{"pageNumber":"4263","pageRowStart":"106550","pageSize":"25","recordCount":184904,"records":[{"id":70196063,"text":"70196063 - 1992 - Characteristics and processing of seismic data collected on thick, floating ice: Results from the Ross Ice Shelf, Antarctica","interactions":[],"lastModifiedDate":"2018-03-15T13:19:09","indexId":"70196063","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1808,"text":"Geophysics","active":true,"publicationSubtype":{"id":10}},"title":"Characteristics and processing of seismic data collected on thick, floating ice: Results from the Ross Ice Shelf, Antarctica","docAbstract":"<p><span>Coincident reflection and refraction data, collected in the austral summer of 1988/89 by Stanford University and the Geophysical Division of the Department of Scientific and Industrial Research, New Zealand, imaged the crust beneath the Ross Ice Shelf, Antarctica. The Ross Ice Shelf is a unique acquisition environment for seismic reflection profiling because of its thick, floating ice cover. The ice shelf velocity structure is multilayered with a high velocity‐gradient firn layer constituting the upper 50 to 100 m. This near surface firn layer influences the data character by amplifying and frequency modulating the incoming wavefield. In addition, the ice‐water column introduces pervasive, high energy seafloor, intra‐ice, and intra‐water multiples that have moveout velocities similar to the expected subseafloor primary velocities. Successful removal of these high energy multiples relies on predictive deconvolution, inverse velocity stack filtering, and frequency filtering. Removal of the multiples reveals a faulted, sedimentary wedge which is truncated at or near the seafloor. Beneath this wedge the reflection character is diffractive to a two‐way traveltime of ∼7.2 s. At this time, a prominent reflection is evident on the southeast end of the reflection profile. This reflection is interpreted as Moho indicating that the crust is ∼21-km thick beneath the profile. These results provide seismic evidence that the extensional features observed in the Ross Sea region of the Ross Embayment extend beneath the Ross Ice Shelf.</span><span><br></span></p>","language":"English","publisher":"Society of Exploration Geophysicists","doi":"10.1190/1.1443205","usgsCitation":"Beaudoin, B.C., ten Brink, U., and Stern, T.A., 1992, Characteristics and processing of seismic data collected on thick, floating ice: Results from the Ross Ice Shelf, Antarctica: Geophysics, v. 57, no. 10, p. 1359-1372, https://doi.org/10.1190/1.1443205.","productDescription":"14 p.","startPage":"1359","endPage":"1372","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":352566,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Ross Ice Shelf, Antarctica","volume":"57","issue":"10","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5aff2826e4b0da30c1bfd76e","contributors":{"authors":[{"text":"Beaudoin, Bruce C.","contributorId":58140,"corporation":false,"usgs":true,"family":"Beaudoin","given":"Bruce","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":731178,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"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":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true},{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"preferred":false,"id":731179,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stern, Tim A.","contributorId":189814,"corporation":false,"usgs":false,"family":"Stern","given":"Tim","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":731180,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70186639,"text":"70186639 - 1992 - Exploration for submarine mineral deposits by use of gamma-ray radiometric methods","interactions":[],"lastModifiedDate":"2017-04-06T12:57:40","indexId":"70186639","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Exploration for submarine mineral deposits by use of gamma-ray radiometric methods","docAbstract":"<p>No abstract available&nbsp;</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Handbook of geophysical exploration at sea","largerWorkSubtype":{"id":12,"text":"Conference publication"},"language":"English","publisher":"CRC Press","usgsCitation":"Grosz, A.E., 1992, Exploration for submarine mineral deposits by use of gamma-ray radiometric methods, chap. <i>of</i> Handbook of geophysical exploration at sea, p. 283-310.","productDescription":"28 p.","startPage":"283","endPage":"310","costCenters":[],"links":[{"id":339332,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":339331,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.crcpress.com/Handbook-of-Geophysical-Exploration-at-Sea/Geyer-Ashwell/p/book/9780849342523"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58e7540ae4b09da6799c0ca6","contributors":{"authors":[{"text":"Grosz, A. E.","contributorId":87925,"corporation":false,"usgs":true,"family":"Grosz","given":"A.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":690124,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70017188,"text":"70017188 - 1992 - A hydrogen-oxidizing, Fe(III)-reducing microorganism from the Great Bay estuary, New Hampshire","interactions":[],"lastModifiedDate":"2023-01-20T17:29:53.355364","indexId":"70017188","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","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":"A hydrogen-oxidizing, Fe(III)-reducing microorganism from the Great Bay estuary, New Hampshire","docAbstract":"<p><span>A dissimilatory Fe(III)- and Mn(IV)-reducing bacterium was isolated from bottom sediments of the Great Bay estuary, New Hampshire. The isolate was a facultatively anaerobic gram-negative rod which did not appear to fit into any previously described genus. It was temporarily designated strain BrY. BrY grew anaerobically in a defined medium with hydrogen or lactate as the electron donor and Fe(III) as the electron acceptor. BrY required citrate, fumarate, or malate as a carbon source for growth on H</span><sub>2</sub><span>&nbsp;and Fe(III). With Fe(III) as the sole electron acceptor, BrY metabolized hydrogen to a minimum threshold at least 60-fold lower than the threshold reported for pure cultures of sulfate reducers. This finding supports the hypothesis that when Fe(III) is available, Fe(III) reducers can outcompete sulfate reducers for electron donors. Lactate was incompletely oxidized to acetate and carbon dioxide with Fe(III) as the electron acceptor. Lactate oxidation was also coupled to the reduction of Mn(IV), U(VI), fumarate, thiosulfate, or trimethylamine&nbsp;</span><i>n</i><span>-oxide under anaerobic conditions. BrY provides a model for how enzymatic metal reduction by respiratory metal-reducing microorganisms has the potential to contribute to the mobilization of iron and trace metals and to the immobilization of uranium in sediments of Great Bay Estuary.</span></p>","language":"English","publisher":"American Society for Microbiology","doi":"10.1128/aem.58.10.3211-3216.1992","issn":"00992240","usgsCitation":"Caccavo, F., Blakemore, R., and Lovley, D.R., 1992, A hydrogen-oxidizing, Fe(III)-reducing microorganism from the Great Bay estuary, New Hampshire: Applied and Environmental Microbiology, v. 58, no. 10, p. 3211-3216, https://doi.org/10.1128/aem.58.10.3211-3216.1992.","productDescription":"6 p.","startPage":"3211","endPage":"3216","costCenters":[],"links":[{"id":480363,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1128/aem.58.10.3211-3216.1992","text":"Publisher Index 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Jr.","contributorId":15351,"corporation":false,"usgs":true,"family":"Caccavo","given":"F.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":375664,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Blakemore, R.P.","contributorId":104635,"corporation":false,"usgs":true,"family":"Blakemore","given":"R.P.","email":"","affiliations":[],"preferred":false,"id":375665,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lovley, Derek R.","contributorId":107852,"corporation":false,"usgs":true,"family":"Lovley","given":"Derek","middleInitial":"R.","affiliations":[],"preferred":false,"id":375666,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70186695,"text":"70186695 - 1992 - Late Cenozoic faulting at the boundary between the Mojave and Sonoran blocks; Bristol Lake area, California","interactions":[],"lastModifiedDate":"2017-04-07T10:51:53","indexId":"70186695","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Late Cenozoic faulting at the boundary between the Mojave and Sonoran blocks; Bristol Lake area, California","docAbstract":"<p>No abstract available&nbsp;</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Deformation associated with the Neogene, eastern California shear zone, south­ eastern California and southwestern Arizona","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"Workshop on the Eastern California Shear Zone, southeastern California and southwestern Arizona","conferenceDate":"September 4-6, 1991","conferenceLocation":"Santa Barbara, California","language":"English","usgsCitation":"Howard, K.A., and Miller, D., 1992, Late Cenozoic faulting at the boundary between the Mojave and Sonoran blocks; Bristol Lake area, California, <i>in</i> Deformation associated with the Neogene, eastern California shear zone, south­ eastern California and southwestern Arizona, Santa Barbara, California, September 4-6, 1991, p. 37-47.","productDescription":"11 p. ","startPage":"37","endPage":"47","costCenters":[],"links":[{"id":339409,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58e8a554e4b09da6799d641a","contributors":{"authors":[{"text":"Howard, K. A.","contributorId":48938,"corporation":false,"usgs":false,"family":"Howard","given":"K.","middleInitial":"A.","affiliations":[],"preferred":false,"id":690302,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miller, D. M. 0000-0003-3711-0441","orcid":"https://orcid.org/0000-0003-3711-0441","contributorId":104422,"corporation":false,"usgs":true,"family":"Miller","given":"D. M.","affiliations":[],"preferred":false,"id":690303,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70187575,"text":"70187575 - 1992 - Developing a raster profile for the spatial data transfer standard","interactions":[],"lastModifiedDate":"2017-05-09T13:29:53","indexId":"70187575","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1192,"text":"Cartography and Geographic Information Systems","active":true,"publicationSubtype":{"id":10}},"title":"Developing a raster profile for the spatial data transfer standard","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Taylor & Francis","doi":"10.1559/152304092783762146","usgsCitation":"Greenlee, D.D., 1992, Developing a raster profile for the spatial data transfer standard: Cartography and Geographic Information Systems, v. 19, no. 5, p. 300-302, https://doi.org/10.1559/152304092783762146.","productDescription":"3 p.","startPage":"300","endPage":"302","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":341004,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"19","issue":"5","noUsgsAuthors":false,"publicationDate":"2013-03-14","publicationStatus":"PW","scienceBaseUri":"5912d54fe4b0e541a03d456d","contributors":{"authors":[{"text":"Greenlee, David D.","contributorId":59802,"corporation":false,"usgs":true,"family":"Greenlee","given":"David","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":694619,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70016988,"text":"70016988 - 1992 - Evaluation of methyl fluoride and dimethyl ether as inhibitors of aerobic methane oxidation","interactions":[],"lastModifiedDate":"2023-01-20T17:17:11.467845","indexId":"70016988","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","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":"Evaluation of methyl fluoride and dimethyl ether as inhibitors of aerobic methane oxidation","docAbstract":"<p><span>Methyl fluoride (MF) and dimethyl ether (DME) were effective inhibitors of aerobic methanotrophy in a variety of soils. MF and DME blocked consumption of CH</span><sub>4</sub><span>&nbsp;as well as the oxidation of&nbsp;</span><sup>14</sup><span>CH</span><sub>4</sub><span>&nbsp;to&nbsp;</span><sup>14</sup><span>CO</span><sub>2</sub><span>, but neither MF nor DME affected the oxidation of [</span><sup>14</sup><span>C]methanol or [</span><sup>14</sup><span>C]formate to&nbsp;</span><sup>14</sup><span>CO</span><sub>2</sub><span>. Cooxidation of ethane and propane by methane-oxidizing soils was also inhibited by MF. Nitrification (ammonia oxidation) in soils was inhibited by both MF and DME. Production of N</span><sub>2</sub><span>O via nitrification was inhibited by MF; however, MF did not affect N</span><sub>2</sub><span>O production associated with denitrification. Methanogenesis was partially inhibited by MF but not by DME. Methane oxidation was ∼100-fold more sensitive to MF than was methanogenesis, indicating that an optimum concentration could be employed to selectively block methanotrophy. MF inhibited methane oxidation by cell suspensions of&nbsp;</span><i>Methylococcus capsulatus</i><span>; however, DME was a much less effective inhibitor.</span></p>","language":"English","publisher":"American Society for Microbiology","doi":"10.1128/aem.58.9.2983-2992.1992","issn":"00992240","usgsCitation":"Oremland, R.S., and Culbertson, C.W., 1992, Evaluation of methyl fluoride and dimethyl ether as inhibitors of aerobic methane oxidation: Applied and Environmental Microbiology, v. 58, no. 9, p. 2983-2992, https://doi.org/10.1128/aem.58.9.2983-2992.1992.","productDescription":"10 p.","startPage":"2983","endPage":"2992","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":480362,"rank":2,"type":{"id":40,"text":"Open Access 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Branch","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":true,"id":759559,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Culbertson, Charles W. cculbert@usgs.gov","contributorId":1607,"corporation":false,"usgs":true,"family":"Culbertson","given":"Charles","email":"cculbert@usgs.gov","middleInitial":"W.","affiliations":[{"id":371,"text":"Maine Water Science Center","active":true,"usgs":true}],"preferred":true,"id":759560,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70187590,"text":"70187590 - 1992 - Ground-water-quality monitoring for septic-tank-use effects, central New Mexico","interactions":[],"lastModifiedDate":"2017-05-09T17:18:51","indexId":"70187590","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Ground-water-quality monitoring for septic-tank-use effects, central New Mexico","docAbstract":"<p>No abstract available&nbsp;</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Proceedings of the national symposium on the future availability of ground water resources. ","largerWorkSubtype":{"id":12,"text":"Conference publication"},"language":"English","publisher":"American Water Resources Association ","usgsCitation":"Kues, G., 1992, Ground-water-quality monitoring for septic-tank-use effects, central New Mexico, <i>in</i> Proceedings of the national symposium on the future availability of ground water resources. , p. 273-276.","productDescription":"4 p. ","startPage":"273","endPage":"276","costCenters":[],"links":[{"id":341020,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5912d53ee4b0e541a03d4555","contributors":{"authors":[{"text":"Kues, G.E.","contributorId":45722,"corporation":false,"usgs":true,"family":"Kues","given":"G.E.","email":"","affiliations":[],"preferred":false,"id":694657,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70187579,"text":"70187579 - 1992 - A technique for the reduction of banding in Landsat Thematic Mapper Images","interactions":[],"lastModifiedDate":"2017-05-09T13:43:57","indexId":"70187579","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3052,"text":"Photogrammetric Engineering and Remote Sensing","active":true,"publicationSubtype":{"id":10}},"title":"A technique for the reduction of banding in Landsat Thematic Mapper Images","docAbstract":"<p>The radiometric difference between forward and reverse scans in Landsat thematic mapper (TM) images, referred to as \"banding,\" can create problems when enhancing the image for interpretation or when performing quantitative studies. Recent research has led to the development of a method that reduces the banding in Landsat TM data sets. It involves passing a one-dimensional spatial kernel over the data set. This kernel is developed from the statistics of the banding pattern and is based on the Wiener filter. It has been implemented on both a DOS-based microcomputer and several UNIX-based computer systems. The algorithm has successfully reduced the banding in several test data sets.</p>","language":"English","publisher":"ASPRS","usgsCitation":"Helder, D.L., Quirk, B.K., and Hood, J.J., 1992, A technique for the reduction of banding in Landsat Thematic Mapper Images: Photogrammetric Engineering and Remote Sensing, v. 58, no. 10, p. 1425-1431.","productDescription":"7 p.","startPage":"1425","endPage":"1431","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":341008,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"58","issue":"10","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5912d53ee4b0e541a03d4557","contributors":{"authors":[{"text":"Helder, Dennis L.","contributorId":105613,"corporation":false,"usgs":true,"family":"Helder","given":"Dennis","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":694626,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Quirk, Bruce K. quirk@usgs.gov","contributorId":4285,"corporation":false,"usgs":true,"family":"Quirk","given":"Bruce","email":"quirk@usgs.gov","middleInitial":"K.","affiliations":[],"preferred":true,"id":694627,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hood, Joy J. jhood@usgs.gov","contributorId":5510,"corporation":false,"usgs":true,"family":"Hood","given":"Joy","email":"jhood@usgs.gov","middleInitial":"J.","affiliations":[],"preferred":true,"id":694628,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70185091,"text":"70185091 - 1992 - Structural evolution of an arc-basin: The Gravina Belt in central southeastern Alaska","interactions":[],"lastModifiedDate":"2023-11-09T14:47:12.178594","indexId":"70185091","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3524,"text":"Tectonics","active":true,"publicationSubtype":{"id":10}},"title":"Structural evolution of an arc-basin: The Gravina Belt in central southeastern Alaska","docAbstract":"<p><span>The upper Middle Jurassic-Lower Cretaceous Gravina belt lies along the eastern margin of the Alexander terrane in southeastern Alaska. This group of turbidites and mafic to intermediate volcanic rocks was deformed during mid to Late Cretaceous time during the closing of a basin of unknown size between the Alexander terrane on the west and the Stikine terrane to the east. Therefore structures of Gravina belt rocks largely reflect the final accretion and subsequent transport of the Alexander terrane. Six geologic transects across the central Gravina belt (southern Mitkof Island to northern Douglas Island) define a structural history that includes (1) syndepositional soft-sediment folding and faulting, possibly in conjunction with block tilting and extension; (2) tight to isoclinal folding or thrust faulting, with formation of a slaty cleavage (S</span><sub>1</sub><span>) striking ∼330°; (3) local coaxial refolding with formation of crenulation cleavage (S</span><sub>2</sub><span>); (4) development of domainal crenulation folds and cleavage (S</span><sub>3</sub><span>) oriented at a large angle to the margin of the belt; (5) intrusion of tonalitic plutons around 90 Ma; and (6) right-lateral strike-slip displacement on faults oriented ∼330°. Finite strain measurements on sedimentary rocks suggest the belt was at least twice its present width, normal to the foliation, before deformation. Subhorizontal margin-parallel fold axes, margin-parallel slaty cleavage, and margin-perpendicular stretching lineations suggest orthogonal contraction of the Gravina basin, assuming that oblique plate convergence was not decoupled along strike-slip faults. After contractional deformation, strike-slip faults indicate dextral displacement (probably of the order of several tens of kilometers) of the Alexander terrane with respect to the terranes to the east. Domainal crenulation folds and cleavages at a high angle to the margin of the belt suggest that the change in convergence directions occurred while the rocks (presently at the surface) could still plastically deform. This kinematic interpretation of structures is consistent with changes in plate motions [Engebretson et al., 1985]. Before 100 Ma, the convergence directions between the Kula and North America plates were at a high angle to the continental margin, whereas after 100 Ma, convergence directions were at a small angle to the continental margin. In addition, after 100 Ma, the Kula-North America, and not the Farallon-North America, convergence direction is most compatible with a N-S principal paleostress orientation derived from inversion of strike-slip fault data. This relationship suggests that it may have been the Kula plate that drove northward transport of the Alexander terrane along the margin of North America.</span></p>","language":"English","publisher":"Wiley","doi":"10.1029/92TC01107","usgsCitation":"Haeussler, P.J., 1992, Structural evolution of an arc-basin: The Gravina Belt in central southeastern Alaska: Tectonics, v. 11, no. 6, p. 1245-1265, https://doi.org/10.1029/92TC01107.","productDescription":"21 p.","startPage":"1245","endPage":"1265","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":337548,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Alexander terrane","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -135.92998305119977,\n              58.76028709475264\n            ],\n            [\n              -135.92998305119977,\n              56.61312544505941\n            ],\n            [\n              -133.71072320749985,\n              56.61312544505941\n            ],\n            [\n              -133.71072320749985,\n              58.76028709475264\n            ],\n            [\n              -135.92998305119977,\n              58.76028709475264\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"11","issue":"6","noUsgsAuthors":false,"publicationDate":"2010-07-26","publicationStatus":"PW","scienceBaseUri":"58c90130e4b0849ce97abd57","contributors":{"authors":[{"text":"Haeussler, Peter J. 0000-0002-1503-6247 pheuslr@usgs.gov","orcid":"https://orcid.org/0000-0002-1503-6247","contributorId":503,"corporation":false,"usgs":true,"family":"Haeussler","given":"Peter","email":"pheuslr@usgs.gov","middleInitial":"J.","affiliations":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":119,"text":"Alaska Science Center Geology Minerals","active":true,"usgs":true}],"preferred":true,"id":684323,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70180689,"text":"70180689 - 1992 - Prevalence of Renibacterium salmoninarum among downstream-migrating salmonids in the Columbia River","interactions":[],"lastModifiedDate":"2017-01-31T13:52:35","indexId":"70180689","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2177,"text":"Journal of Aquatic Animal Health","active":true,"publicationSubtype":{"id":10}},"title":"Prevalence of Renibacterium salmoninarum among downstream-migrating salmonids in the Columbia River","docAbstract":"<p><span>Bacterial kidney disease (BKD) is an important contributor to mortality of salmonids in hatcheries in the Columbia River basin. However, the impact of BKD on the survival of downstream migrants is difficult to determine because there is little information on the disease-related mortality among these fish. In this study, the impact of BKD on juvenile salmonids was examined by determining the percentage of downriver migrants infected with </span><i>Renibacterium salmoninarum</i><span> (the causative agent of BKD) and evaluating the effects of salt water on the progress of the disease. During the 2 years of this study, approximately 20% of the three species of migrating hatchery and wild salmonids (</span><i>Oncorhynchus</i><span> spp.) collected were infected with </span><i>R. salmoninarum</i><span>. Mortality caused by BKD increased when fish were held in salt water.</span></p>","language":"English","publisher":"Taylor & Francis","doi":"10.1577/1548-8667(1992)004<0072:PORSAD>2.3.CO;2","usgsCitation":"Sanders, J.E., Long, J., Arakawa, C., Bartholomew, J.L., and Rohovec, J., 1992, Prevalence of Renibacterium salmoninarum among downstream-migrating salmonids in the Columbia River: Journal of Aquatic Animal Health, v. 4, no. 1, p. 72-75, https://doi.org/10.1577/1548-8667(1992)004<0072:PORSAD>2.3.CO;2.","productDescription":"4 p. ","startPage":"72","endPage":"75","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":334480,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"4","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5891b0bce4b072a7ac129980","contributors":{"authors":[{"text":"Sanders, J. E.","contributorId":20007,"corporation":false,"usgs":true,"family":"Sanders","given":"J.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":662015,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Long, J.J","contributorId":179002,"corporation":false,"usgs":false,"family":"Long","given":"J.J","email":"","affiliations":[],"preferred":false,"id":662016,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Arakawa, C.K.","contributorId":152140,"corporation":false,"usgs":false,"family":"Arakawa","given":"C.K.","email":"","affiliations":[],"preferred":false,"id":662017,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bartholomew, J. L.","contributorId":91661,"corporation":false,"usgs":true,"family":"Bartholomew","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":662018,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Rohovec, J. S.","contributorId":95979,"corporation":false,"usgs":true,"family":"Rohovec","given":"J. S.","affiliations":[],"preferred":false,"id":662019,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70017026,"text":"70017026 - 1992 - Modernization and multiscale databases at the U.S. Geological Survey","interactions":[],"lastModifiedDate":"2023-09-21T16:19:07.974197","indexId":"70017026","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1317,"text":"Computers, Environment and Urban Systems","active":true,"publicationSubtype":{"id":10}},"title":"Modernization and multiscale databases at the U.S. Geological Survey","docAbstract":"<p><span>The U.S. Geological Survey (USGS) has begun a digital cartographic modernization program. Keys to that program are the creation of a multiscale database, a feature-based file structure that is derived from a spatial data model, and a series of “templates” or rules that specify the relationships between instances of entities in reality and features in the database. The database will initially hold data collected from the USGS standard map products at scales of 1:24,000, 1:100,000, and 1:2,000,000. The spatial data model is called the digital line graph-enhanced model, and the comprehensive rule set consists of collection rules, product generation rules, and conflict resolution rules. This modernization program will affect the USGS mapmaking process because both digital and graphic products will be created from the database. In addition, non-USGS map users will have more flexibility in uses of the databases. These remarks are those of the session discussant made in response to the six papers and the keynote address given in the session.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0198-9715(92)90012-G","usgsCitation":"Morrison, J.L., 1992, Modernization and multiscale databases at the U.S. Geological Survey: Computers, Environment and Urban Systems, v. 16, no. 4, p. 313-319, https://doi.org/10.1016/0198-9715(92)90012-G.","productDescription":"7 p.","startPage":"313","endPage":"319","numberOfPages":"7","costCenters":[],"links":[{"id":224864,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"16","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a5ca5e4b0c8380cd6fe55","contributors":{"authors":[{"text":"Morrison, J. L.","contributorId":28012,"corporation":false,"usgs":true,"family":"Morrison","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":375184,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1014567,"text":"1014567 - 1992 - Hormonal control of sulfate uptake by bronchial cartilage of coho salmon: Role of IGF-I","interactions":[],"lastModifiedDate":"2024-04-30T15:15:55.156093","indexId":"1014567","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2278,"text":"Journal of Experimental Zoology","active":true,"publicationSubtype":{"id":10}},"title":"Hormonal control of sulfate uptake by bronchial cartilage of coho salmon: Role of IGF-I","docAbstract":"<p><span>The direct hormonal control of sulfate uptake by cartilage matrix of coho salmon was examined by exposing branchial cartilage to 1 μCi · ml</span><sup>−1</sup><span>&nbsp;</span><sup>35</sup><span>SO</span><sub>4</sub><span>&nbsp;for 48 hours at 15°C in a defined medium. Sulfate uptake occurred primarily in cartilage (rather than bone) and the amount of specific uptake was similar in epibranchial and ceratobranchial cartilages. Intact and hypophysectomized coho salmon starved for 22 days had equivalent in vitro sulfate uptake, which in both cases were 30% of the uptake seen in branchial cartilage of fed, intact controls. In branchial cartilage from starved coho salmon, in vitro exposure to recombinant bovine insulin-like growth factor I (rbIGF-I) at 1, 10, 100, and 1,000 ng · ml</span><sup>−1</sup><span>&nbsp;caused a dose-dependent increase in sulfate uptake, with a maximum 3-fold increase over control at 1,000 ng · ml</span><sup>−1</sup><span>&nbsp;rbIGF-I. Coho salmon insulin (1, 10, 100, and 1,000 ng · ml</span><sup>−1</sup><span>) resulted in a maximum 30% increase in sulfate uptake at the highest dose. Growth hormone and triiodo-L-thyronine had no direct effect on in vitro sulfate uptake. The results indicate that IGF-I has direct effects on coho salmon cartilage and may be an important regulator of growth in salmon and other teleosts.</span></p>","language":"English","publisher":"Wiley","doi":"10.1002/jez.1402620206","usgsCitation":"McCormick, S., Tsai, P., Kelley, K., Nishioka, R.S., and Bern, H.A., 1992, Hormonal control of sulfate uptake by bronchial cartilage of coho salmon: Role of IGF-I: Journal of Experimental Zoology, v. 262, no. 2, p. 166-171, https://doi.org/10.1002/jez.1402620206.","productDescription":"6 p.","startPage":"166","endPage":"171","numberOfPages":"6","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":132322,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"262","issue":"2","noUsgsAuthors":false,"publicationDate":"2005-04-26","publicationStatus":"PW","scienceBaseUri":"4f4e4a54e4b07f02db62be3c","contributors":{"authors":[{"text":"McCormick, S. D. 0000-0003-0621-6200","orcid":"https://orcid.org/0000-0003-0621-6200","contributorId":20278,"corporation":false,"usgs":true,"family":"McCormick","given":"S. D.","affiliations":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"preferred":false,"id":320626,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tsai, P.I.","contributorId":100775,"corporation":false,"usgs":true,"family":"Tsai","given":"P.I.","email":"","affiliations":[],"preferred":false,"id":320630,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kelley, K.M.","contributorId":62952,"corporation":false,"usgs":true,"family":"Kelley","given":"K.M.","email":"","affiliations":[],"preferred":false,"id":320628,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Nishioka, R. S.","contributorId":69915,"corporation":false,"usgs":false,"family":"Nishioka","given":"R.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":320629,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Bern, H. A.","contributorId":61771,"corporation":false,"usgs":false,"family":"Bern","given":"H.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":320627,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":2000059,"text":"2000059 - 1992 - Surficial substrates and bathymetry of five historical lake trout spawning reefs in near-shore waters of the Great Lakes","interactions":[],"lastModifiedDate":"2012-02-02T00:14:57","indexId":"2000059","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":3,"text":"Organization Series"},"seriesTitle":{"id":222,"text":"Technical Report","active":false,"publicationSubtype":{"id":3}},"seriesNumber":"58","title":"Surficial substrates and bathymetry of five historical lake trout spawning reefs in near-shore waters of the Great Lakes","docAbstract":"The reestablishment of self-sustaining stocks of lake trout (Salvelinus namaycush) in the lower four Great Lakes has been substantially impeded because planted fish do not produce enough progeny that survive and reproduce.  The causes for this failure are unknown, but many historical spawning sites of lake trout have been degraded by human activities and can no longer produce viable swim-up fry.  In this study, we used side-scan sonar and an underwater video camera to survey, map, and evaluate the sustainability of one reef in each of the five Great Lakes for lake trout spawning and fry production.  At four of the reef sites, we found good-to-excellent substrate for spawning and fry production by the shallow-water strains of lake trout that are now being planted.  These substrates were in water 6-22 m deep and were composed largely of rounded or angular rubble and cobble.  Interstitial spaces in these substrates were 20 cm or deeper and would protect naturally spawned eggs and fry from predators, ice scour, and buffeting by waves and currents.  Subsequent studies of egg survival by other researchers confirmed our evaluation that the best substrates at two of these sites still have the potential to produce viable swim-up fry.","language":"English","publisher":"Great Lakes Fishery Commission","collaboration":"Out-of-print","usgsCitation":"Edsall, T.A., Brown, C.L., Kennedy, G.W., and French, J.R., 1992, Surficial substrates and bathymetry of five historical lake trout spawning reefs in near-shore waters of the Great Lakes: Technical Report 58, 53 p.","productDescription":"53 p.","startPage":"0","endPage":"53","numberOfPages":"53","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":92045,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://www.glfc.org/pubs/TechReports/Tr58.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":198862,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae1e4b07f02db68884b","contributors":{"authors":[{"text":"Edsall, Thomas A.","contributorId":84302,"corporation":false,"usgs":true,"family":"Edsall","given":"Thomas","email":"","middleInitial":"A.","affiliations":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"preferred":false,"id":325018,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brown, Charles L.","contributorId":102421,"corporation":false,"usgs":true,"family":"Brown","given":"Charles","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":325019,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kennedy, Gregory W. 0000-0003-1686-6960 gkennedy@usgs.gov","orcid":"https://orcid.org/0000-0003-1686-6960","contributorId":3700,"corporation":false,"usgs":true,"family":"Kennedy","given":"Gregory","email":"gkennedy@usgs.gov","middleInitial":"W.","affiliations":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"preferred":true,"id":325017,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"French, John R. P. III","contributorId":107635,"corporation":false,"usgs":true,"family":"French","given":"John","suffix":"III","email":"","middleInitial":"R. P.","affiliations":[],"preferred":false,"id":325020,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70194970,"text":"70194970 - 1992 - Resistance of young wolf pups to inclement weather","interactions":[],"lastModifiedDate":"2018-01-31T17:01:54","indexId":"70194970","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":70,"text":"Research Information Bulletin","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"93","title":"Resistance of young wolf pups to inclement weather","docAbstract":"<p>Based on information about young dog (<span id=\"_mce_caret\" data-mce-bogus=\"true\"><i>Canis familiaris</i><span id=\"_mce_caret\" data-mce-bogus=\"true\">) pups, it was thought that wolf (<span id=\"_mce_caret\" data-mce-bogus=\"true\"><i>Canis lupus</i><span id=\"_mce_caret\" data-mce-bogus=\"true\">) pups 0-2 weeks of age do not thermoregulate well. This problem, plus the relative immobility of young pups, was thought to explain why pups generally remain inside dens until about 3 weeks of age, and pups younger than 3-weeks-old were thought to be highly vulnerable to loss from exposure. this report details more information about the tolerance of young wolf pups to exposure.</span></span></span></span></p>","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Mech, L.D., 1992, Resistance of young wolf pups to inclement weather: Research Information Bulletin 93, 2 p.","productDescription":"2 p.","costCenters":[],"links":[{"id":350866,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5a72e3ebe4b0a9a2e9e08efd","contributors":{"authors":[{"text":"Mech, L. David 0000-0003-3944-7769 david_mech@usgs.gov","orcid":"https://orcid.org/0000-0003-3944-7769","contributorId":2518,"corporation":false,"usgs":true,"family":"Mech","given":"L.","email":"david_mech@usgs.gov","middleInitial":"David","affiliations":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"preferred":true,"id":726311,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70187932,"text":"70187932 - 1992 - Histopathologic biomarkers","interactions":[],"lastModifiedDate":"2017-05-24T15:33:42","indexId":"70187932","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Histopathologic biomarkers","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Biomarkers; biochemical, physiological, and histological markers of anthropogenic stress","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Lewis Publishers","publisherLocation":"Boca Raton, FL","usgsCitation":"Hinton, D., Baumann, P.C., Gardner, G.R., Hawkins, W.E., Hendricks, J.D., Murchelano, R.A., and Okihiro, M., 1992, Histopathologic biomarkers, chap. <i>of</i> Biomarkers; biochemical, physiological, and histological markers of anthropogenic stress, p. 155-209.","productDescription":"55 p.","startPage":"155","endPage":"209","costCenters":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"links":[{"id":341701,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"59269bd2e4b0b7ff9fb489da","contributors":{"editors":[{"text":"Huggett, R.J.","contributorId":113557,"corporation":false,"usgs":true,"family":"Huggett","given":"R.J.","email":"","affiliations":[],"preferred":false,"id":696040,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Kimerle, R. A.","contributorId":111538,"corporation":false,"usgs":false,"family":"Kimerle","given":"R. A.","affiliations":[],"preferred":false,"id":696041,"contributorType":{"id":2,"text":"Editors"},"rank":2},{"text":"Mehrle, P. M.","contributorId":91767,"corporation":false,"usgs":true,"family":"Mehrle","given":"P. M.","affiliations":[],"preferred":false,"id":696042,"contributorType":{"id":2,"text":"Editors"},"rank":3},{"text":"Bergman, H.L.","contributorId":73553,"corporation":false,"usgs":true,"family":"Bergman","given":"H.L.","email":"","affiliations":[],"preferred":false,"id":696043,"contributorType":{"id":2,"text":"Editors"},"rank":4}],"authors":[{"text":"Hinton, D.E.","contributorId":75489,"corporation":false,"usgs":true,"family":"Hinton","given":"D.E.","email":"","affiliations":[],"preferred":false,"id":696033,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Baumann, P. C.","contributorId":43297,"corporation":false,"usgs":false,"family":"Baumann","given":"P.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":696034,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gardner, G. R.","contributorId":192266,"corporation":false,"usgs":false,"family":"Gardner","given":"G.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":696035,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hawkins, W. E.","contributorId":192267,"corporation":false,"usgs":false,"family":"Hawkins","given":"W.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":696036,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Hendricks, J. D.","contributorId":40187,"corporation":false,"usgs":true,"family":"Hendricks","given":"J.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":696037,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Murchelano, R. A.","contributorId":192268,"corporation":false,"usgs":false,"family":"Murchelano","given":"R.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":696038,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Okihiro, M.S.","contributorId":28551,"corporation":false,"usgs":true,"family":"Okihiro","given":"M.S.","email":"","affiliations":[],"preferred":false,"id":696039,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":2000063,"text":"2000063 - 1992 - Selection of prey by walleyes in the Ohio waters of the central basin of Lake Erie, 1985-1987","interactions":[],"lastModifiedDate":"2016-11-16T16:04:30","indexId":"2000063","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":79,"text":"Resource Publication","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"182","title":"Selection of prey by walleyes in the Ohio waters of the central basin of Lake Erie, 1985-1987","docAbstract":"Walleyes (Stizostedion vitreum vitreum) were collected at five locations in the central basin of Lake Erie in 1985-87.  The contents of the fishes' stomachs were examined to identify the species of prey. The seasonal availability of potential prey was determined from sampling with trawl tows.  Food electivity indexes for young-of-the-year (YOY) and older walleyes were calculated. Electivity indexes changed monthly in YOY walleyes that consumed mostly YOY gizzard shads (Dorosoma cepedianum) in July and fed moderately on gizzard shads, but more on smelts (Osmerus mordax), in August.  In September and October YOY walleyes did not consume YOY white perch (Morone americana).  During October, they continued to eat YOY gizzard shads moderately but consumed mostly emerald shiners (Notropis atherinoides).  Older walleys were highly partial to YOY gizzard shads, emerald shiners, and smelts and consumed no YOY white perch.  The numbers of YOY yellow perch (Perca flavescens) in stomachs were limited.  Prey selection by walleyes in the central basin was species-specific irrespective of abundance of prey.","language":"English","publisher":"U.S. Fish and Wildlife Service","publisherLocation":"Washington, D.C.","usgsCitation":"Wolfert, D.R., and Bur, M.T., 1992, Selection of prey by walleyes in the Ohio waters of the central basin of Lake Erie, 1985-1987: Resource Publication 182, 14 p.","productDescription":"14 p.","numberOfPages":"14","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":198637,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4c20","contributors":{"authors":[{"text":"Wolfert, David R.","contributorId":49305,"corporation":false,"usgs":true,"family":"Wolfert","given":"David","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":325029,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bur, Michael T.","contributorId":102015,"corporation":false,"usgs":true,"family":"Bur","given":"Michael","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":325030,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70017148,"text":"70017148 - 1992 - Discordant 14C ages from buried tidal-marsh soils in the Cascadia subduction zone, southern Oregon coast","interactions":[],"lastModifiedDate":"2013-01-25T14:00:01","indexId":"70017148","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","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":"Discordant 14C ages from buried tidal-marsh soils in the Cascadia subduction zone, southern Oregon coast","docAbstract":"Peaty, tidal-marsh soils interbedded with estuarine mud in late Holocene stratigraphic sequences near Coos Bay, Oregon, may have been submerged and buried during great (M > 8) subduction earthquakes, smaller localized earthquakes, or by nontectonic processes. Radiocarbon dating might help distinguish among these alternatives by showing that soils at different sites were submerged at different times along this part of the Cascadia subduction zone. But comparison of conventional 14C ages for different materials from the same buried soils shows that they contain materials that differ in age by many hundreds of years. Errors in calibrated soil ages represent about the same length of time as recurrence times for submergence events (150-500 yr)-this similarity precludes using conventional 14C ages to distinguish buried soils along the southern Oregon coast. Accelerator mass spectrometer 14C ages of carefully selected macrofossils from the tops of peaty soils should provide more precise estimates of the times of submergence events. ?? 1992.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Quaternary Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","publisherLocation":"Amsterdam, Netherlands","doi":"10.1016/0033-5894(92)90031-D","issn":"00335894","usgsCitation":"Nelson, A., 1992, Discordant 14C ages from buried tidal-marsh soils in the Cascadia subduction zone, southern Oregon coast: Quaternary Research, v. 38, no. 1, p. 74-90, https://doi.org/10.1016/0033-5894(92)90031-D.","startPage":"74","endPage":"90","numberOfPages":"17","costCenters":[],"links":[{"id":266482,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0033-5894(92)90031-D"},{"id":224778,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"38","issue":"1","noUsgsAuthors":false,"publicationDate":"2017-01-20","publicationStatus":"PW","scienceBaseUri":"505a01ece4b0c8380cd4fdbd","contributors":{"authors":[{"text":"Nelson, A.R. 0000-0001-7117-7098","orcid":"https://orcid.org/0000-0001-7117-7098","contributorId":55078,"corporation":false,"usgs":true,"family":"Nelson","given":"A.R.","affiliations":[],"preferred":false,"id":375558,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70187311,"text":"70187311 - 1992 - Depositional history, nannofossil biostratigraphy, and correlation of Argo Abyssal Plain Sites 765 and 261","interactions":[],"lastModifiedDate":"2018-05-07T21:15:38","indexId":"70187311","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":3,"text":"Organization Series"},"seriesTitle":{"id":5640,"text":"Proceedings of the Ocean Drilling Program: Scientific Results","onlineIssn":"1096-7451","printIssn":"0884-5891","active":true,"publicationSubtype":{"id":3}},"seriesNumber":"123","chapter":"1","title":"Depositional history, nannofossil biostratigraphy, and correlation of Argo Abyssal Plain Sites 765 and 261","docAbstract":"<p>Sediments from the Argo Abyssal Plain (AAP), northwest of Australia, are the oldest known from the Indian Ocean and were recovered from ODP Site 765 and DSDP Site 261. New biostratigraphic and sedimentologic data from these sites, as well as reinterpretations of earlier findings, indicate that basal sediments at both localities are of Late Jurassic age and delineate a history of starved sedimentation punctuated by periodic influx of calcareous pelagic turbidites.</p><p>Biostratigraphy and correlation of Upper Jurassic-Lower Cretaceous sediments is based largely on calcareous nannofossils. Both sites yielded variably preserved nannofossil successions ranging from Tithonian to Hauterivian at Site 765 and Kimmeridgian to Hauterivian at Site 261. The nannofloras are comparable to those present in the European and Atlantic Boreal and Tethyan areas, but display important differences that reflect biogeographic differentiation. The Argo region is thought to have occupied a position at the southern limit of the Tethyan nannofloral realm, thus yielding both Tethyan and Austral biogeographic features.</p><p>Sedimentary successions at the two sites are grossly similar, and differences largely reflect Site 765 's greater proximity to the continental margin. Jurassic sediments were deposited at rates of about 2 m/m.y. near the carbonate compensation depth (CCD) and contain winnowed concentrations of inoceramid prisms and nannofossils, redeposited layers rich in calcispheres and calcisphere debris, manganese nodules, and volcanic detritus. Lower Cretaceous and all younger sediments accumulated below the CCD at rates that were highest (about 20 m/m.y.) during mid-Cretaceous and Neogene time. Background sediment in this interval is noncalcareous claystone; turbidites dominate the sequence and are thicker and coarser grained at Site 765.</p><p>AAP turbidites consist mostly of calcareous and siliceous biogenic components and volcanogenic smectite clay; they were derived from relatively deep parts of the continental margin that lay below the photic zone, but above the CCD. The Jurassic-Lower Cretaceous section is about the same thickness across the AAP; turbidites in this interval appear to have had multiple sources along the Australian margin. The Upper Cretaceous-Cenozoic section, however, is three times thicker at Site 765 than at Site 261; turbidites in this interval were derived predominantly from the south.</p><p>Patterns of sedimentation across the AAP have been influenced by shifts in sea level, the CCD, and configuration of the continental margin. Major pulses of calcareous turbidite deposition occurred during Valanginian, Aptian, and Neogene time—all periods of eustatic lowstands and depressed CCD levels. Sediment redeposited on the AAP has come largely from the Australian outer shelf, continental slope, or rise, rather than the continent itself. Most terrigenous detritus was trapped in epicontinental basins that have flanked northwestern Australia since the early Mesozoic.</p>","language":"English","publisher":"Ocean Drilling Program, Texas A&M University","publisherLocation":"College Station, TX","doi":"10.2973/odp.proc.sr.123.156.1992","usgsCitation":"Dumoulin, J.A., and Bown, P.R., 1992, Depositional history, nannofossil biostratigraphy, and correlation of Argo Abyssal Plain Sites 765 and 261: Proceedings of the Ocean Drilling Program: Scientific Results 123, v. 123, 54 p., https://doi.org/10.2973/odp.proc.sr.123.156.1992.","productDescription":"54 p.","startPage":"3","endPage":"56","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":488638,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"http://doi.org/10.2973/odp.proc.sr.123.156.1992","text":"Publisher Index Page"},{"id":340547,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Argo Abyssal Plain","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              123,\n              -21\n            ],\n            [\n              112,\n              -21\n            ],\n            [\n              112,\n              -10\n            ],\n            [\n              123,\n              -10\n            ],\n            [\n              123,\n              -21\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"123","publicComments":"Volume topic: <i>Argo Abyssal Plain/Exmouth Plateau, covering Leg 123 of the cruises of the Drilling Vessel JOIDES Resolution, Singapore, Republic of Sing., to Singapore, Republic of Sing., Sites 765-766, 28 August 1988 - 1 November 1988</i>","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"59030339e4b0e862d230f7fc","contributors":{"editors":[{"text":"Stewart, Sondra K.","contributorId":117324,"corporation":false,"usgs":false,"family":"Stewart","given":"Sondra","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":730052,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Kennett, Diana","contributorId":27521,"corporation":false,"usgs":false,"family":"Kennett","given":"Diana","email":"","affiliations":[],"preferred":false,"id":730053,"contributorType":{"id":2,"text":"Editors"},"rank":2},{"text":"Mazzullo, Elsa K.","contributorId":60618,"corporation":false,"usgs":false,"family":"Mazzullo","given":"Elsa","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":730054,"contributorType":{"id":2,"text":"Editors"},"rank":3}],"authors":[{"text":"Dumoulin, Julie A. 0000-0003-1754-1287 dumoulin@usgs.gov","orcid":"https://orcid.org/0000-0003-1754-1287","contributorId":203209,"corporation":false,"usgs":true,"family":"Dumoulin","given":"Julie","email":"dumoulin@usgs.gov","middleInitial":"A.","affiliations":[{"id":119,"text":"Alaska Science Center Geology Minerals","active":true,"usgs":true},{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"preferred":true,"id":693301,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bown, Paul R.","contributorId":15408,"corporation":false,"usgs":false,"family":"Bown","given":"Paul","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":693302,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70187681,"text":"70187681 - 1992 - Data integration through region-based nominal filtering","interactions":[],"lastModifiedDate":"2017-05-12T14:04:36","indexId":"70187681","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2047,"text":"International Journal of Geographical Information Systems","active":true,"publicationSubtype":{"id":10}},"title":"Data integration through region-based nominal filtering","docAbstract":"<p><span>Resource models integrating disparate nominal or class grid-cell data can be implemented by using spatial filters. Most modelling procedures do not adequately handle noise created during the process of merging and integrating multiple grid-cell data sets. Data integration can be best accomplished in an environment where ready access to statistical and database management systems support the reclassification of noise grid-cells. These systems provide access to functionality and information which support the design of the spatial filter and the evaluation of the result of the spatial filter and the resource model.</span></p>","language":"English","publisher":"Taylor & Francis","doi":"10.1080/02693799208901929","usgsCitation":"Fosnight, E.A., 1992, Data integration through region-based nominal filtering: International Journal of Geographical Information Systems, v. 6, no. 6, p. 469-478, https://doi.org/10.1080/02693799208901929.","productDescription":"10 p.","startPage":"469","endPage":"478","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":341236,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"6","issue":"6","noUsgsAuthors":false,"publicationDate":"2007-02-05","publicationStatus":"PW","scienceBaseUri":"5916c9bfe4b044b359e486d6","contributors":{"authors":[{"text":"Fosnight, Eugene A. 0000-0002-8557-3697 fosnight@usgs.gov","orcid":"https://orcid.org/0000-0002-8557-3697","contributorId":2961,"corporation":false,"usgs":true,"family":"Fosnight","given":"Eugene","email":"fosnight@usgs.gov","middleInitial":"A.","affiliations":[{"id":223,"text":"Earth Resources Observation and Science (EROS) Center (Geography)","active":false,"usgs":true}],"preferred":true,"id":695057,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70185793,"text":"70185793 - 1992 - Nitrate is a preferred electron acceptor for growth of freshwater selenate-respiring bacteria","interactions":[],"lastModifiedDate":"2023-01-20T16:43:50.037905","indexId":"70185793","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","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":"Nitrate is a preferred electron acceptor for growth of freshwater selenate-respiring bacteria","docAbstract":"<p><span>An anaerobic, freshwater enrichment grew with either nitrate or selenate as an electron acceptor. With both ions present, nitrate reduction preceded selenate reduction. An isolate from the enrichment grew on either ion, but the presence of nitrate precluded the reduction of selenate. Stock cultures of denitrifiers grew anaerobically on nitrate but not on selenate.</span></p>","language":"English","publisher":"American Society for Microbiology","doi":"10.1128/aem.58.1.426-428.1992","usgsCitation":"Steinberg, N.A., Blum, J.S., Hochstein, L., and Oremland, R.S., 1992, Nitrate is a preferred electron acceptor for growth of freshwater selenate-respiring bacteria: Applied and Environmental Microbiology, v. 58, no. 1, p. 426-428, https://doi.org/10.1128/aem.58.1.426-428.1992.","productDescription":"3 p.","startPage":"426","endPage":"428","costCenters":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":479648,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1128/aem.58.1.426-428.1992","text":"Publisher Index Page"},{"id":338544,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"58","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58dcc81ee4b02ff32c685722","contributors":{"authors":[{"text":"Steinberg, Nisan A.","contributorId":189726,"corporation":false,"usgs":false,"family":"Steinberg","given":"Nisan","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":686753,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Blum, Jodi Switzer","contributorId":96946,"corporation":false,"usgs":true,"family":"Blum","given":"Jodi","email":"","middleInitial":"Switzer","affiliations":[],"preferred":false,"id":686754,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hochstein, Lawrence","contributorId":190004,"corporation":false,"usgs":false,"family":"Hochstein","given":"Lawrence","email":"","affiliations":[],"preferred":false,"id":686755,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Oremland, Ronald S. 0000-0001-7382-0147 roremlan@usgs.gov","orcid":"https://orcid.org/0000-0001-7382-0147","contributorId":931,"corporation":false,"usgs":true,"family":"Oremland","given":"Ronald","email":"roremlan@usgs.gov","middleInitial":"S.","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":true,"id":686756,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":30083,"text":"wri914130 - 1992 - Techniques for estimating 7-day, 10-year low-flow characteristics for ungaged sites on streams in Mississippi","interactions":[],"lastModifiedDate":"2023-04-04T21:49:38.53325","indexId":"wri914130","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"91-4130","title":"Techniques for estimating 7-day, 10-year low-flow characteristics for ungaged sites on streams in Mississippi","docAbstract":"<p>Mississippi State water laws require that the 7-day, 10-year low-flow characteristic (7Q10) of streams be used as a criterion for issuing wastedischarge permits to dischargers to streams and for limiting withdrawals of water from streams. This report presents techniques for estimating the 7Q10 for ungaged sites on streams in Mississippi based on the availability of baseflow discharge measurements at the site, location of nearby gaged sites on the same stream, and drainage area of the ungaged site. These techniques may be used to estimate the 7Q10 at sites on natural, unregulated or partially regulated, and non-tidal streams. Low-flow characteristics for streams in the Mississippi River alluvial plain were not estimated because the annual lowflow data exhibit decreasing trends with time. Also presented are estimates of the 7Q10 for 493 gaged sites on Mississippi streams.</p><p>Techniques for estimating the 7Q10 have been developed for ungaged sites with base-flow discharge measurements, for ungaged sites on gaged streams, and for ungaged sites on ungaged streams. For an ungaged site with one or more base-flow discharge measurements, base-flow discharge data at the ungaged site are related to concurrent discharge data at a nearby gaged site. For ungaged sites on gaged streams, several methods of transferring the 7Q10 from a gaged site to an ungaged site were developed; the resulting 7Q10 values are based on drainage area prorations for the sites. For ungaged sites on ungaged streams, the 7Q10 is estimated from a map developed for. this study that shows the unit 7Q10 (7Q10 per square mile of drainage area) for ungaged basins in the State. The mapped values were estimated from the unit 7Q10 determined for nearby gaged basins, adjusted on the basis of the geology and topography of the ungaged basins.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri914130","collaboration":"Prepared in cooperation with the Pat Harrison Waterway District, Pearl River Basin Development District, Tombigbee River Valley Water Management District, Mississippi Department of Environmental Quality, Mississippi Office of Land and Water Resources, Mississippi Office of Pollution Control","usgsCitation":"Telis, P.A., 1992, Techniques for estimating 7-day, 10-year low-flow characteristics for ungaged sites on streams in Mississippi: U.S. Geological Survey Water-Resources Investigations Report 91-4130, Report: iv, 143 p.; Plate: 35.61 x 48.12 inches, https://doi.org/10.3133/wri914130.","productDescription":"Report: iv, 143 p.; Plate: 35.61 x 48.12 inches","costCenters":[{"id":269,"text":"FLWSC-Ft. Lauderdale","active":true,"usgs":true}],"links":[{"id":415198,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_47531.htm","linkFileType":{"id":5,"text":"html"}},{"id":58894,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1991/4130/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":160689,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1991/4130/report-thumb.jpg"},{"id":347202,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1991/4130/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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 \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adce4b07f02db6861d2","contributors":{"authors":[{"text":"Telis, Pamela A. patelis@usgs.gov","contributorId":1461,"corporation":false,"usgs":true,"family":"Telis","given":"Pamela","email":"patelis@usgs.gov","middleInitial":"A.","affiliations":[{"id":269,"text":"FLWSC-Ft. 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,{"id":70196055,"text":"70196055 - 1992 - Barrier island erosion accelerating","interactions":[],"lastModifiedDate":"2018-03-15T11:42:38","indexId":"70196055","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5654,"text":" Coastwise, Publication of the Coalition to Restore Coastal Louisiana","active":true,"publicationSubtype":{"id":10}},"title":"Barrier island erosion accelerating","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Coalition to Restore Coastal Louisiana","usgsCitation":"McBride, R., Groat, C., Penland, P., Williams, S., and Sallenger, A.H., 1992, Barrier island erosion accelerating:  Coastwise, Publication of the Coalition to Restore Coastal Louisiana, v. 3, no. 4, p. 1, 4-6.","productDescription":"4 p.","startPage":"1, 4","endPage":"6","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":352552,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Louisiana","volume":"3","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5aff2826e4b0da30c1bfd770","contributors":{"authors":[{"text":"McBride, R.A.","contributorId":13257,"corporation":false,"usgs":true,"family":"McBride","given":"R.A.","email":"","affiliations":[],"preferred":false,"id":731157,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Groat, C.G.","contributorId":51512,"corporation":false,"usgs":true,"family":"Groat","given":"C.G.","email":"","affiliations":[],"preferred":false,"id":731158,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Penland, P.S.","contributorId":21897,"corporation":false,"usgs":false,"family":"Penland","given":"P.S.","email":"","affiliations":[],"preferred":false,"id":731159,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Williams, S.J.","contributorId":85203,"corporation":false,"usgs":true,"family":"Williams","given":"S.J.","email":"","affiliations":[],"preferred":false,"id":731160,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Sallenger, A. H. Jr.","contributorId":8818,"corporation":false,"usgs":true,"family":"Sallenger","given":"A.","suffix":"Jr.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":731161,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":1000764,"text":"1000764 - 1992 - A mass spectroscopic method for analysis of AHH-inducing and other polychlorinated biphenyl congeners and selected pesticides in fish","interactions":[],"lastModifiedDate":"2013-01-28T12:44:01","indexId":"1000764","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","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":"A mass spectroscopic method for analysis of AHH-inducing and other polychlorinated biphenyl congeners and selected pesticides in fish","docAbstract":"The 209 polychlorinated biphenyl (PCB) congeners exhibit a wide range in toxicity to fish, birds, and mammals. This paper discusses the use of gas chromatography/mass spectrometry negative chemical ionization (GC/MS-NCI) to quantify congeners of highly suspected toxicity such as IUPAC #77 (3,3',4,4'-tetrachlorobiphenyl) and #126 (3,3',4,4',5-pentachlorobiphenyl). GC/MS analysis time needed to produce the necessary resolution was reduced to 1 h per sample or standard, allowing an autosampler to inject 12 samples in 24 hours, plus 12 standards/QC samples. Identification and quantification of some 60+ congeners and several selected pesticides and estimation of total PCBs are also possible within the 1 h analysis. For congeners of high chlorination (penta through octa), the method exhibited excellent sensitivity, such that we could not locate a fish which exhibited PCB levels below our calibrated quantitation range. NCI was not as sensitive for mono through tri and for some tetrachlorinated PCB congeners, an exception being PCB #77, for which sensitivity was of the same order as for the more highly chlorinated biphenyls. Long term stability was excellent. Over a 6-mo period, results of replicate analyses for PCB congeners and pesticides in a composited sample of lake trout (<i>Salvelinus namaycush</i>) from Lake Michigan had a relative standard deviation of 12% of the mean. Over the same time period, mean recoveries for samples spiked at concentrations similar to those in Lake Michigan lake trout were 90-102%. Response was linear over a wide range of concentrations for each of the analyzed compounds. This method is now being used for routine analysis of PCB congeners and selected pesticides in our laboratory.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Archives of Environmental Contamination and Toxicology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Springer","publisherLocation":"Amsterdam, Netherlands","doi":"10.1007/BF00225993","usgsCitation":"Schmidt, L., and Hesselberg, R.J., 1992, A mass spectroscopic method for analysis of AHH-inducing and other polychlorinated biphenyl congeners and selected pesticides in fish: Archives of Environmental Contamination and Toxicology, v. 23, no. 1, p. 37-44, https://doi.org/10.1007/BF00225993.","productDescription":"p. 37-44","startPage":"37","endPage":"44","numberOfPages":"7","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":133643,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":266610,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF00225993"}],"volume":"23","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae143","contributors":{"authors":[{"text":"Schmidt, Larry J.","contributorId":51238,"corporation":false,"usgs":true,"family":"Schmidt","given":"Larry J.","affiliations":[],"preferred":false,"id":309372,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hesselberg, Robert J.","contributorId":36074,"corporation":false,"usgs":true,"family":"Hesselberg","given":"Robert","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":309371,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1000745,"text":"1000745 - 1992 - Diets of emerald and spottail shiners and potential interactions with other western Lake Erie planktivorous fishes","interactions":[],"lastModifiedDate":"2016-04-25T08:59:01","indexId":"1000745","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2330,"text":"Journal of Great Lakes Research","active":true,"publicationSubtype":{"id":10}},"title":"Diets of emerald and spottail shiners and potential interactions with other western Lake Erie planktivorous fishes","docAbstract":"<p><span>Emerald shiner (</span><i>Notropis atherinoides</i><span>) and spottail shiner (</span><i>N. hudsonius</i><span>) were abundant historically in western Lake Erie. Recent changes in the fish community suggest that shiners may not compete favorably with the invading white perch (</span><i>Morone americana</i><span>) or the gizzard shad (</span><i>Dorosoma cepedianum</i><span>). We examined the diets of emerald and spottail shiner and compared them to other planktivores in western Lake Erie. Emerald and spottail shiner ate cladocerans such as&nbsp;</span><i>Daphnia</i><span>&nbsp;spp.,</span><i>Leptodora</i><span>, and&nbsp;</span><i>Bythotrephes</i><span>. Biologically significant overlaps (Schoener 1970 index &ge; 0.6) among zooplanktivores occurred from July through September, but most occurred during July. The frequency of significant diet overlaps among planktivores declined since an earlier study in the mid-1970s (Muth and Busch 1989) possibly indicating that competitive interactions have eased since 1975. In addition to competitive interactions, other factors such as increased eutrophication and predator mediated mortality likely played a role in planktivore community changes since the early 1970s.</span></p>","language":"English","publisher":"Taylor & Francis","doi":"10.1016/S0380-1330(92)71273-8","usgsCitation":"Hartman, K.J., Vondracek, B., Parrish, D., and Muth, K.M., 1992, Diets of emerald and spottail shiners and potential interactions with other western Lake Erie planktivorous fishes: Journal of Great Lakes Research, v. 18, no. 1, p. 43-50, https://doi.org/10.1016/S0380-1330(92)71273-8.","productDescription":"8 p.","startPage":"43","endPage":"50","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":133200,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"18","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d7bf","contributors":{"authors":[{"text":"Hartman, Kyle J.","contributorId":6414,"corporation":false,"usgs":false,"family":"Hartman","given":"Kyle","email":"","middleInitial":"J.","affiliations":[{"id":16210,"text":"Division of Forestry and Natural Resources, West Virginia University","active":true,"usgs":false}],"preferred":false,"id":309306,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Vondracek, Bruce","contributorId":30587,"corporation":false,"usgs":true,"family":"Vondracek","given":"Bruce","affiliations":[],"preferred":false,"id":309307,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Parrish, Donna L. dparrish@usgs.gov","contributorId":3559,"corporation":false,"usgs":true,"family":"Parrish","given":"Donna L.","email":"dparrish@usgs.gov","affiliations":[{"id":611,"text":"Vermont Cooperative Fish and Wildlife Research Unit","active":false,"usgs":true}],"preferred":false,"id":309305,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Muth, Kenneth M.","contributorId":44863,"corporation":false,"usgs":true,"family":"Muth","given":"Kenneth","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":309308,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70186218,"text":"70186218 - 1992 - Structural framework of the Chile margin at the Chile ridge collision zone","interactions":[],"lastModifiedDate":"2017-03-31T15:50:43","indexId":"70186218","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Structural framework of the Chile margin at the Chile ridge collision zone","docAbstract":"<p>No abstract available</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Proceedings of the ocean drilling program, Part A: Initial reports","largerWorkSubtype":{"id":12,"text":"Conference publication"},"language":"English","usgsCitation":"Bangs, N., Cande, S., Lewis, S., and Miller, J., 1992, Structural framework of the Chile margin at the Chile ridge collision zone, <i>in</i> Proceedings of the ocean drilling program, Part A: Initial reports, p. 11-21.","productDescription":"12 p.","startPage":"11","endPage":"21","costCenters":[],"links":[{"id":338985,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58df6acae4b02ff32c6aea9d","contributors":{"authors":[{"text":"Bangs, N.L.","contributorId":17385,"corporation":false,"usgs":true,"family":"Bangs","given":"N.L.","email":"","affiliations":[],"preferred":false,"id":687909,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cande, S.C.","contributorId":190243,"corporation":false,"usgs":false,"family":"Cande","given":"S.C.","email":"","affiliations":[],"preferred":false,"id":687910,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lewis, S.D.","contributorId":11618,"corporation":false,"usgs":true,"family":"Lewis","given":"S.D.","email":"","affiliations":[],"preferred":false,"id":687911,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Miller, John","contributorId":190242,"corporation":false,"usgs":false,"family":"Miller","given":"John","email":"","affiliations":[],"preferred":false,"id":687912,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
]}