{"pageNumber":"1782","pageRowStart":"44525","pageSize":"25","recordCount":184660,"records":[{"id":70201980,"text":"70201980 - 2011 - Constraints on mechanisms for the growth of gully alcoves in Gasa crater, Mars, from two-dimensional stability assessments of rock slopes","interactions":[],"lastModifiedDate":"2019-02-04T11:17:39","indexId":"70201980","displayToPublicDate":"2011-01-01T11:17:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1963,"text":"Icarus","active":true,"publicationSubtype":{"id":10}},"title":"Constraints on mechanisms for the growth of gully alcoves in Gasa crater, Mars, from two-dimensional stability assessments of rock slopes","docAbstract":"<p><span>The value of&nbsp;slope stability&nbsp;analyses for gaining insight into the geologic conditions that would facilitate the growth of gully alcoves on Mars is demonstrated in Gasa&nbsp;crater. Two-dimensional limit&nbsp;equilibrium methods&nbsp;are used in conjunction with&nbsp;high-resolution topography derived from stereo High Resolution Imaging Science Experiment (HiRISE) imagery. These analyses reveal three conditions that may produce observed alcove morphologies through&nbsp;slope failure: (1) a&nbsp;</span><i>ca.</i><span>&nbsp;&gt;10</span><span>&nbsp;</span><span>m thick&nbsp;surface layer&nbsp;that is either saturated with H</span><sub>2</sub><span>O ground ice or contains no groundwater/ice at all, above a zone of melting H</span><sub>2</sub><span>O ice or groundwater and under dynamic loading (i.e., seismicity), (2) a 1–10</span><span>&nbsp;</span><span>m thick surface layer that is saturated with either melting H</span><sub>2</sub><span>O ice or groundwater and under dynamic loading, or (3) a &gt;100</span><span>&nbsp;</span><span>m thick surface layer that is saturated with either melting H</span><sub>2</sub><span>O ice or groundwater and under&nbsp;static&nbsp;loading. This finding of three plausible scenarios for slope failure demonstrates how the triggering mechanisms and characteristics of future alcove growth would be affected by prevailing environmental conditions. HiRISE images also reveal&nbsp;normal faults&nbsp;and other fractures tangential to the crowns of some gully alcoves that are interpreted to be the result of slope instability, which may facilitate future slope movement. Stability analyses show that the most failure-prone slopes in this area are found in alcoves that are adjacent to crown fractures. Accordingly, crown fractures appear to be a useful indicator of those alcoves that should be monitored for future landslide activity.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.icarus.2010.09.025","usgsCitation":"Okubo, C.H., Tornabene, L.L., and Lanza, N.L., 2011, Constraints on mechanisms for the growth of gully alcoves in Gasa crater, Mars, from two-dimensional stability assessments of rock slopes: Icarus, v. 211, no. 1, p. 207-221, https://doi.org/10.1016/j.icarus.2010.09.025.","productDescription":"15 p.","startPage":"207","endPage":"221","costCenters":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"links":[{"id":360969,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Gasa crater, Mars","volume":"211","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Okubo, Chris H. 0000-0001-9776-8128 cokubo@usgs.gov","orcid":"https://orcid.org/0000-0001-9776-8128","contributorId":140482,"corporation":false,"usgs":true,"family":"Okubo","given":"Chris","email":"cokubo@usgs.gov","middleInitial":"H.","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":false,"id":756415,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tornabene, Livio L.","contributorId":203691,"corporation":false,"usgs":false,"family":"Tornabene","given":"Livio","email":"","middleInitial":"L.","affiliations":[{"id":13255,"text":"University of Western Ontario","active":true,"usgs":false}],"preferred":false,"id":756416,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lanza, Nina L.","contributorId":140299,"corporation":false,"usgs":false,"family":"Lanza","given":"Nina","email":"","middleInitial":"L.","affiliations":[{"id":13447,"text":"Los Alamos National Laboratory","active":true,"usgs":false}],"preferred":false,"id":756417,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70046915,"text":"70046915 - 2011 - Natural phosphorus sources for the Pacific Northwest","interactions":[],"lastModifiedDate":"2013-07-09T11:20:25","indexId":"70046915","displayToPublicDate":"2011-01-01T11:15:00","publicationYear":"2011","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Natural phosphorus sources for the Pacific Northwest","docAbstract":"Phosphorus is a naturally occurring element found in all rocks; the amount varies by the type of rock. The amount of phosphorus in sediments is expected to be correlated with the amount of phosphorus in the parent rocks. Streambed sediment collected by the National Uranium Resource Evaluation (NURE) Program were used to estimate the variation of phosphorus across the Pacific Northwest. This file provides an estimate of the mean concentration of phosphorus in soils for each incremental catchment of the USGS Pacific Northwest SPARROW model.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70046915","usgsCitation":"Johnson, H.M., 2011, Natural phosphorus sources for the Pacific Northwest, Dataset, https://doi.org/10.3133/70046915.","productDescription":"Dataset","onlineOnly":"Y","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":274750,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":274748,"type":{"id":16,"text":"Metadata"},"url":"https://water.usgs.gov/GIS/metadata/usgswrd/XML/naturalPhosphorusSources_MRB7.xml"}],"country":"United States","state":"Idaho;Oregon;Washington","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -129.351779,39.745375 ], [ -129.351779,55.265926 ], [ -109.448056,55.265926 ], [ -109.448056,39.745375 ], [ -129.351779,39.745375 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51dd30ede4b0f72b44719cab","contributors":{"authors":[{"text":"Johnson, Henry M. 0000-0002-7571-4994 hjohnson@usgs.gov","orcid":"https://orcid.org/0000-0002-7571-4994","contributorId":869,"corporation":false,"usgs":true,"family":"Johnson","given":"Henry","email":"hjohnson@usgs.gov","middleInitial":"M.","affiliations":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"preferred":true,"id":480620,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70006224,"text":"70006224 - 2011 - Status and limiting factors of three rare plant species in the coastal lowlands and mid-elevation woodlands of Hawai`i Volcanoes National Park","interactions":[],"lastModifiedDate":"2013-11-15T10:14:49","indexId":"70006224","displayToPublicDate":"2011-01-01T11:10:00","publicationYear":"2011","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesNumber":"Technical Report HCSU-024","title":"Status and limiting factors of three rare plant species in the coastal lowlands and mid-elevation woodlands of Hawai`i Volcanoes National Park","docAbstract":"Two endangered plant species (<i>Portulaca sclerocarpa</i>, `ihi mākole, and <i>Sesbania tomentosa</i>, `ōhai) and a species of concern (<i>Bobea timonioides</i>, `ahakea) native to the coastal lowlands and dry mid-elevation woodlands of Hawai`i Volcanoes National Park were studied for more than two years to determine their stand structure, short-term mortality rates, patterns of reproductive phenology, success of fruit production, seed germination rates in the greenhouse, presence of soil seed bank, and survival of both natural and planted seedlings. The role of rodents as fruit and seed predators was evaluated using exclosures and seed offerings in open and closed stations or cages. Rodents were excluded from randomly selected plants of P. sclerocarpa and from branches of S. tomentosa, and flower and fruit production were compared to that of adjacent unprotected plants. Tagged <i>S. tomentosa</i> fruit were also monitored monthly to detect rodent predation.","language":"English","publisher":"University of Hawai'i at Hilo","publisherLocation":"Hilo, HI","usgsCitation":"Pratt, L.W., VanDeMark, J., and Euaparadorn, M., 2011, Status and limiting factors of three rare plant species in the coastal lowlands and mid-elevation woodlands of Hawai`i Volcanoes National Park, viii, 79 p.","productDescription":"viii, 79 p.","numberOfPages":"90","ipdsId":"IP-026474","costCenters":[{"id":521,"text":"Pacific Island Ecosystems Research Center","active":false,"usgs":true}],"links":[{"id":111142,"type":{"id":11,"text":"Document"},"url":"https://hilo.hawaii.edu/hcsu/documents/PrattL_TR024_StatusandLimitingFactorsofThreeHAVOFINALno508.pdf"},{"id":279096,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":279095,"type":{"id":15,"text":"Index Page"},"url":"https://hilo.hawaii.edu/hcsu/publications.php"}],"country":"United States","state":"Hawai'i","otherGeospatial":"Hawai`i Volcanoes National Park","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -155.398865,19.165924 ], [ -155.398865,19.452349 ], [ -155.087814,19.452349 ], [ -155.087814,19.165924 ], [ -155.398865,19.165924 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5287509ce4b03b89f6f155d0","contributors":{"authors":[{"text":"Pratt, Linda W. lpratt@usgs.gov","contributorId":3708,"corporation":false,"usgs":true,"family":"Pratt","given":"Linda","email":"lpratt@usgs.gov","middleInitial":"W.","affiliations":[],"preferred":true,"id":354127,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"VanDeMark, Joshua R.","contributorId":28156,"corporation":false,"usgs":true,"family":"VanDeMark","given":"Joshua R.","affiliations":[],"preferred":false,"id":354128,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Euaparadorn, Melody","contributorId":37240,"corporation":false,"usgs":true,"family":"Euaparadorn","given":"Melody","affiliations":[],"preferred":false,"id":354129,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70047369,"text":"70047369 - 2011 - Regional-scale stratigraphy of surface units in Tyrrhena and Iapygia Terrae, Mars: Insights into highland crustal evolution and alteration history","interactions":[],"lastModifiedDate":"2021-05-07T17:59:08.332305","indexId":"70047369","displayToPublicDate":"2011-01-01T11:09:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":7353,"text":"Journal of Geophysical Research - Planets","active":true,"publicationSubtype":{"id":10}},"title":"Regional-scale stratigraphy of surface units in Tyrrhena and Iapygia Terrae, Mars: Insights into highland crustal evolution and alteration history","docAbstract":"<p><span>The compositional, thermophysical and geologic characteristics of surface units in Iapygia and Tyrrhena Terra (60°E–100°E, 0°–30°S) provide new insights into the compositional stratigraphy of the region. Intercrater plains are dominated by two surface units. The older unit (unit 1) is deficient in olivine and more degraded and likely consists of a mixture of impact, volcanic and sedimentary materials. The younger unit (unit 2) is enriched in olivine, exhibits a resistant morphology and higher thermal inertia, and likely represents volcanic infilling of plains. Units 1 and 2 bear a strong resemblance to those previously mapped in Mare Serpentis, a section of highlands crust located northwest of Hellas Basin. Thus, the two major intercrater plains units are even more widespread than previously thought and therefore likely constitute important components of Mars' highland stratigraphy. Many craters in the region contain high thermal inertia deposits (unit 3) that are compositionally identical to unit 2. These may have formed via volcanic infilling or may represent sedimentary materials that have been eroded from crater walls and lithified. Less common units include olivine and/or pyroxene‐rich massifs and crater central peaks. These are primarily found within Hellas Basin rim units and may represent mantle materials brought toward the surface during the Hellas impact. Putative chloride deposits are primarily associated with olivine‐deficient surfaces (unit 1) that may be heavily degraded occurrences of unit 2. The observations raise a variety of questions related to Martian crustal evolution and alteration that may have more widespread implications outside the study region.</span></p>","language":"English","publisher":"Wiley","doi":"10.1029/2010JE003772","usgsCitation":"Rogers, A.D., and Fergason, R.L., 2011, Regional-scale stratigraphy of surface units in Tyrrhena and Iapygia Terrae, Mars: Insights into highland crustal evolution and alteration history: Journal of Geophysical Research - Planets, v. 116, no. E8, E08005, 24 p., https://doi.org/10.1029/2010JE003772.","productDescription":"E08005, 24 p.","numberOfPages":"24","ipdsId":"IP-039189","costCenters":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"links":[{"id":475052,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1029/2010je003772","text":"Publisher Index Page"},{"id":275942,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Iapygia Terrae, Mars, Tyrrhena","volume":"116","issue":"E8","noUsgsAuthors":false,"publicationDate":"2011-08-20","publicationStatus":"PW","scienceBaseUri":"51fcd4e8e4b0296e5a4b5c88","contributors":{"authors":[{"text":"Rogers, A. Deanne","contributorId":108019,"corporation":false,"usgs":true,"family":"Rogers","given":"A.","email":"","middleInitial":"Deanne","affiliations":[],"preferred":false,"id":481854,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fergason, Robin L. 0000-0002-2044-1714 rfergason@usgs.gov","orcid":"https://orcid.org/0000-0002-2044-1714","contributorId":2753,"corporation":false,"usgs":true,"family":"Fergason","given":"Robin","email":"rfergason@usgs.gov","middleInitial":"L.","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":true,"id":481853,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70236198,"text":"70236198 - 2011 - Seismology, Rotational","interactions":[],"lastModifiedDate":"2022-08-30T16:14:25.314693","indexId":"70236198","displayToPublicDate":"2011-01-01T11:08:21","publicationYear":"2011","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Seismology, Rotational","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Encyclopedia of solid earth geophysics","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Springer Link","doi":"10.1007/978-90-481-8702-7_17","usgsCitation":"Lee, W.H., 2011, Seismology, Rotational, chap. <i>of</i> Encyclopedia of solid earth geophysics, p. 1344-1355, https://doi.org/10.1007/978-90-481-8702-7_17.","productDescription":"12 p.","startPage":"1344","endPage":"1355","costCenters":[],"links":[{"id":405917,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationDate":"2014-08-27","publicationStatus":"PW","contributors":{"authors":[{"text":"Lee, William H. K. whklee@usgs.gov","contributorId":623,"corporation":false,"usgs":true,"family":"Lee","given":"William","email":"whklee@usgs.gov","middleInitial":"H. K.","affiliations":[],"preferred":true,"id":850288,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70256012,"text":"70256012 - 2011 - Land cover change, biogeochemical modelling of carbon stocks, and climate change in West Africa","interactions":[],"lastModifiedDate":"2024-07-12T16:01:17.889179","indexId":"70256012","displayToPublicDate":"2011-01-01T10:52:31","publicationYear":"2011","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Land cover change, biogeochemical modelling of carbon stocks, and climate change in West Africa","docAbstract":"<p>The carbon in ecosystems exists in dynamic soil and vegetation pools which vary in amounts and cycle with the global atmosphere at varying rates. These stocks and fluxes play important roles in global carbon regulation and in the maintenance of goods and services. Changes in land cover or ecosystems result in increased or decreased fluxes to the atmosphere and play a major role in climate regulation. Carbon in soil is closely coupled to soil nitrogen and the continued mining of soil for crops or fuel without replenishment of nutrients results in decreased productivity and impacts food security. The assessment of these processes across large areas, although difficult, is aided by the integration of simulation modelling (biogeochemical and ecosystem) and remote sensing. </p><p>We acquired satellite imagery for four periods from the 1960s to 2000s, trained environmental scientists from 14 countries on image analysis and interpretation, and now report systematic analyses of land cover changes in select countries of West Africa and quantify potential impacts of climate change and management at specific sites. Statistical changes and maps of land cover are documented for most countries. Senegal, for example, illustrates a 57 percent loss in dense forests between 1975 and 2000 with an even greater loss rate in the preceding 10 years. Bare soil increased 16.6 percent, often related to unproductive “badland” formation. Settlements increased 45.6 percent, and reforestation replaced bare sandy areas for sand dune stabilization. In some countries (Senegal and Ghana), the impact of these conversions and changes in land management and future projections has been incorporated into biogeochemical models to quantify carbon changes and project future carbon and crop scenarios. We present current assessments of carbon fluxes and the availability of data for these West African countries.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Africa and the carbon cycle:  Proceedings of the open science conference","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"Open Science Conference on “Africa and Carbon Cycle: the CarboAfrica project”","conferenceDate":"November 25-27, 2008","conferenceLocation":"Accra, Ghana","language":"English","publisher":"FAO Viale delle Terme di Caracalla","usgsCitation":"Tieszen, L.L., Tappan, G.G., Tan, Z., and Tachie-Obeng, E., 2011, Land cover change, biogeochemical modelling of carbon stocks, and climate change in West Africa, <i>in</i> Africa and the carbon cycle:  Proceedings of the open science conference, Accra, Ghana, November 25-27, 2008, p. 75-83.","productDescription":"9 p.","startPage":"75","endPage":"83","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":431021,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":431020,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.fao.org/docrep/014/i2240e/i2240e00.htm","linkFileType":{"id":5,"text":"html"}}],"otherGeospatial":"West Africa","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              18.03221857254192,\n              19.06394261582861\n            ],\n            [\n              -20.794232823840474,\n              19.06394261582861\n            ],\n            [\n              -20.794232823840474,\n              0.5812016335944179\n            ],\n            [\n              18.03221857254192,\n              0.5812016335944179\n            ],\n            [\n              18.03221857254192,\n              19.06394261582861\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Tieszen, Larry L. tieszen@usgs.gov","contributorId":2831,"corporation":false,"usgs":true,"family":"Tieszen","given":"Larry","email":"tieszen@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":true,"id":906381,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tappan, G. Gray 0000-0002-2240-6963 tappan@usgs.gov","orcid":"https://orcid.org/0000-0002-2240-6963","contributorId":3624,"corporation":false,"usgs":true,"family":"Tappan","given":"G.","email":"tappan@usgs.gov","middleInitial":"Gray","affiliations":[{"id":223,"text":"Earth Resources Observation and Science (EROS) Center (Geography)","active":false,"usgs":true}],"preferred":true,"id":906382,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Tan, Z.","contributorId":60831,"corporation":false,"usgs":true,"family":"Tan","given":"Z.","email":"","affiliations":[],"preferred":false,"id":906383,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Tachie-Obeng, E.","contributorId":82550,"corporation":false,"usgs":true,"family":"Tachie-Obeng","given":"E.","email":"","affiliations":[],"preferred":false,"id":906384,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70148713,"text":"70148713 - 2011 - Life-history notes on <i>Cambarus hubbsi</i> creaser (Hubbs crayfish) from the South Fork Spring River, Arkansas","interactions":[],"lastModifiedDate":"2015-06-22T09:41:57","indexId":"70148713","displayToPublicDate":"2011-01-01T10:45:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3444,"text":"Southeastern Naturalist","active":true,"publicationSubtype":{"id":10}},"title":"Life-history notes on <i>Cambarus hubbsi</i> creaser (Hubbs crayfish) from the South Fork Spring River, Arkansas","docAbstract":"<p>Many crayfish species native to the southeastern United States are imperiled due to small range sizes and anthropogenic impacts such as habitat loss and introduction of non-native species. Furthermore, effective management of crayfish is limited by the scarcity of life-history and ecological data for many of these species. We report results of the first life-history study of the crayfish <i>Cambarus hubbsi</i> (Hubbs Crayfish). We collected 466 Hubbs Crayfish from the South Fork Spring River, AR throughout 2006 and recorded carapace lengths, wet weights, indicators of reproductive activity, and number of eggs on ovigerous females. Using length-frequency distributions, we identified four Hubbs Crayfish age classes and evaluated growth rates by plotting size by season (winter, spring, summer, autumn). Male Hubbs Crayfish were more common than females in all seasons except autumn, and males weighed more at equivalent lengths than females. Reproductive activity in Hubbs Crayfish peaked in late winter and spring, and ovigerous females were collected in March, April, and June. Ovigerous females were age II or III and carried few eggs relative to co-occurring crayfish of the genus <i>Orconectes.</i> Compared to these <i>Orconectes</i> species, Hubbs Crayfish is comparatively slow growing, long lived, with low reproductive potential, and as a result may be categorized as a K life-history strategist. Based on this species' life-history strategy and previously documented habitat specificity and taxonomic distinctiveness, Hubbs Crayfish may require monitoring and management attention normally reserved for species with smaller ranges.</p>","language":"English","publisher":"Humboldt Field Research Institute","publisherLocation":"Steuben, ME","doi":"10.1656/058.010.0110","collaboration":"Arkansas Game and Fish Commission; University of Arkansas; USGS; Wildlife Management Institute","usgsCitation":"Larson, E., and Magoulick, D.D., 2011, Life-history notes on <i>Cambarus hubbsi</i> creaser (Hubbs crayfish) from the South Fork Spring River, Arkansas: Southeastern Naturalist, v. 10, no. 1, p. 121-132, https://doi.org/10.1656/058.010.0110.","productDescription":"12 p.","startPage":"121","endPage":"132","numberOfPages":"12","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-015638","costCenters":[{"id":198,"text":"Coop Res Unit Atlanta","active":true,"usgs":true}],"links":[{"id":301403,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"10","issue":"1","publishingServiceCenter":{"id":8,"text":"Raleigh PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"558931cfe4b0b6d21dd61bf7","contributors":{"authors":[{"text":"Larson, E.R.","contributorId":94114,"corporation":false,"usgs":true,"family":"Larson","given":"E.R.","email":"","affiliations":[],"preferred":false,"id":549104,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Magoulick, Daniel D. 0000-0001-9665-5957 danmag@usgs.gov","orcid":"https://orcid.org/0000-0001-9665-5957","contributorId":2513,"corporation":false,"usgs":true,"family":"Magoulick","given":"Daniel","email":"danmag@usgs.gov","middleInitial":"D.","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":549080,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70150462,"text":"70150462 - 2011 - Factors affecting detectability of river otters during sign surveys","interactions":[],"lastModifiedDate":"2015-06-26T09:30:03","indexId":"70150462","displayToPublicDate":"2011-01-01T10:30:00","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":"Factors affecting detectability of river otters during sign surveys","docAbstract":"<p>Sign surveys are commonly used to study and monitor wildlife species but may be flawed when surveys are conducted only once and cover short distances, which can lead to a lack of accountability for false absences. Multiple observers surveyed for river otter (<i>Lontra canadensis</i>) scat and tracks along stream and reservoir shorelines at 110 randomly selected sites in eastern Kansas from January to April 2008 and 2009 to determine if detection probability differed among substrates, sign types, observers, survey lengths, and near access points. We estimated detection probabilities (<i>p</i>) of river otters using occupancy models in Program PRESENCE. Mean detection probability for a 400-m survey was highest in mud substrates (<i>p</i> = 0.60) and lowest in snow (<i>p</i> = 0.18) and leaf litter substrates (<i>p</i> = 0.27). Scat had a higher detection probability (<i>p</i> = 0.53) than tracks (<i>p</i> = 0.18), and experienced observers had higher detection probabilities (<i>p</i> &lt; 0.71) than novice observers (<i>p</i> &lt; 0.55). Detection probabilities increased almost 3-fold as survey length increased from 200 m to 1,000 m, and otter sign was not concentrated near access points. After accounting for imperfect detection, our estimates of otter site occupancy based on a 400-m survey increased &gt;3-fold, providing further evidence of the potential negative bias that can occur in estimates from sign surveys when imperfect detection is not addressed. Our study identifies areas for improvement in sign survey methodologies and results are applicable for sign surveys commonly used for many species across a range of habitats.</p>","language":"English","publisher":"Wildlife Society","publisherLocation":"Washington, D.C.","doi":"10.1002/jwmg.12","usgsCitation":"Jeffress, M.R., Paukert, C.P., Sandercock, B.K., and Gipson, P.S., 2011, Factors affecting detectability of river otters during sign surveys: Journal of Wildlife Management, v. 75, no. 1, p. 144-150, https://doi.org/10.1002/jwmg.12.","productDescription":"7 p.","startPage":"144","endPage":"150","numberOfPages":"7","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-014955","costCenters":[{"id":198,"text":"Coop Res Unit Atlanta","active":true,"usgs":true}],"links":[{"id":302358,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"75","issue":"1","publishingServiceCenter":{"id":8,"text":"Raleigh PSC"},"noUsgsAuthors":false,"publicationDate":"2011-01-31","publicationStatus":"PW","scienceBaseUri":"558e77b6e4b0b6d21dd65952","contributors":{"authors":[{"text":"Jeffress, Mackenzie R.","contributorId":67346,"corporation":false,"usgs":true,"family":"Jeffress","given":"Mackenzie","email":"","middleInitial":"R.","affiliations":[{"id":352,"text":"Kansas Cooperative Fish and Wildlife Research Unit","active":false,"usgs":true}],"preferred":false,"id":556935,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Paukert, Craig P. 0000-0002-9369-8545 cpaukert@usgs.gov","orcid":"https://orcid.org/0000-0002-9369-8545","contributorId":879,"corporation":false,"usgs":true,"family":"Paukert","given":"Craig","email":"cpaukert@usgs.gov","middleInitial":"P.","affiliations":[{"id":198,"text":"Coop Res Unit Atlanta","active":true,"usgs":true}],"preferred":true,"id":556920,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sandercock, Brett K.","contributorId":95816,"corporation":false,"usgs":true,"family":"Sandercock","given":"Brett","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":556936,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Gipson, Philip S.","contributorId":71495,"corporation":false,"usgs":true,"family":"Gipson","given":"Philip","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":556937,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70035898,"text":"70035898 - 2011 - The May 2005 eruption of Fernandina volcano, Galápagos: The first circumferential dike intrusion observed by GPS and InSAR","interactions":[],"lastModifiedDate":"2018-10-30T09:34:17","indexId":"70035898","displayToPublicDate":"2011-01-01T10:30:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1109,"text":"Bulletin of Volcanology","active":true,"publicationSubtype":{"id":10}},"title":"The May 2005 eruption of Fernandina volcano, Galápagos: The first circumferential dike intrusion observed by GPS and InSAR","docAbstract":"The May 2005 eruption of Fernandina volcano, Galápagos, occurred along circumferential fissures parallel to the caldera rim and fed lava flows down the steep southwestern slope of the volcano for several weeks. This was the first circumferential dike intrusion ever observed by both InSAR and GPS measurements and thus provides an opportunity to determine the subsurface geometry of these enigmatic structures that are common on Galápagos volcanoes but are rare elsewhere. Pre- and post- eruption ground deformation between 2002 and 2006 can be modeled by the inflation of two separate magma reservoirs beneath the caldera: a shallow sill at ~1 km depth and a deeper point-source at ~5 km depth, and we infer that this system also existed at the time of the 2005 eruption. The co-eruption deformation is dominated by uplift near the 2005 eruptive fissures, superimposed on a broad subsidence centered on the caldera. Modeling of the co-eruption deformation was performed by including various combinations of planar dislocations to simulate the 2005 circumferential dike intrusion. We found that a single planar dike could not match both the InSAR and GPS data. Our best-fit model includes three planar dikes connected along hinge lines to simulate a curved concave shell that is steeply dipping (~45–60°) toward the caldera at the surface and more gently dipping (~12–14°) at depth where it connects to the horizontal sub-caldera sill. The shallow sill is underlain by the deep point source. The geometry of this modeled magmatic system is consistent with the petrology of Fernandina lavas, which suggest that circumferential eruptions tap the shallowest parts of the system, whereas radial eruptions are fed from deeper levels. The recent history of eruptions at Fernandina is also consistent with the idea that circumferential and radial intrusions are sometimes in a stress-feedback relationship and alternate in time with one another.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Bulletin of Volcanology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1007/s00445-010-0433-0","issn":"02588900","usgsCitation":"Chadwick, W., Jonsson, S., Geist, D.J., Poland, M.P., Johnson, D., Batt, S., Harpp, K.S., and Ruiz, A., 2011, The May 2005 eruption of Fernandina volcano, Galápagos: The first circumferential dike intrusion observed by GPS and InSAR: Bulletin of Volcanology, v. 73, no. 6, p. 679-697, https://doi.org/10.1007/s00445-010-0433-0.","productDescription":"19 p.","startPage":"679","endPage":"697","numberOfPages":"19","costCenters":[{"id":336,"text":"Hawaiian Volcano Observatory","active":false,"usgs":true},{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"links":[{"id":244249,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":216385,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/s00445-010-0433-0"}],"country":"Galápagos Islands","otherGeospatial":"Fernandina volcano","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -91.666077,-0.514632 ], [ -91.666077,-0.256913 ], [ -91.36665,-0.256913 ], [ -91.36665,-0.514632 ], [ -91.666077,-0.514632 ] ] ] } } ] }","volume":"73","issue":"6","noUsgsAuthors":false,"publicationDate":"2010-12-15","publicationStatus":"PW","scienceBaseUri":"505ba7dae4b08c986b321842","contributors":{"authors":[{"text":"Chadwick, W.W. Jr.","contributorId":35876,"corporation":false,"usgs":true,"family":"Chadwick","given":"W.W.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":453000,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jonsson, Sigurjon","contributorId":72123,"corporation":false,"usgs":true,"family":"Jonsson","given":"Sigurjon","email":"","affiliations":[],"preferred":false,"id":453006,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Geist, Dennis J.","contributorId":47145,"corporation":false,"usgs":true,"family":"Geist","given":"Dennis","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":453001,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Poland, Michael P. 0000-0001-5240-6123 mpoland@usgs.gov","orcid":"https://orcid.org/0000-0001-5240-6123","contributorId":146118,"corporation":false,"usgs":true,"family":"Poland","given":"Michael","email":"mpoland@usgs.gov","middleInitial":"P.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":453002,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Johnson, Daniel J.","contributorId":71970,"corporation":false,"usgs":true,"family":"Johnson","given":"Daniel J.","affiliations":[],"preferred":false,"id":453005,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Batt, S.","contributorId":71414,"corporation":false,"usgs":true,"family":"Batt","given":"S.","email":"","affiliations":[],"preferred":false,"id":453004,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Harpp, Karen S.","contributorId":12271,"corporation":false,"usgs":true,"family":"Harpp","given":"Karen","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":452999,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Ruiz, A.","contributorId":52425,"corporation":false,"usgs":true,"family":"Ruiz","given":"A.","email":"","affiliations":[],"preferred":false,"id":453003,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":70046859,"text":"70046859 - 2011 - Water Use in Louisiana, 2010","interactions":[],"lastModifiedDate":"2016-02-05T11:00:57","indexId":"70046859","displayToPublicDate":"2011-01-01T10:28:00","publicationYear":"2011","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"title":"Water Use in Louisiana, 2010","docAbstract":"<p>In 2010, approximately 8,500 million gallons per day (Mgal/d) of water was withdrawn from groundwater and surface-water sources in Louisiana. Total groundwater withdrawals were about 1,600 Mgal/d, and total surfacewater withdrawals were about 7,000 Mgal/d. From 2005 to 2010, groundwater withdrawals in Louisiana increased by 1.8 percent, and surface-water withdrawals decreased by 19 percent. Total water withdrawals in Louisiana decreased by 17 percent from 2005 to 2010. Water withdrawal totals in Mgal/d in 2010 for various categories of use were as follows: public supply-750, industry-2,100, power generation-4,400, rural domestic-41, livestock-8.0, rice irrigation-690, general irrigation-240, and aquaculture-300. From 2005 to 2010, changes in withdrawals, in percent, for the categories of use were as follows: public supply increased by 3.7, industry decreased by 33, power generation decreased by 14, rural domestic decreased by 6.1, livestock was unchanged, rice irrigation decreased by 13, general irrigation increased by 17, and aquaculture increased by 12. Forty-one percent (about 650 Mgal/d) of all groundwater was withdrawn from the Chicot aquifer system, and 25 percent (about 390 Mgal/d) was withdrawn from the Mississippi River alluvial aquifer. Since 2005, withdrawals from the Chicot aquifer system decreased by 2.1 percent, and withdrawals from the Mississippi River alluvial aquifer increased by 2.7 percent. About 72 percent (5,000 Mgal/d) of all surface water withdrawn was from the Mississippi River mainstem. This value represents a 24 percent decrease in withdrawals from 2005 to 2010.</p>","language":"English","publisher":"Louisiana Department of Transportation and Development","publisherLocation":"Baton Rouge, LA","usgsCitation":"Sargent, B.P., 2011, Water Use in Louisiana, 2010 (Revised December 2012), vii, 136 p.","productDescription":"vii, 136 p.","numberOfPages":"145","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-034541","costCenters":[],"links":[{"id":277231,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":277230,"type":{"id":11,"text":"Document"},"url":"https://la.water.usgs.gov/publications/pdfs/WaterUse2010.pdf"}],"country":"United States","state":"Louisiana","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -94.0431,28.9210 ], [ -94.0431,33.0195 ], [ -88.817,33.0195 ], [ -88.817,28.9210 ], [ -94.0431,28.9210 ] ] ] } } ] }","edition":"Revised December 2012","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"522747ebe4b01904cf5a81c8","contributors":{"authors":[{"text":"Sargent, B. Pierre 0000-0002-3967-9036 psargent@usgs.gov","orcid":"https://orcid.org/0000-0002-3967-9036","contributorId":1228,"corporation":false,"usgs":true,"family":"Sargent","given":"B.","email":"psargent@usgs.gov","middleInitial":"Pierre","affiliations":[{"id":24708,"text":"Lower Mississippi-Gulf Water Science Center","active":true,"usgs":true},{"id":369,"text":"Louisiana Water Science Center","active":true,"usgs":true}],"preferred":true,"id":480480,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70199878,"text":"70199878 - 2011 - Input, calibration, uncertainty, and limitations of the basin characterization model: appendix three","interactions":[],"lastModifiedDate":"2018-10-02T10:25:12","indexId":"70199878","displayToPublicDate":"2011-01-01T10:23:31","publicationYear":"2011","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Input, calibration, uncertainty, and limitations of the basin characterization model: appendix three","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Conceptual model of the Great Basic carbonate and alluvial aquifer system","language":"English","publisher":"US Geological Survey","usgsCitation":"Flint, A.L., Flint, L.E., and Masbruch, M.D., 2011, Input, calibration, uncertainty, and limitations of the basin characterization model: appendix three, chap. <i>of</i> Conceptual model of the Great Basic carbonate and alluvial aquifer system, 20 p.","productDescription":"20 p.","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"links":[{"id":358011,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5c10c276e4b034bf6a7f1847","contributors":{"editors":[{"text":"Heilweil, Victor M. heilweil@usgs.gov","contributorId":837,"corporation":false,"usgs":true,"family":"Heilweil","given":"Victor","email":"heilweil@usgs.gov","middleInitial":"M.","affiliations":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"preferred":true,"id":747107,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Brooks, Lynette E. 0000-0002-9074-0939 lebrooks@usgs.gov","orcid":"https://orcid.org/0000-0002-9074-0939","contributorId":2718,"corporation":false,"usgs":true,"family":"Brooks","given":"Lynette","email":"lebrooks@usgs.gov","middleInitial":"E.","affiliations":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"preferred":true,"id":747108,"contributorType":{"id":2,"text":"Editors"},"rank":2}],"authors":[{"text":"Flint, Alan L. 0000-0002-5118-751X aflint@usgs.gov","orcid":"https://orcid.org/0000-0002-5118-751X","contributorId":1492,"corporation":false,"usgs":true,"family":"Flint","given":"Alan","email":"aflint@usgs.gov","middleInitial":"L.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true},{"id":657,"text":"Western Geographic Science Center","active":true,"usgs":true}],"preferred":true,"id":747104,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Flint, Lorraine E. 0000-0002-7868-441X lflint@usgs.gov","orcid":"https://orcid.org/0000-0002-7868-441X","contributorId":1184,"corporation":false,"usgs":true,"family":"Flint","given":"Lorraine","email":"lflint@usgs.gov","middleInitial":"E.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":747105,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Masbruch, Melissa D. 0000-0001-6568-160X mmasbruch@usgs.gov","orcid":"https://orcid.org/0000-0001-6568-160X","contributorId":1902,"corporation":false,"usgs":true,"family":"Masbruch","given":"Melissa","email":"mmasbruch@usgs.gov","middleInitial":"D.","affiliations":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"preferred":true,"id":747106,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70118768,"text":"70118768 - 2011 - Sagebrush ecosystem conservation and management: Ecoregional assessment tools and models for the Wyoming Basins","interactions":[{"subject":{"id":70175150,"text":"70175150 - 2011 - Chapter 1: Study area description","indexId":"70175150","publicationYear":"2011","noYear":false,"chapter":"1","title":"Chapter 1: Study area description"},"predicate":"IS_PART_OF","object":{"id":70118768,"text":"70118768 - 2011 - Sagebrush ecosystem conservation and management: Ecoregional assessment tools and models for the Wyoming Basins","indexId":"70118768","publicationYear":"2011","noYear":false,"title":"Sagebrush ecosystem conservation and management: Ecoregional assessment tools and models for the Wyoming Basins"},"id":1},{"subject":{"id":70175156,"text":"70175156 - 2011 - Chapter 2: Sagebrush-associated species of conservation concern","indexId":"70175156","publicationYear":"2011","noYear":false,"chapter":"2","title":"Chapter 2: Sagebrush-associated species of conservation concern"},"predicate":"IS_PART_OF","object":{"id":70118768,"text":"70118768 - 2011 - Sagebrush ecosystem conservation and management: Ecoregional assessment tools and models for the Wyoming Basins","indexId":"70118768","publicationYear":"2011","noYear":false,"title":"Sagebrush ecosystem conservation and management: Ecoregional assessment tools and models for the Wyoming Basins"},"id":2},{"subject":{"id":70175157,"text":"70175157 - 2011 - Chapter 3: Changes to the Wyoming Basins landscape from oil and natural gas development","indexId":"70175157","publicationYear":"2011","noYear":false,"chapter":"3","title":"Chapter 3: Changes to the Wyoming Basins landscape from oil and natural gas development"},"predicate":"IS_PART_OF","object":{"id":70118768,"text":"70118768 - 2011 - Sagebrush ecosystem conservation and management: Ecoregional assessment tools and models for the Wyoming Basins","indexId":"70118768","publicationYear":"2011","noYear":false,"title":"Sagebrush ecosystem conservation and management: Ecoregional assessment tools and models for the Wyoming Basins"},"id":3},{"subject":{"id":70175161,"text":"70175161 - 2011 - Chapter 4: A sampling and analytical approach to develop spatial distribution models for sagebrush-associated species","indexId":"70175161","publicationYear":"2011","noYear":false,"chapter":"4","title":"Chapter 4: A sampling and analytical approach to develop spatial distribution models for sagebrush-associated species"},"predicate":"IS_PART_OF","object":{"id":70118768,"text":"70118768 - 2011 - Sagebrush ecosystem conservation and management: Ecoregional assessment tools and models for the Wyoming Basins","indexId":"70118768","publicationYear":"2011","noYear":false,"title":"Sagebrush ecosystem conservation and management: Ecoregional assessment tools and models for the Wyoming Basins"},"id":4},{"subject":{"id":70175386,"text":"70175386 - 2011 - Chapter 5: Greater sage-grouse: General use and roost site occurrence with pellet counts as a measure of relative abundance","indexId":"70175386","publicationYear":"2011","noYear":false,"chapter":"5","title":"Chapter 5: Greater sage-grouse: General use and roost site occurrence with pellet counts as a measure of relative abundance"},"predicate":"IS_PART_OF","object":{"id":70118768,"text":"70118768 - 2011 - Sagebrush ecosystem conservation and management: Ecoregional assessment tools and models for the Wyoming Basins","indexId":"70118768","publicationYear":"2011","noYear":false,"title":"Sagebrush ecosystem conservation and management: Ecoregional assessment tools and models for the Wyoming Basins"},"id":5},{"subject":{"id":70175388,"text":"70175388 - 2011 - Chapter 6: Detectability adjusted count models of songbird abundance","indexId":"70175388","publicationYear":"2011","noYear":false,"chapter":"6","title":"Chapter 6: Detectability adjusted count models of songbird abundance"},"predicate":"IS_PART_OF","object":{"id":70118768,"text":"70118768 - 2011 - Sagebrush ecosystem conservation and management: Ecoregional assessment tools and models for the Wyoming Basins","indexId":"70118768","publicationYear":"2011","noYear":false,"title":"Sagebrush ecosystem conservation and management: Ecoregional assessment tools and models for the Wyoming Basins"},"id":6},{"subject":{"id":70175389,"text":"70175389 - 2011 - Chapter 7: Occurrence and abundance of ants, reptiles, and mammals","indexId":"70175389","publicationYear":"2011","noYear":false,"chapter":"7","title":"Chapter 7: Occurrence and abundance of ants, reptiles, and mammals"},"predicate":"IS_PART_OF","object":{"id":70118768,"text":"70118768 - 2011 - Sagebrush ecosystem conservation and management: Ecoregional assessment tools and models for the Wyoming Basins","indexId":"70118768","publicationYear":"2011","noYear":false,"title":"Sagebrush ecosystem conservation and management: Ecoregional assessment tools and models for the Wyoming Basins"},"id":7},{"subject":{"id":70175392,"text":"70175392 - 2011 - Chapter 8: Occurrence of large and medium-sized mammals: Occurrence but not count models predict pronghorn distribution","indexId":"70175392","publicationYear":"2011","noYear":false,"chapter":"8","title":"Chapter 8: Occurrence of large and medium-sized mammals: Occurrence but not count models predict pronghorn distribution"},"predicate":"IS_PART_OF","object":{"id":70118768,"text":"70118768 - 2011 - Sagebrush ecosystem conservation and management: Ecoregional assessment tools and models for the Wyoming Basins","indexId":"70118768","publicationYear":"2011","noYear":false,"title":"Sagebrush ecosystem conservation and management: Ecoregional assessment tools and models for the Wyoming Basins"},"id":8},{"subject":{"id":70175491,"text":"70175491 - 2011 - Chapter 9: Occurrence of small mammals: Deer mice and challenge of trapping across large spatial extents","indexId":"70175491","publicationYear":"2011","noYear":false,"chapter":"9","title":"Chapter 9: Occurrence of small mammals: Deer mice and challenge of trapping across large spatial extents"},"predicate":"IS_PART_OF","object":{"id":70118768,"text":"70118768 - 2011 - Sagebrush ecosystem conservation and management: Ecoregional assessment tools and models for the Wyoming Basins","indexId":"70118768","publicationYear":"2011","noYear":false,"title":"Sagebrush ecosystem conservation and management: Ecoregional assessment tools and models for the Wyoming Basins"},"id":9},{"subject":{"id":70175492,"text":"70175492 - 2011 - Chapter 10: Occurrence of non-native invasive plants: The role of anthropogenic features","indexId":"70175492","publicationYear":"2011","noYear":false,"chapter":"10","title":"Chapter 10: Occurrence of non-native invasive plants: The role of anthropogenic features"},"predicate":"IS_PART_OF","object":{"id":70118768,"text":"70118768 - 2011 - Sagebrush ecosystem conservation and management: Ecoregional assessment tools and models for the Wyoming Basins","indexId":"70118768","publicationYear":"2011","noYear":false,"title":"Sagebrush ecosystem conservation and management: Ecoregional assessment tools and models for the Wyoming Basins"},"id":10},{"subject":{"id":70175493,"text":"70175493 - 2011 - Chapter 11: Management considerations","indexId":"70175493","publicationYear":"2011","noYear":false,"chapter":"11","title":"Chapter 11: Management considerations"},"predicate":"IS_PART_OF","object":{"id":70118768,"text":"70118768 - 2011 - Sagebrush ecosystem conservation and management: Ecoregional assessment tools and models for the Wyoming Basins","indexId":"70118768","publicationYear":"2011","noYear":false,"title":"Sagebrush ecosystem conservation and management: Ecoregional assessment tools and models for the Wyoming Basins"},"id":11},{"subject":{"id":70212839,"text":"70212839 - 2011 - Introduction: An ecoregional assessment of the Wyoming Basins","indexId":"70212839","publicationYear":"2011","noYear":false,"chapter":"Introduction","title":"Introduction: An ecoregional assessment of the Wyoming Basins"},"predicate":"IS_PART_OF","object":{"id":70118768,"text":"70118768 - 2011 - Sagebrush ecosystem conservation and management: Ecoregional assessment tools and models for the Wyoming Basins","indexId":"70118768","publicationYear":"2011","noYear":false,"title":"Sagebrush ecosystem conservation and management: Ecoregional assessment tools and models for the Wyoming Basins"},"id":12}],"lastModifiedDate":"2020-08-31T13:45:58.097435","indexId":"70118768","displayToPublicDate":"2011-01-01T10:13:24","publicationYear":"2011","noYear":false,"publicationType":{"id":4,"text":"Book"},"title":"Sagebrush ecosystem conservation and management: Ecoregional assessment tools and models for the Wyoming Basins","docAbstract":"<p>The Wyoming Basins are one of the remaining strongholds of the sagebrush ecosystem. However, like most sagebrush habitats, threats to this region are numerous. This book adds to current knowledge about the regional status of the sagebrush ecosystem, the distribution of habitats, the threats to the ecosystem, and the influence of threats and habitat conditions on occurrence and abundance of sagebrush associated fauna and flora in the Wyoming Basins. Comprehensive methods are outlined for use in data collection and monitoring of wildlife and plant populations. Field and spatial data are integrated into a spatially explicit analytical framework to develop models of species occurrence and abundance for the egion. This book provides significant new information on distributions, abundances, and habitat relationships for a number of species of conservation concern that depend on sagebrush in the region. The tools and models presented in this book increase our understanding of impacts from land uses and can contribute to the development of comprehensive management and conservation strategies.</p>","language":"English","publisher":"Allen Press","publisherLocation":"Lawrence, KS","isbn":"978-0-615-55530-0","usgsCitation":"2011, Sagebrush ecosystem conservation and management: Ecoregional assessment tools and models for the Wyoming Basins, 409 p.","productDescription":"409 p.","numberOfPages":"409","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true}],"links":[{"id":378010,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/ja/70118768/70118768.pdf","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"The U.S. Geological Survey has been given express permission by the publisher to provide full-text access online for this publication, and is posted with the express permission from the Publications Warehouse Guidance Subcommittee"},{"id":291381,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Wyoming","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -111.0569,40.9947 ], [ -111.0569,45.0059 ], [ -104.0522,45.0059 ], [ -104.0522,40.9947 ], [ -111.0569,40.9947 ] ] ] } } ] }","publicComments":"The U.S. Geological Survey has been given express permission by the publisher to provide full-text access online for this publication, and is posted with the express permission from the Publications Warehouse Guidance Subcommittee","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57fe7fd9e4b0824b2d147982","contributors":{"editors":[{"text":"Hanser, Steve E. 0000-0002-4430-2073 shanser@usgs.gov","orcid":"https://orcid.org/0000-0002-4430-2073","contributorId":152523,"corporation":false,"usgs":true,"family":"Hanser","given":"Steve","email":"shanser@usgs.gov","middleInitial":"E.","affiliations":[{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true},{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true},{"id":289,"text":"Forest and Rangeland Ecosys Science Center","active":true,"usgs":true},{"id":411,"text":"National Climate Change and Wildlife Science Center","active":true,"usgs":true},{"id":506,"text":"Office of the AD Ecosystems","active":true,"usgs":true}],"preferred":true,"id":797619,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Leu, Matthias","contributorId":68393,"corporation":false,"usgs":true,"family":"Leu","given":"Matthias","affiliations":[],"preferred":false,"id":797620,"contributorType":{"id":2,"text":"Editors"},"rank":2},{"text":"Knick, Steven T. 0000-0003-4025-1704 steve_knick@usgs.gov","orcid":"https://orcid.org/0000-0003-4025-1704","contributorId":159,"corporation":false,"usgs":true,"family":"Knick","given":"Steven","email":"steve_knick@usgs.gov","middleInitial":"T.","affiliations":[{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true},{"id":289,"text":"Forest and Rangeland Ecosys Science Center","active":true,"usgs":true}],"preferred":true,"id":797621,"contributorType":{"id":2,"text":"Editors"},"rank":3},{"text":"Aldridge, Cameron L. 0000-0003-3926-6941 aldridgec@usgs.gov","orcid":"https://orcid.org/0000-0003-3926-6941","contributorId":191773,"corporation":false,"usgs":true,"family":"Aldridge","given":"Cameron","email":"aldridgec@usgs.gov","middleInitial":"L.","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":false,"id":797622,"contributorType":{"id":2,"text":"Editors"},"rank":4}]}}
,{"id":70138911,"text":"70138911 - 2011 - Long-term increases in young-of-the-year growth of Arctic cisco Coregonus autumnalis and environmental influences","interactions":[],"lastModifiedDate":"2018-08-01T11:11:41","indexId":"70138911","displayToPublicDate":"2011-01-01T10:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2285,"text":"Journal of Fish Biology","active":true,"publicationSubtype":{"id":10}},"title":"Long-term increases in young-of-the-year growth of Arctic cisco Coregonus autumnalis and environmental influences","docAbstract":"<p>Arctic cisco Coregonus autumnalis young-of-year (YOY) growth was used as a proxy to examine the long-term response of a high-latitude fish population to changing climate from 1978 to 2004. YOY growth increased over time (r2 = 0&middot;29) and was correlated with monthly averages of the Arctic oscillation index, air temperature, east wind speed, sea-ice concentration and river discharge with and without time lags. Overall, the most prevalent correlates to YOY growth were sea-ice concentration lagged 1 year (significant correlations in 7 months; r<sup>2</sup> = 0&middot;14-0&middot;31) and Mackenzie River discharge lagged 2 years (significant correlations in 8 months; r<sup>2</sup> = 0&middot;13-0&middot;50). The results suggest that decreased sea-ice concentrations and increased river discharge fuel primary production and that life cycles of prey species linking increased primary production to fish growth are responsible for the time lag. Oceanographic studies also suggest that sea ice concentration and fluvial inputs from the Mackenzie River are key factors influencing productivity in the Beaufort Sea. Future research should assess the possible mechanism relating sea ice concentration and river discharge to productivity at upper trophic levels.</p>","language":"English","publisher":"Fisheries Society of the British Isles","publisherLocation":"London, England","doi":"10.1111/j.1095-8649.2010.02832.x","usgsCitation":"von Biela, V.R., Zimmerman, C.E., and Moulton, L.L., 2011, Long-term increases in young-of-the-year growth of Arctic cisco Coregonus autumnalis and environmental influences: Journal of Fish Biology, v. 78, no. 1, p. 39-56, https://doi.org/10.1111/j.1095-8649.2010.02832.x.","productDescription":"18 p.","startPage":"39","endPage":"56","numberOfPages":"18","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-015034","costCenters":[{"id":116,"text":"Alaska Science Center Biology MFEB","active":true,"usgs":true}],"links":[{"id":297510,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"78","issue":"1","publishingServiceCenter":{"id":12,"text":"Tacoma PSC"},"noUsgsAuthors":false,"publicationDate":"2010-12-03","publicationStatus":"PW","scienceBaseUri":"54dd2be9e4b08de9379b3563","contributors":{"authors":[{"text":"von Biela, Vanessa R. 0000-0002-7139-5981 vvonbiela@usgs.gov","orcid":"https://orcid.org/0000-0002-7139-5981","contributorId":3104,"corporation":false,"usgs":true,"family":"von Biela","given":"Vanessa","email":"vvonbiela@usgs.gov","middleInitial":"R.","affiliations":[{"id":116,"text":"Alaska Science Center Biology MFEB","active":true,"usgs":true},{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":120,"text":"Alaska Science Center Water","active":true,"usgs":true}],"preferred":true,"id":539186,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Zimmerman, Christian E. 0000-0002-3646-0688 czimmerman@usgs.gov","orcid":"https://orcid.org/0000-0002-3646-0688","contributorId":410,"corporation":false,"usgs":true,"family":"Zimmerman","given":"Christian","email":"czimmerman@usgs.gov","middleInitial":"E.","affiliations":[{"id":116,"text":"Alaska Science Center Biology MFEB","active":true,"usgs":true},{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":120,"text":"Alaska Science Center Water","active":true,"usgs":true}],"preferred":true,"id":539187,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Moulton, L. L.","contributorId":138892,"corporation":false,"usgs":false,"family":"Moulton","given":"L.","email":"","middleInitial":"L.","affiliations":[{"id":12569,"text":"MJM Research","active":true,"usgs":false}],"preferred":false,"id":539188,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70198712,"text":"70198712 - 2011 - Nanoparticles formed from bacterial oxyanion reduction of toxic Group 15 and 16 metalloids","interactions":[],"lastModifiedDate":"2018-08-29T07:38:52","indexId":"70198712","displayToPublicDate":"2011-01-01T09:59:33","publicationYear":"2011","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"chapter":"16","title":"Nanoparticles formed from bacterial oxyanion reduction of toxic Group 15 and 16 metalloids","docAbstract":"<p><span>This chapter presents some examples of nanoparticles formed by only a few microbial species that are cultivated in only a handful of laboratories worldwide. The investigations so far have just scratched the surface of the potential of the natural world to yield bionanomineral producers. While future research should involve screening surveys of the prokaryotes for this biomineralizing phenomenon, more detailed investigations are justified. The chapter discusses microbial Interaction with Group 15 and 16 Toxic Metalloids. The toxicity of the metalloids Se, Te, and As is due to the disruption of thiol intracellular biochemistry through the formation of stable, long-lived sulfur complexes. Selenium oxyanion reduction occurs in a wide range of microbes, including representatives of the&nbsp;</span><span class=\"jp-italic\">Wolinella</span><span>,&nbsp;</span><span class=\"jp-italic\">Pseudomonas</span><span>,&nbsp;</span><span class=\"jp-italic\">Sulfurospirillum</span><span>,&nbsp;</span><span class=\"jp-italic\">Enterobacter</span><span>,&nbsp;</span><span class=\"jp-italic\">Thaurea</span><span>,&nbsp;</span><span class=\"jp-italic\">Bacillus</span><span>,&nbsp;</span><span class=\"jp-italic\">Shewanella</span><span>, and&nbsp;</span><span class=\"jp-italic\">Citrobacter</span><span>&nbsp;genera. Technological applications of Se(0) and Te(0) nanoparticles include their use in photocopiers, microelectronic circuits, and solar cells as a result of their photo-optical and semiconducting physical properties. Nonetheless, once novel Se, Te, and As bionanoparticles are identified as having significant technical applications, applied research into their practical commercial production will without doubt ensue rapidly.</span></p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Microbial metal and metalloid metabolism: Advances and applications","language":"English","publisher":"ASM","publisherLocation":"Washington, D.C.","doi":"10.1128/9781555817190","isbn":"978-1-55581-536-3","usgsCitation":"Pearce, C., Baseman, S., Fellowes, J., and Oremland, R.S., 2011, Nanoparticles formed from bacterial oxyanion reduction of toxic Group 15 and 16 metalloids, chap. 16 <i>of</i> Microbial metal and metalloid metabolism: Advances and applications, p. 297-319, https://doi.org/10.1128/9781555817190.","productDescription":"23 p.","startPage":"297","endPage":"319","costCenters":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":356498,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5b98b488e4b0702d0e844b47","contributors":{"editors":[{"text":"Stolz, J.F.","contributorId":94022,"corporation":false,"usgs":true,"family":"Stolz","given":"J.F.","email":"","affiliations":[],"preferred":false,"id":742673,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Oremland, Ronald S. 0000-0001-7382-0147 roremlan@usgs.gov","orcid":"https://orcid.org/0000-0001-7382-0147","contributorId":931,"corporation":false,"usgs":true,"family":"Oremland","given":"Ronald","email":"roremlan@usgs.gov","middleInitial":"S.","affiliations":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true},{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":742674,"contributorType":{"id":2,"text":"Editors"},"rank":2}],"authors":[{"text":"Pearce, C.I.","contributorId":65315,"corporation":false,"usgs":true,"family":"Pearce","given":"C.I.","email":"","affiliations":[],"preferred":false,"id":742669,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Baseman, S.","contributorId":207075,"corporation":false,"usgs":false,"family":"Baseman","given":"S.","email":"","affiliations":[],"preferred":false,"id":742670,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fellowes, J.W.","contributorId":85451,"corporation":false,"usgs":true,"family":"Fellowes","given":"J.W.","email":"","affiliations":[],"preferred":false,"id":742671,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Oremland, Ronald S. 0000-0001-7382-0147 roremlan@usgs.gov","orcid":"https://orcid.org/0000-0001-7382-0147","contributorId":931,"corporation":false,"usgs":true,"family":"Oremland","given":"Ronald","email":"roremlan@usgs.gov","middleInitial":"S.","affiliations":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true},{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":742672,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70118766,"text":"70118766 - 2011 - <i>Boiga irregularis</i> (Brown Treesnake). Predation attempt by praying mantis","interactions":[],"lastModifiedDate":"2014-07-30T09:59:06","indexId":"70118766","displayToPublicDate":"2011-01-01T09:57:20","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1898,"text":"Herpetological Review","active":true,"publicationSubtype":{"id":10}},"title":"<i>Boiga irregularis</i> (Brown Treesnake). Predation attempt by praying mantis","docAbstract":"No abstract available.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Herpetological Review","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Society for the Study of Amphibians and Reptiles","publisherLocation":"Lawrence, KS","usgsCitation":"Lardner, B., Savidge, J., Reed, R., and Rodda, G.H., 2011, <i>Boiga irregularis</i> (Brown Treesnake). Predation attempt by praying mantis: Herpetological Review, v. 42, no. 3, p. 435-436.","productDescription":"2 p.","startPage":"435","endPage":"436","numberOfPages":"2","costCenters":[],"links":[{"id":291378,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"42","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57fe7fd9e4b0824b2d147984","contributors":{"authors":[{"text":"Lardner, Bjorn lardnerb@usgs.gov","contributorId":5546,"corporation":false,"usgs":true,"family":"Lardner","given":"Bjorn","email":"lardnerb@usgs.gov","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":true,"id":497185,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Savidge, Julie A.","contributorId":10225,"corporation":false,"usgs":true,"family":"Savidge","given":"Julie A.","affiliations":[],"preferred":false,"id":497187,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Reed, Robert N.","contributorId":10115,"corporation":false,"usgs":true,"family":"Reed","given":"Robert N.","affiliations":[],"preferred":false,"id":497186,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Rodda, Gordon H. roddag@usgs.gov","contributorId":3196,"corporation":false,"usgs":true,"family":"Rodda","given":"Gordon","email":"roddag@usgs.gov","middleInitial":"H.","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":true,"id":497184,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70048204,"text":"70048204 - 2011 - What is that mysterious booming sound?","interactions":[],"lastModifiedDate":"2013-09-17T09:59:48","indexId":"70048204","displayToPublicDate":"2011-01-01T09:57:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3372,"text":"Seismological Research Letters","onlineIssn":"1938-2057","printIssn":"0895-0695","active":true,"publicationSubtype":{"id":10}},"title":"What is that mysterious booming sound?","docAbstract":"The residents of coastal North Carolina are occasionally treated to sequences of booming sounds of unknown origin. The sounds are often energetic enough to rattle windows and doors. A recent sequence occurred in early January 2011 during clear weather with no evidence of local thunder storms. Queries by a local reporter (Colin Hackman of the NBC affiliate WETC in Wilmington, North Carolina, personal communication 2011) seemed to eliminate common anthropogenic sources such as sonic booms or quarry blasts. So the commonly asked question, “What's making these booming sounds?” remained (and remains) unanswered.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Seismological Research Letters","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Seismological Society of America","doi":"10.1785/gssrl.82.5.619","usgsCitation":"Hill, D.P., 2011, What is that mysterious booming sound?: Seismological Research Letters, v. 82, no. 5, p. 619-622, https://doi.org/10.1785/gssrl.82.5.619.","productDescription":"4 p.","startPage":"619","endPage":"622","numberOfPages":"4","ipdsId":"IP-030039","costCenters":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"links":[{"id":277609,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":277604,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1785/gssrl.82.5.619"}],"volume":"82","issue":"5","noUsgsAuthors":false,"publicationDate":"2011-09-02","publicationStatus":"PW","scienceBaseUri":"523979fde4b04b9308ae4fc3","contributors":{"authors":[{"text":"Hill, David P. hill@usgs.gov","contributorId":2600,"corporation":false,"usgs":true,"family":"Hill","given":"David","email":"hill@usgs.gov","middleInitial":"P.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true},{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true}],"preferred":false,"id":483984,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70256007,"text":"70256007 - 2011 - Land remote sensing and global environmental change: NASA's Earth observing system and the science of ASTER and MODIS","interactions":[],"lastModifiedDate":"2024-07-12T15:00:53.809854","indexId":"70256007","displayToPublicDate":"2011-01-01T09:56:23","publicationYear":"2011","noYear":false,"publicationType":{"id":4,"text":"Book"},"publicationSubtype":{"id":15,"text":"Monograph"},"title":"Land remote sensing and global environmental change: NASA's Earth observing system and the science of ASTER and MODIS","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Springer","doi":"10.1007/978-1-4419-6749-7","usgsCitation":"Ramachandran, B., Justice, C.O., and Abrams, M.J., 2011, Land remote sensing and global environmental change: NASA's Earth observing system and the science of ASTER and MODIS, 873 p., https://doi.org/10.1007/978-1-4419-6749-7.","productDescription":"873 p.","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":431009,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Ramachandran, Bhaskar bhaskar@usgs.gov","contributorId":3334,"corporation":false,"usgs":true,"family":"Ramachandran","given":"Bhaskar","email":"bhaskar@usgs.gov","affiliations":[{"id":223,"text":"Earth Resources Observation and Science (EROS) Center (Geography)","active":false,"usgs":true}],"preferred":true,"id":906342,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Justice, Christopher O.","contributorId":340140,"corporation":false,"usgs":false,"family":"Justice","given":"Christopher","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":906343,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Abrams, Michael J.","contributorId":88229,"corporation":false,"usgs":false,"family":"Abrams","given":"Michael","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":906344,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70118765,"text":"70118765 - 2011 - Alien reptiles and amphibians: a scientific compendium and analysis, by Fred Kraus","interactions":[],"lastModifiedDate":"2014-07-30T09:56:06","indexId":"70118765","displayToPublicDate":"2011-01-01T09:55:22","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1898,"text":"Herpetological Review","active":true,"publicationSubtype":{"id":10}},"title":"Alien reptiles and amphibians: a scientific compendium and analysis, by Fred Kraus","docAbstract":"No abstract available.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Herpetological Review","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Society for the Study of Amphibians and Reptiles","publisherLocation":"Lawrence, KS","usgsCitation":"Reed, R., 2011, Alien reptiles and amphibians: a scientific compendium and analysis, by Fred Kraus: Herpetological Review, v. 42, no. 2, p. 306-309.","productDescription":"4 p.","startPage":"306","endPage":"309","numberOfPages":"4","costCenters":[],"links":[{"id":291377,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"42","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57fe7fd9e4b0824b2d147986","contributors":{"authors":[{"text":"Reed, R.N. 0000-0001-8349-6168","orcid":"https://orcid.org/0000-0001-8349-6168","contributorId":49092,"corporation":false,"usgs":true,"family":"Reed","given":"R.N.","affiliations":[],"preferred":false,"id":497183,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70138917,"text":"70138917 - 2011 - Evaluation of adrenocortical function in Florida manatees (Trichechus manatus latirostris)","interactions":[],"lastModifiedDate":"2017-08-26T17:55:51","indexId":"70138917","displayToPublicDate":"2011-01-01T09:45:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3807,"text":"Zoo Biology","active":true,"publicationSubtype":{"id":10}},"title":"Evaluation of adrenocortical function in Florida manatees (Trichechus manatus latirostris)","docAbstract":"<p>The study objectives were to determine the predominant manatee glucocorticoid; validate assays to measure this glucocorticoid and adrenocorticotropic hormone (ACTH); determine diagnostic thresholds to distinguish physiological vs. pathological concentrations; identify differences associated with sex, age class, female reproductive status, capture time, and lactate; and determine the best methods for manatee biologists and clinicians to diagnose stress. Cortisol is the predominant manatee glucocorticoid. IMMULITE 1000 assays for cortisol and ACTH were validated. Precision yielded intra- and inter-assay coefficients of variation for serum cortisol: &le;23.5 and &le;16.7%; and ACTH: &le;6.9 and &le;8.5%. Accuracy resulted in a mean adjusted R(2)&ge;0.87 for serum cortisol and &ge;0.96 for ACTH. Assay analytical sensitivities for cortisol (0.1 &micro;g/dl) and ACTH (10.0 pg/ml) were verified. Methods were highly correlated with another IMMULITE 1000 for serum cortisol (r=0.97) and ACTH (r=0.98). There was no significant variation in cortisol or ACTH with sex or age class and no correlation with female progesterone concentrations. Cortisol concentrations were highest in unhealthy manatees, chronically stressed by disease or injury. ACTH was greatest in healthy free-ranging or short-term rehabilitating individuals, peracutely stressed by capture and handling. Cortisol concentrations &ge;1.0 &micro;g/dl were diagnostic of chronic stress; ACTH concentrations &ge;87.5 pg/ml were diagnostic of peracute stress. In healthy long-term captive manatees, cortisol (0.4&plusmn;0.2 &micro;g/dl) and ACTH (47.7&plusmn;15.9 pg/ml) concentrations were lower than healthy free-ranging, short-term rehabilitated or unhealthy manatees. Capture time was not significantly correlated with cortisol; ACTH correlation was borderline significant. Cortisol and ACTH were positively correlated with lactate.</p>","language":"English","publisher":"American Zoo and Aquarium Association","publisherLocation":"New York, NY","doi":"10.1002/zoo.20311","usgsCitation":"Tripp, K., Verstegen, J., Deutsch, C., Bonde, R.K., de Wit, M., Manire, C.A., Gaspard, J., and Harr, K., 2011, Evaluation of adrenocortical function in Florida manatees (Trichechus manatus latirostris): Zoo Biology, v. 30, no. 1, p. 17-31, https://doi.org/10.1002/zoo.20311.","productDescription":"15 p.","startPage":"17","endPage":"31","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-009224","costCenters":[{"id":566,"text":"Southeast Ecological Science Center","active":true,"usgs":true}],"links":[{"id":297507,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Florida","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -87.703857421875,\n              31.034108344903512\n            ],\n            [\n              -87.71484375,\n              30.845647420182598\n            ],\n            [\n              -87.528076171875,\n              30.230594564932193\n            ],\n            [\n              -86.165771484375,\n              30.20211367909724\n            ],\n            [\n              -85.440673828125,\n              29.554345125748267\n            ],\n            [\n              -84.034423828125,\n              29.878755346037977\n            ],\n            [\n              -83.03466796874999,\n              28.758028282691143\n            ],\n            [\n              -83.1884765625,\n              27.877928333679495\n            ],\n            [\n              -81.38671875,\n              25.055745117015316\n            ],\n            [\n              -81.97998046875,\n              24.47715001114869\n            ],\n            [\n              -81.134033203125,\n              24.53712939907994\n            ],\n            [\n              -79.9365234375,\n              25.443274612305746\n            ],\n            [\n              -79.87060546875,\n              26.853479438420024\n            ],\n            [\n              -81.265869140625,\n              30.65681556429287\n            ],\n            [\n              -81.990966796875,\n              30.93992433102347\n            ],\n            [\n              -82.19970703125,\n              30.694611546632302\n            ],\n            [\n              -84.7705078125,\n              30.78903675126116\n            ],\n            [\n              -84.9462890625,\n              31.005862904624205\n            ],\n            [\n              -87.703857421875,\n              31.034108344903512\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"30","issue":"1","publishingServiceCenter":{"id":7,"text":"Ft. Lauderdale PSC"},"noUsgsAuthors":false,"publicationDate":"2011-02-11","publicationStatus":"PW","scienceBaseUri":"54dd2b96e4b08de9379b3414","contributors":{"authors":[{"text":"Tripp, K.M.","contributorId":64774,"corporation":false,"usgs":true,"family":"Tripp","given":"K.M.","email":"","affiliations":[],"preferred":false,"id":539192,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Verstegen, J.P.","contributorId":9751,"corporation":false,"usgs":true,"family":"Verstegen","given":"J.P.","email":"","affiliations":[],"preferred":false,"id":539193,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Deutsch, C.","contributorId":29343,"corporation":false,"usgs":true,"family":"Deutsch","given":"C.","affiliations":[],"preferred":false,"id":539190,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bonde, Robert K. 0000-0001-9179-4376 rbonde@usgs.gov","orcid":"https://orcid.org/0000-0001-9179-4376","contributorId":2675,"corporation":false,"usgs":true,"family":"Bonde","given":"Robert","email":"rbonde@usgs.gov","middleInitial":"K.","affiliations":[{"id":566,"text":"Southeast Ecological Science Center","active":true,"usgs":true},{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"preferred":true,"id":539189,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"de Wit, M.","contributorId":43223,"corporation":false,"usgs":true,"family":"de Wit","given":"M.","email":"","affiliations":[],"preferred":false,"id":539194,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Manire, Charles A.","contributorId":20572,"corporation":false,"usgs":false,"family":"Manire","given":"Charles","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":539191,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Gaspard, J.","contributorId":77769,"corporation":false,"usgs":true,"family":"Gaspard","given":"J.","email":"","affiliations":[],"preferred":false,"id":539220,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Harr, K.E.","contributorId":102023,"corporation":false,"usgs":true,"family":"Harr","given":"K.E.","email":"","affiliations":[],"preferred":false,"id":539221,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":70198710,"text":"70198710 - 2011 - Hydrology and biogeochemistry linkages","interactions":[],"lastModifiedDate":"2018-08-29T09:44:23","indexId":"70198710","displayToPublicDate":"2011-01-01T09:39:27","publicationYear":"2011","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Hydrology and biogeochemistry linkages","docAbstract":"<div id=\"abstracts\" class=\"Abstracts\"><div id=\"aep-abstract-id1\" class=\"abstract author\"><div id=\"aep-abstract-sec-id2\"><p id=\"mc0042\">This chapter provides an overview of the linkages between hydrology and biogeochemistry in terrestrial and aquatic systems. Selected topics include hydrological pathways on drainage basin slopes, mountain environments, within-river (or in-stream) processes, wetlands, groundwater (and groundwater–surface water interactions), and lakes. Beginning from catchment headwaters, This chapter introduces mechanisms delivering water from hillslopes to stream channels, highlighting the relative importance of biogeochemical processes along hydrological pathways. It considers processes affecting components of the water budget, including snow formation and ablation processes, and interactions with the soil below snow cover and during snowmelt. It presents the concept of nutrient spiraling and the importance of temperature and stream flow variability on biogeochemistry, as well as groundwater–surface water interactions through hyporheic and riparian zones. This chapter contrasts important processes in hydrologically isolated wetlands with those temporally connected to streams and rivers. It addresses stream and groundwater inputs, stratification, and within-lake processes, interactions with sediments, and a discussion about limiting nutrients. This chapter presents information about typical reactions controlled by hydrological pathways, lithology (mineralogy) and biota, the importance of residence time in biogeochemical evolution, and linkages between groundwater Acidic atmospheric deposition</p></div></div></div><div class=\"Keywords\"><div id=\"aep-keywords-id3\" class=\"keywords-section\"><div class=\"keyword\"><br data-mce-bogus=\"1\"></div></div></div>","largerWorkType":{"id":5,"text":"Book chapter"},"largerWorkTitle":"Treatise on water science  ","language":"English","publisher":"Elsevier","doi":"10.1016/B978-0-444-53199-5.00038-5","usgsCitation":"Peters, N.E., Bohlke, J., Brooks, P.D., Burt, T., Gooseff, M.N., Hamilton, D., Mulholland, P.J., Roulet, N., and Turner, J., 2011, Hydrology and biogeochemistry linkages, chap. <i>of</i> Treatise on water science  , v. 2, p. 271-304, https://doi.org/10.1016/B978-0-444-53199-5.00038-5.","productDescription":"34 p.","startPage":"271","endPage":"304","costCenters":[{"id":316,"text":"Georgia Water Science Center","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true},{"id":34983,"text":"Contaminant Biology Program","active":true,"usgs":true}],"links":[{"id":356496,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5b98b489e4b0702d0e844b49","contributors":{"editors":[{"text":"Wilderer, P.","contributorId":207071,"corporation":false,"usgs":false,"family":"Wilderer","given":"P.","email":"","affiliations":[],"preferred":false,"id":742665,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Peters, Norman E. nepeters@usgs.gov","contributorId":1324,"corporation":false,"usgs":true,"family":"Peters","given":"Norman","email":"nepeters@usgs.gov","middleInitial":"E.","affiliations":[{"id":316,"text":"Georgia Water Science Center","active":true,"usgs":true}],"preferred":true,"id":742656,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bohlke, J. K. 0000-0001-5693-6455","orcid":"https://orcid.org/0000-0001-5693-6455","contributorId":59481,"corporation":false,"usgs":true,"family":"Bohlke","given":"J. K.","affiliations":[],"preferred":false,"id":742657,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brooks, P. D.","contributorId":46060,"corporation":false,"usgs":true,"family":"Brooks","given":"P.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":742658,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Burt, T.P.","contributorId":207072,"corporation":false,"usgs":false,"family":"Burt","given":"T.P.","email":"","affiliations":[],"preferred":false,"id":742659,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Gooseff, Michael N.","contributorId":71880,"corporation":false,"usgs":true,"family":"Gooseff","given":"Michael","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":742660,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Hamilton, David P.","contributorId":18633,"corporation":false,"usgs":true,"family":"Hamilton","given":"David P.","affiliations":[],"preferred":false,"id":742661,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Mulholland, P. J.","contributorId":89081,"corporation":false,"usgs":false,"family":"Mulholland","given":"P.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":742662,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Roulet, Nigel","contributorId":204027,"corporation":false,"usgs":false,"family":"Roulet","given":"Nigel","email":"","affiliations":[{"id":36802,"text":"McGill University, Canada","active":true,"usgs":false}],"preferred":false,"id":742663,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Turner, J.V.","contributorId":207073,"corporation":false,"usgs":false,"family":"Turner","given":"J.V.","email":"","affiliations":[],"preferred":false,"id":742664,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}}
,{"id":70006125,"text":"70006125 - 2011 - The Edwardsburg Formation and related rocks, Windermere Supergroup, central Idaho, USA","interactions":[],"lastModifiedDate":"2013-07-31T09:53:37","indexId":"70006125","displayToPublicDate":"2011-01-01T09:38:00","publicationYear":"2011","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"The Edwardsburg Formation and related rocks, Windermere Supergroup, central Idaho, USA","docAbstract":"In central Idaho, Neoproterozoic stratified rocks are engulfed by the Late Cretaceous Idaho batholith and by Eocene volcanic and plutonic rocks of the Challis event. Studied sections in the Gospel Peaks and Big Creek areas of west-central Idaho are in roof pendants of the Idaho batholith. A drill core section studied from near Challis, east-central Idaho, lies beneath the Challis Volcanic Group and is not exposed at the surface. Metamorphic and deformational overprinting, as well as widespread dismembering by the younger igneous rocks, conceals many primary details. Despite this, these rocks provide important links for regional correlations and have produced critical geochronological data for two Neoproterozoic glacial periods in the North American Cordillera.\n<br>\n<br>\nAt the base of the section, the more than 700-m-thick Edwardsburg Formation (Fm.) contains interlayered diamictite and volcanic rocks. There are two diamictite-bearing members in the Edwardsburg Fm. that are closely related in time. Each of the diamictites is associated with intermediate composition tuff or flow rocks and the diamictites are separated by mafic volcanic rocks. SHRIMP U–Pb dating indicates that the lower diamictite is about 685&plusmn;7 Ma, whereas the upper diamictite is 684&plusmn;4 Ma. The diamictite units are part of a cycle of rocks from coarse clastic, to fine clastic, to carbonate rocks that, by correlation to better preserved sections, are thought to record an older Cryogenian glacial to interglacial period in the northern US Cordillera.\n<br>\n<br>\nThe more than 75-m-thick diamictite of Daugherty Gulch is dated at 664&plusmn;6 Ma. This unit is preserved only in drill core and the palaeoenvironmental interpretation and local stratigraphic relations are non-unique. Thus, the date for this diamictite may provide a date for a newly recognized glaciogenic horizon or may be a minimum age for the diamictite in the Edwardsburg Fm.\n<br>\n<br>\nThe c. 1000-m-thick Moores Lake Fm. is an amphibolite facies diamictite in which glacial features have not been observed. However, it is part of a sedimentary cycle from unsorted siliclastic deposits to mud and carbonate deposits. Using lithostratigraphy and available geochronology, the Moores Lake Fm. is correlated with a younger succession of Cryogenian glaciogenic rocks in southeastern Idaho.\n<br>\n<br>\nTraditional correlations of Neoproterozoic rocks in the Cordillera recognize two levels of Cryogenian diamictites. The Edwardsburg and Moores Lake diamictites along the middle Cordillera fit well into the scenario of two glacial events. Because of the correlations, dates that provide ages for the diamictites in central Idaho (and corroborated in southeastern Idaho, Link & Fanning 2008) could constrain the age of correlated glaciogenic deposits elsewhere in the Cordillera. However, in the absence of dates for the glaciogenic diamictites in Canadian and southern US Cordilleran sections, the correlations are considered possible but uncertain.","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"The Geological Record of Neoproterozoic","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","publisher":"The Geological Society","publisherLocation":"London, UK","doi":"10.1144/M36.39","isbn":"9781862393349; 1862393346","usgsCitation":"Lund, K., Aleinikoff, J.N., and Evans, K.V., 2011, The Edwardsburg Formation and related rocks, Windermere Supergroup, central Idaho, USA, chap. <i>of</i> The Geological Record of Neoproterozoic, v. 36, p. 437-448, https://doi.org/10.1144/M36.39.","productDescription":"12 p.","startPage":"437","endPage":"448","numberOfPages":"12","ipdsId":"IP-003509","costCenters":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"links":[{"id":275616,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":275615,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1144/M36.39"}],"country":"United States","state":"Idaho","otherGeospatial":"Gospel Peaks;Big Creek","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -117.243,43.7115 ], [ -117.243,46.8441 ], [ -111.0436,46.8441 ], [ -111.0436,43.7115 ], [ -117.243,43.7115 ] ] ] } } ] }","volume":"36","noUsgsAuthors":false,"publicationDate":"2011-11-16","publicationStatus":"PW","scienceBaseUri":"51fa31e7e4b076c3a8d8268b","contributors":{"authors":[{"text":"Lund, Karen 0000-0002-4249-3582 klund@usgs.gov","orcid":"https://orcid.org/0000-0002-4249-3582","contributorId":1235,"corporation":false,"usgs":true,"family":"Lund","given":"Karen","email":"klund@usgs.gov","affiliations":[{"id":387,"text":"Mineral Resources Program","active":true,"usgs":true},{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":353888,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Aleinikoff, John N. 0000-0003-3494-6841 jaleinikoff@usgs.gov","orcid":"https://orcid.org/0000-0003-3494-6841","contributorId":1478,"corporation":false,"usgs":true,"family":"Aleinikoff","given":"John","email":"jaleinikoff@usgs.gov","middleInitial":"N.","affiliations":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":353889,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Evans, Karl V. kvevans@usgs.gov","contributorId":194,"corporation":false,"usgs":true,"family":"Evans","given":"Karl","email":"kvevans@usgs.gov","middleInitial":"V.","affiliations":[],"preferred":true,"id":353887,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70243780,"text":"70243780 - 2011 - Patch reefs: Lidar morphometric analysis","interactions":[],"lastModifiedDate":"2023-05-22T13:23:36.470597","indexId":"70243780","displayToPublicDate":"2011-01-01T09:35:53","publicationYear":"2011","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Patch reefs: Lidar morphometric analysis","docAbstract":"<p><span>Alina Reef is one of several thousand patch reefs that lie across the shallow carbonate platform seaward of Hawk Channel off the northern Florida Keys. The site is near the northern latitudinal fringe of the late Holocene western Atlantic coral reef distribution (Figure&nbsp;</span>1<span>). The area is covered by calcareous sand and discontinuous&nbsp;</span><i>Thalassia testudinum</i><span>&nbsp;seagrass meadows and is studded with numerous scattered Holocene patch reefs. Most of the patch reefs are found in water depths of 2–9 m, are subcircular, elliptical, or irregular in plan view, and range up to about 8 m in vertical relief and 700 m in width. Coring has demonstrated thicknesses of 4.5–6 m and has revealed frameworks built by large, massive head corals.</span></p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Encyclopedia of modern coral reefs: Structure, form and process","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Springer","doi":"10.1007/978-90-481-2639-2_240","usgsCitation":"Brock, J., and Palaseanu-Lovejoy, M., 2011, Patch reefs: Lidar morphometric analysis, chap. <i>of</i> Encyclopedia of modern coral reefs: Structure, form and process, p. 785-789, https://doi.org/10.1007/978-90-481-2639-2_240.","productDescription":"5 p.","startPage":"785","endPage":"789","ipdsId":"IP-016998","costCenters":[{"id":574,"text":"St. Petersburg Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":417245,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Florida","otherGeospatial":"Alina Reef, Atlantic Ocean, Florida Keys, Hawk Channel","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -80.18954542289619,\n              25.415248591004698\n            ],\n            [\n              -80.18954542289619,\n              25.382857620392258\n            ],\n            [\n              -80.15300840793584,\n              25.382857620392258\n            ],\n            [\n              -80.15300840793584,\n              25.415248591004698\n            ],\n            [\n              -80.18954542289619,\n              25.415248591004698\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"editors":[{"text":"Hopley, David","contributorId":305582,"corporation":false,"usgs":false,"family":"Hopley","given":"David","email":"","affiliations":[],"preferred":false,"id":873243,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Brock, John 0000-0002-5289-9332 jbrock@usgs.gov","orcid":"https://orcid.org/0000-0002-5289-9332","contributorId":2261,"corporation":false,"usgs":true,"family":"Brock","given":"John","email":"jbrock@usgs.gov","affiliations":[{"id":5061,"text":"National Cooperative Geologic Mapping and Landslide Hazards","active":true,"usgs":true}],"preferred":true,"id":873230,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Palaseanu-Lovejoy, Monica 0000-0002-3786-5118","orcid":"https://orcid.org/0000-0002-3786-5118","contributorId":305576,"corporation":false,"usgs":true,"family":"Palaseanu-Lovejoy","given":"Monica","affiliations":[],"preferred":true,"id":873231,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70199908,"text":"70199908 - 2011 - Long-term natural attenuation of crude oil in the subsurface","interactions":[],"lastModifiedDate":"2018-10-03T11:07:21","indexId":"70199908","displayToPublicDate":"2011-01-01T09:25:50","publicationYear":"2011","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Long-term natural attenuation of crude oil in the subsurface","docAbstract":"<p>The time frame for natural attenuation of crude oil contamination in the subsurface has been studied for the last 27 years at a spill site located near Bemidji, Minnesota, USA. Data from the<br>groundwater contaminant plume show that dissolved benzene concentrations adjacent to the oil decreased by 50% between 1993 and 2007. To assess how this decrease is related to benzene<br>concentrations in the crude oil, samples of oil were bailed from floating oil in five wells and analysed for volatile components. Compared to reference oil collected from the pipeline in 1984, benzene<br>concentrations in the well located farthest downgradient in the oil have decreased an average of 50%. Benzene and ethylbenzene depletion are linearly correlated with oil saturation in the pore space<br>suggesting that dissolution is the primary removal mechanism and biodegradation within the oil body is insignificant.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Groundwater management in a rapidly changing world: Proceedings of the 7th international groundwater quality conference","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"7th International Groundwater Quality Conference","conferenceLocation":"Zurich, Switzerland","language":"English","publisher":"International Association of Hydrologic Sciences","publisherLocation":"Zurich, Switzerland","usgsCitation":"Bekins, B.A., Baedecker, M.J., Eganhouse, R., and Herkelrath, W.N., 2011, Long-term natural attenuation of crude oil in the subsurface, <i>in</i> Groundwater management in a rapidly changing world: Proceedings of the 7th international groundwater quality conference, Zurich, Switzerland, p. 123-127.","productDescription":"5 p.","startPage":"123","endPage":"127","costCenters":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true},{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true},{"id":36183,"text":"Hydro-Ecological Interactions Branch","active":true,"usgs":true}],"links":[{"id":358083,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5c10c276e4b034bf6a7f1849","contributors":{"authors":[{"text":"Bekins, Barbara A. 0000-0002-1411-6018 babekins@usgs.gov","orcid":"https://orcid.org/0000-0002-1411-6018","contributorId":1348,"corporation":false,"usgs":true,"family":"Bekins","given":"Barbara","email":"babekins@usgs.gov","middleInitial":"A.","affiliations":[{"id":36183,"text":"Hydro-Ecological Interactions Branch","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true},{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true},{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":747246,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Baedecker, Mary Jo 0000-0002-4865-1043 mjbaedec@usgs.gov","orcid":"https://orcid.org/0000-0002-4865-1043","contributorId":197793,"corporation":false,"usgs":true,"family":"Baedecker","given":"Mary","email":"mjbaedec@usgs.gov","middleInitial":"Jo","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":747247,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Eganhouse, Robert P. eganhous@usgs.gov","contributorId":2031,"corporation":false,"usgs":true,"family":"Eganhouse","given":"Robert P.","email":"eganhous@usgs.gov","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":747248,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Herkelrath, William N. 0000-0002-6149-5524 wnherkel@usgs.gov","orcid":"https://orcid.org/0000-0002-6149-5524","contributorId":2612,"corporation":false,"usgs":true,"family":"Herkelrath","given":"William","email":"wnherkel@usgs.gov","middleInitial":"N.","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":747249,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70212839,"text":"70212839 - 2011 - Introduction: An ecoregional assessment of the Wyoming Basins","interactions":[{"subject":{"id":70212839,"text":"70212839 - 2011 - Introduction: An ecoregional assessment of the Wyoming Basins","indexId":"70212839","publicationYear":"2011","noYear":false,"chapter":"Introduction","title":"Introduction: An ecoregional assessment of the Wyoming Basins"},"predicate":"IS_PART_OF","object":{"id":70118768,"text":"70118768 - 2011 - Sagebrush ecosystem conservation and management: Ecoregional assessment tools and models for the Wyoming Basins","indexId":"70118768","publicationYear":"2011","noYear":false,"title":"Sagebrush ecosystem conservation and management: Ecoregional assessment tools and models for the Wyoming Basins"},"id":1}],"isPartOf":{"id":70118768,"text":"70118768 - 2011 - Sagebrush ecosystem conservation and management: Ecoregional assessment tools and models for the Wyoming Basins","indexId":"70118768","publicationYear":"2011","noYear":false,"title":"Sagebrush ecosystem conservation and management: Ecoregional assessment tools and models for the Wyoming Basins"},"lastModifiedDate":"2020-08-31T14:50:13.685895","indexId":"70212839","displayToPublicDate":"2011-01-01T09:19:17","publicationYear":"2011","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"chapter":"Introduction","title":"Introduction: An ecoregional assessment of the Wyoming Basins","docAbstract":"<p>The Wyoming Basins Ecoregional Assessment (WBEA) area in the western United States contains a number of important land cover types, including nearly one-fourth of the sagebrush (<i>Artemisia</i> spp.) in North America. Although relatively unappreciated until recent decades, the broad open landscapes dominated by sagebrush communities have received increasing attention for their ecological value and the resources that they contain (Knick and Connelly 2011). As many as 350 wildlife species depend on sagebrush ecosystems for all or part of their life requirements (Wisdom et al. 2005a). Within the WBEA, intact sagebrush landscapes provide an important stronghold for populations of greater sage-grouse (<i>Centrocercus urophasianus</i>), recently listed as a candidate species under the Endangered Species Act (U.S. Department of the Interior 2010). Numerous other plant and vertebrate species of state or national concern also occur within the WBEA study area (Ch. 2). Conserving sagebrush ecosystems is a major conservation challenge that will require an understanding not only of current trajectories and scales of habitat change due to natural and anthropogenic disturbances (Leu and Hanser 2011), but also the potential exacerbation of these trends from climate change (Wiens and Bachelet 2010, Miller et al. 2011).</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Sagebrush ecosystem conservation and management: Ecoregional assessment tools and models for the Wyoming Basins","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Allen Press","publisherLocation":"Lawrence, Kansas","isbn":"978-0-615-55530-0","usgsCitation":"Knick, S.T., Hanser, S.E., Leu, M., Aldridge, C.L., and Wisdom, M.J., 2011, Introduction: An ecoregional assessment of the Wyoming Basins, chap. Introduction <i>of</i> Sagebrush ecosystem conservation and management: Ecoregional assessment tools and models for the Wyoming Basins, p. 1-9.","productDescription":"9 p.","startPage":"1","endPage":"9","numberOfPages":"9","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true},{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"links":[{"id":378006,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":378032,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/ja/70212839/70212839.pdf","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"The U.S. Geological Survey has been given express permission by the publisher to provide full-text access online for this publication, and is posted with the express permission from the Publications Warehouse Guidance Subcommittee"}],"country":"United States","state":"Wyoming","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -111.0569,40.9947 ], [ -111.0569,45.0059 ], [ -104.0522,45.0059 ], [ -104.0522,40.9947 ], [ -111.0569,40.9947 ] ] ] } } ] }","publicComments":"The U.S. Geological Survey has been given express permission by the publisher to provide full-text access online for this publication, and is posted with the express permission from the Publications Warehouse Guidance Subcommittee","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Knick, Steven T. 0000-0003-4025-1704 steve_knick@usgs.gov","orcid":"https://orcid.org/0000-0003-4025-1704","contributorId":159,"corporation":false,"usgs":true,"family":"Knick","given":"Steven","email":"steve_knick@usgs.gov","middleInitial":"T.","affiliations":[{"id":289,"text":"Forest and Rangeland Ecosys Science Center","active":true,"usgs":true},{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true}],"preferred":true,"id":797614,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hanser, Steve E. 0000-0002-4430-2073 shanser@usgs.gov","orcid":"https://orcid.org/0000-0002-4430-2073","contributorId":152523,"corporation":false,"usgs":true,"family":"Hanser","given":"Steve","email":"shanser@usgs.gov","middleInitial":"E.","affiliations":[{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true},{"id":289,"text":"Forest and Rangeland Ecosys Science Center","active":true,"usgs":true},{"id":411,"text":"National Climate Change and Wildlife Science Center","active":true,"usgs":true},{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true},{"id":506,"text":"Office of the AD Ecosystems","active":true,"usgs":true}],"preferred":true,"id":797615,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Leu, Matthias","contributorId":68393,"corporation":false,"usgs":true,"family":"Leu","given":"Matthias","affiliations":[],"preferred":false,"id":797616,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Aldridge, Cameron L. 0000-0003-3926-6941 aldridgec@usgs.gov","orcid":"https://orcid.org/0000-0003-3926-6941","contributorId":191773,"corporation":false,"usgs":true,"family":"Aldridge","given":"Cameron","email":"aldridgec@usgs.gov","middleInitial":"L.","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":false,"id":797617,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Wisdom, Michael J.","contributorId":63934,"corporation":false,"usgs":true,"family":"Wisdom","given":"Michael","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":797618,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70048665,"text":"70048665 - 2011 - Deep rock damage in the San Andreas Fault revealed by P- and S-type fault-zone-guided waves","interactions":[],"lastModifiedDate":"2019-06-18T18:05:35","indexId":"70048665","displayToPublicDate":"2011-01-01T09:17:00","publicationYear":"2011","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Deep rock damage in the San Andreas Fault revealed by P- and S-type fault-zone-guided waves","docAbstract":"Damage to fault-zone rocks during fault slip results in the formation of a channel of low seismic-wave velocities. Within such channels guided seismic waves, denoted by Fg, can propagate.  Here we show with core samples, well logs and Fg-waves that such a channel is crossed by the SAFOD (San Andreas Fault Observatory at Depth) borehole at a depth of 2.7 km near Parkfield, California, USA. This laterally extensive channel extends downwards to at least half way through the seismogenic crust, more than about 7 km. The channel supports not only the previously recognized Love-type- (FL) and Rayleigh-type- (FR) guided waves, but also a new fault-guided wave, which we name FF. As recorded 2.7 km underground, FF is normally dispersed, ends in an Airy phase, and arrives between the P- and S-waves. Modelling shows that FF travels as a leaky mode within the core of the fault zone. Combined with the drill core samples, well logs and the two other types of guided waves, FF at SAFOD reveals a zone of profound, deep, rock damage.  Originating from damage accumulated over the recent history of fault movement, we suggest it is maintained either by fracturing near the slip surface of earthquakes, such as the 1857 Fort Tejon M 7.9, or is an unexplained part of the fault-creep process known to be active at this site.","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Geology of the earthquake source: a volume in honour of Rick Sibson","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","publisher":"Geological Society of London","doi":"10.1144/SP359.3","isbn":"9781862393370","usgsCitation":"Ellsworth, W.L., and Malin, P.E., 2011, Deep rock damage in the San Andreas Fault revealed by P- and S-type fault-zone-guided waves, chap. <i>of</i> Geology of the earthquake source: a volume in honour of Rick Sibson, v. 359, p. 39-53, https://doi.org/10.1144/SP359.3.","productDescription":"15 p.","startPage":"39","endPage":"53","ipdsId":"IP-012016","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"links":[{"id":278498,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":278497,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1144/SP359.3"}],"country":"United States","state":"California","otherGeospatial":"San Andreas Fault","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -120.452654,35.879686 ], [ -120.452654,35.919686 ], [ -120.412654,35.919686 ], [ -120.412654,35.879686 ], [ -120.452654,35.879686 ] ] ] } } ] }","volume":"359","noUsgsAuthors":false,"publicationDate":"2011-12-02","publicationStatus":"PW","scienceBaseUri":"5270d902e4b0f7a10664fb9d","contributors":{"authors":[{"text":"Ellsworth, William L. ellsworth@usgs.gov","contributorId":787,"corporation":false,"usgs":true,"family":"Ellsworth","given":"William","email":"ellsworth@usgs.gov","middleInitial":"L.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":485347,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Malin, Peter E.","contributorId":40889,"corporation":false,"usgs":true,"family":"Malin","given":"Peter","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":485348,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
]}