{"pageNumber":"804","pageRowStart":"20075","pageSize":"25","recordCount":68926,"records":[{"id":70155134,"text":"70155134 - 2010 - Summary of groundwater-recharge estimates for Pennsylvania","interactions":[],"lastModifiedDate":"2017-05-13T16:43:11","indexId":"70155134","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":143,"text":"Water Resource Report","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"70","title":"Summary of groundwater-recharge estimates for Pennsylvania","docAbstract":"<p>Groundwater recharge is water that infiltrates through the subsurface to the zone of saturation beneath the water table. Because recharge is a difficult parameter to quantify, it is typically estimated from measurements of other parameters like streamflow and precipitation. This report provides a general overview of processes affecting recharge in Pennsylvania and presents estimates of recharge rates from studies at various scales.</p><p>The most common method for estimating recharge in Pennsylvania has been to estimate base flow from measurements of streamflow and assume that base flow (expressed in inches over the basin) approximates recharge. Statewide estimates of mean annual groundwater recharge were developed by relating base flow to basin characteristics of HUC10 watersheds (a fifth-level classification that uses 10 digits to define unique hydrologic units) using a regression equation. The regression analysis indicated that mean annual precipitation, average daily maximum temperature, percent of sand in soil, percent of carbonate rock in the watershed, and average stream-channel slope were significant factors in the explaining the variability of groundwater recharge across the Commonwealth.</p><p>Several maps are included in this report to illustrate the principal factors affecting recharge and provide additional information about the spatial distribution of recharge in Pennsylvania. The maps portray the patterns of precipitation, temperature, prevailing winds across Pennsylvania’s varied physiography; illustrate the error associated with recharge estimates; and show the spatial variability of recharge as a percent of precipitation. National, statewide, regional, and local values of recharge, based on numerous studies, are compiled to allow comparison of estimates from various sources. Together these plates provide a synopsis of groundwater-recharge estimations and factors in Pennsylvania.</p><p>Areas that receive the most recharge are typically those that get the most rainfall, have favorable surface conditions for infiltration, and are less susceptible to the influences of high temperatures, and thus, evapotranspiration. Areas that have less recharge in Pennsylvania are typically those with less precipitation, less permeable soils, and higher temperatures that are conducive to greater rates of evapotranspiration.</p>","language":"English","publisher":"Pennsylvania Geological Survey","publisherLocation":"Harrisburg, PA","usgsCitation":"Reese, S.O., and Risser, D.W., 2010, Summary of groundwater-recharge estimates for Pennsylvania: Water Resource Report 70, ii, 18 p.","productDescription":"ii, 18 p.","numberOfPages":"28","ipdsId":"IP-018178","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":341278,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":305760,"type":{"id":15,"text":"Index Page"},"url":"https://www.dcnr.state.pa.us/topogeo/publications/pgspub/water/index.htm"}],"country":"United States","state":"Pennsylvania","publishingServiceCenter":{"id":10,"text":"Baltimore PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"59181b33e4b044b359e48915","contributors":{"authors":[{"text":"Reese, Stuart O.","contributorId":145639,"corporation":false,"usgs":false,"family":"Reese","given":"Stuart","email":"","middleInitial":"O.","affiliations":[{"id":16182,"text":"Pennsylvania Geological Survey","active":true,"usgs":false}],"preferred":false,"id":564864,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Risser, Dennis W. 0000-0001-9597-5406 dwrisser@usgs.gov","orcid":"https://orcid.org/0000-0001-9597-5406","contributorId":898,"corporation":false,"usgs":true,"family":"Risser","given":"Dennis","email":"dwrisser@usgs.gov","middleInitial":"W.","affiliations":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"preferred":true,"id":564863,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70193762,"text":"70193762 - 2010 - Improved hydrogeophysical characterization and monitoring through parallel modeling and inversion of time-domain resistivity andinduced-polarization data","interactions":[],"lastModifiedDate":"2019-10-23T17:00:27","indexId":"70193762","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1808,"text":"Geophysics","active":true,"publicationSubtype":{"id":10}},"title":"Improved hydrogeophysical characterization and monitoring through parallel modeling and inversion of time-domain resistivity andinduced-polarization data","docAbstract":"<p><span>Electrical geophysical methods have found wide use in the growing discipline of hydrogeophysics for characterizing the electrical properties of the subsurface and for monitoring subsurface processes in terms of the spatiotemporal changes in subsurface conductivity, chargeability, and source currents they govern. Presently, multichannel and multielectrode data collections systems can collect large data sets in relatively short periods of time. Practitioners, however, often are unable to fully utilize these large data sets and the information they contain because of standard desktop-computer processing limitations. These limitations can be addressed by utilizing the storage and processing capabilities of parallel computing environments. We have developed a parallel distributed-memory forward and inverse modeling algorithm for analyzing resistivity and time-domain induced polar-ization (IP) data. The primary components of the parallel computations include distributed computation of the pole solutions in forward mode, distributed storage and computation of the Jacobian matrix in inverse mode, and parallel execution of the inverse equation solver. We have tested the corresponding parallel code in three efforts: (1) resistivity characterization of the Hanford 300 Area Integrated Field Research Challenge site in Hanford, Washington, U.S.A., (2) resistivity characterization of a volcanic island in the southern Tyrrhenian Sea in Italy, and (3) resistivity and IP monitoring of biostimulation at a Superfund site in Brandywine, Maryland, U.S.A. Inverse analysis of each of these data sets would be limited or impossible in a standard serial computing environment, which underscores the need for parallel high-performance computing to fully utilize the potential of electrical geophysical methods in hydrogeophysical applications.</span></p>","language":"English","publisher":"Society of Exploration Geophysicists","doi":"10.1190/1.3475513","usgsCitation":"Johnson, T., Versteeg, R.J., Ward, A., Day-Lewis, F.D., and Revil, A., 2010, Improved hydrogeophysical characterization and monitoring through parallel modeling and inversion of time-domain resistivity andinduced-polarization data: Geophysics, v. 75, no. 4, p. WA27-WA41, https://doi.org/10.1190/1.3475513.","productDescription":"15 p.","startPage":"WA27","endPage":"WA41","ipdsId":"IP-017886","costCenters":[{"id":486,"text":"OGW Branch of Geophysics","active":true,"usgs":true},{"id":493,"text":"Office of Ground Water","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":349080,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"75","issue":"4","publishingServiceCenter":{"id":11,"text":"Pembroke PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5a610acee4b06e28e9c256e7","contributors":{"authors":[{"text":"Johnson, Timothy C.","contributorId":99884,"corporation":false,"usgs":true,"family":"Johnson","given":"Timothy C.","affiliations":[],"preferred":false,"id":722689,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Versteeg, Roelof J.","contributorId":199843,"corporation":false,"usgs":false,"family":"Versteeg","given":"Roelof","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":722690,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ward, Andy","contributorId":7184,"corporation":false,"usgs":true,"family":"Ward","given":"Andy","email":"","affiliations":[],"preferred":false,"id":722691,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Day-Lewis, Frederick D. 0000-0003-3526-886X daylewis@usgs.gov","orcid":"https://orcid.org/0000-0003-3526-886X","contributorId":1672,"corporation":false,"usgs":true,"family":"Day-Lewis","given":"Frederick","email":"daylewis@usgs.gov","middleInitial":"D.","affiliations":[{"id":486,"text":"OGW Branch of Geophysics","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true},{"id":493,"text":"Office of Ground Water","active":true,"usgs":true}],"preferred":true,"id":722692,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Revil, André","contributorId":38879,"corporation":false,"usgs":true,"family":"Revil","given":"André","affiliations":[],"preferred":false,"id":722693,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70193766,"text":"70193766 - 2010 - Marine electrical resistivity imaging of submarine groundwater discharge: Sensitivity analysis and application in Waquoit Bay, Massachusetts, USA","interactions":[],"lastModifiedDate":"2019-10-21T12:49:34","indexId":"70193766","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1923,"text":"Hydrogeology Journal","active":true,"publicationSubtype":{"id":10}},"title":"Marine electrical resistivity imaging of submarine groundwater discharge: Sensitivity analysis and application in Waquoit Bay, Massachusetts, USA","docAbstract":"<p>Electrical resistivity imaging has been used in coastal settings to characterize fresh submarine groundwater discharge and the position of the freshwater/salt-water interface because of the relation of bulk electrical conductivity to pore-fluid conductivity, which in turn is a function of salinity. Interpretation of tomograms for hydrologic processes is complicated by inversion artifacts, uncertainty associated with survey geometry limitations, measurement errors, and choice of regularization method. Variation of seawater over tidal cycles poses unique challenges for inversion. The capabilities and limitations of resistivity imaging are presented for characterizing the distribution of freshwater and saltwater beneath a beach. The experimental results provide new insight into fresh submarine groundwater discharge at Waquoit Bay National Estuarine Research Reserve, East Falmouth, Massachusetts (USA). Tomograms from the experimental data indicate that fresh submarine groundwater discharge may shut down at high tide, whereas temperature data indicate that the discharge continues throughout the tidal cycle. Sensitivity analysis and synthetic modeling provide insight into resolving power in the presence of a time-varying saline water layer. In general, vertical electrodes and cross-hole measurements improve the inversion results regardless of the tidal level, whereas the resolution of surface arrays is more sensitive to time-varying saline water layer.</p>","language":"English","publisher":"Springer","doi":"10.1007/s10040-009-0498-z","usgsCitation":"Henderson, R., Day-Lewis, F.D., Abarca, E., Harvey, C.F., Karam, H.N., Liu, L., and Lane, J.W., 2010, Marine electrical resistivity imaging of submarine groundwater discharge: Sensitivity analysis and application in Waquoit Bay, Massachusetts, USA: Hydrogeology Journal, v. 18, no. 1, p. 173-185, https://doi.org/10.1007/s10040-009-0498-z.","productDescription":"13 p.","startPage":"173","endPage":"185","ipdsId":"IP-011944","costCenters":[{"id":486,"text":"OGW Branch of Geophysics","active":true,"usgs":true},{"id":493,"text":"Office of Ground Water","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":348723,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Massachusetts","otherGeospatial":"Waquoit Bay","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -70.54252624511719,\n              41.54815851009314\n            ],\n            [\n              -70.46974182128906,\n              41.54815851009314\n            ],\n            [\n              -70.46974182128906,\n              41.672398925907906\n            ],\n            [\n              -70.54252624511719,\n              41.672398925907906\n            ],\n            [\n              -70.54252624511719,\n              41.54815851009314\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"18","issue":"1","publishingServiceCenter":{"id":11,"text":"Pembroke PSC"},"noUsgsAuthors":false,"publicationDate":"2009-09-10","publicationStatus":"PW","scienceBaseUri":"5a610acde4b06e28e9c256e5","contributors":{"authors":[{"text":"Henderson, Rory rhenders@usgs.gov","contributorId":2083,"corporation":false,"usgs":true,"family":"Henderson","given":"Rory","email":"rhenders@usgs.gov","affiliations":[{"id":486,"text":"OGW Branch of Geophysics","active":true,"usgs":true}],"preferred":false,"id":720313,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Day-Lewis, Frederick D. 0000-0003-3526-886X daylewis@usgs.gov","orcid":"https://orcid.org/0000-0003-3526-886X","contributorId":1672,"corporation":false,"usgs":true,"family":"Day-Lewis","given":"Frederick","email":"daylewis@usgs.gov","middleInitial":"D.","affiliations":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true},{"id":486,"text":"OGW Branch of Geophysics","active":true,"usgs":true},{"id":493,"text":"Office of Ground Water","active":true,"usgs":true}],"preferred":true,"id":720311,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Abarca, Elena","contributorId":199905,"corporation":false,"usgs":false,"family":"Abarca","given":"Elena","email":"","affiliations":[{"id":13299,"text":"Department of Civil and Environmental Engineering, Massachusetts Institute of Technology, Cambridge, MA","active":true,"usgs":false}],"preferred":false,"id":720312,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Harvey, Charles F.","contributorId":199836,"corporation":false,"usgs":false,"family":"Harvey","given":"Charles","email":"","middleInitial":"F.","affiliations":[{"id":12444,"text":"Massachusetts Institute of Technology","active":true,"usgs":false}],"preferred":false,"id":721861,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Karam, Hanan N.","contributorId":199837,"corporation":false,"usgs":false,"family":"Karam","given":"Hanan","email":"","middleInitial":"N.","affiliations":[{"id":13299,"text":"Department of Civil and Environmental Engineering, Massachusetts Institute of Technology, Cambridge, MA","active":true,"usgs":false}],"preferred":false,"id":721862,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Liu, Lanbo","contributorId":199850,"corporation":false,"usgs":false,"family":"Liu","given":"Lanbo","email":"","affiliations":[{"id":6619,"text":"University of Connecticutt","active":true,"usgs":false}],"preferred":false,"id":720315,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Lane, John W. Jr. jwlane@usgs.gov","contributorId":1738,"corporation":false,"usgs":true,"family":"Lane","given":"John","suffix":"Jr.","email":"jwlane@usgs.gov","middleInitial":"W.","affiliations":[{"id":486,"text":"OGW Branch of Geophysics","active":true,"usgs":true}],"preferred":false,"id":720314,"contributorType":{"id":1,"text":"Authors"},"rank":12}]}}
,{"id":70193742,"text":"70193742 - 2010 - Brine delineation and monitoring with electrical resistivity tomography and electromagnetic borehole logging at the Fort Knox well field near West Point, Kentucky","interactions":[],"lastModifiedDate":"2020-03-10T14:37:58","indexId":"70193742","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Brine delineation and monitoring with electrical resistivity tomography and electromagnetic borehole logging at the Fort Knox well field near West Point, Kentucky","docAbstract":"<p><span>The potable water system at Fort Knox is threatened by brine contamination from improperly abandoned natural gas exploration wells. The Fort Knox well field is located near the town of West Point, Kentucky, in the flood plain of the Ohio River. At the site, unconsolidated sediments approximately 30 – 40 m thick, overlie shale and porous limestone. Brine is believed to flow vertically from the underlying formations to the unconsolidated aquifer through damaged or leaky well casings under a high hydraulic gradient from the artificially pressurized porous limestone, which is utilized for natural gas storage by a regional energy company. Upon reaching the unconsolidated aquifer, brinecontaminated groundwater enters water supply production wells under the pumping‐induced gradient. As part of the Fort Knox remediation strategy to reduce the impact of brine contamination, electrical resistivity tomography (ERT) and borehole electromagnetic (EM) logs are being collected annually to detect gross changes in subsurface conductivity. The 2009 ERT data show areas of high conductivity on the western (contaminated) side of the site with conductivities more than an order of magnitude higher than on the eastern (uncontaminated) side of the site. The areas of high conductivity are interpreted as brine contamination, consistent with known regions of brine contamination. Conductivities from the EM logs are consistent with the results from the ERT inversions. The EM logs show little change between 2008 and 2009, except for some small changes in the brine distribution in well PZ1. Yearly ERT surveys will be continued to detect new areas of brine contamination and monitor the remediation effort.</span><span></span></p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Symposium on the Application of Geophysics to Engineering and Environmental Problems 2010","largerWorkSubtype":{"id":12,"text":"Conference publication"},"language":"English","publisher":"Society of Exploration Geophysicists","doi":"10.4133/1.3445533","usgsCitation":"Henderson, R., Unthank, M.D., Zettwoch, D.D., and Lane, J.W., 2010, Brine delineation and monitoring with electrical resistivity tomography and electromagnetic borehole logging at the Fort Knox well field near West Point, Kentucky, <i>in</i> Symposium on the Application of Geophysics to Engineering and Environmental Problems 2010, p. 913-922, https://doi.org/10.4133/1.3445533.","productDescription":"10 p.","startPage":"913","endPage":"922","ipdsId":"IP-019006","costCenters":[{"id":486,"text":"OGW Branch of Geophysics","active":true,"usgs":true},{"id":493,"text":"Office of Ground Water","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":350809,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Kentucky","city":"West Point","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -86.02844238281249,\n              37.92984646868451\n            ],\n            [\n              -85.91892242431639,\n              37.92984646868451\n            ],\n            [\n              -85.91892242431639,\n              38.0096892410326\n            ],\n            [\n              -86.02844238281249,\n              38.0096892410326\n            ],\n            [\n              -86.02844238281249,\n              37.92984646868451\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","publishingServiceCenter":{"id":11,"text":"Pembroke PSC"},"noUsgsAuthors":false,"publicationDate":"2010-05-17","publicationStatus":"PW","scienceBaseUri":"5a719271e4b0a9a2e9dbde28","contributors":{"authors":[{"text":"Henderson, Rory rhenders@usgs.gov","contributorId":2083,"corporation":false,"usgs":true,"family":"Henderson","given":"Rory","email":"rhenders@usgs.gov","affiliations":[{"id":486,"text":"OGW Branch of Geophysics","active":true,"usgs":true}],"preferred":false,"id":720151,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Unthank, Michael D. 0000-0003-2483-0431 munthank@usgs.gov","orcid":"https://orcid.org/0000-0003-2483-0431","contributorId":3902,"corporation":false,"usgs":true,"family":"Unthank","given":"Michael","email":"munthank@usgs.gov","middleInitial":"D.","affiliations":[{"id":27231,"text":"Indiana-Kentucky Water Science Center","active":true,"usgs":true}],"preferred":true,"id":720150,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Zettwoch, Douglas D.","contributorId":56709,"corporation":false,"usgs":true,"family":"Zettwoch","given":"Douglas","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":720152,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lane, John W. Jr. 0000-0002-3558-243X jwlane@usgs.gov","orcid":"https://orcid.org/0000-0002-3558-243X","contributorId":189168,"corporation":false,"usgs":true,"family":"Lane","given":"John","suffix":"Jr.","email":"jwlane@usgs.gov","middleInitial":"W.","affiliations":[{"id":486,"text":"OGW Branch of Geophysics","active":true,"usgs":true},{"id":493,"text":"Office of Ground Water","active":true,"usgs":true}],"preferred":false,"id":720149,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70187016,"text":"70187016 - 2010 - Interpreting canopy water balance and fog screen observations: separating cloud water from wind-blown rainfall at two contrasting forest sites in Hawai'i","interactions":[],"lastModifiedDate":"2017-04-19T10:02:29","indexId":"70187016","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Interpreting canopy water balance and fog screen observations: separating cloud water from wind-blown rainfall at two contrasting forest sites in Hawai'i","docAbstract":"<p>No abstract available.<br></p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Tropical montane cloud forests: science for conservation and management","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Cambridge University Press","usgsCitation":"Giambelluca, T.W., DeLay, J.K., Nullet, M., Scholl, M.A., and Gingerich, S.B., 2010, Interpreting canopy water balance and fog screen observations: separating cloud water from wind-blown rainfall at two contrasting forest sites in Hawai'i, chap. <i>of</i> Tropical montane cloud forests: science for conservation and management, p. 342-352.","productDescription":"11 p.","startPage":"342","endPage":"352","ipdsId":"IP-017121","costCenters":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"links":[{"id":339912,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":339911,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.cambridge.org/catalogue/catalogue.asp?isbn=9780521760355"}],"country":"United 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W.","contributorId":70069,"corporation":false,"usgs":true,"family":"Giambelluca","given":"Thomas","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":691907,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"DeLay, J. K.","contributorId":191118,"corporation":false,"usgs":false,"family":"DeLay","given":"J.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":691904,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Nullet, M.A.","contributorId":191119,"corporation":false,"usgs":false,"family":"Nullet","given":"M.A.","affiliations":[],"preferred":false,"id":691905,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Scholl, Martha A. 0000-0001-6994-4614 mascholl@usgs.gov","orcid":"https://orcid.org/0000-0001-6994-4614","contributorId":1920,"corporation":false,"usgs":true,"family":"Scholl","given":"Martha","email":"mascholl@usgs.gov","middleInitial":"A.","affiliations":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":true,"id":691903,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Gingerich, Stephen B. 0000-0002-4381-0746 sbginger@usgs.gov","orcid":"https://orcid.org/0000-0002-4381-0746","contributorId":1426,"corporation":false,"usgs":true,"family":"Gingerich","given":"Stephen","email":"sbginger@usgs.gov","middleInitial":"B.","affiliations":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true},{"id":525,"text":"Pacific Islands Water Science Center","active":true,"usgs":true}],"preferred":true,"id":691906,"contributorType":{"id":1,"text":"Authors"},"rank":14}]}}
,{"id":70037091,"text":"70037091 - 2010 - Life history and demographics of the endangered birdwing pearlymussel (<i>Lemiox rimosus</i>) (Bivalvia: Unionidae)","interactions":[],"lastModifiedDate":"2016-07-08T12:36:28","indexId":"70037091","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":737,"text":"American Midland Naturalist","active":true,"publicationSubtype":{"id":10}},"title":"Life history and demographics of the endangered birdwing pearlymussel (<i>Lemiox rimosus</i>) (Bivalvia: Unionidae)","docAbstract":"<div class=\"articleAbstractBox\">\n<div class=\"abstractSection\">\n<p class=\"last\">The life history and population demography of the endangered birdwing pearlymussel (<i>Lemiox rimosus</i>) were studied in the Clinch and Duck rivers, Tennessee. Reproducing populations of&nbsp;<i>L. rimosus</i>&nbsp;now occur only in the Clinch, Duck and Powell rivers, as the species is considered extirpated from the remaining portions of its range in the Tennessee River drainage. Females are long-term winter brooders, typically gravid from Oct. to May. Glochidia are contained in the outer gills and are released in association with a mantle-lure that resembles a small freshwater snail. Estimated fecundity, based on 8 gravid females collected from the Clinch and Duck rivers, ranged from 4132 to 58,700 glochidia/mussel. Seven fish species were tested for suitability as hosts for glochidia, and five darter species were confirmed through induced infestations:&nbsp;<i>Etheostoma blennioides</i>,&nbsp;<i>E. camurum</i>,&nbsp;<i>E. rufilineatum</i>,&nbsp;<i>E. simoterum</i>&nbsp;and&nbsp;<i>E. zonale</i>. Ages of&nbsp;<i>L. rimosus</i>&nbsp;shells were determined by thin-sectioning and ranged from 3 to 15&nbsp;y in both rivers. Shell growth was higher and maximum size greater in males than females in both rivers. Shell growth was greatest in the Duck River. Densities of&nbsp;<i>L. rimosus</i>&nbsp;in the Clinch River were maintained at seemingly stable but low levels ranging from 0.07 to 0.27&nbsp;m<sup>&minus;2</sup>&nbsp;from 2004&ndash;2007, and in the Duck River at similar but higher levels ranging from 0.6 to 1.0&nbsp;m<sup>&minus;2</sup>&nbsp;from 2004&ndash;2006. In the latter river, abundance has increased since 1988, likely due to improved minimum flows and dissolved oxygen levels in water releases from a reservoir upstream.</p>\n<p>&nbsp;</p>\n</div>\n</div>\n<p class=\"articleCitation epubDate\">&nbsp;</p>","language":"English","publisher":"University of Notre Dame","doi":"10.1674/0003-0031-163.2.335","issn":"00030031","usgsCitation":"Jones, J.W., Neves, R.J., Ahlstedt, S.A., Hubbs, D., Johnson, M., Dan, H., and Ostby, B.J., 2010, Life history and demographics of the endangered birdwing pearlymussel (<i>Lemiox rimosus</i>) (Bivalvia: Unionidae): American Midland Naturalist, v. 163, no. 2, p. 335-350, https://doi.org/10.1674/0003-0031-163.2.335.","productDescription":"16 p.","startPage":"335","endPage":"350","numberOfPages":"16","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":245112,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Tennessee","otherGeospatial":"Clinch River, Duck River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -80.980224609375,\n              37.405073750176946\n            ],\n            [\n              -81.23291015625,\n              37.405073750176946\n            ],\n            [\n              -81.683349609375,\n              37.26530995561875\n            ],\n            [\n              -82.628173828125,\n              37.01132594307015\n            ],\n            [\n              -82.96875,\n              36.84446074079564\n            ],\n            [\n              -83.199462890625,\n              36.721273880045004\n            ],\n            [\n              -83.726806640625,\n              36.633162095586556\n            ],\n            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-82.254638671875,\n              36.27085020723905\n            ],\n            [\n              -81.88110351562499,\n              36.46547188679816\n            ],\n            [\n              -81.683349609375,\n              36.50963615733049\n            ],\n            [\n              -81.474609375,\n              36.58906837139909\n            ],\n            [\n              -80.947265625,\n              36.70365959719453\n            ],\n            [\n              -80.870361328125,\n              36.84446074079564\n            ],\n            [\n              -80.870361328125,\n              37.046408899699564\n            ],\n            [\n              -80.980224609375,\n              37.405073750176946\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"163","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a4756e4b0c8380cd67826","contributors":{"authors":[{"text":"Jones, Jess W.","contributorId":84279,"corporation":false,"usgs":true,"family":"Jones","given":"Jess","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":459334,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Neves, Richard J.","contributorId":8909,"corporation":false,"usgs":true,"family":"Neves","given":"Richard","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":459329,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ahlstedt, Steven A. ahlstedt@usgs.gov","contributorId":3957,"corporation":false,"usgs":true,"family":"Ahlstedt","given":"Steven","email":"ahlstedt@usgs.gov","middleInitial":"A.","affiliations":[{"id":581,"text":"Tennessee Water Science Center","active":true,"usgs":true}],"preferred":false,"id":459335,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hubbs, Don","contributorId":172760,"corporation":false,"usgs":false,"family":"Hubbs","given":"Don","affiliations":[{"id":13408,"text":"Tennessee Wildlife Resources Agency","active":true,"usgs":false}],"preferred":false,"id":459330,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Johnson, Matthew mjjohnson@usgs.gov","contributorId":29536,"corporation":false,"usgs":true,"family":"Johnson","given":"Matthew","email":"mjjohnson@usgs.gov","affiliations":[],"preferred":false,"id":459333,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Dan, Hua","contributorId":172761,"corporation":false,"usgs":false,"family":"Dan","given":"Hua","email":"","affiliations":[{"id":25550,"text":"Virginia Polytechnic Institute and State University","active":true,"usgs":false}],"preferred":false,"id":459331,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Ostby, Brett J.K.","contributorId":146480,"corporation":false,"usgs":false,"family":"Ostby","given":"Brett","email":"","middleInitial":"J.K.","affiliations":[{"id":16709,"text":"VaTech","active":true,"usgs":false}],"preferred":false,"id":459332,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70043327,"text":"70043327 - 2010 - Quantifying terrestrial ecosystem carbon dynamics in the Jinsha watershed, Upper Yangtze, China from 1975 to 2000","interactions":[],"lastModifiedDate":"2017-04-25T13:10:33","indexId":"70043327","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1547,"text":"Environmental Management","active":true,"publicationSubtype":{"id":10}},"title":"Quantifying terrestrial ecosystem carbon dynamics in the Jinsha watershed, Upper Yangtze, China from 1975 to 2000","docAbstract":"Quantifying the spatial and temporal dynamics of carbon stocks in terrestrial ecosystems and carbon fluxes between the terrestrial biosphere and the atmosphere is critical to our understanding of regional patterns of carbon budgets. Here we use the General Ensemble biogeochemical Modeling System to simulate the terrestrial ecosystem carbon dynamics in the Jinsha watershed of China’s upper Yangtze basin from 1975 to 2000, based on unique combinations of spatial and temporal dynamics of major driving forces, such as climate, soil properties, nitrogen deposition, and land use and land cover changes. Our analysis demonstrates that the Jinsha watershed ecosystems acted as a carbon sink during the period of 1975–2000, with an average rate of 0.36 Mg/ha/yr, primarily resulting from regional climate variation and local land use and land cover change. Vegetation biomass accumulation accounted for 90.6% of the sink, while soil organic carbon loss before 1992 led to a lower net gain of carbon in the watershed, and after that soils became a small sink. Ecosystem carbon sink/source patterns showed a high degree of spatial heterogeneity. Carbon sinks were associated with forest areas without disturbances, whereas carbon sources were primarily caused by stand-replacing disturbances. It is critical to adequately represent the detailed fast-changing dynamics of land use activities in regional biogeochemical models to determine the spatial and temporal evolution of regional carbon sink/source patterns.","language":"English","publisher":"Springer","doi":"10.1007/s00267-009-9285-9","usgsCitation":"Zhao, S., Liu, S., Yin, R., Li, Z., Deng, Y., Tan, K., Deng, X., Rothstein, D., and Qi, J., 2010, Quantifying terrestrial ecosystem carbon dynamics in the Jinsha watershed, Upper Yangtze, China from 1975 to 2000: Environmental Management, v. 45, no. 3, p. 466-475, https://doi.org/10.1007/s00267-009-9285-9.","productDescription":"10 p.","startPage":"466","endPage":"475","ipdsId":"IP-011153","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":271686,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"China","otherGeospatial":"Jinsha watershed, Yangtze River","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 97.36,21.62 ], [ 97.36,32.38 ], [ 104.08,32.38 ], [ 104.08,21.62 ], [ 97.36,21.62 ] ] ] } } ] }","volume":"45","issue":"3","noUsgsAuthors":false,"publicationDate":"2009-03-19","publicationStatus":"PW","scienceBaseUri":"5180e7ebe4b0df838b924d90","contributors":{"authors":[{"text":"Zhao, Shuqing","contributorId":9152,"corporation":false,"usgs":true,"family":"Zhao","given":"Shuqing","email":"","affiliations":[],"preferred":false,"id":473394,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Liu, Shuguang 0000-0002-6027-3479 sliu@usgs.gov","orcid":"https://orcid.org/0000-0002-6027-3479","contributorId":147403,"corporation":false,"usgs":true,"family":"Liu","given":"Shuguang","email":"sliu@usgs.gov","affiliations":[{"id":223,"text":"Earth Resources Observation and Science (EROS) Center (Geography)","active":false,"usgs":true}],"preferred":true,"id":692785,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Yin, Runsheng","contributorId":150057,"corporation":false,"usgs":false,"family":"Yin","given":"Runsheng","email":"","affiliations":[{"id":17896,"text":"State Key Laboratory of Ore Deposit Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang, China","active":true,"usgs":false}],"preferred":false,"id":692786,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Li, Zhengpeng","contributorId":80812,"corporation":false,"usgs":true,"family":"Li","given":"Zhengpeng","affiliations":[],"preferred":false,"id":692787,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Deng, Yulin","contributorId":191348,"corporation":false,"usgs":false,"family":"Deng","given":"Yulin","email":"","affiliations":[],"preferred":false,"id":692788,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Tan, Kun","contributorId":191349,"corporation":false,"usgs":false,"family":"Tan","given":"Kun","email":"","affiliations":[],"preferred":false,"id":692789,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Deng, Xiangzheng","contributorId":191350,"corporation":false,"usgs":false,"family":"Deng","given":"Xiangzheng","email":"","affiliations":[],"preferred":false,"id":692790,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Rothstein, David","contributorId":191351,"corporation":false,"usgs":false,"family":"Rothstein","given":"David","email":"","affiliations":[],"preferred":false,"id":692791,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Qi, Jiaguo","contributorId":191352,"corporation":false,"usgs":false,"family":"Qi","given":"Jiaguo","email":"","affiliations":[],"preferred":false,"id":692792,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}}
,{"id":70046763,"text":"dds49126 - 2010 - Attributes for MRB_E2RF1 Catchments by Major River Basins in the Conterminous United States: STATSGO Soil Characteristics","interactions":[],"lastModifiedDate":"2013-11-25T16:06:02","indexId":"dds49126","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":310,"text":"Data Series","code":"DS","onlineIssn":"2327-638X","printIssn":"2327-0271","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"491-26","title":"Attributes for MRB_E2RF1 Catchments by Major River Basins in the Conterminous United States: STATSGO Soil Characteristics","docAbstract":"This tabular data set represents estimated soil variables compiled for every MRB_E2RF1 catchment of selected Major River Basins (MRBs, Crawford and others, 2006). The variables included are cation exchange capacity, percent calcium carbonate, slope, water-table depth, soil thickness, hydrologic soil group, soil erodibility (k-factor), permeability, average water capacity, bulk density, percent organic material, percent clay, percent sand, and percent silt. The source data set is the State Soil ( STATSGO ) Geographic Database (Wolock, 1997). The MRB_E2RF1 catchments are based on a modified version of the U.S. Environmental Protection Agency's (USEPA) ERF1_2 and include enhancements to support national and regional-scale surface-water quality modeling (Nolan and others, 2002; Brakebill and others, 2011). Data were compiled for every MRB_E2RF1 catchment for the conterminous United States covering New England and Mid-Atlantic (MRB1), South Atlantic-Gulf and Tennessee (MRB2), the Great Lakes, Ohio, Upper Mississippi, and Souris-Red-Rainy (MRB3), the Missouri (MRB4), the Lower Mississippi, Arkansas-White-Red, and Texas-Gulf (MRB5), the Rio Grande, Colorado, and the Great basin (MRB6), the Pacific Northwest (MRB7) river basins, and California (MRB8).","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/dds49126","usgsCitation":"Wieczorek, M., and LaMotte, A.E., 2010, Attributes for MRB_E2RF1 Catchments by Major River Basins in the Conterminous United States: STATSGO Soil Characteristics: U.S. Geological Survey Data Series 491-26, Dataset, https://doi.org/10.3133/dds49126.","productDescription":"Dataset","onlineOnly":"Y","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":274429,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":274427,"type":{"id":16,"text":"Metadata"},"url":"https://water.usgs.gov/GIS/metadata/usgswrd/XML/mrb_e2rf1_statsgo.xml"}],"country":"United States","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -127.910792,23.243486 ], [ -127.910792,51.657387 ], [ -65.327751,51.657387 ], [ -65.327751,23.243486 ], [ -127.910792,23.243486 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51d3f663e4b09630fbdc527d","contributors":{"authors":[{"text":"Wieczorek, Michael mewieczo@usgs.gov","contributorId":2309,"corporation":false,"usgs":true,"family":"Wieczorek","given":"Michael","email":"mewieczo@usgs.gov","affiliations":[{"id":374,"text":"Maryland Water Science Center","active":true,"usgs":true}],"preferred":false,"id":480183,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"LaMotte, Andrew E. 0000-0002-1434-6518 alamotte@usgs.gov","orcid":"https://orcid.org/0000-0002-1434-6518","contributorId":2842,"corporation":false,"usgs":true,"family":"LaMotte","given":"Andrew","email":"alamotte@usgs.gov","middleInitial":"E.","affiliations":[{"id":374,"text":"Maryland Water Science Center","active":true,"usgs":true}],"preferred":true,"id":480184,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70037725,"text":"70037725 - 2010 - Controls on rind thickness on basaltic andesite clasts weathering in Guadeloupe","interactions":[],"lastModifiedDate":"2012-04-30T16:43:33","indexId":"70037725","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1213,"text":"Chemical Geology","active":true,"publicationSubtype":{"id":10}},"title":"Controls on rind thickness on basaltic andesite clasts weathering in Guadeloupe","docAbstract":"A clast of low porosity basaltic andesite collected from the B horizon of a soil developed on a late Quaternary volcaniclastic debris flow in the Bras David watershed on Basse-Terre Island, Guadeloupe, exhibits weathering like that observed in many weathered clasts of similar composition in other tropical locations. Specifically, elemental profiles measured across the core-rind interface document that primary minerals and glass weather to Fe oxyhydroxides, gibbsite and minor kaolinite in the rind. The earliest reaction identified in the core is oxidation of Fe in pyroxene but the earliest reaction that creates significant porosity is plagioclase dissolution. Elemental loss varies in the order Ca???Na&gt;K???Mg&gt;Si&gt;Al&gt;Fe???P??Ti, consistent with the relative reactivity of phases in the clast from plagioclase???pyroxene???glass&gt;apatite&gt;ilmenite. The rind surrounds a core of unaltered material that is more spherical than the original clast. The distance from the core-rind boundary to a visually prominent rind layer, L, was measured as a proxy for the rind thickness at 36 locations on a slab cut vertically through the nominal center of the clast. This distance averaged 24.4??3.1mm. Maximum and minimum values for L, 35.8 and 20.6mm, were observed where curvature of the core-rind boundary is greatest (0.12mm-1) and smallest (0.018mm-1) respectively. Extrapolating from other rinds in other locations, the rate of rind formation is estimated to vary by a factor of about 2 (from ~4 to 7??10-14ms-1) from low to high curvature. The observation of a higher rate of rind formation for a higher curvature interface is consistent with a diffusion-limited model for weathering rind formation. The diffusion-limited model predicts that, like rind thickness, values of the thickness of the reaction front (h) for a given reaction, defined as the zone over which a parent mineral such as plagioclase completely weathers to rind material, should also increase with curvature. Values of h were quantified as a function of interface curvature using bulk chemical analysis (500&lt;h&lt;2000??m). Values of h were also quantified by measuring loss of matrix glass and increase in porosity as a function of curvature. In contrast to rind thickness, h shows no consistent increase with curvature. This contradiction is attributed to the mm-scale roughness of the interface which is related to phenocryst grain size. Therefore, the overall rind formation rate is strongly affected by curvature measured at the scale of the clast, while mineral reaction rates documented by reaction front thickness are strongly affected by curvature at the scale of phenocrysts. Similarly, the weathering advance rate (ms-1) for the entire Bras David watershed can be extrapolated from the clast weathering rate if roughness at the watershed scale equals values of approximately 400-800. ?? 2010 Elsevier B.V.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Chemical Geology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.chemgeo.2010.05.002","issn":"00092541","usgsCitation":"Sak, P., Navarre-Sitchler, A., Miller, C., Daniel, C., Gaillardet, J., Buss, H., Lebedeva, M., and Brantley, S., 2010, Controls on rind thickness on basaltic andesite clasts weathering in Guadeloupe: Chemical Geology, v. 276, no. 3-4, p. 129-143, https://doi.org/10.1016/j.chemgeo.2010.05.002.","startPage":"129","endPage":"143","numberOfPages":"15","costCenters":[],"links":[{"id":217999,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.chemgeo.2010.05.002"},{"id":245974,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"276","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059fbd3e4b0c8380cd4dfaf","contributors":{"authors":[{"text":"Sak, P.B.","contributorId":81519,"corporation":false,"usgs":true,"family":"Sak","given":"P.B.","affiliations":[],"preferred":false,"id":462507,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Navarre-Sitchler, A. K.","contributorId":41711,"corporation":false,"usgs":true,"family":"Navarre-Sitchler","given":"A. K.","affiliations":[],"preferred":false,"id":462503,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Miller, C.E.","contributorId":52050,"corporation":false,"usgs":true,"family":"Miller","given":"C.E.","email":"","affiliations":[],"preferred":false,"id":462504,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Daniel, C.C.","contributorId":53427,"corporation":false,"usgs":true,"family":"Daniel","given":"C.C.","email":"","affiliations":[],"preferred":false,"id":462505,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Gaillardet, J.","contributorId":34789,"corporation":false,"usgs":true,"family":"Gaillardet","given":"J.","affiliations":[],"preferred":false,"id":462502,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Buss, H.L.","contributorId":13726,"corporation":false,"usgs":true,"family":"Buss","given":"H.L.","email":"","affiliations":[],"preferred":false,"id":462501,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Lebedeva, M.I.","contributorId":90990,"corporation":false,"usgs":true,"family":"Lebedeva","given":"M.I.","email":"","affiliations":[],"preferred":false,"id":462508,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Brantley, S.L.","contributorId":71676,"corporation":false,"usgs":true,"family":"Brantley","given":"S.L.","email":"","affiliations":[],"preferred":false,"id":462506,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":70037168,"text":"70037168 - 2010 - Detecting the spatial and temporal variability of chlorophyll-a concentration and total suspended solids in Apalachicola Bay, Florida using MODIS imagery","interactions":[],"lastModifiedDate":"2019-06-17T15:27:47","indexId":"70037168","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2068,"text":"International Journal of Remote Sensing","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Detecting the spatial and temporal variability of chlorophyll-<i>a</i> concentration and total suspended solids in Apalachicola Bay, Florida using MODIS imagery","title":"Detecting the spatial and temporal variability of chlorophyll-a concentration and total suspended solids in Apalachicola Bay, Florida using MODIS imagery","docAbstract":"<div class=\"hlFld-Abstract\"><div class=\"abstractSection abstractInFull\"><p>Apalachicola Bay, Florida, accounts for 90% of Florida's and 10% of the nation's eastern oyster (<i>Crassostrea virginica</i>) harvesting. Chlorophyll-<i>a</i><span>&nbsp;</span>concentration and total suspended solids (TSS) are two important water quality variables, among other environmental factors such as salinity, for eastern oyster production in Apalachicola Bay. In this research, we developed regression models of the relationships between the reflectance of the Moderate-Resolution Imaging Spectroradiometer (MODIS) Terra 250&nbsp;m data and the two water quality variables based on the Bay-wide field data collected during 14–17 October 2002, a relatively dry period, and 3–5 April 2006, a relatively wet period, respectively. Then we selected the best regression models (highest coefficient of determination,<span>&nbsp;</span><i>R</i><span>&nbsp;</span><sup>2</sup>) to derive Bay-wide maps of chlorophyll-<i>a</i><span>&nbsp;</span>concentration and TSS for the two periods. The MODIS-derived maps revealed large spatial and temporal variations in chlorophyll-<i>a</i><span>&nbsp;</span>concentration and TSS across the entire Apalachicola Bay.</p></div></div>","language":"English","publisher":"Taylor & Francis","doi":"10.1080/01431160902893485","issn":"01431161","usgsCitation":"Wang, H., Hladik, C., Huang, W., Milla, K., Edmiston, L., Harwell, M., and Schalles, J., 2010, Detecting the spatial and temporal variability of chlorophyll-a concentration and total suspended solids in Apalachicola Bay, Florida using MODIS imagery: International Journal of Remote Sensing, v. 31, no. 2, p. 439-453, https://doi.org/10.1080/01431160902893485.","productDescription":"15 p.","startPage":"439","endPage":"453","costCenters":[{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true},{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"links":[{"id":245372,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Florida","otherGeospatial":"Apalachicola Bay","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -85.089111328125,\n              29.596147812456916\n            ],\n            [\n              -84.86801147460938,\n              29.596147812456916\n            ],\n            [\n              -84.86801147460938,\n              29.72264453862633\n            ],\n            [\n              -85.089111328125,\n              29.72264453862633\n            ],\n            [\n              -85.089111328125,\n              29.596147812456916\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"31","issue":"2","noUsgsAuthors":false,"publicationDate":"2010-01-08","publicationStatus":"PW","scienceBaseUri":"5059ff63e4b0c8380cd4f16b","contributors":{"authors":[{"text":"Wang, Hongqing 0000-0002-2977-7732 wangh@usgs.gov","orcid":"https://orcid.org/0000-0002-2977-7732","contributorId":140432,"corporation":false,"usgs":true,"family":"Wang","given":"Hongqing","email":"wangh@usgs.gov","affiliations":[{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true},{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"preferred":true,"id":459708,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hladik, C.M.","contributorId":76974,"corporation":false,"usgs":true,"family":"Hladik","given":"C.M.","email":"","affiliations":[],"preferred":false,"id":459706,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Huang, W.","contributorId":42748,"corporation":false,"usgs":true,"family":"Huang","given":"W.","email":"","affiliations":[],"preferred":false,"id":459705,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Milla, K.","contributorId":104313,"corporation":false,"usgs":true,"family":"Milla","given":"K.","email":"","affiliations":[],"preferred":false,"id":459710,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Edmiston, L.","contributorId":88982,"corporation":false,"usgs":true,"family":"Edmiston","given":"L.","affiliations":[],"preferred":false,"id":459707,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Harwell, M.A.","contributorId":34362,"corporation":false,"usgs":true,"family":"Harwell","given":"M.A.","email":"","affiliations":[],"preferred":false,"id":459704,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Schalles, J.F.","contributorId":99404,"corporation":false,"usgs":true,"family":"Schalles","given":"J.F.","email":"","affiliations":[],"preferred":false,"id":459709,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70037320,"text":"70037320 - 2010 - Genesis of a regionally widespread celadonitic chert ironstone bed overlying upper Lias manganese deposits, Hungary","interactions":[],"lastModifiedDate":"2012-03-12T17:22:07","indexId":"70037320","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2545,"text":"Journal of the Geological Society","active":true,"publicationSubtype":{"id":10}},"title":"Genesis of a regionally widespread celadonitic chert ironstone bed overlying upper Lias manganese deposits, Hungary","docAbstract":"Mineralogy and chemical composition are presented for a chert-ironstone bed that overlies the ??rk??t Mn deposit. This bed is mottled green-brown in its lower and upper parts, which are composed of quartz, goethite and celadonite. These parts of the bed are interpreted to be strongly altered tuffs, reflecting oxidic, low-temperature alteration of a hydrated, Fe-rich, Al-poor tuff, and K and Mg uptake from seawater. The middle part of the bed is a mineralized bacterial mat (quartz, goethite). Textures resembling bacterial cells and colonies are common, with wavy, bulbous laminations composed of mounds overlying a mesh-work stromatolite-like texture constructed of micrometre-size Fe oxides. This bed is concordant with the underlying Mn deposit and marks the termination of Mn accumulation. Although no genetic connection exists between the two, the rocks adjacent to the contact record the oceanographic and bottom-water conditions extant when accumulation of one of the major Mn deposits of Europe ended, when the Transdanubian Range was located in the middle of the Adria-Apulian microcontinent between the Neotethys and Atlantic-Ligurian seaways. A pyroclastic origin for part of the bed has significance for the Toarcian of Central Europe because evidence of volcanism occurring at that time is otherwise sparse. ?? 2010 Geological Society of London.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of the Geological Society","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1144/0016-76492008-132","issn":"00167649","usgsCitation":"Polgari, M., Hein, J., Toth, M., Brukner-Wein, A., Vigh, T., Biro, L., and Cserhati, C., 2010, Genesis of a regionally widespread celadonitic chert ironstone bed overlying upper Lias manganese deposits, Hungary: Journal of the Geological Society, v. 167, no. 2, p. 313-328, https://doi.org/10.1144/0016-76492008-132.","startPage":"313","endPage":"328","numberOfPages":"16","costCenters":[],"links":[{"id":217376,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1144/0016-76492008-132"},{"id":245321,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"167","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a1558e4b0c8380cd54d84","contributors":{"authors":[{"text":"Polgari, Marta","contributorId":75750,"corporation":false,"usgs":true,"family":"Polgari","given":"Marta","email":"","affiliations":[],"preferred":false,"id":460459,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hein, J.R. 0000-0002-5321-899X","orcid":"https://orcid.org/0000-0002-5321-899X","contributorId":61429,"corporation":false,"usgs":true,"family":"Hein","given":"J.R.","affiliations":[],"preferred":false,"id":460458,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Toth, M.","contributorId":85442,"corporation":false,"usgs":true,"family":"Toth","given":"M.","affiliations":[],"preferred":false,"id":460460,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Brukner-Wein, A.","contributorId":98568,"corporation":false,"usgs":true,"family":"Brukner-Wein","given":"A.","email":"","affiliations":[],"preferred":false,"id":460461,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Vigh, T.","contributorId":47613,"corporation":false,"usgs":true,"family":"Vigh","given":"T.","email":"","affiliations":[],"preferred":false,"id":460456,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Biro, L.","contributorId":47207,"corporation":false,"usgs":true,"family":"Biro","given":"L.","email":"","affiliations":[],"preferred":false,"id":460455,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Cserhati, C.","contributorId":53633,"corporation":false,"usgs":true,"family":"Cserhati","given":"C.","email":"","affiliations":[],"preferred":false,"id":460457,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70037258,"text":"70037258 - 2010 - Identifying sources of stream water sulfate after a summer drought in the Sleepers River watershed (Vermont, USA) using hydrological, chemical, and isotopic techniques","interactions":[],"lastModifiedDate":"2012-03-12T17:22:11","indexId":"70037258","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":835,"text":"Applied Geochemistry","active":true,"publicationSubtype":{"id":10}},"title":"Identifying sources of stream water sulfate after a summer drought in the Sleepers River watershed (Vermont, USA) using hydrological, chemical, and isotopic techniques","docAbstract":"In many forested headwater catchments, peak SO<sub>4</sub><sup>2 -</sup> concentrations in stream water occur in the late summer or fall following drought potentially resulting in episodic stream acidification. The sources of highly elevated stream water SO<sub>4</sub><sup>2 -</sup> concentrations were investigated in a first order stream at the Sleepers River watershed (Vermont, USA) after the particularly dry summer of 2001 using a combination of hydrological, chemical and isotopic approaches. Throughout the summer of 2001 SO<sub>4</sub><sup>2 -</sup> concentrations in stream water doubled from ???130 to 270 ??eq/L while flows decreased. Simultaneously increasing Na<sup>+</sup> and Ca<sup>2+</sup> concentrations and ??<sup>34</sup>S values increasing from +7??? towards those of bedrock S (???+10.5???) indicated that chemical weathering involving hydrolysis of silicates and oxidation of sulfide minerals in schists and phyllites was the cause for the initial increase in SO<sub>4</sub><sup>2 -</sup> concentrations. During re-wetting of the watershed in late September and early October of 2001, increasing stream flows were accompanied by decreasing Na<sup>+</sup> and Ca<sup>2+</sup> concentrations, but SO<sub>4</sub><sup>2 -</sup> concentrations continued to increase up to 568 ??eq/L, indicating that a major source of SO<sub>4</sub><sup>2 -</sup> in addition to bedrock weathering contributed to peak SO<sub>4</sub><sup>2 -</sup> concentrations. The further increase in SO<sub>4</sub><sup>2 -</sup> concentrations coincided with an abrupt decrease of ??<sup>34</sup>S values in stream water SO<sub>4</sub><sup>2 -</sup> from maximum values near +10??? to minimum values near -3???. Soil investigations revealed that some C-horizons in the Spodsols of the watershed contained secondary sulfide minerals with ??<sup>34</sup>S values near -22???. The shift to negative ??<sup>34</sup>S values of stream water SO<sub>4</sub><sup>2 -</sup> indicates that secondary sulfides in C-horizons were oxidized to SO<sub>4</sub><sup>2 -</sup> during the particularly dry summer of 2001. The newly formed SO<sub>4</sub><sup>2 -</sup> was transported to the streams during re-wetting of the watershed contributing ???60% of the SO<sub>4</sub><sup>2 -</sup> during peak concentrations in the stream water. Thereafter, the contribution of SO<sub>4</sub><sup>2 -</sup> from oxidation of secondary sulfides in C-horizons decreased rapidly and pedogenic SO<sub>4</sub><sup>2 -</sup> reemerged as a dominant SO<sub>4</sub><sup>2 -</sup> source in concert with decreasing SO<sub>4</sub><sup>2 -</sup> concentrations in spring of 2002. The study provides evidence that a quantitative assessment of the sources of stream water SO<sub>4</sub><sup>2 -</sup> in forested watersheds is possible by combining hydrological, chemical and isotopic techniques, provided that the isotopic compositions of all potential SO<sub>4</sub><sup>2 -</sup> sources are distinctly different. ?? 2010 Elsevier Ltd.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Applied Geochemistry","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.apgeochem.2010.02.007","issn":"08832927","usgsCitation":"Mayer, B., Shanley, J.B., Bailey, S., and Mitchell, M., 2010, Identifying sources of stream water sulfate after a summer drought in the Sleepers River watershed (Vermont, USA) using hydrological, chemical, and isotopic techniques: Applied Geochemistry, v. 25, no. 5, p. 747-754, https://doi.org/10.1016/j.apgeochem.2010.02.007.","startPage":"747","endPage":"754","numberOfPages":"8","costCenters":[],"links":[{"id":217371,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.apgeochem.2010.02.007"},{"id":245316,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"25","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3857e4b0c8380cd6152e","contributors":{"authors":[{"text":"Mayer, B.","contributorId":84538,"corporation":false,"usgs":true,"family":"Mayer","given":"B.","email":"","affiliations":[],"preferred":false,"id":460123,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Shanley, J. B.","contributorId":52226,"corporation":false,"usgs":true,"family":"Shanley","given":"J.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":460121,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bailey, S.W.","contributorId":29113,"corporation":false,"usgs":true,"family":"Bailey","given":"S.W.","email":"","affiliations":[],"preferred":false,"id":460120,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Mitchell, M.J.","contributorId":72940,"corporation":false,"usgs":true,"family":"Mitchell","given":"M.J.","email":"","affiliations":[],"preferred":false,"id":460122,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70043674,"text":"70043674 - 2010 - Juvenile Salmonid survival, passage, and egress at McNary Dam during tests of temporary spillway weirs, 2009","interactions":[],"lastModifiedDate":"2016-12-27T11:10:19","indexId":"70043674","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"title":"Juvenile Salmonid survival, passage, and egress at McNary Dam during tests of temporary spillway weirs, 2009","docAbstract":"We evaluated behavior, passage, and survival of juvenile salmonids at McNary Dam in relation to the temporary spillway weirs (TSWs) using acoustic telemetry during 2009. The TSWs were located in spill bays 4 and 20 during spring and in spill bays 19 and 20 during summer. Our objectives were to assess the performance of the TSWs as a fish passage alternative. We also examined how tailrace conditions might have influenced fish survival by releasing drift buoys (drogues).\nThe TSWs proved to be a relatively effective way to pass juvenile salmonids at McNary Dam (Summary Tables 1.1, 1.2, and 1.3), as was the case in 2007 and 2008. The TSWs passed about 14% of yearling Chinook salmon and 34% of juvenile steelhead with only 5-10% of total project discharge flowing through the TSWs. The TSWs and adjacent spill bays 16-18 passed 27% of subyearling Chinook salmon in the summer with 6-16% of total project discharge flowing through the TSWs. Based on the number of fish passing per the proportion of water flowing through the spillway (i.e., passage effectiveness), the TSWs were the most effective passage route. Passage effectiveness for fish passing through both TSW structures was 2.0 for yearling Chinook salmon, 5.2 for juvenile steelhead, and 2.7 subyearling Chinook salmon for TSW 20 alone. Higher passage of juvenile steelhead through the TSWs could have resulted from juvenile steelhead being more surface-oriented during migration (Plumb et al. 2004; Beeman et al. 2007; Beeman and Maule 2006). Based on passage performance and effectiveness metrics, TSW 4, located on the north end of the spillway, did not perform as well as TSW 20, located on the south end of the spillway. Passage proportions for TSW 4 were at least half that of the levels observed for TSW 20 for both yearling Chinook salmon and juvenile steelhead. This difference may be attributed to TSW location or other variables such as dam operations. Regardless of which TSW was used by fish passing the dam, survival through both TSWs was high (> 0.98 for paired-release dam survival) for yearling Chinook salmon and juvenile steelhead.","language":"English","publisher":"U.S. Army Corps of Engineers","publisherLocation":"Walla Walla, WA","usgsCitation":"Adams, N., and Liedtke, T., 2010, Juvenile Salmonid survival, passage, and egress at McNary Dam during tests of temporary spillway weirs, 2009, 191 p. .","productDescription":"191 p. ","ipdsId":"IP-022316","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":332541,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Oregon, Washington","otherGeospatial":"McNary Dam ","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -119.37366485595702,\n              45.93252776429104\n            ],\n            [\n              -119.29538726806639,\n              45.94709159562572\n            ],\n            [\n              -119.24148559570311,\n              45.95162708963677\n            ],\n            [\n              -119.16183471679688,\n              45.940645781504905\n            ],\n            [\n              -119.10003662109374,\n              45.952104488469985\n            ],\n            [\n              -119.09591674804688,\n              45.91867663909007\n            ],\n            [\n              -119.21539306640626,\n              45.915810457254395\n            ],\n            [\n              -119.34585571289062,\n              45.909122123907295\n            ],\n            [\n              -119.38293457031249,\n              45.90243298453263\n            ],\n            [\n              -119.39117431640625,\n              45.93300532761351\n            ],\n            [\n              -119.37366485595702,\n              45.93252776429104\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58638bd6e4b0cd2dabe7bec4","contributors":{"authors":[{"text":"Adams, N.S.","contributorId":93175,"corporation":false,"usgs":true,"family":"Adams","given":"N.S.","affiliations":[],"preferred":false,"id":656638,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Liedtke, T.L.","contributorId":32800,"corporation":false,"usgs":true,"family":"Liedtke","given":"T.L.","email":"","affiliations":[],"preferred":false,"id":656639,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70176672,"text":"70176672 - 2010 - Microbial ecology of corals, sponges, and algae in mesophotic coral environments","interactions":[],"lastModifiedDate":"2017-04-27T10:50:18","indexId":"70176672","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1619,"text":"FEMS Microbiology Ecology","onlineIssn":"1574-6941","printIssn":"0168-6496","active":true,"publicationSubtype":{"id":10}},"title":"Microbial ecology of corals, sponges, and algae in mesophotic coral environments","docAbstract":"<p><span>Mesophotic coral ecosystems that occur at depths from 30 to 200 m have historically been understudied and yet appear to support a diverse biological community. The microbiology of these systems is particularly poorly understood, especially with regard to the communities associated with corals, sponges, and algae. This lack of information is partly due to the problems associated with gaining access to these environments and poor reproducibility across sampling methods. To summarize what is known about the microbiology of these ecosystems and to highlight areas where research is urgently needed, an overview of the current state of knowledge is presented. Emphasis is placed on the characterization of microbial populations, both prokaryotic and eukaryotic, associated with corals, sponges, and algae and the factors that influence microbial community structure. In topic areas where virtually nothing is known from mesophotic environments, the knowledge pertaining to shallow-water ecosystems is summarized to provide a starting point for a discussion on what might be expected in the mesophotic zone.</span></p>","language":"English","publisher":"Oxford University Press","doi":"10.1111/j.1574-6941.2010.00862.x","usgsCitation":"Olson, J.B., and Kellogg, C.A., 2010, Microbial ecology of corals, sponges, and algae in mesophotic coral environments: FEMS Microbiology Ecology, v. 73, no. 1, p. 17-30, https://doi.org/10.1111/j.1574-6941.2010.00862.x.","productDescription":"14 p.","startPage":"17","endPage":"30","ipdsId":"IP-010146","costCenters":[{"id":574,"text":"St. Petersburg Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":475943,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1111/j.1574-6941.2010.00862.x","text":"Publisher Index Page"},{"id":328949,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"73","issue":"1","noUsgsAuthors":false,"publicationDate":"2010-03-08","publicationStatus":"PW","scienceBaseUri":"57fe8151e4b0824b2d1480c4","contributors":{"authors":[{"text":"Olson, Julie B.","contributorId":174901,"corporation":false,"usgs":false,"family":"Olson","given":"Julie","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":649595,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kellogg, Christina A. 0000-0002-6492-9455 ckellogg@usgs.gov","orcid":"https://orcid.org/0000-0002-6492-9455","contributorId":391,"corporation":false,"usgs":true,"family":"Kellogg","given":"Christina","email":"ckellogg@usgs.gov","middleInitial":"A.","affiliations":[{"id":574,"text":"St. Petersburg Coastal and Marine Science Center","active":true,"usgs":true},{"id":506,"text":"Office of the AD Ecosystems","active":true,"usgs":true}],"preferred":true,"id":649596,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70179280,"text":"70179280 - 2010 - Minimizing effects of over-water docks on federally listed fish stocks in McNary Reservoir: A literature review for criteria","interactions":[],"lastModifiedDate":"2016-12-27T11:47:05","indexId":"70179280","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":9,"text":"Other Report"},"title":"Minimizing effects of over-water docks on federally listed fish stocks in McNary Reservoir: A literature review for criteria","docAbstract":"<p>McNary Lock and Dam were completed in 1953, creating McNary Reservoir, or Lake Wallula. The shoreline of the reservoir is federally owned and as a result the U.S. Army Corps of Engineers (USACE) has certain land and fish habitat management responsibilities to balance with other multipurpose benefits. The Endangered Species Act (ESA) listing of Columbia and Snake River salmon stocks has changed the management of salmon harvest, hydropower operations, hatchery practices, and habitat management in recent years. There are 12 salmon Oncorhynchus spp., steelhead Oncorhynchus mykiss, and bull trout Salvelinus confluentus evolutionarily significant units (ESU‘s) that use this reach of the Columbia River at one or more stages in their life history. Of those 12, 8 are listed as threatened or endangered under the federal Endangered Species Act. The entire portion of the Columbia River in the Hanford Reach and McNary Reservoir is designated critical habitat for seven ESA-listed salmon species. The USACE is in the process of updating the 1983 McNary Lakeshore Management Plan. The updated Shoreline Plan provides criteria for private use of the federal shoreline of McNary Reservoir, specifically the permitting of private docks, over-water structures, and modifications to shoreline vegetation by adjacent land owners. The previous Shoreline Plan was written prior to the federal listing of salmon species. At the request of the USACE, the purpose of this report is to review information from the literature and determine the extent to which the criteria proposed by USACE for the docks and over-water structures are supported by the current body of scientific knowledge. </p>","language":"English","publisher":"U. S. Army Corps of Engineers","usgsCitation":"Rondorf, D.W., Rutz, G.L., and Charrier, J.C., 2010, Minimizing effects of over-water docks on federally listed fish stocks in McNary Reservoir: A literature review for criteria, vii., 41 p. .","productDescription":"vii., 41 p. ","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":332546,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Oregon, Washington ","otherGeospatial":"McNary Dam ","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -119.32250976562499,\n              45.952104488469985\n            ],\n            [\n              -119.08218383789062,\n              45.97406038956237\n            ],\n            [\n              -119.06845092773438,\n              46.051314066826905\n            ],\n            [\n              -119.05609130859374,\n              46.13702492883557\n            ],\n            [\n              -119.25933837890624,\n              46.223552702209886\n            ],\n            [\n              -119.29916381835938,\n              46.27863122156088\n            ],\n            [\n              -119.29779052734375,\n              46.32986150334176\n            ],\n            [\n              -119.23599243164062,\n              46.356406479672486\n            ],\n            [\n              -119.16595458984374,\n              46.27388525189855\n            ],\n            [\n              -119.06845092773438,\n              46.22640294763494\n            ],\n            [\n              -118.9434814453125,\n              46.28622391806706\n            ],\n            [\n              -118.77593994140624,\n              46.3810438458062\n            ],\n            [\n              -118.68804931640625,\n              46.42460580983505\n            ],\n            [\n              -118.6138916015625,\n              46.382938567526786\n            ],\n            [\n              -118.67706298828125,\n              46.33175800051563\n            ],\n            [\n              -118.98193359375,\n              46.20644812194458\n            ],\n            [\n              -118.8775634765625,\n              46.09037664604301\n            ],\n            [\n              -118.8885498046875,\n              45.947330315089275\n            ],\n            [\n              -119.24835205078125,\n              45.89574303912447\n            ],\n            [\n              -119.51751708984375,\n              45.8842726860033\n            ],\n            [\n              -119.5806884765625,\n              45.88618457602257\n            ],\n            [\n              -119.55871582031251,\n              45.93778073466329\n            ],\n            [\n              -119.35546875000001,\n              45.947330315089275\n            ],\n            [\n              -119.32250976562499,\n              45.952104488469985\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58638bd6e4b0cd2dabe7bec0","contributors":{"authors":[{"text":"Rondorf, Dennis W. drondorf@usgs.gov","contributorId":2970,"corporation":false,"usgs":true,"family":"Rondorf","given":"Dennis","email":"drondorf@usgs.gov","middleInitial":"W.","affiliations":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"preferred":true,"id":656642,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rutz, Gary L. grutz@usgs.gov","contributorId":3886,"corporation":false,"usgs":true,"family":"Rutz","given":"Gary","email":"grutz@usgs.gov","middleInitial":"L.","affiliations":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"preferred":false,"id":656643,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Charrier, Jodi C.","contributorId":177675,"corporation":false,"usgs":true,"family":"Charrier","given":"Jodi","email":"","middleInitial":"C.","affiliations":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"preferred":false,"id":656644,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70176789,"text":"70176789 - 2010 - Accuracy of egg flotation throughout incubation to determine embryo age and incubation day in waterbird nests","interactions":[],"lastModifiedDate":"2017-07-01T17:26:20","indexId":"70176789","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3551,"text":"The Condor","active":true,"publicationSubtype":{"id":10}},"title":"Accuracy of egg flotation throughout incubation to determine embryo age and incubation day in waterbird nests","docAbstract":"<p><span>Floating bird eggs to estimate their age is a widely used technique, but few studies have examined its accuracy throughout incubation. We assessed egg flotation for estimating hatch date, day of incubation, and the embryo's developmental age in eggs of the American Avocet (</span><i>Recurvirostra americana</i><span>), Black-necked Stilt (</span><i>Himantopus mexicanus</i><span>), and Forster's Tern (</span><i>Sterna forsteri</i><span>). Predicted hatch dates based on egg flotation during our first visit to a nest were highly correlated with actual hatch dates (</span><i>r</i><span> = 0.99) and accurate within 2.3 ± 1.7 (SD) days. Age estimates based on flotation were correlated with both day of incubation (</span><i>r</i><span> = 0.96) and the embryo's developmental age (</span><i>r</i><span> = 0.86) and accurate within 1.3 ± 1.6 days and 1.9 ± 1.6 days, respectively. However, the technique's accuracy varied substantially throughout incubation. Flotation overestimated the embryo's developmental age between 3 and 9 days, underestimated age between 12 and 21 days, and was most accurate between 0 and 3 days and 9 and 12 days. Age estimates based on egg flotation were generally accurate within 3 days until day 15 but later in incubation were biased progressively lower. Egg flotation was inaccurate and overestimated embryo age in abandoned nests (mean error: 7.5 ± 6.0 days). The embryo's developmental age and day of incubation were highly correlated (</span><i>r</i><span> = 0.94), differed by 2.1 ± 1.6 days, and resulted in similar assessments of the egg-flotation technique. Floating every egg in the clutch and refloating eggs at subsequent visits to a nest can refine age estimates.</span></p>","language":"English","publisher":"Cooper Ornithological Society","doi":"10.1525/cond.2010.090070","usgsCitation":"Ackerman, J., and Eagles-Smith, C.A., 2010, Accuracy of egg flotation throughout incubation to determine embryo age and incubation day in waterbird nests: The Condor, v. 112, no. 3, p. 438-446, https://doi.org/10.1525/cond.2010.090070.","productDescription":"9 p.","startPage":"438","endPage":"446","ipdsId":"IP-013296","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":475906,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1525/cond.2010.090070","text":"Publisher Index Page"},{"id":329351,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"112","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57fe8151e4b0824b2d1480b8","contributors":{"authors":[{"text":"Ackerman, Joshua T. 0000-0002-3074-8322 jackerman@usgs.gov","orcid":"https://orcid.org/0000-0002-3074-8322","contributorId":147078,"corporation":false,"usgs":true,"family":"Ackerman","given":"Joshua T.","email":"jackerman@usgs.gov","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":false,"id":650320,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Eagles-Smith, Collin A. 0000-0003-1329-5285 ceagles-smith@usgs.gov","orcid":"https://orcid.org/0000-0003-1329-5285","contributorId":505,"corporation":false,"usgs":true,"family":"Eagles-Smith","given":"Collin","email":"ceagles-smith@usgs.gov","middleInitial":"A.","affiliations":[{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true},{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true},{"id":289,"text":"Forest and Rangeland Ecosys Science Center","active":true,"usgs":true}],"preferred":true,"id":650321,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70179467,"text":"70179467 - 2010 - Multiple well-shutdown tests and site-scale flow simulation in fractured rocks","interactions":[],"lastModifiedDate":"2018-10-09T10:49:15","indexId":"70179467","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"Multiple well-shutdown tests and site-scale flow simulation in fractured rocks","docAbstract":"<p><span>A new method was developed for conducting aquifer tests in fractured-rock flow systems that have a pump-and-treat (P&amp;T) operation for containing and removing groundwater contaminants. The method involves temporary shutdown of individual pumps in wells of the P&amp;T system. Conducting aquifer tests in this manner has several advantages, including (1) no additional contaminated water is withdrawn, and (2) hydraulic containment of contaminants remains largely intact because pumping continues at most wells. The well-shutdown test method was applied at the former Naval Air Warfare Center (NAWC), West Trenton, New Jersey, where a P&amp;T operation is designed to contain and remove trichloroethene and its daughter products in the dipping fractured sedimentary rocks underlying the site. The detailed site-scale subsurface geologic stratigraphy, a three-dimensional MODFLOW model, and inverse methods in UCODE_2005 were used to analyze the shutdown tests. In the model, a deterministic method was used for representing the highly heterogeneous hydraulic conductivity distribution and simulations were conducted using an equivalent porous media method. This approach was very successful for simulating the shutdown tests, contrary to a common perception that flow in fractured rocks must be simulated using a stochastic or discrete fracture representation of heterogeneity. Use of inverse methods to simultaneously calibrate the model to the multiple shutdown tests was integral to the effectiveness of the approach.</span></p>","language":"English","publisher":"Wiley","doi":"10.1111/j.1745-6584.2009.00651.x","usgsCitation":"Tiedeman, C.R., Lacombe, P., and Goode, D., 2010, Multiple well-shutdown tests and site-scale flow simulation in fractured rocks: Groundwater, v. 48, no. 3, p. 401-415, https://doi.org/10.1111/j.1745-6584.2009.00651.x.","productDescription":"15 p.","startPage":"401","endPage":"415","ipdsId":"IP-014165","costCenters":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":332770,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"48","issue":"3","noUsgsAuthors":false,"publicationDate":"2010-04-28","publicationStatus":"PW","scienceBaseUri":"586cc698e4b0f5ce109fa95b","contributors":{"authors":[{"text":"Tiedeman, Claire R. 0000-0002-0128-3685 tiedeman@usgs.gov","orcid":"https://orcid.org/0000-0002-0128-3685","contributorId":196777,"corporation":false,"usgs":true,"family":"Tiedeman","given":"Claire","email":"tiedeman@usgs.gov","middleInitial":"R.","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":true,"id":657371,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lacombe, Pierre J. placombe@usgs.gov","contributorId":2486,"corporation":false,"usgs":true,"family":"Lacombe","given":"Pierre J.","email":"placombe@usgs.gov","affiliations":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"preferred":false,"id":657372,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Goode, Daniel J. 0000-0002-8527-2456 djgoode@usgs.gov","orcid":"https://orcid.org/0000-0002-8527-2456","contributorId":2433,"corporation":false,"usgs":true,"family":"Goode","given":"Daniel J.","email":"djgoode@usgs.gov","affiliations":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"preferred":false,"id":657373,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70176800,"text":"70176800 - 2010 - Saving our shared birds: Partners in Flight tri-national vision for landbird conservation","interactions":[],"lastModifiedDate":"2016-10-06T11:17:54","indexId":"70176800","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":9,"text":"Other Report"},"title":"Saving our shared birds: Partners in Flight tri-national vision for landbird conservation","docAbstract":"<p>Landbirds are the most abundant and diverse group of birds in North America, with nearly 900 species distributed across every major terrestrial habitat. Birds are indicators of environmental health; their populations track changes in habitat, water, disease, and climate. They are providers of invaluable ecosystem services, such as pest control, seed dispersal, and pollination. As the focus of bird watching, they help generate billions of dollars for national economies. Yet, we are in danger of losing this spectacular and irreplaceable bird diversity: landbirds are experiencing significant declines, ominous threats, and shrinking habitats across a continent with growing human populations, increasing resource consumption, and changing climate. </p><p>Saving Our Shared Birds presents for the first time a comprehensive conservation assessment of landbirds in Canada, Mexico, and the continental United States. This new tri-national vision encompasses the complete range of many migratory species and highlights the vital links among migrants and highly threatened resident species in Mexico. It points to a set of continent-scale actions necessary to maintain the landbird diversity and abundance that are our shared responsibility. </p><p>This collaborative effort of Partners in Flight (PIF) is the next step in linking the countries of the Western Hemisphere to help species at risk and keep common birds common through voluntary partnerships—our mission since 1990. Saving Our Shared Birds builds upon PIF’s 2004 North American Landbird Conservation Plan, which presented science-based priorities for the conservation of 448 landbird species in Canada and the United States. </p><p>Our three nations have expressed their commitment to cooperative conservation through numerous international treaties, agreements, and programs, including formation of the North American Bird Conservation Initiative (NABCI) a decade ago. The NABCI partnership recognizes that effective conservation requires a concerted effort within each country, as well as a tri-national strategy to address issues throughout the full life cycles of our birds. </p><p>Today more than ever, it is urgent for the people of Canada, Mexico, and the United States to work together to keep common birds common, prevent extinction of our bird species at greatest risk, and ensure the diversity and abundance of birdlife across North America and throughout the hemisphere, far into the future. Saving Our Shared Birds shows the way forward.</p>","language":"English","publisher":"Partners in Flight","usgsCitation":"Berlanga, H., Kennedy, J.A., Rich, T.D., Arizmendi, M.D., Beardmore, C.J., Blancher, P.J., Butcher, G.S., Couturier, A.R., Dayer, A.A., Demarest, D.W., Easton, W.E., Gustafson, M., Inigo-Elias, E.E., Krebs, E.A., Panjabi, A.O., Rodriguez Contreras, V., Rosenberg, K.V., Ruth, J.M., Santana Castellon, E., Vidal, R., and Will, T., 2010, Saving our shared birds: Partners in Flight tri-national vision for landbird conservation, 49 p.","productDescription":"49 p.","costCenters":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"links":[{"id":329367,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":329366,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.savingoursharedbirds.org/"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57f7c08ae4b0bc0bec09c7d1","contributors":{"authors":[{"text":"Berlanga, Humberto","contributorId":175178,"corporation":false,"usgs":false,"family":"Berlanga","given":"Humberto","affiliations":[],"preferred":false,"id":650350,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kennedy, Judith A.","contributorId":175179,"corporation":false,"usgs":false,"family":"Kennedy","given":"Judith","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":650351,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rich, Terrell D.","contributorId":112381,"corporation":false,"usgs":true,"family":"Rich","given":"Terrell","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":650352,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Arizmendi, Maria del Coro","contributorId":175180,"corporation":false,"usgs":false,"family":"Arizmendi","given":"Maria","email":"","middleInitial":"del Coro","affiliations":[],"preferred":false,"id":650353,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Beardmore, Carol J.","contributorId":175181,"corporation":false,"usgs":false,"family":"Beardmore","given":"Carol","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":650354,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Blancher, Peter J.","contributorId":175182,"corporation":false,"usgs":false,"family":"Blancher","given":"Peter","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":650355,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Butcher, Gregory S.","contributorId":140856,"corporation":false,"usgs":false,"family":"Butcher","given":"Gregory","email":"","middleInitial":"S.","affiliations":[{"id":6762,"text":"U.S. Forest Service, La Grande, Oregon","active":true,"usgs":false}],"preferred":false,"id":650356,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Couturier, Andrew R.","contributorId":175183,"corporation":false,"usgs":false,"family":"Couturier","given":"Andrew","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":650357,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Dayer, Ashley A.","contributorId":171460,"corporation":false,"usgs":false,"family":"Dayer","given":"Ashley","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":650358,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Demarest, Dean W.","contributorId":175184,"corporation":false,"usgs":false,"family":"Demarest","given":"Dean","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":650359,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Easton, Wendy E.","contributorId":175185,"corporation":false,"usgs":false,"family":"Easton","given":"Wendy","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":650360,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Gustafson, Mary","contributorId":175186,"corporation":false,"usgs":false,"family":"Gustafson","given":"Mary","email":"","affiliations":[],"preferred":false,"id":650361,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Inigo-Elias, Eduardo E.","contributorId":78438,"corporation":false,"usgs":true,"family":"Inigo-Elias","given":"Eduardo","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":650362,"contributorType":{"id":1,"text":"Authors"},"rank":13},{"text":"Krebs, Elizabeth A.","contributorId":175187,"corporation":false,"usgs":false,"family":"Krebs","given":"Elizabeth","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":650363,"contributorType":{"id":1,"text":"Authors"},"rank":14},{"text":"Panjabi, Arvind O.","contributorId":169967,"corporation":false,"usgs":false,"family":"Panjabi","given":"Arvind","email":"","middleInitial":"O.","affiliations":[{"id":25644,"text":"Bird Conservancy of the Rockies","active":true,"usgs":false}],"preferred":false,"id":650364,"contributorType":{"id":1,"text":"Authors"},"rank":15},{"text":"Rodriguez Contreras, Vicente","contributorId":175188,"corporation":false,"usgs":false,"family":"Rodriguez Contreras","given":"Vicente","email":"","affiliations":[],"preferred":false,"id":650365,"contributorType":{"id":1,"text":"Authors"},"rank":16},{"text":"Rosenberg, Kenneth V.","contributorId":171463,"corporation":false,"usgs":false,"family":"Rosenberg","given":"Kenneth","email":"","middleInitial":"V.","affiliations":[{"id":27615,"text":"Cornell Lab of Ornithology, Conservation Science Program","active":true,"usgs":false}],"preferred":false,"id":650366,"contributorType":{"id":1,"text":"Authors"},"rank":17},{"text":"Ruth, Janet M. 0000-0003-1576-5957 janet_ruth@usgs.gov","orcid":"https://orcid.org/0000-0003-1576-5957","contributorId":1408,"corporation":false,"usgs":true,"family":"Ruth","given":"Janet","email":"janet_ruth@usgs.gov","middleInitial":"M.","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":true,"id":650367,"contributorType":{"id":1,"text":"Authors"},"rank":18},{"text":"Santana Castellon, Eduardo","contributorId":175189,"corporation":false,"usgs":false,"family":"Santana Castellon","given":"Eduardo","email":"","affiliations":[],"preferred":false,"id":650368,"contributorType":{"id":1,"text":"Authors"},"rank":19},{"text":"Vidal, Rosa","contributorId":175190,"corporation":false,"usgs":false,"family":"Vidal","given":"Rosa","email":"","affiliations":[],"preferred":false,"id":650369,"contributorType":{"id":1,"text":"Authors"},"rank":20},{"text":"Will, Tom","contributorId":149777,"corporation":false,"usgs":false,"family":"Will","given":"Tom","email":"","affiliations":[{"id":17821,"text":"U.S. Fish and Wildlife Service, Division of Migratory Birds","active":true,"usgs":false}],"preferred":false,"id":650370,"contributorType":{"id":1,"text":"Authors"},"rank":21}]}}
,{"id":70176790,"text":"70176790 - 2010 - Invertebrate mercury bioaccumulation in permanent, seasonal, and flooded rice wetlands within California's Central Valley","interactions":[],"lastModifiedDate":"2018-10-20T08:50:46","indexId":"70176790","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3352,"text":"Science of the Total Environment","active":true,"publicationSubtype":{"id":10}},"title":"Invertebrate mercury bioaccumulation in permanent, seasonal, and flooded rice wetlands within California's Central Valley","docAbstract":"<p><span>We examined methylmercury (MeHg) bioavailability in four of the most predominant wetland habitats in California's Central Valley agricultural region during the spring and summer: white rice, wild rice, permanent wetlands, and shallowly-flooded fallow fields. We sampled MeHg and total mercury (THg) concentrations in two aquatic macroinvertebrate taxa at the inlets, centers, and outlets of four replicated wetland habitats (8 wetlands total) during two time periods bounding the rice growing season and corresponding to flood-up and pre-harvest (96 total samples). In general, THg concentrations (mean&nbsp;±&nbsp;standard error) in Notonectidae (</span><i>Notonecta</i><span>, back swimmers; 1.18&nbsp;±&nbsp;0.08&nbsp;µg&nbsp;g</span><sup>−&nbsp;1</sup><span> dry weight [dw]) were higher than in Corixidae (</span><i>Corisella</i><span>, water boatmen; 0.89&nbsp;±&nbsp;0.06&nbsp;µg&nbsp;g</span><sup>−</sup><span>&nbsp;</span><sup>1</sup><span>&nbsp;dw, MeHg: 0.74&nbsp;±&nbsp;0.05&nbsp;µg&nbsp;g</span><sup>−</sup><span>&nbsp;</span><sup>1</sup><span>&nbsp;dw). MeHg concentrations were correlated with THg concentrations in Corixidae (</span><i>R</i><sup>2</sup><span>&nbsp;=&nbsp;0.80) and 88% of THg was in the MeHg form. Wetland habitat type had an important influence on THg concentrations in aquatic invertebrates, but this effect depended on the sampling time period and taxa. In particular, THg concentrations in Notonectidae, but not Corixidae, were higher in permanent wetlands than in white rice, wild rice, or shallowly-flooded fallow fields. THg concentrations in Notonectidae were higher at the end of the rice growing season than near the time of flood-up, whereas THg concentrations in Corixidae did not differ between time periods. The effect of wetland habitat type was more prevalent near the end of the rice growing season, when Notonectidae THg concentrations were highest in permanent wetlands. Additionally, invertebrate THg concentrations were higher at water outlets than at inlets of wetlands. Our results indicate that although invertebrate THg concentrations increased from the time of flood-up to draw-down of wetlands, temporarily flooded habitats such as white rice, wild rice, and shallowly-flooded fallow fields did not have higher THg or MeHg concentrations in invertebrates than permanent wetlands.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.scitotenv.2009.10.030","usgsCitation":"Ackerman, J., Miles, A.K., and Eagles-Smith, C.A., 2010, Invertebrate mercury bioaccumulation in permanent, seasonal, and flooded rice wetlands within California's Central Valley: Science of the Total Environment, v. 408, no. 3, p. 666-671, https://doi.org/10.1016/j.scitotenv.2009.10.030.","productDescription":"6 p.","startPage":"666","endPage":"671","ipdsId":"IP-008976","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true},{"id":34983,"text":"Contaminant Biology Program","active":true,"usgs":true}],"links":[{"id":329352,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","volume":"408","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57fe8151e4b0824b2d1480b6","contributors":{"authors":[{"text":"Ackerman, Joshua T. 0000-0002-3074-8322 jackerman@usgs.gov","orcid":"https://orcid.org/0000-0002-3074-8322","contributorId":147078,"corporation":false,"usgs":true,"family":"Ackerman","given":"Joshua T.","email":"jackerman@usgs.gov","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":false,"id":650322,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miles, A. Keith 0000-0002-3108-808X keith_miles@usgs.gov","orcid":"https://orcid.org/0000-0002-3108-808X","contributorId":196,"corporation":false,"usgs":true,"family":"Miles","given":"A.","email":"keith_miles@usgs.gov","middleInitial":"Keith","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":true,"id":650323,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Eagles-Smith, Collin A. 0000-0003-1329-5285 ceagles-smith@usgs.gov","orcid":"https://orcid.org/0000-0003-1329-5285","contributorId":505,"corporation":false,"usgs":true,"family":"Eagles-Smith","given":"Collin","email":"ceagles-smith@usgs.gov","middleInitial":"A.","affiliations":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true},{"id":289,"text":"Forest and Rangeland Ecosys Science Center","active":true,"usgs":true},{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true}],"preferred":true,"id":650324,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70176145,"text":"70176145 - 2010 - Mercury concentrations in fish from a Sierra Nevada foothill reservoir located downstream from historic gold-mining operations","interactions":[],"lastModifiedDate":"2018-10-20T09:41:59","indexId":"70176145","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1552,"text":"Environmental Monitoring and Assessment","onlineIssn":"1573-2959","printIssn":"0167-6369","active":true,"publicationSubtype":{"id":10}},"title":"Mercury concentrations in fish from a Sierra Nevada foothill reservoir located downstream from historic gold-mining operations","docAbstract":"<p><span>This study examined mercury concentrations in whole fish from Camp Far West Reservoir, an 830-ha reservoir in northern California, USA, located downstream from lands mined for gold during and following the Gold Rush of 1848–1864. Total mercury (reported as dry weight concentrations) was highest in spotted bass (mean, 0.93&nbsp;μg/g; range, 0.16–4.41&nbsp;μg/g) and lower in bluegill (mean, 0.45&nbsp;μg/g; range, 0.22–1.96&nbsp;μg/g) and threadfin shad (0.44&nbsp;μg/g; range, 0.21–1.34&nbsp;μg/g). Spatial patterns for mercury in fish indicated high concentrations upstream in the Bear River arm and generally lower concentrations elsewhere, including downstream near the dam. These findings coincided with patterns exhibited by methylmercury in water and sediment, and suggested that mercury-laden inflows from the Bear River were largely responsible for contaminating the reservoir ecosystem. Maximum concentrations of mercury in all three fish species, but especially bass, were high enough to warrant concern about toxic effects in fish and consumers of fish.</span></p>","language":"English","publisher":"Springer","doi":"10.1007/s10661-009-0836-6","usgsCitation":"Saiki, M.K., Martin, B.A., May, T.W., and Alpers, C.N., 2010, Mercury concentrations in fish from a Sierra Nevada foothill reservoir located downstream from historic gold-mining operations: Environmental Monitoring and Assessment, v. 163, no. 1, p. 313-326, https://doi.org/10.1007/s10661-009-0836-6.","productDescription":"14 p.","startPage":"313","endPage":"326","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true},{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true},{"id":34983,"text":"Contaminant Biology Program","active":true,"usgs":true}],"links":[{"id":328025,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Camp Far West Reservoir ","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -121.30511283874512,\n              39.070579040524656\n            ],\n            [\n              -121.32768630981444,\n              39.061182684881565\n            ],\n            [\n              -121.30099296569824,\n              39.03071923403441\n            ],\n            [\n              -121.2832260131836,\n              39.02131757437681\n            ],\n            [\n              -121.25344276428221,\n              39.02291794517652\n            ],\n            [\n              -121.24279975891112,\n              39.021117525479646\n            ],\n            [\n              -121.24151229858397,\n              39.02538511251651\n            ],\n            [\n              -121.24889373779295,\n              39.03085258191479\n            ],\n            [\n              -121.27086639404297,\n              39.03571960736407\n            ],\n            [\n              -121.28382682800293,\n              39.0409196203015\n            ],\n            [\n              -121.28751754760741,\n              39.05171842432893\n            ],\n            [\n              -121.2864875793457,\n              39.057916991834084\n            ],\n            [\n              -121.27704620361327,\n              39.056850610370276\n            ],\n            [\n              -121.27112388610838,\n              39.06051622918041\n            ],\n            [\n              -121.27206802368164,\n              39.06584769863456\n            ],\n            [\n              -121.28185272216797,\n              39.06917966257363\n            ],\n            [\n              -121.2919807434082,\n              39.071578579216556\n            ],\n            [\n              -121.30373954772949,\n              39.071045493675875\n            ],\n            [\n              -121.30511283874512,\n              39.070579040524656\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"163","issue":"1","noUsgsAuthors":false,"publicationDate":"2009-03-13","publicationStatus":"PW","scienceBaseUri":"57c6b0c0e4b0f2f0cebe61ef","contributors":{"authors":[{"text":"Saiki, Michael K.","contributorId":54671,"corporation":false,"usgs":true,"family":"Saiki","given":"Michael","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":647465,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Martin, Barbara A. 0000-0002-9415-6377 barbara_ann_martin@usgs.gov","orcid":"https://orcid.org/0000-0002-9415-6377","contributorId":2855,"corporation":false,"usgs":true,"family":"Martin","given":"Barbara","email":"barbara_ann_martin@usgs.gov","middleInitial":"A.","affiliations":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"preferred":true,"id":647466,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"May, Thomas W. tmay@usgs.gov","contributorId":2598,"corporation":false,"usgs":true,"family":"May","given":"Thomas","email":"tmay@usgs.gov","middleInitial":"W.","affiliations":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"preferred":false,"id":647467,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Alpers, Charles N. 0000-0001-6945-7365 cnalpers@usgs.gov","orcid":"https://orcid.org/0000-0001-6945-7365","contributorId":411,"corporation":false,"usgs":true,"family":"Alpers","given":"Charles","email":"cnalpers@usgs.gov","middleInitial":"N.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":647468,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70036230,"text":"70036230 - 2010 - Conservation practice establishment in two northeast Iowa watersheds: Strategies, water quality implications, and lessons learned","interactions":[],"lastModifiedDate":"2012-03-12T17:22:06","indexId":"70036230","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2456,"text":"Journal of Soil and Water Conservation","active":true,"publicationSubtype":{"id":10}},"title":"Conservation practice establishment in two northeast Iowa watersheds: Strategies, water quality implications, and lessons learned","docAbstract":"Coldwater trout streams are important natural resources in northeast Iowa. Extensive efforts have been made by state and federal agencies to protect and improve water quality in northeast Iowa streams that include Sny Magill Creek and Bloody Run Creek, which are located in Clayton County. A series of three water quality projects were implemented in Sny Magill Creek watershed during 1988 to 1999, which were supported by multiple agencies and focused on best management practice (BMP) adoption. Water quality monitoring was performed during 1992 to 2001 to assess the impact of these installed BMPs in the Sny Magill Creek watershed using a paired watershed approach, where the Bloody Run Creek watershed served as the control. Conservation practice adoption still occurred in the Bloody Run Creek watershed during the 10-year monitoring project and accelerated after the project ended, when a multiagency supported water quality project was implemented during 2002 to 2007. Statistical analysis of the paired watershed results using a pre/post model indicated that discharge increased 8% in Sny Magill Creek watershed relative to the Bloody Run Creek watershed, turbidity declined 41%, total suspended sediment declined 7%, and NOx-N (nitrate-nitrogen plus nitrite-nitrogen) increased 15%. Similar results were obtained with a gradual change statistical model.The weak sediment reductions and increased NOx-N levels were both unexpected and indicate that dynamics between adopted BMPs and stream systems need to be better understood. Fish surveys indicate that conditions for supporting trout fisheries have improved in both streams. Important lessons to be taken from the overall study include (1) committed project coordinators, agency collaborators, and landowners/producers are all needed for successful water quality projects; (2) smaller watershed areas should be used in paired studies; (3) reductions in stream discharge may be required in these systems in order for significant sediment load decreases to occur; (4) long-term monitoring on the order of decades can be required to detect meaningful changes in water quality in response to BMP implementation; and (5) all consequences of specific BMPs need to be considered when considering strategies for watershed protection.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Soil and Water Conservation","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.2489/jswc.65.6.381","issn":"00224561","usgsCitation":"Gassman, P.W., Tisl, J., Palas, E., Fields, C., Isenhart, T., Schilling, K.E., Wolter, C., Seigley, L., and Helmers, M., 2010, Conservation practice establishment in two northeast Iowa watersheds: Strategies, water quality implications, and lessons learned: Journal of Soil and Water Conservation, v. 65, no. 6, p. 381-392, https://doi.org/10.2489/jswc.65.6.381.","startPage":"381","endPage":"392","numberOfPages":"12","costCenters":[],"links":[{"id":475817,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.2489/jswc.65.6.381","text":"Publisher Index Page"},{"id":246397,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":218395,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.2489/jswc.65.6.381"}],"volume":"65","issue":"6","noUsgsAuthors":false,"publicationDate":"2010-11-02","publicationStatus":"PW","scienceBaseUri":"5059f9f4e4b0c8380cd4d837","contributors":{"authors":[{"text":"Gassman, Philip W.","contributorId":33952,"corporation":false,"usgs":false,"family":"Gassman","given":"Philip","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":455001,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tisl, J.A.","contributorId":13849,"corporation":false,"usgs":true,"family":"Tisl","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":454999,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Palas, E.A.","contributorId":85449,"corporation":false,"usgs":true,"family":"Palas","given":"E.A.","email":"","affiliations":[],"preferred":false,"id":455006,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Fields, C.L.","contributorId":83343,"corporation":false,"usgs":true,"family":"Fields","given":"C.L.","email":"","affiliations":[],"preferred":false,"id":455005,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Isenhart, T.M.","contributorId":76963,"corporation":false,"usgs":true,"family":"Isenhart","given":"T.M.","email":"","affiliations":[],"preferred":false,"id":455004,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Schilling, K. E.","contributorId":61982,"corporation":false,"usgs":true,"family":"Schilling","given":"K.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":455003,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Wolter, C.F.","contributorId":23301,"corporation":false,"usgs":true,"family":"Wolter","given":"C.F.","email":"","affiliations":[],"preferred":false,"id":455000,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Seigley, L.S.","contributorId":35997,"corporation":false,"usgs":true,"family":"Seigley","given":"L.S.","email":"","affiliations":[],"preferred":false,"id":455002,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Helmers, M.J.","contributorId":89380,"corporation":false,"usgs":true,"family":"Helmers","given":"M.J.","email":"","affiliations":[],"preferred":false,"id":455007,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}}
,{"id":70186154,"text":"70186154 - 2010 - How vegetation and sediment transport feedbacks drive landscape change in the Everglades and wetlands worldwide","interactions":[],"lastModifiedDate":"2018-03-15T10:56:32","indexId":"70186154","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":740,"text":"American Naturalist","active":true,"publicationSubtype":{"id":10}},"title":"How vegetation and sediment transport feedbacks drive landscape change in the Everglades and wetlands worldwide","docAbstract":"<p><span>Mechanisms reported to promote landscape self‐organization cannot explain vegetation patterning oriented parallel to flow. Recent catastrophic shifts in Everglades landscape pattern and ecological function highlight the need to understand the feedbacks governing these ecosystems. We modeled feedback between vegetation, hydrology, and sediment transport on the basis of a decade of experimentation. Results from more than 100 simulations showed that flows just sufficient to redistribute sediment from sparsely vegetated sloughs to dense ridges were needed for an equilibrium patterned landscape oriented parallel to flow. Surprisingly, although vegetation heterogeneity typically conveys resilience, in wetlands governed by flow/sediment feedbacks it indicates metastability, whereby the landscape is prone to catastrophic shifts. Substantial increases or decreases in flow relative to the equilibrium condition caused an expansion of emergent vegetation and loss of open‐water areas that was unlikely to revert upon restoration of the equilibrium hydrology. Understanding these feedbacks is critical in forecasting wetland responses to changing conditions and designing management strategies that optimize ecosystem services, such as carbon sequestration or habitat provision. Our model and new sensitivity analysis techniques address these issues and make it newly apparent that simply returning flow to predrainage conditions in the Everglades may not be sufficient to restore historic landscape patterns and processes.</span></p>","language":"English","publisher":"American Society of Naturalists","doi":"10.1086/655215","usgsCitation":"Larsen, L., and Harvey, J.W., 2010, How vegetation and sediment transport feedbacks drive landscape change in the Everglades and wetlands worldwide: American Naturalist, v. 176, no. 3, p. E66-E79, https://doi.org/10.1086/655215.","productDescription":"14 p.","startPage":"E66","endPage":"E79","ipdsId":"IP-010084","costCenters":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"links":[{"id":338799,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"176","issue":"3","publishingServiceCenter":{"id":9,"text":"Reston PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58de1952e4b02ff32c699cbb","contributors":{"authors":[{"text":"Larsen, Laurel G. lglarsen@usgs.gov","contributorId":1987,"corporation":false,"usgs":true,"family":"Larsen","given":"Laurel G.","email":"lglarsen@usgs.gov","affiliations":[],"preferred":false,"id":687686,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Harvey, Judson W. 0000-0002-2654-9873 jwharvey@usgs.gov","orcid":"https://orcid.org/0000-0002-2654-9873","contributorId":1796,"corporation":false,"usgs":true,"family":"Harvey","given":"Judson","email":"jwharvey@usgs.gov","middleInitial":"W.","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":687685,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70036540,"text":"70036540 - 2010 - Sensitivity of early life stages of freshwater mussels (Unionidae) to acute and chronic toxicity of lead, cadmium, and zinc in water","interactions":[],"lastModifiedDate":"2018-10-20T10:04:56","indexId":"70036540","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1571,"text":"Environmental Toxicology and Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"Sensitivity of early life stages of freshwater mussels (Unionidae) to acute and chronic toxicity of lead, cadmium, and zinc in water","docAbstract":"<p><span>Toxicity of lead, cadmium, or zinc to early life stages of freshwater mussels (fatmucket,&nbsp;</span><i>Lampsilis siliquoidea</i><span>; Neosho mucket,&nbsp;</span><i>L. rafinesqueana</i><span>) was evaluated in 48‐h exposures with mussel larvae (glochidia), in 96‐h exposures with newly transformed (5‐d‐old) and two‐ or six‐month‐old juvenile mussels, or in 28‐d exposures with two‐ or four‐month‐old mussels in reconstituted soft water. The 24‐h median effect concentrations (EC50s) for fatmucket glochidia (&gt;299 µg Pb/L, &gt;227 µg Cd/L, 2,685 µg Zn/L) and 96‐h EC50s for two‐ or six‐month‐old fatmucket (&gt;426 µg Pb/L, 199 µg Cd/L, 1,700 µg Zn/L) were much higher than 96‐h EC50s for newly transformed fatmucket (142 and 298 µg Pb/L, 16 µg Cd/L, 151 and 175 µg Zn/L) and Neosho mucket (188 µg Pb/L, 20 µg Cd/L, 145 µg Zn/L). Chronic values for fatmucket were 10 µg Pb/L, 6.0 µg Cd/L, and 63 and 68 µg Zn/L. When mussel data from the present study and the literature were included in updated databases for deriving U.S. Environmental Protection Agency water quality criteria, mussel genus mean acute values were in the lower percentiles of the sensitivity distribution of all freshwater species for Pb (the 26th percentile), Cd (the 15th to 29th percentile), or Zn (the 12th to 21st percentile). The mussel (</span><i>Lampsilis</i><span>) genus mean chronic value was the lowest value ever reported for Pb (the 9th percentile) but was near the middle of the sensitivity distribution for Cd (the 61st percentile) or Zn (the 44th percentile). These results indicate that mussels were relatively sensitive to the acute toxicity of these three metals and to the chronic toxicity of Pb, but were moderately sensitive to the chronic toxicity of Cd or Zn compared to other freshwater species.</span></p>","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Environmental Toxicology and Chemistry","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1002/etc.250","issn":"07307268","usgsCitation":"Wang, N., Ingersoll, C.G., Ivey, C.D., Hardesty, D., May, T.W., Augspurger, T., Roberts, A., Van Genderen, E., and Barnhart, M., 2010, Sensitivity of early life stages of freshwater mussels (Unionidae) to acute and chronic toxicity of lead, cadmium, and zinc in water: Environmental Toxicology and Chemistry, v. 29, no. 9, p. 2053-2063, https://doi.org/10.1002/etc.250.","productDescription":"11 p.","startPage":"2053","endPage":"2063","numberOfPages":"11","costCenters":[{"id":34983,"text":"Contaminant Biology Program","active":true,"usgs":true}],"links":[{"id":217496,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1002/etc.250"},{"id":245447,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"29","issue":"9","noUsgsAuthors":false,"publicationDate":"2010-09-01","publicationStatus":"PW","scienceBaseUri":"505b8d2de4b08c986b3182b5","contributors":{"authors":[{"text":"Wang, Ning 0000-0002-2846-3352 nwang@usgs.gov","orcid":"https://orcid.org/0000-0002-2846-3352","contributorId":2818,"corporation":false,"usgs":true,"family":"Wang","given":"Ning","email":"nwang@usgs.gov","affiliations":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"preferred":true,"id":456618,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ingersoll, Christopher G. 0000-0003-4531-5949 cingersoll@usgs.gov","orcid":"https://orcid.org/0000-0003-4531-5949","contributorId":2071,"corporation":false,"usgs":true,"family":"Ingersoll","given":"Christopher","email":"cingersoll@usgs.gov","middleInitial":"G.","affiliations":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"preferred":true,"id":456616,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ivey, Chris D. 0000-0002-0485-7242 civey@usgs.gov","orcid":"https://orcid.org/0000-0002-0485-7242","contributorId":3308,"corporation":false,"usgs":true,"family":"Ivey","given":"Chris","email":"civey@usgs.gov","middleInitial":"D.","affiliations":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"preferred":true,"id":456614,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hardesty, Douglas K. dhardesty@usgs.gov","contributorId":3281,"corporation":false,"usgs":true,"family":"Hardesty","given":"Douglas K.","email":"dhardesty@usgs.gov","affiliations":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"preferred":true,"id":456615,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"May, Thomas W. tmay@usgs.gov","contributorId":2598,"corporation":false,"usgs":true,"family":"May","given":"Thomas","email":"tmay@usgs.gov","middleInitial":"W.","affiliations":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"preferred":false,"id":456617,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Augspurger, T.","contributorId":81844,"corporation":false,"usgs":false,"family":"Augspurger","given":"T.","email":"","affiliations":[],"preferred":false,"id":456619,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Roberts, A.D.","contributorId":87757,"corporation":false,"usgs":true,"family":"Roberts","given":"A.D.","email":"","affiliations":[],"preferred":false,"id":456620,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Van Genderen, E.","contributorId":17075,"corporation":false,"usgs":true,"family":"Van Genderen","given":"E.","affiliations":[],"preferred":false,"id":456613,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Barnhart, M.C.","contributorId":107410,"corporation":false,"usgs":true,"family":"Barnhart","given":"M.C.","affiliations":[],"preferred":false,"id":456621,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}}
,{"id":70036481,"text":"70036481 - 2010 - Sap flux-scaled transpiration by tamarisk (Tamarix spp.) before, during and after episodic defoliation by the saltcedar leaf beetle (Diorhabda carinulata)","interactions":[],"lastModifiedDate":"2012-03-12T17:22:04","indexId":"70036481","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":681,"text":"Agricultural and Forest Meteorology","active":true,"publicationSubtype":{"id":10}},"title":"Sap flux-scaled transpiration by tamarisk (Tamarix spp.) before, during and after episodic defoliation by the saltcedar leaf beetle (Diorhabda carinulata)","docAbstract":"The release of the saltcedar beetle (Diorhabda carinulata) has resulted in the periodic defoliation of tamarisk (Tamarix spp.) along more than 1000 river km in the upper Colorado River Basin and is expected to spread along many other river reaches throughout the upper basin, and possibly into the lower Colorado River Basin. Identifying the impacts of these release programs on tamarisk water use and subsequent water cycling in arid riparian systems are largely unknown, due in part to the difficulty of measuring water fluxes in these systems. We used lab-calibrated, modified heat-dissipation sap flux sensors to monitor tamarisk water use (n=20 trees) before, during and after defoliation by the saltcedar leaf beetle during the 2008 and 2009 growing seasons (May-October) in southeastern Utah. We incorporated a simple model that related mean stem sap flux density (Js) with atmospheric vapor pressure deficit (vpd) before the onset of defoliation in 2008. The model was used to calculate differences between predicted Js and Js measured throughout the two growing seasons. Episodic defoliation resulted in a 16% reduction in mean annual rates of Js in both 2008 and 2009, with decreases occurring only during the periods in which the trees were defoliated (about 6-8 weeks per growing season). In other words, rates of Js rebounded to values predicted by the model when the trees produced new leaves after defoliation. Sap flux data were scaled to stand water use by constructing a tamarisk-specific allometric equation to relate conducting sapwood area to stem diameter, and by measuring the size distribution of stems within the stand. Total water use in both years was 0.224m, representing a reduction of about 0.04myr-1. Results showed that repeated defoliation/refoliation cycles did not result in a progressive decrease in either leaf production or water use over the duration of the study. This investigation improves ground-based estimates of tamarisk water use, and will support future efforts to characterize impacts of the beetle on basin-wide hydrologic processes. ?? 2010 Elsevier B.V.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Agricultural and Forest Meteorology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.agrformet.2010.07.009","issn":"01681923","usgsCitation":"Hultine, K.R., Nagler, P., Morino, K., Bush, S., Burtch, K., Dennison, P., Glenn, E.P., and Ehleringer, J., 2010, Sap flux-scaled transpiration by tamarisk (Tamarix spp.) before, during and after episodic defoliation by the saltcedar leaf beetle (Diorhabda carinulata): Agricultural and Forest Meteorology, v. 150, no. 11, p. 1467-1475, https://doi.org/10.1016/j.agrformet.2010.07.009.","startPage":"1467","endPage":"1475","numberOfPages":"9","costCenters":[],"links":[{"id":218265,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.agrformet.2010.07.009"},{"id":246261,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"150","issue":"11","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b86bde4b08c986b3160de","contributors":{"authors":[{"text":"Hultine, K. R.","contributorId":102281,"corporation":false,"usgs":false,"family":"Hultine","given":"K.","middleInitial":"R.","affiliations":[],"preferred":false,"id":456352,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nagler, P.L. 0000-0003-0674-103X","orcid":"https://orcid.org/0000-0003-0674-103X","contributorId":29937,"corporation":false,"usgs":true,"family":"Nagler","given":"P.L.","affiliations":[],"preferred":false,"id":456348,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Morino, K.","contributorId":10614,"corporation":false,"usgs":true,"family":"Morino","given":"K.","affiliations":[],"preferred":false,"id":456345,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bush, S.E.","contributorId":78567,"corporation":false,"usgs":true,"family":"Bush","given":"S.E.","email":"","affiliations":[],"preferred":false,"id":456351,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Burtch, K.G.","contributorId":18213,"corporation":false,"usgs":true,"family":"Burtch","given":"K.G.","email":"","affiliations":[],"preferred":false,"id":456346,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Dennison, P.E.","contributorId":73430,"corporation":false,"usgs":true,"family":"Dennison","given":"P.E.","email":"","affiliations":[],"preferred":false,"id":456350,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Glenn, E. P.","contributorId":24463,"corporation":false,"usgs":false,"family":"Glenn","given":"E.","middleInitial":"P.","affiliations":[],"preferred":false,"id":456347,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Ehleringer, J.R.","contributorId":47965,"corporation":false,"usgs":true,"family":"Ehleringer","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":456349,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":70036479,"text":"70036479 - 2010 - Assemblage patterns of fish functional groups relative to habitat connectivity and conditions in floodplain lakes","interactions":[],"lastModifiedDate":"2012-03-12T17:22:04","indexId":"70036479","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1471,"text":"Ecology of Freshwater Fish","active":true,"publicationSubtype":{"id":10}},"title":"Assemblage patterns of fish functional groups relative to habitat connectivity and conditions in floodplain lakes","docAbstract":"We evaluated the influences of habitat connectivity and local environmental factors on the distribution and abundance patterns of fish functional groups in 17 floodplain lakes in the Yazoo River Basin, USA. The results of univariate and multivariate analyses showed that species-environmental relationships varied with the functional groups. Species richness and assemblage structure of periodic strategists showed strong and positive correlations with habitat connectivity. Densities of most equilibrium and opportunistic strategists decreased with habitat connectivity. Densities of certain equilibrium and opportunistic strategists increased with turbidity. Forested wetlands around the lakes were positively related to the densities of periodic and equilibrium strategists. These results suggest that decreases in habitat connectivity, forested wetland buffers and water quality resulting from environmental manipulations may cause local extinction of certain fish taxa and accelerate the dominance of tolerant fishes in floodplain lakes. ?? 2010 John Wiley & Sons A/S.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Ecology of Freshwater Fish","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1111/j.1600-0633.2010.00438.x","issn":"09066691","usgsCitation":"Miyazono, S., Aycock, J., Miranda, L., and Tietjen, T., 2010, Assemblage patterns of fish functional groups relative to habitat connectivity and conditions in floodplain lakes: Ecology of Freshwater Fish, v. 19, no. 4, p. 578-585, https://doi.org/10.1111/j.1600-0633.2010.00438.x.","startPage":"578","endPage":"585","numberOfPages":"8","costCenters":[],"links":[{"id":218235,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1111/j.1600-0633.2010.00438.x"},{"id":246227,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"19","issue":"4","noUsgsAuthors":false,"publicationDate":"2010-11-11","publicationStatus":"PW","scienceBaseUri":"5059edc5e4b0c8380cd499c1","contributors":{"authors":[{"text":"Miyazono, S.","contributorId":79310,"corporation":false,"usgs":true,"family":"Miyazono","given":"S.","affiliations":[],"preferred":false,"id":456339,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Aycock, J.N.","contributorId":105151,"corporation":false,"usgs":true,"family":"Aycock","given":"J.N.","email":"","affiliations":[],"preferred":false,"id":456341,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Miranda, L.E.","contributorId":58406,"corporation":false,"usgs":true,"family":"Miranda","given":"L.E.","affiliations":[],"preferred":false,"id":456338,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Tietjen, T.E.","contributorId":93249,"corporation":false,"usgs":true,"family":"Tietjen","given":"T.E.","email":"","affiliations":[],"preferred":false,"id":456340,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
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