{"pageNumber":"34","pageRowStart":"825","pageSize":"25","recordCount":11004,"records":[{"id":70238906,"text":"sim3497 - 2022 - Delineating the Pierre Shale from geophysical surveys east and southeast of Ellsworth Air Force Base, South Dakota, 2021","interactions":[],"lastModifiedDate":"2026-04-01T15:30:56.71177","indexId":"sim3497","displayToPublicDate":"2022-12-19T07:51:11","publicationYear":"2022","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":333,"text":"Scientific Investigations Map","code":"SIM","onlineIssn":"2329-132X","printIssn":"2329-1311","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"3497","displayTitle":"Delineating the Pierre Shale from Geophysical Surveys East and Southeast of Ellsworth Air Force Base, South Dakota, 2021","title":"Delineating the Pierre Shale from geophysical surveys east and southeast of Ellsworth Air Force Base, South Dakota, 2021","docAbstract":"<p>The U.S. Geological Survey, in cooperation with the U.S. Air Force Civil Engineer Center, used surface-geophysical methods to delineate the top of Cretaceous Pierre Shale along survey transects in selected areas east and southeast of Ellsworth Air Force Base, South Dakota, from April to September 2021. Two complementary geophysical methods—electrical resistivity and passive seismic—were used along 21 colocated transect surveys east and southeast of Ellsworth Air Force Base for a total of 24.7 line-kilometers. Electrical resistivity results were analyzed using EarthImager2D electrical resistivity tomography processing and inversion software. Two-dimensional earth models showing the electrical properties of the subsurface were evaluated by directly comparing the high and low subsurface resistivity values to a surficial-geologic map and nearby wells with drillers logs. Passive seismic data were analyzed using the horizontal-to-vertical spectral ratio method to determine the depth to the Cretaceous Pierre Shale at each survey point. The depth to the Pierre Shale along the transects ranged from 0.0 to about 19.8 meters, and the mean and median depths were about 6.1 and 5.6 meters, respectively. The elevation of the Pierre Shale and thickness of unconsolidated deposits generally increased with land-surface elevation from south to north; however, some transects displayed topographically high and low areas that did not correlate with land-surface topography.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sim3497","collaboration":"Prepared in cooperation with the U.S. Air Force Civil Engineer Center","usgsCitation":"Medler, C.J., 2022, Delineating the Pierre Shale from geophysical surveys east and southeast of Ellsworth Air Force Base, South Dakota, 2021: U.S. Geological Survey Scientific Investigations Map 3497, 3 sheets, 15-p. pamphlet, https://doi.org/10.3133/sim3497.","productDescription":"Report: vi, 15 p.; 3 Sheets:  64.00 × 53.33 inches or smaller; Data Release","numberOfPages":"24","onlineOnly":"Y","additionalOnlineFiles":"Y","ipdsId":"IP-137098","costCenters":[{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":501938,"rank":10,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_113997.htm","linkFileType":{"id":5,"text":"html"}},{"id":410625,"rank":7,"type":{"id":26,"text":"Sheet"},"url":"https://pubs.usgs.gov/sim/3497/sim3497_sheet03.pdf","text":"Sheet 3","size":"16.7 MB","linkFileType":{"id":1,"text":"pdf"},"description":"SIM 3497, sheet 3","linkHelpText":"—Depth to Pierre Shale from Electrical Resistivity Tomography Inversion and Horizontal-to-Vertical Spectral Ratio Results for Transects 4A, 4B, 4D, 4E, 4FD3, 4FD4, 4FD5, 4G, 4H, and 5, Ellsworth Air Force Base, South Dakota"},{"id":410609,"rank":6,"type":{"id":26,"text":"Sheet"},"url":"https://pubs.usgs.gov/sim/3497/sim3497_sheet02.pdf","text":"Sheet 2","size":"14.9 MB","linkFileType":{"id":1,"text":"pdf"},"description":"SIM 3497, sheet 2","linkHelpText":"—Depth to Pierre Shale from Electrical Resistivity Tomography Inversion and Horizontal-to-Vertical Spectral Ratio Results for Transects 2, 3A, 3B, 3D, 3E, and 3F, Ellsworth Air Force Base, South Dakota"},{"id":410608,"rank":5,"type":{"id":26,"text":"Sheet"},"url":"https://pubs.usgs.gov/sim/3497/sim3497_sheet01.pdf","text":"Sheet 1","size":"16.5 MB","linkFileType":{"id":1,"text":"pdf"},"description":"SIM 3497, sheet 1","linkHelpText":"—Depth to Pierre Shale from Electrical Resistivity Tomography Inversion and Horizontal-to-Vertical Spectral Ratio Results for Transects 1A, 1C, 1D, 4F Alternate 1, and 4F Alternate 2, Ellsworth Air Force Base, South Dakota"},{"id":410607,"rank":4,"type":{"id":34,"text":"Image Folder"},"url":"https://pubs.usgs.gov/sim/3497/images"},{"id":410606,"rank":3,"type":{"id":31,"text":"Publication XML"},"url":"https://pubs.usgs.gov/sim/3497/sim3497.XML"},{"id":410605,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/sim/3497/sim3497.pdf","text":"Report","size":"8.72 MB","linkFileType":{"id":1,"text":"pdf"},"description":"SIM 3497"},{"id":410604,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/sim/3497/coverthb.jpg"},{"id":410698,"rank":9,"type":{"id":39,"text":"HTML Document"},"url":"https://pubs.usgs.gov/publication/sim3497/full","text":"Report","linkFileType":{"id":5,"text":"html"}},{"id":410626,"rank":8,"type":{"id":30,"text":"Data Release"},"url":"https://doi.org/10.5066/P9X57BS0","text":"USGS data release","linkHelpText":"Electrical resistivity tomography (ERT) and horizontal-to-vertical spectral ratio (HVSR) data collected East and Southeast of Ellsworth Air Force Base, South Dakota, in 2021"}],"country":"United States","state":"South Dakota","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -103.08,\n              44.06\n            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Results</li><li>Summary</li><li>References Cited</li></ul>","publishingServiceCenter":{"id":4,"text":"Rolla PSC"},"publishedDate":"2022-12-19","noUsgsAuthors":false,"publicationDate":"2022-12-19","publicationStatus":"PW","contributors":{"authors":[{"text":"Medler, Colton J. 0000-0001-6119-5065","orcid":"https://orcid.org/0000-0001-6119-5065","contributorId":201463,"corporation":false,"usgs":true,"family":"Medler","given":"Colton","email":"","middleInitial":"J.","affiliations":[{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"preferred":true,"id":859116,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70238949,"text":"70238949 - 2022 - Insights from the Alabama Hills into Mesozoic magmatism and tectonics in eastern California","interactions":[],"lastModifiedDate":"2022-12-19T15:24:47.46453","indexId":"70238949","displayToPublicDate":"2022-12-15T09:24:38","publicationYear":"2022","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2626,"text":"Lithosphere","active":true,"publicationSubtype":{"id":10}},"title":"Insights from the Alabama Hills into Mesozoic magmatism and tectonics in eastern California","docAbstract":"<p><span>New zircon U-Pb ages for the Alabama Hills Granite in Owens Valley, eastern California, range from 103 to 102 Ma, nearly 20 Ma older than previously published zircon ages. The data preclude previously implied links between the pluton and the adjacent Late Cretaceous Mount Whitney Intrusive Suite. Geochronologic and isotopic data indicate a connection between the Alabama Hills Granite and leucogranites to the northwest on the Sierra Nevada crest, as well as a pluton to the southeast in the Coso Range. We refer to these units as the Kearsarge plutons. The suite was intruded from 103 to 100.5 Ma with <sup><span class=\"inline-formula no-formula-id\"><span id=\"MathJax-Element-1-Frame\" class=\"MathJax\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;><mmultiscripts xmlns=&quot;&quot;><mrow><mtext>S</mtext></mrow><mprescripts /><none /><mrow><mn>87</mn></mrow></mmultiscripts><mtext xmlns=&quot;&quot;>r</mtext><mo xmlns=&quot;&quot;>/</mo><mmultiscripts xmlns=&quot;&quot;><mrow><mtext>S</mtext></mrow><mprescripts /><none /><mrow><mn>86</mn></mrow></mmultiscripts><msub xmlns=&quot;&quot;><mrow><mtext>r</mtext></mrow><mrow><mtext>i</mtext></mrow></msub><mo xmlns=&quot;&quot;>=</mo><mn xmlns=&quot;&quot;>0.7045</mn></math>\"><span id=\"MathJax-Span-1\" class=\"math\"><span id=\"MathJax-Span-2\" class=\"mrow\"><span id=\"MathJax-Span-3\" class=\"mmultiscripts\"><span id=\"MathJax-Span-6\" class=\"mrow\"><span id=\"MathJax-Span-7\" class=\"mn\">87</span></span></span></span></span></span></span></sup></span><span class=\"inline-formula no-formula-id\"><span id=\"MathJax-Element-1-Frame\" class=\"MathJax\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;><mmultiscripts xmlns=&quot;&quot;><mrow><mtext>S</mtext></mrow><mprescripts /><none /><mrow><mn>87</mn></mrow></mmultiscripts><mtext xmlns=&quot;&quot;>r</mtext><mo xmlns=&quot;&quot;>/</mo><mmultiscripts xmlns=&quot;&quot;><mrow><mtext>S</mtext></mrow><mprescripts /><none /><mrow><mn>86</mn></mrow></mmultiscripts><msub xmlns=&quot;&quot;><mrow><mtext>r</mtext></mrow><mrow><mtext>i</mtext></mrow></msub><mo xmlns=&quot;&quot;>=</mo><mn xmlns=&quot;&quot;>0.7045</mn></math>\"><span id=\"MathJax-Span-1\" class=\"math\"><span><span id=\"MathJax-Span-2\" class=\"mrow\"><span id=\"MathJax-Span-3\" class=\"mmultiscripts\"><span id=\"MathJax-Span-4\" class=\"mrow\"><span id=\"MathJax-Span-5\" class=\"mtext\">S</span></span></span><span id=\"MathJax-Span-8\" class=\"mtext\">r</span><span id=\"MathJax-Span-9\" class=\"mo\">/<sup><span id=\"MathJax-Span-10\" class=\"mmultiscripts\"><span id=\"MathJax-Span-13\" class=\"mrow\"><span id=\"MathJax-Span-14\" class=\"mn\">86</span></span></span></sup></span><span id=\"MathJax-Span-10\" class=\"mmultiscripts\"><span id=\"MathJax-Span-11\" class=\"mrow\"><span id=\"MathJax-Span-12\" class=\"mtext\">S</span></span></span><span id=\"MathJax-Span-15\" class=\"msub\"><span id=\"MathJax-Span-16\" class=\"mrow\"><span id=\"MathJax-Span-17\" class=\"mtext\">r</span></span><span id=\"MathJax-Span-18\" class=\"mrow\"><span id=\"MathJax-Span-19\" class=\"mtext\">i</span></span></span><span id=\"MathJax-Span-20\" class=\"mo\">=</span><span id=\"MathJax-Span-21\" class=\"mn\">0.7045 </span></span></span></span></span></span><span>to 0.7060 and&nbsp;</span><span class=\"inline-formula no-formula-id\"><span id=\"MathJax-Element-2-Frame\" class=\"MathJax\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;><mi xmlns=&quot;&quot;>&amp;#x3B5;</mi><mtext xmlns=&quot;&quot;>N</mtext><msub xmlns=&quot;&quot;><mrow><mtext>d</mtext></mrow><mrow><mi>i</mi></mrow></msub><mo xmlns=&quot;&quot;>=</mo><mo xmlns=&quot;&quot;>&amp;#x2212;</mo><mn xmlns=&quot;&quot;>2.4</mn></math>\"><span id=\"MathJax-Span-22\" class=\"math\"><span><span id=\"MathJax-Span-23\" class=\"mrow\"><i><span id=\"MathJax-Span-24\" class=\"mi\">ε</span></i><span id=\"MathJax-Span-25\" class=\"mtext\">N</span><span id=\"MathJax-Span-26\" class=\"msub\"><span id=\"MathJax-Span-27\" class=\"mrow\"><span id=\"MathJax-Span-28\" class=\"mtext\">d</span></span><sub><i><span id=\"MathJax-Span-29\" class=\"mrow\"><span id=\"MathJax-Span-30\" class=\"mi\">i</span></span></i></sub></span><span id=\"MathJax-Span-31\" class=\"mo\">=</span><span id=\"MathJax-Span-32\" class=\"mo\">−</span><span id=\"MathJax-Span-33\" class=\"mn\">2.4</span></span></span></span></span></span><span>&nbsp;to -4.5 and has distinctive enrichments in high field strength, middle, and heavy rare earth elements, as well as negative Eu anomalies and high Y/Sr. We suggest the Alabama Hills block could not have moved more than 10 km dextrally relative to the Sierra Nevada batholith since the Middle Jurassic and is thus a suitable piercing point for offsets across Owens Valley. The Kearsarge plutons, like other markers on either side of Owens Valley, support approximately 65–75 km of dextral offset across the valley. The suite’s location east of other middle Cretaceous suites, coupled with its mantle-like isotope geochemistry, suggests it could represent backarc magmatism, perhaps controlled by preexisting shear zones or fractures.</span></p>","language":"English","publisher":"GeoScienceWorld","doi":"10.2113/2022/5511120","usgsCitation":"Frazer, R.E., Gaynor, S., Coleman, D., and Wenner, J.M., 2022, Insights from the Alabama Hills into Mesozoic magmatism and tectonics in eastern California: Lithosphere, v. 2022, no. 1, 5511120, 20 p., https://doi.org/10.2113/2022/5511120.","productDescription":"5511120, 20 p.","ipdsId":"IP-140862","costCenters":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"links":[{"id":445659,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.2113/2022/5511120","text":"Publisher Index Page"},{"id":410711,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -119.42366767471628,\n              37.07136849579855\n            ],\n            [\n              -119.42366767471628,\n              35.92292425269048\n            ],\n            [\n              -118.05220813858858,\n              35.92292425269048\n            ],\n            [\n              -118.05220813858858,\n              37.07136849579855\n            ],\n            [\n              -119.42366767471628,\n              37.07136849579855\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"2022","issue":"1","noUsgsAuthors":false,"publicationDate":"2022-12-15","publicationStatus":"PW","contributors":{"authors":[{"text":"Frazer, Ryan Edward 0000-0002-7319-1894","orcid":"https://orcid.org/0000-0002-7319-1894","contributorId":297924,"corporation":false,"usgs":true,"family":"Frazer","given":"Ryan","email":"","middleInitial":"Edward","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":859322,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gaynor, Sean P.","contributorId":297927,"corporation":false,"usgs":false,"family":"Gaynor","given":"Sean P.","affiliations":[],"preferred":false,"id":859323,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Coleman, Drew S.","contributorId":297928,"corporation":false,"usgs":false,"family":"Coleman","given":"Drew S.","affiliations":[],"preferred":false,"id":859324,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Wenner, Jennifer M. 0000-0003-3870-6909","orcid":"https://orcid.org/0000-0003-3870-6909","contributorId":300045,"corporation":false,"usgs":false,"family":"Wenner","given":"Jennifer","email":"","middleInitial":"M.","affiliations":[{"id":65005,"text":"University of Wisconsin Oshkosh","active":true,"usgs":false}],"preferred":false,"id":859325,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70238835,"text":"70238835 - 2022 - Effects of shading on the rare plant species, Physostegia correllii (Lamiaceae) and Trillium texanum (Melanthiaceae)","interactions":[],"lastModifiedDate":"2023-03-28T15:21:45.056918","indexId":"70238835","displayToPublicDate":"2022-12-14T08:34:01","publicationYear":"2022","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2535,"text":"Journal of the Botanical Research Institute of Texas","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Effects of shading on the rare plant species, <i>Physostegia correllii</i> (Lamiaceae) and <i>Trillium texanum</i> (Melanthiaceae)","title":"Effects of shading on the rare plant species, Physostegia correllii (Lamiaceae) and Trillium texanum (Melanthiaceae)","docAbstract":"<p><span>Rare plant species that are constrained by shading may be threatened by a lack of natural disturbance that removes overhanging vegetation. The original distribution of the study species&nbsp;</span><i>Physostegia correllii</i><span>&nbsp;(Lundell) Shinners included freshwater floodplains of large rivers in the southcentral U.S. (Colorado, Rio Grande, and Mississippi rivers). A second species,&nbsp;</span><i>Trillium texanum</i><span>&nbsp;Buckley was found in seep spring baygalls in east-central Texas and extreme northwestern Louisiana. Experiments to determine the effects of shading on&nbsp;</span><i>P. correllii</i><span>&nbsp;and&nbsp;</span><i>T. texanum</i><span>&nbsp;were conducted using short-term shade cloth treatments (full sunlight vs. 30% shading for 2–3 weeks), and a dryness treatment for&nbsp;</span><i>T. texanum</i><span>&nbsp;(moist vs. less moist). Mean height and cover responses of individuals for both species were determined in conservation gardens located in Lafayette, Louisiana.&nbsp;</span><i>Physostegia correllii</i><span>&nbsp;grown in shaded environments for 2.5 weeks had shorter mean height than if grown in full sunlight. Half of the shaded plants in shaded plots had died by the mid-summer. For&nbsp;</span><i>T. texanum,</i><span>&nbsp;shading reduced the mean height and cover of plants. Therefore, management to remove overhanging ground vegetation to mimic natural disturbance might revive&nbsp;</span><i>P. correlli</i><span>i and/or&nbsp;</span><i>T. texanum</i><span>&nbsp;populations where overhanging vegetation is increasing due to lack of natural disturbance (e.g., flood pulsing, grazing, burning).</span></p>","language":"English","publisher":"Botanical Research Institute of Texas","doi":"10.17348/jbrit.v16.i2.1270","usgsCitation":"Middleton, B., Williams, C.R., Doffitt, C., and Johnson, D., 2022, Effects of shading on the rare plant species, Physostegia correllii (Lamiaceae) and Trillium texanum (Melanthiaceae): Journal of the Botanical Research Institute of Texas, v. 16, no. 2, p. 591-603, https://doi.org/10.17348/jbrit.v16.i2.1270.","productDescription":"13 p.; 2 Data Releases","startPage":"591","endPage":"603","ipdsId":"IP-133104","costCenters":[{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"links":[{"id":445669,"rank":4,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.17348/jbrit.v16.i2.1270","text":"Publisher Index Page"},{"id":410472,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":414828,"rank":3,"type":{"id":30,"text":"Data Release"},"url":"https://doi.org/10.5066/P9D28MZ1","linkFileType":{"id":5,"text":"html"}},{"id":414827,"rank":2,"type":{"id":30,"text":"Data Release"},"url":"https://doi.org/10.5066/P95BKVZ3","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Louisiana, Texas","county":"Bexar County, Cameron Parish, Chambers County, Galveston County, Gillespie County, Harris County, Kinney County, Maverick County, Montgomery County, St. Charles Parish, St. James Parish, St. Tammany Parish, Travis County, Val Verde County, Zapata 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Chris","contributorId":258191,"corporation":false,"usgs":false,"family":"Doffitt","given":"Chris","email":"","affiliations":[],"preferred":false,"id":858858,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Johnson, Darren 0000-0002-0502-6045","orcid":"https://orcid.org/0000-0002-0502-6045","contributorId":203921,"corporation":false,"usgs":true,"family":"Johnson","given":"Darren","affiliations":[{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"preferred":true,"id":858859,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70243187,"text":"70243187 - 2022 - Quantifying permanent uplift due to lithosphere-hotspot interaction","interactions":[],"lastModifiedDate":"2023-05-03T11:51:00.692258","indexId":"70243187","displayToPublicDate":"2022-12-08T06:48:03","publicationYear":"2022","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3524,"text":"Tectonics","active":true,"publicationSubtype":{"id":10}},"title":"Quantifying permanent uplift due to lithosphere-hotspot interaction","docAbstract":"<div class=\"article-section__content en main\"><p>Vertical motions that accompany the passage of the lithosphere over a mantle hotspot can shed light on the nature of the hotspot and its effect on the lithosphere. However, quantifying the temporal vertical and spatial extent, is challenging due to the paucity of evidence in the geological record. Here, we utilize dense seismic and well data covering the intersection of the Great Meteor Hotspot (GMH) track with the U.S. Atlantic continental margin to constrain the surface expression of the hotspot passage under the lithosphere. The continuous sedimentary record of the eastern North American margin during its passage over the hotspot allows determination of the timing, magnitude, width and rate of denudation. We find that a ∼300&nbsp;km wide region was denuded by up to 850&nbsp;m between ∼97 and 86&nbsp;Ma, ∼10&nbsp;m.y. after the passage of the GMH. Stratigraphic relationships suggest a decaying rock uplift rate with time and no subsequent sagging. The broad, long-lasting, and delayed uplift was modeled as a surface manifestation of either sub-lithospheric mantle depletion, permanently eroded base of the continental lithosphere, or intrusions of depleted magma. We consider sub-lithospheric depletion to be the most likely cause, based on seismic imaging results.</p></div>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/2022TC007448","usgsCitation":"Lang, G., and ten Brink, U.S., 2022, Quantifying permanent uplift due to lithosphere-hotspot interaction: Tectonics, v. 41, no. 12, e2022TC007448, 16 p., https://doi.org/10.1029/2022TC007448.","productDescription":"e2022TC007448, 16 p.","ipdsId":"IP-138344","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":445696,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1029/2022tc007448","text":"Publisher Index Page"},{"id":416651,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -77.6418461037233,\n              46.41102221638212\n            ],\n            [\n              -77.6418461037233,\n              39.63263170609457\n            ],\n            [\n              -64.1048906255545,\n              39.63263170609457\n            ],\n            [\n              -64.1048906255545,\n              46.41102221638212\n            ],\n            [\n              -77.6418461037233,\n              46.41102221638212\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"41","issue":"12","noUsgsAuthors":false,"publicationDate":"2022-12-24","publicationStatus":"PW","contributors":{"authors":[{"text":"Lang, Guy","contributorId":304702,"corporation":false,"usgs":false,"family":"Lang","given":"Guy","email":"","affiliations":[{"id":66147,"text":"Dept. of Marine Geosciences, University of Haifa","active":true,"usgs":false}],"preferred":false,"id":871409,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"ten Brink, Uri S. 0000-0001-6858-3001","orcid":"https://orcid.org/0000-0001-6858-3001","contributorId":201741,"corporation":false,"usgs":true,"family":"ten Brink","given":"Uri","email":"","middleInitial":"S.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":871410,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70269048,"text":"70269048 - 2022 - The Pondosa fault zone: A distributed dextral-normal-oblique fault system in northeastern California, USA","interactions":[],"lastModifiedDate":"2025-07-15T16:49:27.549522","indexId":"70269048","displayToPublicDate":"2022-12-07T00:00:00","publicationYear":"2022","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1820,"text":"Geosphere","active":true,"publicationSubtype":{"id":10}},"title":"The Pondosa fault zone: A distributed dextral-normal-oblique fault system in northeastern California, USA","docAbstract":"<p><span>The tectonic domains of Basin and Range extension, Cascadia subduction zone contraction, and Walker Lane dextral transtension converge in the Mushroom Rock region of northeastern California, USA. We combined analysis of high-resolution topographic data, bedrock mapping,&nbsp;</span><sup>40</sup><span>Ar/</span><sup>39</sup><span>Ar geochronology, low-temperature thermochronology, and existing geologic and fault mapping to characterize an extensive dextral-normal-oblique fault system called the Pondosa fault zone. This fault zone extends north-northwest from the Pit River east of Soldier Mountain, California, into moderately high-relief volcanic topography as far north as the Bartle (California) townsite with normal and dextral offset apparent in geomorphology and fault exposures. New and existing&nbsp;</span><sup>40</sup><span>Ar/</span><sup>39</sup><span>Ar and radiocarbon dating of offset lava flows provides ages of 12.4 ka to 9.6 Ma for late Cenozoic stratigraphic units. Scarp morphology and geomorphic expression indicate that the fault system was active in the late Pleistocene. The Pondosa fault zone may represent a dextral-oblique accommodation zone between north-south–oriented Basin and Range extensional fault systems and/or part of the Sierra Nevada–Oregon Coast block microplate boundary.</span></p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/GES02450.1","usgsCitation":"Jobe, J.A., Briggs, R.W., Gold, R.D., DeLong, S.B., Hille, M., Delano, J., Johnstone, S., Pickering, A., Phillips, R., and Calvert, A.T., 2022, The Pondosa fault zone: A distributed dextral-normal-oblique fault system in northeastern California, USA: Geosphere, v. 19, no. 1, p. 179-205, https://doi.org/10.1130/GES02450.1.","productDescription":"27 p.","startPage":"179","endPage":"205","ipdsId":"IP-137700","costCenters":[{"id":78686,"text":"Geologic Hazards Science Center - Seismology / Geomagnetism","active":true,"usgs":true}],"links":[{"id":492497,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1130/ges02450.1","text":"Publisher Index Page"},{"id":492284,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"eastern California","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -122.27831636230019,\n              41.12301709043055\n            ],\n            [\n              -122.27831636230019,\n              39.963081252129996\n            ],\n            [\n              -120.53795346715106,\n              39.963081252129996\n            ],\n            [\n              -120.53795346715106,\n              41.12301709043055\n            ],\n            [\n              -122.27831636230019,\n              41.12301709043055\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"19","issue":"1","noUsgsAuthors":false,"publicationDate":"2022-12-07","publicationStatus":"PW","contributors":{"authors":[{"text":"Thompson Jobe, Jessica A. 0000-0001-5574-4523","orcid":"https://orcid.org/0000-0001-5574-4523","contributorId":295377,"corporation":false,"usgs":true,"family":"Thompson Jobe","given":"Jessica","middleInitial":"A.","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":true,"id":943088,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Briggs, Richard W. 0000-0001-8108-0046 rbriggs@usgs.gov","orcid":"https://orcid.org/0000-0001-8108-0046","contributorId":4136,"corporation":false,"usgs":true,"family":"Briggs","given":"Richard","email":"rbriggs@usgs.gov","middleInitial":"W.","affiliations":[{"id":300,"text":"Geologic Hazards Science 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0000-0001-7240-8214","orcid":"https://orcid.org/0000-0001-7240-8214","contributorId":315582,"corporation":false,"usgs":false,"family":"Hille","given":"Madeline","email":"","affiliations":[{"id":37387,"text":"University of Michigan","active":true,"usgs":false}],"preferred":false,"id":943092,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Delano, Jaime 0000-0003-2601-2600","orcid":"https://orcid.org/0000-0003-2601-2600","contributorId":225594,"corporation":false,"usgs":false,"family":"Delano","given":"Jaime","affiliations":[{"id":6605,"text":"USGS","active":true,"usgs":false}],"preferred":false,"id":943093,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Johnstone, Samuel 0000-0002-3945-2499","orcid":"https://orcid.org/0000-0002-3945-2499","contributorId":207545,"corporation":false,"usgs":true,"family":"Johnstone","given":"Samuel","email":"","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true},{"id":35995,"text":"Geology, Geophysics, and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":943094,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Pickering, Alexandra 0000-0002-1281-6117","orcid":"https://orcid.org/0000-0002-1281-6117","contributorId":329929,"corporation":false,"usgs":false,"family":"Pickering","given":"Alexandra","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":false,"id":943095,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Phillips, Rachel","contributorId":341951,"corporation":false,"usgs":false,"family":"Phillips","given":"Rachel","affiliations":[{"id":81813,"text":"Department of Geological Sciences, The University of Texas El Paso, El Paso, TX","active":true,"usgs":false}],"preferred":false,"id":943096,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Calvert, Andrew T. 0000-0001-5237-2218 acalvert@usgs.gov","orcid":"https://orcid.org/0000-0001-5237-2218","contributorId":2694,"corporation":false,"usgs":true,"family":"Calvert","given":"Andrew","email":"acalvert@usgs.gov","middleInitial":"T.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true},{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":943097,"contributorType":{"id":1,"text":"Authors"},"rank":10}]}}
,{"id":70238880,"text":"70238880 - 2022 - GPS data from 2019 and 2020 campaigns in the Chesapeake Bay region towards quantifying vertical land motions","interactions":[],"lastModifiedDate":"2022-12-15T13:54:31.86052","indexId":"70238880","displayToPublicDate":"2022-12-02T07:49:29","publicationYear":"2022","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3907,"text":"Scientific Data","active":true,"publicationSubtype":{"id":10}},"title":"GPS data from 2019 and 2020 campaigns in the Chesapeake Bay region towards quantifying vertical land motions","docAbstract":"<p><span>The Chesapeake Bay is a region along the eastern coast of the United States where sea-level rise is confounded with poorly resolved rates of land subsidence, thus new constraints on vertical land motions (VLM) in the region are warranted. In this paper, we provide a description of two campaign-style Global Positioning System (GPS) datasets, explain the methods used in data collection and validation, and present the experiment designed to quantify a new baseline of VLM in the Chesapeake Bay region of eastern North America. Data from GPS campaigns in 2019 and 2020 are presented as ASCII RINEX2.11 files and logsheets for each observation from the campaigns. Data were quality checked using the open-source program TEQC, resulting in average multipath 1 and 2 values of 0.68 and 0.57, respectively. All data are archived and publicly available for open access at the geodesy facility UNAVCO to abide by Findable, Accessible, Interoperable, Reusable (FAIR) data principles.</span></p>","language":"English","publisher":"Nature","doi":"10.1038/s41597-022-01864-8","usgsCitation":"Troia, G., Stamps, S., Lotspeich, R., Duda, J.M., McCoy, K., Moore, W., Hensel, P., Hippenstiel, R., McKenna, T., Andreasen, D.C., Geoghegan, C., Ulizo, T.P., Kronebusch, M., Carr, J., Walters, D., and Winn, N., 2022, GPS data from 2019 and 2020 campaigns in the Chesapeake Bay region towards quantifying vertical land motions: Scientific Data, v. 9, no. 1, 744, 9 p., https://doi.org/10.1038/s41597-022-01864-8.","productDescription":"744, 9 p.","ipdsId":"IP-122566","costCenters":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true},{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true},{"id":37759,"text":"VA/WV Water Science Center","active":true,"usgs":true}],"links":[{"id":445723,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1038/s41597-022-01864-8","text":"Publisher Index Page"},{"id":410538,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","otherGeospatial":"Chesapeake Bay area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -77.29568067904435,\n              40.12967557474843\n            ],\n            [\n              -77.29568067904435,\n              36.768971760646394\n            ],\n            [\n              -75.43832592966815,\n              36.768971760646394\n            ],\n            [\n              -75.43832592966815,\n              40.12967557474843\n            ],\n            [\n              -77.29568067904435,\n              40.12967557474843\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"9","issue":"1","noUsgsAuthors":false,"publicationDate":"2022-12-02","publicationStatus":"PW","contributors":{"authors":[{"text":"Troia, Gabrielle 0000-0001-6566-4623","orcid":"https://orcid.org/0000-0001-6566-4623","contributorId":299921,"corporation":false,"usgs":false,"family":"Troia","given":"Gabrielle","email":"","affiliations":[{"id":12694,"text":"Virginia Tech","active":true,"usgs":false}],"preferred":false,"id":859036,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stamps, Sarah 0000-0002-3531-1752","orcid":"https://orcid.org/0000-0002-3531-1752","contributorId":299923,"corporation":false,"usgs":false,"family":"Stamps","given":"Sarah","email":"","affiliations":[{"id":12694,"text":"Virginia Tech","active":true,"usgs":false}],"preferred":false,"id":859037,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lotspeich, R. Russell 0000-0002-5572-9064 rlotspei@usgs.gov","orcid":"https://orcid.org/0000-0002-5572-9064","contributorId":194107,"corporation":false,"usgs":true,"family":"Lotspeich","given":"R. 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,{"id":70263604,"text":"70263604 - 2022 - Assessment of carbon dioxide enhanced oil recovery and associated carbon dioxide retention resources of the United States","interactions":[],"lastModifiedDate":"2025-02-18T16:43:58.785838","indexId":"70263604","displayToPublicDate":"2022-12-01T10:38:16","publicationYear":"2022","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Assessment of carbon dioxide enhanced oil recovery and associated carbon dioxide retention resources of the United States","docAbstract":"<p><span>In 2020, the U.S. Geological Survey (USGS) completed a probabilistic assessment of the volume of technically recoverable oil resources that could be produced using current carbon dioxide enhanced oil recovery (CO2-EOR) technologies in amenable conventional oil reservoirs underlying onshore and State-owned offshore waters (herein after, onshore and State waters areas) of the conterminous United States. Our assessment also includes estimates of the mass of CO2 that could be stored (retained) in the assessed oil reservoirs following the application of the CO2-EOR process. The USGS assessment team evaluated more than 3,500 oil reservoirs that were amenable to miscible CO2 injection. The assessed reservoirs are located in 185 plays previously defined by a USGS National Oil and Gas Assessment in 33 petroleum provinces of seven national regions. The team estimated that the total technically recoverable oil resulting from the application of the CO2-EOR process ranges from approximately 25,000 million barrels (MMbbl) at the P5 probability percentile to as much as 32,000 MMbbl at the P95 probability percentile, with a mean of 29,000 MMbbl. The associated CO2 retention ranges from approximately 7,400 million metric tons (Mt) at the P5 percentile to as much as 9,500 Mt at the P95 percentile, with a mean of 8,400 Mt.</span></p>","conferenceTitle":"Social Science Research Network (SSRN), Conference Paper, 16th International Conference on Greenhouse Gas Control Technologies, GHGT-16","conferenceDate":"October 23-27, 2022","conferenceLocation":"Lyon, France","language":"English","publisher":"SSRN Elsevier","doi":"10.2139/ssrn.4279712","usgsCitation":"Warwick, P., Attanasi, E., Blondes, M., Brennan, S., Buursink, M., Cahan, S., Doolan, C.A., Freeman, P., Karacan, C.O., Lohr, C., Merrill, M., Olea, R., Shelton, J., Slucher, E.R., and Varela, B.A., 2022, Assessment of carbon dioxide enhanced oil recovery and associated carbon dioxide retention resources of the United States, Social Science Research Network (SSRN), Conference Paper, 16th International Conference on Greenhouse Gas Control Technologies, GHGT-16, Lyon, France, 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,{"id":70263323,"text":"70263323 - 2022 - Understory structure and heterospecifics influence the occupancy of a ground-nesting species of conservation concern, the Canada Warbler","interactions":[],"lastModifiedDate":"2025-02-06T16:00:27.11247","indexId":"70263323","displayToPublicDate":"2022-12-01T09:54:10","publicationYear":"2022","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":947,"text":"Avian Conservation and Ecology","active":true,"publicationSubtype":{"id":10}},"title":"Understory structure and heterospecifics influence the occupancy of a ground-nesting species of conservation concern, the Canada Warbler","docAbstract":"<p><span>Forest structure and composition in eastern U.S. forests are changing because of forest regeneration after farmland abandonment, less frequent occurrence of severe disturbances, and climate change. Some of these changes may disproportionally affect birds that rely on gap dynamics or other forest canopy disturbances to create understory habitat. The Canada Warbler (</span><i>Cardellina canadensis</i><span>) is one such understory specialist that has undergone consistent declines. We assessed environmental and interspecific factors associated with Canada Warbler space use in its southern breeding distribution to understand potential causes of population declines and inform conservation efforts. We evaluated Canada Warbler occupancy from 840 point count surveys conducted in 2017 and 2018 at 470 unique locations (79% of locations surveyed in both years) throughout Monongahela National Forest, West Virginia, USA. We modeled Canada Warbler occupancy probability as a function of environmental variables and included Black-throated Blue Warbler (</span><i>Setophaga caerulescens</i><span>) and Hermit Thrush (</span><i>Catharus guttatus</i><span>) as interacting species because all three species exhibit similar habitat preferences. Canada Warblers were most likely to occur in areas with rhododendron (</span><i>Rhododendron maximum</i><span>) density &gt; 0.27 stems/m² and within 3 m of riparian areas (streams and wetlands). They were also more likely to occur in mid-elevation (highest occupancy at 930 m) northern hardwood forests when Black-throated Blue Warblers were also present. Black-throated Blue Warblers were most likely to occupy mid-elevation sites with high shrub density, whereas Hermit Thrushes were more likely to occupy high-elevation, old-age forests. Potential management actions could focus on conserving riparian areas in northern hardwood forests, especially those with dense rhododendron thickets. Such potential actions could also be beneficial across the entire elevation range we explored within the region (500–1300 m). Canada Warblers may be benefiting from the recent spread of rhododendron habitats and northern hardwood forest types within West Virginia.</span></p>","language":"English","publisher":"Resilience Alliance Publications","doi":"10.5751/ace-02079-170120","usgsCitation":"Dimmig, G., Rota, C., Wood, P.B., and Lituma, C., 2022, Understory structure and heterospecifics influence the occupancy of a ground-nesting species of conservation concern, the Canada Warbler: Avian Conservation and Ecology, v. 17, no. 1, 20, 16 p., https://doi.org/10.5751/ace-02079-170120.","productDescription":"20, 16 p.","ipdsId":"IP-123270","costCenters":[{"id":199,"text":"Coop Res Unit Leetown","active":true,"usgs":true}],"links":[{"id":487031,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.5751/ace-02079-170120","text":"Publisher Index Page"},{"id":481747,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United sTates","state":"West Virginia","otherGeospatial":"Monongahela National Forest","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -80.58889045378262,\n              37.463537077379684\n            ],\n            [\n              -80.3485425975682,\n              37.51121532612136\n            ],\n            [\n              -79.62749902892529,\n              38.552413228981266\n            ],\n            [\n              -79.33707870266615,\n              38.442685588318085\n            ],\n            [\n              -78.8463684962287,\n              39.0674460432719\n            ],\n            [\n              -79.48729611280025,\n              39.1995023289459\n            ],\n            [\n              -79.48729611280025,\n              39.455139390658985\n            ],\n            [\n              -79.8978903671664,\n              39.37777230668391\n            ],\n            [\n              -81.23983256436323,\n              37.88364086385796\n            ],\n            [\n              -81.01951369616684,\n              37.54298391685913\n            ],\n            [\n              -80.58889045378262,\n              37.463537077379684\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"17","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Dimmig, Gordon W.","contributorId":350556,"corporation":false,"usgs":false,"family":"Dimmig","given":"Gordon W.","affiliations":[{"id":12432,"text":"West Virginia University","active":true,"usgs":false}],"preferred":false,"id":926339,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rota, Christopher T.","contributorId":350557,"corporation":false,"usgs":false,"family":"Rota","given":"Christopher T.","affiliations":[{"id":12432,"text":"West Virginia University","active":true,"usgs":false}],"preferred":false,"id":926340,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wood, Petra B. 0000-0002-8575-1705 pbwood@usgs.gov","orcid":"https://orcid.org/0000-0002-8575-1705","contributorId":199090,"corporation":false,"usgs":true,"family":"Wood","given":"Petra","email":"pbwood@usgs.gov","middleInitial":"B.","affiliations":[{"id":199,"text":"Coop Res Unit Leetown","active":true,"usgs":true}],"preferred":true,"id":926338,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lituma, Christopher M.","contributorId":350558,"corporation":false,"usgs":false,"family":"Lituma","given":"Christopher M.","affiliations":[{"id":12432,"text":"West Virginia University","active":true,"usgs":false}],"preferred":false,"id":926341,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70237132,"text":"70237132 - 2022 - Soils","interactions":[],"lastModifiedDate":"2023-01-13T15:59:55.675314","indexId":"70237132","displayToPublicDate":"2022-12-01T09:52:33","publicationYear":"2022","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"chapter":"V","title":"Soils","docAbstract":"Soils play a strong role in determining how New Mexico’s diverse landscapes will respond to climate change. Soil cover acts like a sponge, holding in water that falls as rain or snow. The presence of soil supports vegetation, and substantially reduces runoff and erosion. Soil enhances other processes such as infiltration of water and aquifer recharge. Soils can be damaged by a warming climate. Loss of vegetation in the Northwest High Desert and Eastern Plains, where soils are not well developed and easily damaged, will lead to dustier conditions in much of the state. On mountain hillslopes, the loss of vegetation cover in response to ongoing climate change will increase soil erosion, which then increases hillslope runoff. This, in turn, causes additional increases in soil erosion and bedrock exposure, which can largely prevent widespread recolonization by most plants, including trees. Soils on mountain hillslopes that face south, which are typically hotter and drier, will be damaged sooner by a warming climate than those on generally north-facing hillslopes that are slightly cooler and moister. Soils take many thousands of years to form, so these hillslopes will increasingly support sparse forests, or, in some circumstances, be entirely deforested. These changes are already well underway in some mountains in New Mexico.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Climate change in New Mexico over the next 50 years: Impacts on water resources (Bulletin 164)","largerWorkSubtype":{"id":2,"text":"State or Local Government Series"},"language":"English","publisher":"New Mexico Bureau of Geology and Mineral Resources","usgsCitation":"McFadden, L.D., Tillery, A.C., and Allen, C., 2022, Soils, 14 p.","productDescription":"14 p.","startPage":"55","endPage":"68","ipdsId":"IP-136194","costCenters":[{"id":472,"text":"New Mexico Water Science Center","active":true,"usgs":true}],"links":[{"id":411866,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":411863,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://geoinfo.nmt.edu/publications/monographs/bulletins/164/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"New 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0000-0002-8777-5989","orcid":"https://orcid.org/0000-0002-8777-5989","contributorId":297137,"corporation":false,"usgs":false,"family":"Allen","given":"Craig","affiliations":[{"id":36307,"text":"University of New Mexico","active":true,"usgs":false}],"preferred":false,"id":853425,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70230030,"text":"70230030 - 2022 - Geologic setting and geomorphic history of La Botica and surrounding area","interactions":[],"lastModifiedDate":"2026-03-18T14:06:14.010431","indexId":"70230030","displayToPublicDate":"2022-12-01T08:54:09","publicationYear":"2022","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":3,"text":"Organization Series"},"seriesTitle":{"id":23617,"text":"Research Contributions","active":true,"publicationSubtype":{"id":3}},"seriesNumber":"115","title":"Geologic setting and geomorphic history of La Botica and surrounding area","docAbstract":"<p>La Botica is located on the gently east-dipping marginal area between the high San Juan Mountains to the west and the San Luis Basin to the east in south-central Colorado. The site is positioned on a topographic bench perched about 70 to 80 m above La Jara Creek (figure 2.1), a tributary to the Rio Grande. The unique floral assemblage at La Botica has resulted in intermittent occupation over the last several thousand years. The physical environment supporting this assemblage is a result of Quaternary surface processes that have modified the underlying Tertiary bedrock. Underlying bedrock at the site consists of Oligocene to Pliocene volcanic and sedimentary deposits related to the Rio Grande rift and the San Juan volcanic locus of the Southern Rocky Mountains volcanic field. Local bedrock is mildly deformed by normal faulting and eastward tilting due to the onset of Oligocene extensional deformation and initial formation of the San Luis Basin. The geomorphic evolution and incision history of La Jara Creek are directly linked to middle to late Pleistocene evolution of the Rio Grande and to regional alpine glacial cycles over the last 500 k.y. (thousand years). Subsequent degradation of surrounding bedrock and development of mass-wasting deposits, such as landslides and talus slopes, have strongly influenced the incision history of La Jara Creek and the local environment at La Botica. In addition, local talus slopes and blockfields can host processes that actively modify the local environment, and these processes may have contributed to establishment of the floral assemblage.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Multidisciplinary research at the La Botica site, Conjeos County, Colorado","largerWorkSubtype":{"id":3,"text":"Organization Series"},"language":"English","publisher":"Paleocultural Research Group","usgsCitation":"Turner, K.J., Ruleman, C.A., and Mahan, S.A., 2022, Geologic setting and geomorphic history of La Botica and surrounding area: Research Contributions 115, 20 p.","productDescription":"20 p.","startPage":"9","endPage":"28","ipdsId":"IP-123501","costCenters":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"links":[{"id":501237,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":501236,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://paleocultural.org/Research/la-botica/"}],"country":"United States","state":"Colorado","otherGeospatial":"La Botica","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -106.79256393659836,\n              37.70573798045494\n            ],\n            [\n              -106.79256393659836,\n              37.02301823232551\n            ],\n            [\n              -105.74755024473933,\n              37.02301823232551\n            ],\n            [\n              -105.74755024473933,\n              37.70573798045494\n            ],\n            [\n              -106.79256393659836,\n              37.70573798045494\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Turner, Kenzie J. 0000-0002-4940-3981 kturner@usgs.gov","orcid":"https://orcid.org/0000-0002-4940-3981","contributorId":496,"corporation":false,"usgs":true,"family":"Turner","given":"Kenzie","email":"kturner@usgs.gov","middleInitial":"J.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":838788,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ruleman, Chester A. 0000-0002-1503-4591 cruleman@usgs.gov","orcid":"https://orcid.org/0000-0002-1503-4591","contributorId":1264,"corporation":false,"usgs":true,"family":"Ruleman","given":"Chester","email":"cruleman@usgs.gov","middleInitial":"A.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true},{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":838789,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mahan, Shannon A. 0000-0001-5214-7774 smahan@usgs.gov","orcid":"https://orcid.org/0000-0001-5214-7774","contributorId":147159,"corporation":false,"usgs":true,"family":"Mahan","given":"Shannon","email":"smahan@usgs.gov","middleInitial":"A.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":838790,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70240308,"text":"70240308 - 2022 - Modeling risk dynamics of contaminants of emerging concern in a temperate-region wastewater effluent-dominated stream","interactions":[],"lastModifiedDate":"2023-02-03T14:45:16.85921","indexId":"70240308","displayToPublicDate":"2022-12-01T08:24:40","publicationYear":"2022","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5112,"text":"Environmental Science: Water Research & Technology","active":true,"publicationSubtype":{"id":10}},"title":"Modeling risk dynamics of contaminants of emerging concern in a temperate-region wastewater effluent-dominated stream","docAbstract":"<p><span>Wastewater effluent-dominated streams are becoming increasingly common worldwide, including in temperate regions, with potential impacts on ecological systems and drinking water sources. We recently quantified the occurrence/spatiotemporal dynamics of pharmaceutical mixtures in a representative temperate-region wastewater effluent-dominated stream (Muddy Creek, Iowa) under baseflow conditions and characterized relevant fate processes. Herein, we quantified the ecological risk quotients (RQs) of 19 effluent-derived contaminants of emerging concern (CECs; including: 14 pharmaceuticals, 2 industrial chemicals, and 3 neonicotinoid insecticides) and 1 run-off-derived compound (atrazine) in the stream under baseflow conditions, and estimated the probabilistic risks of effluent-derived CECs under all-flow conditions (</span><i>i.e.</i><span>, including runoff events) using stochastic risk modeling. We determined that 11 out of 20 CECs pose medium-to-high risks to local ecological systems (</span><i>i.e.</i><span>, algae, invertebrates, fish) based on literature-derived acute effects under measured baseflow conditions. Stochastic risk modeling indicated decreased, but still problematic, risk of effluent-derived CECs (</span><i>i.e.</i><span>, RQ ≥ 0.1) under all-flow conditions when runoff events were included. Dilution of effluent-derived chemicals from storm flows thus only minimally decreased risk to aquatic biota in the effluent-dominated stream. We also modeled in-stream transport. Thirteen out of 14 pharmaceuticals persisted along the stream reach (median attenuation rate constant&nbsp;</span><i>k</i><span>&nbsp;&lt; 0.1 h</span><small><sup>−1</sup></small><span>) and entered the Iowa River at elevated concentrations. Predicted and measured concentrations in the drinking water treatment plant were below the human health benchmarks. This study demonstrates the application of probabilistic risk assessments for effluent-derived CECs in a representative effluent-dominated stream under variable flow conditions (when measurements are less practical) and provides an enhanced prediction tool transferable to other effluent-dominated systems.</span></p>","language":"English","publisher":"Royal Society of Chemistry","doi":"10.1039/D2EW00157H","usgsCitation":"Zhi, H., Webb, D.T., Schnoor, J.L., Kolpin, D., Klaper, R.D., Iwanowicz, L., and LeFevre, G.H., 2022, Modeling risk dynamics of contaminants of emerging concern in a temperate-region wastewater effluent-dominated stream: Environmental Science: Water Research & Technology, v. 8, p. 1408-1422, https://doi.org/10.1039/D2EW00157H.","productDescription":"15 p.","startPage":"1408","endPage":"1422","ipdsId":"IP-129637","costCenters":[{"id":36532,"text":"Central Midwest Water Science Center","active":true,"usgs":true},{"id":50464,"text":"Eastern Ecological Science Center","active":true,"usgs":true}],"links":[{"id":445736,"rank":0,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://www.ncbi.nlm.nih.gov/pmc/articles/9431852","text":"External Repository"},{"id":412670,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Iowa","otherGeospatial":"Muddy Creek","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -91.55039606554381,\n              41.6953124183122\n            ],\n            [\n              -91.54728310759076,\n              41.69428009738749\n            ],\n            [\n              -91.54749768431226,\n              41.69891044541674\n            ],\n            [\n              -91.54924385578545,\n              41.702072402012334\n            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             -91.57783544690375,\n              41.70724555624517\n            ],\n            [\n              -91.57354499632964,\n              41.70396771514703\n            ],\n            [\n              -91.56869788963536,\n              41.70074374361087\n            ],\n            [\n              -91.56367679435925,\n              41.699301843564285\n            ],\n            [\n              -91.5593423445914,\n              41.69981452284023\n            ],\n            [\n              -91.55588922960604,\n              41.69934990742098\n            ],\n            [\n              -91.55041752321569,\n              41.699542162484676\n            ],\n            [\n              -91.55067501528096,\n              41.69691462686407\n            ],\n            [\n              -91.55039606554381,\n              41.6953124183122\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"8","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Zhi, Hui","contributorId":225502,"corporation":false,"usgs":false,"family":"Zhi","given":"Hui","email":"","affiliations":[{"id":6768,"text":"University of Iowa","active":true,"usgs":false}],"preferred":false,"id":863353,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Webb, Danielle T.","contributorId":211879,"corporation":false,"usgs":false,"family":"Webb","given":"Danielle","email":"","middleInitial":"T.","affiliations":[{"id":6768,"text":"University of Iowa","active":true,"usgs":false}],"preferred":false,"id":863354,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Schnoor, Jerald L","contributorId":302047,"corporation":false,"usgs":false,"family":"Schnoor","given":"Jerald","email":"","middleInitial":"L","affiliations":[{"id":6768,"text":"University of Iowa","active":true,"usgs":false}],"preferred":false,"id":863355,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Kolpin, Dana W. 0000-0002-3529-6505","orcid":"https://orcid.org/0000-0002-3529-6505","contributorId":204154,"corporation":false,"usgs":true,"family":"Kolpin","given":"Dana W.","affiliations":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true},{"id":35680,"text":"Illinois-Iowa-Missouri Water Science Center","active":true,"usgs":true},{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true}],"preferred":true,"id":863356,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Klaper, Rebecca D.","contributorId":218114,"corporation":false,"usgs":false,"family":"Klaper","given":"Rebecca","email":"","middleInitial":"D.","affiliations":[{"id":18038,"text":"University of Wisconsin, Milwaukee","active":true,"usgs":false}],"preferred":false,"id":863357,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Iwanowicz, Luke 0000-0002-1197-6178 liwanowicz@usgs.gov","orcid":"https://orcid.org/0000-0002-1197-6178","contributorId":302048,"corporation":false,"usgs":true,"family":"Iwanowicz","given":"Luke","email":"liwanowicz@usgs.gov","affiliations":[{"id":50464,"text":"Eastern Ecological Science Center","active":true,"usgs":true}],"preferred":true,"id":863358,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"LeFevre, Gregory H.","contributorId":211880,"corporation":false,"usgs":false,"family":"LeFevre","given":"Gregory","email":"","middleInitial":"H.","affiliations":[{"id":6768,"text":"University of Iowa","active":true,"usgs":false}],"preferred":true,"id":863359,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70239798,"text":"70239798 - 2022 - Horseshoe crab","interactions":[],"lastModifiedDate":"2023-01-20T14:27:56.757671","indexId":"70239798","displayToPublicDate":"2022-12-01T08:17:53","publicationYear":"2022","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"chapter":"7.1.2","title":"Horseshoe crab","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Technical report for the Delaware estuary and basin, PDE Report No. 22-05","largerWorkSubtype":{"id":3,"text":"Organization Series"},"language":"English","publisher":"Partnership for the Delaware Estuary","usgsCitation":"Smith, D.R., 2022, Horseshoe crab, chap. 7.1.2 <i>of</i> Technical report for the Delaware estuary and basin, PDE Report No. 22-05, p. 308-315.","productDescription":"8 p.","startPage":"308","endPage":"315","ipdsId":"IP-142284","costCenters":[{"id":50464,"text":"Eastern Ecological Science Center","active":true,"usgs":true}],"links":[{"id":412120,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":412119,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://delawareestuary.org/data-and-reports/state-of-the-estuary-report-2/"}],"country":"United States","otherGeospatial":"Delaware Bay","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -74.5,\n              39.85382793829535\n            ],\n            [\n              -75.6425148831999,\n              39.85382793829535\n            ],\n            [\n              -75.6425148831999,\n              38.75\n            ],\n            [\n              -74.5,\n              38.75\n            ],\n            [\n              -74.5,\n              39.85382793829535\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Smith, David R. 0000-0001-6074-9257 drsmith@usgs.gov","orcid":"https://orcid.org/0000-0001-6074-9257","contributorId":168442,"corporation":false,"usgs":true,"family":"Smith","given":"David","email":"drsmith@usgs.gov","middleInitial":"R.","affiliations":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"preferred":true,"id":861983,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70239124,"text":"70239124 - 2022 - Effects of release techniques on parent-reared whooping cranes in the eastern migratory population","interactions":[],"lastModifiedDate":"2022-12-28T13:42:34.222167","indexId":"70239124","displayToPublicDate":"2022-12-01T07:40:38","publicationYear":"2022","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":12807,"text":"Proceedings of the North American Crane Workshop","active":true,"publicationSubtype":{"id":10}},"title":"Effects of release techniques on parent-reared whooping cranes in the eastern migratory population","docAbstract":"<div id=\"sub\"><div id=\"alpha\"><div id=\"abstract\" class=\"element\"><p>Reintroduction of an Eastern Migratory Population (EMP) of whooping cranes (<i>Grus americana</i>) in the United States by release of captive-reared individuals began in 2001. As of 2020, the EMP has approximately 21 breeding pairs and has had limited recruitment of wild-hatched individuals, thus captive-reared juveniles continue to be released into breeding areas in Wisconsin to maintain the population. We investigated the effects of release techniques on survival, behavior, site fidelity, and conspecific associations of 42 captive-parent-reared whooping cranes released during 2013-2019 into the EMP. Individuals were monitored intensively post-release, then as a part of a long-term monitoring program, locational, behavioral, and habitat use data were collected and analyzed. Most cranes roosted in water post-release; however, we documented 4 parent-reared cranes roosting on dry land. Most cranes eventually associated with other whooping cranes; however, juveniles released near single adult cranes were less likely to associate with other whooping cranes during their first migration or winter than juveniles released near other types of whooping crane pairs or groups. Parent-reared and costume-reared whooping cranes had similar rates of survival 1 year post-release (69.0% and 64.4%, respectively). The highest risk of mortality was within the first 100 days post-release, and the leading known causes of death were predation and impact trauma due to powerline or vehicle collisions. Both costume- and parent-reared cranes had strong fidelity to release sites. We advise releasing parent-reared cranes near pairs or groups of whooping cranes and taking measures to reduce the risk of mortality during the immediate period after release (e.g., predator aversion training, marking powerlines).</p></div></div></div>","language":"English","publisher":"North American Crane Working Group","usgsCitation":"Thompson, H.L., Mann, M.S., Wellington, M., Boardman, K.H., and Olsen, G.H., 2022, Effects of release techniques on parent-reared whooping cranes in the eastern migratory population: Proceedings of the North American Crane Workshop, v. 15, p. 53-71.","productDescription":"18 p.","startPage":"53","endPage":"71","ipdsId":"IP-125215","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true},{"id":50464,"text":"Eastern Ecological Science Center","active":true,"usgs":true}],"links":[{"id":411115,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":411112,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://digitalcommons.unl.edu/nacwgproc/387/#:~:text=Parent%2Dreared%20and%20costume%2Dreared,to%20powerline%20or%20vehicle%20collisions."}],"volume":"15","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Thompson, Hillary L.","contributorId":300470,"corporation":false,"usgs":false,"family":"Thompson","given":"Hillary","email":"","middleInitial":"L.","affiliations":[{"id":65168,"text":"International Crane Foundation, Baraboo, Wisconsin","active":true,"usgs":false}],"preferred":false,"id":860255,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mann, M. Susanna","contributorId":300471,"corporation":false,"usgs":false,"family":"Mann","given":"M.","email":"","middleInitial":"Susanna","affiliations":[{"id":65168,"text":"International Crane Foundation, Baraboo, Wisconsin","active":true,"usgs":false}],"preferred":false,"id":860256,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wellington, Marianne","contributorId":300472,"corporation":false,"usgs":false,"family":"Wellington","given":"Marianne","email":"","affiliations":[{"id":65168,"text":"International Crane Foundation, Baraboo, Wisconsin","active":true,"usgs":false}],"preferred":false,"id":860257,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Boardman, Kim H.","contributorId":300473,"corporation":false,"usgs":false,"family":"Boardman","given":"Kim","email":"","middleInitial":"H.","affiliations":[{"id":16606,"text":"International Crane Foundation","active":true,"usgs":false}],"preferred":false,"id":860258,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Olsen, Glenn H. 0000-0002-7188-6203","orcid":"https://orcid.org/0000-0002-7188-6203","contributorId":238130,"corporation":false,"usgs":true,"family":"Olsen","given":"Glenn","email":"","middleInitial":"H.","affiliations":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"preferred":true,"id":860259,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70238765,"text":"70238765 - 2022 - A case study: Temporal trends of environmental stressors and reproductive health of smallmouth bass (Micropterus dolomieu) from a site in the Potomac River Watershed, Maryland, USA","interactions":[],"lastModifiedDate":"2022-12-09T13:18:59.076223","indexId":"70238765","displayToPublicDate":"2022-12-01T06:37:18","publicationYear":"2022","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1479,"text":"Ecotoxicology","active":true,"publicationSubtype":{"id":10}},"displayTitle":"A case study: Temporal trends of environmental stressors and reproductive health of smallmouth bass (<i>Micropterus dolomieu</i>) from a site in the Potomac River Watershed, Maryland, USA","title":"A case study: Temporal trends of environmental stressors and reproductive health of smallmouth bass (Micropterus dolomieu) from a site in the Potomac River Watershed, Maryland, USA","docAbstract":"<div id=\"Abs1-section\" class=\"c-article-section\"><div id=\"Abs1-content\" class=\"c-article-section__content\"><p>Decades of poor reproductive success and young-of-the-year survival, combined with adult mortality events, have led to a decline in the smallmouth bass (SMB;<span>&nbsp;</span><i>Micropterus dolomieu</i>) population in sections of the Potomac River. Previous studies have identified numerous biologic and environmental stressors associated with negative effects on SMB health. To better understand the impact of these stressors, this study was conducted at the confluence of Antietam Creek and the Potomac River from 2013 to 2019 to identify temporal changes associated with SMB reproductive health. Surface water samples were collected and analyzed for over 300 organic contaminants, including pesticides, phytoestrogens, pharmaceuticals, hormones and total estrogenicity (E2Eq). Adult SMB were collected and sampled for multiple endpoints, including gene transcripts associated with reproduction (molecular), histopathology (cellular), and organosomatic indices (tissue). In males, biomarkers of estrogenic endocrine disruption, including testicular oocytes (TO) and plasma vitellogenin (Vtg) were assessed. Numerous agriculture-related contaminants or land use patterns were associated with gene transcript abundance in both male and female SMB. Positive associations between pesticides in the immediate catchment with TO severity and E2Eq with plasma Vtg in males were identified. In males, the prevalence of TO and detectable levels of plasma Vtg, liver vitellogenin transcripts (<i>vtg</i>) and testis<span>&nbsp;</span><i>vtg</i><span>&nbsp;</span>were high throughout the study. Peaks of complex mixtures of numerous contaminants occurred during the spring/early summer when spawning and early development occurs and to a lesser extent in fall/winter during recrudescence. Management practices to reduce exposure during these critical and sensitive periods may enhance reproductive health of these economically important sportfishes.</p></div></div>","language":"English","publisher":"Springer","doi":"10.1007/s10646-022-02605-8","usgsCitation":"Walsh, H.L., Gordon, S.E., Sperry, A.J., Kashiwagi, M., Mullican, J.E., and Blazer, V., 2022, A case study: Temporal trends of environmental stressors and reproductive health of smallmouth bass (Micropterus dolomieu) from a site in the Potomac River Watershed, Maryland, USA: Ecotoxicology, v. 31, p. 1536-1553, https://doi.org/10.1007/s10646-022-02605-8.","productDescription":"18 p.","startPage":"1536","endPage":"1553","ipdsId":"IP-137241","costCenters":[{"id":50464,"text":"Eastern Ecological Science Center","active":true,"usgs":true}],"links":[{"id":445760,"rank":1,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1007/s10646-022-02605-8","text":"Publisher Index Page"},{"id":435602,"rank":0,"type":{"id":30,"text":"Data Release"},"url":"https://doi.org/10.5066/P9XZ7UWK","text":"USGS data release","linkHelpText":"Water Chemistry and Smallmouth Bass Biological Data From the Potomac River, Dargan, Maryland, 2013-2019"},{"id":410193,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Maryland","otherGeospatial":"Potomac River Watershed","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -78.02585441087574,\n              39.83232093177554\n            ],\n            [\n              -78.02585441087574,\n              38.176896831749104\n            ],\n            [\n              -76.4005680754395,\n              38.176896831749104\n            ],\n            [\n              -76.4005680754395,\n              39.83232093177554\n            ],\n            [\n              -78.02585441087574,\n              39.83232093177554\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"31","noUsgsAuthors":false,"publicationDate":"2022-12-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Walsh, Heather L. 0000-0001-6392-4604 hwalsh@usgs.gov","orcid":"https://orcid.org/0000-0001-6392-4604","contributorId":4696,"corporation":false,"usgs":true,"family":"Walsh","given":"Heather","email":"hwalsh@usgs.gov","middleInitial":"L.","affiliations":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"preferred":true,"id":858507,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gordon, Stephanie E. 0000-0002-6292-2612 sgordon@usgs.gov","orcid":"https://orcid.org/0000-0002-6292-2612","contributorId":200931,"corporation":false,"usgs":true,"family":"Gordon","given":"Stephanie","email":"sgordon@usgs.gov","middleInitial":"E.","affiliations":[{"id":242,"text":"Eastern Geographic Science Center","active":true,"usgs":true}],"preferred":true,"id":858536,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sperry, Adam J. 0000-0002-4815-3730 asperry@usgs.gov","orcid":"https://orcid.org/0000-0002-4815-3730","contributorId":5872,"corporation":false,"usgs":true,"family":"Sperry","given":"Adam","email":"asperry@usgs.gov","middleInitial":"J.","affiliations":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"preferred":true,"id":858537,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Kashiwagi, Michael","contributorId":299323,"corporation":false,"usgs":false,"family":"Kashiwagi","given":"Michael","email":"","affiliations":[{"id":33964,"text":"Maryland Department of Natural Resources","active":true,"usgs":false}],"preferred":false,"id":858538,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Mullican, John E.","contributorId":203245,"corporation":false,"usgs":false,"family":"Mullican","given":"John","email":"","middleInitial":"E.","affiliations":[{"id":33964,"text":"Maryland Department of Natural Resources","active":true,"usgs":false}],"preferred":false,"id":858539,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Blazer, Vicki S. 0000-0001-6647-9614 vblazer@usgs.gov","orcid":"https://orcid.org/0000-0001-6647-9614","contributorId":150384,"corporation":false,"usgs":true,"family":"Blazer","given":"Vicki S.","email":"vblazer@usgs.gov","affiliations":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"preferred":true,"id":858508,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70240194,"text":"70240194 - 2022 - 40Ar/39Ar geochronology of magmatic-steam alunite from Alunite Ridge and Deer Trail Mountain, Marysvale Volcanic Field, Utah: Timing and duration of miocene hydrothermal activity associated with concealed intrusions","interactions":[],"lastModifiedDate":"2023-02-01T12:49:12.860875","indexId":"70240194","displayToPublicDate":"2022-11-29T06:43:37","publicationYear":"2022","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5207,"text":"Minerals","active":true,"publicationSubtype":{"id":10}},"title":"40Ar/39Ar geochronology of magmatic-steam alunite from Alunite Ridge and Deer Trail Mountain, Marysvale Volcanic Field, Utah: Timing and duration of miocene hydrothermal activity associated with concealed intrusions","docAbstract":"<div class=\"html-p\">Porphyry and epithermal deposits are important sources of base and precious metals. Most actively mined deposits have been exhumed such that ore bodies are relatively close to the surface and are therefore locatable and economic to extract. Identifying and characterizing concealed deposits, particularly more deeply buried porphyry deposits, represents a far greater challenge for mineral exploration, and will become progressively more important as near-surface resources are gradually exhausted over time. We report high-precision<span>&nbsp;</span><sup>40</sup>Ar/<sup>39</sup>Ar dates for coarsely crystalline alunite that precipitated from magmatic steam in open fractures in Oligocene dacitic volcanic rocks, and a SHRIMP<span>&nbsp;</span><sup>206</sup>Pb/<sup>238</sup>U zircon date for one of several rhyolite dikes present at Alunite Ridge and Deer Trail Mountain, Utah. Both the magmatic-steam alunite and rhyolite dikes are related to concealed intrusions. The rhyolite dike yielded an age of 30.72 ± 0.36 Ma, which is older than a commonly cited 27.1 Ma age estimate for the Three Creeks Tuff Member of the Bullion Canyon Volcanics that is cut by the dike.<span>&nbsp;</span><sup>40</sup>Ar/<sup>39</sup>Ar data for samples of magmatic-steam alunite and sericite from six mines and prospects provide evidence for at least two periods of episodic hydrothermal activity at ca. 15.7–15.1 Ma and ca. 14.7–13.8 Ma, with the older and younger pulses of activity recorded at the more eastern and western sites, respectively. These two periods of hydrothermal activity are consistent with previous interpretations that Alunite Ridge and Deer Trail Mountain are underlain by two concealed porphyry stocks.<span>&nbsp;</span><sup>40</sup>Ar/<sup>39</sup>Ar analyses of individual bands in a sample of massive, centimeter-scale banded vein alunite yield indistinguishable ages with a weighted mean of 13.98 ± 0.12 Ma, consistent with a short-lived (≲250 ka) magmatic event with episodic vapor discharge recurring on short timescales (≲36 ka).<span>&nbsp;</span><sup>40</sup>Ar/<sup>39</sup>Ar geochronology of magmatic-steam alunite is a valuable tool to constrain the timing and duration of magmatic hydrothermal activity associated with unexposed intrusions and potentially porphyry deposits, and therefore may be useful in exploration.</div>","language":"English","publisher":"MDPI","doi":"10.3390/min12121533","usgsCitation":"Mercer, C.M., Cosca, M., Hofstra, A.H., Premo, W.R., Rye, R.O., and Landis, G.P., 2022, 40Ar/39Ar geochronology of magmatic-steam alunite from Alunite Ridge and Deer Trail Mountain, Marysvale Volcanic Field, Utah: Timing and duration of miocene hydrothermal activity associated with concealed intrusions: Minerals, v. 12, no. 12, 1533, 25 p., https://doi.org/10.3390/min12121533.","productDescription":"1533, 25 p.","ipdsId":"IP-145097","costCenters":[{"id":35995,"text":"Geology, Geophysics, and Geochemistry Science Center","active":true,"usgs":true}],"links":[{"id":445787,"rank":1,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.3390/min12121533","text":"Publisher Index Page"},{"id":435609,"rank":0,"type":{"id":30,"text":"Data Release"},"url":"https://doi.org/10.5066/P9IF4UZP","text":"USGS data release","linkHelpText":"Argon and SHRIMP-RG Data for Magmatic Steam Alunite, Sericite, and Zircon from Alunite Ridge and Deer Trail Mountain, Marysvale, Utah"},{"id":412528,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Utah","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -112.81537822381003,\n              37.89618849576978\n            ],\n            [\n              -111.33716402699213,\n              37.89618849576978\n            ],\n            [\n              -111.33716402699213,\n              39.15103885566745\n            ],\n            [\n              -112.81537822381003,\n              39.15103885566745\n            ],\n            [\n              -112.81537822381003,\n              37.89618849576978\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"12","issue":"12","noUsgsAuthors":false,"publicationDate":"2022-11-29","publicationStatus":"PW","contributors":{"authors":[{"text":"Mercer, Cameron Mark 0000-0003-0534-848X","orcid":"https://orcid.org/0000-0003-0534-848X","contributorId":301880,"corporation":false,"usgs":true,"family":"Mercer","given":"Cameron","email":"","middleInitial":"Mark","affiliations":[{"id":35995,"text":"Geology, Geophysics, and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":862926,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cosca, M. 0000-0002-0600-7663","orcid":"https://orcid.org/0000-0002-0600-7663","contributorId":107417,"corporation":false,"usgs":true,"family":"Cosca","given":"M.","affiliations":[{"id":35995,"text":"Geology, Geophysics, and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":862927,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hofstra, Albert H. 0000-0002-2450-1593 ahofstra@usgs.gov","orcid":"https://orcid.org/0000-0002-2450-1593","contributorId":1302,"corporation":false,"usgs":true,"family":"Hofstra","given":"Albert","email":"ahofstra@usgs.gov","middleInitial":"H.","affiliations":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":862928,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Premo, Wayne R. 0000-0001-9904-4801 wpremo@usgs.gov","orcid":"https://orcid.org/0000-0001-9904-4801","contributorId":1697,"corporation":false,"usgs":true,"family":"Premo","given":"Wayne","email":"wpremo@usgs.gov","middleInitial":"R.","affiliations":[],"preferred":true,"id":862929,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Rye, Robert O.","contributorId":301881,"corporation":false,"usgs":false,"family":"Rye","given":"Robert","email":"","middleInitial":"O.","affiliations":[{"id":6676,"text":"USGS (retired)","active":true,"usgs":false}],"preferred":false,"id":862930,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Landis, Gary P.","contributorId":301883,"corporation":false,"usgs":false,"family":"Landis","given":"Gary","email":"","middleInitial":"P.","affiliations":[{"id":6676,"text":"USGS (retired)","active":true,"usgs":false}],"preferred":false,"id":862931,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70238519,"text":"sir20225104 - 2022 - Groundwater-level altitudes and groundwater-flow direction and nature and extent of volatile and semivolatile organic compounds at Petro-Chemical Systems, Inc. (Turtle Bayou), Superfund site, Liberty County, Texas, 2020","interactions":[],"lastModifiedDate":"2026-04-28T14:23:31.866599","indexId":"sir20225104","displayToPublicDate":"2022-11-28T10:09:49","publicationYear":"2022","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":"2022-5104","displayTitle":"Groundwater-Level Altitudes and Groundwater-Flow Direction and Nature and Extent of Volatile and Semivolatile Organic Compounds at Petro-Chemical Systems, Inc. (Turtle Bayou), Superfund Site, Liberty County, Texas, 2020","title":"Groundwater-level altitudes and groundwater-flow direction and nature and extent of volatile and semivolatile organic compounds at Petro-Chemical Systems, Inc. (Turtle Bayou), Superfund site, Liberty County, Texas, 2020","docAbstract":"<p>The Petro-Chemical Systems, Inc. (Turtle Bayou), Superfund site is 15 miles southeast of Liberty, Texas, in Liberty County. Improper disposal of waste oils led to contamination of soil and groundwater at the site. In cooperation with the U.S. Environmental Protection Agency, the U.S. Geological Survey collected water-quality samples from 11 monitoring wells at the site, in particular the area near well MW-109A (the MW-109 area), in August and September 2020 and compared the water-quality results to the results from previous water-quality sampling events at the site in June 2016 and August 2018 with a focus on benzene concentrations. Contours of groundwater-level altitudes in the MW-109 area indicate that groundwater-flow direction is south-southeasterly in the eastern part and south-southwesterly in the western part.</p><p>Of the 51 volatile organic compounds analyzed, 13 were detected in groundwater samples from 1 or more wells. In all but 1 well, MW-109A, concentrations of these compounds were less than 100 micrograms per liter. Benzene is still the principal contaminant of concern, as it persists at concentrations exceeding 53,000 micrograms per liter, although naphthalene also appears to be a contaminant of concern, as it was detected at the greatest concentration of any semivolatile organic compound analyte (1,100 micrograms per liter in the sample from well MW-109A).</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20225104","collaboration":"Prepared in cooperation with the U.S. Environmental Protection Agency","usgsCitation":"Braun, C.L., and Becher, K.D., 2022, Groundwater-level altitudes and groundwater-flow direction and nature and extent of volatile and semivolatile organic compounds at Petro-Chemical Systems, Inc. (Turtle Bayou), Superfund site, Liberty County, Texas, 2020: U.S. Geological Survey Scientific Investigations Report 2022–5104, 17 p., https://doi.org/10.3133/sir20225104.","productDescription":"Report: v, 17 p.; Data Release","numberOfPages":"28","onlineOnly":"Y","ipdsId":"IP-135616","costCenters":[{"id":48595,"text":"Oklahoma-Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":503565,"rank":7,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_113878.htm","linkFileType":{"id":5,"text":"html"}},{"id":409693,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/sir/2022/5104/coverthb.jpg"},{"id":409694,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/sir/2022/5104/sir20225104.pdf","text":"Report","size":"1.56 MB","linkFileType":{"id":1,"text":"pdf"},"description":"SIR 2022–5104"},{"id":411892,"rank":6,"type":{"id":39,"text":"HTML Document"},"url":"https://pubs.usgs.gov/publication/sir20225104/full","text":"Report","linkFileType":{"id":5,"text":"html"}},{"id":409697,"rank":5,"type":{"id":30,"text":"Data Release"},"url":"https://doi.org/10.5066/P9GX8YU7","text":"USGS data release","linkHelpText":"Groundwater-level altitudes and volatile and semivolatile organic compound concentrations at the Petro-Chemical Systems, Inc. (Turtle Bayou) Superfund site, Liberty County, Texas, 2020"},{"id":409696,"rank":4,"type":{"id":34,"text":"Image Folder"},"url":"https://pubs.usgs.gov/sir/2022/5104/images"},{"id":409695,"rank":3,"type":{"id":31,"text":"Publication XML"},"url":"https://pubs.usgs.gov/sir/2022/5104/sir20225104.XML"}],"country":"United States","state":"Texas","county":"Liberty County","otherGeospatial":"Petro-Chemical Systems, Inc. (Turtle Bayou), Superfund site","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -94.7111,\n              29.9222\n            ],\n            [\n              -94.7111,\n              29.9167\n            ],\n            [\n              -94.6667,\n              29.9167\n            ],\n            [\n              -94.6667,\n              29.9222\n            ],\n            [\n              -94.7111,\n              29.9222\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","contact":"<p>Director, <a href=\"https://www.usgs.gov/centers/ot-water\" data-mce-href=\"https://www.usgs.gov/centers/ot-water\">Oklahoma-Texas Water Science Center</a><br>U.S. Geological Survey<br>1505 Ferguson Lane<br>Austin, TX 78754–4501</p><p><a href=\"https://pubs.er.usgs.gov/contact\" data-mce-href=\"../contact\">Contact Pubs Warehouse</a></p>","tableOfContents":"<ul><li>Abstract</li><li>Introduction</li><li>Methods</li><li>Groundwater-Level Altitudes and Groundwater-Flow Direction</li><li>Nature and Extent of Volatile and Semivolatile Organic Compounds</li><li>Summary</li><li>References Cited</li></ul>","publishingServiceCenter":{"id":5,"text":"Lafayette PSC"},"publishedDate":"2022-11-28","noUsgsAuthors":false,"publicationDate":"2022-11-28","publicationStatus":"PW","contributors":{"authors":[{"text":"Braun, Christopher L. 0000-0002-5540-2854 clbraun@usgs.gov","orcid":"https://orcid.org/0000-0002-5540-2854","contributorId":925,"corporation":false,"usgs":true,"family":"Braun","given":"Christopher","email":"clbraun@usgs.gov","middleInitial":"L.","affiliations":[{"id":48595,"text":"Oklahoma-Texas Water Science Center","active":true,"usgs":true}],"preferred":true,"id":857723,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Becher, Kent D. 0000-0002-3947-0793","orcid":"https://orcid.org/0000-0002-3947-0793","contributorId":204184,"corporation":false,"usgs":true,"family":"Becher","given":"Kent","email":"","middleInitial":"D.","affiliations":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"preferred":true,"id":857724,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70238551,"text":"70238551 - 2022 - Preliminary evidence of anticoagulant rodenticide exposure in American kestrels (Falco sparverius) in the western United States","interactions":[],"lastModifiedDate":"2022-11-29T13:10:16.252595","indexId":"70238551","displayToPublicDate":"2022-11-28T07:00:54","publicationYear":"2022","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2442,"text":"Journal of Raptor Research","active":true,"publicationSubtype":{"id":10}},"title":"Preliminary evidence of anticoagulant rodenticide exposure in American kestrels (Falco sparverius) in the western United States","docAbstract":"<p id=\"ID0EF\" class=\"first\">Although there is extensive evidence of declines in the American Kestrel (<i>Falco sparverius</i>) population across North America, the cause of such declines remains a mystery. One hypothesized driver of decline is anticoagulant rodenticide (AR) exposure, which could potentially cause mortality or reduced fitness. We investigated AR exposure in wild American Kestrels in Utah, USA. We collected and tested for AR residues in liver samples (<i>n</i><span>&nbsp;</span>= 8) from kestrels opportunistically encountered dead and in blood samples (<i>n</i><span>&nbsp;</span>= 71) from live wild kestrels, both nestlings and adults. We found high detection rates in both tissues. Adult kestrels were more likely to exhibit exposure than juveniles sampled in nests. Three-quarters (six of eight) of tested liver samples from adult kestrels exhibited evidence of AR exposure. Additionally, liver samples (<i>n</i><span>&nbsp;</span>= 19) opportunistically collected from seven species of raptors within our study area had detectable levels of AR residues, with seven of eight raptor species evidencing exposure; across all raptors, five ARs were detected in liver samples, with brodifacoum the most prevalent, being found in over half (14 of 27) of samples. Over half (7 of 12) of the blood samples from adult kestrels had detectible levels of ARs, while only one of 59 juvenile nest samples tested positive. The difference in exposure rates between adults and juveniles could indicate differential exposure pathways by age class. Based on these findings, we recommend that ARs be further investigated as a potential cause of kestrel declines. Future research could focus on expanding sampling to provide sufficient sample sizes to test for potential nonlethal effects of AR exposure (e.g., fecundity, nesting success), identifying potential exposure pathways, and developing methods for passive sampling of ARs in excreta.</p>","language":"English","publisher":"BioOne","doi":"10.3356/JRR-22-18","usgsCitation":"Buechley, E.R., Oleyar, D., Watson, J., Bridgeman, J., Volker, S., Goldade, D.A., Swift, C.E., and Rattner, B.A., 2022, Preliminary evidence of anticoagulant rodenticide exposure in American kestrels (Falco sparverius) in the western United States: Journal of Raptor Research, v. 57, no. 2, 11 p., https://doi.org/10.3356/JRR-22-18.","productDescription":"11 p.","ipdsId":"IP-137518","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true},{"id":50464,"text":"Eastern Ecological Science Center","active":true,"usgs":true}],"links":[{"id":409788,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Utah","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -112.7171265349214,\n              41.72856999995494\n            ],\n            [\n              -112.7171265349214,\n              39.7315850693289\n            ],\n            [\n              -111.00398688405573,\n              39.7315850693289\n            ],\n            [\n              -111.00398688405573,\n              41.72856999995494\n            ],\n            [\n              -112.7171265349214,\n              41.72856999995494\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"57","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Buechley, Evan R.","contributorId":299452,"corporation":false,"usgs":false,"family":"Buechley","given":"Evan","email":"","middleInitial":"R.","affiliations":[{"id":64849,"text":"Smithsonian Conservaiton Biology Institute","active":true,"usgs":false}],"preferred":false,"id":857836,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Oleyar, Dave","contributorId":299453,"corporation":false,"usgs":false,"family":"Oleyar","given":"Dave","email":"","affiliations":[{"id":35596,"text":"HawkWatch International","active":true,"usgs":false}],"preferred":false,"id":857905,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Watson, Jesse","contributorId":243506,"corporation":false,"usgs":false,"family":"Watson","given":"Jesse","email":"","affiliations":[],"preferred":false,"id":857906,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bridgeman, Jennifer","contributorId":299455,"corporation":false,"usgs":false,"family":"Bridgeman","given":"Jennifer","email":"","affiliations":[{"id":35596,"text":"HawkWatch International","active":true,"usgs":false}],"preferred":false,"id":857907,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Volker, Steven","contributorId":299456,"corporation":false,"usgs":false,"family":"Volker","given":"Steven","affiliations":[{"id":64850,"text":"USDA, APHIS","active":true,"usgs":false}],"preferred":false,"id":857908,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Goldade, David A.","contributorId":299457,"corporation":false,"usgs":false,"family":"Goldade","given":"David","email":"","middleInitial":"A.","affiliations":[{"id":64850,"text":"USDA, APHIS","active":true,"usgs":false}],"preferred":false,"id":857909,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Swift, Catherine E.","contributorId":299495,"corporation":false,"usgs":false,"family":"Swift","given":"Catherine","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":857910,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Rattner, Barnett A. 0000-0003-3676-2843 brattner@usgs.gov","orcid":"https://orcid.org/0000-0003-3676-2843","contributorId":4142,"corporation":false,"usgs":true,"family":"Rattner","given":"Barnett","email":"brattner@usgs.gov","middleInitial":"A.","affiliations":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"preferred":true,"id":857911,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":70238753,"text":"70238753 - 2022 - Ordovician geology of Alaska","interactions":[],"lastModifiedDate":"2022-12-07T12:36:32.458661","indexId":"70238753","displayToPublicDate":"2022-11-28T06:32:58","publicationYear":"2022","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1791,"text":"Geological Society, London, Special Publications","active":true,"publicationSubtype":{"id":10}},"title":"Ordovician geology of Alaska","docAbstract":"<div id=\"abstracts\" data-extent=\"frontmatter\"><div class=\"core-container\"><div>Ordovician rocks, found in northern, east-central, interior and southern Alaska, formed in a variety of depositional and palaeogeographic settings. Shallow- and deep-water strata deposited along the northwestern Laurentian margin occur in east-central Alaska (Yukon River area) and probably correlative rocks crop out to the north in the Porcupine River area. Ordovician strata elsewhere in Alaska are parts of continental or island arc fragments that, as indicated by faunal and detrital zircon data, have been variously displaced. In northern Alaska, Ordovician rocks are included in the Arctic Alaska–Chukotka Microplate (AACM), a composite tectonic entity with a complex history. Some Ordovician strata in the AACM (parts of the North Slope subterrane) represent displaced fragments of the northern Laurentian margin. Coeval strata in southwestern parts of the AACM (York and Seward terranes, Hammond subterrane) share distinctive lithologic and biotic features with Ordovician rocks in interior Alaska (Farewell and related terranes). Ordovician strata in southeastern Alaska (Alexander terrane) also likely compose a composite crustal fragment that accumulated in a complex arc system. Shared features between many of these units suggest similar origins as part of one or more crustal fragments situated in the palaeo-Arctic between Laurentia, Baltica and Siberia during early Paleozoic time.</div></div></div>","language":"English","publisher":"Geological Society of London","doi":"10.1144/SP533-2022-39","usgsCitation":"Dumoulin, J.A., Strauss, J.V., and Repetski, J., 2022, Ordovician geology of Alaska: Geological Society, London, Special Publications, v. 533, 16 p., https://doi.org/10.1144/SP533-2022-39.","productDescription":"16 p.","ipdsId":"IP-137822","costCenters":[{"id":119,"text":"Alaska Science Center Geology Minerals","active":true,"usgs":true}],"links":[{"id":445791,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1144/sp533-2022-39","text":"Publisher Index Page"},{"id":410149,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United 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Julie A. 0000-0003-1754-1287 dumoulin@usgs.gov","orcid":"https://orcid.org/0000-0003-1754-1287","contributorId":203209,"corporation":false,"usgs":true,"family":"Dumoulin","given":"Julie","email":"dumoulin@usgs.gov","middleInitial":"A.","affiliations":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":119,"text":"Alaska Science Center Geology Minerals","active":true,"usgs":true}],"preferred":true,"id":858478,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Strauss, Justin V. 0000-0003-3298-3227","orcid":"https://orcid.org/0000-0003-3298-3227","contributorId":299738,"corporation":false,"usgs":false,"family":"Strauss","given":"Justin","email":"","middleInitial":"V.","affiliations":[{"id":39657,"text":"Dartmouth College","active":true,"usgs":false}],"preferred":false,"id":858479,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Repetski, John 0000-0002-2298-7120","orcid":"https://orcid.org/0000-0002-2298-7120","contributorId":299739,"corporation":false,"usgs":false,"family":"Repetski","given":"John","email":"","affiliations":[{"id":12545,"text":"USGS retired","active":true,"usgs":false}],"preferred":false,"id":858480,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70259410,"text":"70259410 - 2022 - Lava fountain jet noise during the 2018 eruption of fissure 8 of Kīlauea volcano","interactions":[],"lastModifiedDate":"2024-10-07T14:47:49.850068","indexId":"70259410","displayToPublicDate":"2022-11-24T09:40:22","publicationYear":"2022","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":9121,"text":"Frontiers Earth Science Journal","active":true,"publicationSubtype":{"id":10}},"title":"Lava fountain jet noise during the 2018 eruption of fissure 8 of Kīlauea volcano","docAbstract":"<p><span>Real-time monitoring is crucial to assess hazards and mitigate risks of sustained volcanic eruptions that last hours to months or more. Sustained eruptions have been shown to produce a low frequency (infrasonic) form of jet noise. We analyze the lava fountaining at fissure 8 during the 2018 Lower East Rift Zone eruption of Kīlauea volcano, Hawaii, and connect changes in fountain properties with recorded infrasound signals from an array about 500&nbsp;m from the fountain using jet noise scaling laws and visual imagery. Video footage from the eruption reveals a change in lava fountain dynamics from a tall, distinct fountain at the beginning of June to a low fountain with a turbulent, out-pouring lava pond surrounded by a tephra cone by mid-June. During mid-June, the sound pressure level reaches a maximum, and peak frequency drops. We develop a model that uses jet noise scaling relationships to estimate changes in volcanic jet diameter and jet velocity from infrasound sound pressure levels and peak frequencies. The results of this model indicate a decrease in velocity in mid-June which coincides with the decrease in fountain height. Furthermore, the model results suggest an increase in jet diameter, which can be explained by the larger width of the fountain that resembles a turbulent lava pond compared to the distinct fountain at the beginning of June. The agreement between the infrasound-derived and visually observed changes in fountain dynamics suggests that jet noise scaling relationships can be used to monitor lava fountain dynamics using infrasound recordings.</span></p>","language":"English","publisher":"Frontiers Media","doi":"10.3389/feart.2022.1027408","usgsCitation":"Gestrich, J., Fee, D., Matoza, R., Lyons, J.J., Dietterich, H., Cigala, V., Kueppers, U., Patrick, M.R., and Parcheta, C., 2022, Lava fountain jet noise during the 2018 eruption of fissure 8 of Kīlauea volcano: Frontiers Earth Science Journal, v. 10, 1027408, 18 p., https://doi.org/10.3389/feart.2022.1027408.","productDescription":"1027408, 18 p.","ipdsId":"IP-144544","costCenters":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"links":[{"id":467142,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.3389/feart.2022.1027408","text":"Publisher Index Page"},{"id":462663,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Hawaii","otherGeospatial":"Kilauea Volcano","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -155.40616179843389,\n              19.510647106982844\n            ],\n            [\n              -155.40616179843389,\n              19.352324463279487\n            ],\n            [\n              -155.20934216439622,\n              19.352324463279487\n            ],\n            [\n              -155.20934216439622,\n              19.510647106982844\n            ],\n            [\n              -155.40616179843389,\n              19.510647106982844\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  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Robin","contributorId":268788,"corporation":false,"usgs":false,"family":"Matoza","given":"Robin","affiliations":[{"id":7168,"text":"UCSB","active":true,"usgs":false}],"preferred":false,"id":915204,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lyons, John J. 0000-0001-5409-1698 jlyons@usgs.gov","orcid":"https://orcid.org/0000-0001-5409-1698","contributorId":5394,"corporation":false,"usgs":true,"family":"Lyons","given":"John","email":"jlyons@usgs.gov","middleInitial":"J.","affiliations":[{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true},{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":915205,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Dietterich, Hannah R. 0000-0001-7898-4343","orcid":"https://orcid.org/0000-0001-7898-4343","contributorId":212771,"corporation":false,"usgs":true,"family":"Dietterich","given":"Hannah R.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":915206,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Cigala, Valerie","contributorId":344976,"corporation":false,"usgs":false,"family":"Cigala","given":"Valerie","affiliations":[{"id":62362,"text":"LMU","active":true,"usgs":false}],"preferred":false,"id":915207,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Kueppers, Ulrich","contributorId":178534,"corporation":false,"usgs":false,"family":"Kueppers","given":"Ulrich","affiliations":[],"preferred":false,"id":915208,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Patrick, Matthew R. 0000-0002-8042-6639 mpatrick@usgs.gov","orcid":"https://orcid.org/0000-0002-8042-6639","contributorId":2070,"corporation":false,"usgs":true,"family":"Patrick","given":"Matthew","email":"mpatrick@usgs.gov","middleInitial":"R.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":915209,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Parcheta, Carolyn 0000-0001-6556-4630 cparcheta@usgs.gov","orcid":"https://orcid.org/0000-0001-6556-4630","contributorId":215617,"corporation":false,"usgs":true,"family":"Parcheta","given":"Carolyn","email":"cparcheta@usgs.gov","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":915210,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}}
,{"id":70266298,"text":"70266298 - 2022 - Comparative assessment of laboratory-derived thermal maxima of Gila trout (oncorhynchus Gilae) with current stream temperatures","interactions":[],"lastModifiedDate":"2025-05-05T15:16:31.352847","indexId":"70266298","displayToPublicDate":"2022-11-22T00:00:00","publicationYear":"2022","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3451,"text":"Southwestern Naturalist","active":true,"publicationSubtype":{"id":10}},"title":"Comparative assessment of laboratory-derived thermal maxima of Gila trout (oncorhynchus Gilae) with current stream temperatures","docAbstract":"<p><span>Gila trout (</span><i>Oncorhynchus gilae</i><span>) represent an iconic species of the American Southwest. The salmonid has survived extensive logging, livestock grazing, and mining, and is currently threatened by climate change, wildfire, and extended drought. Long-term conservation and recovery of the species and its unique lineages rely on stocking and translocation into historically inhabited streams. Thus, the fish's thermal tolerance is essential in determining suitable habitat and potential vulnerability to a warming climate. We compared a laboratory-derived temperature metric, critical thermal maximum (CTMax), in hatchery-reared Gila trout from three lineages (Main Diamond, South Diamond, and Whiskey Creek) to determine if CTMax differed among the lineages. The average initial (28.9°C,&nbsp;</span><i>SD</i><span>&nbsp;= 0.81°C) and final (29.2°C,&nbsp;</span><i>SD</i><span>&nbsp;= 0.74°C) temperature at loss of righting responses did not differ across the lineages. We compared the CTMax values with stream temperatures across three drainages representative of extant Gila trout populations from spring 2015 to fall 2018. The East Fork Gila River drainage was represented by more extreme stream temperatures. The maximum daily maximum temperature (i.e., single highest temperature) varied from 24.1 to 33.4°C, exceeding CTMax in four of the five streams. The maximum daily temperature varied from 12.1 to 28.6°C, and the mean weekly maximum temperature varied from 19.9 to 31.1°C. Mean weekly maximum temperature in Lower Diamond Creek exceeded CTMax on 11 occasions. Stream temperatures were cooler within the Middle and the West Fork Gila River drainages and did not exceed CTMax. Intermittency loggers within the East Fork Gila River drainage, which supports Main Diamond and South Diamond lineages of Gila trout, recorded over 300 days of intermittency during a drought. Continued long-term monitoring of stream temperature and comparison with CTMax of Gila trout could assist with decisions of which streams in the Gila Drainage are suitable for Gila trout recovery, stocking, and translocation.</span></p><p><span><br data-mce-bogus=\"1\"></span></p>","language":"English","publisher":"BioOne","doi":"10.1894/0038-4909-66.4.317","usgsCitation":"Wallin, T., and Caldwell, C.A., 2022, Comparative assessment of laboratory-derived thermal maxima of Gila trout (oncorhynchus Gilae) with current stream temperatures: Southwestern Naturalist, v. 66, no. 4, p. 317-326, https://doi.org/10.1894/0038-4909-66.4.317.","productDescription":"10 p.","startPage":"317","endPage":"326","ipdsId":"IP-126043","costCenters":[{"id":200,"text":"Coop Res Unit Seattle","active":true,"usgs":true}],"links":[{"id":485385,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New Mexico","otherGeospatial":"United States Fish and Wildlife Service Mora National Fish Hatchery","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -105.34200481715149,\n              35.97866106197155\n            ],\n            [\n              -105.34200481715149,\n              35.973648479810535\n            ],\n            [\n              -105.32973512113179,\n              35.973648479810535\n            ],\n            [\n              -105.32973512113179,\n              35.97866106197155\n            ],\n            [\n              -105.34200481715149,\n              35.97866106197155\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"66","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Wallin, Tyler J.","contributorId":354348,"corporation":false,"usgs":false,"family":"Wallin","given":"Tyler J.","affiliations":[{"id":12628,"text":"New Mexico State University","active":true,"usgs":false}],"preferred":false,"id":935435,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Caldwell, Colleen A. 0000-0002-4730-4867 ccaldwel@usgs.gov","orcid":"https://orcid.org/0000-0002-4730-4867","contributorId":3050,"corporation":false,"usgs":true,"family":"Caldwell","given":"Colleen","email":"ccaldwel@usgs.gov","middleInitial":"A.","affiliations":[{"id":200,"text":"Coop Res Unit Seattle","active":true,"usgs":true}],"preferred":true,"id":935436,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70238581,"text":"70238581 - 2022 - Response of soil respiration to changes in soil temperature and water table level in drained and restored peatlands of the southeastern United States","interactions":[],"lastModifiedDate":"2022-11-30T12:34:57.759355","indexId":"70238581","displayToPublicDate":"2022-11-19T06:32:07","publicationYear":"2022","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1183,"text":"Carbon Balance and Management","active":true,"publicationSubtype":{"id":10}},"title":"Response of soil respiration to changes in soil temperature and water table level in drained and restored peatlands of the southeastern United States","docAbstract":"<p>Extensive drainage of peatlands in the southeastern United States coastal plain for the purposes of agriculture and timber harvesting has led to large releases of soil carbon as carbon dioxide (CO<sub>2</sub>) due to enhanced peat decomposition. Growth in mechanisms that provide financial incentives for reducing emissions from land use and land-use change could increase funding for hydrological restoration that reduces peat CO<sub>2</sub><span>&nbsp;</span>emissions from these ecosystems. Measuring soil respiration and physical drivers across a range of site characteristics and land use histories is valuable for understanding how CO<sub>2</sub><span>&nbsp;</span>emissions from peat decomposition may respond to raising water table levels. We combined measurements of total soil respiration, depth to water table from soil surface, and soil temperature from drained and restored peatlands at three locations in eastern North Carolina and one location in southeastern Virginia to investigate relationships among total soil respiration and physical drivers, and to develop models relating total soil respiration to parameters that can be easily measured and monitored in the field.</p>","language":"English","publisher":"Springer Nature","doi":"10.1186/s13021-022-00219-5","usgsCitation":"Swails, E.E., Ardon, M., Krauss, K., Peralta, A., Emmanuel, R.E., Helton, A., Morse, J., Gutenberg, L., Cormier, N., Shoch, D., Settlemyer, S., Soderholm, E., Boutin, B.P., Peoples, C., and Ward, S., 2022, Response of soil respiration to changes in soil temperature and water table level in drained and restored peatlands of the southeastern United States: Carbon Balance and Management, v. 17, 18, 10 p., https://doi.org/10.1186/s13021-022-00219-5.","productDescription":"18, 10 p.","ipdsId":"IP-127982","costCenters":[{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"links":[{"id":445847,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1186/s13021-022-00219-5","text":"Publisher Index Page"},{"id":409852,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"North Carolina","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -79.74816638869669,\n              34.86985768602176\n            ],\n            [\n              -78.47429331497659,\n              33.323999733572165\n            ],\n            [\n              -76.51955704668092,\n              34.07317373436328\n            ],\n            [\n              -75.17979398638913,\n              35.13971099796244\n            ],\n            [\n              -75.44335393267585,\n              36.61670427026024\n            ],\n            [\n              -78.12288005326047,\n              36.54615713022474\n            ],\n            [\n              -79.74816638869669,\n              34.86985768602176\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"17","noUsgsAuthors":false,"publicationDate":"2022-11-19","publicationStatus":"PW","contributors":{"authors":[{"text":"Swails, Erin E.","contributorId":299540,"corporation":false,"usgs":false,"family":"Swails","given":"Erin","email":"","middleInitial":"E.","affiliations":[{"id":64873,"text":"TerraCarbon LLC, Illinois","active":true,"usgs":false}],"preferred":false,"id":858000,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ardon, Marcelo","contributorId":298014,"corporation":false,"usgs":false,"family":"Ardon","given":"Marcelo","affiliations":[{"id":7091,"text":"North Carolina State University","active":true,"usgs":false}],"preferred":false,"id":858001,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Krauss, Ken 0000-0003-2195-0729","orcid":"https://orcid.org/0000-0003-2195-0729","contributorId":211297,"corporation":false,"usgs":true,"family":"Krauss","given":"Ken","affiliations":[{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"preferred":true,"id":858002,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Peralta, A.L.","contributorId":299541,"corporation":false,"usgs":false,"family":"Peralta","given":"A.L.","email":"","affiliations":[{"id":36317,"text":"East Carolina University","active":true,"usgs":false}],"preferred":false,"id":858003,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Emmanuel, Ryan E.","contributorId":299542,"corporation":false,"usgs":false,"family":"Emmanuel","given":"Ryan","email":"","middleInitial":"E.","affiliations":[{"id":12643,"text":"Duke University","active":true,"usgs":false}],"preferred":false,"id":858004,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Helton, A.M.","contributorId":299543,"corporation":false,"usgs":false,"family":"Helton","given":"A.M.","email":"","affiliations":[{"id":36710,"text":"University of Connecticut","active":true,"usgs":false}],"preferred":false,"id":858005,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Morse, J.L.","contributorId":299544,"corporation":false,"usgs":false,"family":"Morse","given":"J.L.","email":"","affiliations":[{"id":6929,"text":"Portland State University","active":true,"usgs":false}],"preferred":false,"id":858006,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Gutenberg, Laurel","contributorId":217284,"corporation":false,"usgs":false,"family":"Gutenberg","given":"Laurel","email":"","affiliations":[],"preferred":false,"id":858007,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Cormier, Nicole 0000-0003-2453-9900","orcid":"https://orcid.org/0000-0003-2453-9900","contributorId":214726,"corporation":false,"usgs":false,"family":"Cormier","given":"Nicole","affiliations":[{"id":16788,"text":"Macquarie University","active":true,"usgs":false}],"preferred":false,"id":858008,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Shoch, D.","contributorId":299545,"corporation":false,"usgs":false,"family":"Shoch","given":"D.","email":"","affiliations":[{"id":64873,"text":"TerraCarbon LLC, Illinois","active":true,"usgs":false}],"preferred":false,"id":858009,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Settlemyer, Scott","contributorId":299546,"corporation":false,"usgs":false,"family":"Settlemyer","given":"Scott","email":"","affiliations":[{"id":64873,"text":"TerraCarbon LLC, Illinois","active":true,"usgs":false}],"preferred":false,"id":858010,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Soderholm, Eric","contributorId":298011,"corporation":false,"usgs":false,"family":"Soderholm","given":"Eric","email":"","affiliations":[{"id":7041,"text":"The Nature Conservancy","active":true,"usgs":false}],"preferred":false,"id":858011,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Boutin, Brian P.","contributorId":299547,"corporation":false,"usgs":false,"family":"Boutin","given":"Brian","email":"","middleInitial":"P.","affiliations":[{"id":7041,"text":"The Nature Conservancy","active":true,"usgs":false}],"preferred":false,"id":858012,"contributorType":{"id":1,"text":"Authors"},"rank":13},{"text":"Peoples, Chuck","contributorId":299548,"corporation":false,"usgs":false,"family":"Peoples","given":"Chuck","email":"","affiliations":[{"id":7041,"text":"The Nature Conservancy","active":true,"usgs":false}],"preferred":false,"id":858013,"contributorType":{"id":1,"text":"Authors"},"rank":14},{"text":"Ward, Sara","contributorId":299549,"corporation":false,"usgs":false,"family":"Ward","given":"Sara","email":"","affiliations":[{"id":36188,"text":"U.S. Fish and Wildlife Service","active":true,"usgs":false}],"preferred":false,"id":858014,"contributorType":{"id":1,"text":"Authors"},"rank":15}]}}
,{"id":70248899,"text":"70248899 - 2022 - Applying consequence-driven scenario selection to lifelines","interactions":[],"lastModifiedDate":"2023-09-25T14:52:47.193278","indexId":"70248899","displayToPublicDate":"2022-11-16T09:47:33","publicationYear":"2022","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Applying consequence-driven scenario selection to lifelines","docAbstract":"<p><span>We present a new consequence-driven framework for earthquake scenario selection. For emergency managers, utility operators, policy makers, and other stakeholders, a scenario-based seismic risk assessment is often necessary for the purpose of emergency management and planning. In developing a scientifically defensible scenario, stakeholders can simulate a realistic event in order to pre-identify vulnerabilities in the system and support action to address these vulnerabilities. Selecting scenarios is particularly challenging for important population centers and critical infrastructure in stable tectonic environments, such as in the central and eastern United States, where uncertain long-term seismicity and unknown faults offer inadequate constraints. Notably, significant events in these so-called stable regions do occur (e.g.,&nbsp;Nahanni, Canada, 1985, M6.9; Tennant Creek, Australia, 1998, M6.7). In regions of low seismicity, even moderate events can be consequential due to the higher vulnerability of buildings typical of such regions when compared to regions of higher seismicity. Furthermore, communicating seismic risk to stakeholders and the general public in these regions can be especially challenging due to the complexities of characterizing the hazard level. This framework has been developed to address these challenges for scenario selection in low seismic hazard regions. In this new approach, the analysis begins instead with the explicit definition of a consequence of concern to the specific stakeholder. This can range from a definition of loss (in lives, dollars, or another metric of interest), or a performance metric for critical infrastructure. The framework leverages United States Geological Survey software to run the hazard and consequence analysis. Driven by this stakeholder-defined consequence, an inversion analysis generates a complete event set of candidate scenarios that could breach this consequence. The final selection of a scenario, or family of scenarios, is then scientifically informed, but not limited by our lack of constraints in characterizing the hazard.</span></p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Lifelines","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"Lifelines 2022","conferenceDate":"January 31 - February 11, 2022","conferenceLocation":"Online","language":"English","publisher":"American Society of Civil Engineers","usgsCitation":"Lin, Y.C., Wald, D.J., Thompson, E.M., and Lallemant, D., 2022, Applying consequence-driven scenario selection to lifelines, <i>in</i> Lifelines, Online, January 31 - February 11, 2022, p. 411-422.","productDescription":"12 p.","startPage":"411","endPage":"422","ipdsId":"IP-130792","costCenters":[{"id":78686,"text":"Geologic Hazards Science Center - Seismology / Geomagnetism","active":true,"usgs":true}],"links":[{"id":421131,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":421117,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://ascelibrary.org/doi/abs/10.1061/9780784484449.036","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Lin, Yolanda C 0000-0002-0423-4248","orcid":"https://orcid.org/0000-0002-0423-4248","contributorId":317878,"corporation":false,"usgs":false,"family":"Lin","given":"Yolanda","email":"","middleInitial":"C","affiliations":[{"id":36307,"text":"University of New Mexico","active":true,"usgs":false}],"preferred":false,"id":884130,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wald, David J. 0000-0002-1454-4514 wald@usgs.gov","orcid":"https://orcid.org/0000-0002-1454-4514","contributorId":795,"corporation":false,"usgs":true,"family":"Wald","given":"David","email":"wald@usgs.gov","middleInitial":"J.","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":true,"id":884131,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Thompson, Eric M. 0000-0002-6943-4806 emthompson@usgs.gov","orcid":"https://orcid.org/0000-0002-6943-4806","contributorId":150897,"corporation":false,"usgs":true,"family":"Thompson","given":"Eric","email":"emthompson@usgs.gov","middleInitial":"M.","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":true,"id":884132,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lallemant, David 0000-0001-5759-9972","orcid":"https://orcid.org/0000-0001-5759-9972","contributorId":290680,"corporation":false,"usgs":false,"family":"Lallemant","given":"David","email":"","affiliations":[{"id":16631,"text":"Nanyang Technological University","active":true,"usgs":false}],"preferred":false,"id":884133,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70240713,"text":"70240713 - 2022 - Grasshopper species composition differs between prairie dog colonies and undisturbed sites in a sagebrush grassland","interactions":[],"lastModifiedDate":"2023-02-16T12:54:27.069165","indexId":"70240713","displayToPublicDate":"2022-11-16T06:52:32","publicationYear":"2022","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2556,"text":"Journal of the Kansas Entomological Society","active":true,"publicationSubtype":{"id":10}},"title":"Grasshopper species composition differs between prairie dog colonies and undisturbed sites in a sagebrush grassland","docAbstract":"<div class=\"div0\"><div class=\"row ArticleContentRow\"><p id=\"ID0EF\" class=\"first\">Grasshoppers are major consumers of plant biomass in grassland and shrubland ecosystems. While often considered generalists, grasshopper species have differing habitat preferences and interactions with other consumers in grasslands. There are conflicting accounts of how prairie dog colonies and differences in vegetation impact grasshopper abundance and composition. We conducted a landscape-scale survey of grasshopper communities, plant communities, and prairie dogs in a grassland/shrubland ecosystem in eastern Wyoming. Over the study landscape, spurthroat grasshoppers (Melanoplinae) were associated with lower sagebrush cover and lower cover of C3 perennial graminoids, bandwing grasshoppers (Oedipodinae) were associated with low-lying areas with a high cover of C4 grasses and a low cover of cheatgrass, and slantface grasshoppers (Gomphocerinae) were associated with low vegetation height. Prairie dogs, presumably because of their effects on vegetation, had different impacts on different groups of grasshoppers. Melanoplinae grasshoppers, the Wyoming toothpick grasshopper (<i>Paropomala wyomingensis</i><span>&nbsp;</span>Thomas), and grasshoppers with early-season phenology were associated with prairie dog colonies. However, because some species of grasshoppers were positively and others negatively associated with prairie dogs, the net effect of prairie dogs on total grasshopper biomass was neutral. Thus, to determine the role of grasshoppers in prairie ecosystems, it will be important to determine whether there is functional equivalence of grasshopper species in consuming plant biomass and as food for vertebrates.</p></div></div>","language":"English","publisher":"BioOne","doi":"10.2317/0022-8567-94.3.183","usgsCitation":"Pearse, I., Duchardt, C.J., Legg, L., and Porensky, L., 2022, Grasshopper species composition differs between prairie dog colonies and undisturbed sites in a sagebrush grassland: Journal of the Kansas Entomological Society, v. 94, no. 3, p. 183-198, https://doi.org/10.2317/0022-8567-94.3.183.","productDescription":"16 p.","startPage":"183","endPage":"198","ipdsId":"IP-115435","costCenters":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"links":[{"id":435615,"rank":0,"type":{"id":30,"text":"Data Release"},"url":"https://doi.org/10.5066/P9ICAONC","text":"USGS data release","linkHelpText":"Data on grasshopper composition in the Thunder Basin National Grassland, Wyoming, USA"},{"id":413127,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Wyoming","otherGeospatial":"Thunder Basin National Grassland","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -105.95139261133112,\n              44.36517972504339\n            ],\n            [\n              -105.95139261133112,\n              42.95108909336483\n            ],\n            [\n              -104.15040553350202,\n              42.95108909336483\n            ],\n            [\n              -104.15040553350202,\n              44.36517972504339\n            ],\n            [\n              -105.95139261133112,\n              44.36517972504339\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"94","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Pearse, Ian S. 0000-0001-7098-0495","orcid":"https://orcid.org/0000-0001-7098-0495","contributorId":211154,"corporation":false,"usgs":true,"family":"Pearse","given":"Ian","middleInitial":"S.","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":true,"id":864400,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Duchardt, Courtney J. 0000-0003-4563-0199","orcid":"https://orcid.org/0000-0003-4563-0199","contributorId":239754,"corporation":false,"usgs":false,"family":"Duchardt","given":"Courtney","middleInitial":"J.","affiliations":[{"id":48000,"text":"U Wyoming","active":true,"usgs":false}],"preferred":false,"id":864401,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Legg, Lillian","contributorId":302413,"corporation":false,"usgs":false,"family":"Legg","given":"Lillian","email":"","affiliations":[{"id":6621,"text":"Colorado State University","active":true,"usgs":false}],"preferred":false,"id":864402,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Porensky, Lauren M.","contributorId":264925,"corporation":false,"usgs":false,"family":"Porensky","given":"Lauren M.","affiliations":[{"id":36589,"text":"USDA","active":true,"usgs":false}],"preferred":false,"id":864403,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70238701,"text":"70238701 - 2022 - Evidence of active Quaternary deformation on the Great Valley fault system near Winters, northern California","interactions":[],"lastModifiedDate":"2022-12-06T12:49:02.272797","indexId":"70238701","displayToPublicDate":"2022-11-14T06:43:35","publicationYear":"2022","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":10542,"text":"The Seismic Record","active":true,"publicationSubtype":{"id":10}},"title":"Evidence of active Quaternary deformation on the Great Valley fault system near Winters, northern California","docAbstract":"<div id=\"135158858\" class=\"article-section-wrapper js-article-section js-content-section  \" data-section-parent-id=\"0\"><p>The Great Valley fault system defines the tectonic boundary between the Coast Ranges and the Central Valley in California, is active throughout the Quaternary, and has been the source of several significant (<strong>M</strong><span>&nbsp;</span>&gt; 6) historic earthquakes, including the 1983<span>&nbsp;</span><strong>M</strong>&nbsp;6.5 Coalinga earthquake and the 1892 Vacaville–Winters earthquake sequence. However, the locations and geometries of individual faults in the Great Valley fault system are poorly constrained, and fault slip rates and paleoearthquake chronology are largely unknown. Here, we report geomorphic and subsurface geophysical evidence of surface‐deforming displacement on a strand of the Great Valley fault system west of Winters, California. Detailed geomorphic mapping and a high‐resolution seismic reflection and tomography survey along an ∼800&nbsp;m profile across the Bigelow Hills document a fault, which we call the West Winters strand of the Great Valley fault system, with apparent east side‐up displacement of surficial geologic units. These data together suggest that the West Winters strand is active in the latest Quaternary. Together with local reports from the time, this raises the possibility that the West Winters strand may have ruptured and deformed the surface during the 1892<span>&nbsp;</span><strong>M</strong>&nbsp;6 Vacaville–Winters earthquake sequence. Future earthquakes with vertical displacement on this and Great Valley fault system structures could have significant hazard implications, given the region’s low relief and the presence of major water conveyance infrastructure.</p></div>","language":"English","publisher":"Seismological Society of America","doi":"10.1785/0320220029","usgsCitation":"Trexler, C.C., Morelan, A.E., Catchings, R.D., Goldman, M., and Willard, J., 2022, Evidence of active Quaternary deformation on the Great Valley fault system near Winters, northern California: The Seismic Record, v. 2, no. 4, p. 248-259, https://doi.org/10.1785/0320220029.","productDescription":"12 p.","startPage":"248","endPage":"259","ipdsId":"IP-143538","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"links":[{"id":445884,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1785/0320220029","text":"Publisher Index Page"},{"id":410101,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","city":"Winters","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -122.10370420453376,\n              38.58785589344208\n            ],\n            [\n              -122.10370420453376,\n              38.45025735247489\n            ],\n            [\n              -121.89888336029207,\n              38.45025735247489\n            ],\n            [\n              -121.89888336029207,\n              38.58785589344208\n            ],\n            [\n              -122.10370420453376,\n              38.58785589344208\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"2","issue":"4","noUsgsAuthors":false,"publicationDate":"2022-11-14","publicationStatus":"PW","contributors":{"authors":[{"text":"Trexler, Charles Cashman 0000-0001-5046-9729","orcid":"https://orcid.org/0000-0001-5046-9729","contributorId":257823,"corporation":false,"usgs":true,"family":"Trexler","given":"Charles","email":"","middleInitial":"Cashman","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":858302,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Morelan, Alexander E.","contributorId":299686,"corporation":false,"usgs":false,"family":"Morelan","given":"Alexander","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":858303,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Catchings, Rufus D. 0000-0002-5191-6102 catching@usgs.gov","orcid":"https://orcid.org/0000-0002-5191-6102","contributorId":1519,"corporation":false,"usgs":true,"family":"Catchings","given":"Rufus","email":"catching@usgs.gov","middleInitial":"D.","affiliations":[{"id":234,"text":"Earthquake Hazards Program","active":true,"usgs":true},{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":858304,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Goldman, Mark 0000-0002-0802-829X","orcid":"https://orcid.org/0000-0002-0802-829X","contributorId":205863,"corporation":false,"usgs":true,"family":"Goldman","given":"Mark","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true},{"id":234,"text":"Earthquake Hazards Program","active":true,"usgs":true}],"preferred":true,"id":858305,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Willard, Jack 0000-0002-4653-7423","orcid":"https://orcid.org/0000-0002-4653-7423","contributorId":299663,"corporation":false,"usgs":false,"family":"Willard","given":"Jack","email":"","affiliations":[{"id":64922,"text":"Earthquake Science Center","active":true,"usgs":false}],"preferred":false,"id":858306,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70238682,"text":"70238682 - 2022 - Seismic evidence for magmatic underplating along the Kodiak-Bowie Seamount Chain, Gulf of Alaska","interactions":[],"lastModifiedDate":"2022-12-05T12:39:45.220241","indexId":"70238682","displayToPublicDate":"2022-11-14T06:37:46","publicationYear":"2022","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3525,"text":"Tectonophysics","active":true,"publicationSubtype":{"id":10}},"title":"Seismic evidence for magmatic underplating along the Kodiak-Bowie Seamount Chain, Gulf of Alaska","docAbstract":"<div id=\"abstracts\" class=\"Abstracts u-font-serif\"><div id=\"ab0005\" class=\"abstract author\" lang=\"en\"><div id=\"as0005\"><p id=\"sp0045\">Oceanic crust formed at mid-ocean ridges may be later modified by off-ridge magmatism forming seamounts, guyots, and islands. We investigate processes associated with seamount formation in the Gulf of Alaska Seamount Province using two coincident seismic reflection/wide-angle profiles. A north-south profile crosses the Kodiak-Bowie Seamount Chain and Aja fracture zone (FZ), and an orthogonal east-west profile is located about 90&nbsp;km south of the seamount chain over Pacific plate oceanic crust. Structure along the profile away from the seamount chain is consistent with typical oceanic crust. Crust in our study region is thinnest (about 5.6&nbsp;km) at the Aja FZ. Unlike observations from active transform faults, no low-velocity anomaly is observed at the Aja FZ suggesting that the crustal velocities have recovered to normal values through crack closure and crack healing. Higher lower crustal velocities (∼7.3 and&nbsp;&gt;&nbsp;7.5&nbsp;km/s) and thicker crust (∼8.5 and&nbsp;∼7.0&nbsp;km) are observed near the Pratt and Durgin Seamounts and at the intersection of the Kodiak-Bowie Seamount Chain linear trend, respectively. These observations are attributed to magmatic underplating associated with seamount province magmatism. Lithospheric thickness variations across the Aja FZ may form a barrier or impediment to magmatic flow. The thickest crust (8.5&nbsp;km) along our two profiles is located on the younger side of the FZ, and we suggest that the majority of magmatism jumped south of the Aja FZ when thinner lithosphere was encountered by the Bowie hot spot. The crustal structure near the Kodiak-Bowie Seamount Chain is most similar to that of other seamounts and guyots that formed on similarly young lithosphere (8–12&nbsp;Ma). Our results suggest that lithospheric thickness at the time of hot spot interaction has a large control on magmatic underplating at seamounts and seamount provinces.</p></div></div></div>","language":"English","publisher":"Elsevier","doi":"10.1016/j.tecto.2022.229639","usgsCitation":"Christeson, G.L., Gulick, S., Walton, M.A., and Barth, G., 2022, Seismic evidence for magmatic underplating along the Kodiak-Bowie Seamount Chain, Gulf of Alaska: Tectonophysics, v. 845, 229639, 9 p., https://doi.org/10.1016/j.tecto.2022.229639.","productDescription":"229639, 9 p.","ipdsId":"IP-142150","costCenters":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":445886,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1016/j.tecto.2022.229639","text":"Publisher Index Page"},{"id":410045,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Kodiak-Bowie Seamount Chain","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -134.8923517491249,\n              53.57343667670415\n            ],\n            [\n              -134.8923517491249,\n              61.08239410939083\n            ],\n            [\n              -155.66966084808274,\n              61.08239410939083\n            ],\n            [\n              -155.66966084808274,\n              53.57343667670415\n            ],\n            [\n              -134.8923517491249,\n              53.57343667670415\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"845","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Christeson, Gail L.","contributorId":147203,"corporation":false,"usgs":false,"family":"Christeson","given":"Gail","email":"","middleInitial":"L.","affiliations":[{"id":13603,"text":"University of Texas, Austin","active":true,"usgs":false}],"preferred":false,"id":858251,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gulick, Sean P.S. 0000-0003-4740-9068","orcid":"https://orcid.org/0000-0003-4740-9068","contributorId":139644,"corporation":false,"usgs":false,"family":"Gulick","given":"Sean P.S.","affiliations":[{"id":12811,"text":"Institute for Geophysics, Jackson School of Geosciences, University of Texas, Austin","active":true,"usgs":false}],"preferred":false,"id":858252,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Walton, Maureen A. L.","contributorId":147200,"corporation":false,"usgs":false,"family":"Walton","given":"Maureen","email":"","middleInitial":"A. L.","affiliations":[{"id":13603,"text":"University of Texas, Austin","active":true,"usgs":false}],"preferred":false,"id":858253,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Barth, Ginger 0000-0003-0867-7799 gbarth@usgs.gov","orcid":"https://orcid.org/0000-0003-0867-7799","contributorId":264955,"corporation":false,"usgs":true,"family":"Barth","given":"Ginger","email":"gbarth@usgs.gov","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":858254,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
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