{"pageNumber":"203","pageRowStart":"5050","pageSize":"25","recordCount":10466,"records":[{"id":70156341,"text":"70156341 - 2010 - An overview of marine biodiversity in United States waters","interactions":[],"lastModifiedDate":"2022-11-09T15:51:49.76254","indexId":"70156341","displayToPublicDate":"2010-08-02T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2980,"text":"PLoS ONE","active":true,"publicationSubtype":{"id":10}},"title":"An overview of marine biodiversity in United States waters","docAbstract":"<p><span>Marine biodiversity of the United States (U.S.) is extensively documented, but data assembled by the United States National Committee for the Census of Marine Life demonstrate that even the most complete taxonomic inventories are based on records scattered in space and time. The best-known taxa are those of commercial importance. Body size is directly correlated with knowledge of a species, and knowledge also diminishes with distance from shore and depth. Measures of biodiversity other than species diversity, such as ecosystem and genetic diversity, are poorly documented. Threats to marine biodiversity in the U.S. are the same as those for most of the world: overexploitation of living resources; reduced water quality; coastal development; shipping; invasive species; rising temperature and concentrations of carbon dioxide in the surface ocean, and other changes that may be consequences of global change, including shifting currents; increased number and size of hypoxic or anoxic areas; and increased number and duration of harmful algal blooms. More information must be obtained through field and laboratory research and monitoring that involve innovative sampling techniques (such as genetics and acoustics), but data that already exist must be made accessible. And all data must have a temporal component so trends can be identified. As data are compiled, techniques must be developed to make certain that scales are compatible, to combine and reconcile data collected for various purposes with disparate gear, and to automate taxonomic changes. Information on biotic and abiotic elements of the environment must be interactively linked. Impediments to assembling existing data and collecting new data on marine biodiversity include logistical problems as well as shortages in finances and taxonomic expertise.</span></p>","language":"English","publisher":"PubMed Central","doi":"10.1371/journal.pone.0011914","usgsCitation":"Fautin, D.G., Delton, P., Incze, L.S., Leong, J.C., Pautzke, C., Rosenberg, A.A., Sandifer, P., Sedberry, G.R., Tunnell, J.W., Abbott, I., Brainard, R.E., Brodeur, M., Eldredge, L.G., Feldman, M., Moretzsohn, F., Vroom, P.S., Wainstein, M., and Wolff, N., 2010, An overview of marine biodiversity in United States waters: PLoS ONE, v. 5, no. 8, e11914; 47 p., https://doi.org/10.1371/journal.pone.0011914.","productDescription":"e11914; 47 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":475678,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1371/journal.pone.0011914","text":"Publisher Index 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,{"id":70236420,"text":"70236420 - 2010 - Modeling the effects of wave climate and sediment supply variability on large-scale shoreline change","interactions":[],"lastModifiedDate":"2022-09-06T16:54:31.641672","indexId":"70236420","displayToPublicDate":"2010-08-01T11:32:36","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2667,"text":"Marine Geology","active":true,"publicationSubtype":{"id":10}},"title":"Modeling the effects of wave climate and sediment supply variability on large-scale shoreline change","docAbstract":"<p>The application of an integrated data analysis and modeling scheme reveals that decadal-scale shoreline evolution along a U.S. Pacific Northwest littoral cell is highly dependent on both sediment supply and wave climate variability. In particular, accurate estimates of (Columbia River) sediment supply and sediment feeding from the lower shoreface are critical components of balancing the barrier beach sediment budget and are therefore essential to making sensible shoreline change hindcasts and forecasts. A simple deterministic one-line shoreline change model, applied in a quasi-probabilistic manner, enables evaluation of the influence of sediment supply and wave climate variability through simulation of historical shoreline change. Through iteration, a range of realistic scenarios are developed to constrain decadal-scale shoreline change predictions. Modeled shoreline changes are significantly sensitive to directional changes in the incident waves, and therefore sensitive to the occurrence of interannual climatic fluctuations such as major El Niño events. A predicted increase in the intensity of the east Pacific wave climate (1.0 m increase in significant wave height in 20 yr) affects forecast shoreline positions only when this increase occurs during the winter storm season. However, the effect of this increase in storm power during any given year is small relative to the impact of major El Niño events. The model has significant skill in decadal-scale hindcasts suggesting that alongshore gradients in sediment transport dominate coastal change at this scale at this site. However, both data and model results suggest that net onshore feeding from the lower shoreface is responsible for approximately 20% of the decadal-scale coastal change. Field measurements and poor model skill at annual scale indicate that cross-shore processes likely dominate coastal change at shorter time scales.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.margeo.2010.02.008","usgsCitation":"Ruggiero, P., Buijsman, M.C., Kaminsky, G.M., and Gelfenbaum, G.R., 2010, Modeling the effects of wave climate and sediment supply variability on large-scale shoreline change: Marine Geology, v. 273, no. 1-4, p. 127-140, https://doi.org/10.1016/j.margeo.2010.02.008.","productDescription":"14 p.","startPage":"127","endPage":"140","costCenters":[],"links":[{"id":406244,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Oregon, Washington","otherGeospatial":"Columbia River, Grays Harbor, Willapa Bay","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -124.26635742187501,\n              47.12995075666307\n            ],\n            [\n              -124.03564453125,\n              45.72152152227954\n            ],\n            [\n              -122.89306640624999,\n              45.82879925192134\n            ],\n            [\n              -122.98095703125,\n              47.03269459852135\n            ],\n            [\n              -124.26635742187501,\n              47.12995075666307\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"273","issue":"1-4","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Ruggiero, Peter","contributorId":15709,"corporation":false,"usgs":false,"family":"Ruggiero","given":"Peter","affiliations":[{"id":6680,"text":"Oregon State University","active":true,"usgs":false}],"preferred":false,"id":850944,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Buijsman, Maarten C.","contributorId":76340,"corporation":false,"usgs":true,"family":"Buijsman","given":"Maarten","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":850945,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kaminsky, George M.","contributorId":83150,"corporation":false,"usgs":true,"family":"Kaminsky","given":"George","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":850946,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Gelfenbaum, Guy R. 0000-0003-1291-6107 ggelfenbaum@usgs.gov","orcid":"https://orcid.org/0000-0003-1291-6107","contributorId":742,"corporation":false,"usgs":true,"family":"Gelfenbaum","given":"Guy","email":"ggelfenbaum@usgs.gov","middleInitial":"R.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true},{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"preferred":true,"id":850947,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70201009,"text":"70201009 - 2010 - Crater population and resurfacing of the Martian north polar layered deposits","interactions":[],"lastModifiedDate":"2018-11-20T10:32:04","indexId":"70201009","displayToPublicDate":"2010-08-01T10:31:31","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2317,"text":"Journal of Geophysical Research E: Planets","active":true,"publicationSubtype":{"id":10}},"title":"Crater population and resurfacing of the Martian north polar layered deposits","docAbstract":"<p><span>Present‐day accumulation in the north polar layered deposits (NPLD) is thought to occur via deposition on the north polar residual cap. Understanding current mass balance in relation to current climate would provide insight into the climatic record of the NPLD. To constrain processes and rates of NPLD resurfacing, a search for craters was conducted using images from the Mars Reconnaissance Orbiter Context Camera. One hundred thirty craters have been identified on the NPLD, 95 of which are located within a region defined to represent recent accumulation. High Resolution Imaging Science Experiment images of craters in this region reveal a morphological sequence of crater degradation that provides a qualitative understanding of processes involved in crater removal. A classification system for these craters was developed based on the amount of apparent degradation and infilling and where possible depth/diameter ratios were determined. The temporal and spatial distribution of crater degradation is interpreted to be close to uniform. Through comparison of the size‐frequency distribution of these craters with the expected production function, the craters are interpreted to be an equilibrium population with a crater of diameter&nbsp;</span><i>D</i><span>&nbsp;meters having a lifetime of ∼30.75</span><i>D</i><sup>1.14</sup><span>&nbsp;years. Accumulation rates within these craters are estimated at 7.2</span><i>D</i><sup>−0.14</sup><span>mm/yr, which corresponds to values of ∼3–4 mm/yr and are much higher than rates thought to apply to the surrounding flat terrain. The current crater population is estimated to have accumulated in the last ∼20 kyr or less.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/2009JE003523","usgsCitation":"Banks, M.E., Byrne, S., Galla, K., McEwen, A.S., Bray, V.J., Dundas, C.M., Fishbaugh, K.E., Herkenhoff, K.E., and Murray, B.C., 2010, Crater population and resurfacing of the Martian north polar layered deposits: Journal of Geophysical Research E: Planets, v. 115, no. E8, 11 p., https://doi.org/10.1029/2009JE003523.","productDescription":"11 p.","costCenters":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"links":[{"id":475679,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1029/2009je003523","text":"Publisher Index Page"},{"id":359596,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Mars","volume":"115","issue":"E8","noUsgsAuthors":false,"publicationDate":"2010-08-28","publicationStatus":"PW","scienceBaseUri":"5bf52b6be4b045bfcae28014","contributors":{"authors":[{"text":"Banks, Maria E.","contributorId":80914,"corporation":false,"usgs":true,"family":"Banks","given":"Maria","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":751675,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Byrne, Shane","contributorId":192609,"corporation":false,"usgs":false,"family":"Byrne","given":"Shane","email":"","affiliations":[],"preferred":false,"id":751676,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Galla, Kapil","contributorId":210752,"corporation":false,"usgs":false,"family":"Galla","given":"Kapil","email":"","affiliations":[{"id":25655,"text":"Lunar and Planetary Laboratory, 1629 E. University Blvd., The University of Arizona, Tucson, AZ 85721, United States","active":true,"usgs":false}],"preferred":false,"id":751677,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"McEwen, Alfred S.","contributorId":61657,"corporation":false,"usgs":false,"family":"McEwen","given":"Alfred","email":"","middleInitial":"S.","affiliations":[{"id":7042,"text":"University of Arizona","active":true,"usgs":false}],"preferred":false,"id":751678,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Bray, Veronica J.","contributorId":204232,"corporation":false,"usgs":false,"family":"Bray","given":"Veronica","email":"","middleInitial":"J.","affiliations":[{"id":36888,"text":"Lunar and Planetary Laboratory, University of Arizona","active":true,"usgs":false}],"preferred":false,"id":751679,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Dundas, Colin M. 0000-0003-2343-7224 cdundas@usgs.gov","orcid":"https://orcid.org/0000-0003-2343-7224","contributorId":2937,"corporation":false,"usgs":true,"family":"Dundas","given":"Colin","email":"cdundas@usgs.gov","middleInitial":"M.","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":true,"id":751680,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Fishbaugh, Kathryn E.","contributorId":210540,"corporation":false,"usgs":false,"family":"Fishbaugh","given":"Kathryn","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":751681,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Herkenhoff, Kenneth E. 0000-0002-3153-6663 kherkenhoff@usgs.gov","orcid":"https://orcid.org/0000-0002-3153-6663","contributorId":2275,"corporation":false,"usgs":true,"family":"Herkenhoff","given":"Kenneth","email":"kherkenhoff@usgs.gov","middleInitial":"E.","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":true,"id":751682,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Murray, Bruce C.","contributorId":61992,"corporation":false,"usgs":true,"family":"Murray","given":"Bruce","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":751683,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}}
,{"id":98510,"text":"sim3064 - 2010 - Seismicity of the Earth 1900-2007","interactions":[{"subject":{"id":98510,"text":"sim3064 - 2010 - Seismicity of the Earth 1900-2007","indexId":"sim3064","publicationYear":"2010","noYear":false,"title":"Seismicity of the Earth 1900-2007"},"predicate":"SUPERSEDED_BY","object":{"id":70208267,"text":"sim3446 - 2020 - Seismicity of the Earth 1900–2018","indexId":"sim3446","publicationYear":"2020","noYear":false,"title":"Seismicity of the Earth 1900–2018"},"id":1}],"supersededBy":{"id":70208267,"text":"sim3446 - 2020 - Seismicity of the Earth 1900–2018","indexId":"sim3446","publicationYear":"2020","noYear":false,"title":"Seismicity of the Earth 1900–2018"},"lastModifiedDate":"2020-02-11T06:46:50","indexId":"sim3064","displayToPublicDate":"2010-07-13T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":333,"text":"Scientific Investigations Map","code":"SIM","onlineIssn":"2329-132X","printIssn":"2329-1311","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"3064","title":"Seismicity of the Earth 1900-2007","docAbstract":"This map illustrates more than one century of global seismicity in the context of global plate tectonics and the Earth's physiography. Primarily designed for use by earth scientists and engineers interested in earthquake hazards of the 20th and early 21st centuries, this map provides a comprehensive overview of strong earthquakes since 1900. The map clearly identifies the location of the 'great' earthquakes (M8.0 and larger) and the rupture area, if known, of the M8.3 or larger earthquakes. The earthquake symbols are scaled proportional to the moment magnitude and therefore to the area of faulting, thus providing a better understanding of the relative sizes and distribution of earthquakes in the magnitude range 5.5 to 9.5. Plotting the known rupture area of the largest earthquakes also provides a better appreciation of the extent of some of the most famous and damaging earthquakes in modern history. All earthquakes shown on the map were carefully relocated using a standard earth reference model and standardized location procedures, thereby eliminating gross errors and biases in locations of historically important earthquakes that are often found in numerous seismicity catalogs.\r\n","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/sim3064","usgsCitation":"Tarr, A.C., Villasenor, A.H., Furlong, K.P., Rhea, S., and Benz, H.M., 2010, Seismicity of the Earth 1900-2007: U.S. Geological Survey Scientific Investigations Map 3064, 1 Sheet: 74.49 x 36.00 inches, https://doi.org/10.3133/sim3064.","productDescription":"1 Sheet: 74.49 x 36.00 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"links":[{"id":125934,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/sim_3064.jpg"},{"id":13900,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sim/3064/","linkFileType":{"id":5,"text":"html"}}],"scale":"25000000","projection":"Robinson","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e6e4b07f02db5e7768","contributors":{"authors":[{"text":"Tarr, Arthur C. atarr@usgs.gov","contributorId":1925,"corporation":false,"usgs":true,"family":"Tarr","given":"Arthur","email":"atarr@usgs.gov","middleInitial":"C.","affiliations":[],"preferred":true,"id":305585,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Villasenor, Antonio H. 0000-0001-8592-4832","orcid":"https://orcid.org/0000-0001-8592-4832","contributorId":38186,"corporation":false,"usgs":true,"family":"Villasenor","given":"Antonio","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":305587,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Furlong, Kevin P. 0000-0002-2674-5110","orcid":"https://orcid.org/0000-0002-2674-5110","contributorId":19576,"corporation":false,"usgs":false,"family":"Furlong","given":"Kevin","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":305586,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Rhea, Susan","contributorId":81110,"corporation":false,"usgs":true,"family":"Rhea","given":"Susan","email":"","affiliations":[],"preferred":false,"id":305588,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Benz, Harley M. 0000-0002-6860-2134 benz@usgs.gov","orcid":"https://orcid.org/0000-0002-6860-2134","contributorId":794,"corporation":false,"usgs":true,"family":"Benz","given":"Harley","email":"benz@usgs.gov","middleInitial":"M.","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":true,"id":305584,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70156102,"text":"70156102 - 2010 - Sub-weekly to interannual variability of a high-energy shoreline","interactions":[],"lastModifiedDate":"2021-03-17T12:20:47.309201","indexId":"70156102","displayToPublicDate":"2010-07-07T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1262,"text":"Coastal Engineering","active":true,"publicationSubtype":{"id":10}},"title":"Sub-weekly to interannual variability of a high-energy shoreline","docAbstract":"<p><span>Sixty-one Global Positioning System (GPS), sub-aerial beach surveys were completed at 7</span><span>&nbsp;</span><span>km long Ocean Beach, San Francisco, CA (USA), between April 2004 and March 2009. The five-year time series contains over 1</span><span>&nbsp;</span><span>million beach elevation measurements and documents detailed changes in beach morphology over a variety of spatial, temporal, and physical forcing scales. Results show that seasonal processes dominate at Ocean Beach, with the seasonal increase and decrease in wave height being the primary driver of shoreline change. Storm events, while capable of causing large short-term changes in the shoreline, did not singularly account for a large percentage of the overall observed change. Empirical orthogonal function (EOF) analysis shows that the first two modes account for approximately three-quarters of the variance in the data set and are represented by the seasonal onshore/offshore movement of sediment (60%) and the multi-year trend of shoreline rotation (14%). The longer-term trend of shoreline rotation appears to be related to larger-scale bathymetric change. An EOF-based decomposition technique is developed that is capable of estimating the shoreline position to within one standard deviation of the range of shoreline positions observed at most locations along the beach. The foundation of the model is the observed relationship between the temporal amplitudes of the first EOF mode and seasonally-averaged offshore wave height as well as the linear trend of shoreline rotation. This technique, while not truly predictive because of the requirement of real-time wave data, is useful because it can predict shoreline position to within reasonable confidence given the absence of field data once the model is developed at a particular site.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.coastaleng.2010.05.011","usgsCitation":"Hansen, J., and Barnard, P.L., 2010, Sub-weekly to interannual variability of a high-energy shoreline: Coastal Engineering, v. 57, no. 11-12, p. 959-972, https://doi.org/10.1016/j.coastaleng.2010.05.011.","productDescription":"13 p.","startPage":"959","endPage":"972","numberOfPages":"13","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-011159","costCenters":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":306838,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Ocean Beach","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -122.51815795898436,\n              37.68708070686609\n            ],\n            [\n              -122.49412536621094,\n              37.68708070686609\n            ],\n            [\n              -122.49412536621094,\n              37.78102667641841\n            ],\n            [\n              -122.51815795898436,\n              37.78102667641841\n            ],\n            [\n              -122.51815795898436,\n              37.68708070686609\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"57","issue":"11-12","publishingServiceCenter":{"id":14,"text":"Menlo Park PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"55d45734e4b0518e354694f5","contributors":{"authors":[{"text":"Hansen, Jeff E.","contributorId":146437,"corporation":false,"usgs":false,"family":"Hansen","given":"Jeff E.","affiliations":[{"id":590,"text":"U.S. Army Corps of Engineers","active":false,"usgs":false}],"preferred":false,"id":567872,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Barnard, Patrick L. 0000-0003-1414-6476 pbarnard@usgs.gov","orcid":"https://orcid.org/0000-0003-1414-6476","contributorId":140982,"corporation":false,"usgs":true,"family":"Barnard","given":"Patrick","email":"pbarnard@usgs.gov","middleInitial":"L.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":567871,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70236328,"text":"70236328 - 2010 - New southeastern Nearctic Rhynchelmis (Rhynchelmoides) species and the description of Pararhynchelmis n. gen. (Annelida: Clitellata: Lumbriculidae)","interactions":[],"lastModifiedDate":"2022-09-02T13:37:21.81991","indexId":"70236328","displayToPublicDate":"2010-07-01T14:41:47","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3814,"text":"Zootaxa","onlineIssn":"1175-5334","printIssn":"1175-5326","active":true,"publicationSubtype":{"id":10}},"displayTitle":"New southeastern Nearctic <i>Rhynchelmis</i> (<i>Rhynchelmoides</i>) species and the description of <i>Pararhynchelmis</i> n. gen. (Annelida: Clitellata: Lumbriculidae)","title":"New southeastern Nearctic Rhynchelmis (Rhynchelmoides) species and the description of Pararhynchelmis n. gen. (Annelida: Clitellata: Lumbriculidae)","docAbstract":"<p>The first verified records of <i>Rhynchelmis</i> from the southeastern Nearctic represent two new species. Both belong to R. (Rhynchelmoides) (Hrabě) <strong>n. comb.</strong>, which is defined here. <i>Rhynchelmis bolinensis</i> <strong>n. sp.</strong> resembles other R. (Rhynchelmoides) species with elongate spermathecae, but differs in details of the reproductive structures. <i>Rhynchelmis croatanensis</i> <strong>n. sp.</strong> is similar in many respects, but the gonads and male and female pores are shifted anteriad by one segment, a character previously unknown within the genus. <i>Pararhynchelmis murdocki</i> <strong>n. gen.</strong>, <strong>n. sp.</strong> has the spermathecal pores in VIII and IX and male pores in X, and the spermathecae connect to the gut. These characters associate the new species with <i>Rhynchelmis</i>, but the combination of differences in morphology or arrangement of atria, spermathecae, blood vessels and nephridia, and the absence of a proboscis, suggest that it be placed in a related genus. <i>Rhynchelmis bolinensis</i> was collected at several sites in North Carolina, but the other two species are known only from single localities.<br></p>","language":"English","publisher":"Magnolia Press","doi":"10.11646/zootaxa.2554.1.1","usgsCitation":"Fend, S.V., and Lenat, D.R., 2010, New southeastern Nearctic Rhynchelmis (Rhynchelmoides) species and the description of Pararhynchelmis n. gen. (Annelida: Clitellata: Lumbriculidae): Zootaxa, v. 2554, no. 1, p. 1-22, https://doi.org/10.11646/zootaxa.2554.1.1.","productDescription":"22 p.","startPage":"1","endPage":"22","costCenters":[],"links":[{"id":406092,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Nearctic, North America","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -94.5703125,\n              29.458731185355344\n            ],\n            [\n              -90,\n              28.459033019728043\n            ],\n            [\n              -87.099609375,\n              29.76437737516313\n            ],\n            [\n              -85.341796875,\n              29.22889003019423\n            ],\n            [\n              -80.595703125,\n              29.305561325527698\n            ],\n            [\n              -80.771484375,\n              31.653381399664\n            ],\n            [\n              -74.8828125,\n              35.460669951495305\n            ],\n            [\n              -75.41015624999999,\n              37.16031654673677\n            ],\n            [\n              -73.30078125,\n              40.44694705960048\n            ],\n            [\n              -93.69140625,\n              40.97989806962013\n            ],\n            [\n              -94.5703125,\n              29.458731185355344\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"2554","issue":"1","noUsgsAuthors":false,"publicationDate":"2010-07-30","publicationStatus":"PW","contributors":{"authors":[{"text":"Fend, Steven V. 0000-0002-4638-6602 svfend@usgs.gov","orcid":"https://orcid.org/0000-0002-4638-6602","contributorId":3591,"corporation":false,"usgs":true,"family":"Fend","given":"Steven","email":"svfend@usgs.gov","middleInitial":"V.","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":850630,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lenat, David R.","contributorId":23500,"corporation":false,"usgs":true,"family":"Lenat","given":"David","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":850631,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70048508,"text":"70048508 - 2010 - Occurrence of herbicides and pharmaceutical and personal care products in surface water and groundwater around Liberty Bay, Puget Sound, Washington","interactions":[],"lastModifiedDate":"2014-08-20T08:49:11","indexId":"70048508","displayToPublicDate":"2010-07-01T13:43:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2262,"text":"Journal of Environmental Quality","active":true,"publicationSubtype":{"id":10}},"title":"Occurrence of herbicides and pharmaceutical and personal care products in surface water and groundwater around Liberty Bay, Puget Sound, Washington","docAbstract":"Organic contaminants, such as pharmaceuticals and personal care products (PPCPs), pose a risk to water quality and the health of ecosystems. This study was designed to determine if a coastal community lacking point sources, such as waste water treatment plant effluent, could release PPCPs, herbicides, and plasticizers at detectable levels to their surface water and groundwater. Research was conducted in Liberty Bay, an embayment within Puget Sound, where 70% of the population (∼10,000) uses septic systems. Sampling included collection of groundwater and surface water with grab samples and the use of polar organic chemical integrative samplers (POCIS). We analyzed for a broad spectrum of 25 commonly used compounds, including PPCPs, herbicides, and a flame retardant. Twelve contaminants were detected at least once; only N,N-diethyl-meta-toluamide, caffeine, and mecoprop, a herbicide not attributed to septic systems, were detected in more than one grab sample. The use of POCIS was essential because contaminants were present at very low levels (nanograms), which is common for PPCPs in general, but particularly so in such a small community. The use of POCIS allowed the detection of five compounds that were not present in grab samples. Data suggest that the community is contaminating local water with PPCPs; this effect is likely to increase as the population and product usage increase. The results presented here are a first step toward assessing the transport of herbicides and PPCPs into this coastal system.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Environmental Quality","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"American Society of Agronomy","doi":"10.2134/jeq2009.0189","usgsCitation":"Dougherty, J.A., Swarzenski, P.W., Dinicola, R., and Reinhard, M., 2010, Occurrence of herbicides and pharmaceutical and personal care products in surface water and groundwater around Liberty Bay, Puget Sound, Washington: Journal of Environmental Quality, v. 39, no. 4, p. 1173-1180, https://doi.org/10.2134/jeq2009.0189.","productDescription":"8 p.","startPage":"1173","endPage":"1180","numberOfPages":"8","ipdsId":"IP-021878","costCenters":[{"id":622,"text":"Washington Water Science Center","active":true,"usgs":true}],"links":[{"id":488158,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.2134/jeq2009.0189","text":"Publisher Index Page"},{"id":278273,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":278272,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.2134/jeq2009.0189"}],"country":"United States","state":"Washington","otherGeospatial":"Puget Sound","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -122.66,47.68 ], [ -122.66,47.76 ], [ -122.56,47.76 ], [ -122.56,47.68 ], [ -122.66,47.68 ] ] ] } } ] }","volume":"39","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"52625867e4b079a99629a10c","contributors":{"authors":[{"text":"Dougherty, Jennifer A.","contributorId":6114,"corporation":false,"usgs":true,"family":"Dougherty","given":"Jennifer","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":484882,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Swarzenski, Peter W. 0000-0003-0116-0578 pswarzen@usgs.gov","orcid":"https://orcid.org/0000-0003-0116-0578","contributorId":1070,"corporation":false,"usgs":true,"family":"Swarzenski","given":"Peter","email":"pswarzen@usgs.gov","middleInitial":"W.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":484881,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dinicola, Richard S. 0000-0003-4222-294X dinicola@usgs.gov","orcid":"https://orcid.org/0000-0003-4222-294X","contributorId":352,"corporation":false,"usgs":true,"family":"Dinicola","given":"Richard S.","email":"dinicola@usgs.gov","affiliations":[{"id":622,"text":"Washington Water Science Center","active":true,"usgs":true}],"preferred":true,"id":484880,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Reinhard, Martin","contributorId":87060,"corporation":false,"usgs":true,"family":"Reinhard","given":"Martin","affiliations":[],"preferred":false,"id":484883,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70200010,"text":"70200010 - 2010 - Pharmaceutical formulation facilities as sources of opioids and other pharmaceuticals to wastewater treatment plant effluents","interactions":[],"lastModifiedDate":"2021-05-27T18:02:23.725934","indexId":"70200010","displayToPublicDate":"2010-07-01T12:46:09","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1565,"text":"Environmental Science & Technology","onlineIssn":"1520-5851","printIssn":"0013-936X","active":true,"publicationSubtype":{"id":10}},"title":"Pharmaceutical formulation facilities as sources of opioids and other pharmaceuticals to wastewater treatment plant effluents","docAbstract":"<p>Facilities involved in the manufacture of pharmaceutical products are an under-investigated source of pharmaceuticals to the environment. Between 2004 and 2009, 35 to 38 effluent samples were collected from each of three wastewater treatment plants (WWTPs) in New York and analyzed for seven pharmaceuticals including opioids and muscle relaxants. Two WWTPs (NY2 and NY3) receive substantial flows (&gt;20% of plant flow) from pharmaceutical formulation facilities (PFF) and one (NY1) receives no PFF flow. Samples of effluents from 23 WWTPs across the United States were analyzed once for these pharmaceuticals as part of a national survey. Maximum pharmaceutical effluent concentrations for the national survey and NY1 effluent samples were generally &lt;1 microg/L. Four pharmaceuticals (methadone, oxycodone, butalbital, and metaxalone) in samples of NY3 effluent had median concentrations ranging from 3.4 to &gt;400 microg/L. Maximum concentrations of oxycodone (1700 microg/L) and metaxalone (3800 microg/L) in samples from NY3 effluent exceeded 1000 microg/L. Three pharmaceuticals (butalbital, carisoprodol, and oxycodone) in samples of NY2 effluent had median concentrations ranging from 2 to 11 microg/L. These findings suggest that current manufacturing practices at these PFFs can result in pharmaceuticals concentrations from 10 to 1000 times higher than those typically found in WWTP effluents.<br></p>","language":"English","publisher":"American Chemical Society","doi":"10.1021/es100356f","usgsCitation":"Phillips, P.J., Smith, S.G., Kolpin, D.W., Stinson, B.W., Zaugg, S.D., Buxton, H.T., Furlong, E.T., and Esposito, K., 2010, Pharmaceutical formulation facilities as sources of opioids and other pharmaceuticals to wastewater treatment plant effluents: Environmental Science & Technology, v. 44, no. 13, p. 4910-4916, https://doi.org/10.1021/es100356f.","productDescription":"7 p.","startPage":"4910","endPage":"4916","costCenters":[{"id":452,"text":"National Water Quality Laboratory","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":475695,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://www.ncbi.nlm.nih.gov/pmc/articles/2893609","text":"Publisher Index Page"},{"id":358248,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"44","issue":"13","noUsgsAuthors":false,"publicationDate":"2010-06-04","publicationStatus":"PW","scienceBaseUri":"5c10c6b6e4b034bf6a7f4673","contributors":{"authors":[{"text":"Phillips, Patrick J. 0000-0001-5915-2015 pjphilli@usgs.gov","orcid":"https://orcid.org/0000-0001-5915-2015","contributorId":172757,"corporation":false,"usgs":true,"family":"Phillips","given":"Patrick","email":"pjphilli@usgs.gov","middleInitial":"J.","affiliations":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"preferred":true,"id":747734,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smith, Steven G. sgsmith@usgs.gov","contributorId":1560,"corporation":false,"usgs":true,"family":"Smith","given":"Steven","email":"sgsmith@usgs.gov","middleInitial":"G.","affiliations":[],"preferred":true,"id":747735,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kolpin, Dana W. 0000-0002-3529-6505 dwkolpin@usgs.gov","orcid":"https://orcid.org/0000-0002-3529-6505","contributorId":1239,"corporation":false,"usgs":true,"family":"Kolpin","given":"Dana","email":"dwkolpin@usgs.gov","middleInitial":"W.","affiliations":[{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true}],"preferred":true,"id":747736,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Stinson, Brooke W.","contributorId":208570,"corporation":false,"usgs":false,"family":"Stinson","given":"Brooke","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":747737,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Zaugg, Steven D. sdzaugg@usgs.gov","contributorId":768,"corporation":false,"usgs":true,"family":"Zaugg","given":"Steven","email":"sdzaugg@usgs.gov","middleInitial":"D.","affiliations":[],"preferred":true,"id":747738,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Buxton, Herbert T. hbuxton@usgs.gov","contributorId":1911,"corporation":false,"usgs":true,"family":"Buxton","given":"Herbert","email":"hbuxton@usgs.gov","middleInitial":"T.","affiliations":[{"id":5056,"text":"Office of the AD Energy and Minerals, and Environmental Health","active":true,"usgs":true}],"preferred":true,"id":747739,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Furlong, Edward T. 0000-0002-7305-4603 efurlong@usgs.gov","orcid":"https://orcid.org/0000-0002-7305-4603","contributorId":740,"corporation":false,"usgs":true,"family":"Furlong","given":"Edward","email":"efurlong@usgs.gov","middleInitial":"T.","affiliations":[{"id":5046,"text":"Branch of Analytical Serv (NWQL)","active":true,"usgs":true},{"id":503,"text":"Office of Water Quality","active":true,"usgs":true},{"id":27111,"text":"National Water Quality Program","active":true,"usgs":true},{"id":191,"text":"Colorado Water Science Center","active":true,"usgs":true}],"preferred":true,"id":747740,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Esposito, Kathleen","contributorId":21835,"corporation":false,"usgs":true,"family":"Esposito","given":"Kathleen","email":"","affiliations":[],"preferred":false,"id":747741,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":98486,"text":"ofr20101083B - 2010 - Seismicity of the Earth 1900-2010, Aleutian arc and vicinity","interactions":[],"lastModifiedDate":"2023-08-28T18:55:10.981819","indexId":"ofr20101083B","displayToPublicDate":"2010-07-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2010-1083","chapter":"B","title":"Seismicity of the Earth 1900-2010, Aleutian arc and vicinity","docAbstract":"This map shows details of the Aleutian arc not visible in an earlier publication. The Aleutian arc extends about 3,000 km from the Gulf of Alaska to the Kamchatka Peninsula. It marks the region where the Pacific plate subducts into the mantle beneath the North America plate. This subduction is responsible for the generation of the Aleutian Islands and the deep offshore Aleutian Trench. Relative to a fixed North America plate, the Pacific plate is moving northwest at a rate that increases from about 55 mm per year at the arc's eastern edge to 75 mm per year near its western terminus. In the east, the convergence of the plates is nearly perpendicular to the plate boundary. However, because of the boundary's curvature, as one travels westward along the arc, the subduction becomes more and more oblique to the boundary until the relative plate motion becomes parallel to the arc at the Near Islands near its western edge.  Subduction zones such as the Aleutian arc are geologically complex and produce numerous earthquakes from multiple sources. Deformation of the overriding North America plate generates shallow crustal earthquakes, whereas slip at the interface of the plates generates interplate earthquakes that extend from near the base of the trench to depths of 40 to 60 km. At greater depths, Aleutian arc earthquakes occur within the subducting Pacific plate and can reach depths of 300 km. Since 1900, six great earthquakes have occurred along the Aleutian Trench, Alaska Peninsula, and Gulf of Alaska: M8.4 1906 Rat Islands; M8.6 1938 Shumagin Islands; M8.6 1946 Unimak Island; M8.6 1957 Andreanof Islands; M9.2 1964 Prince William Sound; and M8.7 1965 Rat Islands. Several relevant tectonic elements (plate boundaries and active volcanoes) provide a context for the seismicity presented on the main map panel. The plate boundaries are most accurate along the axis of the Aleutian Trench and more diffuse or speculative in extreme northeastern Russia. The active volcanoes parallel the Aleutian Trench from the Gulf of Alaska to the Rat Islands.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20101083B","collaboration":"Pennsylvania State University, CSIC (Consejo Superior de Investigaciones Cientificas)","usgsCitation":"Benz, H.M., Herman, M., Tarr, A.C., Hayes, G., Furlong, K.P., Villaseñor, A., Dart, R.L., and Rhea, S., 2010, Seismicity of the Earth 1900-2010, Aleutian arc and vicinity (Revised September 2011): U.S. Geological Survey Open-File Report 2010-1083, 1 Plate: 35.37 inches x 23.89 inches, https://doi.org/10.3133/ofr20101083B.","productDescription":"1 Plate: 35.37 inches x 23.89 inches","costCenters":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"links":[{"id":13872,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2010/1083/b/","linkFileType":{"id":5,"text":"html"}},{"id":116880,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr_2010_1083_B.png"},{"id":420199,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_93344.htm","linkFileType":{"id":5,"text":"html"}}],"scale":"5000000","projection":"Albers Equal Area Conic Projection","country":"Russia, United States","state":"Alaska","otherGeospatial":"Aleutian Arc","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -179.9,\n             50\n            ],\n            [\n              -144,\n              50\n            ],\n            [\n              -144,\n              62\n            ],\n            [\n              -179.9,\n              62\n            ],\n            [\n              -179.9,\n              50\n            ]\n          ]\n        ]\n      }\n    },\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              179.9,\n              62\n            ],\n            [\n              151.23739492960942,\n              62\n            ],\n            [\n              151.23739492960942,\n              50\n            ],\n            [\n              179.9,\n              50\n            ],\n            [\n              179.9,\n              62\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","edition":"Revised September 2011","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5fa8db","contributors":{"authors":[{"text":"Benz, Harley M. 0000-0002-6860-2134 benz@usgs.gov","orcid":"https://orcid.org/0000-0002-6860-2134","contributorId":794,"corporation":false,"usgs":true,"family":"Benz","given":"Harley","email":"benz@usgs.gov","middleInitial":"M.","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":true,"id":305485,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Herman, Matthew","contributorId":68426,"corporation":false,"usgs":true,"family":"Herman","given":"Matthew","affiliations":[],"preferred":false,"id":305490,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Tarr, Arthur C. atarr@usgs.gov","contributorId":1925,"corporation":false,"usgs":true,"family":"Tarr","given":"Arthur","email":"atarr@usgs.gov","middleInitial":"C.","affiliations":[],"preferred":true,"id":305487,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hayes, Gavin P. 0000-0003-3323-0112","orcid":"https://orcid.org/0000-0003-3323-0112","contributorId":6157,"corporation":false,"usgs":true,"family":"Hayes","given":"Gavin P.","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":true,"id":305488,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Furlong, Kevin P. 0000-0002-2674-5110","orcid":"https://orcid.org/0000-0002-2674-5110","contributorId":19576,"corporation":false,"usgs":false,"family":"Furlong","given":"Kevin","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":305489,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Villaseñor, Antonio","contributorId":100969,"corporation":false,"usgs":true,"family":"Villaseñor","given":"Antonio","affiliations":[],"preferred":false,"id":305492,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Dart, Richard L. dart@usgs.gov","contributorId":1209,"corporation":false,"usgs":true,"family":"Dart","given":"Richard","email":"dart@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":true,"id":305486,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Rhea, Susan","contributorId":81110,"corporation":false,"usgs":true,"family":"Rhea","given":"Susan","email":"","affiliations":[],"preferred":false,"id":305491,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":70209303,"text":"70209303 - 2010 - New York-Alabama lineament: A buried right-slip fault bordering the Appalachians and mid-continent North America","interactions":[],"lastModifiedDate":"2020-03-27T13:37:26","indexId":"70209303","displayToPublicDate":"2010-06-30T13:26:46","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1796,"text":"Geology","active":true,"publicationSubtype":{"id":10}},"title":"New York-Alabama lineament: A buried right-slip fault bordering the Appalachians and mid-continent North America","docAbstract":"<p><span>The&nbsp;</span><span class=\"ScopusTermHighlight\">New</span><span>&nbsp;York-Alabama (NY-AL)&nbsp;</span><span class=\"ScopusTermHighlight\">lineament</span><span>, recognized in 1978, is a magnetic anomaly that delineates a fundamental though historically enigmatic crustal boundary in eastern North America that is deeply buried beneath the Appalachian basin. Data not in the original aeromagnetic data set, particularly the lack of any information available at the time to constrain the southern continuation of the anomaly southwest of Tennessee, left the source of the&nbsp;</span><span class=\"ScopusTermHighlight\">lineament</span><span>&nbsp;open to conjecture. We use modern digital aeromagnetic maps to fill in these data gaps and, for the first time, constrain the southern termination of the NY-AL&nbsp;</span><span class=\"ScopusTermHighlight\">lineament</span><span>. Our analysis indicates that the&nbsp;</span><span class=\"ScopusTermHighlight\">lineament</span><span>&nbsp;reflects a crustal-scale, right-lateral strike-slip fault that has displaced anomalies attributed to Grenville orogenesis by ~220 km. Palinspastic restoration of this displacement rearranges the trace of the Grenville belt in southern Rodinia and implies only passive influence on later-formed Appalachian structures. The precise timing of dextral movement on the NY-AL structure is not resolvable from the existing data set, but it must have occurred during one of, or combinations of, the following events: (1) a late, postcontractional (post-Ottawan) stage of the Grenville orogeny; (2) late Neoproterozoic to Cambrian rifting of Laurentia; or (3) right-slip reactivation during the late Neoproterozoic-Cambrian rifting of Laurentia, or during Appalachian movements. Our palinspastic reconstruction also implies that the host rocks for modern earthquakes in the Eastern Tennessee Seismic Zone are metasedimentary gneisses, and it provides an explanation for the spatial location and size of the seismic zone. © 2010 Geological Society of America.</span></p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/G30978.1","issn":"00917613","usgsCitation":"Steltenpohl, M., Zietz, I., Horton,, J., and Daniels, D.L., 2010, New York-Alabama lineament: A buried right-slip fault bordering the Appalachians and mid-continent North America: Geology, v. 38, no. 6, p. 571-574, https://doi.org/10.1130/G30978.1.","productDescription":"4 p. ","startPage":"571","endPage":"574","costCenters":[],"links":[{"id":373612,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States ","state":"New York, Pennsylvania, Ohio, Kentucky, Tennessee, Virginia, West Virginia, Maryland ","otherGeospatial":"Appalachian Basin ","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -75.9814453125,\n              44.02442151965934\n            ],\n            [\n              -77.431640625,\n              43.26120612479979\n            ],\n            [\n              -78.837890625,\n              43.229195113965005\n            ],\n            [\n              -82.96875,\n              41.47566020027821\n            ],\n            [\n              -83.75976562499999,\n              38.92522904714054\n            ],\n            [\n              -86.8359375,\n              36.84446074079564\n            ],\n            [\n              -87.8466796875,\n              35.782170703266075\n            ],\n            [\n              -78.7060546875,\n              37.89219554724437\n            ],\n            [\n              -75.6298828125,\n              40.64730356252251\n            ],\n            [\n              -74.4873046875,\n              42.22851735620852\n            ],\n            [\n              -75.9814453125,\n              44.02442151965934\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"38","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Steltenpohl, M.G.","contributorId":6272,"corporation":false,"usgs":true,"family":"Steltenpohl","given":"M.G.","affiliations":[],"preferred":false,"id":785981,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Zietz, I.","contributorId":59937,"corporation":false,"usgs":true,"family":"Zietz","given":"I.","email":"","affiliations":[],"preferred":false,"id":785982,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Horton,, J. Wright Jr. 0000-0001-6756-6365","orcid":"https://orcid.org/0000-0001-6756-6365","contributorId":219824,"corporation":false,"usgs":true,"family":"Horton,","given":"J. Wright","suffix":"Jr.","affiliations":[{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true}],"preferred":true,"id":785983,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Daniels, D. L.","contributorId":69114,"corporation":false,"usgs":true,"family":"Daniels","given":"D.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":785984,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70150460,"text":"70150460 - 2010 - The effects of road crossings on prairie stream habitat and function","interactions":[],"lastModifiedDate":"2015-06-26T09:18:13","indexId":"70150460","displayToPublicDate":"2010-06-29T10:15:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2299,"text":"Journal of Freshwater Ecology","active":true,"publicationSubtype":{"id":10}},"title":"The effects of road crossings on prairie stream habitat and function","docAbstract":"<p>Improperly designed stream crossing structures may alter the form and function of stream ecosystems and habitat and prohibit the movement of aquatic organisms. Stream sections adjoining five concrete box culverts, five low-water crossings (concrete slabs vented by one or multiple culverts), and two large, single corrugated culvert vehicle crossings in eastern Kansas streams were compared to reference reaches using a geomorphologic survey and stream classification. Stream reaches were also compared upstream and downstream of crossings, and crossing measurements were used to determine which crossing design best mimicked the natural dimensions of the adjoining stream. Four of five low-water crossings, three of five box culverts, and one of two large, single corrugated pipe culverts changed classification from upstream to downstream of the crossings. Mean riffle spacing upstream at low-water crossings (8.6 bankfull widths) was double that of downstream reaches (mean 4.4 bankfull widths) but was similar upstream and downstream of box and corrugated pipe culverts. There also appeared to be greater deposition of fine sediments directly upstream of these designs. Box and corrugated culverts were more similar to natural streams than low-water crossings at transporting water, sediments, and debris during bankfull flows.</p>","language":"English","publisher":"Oikos Publishers","publisherLocation":"La Crosse, WI","doi":"10.1080/02705060.2010.9664398","usgsCitation":"Bouska, W.W., Keane, T., and Paukert, C.P., 2010, The effects of road crossings on prairie stream habitat and function: Journal of Freshwater Ecology, v. 25, no. 4, p. 499-506, https://doi.org/10.1080/02705060.2010.9664398.","productDescription":"8 p.","startPage":"499","endPage":"506","numberOfPages":"8","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-013445","costCenters":[{"id":198,"text":"Coop Res Unit Atlanta","active":true,"usgs":true}],"links":[{"id":302357,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"25","issue":"4","publishingServiceCenter":{"id":8,"text":"Raleigh PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"558e77bee4b0b6d21dd6597b","contributors":{"authors":[{"text":"Bouska, Wesley W.","contributorId":143724,"corporation":false,"usgs":false,"family":"Bouska","given":"Wesley","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":556933,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Keane, Timothy","contributorId":143725,"corporation":false,"usgs":false,"family":"Keane","given":"Timothy","email":"","affiliations":[],"preferred":false,"id":556934,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Paukert, Craig P. 0000-0002-9369-8545 cpaukert@usgs.gov","orcid":"https://orcid.org/0000-0002-9369-8545","contributorId":879,"corporation":false,"usgs":true,"family":"Paukert","given":"Craig","email":"cpaukert@usgs.gov","middleInitial":"P.","affiliations":[{"id":198,"text":"Coop Res Unit Atlanta","active":true,"usgs":true}],"preferred":true,"id":556918,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70198318,"text":"70198318 - 2010 - An improved proximal tephrochronology for Redoubt Volcano, Alaska","interactions":[],"lastModifiedDate":"2018-07-31T09:43:50","indexId":"70198318","displayToPublicDate":"2010-06-20T09:57:50","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2499,"text":"Journal of Volcanology and Geothermal Research","active":true,"publicationSubtype":{"id":10}},"title":"An improved proximal tephrochronology for Redoubt Volcano, Alaska","docAbstract":"<p><span>Sediment cores from lakes in volcanically active regions can be used to reconstruct the frequency of tephra-fall events. We studied sediment cores from two lakes within 25</span><span>&nbsp;</span><span>km of the summit of Redoubt Volcano, western Cook Inlet, to develop a robust age model for the Holocene tephrochronology, and to assess the extent to which the tephrostratigraphies were correlative between the two nearby lakes. Visually distinct tephra layers were correlated among cores from Bear and Cub lakes, located within 17</span><span>&nbsp;</span><span>km of each other, to construct a composite age model, which incorporates two Pu-activity profiles and 27 radiocarbon ages, and extends the record back to 11,540</span><span>&nbsp;</span><span>cal a BP. The age model was used to interpolate the ages and quantify the uncertainties of ages for all tephras at least 1</span><span>&nbsp;</span><span>mm thick. Between −</span><span>&nbsp;</span><span>55 and 3850</span><span>&nbsp;</span><span>a BP, 31 tephras were deposited in Bear Lake and 41 tephras in Cub Lake. Bear Lake contains an additional 38 tephras deposited between 11,540 and 3850</span><span>&nbsp;</span><span>a BP. During the period of overlap, (−</span><span>&nbsp;</span><span>55 to 3850</span><span>&nbsp;</span><span>a BP), 24 tephras are of significantly different ages, including nine from Bear Lake and 17 from Cub Lake. The presence of these unique tephras indicates that ejecta plumes erupted from Redoubt Volcano can be highly directional, and that sediment cores from more than one lake are needed for a comprehensive reconstruction of tephra-fall events. Unlike distal lakes in south Alaska, where geomorphic and limnological factors dominate the quality of the tephrostratigraphic record, the variability in tephra-fall trajectory near a Redoubt Volcano appears to be a major control on the number of tephras contained in the sediment of proximal lakes.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.jvolgeores.2010.03.015","usgsCitation":"Schiff, C., Kaufman, D.S., Wallace, K.L., and Ketterer, M.E., 2010, An improved proximal tephrochronology for Redoubt Volcano, Alaska: Journal of Volcanology and Geothermal Research, v. 193, no. 3-4, p. 203-214, https://doi.org/10.1016/j.jvolgeores.2010.03.015.","productDescription":"12 p.","startPage":"203","endPage":"214","costCenters":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"links":[{"id":356049,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Redoubt Volcano","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -155.19287109375,\n              59.52317553544798\n            ],\n            [\n              -149.139404296875,\n              59.52317553544798\n            ],\n            [\n              -149.139404296875,\n              62.04213770379758\n            ],\n            [\n              -155.19287109375,\n              62.04213770379758\n            ],\n            [\n              -155.19287109375,\n              59.52317553544798\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"193","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5b98b760e4b0702d0e844e27","contributors":{"authors":[{"text":"Schiff, C.J.","contributorId":34735,"corporation":false,"usgs":true,"family":"Schiff","given":"C.J.","email":"","affiliations":[],"preferred":false,"id":741022,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kaufman, Darrell S. 0000-0002-7572-1414","orcid":"https://orcid.org/0000-0002-7572-1414","contributorId":28308,"corporation":false,"usgs":true,"family":"Kaufman","given":"Darrell","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":741023,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wallace, Kristi L. 0000-0002-0962-048X kwallace@usgs.gov","orcid":"https://orcid.org/0000-0002-0962-048X","contributorId":3454,"corporation":false,"usgs":true,"family":"Wallace","given":"Kristi","email":"kwallace@usgs.gov","middleInitial":"L.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":741024,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ketterer, Michael E.","contributorId":28479,"corporation":false,"usgs":true,"family":"Ketterer","given":"Michael","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":741025,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":5224963,"text":"5224963 - 2010 - Uncovering a latent multinomial: Analysis of mark–recapture data with misidentification","interactions":[],"lastModifiedDate":"2021-02-23T12:40:04.048926","indexId":"5224963","displayToPublicDate":"2010-06-16T12:18:37","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1039,"text":"Biometrics","active":true,"publicationSubtype":{"id":10}},"title":"Uncovering a latent multinomial: Analysis of mark–recapture data with misidentification","docAbstract":"Natural tags based on DNA fingerprints or natural features of animals are now becoming very widely used in wildlife population biology.  However, classic capture-recapture models do not allow for misidentification of animals which is a potentially very serious problem with natural tags.  Statistical analysis of misidentification processes is extremely difficult using traditional likelihood methods but is easily handled using Bayesian methods.  We present a general framework for Bayesian analysis of categorical data arising from a latent multinomial distribution.  Although our work is motivated by a specific model for misidentification in closed population capture-recapture analyses, with crucial assumptions which may not always be appropriate, the methods we develop extend naturally to a variety of other models with similar structure.  Suppose that observed frequencies f are a known linear transformation f=A'x of a latent multinomial variable x with cell probability vector pi= pi(theta).  Given that full conditional distributions [theta | x] can be sampled, implementation of Gibbs sampling requires only that we can sample from the full conditional distribution [x | f, theta], which is made possible by knowledge of the null space of A'.  We illustrate the approach using two data sets with individual misidentification, one simulated, the other summarizing recapture data for salamanders based on natural marks.","language":"English","publisher":"Wiley","doi":"10.1111/j.1541-0420.2009.01244.x","usgsCitation":"Link, W., Yoshizaki, J., Bailey, L., and Pollock, K.H., 2010, Uncovering a latent multinomial: Analysis of mark–recapture data with misidentification: Biometrics, v. 66, no. 1, p. 178-185, https://doi.org/10.1111/j.1541-0420.2009.01244.x.","productDescription":"8 p.","startPage":"178","endPage":"185","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":475711,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1111/j.1541-0420.2009.01244.x","text":"Publisher Index Page"},{"id":383404,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"66","issue":"1","noUsgsAuthors":false,"publicationDate":"2010-03-17","publicationStatus":"PW","scienceBaseUri":"4f4e4a26e4b07f02db60f621","contributors":{"authors":[{"text":"Link, W.A. 0000-0002-9913-0256","orcid":"https://orcid.org/0000-0002-9913-0256","contributorId":8815,"corporation":false,"usgs":true,"family":"Link","given":"W.A.","affiliations":[],"preferred":false,"id":343306,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Yoshizaki, J.","contributorId":79596,"corporation":false,"usgs":true,"family":"Yoshizaki","given":"J.","email":"","affiliations":[],"preferred":false,"id":343309,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bailey, L.L. 0000-0002-5959-2018","orcid":"https://orcid.org/0000-0002-5959-2018","contributorId":61006,"corporation":false,"usgs":true,"family":"Bailey","given":"L.L.","affiliations":[],"preferred":false,"id":343307,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Pollock, K. H.","contributorId":65184,"corporation":false,"usgs":false,"family":"Pollock","given":"K.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":343308,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70189940,"text":"70189940 - 2010 - Microbial oxidation of arsenite in a subarctic environment: diversity of arsenite oxidase genes and identification of a psychrotolerant arsenite oxidiser","interactions":[],"lastModifiedDate":"2018-10-10T16:41:36","indexId":"70189940","displayToPublicDate":"2010-06-16T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5472,"text":"BMC Microbiology","active":true,"publicationSubtype":{"id":10}},"title":"Microbial oxidation of arsenite in a subarctic environment: diversity of arsenite oxidase genes and identification of a psychrotolerant arsenite oxidiser","docAbstract":"<p>Arsenic is toxic to most living cells. The two soluble inorganic forms of arsenic are arsenite (+3) and arsenate (+5), with arsenite the more toxic. Prokaryotic metabolism of arsenic has been reported in both thermal and moderate environments and has been shown to be involved in the redox cycling of arsenic. No arsenic metabolism (either dissimilatory arsenate reduction or arsenite oxidation) has ever been reported in cold environments (i.e. &lt; 10°C).</p><p><strong>Results</strong>: Our study site is located 512 kilometres south of the Arctic Circle in the Northwest Territories, Canada in an inactive gold mine which contains mine waste water in excess of 50 mM arsenic. Several thousand tonnes of arsenic trioxide dust are stored in underground chambers and microbial biofilms grow on the chamber walls below seepage points rich in arsenite-containing solutions. We compared the arsenite oxidisers in two subsamples (which differed in arsenite concentration) collected from one biofilm. 'Species' (sequence) richness did not differ between subsamples, but the relative importance of the three identifiable clades did. An arsenite-oxidising bacterium (designated GM1) was isolated, and was shown to oxidise arsenite in the early exponential growth phase and to grow at a broad range of temperatures (4-25°C). Its arsenite oxidase was constitutively expressed and functioned over a broad temperature range.</p><p><strong>Conclusions</strong>: The diversity of arsenite oxidisers does not significantly differ from two subsamples of a microbial biofilm that vary in arsenite concentrations. GM1 is the first psychrotolerant arsenite oxidiser to be isolated with the ability to grow below 10°C. This ability to grow at low temperatures could be harnessed for arsenic bioremediation in moderate to cold climates.</p>","language":"English","publisher":"BioMed Central","doi":"10.1186/1471-2180-10-205","usgsCitation":"Osborne, T.H., Jamieson, H.E., Hudson-Edwards, K.A., Nordstrom, D.K., Walker, S.R., Ward, S.A., and Santini, J.M., 2010, Microbial oxidation of arsenite in a subarctic environment: diversity of arsenite oxidase genes and identification of a psychrotolerant arsenite oxidiser: BMC Microbiology, v. 10, no. 205, 8 p., https://doi.org/10.1186/1471-2180-10-205.","productDescription":"8 p.","ipdsId":"IP-017174","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true},{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"links":[{"id":475714,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1186/1471-2180-10-205","text":"Publisher Index Page"},{"id":344480,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"10","issue":"205","publishingServiceCenter":{"id":2,"text":"Denver PSC"},"noUsgsAuthors":false,"publicationDate":"2010-07-30","publicationStatus":"PW","scienceBaseUri":"59819317e4b0e2f5d463b7b3","contributors":{"authors":[{"text":"Osborne, Thomas H.","contributorId":195346,"corporation":false,"usgs":false,"family":"Osborne","given":"Thomas","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":706834,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jamieson, Heather E.","contributorId":150176,"corporation":false,"usgs":false,"family":"Jamieson","given":"Heather","email":"","middleInitial":"E.","affiliations":[{"id":7029,"text":"Queen's University, Kingston, Ontario, Canada","active":true,"usgs":false}],"preferred":false,"id":706830,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hudson-Edwards, Karen A.","contributorId":195345,"corporation":false,"usgs":false,"family":"Hudson-Edwards","given":"Karen","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":706832,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Nordstrom, D. Kirk 0000-0003-3283-5136 dkn@usgs.gov","orcid":"https://orcid.org/0000-0003-3283-5136","contributorId":749,"corporation":false,"usgs":true,"family":"Nordstrom","given":"D.","email":"dkn@usgs.gov","middleInitial":"Kirk","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":false,"id":706828,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Walker, Stephen R.","contributorId":195350,"corporation":false,"usgs":false,"family":"Walker","given":"Stephen","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":706833,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Ward, Seamus A.","contributorId":168896,"corporation":false,"usgs":false,"family":"Ward","given":"Seamus","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":706829,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Santini, Joanne M.","contributorId":168895,"corporation":false,"usgs":false,"family":"Santini","given":"Joanne","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":706831,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70189024,"text":"70189024 - 2010 - Mineralogy and stratigraphy of phyllosilicate-bearing and dark mantling units in the greater Mawrth Vallis/west Arabia Terra area: Constraints on geological origin","interactions":[],"lastModifiedDate":"2017-06-29T14:16:25","indexId":"70189024","displayToPublicDate":"2010-06-15T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2312,"text":"Journal of Geophysical Research","active":true,"publicationSubtype":{"id":10}},"title":"Mineralogy and stratigraphy of phyllosilicate-bearing and dark mantling units in the greater Mawrth Vallis/west Arabia Terra area: Constraints on geological origin","docAbstract":"<p><span>Analyses of MRO/CRISM images of the greater Mawrth Vallis region of Mars affirm the presence of two primary phyllosilicate assemblages throughout a region ∼1000 × 1000 km. These two units consist of an Fe/Mg-phyllosilicate assemblage overlain by an Al-phyllosilicate and hydrated silica assemblage. The lower unit contains Fe/Mg-smectites, sometimes combined with one or more of these other Fe/Mg-phyllosilicates: serpentine, chlorite, biotite, and/or vermiculite. It is more than 100 m thick and finely layered at meter scales. The upper unit includes Al-smectite, kaolin group minerals, and hydrated silica. It is tens of meters thick and finely layered as well. A common phyllosilicate stratigraphy and morphology is observed throughout the greater region wherever erosional windows are present. This suggests that the geologic processes forming these units must have occurred on at least a regional scale. Sinuous ridges (interpreted to be inverted channels) and narrow channels cut into the upper clay-bearing unit suggesting that aqueous processes were prevalent after, and possibly during, the deposition of the layered units. We propose that layered units may have been deposited at Mawrth Vallis and then subsequently altered to form the hydrated units. The Fe/Mg-phyllosilicate assemblage is consistent with hydrothermal alteration or pedogenesis of mafic to ultramafic rocks. The Al-phyllosilicate/hydrated silica unit may have formed through alteration of felsic material or via leaching of basaltic material through pedogenic alteration or a mildly acidic environment. These phyllosilicate-bearing units are overlain by a darker, relatively unaltered, and indurated material that has probably experienced a complex geological history.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/2009JE003351","usgsCitation":"Noe Dobrea, E., Bishop, J., McKeown, N., Fu, R., Rossi, C., Michalski, J., Heinlein, C., Hanus, V., Poulet, F., Mustard, R., Murchie, S., McEwen, A.S., Swayze, G., Bibring, J., Malaret, E., and Hash, C., 2010, Mineralogy and stratigraphy of phyllosilicate-bearing and dark mantling units in the greater Mawrth Vallis/west Arabia Terra area: Constraints on geological origin: Journal of Geophysical Research, v. 115, no. E7, Article E00D19: 27 p., https://doi.org/10.1029/2009JE003351.","productDescription":"Article E00D19: 27 p.","ipdsId":"IP-019901","costCenters":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"links":[{"id":343143,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Mars","volume":"115","issue":"E7","publishingServiceCenter":{"id":2,"text":"Denver PSC"},"noUsgsAuthors":false,"publicationDate":"2010-07-31","publicationStatus":"PW","scienceBaseUri":"595611c8e4b0d1f9f05067f4","contributors":{"authors":[{"text":"Noe Dobrea, E.Z.","contributorId":97316,"corporation":false,"usgs":true,"family":"Noe Dobrea","given":"E.Z.","email":"","affiliations":[],"preferred":false,"id":702463,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bishop, J.L.","contributorId":83244,"corporation":false,"usgs":true,"family":"Bishop","given":"J.L.","affiliations":[],"preferred":false,"id":702464,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McKeown, N.K.","contributorId":10529,"corporation":false,"usgs":true,"family":"McKeown","given":"N.K.","email":"","affiliations":[],"preferred":false,"id":702465,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Fu, R.","contributorId":193928,"corporation":false,"usgs":false,"family":"Fu","given":"R.","email":"","affiliations":[],"preferred":false,"id":702630,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Rossi, C.M.","contributorId":193929,"corporation":false,"usgs":false,"family":"Rossi","given":"C.M.","email":"","affiliations":[],"preferred":false,"id":702631,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Michalski, J.R.","contributorId":46202,"corporation":false,"usgs":true,"family":"Michalski","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":702632,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Heinlein, C.","contributorId":193930,"corporation":false,"usgs":false,"family":"Heinlein","given":"C.","email":"","affiliations":[],"preferred":false,"id":702633,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Hanus, V.","contributorId":193931,"corporation":false,"usgs":false,"family":"Hanus","given":"V.","email":"","affiliations":[],"preferred":false,"id":702634,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Poulet, F.","contributorId":61551,"corporation":false,"usgs":true,"family":"Poulet","given":"F.","email":"","affiliations":[],"preferred":false,"id":702725,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Mustard, R.J.F.","contributorId":193932,"corporation":false,"usgs":false,"family":"Mustard","given":"R.J.F.","email":"","affiliations":[],"preferred":false,"id":702726,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Murchie, S.","contributorId":16584,"corporation":false,"usgs":true,"family":"Murchie","given":"S.","email":"","affiliations":[],"preferred":false,"id":702727,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"McEwen, A. S.","contributorId":11317,"corporation":false,"usgs":true,"family":"McEwen","given":"A.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":702728,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Swayze, G. 0000-0002-1814-7823","orcid":"https://orcid.org/0000-0002-1814-7823","contributorId":55131,"corporation":false,"usgs":true,"family":"Swayze","given":"G.","affiliations":[],"preferred":false,"id":702729,"contributorType":{"id":1,"text":"Authors"},"rank":13},{"text":"Bibring, J.-P.","contributorId":86083,"corporation":false,"usgs":true,"family":"Bibring","given":"J.-P.","email":"","affiliations":[],"preferred":false,"id":702733,"contributorType":{"id":1,"text":"Authors"},"rank":14},{"text":"Malaret, E.","contributorId":84487,"corporation":false,"usgs":true,"family":"Malaret","given":"E.","email":"","affiliations":[],"preferred":false,"id":702734,"contributorType":{"id":1,"text":"Authors"},"rank":15},{"text":"Hash, C.","contributorId":59927,"corporation":false,"usgs":true,"family":"Hash","given":"C.","email":"","affiliations":[],"preferred":false,"id":702735,"contributorType":{"id":1,"text":"Authors"},"rank":16}]}}
,{"id":98440,"text":"ofr20101117 - 2010 - Environmental Assessment for a Marine Geophysical Survey of Parts of the Arctic Ocean, August-September 2010","interactions":[],"lastModifiedDate":"2012-02-10T00:11:52","indexId":"ofr20101117","displayToPublicDate":"2010-06-10T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2010-1117","title":"Environmental Assessment for a Marine Geophysical Survey of Parts of the Arctic Ocean, August-September 2010","docAbstract":"According to the United Nations Convention on the Law of the Sea (UNCLOS), individual nations? sovereign rights extend to 200 nautical miles (n.mi.) (370 km) offshore or to a maritime boundary in an area called the continental shelf. These rights include jurisdiction over all resources in the water column and on and beneath the seabed. Article 76 of UNCLOS also establishes the criteria to determine areas beyond the 200 n.mi. (370 km) limit that could be defined as ?extended continental shelf,? where a nation could extend its sovereign rights over the seafloor and sub-seafloor (As used in UNCLOS, ?continental shelf? refers to a legally defined region of the sea floor rather than a morphological shallow-water area adjacent to continents commonly used by geologists and hydrographers.). This jurisdiction provided in Article 76 includes resources on and below the seafloor but not in the water column. The United States has been acquiring data to determine the outer limits of its extended continental shelf in the Arctic and has a vested interest in declaring and receiving international recognition of the reach of its extended continental shelf. \r\n\r\nThe U.S. collaborated with Canada in 2008 and 2009 on extended continental shelf studies in the Arctic Ocean. The U.S. Coast Guard (USCG) Cutter Healy worked with the Canadian Coast Guard ship Louis S. St. Laurent to map the continental shelf beyond 200 n.mi. (370 km) in the Arctic. Each icebreaking vessel contributed different capabilities in order to collect data needed by both nations more efficiently in order to save money, avoid redundancy, and foster cooperation. Generally, the Healy collects bathymetric (sea-floor topography) data and the Louis S. St. Laurent collects seismic reflection profile data. The vessels work in concert when ice conditions are heavy, with one vessel breaking ice for the ship collecting data. The Canadian Environmental Assessments for these projects are available on line at http://www.ceaa.gc.ca/052/details-eng.cfm?pid=38185 (2008) and http://www.ceaa.gc.ca/052/details-eng.cfm?pid=46518 (2009). \r\n\r\nThe U.S. Geological Survey (USGS) and Geological Survey of Canada (GSC) are undertaking a similar partnership again for 2010 in a limited area of U.S. waters during the period between ~10 and 16 August. The survey vessels will then proceed to international or Canadian waters where surveying will proceed until ~3 September, when the two icebreakers will separate to conduct independent work. The survey area of the joint work will be bounded approximately by 145? to 158? W longitude and 71? to 84? N latitude in water depths ranging from ~2,000 to 4,000 m (fig. 1). Ice conditions are expected to range from open water to 10/10 ice cover. The Louis S. St. Laurent will join accompanying vessel Healy in or near the survey area around 10 August to begin the joint survey work. \r\n\r\nAs its energy source, the seismic system aboard Louis S. St. Laurent will employ a 3-airgun array consisting of three Sercel G-airguns. Two guns will have a discharge volume of 500 in3 and the third a discharge volume of 150 in3 for a total array discharge volume of 1,150 in3. The seismic survey will take place in water depths 2,000?4,000 m. This airgun array is identical to the system used in the 2008 and 2009 field programs by the Geological Survey of Canada. \r\n\r\nThe USGS requested that the National Marine Fisheries Service (NMFS) issue an Incidental Harassment Authorization (IHA) to authorize the incidental, that is, not intentional, harassment of small numbers of cetaceans and seals should this occur during the seismic survey in U.S. waters. USGS is also consulting with the U.S. Fish and Wildlife Service (USFWS) regarding concerns about disturbance to walruses and polar bears. Through informal consultation with the Office of Protected Resources with the National Oceanic and Atmospheric Administration (NOAA), USGS proposes that no ESA-listed marine species?bowhead, fin, humpback or sperm whale?w","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20101117","usgsCitation":"Haley, B., Ireland, D., and Childs, J.R., 2010, Environmental Assessment for a Marine Geophysical Survey of Parts of the Arctic Ocean, August-September 2010: U.S. Geological Survey Open-File Report 2010-1117, x, 111 p.; Appendices; Finding of No Significant Impact File, https://doi.org/10.3133/ofr20101117.","productDescription":"x, 111 p.; Appendices; Finding of No Significant Impact File","onlineOnly":"Y","additionalOnlineFiles":"Y","costCenters":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":125569,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr_2010_1117.jpg"},{"id":13705,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2010/1117/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -160,71 ], [ -160,78 ], [ -144,78 ], [ -144,71 ], [ -160,71 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db6025c7","contributors":{"authors":[{"text":"Haley, Beth","contributorId":44258,"corporation":false,"usgs":true,"family":"Haley","given":"Beth","email":"","affiliations":[],"preferred":false,"id":305309,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ireland, Darren","contributorId":50244,"corporation":false,"usgs":true,"family":"Ireland","given":"Darren","email":"","affiliations":[],"preferred":false,"id":305310,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Childs, Jonathan R. jchilds@usgs.gov","contributorId":3155,"corporation":false,"usgs":true,"family":"Childs","given":"Jonathan","email":"jchilds@usgs.gov","middleInitial":"R.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":305308,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70243664,"text":"70243664 - 2010 - A snapshot of climate variability at Tahiti ~ 9 ka using a fossil coral from IODP Expedition 310","interactions":[],"lastModifiedDate":"2023-05-16T18:11:42.934275","indexId":"70243664","displayToPublicDate":"2010-06-08T13:02:31","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1757,"text":"Geochemistry, Geophysics, Geosystems","active":true,"publicationSubtype":{"id":10}},"title":"A snapshot of climate variability at Tahiti ~ 9 ka using a fossil coral from IODP Expedition 310","docAbstract":"<p><span>The Integrated Ocean Drilling Program (IODP) Expedition 310 recovered drill cores from the drowned reefs around the island of Tahiti (17°40′S, 149°30′W), many of which contained samples of massive corals from the genus&nbsp;</span><i>Porites</i><span>. Herein we report on one well-preserved fossil coral sample: a 13.6 cm long&nbsp;</span><i>Porites</i><span>&nbsp;sp. dated by uranium series techniques at 9523 ± 33 years. Monthly&nbsp;</span><i>δ</i><sup>18</sup><span>O and Sr/Ca determinations reveal nine clear and robust annual cycles. Coral&nbsp;</span><i>δ</i><sup>18</sup><span>O and Sr/Ca determinations estimate a mean temperature of ∼24.3°C (∼3.2°C colder than modern) for Tahiti at 9.5 ka; however, this estimate is viewed with caution since potential sources of cold bias in coral geochemistry remain to be resolved. The interannual variability in coral&nbsp;</span><i>δ</i><sup>18</sup><span>O is similar between the 9.5 ka coral record and a modern record from nearby Moorea. The seasonal cycle in coral Sr/Ca is approximately the same or greater in the 9.5 ka coral record than in modern coral records from Tahiti. Paired analysis of coral&nbsp;</span><i>δ</i><sup>18</sup><span>O and Sr/Ca indicates cold/wet (warm/dry) interannual anomalies, opposite from those observed in the modern instrumental record.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/2009GC002758","usgsCitation":"DeLong, K.L., Quinn, T., Shen, C., and Lin, K., 2010, A snapshot of climate variability at Tahiti ~ 9 ka using a fossil coral from IODP Expedition 310: Geochemistry, Geophysics, Geosystems, v. 11, no. 6, Q06005, 14 p., https://doi.org/10.1029/2009GC002758.","productDescription":"Q06005, 14 p.","ipdsId":"IP-014561","costCenters":[{"id":574,"text":"St. Petersburg Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":417103,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Tahiti","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -149.97340625761515,\n              -17.37818620895858\n            ],\n            [\n              -149.97340625761515,\n              -17.956825850324933\n            ],\n            [\n              -149.0404249716099,\n              -17.956825850324933\n            ],\n            [\n              -149.0404249716099,\n              -17.37818620895858\n            ],\n            [\n              -149.97340625761515,\n              -17.37818620895858\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"11","issue":"6","noUsgsAuthors":false,"publicationDate":"2010-06-08","publicationStatus":"PW","contributors":{"authors":[{"text":"DeLong, Kristine L","contributorId":305465,"corporation":false,"usgs":true,"family":"DeLong","given":"Kristine","email":"","middleInitial":"L","affiliations":[],"preferred":true,"id":872848,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Quinn, Terrence M.","contributorId":305466,"corporation":false,"usgs":false,"family":"Quinn","given":"Terrence M.","affiliations":[{"id":13603,"text":"University of Texas, Austin","active":true,"usgs":false}],"preferred":false,"id":872849,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Shen, Chuan-Chou","contributorId":305467,"corporation":false,"usgs":false,"family":"Shen","given":"Chuan-Chou","affiliations":[{"id":30216,"text":"National Taiwan University","active":true,"usgs":false}],"preferred":false,"id":872850,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lin, Ke","contributorId":305468,"corporation":false,"usgs":false,"family":"Lin","given":"Ke","affiliations":[{"id":30216,"text":"National Taiwan University","active":true,"usgs":false}],"preferred":false,"id":872851,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70236352,"text":"70236352 - 2010 - Upper mantle rheology from GRACE and GPS postseismic deformation after the 2004 Sumatra-Andaman earthquake","interactions":[],"lastModifiedDate":"2022-09-02T17:43:28.635127","indexId":"70236352","displayToPublicDate":"2010-06-01T11:58:51","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1757,"text":"Geochemistry, Geophysics, Geosystems","active":true,"publicationSubtype":{"id":10}},"title":"Upper mantle rheology from GRACE and GPS postseismic deformation after the 2004 Sumatra-Andaman earthquake","docAbstract":"<div class=\"article-section__content en main\"><p>Mantle rheology is one of the essential, yet least understood, material properties of our planet, controlling the dynamic processes inside the Earth's mantle and the Earth's response to various forces. With the advent of GRACE satellite gravity, measurements of mass displacements associated with many processes are now available. In the case of mass displacements related to postseismic deformation, these data may provide new constraints on the mantle rheology. We consider the postseismic deformation due to the<span>&nbsp;</span><i>M</i><sub><i>w</i></sub><span>&nbsp;</span>= 9.2 Sumatra 26 December 2004 and<span>&nbsp;</span><i>M</i><sub><i>w</i></sub><span>&nbsp;</span>= 8.7 Nias 28 March 2005 earthquakes. Applying wavelet analyses to enhance those local signals in the GRACE time varying geoids up to September 2007, we detect a clear postseismic gravity signal. We supplement these gravity variations with GPS measurements of postseismic crustal displacements to constrain postseismic relaxation processes throughout the upper mantle. The observed GPS displacements and gravity variations are well explained by a model of viscoelastic relaxation plus a small amount of afterslip at the downdip extension of the coseismically ruptured fault planes. Our model uses a 60 km thick elastic layer above a viscoelastic asthenosphere with Burgers body rheology. The mantle below depth 220 km has a Maxwell rheology. Assuming a low transient viscosity in the 60–220 km depth range, the GRACE data are best explained by a constant steady state viscosity throughout the ductile portion of the upper mantle (e.g., 60–660 km). This suggests that the localization of relatively low viscosity in the asthenosphere is chiefly in the transient viscosity rather than the steady state viscosity. We find a 8.10<sup>18</sup><span>&nbsp;</span>Pa s mantle viscosity in the 220–660 km depth range. This may indicate a transient response of the upper mantle to the high amount of stress released by the earthquakes. To fit the remaining misfit to the GRACE data, larger at the smaller spatial scales, cumulative afterslip of about 75 cm at depth should be added over the period spanned by the GRACE models. It produces only small crustal displacements. Our results confirm that satellite gravity data are an essential complement to ground geodetic and geophysical networks in order to understand the seismic cycle and the Earth's inner structure.</p></div>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/2009GC002905","usgsCitation":"Panet, I., Pollitz, F., Mikhailov, V., Diament, M., Banerjee, P., and Grijalva, K., 2010, Upper mantle rheology from GRACE and GPS postseismic deformation after the 2004 Sumatra-Andaman earthquake: Geochemistry, Geophysics, Geosystems, v. 11, no. 6, Q06008, 20 p., https://doi.org/10.1029/2009GC002905.","productDescription":"Q06008, 20 p.","costCenters":[],"links":[{"id":475717,"rank":0,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://insu.hal.science/insu-01356011","text":"External Repository"},{"id":406158,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Indonesia","otherGeospatial":"Andaman Sea, Sumatra","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              97.84423828125,\n              -0.06591795420830737\n            ],\n            [\n              99.07470703125,\n              0.7031073524364909\n            ],\n            [\n              98.7451171875,\n              1.845383988573187\n            ],\n            [\n              97.8662109375,\n              2.5040852618529215\n            ],\n            [\n              97.71240234375,\n              3.030812122664383\n            ],\n            [\n              96.85546875,\n              3.9519408561575946\n            ],\n            [\n              95.38330078125,\n              5.156598738411155\n            ],\n            [\n              94.15283203125,\n              7.27529233637217\n            ],\n            [\n              92.8125,\n              9.925565912405506\n            ],\n            [\n              93.27392578125,\n              13.7313809749427\n            ],\n            [\n              92.46093749999999,\n              13.987376214146467\n            ],\n            [\n              91.93359375,\n              14.00869637063467\n            ],\n            [\n              91.49414062499999,\n              10.595820834654047\n            ],\n            [\n              93.2958984375,\n              6.075011000682009\n            ],\n            [\n              95.625,\n              2.701635047944533\n            ],\n            [\n              96.6357421875,\n              1.691648704756987\n            ],\n            [\n              97.84423828125,\n              -0.06591795420830737\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"11","issue":"6","noUsgsAuthors":false,"publicationDate":"2010-06-19","publicationStatus":"PW","contributors":{"authors":[{"text":"Panet, I.","contributorId":103862,"corporation":false,"usgs":true,"family":"Panet","given":"I.","email":"","affiliations":[],"preferred":false,"id":850724,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pollitz, Frederick 0000-0002-4060-2706 fpollitz@usgs.gov","orcid":"https://orcid.org/0000-0002-4060-2706","contributorId":139578,"corporation":false,"usgs":true,"family":"Pollitz","given":"Frederick","email":"fpollitz@usgs.gov","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":850725,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mikhailov, V.","contributorId":37953,"corporation":false,"usgs":true,"family":"Mikhailov","given":"V.","affiliations":[],"preferred":false,"id":850726,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Diament, M.","contributorId":90104,"corporation":false,"usgs":true,"family":"Diament","given":"M.","affiliations":[],"preferred":false,"id":850727,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Banerjee, P.","contributorId":90525,"corporation":false,"usgs":true,"family":"Banerjee","given":"P.","email":"","affiliations":[],"preferred":false,"id":850728,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Grijalva, K.","contributorId":72204,"corporation":false,"usgs":true,"family":"Grijalva","given":"K.","email":"","affiliations":[],"preferred":false,"id":850729,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70189349,"text":"70189349 - 2010 - Source and fate of inorganic solutes in the Gibbon River, Yellowstone National Park, Wyoming, USA: I. Low-flow discharge and major solute chemistry","interactions":[],"lastModifiedDate":"2018-10-10T13:17:22","indexId":"70189349","displayToPublicDate":"2010-06-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2499,"text":"Journal of Volcanology and Geothermal Research","active":true,"publicationSubtype":{"id":10}},"title":"Source and fate of inorganic solutes in the Gibbon River, Yellowstone National Park, Wyoming, USA: I. Low-flow discharge and major solute chemistry","docAbstract":"<p><span>The Gibbon River in Yellowstone National Park (YNP) is an important natural resource and habitat for fisheries and wildlife. However, the Gibbon River differs from most other mountain rivers because its chemistry is affected by several geothermal sources including Norris Geyser Basin, Chocolate Pots, Gibbon Geyser Basin, Beryl Spring, and Terrace Spring. Norris Geyser Basin is one of the most dynamic geothermal areas in YNP, and the water discharging from Norris is much more acidic (pH 3) than other geothermal basins in the upper-Madison drainage (Gibbon and Firehole Rivers). Water samples and discharge data were obtained from the Gibbon River and its major tributaries near Norris Geyser Basin under the low-flow conditions of September 2006. Surface inflows from Norris Geyser Basin were sampled to identify point sources and to quantify solute loading to the Gibbon River. The source and fate of the major solutes (Ca, Mg, Na, K, SiO</span><sub>2</sub><span>, Cl, F, HCO</span><sub>3</sub><span>, SO</span><sub>4</sub><span>, NO</span><sub>3</sub><span>, and NH</span><sub>4</sub><span>) in the Gibbon River were determined in this study and these results may provide an important link in understanding the health of the ecosystem and the behavior of many trace solutes. Norris Geyser Basin is the primary source of Na, K, Cl, SO</span><sub>4</sub><span>, and N loads (35–58%) in the Gibbon River. The largest source of HCO</span><sub>3</sub><span><span>&nbsp;</span>and F is in the lower Gibbon River reach. Most of the Ca and Mg originate in the Gibbon River upstream from Norris Geyser Basin. All the major solutes behave conservatively except for NH</span><sub>4</sub><span>, which decreased substantially downstream from Gibbon Geyser Basin, and SiO</span><sub>2</sub><span>, small amounts of which precipitated on mixing of thermal drainage with the river. As much as 9–14% of the river discharge at the gage is from thermal flows during this period.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.jvolgeores.2010.03.014","usgsCitation":"McCleskey, R.B., Nordstrom, D.K., Susong, D.D., Ball, J.W., and Holloway, J.M., 2010, Source and fate of inorganic solutes in the Gibbon River, Yellowstone National Park, Wyoming, USA: I. Low-flow discharge and major solute chemistry: Journal of Volcanology and Geothermal Research, v. 193, no. 34-4, p. 189-202, https://doi.org/10.1016/j.jvolgeores.2010.03.014.","productDescription":"14 p.","startPage":"189","endPage":"202","ipdsId":"IP-016033","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true},{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"links":[{"id":343607,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Wyoming","otherGeospatial":"Yellowstone National Park","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -110.89324951171875,\n              44.6334823448553\n            ],\n            [\n              -110.65292358398438,\n              44.6334823448553\n            ],\n            [\n              -110.65292358398438,\n              44.75356026127114\n            ],\n            [\n              -110.89324951171875,\n              44.75356026127114\n            ],\n            [\n              -110.89324951171875,\n              44.6334823448553\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"193","issue":"34-4","publishingServiceCenter":{"id":2,"text":"Denver PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5965bff1e4b0d1f9f05b392d","contributors":{"authors":[{"text":"McCleskey, R. Blaine 0000-0002-2521-8052 rbmccles@usgs.gov","orcid":"https://orcid.org/0000-0002-2521-8052","contributorId":147399,"corporation":false,"usgs":true,"family":"McCleskey","given":"R.","email":"rbmccles@usgs.gov","middleInitial":"Blaine","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true},{"id":503,"text":"Office of Water Quality","active":true,"usgs":true},{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":704320,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nordstrom, D. Kirk 0000-0003-3283-5136 dkn@usgs.gov","orcid":"https://orcid.org/0000-0003-3283-5136","contributorId":749,"corporation":false,"usgs":true,"family":"Nordstrom","given":"D.","email":"dkn@usgs.gov","middleInitial":"Kirk","affiliations":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true},{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":false,"id":704318,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Susong, David D. ddsusong@usgs.gov","contributorId":1040,"corporation":false,"usgs":true,"family":"Susong","given":"David","email":"ddsusong@usgs.gov","middleInitial":"D.","affiliations":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"preferred":true,"id":704317,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ball, James W.","contributorId":38946,"corporation":false,"usgs":true,"family":"Ball","given":"James","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":704319,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Holloway, JoAnn M. 0000-0003-3603-7668 jholloway@usgs.gov","orcid":"https://orcid.org/0000-0003-3603-7668","contributorId":918,"corporation":false,"usgs":true,"family":"Holloway","given":"JoAnn","email":"jholloway@usgs.gov","middleInitial":"M.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":704321,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70138811,"text":"70138811 - 2010 - A comparison of methods for estimating open-water evaporation in small wetlands","interactions":[],"lastModifiedDate":"2018-10-10T10:25:27","indexId":"70138811","displayToPublicDate":"2010-06-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3750,"text":"Wetlands","onlineIssn":"1943-6246","printIssn":"0277-5212","active":true,"publicationSubtype":{"id":10}},"title":"A comparison of methods for estimating open-water evaporation in small wetlands","docAbstract":"<p><span>We compared evaporation measurements from a floating pan, land pan, chamber, and the Priestley-Taylor (PT) equation. Floating pan, land pan, and meteorological data were collected from June 6 to July 21, 2005, at a small wetland in the Canadian River alluvium in central Oklahoma, USA. Evaporation measured with the floating pan compared favorably to 12&nbsp;h chamber measurements. Differences between chamber and floating pan rates ranged from &minus;0.2 to 0.3&nbsp;mm, mean of 0.1&nbsp;mm. The difference between chamber and land pan rates ranged from 0.8 to 2.0&nbsp;mm, mean of 1.5&nbsp;mm. The mean chamber-to-floating pan ratio was 0.97 and the mean chamber-to-land pan ratio was 0.73. The chamber-to-floating pan ratio of 0.97 indicates the use of a floating pan to measure evaporation in small limited-fetch water bodies is an appropriate and accurate method for the site investigated. One-sided Paired t-Tests indicate daily floating pan rates were significantly less than land pan and PT rates. A two-sided Paired t-Test indicated there was no significant difference between land pan and PT values. The PT equation tends to overestimate evaporation during times when the air is of low drying power and tends to underestimate as drying power increases.</span></p>","language":"English","publisher":"Springer","doi":"10.1007/s13157-010-0041-y","usgsCitation":"Masoner, J.R., and Stannard, D.I., 2010, A comparison of methods for estimating open-water evaporation in small wetlands: Wetlands, v. 30, no. 3, p. 513-524, https://doi.org/10.1007/s13157-010-0041-y.","productDescription":"12 p.","startPage":"513","endPage":"524","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-013356","costCenters":[{"id":516,"text":"Oklahoma Water Science Center","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":297518,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Oklahoma","otherGeospatial":"Canadian River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -102.919921875,\n              37.020098201368114\n            ],\n            [\n              -94.2626953125,\n              36.914764288955936\n            ],\n            [\n              -94.4384765625,\n              33.43144133557529\n            ],\n            [\n              -100.107421875,\n              34.415973384481866\n            ],\n            [\n              -102.919921875,\n              37.020098201368114\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"30","issue":"3","publishingServiceCenter":{"id":5,"text":"Lafayette PSC"},"noUsgsAuthors":false,"publicationDate":"2010-05-19","publicationStatus":"PW","scienceBaseUri":"54dd2b17e4b08de9379b3235","contributors":{"authors":[{"text":"Masoner, Jason R. 0000-0002-4829-6379 jmasoner@usgs.gov","orcid":"https://orcid.org/0000-0002-4829-6379","contributorId":3193,"corporation":false,"usgs":true,"family":"Masoner","given":"Jason","email":"jmasoner@usgs.gov","middleInitial":"R.","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true},{"id":516,"text":"Oklahoma Water Science Center","active":true,"usgs":true}],"preferred":true,"id":538919,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stannard, David I. distanna@usgs.gov","contributorId":562,"corporation":false,"usgs":true,"family":"Stannard","given":"David","email":"distanna@usgs.gov","middleInitial":"I.","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":false,"id":538918,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70175137,"text":"70175137 - 2010 - Taqman Real-Time PCR Detects <i>Avipoxvirus</i> DNA in Blood of Hawaìi `Amakihi (<i>Hemignathus virens</i>)","interactions":[],"lastModifiedDate":"2018-01-04T12:54:20","indexId":"70175137","displayToPublicDate":"2010-05-27T14:30:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2980,"text":"PLoS ONE","active":true,"publicationSubtype":{"id":10}},"title":"Taqman Real-Time PCR Detects <i>Avipoxvirus</i> DNA in Blood of Hawaìi `Amakihi (<i>Hemignathus virens</i>)","docAbstract":"<h3>Background</h3>\n<p><i>Avipoxvirus</i>&nbsp;sp. is a significant threat to endemic bird populations on several groups of islands worldwide, including Hawa&igrave;i, the Galapagos Islands, and the Canary Islands. Accurate identification and genotyping of&nbsp;<i>Avipoxvirus</i>&nbsp;is critical to the study of this disease and how it interacts with other pathogens, but currently available methods rely on invasive sampling of pox-like lesions and may be especially harmful in smaller birds.</p>\n<h3>Methodology/Principal Findings</h3>\n<p>Here, we present a nested TaqMan Real-Time PCR for the detection of the&nbsp;<i>Avipoxvirus</i>&nbsp;4b core protein gene in archived blood samples from Hawaiian birds. The method was successful in amplifying&nbsp;<i>Avipoxvirus</i>&nbsp;DNA from packed blood cells of one of seven Hawaiian honeycreepers with confirmed&nbsp;<i>Avipoxvirus</i>&nbsp;infections and 13 of 28 Hawa&igrave;i `amakihi (<i>Hemignathus virens</i>) with suspected&nbsp;<i>Avipoxvirus</i>&nbsp;infections based on the presence of pox-like lesions. Mixed genotype infections have not previously been documented in Hawa&igrave;i but were observed in two individuals in this study.</p>\n<h3>Conclusions/Significance</h3>\n<p>We anticipate that this method will be applicable to other closely related strains of&nbsp;<i>Avipoxvirus&nbsp;</i>and will become an important and useful tool in global studies of the epidemiology of&nbsp;<i>Avipoxvirus</i>.</p>","language":"English","publisher":"PLoS","doi":"10.1371/journal.pone.0010745","usgsCitation":"Farias, M.E., LaPointe, D., Atkinson, C.T., Czerwonka, C., Shrestha, R., and Jarvi, S.I., 2010, Taqman Real-Time PCR Detects <i>Avipoxvirus</i> DNA in Blood of Hawaìi `Amakihi (<i>Hemignathus virens</i>): PLoS ONE, v. 5, no. 5, p. 1-6, https://doi.org/10.1371/journal.pone.0010745.","productDescription":"6 p.","startPage":"1","endPage":"6","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-017575","costCenters":[{"id":521,"text":"Pacific Island Ecosystems Research Center","active":false,"usgs":true}],"links":[{"id":475721,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1371/journal.pone.0010745","text":"Publisher Index Page"},{"id":325858,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Ecuador, Spain, United States","state":"Hawaii","otherGeospatial":"Canary Islands, Galapagos Islands","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -154.51171875,\n              19.766703551716976\n            ],\n            [\n              -156.29150390625,\n              21.53484700204879\n            ],\n            [\n              -157.8955078125,\n              22.248428704383624\n            ],\n            [\n              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Center","active":true,"usgs":true}],"preferred":false,"id":644075,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Atkinson, C. T.","contributorId":24296,"corporation":false,"usgs":true,"family":"Atkinson","given":"C.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":644076,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Czerwonka, Christopher","contributorId":173284,"corporation":false,"usgs":false,"family":"Czerwonka","given":"Christopher","email":"","affiliations":[],"preferred":false,"id":644077,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Shrestha, Rajesh","contributorId":173288,"corporation":false,"usgs":false,"family":"Shrestha","given":"Rajesh","email":"","affiliations":[],"preferred":false,"id":644078,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Jarvi, Susan I.","contributorId":47748,"corporation":false,"usgs":true,"family":"Jarvi","given":"Susan","email":"","middleInitial":"I.","affiliations":[],"preferred":false,"id":644079,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70210253,"text":"70210253 - 2010 - Comparative analysis of Mourning Dove population change in North America","interactions":[],"lastModifiedDate":"2020-05-27T12:11:47.772599","indexId":"70210253","displayToPublicDate":"2010-05-26T14:00:55","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2508,"text":"Journal of Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"Comparative analysis of Mourning Dove population change in North America","docAbstract":"<p>Mourning doves (Zenaida macroura) are surveyed in North America with a Call-Count Survey (CCS) and the North American Breeding Bird Survey (BBS). Analyses in recent years have identified inconsistencies in results between surveys, and a need exists to analyze the surveys using modern methods and examine possible causes of differences in survey results. Call-Count Survey observers collect separate information on number of doves heard and number of doves seen during counting, whereas BBS observers record one index containing all doves observed. We used hierarchical log-linear models to estimate trend and annual indices of abundance for 1966–2007 from BBS data, CCS-heard data, and CCS-seen data. Trend estimates from analyses provided inconsistent results for several states and for eastern and central dovemanagement units. We examined differential effects of change in land use and noise-related disturbance on the CCS indices. Changes in noiserelated disturbance along CCS routes had a larger influence on the heard index than on the seen index, but association analyses among states of changes in temperature and of amounts of developed land suggest that CCS indices are differentially influenced by changes in these environmental features. Our hierarchical model should be used to estimate population change from dove surveys, because it provides an efficient framework for estimating population trends from dove indices while controlling for environmental features that differentially influence the indices.</p>","language":"English","publisher":"BioOne","doi":"10.2193/2008-459","usgsCitation":"Sauer, J.R., Link, W.A., Kendall, W.L., and Dolton, D., 2010, Comparative analysis of Mourning Dove population change in North America: Journal of Wildlife Management, v. 74, no. 5, p. 1059-1069, https://doi.org/10.2193/2008-459.","productDescription":"11 p.","startPage":"1059","endPage":"1069","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":375039,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"74","issue":"5","noUsgsAuthors":false,"publicationDate":"2010-12-13","publicationStatus":"PW","contributors":{"authors":[{"text":"Sauer, John R. 0000-0002-4557-3019 jrsauer@usgs.gov","orcid":"https://orcid.org/0000-0002-4557-3019","contributorId":146917,"corporation":false,"usgs":true,"family":"Sauer","given":"John","email":"jrsauer@usgs.gov","middleInitial":"R.","affiliations":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"preferred":true,"id":789767,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Link, William A. 0000-0002-9913-0256 wlink@usgs.gov","orcid":"https://orcid.org/0000-0002-9913-0256","contributorId":146920,"corporation":false,"usgs":true,"family":"Link","given":"William","email":"wlink@usgs.gov","middleInitial":"A.","affiliations":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"preferred":true,"id":789768,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kendall, William L. 0000-0003-0084-9891","orcid":"https://orcid.org/0000-0003-0084-9891","contributorId":204844,"corporation":false,"usgs":true,"family":"Kendall","given":"William","email":"","middleInitial":"L.","affiliations":[{"id":200,"text":"Coop Res Unit Seattle","active":true,"usgs":true}],"preferred":true,"id":789769,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Dolton, David D.","contributorId":100452,"corporation":false,"usgs":true,"family":"Dolton","given":"David D.","affiliations":[],"preferred":false,"id":789770,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70209949,"text":"70209949 - 2010 - Ecosystem development in the Girdwood area, south-central Alaska, following late Wisconsin glaciation","interactions":[],"lastModifiedDate":"2020-05-06T19:29:31.664539","indexId":"70209949","displayToPublicDate":"2010-05-06T14:19:18","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1168,"text":"Canadian Journal of Earth Sciences","active":true,"publicationSubtype":{"id":10}},"title":"Ecosystem development in the Girdwood area, south-central Alaska, following late Wisconsin glaciation","docAbstract":"<p><span>Pollen analysis of two cores with discontinuous records from a peat bog near Girdwood, in south-central Alaska, provides the basis for reconstructing the first radiocarbon-dated outline of postglacial history of vegetation in the upper Turnagain Arm area of Cook Inlet. Pollen data from clayey silt underlying peat at one site indicate that the earliest known vegetation in the Girdwood area was shrub–herb tundra. Tundra vegetation developed by ∼13 800 cal years BP, soon after local retreat of glacial ice from the maximum position of the Elmendorf glacial advance (∼15 000 – 11 000 cal years BP). By ∼10 900 cal years BP, the tundra vegetation became shrubbier as&nbsp;</span>Betula nana<span>,&nbsp;</span>Salix<span>, and Ericales increased, and scattered&nbsp;</span>Alnus<span>&nbsp;shrubs began to colonize Turnagain Arm. By ∼9600 cal years BP,&nbsp;</span>Alnus<span>&nbsp;thickets with Polypodiaceae ferns became the dominant vegetation. By ∼6600 cal years BP, birch trees (</span>Betula neoalaskana<span>,&nbsp;</span>B. kenaica<span>) from the Anchorage and Kenai lowlands began to spread eastward into eastern Turnagain Arm. Mountain hemlock (</span>Tsuga mertensiana<span>) began to colonize the Girdwood area by ∼3400 cal years BP, followed soon after by Sitka spruce (</span>Picea sitchensis<span>), both Pacific coastal forest species that spread westward from Prince William Sound after a long migration from southeastern Alaska. For at least the past 2700 cal years, Pacific coastal forest composed mostly of&nbsp;</span>Tsuga mertensiana<span>,&nbsp;</span>Picea sitchensis<span>, and&nbsp;</span>Alnus<span>&nbsp;has been the dominant vegetation of eastern Turnagain Arm.</span></p>","language":"English","publisher":"Canadian Science Publishing","doi":"10.1139/E10-020","usgsCitation":"Ager, T.A., Carrara, P.E., and McGeehin, J., 2010, Ecosystem development in the Girdwood area, south-central Alaska, following late Wisconsin glaciation: Canadian Journal of Earth Sciences, v. 47, no. 7, p. 971-985, https://doi.org/10.1139/E10-020.","productDescription":"15 p.","startPage":"971","endPage":"985","costCenters":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"links":[{"id":374502,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Girdwood south-central Alaska","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -152.0068359375,\n              60.457217797743944\n            ],\n            [\n              -148.0517578125,\n              60.457217797743944\n            ],\n            [\n              -148.0517578125,\n              61.85614879566797\n            ],\n            [\n              -152.0068359375,\n              61.85614879566797\n            ],\n            [\n              -152.0068359375,\n              60.457217797743944\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"47","issue":"7","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Ager, T. A.","contributorId":88386,"corporation":false,"usgs":true,"family":"Ager","given":"T.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":788604,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Carrara, Paul E. pcarrara@usgs.gov","contributorId":1342,"corporation":false,"usgs":true,"family":"Carrara","given":"Paul","email":"pcarrara@usgs.gov","middleInitial":"E.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":788605,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McGeehin, John mcgeehin@usgs.gov","contributorId":167455,"corporation":false,"usgs":true,"family":"McGeehin","given":"John","email":"mcgeehin@usgs.gov","affiliations":[{"id":242,"text":"Eastern Geographic Science Center","active":true,"usgs":true},{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"preferred":true,"id":788606,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70209932,"text":"70209932 - 2010 - Geologic history of Mars","interactions":[],"lastModifiedDate":"2022-09-08T17:35:33.348795","indexId":"70209932","displayToPublicDate":"2010-05-06T11:54:47","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1427,"text":"Earth and Planetary Science Letters","active":true,"publicationSubtype":{"id":10}},"title":"Geologic history of Mars","docAbstract":"<p><span>Mars accumulated and differentiated into crust, mantle and core within a few tens of millions of years of Solar System formation. Formation of Hellas, which has been adopted as the base of the Noachian period, is estimated to have occurred around 4.1 to 3.8&nbsp;Gyr ago, depending on whether or not the planet experienced a late cataclysm. Little is known of the pre-Noachian period except that it was characterized by a magnetic field, subject to numerous large basin-forming impacts, probably including one that formed the global dichotomy. The Noachian period, which ended around 3.7&nbsp;Gyr ago, was characterized by high rates of cratering, erosion, and valley formation. Most of Tharsis formed and surface conditions were at least episodically such as to cause widespread production of hydrous weathering products such as phyllosilicates. Extensive sulfate deposits accumulated late in the era. Average erosion rates, though high compared with later epochs, fell short of the lowest average terrestrial rates. The record suggests that warm, wet conditions necessary for fluvial activity were met only occasionally, such as might occur if caused by large impacts or volcanic eruptions. At the end of the Noachian, rates of impact, valley formation, weathering, and erosion all dropped precipitously but volcanism continued at a relatively high average rate throughout the Hesperian, resulting in the resurfacing of at least 30% of the planet. Large water floods formed episodically, possibly leaving behind large bodies of water. The canyons formed. The observations suggest the change at the end of the Noachian suppressed most aqueous activity at the surface other than large floods, and resulted in growth of a thick cryosphere. However, presence of discrete sulfate rich deposits, sulfate concentrations in soils, and occasional presence of Hesperian valley networks indicates that water activity did not decline to zero. After the end of the Hesperian around 3&nbsp;Gyr ago the pace of geologic activity slowed further. The average rate of volcanism during the Amazonian was approximately a factor of ten lower than in the Hesperian and activity was confined largely to Tharsis and Elysium. The main era of water flooding was over, although small floods occurred episodically until geologically recent times. Canyon development was largely restricted to formation of large landslides. Erosion and weathering rates remained extremely low. The most distinctive characteristic of the Amazonian is formation of features that have been attributed to the presence, accumulation, and movement of ice. Included are the polar layered deposits, glacial deposits on volcanoes, ice-rich veneers at high latitudes, and a variety of landforms in the 30–55° latitude belts, including lobate debris aprons, lineated valley fill and concentric crater fill. Most of the gullies on steep slopes also formed late in this era. The rate of formation of the ice-related features and the gullies probably varied as changes in obliquity affected the ice stability relations.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.epsl.2009.06.042","usgsCitation":"Carr, M.H., and Head, J.W., 2010, Geologic history of Mars: Earth and Planetary Science Letters, v. 294, no. 3-4, p. 185-203, https://doi.org/10.1016/j.epsl.2009.06.042.","productDescription":"19 p.","startPage":"185","endPage":"203","costCenters":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"links":[{"id":374491,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Mars","volume":"294","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Carr, Michael H.","contributorId":61894,"corporation":false,"usgs":true,"family":"Carr","given":"Michael","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":788588,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Head, James W. III","contributorId":102954,"corporation":false,"usgs":true,"family":"Head","given":"James","suffix":"III","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":851240,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":98359,"text":"sir20105023 - 2010 - Water Quality in the Equus Beds Aquifer and the Little Arkansas River Before Implementation of Large-Scale Artificial Recharge, South-Central Kansas, 1995-2005","interactions":[],"lastModifiedDate":"2012-03-08T17:16:29","indexId":"sir20105023","displayToPublicDate":"2010-05-05T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2010-5023","title":"Water Quality in the Equus Beds Aquifer and the Little Arkansas River Before Implementation of Large-Scale Artificial Recharge, South-Central Kansas, 1995-2005","docAbstract":"Artificial recharge of the Equus Beds aquifer using runoff from the Little Arkansas River in south-central Kansas was first proposed in 1956 and was one of many options considered by the city of Wichita to preserve its water supply. Declining aquifer water levels of as much as 50 feet exacerbated concerns about future water availability and enhanced migration of saltwater into the aquifer from past oil and gas activities near Burrton and from the Arkansas River. Because Wichita changed water-management strategies and decreased pumping from the Equus Beds aquifer in 1992, water storage in the aquifer recovered by about 50 percent. This recovery is the result of increased reliance on Cheney Reservoir for Wichita water supply, decreased aquifer pumping, and larger than normal precipitation. Accompanying the water-level recovery, the average water-level gradient in the aquifer decreased from about 12 feet per mile in 1992 to about 8 feet per mile in January 2006.\r\n\r\nAn important component of artificial recharge is the water quality of the receiving aquifer and the water being recharged (source water). Water quality within the Little Arkansas River was defined using data from two real-time surface-water-quality sites and discrete samples. Water quality in the Equus Beds aquifer was defined using sample analyses collected at 38 index sites, each with a well completed in the shallow and deep parts of the Equus Beds aquifer. In addition, data were collected at diversion well sites, recharge sites, background wells, and prototype wells for the aquifer storage and recovery project. Samples were analyzed for major ions, nutrients, trace metals, radionuclides, organic compounds, and bacterial and viral indicators.\r\n\r\nWater-quality constituents of concern for artificial recharge are those constituents that frequently (more than 5 percent of samples) may exceed Federal [U.S. Environmental Protection Agency (USEPA)] and State drinking-water criteria in water samples from the receiving aquifer or in samples from the source water. Constituents of concern include major ions (sulfate and chloride), nutrients (nitrite plus nitrate), trace elements (arsenic, iron, and manganese), organic compounds (atrazine), and fecal bacterial indicators. This report describes the water quality in the Equus Beds aquifer and the Little Arkansas River from 1995 through 2005 before implementation of large-scale recharge activities.\r\n\r\nSulfate concentrations in water samples from the Little Arkansas River rarely exceeded Federal secondary drinking water regulation (SDWR) of 250 milligrams per liter (mg/L). Sulfate concentrations in groundwater were exceeded in about 18 percent of the wells in the shallow (less than or equal to 80 feet deep) parts of the aquifer and in about 13 percent of the wells in the deep parts the aquifer. Larger sulfate concentrations were associated with parts of the aquifer with the largest water-level declines. Water-quality changes in the Equus Beds aquifer likely were caused by dewatering and oxidation of aquifer material that subsequently resulted in increased sulfate concentrations as water levels recovered.\r\n\r\nThe primary sources of chloride to the Equus Beds aquifer are from past oil and gas activities near Burrton and from the Arkansas River. Computed chloride concentrations in the Little Arkansas River near Halstead exceeded the Federal SDWR of 250 mg/L about 27 percent of the time (primarily during low-flow conditions). Chloride concentrations in groundwater exceeded 250 mg/L in about 8 percent or less of the study area, primarily near Burrton and along the Arkansas River. Chloride in groundwater near Burrton has migrated downgradient about 3 miles during the past 40 to 45 years. The downward and horizontal migration of the chloride is controlled by the hydraulic gradient in the aquifer, dispersion of chloride, and discontinuous clay layers that can inhibit further downward migration. Chloride in the shallow parts of the Equus Beds","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/sir20105023","collaboration":"Prepared in cooperation with the City of Wichita, Kansas, as part of the Equus Beds Groundwater Recharge Project","usgsCitation":"Ziegler, A., Hansen, C.V., and Finn, D.A., 2010, Water Quality in the Equus Beds Aquifer and the Little Arkansas River Before Implementation of Large-Scale Artificial Recharge, South-Central Kansas, 1995-2005: U.S. Geological Survey Scientific Investigations Report 2010-5023, Report: vii, 143 p. ; oversized figure (PDF), https://doi.org/10.3133/sir20105023.","productDescription":"Report: vii, 143 p. ; oversized figure (PDF)","onlineOnly":"N","additionalOnlineFiles":"Y","temporalStart":"1995-01-01","temporalEnd":"2005-12-31","costCenters":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"links":[{"id":118645,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/sir_2010_5023.jpg"},{"id":13607,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2010/5023/","linkFileType":{"id":5,"text":"html"}}],"projection":"Universal Transverse Mercator","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -97.83333333333333,37.666666666666664 ], [ -97.83333333333333,38.333333333333336 ], [ -97.33333333333333,38.333333333333336 ], [ -97.33333333333333,37.666666666666664 ], [ -97.83333333333333,37.666666666666664 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0de4b07f02db5fd397","contributors":{"authors":[{"text":"Ziegler, Andrew C. aziegler@usgs.gov","contributorId":433,"corporation":false,"usgs":true,"family":"Ziegler","given":"Andrew C.","email":"aziegler@usgs.gov","affiliations":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"preferred":false,"id":305071,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hansen, Cristi V. chansen@usgs.gov","contributorId":435,"corporation":false,"usgs":true,"family":"Hansen","given":"Cristi","email":"chansen@usgs.gov","middleInitial":"V.","affiliations":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"preferred":false,"id":305072,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Finn, Daniel A.","contributorId":86064,"corporation":false,"usgs":true,"family":"Finn","given":"Daniel","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":305073,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
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