{"pageNumber":"975","pageRowStart":"24350","pageSize":"25","recordCount":184660,"records":[{"id":70188852,"text":"70188852 - 2017 - Tolerance to disturbance regulated by attractiveness of resources: A case study of desert bighorn sheep within the River Mountains, Nevada","interactions":[],"lastModifiedDate":"2017-06-26T14:33:28","indexId":"70188852","displayToPublicDate":"2017-06-26T00:00:00","publicationYear":"2017","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3746,"text":"Western North American Naturalist","onlineIssn":"1944-8341","printIssn":"1527-0904","active":true,"publicationSubtype":{"id":10}},"title":"Tolerance to disturbance regulated by attractiveness of resources: A case study of desert bighorn sheep within the River Mountains, Nevada","docAbstract":"<p><span>Human activity may mimic predation risks for wildlife by causing abandonment of foraging sites and increasing expenditure of energy. Animals that can tolerate nonlethal disturbance may minimize these fitness costs. We examine this aspect of the risk—disturbance hypothesis by first analyzing recent habitat use of desert bighorn sheep relative to areas of attraction and disturbance. We then compare and contrast sheep responses to differing levels of anthropogenic disturbance between 2 time periods, 30 years apart. Desert bighorn sheep were tolerant of suburban activity when a consistent forage resource (municipal grass) was provided. Males were more tolerant than females, and females returned to natural, steep areas during the birthing season. Increased recreation activity, specifically mountain bike use, may have resulted in avoidance by sheep of otherwise suitable habitat that had been occupied decades earlier, thereby reducing availability of limited habitat. Tolerance increased only when attractiveness was relatively high and decreased as perceived fitness decreased, supporting risk—disturbance theory.</span></p>","language":"English","publisher":"Monte L. Bean Life Science Museum","doi":"10.3398/064.077.0109","usgsCitation":"Lowrey, C.E., and Longshore, K.M., 2017, Tolerance to disturbance regulated by attractiveness of resources: A case study of desert bighorn sheep within the River Mountains, Nevada: Western North American Naturalist, v. 77, no. 1, p. 82-98, https://doi.org/10.3398/064.077.0109.","productDescription":"17 p.","startPage":"82","endPage":"98","ipdsId":"IP-081658","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":488682,"rank":0,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://scholarsarchive.byu.edu/wnan/vol77/iss1/8","text":"External Repository"},{"id":342909,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Nevada","otherGeospatial":"River Mountains","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -114.96849060058592,\n              35.88960636579773\n            ],\n            [\n              -114.78034973144531,\n              35.88960636579773\n            ],\n            [\n              -114.78034973144531,\n              36.12678323326426\n            ],\n            [\n              -114.96849060058592,\n              36.12678323326426\n            ],\n            [\n              -114.96849060058592,\n              35.88960636579773\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"77","issue":"1","publishingServiceCenter":{"id":1,"text":"Sacramento PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"59521d1ce4b062508e3c3640","contributors":{"authors":[{"text":"Lowrey, Chris E. 0000-0001-5084-7275 clowrey@usgs.gov","orcid":"https://orcid.org/0000-0001-5084-7275","contributorId":3225,"corporation":false,"usgs":true,"family":"Lowrey","given":"Chris","email":"clowrey@usgs.gov","middleInitial":"E.","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":true,"id":700695,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Longshore, Kathleen M. 0000-0001-6621-1271 longshore@usgs.gov","orcid":"https://orcid.org/0000-0001-6621-1271","contributorId":2677,"corporation":false,"usgs":true,"family":"Longshore","given":"Kathleen","email":"longshore@usgs.gov","middleInitial":"M.","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":false,"id":700694,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70188808,"text":"70188808 - 2017 - Highlighting the complexities of a groundwater pilot study during an avian influenza outbreak: Methods, lessons learned, and select contaminant results","interactions":[],"lastModifiedDate":"2018-09-18T11:09:22","indexId":"70188808","displayToPublicDate":"2017-06-26T00:00:00","publicationYear":"2017","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1561,"text":"Environmental Research","active":true,"publicationSubtype":{"id":10}},"title":"Highlighting the complexities of a groundwater pilot study during an avian influenza outbreak: Methods, lessons learned, and select contaminant results","docAbstract":"<div class=\"abstract svAbstract \" data-etype=\"ab\"><p id=\"sp0055\">The highly pathogenic avian influenza (H5N2) outbreak in the Midwestern United States (US) in 2015 was historic due to the number of birds and poultry operations impacted and the corresponding economic loss to the poultry industry and was the largest animal health emergency in US history. The U.S. Geological Survey (USGS), with the assistance of several state and federal agencies, aided the response to the outbreak by developing a study to determine the extent of virus transport in the environment. The study goals were to: develop the appropriate sampling methods and protocols for measuring avian influenza virus (AIV) in groundwater, provide the first baseline data on AIV and outbreak- and poultry-related contaminant occurrence and movement into groundwater, and document climatological factors that may have affected both survival and transport of AIV to groundwater during the months of the 2015 outbreak. While site selection was expedient, there were often delays in sample response times due to both relationship building between agencies, groups, and producers and logistical time constraints. This study's design and sampling process highlights the unpredictable nature of disease outbreaks and the corresponding difficulty in environmental sampling of such events. The lessons learned, including field protocols and approaches, can be used to improve future research on AIV in the environment.</p></div>","language":"English","publisher":"Elsevier","doi":"10.1016/j.envres.2017.06.010","usgsCitation":"Hubbard, L.E., Kolpin, D.W., Fields, C.L., Hladik, M., and Iwanowicz, L.R., 2017, Highlighting the complexities of a groundwater pilot study during an avian influenza outbreak: Methods, lessons learned, and select contaminant results: Environmental Research, v. 158, p. 212-224, https://doi.org/10.1016/j.envres.2017.06.010.","productDescription":"13 p.","startPage":"212","endPage":"224","ipdsId":"IP-081580","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true},{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":469733,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1016/j.envres.2017.06.010","text":"Publisher Index 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Center","active":true,"usgs":true}],"preferred":true,"id":700454,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fields, Chad L.","contributorId":192692,"corporation":false,"usgs":false,"family":"Fields","given":"Chad","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":700455,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hladik, Michelle L. 0000-0002-0891-2712 mhladik@usgs.gov","orcid":"https://orcid.org/0000-0002-0891-2712","contributorId":189904,"corporation":false,"usgs":true,"family":"Hladik","given":"Michelle L.","email":"mhladik@usgs.gov","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":false,"id":700456,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Iwanowicz, Luke R. 0000-0002-1197-6178 liwanowicz@usgs.gov","orcid":"https://orcid.org/0000-0002-1197-6178","contributorId":190787,"corporation":false,"usgs":true,"family":"Iwanowicz","given":"Luke","email":"liwanowicz@usgs.gov","middleInitial":"R.","affiliations":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"preferred":true,"id":700457,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70188840,"text":"70188840 - 2017 - Use of electricity to sedate Lake Trout for intracoelomic implantation of electronic transmitters","interactions":[],"lastModifiedDate":"2017-06-26T12:12:54","indexId":"70188840","displayToPublicDate":"2017-06-26T00:00:00","publicationYear":"2017","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2886,"text":"North American Journal of Fisheries Management","active":true,"publicationSubtype":{"id":10}},"title":"Use of electricity to sedate Lake Trout for intracoelomic implantation of electronic transmitters","docAbstract":"<p><span>Use of telemetry data to inform fisheries conservation and management is becoming increasingly common; as such, fish typically must be sedated before surgical implantation of transmitters into the coelom. Given that no widely available, immediate-release chemical sedative currently exists in North America, we investigated the feasibility of using electricity to sedate Lake Trout </span><i>Salvelinus namaycush</i><span> long enough for an experienced surgeon to implant an electronic transmitter (i.e., 180 s). Specifically, our study objectives were to determine (1) whether some combination of electrical waveform characteristics (i.e., duty cycle, frequency, voltage, and pulse type) could sedate Lake Trout for at least 180 s; and (2) whether Lake Trout that were sequentially exposed to continuous DC and pulsed DC had greater rates of spinal injury and short-term mortality than control fish. A Portable Electrosedation System unit was used to sedate hatchery and wild Lake Trout. Dual-frequency pulsed-DC and two-stage approaches successfully sedated Lake Trout and had similar induction and recovery times. Lake Trout sedated using the two-stage approach did not have survival rates or spinal abnormalities that were significantly different from those of control fish. We concluded that electricity was a viable alternative to chemical sedatives for sedating Lake Trout before surgical implantation of an electronic transmitter, but we suggest that Lake Trout and other closely related species (e.g., Arctic Char </span><i>Salvelinus alpinus</i><span>) may require morphotype-specific electrical waveforms due to their morphological diversity.</span></p>","language":"English","publisher":"Taylor and Francis","doi":"10.1080/02755947.2017.1324544","usgsCitation":"Faust, M.D., Vandergoot, C., Hostnik, E.T., Binder, T., Mida Hinderer, J.L., Ives, J.T., and Krueger, C., 2017, Use of electricity to sedate Lake Trout for intracoelomic implantation of electronic transmitters: North American Journal of Fisheries Management, v. 37, no. 4, p. 768-777, https://doi.org/10.1080/02755947.2017.1324544.","productDescription":"10 p.","startPage":"768","endPage":"777","ipdsId":"IP-083769","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":469732,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1080/02755947.2017.1324544","text":"Publisher Index Page"},{"id":342877,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"37","issue":"4","publishingServiceCenter":{"id":6,"text":"Columbus PSC"},"noUsgsAuthors":false,"publicationDate":"2017-05-01","publicationStatus":"PW","scienceBaseUri":"59521d1de4b062508e3c3644","contributors":{"authors":[{"text":"Faust, Matthew D.","contributorId":145776,"corporation":false,"usgs":false,"family":"Faust","given":"Matthew","email":"","middleInitial":"D.","affiliations":[{"id":16232,"text":"Ohio Department of Natural Resources","active":true,"usgs":false}],"preferred":false,"id":700593,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Vandergoot, Christopher 0000-0003-4128-3329 cvandergoot@usgs.gov","orcid":"https://orcid.org/0000-0003-4128-3329","contributorId":178356,"corporation":false,"usgs":true,"family":"Vandergoot","given":"Christopher","email":"cvandergoot@usgs.gov","affiliations":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"preferred":true,"id":700592,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hostnik, Eric T.","contributorId":193488,"corporation":false,"usgs":false,"family":"Hostnik","given":"Eric","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":700594,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Binder, Thomas R.","contributorId":21093,"corporation":false,"usgs":true,"family":"Binder","given":"Thomas R.","affiliations":[],"preferred":false,"id":700595,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Mida Hinderer, Julia L.","contributorId":193489,"corporation":false,"usgs":false,"family":"Mida Hinderer","given":"Julia","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":700596,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Ives, Jessica T.","contributorId":193490,"corporation":false,"usgs":false,"family":"Ives","given":"Jessica","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":700597,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Krueger, Charles C.","contributorId":67821,"corporation":false,"usgs":false,"family":"Krueger","given":"Charles C.","affiliations":[{"id":7019,"text":"Great Lakes Fishery Commission","active":true,"usgs":false}],"preferred":false,"id":700598,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70188721,"text":"ofr20171080 - 2017 - Spatial and temporal distribution of bull trout (<em>Salvelinus confluentus</em>)-size fish near the floating surface collector in the North Fork Reservoir, Oregon, 2016","interactions":[],"lastModifiedDate":"2017-06-27T09:00:11","indexId":"ofr20171080","displayToPublicDate":"2017-06-26T00:00:00","publicationYear":"2017","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2017-1080","displayTitle":"Spatial and temporal distribution of bull trout (<em>Salvelinus confluentus</em>)-size fish near the floating surface collector in the North Fork Reservoir, Oregon, 2016","title":"Spatial and temporal distribution of bull trout (<em>Salvelinus confluentus</em>)-size fish near the floating surface collector in the North Fork Reservoir, Oregon, 2016","docAbstract":"<p class=\"p1\">Acoustic cameras were used to assess the behavior and abundance of bull trout (<i>Salvelinus confluentus</i>)-size fish at the entrance to the North Fork Reservoir juvenile fish floating surface collector (FSC). The purpose of the FSC is to collect downriver migrating juvenile salmonids at the North Fork Dam, and safely route them around the hydroelectric projects. The objective of the acoustic camera component of this study was to assess the behaviors of bull trout-size fish observed near the FSC, and to determine if the presence of bull trout-size fish influenced the collection or abundance of juvenile salmonids. Acoustic cameras were deployed near the surface and floor of the entrance to the FSC. The acoustic camera technology was an informative tool for assessing abundance and spatial and temporal behaviors of bull trout-size fish near the entrance of the FSC. Bull trout-size fish were regularly observed near the entrance, with greater abundances on the deep camera than on the shallow camera. Additionally, greater abundances were observed during the hours of sunlight than were observed during the night. Behavioral differences also were observed at the two depths, with surface fish traveling faster and straighter with more directed movement, and fish observed on the deep camera generally showing more milling behavior. Modeling potential predator-prey interactions and influences using collected passive integrated transponder (PIT) -tagged juvenile salmonids proved largely unpredictable, although these fish provided relevant timing and collection information. Overall, the results indicate that bull trout-size fish are present near the entrance of the FSC, concomitant with juvenile salmonids, and their abundances and behaviors indicate that they may be drawn to the entrance of the FSC because of the abundance of prey-sized fish.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20171080","collaboration":"Prepared in cooperation with Portland General Electric","usgsCitation":"Adams, N.S., and Smith, C.D., 2017, Spatial and temporal distribution of bull trout (<em>Salvelinus confluentus</em>)-size fish near the floating surface collector in the North Fork Reservoir, Oregon, 2016: U.S. Geological Survey Open-File Report 2017-1080, 27 p., https://doi.org/10.3133/ofr20171080.","productDescription":"vi, 27 p.","onlineOnly":"Y","ipdsId":"IP-084992","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":342923,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2017/1080/coverthb.jpg"},{"id":342924,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2017/1080/ofr20171080.pdf","text":"Report","size":"4.6 MB","linkFileType":{"id":1,"text":"pdf"},"description":"OFR 2017-1080"}],"country":"United States","state":"Oregon","otherGeospatial":"North Fork Reservoir","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -122.29714393615721,\n              45.22104488768461\n            ],\n            [\n              -122.24092483520508,\n              45.22104488768461\n            ],\n            [\n              -122.24092483520508,\n              45.24969422012565\n            ],\n            [\n              -122.29714393615721,\n              45.24969422012565\n            ],\n            [\n              -122.29714393615721,\n              45.22104488768461\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","contact":"<p>Director, <a href=\"https://wfrc.usgs.gov/\" target=\"blank\" data-mce-href=\"https://wfrc.usgs.gov/\">Western Fisheries Research Center</a><br> U.S. Geological Survey<br> 6505 NE 65th Street<br> Seattle, Washington 98115</p>","tableOfContents":"<ul><li>Abstract<br></li><li>Introduction<br></li><li>Methods<br></li><li>Results<br></li><li>Discussion<br></li><li>Acknowledgments<br></li><li>References Cited<br></li></ul>","publishingServiceCenter":{"id":12,"text":"Tacoma PSC"},"publishedDate":"2017-06-26","noUsgsAuthors":false,"publicationDate":"2017-06-26","publicationStatus":"PW","scienceBaseUri":"59521d1ee4b062508e3c364d","contributors":{"authors":[{"text":"Adams, Noah S. 0000-0002-8354-0293 nadams@usgs.gov","orcid":"https://orcid.org/0000-0002-8354-0293","contributorId":3521,"corporation":false,"usgs":true,"family":"Adams","given":"Noah","email":"nadams@usgs.gov","middleInitial":"S.","affiliations":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"preferred":true,"id":699179,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smith, Collin D. 0000-0003-4184-5686 cdsmith@usgs.gov","orcid":"https://orcid.org/0000-0003-4184-5686","contributorId":7915,"corporation":false,"usgs":true,"family":"Smith","given":"Collin D.","email":"cdsmith@usgs.gov","affiliations":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"preferred":false,"id":699178,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70225827,"text":"70225827 - 2017 - What has been learned from pressure cores","interactions":[],"lastModifiedDate":"2021-11-10T14:59:17.774184","indexId":"70225827","displayToPublicDate":"2017-06-25T08:52:09","publicationYear":"2017","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"What has been learned from pressure cores","docAbstract":"<p><span>The advancement of pressure core acquisition and analysis technology in recent decades has enabled detailed imaging and direct measurement of naturally occurring hydrate-bearing sediments and has shed light onto hydrate habits, formation processes, fundamental physical properties, and hydrate deposit responses during gas production. This paper reviews the development and capabilities of the pressure core technology, discusses insights learned from hydrate-bearing pressure cores and inherent limitations of this technology, and concludes with suggestions for potential applications of pressure core technology for investigating hydrate deposits.</span></p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"9th International conference on gas hydrates, Denver Colorado, June 25-30, 2017","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"9th International Conference on Gas Hydrates","conferenceDate":"Jun 25-30, 2017","conferenceLocation":"Denver. CO","language":"English","publisher":"Colorado School of Mines","usgsCitation":"Dai, S., Boswell, R., Waite, W., Jang, J., Lee, J.Y., and Seol, Y., 2017, What has been learned from pressure cores, <i>in</i> 9th International conference on gas hydrates, Denver Colorado, June 25-30, 2017, Denver. CO, Jun 25-30, 2017, 17 p.","productDescription":"17 p.","ipdsId":"IP-084776","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":391574,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Dai, Sheng","contributorId":213194,"corporation":false,"usgs":false,"family":"Dai","given":"Sheng","email":"","affiliations":[{"id":38715,"text":"Georgia Institute of Technology, Atlanta, GA","active":true,"usgs":false}],"preferred":false,"id":826566,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Boswell, Ray","contributorId":242633,"corporation":false,"usgs":false,"family":"Boswell","given":"Ray","affiliations":[{"id":34152,"text":"US Department of Energy","active":true,"usgs":false}],"preferred":false,"id":826568,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Waite, William F. 0000-0002-9436-4109 wwaite@usgs.gov","orcid":"https://orcid.org/0000-0002-9436-4109","contributorId":625,"corporation":false,"usgs":true,"family":"Waite","given":"William F.","email":"wwaite@usgs.gov","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true},{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"preferred":true,"id":826569,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Jang, Junbong 0000-0001-5500-7558 jjang@usgs.gov","orcid":"https://orcid.org/0000-0001-5500-7558","contributorId":189400,"corporation":false,"usgs":true,"family":"Jang","given":"Junbong","email":"jjang@usgs.gov","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":826567,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Lee, J. Y.","contributorId":195962,"corporation":false,"usgs":false,"family":"Lee","given":"J.","email":"","middleInitial":"Y.","affiliations":[],"preferred":false,"id":826570,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Seol, Y","contributorId":189553,"corporation":false,"usgs":false,"family":"Seol","given":"Y","affiliations":[],"preferred":false,"id":826571,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70188796,"text":"70188796 - 2017 - Sylvatic plague vaccine partially protects prairie dogs (Cynomys spp.) in field trials","interactions":[],"lastModifiedDate":"2023-06-21T15:02:41.535426","indexId":"70188796","displayToPublicDate":"2017-06-24T00:00:00","publicationYear":"2017","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1443,"text":"EcoHealth","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Sylvatic plague vaccine partially protects prairie dogs (<i>Cynomys</i> spp.) in field trials","title":"Sylvatic plague vaccine partially protects prairie dogs (Cynomys spp.) in field trials","docAbstract":"<p><span>Sylvatic plague, caused by </span><i class=\"EmphasisTypeItalic \">Yersinia pestis</i><span>, frequently afflicts prairie dogs (</span><i class=\"EmphasisTypeItalic \">Cynomys</i><span> spp.), causing population declines and local extirpations. We tested the effectiveness of bait-delivered sylvatic plague vaccine (SPV) in prairie dog colonies on 29 paired placebo and treatment plots (1–59&nbsp;ha in size; average 16.9&nbsp;ha) in 7 western states from 2013 to 2015. We compared relative abundance (using catch per unit effort (CPUE) as an index) and apparent survival of prairie dogs on 26 of the 29 paired plots, 12 with confirmed or suspected plague (</span><i class=\"EmphasisTypeItalic \">Y. pestis</i><span> positive carcasses or fleas). Even though plague mortality occurred in prairie dogs on vaccine plots, SPV treatment had an overall positive effect on CPUE in all three years, regardless of plague status. Odds of capturing a unique animal were 1.10 (95% confidence interval [C.I.] 1.02–1.19) times higher per trap day on vaccine-treated plots than placebo plots in 2013, 1.47 (95% C.I. 1.41–1.52) times higher in 2014 and 1.19 (95% C.I. 1.13–1.25) times higher in 2015. On pairs where plague occurred, odds of apparent survival were 1.76 (95% Bayesian credible interval [B.C.I.] 1.28–2.43) times higher on vaccine plots than placebo plots for adults and 2.41 (95% B.C.I. 1.72–3.38) times higher for juveniles. Our results provide evidence that consumption of vaccine-laden baits can protect prairie dogs against plague; however, further evaluation and refinement are needed to optimize SPV use as a management tool.</span></p>","language":"English","publisher":"Springer","doi":"10.1007/s10393-017-1253-x","usgsCitation":"Rocke, T.E., Tripp, D.W., Russell, R.E., Abbott, R.C., Richgels, K., Matchett, M.R., Biggins, D.E., Griebel, R., Schroeder, G., Grassel, S.M., Pipkin, D.R., Cordova, J., Kavalunas, A., Maxfield, B., Boulerice, J.T., and Miller, M.W., 2017, Sylvatic plague vaccine partially protects prairie dogs (Cynomys spp.) in field trials: EcoHealth, v. 14, no. 3, p. 438-450, https://doi.org/10.1007/s10393-017-1253-x.","productDescription":"13 p.; Data Release","startPage":"438","endPage":"450","ipdsId":"IP-080843","costCenters":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"links":[{"id":469736,"rank":4,"type":{"id":40,"text":"Open Access Publisher Index 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,{"id":70189646,"text":"70189646 - 2017 - Evidence of fuels management and fire weather influencing fire severity in an extreme fire event","interactions":[],"lastModifiedDate":"2017-10-02T12:53:15","indexId":"70189646","displayToPublicDate":"2017-06-23T00:00:00","publicationYear":"2017","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1450,"text":"Ecological Applications","active":true,"publicationSubtype":{"id":10}},"title":"Evidence of fuels management and fire weather influencing fire severity in an extreme fire event","docAbstract":"Following changes in vegetation structure and pattern, along with a changing climate, large wildfire incidence has increased in forests throughout the western U.S. Given this increase there is great interest in whether fuels treatments and previous wildfire can alter fire severity patterns in large wildfires. We assessed the relative influence of previous fuels treatments (including wildfire), fire weather, vegetation and water balance on fire severity in the Rim Fire of 2013. We did this at three different spatial scales to investigate whether the influences on fire severity changed across scales. Both fuels treatments and previous low to moderate severity wildfire reduced the prevalence of high severity fire. In general, areas without recent fuels treatments and areas that previously burned at high severity tended to have a greater proportion of high severity fire in the Rim Fire. Areas treated with prescribed fire, especially when combined with thinning, had the lowest proportions of high severity. Proportion of the landscape burned at high severity was most strongly influenced by fire weather and proportional area previously treated for fuels or burned by low to moderate severity wildfire. The proportion treated needed to effectively reduce the amount of high fire severity fire varied by spatial scale of analysis, with smaller spatial scales requiring a greater proportion treated to see an effect on fire severity. When moderate and high severity fire encountered a previously treated area, fire severity was significantly reduced in the treated area relative to the adjacent untreated area. Our results show that fuels treatments and low to moderate severity wildfire can reduce fire severity in a subsequent wildfire, even when burning under fire growth conditions. These results serve as further evidence that both fuels treatments and lower severity wildfire can increase forest resilience.","language":"English","publisher":"Ecological Society of America","doi":"10.1002/eap.1586","usgsCitation":"Lydersen, J., Collins, B.M., Brooks, M.L., Matchett, J.R., Shive, K.L., Povak, N.A., Kane, V.R., and Smith, D., 2017, Evidence of fuels management and fire weather influencing fire severity in an extreme fire event: Ecological Applications, v. 27, no. 7, p. 2013-2030, https://doi.org/10.1002/eap.1586.","productDescription":"18 p.","startPage":"2013","endPage":"2030","ipdsId":"IP-084221","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":344045,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Stanislaus National Forest, Yosemite National Park ","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -120.319948,37.550566 ], [ -120.319948,38.250044 ], [ -119.629869,38.250044 ], [ -119.629869,37.550566 ], [ -120.319948,37.550566 ] ] ] } } ] }","volume":"27","issue":"7","publishingServiceCenter":{"id":1,"text":"Sacramento PSC"},"noUsgsAuthors":false,"publicationDate":"2017-08-17","publicationStatus":"PW","scienceBaseUri":"59706fb5e4b0d1f9f065a882","contributors":{"authors":[{"text":"Lydersen, Jamie M","contributorId":194876,"corporation":false,"usgs":false,"family":"Lydersen","given":"Jamie M","affiliations":[],"preferred":false,"id":705565,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Collins, Brandon M.","contributorId":127850,"corporation":false,"usgs":false,"family":"Collins","given":"Brandon","email":"","middleInitial":"M.","affiliations":[{"id":7169,"text":"USDA Forest Service, UC Berkeley","active":true,"usgs":false}],"preferred":false,"id":705566,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brooks, Matthew L. 0000-0002-3518-6787 mlbrooks@usgs.gov","orcid":"https://orcid.org/0000-0002-3518-6787","contributorId":393,"corporation":false,"usgs":true,"family":"Brooks","given":"Matthew","email":"mlbrooks@usgs.gov","middleInitial":"L.","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":true,"id":705564,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Matchett, John R. 0000-0002-2905-6468 jmatchett@usgs.gov","orcid":"https://orcid.org/0000-0002-2905-6468","contributorId":1669,"corporation":false,"usgs":true,"family":"Matchett","given":"John","email":"jmatchett@usgs.gov","middleInitial":"R.","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":true,"id":705567,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Shive, Kristen L.","contributorId":194877,"corporation":false,"usgs":false,"family":"Shive","given":"Kristen","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":705568,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Povak, Nicholas A.","contributorId":194878,"corporation":false,"usgs":false,"family":"Povak","given":"Nicholas","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":705569,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Kane, Van R.","contributorId":194879,"corporation":false,"usgs":false,"family":"Kane","given":"Van","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":705570,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Smith, Douglas F.","contributorId":181753,"corporation":false,"usgs":false,"family":"Smith","given":"Douglas F.","affiliations":[],"preferred":false,"id":705571,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":70188710,"text":"sir20175022 - 2017 - Field-trip guides to selected volcanoes and volcanic landscapes of the western United States","interactions":[{"subject":{"id":70185497,"text":"sir20175022B - 2017 - Field-trip guide to subaqueous volcaniclastic facies in the Ancestral Cascades arc in southern Washington State—The Ohanapecosh Formation and Wildcat Creek beds","indexId":"sir20175022B","publicationYear":"2017","noYear":false,"chapter":"B","title":"Field-trip guide to subaqueous volcaniclastic facies in the Ancestral Cascades arc in southern Washington State—The Ohanapecosh Formation and Wildcat Creek beds"},"predicate":"IS_PART_OF","object":{"id":70188710,"text":"sir20175022 - 2017 - Field-trip guides to selected volcanoes and volcanic landscapes of the western United States","indexId":"sir20175022","publicationYear":"2017","noYear":false,"title":"Field-trip guides to selected volcanoes and volcanic landscapes of the western United States"},"id":1},{"subject":{"id":70185506,"text":"sir20175022G - 2017 - Field-trip guide to Mount Hood, Oregon, highlighting eruptive history and hazards","indexId":"sir20175022G","publicationYear":"2017","noYear":false,"chapter":"G","title":"Field-trip guide to Mount Hood, Oregon, highlighting eruptive history and hazards"},"predicate":"IS_PART_OF","object":{"id":70188710,"text":"sir20175022 - 2017 - Field-trip guides to selected volcanoes and volcanic landscapes of the western United States","indexId":"sir20175022","publicationYear":"2017","noYear":false,"title":"Field-trip guides to selected volcanoes and volcanic landscapes of the western United States"},"id":2},{"subject":{"id":70187070,"text":"sir20175022N - 2017 - Field-trip guide to the vents, dikes, stratigraphy, and structure of the Columbia River Basalt Group, eastern Oregon and southeastern Washington","indexId":"sir20175022N","publicationYear":"2017","noYear":false,"chapter":"N","title":"Field-trip guide to the vents, dikes, stratigraphy, and structure of the Columbia River Basalt Group, eastern Oregon and southeastern Washington"},"predicate":"IS_PART_OF","object":{"id":70188710,"text":"sir20175022 - 2017 - Field-trip guides to selected volcanoes and volcanic landscapes of the western United States","indexId":"sir20175022","publicationYear":"2017","noYear":false,"title":"Field-trip guides to selected volcanoes and volcanic landscapes of the western United States"},"id":3},{"subject":{"id":70187106,"text":"sir20175022L - 2017 - Geologic field-trip guide to Long Valley Caldera, California","indexId":"sir20175022L","publicationYear":"2017","noYear":false,"chapter":"L","title":"Geologic field-trip guide to Long Valley Caldera, California"},"predicate":"IS_PART_OF","object":{"id":70188710,"text":"sir20175022 - 2017 - Field-trip guides to selected volcanoes and volcanic landscapes of the western United States","indexId":"sir20175022","publicationYear":"2017","noYear":false,"title":"Field-trip guides to selected volcanoes and volcanic landscapes of the western United States"},"id":4},{"subject":{"id":70188427,"text":"sir20175022I - 2017 - Emplacement of Holocene silicic lava flows and domes at Newberry, South Sister, and Medicine Lake volcanoes, California and Oregon","indexId":"sir20175022I","publicationYear":"2017","noYear":false,"chapter":"I","title":"Emplacement of Holocene silicic lava flows and domes at Newberry, South Sister, and Medicine Lake volcanoes, California and Oregon"},"predicate":"IS_PART_OF","object":{"id":70188710,"text":"sir20175022 - 2017 - Field-trip guides to selected volcanoes and volcanic landscapes of the western United States","indexId":"sir20175022","publicationYear":"2017","noYear":false,"title":"Field-trip guides to selected volcanoes and volcanic landscapes of the western United States"},"id":5},{"subject":{"id":70188626,"text":"sir20175022K - 2017 - Overview for geologic field-trip guides to volcanoes of the Cascades Arc in northern California","indexId":"sir20175022K","publicationYear":"2017","noYear":false,"chapter":"K","title":"Overview for geologic field-trip guides to volcanoes of the Cascades Arc in northern California"},"predicate":"IS_PART_OF","object":{"id":70188710,"text":"sir20175022 - 2017 - Field-trip guides to selected volcanoes and volcanic landscapes of the western United States","indexId":"sir20175022","publicationYear":"2017","noYear":false,"title":"Field-trip guides to selected volcanoes and volcanic landscapes of the western United States"},"id":6},{"subject":{"id":70188646,"text":"sir20175022D - 2017 - Field-trip guide to Mount St. Helens, Washington - An overview of the eruptive history and petrology, tephra deposits, 1980 pyroclastic density current deposits, and the crater","indexId":"sir20175022D","publicationYear":"2017","noYear":false,"chapter":"D","title":"Field-trip guide to Mount St. Helens, Washington - An overview of the eruptive history and petrology, tephra deposits, 1980 pyroclastic density current deposits, and the crater"},"predicate":"IS_PART_OF","object":{"id":70188710,"text":"sir20175022 - 2017 - Field-trip guides to selected volcanoes and volcanic landscapes of the western United States","indexId":"sir20175022","publicationYear":"2017","noYear":false,"title":"Field-trip guides to selected volcanoes and volcanic landscapes of the western United States"},"id":7},{"subject":{"id":70188705,"text":"sir20175022J1 - 2017 - Geologic field trip guide to Mount Mazama and Crater Lake Caldera, Oregon","indexId":"sir20175022J1","publicationYear":"2017","noYear":false,"chapter":"J1","title":"Geologic field trip guide to Mount Mazama and Crater Lake Caldera, Oregon"},"predicate":"IS_PART_OF","object":{"id":70188710,"text":"sir20175022 - 2017 - Field-trip guides to selected volcanoes and volcanic landscapes of the western United States","indexId":"sir20175022","publicationYear":"2017","noYear":false,"title":"Field-trip guides to selected volcanoes and volcanic landscapes of the western United States"},"id":8},{"subject":{"id":70189018,"text":"sir20175022C - 2017 - Field-trip guide for exploring pyroclastic density current deposits from the May 18, 1980, eruption of Mount St. Helens, Washington","indexId":"sir20175022C","publicationYear":"2017","noYear":false,"chapter":"C","title":"Field-trip guide for exploring pyroclastic density current deposits from the May 18, 1980, eruption of Mount St. Helens, Washington"},"predicate":"IS_PART_OF","object":{"id":70188710,"text":"sir20175022 - 2017 - Field-trip guides to selected volcanoes and volcanic landscapes of the western United States","indexId":"sir20175022","publicationYear":"2017","noYear":false,"title":"Field-trip guides to selected volcanoes and volcanic landscapes of the western United States"},"id":9},{"subject":{"id":70189262,"text":"sir20175022H - 2017 - Field-trip guide to mafic volcanism of the Cascade Range in Central Oregon—A volcanic, tectonic, hydrologic, and geomorphic journey","indexId":"sir20175022H","publicationYear":"2017","noYear":false,"chapter":"H","title":"Field-trip guide to mafic volcanism of the Cascade Range in Central Oregon—A volcanic, tectonic, hydrologic, and geomorphic journey"},"predicate":"IS_PART_OF","object":{"id":70188710,"text":"sir20175022 - 2017 - Field-trip guides to selected volcanoes and volcanic landscapes of the western United States","indexId":"sir20175022","publicationYear":"2017","noYear":false,"title":"Field-trip guides to selected volcanoes and volcanic landscapes of the western United States"},"id":10},{"subject":{"id":70189425,"text":"sir20175022O - 2017 - Field-trip guide to Columbia River flood basalts, associated rhyolites, and diverse post-plume volcanism in eastern Oregon","indexId":"sir20175022O","publicationYear":"2017","noYear":false,"chapter":"O","title":"Field-trip guide to Columbia River flood basalts, associated rhyolites, and diverse post-plume volcanism in eastern Oregon"},"predicate":"IS_PART_OF","object":{"id":70188710,"text":"sir20175022 - 2017 - Field-trip guides to selected volcanoes and volcanic landscapes of the western United States","indexId":"sir20175022","publicationYear":"2017","noYear":false,"title":"Field-trip guides to selected volcanoes and volcanic landscapes of the western United States"},"id":11},{"subject":{"id":70189426,"text":"sir20175022M - 2017 - Field-trip guide to a volcanic transect of the Pacific Northwest","indexId":"sir20175022M","publicationYear":"2017","noYear":false,"chapter":"M","title":"Field-trip guide to a volcanic transect of the Pacific Northwest"},"predicate":"IS_PART_OF","object":{"id":70188710,"text":"sir20175022 - 2017 - Field-trip guides to selected volcanoes and volcanic landscapes of the western United States","indexId":"sir20175022","publicationYear":"2017","noYear":false,"title":"Field-trip guides to selected volcanoes and volcanic landscapes of the western United States"},"id":12},{"subject":{"id":70189725,"text":"sir20175022J2 - 2017 - Field-trip guide to the geologic highlights of Newberry Volcano, Oregon","indexId":"sir20175022J2","publicationYear":"2017","noYear":false,"chapter":"J2","title":"Field-trip guide to the geologic highlights of Newberry Volcano, Oregon"},"predicate":"IS_PART_OF","object":{"id":70188710,"text":"sir20175022 - 2017 - Field-trip guides to selected volcanoes and volcanic landscapes of the western United States","indexId":"sir20175022","publicationYear":"2017","noYear":false,"title":"Field-trip guides to selected volcanoes and volcanic landscapes of the western United States"},"id":13},{"subject":{"id":70189797,"text":"sir20175022J - 2017 - Overview for geologic field-trip guides to Mount Mazama, Crater Lake Caldera, and Newberry Volcano, Oregon","indexId":"sir20175022J","publicationYear":"2017","noYear":false,"chapter":"J","title":"Overview for geologic field-trip guides to Mount Mazama, Crater Lake Caldera, and Newberry Volcano, Oregon"},"predicate":"IS_PART_OF","object":{"id":70188710,"text":"sir20175022 - 2017 - Field-trip guides to selected volcanoes and volcanic landscapes of the western United States","indexId":"sir20175022","publicationYear":"2017","noYear":false,"title":"Field-trip guides to selected volcanoes and volcanic landscapes of the western United States"},"id":14},{"subject":{"id":70189877,"text":"sir20175022K1 - 2017 - Geologic field-trip guide to Medicine Lake Volcano, northern California, including Lava Beds National Monument","indexId":"sir20175022K1","publicationYear":"2017","noYear":false,"chapter":"K1","title":"Geologic field-trip guide to Medicine Lake Volcano, northern California, including Lava Beds National Monument"},"predicate":"IS_PART_OF","object":{"id":70188710,"text":"sir20175022 - 2017 - Field-trip guides to selected volcanoes and volcanic landscapes of the western United States","indexId":"sir20175022","publicationYear":"2017","noYear":false,"title":"Field-trip guides to selected volcanoes and volcanic landscapes of the western United States"},"id":15},{"subject":{"id":70189947,"text":"sir20175022K2 - 2017 - Geologic field-trip guide to the Lassen segment of the Cascades Arc, northern California","indexId":"sir20175022K2","publicationYear":"2017","noYear":false,"chapter":"K2","title":"Geologic field-trip guide to the Lassen segment of the Cascades Arc, northern California"},"predicate":"IS_PART_OF","object":{"id":70188710,"text":"sir20175022 - 2017 - Field-trip guides to selected volcanoes and volcanic landscapes of the western United States","indexId":"sir20175022","publicationYear":"2017","noYear":false,"title":"Field-trip guides to selected volcanoes and volcanic landscapes of the western United States"},"id":16},{"subject":{"id":70189955,"text":"sir20175022K3 - 2017 - Geologic field-trip guide to Mount Shasta Volcano, northern California","indexId":"sir20175022K3","publicationYear":"2017","noYear":false,"chapter":"K3","title":"Geologic field-trip guide to Mount Shasta Volcano, northern California"},"predicate":"IS_PART_OF","object":{"id":70188710,"text":"sir20175022 - 2017 - Field-trip guides to selected volcanoes and volcanic landscapes of the western United States","indexId":"sir20175022","publicationYear":"2017","noYear":false,"title":"Field-trip guides to selected volcanoes and volcanic landscapes of the western United States"},"id":17},{"subject":{"id":70189980,"text":"sir20175022P - 2017 - Geologic field-trip guide to the volcanic and hydrothermal landscape of the Yellowstone Plateau","indexId":"sir20175022P","publicationYear":"2017","noYear":false,"chapter":"P","title":"Geologic field-trip guide to the volcanic and hydrothermal landscape of the Yellowstone Plateau"},"predicate":"IS_PART_OF","object":{"id":70188710,"text":"sir20175022 - 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Geologic field-trip guide of volcaniclastic sediments from snow- and ice-capped volcanoes—Mount St. Helens, Washington, and Mount Hood, Oregon","indexId":"sir20175022F","publicationYear":"2018","noYear":false,"chapter":"F","title":"Geologic field-trip guide of volcaniclastic sediments from snow- and ice-capped volcanoes—Mount St. Helens, Washington, and Mount Hood, Oregon"},"predicate":"IS_PART_OF","object":{"id":70188710,"text":"sir20175022 - 2017 - Field-trip guides to selected volcanoes and volcanic landscapes of the western United States","indexId":"sir20175022","publicationYear":"2017","noYear":false,"title":"Field-trip guides to selected volcanoes and volcanic landscapes of the western United States"},"id":20},{"subject":{"id":70206645,"text":"sir20175022E - 2019 - Field trip guide to Mount St. Helens, Washington—Recent and ancient volcaniclastic processes and deposits","indexId":"sir20175022E","publicationYear":"2019","noYear":false,"chapter":"E","displayTitle":"Field Trip Guide to Mount St. Helens, Washington—Recent and Ancient Volcaniclastic Processes and Deposits","title":"Field trip guide to Mount St. Helens, Washington—Recent and ancient volcaniclastic processes and deposits"},"predicate":"IS_PART_OF","object":{"id":70188710,"text":"sir20175022 - 2017 - Field-trip guides to selected volcanoes and volcanic landscapes of the western United States","indexId":"sir20175022","publicationYear":"2017","noYear":false,"title":"Field-trip guides to selected volcanoes and volcanic landscapes of the western United States"},"id":21},{"subject":{"id":70233771,"text":"sir20175022R - 2022 - Field-trip guide to continental arc to rift volcanism of the southern Rocky Mountains—Southern Rocky Mountain, Taos Plateau, and Jemez Mountains volcanic fields of southern Colorado and northern New Mexico","indexId":"sir20175022R","publicationYear":"2022","noYear":false,"chapter":"R","displayTitle":"Field-Trip Guide to Continental Arc to Rift Volcanism of the Southern Rocky Mountains—Southern Rocky Mountain, Taos Plateau, and Jemez Mountains Volcanic Fields of Southern Colorado and Northern New Mexico","title":"Field-trip guide to continental arc to rift volcanism of the southern Rocky Mountains—Southern Rocky Mountain, Taos Plateau, and Jemez Mountains volcanic fields of southern Colorado and northern New Mexico"},"predicate":"IS_PART_OF","object":{"id":70188710,"text":"sir20175022 - 2017 - Field-trip guides to selected volcanoes and volcanic landscapes of the western United States","indexId":"sir20175022","publicationYear":"2017","noYear":false,"title":"Field-trip guides to selected volcanoes and volcanic landscapes of the western United States"},"id":22},{"subject":{"id":70238114,"text":"sir20175022A - 2022 - Geologic field-trip guide to volcanism and its interaction with snow and ice at Mount Rainier, Washington","indexId":"sir20175022A","publicationYear":"2022","noYear":false,"chapter":"A","displayTitle":"Geologic Field-Trip Guide to Volcanism and its Interaction with Snow and Ice at Mount Rainier, Washington","title":"Geologic field-trip guide to volcanism and its interaction with snow and ice at Mount Rainier, Washington"},"predicate":"IS_PART_OF","object":{"id":70188710,"text":"sir20175022 - 2017 - Field-trip guides to selected volcanoes and volcanic landscapes of the western United States","indexId":"sir20175022","publicationYear":"2017","noYear":false,"title":"Field-trip guides to selected volcanoes and volcanic landscapes of the western United States"},"id":23}],"lastModifiedDate":"2017-07-27T12:29:42","indexId":"sir20175022","displayToPublicDate":"2017-06-23T00:00:00","publicationYear":"2017","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2017-5022","title":"Field-trip guides to selected volcanoes and volcanic landscapes of the western United States","docAbstract":"<p>The North American Cordillera is home to a greater diversity of volcanic provinces than any comparably sized region in the world. The interplay between changing plate-margin interactions, tectonic complexity, intra-crustal magma differentiation, and mantle melting have resulted in a wealth of volcanic landscapes.&nbsp; Field trips in this guide book collection (published as USGS Scientific Investigations Report 2017–5022) visit many of these landscapes, including (1) active subduction-related arc volcanoes in the Cascade Range; (2) flood basalts of the Columbia Plateau; (3) bimodal volcanism of the Snake River Plain-Yellowstone volcanic system; (4) some of the world’s largest known ignimbrites from southern Utah, central Colorado, and northern Nevada; (5) extension-related volcanism in the Rio Grande Rift and Basin and Range Province; and (6) the eastern Sierra Nevada featuring Long Valley Caldera and the iconic Bishop Tuff.&nbsp; Some of the field trips focus on volcanic eruptive and emplacement processes, calling attention to the fact that the western United States provides opportunities to examine a wide range of volcanological phenomena at many scales.</p><p>The 2017 Scientific Assembly of the International Association of Volcanology and Chemistry of the Earth’s Interior (IAVCEI) in Portland, Oregon, was the impetus to update field guides for many of the volcanoes in the Cascades Arc, as well as publish new guides for numerous volcanic provinces and features of the North American Cordillera. This collection of guidebooks summarizes decades of advances in understanding of magmatic and tectonic processes of volcanic western North America.&nbsp;</p><p>These field guides are intended for future generations of scientists and the general public as introductions to these fascinating areas; the hope is that the general public will be enticed toward further exploration and that scientists will pursue further field-based research.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20175022","costCenters":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"links":[{"id":342832,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/sir/2017/5022/coverthb.jpg"},{"id":342833,"rank":2,"type":{"id":13,"text":"Illustration"},"url":"https://pubs.usgs.gov/sir/2017/5022/sir20175022_map.pdf","text":"Field-trip overview map","size":"5 MB","linkFileType":{"id":1,"text":"pdf"},"description":"SIR 2017-5022"}],"contact":"<p><a href=\"http://volcanoes.usgs.gov/\" data-mce-href=\"http://volcanoes.usgs.gov/\">Volcano Science Center</a> - Menlo Park<br><a href=\"https://usgs.gov/\" data-mce-href=\"https://usgs.gov/\">U.S. Geological Survey</a><br>345 Middlefield Road, MS 910<br>Menlo Park, CA 94025</p>","publishingServiceCenter":{"id":14,"text":"Menlo Park PSC"},"publishedDate":"2017-06-23","noUsgsAuthors":false,"publicationDate":"2017-06-23","publicationStatus":"PW","scienceBaseUri":"594e28b4e4b062508e3abe22","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":700672,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70188778,"text":"70188778 - 2017 - Payments for carbon sequestration to alleviate development pressure in a rapidly urbanizing region","interactions":[],"lastModifiedDate":"2017-09-05T12:41:58","indexId":"70188778","displayToPublicDate":"2017-06-23T00:00:00","publicationYear":"2017","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1688,"text":"Forest Science","active":true,"publicationSubtype":{"id":10}},"title":"Payments for carbon sequestration to alleviate development pressure in a rapidly urbanizing region","docAbstract":"The purpose of this study was to determine individuals' willingness to enroll in voluntary payments for carbon sequestration programs through the use of a discrete choice experiment delivered to forest owners living in the rapidly urbanizing region surrounding Charlotte, North Carolina. We examined forest owners' willingness to enroll in payments for carbon sequestration policies under different levels of financial incentives (annual revenue), different contract lengths, and different program administrators (e.g., private companies versus a state or federal agency). We also examined the influence forest owners' sense of place had on their willingness to enroll in hypothetical programs. Our results showed a high level of ambivalence toward participating in payments for carbon sequestration programs. However, both financial incentives and contract lengths significantly influenced forest owners' intent to enroll. Neither program administration nor forest owners' sense of place influenced intent to enroll. Although our analyses indicated that payments from carbon sequestration programs are not currently competitive with the monetary returns expected from timber harvest or property sales, certain forest owners might see payments for carbon sequestration programs as a viable option for offsetting increasing tax costs as development encroaches and property values rise.","language":"English","publisher":"Society of American Foresters","doi":"10.5849/FS-2016-084R1","usgsCitation":"Smith, J.W., Dorning, M., Shoemaker, D.A., Meley, A., Dupey, L., and Meentemeyer, R.K., 2017, Payments for carbon sequestration to alleviate development pressure in a rapidly urbanizing region: Forest Science, v. 63, no. 3, p. 270-282, https://doi.org/10.5849/FS-2016-084R1.","productDescription":"13 p","startPage":"270","endPage":"282","ipdsId":"IP-070097","costCenters":[{"id":318,"text":"Geosciences and Environmental Change Science 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University","active":true,"usgs":false}],"preferred":false,"id":700337,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70188753,"text":"70188753 - 2017 - Prevalence of Batrachochytrium dendrobatidis and B. salamandrivorans in the Gulf Coast Waterdog, Necturus beyeri, from Southeast Louisiana, USA","interactions":[],"lastModifiedDate":"2017-06-23T15:50:47","indexId":"70188753","displayToPublicDate":"2017-06-23T00:00:00","publicationYear":"2017","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1898,"text":"Herpetological Review","active":true,"publicationSubtype":{"id":10}},"title":"Prevalence of Batrachochytrium dendrobatidis and B. salamandrivorans in the Gulf Coast Waterdog, Necturus beyeri, from Southeast Louisiana, USA","docAbstract":"The globally widespread amphibian fungal pathogen Batrachochytrium dendrobatidis (Bd) has been linked to amphibian declines worldwide (Lips et al. 2006; Skerratt et al. 2007). In Louisiana, USA, Bd has been found in several amphibian species (Chatfield et al. 2012; Rothermel et al. 2008), but to our knowledge no population-level die-offs have been observed. Published literature on Bd prevalence in Louisiana is scant for some amphibian species and completely absent for many others. This trend is likely driven by the perception that Bd is not a major problem in this area due to a lack of observed dieoffs attributable to chytridiomycosis.","language":"English","publisher":"Society for the Study of Amphibians and Reptiles","usgsCitation":"Glorioso, B.M., Waddle, J., and Richards-Zawacki, C.L., 2017, Prevalence of Batrachochytrium dendrobatidis and B. salamandrivorans in the Gulf Coast Waterdog, Necturus beyeri, from Southeast Louisiana, USA: Herpetological Review, v. 48, no. 2, p. 360-363.","productDescription":"4 p.","startPage":"360","endPage":"363","ipdsId":"IP-084027","costCenters":[{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"links":[{"id":342831,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"48","issue":"2","publishingServiceCenter":{"id":5,"text":"Lafayette PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"594e28b3e4b062508e3abe1d","contributors":{"authors":[{"text":"Glorioso, Brad M. 0000-0002-5400-7414 gloriosob@usgs.gov","orcid":"https://orcid.org/0000-0002-5400-7414","contributorId":4241,"corporation":false,"usgs":true,"family":"Glorioso","given":"Brad","email":"gloriosob@usgs.gov","middleInitial":"M.","affiliations":[{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true},{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"preferred":true,"id":699728,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Waddle, J. Hardin 0000-0003-1940-2133 waddleh@usgs.gov","orcid":"https://orcid.org/0000-0003-1940-2133","contributorId":168952,"corporation":false,"usgs":true,"family":"Waddle","given":"J. Hardin","email":"waddleh@usgs.gov","affiliations":[{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true},{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"preferred":false,"id":699729,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Richards-Zawacki, Corinne L.","contributorId":193276,"corporation":false,"usgs":false,"family":"Richards-Zawacki","given":"Corinne","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":699730,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70193816,"text":"70193816 - 2017 - Acute toxicity of polyacrylamide flocculants to early life stages of freshwater mussels","interactions":[],"lastModifiedDate":"2017-11-08T15:14:05","indexId":"70193816","displayToPublicDate":"2017-06-23T00:00:00","publicationYear":"2017","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1571,"text":"Environmental Toxicology and Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"Acute toxicity of polyacrylamide flocculants to early life stages of freshwater mussels","docAbstract":"<p><span>Polyacrylamide has become an effective tool for reducing construction-related suspended sediment and turbidity, which are considered to have significant adverse impacts on aquatic ecosystems and are a leading cause of the degradation of North American streams and rivers. However, little is known about the effects of polyacrylamide on many freshwater organisms, and prior to the present study, no information existed on the toxicity of polyacrylamide compounds to native freshwater mussels (family Unionidae), one of the most imperiled faunal groups globally. Following standard test guidelines, we exposed juvenile mussels (test duration 96 h) and glochidia larvae (test duration 24 h) to 5 different anionic polyacrylamide compounds and 1 non-ionic compound. Species tested included the yellow lampmussel (</span><i>Lampsilis cariosa</i><span>), an Atlantic Slope species that is listed as endangered in North Carolina; the Appalachian elktoe (</span><i>Alasmidonta raveneliana</i><span>), a federally endangered Interior Basin species; and the washboard (</span><i>Megalonaias nervosa</i><span>), a common Interior Basin species. We found that median lethal concentrations (LC50s) of polyacrylamide ranged from 411.7 to &gt;1000 mg/L for glochidia and from 126.8 to &gt;1000 mg/L for juveniles. All LC50s were orders of magnitude greater (2–3) than concentrations typically recommended for turbidity control (1–5 mg/L), regardless of their molecular weight or charge density. The results demonstrate that the polyacrylamide compounds tested were not acutely toxic to the mussel species and life stages tested, indicating minimal risk of short-term exposure from polyacrylamide applications in the environment. However, other potential uses of polyacrylamide in the environment (e.g., wastewater treatment, paper processing, mining, algae removal) and their chronic or sublethal effects remain uncertain and warrant additional investigation.</span></p>","language":"English","publisher":"John Wiley & Sons, Inc.","doi":"10.1002/etc.3821","usgsCitation":"Buczek, S.B., Cope, W., McLaughlin, R.A., and Kwak, T.J., 2017, Acute toxicity of polyacrylamide flocculants to early life stages of freshwater mussels: Environmental Toxicology and Chemistry, v. 36, no. 10, p. 2715-2721, https://doi.org/10.1002/etc.3821.","productDescription":"7 p.","startPage":"2715","endPage":"2721","ipdsId":"IP-086264","costCenters":[{"id":198,"text":"Coop Res Unit Atlanta","active":true,"usgs":true}],"links":[{"id":348489,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"36","issue":"10","publishingServiceCenter":{"id":9,"text":"Reston PSC"},"noUsgsAuthors":false,"publicationDate":"2017-04-11","publicationStatus":"PW","scienceBaseUri":"5a0425b6e4b0dc0b45b4534a","contributors":{"authors":[{"text":"Buczek, Sean B.","contributorId":200188,"corporation":false,"usgs":false,"family":"Buczek","given":"Sean","email":"","middleInitial":"B.","affiliations":[{"id":33914,"text":"North Carolina State University, Raleigh","active":true,"usgs":false}],"preferred":false,"id":721345,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cope, W. Gregory","contributorId":70353,"corporation":false,"usgs":true,"family":"Cope","given":"W. Gregory","affiliations":[],"preferred":false,"id":721346,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McLaughlin, Richard A.","contributorId":200189,"corporation":false,"usgs":false,"family":"McLaughlin","given":"Richard","email":"","middleInitial":"A.","affiliations":[{"id":33914,"text":"North Carolina State University, Raleigh","active":true,"usgs":false}],"preferred":false,"id":721347,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Kwak, Thomas J. 0000-0002-0616-137X tkwak@usgs.gov","orcid":"https://orcid.org/0000-0002-0616-137X","contributorId":834,"corporation":false,"usgs":true,"family":"Kwak","given":"Thomas","email":"tkwak@usgs.gov","middleInitial":"J.","affiliations":[{"id":198,"text":"Coop Res Unit Atlanta","active":true,"usgs":true}],"preferred":true,"id":720596,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70188789,"text":"70188789 - 2017 - The Niobrara Formation as a challenge to water quality in the Arkansas River, Colorado, USA","interactions":[],"lastModifiedDate":"2017-06-23T15:28:28","indexId":"70188789","displayToPublicDate":"2017-06-23T00:00:00","publicationYear":"2017","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3823,"text":"Journal of Hydrology: Regional Studies","active":true,"publicationSubtype":{"id":10}},"title":"The Niobrara Formation as a challenge to water quality in the Arkansas River, Colorado, USA","docAbstract":"<p id=\"absSec_1\"><strong>Study region</strong></p><p id=\"spar0060\">Arkansas River, east of the Rocky Mountains.</p><p id=\"absSec_2\"><strong>Study focus</strong></p><p id=\"spar0065\">Cretaceous sedimentary rocks in the western United States generally pose challenges to water quality, often through mobilization of salts and trace metals by irrigation. However, in the Arkansas River Basin of Colorado, patchy exposure of multiple Cretaceous formations has made it difficult to identify which formations are most problematic. This paper examines water quality in surface-water inflows along a 26-km reach of the Arkansas River relative to the presence or absence of the Cretaceous Niobrara Formation within the watershed.</p><p id=\"absSec_3\"><strong>New hydrological insights for the region</strong></p><p id=\"spar0070\">Principal component analysis (PCA) shows Niobrara-influenced inflows have distinctive geochemistry, particularly with respect to Na, Mg, SO4<sup>2−</sup>, and Se. Uranium concentrations are also greater in Niobrara-influenced inflows. During the irrigation season, median dissolved solids, Se, and U concentrations in Niobrara-influenced inflows were 83%, 646%, and 55%, respectively, greater than medians where Niobrara Formation surface exposures were absent. During the non-irrigation season, which better reflects geologic influence, the differences were more striking. Median dissolved solids, Se, and U concentrations in Niobrara-influenced inflows were 288%, 863%, and 155%, respectively, greater than median concentrations where the Niobrara Formation was absent. Identification of the Niobrara Formation as a disproportionate source for dissolved solids, Se, and U will allow for more targeted studies and management, particularly where exposures underlie irrigated agriculture.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.ejrh.2017.05.001","usgsCitation":"Bern, C.R., and Stogner, 2017, The Niobrara Formation as a challenge to water quality in the Arkansas River, Colorado, USA: Journal of Hydrology: Regional Studies, v. 12, p. 181-195, https://doi.org/10.1016/j.ejrh.2017.05.001.","productDescription":"15 p.","startPage":"181","endPage":"195","ipdsId":"IP-081119","costCenters":[{"id":191,"text":"Colorado Water Science Center","active":true,"usgs":true}],"links":[{"id":461505,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1016/j.ejrh.2017.05.001","text":"Publisher Index Page"},{"id":342827,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Colorado","otherGeospatial":"Arkansas River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -105.3369140625,\n              38.33196157898413\n            ],\n            [\n              -104.94964599609374,\n              38.33196157898413\n            ],\n            [\n              -104.94964599609374,\n              38.5213096674994\n            ],\n            [\n              -105.3369140625,\n              38.5213096674994\n            ],\n            [\n              -105.3369140625,\n              38.33196157898413\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"12","publishingServiceCenter":{"id":2,"text":"Denver PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"594e28b1e4b062508e3abe13","contributors":{"authors":[{"text":"Bern, Carleton R. 0000-0002-8980-1781 cbern@usgs.gov","orcid":"https://orcid.org/0000-0002-8980-1781","contributorId":166816,"corporation":false,"usgs":true,"family":"Bern","given":"Carleton","email":"cbern@usgs.gov","middleInitial":"R.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true},{"id":191,"text":"Colorado Water Science Center","active":true,"usgs":true}],"preferred":false,"id":700374,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stogner 0000-0002-3185-1452 rstogner@usgs.gov","orcid":"https://orcid.org/0000-0002-3185-1452","contributorId":938,"corporation":false,"usgs":true,"family":"Stogner","email":"rstogner@usgs.gov","affiliations":[{"id":191,"text":"Colorado Water Science Center","active":true,"usgs":true}],"preferred":false,"id":700375,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70188470,"text":"ofr20171070 - 2017 - Juvenile salmonid monitoring in the White Salmon River, Washington, post-Condit Dam removal, 2016","interactions":[],"lastModifiedDate":"2017-06-24T10:59:14","indexId":"ofr20171070","displayToPublicDate":"2017-06-23T00:00:00","publicationYear":"2017","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2017-1070","title":"Juvenile salmonid monitoring in the White Salmon River, Washington, post-Condit Dam removal, 2016","docAbstract":"<p class=\"p1\">Condit Dam, at river kilometer 5.3 on the White Salmon River, Washington, was breached in 2011 and removed completely in 2012, allowing anadromous salmonids access to habitat that had been blocked for nearly 100 years. A multi-agency workgroup concluded that the preferred salmonid restoration alternative was natural recolonization with monitoring to assess efficacy, followed by a management evaluation 5 years after dam removal. Limited monitoring of salmon and steelhead spawning has occurred since 2011, but no monitoring of juveniles occurred until 2016. During 2016, we operated a rotary screw trap at river kilometer 2.3 (3 kilometers downstream of the former dam site) from late March through May and used backpack electrofishing during summer to assess juvenile salmonid distribution and abundance. The screw trap captured primarily steelhead (<i>Oncorhynchus mykiss</i>; smolts, parr, and fry) and coho salmon (<i>O. kisutch</i>; smolts and fry). We estimated the number of steelhead smolts at 3,851 (standard error = 1,454) and coho smolts at 1,093 (standard error = 412). In this document, we refer to <i>O. mykiss </i>caught at the screw trap as steelhead because they were actively migrating, but because we did not know migratory status of <i>O. mykiss </i>caught in electrofishing surveys, we simply refer to them as <i>O. mykiss </i>or steelhead/rainbow trout. Steelhead and coho smolts tagged with passive integrated transponder tags were subsequently detected downstream at Bonneville Dam on the Columbia River. Few Chinook salmon (<i>O. tshawytscha</i>) fry were captured, possibly as a result of trap location or effects of a December 2015 flood. Sampling in Mill, Buck, and Rattlesnake Creeks (all upstream of the former dam site) showed that juvenile coho were present in Mill and Buck Creeks, suggesting spawning had occurred there. We compared <i>O. mykiss </i>abundance data in sites on Buck and Rattlesnake Creeks to pre-dam removal data. During 2016, age-0 <i>O. mykiss </i>were more abundant in Buck Creek than in 2009 or 2010, though age-1 and older <i>O. mykiss </i>abundance was similar. In Rattlesnake Creek, age-0 <i>O. mykiss </i>abundance during 2016 slightly exceeded the mean abundance from 2001 through 2005, although age-1 and older <i>O. mykiss </i>abundance was lower than from 2001 through 2005. These sampling efforts also provided the opportunity to collect genetic samples to investigate parental and stock origin, although funding to analyze the samples was not part of this grant. Juvenile salmonid sampling efforts during 2016 have shown that natural spawning produced steelhead and coho smolts and that coho were colonizing some tributaries. The 2016 efforts also provided the first post-dam juvenile abundance estimates. We hope to continue monitoring to better understand abundance trends, distribution, and life history patterns of recolonizing salmonids in the White Salmon River to assess efficacy of natural recolonization and to inform management decisions.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20171070","collaboration":"Prepared in cooperation with Mid-Columbia Fisheries Enhancement Group","usgsCitation":"Jezorek, I.G., and Hardiman, J.M., 2017, Juvenile salmonid monitoring in the White Salmon River, Washington, post-Condit Dam removal, 2016: U.S. Geological Survey Open-File Report 2017-1070, 34 p., https://doi.org/10.3133/ofr20171070.","productDescription":"iv, 34 p.","onlineOnly":"Y","ipdsId":"IP-083906","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":342774,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2017/1070/coverthb.jpg"},{"id":342775,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2017/1070/ofr20171070.pdf","text":"Report","size":"1.1 MB","linkFileType":{"id":1,"text":"pdf"},"description":"OFR 2017-1070"}],"country":"United States","state":"Washington","otherGeospatial":"White Salmon River watershed","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -121.75460815429686,\n              45.64428817847555\n            ],\n            [\n              -121.27258300781251,\n              45.64428817847555\n            ],\n            [\n              -121.27258300781251,\n              45.99076013759662\n            ],\n            [\n              -121.75460815429686,\n              45.99076013759662\n            ],\n            [\n              -121.75460815429686,\n              45.64428817847555\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","contact":"<p>Director, <a href=\"https://wfrc.usgs.gov/\" target=\"blank\" data-mce-href=\"https://wfrc.usgs.gov/\">Western Fisheries Research Center</a><br> U.S. Geological Survey<br> 6505 NE 65th Street<br> Seattle, Washington 98115</p>","tableOfContents":"<ul><li>Abstract<br></li><li>Introduction<br></li><li>Description of Study Site<br></li><li>Study Methods<br></li><li>Results<br></li><li>Discussion<br></li><li>Acknowledgments<br></li><li>References Cited<br></li><li>Appendix A. Length Frequencies<br></li></ul>","publishingServiceCenter":{"id":12,"text":"Tacoma PSC"},"publishedDate":"2017-06-23","noUsgsAuthors":false,"publicationDate":"2017-06-23","publicationStatus":"PW","scienceBaseUri":"594e28b5e4b062508e3abe25","contributors":{"authors":[{"text":"Jezorek, Ian G. 0000-0002-3842-3485 ijezorek@usgs.gov","orcid":"https://orcid.org/0000-0002-3842-3485","contributorId":3572,"corporation":false,"usgs":true,"family":"Jezorek","given":"Ian","email":"ijezorek@usgs.gov","middleInitial":"G.","affiliations":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"preferred":true,"id":697908,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hardiman, Jill M. 0000-0002-3661-9695 jhardiman@usgs.gov","orcid":"https://orcid.org/0000-0002-3661-9695","contributorId":2672,"corporation":false,"usgs":true,"family":"Hardiman","given":"Jill","email":"jhardiman@usgs.gov","middleInitial":"M.","affiliations":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"preferred":true,"id":697909,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70188597,"text":"fs20173049 - 2017 - Selected water-resources activities of the U.S. Geological Survey in New England in 2017","interactions":[],"lastModifiedDate":"2017-06-23T10:27:25","indexId":"fs20173049","displayToPublicDate":"2017-06-22T12:00:00","publicationYear":"2017","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2017-3049","title":"Selected water-resources activities of the U.S. Geological Survey in New England in 2017","docAbstract":"The New England Water Science Center of the U.S. Geological Survey (USGS) is headquartered in Pembroke, New Hampshire, with offices in East Hartford, Connecticut; Augusta, Maine; Northborough, Massachusetts; and Montpelier, Vermont. The areas of expertise covered by the water science center’s staff of 130 include aquatic biology, chemistry, geographic information systems, geology, hydrologic sciences and engineering, and water use.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/fs20173049","usgsCitation":"Weiskel, P.K., 2017, Selected water-resources activities of the U.S. Geological Survey in New England in 2017: U.S. Geological Survey Fact Sheet 2017–3049, 2 p., https://doi.org/10.3133/fs20173049.","productDescription":"2 p.","onlineOnly":"Y","additionalOnlineFiles":"N","ipdsId":"IP-088015","costCenters":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"links":[{"id":342744,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/2017/3049/fs20173049.pdf","text":"Report","size":"665 KB","linkFileType":{"id":1,"text":"pdf"},"description":"FS 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 \"}}]}","contact":"<p><a href=\"mailto:dc_nh@usgs.gov\" data-mce-href=\"mailto:dc_nh@usgs.gov\">Director</a>, <a href=\"https://newengland.water.usgs.gov/\" data-mce-href=\"https://newengland.water.usgs.gov/\">New England Water Science Center</a><br> U.S. Geological Survey<br> 331 Commerce Way, Suite 2<br> Pembroke, NH 03275-3718</p>","tableOfContents":"<ul><li>Selected Regional-Scale USGS Water-Resource Activities in New&nbsp;England</li><li>Selected State- and Local-Scale Water-Resources Activities in New&nbsp;England</li></ul>","publishingServiceCenter":{"id":11,"text":"Pembroke PSC"},"publishedDate":"2017-06-22","noUsgsAuthors":false,"publicationDate":"2017-06-22","publicationStatus":"PW","scienceBaseUri":"594cd73ae4b062508e3951b7","contributors":{"authors":[{"text":"Weiskel, Peter K. pweiskel@usgs.gov","contributorId":1099,"corporation":false,"usgs":true,"family":"Weiskel","given":"Peter","email":"pweiskel@usgs.gov","middleInitial":"K.","affiliations":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true},{"id":376,"text":"Massachusetts Water Science Center","active":true,"usgs":true}],"preferred":true,"id":698505,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70187070,"text":"sir20175022N - 2017 - Field-trip guide to the vents, dikes, stratigraphy, and structure of the Columbia River Basalt Group, eastern Oregon and southeastern Washington","interactions":[{"subject":{"id":70187070,"text":"sir20175022N - 2017 - Field-trip guide to the vents, dikes, stratigraphy, and structure of the Columbia River Basalt Group, eastern Oregon and southeastern Washington","indexId":"sir20175022N","publicationYear":"2017","noYear":false,"chapter":"N","title":"Field-trip guide to the vents, dikes, stratigraphy, and structure of the Columbia River Basalt Group, eastern Oregon and southeastern Washington"},"predicate":"IS_PART_OF","object":{"id":70188710,"text":"sir20175022 - 2017 - Field-trip guides to selected volcanoes and volcanic landscapes of the western United States","indexId":"sir20175022","publicationYear":"2017","noYear":false,"title":"Field-trip guides to selected volcanoes and volcanic landscapes of the western United States"},"id":1}],"isPartOf":{"id":70188710,"text":"sir20175022 - 2017 - Field-trip guides to selected volcanoes and volcanic landscapes of the western United States","indexId":"sir20175022","publicationYear":"2017","noYear":false,"title":"Field-trip guides to selected volcanoes and volcanic landscapes of the western United States"},"lastModifiedDate":"2017-07-27T12:29:58","indexId":"sir20175022N","displayToPublicDate":"2017-06-22T00:00:00","publicationYear":"2017","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2017-5022","chapter":"N","title":"Field-trip guide to the vents, dikes, stratigraphy, and structure of the Columbia River Basalt Group, eastern Oregon and southeastern Washington","docAbstract":"<p class=\"m_-3446220523471206107gmail-m_1434392373000247235gmail-m_-1333559155352269249gmail-p1\">The Columbia River Basalt Group covers an area of more than 210,000 km<span class=\"m_-3446220523471206107gmail-m_1434392373000247235gmail-m_-1333559155352269249gmail-s1\"><sup><span>2</span></sup>&nbsp;</span>with an estimated volume of 210,000 km<sup><span class=\"m_-3446220523471206107gmail-m_1434392373000247235gmail-m_-1333559155352269249gmail-s1\"><span>3</span></span></sup>. As the youngest continental flood-basalt province on Earth (16.7–5.5 Ma), it is well preserved, with a coherent and detailed stratigraphy exposed in the deep canyonlands of eastern Oregon and southeastern Washington. The Columbia River flood-basalt province is often cited as a model for the study of similar provinces worldwide.</p><p class=\"m_-3446220523471206107gmail-m_1434392373000247235gmail-m_-1333559155352269249gmail-p1\">This field-trip guide explores the main source region of the&nbsp;<span>Columbia River Basalt Group</span>&nbsp;and is written for trip participants attending the 2017 International Association of Volcanology and Chemistry of the Earth’s Interior (IAVCEI) Scientific Assembly in Portland, Oregon, USA. The first part of the guide provides an overview of the geologic features common in the Columbia River flood-basalt province&nbsp;and the stratigraphic terminology used in the Columbia River Basalt Group. The accompanying road log examines the stratigraphic evolution, eruption history, and structure of the province through a field examination of the lavas, dikes, and pyroclastic rocks of the Columbia River Basalt Group.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20175022N","usgsCitation":"Camp, V.E., Reidel, S.P., Ross, M.E., Brown, R.J., and Self, S., 2017, Field-trip guide to the vents, dikes, stratigraphy, and structure of the Columbia River Basalt Group, eastern Oregon and southeastern Washington: U.S. Geological Survey Scientific Investigations Report 2017–5022–N, 88 p., https://doi.org/10.3133/sir20175022N.","productDescription":"Report: x, 88 p.","startPage":"1","endPage":"88","numberOfPages":"104","onlineOnly":"Y","ipdsId":"IP-076082","costCenters":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"links":[{"id":342752,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/sir/2017/5022/n/sir20175022n.pdf","text":"Report","size":"13 MB","linkFileType":{"id":1,"text":"pdf"},"description":"SIR 2017-5022 N"},{"id":342749,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/sir/2017/5022/n/coverthb.jpg"}],"country":" United States","state":"Oregon, Washington","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -123,\n              42.5\n            ],\n            [\n              -116.6666,\n              42.5\n            ],\n            [\n              -116.6666,\n              47.25\n            ],\n            [\n              -123,\n              47.25\n            ],\n            [\n              -123,\n              42.5\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","contact":"<p><a href=\"http://volcanoes.usgs.gov/\" data-mce-href=\"http://volcanoes.usgs.gov/\">Volcano Science Center</a> - Menlo Park<br><a href=\"https://usgs.gov/\" data-mce-href=\"https://usgs.gov/\">U.S. Geological Survey</a><br>345 Middlefield Road, MS 910<br>Menlo Park, CA 94025</p>","tableOfContents":"<ul><li>Preface<br></li><li>Contributing Authors<br></li><li>Introduction<br></li><li>Physiography and Regional Setting<br></li><li>Stratigraphy of the Columbia River Basalt Group<br></li><li>Feeder Dikes<br></li><li>Physical Volcanology<br></li><li>Deformation and Crustal Stress During and After the CRBG Eruptions<br></li><li>Petrogenesis<br></li><li>Road Log<br></li><li>References Cited<br></li></ul>","publishingServiceCenter":{"id":14,"text":"Menlo Park PSC"},"publishedDate":"2017-06-22","noUsgsAuthors":false,"publicationDate":"2017-06-22","publicationStatus":"PW","scienceBaseUri":"594cd73ee4b062508e3951cf","contributors":{"authors":[{"text":"Camp, Victor E","contributorId":138632,"corporation":false,"usgs":false,"family":"Camp","given":"Victor E","affiliations":[{"id":6608,"text":"San Diego State University","active":true,"usgs":false}],"preferred":false,"id":698240,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reidel, Stephen P.","contributorId":191215,"corporation":false,"usgs":false,"family":"Reidel","given":"Stephen","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":698241,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ross, Martin E.","contributorId":191217,"corporation":false,"usgs":false,"family":"Ross","given":"Martin","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":698243,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Brown, Richard J.","contributorId":191216,"corporation":false,"usgs":false,"family":"Brown","given":"Richard J.","affiliations":[],"preferred":false,"id":698242,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Self, Stephen","contributorId":191218,"corporation":false,"usgs":false,"family":"Self","given":"Stephen","email":"","affiliations":[],"preferred":false,"id":698244,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70185506,"text":"sir20175022G - 2017 - Field-trip guide to Mount Hood, Oregon, highlighting eruptive history and hazards","interactions":[{"subject":{"id":70185506,"text":"sir20175022G - 2017 - Field-trip guide to Mount Hood, Oregon, highlighting eruptive history and hazards","indexId":"sir20175022G","publicationYear":"2017","noYear":false,"chapter":"G","title":"Field-trip guide to Mount Hood, Oregon, highlighting eruptive history and hazards"},"predicate":"IS_PART_OF","object":{"id":70188710,"text":"sir20175022 - 2017 - Field-trip guides to selected volcanoes and volcanic landscapes of the western United States","indexId":"sir20175022","publicationYear":"2017","noYear":false,"title":"Field-trip guides to selected volcanoes and volcanic landscapes of the western United States"},"id":1}],"isPartOf":{"id":70188710,"text":"sir20175022 - 2017 - Field-trip guides to selected volcanoes and volcanic landscapes of the western United States","indexId":"sir20175022","publicationYear":"2017","noYear":false,"title":"Field-trip guides to selected volcanoes and volcanic landscapes of the western United States"},"lastModifiedDate":"2017-07-27T12:30:25","indexId":"sir20175022G","displayToPublicDate":"2017-06-22T00:00:00","publicationYear":"2017","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2017-5022","chapter":"G","title":"Field-trip guide to Mount Hood, Oregon, highlighting eruptive history and hazards","docAbstract":"<p>This guidebook describes stops of interest for a geological field trip around Mount Hood volcano. It was developed for the 2017 International Association of Volcanology and Chemistry of the Earth’s Interior (IAVCEI) Scientific Assembly in Portland, Oregon. The intent of this guidebook and accompanying contributions is to provide an overview of Mount Hood, including its chief geologic processes, magmatic system, eruptive history, local tectonics, and hazards, by visiting a variety of readily accessible localities. We also describe coeval, largely monogenetic, volcanoes in the region. Accompanying the field-trip guidebook are separately authored contributions that discuss in detail the Mount Hood magmatic system and its products and behavior (Kent and Koleszar, this volume); Mount Hood earthquakes and their relation to regional tectonics and the volcanic system (Thelen and Moran, this volume); and young surface faults cutting the broader Mount Hood area whose extent has come to light after acquisition of regional light detection and ranging coverage (Madin and others, this volume).</p><p>The trip makes an approximately 175-mile (280-kilometer) clockwise loop around Mount Hood, starting and ending in Portland. The route heads east on Interstate 84 through the Columbia River Gorge National Scenic Area. The guidebook points out only a few conspicuous features of note in the gorge, but many other guides to the gorge are available. The route continues south on the Mount Hood National Scenic Byway on Oregon Route 35 following Hood River, and returns to Portland on U.S. Highway 26 following Sandy River. The route traverses rocks as old as the early Miocene Eagle Creek Formation and overlying Columbia River Basalt Group of middle Miocene age, but chiefly lava flows and clastic products of arc volcanism of late Miocene to Holocene age.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20175022G","usgsCitation":"Scott, W.E., and Gardner, C.A., 2017, Field-trip guide to Mount Hood, Oregon, highlighting eruptive history and hazards: U.S. Geological Survey Scientific Investigations Report 2017–5022–G, 115 p., https://doi.org/10.3133/sir20175022g.","productDescription":"xii, 115 p.","numberOfPages":"132","ipdsId":"IP-077540","costCenters":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"links":[{"id":342738,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/sir/2017/5022/g/coverthb2.jpg"},{"id":342761,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/sir/2017/5022/g/sir20175022g.pdf","text":"Report","size":"27 MB","linkFileType":{"id":1,"text":"pdf"},"description":"SIR 2017-5022 G"}],"country":"United States","state":"Oregon","otherGeospatial":"Mount 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href=\"http://volcanoes.usgs.gov/\" data-mce-href=\"http://volcanoes.usgs.gov/\">Volcano Science Center</a> - Menlo Park<br><a href=\"https://usgs.gov/\" data-mce-href=\"https://usgs.gov/\">U.S. Geological Survey</a><br>345 Middlefield Road, MS 910<br>Menlo Park, CA 94025<br></p>","tableOfContents":"<ul><li>Introduction<br></li><li>Highlights of Quaternary Volcanism<br></li><li>Route From Portland to Hood River<br></li><li>Field-Trip Stops<br></li><li>Stop 1. Panorama Point Overlook of the Cascade Range, Mount Hood, and Hood River Valley<br></li><li>Stop 2. Hood River Lahar<br></li><li>Stop 3. Andesite of Parkdale<br></li><li>Stop 4. Quarry in Lower Pleistocene Basalt of Tilly Jane; View of North Flank of Mount Hood<br></li><li>Stop 5. Basaltic Andesite and Andesite of Cloud Cap and Basaltic Andesite of Dog River<br></li><li>Stop 6. Quarry in Lava Flow of Cloud Cap Volcano<br></li><li>Stop 7. View Up Eliot Branch From Inspiration Point<br></li><li>Stop 8. Cloud Cap Inn<br></li><li>Stop 9. Pre-Hood Andesite of Doe Creek<br></li><li>1980 Debris Flow and Flood on Polallie Creek<br></li><li>Stop 10. Late Pleistocene Andesite Lava Flow of Tamanawas Falls, Part of Langille Crags-Texas Eruptive Episode of High-strontium Lava<br></li><li>Mafic Enclaves in Mount Hood Andesite<br></li><li>Stop 11. Pocket Creek—LGM End Moraines Rich in Dome Lava and View of Southeast Flank of Mount Hood<br></li><li>Stop 12. Bennett Pass Till Exposure&nbsp;<br></li><li>Stop 13. Main Parking Lot at Mount Hood Meadows Ski Resort<br></li><li>Stop 14. White River Pyroclastic-Flow and Lahar Deposits of Old Maid Age<br></li><li>Stop 15. Frog Lake Fault Scarps&nbsp;<br></li><li>Stop 16. U.S. Highway 26 Roadcuts in Andesite of South Flank<br></li><li>Stop 17. Three Stops Along Timberline Road<br></li><li>Timberline Lodge Area<br></li><li>Stop 18. Hike East from Timberline Lodge on Timberline Trail to Rim of White River Canyon and Additional Sites<br></li><li>Stop 19. Hike Timberline Trail West from Timberline Lodge to Little Zigzag and Zigzag Canyons<br></li><li>Stop 20. Andesite of Yocum Falls<br></li><li>Stop 21. Quarry in Basaltic Andesite and Andesite of Little Zigzag River; Timberline Deposits and Contact Between Timberline and Polallie Deposits<br></li><li>Stop 22. Andesite of Lower Zigzag Canyon and Andesite of Lady Creek<br></li><li>Stop 23. Late Holocene Lahar Deposits Along Upper Sandy River<br></li><li>Stop 24. West Flank of Mount Hood and Sandy Glacier Volcano<br></li><li>Stop 25. Basalt of Bald Mountain, and View of West Flank of Mount Hood and Sandy Glacier Volcano<br></li><li>Stop 26. Jonsrud Viewpoint Park<br></li><li>Stop 27. Lahar and Lahar-Runout Deposits of Timberline Age on West Bank of Sandy River<br></li><li>Mount Hood Volcano Hazards<br></li><li>References Cited<br></li></ul><h4>Sections</h4><ul><li>A Summary of Recent Petrological and Geochemical Studies of Mount Hood, Oregon<br></li><li>The Mount Hood Fault Zone—Late Quaternary and Holocene Fault Features Newly Mapped with High-resolution Lidar Imagery<br></li><li>Seismicity At and Around Mount Hood, Oregon<br></li></ul>","publishingServiceCenter":{"id":14,"text":"Menlo Park PSC"},"publishedDate":"2017-06-22","noUsgsAuthors":false,"publicationDate":"2017-06-22","publicationStatus":"PW","scienceBaseUri":"594cd73fe4b062508e3951d3","contributors":{"authors":[{"text":"Scott, William E. 0000-0001-8156-979X wescott@usgs.gov","orcid":"https://orcid.org/0000-0001-8156-979X","contributorId":1725,"corporation":false,"usgs":true,"family":"Scott","given":"William","email":"wescott@usgs.gov","middleInitial":"E.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":697691,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gardner, Cynthia A. 0000-0002-6214-6182 cgardner@usgs.gov","orcid":"https://orcid.org/0000-0002-6214-6182","contributorId":1959,"corporation":false,"usgs":true,"family":"Gardner","given":"Cynthia","email":"cgardner@usgs.gov","middleInitial":"A.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true},{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"preferred":true,"id":697692,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70188743,"text":"70188743 - 2017 - RNA sequencing analysis of transcriptional change in the freshwater mussel Elliptio complanata after environmentally relevant sodium chloride exposure","interactions":[],"lastModifiedDate":"2017-08-27T18:26:16","indexId":"70188743","displayToPublicDate":"2017-06-22T00:00:00","publicationYear":"2017","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1571,"text":"Environmental Toxicology and Chemistry","active":true,"publicationSubtype":{"id":10}},"displayTitle":"RNA sequencing analysis of transcriptional change in the freshwater mussel <i>Elliptio complanata</i> after environmentally relevant sodium chloride exposure","title":"RNA sequencing analysis of transcriptional change in the freshwater mussel Elliptio complanata after environmentally relevant sodium chloride exposure","docAbstract":"<p><span>To identify potential biomarkers of salt stress in a freshwater sentinel species, we examined transcriptional responses of the common mussel </span><i>Elliptio complanata</i><span> to controlled sodium chloride (NaCl) exposures. Ribonucleic acid sequencing (RNA-Seq) of mantle tissue identified 481 transcripts differentially expressed in adult mussels exposed to 2 ppt NaCl (1.2 ppt chloride) for 7 d, of which 290 had nonoverlapping intervals. Differentially expressed gene categories included ion and transmembrane transport, oxidoreductase activity, maintenance of protein folding, and amino acid metabolism. The rate-limiting enzyme for synthesis of taurine, an amino acid frequently linked to osmotic stress in aquatic species, was upregulated, as was the transmembrane ion pump sodium/potassium adenosine 5′-triphosphatase. These patterns confirm a primary transcriptional response to the experimental dose, albeit likely overlapping with nonspecific secondary stress responses. Substantial involvement of the heat shock protein 70 chaperone family and the water-transporting aquaporin family was not detected, however, in contrast to some studies in other bivalves. A subset of the most significantly regulated genes was confirmed by quantitative polymerase chain reaction in an independent sample. Cluster analysis showed separation of mussels exposed to 2 ppt NaCl from control mussels in multivariate space, but mussels exposed to 1 ppt NaCl were largely indistinguishable from controls. Transcriptome-scale analysis of salt exposure under laboratory conditions efficiently identified candidate biomarkers for further functional analysis and field validation</span></p>","language":"English","publisher":"Society of Environmental Toxicology and Chemistry","doi":"10.1002/etc.3774","usgsCitation":"Robertson, L.S., Galbraith, H.S., Iwanowicz, D.D., Blakeslee, C.J., and Cornman, R.S., 2017, RNA sequencing analysis of transcriptional change in the freshwater mussel Elliptio complanata after environmentally relevant sodium chloride exposure: Environmental Toxicology and Chemistry, v. 36, no. 9, p. 2352-2366, https://doi.org/10.1002/etc.3774.","productDescription":"15 p.","startPage":"2352","endPage":"2366","ipdsId":"IP-062505","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":438294,"rank":0,"type":{"id":30,"text":"Data Release"},"url":"https://doi.org/10.5066/F7P26WCG","text":"USGS data release","linkHelpText":"Experimental analysis of Elliptio complanata transcriptional response to salt stress"},{"id":342788,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"36","issue":"9","publishingServiceCenter":{"id":10,"text":"Baltimore PSC"},"noUsgsAuthors":false,"publicationDate":"2017-02-22","publicationStatus":"PW","scienceBaseUri":"594cd73ce4b062508e3951c1","contributors":{"authors":[{"text":"Robertson, Laura S. lrobertson@usgs.gov","contributorId":193277,"corporation":false,"usgs":false,"family":"Robertson","given":"Laura","email":"lrobertson@usgs.gov","middleInitial":"S.","affiliations":[],"preferred":false,"id":699586,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Galbraith, Heather S. 0000-0003-3704-3517 hgalbraith@usgs.gov","orcid":"https://orcid.org/0000-0003-3704-3517","contributorId":4519,"corporation":false,"usgs":true,"family":"Galbraith","given":"Heather","email":"hgalbraith@usgs.gov","middleInitial":"S.","affiliations":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"preferred":true,"id":699587,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Iwanowicz, Deborah D. 0000-0002-9613-8594 diwanowicz@usgs.gov","orcid":"https://orcid.org/0000-0002-9613-8594","contributorId":2253,"corporation":false,"usgs":true,"family":"Iwanowicz","given":"Deborah","email":"diwanowicz@usgs.gov","middleInitial":"D.","affiliations":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"preferred":true,"id":699589,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Blakeslee, Carrie J. 0000-0002-0801-5325 cblakeslee@usgs.gov","orcid":"https://orcid.org/0000-0002-0801-5325","contributorId":5462,"corporation":false,"usgs":true,"family":"Blakeslee","given":"Carrie","email":"cblakeslee@usgs.gov","middleInitial":"J.","affiliations":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"preferred":true,"id":699588,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"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":365,"text":"Leetown Science Center","active":true,"usgs":true},{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":true,"id":699585,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70188723,"text":"70188723 - 2017 - Can we save large carnivores without losing large carnivore science?","interactions":[],"lastModifiedDate":"2017-09-25T13:57:04","indexId":"70188723","displayToPublicDate":"2017-06-22T00:00:00","publicationYear":"2017","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5453,"text":"Food Webs","active":true,"publicationSubtype":{"id":10}},"title":"Can we save large carnivores without losing large carnivore science?","docAbstract":"<p><span>Large carnivores are depicted to shape entire ecosystems through top-down processes. Studies describing these processes are often used to support interventionist wildlife management practices, including carnivore reintroduction or lethal control programs. Unfortunately, there is an increasing tendency to ignore, disregard or devalue fundamental principles of the scientific method when communicating the reliability of current evidence for the ecological roles that large carnivores may play, eroding public confidence in large carnivore science and scientists. Here, we discuss six interrelated issues that currently undermine the reliability of the available literature on the ecological roles of large carnivores: (1) the overall paucity of available data, (2) reliability of carnivore population sampling techniques, (3) general disregard for alternative hypotheses to top-down forcing, (4) lack of applied science studies, (5) frequent use of logical fallacies, and (6) generalisation of results from relatively pristine systems to those substantially altered by humans. We first describe how widespread these issues are, and given this, show, for example, that evidence for the roles of wolves (</span><i>Canis lupus</i><span>) and dingoes (</span><i>Canis lupus dingo</i><span>) in initiating trophic cascades is not as strong as is often claimed. Managers and policy makers should exercise caution when relying on this literature to inform wildlife management decisions. We emphasise the value of manipulative experiments and discuss the role of scientific knowledge in the decision-making process. We hope that the issues we raise here prompt deeper consideration of actual evidence, leading towards an improvement in both the rigour and communication of large carnivore science.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.fooweb.2017.02.008","usgsCitation":"Allen, B.L., Allen, L.R., Andren, H., Ballard, G., Boitani, L., Engeman, R., Fleming, P.J., Haswell, P.M., Ford, A.T., Kowalczyk, R., Linnell, J., Mech, L.D., and Parker, D.M., 2017, Can we save large carnivores without losing large carnivore science?: Food Webs, v. 12, p. 64-75, https://doi.org/10.1016/j.fooweb.2017.02.008.","productDescription":"12 p.","startPage":"64","endPage":"75","ipdsId":"IP-081591","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":469738,"rank":0,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://research.bangor.ac.uk/portal/en/researchoutputs/can-we-save-large-carnivores-without-losing-large-carnivore-science(99119441-5301-469d-a9fd-bd132f9067df).html","text":"External Repository"},{"id":342755,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"12","publishingServiceCenter":{"id":4,"text":"Rolla PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"594cd73de4b062508e3951c5","contributors":{"authors":[{"text":"Allen, Benjamin L.","contributorId":193210,"corporation":false,"usgs":false,"family":"Allen","given":"Benjamin","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":699220,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Allen, Lee R.","contributorId":193219,"corporation":false,"usgs":false,"family":"Allen","given":"Lee","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":699266,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Andren, Henrik","contributorId":193220,"corporation":false,"usgs":false,"family":"Andren","given":"Henrik","email":"","affiliations":[],"preferred":false,"id":699267,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ballard, Guy","contributorId":193221,"corporation":false,"usgs":false,"family":"Ballard","given":"Guy","email":"","affiliations":[],"preferred":false,"id":699268,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Boitani, Luigi","contributorId":193211,"corporation":false,"usgs":false,"family":"Boitani","given":"Luigi","email":"","affiliations":[],"preferred":false,"id":699221,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Engeman, Richard M.","contributorId":39301,"corporation":false,"usgs":true,"family":"Engeman","given":"Richard M.","affiliations":[],"preferred":false,"id":699269,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Fleming, Peter J.S.","contributorId":193222,"corporation":false,"usgs":false,"family":"Fleming","given":"Peter","email":"","middleInitial":"J.S.","affiliations":[],"preferred":false,"id":699270,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Haswell, Peter M.","contributorId":193224,"corporation":false,"usgs":false,"family":"Haswell","given":"Peter","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":699274,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Ford, Adam T.","contributorId":193223,"corporation":false,"usgs":false,"family":"Ford","given":"Adam","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":699271,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Kowalczyk, Rafal","contributorId":193212,"corporation":false,"usgs":false,"family":"Kowalczyk","given":"Rafal","email":"","affiliations":[],"preferred":false,"id":699272,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Mech, L. David 0000-0003-3944-7769 david_mech@usgs.gov","orcid":"https://orcid.org/0000-0003-3944-7769","contributorId":2518,"corporation":false,"usgs":true,"family":"Mech","given":"L.","email":"david_mech@usgs.gov","middleInitial":"David","affiliations":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"preferred":true,"id":699219,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Linnell, John","contributorId":193225,"corporation":false,"usgs":false,"family":"Linnell","given":"John","email":"","affiliations":[],"preferred":false,"id":699273,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Parker, Daniel M.","contributorId":193226,"corporation":false,"usgs":false,"family":"Parker","given":"Daniel","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":699275,"contributorType":{"id":1,"text":"Authors"},"rank":13}]}}
,{"id":70188711,"text":"70188711 - 2017 - Influence of lithostatic stress on earthquake stress drops in North America","interactions":[],"lastModifiedDate":"2017-06-22T09:57:57","indexId":"70188711","displayToPublicDate":"2017-06-22T00:00:00","publicationYear":"2017","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1135,"text":"Bulletin of the Seismological Society of America","onlineIssn":"1943-3573","printIssn":"0037-1106","active":true,"publicationSubtype":{"id":10}},"title":"Influence of lithostatic stress on earthquake stress drops in North America","docAbstract":"<p><span>We estimate stress drops for earthquakes in and near the continental United States using the method of spectral ratios. The ratio of acceleration spectra between collocated earthquakes recorded at a given station removes the effects of path and recording site and yields source parameters including corner frequency for, and the ratio of seismic moment between, the two earthquakes. We determine stress drop from these parameters for 1121 earthquakes greater than </span><i>M</i><span>∼3 in 60 earthquake clusters. We find that the average Brune stress drop for the few eastern United States (EUS) tectonic mainshocks studied (2.6–36&nbsp;MPa) is about three times greater than that of tectonic mainshocks in the western United States (WUS, 1.0–7.9&nbsp;MPa) and five times greater than mainshocks potentially induced by wastewater injection in the central United States (CUS, 0.6–5.6&nbsp;MPa). EUS events tend to be deeper thrusting events, whereas WUS events tend to be shallower but have a wide range of focal mechanisms. CUS events tend to be shallow with strike‐slip to normal‐faulting mechanisms. With the possible exception of CUS aftershocks, we find that differences in stress drop among all events can be taken into account, within one standard deviation of significance, by differences in the shear failure stress as outlined by Mohr–Coulomb theory. The shear failure stress is a function of vertical stress (or depth), the fault style (normal, strike slip, or reverse), and coefficient of friction (estimated here to be, on average, 0.64). After accounting for faulting style and depth dependence, we find that the average Brune stress drop is about 3% of the failure stress. These results suggest that high‐frequency shaking hazard (&gt;∼1  Hz) from shallow induced events and aftershocks is reduced to some extent by lower stress drop. However, the shallow hypocenters will increase hazard within several kilometers of the source.</span></p>","language":"English","publisher":"Seismological Society of America","doi":"10.1785/0120160219","usgsCitation":"Boyd, O.S., McNamara, D.E., Hartzell, S.H., and Choy, G., 2017, Influence of lithostatic stress on earthquake stress drops in North America: Bulletin of the Seismological Society of America, v. 107, no. 2, p. 856-868, https://doi.org/10.1785/0120160219.","productDescription":"13 p.","startPage":"856","endPage":"868","ipdsId":"IP-077193","costCenters":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"links":[{"id":342746,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United 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States\"}}]}","volume":"107","issue":"2","publishingServiceCenter":{"id":2,"text":"Denver PSC"},"noUsgsAuthors":false,"publicationDate":"2017-02-21","publicationStatus":"PW","scienceBaseUri":"594cd73ee4b062508e3951cb","contributors":{"authors":[{"text":"Boyd, Oliver S. 0000-0001-9457-0407 olboyd@usgs.gov","orcid":"https://orcid.org/0000-0001-9457-0407","contributorId":140739,"corporation":false,"usgs":true,"family":"Boyd","given":"Oliver","email":"olboyd@usgs.gov","middleInitial":"S.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true},{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true},{"id":234,"text":"Earthquake Hazards Program","active":true,"usgs":true}],"preferred":true,"id":698985,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McNamara, Daniel E. 0000-0001-6860-0350 mcnamara@usgs.gov","orcid":"https://orcid.org/0000-0001-6860-0350","contributorId":402,"corporation":false,"usgs":true,"family":"McNamara","given":"Daniel","email":"mcnamara@usgs.gov","middleInitial":"E.","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":true,"id":698986,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hartzell, Stephen H. 0000-0003-0858-9043 shartzell@usgs.gov","orcid":"https://orcid.org/0000-0003-0858-9043","contributorId":2594,"corporation":false,"usgs":true,"family":"Hartzell","given":"Stephen","email":"shartzell@usgs.gov","middleInitial":"H.","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":true,"id":698987,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Choy, George choy@usgs.gov","contributorId":2161,"corporation":false,"usgs":true,"family":"Choy","given":"George","email":"choy@usgs.gov","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":true,"id":698988,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70208289,"text":"70208289 - 2017 - Towards a planetary spatial data infrastructure","interactions":[],"lastModifiedDate":"2020-02-04T06:32:09","indexId":"70208289","displayToPublicDate":"2017-06-21T10:24:47","publicationYear":"2017","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5685,"text":"ISPRS International Journal of Geo-Information ","printIssn":"2220-9964","active":true,"publicationSubtype":{"id":10}},"title":"Towards a planetary spatial data infrastructure","docAbstract":"<p><span>Planetary science is the study of planets, moons, irregular bodies such as asteroids and the processes that create and modify them. Like terrestrial sciences, planetary science research is heavily dependent on collecting, processing and archiving large quantities of spatial data to support a range of activities. To address the complexity of storing, discovering, accessing, and utilizing spatial data, the terrestrial research community has developed conceptual Spatial Data Infrastructure (SDI) models and cyberinfrastructures. The needs that these systems seek to address for terrestrial spatial data users are similar to the needs of the planetary science community: spatial data should just work for the non-spatial expert. Here we discuss a path towards a Planetary Spatial Data Infrastructure (PSDI) solution that fulfills this primary need. We first explore the linkage between SDI models and cyberinfrastructures, then describe the gaps in current PSDI concepts, and discuss the overlap between terrestrial SDIs and a new, conceptual PSDI that best serves the needs of the planetary science community.</span></p>","language":"English","publisher":"MDPI","doi":"10.3390/ijgi6060181","usgsCitation":"Laura, J., Hare, T.M., Gaddis, L.R., Fergason, R.L., Skinner, Hagerty, J., and Archinal, B., 2017, Towards a planetary spatial data infrastructure: ISPRS International Journal of Geo-Information , v. 6, no. 6, 181, 18 p., https://doi.org/10.3390/ijgi6060181.","productDescription":"181, 18 p.","ipdsId":"IP-087170","costCenters":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"links":[{"id":469739,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.3390/ijgi6060181","text":"Publisher Index Page"},{"id":371916,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"6","issue":"6","publishingServiceCenter":{"id":14,"text":"Menlo Park PSC"},"noUsgsAuthors":false,"publicationDate":"2017-06-21","publicationStatus":"PW","contributors":{"authors":[{"text":"Laura, Jason 0000-0002-1377-8159","orcid":"https://orcid.org/0000-0002-1377-8159","contributorId":222124,"corporation":false,"usgs":true,"family":"Laura","given":"Jason","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":true,"id":781270,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hare, Trent M. 0000-0001-8842-389X thare@usgs.gov","orcid":"https://orcid.org/0000-0001-8842-389X","contributorId":3188,"corporation":false,"usgs":true,"family":"Hare","given":"Trent","email":"thare@usgs.gov","middleInitial":"M.","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":true,"id":781271,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gaddis, Lisa R. 0000-0001-9953-5483 lgaddis@usgs.gov","orcid":"https://orcid.org/0000-0001-9953-5483","contributorId":2817,"corporation":false,"usgs":true,"family":"Gaddis","given":"Lisa","email":"lgaddis@usgs.gov","middleInitial":"R.","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":true,"id":781272,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Fergason, Robin L. 0000-0002-2044-1714","orcid":"https://orcid.org/0000-0002-2044-1714","contributorId":206167,"corporation":false,"usgs":true,"family":"Fergason","given":"Robin","email":"","middleInitial":"L.","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":true,"id":781273,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Skinner, Jr. 0000-0002-3644-7010","orcid":"https://orcid.org/0000-0002-3644-7010","contributorId":222125,"corporation":false,"usgs":true,"family":"Skinner","suffix":"Jr.","email":"","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":true,"id":781274,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Hagerty, Justin 0000-0003-3800-7948 jhagerty@usgs.gov","orcid":"https://orcid.org/0000-0003-3800-7948","contributorId":911,"corporation":false,"usgs":true,"family":"Hagerty","given":"Justin","email":"jhagerty@usgs.gov","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":true,"id":781275,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Archinal, Brent A. 0000-0002-6654-0742","orcid":"https://orcid.org/0000-0002-6654-0742","contributorId":206341,"corporation":false,"usgs":true,"family":"Archinal","given":"Brent A.","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":true,"id":781276,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70188658,"text":"70188658 - 2017 - Younger-Dryas cooling and sea-ice feedbacks were prominent features of the Pleistocene-Holocene transition in Arctic Alaska","interactions":[],"lastModifiedDate":"2019-12-19T15:15:21","indexId":"70188658","displayToPublicDate":"2017-06-21T00:00:00","publicationYear":"2017","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3219,"text":"Quaternary Science Reviews","active":true,"publicationSubtype":{"id":10}},"title":"Younger-Dryas cooling and sea-ice feedbacks were prominent features of the Pleistocene-Holocene transition in Arctic Alaska","docAbstract":"<p><span>Declining sea-ice extent is currently amplifying climate warming in the Arctic. Instrumental records at high latitudes are too short-term to provide sufficient historical context for these trends, so paleoclimate archives are needed to better understand the functioning of the sea ice-albedo feedback. Here we use the oxygen isotope values of wood cellulose in living and sub-fossil willow shrubs (δ</span><sup>18</sup><span>O</span><sub>wc</sub><span>) (</span><i>Salix</i><span> spp.) that have been radiocarbon-dated (</span><sup>14</sup><span>C) to produce a multi-millennial record of climatic change on Alaska's North Slope during the Pleistocene-Holocene transition (13,500–7500 calibrated </span><sup>14</sup><span>C years before present; 13.5–7.5 ka). We first analyzed the spatial and temporal patterns of δ</span><sup>18</sup><span>O</span><sub>wc</sub><span> in living willows growing at upland sites and found that over the last 30 years δ</span><sup>18</sup><span>O</span><sub>wc</sub><span> values in individual growth rings correlate with local summer temperature and inter-annual variations in summer sea-ice extent. Deglacial δ</span><sup>18</sup><span>O</span><sub>wc</sub><span>values from 145 samples of subfossil willows clearly record the Allerød warm period (∼13.2 ka), the Younger Dryas cold period (12.9–11.7 ka), and the Holocene Thermal Maximum (11.7–9.0 ka). The magnitudes of isotopic changes over these rapid climate oscillations were ∼4.5‰, which is about 60% of the differences in δ</span><sup>18</sup><span>O</span><sub>wc</sub><span> between those willows growing during the last glacial period and today. Modeling of isotope-precipitation relationships based on Rayleigh distillation processes suggests that during the Younger Dryas these large shifts in δ</span><sup>18</sup><span>O</span><sub>wc</sub><span> values were caused by interactions between local temperature and changes in evaporative moisture sources, the latter controlled by seaice extent in the Arctic Ocean and Bering Sea. Based on these results and on the effects that sea-ice have on climate today, we infer that ocean-derived feedbacks amplified temperature changes and enhanced precipitation in coastal regions of Arctic Alaska during warm times in the past. Today, isotope values in willows on the North Slope of Alaska are similar to those growing during the warmest times of the Pleistocene-Holocene transition, which were times of widespread permafrost thaw and striking ecological changes.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.quascirev.2017.05.012","usgsCitation":"Gaglioti, B.V., Mann, D.H., Wooller, M.J., Jones, B.M., Wiles, G.C., Groves, P., Kunz, M.L., Baughman, C., and Reanier, R.E., 2017, Younger-Dryas cooling and sea-ice feedbacks were prominent features of the Pleistocene-Holocene transition in Arctic Alaska: Quaternary Science Reviews, v. 169, p. 330-343, https://doi.org/10.1016/j.quascirev.2017.05.012.","productDescription":"14 p.","startPage":"330","endPage":"343","ipdsId":"IP-084358","costCenters":[{"id":118,"text":"Alaska Science Center Geography","active":true,"usgs":true}],"links":[{"id":469740,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1016/j.quascirev.2017.05.012","text":"Publisher Index Page"},{"id":342699,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -164.1796875,\n              67.33986082559095\n            ],\n            [\n              -142.03125,\n              67.33986082559095\n            ],\n            [\n              -142.03125,\n              71.63599288330609\n            ],\n            [\n              -164.1796875,\n              71.63599288330609\n            ],\n            [\n              -164.1796875,\n              67.33986082559095\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"169","publishingServiceCenter":{"id":12,"text":"Tacoma PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"594b85b2e4b062508e382b70","contributors":{"authors":[{"text":"Gaglioti, Benjamin V. 0000-0003-0591-5253 bgaglioti@usgs.gov","orcid":"https://orcid.org/0000-0003-0591-5253","contributorId":4521,"corporation":false,"usgs":true,"family":"Gaglioti","given":"Benjamin","email":"bgaglioti@usgs.gov","middleInitial":"V.","affiliations":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":118,"text":"Alaska Science Center Geography","active":true,"usgs":true}],"preferred":true,"id":698793,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mann, Daniel H.","contributorId":67010,"corporation":false,"usgs":true,"family":"Mann","given":"Daniel","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":698794,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wooller, Matthew J.","contributorId":192799,"corporation":false,"usgs":false,"family":"Wooller","given":"Matthew","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":698795,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Jones, Benjamin M. 0000-0002-1517-4711 bjones@usgs.gov","orcid":"https://orcid.org/0000-0002-1517-4711","contributorId":2286,"corporation":false,"usgs":true,"family":"Jones","given":"Benjamin","email":"bjones@usgs.gov","middleInitial":"M.","affiliations":[{"id":118,"text":"Alaska Science Center Geography","active":true,"usgs":true},{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"preferred":true,"id":698792,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Wiles, Gregory C.","contributorId":39278,"corporation":false,"usgs":true,"family":"Wiles","given":"Gregory","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":698796,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Groves, Pamela","contributorId":193132,"corporation":false,"usgs":false,"family":"Groves","given":"Pamela","email":"","affiliations":[],"preferred":false,"id":698797,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Kunz, Michael L.","contributorId":42157,"corporation":false,"usgs":true,"family":"Kunz","given":"Michael","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":698798,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Baughman, Carson 0000-0002-9423-9324 cbaughman@usgs.gov","orcid":"https://orcid.org/0000-0002-9423-9324","contributorId":169657,"corporation":false,"usgs":true,"family":"Baughman","given":"Carson","email":"cbaughman@usgs.gov","affiliations":[{"id":118,"text":"Alaska Science Center Geography","active":true,"usgs":true}],"preferred":true,"id":698799,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Reanier, Richard E.","contributorId":77850,"corporation":false,"usgs":true,"family":"Reanier","given":"Richard","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":698800,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}}
,{"id":70190131,"text":"70190131 - 2017 - Challenges in recovering resources from acid mine drainage","interactions":[],"lastModifiedDate":"2024-01-24T14:15:25.772446","indexId":"70190131","displayToPublicDate":"2017-06-21T00:00:00","publicationYear":"2017","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Challenges in recovering resources from acid mine drainage","docAbstract":"<p>Metal recovery from mine waters and effluents is not a new approach but one that has occurred largely opportunistically over the last four millennia. Due to the need for low-cost resources and increasingly stringent environmental conditions, mine waters are being considered in a fresh light with a designed, deliberate approach to resource recovery often as part of a larger water treatment evaluation. Mine water chemistry is highly dependent on many factors including geology, ore deposit composition and mineralogy, mining methods, climate, site hydrology, and others. Mine waters are typically Ca-Mg-SO4±Al±Fe with a broad range in pH and metal content. The main issue in recovering components of these waters having potential economic value, such as base metals or rare earth elements, is the separation of these from more reactive metals such as Fe and Al. Broad categories of methods for separating and extracting substances from acidic mine drainage are chemical and biological. Chemical methods include solution, physicochemical, and electrochemical technologies. Advances in membrane techniques such as reverse osmosis have been substantial and the technique is both physical and chemical. Biological methods may be further divided into microbiological and macrobiological, but only the former is considered here as a recovery method, as the latter is typically used as a passive form of water treatment. </p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Mine water and circular economy","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"IMWA 2017","conferenceDate":"June 25-30, 2017","conferenceLocation":"Lappeenranta, Finland","language":"English","publisher":"International Mine Water Association","usgsCitation":"Nordstrom, D.K., Bowell, R.J., Campbell, K.M., and Alpers, C.N., 2017, Challenges in recovering resources from acid mine drainage, <i>in</i> Mine water and circular economy, Lappeenranta, Finland, June 25-30, 2017, p. 1138-1146.","productDescription":"9 p.","startPage":"1138","endPage":"1146","ipdsId":"IP-086476","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true},{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"links":[{"id":424860,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"http://www.imwa.de/imwaconferencesandcongresses/proceedings/300-proceedings-2017.html","linkFileType":{"id":5,"text":"html"}},{"id":344788,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"publishingServiceCenter":{"id":2,"text":"Denver PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"59b76ee5e4b08b1644ddfad8","contributors":{"authors":[{"text":"Nordstrom, D. Kirk 0000-0003-3283-5136 dkn@usgs.gov","orcid":"https://orcid.org/0000-0003-3283-5136","contributorId":749,"corporation":false,"usgs":true,"family":"Nordstrom","given":"D.","email":"dkn@usgs.gov","middleInitial":"Kirk","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":false,"id":707607,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bowell, Robert J.","contributorId":150175,"corporation":false,"usgs":false,"family":"Bowell","given":"Robert","email":"","middleInitial":"J.","affiliations":[{"id":17927,"text":"SRK Consulting Ltd.","active":true,"usgs":false}],"preferred":false,"id":707608,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Campbell, Kate M. 0000-0002-8715-5544 kcampbell@usgs.gov","orcid":"https://orcid.org/0000-0002-8715-5544","contributorId":1441,"corporation":false,"usgs":true,"family":"Campbell","given":"Kate","email":"kcampbell@usgs.gov","middleInitial":"M.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":707609,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Alpers, Charles N. 0000-0001-6945-7365 cnalpers@usgs.gov","orcid":"https://orcid.org/0000-0001-6945-7365","contributorId":411,"corporation":false,"usgs":true,"family":"Alpers","given":"Charles","email":"cnalpers@usgs.gov","middleInitial":"N.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":707610,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
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