Submerged passive acoustic technology allows researchers to investigate spatial and temporal movement patterns of many marine and freshwater species. The technology uses receivers to detect and record acoustic transmissions emitted from tags attached to an individual. Acoustic signal strength naturally attenuates over distance, but numerous environmental variables also affect the probability a tag is detected. Knowledge of receiver range is crucial for designing acoustic arrays and analyzing telemetry data. Here, we present a method for testing a relatively large-scale receiver array in a dynamic Caribbean coastal environment intended for long-term monitoring of multiple species. The U.S. Geological Survey and several academic institutions in collaboration with resource management at Buck Island Reef National Monument (BIRNM), off the coast of St. Croix, recently deployed a 52 passive acoustic receiver array. We targeted 19 array-representative receivers for range-testing by submersing fixed delay interval range-testing tags at various distance intervals in each cardinal direction from a receiver for a minimum of an hour. Using a generalized linear mixed model (GLMM), we estimated the probability of detection across the array and assessed the effect of water depth, habitat, wind, temperature, and time of day on the probability of detection. The predicted probability of detection across the entire array at 100 m distance from a receiver was 58.2% (95% CI: 44.0–73.0%) and dropped to 26.0% (95% CI: 11.4–39.3%) 200 m from a receiver indicating a somewhat constrained effective detection range. Detection probability varied across habitat classes with the greatest effective detection range occurring in homogenous sand substrate and the smallest in high rugosity reef. Predicted probability of detection across BIRNM highlights potential gaps in coverage using the current array as well as limitations of passive acoustic technology within a complex coral reef environment.
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Range-testing a submerged passive acoustic receiver array in a Caribbean coral reef habitat: Ecology and Evolution, v. 6, no. 14, p. 4823-4835, https://doi.org/10.1002/ece3.2228.","productDescription":"13 p.","startPage":"4823","endPage":"4835","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-070624","costCenters":[{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"links":[{"id":470751,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1002/ece3.2228","text":"Publisher Index Page"},{"id":325231,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Buck Island Reef National Monument","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -64.65763092041016,\n 17.771573896194067\n ],\n [\n -64.65763092041016,\n 17.833027985030018\n ],\n [\n -64.57592010498047,\n 17.833027985030018\n ],\n [\n -64.57592010498047,\n 17.771573896194067\n ],\n [\n -64.65763092041016,\n 17.771573896194067\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"6","issue":"14","publishingServiceCenter":{"id":5,"text":"Lafayette PSC"},"noUsgsAuthors":false,"publicationDate":"2016-06-17","publicationStatus":"PW","scienceBaseUri":"57875827e4b0d27deb364f54","contributors":{"authors":[{"text":"Selby, Thomas H. 0000-0003-2116-0807 tselby@usgs.gov","orcid":"https://orcid.org/0000-0003-2116-0807","contributorId":5685,"corporation":false,"usgs":true,"family":"Selby","given":"Thomas","email":"tselby@usgs.gov","middleInitial":"H.","affiliations":[],"preferred":true,"id":642332,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hart, Kristen M. 0000-0002-5257-7974 kristen_hart@usgs.gov","orcid":"https://orcid.org/0000-0002-5257-7974","contributorId":1966,"corporation":false,"usgs":true,"family":"Hart","given":"Kristen","email":"kristen_hart@usgs.gov","middleInitial":"M.","affiliations":[{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"preferred":true,"id":642331,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fujisaki, Ikuko","contributorId":38359,"corporation":false,"usgs":false,"family":"Fujisaki","given":"Ikuko","affiliations":[],"preferred":false,"id":642333,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Smith, Brian J. 0000-0002-0531-0492 bjsmith@usgs.gov","orcid":"https://orcid.org/0000-0002-0531-0492","contributorId":899,"corporation":false,"usgs":true,"family":"Smith","given":"Brian","email":"bjsmith@usgs.gov","middleInitial":"J.","affiliations":[{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"preferred":false,"id":642334,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Pollock, Clayton J","contributorId":172870,"corporation":false,"usgs":false,"family":"Pollock","given":"Clayton","email":"","middleInitial":"J","affiliations":[{"id":5106,"text":"National Park Service, Yellowstone National Park, Mammoth, Wyoming 82190","active":true,"usgs":false}],"preferred":false,"id":642335,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Hillis-Star, Zandy M","contributorId":106418,"corporation":false,"usgs":true,"family":"Hillis-Star","given":"Zandy","email":"","middleInitial":"M","affiliations":[],"preferred":false,"id":642336,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Lundgren, Ian","contributorId":29727,"corporation":false,"usgs":true,"family":"Lundgren","given":"Ian","affiliations":[],"preferred":false,"id":642337,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Oli, Madan K.","contributorId":86089,"corporation":false,"usgs":true,"family":"Oli","given":"Madan","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":642338,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}} ,{"id":70174032,"text":"fs20163041 - 2016 - The Water-Quality Partnership for National Parks—U.S. Geological Survey and National Park Service, 1998–2016","interactions":[],"lastModifiedDate":"2017-06-30T10:16:15","indexId":"fs20163041","displayToPublicDate":"2016-07-13T16:45:00","publicationYear":"2016","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":"2016-3041","title":"The Water-Quality Partnership for National Parks—U.S. Geological Survey and National Park Service, 1998–2016","docAbstract":"The U.S. Geological Survey (USGS) and the National Park Service (NPS) work together through the USGS–NPS Water-Quality Partnership to support a broad range of policy and management needs related to high-priority water-quality issues in national parks. 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The National Park Service manages many of our Nation’s most highly valued aquatic systems across the country, including portions of the Great Lakes, ocean and coastal zones, historic canals, reservoirs, large rivers, high-elevation lakes and streams, geysers, springs, and wetlands. So far, the Water-Quality Partnership has undertaken 217 projects in 119 national parks. In each project, USGS studies and assessments (http://water.usgs.gov/nps_partnership/pubs.php) have supported science-based management by the NPS to protect and improve water quality in parks. Some of the current projects are highlighted in the NPS Call to Action Centennial initiative, Crystal Clear, which celebrates national park water-resource efforts to ensure clean water for the next century of park management (http://www.nature.nps.gov/water/crystalclear/).
New projects are proposed each year by USGS scientists working in collaboration with NPS staff in specific parks. Project selection is highly competitive, with an average of only eight new projects funded each year out of approximately 75 proposals that are submitted. Since the beginning of the Partnership in 1998, 189 publications detailing project findings have been completed. The 217 studies have been conducted in 119 NPS-administered lands, extending from Denali National Park and Preserve in Alaska to Everglades National Park in Florida, and from Acadia National Park in the Northeast to park lands in Hawaii and Pacific Island territories in the West. Project goals range from periodic stream monitoring, to determining the occurrence and concentrations of contaminants and the potential for them to exceed human health or aquatic life criteria, to conducting interpretive studies to evaluate the effect(s) on or vulnerability of national park resources to visitor usage and other natural and anthropogenic activities.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/fs20163041","collaboration":"Prepared in cooperation with the National Park Service","usgsCitation":"Nilles, M.A., Penoyer, P.E., Ludtke, A.S., and Ellsworth, A.C., 2016, The Water-Quality Partnership for national parks—U.S. Geological Survey and National Park Service, 1998–2016: U.S. Geological Survey Fact Sheet 2016–3041, 6 p., https://dx.doi.org/10.3133/fs20163041.","productDescription":"6 p.","numberOfPages":"6","onlineOnly":"Y","additionalOnlineFiles":"N","ipdsId":"IP-073494","costCenters":[{"id":27111,"text":"National Water Quality Program","active":true,"usgs":true}],"links":[{"id":324980,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/2016/3041/coverthb1.jpg"},{"id":324981,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/2016/3041/fs20163041.pdf","text":"Report","size":"7.81 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States\"}}]}","contact":"Program Coordinator, National Water Quality Program
U.S. Geological Survey
413 National Center
12201 Sunrise Valley Drive
Reston, VA 20192
https://www.usgs.gov/science/mission-areas/water/national-water-quality-program
At least 170 volcanoes in 12 States and 2 territories have erupted in the past 12,000 years and have the potential to erupt again. Consequences of eruptions from U.S. volcanoes can extend far beyond the volcano’s immediate area. Many aspects of our daily life are vulnerable to volcano hazards, including air travel, regional power generation and transmission infrastructure, interstate transportation, port facilities, communications infrastructure, and public health. The U.S. Geological Survey has the Federal responsibility to issue timely warnings of potential volcanic activity to the affected populace and civil authorities. The Volcano Hazards Program (VHP) is funded to carry out that mission and does so through a combination of volcano monitoring, short-term warnings, research on how volcanoes work, and community education and outreach.
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This integrated collection of spatial databases provides location, geologic and mineral resource data, and source references for deposits, significant prospects, and areas permissive for undiscovered deposits of both porphyry copper and sediment-hosted copper. The copper resource database allows for efficient modeling on a global scale in a geographic information system (GIS) and is provided in an Esri ArcGIS file geodatabase format.
","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Global mineral resource assessment (Scientific Investigations Report 2010-5090)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20105090Z","usgsCitation":"Dicken, C.L., Dunlap, Pamela, Parks, H.L., Hammarstrom, J.M., and Zientek, M.L., 2016, Spatial database for a global assessment of undiscovered copper resources: U.S. Geological Survey Scientific Investigations Report 2010–5090–Z, 29 p., and GIS data, available at https://dx.doi.org/10.3133/sir20105090Z.","productDescription":"Report: v, 29 p.; GIS Data","numberOfPages":"40","onlineOnly":"Y","additionalOnlineFiles":"Y","ipdsId":"IP-066779","costCenters":[{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true},{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":325183,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/sir/2010/5090/z/sir20105090z.pdf","text":"Report","size":"2 MB","linkFileType":{"id":1,"text":"pdf"},"description":"SIR 2010-5090-Z Report PDF"},{"id":325184,"rank":3,"type":{"id":23,"text":"Spatial Data"},"url":"https://pubs.usgs.gov/sir/2010/5090/z/sir20105090z_gis.zip","text":"GIS Data","size":"66 MB","linkFileType":{"id":6,"text":"zip"},"description":"SIR 2010-5090-Z GIS Data"},{"id":325182,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/sir/2010/5090/z/coverthb.jpg"}],"contact":"Contact Information, Mineral Resources Program
U.S. Geological Survey
12201 Sunrise Valley Drive
913 National Center
Reston, VA 20192
http://minerals.usgs.gov/
In 2015, as part of an on-going screening program for contaminants of emerging concern (CECs) in conjunction with the Environmental Protection Agency (EPA) Region 8, surface waters at 18 locations in or near seven national park units within the Northern Colorado Plateau Network (NCPN) were sampled for pesticides and pesticide degradation products, pharmaceuticals and personal care products, hormones, organic-wastewater-indictor chemicals, and nutrients. Most sites were sampled in spring (May or June) and fall (September).
\nThe Colorado River at the Potash boat ramp site, just upstream of Canyonlands National Park, continued to show chronic contamination by caffeine, the pesticide 2,4-D, and prescription drugs (gabapentin, lamotrigine, metformin, and sulfamethoxazole). Samples at the Moab wastewater treatment plant effluent outflow pipe showed a high number and concentration of contaminants entering the river about 14 miles upstream of the long-term sampling location and are the nearest point source for contaminants of emerging concern. Samples from 400 m downstream of the effluent pipe in the Colorado River had decreased numbers and concentrations of contaminants, indicating relatively quick dilution by the river. However, some contaminants persisted at the long-term sampling site downstream.
\nPatterns of detections at other sampling locations will be explored in future reports. This is an interim report. Limited sampling will continue in 2016 at selected sites in coordination with the USGS. A final report is expected upon completion of the USGS project in 2017.
","language":"English","publisher":"US National Park Service","publisherLocation":"Fort Collins, CO","usgsCitation":"Weissinger, R., Battaglin, W.A., and Bradley, P.M., 2016, Screening for contaminants of emerging concern in Northern Colorado Plateau Network waters: 2015 surface-water data: Natural Resource Report 2016-1239, xi, 41 p.","productDescription":"xi, 41 p.","numberOfPages":"58","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-076062","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":325169,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":324700,"type":{"id":15,"text":"Index Page"},"url":"https://irma.nps.gov/DataStore/DownloadFile/551578"}],"country":"United States","state":"Arizona, Colorado, Idaho, Utah, Wyoming","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -113.3349609375,\n 36.50963615733049\n ],\n [\n -114.356689453125,\n 39.74943369178247\n ],\n [\n -113.851318359375,\n 40.75557964275591\n ],\n [\n -112.950439453125,\n 42.032974332441405\n ],\n [\n -111.95068359374999,\n 42.779275360241904\n ],\n [\n -111.07177734375,\n 42.67435857693384\n ],\n [\n -109.4073486328125,\n 43.15710884095329\n ],\n [\n -105.09521484375,\n 38.013476231041935\n ],\n [\n -109.061279296875,\n 36.98500309285596\n ],\n [\n -110.55541992187499,\n 38.12159327165922\n ],\n [\n -113.3349609375,\n 36.50963615733049\n ]\n ]\n ]\n }\n }\n ]\n}","publishingServiceCenter":{"id":9,"text":"Reston PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57875828e4b0d27deb364f60","contributors":{"authors":[{"text":"Weissinger, R","contributorId":172623,"corporation":false,"usgs":false,"family":"Weissinger","given":"R","email":"","affiliations":[{"id":20307,"text":"US National Park Service","active":true,"usgs":false}],"preferred":false,"id":641453,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Battaglin, William A. 0000-0001-7287-7096 wbattagl@usgs.gov","orcid":"https://orcid.org/0000-0001-7287-7096","contributorId":1527,"corporation":false,"usgs":true,"family":"Battaglin","given":"William","email":"wbattagl@usgs.gov","middleInitial":"A.","affiliations":[{"id":191,"text":"Colorado Water Science Center","active":true,"usgs":true}],"preferred":true,"id":641454,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bradley, Paul M. 0000-0001-7522-8606 pbradley@usgs.gov","orcid":"https://orcid.org/0000-0001-7522-8606","contributorId":361,"corporation":false,"usgs":true,"family":"Bradley","given":"Paul","email":"pbradley@usgs.gov","middleInitial":"M.","affiliations":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"preferred":true,"id":641452,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70174953,"text":"70174953 - 2016 - The PRISM4 (mid-Piacenzian) paleoenvironmental reconstruction","interactions":[],"lastModifiedDate":"2016-07-22T16:26:06","indexId":"70174953","displayToPublicDate":"2016-07-13T10:30:00","publicationYear":"2016","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1250,"text":"Climate of the Past","active":true,"publicationSubtype":{"id":10}},"title":"The PRISM4 (mid-Piacenzian) paleoenvironmental reconstruction","docAbstract":"The mid-Piacenzian is known as a period of relative warmth when compared to the present day. A comprehensive understanding of conditions during the Piacenzian serves as both a conceptual model and a source for boundary conditions as well as means of verification of global climate model experiments. In this paper we present the PRISM4 reconstruction, a paleoenvironmental reconstruction of the mid-Piacenzian ( ∼ 3 Ma) containing data for paleogeography, land and sea ice, sea-surface temperature, vegetation, soils, and lakes. Our retrodicted paleogeography takes into account glacial isostatic adjustments and changes in dynamic topography. Soils and lakes, both significant as land surface features, are introduced to the PRISM reconstruction for the first time. Sea-surface temperature and vegetation reconstructions are unchanged but now have confidence assessments. The PRISM4 reconstruction is being used as boundary condition data for the Pliocene Model Intercomparison Project Phase 2 (PlioMIP2) experiments.
","language":"English","publisher":"Copernicus Publications","doi":"10.5194/cp-12-1519-2016","usgsCitation":"Dowsett, H.J., Dolan, A.M., Rowley, D., Moucha, R., Forte, A., Mitrovica, J.X., Pound, M., Salzmann, U., Robinson, M.M., Chandler, M., Foley, K.M., and Haywood, A.M., 2016, The PRISM4 (mid-Piacenzian) paleoenvironmental reconstruction: Climate of the Past, v. 12, no. 7, p. 1519-1538, https://doi.org/10.5194/cp-12-1519-2016.","productDescription":"20 p.","startPage":"1519","endPage":"1538","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-074298","costCenters":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"links":[{"id":470753,"rank":1,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.5194/cp-12-1519-2016","text":"Publisher Index Page"},{"id":438588,"rank":0,"type":{"id":30,"text":"Data Release"},"url":"https://doi.org/10.5066/P9NF43WW","text":"USGS data release","linkHelpText":"PRISM4 (mid-Piacenzian) Paleoenvironmental Reconstruction Data"},{"id":325569,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"12","issue":"7","publishingServiceCenter":{"id":9,"text":"Reston PSC"},"noUsgsAuthors":false,"publicationDate":"2016-07-13","publicationStatus":"PW","scienceBaseUri":"5793444de4b0eb1ce79e8c1b","contributors":{"authors":[{"text":"Dowsett, Harry J. 0000-0003-1983-7524 hdowsett@usgs.gov","orcid":"https://orcid.org/0000-0003-1983-7524","contributorId":949,"corporation":false,"usgs":true,"family":"Dowsett","given":"Harry","email":"hdowsett@usgs.gov","middleInitial":"J.","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true},{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true}],"preferred":true,"id":643308,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dolan, Aisling M.","contributorId":30117,"corporation":false,"usgs":true,"family":"Dolan","given":"Aisling","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":643309,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rowley, David","contributorId":173099,"corporation":false,"usgs":false,"family":"Rowley","given":"David","email":"","affiliations":[{"id":12621,"text":"University of Chicago and University of South Florida","active":true,"usgs":false}],"preferred":false,"id":643310,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Moucha, Robert","contributorId":173102,"corporation":false,"usgs":false,"family":"Moucha","given":"Robert","email":"","affiliations":[{"id":5082,"text":"Syracuse University","active":true,"usgs":false}],"preferred":false,"id":643317,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Forte, Alessandro","contributorId":173103,"corporation":false,"usgs":false,"family":"Forte","given":"Alessandro","email":"","affiliations":[{"id":12557,"text":"University of Florida, FLREC","active":true,"usgs":false}],"preferred":false,"id":643318,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Mitrovica, Jerry X.","contributorId":86200,"corporation":false,"usgs":true,"family":"Mitrovica","given":"Jerry","email":"","middleInitial":"X.","affiliations":[],"preferred":false,"id":643319,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Pound, Matthew","contributorId":173100,"corporation":false,"usgs":false,"family":"Pound","given":"Matthew","email":"","affiliations":[{"id":18103,"text":"Northumbria University, Newcastle Upon Tyne, UK","active":true,"usgs":false}],"preferred":false,"id":643311,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Salzmann, Ulrich","contributorId":173101,"corporation":false,"usgs":false,"family":"Salzmann","given":"Ulrich","email":"","affiliations":[{"id":18103,"text":"Northumbria University, Newcastle Upon Tyne, UK","active":true,"usgs":false}],"preferred":false,"id":643312,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Robinson, Marci M. 0000-0002-9200-4097 mmrobinson@usgs.gov","orcid":"https://orcid.org/0000-0002-9200-4097","contributorId":2082,"corporation":false,"usgs":true,"family":"Robinson","given":"Marci","email":"mmrobinson@usgs.gov","middleInitial":"M.","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true},{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true}],"preferred":true,"id":643313,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Chandler, Mark","contributorId":17320,"corporation":false,"usgs":true,"family":"Chandler","given":"Mark","affiliations":[],"preferred":false,"id":643314,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Foley, Kevin M. 0000-0003-1013-462X kfoley@usgs.gov","orcid":"https://orcid.org/0000-0003-1013-462X","contributorId":2543,"corporation":false,"usgs":true,"family":"Foley","given":"Kevin","email":"kfoley@usgs.gov","middleInitial":"M.","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true},{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true}],"preferred":true,"id":643315,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Haywood, Alan M.","contributorId":86663,"corporation":false,"usgs":true,"family":"Haywood","given":"Alan","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":643316,"contributorType":{"id":1,"text":"Authors"},"rank":12}]}} ,{"id":70174517,"text":"70174517 - 2016 - Territoriality and inter-pack aggression in gray wolves: shaping a social carnivore's life history","interactions":[],"lastModifiedDate":"2016-07-13T09:43:36","indexId":"70174517","displayToPublicDate":"2016-07-13T10:30:00","publicationYear":"2016","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3802,"text":"Yellowstone Science","active":true,"publicationSubtype":{"id":10}},"title":"Territoriality and inter-pack aggression in gray wolves: shaping a social carnivore's life history","docAbstract":"When Rudyard Kipling wrote The Jungle Book in 1894 and included the famous line \"For the strength of the Wolf is the Pack, and the strength of the Pack is the Wolf,\" he would have had no idea that over a century later, scientific research would back up his poetic phrase. Recent studies in Yellowstone have found that both the individual wolf and the collective pack rely on each other and play important roles in territoriality. At a time when most fairy tales and fables were portraying wolves as demonic killers or, at best, slapstick gluttons, Kipling seemed to have a respect or even reverence for the wolf. Wolves in The Jungle Book raise and mentor the main character Mowgli, with the pack's leader eventually dying to save the \"man-cub\" from a pack of wolves. Kipling may have extended intra- pack benevolence to a human boy for literary sake, but he was clearly enthralled with how pack members treat each other. As wolf packs are almost always family units, most commonly comprised of a breeding pair and their offspring from several years, amiable behavior within the pack is unsurprising. By contrast, wolf packs are fiercely intolerant of their neighbors, their rivals. And this competition is proving to be an important facet in the life of a wolf and its pack.
","language":"English","publisher":"Yellowstone Science","usgsCitation":"Cassidy, K.A., Smith, D.W., Mech, L.D., MacNulty, D.R., Stahler, D.R., and Metz, M.C., 2016, Territoriality and inter-pack aggression in gray wolves: shaping a social carnivore's life history: Yellowstone Science, v. 24, no. 1, p. 37-42.","productDescription":"6 p.","startPage":"37","endPage":"42","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-069054","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":325167,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":325166,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://www.nps.gov/yell/learn/ys-24-1-territoriality-and-inter-pack-aggression-in-gray-wolves-shaping-a-social-carnivores-life-history.htm"}],"volume":"24","issue":"1","publishingServiceCenter":{"id":4,"text":"Rolla PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57875829e4b0d27deb364f64","contributors":{"authors":[{"text":"Cassidy, Kira A.","contributorId":145492,"corporation":false,"usgs":false,"family":"Cassidy","given":"Kira","email":"","middleInitial":"A.","affiliations":[{"id":16134,"text":"Yellowstone Wolf Project, Yellowstone Ctr for Resources","active":true,"usgs":false}],"preferred":false,"id":642275,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smith, Douglas W.","contributorId":95727,"corporation":false,"usgs":true,"family":"Smith","given":"Douglas","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":642276,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mech, L. David 0000-0003-3944-7769 david_mech@usgs.gov","orcid":"https://orcid.org/0000-0003-3944-7769","contributorId":2518,"corporation":false,"usgs":true,"family":"Mech","given":"L.","email":"david_mech@usgs.gov","middleInitial":"David","affiliations":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"preferred":true,"id":642274,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"MacNulty, Daniel R.","contributorId":64069,"corporation":false,"usgs":true,"family":"MacNulty","given":"Daniel","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":642277,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Stahler, Daniel R.","contributorId":57703,"corporation":false,"usgs":true,"family":"Stahler","given":"Daniel","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":642278,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Metz, Matthew C.","contributorId":172854,"corporation":false,"usgs":false,"family":"Metz","given":"Matthew","email":"","middleInitial":"C.","affiliations":[{"id":27103,"text":"Yellowston Wolf Project","active":true,"usgs":false}],"preferred":false,"id":642279,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}} ,{"id":70173803,"text":"pp1812 - 2016 - Eruptive history of Mammoth Mountain and its mafic periphery, California","interactions":[],"lastModifiedDate":"2017-01-05T10:07:20","indexId":"pp1812","displayToPublicDate":"2016-07-13T00:00:00","publicationYear":"2016","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1812","title":"Eruptive history of Mammoth Mountain and its mafic periphery, California","docAbstract":"This report and accompanying geologic map portray the eruptive history of Mammoth Mountain and a surrounding array of contemporaneous volcanic units that erupted in its near periphery. The moderately alkaline Mammoth eruptive suite, basaltic to rhyodacitic, represents a discrete new magmatic system, less than 250,000 years old, that followed decline of the subalkaline rhyolitic system active beneath adjacent Long Valley Caldera since 2.2 Ma (Hildreth, 2004). The scattered vent array of the Mammoth system, 10 by 20 km wide, is unrelated to the rangefront fault zone, and its broad nonlinear footprint ignores both Long Valley Caldera and the younger Mono-Inyo rangefront vent alignment.
\nThe Mammoth Lakes area of Mono County, owing to its spectacular alpine landscape, has become one of California’s busiest recreational playgrounds and a regional center of real estate development. The name applies to the town of Mammoth Lakes as well as to the cluster of lakes in a large cirque southwest of town that is now locally called the Lakes Basin. The town has spread around the eastern base of Mammoth Mountain, a late Pleistocene pile of silicic lava domes, and has locally expanded onto lower slopes of the mountain itself (fig. 1). Looming nearly 1,000 m above the downtown area, much of the 5-km-wide volcanic edifice has been laced with chair lifts, gondolas, ski runs, and bike paths by the Mammoth Mountain Ski Area, a corporate entity under permit from Inyo National Forest. In addition to skiing, longestablished, snowboarding and summertime mountain biking have recently become major activities. Tourism to Mammoth Lakes is estimated to be 1,300,000 visitors per winter and 1,500,000 per summer. Some of America’s top long-distance runners also live and train in Mammoth Lakes, attracted by its elevation and its variety of challenging trails.
\nAt the western base of Mammoth Mountain, along the canyon of the Middle Fork San Joaquin River, lies the Devils Postpile National Monument, a National Park Service enclave surrounded by extensive wilderness areas administered by the U.S. Forest Service. As many as 2,000 visitors per day enter the monument during the summer season. The area also contains several of the busiest trailheads in the Sierra Nevada, providing wilderness access for hikers, pack animals, mountaineers, and fishermen.
\nMany geographic names that appear in this report are informal despite having been in local use for decades. Most appear on maps distributed by the Town of Mammoth Lakes or the Mammoth Mountain Ski Area and can be found here on map figures 2–5, on several photo figures, and on the geologic map.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/pp1812","usgsCitation":"Hildreth, Wes, and Fierstein, Judy, 2016, Eruptive history of Mammoth Mountain and its mafic periphery, California: U.S. Geological Survey Professional Paper 1812, 128 p., 2 plates, scale 1:24,000, https://www.dx.doi.org/10.3133/pp1812. ","productDescription":"Pamphlet: vi, 128 p.; 2 Plates: 52.28 x 50.79 inches and 46.27 x 38.77 inches; Appendix; Metadata; Read Me; Spatial Data","numberOfPages":"138","onlineOnly":"N","additionalOnlineFiles":"Y","ipdsId":"IP-046206","costCenters":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"links":[{"id":325069,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1812/pp1812_plate1.pdf","text":"Plate 1","size":"11 MB","linkFileType":{"id":1,"text":"pdf"},"description":"PP 1812 Plate 1"},{"id":325068,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1812/pp1812_pamphlet.pdf","text":"Pamphlet","size":"27.8 MB","linkFileType":{"id":1,"text":"pdf"},"description":"PP 1812 Pamphlet"},{"id":325070,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1812/pp1812_plate2.pdf","text":"Plate 2","size":"4.9 MB","linkFileType":{"id":1,"text":"pdf"},"description":"PP 1812 Plate 2"},{"id":325071,"rank":5,"type":{"id":3,"text":"Appendix"},"url":"https://pubs.usgs.gov/pp/1812/pp1812_appendix.xls","text":"Appendix","size":"474 KB","linkFileType":{"id":3,"text":"xlsx"},"description":"PP 1812 Appendix"},{"id":325067,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1812/coverthb.jpg"},{"id":329500,"rank":6,"type":{"id":23,"text":"Spatial Data"},"url":"https://pubs.usgs.gov/pp/1812/pp1812_mammothmountain.zip","text":"Database","size":"213.7 MB","linkFileType":{"id":6,"text":"zip"},"description":"PP 1812 Spatial Data"},{"id":329501,"rank":7,"type":{"id":20,"text":"Read Me"},"url":"https://pubs.usgs.gov/pp/1812/pp1812_readme.txt","size":"3 KB","linkFileType":{"id":2,"text":"txt"},"description":"PP 1812 Read Me"},{"id":329502,"rank":8,"type":{"id":16,"text":"Metadata"},"url":"https://pubs.usgs.gov/pp/1812/pp1812_mammothmountain.txt","text":"Data","size":"21 KB","linkFileType":{"id":2,"text":"txt"},"description":"PP 1812 Metadata"},{"id":329503,"rank":9,"type":{"id":16,"text":"Metadata"},"url":"https://pubs.usgs.gov/pp/1812/pp1812_topo_base_NAD83_FGDC.txt","text":"Base Map","size":"11 KB","linkFileType":{"id":2,"text":"txt"},"description":"PP 1812 Base Map Metadata"}],"country":"United States","state":"California","otherGeospatial":"Mammoth Mountain","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -119.27307128906249,\n 37.53368798315969\n ],\n [\n -119.27307128906249,\n 37.96477144899956\n ],\n [\n -118.52462768554686,\n 37.96477144899956\n ],\n [\n -118.52462768554686,\n 37.53368798315969\n ],\n [\n -119.27307128906249,\n 37.53368798315969\n ]\n ]\n ]\n }\n }\n ]\n}","contact":"Contact Information, Volcano Science Center - Menlo Park
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345 Middlefield Road, MS 910
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http://volcanoes.usgs.gov/
Alaska, the largest State within the United States, and mainly located north of latitude 60°, is an important part of the Circum-Arctic region. Alaska is a richly endowed region with a long and complex geologic history. The mining history is short by world standards but nevertheless there are a number of world-class deposits in Alaska, of which Red Dog and Pebble are among the largest of their respective types in the world.
Alaska is a collection of geologic terranes or regions having distinct histories, most of which were tectonically assembled in the period from 400 million years to 50 million years ago (late Paleozoic through early Tertiary). They now occur as numerous fault-bounded blocks in the northernmost part of the North American Cordillera on the western margin of the Laurentian craton. These terranes are comprised of rocks ranging in age from Paleoproterozoic to Recent.
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Mineral resources in the Arctic","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Geological Survey of Norway","publisherLocation":"Trondheim, Norway","isbn":"978-82-7385-160-4","usgsCitation":"Goldfarb, R.J., Meighan, C.J., Meinert, L.D., and Wilson, F.H., 2016, Mineral deposits and metallogeny of Alaska, chap. of Mineral resources in the Arctic, p. 12-20.","productDescription":"9 p.","startPage":"12","endPage":"20","ipdsId":"IP-070451","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"links":[{"id":342974,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":342973,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://www.ngu.no/en/publikasjon/mineral-resources-arctic"}],"country":"United 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Center","active":true,"usgs":true}],"preferred":true,"id":700524,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Meinert, Lawrence D. lmeinert@usgs.gov","contributorId":1639,"corporation":false,"usgs":true,"family":"Meinert","given":"Lawrence","email":"lmeinert@usgs.gov","middleInitial":"D.","affiliations":[{"id":387,"text":"Mineral Resources Program","active":true,"usgs":true}],"preferred":true,"id":700525,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Wilson, Frederic H. 0000-0003-1761-6437 fwilson@usgs.gov","orcid":"https://orcid.org/0000-0003-1761-6437","contributorId":67174,"corporation":false,"usgs":true,"family":"Wilson","given":"Frederic","email":"fwilson@usgs.gov","middleInitial":"H.","affiliations":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":119,"text":"Alaska Science Center Geology Minerals","active":true,"usgs":true}],"preferred":true,"id":700523,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70188883,"text":"70188883 - 2016 - GIS methodology for geothermal play fairway analysis: Example from the Snake River Plain volcanic province","interactions":[],"lastModifiedDate":"2017-06-27T13:33:24","indexId":"70188883","displayToPublicDate":"2016-07-13T00:00:00","publicationYear":"2016","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"GIS methodology for geothermal play fairway analysis: Example from the Snake River Plain volcanic province","docAbstract":"Play fairway analysis in geothermal exploration derives from a systematic methodology originally developed within the petroleum industry and is based on a geologic and hydrologic framework of identified geothermal systems. We are tailoring this methodology to study the geothermal resource potential of the Snake River Plain and surrounding region. This project has contributed to the success of this approach by cataloging the critical elements controlling exploitable hydrothermal systems, establishing risk matrices that evaluate these elements in terms of both probability of success and level of knowledge, and building automated tools to process results. ArcGIS was used to compile a range of different data types, which we refer to as ‘elements’ (e.g., faults, vents, heatflow…), with distinct characteristics and confidence values.
Raw data for each element were transformed into data layers with a common format. Because different data types have different uncertainties, each evidence layer had an accompanying confidence layer, which reflects spatial variations in these uncertainties. Risk maps represent the product of evidence and confidence layers, and are the basic building blocks used to construct Common Risk Segment (CRS) maps for heat, permeability, and seal. CRS maps quantify the variable risk associated with each of these critical components. In a final step, the three CRS maps were combined into a Composite Common Risk Segment (CCRS) map for analysis that reveals favorable areas for geothermal exploration.
Python scripts were developed to automate data processing and to enhance the flexibility of the data analysis. Python scripting provided the structure that makes a custom workflow possible. Nearly every tool available in the ArcGIS ArcToolbox can be executed using commands in the Python programming language. This enabled the construction of a group of tools that could automate most of the processing for the project. Currently, our tools are repeatable, scalable, modifiable, and transferrable, allowing us to automate the task of data analysis and the production of CRS and CCRS maps. Our ultimate goal is to produce a toolkit that can be imported into ArcGIS and applied to any geothermal play type, with fully tunable parameters that will allow for the production of multiple versions of the CRS and CCRS maps in order to better test for sensitivity and to validate results.
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Proceedings, 41st Workshop on Geothermal Reservoir Engineering","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"41st Workshop on Geothermal Reservoir Engineering","conferenceDate":"February 22-24, 2016","conferenceLocation":"Stanford, CA","language":"English","publisher":"Stanford University","publisherLocation":"Stanford, CA","usgsCitation":"DeAngelo, J., Shervais, J.W., Glen, J.M., Nielson, D.L., Garg, S., Dobson, P., Gasperikova, E., Sonnenthal, E., Visser, C., Liberty, L.M., Siler, D., Evans, J.P., and Santellanes, S., 2016, GIS methodology for geothermal play fairway analysis: Example from the Snake River Plain volcanic province, in Proceedings, 41st Workshop on Geothermal Reservoir Engineering, Stanford, CA, February 22-24, 2016, 10 p.","productDescription":"10 p.","ipdsId":"IP-070241","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science 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Sabodh","contributorId":193564,"corporation":false,"usgs":false,"family":"Garg","given":"Sabodh","email":"","affiliations":[],"preferred":false,"id":700822,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Dobson, Patrick","contributorId":193558,"corporation":false,"usgs":false,"family":"Dobson","given":"Patrick","email":"","affiliations":[],"preferred":false,"id":700815,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Gasperikova, Erika","contributorId":193561,"corporation":false,"usgs":false,"family":"Gasperikova","given":"Erika","affiliations":[],"preferred":false,"id":700818,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Sonnenthal, Eric","contributorId":146807,"corporation":false,"usgs":false,"family":"Sonnenthal","given":"Eric","affiliations":[],"preferred":false,"id":700819,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Visser, Charles","contributorId":193562,"corporation":false,"usgs":false,"family":"Visser","given":"Charles","email":"","affiliations":[],"preferred":false,"id":700820,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Liberty, Lee M.","contributorId":89631,"corporation":false,"usgs":true,"family":"Liberty","given":"Lee","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":700817,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Siler, Drew","contributorId":193559,"corporation":false,"usgs":false,"family":"Siler","given":"Drew","affiliations":[],"preferred":false,"id":700816,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Evans, James P.","contributorId":53760,"corporation":false,"usgs":true,"family":"Evans","given":"James","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":700823,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Santellanes, Sean","contributorId":193566,"corporation":false,"usgs":false,"family":"Santellanes","given":"Sean","email":"","affiliations":[],"preferred":false,"id":700824,"contributorType":{"id":1,"text":"Authors"},"rank":13}]}} ,{"id":70188890,"text":"70188890 - 2016 - Aeromagnetic map of northwest Utah and adjacent parts of Nevada and Idaho","interactions":[],"lastModifiedDate":"2025-02-25T15:22:21.086949","indexId":"70188890","displayToPublicDate":"2016-07-13T00:00:00","publicationYear":"2016","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5437,"text":"Utah Geological Survey Miscellaneous Publication","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"16-4","title":"Aeromagnetic map of northwest Utah and adjacent parts of Nevada and Idaho","docAbstract":"Two aeromagnetic surveys were flown to promote further understanding of the geology and structure in northwest Utah and adjacent parts of Nevada and Idaho by serving as a basis for geophysical interpretations and by supporting geological mapping, water and mineral resource investigations, and other topical studies. Although this area is in general sparsely populated, (except for cities and towns along the Wasatch Front such as Ogden and Brigham City), it encompasses metamorphic core complexes in the Grouse Creek and Raft River Mountains (figure 1) of interest to earth scientists studying Cenozoic extension. The region was shaken in 1909 and 1934 by M6+ earthquakes east of the Hansel Mountains (Doser, 1989; Arabasz and others, 1994); damage from the 1934 earthquake occurred as far east as Logan, Utah (http:// www.seis.utah.edu/lqthreat/nehrp_htm/1934hans/n1934ha1. shtml#urbse). The presence of Quaternary shield volcanoes and bimodal Pleistocene volcanism in Curlew Valley (Miller and others, 1995; Felger and others, 2016) as well as relatively high temperature gradients encountered in the Indian Cove drillhole in the north arm of Great Salt Lake (Blackett and others, 2014) may indicate some potential for geothermal energy development in the area (Miller and others, 1995). The area also hosts four significant mining districts, in the northern Pilot Range, the Goose Creek Mountains in the northwest corner of the map, the southern end of the Promontory Mountains, and the southwest part of the Raft River Mountains, although production notably waned after World War II (Doelling, 1980). Other prospects of interest include those in the southern Grouse Creek Mountains, Silver Island, and the northern Newfoundland Mountains.
Large areas of northwest Utah are covered by young, surficial deposits or by Great Salt Lake or are down-dropped into deep Cenozoic basins, making extrapolation of bedrock geology from widely spaced exposures difficult or tenuous (figure 1). Local spatial variations in the Earth's magnetic field (evident as anomalies on aeromagnetic maps) reflect the distribution of magnetic minerals, primarily magnetite, in the underlying rocks. In many cases the volume content of magnetic minerals can be related to rock type, and abrupt spatial changes in the amount of magnetic minerals commonly mark lithologic or structural boundaries. Magnetic data reflect magnetization variations within the crust and are well suited for mapping the distribution of mafic igneous rocks, although felsic igneous rocks, some mineralized zones, and other rock types also can produce measurable magnetic anomalies. For these reasons, the U.S. Geological Survey (USGS) and Utah Geological Survey (UGS) contracted for the collection of aeromagnetic data in this area.
","language":"English","publisher":"Utah Geological Survey","publisherLocation":"Salt Lake City, UT","doi":"10.34191/MP-16-4","isbn":"978-1-55791-931-1","collaboration":"Prepared in cooperation with U.S. Department of the Interior, U.S. Geological Survey","usgsCitation":"Langenheim, V., 2016, Aeromagnetic map of northwest Utah and adjacent parts of Nevada and Idaho: Utah Geological Survey Miscellaneous Publication 16-4, 13 p., https://doi.org/10.34191/MP-16-4.","productDescription":"13 p.","ipdsId":"IP-073411","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":342956,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Idaho, Nevada, Utah","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -114.141667,\n 42.041667\n ],\n [\n -111.916667,\n 42.041667\n ],\n [\n -111.916667,\n 40.858333\n ],\n [\n -114.141667,\n 40.858333\n ],\n [\n -114.141667,\n 42.041667\n ]\n ]\n ]\n }\n }\n ]\n}","publishingServiceCenter":{"id":14,"text":"Menlo Park PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"59536ea7e4b062508e3c7a75","contributors":{"authors":[{"text":"Langenheim, Victoria E. 0000-0003-2170-5213 zulanger@usgs.gov","orcid":"https://orcid.org/0000-0003-2170-5213","contributorId":151042,"corporation":false,"usgs":true,"family":"Langenheim","given":"Victoria E.","email":"zulanger@usgs.gov","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":700845,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70189147,"text":"70189147 - 2016 - A synthesis of Jurassic and Early Cretaceous crustal evolution along the southern margin of the Arctic Alaska–Chukotka microplate and implications for defining tectonic boundaries active during opening of Arctic Ocean basins","interactions":[],"lastModifiedDate":"2019-12-21T08:26:10","indexId":"70189147","displayToPublicDate":"2016-07-13T00:00:00","publicationYear":"2016","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2626,"text":"Lithosphere","active":true,"publicationSubtype":{"id":10}},"title":"A synthesis of Jurassic and Early Cretaceous crustal evolution along the southern margin of the Arctic Alaska–Chukotka microplate and implications for defining tectonic boundaries active during opening of Arctic Ocean basins","docAbstract":"A synthesis of Late Jurassic and Early Cretaceous collision-related metamorphic events in the Arctic Alaska–Chukotka microplate clarifies its likely movement history during opening of the Amerasian and Canada basins. Comprehensive tectonic reconstructions of basin opening have been problematic, in part, because of the large size of the microplate, uncertainties in the location and kinematics of structures bounding the microplate, and lack of information on its internal deformation history. Many reconstructions have treated Arctic Alaska and Chukotka as a single crustal entity largely on the basis of similarities in their Mesozoic structural trends and similar late Proterozoic and early Paleozoic histories. Others have located Chukotka near Siberia during the Triassic and Jurassic, on the basis of detrital zircon age populations, and suggested that it was Arctic Alaska alone that rotated. The Mesozoic metamorphic histories of Arctic Alaska and Chukotka can be used to test the validity of these two approaches.
A synthesis of the distribution, character, and timing of metamorphic events reveals substantial differences in the histories of the southern margin of the microplate in Chukotka in comparison to Arctic Alaska and places specific limitations on tectonic reconstructions. During the Late Jurassic and earliest Cretaceous, the Arctic Alaska margin was subducted to the south, while the Chukotka margin was the upper plate of a north-dipping subduction zone or a zone of transpression. An early Aptian blueschist- and greenschist-facies belt records the most profound crustal thickening event in the evolution of the orogen. It may have resulted in thicknesses of 50–60 km and was likely the cause of flexural subsidence in the foredeep of the Brooks Range. This event involved northern Alaska and northeasternmost Chukotka; it did not involve central and western Chukotka. Arctic Alaska and Chukotka evolved separately until the Aptian thickening event, which was likely a result of the rotation of Arctic Alaska into central and western Chukotka. In northeastern Chukotka, the thickened rocks are separated from the relatively little thickened continental crust of the remainder of Chukotka by the oceanic rocks of the Kolyuchin-Mechigmen zone. The zone is a candidate for an Early Cretaceous suture that separated most of Chukotka from northeast Chukotka and Alaska. Albian patterns of magmatism, metamorphism, and deformation in Chukotka and the Seward Peninsula may represent an example of escape tectonics that developed in response to final amalgamation of Chukotka with Eurasia.
","language":"English","publisher":"Geological Society of America","doi":"10.1130/L471.1","usgsCitation":"Till, A.B., 2016, A synthesis of Jurassic and Early Cretaceous crustal evolution along the southern margin of the Arctic Alaska–Chukotka microplate and implications for defining tectonic boundaries active during opening of Arctic Ocean basins: Lithosphere, v. 8, no. 2, p. 219-237, https://doi.org/10.1130/L471.1.","productDescription":"19 p.","startPage":"219","endPage":"237","ipdsId":"IP-071854","costCenters":[{"id":119,"text":"Alaska Science Center Geology Minerals","active":true,"usgs":true}],"links":[{"id":470755,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1130/l471.1","text":"Publisher Index Page"},{"id":343262,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Russia, United States","otherGeospatial":"Arctic Alaska-Chukotka microplate","volume":"8","issue":"2","publishingServiceCenter":{"id":12,"text":"Tacoma PSC"},"noUsgsAuthors":false,"publicationDate":"2016-03-03","publicationStatus":"PW","scienceBaseUri":"595b5798e4b0d1f9f0536db8","contributors":{"authors":[{"text":"Till, Alison B. atill@usgs.gov","contributorId":2482,"corporation":false,"usgs":true,"family":"Till","given":"Alison","email":"atill@usgs.gov","middleInitial":"B.","affiliations":[{"id":119,"text":"Alaska Science Center Geology Minerals","active":true,"usgs":true}],"preferred":true,"id":703161,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70189730,"text":"70189730 - 2016 - Research on Golden-winged Warblers: Recent progress and current needs","interactions":[],"lastModifiedDate":"2020-08-25T18:22:31.41003","indexId":"70189730","displayToPublicDate":"2016-07-13T00:00:00","publicationYear":"2016","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"seriesTitle":{"id":5103,"text":"Studies in Avian Biology","printIssn":"0197-9922","active":true,"publicationSubtype":{"id":24}},"chapter":"14","title":"Research on Golden-winged Warblers: Recent progress and current needs","docAbstract":"Considerable advances have been made in knowledge about Golden-winged Warblers (Vermivora chrysoptera) in the past decade. Recent employment of molecular analysis, stable-isotope analysis, telemetry-based monitoring of survival and behavior, and spatially explicit modeling techniques have added to, and revised, an already broad base of published knowledge. Here, we synthesize findings primarily from recent peer-reviewed literature on Golden-winged Warblers, from this volume and elsewhere, and we identify some of the substantial remaining research needs. We have organized this synthesis by stages of the Golden-winged Warbler annual cycle. First, we discuss the relatively well-studied breeding-grounds ecology including nesting and post-fledging ecology and hybridization with closely related Blue-winged Warblers (Vermivora cyanoptera). Second, we discuss the much-less-studied, non-breeding-grounds ecology, including the first empirical studies of non-breeding-grounds cover-type associations and spatial and social behavioral ecology. Third, we address migratory connectivity and migration ecology, for which little is known and research has only just begun. Last, we close with cautious optimism that current knowledge is adequate to inform initial conservation and management plans for Golden-winged Warblers, and with a sobering acknowledgement of the quantity of research still needed.
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Golden-winged Warbler ecology, conservation, and habitat management (Studies in Avian Biology, volume 49)","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"CRC Press","publisherLocation":"Boca Raton, FL","isbn":"978-1-4822-4068-9","usgsCitation":"Streby, H.M., Rohrbaugh, R.W., Buehler, D.A., Andersen, D., Vallender, R., King, D.I., and Will, T., 2016, Research on Golden-winged Warblers: Recent progress and current needs, chap. 14 of Golden-winged Warbler ecology, conservation, and habitat management (Studies in Avian Biology, volume 49): Studies in Avian Biology, v. 49, p. 217-227.","productDescription":"11 p.","startPage":"217","endPage":"227","ipdsId":"IP-059592","costCenters":[{"id":199,"text":"Coop Res Unit Leetown","active":true,"usgs":true}],"links":[{"id":344213,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":344211,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://hdl.handle.net/11299/189700"}],"volume":"49","publishingServiceCenter":{"id":9,"text":"Reston PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"597312ade4b0ec1a488718ed","contributors":{"authors":[{"text":"Streby, Henry M.","contributorId":11024,"corporation":false,"usgs":false,"family":"Streby","given":"Henry","email":"","middleInitial":"M.","affiliations":[{"id":12455,"text":"University of Toledo","active":true,"usgs":false}],"preferred":false,"id":705967,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rohrbaugh, Roland W.","contributorId":194965,"corporation":false,"usgs":false,"family":"Rohrbaugh","given":"Roland","email":"","middleInitial":"W.","affiliations":[{"id":27615,"text":"Cornell Lab of Ornithology, Conservation Science Program","active":true,"usgs":false}],"preferred":false,"id":705968,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Buehler, David A.","contributorId":176238,"corporation":false,"usgs":false,"family":"Buehler","given":"David","email":"","middleInitial":"A.","affiliations":[{"id":12716,"text":"University of Tennessee","active":true,"usgs":false}],"preferred":false,"id":705969,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Andersen, David E. 0000-0001-9535-3404 dea@usgs.gov","orcid":"https://orcid.org/0000-0001-9535-3404","contributorId":2168,"corporation":false,"usgs":true,"family":"Andersen","given":"David E.","email":"dea@usgs.gov","affiliations":[{"id":34539,"text":"Minnesota Cooperative Fish and Wildlife Research Unit","active":true,"usgs":false},{"id":199,"text":"Coop Res Unit Leetown","active":true,"usgs":true}],"preferred":true,"id":705966,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Vallender, Rachel","contributorId":194966,"corporation":false,"usgs":false,"family":"Vallender","given":"Rachel","email":"","affiliations":[{"id":27312,"text":"Canadian Wildlife Service, Environment and Climate Change Canada, 6 Bruce Street, Mount","active":true,"usgs":false},{"id":34540,"text":"Canadian Museum of Nature","active":true,"usgs":false}],"preferred":false,"id":705970,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"King, David I.","contributorId":34390,"corporation":false,"usgs":false,"family":"King","given":"David","email":"","middleInitial":"I.","affiliations":[{"id":18918,"text":"Department of Environmental Conservation, University of Massachusetts, Amherst, MA, 01003, USA","active":true,"usgs":false},{"id":13259,"text":"USDA Forest Service Northern Research Station","active":true,"usgs":false}],"preferred":false,"id":705971,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Will, Tom","contributorId":149777,"corporation":false,"usgs":false,"family":"Will","given":"Tom","email":"","affiliations":[{"id":17821,"text":"U.S. Fish and Wildlife Service, Division of Migratory Birds","active":true,"usgs":false}],"preferred":false,"id":705972,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}} ,{"id":70187102,"text":"70187102 - 2016 - Conservation of avian species","interactions":[],"lastModifiedDate":"2020-08-25T18:24:18.094518","indexId":"70187102","displayToPublicDate":"2016-07-13T00:00:00","publicationYear":"2016","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"chapter":"23","title":"Conservation of avian species","docAbstract":"Health of humans, animals, plants, and ecosystems are intertwined. Disturbance tips the balance in favor of weedy species, vectors, and disease agents. Biodiversity is important to prevent imbalance in nature. However, more scholarship is needed, and there is still much more to study, understand, and manage than we currently know.
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Current therapy in avian medicine and surgery","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Elsevier","publisherLocation":"St. Louis, MO","doi":"10.1016/B978-1-4557-4671-2.00032-X","usgsCitation":"Olsen, G.H., Crosta, L., Gartrell, B.D., Marsh, P., and Stringfield, C.E., 2016, Conservation of avian species, chap. 23 of Current therapy in avian medicine and surgery, p. 719-748, https://doi.org/10.1016/B978-1-4557-4671-2.00032-X.","productDescription":"30 p.","startPage":"719","endPage":"748","ipdsId":"IP-062990","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":340095,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"publishingServiceCenter":{"id":10,"text":"Baltimore PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58fb1a4ce4b0c3010a8087bf","contributors":{"authors":[{"text":"Olsen, Glenn H. 0000-0002-7188-6203 golsen@usgs.gov","orcid":"https://orcid.org/0000-0002-7188-6203","contributorId":40918,"corporation":false,"usgs":true,"family":"Olsen","given":"Glenn","email":"golsen@usgs.gov","middleInitial":"H.","affiliations":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"preferred":false,"id":692422,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Crosta, Lorenzo","contributorId":191236,"corporation":false,"usgs":false,"family":"Crosta","given":"Lorenzo","email":"","affiliations":[],"preferred":false,"id":692434,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gartrell, Brett D.","contributorId":10299,"corporation":false,"usgs":false,"family":"Gartrell","given":"Brett","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":692435,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Marsh, Philip M.","contributorId":191237,"corporation":false,"usgs":false,"family":"Marsh","given":"Philip M.","affiliations":[],"preferred":false,"id":692436,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Stringfield, Cynthia E.","contributorId":191238,"corporation":false,"usgs":false,"family":"Stringfield","given":"Cynthia","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":692437,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":70178039,"text":"70178039 - 2016 - Are we preparing the next generation of fisheries professionals to succeed in their careers?: A survey of AFS members","interactions":[],"lastModifiedDate":"2018-02-28T14:33:44","indexId":"70178039","displayToPublicDate":"2016-07-13T00:00:00","publicationYear":"2016","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1657,"text":"Fisheries","onlineIssn":"1548-8446","printIssn":"0363-2415","active":true,"publicationSubtype":{"id":10}},"title":"Are we preparing the next generation of fisheries professionals to succeed in their careers?: A survey of AFS members","docAbstract":"Natural resource professionals have frequently criticized universities for poorly preparing graduates to succeed in their jobs. We surveyed members of the American Fisheries Society to determine which job skills and knowledge of academic topics employers, students, and university faculty members deemed most important to early-career success of fisheries professionals. Respondents also rated proficiency of recently hired, entry-level professionals (employers) on how well their programs prepared them for career success (students and faculty) in those same job skills and academic topics. Critical thinking and written and oral communication skills topped the list of important skills and academic topics. Employers perceived recent entry-level hires to be less well-prepared to succeed in their careers than either university faculty or students. Entry-level hires with post-graduate degrees rated higher in proficiency for highly important skills and knowledge than those with bachelor's degrees. We conclude that although universities have the primary responsibility for developing critical thinking and basic communication skills of students, employers have equal or greater responsibility for enhancing skills of employees in teamwork, field techniques, and communicating with stakeholders. The American Fisheries Society can significantly contribute to the preparation of young fisheries professionals by providing opportunities for continuing education and networking with peers at professional conferences.
","language":"English","publisher":"American Fisheries Society","publisherLocation":"Bethesda, MD","doi":"10.1080/03632415.2016.1199218","usgsCitation":"McMullin, S.L., DiCenzo, V., Essig, R., Bonds, C., DeBruyne, R.L., Kaemingk, M.A., Mather, M.E., Myrick, C.A., Phelps, Q.E., Sutton, T.M., and Triplett, J., 2016, Are we preparing the next generation of fisheries professionals to succeed in their careers?: A survey of AFS members: Fisheries, v. 41, no. 8, p. 436-449, https://doi.org/10.1080/03632415.2016.1199218.","productDescription":"14 p.","startPage":"436","endPage":"449","numberOfPages":"14","ipdsId":"IP-069045","costCenters":[{"id":198,"text":"Coop Res Unit Atlanta","active":true,"usgs":true}],"links":[{"id":330599,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"41","issue":"8","publishingServiceCenter":{"id":8,"text":"Raleigh PSC"},"noUsgsAuthors":false,"publicationDate":"2016-08-02","publicationStatus":"PW","scienceBaseUri":"5819a9c3e4b0bb36a4c9101f","contributors":{"authors":[{"text":"McMullin, Steve L.","contributorId":176514,"corporation":false,"usgs":false,"family":"McMullin","given":"Steve","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":652636,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"DiCenzo, Vic","contributorId":176515,"corporation":false,"usgs":false,"family":"DiCenzo","given":"Vic","email":"","affiliations":[],"preferred":false,"id":652637,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Essig, Ron","contributorId":176516,"corporation":false,"usgs":false,"family":"Essig","given":"Ron","email":"","affiliations":[],"preferred":false,"id":652638,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bonds, Craig","contributorId":176517,"corporation":false,"usgs":false,"family":"Bonds","given":"Craig","email":"","affiliations":[],"preferred":false,"id":652639,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"DeBruyne, Robin L. 0000-0002-9232-7937 rdebruyne@usgs.gov","orcid":"https://orcid.org/0000-0002-9232-7937","contributorId":4936,"corporation":false,"usgs":true,"family":"DeBruyne","given":"Robin","email":"rdebruyne@usgs.gov","middleInitial":"L.","affiliations":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"preferred":true,"id":652640,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Kaemingk, Mark A.","contributorId":40510,"corporation":false,"usgs":true,"family":"Kaemingk","given":"Mark","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":652641,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Mather, Martha E. 0000-0003-3027-0215 mather@usgs.gov","orcid":"https://orcid.org/0000-0003-3027-0215","contributorId":2580,"corporation":false,"usgs":true,"family":"Mather","given":"Martha","email":"mather@usgs.gov","middleInitial":"E.","affiliations":[{"id":200,"text":"Coop Res Unit Seattle","active":true,"usgs":true},{"id":198,"text":"Coop Res Unit Atlanta","active":true,"usgs":true}],"preferred":true,"id":652642,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Myrick, Christopher A.","contributorId":78559,"corporation":false,"usgs":true,"family":"Myrick","given":"Christopher","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":652643,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Phelps, Quinton E.","contributorId":173401,"corporation":false,"usgs":false,"family":"Phelps","given":"Quinton","email":"","middleInitial":"E.","affiliations":[{"id":27224,"text":"Big Rivers and Wetlands Field Station, Missouri Department of Conservation, Jackson, MO","active":true,"usgs":false}],"preferred":false,"id":652644,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Sutton, Trent M.","contributorId":77893,"corporation":false,"usgs":false,"family":"Sutton","given":"Trent","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":652645,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Triplett, James","contributorId":93565,"corporation":false,"usgs":true,"family":"Triplett","given":"James","email":"","affiliations":[],"preferred":false,"id":652646,"contributorType":{"id":1,"text":"Authors"},"rank":11}]}} ,{"id":70170883,"text":"70170883 - 2016 - Planning and setting objectives in field studies: Chapter 2","interactions":[],"lastModifiedDate":"2016-07-12T16:08:40","indexId":"70170883","displayToPublicDate":"2016-07-12T17:00:00","publicationYear":"2016","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Planning and setting objectives in field studies: Chapter 2","docAbstract":"","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Reptile ecology and conservation","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Oxford University Press","doi":"10.1093/acprof:oso/9780198726135.003.0002","isbn":"9780198726135","usgsCitation":"Fisher, R.N., 2016, Planning and setting objectives in field studies: Chapter 2, chap. of Reptile ecology and conservation, https://doi.org/10.1093/acprof:oso/9780198726135.003.0002.","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-066473","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":325126,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":321035,"type":{"id":15,"text":"Index Page"},"url":"https://global.oup.com/academic/product/reptile-ecology-and-conservation-9780198726135?cc=us&lang=en&#"}],"publishingServiceCenter":{"id":1,"text":"Sacramento PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"579dc1b1e4b0589fa1cb7e6e","contributors":{"editors":[{"text":"Dodd, C. 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We applied PCA-EMMA in 10 watersheds located in Indiana, Iowa, Maryland, Nebraska, Mississippi, and Washington ranging in size from 5 to 1254 km2 with four nested watersheds. Watershed Surplus N was determined by subtracting estimates of crop uptake and volatilization from estimates of N input from atmospheric deposition, plant fixation, fertilizer, and manure for the period from 1987 to 2004. Watershed average Surplus N ranged from 11 to 52 kg N ha−1 and from 9 to 32% of N input. Solute concentrations in streams, overland runoff, tile drainage, groundwater (GW), streambeds, and the unsaturated zone were used in the PCA-EMMA procedure to identify independent components contributing to observed stream concentration variability and the end-members contributing to streamflow and NO3 load. End-members included dilute runoff, agricultural runoff, benthic-processing, tile drainage, and oxic and anoxic GW. Surplus N was larger in watersheds with more permeable soils (Washington, Nebraska, and Maryland) that allowed greater infiltration, and oxic GW was the primary source of NO3 load. Subsurface transport of NO3 in these watersheds resulted in some removal of Surplus N by denitrification. In less permeable watersheds (Iowa, Indiana, and Mississippi), NO3 was rapidly transported to the stream by tile drainage and runoff with little removal. Evidence of streambed removal of NO3 by benthic diatoms was observed in the larger watersheds.
","language":"English","publisher":"Alliance of Crop, Soil, and Environmental Science Societies","doi":"10.2134/jeq2016.02.0071","usgsCitation":"Essaid, H.I., Baker, N.T., and McCarthy, K.A., 2016, Contrasting nitrogen fate in watersheds using agricultural and water quality information: Journal of Environmental Quality, v. 45, no. 5, p. 1616-1626, https://doi.org/10.2134/jeq2016.02.0071.","productDescription":"11 p.","startPage":"1616","endPage":"1626","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-073514","costCenters":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"links":[{"id":325123,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Indiana, Iowa, Maryland, Nebraska, Mississippi, Washington","volume":"45","issue":"5","publishingServiceCenter":{"id":14,"text":"Menlo Park PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57934443e4b0eb1ce79e8be2","contributors":{"authors":[{"text":"Essaid, Hedeff I. 0000-0003-0154-8628 hiessaid@usgs.gov","orcid":"https://orcid.org/0000-0003-0154-8628","contributorId":2284,"corporation":false,"usgs":true,"family":"Essaid","given":"Hedeff","email":"hiessaid@usgs.gov","middleInitial":"I.","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":642225,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Baker, Nancy T. 0000-0002-7979-5744 ntbaker@usgs.gov","orcid":"https://orcid.org/0000-0002-7979-5744","contributorId":1955,"corporation":false,"usgs":true,"family":"Baker","given":"Nancy","email":"ntbaker@usgs.gov","middleInitial":"T.","affiliations":[{"id":27231,"text":"Indiana-Kentucky Water Science Center","active":true,"usgs":true},{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true},{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true},{"id":27111,"text":"National Water Quality Program","active":true,"usgs":true}],"preferred":true,"id":642226,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McCarthy, Kathleen A. mccarthy@usgs.gov","contributorId":1159,"corporation":false,"usgs":true,"family":"McCarthy","given":"Kathleen","email":"mccarthy@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":642227,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70175024,"text":"70175024 - 2016 - Spatial variation in biofouling of a unionid mussel (Lampsilis siliquoidea) across the western basin of Lake Erie","interactions":[],"lastModifiedDate":"2016-07-27T08:58:20","indexId":"70175024","displayToPublicDate":"2016-07-12T13:15:00","publicationYear":"2016","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5153,"text":"The American Midland Naturalist","active":true,"publicationSubtype":{"id":10}},"title":"Spatial variation in biofouling of a unionid mussel (Lampsilis siliquoidea) across the western basin of Lake Erie","docAbstract":"Invasion of North American waters by nonnative Dreissena polymorpha and D. rostriformis bugensishas resulted in declines of the Unionidae family of native North American mussels. Dreissenid mussels biofoul unionid mussels in large numbers and interfere with unionid movement, their acquisition of food, and the native mussels' ability to open and close their shells. Initial expectations for the Great Lakes included extirpation of unionids where they co-occurred with dreissenids, but recently adult and juvenile unionids have been found alive in several apparent refugia. These unionid populations may persist due to reduced dreissenid biofouling in these areas, and/or due to processes that remove biofoulers. For example locations inaccessible to dreissenid veligers may reduce biofouling and habitats with soft substrates may allow unionids to burrow and thus remove dreissenids. We deployed caged unionid mussels (Lampsilis siliquoidea) at 36 sites across the western basin of Lake Erie to assess spatial variation in biofouling and to identify other areas that might promote the persistence or recovery of native unionid mussels. Biofouling ranged from 0.03 – 26.33 g per mussel, reached a maximum in the immediate vicinity of the mouth of the Maumee River, and appeared to primarily consist of dreissenid mussels. A known mussel refugium in the vicinity of a power plant near the mouth of the Maumee actually exhibited very high biofouling rates, suggesting that low dreissenid colonization did not adequately explain unionid survival in this refugium. In contrast, the southern nearshore area of Lake Erie, near another refugium, had very low biofouling. A large stretch of the western basin appeared to have low biofouling rates and muddy substrates, raising the possibility that these open water areas could support remnant and returning populations of unionid mussels. Previous observations of unionid refugia and the occurrence of low biofouling rates in large areas of the western basin of Lake Erie raise the possibility that unionid and dreissenid coexistence may be possible here and elsewhere.
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2016 - Potential corrosivity of untreated groundwater in the United States","interactions":[],"lastModifiedDate":"2016-08-08T09:07:37","indexId":"sir20165092","displayToPublicDate":"2016-07-12T12:30:00","publicationYear":"2016","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":"2016-5092","title":"Potential corrosivity of untreated groundwater in the United States","docAbstract":"Corrosive groundwater, if untreated, can dissolve lead and other metals from pipes and other components in water distribution systems. Two indicators of potential corrosivity—the Langelier Saturation Index (LSI) and the Potential to Promote Galvanic Corrosion (PPGC)—were used to identify which areas in the United States might be more susceptible to elevated concentrations of metals in household drinking water and which areas might be less susceptible. On the basis of the LSI, about one-third of the samples collected from about 21,000 groundwater sites are classified as potentially corrosive. On the basis of the PPGC, about two-thirds of the samples collected from about 27,000 groundwater sites are classified as moderate PPGC, and about one-tenth as high PPGC. Potentially corrosive groundwater occurs in all 50 states and the District of Columbia.
National maps have been prepared to identify the occurrence of potentially corrosive groundwater in the 50 states and the District of Columbia. Eleven states and the District of Columbia were classified as having a very high prevalence of potentially corrosive groundwater, 14 states as having a high prevalence of potentially corrosive groundwater, 19 states as having a moderate prevalence of potentially corrosive groundwater, and 6 states as having a low prevalence of potentially corrosive groundwater. These findings have the greatest implication for people dependent on untreated groundwater for drinking water, such as the 44 million people that are self-supplied and depend on domestic wells or springs for their water supply.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20165092","usgsCitation":"Belitz, Kenneth, Jurgens, B.C., and Johnson, T.D., 2016, Potential corrosivity of untreated groundwater in the United States: U.S. Geological Survey Scientific Investigations Report 2016–5092, 16 p., https://dx.doi.org/10.3133/sir20165092. 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data release - Classification of chloride-to-sulfate mass ratio for U.S groundwater with respect to the Potential to Promote Galvanic Corrosion of lead, 1991–2015; Water well data and characteristic values for states","description":"SIR 2016-5092"},{"id":324828,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/sir/2016/5092/coverthb.jpg"},{"id":324830,"rank":3,"type":{"id":30,"text":"Data Release"},"url":"https://dx.doi.org/10.5066/F7XW4GWX","text":"USGS data release - Langelier Saturation Indices computed for U.S. groundwater, 1991–2015; Water well data and characteristic values for states","description":"SIR 2016-5092"},{"id":324829,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/sir/2016/5092/sir20165092.pdf","text":"Report","size":"3.98 MB","linkFileType":{"id":1,"text":"pdf"},"description":"SIR 2016-5092"}],"country":"United 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U.S. Geological Survey
Denver Federal Center
West 6th Avenue and Kipling Street
Lakewood, CO 80225
http://water.usgs.gov/nawqa/
The “Judas” technique is based on the idea that a radio-tagged individual can be used to “betray” conspecifics during the course of its routine social behavior. The Burmese python (Python bivittatus) is an invasive constrictor in southern Florida, and few methods are available for its control. Pythons are normally solitary, but from December–April in southern Florida, they form breeding aggregations containing up to 8 individuals, providing an opportunity to apply the technique. We radio-tracked 25 individual adult pythons of both sexes during the breeding season from 2007–2012. Our goals were to (1) characterize python movements and determine habitat selection for betrayal events, (2) quantify betrayal rates of Judas pythons, and (3) compare the efficacy of this tool with current tools for capturing pythons, both in terms of cost per python removed (CPP) and catch per unit effort (CPUE). In a total of 33 python-seasons, we had 8 betrayal events (24 %) in which a Judas python led us to new pythons. Betrayal events occurred more frequently in lowland forest (including tree islands) than would be expected by chance alone. These 8 events resulted in the capture of 14 new individuals (1–4 new pythons per event). Our effort comparison shows that while the Judas technique is more costly than road cruising surveys per python removed, the Judas technique yields more large, reproductive females and is effective at a time of year that road cruising is not, making it a potential complement to the status quo removal effort.
","language":"English","publisher":"Kluwer Academic Publishers","doi":"10.1007/s10530-016-1211-5","usgsCitation":"Smith, B.J., Cherkiss, M.S., Hart, K.M., Rochford, M., Selby, T.H., Snow, R., and Mazzotti, F., 2016, Betrayal: radio-tagged Burmese pythons reveal locations of conspecifics in Everglades National Park: Biological Invasions, v. 18, no. 11, p. 3239-3250, https://doi.org/10.1007/s10530-016-1211-5.","productDescription":"12 p.","startPage":"3239","endPage":"3250","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-070988","costCenters":[{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"links":[{"id":325095,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Florida","otherGeospatial":"Everglades National Park","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -81.221923828125,\n 25.095548539604252\n ],\n [\n -81.221923828125,\n 25.473033261279515\n ],\n [\n -80.37597656249999,\n 25.473033261279515\n ],\n [\n -80.37597656249999,\n 25.095548539604252\n ],\n [\n -81.221923828125,\n 25.095548539604252\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"18","issue":"11","publishingServiceCenter":{"id":5,"text":"Lafayette PSC"},"noUsgsAuthors":false,"publicationDate":"2016-07-05","publicationStatus":"PW","scienceBaseUri":"579dc1a1e4b0589fa1cb7d72","chorus":{"doi":"10.1007/s10530-016-1211-5","url":"http://dx.doi.org/10.1007/s10530-016-1211-5","publisher":"Springer Nature","authors":"Smith Brian J., Cherkiss Michael S., Hart Kristen M., Rochford Michael R., Selby Thomas H., Snow Ray W., Mazzotti Frank J.","journalName":"Biological Invasions","publicationDate":"7/5/2016","auditedOn":"2/15/2017","publiclyAccessibleDate":"7/5/2016"},"contributors":{"authors":[{"text":"Smith, Brian J. 0000-0002-0531-0492 bjsmith@usgs.gov","orcid":"https://orcid.org/0000-0002-0531-0492","contributorId":899,"corporation":false,"usgs":true,"family":"Smith","given":"Brian","email":"bjsmith@usgs.gov","middleInitial":"J.","affiliations":[{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"preferred":false,"id":642186,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cherkiss, Michael S. 0000-0002-7802-6791 mcherkiss@usgs.gov","orcid":"https://orcid.org/0000-0002-7802-6791","contributorId":4571,"corporation":false,"usgs":true,"family":"Cherkiss","given":"Michael","email":"mcherkiss@usgs.gov","middleInitial":"S.","affiliations":[{"id":566,"text":"Southeast Ecological Science Center","active":true,"usgs":true},{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"preferred":true,"id":642185,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hart, Kristen M. 0000-0002-5257-7974 kristen_hart@usgs.gov","orcid":"https://orcid.org/0000-0002-5257-7974","contributorId":1966,"corporation":false,"usgs":true,"family":"Hart","given":"Kristen","email":"kristen_hart@usgs.gov","middleInitial":"M.","affiliations":[{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"preferred":true,"id":642187,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Rochford, Michael R.","contributorId":6574,"corporation":false,"usgs":true,"family":"Rochford","given":"Michael R.","affiliations":[],"preferred":false,"id":642188,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Selby, Thomas H. 0000-0003-2116-0807 tselby@usgs.gov","orcid":"https://orcid.org/0000-0003-2116-0807","contributorId":5685,"corporation":false,"usgs":true,"family":"Selby","given":"Thomas","email":"tselby@usgs.gov","middleInitial":"H.","affiliations":[],"preferred":true,"id":642189,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Snow, Ray W","contributorId":121376,"corporation":false,"usgs":true,"family":"Snow","given":"Ray W","affiliations":[],"preferred":false,"id":642190,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Mazzotti, Frank J.","contributorId":12358,"corporation":false,"usgs":false,"family":"Mazzotti","given":"Frank J.","affiliations":[{"id":12604,"text":"Department of Wildlife Ecology and Conservation, Fort Lauderdale Research and Education Center, 3205 College Avenue, University of Florida, Davie, FL 33314, USA","active":true,"usgs":false}],"preferred":false,"id":642191,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}} ]}