAbstract":"<p>Identifying spawning behavior in Pacific halibut, Hippoglossus stenolepis, is particularly challenging because they occupy a deep, remote environment during the spawning season. To identify spawning events, a method is needed in which direct observation by humans is not employed. Spawning behavior of seven other flatfish, species has been directly observed in their natural environment by investigators using SCUBA. All of these flatfish species display almost identical spawning behavior that follows a routine. Therefore, it is reasonable to believe that this spawning behavior occurs in other flatfish species, including Pacific halibut. As part of a larger study, we recaptured two Pacific halibut on which Pop-up Archival Transmitting (PAT) tags had been attached during the winter spawning season. Because the tags were physically retrieved, we were able to collect minute-by-minute depth records for 135 and 155 days. We used these depth data to tentatively identify spawning events. On seven separate occasions between 20 January 2001 and 9 February 2001, one fish displayed a conspicuous routine only seen during the spawning season of Pacific halibut and the routine parallels the actions of other spawning flatfish directly observed by humans using SCUBA. Therefore, we propose this routine represents spawning behavior in Pacific halibut. The second tagged fish did not display the conspicuous routine, thus challenging the assumption that Pacific halibut are annual spawners. PAT tags may prove to be a useful tool for identifying spawning events of Pacific halibut, and that knowledge may be used for improved management in the future.&nbsp;</p>","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Environmental Biology of Fishes","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Springer","doi":"10.1007/s10641-005-3216-2","issn":"03781909","usgsCitation":"Seitz, A., Norcross, B.L., Wilson, D., and Nielsen, J., 2005, Identifying spawning behavior in Pacific halibut (<i>Hippoglossus stenolepis</i>) using electronic tags: Environmental Biology of Fishes, v. 73, no. 4, p. 445-451, https://doi.org/10.1007/s10641-005-3216-2.","productDescription":"7 p.","startPage":"445","endPage":"451","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":237926,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":210872,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/s10641-005-3216-2"}],"volume":"73","issue":"4","noUsgsAuthors":false,"publicationDate":"2005-08-01","publicationStatus":"PW","scienceBaseUri":"505a3858e4b0c8380cd61534","contributors":{"authors":[{"text":"Seitz, A.C.","contributorId":71756,"corporation":false,"usgs":true,"family":"Seitz","given":"A.C.","email":"","affiliations":[],"preferred":false,"id":423051,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Norcross, Brenda L.","contributorId":21497,"corporation":false,"usgs":false,"family":"Norcross","given":"Brenda","email":"","middleInitial":"L.","affiliations":[{"id":7211,"text":"University of Alaska, Fairbanks","active":true,"usgs":false}],"preferred":false,"id":423049,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wilson, D.","contributorId":30353,"corporation":false,"usgs":true,"family":"Wilson","given":"D.","affiliations":[],"preferred":false,"id":423050,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Nielsen, J.L.","contributorId":105665,"corporation":false,"usgs":true,"family":"Nielsen","given":"J.L.","email":"","affiliations":[],"preferred":false,"id":423052,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70027303,"text":"70027303 - 2005 - Nature's style: Naturally trendy","interactions":[],"lastModifiedDate":"2012-03-12T17:20:27","indexId":"70027303","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1807,"text":"Geophysical Research Letters","active":true,"publicationSubtype":{"id":10}},"title":"Nature's style: Naturally trendy","docAbstract":"Hydroclimatological time series often exhibit trends. While trend magnitude can be determined with little ambiguity, the corresponding statistical significance, sometimes cited to bolster scientific and political argument, is less certain because significance depends critically on the null hypothesis which in turn reflects subjective notions about what one expects to see. We consider statistical trend tests of hydroclimatological data in the presence of long-term persistence (LTP). Monte Carlo experiments employing FARIMA models indicate that trend tests which fail to consider LTP greatly overstate the statistical significance of observed trends when LTP is present. A new test is presented that avoids this problem. From a practical standpoint, however, it may be preferable to acknowledge that the concept of statistical significance is meaningless when discussing poorly understood systems.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Geophysical Research Letters","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1029/2005GL024476","issn":"00948276","usgsCitation":"Cohn, T., and Lins, H., 2005, Nature's style: Naturally trendy: Geophysical Research Letters, v. 32, no. 23, p. 1-5, https://doi.org/10.1029/2005GL024476.","startPage":"1","endPage":"5","numberOfPages":"5","costCenters":[],"links":[{"id":477892,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1029/2005gl024476","text":"Publisher Index Page"},{"id":209332,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1029/2005GL024476"},{"id":235639,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"32","issue":"23","noUsgsAuthors":false,"publicationDate":"2005-12-08","publicationStatus":"PW","scienceBaseUri":"505a63a0e4b0c8380cd725e3","contributors":{"authors":[{"text":"Cohn, T.A.","contributorId":84789,"corporation":false,"usgs":true,"family":"Cohn","given":"T.A.","email":"","affiliations":[],"preferred":false,"id":413107,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lins, H.F.","contributorId":81508,"corporation":false,"usgs":true,"family":"Lins","given":"H.F.","affiliations":[],"preferred":false,"id":413106,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
]}