{"pageNumber":"2595","pageRowStart":"64850","pageSize":"25","recordCount":184617,"records":[{"id":70031428,"text":"70031428 - 2005 - Population genetic structure and conservation of marbled murrelets (<i>Brachyramphus marmoratus</i>)","interactions":[],"lastModifiedDate":"2017-11-18T09:37:41","indexId":"70031428","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1324,"text":"Conservation Genetics","active":true,"publicationSubtype":{"id":10}},"title":"Population genetic structure and conservation of marbled murrelets (<i>Brachyramphus marmoratus</i>)","docAbstract":"<p>Marbled murrelets (<i>Brachyramphus marmoratus</i>) are coastal seabirds that nest from California to the Aleutian Islands. They are declining and considered threatened in several regions. We compared variation in the mitochondrial control region, four nuclear introns and three microsatellite loci among 194 murrelets from throughout their range except Washington and Oregon. Significant population genetic structure was found: nine private control region haplotypes and three private intron alleles occurred at high frequency in the Aleutians and California; global estimates of FST or ??ST and most pairwise estimates involving the Aleutians and/or California were significant; and marked isolation-by-distance was found. Given the available samples, murrelets appear to comprise five genetic management units: (1) western Aleutian Islands, (2) central Aleutian Islands, (3) mainland Alaska and British Columbia, (4) northern California, and (5) central California.</p>","largerWorkTitle":"onservation Genetics","language":"English","publisher":"Springer","doi":"10.1007/s10592-005-9012-x","issn":"15660621","usgsCitation":"Friesen, V.L., Birt, T., Piatt, J.F., Golightly, R., Newman, S.H., Hebert, P., Congdon, B., and Gissing, G., 2005, Population genetic structure and conservation of marbled murrelets (<i>Brachyramphus marmoratus</i>): Conservation Genetics, v. 6, no. 4, p. 607-614, https://doi.org/10.1007/s10592-005-9012-x.","productDescription":"8 p.","startPage":"607","endPage":"614","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":240137,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Canada, United States","volume":"6","issue":"4","noUsgsAuthors":false,"publicationDate":"2005-12-02","publicationStatus":"PW","scienceBaseUri":"505a7d71e4b0c8380cd79f4f","contributors":{"authors":[{"text":"Friesen, Vicki L.","contributorId":59407,"corporation":false,"usgs":false,"family":"Friesen","given":"Vicki","email":"","middleInitial":"L.","affiliations":[{"id":7029,"text":"Queen's University, Kingston, Ontario, Canada","active":true,"usgs":false}],"preferred":false,"id":431458,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Birt, T.P.","contributorId":82411,"corporation":false,"usgs":true,"family":"Birt","given":"T.P.","email":"","affiliations":[],"preferred":false,"id":431461,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Piatt, John F. 0000-0002-4417-5748 jpiatt@usgs.gov","orcid":"https://orcid.org/0000-0002-4417-5748","contributorId":3025,"corporation":false,"usgs":true,"family":"Piatt","given":"John","email":"jpiatt@usgs.gov","middleInitial":"F.","affiliations":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":116,"text":"Alaska Science Center Biology MFEB","active":true,"usgs":true},{"id":117,"text":"Alaska Science Center Biology WTEB","active":true,"usgs":true}],"preferred":true,"id":431462,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Golightly, R.T.","contributorId":10743,"corporation":false,"usgs":true,"family":"Golightly","given":"R.T.","email":"","affiliations":[],"preferred":false,"id":431455,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Newman, S. H.","contributorId":21888,"corporation":false,"usgs":false,"family":"Newman","given":"S.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":431456,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Hebert, P.N.","contributorId":80878,"corporation":false,"usgs":true,"family":"Hebert","given":"P.N.","email":"","affiliations":[],"preferred":false,"id":431460,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Congdon, B.C.","contributorId":55397,"corporation":false,"usgs":true,"family":"Congdon","given":"B.C.","email":"","affiliations":[],"preferred":false,"id":431457,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Gissing, G.","contributorId":66484,"corporation":false,"usgs":true,"family":"Gissing","given":"G.","email":"","affiliations":[],"preferred":false,"id":431459,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":70031427,"text":"70031427 - 2005 - A note on the comparative turbidity of some estuaries of the Americas","interactions":[],"lastModifiedDate":"2012-03-12T17:21:08","indexId":"70031427","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":"A note on the comparative turbidity of some estuaries of the Americas","docAbstract":"Field data from 27 estuaries of the Americas are used to show that, in broad terms, there is a large difference in turbidity between the analyzed east and west-coast estuaries and that tidal range and tidal length have an important influence on that turbidity. Generic, numerical sediment-transport modeling is used to illustrate this influence, which exists over a range of space scales from, e.g., the Rogue River Estuary (few km, few mg l-1) to the Bay of Fundy (hundreds of km, few g l-1). The difference in Pacific and Atlantic seaboard estuarine turbidity for the analyzed estuaries is ultimately related to the broad-scale geomorphology of the two continents.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Coastal Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.2112/016-NIS.1","issn":"07490208","usgsCitation":"Uncles, R., and Smith, R.E., 2005, A note on the comparative turbidity of some estuaries of the Americas: Journal of Coastal Research, v. 21, no. 4, p. 845-852, https://doi.org/10.2112/016-NIS.1.","startPage":"845","endPage":"852","numberOfPages":"8","costCenters":[],"links":[{"id":212621,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.2112/016-NIS.1"},{"id":240136,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"21","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e4c3e4b0c8380cd468e5","contributors":{"authors":[{"text":"Uncles, R.J.","contributorId":33468,"corporation":false,"usgs":true,"family":"Uncles","given":"R.J.","affiliations":[],"preferred":false,"id":431453,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smith, R. E.","contributorId":76366,"corporation":false,"usgs":true,"family":"Smith","given":"R.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":431454,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70029010,"text":"70029010 - 2005 - Changes toward earlier streamflow timing across western North America","interactions":[],"lastModifiedDate":"2018-10-31T09:32:18","indexId":"70029010","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2216,"text":"Journal of Climate","active":true,"publicationSubtype":{"id":10}},"title":"Changes toward earlier streamflow timing across western North America","docAbstract":"<p>The highly variable timing of streamflow in snowmelt-dominated basins across western North America is an important consequence, and indicator, of climate fluctuations. Changes in the timing of snowmelt-derived streamflow from 1948 to 2002 were investigated in a network of 302 western North America gauges by examining the center of mass for flow, spring pulse onset dates, and seasonal fractional flows through trend and principal component analyses. Statistical analysis of the streamflow timing measures with Pacific climate indicators identified local and key large-scale processes that govern the regionally coherent parts of the changes and their relative importance.</p><p>Widespread and regionally coherent trends toward earlier onsets of springtime snowmelt and streamflow have taken place across most of western North America, affecting an area that is much larger than previously recognized. These timing changes have resulted in increasing fractions of annual flow occurring earlier in the water year by 1–4 weeks. The immediate (or proximal) forcings for the spatially coherent parts of the year-to-year fluctuations and longer-term trends of streamflow timing have been higher winter and spring temperatures. Although these temperature changes are partly controlled by the decadal-scale Pacific climate mode [Pacific decadal oscillation (PDO)], a separate and significant part of the variance is associated with a springtime warming trend that spans the PDO phases.</p>","language":"English","publisher":"AMS","doi":"10.1175/JCLI3321.1","issn":"08948755","usgsCitation":"Stewart, I., Cayan, D., and Dettinger, M.D., 2005, Changes toward earlier streamflow timing across western North America: Journal of Climate, v. 18, no. 8, p. 1136-1155, https://doi.org/10.1175/JCLI3321.1.","productDescription":"20 p.","startPage":"1136","endPage":"1155","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":477713,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1175/jcli3321.1","text":"Publisher Index Page"},{"id":236798,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":210010,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1175/JCLI3321.1"}],"volume":"18","issue":"8","noUsgsAuthors":false,"publicationDate":"2005-04-15","publicationStatus":"PW","scienceBaseUri":"5059f43de4b0c8380cd4bc11","contributors":{"authors":[{"text":"Stewart, I.T.","contributorId":80062,"corporation":false,"usgs":true,"family":"Stewart","given":"I.T.","email":"","affiliations":[],"preferred":false,"id":420944,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cayan, D.R.","contributorId":25961,"corporation":false,"usgs":false,"family":"Cayan","given":"D.R.","email":"","affiliations":[{"id":16196,"text":"Scripps Institution of Oceanography, La Jolla, CA","active":true,"usgs":false}],"preferred":false,"id":420943,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dettinger, M. D. 0000-0002-7509-7332","orcid":"https://orcid.org/0000-0002-7509-7332","contributorId":93069,"corporation":false,"usgs":false,"family":"Dettinger","given":"M.","middleInitial":"D.","affiliations":[{"id":16196,"text":"Scripps Institution of Oceanography, La Jolla, CA","active":true,"usgs":false}],"preferred":false,"id":420945,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70031425,"text":"70031425 - 2005 - Repeating coupled earthquakes at Shishaldin Volcano, Alaska","interactions":[],"lastModifiedDate":"2019-04-30T12:16:07","indexId":"70031425","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2499,"text":"Journal of Volcanology and Geothermal Research","active":true,"publicationSubtype":{"id":10}},"title":"Repeating coupled earthquakes at Shishaldin Volcano, Alaska","docAbstract":"Since it last erupted in 1999, Shishaldin Volcano, Aleutian Islands, Alaska, has produced hundreds to thousands of long-period (1-2 Hz; LP) earthquakes every day with no other sign of volcanic unrest. In 2002, the earthquakes also exhibited a short-period (4-7 Hz; SP) signal occurring between 3 and 15 s before the LP phase. Although the SP phase contains higher frequencies than the LP phase, its spectral content is still well below that expected of brittle failure events. The SP phase was never observed without the LP phase, although LP events continued to occur in the absence of the precursory signal. The two-phased events are termed \"coupled events\", reflecting a triggered relationship between two discrete event types. Both phases are highly repetitive in time series, suggestive of stable, non-destructive sources. Waveform cross-correlation and spectral coherence are used to extract waveforms from the continuous record and determine precise P-wave arrivals for the SP phase. Although depths are poorly constrained, the SP phase is believed to lie at shallow (<4 km) depths just west of Shishaldin's summit. The variable timing between the SP and LP arrivals indicates that the trigger mechanism between the phases itself moves at variable speeds. A model is proposed in which the SP phase results from fluid moving within the conduit, possibly around an obstruction and the LP phase results from the coalescence of a shallow gas bubble. The variable timing is attributed to changes in gas content within the conduit. The destruction of the conduit obstacle on November 21, 2002 resulted in the abrupt disappearance of the SP phase.","largerWorkTitle":"Journal of Volcanology and Geothermal Research","language":"English","doi":"10.1016/j.jvolgeores.2005.01.011","issn":"03770273","usgsCitation":"Caplan-Auerbach, J., and Petersen, T., 2005, Repeating coupled earthquakes at Shishaldin Volcano, Alaska: Journal of Volcanology and Geothermal Research, v. 145, no. 1-2, p. 151-172, https://doi.org/10.1016/j.jvolgeores.2005.01.011.","productDescription":"22 p.","startPage":"151","endPage":"172","numberOfPages":"22","costCenters":[{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true}],"links":[{"id":240134,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":212620,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.jvolgeores.2005.01.011"}],"country":"United States","state":"Alaska","otherGeospatial":"Mount Shishaldin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -164.20989990234375,\n              54.69288437829768\n            ],\n            [\n              -163.8336181640625,\n              54.69288437829768\n            ],\n            [\n              -163.8336181640625,\n              54.82126112097626\n            ],\n            [\n              -164.20989990234375,\n              54.82126112097626\n            ],\n            [\n              -164.20989990234375,\n              54.69288437829768\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"145","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505aa750e4b0c8380cd85342","contributors":{"authors":[{"text":"Caplan-Auerbach, J.","contributorId":7057,"corporation":false,"usgs":true,"family":"Caplan-Auerbach","given":"J.","email":"","affiliations":[],"preferred":false,"id":431450,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Petersen, T.","contributorId":104705,"corporation":false,"usgs":true,"family":"Petersen","given":"T.","email":"","affiliations":[],"preferred":false,"id":431451,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70031422,"text":"70031422 - 2005 - Dynamic modeling of Tampa Bay urban development using parallel computing","interactions":[],"lastModifiedDate":"2017-04-10T13:05:38","indexId":"70031422","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1315,"text":"Computers & Geosciences","printIssn":"0098-3004","active":true,"publicationSubtype":{"id":10}},"title":"Dynamic modeling of Tampa Bay urban development using parallel computing","docAbstract":"<p><span>Urban land use and land cover has changed significantly in the environs of Tampa Bay, Florida, over the past 50 years. Extensive urbanization has created substantial change to the region's landscape and ecosystems. This paper uses a dynamic urban-growth model, SLEUTH, which applies six geospatial data themes (slope, land use, exclusion, urban extent, transportation, hillside), to study the process of urbanization and associated land use and land cover change in the Tampa Bay area. To reduce processing time and complete the modeling process within an acceptable period, the model is recoded and ported to a Beowulf cluster. The parallel-processing computer system accomplishes the massive amount of computation the modeling simulation requires. SLEUTH calibration process for the Tampa Bay urban growth simulation spends only 10&nbsp;h CPU time. The model predicts future land use/cover change trends for Tampa Bay from 1992 to 2025. Urban extent is predicted to double in the Tampa Bay watershed between 1992 and 2025. Results show an upward trend of urbanization at the expense of a decline of 58% and 80% in agriculture and forested lands, respectively.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.cageo.2005.03.006","issn":"00983004","usgsCitation":"Xian, G., Crane, M., and Steinwand, D., 2005, Dynamic modeling of Tampa Bay urban development using parallel computing: Computers & Geosciences, v. 31, no. 7, p. 920-928, https://doi.org/10.1016/j.cageo.2005.03.006.","productDescription":"9 p.","startPage":"920","endPage":"928","numberOfPages":"9","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":240097,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":212591,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.cageo.2005.03.006"}],"volume":"31","issue":"7","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0427e4b0c8380cd50800","contributors":{"authors":[{"text":"Xian, G. 0000-0001-5674-2204","orcid":"https://orcid.org/0000-0001-5674-2204","contributorId":65656,"corporation":false,"usgs":true,"family":"Xian","given":"G.","affiliations":[],"preferred":false,"id":431441,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Crane, M.","contributorId":86957,"corporation":false,"usgs":true,"family":"Crane","given":"M.","email":"","affiliations":[],"preferred":false,"id":431442,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Steinwand, D.","contributorId":9863,"corporation":false,"usgs":true,"family":"Steinwand","given":"D.","email":"","affiliations":[],"preferred":false,"id":431440,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70028994,"text":"70028994 - 2005 - Late Pennsylvanian and early permian chondrichthyan microremains from San Salvador Patlanoaya (Puebla, Mexico)","interactions":[],"lastModifiedDate":"2012-03-12T17:20:42","indexId":"70028994","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1752,"text":"Geobios","active":true,"publicationSubtype":{"id":10}},"title":"Late Pennsylvanian and early permian chondrichthyan microremains from San Salvador Patlanoaya (Puebla, Mexico)","docAbstract":"The San Salvador Patlanoaya section (Puebla State, Mexico) is known for its richness of many fossil groups. Among them, the calcareous shells have been principally investigated. This paper deals with Missourian-Virgilian (Late Pennsylvanian) and Leonardian (late Early Permian) Mexican fish remains. A discussion about Helicoprion and related genera, is followed by the systematic description of the revised or discovered taxa: Cooperella typicalis, Moreyella cf. M. typicalis, M. (?) sp., \"Sturgeonella\" quinqueloba, Hybodontidae gen. sp. 1 and 2, scale indet. Palaeobiogeographic implications are suggested. ?? 2005 Elsevier SAS. All rights reserved.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Geobios","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.geobios.2003.06.008","issn":"00166995","usgsCitation":"Derycke-Khatir, C., Vachard, D., Degardin, J., Flores de Dios, A., Buitron, B., and Hansen, M., 2005, Late Pennsylvanian and early permian chondrichthyan microremains from San Salvador Patlanoaya (Puebla, Mexico): Geobios, v. 38, no. 1, p. 43-55, https://doi.org/10.1016/j.geobios.2003.06.008.","startPage":"43","endPage":"55","numberOfPages":"13","costCenters":[],"links":[{"id":209913,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.geobios.2003.06.008"},{"id":236665,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"38","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a4505e4b0c8380cd66f7d","contributors":{"authors":[{"text":"Derycke-Khatir, C.","contributorId":93685,"corporation":false,"usgs":true,"family":"Derycke-Khatir","given":"C.","email":"","affiliations":[],"preferred":false,"id":420871,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Vachard, D.","contributorId":65274,"corporation":false,"usgs":true,"family":"Vachard","given":"D.","email":"","affiliations":[],"preferred":false,"id":420868,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Degardin, J.-M.","contributorId":74942,"corporation":false,"usgs":true,"family":"Degardin","given":"J.-M.","email":"","affiliations":[],"preferred":false,"id":420869,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Flores de Dios, A.","contributorId":80886,"corporation":false,"usgs":true,"family":"Flores de Dios","given":"A.","email":"","affiliations":[],"preferred":false,"id":420870,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Buitron, B.","contributorId":34706,"corporation":false,"usgs":true,"family":"Buitron","given":"B.","email":"","affiliations":[],"preferred":false,"id":420867,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Hansen, M.","contributorId":34670,"corporation":false,"usgs":true,"family":"Hansen","given":"M.","affiliations":[],"preferred":false,"id":420866,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70031394,"text":"70031394 - 2005 - Unexpected trend in the compositional maturity of second-cycle sand","interactions":[],"lastModifiedDate":"2012-03-12T17:21:11","indexId":"70031394","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3368,"text":"Sedimentary Geology","active":true,"publicationSubtype":{"id":10}},"title":"Unexpected trend in the compositional maturity of second-cycle sand","docAbstract":"It is generally accepted that recycling of sandstone generates relatively more mature sand than its parent sandstone. Such maturity is accomplished mainly through chemical weathering as the chemically unstable minerals are eliminated. Because chemical weathering is ubiquitous on the Earth's surface, maturity due to recycling is expected in most geological settings. However, contrary to one's expectation, second-cycle Holocene sand, exclusively derived from sandy facies of the first-cycle Pennsylvanian-Permian Cutler Formation, is actually less mature than its first-cycle parent near Gateway, Colorado. Both the Cutler sandstone and Holocene sand were the products of similar geological processes that controlled their respective composition. In spite of such similarities, a significant difference in composition is observed. We propose that the unexpected immaturity in second-cycle Holocene sand may be due to mechanical disintegration of coarse-grained feldspar and feldspar-rich rock fragments into relatively smaller fractions. Results presented in this paper are the first quantitative estimation of recycling of parent sandstone into daughter sand, and the first observed reverse maturity trend in second-cycle sand. These unexpected results suggest the need for further research to quantitatively understand the recycling process. ?? 2005 Elsevier B.V. All rights reserved.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Sedimentary Geology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.sedgeo.2005.05.008","issn":"00370738","usgsCitation":"Solano-Acosta, W., and Dutta, P., 2005, Unexpected trend in the compositional maturity of second-cycle sand: Sedimentary Geology, v. 178, no. 3-4, p. 275-283, https://doi.org/10.1016/j.sedgeo.2005.05.008.","startPage":"275","endPage":"283","numberOfPages":"9","costCenters":[],"links":[{"id":212202,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.sedgeo.2005.05.008"},{"id":239653,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"178","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bbc7be4b08c986b328c55","contributors":{"authors":[{"text":"Solano-Acosta, W.","contributorId":29212,"corporation":false,"usgs":true,"family":"Solano-Acosta","given":"W.","email":"","affiliations":[],"preferred":false,"id":431317,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dutta, P.K.","contributorId":30037,"corporation":false,"usgs":true,"family":"Dutta","given":"P.K.","email":"","affiliations":[],"preferred":false,"id":431318,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70031712,"text":"70031712 - 2005 - Growth hormone and insulin-like growth factors in fish: Where we are and where to go","interactions":[],"lastModifiedDate":"2012-03-12T17:21:13","indexId":"70031712","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Growth hormone and insulin-like growth factors in fish: Where we are and where to go","docAbstract":"This communication summarizes viewpoints, discussion, perspectives, and questions, put forward at a workshop on \"Growth hormone and insulin-like growth factors in fish\" held on September 7th, 2004, at the 5th International Symposium on Fish Endocrinology in Castello??n, Spain. ?? 2005 Elsevier Inc. All rights reserved.","largerWorkTitle":"General and Comparative Endocrinology","language":"English","doi":"10.1016/j.ygcen.2005.01.016","issn":"00166480","usgsCitation":"Reinecke, M., Bjornsson, B.T., Dickhoff, W.W., McCormick, S., Navarro, I., Power, D., and Gutierrez, J., 2005, Growth hormone and insulin-like growth factors in fish: Where we are and where to go, <i>in</i> General and Comparative Endocrinology, v. 142, no. 1-2 SPEC. ISS., p. 20-24, https://doi.org/10.1016/j.ygcen.2005.01.016.","startPage":"20","endPage":"24","numberOfPages":"5","costCenters":[],"links":[{"id":212278,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.ygcen.2005.01.016"},{"id":239740,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"142","issue":"1-2 SPEC. ISS.","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a2df4e4b0c8380cd5c18d","contributors":{"authors":[{"text":"Reinecke, M.","contributorId":106313,"corporation":false,"usgs":true,"family":"Reinecke","given":"M.","email":"","affiliations":[],"preferred":false,"id":432803,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bjornsson, Bjorn Thrandur","contributorId":28928,"corporation":false,"usgs":true,"family":"Bjornsson","given":"Bjorn","email":"","middleInitial":"Thrandur","affiliations":[],"preferred":false,"id":432798,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dickhoff, Walton W.","contributorId":85133,"corporation":false,"usgs":true,"family":"Dickhoff","given":"Walton","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":432802,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"McCormick, S. D. 0000-0003-0621-6200","orcid":"https://orcid.org/0000-0003-0621-6200","contributorId":20278,"corporation":false,"usgs":true,"family":"McCormick","given":"S. D.","affiliations":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"preferred":false,"id":432797,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Navarro, I.","contributorId":68534,"corporation":false,"usgs":true,"family":"Navarro","given":"I.","email":"","affiliations":[],"preferred":false,"id":432801,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Power, D.M.","contributorId":53164,"corporation":false,"usgs":true,"family":"Power","given":"D.M.","email":"","affiliations":[],"preferred":false,"id":432800,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Gutierrez, J.","contributorId":30822,"corporation":false,"usgs":true,"family":"Gutierrez","given":"J.","email":"","affiliations":[],"preferred":false,"id":432799,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70031391,"text":"70031391 - 2005 - Population genetic structure in migratory sandhill cranes and the role of Pleistocene glaciations","interactions":[],"lastModifiedDate":"2017-12-29T12:30:16","indexId":"70031391","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2774,"text":"Molecular Ecology","active":true,"publicationSubtype":{"id":10}},"title":"Population genetic structure in migratory sandhill cranes and the role of Pleistocene glaciations","docAbstract":"Previous studies of migratory sandhill cranes (Grus canadensis) have made significant progress explaining evolution of this group at the species scale, but have been unsuccessful in explaining the geographically partitioned variation in morphology seen on the population scale. The objectives of this study were to assess the population structure and gene flow patterns among migratory sandhill cranes using microsatellite DNA genotypes and mitochondrial DNA haplotypes of a large sample of individuals across three populations. In particular, we were interested in evaluating the roles of Pleistocene glaciation events and postglaciation gene flow in shaping the present-day population structure. Our results indicate substantial gene flow across regions of the Midcontinental population that are geographically adjacent, suggesting that gene flow for most of the region follows an isolation-by-distance model. Male-mediated gene flow and strong female philopatry may explain the differing patterns of nuclear and mitochondrial variation. Taken in context with precise geographical information on breeding locations, the morphologic and microsatellite DNA variation shows a gradation from the Arctic-nesting subspecies G. c. canadensis to the non-Arctic subspecies G. c. tabida. Analogous to other Arctic-nesting birds, it is probable that the population structure seen in Midcontinental sandhill cranes reflects the result of post-glacial secondary contact. Our data suggest that subspecies of migratory sandhills experience significant gene flow and therefore do not represent distinct and independent genetic entities. ??2005 Blackwell Publishing Ltd.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Molecular Ecology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1111/j.1365-294X.2005.02622.x","issn":"09621083","usgsCitation":"Jones, K., Krapu, G., Brandt, D., and Ashley, M., 2005, Population genetic structure in migratory sandhill cranes and the role of Pleistocene glaciations: Molecular Ecology, v. 14, no. 9, p. 2645-2657, https://doi.org/10.1111/j.1365-294X.2005.02622.x.","productDescription":"13 p.","startPage":"2645","endPage":"2657","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":240133,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":212619,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1111/j.1365-294X.2005.02622.x"}],"volume":"14","issue":"9","noUsgsAuthors":false,"publicationDate":"2005-06-13","publicationStatus":"PW","scienceBaseUri":"505a7d73e4b0c8380cd79f5f","contributors":{"authors":[{"text":"Jones, K.L.","contributorId":102024,"corporation":false,"usgs":true,"family":"Jones","given":"K.L.","email":"","affiliations":[],"preferred":false,"id":431305,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Krapu, Gary L.","contributorId":56994,"corporation":false,"usgs":true,"family":"Krapu","given":"Gary L.","affiliations":[],"preferred":false,"id":431303,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brandt, D.A.","contributorId":67448,"corporation":false,"usgs":true,"family":"Brandt","given":"D.A.","email":"","affiliations":[],"preferred":false,"id":431304,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ashley, M.V.","contributorId":15556,"corporation":false,"usgs":true,"family":"Ashley","given":"M.V.","email":"","affiliations":[],"preferred":false,"id":431302,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70029034,"text":"70029034 - 2005 - ATR-FTIR spectroscopic characterization of coexisting carbonate surface complexes on hematite","interactions":[],"lastModifiedDate":"2012-03-12T17:20:59","indexId":"70029034","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1759,"text":"Geochimica et Cosmochimica Acta","active":true,"publicationSubtype":{"id":10}},"title":"ATR-FTIR spectroscopic characterization of coexisting carbonate surface complexes on hematite","docAbstract":"The speciation of carbonate adsorbed to hematite in air-equilibrated aqueous solutions has been studied using ATR-FTIR spectroscopy. Samples were measured over a range of pH conditions, at 0.1 M NaCl and at low ionic strength, and in H2O and D2O solutions to permit a multispecies analysis of the data. Second-derivative analyses and fits to the spectra indicate the presence of two major and two minor surface-bound carbonate species. The two major complexes coexist at near-neutral pH and low ionic strength. One of these two complexes is relatively sensitive to ionic strength, being displaced at 0.1 M NaCl, whereas the other is not. Comparison of experimental to DFT/MO-calculated frequencies suggest these two major species to be (a) a monodentate binuclear inner-sphere carbonate surface complex, and (b) a fully or partially solvated carbonate (CO32-) species that is symmetry broken and appears to reside in the structured vicinal water layers at the hematite-water interface, retained by hydrogen bonding and/or other forces. Minor carbonate complexes include diffuse layer CO32- and an unidentified inner-sphere species. Both of the dominant species observed here are likely to be significant controls of the surface charge and sorptive properties of Fe-oxides. Copyright ?? 2005 Elsevier Ltd.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Geochimica et Cosmochimica Acta","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.gca.2004.08.002","issn":"00167037","usgsCitation":"Bargar, J., Kubicki, J.D., Reitmeyer, R., and Davis, J., 2005, ATR-FTIR spectroscopic characterization of coexisting carbonate surface complexes on hematite: Geochimica et Cosmochimica Acta, v. 69, no. 6, p. 1527-1542, https://doi.org/10.1016/j.gca.2004.08.002.","startPage":"1527","endPage":"1542","numberOfPages":"16","costCenters":[],"links":[{"id":209703,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.gca.2004.08.002"},{"id":236388,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"69","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e63ce4b0c8380cd47288","contributors":{"authors":[{"text":"Bargar, J.R.","contributorId":82466,"corporation":false,"usgs":true,"family":"Bargar","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":421038,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kubicki, J. D.","contributorId":63212,"corporation":false,"usgs":true,"family":"Kubicki","given":"J.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":421036,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Reitmeyer, R.","contributorId":87710,"corporation":false,"usgs":true,"family":"Reitmeyer","given":"R.","affiliations":[],"preferred":false,"id":421039,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Davis, J.A.","contributorId":71694,"corporation":false,"usgs":true,"family":"Davis","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":421037,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70031716,"text":"70031716 - 2005 - Wagon loads of sand blows in White County, Illinois","interactions":[],"lastModifiedDate":"2022-06-02T16:33:58.336867","indexId":"70031716","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3372,"text":"Seismological Research Letters","onlineIssn":"1938-2057","printIssn":"0895-0695","active":true,"publicationSubtype":{"id":10}},"title":"Wagon loads of sand blows in White County, Illinois","docAbstract":"<p><span>Several anecdotal accounts provide compelling evidence that liquefaction occurred at several sites in Illinois during the 1811-1812 New Madrid sequence, as much as 250 km north of the New Madrid seismic zone (NMSZ). At one Wabash Valley location, sand blows are still evident near Big Prairie, Illinois, a location described in a particularly detailed and precise historic account. This account includes descriptions of substantial liquefaction (sand blows) as well as a two-mile-long east-west-trending “crack” along which two feet of south-side-down displacement occurred. An offset can no longer be seen at this location, which has been extensively farmed and plowed for decades. Field reconnaissance verifies many of the details provided in the account, however. We conducted a seismic-reflection experiment at this location and observed a modest offset in the Paleozoic strata at this location. The offset is opposite to that described in the historic account, consistent with the hypothesis that large midcontinent earthquakes occur on faults reactivated in a Holocene stress regime different from the one in which they were formed. Only two explanations can account for these observations: Either large NMSZ events triggered substantial liquefaction at distances greater than hitherto realized, or at least one large “New Madrid” event occurred significantly north of the NMSZ. We explore these possibilities and conclude that, while neither one can be ruled out, several disparate lines of evidence suggest that the 23 January 1812 “New Madrid mainshock” occurred in White County, Illinois, near the location of the&nbsp;</span><i>m<sub>b</sub></i><span>&nbsp;5.5 1968 southern Illinois earthquake and recent microearthquake activity.</span></p>","language":"English","publisher":"Seismological Society of America","doi":"10.1785/gssrl.76.3.373","usgsCitation":"Hough, S.E., Bilham, R., Mueller, K., Stephenson, W., Williams, R., and Odum, J., 2005, Wagon loads of sand blows in White County, Illinois: Seismological Research Letters, v. 76, no. 3, p. 373-386, https://doi.org/10.1785/gssrl.76.3.373.","productDescription":"14 p.","startPage":"373","endPage":"386","numberOfPages":"14","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true},{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"links":[{"id":239805,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Illinois","county":"White 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Boulder","active":true,"usgs":false}],"preferred":false,"id":432823,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Stephenson, William","contributorId":38804,"corporation":false,"usgs":true,"family":"Stephenson","given":"William","affiliations":[],"preferred":false,"id":432824,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Williams, Robert 0000-0002-2973-8493 rawilliams@usgs.gov","orcid":"https://orcid.org/0000-0002-2973-8493","contributorId":140741,"corporation":false,"usgs":true,"family":"Williams","given":"Robert","email":"rawilliams@usgs.gov","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":true,"id":432821,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Odum, Jack","contributorId":34798,"corporation":false,"usgs":true,"family":"Odum","given":"Jack","affiliations":[],"preferred":false,"id":432822,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70031431,"text":"70031431 - 2005 - A new species of Ischyodus (Chondrichthyes: Holocephali: Callorhynchidae) from Upper Maastrichtian Shallow marine facies of the Fox Hills and Hell Creek Formations, Williston basin, North Dakota, USA","interactions":[],"lastModifiedDate":"2012-03-12T17:21:11","indexId":"70031431","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2998,"text":"Palaeontology","active":true,"publicationSubtype":{"id":10}},"title":"A new species of Ischyodus (Chondrichthyes: Holocephali: Callorhynchidae) from Upper Maastrichtian Shallow marine facies of the Fox Hills and Hell Creek Formations, Williston basin, North Dakota, USA","docAbstract":"A new species of chimaeroid, Ischyodus rayhaasi sp. nov., is described based primarily upon the number and configuration of tritors on palatine and mandibular tooth plates. This new species is named in honour of Mr Raymond Haas. Fossils of I. rayhaasi have been recovered from the Upper Maastrichtian Fox Hills Formation and the Breien Member and an unnamed member of the Hell Creek Formation at sites in south-central North Dakota and north-central South Dakota, USA. Ischyodus rayhaasi inhabited shallow marine waters in the central part of the Western Interior Seaway during the latest Cretaceous. Apparently it was also present in similar habitats at that time in the Volga region of Russia. Ischyodus rayhaasi is the youngest Cretaceous species Ischyodus known to exist before the Cretaceous/Tertiary extinction, and the species apparently did not survive that event. It was replaced by Ischyodus dolloi, which is found in the Paleocene Cannonball Formation of the Williston Basin region of North Dakota and is widely distributed elsewhere. ?? The Palaeontological Association.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Palaeontology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1111/j.1475-4983.2005.00475.x","issn":"00310239","usgsCitation":"Hoganson, J., and Erickson, J., 2005, A new species of Ischyodus (Chondrichthyes: Holocephali: Callorhynchidae) from Upper Maastrichtian Shallow marine facies of the Fox Hills and Hell Creek Formations, Williston basin, North Dakota, USA: Palaeontology, v. 48, no. 4, p. 709-721, https://doi.org/10.1111/j.1475-4983.2005.00475.x.","startPage":"709","endPage":"721","numberOfPages":"13","costCenters":[],"links":[{"id":477965,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1111/j.1475-4983.2005.00475.x","text":"Publisher Index Page"},{"id":212174,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1111/j.1475-4983.2005.00475.x"},{"id":239624,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"48","issue":"4","noUsgsAuthors":false,"publicationDate":"2005-07-19","publicationStatus":"PW","scienceBaseUri":"5059e4b2e4b0c8380cd46858","contributors":{"authors":[{"text":"Hoganson, J.W.","contributorId":100127,"corporation":false,"usgs":true,"family":"Hoganson","given":"J.W.","email":"","affiliations":[],"preferred":false,"id":431468,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Erickson, J.M.","contributorId":15033,"corporation":false,"usgs":true,"family":"Erickson","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":431467,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70031364,"text":"70031364 - 2005 - Dating floodplain sediments using tree-ring response to burial","interactions":[],"lastModifiedDate":"2012-03-12T17:21:10","indexId":"70031364","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1425,"text":"Earth Surface Processes and Landforms","active":true,"publicationSubtype":{"id":10}},"title":"Dating floodplain sediments using tree-ring response to burial","docAbstract":"Floodplain sediments can be dated precisely based on the change in anatomy of tree rings upon burial. When a stem of tamarisk (Tamarix ramosissima) or sandbar willow (Salix exigua) is buried, subsequent annual rings in the buried section resemble the rings of roots: rings become narrower, vessels within the rings become larger, and transitions between rings become less distinct. We combined observations of these changes with tree-ring counts to determine the year of deposition of sedimentary beds exposed in a 150-m-long trench across the floodplain of the Rio Puerco, a rapidly filling arroyo in New Mexico. This method reliably dated most beds thicker than about 30 cm to within a year of deposition. Floodplain aggradation rates varied dramatically through time and space. Sediment deposition was mostly limited to brief overbank flows occurring every few years. The most rapid deposition occurred on channel-margin levees, which migrated laterally during channel narrowing. At the decadal timescale, the cross-section-average sediment deposition rate was steady, but there was a shift in the spatial pattern of deposition in the 1980s. From 1936 to 1986, sediment deposition occurred by channel narrowing, with little change in elevation of the thalweg. After 1986 sediment deposition occurred by vertical aggradation. From 1936 to 2000 about 27 per cent of the arroyo cross-section filled with sediment. The rate of filling from 1962 to 2000 was 0-8 vertical m/decade or 85 m2/decade. Published in 2005 by John Wiley & Sons, Ltd.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Earth Surface Processes and Landforms","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1002/esp.1263","issn":"01979337","usgsCitation":"Friedman, J.M., Vincent, K., and Shafroth, P., 2005, Dating floodplain sediments using tree-ring response to burial: Earth Surface Processes and Landforms, v. 30, no. 9, p. 1077-1091, https://doi.org/10.1002/esp.1263.","startPage":"1077","endPage":"1091","numberOfPages":"15","costCenters":[],"links":[{"id":212230,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1002/esp.1263"},{"id":239687,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"30","issue":"9","noUsgsAuthors":false,"publicationDate":"2005-08-30","publicationStatus":"PW","scienceBaseUri":"5059fddfe4b0c8380cd4e9a4","contributors":{"authors":[{"text":"Friedman, Jonathan M. 0000-0002-1329-0663","orcid":"https://orcid.org/0000-0002-1329-0663","contributorId":44495,"corporation":false,"usgs":true,"family":"Friedman","given":"Jonathan","middleInitial":"M.","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":true,"id":431208,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Vincent, K.R.","contributorId":42563,"corporation":false,"usgs":true,"family":"Vincent","given":"K.R.","email":"","affiliations":[],"preferred":false,"id":431207,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Shafroth, P.B.","contributorId":65041,"corporation":false,"usgs":true,"family":"Shafroth","given":"P.B.","email":"","affiliations":[],"preferred":false,"id":431209,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70031365,"text":"70031365 - 2005 - Resilience of predators to fishing pressure on coral patch reefs","interactions":[],"lastModifiedDate":"2012-03-12T17:21:10","indexId":"70031365","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2277,"text":"Journal of Experimental Marine Biology and Ecology","active":true,"publicationSubtype":{"id":10}},"title":"Resilience of predators to fishing pressure on coral patch reefs","docAbstract":"Numbers and biomass of piscivorous fish and their predation on other fish may often be high in undisturbed coral reef communities. The effects of such predation have sometimes been studied by removal of piscivores (either experimentally or by fishermen). Such perturbations have usually involved removal of large, highly vulnerable, mobile piscivores that are often actively sought in fisheries. The effects of fishing on smaller, demersal, semi-resident piscivores have been little studied. We studied such effects on the fish communities of patch reefs at Midway atoll by experimentally removing major resident, demersal, piscivorous fishes. First, four control reefs and four experimental reefs were selected, their dimensions and habitats mapped, and their visible fish communities censused repeatedly over 1 year. Census of all control and experimental reefs was continued for the following 39 months, during which known piscivores were collected repeatedly by hand spearing. Records were kept of catch and effort to calculate CPUE as an index of predator density. Spearfishing on the experimental reefs removed 2504 piscivorous fish from 12 families and 43 taxa (mostly species). The species richness of the catch did not show an overall change over the duration of the experiment. Spearman rank correlation analysis showed some unexpected positive correlations for density in numbers and biomass of major fished piscivorous groups (especially lizardfish) over the experiment. Only two relatively minor fished piscivorous taxa declined in abundance over the experiment, while the overall abundance of piscivores increased. Visual censuses of fish on the experimental reefs also failed to show reduction of total piscivores over the full experimental period. No significant trend in the abundance of lizardfish censused over the full period was apparent on any of the control reefs. The high resilience of piscivores on these experimental reefs to relatively intense fishing pressure could result from their protracted recruitment seasons, high immigration rates, cryptic habits, or naturally high abundances. A major factor was the high immigration rates of lizardfish, replacing lizardfish and other less mobile piscivores removed from the reefs by spearing. On the fished reefs, the removed lizardfish population replaced itself >20 times during the experiment; other piscivorous taxa replaced themselves only 5 times.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Experimental Marine Biology and Ecology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.jembe.2005.01.007","issn":"00220981","usgsCitation":"Schroeder, R., and Parrish, J., 2005, Resilience of predators to fishing pressure on coral patch reefs: Journal of Experimental Marine Biology and Ecology, v. 321, no. 2, p. 93-107, https://doi.org/10.1016/j.jembe.2005.01.007.","startPage":"93","endPage":"107","numberOfPages":"15","costCenters":[],"links":[{"id":212259,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.jembe.2005.01.007"},{"id":239720,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"321","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505aa9bce4b0c8380cd85f48","contributors":{"authors":[{"text":"Schroeder, R.E.","contributorId":30436,"corporation":false,"usgs":true,"family":"Schroeder","given":"R.E.","email":"","affiliations":[],"preferred":false,"id":431210,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Parrish, J.D.","contributorId":63083,"corporation":false,"usgs":true,"family":"Parrish","given":"J.D.","email":"","affiliations":[],"preferred":false,"id":431211,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70028997,"text":"70028997 - 2005 - The impact of introduced round gobies (Neogobius melanostomus) on phosphorus cycling in central Lake Erie","interactions":[],"lastModifiedDate":"2012-03-12T17:20:42","indexId":"70028997","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1169,"text":"Canadian Journal of Fisheries and Aquatic Sciences","active":true,"publicationSubtype":{"id":10}},"title":"The impact of introduced round gobies (Neogobius melanostomus) on phosphorus cycling in central Lake Erie","docAbstract":"We used an individual-based bioenergetic model to simulate the phosphorus flux of the round goby (Neogobius melanostomus) population in central Lake Erie during 1995-2002. Estimates of round goby diet composition, growth rates, and population abundance were derived from field sampling. As an abundant introduced fish, we predicted that round gobies would influence phosphorus cycling both directly, through excretion, and indirectly, through consumption of dreissenid mussels, whose high mass-specific phosphorus excretion enhances recycling. In 1999, when age-1+ round gobies reached peak abundance near 350 million (2.4 kg??ha-1), annual phosphorus excretion was estimated at 7 t (1.4 ?? 10-3 mg P??m-2??day -1). From an ecosystem perspective, however, round gobies excreted only 0.4% of the phosphorus needed by the benthic community for primary production. Indirectly, round gobies consumed <0.2% of dreissenid population biomass, indicating that round gobies did not reduce nutrient availability by consuming dreissenids. Compared with previous studies that have revealed introduced species to influence phosphorus cycling, round gobies likely did not attain a sufficiently high biomass density to influence phosphorus cycling in Lake Erie. ?? 2005 NRC Canada.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Canadian Journal of Fisheries and Aquatic Sciences","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1139/f04-172","issn":"0706652X","usgsCitation":"Bunnell, D., Johnson, T., and Knight, C., 2005, The impact of introduced round gobies (Neogobius melanostomus) on phosphorus cycling in central Lake Erie: Canadian Journal of Fisheries and Aquatic Sciences, v. 62, no. 1, p. 15-29, https://doi.org/10.1139/f04-172.","startPage":"15","endPage":"29","numberOfPages":"15","costCenters":[],"links":[{"id":209940,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1139/f04-172"},{"id":236701,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"62","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bace7e4b08c986b323824","contributors":{"authors":[{"text":"Bunnell, D.B.","contributorId":8610,"corporation":false,"usgs":true,"family":"Bunnell","given":"D.B.","affiliations":[],"preferred":false,"id":420879,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Johnson, T.B.","contributorId":21490,"corporation":false,"usgs":true,"family":"Johnson","given":"T.B.","email":"","affiliations":[],"preferred":false,"id":420880,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Knight, C.T.","contributorId":66042,"corporation":false,"usgs":true,"family":"Knight","given":"C.T.","email":"","affiliations":[],"preferred":false,"id":420881,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70031366,"text":"70031366 - 2005 - Blue tilapia (Oreochromis aureus) predation on fishes in the Muddy River system, Clark County, Nevada","interactions":[],"lastModifiedDate":"2016-05-12T15:24:17","indexId":"70031366","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3746,"text":"Western North American Naturalist","onlineIssn":"1944-8341","printIssn":"1527-0904","active":true,"publicationSubtype":{"id":10}},"title":"Blue tilapia (Oreochromis aureus) predation on fishes in the Muddy River system, Clark County, Nevada","docAbstract":"<p>Blue tilapia (Oreochromis aureus), native to North Africa and the Middle East (Courtenay and Robins 1973, Fuller et al. 1999), has been introduced around the world as a human food source, for vegetation control, and as a game fish (Costa-Pierce and Riedel 2000). Blue tilapia has been particularly successful in establishing and spreading in North American waters where it has been reported to change fish community structure and cause native fish decline (Courtenay and Robins 1973, Fuller et al. 1999). Because of these detrimental effects, it is now generally considered an unwelcome introduction into North American waters (Dill and Cordone 1997, Fuller et al. 1999).</p>","language":"English","issn":"15270904","usgsCitation":"Scoppettone, G., Salgado, J., and Nielsen, M., 2005, Blue tilapia (Oreochromis aureus) predation on fishes in the Muddy River system, Clark County, Nevada: Western North American Naturalist, v. 65, no. 3, p. 410-414.","productDescription":"5 p.","startPage":"410","endPage":"414","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":239721,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"65","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f1ece4b0c8380cd4aed5","contributors":{"authors":[{"text":"Scoppettone, G.G.","contributorId":22793,"corporation":false,"usgs":true,"family":"Scoppettone","given":"G.G.","email":"","affiliations":[],"preferred":false,"id":431214,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Salgado, J.A.","contributorId":15831,"corporation":false,"usgs":true,"family":"Salgado","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":431213,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Nielsen, M.B.","contributorId":9801,"corporation":false,"usgs":true,"family":"Nielsen","given":"M.B.","email":"","affiliations":[],"preferred":false,"id":431212,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70031715,"text":"70031715 - 2005 - Comparison of velocity-log data collected using impeller and electromagnetic flowmeters","interactions":[],"lastModifiedDate":"2025-05-14T15:08:57.231874","indexId":"70031715","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1861,"text":"Ground Water","active":true,"publicationSubtype":{"id":10}},"title":"Comparison of velocity-log data collected using impeller and electromagnetic flowmeters","docAbstract":"<p><span>Previous studies have used flowmeters in environments that are within the expectations of their published ranges. Electromagnetic flowmeters have a published range from 0.1 to 79.0 m/min, and impeller flowmeters have a published range from 1.2 to 61.0 m/min. Velocity-log data collected in five long-screened production wells in the Pleasant Valley area of southern California showed that (1) electromagnetic flowmeter results were comparable within ±2% to results obtained using an impeller flowmeter for comparable depths; (2) the measured velocities from the electromagnetic flowmeter were up to 36% greater than the published maximum range; and (3) both data sets, collected without the use of centralizers or flow diverters, produced comparable and interpretable results. Although either method is acceptable for measuring wellbore velocities and the distribution of flow, the electromagnetic flowmeter enables collection of data over a now greater range of flows. In addition, changes in fluid temperature and fluid resistivity, collected as part of the electromagnetic flowmeter log, are useful in the identification of flow and hydrogeologic interpretation.</span></p>","language":"English","publisher":"National Ground Water Association","doi":"10.1111/j.1745-6584.2005.0030.x","issn":"0017467X","usgsCitation":"Newhouse, M., Izbicki, J., and Smith, G., 2005, Comparison of velocity-log data collected using impeller and electromagnetic flowmeters: Ground Water, v. 43, no. 3, p. 434-438, https://doi.org/10.1111/j.1745-6584.2005.0030.x.","productDescription":"5 p.","startPage":"434","endPage":"438","numberOfPages":"5","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"links":[{"id":239774,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"43","issue":"3","noUsgsAuthors":false,"publicationDate":"2005-05-09","publicationStatus":"PW","scienceBaseUri":"5059f8bce4b0c8380cd4d270","contributors":{"authors":[{"text":"Newhouse, M.W.","contributorId":65892,"corporation":false,"usgs":true,"family":"Newhouse","given":"M.W.","email":"","affiliations":[],"preferred":false,"id":432819,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Izbicki, J. A. 0000-0003-0816-4408","orcid":"https://orcid.org/0000-0003-0816-4408","contributorId":28244,"corporation":false,"usgs":true,"family":"Izbicki","given":"J. A.","affiliations":[],"preferred":false,"id":432817,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Smith, G.A. 0000-0001-8170-9924","orcid":"https://orcid.org/0000-0001-8170-9924","contributorId":38350,"corporation":false,"usgs":true,"family":"Smith","given":"G.A.","email":"","affiliations":[],"preferred":false,"id":432818,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70029001,"text":"70029001 - 2005 - Performance of four turbulence closure models implemented using a generic length scale method","interactions":[],"lastModifiedDate":"2017-09-14T12:22:39","indexId":"70029001","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2925,"text":"Ocean Modelling","active":true,"publicationSubtype":{"id":10}},"title":"Performance of four turbulence closure models implemented using a generic length scale method","docAbstract":"<p>A two-equation turbulence model (one equation for turbulence kinetic energy and a second for a generic turbulence length-scale quantity) proposed by Umlauf and Burchard [J. Marine Research 61 (2003) 235] is implemented in a three-dimensional oceanographic model (Regional Oceanographic Modeling System; ROMS v2.0). These two equations, along with several stability functions, can represent many popular turbulence closures, including the k-kl (Mellor-Yamada Level 2.5), k-??, and k-?? schemes. The implementation adds flexibility to the model by providing an unprecedented range of turbulence closure selections in a single 3D oceanographic model and allows comparison and evaluation of turbulence models in an otherwise identical numerical environment. This also allows evaluation of the effect of turbulence models on other processes such as suspended-sediment distribution or ecological processes. Performance of the turbulence models and sediment-transport schemes is investigated with three test cases for (1) steady barotropic flow in a rectangular channel, (2) wind-induced surface mixed-layer deepening in a stratified fluid, and (3) oscillatory stratified pressure-gradient driven flow (estuarine circulation) in a rectangular channel. Results from k-??, k-??, and gen (a new closure proposed by Umlauf and Burchard [J. Marine Research 61 (2003) 235]) are very similar for these cases, but the k-kl closure results depend on a wall-proximity function that must be chosen to suit the flow. Greater variations appear in simulations of suspended-sediment concentrations than in salinity simulations because the transport of suspended-sediment amplifies minor variations in the methods. The amplification is caused by the added physics of a vertical settling rate, bottom stress dependent resuspension, and diffusive transport of sediment in regions of well mixed salt and temperature. Despite the amplified sensitivity of sediment to turbulence models in the estuary test case, the four closures investigated here all generated estuarine turbidity maxima that were similar in their shape, location, and concentrations.&nbsp;</p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.ocemod.2003.12.003","issn":"14635003","usgsCitation":"Warner, J., Sherwood, C.R., Arango, H., and Signell, R.P., 2005, Performance of four turbulence closure models implemented using a generic length scale method: Ocean Modelling, v. 8, no. 1-2, p. 81-113, https://doi.org/10.1016/j.ocemod.2003.12.003.","productDescription":"33 p.","startPage":"81","endPage":"113","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":236703,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"8","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a7688e4b0c8380cd78177","contributors":{"authors":[{"text":"Warner, J.C.","contributorId":46644,"corporation":false,"usgs":true,"family":"Warner","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":420892,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sherwood, C. R.","contributorId":48235,"corporation":false,"usgs":true,"family":"Sherwood","given":"C.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":420893,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Arango, H.G.","contributorId":103772,"corporation":false,"usgs":true,"family":"Arango","given":"H.G.","email":"","affiliations":[],"preferred":false,"id":420895,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Signell, R. P.","contributorId":89147,"corporation":false,"usgs":true,"family":"Signell","given":"R.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":420894,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70029018,"text":"70029018 - 2005 - Bedrock erosion surface beneath the rocky flats alluvial fan, Jefferson and Boulder counties, Colorado","interactions":[],"lastModifiedDate":"2012-03-12T17:21:00","indexId":"70029018","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2789,"text":"Mountain Geologist","active":true,"publicationSubtype":{"id":10}},"title":"Bedrock erosion surface beneath the rocky flats alluvial fan, Jefferson and Boulder counties, Colorado","docAbstract":"The early Pleistocene Rocky Flats alluvial fan formed at the mouth of unglaciated Coal Creek Canyon along the eastern flank of the Colorado Front Range. The fan consists of boulder, cobble, and pebble gravel deposited on an erosional surface cut on tilted Mesozoic sedimentary strata. A north-trending hogback of steeply dipping Cretaceous Laramie Formation and Fox Hills Sandstone is exposed through the gravel across the central portion of the fan. Elevations on the gravel-bedrock contact were used in a GIS to reconstruct the bedrock surface at the base of the gravel, providing a glimpse of the geomorphology of the early Pleistocene Colorado Piedmont. The reconstructed erosional bedrock surface portrays a landscape carved by a series of easterly flowing streams that eroded headward to the resistant hogback units, creating a bedrock step up to 37 m high. East-trending ridges on the bedrock surface are remnants of drainage divides between the Pleistocene streams. Water gaps in the bedrock step allowed the streams access to the upper surface of the step. This entire surface, except the hogback, was covered by gravel about 1.35 to 1.5 Ma ago. Subsequent erosion of the alluvial fan has been by headward (westward) erosion of easterly flowing streams incising into the eastern portion of the fan. Because the gravel is more resistant than the underlying bedrock, modern streams are established over the Pleistocene drainage divides, where the gravel was thinnest. Thicker gravel in the Pleistocene paleovalleys now caps modern drainage divides, producing an inverted topography.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Mountain Geologist","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"0027254X","usgsCitation":"Knepper, D.H., 2005, Bedrock erosion surface beneath the rocky flats alluvial fan, Jefferson and Boulder counties, Colorado: Mountain Geologist, v. 42, no. 1, p. 1-10.","startPage":"1","endPage":"10","numberOfPages":"10","costCenters":[],"links":[{"id":236280,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"42","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f04be4b0c8380cd4a6c9","contributors":{"authors":[{"text":"Knepper, D. H. Jr.","contributorId":106129,"corporation":false,"usgs":true,"family":"Knepper","given":"D.","suffix":"Jr.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":420984,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70027733,"text":"70027733 - 2005 - Uncertainty and research needs for supplementing wild populations of anadromous Pacific salmon","interactions":[],"lastModifiedDate":"2012-03-12T17:20:49","indexId":"70027733","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":718,"text":"American Fisheries Society Symposium","active":true,"publicationSubtype":{"id":10}},"title":"Uncertainty and research needs for supplementing wild populations of anadromous Pacific salmon","docAbstract":"Substantial disagreement and uncertainty attend the question of whether the benefits from supplementing wild populations of anadromous salmonids with hatchery fish outweigh the risks. Prudent decisions about supplementation are most likely when the suite of potential benefits and hazards and the various sources of uncertainty are explicitly identified. Models help by indicating the potential consequences of various levels of supplementation but perhaps are most valuable for showing the limitations of available data and helping design studies and monitoring to provide critical data. Information and understanding about the issue are deficient. I discuss various benefits, hazards, and associated uncertainties for supplementation, and implications for the design of monitoring and research. Several studies to reduce uncertainty and facilitate prudent supplementation are described and range from short-term reductionistic studies that help define the issue or help avoid deleterious consequences from supplementation to long-term studies (ca. 10 or more fish generations) that evaluate the net result of positive and negative genetic, behavioral, and ecological effects from supplementation.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"American Fisheries Society Symposium","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"08922284","usgsCitation":"Reisenbichler, R., 2005, Uncertainty and research needs for supplementing wild populations of anadromous Pacific salmon: American Fisheries Society Symposium, v. 2005, no. 44, p. 263-275.","startPage":"263","endPage":"275","numberOfPages":"13","costCenters":[],"links":[{"id":238241,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"2005","issue":"44","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bbc1fe4b08c986b328a43","contributors":{"authors":[{"text":"Reisenbichler, R.R.","contributorId":77356,"corporation":false,"usgs":true,"family":"Reisenbichler","given":"R.R.","email":"","affiliations":[],"preferred":false,"id":414985,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70027738,"text":"70027738 - 2005 - Ocean science: Radiocarbon variability in the western North Atlantic during the last deglaciation","interactions":[],"lastModifiedDate":"2012-03-12T17:20:49","indexId":"70027738","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Ocean science: Radiocarbon variability in the western North Atlantic during the last deglaciation","docAbstract":"We present a detailed history of glacial to Holocene radiocarbon in the deep western North Atlantic from deep-sea corals and paired benthic-planktonic foraminifera. The deglaciation is marked by switches between radiocarbon-enriched and -depleted waters, leading to large radiocarbon gradients in the water column. These changes played an important role in modulating atmospheric radiocarbon. The deep-ocean record supports the notion of a bipolar seesaw with increased Northern-source deep-water formation linked to Northern Hemisphere warming and the reverse. In contrast, the more frequent radiocarbon variations in the intermediate/deep ocean are associated with roughly synchronous changes at the poles.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Science","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1126/science.1114832","issn":"00368075","usgsCitation":"Robinson, L., Adkins, J., Keigwin, L., Southon, J., Fernandez, D.P., Wang, S., and Scheirer, D., 2005, Ocean science: Radiocarbon variability in the western North Atlantic during the last deglaciation: Science, v. 310, no. 5753, p. 1469-1473, https://doi.org/10.1126/science.1114832.","startPage":"1469","endPage":"1473","numberOfPages":"5","costCenters":[],"links":[{"id":211097,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1126/science.1114832"},{"id":238280,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"310","issue":"5753","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a6c94e4b0c8380cd74cd5","contributors":{"authors":[{"text":"Robinson, L.F.","contributorId":75256,"corporation":false,"usgs":true,"family":"Robinson","given":"L.F.","email":"","affiliations":[],"preferred":false,"id":415008,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Adkins, J.F.","contributorId":90857,"corporation":false,"usgs":true,"family":"Adkins","given":"J.F.","email":"","affiliations":[],"preferred":false,"id":415010,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Keigwin, L.D.","contributorId":27213,"corporation":false,"usgs":true,"family":"Keigwin","given":"L.D.","affiliations":[],"preferred":false,"id":415004,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Southon, J.","contributorId":88922,"corporation":false,"usgs":true,"family":"Southon","given":"J.","affiliations":[],"preferred":false,"id":415009,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Fernandez, D. P.","contributorId":45108,"corporation":false,"usgs":false,"family":"Fernandez","given":"D.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":415006,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Wang, S.-L.","contributorId":30031,"corporation":false,"usgs":true,"family":"Wang","given":"S.-L.","email":"","affiliations":[],"preferred":false,"id":415005,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Scheirer, D.S.","contributorId":49165,"corporation":false,"usgs":true,"family":"Scheirer","given":"D.S.","email":"","affiliations":[],"preferred":false,"id":415007,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70027728,"text":"70027728 - 2005 - An efficient algorithm for double-difference tomography and location in heterogeneous media, with an application to the Kilauea volcano","interactions":[],"lastModifiedDate":"2019-05-08T08:48:32","indexId":"70027728","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":"An efficient algorithm for double-difference tomography and location in heterogeneous media, with an application to the Kilauea volcano","docAbstract":"Improving our understanding of crustal processes requires a better knowledge of the geometry and the position of geological bodies. In this study we have designed a method based upon double-difference relocation and tomography to image, as accurately as possible, a heterogeneous medium containing seismogenic objects. Our approach consisted not only of incorporating double difference in tomography but also partly in revisiting tomographic schemes for choosing accurate and stable numerical strategies, adapted to the use of cross-spectral time delays. We used a finite difference solution to the eikonal equation for travel time computation and a Tarantola-Valette approach for both the classical and double-difference three-dimensional tomographic inversion to find accurate earthquake locations and seismic velocity estimates. We estimated efficiently the square root of the inverse model's covariance matrix in the case of a Gaussian correlation function. It allows the use of correlation length and a priori model variance criteria to determine the optimal solution. Double-difference relocation of similar earthquakes is performed in the optimal velocity model, making absolute and relative locations less biased by the velocity model. Double-difference tomography is achieved by using high-accuracy time delay measurements. These algorithms have been applied to earthquake data recorded in the vicinity of Kilauea and Mauna Loa volcanoes for imaging the volcanic structures. Stable and detailed velocity models are obtained: the regional tomography unambiguously highlights the structure of the island of Hawaii and the double-difference tomography shows a detailed image of the southern Kilauea caldera-upper east rift zone magmatic complex. Copyright 2005 by the American Geophysical Union.","language":"English","publisher":"AGU","doi":"10.1029/2004JB003466","issn":"01480227","usgsCitation":"Monteiller, V., Got, J., Virieux, J., and Okubo, P., 2005, An efficient algorithm for double-difference tomography and location in heterogeneous media, with an application to the Kilauea volcano: Journal of Geophysical Research B: Solid Earth, v. 110, no. 12, p. 1-22, https://doi.org/10.1029/2004JB003466.","productDescription":"22 p.","startPage":"1","endPage":"22","numberOfPages":"22","costCenters":[{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true}],"links":[{"id":477690,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1029/2004jb003466","text":"Publisher Index Page"},{"id":238140,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":211005,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1029/2004JB003466"}],"country":"United States","state":"Hawaii","otherGeospatial":"Kilauea volcano","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -155.3679656982422,\n              19.281980191903514\n            ],\n            [\n              -155.137939453125,\n              19.281980191903514\n            ],\n            [\n              -155.137939453125,\n              19.479539596600667\n            ],\n            [\n              -155.3679656982422,\n              19.479539596600667\n            ],\n            [\n              -155.3679656982422,\n              19.281980191903514\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"110","issue":"12","noUsgsAuthors":false,"publicationDate":"2005-12-16","publicationStatus":"PW","scienceBaseUri":"5059ea2fe4b0c8380cd486b4","contributors":{"authors":[{"text":"Monteiller, V.","contributorId":62409,"corporation":false,"usgs":true,"family":"Monteiller","given":"V.","email":"","affiliations":[],"preferred":false,"id":414968,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Got, J.-L.","contributorId":80867,"corporation":false,"usgs":true,"family":"Got","given":"J.-L.","email":"","affiliations":[],"preferred":false,"id":414969,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Virieux, J.","contributorId":10617,"corporation":false,"usgs":true,"family":"Virieux","given":"J.","email":"","affiliations":[],"preferred":false,"id":414966,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Okubo, P. 0000-0002-0381-6051","orcid":"https://orcid.org/0000-0002-0381-6051","contributorId":49432,"corporation":false,"usgs":true,"family":"Okubo","given":"P.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":false,"id":414967,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70027739,"text":"70027739 - 2005 - Part 1: Vadose-zone column studies of toluene (enhanced bioremediation) in a shallow unconfined aquifer","interactions":[],"lastModifiedDate":"2018-10-31T09:37:31","indexId":"70027739","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3728,"text":"Water, Air, & Soil Pollution","onlineIssn":"1573-2932","printIssn":"0049-6979","active":true,"publicationSubtype":{"id":10}},"title":"Part 1: Vadose-zone column studies of toluene (enhanced bioremediation) in a shallow unconfined aquifer","docAbstract":"<p class=\"Para\">The objectives of the laboratory study described in this paper were (1) to determine the effectiveness of four nutrient solutions and a control in stimulating the microbial degradation of toluene in the unsaturated zone as an alternative to bioremediation methodologies such as air sparging,<span>&nbsp;</span><i class=\"EmphasisTypeItalic \">in situ</i><span>&nbsp;</span>vitrification, or others (Part I), and (2) to compare the effectiveness of the addition of the most effective nutrient solution from Part I (modified Hoagland type, nitrate-rich) and hydrogen peroxide (H<sub>2</sub>O<sub>2</sub>) on microbial degradation of toluene for repeated, simulated spills in the unsaturated zone (Part II).</p><p class=\"Para\">For Part 1, fifteen columns (30-cm diameter by 150-cm height), packed with air-dried, 0.25-mm, medium-fine sand, were prepared to simulate shallow unconfined aquifer conditions. Toluene (10 mL) was added to the surface of each column, and soil solution and soil gas samples were collected from the columns every third day for 21 days. On day 21, a second application of toluene (10 mL) was made, and the experiment was run for another 21 days. Solution 4 was the most effective for microbial degradation in Part I. For Part II, three columns were designated nutrient-rich 3-day toluene columns and received toluene injections every 3 days; three columns were designated as nutrient-rich 7-day columns and received toluene injections every 7 days; and two columns were used as controls to which no nutrient was added.</p><p class=\"Para\">As measured by CO<sub>2</sub><span>&nbsp;</span>respiration, the initial benefits for aerobic organisms from the O<sub>2</sub>enhancement were sustained by the bacteria for only a short period of time (about 8 days). Degradation benefits from the nutrient solution were sustained throughout the experiment.</p><p class=\"Para\">The O<sub>2</sub><span>&nbsp;</span>and nutrient-enhanced columns degraded significantly more toluene than the control columns when simulating repeated spills onto the unsaturated zone, and demonstrated a potentially effective<span>&nbsp;</span><i class=\"EmphasisTypeItalic \">in situ</i><span>&nbsp;</span>bioremediation technology when used immediately or within days after a spill. The combined usage of H<sub>2</sub>O<sub>2</sub><span>&nbsp;</span>and nitrate-rich nutrients served to effectively maximize natural aerobic and anaerobic metabolic processes that biodegrade hydrocarbons in petroleum-contaminated media. Applications of this technology in the field may offer economical advantages to other, more intrusive abatement technologies.</p>","language":"English","publisher":"Springer","doi":"10.1007/s11270-005-1486-0","issn":"00496979","usgsCitation":"Tindall, J., Friedel, M., Szmajter, R., and Cuffin, S., 2005, Part 1: Vadose-zone column studies of toluene (enhanced bioremediation) in a shallow unconfined aquifer: Water, Air, & Soil Pollution, v. 168, no. 1-4, p. 325-357, https://doi.org/10.1007/s11270-005-1486-0.","productDescription":"33 p.","startPage":"325","endPage":"357","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":238312,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":211118,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/s11270-005-1486-0"}],"volume":"168","issue":"1-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a7518e4b0c8380cd779ae","contributors":{"authors":[{"text":"Tindall, J.A.","contributorId":25711,"corporation":false,"usgs":true,"family":"Tindall","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":415012,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Friedel, M.J.","contributorId":90823,"corporation":false,"usgs":true,"family":"Friedel","given":"M.J.","email":"","affiliations":[],"preferred":false,"id":415014,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Szmajter, R.J.","contributorId":87573,"corporation":false,"usgs":true,"family":"Szmajter","given":"R.J.","affiliations":[],"preferred":false,"id":415013,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Cuffin, S.M.","contributorId":6898,"corporation":false,"usgs":true,"family":"Cuffin","given":"S.M.","affiliations":[],"preferred":false,"id":415011,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70027656,"text":"70027656 - 2005 - Reproduction and mating behavior of the atlantic flyingfish, <i>Cheilopogon melanurus</i> (Exocoetidae), off North Carolina","interactions":[],"lastModifiedDate":"2017-04-26T15:37:36","indexId":"70027656","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1106,"text":"Bulletin of Marine Science","active":true,"publicationSubtype":{"id":10}},"title":"Reproduction and mating behavior of the atlantic flyingfish, <i>Cheilopogon melanurus</i> (Exocoetidae), off North Carolina","docAbstract":"<p><span>The reproductive biology of </span><i>Cheilopogon melanurus</i><span> (Valenciennes, 1847) was examined off North Carolina during the summers of 1991–1992 and 1999–2003. Specimens were collected using a small mesh neuston net and dip nets. A spawning event, the first observation of mating behavior for this species, was recorded off Cape Fear, North Carolina, on 19 August 2003. It was considered to be a spawning event due to: 1) unusual coloration of both sexes, 2) unusual swimming behavior of both sexes, and 3) ready release of gametes by both sexes upon capture. The spawning event occurred in the presence of small clumps of floating </span><i>Sargassum</i><span>, but the fish did not appear to use the algae. Over all collections, female gonadosomatic indices were highest in June and July, but mature females were collected each month (June, July, and August). The overall female to male sex ratio did not vary significantly from 1:1. Number of ova increased with increasing fish size, but the relationship was not strong. Our data indicate a spawning season of at least June through August off North Carolina due to high female gonadosomatic indices, large egg diameters, presence of egg filaments, presence of spent females in July and August, and presence of small juveniles (≤ 25 mm) in July and August. This is the first report of single pair spawning for this family; other species reportedly spawn in large aggregations.</span></p>","language":"English","publisher":"APT Online Publ.","issn":"00074977","usgsCitation":"Casazza, T.L., Ross, S., Necaise, A.M., and Sulak, K.J., 2005, Reproduction and mating behavior of the atlantic flyingfish, <i>Cheilopogon melanurus</i> (Exocoetidae), off North Carolina: Bulletin of Marine Science, v. 77, no. 3, p. 363-375.","productDescription":"13 p.","startPage":"363","endPage":"375","costCenters":[],"links":[{"id":238203,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":340479,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://www.ingentaconnect.com/contentone/umrsmas/bullmar/2005/00000077/00000003/art00003"}],"country":"United States","state":"North Carolina","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -75.882568359375,\n              35.55904339525896\n            ],\n            [\n              -76.17370605468749,\n              35.357696204467516\n            ],\n            [\n              -76.5802001953125,\n              35.12889434101051\n            ],\n            [\n              -76.83837890625,\n              34.76417891445512\n            ],\n            [\n              -76.761474609375,\n              34.52013562807766\n            ],\n            [\n              -76.5252685546875,\n              34.4069096565206\n            ],\n            [\n              -76.2945556640625,\n              34.511083202999714\n            ],\n            [\n              -75.6683349609375,\n              34.7506398050501\n            ],\n            [\n              -75.1959228515625,\n              35.232159412017154\n            ],\n            [\n              -75.21240234375,\n              35.38457160381764\n            ],\n            [\n              -75.3717041015625,\n              35.50092819950358\n            ],\n            [\n              -75.5804443359375,\n              35.6126508187567\n            ],\n            [\n              -75.69580078125,\n              35.61711648382185\n            ],\n            [\n              -75.882568359375,\n              35.55904339525896\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"77","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505aa892e4b0c8380cd859a0","contributors":{"authors":[{"text":"Casazza, Tara L.","contributorId":68453,"corporation":false,"usgs":true,"family":"Casazza","given":"Tara","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":414595,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ross, Steve W.","contributorId":41134,"corporation":false,"usgs":false,"family":"Ross","given":"Steve W.","affiliations":[{"id":32398,"text":"University of North Carolina Wilmington","active":true,"usgs":false}],"preferred":false,"id":414597,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Necaise, Ann Marie","contributorId":28062,"corporation":false,"usgs":true,"family":"Necaise","given":"Ann","email":"","middleInitial":"Marie","affiliations":[],"preferred":false,"id":414594,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Sulak, Kenneth J. 0000-0002-4795-9310 ksulak@usgs.gov","orcid":"https://orcid.org/0000-0002-4795-9310","contributorId":2217,"corporation":false,"usgs":true,"family":"Sulak","given":"Kenneth","email":"ksulak@usgs.gov","middleInitial":"J.","affiliations":[{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true},{"id":566,"text":"Southeast Ecological Science Center","active":true,"usgs":true}],"preferred":true,"id":414596,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70027655,"text":"70027655 - 2005 - Coseismic slip distribution of the 1923 Kanto earthquake, Japan","interactions":[],"lastModifiedDate":"2012-03-12T17:20:48","indexId":"70027655","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":"Coseismic slip distribution of the 1923 Kanto earthquake, Japan","docAbstract":"The slip distribution associated with the 1923 M = 7.9 Kanto, Japan, earthquake is reexamined in light of new data and modeling. We utilize a combination of first-order triangulation, second-order triangulation, and leveling data in order to constrain the coseismic deformation. The second-order triangulation data, which have not been utilized in previous studies of 1923 coseismic deformation, are associated with only slightly smaller errors than the first-order triangulation data and expand the available triangulation data set by about a factor of 10. Interpretation of these data in terms of uniform-slip models in a companion study by Nyst et al. shows that a model involving uniform coseismic slip on two distinct rupture planes explains the data very well and matches or exceeds the fit obtained by previous studies, even one which involved distributed slip. Using the geometry of the Nyst et al. two-plane slip model, we perform inversions of the same geodetic data set for distributed slip. Our preferred model of distributed slip on the Philippine Sea plate interface has a moment magnitude of 7.86. We find slip maxima of ???8-9 m beneath Odawara and ???7-8 m beneath the Miura peninsula, with a roughly 2:1 ratio of strike-slip to dip-slip motion, in agreement with a previous study. However, the Miura slip maximum is imaged as a more broadly extended feature in our study, with the high-slip region continuing from the Miura peninsula to the southern Boso peninsula region. The second-order triangulation data provide good evidence for ???3 m right-lateral strike slip on a 35-km-long splay structure occupying the volume between the upper surface of the descending Philippine Sea plate and the southern Boso peninsula. 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":"10.1029/2005JB003638","issn":"01480227","usgsCitation":"Pollitz, F., Nyst, M., Nishimura, T., and Thatcher, W., 2005, Coseismic slip distribution of the 1923 Kanto earthquake, Japan: Journal of Geophysical Research B: Solid Earth, v. 110, no. 11, p. 1-16, https://doi.org/10.1029/2005JB003638.","startPage":"1","endPage":"16","numberOfPages":"16","costCenters":[],"links":[{"id":211047,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1029/2005JB003638"},{"id":238202,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"110","issue":"11","noUsgsAuthors":false,"publicationDate":"2005-11-23","publicationStatus":"PW","scienceBaseUri":"5059fc5ce4b0c8380cd4e246","contributors":{"authors":[{"text":"Pollitz, F. F.","contributorId":108280,"corporation":false,"usgs":true,"family":"Pollitz","given":"F. F.","affiliations":[],"preferred":false,"id":414593,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nyst, M.","contributorId":66453,"corporation":false,"usgs":true,"family":"Nyst","given":"M.","email":"","affiliations":[],"preferred":false,"id":414591,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Nishimura, T.","contributorId":94834,"corporation":false,"usgs":true,"family":"Nishimura","given":"T.","email":"","affiliations":[],"preferred":false,"id":414592,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Thatcher, W.","contributorId":32669,"corporation":false,"usgs":true,"family":"Thatcher","given":"W.","email":"","affiliations":[],"preferred":false,"id":414590,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
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