{"pageNumber":"917","pageRowStart":"22900","pageSize":"25","recordCount":68937,"records":[{"id":70032147,"text":"70032147 - 2008 - Predicting recolonization patterns and interactions between potamodromous and anadromous salmonids in response to dam removal in the Elwha River, Washington State, USA","interactions":[],"lastModifiedDate":"2017-11-17T14:27:50","indexId":"70032147","displayToPublicDate":"2008-01-01T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2900,"text":"Northwest Science","onlineIssn":"2161-9859","printIssn":"0029-344X","active":true,"publicationSubtype":{"id":10}},"title":"Predicting recolonization patterns and interactions between potamodromous and anadromous salmonids in response to dam removal in the Elwha River, Washington State, USA","docAbstract":"The restoration of salmonids in the Elwha River following dam removal will cause interactions between anadromous and potamodromous forms as recolonization occurs in upstream and downstream directions. Anadromous salmonids are expected to recolonize historic habitats, and rainbow trout (Oncorhynchus mykiss) and bull trout (Salvelinus confluentus) isolated above the dams for 90 years are expected to reestablish anadromy. We summarized the distribution and abundance of potamodromous salmonids, determined locations of spawning areas, and mapped natural barriers to fish migration at the watershed scale based on data collected from 1993 to 2006. Rainbow trout were far more abundant than bull trout throughout the watershed and both species were distributed up to river km 71. Spawning locations for bull trout and rainbow trout occurred in areas where we anticipate returning anadromous fish to spawn. Nonnative brook trout were confined to areas between and below the dams, and seasonal velocity barriers are expected to prevent their upstream movements. We hypothesize that the extent of interaction between potamodromous and anadromous salmonids will vary spatially due to natural barriers that will limit upstream-directed recolonization for some species of salmonids. Consequently, most competitive interactions will occur in the main stem and floodplain downstream of river km 25 and in larger tributaries. Understanding future responses of Pacific salmonids after dam removal in the Elwha River depends upon an understanding of existing conditions of the salmonid community upstream of the dams prior to dam removal.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Northwest Science","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"0029344X","usgsCitation":"Brenkman, S., Pess, G., Torgersen, C., Kloehn, K., Duda, J., and Corbett, S., 2008, Predicting recolonization patterns and interactions between potamodromous and anadromous salmonids in response to dam removal in the Elwha River, Washington State, USA: Northwest Science, v. 82, no. SPEC.ISS., p. 91-106.","startPage":"91","endPage":"106","numberOfPages":"16","costCenters":[{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true}],"links":[{"id":242366,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"82","issue":"SPEC.ISS.","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a81c4e4b0c8380cd7b6fe","contributors":{"authors":[{"text":"Brenkman, S.J.","contributorId":106318,"corporation":false,"usgs":true,"family":"Brenkman","given":"S.J.","affiliations":[],"preferred":false,"id":434732,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pess, G.R.","contributorId":33037,"corporation":false,"usgs":true,"family":"Pess","given":"G.R.","affiliations":[],"preferred":false,"id":434727,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Torgersen, C.E.","contributorId":34459,"corporation":false,"usgs":true,"family":"Torgersen","given":"C.E.","affiliations":[],"preferred":false,"id":434728,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Kloehn, K.K.","contributorId":84995,"corporation":false,"usgs":true,"family":"Kloehn","given":"K.K.","email":"","affiliations":[],"preferred":false,"id":434730,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Duda, J.J. 0000-0001-7431-8634","orcid":"https://orcid.org/0000-0001-7431-8634","contributorId":105073,"corporation":false,"usgs":true,"family":"Duda","given":"J.J.","affiliations":[],"preferred":false,"id":434731,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Corbett, S.C.","contributorId":79318,"corporation":false,"usgs":true,"family":"Corbett","given":"S.C.","email":"","affiliations":[],"preferred":false,"id":434729,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70010011,"text":"70010011 - 2008 - Decadal-scale changes of nitrate in ground water of the United States, 1988-2004","interactions":[],"lastModifiedDate":"2017-01-18T14:40:39","indexId":"70010011","displayToPublicDate":"2008-01-01T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2262,"text":"Journal of Environmental Quality","active":true,"publicationSubtype":{"id":10}},"title":"Decadal-scale changes of nitrate in ground water of the United States, 1988-2004","docAbstract":"This study evaluated decadal-scale changes of nitrate concentrations in groundwater samples collected by the USGS National Water-Quality Assessment Program from 495 wells in 24 well networks across the USA in predominantly agricultural areas. Each well network was sampled once during 1988-1995 and resampled once during 2000-2004. Statistical tests of decadal-scale changes of nitrate concentrations in water from all 495 wells combined indicate there is a significant increase in nitrate concentrations in the data set as a whole. Eight out of the 24 well networks, or about 33%, had significant changes of nitrate concentrations. Of the eight well networks with significant decadal-scale changes of nitrate, all except one, the Willamette Valley of Oregon, had increasing nitrate concentrations. Median nitrate concentrations of three of those eight well networks increased above the USEPA maximum contaminant level of 10 mg L-1. Nitrate in water from wells with reduced conditions had significantly smaller decadal-scale changes in nitrate concentrations than oxidized and mixed waters. A subset of wells had data on ground water recharge date; nitrate concentrations increased in response to the increase of N fertilizer use since about 1950. Determining ground water recharge dates is an important component of a ground water trends investigation because recharge dates provide a link between changes in ground water quality and changes in land-use practices. Copyright ?? 2008 by the American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America. All rights reserved.","language":"English","publisher":"ACSESS","doi":"10.2134/jeq2007.0055","issn":"00472425","usgsCitation":"Rupert, M.G., 2008, Decadal-scale changes of nitrate in ground water of the United States, 1988-2004: Journal of Environmental Quality, v. 37, no. SUPPL. 5, p. S240-S248, https://doi.org/10.2134/jeq2007.0055.","productDescription":"9 p.","startPage":"S240","endPage":"S248","costCenters":[{"id":191,"text":"Colorado Water Science Center","active":true,"usgs":true}],"links":[{"id":219049,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":204909,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.2134/jeq2007.0055"}],"volume":"37","issue":"SUPPL. 5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059fe00e4b0c8380cd4ea6c","contributors":{"authors":[{"text":"Rupert, Michael G. mgrupert@usgs.gov","contributorId":1194,"corporation":false,"usgs":true,"family":"Rupert","given":"Michael","email":"mgrupert@usgs.gov","middleInitial":"G.","affiliations":[{"id":191,"text":"Colorado Water Science Center","active":true,"usgs":true}],"preferred":true,"id":357669,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70032948,"text":"70032948 - 2008 - Evidence for ponding and catastrophic floods in central Valles Marineris, Mars","interactions":[],"lastModifiedDate":"2012-03-12T17:21:39","indexId":"70032948","displayToPublicDate":"2008-01-01T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1963,"text":"Icarus","active":true,"publicationSubtype":{"id":10}},"title":"Evidence for ponding and catastrophic floods in central Valles Marineris, Mars","docAbstract":"The Valles Marineris canyon system of Mars is closely related to large flood channels, some of which emerge full born from chaotic terrain in canyon floors. Coprates Chasma, one of the largest Valles Marineris canyons, is connected at its west end to Melas Chasma and on its east end to chaotic terrain-filled Capri and Eos Chasmata. The area from central Melas to Eos Chasmata contains a 1500 km long and about 1 km deep depression in its floor. Despite the large volumes of groundwater that likely discharged from chaotic terrain in this depression, no evidence of related fluvial activity has thus far been reported. We present an analysis of the regional topography which, together with photogeologic interpretation of available imagery, suggests that ponding due to late Hesperian discharge of water possibly produced a lake (mean depth 842 m) spanning parts of the Valles Marineris depression (VMD). Overflow of this lake at its eastern end resulted in delivery of water to downstream chaos regions and outflow channels. Our ponding hypothesis is motivated primarily by the identification of scarp and terrace features which, despite a lateral spread of about 1500 km, have similar elevations. Furthermore, these elevations correspond to the maximum ponding elevation of the region (-3560 m). Simulated ponding in the VMD yields an overflow point at its eastern extremity, in Eos Chasma. The neighborhood of this overflow point contains clear indicators of fluvial erosion in a consistent east-west orientation. ?? 2008 Elsevier Inc.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Icarus","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.icarus.2008.08.003","issn":"00191","usgsCitation":"Harrison, K., and Chapman, M.G., 2008, Evidence for ponding and catastrophic floods in central Valles Marineris, Mars: Icarus, v. 198, no. 2, p. 351-364, https://doi.org/10.1016/j.icarus.2008.08.003.","startPage":"351","endPage":"364","numberOfPages":"14","costCenters":[],"links":[{"id":213114,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.icarus.2008.08.003"},{"id":240706,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"198","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0d4de4b0c8380cd52f2a","contributors":{"authors":[{"text":"Harrison, K.P.","contributorId":34329,"corporation":false,"usgs":true,"family":"Harrison","given":"K.P.","email":"","affiliations":[],"preferred":false,"id":438660,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Chapman, M. G.","contributorId":105737,"corporation":false,"usgs":true,"family":"Chapman","given":"M.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":438661,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70032060,"text":"70032060 - 2008 - Inverse geochemical modeling of groundwater evolution with emphasis on arsenic in the Mississippi River Valley alluvial aquifer, Arkansas (USA)","interactions":[],"lastModifiedDate":"2012-03-12T17:21:27","indexId":"70032060","displayToPublicDate":"2008-01-01T00:00:00","publicationYear":"2008","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":"Inverse geochemical modeling of groundwater evolution with emphasis on arsenic in the Mississippi River Valley alluvial aquifer, Arkansas (USA)","docAbstract":"Inverse geochemical modeling (PHREEQC) was used to identify the evolution of groundwater with emphasis on arsenic (As) release under reducing conditions in the shallow (25-30 m) Mississippi River Valley Alluvial aquifer, Arkansas, USA. The modeling was based on flow paths defined by high-precision (??2 cm) water level contour map; X-ray diffraction (XRD), scanning electron microscopic (SEM), and chemical analysis of boring-sediments for minerals; and detailed chemical analysis of groundwater along the flow paths. Potential phases were constrained using general trends in chemical analyses data of groundwater and sediments, and saturation indices data (MINTEQA2) of minerals in groundwater. Modeling results show that calcite, halite, fluorite, Fe oxyhydroxide, organic matter, H2S (gas) were dissolving with mole transfers of 1.40E - 03, 2.13E - 04, 4.15E - 06, 1.25E + 01, 3.11, and 9.34, respectively along the dominant flow line. Along the same flow line, FeS, siderite, and vivianite were precipitating with mole transfers of 9.34, 3.11, and 2.64E - 07, respectively. Cation exchange reactions of Ca2+ (4.93E - 04 mol) for Na+ (2.51E - 04 mol) on exchange sites occurred along the dominant flow line. Gypsum dissolution reactions were dominant over calcite dissolution in some of the flow lines due to the common ion effect. The concentration of As in groundwater ranged from <0.5 to 77 ??g/L. Twenty percent total As was complexed with Fe and Mn oxyhydroxides. The redox environment, chemical data of sediments and groundwater, and the results of inverse geochemical modeling indicate that reductive dissolution of Fe oxyhydroxide is the dominant process of As release in the groundwater. The relative rate of reduction of Fe oxyhydroxide over SO42 - with co-precipitation of As into sulfide is the limiting factor controlling dissolved As in groundwater. ?? 2007 Elsevier B.V. All rights reserved.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Hydrology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.jhydrol.2007.11.027","issn":"00221694","usgsCitation":"Sharif, M., Davis, R., Steele, K., Kim, B., Kresse, T., and Fazio, J., 2008, Inverse geochemical modeling of groundwater evolution with emphasis on arsenic in the Mississippi River Valley alluvial aquifer, Arkansas (USA): Journal of Hydrology, v. 350, no. 1-2, p. 41-55, https://doi.org/10.1016/j.jhydrol.2007.11.027.","startPage":"41","endPage":"55","numberOfPages":"15","costCenters":[],"links":[{"id":214875,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.jhydrol.2007.11.027"},{"id":242631,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"350","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3e4be4b0c8380cd63c5e","contributors":{"authors":[{"text":"Sharif, M.U.","contributorId":106243,"corporation":false,"usgs":true,"family":"Sharif","given":"M.U.","email":"","affiliations":[],"preferred":false,"id":434358,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Davis, R.K.","contributorId":85307,"corporation":false,"usgs":true,"family":"Davis","given":"R.K.","email":"","affiliations":[],"preferred":false,"id":434356,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Steele, K.F.","contributorId":50270,"corporation":false,"usgs":true,"family":"Steele","given":"K.F.","email":"","affiliations":[],"preferred":false,"id":434354,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Kim, B.","contributorId":93173,"corporation":false,"usgs":true,"family":"Kim","given":"B.","email":"","affiliations":[],"preferred":false,"id":434357,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Kresse, T.M.","contributorId":107019,"corporation":false,"usgs":true,"family":"Kresse","given":"T.M.","email":"","affiliations":[],"preferred":false,"id":434359,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Fazio, J.A.","contributorId":63135,"corporation":false,"usgs":true,"family":"Fazio","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":434355,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70010004,"text":"70010004 - 2008 - Temporal trends in nitrate and selected pesticides in mid-atlantic ground water","interactions":[],"lastModifiedDate":"2012-03-12T17:18:22","indexId":"70010004","displayToPublicDate":"2008-01-01T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Temporal trends in nitrate and selected pesticides in mid-atlantic ground water","docAbstract":"Evaluating long-term temporal trends in regional ground-water quality is complicated by variable hydrogeologic conditions and typically slow flow, and such trends have rarely been directly measured. Ground-water samples were collected over near-decadal and annual intervals from unconfined aquifers in agricultural areas of the Mid-Atlantic region, including fractured carbonate rocks in the Great Valley, Potomac River Basin, and unconsolidated sediments on the Delmarva Peninsula. Concentrations of nitrate and selected pesticides and degradates were compared among sampling events and to apparent recharge dates. Observed temporal trends are related to changes in land use and chemical applications, and to hydrogeology and climate. Insignificant differences in nitrate concentrations in the Great Valley between 1993 and 2002 are consistent with relatively steady fertilizer application during respective recharge periods and are likely related to drought conditions in the later sampling period. Detecting trends in Great Valley ground water is complicated by long open boreholes characteristic of wells sampled in this setting which facilitate significant ground-water mixing. Decreasing atrazine and prometon concentrations, however, reflect reported changes in usage. On the Delmarva Peninsula between 1988 and 2001, median nitrate concentrations increased 2 mg per liter in aerobic ground water, reflecting increasing fertilizer applications. Correlations between selected pesticide compounds and apparent recharge date are similarly related to changing land use and chemical application. Observed trends in the two settings demonstrate the importance of considering hydrogeology and recharge date along with, changing land and chemical uses when interpreting trends in regional ground-water quality. Copyright ?? 2008 by the American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America. All rights reserved.","largerWorkTitle":"Journal of Environmental Quality","language":"English","doi":"10.2134/jeq2007.0664","issn":"00472425","usgsCitation":"Debrewer, L., Ator, S., and Denver, J.M., 2008, Temporal trends in nitrate and selected pesticides in mid-atlantic ground water, <i>in</i> Journal of Environmental Quality, v. 37, no. SUPPL. 5, https://doi.org/10.2134/jeq2007.0664.","costCenters":[],"links":[{"id":204897,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.2134/jeq2007.0664"},{"id":218925,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"37","issue":"SUPPL. 5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505ba51ee4b08c986b320809","contributors":{"authors":[{"text":"Debrewer, L.M.","contributorId":30747,"corporation":false,"usgs":true,"family":"Debrewer","given":"L.M.","affiliations":[],"preferred":false,"id":357644,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ator, S.W. 0000-0002-9186-4837","orcid":"https://orcid.org/0000-0002-9186-4837","contributorId":104100,"corporation":false,"usgs":true,"family":"Ator","given":"S.W.","affiliations":[],"preferred":false,"id":357646,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Denver, J. M.","contributorId":100356,"corporation":false,"usgs":true,"family":"Denver","given":"J.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":357645,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70032009,"text":"70032009 - 2008 - Thermal history of the unsaturated zone at Yucca Mountain, Nevada, USA","interactions":[],"lastModifiedDate":"2012-03-12T17:21:28","indexId":"70032009","displayToPublicDate":"2008-01-01T00:00:00","publicationYear":"2008","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":"Thermal history of the unsaturated zone at Yucca Mountain, Nevada, USA","docAbstract":"Secondary calcite, silica and minor amounts of fluorite deposited in fractures and cavities record the chemistry, temperatures, and timing of past fluid movement in the unsaturated zone at Yucca Mountain, Nevada, the proposed site of a high-level radioactive waste repository. The distribution and geochemistry of these deposits are consistent with low-temperature precipitation from meteoric waters that infiltrated at the surface and percolated down through the unsaturated zone. However, the discovery of fluid inclusions in calcite with homogenization temperatures (Th) up to ???80 ??C was construed by some scientists as strong evidence for hydrothermal deposition. This paper reports the results of investigations to test the hypothesis of hydrothermal deposition and to determine the temperature and timing of secondary mineral deposition. Mineral precipitation temperatures in the unsaturated zone are estimated from calcite- and fluorite-hosted fluid inclusions and calcite ??18O values, and depositional timing is constrained by the 207Pb/235U ages of chalcedony or opal in the deposits. Fluid inclusion Th from 50 samples of calcite and four samples of fluorite range from ???35 to ???90 ??C. Calcite ??18O values range from ???0 to ???22??? (SMOW) but most fall between 12 and 20???. The highest Th and the lowest ??18O values are found in the older calcite. Calcite Th and ??18O values indicate that most calcite precipitated from water with ??18O values between -13 and -7???, similar to modern meteoric waters. Twenty-two 207Pb/235U ages of chalcedony or opal that generally postdate elevated depositional temperatures range from ???9.5 to 1.9 Ma. New and published 207Pb/235U and 230Th/Uages coupled with the Th values and estimates of temperature from calcite ??18O values indicate that maximum unsaturated zone temperatures probably predate ???10 Ma and that the unsaturated zone had cooled to near-present-day temperatures (24-26 ??C at a depth of 250 m) by 2-4 Ma. The evidence of elevated temperatures persisting in ash flow tuffs adjacent to parent calderas for as much as ???8 Ma is a new finding, but consistent with thermal modeling. Simulations using the HEAT code demonstrate that prolonged cooling of the unsaturated zone is consistent with magmatic heat inputs and deep-seated (sub-water table) hydrothermal activity generated by the large magma body ???8 km to the north that produced the 15-11 Ma ash flows and ash falls that make up Yucca Mountain. The evidence discussed in this and preceding papers strongly supports unsaturated zone deposition of the secondary minerals from descending meteoric waters. Although depositional temperatures reflect conductive (and possibly vapor-phase convective) heating of the unsaturated zone related to regional magmatic sources until perhaps 6 Ma, depositional conditions similar to the present-day unsaturated zone have prevailed for at least the past 2-4 Ma.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Applied Geochemistry","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.apgeochem.2007.08.009","issn":"08832927","usgsCitation":"Whelan, J.F., Neymark, L., Moscati, R., Marshall, B., and Roedder, E., 2008, Thermal history of the unsaturated zone at Yucca Mountain, Nevada, USA: Applied Geochemistry, v. 23, no. 5, p. 1041-1075, https://doi.org/10.1016/j.apgeochem.2007.08.009.","startPage":"1041","endPage":"1075","numberOfPages":"35","costCenters":[],"links":[{"id":214588,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.apgeochem.2007.08.009"},{"id":242327,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"23","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb226e4b08c986b32561e","contributors":{"authors":[{"text":"Whelan, J. F.","contributorId":45328,"corporation":false,"usgs":true,"family":"Whelan","given":"J.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":434125,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Neymark, L.A. 0000-0003-4190-0278","orcid":"https://orcid.org/0000-0003-4190-0278","contributorId":56673,"corporation":false,"usgs":true,"family":"Neymark","given":"L.A.","affiliations":[],"preferred":false,"id":434126,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Moscati, R.J.","contributorId":27882,"corporation":false,"usgs":true,"family":"Moscati","given":"R.J.","affiliations":[],"preferred":false,"id":434124,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Marshall, B.D.","contributorId":19581,"corporation":false,"usgs":true,"family":"Marshall","given":"B.D.","email":"","affiliations":[],"preferred":false,"id":434123,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Roedder, E.","contributorId":100986,"corporation":false,"usgs":true,"family":"Roedder","given":"E.","affiliations":[],"preferred":false,"id":434127,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70033145,"text":"70033145 - 2008 - Complex seasonal patterns of primary producers at the land-sea interface","interactions":[],"lastModifiedDate":"2018-10-17T10:28:02","indexId":"70033145","displayToPublicDate":"2008-01-01T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1466,"text":"Ecology Letters","active":true,"publicationSubtype":{"id":10}},"title":"Complex seasonal patterns of primary producers at the land-sea interface","docAbstract":"<div class=\"abstract-group\"><div class=\"article-section__content en main\"><p>Seasonal fluctuations of plant biomass and photosynthesis are key features of the Earth system because they drive variability of atmospheric CO<sub>2</sub>, water and nutrient cycling, and food supply to consumers. There is no inventory of phytoplankton seasonal cycles in nearshore coastal ecosystems where forcings from ocean, land and atmosphere intersect. We compiled time series of phytoplankton biomass (chlorophyll<span>&nbsp;</span><i>a</i>) from 114 estuaries, lagoons, inland seas, bays and shallow coastal waters around the world, and searched for seasonal patterns as common timing and amplitude of monthly variability. The data revealed a broad continuum of seasonal patterns, with large variability across and within ecosystems. This contrasts with annual cycles of terrestrial and oceanic primary producers for which seasonal fluctuations are recurrent and synchronous over large geographic regions. This finding bears on two fundamental ecological questions: (1) how do estuarine and coastal consumers adapt to an irregular and unpredictable food supply, and (2) how can we extract signals of climate change from phytoplankton observations in coastal ecosystems where local‐scale processes can mask responses to changing climate?</p></div></div>","language":"English","publisher":"Wiley","doi":"10.1111/j.1461-0248.2008.01244.x","issn":"14610","usgsCitation":"Cloern, J., and Jassby, A., 2008, Complex seasonal patterns of primary producers at the land-sea interface: Ecology Letters, v. 11, no. 12, p. 1294-1303, https://doi.org/10.1111/j.1461-0248.2008.01244.x.","productDescription":"10 p.","startPage":"1294","endPage":"1303","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true},{"id":552,"text":"San Francisco Bay-Delta","active":false,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true},{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true}],"links":[{"id":241122,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":213493,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1111/j.1461-0248.2008.01244.x"}],"volume":"11","issue":"12","noUsgsAuthors":false,"publicationDate":"2008-11-05","publicationStatus":"PW","scienceBaseUri":"5059f910e4b0c8380cd4d3f5","contributors":{"authors":[{"text":"Cloern, J. E.","contributorId":59453,"corporation":false,"usgs":true,"family":"Cloern","given":"J. E.","affiliations":[],"preferred":false,"id":439562,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jassby, A.D.","contributorId":43798,"corporation":false,"usgs":true,"family":"Jassby","given":"A.D.","affiliations":[],"preferred":false,"id":439561,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70032043,"text":"70032043 - 2008 - Using semi-permeable membrane devices and stable nitrogen isotopes to detect anthropogenic influences on the Truckee River, USA","interactions":[],"lastModifiedDate":"2012-03-12T17:21:28","indexId":"70032043","displayToPublicDate":"2008-01-01T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1535,"text":"Environmental Engineering Science","active":true,"publicationSubtype":{"id":10}},"title":"Using semi-permeable membrane devices and stable nitrogen isotopes to detect anthropogenic influences on the Truckee River, USA","docAbstract":"Stable nitrogen isotopes (??15N) and semipermeable membrane devices (SPMDs) were used together to provide evidence of potential anthropogenic connections to aquatic organisms in the Truckee River, which flows through the Reno/Sparks metropolitan area in Nevada. Crayfish, snail, and periphyton ??15N values, and SPMD toxicity data collected during high and low flow periods at seven primary sites on the river were used with water quality and flow data for the assessment. All biota showed an increase of ??15N on both dates at sites downstream of inflows of a water-quality impaired tributary and urban drain relative to upstream. In addition, most of the lowest ??15N values on each date occurred at the most downstream site on the river. SPMDs sample lipophilic organic contaminants and can be used to assess organic contaminant toxicity to aquatic organisms because they use a membrane that mimics organic contaminant uptake by fish. In this study, results from a fluoroscan test [pyrene index (PI)] of SPMD extracts that responds to higher molecular weight polycyclic aromatic hydrocarbons (PAHs) showed patterns similar to stable isotope data, although observed peaks in PI values occurred in the urban area upstream of where peak ??15N values occurred. The CYP1A biomarker test, which responds to PAHs, certain polychlorinated biphenyls (PCBs), and organochlorines, showed peak toxic equivalents (TEQ) values farther downstream of the urban area. Thus, it is likely that PAHs were contributing to toxicity in the urban area, whereas other nonurban sources of organic carbon may have been present farther downstream. The combined use of stable isotope measurements and SPMDs provided a means of simultaneously examining whether aquatic biota are incorporating constituents from potential food sources (via stable isotopes) or exposure through water (via SPMDs). ?? Mary Ann Liebert, Inc. 2008.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Environmental Engineering Science","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1089/ees.2007.0090","issn":"10928758","usgsCitation":"Saito, L., Rosen, M.R., Chandra, S., Fritsen, C., Arufe, J., and Redd, C., 2008, Using semi-permeable membrane devices and stable nitrogen isotopes to detect anthropogenic influences on the Truckee River, USA: Environmental Engineering Science, v. 25, no. 4, p. 585-600, https://doi.org/10.1089/ees.2007.0090.","startPage":"585","endPage":"600","numberOfPages":"16","costCenters":[],"links":[{"id":214590,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1089/ees.2007.0090"},{"id":242329,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"25","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bc09ce4b08c986b32a20e","contributors":{"authors":[{"text":"Saito, L.","contributorId":59402,"corporation":false,"usgs":true,"family":"Saito","given":"L.","email":"","affiliations":[],"preferred":false,"id":434288,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rosen, Michael R.","contributorId":43096,"corporation":false,"usgs":true,"family":"Rosen","given":"Michael","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":434285,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Chandra, S.","contributorId":68867,"corporation":false,"usgs":true,"family":"Chandra","given":"S.","email":"","affiliations":[],"preferred":false,"id":434289,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Fritsen, C.H.","contributorId":43979,"corporation":false,"usgs":true,"family":"Fritsen","given":"C.H.","email":"","affiliations":[],"preferred":false,"id":434286,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Arufe, J.A.","contributorId":53184,"corporation":false,"usgs":true,"family":"Arufe","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":434287,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Redd, C.","contributorId":26514,"corporation":false,"usgs":true,"family":"Redd","given":"C.","email":"","affiliations":[],"preferred":false,"id":434284,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70033620,"text":"70033620 - 2008 - Mercury and organic carbon dynamics during runoff episodes from a northeastern USA watershed","interactions":[],"lastModifiedDate":"2018-10-22T08:39:36","indexId":"70033620","displayToPublicDate":"2008-01-01T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3728,"text":"Water, Air, & Soil Pollution","onlineIssn":"1573-2932","printIssn":"0049-6979","active":true,"publicationSubtype":{"id":10}},"title":"Mercury and organic carbon dynamics during runoff episodes from a northeastern USA watershed","docAbstract":"<p class=\"Para\">Mercury and organic carbon concentrations vary dynamically in streamwater at the Sleepers River Research Watershed in Vermont, USA. Total mercury (THg) concentrations ranged from 0.53 to 93.8&nbsp;ng/L during a 3-year period of study. The highest mercury (Hg) concentrations occurred slightly before peak flows and were associated with the highest organic carbon (OC) concentrations. Dissolved Hg (DHg) was the dominant form in the upland catchments; particulate Hg (PHg) dominated in the lowland catchments. The concentration of hydrophobic acid (HPOA), the major component of dissolved organic carbon (DOC), explained 41–98% of the variability of DHg concentration while DOC flux explained 68–85% of the variability in DHg flux, indicating both quality and quantity of the DOC substantially influenced the transport and fate of DHg. Particulate organic carbon (POC) concentrations explained 50% of the PHg variability, indicating that POC is an important transport mechanism for PHg. Despite available sources of DHg and wetlands in the upland catchments, dissolved methylmercury (DmeHg) concentrations in streamwaters were below detection limit (0.04&nbsp;ng/L). PHg and particulate methylmercury (PmeHg) had a strong positive correlation (<i class=\"EmphasisTypeItalic \">r</i><span>&nbsp;</span><sup>2</sup> = 0.84,<span>&nbsp;</span><i class=\"EmphasisTypeItalic \">p</i> &lt; 0.0001), suggesting a common source; likely in-stream or near-stream POC eroded or re-suspended during spring snowmelt and summer storms. Ratios of PmeHg to THg were low and fairly constant despite an apparent higher methylmercury (meHg) production potential in the summer. Methylmercury production in soils and stream sediments was below detection during snowmelt in April and highest in stream sediments (compared to forest and wetland soils) sampled in July. Using the watershed approach, the correlation of the percent of wetland cover to TmeHg concentrations in streamwater indicates that poorly drained wetland soils are a source of meHg and the relatively high concentrations found in stream surface sediments in July indicate these zones are a meHg sink.</p><div class=\"KeywordGroup\" lang=\"en\"><br data-mce-bogus=\"1\"></div>","language":"English","publisher":"Springer","doi":"10.1007/s11270-007-9500-3","issn":"00496979","usgsCitation":"Schuster, P., Shanley, J.B., Marvin-DiPasquale, M., Reddy, M., Aiken, G., Roth, D., Taylor, H.E., Krabbenhoft, D., and DeWild, J., 2008, Mercury and organic carbon dynamics during runoff episodes from a northeastern USA watershed: Water, Air, & Soil Pollution, v. 187, no. 1-4, p. 89-108, https://doi.org/10.1007/s11270-007-9500-3.","productDescription":"20 p.","startPage":"89","endPage":"108","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":242287,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":214552,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/s11270-007-9500-3"}],"volume":"187","issue":"1-4","noUsgsAuthors":false,"publicationDate":"2007-10-12","publicationStatus":"PW","scienceBaseUri":"505a53dce4b0c8380cd6cd7d","contributors":{"authors":[{"text":"Schuster, P. F.","contributorId":30197,"corporation":false,"usgs":true,"family":"Schuster","given":"P. F.","affiliations":[],"preferred":false,"id":441705,"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":441707,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Marvin-DiPasquale, M.","contributorId":28367,"corporation":false,"usgs":true,"family":"Marvin-DiPasquale","given":"M.","affiliations":[],"preferred":false,"id":441704,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Reddy, M.M.","contributorId":24363,"corporation":false,"usgs":true,"family":"Reddy","given":"M.M.","email":"","affiliations":[],"preferred":false,"id":441703,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Aiken, G. R. 0000-0001-8454-0984","orcid":"https://orcid.org/0000-0001-8454-0984","contributorId":14452,"corporation":false,"usgs":true,"family":"Aiken","given":"G. R.","affiliations":[],"preferred":false,"id":441702,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Roth, D.A.","contributorId":100864,"corporation":false,"usgs":true,"family":"Roth","given":"D.A.","email":"","affiliations":[],"preferred":false,"id":441710,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Taylor, Howard E. hetaylor@usgs.gov","contributorId":1551,"corporation":false,"usgs":true,"family":"Taylor","given":"Howard","email":"hetaylor@usgs.gov","middleInitial":"E.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":441706,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Krabbenhoft, D. P. 0000-0003-1964-5020","orcid":"https://orcid.org/0000-0003-1964-5020","contributorId":90765,"corporation":false,"usgs":true,"family":"Krabbenhoft","given":"D. P.","affiliations":[],"preferred":false,"id":441709,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"DeWild, J.F. 0000-0003-4097-2798 jfdewild@usgs.gov","orcid":"https://orcid.org/0000-0003-4097-2798","contributorId":56375,"corporation":false,"usgs":true,"family":"DeWild","given":"J.F.","email":"jfdewild@usgs.gov","affiliations":[],"preferred":false,"id":441708,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}}
,{"id":70030548,"text":"70030548 - 2008 - High-resolution foraminiferal, isotopic, and trace element records from holocene estuarine deposits of San Francisco Bay, California","interactions":[],"lastModifiedDate":"2012-03-12T17:21:04","indexId":"70030548","displayToPublicDate":"2008-01-01T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"High-resolution foraminiferal, isotopic, and trace element records from holocene estuarine deposits of San Francisco Bay, California","docAbstract":"A 3.5-m gravity core (DJ6-93SF-6) from San Francisco Bay reveals a complex paleoclimatic history of the region over the last 3870 cal YBP. A polynomial equation based on 11 AMS 14C ages provides an excellent age model for the core, and environmental proxies for water temperature and salinity are derived from various foraminiferal abundances, stable carbon and oxygen isotopes, and Mg/Ca ratios. Two foraminiferal associations were identified by Q-mode cluster analysis: a colder-water Elphidium excavatum association and the warmer-water Ammonia beccarii-Elphidium gunteri association. The E. excavatum association dominates the core for all but about 600 years out of the last four millennia. At 3870 cal YBP, water temperatures were warm (13.9??C) and freshwater inflow was reduced compared with today. From 3590 to 2860 cal YBP, temperatures dropped 0.5??C and the climate remained dry. This was followed by a period of pronounced lower ??13C values, indicating that conditions became considerably wetter from 2860 to 2170 cal YBP. During this interval, the temperature oscillated frequently, peaking at 13.9??C at 2710 cal YBP, then dropping shortly thereafter to 12.8??C at 2420 cal YBP. Freshwater inflow gradually decreased between 2170 and 1950 cal YBP with a minimal rise in temperature, then changed quickly to colder and wetter conditions at 1900 cal YBP. Drier conditions then prevailed until 1480 cal YBP with water temperatures fluctuating between 13.1??C and 13.8??C, followed by wetter climate from 1480 to 1320 cal YBP. A significant faunal shift from the E. excavatum association to the A. beccarii-E. gunteri association occurred from 1250 to 650 cal YBP, possibly due to regional warming, decreased oxygen availability, and/or a change in the phyto-plankton community. Associated with this change in faunal composition were warm and dry conditions, representative of the Medieval Warm Period (Medieval Climatic Anomaly). A climatic shift coincident with the onset of the Little Ice Age (LIA I and LIA II) is evident from 650 to 280 cal YBP, with the return of the E. excavatum association and an extreme drop in ??18O values, all indicating increased precipitation and fresh water inflow. This was followed by generally drier conditions to the present, except for a brief wet period around 100 cal YBP, and fairly consistent water temperatures in the middle 13??C, except for a drop to 12.8??C at 200 cal YBP. Two significant faunal changes occur near the top of the core. First, there is the reappearance of the A. beccarii-E. gunteri association, suggesting that, once again, regional warming has taken place, oxygen availability has declined, and/or environmental conditions changed such that diatoms have become a scarce food source. Second, there is the first appearance of the invasive Japanese foraminifera Trochammina hadai Uchio, a species that commonly lives in highly polluted areas and is an indicator of eutrophication in its native estuaries. At the same time, freshwater inflow decreased, which may be explained by global warming during the last 100 years, or more likely due to modern water diversion for agriculture in the central valley of California. ADDITIONAL INDEX WORDS: Climate, San Francisco Bay, Holocene, foraminifers, isotopes, trace metals, Medieval Warm Period, Little Ice Age.","largerWorkTitle":"Journal of Coastal Research","language":"English","doi":"10.2112/08A-0003.1","issn":"07490","usgsCitation":"McGann, M., 2008, High-resolution foraminiferal, isotopic, and trace element records from holocene estuarine deposits of San Francisco Bay, California, <i>in</i> Journal of Coastal Research, v. 24, no. 5, p. 1092-1109, https://doi.org/10.2112/08A-0003.1.","startPage":"1092","endPage":"1109","numberOfPages":"18","costCenters":[],"links":[{"id":211756,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.2112/08A-0003.1"},{"id":239107,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"24","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3100e4b0c8380cd5db52","contributors":{"authors":[{"text":"McGann, M. 0000-0002-3057-2945","orcid":"https://orcid.org/0000-0002-3057-2945","contributorId":49125,"corporation":false,"usgs":true,"family":"McGann","given":"M.","affiliations":[],"preferred":false,"id":427601,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70031990,"text":"70031990 - 2008 - Age and growth of the knobbed whelk Busycon carica (Gmelin 1791) in South Carolina subtidal waters","interactions":[],"lastModifiedDate":"2012-03-12T17:21:28","indexId":"70031990","displayToPublicDate":"2008-01-01T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2455,"text":"Journal of Shellfish Research","active":true,"publicationSubtype":{"id":10}},"title":"Age and growth of the knobbed whelk Busycon carica (Gmelin 1791) in South Carolina subtidal waters","docAbstract":"Knobbed whelk, Busycon carica (Gmelin, 1791), age and growth were estimated using tagged and recaptured individuals (n = 396) from areas off South Carolina coastal islands. Recaptured whelks were at large an average of 298 d (4-2,640 d). Growth, an increase in shell length (SL), was evident in 24% of the recaptured whelks, whereas 29% of recaptured individuals were the same size as when released and 47% were smaller than the released size. Mean growth rate was <0.001 mm SL/d and 0.022 mm SL/d if decreases in SL were assumed to be zero. Smaller whelks (???90 mm SL) at large for over one year grew seven times faster than larger whelks. The von Bertalanffy growth model: SL1 = 159.5(1 - e-0.0765(t+0.4162)), was developed from the mark - recapture whelks exhibiting growth. Based on a South Carolina minimum legal size of 102 mm SL, whelks recruit into the fishery at 13 y of age. The longevity, large size at maturity and slow growth suggest the potential for over harvest of knobbed whelk. Future whelk management plans may wish to consider whether economically viable commercial harvest can be sustainable.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Shellfish Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.2983/0730-8000(2008)27[423:AAGOTK]2.0.CO;2","issn":"07308000","usgsCitation":"Eversole, A., Anderson, W., and Isely, J.J., 2008, Age and growth of the knobbed whelk Busycon carica (Gmelin 1791) in South Carolina subtidal waters: Journal of Shellfish Research, v. 27, no. 2, p. 423-426, https://doi.org/10.2983/0730-8000(2008)27[423:AAGOTK]2.0.CO;2.","startPage":"423","endPage":"426","numberOfPages":"4","costCenters":[],"links":[{"id":214778,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.2983/0730-8000(2008)27[423:AAGOTK]2.0.CO;2"},{"id":242528,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"27","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e8dbe4b0c8380cd47f0d","contributors":{"authors":[{"text":"Eversole, A.G.","contributorId":99727,"corporation":false,"usgs":true,"family":"Eversole","given":"A.G.","email":"","affiliations":[],"preferred":false,"id":434021,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Anderson, W.D.","contributorId":89735,"corporation":false,"usgs":true,"family":"Anderson","given":"W.D.","email":"","affiliations":[],"preferred":false,"id":434019,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Isely, J. Jeffery","contributorId":97224,"corporation":false,"usgs":true,"family":"Isely","given":"J.","email":"","middleInitial":"Jeffery","affiliations":[],"preferred":false,"id":434020,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70032002,"text":"70032002 - 2008 - Comparison of macroinvertebrate-derived stream quality metrics between snag and riffle habitats","interactions":[],"lastModifiedDate":"2012-03-12T17:21:26","indexId":"70032002","displayToPublicDate":"2008-01-01T00:00:00","publicationYear":"2008","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":"Comparison of macroinvertebrate-derived stream quality metrics between snag and riffle habitats","docAbstract":"We compared benthic macroinvertebrate assemblage structure at snag and riffle habitats in 43 Wisconsin streams across a range of watershed urbanization using a variety of stream quality metrics. Discriminant analysis indicated that dominant taxa at riffles and snags differed; Hydropsychid caddisflies (Hydropsyche betteni and Cheumatopsyche spp.) and elmid beetles (Optioservus spp. and Stenemlis spp.) typified riffles, whereas isopods (Asellus intermedius) and amphipods (Hyalella azteca and Gammarus pseudolimnaeus) predominated in snags. Analysis of covariance indicated that samples from snag and riffle habitats differed significantly in their response to the urbanization gradient for the Hilsenhoff biotic index (BI), Shannon's diversity index, and percent of filterers, shredders, and pollution intolerant Ephemeroptera, Plecoptera, and Trichoptera (EPT) at each stream site (p ??? 0.10). These differences suggest that although macroinvertebrate assemblages present in either habitat type are sensitive to detecting the effects of urbanization, metrics derived from different habitats should not be intermixed when assessing stream quality through biomonitoring. This can be a limitation to resource managers who wish to compare water quality among streams where the same habitat type is not available at all stream locations, or where a specific habitat type (i.e., a riffle) is required to determine a metric value (i.e., BI). To account for differences in stream quality at sites lacking riffle habitat, snag-derived metric values can be adjusted based on those obtained from riffles that have been exposed to the same level of urbanization. Comparison of nonlinear regression equations that related stream quality metric values from the two habitat types to percent watershed urbanization indicated that snag habitats had on average 30.2 fewer percent EPT individuals, a lower diversity index value than riffles, and a BI value of 0.29 greater than riffles. ?? 2008 American Water Resources Association.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of the American Water Resources Association","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1111/j.1752-1688.2008.00197.x","issn":"1093474X","usgsCitation":"Stepenuck, K., Crunkilton, R., Bozek, M.A., and Wang, L., 2008, Comparison of macroinvertebrate-derived stream quality metrics between snag and riffle habitats: Journal of the American Water Resources Association, v. 44, no. 3, p. 670-678, https://doi.org/10.1111/j.1752-1688.2008.00197.x.","startPage":"670","endPage":"678","numberOfPages":"9","costCenters":[],"links":[{"id":476778,"rank":10000,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"http://hdl.handle.net/2027.42/74406>","text":"External Repository"},{"id":214995,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1111/j.1752-1688.2008.00197.x"},{"id":242759,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"44","issue":"3","noUsgsAuthors":false,"publicationDate":"2008-05-16","publicationStatus":"PW","scienceBaseUri":"5059f870e4b0c8380cd4d0e2","contributors":{"authors":[{"text":"Stepenuck, K.F.","contributorId":72975,"corporation":false,"usgs":true,"family":"Stepenuck","given":"K.F.","affiliations":[],"preferred":false,"id":434094,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Crunkilton, R.L.","contributorId":58048,"corporation":false,"usgs":true,"family":"Crunkilton","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":434093,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bozek, Michael A.","contributorId":51030,"corporation":false,"usgs":true,"family":"Bozek","given":"Michael","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":434092,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Wang, L.","contributorId":76904,"corporation":false,"usgs":true,"family":"Wang","given":"L.","email":"","affiliations":[],"preferred":false,"id":434095,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70032207,"text":"70032207 - 2008 - Wetlands as principal zones of methylmercury production in southern Louisiana and the Gulf of Mexico region","interactions":[],"lastModifiedDate":"2018-10-17T08:14:29","indexId":"70032207","displayToPublicDate":"2008-01-01T00:00:00","publicationYear":"2008","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":"Wetlands as principal zones of methylmercury production in southern Louisiana and the Gulf of Mexico region","docAbstract":"<p>It is widely recognized that wetlands, especially those rich in organic matter and receiving appreciable atmospheric mercury (Hg) inputs, are important sites of methylmercury (MeHg) production. Extensive wetlands in the southeastern United States have many ecosystem attributes ideal for promoting high MeHg production rates; however, relatively few mercury cycling studies have been conducted in these environments. We conducted a landscape scale study examining Hg cycling in coastal Louisiana (USA) including four field trips conducted between August 2003 and May 2005. Sites were chosen to represent different ecosystem types, including: a large shallow eutrophic estuarine lake (Lake Pontchartrain), three rivers draining into the lake, a cypress-tupelo dominated freshwater swamp, and six emergent marshes ranging from a freshwater marsh dominated by<span>&nbsp;</span><i>Panicum hemitomon</i><span>&nbsp;</span>to a<span>&nbsp;</span><i>Spartina alterniflora</i><span>&nbsp;</span>dominated salt marsh close to the Gulf of Mexico. We measured MeHg and total Hg (THg) concentrations, and ancillary chemical characteristics, in whole and filtered surface water, and filtered porewater.</p><p>Overall, MeHg concentrations were greatest in surface water of freshwater wetlands and lowest in the profundal (non-vegetated) regions of the lake and river mainstems. Concentrations of THg and MeHg in filtered surface water were positively correlated with the highly reactive, aromatic (hydrophobic organic acid) fraction of dissolved organic carbon (DOC). These results suggest that DOC plays an important role in promoting the mobility, transport and bioavailability of inorganic Hg in these environments. Further, elevated porewater concentrations in marine and brackish wetlands suggest coastal wetlands along the Gulf Coast are key sites for MeHg production and may be a principal source of MeHg to foodwebs in the Gulf of Mexico.</p><p>Examining the relationships among MeHg, THg, and DOC across these multiple landscape types is a first step in evaluating possible links between key zones for Hg(II)-methylation and the bioaccumulation of mercury in the biota inhabiting the Gulf of Mexico region</p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.envpol.2007.12.017","issn":"02697491","usgsCitation":"Hall, B., Aiken, G., Krabbenhoft, D., Marvin-DiPasquale, M., and Swarzenski, C., 2008, Wetlands as principal zones of methylmercury production in southern Louisiana and the Gulf of Mexico region: Environmental Pollution, v. 154, no. 1, p. 124-134, https://doi.org/10.1016/j.envpol.2007.12.017.","productDescription":"11 p.","startPage":"124","endPage":"134","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":242802,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":215035,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.envpol.2007.12.017"}],"volume":"154","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bd028e4b08c986b32ecd6","contributors":{"authors":[{"text":"Hall, B.D.","contributorId":42408,"corporation":false,"usgs":true,"family":"Hall","given":"B.D.","email":"","affiliations":[],"preferred":false,"id":435035,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Aiken, G. R. 0000-0001-8454-0984","orcid":"https://orcid.org/0000-0001-8454-0984","contributorId":14452,"corporation":false,"usgs":true,"family":"Aiken","given":"G. R.","affiliations":[],"preferred":false,"id":435033,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Krabbenhoft, D. P. 0000-0003-1964-5020","orcid":"https://orcid.org/0000-0003-1964-5020","contributorId":90765,"corporation":false,"usgs":true,"family":"Krabbenhoft","given":"D. P.","affiliations":[],"preferred":false,"id":435037,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Marvin-DiPasquale, M.","contributorId":28367,"corporation":false,"usgs":true,"family":"Marvin-DiPasquale","given":"M.","affiliations":[],"preferred":false,"id":435034,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Swarzenski, C.M.","contributorId":74856,"corporation":false,"usgs":true,"family":"Swarzenski","given":"C.M.","email":"","affiliations":[],"preferred":false,"id":435036,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70032203,"text":"70032203 - 2008 - The effect of variations in relative spectral response on the retrieval of land surface parameters from multiple sources of remotely sensed imagery","interactions":[],"lastModifiedDate":"2022-05-18T14:44:49.389973","indexId":"70032203","displayToPublicDate":"2008-01-01T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"The effect of variations in relative spectral response on the retrieval of land surface parameters from multiple sources of remotely sensed imagery","docAbstract":"<div class=\"abstract-text row\"><div class=\"col-12\"><div class=\"u-mb-1\"><div>Airborne visible infrared imaging spectrometer (AVIRIS) images, collected over Sioux Falls, South Dakota, were used to quantify the effect of spectral response on different surface materials and to develop spectral \"figures-of-merit\" for spectral responses covering similar, but not identical spectral bands. In this simulation, AVIRIS images were converted to radiance, then spectrally resampled to six wavelength bands commonly used for terrestrial observation. Preliminary results indicate that differences between the simulations can be attributed to variations in surface reflectance within spectral bands, and suggest influences due to water vapor absorption. Radiance simulated from the spectrally narrow Moderate Resolution Imaging Spectroradiometer (MODIS) relative spectral responses (RSR) was generally higher than that using the broader Enhanced Thematic Mapper Plus (ETM+) RSRs over most targets encountered over the test area. This is consistent with many MODIS bands being biased toward shorter wavelengths compared to corresponding ETM+ bands when viewing targets whose radiance decreases with wavelength. In some cases the higher radiance values appeared to occur where the MODIS RSR is better situated over peak reflected wavelengths. Simulation differences between MODIS &amp; ETM+ bands in the near-infrared indicated higher MODIS radiance values that suggest the influence of water vapor absorption at 820 nanometers. This result agreed with water vapor values retrieved from the AVIRIS images themselves at around 2.7 cm precipitable water, and measurements made at a nearby AERONET node at around 2.8 cm during the AVIRIS overflight.</div></div></div></div>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"International Geoscience and Remote Sensing Symposium (IGARSS)","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"2007 IEEE International Geoscience and Remote Sensing Symposium, IGARSS 2007","conferenceDate":"Jun 23-28, 2007","conferenceLocation":"Barcelona, Spain","language":"English","publisher":"IEEE","doi":"10.1109/IGARSS.2007.4424021","usgsCitation":"Meyer, D.J., and Chander, G., 2008, The effect of variations in relative spectral response on the retrieval of land surface parameters from multiple sources of remotely sensed imagery, <i>in</i> International Geoscience and Remote Sensing Symposium (IGARSS), Barcelona, Spain, Jun 23-28, 2007, p. 5150-5153, https://doi.org/10.1109/IGARSS.2007.4424021.","productDescription":"4 p.","startPage":"5150","endPage":"5153","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":242738,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bab60e4b08c986b322dd1","contributors":{"authors":[{"text":"Meyer, D. J.","contributorId":46721,"corporation":false,"usgs":true,"family":"Meyer","given":"D.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":435026,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Chander, G.","contributorId":51449,"corporation":false,"usgs":true,"family":"Chander","given":"G.","affiliations":[],"preferred":false,"id":435027,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70032003,"text":"70032003 - 2008 - Origins of sediment-associated contaminants to the Marais Vernier, the Seine Estuary, France","interactions":[],"lastModifiedDate":"2012-03-12T17:21:26","indexId":"70032003","displayToPublicDate":"2008-01-01T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3728,"text":"Water, Air, & Soil Pollution","onlineIssn":"1573-2932","printIssn":"0049-6979","active":true,"publicationSubtype":{"id":10}},"title":"Origins of sediment-associated contaminants to the Marais Vernier, the Seine Estuary, France","docAbstract":"The Marais Vernier is the largest freshwater wetland in the Seine Estuary in northern France. It is in a heavily urbanized and industrialized region and could be affected by atmospheric deposition and by fluvial input of contaminants in water diverted from the Seine River. To evaluate contaminant histories in the wetland and the region, sediment cores were collected from two open-water ponds in the Marais Vernier: the Grand-Mare, which was connected to the Seine by a canal from 1950 to 1996, and the Petite Mare, which has a small rural watershed. Diversions from the Seine to the Grand-Mare increased sedimentation rates but mostly resulted in low contaminant concentrations and loading rates, indicating that the sediment from the Seine was predominantly brought upstream by tidal currents from the estuary and was not from the watershed. Atmospheric sources of metals dominate inputs to the Petite Mare; however, runoff of metals from vehicle-related sources in the watershed might contribute to the upward trends in concentrations of Cr, Cu, and Zn. Estimates of atmospheric deposition using the Petite Mare core are consistent with measured deposition in the region and are mixed (similar for Hg and Pb; larger for Cd, Cu, and Zn) compared with deposition estimated from sediment cores in the northeastern United States. A local source of PAHs in the watershed of the Petite Mare is indicated by higher concentrations, higher accumulation rates, and a different, more petrogenic, PAH assemblage than in the Grand-Mare. The study illustrates how diverse sources and transport pathways can affect wetlands in industrial regions and can be evaluated using sediment cores from the wetland ponds. ?? 2008 Springer Science+Business Media B.V.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Water, Air, and Soil Pollution","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1007/s11270-008-9628-9","issn":"00496979","usgsCitation":"Van Metre, P., Mesnage, V., Laignel, B., Motelay, A., and Deloffre, J., 2008, Origins of sediment-associated contaminants to the Marais Vernier, the Seine Estuary, France: Water, Air, & Soil Pollution, v. 191, no. 1-4, p. 331-344, https://doi.org/10.1007/s11270-008-9628-9.","startPage":"331","endPage":"344","numberOfPages":"14","costCenters":[],"links":[{"id":214996,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/s11270-008-9628-9"},{"id":242760,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"191","issue":"1-4","noUsgsAuthors":false,"publicationDate":"2008-02-20","publicationStatus":"PW","scienceBaseUri":"505a711ce4b0c8380cd76468","contributors":{"authors":[{"text":"Van Metre, P. C.","contributorId":92999,"corporation":false,"usgs":true,"family":"Van Metre","given":"P. C.","affiliations":[],"preferred":false,"id":434100,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mesnage, V.","contributorId":42101,"corporation":false,"usgs":true,"family":"Mesnage","given":"V.","email":"","affiliations":[],"preferred":false,"id":434097,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Laignel, B.","contributorId":83804,"corporation":false,"usgs":true,"family":"Laignel","given":"B.","affiliations":[],"preferred":false,"id":434099,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Motelay, A.","contributorId":82191,"corporation":false,"usgs":true,"family":"Motelay","given":"A.","email":"","affiliations":[],"preferred":false,"id":434098,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Deloffre, J.","contributorId":39254,"corporation":false,"usgs":true,"family":"Deloffre","given":"J.","email":"","affiliations":[],"preferred":false,"id":434096,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70032005,"text":"70032005 - 2008 - Influence of sulfate input on freshwater sediments: Insights from incubation experiments","interactions":[],"lastModifiedDate":"2012-03-12T17:21:26","indexId":"70032005","displayToPublicDate":"2008-01-01T00:00:00","publicationYear":"2008","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":"Influence of sulfate input on freshwater sediments: Insights from incubation experiments","docAbstract":"Incubation experiments were carried out under high and low SO42 - conditions to investigate the buffering capacity of lake sediments. Increased SO42 - content in the water column enhanced microbial SO42 - reduction, causing a continuous decrease of SO42 - content from 1086 to 83 mg/L paralleled by an increase of pH in the water column from 3.76 to 7.20. These changes were accompanied by decreased methanogenesis in the incubated sediments. The results demonstrate that the buffering capacity resulted from a variety of biodegradation pathways controlled to a large extent by SO42 - reduction, rather than by direct anaerobic oxidation of CH4. This is documented by distinctly lower ??13C values (from -73.99 to -65.24???) of the CH4 generated under higher SO42 - conditions compared to higher ??13C values (from -68.98 to -61.37???) of the CH4 generated under lower SO42 - conditions. ?? 2008 Elsevier Ltd. All rights reserved.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Applied Geochemistry","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.apgeochem.2007.12.034","issn":"08832927","usgsCitation":"Szynkiewicz, A., Jedrysek, M.O., Kurasiewicz, M., and Mastalerz, M., 2008, Influence of sulfate input on freshwater sediments: Insights from incubation experiments: Applied Geochemistry, v. 23, no. 6, p. 1607-1622, https://doi.org/10.1016/j.apgeochem.2007.12.034.","startPage":"1607","endPage":"1622","numberOfPages":"16","costCenters":[],"links":[{"id":215026,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.apgeochem.2007.12.034"},{"id":242792,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"23","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3b81e4b0c8380cd625c0","contributors":{"authors":[{"text":"Szynkiewicz, Anna","contributorId":39599,"corporation":false,"usgs":true,"family":"Szynkiewicz","given":"Anna","email":"","affiliations":[],"preferred":false,"id":434108,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jedrysek, Mariusz Orion","contributorId":94513,"corporation":false,"usgs":true,"family":"Jedrysek","given":"Mariusz","email":"","middleInitial":"Orion","affiliations":[],"preferred":false,"id":434111,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kurasiewicz, M.","contributorId":47652,"corporation":false,"usgs":true,"family":"Kurasiewicz","given":"M.","email":"","affiliations":[],"preferred":false,"id":434109,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Mastalerz, Maria","contributorId":78065,"corporation":false,"usgs":true,"family":"Mastalerz","given":"Maria","affiliations":[],"preferred":false,"id":434110,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70032012,"text":"70032012 - 2008 - Groundwater chemistry and occurrence of arsenic in the Meghna floodplain aquifer, southeastern Bangladesh","interactions":[],"lastModifiedDate":"2012-03-12T17:21:28","indexId":"70032012","displayToPublicDate":"2008-01-01T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1539,"text":"Environmental Geology","active":true,"publicationSubtype":{"id":10}},"title":"Groundwater chemistry and occurrence of arsenic in the Meghna floodplain aquifer, southeastern Bangladesh","docAbstract":"Dissolved major ions and important heavy metals including total arsenic and iron were measured in groundwater from shallow (25-33 m) and deep (191-318 m) tube-wells in southeastern Bangladesh. These analyses are intended to help describe geochemical processes active in the aquifers and the source and release mechanism of arsenic in sediments for the Meghna Floodplain aquifer. The elevated Cl- and higher proportions of Na+ relative to Ca2+, Mg2+, and K+ in groundwater suggest the influence by a source of Na+ and Cl-. Use of chemical fertilizers may cause higher concentrations of NH 4+ and PO 43- in shallow well samples. In general, most ions are positively correlated with Cl-, with Na+ showing an especially strong correlation with Cl-, indicating that these ions are derived from the same source of saline waters. The relationship between Cl-/HCO 3- ratios and Cl- also shows mixing of fresh groundwater and seawater. Concentrations of dissolved HCO 3- reflect the degree of water-rock interaction in groundwater systems and integrated microbial degradation of organic matter. Mn and Fe-oxyhydroxides are prominent in the clayey subsurface sediment and well known to be strong adsorbents of heavy metals including arsenic. All five shallow well samples had high arsenic concentration that exceeded WHO recommended limit for drinking water. Very low concentrations of SO 42- and NO 3- and high concentrations of dissolved Fe and PO 43- and NH 4+ ions support the reducing condition of subsurface aquifer. Arsenic concentrations demonstrate negative co-relation with the concentrations of SO 42- and NO 3- but correlate weakly with Mo, Fe concentrations and positively with those of P, PO 43- and NH 4+ ions. ?? 2007 Springer-Verlag.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Environmental Geology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1007/s00254-007-0907-3","issn":"09430105","usgsCitation":"Zahid, A., Hassan, M., Balke, K., Flegr, M., and Clark, D., 2008, Groundwater chemistry and occurrence of arsenic in the Meghna floodplain aquifer, southeastern Bangladesh: Environmental Geology, v. 54, no. 6, p. 1247-1260, https://doi.org/10.1007/s00254-007-0907-3.","startPage":"1247","endPage":"1260","numberOfPages":"14","costCenters":[],"links":[{"id":214619,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/s00254-007-0907-3"},{"id":242359,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"54","issue":"6","noUsgsAuthors":false,"publicationDate":"2007-07-13","publicationStatus":"PW","scienceBaseUri":"505a2d95e4b0c8380cd5bf39","contributors":{"authors":[{"text":"Zahid, A.","contributorId":56875,"corporation":false,"usgs":true,"family":"Zahid","given":"A.","email":"","affiliations":[],"preferred":false,"id":434136,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hassan, M.Q.","contributorId":71783,"corporation":false,"usgs":true,"family":"Hassan","given":"M.Q.","email":"","affiliations":[],"preferred":false,"id":434138,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Balke, K.-D.","contributorId":7927,"corporation":false,"usgs":true,"family":"Balke","given":"K.-D.","email":"","affiliations":[],"preferred":false,"id":434134,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Flegr, M.","contributorId":61660,"corporation":false,"usgs":true,"family":"Flegr","given":"M.","email":"","affiliations":[],"preferred":false,"id":434137,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Clark, D.W.","contributorId":22765,"corporation":false,"usgs":true,"family":"Clark","given":"D.W.","email":"","affiliations":[],"preferred":false,"id":434135,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70031980,"text":"70031980 - 2008 - A linked hydrodynamic and water quality model for the Salton Sea","interactions":[],"lastModifiedDate":"2018-02-06T12:19:24","indexId":"70031980","displayToPublicDate":"2008-01-01T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1919,"text":"Hydrobiologia","onlineIssn":"1573-5117","printIssn":"0018-8158","active":true,"publicationSubtype":{"id":10}},"title":"A linked hydrodynamic and water quality model for the Salton Sea","docAbstract":"A linked hydrodynamic and water quality model was developed and applied to the Salton Sea. The hydrodynamic component is based on the one-dimensional numerical model, DLM. The water quality model is based on a new conceptual model for nutrient cycling in the Sea, and simulates temperature, total suspended sediment concentration, nutrient concentrations, including PO4-3, NO3-1 and NH4+1, DO concentration and chlorophyll a concentration as functions of depth and time. Existing water temperature data from 1997 were used to verify that the model could accurately represent the onset and breakup of thermal stratification. 1999 is the only year with a near-complete dataset for water quality variables for the Salton Sea. The linked hydrodynamic and water quality model was run for 1999, and by adjustment of rate coefficients and other water quality parameters, a good match with the data was obtained. In this article, the model is fully described and the model results for reductions in external phosphorus load on chlorophyll a distribution are presented. ?? 2008 Springer Science+Business Media B.V.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Hydrobiologia","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1007/s10750-008-9311-6","issn":"00188158","usgsCitation":"Chung, E., Schladow, S., Perez-Losada, J., and Robertson, D.M., 2008, A linked hydrodynamic and water quality model for the Salton Sea: Hydrobiologia, v. 604, no. 1, p. 57-75, https://doi.org/10.1007/s10750-008-9311-6.","startPage":"57","endPage":"75","numberOfPages":"19","costCenters":[],"links":[{"id":242392,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":214648,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/s10750-008-9311-6"}],"volume":"604","issue":"1","noUsgsAuthors":false,"publicationDate":"2008-03-18","publicationStatus":"PW","scienceBaseUri":"5059e438e4b0c8380cd464f0","contributors":{"authors":[{"text":"Chung, E.G.","contributorId":89773,"corporation":false,"usgs":true,"family":"Chung","given":"E.G.","email":"","affiliations":[],"preferred":false,"id":433987,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schladow, S.G.","contributorId":92791,"corporation":false,"usgs":true,"family":"Schladow","given":"S.G.","email":"","affiliations":[],"preferred":false,"id":433988,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Perez-Losada, J.","contributorId":48054,"corporation":false,"usgs":true,"family":"Perez-Losada","given":"J.","email":"","affiliations":[],"preferred":false,"id":433986,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Robertson, Dale M. 0000-0001-6799-0596 dzrobert@usgs.gov","orcid":"https://orcid.org/0000-0001-6799-0596","contributorId":150760,"corporation":false,"usgs":true,"family":"Robertson","given":"Dale","email":"dzrobert@usgs.gov","middleInitial":"M.","affiliations":[{"id":37947,"text":"Upper Midwest Water Science Center","active":true,"usgs":true}],"preferred":true,"id":433985,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70031974,"text":"70031974 - 2008 - Sandwave migration in Monterey Submarine Canyon, Central California","interactions":[],"lastModifiedDate":"2012-03-12T17:21:54","indexId":"70031974","displayToPublicDate":"2008-01-01T00:00:00","publicationYear":"2008","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":"Sandwave migration in Monterey Submarine Canyon, Central California","docAbstract":"Repeated high-resolution multibeam bathymetric surveys from 2002 through 2006 at the head of the Monterey Submarine Canyon reveal a sandwave field along the canyon axis between 20 and 250??m water depth. These sandwaves range in wavelength from 20 to 70??m and 1 to 3??m in height. A quantitative measure was devised to determine the direction of sandwave migration based on the asymmetry of their profiles. Despite appreciable spatial variation the sandwaves were found to migrate in a predominantly down-canyon direction, regardless of season and tidal phases. A yearlong ADCP measurement at 250??m water depth showed that intermittent internal tidal oscillations dominated the high-speed canyon currents (50-80??cm/s), which are not correlated with the spring-neap tidal cycle. Observed currents of 50??cm/s or higher were predominantly down-canyon. Applying a simple empirical model, flows of such magnitudes were shown to be able to generate sandwaves of a size similar to the observed ones. ?? 2007 Elsevier B.V. All rights reserved.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Marine Geology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.margeo.2007.11.005","issn":"00253227","usgsCitation":"Xu, J.P., Wong, F.L., Kvitek, R., Smith, D., and Paull, C.K., 2008, Sandwave migration in Monterey Submarine Canyon, Central California: Marine Geology, v. 248, no. 3-4, p. 193-212, https://doi.org/10.1016/j.margeo.2007.11.005.","startPage":"193","endPage":"212","numberOfPages":"20","costCenters":[],"links":[{"id":215053,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.margeo.2007.11.005"},{"id":242822,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"248","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b86aee4b08c986b31608d","contributors":{"authors":[{"text":"Xu, J. P.","contributorId":74528,"corporation":false,"usgs":true,"family":"Xu","given":"J.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":433962,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wong, F. L.","contributorId":87515,"corporation":false,"usgs":true,"family":"Wong","given":"F.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":433964,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kvitek, R.","contributorId":65683,"corporation":false,"usgs":true,"family":"Kvitek","given":"R.","email":"","affiliations":[],"preferred":false,"id":433961,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Smith, D.P.","contributorId":64911,"corporation":false,"usgs":true,"family":"Smith","given":"D.P.","email":"","affiliations":[],"preferred":false,"id":433960,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Paull, C. K.","contributorId":86845,"corporation":false,"usgs":false,"family":"Paull","given":"C.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":433963,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70032013,"text":"70032013 - 2008 - A simple model for predicting survival of angler-caught and released largemouth bass","interactions":[],"lastModifiedDate":"2012-03-12T17:21:28","indexId":"70032013","displayToPublicDate":"2008-01-01T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3624,"text":"Transactions of the American Fisheries Society","active":true,"publicationSubtype":{"id":10}},"title":"A simple model for predicting survival of angler-caught and released largemouth bass","docAbstract":"We conducted a controlled experiment in the laboratory to assess the influence of anatomical hooking location and water temperature on survival of angler-caught and released largemouth bass Micropterus salmoides. Survival was 98% (58 of 59 fish) among fish that were hand-hooked within the oral cavity (including the gills), whereas survival was 66% (33 of 50 fish) among fish that were hand-hooked in the esophagus. Survival of hooked fish was not significantly influenced by water temperature (7-27??C) or the hooking location X water temperature interaction. We combined our results with prior research to develop a predictive model of largemouth bass survival, which was 98.3% (SD = 1.87%) for fish hooked in the oral cavity and 55.0% (SD = 9.70%) for fish hooked in the esophagus. The model is valid for water temperatures ranging from 7??C to 27??C and allows one to estimate, with known precision, the survival of angler-caught and released largemouth bass without the need for controlled studies or for holding fish in pens or cages to assess delayed mortality. ?? Copyright by the American Fisheries Society 2008.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Transactions of the American Fisheries Society","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1577/T06-273.1","issn":"00028487","usgsCitation":"Wilde, G., and Pope, K., 2008, A simple model for predicting survival of angler-caught and released largemouth bass: Transactions of the American Fisheries Society, v. 137, no. 3, p. 834-840, https://doi.org/10.1577/T06-273.1.","startPage":"834","endPage":"840","numberOfPages":"7","costCenters":[],"links":[{"id":214649,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1577/T06-273.1"},{"id":242393,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"137","issue":"3","noUsgsAuthors":false,"publicationDate":"2011-01-09","publicationStatus":"PW","scienceBaseUri":"5059e590e4b0c8380cd46e1e","contributors":{"authors":[{"text":"Wilde, G.R.","contributorId":54799,"corporation":false,"usgs":true,"family":"Wilde","given":"G.R.","email":"","affiliations":[],"preferred":false,"id":434140,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pope, K.L.","contributorId":20454,"corporation":false,"usgs":true,"family":"Pope","given":"K.L.","email":"","affiliations":[],"preferred":false,"id":434139,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70032016,"text":"70032016 - 2008 - Analysis of chlorothalonil and three degradates in sediment and soil","interactions":[],"lastModifiedDate":"2018-10-22T08:11:06","indexId":"70032016","displayToPublicDate":"2008-01-01T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2149,"text":"Journal of Agricultural and Food Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"Analysis of chlorothalonil and three degradates in sediment and soil","docAbstract":"<p class=\"articleBody_abstractText\">A method has been developed for the simultaneous extraction of chlorothalonil and three of its degradates (4-hydroxy-2,5,6-trichloroisophthalonitrile, 1-carbamoyl-3-cyano-4-hydroxy-2,5,6-trichlorobenzene, and 1,3-dicarbamoyl-2,4,5,6-tetrachlorobenzene) from soils and sediments; the compounds were extracted using sonication with acetone and isolation of the parent compound and matrix interferences from the degradates by solid phase extraction (SPE). The chlorothalonil fraction underwent further coextracted matrix interference removal with Florisil. The degradates were derivatized with<span>&nbsp;</span><i>N</i>,<i>O-</i>bis(trimethylsilyl) trifluoroacetamide (BSTFA) and chlorotrimethylsilane (TMCS). All compounds were analyzed by gas chromatography–mass spectrometry (GC-MS). Recoveries on a spiked (20 and 200 µg kg<sup>−1</sup>) sediment ranged from 80% to 91% with calculated limits of detection of 1−5 µg kg<sup>−1</sup><span>&nbsp;</span>dry weight sediment. An additional 20 sediment samples were collected in watersheds from the Southeastern United States where chlorothalonil is used widely on peanuts and other crops. None of the target compounds were detected. Laboratory fortified recoveries of chlorothalonil and its degradates in these environmental sediment samples ranged from 75% to 89%.</p>","language":"English","publisher":"ACS","doi":"10.1021/jf703695s","issn":"00218561","usgsCitation":"Hladik, M., and Kuivila, K., 2008, Analysis of chlorothalonil and three degradates in sediment and soil: Journal of Agricultural and Food Chemistry, v. 56, no. 7, p. 2310-2314, https://doi.org/10.1021/jf703695s.","productDescription":"5 p.","startPage":"2310","endPage":"2314","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":242427,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":214681,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1021/jf703695s"}],"volume":"56","issue":"7","noUsgsAuthors":false,"publicationDate":"2008-03-13","publicationStatus":"PW","scienceBaseUri":"5059eb0de4b0c8380cd48ba3","contributors":{"authors":[{"text":"Hladik, M.L. 0000-0002-0891-2712","orcid":"https://orcid.org/0000-0002-0891-2712","contributorId":51111,"corporation":false,"usgs":true,"family":"Hladik","given":"M.L.","affiliations":[],"preferred":false,"id":434149,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kuivila, K.M.","contributorId":34529,"corporation":false,"usgs":true,"family":"Kuivila","given":"K.M.","email":"","affiliations":[],"preferred":false,"id":434148,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70032018,"text":"70032018 - 2008 - Comparison and assessment of aerial and ground estimates of waterbird colonies","interactions":[],"lastModifiedDate":"2012-03-12T17:21:28","indexId":"70032018","displayToPublicDate":"2008-01-01T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2508,"text":"Journal of Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"Comparison and assessment of aerial and ground estimates of waterbird colonies","docAbstract":"Aerial surveys are often used to quantify sizes of waterbird colonies; however, these surveys would benefit from a better understanding of associated biases. We compared estimates of breeding pairs of waterbirds, in colonies across southern Louisiana, USA, made from the ground, fixed-wing aircraft, and a helicopter. We used a marked-subsample method for ground-counting colonies to obtain estimates of error and visibility bias. We made comparisons over 2 sampling periods: 1) surveys conducted on the same colonies using all 3 methods during 3-11 May 2005 and 2) an expanded fixed-wing and ground-survey comparison conducted over 4 periods (May and Jun, 2004-2005). Estimates from fixed-wing aircraft were approximately 65% higher than those from ground counts for overall estimated number of breeding pairs and for both dark and white-plumaged species. The coefficient of determination between estimates based on ground and fixed-wing aircraft was ???0.40 for most species, and based on the assumption that estimates from the ground were closer to the true count, fixed-wing aerial surveys appeared to overestimate numbers of nesting birds of some species; this bias often increased with the size of the colony. Unlike estimates from fixed-wing aircraft, numbers of nesting pairs made from ground and helicopter surveys were very similar for all species we observed. Ground counts by one observer resulted in underestimated number of breeding pairs by 20% on average. The marked-subsample method provided an estimate of the number of missed nests as well as an estimate of precision. These estimates represent a major advantage of marked-subsample ground counts over aerial methods; however, ground counts are difficult in large or remote colonies. Helicopter surveys and ground counts provide less biased, more precise estimates of breeding pairs than do surveys made from fixed-wing aircraft. We recommend managers employ ground counts using double observers for surveying waterbird colonies when feasible. Fixed-wing aerial surveys may be suitable to determine colony activity and composition of common waterbird species. The most appropriate combination of survey approaches will be based on the need for precise and unbiased estimates, balanced with financial and logistical constraints.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Wildlife Management","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.2193/2006-391","issn":"0022541X","usgsCitation":"Green, M., Luent, M., Michot, T., Jeske, C., and Leberg, P., 2008, Comparison and assessment of aerial and ground estimates of waterbird colonies: Journal of Wildlife Management, v. 72, no. 3, p. 697-706, https://doi.org/10.2193/2006-391.","startPage":"697","endPage":"706","numberOfPages":"10","costCenters":[],"links":[{"id":214714,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.2193/2006-391"},{"id":242463,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"72","issue":"3","noUsgsAuthors":false,"publicationDate":"2010-12-13","publicationStatus":"PW","scienceBaseUri":"5059f83ce4b0c8380cd4cf74","contributors":{"authors":[{"text":"Green, M.C.","contributorId":37974,"corporation":false,"usgs":true,"family":"Green","given":"M.C.","email":"","affiliations":[],"preferred":false,"id":434161,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Luent, M.C.","contributorId":107953,"corporation":false,"usgs":true,"family":"Luent","given":"M.C.","affiliations":[],"preferred":false,"id":434164,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Michot, T.C. 0000-0002-7044-987X","orcid":"https://orcid.org/0000-0002-7044-987X","contributorId":43426,"corporation":false,"usgs":true,"family":"Michot","given":"T.C.","affiliations":[],"preferred":false,"id":434163,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Jeske, C.W.","contributorId":35557,"corporation":false,"usgs":true,"family":"Jeske","given":"C.W.","email":"","affiliations":[],"preferred":false,"id":434160,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Leberg, P.L.","contributorId":42048,"corporation":false,"usgs":true,"family":"Leberg","given":"P.L.","affiliations":[],"preferred":false,"id":434162,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70031791,"text":"70031791 - 2008 - The role of lecithin cholesterol acyltransferase and organic substances from coal in the etiology of Balkan endemic nephropathy: A new hypothesis","interactions":[],"lastModifiedDate":"2012-03-12T17:21:12","indexId":"70031791","displayToPublicDate":"2008-01-01T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1685,"text":"Food and Chemical Toxicology","active":true,"publicationSubtype":{"id":10}},"title":"The role of lecithin cholesterol acyltransferase and organic substances from coal in the etiology of Balkan endemic nephropathy: A new hypothesis","docAbstract":"Balkan endemic nephropathy (BEN) occurs in Serbia, Bulgaria, Romania, Bosnia and Herzegovina, and Croatia. BEN has been characterized as a chronic, slowly progressive renal disease of unknown etiology. In this study, we examined the influence of soluble organic compounds in drinking water leached from Pliocene lignite from BEN-endemic areas on plasma lecithin-cholesterol acyltransferase (LCAT) activity. We found that changes for all samples were the most prominent for the dilution category containing 90% plasma and 10% of diluting media. Water samples from BEN villages from Serbia and Romania showed higher LCAT inhibiting activity (p = 0.02) and (p = 0.003), respectively, compared to deionised water and non-endemic water. A secondary LCAT deficiency could result from this inhibitory effect of the organic compounds found in endemic water supplies and provide an ethiopathogenic basis for the development of BEN in the susceptible population. ?? 2007 Elsevier Ltd. All rights reserved.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Food and Chemical Toxicology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.fct.2007.10.033","issn":"02786915","usgsCitation":"Pavlovic, N., Orem, W., Tatu, C., Lerch, H., Bunnell, J., Feder, G.L., Kostic, E., and Ordodi, V., 2008, The role of lecithin cholesterol acyltransferase and organic substances from coal in the etiology of Balkan endemic nephropathy: A new hypothesis: Food and Chemical Toxicology, v. 46, no. 3, p. 949-954, https://doi.org/10.1016/j.fct.2007.10.033.","startPage":"949","endPage":"954","numberOfPages":"6","costCenters":[],"links":[{"id":239981,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":212490,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.fct.2007.10.033"}],"volume":"46","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505baf7ee4b08c986b324835","contributors":{"authors":[{"text":"Pavlovic, N.M.","contributorId":78550,"corporation":false,"usgs":true,"family":"Pavlovic","given":"N.M.","email":"","affiliations":[],"preferred":false,"id":433150,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Orem, W. H. 0000-0003-4990-0539","orcid":"https://orcid.org/0000-0003-4990-0539","contributorId":93084,"corporation":false,"usgs":true,"family":"Orem","given":"W. H.","affiliations":[],"preferred":false,"id":433154,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Tatu, C. A.","contributorId":89942,"corporation":false,"usgs":false,"family":"Tatu","given":"C. A.","affiliations":[],"preferred":false,"id":433153,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lerch, H.E.","contributorId":100371,"corporation":false,"usgs":true,"family":"Lerch","given":"H.E.","email":"","affiliations":[],"preferred":false,"id":433155,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Bunnell, J.E.","contributorId":63512,"corporation":false,"usgs":true,"family":"Bunnell","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":433149,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Feder, G. L.","contributorId":79508,"corporation":false,"usgs":true,"family":"Feder","given":"G.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":433151,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Kostic, E.N.","contributorId":84981,"corporation":false,"usgs":true,"family":"Kostic","given":"E.N.","email":"","affiliations":[],"preferred":false,"id":433152,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Ordodi, V.L.","contributorId":55210,"corporation":false,"usgs":true,"family":"Ordodi","given":"V.L.","email":"","affiliations":[],"preferred":false,"id":433148,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":70031796,"text":"70031796 - 2008 - Climatic and anthropogenic factors affecting river discharge to the global ocean, 1951-2000","interactions":[],"lastModifiedDate":"2012-03-12T17:21:07","indexId":"70031796","displayToPublicDate":"2008-01-01T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1844,"text":"Global and Planetary Change","active":true,"publicationSubtype":{"id":10}},"title":"Climatic and anthropogenic factors affecting river discharge to the global ocean, 1951-2000","docAbstract":"During the last half of the 20th century, cumulative annual discharge from 137 representative rivers (watershed areas ranging from 0.3 to 6300 ?? 103??km2) to the global ocean remained constant, although annual discharge from about one-third of these rivers changed by more than 30%. Discharge trends for many rivers reflected mostly changes in precipitation, primarily in response to short- and longer-term atmospheric-oceanic signals; with the notable exception of the Parana, Mississippi, Niger and Cunene rivers, few of these \"normal\" rivers experienced significant changes in either discharge or precipitation. Cumulative discharge from many mid-latitude rivers, in contrast, decreased by 60%, reflecting in large part impacts due to damming, irrigation and interbasin water transfers. A number of high-latitude and high-altitude rivers experienced increased discharge despite generally declining precipitation. Poorly constrained meteorological and hydrological data do not seem to explain fully these \"excess\" rivers; changed seasonality in discharge, decreased storage and/or decreased evapotranspiration also may play important roles. ?? 2008 Elsevier B.V. All rights reserved.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Global and Planetary Change","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.gloplacha.2008.03.001","issn":"09218181","usgsCitation":"Milliman, J., Farnsworth, K., Jones, P.D., Xu, K., and Smith, L., 2008, Climatic and anthropogenic factors affecting river discharge to the global ocean, 1951-2000: Global and Planetary Change, v. 62, no. 3-4, p. 187-194, https://doi.org/10.1016/j.gloplacha.2008.03.001.","startPage":"187","endPage":"194","numberOfPages":"8","costCenters":[],"links":[{"id":212553,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.gloplacha.2008.03.001"},{"id":240054,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"62","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f65ae4b0c8380cd4c6f9","contributors":{"authors":[{"text":"Milliman, John D.","contributorId":76735,"corporation":false,"usgs":false,"family":"Milliman","given":"John D.","affiliations":[{"id":6706,"text":"Woods Hole Oceanographic Institution,","active":true,"usgs":false}],"preferred":false,"id":433174,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Farnsworth, K.L.","contributorId":36746,"corporation":false,"usgs":true,"family":"Farnsworth","given":"K.L.","email":"","affiliations":[],"preferred":false,"id":433171,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Jones, P. D.","contributorId":46462,"corporation":false,"usgs":false,"family":"Jones","given":"P.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":433172,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Xu, K.H.","contributorId":63222,"corporation":false,"usgs":true,"family":"Xu","given":"K.H.","email":"","affiliations":[],"preferred":false,"id":433173,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Smith, L.C.","contributorId":88561,"corporation":false,"usgs":true,"family":"Smith","given":"L.C.","email":"","affiliations":[],"preferred":false,"id":433175,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70031955,"text":"70031955 - 2008 - Are we missing a mineralocorticoid in teleost fish? Effects of cortisol, deoxycorticosterone and aldosterone on osmoregulation, gill Na<sup>+</sup>,K<sup>+</sup>-ATPase activity and isoform mRNA levels in Atlantic salmon","interactions":[],"lastModifiedDate":"2013-04-09T11:14:38","indexId":"70031955","displayToPublicDate":"2008-01-01T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1738,"text":"General and Comparative Endocrinology","active":true,"publicationSubtype":{"id":10}},"title":"Are we missing a mineralocorticoid in teleost fish? Effects of cortisol, deoxycorticosterone and aldosterone on osmoregulation, gill Na<sup>+</sup>,K<sup>+</sup>-ATPase activity and isoform mRNA levels in Atlantic salmon","docAbstract":"It has long been held that cortisol, acting through a single receptor, carries out both glucocorticoid and mineralocorticoid actions in teleost fish. The recent finding that fish express a gene with high sequence similarity to the mammalian mineralocorticoid receptor (MR) suggests the possibility that a hormone other than cortisol carries out some mineralocorticoid functions in fish. To test for this possibility, we examined the effect of in vivo cortisol, 11-deoxycorticosterone (DOC) and aldosterone on salinity tolerance, gill Na<sup>+</sup>,K<sup>+</sup>-ATPase (NKA) activity and mRNA levels of NKA α1a and α1b in Atlantic salmon. Cortisol treatment for 6–14 days resulted in increased, physiological levels of cortisol, increased gill NKA activity and improved salinity tolerance (lower plasma chloride after a 24 h seawater challenge), whereas DOC and aldosterone had no effect on either NKA activity or salinity tolerance. NKA α1a and α1b mRNA levels, which increase in response to fresh water and seawater acclimation, respectively, were both upregulated by cortisol, whereas DOC and aldosterone were without effect. Cortisol, DOC and aldosterone had no effect on gill glucocorticoid receptor GR1, GR2 and MR mRNA levels, although there was some indication of possible upregulation of GR1 by cortisol (p = 0.07). The putative GR blocker RU486 inhibited cortisol-induced increases in salinity tolerance, NKA activity and NKA α1a and α1b transcription, whereas the putative MR blocker spironolactone had no effect. The results provide support that cortisol, and not DOC or aldosterone, is involved in regulating the mineralocorticoid functions of ion uptake and salt secretion in teleost fish.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"General and Comparative Endocrinology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","publisherLocation":"Amsterdam, Netherlands","doi":"10.1016/j.ygcen.2008.03.024","issn":"00166480","usgsCitation":"McCormick, S., Regish, A., O’Dea, M.F., and Shrimpton, J., 2008, Are we missing a mineralocorticoid in teleost fish? Effects of cortisol, deoxycorticosterone and aldosterone on osmoregulation, gill Na<sup>+</sup>,K<sup>+</sup>-ATPase activity and isoform mRNA levels in Atlantic salmon: General and Comparative Endocrinology, v. 157, no. 1, p. 35-40, https://doi.org/10.1016/j.ygcen.2008.03.024.","productDescription":"6 p.","startPage":"35","endPage":"40","costCenters":[{"id":197,"text":"Conte Anadromous Fish Research Center","active":false,"usgs":true}],"links":[{"id":214808,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.ygcen.2008.03.024"},{"id":242560,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"157","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059ed63e4b0c8380cd497ae","contributors":{"authors":[{"text":"McCormick, S. D. 0000-0003-0621-6200","orcid":"https://orcid.org/0000-0003-0621-6200","contributorId":20278,"corporation":false,"usgs":true,"family":"McCormick","given":"S. D.","affiliations":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"preferred":false,"id":433873,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Regish, A. 0000-0003-4747-4265","orcid":"https://orcid.org/0000-0003-4747-4265","contributorId":73837,"corporation":false,"usgs":true,"family":"Regish","given":"A.","affiliations":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"preferred":false,"id":433875,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"O’Dea, M. F.","contributorId":30579,"corporation":false,"usgs":true,"family":"O’Dea","given":"M.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":433874,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Shrimpton, J. M.","contributorId":10362,"corporation":false,"usgs":true,"family":"Shrimpton","given":"J. M.","affiliations":[],"preferred":false,"id":433872,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
]}