{"pageNumber":"809","pageRowStart":"20200","pageSize":"25","recordCount":68927,"records":[{"id":70037206,"text":"70037206 - 2010 - Timing and duration of garnet granulite metamorphism in magmatic arc crust, Fiordland, New Zealand","interactions":[],"lastModifiedDate":"2012-03-12T17:22:07","indexId":"70037206","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1213,"text":"Chemical Geology","active":true,"publicationSubtype":{"id":10}},"title":"Timing and duration of garnet granulite metamorphism in magmatic arc crust, Fiordland, New Zealand","docAbstract":"Pembroke Granulite from Fiordland, New Zealand provides a window into the mid- to lower crust of magmatic arcs. Garnet Sm-Nd and zircon U-Pb ages constrain the timing and duration of high-P partial melting that produced trondhjemitic high Sr/Y magma. Trace element zoning in large, euhedral garnet is compatible with little post growth modification and supports the interpretation that garnet Sm-Nd ages of 126.1??2.0 and 122.6??2.0. Ma date crystal growth. Integration of the garnet ages with U-Pb zircon ages elucidates a history of intrusion(?) and a protracted period of high-temperature metamorphism and partial melting. The oldest zircon ages of 163 to 150. Ma reflect inheritance or intrusion and a cluster of zircon ages ca. 134. Ma date orthopyroxene-bearing mineral assemblages that may be magmatic or metamorphic in origin. Zircon and garnet ages from unmelted gneiss and garnet reaction zones record garnet granulite facies metamorphism at 128 to 126. Ma. Peritectic garnet and additional zircon ages from trondhjemite veins and garnet reaction zones indicate that garnet growth and partial melting lasted until ca. 123. Ma. Two single fraction garnet ages and young zircon ages suggest continued high-temperature re-equilibration until ca. 95. Ma. Phase diagram sections constrain orthopyroxene assemblages to <0.6 GPa @ 650??C, peak garnet granulite facies metamorphic conditions to 680-815??C @ 1.1-1.4. GPa, and a P-T path with a P increase of???0.5. GPa. These sections are compatible with water contents???0.28wt.%, local dehydration during garnet granulite metamorphism, and <0.3. GPa P increases during garnet growth. Results demonstrate the utility of integrated U-Pb zircon and Sm-Nd garnet ages, and phase diagram sections for understanding the nature, duration, and conditions of deep crustal metamorphism and melting. Geochronologic and thermobarometric data for garnet granulite indicate that thickening of arc crust, which caused high-pressure metamorphism in northern Fiordland, must have occurred prior to 126. Ma, that loading occurred at a rate of ca. 0.06. GPa/m.y., and that garnet granulite metamorphism lasted 3-7m.y. Locally-derived partial melts formed and crystallized in considerably less than 10 and perhaps as little as 3m.y. ?? 2010 Elsevier B.V.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Chemical Geology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.chemgeo.2010.02.015","issn":"00092541","usgsCitation":"Stowell, H., Tulloch, A., Zuluaga, C., and Koenig, A., 2010, Timing and duration of garnet granulite metamorphism in magmatic arc crust, Fiordland, New Zealand: Chemical Geology, v. 273, no. 1-2, p. 91-110, https://doi.org/10.1016/j.chemgeo.2010.02.015.","startPage":"91","endPage":"110","numberOfPages":"20","costCenters":[],"links":[{"id":244964,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":217053,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.chemgeo.2010.02.015"}],"volume":"273","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb3e4e4b08c986b326051","contributors":{"authors":[{"text":"Stowell, H.","contributorId":19409,"corporation":false,"usgs":true,"family":"Stowell","given":"H.","email":"","affiliations":[],"preferred":false,"id":459899,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tulloch, A.","contributorId":10645,"corporation":false,"usgs":true,"family":"Tulloch","given":"A.","email":"","affiliations":[],"preferred":false,"id":459898,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Zuluaga, C.","contributorId":37177,"corporation":false,"usgs":true,"family":"Zuluaga","given":"C.","email":"","affiliations":[],"preferred":false,"id":459900,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Koenig, A. 0000-0002-5230-0924","orcid":"https://orcid.org/0000-0002-5230-0924","contributorId":64037,"corporation":false,"usgs":true,"family":"Koenig","given":"A.","affiliations":[],"preferred":false,"id":459901,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70037228,"text":"70037228 - 2010 - Dramatic beach and nearshore morphological changes due to extreme flooding at a wave-dominated river mouth","interactions":[],"lastModifiedDate":"2013-05-02T14:42:27","indexId":"70037228","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2667,"text":"Marine Geology","active":true,"publicationSubtype":{"id":10}},"title":"Dramatic beach and nearshore morphological changes due to extreme flooding at a wave-dominated river mouth","docAbstract":"Record flooding on the Santa Clara River of California (USA) during January 2005 injected ∼ 5 million m<sup>3</sup> of littoral-grade sediment into the Santa Barbara Littoral Cell, approximately an order of magnitude more than both the average annual river loads and the average annual alongshore littoral transport in this portion of the cell. This event appears to be the largest sediment transport event on record for a Southern California river. Over 170 m of local shoreline (mean high water (MHW)) progradation was observed as a result of the flood, followed by 3 years of rapid local shoreline recession. During this post-flood stage, linear regression-determined shoreline change rates are up to −45 m a<sup>− 1</sup> on the subaerial beach (MHW) and − 114 m a<sup>− 1</sup> on the submarine delta (6 m isobath). Starting approximately 1 km downdrift of the river mouth, shoreline progradation persisted throughout the 3-year post-flood monitoring period, with rates up to + 19 m a<sup>− 1</sup>. Post-flood bathymetric surveys show nearshore (0 to 12 m depth) erosion on the delta exceeding 400 m<sup>3</sup>/m a<sup>− 1</sup>, more than an order of magnitude higher than mean seasonal cross-shore sediment transport rates in the region. Changes were not constant with depth, however; sediment accumulation and subsequent erosion on the delta were greatest at − 5 to − 8 m, and accretion in downdrift areas was greatest above –2 m. Thus, this research shows that the topographic bulge (or “wave”) of sediment exhibited both advective and diffusive changes with time, although there were significant variations in the rates of change with depth. The advection and diffusion of the shoreline position was adequately reproduced with a simple “one line” model, although these modeling techniques miss the important cross-shore variations observed in this area. This study illustrates the importance of understanding low-frequency, high volume coastal discharge events for understanding short- and long-term sediment supply, littoral transport, and beach and nearshore evolution in coastal systems adjacent to river mouths.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Marine Geology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","doi":"10.1016/j.margeo.2010.01.018","issn":"00253227","usgsCitation":"Barnard, P., and Warrick, J., 2010, Dramatic beach and nearshore morphological changes due to extreme flooding at a wave-dominated river mouth: Marine Geology, v. 271, no. 1-2, p. 131-148, https://doi.org/10.1016/j.margeo.2010.01.018.","productDescription":"18 p.","startPage":"131","endPage":"148","costCenters":[{"id":528,"text":"Pacific Science Center","active":false,"usgs":true}],"links":[{"id":217369,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.margeo.2010.01.018"},{"id":245314,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"271","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a03d4e4b0c8380cd50684","contributors":{"authors":[{"text":"Barnard, P.L.","contributorId":20527,"corporation":false,"usgs":true,"family":"Barnard","given":"P.L.","email":"","affiliations":[],"preferred":false,"id":459978,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Warrick, J.A.","contributorId":53503,"corporation":false,"usgs":true,"family":"Warrick","given":"J.A.","affiliations":[],"preferred":false,"id":459979,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70037230,"text":"70037230 - 2010 - Rate of formation and dissolution of mercury sulfide nanoparticles: The dual role of natural organic matter","interactions":[],"lastModifiedDate":"2013-03-19T15:33:09","indexId":"70037230","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","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":"Rate of formation and dissolution of mercury sulfide nanoparticles: The dual role of natural organic matter","docAbstract":"Mercury is a global contaminant of concern due to its transformation by microorganisms to form methylmercury, a toxic species that accumulates in biological tissues. The effect of dissolved organic matter (DOM) isolated from natural waters on reactions between mercury(II) (Hg) and sulfide (S(-II)) to form HgS<sub>(s)</sub> nanoparticles across a range of Hg and S(-II) concentrations was investigated. Hg was equilibrated with DOM, after which S(-II) was added. Dissolved Hg (Hg<sub>aq</sub>) was periodically quantified using ultracentrifugation and chemical analysis following the addition of S(-II). Particle size and identity were determined using dynamic light scattering and X-ray absorption spectroscopy. S(-II) reacts with Hg to form 20 to 200nm aggregates consisting of 1-2 nm HgS<sub>(s)</sub> subunits that are more structurally disordered than metacinnabar in the presence of 2 x 10<sup>-9</sup> to 8 x 10<sup>-6</sup>M Hg and 10 (mg C)L<sup>-1</sup> DOM. Some of the HgS(s) nanoparticle aggregates are subsequently dissolved by DOM and (re)precipitated by S(-II) over periods of hours to days. At least three fractions of Hg-DOM species were observed with respect to reactivity toward S(-II): 0.3 &mu;mol reactive Hg per mmol C (60 percent), 0.1 &mu;mol per mmol C (20 percent) that are kinetically hindered, and another 0.1 &mu;mol Hg per mmol C (20 percent) that are inert to reaction with S(-II). Following an initial S(-II)-driven precipitation of HgS<sub>(s)</sub>, HgS<sub>(s)</sub> was dissolved by DOM or organic sulfur compounds. HgS<sub>(s)</sub> formation during this second phase was counterintuitively favored by lower S(-II) concentrations, suggesting surface association of DOM moieties that are less capable of dissolving HgS<sub>(s)</sub>. DOM partially inhibits HgS(s) formation and mediates reactions between Hg and S(-II) such that HgS<sub>(s)</sub> is susceptible to dissolution. These findings indicate that Hg accessibility to microorganisms could be controlled by kinetic (intermediate) species in the presence of S(-II) and DOM, undermining the premise that equilibrium Hg species distributions should correlate to the extent or rate of Hg methylation in soils and sediments.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Geochimica et Cosmochimica Acta","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","publisherLocation":"Amsterdam, Netherlands","doi":"10.1016/j.gca.2010.05.012","issn":"00167037","usgsCitation":"Slowey, A.J., 2010, Rate of formation and dissolution of mercury sulfide nanoparticles: The dual role of natural organic matter: Geochimica et Cosmochimica Acta, v. 74, no. 16, p. 4693-4708, https://doi.org/10.1016/j.gca.2010.05.012.","startPage":"4693","endPage":"4708","numberOfPages":"16","additionalOnlineFiles":"N","costCenters":[{"id":148,"text":"Branch of Regional Research-Western Region","active":false,"usgs":true}],"links":[{"id":217400,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.gca.2010.05.012"},{"id":245346,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"74","issue":"16","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a9536e4b0c8380cd8188b","contributors":{"authors":[{"text":"Slowey, Aaron J.","contributorId":30706,"corporation":false,"usgs":true,"family":"Slowey","given":"Aaron","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":459984,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70037232,"text":"70037232 - 2010 - Radar image and data fusion for natural hazards characterisation","interactions":[],"lastModifiedDate":"2017-04-05T16:38:44","indexId":"70037232","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2052,"text":"International Journal of Image and Data Fusion","active":true,"publicationSubtype":{"id":10}},"title":"Radar image and data fusion for natural hazards characterisation","docAbstract":"Fusion of synthetic aperture radar (SAR) images through interferometric, polarimetric and tomographic processing provides an all - weather imaging capability to characterise and monitor various natural hazards. This article outlines interferometric synthetic aperture radar (InSAR) processing and products and their utility for natural hazards characterisation, provides an overview of the techniques and applications related to fusion of SAR/InSAR images with optical and other images and highlights the emerging SAR fusion technologies. In addition to providing precise land - surface digital elevation maps, SAR - derived imaging products can map millimetre - scale elevation changes driven by volcanic, seismic and hydrogeologic processes, by landslides and wildfires and other natural hazards. With products derived from the fusion of SAR and other images, scientists can monitor the progress of flooding, estimate water storage changes in wetlands for improved hydrological modelling predictions and assessments of future flood impacts and map vegetation structure on a global scale and monitor its changes due to such processes as fire, volcanic eruption and deforestation. With the availability of SAR images in near real - time from multiple satellites in the near future, the fusion of SAR images with other images and data is playing an increasingly important role in understanding and forecasting natural hazards.","language":"English","publisher":"Taylor & Francis","doi":"10.1080/19479832.2010.499219","issn":"19479832","usgsCitation":"Lu, Z., Dzurisin, D., Jung, H., Zhang, J., and Zhang, Y., 2010, Radar image and data fusion for natural hazards characterisation: International Journal of Image and Data Fusion, v. 1, no. 3, p. 217-242, https://doi.org/10.1080/19479832.2010.499219.","productDescription":"26 p.","startPage":"217","endPage":"242","numberOfPages":"26","costCenters":[{"id":157,"text":"Cascades Volcano Observatory","active":false,"usgs":true},{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":245376,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":217429,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1080/19479832.2010.499219"}],"volume":"1","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a9383e4b0c8380cd80e78","contributors":{"authors":[{"text":"Lu, Zhong 0000-0001-9181-1818 lu@usgs.gov","orcid":"https://orcid.org/0000-0001-9181-1818","contributorId":901,"corporation":false,"usgs":true,"family":"Lu","given":"Zhong","email":"lu@usgs.gov","affiliations":[],"preferred":true,"id":459988,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dzurisin, Daniel 0000-0002-0138-5067 dzurisin@usgs.gov","orcid":"https://orcid.org/0000-0002-0138-5067","contributorId":538,"corporation":false,"usgs":true,"family":"Dzurisin","given":"Daniel","email":"dzurisin@usgs.gov","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":459987,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Jung, Hyung-Sup","contributorId":58382,"corporation":false,"usgs":true,"family":"Jung","given":"Hyung-Sup","email":"","affiliations":[],"preferred":false,"id":459990,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Zhang, Jixian","contributorId":36396,"corporation":false,"usgs":true,"family":"Zhang","given":"Jixian","affiliations":[],"preferred":false,"id":459989,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Zhang, Yonghong","contributorId":82563,"corporation":false,"usgs":true,"family":"Zhang","given":"Yonghong","email":"","affiliations":[],"preferred":false,"id":459991,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70037234,"text":"70037234 - 2010 - Antidepressant pharmaceuticals in two U.S. effluent-impacted streams: Occurrence and fate in water and sediment and selective uptake in fish neural tissue","interactions":[],"lastModifiedDate":"2018-10-10T12:20:34","indexId":"70037234","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1565,"text":"Environmental Science & Technology","onlineIssn":"1520-5851","printIssn":"0013-936X","active":true,"publicationSubtype":{"id":10}},"title":"Antidepressant pharmaceuticals in two U.S. effluent-impacted streams: Occurrence and fate in water and sediment and selective uptake in fish neural tissue","docAbstract":"<p>Antidepressant pharmaceuticals are widely prescribed in the United States; release of municipal wastewater effluent is a primary route introducing them to aquatic environments, where little is known about their distribution and fate. Water, bed sediment, and brain tissue from native white suckers (Catostomus commersoni)were collected upstream and atpoints progressively downstream from outfalls discharging to two effluentimpacted streams, Boulder Creek (Colorado) and Fourmile Creek (Iowa). A liquid chromatography/tandem mass spectrometry method was used to quantify antidepressants, including fluoxetine, norfluoxetine (degradate), sertraline, norsertraline (degradate), paroxetine, Citalopram, fluvoxamine, duloxetine, venlafaxine, and bupropion in all three sample matrices. Antidepressants were not present above the limit of quantitation in water samples upstream from the effluent outfalls but were present at points downstream at ng/L concentrations, even at the farthest downstream sampling site 8.4 km downstream from the outfall. The antidepressants with the highest measured concentrations in both streams were venlafaxine, bupropion, and Citalopram and typically were observed at concentrations of at least an order of magnitude greater than the more commonly investigated antidepressants fluoxetine and sertraline. Concentrations of antidepressants in bed sediment were measured at ng/g levels; venlafaxine and fluoxetine were the predominant chemicals observed. Fluoxetine, sertraline, and their degradates were the principal antidepressants observed in fish brain tissue, typically at low ng/g concentrations. Aqualitatively different antidepressant profile was observed in brain tissue compared to streamwater samples. This study documents that wastewater effluent can be a point source of antidepressants to stream ecosystems and that the qualitative composition of antidepressants in brain tissue from exposed fish differs substantially from the compositions observed in streamwater and sediment, suggesting selective uptake.</p>","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Environmental Science and Technology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"American Chemical Society","doi":"10.1021/es9022706","issn":"0013936X","usgsCitation":"Schultz, M., Furlong, E.T., Kolpin, D.W., Werner, S.L., Schoenfuss, H., Barber, L.B., Blazer, V., Norris, D., and Vajda, A., 2010, Antidepressant pharmaceuticals in two U.S. effluent-impacted streams: Occurrence and fate in water and sediment and selective uptake in fish neural tissue: Environmental Science & Technology, v. 44, no. 6, p. 1918-1925, https://doi.org/10.1021/es9022706.","productDescription":"8 p.","startPage":"1918","endPage":"1925","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":244904,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":216997,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1021/es9022706"}],"country":"United States","state":"Colorado, Iowa","volume":"44","issue":"6","noUsgsAuthors":false,"publicationDate":"2010-02-01","publicationStatus":"PW","scienceBaseUri":"5059ec62e4b0c8380cd4923f","contributors":{"authors":[{"text":"Schultz, M.M.","contributorId":18993,"corporation":false,"usgs":true,"family":"Schultz","given":"M.M.","email":"","affiliations":[],"preferred":false,"id":459998,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Furlong, Edward T. 0000-0002-7305-4603 efurlong@usgs.gov","orcid":"https://orcid.org/0000-0002-7305-4603","contributorId":740,"corporation":false,"usgs":true,"family":"Furlong","given":"Edward","email":"efurlong@usgs.gov","middleInitial":"T.","affiliations":[{"id":503,"text":"Office of Water Quality","active":true,"usgs":true},{"id":191,"text":"Colorado Water Science Center","active":true,"usgs":true},{"id":5046,"text":"Branch of Analytical Serv (NWQL)","active":true,"usgs":true},{"id":27111,"text":"National Water Quality Program","active":true,"usgs":true}],"preferred":true,"id":460005,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kolpin, Dana W. 0000-0002-3529-6505 dwkolpin@usgs.gov","orcid":"https://orcid.org/0000-0002-3529-6505","contributorId":1239,"corporation":false,"usgs":true,"family":"Kolpin","given":"Dana","email":"dwkolpin@usgs.gov","middleInitial":"W.","affiliations":[{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true}],"preferred":true,"id":460004,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Werner, Stephen L. slwerner@usgs.gov","contributorId":1199,"corporation":false,"usgs":true,"family":"Werner","given":"Stephen","email":"slwerner@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":true,"id":460003,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Schoenfuss, H.L.","contributorId":103877,"corporation":false,"usgs":true,"family":"Schoenfuss","given":"H.L.","affiliations":[],"preferred":false,"id":460006,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Barber, Larry B. 0000-0002-0561-0831 lbbarber@usgs.gov","orcid":"https://orcid.org/0000-0002-0561-0831","contributorId":921,"corporation":false,"usgs":true,"family":"Barber","given":"Larry","email":"lbbarber@usgs.gov","middleInitial":"B.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true},{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":460002,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Blazer, Vicki S. 0000-0001-6647-9614 vblazer@usgs.gov","orcid":"https://orcid.org/0000-0001-6647-9614","contributorId":150384,"corporation":false,"usgs":true,"family":"Blazer","given":"Vicki S.","email":"vblazer@usgs.gov","affiliations":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"preferred":true,"id":460000,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Norris, D.O.","contributorId":58475,"corporation":false,"usgs":true,"family":"Norris","given":"D.O.","email":"","affiliations":[],"preferred":false,"id":460001,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Vajda, A.M.","contributorId":35961,"corporation":false,"usgs":true,"family":"Vajda","given":"A.M.","affiliations":[],"preferred":false,"id":459999,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}}
,{"id":70037237,"text":"70037237 - 2010 - Applying the silver-tube introduction method for thermal conversion elemental analyses and a new δ<sup>2</sup>H value for NBS 22 oil","interactions":[],"lastModifiedDate":"2013-04-14T13:16:10","indexId":"70037237","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3233,"text":"Rapid Communications in Mass Spectrometry","active":true,"publicationSubtype":{"id":10}},"title":"Applying the silver-tube introduction method for thermal conversion elemental analyses and a new δ<sup>2</sup>H value for NBS 22 oil","docAbstract":"The δ<sup>2</sup>H<sub>VSMOW–SLAP</sub> value of total hydrogen of the international measurement standard NBS 22 oil was determined by a new method of sealing water in silver tubes for use in a thermal conversion elemental analysis (TC/EA) reduction unit. The isotopic fractionation of water due to evaporation is virtually non-existent in this silver-tube method. A new value for the δ<sup>2</sup>H<sub>VSMOW–SLAP</sub> of NBS 22 oil, calibrated with isotopic reference waters, was determined to be −116.9 ± 0.8‰ (1σ and n = 31).","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Rapid Communications in Mass Spectrometry","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Wiley","publisherLocation":"Hoboken, NJ","doi":"10.1002/rcm.4638","issn":"09514198","usgsCitation":"Coplen, T.B., and Qi, H., 2010, Applying the silver-tube introduction method for thermal conversion elemental analyses and a new δ<sup>2</sup>H value for NBS 22 oil: Rapid Communications in Mass Spectrometry, v. 24, no. 15, p. 2269-2276, https://doi.org/10.1002/rcm.4638.","productDescription":"8 p.","startPage":"2269","endPage":"2276","costCenters":[],"links":[{"id":217025,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1002/rcm.4638"},{"id":244936,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"24","issue":"15","noUsgsAuthors":false,"publicationDate":"2010-07-13","publicationStatus":"PW","scienceBaseUri":"5059ecd1e4b0c8380cd494ef","contributors":{"authors":[{"text":"Coplen, Tyler B. 0000-0003-4884-6008 tbcoplen@usgs.gov","orcid":"https://orcid.org/0000-0003-4884-6008","contributorId":508,"corporation":false,"usgs":true,"family":"Coplen","given":"Tyler","email":"tbcoplen@usgs.gov","middleInitial":"B.","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true},{"id":37464,"text":"WMA - Laboratory & Analytical Services Division","active":true,"usgs":true},{"id":27111,"text":"National Water Quality Program","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":true,"id":460015,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Qi, Haiping 0000-0002-8339-744X haipingq@usgs.gov","orcid":"https://orcid.org/0000-0002-8339-744X","contributorId":507,"corporation":false,"usgs":true,"family":"Qi","given":"Haiping","email":"haipingq@usgs.gov","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":460014,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70037253,"text":"70037253 - 2010 - Characterization of pyroclastic deposits and pre-eruptive soils following the 2008 eruption of Kasatochi Island Volcano, Alaska","interactions":[],"lastModifiedDate":"2012-03-12T17:22:11","indexId":"70037253","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":899,"text":"Arctic, Antarctic, and Alpine Research","active":true,"publicationSubtype":{"id":10}},"title":"Characterization of pyroclastic deposits and pre-eruptive soils following the 2008 eruption of Kasatochi Island Volcano, Alaska","docAbstract":"The 78 August 2008 eruption of Kasatochi Island volcano blanketed the island in newly generated pyroclastic deposits and deposited ash into the ocean and onto nearby islands. Concentrations of water soluble Fe, Cu, and Zn determined from a 1:20 deionized water leachate of the ash were sufficient to provide short-term fertilization of the surface ocean. The 2008 pyroclastic deposits were thicker in concavities at bases of steeper slopes and thinner on steep slopes and ridge crests. By summer 2009, secondary erosion had exposed the pre-eruption soils along gulley walls and in gully bottoms on the southern and eastern slopes, respectively. Topographic and microtopographic position altered the depositional patterns of the pyroclastic flows and resulted in pre-eruption soils being buried by as little as 1 m of ash. The different erosion patterns gave rise to three surfaces on which future ecosystems will likely develop: largely pre-eruptive soils; fresh pyroclastic deposits influenced by shallowly buried, pre-eruptive soil; and thick (>1 m) pyroclastic deposits. As expected, the chemical composition differed between the pyroclastic deposits and the pre-eruptive soils. Pre-eruptive soils hold stocks of C and N important for establishing biota that are lacking in the fresh pyroclastic deposits. The pyroclastic deposits are a source for P and K but have negligible nutrient holding capacity, making these elements vulnerable to leaching loss. Consequently, the pre-eruption soils may also represent an important long-term P and K source. ?? 2010 Regents of the University of Colorado.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Arctic, Antarctic, and Alpine Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1657/1938-4246-42.3.276","issn":"15230430","usgsCitation":"Wang, B., Michaelson, G., Ping, C., Plumlee, G., and Hageman, P., 2010, Characterization of pyroclastic deposits and pre-eruptive soils following the 2008 eruption of Kasatochi Island Volcano, Alaska: Arctic, Antarctic, and Alpine Research, v. 42, no. 3, p. 276-284, https://doi.org/10.1657/1938-4246-42.3.276.","startPage":"276","endPage":"284","numberOfPages":"9","costCenters":[],"links":[{"id":475836,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1657/1938-4246-42.3.276","text":"Publisher Index Page"},{"id":245221,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":217286,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1657/1938-4246-42.3.276"}],"volume":"42","issue":"3","noUsgsAuthors":false,"publicationDate":"2018-01-17","publicationStatus":"PW","scienceBaseUri":"5059f4d6e4b0c8380cd4bf5d","contributors":{"authors":[{"text":"Wang, B.","contributorId":29011,"corporation":false,"usgs":true,"family":"Wang","given":"B.","email":"","affiliations":[],"preferred":false,"id":460100,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Michaelson, G.","contributorId":30851,"corporation":false,"usgs":true,"family":"Michaelson","given":"G.","affiliations":[],"preferred":false,"id":460101,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ping, C.-L.","contributorId":60843,"corporation":false,"usgs":true,"family":"Ping","given":"C.-L.","email":"","affiliations":[],"preferred":false,"id":460103,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Plumlee, G.","contributorId":58124,"corporation":false,"usgs":true,"family":"Plumlee","given":"G.","email":"","affiliations":[],"preferred":false,"id":460102,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Hageman, P. 0000-0002-3440-2150","orcid":"https://orcid.org/0000-0002-3440-2150","contributorId":92521,"corporation":false,"usgs":true,"family":"Hageman","given":"P.","affiliations":[],"preferred":false,"id":460104,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70037258,"text":"70037258 - 2010 - Identifying sources of stream water sulfate after a summer drought in the Sleepers River watershed (Vermont, USA) using hydrological, chemical, and isotopic techniques","interactions":[],"lastModifiedDate":"2012-03-12T17:22:11","indexId":"70037258","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":835,"text":"Applied Geochemistry","active":true,"publicationSubtype":{"id":10}},"title":"Identifying sources of stream water sulfate after a summer drought in the Sleepers River watershed (Vermont, USA) using hydrological, chemical, and isotopic techniques","docAbstract":"In many forested headwater catchments, peak SO<sub>4</sub><sup>2 -</sup> concentrations in stream water occur in the late summer or fall following drought potentially resulting in episodic stream acidification. The sources of highly elevated stream water SO<sub>4</sub><sup>2 -</sup> concentrations were investigated in a first order stream at the Sleepers River watershed (Vermont, USA) after the particularly dry summer of 2001 using a combination of hydrological, chemical and isotopic approaches. Throughout the summer of 2001 SO<sub>4</sub><sup>2 -</sup> concentrations in stream water doubled from ???130 to 270 ??eq/L while flows decreased. Simultaneously increasing Na<sup>+</sup> and Ca<sup>2+</sup> concentrations and ??<sup>34</sup>S values increasing from +7??? towards those of bedrock S (???+10.5???) indicated that chemical weathering involving hydrolysis of silicates and oxidation of sulfide minerals in schists and phyllites was the cause for the initial increase in SO<sub>4</sub><sup>2 -</sup> concentrations. During re-wetting of the watershed in late September and early October of 2001, increasing stream flows were accompanied by decreasing Na<sup>+</sup> and Ca<sup>2+</sup> concentrations, but SO<sub>4</sub><sup>2 -</sup> concentrations continued to increase up to 568 ??eq/L, indicating that a major source of SO<sub>4</sub><sup>2 -</sup> in addition to bedrock weathering contributed to peak SO<sub>4</sub><sup>2 -</sup> concentrations. The further increase in SO<sub>4</sub><sup>2 -</sup> concentrations coincided with an abrupt decrease of ??<sup>34</sup>S values in stream water SO<sub>4</sub><sup>2 -</sup> from maximum values near +10??? to minimum values near -3???. Soil investigations revealed that some C-horizons in the Spodsols of the watershed contained secondary sulfide minerals with ??<sup>34</sup>S values near -22???. The shift to negative ??<sup>34</sup>S values of stream water SO<sub>4</sub><sup>2 -</sup> indicates that secondary sulfides in C-horizons were oxidized to SO<sub>4</sub><sup>2 -</sup> during the particularly dry summer of 2001. The newly formed SO<sub>4</sub><sup>2 -</sup> was transported to the streams during re-wetting of the watershed contributing ???60% of the SO<sub>4</sub><sup>2 -</sup> during peak concentrations in the stream water. Thereafter, the contribution of SO<sub>4</sub><sup>2 -</sup> from oxidation of secondary sulfides in C-horizons decreased rapidly and pedogenic SO<sub>4</sub><sup>2 -</sup> reemerged as a dominant SO<sub>4</sub><sup>2 -</sup> source in concert with decreasing SO<sub>4</sub><sup>2 -</sup> concentrations in spring of 2002. The study provides evidence that a quantitative assessment of the sources of stream water SO<sub>4</sub><sup>2 -</sup> in forested watersheds is possible by combining hydrological, chemical and isotopic techniques, provided that the isotopic compositions of all potential SO<sub>4</sub><sup>2 -</sup> sources are distinctly different. ?? 2010 Elsevier Ltd.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Applied Geochemistry","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.apgeochem.2010.02.007","issn":"08832927","usgsCitation":"Mayer, B., Shanley, J.B., Bailey, S., and Mitchell, M., 2010, Identifying sources of stream water sulfate after a summer drought in the Sleepers River watershed (Vermont, USA) using hydrological, chemical, and isotopic techniques: Applied Geochemistry, v. 25, no. 5, p. 747-754, https://doi.org/10.1016/j.apgeochem.2010.02.007.","startPage":"747","endPage":"754","numberOfPages":"8","costCenters":[],"links":[{"id":217371,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.apgeochem.2010.02.007"},{"id":245316,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"25","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3857e4b0c8380cd6152e","contributors":{"authors":[{"text":"Mayer, B.","contributorId":84538,"corporation":false,"usgs":true,"family":"Mayer","given":"B.","email":"","affiliations":[],"preferred":false,"id":460123,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Shanley, J. B.","contributorId":52226,"corporation":false,"usgs":true,"family":"Shanley","given":"J.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":460121,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bailey, S.W.","contributorId":29113,"corporation":false,"usgs":true,"family":"Bailey","given":"S.W.","email":"","affiliations":[],"preferred":false,"id":460120,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Mitchell, M.J.","contributorId":72940,"corporation":false,"usgs":true,"family":"Mitchell","given":"M.J.","email":"","affiliations":[],"preferred":false,"id":460122,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70037261,"text":"70037261 - 2010 - Evolution of a natural debris flow: In situ measurements of flow dynamics, video imagery, and terrestrial laser scanning","interactions":[],"lastModifiedDate":"2012-03-12T17:22:11","indexId":"70037261","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1796,"text":"Geology","active":true,"publicationSubtype":{"id":10}},"title":"Evolution of a natural debris flow: In situ measurements of flow dynamics, video imagery, and terrestrial laser scanning","docAbstract":"Many theoretical and laboratory studies have been undertaken to understand debris-flow processes and their associated hazards. However, complete and quantitative data sets from natural debris flows needed for confirmation of these results are limited. We used a novel combination of in situ measurements of debris-flow dynamics, video imagery, and pre- and postflow 2-cm-resolution digital terrain models to study a natural debris-flow event. Our field data constrain the initial and final reach morphology and key flow dynamics. The observed event consisted of multiple surges, each with clear variation of flow properties along the length of the surge. Steep, highly resistant, surge fronts of coarse-grained material without measurable pore-fluid pressure were pushed along by relatively fine-grained and water-rich tails that had a wide range of pore-fluid pressures (some two times greater than hydrostatic). Surges with larger nonequilibrium pore-fluid pressures had longer travel distances. A wide range of travel distances from different surges of similar size indicates that dynamic flow properties are of equal or greater importance than channel properties in determining where a particular surge will stop. Progressive vertical accretion of multiple surges generated the total thickness of mapped debris-flow deposits; nevertheless, deposits had massive, vertically unstratified sedimentological textures. ?? 2010 Geological Society of America.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Geology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1130/G30928.1","issn":"00917613","usgsCitation":"McCoy, S., Kean, J., Coe, J.A., Staley, D., Wasklewicz, T., and Tucker, G., 2010, Evolution of a natural debris flow: In situ measurements of flow dynamics, video imagery, and terrestrial laser scanning: Geology, v. 38, no. 8, p. 735-738, https://doi.org/10.1130/G30928.1.","startPage":"735","endPage":"738","numberOfPages":"4","costCenters":[],"links":[{"id":245349,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":217403,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1130/G30928.1"}],"volume":"38","issue":"8","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0d7ce4b0c8380cd5304a","contributors":{"authors":[{"text":"McCoy, S.W.","contributorId":74608,"corporation":false,"usgs":true,"family":"McCoy","given":"S.W.","affiliations":[],"preferred":false,"id":460139,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kean, J. W. 0000-0003-3089-0369","orcid":"https://orcid.org/0000-0003-3089-0369","contributorId":71679,"corporation":false,"usgs":true,"family":"Kean","given":"J. W.","affiliations":[],"preferred":false,"id":460138,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Coe, J. A.","contributorId":8867,"corporation":false,"usgs":true,"family":"Coe","given":"J.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":460135,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Staley, D.M.","contributorId":17851,"corporation":false,"usgs":true,"family":"Staley","given":"D.M.","email":"","affiliations":[],"preferred":false,"id":460136,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Wasklewicz, T.A.","contributorId":64922,"corporation":false,"usgs":true,"family":"Wasklewicz","given":"T.A.","affiliations":[],"preferred":false,"id":460137,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Tucker, G.E.","contributorId":102992,"corporation":false,"usgs":true,"family":"Tucker","given":"G.E.","affiliations":[],"preferred":false,"id":460140,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70037268,"text":"70037268 - 2010 - Migration of waterfowl in the east asian flyway and spatial relationship to HPAI H5N1 outbreaks","interactions":[],"lastModifiedDate":"2018-05-06T11:42:10","indexId":"70037268","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":948,"text":"Avian Diseases","active":true,"publicationSubtype":{"id":10}},"title":"Migration of waterfowl in the east asian flyway and spatial relationship to HPAI H5N1 outbreaks","docAbstract":"<p>Poyang Lake is situated within the East Asian Flyway, a migratory corridor for waterfowl that also encompasses Guangdong Province, China, the epicenter of highly pathogenic avian influenza (HPAI) H5N1. The lake is the largest freshwater body in China and a significant congregation site for waterfowl; however, surrounding rice fields and poultry grazing have created an overlap with wild waterbirds, a situation conducive to avian influenza transmission. Reports of HPAI H5N1 in healthy wild ducks at Poyang Lake have raised concerns about the potential of resilient free-ranging birds to disseminate the virus. Yet the role wild ducks play in connecting regions of HPAI H5N1 outbreak in Asia is hindered by a lack of information about their migratory ecology. During 2007-08 we marked wild ducks at Poyang Lake with satellite transmitters to examine the location and timing of spring migration and identify any spatiotemporal relationship with HPAI H5N1 outbreaks. Species included the Eurasian wigeon (<i>Anas penelope</i>), northern pintail (<i>Anas acuta</i>), common teal (<i>Anas crecca</i>), falcated teal (<i>Anas falcata</i>), Baikal teal (<i>Anas formosa</i>), mallard (<i>Anas platyrhynchos</i>), garganey (<i>Anas querquedula</i>), and Chinese spotbill (<i>Anas poecilohyncha</i>). These wild ducks (excluding the resident mallard and Chinese spotbill ducks) followed the East Asian Flyway along the coast to breeding areas in northern China, eastern Mongolia, and eastern Russia. None migrated west toward Qinghai Lake (site of the largest wild bird epizootic), thus failing to demonstrate any migratory connection to the Central Asian Flyway. A newly developed Brownian bridge spatial analysis indicated that HPAI H5N1 outbreaks reported in the flyway were related to latitude and poultry density but not to the core migration corridor or to wetland habitats. Also, we found a temporal mismatch between timing of outbreaks and wild duck movements. These analyses depend on complete or representative reporting of outbreaks, but by documenting movements of wild waterfowl, we present ecological knowledge that better informs epidemiological investigations seeking to explain and predict the spread of avian influenza viruses. ?? 2010 American Association of Avian Pathologists.</p>","publisher":"American Association of Avian Pathologists","doi":"10.1637/8914-043009-Reg.1","issn":"00052086","usgsCitation":"Takekawa, J.Y., Newman, S.H., Xiao, X., Prosser, D., Spragens, K., Palm, E., Yan, B., Li, T., Lei, F., Zhao, D., Douglas, D., Muzaffar, S., and Ji, W., 2010, Migration of waterfowl in the east asian flyway and spatial relationship to HPAI H5N1 outbreaks: Avian Diseases, v. 54, no. S1, p. 466-476, https://doi.org/10.1637/8914-043009-Reg.1.","productDescription":"11 p.","startPage":"466","endPage":"476","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":475834,"rank":1,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://www.ncbi.nlm.nih.gov/pmc/articles/4878034","text":"External Repository"},{"id":244967,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"54","issue":"S1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a5711e4b0c8380cd6da25","contributors":{"authors":[{"text":"Takekawa, John Y. 0000-0003-0217-5907 john_takekawa@usgs.gov","orcid":"https://orcid.org/0000-0003-0217-5907","contributorId":176168,"corporation":false,"usgs":true,"family":"Takekawa","given":"John","email":"john_takekawa@usgs.gov","middleInitial":"Y.","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":false,"id":460185,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Newman, S. H.","contributorId":21888,"corporation":false,"usgs":false,"family":"Newman","given":"S.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":460179,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Xiao, X.","contributorId":82869,"corporation":false,"usgs":true,"family":"Xiao","given":"X.","email":"","affiliations":[],"preferred":false,"id":460187,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Prosser, D.J. 0000-0002-5251-1799","orcid":"https://orcid.org/0000-0002-5251-1799","contributorId":65185,"corporation":false,"usgs":true,"family":"Prosser","given":"D.J.","affiliations":[],"preferred":false,"id":460186,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Spragens, K.A.","contributorId":38372,"corporation":false,"usgs":true,"family":"Spragens","given":"K.A.","affiliations":[],"preferred":false,"id":460181,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Palm, E.C.","contributorId":40708,"corporation":false,"usgs":true,"family":"Palm","given":"E.C.","email":"","affiliations":[],"preferred":false,"id":460183,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Yan, B.","contributorId":11739,"corporation":false,"usgs":true,"family":"Yan","given":"B.","email":"","affiliations":[],"preferred":false,"id":460177,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Li, T.","contributorId":84993,"corporation":false,"usgs":true,"family":"Li","given":"T.","email":"","affiliations":[],"preferred":false,"id":460188,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Lei, F.","contributorId":85413,"corporation":false,"usgs":true,"family":"Lei","given":"F.","email":"","affiliations":[],"preferred":false,"id":460189,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Zhao, D.","contributorId":28834,"corporation":false,"usgs":true,"family":"Zhao","given":"D.","email":"","affiliations":[],"preferred":false,"id":460180,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Douglas, David C. 0000-0003-0186-1104 ddouglas@usgs.gov","orcid":"https://orcid.org/0000-0003-0186-1104","contributorId":150115,"corporation":false,"usgs":true,"family":"Douglas","given":"David C.","email":"ddouglas@usgs.gov","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":460178,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Muzaffar, S.B.","contributorId":55561,"corporation":false,"usgs":true,"family":"Muzaffar","given":"S.B.","affiliations":[],"preferred":false,"id":460184,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Ji, W.","contributorId":40381,"corporation":false,"usgs":true,"family":"Ji","given":"W.","email":"","affiliations":[],"preferred":false,"id":460182,"contributorType":{"id":1,"text":"Authors"},"rank":13}]}}
,{"id":70037286,"text":"70037286 - 2010 - Quantifying restoration success and recovery in a metal-polluted stream: A 17-year assessment of physicochemical and biological responses","interactions":[],"lastModifiedDate":"2012-03-12T17:22:07","indexId":"70037286","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2163,"text":"Journal of Applied Ecology","active":true,"publicationSubtype":{"id":10}},"title":"Quantifying restoration success and recovery in a metal-polluted stream: A 17-year assessment of physicochemical and biological responses","docAbstract":"Evaluating the effectiveness of stream restoration is often challenging because of the lack of pre-treatment data, narrow focus on physicochemical measures and insufficient post-restoration monitoring. Even when these fundamental elements are present, quantifying restoration success is difficult because of the challenges associated with distinguishing treatment effects from seasonal variation, episodic events and long-term climatic changes.2. We report results of one of the most comprehensive and continuous records of physical, chemical and biological data available to assess restoration success for a stream ecosystem in North America. Over a 17 year period we measured seasonal and annual changes in metal concentrations, physicochemical characteristics, macroinvertebrate communities, and brown trout Salmo trutta populations in the Arkansas River, a metal-contaminated stream in Colorado, USA.3. Although we observed significant improvements in water quality after treatment, the effectiveness of restoration varied temporally, spatially and among biological response variables. The fastest recovery was observed at stations where restoration eliminated point sources of metal contamination. Recovery of macroinvertebrates was significantly delayed at some stations because of residual sediment contamination and because extreme seasonal and episodic variation in metal concentrations prevented recolonization by sensitive species. Synthesis and applications. Because recovery trajectories after the removal of a stressor are often complex or nonlinear, long-term studies are necessary to assess restoration success within the context of episodic events and changes in regional climate. The observed variation in recovery among chemical and biological endpoints highlights the importance of developing objective criteria to assess restoration success. Although the rapid response of macroinvertebrates to reduced metal concentrations is encouraging, we have previously demonstrated that benthic communities from the Arkansas River remained susceptible to other novel anthropogenic stressors. We suggest that the resistance or resilience of benthic macroinvertebrate communities to novel stressors may be effective indicators of restoration success that can account for the non-additive (e.g. synergistic) nature of compound perturbations. ?? 2010 The Authors. Journal compilation ?? 2010 British Ecological Society.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Applied Ecology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1111/j.1365-2664.2010.01838.x","issn":"00218901","usgsCitation":"Clements, W., Vieira, N., and Church, S.E., 2010, Quantifying restoration success and recovery in a metal-polluted stream: A 17-year assessment of physicochemical and biological responses: Journal of Applied Ecology, v. 47, no. 4, p. 899-910, https://doi.org/10.1111/j.1365-2664.2010.01838.x.","startPage":"899","endPage":"910","numberOfPages":"12","costCenters":[],"links":[{"id":475855,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1111/j.1365-2664.2010.01838.x","text":"Publisher Index Page"},{"id":217318,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1111/j.1365-2664.2010.01838.x"},{"id":245256,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"47","issue":"4","noUsgsAuthors":false,"publicationDate":"2010-06-29","publicationStatus":"PW","scienceBaseUri":"505a91dae4b0c8380cd804da","contributors":{"authors":[{"text":"Clements, W.H.","contributorId":78855,"corporation":false,"usgs":true,"family":"Clements","given":"W.H.","email":"","affiliations":[],"preferred":false,"id":460282,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Vieira, N.K.M.","contributorId":71034,"corporation":false,"usgs":true,"family":"Vieira","given":"N.K.M.","email":"","affiliations":[],"preferred":false,"id":460281,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Church, S. E.","contributorId":58260,"corporation":false,"usgs":true,"family":"Church","given":"S.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":460280,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70037288,"text":"70037288 - 2010 - Agricultural wetlands as potential hotspots for mercury bioaccumulation: Experimental evidence using caged fish","interactions":[],"lastModifiedDate":"2018-10-20T08:48:07","indexId":"70037288","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1565,"text":"Environmental Science & Technology","onlineIssn":"1520-5851","printIssn":"0013-936X","active":true,"publicationSubtype":{"id":10}},"title":"Agricultural wetlands as potential hotspots for mercury bioaccumulation: Experimental evidence using caged fish","docAbstract":"<p><span>Wetlands provide numerous ecosystem services, but also can be sources of methylmercury (MeHg) production and export. Rice agricultural wetlands in particular may be important sites for MeHg bioaccumulation due to their worldwide ubiquity, periodic flooding schedules, and high use by wildlife. We assessed MeHg bioaccumulation within agricultural and perennial wetlands common to California’s Central Valley during summer, when the majority of wetland habitats are shallowly flooded rice fields. We introduced caged western mosquitofish (</span><i>Gambusia affinis</i><span>) within white rice (</span><i>Oryza sativa</i><span>), wild rice (</span><i>Zizania palustris</i><span>), and permanent wetlands at water inlets, centers, and outlets. Total mercury (THg) concentrations and body burdens in caged mosquitofish increased rapidly, exceeding baseline values at introduction by 135% to 1197% and 29% to 1566% among sites, respectively, after only 60 days. Mercury bioaccumulation in caged mosquitofish was greater in rice fields than in permanent wetlands, with THg concentrations at wetland outlets increasing by 12.1, 5.8, and 2.9 times over initial concentrations in white rice, wild rice, and permanent wetlands, respectively. In fact, mosquitofish caged at white rice outlets accumulated 721 ng Hg/fish in just 60 days. Mercury in wild mosquitofish and Mississippi silversides (</span><i>Menidia audens</i><span>) concurrently sampled at wetland outlets also were greater in white rice and wild rice than permanent wetlands. Within wetlands, THg concentrations and body burdens of both caged and wild fish increased from water inlets to outlets in white rice fields, and tended to not vary among sites in permanent wetlands. Fish THg concentrations in agricultural wetlands were high, exceeding 0.2 μg/g ww in 82% of caged fish and 59% of wild fish. Our results indicate that shallowly flooded rice fields are potential hotspots for MeHg bioaccumulation and, due to their global prevalence, suggest that agricultural wetlands may be important contributors to MeHg contamination.</span></p>","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Environmental Science and Technology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1021/es9028364","issn":"0013936X","usgsCitation":"Ackerman, J., and Eagles-Smith, C.A., 2010, Agricultural wetlands as potential hotspots for mercury bioaccumulation: Experimental evidence using caged fish: Environmental Science & Technology, v. 44, no. 4, p. 1451-1457, https://doi.org/10.1021/es9028364.","productDescription":"7 p.","startPage":"1451","endPage":"1457","numberOfPages":"7","costCenters":[{"id":34983,"text":"Contaminant Biology Program","active":true,"usgs":true}],"links":[{"id":245288,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":217344,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1021/es9028364"}],"country":"United States","state":"California","volume":"44","issue":"4","noUsgsAuthors":false,"publicationDate":"2010-01-12","publicationStatus":"PW","scienceBaseUri":"5059e915e4b0c8380cd480ab","contributors":{"authors":[{"text":"Ackerman, Joshua T. 0000-0002-3074-8322 jackerman@usgs.gov","orcid":"https://orcid.org/0000-0002-3074-8322","contributorId":147078,"corporation":false,"usgs":true,"family":"Ackerman","given":"Joshua T.","email":"jackerman@usgs.gov","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":false,"id":460287,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Eagles-Smith, Collin A. 0000-0003-1329-5285 ceagles-smith@usgs.gov","orcid":"https://orcid.org/0000-0003-1329-5285","contributorId":505,"corporation":false,"usgs":true,"family":"Eagles-Smith","given":"Collin","email":"ceagles-smith@usgs.gov","middleInitial":"A.","affiliations":[{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true},{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true},{"id":289,"text":"Forest and Rangeland Ecosys Science Center","active":true,"usgs":true}],"preferred":true,"id":460288,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70037290,"text":"70037290 - 2010 - Mapping elevations of tidal wetland restoration sites in San Francisco Bay: Comparing accuracy of aerial lidar with a singlebeam echosounder","interactions":[],"lastModifiedDate":"2017-08-26T16:28:19","indexId":"70037290","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","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":"Mapping elevations of tidal wetland restoration sites in San Francisco Bay: Comparing accuracy of aerial lidar with a singlebeam echosounder","docAbstract":"The southern edge of San Francisco Bay is surrounded by former salt evaporation ponds, where tidal flow has been restricted since the mid to late 1890s. These ponds are now the focus of a large wetland restoration project, and accurate measurement of current pond bathymetry and adjacent mud flats has been critical to restoration planning. Aerial light detection and ranging (lidar) has become a tool for mapping surface elevations, but its accuracy had rarely been assessed for wetland habitats. We used a singlebeam echosounder system we developed for surveying shallow wetlands to map submerged pond bathymetry in January of 2004 and compared those results with aerial lidar surveys in two ponds that were dry in May of 2004. From those data sets, we compared elevations for 5164 (Pond E9, 154 ha) and 2628 (Pond E14, 69 ha) echosounder and lidar points within a 0.375-m radius of each other (0.750-m diameter lidar spot size). We found that mean elevations of the lidar points were lower than the echosounder results by 5 ?? 0.1 cm in Pond E9 and 2 ?? 0.2 cm in Pond E14. Only a few points (5% in Pond E9, 2% in Pond E14) differed by more than 20 cm, and some of these values may be explained by residual water in the ponds during the lidar survey or elevation changes that occurred between surveys. Our results suggest that aerial lidar may be a very accurate and rapid way to assess terrain elevations for wetland restoration projects. ?? 2010 Coastal Education and Research Foundation.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Coastal Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.2112/08-1076.1","issn":"07490208","usgsCitation":"Athearn, N., Takekawa, J.Y., Jaffe, B., Hattenbach, B., and Foxgrover, A., 2010, Mapping elevations of tidal wetland restoration sites in San Francisco Bay: Comparing accuracy of aerial lidar with a singlebeam echosounder: Journal of Coastal Research, v. 26, no. 2, p. 312-319, https://doi.org/10.2112/08-1076.1.","startPage":"312","endPage":"319","numberOfPages":"8","costCenters":[],"links":[{"id":217374,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.2112/08-1076.1"},{"id":245319,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"26","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a5056e4b0c8380cd6b60c","contributors":{"authors":[{"text":"Athearn, N.D.","contributorId":86958,"corporation":false,"usgs":true,"family":"Athearn","given":"N.D.","affiliations":[],"preferred":false,"id":460298,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Takekawa, John Y. 0000-0003-0217-5907 john_takekawa@usgs.gov","orcid":"https://orcid.org/0000-0003-0217-5907","contributorId":176168,"corporation":false,"usgs":true,"family":"Takekawa","given":"John","email":"john_takekawa@usgs.gov","middleInitial":"Y.","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":false,"id":460296,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Jaffe, B.","contributorId":78517,"corporation":false,"usgs":true,"family":"Jaffe","given":"B.","affiliations":[],"preferred":false,"id":460297,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hattenbach, B.J.","contributorId":103902,"corporation":false,"usgs":true,"family":"Hattenbach","given":"B.J.","email":"","affiliations":[],"preferred":false,"id":460299,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Foxgrover, A.C.","contributorId":34321,"corporation":false,"usgs":true,"family":"Foxgrover","given":"A.C.","email":"","affiliations":[],"preferred":false,"id":460295,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70037316,"text":"70037316 - 2010 - The impact of rare taxa on a fish index of biotic integrity","interactions":[],"lastModifiedDate":"2012-03-12T17:22:07","indexId":"70037316","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1456,"text":"Ecological Indicators","active":true,"publicationSubtype":{"id":10}},"title":"The impact of rare taxa on a fish index of biotic integrity","docAbstract":"The index of biotic integrity (IBI) is a commonly used bioassessment tool that integrates abundance and richness measures to assess water quality. In developing IBIs that are both responsive to human disturbance and resistant to natural variability and sampling error, water managers must decide how to weigh information about rare and abundant taxa, which in turn requires an understanding of the sensitivity of indices to rare taxa. Herein, we investigated the influence of rare fish taxa (within the lower 5% of rank abundance curves) on IBI metric and total scores for stream sites in two of Minnesota's major river basins, the St. Croix (n = 293 site visits) and Upper Mississippi (n = 210 site visits). We artificially removed rare taxa from biological samples by (1) separately excluding each individual taxon that fell within the lower 5% of rank abundance curves; (2) simultaneously excluding all taxa that had an abundance of one (singletons) or two (doubletons); and (3) simultaneously excluding all taxa that fell within the lower 5% of rank abundance curves. We then compared IBI metric and total scores before and after removal of rare taxa using the normalized root mean square error (nRMSE) and regression analysis. The difference in IBI metric and total scores increased as more taxa were removed. Moreover, when multiple rare taxa were removed, the nRMSE was related to sample abundance and to total taxa richness, with greater nRMSE observed in samples with a larger number of taxa or sample abundance. Metrics based on relative abundance of fish taxa were less sensitive to the loss of rare taxa, whereas those based on taxa richness were more sensitive, because taxa richness metrics give more weight to rare taxa compared to the relative abundance metrics. ?? 2010 Elsevier Ltd.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Ecological Indicators","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.ecolind.2009.12.006","issn":"1470160X","usgsCitation":"Wan, H., Chizinski, C., Dolph, C., Vondracek, B., and Wilson, B., 2010, The impact of rare taxa on a fish index of biotic integrity: Ecological Indicators, v. 10, no. 4, p. 781-788, https://doi.org/10.1016/j.ecolind.2009.12.006.","startPage":"781","endPage":"788","numberOfPages":"8","costCenters":[],"links":[{"id":475837,"rank":10000,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"http://hdl.handle.net/11299/183649","text":"External Repository"},{"id":217320,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.ecolind.2009.12.006"},{"id":245258,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"10","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505baceae4b08c986b32383b","contributors":{"authors":[{"text":"Wan, H.","contributorId":29246,"corporation":false,"usgs":true,"family":"Wan","given":"H.","email":"","affiliations":[],"preferred":false,"id":460438,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Chizinski, C.J.","contributorId":50635,"corporation":false,"usgs":true,"family":"Chizinski","given":"C.J.","email":"","affiliations":[],"preferred":false,"id":460439,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dolph, C.L.","contributorId":58864,"corporation":false,"usgs":true,"family":"Dolph","given":"C.L.","affiliations":[],"preferred":false,"id":460440,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Vondracek, B.","contributorId":69930,"corporation":false,"usgs":true,"family":"Vondracek","given":"B.","affiliations":[],"preferred":false,"id":460441,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Wilson, B.N.","contributorId":84192,"corporation":false,"usgs":true,"family":"Wilson","given":"B.N.","email":"","affiliations":[],"preferred":false,"id":460442,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70037320,"text":"70037320 - 2010 - Genesis of a regionally widespread celadonitic chert ironstone bed overlying upper Lias manganese deposits, Hungary","interactions":[],"lastModifiedDate":"2012-03-12T17:22:07","indexId":"70037320","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2545,"text":"Journal of the Geological Society","active":true,"publicationSubtype":{"id":10}},"title":"Genesis of a regionally widespread celadonitic chert ironstone bed overlying upper Lias manganese deposits, Hungary","docAbstract":"Mineralogy and chemical composition are presented for a chert-ironstone bed that overlies the ??rk??t Mn deposit. This bed is mottled green-brown in its lower and upper parts, which are composed of quartz, goethite and celadonite. These parts of the bed are interpreted to be strongly altered tuffs, reflecting oxidic, low-temperature alteration of a hydrated, Fe-rich, Al-poor tuff, and K and Mg uptake from seawater. The middle part of the bed is a mineralized bacterial mat (quartz, goethite). Textures resembling bacterial cells and colonies are common, with wavy, bulbous laminations composed of mounds overlying a mesh-work stromatolite-like texture constructed of micrometre-size Fe oxides. This bed is concordant with the underlying Mn deposit and marks the termination of Mn accumulation. Although no genetic connection exists between the two, the rocks adjacent to the contact record the oceanographic and bottom-water conditions extant when accumulation of one of the major Mn deposits of Europe ended, when the Transdanubian Range was located in the middle of the Adria-Apulian microcontinent between the Neotethys and Atlantic-Ligurian seaways. A pyroclastic origin for part of the bed has significance for the Toarcian of Central Europe because evidence of volcanism occurring at that time is otherwise sparse. ?? 2010 Geological Society of London.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of the Geological Society","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1144/0016-76492008-132","issn":"00167649","usgsCitation":"Polgari, M., Hein, J., Toth, M., Brukner-Wein, A., Vigh, T., Biro, L., and Cserhati, C., 2010, Genesis of a regionally widespread celadonitic chert ironstone bed overlying upper Lias manganese deposits, Hungary: Journal of the Geological Society, v. 167, no. 2, p. 313-328, https://doi.org/10.1144/0016-76492008-132.","startPage":"313","endPage":"328","numberOfPages":"16","costCenters":[],"links":[{"id":217376,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1144/0016-76492008-132"},{"id":245321,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"167","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a1558e4b0c8380cd54d84","contributors":{"authors":[{"text":"Polgari, Marta","contributorId":75750,"corporation":false,"usgs":true,"family":"Polgari","given":"Marta","email":"","affiliations":[],"preferred":false,"id":460459,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hein, J.R. 0000-0002-5321-899X","orcid":"https://orcid.org/0000-0002-5321-899X","contributorId":61429,"corporation":false,"usgs":true,"family":"Hein","given":"J.R.","affiliations":[],"preferred":false,"id":460458,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Toth, M.","contributorId":85442,"corporation":false,"usgs":true,"family":"Toth","given":"M.","affiliations":[],"preferred":false,"id":460460,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Brukner-Wein, A.","contributorId":98568,"corporation":false,"usgs":true,"family":"Brukner-Wein","given":"A.","email":"","affiliations":[],"preferred":false,"id":460461,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Vigh, T.","contributorId":47613,"corporation":false,"usgs":true,"family":"Vigh","given":"T.","email":"","affiliations":[],"preferred":false,"id":460456,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Biro, L.","contributorId":47207,"corporation":false,"usgs":true,"family":"Biro","given":"L.","email":"","affiliations":[],"preferred":false,"id":460455,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Cserhati, C.","contributorId":53633,"corporation":false,"usgs":true,"family":"Cserhati","given":"C.","email":"","affiliations":[],"preferred":false,"id":460457,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70037322,"text":"70037322 - 2010 - Sexing California gulls using morphometrics and discriminant function analysis","interactions":[],"lastModifiedDate":"2017-07-19T15:21:12","indexId":"70037322","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3731,"text":"Waterbirds","onlineIssn":"19385390","printIssn":"15244695","active":true,"publicationSubtype":{"id":10}},"title":"Sexing California gulls using morphometrics and discriminant function analysis","docAbstract":"A discriminant function analysis (DFA) model was developed with DNA sex verification so that external morphology could be used to sex 203 adult California Gulls (Larus californicus) in San Francisco Bay (SFB). The best model was 97% accurate and included head-to-bill length, culmen depth at the gonys, and wing length. Using an iterative process, the model was simplified to a single measurement (head-to-bill length) that still assigned sex correctly 94% of the time. A previous California Gull sex determination model developed for a population in Wyoming was then assessed by fitting SFB California Gull measurement data to the Wyoming model; this new model failed to converge on the same measurements as those originally used by the Wyoming model. Results from the SFB discriminant function model were compared to the Wyoming model results (by using SFB data with the Wyoming model); the SFB model was 7% more accurate for SFB California gulls. The simplified DFA model (head-to-bill length only) provided highly accurate results (94%) and minimized the measurements and time required to accurately sex California Gulls.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Waterbirds","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1675/063.033.0109","issn":"15244695","usgsCitation":"Herring, G., Ackerman, J., Eagles-Smith, C.A., and Takekawa, J.Y., 2010, Sexing California gulls using morphometrics and discriminant function analysis: Waterbirds, v. 33, no. 1, p. 79-85, https://doi.org/10.1675/063.033.0109.","startPage":"79","endPage":"85","numberOfPages":"7","costCenters":[],"links":[{"id":245352,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":217406,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1675/063.033.0109"}],"volume":"33","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b8db4e4b08c986b3184f1","contributors":{"authors":[{"text":"Herring, Garth 0000-0003-1106-4731 gherring@usgs.gov","orcid":"https://orcid.org/0000-0003-1106-4731","contributorId":4403,"corporation":false,"usgs":true,"family":"Herring","given":"Garth","email":"gherring@usgs.gov","affiliations":[{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true},{"id":289,"text":"Forest and Rangeland Ecosys Science Center","active":true,"usgs":true}],"preferred":true,"id":460470,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ackerman, Joshua T. 0000-0002-3074-8322 jackerman@usgs.gov","orcid":"https://orcid.org/0000-0002-3074-8322","contributorId":147078,"corporation":false,"usgs":true,"family":"Ackerman","given":"Joshua T.","email":"jackerman@usgs.gov","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":false,"id":460469,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Eagles-Smith, Collin A. 0000-0003-1329-5285 ceagles-smith@usgs.gov","orcid":"https://orcid.org/0000-0003-1329-5285","contributorId":505,"corporation":false,"usgs":true,"family":"Eagles-Smith","given":"Collin","email":"ceagles-smith@usgs.gov","middleInitial":"A.","affiliations":[{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true},{"id":289,"text":"Forest and Rangeland Ecosys Science Center","active":true,"usgs":true},{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"preferred":true,"id":460471,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Takekawa, John Y. 0000-0003-0217-5907 john_takekawa@usgs.gov","orcid":"https://orcid.org/0000-0003-0217-5907","contributorId":176168,"corporation":false,"usgs":true,"family":"Takekawa","given":"John","email":"john_takekawa@usgs.gov","middleInitial":"Y.","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":false,"id":460468,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70037323,"text":"70037323 - 2010 - Snowmelt hydrograph interpretation: Revealing watershed scale hydrologic characteristics of the Yellowstone volcanic plateau","interactions":[],"lastModifiedDate":"2012-03-12T17:22:11","indexId":"70037323","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2342,"text":"Journal of Hydrology","active":true,"publicationSubtype":{"id":10}},"title":"Snowmelt hydrograph interpretation: Revealing watershed scale hydrologic characteristics of the Yellowstone volcanic plateau","docAbstract":"Snowmelt hydrograph analysis and groundwater age dates of cool water springs on the Yellowstone volcanic plateau provide evidence of high volumes of groundwater circulation in watersheds comprised of quaternary Yellowstone volcanics. Ratios of maximum to minimum mean daily discharge and average recession indices are calculated for watersheds within and surrounding the Yellowstone volcanic plateau. A model for snowmelt recession is used to separate groundwater discharge from overland runoff, and compare groundwater systems. Hydrograph signal interpretation is corroborated with chlorofluorocarbon (CFC) and tritium concentrations in cool water springs on the Yellowstone volcanic plateau. Hydrograph parameters show a spatial pattern correlated with watershed geology. Watersheds comprised dominantly of quaternary Yellowstone volcanics are characterized by slow streamflow recession, low maximum to minimum flow ratios. Cool springs sampled within the Park contain CFC's and tritium and have apparent CFC age dates that range from about 50 years to modern. Watersheds comprised of quaternary Yellowstone volcanics have a large volume of active groundwater circulation. A large, advecting groundwater field would be the dominant mechanism for mass and energy transport in the shallow crust of the Yellowstone volcanic plateau, and thus control the Yellowstone hydrothermal system. ?? 2009 Elsevier B.V.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Hydrology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.jhydrol.2009.12.037","issn":"00221694","usgsCitation":"Payton, G., Susong, D., Kip, S.D., and Heasler, H., 2010, Snowmelt hydrograph interpretation: Revealing watershed scale hydrologic characteristics of the Yellowstone volcanic plateau: Journal of Hydrology, v. 383, no. 3-4, p. 209-222, https://doi.org/10.1016/j.jhydrol.2009.12.037.","startPage":"209","endPage":"222","numberOfPages":"14","costCenters":[],"links":[{"id":245353,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":217407,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.jhydrol.2009.12.037"}],"volume":"383","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b91b8e4b08c986b319a67","contributors":{"authors":[{"text":"Payton, Gardner W.","contributorId":87395,"corporation":false,"usgs":true,"family":"Payton","given":"Gardner W.","affiliations":[],"preferred":false,"id":460474,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Susong, D. D.","contributorId":12868,"corporation":false,"usgs":true,"family":"Susong","given":"D. D.","affiliations":[],"preferred":false,"id":460473,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kip, Solomon D.","contributorId":107484,"corporation":false,"usgs":true,"family":"Kip","given":"Solomon","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":460475,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Heasler, H.","contributorId":7818,"corporation":false,"usgs":true,"family":"Heasler","given":"H.","email":"","affiliations":[],"preferred":false,"id":460472,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70037329,"text":"70037329 - 2010 - Lake temperature and ice cover regimes in the Alaskan Subarctic and Arctic: Integrated monitoring, remote sensing, and modeling","interactions":[],"lastModifiedDate":"2018-06-16T18:02:28","indexId":"70037329","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2529,"text":"Journal of the American Water Resources Association","active":true,"publicationSubtype":{"id":10}},"title":"Lake temperature and ice cover regimes in the Alaskan Subarctic and Arctic: Integrated monitoring, remote sensing, and modeling","docAbstract":"Lake surface regimes are fundamental attributes of lake ecosystems and their interaction with the land and atmosphere. High latitudes may be particularly sensitive to climate change, however, adequate baselines for these lakes are often lacking. In this study, we couple monitoring, remote sensing, and modeling techniques to generate baseline datasets of lake surface temperature and ice cover in the Alaskan Subarctic and Arctic. No detectable trends were observed during this study period, but a number of interesting patterns were noted among lakes and between regions. The largest Arctic lake was relatively unresponsive to air temperature, while the largest Subarctic lake was very responsive likely because it is fed by glacial runoff. Mean late summer water temperatures were higher than air temperatures with differences ranging from 1.7 to 5.4°C in Subarctic lakes and from 2.4 to 3.2°C in Arctic lakes. The warmest mean summer water temperature in both regions was in 2004, with the exception of Subarctic glacially fed lake that was highest in 2005. Ice-out timing had high coherence within regions and years, typically occurring in late May in Subarctic and in early-July in Arctic lakes. Ice-on timing was more dependent on lake size and depth, often varying among lakes within a region. Such analyses provide an important baseline of lake surface regimes at a time when there is increasing interest in high-latitude water ecosystems and resources during an uncertain climate future.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of the American Water Resources Association","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Wiley","doi":"10.1111/j.1752-1688.2010.00451.x","issn":"1093474X","usgsCitation":"Arp, C., Jones, B.M., Whitman, M., Larsen, A., and Urban, F., 2010, Lake temperature and ice cover regimes in the Alaskan Subarctic and Arctic: Integrated monitoring, remote sensing, and modeling: Journal of the American Water Resources Association, v. 46, no. 4, p. 777-791, https://doi.org/10.1111/j.1752-1688.2010.00451.x.","productDescription":"15 p.","startPage":"777","endPage":"791","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":487958,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1111/j.1752-1688.2010.00451.x","text":"Publisher Index Page"},{"id":244942,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":217031,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1111/j.1752-1688.2010.00451.x"}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -180.0,51.2 ], [ -180.0,90.0 ], [ 180.0,90.0 ], [ 180.0,51.2 ], [ -180.0,51.2 ] ] ] } } ] }","volume":"46","issue":"4","noUsgsAuthors":false,"publicationDate":"2010-07-26","publicationStatus":"PW","scienceBaseUri":"505a4163e4b0c8380cd654f2","contributors":{"authors":[{"text":"Arp, C.D.","contributorId":54715,"corporation":false,"usgs":true,"family":"Arp","given":"C.D.","email":"","affiliations":[],"preferred":false,"id":460502,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jones, Benjamin M. 0000-0002-1517-4711 bjones@usgs.gov","orcid":"https://orcid.org/0000-0002-1517-4711","contributorId":2286,"corporation":false,"usgs":true,"family":"Jones","given":"Benjamin","email":"bjones@usgs.gov","middleInitial":"M.","affiliations":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":118,"text":"Alaska Science Center Geography","active":true,"usgs":true}],"preferred":true,"id":460501,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Whitman, Matthew","contributorId":19257,"corporation":false,"usgs":false,"family":"Whitman","given":"Matthew","affiliations":[],"preferred":false,"id":460499,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Larsen, A.","contributorId":15438,"corporation":false,"usgs":true,"family":"Larsen","given":"A.","email":"","affiliations":[],"preferred":false,"id":460498,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Urban, F.E. 0000-0002-1329-1703","orcid":"https://orcid.org/0000-0002-1329-1703","contributorId":34352,"corporation":false,"usgs":true,"family":"Urban","given":"F.E.","affiliations":[],"preferred":false,"id":460500,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70037346,"text":"70037346 - 2010 - Hepatic pathologies in the brackish water catfish (Chrysichthys nigrodigitatus) from contaminated locations of the Lagos lagoon complex","interactions":[],"lastModifiedDate":"2023-02-28T16:52:57.016663","indexId":"70037346","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":830,"text":"Applied Ecology and Environmental Research","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Hepatic pathologies in the brackish water catfish (<i>Chrysichthys nigrodigitatus</i>) from contaminated locations of the Lagos lagoon complex","title":"Hepatic pathologies in the brackish water catfish (Chrysichthys nigrodigitatus) from contaminated locations of the Lagos lagoon complex","docAbstract":"<p>Several toxicological studies into the effects of aquatic pollutants on the liver of teleost fish exist in literature. The focus on the liver in these studies is predicated on its central nature in the scheme of biotransformation and excretion of xenobiotics following exposure in polluted water bodies. As a consequence of the latter primary role of the liver in these processes it is regarded as a predilective site for the sub lethal effects of xenobiotics on the organism usually detectable at histological level. Hepatic histopathology recorded in livers from feral populations of the brackish water catfish <i>Chrysichthys nigrodigitatus</i> from locations on the Lagos lagoon complex with significant anthropogenic inputs from denizen populations and industries are presented. Liver sections from sixty specimens from two locations on the Lagos lagoon complex (Badagry lagoon: 6°24'N, 2°56'E; and Lagos lagoon: 6°29'N, 3°22'E) were analysed. Observed pathologies included hydropic degeneration (58%), portal / sinusoidal congestion (33%), hepatic necrosis (26%), hemosiderosis (12%) and foci of cellular alterations (FCA's). No obvious oncologic features were observed; the presence of the hydropic Vacuolation lesion was taken as prelude to the development of neoplasms and discussed as such.&nbsp;</p>","language":"English","publisher":"Penkala Bt.","doi":"10.15666/aeer/0703_277286","usgsCitation":"Olarinmoye, O., Taiwo, V., Clarke, E., Kumolu-Johnson, C., Aderinola, O., and Adekunbi, F., 2010, Hepatic pathologies in the brackish water catfish (Chrysichthys nigrodigitatus) from contaminated locations of the Lagos lagoon complex: Applied Ecology and Environmental Research, v. 7, no. 3, p. 277-286, https://doi.org/10.15666/aeer/0703_277286.","productDescription":"10 p.","startPage":"277","endPage":"286","costCenters":[],"links":[{"id":487238,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.15666/aeer/0703_277286","text":"Publisher Index Page"},{"id":413483,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Lagos","otherGeospatial":"Badagry Lagoon, Lagos Lagoon","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              2.9,\n              6.423914548203811\n            ],\n            [\n              2.9,\n              6.396531107011754\n            ],\n            [\n              2.95,\n              6.396531107011754\n            ],\n            [\n              2.95,\n              6.423914548203811\n            ],\n            [\n              2.9,\n              6.423914548203811\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    },\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              3.4,\n              6.5\n            ],\n            [\n              3.34,\n              6.5\n            ],\n            [\n              3.34,\n              6.46\n            ],\n            [\n              3.4,\n              6.46\n            ],\n            [\n              3.4,\n              6.5\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"7","issue":"3","noUsgsAuthors":false,"publicationDate":"2009-07-20","publicationStatus":"PW","scienceBaseUri":"505a3061e4b0c8380cd5d5d3","contributors":{"authors":[{"text":"Olarinmoye, O.","contributorId":48053,"corporation":false,"usgs":true,"family":"Olarinmoye","given":"O.","email":"","affiliations":[],"preferred":false,"id":460557,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Taiwo, V.","contributorId":85847,"corporation":false,"usgs":true,"family":"Taiwo","given":"V.","email":"","affiliations":[],"preferred":false,"id":460561,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Clarke, E.","contributorId":60507,"corporation":false,"usgs":true,"family":"Clarke","given":"E.","email":"","affiliations":[],"preferred":false,"id":460560,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Kumolu-Johnson, C.","contributorId":51614,"corporation":false,"usgs":true,"family":"Kumolu-Johnson","given":"C.","email":"","affiliations":[],"preferred":false,"id":460558,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Aderinola, O.","contributorId":104781,"corporation":false,"usgs":true,"family":"Aderinola","given":"O.","email":"","affiliations":[],"preferred":false,"id":460562,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Adekunbi, F.","contributorId":59311,"corporation":false,"usgs":true,"family":"Adekunbi","given":"F.","email":"","affiliations":[],"preferred":false,"id":460559,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70037347,"text":"70037347 - 2010 - Sediment transport on the Palos Verdes shelf, California","interactions":[],"lastModifiedDate":"2012-03-12T17:22:08","indexId":"70037347","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1333,"text":"Continental Shelf Research","active":true,"publicationSubtype":{"id":10}},"title":"Sediment transport on the Palos Verdes shelf, California","docAbstract":"Sediment transport and the potential for erosion or deposition have been investigated on the Palos Verdes (PV) and San Pedro shelves in southern California to help assess the fate of an effluent-affected deposit contaminated with DDT and PCBs. Bottom boundary layer measurements at two 60-m sites in spring 2004 were used to set model parameters and evaluate a one-dimensional (vertical) model of local, steady-state resuspension, and suspended-sediment transport. The model demonstrated skill (Brier scores up to 0.75) reproducing the magnitudes of bottom shear stress, current speeds, and suspended-sediment concentrations measured during an April transport event, but the model tended to underpredict observed rotation in the bottom-boundary layer, possibly because the model did not account for the effects of temperature-salinity stratification. The model was run with wave input estimated from a nearby buoy and current input from four to six years of measurements at thirteen sites on the 35- and 65-m isobaths on the PV and San Pedro shelves. Sediment characteristics and erodibility were based on gentle wet-sieve analysis and erosion-chamber measurements. Modeled flow and sediment transport were mostly alongshelf toward the northwest on the PV shelf with a significant offshore component. The 95th percentile of bottom shear stresses ranged from 0.09 to 0.16 Pa at the 65-m sites, and the lowest values were in the middle of the PV shelf, near the Whites Point sewage outfalls where the effluent-affected layer is thickest. Long-term mean transport rates varied from 0.9 to 4.8 metric tons m<sup>-1</sup> yr<sup>-1</sup> along the 65-m isobaths on the PV shelf, and were much higher at the 35-m sites. Gradients in modeled alongshore transport rates suggest that, in the absence of a supply of sediment from the outfalls or PV coast, erosion at rates of ???0.2 mm yr<sup>-1</sup> might occur in the region southeast of the outfalls. These rates are small compared to some estimates of background natural sedimentation rates (???5 mm yr<sup>-1</sup>), but do not preclude higher localized rates near abrupt transitions in sediment characteristics. However, low particle settling velocities and strong currents result in transport length-scales that are long relative to the narrow width of the PV shelf, which combined with the significant offshore component in transport, means that transport of resuspended sediment towards deep water is as likely as transport along the axis of the effluent-affected deposit.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Continental Shelf Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.csr.2010.01.011","issn":"02784343","usgsCitation":"Ferre, B., Sherwood, C.R., and Wiberg, P., 2010, Sediment transport on the Palos Verdes shelf, California: Continental Shelf Research, v. 30, no. 7, p. 761-780, https://doi.org/10.1016/j.csr.2010.01.011.","startPage":"761","endPage":"780","numberOfPages":"20","costCenters":[],"links":[{"id":475870,"rank":10000,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://hdl.handle.net/10037/13266","text":"External Repository"},{"id":245226,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":217291,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.csr.2010.01.011"}],"volume":"30","issue":"7","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b89e7e4b08c986b316f28","contributors":{"authors":[{"text":"Ferre, B.","contributorId":56481,"corporation":false,"usgs":true,"family":"Ferre","given":"B.","email":"","affiliations":[],"preferred":false,"id":460565,"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":460564,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wiberg, P.L.","contributorId":33827,"corporation":false,"usgs":true,"family":"Wiberg","given":"P.L.","email":"","affiliations":[],"preferred":false,"id":460563,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70037348,"text":"70037348 - 2010 - Cassini spectra and photometry 0.25–5.1 μm of the small inner satellites of Saturn","interactions":[],"lastModifiedDate":"2015-03-23T13:21:43","indexId":"70037348","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1963,"text":"Icarus","active":true,"publicationSubtype":{"id":10}},"title":"Cassini spectra and photometry 0.25–5.1 μm of the small inner satellites of Saturn","docAbstract":"The nominal tour of the Cassini mission enabled the first spectra and solar phase curves of the small inner satellites of Saturn. We present spectra from the Visual Infrared Mapping Spectrometer (VIMS) and the Imaging Science Subsystem (ISS) that span the 0.25-5.1 ??m spectral range. The composition of Atlas, Pandora, Janus, Epimetheus, Calypso, and Telesto is primarily water ice, with a small amount (???5%) of contaminant, which most likely consists of hydrocarbons. The optical properties of the \"shepherd\" satellites and the coorbitals are tied to the A-ring, while those of the Tethys Lagrangians are tied to the E-ring of Saturn. The color of the satellites becomes progressively bluer with distance from Saturn, presumably from the increased influence of the E-ring; Telesto is as blue as Enceladus. Janus and Epimetheus have very similar spectra, although the latter appears to have a thicker coating of ring material. For at least four of the satellites, we find evidence for the spectral line at 0.68 ??m that Vilas et al. [Vilas, F., Larsen, S.M., Stockstill, K.R., Gaffley, M.J., 1996. Icarus 124, 262-267] attributed to hydrated iron minerals on Iapetus and Hyperion. However, it is difficult to produce a spectral mixing model that includes this component. We find no evidence for CO<sub>2</sub> on any of the small satellites. There was a sufficient excursion in solar phase angle to create solar phase curves for Janus and Telesto. They bear a close similarity to the solar phase curves of the medium-sized inner icy satellites. Preliminary spectral modeling suggests that the contaminant on these bodies is not the same as the exogenously placed low-albedo material on Iapetus, but is rather a native material. The lack of CO<sub>2</sub> on the small inner satellites also suggests that their low-albedo material is distinct from that on Iapetus, Phoebe, and Hyperion. ?? 2009 Elsevier Inc.","language":"English","publisher":"Elsevier","doi":"10.1016/j.icarus.2009.08.015","issn":"00191035","usgsCitation":"Buratti, B.J., Bauer, J., Hicks, M., Mosher, J.A., Filacchione, G., Momary, T., Baines, K.H., Brown, R.H., Clark, R.N., and Nicholson, P.D., 2010, Cassini spectra and photometry 0.25–5.1 μm of the small inner satellites of Saturn: Icarus, v. 206, no. 2, p. 524-536, https://doi.org/10.1016/j.icarus.2009.08.015.","productDescription":"13 p.","startPage":"524","endPage":"536","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":245227,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":217292,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.icarus.2009.08.015"}],"otherGeospatial":"Saturn","volume":"206","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f38fe4b0c8380cd4b8a5","contributors":{"authors":[{"text":"Buratti, B. J.","contributorId":69280,"corporation":false,"usgs":false,"family":"Buratti","given":"B.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":460574,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bauer, J.M.","contributorId":88543,"corporation":false,"usgs":true,"family":"Bauer","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":460575,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hicks, M.D.","contributorId":7045,"corporation":false,"usgs":true,"family":"Hicks","given":"M.D.","email":"","affiliations":[],"preferred":false,"id":460567,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Mosher, J. A.","contributorId":34605,"corporation":false,"usgs":false,"family":"Mosher","given":"J.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":460570,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Filacchione, G.","contributorId":48740,"corporation":false,"usgs":true,"family":"Filacchione","given":"G.","affiliations":[],"preferred":false,"id":460572,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Momary, T.","contributorId":17415,"corporation":false,"usgs":true,"family":"Momary","given":"T.","affiliations":[],"preferred":false,"id":460568,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Baines, K. H.","contributorId":37868,"corporation":false,"usgs":false,"family":"Baines","given":"K.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":460571,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Brown, R. H.","contributorId":19931,"corporation":false,"usgs":false,"family":"Brown","given":"R.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":460569,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Clark, R. N.","contributorId":6568,"corporation":false,"usgs":true,"family":"Clark","given":"R.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":460566,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Nicholson, P. D.","contributorId":54330,"corporation":false,"usgs":false,"family":"Nicholson","given":"P.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":460573,"contributorType":{"id":1,"text":"Authors"},"rank":10}]}}
,{"id":70037354,"text":"70037354 - 2010 - Relationships between water temperatures and upstream migration, cold water refuge use, and spawning of adult bull trout from the Lostine River, Oregon, USA","interactions":[],"lastModifiedDate":"2017-11-17T16:02:42","indexId":"70037354","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1471,"text":"Ecology of Freshwater Fish","active":true,"publicationSubtype":{"id":10}},"title":"Relationships between water temperatures and upstream migration, cold water refuge use, and spawning of adult bull trout from the Lostine River, Oregon, USA","docAbstract":"Understanding thermal habitat use by migratory fish has been limited by difficulties in matching fish locations with water temperatures. To describe spatial and temporal patterns of thermal habitat use by migratory adult bull trout, Salvelinus confluentus, that spawn in the Lostine River, Oregon, we employed a combination of archival temperature tags, radio tags, and thermographs. We also compared temperatures of the tagged fish to ambient water temperatures to determine if the fish were using thermal refuges. The timing and temperatures at which fish moved upstream from overwintering areas to spawning locations varied considerably among individuals. The annual maximum 7-day average daily maximum (7DADM) temperatures of tagged fish were 16-18 ??C and potentially as high as 21 ??C. Maximum 7DADM ambient water temperatures within the range of tagged fish during summer were 18-25 ??C. However, there was no evidence of the tagged fish using localized cold water refuges. Tagged fish appeared to spawn at 7DADM temperatures of 7-14 ??C. Maximum 7DADM temperatures of tagged fish and ambient temperatures at the onset of the spawning period in late August were 11-18 ??C. Water temperatures in most of the upper Lostine River used for spawning and rearing appear to be largely natural since there has been little development, whereas downstream reaches used by migratory bull trout are heavily diverted for irrigation. Although the population effects of these temperatures are unknown, summer temperatures and the higher temperatures observed for spawning fish appear to be at or above the upper range of suitability reported for the species. Published 2009. This article is a US Governmentwork and is in the public domain in the USA.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Ecology of Freshwater Fish","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1111/j.1600-0633.2009.00393.x","issn":"09066691","usgsCitation":"Howell, P., Dunham, J., and Sankovich, P., 2010, Relationships between water temperatures and upstream migration, cold water refuge use, and spawning of adult bull trout from the Lostine River, Oregon, USA: Ecology of Freshwater Fish, v. 19, no. 1, p. 96-106, https://doi.org/10.1111/j.1600-0633.2009.00393.x.","startPage":"96","endPage":"106","numberOfPages":"11","costCenters":[{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true}],"links":[{"id":245323,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":217378,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1111/j.1600-0633.2009.00393.x"}],"volume":"19","issue":"1","noUsgsAuthors":false,"publicationDate":"2010-02-19","publicationStatus":"PW","scienceBaseUri":"505aa65ae4b0c8380cd84de9","contributors":{"authors":[{"text":"Howell, P.J.","contributorId":34361,"corporation":false,"usgs":true,"family":"Howell","given":"P.J.","email":"","affiliations":[],"preferred":false,"id":460620,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dunham, J. B. 0000-0002-6268-0633","orcid":"https://orcid.org/0000-0002-6268-0633","contributorId":96637,"corporation":false,"usgs":true,"family":"Dunham","given":"J. B.","affiliations":[],"preferred":false,"id":460622,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sankovich, P.M.","contributorId":64487,"corporation":false,"usgs":true,"family":"Sankovich","given":"P.M.","email":"","affiliations":[],"preferred":false,"id":460621,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70037358,"text":"70037358 - 2010 - Tet and sul antibiotic resistance genes in livestock lagoons of various operation type, configuration, and antibiotic occurrence","interactions":[],"lastModifiedDate":"2018-10-09T10:57:13","indexId":"70037358","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1565,"text":"Environmental Science & Technology","onlineIssn":"1520-5851","printIssn":"0013-936X","active":true,"publicationSubtype":{"id":10}},"title":"Tet and sul antibiotic resistance genes in livestock lagoons of various operation type, configuration, and antibiotic occurrence","docAbstract":"<p>Although livestock operations are known to harbor elevated levels of antibiotic resistant bacteria, few studies have examined the potential of livestock waste lagoons to reduce antibiotic resistance genes (ARGs). The purpose of this study was to determine the prevalence and examine the behavior of tetracycline [tet(O) and tet(W)] and sulfonamide [sul(I) and su/(II)] ARGsin a broad cross-section of livestock lagoons within the same semiarid western watershed. ARGs were monitored for one year in the water and the settled solids of eight lagoon systems by quantitative polymerase chain reaction. In addition, antibiotic residues and various bulk water quality constituents were analyzed. It was found that the lagoons of the chicken layer operation had the lowest concentrations of both tet and sul ARGs and low total antibiotic concentrations, whereas su ARGs were highest in the swine lagoons, which generally corresponded to the highest total antibiotic concentrations. A marginal benefit of organic and small dairy operations also was observed compared to conventional and large dairies, respectively. In all lagoons, su ARGs were observed to be generally more recalcitrant than tet ARGs. Also, positive correlations of various bulk water quality constituents were identified with tet ARGs but not sul ARGs. Significant positive correlations were identified between several metals and tet ARGs, but Pearson's correlation coefficients were mostly lower than those determined between antibiotic residues and ARGs. This study represents a quantitative characterization of ARGs in lagoons across a variety of livestock operations and provides insight into potential options for managing antibiotic resistance emanating from agricultural activities.</p>","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Environmental Science and Technology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1021/es9038165","issn":"0013936X","usgsCitation":"McKinney, C., Loftin, K.A., Meyer, M.T., Davis, J., and Pruden, A., 2010, Tet and sul antibiotic resistance genes in livestock lagoons of various operation type, configuration, and antibiotic occurrence: Environmental Science & Technology, v. 44, no. 16, p. 6102-6109, https://doi.org/10.1021/es9038165.","productDescription":"8p.","startPage":"6102","endPage":"6109","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":245385,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":217437,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1021/es9038165"}],"volume":"44","issue":"16","noUsgsAuthors":false,"publicationDate":"2010-07-21","publicationStatus":"PW","scienceBaseUri":"505ba5e5e4b08c986b320d65","contributors":{"authors":[{"text":"McKinney, C.W.","contributorId":7943,"corporation":false,"usgs":true,"family":"McKinney","given":"C.W.","email":"","affiliations":[],"preferred":false,"id":460636,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Loftin, Keith A. 0000-0001-5291-876X kloftin@usgs.gov","orcid":"https://orcid.org/0000-0001-5291-876X","contributorId":868,"corporation":false,"usgs":true,"family":"Loftin","given":"Keith","email":"kloftin@usgs.gov","middleInitial":"A.","affiliations":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"preferred":true,"id":460639,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Meyer, Michael T. 0000-0001-6006-7985 mmeyer@usgs.gov","orcid":"https://orcid.org/0000-0001-6006-7985","contributorId":866,"corporation":false,"usgs":true,"family":"Meyer","given":"Michael","email":"mmeyer@usgs.gov","middleInitial":"T.","affiliations":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"preferred":true,"id":460640,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Davis, J.G.","contributorId":9447,"corporation":false,"usgs":true,"family":"Davis","given":"J.G.","email":"","affiliations":[],"preferred":false,"id":460637,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Pruden, A.","contributorId":11451,"corporation":false,"usgs":true,"family":"Pruden","given":"A.","email":"","affiliations":[],"preferred":false,"id":460638,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70037359,"text":"70037359 - 2010 - Determination of antibiotics in sewage from hospitals, nursery and slaughter house, wastewater treatment plant and source water in Chongqing region of Three Gorge Reservoir in China","interactions":[],"lastModifiedDate":"2018-10-11T18:00:07","indexId":"70037359","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1555,"text":"Environmental Pollution","active":true,"publicationSubtype":{"id":10}},"title":"Determination of antibiotics in sewage from hospitals, nursery and slaughter house, wastewater treatment plant and source water in Chongqing region of Three Gorge Reservoir in China","docAbstract":"<p><span>Sewage samples from 4 hospitals, 1 nursery, 1 slaughter house, 1&nbsp;wastewater treatment plant&nbsp;and 5 source water samples of Chongqing region of Three Gorge Reservoir were analyzed for macrolide, lincosamide, trimethoprim, fluorouinolone, sulfonamide and tetracycline&nbsp;antibiotics&nbsp;by online solid-phase extraction and liquid chromatography-tandem mass spectrometry. Results showed that the concentration of ofloxacin (OFX) in hospital was the highest among all water environments ranged from 1.660&nbsp;μg/L to 4.240&nbsp;μg/L and norfloxacin (NOR, 0.136–1.620&nbsp;μg/L), ciproflaxacin (CIP, ranged from 0.011&nbsp;μg/L to 0.136&nbsp;μg/L), trimethoprim (TMP, 0.061–0.174&nbsp;μg/L) were commonly detected. Removal range of antibiotics in the wastewater treatment plant was 18–100% and the removal ratio of tylosin, oxytetracycline and tetracycline were 100%. Relatively higher removal efficiencies were observed for tylosin (TYL), oxytetracycline (OXY) and tetracycline (TET)(100%), while lower removal efficiencies were observed for Trimethoprim (TMP, 1%), Epi-iso-chlorotetracycline (EICIC, 18%) and Erythromycin-H</span><sub>2</sub><span>O (ERY-H</span><sub>2</sub><span>O, 24%). Antibiotics were removed more efficiently in&nbsp;primary treatment compared with those in&nbsp;secondary treatment.</span></p>","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Environmental Pollution","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","doi":"10.1016/j.envpol.2009.12.034","issn":"02697491","usgsCitation":"Chang, X., Meyer, M.T., Liu, X., Zhao, Q., Hao, C., Chen, J., Qiu, Z., Yang, L., Cao, J., and Shu, W., 2010, Determination of antibiotics in sewage from hospitals, nursery and slaughter house, wastewater treatment plant and source water in Chongqing region of Three Gorge Reservoir in China: Environmental Pollution, v. 158, no. 5, p. 1444-1450, https://doi.org/10.1016/j.envpol.2009.12.034.","productDescription":"7 p.","startPage":"1444","endPage":"1450","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":244912,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":217003,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.envpol.2009.12.034"}],"country":"China","otherGeospatial":"Chongqing region, Three Gorge Reservoir","volume":"158","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059ff92e4b0c8380cd4f277","contributors":{"authors":[{"text":"Chang, Xiaotian","contributorId":64834,"corporation":false,"usgs":true,"family":"Chang","given":"Xiaotian","email":"","affiliations":[],"preferred":false,"id":460645,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Meyer, Michael T. 0000-0001-6006-7985 mmeyer@usgs.gov","orcid":"https://orcid.org/0000-0001-6006-7985","contributorId":866,"corporation":false,"usgs":true,"family":"Meyer","given":"Michael","email":"mmeyer@usgs.gov","middleInitial":"T.","affiliations":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"preferred":true,"id":460649,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Liu, Xiuying","contributorId":76529,"corporation":false,"usgs":true,"family":"Liu","given":"Xiuying","email":"","affiliations":[],"preferred":false,"id":460647,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Zhao, Q.","contributorId":74985,"corporation":false,"usgs":true,"family":"Zhao","given":"Q.","email":"","affiliations":[],"preferred":false,"id":460646,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Hao, Chen","contributorId":89306,"corporation":false,"usgs":true,"family":"Hao","given":"Chen","email":"","affiliations":[],"preferred":false,"id":460648,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Chen, J.-a.","contributorId":27715,"corporation":false,"usgs":true,"family":"Chen","given":"J.-a.","email":"","affiliations":[],"preferred":false,"id":460643,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Qiu, Z.","contributorId":99802,"corporation":false,"usgs":true,"family":"Qiu","given":"Z.","email":"","affiliations":[],"preferred":false,"id":460650,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Yang, L.","contributorId":6200,"corporation":false,"usgs":true,"family":"Yang","given":"L.","affiliations":[],"preferred":false,"id":460641,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Cao, J.","contributorId":64483,"corporation":false,"usgs":true,"family":"Cao","given":"J.","email":"","affiliations":[],"preferred":false,"id":460644,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Shu, W.","contributorId":6290,"corporation":false,"usgs":true,"family":"Shu","given":"W.","email":"","affiliations":[],"preferred":false,"id":460642,"contributorType":{"id":1,"text":"Authors"},"rank":10}]}}
,{"id":70037373,"text":"70037373 - 2010 - Effectiveness of capture techniques for rails in emergent marsh and agricultural wetlands","interactions":[],"lastModifiedDate":"2012-03-12T17:22:08","indexId":"70037373","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3731,"text":"Waterbirds","onlineIssn":"19385390","printIssn":"15244695","active":true,"publicationSubtype":{"id":10}},"title":"Effectiveness of capture techniques for rails in emergent marsh and agricultural wetlands","docAbstract":"A reliable and effective technique for capturing rails would improve researchers' ability to study these secretive marsh birds. The time effectiveness and capture success of four methods for capturing rails in emergent marsh and agricultural wetlands in southern Louisiana and Texas were evaluated during winter and breeding seasons. Methods were hand and net capture from an airboat at night, an all-terrain vehicle (ATV) at night, an ATV during daylight rice harvest and passive capture using drop-door traps with drift fencing. Five hundred and twenty rails were captured (and 21 recaptures): 192 King Rails (Rallus elegans), 74 Clapper Rails (R. longirostris), 110 Virginia Rails (R. limicola), 125 Sora (Porzana Carolina) and 40 Yellow Rails (Coturnicops noveboracensis). Methods used at night were effective at capturing rails: capture from airboats yielded 2.13 rails per hour each airboat was operated and capture from ATVs yielded 1.80 rails per hour each ATV was operated. During daylight, captures from ATVs during rice harvest (0.25 rails per hour each ATV was operated) and passive drop-door traps with drift fencing (0.0054 rails per trap hour) were both inefficient.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Waterbirds","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1675/063.033.0315","issn":"15244695","usgsCitation":"Perkins, M., King, S., and Linscombe, J., 2010, Effectiveness of capture techniques for rails in emergent marsh and agricultural wetlands: Waterbirds, v. 33, no. 3, p. 376-380, https://doi.org/10.1675/063.033.0315.","startPage":"376","endPage":"380","numberOfPages":"5","costCenters":[],"links":[{"id":245160,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":217232,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1675/063.033.0315"}],"volume":"33","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0639e4b0c8380cd5116e","contributors":{"authors":[{"text":"Perkins, Marie","contributorId":22957,"corporation":false,"usgs":false,"family":"Perkins","given":"Marie","email":"","affiliations":[],"preferred":false,"id":460738,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"King, S.L.","contributorId":105663,"corporation":false,"usgs":true,"family":"King","given":"S.L.","email":"","affiliations":[],"preferred":false,"id":460740,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Linscombe, J.","contributorId":95712,"corporation":false,"usgs":true,"family":"Linscombe","given":"J.","email":"","affiliations":[],"preferred":false,"id":460739,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
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