{"pageNumber":"1229","pageRowStart":"30700","pageSize":"25","recordCount":165227,"records":[{"id":70227708,"text":"70227708 - 2015 - Book reviews: The Double-crested Cormorant, plight of a feathered pariah, by L.R. Wires/The birds of New Hampshire by Allan R, Keith and Robert P. Fox","interactions":[],"lastModifiedDate":"2022-01-27T15:08:37.814516","indexId":"70227708","displayToPublicDate":"2015-01-01T09:00:18","publicationYear":"2015","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3544,"text":"The Auk","onlineIssn":"1938-4254","printIssn":"0004-8038","active":true,"publicationSubtype":{"id":10}},"title":"Book reviews: The Double-crested Cormorant, plight of a feathered pariah, by L.R. Wires/The birds of New Hampshire by Allan R, Keith and Robert P. Fox","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Oxford Academic","doi":"10.1642/AUK-14-177.1","usgsCitation":"Engstrom, R.T., Roby, D., and Greenlaw, J.S., 2015, Book reviews: The Double-crested Cormorant, plight of a feathered pariah, by L.R. Wires/The birds of New Hampshire by Allan R, Keith and Robert P. Fox: The Auk, v. 132, no. 1, p. 315-317, https://doi.org/10.1642/AUK-14-177.1.","productDescription":"3 p.","startPage":"315","endPage":"317","ipdsId":"IP-077721","costCenters":[{"id":200,"text":"Coop Res Unit Seattle","active":true,"usgs":true}],"links":[{"id":472387,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1642/auk-14-177.1","text":"Publisher Index Page"},{"id":394969,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"132","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Engstrom, R. Todd","contributorId":32773,"corporation":false,"usgs":true,"family":"Engstrom","given":"R.","email":"","middleInitial":"Todd","affiliations":[],"preferred":false,"id":831966,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Roby, Daniel D. 0000-0001-9844-0992","orcid":"https://orcid.org/0000-0001-9844-0992","contributorId":272248,"corporation":false,"usgs":true,"family":"Roby","given":"Daniel D.","affiliations":[{"id":200,"text":"Coop Res Unit Seattle","active":true,"usgs":true}],"preferred":true,"id":831856,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Greenlaw, Jon S.","contributorId":272347,"corporation":false,"usgs":false,"family":"Greenlaw","given":"Jon","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":831967,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70191871,"text":"70191871 - 2015 - Climate change in the Northeast and Midwest United States","interactions":[],"lastModifiedDate":"2020-07-29T14:04:14.1715","indexId":"70191871","displayToPublicDate":"2015-01-01T00:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":9,"text":"Other Report"},"chapter":"1","title":"Climate change in the Northeast and Midwest United States","docAbstract":"<p>The climate is changing rapidly in ways that have already impacted wildlife and their habitats. Here, we present a summary of the observed past and projected future climate changes in the region that are relevant to wildlife and ecosystems, as well as what we know and don’t know in order to raise managers’ confidence in their planning. A number of large-scale regional changes affect the overall terrestrial landscape within the Northeast and Midwest United States: </p><p><ul><li>Warming is occurring in every season, particularly in winter, at higher latitudes, at higher elevations, and inland (i.e. away from the ocean and lake coasts).<br></li><li>Heatwaves may become more frequent, more intense, and last longer.<br></li><li>Precipitation amounts are increasing, particularly in winter and with respect to highintensity events in summer.<br></li><li>Snow is shifting to rain, leading to reduced snowpacks and extent of snow cover, as well as harder, crustier snowpacks.<br></li><li>Atmospheric moisture content is likely to increase.<br></li><li>Wind speeds are declining, though wind gusts may be intensifying.<br></li><li>Streamflows are intensifying.<br></li><li>Streams are warming.<br></li><li>Thunderstorms may become more severe.<br></li><li>Floods are intensifying, yet droughts are also on the rise as dry periods between events get longer.<br></li><li>Blizzards and ice storms are occurring more often in some areas, though most areas experiencing milder winters (i.e., warmer and with less snow).<br></li><li>Growing seasons are getting longer, with more growing degree days accumulating earlier in the season.<br></li></ul></p><p>In addition, localized climate change is occurring in specific regions: </p><p><ul><li>U.S. Atlantic coast<br></li><ul><li>Sea level is rising at an accelerating rate.</li><li>Tropical cyclones and hurricanes may be intensifying and storm tracks have been shifting northward along the coast.</li><li>Oceans are warming and becoming more acidic.</li></ul><li>Great Lakes<br></li><ul><li>The lakes are warming.</li><li>Winter maximum lake ice extent is shrinking.</li><li>Lake evaporation rates are increasing.</li><li>Lake-effect snow events are becoming more severe, longer lasting, and shifting to rain, but occurring less often.</li><li>Water levels have decreased, but may not be linked to anthropogenic climate change.</li></ul><li>Appalachians<br></li><ul><li>Warming may be occurring more rapidly at higher elevations.</li><li>Greater intensification of heavy rainfall events may be occurring.</li></ul></ul></p><p>In the short term (i.e., over the next 5-20 years), the direction and magnitude of warming in the global climate are mostly consistent across all emissions scenarios and with strong agreement across models. Accordingly, we are certain that the Northeast and Midwest will see longer growing seasons. We are likely to see shifts from snow to rain, though shifts in the amount of total precipitation (rain and snow) are less certain. Severe weather events (e.g., thunderstorms, tornadoes) are challenging to detect. Soil moisture and evapotranspiration trends are neither robustly observed nor consistent amongst modeling studies.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Integrating climate change into northeast and midwest State Wildlife Action Plans","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","publisher":"Northeast Climate Science Center","usgsCitation":"Bryan, A., Karmalkar, A., Coffel, E., Ning, L., Horton, R.M., Demaria, E., Fan, F., Bradley, R.S., and Palmer, R., 2015, Climate change in the Northeast and Midwest United States, 51 p.","productDescription":"51 p.","startPage":"6","endPage":"57","ipdsId":"IP-065184","costCenters":[{"id":41705,"text":"Northeast Climate Science Center","active":true,"usgs":true}],"links":[{"id":352203,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":346866,"type":{"id":15,"text":"Index Page"},"url":"https://necsc.umass.edu/projects/integrating-climate-change-state-wildlife-action-plans"}],"country":"United States","state":"Connecticut, Delaware, Iowa, Illinois, Indiana, Kentucky, Massachusetts, Maryland, Maine, Michigan, Missouri, Minnesota, New Hampshire, New Jersey, New York, Ohio, Pennsylvania, Rhode Island, Virginia, Vermont, Wisconsin, West 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,{"id":70048179,"text":"70048179 - 2015 - Lake formation, characteristics and evolution in retroarc deposystems:  A synthesis of data from the modern Andean orogen and its associated basins","interactions":[],"lastModifiedDate":"2018-07-17T09:41:09","indexId":"70048179","displayToPublicDate":"2015-01-01T00:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Lake formation, characteristics and evolution in retroarc deposystems:  A synthesis of data from the modern Andean orogen and its associated basins","docAbstract":"<p>Lake deposystems are commonly associated with retroarc mountain belts in the geological record. These deposystems are poorly characterized in modern retroarcs, placing limits on our ability to interpret environmental signals from ancient deposits. To address this problem, we have synthesized our existing knowledge about the distribution, morphometrics, and sedimentary geochemical characteristics of tectonically formed lakes in the central Andean retroarc. Large, active mountain belts such as the Andes frequently create an excess of sediment, to the point that modeling and observational data both suggest their adjacent retroarc basins will be rapidly overfilled by sediments. Lake formation, requiring topographic closure, demands special conditions such as topographic isolation and arid climatic conditions to reduce sediment generation, and bedrock lithologies that yield little siliciclastic sediment.</p><p>Lacustrine deposition in the modern Andean retroarc has different characteristics in the six major morphotectonic zones discussed. (1) High-elevation hinterland basins of the arid Puna-Altiplano Plateau frequently contain underfilled and balanced-filled lakes that are potentially long-lived and display relatively rapid sedimentation rates. (2) Lakes are rare in piggyback basins, although a transition zone exists where basins that originally formed as piggybacks are transferred to the hinterland through forward propagation of the thrust belt. Here, lakes are moderately abundant and long-lived and display somewhat lower sedimentation rates than in the hinterland. (3) Wedge-top and (4) foredeep deposystems of the Andean retroarc are generally overfilled, and lakes are small and ephemeral. (5) Semihumid Andean back-bulge basins contain abundant small lakes, which are moderately long-lived because of underfilling by sediment and low sedimentation rates. (6) Broken foreland lakes are common, typically underfilled, large, and long-lived playa or shallow systems.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Geodynamic of a cordilleran orogenic system: The central Andes of Argentina and northern Chile ","publisher":"Geological Society of America","doi":"10.1130/2015.1212(16)","usgsCitation":"Cohen, A.S., McGlue, M., Ellis, G.S., Zani, H., Swarzenski, P.W., Assine, M.L., and Silva, A., 2015, Lake formation, characteristics and evolution in retroarc deposystems:  A synthesis of data from the modern Andean orogen and its associated basins, chap. <i>of</i> Geodynamic of a cordilleran orogenic system: The central Andes of Argentina and northern Chile , v. 212, p. 309-335, https://doi.org/10.1130/2015.1212(16).","productDescription":"27 p.","startPage":"309","endPage":"335","ipdsId":"IP-043891","costCenters":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"links":[{"id":488780,"rank":0,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"http://hdl.handle.net/11449/227914","text":"External Repository"},{"id":355704,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Andes Mountains","volume":"212","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5b6fcc80e4b0f5d57878ece3","contributors":{"editors":[{"text":"DeCelles, Peter G.","contributorId":16318,"corporation":false,"usgs":true,"family":"DeCelles","given":"Peter","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":740145,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Ducea, Mihai N.","contributorId":86913,"corporation":false,"usgs":true,"family":"Ducea","given":"Mihai N.","affiliations":[],"preferred":false,"id":740146,"contributorType":{"id":2,"text":"Editors"},"rank":2},{"text":"Carrapa, Barbara","contributorId":9958,"corporation":false,"usgs":true,"family":"Carrapa","given":"Barbara","email":"","affiliations":[],"preferred":false,"id":740147,"contributorType":{"id":2,"text":"Editors"},"rank":3},{"text":"Kapp, Paul","contributorId":79402,"corporation":false,"usgs":true,"family":"Kapp","given":"Paul","email":"","affiliations":[],"preferred":false,"id":740148,"contributorType":{"id":2,"text":"Editors"},"rank":4}],"authors":[{"text":"Cohen, Andrew S.","contributorId":138496,"corporation":false,"usgs":false,"family":"Cohen","given":"Andrew","email":"","middleInitial":"S.","affiliations":[{"id":6624,"text":"University of Arizona, Laboratory of Tree-Ring Research","active":true,"usgs":false}],"preferred":false,"id":740141,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McGlue, Michael M.","contributorId":118649,"corporation":false,"usgs":true,"family":"McGlue","given":"Michael M.","affiliations":[],"preferred":false,"id":518193,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ellis, Geoffrey S. 0000-0003-4519-3320 gsellis@usgs.gov","orcid":"https://orcid.org/0000-0003-4519-3320","contributorId":1058,"corporation":false,"usgs":true,"family":"Ellis","given":"Geoffrey","email":"gsellis@usgs.gov","middleInitial":"S.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":518192,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Zani, Hiran","contributorId":29119,"corporation":false,"usgs":true,"family":"Zani","given":"Hiran","email":"","affiliations":[],"preferred":false,"id":740142,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Swarzenski, Peter W. 0000-0003-0116-0578 pswarzen@usgs.gov","orcid":"https://orcid.org/0000-0003-0116-0578","contributorId":1070,"corporation":false,"usgs":true,"family":"Swarzenski","given":"Peter","email":"pswarzen@usgs.gov","middleInitial":"W.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":518194,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Assine, Mario L.","contributorId":102618,"corporation":false,"usgs":true,"family":"Assine","given":"Mario","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":740143,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Silva, Aguinaldo","contributorId":15750,"corporation":false,"usgs":true,"family":"Silva","given":"Aguinaldo","email":"","affiliations":[],"preferred":false,"id":740144,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70179620,"text":"70179620 - 2015 - Scale-appropriate adaptation strategies and actions in the Northeast and Midwest United States","interactions":[],"lastModifiedDate":"2020-07-29T14:11:33.713224","indexId":"70179620","displayToPublicDate":"2015-01-01T00:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"chapter":"4","title":"Scale-appropriate adaptation strategies and actions in the Northeast and Midwest United States","docAbstract":"<ul><li>Climate Change Adaptation is a growing field within conservation and natural resource management. Actions taken toward climate change adaptation account for climate impacts and ecological responses, both current and projected into the future. These actions attempt to accomplish a number of goals, including the conservation of wildlife and ecosystems by reducing vulnerability and increasing resilience.<br></li><li>Climate change adaptation strategies and approaches for natural resources can be thought of as part of a continuum of potential actions ranging from 1) options or goals to 2) strategies, 3) approaches, and 4) tactics.<br></li><li>There are a range of decision support tools and processes to aid climate change adaptation. This document highlights several including the Adaptation Workbook, Climate Change Vulnerability Assessments, Structured Decision Making, Adaptive Resource Management, and Scenario Planning. It will also provide case studies on the application of these tools across the Northeast and Midwest.<br></li><li>Improved, better-integrated, and increasingly coordinated monitoring systems would be helpful to detect, track, and attribute species and habitat shifts to climate change over spatiotemporal scales. We highlight regional examples of projects and programs addressing these challenges.<br></li><li>Illustrative case studies of climate change adaptation efforts are presented across landscape/ecoregion, state, and local scales.<br></li><li>Appendix 4.1 provides a synthesis of over 900 general, species and habitat-specific adaptation strategies and tactics from 9 regional studies being considered or implemented across the region.<br></li></ul><p>The study of climate change adaptation is a relatively new and rapidly growing field focused on preparing for and responding to the current and future impacts of climate change. The goal of this chapter is to highlight different approaches, processes, and tools currently being used across the region through illustrative case studies at varying scales. In addition, we provide a synthesis of numerous species and habitat-specific adaptation strategies and actions from existing assessment reports and management plans, which is intended to showcase a range of possibilities for natural resource management under future global change. This report does not prescribe one specific approach to taking action; instead, we outline a range of adaptation 5 tactics, which will require thoughtful consideration of the needs of the species, habitat, and location, the stakeholders and partners involved, the scale that a decision or policy is being implemented at, and the financial and personnel resources available to managers. </p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Integrating climate change into northeast and midwest State Wildlife Action Plans","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","publisher":"Northeast Climate Science Center","usgsCitation":"Staudinger, M., Hilberg, L., Janowiak, M., Caldwell, C., D’Amato, A.W., Grant, E., Horton, R., Katz, R.A., Neiil, C., Nislow, K.H., Potter, K., Rowland, E., Swanston, C., Thompson, F., and Winiarski, K.J., 2015, Scale-appropriate adaptation strategies and actions in the Northeast and Midwest United States, 52 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,{"id":70193069,"text":"70193069 - 2015 - Ursus maritimus","interactions":[],"lastModifiedDate":"2017-11-30T13:18:50","indexId":"70193069","displayToPublicDate":"2015-01-01T00:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Ursus maritimus","docAbstract":"<p>No abstract available.</p>","largerWorkTitle":"The IUCN Red List of Threatened Species 2015","language":"English","publisher":"International Union for Conservation of Nature","doi":"10.2305/IUCN.UK.2015-4.RLTS.T22823A14871490.en","usgsCitation":"Wiig, O., Amstrup, S.C., Atwood, T.C., Kaidre, K.L., Lunn, N.J., Obbard, M.E., Regehr, E.V., and Thiemann, G.W., 2015, Ursus maritimus, chap. <i>of</i> The IUCN Red List of Threatened Species 2015, HTML Document, https://doi.org/10.2305/IUCN.UK.2015-4.RLTS.T22823A14871490.en.","productDescription":"HTML Document","ipdsId":"IP-070477","costCenters":[{"id":116,"text":"Alaska Science Center Biology MFEB","active":true,"usgs":true}],"links":[{"id":472410,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.2305/iucn.uk.2015-4.rlts.t22823a14871490.en","text":"Publisher Index Page"},{"id":349595,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"publishingServiceCenter":{"id":12,"text":"Tacoma PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5a60fec8e4b06e28e9c2535f","contributors":{"authors":[{"text":"Wiig, Oystein","contributorId":192053,"corporation":false,"usgs":false,"family":"Wiig","given":"Oystein","email":"","affiliations":[],"preferred":false,"id":717806,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Amstrup, Steven C.","contributorId":67034,"corporation":false,"usgs":false,"family":"Amstrup","given":"Steven","email":"","middleInitial":"C.","affiliations":[{"id":13182,"text":"Polar Bears International","active":true,"usgs":false}],"preferred":false,"id":717807,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Atwood, Todd C. 0000-0002-1971-3110 tatwood@usgs.gov","orcid":"https://orcid.org/0000-0002-1971-3110","contributorId":4368,"corporation":false,"usgs":true,"family":"Atwood","given":"Todd","email":"tatwood@usgs.gov","middleInitial":"C.","affiliations":[{"id":116,"text":"Alaska Science Center Biology MFEB","active":true,"usgs":true},{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"preferred":true,"id":717805,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Kaidre, Kristin L","contributorId":198990,"corporation":false,"usgs":false,"family":"Kaidre","given":"Kristin","email":"","middleInitial":"L","affiliations":[],"preferred":false,"id":717808,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Lunn, Nicholas J","contributorId":198991,"corporation":false,"usgs":false,"family":"Lunn","given":"Nicholas","email":"","middleInitial":"J","affiliations":[],"preferred":false,"id":717809,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Obbard, Martyn E.","contributorId":108002,"corporation":false,"usgs":false,"family":"Obbard","given":"Martyn","email":"","middleInitial":"E.","affiliations":[{"id":6780,"text":"Ontario Ministry of Natural Resources","active":true,"usgs":false}],"preferred":false,"id":717810,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Regehr, Eric V. 0000-0003-4487-3105","orcid":"https://orcid.org/0000-0003-4487-3105","contributorId":66364,"corporation":false,"usgs":false,"family":"Regehr","given":"Eric","email":"","middleInitial":"V.","affiliations":[{"id":12428,"text":"U. S. Fish and Wildlife Service","active":true,"usgs":false}],"preferred":false,"id":717811,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Thiemann, Gregory W.","contributorId":83023,"corporation":false,"usgs":false,"family":"Thiemann","given":"Gregory","email":"","middleInitial":"W.","affiliations":[{"id":27291,"text":"York University, Toronto, ON","active":true,"usgs":false}],"preferred":false,"id":717812,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":70187040,"text":"70187040 - 2015 - San Andreas tremor cascades define deep fault zone complexity","interactions":[],"lastModifiedDate":"2017-04-19T15:43:23","indexId":"70187040","displayToPublicDate":"2015-01-01T00:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2845,"text":"Nature Geoscience","active":true,"publicationSubtype":{"id":10}},"title":"San Andreas tremor cascades define deep fault zone complexity","docAbstract":"<p><span>Weak seismic vibrations - tectonic tremor - can be used to delineate some plate boundary faults. Tremor on the deep San&nbsp;Andreas Fault, located at the boundary between the Pacific and North American plates, is thought to be a passive indicator of slow fault slip. San Andreas Fault tremor migrates at up to 30 m s<sup>-</sup></span><sup>1</sup><span>, but the processes regulating tremor migration are unclear. Here I use a 12-year catalogue of more than 850,000 low-frequency earthquakes to systematically analyse the high-speed migration of tremor along the San Andreas Fault. I find that tremor migrates most effectively through regions of greatest tremor production and does not propagate through regions with gaps in tremor production. I interpret the rapid tremor migration as a self-regulating cascade of seismic ruptures along the fault, which implies that tremor may be an active, rather than passive participant in the slip propagation. I also identify an isolated group of tremor sources that are offset eastwards beneath the San Andreas Fault, possibly indicative of the interface between the Monterey Microplate, a hypothesized remnant of the subducted Farallon Plate, and the North American Plate. These observations illustrate a possible link between the central San Andreas Fault and tremor-producing subduction zones.</span></p>","language":"English","publisher":"Nature Publishing Group","doi":"10.1038/ngeo2335","usgsCitation":"Shelly, D.R., 2015, San Andreas tremor cascades define deep fault zone complexity: Nature Geoscience, v. 8, no. 2, p. 145-252, https://doi.org/10.1038/ngeo2335.","productDescription":"8 p.","startPage":"145","endPage":"252","ipdsId":"IP-057784","costCenters":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"links":[{"id":339995,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"San Andreas Fault","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -121.1,\n              36.6\n            ],\n            [\n              -119.8,\n              36.6\n            ],\n            [\n              -119.8,\n              35.3\n            ],\n            [\n              -121.1,\n              35.3\n            ],\n            [\n              -121.1,\n              36.6\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"8","issue":"2","publishingServiceCenter":{"id":14,"text":"Menlo Park PSC"},"noUsgsAuthors":false,"publicationDate":"2015-01-05","publicationStatus":"PW","scienceBaseUri":"58f877bae4b0b7ea54521c2a","contributors":{"authors":[{"text":"Shelly, David R. dshelly@usgs.gov","contributorId":2978,"corporation":false,"usgs":true,"family":"Shelly","given":"David","email":"dshelly@usgs.gov","middleInitial":"R.","affiliations":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":692059,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70187041,"text":"70187041 - 2015 - Fluid-faulting interactions: Fracture-mesh and fault-valve behavior in the February 2014 Mammoth Mountain, California, earthquake swarm","interactions":[],"lastModifiedDate":"2017-04-19T15:54:33","indexId":"70187041","displayToPublicDate":"2015-01-01T00:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1807,"text":"Geophysical Research Letters","active":true,"publicationSubtype":{"id":10}},"title":"Fluid-faulting interactions: Fracture-mesh and fault-valve behavior in the February 2014 Mammoth Mountain, California, earthquake swarm","docAbstract":"<p><span>Faulting and fluid transport in the subsurface are highly coupled processes, which may manifest seismically as earthquake swarms. A swarm in February 2014 beneath densely monitored Mammoth Mountain, California, provides an opportunity to witness these interactions in high resolution. Toward this goal, we employ massive waveform-correlation-based event detection and relative relocation, which quadruples the swarm catalog to more than 6000 earthquakes and produces high-precision locations even for very small events. The swarm's main seismic zone forms a distributed fracture mesh, with individual faults activated in short earthquake bursts. The largest event of the sequence, </span><i>M</i><span> 3.1, apparently acted as a fault valve and was followed by a distinct wave of earthquakes propagating ~1 km westward from the updip edge of rupture, 1–2 h later. Late in the swarm, multiple small, shallower subsidiary faults activated with pronounced hypocenter migration, suggesting that a broader fluid pressure pulse propagated through the subsurface.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1002/2015GL064325","usgsCitation":"Shelly, D.R., Taira, T., Prejean, S., Hill, D.P., and Dreger, D.S., 2015, Fluid-faulting interactions: Fracture-mesh and fault-valve behavior in the February 2014 Mammoth Mountain, California, earthquake swarm: Geophysical Research Letters, v. 42, no. 14, p. 5803-5812, https://doi.org/10.1002/2015GL064325.","productDescription":"10 p.","startPage":"5803","endPage":"5812","ipdsId":"IP-065501","costCenters":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"links":[{"id":482081,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1002/2015gl064325","text":"Publisher Index Page"},{"id":339999,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Mammoth Mountain","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -119.09,\n              37.66\n            ],\n            [\n              -119,\n              37.66\n            ],\n            [\n              -119,\n              37.59\n            ],\n            [\n              -119.09,\n              37.59\n            ],\n            [\n              -119.09,\n              37.66\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"42","issue":"14","publishingServiceCenter":{"id":14,"text":"Menlo Park PSC"},"noUsgsAuthors":false,"publicationDate":"2015-07-23","publicationStatus":"PW","scienceBaseUri":"58f877bae4b0b7ea54521c28","contributors":{"authors":[{"text":"Shelly, David R. dshelly@usgs.gov","contributorId":2978,"corporation":false,"usgs":true,"family":"Shelly","given":"David","email":"dshelly@usgs.gov","middleInitial":"R.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true},{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"preferred":true,"id":692104,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Taira, Taka’aki","contributorId":191168,"corporation":false,"usgs":false,"family":"Taira","given":"Taka’aki","affiliations":[],"preferred":false,"id":692105,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Prejean, Stephanie 0000-0003-0510-1989 sprejean@usgs.gov","orcid":"https://orcid.org/0000-0003-0510-1989","contributorId":172404,"corporation":false,"usgs":true,"family":"Prejean","given":"Stephanie","email":"sprejean@usgs.gov","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":692106,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"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":615,"text":"Volcano Hazards Program","active":true,"usgs":true},{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":false,"id":692107,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Dreger, Douglas S.","contributorId":55600,"corporation":false,"usgs":false,"family":"Dreger","given":"Douglas","email":"","middleInitial":"S.","affiliations":[{"id":6643,"text":"University of California - Berkeley","active":true,"usgs":false}],"preferred":false,"id":692108,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70193155,"text":"70193155 - 2015 - Golden Eagle predation of an adult turkey vulture","interactions":[],"lastModifiedDate":"2017-11-20T16:21:10","indexId":"70193155","displayToPublicDate":"2015-01-01T00:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1137,"text":"Bulletin of the Texas Ornithological Society","active":true,"publicationSubtype":{"id":10}},"title":"Golden Eagle predation of an adult turkey vulture","docAbstract":"<p>The Golden Eagle (Aquila chrysaetos) is a large, apex predator that occurs at low densities, has a long life span, experiences delayed maturity, has low reproductive rates, and has no natural predators (Watson 1997, Kochert et al. 2002). Golden Eagles are sensitive to anthropogenic driven landscape changes in land cover and land use (Hunt 2002, Kochert and Steenhof 2002). Landscape level alterations, such as encroachment of woody vegetation in eagle foraging areas, may result in decreased abundance of suitable prey or interfere with the eagle’s ability to see or capture prey. Currently, there is substantial concern for Golden Eagle conservation due to widespread anthropogenic changes to landscapes across much of the species distribution (U.S. Fish and Wildlife Service 2013). In particular, the rapid expansion of wind energy development has led to heightened concerns for Golden Eagle conservation, as the species is susceptible to mortality through collision with turbines (Hunt 2002, U.S. Fish and Wildlife Service 2013). This has resulted in a recent increase&nbsp;in research to develop a better understanding of the species’ ecology.&nbsp;</p>","language":"English","publisher":"Texas Ornithological Society","usgsCitation":"Boal, C.W., 2015, Golden Eagle predation of an adult turkey vulture: Bulletin of the Texas Ornithological Society, v. 48, no. 1-2, p. 53-55.","productDescription":"3 p.","startPage":"53","endPage":"55","ipdsId":"IP-072553","costCenters":[{"id":198,"text":"Coop Res Unit Atlanta","active":true,"usgs":true}],"links":[{"id":349164,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":349163,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.texasbirds.org/publications.php"}],"volume":"48","issue":"1-2","publishingServiceCenter":{"id":9,"text":"Reston PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5a60fec8e4b06e28e9c25359","contributors":{"authors":[{"text":"Boal, Clint W. 0000-0001-6008-8911 cboal@usgs.gov","orcid":"https://orcid.org/0000-0001-6008-8911","contributorId":1909,"corporation":false,"usgs":true,"family":"Boal","given":"Clint","email":"cboal@usgs.gov","middleInitial":"W.","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":718103,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70156593,"text":"ofr20131280D - 2015 - Database creation, data quality assessment, and geochemical maps (phase V, deliverable 59)—Final report on compilation and validation of geochemical data","interactions":[{"subject":{"id":70156593,"text":"ofr20131280D - 2015 - Database creation, data quality assessment, and geochemical maps (phase V, deliverable 59)—Final report on compilation and validation of geochemical data","indexId":"ofr20131280D","publicationYear":"2015","noYear":false,"chapter":"D","title":"Database creation, data quality assessment, and geochemical maps (phase V, deliverable 59)—Final report on compilation and validation of geochemical data"},"predicate":"IS_PART_OF","object":{"id":70160523,"text":"ofr20131280 - 2015 - Second Projet de Renforcement Institutionnel du Secteur Minier de la République  Islamique de Mauritanie (PRISM-II) Phase V","indexId":"ofr20131280","publicationYear":"2015","noYear":false,"title":"Second Projet de Renforcement Institutionnel du Secteur Minier de la République  Islamique de Mauritanie (PRISM-II) Phase V"},"id":1}],"isPartOf":{"id":70160523,"text":"ofr20131280 - 2015 - Second Projet de Renforcement Institutionnel du Secteur Minier de la République  Islamique de Mauritanie (PRISM-II) Phase V","indexId":"ofr20131280","publicationYear":"2015","noYear":false,"title":"Second Projet de Renforcement Institutionnel du Secteur Minier de la République  Islamique de Mauritanie (PRISM-II) Phase V"},"lastModifiedDate":"2022-12-08T17:45:35.163813","indexId":"ofr20131280D","displayToPublicDate":"2015-01-01T00:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2013-1280","chapter":"D","title":"Database creation, data quality assessment, and geochemical maps (phase V, deliverable 59)—Final report on compilation and validation of geochemical data","docAbstract":"<p>Under the World Bank-funded Second Projet de Renforcement Institutionnel du Secteur Minier de la Republique Islamique de Mauritanie (PRISM-II), this Phase V geochemistry report follows earlier Phase I and Phase II summary reports on geochemical data (U.S. Geological Survey, 2007 and Eppinger, 2007; respectively). All the reports are based on evaluations of geochemical data collected in 1999-2004 under an earlier World Bank program (PRISM-I) by the British Geological Survey (BGS) and the Bureau de Recherches G&eacute;ologiques et Mini&egrave;res (BRGM) for the Government of Mauritania. There are no associated Phase III or IV reports.</p>\n<p>The geochemical sample media collected by the BGS and BRGM under the PRISM-I contract included rock, sediment, regolith, and soil samples. Details on sample collection procedures are in unpublished reports available from PRISM. These samples were analyzed under PRISM-I contract by ALS Chemex Laboratories using various combinations of modern methods including fire-assay inductively coupled plasma-atomic emission spectrometry (ICPAES) and ICP-mass spectrometry (ICP-MS) for Au; multi-acid digestion, atomic absorption spectroscopy (AAS) for Ag and As; 47-element, four-acid digestion, ICP-MS; 27-element, fouracid digestion, ICP-AES; special four-acid ICP-MS techniques for Pt and B; fire assay followed by ICP-AES for platinum-group elements; whole-rock analyses by wavelength dispersive X-ray fluorescence (XRF); special techniques for loss-on-ignition, inorganic C, and total S; and special ore-grade AAS techniques for Ag, Au, Cu, Ni, Pb, and Zn. Around 30,000 samples were analyzed by at least one technique. However, it is stressed here that: (1) there was no common sample medium collected at all sites, likely due to the vast geological and geomorphologic differences across the country, (2) the sample site distribution is very irregular, likely due in part to access constraints and sand dune cover, and (3) there was no common across-the-board trace element analytical package used for all samples. These three aspects fundamentally affect the ability to produce country-wide geochemical maps of Mauritania. Gold (Au), silver (Ag), and arsenic (As) were the three elements that were most commonly analyzed.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Second projet de renforcement institutionnel du secteur minier de la République  Islamique de Mauritanie (PRISM-II) (Open File Report 2013-1280)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20131280D","collaboration":"Prepared in cooperation with the Ministry of Petroleum, Energy, and Mines of the Islamic Republic of Mauritania","usgsCitation":"Eppinger, R.G., Giles, S.A., Lee, G.K., and Smith, S.M., 2015, Database creation, data quality assessment, and geochemical maps (phase V, deliverable 59)—Final report on compilation and validation of geochemical data: U.S. Geological Survey Open-File Report 2013-1280, viii, 52 p., https://doi.org/10.3133/ofr20131280D.","productDescription":"viii, 52 p.","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-052690","costCenters":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"links":[{"id":319066,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr20131280D.PNG"},{"id":319065,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2013/1280/Final_Reports_English/deliverable_59-Geochemistry-chapter_D.pdf","text":"Chapter D","linkFileType":{"id":1,"text":"pdf"}}],"country":"Mauritania","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-12.17075,14.61683],[-12.83066,15.30369],[-13.43574,16.03938],[-14.09952,16.3043],[-14.57735,16.59826],[-15.13574,16.58728],[-15.62367,16.36934],[-16.12069,16.45566],[-16.4631,16.13504],[-16.54971,16.67389],[-16.27055,17.16696],[-16.14635,18.10848],[-16.25688,19.09672],[-16.37765,19.59382],[-16.27784,20.09252],[-16.53632,20.56787],[-17.06342,20.99975],[-16.84519,21.33332],[-12.9291,21.32707],[-13.11875,22.77122],[-12.87422,23.28483],[-11.93722,23.37459],[-11.96942,25.93335],[-8.68729,25.88106],[-8.6844,27.39574],[-4.92334,24.97457],[-6.45379,24.95659],[-5.97113,20.64083],[-5.48852,16.3251],[-5.31528,16.20185],[-5.53774,15.50169],[-9.55024,15.4865],[-9.70026,15.26411],[-10.08685,15.33049],[-10.65079,15.13275],[-11.3491,15.41126],[-11.66608,15.38821],[-11.83421,14.7991],[-12.17075,14.61683]]]},\"properties\":{\"name\":\"Mauritania\"}}]}","publishingServiceCenter":{"id":2,"text":"Denver PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56f11b3ce4b0f59b85ddc347","contributors":{"authors":[{"text":"Eppinger, Robert G. eppinger@usgs.gov","contributorId":849,"corporation":false,"usgs":true,"family":"Eppinger","given":"Robert","email":"eppinger@usgs.gov","middleInitial":"G.","affiliations":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":622193,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Giles, Stuart A. 0000-0002-8696-5078 sgiles@usgs.gov","orcid":"https://orcid.org/0000-0002-8696-5078","contributorId":1233,"corporation":false,"usgs":true,"family":"Giles","given":"Stuart","email":"sgiles@usgs.gov","middleInitial":"A.","affiliations":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true},{"id":387,"text":"Mineral Resources Program","active":true,"usgs":true}],"preferred":true,"id":622194,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lee, Gregory K. glee@usgs.gov","contributorId":1220,"corporation":false,"usgs":true,"family":"Lee","given":"Gregory","email":"glee@usgs.gov","middleInitial":"K.","affiliations":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":622195,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Smith, Steven M. 0000-0003-3591-5377 smsmith@usgs.gov","orcid":"https://orcid.org/0000-0003-3591-5377","contributorId":1460,"corporation":false,"usgs":true,"family":"Smith","given":"Steven","email":"smsmith@usgs.gov","middleInitial":"M.","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":622196,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70143409,"text":"70143409 - 2015 - Causes and consequences of ecosystem service regionalization in a coastal suburban watershed","interactions":[],"lastModifiedDate":"2015-03-19T09:06:03","indexId":"70143409","displayToPublicDate":"2015-01-01T00:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1584,"text":"Estuaries and Coasts","active":true,"publicationSubtype":{"id":10}},"title":"Causes and consequences of ecosystem service regionalization in a coastal suburban watershed","docAbstract":"<p><span>The demand for ecosystem services and the ability of natural ecosystems to provide those services evolve over time as population, land use, and management practices change. Regionalization of ecosystem service activity, or the expansion of the area providing ecosystem services to a population, is a common response in densely populated coastal regions, with important consequences for watershed water and nitrogen (N) fluxes to the coastal zone. We link biophysical and historical information to explore the causes and consequences of change in ecosystem service activity&mdash;focusing on water provisioning and N regulation&mdash;from 1850 to 2010 in a coastal suburban watershed, the Ipswich River watershed in northeastern Massachusetts, USA. Net interbasin water transfers started in the late 1800s due to regionalization of water supply for use by larger populations living outside the Ipswich watershed boundaries, reaching a peak in the mid-1980s. Over much of the twentieth century, about 20&nbsp;% of river runoff was diverted from reaching the estuary, with greater proportions during drought years. Ongoing regionalization of water supply has contributed to recent declines in diversions, influenced by socioecological feedbacks resulting from the river drying and fish kills. Similarly, the N budget has been greatly perturbed since the suburban era began in the 1950s due to food and lawn fertilizer imports and human waste release. However, natural ecosystems are able to remove most of this anthropogenic N, mitigating impacts on the coastal zone. We propose a conceptual model whereby the amount and type of ecosystem services provided by coastal watersheds in urban regions expand and contract over time as regional population expands and ecosystem services are regionalized. We hypothesize that suburban watersheds can be hotspots of ecosystem service sources because they retain sufficient ecosystem function to still produce services that meet increasing demand from the local population and nearby urban centers. Historical reconstruction of ecosystem service activity provides a perspective that may help to better understand coupled human&ndash;natural system processes and lead to more sustainable management of coastal ecosystems.</span></p>","language":"English","publisher":"Springer","doi":"10.1007/s12237-013-9646-8","usgsCitation":"Wollheim, W.M., Green, M.B., Pellerin, B.A., Morse, N.B., and Hopkinson, C.S., 2015, Causes and consequences of ecosystem service regionalization in a coastal suburban watershed: Estuaries and Coasts, v. 1, no. 38, p. 19-34, https://doi.org/10.1007/s12237-013-9646-8.","productDescription":"16 p.","startPage":"19","endPage":"34","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-043983","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"links":[{"id":472577,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1007/s12237-013-9646-8","text":"Publisher Index Page"},{"id":298737,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Massachusetts","otherGeospatial":"Ipswich River watershed","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -71.02159023284912,\n              42.562879746999684\n            ],\n            [\n              -71.02159023284912,\n              42.56935918843573\n            ],\n            [\n              -71.00137710571288,\n              42.56935918843573\n            ],\n            [\n              -71.00137710571288,\n              42.562879746999684\n            ],\n            [\n              -71.02159023284912,\n              42.562879746999684\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"1","issue":"38","publishingServiceCenter":{"id":1,"text":"Sacramento PSC"},"noUsgsAuthors":false,"publicationDate":"2013-06-07","publicationStatus":"PW","scienceBaseUri":"550bf32be4b02e76d759cddd","contributors":{"authors":[{"text":"Wollheim, Wilfred M.","contributorId":139742,"corporation":false,"usgs":false,"family":"Wollheim","given":"Wilfred","email":"","middleInitial":"M.","affiliations":[{"id":18105,"text":"University of New Hampshire, Durham","active":true,"usgs":false}],"preferred":false,"id":542725,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Green, Mark B.","contributorId":139746,"corporation":false,"usgs":false,"family":"Green","given":"Mark","email":"","middleInitial":"B.","affiliations":[{"id":590,"text":"U.S. Army Corps of Engineers","active":false,"usgs":false}],"preferred":false,"id":542723,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Pellerin, Brian A. bpeller@usgs.gov","contributorId":1451,"corporation":false,"usgs":true,"family":"Pellerin","given":"Brian","email":"bpeller@usgs.gov","middleInitial":"A.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":false,"id":542721,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Morse, Nathaniel B.","contributorId":139747,"corporation":false,"usgs":false,"family":"Morse","given":"Nathaniel","email":"","middleInitial":"B.","affiliations":[{"id":590,"text":"U.S. Army Corps of Engineers","active":false,"usgs":false}],"preferred":false,"id":542724,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Hopkinson, Charles S.","contributorId":139745,"corporation":false,"usgs":false,"family":"Hopkinson","given":"Charles","email":"","middleInitial":"S.","affiliations":[{"id":590,"text":"U.S. Army Corps of Engineers","active":false,"usgs":false}],"preferred":false,"id":542722,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70192722,"text":"70192722 - 2015 - Biodiversity influences plant productivity through niche–efficiency","interactions":[],"lastModifiedDate":"2017-11-08T13:45:31","indexId":"70192722","displayToPublicDate":"2015-01-01T00:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3165,"text":"Proceedings of the National Academy of Sciences of the United States of America","active":true,"publicationSubtype":{"id":10}},"title":"Biodiversity influences plant productivity through niche–efficiency","docAbstract":"<p><span>The loss of biodiversity is threatening ecosystem productivity and services worldwide, spurring efforts to quantify its effects on the functioning of natural ecosystems. Previous research has focused on the positive role of biodiversity on resource acquisition (i.e., niche complementarity), but a lack of study on resource utilization efficiency, a link between resource and productivity, has rendered it difficult to quantify the biodiversity–ecosystem functioning relationship. Here we demonstrate that biodiversity loss reduces plant productivity, other things held constant, through theory, empirical evidence, and simulations under gradually relaxed assumptions. We developed a theoretical model named niche–efficiency to integrate niche complementarity and a heretofore-ignored mechanism of diminishing marginal productivity in quantifying the effects of biodiversity loss on plant productivity. Based on niche–efficiency, we created a relative productivity metric and a productivity impact index (PII) to assist in biological conservation and resource management. Relative productivity provides a standardized measure of the influence of biodiversity on individual productivity, and PII is a functionally based taxonomic index to assess individual species’ inherent value in maintaining current ecosystem productivity. Empirical evidence from the Alaska boreal forest suggests that every 1% reduction in overall plant diversity could render an average of 0.23% decline in individual tree productivity. Out of the 283 plant species of the region, we found that large woody plants generally have greater PII values than other species. This theoretical model would facilitate the integration of biological conservation in the international campaign against several pressing global issues involving energy use, climate change, and poverty.</span></p>","language":"English","publisher":"National Academy of Sciences of the United States of America","doi":"10.1073/pnas.1409853112","usgsCitation":"Liang, J., Zhou, M., Tobin, P.C., McGuire, A.D., and Reich, P., 2015, Biodiversity influences plant productivity through niche–efficiency: Proceedings of the National Academy of Sciences of the United States of America, v. 112, no. 18, p. 5738-5743, https://doi.org/10.1073/pnas.1409853112.","productDescription":"6 p.","startPage":"5738","endPage":"5743","ipdsId":"IP-049472","costCenters":[{"id":200,"text":"Coop Res Unit Seattle","active":true,"usgs":true}],"links":[{"id":472444,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1073/pnas.1409853112","text":"Publisher Index Page"},{"id":348464,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"112","issue":"18","publishingServiceCenter":{"id":12,"text":"Tacoma PSC"},"noUsgsAuthors":false,"publicationDate":"2015-04-21","publicationStatus":"PW","scienceBaseUri":"5a0425c4e4b0dc0b45b4540f","contributors":{"authors":[{"text":"Liang, Jingjing","contributorId":189197,"corporation":false,"usgs":false,"family":"Liang","given":"Jingjing","email":"","affiliations":[],"preferred":false,"id":721281,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Zhou, Mo","contributorId":189200,"corporation":false,"usgs":false,"family":"Zhou","given":"Mo","email":"","affiliations":[],"preferred":false,"id":721282,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Tobin, Patrick C.","contributorId":200172,"corporation":false,"usgs":false,"family":"Tobin","given":"Patrick","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":721283,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"McGuire, A. David 0000-0003-4646-0750 ffadm@usgs.gov","orcid":"https://orcid.org/0000-0003-4646-0750","contributorId":166708,"corporation":false,"usgs":true,"family":"McGuire","given":"A.","email":"ffadm@usgs.gov","middleInitial":"David","affiliations":[{"id":200,"text":"Coop Res Unit Seattle","active":true,"usgs":true}],"preferred":false,"id":716773,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Reich, Peter B.","contributorId":75835,"corporation":false,"usgs":true,"family":"Reich","given":"Peter B.","affiliations":[],"preferred":false,"id":721284,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70191995,"text":"70191995 - 2015 - Spatial and temporal variation in recruitment and growth of Channel Catfish Alabama bass and Tallapoosa Bass in the Tallapoosa River and associated tributaries","interactions":[],"lastModifiedDate":"2018-01-25T12:42:20","indexId":"70191995","displayToPublicDate":"2015-01-01T00:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":5373,"text":"Cooperator Science Series","active":true,"publicationSubtype":{"id":1}},"seriesNumber":"FWS/CSS -116","title":"Spatial and temporal variation in recruitment and growth of Channel Catfish Alabama bass and Tallapoosa Bass in the Tallapoosa River and associated tributaries","docAbstract":"<p>Effects of hydrology on growth and hatching success of age-0 black basses and Channel Catfish were examined in regulated and unregulated reaches of the Tallapoosa River, Alabama. Species of the family Centrarchidae, Ictalurus punctatus Channel Catfish and Pylodictis olivaris Flathead Catfish were also collected from multiple tributaries in the basin. Fish were collected from 2010-2014 and were assigned daily ages using otoliths. Hatch dates of individuals of three species (Micropterus henshalli Alabama Bass, M. tallapoosae Tallapoosa Bass and Channel Catfish) were back calculated, and growth histories were estimated every 5 d post hatch from otolith sections using incremental growth analysis. Hatch dates and incremental growth were related to hydrologic and temperature metrics from environmental data collected during the same time periods. Hatch dates at the regulated sites were related to and typically occurred during periods with low and stable flow conditions; however no clear relations between hatch and thermal or flow metrics were evident for the unregulated sites. Some fish hatched during unsuitable thermal conditions at the regulated site suggesting that some fish may recruit from unregulated tributaries. Ages and growth rates of age-0 black basses ranged from 105 to 131 d and 0.53 to 1.33 mm/day at the regulated sites and 44 to 128 d and 0.44 to 0.96 mm/d at the unregulated sites. In general, growth was highest among age-0 fish from the regulated sites, consistent with findings of other studies. Mortality of age-0 to age-1 fish was also variable among years and between sites and with the exception of one year, was lower at regulated sites. Multiple and single regression models of incremental growth versus age, discharge, and temperature metrics were evaluated with Akaike’s Information Criterion (AICc) to assess models that best described growth parameters. Of the models evaluated, the best overall models predicted that daily incremental growth was positively related to low flow parameters and negatively related to the number of times the hydrograph changed direction (e.g., reversals). These results suggest that specific flow and temperature criteria provided from the dam could potentially enhance growth and hatch success of these important sport fish species.</p>","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Irwin, E.R., and Goar, T., 2015, Spatial and temporal variation in recruitment and growth of Channel Catfish Alabama bass and Tallapoosa Bass in the Tallapoosa River and associated tributaries: Cooperator Science Series FWS/CSS -116, 30 p.","productDescription":"30 p.","ipdsId":"IP-064738","costCenters":[{"id":198,"text":"Coop Res Unit Atlanta","active":true,"usgs":true}],"links":[{"id":350604,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":350603,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://digitalmedia.fws.gov/cdm/ref/collection/document/id/2111"}],"publishingServiceCenter":{"id":8,"text":"Raleigh PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5a6afac7e4b06e28e9c9a913","contributors":{"authors":[{"text":"Irwin, Elise R. 0000-0002-6866-4976 eirwin@usgs.gov","orcid":"https://orcid.org/0000-0002-6866-4976","contributorId":2588,"corporation":false,"usgs":true,"family":"Irwin","given":"Elise","email":"eirwin@usgs.gov","middleInitial":"R.","affiliations":[{"id":506,"text":"Office of the AD Ecosystems","active":true,"usgs":true},{"id":198,"text":"Coop Res Unit Atlanta","active":true,"usgs":true}],"preferred":true,"id":713822,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Goar, Taconya","contributorId":201475,"corporation":false,"usgs":false,"family":"Goar","given":"Taconya","email":"","affiliations":[],"preferred":false,"id":725807,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70191102,"text":"70191102 - 2015 - Composite Sunrise Butte pluton: Insights into Jurassic–Cretaceous collisional tectonics and magmatism in the Blue Mountains Province, northeastern Oregon","interactions":[],"lastModifiedDate":"2020-12-18T15:17:50.459407","indexId":"70191102","displayToPublicDate":"2015-01-01T00:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1727,"text":"GSA Special Papers","active":true,"publicationSubtype":{"id":10}},"title":"Composite Sunrise Butte pluton: Insights into Jurassic–Cretaceous collisional tectonics and magmatism in the Blue Mountains Province, northeastern Oregon","docAbstract":"<p><span>The&nbsp;</span><span class=\"ScopusTermHighlight\">composite</span><span>&nbsp;</span><span class=\"ScopusTermHighlight\">Sunrise</span><span>&nbsp;</span><span class=\"ScopusTermHighlight\">Butte</span><span>&nbsp;</span><span class=\"ScopusTermHighlight\">pluton</span><span>, in the central part of the Blue Mountains Province, northeastern Oregon, preserves a record of subduction-related magmatism, arc-arc collision, crustal thickening, and deep-crustal anatexis. The earliest phase of the&nbsp;</span><span class=\"ScopusTermHighlight\">pluton</span><span>&nbsp;(Desolation Creek unit) was generated in a subduction zone environment, as the oceanic lithosphere between the Wallowa and Olds Ferry island arcs was consumed. Zircons from this unit yielded a&nbsp;</span><sup>206</sup><span>Pb/</span><sup>238</sup><span>U age of 160.2 ± 2.1 Ma. A magmatic lull ensued during arc-arc collision, after which partial melting at the base of the thickened Wallowa arc crust produced siliceous magma that was emplaced into metasedimentary rocks and serpentinite of the overthrust forearc complex. This magma crystallized to form the bulk of the&nbsp;</span><span class=\"ScopusTermHighlight\">Sunrise</span><span>&nbsp;</span><span class=\"ScopusTermHighlight\">Butte</span><span>&nbsp;</span><span class=\"ScopusTermHighlight\">composite</span><span>&nbsp;</span><span class=\"ScopusTermHighlight\">pluton</span><span>&nbsp;(the&nbsp;</span><span class=\"ScopusTermHighlight\">Sunrise</span><span>&nbsp;</span><span class=\"ScopusTermHighlight\">Butte</span><span>&nbsp;unit; 145.8 ± 2.2 Ma). The heat necessary for crustal anatexis was supplied by coeval mantle-derived magma (the Onion Gulch unit; 147.9 ± 1.8 Ma). The lull in magmatic activity between 160 and 148 Ma encompasses the timing of arc-arc collision (159-154 Ma), and it is similar to those lulls observed in adjacent areas of the Blue Mountains Province related to the same shortening event. Previous researchers have proposed a tectonic link between the Blue Mountains Province and the Klamath Mountains and northern Sierra Nevada Provinces farther to the south; however, timing of Late Jurassic deformation in the Blue Mountains Province predates the timing of the so-called Nevadan orogeny in the Klamath Mountains. In both the Blue Mountains Province and Klamath Mountains, the onset of deep-crustal partial melting initiated at ca. 148 Ma, suggesting a possible geodynamic link. One possibility is that the Late Jurassic shortening event recorded in the Blue Mountains Province may be a northerly extension of the Nevadan orogeny. Differences in the timing of these events in the Blue Mountains Province and the Klamath-Sierra Nevada Provinces suggest that shortening and deformation were diachronous, progressing from north to south. We envision that Late Jurassic deformation may have collapsed a Gulf of California-style oceanic extensional basin that extended from the Klamath Mountains (e.g., Josephine ophiolite) to the central Blue Mountains Province, and possibly as far north as the North Cascades (i.e., the coeval Ingalls ophiolite).</span></p><p>The lull in magmatic activity between 160 and 148 Ma encompasses the timing of arc-arc collision (159–154 Ma), and it is similar to those lulls observed in adjacent areas of the Blue Mountains Province related to the same shortening event. Previous researchers have proposed a tectonic link between the Blue Mountains Province and the Klamath Mountains and northern Sierra Nevada Provinces farther to the south; however, timing of Late Jurassic deformation in the Blue Mountains Province predates the timing of the so-called Nevadan orogeny in the Klamath Mountains. In both the Blue Mountains Province and Klamath Mountains, the onset of deep-crustal partial melting initiated at ca. 148 Ma, suggesting a possible geodynamic link. One possibility is that the Late Jurassic shortening event recorded in the Blue Mountains Province may be a northerly extension of the Nevadan orogeny. Differences in the timing of these events in the Blue Mountains Province and the Klamath–Sierra Nevada Provinces suggest that shortening and deformation were diachronous, progressing from north to south. We envision that Late Jurassic deformation may have collapsed a Gulf of California–style oceanic extensional basin that extended from the Klamath Mountains (e.g., Josephine ophiolite) to the central Blue Mountains Province, and possibly as far north as the North Cascades (i.e., the coeval Ingalls ophiolite).</p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/2015.2513(10)","usgsCitation":"Johnson, K.H., Schwartz, J., Zak, J., Verner, K., Barnes, C.G., Walton, C., Wooden, J.L., Wright, J.E., and Kistler, R., 2015, Composite Sunrise Butte pluton: Insights into Jurassic–Cretaceous collisional tectonics and magmatism in the Blue Mountains Province, northeastern Oregon: GSA Special Papers, v. 513, p. 377-398, https://doi.org/10.1130/2015.2513(10).","productDescription":"22 p.","startPage":"377","endPage":"398","ipdsId":"IP-079965","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":346103,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Idaho, Oregon","otherGeospatial":"Blue Mountains Province","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -120.311279296875,\n              43.84245116699039\n            ],\n            [\n              -116.04858398437499,\n              43.84245116699039\n            ],\n            [\n              -116.04858398437499,\n              45.97406038956237\n            ],\n            [\n              -120.311279296875,\n              45.97406038956237\n            ],\n            [\n              -120.311279296875,\n              43.84245116699039\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"513","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"59cb6735e4b017cf3141c6b1","contributors":{"authors":[{"text":"Johnson, Kenneth H. johnson@usgs.gov","contributorId":3103,"corporation":false,"usgs":true,"family":"Johnson","given":"Kenneth","email":"johnson@usgs.gov","middleInitial":"H.","affiliations":[{"id":622,"text":"Washington Water Science Center","active":true,"usgs":true}],"preferred":true,"id":711219,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schwartz, J.J.","contributorId":24572,"corporation":false,"usgs":true,"family":"Schwartz","given":"J.J.","email":"","affiliations":[],"preferred":false,"id":711220,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Zak, Jiri","contributorId":196710,"corporation":false,"usgs":false,"family":"Zak","given":"Jiri","email":"","affiliations":[],"preferred":false,"id":711221,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Verner, Krystof","contributorId":196711,"corporation":false,"usgs":false,"family":"Verner","given":"Krystof","email":"","affiliations":[],"preferred":false,"id":711222,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Barnes, Calvin G.","contributorId":36608,"corporation":false,"usgs":true,"family":"Barnes","given":"Calvin","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":711223,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Walton, Clay","contributorId":196712,"corporation":false,"usgs":false,"family":"Walton","given":"Clay","email":"","affiliations":[],"preferred":false,"id":711224,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Wooden, Joseph L.","contributorId":193587,"corporation":false,"usgs":false,"family":"Wooden","given":"Joseph","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":711225,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Wright, James E.","contributorId":105648,"corporation":false,"usgs":true,"family":"Wright","given":"James","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":711226,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Kistler, Ronald W.","contributorId":56969,"corporation":false,"usgs":true,"family":"Kistler","given":"Ronald W.","affiliations":[],"preferred":false,"id":711227,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}}
,{"id":70156793,"text":"70156793 - 2015 - Geologic framework and evidence for neotectonism in the epicentral area of the 2011 Mineral, Virginia, earthquake","interactions":[],"lastModifiedDate":"2017-04-19T12:45:41","indexId":"70156793","displayToPublicDate":"2015-01-01T00:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1727,"text":"GSA Special Papers","active":true,"publicationSubtype":{"id":10}},"title":"Geologic framework and evidence for neotectonism in the epicentral area of the 2011 Mineral, Virginia, earthquake","docAbstract":"<p><span>The epicenters of the main shock and associated aftershocks of the 2011 moment magnitude, M</span><sub>w</sub><span> 5.8 Mineral, Virginia (USA), earthquake, and the updip projection of the possible fault plane that triggered the quakes, are contained in the areas of 2 adjoining 7.5′ quadrangles in the central Virginia Piedmont. These quadrangles have therefore been the focus of concentrated geologic study in the form of bedrock and surficial mapping and near-surface trenching in order to identify potential seismogenic structures. Bedrock mapping has outlined a series of northeast-southwest–trending lithologic belts that include the Ordovician Chopawamsic and Quantico Formations, the narrow neck of the Late Ordovician Ellisville pluton, and mélange zone III of the Mine Run Complex. The region was affected by at least two ductile deformational events, one in the early Paleozoic that was broadly synchronous with the intrusion of the pluton, and one later in the Paleozoic. The earlier deformation produced the Quantico synclinorium and other regional folds, and the later deformation produced faults with associated high-strain zones. Two of these faults have been trenched at their intersection along the east-dipping eastern contact of the Ellisville neck, near where the causative fault for the earthquake projects to the surface. The trenches have exposed abundant evidence of post-Paleozoic fracturing and faulting, including brecciated quartz-tourmaline veins, slickensided thrust and strike-slip faults, and clay-filled fractures. Fluvial and colluvial gravels that overlie these brittle structures have yielded optically stimulated luminescence ages ranging from ca. 27 to 10 ka. These structures are likely representative of surface features associated with Quaternary earthquakes in the Central Virginia seismic zone.</span></p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/2015.2509(20)","usgsCitation":"Burton, W.C., Harrison, R., Spears, D., Evans, N.H., and Mahan, S.A., 2015, Geologic framework and evidence for neotectonism in the epicentral area of the 2011 Mineral, Virginia, earthquake: GSA Special Papers, v. 509, p. 345-376, https://doi.org/10.1130/2015.2509(20).","productDescription":"32 p.","startPage":"345","endPage":"376","ipdsId":"IP-053258","costCenters":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"links":[{"id":339965,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"509","publishingServiceCenter":{"id":9,"text":"Reston PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58f877bfe4b0b7ea54521c36","contributors":{"authors":[{"text":"Burton, William C. 0000-0001-7519-5787 bburton@usgs.gov","orcid":"https://orcid.org/0000-0001-7519-5787","contributorId":1293,"corporation":false,"usgs":true,"family":"Burton","given":"William","email":"bburton@usgs.gov","middleInitial":"C.","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true},{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true}],"preferred":true,"id":570563,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Harrison, Richard W. rharriso@usgs.gov","contributorId":544,"corporation":false,"usgs":true,"family":"Harrison","given":"Richard W.","email":"rharriso@usgs.gov","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"preferred":true,"id":570564,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Spears, David B.","contributorId":147157,"corporation":false,"usgs":false,"family":"Spears","given":"David B.","affiliations":[{"id":590,"text":"U.S. Army Corps of Engineers","active":false,"usgs":false}],"preferred":false,"id":570565,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Evans, Nicholas H.","contributorId":147158,"corporation":false,"usgs":false,"family":"Evans","given":"Nicholas","email":"","middleInitial":"H.","affiliations":[{"id":590,"text":"U.S. Army Corps of Engineers","active":false,"usgs":false}],"preferred":false,"id":570566,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Mahan, Shannon A. 0000-0001-5214-7774 smahan@usgs.gov","orcid":"https://orcid.org/0000-0001-5214-7774","contributorId":147159,"corporation":false,"usgs":true,"family":"Mahan","given":"Shannon","email":"smahan@usgs.gov","middleInitial":"A.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":570567,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70193151,"text":"70193151 - 2015 - Observational changes to the natural flow regime in Lee Creek in relation to altered precipitation patterns and its implication for fishes","interactions":[],"lastModifiedDate":"2017-11-21T12:46:10","indexId":"70193151","displayToPublicDate":"2015-01-01T00:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3894,"text":"Proceedings of the Oklahoma Academy of Science","active":true,"publicationSubtype":{"id":10}},"title":"Observational changes to the natural flow regime in Lee Creek in relation to altered precipitation patterns and its implication for fishes","docAbstract":"<p>The natural flow regime is important for structuring streams and their resident ichthyofauna and alterations to this regime can have cascading consequences. We sought to determine if changes in hydrology could be attributed to changes in precipitation in a minimally altered watershed (Lee Creek). The stream flow regime was analyzed using Indicators of Hydrologic Alteration (IHA) software, and data from a nearby climate station were used to summarize concurrent precipitation patterns. We discovered that Lee Creek hydrology had become flashier (i.e., increased frequency of extreme events of shorter duration) since 1992 coincident with changes in precipitation patterns. Specifically, our results show fewer but more intense rain events within the Lee Creek watershed. Our research provides evidence that climate-induced changes to the natural flow regime are currently underway and additional research on its effects on the fish community is warranted.</p>","language":"English","publisher":"Oklahoma Academy of Science","usgsCitation":"Gatlin, M.R., Long, J.M., and Turton, D.J., 2015, Observational changes to the natural flow regime in Lee Creek in relation to altered precipitation patterns and its implication for fishes: Proceedings of the Oklahoma Academy of Science, v. 95, p. 135-146.","productDescription":"12 p.","startPage":"135","endPage":"146","ipdsId":"IP-063504","costCenters":[{"id":198,"text":"Coop Res Unit Atlanta","active":true,"usgs":true}],"links":[{"id":349202,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Arkansas, Oklahoma","otherGeospatial":"Lee Creek watershed","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -94.62661743164062,\n              35.464025575544674\n            ],\n            [\n              -94.28123474121094,\n              35.464025575544674\n            ],\n            [\n              -94.28123474121094,\n              35.74874138089811\n            ],\n            [\n              -94.62661743164062,\n              35.74874138089811\n            ],\n            [\n              -94.62661743164062,\n              35.464025575544674\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"95","publishingServiceCenter":{"id":8,"text":"Raleigh PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5a60fec8e4b06e28e9c2535b","contributors":{"authors":[{"text":"Gatlin, Michael R.","contributorId":141324,"corporation":false,"usgs":false,"family":"Gatlin","given":"Michael","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":723033,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Long, James M. 0000-0002-8658-9949 jmlong@usgs.gov","orcid":"https://orcid.org/0000-0002-8658-9949","contributorId":3453,"corporation":false,"usgs":true,"family":"Long","given":"James","email":"jmlong@usgs.gov","middleInitial":"M.","affiliations":[{"id":198,"text":"Coop Res Unit Atlanta","active":true,"usgs":true}],"preferred":true,"id":718099,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Turton, Donald J.","contributorId":200683,"corporation":false,"usgs":false,"family":"Turton","given":"Donald","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":723034,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70148463,"text":"70148463 - 2015 - Lake Ontario benthic prey fish assessment, 2014","interactions":[],"lastModifiedDate":"2020-03-05T12:10:03","indexId":"70148463","displayToPublicDate":"2015-01-01T00:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5114,"text":"NYSDEC Lake Ontario Annual Report ","active":true,"publicationSubtype":{"id":2}},"title":"Lake Ontario benthic prey fish assessment, 2014","docAbstract":"<p>Benthic prey fishes are an important component of the Lake Ontario fish community and serve as vectors that move energy from benthic invertebrates into native and introduced sport fishes. Since the 1970’s, the USGS Lake Ontario Biological Station has assessed benthic fish populations and community dynamics with bottom trawls at depths ranging from 8 m out to depths of 150-225 m along the south and eastern shores of Lake Ontario. From the late 1970’s through the early 2000’s the benthic fish community was dominated by Slimy Sculpin <i>Cottus cognatus</i>, but in 2004 non-native Round Goby <i>Neogobius melanostomus</i> abundance increased and, since then Round Goby have generally been the dominant benthic species. Over the past 10 years the native Deepwater Sculpin <i>Myoxocephalus</i> <i>thompsonii</i>, once considered absent from the lake, have increased. Presently their lake-wide biomass density is equal to, or larger than, Slimy Sculpin. Species-specific assessments found Slimy and Deepwater Sculpin abundance increased slightly in 2014 relative to 2013, while changes in Round Goby abundance differed between spring and fall survey. Recent survey modifications have increased our understanding of benthic prey fish abundance and behavior in Lake Ontario. For instance, increasing the maximum tow depth to 225 m in 2014 improved our understanding of Deepwater Sculpin distribution in this rarely sampled lake habitat.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"2014 Annual Report Bureau of Fisheries Lake Ontario Unit and St. Lawrence River Unit to the Great Lakes Fishery Commission’s Lake Ontario Committee","largerWorkSubtype":{"id":2,"text":"State or Local Government Series"},"conferenceTitle":"Lake Ontario Committee Meeting","conferenceDate":"March 24-25, 2015","conferenceLocation":"Ypsilanti, MI","language":"English","publisher":"New York State Department of Environmental Conservation Division of Fish, Wildlife and Marine Resources","publisherLocation":"Albany, NY","usgsCitation":"Weidel, B., and Walsh, M., 2015, Lake Ontario benthic prey fish assessment, 2014: NYSDEC Lake Ontario Annual Report , 6 p.","productDescription":"6 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]\n}","publishingServiceCenter":{"id":6,"text":"Columbus PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5a8012cfe4b00f54eb298eec","contributors":{"authors":[{"text":"Weidel, Brian 0000-0001-6095-2773 bweidel@usgs.gov","orcid":"https://orcid.org/0000-0001-6095-2773","contributorId":2485,"corporation":false,"usgs":true,"family":"Weidel","given":"Brian","email":"bweidel@usgs.gov","affiliations":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"preferred":true,"id":548329,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Walsh, Maureen 0000-0001-7846-5025 mwalsh@usgs.gov","orcid":"https://orcid.org/0000-0001-7846-5025","contributorId":3659,"corporation":false,"usgs":true,"family":"Walsh","given":"Maureen","email":"mwalsh@usgs.gov","affiliations":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"preferred":true,"id":728180,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70192335,"text":"70192335 - 2015 - Synoptic evaluation of scale-dependent metrics for hydrographic line feature geometry","interactions":[],"lastModifiedDate":"2018-02-02T13:03:49","indexId":"70192335","displayToPublicDate":"2015-01-01T00:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":18,"text":"Abstract or summary"},"title":"Synoptic evaluation of scale-dependent metrics for hydrographic line feature geometry","docAbstract":"<p>Methods of acquisition and feature simplification for vector feature data impact cartographic representations and scientific investigations of these data, and are therefore important considerations for geographic information science (Haunert and Sester 2008). After initial collection, linear features may be simplified to reduce excessive detail or to furnish a reduced-scale version of the features through cartographic generalization (Regnauld and McMaster 2008, Stanislawski et al. 2014). A variety of algorithms exist to simplify linear cartographic features, and all of the methods affect the positional accuracy of the features (Shahriari and Tao 2002, Regnauld and McMaster 2008, Stanislawski et al. 2012). In general, simplification operations are controlled by one or more tolerance parameters that limit the amount of positional change the operation can make to features. Using a single tolerance value can have varying levels of positional change on features; depending on local shape, texture, or geometric characteristics of the original features (McMaster and Shea 1992, Shahriari and Tao 2002, Buttenfield et al. 2010). Consequently, numerous researchers have advocated calibration of simplification parameters to control quantifiable properties of resulting changes to the features (Li and Openshaw 1990, Raposo 2013, Tobler 1988, Veregin 2000, and Buttenfield, 1986, 1989).</p><p>This research identifies relations between local topographic conditions and geometric characteristics of linear features that are available in the National Hydrography Dataset (NHD). The NHD is a comprehensive vector dataset of surface 18 th ICA Workshop on Generalisation and Multiple Representation, Rio de Janiero, Brazil 2015 2 water features within the United States that is maintained by the U.S. Geological Survey (USGS). In this paper, geometric characteristics of cartographic representations for natural stream and river features are summarized for subbasin watersheds within entire regions of the conterminous United States and compared to topographic metrics. A concurrent processing workflow is implemented using a Linux high-performance computing cluster to simultaneously process multiple subbasins, and thereby complete the work in a fraction of the time required for a single-process environment. In addition, similar metrics are generated for several levels of simplification of the hydrographic features to quantify the effects of simplification over the various landscape conditions. </p><p>Objectives of this exploratory investigation are to quantify geometric characteristics of linear hydrographic features over the various terrain conditions within the conterminous United States and thereby illuminate relations between stream geomorphological conditions and cartographic representation. The synoptic view of these characteristics over regional watersheds that is afforded through concurrent processing, in conjunction with terrain conditions, may reveal patterns for classifying cartographic stream features into stream geomorphological classes. Furthermore, the synoptic measurement of the amount of change in geometric characteristics caused by the several levels of simplification can enable estimation of tolerance values that appropriately control simplification-induced geometric change of the cartographic features within the various geomorphological classes in the country. Hence, these empirically derived rules or relations could help generate multiscale-representations of features through automated generalization that adequately maintain surface drainage variations and patterns reflective of the natural stream geomorphological conditions across the country. </p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"18th ICA Workshop on Generalisation and Multiple Representation","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"18th ICA Workshop on Generalisation and Multiple Representation","conferenceDate":"August 21, 2015","conferenceLocation":"Rio de Janeiro, Brazil","language":"English","usgsCitation":"Stanislawski, L.V., Buttenfield, B.P., Raposo, P., Cameron, M., and Falgout, J.T., 2015, Synoptic evaluation of scale-dependent metrics for hydrographic line feature geometry, <i>in</i> 18th ICA Workshop on Generalisation and Multiple Representation, Rio de Janeiro, Brazil, August 21, 2015, 14 p.","productDescription":"14 p.","ipdsId":"IP-066969","costCenters":[{"id":5074,"text":"Center for Geospatial Information Science (CEGIS)","active":true,"usgs":true}],"links":[{"id":350965,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"publishingServiceCenter":{"id":6,"text":"Columbus PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5a7586dce4b00f54eb1d820a","contributors":{"authors":[{"text":"Stanislawski, Larry V. 0000-0002-9437-0576 lstan@usgs.gov","orcid":"https://orcid.org/0000-0002-9437-0576","contributorId":3386,"corporation":false,"usgs":true,"family":"Stanislawski","given":"Larry","email":"lstan@usgs.gov","middleInitial":"V.","affiliations":[{"id":5074,"text":"Center for Geospatial Information Science (CEGIS)","active":true,"usgs":true},{"id":404,"text":"NGTOC Rolla","active":true,"usgs":true}],"preferred":true,"id":715394,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Buttenfield, Barbara P.","contributorId":184069,"corporation":false,"usgs":false,"family":"Buttenfield","given":"Barbara","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":715395,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Raposo, Paulo","contributorId":198220,"corporation":false,"usgs":false,"family":"Raposo","given":"Paulo","email":"","affiliations":[],"preferred":false,"id":715396,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Cameron, Madeline macameron@usgs.gov","contributorId":198221,"corporation":false,"usgs":true,"family":"Cameron","given":"Madeline","email":"macameron@usgs.gov","affiliations":[],"preferred":true,"id":715397,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Falgout, Jeff T. 0000-0002-7108-477X jfalgout@usgs.gov","orcid":"https://orcid.org/0000-0002-7108-477X","contributorId":4957,"corporation":false,"usgs":true,"family":"Falgout","given":"Jeff","email":"jfalgout@usgs.gov","middleInitial":"T.","affiliations":[{"id":208,"text":"Core Science Analytics and Synthesis","active":true,"usgs":true}],"preferred":true,"id":715398,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70191726,"text":"70191726 - 2015 - Field trip guidebook for the post-meeting field trip: The Central Appalachians","interactions":[],"lastModifiedDate":"2018-02-12T13:21:31","indexId":"70191726","displayToPublicDate":"2015-01-01T00:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3481,"text":"Stratigraphy","active":true,"publicationSubtype":{"id":10}},"title":"Field trip guidebook for the post-meeting field trip: The Central Appalachians","docAbstract":"<p>The lower Paleozoic rocks to be examined on this trip through the central Appalachians represent an extreme range of depositional environments. The lithofacies we will examine range from pelagic radiolarian chert and interbedded mudstone that originated on the deep floor of the Iapetus Ocean, through mud cracked supratidal dolomitic laminites that formed during episodes of emergence of the long-lived Laurentian carbonate platform, to meandering fluvial conglomerate and interstratified overbank mudstone packages deposited in the latest stages of infilling of the Taconic foredeep. In many ways this field trip is about contrasts. The Upper Cambrian (Furongian) and Lower Ordovician deposits of the Sauk megasequence record deposition controlled primarily by eustatic sea level sea level fluctuations that influenced deposition along the passive, southern (Appalachian) margin of the paleocontinent of Laurentia. The only tectonic influence apparent in these passive margin deposits is the expected thickening of the carbonate stack toward the platform margin as compared to the thinner (and typically shallower) facies that formed farther in toward the paleoshoreline. Carbonates overwhelmingly dominate the passive margin succession. Clastic influx was minimal and consisted largely of eastward transport of clean cratonic sands across the platform from the adjacent inner detrital belt to the west during higher order (2nd and 3rd order) regressions.</p><p>In contrast, Middle and Upper Ordovician deposits of the Tippecanoe megasequence record the strong influence of tectonics, specifically Iapetus closure. The first signal of this tectonic transformation was the arrival of arc-related ash beds that abound in the active margin carbonates. Subsequent intensification of Taconic orogenesis resulted in the foundering of the carbonate platform under the onslaught of fine siliciclastics arriving from offshore tectonic sources to the east, creating a deep marine flysch basin where graptolitic shale and sandstone turbidites accumulated. The foreland basin thus created would fill with progressively coarser and more shallow/proximal clastic facies through the Upper Ordovician, culminating in deposition of fluvial redbeds that cap the Taconic clastic wedge. Arguably the most controversial rocks within the Tippecanoe Sequence in this area are unusual, Lower Ordovician deep marine facies that are associated with the much younger flysch of the Martinsburg Formation in the Great Valley of eastern Pennsylvania. Long considered the erosional remnants of a Taconic-style thrust sheet, and referred to as the Hamburg Klippe, these deep marine deposits have recently been reinterpreted as olistostromal deposits that were introduced by gravity sliding into the flysch basin contemporaneous with Martinsburg deposition.</p><p>Besides their constituent lithofacies, rocks of the Sauk and Tippecanoe megasequences also present a stark contrast in faunas. Cambrian and Lower Ordovician faunas predate the Great Ordovician Biodiversification Event (GOBE), a global event that saw unprecedented diversification within many major invertebrate groups (mollusks, corals, and bryozoans to name a few) that previously were only minor components of the marine fauna. Unfortunately, the much higher diversity of Middle and Upper Ordovician faunas wrought by the GOBE is somewhat muted in this region by the stresses introduced by conversion of the Appalachian shelf into a flysch basin. Another noteworthy difference between the Cambrian and Ordovician biota related to the paleogeographic setting of the rocks to be examined on this trip derives from their evolution in the shallow marine environments of Laurentia. Several shelf-wide extinctions decimated the shallow marine faunas of the Laurentian shelf through the late Cambrian producing stage-level biostratigraphic units known as biomeres. The biomere phenomenon is discussed in this guidebook and a few stops to examine Cambrian faunas and one biomere boundary extinction are included to provide contrast with stage boundary extinctions that occurred later, in the Ordovician, that lack the defining attributes of the biomere boundary extinctions. Again, it’s all about contrast.</p>","language":"English","publisher":"Micropress","usgsCitation":"Taylor, J.F., Loch, J.D., Ganis, G., Repetski, J.E., Mitchell, C.E., Blackmer, G.C., Brezinski, D.K., Goldman, D., Orndorff, R.C., and Sell, B.K., 2015, Field trip guidebook for the post-meeting field trip: The Central Appalachians: Stratigraphy, v. 12, no. 3-4, p. 297-413.","productDescription":"117 p.","startPage":"297","endPage":"413","ipdsId":"IP-068793","costCenters":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"links":[{"id":351492,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":346787,"type":{"id":15,"text":"Index Page"},"url":"https://www.micropress.org/microaccess/stratigraphy/issue-317/article-1939"}],"country":"United States","otherGeospatial":"Central Appalachians","volume":"12","issue":"3-4","publishingServiceCenter":{"id":9,"text":"Reston PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5afeebefe4b0da30c1bfc6a8","contributors":{"authors":[{"text":"Taylor, John F.","contributorId":80890,"corporation":false,"usgs":false,"family":"Taylor","given":"John","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":713182,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Loch, James D.","contributorId":20139,"corporation":false,"usgs":false,"family":"Loch","given":"James","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":713183,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ganis, G. 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,{"id":70182177,"text":"70182177 - 2015 - High-speed limnology: Using advanced sensors to investigate spatial variability in biogeochemistry and hydrology","interactions":[],"lastModifiedDate":"2023-03-13T17:30:15.126103","indexId":"70182177","displayToPublicDate":"2015-01-01T00:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1565,"text":"Environmental Science & Technology","onlineIssn":"1520-5851","printIssn":"0013-936X","active":true,"publicationSubtype":{"id":10}},"title":"High-speed limnology: Using advanced sensors to investigate spatial variability in biogeochemistry and hydrology","docAbstract":"<p><span>Advanced sensor technology is widely used in aquatic monitoring and research. Most applications focus on temporal variability, whereas spatial variability has been challenging to document. We assess the capability of water chemistry sensors embedded in a high-speed water intake system to document spatial variability. This new sensor platform continuously samples surface water at a range of speeds (0 to &gt;45 km h</span><sup>–1</sup><span>) resulting in high-density, mesoscale spatial data. These novel observations reveal previously unknown variability in physical, chemical, and biological factors in streams, rivers, and lakes. By combining multiple sensors into one platform, we were able to detect terrestrial–aquatic hydrologic connections in a small dystrophic lake, to infer the role of main-channel vs backwater nutrient processing in a large river and to detect sharp chemical changes across aquatic ecosystem boundaries in a stream/lake complex. Spatial sensor data were verified in our examples by comparing with standard lab-based measurements of selected variables. Spatial fDOM data showed strong correlation with wet chemistry measurements of DOC, and optical NO</span><sub>3</sub><span> concentrations were highly correlated with lab-based measurements. High-frequency spatial data similar to our examples could be used to further understand aquatic biogeochemical fluxes, ecological patterns, and ecosystem processes, and will both inform and benefit from fixed-site data.</span></p>","language":"English","publisher":"ACS Publications","doi":"10.1021/es504773x","usgsCitation":"Crawford, J.T., Loken, L., Casson, N.J., Smith, C., Stone, A.G., and Winslow, L.A., 2015, High-speed limnology: Using advanced sensors to investigate spatial variability in biogeochemistry and hydrology: Environmental Science & Technology, v. 49, no. 1, p. 442-450, https://doi.org/10.1021/es504773x.","productDescription":"9 p.","startPage":"442","endPage":"450","ipdsId":"IP-060665","costCenters":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"links":[{"id":472436,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1021/es504773x","text":"Publisher Index Page"},{"id":335832,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Wisconsin","otherGeospatial":"Lake Mendota","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -89.40173033599879,\n              43.07347645438287\n            ],\n            [\n              -89.38023693230257,\n              43.078382654645424\n            ],\n            [\n              -89.36176603850066,\n              43.09800352757304\n            ],\n            [\n              -89.36848272715585,\n              43.11614723923495\n            ],\n            [\n              -89.37721442240766,\n              43.115656939360235\n            ],\n            [\n              -89.36411687953026,\n              43.12938385089856\n            ],\n            [\n              -89.37284857478208,\n              43.13575601287684\n            ],\n            [\n              -89.4020661704318,\n              43.1313445868372\n            ],\n            [\n              -89.40508868032673,\n              43.15486851517488\n            ],\n            [\n              -89.41986539536839,\n              43.1507034790599\n            ],\n            [\n              -89.43766462030436,\n              43.148253325220736\n            ],\n            [\n              -89.439343792468,\n              43.130364226724964\n            ],\n            [\n              -89.45479217637498,\n              43.114921482182126\n            ],\n            [\n              -89.4866964474873,\n              43.10707605564116\n            ],\n            [\n              -89.48568894418901,\n              43.08868439660202\n            ],\n            [\n              -89.4645313749251,\n              43.07642022167718\n            ],\n            [\n              -89.43262710381278,\n              43.08917491253359\n            ],\n            [\n              -89.42826125618721,\n              43.07936384756135\n            ],\n            [\n              -89.42053706423373,\n              43.074948355706226\n            ],\n            [\n              -89.40173033599879,\n              43.07347645438287\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"49","issue":"1","publishingServiceCenter":{"id":2,"text":"Denver PSC"},"noUsgsAuthors":false,"publicationDate":"2014-12-08","publicationStatus":"PW","scienceBaseUri":"58ac0e30e4b0ce4410e7d600","chorus":{"doi":"10.1021/es504773x","url":"http://dx.doi.org/10.1021/es504773x","publisher":"American Chemical Society (ACS)","authors":"Crawford John T., Loken Luke C., Casson Nora J., Smith Colin, Stone Amanda G., Winslow Luke A.","journalName":"Environmental Science & Technology","publicationDate":"1/6/2015","auditedOn":"3/4/2016","publiclyAccessibleDate":"12/8/2014"},"contributors":{"authors":[{"text":"Crawford, John T. 0000-0003-4440-6945 jtcrawford@usgs.gov","orcid":"https://orcid.org/0000-0003-4440-6945","contributorId":4081,"corporation":false,"usgs":true,"family":"Crawford","given":"John","email":"jtcrawford@usgs.gov","middleInitial":"T.","affiliations":[{"id":5044,"text":"National Research Program - 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,{"id":70191918,"text":"70191918 - 2015 - An integrated approach to modeling changes in land use, land cover, and disturbance and their impact on ecosystem carbon dynamics: a case study in the Sierra Nevada Mountains of California","interactions":[],"lastModifiedDate":"2017-10-19T13:04:58","indexId":"70191918","displayToPublicDate":"2015-01-01T00:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3893,"text":"AIMS Environmental Science","active":true,"publicationSubtype":{"id":10}},"title":"An integrated approach to modeling changes in land use, land cover, and disturbance and their impact on ecosystem carbon dynamics: a case study in the Sierra Nevada Mountains of California","docAbstract":"<p><span>Increased land-use intensity (e.g. clearing of forests for cultivation, urbanization), often results in the loss of ecosystem carbon storage, while changes in productivity resulting from climate change may either help offset or exacerbate losses. However, there are large uncertainties in how land and climate systems will evolve and interact to shape future ecosystem carbon dynamics. To address this we developed the Land Use and Carbon Scenario Simulator (LUCAS) to track changes in land use, land cover, land management, and disturbance, and their impact on ecosystem carbon storage and flux within a scenario-based framework. We have combined a state-and-transition simulation model (STSM) of land change with a stock and flow model of carbon dynamics. Land-change projections downscaled from the Intergovernmental Panel on Climate Change’s (IPCC) Special Report on Emission Scenarios (SRES) were used to drive changes within the STSM, while the Integrated Biosphere Simulator (IBIS) ecosystem model was used to derive input parameters for the carbon stock and flow model. The model was applied to the Sierra Nevada Mountains ecoregion in California, USA, a region prone to large wildfires and a forestry sector projected to intensify over the next century. Three scenario simulations were conducted, including a calibration scenario, a climate-change scenario, and an integrated climate- and land-change scenario. Based on results from the calibration scenario, the LUCAS age-structured carbon accounting model was able to accurately reproduce results obtained from the process-based biogeochemical model. Under the climate-only scenario, the ecoregion was projected to be a reliable net sink of carbon, however, when land use and disturbance were introduced, the ecoregion switched to become a net source. This research demonstrates how an integrated approach to carbon accounting can be used to evaluate various drivers of ecosystem carbon change in a robust, yet transparent modeling environment.</span></p>","language":"English","publisher":"AIMS","doi":"10.3934/environsci.2015.3.577","usgsCitation":"Sleeter, B.M., Liu, J., Daniel, C., Frid, L., and Zhu, Z., 2015, An integrated approach to modeling changes in land use, land cover, and disturbance and their impact on ecosystem carbon dynamics: a case study in the Sierra Nevada Mountains of California: AIMS Environmental Science, v. 2, no. 3, p. 577-606, https://doi.org/10.3934/environsci.2015.3.577.","productDescription":"30 p.","startPage":"577","endPage":"606","ipdsId":"IP-064456","costCenters":[{"id":657,"text":"Western Geographic Science Center","active":true,"usgs":true}],"links":[{"id":472411,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.3934/environsci.2015.3.577","text":"Publisher Index Page"},{"id":346968,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Sierra Nevada Mountains","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -122.05810546875,\n              40.6306300839918\n            ],\n            [\n              -120.673828125,\n              38.151837403006766\n            ],\n            [\n              -118.65234374999999,\n              35.46961797120201\n            ],\n            [\n              -117.80639648437499,\n              35.68407153314097\n            ],\n            [\n              -119.99267578124999,\n              39.918162846609455\n            ],\n            [\n              -121.2451171875,\n              41.09591205639546\n            ],\n            [\n              -122.05810546875,\n              40.6306300839918\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"2","issue":"3","publishingServiceCenter":{"id":14,"text":"Menlo Park PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"59e9b998e4b05fe04cd65cda","contributors":{"authors":[{"text":"Sleeter, Benjamin M. 0000-0003-2371-9571 bsleeter@usgs.gov","orcid":"https://orcid.org/0000-0003-2371-9571","contributorId":3479,"corporation":false,"usgs":true,"family":"Sleeter","given":"Benjamin","email":"bsleeter@usgs.gov","middleInitial":"M.","affiliations":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true},{"id":657,"text":"Western Geographic Science Center","active":true,"usgs":true}],"preferred":true,"id":713679,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Liu, Jinxun 0000-0003-0561-8988","orcid":"https://orcid.org/0000-0003-0561-8988","contributorId":197530,"corporation":false,"usgs":false,"family":"Liu","given":"Jinxun","affiliations":[],"preferred":false,"id":713680,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Daniel, Colin","contributorId":197531,"corporation":false,"usgs":false,"family":"Daniel","given":"Colin","affiliations":[],"preferred":false,"id":713681,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Frid, Leonardo","contributorId":196604,"corporation":false,"usgs":false,"family":"Frid","given":"Leonardo","email":"","affiliations":[],"preferred":false,"id":713682,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Zhu, Zhiliang 0000-0002-6860-6936 zzhu@usgs.gov","orcid":"https://orcid.org/0000-0002-6860-6936","contributorId":150078,"corporation":false,"usgs":true,"family":"Zhu","given":"Zhiliang","email":"zzhu@usgs.gov","affiliations":[{"id":5055,"text":"Land Change Science","active":true,"usgs":true},{"id":505,"text":"Office of the AD Climate and Land-Use Change","active":true,"usgs":true},{"id":411,"text":"National Climate Change and Wildlife Science Center","active":true,"usgs":true},{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"preferred":true,"id":713683,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70193678,"text":"70193678 - 2015 - Viewing the status of Virginia’s environment through the lens of freshwater fishes","interactions":[],"lastModifiedDate":"2017-11-13T11:58:02","indexId":"70193678","displayToPublicDate":"2015-01-01T00:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3694,"text":"Virginia Journal of Science","active":true,"publicationSubtype":{"id":10}},"title":"Viewing the status of Virginia’s environment through the lens of freshwater fishes","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Virginia Journal of Science","usgsCitation":"Angermeier, P.L., and Pinder, M.J., 2015, Viewing the status of Virginia’s environment through the lens of freshwater fishes: Virginia Journal of Science, v. 66, p. 147-169.","productDescription":"13 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J.","contributorId":200292,"corporation":false,"usgs":false,"family":"Pinder","given":"M.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":721803,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70187777,"text":"70187777 - 2015 - Early Permian conodont fauna and stratigraphy of the Garden Valley Formation, Eureka County, Nevada","interactions":[],"lastModifiedDate":"2017-05-18T14:27:37","indexId":"70187777","displayToPublicDate":"2015-01-01T00:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2735,"text":"Micropaleontology","active":true,"publicationSubtype":{"id":10}},"title":"Early Permian conodont fauna and stratigraphy of the Garden Valley Formation, Eureka County, Nevada","docAbstract":"The lower part of the Garden Valley Formation yields two distinct conodont faunas. One of late Asselian age dominated by Mesogondolella and Streptognathodus and one of Artinskian age dominated by Sweetognathus with Mesogondolella. The Asselian fauna contains the same species as those found in the type area of the Asselian in the southern Urals including Mesogondolella dentiseparata, described for the first time outside of the Urals. Apparatuses for Sweetognathus whitei, Diplognathodus stevensi, and Idioprioniodus sp. are described. The Garden Valley Formation represents a marine pro-delta basin and platform, and marine and shore fan delta complex deposition. The fan-delta complex was most likely deposited from late Artinskian to late Wordian. The Garden Valley Formation records tremendous swings in depositional setting from shallow-water to basin to shore.","language":"English","publisher":"Micropaleontology Press","usgsCitation":"Wardlaw, B.R., Gallegos, D.M., Chernykh, V.V., and Snyder, W.S., 2015, Early Permian conodont fauna and stratigraphy of the Garden Valley Formation, Eureka County, Nevada: Micropaleontology, v. 61, p. 369-387.","productDescription":"19 p.","startPage":"369","endPage":"387","ipdsId":"IP-071645","costCenters":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"links":[{"id":341481,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":341457,"type":{"id":15,"text":"Index Page"},"url":"https://www.micropress.org/microaccess/micropaleontology/issue-320/article-1955"}],"country":"United States","state":"Nevada","county":"Eureka County","otherGeospatial":"Garden Valley 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V.","contributorId":150733,"corporation":false,"usgs":false,"family":"Chernykh","given":"Valery","email":"","middleInitial":"V.","affiliations":[{"id":18081,"text":"Rusian Academy of Science","active":true,"usgs":false}],"preferred":false,"id":695577,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Snyder, Walter S.","contributorId":150735,"corporation":false,"usgs":false,"family":"Snyder","given":"Walter","email":"","middleInitial":"S.","affiliations":[{"id":18083,"text":"Boise State Univ.","active":true,"usgs":false}],"preferred":false,"id":695578,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70111380,"text":"70111380 - 2015 - Global view of remote sensing of rangelands: Evolution, applications, future pathways","interactions":[],"lastModifiedDate":"2024-06-17T16:26:53.891272","indexId":"70111380","displayToPublicDate":"2015-01-01T00:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"chapter":"10","title":"Global view of remote sensing of rangelands: Evolution, applications, future pathways","docAbstract":"<p>The term “rangeland” is rather nebulous, and there is no single definition of rangeland that is universally accepted by land managers, scientists, or international bodies (Lund, 2007; Reeves and Mitchell, 2011). Dozens and possibly hundreds (Lund, 2007) of definitions and ideologies exist because various stakeholders often have unique objectives requiring different information. For the purpose of describing the role of remote sensing in a global context, it is, however, necessary to provide definitions to orient the reader. The Food and Agricultural Organization (FAO) of the United Nations convened a conference in 2002 and again in 2013 to begin addressing the issue of harmonizing definitions of forest- related activities. Based on this concept, here rangelands are considered lands usually dominated by nonforest vegetation. The Society for Range Management defines rangelands as (SRM, 1998)</p><p>Land on which the indigenous vegetation (climax or natural potential) is predominantly grasses, grass-like plants, forbs, or shrubs and is managed as a natural ecosystem. If plants are introduced, they are managed similarly. Rangelands include natural grasslands, savannas, shrublands, many deserts, tundra, alpine communities, marshes, and wet meadows.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Remote sensing handbook","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"CRC Press","usgsCitation":"Reeves, M., Washington-Allen, R.A., Angerer, J., Hunt, E.R., Wasantha Kulawardhana, R., Kumar, L., Loboda, T., Loveland, T., Metternicht, G., and Ramsey, R.D., 2015, Global view of remote sensing of rangelands: Evolution, applications, future pathways, chap. 10 <i>of</i> Remote sensing handbook, v. 2, p. 237-275.","productDescription":"39 p.","startPage":"237","endPage":"275","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-056556","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":325008,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://www.taylorfrancis.com/chapters/edit/10.1201/b19322-13/global-view-remote-sensing-rangelands-evolution-applications-future-pathways-matthew-reeves-robert-washington-allen-jay-angerer-raymond-hunt-jr-ranjani-wasantha-kulawardhana-lalit-kumar-tatiana-loboda-thomas-loveland-graciela-metternicht-douglas-ramsey?context=ubx&refId=530aa9f9-5624-48f3-b33e-01f0265858dd","linkFileType":{"id":5,"text":"html"}},{"id":325009,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5784c33be4b0e02680be593b","contributors":{"editors":[{"text":"Thenkabail, Prasad S. 0000-0002-2182-8822 pthenkabail@usgs.gov","orcid":"https://orcid.org/0000-0002-2182-8822","contributorId":570,"corporation":false,"usgs":true,"family":"Thenkabail","given":"Prasad","email":"pthenkabail@usgs.gov","middleInitial":"S.","affiliations":[{"id":657,"text":"Western Geographic Science Center","active":true,"usgs":true}],"preferred":true,"id":642111,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Reeves, Matthew","contributorId":95437,"corporation":false,"usgs":true,"family":"Reeves","given":"Matthew","affiliations":[],"preferred":false,"id":642102,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Washington-Allen, Robert A.","contributorId":172793,"corporation":false,"usgs":false,"family":"Washington-Allen","given":"Robert","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":642103,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Angerer, Jay","contributorId":172794,"corporation":false,"usgs":false,"family":"Angerer","given":"Jay","email":"","affiliations":[],"preferred":false,"id":642104,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hunt, E. Raymond Jr.","contributorId":60557,"corporation":false,"usgs":true,"family":"Hunt","given":"E.","suffix":"Jr.","email":"","middleInitial":"Raymond","affiliations":[],"preferred":false,"id":642105,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Wasantha Kulawardhana, Ranjani","contributorId":172795,"corporation":false,"usgs":false,"family":"Wasantha Kulawardhana","given":"Ranjani","email":"","affiliations":[],"preferred":false,"id":642106,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Kumar, Lalit","contributorId":172796,"corporation":false,"usgs":false,"family":"Kumar","given":"Lalit","email":"","affiliations":[],"preferred":false,"id":642107,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Loboda, Tatiana","contributorId":172797,"corporation":false,"usgs":false,"family":"Loboda","given":"Tatiana","email":"","affiliations":[],"preferred":false,"id":642108,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Loveland, Thomas R. 0000-0003-3114-6646 loveland@usgs.gov","orcid":"https://orcid.org/0000-0003-3114-6646","contributorId":3005,"corporation":false,"usgs":true,"family":"Loveland","given":"Thomas R.","email":"loveland@usgs.gov","affiliations":[{"id":223,"text":"Earth Resources Observation and Science (EROS) Center (Geography)","active":false,"usgs":true}],"preferred":false,"id":518919,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Metternicht, Graciela","contributorId":172798,"corporation":false,"usgs":false,"family":"Metternicht","given":"Graciela","email":"","affiliations":[],"preferred":false,"id":642109,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Ramsey, R. Douglas","contributorId":172799,"corporation":false,"usgs":false,"family":"Ramsey","given":"R.","email":"","middleInitial":"Douglas","affiliations":[],"preferred":false,"id":642110,"contributorType":{"id":1,"text":"Authors"},"rank":10}]}}
,{"id":70192202,"text":"70192202 - 2015 - Future land-use scenarios and the loss of wildlife habitats in the southeastern United States","interactions":[],"lastModifiedDate":"2018-12-20T11:57:02","indexId":"70192202","displayToPublicDate":"2015-01-01T00:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1450,"text":"Ecological Applications","active":true,"publicationSubtype":{"id":10}},"title":"Future land-use scenarios and the loss of wildlife habitats in the southeastern United States","docAbstract":"<p><span>Land-use change is a major cause of wildlife habitat loss. Understanding how changes in land-use policies and economic factors can impact future trends in land use and wildlife habitat loss is therefore critical for conservation efforts. Our goal here was to evaluate the consequences of future land-use changes under different conservation policies and crop market conditions on habitat loss for wildlife species in the southeastern United States. We predicted the rates of habitat loss for 336 terrestrial vertebrate species by 2051. We focused on habitat loss due to the expansion of urban, crop, and pasture. Future land-use changes following business-as-usual conditions resulted in relatively low rates of wildlife habitat loss across the entire Southeast, but some ecoregions and species groups experienced much higher habitat loss than others. Increased crop commodity prices exacerbated wildlife habitat loss in most ecoregions, while the implementation of conservation policies (reduced urban sprawl, and payments for land conservation) reduced the projected habitat loss in some regions, to a certain degree. Overall, urban and crop expansion were the main drivers of habitat loss. Reptiles and wildlife species associated with open vegetation (grasslands, open woodlands) were the species groups most vulnerable to future land-use change. Effective conservation of wildlife habitat in the Southeast should give special consideration to future land-use changes, regional variations, and the forces that could shape land-use decisions.</span></p>","language":"English","publisher":"Ecological Society of America","doi":"10.1890/13-2078.1","usgsCitation":"Martinuzzi, S., Withey, J.C., Pidgeon, A.M., Plantinga, A., McKerrow, A., Williams, S.G., Helmers, D., and Radeloff, V.C., 2015, Future land-use scenarios and the loss of wildlife habitats in the southeastern United States: Ecological Applications, v. 25, no. 1, p. 160-171, https://doi.org/10.1890/13-2078.1.","productDescription":"12 p.","startPage":"160","endPage":"171","ipdsId":"IP-053057","costCenters":[{"id":208,"text":"Core Science Analytics and Synthesis","active":true,"usgs":true},{"id":37226,"text":"Core Science Analytics, Synthesis, and Libraries","active":true,"usgs":true},{"id":38315,"text":"GAP Analysis Project","active":true,"usgs":true}],"links":[{"id":347105,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -76.4208984375,\n              38.993572058209466\n            ],\n            [\n              -78.11279296875,\n              39.67337039176558\n            ],\n            [\n              -82.6171875,\n              39.50404070558415\n            ],\n            [\n              -88.72558593749999,\n              39.38526381099774\n            ],\n            [\n              -91.34033203125,\n              33.94335994657882\n            ],\n            [\n              -91.7138671875,\n              30.391830328088137\n            ],\n     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Lab, Department of Forest and Wildlife Ecology, University of Wisconsin-Madison","active":true,"usgs":false}],"preferred":false,"id":714743,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Plantinga, Andrew","contributorId":197998,"corporation":false,"usgs":false,"family":"Plantinga","given":"Andrew","affiliations":[],"preferred":false,"id":714744,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"McKerrow, Alexa 0000-0002-8312-2905 amckerrow@usgs.gov","orcid":"https://orcid.org/0000-0002-8312-2905","contributorId":127753,"corporation":false,"usgs":true,"family":"McKerrow","given":"Alexa","email":"amckerrow@usgs.gov","affiliations":[{"id":208,"text":"Core Science Analytics and Synthesis","active":true,"usgs":true}],"preferred":true,"id":714740,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Williams, Steven G.","contributorId":176234,"corporation":false,"usgs":false,"family":"Williams","given":"Steven","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":714745,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Helmers, David P.","contributorId":177497,"corporation":false,"usgs":false,"family":"Helmers","given":"David P.","affiliations":[],"preferred":false,"id":714746,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Radeloff, Volker C.","contributorId":141124,"corporation":false,"usgs":false,"family":"Radeloff","given":"Volker","email":"","middleInitial":"C.","affiliations":[{"id":13679,"text":"SILVIS Lab, Department of Forest and Wildlife Ecology, University of Wisconsin-Madison","active":true,"usgs":false}],"preferred":false,"id":714747,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":70188440,"text":"70188440 - 2015 - Thermokarst lake methanogenesis along a complete talik profile","interactions":[],"lastModifiedDate":"2017-06-09T14:07:53","indexId":"70188440","displayToPublicDate":"2015-01-01T00:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1011,"text":"Biogeosciences","active":true,"publicationSubtype":{"id":10}},"title":"Thermokarst lake methanogenesis along a complete talik profile","docAbstract":"<p><span>Thermokarst (thaw) lakes emit methane (CH</span><sub>4</sub><span>) to the atmosphere formed from thawed permafrost organic matter (OM), but the relative magnitude of CH</span><sub>4</sub><span> production in surface lake sediments vs. deeper thawed permafrost horizons is not well understood. We assessed anaerobic CH</span><sub>4</sub><span> production potentials from various depths along a 590 cm long lake sediment core that captured the entire sediment package of the talik (thaw bulb) beneath the center of an interior Alaska thermokarst lake, Vault Lake, and the top 40 cm of thawing permafrost beneath the talik. We also studied the adjacent Vault Creek permafrost tunnel that extends through ice-rich yedoma permafrost soils surrounding the lake and into underlying gravel. Our results showed CH</span><sub>4</sub><span> production potentials were highest in the organic-rich surface lake sediments, which were 151 cm thick (mean ± SD: 5.95 ± 1.67 μg C–CH</span><sub>4</sub><span> g dw</span><sup>−1</sup><span> d</span><sup>−1</sup><span>; 125.9 ± 36.2 μg C–CH</span><sub>4</sub><span> g C</span><sup>−1</sup><sub>org</sub><span> d</span><sup>−1</sup><span>). High CH</span><sub>4</sub><span> production potentials were also observed in recently thawed permafrost (1.18 ± 0.61 μg C–CH</span><sub>4</sub><span>g dw</span><sup>−1</sup><span> d</span><sup>−1</sup><span>; 59.60± 51.5 μg C–CH</span><sub>4</sub><span> g C</span><sup>−1</sup><sub>org</sub><span> d</span><sup>−1</sup><span>) at the bottom of the talik, but the narrow thicknesses (43 cm) of this horizon limited its overall contribution to total sediment column CH</span><sub>4</sub><span> production in the core. Lower rates of CH</span><sub>4</sub><span> production were observed in sediment horizons representing permafrost that has been thawing in the talik for a longer period of time. No CH</span><sub>4</sub><span> production was observed in samples obtained from the permafrost tunnel, a non-lake environment. Our findings imply that CH</span><sub>4</sub><span>production is highly variable in thermokarst lake systems and that both modern OM supplied to surface sediments and ancient OM supplied to both surface and deep lake sediments by in situ thaw and shore erosion of yedoma permafrost are important to lake CH</span><sub>4</sub><span> production.</span></p>","language":"English","publisher":"European Geosciences Union","doi":"10.5194/bg-12-4317-2015","usgsCitation":"Heslop, J., Walter Anthony, K., Sepulveda-Jauregui, A., Martinez-Cruz, K., Bondurant, A., Grosse, G., and Jones, M.C., 2015, Thermokarst lake methanogenesis along a complete talik profile: Biogeosciences, v. 12, p. 4317-4331, https://doi.org/10.5194/bg-12-4317-2015.","productDescription":"15 p.","startPage":"4317","endPage":"4331","ipdsId":"IP-064594","costCenters":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"links":[{"id":488681,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.5194/bg-12-4317-2015","text":"Publisher Index Page"},{"id":342339,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"12","publishingServiceCenter":{"id":9,"text":"Reston PSC"},"noUsgsAuthors":false,"publicationDate":"2015-07-24","publicationStatus":"PW","scienceBaseUri":"593bb3a9e4b0764e6c60e7eb","contributors":{"authors":[{"text":"Heslop, J.K.","contributorId":192801,"corporation":false,"usgs":false,"family":"Heslop","given":"J.K.","email":"","affiliations":[],"preferred":false,"id":697757,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Walter Anthony, K.M.","contributorId":169384,"corporation":false,"usgs":false,"family":"Walter Anthony","given":"K.M.","email":"","affiliations":[{"id":6752,"text":"University of Alaska Fairbanks","active":true,"usgs":false}],"preferred":false,"id":697758,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sepulveda-Jauregui, A.","contributorId":192802,"corporation":false,"usgs":false,"family":"Sepulveda-Jauregui","given":"A.","email":"","affiliations":[],"preferred":false,"id":697759,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Martinez-Cruz, K.","contributorId":192803,"corporation":false,"usgs":false,"family":"Martinez-Cruz","given":"K.","email":"","affiliations":[],"preferred":false,"id":697760,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Bondurant, A.","contributorId":192804,"corporation":false,"usgs":false,"family":"Bondurant","given":"A.","affiliations":[],"preferred":false,"id":697761,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Grosse, G.","contributorId":192805,"corporation":false,"usgs":false,"family":"Grosse","given":"G.","email":"","affiliations":[],"preferred":false,"id":697762,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Jones, Miriam C. 0000-0002-6650-7619 miriamjones@usgs.gov","orcid":"https://orcid.org/0000-0002-6650-7619","contributorId":4056,"corporation":false,"usgs":true,"family":"Jones","given":"Miriam","email":"miriamjones@usgs.gov","middleInitial":"C.","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"preferred":true,"id":697756,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
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