{"pageNumber":"1960","pageRowStart":"48975","pageSize":"25","recordCount":184617,"records":[{"id":70034291,"text":"70034291 - 2010 - Current lineages of the epithelioma papulosum cyprini (EPC) cell line are contaminated with fathead minnow, Pimephales promelas, cells","interactions":[],"lastModifiedDate":"2016-12-27T14:19:27","indexId":"70034291","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2286,"text":"Journal of Fish Diseases","active":true,"publicationSubtype":{"id":10}},"title":"Current lineages of the epithelioma papulosum cyprini (EPC) cell line are contaminated with fathead minnow, Pimephales promelas, cells","docAbstract":"Initially established from proliferative skin lesions of the common carp, Cyprinus carpio L., the epithelioma papulosum cyprini (EPC) cell line (Fijan, Sulimanovic, Bearzotti, Muzinic, Zwillenberg, Chilmonczyk, Vautherot & de Kinkelin 1983) has become one of the most widely used tools for research on fish viruses and the diagnosis of fish viral diseases.","language":"English","publisher":"Wiley","doi":"10.1111/j.1365-2761.2010.01165.x","issn":"01407775","usgsCitation":"Winton, J., Batts, W., DeKinkelin, P., LeBerre, M., Bremont, M., and Fijan, N., 2010, Current lineages of the epithelioma papulosum cyprini (EPC) cell line are contaminated with fathead minnow, Pimephales promelas, cells: Journal of Fish Diseases, v. 33, no. 8, p. 701-704, https://doi.org/10.1111/j.1365-2761.2010.01165.x.","productDescription":"4 p.","startPage":"701","endPage":"704","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":244653,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"33","issue":"8","noUsgsAuthors":false,"publicationDate":"2010-07-06","publicationStatus":"PW","scienceBaseUri":"5059fd10e4b0c8380cd4e5fa","contributors":{"authors":[{"text":"Winton, J.","contributorId":55627,"corporation":false,"usgs":true,"family":"Winton","given":"J.","email":"","affiliations":[],"preferred":false,"id":445110,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Batts, W.","contributorId":76533,"corporation":false,"usgs":true,"family":"Batts","given":"W.","email":"","affiliations":[],"preferred":false,"id":445112,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"DeKinkelin, P.","contributorId":82948,"corporation":false,"usgs":true,"family":"DeKinkelin","given":"P.","email":"","affiliations":[],"preferred":false,"id":445113,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"LeBerre, M.","contributorId":31604,"corporation":false,"usgs":true,"family":"LeBerre","given":"M.","email":"","affiliations":[],"preferred":false,"id":445109,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Bremont, M.","contributorId":30349,"corporation":false,"usgs":false,"family":"Bremont","given":"M.","affiliations":[],"preferred":false,"id":445108,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Fijan, N.","contributorId":67333,"corporation":false,"usgs":true,"family":"Fijan","given":"N.","email":"","affiliations":[],"preferred":false,"id":445111,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70034217,"text":"70034217 - 2010 - Emplacement of the youngest flood lava on Mars: A short, turbulent story","interactions":[],"lastModifiedDate":"2018-12-05T08:28:15","indexId":"70034217","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1963,"text":"Icarus","active":true,"publicationSubtype":{"id":10}},"title":"Emplacement of the youngest flood lava on Mars: A short, turbulent story","docAbstract":"<p style=\"text-align: justify;\" data-mce-style=\"text-align: justify;\">Recently acquired data from the High Resolution Imaging Science Experiment (HiRISE), Context (CTX) imager, and Compact Reconnaissance Imaging Spectrometer for Mars (CRISM) onboard the Mars Reconnaissance Orbiter (MRO) spacecraft were used to investigate the emplacement of the youngest flood-lava flow on Mars. Careful mapping finds that the Athabasca Valles flood lava is the product of a single eruption, and it covers 250,000 km<sup>2</sup> of western Elysium Planitia with an estimated 5000-7500 km<sup>3</sup> of mafic or ultramafic lava. Calculations utilizing topographic data enhanced with MRO observations to refine the dimensions of the channel system show that this flood lava was emplaced turbulently over a period of only a few to several weeks. This is the first well-documented example of a turbulently emplaced flood lava anywhere in the Solar System. However, MRO data suggest that this same process may have operated in a number of martian channel systems. The magnitude and dynamics of these lava floods are similar to the aqueous floods that are generally believed to have eroded the channels, raising the intriguing possibility that mechanical erosion by lava could have played a role in their incision.</p>","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Icarus","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","doi":"10.1016/j.icarus.2009.09.011","issn":"00191035","usgsCitation":"Jaeger, W.L., Keszthelyi, L., Skinner, J., Milazzo, M.P., McEwen, A.S., Titus, T.N., Rosiek, M.R., Galuszka, D.M., Howington-Kraus, E., Kirk, R.L., and the HiRISE TEam, 2010, Emplacement of the youngest flood lava on Mars: A short, turbulent story: Icarus, v. 205, no. 1, p. 230-243, https://doi.org/10.1016/j.icarus.2009.09.011.","productDescription":"14 p.","startPage":"230","endPage":"243","numberOfPages":"14","costCenters":[{"id":131,"text":"Astrogeology Science 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,{"id":70033784,"text":"70033784 - 2010 - Lunar Reconnaissance Orbiter Camera (LROC) instrument overview","interactions":[],"lastModifiedDate":"2012-12-18T10:57:20","indexId":"70033784","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3454,"text":"Space Science Reviews","active":true,"publicationSubtype":{"id":10}},"title":"Lunar Reconnaissance Orbiter Camera (LROC) instrument overview","docAbstract":"The Lunar Reconnaissance Orbiter Camera (LROC) Wide Angle Camera (WAC) and Narrow Angle Cameras (NACs) are on the NASA Lunar Reconnaissance Orbiter (LRO). The WAC is a 7-color push-frame camera (100 and 400 m/pixel visible and UV, respectively), while the two NACs are monochrome narrow-angle linescan imagers (0.5 m/pixel). The primary mission of LRO is to obtain measurements of the Moon that will enable future lunar human exploration. The overarching goals of the LROC investigation include landing site identification and certification, mapping of permanently polar shadowed and sunlit regions, meter-scale mapping of polar regions, global multispectral imaging, a global morphology base map, characterization of regolith properties, and determination of current impact hazards.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Space Science Reviews","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Springer","publisherLocation":"Amsterdam, Netherlands","doi":"10.1007/s11214-010-9634-2","issn":"00386308","usgsCitation":"Robinson, M., Brylow, S., Tschimmel, M., Humm, D., Lawrence, S., Thomas, P., Denevi, B., Bowman-Cisneros, E., Zerr, J., Ravine, M., Caplinger, M., Ghaemi, F., Schaffner, J., Malin, M.C., Mahanti, P., Bartels, A., Anderson, J., Tran, T., Eliason, E.M., McEwen, A.S., Turtle, E., Jolliff, B., and Hiesinger, H., 2010, Lunar Reconnaissance Orbiter Camera (LROC) instrument overview: Space Science Reviews, v. 150, no. 1-4, p. 81-124, https://doi.org/10.1007/s11214-010-9634-2.","productDescription":"44 p.","startPage":"81","endPage":"124","costCenters":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"links":[{"id":214499,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/s11214-010-9634-2"},{"id":242232,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"150","issue":"1-4","noUsgsAuthors":false,"publicationDate":"2010-03-11","publicationStatus":"PW","scienceBaseUri":"505a4a96e4b0c8380cd68ea5","contributors":{"authors":[{"text":"Robinson, M.S.","contributorId":34934,"corporation":false,"usgs":true,"family":"Robinson","given":"M.S.","email":"","affiliations":[],"preferred":false,"id":442445,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brylow, S.M.","contributorId":72605,"corporation":false,"usgs":true,"family":"Brylow","given":"S.M.","email":"","affiliations":[],"preferred":false,"id":442455,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Tschimmel, M.","contributorId":52412,"corporation":false,"usgs":true,"family":"Tschimmel","given":"M.","email":"","affiliations":[],"preferred":false,"id":442448,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Humm, D.","contributorId":28346,"corporation":false,"usgs":true,"family":"Humm","given":"D.","email":"","affiliations":[],"preferred":false,"id":442441,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Lawrence, S.J.","contributorId":67922,"corporation":false,"usgs":true,"family":"Lawrence","given":"S.J.","email":"","affiliations":[],"preferred":false,"id":442452,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Thomas, P.C.","contributorId":32690,"corporation":false,"usgs":true,"family":"Thomas","given":"P.C.","affiliations":[],"preferred":false,"id":442444,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Denevi, B.W.","contributorId":20559,"corporation":false,"usgs":true,"family":"Denevi","given":"B.W.","affiliations":[],"preferred":false,"id":442439,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Bowman-Cisneros, E.","contributorId":30466,"corporation":false,"usgs":true,"family":"Bowman-Cisneros","given":"E.","email":"","affiliations":[],"preferred":false,"id":442443,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Zerr, J.","contributorId":94118,"corporation":false,"usgs":true,"family":"Zerr","given":"J.","email":"","affiliations":[],"preferred":false,"id":442458,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Ravine, M.A.","contributorId":91312,"corporation":false,"usgs":true,"family":"Ravine","given":"M.A.","affiliations":[],"preferred":false,"id":442456,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Caplinger, M.A.","contributorId":7878,"corporation":false,"usgs":true,"family":"Caplinger","given":"M.A.","affiliations":[],"preferred":false,"id":442437,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Ghaemi, F.T.","contributorId":37972,"corporation":false,"usgs":true,"family":"Ghaemi","given":"F.T.","email":"","affiliations":[],"preferred":false,"id":442446,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Schaffner, J.A.","contributorId":57284,"corporation":false,"usgs":true,"family":"Schaffner","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":442449,"contributorType":{"id":1,"text":"Authors"},"rank":13},{"text":"Malin, M. 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,{"id":70034423,"text":"70034423 - 2010 - Conserving migratory land birds in the New World: Do we know enough?","interactions":[],"lastModifiedDate":"2012-03-12T17:21:47","indexId":"70034423","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1450,"text":"Ecological Applications","active":true,"publicationSubtype":{"id":10}},"title":"Conserving migratory land birds in the New World: Do we know enough?","docAbstract":"Migratory bird needs must be met during four phases of the year: breeding season, fall migration, wintering, and spring migration; thus, management may be needed during all four phases. The bulk of research and management has focused on the breeding season, although several issues remain unsettled, including the spatial extent of habitat influences on fitness and the importance of habitat on the breeding grounds used after breeding. Although detailed investigations have shed light on the ecology and population dynamics of a few avian species, knowledge is sketchy for most species. Replication of comprehensive studies is needed for multiple species across a range of areas. Information deficiencies are even greater during the wintering season, when birds require sites that provide security and food resources needed for survival and developing nutrient reserves for spring migration and, possibly, reproduction. Research is needed on many species simply to identify geographic distributions, wintering sites, habitat use, and basic ecology. Studies are complicated, however, by the mobility of birds and by sexual segregation during winter. Stable-isotope methodology has offered an opportunity to identify linkages between breeding and wintering sites, which facilitates understanding the complete annual cycle of birds. The twice-annual migrations are the poorest-understood events in a bird's life. Migration has always been a risky undertaking, with such anthropogenic features as tall buildings, towers, and wind generators adding to the risk, Species such as woodland specialists migrating through eastern North America have numerous options for pausing during migration to replenish nutrients, but some species depend on limited stopover locations. Research needs for migration include identifying pathways and timetables of migration, quality and distribution of habitats, threats posed by towers and other tall structures, and any bottlenecks for migration. Issues such as human population growth, acid deposition, climate change, and exotic diseases are global concerns with uncertain consequences to migratory birds and even lesscertain remedies. Despite enormous gaps in our understanding of these birds, research, much of it occurring in the past 30 years, has provided sufficient information to make intelligent conservation efforts but needs to expand to handle future challenges. ?? 2010 by the Ecological Society of America.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Ecological Applications","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1890/09-0397.1","issn":"10510761","usgsCitation":"Faaborg, J., Holmes, R.T., Anders, A., Bildstein, K., Dugger, K., Gauthreaux, S., Heglund, P., Hobson, K., Jahn, A., Johnson, D.H., Latta, S., Levey, D., Marra, P., Merkord, C., Nol, E., Rothstein, S., Sherry, T., Scott, S.T., Thompson, F.R., and Warnock, N., 2010, Conserving migratory land birds in the New World: Do we know enough?: Ecological Applications, v. 20, no. 2, p. 398-418, https://doi.org/10.1890/09-0397.1.","startPage":"398","endPage":"418","numberOfPages":"21","costCenters":[],"links":[{"id":244789,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":216891,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1890/09-0397.1"}],"volume":"20","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f9f8e4b0c8380cd4d854","contributors":{"authors":[{"text":"Faaborg, John","contributorId":32871,"corporation":false,"usgs":true,"family":"Faaborg","given":"John","email":"","affiliations":[],"preferred":false,"id":445704,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Holmes, Richard T.","contributorId":45269,"corporation":false,"usgs":true,"family":"Holmes","given":"Richard","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":445706,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Anders, A.D.","contributorId":28100,"corporation":false,"usgs":true,"family":"Anders","given":"A.D.","email":"","affiliations":[],"preferred":false,"id":445702,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bildstein, K.L.","contributorId":90836,"corporation":false,"usgs":true,"family":"Bildstein","given":"K.L.","affiliations":[],"preferred":false,"id":445714,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Dugger, K.M.","contributorId":25729,"corporation":false,"usgs":true,"family":"Dugger","given":"K.M.","email":"","affiliations":[],"preferred":false,"id":445701,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Gauthreaux, S.A. 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R. III","contributorId":17940,"corporation":false,"usgs":true,"family":"Thompson","given":"F.","suffix":"III","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":445698,"contributorType":{"id":1,"text":"Authors"},"rank":19},{"text":"Warnock, N.","contributorId":80615,"corporation":false,"usgs":true,"family":"Warnock","given":"N.","email":"","affiliations":[],"preferred":false,"id":445712,"contributorType":{"id":1,"text":"Authors"},"rank":20}]}}
,{"id":70034638,"text":"70034638 - 2010 - Occurrence of the Great Lake's most recent invader, <i>Hemimysis anomala</i>, in the diet of fishes in southeastern Lake Ontario","interactions":[],"lastModifiedDate":"2013-02-28T13:39:08","indexId":"70034638","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2330,"text":"Journal of Great Lakes Research","active":true,"publicationSubtype":{"id":10}},"title":"Occurrence of the Great Lake's most recent invader, <i>Hemimysis anomala</i>, in the diet of fishes in southeastern Lake Ontario","docAbstract":"The Ponto-Caspian mysid, <i>Hemimysis anomala</i>, was first observed in southeastern Lake Ontario in May 2006. During July and August 2007, gill nets were fished in 6 to 8 m of water at two locations of known <i>Hemimysis</i> colonization in southeastern Lake Ontario to determine if fish that consume macroinvertebrates were beginning to include this new invasive mysid in their diets. Of nine fish species captured in August, September, and October 2007, three species had consumed <i>Hemimysis</i>: alewife (<i>Alosa pseudoharengus</i>), rock bass (<i>Ambloplites rupestris</i>), and yellow perch (<i>Perca flavescens</i>); and six species had not: round goby <i>Apollonia melanostoma</i>, smallmouth bass <i>Micropterus dolomieu</i>, spottail shiner <i>Notropis hudsonius</i>, gizzard shad <i>Dorosoma cepedianum</i>, white perch <i>Morone americana</i> and log perch <i>Percina caprodes</i>. Diets of alewives from all samples were composed predominantly of <i>Hemimysis</i> (69.6% -100% frequency of occurrence, 46.0%–74.5% dry weight diet composition). Two of 6 rock bass stomachs sampled in August contained ≥ 98.9% <i>Hemimysis</i> (10 and 40 individuals each) and one of 61 yellow perch stomachs sampled in September contained 10.0% <i>Hemimysis</i> (6 individuals) and 90.0% fish. While <i>Hemimysis</i> were observed only sparsely in the diet of most nearshore fish, their predominance in alewife diets and their omnivorous feeding behavior indicated that they have the potential to alter energy flow in Great Lakes' foodwebs.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Great Lakes Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","publisherLocation":"Amsterdam, Netherlands","doi":"10.1016/j.jglr.2009.12.002","issn":"03801330","usgsCitation":"Lantry, B., Walsh, M.G., Johnson, J.H., and McKenna, J., 2010, Occurrence of the Great Lake's most recent invader, <i>Hemimysis anomala</i>, in the diet of fishes in southeastern Lake Ontario: Journal of Great Lakes Research, v. 36, no. 1, p. 179-183, https://doi.org/10.1016/j.jglr.2009.12.002.","productDescription":"5 p.","startPage":"179","endPage":"183","costCenters":[{"id":357,"text":"Lake Ontario Biological Station","active":false,"usgs":true}],"links":[{"id":215779,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.jglr.2009.12.002"},{"id":243604,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Lake Ontario","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -80.1391,43.073 ], [ -80.1391,44.2705 ], [ -75.9829,44.2705 ], [ -75.9829,43.073 ], [ -80.1391,43.073 ] ] ] } } ] }","volume":"36","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a6c39e4b0c8380cd74afe","contributors":{"authors":[{"text":"Lantry, B.F.","contributorId":19105,"corporation":false,"usgs":true,"family":"Lantry","given":"B.F.","email":"","affiliations":[],"preferred":false,"id":446812,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Walsh, M. G.","contributorId":72172,"corporation":false,"usgs":true,"family":"Walsh","given":"M.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":446814,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Johnson, J. H.","contributorId":54914,"corporation":false,"usgs":true,"family":"Johnson","given":"J.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":446813,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"McKenna, J.E. Jr.","contributorId":106065,"corporation":false,"usgs":true,"family":"McKenna","given":"J.E.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":446815,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70033783,"text":"70033783 - 2010 - The ShakeOut earthquake scenario: Verification of three simulation sets","interactions":[],"lastModifiedDate":"2012-03-12T17:21:34","indexId":"70033783","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1803,"text":"Geophysical Journal International","active":true,"publicationSubtype":{"id":10}},"title":"The ShakeOut earthquake scenario: Verification of three simulation sets","docAbstract":"This paper presents a verification of three simulations of the ShakeOut scenario, an M<sub>w</sub> 7.8 earthquake on a portion of the San Andreas fault in southern California, conducted by three different groups at the Southern California Earthquake Center using the SCEC Community Velocity Model for this region. We conducted two simulations using the finite difference method, and one by the finite element method, and performed qualitative and quantitative comparisons between the corresponding results. The results are in good agreement with each other; only small differences occur both in amplitude and phase between the various synthetics at ten observation points located near and away from the fault-as far as 150 km away from the fault. Using an available goodness-of-fit criterion all the comparisons scored above 8, with most above 9.2. This score would be regarded as excellent if the measurements were between recorded and synthetic seismograms. We also report results of comparisons based on time-frequency misfit criteria. Results from these two criteria can be used for calibrating the two methods for comparing seismograms. In those cases in which noticeable discrepancies occurred between the seismograms generated by the three groups, we found that they were the product of inherent characteristics of the various numerical methods used and their implementations. In particular, we found that the major source of discrepancy lies in the difference between mesh and grid representations of the same material model. Overall, however, even the largest differences in the synthetic seismograms are small. Thus, given the complexity of the simulations used in this verification, it appears that the three schemes are consistent, reliable and sufficiently accurate and robust for use in future large-scale simulations. ?? 2009 The Authors Journal compilation ?? 2009 RAS.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Geophysical Journal International","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1111/j.1365-246X.2009.04417.x","issn":"0956540X","usgsCitation":"Bielak, J., Graves, R., Olsen, K., Taborda, R., Ramirez-Guzman, L., Day, S., Ely, G., Roten, D., Jordan, T., Maechling, P., Urbanic, J., Cui, Y., and Juve, G., 2010, The ShakeOut earthquake scenario: Verification of three simulation sets: Geophysical Journal International, v. 180, no. 1, p. 375-404, https://doi.org/10.1111/j.1365-246X.2009.04417.x.","startPage":"375","endPage":"404","numberOfPages":"30","costCenters":[],"links":[{"id":487725,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1111/j.1365-246x.2009.04417.x","text":"Publisher Index Page"},{"id":214498,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1111/j.1365-246X.2009.04417.x"},{"id":242231,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"180","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505ba8e7e4b08c986b321f17","contributors":{"authors":[{"text":"Bielak, J.","contributorId":88572,"corporation":false,"usgs":true,"family":"Bielak","given":"J.","email":"","affiliations":[],"preferred":false,"id":442434,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Graves, R.W. 0000-0001-9758-453X","orcid":"https://orcid.org/0000-0001-9758-453X","contributorId":77691,"corporation":false,"usgs":true,"family":"Graves","given":"R.W.","affiliations":[],"preferred":false,"id":442432,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Olsen, K.B.","contributorId":66022,"corporation":false,"usgs":true,"family":"Olsen","given":"K.B.","email":"","affiliations":[],"preferred":false,"id":442430,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Taborda, R.","contributorId":19792,"corporation":false,"usgs":true,"family":"Taborda","given":"R.","email":"","affiliations":[],"preferred":false,"id":442424,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Ramirez-Guzman, L.","contributorId":60459,"corporation":false,"usgs":true,"family":"Ramirez-Guzman","given":"L.","affiliations":[],"preferred":false,"id":442429,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Day, S.M.","contributorId":41425,"corporation":false,"usgs":true,"family":"Day","given":"S.M.","email":"","affiliations":[],"preferred":false,"id":442426,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Ely, G.P.","contributorId":97719,"corporation":false,"usgs":true,"family":"Ely","given":"G.P.","email":"","affiliations":[],"preferred":false,"id":442436,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Roten, D.","contributorId":73836,"corporation":false,"usgs":true,"family":"Roten","given":"D.","affiliations":[],"preferred":false,"id":442431,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Jordan, T.H.","contributorId":83320,"corporation":false,"usgs":true,"family":"Jordan","given":"T.H.","affiliations":[],"preferred":false,"id":442433,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Maechling, P.J.","contributorId":24582,"corporation":false,"usgs":true,"family":"Maechling","given":"P.J.","email":"","affiliations":[],"preferred":false,"id":442425,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Urbanic, J.","contributorId":47597,"corporation":false,"usgs":true,"family":"Urbanic","given":"J.","email":"","affiliations":[],"preferred":false,"id":442427,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Cui, Y.","contributorId":93717,"corporation":false,"usgs":true,"family":"Cui","given":"Y.","email":"","affiliations":[],"preferred":false,"id":442435,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Juve, G.","contributorId":49993,"corporation":false,"usgs":true,"family":"Juve","given":"G.","email":"","affiliations":[],"preferred":false,"id":442428,"contributorType":{"id":1,"text":"Authors"},"rank":13}]}}
,{"id":70034636,"text":"70034636 - 2010 - Fine scale daily movements and habitat use of East Pacific green turtles at a shallow coastal lagoon in Baja California Sur, Mexico","interactions":[],"lastModifiedDate":"2017-05-17T09:25:51","indexId":"70034636","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2277,"text":"Journal of Experimental Marine Biology and Ecology","active":true,"publicationSubtype":{"id":10}},"title":"Fine scale daily movements and habitat use of East Pacific green turtles at a shallow coastal lagoon in Baja California Sur, Mexico","docAbstract":"<p>Green turtles spend most of their lives in coastal foraging areas where they face multiple anthropogenic impacts. Therefore, understanding their spatial use in this environment is a priority for conservation efforts. We studied the fine scale daily movements and habitat use of East Pacific green turtles (<i>Chelonia mydas</i>) at Laguna San Ignacio, a shallow coastal lagoon in Baja California Sur, Mexico where sea turtles are subject to high levels of gillnet bycatch and directed hunting. Six turtles ranging from 44.6 to 83.5&nbsp;cm in straight carapace length were tracked for short deployments (1 to 6 d) with GPS-VHF telemetry. Turtles were active throughout diurnal, nocturnal, and crepuscular periods. Although they moved greater total distances during daytime, their speed of travel and net displacement remained consistent throughout 24-h periods. A positive selection for areas of seagrass and moderate water depth (5 to 10&nbsp;m) was determined using Ivlev's electivity index, with neutral selection for shallow water (&lt;&nbsp;5&nbsp;m) and avoidance of deep water (&gt;&nbsp;10&nbsp;m). Turtles exhibited two distinct behavioral movement patterns: circular movements with high fidelity to the capture&ndash;release location and meandering movements with low fidelity to the capture&ndash;release location. Our results indicate that green turtles were active throughout the diel cycle while traveling large distances and traversing multiple habitats over short temporal scales.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.jembe.2010.06.017","issn":"00220981","usgsCitation":"Senko, J., Koch, V., Megill, W.M., Carthy, R.R., Templeton, R.P., and Nichols, W.J., 2010, Fine scale daily movements and habitat use of East Pacific green turtles at a shallow coastal lagoon in Baja California Sur, Mexico: Journal of Experimental Marine Biology and Ecology, v. 391, no. 1-2, p. 92-100, https://doi.org/10.1016/j.jembe.2010.06.017.","productDescription":"9 p.","startPage":"92","endPage":"100","numberOfPages":"9","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-022304","costCenters":[{"id":198,"text":"Coop Res Unit 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,{"id":70034635,"text":"70034635 - 2010 - A late Miocene-early Pliocene chain of lakes fed by the Colorado River: Evidence from Sr, C, and O isotopes of the Bouse Formation and related units between Grand Canyon and the Gulf of California","interactions":[],"lastModifiedDate":"2021-12-03T15:31:17.791811","indexId":"70034635","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1786,"text":"Geological Society of America Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"A late Miocene-early Pliocene chain of lakes fed by the Colorado River: Evidence from Sr, C, and O isotopes of the Bouse Formation and related units between Grand Canyon and the Gulf of California","docAbstract":"<p><span>We report strontium isotopic results for the late Miocene Hualapai Limestone of the Lake Mead area (Arizona-Nevada) and the latest Miocene to early Pliocene Bouse Formation and related units of the lower Colorado River trough (Arizona-California-Nevada), together with parallel oxygen and carbon isotopic analyses of Bouse samples, to constrain the lake-overflow model for integration of the Colorado River. Sr isotopic analyses on the basal 1–5 cm of marl, in particular along a transect over a range of altitude in the lowest-altitude basin that contains freshwater, brackish, and marine fossils, document the&nbsp;</span><sup>87</sup><span>Sr/</span><sup>86</sup><span>Sr of first-arriving Bouse waters. Results reinforce the similarity between the&nbsp;</span><sup>87</sup><span>Sr/</span><sup>86</sup><span>Sr of Bouse Formation carbonates and present-day Colorado River water, and the systematic distinction of these values from Neogene marine Sr. Basal Bouse samples show that&nbsp;</span><sup>87</sup><span>Sr/</span><sup>86</sup><span>Sr decreased from 0.7111 to values in the range 0.7107–0.7109 during early basin filling.&nbsp;</span><sup>87</sup><span>Sr/</span><sup>86</sup><span>Sr values from a recently identified marl in the Las Vegas area are within the range of Bouse Sr ratios.&nbsp;</span><sup>87</sup><span>Sr/</span><sup>86</sup><span>Sr values from the Hualapai Limestone decrease upsection from 0.7195 to 0.7137, in the approach to a time soon after 6 Ma when Hualapai deposition ceased and the Colorado River became established through the Lake Mead area. Bouse Formation δ</span><sup>18</sup><span>O values range from –12.9‰ to +1.0‰ Vienna Pee Dee belemnite (VPDB), and δ</span><sup>13</sup><span>C between –6.5‰ and +3.4‰ VPDB. Negative δ</span><sup>18</sup><span>O values appear to require a continental origin for waters, and the trend to higher δ</span><sup>18</sup><span>O suggests evaporation in lake waters. Sr and stable isotopic results for sectioned barnacle shells and from bedding planes of the marine fish fossil&nbsp;</span><i>Colpichthys regis</i><span>&nbsp;demonstrate that these animals lived in saline freshwater, and that there is no evidence for incursions of marine water, either long-lived or brief in duration. Lack of correlation of Sr and O isotopic variations in the same samples also argue strongly against systematic replacement of Sr in Bouse carbonates after deposition. Our results reinforce the conclusion that the Bouse Formation was deposited in a descending series of basins connected by overflow of Colorado River water. The Hualapai Limestone records a separate and earlier lake that may have been progressively influenced by Colorado River water as the time of river integration approached.</span></p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/B30186.1","issn":"00167606","usgsCitation":"Roskowski, J.A., Patchett, P., Spencer, J., Pearthree, P., Dettman, D.L., Faulds, J.E., and Reynolds, A.C., 2010, A late Miocene-early Pliocene chain of lakes fed by the Colorado River: Evidence from Sr, C, and O isotopes of the Bouse Formation and related units between Grand Canyon and the Gulf of California: Geological Society of America Bulletin, v. 122, no. 9-10, p. 1625-1636, https://doi.org/10.1130/B30186.1.","productDescription":"12 p.","startPage":"1625","endPage":"1636","numberOfPages":"12","costCenters":[],"links":[{"id":243571,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Mexico, United States","state":"Arizona, Baja California, California, Nevada, Sonora","otherGeospatial":"Colorado River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -115.75195312499999,\n              31.38177878211098\n            ],\n            [\n              -113.99414062499999,\n              31.38177878211098\n            ],\n            [\n              -113.99414062499999,\n              35.96911507577482\n            ],\n            [\n              -115.75195312499999,\n              35.96911507577482\n            ],\n            [\n              -115.75195312499999,\n              31.38177878211098\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"122","issue":"9-10","noUsgsAuthors":false,"publicationDate":"2010-05-10","publicationStatus":"PW","scienceBaseUri":"5059e434e4b0c8380cd464c4","contributors":{"authors":[{"text":"Roskowski, J. A.","contributorId":95292,"corporation":false,"usgs":true,"family":"Roskowski","given":"J.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":446789,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Patchett, P. J.","contributorId":55152,"corporation":false,"usgs":true,"family":"Patchett","given":"P. J.","affiliations":[],"preferred":false,"id":446785,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Spencer, J.E.","contributorId":91542,"corporation":false,"usgs":true,"family":"Spencer","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":446788,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Pearthree, P. A.","contributorId":77236,"corporation":false,"usgs":false,"family":"Pearthree","given":"P. A.","affiliations":[],"preferred":false,"id":446786,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Dettman, D. L.","contributorId":100538,"corporation":false,"usgs":true,"family":"Dettman","given":"D.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":446790,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Faulds, J. E.","contributorId":84854,"corporation":false,"usgs":true,"family":"Faulds","given":"J.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":446787,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Reynolds, A. C.","contributorId":35110,"corporation":false,"usgs":true,"family":"Reynolds","given":"A.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":446784,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70034258,"text":"70034258 - 2010 - Sources of suspended-sediment flux in streams of the chesapeake bay watershed: A regional application of the sparrow model","interactions":[],"lastModifiedDate":"2012-03-12T17:21:46","indexId":"70034258","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2529,"text":"Journal of the American Water Resources Association","active":true,"publicationSubtype":{"id":10}},"title":"Sources of suspended-sediment flux in streams of the chesapeake bay watershed: A regional application of the sparrow model","docAbstract":"We describe the sources and transport of fluvial suspended sediment in nontidal streams of the Chesapeake Bay watershed and vicinity. We applied SPAtially Referenced Regressions on Watershed attributes, which spatially correlates estimated mean annual flux of suspended sediment in nontidal streams with sources of suspended sediment and transport factors. According to our model, urban development generates on average the greatest amount of suspended sediment per unit area (3,928 Mg/km2/year), although agriculture is much more widespread and is the greatest overall source of suspended sediment (57 Mg/km2/year). Factors affecting sediment transport from uplands to streams include mean basin slope, reservoirs, physiography, and soil permeability. On average, 59% of upland suspended sediment generated is temporarily stored along large rivers draining the Coastal Plain or in reservoirs throughout the watershed. Applying erosion and sediment controls from agriculture and urban development in areas of the northern Piedmont close to the upper Bay, where the combined effects of watershed characteristics on sediment transport have the greatest influence may be most helpful in mitigating sedimentation in the bay and its tributaries. Stream restoration efforts addressing floodplain and bank stabilization and incision may be more effective in smaller, headwater streams outside of the Coastal Plain. ?? 2010 American Water Resources Association. No claim to original U.S. government works.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of the American Water Resources Association","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1111/j.1752-1688.2010.00450.x","issn":"1093474X","usgsCitation":"Brakebill, J., Ator, S., and Schwarz, G., 2010, Sources of suspended-sediment flux in streams of the chesapeake bay watershed: A regional application of the sparrow model: Journal of the American Water Resources Association, v. 46, no. 4, p. 757-776, https://doi.org/10.1111/j.1752-1688.2010.00450.x.","startPage":"757","endPage":"776","numberOfPages":"20","costCenters":[],"links":[{"id":475988,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1111/j.1752-1688.2010.00450.x","text":"Publisher Index Page"},{"id":216764,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1111/j.1752-1688.2010.00450.x"},{"id":244651,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"46","issue":"4","noUsgsAuthors":false,"publicationDate":"2010-07-26","publicationStatus":"PW","scienceBaseUri":"505b9394e4b08c986b31a58c","contributors":{"authors":[{"text":"Brakebill, J. W.","contributorId":48206,"corporation":false,"usgs":true,"family":"Brakebill","given":"J. W.","affiliations":[],"preferred":false,"id":444951,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ator, S.W. 0000-0002-9186-4837","orcid":"https://orcid.org/0000-0002-9186-4837","contributorId":104100,"corporation":false,"usgs":true,"family":"Ator","given":"S.W.","affiliations":[],"preferred":false,"id":444952,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Schwarz, G. E. 0000-0002-9239-4566","orcid":"https://orcid.org/0000-0002-9239-4566","contributorId":14852,"corporation":false,"usgs":true,"family":"Schwarz","given":"G. E.","affiliations":[],"preferred":false,"id":444950,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70033897,"text":"70033897 - 2010 - Microclimate and propagule availability are equally important for rehabilitation of dryland N-fixing lichens","interactions":[],"lastModifiedDate":"2012-03-12T17:21:32","indexId":"70033897","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3271,"text":"Restoration Ecology","active":true,"publicationSubtype":{"id":10}},"title":"Microclimate and propagule availability are equally important for rehabilitation of dryland N-fixing lichens","docAbstract":"In some arid regions, rehabilitation of whole system N-fixation may be strongly facilitated by the recovery of populations of the lichen genus Collema. Identification of the limits to recovery of Collema in apparently suitable habitat should inform selection of rehabilitation techniques. We simultaneously tested the relative importance of three hypothetical limits to Collema recovery: active erosion, resource limitation, and propagule scarcity. We found that in our experimental system, active erosion had no effect on short-term establishment of Collema, whereas propagule addition did enhance recovery and microhabitat (a resource availability gradient) also exerted a strong influence. It is possible that attempts to improve N cycling via re-establishment of Collema might be best served by developing economical means of simulating moister, cooler microhabitats, e.g., sloping soil or creating partial shade, which would favor the establishment of naturally dispersed propagules, rather than introducing propagules. ?? 2009 Society for Ecological Restoration International.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Restoration Ecology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1111/j.1526-100X.2009.00578.x","issn":"10612971","usgsCitation":"Bowker, M.A., Belnap, J., and Davidson, D.W., 2010, Microclimate and propagule availability are equally important for rehabilitation of dryland N-fixing lichens: Restoration Ecology, v. 18, no. 1, p. 30-33, https://doi.org/10.1111/j.1526-100X.2009.00578.x.","startPage":"30","endPage":"33","numberOfPages":"4","costCenters":[],"links":[{"id":214300,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1111/j.1526-100X.2009.00578.x"},{"id":242008,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"18","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a566fe4b0c8380cd6d5bb","contributors":{"authors":[{"text":"Bowker, M. A.","contributorId":18901,"corporation":false,"usgs":true,"family":"Bowker","given":"M.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":443083,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Belnap, J. 0000-0001-7471-2279","orcid":"https://orcid.org/0000-0001-7471-2279","contributorId":23872,"corporation":false,"usgs":true,"family":"Belnap","given":"J.","affiliations":[],"preferred":false,"id":443084,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Davidson, D. W.","contributorId":52389,"corporation":false,"usgs":true,"family":"Davidson","given":"D.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":443085,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70034102,"text":"70034102 - 2010 - Relationship of voluminous ignimbrites to continental arc plutons: Petrology of Jurassic ignimbrites and contemporaneous plutons in southern California","interactions":[],"lastModifiedDate":"2012-03-12T17:21:44","indexId":"70034102","displayToPublicDate":"2010-01-01T00:00:00","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":"Relationship of voluminous ignimbrites to continental arc plutons: Petrology of Jurassic ignimbrites and contemporaneous plutons in southern California","docAbstract":"Volcanism was broadly associated in both space and time with Mesozoic plutonism in the Cordillera continental margin arc, but the precise petrogenetic relationships between volcanic rocks and adjacent zoned plutons are not known. Igneous rocks in a tilted crustal section in California include four laterally extensive Jurassic ash flow tuffs from 550 to &gt;1100 m thick underlain at deeper structural levels by Jurassic plutons. Zircon geochronology confirms previous correlations of individual tuffs, suggesting ignimbrites with eruptive volumes up to 800 km<sup>3</sup> were deposited both during the apparent Early Jurassic plutonic lull as well as contemporaneous with solidification of regionally widespread Middle and Late Jurassic plutons. The tuffs are weakly to strongly porphyritic (5 to 55% phenocrysts) monotonous intermediate porphyritic dacite to low-silica rhyolite and show strong bulk rock chemical affinity to contemporaneous plutons. Trace element compositions of zircons from the tuffs and contemporaneous plutonic rocks record large and consistent differences in Hf/Zr and REE over similar ranges in Ti abundances, supporting bulk compositional similarities and illuminating similarities and variations in thermal histories despite the effects of hydrothermal alteration. ?? 2009 Elsevier B.V. All rights reserved.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Volcanology and Geothermal Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.jvolgeores.2009.07.010","issn":"03770273","usgsCitation":"Fohey-Breting, N., Barth, A.P., Wooden, J.L., Mazdab, F., Carter, C., and Schermer, E., 2010, Relationship of voluminous ignimbrites to continental arc plutons: Petrology of Jurassic ignimbrites and contemporaneous plutons in southern California: Journal of Volcanology and Geothermal Research, v. 189, no. 1-2, p. 1-11, https://doi.org/10.1016/j.jvolgeores.2009.07.010.","startPage":"1","endPage":"11","numberOfPages":"11","costCenters":[],"links":[{"id":216871,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.jvolgeores.2009.07.010"},{"id":244769,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"189","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50e4a780e4b0e8fec6cdc4af","contributors":{"authors":[{"text":"Fohey-Breting, N. K.","contributorId":56883,"corporation":false,"usgs":true,"family":"Fohey-Breting","given":"N. K.","affiliations":[],"preferred":false,"id":444100,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Barth, A. P.","contributorId":16997,"corporation":false,"usgs":true,"family":"Barth","given":"A.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":444098,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wooden, J. L.","contributorId":58678,"corporation":false,"usgs":true,"family":"Wooden","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":444101,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Mazdab, F.K.","contributorId":11650,"corporation":false,"usgs":true,"family":"Mazdab","given":"F.K.","email":"","affiliations":[],"preferred":false,"id":444097,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Carter, C.A.","contributorId":29008,"corporation":false,"usgs":true,"family":"Carter","given":"C.A.","email":"","affiliations":[],"preferred":false,"id":444099,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Schermer, E.R.","contributorId":78756,"corporation":false,"usgs":true,"family":"Schermer","given":"E.R.","email":"","affiliations":[],"preferred":false,"id":444102,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70036160,"text":"70036160 - 2010 - Scallopleaf sage (salvia vaseyi: Lamiaceae) discovered in Arizona","interactions":[],"lastModifiedDate":"2012-03-12T17:22:06","indexId":"70036160","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2535,"text":"Journal of the Botanical Research Institute of Texas","active":true,"publicationSubtype":{"id":10}},"title":"Scallopleaf sage (salvia vaseyi: Lamiaceae) discovered in Arizona","docAbstract":"During the course of field work in Cabeza Prieta National Wildlife Refuge, southwestern Arizona, in 2003, James Cain and Brian Jansen collected Salvia vaseyi, previously known only from the western edge of the Sonoran Desert in California and Baja California. Our findings indicate this shrub might be more widespread in southwestern Arizona mountains. Salvia vaseyi in Arizona seems to represent a relict population. There are other shrubby Salvia in Arizona, but S. vaseyi is the most xeric-mhabiting species and has the narrowest ecological and geographical range.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of the Botanical Research Institute of Texas","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"19345259","usgsCitation":"Cain, J., Felger, R., Jansen, B., and Krausman, P., 2010, Scallopleaf sage (salvia vaseyi: Lamiaceae) discovered in Arizona: Journal of the Botanical Research Institute of Texas, v. 4, no. 2, p. 755-760.","startPage":"755","endPage":"760","numberOfPages":"6","costCenters":[],"links":[{"id":246206,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"4","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b871ee4b08c986b31630b","contributors":{"authors":[{"text":"Cain, J.W. III","contributorId":70910,"corporation":false,"usgs":true,"family":"Cain","given":"J.W.","suffix":"III","email":"","affiliations":[],"preferred":false,"id":454502,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Felger, R.S.","contributorId":80522,"corporation":false,"usgs":true,"family":"Felger","given":"R.S.","email":"","affiliations":[],"preferred":false,"id":454503,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Jansen, B.D.","contributorId":30079,"corporation":false,"usgs":true,"family":"Jansen","given":"B.D.","email":"","affiliations":[],"preferred":false,"id":454500,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Krausman, P.R.","contributorId":35525,"corporation":false,"usgs":true,"family":"Krausman","given":"P.R.","affiliations":[],"preferred":false,"id":454501,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70034105,"text":"70034105 - 2010 - Geomorphic knobs of Candor Chasma, Mars: New Mars Reconnaissance Orbiter data and comparisons to terrestrial analogs","interactions":[],"lastModifiedDate":"2019-02-04T12:05:35","indexId":"70034105","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1963,"text":"Icarus","active":true,"publicationSubtype":{"id":10}},"title":"Geomorphic knobs of Candor Chasma, Mars: New Mars Reconnaissance Orbiter data and comparisons to terrestrial analogs","docAbstract":"<p>High Resolution Imaging Science Experiment (HiRISE) imagery and digital elevation models of the Candor Chasma region of Valles Marineris, Mars, reveal prominent and distinctive positive-relief knobs amidst light-toned layers. Three classifications of knobs, Types 1, 2, and 3, are distinguished from a combination of HiRISE and Thermal Emission Imaging System (THEMIS) images based on physical expressions (geometries, spatial relationships), and spectral data from Compact Reconnaissance Imaging Spectrometer for Mars (CRISM). Type 1 knobs are abundant, concentrated, topographically resistant features with their highest frequency in West Candor, which have consistent stratigraphic correlations of the peak altitude (height). These Type 1 knobs could be erosional remnants of a simple dissected terrain, possibly derived from a more continuous, resistant, capping layer of pre-existing material diagenetically altered through recrystallization or cementation. Types 2 and 3 knobs are not linked to a single stratigraphic layer and are generally solitary to isolated, with variable heights. Type 3 are the largest knobs at nearly an order of magnitude larger than Type 1 knobs. The variable sizes and occasional pits on the tops of Type 2 and 3 knobs suggest a different origin, possibly related to more developed erosion, preferential cementation, or textural differences from sediment/water injection or intrusion, or from a buried impact crater. Enhanced color HiRISE images show a brown coloration of the knob peak crests that is attributable to processing and photometric effects; CRISM data do not show any detectable spectral differences between the knobs and the host rock layers, other than albedo. These intriguing knobs hold important clues to deducing relative rock properties, timing of events, and weathering conditions of Mars history.</p>","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Icarus","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","doi":"10.1016/j.icarus.2009.04.006","issn":"00191035","usgsCitation":"Chan, M.A., Ormö, J., Murchie, S., Okubo, C., Komatsu, G., Wray, J.J., McGuire, P.E., McGovern, J.A., and the HiRISE TEam, 2010, Geomorphic knobs of Candor Chasma, Mars: New Mars Reconnaissance Orbiter data and comparisons to terrestrial analogs: Icarus, v. 205, no. 1, p. 138-153, https://doi.org/10.1016/j.icarus.2009.04.006.","productDescription":"16 p.","startPage":"138","endPage":"153","numberOfPages":"16","costCenters":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"links":[{"id":244836,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Candor Chasma, Mars","volume":"205","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a2793e4b0c8380cd599e7","contributors":{"authors":[{"text":"Chan, Marjorie A.","contributorId":66230,"corporation":false,"usgs":true,"family":"Chan","given":"Marjorie","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":444117,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ormö, Jens","contributorId":166745,"corporation":false,"usgs":false,"family":"Ormö","given":"Jens","affiliations":[],"preferred":false,"id":444118,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Murchie, Scott L.","contributorId":22615,"corporation":false,"usgs":true,"family":"Murchie","given":"Scott L.","affiliations":[],"preferred":false,"id":444114,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Okubo, Chris 0000-0001-9776-8128 cokubo@usgs.gov","orcid":"https://orcid.org/0000-0001-9776-8128","contributorId":174209,"corporation":false,"usgs":true,"family":"Okubo","given":"Chris","email":"cokubo@usgs.gov","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":true,"id":444121,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Komatsu, Goro","contributorId":11061,"corporation":false,"usgs":true,"family":"Komatsu","given":"Goro","email":"","affiliations":[],"preferred":false,"id":444116,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Wray, James J.","contributorId":81736,"corporation":false,"usgs":false,"family":"Wray","given":"James","email":"","middleInitial":"J.","affiliations":[{"id":7032,"text":"School of Earth and Atmospheric Sciences, Georgia Institute of Technology","active":true,"usgs":false}],"preferred":false,"id":444115,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"McGuire, Patrick E.","contributorId":71008,"corporation":false,"usgs":false,"family":"McGuire","given":"Patrick","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":444120,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"McGovern, James A.","contributorId":212718,"corporation":false,"usgs":false,"family":"McGovern","given":"James","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":444119,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"the HiRISE TEam","contributorId":127993,"corporation":true,"usgs":false,"organization":"the HiRISE TEam","id":756427,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}}
,{"id":70033825,"text":"70033825 - 2010 - Night sampling improves indices used for management of yellow perch in Lake Erie","interactions":[],"lastModifiedDate":"2012-03-12T17:21:32","indexId":"70033825","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1659,"text":"Fisheries Management and Ecology","active":true,"publicationSubtype":{"id":10}},"title":"Night sampling improves indices used for management of yellow perch in Lake Erie","docAbstract":"Catch rate (catch per hour) was examined for age-0 and age-1 yellow perch, Perca flavescens (Mitchill), captured in bottom trawls from 1991 to 2005 in western Lake Erie: (1) to examine variation of catch rate among years, seasons, diel periods and their interactions; and (2) to determine whether sampling during particular diel periods improved the management value of CPH data used in models to project abundance of age-2 yellow perch. Catch rate varied with year, season and the diel period during which sampling was conducted as well as by the interaction between year and season. Indices of abundance of age-0 and age-1 yellow perch estimated from night samples typically produced better fitting models and lower estimates of age-2 abundance than those using morning or afternoon samples, whereas indices using afternoon samples typically produced less precise and higher estimates of abundance. The diel period during which sampling is conducted will not affect observed population trends but may affect estimates of abundance of age-0 and age-1 yellow perch, which in turn affect recommended allowable harvest. A field experiment throughout western Lake Erie is recommended to examine potential benefits of night sampling to management of yellow perch. Published 2010. The article is a US Government work and is in the public domain in the USA.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Fisheries Management and Ecology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1111/j.1365-2400.2009.00721.x","issn":"0969997X","usgsCitation":"Kocovsky, P., Stapanian, M., and Knight, C., 2010, Night sampling improves indices used for management of yellow perch in Lake Erie: Fisheries Management and Ecology, v. 17, no. 1, p. 10-18, https://doi.org/10.1111/j.1365-2400.2009.00721.x.","startPage":"10","endPage":"18","numberOfPages":"9","costCenters":[],"links":[{"id":214209,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1111/j.1365-2400.2009.00721.x"},{"id":241908,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","issue":"1","noUsgsAuthors":false,"publicationDate":"2010-01-08","publicationStatus":"PW","scienceBaseUri":"505a6654e4b0c8380cd72d77","contributors":{"authors":[{"text":"Kocovsky, P.M.","contributorId":78447,"corporation":false,"usgs":true,"family":"Kocovsky","given":"P.M.","affiliations":[],"preferred":false,"id":442716,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stapanian, M.A.","contributorId":65437,"corporation":false,"usgs":true,"family":"Stapanian","given":"M.A.","email":"","affiliations":[],"preferred":false,"id":442714,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Knight, C.T.","contributorId":66042,"corporation":false,"usgs":true,"family":"Knight","given":"C.T.","email":"","affiliations":[],"preferred":false,"id":442715,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70034178,"text":"70034178 - 2010 - Color imaging of Mars by the High Resolution Imaging Science Experiment (HiRISE)","interactions":[],"lastModifiedDate":"2018-11-20T11:03:10","indexId":"70034178","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1963,"text":"Icarus","active":true,"publicationSubtype":{"id":10}},"title":"Color imaging of Mars by the High Resolution Imaging Science Experiment (HiRISE)","docAbstract":"<p>HiRISE has been producing a large number of scientifically useful color products of Mars and other planetary objects. The three broad spectral bands, coupled with the highly sensitive 14 bit detectors and time delay integration, enable detection of subtle color differences. The very high spatial resolution of HiRISE can augment the mineralogic interpretations based on multispectral (THEMIS) and hyperspectral datasets (TES, OMEGA and CRISM) and thereby enable detailed geologic and stratigraphic interpretations at meter scales. In addition to providing some examples of color images and their interpretation, we describe the processing techniques used to produce them and note some of the minor artifacts in the output. We also provide an example of how HiRISE color products can be effectively used to expand mineral and lithologic mapping provided by CRISM data products that are backed by other spectral datasets. The utility of high quality color data for understanding geologic processes on Mars has been one of the major successes of HiRISE.</p>","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Icarus","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","doi":"10.1016/j.icarus.2009.03.012","issn":"00191035","usgsCitation":"Delamere, W.A., Tornabene, L., McEwen, A.S., Becker, K.J., Bergstrom, J.W., Bridges, N.T., Eliason, E.M., Gallagher, D., Herkenhoff, K.E., Keszthelyi, L., Mattson, S., McArthur, G.K., Mellon, M.T., Milazzo, M.P., Russell, P.S., and Thomas, N., 2010, Color imaging of Mars by the High Resolution Imaging Science Experiment (HiRISE): Icarus, v. 205, no. 1, p. 38-52, https://doi.org/10.1016/j.icarus.2009.03.012.","productDescription":"15 p.","startPage":"38","endPage":"52","numberOfPages":"15","costCenters":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"links":[{"id":244456,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"205","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f7bce4b0c8380cd4cc9f","contributors":{"authors":[{"text":"Delamere, W. Alan","contributorId":15042,"corporation":false,"usgs":true,"family":"Delamere","given":"W.","email":"","middleInitial":"Alan","affiliations":[],"preferred":false,"id":444456,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tornabene, Livio L.","contributorId":11915,"corporation":false,"usgs":true,"family":"Tornabene","given":"Livio L.","affiliations":[],"preferred":false,"id":444464,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"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":444450,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Becker, Kris J. 0000-0003-1971-5957 kbecker@usgs.gov","orcid":"https://orcid.org/0000-0003-1971-5957","contributorId":2910,"corporation":false,"usgs":true,"family":"Becker","given":"Kris","email":"kbecker@usgs.gov","middleInitial":"J.","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":true,"id":444463,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Bergstrom, James W.","contributorId":210510,"corporation":false,"usgs":false,"family":"Bergstrom","given":"James","email":"","middleInitial":"W.","affiliations":[{"id":6944,"text":"Ball Aerospace Technologies Corporation","active":true,"usgs":false}],"preferred":false,"id":444453,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Bridges, Nathan T.","contributorId":45005,"corporation":false,"usgs":true,"family":"Bridges","given":"Nathan","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":444451,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Eliason, Eric M.","contributorId":21280,"corporation":false,"usgs":true,"family":"Eliason","given":"Eric","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":444462,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Gallagher, Dennis","contributorId":210527,"corporation":false,"usgs":false,"family":"Gallagher","given":"Dennis","email":"","affiliations":[],"preferred":false,"id":444455,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"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":444457,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Keszthelyi, Laszlo P. 0000-0003-1879-4331 laz@usgs.gov","orcid":"https://orcid.org/0000-0003-1879-4331","contributorId":52802,"corporation":false,"usgs":true,"family":"Keszthelyi","given":"Laszlo P.","email":"laz@usgs.gov","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":true,"id":444454,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Mattson, Sarah","contributorId":102391,"corporation":false,"usgs":true,"family":"Mattson","given":"Sarah","affiliations":[],"preferred":false,"id":444452,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"McArthur, Guy K.","contributorId":210528,"corporation":false,"usgs":false,"family":"McArthur","given":"Guy","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":444458,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Mellon, Michael T.","contributorId":8603,"corporation":false,"usgs":false,"family":"Mellon","given":"Michael","email":"","middleInitial":"T.","affiliations":[{"id":7037,"text":"Southwest Research Institute, Boulder, Colorado","active":true,"usgs":false}],"preferred":false,"id":444461,"contributorType":{"id":1,"text":"Authors"},"rank":13},{"text":"Milazzo, Moses P. 0000-0002-9101-2191 moses@usgs.gov","orcid":"https://orcid.org/0000-0002-9101-2191","contributorId":4811,"corporation":false,"usgs":true,"family":"Milazzo","given":"Moses","email":"moses@usgs.gov","middleInitial":"P.","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":true,"id":444460,"contributorType":{"id":1,"text":"Authors"},"rank":14},{"text":"Russell, Patrick S.","contributorId":210529,"corporation":false,"usgs":false,"family":"Russell","given":"Patrick","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":444465,"contributorType":{"id":1,"text":"Authors"},"rank":15},{"text":"Thomas, Nicolas","contributorId":203694,"corporation":false,"usgs":false,"family":"Thomas","given":"Nicolas","email":"","affiliations":[{"id":25430,"text":"University of Bern","active":true,"usgs":false}],"preferred":false,"id":444459,"contributorType":{"id":1,"text":"Authors"},"rank":16}]}}
,{"id":70033896,"text":"70033896 - 2010 - Intraspecific variation in growth of marsh macrophytes in response to salinity and soil type: Implications for wetland restoration","interactions":[],"lastModifiedDate":"2019-03-27T15:22:18","indexId":"70033896","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1584,"text":"Estuaries and Coasts","active":true,"publicationSubtype":{"id":10}},"title":"Intraspecific variation in growth of marsh macrophytes in response to salinity and soil type: Implications for wetland restoration","docAbstract":"<p><span>Genetic diversity within plant populations can influence plant community structure along environmental gradients. In wetland habitats, salinity and soil type are factors that can vary along gradients and therefore affect plant growth. To test for intraspecific growth variation in response to these factors, a greenhouse study was conducted using common plants that occur in northern Gulf of Mexico brackish and salt marshes. Individual plants of&nbsp;</span><i class=\"EmphasisTypeItalic \">Distichlis spicata</i><span>,&nbsp;</span><i class=\"EmphasisTypeItalic \">Phragmites australis</i><span>,&nbsp;</span><i class=\"EmphasisTypeItalic \">Schoenoplectus californicus</i><span>, and&nbsp;</span><i class=\"EmphasisTypeItalic \">Schoenoplectus robustus</i><span>&nbsp;were collected from several locations along the coast in Louisiana, USA. Plant identity, based on collection location, was used as a measure of intraspecific variability. Prepared soil mixtures were organic, silt, or clay, and salinity treatments were 0 or 18&nbsp;psu. Significant intraspecific variation in stem number, total stem height, or biomass was found in all species. Within species, response to soil type varied, but increased salinity significantly decreased growth in all individuals. Findings indicate that inclusion of multiple genets within species is an important consideration for marsh restoration projects that include vegetation plantings. This strategy will facilitate establishment of plant communities that have the flexibility to adapt to changing environmental conditions and, therefore, are capable of persisting over time.</span></p>","language":"English","publisher":"Springer","doi":"10.1007/s12237-009-9227-z","issn":"15592723","usgsCitation":"Howard, R., 2010, Intraspecific variation in growth of marsh macrophytes in response to salinity and soil type: Implications for wetland restoration: Estuaries and Coasts, v. 33, no. 1, p. 127-138, https://doi.org/10.1007/s12237-009-9227-z.","productDescription":"12 p.","startPage":"127","endPage":"138","costCenters":[{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"links":[{"id":242007,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":214299,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/s12237-009-9227-z"}],"volume":"33","issue":"1","noUsgsAuthors":false,"publicationDate":"2009-10-15","publicationStatus":"PW","scienceBaseUri":"505a3dcae4b0c8380cd63851","contributors":{"authors":[{"text":"Howard, R.J. 0000-0001-7264-4364","orcid":"https://orcid.org/0000-0001-7264-4364","contributorId":86452,"corporation":false,"usgs":true,"family":"Howard","given":"R.J.","affiliations":[{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"preferred":false,"id":443082,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70179318,"text":"70179318 - 2010 - Elwha River dam removal: A major opportunity for salmon and steelhead recolonization","interactions":[],"lastModifiedDate":"2016-12-28T12:25:06","indexId":"70179318","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5246,"text":"Osprey ","active":true,"publicationSubtype":{"id":10}},"title":"Elwha River dam removal: A major opportunity for salmon and steelhead recolonization","docAbstract":"<p>In this in-depth paper, authors George R. Pess, Gary A. Winans and Timothy J. Beechie of the NOAA Fisheries, Northwest Fisheries Science Center in Seattle, Samuel J. Brenkman of the National Park Service, Olympic National Park, Michael L. McHenry of the Lower Elwha Klallam Tribe and Jeffrey J. Duda of the U.S. Geological Survey, Western Fisheries Research Center in Seattle, provide an historical overview of the Elwha River system, and its native anadromous fish runs and the prospect of their recolonization after the Elwha and Glines Canyon dams are removed.</p>","language":"English","publisher":"Steelhead Committee Federation of Fly Fishers","usgsCitation":"Pess, G.R., Brenkman, S.J., Winans, G.A., McHenry, M.L., Duda, J.J., and Beechie, T.J., 2010, Elwha River dam removal: A major opportunity for salmon and steelhead recolonization: Osprey , no. 65, 20 p.","productDescription":"20 p.","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":332587,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Washington","otherGeospatial":"Elwha river ","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": 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WA","active":true,"usgs":false}],"preferred":false,"id":656742,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Winans, Gary A.","contributorId":177706,"corporation":false,"usgs":false,"family":"Winans","given":"Gary","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":656743,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"McHenry, Michael L.","contributorId":39672,"corporation":false,"usgs":false,"family":"McHenry","given":"Michael","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":656744,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Duda, Jeffrey J. 0000-0001-7431-8634 jduda@usgs.gov","orcid":"https://orcid.org/0000-0001-7431-8634","contributorId":145486,"corporation":false,"usgs":true,"family":"Duda","given":"Jeffrey","email":"jduda@usgs.gov","middleInitial":"J.","affiliations":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"preferred":false,"id":656745,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Beechie, Timothy J.","contributorId":139468,"corporation":false,"usgs":false,"family":"Beechie","given":"Timothy","email":"","middleInitial":"J.","affiliations":[{"id":6578,"text":"National Marine Fisheries Service, Seattle, WA 98112, USA","active":true,"usgs":false}],"preferred":false,"id":656746,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70034068,"text":"70034068 - 2010 - Eolian transport of geogenic hexavalent chromium to ground water","interactions":[],"lastModifiedDate":"2013-05-12T00:16:20","indexId":"70034068","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1861,"text":"Ground Water","active":true,"publicationSubtype":{"id":10}},"title":"Eolian transport of geogenic hexavalent chromium to ground water","docAbstract":"A conceptual model of eolian transport is proposed to address the widely distributed, high concentrations of hexavalent chromium (Cr<sup>+6</sup>) observed in ground water in the Emirate of Abu Dhabi, United Arab Emirates. Concentrations (30 to more than 1000 μg/L Cr<sup>+6</sup>) extend over thousands of square kilometers of ground water systems. It is hypothesized that the Cr is derived from weathering of chromium-rich pyroxenes and olivines present in ophiolite sequence of the adjacent Oman (Hajar) Mountains. Cr<sup>+3</sup> in the minerals is oxidized to Cr<sup>+6</sup> by reduction of manganese and is subsequently sorbed on iron and manganese oxide coatings of particles. When the surfaces of these particles are abraded in this arid environment, they release fine, micrometer-sized, coated particles that are easily transported over large distances by wind and subsequently deposited on the surface. During ground water recharge events, the readily soluble Cr<sup>+6</sup> is mobilized by rain water and transported by advective flow into the underlying aquifer. Chromium analyses of ground water, rain, dust, and surface (soil) deposits are consistent with this model, as are electron probe analyses of clasts derived from the eroding Oman ophiolite sequence. Ground water recharge flux is proposed to exercise some control over Cr<sup>+6</sup> concentration in the aquifer.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Ground Water","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Wiley","doi":"10.1111/j.1745-6584.2009.00592.x","issn":"0017467X","usgsCitation":"Wood, W., Clark, D., Imes, J., and Councell, T., 2010, Eolian transport of geogenic hexavalent chromium to ground water: Ground Water, v. 48, no. 1, p. 19-29, https://doi.org/10.1111/j.1745-6584.2009.00592.x.","productDescription":"11 p.","startPage":"19","endPage":"29","costCenters":[{"id":326,"text":"Ground-Water Research Program for the Emirate of Abu DhabiUnited Arab Emirates","active":false,"usgs":true}],"links":[{"id":475942,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1111/j.1745-6584.2009.00592.x","text":"Publisher Index Page"},{"id":216867,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1111/j.1745-6584.2009.00592.x"},{"id":244765,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"48","issue":"1","noUsgsAuthors":false,"publicationDate":"2009-12-23","publicationStatus":"PW","scienceBaseUri":"505a0a03e4b0c8380cd52162","contributors":{"authors":[{"text":"Wood, W.W.","contributorId":21974,"corporation":false,"usgs":true,"family":"Wood","given":"W.W.","email":"","affiliations":[],"preferred":false,"id":443912,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Clark, D.","contributorId":94133,"corporation":false,"usgs":true,"family":"Clark","given":"D.","affiliations":[],"preferred":false,"id":443915,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Imes, J. L.","contributorId":61428,"corporation":false,"usgs":true,"family":"Imes","given":"J. L.","affiliations":[],"preferred":false,"id":443914,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Councell, T.B.","contributorId":44187,"corporation":false,"usgs":true,"family":"Councell","given":"T.B.","email":"","affiliations":[],"preferred":false,"id":443913,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70044490,"text":"70044490 - 2010 - Modern climate challenges and the geological record","interactions":[],"lastModifiedDate":"2013-03-12T10:26:07","indexId":"70044490","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":741,"text":"American Paleontologist","active":true,"publicationSubtype":{"id":10}},"title":"Modern climate challenges and the geological record","docAbstract":"Today's changing climate poses challenges about the influence of human activity, such as greenhouse gas emissions and land use changes, the natural variability of Earth's climate, and complex feedback processes. Ice core and instrumental records show that over the last century, atmospheric carbon dioxide (CO<sub>2</sub>) concentrations have risen to 390 parts per million volume (ppmv), about 40% above pre-Industrial Age concentrations of 280 ppmv and nearly twice those of the last glacial maximum about 22,000 years ago. Similar historical increases are recorded in atmospheric methane (CH<sub>4</sub>) and nitrous oxide (N<sub>2</sub>O). There is general agreement that human activity is largely responsible for these trends. Substantial evidence also suggests that elevated greenhouse gas concentrations are responsible for much of the recent atmospheric and oceanic warming, rising sea level, declining Arctic sea-ice cover, retreating glaciers and small ice caps, decreased mass balance of the Greenland and parts of the Antarctic ice sheets, and decreasing ocean pH (ocean \"acidification\"). Elevated CO<sub>2</sub> concentrations raise concern not only from observations of the climate system, but because feedbacks associated with reduced reflectivity from in land and sea ice, sea level, and land vegetation relatively slowly (centuries or longer) to elevated 2 levels. This means that additional human-induced climate change is expected even if the rate of CO<sub>2</sub> emissions is reduced or concentrations immediately stabilized.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"American Paleontologist","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Paleontological Research Institution","publisherLocation":"Ithaca, NY","usgsCitation":"Cronin, T.M., 2010, Modern climate challenges and the geological record: American Paleontologist, v. 18, no. 1, p. 10-12.","productDescription":"3 p.","startPage":"10","endPage":"12","numberOfPages":"3","ipdsId":"IP-018652","costCenters":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"links":[{"id":269127,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"18","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51404e83e4b089809dbf4498","contributors":{"authors":[{"text":"Cronin, Thomas M. 0000-0002-2643-0979 tcronin@usgs.gov","orcid":"https://orcid.org/0000-0002-2643-0979","contributorId":2579,"corporation":false,"usgs":true,"family":"Cronin","given":"Thomas","email":"tcronin@usgs.gov","middleInitial":"M.","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true},{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true}],"preferred":true,"id":475720,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70034064,"text":"70034064 - 2010 - Patterns of mercury dispersion from local and regional emission sources, rural Central Wisconsin, USA","interactions":[],"lastModifiedDate":"2018-10-09T09:45:36","indexId":"70034064","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":923,"text":"Atmospheric Chemistry and Physics Discussions","active":true,"publicationSubtype":{"id":10}},"title":"Patterns of mercury dispersion from local and regional emission sources, rural Central Wisconsin, USA","docAbstract":"<p>Simultaneous real-time changes in mercury (Hg) speciation-reactive gaseous Hg (RGM), elemental Hg (Hg??), and fine particulate Hg (Hg-PM<sub>2.5</sub>), were determined from June to November 2007, in ambient air at three locations in rural Central Wisconsin. Known Hg emission sources within the airshed of the monitoring sites include: 1) a 1114 megawatt (MW) coal-fired electric utility generating station; 2) a Hg-bed chlor-alkali plant; and 3) a smaller (465 MW) coal-burning electric utility. Monitoring sites, showing sporadic elevation of RGM, Hg<sup>o</sup> and Hg-PM <sub>2.5</sub>, were positioned at distances of 25, 50 and 100 km northward of the larger electric utility. A series of RGM events were recorded at each site. The largest, on 23 September, occurred under prevailing southerly winds, with a maximum RGM value (56.8 pg m<sup>-3</sup>) measured at the 100 km site, and corresponding elevated SO<sub>2</sub> (10.41 ppbv; measured at 50 km site). The finding that RGM, Hg<sup>o</sup>, and Hg-PM<sub>2.5</sub> are not always highest at the 25 km site, closest to the large generating station, contradicts the idea that RGM decreases with distance from a large point source. This may be explained if: 1) the 100 km site was influenced by emissions from the chlor-alkali facility or by RGM from regional urban sources; 2) the emission stack height of the larger power plant promoted plume transport at an elevation where the Hg is carried over the closest site; or 3) RGM was being generated in the plume through oxidation of Hg<sup>o</sup>. Operational changes at each emitter since 2007 should reduce their Hg output, potentially allowing quantification of the environmental benefit in future studies.</p>","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Atmospheric Chemistry and Physics Discussions","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.5194/acp-10-4467-2010","issn":"16807367","usgsCitation":"Kolker, A., Olson, M., Krabbenhoft, D., Tate, M., and Engle, M.A., 2010, Patterns of mercury dispersion from local and regional emission sources, rural Central Wisconsin, USA: Atmospheric Chemistry and Physics Discussions, v. 10, no. 1, p. 1823-1846, https://doi.org/10.5194/acp-10-4467-2010.","startPage":"1823","endPage":"1846","numberOfPages":"24","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":475941,"rank":1,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.5194/acp-10-4467-2010","text":"Publisher Index Page"},{"id":244704,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"10","issue":"1","noUsgsAuthors":false,"publicationDate":"2010-05-17","publicationStatus":"PW","scienceBaseUri":"505a75dde4b0c8380cd77db3","contributors":{"authors":[{"text":"Kolker, A. 0000-0002-5768-4533","orcid":"https://orcid.org/0000-0002-5768-4533","contributorId":10947,"corporation":false,"usgs":true,"family":"Kolker","given":"A.","affiliations":[],"preferred":false,"id":443885,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Olson, M.L.","contributorId":21989,"corporation":false,"usgs":true,"family":"Olson","given":"M.L.","email":"","affiliations":[],"preferred":false,"id":443886,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Krabbenhoft, David P. 0000-0003-1964-5020 dpkrabbe@usgs.gov","orcid":"https://orcid.org/0000-0003-1964-5020","contributorId":118001,"corporation":false,"usgs":true,"family":"Krabbenhoft","given":"David P.","email":"dpkrabbe@usgs.gov","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true},{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"preferred":false,"id":443889,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Tate, Michael T. 0000-0003-1525-1219 mttate@usgs.gov","orcid":"https://orcid.org/0000-0003-1525-1219","contributorId":3144,"corporation":false,"usgs":true,"family":"Tate","given":"Michael T.","email":"mttate@usgs.gov","affiliations":[{"id":37947,"text":"Upper Midwest Water Science Center","active":true,"usgs":true},{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"preferred":true,"id":443887,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Engle, Mark A. 0000-0001-5258-7374 engle@usgs.gov","orcid":"https://orcid.org/0000-0001-5258-7374","contributorId":584,"corporation":false,"usgs":true,"family":"Engle","given":"Mark","email":"engle@usgs.gov","middleInitial":"A.","affiliations":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":443888,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70034061,"text":"70034061 - 2010 - Propagule pressure and stream characteristics influence introgression: Cutthroat and rainbow trout in British Columbia","interactions":[],"lastModifiedDate":"2012-03-12T17:21:44","indexId":"70034061","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1450,"text":"Ecological Applications","active":true,"publicationSubtype":{"id":10}},"title":"Propagule pressure and stream characteristics influence introgression: Cutthroat and rainbow trout in British Columbia","docAbstract":"Hybridization and introgression between introduced and native salmonids threaten the continued persistence of many inland cutthroat trout species. Environmental models have been developed to predict the spread of introgression, but few studies have assessed the role of propagule pressure. We used an extensive set of fish stocking records and geographic information system (GIS) data to produce a spatially explicit index of potential propagule pressure exerted by introduced rainbow trout in the Upper Kootenay River, British Columbia, Canada. We then used logistic regression and the information-theoretic approach to test the ability of a set of environmental and spatial variables to predict the level of introgression between native westslope cutthroat trout and introduced rainbow trout. Introgression was assessed using between four and seven co-dominant, diagnostic nuclear markers at 45 sites in 31 different streams. The best model for predicting introgression included our GIS propagule pressure index and an environmental variable that accounted for the biogeoclimatic zone of the site (r<sup>2</sup> = 0.62). This model was 1.4 times more likely to explain introgression than the next-best model, which consisted of only the propagule pressure index variable. We created a composite model based on the model-averaged results of the seven top models that included environmental, spatial, and propagule pressure variables. The propagule pressure index had the highest importance weight (0.995) of all variables tested and was negatively related to sites with no introgression. This study used an index of propagule pressure and demonstrated that propagule pressure had the greatest influence on the level of introgression between a native and introduced trout in a human-induced hybrid zone. ?? 2010 by the Ecological Society of America.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Ecological Applications","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1890/08-0441.1","issn":"10510761","usgsCitation":"Bennett, S., Olson, J., Kershner, J.L., and Corbett, P., 2010, Propagule pressure and stream characteristics influence introgression: Cutthroat and rainbow trout in British Columbia: Ecological Applications, v. 20, no. 1, p. 263-277, https://doi.org/10.1890/08-0441.1.","startPage":"263","endPage":"277","numberOfPages":"15","costCenters":[],"links":[{"id":216752,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1890/08-0441.1"},{"id":244638,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"20","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a8f14e4b0c8380cd7f588","contributors":{"authors":[{"text":"Bennett, S.N.","contributorId":87784,"corporation":false,"usgs":true,"family":"Bennett","given":"S.N.","email":"","affiliations":[],"preferred":false,"id":443870,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Olson, J.R.","contributorId":98976,"corporation":false,"usgs":true,"family":"Olson","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":443871,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kershner, J. L.","contributorId":100322,"corporation":false,"usgs":true,"family":"Kershner","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":443872,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Corbett, P.","contributorId":54434,"corporation":false,"usgs":true,"family":"Corbett","given":"P.","email":"","affiliations":[],"preferred":false,"id":443869,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70034060,"text":"70034060 - 2010 - Community variations in social vulnerability to Cascadia-related tsunamis in the U.S. Pacific Northwest","interactions":[],"lastModifiedDate":"2012-03-12T17:21:44","indexId":"70034060","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2822,"text":"Natural Hazards","active":true,"publicationSubtype":{"id":10}},"title":"Community variations in social vulnerability to Cascadia-related tsunamis in the U.S. Pacific Northwest","docAbstract":"Tsunamis generated by Cascadia subduction zone earthquakes pose significant threats to coastal communities in the U. S. Pacific Northwest. Impacts of future tsunamis to individuals and communities will likely vary due to pre-event socioeconomic and demographic differences. In order to assess social vulnerability to Cascadia tsunamis, we adjust a social vulnerability index based on principal component analysis first developed by Cutter et al. (2003) to operate at the census-block level of geography and focus on community-level comparisons along the Oregon coast. The number of residents from blocks in tsunami-prone areas considered to have higher social vulnerability varies considerably among 26 Oregon cities and most are concentrated in four cities and two unincorporated areas. Variations in the number of residents from census blocks considered to have higher social vulnerability in each city do not strongly correlate with the number of residents or city assets in tsunami-prone areas. Methods presented here will help emergency managers to identify community sub-groups that are more susceptible to loss and to develop risk-reduction strategies that are tailored to local conditions. ?? z.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Natural Hazards","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1007/s11069-009-9376-1","issn":"0921030X","usgsCitation":"Wood, N., Burton, C., and Cutter, S., 2010, Community variations in social vulnerability to Cascadia-related tsunamis in the U.S. Pacific Northwest: Natural Hazards, v. 52, no. 2, p. 369-389, https://doi.org/10.1007/s11069-009-9376-1.","startPage":"369","endPage":"389","numberOfPages":"21","costCenters":[],"links":[{"id":475863,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1007/s11069-009-9376-1","text":"Publisher Index Page"},{"id":216751,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/s11069-009-9376-1"},{"id":244637,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"52","issue":"2","noUsgsAuthors":false,"publicationDate":"2009-03-26","publicationStatus":"PW","scienceBaseUri":"5059f80be4b0c8380cd4ce4d","contributors":{"authors":[{"text":"Wood, N.J.","contributorId":7900,"corporation":false,"usgs":true,"family":"Wood","given":"N.J.","email":"","affiliations":[],"preferred":false,"id":443866,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Burton, C.G.","contributorId":88582,"corporation":false,"usgs":true,"family":"Burton","given":"C.G.","email":"","affiliations":[],"preferred":false,"id":443867,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cutter, S.L.","contributorId":96515,"corporation":false,"usgs":true,"family":"Cutter","given":"S.L.","email":"","affiliations":[],"preferred":false,"id":443868,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70034057,"text":"70034057 - 2010 - Response of benthic macroinvertebrate communities to highway construction in an Appalachian watershed","interactions":[],"lastModifiedDate":"2012-03-12T17:21:44","indexId":"70034057","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1919,"text":"Hydrobiologia","onlineIssn":"1573-5117","printIssn":"0018-8158","active":true,"publicationSubtype":{"id":10}},"title":"Response of benthic macroinvertebrate communities to highway construction in an Appalachian watershed","docAbstract":"Highway construction in mountainous areas can result in sedimentation of streams, negatively impacting stream habitat, water quality, and biotic communities. We assessed the impacts of construction of a segment of Corridor H, a four-lane highway, in the Lost River watershed, West Virginia, by monitoring benthic macroinvertebrate communities and water quality, before, during, and after highway construction and prior to highway use at upstream and downstream sites from 1997 through 2007. Data analysis of temporal impacts of highway construction followed a Before-After-Control-Impact (BACI) study design. Highway construction impacts included an increase in stream sedimentation during the construction phase. This was indicated by an increase in turbidity and total suspended solids. Benthic macroinvertebrate metrics indicated a community more tolerant during and after construction than in the period before construction. The percent of Chironomidae and the Hilsenhoff Biotic Index (HBI) increased, while percent of Ephemeroptera, Plecoptera, and Trichoptera (EPT) decreased. Our 10-year study addressed short-term impacts of highway construction and found that impacts were relatively minimal. A recovery of the number of EPT taxa collected after construction indicated that the benthic macroinvertebrate community may be recovering from impacts of highway construction. However, this study only addressed a period of 3 years before, 3 years during, and 4 years post construction. Inferences cannot be made concerning the long-term impacts of the highway, highway traffic, runoff, and other factors associated with highway use. Continual monitoring of the watershed is necessary to determine if the highway has a continual impact on stream habitat, water quality, and biotic integrity. ?? 2010 Springer Science+Business Media B.V.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Hydrobiologia","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1007/s10750-009-0070-9","issn":"00188158","usgsCitation":"Hedrick, L.B., Welsh, S., Anderson, J.T., Lin, L., Chen, Y., and Wei, X., 2010, Response of benthic macroinvertebrate communities to highway construction in an Appalachian watershed: Hydrobiologia, v. 641, no. 1, p. 115-131, https://doi.org/10.1007/s10750-009-0070-9.","startPage":"115","endPage":"131","numberOfPages":"17","costCenters":[],"links":[{"id":216687,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/s10750-009-0070-9"},{"id":244572,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"641","issue":"1","noUsgsAuthors":false,"publicationDate":"2010-01-12","publicationStatus":"PW","scienceBaseUri":"505aaa35e4b0c8380cd861e4","contributors":{"authors":[{"text":"Hedrick, Lara B.","contributorId":50346,"corporation":false,"usgs":true,"family":"Hedrick","given":"Lara","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":443852,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Welsh, S.A. 0000-0003-0362-054X","orcid":"https://orcid.org/0000-0003-0362-054X","contributorId":10191,"corporation":false,"usgs":true,"family":"Welsh","given":"S.A.","affiliations":[],"preferred":false,"id":443850,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Anderson, James T.","contributorId":28071,"corporation":false,"usgs":false,"family":"Anderson","given":"James","email":"","middleInitial":"T.","affiliations":[{"id":12432,"text":"West Virginia University","active":true,"usgs":false}],"preferred":false,"id":443851,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lin, L.-S.","contributorId":66093,"corporation":false,"usgs":true,"family":"Lin","given":"L.-S.","email":"","affiliations":[],"preferred":false,"id":443854,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Chen, Y.","contributorId":7019,"corporation":false,"usgs":true,"family":"Chen","given":"Y.","email":"","affiliations":[],"preferred":false,"id":443849,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Wei, X.","contributorId":50636,"corporation":false,"usgs":true,"family":"Wei","given":"X.","email":"","affiliations":[],"preferred":false,"id":443853,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70034040,"text":"70034040 - 2010 - Yearling greater sage-grouse response to energy development in Wyoming","interactions":[],"lastModifiedDate":"2012-03-12T17:21:48","indexId":"70034040","displayToPublicDate":"2010-01-01T00:00:00","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":"Yearling greater sage-grouse response to energy development in Wyoming","docAbstract":"Sagebrush (Artemisia spp.)-dominated habitats in the western United States have experienced extensive, rapid changes due to development of natural-gas fields, resulting in localized declines of greater sage-grouse (Centrocercus urophasianus) populations. It is unclear whether population declines in natural-gas fields are caused by avoidance or demographic impacts, or the age classes that are most affected. Land and wildlife management agencies need information on how energy developments affect sage-grouse populations to ensure informed land-use decisions are made, effective mitigation measures are identified, and appropriate monitoring programs are implemented (Sawyer et al. 2006). We used information from radio-equipped greater sage-grouse and lek counts to investigate natural-gas development influences on 1) the distribution of, and 2) the probability of recruiting yearling males and females into breeding populations in the Upper Green River Basin of southwestern Wyoming, USA. Yearling males avoided leks near the infrastructure of natural-gas fields when establishing breeding territories; yearling females avoided nesting within 950 m of the infrastructure of natural-gas fields. Additionally, both yearling males and yearling females reared in areas where infrastructure was present had lower annual survival, and yearling males established breeding territories less often, compared to yearlings reared in areas with no infrastructure. Our results supply mechanisms for population-level declines of sage-grouse documented in natural-gas fields, and suggest to land managers that current stipulations on development may not provide management solutions. Managing landscapes so that suitably sized and located regions remain undeveloped may be an effective strategy to sustain greater sage-grouse populations affected by energy developments. ?? 2010 The Wildlife Society.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Wildlife Management","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.2193/2008-291","issn":"0022541X","usgsCitation":"Holloran, M., Kaiser, R., and Hubert, W., 2010, Yearling greater sage-grouse response to energy development in Wyoming: Journal of Wildlife Management, v. 74, no. 1, p. 65-72, https://doi.org/10.2193/2008-291.","startPage":"65","endPage":"72","numberOfPages":"8","costCenters":[],"links":[{"id":216930,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.2193/2008-291"},{"id":244832,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"74","issue":"1","noUsgsAuthors":false,"publicationDate":"2010-12-13","publicationStatus":"PW","scienceBaseUri":"505bd205e4b08c986b32f630","contributors":{"authors":[{"text":"Holloran, M.J.","contributorId":50000,"corporation":false,"usgs":true,"family":"Holloran","given":"M.J.","email":"","affiliations":[],"preferred":false,"id":443776,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kaiser, R.C.","contributorId":78584,"corporation":false,"usgs":true,"family":"Kaiser","given":"R.C.","email":"","affiliations":[],"preferred":false,"id":443777,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hubert, W.A.","contributorId":12822,"corporation":false,"usgs":true,"family":"Hubert","given":"W.A.","email":"","affiliations":[],"preferred":false,"id":443775,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70034039,"text":"70034039 - 2010 - Quality of the log-geometric distribution extrapolation for smaller undiscovered oil and gas pool size","interactions":[],"lastModifiedDate":"2012-03-12T17:21:48","indexId":"70034039","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2832,"text":"Natural Resources Research","onlineIssn":"1573-8981","printIssn":"1520-7439","active":true,"publicationSubtype":{"id":10}},"title":"Quality of the log-geometric distribution extrapolation for smaller undiscovered oil and gas pool size","docAbstract":"The U.S. Geological Survey procedure for the estimation of the general form of the parent distribution requires that the parameters of the log-geometric distribution be calculated and analyzed for the sensitivity of these parameters to different conditions. In this study, we derive the shape factor of a log-geometric distribution from the ratio of frequencies between adjacent bins. The shape factor has a log straight-line relationship with the ratio of frequencies. Additionally, the calculation equations of a ratio of the mean size to the lower size-class boundary are deduced. For a specific log-geometric distribution, we find that the ratio of the mean size to the lower size-class boundary is the same. We apply our analysis to simulations based on oil and gas pool distributions from four petroleum systems of Alberta, Canada and four generated distributions. Each petroleum system in Alberta has a different shape factor. Generally, the shape factors in the four petroleum systems stabilize with the increase of discovered pool numbers. For a log-geometric distribution, the shape factor becomes stable when discovered pool numbers exceed 50 and the shape factor is influenced by the exploration efficiency when the exploration efficiency is less than 1. The simulation results show that calculated shape factors increase with those of the parent distributions, and undiscovered oil and gas resources estimated through the log-geometric distribution extrapolation are smaller than the actual values. ?? 2010 International Association for Mathematical Geology.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Natural Resources Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1007/s11053-010-9109-x","issn":"15207439","usgsCitation":"Chenglin, L., and Charpentier, R., 2010, Quality of the log-geometric distribution extrapolation for smaller undiscovered oil and gas pool size: Natural Resources Research, v. 19, no. 1, p. 11-21, https://doi.org/10.1007/s11053-010-9109-x.","startPage":"11","endPage":"21","numberOfPages":"11","costCenters":[],"links":[{"id":216929,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/s11053-010-9109-x"},{"id":244831,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"19","issue":"1","noUsgsAuthors":false,"publicationDate":"2010-01-27","publicationStatus":"PW","scienceBaseUri":"505a9143e4b0c8380cd8019f","contributors":{"authors":[{"text":"Chenglin, L.","contributorId":90959,"corporation":false,"usgs":true,"family":"Chenglin","given":"L.","email":"","affiliations":[],"preferred":false,"id":443774,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Charpentier, Ronald R.","contributorId":33674,"corporation":false,"usgs":true,"family":"Charpentier","given":"Ronald R.","affiliations":[],"preferred":false,"id":443773,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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