{"pageNumber":"3909","pageRowStart":"97700","pageSize":"25","recordCount":185161,"records":[{"id":70019144,"text":"70019144 - 1995 - Diatom evidence for earthquake-induced subsidence and tsunami 300 yr ago in southern coastal Washington","interactions":[],"lastModifiedDate":"2023-12-23T15:32:59.428244","indexId":"70019144","displayToPublicDate":"1995-01-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1786,"text":"Geological Society of America Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Diatom evidence for earthquake-induced subsidence and tsunami 300 yr ago in southern coastal Washington","docAbstract":"

Fossil diatoms from four stratigraphic sections along the tidal Niawiakum River, southwestern Washington, provide an independent paleoecological test of a relative sea-level rise that has been attributed to subsidence during an inferred earthquake in the Cascadia subduction zone about 300 yr ago. Diatom assemblages in a buried soil and overlying mud indicate a sudden and lasting shift from marshes and forests near or above highest tides to mud flats and incipient tidal marshes, with a progressive return to high-level tidal marshes by sediment aggradation and, perhaps, gradual tectonic uplift. The amount of coseismic submergence required to generate the paleoecological changes observed at these sites could have ranged from a minimum of 0.8–1.0 m to a maximum of ∼3.0 m.

Fossil diatoms also provide an independent test of previous inferences that the subsidence was shortly followed by a tsunami. The inferred tsunami deposit is a distinct sandy interval that widely overlies the buried marsh and forest soil. Diatoms from this interval consist of species observed on modern sand flats of the open bay, identifying a bayward source for the sand. Occurrences of the same sand-flat species above the buried soil in the farthest up-valley outcrop where a sandy interval is not recognizable suggest that the tsunami extended farther landward than was previously inferred from the stratigraphy.

These data rule out proposed alternatives to the coseismic subsidence model—that is, climatically induced sea-level rise, temporary submergence caused by storms—and support the hypothesis that a great earthquake struck southwestern Washington 300 yr ago.

","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1995)107<0367:DEFEIS>2.3.CO;2","usgsCitation":"Hemphill-Haley, E., 1995, Diatom evidence for earthquake-induced subsidence and tsunami 300 yr ago in southern coastal Washington: Geological Society of America Bulletin, v. 107, no. 3, p. 367-378, https://doi.org/10.1130/0016-7606(1995)107<0367:DEFEIS>2.3.CO;2.","productDescription":"12 p.","startPage":"367","endPage":"378","numberOfPages":"12","costCenters":[],"links":[{"id":226410,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"107","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a00abe4b0c8380cd4f856","contributors":{"authors":[{"text":"Hemphill-Haley, E.","contributorId":69309,"corporation":false,"usgs":true,"family":"Hemphill-Haley","given":"E.","email":"","affiliations":[],"preferred":false,"id":381795,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70171401,"text":"70171401 - 1995 - Distribution of phytobenthos in the Yakima River basin, Washington, in relation to geology, land use, and other environmental factors","interactions":[],"lastModifiedDate":"2016-05-31T10:18:24","indexId":"70171401","displayToPublicDate":"1995-01-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1169,"text":"Canadian Journal of Fisheries and Aquatic Sciences","active":true,"publicationSubtype":{"id":10}},"title":"Distribution of phytobenthos in the Yakima River basin, Washington, in relation to geology, land use, and other environmental factors","docAbstract":"

Benthic-algal distributions in the Yakima River, Washington, basin were, examined in relation to geology, land use, water chemistry, and stream habitat using indicator-species classification (TWINSPAN) and canonical correspondence analysis (CCA). Algal assemblages identified byTWINSPAN were each associated with a narrow range of water-quality conditions. In the Cascade geologic province, where timber harvest and grazing are the dominant land uses, differences in community structure (CCA site scores) and concentrations of major ions (Ca and Mg) and nutrients (solute P, SiO2 and inorganic N) varied with dominant rock type of the basin. In agricultural areas of the Columbia Plateau province, differences in phytobenthos structure were based primarily on the degree of enrichment of dissolved solids, inorganic N, and solute P from irrigation-return flows and subsurface drainage. Habitat characteristics strongly correlated with community structure included reach altitude, turbidity, substratum embeddedness (Columbia Plateau), large woody-debris density (Cascade Range), and composition and density of the riparian vegetation. Algal biomass (AFDM) correlated with composition and density of the riparian vegetation but not with measured chemical-constituent concentrations. Nitrogen limitation in streams of the Cascade Range favored nitrogen-fixing blue-green algae and diatoms with endosymbiotic blue-greens, whereas nitrogen heterotrophs were abundant in agricultural areas of the Columbia Plateau.

","language":"English","publisher":"NRC Research Press","doi":"10.1139/f95-108","usgsCitation":"Leland, H.V., 1995, Distribution of phytobenthos in the Yakima River basin, Washington, in relation to geology, land use, and other environmental factors: Canadian Journal of Fisheries and Aquatic Sciences, v. 52, no. 5, p. 1108-1129, https://doi.org/10.1139/f95-108.","productDescription":"22 p.","startPage":"1108","endPage":"1129","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":622,"text":"Washington Water Science Center","active":true,"usgs":true}],"links":[{"id":321888,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"52","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"574eb5c1e4b0ee97d51a83ae","contributors":{"authors":[{"text":"Leland, Harry V.","contributorId":51158,"corporation":false,"usgs":true,"family":"Leland","given":"Harry","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":630895,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70019089,"text":"70019089 - 1995 - Western frontal fault of the Canyon Range: Is it the breakaway zone of the Sevier Desert detachment?","interactions":[],"lastModifiedDate":"2024-01-21T22:35:48.765039","indexId":"70019089","displayToPublicDate":"1995-01-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1796,"text":"Geology","active":true,"publicationSubtype":{"id":10}},"title":"Western frontal fault of the Canyon Range: Is it the breakaway zone of the Sevier Desert detachment?","docAbstract":"

Geologic evidence developed from surface exposures demonstrates that the western frontal fault of the Canyon Range is a major structure representing the eastern breakaway zone of the Sevier Desert detachment. The western frontal fault of the Canyon Range east of Delta, Utah, is a north-trending, west-dipping, low-angle (18 °–24 ° ) normal fault that juxtaposes syntectonic conglomerates and large-rock avalanches of the Miocene Oak City Formation against footwall rocks that have been ductilely, cataclastically, and brittlely deformed. The Oak City strata dip variably to the east; dips are shallow in eastern outcrops (5 ° –15 ° ), steeper in central outcrops (20 ° –60 ° ), and shallow in the western outcrops (10 ° –20 ° ). In eastern exposures, the shallow dips of the Oak City Formation (5 ° –15 ° ) and the acute angle of 20 ° –35 ° between the western frontal fault and Oak City units limit past rotation of the fault to ≤15 ° . The systematic variation in the dip of Oak City units from east to west suggests that the western frontal fault probably flattens beneath present Oak City outcrops, linking the fault to the shallow reflector seen in the COCORP (Consortium for Continental Reflection Profiling) Utah line 1 seismic line beneath the westernmost outcrops of the Oak City Formation. Upper plate movement is constrained by Oak City clast compositions and rock-avalanche lithologies, fault geometry, and lower plate reconstruction to a maximum of 6–7 km since Oak City syntectonic deposition at ∼12–13 Ma. Maximum upper plate displacement for the entire Sevier Desert detachment cannot be determined from these breakaway-zone exposures.

","language":"English","publisher":"Geological Society of America","doi":"10.1130/0091-7613(1995)023<0547:WFFOTC>2.3.CO;2","issn":"00917613","usgsCitation":"Otton, J.K., 1995, Western frontal fault of the Canyon Range: Is it the breakaway zone of the Sevier Desert detachment?: Geology, v. 23, no. 6, p. 547-550, https://doi.org/10.1130/0091-7613(1995)023<0547:WFFOTC>2.3.CO;2.","productDescription":"4 p.","startPage":"547","endPage":"550","numberOfPages":"4","costCenters":[],"links":[{"id":226317,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"23","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bd009e4b08c986b32ec47","contributors":{"authors":[{"text":"Otton, J. K.","contributorId":52589,"corporation":false,"usgs":true,"family":"Otton","given":"J.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":381643,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":85747,"text":"85747 - 1995 - Marine turtles in the Southeast","interactions":[{"subject":{"id":85747,"text":"85747 - 1995 - Marine turtles in the Southeast","indexId":"85747","publicationYear":"1995","noYear":false,"title":"Marine turtles in the Southeast"},"predicate":"IS_PART_OF","object":{"id":70148108,"text":"70148108 - 1995 - Our living resources: A report to the nation on the distribution, abundance, and health of U.S. plants, animals, and ecosystems","indexId":"70148108","publicationYear":"1995","noYear":false,"title":"Our living resources: A report to the nation on the distribution, abundance, and health of U.S. plants, animals, and ecosystems"},"id":1}],"isPartOf":{"id":70148108,"text":"70148108 - 1995 - Our living resources: A report to the nation on the distribution, abundance, and health of U.S. plants, animals, and ecosystems","indexId":"70148108","publicationYear":"1995","noYear":false,"title":"Our living resources: A report to the nation on the distribution, abundance, and health of U.S. plants, animals, and ecosystems"},"lastModifiedDate":"2017-04-18T16:01:32","indexId":"85747","displayToPublicDate":"1995-01-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Marine turtles in the Southeast","docAbstract":"

Five species of marine turtles frequent the beaches and offshore waters of the southeastern United States: loggerhead (Caretta caretta), green (Chelonia mydas), Kemp's ridley (Lepidochelys kempii), leatherback (Dermochelys coriacea), and hawksbill (Eretmochelys imbricata). All five are reported to nest, but only the loggerhead and green turtle do so in substantial numbers. Most nesting occurs from southern North Carolina to the middle west coast of Florida, but scattered nesting occurs from Virginia through southern Texas. The beaches of Florida, particularly in Brevard and Indian River counties, host what may be the world's largest population of loggerheads.

","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Our living resources: A report to the nation on the distribution, abundance, and health of U.S. plants, animals, and ecosystems","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"National Biological Service","publisherLocation":"Washington, DC","usgsCitation":"Dodd, C.K., 1995, Marine turtles in the Southeast, chap. of Our living resources: A report to the nation on the distribution, abundance, and health of U.S. plants, animals, and ecosystems, p. 121-123.","productDescription":"3 p.","startPage":"121","endPage":"123","costCenters":[{"id":275,"text":"Florida Integrated Science Center","active":false,"usgs":true}],"links":[{"id":339893,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://www.webharvest.gov/peth04/20041019015728/https://biology.usgs.gov/s+t/index.htm","linkHelpText":"Archived website"},{"id":127772,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a25e4b07f02db60ec96","contributors":{"editors":[{"text":"LaRoe, Edward T.","contributorId":112276,"corporation":false,"usgs":true,"family":"LaRoe","given":"Edward","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":504736,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Farris, Gaye S.","contributorId":84410,"corporation":false,"usgs":true,"family":"Farris","given":"Gaye","email":"","middleInitial":"S.","affiliations":[{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true}],"preferred":true,"id":504739,"contributorType":{"id":2,"text":"Editors"},"rank":2},{"text":"Puckett, Catherine E. cpuckett@usgs.gov","contributorId":4629,"corporation":false,"usgs":true,"family":"Puckett","given":"Catherine","email":"cpuckett@usgs.gov","middleInitial":"E.","affiliations":[],"preferred":true,"id":504737,"contributorType":{"id":2,"text":"Editors"},"rank":3},{"text":"Doran, Peter D.","contributorId":17533,"corporation":false,"usgs":true,"family":"Doran","given":"Peter","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":504738,"contributorType":{"id":2,"text":"Editors"},"rank":4},{"text":"Mac, Michael J.","contributorId":16772,"corporation":false,"usgs":true,"family":"Mac","given":"Michael","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":504735,"contributorType":{"id":2,"text":"Editors"},"rank":5}],"authors":[{"text":"Dodd, C. Kenneth Jr.","contributorId":89215,"corporation":false,"usgs":true,"family":"Dodd","given":"C.","suffix":"Jr.","email":"","middleInitial":"Kenneth","affiliations":[],"preferred":false,"id":296314,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70171272,"text":"70171272 - 1995 - Effect of lake-wide planktivory by the pelagic prey fish community in Lakes Michigan and Ontario","interactions":[],"lastModifiedDate":"2016-05-26T10:07:00","indexId":"70171272","displayToPublicDate":"1995-01-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1169,"text":"Canadian Journal of Fisheries and Aquatic Sciences","active":true,"publicationSubtype":{"id":10}},"title":"Effect of lake-wide planktivory by the pelagic prey fish community in Lakes Michigan and Ontario","docAbstract":"

We compared predatory demand by pelagic planktivorous prey fish with invertebrate production in Lake Michigan during 1987 and in Lake Ontario during 1990. Predation by the planktivores in Lake Ontario was nearly fourfold higher than in Lake Michigan (approx. 87 g wet weight∙m−2∙year−1). Predation rates on Mysis were comparable in Lakes Michigan and Ontario (approx. 21 g∙m−2∙year−1), while predation on Diporeia was markedly higher in Lake Michigan than in Lake Ontario (21.3 vs. 8.5 g wet weight∙m−2∙year−1). In Lake Ontario, predatory demand on zooplankton exceeded our best estimate of production by a factor of 1.7. Similarly, predation estimates on Mysis in Lake Ontario were 1.2–2.0 times the estimated rate of production, depending on the production model used. Lake Michigan planktivores consumed approximately 55% of available zooplankton production in 1987, indicating that competition for prey resources, if operating, was not as intense as that in Lake Ontario in 1990. It is unclear how to resolve the paradox that predation could markedly exceed available prey production in some cases. There could be sources of error in the estimates of both the supply and demand sides of these trophic relationships.

","language":"English","publisher":"NRC Research Press","doi":"10.1139/f95-148","usgsCitation":"Rand, P.S., Stewart, D.J., Lantry, B.F., Rudstam, L.G., Johannsson, O.E., Goyke, A.P., Brandt, S., O’Gorman, R., and Eck, G.W., 1995, Effect of lake-wide planktivory by the pelagic prey fish community in Lakes Michigan and Ontario: Canadian Journal of Fisheries and Aquatic Sciences, v. 52, no. 7, p. 1546-1563, https://doi.org/10.1139/f95-148.","productDescription":"18 p.","startPage":"1546","endPage":"1563","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":321719,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"52","issue":"7","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57481e2ee4b07e28b664db9a","contributors":{"authors":[{"text":"Rand, Peter S.","contributorId":63765,"corporation":false,"usgs":true,"family":"Rand","given":"Peter","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":630395,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stewart, Donald J.","contributorId":33660,"corporation":false,"usgs":true,"family":"Stewart","given":"Donald","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":630396,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lantry, Brian F. 0000-0001-8797-3910 bflantry@usgs.gov","orcid":"https://orcid.org/0000-0001-8797-3910","contributorId":3435,"corporation":false,"usgs":true,"family":"Lantry","given":"Brian","email":"bflantry@usgs.gov","middleInitial":"F.","affiliations":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"preferred":true,"id":630397,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Rudstam, Lars G.","contributorId":56609,"corporation":false,"usgs":false,"family":"Rudstam","given":"Lars","email":"","middleInitial":"G.","affiliations":[{"id":12722,"text":"Cornell University","active":true,"usgs":false}],"preferred":false,"id":630398,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Johannsson, Ora E.","contributorId":25527,"corporation":false,"usgs":true,"family":"Johannsson","given":"Ora","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":630399,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Goyke, Andrew P.","contributorId":169636,"corporation":false,"usgs":false,"family":"Goyke","given":"Andrew","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":630400,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Brandt, Stephen B.","contributorId":29588,"corporation":false,"usgs":false,"family":"Brandt","given":"Stephen B.","affiliations":[{"id":12452,"text":"Oregon Sea Grant","active":true,"usgs":false}],"preferred":false,"id":630401,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"O’Gorman, Robert rogorman@usgs.gov","contributorId":3451,"corporation":false,"usgs":true,"family":"O’Gorman","given":"Robert","email":"rogorman@usgs.gov","affiliations":[],"preferred":true,"id":630402,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Eck, Gary W.","contributorId":106053,"corporation":false,"usgs":true,"family":"Eck","given":"Gary","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":630403,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}} ,{"id":70182281,"text":"70182281 - 1995 - Comparison of the polymerases (L genes) of spring viirenira of carp virus and infectious hematopoietic necrosis virus","interactions":[],"lastModifiedDate":"2017-02-22T13:23:50","indexId":"70182281","displayToPublicDate":"1995-01-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3689,"text":"Veterinary Research","active":true,"publicationSubtype":{"id":10}},"title":"Comparison of the polymerases (L genes) of spring viirenira of carp virus and infectious hematopoietic necrosis virus","docAbstract":"

No abstract available 

","language":"English","usgsCitation":"Bjorklund, H., Emmenegger, E., and Kurath, G., 1995, Comparison of the polymerases (L genes) of spring viirenira of carp virus and infectious hematopoietic necrosis virus: Veterinary Research, v. 26, p. 394-398.","productDescription":"5 p. ","startPage":"394","endPage":"398","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":335966,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"26","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58aeb144e4b01ccd54f9ee60","contributors":{"authors":[{"text":"Bjorklund, H.V.","contributorId":152581,"corporation":false,"usgs":false,"family":"Bjorklund","given":"H.V.","affiliations":[],"preferred":false,"id":670358,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Emmenegger, E.J.","contributorId":7463,"corporation":false,"usgs":true,"family":"Emmenegger","given":"E.J.","email":"","affiliations":[],"preferred":false,"id":670359,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kurath, Gael 0000-0003-3294-560X gkurath@usgs.gov","orcid":"https://orcid.org/0000-0003-3294-560X","contributorId":100522,"corporation":false,"usgs":true,"family":"Kurath","given":"Gael","email":"gkurath@usgs.gov","affiliations":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"preferred":true,"id":670360,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70184277,"text":"70184277 - 1995 - Estimating prefledging survival: Allowing for brood mixing and dependence among brood mates","interactions":[],"lastModifiedDate":"2017-03-06T17:12:00","indexId":"70184277","displayToPublicDate":"1995-01-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2508,"text":"Journal of Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"Estimating prefledging survival: Allowing for brood mixing and dependence among brood mates","docAbstract":"

Estimates of juvenile survival from hatch to fledging provide important information on waterfowl productivity. We develop a model for estimating survival of young waterfowl from hatch to fledging. Our model enables interchange of individuals among broods and relaxes the assumption that individuals within broods have independent survival probabilities. The model requires repeated observations of individually identifiable adults and their offspring that are not individually identifiable. A modified Kaplan-Meier procedure (Pollock et al. 1989a,b) and a modified Mayfield procedure (Mayfield 1961, 1975; Johnson 1979) can be used under this general modeling framework, and survival rates and corresponding variances of the point estimators can be determined.

","language":"English","publisher":"Wiley","doi":"10.2307/3802450","usgsCitation":"Flint, P.L., Pollock, K.H., Thomas, D., and Sedinger, J.S., 1995, Estimating prefledging survival: Allowing for brood mixing and dependence among brood mates: Journal of Wildlife Management, v. 59, no. 3, p. 448-455, https://doi.org/10.2307/3802450.","productDescription":"8","startPage":"448","endPage":"455","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":336904,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"59","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58be833fe4b014cc3a3a9a1d","contributors":{"authors":[{"text":"Flint, Paul L. 0000-0002-8758-6993 pflint@usgs.gov","orcid":"https://orcid.org/0000-0002-8758-6993","contributorId":3284,"corporation":false,"usgs":true,"family":"Flint","given":"Paul","email":"pflint@usgs.gov","middleInitial":"L.","affiliations":[{"id":117,"text":"Alaska Science Center Biology WTEB","active":true,"usgs":true},{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"preferred":true,"id":680856,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pollock, Kenneth H.","contributorId":8590,"corporation":false,"usgs":false,"family":"Pollock","given":"Kenneth","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":680857,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Thomas, Dana","contributorId":187556,"corporation":false,"usgs":false,"family":"Thomas","given":"Dana","email":"","affiliations":[],"preferred":false,"id":680858,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Sedinger, James S.","contributorId":84861,"corporation":false,"usgs":false,"family":"Sedinger","given":"James","email":"","middleInitial":"S.","affiliations":[{"id":12742,"text":"University of Nevada Reno","active":true,"usgs":false}],"preferred":false,"id":680859,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70018898,"text":"70018898 - 1995 - Identifying trends in sediment discharge from alterations in upstream land use","interactions":[],"lastModifiedDate":"2013-03-13T21:18:43","indexId":"70018898","displayToPublicDate":"1995-01-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1483,"text":"Effects of scale on interpretation and management of sediment and water quality. Proc. symposium, Boulder, 1995","active":true,"publicationSubtype":{"id":10}},"title":"Identifying trends in sediment discharge from alterations in upstream land use","docAbstract":"Environmental monitoring is a primary reason for collecting sediment data. One emphasis of this monitoring is identification of trends in suspended sediment discharge. A stochastic equation was used to generate time series of annual suspended sediment discharges using statistics from gaging stations with drainage areas between 1606 and 1 805 230 km2. Annual sediment discharge was increased linearly to yield a given increase at the end of a fixed period and trend statistics were computed for each simulation series using Kendal's tau (at 0.05 significance level). A parameter was calculated from two factors that control trend detection time: (a) the magnitude of change in sediment discharge, and (b) the natural variability of sediment discharge. In this analysis the detection of a trend at most stations is well over 100 years for a 20% increase in sediment discharge. Further research is needed to assess the sensitivity of detecting trends at sediment stations.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Effects of scale on interpretation and management of sediment and water quality. Proc. symposium, Boulder, 1995","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Parker, R.S., and Osterkamp, W.R., 1995, Identifying trends in sediment discharge from alterations in upstream land use: Effects of scale on interpretation and management of sediment and water quality. Proc. symposium, Boulder, 1995, v. 226, p. 207-213.","startPage":"207","endPage":"213","numberOfPages":"7","costCenters":[],"links":[{"id":226802,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":269312,"type":{"id":11,"text":"Document"},"url":"https://iahs.info/redbooks/a226/iahs_226_0207.pdf"}],"volume":"226","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a385ce4b0c8380cd6153f","contributors":{"authors":[{"text":"Parker, R. S.","contributorId":104510,"corporation":false,"usgs":true,"family":"Parker","given":"R.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":381049,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Osterkamp, W. R.","contributorId":46044,"corporation":false,"usgs":true,"family":"Osterkamp","given":"W.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":381048,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":85959,"text":"85959 - 1995 - Movements, distribution, and population dynamics of polar bears in the Beaufort Sea","interactions":[],"lastModifiedDate":"2012-02-02T00:04:00","indexId":"85959","displayToPublicDate":"1995-01-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":21,"text":"Thesis"},"publicationSubtype":{"id":28,"text":"Thesis"},"title":"Movements, distribution, and population dynamics of polar bears in the Beaufort Sea","language":"English","publisher":"University of Alaska","publisherLocation":"Fairbanks, AK","usgsCitation":"Amstrup, S.C., 1995, Movements, distribution, and population dynamics of polar bears in the Beaufort Sea, 299.","productDescription":"299","costCenters":[{"id":106,"text":"Alaska Biological Science Center","active":false,"usgs":true}],"links":[{"id":127967,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7fe4b07f02db648696","contributors":{"authors":[{"text":"Amstrup, Steven C.","contributorId":67034,"corporation":false,"usgs":false,"family":"Amstrup","given":"Steven","email":"","middleInitial":"C.","affiliations":[{"id":13182,"text":"Polar Bears International","active":true,"usgs":false}],"preferred":false,"id":296682,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70019064,"text":"70019064 - 1995 - Channel degradation in southeastern Nebraska Rivers","interactions":[],"lastModifiedDate":"2012-03-12T17:19:15","indexId":"70019064","displayToPublicDate":"1995-01-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Channel degradation in southeastern Nebraska Rivers","docAbstract":"Many stream channels in southeastern Nebraska were dredged and straightened during 1904-15. The resulting channels were both shorter and steeper than the original channels. Tests for time trends were conducted using the nonparametric Kendall tau test to see if the channels have responded to these changes. Tests were conducted on the stages associated with specific discharges and on measurement characteristics at gaging stations. Tests also were conducted on hydrologic forcing variables (annual mean precipitation, annual peak discharges, annual mean discharge, and annual mean base flows). The null hypothesis (that the data were free from trend) was rejected for stages associated with the mean of the annual discharges for 6 of 7 gaging stations in the study area, but was accepted for all 3 gages on the main stem of the Missouri River. The trends at the 6 streamflow gaging stations were for decreasing stages (degrading channels) for specific discharges. The rates of change ranged from about 0.2 to 0.5 m per decade. Mean stream bed elevations computed for individual discharge measurements at these streamflow gaging stations confirmed that the channels are degrading. However, neither the precipitation nor flow variables show evidence of trends. The tendency for the channels to degrade thus cannot be attributed to changes in runoff characteristics and are assumed to be a response to the channel modifications in the early 1900's. Indications are that the channels presently are continuing to degrade.","largerWorkTitle":"Watershed Management Symposium - Proceedings","conferenceTitle":"Proceedings of the 1995 Watershed Management Symposium","conferenceDate":"14 August 1995 through 16 August 1995","conferenceLocation":"San Antonio, TX, USA","language":"English","publisher":"ASCE","publisherLocation":"New York, NY, United States","usgsCitation":"Wahl, K.L., and Weiss, L.S., 1995, Channel degradation in southeastern Nebraska Rivers, in Watershed Management Symposium - Proceedings, San Antonio, TX, USA, 14 August 1995 through 16 August 1995, p. 250-259.","startPage":"250","endPage":"259","numberOfPages":"10","costCenters":[],"links":[{"id":226626,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f451e4b0c8380cd4bc74","contributors":{"editors":[{"text":"Ward Rim J.","contributorId":128413,"corporation":true,"usgs":false,"organization":"Ward Rim J.","id":536445,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Wahl, Kenneth L.","contributorId":61024,"corporation":false,"usgs":true,"family":"Wahl","given":"Kenneth","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":381568,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Weiss, Linda S. lsweiss@usgs.gov","contributorId":2955,"corporation":false,"usgs":true,"family":"Weiss","given":"Linda","email":"lsweiss@usgs.gov","middleInitial":"S.","affiliations":[],"preferred":true,"id":381567,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70018814,"text":"70018814 - 1995 - Evidence of active dune sand on the Great Plains in the 19th century from accounts of early explorers","interactions":[],"lastModifiedDate":"2013-01-25T13:35:04","indexId":"70018814","displayToPublicDate":"1995-01-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3218,"text":"Quaternary Research","active":true,"publicationSubtype":{"id":10}},"title":"Evidence of active dune sand on the Great Plains in the 19th century from accounts of early explorers","docAbstract":"Dune fields are found in several areas of the Great Plains, and though mostly stabilised today, the accounts of early explorers show that they were more mobile in the last century. Using an index of dune mobility and tree ring data, it is found that these periods of mobility were related to temperature-induced drought, the high temperatures increasing evapotranspiration. Explorers also record that rivers upwind of these dune fields had shallow braided channels in the 19th century, and these would have supplied further aeolian sand. It is concluded that these dunes are extremely susceptible to climate change and that it may not need global warming to increase their mobility again. -K.Clayton","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Quaternary Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","publisherLocation":"Amsterdam, Netherlands","doi":"10.1006/qres.1995.1020","issn":"00335894","usgsCitation":"Muhs, D., and Holliday, V., 1995, Evidence of active dune sand on the Great Plains in the 19th century from accounts of early explorers: Quaternary Research, v. 43, no. 2, p. 198-208, https://doi.org/10.1006/qres.1995.1020.","startPage":"198","endPage":"208","numberOfPages":"11","costCenters":[],"links":[{"id":227139,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":266467,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1006/qres.1995.1020"}],"volume":"43","issue":"2","noUsgsAuthors":false,"publicationDate":"2017-01-20","publicationStatus":"PW","scienceBaseUri":"505a0d5ee4b0c8380cd52f9e","contributors":{"authors":[{"text":"Muhs, D.R. 0000-0001-7449-251X","orcid":"https://orcid.org/0000-0001-7449-251X","contributorId":61460,"corporation":false,"usgs":true,"family":"Muhs","given":"D.R.","affiliations":[],"preferred":false,"id":380832,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Holliday, V.T.","contributorId":107048,"corporation":false,"usgs":true,"family":"Holliday","given":"V.T.","email":"","affiliations":[],"preferred":false,"id":380833,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70018853,"text":"70018853 - 1995 - Techniques for determining pressure in the hydrothermal diamond- anvil cell: behavior and identification of ice polymorphs (I, III, V, VI)","interactions":[],"lastModifiedDate":"2012-03-12T17:19:13","indexId":"70018853","displayToPublicDate":"1995-01-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":738,"text":"American Mineralogist","active":true,"publicationSubtype":{"id":10}},"title":"Techniques for determining pressure in the hydrothermal diamond- anvil cell: behavior and identification of ice polymorphs (I, III, V, VI)","docAbstract":"For H2O densities > 1.0 g/cm3, a determination of the ice melting temperature provides the density information required to calculate the P-T path that the sample in a hydrothermal diamond-anvil cell follows when the sample is heated isochorically. The principal difficulty is the identification of the polymorph because of metastable behavior of ices in the H2O system. Usually, an accurate identification of the liquidus ice phase can be made without analytical instrumentation and requires only careful observations. -Authors","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"American Mineralogist","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"0003004X","usgsCitation":"Haselton, H., I-Ming, C., Shen, A., and Bassett, W.A., 1995, Techniques for determining pressure in the hydrothermal diamond- anvil cell: behavior and identification of ice polymorphs (I, III, V, VI): American Mineralogist, v. 80, no. 11-12, p. 1302-1306.","startPage":"1302","endPage":"1306","numberOfPages":"5","costCenters":[],"links":[{"id":226889,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"80","issue":"11-12","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505ba41ae4b08c986b3200e8","contributors":{"authors":[{"text":"Haselton, H.T. Jr.","contributorId":83520,"corporation":false,"usgs":true,"family":"Haselton","given":"H.T.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":380935,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"I-Ming, Chou","contributorId":94041,"corporation":false,"usgs":true,"family":"I-Ming","given":"Chou","email":"","affiliations":[],"preferred":false,"id":380936,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Shen, A.H.","contributorId":7855,"corporation":false,"usgs":true,"family":"Shen","given":"A.H.","email":"","affiliations":[],"preferred":false,"id":380933,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bassett, William A.","contributorId":47533,"corporation":false,"usgs":true,"family":"Bassett","given":"William","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":380934,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70018818,"text":"70018818 - 1995 - Glacial morphology and depositional sequences of the Antarctic Continental Shelf","interactions":[],"lastModifiedDate":"2024-01-21T22:43:58.314027","indexId":"70018818","displayToPublicDate":"1995-01-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1796,"text":"Geology","active":true,"publicationSubtype":{"id":10}},"title":"Glacial morphology and depositional sequences of the Antarctic Continental Shelf","docAbstract":"

We propose a simple model for the unusual depositional sequences and morphology of the Antarctic continental shelf. Our model considers the regional stratal geometry and the reversed morphology of the Antarctic continental shelf to be principally the results of time-integrated effects of glacial erosion and sedimentation related to the location of the ice grounding line. The model offers several guidelines for stratigraphic interpretation of the Antarctic shelf and a Northern Hemisphere shelf, both of which were subject to many glacial advances and retreats.

","language":"English","publisher":"Geological Society of America","doi":"10.1130/0091-7613(1995)023<0580:GMADSO>2.3.CO;2","issn":"00917613","usgsCitation":"ten Brink, U., and Schneider, C., 1995, Glacial morphology and depositional sequences of the Antarctic Continental Shelf: Geology, v. 23, no. 7, p. 580-584, https://doi.org/10.1130/0091-7613(1995)023<0580:GMADSO>2.3.CO;2.","productDescription":"5 p.","startPage":"580","endPage":"584","numberOfPages":"5","costCenters":[],"links":[{"id":479266,"rank":2,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://hdl.handle.net/1912/1605","text":"External Repository"},{"id":227186,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"23","issue":"7","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a2909e4b0c8380cd5a61f","contributors":{"authors":[{"text":"ten Brink, Uri S. 0000-0001-6858-3001 utenbrink@usgs.gov","orcid":"https://orcid.org/0000-0001-6858-3001","contributorId":127560,"corporation":false,"usgs":true,"family":"ten Brink","given":"Uri S.","email":"utenbrink@usgs.gov","affiliations":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true},{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":380842,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schneider, Christopher","contributorId":41504,"corporation":false,"usgs":true,"family":"Schneider","given":"Christopher","email":"","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":380841,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70018791,"text":"70018791 - 1995 - Environmental probabilistic quantitative assessment methodologies","interactions":[],"lastModifiedDate":"2013-01-21T13:07:37","indexId":"70018791","displayToPublicDate":"1995-01-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1315,"text":"Computers & Geosciences","printIssn":"0098-3004","active":true,"publicationSubtype":{"id":10}},"title":"Environmental probabilistic quantitative assessment methodologies","docAbstract":"In this paper, four petroleum resource assessment methodologies are presented as possible pollution assessment methodologies, even though petroleum as a resource is desirable, whereas pollution is undesirable. A methodology is defined in this paper to consist of a probability model and a probabilistic method, where the method is used to solve the model. The following four basic types of probability models are considered: 1) direct assessment, 2) accumulation size, 3) volumetric yield, and 4) reservoir engineering. Three of the four petroleum resource assessment methodologies were written as microcomputer systems, viz. TRIAGG for direct assessment, APRAS for accumulation size, and FASPU for reservoir engineering. A fourth microcomputer system termed PROBDIST supports the three assessment systems. The three assessment systems have different probability models but the same type of probabilistic method. The type of advantages of the analytic method are in computational speed and flexibility, making it ideal for a microcomputer. -from Author","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Computers and Geosciences","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","doi":"10.1016/0098-3004(95)00034-6","usgsCitation":"Crovelli, R., 1995, Environmental probabilistic quantitative assessment methodologies: Computers & Geosciences, v. 21, no. 8, p. 971-984, https://doi.org/10.1016/0098-3004(95)00034-6.","startPage":"971","endPage":"984","numberOfPages":"14","costCenters":[],"links":[{"id":227539,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":266155,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0098-3004(95)00034-6"}],"volume":"21","issue":"8","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a09dee4b0c8380cd520c7","contributors":{"authors":[{"text":"Crovelli, R. 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Laboratory and field-testing data will be integrated to calibrate the flow models and to determine sensitivities of the system.","largerWorkTitle":"High Level Radioactive Waste Management - Proceedings of the Annual International Conference","conferenceTitle":"Proceedings of the 6th Annual International Conference on High Level Radioactive Waste Management","conferenceDate":"30 April 1995 through 5 May 1995","conferenceLocation":"Las Vegas, NV, USA","language":"English","publisher":"ASCE","publisherLocation":"New York, NY, United States","usgsCitation":"Anna, L.O., 1995, Discrete fracture modeling-ESF North Portal Area, Yucca Mountain Nevada, in High Level Radioactive Waste Management - Proceedings of the Annual International Conference, Las Vegas, NV, USA, 30 April 1995 through 5 May 1995, p. 126-128.","startPage":"126","endPage":"128","numberOfPages":"3","costCenters":[],"links":[{"id":227140,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a01f5e4b0c8380cd4fdfb","contributors":{"editors":[{"text":"Hughes Howard R.","contributorId":128387,"corporation":true,"usgs":false,"organization":"Hughes Howard R.","id":536441,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Anna, Lawrence O.","contributorId":107318,"corporation":false,"usgs":true,"family":"Anna","given":"Lawrence","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":380834,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":7000012,"text":"7000012 - 1995 - Gemstones: An overview of production of specific U.S. gemstones","interactions":[],"lastModifiedDate":"2012-02-02T00:04:35","indexId":"7000012","displayToPublicDate":"1995-01-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":363,"text":"General Interest Publication","active":false,"publicationSubtype":{"id":6}},"title":"Gemstones: An overview of production of specific U.S. gemstones","language":"ENGLISH","doi":"10.3133/7000012","usgsCitation":"Austin, G.T., 1995, Gemstones: An overview of production of specific U.S. gemstones: General Interest Publication, 41 p. : (col. ill.) ; 22 cm., https://doi.org/10.3133/7000012.","productDescription":"41 p. : (col. ill.) ; 22 cm.","costCenters":[],"links":[{"id":132769,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":18585,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://minerals.usgs.gov/minerals/pubs/commodity/gemstones/sp14-95/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b28e4b07f02db6b10d2","contributors":{"authors":[{"text":"Austin, Gordon T.","contributorId":98688,"corporation":false,"usgs":true,"family":"Austin","given":"Gordon","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":343965,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70018807,"text":"70018807 - 1995 - Relations between pesticide use and riverine flux in the Mississippi River Basin","interactions":[],"lastModifiedDate":"2021-05-27T14:57:01.195032","indexId":"70018807","displayToPublicDate":"1995-01-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1226,"text":"Chemosphere","active":true,"publicationSubtype":{"id":10}},"title":"Relations between pesticide use and riverine flux in the Mississippi River Basin","docAbstract":"In an intensive subcontimental study of pesticides in surface waters of the United States, concentrations of 26 high-use pesticides were measured at nine sites in the Mississippi River basin from May 1991 through March 1992. Calculated total fluxes were combined with agricultural-use data to estimate the percentage of applied pesticide reaching the mouths of the Mississippi River and six major tributaries. For most pesticides, the riverine flux was less than 2% of the mass applied agriculturally. The insecticide diazinon was detected frequently in rivers draining the three basins with the highest population densities, apparently as a result of urban use.","language":"English","publisher":"Elsevier","doi":"10.1016/0045-6535(95)00176-9","usgsCitation":"Larson, S., Capel, P.D., Goolsby, D.A., Zaugg, S.D., and Sandstrom, M.W., 1995, Relations between pesticide use and riverine flux in the Mississippi River Basin: Chemosphere, v. 31, no. 5, p. 3305-3321, https://doi.org/10.1016/0045-6535(95)00176-9.","productDescription":"17 p.","startPage":"3305","endPage":"3321","costCenters":[{"id":452,"text":"National Water Quality Laboratory","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":227051,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","otherGeospatial":"Mississippi River basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -89.4287109375,\n 29.726222319395504\n ],\n [\n -89.736328125,\n 32.13840869677249\n ],\n [\n -87.71484375,\n 33.797408767572485\n ],\n [\n -84.814453125,\n 34.45221847282654\n ],\n [\n -82.001953125,\n 36.35052700542763\n ],\n [\n -79.8046875,\n 39.9434364619742\n ],\n [\n -79.6728515625,\n 42.13082130188811\n ],\n [\n -83.5400390625,\n 41.60722821271717\n ],\n [\n -87.6708984375,\n 41.409775832009565\n ],\n [\n -87.978515625,\n 43.35713822211053\n ],\n [\n -89.736328125,\n 45.36758436884978\n ],\n [\n -90.17578124999999,\n 46.58906908309182\n ],\n [\n -94.52636718749999,\n 46.98025235521883\n ],\n [\n -96.6357421875,\n 46.649436163350245\n ],\n [\n -101.513671875,\n 48.719961222646276\n ],\n [\n -104.23828125,\n 48.951366470947725\n ],\n [\n -114.521484375,\n 49.03786794532644\n ],\n [\n -113.466796875,\n 44.933696389694674\n ],\n [\n -111.3134765625,\n 44.43377984606822\n ],\n [\n -108.6328125,\n 43.03677585761058\n ],\n [\n -108.67675781249999,\n 42.52069952914966\n ],\n [\n -105.64453124999999,\n 40.27952566881291\n ],\n [\n -105.8203125,\n 37.47485808497102\n ],\n [\n -104.23828125,\n 34.63320791137959\n ],\n [\n -97.294921875,\n 33.17434155100208\n ],\n [\n -93.779296875,\n 30.977609093348686\n ],\n [\n -93.6474609375,\n 29.76437737516313\n ],\n [\n -89.8681640625,\n 28.8831596093235\n ],\n [\n -88.9892578125,\n 29.036960648558267\n ],\n [\n -89.4287109375,\n 29.726222319395504\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"31","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50e4a6fae4b0e8fec6cdc31f","contributors":{"authors":[{"text":"Larson, Steven J.","contributorId":29845,"corporation":false,"usgs":true,"family":"Larson","given":"Steven J.","affiliations":[],"preferred":false,"id":380810,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Capel, Paul D. 0000-0003-1620-5185 capel@usgs.gov","orcid":"https://orcid.org/0000-0003-1620-5185","contributorId":1002,"corporation":false,"usgs":true,"family":"Capel","given":"Paul","email":"capel@usgs.gov","middleInitial":"D.","affiliations":[{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true},{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true},{"id":37778,"text":"WMA - Integrated Modeling and Prediction Division","active":true,"usgs":true}],"preferred":true,"id":380814,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Goolsby, Donald A.","contributorId":46083,"corporation":false,"usgs":true,"family":"Goolsby","given":"Donald","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":380812,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Zaugg, Steven D. sdzaugg@usgs.gov","contributorId":768,"corporation":false,"usgs":true,"family":"Zaugg","given":"Steven","email":"sdzaugg@usgs.gov","middleInitial":"D.","affiliations":[],"preferred":true,"id":380813,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Sandstrom, Mark W. 0000-0003-0006-5675 sandstro@usgs.gov","orcid":"https://orcid.org/0000-0003-0006-5675","contributorId":706,"corporation":false,"usgs":true,"family":"Sandstrom","given":"Mark","email":"sandstro@usgs.gov","middleInitial":"W.","affiliations":[{"id":37464,"text":"WMA - Laboratory & Analytical Services Division","active":true,"usgs":true},{"id":503,"text":"Office of Water Quality","active":true,"usgs":true},{"id":5046,"text":"Branch of Analytical Serv (NWQL)","active":true,"usgs":true},{"id":452,"text":"National Water Quality Laboratory","active":true,"usgs":true}],"preferred":true,"id":380811,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":70018861,"text":"70018861 - 1995 - Chemistry and petrography of calcite in the KTB pilot borehole, Bavarian Oberpfalz, Germany","interactions":[],"lastModifiedDate":"2018-03-12T12:29:48","indexId":"70018861","displayToPublicDate":"1995-01-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1213,"text":"Chemical Geology","active":true,"publicationSubtype":{"id":10}},"title":"Chemistry and petrography of calcite in the KTB pilot borehole, Bavarian Oberpfalz, Germany","docAbstract":"The KTB pilot borehole in northeast Bavaria, Germany, penetrates 4000 m of gneiss, amphibolite, and subordinate calc-silicate, lamprophyre and metagabbro. There are three types of calcite in the drilled section: 1) metamorphic calcite in calc-silicate and marble; 2) crack-filling calcite in all lithologies; and 3) replacement calcite in altered minerals. Crack-filling and replacement calcite postdate metamorphic calcite. Multiple calcite generations in individual cracks suggest that different generations of water repeatedly flowed through the same cracks. Crack-filling mineral assemblages that include calcite originally formed at temperatures of 150-350??C. Presently, crack-filling calcite is in chemical and isotopic equilibrium with saline to brackish water in the borehole at temperatures of ???120??C. The saline to brackish water contains a significant proportion of meteoric water. Re-equilibration of crack-filling calcite to lower temperatures means that calcite chemistry tells us little about water-rock interactions in the crystal section of temperatures higher than ~120??C. -from Author","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Chemical Geology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","doi":"10.1016/0009-2541(95)00063-R","issn":"00092541","usgsCitation":"Komor, S., 1995, Chemistry and petrography of calcite in the KTB pilot borehole, Bavarian Oberpfalz, Germany: Chemical Geology, v. 124, no. 3-4, p. 199-215, https://doi.org/10.1016/0009-2541(95)00063-R.","productDescription":"17 p.","startPage":"199","endPage":"215","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":226345,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":266050,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0009-2541(95)00063-R"}],"volume":"124","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f5a6e4b0c8380cd4c342","contributors":{"authors":[{"text":"Komor, S.C.","contributorId":21182,"corporation":false,"usgs":true,"family":"Komor","given":"S.C.","email":"","affiliations":[],"preferred":false,"id":380956,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70018854,"text":"70018854 - 1995 - U-Th-Pb zircon dating of the 13.8-Ma dacite volcanic dome at Cerro Rico de Potosi, Bolivia","interactions":[],"lastModifiedDate":"2013-03-13T15:46:30","indexId":"70018854","displayToPublicDate":"1995-01-01T00:00:00","publicationYear":"1995","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":"U-Th-Pb zircon dating of the 13.8-Ma dacite volcanic dome at Cerro Rico de Potosi, Bolivia","docAbstract":"The temporal relationship between the extrusion of the Miocene dacite volcanic dome at Cerro Rico de Potasi, Bolivia, and the associated Ag-Sn mineralization has an important bearing on the heat and metal sources for this world class mineral deposit. The present study uses U-Th-Pb dating of sparse zircon contained in the dacite to demonstrate that, at most, only several hundred thousand years separate dome emplacement from main stage mineralization. -from Authors","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Earth and Planetary Science Letters","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","doi":"10.1016/0012-821X(95)00093-R","usgsCitation":"Zartman, R., and Cunningham, C.G., 1995, U-Th-Pb zircon dating of the 13.8-Ma dacite volcanic dome at Cerro Rico de Potosi, Bolivia: Earth and Planetary Science Letters, v. 133, no. 3-4, p. 227-237, https://doi.org/10.1016/0012-821X(95)00093-R.","startPage":"227","endPage":"237","numberOfPages":"11","costCenters":[],"links":[{"id":269260,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0012-821X(95)00093-R"},{"id":226890,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"133","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb9e2e4b08c986b327e9a","contributors":{"authors":[{"text":"Zartman, R. E.","contributorId":15632,"corporation":false,"usgs":true,"family":"Zartman","given":"R. E.","affiliations":[],"preferred":false,"id":380937,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cunningham, C. G.","contributorId":76741,"corporation":false,"usgs":true,"family":"Cunningham","given":"C.","middleInitial":"G.","affiliations":[],"preferred":false,"id":380938,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70018806,"text":"70018806 - 1995 - Determination of nanogram per liter concentrations of volatile organic compounds in water by capillary gas chromatography and selected ion monitoring mass spectrometry and its use to define groundwater flow directions in Edwards Aquifer, Texas","interactions":[],"lastModifiedDate":"2021-05-27T15:41:13.404596","indexId":"70018806","displayToPublicDate":"1995-01-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":761,"text":"Analytical Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"Determination of nanogram per liter concentrations of volatile organic compounds in water by capillary gas chromatography and selected ion monitoring mass spectrometry and its use to define groundwater flow directions in Edwards Aquifer, Texas","docAbstract":"A method has been developed to measure nanogram per liter amounts of selected volatile organic compounds (VOCs) including dichlorodifluoromethane, trichlorofluoromethane, cis-1,2-dichloroethene, trichloroethene, tetrachloroethene, and the isomers of dichlorobenzene in water. The method uses purge-and-trap techniques on a 100 mL sample, gas chromatography with a megabore capillary column, and electron impact, selected ion monitoring mass spectrometry. Minimum detection levels for these compounds ranged from 1 to 4 ng/L in water. Recoveries from organic-free distilled water and natural groundwater ranged from 70.5% for dichlorodifluoromethane to 107.8% for 1,4-dichlorobenzene. Precision was generally best for cis-1,2-dichloroethene, tetrachloroethene, and the dichlorobenzene isomers and worst for dichlorodifluoromethane and trichlorofluoromethane. Blank data indicated persistent, trace-level introduction of dichlorodifluoromethane, 1,4-dichlorobenzene, and tetrachloroemene to samples during storage and shipment at concentrations less than the method reporting limits. The largest concentrations of the selected VOCs in 27 water samples from the Edwards aquifer near San Antonio, TX, were from confined-zone wells near an abandoned landfill. The results defined a zone of water with no detectable VOCs in nearly all of the aquifer west of San Antonio and from part of the confined zone beneath San Antonio.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Analytical Chemistry","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1021/ac00116a008","issn":"00032700","usgsCitation":"Buszka, P., Rose, D., Ozuna, G., and Groschen, G., 1995, Determination of nanogram per liter concentrations of volatile organic compounds in water by capillary gas chromatography and selected ion monitoring mass spectrometry and its use to define groundwater flow directions in Edwards Aquifer, Texas: Analytical Chemistry, v. 67, no. 20, p. 3659-3667, https://doi.org/10.1021/ac00116a008.","startPage":"3659","endPage":"3667","numberOfPages":"9","costCenters":[{"id":452,"text":"National Water Quality Laboratory","active":true,"usgs":true}],"links":[{"id":227050,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"67","issue":"20","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","scienceBaseUri":"5059ffb8e4b0c8380cd4f35e","contributors":{"authors":[{"text":"Buszka, P.M.","contributorId":49001,"corporation":false,"usgs":true,"family":"Buszka","given":"P.M.","affiliations":[],"preferred":false,"id":380809,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rose, D.L.","contributorId":36960,"corporation":false,"usgs":true,"family":"Rose","given":"D.L.","email":"","affiliations":[],"preferred":false,"id":380808,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ozuna, G. B.","contributorId":25205,"corporation":false,"usgs":true,"family":"Ozuna","given":"G. B.","affiliations":[],"preferred":false,"id":380807,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Groschen, G.E.","contributorId":17260,"corporation":false,"usgs":true,"family":"Groschen","given":"G.E.","email":"","affiliations":[],"preferred":false,"id":380806,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70018823,"text":"70018823 - 1995 - The spectra program library: A PC based system for gamma-ray spectra analysis and INAA data reduction","interactions":[],"lastModifiedDate":"2012-03-12T17:19:13","indexId":"70018823","displayToPublicDate":"1995-01-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2439,"text":"Journal of Radioanalytical and Nuclear Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"The spectra program library: A PC based system for gamma-ray spectra analysis and INAA data reduction","docAbstract":"A PC based system has been developed for the analysis of gamma-ray spectra and for the complete reduction of data from INAA experiments, including software to average the results from mulitple lines and multiple countings and to produce a final report of analysis. Graphics algorithms may be called for the analysis of complex spectral features, to compare the data from alternate photopeaks and to evaluate detector performance during a given counting cycle. A database of results for control samples can be used to prepare quality control charts to evaluate long term precision and to search for systemic variations in data on reference samples as a function of time. The entire software library can be accessed through a user-friendly menu interface with internal help.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Radioanalytical and Nuclear Chemistry","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1007/BF02038245","issn":"02365731","usgsCitation":"Baedecker, P.A., and Grossman, J.N., 1995, The spectra program library: A PC based system for gamma-ray spectra analysis and INAA data reduction: Journal of Radioanalytical and Nuclear Chemistry, v. 198, no. 1, p. 55-68, https://doi.org/10.1007/BF02038245.","startPage":"55","endPage":"68","numberOfPages":"14","costCenters":[],"links":[{"id":205750,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF02038245"},{"id":226563,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"198","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb05ae4b08c986b324de8","contributors":{"authors":[{"text":"Baedecker, P. A.","contributorId":95444,"corporation":false,"usgs":true,"family":"Baedecker","given":"P.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":380859,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Grossman, J. N.","contributorId":41840,"corporation":false,"usgs":true,"family":"Grossman","given":"J.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":380858,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70018790,"text":"70018790 - 1995 - Maastrichtian ammonites chiefly from the Prairie Bluff Chalk in Alabama and Mississippi","interactions":[],"lastModifiedDate":"2024-06-07T00:37:55.412713","indexId":"70018790","displayToPublicDate":"1995-01-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2412,"text":"Journal of Paleontology","active":true,"publicationSubtype":{"id":10}},"title":"Maastrichtian ammonites chiefly from the Prairie Bluff Chalk in Alabama and Mississippi","docAbstract":"

The Prairie Bluff Chalk of Alabama and Mississippi yields a diverse ammonite fauna of Maastrichtian age. Twenty-eight species, of which three are new, are recorded herein: Pseudophyllites indra (Forbes, 1846), Hauericeras rembda (Forbes, 1846), Pachydiscus (Pachydiscus) maconensis n. sp., P. (P.) cf. gollevillensis (d'Orbigny, 1850), P. (P.) jacquoti (Seunes, 1890), P. (P.) egertoni (Forbes, 1846), Sphenodiscus lobatus (Tuomey, 1854), S. pleurisepta (Conrad, 1857), Coahuilites sheltoni Böse, 1928, Nostoceras (Nostoceras) alternatum (Tuomey, 1854), N. (N.) mendryki Cobban, 1974a, N. (N.) magdadiae Lefeld and Uberna, 1991, N. (N.) irregulare n. sp., Glyptoxoceras torquatum (Morton, 1834), Glyptoxoceras sp. A, Glyptoxoceras? sp., Baculites lomaensis Anderson, 1958, Baculites spp. A–C, Eubaculites labyrinthicus (Morton, 1834), E. carinatus (Morton, 1834), Baculites? trabeatus (Morton, 1834), Trachybaculites columna (Morton, 1834), Discoscaphites conradi (Morton, 1834), D. gulosus (Morton, 1834), Jeletzkytes criptonodosus Riccardi, 1983, Trachyscaphites alabamensis n. sp., and T. yorkensis (Stephenson, 1941). One genus, Trachybaculites, is new. The bulk of the fauna can be referred to a Discoscaphites conradi assemblage zone, but some elements in the fauna are significantly older.

","language":"English","publisher":"Paleontological Society","doi":"10.1017/S0022336000061096","issn":"00223360","usgsCitation":"Cobban, W.A., and Kennedy, W.J., 1995, Maastrichtian ammonites chiefly from the Prairie Bluff Chalk in Alabama and Mississippi: Journal of Paleontology, v. 69, no. 5 Suppl.2, 40 p., https://doi.org/10.1017/S0022336000061096.","productDescription":"40 p.","numberOfPages":"40","costCenters":[],"links":[{"id":227538,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"69","issue":"5 Suppl.2","noUsgsAuthors":false,"publicationDate":"2017-08-11","publicationStatus":"PW","scienceBaseUri":"505a4b04e4b0c8380cd69224","contributors":{"authors":[{"text":"Cobban, W. A.","contributorId":21577,"corporation":false,"usgs":true,"family":"Cobban","given":"W.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":380764,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kennedy, W. J.","contributorId":81873,"corporation":false,"usgs":true,"family":"Kennedy","given":"W.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":380765,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70019063,"text":"70019063 - 1995 - Seismic images of the Brooks Range, Arctic Alaska, reveal crustal- scale duplexing","interactions":[],"lastModifiedDate":"2024-01-21T22:41:33.390943","indexId":"70019063","displayToPublicDate":"1995-01-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1796,"text":"Geology","active":true,"publicationSubtype":{"id":10}},"title":"Seismic images of the Brooks Range, Arctic Alaska, reveal crustal- scale duplexing","docAbstract":"

An integrated set of seismic reflection and refraction data collected across the Brooks Range, Arctic Alaska, in 1990, has yielded a composite image of this Mesozoic and Cenozoic fold-and-thrust belt that reveals duplexing to lower-crustal depths. Interpretations from this image are as follows. (1) Many terranes and subterranes that were amalgamated in the Late Jurassic to Early Cretaceous extend no deeper than the upper crust (3–10 km). (2) In contrast, crustal duplexing, extending to nearly 30 km depth above a south-dipping basal decollement, has produced latest Cretaceous to Cenozoic antiforms, including the Doonerak antiform in the central Brooks Range and anticlinoria near the northern range front. (3) The duplexing occurs in basement rocks of the North Slope subterrane, which core the antiforms. (4) North-dipping structures in the middle crust of the Yukon-Koyukuk basin and southern Brooks Range may postdate Mesozoic terrane amalgamation and predate or coincide with the duplexing. (5) The thickest crust, 50 km, occurs beneath the north-central Brooks Range, north of the root zone of the basal decollement. The position of the thickest crust may indicate that either the duplexed crust above the decollement was thrust onto and depressed the plate beneath the North Slope or the protracted tectonic history of the Brooks Range has left structures not simply explainable in terms of a single collisional event.

","language":"English","publisher":"Geological Society of America","doi":"10.1130/0091-7613(1995)023<0065:SIOTBR>2.3.CO;2","issn":"00917613","usgsCitation":"Fuis, G., Levander, A.R., Lutter, W.J., Wissinger, E.S., Moore, T., and Christensen, N., 1995, Seismic images of the Brooks Range, Arctic Alaska, reveal crustal- scale duplexing: Geology, v. 23, no. 1, p. 65-68, https://doi.org/10.1130/0091-7613(1995)023<0065:SIOTBR>2.3.CO;2.","productDescription":"4 p.","startPage":"65","endPage":"68","numberOfPages":"4","costCenters":[],"links":[{"id":226625,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"23","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b8b22e4b08c986b317608","contributors":{"authors":[{"text":"Fuis, G. S.","contributorId":83131,"corporation":false,"usgs":true,"family":"Fuis","given":"G. S.","affiliations":[],"preferred":false,"id":381562,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Levander, A. R.","contributorId":104644,"corporation":false,"usgs":false,"family":"Levander","given":"A.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":381566,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lutter, W. J.","contributorId":90361,"corporation":false,"usgs":true,"family":"Lutter","given":"W.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":381565,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Wissinger, E. S.","contributorId":86496,"corporation":false,"usgs":false,"family":"Wissinger","given":"E.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":381564,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Moore, Thomas E. 0000-0002-0878-0457","orcid":"https://orcid.org/0000-0002-0878-0457","contributorId":85592,"corporation":false,"usgs":true,"family":"Moore","given":"Thomas E.","affiliations":[],"preferred":false,"id":381563,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Christensen, N.I.","contributorId":28016,"corporation":false,"usgs":true,"family":"Christensen","given":"N.I.","email":"","affiliations":[],"preferred":false,"id":381561,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}} ,{"id":70018812,"text":"70018812 - 1995 - Benzene oxidation coupled to sulfate reduction","interactions":[],"lastModifiedDate":"2023-01-17T18:58:50.805917","indexId":"70018812","displayToPublicDate":"1995-01-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":850,"text":"Applied and Environmental Microbiology","active":true,"publicationSubtype":{"id":10}},"title":"Benzene oxidation coupled to sulfate reduction","docAbstract":"

Highly reduced sediments from San Diego Bay, Calif., that were incubated under strictly anaerobic conditions metabolized benzene within 55 days when they were exposed initially to I μM benzene. The rate of benzene metabolism increased as benzene was added back to the benzene-adapted sediments. When a [14C]benzene tracer was included with the benzene added to benzene-adapted sediments, 92% of the added radioactivity was recovered as 14CO2. Molybdate, an inhibitor of sulfate reduction, inhibited benzene uptake and production of 14CO2 from [14C]benzene. Benzene metabolism stopped when the sediments became sulfate depleted, and benzene uptake resumed when sulfate was added again. The stoichiometry of benzene uptake and sulfate reduction was consistent with the hypothesis that sulfate was the principal electron acceptor for benzene oxidation. Isotope trapping experiments performed with [14C]benzene revealed that there was no production of such potential extracellular intermediates of benzene oxidation as phenol, benzoate, p-hydroxybenzoate, cyclohexane, catechol, and acetate. The results demonstrate that benzene can be oxidized in the absence of O2, with sulfate serving as the electron acceptor, and suggest that some sulfate reducers are capable of completely oxidizing benzene to carbon dioxide without the production of extracellular intermediates. Although anaerobic benzene oxidation coupled to chelated Fe(III) has been documented previously, the study reported here provides the first example of a natural sediment compound that can serve as an electron acceptor for anaerobic benzene oxidation.

","language":"English","publisher":"American Society for Microbiology","doi":"10.1128/aem.61.3.953-958.1995","issn":"00992240","usgsCitation":"Lovley, D.R., Coates, J., Woodward, J., and Phillips, E.J., 1995, Benzene oxidation coupled to sulfate reduction: Applied and Environmental Microbiology, v. 61, no. 3, p. 953-958, https://doi.org/10.1128/aem.61.3.953-958.1995.","productDescription":"6 p.","startPage":"953","endPage":"958","costCenters":[],"links":[{"id":480206,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1128/aem.61.3.953-958.1995","text":"Publisher Index Page"},{"id":227137,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"San Diego Bay, Shelter Island","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -117.23810995830215,\n 32.707734442169766\n ],\n [\n -117.23188723338819,\n 32.70699919493039\n ],\n [\n -117.21884096873957,\n 32.718048443724214\n ],\n [\n -117.21781100047781,\n 32.72245331815786\n ],\n [\n -117.22373331798272,\n 32.72544995262754\n ],\n [\n -117.22716654552178,\n 32.72548605604291\n ],\n [\n -117.22845400584848,\n 32.72394662591029\n ],\n [\n -117.22991312755256,\n 32.72019172754641\n ],\n [\n -117.23574961436893,\n 32.717700409653375\n ],\n [\n -117.23768080485948,\n 32.71206760831814\n ],\n [\n -117.23810995830215,\n 32.707734442169766\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"61","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f0c5e4b0c8380cd4a8e0","contributors":{"authors":[{"text":"Lovley, Derek R.","contributorId":107852,"corporation":false,"usgs":true,"family":"Lovley","given":"Derek","middleInitial":"R.","affiliations":[],"preferred":false,"id":380830,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Coates, J.D.","contributorId":105451,"corporation":false,"usgs":true,"family":"Coates","given":"J.D.","email":"","affiliations":[],"preferred":false,"id":380829,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Woodward, J.C.","contributorId":62590,"corporation":false,"usgs":true,"family":"Woodward","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":380828,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Phillips, Elizabeth J.P.","contributorId":37475,"corporation":false,"usgs":true,"family":"Phillips","given":"Elizabeth","middleInitial":"J.P.","affiliations":[],"preferred":false,"id":380827,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70018857,"text":"70018857 - 1995 - Fate, bioavailability and toxicity of silver in estuarine environments","interactions":[],"lastModifiedDate":"2019-02-25T09:41:59","indexId":"70018857","displayToPublicDate":"1995-01-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2676,"text":"Marine Pollution Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Fate, bioavailability and toxicity of silver in estuarine environments","docAbstract":"

The chemistry and bioavailability of Ag contribute to its high toxicity in marine and estuarine waters. Silver is unusual, in that both the dominant speciation reaction in seawater and the processes important in sorbing Ag in sediments favour enhanced bioavailability. Formation of a stable chloro complex favours dispersal of dissolved Ag, and the abundant chloro complex is available to biota. Sequestration by sediments also occurs, but with relatively slow kinetics. Amorphous aggregated coatings enhance Ag accumulation in sediments, as well as Ag uptake from sediments by deposit feeders. In estuaries, the bioaccumulation of Ag increases 56-fold with each unit of increased Ag concentration in sediments. Toxicity for sensitive marine species occurs at absolute concentrations as low as those observed for any nonalkylated metal, partly because bioaccumulation increases so steeply with contamination. The environmental window of tolerance to Ag in estuaries could be narrower than for many elements.

","language":"English","publisher":"Elsevier","doi":"10.1016/0025-326X(95)00081-W","issn":"0025326X","usgsCitation":"Luoma, S., Ho, Y., and Bryan, G., 1995, Fate, bioavailability and toxicity of silver in estuarine environments: Marine Pollution Bulletin, v. 31, no. 1-3, p. 44-54, https://doi.org/10.1016/0025-326X(95)00081-W.","productDescription":"11 p.","startPage":"44","endPage":"54","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":552,"text":"San Francisco Bay-Delta","active":false,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true},{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true}],"links":[{"id":205812,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0025-326X(95)00081-W"},{"id":226935,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"31","issue":"1-3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0f15e4b0c8380cd5375a","contributors":{"authors":[{"text":"Luoma, S. N.","contributorId":86353,"corporation":false,"usgs":true,"family":"Luoma","given":"S. N.","affiliations":[],"preferred":false,"id":380945,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ho, Y.B.","contributorId":27208,"corporation":false,"usgs":true,"family":"Ho","given":"Y.B.","email":"","affiliations":[],"preferred":false,"id":380943,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bryan, G.W.","contributorId":84402,"corporation":false,"usgs":true,"family":"Bryan","given":"G.W.","email":"","affiliations":[],"preferred":false,"id":380944,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ]}