{"pageNumber":"782","pageRowStart":"19525","pageSize":"25","recordCount":165485,"records":[{"id":70199970,"text":"sir20185121 - 2018 - Relating cyanobacteria and physicochemical water-quality properties in Willow Creek Lake, Nebraska, 2012–14","interactions":[],"lastModifiedDate":"2018-11-19T14:20:04","indexId":"sir20185121","displayToPublicDate":"2018-11-19T06:54:31","publicationYear":"2018","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2018-5121","displayTitle":"Relating Cyanobacteria and Physicochemical Water-Quality Properties in Willow Creek Lake, Nebraska, 2012–14","title":"Relating cyanobacteria and physicochemical water-quality properties in Willow Creek Lake, Nebraska, 2012–14","docAbstract":"<p>Cyanobacteria (also referred to as blue-green algae) are naturally present members of phytoplankton assemblages that may detract from beneficial uses of water because some strains produce cyanotoxins that pose health hazards to people and animals. Cyanobacteria populations observed in Willow Creek Lake during 2012 through 2014 were compared to external nutrient loading from the Willow Creek drainage basin and several other physicochemical properties within the lake, including internal nutrient loading. This report is part of a cooperative study between the U.S. Geological Survey, the Lower Elkhorn Natural Resources District, the Nebraska Department of Environmental Quality, the Nebraska Game and Parks Commission, the Nebraska Department of Natural Resources, the Nebraska Environmental Trust, and the University of Nebraska–Lincoln.</p><p>Cyanobacteria concentrations were quantified using weekly microcystin sampling, intermittent algal taxonomy, and hourly in-situ phycocyanin measurements. External and internal nutrient loads, lake water physical characteristics, and local meteorological conditions were evaluated as potential causes of cyanobacterial blooms. A water balance approach that estimated Willow Creek Lake inflow and outflow volumes identified Willow Creek as the major inflow and groundwater flux as the major outflow for the lake. Nutrient concentrations from several water sources were quantified and combined with flow volumes to compute nutrient loads during the study period.</p><p>Surface flows contributed most external nutrients to the lake, whereas lake nutrients were exported during groundwater losses. The main stem of Willow Creek accounted for most nitrate loads to the lake, whereas total Kjeldahl nitrogen, total phosphorus, and phosphate loads to the lake were more evenly distributed between Willow Creek and the North Tributary, a smaller drainage. Sediment core incubations determined internal phosphorus loading was a negligible component of the overall nutrient load to the lake.</p><p>Cyanobacterial responses were compared to nutrient loads and other external factors that could potentially affect algal growth. A series of univariate comparisons were made by plotting those factors against phycocyanin using biweekly summaries of each and a multivariate model that incorporated seasonality and cumulative nitrate loading. Although the multivariate model only incorporated cumulative nitrate, both nitrogen and phosphorus are likely contributing to cyanobacterial population growth, and management efforts may benefit from the recognition of differences in nutrient loading characteristics between the monitored basins.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20185121","collaboration":"Prepared in cooperation with the Lower Elkhorn Natural Resources District, Nebraska Department of Environmental Quality, Nebraska Game and Parks Commission, Nebraska Department of Natural Resources, Nebraska Environmental Trust, and University of Nebraska–Lincoln","usgsCitation":"Rus, D.L., Hall, B.M., and Thomas, S.A., 2018, Relating cyanobacteria and physicochemical water-quality properties in Willow Creek Lake, Nebraska, 2012–14: U.S. Geological Survey Scientific Investigations Report 2018–5121, 43 p, https://doi.org/10.3133/sir20185121.","productDescription":"Report: x, 43 p.; Data Release","numberOfPages":"58","onlineOnly":"Y","ipdsId":"IP-073831","costCenters":[{"id":464,"text":"Nebraska Water Science Center","active":true,"usgs":true}],"links":[{"id":359466,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/sir/2018/5121/sir20185121.pdf","text":"Report","size":"2.39 MB","linkFileType":{"id":1,"text":"pdf"},"description":"SIR 2018–5121"},{"id":359467,"rank":3,"type":{"id":30,"text":"Data Release"},"url":"https://doi.org/10.5066/P9RBDQI5","text":"USGS data release","description":"USGS Data Release","linkHelpText":"Monitoring Data for Willow Creek Lake, Nebraska, 2012–14"},{"id":359465,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/sir/2018/5121/coverthb2.jpg"}],"country":"United States","state":"Nebraska","otherGeospatial":"Willow Creek Lake","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -98.1667,\n              42\n            ],\n            [\n              -97.3333,\n              42\n            ],\n            [\n              -97.3333,\n              42.333\n            ],\n            [\n              -98.1667,\n              42.333\n            ],\n            [\n              -98.1667,\n              42\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","contact":"<p><a data-mce-href=\"mailto:%20dc_ne@usgs.gov\" href=\"mailto:%20dc_ne@usgs.gov\">Director</a>, <a data-mce-href=\"https://www.usgs.gov/centers/ne-water\" href=\"https://www.usgs.gov/centers/ne-water\">Nebraska Water Science Center</a> <br>U.S. Geological Survey<br>5231 South 19th Street <br>Lincoln, NE 68512</p>","tableOfContents":"<ul><li>Acknowledgments</li><li>Abstract</li><li>Introduction</li><li>Methods</li><li>Cyanobacterial Characteristics in Willow Creek Lake</li><li>Physicochemical Water-Quality Properties of Willow Creek Lake</li><li>Relation of Nutrients and Other Factors to Cyanobacteria</li><li>Summary</li><li>References Cited</li><li>Appendix 1. Development of Stream Nutrient Load Models</li></ul>","publishingServiceCenter":{"id":4,"text":"Rolla PSC"},"publishedDate":"2018-11-19","noUsgsAuthors":false,"publicationDate":"2018-11-19","publicationStatus":"PW","scienceBaseUri":"5bf3d9efe4b045bfcae0c9af","contributors":{"authors":[{"text":"Rus, David L. 0000-0003-3538-7826","orcid":"https://orcid.org/0000-0003-3538-7826","contributorId":208516,"corporation":false,"usgs":true,"family":"Rus","given":"David L.","affiliations":[{"id":464,"text":"Nebraska Water Science Center","active":true,"usgs":true}],"preferred":true,"id":747528,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hall, Brent M. 0000-0003-3815-5158 bhall@usgs.gov","orcid":"https://orcid.org/0000-0003-3815-5158","contributorId":4547,"corporation":false,"usgs":true,"family":"Hall","given":"Brent","email":"bhall@usgs.gov","middleInitial":"M.","affiliations":[{"id":464,"text":"Nebraska Water Science Center","active":true,"usgs":true}],"preferred":true,"id":747529,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Thomas, Steven A. 0000-0002-5249-3500","orcid":"https://orcid.org/0000-0002-5249-3500","contributorId":208517,"corporation":false,"usgs":false,"family":"Thomas","given":"Steven","email":"","middleInitial":"A.","affiliations":[{"id":37813,"text":"Univeristy of Nebraska - Lincoln","active":true,"usgs":false}],"preferred":false,"id":747530,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70216308,"text":"70216308 - 2018 - Landscape drivers and social dynamics shaping microbial contamination risk in three Maya communities in southern Belize, Central America","interactions":[],"lastModifiedDate":"2020-11-11T14:31:12.681462","indexId":"70216308","displayToPublicDate":"2018-11-17T08:18:48","publicationYear":"2018","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3709,"text":"Water","active":true,"publicationSubtype":{"id":10}},"title":"Landscape drivers and social dynamics shaping microbial contamination risk in three Maya communities in southern Belize, Central America","docAbstract":"<div class=\"art-abstract in-tab hypothesis_container\">Land transformation can have cascading effects on hydrology, water quality, and human users of water resources, with serious implications for human health. An interdisciplinary analysis is presented, whereby remote-sensing data of changing land use and cover are related to surface hydrology and microbial contamination in domestic use areas of three indigenous Maya communities in Belize, Central America. We asked whether a departure from traditional land-use patterns toward intensified use led to consequences for hydrology and microbial contamination of drinking water, and investigated how social factors in the three study communities may act to ameliorate human health risks associated with water contamination. We showed that a departure from traditional land use to more intensive cultivation and grazing led to significantly increased surface water runoff, and intensified microbial contamination of surface water sources sometimes used for drinking. Results further suggested that groundwater contamination was widespread regardless of land cover, due to the widespread presence of pit latrines, pigs, and cows on the landscape, and that human users were consistently subject to health risks from potential pathogens as a result. Given that both surface and groundwater resources were found to be contaminated, it is important that water distribution systems (piped water from tanks; shallow and deep wells) be monitored for<span>&nbsp;</span><span class=\"html-italic\">Escherichia coli</span><span>&nbsp;</span>and treated when necessary to reduce or eliminate contaminants and protect public health. Results of interviews suggested that strengthened capacity within the communities to monitor and treat centralized drinking water sources and increase water treatment at the point of use could lead to reduced risk to water consumers.<span id=\"_mce_caret\" data-mce-bogus=\"1\" data-mce-type=\"format-caret\"><span></span></span></div>","language":"English","publisher":"MDPI","doi":"10.3390/w10111678","usgsCitation":"Esselman, P., Jiang, S., Peller, H.A., Bucklin, D.N., and Wainwright, J., 2018, Landscape drivers and social dynamics shaping microbial contamination risk in three Maya communities in southern Belize, Central America: Water, v. 10, no. 11, 1678, 22 p., https://doi.org/10.3390/w10111678.","productDescription":"1678, 22 p.","ipdsId":"IP-101981","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":468241,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.3390/w10111678","text":"Publisher Index Page"},{"id":380406,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Belize","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -89.40673828125,\n              15.845104902273464\n            ],\n            [\n              -88.626708984375,\n              15.845104902273464\n            ],\n            [\n              -88.626708984375,\n              16.56249250837488\n            ],\n            [\n              -89.40673828125,\n              16.56249250837488\n            ],\n            [\n              -89.40673828125,\n              15.845104902273464\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"10","issue":"11","noUsgsAuthors":false,"publicationDate":"2018-11-17","publicationStatus":"PW","contributors":{"authors":[{"text":"Esselman, Peter C. 0000-0002-0085-903X","orcid":"https://orcid.org/0000-0002-0085-903X","contributorId":204291,"corporation":false,"usgs":true,"family":"Esselman","given":"Peter C.","affiliations":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"preferred":true,"id":804617,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jiang, Shiguo 0000-0001-9088-883X","orcid":"https://orcid.org/0000-0001-9088-883X","contributorId":244799,"corporation":false,"usgs":false,"family":"Jiang","given":"Shiguo","email":"","affiliations":[{"id":48981,"text":"State University of New York","active":true,"usgs":false}],"preferred":false,"id":804618,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Peller, Henry A","contributorId":244800,"corporation":false,"usgs":false,"family":"Peller","given":"Henry","email":"","middleInitial":"A","affiliations":[{"id":36630,"text":"Ohio State University","active":true,"usgs":false}],"preferred":false,"id":804619,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bucklin, David N.","contributorId":175273,"corporation":false,"usgs":false,"family":"Bucklin","given":"David","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":804620,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Wainwright, Joel D","contributorId":244801,"corporation":false,"usgs":false,"family":"Wainwright","given":"Joel D","affiliations":[{"id":36630,"text":"Ohio State University","active":true,"usgs":false}],"preferred":false,"id":804621,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70199669,"text":"ofr20181154 - 2018 - Community for Data Integration fiscal year 2017 funded project report","interactions":[],"lastModifiedDate":"2018-11-19T10:21:24","indexId":"ofr20181154","displayToPublicDate":"2018-11-16T17:30:00","publicationYear":"2018","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":"2018-1154","title":"Community for Data Integration fiscal year 2017 funded project report","docAbstract":"<p>The U.S. Geological Survey Community for Data Integration annually funds small projects focusing on data integration for interdisciplinary research, innovative data management, and demonstration of new technologies. This report provides a summary of the 11 projects funded in fiscal year 2017, outlining their goals, activities, and outputs.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20181154","usgsCitation":"Hsu, L., Allstadt, K.E., Bell, T.M., Boydston, E.E., Erickson, R.A., Everette, A.L., Lentz, E., Peters, J., Reichert,  B.E., Nagorsen, S., Sherba, J.T., Signell, R.P., Wiltermuth, M.T., and Young, J.A., 2018, Community for Data Integration fiscal year 2017 funded project report: U.S. Geological Survey Open-File Report 2018–1154, 15 p., https://doi.org/10.3133/ofr20181154.","productDescription":"iv, 15 p.","onlineOnly":"Y","ipdsId":"IP-099013","costCenters":[{"id":38128,"text":"Science Analytics and Synthesis","active":true,"usgs":true}],"links":[{"id":359452,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2018/1154/ofr20181154.pdf","text":"Report","size":"6.35 MB","linkFileType":{"id":1,"text":"pdf"},"description":"OFR 2018-1154"},{"id":359451,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2018/1154/coverthb.jpg"}],"contact":"<p>Director, <a href=\"https://www.usgs.gov/core-science-systems/science-analytics-and-synthesis/\" data-mce-href=\"https://www.usgs.gov/core-science-systems/science-analytics-and-synthesis/\">Science Analytics and Synthesis</a><br>U.S. Geological Survey<br>108 National Center<br>12201 Sunrise Valley Drive<br>Reston, VA 20192</p>","tableOfContents":"<ul><li>Abstract</li><li>Introduction</li><li>Community for Data Integration Funded Projects, Fiscal Year 2017</li><li>Summary</li><li>References Cited</li></ul>","publishingServiceCenter":{"id":2,"text":"Denver PSC"},"publishedDate":"2018-11-16","noUsgsAuthors":false,"publicationDate":"2018-11-16","publicationStatus":"PW","scienceBaseUri":"5befe5b7e4b045bfcadf7f22","contributors":{"authors":[{"text":"Hsu, Leslie 0000-0002-5353-807X lhsu@usgs.gov","orcid":"https://orcid.org/0000-0002-5353-807X","contributorId":191745,"corporation":false,"usgs":true,"family":"Hsu","given":"Leslie","email":"lhsu@usgs.gov","affiliations":[{"id":208,"text":"Core Science Analytics and Synthesis","active":true,"usgs":true}],"preferred":true,"id":746128,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Allstadt, Kate E. 0000-0003-4977-5248 kallstadt@usgs.gov","orcid":"https://orcid.org/0000-0003-4977-5248","contributorId":167684,"corporation":false,"usgs":true,"family":"Allstadt","given":"Kate","email":"kallstadt@usgs.gov","middleInitial":"E.","affiliations":[{"id":234,"text":"Earthquake Hazards Program","active":true,"usgs":true},{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":false,"id":746129,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bell, Tara M. 0000-0002-6010-0869 tbell@usgs.gov","orcid":"https://orcid.org/0000-0002-6010-0869","contributorId":5824,"corporation":false,"usgs":true,"family":"Bell","given":"Tara","email":"tbell@usgs.gov","middleInitial":"M.","affiliations":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"preferred":true,"id":751335,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Boydston, Erin E. 0000-0002-8452-835X eboydston@usgs.gov","orcid":"https://orcid.org/0000-0002-8452-835X","contributorId":1705,"corporation":false,"usgs":true,"family":"Boydston","given":"Erin","email":"eboydston@usgs.gov","middleInitial":"E.","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":true,"id":746131,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Erickson, Richard A. 0000-0003-4649-482X rerickson@usgs.gov","orcid":"https://orcid.org/0000-0003-4649-482X","contributorId":5455,"corporation":false,"usgs":true,"family":"Erickson","given":"Richard","email":"rerickson@usgs.gov","middleInitial":"A.","affiliations":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"preferred":true,"id":746132,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Everette, A. Lance 0000-0003-2539-9129 everettel@usgs.gov","orcid":"https://orcid.org/0000-0003-2539-9129","contributorId":176202,"corporation":false,"usgs":true,"family":"Everette","given":"A.","email":"everettel@usgs.gov","middleInitial":"Lance","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":true,"id":751331,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Lentz, Erika E. 0000-0002-0621-8954 elentz@usgs.gov","orcid":"https://orcid.org/0000-0002-0621-8954","contributorId":173964,"corporation":false,"usgs":true,"family":"Lentz","given":"Erika","email":"elentz@usgs.gov","middleInitial":"E.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":746134,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Peters, Jeff 0000-0003-4312-0590 jpeters@usgs.gov","orcid":"https://orcid.org/0000-0003-4312-0590","contributorId":4711,"corporation":false,"usgs":true,"family":"Peters","given":"Jeff","email":"jpeters@usgs.gov","affiliations":[{"id":657,"text":"Western Geographic Science Center","active":true,"usgs":true},{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":746136,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Reichert, Brian E. 0000-0002-9640-0695","orcid":"https://orcid.org/0000-0002-9640-0695","contributorId":204260,"corporation":false,"usgs":true,"family":"Reichert","given":"Brian","middleInitial":"E.","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":true,"id":751332,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Nagorsen, Sarah 0000-0001-5901-0279","orcid":"https://orcid.org/0000-0001-5901-0279","contributorId":208147,"corporation":false,"usgs":false,"family":"Nagorsen","given":"Sarah","affiliations":[{"id":18047,"text":"n/a","active":true,"usgs":false}],"preferred":false,"id":746135,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Sherba, Jason T. 0000-0001-9151-686X jsherba@usgs.gov","orcid":"https://orcid.org/0000-0001-9151-686X","contributorId":196154,"corporation":false,"usgs":true,"family":"Sherba","given":"Jason","email":"jsherba@usgs.gov","middleInitial":"T.","affiliations":[{"id":657,"text":"Western Geographic Science Center","active":true,"usgs":true}],"preferred":true,"id":751333,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Signell, Richard P. 0000-0003-0682-9613 rsignell@usgs.gov","orcid":"https://orcid.org/0000-0003-0682-9613","contributorId":140906,"corporation":false,"usgs":true,"family":"Signell","given":"Richard","email":"rsignell@usgs.gov","middleInitial":"P.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":751334,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Wiltermuth, Mark T. 0000-0002-8871-2816 mwiltermuth@usgs.gov","orcid":"https://orcid.org/0000-0002-8871-2816","contributorId":708,"corporation":false,"usgs":true,"family":"Wiltermuth","given":"Mark","email":"mwiltermuth@usgs.gov","middleInitial":"T.","affiliations":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true},{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"preferred":true,"id":746140,"contributorType":{"id":1,"text":"Authors"},"rank":13},{"text":"Young, John A. 0000-0002-4500-3673 jyoung@usgs.gov","orcid":"https://orcid.org/0000-0002-4500-3673","contributorId":3777,"corporation":false,"usgs":true,"family":"Young","given":"John","email":"jyoung@usgs.gov","middleInitial":"A.","affiliations":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"preferred":true,"id":746141,"contributorType":{"id":1,"text":"Authors"},"rank":14}]}}
,{"id":70196647,"text":"sim3405 - 2018 - Geologic map of the north half of the Lake Walcott 30'×60' quadrangle, Idaho","interactions":[],"lastModifiedDate":"2018-11-19T10:29:40","indexId":"sim3405","displayToPublicDate":"2018-11-16T17:00:00","publicationYear":"2018","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":333,"text":"Scientific Investigations Map","code":"SIM","onlineIssn":"2329-132X","printIssn":"2329-1311","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"3405","title":"Geologic map of the north half of the Lake Walcott 30'×60' quadrangle, Idaho","docAbstract":"<p>The geologic map of the northern half of the Lake Walcott 30ʹ×60ʹ quadrangle shows the volcanic geology of the southern part of the Craters of the Moon lava field, the complex geologic features of the Holocene Kings Bowl and Wapi lava fields, and the southern part of the Great Rift volcanic rift zone. The long extent and distribution of skylights in lava-tube systems of the Horse Butte and Wapi Park lava fields are depicted on this map. <sup>40</sup>Ar/<sup>39</sup>Ar and K/Ar age determinations give detail to the Holocene, late Pleistocene, and late middle Pleistocene volcanic lava fields in this quadrangle. Most of the younger basalt eruptions (less than 150 thousand years [ka]) have occurred along the Great Rift volcanic rift zone, but two of the younger lava fields are located in the western part of the quadrangle. Kimama Butte, a shield volcano, is 87±11 ka, and Shale Butte is dated at 11±6 ka. Paleomagnetic studies have shown that the Horse Butte-Inferno Chasm eruptive fissure system has at least five paleomagnetic-correlative lava fields, the Claasen vent complex consists of at least seven correlative lava fields, and the Streifling-Flat Top vent complex includes at least four correlative lava fields.</p><p>This map provides geologic, geochronologic, and paleomagnetic data for Holocene lava fields along the southern part of the Great Rift, and for late Pleistocene and late middle Pleistocene lava fields in the central and western parts of the quadrangle. These data can contribute to wise management and preservation of the Craters of the Moon National Monument and for broad-scale understanding of the basaltic-volcanic evolution of the eastern Snake River Plain.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sim3405","collaboration":"Prepared in cooperation with the National Park Service and the Bureau of Land Management","usgsCitation":"Kuntz, M.A., Champion, D.E., Turrin, B.R., Gans, P.B., Covington, H.R., and VanSistine, D.P., 2018, Geologic map of the north half of the Lake Walcott 30'×60' quadrangle, Idaho: U.S. Geological Survey Scientific Investigations Report 3405, pamphlet 25 p., scale 1:100,000, https://doi.org/10.3133/sim3405.","productDescription":"Report: v, 25 p.; Sheet: 49.75 x 34.00 inches; Read Me; Data Release","onlineOnly":"Y","ipdsId":"IP-084554","costCenters":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"links":[{"id":358860,"rank":2,"type":{"id":26,"text":"Sheet"},"url":"https://pubs.usgs.gov/sim/3405/sim3405_sheet_georeferenced.pdf","text":"Map","size":"75.5 MB","linkFileType":{"id":1,"text":"pdf"},"description":"SIM 3405 Hillshaded Map"},{"id":358861,"rank":3,"type":{"id":20,"text":"Read Me"},"url":"https://pubs.usgs.gov/sim/3405/sim3405_Readme.txt","text":"Read Me","size":"8.00 KB","linkFileType":{"id":2,"text":"txt"},"description":"SIM 3405 Read Me"},{"id":358862,"rank":4,"type":{"id":30,"text":"Data Release"},"url":"https://doi.org/10.5066/F7VQ30VZ","text":"USGS data release","description":"USGS Data Release","linkHelpText":"Data Release for Geologic Map of the north half of the Lake Walcott 30' x 60' Quadrangle, Idaho"},{"id":359523,"rank":5,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/sim/3405/sim3405_pamphlet.pdf","text":"Report","size":"5.62 MB","linkFileType":{"id":1,"text":"pdf"},"description":"SIM 3405 Pamphlet"},{"id":358856,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/sim/3405/coverthb2.jpg"}],"country":"United States","state":"Idaho","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -114,\n              42.75\n            ],\n            [\n              -113,\n              42.75\n            ],\n            [\n              -113,\n              43\n            ],\n            [\n              -114,\n              43\n            ],\n            [\n              -114,\n              42.75\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","contact":"<p>Director, <a href=\"http://www.usgs.gov/centers/gecsc/\" data-mce-href=\"http://www.usgs.gov/centers/gecsc/\">Geosciences and Environmental Change Science Center</a><br>U.S. Geological Survey<br>Box 25046, MS-980<br>Denver, CO 80225-0046</p>","tableOfContents":"<ul><li>Introduction</li><li>Evolution, Purpose, and Use of this Map</li><li>Rock Nomenclature, Petrologic Descriptions, and Notes on Rock Names, Descriptions, and Thickness of Lava Flows</li><li>Geochronology</li><li>Description of Map Units</li><li>References Cited</li></ul>","publishingServiceCenter":{"id":2,"text":"Denver PSC"},"publishedDate":"2018-11-16","noUsgsAuthors":false,"publicationDate":"2018-11-16","publicationStatus":"PW","scienceBaseUri":"5befe5b8e4b045bfcadf7f24","contributors":{"authors":[{"text":"Kuntz, Mel A. 0000-0001-8828-5474","orcid":"https://orcid.org/0000-0001-8828-5474","contributorId":204407,"corporation":false,"usgs":false,"family":"Kuntz","given":"Mel A.","affiliations":[{"id":36935,"text":"Retired-USGS","active":true,"usgs":false}],"preferred":false,"id":733902,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Champion, Duane E. 0000-0001-7854-9034 dchamp@usgs.gov","orcid":"https://orcid.org/0000-0001-7854-9034","contributorId":2912,"corporation":false,"usgs":true,"family":"Champion","given":"Duane","email":"dchamp@usgs.gov","middleInitial":"E.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":733903,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Turrin, Brent R.","contributorId":204409,"corporation":false,"usgs":false,"family":"Turrin","given":"Brent","email":"","middleInitial":"R.","affiliations":[{"id":36936,"text":"Dept. of Earth & Planetary Sciences, Rutgers Univ., NJ","active":true,"usgs":false}],"preferred":false,"id":750062,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Gans, Philip B.","contributorId":66791,"corporation":false,"usgs":false,"family":"Gans","given":"Philip","email":"","middleInitial":"B.","affiliations":[{"id":30783,"text":"Department of Earth Science, University of California, Santa Barbara, CA","active":true,"usgs":false}],"preferred":false,"id":750063,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Covington, Harry R.","contributorId":204408,"corporation":false,"usgs":false,"family":"Covington","given":"Harry","email":"","middleInitial":"R.","affiliations":[{"id":12545,"text":"USGS retired","active":true,"usgs":false}],"preferred":false,"id":733904,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"VanSistine, D. Paco 0000-0003-1166-2547 dvansistine@usgs.gov","orcid":"https://orcid.org/0000-0003-1166-2547","contributorId":191642,"corporation":false,"usgs":true,"family":"VanSistine","given":"D.","email":"dvansistine@usgs.gov","middleInitial":"Paco","affiliations":[{"id":308,"text":"Geology and Environmental Change Science Center","active":false,"usgs":true}],"preferred":false,"id":751318,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70200943,"text":"70200943 - 2018 - Currents, waves and sediment transport around the headland of Pt. Dume, California","interactions":[],"lastModifiedDate":"2018-11-16T16:54:43","indexId":"70200943","displayToPublicDate":"2018-11-16T16:54:41","publicationYear":"2018","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1333,"text":"Continental Shelf Research","active":true,"publicationSubtype":{"id":10}},"title":"Currents, waves and sediment transport around the headland of Pt. Dume, California","docAbstract":"<p><span>Sediment transport&nbsp;past rocky headlands has received less attention compared to transport along beaches. Here we explore, in a field-based study, possible pathways for sediment movement adjacent to Point Dume, a headland in Santa Monica&nbsp;Bay, California. This prominent&nbsp;shoreline feature&nbsp;is a nearly symmetrical, triangular-shaped promontory interior to the Santa Monica&nbsp;</span>Littoral<span>&nbsp;Cell. We collected current, wave, and&nbsp;turbidity&nbsp;data for 74 days during which several wave events occurred, including one associated with a remote&nbsp;hurricane&nbsp;and another generated by the first winter storm of 2014. We also acquired sediment samples to quantify&nbsp;seabed&nbsp;grain-size&nbsp;distributions. Near-bottom currents towards the headland dominated on both of its sides and wave-driven&nbsp;longshore currents&nbsp;in the&nbsp;surf zone&nbsp;were faster on the exposed side. Bed&nbsp;shear stresseswere generated mostly by waves with minor contributions from currents, but both wave-driven and other currents contributed to sediment flux. On the wave-exposed west side of the headland,&nbsp;suspended sediment&nbsp;concentrations correlated with bed stress suggesting local&nbsp;resuspension&nbsp;whereas turbidity levels on the sheltered east side of the headland are more easily explained by advective delivery. Most of the suspended sediment appears to be exported offshore due to flow separation at the apex of the headland but may not move far given that sediment fluxes at moorings offshore of the apex were small. Further, wave-driven sediment flux in the surf zone is unlikely to pass the headland due to the discontinuity in wave forcing that causes longshore transport in different directions on each side of the headland. It is thus unlikely that sand is transported past the headland (specifically in a westerly direction), although some transport of finer fractions may occur offshore in deep water. These findings of minimal sediment flux past Point Dume are consistent with its role as a littoral cell boundary, although more complex multi-stage processes and unusual events may account for some transport at times.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.csr.2018.10.011","usgsCitation":"George, D.A., Largier, J.L., Storlazzi, C.D., Robart, M.J., and Gaylord, B., 2018, Currents, waves and sediment transport around the headland of Pt. Dume, California: Continental Shelf Research, v. 171, p. 63-76, https://doi.org/10.1016/j.csr.2018.10.011.","productDescription":"14 p.","startPage":"63","endPage":"76","ipdsId":"IP-091841","costCenters":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":468242,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1016/j.csr.2018.10.011","text":"Publisher Index Page"},{"id":359531,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Pt. Dume","volume":"171","publishingServiceCenter":{"id":14,"text":"Menlo Park PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5befe5b9e4b045bfcadf7f26","contributors":{"authors":[{"text":"George, Douglas A.","contributorId":60328,"corporation":false,"usgs":true,"family":"George","given":"Douglas","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":751417,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Largier, John L.","contributorId":175121,"corporation":false,"usgs":false,"family":"Largier","given":"John","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":751418,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Storlazzi, Curt D. 0000-0001-8057-4490 cstorlazzi@usgs.gov","orcid":"https://orcid.org/0000-0001-8057-4490","contributorId":140584,"corporation":false,"usgs":true,"family":"Storlazzi","given":"Curt","email":"cstorlazzi@usgs.gov","middleInitial":"D.","affiliations":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true},{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":751416,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Robart, Matthew J.","contributorId":210665,"corporation":false,"usgs":false,"family":"Robart","given":"Matthew","email":"","middleInitial":"J.","affiliations":[{"id":38129,"text":"UCD/BML","active":true,"usgs":false}],"preferred":false,"id":751419,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Gaylord, Brian","contributorId":210666,"corporation":false,"usgs":false,"family":"Gaylord","given":"Brian","email":"","affiliations":[{"id":38129,"text":"UCD/BML","active":true,"usgs":false}],"preferred":false,"id":751420,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70198512,"text":"sir20185097 - 2018 - Chemical and isotopic characteristics of methane in groundwater of Ohio, 2016","interactions":[],"lastModifiedDate":"2018-11-19T14:13:05","indexId":"sir20185097","displayToPublicDate":"2018-11-16T16:00:00","publicationYear":"2018","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2018-5097","displayTitle":"Chemical and Isotopic Characteristics of Methane in Groundwater of Ohio, 2016","title":"Chemical and isotopic characteristics of methane in groundwater of Ohio, 2016","docAbstract":"<p>In 2016, the U.S. Geological Survey, in cooperation with the Ohio Water Development Authority, investigated the hydrogeologic setting, chemical and isotopic characteristics, and origin of methane in groundwater of Ohio. Understanding the occurrence and distribution of methane in groundwater is important in terms of public safety because methane in water wells can pose a risk of explosion. In addition, documenting the chemical and isotopic characteristics of methane in groundwater can make an important contribution to future stray gas investigations.</p><p>Water samples were collected from 15 domestic water wells known to produce methane, which were in 12 counties in diverse parts of Ohio. The wells were 75–345 feet deep and tapped a range of aquifer types, including glacial deposits and bedrock of Upper Ordovician, Upper Devonian, Lower Mississippian, and Pennsylvanian ages. Although the hydrogeologic settings were varied, there was a broad similarity among the well sites in that the bedrock was predominantly shale and the glacial deposits were predominantly clay.</p><p>The wells were sampled for dissolved inorganic constituents; dissolved organic carbon; methane and other dissolved gases; stable isotopes (carbon, hydrogen, and oxygen) of methane, water, and dissolved inorganic carbon; and carbon-14 of methane. Gas composition and stable isotopes of methane were used to differentiate thermogenic and microbial methane. The degree of fractionation of hydrogen and carbon isotopes was used to evaluate the pathway of microbial methanogenesis (carbon dioxide [CO<sub>2</sub>] reduction or acetate fermentation) and the effects of secondary processes such as oxidation, mixing, and migration. The concentration of carbon-14 of methane was used to evaluate the relative age of the carbon source.</p><p>The quality of water from the 15 wells differed greatly; water types ranged from CaMgHCO<sub>3</sub> to NaCl, and total dissolved solids concentrations ranged from 318 to 2,940 milligrams per liter (mg/L). Methane concentrations ranged from 1.2 to 120 mg/L. Of the 15 samples, 12 had methane concentrations greater than 28 mg/L, the level that can pose a risk of explosion.</p><p>Of the 15 samples, 12 had chemical and isotopic characteristics or \"signatures\" consistent with microbial methane formed by CO<sub>2</sub> reduction. CO<sub>2</sub> reduction is commonly associated with microbial degradation of organic matter in anaerobic aquifers and with the formation of microbial shale gas and coalbed methane along margins of sedimentary basins. Two of 15 samples were interpreted as having a component of thermogenic methane based on the δ<sup>13</sup>C of methane (−50.96 and −47.74 parts per thousand [per mil]) and gas dryness (28 and 5). One of 15 samples (from the shallowest well) had chemical and isotopic characteristics consistent with methane oxidation by sulfate reduction based on light δ<sup>13</sup>C of dissolved inorganic carbon (−31.6 per mil) and evidence of sulfate reduction in terms of the odor and appearance of the water.</p><p>For the 12 samples interpreted as microbial methane formed by CO<sub>2</sub> reduction, the δ<sup>13</sup>C of methane varied from −75 to −56 per mil. Multiple samples from the same aquifer demonstrated a general trend of increasing δ<sup>13</sup>C of methane with depth. Samples with lighter δ<sup>13</sup>C of methane (−75 to −62 per mil) were from shallower wells (or wells with shallow open intervals), and the isotopic signature of the water was consistent with modern or postglacial groundwater recharge. Three samples with heavier δ<sup>13</sup>C of methane (−61 to −56 per mil) were from deeper wells or more confined aquifers where the isotopic signature of water was consistent with older (glacial) recharge. In addition, δ<sup>13</sup>C of dissolved inorganic carbon was enriched (+12 to +18.9 per mil), and carbon-14 of methane was consistent with carbon associated with Paleozoic bedrock or older glacial deposits. These observations are generally consistent with increased Rayleigh-type fractionation at greater depths; however, other interpretations are possible. Isotopic signatures can be ambiguous, especially in areas with complex geologic histories that include multiple episodes of migration, mixing, and (or) oxidation.</p><p>Many of the wells were in proximity to multiple potential natural and anthropogenic pathways of methane migration; however, it is not possible to determine if the methane in any of the wells is related to human activities based on the chemical and isotopic data collected for this study.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20185097","collaboration":"Prepared in cooperation with the Ohio Water Development Authority","usgsCitation":"Thomas, M.A., 2018, Chemical and isotopic characteristics of methane in groundwater of Ohio, 2016: U.S. Geological Survey Scientific Investigations Report 2018–5097, 42 p., https://doi.org/10.3133/sir20185097.","productDescription":"vi, 42 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 \"}}]}","contact":"<p><a href=\"mailto:dc_oh@usgs.gov\" data-mce-href=\"mailto:dc_oh@usgs.gov\">Director</a>, <a href=\"https://www.usgs.gov/centers/oki-water\" data-mce-href=\"https://www.usgs.gov/centers/oki-water\">Ohio-Kentucky-Indiana Water Science Center</a><br>U.S. Geological Survey<br>6460 Busch Boulevard Ste. 100<br>Columbus, OH 43229-1737</p>","tableOfContents":"<ul><li>Abstract</li><li>Introduction</li><li>Methods of Study&nbsp;</li><li>Characteristics of the Well Network</li><li>Groundwater Quality</li><li>Chemical and Isotopic Characteristics of Methane and Related Constituents</li><li>Interpretation of Methane Origin</li><li>Summary and Conclusions</li><li>References Cited</li></ul>","publishingServiceCenter":{"id":15,"text":"Madison PSC"},"publishedDate":"2018-11-16","noUsgsAuthors":false,"publicationDate":"2018-11-16","publicationStatus":"PW","scienceBaseUri":"5befe5b9e4b045bfcadf7f28","contributors":{"authors":[{"text":"Thomas, Mary Ann 0000-0001-8681-1370 mathomas@usgs.gov","orcid":"https://orcid.org/0000-0001-8681-1370","contributorId":206777,"corporation":false,"usgs":true,"family":"Thomas","given":"Mary Ann","email":"mathomas@usgs.gov","affiliations":[{"id":35860,"text":"Ohio-Kentucky-Indiana Water Science Center","active":true,"usgs":true}],"preferred":true,"id":741734,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70207058,"text":"70207058 - 2018 - Construction of a compact low-cost radiation shield for air-temperature sensors in ecological field studies","interactions":[],"lastModifiedDate":"2019-12-04T15:32:41","indexId":"70207058","displayToPublicDate":"2018-11-16T15:28:11","publicationYear":"2018","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2498,"text":"Journal of Visualized Experiments","active":true,"publicationSubtype":{"id":10}},"title":"Construction of a compact low-cost radiation shield for air-temperature sensors in ecological field studies","docAbstract":"<p><span>With the advent of small, low-cost environmental sensors, it is now possible to deploy high-density networks of sensors to measure hyper localized temperature variation. Here, we provide a detailed methodology for constructing a compact version of a previously described custom-fabricated radiation shield for use with inexpensive thermochrons.</span></p>","language":"English","publisher":"JoVE","doi":"10.3791/58273","usgsCitation":"Terando, A.J., Prado, S.G., and Youngsteadt, E., 2018, Construction of a compact low-cost radiation shield for air-temperature sensors in ecological field studies: Journal of Visualized Experiments, no. 141, e58273, https://doi.org/10.3791/58273.","productDescription":"e58273","ipdsId":"IP-098717","costCenters":[{"id":36940,"text":"National Climate Adaptation Science Center","active":true,"usgs":true}],"links":[{"id":369920,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"issue":"141","noUsgsAuthors":false,"publicationDate":"2018-11-06","publicationStatus":"PW","contributors":{"authors":[{"text":"Terando, Adam J. 0000-0002-9280-043X aterando@usgs.gov","orcid":"https://orcid.org/0000-0002-9280-043X","contributorId":173447,"corporation":false,"usgs":true,"family":"Terando","given":"Adam","email":"aterando@usgs.gov","middleInitial":"J.","affiliations":[{"id":565,"text":"Southeast Climate Science Center","active":true,"usgs":true}],"preferred":true,"id":776664,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Prado, Sara G.","contributorId":204504,"corporation":false,"usgs":false,"family":"Prado","given":"Sara","email":"","middleInitial":"G.","affiliations":[{"id":7091,"text":"North Carolina State University","active":true,"usgs":false}],"preferred":false,"id":776665,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Youngsteadt, Elsa","contributorId":205500,"corporation":false,"usgs":false,"family":"Youngsteadt","given":"Elsa","email":"","affiliations":[{"id":7091,"text":"North Carolina State University","active":true,"usgs":false}],"preferred":false,"id":776666,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70204266,"text":"70204266 - 2018 - Defining blue carbon: The emergence of a climate context for coastal carbon dynamics","interactions":[],"lastModifiedDate":"2019-07-17T12:57:23","indexId":"70204266","displayToPublicDate":"2018-11-16T14:57:39","publicationYear":"2018","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"chapter":"1","title":"Defining blue carbon: The emergence of a climate context for coastal carbon dynamics","docAbstract":"<div class=\"product-details\"><div class=\"chapter-detail-container\"><div class=\"container\"><div class=\"flex-container\"><div class=\"chapter-description-container\"><div class=\"abstract-content\"><p>Blue Carbon Ecosystems (BCEs) are defined as coastal wetland ecosystems with manageable and atmospherically significant carbon stocks and fluxes.</p><p>Policy and management opportunities have promoted the emergence of blue carbon as a concept and spurred scientific interest to reduce uncertainties in coastal carbon budgets.</p><p>The four major BCEs are generally classified by their plant communities: tidal marshes, tidal freshwater forests, mangroves, and seagrass meadows.</p><p><br data-mce-bogus=\"1\"></p></div></div></div></div></div></div>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"A blue carbon primer: The state of coastal wetland carbon science, practice and policy","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Taylor & Francis","doi":"10.1201/9780429435362","usgsCitation":"Crooks, S., Windham-Myers, L., and Tiffany Troxler, 2018, Defining blue carbon: The emergence of a climate context for coastal carbon dynamics, chap. 1 <i>of</i> A blue carbon primer: The state of coastal wetland carbon science, practice and policy, p. 1-8, https://doi.org/10.1201/9780429435362.","productDescription":"8 p.","startPage":"1","endPage":"8","ipdsId":"IP-099272","costCenters":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"links":[{"id":365632,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"publishingServiceCenter":{"id":14,"text":"Menlo Park PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Crooks, Stephen","contributorId":217032,"corporation":false,"usgs":false,"family":"Crooks","given":"Stephen","email":"","affiliations":[{"id":38182,"text":"Silvestrum Climate Associates","active":true,"usgs":false}],"preferred":false,"id":766271,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Windham-Myers, Lisamarie","contributorId":217031,"corporation":false,"usgs":true,"family":"Windham-Myers","given":"Lisamarie","affiliations":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":true,"id":766270,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Tiffany Troxler","contributorId":217029,"corporation":false,"usgs":false,"family":"Tiffany Troxler","affiliations":[{"id":7017,"text":"Florida International University","active":true,"usgs":false}],"preferred":false,"id":766272,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70204267,"text":"70204267 - 2018 - Blue Carbon Futures: moving forward on terra firma","interactions":[],"lastModifiedDate":"2019-07-16T14:54:15","indexId":"70204267","displayToPublicDate":"2018-11-16T14:51:00","publicationYear":"2018","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"chapter":"28","title":"Blue Carbon Futures: moving forward on terra firma","docAbstract":"<p>Maintaining coastal carbon sequestration and storage services is economically valuable in providing a potentially long-term contribution toward climate resilience, both in terms of adaptation and mitigation.</p><p>392The volumetric accumulation of coastal carbon stocks is unique from other terrestrial and aquatic processes, and inconsistent use of terminology is holding back understanding of the range, magnitude, and processes critical to this carbon sink.</p><p>Documenting net greenhouse gas (GHG) benefits of coastal ecosystem management needs integrated models that quantitatively incorporate geomorphic, biogeochemical, atmospheric, and hydrologic exchanges to account for both carbon accumulation and loss, across a range of timescales.</p><p>A community effort is necessary to explore similarities among coastal ecosystems to determine the drivers and scale of true variability, to prioritize specific wetland management options, and develop the most effective monitoring approaches.</p><p>While there are further scientific aspects of blue carbon to be explored, there is sufficient knowledge and experience to advance demonstration projects across a range of systems and conditions, which can inform policy development and scaled implementation.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"A blue carbon primer: The state of coastal wetland carbon science, practice and policy","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Taylor & Francis","doi":"10.1201/9780429435362","usgsCitation":"Windham-Myers, L., Crooks, S., and Tiffany Troxler, 2018, Blue Carbon Futures: moving forward on terra firma, chap. 28 <i>of</i> A blue carbon primer: The state of coastal wetland carbon science, practice and policy, p. 391-402, https://doi.org/10.1201/9780429435362.","productDescription":"11 p.","startPage":"391","endPage":"402","ipdsId":"IP-099273","costCenters":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"links":[{"id":365629,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"publishingServiceCenter":{"id":14,"text":"Menlo Park PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Windham-Myers, Lisamarie","contributorId":217033,"corporation":false,"usgs":true,"family":"Windham-Myers","given":"Lisamarie","affiliations":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":true,"id":766273,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Crooks, Stephen","contributorId":217032,"corporation":false,"usgs":false,"family":"Crooks","given":"Stephen","email":"","affiliations":[{"id":38182,"text":"Silvestrum Climate Associates","active":true,"usgs":false}],"preferred":false,"id":766274,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Tiffany Troxler","contributorId":217029,"corporation":false,"usgs":false,"family":"Tiffany Troxler","affiliations":[{"id":7017,"text":"Florida International University","active":true,"usgs":false}],"preferred":false,"id":766275,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70204497,"text":"70204497 - 2018 - Identification of storm events and contiguous coastal sections for deterministic modeling of extreme coastal flood events in response to climate change","interactions":[],"lastModifiedDate":"2020-12-15T22:35:31.045435","indexId":"70204497","displayToPublicDate":"2018-11-16T14:27:18","publicationYear":"2018","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1262,"text":"Coastal Engineering","active":true,"publicationSubtype":{"id":10}},"title":"Identification of storm events and contiguous coastal sections for deterministic modeling of extreme coastal flood events in response to climate change","docAbstract":"<p>Deterministic dynamical modeling of future climate conditions and associated hazards, such as flooding, can be computationally-expensive if century-long time-series of waves, sea level variations, and overland flow patterns are simulated. To alleviate some of the computational costs, local impacts of individual coastal storms can be explored by first identifying particular events or scenarios of interest and dynamically modeling those events in detail. In this study, an efficient approach to selecting storm events for subsequent deterministic detailed modeling of coastal flooding is presented. The approach identifies locally relevant scenarios derived from regional datasets spanning long time-periods and covering large geographic areas. This is done by identifying storm events from global climate models using a robust, yet computationally simple approach for calculating total water level proxies at the shore, assuming a linear superposition of the important processes contributing to the overall total water level. Clustering of the total water level time-series is used to define coherent coastal cells where similar return period water level extrema occur in response to region-wide storms. Results show that the more severe but rare coastal flood events (e.g., the 100-year (yr) event) typically occur from the same storm across the region, but that a number of different storms are responsible for the less severe but more frequent local extreme water levels (e.g., the 1-yr event). This new ‘storm selection’ approach is applied to the Southern California Bight, a region of varying shoreline orientations that is subject to wave refraction across complex bathymetry, and shadowing, focusing, diffraction, and dissipation of wave energy by islands. Results indicate that wave runup dominates total water level extremes at this study site, highlighting the importance of downscaling global-scale models to nearshore waves when seeking accurate projections of local coastal hazards in response to climate change.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.coastaleng.2018.08.003","usgsCitation":"Erikson, L.H., Espejo, A., Barnard, P., Katherine A. Serafin, Hegermiller, C., O'Neill, A., Ruggerio, P., Limber, P.W., and Mendez, F.J., 2018, Identification of storm events and contiguous coastal sections for deterministic modeling of extreme coastal flood events in response to climate change: Coastal Engineering, v. 140, p. 316-330, https://doi.org/10.1016/j.coastaleng.2018.08.003.","productDescription":"15 p.","startPage":"316","endPage":"330","ipdsId":"IP-077289","costCenters":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":468243,"rank":0,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://doi.org/10.1016/j.coastaleng.2018.08.003","text":"External Repository"},{"id":366001,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Southern California Bight","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -121.2451171875,\n              32.63937487360669\n            ],\n            [\n              -116.5869140625,\n              32.63937487360669\n            ],\n            [\n              -116.5869140625,\n              35.10193405724606\n            ],\n            [\n              -121.2451171875,\n              35.10193405724606\n            ],\n            [\n              -121.2451171875,\n              32.63937487360669\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"140","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Erikson, Li H. 0000-0002-8607-7695 lerikson@usgs.gov","orcid":"https://orcid.org/0000-0002-8607-7695","contributorId":149963,"corporation":false,"usgs":true,"family":"Erikson","given":"Li","email":"lerikson@usgs.gov","middleInitial":"H.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":767253,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Espejo, Antonio","contributorId":217673,"corporation":false,"usgs":false,"family":"Espejo","given":"Antonio","email":"","affiliations":[],"preferred":false,"id":767254,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Barnard, Patrick L. 0000-0003-1414-6476 pbarnard@usgs.gov","orcid":"https://orcid.org/0000-0003-1414-6476","contributorId":147147,"corporation":false,"usgs":true,"family":"Barnard","given":"Patrick L.","email":"pbarnard@usgs.gov","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":767255,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Katherine A. Serafin","contributorId":187534,"corporation":false,"usgs":false,"family":"Katherine A. Serafin","affiliations":[],"preferred":false,"id":767256,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Hegermiller, Christie 0000-0002-6383-7508 chegermiller@usgs.gov","orcid":"https://orcid.org/0000-0002-6383-7508","contributorId":149010,"corporation":false,"usgs":true,"family":"Hegermiller","given":"Christie","email":"chegermiller@usgs.gov","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":767257,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"O'Neill, Andrea C. 0000-0003-1656-4372 aoneill@usgs.gov","orcid":"https://orcid.org/0000-0003-1656-4372","contributorId":5351,"corporation":false,"usgs":true,"family":"O'Neill","given":"Andrea C.","email":"aoneill@usgs.gov","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":767258,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Ruggerio, Peter","contributorId":67403,"corporation":false,"usgs":true,"family":"Ruggerio","given":"Peter","email":"","affiliations":[],"preferred":false,"id":767259,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Limber, Patrick W. 0000-0002-8207-3750 plimber@usgs.gov","orcid":"https://orcid.org/0000-0002-8207-3750","contributorId":196794,"corporation":false,"usgs":true,"family":"Limber","given":"Patrick","email":"plimber@usgs.gov","middleInitial":"W.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":767260,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Mendez, Fernando J.","contributorId":140322,"corporation":false,"usgs":false,"family":"Mendez","given":"Fernando","email":"","middleInitial":"J.","affiliations":[{"id":13456,"text":"IH Cantrabria","active":true,"usgs":false}],"preferred":false,"id":767261,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}}
,{"id":70200699,"text":"70200699 - 2018 - Subsurface controls on the development of the Cape Fear Slide Complex, central US Atlantic Margin","interactions":[],"lastModifiedDate":"2019-10-09T08:37:04","indexId":"70200699","displayToPublicDate":"2018-11-16T13:02:32","publicationYear":"2018","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5011,"text":"Geological Society of London Special Publications","active":true,"publicationSubtype":{"id":10}},"title":"Subsurface controls on the development of the Cape Fear Slide Complex, central US Atlantic Margin","docAbstract":"<p><span>The Cape Fear Slide is one of the largest (&gt;25 000 km</span><sup>3</sup><span>) submarine slope failure complexes on the US Atlantic margin. Here we use a combination of new high-resolution multichannel seismic data (MCS) from the National Science Foundation Geodynamic Processes at Rifting and Subducting Margins (NSF GeoPRISMS) Community Seismic Experiment and legacy industry MCS to derive detailed stratigraphy of this slide and constrain the conditions that lead to slope instability. Limited outer-shelf and upper-slope accommodation space during the Neogene, combined with lowstand fluvial inputs and northwards Gulf Stream sediment transport, appears to have contributed to thick Miocene and Pliocene deposits that onlapped the lower slope. This resulted in burial of an upper-slope bypass zone developed from earlier erosional truncation of Paleogene strata. These deposits created a broad ramp that allowed accumulation of thick Quaternary strata across a low-gradient (&lt;3.5°) upper slope. Upslope of one of the larger headwalls, undulating Quaternary strata appear to downlap onto a buried failure plane. Many of the nested headwalls of the upper-slope portion of slide complex are underlain by deformed strata, which may be the result of fluid migration associated with localized subsidence from salt migration. These new data and observations suggest that antecedent margin physiography, sediment loading and substrate fluid flow were key factors in preconditioning the Cape Fear slope for failure.</span></p>","language":"English","publisher":"Geological Society of London","doi":"10.1144/SP477.17","usgsCitation":"Hill, J.C., Brothers, D., Hornbach, M.J., Sawyer, D.E., Shillington, D.J., and Becel, A., 2018, Subsurface controls on the development of the Cape Fear Slide Complex, central US Atlantic Margin: Geological Society of London Special Publications, v. 477, p. 169-182, https://doi.org/10.1144/SP477.17.","productDescription":"14 p.","startPage":"169","endPage":"182","ipdsId":"IP-089531","costCenters":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":359515,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","volume":"477","publishingServiceCenter":{"id":14,"text":"Menlo Park PSC"},"noUsgsAuthors":false,"publicationDate":"2018-03-28","publicationStatus":"PW","scienceBaseUri":"5befe5bae4b045bfcadf7f2a","contributors":{"authors":[{"text":"Hill, Jenna C. 0000-0002-7475-357X","orcid":"https://orcid.org/0000-0002-7475-357X","contributorId":21987,"corporation":false,"usgs":true,"family":"Hill","given":"Jenna","email":"","middleInitial":"C.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":750155,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brothers, Daniel S. 0000-0001-7702-157X","orcid":"https://orcid.org/0000-0001-7702-157X","contributorId":210199,"corporation":false,"usgs":true,"family":"Brothers","given":"Daniel S.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":750156,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hornbach, Matthew J.","contributorId":210200,"corporation":false,"usgs":false,"family":"Hornbach","given":"Matthew","email":"","middleInitial":"J.","affiliations":[{"id":20300,"text":"Southern Methodist University","active":true,"usgs":false}],"preferred":false,"id":750157,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Sawyer, Derek E.","contributorId":210201,"corporation":false,"usgs":false,"family":"Sawyer","given":"Derek","email":"","middleInitial":"E.","affiliations":[{"id":18155,"text":"The Ohio State University","active":true,"usgs":false}],"preferred":false,"id":750158,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Shillington, Donna J.","contributorId":210202,"corporation":false,"usgs":false,"family":"Shillington","given":"Donna","email":"","middleInitial":"J.","affiliations":[{"id":38091,"text":"Lamont Doherty Earth Observatory, Columbia University","active":true,"usgs":false}],"preferred":false,"id":750159,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Becel, Anne","contributorId":210203,"corporation":false,"usgs":false,"family":"Becel","given":"Anne","email":"","affiliations":[{"id":38091,"text":"Lamont Doherty Earth Observatory, Columbia University","active":true,"usgs":false}],"preferred":false,"id":750160,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70201041,"text":"70201041 - 2018 - American Recent Eulipotyphla: Nesophontids, Solenodons, Moles, and Shrews in the New World","interactions":[],"lastModifiedDate":"2018-11-26T11:50:23","indexId":"70201041","displayToPublicDate":"2018-11-16T11:50:13","publicationYear":"2018","noYear":false,"publicationType":{"id":4,"text":"Book"},"title":"American Recent Eulipotyphla: Nesophontids, Solenodons, Moles, and Shrews in the New World","docAbstract":"The mammalian taxonomic order Eulipotyphla is comprised of the living taxonomic families Erinaceidae (gymnures, hedgehogs, and moonrats), Solenodontidae (solenodonts), Soricidae (shrews), and Talpidae (desmans and moles).  Morphological and molecular studies continue to alter our view of relationships within and among these families, and this research has added considerably to our understanding of the diversity, distributions, and relationships of many of the New World species that belong to them. Currently, there are more than 450 recognized living species worldwide, making the Eulipotyphla the third most speciose order of mammals. New World (North and South America and associated islands) eulipotyphlans currently include 110 recognized species of shrews, seven species of moles, and both living species of solenodons.  In this work, I attempt to summarize the taxonomic results of recent studies and provide a guide to the most appropriate current applications of taxonomic names in this region.","language":"English","publisher":"Smithsonian Institute Scholarly Press","doi":"10.5479/si.1943-6696.650","usgsCitation":"Woodman, N., 2018, American Recent Eulipotyphla: Nesophontids, Solenodons, Moles, and Shrews in the New World, v. 650, vi, 107 p., https://doi.org/10.5479/si.1943-6696.650.","productDescription":"vi, 107 p.","ipdsId":"IP-097553","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":359655,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"650","publishingServiceCenter":{"id":10,"text":"Baltimore PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5bfd146ee4b0815414ca38f0","contributors":{"authors":[{"text":"Woodman, Neal 0000-0003-2689-7373 nwoodman@usgs.gov","orcid":"https://orcid.org/0000-0003-2689-7373","contributorId":3547,"corporation":false,"usgs":true,"family":"Woodman","given":"Neal","email":"nwoodman@usgs.gov","affiliations":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"preferred":true,"id":751971,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70200934,"text":"70200934 - 2018 - The influence of seep habitats on sediment macrofaunal biodiversity and functional traits","interactions":[],"lastModifiedDate":"2018-12-05T14:05:19","indexId":"70200934","displayToPublicDate":"2018-11-16T11:21:28","publicationYear":"2018","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1370,"text":"Deep-Sea Research Part I: Oceanographic Research Papers","active":true,"publicationSubtype":{"id":10}},"title":"The influence of seep habitats on sediment macrofaunal biodiversity and functional traits","docAbstract":"<p><span>Chemosynthetic ecosystems in the Gulf of Mexico (GOM) support dense communities of seep megafaunal&nbsp;invertebrates&nbsp;that rely on endosymbiotic bacteria for nutrition. Distinct infaunal communities are associated with the&nbsp;biogenic&nbsp;habitats created by seep biota, where habitat heterogeneity and sediment&nbsp;geochemistry&nbsp;influence local macrofaunal community structure. Here we examine the community structure and function of seep infaunal communities in the GOM in relation to environmental drivers and estimated proximity to seeps. We modeled seep distribution within 3 major seep fields (AC601, GC852, and AT340), and examined the influence of proximity to seep and associated sediment environment on infaunal community structure and function. To model seep habitat distribution, we used known seep occurrence data from&nbsp;ROV&nbsp;and towed camera images, terrain variables derived from high resolution multibeam&nbsp;bathymetry&nbsp;(gridded to 3 m resolution), and a maximum&nbsp;entropy&nbsp;(Maxent) approach. Model performance was high, with mean area under the curve for each habitat ranging from 0.851 for mussel to 0.908 for&nbsp;</span>tubeworm<span>&nbsp;habitat, with the models highly influenced by terrain&nbsp;rugosity. Replicate&nbsp;sediment cores&nbsp;were collected from the three sites in 2007 and processed for&nbsp;macrofauna&nbsp;and environmental characteristics. A majority of the taxa (86%) occurred within 16 m of modeled seep habitat and increased distance from modeled seeps was generally associated with lower calculated seep index coupled with decreased macrofaunal densities. Distance-based linear regression indicated that patterns in macrofaunal communities were driven by proximity to modeled seep habitat and profile curvature, a metric for the shape of the maximum slope. Similarly, variance in infaunal functional traits was best explained by proximity to seep, but also sediment C:N, reflecting the relative influence of&nbsp;sediment chemistry, including organic content, on infaunal communities. Results suggest that northern GOM seep infaunal community assemblages and their function are structured by factors that influence&nbsp;food availability&nbsp;and habitat heterogeneity. Given the abundance of seeps in the GOM and in the world’s oceans, this study supports the premise that the sphere of influence of seeps is spatially extensive.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.dsr.2018.10.004","usgsCitation":"Demopoulos, A.W., Bourque, J.R., Durkin, A., and Cordes, E.E., 2018, The influence of seep habitats on sediment macrofaunal biodiversity and functional traits: Deep-Sea Research Part I: Oceanographic Research Papers, v. 142, p. 77-93, https://doi.org/10.1016/j.dsr.2018.10.004.","productDescription":"17 p.","startPage":"77","endPage":"93","ipdsId":"IP-092914","costCenters":[{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"links":[{"id":468244,"rank":1,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1016/j.dsr.2018.10.004","text":"Publisher Index Page"},{"id":437683,"rank":0,"type":{"id":30,"text":"Data Release"},"url":"https://doi.org/10.5066/F7FB524M","text":"USGS data release","linkHelpText":"The influence of hydrocarbon seeps on sediment macrofaunal biodiversity and functional traits"},{"id":359513,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Gulf of Mexico","volume":"142","publishingServiceCenter":{"id":5,"text":"Lafayette PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5befe5bae4b045bfcadf7f2c","contributors":{"authors":[{"text":"Demopoulos, Amanda W. J. 0000-0003-2096-4694","orcid":"https://orcid.org/0000-0003-2096-4694","contributorId":206536,"corporation":false,"usgs":true,"family":"Demopoulos","given":"Amanda","email":"","middleInitial":"W. J.","affiliations":[{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"preferred":true,"id":751380,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bourque, Jill R. 0000-0003-3809-2601 jbourque@usgs.gov","orcid":"https://orcid.org/0000-0003-3809-2601","contributorId":5452,"corporation":false,"usgs":true,"family":"Bourque","given":"Jill","email":"jbourque@usgs.gov","middleInitial":"R.","affiliations":[{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"preferred":true,"id":751381,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Durkin, Alanna","contributorId":210654,"corporation":false,"usgs":false,"family":"Durkin","given":"Alanna","email":"","affiliations":[{"id":12547,"text":"Temple University","active":true,"usgs":false}],"preferred":false,"id":751382,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Cordes, Erik E.","contributorId":37623,"corporation":false,"usgs":false,"family":"Cordes","given":"Erik","email":"","middleInitial":"E.","affiliations":[{"id":16710,"text":"Temple University, Department of Biology","active":true,"usgs":false}],"preferred":false,"id":751383,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70204947,"text":"70204947 - 2018 - Integrated observations and informatics improve understanding of changing marine ecosystems","interactions":[],"lastModifiedDate":"2019-08-26T10:55:19","indexId":"70204947","displayToPublicDate":"2018-11-16T10:45:09","publicationYear":"2018","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3912,"text":"Frontiers in Marine Science","onlineIssn":"2296-7745","active":true,"publicationSubtype":{"id":10}},"title":"Integrated observations and informatics improve understanding of changing marine ecosystems","docAbstract":"<p><span>Marine ecosystems have numerous benefits for human societies around the world and many policy initiatives now seek to maintain the health of these ecosystems. To enable wise decisions, up to date and accurate information on marine species and the state of the environment they live in is required. Moreover, this information needs to be openly accessible to build indicators and conduct timely assessments that decision makers can use. The questions and problems being addressed demand global-scale investigations, transdisciplinary science, and mechanisms to integrate and distribute data that otherwise would appear to be disparate. Essential Ocean Variables (EOVs) and marine Essential Biodiversity Variables (EBVs), conceptualized by the Global Ocean Observing System (GOOS) and the Marine Biodiversity Observation Network (MBON), respectively, guide observation of the ocean. Additionally, significant progress has been made to coordinate efforts between existing programs, such as the GOOS, MBON, and Ocean Biogeographic Information System collaboration agreement. Globally and nationally relevant indicators and assessments require increased sharing of data and analytical methods, sustained long-term and large-scale observations, and resources to dedicated to these tasks. We propose a vision and key tenets as a guiding framework for building a global integrated system for understanding marine biological diversity and processes to address policy and resource management needs. This framework includes: using EOVs and EBVs and implementing the guiding principles of Findable, Accessible, Interoperable, Reusable (FAIR) data and action ecology. In doing so, we can encourage relevant, rapid, and integrative scientific advancement that can be implemented by decision makers to maintain marine ecosystem health.</span></p>","language":"English","publisher":"Frontiers Media","doi":"10.3389/fmars.2018.00428","usgsCitation":"Benson, A.L., Brooks, C.M., Canonico, G., Duffy, J.E., Muller-Karger, F., Sosik, H.M., Miloslavich, P., and Klein, E., 2018, Integrated observations and informatics improve understanding of changing marine ecosystems: Frontiers in Marine Science, v. 5, 428, 8 p., https://doi.org/10.3389/fmars.2018.00428.","productDescription":"428, 8 p.","ipdsId":"IP-100471","costCenters":[{"id":208,"text":"Core Science Analytics and Synthesis","active":true,"usgs":true}],"links":[{"id":468245,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.3389/fmars.2018.00428","text":"Publisher Index Page"},{"id":366906,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"5","noUsgsAuthors":false,"publicationDate":"2018-11-16","publicationStatus":"PW","contributors":{"authors":[{"text":"Benson, Abigail L. 0000-0002-4391-107X albenson@usgs.gov","orcid":"https://orcid.org/0000-0002-4391-107X","contributorId":4562,"corporation":false,"usgs":true,"family":"Benson","given":"Abigail","email":"albenson@usgs.gov","middleInitial":"L.","affiliations":[{"id":208,"text":"Core Science Analytics and Synthesis","active":true,"usgs":true}],"preferred":true,"id":769213,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brooks, Cassandra M.","contributorId":218423,"corporation":false,"usgs":false,"family":"Brooks","given":"Cassandra","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":769214,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Canonico, Gabrielle","contributorId":217563,"corporation":false,"usgs":false,"family":"Canonico","given":"Gabrielle","email":"","affiliations":[{"id":39659,"text":"National Oceanographic and Atmospheric Administration, US Integrated Ocean Observing System, Silver Spring, MD, USA","active":true,"usgs":false}],"preferred":false,"id":769215,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Duffy, J. Emmett","contributorId":78186,"corporation":false,"usgs":true,"family":"Duffy","given":"J.","email":"","middleInitial":"Emmett","affiliations":[],"preferred":false,"id":769216,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Muller-Karger, Frank","contributorId":218424,"corporation":false,"usgs":false,"family":"Muller-Karger","given":"Frank","affiliations":[],"preferred":false,"id":769217,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Sosik, Heidi M.","contributorId":218425,"corporation":false,"usgs":false,"family":"Sosik","given":"Heidi","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":769218,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Miloslavich, Patricia","contributorId":206627,"corporation":false,"usgs":false,"family":"Miloslavich","given":"Patricia","email":"","affiliations":[{"id":37357,"text":"University of Tasmania, Hobart, Tasmania, Australia","active":true,"usgs":false}],"preferred":false,"id":769219,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Klein, Eduardo","contributorId":206675,"corporation":false,"usgs":false,"family":"Klein","given":"Eduardo","email":"","affiliations":[],"preferred":false,"id":769220,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":70216314,"text":"70216314 - 2018 - Degradation of 100‐m‐scale rocky ejecta craters at the InSight Landing Site on Mars and implications for surface processes and erosion rates in the hesperian and amazonian","interactions":[],"lastModifiedDate":"2020-11-11T15:38:23.698218","indexId":"70216314","displayToPublicDate":"2018-11-16T09:36:39","publicationYear":"2018","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":7353,"text":"Journal of Geophysical Research - Planets","active":true,"publicationSubtype":{"id":10}},"title":"Degradation of 100‐m‐scale rocky ejecta craters at the InSight Landing Site on Mars and implications for surface processes and erosion rates in the hesperian and amazonian","docAbstract":"<div class=\"article-section__content en main\"><p>Rocky ejecta craters (RECs) at the Interior Exploration using Seismic Investigations, Geodesy and Heat Transport (InSight) landing site on Elysium Planitia, Mars, provide constraints on crater modification and rates for the Hesperian and Amazonian. The RECs are between 10&nbsp;m and 1.2&nbsp;km in diameter and exhibit five classes of preservation. Class 1 represents pristine craters with sharp rims and abundant ejected rocks. From Classes 2 to 5, rims become more subdued, craters are infilled, and the ejecta become discontinuously distributed. High‐Resolution Imaging Science Experiment digital elevation models indicate a maximum depth to diameter ratio of ~0.15, which is lower than pristine models for craters of similar size. The low ratio is related to the presence of a loosely consolidated regolith and early‐stage eolian infill. Rim heights have an average height to diameter ratio of ~0.03 for the most pristine class. The size‐frequency distribution of RECs, plotted using cumulative and differential methods, indicates that crater classes within the diameter range of 200&nbsp;m to 1.2&nbsp;km are separated by ~100 to 200&nbsp;Myr. Smaller craters degrade faster, with classes separated by &lt;100&nbsp;Myr. Rim erosion can be entirely modeled by nonlinear diffusional processes using the calculated timescales and a constant diffusivity of 8&nbsp;×&nbsp;10<sup>−7</sup>&nbsp;m<sup>2</sup>/year for craters 200 to 500&nbsp;m in diameter. Diffusion models only partly capture depth‐related degradation, which requires eolian infill. Depth degradation and rim erosion rates are 10<sup>−2</sup><span>&nbsp;</span>to 10<sup>−3</sup>&nbsp;m/Myr, respectively. The rates are consistent with relatively slow modification that is typical of the last two epochs of Martian history.</p></div>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/2018JE005618","usgsCitation":"Sweeney, J., Warner, N.H., Ganti, V., Golombek, M.P., Lamb, M.P., Fergason, R.L., and Kirk, R.L., 2018, Degradation of 100‐m‐scale rocky ejecta craters at the InSight Landing Site on Mars and implications for surface processes and erosion rates in the hesperian and amazonian: Journal of Geophysical Research - Planets, v. 123, no. 10, p. 2732-2759, https://doi.org/10.1029/2018JE005618.","productDescription":"28 p.","startPage":"2732","endPage":"2759","ipdsId":"IP-097429","costCenters":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"links":[{"id":468246,"rank":0,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://doi.org/10.1029/2018je005618","text":"External Repository"},{"id":380417,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"123","issue":"10","noUsgsAuthors":false,"publicationDate":"2018-10-23","publicationStatus":"PW","contributors":{"authors":[{"text":"Sweeney, J.","contributorId":196344,"corporation":false,"usgs":false,"family":"Sweeney","given":"J.","email":"","affiliations":[],"preferred":false,"id":804642,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Warner, N. H","contributorId":244804,"corporation":false,"usgs":false,"family":"Warner","given":"N.","email":"","middleInitial":"H","affiliations":[{"id":48982,"text":"Department of Geological Sciences, State University of New York at Geneseo","active":true,"usgs":false}],"preferred":false,"id":804643,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ganti, V.","contributorId":167364,"corporation":false,"usgs":false,"family":"Ganti","given":"V.","email":"","affiliations":[{"id":13711,"text":"Caltech","active":true,"usgs":false}],"preferred":false,"id":804644,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Golombek, Matthew P.","contributorId":175450,"corporation":false,"usgs":false,"family":"Golombek","given":"Matthew","email":"","middleInitial":"P.","affiliations":[{"id":7023,"text":"Jet Propulsion Laboratory, California Institute of Technology","active":true,"usgs":false}],"preferred":false,"id":804645,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Lamb, M. P.","contributorId":172652,"corporation":false,"usgs":false,"family":"Lamb","given":"M.","email":"","middleInitial":"P.","affiliations":[{"id":13711,"text":"Caltech","active":true,"usgs":false}],"preferred":false,"id":804646,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Fergason, Robin L. 0000-0002-2044-1714","orcid":"https://orcid.org/0000-0002-2044-1714","contributorId":206167,"corporation":false,"usgs":true,"family":"Fergason","given":"Robin","email":"","middleInitial":"L.","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":true,"id":804648,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Kirk, Randolph L. 0000-0003-0842-9226 rkirk@usgs.gov","orcid":"https://orcid.org/0000-0003-0842-9226","contributorId":2765,"corporation":false,"usgs":true,"family":"Kirk","given":"Randolph","email":"rkirk@usgs.gov","middleInitial":"L.","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":true,"id":804647,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70254571,"text":"70254571 - 2018 - Calibration of regional hydraulic and transport properties of an arid-region aquifer under modern and paleorecharge conditions using water levels and environmental tracers","interactions":[],"lastModifiedDate":"2024-06-03T11:44:55.821178","indexId":"70254571","displayToPublicDate":"2018-11-16T06:41:59","publicationYear":"2018","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1923,"text":"Hydrogeology Journal","active":true,"publicationSubtype":{"id":10}},"title":"Calibration of regional hydraulic and transport properties of an arid-region aquifer under modern and paleorecharge conditions using water levels and environmental tracers","docAbstract":"<div id=\"Abs1-section\" class=\"c-article-section\"><div id=\"Abs1-content\" class=\"c-article-section__content\"><p>A two-dimensional numerical groundwater flow model was established and calibrated for the hyperarid Najd region in southern Oman. The results indicate that recent recharge rates are required to sustain the observed groundwater heads in the Najd. The model was also used to estimate possible ranges of past recharge rates and the effective porosity of the main aquifer unit. Recharge rates during past humid periods were estimated to be no more than 1–3 times modern rates. The effective porosity was estimated to be between 0.06 and 0.093. Insight into the nature of the long-term transport within the aquifer was gained by using transient model runs over the last 350&nbsp;ka and (1) varying the recharge intensity (from 0.1 to 2.5 times modern), and (2) the timing and duration of humid and dry periods. Finally, results indicate that although recharge rates and the flow conditions have likely changed over time, a steady-state model is capable of reproducing the observed groundwater residence times in the Najd based on carbon-14, helium and chlorine-36 dating.</p></div></div><div id=\"Abs2-section\" class=\"c-article-section\"><br></div>","language":"English","publisher":"Springer","doi":"10.1007/s10040-018-1894-z","usgsCitation":"Muller, T., and Sanford, W.E., 2018, Calibration of regional hydraulic and transport properties of an arid-region aquifer under modern and paleorecharge conditions using water levels and environmental tracers: Hydrogeology Journal, v. 27, no. 2, p. 685-701, https://doi.org/10.1007/s10040-018-1894-z.","productDescription":"17 p.","startPage":"685","endPage":"701","ipdsId":"IP-099686","costCenters":[{"id":37778,"text":"WMA - Integrated Modeling and Prediction Division","active":true,"usgs":true}],"links":[{"id":429442,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Oman","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"MultiPolygon\",\"coordinates\":[[[[58.86114,21.11403],[58.48799,20.42899],[58.03432,20.48144],[57.82637,20.243],[57.66576,19.736],[57.7887,19.06757],[57.69439,18.94471],[57.23426,18.94799],[56.60965,18.57427],[56.51219,18.08711],[56.28352,17.87607],[55.66149,17.88413],[55.26994,17.63231],[55.2749,17.22835],[54.791,16.9507],[54.23925,17.04498],[53.57051,16.70766],[53.10857,16.65105],[52.78218,17.34974],[52.00001,19],[54.99998,19.99999],[55.66666,22],[55.20834,22.70833],[55.23449,23.11099],[55.52584,23.52487],[55.52863,23.9336],[55.98121,24.13054],[55.80412,24.2696],[55.88623,24.92083],[56.39685,24.92473],[56.84514,24.24167],[57.40345,23.87859],[58.13695,23.74793],[58.72921,23.56567],[59.1805,22.9924],[59.4501,22.66027],[59.80806,22.53361],[59.80615,22.31052],[59.44219,21.71454],[59.28241,21.43389],[58.86114,21.11403]]],[[[56.39142,25.89599],[56.26104,25.71461],[56.07082,26.05546],[56.36202,26.39593],[56.48568,26.30912],[56.39142,25.89599]]]]},\"properties\":{\"name\":\"Oman\"}}]}","volume":"27","issue":"2","noUsgsAuthors":false,"publicationDate":"2018-11-16","publicationStatus":"PW","contributors":{"authors":[{"text":"Muller, Thomas","contributorId":337080,"corporation":false,"usgs":false,"family":"Muller","given":"Thomas","email":"","affiliations":[{"id":80964,"text":"Department of Hydrogeology, Helmhoz-Centre for Environmental Research","active":true,"usgs":false}],"preferred":false,"id":901928,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sanford, Ward E. 0000-0002-6624-0280 wsanford@usgs.gov","orcid":"https://orcid.org/0000-0002-6624-0280","contributorId":2268,"corporation":false,"usgs":true,"family":"Sanford","given":"Ward","email":"wsanford@usgs.gov","middleInitial":"E.","affiliations":[{"id":37778,"text":"WMA - Integrated Modeling and Prediction Division","active":true,"usgs":true},{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":901929,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70202341,"text":"70202341 - 2018 - Do we know how much fluvial sediment reaches the sea? Decreased river monitoring of U.S. coastal rivers","interactions":[],"lastModifiedDate":"2019-02-22T16:53:40","indexId":"70202341","displayToPublicDate":"2018-11-15T16:53:35","publicationYear":"2018","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1924,"text":"Hydrological Processes","active":true,"publicationSubtype":{"id":10}},"title":"Do we know how much fluvial sediment reaches the sea? Decreased river monitoring of U.S. coastal rivers","docAbstract":"Given the present and future changing climate and human changes to land use and river control, river sediment fluxes to coastal systems are changing and will continue to change in the future.  To delineate these changes and their effects, it is increasingly important to document the fluxes of river-borne sediment discharged to the sea.  Unfortunately, broad-scale river sediment monitoring programs established more than 50 years ago in the U.S. have diminished substantially and now focus principally on the largest rivers and estuaries.  Unless addressed, these data gaps will provide significant challenges in addressing fundamental scientific and management questions about the effects of climate change and sea-level rise in our estuaries and on our coasts.","language":"English","publisher":"Wiley","doi":"10.1002/hyp.13276","usgsCitation":"Warrick, J.A., and Milliman, J.D., 2018, Do we know how much fluvial sediment reaches the sea? Decreased river monitoring of U.S. coastal rivers: Hydrological Processes, v. 32, no. 23, p. 3561-3567, https://doi.org/10.1002/hyp.13276.","productDescription":"7 p.","startPage":"3561","endPage":"3567","ipdsId":"IP-092050","costCenters":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":468247,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1002/hyp.13276","text":"Publisher Index Page"},{"id":361482,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"32","issue":"23","publishingServiceCenter":{"id":14,"text":"Menlo Park PSC"},"noUsgsAuthors":false,"publicationDate":"2018-10-11","publicationStatus":"PW","contributors":{"authors":[{"text":"Warrick, Jonathan A. 0000-0002-0205-3814 jwarrick@usgs.gov","orcid":"https://orcid.org/0000-0002-0205-3814","contributorId":167736,"corporation":false,"usgs":true,"family":"Warrick","given":"Jonathan","email":"jwarrick@usgs.gov","middleInitial":"A.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":757911,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Milliman, John D.","contributorId":213518,"corporation":false,"usgs":false,"family":"Milliman","given":"John","email":"","middleInitial":"D.","affiliations":[{"id":38770,"text":"College of William and Mary, Virginia Institute of Marine Science","active":true,"usgs":false}],"preferred":false,"id":757912,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70202368,"text":"70202368 - 2018 - Effect of heat and singeing on stable hydrogen isotope ratios of bird feathers and implications for their use in determining geographic origin","interactions":[],"lastModifiedDate":"2019-02-26T14:44:31","indexId":"70202368","displayToPublicDate":"2018-11-15T14:44:24","publicationYear":"2018","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3233,"text":"Rapid Communications in Mass Spectrometry","active":true,"publicationSubtype":{"id":10}},"title":"Effect of heat and singeing on stable hydrogen isotope ratios of bird feathers and implications for their use in determining geographic origin","docAbstract":"<div id=\"rcm8253-sec-0001\" class=\"article-section__content\"><p class=\"article-section__sub-title section1\"><strong>Rationale</strong></p><p>Stable hydrogen isotope (<i>δ</i><sup>2</sup>H) ratios of animal tissues are useful for assessing movement and geographic origin of mobile organisms. However, it is uncertain whether heat and singeing affects feather<span>&nbsp;</span><i>δ</i><sup>2</sup>H values and thus subsequent geographic assignments. This is relevant for birds of conservation interest that are burned and killed at concentrating solar‐energy facilities that reflect sunlight to a receiving tower and generate a solar flux field.</p></div><div id=\"rcm8253-sec-0002\" class=\"article-section__content\"><p class=\"article-section__sub-title section1\"><strong>Methods</strong></p><p>We used a controlled experiment to test the effect of known heat loads (exposure to 200, 250 or 300°C for 1 min) on the morphology and<span>&nbsp;</span><i>δ</i><sup>2</sup>H values of feathers from two songbird species. Subsequently, we examined the effects of singeing on<span>&nbsp;</span><i>δ</i><sup>2</sup>H values of feathers from three other songbird species that were found dead in the field at a concentrating solar‐energy facility.</p></div><div id=\"rcm8253-sec-0003\" class=\"article-section__content\"><p class=\"article-section__sub-title section1\"><strong>Results</strong></p><p>Relative to control samples, heating caused visual morphological changes to feathers, including shriveling at 250°C and charring at 300°C. The<span>&nbsp;</span><i>δ</i><sup>2</sup>H values significantly declined by a mean of 27.8‰ in experimental samples exposed to 300°C. There was no statistically detectable difference between<span>&nbsp;</span><i>δ</i><sup>2</sup>H values of the singed and unsinged portions of field‐collected feathers from the same bird.</p></div><div id=\"rcm8253-sec-0004\" class=\"article-section__content\"><p class=\"article-section__sub-title section1\"><strong>Conclusions</strong></p><p>Limited singeing that did not dramatically alter the feather morphology did not substantially affect<span>&nbsp;</span><i>δ</i><sup>2</sup>H values of feathers from these songbirds. However, higher temperatures induced charring and reduced<span>&nbsp;</span><i>δ</i><sup>2</sup>H values. Therefore, severely charred feathers should be avoided when selecting feathers for<span>&nbsp;</span><i>δ</i><sup>2</sup>H‐based assessment of geographic origin.</p></div>","language":"English","publisher":"Wiley","doi":"10.1002/rcm.8253","usgsCitation":"Vander Zanden, H.B., Reid, A., Katzner, T., and Nelson, D.M., 2018, Effect of heat and singeing on stable hydrogen isotope ratios of bird feathers and implications for their use in determining geographic origin: Rapid Communications in Mass Spectrometry, v. 32, no. 21, p. 1859-1866, https://doi.org/10.1002/rcm.8253.","productDescription":"8 p.","startPage":"1859","endPage":"1866","ipdsId":"IP-097643","costCenters":[{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true}],"links":[{"id":361557,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"32","issue":"21","publishingServiceCenter":{"id":12,"text":"Tacoma PSC"},"noUsgsAuthors":false,"publicationDate":"2018-09-25","publicationStatus":"PW","contributors":{"authors":[{"text":"Vander Zanden, Hannah B.","contributorId":138885,"corporation":false,"usgs":false,"family":"Vander Zanden","given":"Hannah","email":"","middleInitial":"B.","affiliations":[{"id":12562,"text":"Department of Geology and Geophysics, University of Utah; Archie Carr Center for Sea Turtle Research, University of Florida","active":true,"usgs":false}],"preferred":false,"id":758044,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reid, Abigail","contributorId":213574,"corporation":false,"usgs":false,"family":"Reid","given":"Abigail","email":"","affiliations":[{"id":38801,"text":"Pawling High School","active":true,"usgs":false}],"preferred":false,"id":758045,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Katzner, Todd E. 0000-0003-4503-8435 tkatzner@usgs.gov","orcid":"https://orcid.org/0000-0003-4503-8435","contributorId":191353,"corporation":false,"usgs":true,"family":"Katzner","given":"Todd E.","email":"tkatzner@usgs.gov","affiliations":[{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true}],"preferred":true,"id":758043,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Nelson, David M.","contributorId":175098,"corporation":false,"usgs":false,"family":"Nelson","given":"David","email":"","middleInitial":"M.","affiliations":[{"id":13479,"text":"University of Maryland Center for Environmental Science, Appalachian Laboratory,  301 Braddock Road, Frostburg, Maryland","active":true,"usgs":false}],"preferred":false,"id":758046,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70200816,"text":"fs20183061 - 2018 - Unmanned aerial systems capabilities of the U.S. Geological Survey Woods Hole Coastal and Marine Science Center","interactions":[],"lastModifiedDate":"2018-11-20T11:18:54","indexId":"fs20183061","displayToPublicDate":"2018-11-15T14:30:00","publicationYear":"2018","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2018-3061","displayTitle":"Unmanned Aerial Systems Capabilities of the U.S. Geological Survey Woods Hole Coastal and Marine Science Center","title":"Unmanned aerial systems capabilities of the U.S. Geological Survey Woods Hole Coastal and Marine Science Center","docAbstract":"<p>Unmanned aerial system (UAS) technology provides a rapid and low-cost solution for mapping coastal environments and assessing short- and long-term changes. The interdisciplinary nature of the data collected and the breadth of applications make UAS technology applicable to multiple scientific investigations. The Aerial Imaging and Mapping (AIM) group at the U.S. Geological Survey (USGS) Woods Hole Coastal and Marine Science Center provides UAS services to scientists to advance the science mission of the Coastal-Marine Hazards and Resources Program. Scientists at the Woods Hole Coastal and Marine Science Center use UASs to acquire imagery of coastal and wetland environments, which is then used to produce detailed topographic and visual reflectance datasets. UAS technology supports the work of geologists, engineers, physical scientists, geographers, and geochemists who study coastal erosion, sediment transport, storm impacts, habitats, biomass, and marsh stability.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/fs20183061","usgsCitation":"Brosnahan, S., and Sherwood, C., 2018, Unmanned aerial systems capabilities of the U.S. Geological Survey Woods Hole Coastal and Marine Science Center: U.S. Geological Survey Fact Sheet 2018–3061, 2 p., https://doi.org/10.3133/fs20183061.","productDescription":"2 p.","onlineOnly":"Y","additionalOnlineFiles":"N","ipdsId":"IP-098218","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":359425,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/2018/3061/fs20183061.pdf","text":"Report","size":"926 KB","linkFileType":{"id":1,"text":"pdf"},"description":"FS 2018-3061"},{"id":359424,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/2018/3061/coverthb.jpg"}],"contact":"<p><a href=\"https://www.usgs.gov/centers/whcmsc\" data-mce-href=\"https://www.usgs.gov/centers/whcmsc\">Woods Hole Coastal and Marine Science Center</a><br><a href=\"https://www.usgs.gov/centers/whcmsc/science/aerial-imaging-and-mapping\" data-mce-href=\"https://www.usgs.gov/centers/whcmsc/science/aerial-imaging-and-mapping\">Aerial Imaging and Mapping</a> Group<br>U.S. Geological Survey<br>384 Woods Hole Road<br>Quissett Campus<br>Woods Hole, MA 02543</p>","tableOfContents":"<ul><li>Science Applications</li><li>UAS Capabilities</li></ul>","publishingServiceCenter":{"id":11,"text":"Pembroke PSC"},"publishedDate":"2018-11-19","noUsgsAuthors":false,"publicationDate":"2018-11-19","publicationStatus":"PW","scienceBaseUri":"5bf3d9f0e4b045bfcae0c9b1","contributors":{"authors":[{"text":"Brosnahan, Sandra 0000-0003-3797-4207 sbrosnahan@usgs.gov","orcid":"https://orcid.org/0000-0003-3797-4207","contributorId":192274,"corporation":false,"usgs":true,"family":"Brosnahan","given":"Sandra","email":"sbrosnahan@usgs.gov","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":750756,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sherwood, Christopher R. 0000-0001-6135-3553 csherwood@usgs.gov","orcid":"https://orcid.org/0000-0001-6135-3553","contributorId":2866,"corporation":false,"usgs":true,"family":"Sherwood","given":"Christopher","email":"csherwood@usgs.gov","middleInitial":"R.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":750757,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70200528,"text":"sir20185148 - 2018 - Flood frequency of rural streams in Mississippi, 2013","interactions":[{"subject":{"id":28223,"text":"wri914037 - 1991 - Flood characteristics of Mississippi streams","indexId":"wri914037","publicationYear":"1991","noYear":false,"title":"Flood characteristics of Mississippi streams"},"predicate":"SUPERSEDED_BY","object":{"id":70200528,"text":"sir20185148 - 2018 - Flood frequency of rural streams in Mississippi, 2013","indexId":"sir20185148","publicationYear":"2018","noYear":false,"title":"Flood frequency of rural streams in Mississippi, 2013"},"id":1}],"lastModifiedDate":"2018-11-26T09:50:24","indexId":"sir20185148","displayToPublicDate":"2018-11-15T13:33:02","publicationYear":"2018","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2018-5148","displayTitle":"Flood Frequency of Rural Streams in Mississippi, 2013","title":"Flood frequency of rural streams in Mississippi, 2013","docAbstract":"<p>To improve flood-frequency estimates at rural streams in Mississippi, annual exceedance probability flows at gaged streams and regional regression equations used to estimate annual exceedance probability flows for ungaged streams were developed by using current geospatial data, new analytical methods, and annual peak-flow data through the 2013 water year. The regional regression equations were derived from statistical analyses of peak-flow data and basin characteristics for 281 streamgages and incorporated a newly developed study-specific skew coefficient at streamgages located in five subregional watersheds (Middle Tennessee-Elk, Mobile-Tombigbee, Lower Mississippi-Big Black, Pearl, and Pascagoula) in Mississippi. Three flood regions—A, B, and C—were identified based on residuals from the regional regression analyses and contain sites with similar basin characteristics. Analysis was not conducted for the fourth flood region, the Mississippi Alluvial Plain, because of insufficient long-term streamflow data and poorly defined basin characteristics.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20185148","collaboration":"Prepared in cooperation with the Mississippi Department of Transportation","usgsCitation":"Anderson, B.T., 2018, Flood frequency of rural streams in Mississippi, 2013: U.S. Geological Survey Scientific Investigations Report 2018–5148, 12 p., https://doi.org/10.3133/sir20185148. 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 \"}}]}","contact":"<p><a data-mce-href=\"mailto:%20dc_tn@usgs.gov\" href=\"mailto:%20dc_tn@usgs.gov\">Director</a>, <a data-mce-href=\"https://www.usgs.gov/centers/lmg-water\" href=\"https://www.usgs.gov/centers/lmg-water\">Lower Mississippi-Gulf Water Science Center</a><br>U.S. Geological Survey<br>640 Grassmere Park, Suite 100<br>Nashville, Tennessee 37211 </p>","tableOfContents":"<ul><li>Acknowledgments</li><li>Abstract</li><li>Introduction</li><li>Data Compilation</li><li>Application of Methods</li><li>Summary and Conclusions</li><li>References Cited</li></ul>","publishingServiceCenter":{"id":5,"text":"Lafayette PSC"},"publishedDate":"2018-11-15","noUsgsAuthors":false,"publicationDate":"2018-11-15","publicationStatus":"PW","scienceBaseUri":"5bee93e3e4b08f163c24a1b5","contributors":{"authors":[{"text":"Anderson, Brandon T. 0000-0001-6698-0791","orcid":"https://orcid.org/0000-0001-6698-0791","contributorId":209976,"corporation":false,"usgs":true,"family":"Anderson","given":"Brandon","email":"","middleInitial":"T.","affiliations":[{"id":24708,"text":"Lower Mississippi-Gulf Water Science Center","active":true,"usgs":true}],"preferred":true,"id":749375,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70199131,"text":"70199131 - 2018 - Filtering of periodic infiltration in a layered vadose zone: 2. Applications and a freeware screening tool","interactions":[],"lastModifiedDate":"2018-11-20T12:05:24","indexId":"70199131","displayToPublicDate":"2018-11-15T12:05:18","publicationYear":"2018","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3674,"text":"Vadose Zone Journal","active":true,"publicationSubtype":{"id":10}},"title":"Filtering of periodic infiltration in a layered vadose zone: 2. Applications and a freeware screening tool","docAbstract":"<p><span>We have developed a screening tool to visualize and conceptualize the filtering properties of a layered vadose zone. Climate projections indicate that rainfall timing and magnitude may change and impact groundwater resources. This increases the importance of understanding how the vadose zone filters infiltration variability and ultimately affects recharge and groundwater resources. An approximate solution for the filtering of surface forcings through soil layers was developed previously, and the soil and conditions where its approximations are appropriate was evaluated. Here we present a screening tool based on the solution for estimating how periodic infiltration forcings filter in a layered vadose zone for different soil properties and surface flux conditions. The solutions identify time-varying elements of surface forcings that persist to the depth of the water table, leading to transient recharge. We investigated the filtering properties of the vadose zone in Central Valley, California, and identified areas where surface forcings are essentially damped and recharge can be approximated as steady. We also determined the travel time for infiltration pulses to reach the depth of the water table.</span></p>","language":"English","publisher":"ACSESS","doi":"10.2136/vzj2018.03.0048","usgsCitation":"Dickinson, J.E., and Ferre, T.P., 2018, Filtering of periodic infiltration in a layered vadose zone: 2. Applications and a freeware screening tool: Vadose Zone Journal, v. 17, no. 1, p. 1-12, https://doi.org/10.2136/vzj2018.03.0048.","productDescription":"Article 180048; 12 p.","startPage":"1","endPage":"12","ipdsId":"IP-096156","costCenters":[{"id":128,"text":"Arizona Water Science Center","active":true,"usgs":true}],"links":[{"id":468248,"rank":1,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.2136/vzj2018.03.0048","text":"Publisher Index Page"},{"id":437684,"rank":0,"type":{"id":30,"text":"Data Release"},"url":"https://doi.org/10.5066/P9BHD74M","text":"USGS data release","linkHelpText":"Code for computing the responses to cyclical infiltration in a layered vadose zone in Central Valley, California"},{"id":359606,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","issue":"1","publishingServiceCenter":{"id":14,"text":"Menlo Park PSC"},"noUsgsAuthors":false,"publicationDate":"2018-11-15","publicationStatus":"PW","scienceBaseUri":"5bf52b68e4b045bfcae28006","contributors":{"authors":[{"text":"Dickinson, Jesse E. 0000-0002-0048-0839 jdickins@usgs.gov","orcid":"https://orcid.org/0000-0002-0048-0839","contributorId":152545,"corporation":false,"usgs":true,"family":"Dickinson","given":"Jesse","email":"jdickins@usgs.gov","middleInitial":"E.","affiliations":[{"id":128,"text":"Arizona Water Science Center","active":true,"usgs":true}],"preferred":true,"id":744269,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ferre, T. P. A","contributorId":206539,"corporation":false,"usgs":false,"family":"Ferre","given":"T.","email":"","middleInitial":"P. A","affiliations":[{"id":7042,"text":"University of Arizona","active":true,"usgs":false}],"preferred":false,"id":744270,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70199133,"text":"70199133 - 2018 - Filtering of cyclic period infiltration in a layered vadose zone: 1. Approximation of damping and time lags","interactions":[],"lastModifiedDate":"2021-02-01T17:54:29.16291","indexId":"70199133","displayToPublicDate":"2018-11-15T11:53:24","publicationYear":"2018","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3674,"text":"Vadose Zone Journal","active":true,"publicationSubtype":{"id":10}},"title":"Filtering of cyclic period infiltration in a layered vadose zone: 1. Approximation of damping and time lags","docAbstract":"<h3 id=\"vzj2vzj2018030047-sec-0001-title\" class=\"article-section__sub-title section1\">Core Ideas</h3><div class=\"paragraph-element\"><ul class=\"unordered-list\"><li>We describe an approximation for filtering of periodic infiltration in layered soil.</li><li>Transitions in soil‐water properties between soil layers affect the filtering.</li><li>Errors are smaller in soils where changes in soil‐water properties are small.</li></ul></div><p>Infiltration and downward percolation of water in the vadose zone are important processes that can define the availability of water resources. We present an approach that provides insight into how periodic infiltration forcings at the land surface filter in a layered vadose zone in terms of changes in the timing and magnitude of hydrologic responses. To represent geologically realistic systems, we used vertical sequences of one‐dimensional periodic solutions, where each solution represents a single soil in a layered profile. The overall approach is based on a linearized Richards equation and assumes that the effects on flow of continuous pressure head changes at soil interfaces are negligible. We evaluated the limit of these approximations by comparison with results from the numerical model HYDRUS‐1D, which uses the full Richards equation. We compared (i) the depth at which flux variations became steady, and (ii) the travel time of wetting fronts to reach a depth of 3 m. The solution was reasonably accurate (error less than a factor of 2) for infiltration cycles with periods from 30 to 365 d and for fluxes common in arid and semiarid environments (0–2 mm d<sup>−1</sup>). Lag times between a surface forcing and response at any depth were accurate (error less than a factor of 1.1). The approximation generally provided consistent estimates of the damping and time lag, such that it overestimated the depths where fluxes were steady and underestimated the time for a forcing to reach a specific depth.</p>","language":"English","publisher":"ACSESS","doi":"10.2136/vzj2018.03.0047","usgsCitation":"Dickinson, J.E., and Ferre, T.P., 2018, Filtering of cyclic period infiltration in a layered vadose zone: 1. Approximation of damping and time lags: Vadose Zone Journal, v. 17, no. 1, p. 1-16, https://doi.org/10.2136/vzj2018.03.0047.","productDescription":"16 p.","startPage":"1","endPage":"16","ipdsId":"IP-077789","costCenters":[{"id":128,"text":"Arizona Water Science Center","active":true,"usgs":true}],"links":[{"id":468249,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.2136/vzj2018.03.0047","text":"Publisher Index Page"},{"id":382854,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","issue":"1","publishingServiceCenter":{"id":14,"text":"Menlo Park PSC"},"noUsgsAuthors":false,"publicationDate":"2018-11-15","publicationStatus":"PW","contributors":{"authors":[{"text":"Dickinson, Jesse E. 0000-0002-0048-0839 jdickins@usgs.gov","orcid":"https://orcid.org/0000-0002-0048-0839","contributorId":152545,"corporation":false,"usgs":true,"family":"Dickinson","given":"Jesse","email":"jdickins@usgs.gov","middleInitial":"E.","affiliations":[{"id":128,"text":"Arizona Water Science Center","active":true,"usgs":true}],"preferred":true,"id":744271,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ferre, T. P. A","contributorId":206539,"corporation":false,"usgs":false,"family":"Ferre","given":"T.","email":"","middleInitial":"P. A","affiliations":[{"id":7042,"text":"University of Arizona","active":true,"usgs":false}],"preferred":false,"id":744272,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70211496,"text":"70211496 - 2018 - New England and northern New York forest ecosystem vulnerability assessment and synthesis: A report from the New England Climate Change Response Framework project","interactions":[],"lastModifiedDate":"2020-08-04T21:01:51.925161","indexId":"70211496","displayToPublicDate":"2018-11-15T10:42:41","publicationYear":"2018","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":32,"text":"General Technical Report","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"NRS-173","title":"New England and northern New York forest ecosystem vulnerability assessment and synthesis: A report from the New England Climate Change Response Framework project","docAbstract":"<p><span>Forest ecosystems will face direct and indirect impacts from a changing climate over the 21st century. This assessment evaluates the vulnerability of forest ecosystems across the New England region (Connecticut, Maine, Massachusetts, New Hampshire, northern New York, Rhode Island, and Vermont) under a range of future climates. We synthesized and summarized information on the contemporary landscape, provided information on past climate trends, and described a range of projected future climates. This information was used to parameterize and run multiple vegetation impact models, which provided a range of potential vegetative responses to climate. Finally, we brought these results before a multidisciplinary panel of scientists and natural resource professionals familiar with the forests of this region to assess ecosystem vulnerability through a formal consensus-based expert elicitation process. Observed trends in climate over the historical record from 1901 through 2011 show that the mean annual temperature has increased across the region by 2.4 °F, with even greater warming during winter. Precipitation patterns also changed during this time, with a slight trend toward greater annual precipitation and a substantial increase in extreme precipitation events. Projected climate trends using downscaled global climate model data indicate a potential increase in mean annual temperature of 3 to 8 °F for the assessment area by 2100. Projections for precipitation indicate an increase in fall and winter precipitation, and spring and summer precipitation projections vary by scenario. We identified potential impacts on forests by incorporating these future climate projections into three forest impact models (DISTRIB, LINKAGES, and LANDIS PRO). Model projections suggest that many northern and boreal species, including balsam fir, red spruce, and black spruce, may fare worse under future conditions, but other species may benefit from projected changes in climate. Published literature on climate impacts related to wildfire, invasive species, and forest pests and diseases also contributed to the overall determination of climate change vulnerability. We assessed vulnerability for eight forest communities in the assessment area. The assessment was conducted through a formal elicitation process with 20 scientists and resource managers from across the area, who considered vulnerability in terms of the potential impacts and the adaptive capacity for an individual community. Montane spruce-fir, low-elevation spruce-fir, and lowland mixed conifer forests were determined to be the most vulnerable communities. Central hardwoods, transition hardwoods, and pitch pine-scrub oak forests were perceived as having lower vulnerability to projected changes in climate. These projected changes in climate and the associated impacts and vulnerabilities will have important implications for economically valuable timber species, forest-dependent animals and plants, recreation, and long-term natural resource planning.</span></p>","language":"English","publisher":"Northern Research Station","doi":"10.2737/NRS-GTR-173","usgsCitation":"Janowiak, M., D’Amato, A., Swanston, C., Iverson, L.R., Thompson, F., Dijak, W.D., Matthews, S., Peters, M.P., Prasad, A., Fraser, J.S., Brandt, L.A., Butler-Leopold, P.R., Handler, S.D., Shannon, P.D., Burbank, D., Campbell, J., Cogbill, C., Duveneck, M.J., Emery, M.R., Fisichelli, N., Foster, J., Hushaw, J., Kenefic, L., Mahaffey, A., Morelli, T.L., Reo, N., Schaberg, P.G., Simmons, K.R., Weiskittel, A., Wilmot, S., Hollinger, D., Lane, E., Rustad, L., and Templar, P.H., 2018, New England and northern New York forest ecosystem vulnerability assessment and synthesis: A report from the New England Climate Change Response 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,{"id":70201370,"text":"70201370 - 2018 - Shared habitat use by juveniles of three sea turtle species","interactions":[],"lastModifiedDate":"2018-12-12T09:53:13","indexId":"70201370","displayToPublicDate":"2018-11-15T09:53:04","publicationYear":"2018","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2663,"text":"Marine Ecology Progress Series","active":true,"publicationSubtype":{"id":10}},"title":"Shared habitat use by juveniles of three sea turtle species","docAbstract":"<p><span>The first step in understanding how sympatric species share habitat is defining spatial boundaries. While home range data for juvenile sea turtles exists, few studies have examined spatial overlap of multiple species in foraging habitat. Using satellite tracking technology, we define home ranges for juveniles of 3 sea turtle species (loggerhead, Kemp’s ridley, and green; n = 21) captured at 2 adjacent foraging sites in the northern Gulf of Mexico. In these areas, green turtles are known to be primarily herbivorous, whereas Kemp’s ridley turtles forage predominately on crabs, and loggerhead turtles on various hard-shelled benthic invertebrates. No differences in home range size or characteristics, such as water depth and distance to shore, were observed among species, although fine-scale foraging patches were not examined in this study. A high degree of overlap in habitat-use among all 3 species was documented in summer at both sites. Seasonal movements, triggered by colder winter temperatures, were documented and appeared to differ among species, with Kemp’s ridley and loggerhead turtles leaving bays, and green turtles overwintering inside bays. By identifying shared habitat-use by juvenile sea turtles, we have created a foundation for further fine-scale studies on resource partitioning that will aid in habitat management and conservation of these threatened and endangered species.</span></p>","language":"English","publisher":"Inter-Research","doi":"10.3354/meps12748","usgsCitation":"Lamont, M.M., and Iverson, A., 2018, Shared habitat use by juveniles of three sea turtle species: Marine Ecology Progress Series, v. 606, p. 187-200, https://doi.org/10.3354/meps12748.","productDescription":"14 p.","startPage":"187","endPage":"200","ipdsId":"IP-098002","costCenters":[{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"links":[{"id":360185,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"606","publishingServiceCenter":{"id":5,"text":"Lafayette PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5c122c55e4b034bf6a8569df","contributors":{"authors":[{"text":"Lamont, Margaret M. 0000-0001-7520-6669 mlamont@usgs.gov","orcid":"https://orcid.org/0000-0001-7520-6669","contributorId":4525,"corporation":false,"usgs":true,"family":"Lamont","given":"Margaret","email":"mlamont@usgs.gov","middleInitial":"M.","affiliations":[{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"preferred":true,"id":753832,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Iverson, Autumn R. 0000-0002-8353-6745","orcid":"https://orcid.org/0000-0002-8353-6745","contributorId":173555,"corporation":false,"usgs":false,"family":"Iverson","given":"Autumn R.","affiliations":[{"id":590,"text":"U.S. Army Corps of Engineers","active":false,"usgs":false}],"preferred":false,"id":753833,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70216309,"text":"70216309 - 2018 - Fire and tree death: Understanding and improving modeling of fire-induced tree mortality","interactions":[],"lastModifiedDate":"2020-11-11T14:42:14.27702","indexId":"70216309","displayToPublicDate":"2018-11-15T08:36:33","publicationYear":"2018","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1562,"text":"Environmental Research Letters","active":true,"publicationSubtype":{"id":10}},"title":"Fire and tree death: Understanding and improving modeling of fire-induced tree mortality","docAbstract":"<div class=\"article-text wd-jnl-art-abstract cf\"><p>Each year wildland fires kill and injure trees on millions of forested hectares globally, affecting plant and animal biodiversity, carbon storage, hydrologic processes, and ecosystem services. The underlying mechanisms of fire-caused tree mortality remain poorly understood, however, limiting the ability to accurately predict mortality and develop robust modeling applications, especially under novel future climates. Virtually all post-fire tree mortality prediction systems are based on the same underlying empirical model described in Ryan and Reinhardt (1988&nbsp;<i>Can. J. For. Res.</i>&nbsp;18&nbsp;1291–7), which was developed from a limited number of species, stretching model assumptions beyond intended limits. We review the current understanding of the mechanisms of fire-induced tree mortality, provide recommended standardized terminology, describe model applications and limitations, and conclude with key knowledge gaps and future directions for research. We suggest a two-pronged approach to future research: (1) continued improvements and evaluations of empirical models to quantify uncertainty and incorporate new regions and species and (2) acceleration of basic, physiological research on the proximate and ultimate causes of fire-induced tree mortality to incorporate processes of tree death into models. Advances in both empirical and process fire-induced tree modeling will allow creation of hybrid models that could advance understanding of how fire injures and kills trees, while improving prediction accuracy of fire-driven feedbacks on ecosystems and landscapes, particularly under novel future conditions.</p></div>","language":"English","publisher":"IOP Publishing","doi":"10.1088/1748-9326/aae934","usgsCitation":"Hood, S.M., Varner, J.M., van Mantgem, P., and Cansler, C.A., 2018, Fire and tree death: Understanding and improving modeling of fire-induced tree mortality: Environmental Research Letters, v. 13, no. 11, 113004, 17 p., https://doi.org/10.1088/1748-9326/aae934.","productDescription":"113004, 17 p.","ipdsId":"IP-091982","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":468250,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1088/1748-9326/aae934","text":"Publisher Index Page"},{"id":380408,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"13","issue":"11","noUsgsAuthors":false,"publicationDate":"2018-11-15","publicationStatus":"PW","contributors":{"authors":[{"text":"Hood, Sharon M.","contributorId":221183,"corporation":false,"usgs":false,"family":"Hood","given":"Sharon","email":"","middleInitial":"M.","affiliations":[{"id":37389,"text":"U.S. Forest Service","active":true,"usgs":false}],"preferred":false,"id":804622,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Varner, J. Morgan 0000-0003-3781-5839","orcid":"https://orcid.org/0000-0003-3781-5839","contributorId":244802,"corporation":false,"usgs":false,"family":"Varner","given":"J.","email":"","middleInitial":"Morgan","affiliations":[{"id":36493,"text":"USDA Forest Service","active":true,"usgs":false}],"preferred":false,"id":804623,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"van Mantgem, Phillip J. 0000-0002-3068-9422","orcid":"https://orcid.org/0000-0002-3068-9422","contributorId":204320,"corporation":false,"usgs":true,"family":"van Mantgem","given":"Phillip J.","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":true,"id":804624,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Cansler, C. Alina 0000-0002-2155-4438","orcid":"https://orcid.org/0000-0002-2155-4438","contributorId":225029,"corporation":false,"usgs":false,"family":"Cansler","given":"C.","email":"","middleInitial":"Alina","affiliations":[{"id":41022,"text":"Missoula Fire Science Lab","active":true,"usgs":false}],"preferred":false,"id":804625,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
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