{"pageNumber":"1801","pageRowStart":"45000","pageSize":"25","recordCount":184617,"records":[{"id":70035118,"text":"70035118 - 2011 - The development of an EDSS: Lessons learned and implications for DSS research","interactions":[],"lastModifiedDate":"2021-06-14T19:51:32.448528","indexId":"70035118","displayToPublicDate":"2011-01-01T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"The development of an EDSS: Lessons learned and implications for DSS research","docAbstract":"<p><span>The Solar and Wind Energy Resource Assessment (SWERA) project is focused on providing renewable energy (RE) planning resources to the public. Examples include wind, solar, and hydro assessments. SWERA DSS consists of three major components. First, SWERA 'Product Archive' provides for a discovery DSS upon which users can find and access renewable energy data and supporting models. Second, the 'Renewable Resource EXplorer' (RREX) component serves as a web-based, GIS analysis tool for viewing RE resource data available through the SWERA Product Archive. Third, the SWERA web service provides computational access to the data available in the SWERA spatial database through a location based query, and is also utilized in the RREX component. We provide a discussion of various design decisions used in the construction of this EDSS, followed by project experiences and implications for EDSS and broader DSS research.</span></p>","largerWorkType":{"id":24,"text":"Conference Paper"},"largerWorkTitle":"Proceedings of the Annual Hawaii International Conference on System Sciences","largerWorkSubtype":{"id":19,"text":"Conference Paper"},"conferenceTitle":"44th Hawaii International Conference on System Sciences, HICSS-44 2010","conferenceDate":"January, 4-7,2011","conferenceLocation":"Koloa, Kauai, HI","language":"English","publisher":"IEEE","doi":"10.1109/HICSS.2011.405","issn":"15301605","isbn":"9780769542829","usgsCitation":"El-Gayar, O., Deokar, A., Michels, L., and Fosnight, E.A., 2011, The development of an EDSS: Lessons learned and implications for DSS research, <i>in</i> Proceedings of the Annual Hawaii International Conference on System Sciences, Koloa, Kauai, HI, January, 4-7,2011, 10 p., https://doi.org/10.1109/HICSS.2011.405.","productDescription":"10 p.","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":243192,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":215392,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1109/HICSS.2011.405"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505baaa4e4b08c986b3228ec","contributors":{"authors":[{"text":"El-Gayar, O.","contributorId":64914,"corporation":false,"usgs":true,"family":"El-Gayar","given":"O.","email":"","affiliations":[],"preferred":false,"id":449365,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Deokar, A.","contributorId":69802,"corporation":false,"usgs":true,"family":"Deokar","given":"A.","email":"","affiliations":[],"preferred":false,"id":449366,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Michels, L.","contributorId":92073,"corporation":false,"usgs":true,"family":"Michels","given":"L.","email":"","affiliations":[],"preferred":false,"id":449367,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Fosnight, Eugene A. 0000-0002-8557-3697 fosnight@usgs.gov","orcid":"https://orcid.org/0000-0002-8557-3697","contributorId":2961,"corporation":false,"usgs":true,"family":"Fosnight","given":"Eugene","email":"fosnight@usgs.gov","middleInitial":"A.","affiliations":[{"id":223,"text":"Earth Resources Observation and Science (EROS) Center (Geography)","active":false,"usgs":true}],"preferred":true,"id":449368,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70035117,"text":"70035117 - 2011 - Lead isotopes in soils and groundwaters as tracers of the impact of human activities on the surface environment: The Domizio-Flegreo Littoral (Italy) case study","interactions":[],"lastModifiedDate":"2021-03-01T20:05:47.474207","indexId":"70035117","displayToPublicDate":"2011-01-01T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2302,"text":"Journal of Geochemical Exploration","active":true,"publicationSubtype":{"id":10}},"title":"Lead isotopes in soils and groundwaters as tracers of the impact of human activities on the surface environment: The Domizio-Flegreo Littoral (Italy) case study","docAbstract":"<p id=\"sp0055\"><span>The isotopic signature of geogenic and anthropogenic materials, in combination with concentration data for pollutants, can help trace the origin and the extent of contamination in the environment. This approach is particularly effective if naturally occurring and anthropogenically introduced metals have different&nbsp;isotopic ratios.&nbsp;Lead isotope&nbsp;analysis on soils from 7 profiles (1</span>&nbsp;<span>m depth) and on groundwaters from 8 wells have been used to determine the impact of human activities on the surface environment of Domizio-Flegreo&nbsp;Littoral.</span></p><p id=\"sp0060\">Result obtained show that in sub-rural areas the<span>&nbsp;</span>isotopic composition<span>&nbsp;</span>of the samples collected along the soil profiles of Domizio-Flegreo Littoral is likely mostly controlled by the nature of the parent geologic material (natural) while in more urbanized areas (Giugliano) Pb isotopic composition in superficial soils is mostly influenced by anthropic sources such as motor vehicles. Lead isotopic ratios in groundwaters also show that the use of pesticides and, probably, the influence of aerosols and the presence of illegal waste disposal can influence water quality.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.gexplo.2010.09.012","issn":"03756742","usgsCitation":"Grezzi, G., Ayuso, R.A., de Vivo, B., Lima, A., and Albanese, S., 2011, Lead isotopes in soils and groundwaters as tracers of the impact of human activities on the surface environment: The Domizio-Flegreo Littoral (Italy) case study: Journal of Geochemical Exploration, v. 109, no. 1-3, p. 51-58, https://doi.org/10.1016/j.gexplo.2010.09.012.","productDescription":"8 p.","startPage":"51","endPage":"58","costCenters":[{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"links":[{"id":215391,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.gexplo.2010.09.012"},{"id":243191,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Italy","otherGeospatial":"The Domizio-Flegreo Littoral","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              13.436279296875,\n              41.261291493919884\n            ],\n            [\n              13.9581298828125,\n              40.78470081841747\n            ],\n            [\n              14.23828125,\n              40.79301881008675\n            ],\n            [\n              14.501953124999998,\n              41.04207384890103\n            ],\n            [\n              14.315185546875,\n              41.31082388091818\n            ],\n            [\n              14.007568359374998,\n              41.52502957323801\n            ],\n            [\n              13.436279296875,\n              41.261291493919884\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"109","issue":"1-3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a45c5e4b0c8380cd674ba","contributors":{"authors":[{"text":"Grezzi, G.","contributorId":62425,"corporation":false,"usgs":true,"family":"Grezzi","given":"G.","email":"","affiliations":[],"preferred":false,"id":449363,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ayuso, Robert A. 0000-0002-8496-9534 rayuso@usgs.gov","orcid":"https://orcid.org/0000-0002-8496-9534","contributorId":2654,"corporation":false,"usgs":true,"family":"Ayuso","given":"Robert","email":"rayuso@usgs.gov","middleInitial":"A.","affiliations":[{"id":387,"text":"Mineral Resources Program","active":true,"usgs":true},{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":449360,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"de Vivo, B.","contributorId":50549,"corporation":false,"usgs":false,"family":"de Vivo","given":"B.","affiliations":[],"preferred":false,"id":449362,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lima, A.","contributorId":74884,"corporation":false,"usgs":true,"family":"Lima","given":"A.","affiliations":[],"preferred":false,"id":449364,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Albanese, S.","contributorId":35972,"corporation":false,"usgs":true,"family":"Albanese","given":"S.","affiliations":[],"preferred":false,"id":449361,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70035028,"text":"70035028 - 2011 - Enhanced transpiration by riparian buffer trees in response to advection in a humid temperate agricultural landscape","interactions":[],"lastModifiedDate":"2021-03-02T20:51:06.535692","indexId":"70035028","displayToPublicDate":"2011-01-01T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1687,"text":"Forest Ecology and Management","active":true,"publicationSubtype":{"id":10}},"title":"Enhanced transpiration by riparian buffer trees in response to advection in a humid temperate agricultural landscape","docAbstract":"<p><span>Riparian buffers are designed as management practices to increase infiltration and reduce surface runoff and transport of sediment and nonpoint source pollutants from crop fields to adjacent streams. Achieving these ecosystem service goals depends, in part, on their ability to remove water from the soil via transpiration. In these systems, edges between crop fields and trees of the buffer systems can create advection processes, which could influence water use by trees. We conducted a field study in a riparian buffer system established in 1994 under a humid temperate climate, located in the Corn Belt region of the Midwestern U.S. (Iowa). The goals were to estimate stand level transpiration by the riparian buffer, quantify the controls on water use by the buffer system, and determine to what extent advective energy and tree position within the buffer system influence individual tree transpiration rates. We primarily focused on the water use response (determined with the Heat Ratio Method) of one of the dominant species (</span><i>Acer saccharinum</i><span>) and a subdominant (</span><i>Juglans nigra</i><span>). A few individuals of three additional species (</span><i>Quercus bicolor, Betula nigra, Platanus occidentalis</i><span>) were monitored over a shorter time period to assess the generality of responses. Meteorological stations were installed along a transect across the riparian buffer to determine the microclimate conditions. The differences found among individuals were attributed to differences in species sap velocities and sapwood depths, location relative to the forest edge and prevailing winds and canopy exposure and dominance. Sapflow rates for&nbsp;</span><i>A. saccharinum</i><span>&nbsp;trees growing at the SE edge (prevailing winds) were 39% greater than SE&nbsp;</span><i>interior</i><span>&nbsp;trees and 30% and 69% greater than NW&nbsp;</span><i>interior</i><span>&nbsp;and&nbsp;</span><i>edge</i><span>&nbsp;trees, respectively. No transpiration enhancement due to edge effect was detected in the subdominant&nbsp;</span><i>J. nigra</i><span>. The results were interpreted as indicative of advection effects from the surrounding crops. Further, significant differences were document in sapflow rates between the five study species, suggesting that selection of species is important for enhancing specific riparian buffer functions. However, more information is needed on water use patterns among diverse species growing under different climatic and biophysical conditions to assist policy and management decisions regarding effective buffer design.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.foreco.2011.01.027","issn":"03781127","usgsCitation":"Hernandez-Santana, V., Asbjornsen, H., Sauer, T., Isenhart, T., Schilling, K., and Schultz, R., 2011, Enhanced transpiration by riparian buffer trees in response to advection in a humid temperate agricultural landscape: Forest Ecology and Management, v. 261, no. 8, p. 1415-1427, https://doi.org/10.1016/j.foreco.2011.01.027.","productDescription":"13 p.","startPage":"1415","endPage":"1427","costCenters":[],"links":[{"id":475519,"rank":10000,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://lib.dr.iastate.edu/nrem_pubs/176","text":"External Repository"},{"id":242886,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":215111,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.foreco.2011.01.027"}],"volume":"261","issue":"8","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0970e4b0c8380cd51ef3","contributors":{"authors":[{"text":"Hernandez-Santana, V.","contributorId":90126,"corporation":false,"usgs":true,"family":"Hernandez-Santana","given":"V.","email":"","affiliations":[],"preferred":false,"id":448955,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Asbjornsen, H.","contributorId":86968,"corporation":false,"usgs":true,"family":"Asbjornsen","given":"H.","affiliations":[],"preferred":false,"id":448954,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sauer, T.","contributorId":43998,"corporation":false,"usgs":true,"family":"Sauer","given":"T.","email":"","affiliations":[],"preferred":false,"id":448953,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Isenhart, T.","contributorId":27691,"corporation":false,"usgs":true,"family":"Isenhart","given":"T.","affiliations":[],"preferred":false,"id":448952,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Schilling, K.","contributorId":101423,"corporation":false,"usgs":true,"family":"Schilling","given":"K.","affiliations":[],"preferred":false,"id":448956,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Schultz, Ronald","contributorId":13815,"corporation":false,"usgs":false,"family":"Schultz","given":"Ronald","email":"","affiliations":[],"preferred":false,"id":448951,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70035027,"text":"70035027 - 2011 - Evaluating the effect of predators on white-tailed deer: Movement and diet of coyotes","interactions":[],"lastModifiedDate":"2017-04-06T13:43:08","indexId":"70035027","displayToPublicDate":"2011-01-01T00:00:00","publicationYear":"2011","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":"Evaluating the effect of predators on white-tailed deer: Movement and diet of coyotes","docAbstract":"<p><span>Coyotes (</span><i>Canis latrans</i><span>) may affect adult and neonate white-tailed deer (</span><i>Odocoileus virginianus</i><span>) survival and have been implicated as a contributor to the decline of deer populations. Additionally, coyote diet composition is influenced by prey availability, season, and region. Because coyote movement and diet vary by region, local data are important to understand coyote population dynamics and their impact on prey species. In southeast Minnesota, we investigated the effect of coyotes on white-tailed deer populations by documenting movement rates, distances moved, and habitats searched by coyotes during fawning and nonfawning periods. Additionally, we determined survival, cause-specific mortality, and seasonal diet composition of coyotes. From 2001 to 2003, we captured and radiocollared 30 coyotes. Per-hour rate of movement averaged 0.87 km and was greater (</span><i>P</i><span> = 0.046) during the fawning (1.07 km) than the nonfawning period (0.80 km); areas searched were similar (</span><i>P</i><span> = 0.175) between seasons. Coyote habitat use differed during both seasons; habitats were not used in proportion to their availability (</span><i>P</i><span> &lt; 0.001). Croplands were used more (</span><i>P</i><span> &lt; 0.001) than their proportional availability during both seasons. Use of grasslands was greater during the fawning period (</span><i>P</i><span> = 0.030), whereas use of cropland was greater in the nonfawning period (</span><i>P</i><span> &lt; 0.001). We collected 66 fecal samples during the nonfawning period; coyote diets were primarily composed of </span><i>Microtus</i><span> spp. (65.2%), and consumption of deer was 9.1%. During the study, 19 coyotes died; annual survival rate range was 0.33–0.41, which was low compared with other studies. Consumption of deer was low and coyotes searched open areas (i.e., cropland) more than fawning areas with dense cover. These factors in addition to high coyote mortality suggested that coyote predation was not likely limiting white-tailed deer populations in southeast Minnesota. </span></p>","language":"English","publisher":"Wiley","doi":"10.1002/jwmg.109","issn":"0022541X","usgsCitation":"Turner, M., Rockhill, A., Deperno, C., Jenks, J., Klaver, R., Jarding, A., Grovenburg, T., and Pollock, K.H., 2011, Evaluating the effect of predators on white-tailed deer: Movement and diet of coyotes: Journal of Wildlife Management, v. 75, no. 4, p. 905-912, https://doi.org/10.1002/jwmg.109.","productDescription":"8 p.","startPage":"905","endPage":"912","numberOfPages":"8","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":242853,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":215081,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1002/jwmg.109"}],"volume":"75","issue":"4","noUsgsAuthors":false,"publicationDate":"2011-05-25","publicationStatus":"PW","scienceBaseUri":"505a0bf7e4b0c8380cd52983","contributors":{"authors":[{"text":"Turner, M.M.","contributorId":26895,"corporation":false,"usgs":true,"family":"Turner","given":"M.M.","email":"","affiliations":[],"preferred":false,"id":448943,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rockhill, A.P.","contributorId":70200,"corporation":false,"usgs":true,"family":"Rockhill","given":"A.P.","affiliations":[],"preferred":false,"id":448947,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Deperno, C.S.","contributorId":97870,"corporation":false,"usgs":true,"family":"Deperno","given":"C.S.","affiliations":[],"preferred":false,"id":448949,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Jenks, J.A.","contributorId":31726,"corporation":false,"usgs":true,"family":"Jenks","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":448944,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Klaver, R. W. 0000-0002-3263-9701","orcid":"https://orcid.org/0000-0002-3263-9701","contributorId":50267,"corporation":false,"usgs":true,"family":"Klaver","given":"R. W.","affiliations":[],"preferred":false,"id":448945,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Jarding, A.R.","contributorId":108329,"corporation":false,"usgs":true,"family":"Jarding","given":"A.R.","affiliations":[],"preferred":false,"id":448950,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Grovenburg, T.W.","contributorId":78163,"corporation":false,"usgs":true,"family":"Grovenburg","given":"T.W.","affiliations":[],"preferred":false,"id":448948,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Pollock, K. H.","contributorId":65184,"corporation":false,"usgs":false,"family":"Pollock","given":"K.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":448946,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":70035026,"text":"70035026 - 2011 - Late Quaternary environmental change inferred from phytoliths and other soil-related proxies: Case studies from the central and southern Great Plains, USA","interactions":[],"lastModifiedDate":"2021-03-04T14:28:18.184017","indexId":"70035026","displayToPublicDate":"2011-01-01T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1198,"text":"Catena","active":true,"publicationSubtype":{"id":10}},"title":"Late Quaternary environmental change inferred from phytoliths and other soil-related proxies: Case studies from the central and southern Great Plains, USA","docAbstract":"<p id=\"sp0130\">This study investigates stable carbon isotopes (<i>δ</i><sup>13</sup>C), opal phytolith assemblages, burnt phytoliths, microscopic charcoal and<span>&nbsp;</span><i>Sporormiella</i><span>&nbsp;</span>spores from modern soils and paleosols in Kansas and Oklahoma. Grass and dicot phytoliths in combination with<span>&nbsp;</span><i>δ</i><sup>13</sup>C are used as proxies for reconstructing the structure of grasslands and woodlands. Burnt grass phytoliths and microscopic charcoal are evaluated as proxies for reconstructing paleofire incidence. Concentrations of the fungal spore<span>&nbsp;</span><i>Sporormiella</i><span>&nbsp;</span>are used as a proxy for assessing large herbivore activity. These proxies were tested on various modern grassland communities of the central and southern Great Plains, including areas with bison, cattle, and small herbivores, and areas under different fire frequencies.</p><p id=\"sp0135\">Opal phytolith assemblages and<span>&nbsp;</span><i>δ</i><sup>13</sup>C values show that before cal 11&nbsp;ka, C<sub>3</sub><span>&nbsp;</span>grasses and woody plants predominated in areas that today are dominated by C<sub>4</sub><span>&nbsp;</span>grasses. The origin of the shortgrass prairie dates back to about cal 10&nbsp;ka. The origin of the tallgrass prairie, however, is not clear as phytolith data show variable assemblages throughout the Holocene (mixed-grass, tallgrass, and tallgrass–woodland mosaic). Different proxies (burnt phytoliths vs. charcoal) reveal different fire frequencies, but it is apparent that microfossil evidence for fire incidence is closely related to the abundance of woody plants in the landscape.</p><p id=\"sp0140\">Before cal 12&nbsp;ka, soils show somewhat elevated concentration of<span>&nbsp;</span><i>Sporormiella</i>, but lower concentrations than the modern high-density bison and cattle grazing areas. Throughout the Holocene,<span>&nbsp;</span><i>Sporormiella</i><span>&nbsp;</span>frequencies are low, which suggests lower large ungulate densities and perhaps high mobility.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.catena.2010.08.015","issn":"03418162","usgsCitation":"Cordova, C., Johnson, W., Mandel, R., and Palmer, M., 2011, Late Quaternary environmental change inferred from phytoliths and other soil-related proxies: Case studies from the central and southern Great Plains, USA: Catena, v. 85, no. 2, p. 87-108, https://doi.org/10.1016/j.catena.2010.08.015.","productDescription":"22 p.","startPage":"87","endPage":"108","costCenters":[],"links":[{"id":242852,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Colorado, Kansas, New Mexico, Oklahoma, Texas","otherGeospatial":"Central and southern Great Plains","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -107.05078125,\n              31.728167146023935\n            ],\n            [\n              -104.94140625,\n              30.90222470517144\n            ],\n            [\n              -103.53515625,\n              29.152161283318915\n            ],\n            [\n              -101.689453125,\n              29.916852233070173\n            ],\n            [\n              -97.822265625,\n              25.799891182088334\n            ],\n            [\n              -97.20703125,\n              27.527758206861886\n            ],\n            [\n              -93.33984375,\n              29.916852233070173\n            ],\n            [\n              -93.955078125,\n              32.69486597787505\n            ],\n            [\n              -94.5703125,\n              35.460669951495305\n            ],\n            [\n              -94.74609375,\n              39.436192999314095\n            ],\n            [\n              -95.25146484374999,\n              40.06125658140474\n            ],\n            [\n              -102.216796875,\n              40.17887331434696\n            ],\n            [\n              -102.3046875,\n              41.11246878918088\n            ],\n            [\n              -109.3359375,\n              40.97989806962013\n            ],\n            [\n              -109.16015624999999,\n              31.27855085894653\n            ],\n            [\n              -107.9296875,\n              31.27855085894653\n            ],\n            [\n              -107.841796875,\n              31.80289258670676\n            ],\n            [\n              -107.05078125,\n              31.728167146023935\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"85","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a4526e4b0c8380cd67098","contributors":{"authors":[{"text":"Cordova, C.E.","contributorId":8303,"corporation":false,"usgs":true,"family":"Cordova","given":"C.E.","email":"","affiliations":[],"preferred":false,"id":448939,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Johnson, W.C.","contributorId":68003,"corporation":false,"usgs":true,"family":"Johnson","given":"W.C.","email":"","affiliations":[],"preferred":false,"id":448941,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mandel, R.D.","contributorId":58000,"corporation":false,"usgs":true,"family":"Mandel","given":"R.D.","email":"","affiliations":[],"preferred":false,"id":448940,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Palmer, M.W.","contributorId":88703,"corporation":false,"usgs":true,"family":"Palmer","given":"M.W.","email":"","affiliations":[],"preferred":false,"id":448942,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70035025,"text":"70035025 - 2011 - Multimodel inference and adaptive management","interactions":[],"lastModifiedDate":"2018-01-12T12:07:22","indexId":"70035025","displayToPublicDate":"2011-01-01T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2258,"text":"Journal of Environmental Management","active":true,"publicationSubtype":{"id":10}},"title":"Multimodel inference and adaptive management","docAbstract":"<p><span>Ecology is an inherently complex science coping with correlated variables, nonlinear interactions and multiple scales of pattern and process, making it difficult for experiments to result in clear, strong inference. Natural resource managers, policy makers, and stakeholders rely on science to provide timely and accurate management recommendations. However, the time necessary to untangle the complexities of interactions within ecosystems is often far greater than the time available to make management decisions. One method of coping with this problem is multimodel inference. Multimodel inference assesses uncertainty by calculating likelihoods among multiple competing hypotheses, but multimodel inference results are often equivocal. Despite this, there may be pressure for ecologists to provide management recommendations regardless of the strength of their study&rsquo;s inference. We reviewed papers in the Journal of Wildlife Management (JWM) and the journal Conservation Biology (CB) to quantify the prevalence of multimodel inference approaches, the resulting inference (weak versus strong), and how authors dealt with the uncertainty. Thirty-eight percent and 14%, respectively, of articles in the JWM and CB used multimodel inference approaches. Strong inference was rarely observed, with only 7% of JWM and 20% of CB articles resulting in strong inference. We found the majority of weak inference papers in both journals (59%) gave specific management recommendations. Model selection uncertainty was ignored in most recommendations for management. We suggest that adaptive management is an ideal method to resolve uncertainty when research results in weak inference.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.jenvman.2010.10.012","issn":"03014797","usgsCitation":"Rehme, S., Powell, L., and Allen, C.R., 2011, Multimodel inference and adaptive management: Journal of Environmental Management, v. 92, no. 5, p. 1360-1364, https://doi.org/10.1016/j.jenvman.2010.10.012.","startPage":"1360","endPage":"1364","numberOfPages":"5","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-021299","costCenters":[],"links":[{"id":215535,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.jenvman.2010.10.012"},{"id":243346,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"92","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a6031e4b0c8380cd71363","contributors":{"authors":[{"text":"Rehme, S.E.","contributorId":9890,"corporation":false,"usgs":true,"family":"Rehme","given":"S.E.","email":"","affiliations":[],"preferred":false,"id":448936,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Powell, L.A.","contributorId":51262,"corporation":false,"usgs":true,"family":"Powell","given":"L.A.","email":"","affiliations":[],"preferred":false,"id":448937,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Allen, Craig R. 0000-0001-8655-8272 allencr@usgs.gov","orcid":"https://orcid.org/0000-0001-8655-8272","contributorId":1979,"corporation":false,"usgs":true,"family":"Allen","given":"Craig","email":"allencr@usgs.gov","middleInitial":"R.","affiliations":[{"id":200,"text":"Coop Res Unit Seattle","active":true,"usgs":true},{"id":198,"text":"Coop Res Unit Atlanta","active":true,"usgs":true}],"preferred":true,"id":448938,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70034997,"text":"70034997 - 2011 - Greater sage-grouse of Grand Teton National Park: where do they roam?","interactions":[],"lastModifiedDate":"2013-06-02T19:00:19","indexId":"70034997","displayToPublicDate":"2011-01-01T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3014,"text":"Park Science","active":true,"publicationSubtype":{"id":10}},"title":"Greater sage-grouse of Grand Teton National Park: where do they roam?","docAbstract":"Greater sage-grouse (Centrocercus urophasianus) population declines may be caused by range-wide degradation of sagebrush (woody Artemisia spp.) steppe ecosystems. Understanding how greater sage-grouse use the landscape is essential for successful management. We assessed greater sage-grouse habitat selection on a landscape level in Jackson Hole, Wyoming. We used a Geographic Information System (GIS) and radio-collared sage-grouse to compare habitat used and the total available landscape. Greater sage-grouse selected mountain big sagebrush (A. tridentata var. vaseyana) communities or mixed mountain big sagebrush–antelope bitterbrush (Purshia tridentata) communities and avoided low-sagebrush (A. arbuscula) dwarf shrubland. In spring and summer, sage-grouse primarily used sagebrush-dominated habitats on the valley floor and did not concentrate in mesic areas later in the summer as is typical of the species. The diversity of habitats used in winter exceeds that reported in the literature. In winter, Jackson Hole greater sage-grouse moved to hills, where they used various communities in proportion to their availability, including tall deciduous shrublands, cottonwood (Populus angustifolia) stands, exposed hillsides, and aspen (P. tremuloides) stands. Because seasonal habitat selection is not necessarily consistent across populations residing in different landscapes, habitat management should be specific to each population and landscape. This sage-grouse population provides an example that may offer insight into other species with seasonal habitat needs.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Park Science","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"National Park Service","issn":"07359462","usgsCitation":"Chong, G., Wetzel, W., and Holloran, M., 2011, Greater sage-grouse of Grand Teton National Park: where do they roam?: Park Science, v. 27, no. 3, p. 42-49.","productDescription":"8 p.","startPage":"42","endPage":"49","costCenters":[{"id":481,"text":"Northern Rocky Mountain Science Center","active":true,"usgs":true}],"links":[{"id":242885,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":273069,"type":{"id":11,"text":"Document"},"url":"https://www.nature.nps.gov/ParkScience/archive/PDF/Article_PDFs/ParkScience27(3)Winter2010-2011_42-49_Chong_et_al_2761.pdf"}],"country":"United States","otherGeospatial":"Grand Teton National Park","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -110.9489,43.5371 ], [ -110.9489,44.0838 ], [ -110.4202,44.0838 ], [ -110.4202,43.5371 ], [ -110.9489,43.5371 ] ] ] } } ] }","volume":"27","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a2a66e4b0c8380cd5b140","contributors":{"authors":[{"text":"Chong, G.W.","contributorId":54153,"corporation":false,"usgs":true,"family":"Chong","given":"G.W.","email":"","affiliations":[],"preferred":false,"id":448775,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wetzel, W.C.","contributorId":64050,"corporation":false,"usgs":true,"family":"Wetzel","given":"W.C.","email":"","affiliations":[],"preferred":false,"id":448776,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Holloran, M.J.","contributorId":50000,"corporation":false,"usgs":true,"family":"Holloran","given":"M.J.","email":"","affiliations":[],"preferred":false,"id":448774,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70034996,"text":"70034996 - 2011 - U-Pb (zircon) and geochemical constraints on the age, origin, and evolution of Paleozoic arc magmas in the Oyu Tolgoi porphyry Cu-Au district, southern Mongolia","interactions":[],"lastModifiedDate":"2021-03-03T18:07:09.03165","indexId":"70034996","displayToPublicDate":"2011-01-01T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1848,"text":"Gondwana Research","active":true,"publicationSubtype":{"id":10}},"title":"U-Pb (zircon) and geochemical constraints on the age, origin, and evolution of Paleozoic arc magmas in the Oyu Tolgoi porphyry Cu-Au district, southern Mongolia","docAbstract":"<p><span>Uranium–Pb (zircon) ages are linked with geochemical data for&nbsp;<a title=\"Learn more about Porphyry from ScienceDirect's AI-generated Topic Pages\" href=\"https://www.sciencedirect.com/topics/earth-and-planetary-sciences/porphyry\" data-mce-href=\"https://www.sciencedirect.com/topics/earth-and-planetary-sciences/porphyry\">porphyry</a>&nbsp;intrusions associated with giant porphyry Cu–Au systems at Oyu Tolgoi to place those rocks within the&nbsp;<a title=\"Learn more about Petrochemical from ScienceDirect's AI-generated Topic Pages\" href=\"https://www.sciencedirect.com/topics/earth-and-planetary-sciences/petrochemical\" data-mce-href=\"https://www.sciencedirect.com/topics/earth-and-planetary-sciences/petrochemical\">petrochemical</a>&nbsp;framework of&nbsp;<a title=\"Learn more about Devonian from ScienceDirect's AI-generated Topic Pages\" href=\"https://www.sciencedirect.com/topics/earth-and-planetary-sciences/devonian\" data-mce-href=\"https://www.sciencedirect.com/topics/earth-and-planetary-sciences/devonian\">Devonian</a>&nbsp;and Carboniferous rocks of southern Mongolia. In this part of the Gurvansayhan&nbsp;<a title=\"Learn more about Terrane from ScienceDirect's AI-generated Topic Pages\" href=\"https://www.sciencedirect.com/topics/earth-and-planetary-sciences/terrane\" data-mce-href=\"https://www.sciencedirect.com/topics/earth-and-planetary-sciences/terrane\">terrane</a>&nbsp;within the Central Asian&nbsp;<a title=\"Learn more about Orogenic Belt from ScienceDirect's AI-generated Topic Pages\" href=\"https://www.sciencedirect.com/topics/earth-and-planetary-sciences/orogenic-belt\" data-mce-href=\"https://www.sciencedirect.com/topics/earth-and-planetary-sciences/orogenic-belt\">Orogenic Belt</a>, the transition from Devonian tholeiitic marine rocks to unconformably overlying Carboniferous calc-alkaline subaerial to shallow marine volcanic rocks reflects&nbsp;<a title=\"Learn more about Volcanic Arc from ScienceDirect's AI-generated Topic Pages\" href=\"https://www.sciencedirect.com/topics/earth-and-planetary-sciences/volcanic-arc\" data-mce-href=\"https://www.sciencedirect.com/topics/earth-and-planetary-sciences/volcanic-arc\">volcanic arc</a>&nbsp;thickening and maturation. Radiogenic Nd and Pb&nbsp;<a title=\"Learn more about Isotopic Composition from ScienceDirect's AI-generated Topic Pages\" href=\"https://www.sciencedirect.com/topics/earth-and-planetary-sciences/isotopic-composition\" data-mce-href=\"https://www.sciencedirect.com/topics/earth-and-planetary-sciences/isotopic-composition\">isotopic compositions</a>&nbsp;(</span><i>ε</i><sub>Nd(t)</sub><span>&nbsp;range from +</span><span>&nbsp;</span><span>3.1 to +</span><span>&nbsp;</span><span>7.5 and&nbsp;</span><sup>206</sup><span>Pb/</span><sup>204</sup><span>Pb values for&nbsp;<a title=\"Learn more about Feldspar from ScienceDirect's AI-generated Topic Pages\" href=\"https://www.sciencedirect.com/topics/earth-and-planetary-sciences/feldspar\" data-mce-href=\"https://www.sciencedirect.com/topics/earth-and-planetary-sciences/feldspar\">feldspars</a>&nbsp;range from 17.97 to 18.72), as well as low high-field strength element (HFSE) contents of most rocks (mafic rocks typically have &lt;</span><span>&nbsp;</span><span>1.5% TiO</span><sub>2</sub><span>) are consistent with&nbsp;<a title=\"Learn more about Magma from ScienceDirect's AI-generated Topic Pages\" href=\"https://www.sciencedirect.com/topics/earth-and-planetary-sciences/magma\" data-mce-href=\"https://www.sciencedirect.com/topics/earth-and-planetary-sciences/magma\">magma</a>&nbsp;derivation from depleted mantle in an intra-oceanic volcanic arc. The&nbsp;<a title=\"Learn more about Late Devonian from ScienceDirect's AI-generated Topic Pages\" href=\"https://www.sciencedirect.com/topics/earth-and-planetary-sciences/late-devonian\" data-mce-href=\"https://www.sciencedirect.com/topics/earth-and-planetary-sciences/late-devonian\">Late Devonian</a>&nbsp;and Carboniferous&nbsp;<a title=\"Learn more about Felsic Rock from ScienceDirect's AI-generated Topic Pages\" href=\"https://www.sciencedirect.com/topics/earth-and-planetary-sciences/felsic-rock\" data-mce-href=\"https://www.sciencedirect.com/topics/earth-and-planetary-sciences/felsic-rock\">felsic rocks</a>&nbsp;are dominantly medium- to high-K calc-alkaline and characterized by a decrease in Sr/Y ratios through time, with the Carboniferous rocks being more felsic than those of Devonian age. Porphyry Cu–Au related intrusions were emplaced in the Late Devonian during the transition from tholeiitic to calc-alkaline arc&nbsp;<a title=\"Learn more about Magmatism from ScienceDirect's AI-generated Topic Pages\" href=\"https://www.sciencedirect.com/topics/earth-and-planetary-sciences/magmatism\" data-mce-href=\"https://www.sciencedirect.com/topics/earth-and-planetary-sciences/magmatism\">magmatism</a>. Uranium–Pb (zircon)&nbsp;<a title=\"Learn more about Geochronology from ScienceDirect's AI-generated Topic Pages\" href=\"https://www.sciencedirect.com/topics/earth-and-planetary-sciences/geochronology\" data-mce-href=\"https://www.sciencedirect.com/topics/earth-and-planetary-sciences/geochronology\">geochronology</a>&nbsp;indicates that the Late Devonian pre- to syn-mineral&nbsp;<a title=\"Learn more about Quartz from ScienceDirect's AI-generated Topic Pages\" href=\"https://www.sciencedirect.com/topics/earth-and-planetary-sciences/quartz\" data-mce-href=\"https://www.sciencedirect.com/topics/earth-and-planetary-sciences/quartz\">quartz</a>&nbsp;monzodiorite intrusions associated with the porphyry Cu–Au deposits are ~</span><span>&nbsp;</span><span>372</span><span>&nbsp;</span><span>Ma, whereas&nbsp;<a title=\"Learn more about Granodiorite from ScienceDirect's AI-generated Topic Pages\" href=\"https://www.sciencedirect.com/topics/earth-and-planetary-sciences/granodiorite\" data-mce-href=\"https://www.sciencedirect.com/topics/earth-and-planetary-sciences/granodiorite\">granodiorite</a>&nbsp;intrusions that post-date major shortening and are associated with less well-developed porphyry Cu–Au&nbsp;<a title=\"Learn more about Mineralization from ScienceDirect's AI-generated Topic Pages\" href=\"https://www.sciencedirect.com/topics/earth-and-planetary-sciences/mineralization\" data-mce-href=\"https://www.sciencedirect.com/topics/earth-and-planetary-sciences/mineralization\">mineralization</a>&nbsp;are ~</span><span>&nbsp;</span><span>366</span><span>&nbsp;</span><span>Ma.&nbsp;<a title=\"Learn more about Trace Element Geochemistry from ScienceDirect's AI-generated Topic Pages\" href=\"https://www.sciencedirect.com/topics/earth-and-planetary-sciences/trace-element-geochemistry\" data-mce-href=\"https://www.sciencedirect.com/topics/earth-and-planetary-sciences/trace-element-geochemistry\">Trace element geochemistry</a>&nbsp;of zircons in the Late Devonian intrusions associated with the porphyry Cu–Au systems contain distinct Th/U and Yb/Gd ratios, as well as Hf and Y concentrations that reflect mixing of magma of distinct compositions. These characteristics are missing in the unmineralized Carboniferous intrusions. High Sr/Y and evidence for magma mixing in syn- to late-mineral intrusions distinguish the Late Devonian rocks associated with giant Cu–Au deposits from younger magmatic suites in the district.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.gr.2010.11.012","issn":"1342937X","usgsCitation":"Wainwright, A., Tosdal, R., Wooden, J.L., Mazdab, F., and Friedman, R., 2011, U-Pb (zircon) and geochemical constraints on the age, origin, and evolution of Paleozoic arc magmas in the Oyu Tolgoi porphyry Cu-Au district, southern Mongolia: Gondwana Research, v. 19, no. 3, p. 764-787, https://doi.org/10.1016/j.gr.2010.11.012.","productDescription":"24 p.","startPage":"764","endPage":"787","costCenters":[],"links":[{"id":242884,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":215110,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.gr.2010.11.012"}],"country":"Mongolia","otherGeospatial":"Southern Mongolia","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              87.802734375,\n              48.922499263758255\n            ],\n            [\n              89.736328125,\n              47.517200697839414\n            ],\n            [\n              90.791015625,\n              45.336701909968134\n            ],\n            [\n              96.328125,\n              42.87596410238256\n            ],\n            [\n              104.501953125,\n              41.902277040963696\n            ],\n            [\n              111.884765625,\n              43.89789239125797\n            ],\n            [\n              111.181640625,\n              44.96479793033101\n            ],\n            [\n              113.5546875,\n              44.96479793033101\n            ],\n            [\n              119.53125,\n              46.6795944656402\n            ],\n            [\n              118.65234374999999,\n              47.517200697839414\n            ],\n            [\n              110.478515625,\n              46.98025235521883\n            ],\n            [\n              99.580078125,\n              47.57652571374621\n            ],\n            [\n              87.802734375,\n              48.922499263758255\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"19","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb9bce4b08c986b327d8a","contributors":{"authors":[{"text":"Wainwright, A.J.","contributorId":34737,"corporation":false,"usgs":true,"family":"Wainwright","given":"A.J.","email":"","affiliations":[],"preferred":false,"id":448770,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tosdal, R. M.","contributorId":54982,"corporation":false,"usgs":true,"family":"Tosdal","given":"R. M.","affiliations":[],"preferred":false,"id":448772,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wooden, J. L.","contributorId":58678,"corporation":false,"usgs":true,"family":"Wooden","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":448773,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Mazdab, F.K.","contributorId":11650,"corporation":false,"usgs":true,"family":"Mazdab","given":"F.K.","email":"","affiliations":[],"preferred":false,"id":448769,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Friedman, R.M.","contributorId":43997,"corporation":false,"usgs":true,"family":"Friedman","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":448771,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70034994,"text":"70034994 - 2011 - Transient changes in shallow groundwater chemistry during the MSU ZERT CO2 injection experiment","interactions":[],"lastModifiedDate":"2021-03-08T17:38:55.752959","indexId":"70034994","displayToPublicDate":"2011-01-01T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Transient changes in shallow groundwater chemistry during the MSU ZERT CO2 injection experiment","docAbstract":"<div id=\"abstracts\" class=\"Abstracts u-font-serif\"><div id=\"aep-abstract-id12\" class=\"abstract author\" lang=\"en\"><div id=\"aep-abstract-sec-id13\"><p id=\"sp000005\">Food-grade CO<sub>2</sub><span>&nbsp;</span>was injected into a shallow aquifer through a perforated pipe placed horizontally 1–2&nbsp;m below the water table at the Montana State University Zero Emission Research and Technology (MSU-ZERT) field site at Bozeman, Montana. The possible impact of elevated CO<sub>2</sub><span>&nbsp;</span>levels on groundwater quality was investigated by analyzing 80 water samples taken before, during, and following CO<sub>2</sub><span>&nbsp;</span>injection. Field determinations and laboratory analyses showed rapid and systematic changes in pH, alkalinity, and conductance, as well as increases in the aqueous concentrations of trace element species. The geochemical data were first evaluated using principal component analysis (PCA) in order to identify correlations between aqueous species. The PCA findings were then used in formulating a geochemical model to simulate the processes likely to be responsible for the observed increases in the concentrations of dissolved constituents. Modeling was conducted taking into account aqueous and surface complexation, cation exchange, and mineral precipitation and dissolution. Reasonable matches between measured data and model results suggest that: (1) CO<sub>2</sub><span>&nbsp;</span>dissolution in the groundwater causes calcite to dissolve. (2) Observed increases in the concentration of dissolved trace metals result likely from Ca<sup>+2</sup>-driven ion exchange with clays (smectites) and sorption/desorption reactions likely involving Fe (hydr)oxides. (3) Bicarbonate from CO<sub>2</sub><span>&nbsp;</span>dissolution appears to compete for sorption with anionic species such as HAsO<sub>4</sub><sup>−2</sup>, potentially increasing dissolved As levels in groundwater.</p></div></div></div>","largerWorkTitle":"Energy Procedia","conferenceTitle":"10th International Conference on Greenhouse Gas Control Technologies","conferenceDate":"September 19-23, 2010","conferenceLocation":"Amsterdam","language":"English","publisher":"Elsevier","doi":"10.1016/j.egypro.2011.02.241","issn":"18766102","usgsCitation":"Apps, J.A., Zheng, L., Spycher, N., Birkholzer, J., Kharaka, Y.K., Thordsen, J., Kakouros, E., and Trautz, R., 2011, Transient changes in shallow groundwater chemistry during the MSU ZERT CO2 injection experiment, <i>in</i> Energy Procedia, v. 4, Amsterdam, September 19-23, 2010, p. 3231-3238, https://doi.org/10.1016/j.egypro.2011.02.241.","productDescription":"8 p.","startPage":"3231","endPage":"3238","costCenters":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"links":[{"id":475072,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1016/j.egypro.2011.02.241","text":"Publisher Index Page"},{"id":243343,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":215532,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.egypro.2011.02.241"}],"volume":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb6f9e4b08c986b326f98","contributors":{"authors":[{"text":"Apps, J. A.","contributorId":60386,"corporation":false,"usgs":false,"family":"Apps","given":"J.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":448749,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Zheng, Lingyun","contributorId":68495,"corporation":false,"usgs":true,"family":"Zheng","given":"Lingyun","email":"","affiliations":[],"preferred":false,"id":448751,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Spycher, N.","contributorId":54424,"corporation":false,"usgs":true,"family":"Spycher","given":"N.","email":"","affiliations":[],"preferred":false,"id":448748,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Birkholzer, J.T.","contributorId":18596,"corporation":false,"usgs":true,"family":"Birkholzer","given":"J.T.","email":"","affiliations":[],"preferred":false,"id":448746,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Kharaka, Yousif K. 0000-0001-9861-8260 ykharaka@usgs.gov","orcid":"https://orcid.org/0000-0001-9861-8260","contributorId":1928,"corporation":false,"usgs":true,"family":"Kharaka","given":"Yousif","email":"ykharaka@usgs.gov","middleInitial":"K.","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":448750,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Thordsen, James J. jthordsn@usgs.gov","contributorId":3329,"corporation":false,"usgs":true,"family":"Thordsen","given":"James J.","email":"jthordsn@usgs.gov","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":448753,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Kakouros, Evangelos 0000-0002-4778-4039 kakouros@usgs.gov","orcid":"https://orcid.org/0000-0002-4778-4039","contributorId":2587,"corporation":false,"usgs":true,"family":"Kakouros","given":"Evangelos","email":"kakouros@usgs.gov","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true},{"id":37464,"text":"WMA - Laboratory & Analytical Services Division","active":true,"usgs":true}],"preferred":true,"id":448747,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Trautz, R.","contributorId":95290,"corporation":false,"usgs":true,"family":"Trautz","given":"R.","affiliations":[],"preferred":false,"id":448752,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":70034992,"text":"70034992 - 2011 - Hydrostratigraphic analysis of the MADE site with full-resolution GPR and direct-push hydraulic profiling","interactions":[],"lastModifiedDate":"2021-03-03T18:44:03.210543","indexId":"70034992","displayToPublicDate":"2011-01-01T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1807,"text":"Geophysical Research Letters","active":true,"publicationSubtype":{"id":10}},"title":"Hydrostratigraphic analysis of the MADE site with full-resolution GPR and direct-push hydraulic profiling","docAbstract":"<p><span class=\"paraNumber\"><span>&nbsp;</span></span><span>Full‐resolution 3D Ground‐Penetrating Radar (GPR) data were combined with high‐resolution hydraulic conductivity (</span><i>K</i><span>) data from vertical Direct‐Push (DP) profiles to characterize a portion of the highly heterogeneous MAcro Dispersion Experiment (MADE) site. This is an important first step to better understand the influence of aquifer heterogeneities on observed anomalous transport. Statistical evaluation of DP data indicates non‐normal distributions that have much higher similarity within each GPR facies than between facies. The analysis of GPR and DP data provides high‐resolution estimates of the 3D geometry of hydrostratigraphic zones, which can then be populated with stochastic&nbsp;</span><i>K</i><span>&nbsp;fields. The lack of such estimates has been a significant limitation for testing and parameterizing a range of novel transport theories at sites where the traditional advection‐dispersion model has proven inadequate.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/2010GL046439","issn":"00948276","usgsCitation":"Dogan, M., Van Dam, R.L., Bohling, G.C., Butler, J., and Hyndman, D., 2011, Hydrostratigraphic analysis of the MADE site with full-resolution GPR and direct-push hydraulic profiling: Geophysical Research Letters, v. 38, no. 6, L06405, 6 p., https://doi.org/10.1029/2010GL046439.","productDescription":"L06405, 6 p.","costCenters":[],"links":[{"id":475062,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1029/2010gl046439","text":"Publisher Index Page"},{"id":243282,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":215474,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1029/2010GL046439"}],"country":"United States","state":"Mississippi","otherGeospatial":"Columbus Air Force Base","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -88.49178314208983,\n              33.59374516555303\n            ],\n            [\n              -88.39736938476562,\n              33.59374516555303\n            ],\n            [\n              -88.39736938476562,\n              33.68521069542541\n            ],\n            [\n              -88.49178314208983,\n              33.68521069542541\n            ],\n            [\n              -88.49178314208983,\n              33.59374516555303\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"38","issue":"6","noUsgsAuthors":false,"publicationDate":"2011-03-22","publicationStatus":"PW","scienceBaseUri":"505a378be4b0c8380cd60f69","contributors":{"authors":[{"text":"Dogan, M.","contributorId":81708,"corporation":false,"usgs":true,"family":"Dogan","given":"M.","email":"","affiliations":[],"preferred":false,"id":448740,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Van Dam, R. L.","contributorId":64473,"corporation":false,"usgs":true,"family":"Van Dam","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":448739,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bohling, Geoffrey C.","contributorId":43109,"corporation":false,"usgs":false,"family":"Bohling","given":"Geoffrey","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":448738,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Butler, J.J. Jr.","contributorId":12194,"corporation":false,"usgs":true,"family":"Butler","given":"J.J.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":448737,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Hyndman, D.W.","contributorId":83318,"corporation":false,"usgs":true,"family":"Hyndman","given":"D.W.","email":"","affiliations":[],"preferred":false,"id":448741,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70034990,"text":"70034990 - 2011 - Population cycles are highly correlated over long time series and large spatial scales in two unrelated species: Greater sage-grouse and cottontail rabbits","interactions":[],"lastModifiedDate":"2021-03-03T19:12:33.947741","indexId":"70034990","displayToPublicDate":"2011-01-01T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2932,"text":"Oecologia","active":true,"publicationSubtype":{"id":10}},"title":"Population cycles are highly correlated over long time series and large spatial scales in two unrelated species: Greater sage-grouse and cottontail rabbits","docAbstract":"<p><span>Animal species across multiple taxa demonstrate multi-annual population cycles, which have long been of interest to ecologists. Correlated population cycles between species that do not share a predator–prey relationship are particularly intriguing and challenging to explain. We investigated annual population trends of greater sage-grouse (</span><i>Centrocercus urophasianus</i><span>) and cottontail rabbits (</span><i>Sylvilagus</i><span>&nbsp;sp.) across Wyoming to explore the possibility of correlations between unrelated species, over multiple cycles, very large spatial areas, and relatively southern latitudes in terms of cycling species. We analyzed sage-grouse lek counts and annual hunter harvest indices from 1982 to 2007. We show that greater sage-grouse, currently listed as warranted but precluded under the US Endangered Species Act, and cottontails have highly correlated cycles (</span><i>r</i><span>&nbsp;=&nbsp;0.77). We explore possible mechanistic hypotheses to explain the synchronous population cycles. Our research highlights the importance of control populations in both adaptive management and impact studies. Furthermore, we demonstrate the functional value of these indices (lek counts and hunter harvest) for tracking broad-scale fluctuations in the species. This level of highly correlated long-term cycling has not previously been documented between two non-related species, over a long time-series, very large spatial scale, and within more southern latitudes.</span></p>","language":"English","publisher":"Springer Link","doi":"10.1007/s00442-010-1768-0","issn":"00298549","usgsCitation":"Fedy, B., and Doherty, K., 2011, Population cycles are highly correlated over long time series and large spatial scales in two unrelated species: Greater sage-grouse and cottontail rabbits: Oecologia, v. 165, no. 4, p. 915-924, https://doi.org/10.1007/s00442-010-1768-0.","productDescription":"10 p.","startPage":"915","endPage":"924","costCenters":[],"links":[{"id":243249,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":215442,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/s00442-010-1768-0"}],"country":"United States","state":"Wyoming","otherGeospatial":"Wyoming","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -111.005859375,\n              41.0130657870063\n            ],\n            [\n              -104.0625,\n              41.0130657870063\n            ],\n            [\n              -104.0625,\n              44.96479793033101\n            ],\n            [\n              -111.005859375,\n              44.96479793033101\n            ],\n            [\n              -111.005859375,\n              41.0130657870063\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"165","issue":"4","noUsgsAuthors":false,"publicationDate":"2010-09-17","publicationStatus":"PW","scienceBaseUri":"505a7d33e4b0c8380cd79deb","contributors":{"authors":[{"text":"Fedy, B.C.","contributorId":35427,"corporation":false,"usgs":true,"family":"Fedy","given":"B.C.","email":"","affiliations":[],"preferred":false,"id":448729,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Doherty, K.E.","contributorId":38374,"corporation":false,"usgs":true,"family":"Doherty","given":"K.E.","email":"","affiliations":[],"preferred":false,"id":448730,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70034966,"text":"70034966 - 2011 - Ungulate herbivory on alpine willow in the Sangre de Cristo Mountains of Colorado","interactions":[],"lastModifiedDate":"2021-03-03T19:33:24.394889","indexId":"70034966","displayToPublicDate":"2011-01-01T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3746,"text":"Western North American Naturalist","onlineIssn":"1944-8341","printIssn":"1527-0904","active":true,"publicationSubtype":{"id":10}},"title":"Ungulate herbivory on alpine willow in the Sangre de Cristo Mountains of Colorado","docAbstract":"<p><span>In many areas of the Rocky Mountains, elk (</span><i>Cervus elaphus</i><span>) migrate from low-elevation mountain valleys during spring to high-elevation subalpine and alpine areas for the summer. Research has focused on the impacts of elk herbivory on winter-range plant communities, particularly on woody species such as willow and aspen; however, little information is available on the effects of elk herbivory on alpine willows. In the Sangre de Cristo Mountains of south central Colorado, select alpine areas appear to receive high levels of summer elk herbivory, while other areas are nearly unbrowsed. In 2005 and 2008, we measured willow height, cover, and utilization on sites that appeared to be used heavily by elk, as well as on sites that appeared to be used lightly, to determine differences between these communities over time. We found less willow cover and shorter willows at sites that received higher levels of browsing compared to those that had lower levels of browsing. Human recreational use was greater at lightly browsed sites than at highly browsed sites. From 2005 to 2008, willow utilization declined, and willow cover and height increased at sites with heavy browsing, likely owing to ownership change of adjacent valley land which led to (1) removal of grazing competition from, cattle at valley locations and (2) increased human use in alpine areas, which displaced elk. We discuss the implications of increased human use and climate change on elk use of these alpine habitats.</span></p>","language":"English","publisher":"BioOne","doi":"10.3398/064.071.0112","issn":"15270904","usgsCitation":"Zeigenfuss, L., Schoenecker, K.A., and Amburg, L., 2011, Ungulate herbivory on alpine willow in the Sangre de Cristo Mountains of Colorado: Western North American Naturalist, v. 71, no. 1, p. 86-96, https://doi.org/10.3398/064.071.0112.","productDescription":"11 p.","startPage":"86","endPage":"96","costCenters":[],"links":[{"id":487796,"rank":10000,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://scholarsarchive.byu.edu/wnan/vol71/iss1/12","text":"External Repository"},{"id":243872,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":216033,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.3398/064.071.0112"}],"country":"United States","otherGeospatial":"Rocky Mountains","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -107.841796875,\n              37.23907530202184\n            ],\n            [\n              -105.084228515625,\n              37.23907530202184\n            ],\n            [\n              -105.084228515625,\n              38.453588708941375\n            ],\n            [\n              -107.841796875,\n              38.453588708941375\n            ],\n            [\n              -107.841796875,\n              37.23907530202184\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"71","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bbc7ce4b08c986b328c5b","contributors":{"authors":[{"text":"Zeigenfuss, Linda 0000-0002-6700-8563 linda_zeigenfuss@usgs.gov","orcid":"https://orcid.org/0000-0002-6700-8563","contributorId":2079,"corporation":false,"usgs":true,"family":"Zeigenfuss","given":"Linda","email":"linda_zeigenfuss@usgs.gov","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":true,"id":448622,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schoenecker, Kathryn A. 0000-0001-9906-911X schoeneckerk@usgs.gov","orcid":"https://orcid.org/0000-0001-9906-911X","contributorId":2001,"corporation":false,"usgs":true,"family":"Schoenecker","given":"Kathryn","email":"schoeneckerk@usgs.gov","middleInitial":"A.","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":true,"id":448623,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Amburg, L.K.V.","contributorId":48408,"corporation":false,"usgs":true,"family":"Amburg","given":"L.K.V.","email":"","affiliations":[],"preferred":false,"id":448621,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70034965,"text":"70034965 - 2011 - The distance that contaminated aquatic subsidies extend into lake riparian zones","interactions":[],"lastModifiedDate":"2021-03-03T19:44:53.745549","indexId":"70034965","displayToPublicDate":"2011-01-01T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1450,"text":"Ecological Applications","active":true,"publicationSubtype":{"id":10}},"title":"The distance that contaminated aquatic subsidies extend into lake riparian zones","docAbstract":"<p><span>Consumption of emergent aquatic insects by terrestrial invertebrates is a poorly resolved, but potentially important, mechanism of contaminant flux across ecosystem borders leading to contaminant exposure in terrestrial invertivores. We characterized the spatial extent and magnitude of contaminant transfer from aquatic sediments to terrestrial invertebrate predators by examining riparian araneid spiders, terrestrial insects, and emergent aquatic insects for stable isotopes and polychlorinated biphenyls (PCBs, sum of 141 congeners) at Lake Hartwell, (Clemson, South Carolina, USA). PCB concentrations in aquatic insects were orders of magnitude higher than in terrestrial insects. Aquatic insect consumption by spiders (as indicated by δ</span><sup>13</sup><span>C and δ</span><sup>15</sup><span>N), PCB concentrations in spiders, and aquatic prey availability were greatest at the shoreline and declined inland, while terrestrial prey availability was invariant with distance. These patterns indicate PCB transfer to spiders through consumption of emergent aquatic insects extending to a distance of ∼5 m inland. Measurable, but much lower, PCBs were present in insect predators dominated by social wasps up to 30 m inland. These results illustrate the importance of emergent insects as vectors of contaminant transfer from lake sediments to riparian food webs, and that spiders are key predators in this process.</span></p>","language":"English","publisher":"Ecological Society of America","doi":"10.1890/09-1504.1","issn":"10510761","usgsCitation":"Raikow, D., Walters, D., Fritz, K., and Mills, M., 2011, The distance that contaminated aquatic subsidies extend into lake riparian zones: Ecological Applications, v. 21, no. 3, p. 983-990, https://doi.org/10.1890/09-1504.1.","productDescription":"8 p.","startPage":"983","endPage":"990","costCenters":[],"links":[{"id":243871,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":216032,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1890/09-1504.1"}],"country":"United States","state":"South Carolina","otherGeospatial":"Lake Hartwell","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -82.935791015625,\n              34.555204483709474\n            ],\n            [\n              -82.74215698242188,\n              34.555204483709474\n            ],\n            [\n              -82.74215698242188,\n              34.722426197808446\n            ],\n            [\n              -82.935791015625,\n              34.722426197808446\n            ],\n            [\n              -82.935791015625,\n              34.555204483709474\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"21","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505baac8e4b08c986b3229e7","contributors":{"authors":[{"text":"Raikow, D.F.","contributorId":98972,"corporation":false,"usgs":true,"family":"Raikow","given":"D.F.","email":"","affiliations":[],"preferred":false,"id":448620,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Walters, D.M.","contributorId":41507,"corporation":false,"usgs":true,"family":"Walters","given":"D.M.","email":"","affiliations":[],"preferred":false,"id":448617,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fritz, K.M.","contributorId":93300,"corporation":false,"usgs":true,"family":"Fritz","given":"K.M.","email":"","affiliations":[],"preferred":false,"id":448619,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Mills, M.A.","contributorId":77764,"corporation":false,"usgs":true,"family":"Mills","given":"M.A.","email":"","affiliations":[],"preferred":false,"id":448618,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70034964,"text":"70034964 - 2011 - New optically stimulated luminescence ages provide evidence of MIS3 and MIS2 eolian activity on Black Mesa, northeastern Arizona, USA","interactions":[],"lastModifiedDate":"2021-03-03T20:05:12.137085","indexId":"70034964","displayToPublicDate":"2011-01-01T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3218,"text":"Quaternary Research","active":true,"publicationSubtype":{"id":10}},"title":"New optically stimulated luminescence ages provide evidence of MIS3 and MIS2 eolian activity on Black Mesa, northeastern Arizona, USA","docAbstract":"<p><span>Eolian deposition on the semiarid southern Colorado Plateau has been attributed to episodic aridity during the Quaternary Period. However, OSL ages from three topographically controlled (e.g. falling) dunes on Black Mesa in northeastern Arizona indicate that eolian sediments there were deposited in deep tributary valleys as early as 35–30 ka, with most sand deposited before 20 ka. In contrast, the oldest OSL ages for sand sheets fall within the Pleistocene-Holocene climatic transition (~ 12–8 ka). Thus most eolian sediment accumulated on Black Mesa under climatic conditions that were in general cooler, moister, and more variable than today, not more arid, pointing to a considerable increase in sediment supply.</span></p>","language":"English","publisher":"Cambridge University Press","doi":"10.1016/j.yqres.2010.12.002","issn":"00335894","usgsCitation":"Ellwein, A., Mahan, S.A., and McFadden, L.D., 2011, New optically stimulated luminescence ages provide evidence of MIS3 and MIS2 eolian activity on Black Mesa, northeastern Arizona, USA: Quaternary Research, v. 75, no. 3, p. 395-398, https://doi.org/10.1016/j.yqres.2010.12.002.","productDescription":"4 p.","startPage":"395","endPage":"398","costCenters":[],"links":[{"id":243839,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":216000,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.yqres.2010.12.002"}],"country":"United States","state":"Arizona","otherGeospatial":"Black Mesa, Northeastern Arizona","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -111.46728515624999,\n              35.209721645221386\n            ],\n            [\n              -109.072265625,\n              35.209721645221386\n            ],\n            [\n              -109.072265625,\n              37.00255267215955\n            ],\n            [\n              -111.46728515624999,\n              37.00255267215955\n            ],\n            [\n              -111.46728515624999,\n              35.209721645221386\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"75","issue":"3","noUsgsAuthors":false,"publicationDate":"2017-01-20","publicationStatus":"PW","scienceBaseUri":"505a65f5e4b0c8380cd72cb6","contributors":{"authors":[{"text":"Ellwein, A.L.","contributorId":83354,"corporation":false,"usgs":true,"family":"Ellwein","given":"A.L.","affiliations":[],"preferred":false,"id":448615,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mahan, Shannon A. 0000-0001-5214-7774 smahan@usgs.gov","orcid":"https://orcid.org/0000-0001-5214-7774","contributorId":147159,"corporation":false,"usgs":true,"family":"Mahan","given":"Shannon","email":"smahan@usgs.gov","middleInitial":"A.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":448616,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McFadden, L. D.","contributorId":15765,"corporation":false,"usgs":false,"family":"McFadden","given":"L.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":448614,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70034963,"text":"70034963 - 2011 - Allelopathic cover crop prior to seeding is more important than subsequent grazing/mowing in Grassland establishment","interactions":[],"lastModifiedDate":"2021-03-03T20:25:40.269736","indexId":"70034963","displayToPublicDate":"2011-01-01T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3228,"text":"Rangeland Ecology and Management","onlineIssn":"1551-5028","printIssn":"1550-7424","active":true,"publicationSubtype":{"id":10}},"title":"Allelopathic cover crop prior to seeding is more important than subsequent grazing/mowing in Grassland establishment","docAbstract":"<p><span>The effects of grazing, mowing, and type of cover crop were evaluated in a previous winter wheat–fallow cropland seeded to grassland under the&nbsp;Conservation Reserve Program&nbsp;in eastern Colorado. Prior to seeding, the fallow strips were planted to forage sorghum or wheat in alternating strips (cover crops), with no grazing, moderate to heavy grazing, and mowing (grazing treatments) superimposed 4</span><span>&nbsp;</span><span>yr after planting and studied for 3</span><span>&nbsp;</span><span>yr. Plots previously in wheat had more annual and exotic species than sorghum plots. Concomitantly, there were much greater abundances of&nbsp;perennial&nbsp;native grass and all native species in sorghum than wheat cropped areas. The competitive advantage gained by seeded species in sorghum plots resulted in large increases in rhizomatous western wheatgrass. Sorghum is known to be allelopathic and is used in crop agriculture rotations to suppress weeds and&nbsp;increase crop yields, consistent with the responses of weed and desired native species in this study. Grazing treatment had relatively minor effects on basal and canopy cover composition of annual or exotic species versus perennial native grass or native species. Although grazing treatment never was a significant main effect, it occasionally modified cover crop or year effects. Opportunistic grazing reduced exotic&nbsp;cheatgrass&nbsp;by year 3 but also decreased the native palatable western wheatgrass. Mowing was a less effective weed control practice than grazing. Vegetative basal cover and aboveground primary production varied primarily with year. Common management practices for revegetation/restoration currently use herbicides and mowing as weed control practices and restrict grazing in all stages of development. Results suggest that allelopathic cover crop selection and opportunistic grazing can be effective alternative grass establishment and weed control practices. Susceptibility, resistance, and interactions of weed and seeded species to allelopathic cover species/cultivars may be a fruitful area of research.</span></p>","language":"English","publisher":"Elsevier","doi":"10.2111/REM-D-10-00117.1","issn":"15507424","usgsCitation":"Milchunas, D., Vandever, M.W., Ball, L., and Hyberg, S., 2011, Allelopathic cover crop prior to seeding is more important than subsequent grazing/mowing in Grassland establishment: Rangeland Ecology and Management, v. 64, no. 3, p. 291-300, https://doi.org/10.2111/REM-D-10-00117.1.","productDescription":"10 p.","startPage":"291","endPage":"300","costCenters":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"links":[{"id":243838,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":215999,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.2111/REM-D-10-00117.1"}],"volume":"64","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e96be4b0c8380cd48280","contributors":{"authors":[{"text":"Milchunas, D.G.","contributorId":75778,"corporation":false,"usgs":true,"family":"Milchunas","given":"D.G.","affiliations":[],"preferred":false,"id":448611,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Vandever, Mark W. 0000-0003-0247-2629 vandeverm@usgs.gov","orcid":"https://orcid.org/0000-0003-0247-2629","contributorId":197674,"corporation":false,"usgs":true,"family":"Vandever","given":"Mark","email":"vandeverm@usgs.gov","middleInitial":"W.","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":true,"id":448613,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ball, L.O.","contributorId":75779,"corporation":false,"usgs":true,"family":"Ball","given":"L.O.","email":"","affiliations":[],"preferred":false,"id":448612,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hyberg, S.","contributorId":37985,"corporation":false,"usgs":true,"family":"Hyberg","given":"S.","affiliations":[],"preferred":false,"id":448610,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70034961,"text":"70034961 - 2011 - Diagnostic methodology is critical for accurately determining the prevalence of ichthyophonus infections in wild fish populations","interactions":[],"lastModifiedDate":"2013-04-25T08:57:24","indexId":"70034961","displayToPublicDate":"2011-01-01T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2414,"text":"Journal of Parasitology","active":true,"publicationSubtype":{"id":10}},"title":"Diagnostic methodology is critical for accurately determining the prevalence of ichthyophonus infections in wild fish populations","docAbstract":"Several different techniques have been employed to detect and identify Ichthyophonus spp. in infected fish hosts; these include macroscopic observation, microscopic examination of tissue squashes, histological evaluation, in vitro culture, and molecular techniques. Examination of the peer-reviewed literature revealed that when more than 1 diagnostic method is used, they often result in significantly different results; for example, when in vitro culture was used to identify infected trout in an experimentally exposed population, 98.7% of infected trout were detected, but when standard histology was used to confirm known infected tissues from wild salmon, it detected ~50% of low-intensity infections and ~85% of high-intensity infections. Other studies on different species reported similar differences. When we examined a possible mechanism to explain the disparity between different diagnostic techniques, we observed non-random distribution of the parasite in 3-dimensionally visualized tissue sections from infected hosts, thus providing a possible explanation for the different sensitivities of commonly used diagnostic techniques. Based on experimental evidence and a review of the peer-reviewed literature, we have concluded that in vitro culture is currently the most accurate diagnostic technique for determining infection prevalence of Ichthyophonus, particularly when the exposure history of the population is not known.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Parasitology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"American Society of Parasitologists","doi":"10.1645/GE-2589.1","issn":"00223395","usgsCitation":"Kocan, R., Dolan, H., and Hershberger, P., 2011, Diagnostic methodology is critical for accurately determining the prevalence of ichthyophonus infections in wild fish populations: Journal of Parasitology, v. 97, no. 2, p. 344-348, https://doi.org/10.1645/GE-2589.1.","productDescription":"5 p.","startPage":"344","endPage":"348","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":243777,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":215940,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1645/GE-2589.1"}],"volume":"97","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a00a0e4b0c8380cd4f81d","contributors":{"authors":[{"text":"Kocan, R.","contributorId":95665,"corporation":false,"usgs":true,"family":"Kocan","given":"R.","affiliations":[],"preferred":false,"id":448597,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dolan, H.","contributorId":96112,"corporation":false,"usgs":true,"family":"Dolan","given":"H.","email":"","affiliations":[],"preferred":false,"id":448598,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hershberger, P.","contributorId":64826,"corporation":false,"usgs":true,"family":"Hershberger","given":"P.","email":"","affiliations":[],"preferred":false,"id":448596,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70034960,"text":"70034960 - 2011 - Distribution and habitat utilization of the gopher tortoise tick (Amblyomma tuberculatum) in Southern Mississippi","interactions":[],"lastModifiedDate":"2021-03-03T21:01:47.119622","indexId":"70034960","displayToPublicDate":"2011-01-01T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2414,"text":"Journal of Parasitology","active":true,"publicationSubtype":{"id":10}},"title":"Distribution and habitat utilization of the gopher tortoise tick (Amblyomma tuberculatum) in Southern Mississippi","docAbstract":"<p><span>The distribution of the gopher tortoise tick (</span><span class=\"genus-species\">Amblyomma tuberculatum</span><span>) has been considered intrinsically linked to the distribution of its primary host, gopher tortoises (</span><span class=\"genus-species\">Gopherus polyphemus</span><span>). However, the presence of&nbsp;</span><span class=\"genus-species\">G. polyphemus</span><span>&nbsp;does not always equate to the presence of&nbsp;</span><span class=\"genus-species\">A. tuberculatum</span><span>. There is a paucity of data on the ecology, habitat preferences, and distribution of&nbsp;</span><span class=\"genus-species\">A. tuberculatum</span><span>. The goals of this study were to assess the distribution of&nbsp;</span><span class=\"genus-species\">A. tuberculatum</span><span>&nbsp;in southern Mississippi and to determine which, if any, habitat parameters explain the distribution pattern of&nbsp;</span><span class=\"genus-species\">A. tuberculatum</span><span>. During 2006–2007, we examined 13&nbsp;</span><span class=\"genus-species\">G. polyphemus</span><span>&nbsp;populations in southern Mississippi for the presence of&nbsp;</span><span class=\"genus-species\">A. tuberculatum</span><span>, and we measured a suite of habitat parameters at each site. Only 23% of the&nbsp;</span><span class=\"genus-species\">G. polyphemus</span><span>&nbsp;populations supported&nbsp;</span><span class=\"genus-species\">A. tuberculatum</span><span>, suggesting a more restricted distribution than its host. The results of our multivariate analyses identified several habitat variables, e.g., depth of sand and percentage of sand in the topsoil and burrow apron, as being important in discriminating between sites with, and without,&nbsp;</span><span class=\"genus-species\">A. tuberculatum</span><span>.&nbsp;</span><span class=\"genus-species\">Amblyomma tuberculatum</span><span>&nbsp;was only found at sites with a mean sand depth of &gt;100&nbsp;cm and a mean percentage of topsoil and burrow apron sand composition &gt;94.0 and 92.4, respectively. Thus, environmental factors, and not just its host's range, seem to influence the distribution of&nbsp;</span><span class=\"genus-species\">A. tuberculatum</span><span>.</span></p>","language":"English","publisher":"BioOne","doi":"10.1645/GE-2599.1","issn":"00223395","usgsCitation":"Ennen, J., and Qualls, C., 2011, Distribution and habitat utilization of the gopher tortoise tick (Amblyomma tuberculatum) in Southern Mississippi: Journal of Parasitology, v. 97, no. 2, p. 202-206, https://doi.org/10.1645/GE-2599.1.","productDescription":"5 p.","startPage":"202","endPage":"206","costCenters":[],"links":[{"id":215911,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1645/GE-2599.1"},{"id":243747,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Southern Mississippi","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -88.35205078124999,\n              32.175612478499325\n            ],\n            [\n              -91.01074218749999,\n              32.194208672875384\n            ],\n            [\n              -91.669921875,\n              31.071755902820133\n            ],\n            [\n              -89.7802734375,\n              30.977609093348686\n            ],\n            [\n              -89.62646484375,\n              30.12612436422458\n            ],\n            [\n              -88.3740234375,\n              30.315987718557867\n            ],\n            [\n              -88.35205078124999,\n              32.175612478499325\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"97","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0290e4b0c8380cd500db","contributors":{"authors":[{"text":"Ennen, J.R.","contributorId":108335,"corporation":false,"usgs":true,"family":"Ennen","given":"J.R.","affiliations":[],"preferred":false,"id":448595,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Qualls, C.P.","contributorId":37983,"corporation":false,"usgs":true,"family":"Qualls","given":"C.P.","email":"","affiliations":[],"preferred":false,"id":448594,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70034957,"text":"70034957 - 2011 - Sensitivity of leaf size and shape to climate: Global patterns and paleoclimatic applications","interactions":[],"lastModifiedDate":"2021-03-04T12:50:03.948716","indexId":"70034957","displayToPublicDate":"2011-01-01T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2863,"text":"New Phytologist","active":true,"publicationSubtype":{"id":10}},"title":"Sensitivity of leaf size and shape to climate: Global patterns and paleoclimatic applications","docAbstract":"<ul><li><p>Paleobotanists have long used models based on leaf size and shape to reconstruct paleoclimate. However, most models incorporate a single variable or use traits that are not physiologically or functionally linked to climate, limiting their predictive power. Further, they often underestimate paleotemperature relative to other proxies.</p></li><li><p>Here we quantify leaf–climate correlations from 92 globally distributed, climatically diverse sites, and explore potential confounding factors. Multiple linear regression models for mean annual temperature (MAT) and mean annual precipitation (MAP) are developed and applied to nine well‐studied fossil floras.</p></li><li><p>We find that leaves in cold climates typically have larger, more numerous teeth, and are more highly dissected. Leaf habit (deciduous vs evergreen), local water availability, and phylogenetic history all affect these relationships. Leaves in wet climates are larger and have fewer, smaller teeth. Our multivariate MAT and MAP models offer moderate improvements in precision over univariate approaches (± 4.0 vs 4.8°C for MAT) and strong improvements in accuracy. For example, our provisional MAT estimates for most North American fossil floras are considerably warmer and in better agreement with independent paleoclimate evidence.</p></li><li><p>Our study demonstrates that the inclusion of additional leaf traits that are functionally linked to climate improves paleoclimate reconstructions. This work also illustrates the need for better understanding of the impact of phylogeny and leaf habit on leaf–climate relationships.</p></li></ul>","language":"English","publisher":"Wiley","doi":"10.1111/j.1469-8137.2010.03615.x","issn":"0028646X","usgsCitation":"Peppe, D., Royer, D., Cariglino, B., Oliver, S., Newman, S., Leight, E., Enikolopov, G., Fernandez-Burgos, M., Herrera, F., Adams, J., Correa, E., Currano, E., Erickson, J., Hinojosa, L., Hoganson, J., Iglesias, A., Jaramillo, C., Johnson, K., Jordan, G., Kraft, N., Lovelock, E., Lusk, C., Niinemets, U., Penuelas, J., Rapson, G., Wing, S., and Wright, I., 2011, Sensitivity of leaf size and shape to climate: Global patterns and paleoclimatic applications: New Phytologist, v. 190, no. 3, p. 724-739, https://doi.org/10.1111/j.1469-8137.2010.03615.x.","productDescription":"16 p.","startPage":"724","endPage":"739","costCenters":[],"links":[{"id":475524,"rank":1,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1111/j.1469-8137.2010.03615.x","text":"Publisher Index Page"},{"id":243716,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"190","issue":"3","noUsgsAuthors":false,"publicationDate":"2011-02-05","publicationStatus":"PW","scienceBaseUri":"505b8d31e4b08c986b3182c5","contributors":{"authors":[{"text":"Peppe, D.J.","contributorId":53191,"corporation":false,"usgs":true,"family":"Peppe","given":"D.J.","email":"","affiliations":[],"preferred":false,"id":448577,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Royer, D.L.","contributorId":37168,"corporation":false,"usgs":true,"family":"Royer","given":"D.L.","email":"","affiliations":[],"preferred":false,"id":448570,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cariglino, B.","contributorId":30067,"corporation":false,"usgs":true,"family":"Cariglino","given":"B.","email":"","affiliations":[],"preferred":false,"id":448569,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Oliver, S.Y.","contributorId":12285,"corporation":false,"usgs":true,"family":"Oliver","given":"S.Y.","email":"","affiliations":[],"preferred":false,"id":448564,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Newman, S.","contributorId":7678,"corporation":false,"usgs":true,"family":"Newman","given":"S.","affiliations":[],"preferred":false,"id":448559,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Leight, E.","contributorId":12709,"corporation":false,"usgs":true,"family":"Leight","given":"E.","email":"","affiliations":[],"preferred":false,"id":448565,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Enikolopov, G.","contributorId":42452,"corporation":false,"usgs":true,"family":"Enikolopov","given":"G.","email":"","affiliations":[],"preferred":false,"id":448573,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Fernandez-Burgos, M.","contributorId":40444,"corporation":false,"usgs":true,"family":"Fernandez-Burgos","given":"M.","email":"","affiliations":[],"preferred":false,"id":448572,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Herrera, F.","contributorId":101907,"corporation":false,"usgs":true,"family":"Herrera","given":"F.","email":"","affiliations":[],"preferred":false,"id":448584,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Adams, J.M.","contributorId":39213,"corporation":false,"usgs":true,"family":"Adams","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":448571,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Correa, 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J.W.","contributorId":100127,"corporation":false,"usgs":true,"family":"Hoganson","given":"J.W.","email":"","affiliations":[],"preferred":false,"id":448583,"contributorType":{"id":1,"text":"Authors"},"rank":15},{"text":"Iglesias, A.","contributorId":26538,"corporation":false,"usgs":true,"family":"Iglesias","given":"A.","email":"","affiliations":[],"preferred":false,"id":448567,"contributorType":{"id":1,"text":"Authors"},"rank":16},{"text":"Jaramillo, C.A.","contributorId":9891,"corporation":false,"usgs":true,"family":"Jaramillo","given":"C.A.","email":"","affiliations":[],"preferred":false,"id":448561,"contributorType":{"id":1,"text":"Authors"},"rank":17},{"text":"Johnson, K.R.","contributorId":28599,"corporation":false,"usgs":true,"family":"Johnson","given":"K.R.","email":"","affiliations":[],"preferred":false,"id":448568,"contributorType":{"id":1,"text":"Authors"},"rank":18},{"text":"Jordan, G.J.","contributorId":51122,"corporation":false,"usgs":true,"family":"Jordan","given":"G.J.","email":"","affiliations":[],"preferred":false,"id":448576,"contributorType":{"id":1,"text":"Authors"},"rank":19},{"text":"Kraft, N.J.B.","contributorId":90565,"corporation":false,"usgs":true,"family":"Kraft","given":"N.J.B.","email":"","affiliations":[],"preferred":false,"id":448582,"contributorType":{"id":1,"text":"Authors"},"rank":20},{"text":"Lovelock, E.C.","contributorId":9892,"corporation":false,"usgs":true,"family":"Lovelock","given":"E.C.","email":"","affiliations":[],"preferred":false,"id":448562,"contributorType":{"id":1,"text":"Authors"},"rank":21},{"text":"Lusk, C.H.","contributorId":44757,"corporation":false,"usgs":true,"family":"Lusk","given":"C.H.","email":"","affiliations":[],"preferred":false,"id":448574,"contributorType":{"id":1,"text":"Authors"},"rank":22},{"text":"Niinemets, U.","contributorId":88176,"corporation":false,"usgs":true,"family":"Niinemets","given":"U.","affiliations":[],"preferred":false,"id":448581,"contributorType":{"id":1,"text":"Authors"},"rank":23},{"text":"Penuelas, J.","contributorId":45541,"corporation":false,"usgs":true,"family":"Penuelas","given":"J.","affiliations":[],"preferred":false,"id":448575,"contributorType":{"id":1,"text":"Authors"},"rank":24},{"text":"Rapson, G.","contributorId":8694,"corporation":false,"usgs":true,"family":"Rapson","given":"G.","email":"","affiliations":[],"preferred":false,"id":448560,"contributorType":{"id":1,"text":"Authors"},"rank":25},{"text":"Wing, S.L.","contributorId":63588,"corporation":false,"usgs":true,"family":"Wing","given":"S.L.","email":"","affiliations":[],"preferred":false,"id":448578,"contributorType":{"id":1,"text":"Authors"},"rank":26},{"text":"Wright, I.J.","contributorId":10634,"corporation":false,"usgs":true,"family":"Wright","given":"I.J.","email":"","affiliations":[],"preferred":false,"id":448563,"contributorType":{"id":1,"text":"Authors"},"rank":27}]}}
,{"id":70034938,"text":"70034938 - 2011 - 2-D inner-shelf current observations from a single VHF WEllen RAdar (WERA) station","interactions":[],"lastModifiedDate":"2021-11-10T16:41:56.712004","indexId":"70034938","displayToPublicDate":"2011-01-01T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"2-D inner-shelf current observations from a single VHF WEllen RAdar (WERA) station","docAbstract":"<p><span>The majority of High Frequency (HF) radars used worldwide operate at medium to high frequencies (8 to 30 MHz) providing spatial resolutions ranging from 3 to 1.5 km and ranges from 150 to 50 km. This paper presents results from the deployment of a single Very High Frequency (VHF, 48 MHz) WEllen RAdar (WERA) radar with spatial resolution of 150 m and range 10-15 km, used in the nearshore off Cape Hatteras, NC, USA. It consisted of a linear array of 12 antennas operating in beam forming mode. Radial velocities were estimated from radar backscatter for a variety of wind and nearshore wave conditions. A methodology similar to that used for converting acoustically derived beam velocities to an orthogonal system is presented for obtaining 2-D current fields from a single station. The accuracy of the VHF radar-derived radial velocities is examined using a new statistical technique that evaluates the system over the range of measured velocities. The VHF radar velocities showed a bias of 3 to 7 cm/s over the experimental period explainable by the differences in radar penetration and in-situ measurement height. The 2-D current field shows good agreement with the in-situ measurements. Deviations and inaccuracies are well explained by the geometric dilution analysis.</span></p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"2011 IEEE/OES/CWTM 10th working conference on current, waves and turbulence measurement, CWTM 2011","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"2011 IEEE/OES/CWTM 10th Working Conference on Current, Waves and Turbulence Measurement, CWTM 2011","conferenceDate":"March 20-23, 2011","conferenceLocation":"Monterey, CA","language":"English","publisher":"IEEE","doi":"10.1109/CWTM.2011.5759525","isbn":"9781457700224","usgsCitation":"Voulgaris, G., Kumar, N., Gurgel, K., Warner, J., and List, J.H., 2011, 2-D inner-shelf current observations from a single VHF WEllen RAdar (WERA) station, <i>in</i> 2011 IEEE/OES/CWTM 10th working conference on current, waves and turbulence measurement, CWTM 2011, Monterey, CA, March 20-23, 2011, p. 57-65, https://doi.org/10.1109/CWTM.2011.5759525.","productDescription":"9 p.","startPage":"57","endPage":"65","ipdsId":"IP-027116","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":243869,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"North Carolina","otherGeospatial":"Cape Hattaras","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -75.66558837890625,\n              35.18166571475282\n            ],\n            [\n              -75.49667358398438,\n              35.18166571475282\n            ],\n            [\n              -75.49667358398438,\n              35.285984736065764\n            ],\n            [\n              -75.66558837890625,\n              35.285984736065764\n            ],\n            [\n              -75.66558837890625,\n              35.18166571475282\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e243e4b0c8380cd45a66","contributors":{"authors":[{"text":"Voulgaris, G.","contributorId":73701,"corporation":false,"usgs":true,"family":"Voulgaris","given":"G.","affiliations":[],"preferred":false,"id":448414,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kumar, N.","contributorId":55227,"corporation":false,"usgs":true,"family":"Kumar","given":"N.","affiliations":[],"preferred":false,"id":448412,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gurgel, K.-W.","contributorId":74593,"corporation":false,"usgs":true,"family":"Gurgel","given":"K.-W.","email":"","affiliations":[],"preferred":false,"id":448415,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Warner, John C. 0000-0002-3734-8903 jcwarner@usgs.gov","orcid":"https://orcid.org/0000-0002-3734-8903","contributorId":2681,"corporation":false,"usgs":true,"family":"Warner","given":"John C.","email":"jcwarner@usgs.gov","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":448411,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"List, Jeffrey H. 0000-0001-8594-2491 jlist@usgs.gov","orcid":"https://orcid.org/0000-0001-8594-2491","contributorId":174581,"corporation":false,"usgs":true,"family":"List","given":"Jeffrey","email":"jlist@usgs.gov","middleInitial":"H.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":448413,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70034937,"text":"70034937 - 2011 - Compositional diversity and geologic insights of the Aristarchus crater from Moon Mineralogy Mapper data","interactions":[],"lastModifiedDate":"2017-06-29T13:41:02","indexId":"70034937","displayToPublicDate":"2011-01-01T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2317,"text":"Journal of Geophysical Research E: Planets","active":true,"publicationSubtype":{"id":10}},"title":"Compositional diversity and geologic insights of the Aristarchus crater from Moon Mineralogy Mapper data","docAbstract":"The Moon Mineralogy Mapper (M3) acquired high spatial and spectral resolution data of the Aristarchus Plateau with 140 m/pixel in 85 spectral bands from 0.43 to 3.0 m. The data were collected as radiance and converted to reflectance using the observational constraints and a solar spectrum scaled to the Moon-Sun distance. Summary spectral parameters for the area of mafic silicate 1 and 2 m bands were calculated from the M3 data and used to map the distribution of key units that were then analyzed in detail with the spectral data. This analysis focuses on five key compositional units in the region. (1) The central peaks are shown to be strongly enriched in feldspar and are likely from the upper plagioclase-rich crust of the Moon. (2) The impact melt is compositionally diverse with clear signatures of feldspathic crust, olivine, and glass. (3) The crater walls and ejecta show a high degree of spatial heterogeneity and evidence for massive breccia blocks. (4) Olivine, strongly concentrated on the rim, wall, and exterior of the southeastern quadrant of the crater, is commonly associated the impact melt. (5) There are at least two types of glass deposits observed: pyroclastic glass and impact glass. Copyright 2011 by the American Geophysical Union.","language":"English","publisher":"AGU","doi":"10.1029/2010JE003726","issn":"01480227","usgsCitation":"Mustard, J., Pieters, C., Isaacson, P., Head, J., Besse, S., Clark, R.N., Klima, R., Petro, N., Staid, M., Sunshine, J., Runyon, C., and Tompkins, S., 2011, Compositional diversity and geologic insights of the Aristarchus crater from Moon Mineralogy Mapper data: Journal of Geophysical Research E: Planets, v. 116, no. 5, Article E00G12; 17 p., https://doi.org/10.1029/2010JE003726.","productDescription":"Article E00G12; 17 p.","ipdsId":"IP-024467","costCenters":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"links":[{"id":475441,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1029/2010je003726","text":"Publisher Index Page"},{"id":243837,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":215998,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1029/2010JE003726"}],"volume":"116","issue":"5","noUsgsAuthors":false,"publicationDate":"2011-05-10","publicationStatus":"PW","scienceBaseUri":"5059f936e4b0c8380cd4d4d4","contributors":{"authors":[{"text":"Mustard, J.F.","contributorId":91605,"corporation":false,"usgs":true,"family":"Mustard","given":"J.F.","email":"","affiliations":[],"preferred":false,"id":448410,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pieters, C.M.","contributorId":48733,"corporation":false,"usgs":true,"family":"Pieters","given":"C.M.","email":"","affiliations":[{"id":16929,"text":"Brown University","active":true,"usgs":false}],"preferred":false,"id":448403,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Isaacson, P.J.","contributorId":63236,"corporation":false,"usgs":true,"family":"Isaacson","given":"P.J.","email":"","affiliations":[],"preferred":false,"id":448405,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Head, J.W.","contributorId":67982,"corporation":false,"usgs":true,"family":"Head","given":"J.W.","email":"","affiliations":[],"preferred":false,"id":448406,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Besse, S.","contributorId":79330,"corporation":false,"usgs":true,"family":"Besse","given":"S.","email":"","affiliations":[],"preferred":false,"id":448409,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Clark, R. N.","contributorId":6568,"corporation":false,"usgs":true,"family":"Clark","given":"R.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":448399,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Klima, R.L.","contributorId":29238,"corporation":false,"usgs":true,"family":"Klima","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":448402,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Petro, N.E.","contributorId":18999,"corporation":false,"usgs":true,"family":"Petro","given":"N.E.","email":"","affiliations":[],"preferred":false,"id":448400,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Staid, M.I.","contributorId":76505,"corporation":false,"usgs":true,"family":"Staid","given":"M.I.","email":"","affiliations":[],"preferred":false,"id":448408,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Sunshine, J.M.","contributorId":74591,"corporation":false,"usgs":true,"family":"Sunshine","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":448407,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Runyon, C.J.","contributorId":19398,"corporation":false,"usgs":true,"family":"Runyon","given":"C.J.","email":"","affiliations":[],"preferred":false,"id":448401,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Tompkins, S.","contributorId":51123,"corporation":false,"usgs":true,"family":"Tompkins","given":"S.","email":"","affiliations":[],"preferred":false,"id":448404,"contributorType":{"id":1,"text":"Authors"},"rank":12}]}}
,{"id":70034935,"text":"70034935 - 2011 - Using a semi-natural stream to produce young sturgeons for conservation stocking: Maintaining natural selection during spawning and rearing","interactions":[],"lastModifiedDate":"2021-03-08T17:24:47.907165","indexId":"70034935","displayToPublicDate":"2011-01-01T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2166,"text":"Journal of Applied Ichthyology","active":true,"publicationSubtype":{"id":10}},"title":"Using a semi-natural stream to produce young sturgeons for conservation stocking: Maintaining natural selection during spawning and rearing","docAbstract":"<p><span>Young sturgeons used for conservation stocking are presently produced using the same methods used for commercial culture. To determine if young sturgeons could be produced without relaxing natural selection factors, we developed a semi‐natural stream where we annually studied mating of wild shortnose sturgeon (</span><i>Acipenser brevirostrum</i><span>) observed movement of gametes released freely during spawning, and estimated the number of larvae produced by various densities of spawned eggs. The stream had a bottom area of 18.8 m</span><sup>2</sup><span>, a rubble–gravel bottom, and a mean bottom current at 0.6 depth during spawning of 48 cm s</span><sup>−1</sup><span>&nbsp;(range, 17–126 cm s</span><sup>−1</sup><span>). Wild adults successfully spawned in the stream each year for 7 years (2002–2008). Some females and males were more successful during spawning than others, suggesting an unequal fitness during spawning among wild individuals, which is different than the controlled spawning fitness of individuals in hatcheries. Male and female gametes spawned naturally must connect quickly in the fast current or fail, a selection factor absent in hatcheries. The number of larvae produced was inversely related to spawned egg density m</span><sup>−2</sup><span>&nbsp;(</span><i>R</i><sup>2</sup><span> = 0.65) and the maximum number of larvae produced was 8000–16 000 (425–851 larvae m</span><sup>−2</sup><span>&nbsp;of bottom). Artificial spawning streams have the potential to contribute to sturgeon restoration.</span></p>","language":"English","publisher":"Wiley","doi":"10.1111/j.1439-0426.2010.01630.x","issn":"01758659","usgsCitation":"Kynard, B., Pugh, D., Parker, T., and Kieffer, M., 2011, Using a semi-natural stream to produce young sturgeons for conservation stocking: Maintaining natural selection during spawning and rearing: Journal of Applied Ichthyology, v. 27, no. 2, p. 420-424, https://doi.org/10.1111/j.1439-0426.2010.01630.x.","productDescription":"5 p.","startPage":"420","endPage":"424","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":475119,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1111/j.1439-0426.2010.01630.x","text":"Publisher Index Page"},{"id":243808,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":215971,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1111/j.1439-0426.2010.01630.x"}],"volume":"27","issue":"2","noUsgsAuthors":false,"publicationDate":"2011-03-28","publicationStatus":"PW","scienceBaseUri":"505bc029e4b08c986b329f77","contributors":{"authors":[{"text":"Kynard, B.","contributorId":51232,"corporation":false,"usgs":true,"family":"Kynard","given":"B.","email":"","affiliations":[],"preferred":false,"id":448392,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pugh, D.","contributorId":99367,"corporation":false,"usgs":true,"family":"Pugh","given":"D.","email":"","affiliations":[],"preferred":false,"id":448394,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Parker, T.","contributorId":90901,"corporation":false,"usgs":true,"family":"Parker","given":"T.","affiliations":[],"preferred":false,"id":448393,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Kieffer, Micah 0000-0001-9310-018X mkieffer@usgs.gov","orcid":"https://orcid.org/0000-0001-9310-018X","contributorId":2641,"corporation":false,"usgs":true,"family":"Kieffer","given":"Micah","email":"mkieffer@usgs.gov","affiliations":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"preferred":true,"id":448391,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70034934,"text":"70034934 - 2011 - Study design and sampling intensity for demographic analyses of bear populations","interactions":[],"lastModifiedDate":"2012-03-12T17:21:42","indexId":"70034934","displayToPublicDate":"2011-01-01T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3671,"text":"Ursus","active":true,"publicationSubtype":{"id":10}},"title":"Study design and sampling intensity for demographic analyses of bear populations","docAbstract":"The rate of population change through time (??) is a fundamental element of a wildlife population's conservation status, yet estimating it with acceptable precision for bears is difficult. For studies that follow known (usually marked) bears, ?? can be estimated during some defined time by applying either life-table or matrix projection methods to estimates of individual vital rates. Usually however, confidence intervals surrounding the estimate are broader than one would like. Using an estimator suggested by Doak et al. (2005), we explored the precision to be expected in ?? from demographic analyses of typical grizzly (Ursus arctos) and American black (U. americanus) bear data sets. We also evaluated some trade-offs among vital rates in sampling strategies. Confidence intervals around ?? were more sensitive to adding to the duration of a short (e.g., 3 yrs) than a long (e.g., 10 yrs) study, and more sensitive to adding additional bears to studies with small (e.g., 10 adult females/yr) than large (e.g., 30 adult females/yr) sample sizes. Confidence intervals of ?? projected using process-only variance of vital rates were only slightly smaller than those projected using total variances of vital rates. Under sampling constraints typical of most bear studies, it may be more efficient to invest additional resources into monitoring recruitment and juvenile survival rates of females already a part of the study, than to simply increase the sample size of study females. ?? 2011 International Association for Bear Research and Management.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Ursus","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.2192/URSUS-D-10-00028.1","issn":"15376176","usgsCitation":"Harris, R., Schwartz, C., Mace, R., and Haroldson, M., 2011, Study design and sampling intensity for demographic analyses of bear populations: Ursus, v. 22, no. 1, p. 24-36, https://doi.org/10.2192/URSUS-D-10-00028.1.","startPage":"24","endPage":"36","numberOfPages":"13","costCenters":[],"links":[{"id":215970,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.2192/URSUS-D-10-00028.1"},{"id":243807,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"22","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b9ccde4b08c986b31d4c6","contributors":{"authors":[{"text":"Harris, R.B.","contributorId":102271,"corporation":false,"usgs":true,"family":"Harris","given":"R.B.","email":"","affiliations":[],"preferred":false,"id":448388,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schwartz, C.C.","contributorId":33658,"corporation":false,"usgs":true,"family":"Schwartz","given":"C.C.","email":"","affiliations":[],"preferred":false,"id":448387,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mace, R.D.","contributorId":103881,"corporation":false,"usgs":true,"family":"Mace","given":"R.D.","email":"","affiliations":[],"preferred":false,"id":448389,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Haroldson, M.A. 0000-0002-7457-7676","orcid":"https://orcid.org/0000-0002-7457-7676","contributorId":108047,"corporation":false,"usgs":true,"family":"Haroldson","given":"M.A.","affiliations":[],"preferred":false,"id":448390,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70034933,"text":"70034933 - 2011 - Adaptive management of natural resources-framework and issues","interactions":[],"lastModifiedDate":"2021-03-08T17:30:35.709623","indexId":"70034933","displayToPublicDate":"2011-01-01T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2258,"text":"Journal of Environmental Management","active":true,"publicationSubtype":{"id":10}},"title":"Adaptive management of natural resources-framework and issues","docAbstract":"<p><span>Adaptive management, an approach for simultaneously managing and learning about natural resources, has been around for several decades. Interest in adaptive decision making has grown steadily over that time, and by now many in&nbsp;</span><a title=\"Learn more about Natural Resource Conservation from ScienceDirect's AI-generated Topic Pages\" href=\"https://www.sciencedirect.com/topics/earth-and-planetary-sciences/natural-resource-conservation\" data-mce-href=\"https://www.sciencedirect.com/topics/earth-and-planetary-sciences/natural-resource-conservation\">natural resources conservation</a><span>&nbsp;claim that adaptive management is the approach they use in meeting their resource management responsibilities. Yet there remains considerable ambiguity about what adaptive management actually is, and how it is to be implemented by practitioners. The objective of this paper is to present a framework and conditions for adaptive decision making, and discuss some important challenges in its application. Adaptive management is described as a two-phase process of deliberative and iterative phases, which are implemented sequentially over the timeframe of an application. Key elements, processes, and issues in adaptive decision making are highlighted in terms of this framework. Special emphasis is given to the question of geographic scale, the difficulties presented by non-stationarity, and organizational challenges in implementing adaptive management.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.jenvman.2010.10.041","issn":"03014797","usgsCitation":"Williams, B.K., 2011, Adaptive management of natural resources-framework and issues: Journal of Environmental Management, v. 92, no. 5, p. 1346-1353, https://doi.org/10.1016/j.jenvman.2010.10.041.","productDescription":"8 p.","startPage":"1346","endPage":"1353","costCenters":[{"id":554,"text":"Science and Decisions Center","active":true,"usgs":true}],"links":[{"id":243806,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":215969,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.jenvman.2010.10.041"}],"volume":"92","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e6e5e4b0c8380cd476ef","contributors":{"authors":[{"text":"Williams, Byron K. 0000-0001-7644-1396","orcid":"https://orcid.org/0000-0001-7644-1396","contributorId":207067,"corporation":false,"usgs":true,"family":"Williams","given":"Byron","email":"","middleInitial":"K.","affiliations":[{"id":554,"text":"Science and Decisions Center","active":true,"usgs":true}],"preferred":true,"id":448386,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70034907,"text":"70034907 - 2011 - The path to a successful one-million tonne demonstration of geological sequestration: Characterization, cooperation, and collaboration","interactions":[],"lastModifiedDate":"2021-03-08T20:12:37.233188","indexId":"70034907","displayToPublicDate":"2011-01-01T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"The path to a successful one-million tonne demonstration of geological sequestration: Characterization, cooperation, and collaboration","docAbstract":"<p><span>The development of the Illinois Basin-Decatur USA test site for a 1&nbsp;million tonne injection of CO</span><sub>2</sub><span>&nbsp;into the Mount Simon Sandstone saline reservoir beginning in 2011 has been a multiphase process requiring a wide array of personnel and resources that began in 2003. The process of regional characterization took two years as part of a Phase I effort focused on the entire Illinois Basin, located in Illinois, Indiana, and Kentucky, USA. Seeking the cooperation of an industrial source of CO</span><sub>2</sub><span>&nbsp;and site selection within the Basin took place during Phase II while most of the concurrent research emphasis was on a set of small-scale tests of Enhanced Oil Recovery (EOR) and CO</span><sub>2</sub><span>&nbsp;injection into a coal seam. Phase III began the commitment to the 1&nbsp;million-tonne test site development through the collaboration of the Archer Daniels Midland Company (ADM) who is providing a site, the CO</span><sub>2</sub><span>, and developing a compression facility, of Schlumberger Carbon Services who is providing expertise for operations, drilling, geophysics, risk assessment, and reservoir modelling, and of the Illinois State Geological Survey (ISGS) whose geologists and engineers lead the Midwest Geological Sequestration Consortium (MGSC). Communications and outreach has been a collaborative effort of ADM, ISGS and Schlumberger Carbon Services. The Consortium is one of the seven Regional Carbon Sequestration Partnerships, a carbon sequestration research program supported by the National Energy Technology Laboratory of the U.S. Department of Energy.</span></p>","largerWorkTitle":"Energy Procedia","conferenceTitle":"10th International Conference on Greenhouse Gas Control Technologies","conferenceDate":"September, 19-23, 2010","conferenceLocation":"Amsterdam","language":"English","publisher":"Elsevier","doi":"10.1016/j.egypro.2011.02.441","issn":"18766102","usgsCitation":"Finley, R., Greenberg, S., Frailey, S., Krapac, I., Leetaru, H., and Marsteller, S., 2011, The path to a successful one-million tonne demonstration of geological sequestration: Characterization, cooperation, and collaboration, <i>in</i> Energy Procedia, v. 4, Amsterdam, September, 19-23, 2010, p. 4770-4776, https://doi.org/10.1016/j.egypro.2011.02.441.","productDescription":"7 p.","startPage":"4770","endPage":"4776","costCenters":[],"links":[{"id":487844,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1016/j.egypro.2011.02.441","text":"Publisher Index Page"},{"id":243396,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":215582,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.egypro.2011.02.441"}],"country":"United States","state":"Illinois","otherGeospatial":"Illinois Basin-Decatur","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -89.197998046875,\n              39.60145584096999\n            ],\n            [\n              -88.648681640625,\n              39.60145584096999\n            ],\n            [\n              -88.648681640625,\n              40.065460682065535\n            ],\n            [\n              -89.197998046875,\n              40.065460682065535\n            ],\n            [\n              -89.197998046875,\n              39.60145584096999\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bae80e4b08c986b324140","contributors":{"authors":[{"text":"Finley, R.J.","contributorId":70984,"corporation":false,"usgs":true,"family":"Finley","given":"R.J.","email":"","affiliations":[],"preferred":false,"id":448265,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Greenberg, S.E.","contributorId":56441,"corporation":false,"usgs":true,"family":"Greenberg","given":"S.E.","email":"","affiliations":[],"preferred":false,"id":448264,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Frailey, S.M.","contributorId":93263,"corporation":false,"usgs":true,"family":"Frailey","given":"S.M.","email":"","affiliations":[],"preferred":false,"id":448266,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Krapac, I.G.","contributorId":33850,"corporation":false,"usgs":true,"family":"Krapac","given":"I.G.","email":"","affiliations":[],"preferred":false,"id":448262,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Leetaru, H.E.","contributorId":47123,"corporation":false,"usgs":true,"family":"Leetaru","given":"H.E.","email":"","affiliations":[],"preferred":false,"id":448263,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Marsteller, S.","contributorId":27288,"corporation":false,"usgs":true,"family":"Marsteller","given":"S.","email":"","affiliations":[],"preferred":false,"id":448261,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70034906,"text":"70034906 - 2011 - Dispersal and behavior of Pacific halibut Hippoglossus stenolepis in the Bering Sea and Aleutian Islands region","interactions":[],"lastModifiedDate":"2021-03-08T20:40:08.694304","indexId":"70034906","displayToPublicDate":"2011-01-01T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":860,"text":"Aquatic Biology","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Dispersal and behavior of Pacific halibut <i>hippoglossus stenolepis</i> in the Bering Sea and Aleutian islands region","title":"Dispersal and behavior of Pacific halibut Hippoglossus stenolepis in the Bering Sea and Aleutian Islands region","docAbstract":"<p class=\"abstract_block\">Currently, it is assumed that eastern Pacific halibut<span>&nbsp;</span><i>Hippoglossus stenolepis</i><span>&nbsp;</span>belong to a&nbsp;single, fully mixed population extending from California through the Bering Sea, in which adult ­halibut disperse randomly throughout their range during their lifetime. However, we hypothesize that hali­but dispersal is more complex than currently assumed and is not spatially random. To test this hypo­thesis, we studied the seasonal dispersal and behavior of Pacific halibut in the Bering Sea and Aleutian Islands (BSAI). Pop-up Archival Transmitting tags attached to halibut (82 to 154 cm fork length) during the summer provided no evidence that individuals moved out of the Bering Sea and Aleutian Islands region into the Gulf of Alaska during the mid-winter spawning season, supporting the concept that this region contains a separate spawning group of adult halibut. There was evidence for geographically localized groups of halibut along the Aleutian Island chain, as all of the individuals tagged there displayed residency, with their movements possibly impeded by tidal currents in the passes between islands. Mid-winter aggregation areas of halibut are assumed to be spawning grounds, of which 2 were previously unidentified and extend the species’ presumed spawning range ~1000 km west and ~600 km north of the nearest documented spawning area. If there are indeed&nbsp; independent spawning groups of Pacific halibut in the BSAI, their dynamics may vary sufficiently from those of the Gulf of Alaska, so that specifically accounting for their relative segregation and unique ­dynamics within the larger population model will be necessary for correctly predicting how these components may respond to fishing pressure and changing environmental conditions.</p>","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Aquatic Biology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Inter-Research Science Publisher","doi":"10.3354/ab00333","issn":"18647782","usgsCitation":"Seitz, A., Loher, T., Norcross, B.L., and Nielsen, J.L., 2011, Dispersal and behavior of Pacific halibut Hippoglossus stenolepis in the Bering Sea and Aleutian Islands region: Aquatic Biology, v. 12, no. 3, p. 225-239, https://doi.org/10.3354/ab00333.","productDescription":"15 p.","startPage":"225","endPage":"239","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":475205,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.3354/ab00333","text":"Publisher Index Page"},{"id":243868,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":216029,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.3354/ab00333"}],"country":"United States","state":"Alaska","otherGeospatial":"Bering Sea and Aleutian Islands","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -179.82421875,\n              49.83798245308484\n            ],\n            [\n              -159.521484375,\n              49.83798245308484\n            ],\n            [\n              -159.521484375,\n              59.489726035537075\n            ],\n            [\n              -179.82421875,\n              59.489726035537075\n            ],\n            [\n              -179.82421875,\n              49.83798245308484\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"12","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0217e4b0c8380cd4fe9e","contributors":{"authors":[{"text":"Seitz, A.C.","contributorId":71756,"corporation":false,"usgs":true,"family":"Seitz","given":"A.C.","email":"","affiliations":[],"preferred":false,"id":448259,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Loher, Timothy","contributorId":26130,"corporation":false,"usgs":false,"family":"Loher","given":"Timothy","email":"","affiliations":[{"id":33614,"text":"International Pacific Halibut Comission","active":true,"usgs":false}],"preferred":false,"id":448258,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Norcross, Brenda L.","contributorId":21497,"corporation":false,"usgs":false,"family":"Norcross","given":"Brenda","email":"","middleInitial":"L.","affiliations":[{"id":7211,"text":"University of Alaska, Fairbanks","active":true,"usgs":false}],"preferred":false,"id":448257,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Nielsen, Jennifer L.","contributorId":43722,"corporation":false,"usgs":true,"family":"Nielsen","given":"Jennifer","email":"","middleInitial":"L.","affiliations":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"preferred":true,"id":448260,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
]}