{"pageNumber":"1182","pageRowStart":"29525","pageSize":"25","recordCount":165309,"records":[{"id":70148590,"text":"70148590 - 2015 - Nest-site selection and reproductive success of greater sage-grouse in a fire-affected habitat of northwestern Nevada","interactions":[],"lastModifiedDate":"2016-04-13T12:38:01","indexId":"70148590","displayToPublicDate":"2015-06-17T12:00:00","publicationYear":"2015","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":"Nest-site selection and reproductive success of greater sage-grouse in a fire-affected habitat of northwestern Nevada","docAbstract":"<p><span>Identifying links between micro-habitat selection and wildlife reproduction is imperative to population persistence and recovery. This information is particularly important for landscape species such as greater sage-grouse (</span><i>Centrocercus urophasianus</i><span>; sage-grouse). Although this species has been widely studied, because environmental factors can affect sage-grouse populations, local and regional studies are crucial for developing viable conservation strategies. We studied the habitat-use patterns of 71 radio-marked sage-grouse inhabiting an area affected by wildfire in the Virginia Mountains of northwestern Nevada during 2009&ndash;2011 to determine the effect of micro-habitat attributes on reproductive success. We measured standard vegetation parameters at nest and random sites using a multi-scale approach (range&thinsp;=&thinsp;0.01&ndash;15,527&thinsp;ha). We used an information-theoretic modeling approach to identify environmental factors influencing nest-site selection and survival, and determine whether nest survival was a function of resource selection. Sage-grouse selected micro-sites with greater shrub canopy cover and less cheatgrass (</span><i>Bromus tectorum</i><span>) cover than random sites. Total shrub canopy, including sagebrush (</span><i>Artemisia</i><span>&nbsp;spp.) and other shrub species, at small spatial scales (0.8&thinsp;ha and 3.1&thinsp;ha) was the single contributing selection factor to higher nest survival. These results indicate that reducing the risk of wildfire to maintain important sagebrush habitats could be emphasized in sage-grouse conservation strategies in Nevada. Managers may seek to mitigate the influx of annual grass invasion by preserving large intact sagebrush-dominated stands with a mixture of other shrub species. For this area of Nevada, the results suggest that &ge;40% total shrub canopy cover in sage-grouse nesting areas could yield improved reproductive success.&nbsp;</span></p>","language":"English","publisher":"Wildlife Society","doi":"10.1002/jwmg.899","usgsCitation":"Lockyer, Z.B., Coates, P.S., Casazza, M.L., Espinosa, S., and Delehanty, D., 2015, Nest-site selection and reproductive success of greater sage-grouse in a fire-affected habitat of northwestern Nevada: Journal of Wildlife Management, v. 79, no. 5, p. 785-797, https://doi.org/10.1002/jwmg.899.","productDescription":"13 p.","startPage":"785","endPage":"797","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-043230","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":301275,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Nevada","otherGeospatial":"Virginia Mountains","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -119.56558227539062,\n              39.90973623453719\n            ],\n            [\n              -119.65484619140625,\n              39.86231722624386\n            ],\n            [\n              -119.77157592773436,\n              39.94238358098156\n            ],\n            [\n              -119.79629516601562,\n              39.929747745342944\n            ],\n            [\n              -119.73999023437499,\n              39.871803651624425\n            ],\n            [\n              -119.77981567382812,\n              39.83174093314558\n            ],\n            [\n              -119.81689453125,\n              39.83490462943255\n            ],\n            [\n              -119.86495971679686,\n 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Peter S. 0000-0003-2672-9994 pcoates@usgs.gov","orcid":"https://orcid.org/0000-0003-2672-9994","contributorId":3263,"corporation":false,"usgs":true,"family":"Coates","given":"Peter","email":"pcoates@usgs.gov","middleInitial":"S.","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":true,"id":548781,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Casazza, Michael L. 0000-0002-5636-735X mike_casazza@usgs.gov","orcid":"https://orcid.org/0000-0002-5636-735X","contributorId":2091,"corporation":false,"usgs":true,"family":"Casazza","given":"Michael","email":"mike_casazza@usgs.gov","middleInitial":"L.","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":true,"id":548779,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Espinosa, Shawn","contributorId":20253,"corporation":false,"usgs":true,"family":"Espinosa","given":"Shawn","affiliations":[],"preferred":false,"id":548782,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Delehanty, David J.","contributorId":86683,"corporation":false,"usgs":true,"family":"Delehanty","given":"David J.","affiliations":[],"preferred":false,"id":548783,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70148593,"text":"70148593 - 2015 - Weathering and transport of chromium and nickel from serpentinite in the Coast Range ophiolite to the Sacramento Valley, California, USA","interactions":[],"lastModifiedDate":"2015-06-17T11:06:53","indexId":"70148593","displayToPublicDate":"2015-06-17T12:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":835,"text":"Applied Geochemistry","active":true,"publicationSubtype":{"id":10}},"title":"Weathering and transport of chromium and nickel from serpentinite in the Coast Range ophiolite to the Sacramento Valley, California, USA","docAbstract":"<p><span>A soil geochemical study in northern California was done to investigate the role that weathering and transport play in the regional distribution and mobility of geogenic Cr and Ni, which are both potentially toxic and carcinogenic. These elements are enriched in ultramafic rocks (primarily serpentinite) and the soils derived from them (1700&ndash;10,000&nbsp;mg Cr per kg soil and 1300&ndash;3900&nbsp;mg Ni per kg soil) in the Coast Range ophiolite. Chromium and Ni have been transported eastward from the Coast Range into the western Sacramento Valley and as a result, valley soil is enriched in Cr (80&ndash;1420&nbsp;mg&nbsp;kg</span><sup>&minus;1</sup><span>) and Ni (65&ndash;224&nbsp;mg&nbsp;kg</span><sup>&minus;1</sup><span>) compared to median values of U.S. soils of 50 and 15&nbsp;mg&nbsp;kg</span><sup>&minus;1</sup><span>, respectively. Nickel in ultramafic source rocks and soils is present in serpentine minerals (lizardite, antigorite, and chrysotile) and is more easily weathered compared to Cr, which primarily resides in highly refractory chromite ([Mg,Fe</span><sup>2+</sup><span>][Cr</span><sup>3+</sup><span>,Al,Fe</span><sup>3+</sup><span>]</span><sub>2</sub><span>O</span><sub>4</sub><span>). Although the majority of Cr and Ni in soils are in refractory chromite and serpentine minerals, the etching and dissolution of these minerals, presence of Cr- and Ni-enriched clay minerals and development of nanocrystalline Fe (hydr)oxides is evidence that a significant fractions of these elements have been transferred to potentially more labile phases.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.apgeochem.2015.05.018","usgsCitation":"Morrison, J.M., Goldhaber, M.B., Mills, C., Breit, G.N., Hooper, R.L., Holloway, J.M., Diehl, S.F., and Ranville, J.F., 2015, Weathering and transport of chromium and nickel from serpentinite in the Coast Range ophiolite to the Sacramento Valley, California, USA: Applied Geochemistry, v. 62, p. 72-86, https://doi.org/10.1016/j.apgeochem.2015.05.018.","productDescription":"15 p.","startPage":"72","endPage":"86","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-033273","costCenters":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"links":[{"id":301274,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Sacramento Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -122.48657226562499,\n              37.68382032669382\n            ],\n            [\n              -119.5751953125,\n              38.71980474264239\n            ],\n            [\n              -119.981689453125,\n              38.93377552819722\n            ],\n            [\n              -120.0146484375,\n              39.64799732373418\n            ],\n            [\n              -123.71704101562499,\n              38.882481197550774\n            ],\n      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mgold@usgs.gov","orcid":"https://orcid.org/0000-0002-1785-4243","contributorId":1339,"corporation":false,"usgs":true,"family":"Goldhaber","given":"Martin","email":"mgold@usgs.gov","middleInitial":"B.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true},{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":548796,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mills, Christopher T. cmills@usgs.gov","contributorId":141191,"corporation":false,"usgs":true,"family":"Mills","given":"Christopher T.","email":"cmills@usgs.gov","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":false,"id":548791,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Breit, George N. 0000-0003-2188-6798 gbreit@usgs.gov","orcid":"https://orcid.org/0000-0003-2188-6798","contributorId":1480,"corporation":false,"usgs":true,"family":"Breit","given":"George","email":"gbreit@usgs.gov","middleInitial":"N.","affiliations":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true},{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":548793,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Hooper, Robert L.","contributorId":141193,"corporation":false,"usgs":false,"family":"Hooper","given":"Robert","email":"","middleInitial":"L.","affiliations":[{"id":13710,"text":"Univ of Wisconsin-Eau claire","active":true,"usgs":false}],"preferred":false,"id":548798,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Holloway, JoAnn M. 0000-0003-3603-7668 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Golden","active":true,"usgs":false}],"preferred":false,"id":548797,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":70148574,"text":"70148574 - 2015 - Documentation of mountain lions in Marin County, California, 2010–2013","interactions":[],"lastModifiedDate":"2016-08-10T10:55:54","indexId":"70148574","displayToPublicDate":"2015-06-17T11:45:00","publicationYear":"2015","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1153,"text":"California Fish and Game","active":true,"publicationSubtype":{"id":10}},"title":"Documentation of mountain lions in Marin County, California, 2010–2013","docAbstract":"<p>Prior to 2010, mountain lions (<i>Puma concolor</i>) have rarely been documented in Marin County, California. Although there are reports of sightings of mountain lions or observations of mountain lion sign, most have not been verified by photographs or physical samples.&nbsp;Beginning in 2010, we conducted a pilot study of mountain lions in Marin County using motion-triggered cameras. Our objectives were to obtain additional documentations, confirm the presence of mountain lions outside of Point Reyes National Seashore, and determine if mountain lions had a regular presence in the county.&nbsp;</p>","language":"English","publisher":"California Department of Fish and Wildlife","usgsCitation":"Fifield, V.L., Rossi, A.J., and Boydston, E.E., 2015, Documentation of mountain lions in Marin County, California, 2010–2013: California Fish and Game, v. 101, no. 1, p. 66-71.","productDescription":"6 p.","startPage":"66","endPage":"71","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-054878","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":301273,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":301225,"type":{"id":15,"text":"Index Page"},"url":"https://www.wildlife.ca.gov/Publications/Journal/Contents"}],"country":"United 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eboydston@usgs.gov","orcid":"https://orcid.org/0000-0002-8452-835X","contributorId":1705,"corporation":false,"usgs":true,"family":"Boydston","given":"Erin","email":"eboydston@usgs.gov","middleInitial":"E.","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":true,"id":548684,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70148578,"text":"70148578 - 2015 - Geochemistry of magnetite from porphyry Cu and skarn deposits in the southwestern United States","interactions":[],"lastModifiedDate":"2015-06-17T10:48:24","indexId":"70148578","displayToPublicDate":"2015-06-17T11:45:00","publicationYear":"2015","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2746,"text":"Mineralium Deposita","active":true,"publicationSubtype":{"id":10}},"title":"Geochemistry of magnetite from porphyry Cu and skarn deposits in the southwestern United States","docAbstract":"<p><span>A combination of petrographic observations, laser ablation inductively coupled plasma mass spectrometry (LA-ICP-MS), and statistical data exploration was used in this study to determine compositional variations in hydrothermal and igneous magnetite from five porphyry Cu&ndash;Mo and skarn deposits in the southwestern United States, and igneous magnetite from the unmineralized, granodioritic Inner Zone Batholith, Japan. The most important overall discriminators for the minor and trace element chemistry of magnetite from the investigated porphyry and skarn deposits are Mg, Al, Ti, V, Mn, Co, Zn, and Ga&mdash;of these the elements with the highest variance for (I) igneous magnetite are Mg, Al, Ti, V, Mn, Zn, for (II) hydrothermal porphyry magnetite are Mg, Ti, V, Mn, Co, Zn, and for (III) hydrothermal skarn magnetite are Mg, Ti, Mn, Zn, and Ga. Nickel could only be detected at levels above the limit of reporting (LOR) in two igneous magnetites. Equally, Cr could only be detected in one igneous occurrence. Copper, As, Mo, Ag, Au, and Pb have been reported in magnetite by other authors but could not be detected at levels greater than their respective LORs in our samples. Comparison with the chemical signature of igneous magnetite from the barren Inner Zone Batholith, Japan, suggests that V, Mn, Co, and Ga concentrations are relatively depleted in magnetite from the porphyry and skarn deposits. Higher formation conditions in combination with distinct differences between melt and hydrothermal fluid compositions are reflected in Al, Ti, V, and Ga concentrations that are, on average, higher in igneous magnetite than in hydrothermal magnetite (including porphyry and skarn magnetite). Low Ti and V concentrations in combination with high Mn concentrations are characteristic features of magnetite from skarn deposits. High Mg concentrations (&lt;1,000&nbsp;ppm) are characteristic for magnetite from magnesian skarn and likely reflect extensive fluid/rock interaction. In porphyry deposits, hydrothermal magnetite from different vein types can be distinguished by varying Ti, V, Mn, and Zn contents. Titanium and V concentrations are highly variable among hydrothermal and igneous magnetites, but Ti concentrations above 3,560&nbsp;ppm could only be detected in igneous magnetite, and V concentrations are on average lower in hydrothermal magnetite. The highest Ti concentrations are present in igneous magnetite from gabbro and monzonite. The lowest Ti concentrations were recorded in igneous magnetite from granodiorite and granodiorite breccia and largely overlap with Ti concentrations found in hydrothermal porphyry magnetite. Magnesium and Mn concentrations vary between magnetite from different skarn deposits but are generally greater than in hydrothermal magnetite from the porphyry deposits. High Mg, and low Ti and V concentrations characterize hydrothermal magnetite from magnesian skarn deposits and follow a trend that indicates that magnetite from skarn (calcic and magnesian) commonly has low Ti and V concentrations.</span></p>","language":"English","publisher":"Springer","doi":"10.1007/s00126-014-0539-y","usgsCitation":"Nadoll, P., Mauk, J.L., LeVeille, R.A., and Koenig, A.E., 2015, Geochemistry of magnetite from porphyry Cu and skarn deposits in the southwestern United States: Mineralium Deposita, v. 50, no. 4, p. 493-515, https://doi.org/10.1007/s00126-014-0539-y.","productDescription":"23 p.","startPage":"493","endPage":"515","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-045865","costCenters":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"links":[{"id":301272,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Arizona, New Mexico","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -110.9619140625,\n              32.91648534731439\n            ],\n            [\n              -110.9619140625,\n              34.56085936708384\n            ],\n            [\n              -106.8310546875,\n              34.56085936708384\n            ],\n            [\n              -106.8310546875,\n              32.91648534731439\n            ],\n            [\n              -110.9619140625,\n              32.91648534731439\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"50","issue":"4","publishingServiceCenter":{"id":2,"text":"Denver PSC"},"noUsgsAuthors":false,"publicationDate":"2014-08-23","publicationStatus":"PW","scienceBaseUri":"55828c22e4b023124e8f3fa4","contributors":{"authors":[{"text":"Nadoll, Patrick","contributorId":106407,"corporation":false,"usgs":true,"family":"Nadoll","given":"Patrick","affiliations":[],"preferred":false,"id":548710,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mauk, Jeffrey L. 0000-0002-6244-2774 jmauk@usgs.gov","orcid":"https://orcid.org/0000-0002-6244-2774","contributorId":4101,"corporation":false,"usgs":true,"family":"Mauk","given":"Jeffrey","email":"jmauk@usgs.gov","middleInitial":"L.","affiliations":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":548709,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"LeVeille, Richard A.","contributorId":141177,"corporation":false,"usgs":false,"family":"LeVeille","given":"Richard","email":"","middleInitial":"A.","affiliations":[{"id":13705,"text":"Freeport McMoRan Copper & Gold Inc.","active":true,"usgs":false}],"preferred":false,"id":548711,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Koenig, Alan E. 0000-0002-5230-0924 akoenig@usgs.gov","orcid":"https://orcid.org/0000-0002-5230-0924","contributorId":1564,"corporation":false,"usgs":true,"family":"Koenig","given":"Alan","email":"akoenig@usgs.gov","middleInitial":"E.","affiliations":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":548712,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70148581,"text":"70148581 - 2015 - Observations of two non-native snake species in the same remote area of southern Florida","interactions":[],"lastModifiedDate":"2015-06-17T10:35:43","indexId":"70148581","displayToPublicDate":"2015-06-17T11:30:00","publicationYear":"2015","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1951,"text":"IRCF Reptiles & Amphibians","active":true,"publicationSubtype":{"id":10}},"title":"Observations of two non-native snake species in the same remote area of southern Florida","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"IRCF","usgsCitation":"Hanslowe, E., Falk, B.G., McEachern, M., and Reed, R., 2015, Observations of two non-native snake species in the same remote area of southern Florida: IRCF Reptiles & Amphibians, v. 22, no. 2, p. 90-92.","productDescription":"3 p.","startPage":"90","endPage":"92","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-065582","costCenters":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"links":[{"id":301270,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":301239,"type":{"id":15,"text":"Index Page"},"url":"https://www.ircf.org/journal/volume-22-no-2-june/"}],"country":"United States","state":"Florida","county":"Collier County","otherGeospatial":"Big Cypress National Preserve","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -81.3262939453125,\n              25.606855993715016\n            ],\n            [\n              -81.3262939453125,\n              26.22937459341778\n            ],\n            [\n              -80.85113525390625,\n              26.22937459341778\n            ],\n            [\n              -80.85113525390625,\n              25.606855993715016\n            ],\n            [\n              -81.3262939453125,\n              25.606855993715016\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"22","issue":"2","publishingServiceCenter":{"id":2,"text":"Denver PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"55828c22e4b023124e8f3fac","contributors":{"authors":[{"text":"Hanslowe, Emma B.","contributorId":141178,"corporation":false,"usgs":false,"family":"Hanslowe","given":"Emma B.","affiliations":[{"id":12557,"text":"University of Florida, FLREC","active":true,"usgs":false}],"preferred":false,"id":548739,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Falk, Bryan G. bfalk@usgs.gov","contributorId":141179,"corporation":false,"usgs":true,"family":"Falk","given":"Bryan","email":"bfalk@usgs.gov","middleInitial":"G.","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":false,"id":548740,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McEachern, Michelle A. mmceachern@usgs.gov","contributorId":5539,"corporation":false,"usgs":true,"family":"McEachern","given":"Michelle A.","email":"mmceachern@usgs.gov","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":true,"id":548741,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Reed, Robert N. reedr@usgs.gov","contributorId":141036,"corporation":false,"usgs":true,"family":"Reed","given":"Robert N.","email":"reedr@usgs.gov","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":false,"id":548738,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70148582,"text":"70148582 - 2015 - Running a network on a shoestring: the Global Invasive Species Information Network","interactions":[],"lastModifiedDate":"2018-08-10T16:26:52","indexId":"70148582","displayToPublicDate":"2015-06-17T11:30:00","publicationYear":"2015","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2655,"text":"Management of Biological Invasions","active":true,"publicationSubtype":{"id":10}},"title":"Running a network on a shoestring: the Global Invasive Species Information Network","docAbstract":"<p>The Global Invasive Species Information Network (GISIN) was conceptualized in 2004 to aggregate and disseminate invasive species data in a standardized way. A decade later the GISIN community has implemented a data portal and three of six GISIN data aggregation models in the GISIN data exchange Protocol, including invasive species status information, resource URLs, and occurrence data. The portal is based on a protocol developed by representatives from 15 countries and 27 organizations of the global invasive species information management community. The GISIN has 19 data providers sharing 34,343 species status records, 1,693,073 occurrences, and 15,601 resource URLs. While the GISIN's goal is to be global, much of its data and funding are provided by the United States. Several initiatives use the GISIN as their information backbone, such as the Great Lakes Early Detection Network (GLEDN) and the North American Invasive Species Network (NAISN). Here we share several success stories and organizational challenges that remain.</p>","language":"English","publisher":"The Regional Euro-Asian Biological Invasions Centre","doi":"10.3391/mbi.2015.6.2.04","usgsCitation":"Jarnevich, C.S., Simpson, A., Graham, J.J., Newman, G.J., and Bargeron, C.T., 2015, Running a network on a shoestring: the Global Invasive Species Information Network: Management of Biological Invasions, v. 6, no. 2, p. 137-146, https://doi.org/10.3391/mbi.2015.6.2.04.","productDescription":"10 p.","startPage":"137","endPage":"146","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-061163","costCenters":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true},{"id":37226,"text":"Core Science Analytics, Synthesis, and Libraries","active":true,"usgs":true}],"links":[{"id":472009,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.3391/mbi.2015.6.2.04","text":"Publisher Index Page"},{"id":301269,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"6","issue":"2","publishingServiceCenter":{"id":2,"text":"Denver PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"55828c23e4b023124e8f3fb0","contributors":{"authors":[{"text":"Jarnevich, Catherine S. 0000-0002-9699-2336 jarnevichc@usgs.gov","orcid":"https://orcid.org/0000-0002-9699-2336","contributorId":3424,"corporation":false,"usgs":true,"family":"Jarnevich","given":"Catherine","email":"jarnevichc@usgs.gov","middleInitial":"S.","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":true,"id":548742,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Simpson, Annie 0000-0001-8338-5134 asimpson@usgs.gov","orcid":"https://orcid.org/0000-0001-8338-5134","contributorId":127,"corporation":false,"usgs":true,"family":"Simpson","given":"Annie","email":"asimpson@usgs.gov","affiliations":[{"id":208,"text":"Core Science Analytics and Synthesis","active":true,"usgs":true}],"preferred":true,"id":548743,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Graham, James J","contributorId":141180,"corporation":false,"usgs":false,"family":"Graham","given":"James","email":"","middleInitial":"J","affiliations":[{"id":7067,"text":"Humboldt State University","active":true,"usgs":false}],"preferred":false,"id":548744,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Newman, Gregory J.","contributorId":19487,"corporation":false,"usgs":true,"family":"Newman","given":"Gregory","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":548745,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Bargeron, Chuck T.","contributorId":141181,"corporation":false,"usgs":false,"family":"Bargeron","given":"Chuck","email":"","middleInitial":"T.","affiliations":[{"id":12697,"text":"University of Georgia","active":true,"usgs":false}],"preferred":false,"id":548746,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70148580,"text":"70148580 - 2015 - The role of benefit transfer in ecosystem service valuation","interactions":[],"lastModifiedDate":"2015-06-17T10:38:18","indexId":"70148580","displayToPublicDate":"2015-06-17T11:30:00","publicationYear":"2015","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1453,"text":"Ecological Economics","active":true,"publicationSubtype":{"id":10}},"title":"The role of benefit transfer in ecosystem service valuation","docAbstract":"<p><span>The demand for timely monetary estimates of the economic value of nonmarket ecosystem goods and services has steadily increased over the last few decades. This article describes the use of benefit transfer to generate monetary value estimates of ecosystem services specifically. The article provides guidance for conducting such benefit transfers and summarizes advancements in benefit transfer methods, databases and analysis tools designed to facilitate its application.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.ecolecon.2014.02.018","usgsCitation":"Richardson, L.A., Loomis, J., Kroeger, T., and Casey, F., 2015, The role of benefit transfer in ecosystem service valuation: Ecological Economics, v. 115, p. 51-58, https://doi.org/10.1016/j.ecolecon.2014.02.018.","productDescription":"8 p.","startPage":"51","endPage":"58","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-051458","costCenters":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"links":[{"id":301271,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"115","publishingServiceCenter":{"id":2,"text":"Denver PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"55828c25e4b023124e8f3fb4","contributors":{"authors":[{"text":"Richardson, Leslie A. lrichardson@usgs.gov","contributorId":4810,"corporation":false,"usgs":true,"family":"Richardson","given":"Leslie","email":"lrichardson@usgs.gov","middleInitial":"A.","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":true,"id":548734,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Loomis, John","contributorId":60746,"corporation":false,"usgs":true,"family":"Loomis","given":"John","affiliations":[],"preferred":false,"id":548735,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kroeger, Timm","contributorId":17165,"corporation":false,"usgs":true,"family":"Kroeger","given":"Timm","affiliations":[],"preferred":false,"id":548737,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Casey, Frank ccasey@usgs.gov","contributorId":95821,"corporation":false,"usgs":true,"family":"Casey","given":"Frank","email":"ccasey@usgs.gov","affiliations":[],"preferred":false,"id":548799,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70148589,"text":"70148589 - 2015 - Effects of the environmental estrogenic contaminants bisphenol A and 17α-ethinyl estradiol on sexual development and adult behaviors in aquatic wildlife species","interactions":[],"lastModifiedDate":"2018-09-04T15:53:31","indexId":"70148589","displayToPublicDate":"2015-06-17T11:15:00","publicationYear":"2015","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1738,"text":"General and Comparative Endocrinology","active":true,"publicationSubtype":{"id":10}},"title":"Effects of the environmental estrogenic contaminants bisphenol A and 17α-ethinyl estradiol on sexual development and adult behaviors in aquatic wildlife species","docAbstract":"<p>Endocrine<span>&nbsp;disrupting chemicals (</span>EDCs<span>), including the mass-produced component of plastics, bisphenol A (BPA) are widely prevalent in aquatic and terrestrial habitats. Many aquatic species, such as fish, amphibians, aquatic reptiles and mammals, are exposed daily to high concentrations of BPA and&nbsp;</span>ethinyl estradiol<span>&nbsp;(EE2),&nbsp;</span>estrogen<span>&nbsp;in birth control pills. In this review, we will predominantly focus on BPA and EE2, well-described estrogenic EDCs. First, the evidence that BPA and EE2 are detectable in almost all bodies of water will be discussed. We will consider how BPA affects sexual and neural development in these species, as these effects have been the best characterized across taxa. For instance, such chemicals have been in many cases reported to cause sex-reversal of males to females. Even if these chemicals do not overtly alter the gonadal sex, there are indications that several EDCs might demasculinize male-specific behaviors that are essential for attracting a mate. In so doing, these chemicals may reduce the likelihood that these males reproduce. If exposed males do reproduce, the concern is that they will then be passing on compromised genetic fitness to their offspring and transmitting potential transgenerational effects through their sperm&nbsp;</span>epigenome<span>. We will thus consider how diverse epigenetic changes might be a unifying mechanism of how BPA and EE2 disrupt several processes across species. Such changes might also serve as universal species diagnostic biomarkers of BPA and other EDCs exposure. Lastly, the evidence that estrogenic EDCs-induced effects in aquatic species might translate to humans will be considered.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.ygcen.2014.09.014","usgsCitation":"Bhandari, R.K., Deem, S.L., Holliday, D.K., Jandegian, C.M., Kassotis, C., Nagel, S., Tillitt, D.E., vom Saal, F., and Rosenfeld, C.S., 2015, Effects of the environmental estrogenic contaminants bisphenol A and 17α-ethinyl estradiol on sexual development and adult behaviors in aquatic wildlife species: General and Comparative Endocrinology, v. 214, p. 195-214, https://doi.org/10.1016/j.ygcen.2014.09.014.","productDescription":"20 p.","startPage":"195","endPage":"214","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-056661","costCenters":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true},{"id":34983,"text":"Contaminant Biology Program","active":true,"usgs":true}],"links":[{"id":301268,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"214","publishingServiceCenter":{"id":4,"text":"Rolla PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"55828c21e4b023124e8f3f9e","contributors":{"authors":[{"text":"Bhandari, Ramji K. rbhandari@usgs.gov","contributorId":5930,"corporation":false,"usgs":true,"family":"Bhandari","given":"Ramji","email":"rbhandari@usgs.gov","middleInitial":"K.","affiliations":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"preferred":true,"id":548771,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Deem, Sharon L.","contributorId":139277,"corporation":false,"usgs":false,"family":"Deem","given":"Sharon","email":"","middleInitial":"L.","affiliations":[{"id":12719,"text":"Whitney R. Harris, World Ecology Center, Uni. of Missouri St. Louis","active":true,"usgs":false}],"preferred":false,"id":548772,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Holliday, Dawn K.","contributorId":141187,"corporation":false,"usgs":false,"family":"Holliday","given":"Dawn","email":"","middleInitial":"K.","affiliations":[{"id":13706,"text":"University of Missouri-Columbia","active":true,"usgs":false}],"preferred":false,"id":548773,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Jandegian, Caitlin M. cjandegian@usgs.gov","contributorId":5941,"corporation":false,"usgs":true,"family":"Jandegian","given":"Caitlin","email":"cjandegian@usgs.gov","middleInitial":"M.","affiliations":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"preferred":true,"id":548774,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Kassotis, Christopher D.","contributorId":26967,"corporation":false,"usgs":true,"family":"Kassotis","given":"Christopher D.","affiliations":[],"preferred":false,"id":548775,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Nagel, Susan C.","contributorId":56147,"corporation":false,"usgs":true,"family":"Nagel","given":"Susan C.","affiliations":[],"preferred":false,"id":548776,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Tillitt, Donald E. 0000-0002-8278-3955 dtillitt@usgs.gov","orcid":"https://orcid.org/0000-0002-8278-3955","contributorId":1875,"corporation":false,"usgs":true,"family":"Tillitt","given":"Donald","email":"dtillitt@usgs.gov","middleInitial":"E.","affiliations":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"preferred":true,"id":548770,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"vom Saal, Frederick S.","contributorId":17488,"corporation":false,"usgs":true,"family":"vom Saal","given":"Frederick S.","affiliations":[],"preferred":false,"id":548777,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Rosenfeld, Cheryl S.","contributorId":141188,"corporation":false,"usgs":false,"family":"Rosenfeld","given":"Cheryl","email":"","middleInitial":"S.","affiliations":[{"id":13706,"text":"University of Missouri-Columbia","active":true,"usgs":false}],"preferred":false,"id":548778,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}}
,{"id":70148583,"text":"70148583 - 2015 - Incorporating climate change projections into riparian restoration planning and design","interactions":[],"lastModifiedDate":"2015-08-03T10:24:52","indexId":"70148583","displayToPublicDate":"2015-06-17T11:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1447,"text":"Ecohydrology","active":true,"publicationSubtype":{"id":10}},"title":"Incorporating climate change projections into riparian restoration planning and design","docAbstract":"<div class=\"para\">\n<p>Climate change and associated changes in streamflow may alter riparian habitats substantially in coming decades. Riparian restoration provides opportunities to respond proactively to projected climate change effects, increase riparian ecosystem resilience to climate change, and simultaneously address effects of both climate change and other human disturbances. However, climate change may alter which restoration methods are most effective and which restoration goals can be achieved. Incorporating climate change into riparian restoration planning and design is critical to long-term restoration of desired community composition and ecosystem services.</p>\n</div>\n<div class=\"para\">\n<p>In this review, we discuss and provide examples of how climate change might be incorporated into restoration planning at the key stages of assessing the project context, establishing restoration goals and design criteria, evaluating design alternatives, and monitoring restoration outcomes. Restoration planners have access to numerous tools to predict future climate, streamflow, and riparian ecology at restoration sites. Planners can use those predictions to assess which species or ecosystem services will be most vulnerable under future conditions, and which sites will be most suitable for restoration. To accommodate future climate and streamflow change, planners may need to adjust methods for planting, invasive species control, channel and floodplain reconstruction, and water management. Given the considerable uncertainty in future climate and streamflow projections, riparian ecological responses, and effects on restoration outcomes, planners will need to consider multiple potential future scenarios, implement a variety of restoration methods, design projects with flexibility to adjust to future conditions, and plan to respond adaptively to unexpected change.</p>\n</div>","language":"English","publisher":"Wiley","doi":"10.1002/eco.1645","usgsCitation":"Perry, L., Reynolds, L.V., Beechie, T.J., Collins, M.J., and Shafroth, P.B., 2015, Incorporating climate change projections into riparian restoration planning and design: Ecohydrology, v. 8, no. 5, p. 863-879, https://doi.org/10.1002/eco.1645.","productDescription":"17 p.","startPage":"863","endPage":"879","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-065479","costCenters":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"links":[{"id":301266,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"8","issue":"5","publishingServiceCenter":{"id":2,"text":"Denver PSC"},"noUsgsAuthors":false,"publicationDate":"2015-06-02","publicationStatus":"PW","scienceBaseUri":"55828c22e4b023124e8f3fa8","contributors":{"authors":[{"text":"Perry, Laura G.","contributorId":45565,"corporation":false,"usgs":true,"family":"Perry","given":"Laura G.","affiliations":[],"preferred":false,"id":548748,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reynolds, Lindsay V.","contributorId":141182,"corporation":false,"usgs":false,"family":"Reynolds","given":"Lindsay","email":"","middleInitial":"V.","affiliations":[{"id":6737,"text":"Colorado State University, Department of Ecosystem Science and Sustainability, and Natural Resource Ecology Laboratory","active":true,"usgs":false}],"preferred":false,"id":548749,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"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":548750,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Collins, Mathias J.","contributorId":19086,"corporation":false,"usgs":true,"family":"Collins","given":"Mathias","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":548751,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Shafroth, Patrick B. 0000-0002-6064-871X shafrothp@usgs.gov","orcid":"https://orcid.org/0000-0002-6064-871X","contributorId":2000,"corporation":false,"usgs":true,"family":"Shafroth","given":"Patrick","email":"shafrothp@usgs.gov","middleInitial":"B.","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":true,"id":548747,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70148592,"text":"70148592 - 2015 - Darcy’s law predicts widespread forest mortality under climate warming","interactions":[],"lastModifiedDate":"2018-01-12T13:13:00","indexId":"70148592","displayToPublicDate":"2015-06-17T11:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2841,"text":"Nature Climate Change","onlineIssn":"1758-6798","printIssn":"1758-678X","active":true,"publicationSubtype":{"id":10}},"title":"Darcy’s law predicts widespread forest mortality under climate warming","docAbstract":"<p><span>Drought and heat-induced tree mortality is accelerating in many forest biomes as a consequence of a warming climate, resulting in a threat to global forests unlike any in recorded history</span><span>. Forests store the majority of terrestrial carbon, thus their loss may have significant and sustained impacts on the global carbon cycle</span><span>. We use a hydraulic corollary to Darcy</span><span class=\"mb\">’</span><span>s law, a core principle of vascular plant physiology</span><span>, to predict characteristics of plants that will survive and die during drought under warmer future climates. Plants that are tall with isohydric stomatal regulation, low hydraulic conductance, and high leaf area are most likely to die from future drought stress. Thus, tall trees of old-growth forests are at the greatest risk of loss, which has ominous implications for terrestrial carbon storage. This application of Darcy</span><span class=\"mb\">’</span><span>s law indicates today</span><span class=\"mb\">’</span><span>s forests generally should be replaced by shorter and more xeric plants, owing to future warmer droughts and associated wildfires and pest attacks. The Darcy</span><span class=\"mb\">’</span><span>s corollary also provides a simple, robust framework for informing forest management interventions needed to promote the survival of current forests. Given the robustness of Darcy</span><span class=\"mb\">’</span><span>s law for predictions of vascular plant function, we conclude with high certainty that today</span><span class=\"mb\">’</span><span>s forests are going to be subject to continued increases in mortality rates that will result in substantial reorganization of their structure and carbon storage.</span></p>","language":"English","publisher":"Nature Publishing Group","doi":"10.1038/nclimate2641","usgsCitation":"McDowell, N.G., and Allen, C.D., 2015, Darcy’s law predicts widespread forest mortality under climate warming: Nature Climate Change, v. 5, p. 669-672, https://doi.org/10.1038/nclimate2641.","productDescription":"4 p.","startPage":"669","endPage":"672","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-058456","costCenters":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"links":[{"id":301265,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"5","publishingServiceCenter":{"id":2,"text":"Denver PSC"},"noUsgsAuthors":false,"publicationDate":"2015-05-18","publicationStatus":"PW","scienceBaseUri":"55828c20e4b023124e8f3f98","contributors":{"authors":[{"text":"McDowell, Nate G.","contributorId":46839,"corporation":false,"usgs":true,"family":"McDowell","given":"Nate","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":548788,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Allen, Craig D. 0000-0002-8777-5989 craig_allen@usgs.gov","orcid":"https://orcid.org/0000-0002-8777-5989","contributorId":2597,"corporation":false,"usgs":true,"family":"Allen","given":"Craig","email":"craig_allen@usgs.gov","middleInitial":"D.","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true},{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true}],"preferred":true,"id":548787,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70150427,"text":"70150427 - 2015 - Two tickets to paradise: multiple dispersal events in the founding of hoary bat populations in Hawai'i","interactions":[],"lastModifiedDate":"2018-01-04T12:43:36","indexId":"70150427","displayToPublicDate":"2015-06-17T11:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2980,"text":"PLoS ONE","active":true,"publicationSubtype":{"id":10}},"title":"Two tickets to paradise: multiple dispersal events in the founding of hoary bat populations in Hawai'i","docAbstract":"<p>The Hawaiian islands are an extremely isolated oceanic archipelago, and their fauna has long served as models of dispersal in island biogeography. While molecular data have recently been applied to investigate the timing and origin of dispersal events for several animal groups including birds, insects, and snails, these questions have been largely unaddressed in Hawai'i's only native terrestrial mammal, the Hawaiian hoary bat, <i>Lasiurus cinereus semotus</i>. Here, we use molecular data to test the hypotheses that (1) Hawaiian <i>L</i>. <i>c</i>. <i>semotus</i> originated via dispersal from North American populations of <i>L</i>. <i>c</i>. <i>cinereus</i> rather than from South American <i>L</i>. <i>c</i>. <i>villosissimus</i>, and (2) modern Hawaiian populations were founded from a single dispersal event. Contrary to the latter hypothesis, our mitochondrial data support a biogeographic history of multiple, relatively recent dispersals of hoary bats from North America to the Hawaiian islands. Coalescent demographic analyses of multilocus data suggest that modern populations of Hawaiian hoary bats were founded no more than 10 kya. Our finding of multiple evolutionarily significant units in Hawai'i highlights information that should be useful for re-evaluation of the conservation status of hoary bats in Hawai'i.</p>","language":"English","publisher":"Public Library of Science","publisherLocation":"San Francisco, CA","doi":"10.1371/journal.pone.0127912","collaboration":"US Fish and Wildlife Service;\nHawaii Department of Forestry and Wildlife","usgsCitation":"Russell, A.L., Pinzari, C., Vonhof, M.J., Olival, K.J., and Bonaccorso, F., 2015, Two tickets to paradise: multiple dispersal events in the founding of hoary bat populations in Hawai'i: PLoS ONE, v. 6, no. 10, p. 1-13, https://doi.org/10.1371/journal.pone.0127912.","productDescription":"13 p.","startPage":"1","endPage":"13","numberOfPages":"13","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-064494","costCenters":[{"id":521,"text":"Pacific Island Ecosystems Research Center","active":false,"usgs":true}],"links":[{"id":472011,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1371/journal.pone.0127912","text":"Publisher Index Page"},{"id":305426,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"6","issue":"10","publishingServiceCenter":{"id":14,"text":"Menlo Park PSC"},"noUsgsAuthors":false,"publicationDate":"2015-06-17","publicationStatus":"PW","scienceBaseUri":"55925e5ae4b0b6d21dd6767b","contributors":{"authors":[{"text":"Russell, Amy L.","contributorId":143710,"corporation":false,"usgs":false,"family":"Russell","given":"Amy","email":"","middleInitial":"L.","affiliations":[{"id":15305,"text":"Grand Valley State University","active":true,"usgs":false}],"preferred":false,"id":556867,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pinzari, Corinna A.","contributorId":57359,"corporation":false,"usgs":true,"family":"Pinzari","given":"Corinna A.","affiliations":[],"preferred":false,"id":556868,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Vonhof, Maarten J.","contributorId":143711,"corporation":false,"usgs":false,"family":"Vonhof","given":"Maarten","email":"","middleInitial":"J.","affiliations":[{"id":15306,"text":"Western Michigan University","active":true,"usgs":false}],"preferred":false,"id":556869,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Olival, Kevin J.","contributorId":143712,"corporation":false,"usgs":false,"family":"Olival","given":"Kevin","email":"","middleInitial":"J.","affiliations":[{"id":7118,"text":"EcoHealth Alliance","active":true,"usgs":false}],"preferred":false,"id":556870,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Bonaccorso, Frank 0000-0002-5490-3083 fbonaccorso@usgs.gov","orcid":"https://orcid.org/0000-0002-5490-3083","contributorId":143709,"corporation":false,"usgs":true,"family":"Bonaccorso","given":"Frank","email":"fbonaccorso@usgs.gov","affiliations":[{"id":5049,"text":"Pacific Islands Ecosys Research Center","active":true,"usgs":true},{"id":521,"text":"Pacific Island Ecosystems Research Center","active":false,"usgs":true}],"preferred":true,"id":556866,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70146883,"text":"ofr20151079 - 2015 - Carbon dioxide storage in unconventional reservoirs workshop: summary of recommendations","interactions":[],"lastModifiedDate":"2015-06-17T09:31:13","indexId":"ofr20151079","displayToPublicDate":"2015-06-17T10:30:00","publicationYear":"2015","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2015-1079","title":"Carbon dioxide storage in unconventional reservoirs workshop: summary of recommendations","docAbstract":"<p>&ldquo;Unconventional reservoirs&rdquo; for carbon dioxide (CO<sub>2</sub>) storage&mdash;that is, geologic reservoirs in which changes to the rock trap CO<sub>2</sub>&nbsp;and therefore contribute to CO<sub>2</sub>&nbsp;storage&mdash;including coal, shale, basalt, and ultramafic rocks, were the focus of a U.S. Geological Survey (USGS) workshop held March 28 and 29, 2012, at the National Conservation Training Center in Shepherdstown, West Virginia. The goals of the workshop were to determine whether a detailed assessment of CO<sub>2</sub>&nbsp;storage capacity in unconventional reservoirs is warranted, and if so, to build a set of recommendations that could be used to develop a methodology to assess this storage capacity. Such an assessment would address only the technically available resource, independent of economic or policy factors. At the end of the workshop, participants agreed that sufficient knowledge exists to allow an assessment of the potential CO<sub>2</sub>&nbsp;storage resource in coals, organic-rich shales, and basalts. More work remains to be done before the storage resource in ultramafic rocks can be meaningfully assessed.</p>\n<p>In order to assess the CO<sub>2</sub>&nbsp;storage capacity of coals and organic-rich shales, the workshop participants agreed that the following several factors are key: sorption mechanisms and capacity, pore fluid composition and saturation, thermal maturity, formation thickness, and whether hydrocarbons have been extracted from the formation previously (for example, by enhanced gas or oil recovery).</p>\n<p>In order to assess the CO<sub>2</sub>&nbsp;storage capacity of basalts, the workshop participants agreed that key factors include temperature, pressure, pH, water chemistry, mineral chemistry, organic content, mineralogy, porosity, permeability, relative permeabilities, and CO<sub>2</sub>&nbsp;phase.</p>\n<p>The storage capacity for all unconventional reservoirs may be modeled using a volumetric equation starting with the extent of the rock unit and adjusted using these key factors and reaction terms. The ideas that were developed during this workshop can be used by USGS scientists to develop a methodology to assess the CO<sub>2</sub>&nbsp;storage resource in unconventional reservoirs. This methodology could then be released for public comment and peer review. After completing this development process, the USGS could then use the methodology to assess the CO<sub>2</sub>&nbsp;storage resource in unconventional reservoirs.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20151079","usgsCitation":"Jones, K.B., and Blondes, M., 2015, Carbon dioxide storage in unconventional reservoirs workshop: summary of recommendations: U.S. Geological Survey Open-File Report 2015-1079, iii, 10 p., https://doi.org/10.3133/ofr20151079.","productDescription":"iii, 10 p.","numberOfPages":"18","onlineOnly":"Y","additionalOnlineFiles":"N","ipdsId":"IP-059685","costCenters":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true}],"links":[{"id":301263,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2015/1079/pdf/ofr2015-1079.pdf","text":"Report","size":"213 KB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":301264,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr20151079.jpg"},{"id":301262,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2015/1079/"}],"publishingServiceCenter":{"id":9,"text":"Reston PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"55828c20e4b023124e8f3f96","contributors":{"authors":[{"text":"Jones, Kevin B. 0000-0002-6386-2623 kevinjones@usgs.gov","orcid":"https://orcid.org/0000-0002-6386-2623","contributorId":565,"corporation":false,"usgs":true,"family":"Jones","given":"Kevin","email":"kevinjones@usgs.gov","middleInitial":"B.","affiliations":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":545471,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Blondes, Madalyn S. 0000-0003-0320-0107 mblondes@usgs.gov","orcid":"https://orcid.org/0000-0003-0320-0107","contributorId":3598,"corporation":false,"usgs":true,"family":"Blondes","given":"Madalyn S.","email":"mblondes@usgs.gov","affiliations":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":545472,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70148337,"text":"ofr20151062 - 2015 - Framework for a hydrologic climate-response network in New England","interactions":[],"lastModifiedDate":"2015-06-17T09:22:03","indexId":"ofr20151062","displayToPublicDate":"2015-06-17T10:15:00","publicationYear":"2015","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2015-1062","title":"Framework for a hydrologic climate-response network in New England","docAbstract":"<p><span>Many climate-related hydrologic variables in New England have changed in the past century, and many are expected to change during the next century. It is important to understand and monitor these changes because they can affect human water supply, hydroelectric power generation, transportation infrastructure, and stream and riparian ecology. This report describes a framework for hydrologic monitoring in New England by means of a climate-response network. The framework identifies specific inland hydrologic variables that are sensitive to climate variation; identifies geographic regions with similar hydrologic responses; proposes a fixed-station monitoring network composed of existing streamflow, groundwater, lake ice, snowpack, and meteorological data-collection stations for evaluation of hydrologic response to climate variation; and identifies streamflow basins for intensive, process-based studies and for estimates of future hydrologic conditions.</span></p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20151062","usgsCitation":"Lent, R.M., Hodgkins, G.A., Dudley, R.W., and Schalk, L., 2015, Framework for a hydrologic climate-response network in New England: U.S. Geological Survey Open-File Report 2015-1062, v, 34 p., https://doi.org/10.3133/ofr20151062.","productDescription":"v, 34 p.","numberOfPages":"44","onlineOnly":"Y","additionalOnlineFiles":"N","ipdsId":"IP-058608","costCenters":[{"id":371,"text":"Maine Water Science Center","active":true,"usgs":true}],"links":[{"id":301259,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr20151062.jpg"},{"id":301243,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2015/1062/"},{"id":301258,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2015/1062/pdf/ofr2015-1062.pdf","text":"Report","size":"24.9 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"United States","state":"Conecticut, Maine, Massachusetts, New Hampshire, Rhode Island, Vermont","otherGeospatial":"New England","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n          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PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"55828c22e4b023124e8f3fa2","contributors":{"authors":[{"text":"Lent, Robert M. rmlent@usgs.gov","contributorId":284,"corporation":false,"usgs":true,"family":"Lent","given":"Robert","email":"rmlent@usgs.gov","middleInitial":"M.","affiliations":[{"id":371,"text":"Maine Water Science Center","active":true,"usgs":true}],"preferred":true,"id":548753,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hodgkins, Glenn A. 0000-0002-4916-5565 gahodgki@usgs.gov","orcid":"https://orcid.org/0000-0002-4916-5565","contributorId":2020,"corporation":false,"usgs":true,"family":"Hodgkins","given":"Glenn","email":"gahodgki@usgs.gov","middleInitial":"A.","affiliations":[{"id":371,"text":"Maine Water Science Center","active":true,"usgs":true},{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":548754,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dudley, Robert W. 0000-0002-0934-0568 rwdudley@usgs.gov","orcid":"https://orcid.org/0000-0002-0934-0568","contributorId":2223,"corporation":false,"usgs":true,"family":"Dudley","given":"Robert","email":"rwdudley@usgs.gov","middleInitial":"W.","affiliations":[{"id":371,"text":"Maine Water Science Center","active":true,"usgs":true},{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":548755,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Schalk, Luther 0000-0003-3957-1794 lschalk@usgs.gov","orcid":"https://orcid.org/0000-0003-3957-1794","contributorId":4366,"corporation":false,"usgs":true,"family":"Schalk","given":"Luther","email":"lschalk@usgs.gov","affiliations":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":548756,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70174031,"text":"70174031 - 2015 - On the sensitivity of transtensional versus transpressional tectonic regimes to remote dynamic triggering by Coulomb failure","interactions":[],"lastModifiedDate":"2016-06-24T10:54:14","indexId":"70174031","displayToPublicDate":"2015-06-17T10:15:00","publicationYear":"2015","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1135,"text":"Bulletin of the Seismological Society of America","onlineIssn":"1943-3573","printIssn":"0037-1106","active":true,"publicationSubtype":{"id":10}},"title":"On the sensitivity of transtensional versus transpressional tectonic regimes to remote dynamic triggering by Coulomb failure","docAbstract":"<p>&nbsp;Accumulating evidence, although still strongly spatially aliased, indicates that although remote dynamic triggering of small-to-moderate (M<sub>w</sub>&lt;5) earthquakes can occur in all tectonic settings, transtensional stress regimes with normal and subsidiary strike-slip faulting seem to be more susceptible to dynamic triggering than transpressional regimes with reverse and subsidiary strike-slip faulting. Analysis of the triggering potential of Love- and Rayleigh-wave dynamic stresses incident on normal, reverse, and strike-slip faults assuming Andersonian faulting theory and simple Coulomb failure supports this apparent difference for rapid-onset triggering susceptibility.</p>","language":"English","publisher":"Seismological Society of America","doi":"10.1785/0120140292","usgsCitation":"Hill, D.P., 2015, On the sensitivity of transtensional versus transpressional tectonic regimes to remote dynamic triggering by Coulomb failure: Bulletin of the Seismological Society of America, v. 105, no. 3, p. 1339-1348, https://doi.org/10.1785/0120140292.","productDescription":"10 p.","startPage":"1339","endPage":"1348","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-060012","costCenters":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"links":[{"id":324357,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United 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,{"id":70148016,"text":"ofr20151098 - 2015 - California State Waters Map Series — Offshore of Salt Point, California","interactions":[],"lastModifiedDate":"2022-04-18T20:29:14.829189","indexId":"ofr20151098","displayToPublicDate":"2015-06-17T10:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2015-1098","title":"California State Waters Map Series — Offshore of Salt Point, California","docAbstract":"<p>In 2007, the California Ocean Protection Council initiated the California Seafloor Mapping Program (CSMP), designed to create a comprehensive seafloor map of high-resolution bathymetry, marine benthic habitats, and geology within the 3-nautical-mile limit of California&rsquo;s State Waters. The CSMP approach is to create highly detailed seafloor maps through collection, integration, interpretation, and visualization of swath sonar data, acoustic backscatter, seafloor video, seafloor photography, high-resolution seismic-reflection profiles, and bottom-sediment sampling data. The map products display seafloor morphology and character, identify potential marine benthic habitats, and illustrate both the surficial seafloor geology and shallow (to about 100 m) subsurface geology.</p>\n<p>The Offshore of Salt Point map area is located in northern California, about 110 km north of San Francisco and 50 km south of Point Arena. The map area includes three California Marine Protected Areas: the southern portion of the Stewarts Point State Marine Reserve, the Salt Point State Marine Conservation Area, and the Gerstle Cove State Marine Reserve. The coast and shoreline are rugged and scenic, characterized by rocky promontories, steep bluffs capped by bare to forested marine terraces, kelp-rich coves, and nearshore rocks and pinnacles. The largely undeveloped onshore part of the map area is used primarily for grazing and recreation. U.S. Highway 1 extends along the coast through the map area, passing through Salt Point State Park, Kruse Rhododendron State Natural Reserve, and Stillwater Cove Regional Park. Sandy beaches are uncommon, present only in relatively protected coves.</p>\n<p>The seafloor in the map area extends from the shoreline to water depths of about 90 to 100 m. The nearshore to inner shelf area (to water depths of about 50 to 60 m) typically dips seaward about 1.0&deg; to 1.5&deg; and is underlain by bedrock and sand-sized to coarser grained sediment. The midshelf, underlain predominantly by muddy sediments, slopes more gently (less than 0.5&deg;). Surficial and shallow sediments were deposited in the last about 21,000 years during the approximately 125-m sea-level rise that followed the last major lowstand associated with the Last Glacial Maximum, at which time the entire Offshore of Salt Point map area was emergent and the shoreline was about 20 km west of the present-day shoreline.</p>\n<p>Tectonic influences that impact the shelf morphology and geology in the map area are related to local faulting, folding, uplift, and subsidence. The onshore part of the map area is cut by the northwest-striking San Andreas Fault&mdash;the right-lateral transform boundary between the North American and Pacific tectonic plates with an estimated slip rate of about 17 to 25 mm/yr in this area. The region between Fort Ross and Point Arena, west of the San Andreas Fault, is the known as the &ldquo;Gualala Block&rdquo; on the basis of its distinctive geology. The Gualala Block consists of a thick, discontinuous Upper Cretaceous to Miocene stratigraphic section, however, only the submarine fan deposits of the Paleocene and Eocene German Rancho Formation are exposed along the coast in the Offshore of Salt Point map area. The German Rancho Formation also forms all of the rugged seafloor bedrock outcrops in the map area. The western boundary of the Gualala Block lies 3 to 5 km offshore, perhaps at the shore-parallel Gualala Fault. High-resolution seismic-reflection data reveal shallow folding and faulting in inferred upper Pleistocene strata along the Gualala Fault trend, suggesting this structure is now or has been recently active. The last ground rupture in the map area occurred during the devastating great 1906 California earthquake (M7.8, 4/18/1906), thought to have nucleated on the San Andreas Fault about 100 kilometers to the south offshore of San Francisco.</p>\n<p>Circulation over the continental shelf in the map area is dominated by the southward-flowing California Current, the eastern limb of the North Pacific Gyre. Associated upwelling brings cool, nutrient-rich waters to the surface, resulting in high biological productivity. The current flow generally is southeastward during the spring and summer; however, during the fall and winter, the otherwise persistent northwest winds are sometimes weak or absent, causing the California Current to move farther offshore and the Davidson Current, a weaker, northward-flowing countercurrent, to become active.</p>\n<p>Throughout the year, this part of the central California coast is exposed to four wave climate regimes: the north Pacific swell, the southern swell, northwest wind waves, and local wind waves. The north Pacific swell dominates in winter months, with wave heights at offshore buoys ranging from 2 to 10 m and wave periods ranging from 10 to 25 s. During summer months, the largest waves come from the southern swell, generated by storms in the south Pacific and offshore Central America. Characteristically, these swells have smaller wave heights (0.3 to 3 m) and similarly long periods (range 10 to 25 s). Northwest wind waves affect the coast throughout the year, while local wind waves are most common from October to April. These two wind-wave regimes typically have wave heights of 1 to 4 m and short periods (3 to 10 s).</p>\n<p>Potential marine benthic habitats in the Offshore of Salt Point map area include unconsolidated continental shelf sediments, mixed continental shelf substrate, and hard continental shelf substrate. Rocky-shelf outcrops and rubble are considered to be promising potential habitats for rockfish and lingcod, both of which are recreationally and commercially important species.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20151098","usgsCitation":"Johnson, S.Y., Dartnell, P., Golden, N., Hartwell, S., Erdey, M.D., Greene, H., Cochrane, G.R., Kvitek, R.G., Manson, M., Endris, C.A., Dieter, B.E., Watt, J., Krigsman, L.M., Sliter, R.W., Lowe, E.N., and Chinn, J.L., 2015, California State Waters Map Series — Offshore of Salt Point, California: U.S. Geological Survey Open-File Report 2015-1098, Pamphlet: iv, 37 p.; 10 Sheets: 52 x 36 inches or smaller; Metadata, Data Catalog, https://doi.org/10.3133/ofr20151098.","productDescription":"Pamphlet: iv, 37 p.; 10 Sheets: 52 x 36 inches or smaller; Metadata, Data Catalog","numberOfPages":"41","onlineOnly":"Y","additionalOnlineFiles":"Y","ipdsId":"IP-057589","costCenters":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":301257,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr20151098.jpg"},{"id":399001,"rank":16,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_102031.htm"},{"id":301255,"rank":11,"type":{"id":26,"text":"Sheet"},"url":"https://pubs.usgs.gov/of/2015/1098/pdf/ofr20151098_sheet9.pdf","text":"Sheet 9","linkFileType":{"id":1,"text":"pdf"},"description":"Sheet 9","linkHelpText":"Local (Offshore of Salt Point Map Area) and Regional (Offshore from Salt Point to Drakes Bay) Shallow-Subsurface Geology and Structure, California By Samuel Y. Johnson, Stephen R. Hartwell, and Janet T. Watt (45.5\" x 36\", 6.8 MB)"},{"id":301256,"rank":12,"type":{"id":26,"text":"Sheet"},"url":"https://pubs.usgs.gov/of/2015/1098/pdf/ofr20151098_sheet10.pdf","text":"Sheet 10","linkFileType":{"id":1,"text":"pdf"},"description":"Sheet 10","linkHelpText":"Offshore and Onshore Geology and Geomorphology, Offshore of Salt Point Map Area, California By Stephen R. Hartwell, Samuel Y. Johnson, and Michael W. 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Pallid sturgeon were sampled by trotlines year round from 2008 to 2011. A logistic regression model indicated water temperature (</span><i>T</i><span>; P</span><i>&nbsp;</i><span>&lt;</span><i>&nbsp;</i><span>0.01) and depth (</span><i>D</i><span>; P</span><i>&nbsp;</i><span>=</span><i>&nbsp;</i><span>0.03) had significant effects on capture probability (</span><i>Y</i><span>&nbsp;=&nbsp;&minus;1.75&nbsp;&minus; 0.06</span><i>T</i><span>&nbsp;+&nbsp;0.10</span><i>D</i><span>). Habitat type, surface current velocity, river stage, stage change and non-sturgeon bycatch were not significant predictors (P</span><i>&nbsp;</i><span>=</span><i>&nbsp;</i><span>0.26&ndash;0.63). Although pallid sturgeon were caught throughout the year, the model predicted that sampling should focus on times when the water temperature is less than 12&deg;C and in deeper water to maximize capture probability; these water temperature conditions commonly occur during November to March in the lower Mississippi River. Further, the significant effect of water temperature which varies widely over time, as well as water depth indicate that any efforts to use the catch rate to infer population trends will require the consideration of temperature and depth in standardized sampling efforts or adjustment of estimates.</span></p>","language":"English","publisher":"John Wiley & Sons, Inc.","doi":"10.1111/jai.12814","usgsCitation":"DeVries, R.J., Hann, D.A., and Schramm, H., 2015, Increasing capture efficiency of pallid sturgeon <i>Scaphirhynchus albus</i> (Forbes and Richardson, 1905) and the reliability of catch rate estimates: Journal of Applied Ichthyology, v. 31, no. 4, p. 603-608, https://doi.org/10.1111/jai.12814.","productDescription":"6 p.","startPage":"603","endPage":"608","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-059805","costCenters":[{"id":198,"text":"Coop Res Unit Atlanta","active":true,"usgs":true}],"links":[{"id":472012,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1111/jai.12814","text":"Publisher Index Page"},{"id":324979,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Mississippi","otherGeospatial":"Lower Mississippi River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -91.2579345703125,\n              32.65325087996883\n            ],\n            [\n              -91.2579345703125,\n              33.83848275599514\n            ],\n            [\n              -90.8953857421875,\n              33.83848275599514\n            ],\n            [\n              -90.8953857421875,\n              32.65325087996883\n            ],\n            [\n              -91.2579345703125,\n              32.65325087996883\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"31","issue":"4","publishingServiceCenter":{"id":8,"text":"Raleigh PSC"},"noUsgsAuthors":false,"publicationDate":"2015-06-17","publicationStatus":"PW","scienceBaseUri":"5780ceb9e4b081161682236b","chorus":{"doi":"10.1111/jai.12814","url":"http://dx.doi.org/10.1111/jai.12814","publisher":"Wiley-Blackwell","authors":"DeVries R. 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,{"id":70178131,"text":"70178131 - 2015 - Increasing seismicity in the U. S. midcontinent: Implications for earthquake hazard","interactions":[],"lastModifiedDate":"2016-11-03T13:10:36","indexId":"70178131","displayToPublicDate":"2015-06-17T00:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3568,"text":"The Leading Edge","active":true,"publicationSubtype":{"id":10}},"title":"Increasing seismicity in the U. S. midcontinent: Implications for earthquake hazard","docAbstract":"<p><span>Earthquake activity in parts of the central United States has increased dramatically in recent years. The space-time distribution of the increased seismicity, as well as numerous published case studies, indicates that the increase is of anthropogenic origin, principally driven by injection of wastewater coproduced with oil and gas from tight formations. Enhanced oil recovery and long-term production also contribute to seismicity at a few locations. Preliminary hazard models indicate that areas experiencing the highest rate of earthquakes in 2014 have a short-term (one-year) hazard comparable to or higher than the hazard in the source region of tectonic earthquakes in the New Madrid and Charleston seismic zones.</span><span><br></span></p>","language":"English","publisher":"Society of Exploration Geophysicists","publisherLocation":"Tulsa, OK","doi":"10.1190/tle34060618.1","usgsCitation":"Ellsworth, W.L., Llenos, A.L., McGarr, A.F., Michael, A.J., Rubinstein, J.L., Mueller, C.S., Petersen, M.D., and Calais, E., 2015, Increasing seismicity in the U. 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,{"id":70148023,"text":"70148023 - 2015 - Changes in total phosphorus concentration in the Red River of the North Basin, 1970-2012","interactions":[],"lastModifiedDate":"2017-10-12T20:01:18","indexId":"70148023","displayToPublicDate":"2015-06-17T00:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Changes in total phosphorus concentration in the Red River of the North Basin, 1970-2012","docAbstract":"<p><span>The Red River of the North drains much of eastern North Dakota and northwestern Minnesota and flows north into Manitoba, Canada, ultimately into Lake Winnipeg; therefore, water quality is an International concern. With increased runoff in the past few decades, phosphorus flux (the amount of phosphorus transported by the river) has increased. This is a concern, especially with respect to Lake Winnipeg, an important inland fishery and recreational destination. There is pressure at the State and International levels to reduce phosphorus flux, an expensive proposition. Depending on the method (controlling sources, settling ponds, buffer strips), control of phosphorus flux is not always effective during spring runoff. This work represents a first step in developing a causal model for phosphorus flux by examining available data and changes in concentration over time. Total phosphorus concentration data for the Red River at Emerson, Manitoba, and at Fargo, North Dakota-Moorhead, Minnesota, were summarized and then analyzed using WRTDS (Weighted Regressions on Time, Discharge, and Season) to describe total phosphorus changes over time in two analysis periods: 1970-1993 and 1993-2012. Total phosphorus concentration increased in the first period at Emerson, Manitoba, indicating phosphorus was likely being transported to streams during runoff events. A very different pattern occurred at Fargo-Moorhead with declines in concentration, except at high discharge. While concentration continually changes, during the second period it decreased during spring runoff at Emerson and Fargo-Moorhead and during the growing season at Fargo-Moorhead, perhaps because of improved agricultural practices and declines in some uses of phosphorus.</span></p>","largerWorkTitle":"ASABE/CSBE North Central Intersectional Meeting Papers","conferenceTitle":"ASABE/CSBE North Central Intersectional Meeting","conferenceDate":"April 10-11, 2015","conferenceLocation":"Fargo, ND","language":"English","publisher":"American Society of Agricultural and Biological Engineers","doi":"10.13031/rrv2015054","usgsCitation":"Ryberg, K.R., Akyuz, F.A., and Lin, W., 2015, Changes in total phosphorus concentration in the Red River of the North Basin, 1970-2012, <i>in</i> ASABE/CSBE North Central Intersectional Meeting Papers, Fargo, ND, April 10-11, 2015, Paper number RRV15-054, https://doi.org/10.13031/rrv2015054.","productDescription":"Paper number 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Adnan","contributorId":140760,"corporation":false,"usgs":false,"family":"Akyuz","given":"F.","email":"","middleInitial":"Adnan","affiliations":[{"id":13555,"text":"North Dakota Climate Office","active":true,"usgs":false}],"preferred":false,"id":546847,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lin, Wei","contributorId":93805,"corporation":false,"usgs":true,"family":"Lin","given":"Wei","email":"","affiliations":[],"preferred":false,"id":546848,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70173509,"text":"70173509 - 2015 - Repeated count surveys help standardize multi-agency estimates of American Oystercatcher (<i>Haematopus palliatus</i>) abundance","interactions":[],"lastModifiedDate":"2016-06-16T16:10:58","indexId":"70173509","displayToPublicDate":"2015-06-17T00:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3551,"text":"The Condor","active":true,"publicationSubtype":{"id":10}},"title":"Repeated count surveys help standardize multi-agency estimates of American Oystercatcher (<i>Haematopus palliatus</i>) abundance","docAbstract":"<p><span>The extensive breeding range of many shorebird species can make integration of survey data problematic at regional spatial scales. We evaluated the effectiveness of standardized repeated count surveys coordinated across 8 agencies to estimate the abundance of American Oystercatcher (</span><i>Haematopus palliatus</i><span>) breeding pairs in the southeastern United States. Breeding season surveys were conducted across coastal North Carolina (90 plots) and the Eastern Shore of Virginia (3 plots). Plots were visited on 1&ndash;5 occasions during April&ndash;June 2013.&nbsp;</span><i>N</i><span>-mixture models were used to estimate abundance and detection probability in relation to survey date, tide stage, plot size, and plot location (coastal bay vs. barrier island). The estimated abundance of oystercatchers in the surveyed area was 1,048 individuals (95% credible interval: 851&ndash;1,408) and 470 pairs (384&ndash;637), substantially higher than estimates that did not account for detection probability (maximum counts of 674 individuals and 316 pairs). Detection probability was influenced by a quadratic function of survey date, and increased from mid-April (~0.60) to mid-May (~0.80), then remained relatively constant through June. Detection probability was also higher during high tide than during low, rising, or falling tides. Abundance estimates from&nbsp;</span><i>N</i><span>-mixture models were validated at 13 plots by exhaustive productivity studies (2&ndash;5 surveys wk</span><sup>&minus;1</sup><span>). Intensive productivity studies identified 78 breeding pairs across 13 productivity plots while the&nbsp;</span><i>N</i><span>-mixture model abundance estimate was 74 pairs (62&ndash;119) using only 1&ndash;5 replicated surveys season</span><sup>&minus;1</sup><span>. Our results indicate that standardized replicated count surveys coordinated across multiple agencies and conducted during a relatively short time window (closure assumption) provide tremendous potential to meet both agency-level (e.g., state) and regional-level (e.g., flyway) objectives in large-scale shorebird monitoring programs.</span></p>","language":"English","publisher":"Cooper Ornithological Club","publisherLocation":"Santa Clara, CA","doi":"10.1650/CONDOR-14-185.1","usgsCitation":"Hostetter, N.J., Gardner, B., Schweitzer, S.H., Boettcher, R., Wilke, A.L., Addison, L., Swilling, W.R., Pollock, K.H., and Simons, T.R., 2015, Repeated count surveys help standardize multi-agency estimates of American Oystercatcher (<i>Haematopus palliatus</i>) abundance: The Condor, v. 117, no. 3, p. 354-363, https://doi.org/10.1650/CONDOR-14-185.1.","productDescription":"10 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,{"id":70173652,"text":"70173652 - 2015 - Tidal management sffects sub-adult fish assemblages in impounded South Carolina Marshes","interactions":[],"lastModifiedDate":"2016-11-30T15:05:05","indexId":"70173652","displayToPublicDate":"2015-06-17T00:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3751,"text":"Wetlands Ecology and Management","active":true,"publicationSubtype":{"id":10}},"title":"Tidal management sffects sub-adult fish assemblages in impounded South Carolina Marshes","docAbstract":"<p><span>In coastal South Carolina, most impounded marshes are managed for waterfowl; fewer are managed for fishes. Tidal control is central to each strategy but raises concerns that nursery function could be impaired. This research examined the assemblage composition of fishes during early-life stages. We sampled two impoundments of each management type monthly in 2008 and 2009. We used light traps to collect 61,527 sub-adult fish representing 21 species and 16 families and push nets to collect 12,670 sub-adult fish representing 13 species and 11 families. The effective number of species detected at larval stage in &ldquo;fish&rdquo; impoundments (summer mean&nbsp;=&nbsp;2.52&nbsp;&plusmn;&nbsp;0.20, winter mean&nbsp;=&nbsp;2.02&nbsp;&plusmn;&nbsp;0.66) was greater than in &ldquo;waterfowl&rdquo; impoundments (summer mean&nbsp;=&nbsp;1.27&nbsp;&plusmn;&nbsp;0.14, winter mean&nbsp;=&nbsp;1.06&nbsp;&plusmn;&nbsp;0.09); CI&nbsp;=&nbsp;90&nbsp;%. Species richness did not differ between management types, but hierarchical linear models predicted differences in assemblage composition. These findings underscore the importance of frequent water exchange for maintaining diverse assemblages of early-life-stage fishes in marsh impoundments.</span></p>","language":"English","publisher":"Springer Netherlands","doi":"10.1007/s11273-015-9435-1","usgsCitation":"Carswell, B.L., Peterson, J., and Jennings, C.A., 2015, Tidal management sffects sub-adult fish assemblages in impounded South Carolina Marshes: Wetlands Ecology and Management, v. 23, no. 6, p. 1015-1031, https://doi.org/10.1007/s11273-015-9435-1.","productDescription":"17 p.","startPage":"1015","endPage":"1031","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-056879","costCenters":[{"id":198,"text":"Coop Res Unit Atlanta","active":true,"usgs":true},{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":323227,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"South Carolina","county":"Beaufort","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -80.68702697753906,\n              32.67752870965116\n            ],\n            [\n              -80.69526672363281,\n              32.66539061924646\n            ],\n            [\n              -80.70762634277344,\n              32.65382900017623\n            ],\n            [\n              -80.68771362304686,\n              32.62318347873869\n            ],\n            [\n              -80.66230773925781,\n              32.62318347873869\n            ],\n            [\n              -80.64239501953125,\n              32.637061996573436\n            ],\n            [\n              -80.6568145751953,\n              32.67752870965116\n            ],\n            [\n              -80.68702697753906,\n              32.67752870965116\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"23","issue":"6","publishingServiceCenter":{"id":8,"text":"Raleigh PSC"},"noUsgsAuthors":false,"publicationDate":"2015-06-17","publicationStatus":"PW","scienceBaseUri":"5757f064e4b04f417c24dd2e","contributors":{"authors":[{"text":"Carswell, Ben L.","contributorId":171502,"corporation":false,"usgs":false,"family":"Carswell","given":"Ben","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":637756,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Peterson, James T. 0000-0002-7709-8590 james_peterson@usgs.gov","orcid":"https://orcid.org/0000-0002-7709-8590","contributorId":2111,"corporation":false,"usgs":true,"family":"Peterson","given":"James","email":"james_peterson@usgs.gov","middleInitial":"T.","affiliations":[{"id":200,"text":"Coop Res Unit Seattle","active":true,"usgs":true}],"preferred":true,"id":637757,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Jennings, Cecil A. 0000-0002-6159-6026 jennings@usgs.gov","orcid":"https://orcid.org/0000-0002-6159-6026","contributorId":874,"corporation":false,"usgs":true,"family":"Jennings","given":"Cecil","email":"jennings@usgs.gov","middleInitial":"A.","affiliations":[{"id":198,"text":"Coop Res Unit Atlanta","active":true,"usgs":true}],"preferred":true,"id":637758,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70189936,"text":"70189936 - 2015 - Measurements of the initiation of post-wildfire runoff during rainstorms using in situ overland flow detectors","interactions":[],"lastModifiedDate":"2017-07-31T09:02:59","indexId":"70189936","displayToPublicDate":"2015-06-17T00:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1425,"text":"Earth Surface Processes and Landforms","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Measurements of the initiation of post-wildfire runoff during rainstorms using <i>in situ</i> overland flow detectors","title":"Measurements of the initiation of post-wildfire runoff during rainstorms using in situ overland flow detectors","docAbstract":"<p>Overland flow detectors (OFDs) were deployed in 2012 on a hillslope burned by the 2010 Fourmile Canyon fire near Boulder, Colorado, USA. These detectors were simple, electrical resistor-type instruments that output a voltage (0–2·5 V) and were designed to measure and record the time of runoff initiation, a signal proportional to water depth, and the runoff hydrograph during natural convective rainstorms.</p><p>Initiation of runoff was found to be spatially complex and began at different times in different locations on the hillslope. Runoff started first at upstream detectors 56% of the time, at the mid-stream detectors 6%, and at the downstream detectors 38% of the time. Initiation of post-wildfire runoff depended on the time-to-ponding, travel time between points, and the time to fill surface depression storage. These times ranged from 0·5–54, 0·4–1·1, and 0·2–14 minutes, respectively, indicating the importance of the ponding process in controlling the initiation of runoff at this site. Time-to-ponding was modeled as a function of the rainfall acceleration (i.e. the rate of change of rainfall intensity) and either the cumulative rainfall at the start of runoff or the soil–water deficit.</p><p>Measurements made by the OFDs provided physical insight into the spatial and temporal initiation of post-wildfire runoff during unsteady flow in response to time varying natural rainfall. They also provided data that can be telemetered and used to determine critical input parameters for hydrologic rainfall–runoff models.</p>","language":"English","publisher":"Wiley","doi":"10.1002/esp.3704","usgsCitation":"Moody, J.A., and Martin, R., 2015, Measurements of the initiation of post-wildfire runoff during rainstorms using in situ overland flow detectors: Earth Surface Processes and Landforms, v. 40, no. 8, p. 1043-1056, https://doi.org/10.1002/esp.3704.","productDescription":"14 p.","startPage":"1043","endPage":"1056","ipdsId":"IP-061823","costCenters":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"links":[{"id":344455,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"40","issue":"8","publishingServiceCenter":{"id":2,"text":"Denver PSC"},"noUsgsAuthors":false,"publicationDate":"2015-01-28","publicationStatus":"PW","scienceBaseUri":"5980419be4b0a38ca2789349","contributors":{"authors":[{"text":"Moody, John A. 0000-0003-2609-364X jamoody@usgs.gov","orcid":"https://orcid.org/0000-0003-2609-364X","contributorId":771,"corporation":false,"usgs":true,"family":"Moody","given":"John","email":"jamoody@usgs.gov","middleInitial":"A.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":true,"id":706815,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Martin, Richard G.","contributorId":195347,"corporation":false,"usgs":false,"family":"Martin","given":"Richard G.","affiliations":[],"preferred":false,"id":706816,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70188062,"text":"70188062 - 2015 - Projection of corn production and stover-harvesting impacts on soil organic carbon dynamics in the U.S. Temperate Prairies","interactions":[],"lastModifiedDate":"2017-05-31T16:08:46","indexId":"70188062","displayToPublicDate":"2015-06-17T00:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3358,"text":"Scientific Reports","active":true,"publicationSubtype":{"id":10}},"title":"Projection of corn production and stover-harvesting impacts on soil organic carbon dynamics in the U.S. Temperate Prairies","docAbstract":"<p><span>Terrestrial carbon sequestration potential is widely considered as a realistic option for mitigating greenhouse gas emissions. However, this potential may be threatened by global changes including climate, land use, and management changes such as increased corn stover harvesting for rising production of cellulosic biofuel. Therefore, it is critical to investigate the dynamics of soil organic carbon (SOC) at regional or global scale. This study simulated the corn production and spatiotemporal changes of SOC in the U.S. Temperate Prairies, which covers over one-third of the U.S. corn acreage, using a biogeochemical model with multiple climate and land-use change projections. The corn production (either grain yield or stover biomass) could reach 88.7–104.7 TgC as of 2050, 70–101% increase when compared to the base year of 2010. A removal of 50% stover at the regional scale could be a reasonable cap in view of maintaining SOC content and soil fertility especially in the beginning years. The projected SOC dynamics indicated that the average carbon sequestration potential across the entire region may vary from 12.7 to 19.6 g C/m</span><sup>2</sup><span>/yr (i.e., 6.6–10.2 g TgC/yr). This study not only helps understand SOC dynamics but also provides decision support for sustainable biofuel development.</span></p>","language":"English","publisher":"Nature Publishing Group","doi":"10.1038/srep10830","usgsCitation":"Wu, Y., Liu, S., Young, C.J., Dahal, D., Sohl, T.L., and Davis, B., 2015, Projection of corn production and stover-harvesting impacts on soil organic carbon dynamics in the U.S. Temperate Prairies: Scientific Reports, v. 5, Article 10830: 12 p., https://doi.org/10.1038/srep10830.","productDescription":"Article 10830: 12 p.","ipdsId":"IP-064045","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":472016,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1038/srep10830","text":"Publisher Index Page"},{"id":341844,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United 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,{"id":70155866,"text":"70155866 - 2015 - Velocity bias induced by flow patterns around ADCPs and associated deployment platforms","interactions":[],"lastModifiedDate":"2017-05-30T10:12:36","indexId":"70155866","displayToPublicDate":"2015-06-17T00:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Velocity bias induced by flow patterns around ADCPs and associated deployment platforms","docAbstract":"<p>Velocity measurements near the Acoustic Doppler Current Profiler (ADCP) are important for mapping surface currents, measuring velocity and discharge in shallow streams, and providing accurate estimates of discharge in the top unmeasured portion of the water column. Improvements to ADCP performance permit measurement of velocities much closer (5 cm) to the transducer than has been possible in the past (25 cm). Velocity profiles collected by the U.S. Geological Survey (USGS) with a 1200 kHz Rio Grande Zedhead ADCP in 2002 showed a negative bias in measured velocities near the transducers. On the basis of these results, the USGS initiated a study combining field, laboratory, and numerical modeling data to assess the effect of flow patterns caused by flow around the ADCP and deployment platforms on velocities measured near the transducers. This ongoing study has shown that the negative bias observed in the field is due to the flow pattern around the ADCP. The flow pattern around an ADCP violates the basic assumption of flow homogeneity required for an accurate three-dimensional velocity solution. Results, to date (2014), have indicated velocity biases within the measurable profile, due to flow disturbance, for the TRDI 1200 kHz Rio Grande Zedhead and the SonTek RiverSurveyor M9 ADCPs. The flow speed past the ADCP, the mount and the deployment platform have also been shown to play an important role in the magnitude and extent of the velocity bias. </p>","conferenceTitle":"2015 IEEE/OES Eleveth Current, Waves and Turbulence Measurement (CWTM)","conferenceDate":"March 2-6, 2015","conferenceLocation":"St. Petersburg, FL","language":"English","publisher":"IEEE","doi":"10.1109/CWTM.2015.7098103","usgsCitation":"Mueller, D.S., 2015, Velocity bias induced by flow patterns around ADCPs and associated deployment platforms, 2015 IEEE/OES Eleveth Current, Waves and Turbulence Measurement (CWTM), St. Petersburg, FL, March 2-6, 2015, 7 p., https://doi.org/10.1109/CWTM.2015.7098103.","productDescription":"7 p.","ipdsId":"IP-062183","costCenters":[{"id":502,"text":"Office of Surface Water","active":true,"usgs":true}],"links":[{"id":472017,"rank":0,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://zenodo.org/record/1266880","text":"External Repository"},{"id":341822,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"publishingServiceCenter":{"id":9,"text":"Reston PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"592d8edee4b08f9d15be7b83","contributors":{"authors":[{"text":"Mueller, David S. dmueller@usgs.gov","contributorId":1499,"corporation":false,"usgs":true,"family":"Mueller","given":"David","email":"dmueller@usgs.gov","middleInitial":"S.","affiliations":[{"id":502,"text":"Office of Surface Water","active":true,"usgs":true}],"preferred":true,"id":566633,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70189145,"text":"70189145 - 2015 - Megathrust earthquakes and sea-level change: A tribute to George Plafker","interactions":[],"lastModifiedDate":"2017-07-03T09:20:05","indexId":"70189145","displayToPublicDate":"2015-06-17T00:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3219,"text":"Quaternary Science Reviews","active":true,"publicationSubtype":{"id":10}},"title":"Megathrust earthquakes and sea-level change: A tribute to George Plafker","docAbstract":"<p><span>For numerous scientific disciplines that contribute to the understanding of megathrust earthquakes, 2014 was an anniversary year of two great, &gt;M</span><sub>w</sub><span>9, earthquakes; fifty years since the March 27 1964 earthquake in Alaska and ten years since the December 26 2004 Aceh-Andaman earthquake and attendant tsunami. 2014 was also the final year of International Geoscience Programme (IGCP) Project 588 “Preparing for Coastal Change”, which was the latest in the 25 year history of IGCP coastal change research.</span></p>","language":"English","publisher":"Elseivier","doi":"10.1016/j.quascirev.2015.01.026","usgsCitation":"Freymueller, J., 2015, Megathrust earthquakes and sea-level change: A tribute to George Plafker: Quaternary Science Reviews, v. 113, p. 1-2, https://doi.org/10.1016/j.quascirev.2015.01.026.","productDescription":"2 p.","startPage":"1","endPage":"2","ipdsId":"IP-064200","costCenters":[{"id":119,"text":"Alaska Science Center Geology Minerals","active":true,"usgs":true}],"links":[{"id":343263,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"113","publishingServiceCenter":{"id":12,"text":"Tacoma PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"595b5799e4b0d1f9f0536dcb","contributors":{"authors":[{"text":"Freymueller, Jeffrey T.","contributorId":96841,"corporation":false,"usgs":false,"family":"Freymueller","given":"Jeffrey T.","affiliations":[{"id":26875,"text":"Michigan State University, East Lansing, MI","active":true,"usgs":false}],"preferred":false,"id":703159,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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