{"pageNumber":"1726","pageRowStart":"43125","pageSize":"25","recordCount":184617,"records":[{"id":70157113,"text":"70157113 - 2011 - Carbofuran: Toxicity, diagnosing poisoning and rehabilitation of poisoned birds","interactions":[],"lastModifiedDate":"2023-10-20T16:43:11.339186","indexId":"70157113","displayToPublicDate":"2011-11-21T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"chapter":"2","title":"Carbofuran: Toxicity, diagnosing poisoning and rehabilitation of poisoned birds","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Carbofuran and wildlife poisoning global perspectives and forensic approaches","language":"English","publisher":"Wiley-Blackwell","publisherLocation":"Chichester, West Sussex; Hoboken, NJ","doi":"10.1002/9781119998532.ch2","usgsCitation":"Mineau, P., Porter, S., and Meteyer, C.U., 2011, Carbofuran: Toxicity, diagnosing poisoning and rehabilitation of poisoned birds, chap. 2 <i>of</i> Carbofuran and wildlife poisoning global perspectives and forensic approaches, p. 19-38, https://doi.org/10.1002/9781119998532.ch2.","productDescription":"20 p.","startPage":"19","endPage":"38","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-037394","costCenters":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"links":[{"id":307966,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationDate":"2011-11-21","publicationStatus":"PW","scienceBaseUri":"560bb63fe4b058f706e53b58","contributors":{"editors":[{"text":"Richards, Ngaio","contributorId":147440,"corporation":false,"usgs":false,"family":"Richards","given":"Ngaio","email":"","affiliations":[],"preferred":false,"id":571703,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Mineau, Pierre","contributorId":147441,"corporation":false,"usgs":false,"family":"Mineau","given":"Pierre","email":"","affiliations":[],"preferred":false,"id":571700,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Porter, Stuart","contributorId":147442,"corporation":false,"usgs":false,"family":"Porter","given":"Stuart","email":"","affiliations":[],"preferred":false,"id":571701,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Meteyer, Carol Uphoff 0000-0002-4007-3410","orcid":"https://orcid.org/0000-0002-4007-3410","contributorId":78079,"corporation":false,"usgs":true,"family":"Meteyer","given":"Carol","email":"","middleInitial":"Uphoff","affiliations":[],"preferred":false,"id":571702,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70006018,"text":"sim3156 - 2011 - Geologic map of the Bailey 30' x 60' quadrangle, North-Central Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:15:58","indexId":"sim3156","displayToPublicDate":"2011-11-21T00:00:00","publicationYear":"2011","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":"3156","title":"Geologic map of the Bailey 30' x 60' quadrangle, North-Central Colorado","docAbstract":"The Bailey, Colo. 1:100,000-scale quadrangle lies within two physiographic and geologic provinces in central Colorado: 1) the Front Range and 2) South Park. Most of the Front Range is composed of Proterozoic rocks ranging in age from 1,790 Ma to 1,074 Ma. Along the eastern flanks and within the Denver Basin, sedimentary rocks ranging from Pennsylvanian to Cretaceous are deformed and steeply tilted to the east. Upper Cretaceous through Paleocene rocks were deposited in the foreland (that is, the Front Range eastern flank) and hinterland (that is, South Park) of this thrust and reverse fault system developed during the Late Cretaceous to Paleocene Laramide orogeny. Within South Park, rocks range in age from Pennsylvanian to Miocene with Quaternary deposits indicating tectonic subsidence of the basin. These rocks record five major geologic episodes: 1) the Paleozoic Anasazi uplift that formed the Ancestral Rockies, 2) the Late Cretaceous to Paleocene Laramide orogeny, 3) widespread Eocene to Oligocene volcanism, 4) Oligocene-Quaternary tectonics, and 5) Quaternary glacial episodes.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sim3156","usgsCitation":"Ruleman, C., Bohannon, R.G., Bryant, B., Shroba, R.R., and Premo, W.R., 2011, Geologic map of the Bailey 30' x 60' quadrangle, North-Central Colorado: U.S. Geological Survey Scientific Investigations Map 3156, iv, 38 p.; Map: ; Data Directory, https://doi.org/10.3133/sim3156.","productDescription":"iv, 38 p.; Map: ; Data Directory","startPage":"i","endPage":"38","numberOfPages":"42","additionalOnlineFiles":"Y","costCenters":[{"id":308,"text":"Geology and Environmental Change Science Center","active":false,"usgs":true}],"links":[{"id":116787,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/sim_3156.png"},{"id":110878,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sim/3156/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Colorado","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db69812e","contributors":{"authors":[{"text":"Ruleman, Chester A.","contributorId":41533,"corporation":false,"usgs":true,"family":"Ruleman","given":"Chester A.","affiliations":[],"preferred":false,"id":353681,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bohannon, Robert G. rbohannon@usgs.gov","contributorId":2255,"corporation":false,"usgs":true,"family":"Bohannon","given":"Robert","email":"rbohannon@usgs.gov","middleInitial":"G.","affiliations":[],"preferred":true,"id":353680,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bryant, Bruce bbryant@usgs.gov","contributorId":1355,"corporation":false,"usgs":true,"family":"Bryant","given":"Bruce","email":"bbryant@usgs.gov","affiliations":[],"preferred":false,"id":353678,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Shroba, Ralph R. 0000-0002-2664-1813 rshroba@usgs.gov","orcid":"https://orcid.org/0000-0002-2664-1813","contributorId":1266,"corporation":false,"usgs":true,"family":"Shroba","given":"Ralph","email":"rshroba@usgs.gov","middleInitial":"R.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":353677,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"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":353679,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70005861,"text":"70005861 - 2011 - Mercury bioaccumulation and biomagnification in Ozark stream ecosystems","interactions":[],"lastModifiedDate":"2020-01-11T10:21:13","indexId":"70005861","displayToPublicDate":"2011-11-21T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1480,"text":"Ecotoxicology and Environmental Safety","active":true,"publicationSubtype":{"id":10}},"title":"Mercury bioaccumulation and biomagnification in Ozark stream ecosystems","docAbstract":"<p><span>Crayfish (</span><i>Orconectes</i><span> spp.), Asian clam (</span><i>Corbicula fluminea</i><span>), northern hog sucker (hog sucker; </span><i>Hypentelium nigricans</i><span>), and smallmouth bass (smallmouth; </span><i>Micropterus dolomieu</i><span>) from streams in southeastern Missouri (USA) were analyzed for total mercury (HgT) and for stable isotopes of carbon (δ</span><sup>13</sup><span>C), nitrogen (δ</span><sup>15</sup><span>N), and sulfur (δ</span><sup>34</sup><span>S) to discern Hg transfer pathways. HgT concentrations were generally lowest in crayfish (0.005–0.112&nbsp;μg/g&nbsp;dw) and highest in smallmouth (0.093–4.041&nbsp;μg/g&nbsp;dw), as was δ</span><sup>15</sup><span>N. HgT was also lower and δ</span><sup>15</sup><span>N was higher in all biota from a stream draining a more heavily populated historical lead–zinc mining area than from similar sites with mostly undeveloped forested watersheds. δ</span><sup>13</sup><span>C in biota was lowest at spring-influenced sites, reflecting CO</span><sub>2</sub><span> inputs and temperature influences, and δ</span><sup>34</sup><span>S increased from south to north in all taxa. However, HgT was not strongly correlated with either δ</span><sup>13</sup><span>C or δ</span><sup>34</sup><span>S in biota. Trophic position (TP) computed from crayfish δ</span><sup>15</sup><span>N was lower in hog suckers (mean=2.8) than in smallmouth (mean=3.2), but not at all sites. HgT, δ</span><sup>13</sup><span>C, δ</span><sup>34</sup><span>S, and TP in hog suckers increased with total length (length) at some sites, indicating site-specific ontogenetic diet shifts. Changes with length were less evident in smallmouth. Length-adjusted HgT site means in both species were strongly correlated with HgT in crayfish (</span><i>r</i><sup><i>2</i></sup><span>=0.97, </span><i>P</i><span>&lt;0.01), but not with HgT in </span><i>Corbicula</i><span> (</span><i>r</i><sup>2</sup><span>=0.02, </span><i>P</i><span>&gt;0.05). ANCOVA and regression models incorporating only TP and, for hog suckers, length, accurately and precisely predicted HgT concentrations in both fish species from all locations. Although low compared to many areas of the USA, HgT (and therefore methylmercury) concentrations in smallmouth and hog suckers are sufficiently high to represent a threat to human health and wildlife. Our data indicate that in Ozark streams, Hg concentrations in crayfish are at least partly determined by their diet, with concentrations in hog suckers, smallmouth, and possibly other higher-level consumers largely determined by concentrations in crayfish and other primary and secondary consumers, fish growth rates, and TP.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.ecoenv.2011.08.008","usgsCitation":"Schmitt, C.J., Stricker, C.A., and Brumbaugh, W.G., 2011, Mercury bioaccumulation and biomagnification in Ozark stream ecosystems: Ecotoxicology and Environmental Safety, v. 74, no. 8, p. 2215-2224, https://doi.org/10.1016/j.ecoenv.2011.08.008.","productDescription":"10 p.","startPage":"2215","endPage":"2224","numberOfPages":"10","costCenters":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true},{"id":34983,"text":"Contaminant Biology Program","active":true,"usgs":true}],"links":[{"id":204378,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Missouri","otherGeospatial":"Ozark Mountains","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -90.5,\n              38.0\n            ],\n            [\n              -91.5,\n              38.0\n            ],\n            [\n              -91.5,\n              36.5\n            ],\n            [\n              -90.5,\n              36.5\n            ],\n            [\n              -90.5,\n              38.0\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"74","issue":"8","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ae4b07f02db624b4d","contributors":{"authors":[{"text":"Schmitt, Christopher J. 0000-0001-6804-2360 cjschmitt@usgs.gov","orcid":"https://orcid.org/0000-0001-6804-2360","contributorId":491,"corporation":false,"usgs":true,"family":"Schmitt","given":"Christopher","email":"cjschmitt@usgs.gov","middleInitial":"J.","affiliations":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"preferred":true,"id":353420,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stricker, Craig A. 0000-0002-5031-9437 cstricker@usgs.gov","orcid":"https://orcid.org/0000-0002-5031-9437","contributorId":1097,"corporation":false,"usgs":true,"family":"Stricker","given":"Craig","email":"cstricker@usgs.gov","middleInitial":"A.","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":true,"id":353422,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brumbaugh, William G. 0000-0003-0081-375X bbrumbaugh@usgs.gov","orcid":"https://orcid.org/0000-0003-0081-375X","contributorId":493,"corporation":false,"usgs":true,"family":"Brumbaugh","given":"William","email":"bbrumbaugh@usgs.gov","middleInitial":"G.","affiliations":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"preferred":true,"id":353421,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70003655,"text":"70003655 - 2011 - Enhanced decomposition offsets enhanced productivity and soil carbon accumulation in coastal wetlands responding to climate change","interactions":[],"lastModifiedDate":"2021-01-06T16:12:18.623819","indexId":"70003655","displayToPublicDate":"2011-11-20T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1011,"text":"Biogeosciences","active":true,"publicationSubtype":{"id":10}},"title":"Enhanced decomposition offsets enhanced productivity and soil carbon accumulation in coastal wetlands responding to climate change","docAbstract":"<p><span>Coastal wetlands are responsible for about half of all carbon burial in oceans, and their persistence as a valuable ecosystem depends largely on the ability to accumulate organic material at rates equivalent to relative sea level rise. Recent work suggests that elevated CO</span><sub>2</sub><span>&nbsp;and temperature warming will increase organic matter productivity and the ability of marshes to survive sea level rise. However, we find in a series of preliminary experiments that organic decomposition rates increase by about 20% per degree of warming. Our measured temperature sensitivity is similar to studies from terrestrial systems, three times as high as the response of salt marsh productivity to temperature warming, and greater than the productivity response associated with elevated CO</span><sub>2</sub><span>&nbsp;in C</span><sub>3</sub><span>&nbsp;marsh plants. Although the experiments were simple and of short duration, they suggest that enhanced CO</span><sub>2</sub><span>&nbsp;and warmer temperatures could actually make marshes less resilient to sea level rise, and tend to promote a release of soil carbon. Simple projections indicate that elevated temperatures will increase rates of sea level rise more than any acceleration in organic matter accumulation, suggesting the possibility of a positive feedback between climate, sea level rise, and carbon emissions in coastal environments.</span></p>","language":"English","publisher":"Copernicus GmbH","publisherLocation":"Goettingen, Germany","doi":"10.5194/bg-8-987-2011","usgsCitation":"Kirwan, M.L., and Blum, L.K., 2011, Enhanced decomposition offsets enhanced productivity and soil carbon accumulation in coastal wetlands responding to climate change: Biogeosciences, v. 8, no. 4, p. 987-993, https://doi.org/10.5194/bg-8-987-2011.","productDescription":"7 p.","startPage":"987","endPage":"993","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":474895,"rank":1,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.5194/bg-8-987-2011","text":"Publisher Index Page"},{"id":204250,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Virginia","otherGeospatial":"Phillips Creek","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -75.94470977783203,\n              37.38979975341983\n            ],\n            [\n              -75.83415985107422,\n              37.38979975341983\n            ],\n            [\n              -75.83415985107422,\n              37.47349573285831\n            ],\n            [\n              -75.94470977783203,\n              37.47349573285831\n            ],\n            [\n              -75.94470977783203,\n              37.38979975341983\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"8","issue":"4","noUsgsAuthors":false,"publicationDate":"2011-04-21","publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db60268c","contributors":{"authors":[{"text":"Kirwan, M. L.","contributorId":74094,"corporation":false,"usgs":true,"family":"Kirwan","given":"M.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":348194,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Blum, L. K.","contributorId":86208,"corporation":false,"usgs":false,"family":"Blum","given":"L.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":348195,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70005830,"text":"70005830 - 2011 - First record of interspecific breeding of Least Bell's Vireo and White-eyed Vireo","interactions":[],"lastModifiedDate":"2021-05-21T19:50:06.977939","indexId":"70005830","displayToPublicDate":"2011-11-20T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3784,"text":"Wilson Journal of Ornithology","active":true,"publicationSubtype":{"id":10}},"title":"First record of interspecific breeding of Least Bell's Vireo and White-eyed Vireo","docAbstract":"<p><span>We provide the first known documentation of a male Least Bell's Vireo (</span><i><span class=\"genus-species\">Vireo bellii pusillus</span></i><span>) breeding with a female White-eyed Vireo (</span><i><span class=\"genus-species\">V. griseus</span></i><span>) and the first report of a White-eyed Vireo breeding in California at the San Luis Rey River, Oceanside, San Diego County. We discovered the pair building a nest on 12 May 2010. The female laid four eggs, and the pair successfully raised and fledged four nestlings. We collected DNA samples from each nestling and the female during the nestling stage and banded them with a numbered federal leg band for future identification. We obtained detailed nest measurements after fledging and monitored the territory for further nesting attempts. No additional nesting attempts were detected.</span></p>","language":"English","publisher":"The Wilson Ornithological Society","publisherLocation":"Waco, TX","doi":"10.1676/10-184.1","usgsCitation":"Blundell, M.A., and Kus, B., 2011, First record of interspecific breeding of Least Bell's Vireo and White-eyed Vireo: Wilson Journal of Ornithology, v. 123, no. 3, p. 628-631, https://doi.org/10.1676/10-184.1.","productDescription":"4 p.","startPage":"628","endPage":"631","numberOfPages":"4","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":204319,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","county":"San Diego County","city":"Oceanside","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -117.41638183593749,\n              33.114549382824535\n            ],\n            [\n              -117.26943969726562,\n              33.114549382824535\n            ],\n            [\n              -117.26943969726562,\n              33.23868752757414\n            ],\n            [\n              -117.41638183593749,\n              33.23868752757414\n            ],\n            [\n              -117.41638183593749,\n              33.114549382824535\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"123","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f9e4b07f02db5f3c88","contributors":{"authors":[{"text":"Blundell, Melissa A.","contributorId":88476,"corporation":false,"usgs":true,"family":"Blundell","given":"Melissa","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":353320,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kus, Barbara E. 0000-0002-3679-3044 barbara_kus@usgs.gov","orcid":"https://orcid.org/0000-0002-3679-3044","contributorId":3026,"corporation":false,"usgs":true,"family":"Kus","given":"Barbara E.","email":"barbara_kus@usgs.gov","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":true,"id":353319,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70005998,"text":"70005998 - 2011 - 40Ar∗ loss in experimentally deformed muscovite and biotite with implications for 40Ar/39Ar geochronology of naturally deformed rocks","interactions":[],"lastModifiedDate":"2021-02-25T20:34:44.896532","indexId":"70005998","displayToPublicDate":"2011-11-20T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1759,"text":"Geochimica et Cosmochimica Acta","active":true,"publicationSubtype":{"id":10}},"displayTitle":"<sup>40</sup>Ar* loss in experimentally deformed muscovite and biotite with implications for <sup>40</sup>Ar/<sup>39</sup>Ar geochronology of naturally deformed rocks","title":"40Ar∗ loss in experimentally deformed muscovite and biotite with implications for 40Ar/39Ar geochronology of naturally deformed rocks","docAbstract":"<p id=\"sp005\">The effects of deformation on radiogenic argon (<sup>40</sup>Ar<sup>∗</sup>) retentivity in mica are described from high pressure experiments performed on rock samples of peraluminous granite containing euhedral muscovite and biotite. Cylindrical cores, ∼15&nbsp;mm in length and 6.25&nbsp;mm in diameter, were drilled from granite collected from the South Armorican Massif in northwestern France, loaded into gold capsules, and weld-sealed in the presence of excess water. The samples were deformed at a pressure of 10&nbsp;kb and a temperature of 600&nbsp;°C over a period 29 of hours within a solid medium assembly in a Griggs-type triaxial hydraulic deformation apparatus. Overall shortening in the experiments was approximately 10%. Transmitted light and secondary and backscattered electron imaging of the deformed granite samples reveals evidence of induced defects and for significant physical grain size reduction by kinking, cracking, and grain segmentation of the micas.</p><p id=\"sp010\">Infrared (IR) laser (CO<sub>2</sub>) heating of individual 1.5–2.5&nbsp;mm diameter grains of muscovite and biotite separated from the undeformed granite yield well-defined<span>&nbsp;</span><sup>40</sup>Ar/<sup>39</sup>Ar plateau ages of 311&nbsp;±&nbsp;2&nbsp;Ma (2σ). Identical experiments on single grains separated from the experimentally deformed granite yield results indicating<span>&nbsp;</span><sup>40</sup>Ar<sup>∗</sup><span>&nbsp;</span>loss of 0–35% in muscovite and 2–3%<span>&nbsp;</span><sup>40</sup>Ar<sup>∗</sup><span>&nbsp;</span>loss in biotite. Intragrain<span>&nbsp;</span><i>in situ</i><span>&nbsp;</span>ultraviolet (UV) laser ablation<span>&nbsp;</span><sup>40</sup>Ar/<sup>39</sup>Ar ages (±4–10%, 1σ) of deformed muscovites range from 309&nbsp;±&nbsp;13 to 264&nbsp;±&nbsp;7&nbsp;Ma, consistent with 0–16%<span>&nbsp;</span><sup>40</sup>Ar<sup>∗</sup><span>&nbsp;</span>loss relative to the undeformed muscovite. The<span>&nbsp;</span><i>in situ</i><span>&nbsp;</span>UV laser ablation<span>&nbsp;</span><sup>40</sup>Ar/<sup>39</sup>Ar ages of deformed biotite vary from 301 to 217&nbsp;Ma, consistent with up to 32%<span>&nbsp;</span><sup>40</sup>Ar<sup>∗</sup><span>&nbsp;</span>loss. No spatial correlation is observed between<span>&nbsp;</span><i>in situ</i><span>&nbsp;</span><sup>40</sup>Ar/<sup>39</sup>Ar age and position within individual grains. Using available argon diffusion data for muscovite the observed<span>&nbsp;</span><sup>40</sup>Ar<sup>∗</sup><span>&nbsp;</span>loss in the experimentally treated muscovite can be utilized to predict average<span>&nbsp;</span><sup>40</sup>Ar<sup>∗</sup><span>&nbsp;</span>diffusion dimensions. Maximum<span>&nbsp;</span><sup>40</sup>Ar/<sup>39</sup>Ar ages obtained by UV laser ablation overlap those of the undeformed muscovite, indicating argon loss of &lt;1% and an average effective grain radius for<span>&nbsp;</span><sup>40</sup>Ar<sup>∗</sup><span>&nbsp;</span>diffusion ⩾700&nbsp;μm. The UV laser ablation and IR laser incremental<span>&nbsp;</span><sup>40</sup>Ar/<sup>39</sup>Ar ages indicating<span>&nbsp;</span><sup>40</sup>Ar<sup>∗</sup><span>&nbsp;</span>loss of 16% and 35%, respectively, are consistent with an average diffusion radius ≪100&nbsp;μm. These results support a hypothesis of grain-scale<span>&nbsp;</span><sup>40</sup>Ar<sup>∗</sup><span>&nbsp;</span>diffusion distances in undeformed mica and a heterogeneous mechanical reduction in the intragrain effective diffusion length scale for<span>&nbsp;</span><sup>40</sup>Ar<sup>∗</sup><span>&nbsp;</span>in deformed mica. Reduction in the effective diffusion length scale in naturally deformed samples occurs most probably through production of mesoscopic and submicroscopic defects such as, e.g., stacking faults. A network of interconnected defects, continuously forming and annealing during dynamic deformation likely plays an important role in controlling both<span>&nbsp;</span><sup>40</sup>Ar<sup>∗</sup><span>&nbsp;</span>retention and intragrain distribution in deformed mica. Intragrain<span>&nbsp;</span><sup>40</sup>Ar/<sup>39</sup>Ar ages, when combined with estimates of diffusion kinetics and distances, may provide a means of establishing thermochronological histories from individual micas.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.gca.2011.10.012","usgsCitation":"Cosca, M., Stunitz, H., Bourgiex, A., and Lee, J.P., 2011, 40Ar∗ loss in experimentally deformed muscovite and biotite with implications for 40Ar/39Ar geochronology of naturally deformed rocks: Geochimica et Cosmochimica Acta, v. 75, no. 24, p. 7759-7778, https://doi.org/10.1016/j.gca.2011.10.012.","productDescription":"20 p.","startPage":"7759","endPage":"7778","costCenters":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"links":[{"id":204320,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"France","state":"Brittany","city":"Pontivy","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -3.2684326171875,\n              47.964180715412276\n            ],\n            [\n              -2.9937744140625,\n              47.964180715412276\n            ],\n            [\n              -2.9937744140625,\n              48.143181585289554\n            ],\n            [\n              -3.2684326171875,\n              48.143181585289554\n            ],\n            [\n              -3.2684326171875,\n              47.964180715412276\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"75","issue":"24","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b42d7","contributors":{"authors":[{"text":"Cosca, Michael 0000-0002-0600-7663","orcid":"https://orcid.org/0000-0002-0600-7663","contributorId":33043,"corporation":false,"usgs":true,"family":"Cosca","given":"Michael","affiliations":[{"id":35995,"text":"Geology, Geophysics, and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":353623,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stunitz, Holger","contributorId":46680,"corporation":false,"usgs":true,"family":"Stunitz","given":"Holger","email":"","affiliations":[],"preferred":false,"id":353624,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bourgiex, Anne-Lise","contributorId":60371,"corporation":false,"usgs":true,"family":"Bourgiex","given":"Anne-Lise","email":"","affiliations":[],"preferred":false,"id":353625,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lee, John P. jplee@usgs.gov","contributorId":3291,"corporation":false,"usgs":true,"family":"Lee","given":"John","email":"jplee@usgs.gov","middleInitial":"P.","affiliations":[],"preferred":true,"id":353622,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70174946,"text":"70174946 - 2011 - Neither a year nor an annus can be a derived unit in the SI","interactions":[],"lastModifiedDate":"2016-07-22T18:04:21","indexId":"70174946","displayToPublicDate":"2011-11-19T11:45:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1222,"text":"Chemistry International","active":true,"publicationSubtype":{"id":10}},"title":"Neither a year nor an annus can be a derived unit in the SI","docAbstract":"<div class=\"page\" title=\"Page 1\">\n<div class=\"section\">\n<div class=\"layoutArea\">\n<div class=\"column\">\n<p><span>The year is not a unit of the SI. The only SI unit of measurement for time is the second. The word &ldquo;annus&rdquo; or &ldquo;annum&rdquo; does not appear anywhere in the current SI document. The word &ldquo;year&rdquo; is not in the table of &ldquo;Non-SI units accepted for use with the International System of Units,&rdquo; nor in the table of &ldquo;Non-SI units whose values in SI units must be obtained experimentally,&rdquo; nor even in the table of &ldquo;Other non-SI units.&rdquo; The year can be found, however, through the list of &ldquo;Other non-SI units not recommended for use.&rdquo; This heading directs the reader to a National Institute of Standards and Technology (NIST) list where three kinds of year (365 days, sidereal, and tropical) are given with conversion to seconds, but are set in type to indicate &ldquo;in general not to be used in NIST publications.&rdquo; Table 1 summarizes some of the uses of the year in other publications. For example, in the IUPAC chemistry document,</span><span>&nbsp;</span><span>the year is not a constant; in the International Astronomy Union Style Guide,</span><span>&nbsp;</span><span>the year (Julian) is a constant.&nbsp;</span></p>\n</div>\n</div>\n</div>\n</div>\n<p>&nbsp;</p>","language":"English","publisher":"International Union of Pure and Applied Chemistry","usgsCitation":"Edwards, L.E., 2011, Neither a year nor an annus can be a derived unit in the SI: Chemistry International, v. 33, no. 6.","startPage":"S1-S2","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-030497","costCenters":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"links":[{"id":325575,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":325556,"type":{"id":15,"text":"Index Page"},"url":"https://www.iupac.org/publications/ci/2011/3306/pac_letters-sup.html"}],"volume":"33","issue":"6","publishingServiceCenter":{"id":9,"text":"Reston PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57934449e4b0eb1ce79e8c07","contributors":{"authors":[{"text":"Edwards, Lucy E. 0000-0003-4075-3317 leedward@usgs.gov","orcid":"https://orcid.org/0000-0003-4075-3317","contributorId":2647,"corporation":false,"usgs":true,"family":"Edwards","given":"Lucy","email":"leedward@usgs.gov","middleInitial":"E.","affiliations":[{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true},{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"preferred":true,"id":643268,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70006002,"text":"cir1348 - 2011 - Integrating science and resource management in Tampa Bay, Florida","interactions":[],"lastModifiedDate":"2012-02-10T00:12:00","indexId":"cir1348","displayToPublicDate":"2011-11-18T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1348","title":"Integrating science and resource management in Tampa Bay, Florida","docAbstract":"Tampa Bay is recognized internationally for its remarkable progress towards recovery since it was pronounced \"dead\" in the late 1970s. Due to significant efforts by local governments, industries and private citizens throughout the watershed, water clarity in Tampa Bay is now equal to what it was in 1950, when population in the watershed was less than one-quarter of what it is today. Seagrass extent has increased by more than 8,000 acres since the mid-1980s, and fish and wildlife populations are increasing. Central to this successful turn-around has been the Tampa Bay resource management community's long-term commitment to development and implementation of strong science-based management strategies. Research institutions and agencies, including Eckerd College, the Florida Wildlife Commission Fish and Wildlife Research Institute, Mote Marine Laboratory, National Oceanic and Atmospheric Administration, the Southwest Florida Water Management District, University of South Florida, U.S. Environmental Protection Agency, U.S. Geological Survey, local and State governments, and private companies contribute significantly to the scientific basis of our understanding of Tampa Bay's structure and ecological function. Resource management agencies, including the Tampa Bay Regional Planning Council's Agency on Bay Management, the Southwest Florida Water Management District's Surface Water Improvement and Management Program, and the Tampa Bay Estuary Program, depend upon this scientific basis to develop and implement regional adaptive management programs. The importance of integrating science with management has become fully recognized by scientists and managers throughout the region, State and Nation. Scientific studies conducted in Tampa Bay over the past 10&ndash;15 years are increasingly diverse and complex, and resource management programs reflect our increased knowledge of geology, hydrology and hydrodynamics, ecology and restoration techniques. However, a synthesis of this research and its integration into resource management has not been prepared for Tampa Bay since the mid-1980s. The need for an up-to-date synthesis of Tampa Bay science and management has resulted in the production of this document. The U.S. Geological Survey recently completed a 5-year Tampa Bay Integrated Science Study, and the Tampa Bay Estuary Program updated the Comprehensive Conservation and Management Plan for Tampa Bay in 2006. These efforts build upon results of the many research and management studies and programs summarized here.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/cir1348","collaboration":"Prepared in partnership with the Tampa Bay Estuary Program","usgsCitation":"Yates, K.K., Greening, H., and Morrison, G., 2011, Integrating science and resource management in Tampa Bay, Florida: U.S. Geological Survey Circular 1348, xviii, 280 p.; PDF Download of Report Cover; PDF Download of Front Matter; PDF Downloads of Chapters 1-8; PDF Download of Highlight Boxes, https://doi.org/10.3133/cir1348.","productDescription":"xviii, 280 p.; PDF Download of Report Cover; PDF Download of Front Matter; PDF Downloads of Chapters 1-8; PDF Download of Highlight Boxes","startPage":"i","endPage":"280","numberOfPages":"298","additionalOnlineFiles":"Y","costCenters":[{"id":574,"text":"St. Petersburg Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":116831,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/cir_1348.jpg"},{"id":110867,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/circ/1348/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Florida","city":"Tampa Bay","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -84,27 ], [ -84,29 ], [ -82,29 ], [ -82,27 ], [ -84,27 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dbe4b07f02db5e0e4c","contributors":{"authors":[{"text":"Yates, Kimberly K. 0000-0001-8764-0358 kyates@usgs.gov","orcid":"https://orcid.org/0000-0001-8764-0358","contributorId":420,"corporation":false,"usgs":true,"family":"Yates","given":"Kimberly","email":"kyates@usgs.gov","middleInitial":"K.","affiliations":[{"id":574,"text":"St. Petersburg Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":353628,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Greening, Holly","contributorId":64299,"corporation":false,"usgs":true,"family":"Greening","given":"Holly","email":"","affiliations":[],"preferred":false,"id":353630,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Morrison, Gerold","contributorId":58150,"corporation":false,"usgs":true,"family":"Morrison","given":"Gerold","email":"","affiliations":[],"preferred":false,"id":353629,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70005770,"text":"70005770 - 2011 - Relating injury to the forest ecosystem near Palmerton, PA, to zinc contamination from smelting","interactions":[],"lastModifiedDate":"2020-01-28T16:06:44","indexId":"70005770","displayToPublicDate":"2011-11-18T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":887,"text":"Archives of Environmental Contamination and Toxicology","active":true,"publicationSubtype":{"id":10}},"title":"Relating injury to the forest ecosystem near Palmerton, PA, to zinc contamination from smelting","docAbstract":"The forest on Blue Mountain, near Lehigh Gap, has been injured by emissions from two historical zinc (Zn) smelters in Palmerton, PA, located at the northern base of the mountain. The uppermost mineral soil and lower litter from sites along a transect, just south of the ridgetop, contained from 64 to 4400 mg/kg Zn. We measured forest metrics at 15 sampling sites to ascertain how forest structure, species composition and regeneration are related to soil concentrations of Zn, the probable principal cause of the injury. Understanding how ecotoxicological injury is related to soil Zn concentrations helps us quantify the extent of injury to the ecosystem on Blue Mountain as well as to generalize to other sites. The sum of canopy closure and shrub cover, suggested as a broadly inclusive measure of forest structure, was decreased to half at approximately 2060 mg/kg Zn (102 mg/kg Sr(N0<sub>3</sub>)<sup>2</sup>-extractable Zn). Tree-seedling density was decreased by 80% (from 10.5/m<sup>2</sup> to 2.1/m<sup>2</sup>) at a much lower concentration: 1080 mg/kg Zn (59 mg/kg Sr(N0<sub>3</sub>)<sup>2</sup>-extractable Zn). Changes in species composition and richness were not as useful for quantifying injury to the forest. Phytotoxicity, desiccation from exposure, and a gypsy moth infestation combined to form a barren area on the ridgetop. Liming the strongly acid Hazleton soils at the sites would partially ameliorate the observed phytotoxicity and should be considered in planning restoration.","language":"English","publisher":"Springer","doi":"10.1007/s00244-010-9640-0","usgsCitation":"Beyer, W.N., Krafft, C., Klassen, S., Green, C.E., and Chaney, R.L., 2011, Relating injury to the forest ecosystem near Palmerton, PA, to zinc contamination from smelting: Archives of Environmental Contamination and Toxicology, v. 61, no. 3, p. 376-388, https://doi.org/10.1007/s00244-010-9640-0.","productDescription":"13 p.","startPage":"376","endPage":"388","numberOfPages":"13","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true},{"id":34983,"text":"Contaminant Biology Program","active":true,"usgs":true}],"links":[{"id":204480,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Pennsylvania","city":"Palmerton","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-75.9977,40.9133],[-75.9027,40.9471],[-75.888,40.9523],[-75.8604,40.962],[-75.8481,40.9664],[-75.8388,40.973],[-75.8186,40.98],[-75.8039,40.9839],[-75.8014,40.9843],[-75.7861,40.9891],[-75.756,41.001],[-75.7498,41.0041],[-75.735,41.0107],[-75.7386,41.0144],[-75.7438,41.0262],[-75.7438,41.0271],[-75.7442,41.0317],[-75.7454,41.0353],[-75.7496,41.0372],[-75.7581,41.0368],[-75.7622,41.0442],[-75.7646,41.0469],[-75.767,41.0497],[-75.7687,41.0542],[-75.7692,41.0588],[-75.7707,41.0729],[-75.7692,41.081],[-75.7655,41.0841],[-75.7666,41.091],[-75.7646,41.0946],[-75.758,41.0936],[-75.7524,41.0958],[-75.7523,41.0998],[-75.7529,41.1026],[-75.751,41.1048],[-75.7327,41.1037],[-75.7302,41.1054],[-75.7295,41.1086],[-75.7258,41.1104],[-75.7222,41.1117],[-75.7209,41.1139],[-75.719,41.1162],[-75.7183,41.1189],[-75.7165,41.1189],[-75.7146,41.1193],[-75.7092,41.117],[-75.7055,41.1187],[-75.7042,41.1232],[-75.6924,41.1308],[-75.6863,41.1311],[-75.6808,41.1324],[-75.6734,41.1337],[-75.6655,41.134],[-75.6631,41.1317],[-75.6613,41.1308],[-75.6577,41.1276],[-75.656,41.123],[-75.6555,41.1189],[-75.6518,41.1184],[-75.6474,41.1233],[-75.6451,41.1206],[-75.6452,41.1156],[-75.6428,41.1146],[-75.6337,41.1136],[-75.6331,41.1131],[-75.6319,41.1099],[-75.6307,41.1095],[-75.6259,41.1085],[-75.6252,41.1098],[-75.6246,41.1112],[-75.6227,41.1116],[-75.6209,41.1111],[-75.6185,41.1093],[-75.6144,41.1042],[-75.6127,41.1006],[-75.6121,41.0974],[-75.6043,41.095],[-75.6038,41.0905],[-75.6033,41.0877],[-75.6015,41.0863],[-75.5973,41.0845],[-75.5919,41.0808],[-75.5811,41.0724],[-75.5745,41.0678],[-75.5716,41.0632],[-75.5693,41.0573],[-75.5689,41.0527],[-75.5676,41.0523],[-75.5616,41.0494],[-75.5527,41.042],[-75.5468,41.0356],[-75.539,41.0287],[-75.5301,41.0208],[-75.4963,40.9894],[-75.5,40.9863],[-75.5389,40.967],[-75.5343,40.9596],[-75.5663,40.9461],[-75.5552,40.9286],[-75.5347,40.9016],[-75.5171,40.8786],[-75.4995,40.8547],[-75.4989,40.8538],[-75.4866,40.8382],[-75.4826,40.83],[-75.4757,40.8135],[-75.5434,40.8037],[-75.5855,40.7966],[-75.5929,40.7936],[-75.5972,40.7905],[-75.6015,40.7882],[-75.6107,40.7861],[-75.6277,40.7841],[-75.6656,40.7769],[-75.6821,40.7735],[-75.6857,40.7727],[-75.6943,40.7674],[-75.6993,40.7643],[-75.7281,40.7524],[-75.733,40.7489],[-75.7411,40.7412],[-75.7467,40.7382],[-75.7546,40.7351],[-75.7881,40.756],[-75.7995,40.7629],[-75.8096,40.7694],[-75.8413,40.7898],[-75.8593,40.8013],[-75.8724,40.8083],[-75.8856,40.8162],[-75.9083,40.8328],[-75.9149,40.8388],[-75.9214,40.8448],[-75.9632,40.8825],[-75.9787,40.8968],[-75.984,40.9014],[-75.9888,40.9055],[-75.9977,40.9133]]]},\"properties\":{\"name\":\"Carbon\",\"state\":\"PA\"}}]}","volume":"61","issue":"3","noUsgsAuthors":false,"publicationDate":"2011-02-01","publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c4c0","contributors":{"authors":[{"text":"Beyer, W. Nelson 0000-0002-8911-9141 nbeyer@usgs.gov","orcid":"https://orcid.org/0000-0002-8911-9141","contributorId":3301,"corporation":false,"usgs":true,"family":"Beyer","given":"W.","email":"nbeyer@usgs.gov","middleInitial":"Nelson","affiliations":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"preferred":true,"id":353179,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Krafft, Cairn ckrafft@usgs.gov","contributorId":3480,"corporation":false,"usgs":true,"family":"Krafft","given":"Cairn","email":"ckrafft@usgs.gov","affiliations":[],"preferred":true,"id":353180,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Klassen, Stephen","contributorId":41578,"corporation":false,"usgs":true,"family":"Klassen","given":"Stephen","email":"","affiliations":[],"preferred":false,"id":353182,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Green, Carrie E.","contributorId":95605,"corporation":false,"usgs":true,"family":"Green","given":"Carrie","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":353183,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Chaney, Rufus L.","contributorId":35455,"corporation":false,"usgs":true,"family":"Chaney","given":"Rufus","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":353181,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70005997,"text":"sim3182 - 2011 - Potentiometric surface of the Upper Floridan aquifer in Florida and parts of Georgia, South Carolina, and Alabama, May &ndash; June 2010","interactions":[],"lastModifiedDate":"2017-01-31T08:35:08","indexId":"sim3182","displayToPublicDate":"2011-11-18T00:00:00","publicationYear":"2011","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":"3182","title":"Potentiometric surface of the Upper Floridan aquifer in Florida and parts of Georgia, South Carolina, and Alabama, May &ndash; June 2010","docAbstract":"The Floridan aquifer system covers nearly 100,000 square miles in the southeastern United States throughout Florida and in parts of Georgia, South Carolina, and Alabama, and is one of the most productive aquifers in the world (Miller, 1990). This sequence of carbonate rocks is hydraulically connected and is over 300 feet thick in south Florida and thins toward the north. Typically, this sequence is subdivided into the Upper Floridan aquifer, the middle confining unit, and the Lower Floridan aquifer. The majority of freshwater is contained in the Upper Floridan aquifer and is used for water supply (Miller, 1986). The Lower Floridan aquifer contains fresh to brackish water in northeastern Florida and Georgia, while in south Florida it is saline. The potentiometric surface of the Upper Floridan aquifer in May&ndash;June 2010 shown on this map was constructed as part of the U.S. Geological Survey Floridan Aquifer System Groundwater Availability Study (U.S. Geological Survey database, 2011). Previous synoptic measurements and regional potentiometric maps of the Upper Floridan aquifer were prepared for May 1980 (Johnston and others, 1981) and May 1985 (Bush and others, 1986) as part of the Floridan Regional Aquifer System Analysis.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sim3182","collaboration":"Product of the U.S. Geological Survey Groundwater Resources Program","usgsCitation":"Kinnaman, S.L., and Dixon, J.F., 2011, Potentiometric surface of the Upper Floridan aquifer in Florida and parts of Georgia, South Carolina, and Alabama, May &ndash; June 2010: U.S. Geological Survey Scientific Investigations Map 3182, Map: 36 x 50 inches, https://doi.org/10.3133/sim3182.","productDescription":"Map: 36 x 50 inches","temporalStart":"2010-05-01","temporalEnd":"2010-06-30","costCenters":[{"id":287,"text":"Florida Water Science Center-Orlando","active":false,"usgs":true},{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":110861,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sim/3182/","linkFileType":{"id":5,"text":"html"}},{"id":116832,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/sim_3182.jpg"}],"scale":"100000","projection":"Albers Equal-Area Conic","datum":"NAD83","country":"United States","state":"Alabama, Florida, Georgia, South 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,{"id":70003899,"text":"70003899 - 2011 - Reply to the comment on the paper \"Is the track of the Yellowstone hotspot driven by a deep mantle plume?-Review of volcanism, faulting, and uplift in light of new data\"","interactions":[],"lastModifiedDate":"2012-02-02T00:15:58","indexId":"70003899","displayToPublicDate":"2011-11-18T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2499,"text":"Journal of Volcanology and Geothermal Research","active":true,"publicationSubtype":{"id":10}},"title":"Reply to the comment on the paper \"Is the track of the Yellowstone hotspot driven by a deep mantle plume?-Review of volcanism, faulting, and uplift in light of new data\"","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Volcanology and Geothermal Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","publisherLocation":"Amsterdam, Netherlands","usgsCitation":"Pierce, K.L., and Morgan, L.A., 2011, Reply to the comment on the paper \"Is the track of the Yellowstone hotspot driven by a deep mantle plume?-Review of volcanism, faulting, and uplift in light of new data\": Journal of Volcanology and Geothermal Research, v. 202, no. 3-4, p. 264-265.","productDescription":"2 p.","startPage":"264","endPage":"265","numberOfPages":"2","costCenters":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"links":[{"id":204354,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":110866,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://www.mantleplumes.org/WebDocuments/Pierce2011.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","otherGeospatial":"Yellowstone Hotspot","volume":"202","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a5fe4b07f02db633fbd","contributors":{"authors":[{"text":"Pierce, Kenneth L. kpierce@usgs.gov","contributorId":1609,"corporation":false,"usgs":true,"family":"Pierce","given":"Kenneth","email":"kpierce@usgs.gov","middleInitial":"L.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true},{"id":481,"text":"Northern Rocky Mountain Science Center","active":true,"usgs":true},{"id":547,"text":"Rocky Mountain Geographic Science Center","active":true,"usgs":true}],"preferred":true,"id":349365,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Morgan, Lisa A.","contributorId":66300,"corporation":false,"usgs":true,"family":"Morgan","given":"Lisa","email":"","middleInitial":"A.","affiliations":[{"id":481,"text":"Northern Rocky Mountain Science Center","active":true,"usgs":true}],"preferred":false,"id":349366,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70005467,"text":"70005467 - 2011 - Relating nutrient and herbicide fate with landscape features and characteristics of 15 subwatersheds in the Choptank River watershed","interactions":[],"lastModifiedDate":"2021-05-21T16:44:25.341427","indexId":"70005467","displayToPublicDate":"2011-11-18T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3352,"text":"Science of the Total Environment","active":true,"publicationSubtype":{"id":10}},"title":"Relating nutrient and herbicide fate with landscape features and characteristics of 15 subwatersheds in the Choptank River watershed","docAbstract":"Excess nutrients and agrochemicals from non-point sources contribute to water quality impairment in the Chesapeake Bay watershed and their loading rates are related to land use, agricultural practices, hydrology, and pollutant fate and transport processes. In this study, monthly baseflow stream samples from 15 agricultural subwatersheds of the Choptank River in Maryland USA (2005 to 2007) were characterized for nutrients, herbicides, and herbicide transformation products. High-resolution digital maps of land use and forested wetlands were derived from remote sensing imagery. Examination of landscape metrics and water quality data, partitioned according to hydrogeomorphic class, provided insight into the fate, delivery, and transport mechanisms associated with agricultural pollutants. Mean Nitrate-N concentrations (4.9 mg/L) were correlated positively with percent agriculture (R<sup>2</sup> = 0.56) and negatively with percent forest (R<sup>2</sup> = 0.60). Concentrations were greater (<i>p</i> = 0.0001) in the well-drained upland (WDU) hydrogeomorphic region than in poorly drained upland (PDU), reflecting increased denitrification and reduced agricultural land use intensity in the PDU landscape due to the prevalence of hydric soils. Atrazine and metolachlor concentrations (mean 0.29 &mu;g/L and 0.19 &mu;g/L) were also greater (<i>p</i> = 0.0001) in WDU subwatersheds than in PDU subwatersheds. Springtime herbicide concentrations exhibited a strong, positive correlation (R<sup>2</sup> = 0.90) with percent forest in the WDU subwatersheds but not in the PDU subwatersheds. In addition, forested riparian stream buffers in the WDU were more prevalent than in the PDU where forested patches are typically not located near streams, suggesting an alternative delivery mechanism whereby volatilized herbicides are captured by the riparian forest canopy and subsequently washed off during rainfall. Orthophosphate, CIAT (6-chloro-<i>N</i>-(1-methylethyl)-1,3,5-triazine-2,4-diamine), CEAT (6-chloro-<i>N</i>-ethyl-1,3,5-triazine-2,4-diamine), and MESA (2-[(2-ethyl-6-methylphenyl) (2-methoxy-1-methylethyl)amino]-2-oxoethanesulfonic acid) were also analyzed. These findings will assist efforts in targeting implementation of conservation practices to the most environmentally-critical areas within watersheds to achieve water quality improvements in a cost-effective manner.","language":"English","publisher":"Elsevier","publisherLocation":"Amsterdam, Netherlands","doi":"10.1016/j.scitotenv.2011.05.024","usgsCitation":"Hively, W., Hapeman, C.J., McConnell, L.L., Fisher, T.R., Rice, C.P., McCarty, G.W., Sadeghi, A.M., Whitall, D.R., Downey, P.M., de Guzman, G.T., Bialek-Kalinski, K., Lang, M., Gustafson, A.B., Sutton, A.J., Sefton, K.A., and Harman Fetcho, J.A., 2011, Relating nutrient and herbicide fate with landscape features and characteristics of 15 subwatersheds in the Choptank River watershed: Science of the Total Environment, v. 409, no. 19, p. 3866-3878, https://doi.org/10.1016/j.scitotenv.2011.05.024.","productDescription":"13 p.","startPage":"3866","endPage":"3878","costCenters":[{"id":242,"text":"Eastern Geographic Science Center","active":true,"usgs":true}],"links":[{"id":204377,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Delaware, Maryland","otherGeospatial":"Choptank River watershed","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -76.1407470703125,\n              38.646908247760706\n            ],\n            [\n              -75.58868408203125,\n              38.646908247760706\n            ],\n            [\n              -75.58868408203125,\n              39.29392267616436\n            ],\n            [\n              -76.1407470703125,\n              39.29392267616436\n            ],\n            [\n              -76.1407470703125,\n              38.646908247760706\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"409","issue":"19","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c35e","contributors":{"authors":[{"text":"Hively, W. Dean 0000-0002-5383-8064","orcid":"https://orcid.org/0000-0002-5383-8064","contributorId":9391,"corporation":false,"usgs":true,"family":"Hively","given":"W. Dean","affiliations":[],"preferred":false,"id":352573,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hapeman, Cathleen J.","contributorId":63154,"corporation":false,"usgs":true,"family":"Hapeman","given":"Cathleen","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":352584,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McConnell, Laura L.","contributorId":106437,"corporation":false,"usgs":true,"family":"McConnell","given":"Laura","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":352588,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Fisher, Thomas R.","contributorId":40721,"corporation":false,"usgs":true,"family":"Fisher","given":"Thomas","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":352577,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Rice, Clifford P.","contributorId":56594,"corporation":false,"usgs":true,"family":"Rice","given":"Clifford","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":352582,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"McCarty, Gregory W.","contributorId":78861,"corporation":false,"usgs":true,"family":"McCarty","given":"Gregory","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":352585,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Sadeghi, Ali M.","contributorId":50645,"corporation":false,"usgs":true,"family":"Sadeghi","given":"Ali","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":352579,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Whitall, David R.","contributorId":24908,"corporation":false,"usgs":true,"family":"Whitall","given":"David","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":352575,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Downey, Peter M.","contributorId":48694,"corporation":false,"usgs":true,"family":"Downey","given":"Peter","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":352578,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"de Guzman, Gabriela T. Nino","contributorId":54723,"corporation":false,"usgs":true,"family":"de Guzman","given":"Gabriela","email":"","middleInitial":"T. Nino","affiliations":[],"preferred":false,"id":352581,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Bialek-Kalinski, Krystyna","contributorId":12613,"corporation":false,"usgs":true,"family":"Bialek-Kalinski","given":"Krystyna","email":"","affiliations":[],"preferred":false,"id":352574,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Lang, Megan W.","contributorId":58014,"corporation":false,"usgs":true,"family":"Lang","given":"Megan W.","affiliations":[],"preferred":false,"id":352583,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Gustafson, Anne B.","contributorId":36279,"corporation":false,"usgs":true,"family":"Gustafson","given":"Anne","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":352576,"contributorType":{"id":1,"text":"Authors"},"rank":13},{"text":"Sutton, Adrienne J.","contributorId":98872,"corporation":false,"usgs":true,"family":"Sutton","given":"Adrienne","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":352587,"contributorType":{"id":1,"text":"Authors"},"rank":14},{"text":"Sefton, Kerry A.","contributorId":86097,"corporation":false,"usgs":true,"family":"Sefton","given":"Kerry","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":352586,"contributorType":{"id":1,"text":"Authors"},"rank":15},{"text":"Harman Fetcho, Jennifer A.","contributorId":51444,"corporation":false,"usgs":true,"family":"Harman Fetcho","given":"Jennifer","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":352580,"contributorType":{"id":1,"text":"Authors"},"rank":16}]}}
,{"id":70005984,"text":"sir20115162 - 2011 - Lithogeochemistry of mineralized and altered rock samples from the northern Talkeetna Mountains, south-central Alaska","interactions":[],"lastModifiedDate":"2012-02-10T00:12:01","indexId":"sir20115162","displayToPublicDate":"2011-11-16T00:00:00","publicationYear":"2011","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":"2011-5162","title":"Lithogeochemistry of mineralized and altered rock samples from the northern Talkeetna Mountains, south-central Alaska","docAbstract":"Mineralized and altered rock samples collected from the northern Talkeetna Mountains, Alaska, were analyzed by two different inductively coupled plasma atomic-emission spectrometry (ICP-AES) methods for as many as 44 elements; by fire assay and either direct-coupled plasma (DCP) or atomic absorption spectrophotometry (AAS) for gold (Au); by cold vapor atomic absorption (CVAA) for mercury (Hg); and by irradiated neutron activation analysis (INAA) for tungsten (W). The analytical results showed that some samples contain high values of multiple elements and may be potential indicators of hydrothermal mineralization in the area.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20115162","usgsCitation":"Light, T., and Schmidt, J.M., 2011, Lithogeochemistry of mineralized and altered rock samples from the northern Talkeetna Mountains, south-central Alaska: U.S. Geological Survey Scientific Investigations Report 2011-5162, vi, 7 p.; Figures; Tables; Table 1 Download, https://doi.org/10.3133/sir20115162.","productDescription":"vi, 7 p.; Figures; Tables; Table 1 Download","onlineOnly":"Y","additionalOnlineFiles":"Y","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":116425,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/sir_2011_5162.gif"},{"id":110844,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2011/5162/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Alaska","otherGeospatial":"Talkeetna Mountains","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -149.5,62.25 ], [ -149.5,63.25 ], [ -147.5,63.25 ], [ -147.5,62.25 ], [ -149.5,62.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4d0e","contributors":{"authors":[{"text":"Light, Thomas D.","contributorId":46098,"corporation":false,"usgs":true,"family":"Light","given":"Thomas D.","affiliations":[],"preferred":false,"id":353600,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schmidt, Jeanine M. jschmidt@usgs.gov","contributorId":3138,"corporation":false,"usgs":true,"family":"Schmidt","given":"Jeanine","email":"jschmidt@usgs.gov","middleInitial":"M.","affiliations":[{"id":119,"text":"Alaska Science Center Geology Minerals","active":true,"usgs":true}],"preferred":true,"id":353599,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70003844,"text":"70003844 - 2011 - Reactive-transport modeling of iron diagenesis and associated organic carbon remineralization in a Florida (USA) subterranean estuary","interactions":[],"lastModifiedDate":"2025-05-13T18:17:56.977032","indexId":"70003844","displayToPublicDate":"2011-11-16T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1427,"text":"Earth and Planetary Science Letters","active":true,"publicationSubtype":{"id":10}},"title":"Reactive-transport modeling of iron diagenesis and associated organic carbon remineralization in a Florida (USA) subterranean estuary","docAbstract":"<p><span>Iron oxides are important terminal electron acceptors for organic carbon (OC) remineralization in subterranean estuaries, particularly where oxygen and nitrate concentrations are low. In Indian River Lagoon, Florida, USA, terrestrial Fe-oxides dissolve at the seaward edge of the seepage face and flow upward into overlying marine sediments where they precipitate as Fe-sulfides. The dissolved Fe concentrations vary by over three orders of magnitude, but Fe-oxide dissolution rates are similar across the 25-m wide seepage face, averaging around 0.21</span><span>&nbsp;</span><span>mg/cm</span><sup>2</sup><span>/yr. The constant dissolution rate, but differing concentrations, indicate Fe dissolution is controlled by a combination of increasing lability of dissolved organic carbon (DOC) and slower porewater flow velocities with distance offshore. In contrast, the average rate constants of Fe-sulfide precipitation decrease from 21.9</span><span>&nbsp;</span><span>×</span><span>&nbsp;</span><span>10</span><sup>−&nbsp;8</sup><span>&nbsp;</span><span>s</span><sup>−&nbsp;1</sup><span>&nbsp;to 0.64</span><span>&nbsp;</span><span>×</span><span>&nbsp;</span><span>10</span><sup>−&nbsp;8</sup><span>&nbsp;</span><span>s</span><sup>−&nbsp;1</sup><span>&nbsp;from the shoreline to the seaward edge of the seepage face as more oxygenated surface water circulates through the sediment. The amount of OC remineralized by Fe-oxides varies little across the seepage face, averaging 5.34</span><span>&nbsp;</span><span>×</span><span>&nbsp;</span><span>10</span><sup>−&nbsp;2</sup><span>&nbsp;</span><span>mg/cm</span><sup>2</sup><span>/yr. These rates suggest about 3.4</span><span>&nbsp;</span><span>kg of marine DOC was remineralized in a 1-m wide, shore-perpendicular strip of the seepage face as the terrestrial sediments were transgressed over the past 280</span><span>&nbsp;</span><span>years. During this time, about 10 times more marine solid organic carbon (SOC) accumulated in marine sediments than were removed from the underlying terrestrial sediments. Indian River Lagoon thus appears to be a net sink for marine OC.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.epsl.2011.02.002","usgsCitation":"Roy, M., Martin, J., Smith, C.G., and Cable, J.E., 2011, Reactive-transport modeling of iron diagenesis and associated organic carbon remineralization in a Florida (USA) subterranean estuary: Earth and Planetary Science Letters, v. 304, no. 1-2, p. 191-201, https://doi.org/10.1016/j.epsl.2011.02.002.","productDescription":"11 p.","startPage":"191","endPage":"201","costCenters":[{"id":574,"text":"St. Petersburg Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":204549,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Florida","otherGeospatial":"Indian River Lagoon","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -80.8648681640625,\n              27.103143960595734\n            ],\n            [\n              -80.1507568359375,\n              27.103143960595734\n            ],\n            [\n              -80.1507568359375,\n              28.478348692223165\n            ],\n            [\n              -80.8648681640625,\n              28.478348692223165\n            ],\n            [\n              -80.8648681640625,\n              27.103143960595734\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"304","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7fe4b07f02db6486b6","contributors":{"authors":[{"text":"Roy, Moutusi","contributorId":27998,"corporation":false,"usgs":true,"family":"Roy","given":"Moutusi","email":"","affiliations":[],"preferred":false,"id":349132,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Martin, Jonathan B.","contributorId":68450,"corporation":false,"usgs":true,"family":"Martin","given":"Jonathan B.","affiliations":[],"preferred":false,"id":349133,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Smith, Christopher G. 0000-0002-8075-4763 cgsmith@usgs.gov","orcid":"https://orcid.org/0000-0002-8075-4763","contributorId":3410,"corporation":false,"usgs":true,"family":"Smith","given":"Christopher","email":"cgsmith@usgs.gov","middleInitial":"G.","affiliations":[{"id":24708,"text":"Lower Mississippi-Gulf Water Science Center","active":true,"usgs":true},{"id":574,"text":"St. Petersburg Coastal and Marine Science Center","active":true,"usgs":true},{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"preferred":true,"id":349131,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Cable, Jaye E.","contributorId":83658,"corporation":false,"usgs":true,"family":"Cable","given":"Jaye","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":349134,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70005983,"text":"ofr20111194 - 2011 - Shallow stratigraphy of the Skagit River Delta, Washington, derived from sediment cores","interactions":[],"lastModifiedDate":"2012-02-10T00:12:01","indexId":"ofr20111194","displayToPublicDate":"2011-11-16T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2011-1194","title":"Shallow stratigraphy of the Skagit River Delta, Washington, derived from sediment cores","docAbstract":"Sedimentologic analyses of 21 sediment cores, ranging from 0.4 to 9.6 m in length, reveal that the shallow geologic framework of the Skagit River Delta, western Washington, United States, has changed significantly since 1850. The cores collected from elevations of 3.94 to -2.41 m (relative to mean lower low water) along four cross-shore transects between the emergent marsh and delta front show relatively similar environmental changes across an area spanning ~75 km<sup>2</sup>. Offshore of the present North Fork Skagit River and South Fork Skagit River mouths where river discharge is focused by diked channels through the delta, the entire 5&ndash;7-km-wide tidal flats are covered with 1&ndash;2 m of cross-bedded medium-to-coarse sands. The bottoms of cores, collected in these areas are composed of mud. A sharp transition from mud to a cross-bedded sand unit indicates that the tidal flats changed abruptly from a calm environment to an energetic one. This is in stark contrast to the Martha's Bay tidal flats north of the Skagit Bay jetty that was completed in the 1940s to protect the newly constructed Swinomish Channel from flooding and sedimentation. North of the jetty, mud ranging from 1 to 2 m thick drapes a previously silt- and sand-rich tidal flat. The silty sand is a sediment facies that would be expected there where North Fork Skagit River sedimentation occurred prior to jetty emplacement.  This report describes the compositional and textural properties of the sediment cores by using geophysical, photographic, x-radiography, and standard sediment grain-size and carbon-analytical methods. The findings help to characterize benthic habitat structure and sediment transport processes and the environmental changes that have occurred across the nearshore of the Skagit River Delta. The findings will be useful for quantifying changes to nearshore marine resources, including impacts resulting from diking, river-delta channelization, shoreline development, and natural variations in fluvial-sediment inputs. These results also provide important quantitative data on the amount of sediment delivered to the nearshore from the Skagit River for use in calculating sediment budgets for application to watershed planning and wetland and coastal-ecosystem restoration.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20111194","usgsCitation":"Grossman, E., George, D.A., and Lam, A., 2011, Shallow stratigraphy of the Skagit River Delta, Washington, derived from sediment cores: U.S. Geological Survey Open-File Report 2011-1194, vi, 26 p.; Appendices, https://doi.org/10.3133/ofr20111194.","productDescription":"vi, 26 p.; Appendices","onlineOnly":"Y","costCenters":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":116424,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr_2011_1194.gif"},{"id":110843,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2011/1194/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Washington","otherGeospatial":"Skagit River Delta","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -124,47 ], [ -124,49 ], [ -121.25,49 ], [ -121.25,47 ], [ -124,47 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abde4b07f02db673b8a","contributors":{"authors":[{"text":"Grossman, Eric E.","contributorId":40677,"corporation":false,"usgs":true,"family":"Grossman","given":"Eric E.","affiliations":[],"preferred":false,"id":353597,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"George, Douglas A.","contributorId":60328,"corporation":false,"usgs":true,"family":"George","given":"Douglas","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":353598,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lam, Angela","contributorId":37312,"corporation":false,"usgs":true,"family":"Lam","given":"Angela","email":"","affiliations":[],"preferred":false,"id":353596,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70005992,"text":"sir20115188 - 2011 - Groundwater conditions and studies in the Augusta&ndash;Richmond County area, Georgia, 2008&ndash;2009","interactions":[],"lastModifiedDate":"2017-01-18T12:40:09","indexId":"sir20115188","displayToPublicDate":"2011-11-16T00:00:00","publicationYear":"2011","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":"2011-5188","title":"Groundwater conditions and studies in the Augusta&ndash;Richmond County area, Georgia, 2008&ndash;2009","docAbstract":"Groundwater studies and monitoring efforts conducted during 2008&ndash;2009, as part of the U.S. Geological Survey (USGS) Cooperative Water Program with the City of Augusta in Richmond County, Georgia, provided data for the effective management of local water resources. During 2008&ndash;2009 the USGS completed: (1) installation of three monitoring wells and the collection of lithologic and geophysical logging data to determine the extent of hydrogeologic units, (2) collection of continuous groundwater-level data from wells near Well Fields 2 and 3, (3) collection of synoptic groundwater-level measurements and construction of potentiometric-surface maps in Richmond County to establish flow gradients and groundwater-flow directions in the Dublin and Midville aquifer systems, (4) completion of a 24-hour aquifer test to determine hydraulic characteristics of the lower Dublin aquifer, and upper and lower Midville aquifers in Well Field 2, and (5) collection of groundwater samples from selected wells in Well Field 2 for laboratory analysis of volatile organic compounds and groundwater tracers to assess groundwater quality and estimate the time of groundwater recharge.  Potentiometric-surface maps of the Dublin and Midville aquifer systems for 2008&ndash;2009 indicate that the general groundwater flow direction within Richmond County is eastward toward the Savannah River, with the exception of the area around Well Field 2, where pumping interrupts the eastward flow of water toward the Savannah River and causes flow lines to bend toward the center of pumping.  Results from a 24-hour aquifer test conducted in 2009 within the upper and lower Midville aquifers at Well Field 2 indicated a transmissivity and storativity for the upper and lower Midville aquifers, combined, of 4,000 feet-squared per day and 2x10<sup>-4</sup>, respectively. The upper and lower Midville aquifers and the middle lower Midville confining unit, which is 85-feet thick in this area, yielded horizontal hydraulic conductivity and specific storage values of about 45 feet per day and 2x10<sup>-6</sup> ft<sup>-1</sup>, respectively. Results from the 24-hour aquifer test also indicate a low horizontal hydraulic conductivity for the lower Dublin aquifer of less than 1 foot per day.  Of the 35 volatile organic compounds (VOCs) analyzed in 23 groundwater samples during 2008&ndash;2009, only six were detected above laboratory reporting limits in samples from eight wells. No concentration in groundwater samples collected during 2008&ndash;2009 exceeded drinking water standards. Trichloroethene had the maximum VOC concentration (1.9 micrograms per liter) collected from a water sample during 2008&ndash;2009. Water-quality sampling of several wells near Well Field 2 indicate that, while in operation, the northernmost production well might have diverted groundwater, containing low levels of trichloroethene from at least two other production wells. Analysis of sulfur hexafluoride data indicate the average year of recharge ranges between 1981 and 1984 for water samples from five wells open to the upper and lower Midville aquifers, and 1991 for a water sample from one shallow well open to the lower Dublin aquifer. All of these ages suggest a short flow path and nearby source of contamination. The actual source of low levels of VOCs at Well Field 2 remains unknown.  Three newly installed monitoring wells indicate that hydrogeologic units beneath Well Fields 2 and 3 are composed of sand and clay layers. Hydrogeologic units, encountered at Well Field 2, in order of increasing depth are the lower Dublin confining unit, lower Dublin aquifer, upper Midville confining unit, upper Midville aquifer, lower Midville confining unit, and lower Midville aquifer. West of Well Field 3, hydrogeologic units, in order of increasing depth are the Upper Three Runs aquifer, Gordon confining unit, Gordon aquifer, lower Dublin confining unit, lower Dublin aquifer, upper Midville confining unit, upper Midville aquifer, lower Midville confining unit, and lower Midville aquifer.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20115188","collaboration":"Prepared in cooperation with the City of Augusta, Georgia","usgsCitation":"Gonthier, G., Lawrence, S.J., Peck, M., and Holloway, O.G., 2011, Groundwater conditions and studies in the Augusta&ndash;Richmond County area, Georgia, 2008&ndash;2009: U.S. Geological Survey Scientific Investigations Report 2011-5188, viii, 38 p.; Appendices, https://doi.org/10.3133/sir20115188.","productDescription":"viii, 38 p.; Appendices","temporalStart":"2008-01-01","temporalEnd":"2009-12-31","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":116429,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/sir_2011_5188.jpg"},{"id":110849,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2011/5188/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Georgia","county":"Richmond County","city":"Augusta","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -82.33333333333333,33.25 ], [ -82.33333333333333,33.583333333333336 ], [ -81.83333333333333,33.583333333333336 ], [ -81.83333333333333,33.25 ], [ -82.33333333333333,33.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a95e4b07f02db659df5","contributors":{"authors":[{"text":"Gonthier, Gerard  0000-0003-4078-8579 gonthier@usgs.gov","orcid":"https://orcid.org/0000-0003-4078-8579","contributorId":3141,"corporation":false,"usgs":true,"family":"Gonthier","given":"Gerard ","email":"gonthier@usgs.gov","affiliations":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"preferred":false,"id":353613,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lawrence, Stephen J. slawrenc@usgs.gov","contributorId":1885,"corporation":false,"usgs":true,"family":"Lawrence","given":"Stephen","email":"slawrenc@usgs.gov","middleInitial":"J.","affiliations":[{"id":316,"text":"Georgia Water Science Center","active":true,"usgs":true}],"preferred":true,"id":353612,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Peck, Michael F. mfpeck@usgs.gov","contributorId":1467,"corporation":false,"usgs":true,"family":"Peck","given":"Michael F.","email":"mfpeck@usgs.gov","affiliations":[],"preferred":false,"id":353610,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Holloway, O. Gary ghollowa@usgs.gov","contributorId":1860,"corporation":false,"usgs":true,"family":"Holloway","given":"O.","email":"ghollowa@usgs.gov","middleInitial":"Gary","affiliations":[],"preferred":true,"id":353611,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70005985,"text":"ofr20101240 - 2011 - Palos Verdes Shelf oceanographic study; data report for observations December 2007&ndash;April 2008","interactions":[],"lastModifiedDate":"2012-02-10T00:12:01","indexId":"ofr20101240","displayToPublicDate":"2011-11-16T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2010-1240","title":"Palos Verdes Shelf oceanographic study; data report for observations December 2007&ndash;April 2008","docAbstract":"Beginning in 1997, the Environmental Protection Agency (EPA) defined a contaminated section of the Palos Verdes Shelf region in southern California as a Superfund Site, initiating a continuing investigation of this area. The investigation involved the EPA, the U.S. Geological Survey (USGS), Science Applications International Corporation (SAIC), Los Angeles County Sanitation Districts (LACSD) data, and other allied agencies.  In mid-2007, the Palos Verdes Shelf project team identified the need for additional data on the sediment properties and oceanographic conditions at the Palos Verdes Superfund Site and deployed seven bottom platforms, three subsurface moorings, and three surface moorings on the shelf. This additional data was needed to support ongoing modeling and feasibility studies and to improve our ability to model the fate of the effluent-affected deposit over time. It provided more detail on the spatial variability and magnitude of resuspension of the deposit during multiple storms that are expected to transit the region during a winter season.  The operation began in early December 2007 and ended in early April 2008. The goal was to measure the sediment response (threshold of resuspension, suspended-sediment concentrations, and suspended-sediment transport rates) to bed stresses associated with waves and currents. Other objectives included determining the structure of the bottom boundary layer (BBL) relating nearbed currents with those measured at 10 m above bottom (mab) and comparing those with the long-term data from the LACSD Acoustic Doppler Current Profiler (ADCP) deployments for nearbed current speed and direction. Low-profile tripods with high-frequency ADCPs co-located with two of the large tripods were selected for this goal.  This report describes the data obtained during the field program, the instruments and data-processing procedures used, and the archive that contains the data sets that have passed our quality-assurance procedures.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20101240","usgsCitation":"Rosenberger, K.J., Noble, M.A., Sherwood, C.R., Martini, M., Ferreira, J., and Montgomery, E., 2011, Palos Verdes Shelf oceanographic study; data report for observations December 2007&ndash;April 2008: U.S. Geological Survey Open-File Report 2010-1240, v, 27 p.; Figures; Appendices, https://doi.org/10.3133/ofr20101240.","productDescription":"v, 27 p.; Figures; Appendices","onlineOnly":"Y","temporalStart":"2007-12-01","temporalEnd":"2008-04-30","costCenters":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":116426,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr_2010_1240.gif"},{"id":110845,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2010/1240/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"California","otherGeospatial":"Palos Verdes Shelf","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -118.35111111111111,33.66777777777777 ], [ -118.35111111111111,33.7175 ], [ -118.28444444444445,33.7175 ], [ -118.28444444444445,33.66777777777777 ], [ -118.35111111111111,33.66777777777777 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b08e4b07f02db69b9ad","contributors":{"authors":[{"text":"Rosenberger, Kurt J. krosenberger@usgs.gov","contributorId":2575,"corporation":false,"usgs":true,"family":"Rosenberger","given":"Kurt","email":"krosenberger@usgs.gov","middleInitial":"J.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":353603,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Noble, Marlene A. mnoble@usgs.gov","contributorId":1429,"corporation":false,"usgs":true,"family":"Noble","given":"Marlene","email":"mnoble@usgs.gov","middleInitial":"A.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":353602,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sherwood, Christopher R. 0000-0001-6135-3553 csherwood@usgs.gov","orcid":"https://orcid.org/0000-0001-6135-3553","contributorId":2866,"corporation":false,"usgs":true,"family":"Sherwood","given":"Christopher","email":"csherwood@usgs.gov","middleInitial":"R.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":353604,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Martini, Marinna M.","contributorId":53518,"corporation":false,"usgs":true,"family":"Martini","given":"Marinna M.","affiliations":[],"preferred":false,"id":353605,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Ferreira, Joanne T.","contributorId":59174,"corporation":false,"usgs":true,"family":"Ferreira","given":"Joanne T.","affiliations":[],"preferred":false,"id":353606,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Montgomery, Ellyn T. emontgomery@usgs.gov","contributorId":407,"corporation":false,"usgs":true,"family":"Montgomery","given":"Ellyn T.","email":"emontgomery@usgs.gov","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":353601,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70005933,"text":"ds642 - 2011 - Data from <i>in situ</i> Observations of Fish Traps Set by Fishermen in St. John Waters, U.S. Virgin Islands, 1992-94","interactions":[],"lastModifiedDate":"2012-02-10T00:12:00","indexId":"ds642","displayToPublicDate":"2011-11-16T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":310,"text":"Data Series","code":"DS","onlineIssn":"2327-638X","printIssn":"2327-0271","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"642","title":"Data from <i>in situ</i> Observations of Fish Traps Set by Fishermen in St. John Waters, U.S. Virgin Islands, 1992-94","docAbstract":"In order to estimate (1) the trapping pressure within Virgin Islands National Park (VINP) waters, (2) the effect of fish traps on park marine resources (both fishes and habitats), and (3) the effectiveness of park regulations in protecting marine resources, traps set by fishers were visually observed and contents censused <i>in situ</i> in 1992, 1993, and 1994, around St. John (U.S. Virgin Islands), within and outside of park waters. A total of 1,340 individual fish (56 species and 23 families) were identified and their lengths estimated for the 211 of 285 visually censused traps that contained fish. This dataset includes for each censused trap: location, depth, substrate/habitat, trap type and construction details, in or out of park waters, and species and estimated fork length (in centimeters) of each individual fish in a trap. Analysis and interpretation of this dataset are provided in previously published reports by the author.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ds642","collaboration":"Prepared in cooperation with the National Park Service","usgsCitation":"Garrison, V.H., Beets, J., Friedlander, A.M., and Canty, S., 2011, Data from <i>in situ</i> Observations of Fish Traps Set by Fishermen in St. John Waters, U.S. Virgin Islands, 1992-94: U.S. Geological Survey Data Series 642, HTML Document; TXT Download of Metadata File; XLSX Download of Data File, https://doi.org/10.3133/ds642.","productDescription":"HTML Document; TXT Download of Metadata File; XLSX Download of Data File","additionalOnlineFiles":"Y","temporalStart":"1992-01-01","temporalEnd":"1994-12-31","costCenters":[{"id":566,"text":"Southeast Ecological Science Center","active":true,"usgs":true}],"links":[{"id":116428,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ds_642.png"},{"id":110848,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/ds/642/","linkFileType":{"id":5,"text":"html"}}],"country":"U.S. Virgin Islands","otherGeospatial":"St. John","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -65,18 ], [ -65,19 ], [ -64,19 ], [ -64,18 ], [ -65,18 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c94c","contributors":{"authors":[{"text":"Garrison, Virginia H. ginger_garrison@usgs.gov","contributorId":2386,"corporation":false,"usgs":true,"family":"Garrison","given":"Virginia","email":"ginger_garrison@usgs.gov","middleInitial":"H.","affiliations":[{"id":566,"text":"Southeast Ecological Science Center","active":true,"usgs":true}],"preferred":true,"id":353486,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Beets, Jim","contributorId":99686,"corporation":false,"usgs":true,"family":"Beets","given":"Jim","email":"","affiliations":[],"preferred":false,"id":353489,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Friedlander, Alan M. afriedlander@usgs.gov","contributorId":53079,"corporation":false,"usgs":true,"family":"Friedlander","given":"Alan","email":"afriedlander@usgs.gov","middleInitial":"M.","affiliations":[],"preferred":false,"id":353487,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Canty, Steven","contributorId":83255,"corporation":false,"usgs":true,"family":"Canty","given":"Steven","email":"","affiliations":[],"preferred":false,"id":353488,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70005986,"text":"sir20115189 - 2011 - Development of a flood-warning network and flood-inundation mapping for the Blanchard River in Ottawa, Ohio","interactions":[],"lastModifiedDate":"2012-03-08T17:16:43","indexId":"sir20115189","displayToPublicDate":"2011-11-16T00:00:00","publicationYear":"2011","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":"2011-5189","title":"Development of a flood-warning network and flood-inundation mapping for the Blanchard River in Ottawa, Ohio","docAbstract":"Digital flood-inundation maps of the Blanchard River in Ottawa, Ohio, were created by the U.S. Geological Survey (USGS) in cooperation with the U.S. Department of Agriculture, Natural Resources Conservation Service and the Village of Ottawa, Ohio. The maps, which correspond to water levels (stages) at the USGS streamgage at Ottawa (USGS streamgage site number 04189260), were provided to the National Weather Service (NWS) for incorporation into a Web-based flood-warning Network that can be used in conjunction with NWS flood-forecast data to show areas of predicted flood inundation associated with forecasted flood-peak stages.  Flood profiles were computed by means of a step-backwater model calibrated to recent field measurements of streamflow. The step-backwater model was then used to determine water-surface-elevation profiles for 12 flood stages with corresponding streamflows ranging from less than the 2-year and up to nearly the 500-year recurrence-interval flood. The computed flood profiles were used in combination with digital elevation data to delineate flood-inundation areas. Maps of the Village of Ottawa showing flood-inundation areas overlain on digital orthophotographs are presented for the selected floods.  As part of this flood-warning network, the USGS upgraded one streamgage and added two new streamgages, one on the Blanchard River and one on Riley Creek, which is tributary to the Blanchard River. The streamgage sites were equipped with both satellite and telephone telemetry. The telephone telemetry provides dual functionality, allowing village officials and the public to monitor current stage conditions and enabling the streamgage to call village officials with automated warnings regarding flood stage and/or predetermined rates of stage increase. Data from the streamgages serve as a flood warning that emergency management personnel can use in conjunction with the flood-inundation maps by to determine a course of action when flooding is imminent.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20115189","collaboration":"Prepared in cooperation with the Village of Ottawa, Ohio, and the U.S. Department of Agriculture, Natural Resources Conservation Service","usgsCitation":"Whitehead, M.T., 2011, Development of a flood-warning network and flood-inundation mapping for the Blanchard River in Ottawa, Ohio: U.S. Geological Survey Scientific Investigations Report 2011-5189, iv, 8 p.; 12 Plates - Plate 1: 15 x 14.17 inches, Plate 2: 15 x 14.17 inches, Plate 3: 15 x 14.17 inches, Plate 4: 15 x 14.17 inches, Plate 5: 15 x 14.17 inches, Plate 6: 15 x 14.17 inches, Plate 7: 15 x 14.17 inches, Plate 8: 15 x 14.17 inches, Plate 9: 15 x 14.17 inches, Plate 10: 15 x 14.17 inches, Plate 11: 15 x 14.17 inches, Plate 12: 15 x 14.17 inches, https://doi.org/10.3133/sir20115189.","productDescription":"iv, 8 p.; 12 Plates - Plate 1: 15 x 14.17 inches, Plate 2: 15 x 14.17 inches, Plate 3: 15 x 14.17 inches, Plate 4: 15 x 14.17 inches, Plate 5: 15 x 14.17 inches, Plate 6: 15 x 14.17 inches, Plate 7: 15 x 14.17 inches, Plate 8: 15 x 14.17 inches, Plate 9: 15 x 14.17 inches, Plate 10: 15 x 14.17 inches, Plate 11: 15 x 14.17 inches, Plate 12: 15 x 14.17 inches","additionalOnlineFiles":"Y","costCenters":[{"id":513,"text":"Ohio Water Science Center","active":true,"usgs":true}],"links":[{"id":116423,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/sir_2011_5189.jpg"},{"id":110846,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2011/5189/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Ohio","city":"Ottowa","otherGeospatial":"Blanchard River","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa7e4b07f02db66701a","contributors":{"authors":[{"text":"Whitehead, Matthew T. mtwhiteh@usgs.gov","contributorId":2158,"corporation":false,"usgs":true,"family":"Whitehead","given":"Matthew","email":"mtwhiteh@usgs.gov","middleInitial":"T.","affiliations":[{"id":513,"text":"Ohio Water Science Center","active":true,"usgs":true}],"preferred":false,"id":353607,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70003857,"text":"70003857 - 2011 - Recent faulting in western Nevada revealed by multi-scale seismic reflection","interactions":[],"lastModifiedDate":"2013-01-25T12:50:16","indexId":"70003857","displayToPublicDate":"2011-11-16T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3317,"text":"SEG Technical Program Expanded Abstracts","active":true,"publicationSubtype":{"id":10}},"title":"Recent faulting in western Nevada revealed by multi-scale seismic reflection","docAbstract":"The main goal of this study is to compare different reflection methods used to image subsurface structure within different physical environments in western Nevada. With all the methods employed, the primary goal is fault imaging for structural information toward geothermal exploration and seismic hazard estimation. We use seismic CHIRP (a swept-frequency marine acquisition system), weight drop (an accelerated hammer source), and two different vibroseis systems to characterize fault structure. We focused our efforts in the Reno metropolitan area and the area within and surrounding Pyramid Lake in northern Nevada. These different methods have provided valuable constraints on the fault geometry and activity, as well as associated fluid movement. These are critical in evaluating the potential for large earthquakes in these areas, and geothermal exploration possibilities near these structures.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"SEG Technical Program Expanded Abstracts","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Society of Exploration Geophysicists","publisherLocation":"Tulsa, OK","doi":"10.1190/1.3627458","usgsCitation":"Frary, R.N., Louie, J.N., Stephenson, W.J., Odum, J., Kell, A., Eisses, A., Kent, G.M., Driscoll, N.W., Karlin, R., Baskin, R.L., Pullammanappallil, S., and Liberty, L.M., 2011, Recent faulting in western Nevada revealed by multi-scale seismic reflection: SEG Technical Program Expanded Abstracts, v. 30, https://doi.org/10.1190/1.3627458.","startPage":"1373","costCenters":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"links":[{"id":266449,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1190/1.3627458"},{"id":204300,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Nevada","volume":"30","noUsgsAuthors":false,"publicationDate":"2011-05-25","publicationStatus":"PW","scienceBaseUri":"4f4e4a57e4b07f02db62e0b6","contributors":{"authors":[{"text":"Frary, Roxanna N.","contributorId":97774,"corporation":false,"usgs":true,"family":"Frary","given":"Roxanna","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":349175,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Louie, John N.","contributorId":100253,"corporation":false,"usgs":true,"family":"Louie","given":"John","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":349176,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stephenson, William J. 0000-0001-8699-0786 wstephens@usgs.gov","orcid":"https://orcid.org/0000-0001-8699-0786","contributorId":695,"corporation":false,"usgs":true,"family":"Stephenson","given":"William","email":"wstephens@usgs.gov","middleInitial":"J.","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":true,"id":349166,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Odum, Jackson K. 0000-0003-4697-2430 odum@usgs.gov","orcid":"https://orcid.org/0000-0003-4697-2430","contributorId":1365,"corporation":false,"usgs":true,"family":"Odum","given":"Jackson K.","email":"odum@usgs.gov","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":true,"id":349167,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Kell, Annie","contributorId":68176,"corporation":false,"usgs":true,"family":"Kell","given":"Annie","affiliations":[],"preferred":false,"id":349172,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Eisses, Amy","contributorId":19037,"corporation":false,"usgs":true,"family":"Eisses","given":"Amy","email":"","affiliations":[],"preferred":false,"id":349168,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Kent, Graham M.","contributorId":75819,"corporation":false,"usgs":true,"family":"Kent","given":"Graham","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":349173,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Driscoll, Neal W.","contributorId":63266,"corporation":false,"usgs":true,"family":"Driscoll","given":"Neal","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":349171,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Karlin, Robert","contributorId":62470,"corporation":false,"usgs":true,"family":"Karlin","given":"Robert","email":"","affiliations":[],"preferred":false,"id":349170,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Baskin, Robert L. 0000-0002-2175-8502 rbaskin@usgs.gov","orcid":"https://orcid.org/0000-0002-2175-8502","contributorId":360,"corporation":false,"usgs":true,"family":"Baskin","given":"Robert","email":"rbaskin@usgs.gov","middleInitial":"L.","affiliations":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"preferred":true,"id":349165,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Pullammanappallil, Satish","contributorId":32785,"corporation":false,"usgs":true,"family":"Pullammanappallil","given":"Satish","email":"","affiliations":[],"preferred":false,"id":349169,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Liberty, Lee M.","contributorId":89631,"corporation":false,"usgs":true,"family":"Liberty","given":"Lee","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":349174,"contributorType":{"id":1,"text":"Authors"},"rank":12}]}}
,{"id":70003717,"text":"70003717 - 2011 - Regional geomorphology and history of Titan's Xanadu province","interactions":[],"lastModifiedDate":"2021-02-26T15:57:19.721227","indexId":"70003717","displayToPublicDate":"2011-11-16T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1963,"text":"Icarus","active":true,"publicationSubtype":{"id":10}},"title":"Regional geomorphology and history of Titan's Xanadu province","docAbstract":"<p><span>Titan’s enigmatic Xanadu province has been seen in some detail with instruments from the Cassini spacecraft. The region contains some of the most rugged, mountainous terrain on Titan, with relief over 2000</span><span>&nbsp;</span><span>m. Xanadu contains evolved and integrated river channels, impact&nbsp;<a title=\"Learn more about Crater from ScienceDirect's AI-generated Topic Pages\" href=\"https://www.sciencedirect.com/topics/earth-and-planetary-sciences/crater\" data-mce-href=\"https://www.sciencedirect.com/topics/earth-and-planetary-sciences/crater\">craters</a>, and dry basins filled with smooth, radar-dark material, perhaps sediments from past&nbsp;<a title=\"Learn more about Bed (Geology) from ScienceDirect's AI-generated Topic Pages\" href=\"https://www.sciencedirect.com/topics/earth-and-planetary-sciences/bed-geology\" data-mce-href=\"https://www.sciencedirect.com/topics/earth-and-planetary-sciences/bed-geology\">lake beds</a>. Arcuate and aligned mountain chains give evidence of compressional tectonism, yet the overall elevation of Xanadu is puzzlingly low compared to surrounding sand seas.&nbsp;<a title=\"Learn more about Lineation from ScienceDirect's AI-generated Topic Pages\" href=\"https://www.sciencedirect.com/topics/earth-and-planetary-sciences/lineation\" data-mce-href=\"https://www.sciencedirect.com/topics/earth-and-planetary-sciences/lineation\">Lineations</a>&nbsp;associated with mountain fronts and valley floors give evidence of extension that probably contributed to this regional lowering. Several locations on Xanadu’s western and southern margins contain flow-like features that may be cryovolcanic in origin, perhaps ascended from lithospheric faults related to regional downdropping late in its history. Radiometry and scatterometry observations are consistent with a water–ice or water–ammonia–ice composition to its exposed, eroded, fractured bedrock; both microwave and visible to&nbsp;<a title=\"Learn more about Near Infrared from ScienceDirect's AI-generated Topic Pages\" href=\"https://www.sciencedirect.com/topics/earth-and-planetary-sciences/near-infrared\" data-mce-href=\"https://www.sciencedirect.com/topics/earth-and-planetary-sciences/near-infrared\">near-infrared</a>&nbsp;(v-nIR) data indicate a thin overcoating of organics, likely derived from the atmosphere. We suggest Xanadu is one of the oldest terrains on Titan and that its origin and evolution have been controlled and shaped by compressional and then extensional tectonism in the icy crust and ongoing erosion by methane rainfall.</span></p>","language":"English","publisher":"Elsevier","publisherLocation":"Amsterdam, Netherlands","doi":"10.1016/j.icarus.2010.07.022","usgsCitation":"Radebaugh, J., Lorenz, R.D., Wall, S.D., Kirk, R.L., Wood, C.A., Lunine, J., Stofan, E.R., Lopes, R., Valora, P., Farr, T., Hayes, A., Stiles, B., Mitri, G., Zebker, H., Janssen, M., Wye, L., LeGall, A., Mitchell, K.L., Paganelli, F., West, R., Schaller, E., and The Cassini Radar Team, 2011, Regional geomorphology and history of Titan's Xanadu province: Icarus, v. 211, no. 1, p. 672-685, https://doi.org/10.1016/j.icarus.2010.07.022.","productDescription":"13 p.","startPage":"672","endPage":"685","costCenters":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"links":[{"id":204281,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Titan, Xanadu province","volume":"211","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c57b","contributors":{"authors":[{"text":"Radebaugh, J.","contributorId":34639,"corporation":false,"usgs":false,"family":"Radebaugh","given":"J.","affiliations":[],"preferred":false,"id":348475,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lorenz, R. D.","contributorId":90441,"corporation":false,"usgs":false,"family":"Lorenz","given":"R.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":348487,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wall, S. D.","contributorId":86468,"corporation":false,"usgs":false,"family":"Wall","given":"S.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":348486,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Kirk, R. L.","contributorId":94698,"corporation":false,"usgs":true,"family":"Kirk","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":348488,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Wood, C. A.","contributorId":35057,"corporation":false,"usgs":false,"family":"Wood","given":"C.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":348477,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Lunine, J. I.","contributorId":51899,"corporation":false,"usgs":false,"family":"Lunine","given":"J. I.","affiliations":[],"preferred":false,"id":348481,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Stofan, E. R.","contributorId":103403,"corporation":false,"usgs":false,"family":"Stofan","given":"E.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":348490,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Lopes, R M.C.","contributorId":31634,"corporation":false,"usgs":true,"family":"Lopes","given":"R M.C.","affiliations":[],"preferred":false,"id":348474,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Valora, P.","contributorId":52706,"corporation":false,"usgs":true,"family":"Valora","given":"P.","email":"","affiliations":[],"preferred":false,"id":348482,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Farr, T.G.","contributorId":49932,"corporation":false,"usgs":true,"family":"Farr","given":"T.G.","email":"","affiliations":[],"preferred":false,"id":348480,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Hayes, A.","contributorId":26415,"corporation":false,"usgs":true,"family":"Hayes","given":"A.","affiliations":[],"preferred":false,"id":348473,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Stiles, B.","contributorId":59547,"corporation":false,"usgs":true,"family":"Stiles","given":"B.","email":"","affiliations":[],"preferred":false,"id":348483,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Mitri, Giuseppe","contributorId":35052,"corporation":false,"usgs":false,"family":"Mitri","given":"Giuseppe","email":"","affiliations":[],"preferred":false,"id":348476,"contributorType":{"id":1,"text":"Authors"},"rank":13},{"text":"Zebker, H.","contributorId":25276,"corporation":false,"usgs":false,"family":"Zebker","given":"H.","affiliations":[],"preferred":false,"id":348472,"contributorType":{"id":1,"text":"Authors"},"rank":14},{"text":"Janssen, M.","contributorId":22893,"corporation":false,"usgs":true,"family":"Janssen","given":"M.","email":"","affiliations":[],"preferred":false,"id":348471,"contributorType":{"id":1,"text":"Authors"},"rank":15},{"text":"Wye, L.","contributorId":40333,"corporation":false,"usgs":true,"family":"Wye","given":"L.","affiliations":[],"preferred":false,"id":348479,"contributorType":{"id":1,"text":"Authors"},"rank":16},{"text":"LeGall, A.","contributorId":62735,"corporation":false,"usgs":true,"family":"LeGall","given":"A.","email":"","affiliations":[],"preferred":false,"id":348485,"contributorType":{"id":1,"text":"Authors"},"rank":17},{"text":"Mitchell, K. L.","contributorId":62734,"corporation":false,"usgs":false,"family":"Mitchell","given":"K.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":348484,"contributorType":{"id":1,"text":"Authors"},"rank":18},{"text":"Paganelli, F.","contributorId":17353,"corporation":false,"usgs":true,"family":"Paganelli","given":"F.","email":"","affiliations":[],"preferred":false,"id":348469,"contributorType":{"id":1,"text":"Authors"},"rank":19},{"text":"West, R.D.","contributorId":103399,"corporation":false,"usgs":true,"family":"West","given":"R.D.","email":"","affiliations":[],"preferred":false,"id":348489,"contributorType":{"id":1,"text":"Authors"},"rank":20},{"text":"Schaller, E.L.","contributorId":22601,"corporation":false,"usgs":true,"family":"Schaller","given":"E.L.","email":"","affiliations":[],"preferred":false,"id":348470,"contributorType":{"id":1,"text":"Authors"},"rank":21},{"text":"The Cassini Radar Team","contributorId":127994,"corporation":true,"usgs":false,"organization":"The Cassini Radar Team","id":535121,"contributorType":{"id":1,"text":"Authors"},"rank":22}]}}
,{"id":70005590,"text":"70005590 - 2011 - Recovery of little brown bats (Myotis lucifugus) from natural infection with Geomyces destructans, white-nose syndrome","interactions":[],"lastModifiedDate":"2023-10-16T19:08:41.27987","indexId":"70005590","displayToPublicDate":"2011-11-16T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2507,"text":"Journal of Wildlife Diseases","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Recovery of little brown bats (<i>Myotis lucifugus</i>) from natural infection with <i>Geomyces destructans</i>, white-nose syndrome","title":"Recovery of little brown bats (Myotis lucifugus) from natural infection with Geomyces destructans, white-nose syndrome","docAbstract":"<p><i>Geomyces destructans</i> produces the white fungal growth on the muzzle and the tacky white discoloration on wings and ears that characterize white-nose syndrome (WNS) in cave-hibernating bats. To test the hypothesis that postemergent WNS-infected bats recover from infection with <i>G. destructans</i>, 30 little brown bats (<i>Myotis lucifugus</i>) were collected in May 2009 from a WNS-affected hibernation site in New Jersey. All bats were confirmed to be infected with <i>G. destructans</i> using a noninvasive fungal tape method to identify the conidia of <i>G. destructans</i> and polymerase chain reaction (PCR). The bats were then held in captivity and given supportive care for 70 days. Of the 26 bats that survived and were humanely killed after 70 days, 25 showed significant improvement in the external appearance of wing membranes, had no microscopic evidence of infection by <i>G. destructans</i>, and had wing tissue samples that were negative for <i>G. destructans</i> by PCR. A subset of the bats was treated topically at the beginning of the rehabilitation study with a dilute vinegar solution, but treatment with vinegar provided no added advantage to recovery. Provision of supportive care to homeothermic bats was sufficient for full recovery from WNS. One bat at day 70 still had both gross pathology and microscopic evidence of WNS in wing membranes and was PCR-positive for <i>G. destructans</i>. Dense aggregates of neutrophils surrounded the hyphae that remained in the wing membrane of this bat.</p>","language":"English","publisher":"Wildlife Disease Association","publisherLocation":"Lawrence, KS","doi":"10.7589/0090-3558-47.3.618","usgsCitation":"Meteyer, C.U., Valent, M., Kashmer, J., Buckles, E.L., Lorch, J.M., Blehert, D., Lollar, A., Berndt, D., Wheeler, E., White, C.L., and Ballmann, A.E., 2011, Recovery of little brown bats (Myotis lucifugus) from natural infection with Geomyces destructans, white-nose syndrome: Journal of Wildlife Diseases, v. 47, no. 3, p. 618-626, https://doi.org/10.7589/0090-3558-47.3.618.","productDescription":"9 p.","startPage":"618","endPage":"626","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-025621","costCenters":[{"id":456,"text":"National Wildlife Health 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,{"id":70005696,"text":"70005696 - 2011 - Refugial isolation and divergence in the Narrowheaded Gartersnake species complex (Thamnophis rufipunctatus) as revealed by multilocus DNA sequence data","interactions":[],"lastModifiedDate":"2021-05-18T15:33:29.966251","indexId":"70005696","displayToPublicDate":"2011-11-16T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2774,"text":"Molecular Ecology","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Refugial isolation and divergence in the Narrowheaded Gartersnake species complex (<i>Thamnophis rufipunctatus</i>) as revealed by multilocus DNA sequence data","title":"Refugial isolation and divergence in the Narrowheaded Gartersnake species complex (Thamnophis rufipunctatus) as revealed by multilocus DNA sequence data","docAbstract":"<p><span>Glacial–interglacial cycles of the Pleistocene are hypothesized as one of the foremost contributors to biological diversification. This is especially true for cold‐adapted montane species, where range shifts have had a pronounced effect on population‐level divergence. Gartersnakes of the&nbsp;</span><i>Thamnophis rufipunctatus</i><span>&nbsp;species complex are restricted to cold headwater streams in the highlands of the Sierra Madre Occidental and southwestern USA. We used coalescent and multilocus phylogenetic approaches to test whether genetic diversification of this montane‐restricted species complex is consistent with two prevailing models of range fluctuation for species affected by Pleistocene climate changes. Our concatenated nuDNA and multilocus species analyses recovered evidence for the persistence of multiple lineages that are restricted geographically, despite a mtDNA signature consistent with either more recent connectivity (and introgression) or recent expansion (and incomplete lineage sorting). Divergence times estimated using a relaxed molecular clock and fossil calibrations fall within the Late Pleistocene, and zero gene flow scenarios among current geographically isolated lineages could not be rejected. These results suggest that increased climate shifts in the Late Pleistocene have driven diversification and current range retraction patterns and that the differences between markers reflect the stochasticity of gene lineages (i.e. ancestral polymorphism) rather than gene flow and introgression. These results have important implications for the conservation of&nbsp;</span><i>T.&nbsp;rufipunctatus</i><span>&nbsp;(sensu novo), which is restricted to two drainage systems in the southwestern US and has undergone a recent and dramatic decline.</span></p>","language":"English","publisher":"Wiley","publisherLocation":"Malden, MA","doi":"10.1111/j.1365-294X.2011.05211.x","usgsCitation":"Wood, D.A., Vandergast, A.G., Espinal, A.L., Fisher, R., and Holycross, A., 2011, Refugial isolation and divergence in the Narrowheaded Gartersnake species complex (Thamnophis rufipunctatus) as revealed by multilocus DNA sequence data: Molecular Ecology, v. 20, no. 18, p. 3856-3878, https://doi.org/10.1111/j.1365-294X.2011.05211.x.","productDescription":"23 p.","startPage":"3856","endPage":"3878","numberOfPages":"23","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":204336,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"20","issue":"18","noUsgsAuthors":false,"publicationDate":"2011-08-18","publicationStatus":"PW","scienceBaseUri":"4f4e4a60e4b07f02db63516f","contributors":{"authors":[{"text":"Wood, Dustin A. 0000-0002-7668-9911 dawood@usgs.gov","orcid":"https://orcid.org/0000-0002-7668-9911","contributorId":4179,"corporation":false,"usgs":true,"family":"Wood","given":"Dustin","email":"dawood@usgs.gov","middleInitial":"A.","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":true,"id":353076,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Vandergast, Amy G. 0000-0002-7835-6571","orcid":"https://orcid.org/0000-0002-7835-6571","contributorId":57201,"corporation":false,"usgs":true,"family":"Vandergast","given":"Amy","middleInitial":"G.","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":true,"id":353078,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Espinal, A. Lemos","contributorId":81623,"corporation":false,"usgs":false,"family":"Espinal","given":"A.","email":"","middleInitial":"Lemos","affiliations":[],"preferred":false,"id":353080,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Fisher, Robert N. 0000-0002-2956-3240","orcid":"https://orcid.org/0000-0002-2956-3240","contributorId":51675,"corporation":false,"usgs":true,"family":"Fisher","given":"Robert N.","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":true,"id":353077,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Holycross, A.T.","contributorId":79060,"corporation":false,"usgs":false,"family":"Holycross","given":"A.T.","affiliations":[],"preferred":false,"id":353079,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70005949,"text":"sir20105160 - 2011 - Highway-runoff quality, and treatment efficiencies of a hydrodynamic-settling device and a stormwater-filtration device in Milwaukee, Wisconsin","interactions":[],"lastModifiedDate":"2012-03-08T17:16:43","indexId":"sir20105160","displayToPublicDate":"2011-11-16T00:00:00","publicationYear":"2011","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":"2010-5160","title":"Highway-runoff quality, and treatment efficiencies of a hydrodynamic-settling device and a stormwater-filtration device in Milwaukee, Wisconsin","docAbstract":"The treatment efficiencies of two prefabricated stormwater-treatment devices were tested at a freeway site in a high-density urban part of Milwaukee, Wisconsin. One treatment device is categorized as a hydrodynamic-settling device (HSD), which removes pollutants by sedimentation and flotation. The other treatment device is categorized as a stormwater-filtration device (SFD), which removes pollutants by filtration and sedimentation. During runoff events, flow measurements were recorded and water-quality samples were collected at the inlet and outlet of each device. Efficiency-ratio and summation-of-load (SOL) calculations were used to estimate the treatment efficiency of each device. Event-mean concentrations and loads that were decreased by passing through the HSD include total suspended solids (TSS), suspended sediment (SS), total phosphorus (TP), total copper (TCu), and total zinc (TZn). The efficiency ratios for these constituents were 42, 57, 17, 33, and 23 percent, respectively. The SOL removal rates for these constituents were 25, 49, 10, 27, and 16 percent, respectively. Event-mean concentrations and loads that increased by passing through the HSD include chloride (Cl), total dissolved solids (TDS), and dissolved zinc (DZn). The efficiency ratios for these constituents were -347, -177, and 20 percent, respectively. Four constituents&mdash;dissolved phosphorus (DP), chemical oxygen demand (COD), total polycyclic aromatic hydrocarbon (PAH), and dissolved copper (DCu)&mdash;are not included in the list of computed efficiency ratio and SOL because the variability between sampled inlet and outlet pairs were not significantly different. Event-mean concentrations and loads that decreased by passing through the SFD include TSS, SS, TP, DCu, TCu, DZn, TZn, and COD. The efficiency ratios for these constituents were 59, 90, 40, 21, 66, 23, 66, and 18, respectively. The SOLs for these constituents were 50, 89, 37, 19, 60, 20, 65, and 21, respectively. Two constituents&mdash;DP and PAH&mdash;are not included in the lists of computed efficiency ratio and SOL because the variability between sampled inlet and outlet pairs were not significantly different. Similar to the HSD, the average efficiency ratios and SOLs for TDS and Cl were negative. Flow rates, high concentrations of SS, and particle-size distributions (PSD) can affect the treatment efficacies of the two devices. Flow rates equal to or greater than the design flow rate of the HSD had minimal or negative removal efficiencies for TSS and SS loads. Similar TSS removal efficiencies were observed at the SFD, but SS was consistently removed throughout the flow regime. Removal efficiencies were high for both devices when concentrations of SS and TSS approached 200 mg/L. A small number of runoff events were analyzed for PSD; the average sand content at the HSD was 33 percent and at the SFD was 71 percent. The 71-percent sand content may reflect the 90-percent removal efficiency of SS at the SFD. Particles retained at the bottom of both devices were largely sand-size or greater.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20105160","collaboration":"Prepared in cooperation with the Wisconsin Department of Transportation and the Wisconsin Department of Natural Resources","usgsCitation":"Horwatich, J.A., Bannerman, R.T., and Pearson, R., 2011, Highway-runoff quality, and treatment efficiencies of a hydrodynamic-settling device and a stormwater-filtration device in Milwaukee, Wisconsin: U.S. Geological Survey Scientific Investigations Report 2010-5160, vii, 40 p.; Appendices, https://doi.org/10.3133/sir20105160.","productDescription":"vii, 40 p.; Appendices","startPage":"i","endPage":"76","numberOfPages":"83","additionalOnlineFiles":"N","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":116427,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/sir_2010_5160.jpg"},{"id":110850,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2010/5160/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Wisconsin","county":"Milwaukee County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -88.5,41 ], [ -88.5,43.5 ], [ -87,43.5 ], [ -87,41 ], [ -88.5,41 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae1e4b07f02db688763","contributors":{"authors":[{"text":"Horwatich, Judy A. 0000-0003-0582-0836 jahorwat@usgs.gov","orcid":"https://orcid.org/0000-0003-0582-0836","contributorId":1388,"corporation":false,"usgs":true,"family":"Horwatich","given":"Judy","email":"jahorwat@usgs.gov","middleInitial":"A.","affiliations":[{"id":37947,"text":"Upper Midwest Water Science Center","active":true,"usgs":true}],"preferred":true,"id":353519,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bannerman, Roger T. 0000-0001-9221-2905 rbannerman@usgs.gov","orcid":"https://orcid.org/0000-0001-9221-2905","contributorId":5560,"corporation":false,"usgs":true,"family":"Bannerman","given":"Roger","email":"rbannerman@usgs.gov","middleInitial":"T.","affiliations":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"preferred":true,"id":353520,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Pearson, Robert","contributorId":50409,"corporation":false,"usgs":true,"family":"Pearson","given":"Robert","affiliations":[],"preferred":false,"id":353521,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70003554,"text":"70003554 - 2011 - Refocusing the Debate about Advocacy","interactions":[],"lastModifiedDate":"2015-06-05T11:22:03","indexId":"70003554","displayToPublicDate":"2011-11-16T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1321,"text":"Conservation Biology","active":true,"publicationSubtype":{"id":10}},"title":"Refocusing the Debate about Advocacy","language":"English","publisher":"Blackwell Publishing","publisherLocation":"Malden, MA","doi":"10.1111/j.1523-1739.2010.01629.x","usgsCitation":"Scott, J.M., and Rachlow, J.L., 2011, Refocusing the Debate about Advocacy: Conservation Biology, v. 25, no. 1, p. 1-3, https://doi.org/10.1111/j.1523-1739.2010.01629.x.","productDescription":"3 p.","startPage":"1","endPage":"3","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":474896,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1111/j.1523-1739.2010.01629.x","text":"Publisher Index Page"},{"id":204279,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"25","issue":"1","noUsgsAuthors":false,"publicationDate":"2011-01-19","publicationStatus":"PW","scienceBaseUri":"4f4e4a60e4b07f02db63513c","contributors":{"authors":[{"text":"Scott, J. Michael","contributorId":98877,"corporation":false,"usgs":true,"family":"Scott","given":"J.","email":"","middleInitial":"Michael","affiliations":[],"preferred":false,"id":347714,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rachlow, Janet L.","contributorId":69298,"corporation":false,"usgs":true,"family":"Rachlow","given":"Janet","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":347713,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
]}