{"pageNumber":"1362","pageRowStart":"34025","pageSize":"25","recordCount":165415,"records":[{"id":70107378,"text":"70107378 - 2014 - Distribution of soil organic carbon in the conterminous United States","interactions":[],"lastModifiedDate":"2014-07-02T10:34:40","indexId":"70107378","displayToPublicDate":"2014-01-01T10:30:03","publicationYear":"2014","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Distribution of soil organic carbon in the conterminous United States","docAbstract":"<p>The U.S. Soil Survey Geographic (SSURGO) database provides detailed soil mapping for most of the conterminous United States (CONUS). These data have been used to formulate estimates of soil carbon stocks, and have been useful for environmental models, including plant productivity models, hydrologic models, and ecological models for studies of greenhouse gas exchange. The data were compiled by the U.S. Department of Agriculture Natural Resources Conservation Service (NRCS) from 1:24,000-scale or 1:12,000-scale maps. It was found that the total soil organic carbon stock in CONUS to 1 m depth is 57 Pg C and for the total profile is 73 Pg C, as estimated from SSURGO with data gaps filled from the 1:250,000-scale Digital General Soil Map. We explore the non-linear distribution of soil carbon on the landscape and with depth in the soil, and the implications for sampling strategies that result from the observed soil carbon variability.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Soil Carbon","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","publisher":"Springer International Publishing","publisherLocation":"New York, NY","doi":"10.1007/978-3-319-04084-4_9","isbn":"978-3-319-04083-7","usgsCitation":"Bliss, N.B., Waltman, S., West, L.T., Neale, A., and Mehaffey, M., 2014, Distribution of soil organic carbon in the conterminous United States, chap. <i>of</i> Soil Carbon, p. 85-93, https://doi.org/10.1007/978-3-319-04084-4_9.","productDescription":"p. 85-93","numberOfPages":"9","ipdsId":"IP-054429","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":289366,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":287316,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/978-3-319-04084-4_9"}],"noUsgsAuthors":false,"publicationDate":"2014-03-03","publicationStatus":"PW","scienceBaseUri":"53b7b101e4b0388651d916cb","contributors":{"editors":[{"text":"Hartemink, Alfred E.","contributorId":111952,"corporation":false,"usgs":true,"family":"Hartemink","given":"Alfred","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":509850,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"McSweeney, Kevin M.","contributorId":113219,"corporation":false,"usgs":true,"family":"McSweeney","given":"Kevin","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":509851,"contributorType":{"id":2,"text":"Editors"},"rank":2}],"authors":[{"text":"Bliss, Norman B. 0000-0003-2409-5211 bliss@usgs.gov","orcid":"https://orcid.org/0000-0003-2409-5211","contributorId":1921,"corporation":false,"usgs":true,"family":"Bliss","given":"Norman","email":"bliss@usgs.gov","middleInitial":"B.","affiliations":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true},{"id":223,"text":"Earth Resources Observation and Science (EROS) Center (Geography)","active":false,"usgs":true}],"preferred":true,"id":493903,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Waltman, Sharon","contributorId":96596,"corporation":false,"usgs":true,"family":"Waltman","given":"Sharon","affiliations":[],"preferred":false,"id":493907,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"West, Larry T.","contributorId":18681,"corporation":false,"usgs":true,"family":"West","given":"Larry","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":493904,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Neale, Anne","contributorId":43275,"corporation":false,"usgs":true,"family":"Neale","given":"Anne","email":"","affiliations":[],"preferred":false,"id":493905,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Mehaffey, Megan","contributorId":58568,"corporation":false,"usgs":true,"family":"Mehaffey","given":"Megan","affiliations":[],"preferred":false,"id":493906,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70148075,"text":"70148075 - 2014 - Temperature sensitivity of organic-matter decay in tidal marshes","interactions":[],"lastModifiedDate":"2015-05-19T09:19:29","indexId":"70148075","displayToPublicDate":"2014-01-01T10:30:00","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1011,"text":"Biogeosciences","active":true,"publicationSubtype":{"id":10}},"title":"Temperature sensitivity of organic-matter decay in tidal marshes","docAbstract":"<p>Approximately half of marine carbon sequestration takes place in coastal wetlands, including tidal marshes, where organic matter contributes to soil elevation and ecosystem persistence in the face of sea-level rise. The long-term viability of marshes and their carbon pools depends, in part, on how the balance between productivity and decay responds to climate change. Here, we report the sensitivity of labile soil organic-matter decay in tidal marshes to seasonal and latitudinal variations in temperature measured over a 3-year period. We find a moderate increase in decay rate at warmer temperatures (3-6% per &deg;C, Q<sub>10</sub> = 1.3-1.5). Despite the profound differences between microbial metabolism in wetlands and uplands, our results indicate a strong conservation of temperature sensitivity. Moreover, simple comparisons with organic-matter production suggest that elevated atmospheric CO<sub>2</sub> and warmer temperatures will accelerate carbon accumulation in marsh soils, and potentially enhance their ability to survive sea-level rise.</p>","language":"English","publisher":"European Geosciences Union","publisherLocation":"Katlenberg-Lindau, Germany","doi":"10.5194/bg-11-4801-2014","usgsCitation":"Kirwan, M., Guntenspergen, G.R., and Langley, J., 2014, Temperature sensitivity of organic-matter decay in tidal marshes: Biogeosciences, v. 11, p. 4801-4808, https://doi.org/10.5194/bg-11-4801-2014.","productDescription":"8 p.","startPage":"4801","endPage":"4808","numberOfPages":"8","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-058767","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":473262,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.5194/bg-11-4801-2014","text":"Publisher Index Page"},{"id":300531,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"11","publishingServiceCenter":{"id":10,"text":"Baltimore PSC"},"noUsgsAuthors":false,"publicationDate":"2014-09-11","publicationStatus":"PW","scienceBaseUri":"555c5ebae4b0a92fa7eacc11","contributors":{"authors":[{"text":"Kirwan, Matthew L. 0000-0002-0658-3038","orcid":"https://orcid.org/0000-0002-0658-3038","contributorId":84060,"corporation":false,"usgs":true,"family":"Kirwan","given":"Matthew L.","affiliations":[],"preferred":false,"id":547210,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Guntenspergen, Glenn R. 0000-0002-8593-0244 glenn_guntenspergen@usgs.gov","orcid":"https://orcid.org/0000-0002-8593-0244","contributorId":2885,"corporation":false,"usgs":true,"family":"Guntenspergen","given":"Glenn","email":"glenn_guntenspergen@usgs.gov","middleInitial":"R.","affiliations":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"preferred":true,"id":547173,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Langley, J.A.","contributorId":89246,"corporation":false,"usgs":true,"family":"Langley","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":547211,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70145466,"text":"70145466 - 2014 - A simple headspace equilibration method for measuring dissolved methane","interactions":[],"lastModifiedDate":"2015-04-07T09:28:34","indexId":"70145466","displayToPublicDate":"2014-01-01T10:30:00","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2622,"text":"Limnology and Oceanography: Methods","active":true,"publicationSubtype":{"id":10}},"title":"A simple headspace equilibration method for measuring dissolved methane","docAbstract":"<p>Dissolved methane concentrations in the ocean are close to equilibrium with the atmosphere. Because methane is only sparingly soluble in seawater, measuring it without contamination is challenging for samples collected and processed in the presence of air. Several methods for analyzing dissolved methane are described in the literature, yet none has conducted a thorough assessment of the method yield, contamination issues during collection, transport and storage, and the effect of temperature changes and preservative. Previous extraction methods transfer methane from water to gas by either a \"sparge and trap\" or a \"headspace equilibration\" technique. The gas is then analyzed for methane by gas chromatography. Here, we revisit the headspace equilibration technique and describe a simple, inexpensive, and reliable method to measure methane in fresh and seawater, regardless of concentration. Within the range of concentrations typically found in surface seawaters (2-1000 nmol L<sup>-1</sup>), the yield of the method nears 100% of what is expected from solubility calculation following the addition of known amount of methane. In addition to being sensitive (detection limit of 0.1 ppmv, or 0.74 nmol L<sup>-1</sup>), this method requires less than 10 min per sample, and does not use highly toxic chemicals. It can be conducted with minimum materials and does not require the use of a gas chromatograph at the collection site. It can therefore be used in various remote working environments and conditions.</p>","language":"English","publisher":"American Society of Limnology and Oceanography","publisherLocation":"Waco, TX","doi":"10.4319/lom.2014.12.637","usgsCitation":"Magen, C., Lapham, L.L., Pohlman, J.W., Marshall, K.N., Bosman, S., Casso, M., and Chanton, J., 2014, A simple headspace equilibration method for measuring dissolved methane: Limnology and Oceanography: Methods, v. 12, p. 637-650, https://doi.org/10.4319/lom.2014.12.637.","productDescription":"14 p.","startPage":"637","endPage":"650","numberOfPages":"14","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-059425","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":473263,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.4319/lom.2014.12.637","text":"Publisher Index Page"},{"id":299436,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"12","publishingServiceCenter":{"id":11,"text":"Pembroke PSC"},"noUsgsAuthors":false,"publicationDate":"2014-09-08","publicationStatus":"PW","scienceBaseUri":"5524ffa9e4b027f0aee3d46d","contributors":{"authors":[{"text":"Magen, C","contributorId":140084,"corporation":false,"usgs":false,"family":"Magen","given":"C","affiliations":[{"id":13382,"text":"Earth, Ocean and Atmospheric Science, Florida State University, Tallahassee, Florida 32306","active":true,"usgs":false}],"preferred":false,"id":544191,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lapham, L. L.","contributorId":140085,"corporation":false,"usgs":false,"family":"Lapham","given":"L.","email":"","middleInitial":"L.","affiliations":[{"id":13383,"text":"University of Maryland Center for Environmental Science, Chesapeake Biological Laboratory, 6 Solomons, Maryland 20688","active":true,"usgs":false}],"preferred":false,"id":544192,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Pohlman, John W. jpohlman@usgs.gov","contributorId":139874,"corporation":false,"usgs":true,"family":"Pohlman","given":"John","email":"jpohlman@usgs.gov","middleInitial":"W.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":544190,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Marshall, Kristin N.","contributorId":27178,"corporation":false,"usgs":true,"family":"Marshall","given":"Kristin","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":544193,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Bosman, S.","contributorId":140086,"corporation":false,"usgs":false,"family":"Bosman","given":"S.","email":"","affiliations":[{"id":13382,"text":"Earth, Ocean and Atmospheric Science, Florida State University, Tallahassee, Florida 32306","active":true,"usgs":false}],"preferred":false,"id":544194,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Casso, Michael 0000-0002-6990-9090 mcasso@usgs.gov","orcid":"https://orcid.org/0000-0002-6990-9090","contributorId":2904,"corporation":false,"usgs":true,"family":"Casso","given":"Michael","email":"mcasso@usgs.gov","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":544195,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Chanton, J. P.","contributorId":7429,"corporation":false,"usgs":false,"family":"Chanton","given":"J. P.","affiliations":[],"preferred":false,"id":544196,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70141773,"text":"70141773 - 2014 - The role of defensible space for residential structure protection during wildfires","interactions":[],"lastModifiedDate":"2015-02-23T09:16:33","indexId":"70141773","displayToPublicDate":"2014-01-01T10:30:00","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2083,"text":"International Journal of Wildland Fire","active":true,"publicationSubtype":{"id":10}},"title":"The role of defensible space for residential structure protection during wildfires","docAbstract":"<p>With the potential for worsening fire conditions, discussion is escalating over how to best reduce effects on urban communities. A widely supported strategy is the creation of defensible space immediately surrounding homes and other structures. Although state and local governments publish specific guidelines and requirements, there is little empirical evidence to suggest how much vegetation modification is needed to provide significant benefits. We analysed the role of defensible space by mapping and measuring a suite of variables on modern pre-fire aerial photography for 1000 destroyed and 1000 surviving structures for all fires where homes burned from 2001 to 2010 in San Diego County, CA, USA. Structures were more likely to survive a fire with defensible space immediately adjacent to them. The most effective treatment distance varied between 5 and 20 m (16&ndash;58 ft) from the structure, but distances larger than 30 m (100 ft) did not provide additional protection, even for structures located on steep slopes. The most effective actions were reducing woody cover up to 40% immediately adjacent to structures and ensuring that vegetation does not overhang or touch the structure. Multiple-regression models showed landscape-scale factors, including low housing density and distances to major roads, were more important in explaining structure destruction. The best long-term solution will involve a suite of prevention measures that include defensible space as well as building design approach, community education and proactive land use planning that limits exposure to fire.</p>","language":"English","publisher":"Fire Research Institute","publisherLocation":"Rosyn, WA","doi":"10.1071/WF13158","usgsCitation":"Syphard, A.D., Brennan, T.J., and Keeley, J.E., 2014, The role of defensible space for residential structure protection during wildfires: International Journal of Wildland Fire, v. 23, p. 1165-1175, https://doi.org/10.1071/WF13158.","productDescription":"11 p.","startPage":"1165","endPage":"1175","numberOfPages":"11","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-051439","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":298093,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"23","publishingServiceCenter":{"id":1,"text":"Sacramento PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"54ec5d48e4b02d776a67dab5","contributors":{"authors":[{"text":"Syphard, Alexandra D.","contributorId":8977,"corporation":false,"usgs":false,"family":"Syphard","given":"Alexandra","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":541063,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brennan, Teresa J. 0000-0002-0646-3298 tjbrennan@usgs.gov","orcid":"https://orcid.org/0000-0002-0646-3298","contributorId":4323,"corporation":false,"usgs":true,"family":"Brennan","given":"Teresa","email":"tjbrennan@usgs.gov","middleInitial":"J.","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":true,"id":541064,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Keeley, Jon E. 0000-0002-4564-6521 jon_keeley@usgs.gov","orcid":"https://orcid.org/0000-0002-4564-6521","contributorId":1268,"corporation":false,"usgs":true,"family":"Keeley","given":"Jon","email":"jon_keeley@usgs.gov","middleInitial":"E.","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":true,"id":541062,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70146040,"text":"70146040 - 2014 - Habitat and food preferences of the endangered Palila (Loxioides bailleui) on Mauna Kea, Hawai'i","interactions":[],"lastModifiedDate":"2018-01-04T12:51:11","indexId":"70146040","displayToPublicDate":"2014-01-01T10:30:00","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3784,"text":"Wilson Journal of Ornithology","active":true,"publicationSubtype":{"id":10}},"title":"Habitat and food preferences of the endangered Palila (Loxioides bailleui) on Mauna Kea, Hawai'i","docAbstract":"<p>Seeds and flowers of the leguminous māmane (<i>Sophora chrysophylla</i>) tree are the primary food resource of the federally endangered Palila (<i>Loxioides bailleui</i>; Fringillidae: Drepanidinae), which is now restricted to dry subalpine woodland on Mauna Kea Volcano on the island of Hawai'i because of centuries of habitat degradation by non-native ungulates. Palila are morphologically and behaviorally adapted to consume m&Auml;mane seeds by grasping seed pods with their feet and opening pods with stout bills and demonstrate limited ability to exploit alternative food resources. This degree of single species dependency is rare among birds and illustrates unique adaptations that also occurred in other Hawaiian species that are now extinct. In mixed-woodland with co-dominant naio (<i>Myoporum sandwicense</i>), Palila spent 1.7-3.9 times longer in māmane than in naio during foraging observations where naio was 1.3-4.6 times as dense as māmane. Naio fruit was readily available, but it comprised proportionally &lt;11% of food items taken by Palila. Although māmane flowers were more abundant than māmane pods throughout this study except at one lower-elevation mixed-woodland site, Palila spent more time foraging on pods than flowers in both māmane woodland and mixed-woodland, but consumed more flowers than pods in mixed-woodland. Insects, which have been reported as an important component of the diet of Palila, were apparently taken rarely in this study. Protecting and restoring māmane in woodlands adjacent to the current range of Palila will benefit their recovery, allowing them to exploit increased food availability in areas of their former range.</p>","language":"English","publisher":"Wilson Ornithological Society","publisherLocation":"Lawrence, KS","doi":"10.1676/13-220.1","usgsCitation":"Hess, S.C., Banko, P.C., Miller, L.J., and Laniawe, L.P., 2014, Habitat and food preferences of the endangered Palila (Loxioides bailleui) on Mauna Kea, Hawai'i: Wilson Journal of Ornithology, v. 126, no. 4, p. 728-738, https://doi.org/10.1676/13-220.1.","productDescription":"11 p.","startPage":"728","endPage":"738","numberOfPages":"11","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-056581","costCenters":[{"id":521,"text":"Pacific Island Ecosystems Research Center","active":false,"usgs":true}],"links":[{"id":299597,"type":{"id":15,"text":"Index Page"},"url":"https://www.bioone.org/doi/abs/10.1676/13-220.1"},{"id":299600,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Hawai'i","otherGeospatial":"Mauna Kea","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -155.55679321289062,\n              19.75701045794938\n            ],\n            [\n              -155.55679321289062,\n              19.91332029680867\n            ],\n            [\n              -155.37620544433594,\n              19.91332029680867\n            ],\n            [\n              -155.37620544433594,\n              19.75701045794938\n            ],\n            [\n              -155.55679321289062,\n              19.75701045794938\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"126","issue":"4","publishingServiceCenter":{"id":14,"text":"Menlo Park PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"552ce8b7e4b0b22a157f50b1","contributors":{"authors":[{"text":"Hess, Steven C. 0000-0001-6403-9922 shess@usgs.gov","orcid":"https://orcid.org/0000-0001-6403-9922","contributorId":3156,"corporation":false,"usgs":true,"family":"Hess","given":"Steven","email":"shess@usgs.gov","middleInitial":"C.","affiliations":[{"id":5049,"text":"Pacific Islands Ecosys Research Center","active":true,"usgs":true}],"preferred":false,"id":544639,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Banko, Paul C. 0000-0002-6035-9803 pbanko@usgs.gov","orcid":"https://orcid.org/0000-0002-6035-9803","contributorId":3179,"corporation":false,"usgs":true,"family":"Banko","given":"Paul","email":"pbanko@usgs.gov","middleInitial":"C.","affiliations":[{"id":5049,"text":"Pacific Islands Ecosys Research Center","active":true,"usgs":true},{"id":521,"text":"Pacific Island Ecosystems Research Center","active":false,"usgs":true}],"preferred":true,"id":544640,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Miller, Linda J.","contributorId":140189,"corporation":false,"usgs":false,"family":"Miller","given":"Linda","email":"","middleInitial":"J.","affiliations":[{"id":13405,"text":"Department of Zoology, University of Maryland, College Park, MD","active":true,"usgs":false}],"preferred":false,"id":544641,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Laniawe, Leona P.","contributorId":140190,"corporation":false,"usgs":false,"family":"Laniawe","given":"Leona","email":"","middleInitial":"P.","affiliations":[{"id":13406,"text":"U.S. Fish and Wildlife Service, 300 Ala Moana Blvd., P. O. Box 50617,          Honolulu,","active":true,"usgs":false}],"preferred":false,"id":544642,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70056519,"text":"70056519 - 2014 - Holocene and latest Pleistocene paleoseismology of the Salt Lake City segment of the Wasatch Fault Zone, Utah, at the Penrose Drive Trench Site","interactions":[],"lastModifiedDate":"2014-10-02T15:51:23","indexId":"70056519","displayToPublicDate":"2014-01-01T10:25:00","publicationYear":"2014","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesNumber":"149","title":"Holocene and latest Pleistocene paleoseismology of the Salt Lake City segment of the Wasatch Fault Zone, Utah, at the Penrose Drive Trench Site","docAbstract":"<p>The Salt Lake City segment (SLCS) of the Wasatch fault zone (WFZ) and the West Valley fault zone (WVFZ) compromise Holocene-active normal faults that bound a large intrabasin graben in northern Salt Lake Valley and have evidence of recurrent, large-magnitude (M ~6-7) surface-faulting earthquakes. However, at the time of this investigation, questions remained regarding the timing, displacement, and recurrence of latest Pleistocene and Holocene earthquakes on the northern SLCS and WVFZ , and whether the WVFZ is seismically independent of, or moves coseismically with, the SLCS.</p>\n<br>\n<p>To improve paleoseismic data for the SLCS, we conducted a fault-trench investigation at the Penrose Drive site on the northern SLCS. Two trenches, excavated across an 11-m-high scarp near the northern end of the East Bench fault, exposed colluvial-wedge evidence for fize of six (preferred) surface-faulting earthquakes postdating to Provo-phase shoreline of Lake Bonneville (~14-18 ka). Radiocarbon and luminescence ages support earthquake times at 4.0 ± 0.5 ka (2σ) (PD1), 5.9 ± 0.7 ka (PD2), 7.5 ± 0.8 ka (PD3a), 9.7 ± 1.1 ka (PD3b), 10.9 ± 0.2 ka (PD4), and 12.1 ± 1.6 ka (PD5). At least one additional earthquake occurred at 16.5 ± 1.9 ka (PD6) based on an erosional unconformity that separates deformed Lake Bonneville sily and flat-lying Provo-phase shoreline gravel. Earthquakes PD5-PD1 yield latest Pleistocene (post-Provo) and Holocene mean recurrence intervals of ~1.6 kyr and ~1.7-1.9 kyr, respectively. Using 1.0-1.4 m of per-event vertical displacement for PD5-PD3b corroborate previously identified SLCS earthquakes at 4-10 ka. PD4 and PD5 occurred within an ~8-kyr *17-9 ka) time interval on the SLCS previously interpreted as a period of seismic quiescence, and PD6 possibly corresponds with a previously identified earthquake at ~17 ka (although both events have large timing uncertainties).</p>\n<br>\n<p>The Penrose data, when combined with previous paleoseismic results, improve the latest Pleistocene-Holocene earthquake chronology of the SLCS, and demonstrate that the SLCS has been a consistently active source of large-magnitude earthquakes since the latest Pleistocene. At least nine surface-faulting earthquakes (S1-S9) have occurred since the highstand of Lake Bonneville (~18 ka). Where the SLCS earthquake record is most complete (since ~14 ka), per-site estimates of mean recurrence are similar for the latest Pleistocene (post-Provo) (~1.6 kyr), Holocene (~1.6-1.9 kyr), and late Holocene (~1.2-1.4 kyr). These SLCS paleoearthquake data indicate an essentially stable rate of earthquake recurrence since the latest Pleistocene and are important for understanding the earthquake potential of the SLCS, clarifying the seismogenic relation between the SLCS and WVFZ, and forecasting the probabilities of future large-magnitude earthquake in the Wasatch Front region.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Evaluating surface faulting chronologies of Graben-Bounding Faults in Salt Lake Valley, Utah: new paleoseismic data from the Salt Lake City segment of the Wasatch Fault Zone and the West Valley Fault Zone","largerWorkSubtype":{"id":2,"text":"State or Local Government Series"},"language":"English","publisher":"Utah Geological Survey","publisherLocation":"Salt Lake City, UT","usgsCitation":"DuRoss, C., Hylland, M., McDonald, G., Crone, A.J., Personius, S.F., Gold, R.D., and Mahan, S., 2014, Holocene and latest Pleistocene paleoseismology of the Salt Lake City segment of the Wasatch Fault Zone, Utah, at the Penrose Drive Trench Site, v. 24, 39 p.","productDescription":"39 p.","numberOfPages":"39","ipdsId":"IP-051371","costCenters":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"links":[{"id":294884,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":294883,"type":{"id":11,"text":"Document"},"url":"https://geology.utah.gov/online/ss/ss-149/SS-149_PenroseDrive_report.pdf"}],"country":"United States","state":"Utah","otherGeospatial":"Wasatch Fault Zone","volume":"24","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"542e6963e4b092f17df5a8a2","contributors":{"authors":[{"text":"DuRoss, Christopher B.","contributorId":100764,"corporation":false,"usgs":true,"family":"DuRoss","given":"Christopher B.","affiliations":[],"preferred":false,"id":486582,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hylland, Michael D.","contributorId":106031,"corporation":false,"usgs":true,"family":"Hylland","given":"Michael D.","affiliations":[],"preferred":false,"id":486583,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McDonald, Greg N.","contributorId":55362,"corporation":false,"usgs":true,"family":"McDonald","given":"Greg N.","affiliations":[],"preferred":false,"id":486581,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Crone, Anthony J. 0000-0002-3006-406X crone@usgs.gov","orcid":"https://orcid.org/0000-0002-3006-406X","contributorId":790,"corporation":false,"usgs":true,"family":"Crone","given":"Anthony","email":"crone@usgs.gov","middleInitial":"J.","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":true,"id":486577,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Personius, Stephen F. personius@usgs.gov","contributorId":1214,"corporation":false,"usgs":true,"family":"Personius","given":"Stephen","email":"personius@usgs.gov","middleInitial":"F.","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":false,"id":486578,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Gold, Ryan D. 0000-0002-4464-6394 rgold@usgs.gov","orcid":"https://orcid.org/0000-0002-4464-6394","contributorId":3883,"corporation":false,"usgs":true,"family":"Gold","given":"Ryan","email":"rgold@usgs.gov","middleInitial":"D.","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":true,"id":486580,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Mahan, Shannon 0000-0001-5214-7774 smahan@usgs.gov","orcid":"https://orcid.org/0000-0001-5214-7774","contributorId":1215,"corporation":false,"usgs":true,"family":"Mahan","given":"Shannon","email":"smahan@usgs.gov","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":false,"id":486579,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70101407,"text":"70101407 - 2014 - Southern San Andreas Fault evaluation field activity: approaches to measuring small geomorphic offsets--challenges and recommendations for active fault studies","interactions":[],"lastModifiedDate":"2014-04-11T10:27:41","indexId":"70101407","displayToPublicDate":"2014-01-01T10:21:00","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3372,"text":"Seismological Research Letters","onlineIssn":"1938-2057","printIssn":"0895-0695","active":true,"publicationSubtype":{"id":10}},"title":"Southern San Andreas Fault evaluation field activity: approaches to measuring small geomorphic offsets--challenges and recommendations for active fault studies","docAbstract":"In southern California, where fast slip rates and sparse vegetation contribute to crisp expression of faults and microtopography, field and high‐resolution topographic data (<1  m/pixel) increasingly are used to investigate the mark left by large earthquakes on the landscape (e.g., Zielke et al., 2010; Zielke et al., 2012; Salisbury, Rockwell, et al., 2012, Madden et al., 2013). These studies measure offset streams or other geomorphic features along a stretch of a fault, analyze the offset values for concentrations or trends along strike, and infer that the common magnitudes reflect successive surface‐rupturing earthquakes along that fault section. Wallace (1968) introduced the use of such offsets, and the challenges in interpreting their “unique complex history” with offsets on the Carrizo section of the San Andreas fault; these were more fully mapped by Sieh (1978) and followed by similar field studies along other faults (e.g., Lindvall et al., 1989; McGill and Sieh, 1991). Results from such compilations spurred the development of classic fault behavior models, notably the characteristic earthquake and slip‐patch models, and thus constitute an important component of the long‐standing contrast between magnitude–frequency models (Schwartz and Coppersmith, 1984; Sieh, 1996; Hecker et al., 2013). The proliferation of offset datasets has led earthquake geologists to examine the methods and approaches for measuring these offsets, uncertainties associated with measurement of such features, and quality ranking schemes (Arrowsmith and Rockwell, 2012; Salisbury, Arrowsmith, et al., 2012; Gold et al., 2013; Madden et al., 2013). In light of this, the Southern San Andreas Fault Evaluation (SoSAFE) project at the Southern California Earthquake Center (SCEC) organized a combined field activity and workshop (the “Fieldshop”) to measure offsets, compare techniques, and explore differences in interpretation. A thorough analysis of the measurements from the field activity will be provided separately; this paper discusses the complications presented by such offset measurements using two channels from the San Andreas fault as illustrative cases. We conclude with best approaches for future data collection efforts based on input from the Fieldshop.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Seismological Research Letters","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Seismological Society of America","doi":"10.1785/0220130108","usgsCitation":"Scharer, K.M., Salisbury, J.B., Arrowsmith, J.R., and Rockwell, T.K., 2014, Southern San Andreas Fault evaluation field activity: approaches to measuring small geomorphic offsets--challenges and recommendations for active fault studies: Seismological Research Letters, v. 85, no. 1, p. 68-76, https://doi.org/10.1785/0220130108.","productDescription":"9 p.","startPage":"68","endPage":"76","numberOfPages":"9","ipdsId":"IP-049065","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"links":[{"id":286259,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":286258,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1785/0220130108"}],"country":"United States","state":"California","otherGeospatial":"San Andreas Fault","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -120.76,32.53 ], [ -120.76,35.77 ], [ -115.21,35.77 ], [ -115.21,32.53 ], [ -120.76,32.53 ] ] ] } } ] }","volume":"85","issue":"1","noUsgsAuthors":false,"publicationDate":"2014-01-02","publicationStatus":"PW","scienceBaseUri":"53559565e4b0120853e8c1fa","contributors":{"authors":[{"text":"Scharer, Katherine M. 0000-0003-2811-2496 kscharer@usgs.gov","orcid":"https://orcid.org/0000-0003-2811-2496","contributorId":3385,"corporation":false,"usgs":true,"family":"Scharer","given":"Katherine","email":"kscharer@usgs.gov","middleInitial":"M.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":492682,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Salisbury, J. Barrett","contributorId":36852,"corporation":false,"usgs":true,"family":"Salisbury","given":"J.","email":"","middleInitial":"Barrett","affiliations":[],"preferred":false,"id":492683,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Arrowsmith, J. Ramon","contributorId":101185,"corporation":false,"usgs":true,"family":"Arrowsmith","given":"J.","email":"","middleInitial":"Ramon","affiliations":[],"preferred":false,"id":492685,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Rockwell, Thomas K.","contributorId":53290,"corporation":false,"usgs":true,"family":"Rockwell","given":"Thomas","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":492684,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70129146,"text":"70129146 - 2014 - Transcriptome resources for the frogs <i>Lithobates clamitans</i> and <i>Pseudacris regilla</i>, emphasizing antimicrobial peptides and conserved loci for phylogenetics","interactions":[],"lastModifiedDate":"2014-10-17T10:21:19","indexId":"70129146","displayToPublicDate":"2014-01-01T10:16:48","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2776,"text":"Molecular Ecology Resources","active":true,"publicationSubtype":{"id":10}},"title":"Transcriptome resources for the frogs <i>Lithobates clamitans</i> and <i>Pseudacris regilla</i>, emphasizing antimicrobial peptides and conserved loci for phylogenetics","docAbstract":"We developed genetic resources for two North American frogs, <i>Lithobates clamitans</i> and <i>Pseudacris regilla</i>, widespread native amphibians that are potential indicator species of environmental health. For both species, mRNA from multiple tissues was sequenced using 454 technology. <i>De novo</i> assemblies with Mira3 resulted in 50 238 contigs (N50 = 687 bp) and 48 213 contigs (N50 = 686 bp) for <i>L. clamitans</i> and <i>P. regilla</i>, respectively, after clustering with CD-Hit-EST and purging contigs below 200 bp. We performed BLASTX similarity searches against the <i>Xenopus tropicalis</i> proteome and, for predicted ORFs, HMMER similarity searches against the Pfam-A database. Because there is broad interest in amphibian immune factors, we manually annotated putative antimicrobial peptides. To identify conserved regions suitable for amplicon resequencing across a broad taxonomic range, we performed an additional assembly of public short-read transcriptome data derived from two species of the genus <i>Rana</i> and identified reciprocal best TBLASTX matches among all assemblies. Although <i>P. regilla</i>, a hylid frog, is substantially more diverged from the ranid species, we identified 56 genes that were sufficiently conserved to allow nondegenerate primer design with Primer3. In addition to providing a foundation for comparative genomics and quantitative gene expression analysis, our results enable quick development of nuclear sequence-based markers for phylogenetics or population genetics.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Molecular Ecology Resources","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Wiley","doi":"10.1111/1755-0998.12164","usgsCitation":"Robertson, L.S., and Cornman, R.S., 2014, Transcriptome resources for the frogs <i>Lithobates clamitans</i> and <i>Pseudacris regilla</i>, emphasizing antimicrobial peptides and conserved loci for phylogenetics: Molecular Ecology Resources, v. 14, no. 1, p. 178-183, https://doi.org/10.1111/1755-0998.12164.","productDescription":"6 p.","startPage":"178","endPage":"183","numberOfPages":"6","ipdsId":"IP-050619","costCenters":[{"id":506,"text":"Office of the AD Ecosystems","active":true,"usgs":true}],"links":[{"id":295444,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":295443,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1111/1755-0998.12164"}],"volume":"14","issue":"1","noUsgsAuthors":false,"publicationDate":"2013-09-13","publicationStatus":"PW","scienceBaseUri":"54422fa4e4b0192a5a42f3e2","contributors":{"authors":[{"text":"Robertson, Laura S. lrobertson@usgs.gov","contributorId":2288,"corporation":false,"usgs":true,"family":"Robertson","given":"Laura","email":"lrobertson@usgs.gov","middleInitial":"S.","affiliations":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"preferred":false,"id":503444,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cornman, Robert S. 0000-0001-9511-2192 rcornman@usgs.gov","orcid":"https://orcid.org/0000-0001-9511-2192","contributorId":5356,"corporation":false,"usgs":true,"family":"Cornman","given":"Robert","email":"rcornman@usgs.gov","middleInitial":"S.","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true},{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"preferred":true,"id":503445,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70228708,"text":"70228708 - 2014 - Yellowstone grizzly bear investigations—Annual report of the Interagency Grizzly Bear Study Team 2013","interactions":[],"lastModifiedDate":"2022-09-13T15:13:29.769041","indexId":"70228708","displayToPublicDate":"2014-01-01T10:04:23","publicationYear":"2014","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":3,"text":"Annual Report","active":false,"publicationSubtype":{"id":1}},"title":"Yellowstone grizzly bear investigations—Annual report of the Interagency Grizzly Bear Study Team 2013","docAbstract":"<p>This Annual Report summarizes results of grizzly bear (<i>Ursus arctos</i>) monitoring and research conducted in the Greater Yellowstone Ecosystem (GYE) by the Interagency Grizzly Bear Study Team (IGBST) during 2013. The report also contains a summary of nuisance grizzly bear management actions.&nbsp;</p>","language":"English","publisher":"Interagency Grizzly Bear Study Team","usgsCitation":"2014, Yellowstone grizzly bear investigations—Annual report of the Interagency Grizzly Bear Study Team 2013: Annual Report, 109 p.","productDescription":"109 p.","ipdsId":"IP-130250","costCenters":[{"id":481,"text":"Northern Rocky Mountain Science Center","active":true,"usgs":true}],"links":[{"id":406602,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":406601,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://www.sciencebase.gov/catalog/file/get/6266a697d34e76103cce5808?f=__disk__42%2Fb8%2F4f%2F42b84f8d187242f660a0c0b50b076d4f3fe866c0","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Idaho, Montana, Wyoming","otherGeospatial":"Greater Yellowstone Ecosystem","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -111.68701171875,\n              42.85985981506279\n            ],\n            [\n              -109.27001953125,\n              42.85985981506279\n            ],\n            [\n              -109.27001953125,\n              45.583289756006316\n            ],\n            [\n              -111.68701171875,\n              45.583289756006316\n            ],\n            [\n              -111.68701171875,\n              42.85985981506279\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"editors":[{"text":"van Manen, Frank T. 0000-0001-5340-8489 fvanmanen@usgs.gov","orcid":"https://orcid.org/0000-0001-5340-8489","contributorId":2267,"corporation":false,"usgs":true,"family":"van Manen","given":"Frank","email":"fvanmanen@usgs.gov","middleInitial":"T.","affiliations":[{"id":481,"text":"Northern Rocky Mountain Science Center","active":true,"usgs":true}],"preferred":true,"id":835173,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Haroldson, Mark A. 0000-0002-7457-7676 mharoldson@usgs.gov","orcid":"https://orcid.org/0000-0002-7457-7676","contributorId":1773,"corporation":false,"usgs":true,"family":"Haroldson","given":"Mark","email":"mharoldson@usgs.gov","middleInitial":"A.","affiliations":[{"id":481,"text":"Northern Rocky Mountain Science Center","active":true,"usgs":true}],"preferred":true,"id":835174,"contributorType":{"id":2,"text":"Editors"},"rank":2},{"text":"West, Karrie","contributorId":279597,"corporation":false,"usgs":false,"family":"West","given":"Karrie","affiliations":[{"id":57306,"text":"Northern Rocky Mountain Science Center","active":true,"usgs":false}],"preferred":false,"id":835175,"contributorType":{"id":2,"text":"Editors"},"rank":3},{"text":"Soileau, Suzanna C. 0000-0002-4331-0098","orcid":"https://orcid.org/0000-0002-4331-0098","contributorId":204690,"corporation":false,"usgs":true,"family":"Soileau","given":"Suzanna C.","affiliations":[{"id":506,"text":"Office of the AD Ecosystems","active":true,"usgs":true}],"preferred":true,"id":835176,"contributorType":{"id":2,"text":"Editors"},"rank":4}]}}
,{"id":70073974,"text":"70073974 - 2014 - Ancient aqueous environments at Endeavour crater, Mars","interactions":[],"lastModifiedDate":"2018-11-14T10:29:17","indexId":"70073974","displayToPublicDate":"2014-01-01T10:04:00","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Ancient aqueous environments at Endeavour crater, Mars","docAbstract":"Opportunity has investigated in detail rocks on the rim of the Noachian age Endeavour crater, where orbital spectral reflectance signatures indicate the presence of Fe<sup>+3</sup>-rich smectites. The signatures are associated with fine-grained, layered rocks containing spherules of diagenetic or impact origin. The layered rocks are overlain by breccias, and both units are cut by calcium sulfate veins precipitated from fluids that circulated after the Endeavour impact. Compositional data for fractures in the layered rocks suggest formation of Al-rich smectites by aqueous leaching. Evidence is thus preserved for water-rock interactions before and after the impact, with aqueous environments of slightly acidic to circum-neutral pH that would have been more favorable for prebiotic chemistry and microorganisms than those recorded by younger sulfate-rich rocks at Meridiani Planum.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Science","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.1248097","usgsCitation":"Arvidson, R., Squyres, S.W., Bell, J., Catalano, J., Clark, B.C., Crumpler, L., de Souza, P., Fairén, A., Farrand, W.H., Fox, V., Gellert, R., Ghosh, A., Golombeck, M., Grotzinger, J., Guinness, E., Herkenhoff, K.E., Jolliff, B., Knoll, A., Li, R., McLennan, S.M., Ming, D.W., Mittlefehldt, D.W., Moore, J.N., Morris, R., Murchie, S., Parker, T.J., Paulsen, G., Rice, J., Ruff, S.W., Smith, M.D., and Wolff, M., 2014, Ancient aqueous environments at Endeavour crater, Mars: Science, v. 343, no. 6169, 9 p., https://doi.org/10.1126/science.1248097.","productDescription":"9 p.","onlineOnly":"Y","ipdsId":"IP-050620","costCenters":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"links":[{"id":473264,"rank":0,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"http://nrs.harvard.edu/urn-3:HUL.InstRepos:12330889","text":"External Repository"},{"id":281552,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":281551,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1126/science.1248097"}],"otherGeospatial":"Mars;Endeavour Crater","volume":"343","issue":"6169","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd4d3be4b0b290850f169d","contributors":{"authors":[{"text":"Arvidson, R. E.","contributorId":46666,"corporation":false,"usgs":true,"family":"Arvidson","given":"R. E.","affiliations":[],"preferred":false,"id":489321,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Squyres, S. W.","contributorId":31836,"corporation":false,"usgs":true,"family":"Squyres","given":"S.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":489318,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bell, J.F. III","contributorId":97612,"corporation":false,"usgs":true,"family":"Bell","given":"J.F.","suffix":"III","email":"","affiliations":[],"preferred":false,"id":489337,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Catalano, J.G.","contributorId":51196,"corporation":false,"usgs":true,"family":"Catalano","given":"J.G.","email":"","affiliations":[],"preferred":false,"id":489322,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Clark, B. C.","contributorId":39918,"corporation":false,"usgs":true,"family":"Clark","given":"B.","middleInitial":"C.","affiliations":[],"preferred":false,"id":489320,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Crumpler, L.S.","contributorId":81575,"corporation":false,"usgs":true,"family":"Crumpler","given":"L.S.","email":"","affiliations":[],"preferred":false,"id":489331,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"de Souza, P.A. Jr.","contributorId":107606,"corporation":false,"usgs":true,"family":"de Souza","given":"P.A.","suffix":"Jr.","affiliations":[],"preferred":false,"id":489340,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Fairén, A.G.","contributorId":107186,"corporation":false,"usgs":true,"family":"Fairén","given":"A.G.","affiliations":[],"preferred":false,"id":489339,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Farrand, W. H.","contributorId":64372,"corporation":false,"usgs":true,"family":"Farrand","given":"W.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":489325,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Fox, V.K.","contributorId":69058,"corporation":false,"usgs":true,"family":"Fox","given":"V.K.","email":"","affiliations":[],"preferred":false,"id":489328,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Gellert, Ralf","contributorId":35049,"corporation":false,"usgs":false,"family":"Gellert","given":"Ralf","email":"","affiliations":[{"id":12660,"text":"University of Guelph","active":true,"usgs":false}],"preferred":false,"id":489319,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Ghosh, A.","contributorId":17407,"corporation":false,"usgs":true,"family":"Ghosh","given":"A.","email":"","affiliations":[],"preferred":false,"id":489314,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Golombeck, M.P.","contributorId":95793,"corporation":false,"usgs":true,"family":"Golombeck","given":"M.P.","email":"","affiliations":[],"preferred":false,"id":489334,"contributorType":{"id":1,"text":"Authors"},"rank":13},{"text":"Grotzinger, J.P.","contributorId":76053,"corporation":false,"usgs":true,"family":"Grotzinger","given":"J.P.","affiliations":[],"preferred":false,"id":489329,"contributorType":{"id":1,"text":"Authors"},"rank":14},{"text":"Guinness, E.A.","contributorId":78070,"corporation":false,"usgs":true,"family":"Guinness","given":"E.A.","email":"","affiliations":[],"preferred":false,"id":489330,"contributorType":{"id":1,"text":"Authors"},"rank":15},{"text":"Herkenhoff, Kenneth E. 0000-0002-3153-6663 kherkenhoff@usgs.gov","orcid":"https://orcid.org/0000-0002-3153-6663","contributorId":2275,"corporation":false,"usgs":true,"family":"Herkenhoff","given":"Kenneth","email":"kherkenhoff@usgs.gov","middleInitial":"E.","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":true,"id":489310,"contributorType":{"id":1,"text":"Authors"},"rank":16},{"text":"Jolliff, B.L.","contributorId":21268,"corporation":false,"usgs":true,"family":"Jolliff","given":"B.L.","email":"","affiliations":[],"preferred":false,"id":489315,"contributorType":{"id":1,"text":"Authors"},"rank":17},{"text":"Knoll, A.H.","contributorId":84885,"corporation":false,"usgs":true,"family":"Knoll","given":"A.H.","email":"","affiliations":[],"preferred":false,"id":489332,"contributorType":{"id":1,"text":"Authors"},"rank":18},{"text":"Li, R.","contributorId":68441,"corporation":false,"usgs":true,"family":"Li","given":"R.","affiliations":[],"preferred":false,"id":489327,"contributorType":{"id":1,"text":"Authors"},"rank":19},{"text":"McLennan, S. 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W.","contributorId":54711,"corporation":false,"usgs":true,"family":"Mittlefehldt","given":"D.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":489323,"contributorType":{"id":1,"text":"Authors"},"rank":22},{"text":"Moore, Johnnie N.","contributorId":13668,"corporation":false,"usgs":true,"family":"Moore","given":"Johnnie","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":489313,"contributorType":{"id":1,"text":"Authors"},"rank":23},{"text":"Morris, R.V.","contributorId":6978,"corporation":false,"usgs":true,"family":"Morris","given":"R.V.","affiliations":[],"preferred":false,"id":489311,"contributorType":{"id":1,"text":"Authors"},"rank":24},{"text":"Murchie, S.L.","contributorId":7369,"corporation":false,"usgs":true,"family":"Murchie","given":"S.L.","email":"","affiliations":[],"preferred":false,"id":489312,"contributorType":{"id":1,"text":"Authors"},"rank":25},{"text":"Parker, T. J.","contributorId":30776,"corporation":false,"usgs":false,"family":"Parker","given":"T.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":489317,"contributorType":{"id":1,"text":"Authors"},"rank":26},{"text":"Paulsen, G.","contributorId":94192,"corporation":false,"usgs":true,"family":"Paulsen","given":"G.","email":"","affiliations":[],"preferred":false,"id":489333,"contributorType":{"id":1,"text":"Authors"},"rank":27},{"text":"Rice, J.W.","contributorId":103046,"corporation":false,"usgs":true,"family":"Rice","given":"J.W.","email":"","affiliations":[],"preferred":false,"id":489338,"contributorType":{"id":1,"text":"Authors"},"rank":28},{"text":"Ruff, S. W.","contributorId":63136,"corporation":false,"usgs":false,"family":"Ruff","given":"S.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":489324,"contributorType":{"id":1,"text":"Authors"},"rank":29},{"text":"Smith, M. D.","contributorId":25724,"corporation":false,"usgs":false,"family":"Smith","given":"M.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":489316,"contributorType":{"id":1,"text":"Authors"},"rank":30},{"text":"Wolff, M.J.","contributorId":64374,"corporation":false,"usgs":true,"family":"Wolff","given":"M.J.","email":"","affiliations":[],"preferred":false,"id":489326,"contributorType":{"id":1,"text":"Authors"},"rank":31}]}}
,{"id":70118038,"text":"70118038 - 2014 - Vegetation classification and mapping Vicksburg National Military Park, Mississippi","interactions":[],"lastModifiedDate":"2014-07-25T10:02:46","indexId":"70118038","displayToPublicDate":"2014-01-01T10:00:14","publicationYear":"2014","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":9,"text":"Other Report"},"seriesNumber":"2013-710","title":"Vegetation classification and mapping Vicksburg National Military Park, Mississippi","docAbstract":"No abstract available.","language":"English","publisher":"National Park Service","publisherLocation":"Washington, D.C.","usgsCitation":"Lea, C., Waltermire, B., and Nordman, C., 2014, Vegetation classification and mapping Vicksburg National Military Park, Mississippi, 128 p.","productDescription":"128 p.","numberOfPages":"128","costCenters":[],"links":[{"id":290980,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Mississippi","city":"Vicksburg","otherGeospatial":"Vicksburg National Military Park","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -90.899451,32.309758 ], [ -90.899451,32.381171 ], [ -90.831631,32.381171 ], [ -90.831631,32.309758 ], [ -90.899451,32.309758 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57f7f184e4b0bc0bec09fe24","contributors":{"authors":[{"text":"Lea, C.","contributorId":101191,"corporation":false,"usgs":true,"family":"Lea","given":"C.","email":"","affiliations":[],"preferred":false,"id":496165,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Waltermire, B.","contributorId":70699,"corporation":false,"usgs":true,"family":"Waltermire","given":"B.","email":"","affiliations":[],"preferred":false,"id":496164,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Nordman, C.","contributorId":42885,"corporation":false,"usgs":true,"family":"Nordman","given":"C.","email":"","affiliations":[],"preferred":false,"id":496163,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70135075,"text":"70135075 - 2014 - Movements and activity of juvenile Brown Treesnakes (<i>Boiga irregularis</i>)","interactions":[],"lastModifiedDate":"2015-02-23T11:29:02","indexId":"70135075","displayToPublicDate":"2014-01-01T10:00:00","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1337,"text":"Copeia","active":true,"publicationSubtype":{"id":10}},"title":"Movements and activity of juvenile Brown Treesnakes (<i>Boiga irregularis</i>)","docAbstract":"<p>Understanding the spatial ecology and foraging strategy of invasive animals is essential for success in control or eradication. We studied movements and activity in juvenile Brown Treesnakes on Guam, as this population segment has proven particularly difficult to control. Distance between daytime refugia (from telemetry of 18 juveniles, 423-800 mm snout-vent length) ranged from 0-118 m (<i>n</i>  =  86), with a grand mean of 43 m. There were tendencies for shorter snake movements on nights directly following a full moon and on dry nights, but variation among snakes was of a larger magnitude and would greatly reduce chances to detect moon or rain effects unless corrected for. Snake activity was estimated from audio recordings of signals from &ldquo;tipping&rdquo; radio transmitters, analyzed for pulse period and amplitude. Activity was highest in the hours immediately after sunset, and gradually declined throughout the night before dropping abruptly in conjunction with sunrise. Snake activity was higher on rainy nights, and tended to be highest during waning moons and when the moon was below the horizon. We conclude that small Brown Treesnakes forage actively and appear to move far enough to regularly encounter the traps and bait used on Guam for control purposes, suggesting that alternative explanations are required for their low capture rates with these control tools.</p>","language":"English","publisher":"The American Society of Ichthyologists and Herpetologists","publisherLocation":"New York, NY","doi":"10.1643/CE-14-050","usgsCitation":"Lardner, B., Savidge, J., Reed, R., and Rodda, G.H., 2014, Movements and activity of juvenile Brown Treesnakes (<i>Boiga irregularis</i>): Copeia, v. 2014, no. 3, p. 428-436, https://doi.org/10.1643/CE-14-050.","productDescription":"9 p.","startPage":"428","endPage":"436","numberOfPages":"9","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-055312","costCenters":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"links":[{"id":296501,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"2014","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"54882b5ae4b02acb4f0c8c42","contributors":{"authors":[{"text":"Lardner, Bjorn lardnerb@usgs.gov","contributorId":5546,"corporation":false,"usgs":true,"family":"Lardner","given":"Bjorn","email":"lardnerb@usgs.gov","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":true,"id":526783,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Savidge, Julie A.","contributorId":10225,"corporation":false,"usgs":true,"family":"Savidge","given":"Julie A.","affiliations":[],"preferred":false,"id":526784,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Reed, Robert N. reedr@usgs.gov","contributorId":1686,"corporation":false,"usgs":true,"family":"Reed","given":"Robert N.","email":"reedr@usgs.gov","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":false,"id":526782,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Rodda, Gordon H. roddag@usgs.gov","contributorId":3196,"corporation":false,"usgs":true,"family":"Rodda","given":"Gordon","email":"roddag@usgs.gov","middleInitial":"H.","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":true,"id":526785,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70125296,"text":"70125296 - 2014 - Uranium-series ages of corals, sea level history, and palaeozoogeography, Canary Islands, Spain: an exploratory study for two Quaternary interglacial periods","interactions":[],"lastModifiedDate":"2014-09-18T10:01:01","indexId":"70125296","displayToPublicDate":"2014-01-01T09:57:00","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2996,"text":"Palaeogeography, Palaeoclimatology, Palaeoecology","printIssn":"0031-0182","active":true,"publicationSubtype":{"id":10}},"title":"Uranium-series ages of corals, sea level history, and palaeozoogeography, Canary Islands, Spain: an exploratory study for two Quaternary interglacial periods","docAbstract":"We present the first U-series ages of corals from emergent marine deposits on the Canary Islands. Deposits at + 20 m are 481 ± 39 ka, possibly correlative to marine isotope stage (or MIS) 11, while those at + 12 and + 8 m are 120.5 ± 0.8 ka and 130.2 ± 0.8 ka, respectively, correlative to MIS 5.5. The age, elevations, and uplift rates derived from MIS 5.5 deposits on the Canary Islands allow calculations of hypothetical palaeo-sea levels during the MIS 11 high sea stand. Estimates indicate that the MIS 11 high sea stand likely was at least + 9 m (relative to present sea level) and could have been as high as + 24 m. The most conservative estimates of palaeo-sea level during MIS 11 would require an ice mass loss equivalent to all of the modern Greenland and West Antarctic ice sheets; the more extreme estimates would require additional ice mass loss from the East Antarctic ice sheet. Extralimital southern species of mollusks, found in both MIS 11 and MIS 5.5 deposits on the Canary Islands, imply warmer-than-modern sea surface temperatures during at least a part of MIS 11 and much warmer sea surface temperatures during at least a part of MIS 5.5. Both MIS 11 and MIS 5.5 marine deposits on the Canary Islands contain extralimital northern species of mollusks as well, indicating cooler-than-present waters at times during these interglacial periods. We hypothesize that the co-occurrence of extralimital southern and northern species of marine invertebrates in the fossil record of the Canary Islands reflects its geographic location with respect to major synoptic-scale controls on climate and ocean currents. Previous interglacials may have been characterized by early, insolation-forced warming, along with northward migration of the intertropical convergence zone (ITCZ), accompanied by weakened trade winds and diminished upwelling. This allowed the arrival of extralimital southern taxa from the tropical Senegalese faunal province. During later parts of the MIS 11 and 5.5 interglacials, decreased insolation may have resulted in southward migration of the ITCZ, strengthened trade winds, and re-establishment of upwelling. Such conditions may have brought about not only local extinction of the Senegalese fauna, but allowed southward migration of the cooler-water Mediterranean fauna to the Canary Islands in the later parts of interglacials, a complex palaeoclimate record that is mirrored in the deep-sea core record.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Palaeogeography, Palaeoclimatology, Palaeoecology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","doi":"10.1016/j.palaeo.2013.11.015","usgsCitation":"Muhs, D.R., Meco, J., and Simmons, K., 2014, Uranium-series ages of corals, sea level history, and palaeozoogeography, Canary Islands, Spain: an exploratory study for two Quaternary interglacial periods: Palaeogeography, Palaeoclimatology, Palaeoecology, v. 394, p. 99-118, https://doi.org/10.1016/j.palaeo.2013.11.015.","productDescription":"20 p.","startPage":"99","endPage":"118","numberOfPages":"20","ipdsId":"IP-048991","costCenters":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"links":[{"id":488278,"rank":0,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"http://hdl.handle.net/10553/17952","text":"External Repository"},{"id":294108,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":294107,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.palaeo.2013.11.015"}],"country":"Spain","otherGeospatial":"Canary Islands","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -18.1612,27.6378 ], [ -18.1612,29.4165 ], [ -13.3336,29.4165 ], [ -13.3336,27.6378 ], [ -18.1612,27.6378 ] ] ] } } ] }","volume":"394","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"541bf460e4b0e96537ddf8fd","contributors":{"authors":[{"text":"Muhs, Daniel R. 0000-0001-7449-251X dmuhs@usgs.gov","orcid":"https://orcid.org/0000-0001-7449-251X","contributorId":1857,"corporation":false,"usgs":true,"family":"Muhs","given":"Daniel","email":"dmuhs@usgs.gov","middleInitial":"R.","affiliations":[{"id":218,"text":"Denver Federal Center","active":false,"usgs":true}],"preferred":true,"id":501174,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Meco, Joaquin","contributorId":38485,"corporation":false,"usgs":true,"family":"Meco","given":"Joaquin","email":"","affiliations":[],"preferred":false,"id":501176,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Simmons, Kathleen R. ksimmons@usgs.gov","contributorId":4742,"corporation":false,"usgs":true,"family":"Simmons","given":"Kathleen R.","email":"ksimmons@usgs.gov","affiliations":[{"id":218,"text":"Denver Federal Center","active":false,"usgs":true}],"preferred":false,"id":501175,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70074794,"text":"70074794 - 2014 - Mountain plover nest survival in relation to prairie dog and fire dynamics in shortgrass steppe","interactions":[],"lastModifiedDate":"2017-11-27T13:15:08","indexId":"70074794","displayToPublicDate":"2014-01-01T09:48:00","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2508,"text":"Journal of Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"Mountain plover nest survival in relation to prairie dog and fire dynamics in shortgrass steppe","docAbstract":"<p><span>Disturbed xeric grasslands with short, sparse vegetation provide breeding habitat for mountain plovers (</span><i>Charadrius montanus</i><span>) across the western Great Plains. Maintaining local disturbance regimes through prairie dog conservation and prescribed fire may contribute to the sustainability of recently declining mountain plover populations, but these management approaches can be controversial. We estimated habitat-specific mountain plover densities and nest survival rates on black-tailed prairie dog (</span><i>Cynomys ludovicianus</i><span>) colonies and burns in the shortgrass steppe of northeastern Colorado. Mountain plover densities were similar on prairie dog colonies (5.9 birds/km</span><sup>2</sup><span>; 95% CI = 4.7–7.4) and sites burned during the preceding dormant season (6.7 birds/km</span><sup>2</sup><span>; 95% CI = 4.6–9.6), whereas the 29-day nest survival rate was greater on prairie dog colonies (0.81 in 2011 and 0.39 in 2012) compared to the burned sites (0.64 in 2011 and 0.17 in 2012). Reduced nest survival in 2012 compared to 2011 was associated with higher maximum daily temperatures in 2012, consistent with a previous weather-based model of mountain plover nest survival in the southern Great Plains. Measurements of mountain plover density relative to time since disturbance showed that removal of prairie dog disturbance by sylvatic plague reduced mountain plover density by 70% relative to active prairie dog colonies after 1 year. Plover densities declined at a similar rate (by 78%) at burned sites between the first and second post-burn growing season. Results indicate that black-tailed prairie dog colonies are a particularly important nesting habitat for mountain plovers in the southern Great Plains. In addition, findings suggest that prescribed burning can be a valuable means to create nesting habitat in landscapes where other types of disturbances (such as prairie dog colonies) are limited in distribution and size.<span>&nbsp;</span></span></p>","language":"English","publisher":"Wiley","doi":"10.1002/jwmg.700","usgsCitation":"Augustine, D., and Skagen, S., 2014, Mountain plover nest survival in relation to prairie dog and fire dynamics in shortgrass steppe: Journal of Wildlife Management, v. 78, no. 4, p. 595-602, https://doi.org/10.1002/jwmg.700.","productDescription":"8 p.","startPage":"595","endPage":"602","ipdsId":"IP-052363","costCenters":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"links":[{"id":282023,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Colorado","county":"Weld County","volume":"78","issue":"4","noUsgsAuthors":false,"publicationDate":"2014-04-08","publicationStatus":"PW","scienceBaseUri":"53cd6035e4b0b290850fcc62","contributors":{"authors":[{"text":"Augustine, David J.","contributorId":36849,"corporation":false,"usgs":true,"family":"Augustine","given":"David J.","affiliations":[],"preferred":false,"id":489891,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Skagen, Susan K. 0000-0002-6744-1244 skagens@usgs.gov","orcid":"https://orcid.org/0000-0002-6744-1244","contributorId":167829,"corporation":false,"usgs":true,"family":"Skagen","given":"Susan K.","email":"skagens@usgs.gov","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":false,"id":723574,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70160456,"text":"70160456 - 2014 - Space use of wintering waterbirds in India: Influence of trophic ecology on home-range size","interactions":[],"lastModifiedDate":"2020-12-23T15:18:34.518003","indexId":"70160456","displayToPublicDate":"2014-01-01T09:45:00","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1362,"text":"Current Zoology","active":true,"publicationSubtype":{"id":10}},"title":"Space use of wintering waterbirds in India: Influence of trophic ecology on home-range size","docAbstract":"<p>Relationship between species' home range and their other biological traits remains poorly understood, especially in migratory birds due to the difficulty associated with tracking them. Advances in satellite telemetry and remote sensing techniques have proved instrumental in overcoming such challenges. We studied the space use of migratory ducks through satellite telemetry with an objective of understanding the influence of body mass and feeding habits on their home-range sizes. We marked 26 individuals, representing five species of migratory ducks, with satellite transmitters during two consecutive winters in three Indian states. We used kernel methods to estimate home ranges and core use areas of these waterfowl, and assessed the influence of body mass and feeding habits on home-range size. Feeding habits influenced the home-range size of the migratory ducks. Carnivorous ducks had the largest home ranges, herbivorous ducks the smallest, while omnivorous species had intermediate home-ranges. Body mass did not explain variation in home-range size. To our knowledge, this is the first study of its kind on migratory ducks, and it has important implications for their conservation and management.</p>","language":"English","publisher":"Chinese Academy of Sciences","publisherLocation":"Beijing","doi":"10.1093/czoolo/60.5.616","usgsCitation":"Namgail, T., Takekawa, J.Y., Balachandran, S., Sathiyaselvam, P., Mundkur, T., and Newman, S.H., 2014, Space use of wintering waterbirds in India: Influence of trophic ecology on home-range size: Current Zoology, v. 60, no. 5, p. 616-621, https://doi.org/10.1093/czoolo/60.5.616.","productDescription":"6 p.","startPage":"616","endPage":"621","numberOfPages":"6","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-035554","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":473267,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1093/czoolo/60.5.616","text":"Publisher Index Page"},{"id":312566,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"India","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[77.83745,35.49401],[78.91227,34.32194],[78.81109,33.5062],[79.20889,32.99439],[79.17613,32.48378],[78.45845,32.61816],[78.73889,31.51591],[79.72137,30.88271],[81.11126,30.18348],[80.47672,29.72987],[80.08842,28.79447],[81.0572,28.4161],[81.99999,27.92548],[83.30425,27.36451],[84.67502,27.2349],[85.25178,26.7262],[86.02439,26.63098],[87.22747,26.3979],[88.06024,26.41462],[88.1748,26.81041],[88.04313,27.44582],[88.12044,27.87654],[88.73033,28.08686],[88.81425,27.29932],[88.83564,27.09897],[89.74453,26.7194],[90.37327,26.87572],[91.21751,26.80865],[92.03348,26.83831],[92.10371,27.45261],[91.69666,27.77174],[92.50312,27.89688],[93.41335,28.64063],[94.56599,29.27744],[95.4048,29.03172],[96.11768,29.4528],[96.58659,28.83098],[96.24883,28.41103],[97.32711,28.26158],[97.40256,27.88254],[97.05199,27.69906],[97.134,27.08377],[96.41937,27.26459],[95.12477,26.57357],[95.15515,26.00131],[94.60325,25.1625],[94.55266,24.67524],[94.10674,23.85074],[93.32519,24.07856],[93.28633,23.04366],[93.06029,22.70311],[93.16613,22.27846],[92.67272,22.04124],[92.14603,23.6275],[91.86993,23.62435],[91.70648,22.98526],[91.15896,23.50353],[91.46773,24.07264],[91.91509,24.13041],[92.3762,24.97669],[91.7996,25.14743],[90.87221,25.1326],[89.92069,25.26975],[89.83248,25.96508],[89.35509,26.01441],[88.56305,26.44653],[88.20979,25.76807],[88.93155,25.23869],[88.30637,24.86608],[88.08442,24.50166],[88.69994,24.23371],[88.52977,23.63114],[88.87631,22.87915],[89.03196,22.05571],[88.88877,21.69059],[88.2085,21.70317],[86.9757,21.49556],[87.03317,20.74331],[86.49935,20.15164],[85.06027,19.47858],[83.94101,18.30201],[83.18922,17.67122],[82.19279,17.01664],[82.19124,16.55666],[81.69272,16.31022],[80.792,15.95197],[80.3249,15.89918],[80.02507,15.13641],[80.23327,13.83577],[80.28629,13.00626],[79.86255,12.05622],[79.858,10.35728],[79.34051,10.30885],[78.88535,9.54614],[79.18972,9.21654],[78.27794,8.93305],[77.94117,8.25296],[77.5399,7.96553],[76.59298,8.89928],[76.13006,10.29963],[75.74647,11.30825],[75.3961,11.78125],[74.86482,12.74194],[74.61672,13.99258],[74.44386,14.61722],[73.5342,15.99065],[73.11991,17.92857],[72.82091,19.20823],[72.82448,20.4195],[72.63053,21.35601],[71.17527,20.75744],[70.47046,20.87733],[69.16413,22.0893],[69.64493,22.45077],[69.3496,22.84318],[68.17665,23.69197],[68.8426,24.35913],[71.04324,24.35652],[70.8447,25.2151],[70.28287,25.72223],[70.16893,26.49187],[69.51439,26.94097],[70.6165,27.9892],[71.77767,27.91318],[72.82375,28.96159],[73.45064,29.97641],[74.42138,30.97981],[74.40593,31.69264],[75.25864,32.27111],[74.45156,32.7649],[74.10429,33.44147],[73.74995,34.3177],[74.2402,34.74889],[75.75706,34.50492],[76.87172,34.65354],[77.83745,35.49401]]]},\"properties\":{\"name\":\"India\"}}]}","volume":"60","issue":"5","publishingServiceCenter":{"id":1,"text":"Sacramento PSC"},"noUsgsAuthors":false,"publicationDate":"2014-10-01","publicationStatus":"PW","scienceBaseUri":"567930d4e4b0da412f4fb599","contributors":{"authors":[{"text":"Namgail, Tsewang","contributorId":150756,"corporation":false,"usgs":false,"family":"Namgail","given":"Tsewang","email":"","affiliations":[{"id":18092,"text":"formerly with U.S. Geological Survey, Western Ecological Research Center","active":true,"usgs":false}],"preferred":false,"id":582949,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Takekawa, John Y. 0000-0003-0217-5907 john_takekawa@usgs.gov","orcid":"https://orcid.org/0000-0003-0217-5907","contributorId":176168,"corporation":false,"usgs":true,"family":"Takekawa","given":"John","email":"john_takekawa@usgs.gov","middleInitial":"Y.","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":false,"id":582948,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Balachandran, Sivananinthaperumal","contributorId":20593,"corporation":false,"usgs":true,"family":"Balachandran","given":"Sivananinthaperumal","affiliations":[],"preferred":false,"id":582950,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Sathiyaselvam, Ponnusamy","contributorId":150757,"corporation":false,"usgs":false,"family":"Sathiyaselvam","given":"Ponnusamy","email":"","affiliations":[{"id":18093,"text":"Bombay Natural History Society","active":true,"usgs":false}],"preferred":false,"id":582951,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Mundkur, Taej","contributorId":107843,"corporation":false,"usgs":true,"family":"Mundkur","given":"Taej","affiliations":[],"preferred":false,"id":582952,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Newman, Scott H.","contributorId":101372,"corporation":false,"usgs":true,"family":"Newman","given":"Scott","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":582953,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70137376,"text":"70137376 - 2014 - Wintering ecology of adult North American ospreys","interactions":[],"lastModifiedDate":"2017-11-24T17:58:10","indexId":"70137376","displayToPublicDate":"2014-01-01T09:45:00","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2442,"text":"Journal of Raptor Research","active":true,"publicationSubtype":{"id":10}},"title":"Wintering ecology of adult North American ospreys","docAbstract":"<p>North American Ospreys (<i>Pandion haliaetus</i>) typically migrate long distances to their wintering grounds in the tropics. Beyond the general distribution of their wintering range (i.e., the Caribbean, South America, and Central America), very little is known about the wintering ecology of these birds. We used satellite telemetry to determine the duration of wintering period, to examine the characteristics of wintering areas used by Ospreys, and to quantify space use and activity patterns of wintering Ospreys. Adult Ospreys migrated to wintering sites and exhibited high wintering site fidelity among years. Overall, Ospreys wintered on river systems (50.6%) more than on lakes (19.0%), and use of coastal areas was (30.4%) intermediate. Ospreys remained on their wintering grounds for an average of 154 d for males and 167 d for females. Locations of wintering Ospreys obtained via GPS-capable satellite telemetry suggest these birds move infrequently and their movements are very localized (i.e., 2 and 1.4 km<sup>2</sup>, respectively. Overall, our findings suggest wintering adult North American Ospreys are very sedentary, demonstrating a pattern of limited daily movements and high fidelity to a few select locations (presumably roosts). We suggest this wintering strategy might be effective for reducing the risk of mortality and maximizing energy conservation.</p>","language":"English","publisher":"Raptor Research Foundation","publisherLocation":"Hastings, MN","doi":"10.3356/JRR-OSPR-13-01.1","usgsCitation":"Washburn, B.E., Martell, M.S., Bierregaard, R.O., Henny, C.J., Dorr, B.S., and Olexa, T.J., 2014, Wintering ecology of adult North American ospreys: Journal of Raptor Research, v. 48, no. 4, p. 325-333, https://doi.org/10.3356/JRR-OSPR-13-01.1.","productDescription":"9 p.","startPage":"325","endPage":"333","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-023638","costCenters":[{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true}],"links":[{"id":473266,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.3356/jrr-ospr-13-01.1","text":"Publisher Index Page"},{"id":297067,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"48","issue":"4","publishingServiceCenter":{"id":12,"text":"Tacoma PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"54dd2c93e4b08de9379b387d","contributors":{"authors":[{"text":"Washburn, Brian E.","contributorId":138539,"corporation":false,"usgs":false,"family":"Washburn","given":"Brian","email":"","middleInitial":"E.","affiliations":[{"id":12434,"text":"USDA, Wildlife Services, National Wildlife Research Center","active":true,"usgs":false}],"preferred":false,"id":537779,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Martell, Mark S.","contributorId":138541,"corporation":false,"usgs":false,"family":"Martell","given":"Mark","email":"","middleInitial":"S.","affiliations":[{"id":35833,"text":"The Raptor Center at the University of Minnesota","active":true,"usgs":false},{"id":12435,"text":"Audubon Minnesota","active":true,"usgs":false}],"preferred":false,"id":537781,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bierregaard, Richard O. Jr.","contributorId":138542,"corporation":false,"usgs":false,"family":"Bierregaard","given":"Richard","suffix":"Jr.","email":"","middleInitial":"O.","affiliations":[{"id":12436,"text":"University of North Carolina at Charlotte","active":true,"usgs":false}],"preferred":false,"id":537782,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Henny, Charles J. 0000-0001-7474-350X hennyc@usgs.gov","orcid":"https://orcid.org/0000-0001-7474-350X","contributorId":3461,"corporation":false,"usgs":true,"family":"Henny","given":"Charles","email":"hennyc@usgs.gov","middleInitial":"J.","affiliations":[{"id":289,"text":"Forest and Rangeland Ecosys Science Center","active":true,"usgs":true}],"preferred":true,"id":537778,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Dorr, Brian S.","contributorId":138540,"corporation":false,"usgs":false,"family":"Dorr","given":"Brian","email":"","middleInitial":"S.","affiliations":[{"id":12434,"text":"USDA, Wildlife Services, National Wildlife Research Center","active":true,"usgs":false}],"preferred":false,"id":537780,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Olexa, Thomas J.","contributorId":138543,"corporation":false,"usgs":false,"family":"Olexa","given":"Thomas","email":"","middleInitial":"J.","affiliations":[{"id":12434,"text":"USDA, Wildlife Services, National Wildlife Research Center","active":true,"usgs":false}],"preferred":false,"id":537783,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70099986,"text":"70099986 - 2014 - Glacial and Quaternary geology of the northern Yellowstone area, Montana and Wyoming","interactions":[],"lastModifiedDate":"2014-06-03T15:59:54","indexId":"70099986","displayToPublicDate":"2014-01-01T09:39:00","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1724,"text":"GSA Field Guides","active":true,"publicationSubtype":{"id":10}},"title":"Glacial and Quaternary geology of the northern Yellowstone area, Montana and Wyoming","docAbstract":"<p>This field guide focuses on the glacial geology and paleoecology beginning in the Paradise Valley and progressing southward into northern Yellowstone National Park. During the last (Pinedale) glaciation, the northern Yellowstone outlet glacier flowed out of Yellowstone Park and down the Yellowstone River Valley into the Paradise Valley. The field trip will traverse the following Pinedale glacial sequence: (1) deposition of the Eightmile terminal moraines and outwash 16.5 ± 1.4 10Be ka in the Paradise Valley; (2) glacial recession of ~8 km and deposition of the Chico moraines and outwash 16.1 ± 1.7 10Be ka; (3) glacial recession of 45 km to near the northern Yellowstone boundary and moraine deposition during the Deckard Flats readjustment 14.2 ± 1.2 10Be ka; and (4) glacial recession of ~37 km and deposition of the Junction Butte moraines 15.2 ± 1.3 10Be ka (this age is a little too old based on the stratigraphic sequence). Yellowstone's northern range of sagebrush-grasslands and bison, elk, wolf, and bear inhabitants is founded on glacial moraines, sub-glacial till, and outwash deposited during the last glaciation. Floods released from glacially dammed lakes and a landslide-dammed lake punctuate this record.</p>\n<br>\n<p>The glacial geologic reconstruction was evaluated by calculation of basal shear stress, and yielded the following values for flow pattern in plan view: strongly converging—1.21 ± 0.12 bars (n = 15); nearly uniform—1.04 ± 0.16 bars (n = 11); and strongly diverging—0.84 ± 0.14 bars (n = 16). Reconstructed mass balance yielded accumulation and ablation each of ~3 km3/yr, with glacial movement near the equilibrium line altitude dominated by basal sliding.</p>\n<br>\n<p>Pollen and charcoal records from three lakes in northern Yellowstone provide information on the postglacial vegetation and fire history. Following glacial retreat, sparsely vegetated landscapes were colonized first by spruce parkland and then by closed subalpine forests. Regional fire activity increased significantly with the development of closed subalpine forests as a result of increased fuel biomass and warmer summers. Warm dry conditions prevailed at low elevations during the early Holocene, as indicated by the presence of steppe and open mixed conifer forest. At the same time, closed subalpine forests with low fire frequency were present at higher elevations, suggesting relatively wet summer conditions. Douglas fir populations expanded throughout northern Yellowstone in the middle Holocene as a result of effectively drier conditions than before, and a decline of mesophytic plant taxa during the late Holocene imply continued drying, even though fire frequency decreased in recent millennia.</p>","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"GSA Field Guides","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Geological Society of America","doi":"10.1130/2014.0037(09)","usgsCitation":"Pierce, K.L., Licciardi, J.M., Krause, T., and Whitlock, C., 2014, Glacial and Quaternary geology of the northern Yellowstone area, Montana and Wyoming: GSA Field Guides, v. 37, p. 189-203, https://doi.org/10.1130/2014.0037(09).","productDescription":"15 p.","startPage":"189","endPage":"203","numberOfPages":"15","ipdsId":"IP-053643","costCenters":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"links":[{"id":288049,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":288048,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1130/2014.0037(09)"}],"country":"United States","state":"Montana;Wyoming","otherGeospatial":"Yellowstone Park;Yellowstone River Valley","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -111.0,45.0 ], [ -111.0,45.5 ], [ -110.0,45.5 ], [ -110.0,45.0 ], [ -111.0,45.0 ] ] ] } } ] }","volume":"37","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"538eee8de4b0d497d4968504","contributors":{"authors":[{"text":"Pierce, Kenneth L. kpierce@usgs.gov","contributorId":1609,"corporation":false,"usgs":true,"family":"Pierce","given":"Kenneth","email":"kpierce@usgs.gov","middleInitial":"L.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true},{"id":481,"text":"Northern Rocky Mountain Science Center","active":true,"usgs":true},{"id":547,"text":"Rocky Mountain Geographic Science Center","active":true,"usgs":true}],"preferred":true,"id":492091,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Licciardi, Joseph M.","contributorId":9759,"corporation":false,"usgs":false,"family":"Licciardi","given":"Joseph","email":"","middleInitial":"M.","affiliations":[{"id":12667,"text":"University of New Hampshire","active":true,"usgs":false}],"preferred":false,"id":492092,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Krause, Teresa R.","contributorId":71479,"corporation":false,"usgs":true,"family":"Krause","given":"Teresa R.","affiliations":[],"preferred":false,"id":492093,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Whitlock, Cathy","contributorId":79745,"corporation":false,"usgs":false,"family":"Whitlock","given":"Cathy","email":"","affiliations":[{"id":6604,"text":"University of Oregon","active":true,"usgs":false}],"preferred":false,"id":492094,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70127994,"text":"70127994 - 2014 - Dendroclimatic potential of plains cottonwood (Populus deltoides subsp. monilifera) from the Northern Great Plains, USA","interactions":[],"lastModifiedDate":"2018-02-12T18:29:14","indexId":"70127994","displayToPublicDate":"2014-01-01T09:38:00","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3650,"text":"Tree-Ring Research","onlineIssn":"2162-4585","printIssn":"1536-1098","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Dendroclimatic potential of plains cottonwood (<i>Populus deltoides</i> subsp. <i>monilifera</i>) from the Northern Great Plains, USA","title":"Dendroclimatic potential of plains cottonwood (Populus deltoides subsp. monilifera) from the Northern Great Plains, USA","docAbstract":"<p><span>A new 368-year tree-ring chronology (A.D. 1643–2010) has been developed in western North Dakota using plains cottonwood (</span><i>Populus deltoides</i><span><span>&nbsp;</span>subsp.<span>&nbsp;</span></span><i>monilifera</i><span>) growing on the relatively undisturbed floodplain of the Little Missouri River in the North Unit of Theodore Roosevelt National Park. We document many slow-growing living trees between 150–370&nbsp;years old that contradict the common understanding that cottonwoods grow fast and die young. In this northern location, cottonwood produces distinct annual rings with dramatic interannual variability that strongly crossdate. The detrended tree-ring chronology is significantly positively correlated with local growing season precipitation and soil moisture conditions (r  =  0.69). This time series shows periods of prolonged low radial tree growth during the known droughts of the instrumental record (</span><i>e.g.</i><span><span>&nbsp;</span>1931–1939 and 1980–1981) and also during prehistory (</span><i>e.g.</i><span><span>&nbsp;</span>1816–1823 and 1856–1865) when other paleoclimate studies have documented droughts in this region. Tree rings of cottonwood will be a useful tool to help reconstruct climate, streamflow, and the floodplain history of the Little Missouri River and other northern river systems.</span></p>","language":"English","publisher":"Tree-Ring Society","doi":"10.3959/1536-1098-70.1.21","usgsCitation":"Edmonson, J., Friedman, J., Meko, D., Touchan, R., Scott, J., and Edmonson, A., 2014, Dendroclimatic potential of plains cottonwood (Populus deltoides subsp. monilifera) from the Northern Great Plains, USA: Tree-Ring Research, v. 70, no. 1, p. 21-30, https://doi.org/10.3959/1536-1098-70.1.21.","productDescription":"10 p.","startPage":"21","endPage":"30","ipdsId":"IP-051062","costCenters":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"links":[{"id":473269,"rank":0,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://doi.org/10.3959/1536-1098-70.1.21","text":"External Repository"},{"id":294894,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"North Dakota","otherGeospatial":"Little Missouri River, Theodore Roosevelt National Park","volume":"70","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"542fba9ae4b092f17df61cf8","contributors":{"authors":[{"text":"Edmonson, Jesse","contributorId":19494,"corporation":false,"usgs":true,"family":"Edmonson","given":"Jesse","email":"","affiliations":[],"preferred":false,"id":502725,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Friedman, Jonathan","contributorId":33241,"corporation":false,"usgs":true,"family":"Friedman","given":"Jonathan","email":"","affiliations":[],"preferred":false,"id":502726,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Meko, David","contributorId":17166,"corporation":false,"usgs":true,"family":"Meko","given":"David","affiliations":[],"preferred":false,"id":502724,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Touchan, Ramzi","contributorId":77863,"corporation":false,"usgs":true,"family":"Touchan","given":"Ramzi","affiliations":[],"preferred":false,"id":502729,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Scott, Julian","contributorId":61764,"corporation":false,"usgs":false,"family":"Scott","given":"Julian","affiliations":[{"id":12742,"text":"University of Nevada Reno","active":true,"usgs":false}],"preferred":false,"id":502727,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Edmonson, Alan","contributorId":77068,"corporation":false,"usgs":true,"family":"Edmonson","given":"Alan","email":"","affiliations":[],"preferred":false,"id":502728,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70119659,"text":"70119659 - 2014 - Suspended particulate layers and internal waves over the southern Monterey Bay continental shelf: an important control on shelf mud belts?","interactions":[],"lastModifiedDate":"2014-08-08T09:41:25","indexId":"70119659","displayToPublicDate":"2014-01-01T09:38:00","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2315,"text":"Journal of Geophysical Research C: Oceans","active":true,"publicationSubtype":{"id":10}},"title":"Suspended particulate layers and internal waves over the southern Monterey Bay continental shelf: an important control on shelf mud belts?","docAbstract":"<p>Physical and optical measurements taken over the mud belt on the southern continental shelf of Monterey Bay, California documented the frequent occurrence of suspended particulate matter features, the majority of which were detached from the seafloor, centered 9–33 m above the bed. In fall 2011, an automated profiling mooring and fixed instrumentation, including a thermistor chain and upward-looking acoustic Doppler current profiler, were deployed at 70 m depth for 5 weeks, and from 12 to 16 October a long-range autonomous underwater vehicle performed across-shelf transects. Individual SPM events were uncorrelated with local bed shear stress caused by surface waves and bottom currents. Nearly half of all observed SPM layers occurred during 1 week of the study, 9–16 October 2011, and were advected past the fixed profiling mooring by the onshore phase of semidiurnal internal tide bottom currents. At the start of the 9–16 October period, we observed intense near-bed vertical velocities capable of lifting particulates into the middle of the water column. This “updraft” event appears to have been associated with nonlinear adjustment of high-amplitude internal tides over the mid and outer shelf. These findings suggest that nonlinear internal tidal motions can erode material over the outer shelf and that, once suspended, this SPM can then be transported shoreward to the middle and shallow sections of the mud belt. This represents a fundamental broadening of our understanding of how shelf mud belts may be built up and sustained.</p>","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Geophysical Research C: Oceans","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Wiley","doi":"10.1002/2013JC009360","usgsCitation":"Cheriton, O., McPhee-Shaw, E.E., Shaw, W.J., Stanton, T., Bellingham, J.G., and Storlazzi, C., 2014, Suspended particulate layers and internal waves over the southern Monterey Bay continental shelf: an important control on shelf mud belts?: Journal of Geophysical Research C: Oceans, v. 119, no. 1, p. 428-444, https://doi.org/10.1002/2013JC009360.","productDescription":"17 p.","startPage":"428","endPage":"444","numberOfPages":"17","ipdsId":"IP-054074","costCenters":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":473268,"rank":0,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"http://hdl.handle.net/10945/46126","text":"External Repository"},{"id":291898,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":291897,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1002/2013JC009360"}],"country":"United States","state":"California","otherGeospatial":"Monterey Bay","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -122.5,36.6 ], [ -122.5,37.0 ], [ -121.8,37.0 ], [ -121.8,36.6 ], [ -122.5,36.6 ] ] ] } } ] }","volume":"119","issue":"1","noUsgsAuthors":false,"publicationDate":"2014-01-21","publicationStatus":"PW","scienceBaseUri":"53e5e445e4b0b6c2798afaf8","contributors":{"authors":[{"text":"Cheriton, Olivia M. 0000-0003-3011-9136","orcid":"https://orcid.org/0000-0003-3011-9136","contributorId":7630,"corporation":false,"usgs":true,"family":"Cheriton","given":"Olivia M.","affiliations":[],"preferred":false,"id":497752,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McPhee-Shaw, Erika E.","contributorId":77855,"corporation":false,"usgs":true,"family":"McPhee-Shaw","given":"Erika","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":497755,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Shaw, William J.","contributorId":79029,"corporation":false,"usgs":true,"family":"Shaw","given":"William","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":497757,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Stanton, Timothy P.","contributorId":18281,"corporation":false,"usgs":true,"family":"Stanton","given":"Timothy P.","affiliations":[],"preferred":false,"id":497753,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Bellingham, James G.","contributorId":69071,"corporation":false,"usgs":true,"family":"Bellingham","given":"James","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":497754,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Storlazzi, Curt D. 0000-0001-8057-4490","orcid":"https://orcid.org/0000-0001-8057-4490","contributorId":77889,"corporation":false,"usgs":true,"family":"Storlazzi","given":"Curt D.","affiliations":[],"preferred":false,"id":497756,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70095528,"text":"70095528 - 2014 - A tetrapod-like repertoire of innate immune receptors and effectors for coelacanths","interactions":[],"lastModifiedDate":"2016-04-26T15:47:47","indexId":"70095528","displayToPublicDate":"2014-01-01T09:30:00","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2281,"text":"Journal of Experimental Zoology Part B: Molecular and Developmental Evolution","active":true,"publicationSubtype":{"id":10}},"title":"A tetrapod-like repertoire of innate immune receptors and effectors for coelacanths","docAbstract":"<p>The recent availability of both robust transcriptome and genome resources for coelacanth (<i>Latimeria chalumnae</i>) has led to unique discoveries for coelacanth immunity such as the lack of IgM, a central component of adaptive immunity. This study was designed to more precisely address the origins and evolution of gene families involved in the initial recognition and response to microbial pathogens, which effect innate immunity. Several multigene families involved in innate immunity are addressed, including: Toll-like receptors (TLRs), retinoic acid inducible gene 1 (RIG1)-like receptors (RLRs), the nucleotide-binding domain and leucine-rich repeat containing proteins (NLRs), diverse immunoglobulin domain-containing proteins (DICP) and modular domain immune-type receptors (MDIRs). Our analyses also include the tripartite motif-containing proteins (TRIM), which are involved in pathogen recognition as well as the positive regulation of antiviral immunity. Finally, this study addressed some of the downstream effectors of the antimicrobial response including IL-1 family members, type I and II interferons (IFN) and IFN-stimulated effectors (ISGs). Collectively, the genes and gene families in coelacanth that effect innate immune functions share characteristics both in content, structure and arrangement with those found in tetrapods but not in teleosts. The findings support the sister group relationship of coelacanth fish with tetrapods.</p>","language":"English","publisher":"Wiley","doi":"10.1002/jez.b.22559","usgsCitation":"Boudinot, P., Zou, J., Ota, T., Buonocore, F., Scapigliati, G., Canapa, A., Cannon, J., Litman, G., and Hansen, J.D., 2014, A tetrapod-like repertoire of innate immune receptors and effectors for coelacanths: Journal of Experimental Zoology Part B: Molecular and Developmental Evolution, v. 322, no. 6, p. 415-437, https://doi.org/10.1002/jez.b.22559.","productDescription":"23 p.","startPage":"415","endPage":"437","numberOfPages":"23","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-050912","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":502436,"rank":0,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://ir.soken.ac.jp/records/5433","text":"External Repository"},{"id":283453,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":283361,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1002/jez.b.22559"}],"volume":"322","issue":"6","noUsgsAuthors":false,"publicationDate":"2014-01-30","publicationStatus":"PW","scienceBaseUri":"53cd4ac1e4b0b290850eff67","contributors":{"authors":[{"text":"Boudinot, Pierre","contributorId":106013,"corporation":false,"usgs":true,"family":"Boudinot","given":"Pierre","affiliations":[],"preferred":false,"id":491255,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Zou, Jun","contributorId":31676,"corporation":false,"usgs":true,"family":"Zou","given":"Jun","email":"","affiliations":[],"preferred":false,"id":491248,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ota, Tatsuya","contributorId":61336,"corporation":false,"usgs":true,"family":"Ota","given":"Tatsuya","affiliations":[],"preferred":false,"id":491251,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Buonocore, Francesco","contributorId":39693,"corporation":false,"usgs":true,"family":"Buonocore","given":"Francesco","email":"","affiliations":[],"preferred":false,"id":491249,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Scapigliati, Giuseppe","contributorId":46419,"corporation":false,"usgs":true,"family":"Scapigliati","given":"Giuseppe","email":"","affiliations":[],"preferred":false,"id":491250,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Canapa, Adriana","contributorId":64557,"corporation":false,"usgs":true,"family":"Canapa","given":"Adriana","email":"","affiliations":[],"preferred":false,"id":491252,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Cannon, John","contributorId":98218,"corporation":false,"usgs":true,"family":"Cannon","given":"John","email":"","affiliations":[],"preferred":false,"id":491254,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Litman, Gary","contributorId":94975,"corporation":false,"usgs":true,"family":"Litman","given":"Gary","affiliations":[],"preferred":false,"id":491253,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Hansen, John D. 0000-0002-3006-2734 jhansen@usgs.gov","orcid":"https://orcid.org/0000-0002-3006-2734","contributorId":3440,"corporation":false,"usgs":true,"family":"Hansen","given":"John","email":"jhansen@usgs.gov","middleInitial":"D.","affiliations":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"preferred":true,"id":491247,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}}
,{"id":70126404,"text":"70126404 - 2014 - The geochemistry of deep-sea coral skeletons: a review of vital effects and applications for palaeoceanography","interactions":[],"lastModifiedDate":"2017-06-30T14:04:14","indexId":"70126404","displayToPublicDate":"2014-01-01T09:25:00","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1371,"text":"Deep-Sea Research Part II: Topical Studies in Oceanography","active":true,"publicationSubtype":{"id":10}},"title":"The geochemistry of deep-sea coral skeletons: a review of vital effects and applications for palaeoceanography","docAbstract":"Deep-sea corals were discovered over a century ago, but it is only over recent years that focused efforts have been made to explore the history of the oceans using the geochemistry of their skeletal remains. They offer a promising archive of past oceanic environments given their global distribution, layered growth patterns, longevity and preservation as well as our ability to date them using radiometric techniques. This paper provides an overview of the current state-of-the-art in terms of geochemical approaches to using deep-sea coral skeletons to explore the history of the ocean. Deep-sea coral skeletons have a wide array of morphologies (e.g. solitary cup corals, branching colonial corals) and materials (calcite, aragonite and proteins). As such their biomineralization strategies are diverse, leading to complex geochemistry within coral skeletons. Notwithstanding these complications, progress has been made on developing methods for reconstructing the oceanographic environment in the past using trace elements and isotopic methods. Promising approaches within certain coral groups include clumped isotopes and Mg/Li for temperature reconstructions, boron isotopes and radiocarbon for carbon cycling, εNd, and radiocarbon for circulation studies and δ<sup>15</sup>N, P/Ca and Ba/Ca for nutrient tracer studies. Likewise there is now a range of techniques for dating deep-sea corals skeletons (e.g. U-series, radiocarbon), and determining their growth rates (e.g. radiocarbon and <sup>210</sup>Pb). Dating studies on historic coral populations in the Atlantic, Southern Ocean and Pacific point to climate and environmental changes being dominant controls on coral populations over millennial and orbital timescales. This paper provides a review of a range of successes and promising approaches. It also highlights areas in which further research would likely provide new insights into biomineralization, palaeoceanography and distribution of past coral populations.","language":"English","publisher":"Elsevier","doi":"10.1016/j.dsr2.2013.06.005","usgsCitation":"Robinson, L., Adkins, J.F., Frank, N., Gagon, A.C., Prouty, N.G., Roark, E., and van de Flierdt, T., 2014, The geochemistry of deep-sea coral skeletons: a review of vital effects and applications for palaeoceanography: Deep-Sea Research Part II: Topical Studies in Oceanography, v. 99, p. 184-198, https://doi.org/10.1016/j.dsr2.2013.06.005.","productDescription":"15 p.","startPage":"184","endPage":"198","numberOfPages":"15","ipdsId":"IP-052683","costCenters":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":294287,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":294286,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.dsr2.2013.06.005"}],"volume":"99","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5422bb33e4b08312ac7cf0f0","contributors":{"authors":[{"text":"Robinson, Laura F.","contributorId":6179,"corporation":false,"usgs":true,"family":"Robinson","given":"Laura F.","affiliations":[],"preferred":false,"id":502004,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Adkins, Jess F.","contributorId":7639,"corporation":false,"usgs":true,"family":"Adkins","given":"Jess","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":502005,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Frank, Norbert","contributorId":17546,"corporation":false,"usgs":true,"family":"Frank","given":"Norbert","affiliations":[],"preferred":false,"id":502006,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Gagon, Alexander C.","contributorId":48117,"corporation":false,"usgs":true,"family":"Gagon","given":"Alexander","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":502009,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Prouty, Nancy G. 0000-0002-8922-0688 nprouty@usgs.gov","orcid":"https://orcid.org/0000-0002-8922-0688","contributorId":3350,"corporation":false,"usgs":true,"family":"Prouty","given":"Nancy","email":"nprouty@usgs.gov","middleInitial":"G.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":502003,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Roark, E. Brendan","contributorId":25464,"corporation":false,"usgs":true,"family":"Roark","given":"E. Brendan","affiliations":[],"preferred":false,"id":502007,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"van de Flierdt, Tina","contributorId":34434,"corporation":false,"usgs":true,"family":"van de Flierdt","given":"Tina","affiliations":[],"preferred":false,"id":502008,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70260406,"text":"70260406 - 2014 - Mount St. Helens, Washington, USA","interactions":[],"lastModifiedDate":"2024-11-01T14:24:59.869231","indexId":"70260406","displayToPublicDate":"2014-01-01T09:18:40","publicationYear":"2014","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Mount St. Helens, Washington, USA","docAbstract":"<p><span>May 18, 1980. Sunrise and a crystal-clear morning. Mount St. Helens was a beautiful, peaceful, snow-capped mountain surrounded by pristine forests and lakes(Fig.&nbsp;15.1). Yes, it was known to be spitting ash and shaking, but it was still fundamentally the same Mount St. Helens that had for decades been a favorite camping and fishing destination of local residents. At 8:32 a.m. Mount St. Helens turned ugly, unleashing a mind-boggling landslide that left a huge crater where the peak had been and a thick jumble of rock with an average thickness of 150-feet (45.7&nbsp;m) filling the lush valley that once led to much-beloved Spirit Lake.</span></p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Volcanic tourist destinations","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Springer","doi":"10.1007/978-3-642-16191-9_15","usgsCitation":"Newhall, C., Frenzen, P., and Driedger, C.L., 2014, Mount St. Helens, Washington, USA, chap. <i>of</i> Volcanic tourist destinations, p. 201-208, https://doi.org/10.1007/978-3-642-16191-9_15.","productDescription":"8 p.","startPage":"201","endPage":"208","ipdsId":"IP-041629","costCenters":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"links":[{"id":463536,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Washington","otherGeospatial":"Mount St. Helens","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -122.3543690100102,\n              46.32788682070907\n            ],\n            [\n              -122.3543690100102,\n              46.089206778543655\n            ],\n            [\n              -122.03438903007604,\n              46.089206778543655\n            ],\n            [\n              -122.03438903007604,\n              46.32788682070907\n            ],\n            [\n              -122.3543690100102,\n              46.32788682070907\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationDate":"2014-08-10","publicationStatus":"PW","contributors":{"editors":[{"text":"Erfurt-Cooper, Patricia","contributorId":345852,"corporation":false,"usgs":false,"family":"Erfurt-Cooper","given":"Patricia","email":"","affiliations":[],"preferred":false,"id":917702,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Newhall, Chris","contributorId":9417,"corporation":false,"usgs":true,"family":"Newhall","given":"Chris","affiliations":[],"preferred":false,"id":917561,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Frenzen, Peter","contributorId":36255,"corporation":false,"usgs":true,"family":"Frenzen","given":"Peter","affiliations":[],"preferred":false,"id":917562,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mastin, Carolyn L. 0000-0002-4011-4112","orcid":"https://orcid.org/0000-0002-4011-4112","contributorId":204744,"corporation":false,"usgs":true,"family":"Mastin","given":"Carolyn","middleInitial":"L.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":917560,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70111780,"text":"70111780 - 2014 - Corridor- and stopover-use of the Hawaiian goose (<i>Branta sandvicensis</i>), an intratropical altitudinal migrant","interactions":[],"lastModifiedDate":"2014-06-09T09:21:22","indexId":"70111780","displayToPublicDate":"2014-01-01T09:18:00","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2487,"text":"Journal of Tropical Ecology","active":true,"publicationSubtype":{"id":10}},"title":"Corridor- and stopover-use of the Hawaiian goose (<i>Branta sandvicensis</i>), an intratropical altitudinal migrant","docAbstract":"We outfitted six male Hawaiian geese, or nene (Branta sandvicensis), with 45-g solar-powered satellite transmitters and collected four location coordinates d<sup>−1</sup> from 2010 to 2012. We used 6193 coordinates to characterize migration corridors, habitat preferences and temporal patterns of displacement for 16 migration events with Brownian bridge utilization distributions (BBUD). We used 1552 coordinates to characterize stopovers from 37 shorter-distance movement events with 25% BBUDs. Two subpopulations used a well-defined common migration corridor spanning a broad gradient of elevation. Use of native-dominated subalpine shrubland was 2.81 times more likely than the availability of this land-cover type. The nene differed from other tropical and temperate-zone migrant birds in that: (1) migration distance and the number of stopovers were unrelated (Mann–Whitney test W = 241, P < 0.006), and; (2) individual movements were not unidirectional suggesting that social interactions may be more important than refuelling en route; but like other species, nene made more direct migrations with fewer stopovers in return to breeding areas (0.58 ± 0.50) than in migration away from breeding areas (1.64 ± 0.48). Our findings, combined with the direction and timing of migration, which is opposite that of most other intratropical migrants, suggest fundamentally different drivers of altitudinal migration.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Tropical Ecology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Cambridge University Press","doi":"10.1017/S0266467413000783","usgsCitation":"Leopold, C.R., and Hess, S., 2014, Corridor- and stopover-use of the Hawaiian goose (<i>Branta sandvicensis</i>), an intratropical altitudinal migrant: Journal of Tropical Ecology, v. 30, no. 1, p. 67-78, https://doi.org/10.1017/S0266467413000783.","productDescription":"12 p.","startPage":"67","endPage":"78","numberOfPages":"12","ipdsId":"IP-052393","costCenters":[{"id":521,"text":"Pacific Island Ecosystems Research Center","active":false,"usgs":true}],"links":[{"id":288169,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":288164,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1017/S0266467413000783"}],"volume":"30","issue":"1","noUsgsAuthors":false,"publicationDate":"2013-12-13","publicationStatus":"PW","scienceBaseUri":"5396d765e4b0f7580bc0a8e5","contributors":{"authors":[{"text":"Leopold, Christina R.","contributorId":46817,"corporation":false,"usgs":true,"family":"Leopold","given":"Christina","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":494470,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hess, Steven C.","contributorId":74462,"corporation":false,"usgs":true,"family":"Hess","given":"Steven C.","affiliations":[],"preferred":false,"id":494471,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70198625,"text":"70198625 - 2014 - Decision making, risk, and uncertainty","interactions":[],"lastModifiedDate":"2018-08-13T10:28:23","indexId":"70198625","displayToPublicDate":"2014-01-01T09:03:23","publicationYear":"2014","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"chapter":"4","title":"Decision making, risk, and uncertainty","docAbstract":"<p>No abstract available.&nbsp;</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Sampling and monitoring for the mine life cycle: Management technologies for metal mining influenced water","language":"English","publisher":"Society for Mining, Metallurgy, and Exploration ","usgsCitation":"Russell, C.C., Smith, K.S., and McLemore, V.T., 2014, Decision making, risk, and uncertainty, chap. 4 <i>of</i> Sampling and monitoring for the mine life cycle: Management technologies for metal mining influenced water.","costCenters":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":356402,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5b98ab98e4b0702d0e843149","contributors":{"editors":[{"text":"McLemore, Virginia T.","contributorId":113338,"corporation":false,"usgs":true,"family":"McLemore","given":"Virginia","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":742221,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Smith, Kathleen S. 0000-0001-8547-9804 ksmith@usgs.gov","orcid":"https://orcid.org/0000-0001-8547-9804","contributorId":182,"corporation":false,"usgs":true,"family":"Smith","given":"Kathleen","email":"ksmith@usgs.gov","middleInitial":"S.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":742222,"contributorType":{"id":2,"text":"Editors"},"rank":2},{"text":"Russell, Carol C.","contributorId":140998,"corporation":false,"usgs":false,"family":"Russell","given":"Carol","email":"","middleInitial":"C.","affiliations":[{"id":6914,"text":"U.S. Environmental Protection Agency","active":true,"usgs":false}],"preferred":false,"id":742223,"contributorType":{"id":2,"text":"Editors"},"rank":3}],"authors":[{"text":"Russell, Carol C.","contributorId":140998,"corporation":false,"usgs":false,"family":"Russell","given":"Carol","email":"","middleInitial":"C.","affiliations":[{"id":6914,"text":"U.S. Environmental Protection Agency","active":true,"usgs":false}],"preferred":false,"id":742218,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smith, Kathleen S. 0000-0001-8547-9804 ksmith@usgs.gov","orcid":"https://orcid.org/0000-0001-8547-9804","contributorId":182,"corporation":false,"usgs":true,"family":"Smith","given":"Kathleen","email":"ksmith@usgs.gov","middleInitial":"S.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":742219,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McLemore, Virginia T.","contributorId":113338,"corporation":false,"usgs":true,"family":"McLemore","given":"Virginia","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":742220,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70137895,"text":"70137895 - 2014 - Sylphella puccoon gen. n., sp. n. and two additional new species of aquatic oligochaetes (Lumbriculidae, Clitellata) from poorly-known lotic habitats in North Carolina (USA)","interactions":[],"lastModifiedDate":"2015-01-14T08:47:20","indexId":"70137895","displayToPublicDate":"2014-01-01T09:00:00","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3808,"text":"ZooKeys","active":true,"publicationSubtype":{"id":10}},"title":"Sylphella puccoon gen. n., sp. n. and two additional new species of aquatic oligochaetes (Lumbriculidae, Clitellata) from poorly-known lotic habitats in North Carolina (USA)","docAbstract":"<p>Three new species of <i>Lumbriculidae</i> were collected from floodplain seeps and small streams in southeastern North America. Some of these habitats are naturally acidic. <i>Sylphella puccoon</i> <strong>gen. n., sp. n.</strong> has prosoporous male ducts in X-XI, and spermathecae in XII-XIII. Muscular, spherical atrial ampullae and acuminate penial sheaths distinguish this monotypic new genus from other lumbriculid genera having similar arrangements of reproductive organs. <i>Cookidrilus pocosinus</i> <strong>sp. n.</strong> resembles its two subterranean, Palearctic congeners in the arrangement of reproductive organs, but is easily distinguished by the position of the spermathecal pores in front of the chaetae in X-XIII. <i>Stylodrilus coreyi</i> <strong>sp. n.</strong> differs from congeners having simple-pointed chaetae and elongate atria primarily by the structure of the male duct and the large clusters of prostate cells. Streams and wetlands of Southeastern USA have a remarkably high diversity of endemic lumbriculids, and these poorly-known invertebrates should be considered in conservation efforts.</p>","language":"English","publisher":"Pensoft Publishers","publisherLocation":"Sofia, Bulgaria","doi":"10.3897/zookeys.451.7304","collaboration":"Pilar Rodriguez, Universidad del Pais Vasco, Spain; David R Lenat, North Carolina Dept. Environment and Natural Resources","usgsCitation":"Rodriguez, P., Fend, S.V., and Lenat, D.R., 2014, Sylphella puccoon gen. n., sp. n. and two additional new species of aquatic oligochaetes (Lumbriculidae, Clitellata) from poorly-known lotic habitats in North Carolina (USA): ZooKeys, v. 451, p. 1-32, https://doi.org/10.3897/zookeys.451.7304.","productDescription":"32 p.","startPage":"1","endPage":"32","numberOfPages":"32","onlineOnly":"Y","additionalOnlineFiles":"N","ipdsId":"IP-058224","costCenters":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"links":[{"id":473270,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.3897/zookeys.451.7304","text":"Publisher Index Page"},{"id":297207,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":297206,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4258618/"}],"country":"United States","state":"North Carolina","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -81.80419921875,\n              36.65079252503471\n            ],\n            [\n              -82.705078125,\n              36.1733569352216\n            ],\n            [\n              -82.72705078125,\n              35.496456056584165\n            ],\n            [\n              -82.46337890625,\n              35.11990857099681\n            ],\n            [\n              -81.18896484375,\n              34.939985151560435\n            ],\n            [\n              -80.88134765625,\n              34.687427949314845\n            ],\n            [\n              -79.8046875,\n              34.66935854524543\n            ],\n            [\n              -78.55224609374999,\n              33.76088200086917\n            ],\n            [\n              -76.0693359375,\n              34.77771580360469\n            ],\n            [\n              -75.322265625,\n              35.28150065789119\n            ],\n            [\n              -75.30029296875,\n              35.817813158696616\n            ],\n            [\n              -75.7177734375,\n              36.61552763134925\n            ],\n            [\n              -81.80419921875,\n              36.65079252503471\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"451","publishingServiceCenter":{"id":14,"text":"Menlo Park PSC"},"noUsgsAuthors":false,"publicationDate":"2014-11-03","publicationStatus":"PW","scienceBaseUri":"54dd2c67e4b08de9379b3798","contributors":{"authors":[{"text":"Rodriguez, Pilar","contributorId":91002,"corporation":false,"usgs":true,"family":"Rodriguez","given":"Pilar","email":"","affiliations":[],"preferred":false,"id":538283,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fend, Steven V. 0000-0002-4638-6602 svfend@usgs.gov","orcid":"https://orcid.org/0000-0002-4638-6602","contributorId":3591,"corporation":false,"usgs":true,"family":"Fend","given":"Steven","email":"svfend@usgs.gov","middleInitial":"V.","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":538282,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lenat, David R.","contributorId":23500,"corporation":false,"usgs":true,"family":"Lenat","given":"David","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":538284,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
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