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Recovery rates in this study varied greatly among species, but did not vary among station types (cove or shoreline) or sample years (1976 or 1977). Tagged fishes, used to establish recovery rates, did not change in weight due to the sampling procedures from time of introduction to time of collection. Total adjusted abundance estimates ranged from 157 to 18,300 fishes/hectare and from 36 to 4,080 kg/hectare for fishes greater than 124 mm in Texas estuaries. Mean number and weight of fishes per hectare were generally greater at cove stations than at shoreline stations. Timing for the application of rote‐none in estuaries is important to avoid extensive bird predation.</span></p>","language":"English","publisher":"American Fisheries Society","doi":"10.1577/1548-8659(1982)111<326:SNEFWR>2.0.CO;2","usgsCitation":"Matlock, G., Weaver, J., and Green, A., 1982, Sampling nearshore estuarine fishes with rotenone: Transactions of the American Fisheries Society, v. 111, no. 3, p. 326-331, https://doi.org/10.1577/1548-8659(1982)111<326:SNEFWR>2.0.CO;2.","productDescription":"6 p.","startPage":"326","endPage":"331","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":129414,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Texas","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -103.01686386982905,\n              36.54934470361806\n            ],\n            [\n              -103.16447562172418,\n              32.150318163627794\n            ],\n            [\n              -106.46644145089786,\n              31.987381620989126\n            ],\n            [\n              -106.5461615425177,\n              31.661940230648177\n            ],\n            [\n              -105.00356801771821,\n              30.454952016172175\n            ],\n            [\n              -104.80013205947722,\n              29.619951638485226\n            ],\n            [\n              -103.31293428443124,\n              28.828882427211\n            ],\n            [\n              -102.65099139863595,\n              29.181308520996676\n            ],\n            [\n              -102.48376502365687,\n              29.599147009542\n            ],\n            [\n              -101.54604678171064,\n              29.586378221131856\n            ],\n            [\n              -100.85537631214015,\n              28.6669367123218\n            ],\n            [\n              -100.21186048135847,\n              27.654119650851904\n            ],\n            [\n              -99.90814398825981,\n              26.85165787533441\n            ],\n            [\n              -98.92713783016438,\n              25.803398989119685\n            ],\n            [\n              -97.08381437026614,\n              25.96647385913593\n            ],\n            [\n              -96.58487103798741,\n              27.900739581434543\n            ],\n            [\n              -93.67735996380688,\n              29.690109364070164\n            ],\n            [\n              -93.46829303313868,\n              31.08327617457777\n            ],\n            [\n              -94.16894804359433,\n              33.48940905403634\n            ],\n            [\n              -99.95888844975084,\n              34.59784326548461\n            ],\n            [\n              -100.08126145602463,\n              36.54131724278918\n            ],\n            [\n              -103.01686386982905,\n              36.54934470361806\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"111","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ee4b07f02db5fddf2","contributors":{"authors":[{"text":"Matlock, G.C.","contributorId":76262,"corporation":false,"usgs":true,"family":"Matlock","given":"G.C.","email":"","affiliations":[],"preferred":false,"id":320357,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Weaver, J.E.","contributorId":81840,"corporation":false,"usgs":true,"family":"Weaver","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":320358,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Green, A.W.","contributorId":34863,"corporation":false,"usgs":true,"family":"Green","given":"A.W.","affiliations":[],"preferred":false,"id":320356,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70180852,"text":"70180852 - 1982 - Lakes and lake-like waters of the Hawaiian Archipelago","interactions":[],"lastModifiedDate":"2017-02-03T15:24:38","indexId":"70180852","displayToPublicDate":"1982-04-30T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5287,"text":"Occasional Papers Bernice P. Bishop Museum","active":true,"publicationSubtype":{"id":10}},"title":"Lakes and lake-like waters of the Hawaiian Archipelago","docAbstract":"<p>This summary&nbsp;of Hawaiian lacustrine limnology is based on 12 years of field and literature surveys of archipelagic inland waters. Lakes here are distinguished from other standing waters by limits on surface oceanic area (&gt; 0.1 ha) and depth (&gt; 2 m), and by the absence of flatural surface oceanic connection. A variety of extinct and existing water bodies, sometimes referred to as lakes, are noted. Six lakes are described. Five of them are in crater basins, 3 are freshwater, and 2 are elevated (highest = 3969 m). The scarcity of elevated lakes results from general permeability of the substrata. Among the 6 lakes, surface areas range from 0.22 to 88 ha and maximum depths from 3 to 248 m. Naturally occurring aquatic biota generally is low in species diversity except for phytoplankton; fishes and submersed vascular plants are absent. Two lowland lakes, freshwater Green (Wai a Pele) and saline Kauhak6, are described for the first time. Profundal Kauhak6, 248 m deep, has a surface area of only 0.35 ha, which results in an extraordinary relative depth of 370%. It is permanently stratified, a condition apparently due primarily to the unique morphometry of its basin.&nbsp;<br></p>","language":"English","publisher":"Bernice P. Bishop Museum ","usgsCitation":"Maciolek, J.A., 1982, Lakes and lake-like waters of the Hawaiian Archipelago: Occasional Papers Bernice P. 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,{"id":70209772,"text":"70209772 - 1982 - Geomagnetic Workshop","interactions":[],"lastModifiedDate":"2020-04-24T19:51:39.684499","indexId":"70209772","displayToPublicDate":"1982-04-24T14:43:15","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Geomagnetic Workshop","docAbstract":"<p>A workshop on geomagnetism, sponsored by the Geologic Division of the U.S. Geological Survey, was held in the Denver West Office Complex in Golden, Colorado, April 13–15, 1982. There were 90 registered participants from government agencies, academic institutions, and industry.</p><p>This effort stemmed from the realization that geomagnetism, once a small but coherent discipline, has now expanded into numerous areas of the geosciences, yet those doing research in these specialties seldom make contact outside their area of immediate interest. The impetus for this event came from the members of a committee formed to review the geomagnetic activities within the U.S. Geological Survey. They observed that the level of communication between the various elements of this now diverse discipline was inadequate, not only within their organization but also between federal agencies, academia, and the private sector. While the desire was to cover as much of geomagnetism as possible, it was necessary for a workshop of reasonable size and length to exclude some important areas of the subject: magnetic reversal chronology, studies of the externally produced variations, and most aspects of internal induction. The plan was to give emphasis to some of the newer areas: those which have recently seen a high level of activity and those with increasing activity abroad compared to that in the United States. The purpose was to evaluate the status and problems in selected areas with an eye to those whose emphasis might produce fruitful results in the next decade.</p>","language":"English","publisher":"Wiley","doi":"10.1029/EO063i035p00645","usgsCitation":"DeNoyer, J.M., Cain, J., Banerjee, S., Benton, E., Blakely, R.J., Coe, R.S., Harrison, C., Johnston, M.J., and Regan, R., 1982, Geomagnetic Workshop: Eos, Transactions, American Geophysical Union, v. 63, no. 35, p. 645-648, https://doi.org/10.1029/EO063i035p00645.","productDescription":"4 p.","startPage":"645","endPage":"648","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":374271,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"63","issue":"35","noUsgsAuthors":false,"publicationDate":"2011-06-03","publicationStatus":"PW","contributors":{"authors":[{"text":"DeNoyer, John M.","contributorId":96271,"corporation":false,"usgs":true,"family":"DeNoyer","given":"John","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":787945,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cain, J.C.","contributorId":68457,"corporation":false,"usgs":true,"family":"Cain","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":787946,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Banerjee, S.","contributorId":74606,"corporation":false,"usgs":true,"family":"Banerjee","given":"S.","email":"","affiliations":[],"preferred":false,"id":787947,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Benton, E.R.","contributorId":100550,"corporation":false,"usgs":true,"family":"Benton","given":"E.R.","email":"","affiliations":[],"preferred":false,"id":787948,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Blakely, Richard J. 0000-0003-1701-5236 blakely@usgs.gov","orcid":"https://orcid.org/0000-0003-1701-5236","contributorId":1540,"corporation":false,"usgs":true,"family":"Blakely","given":"Richard","email":"blakely@usgs.gov","middleInitial":"J.","affiliations":[{"id":662,"text":"Western Mineral and Environmental Resources Science Center","active":true,"usgs":true},{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":787949,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Coe, Robert S.","contributorId":20477,"corporation":false,"usgs":true,"family":"Coe","given":"Robert","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":787950,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Harrison, C.G.A.","contributorId":224360,"corporation":false,"usgs":false,"family":"Harrison","given":"C.G.A.","email":"","affiliations":[],"preferred":false,"id":787951,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Johnston, Malcolm J. 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,{"id":1007621,"text":"1007621 - 1982 - Hematology of the West Indian manatee (Trichechus manatus)","interactions":[],"lastModifiedDate":"2026-03-16T13:39:13.07585","indexId":"1007621","displayToPublicDate":"1982-04-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3680,"text":"Veterinary Clinical Pathology","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Hematology of the West Indian manatee (<i>Trichechus manatus</i>)","title":"Hematology of the West Indian manatee (Trichechus manatus)","docAbstract":"<p><span>Hemograms on blood obtained from 10 clinically normal West Indian Manatees (<i>Trichechus manatus</i>) were studied. The red cells were large and in lower number than in most terrestrial species. The manatee does not have a neutrophil as is present in most species, but it has a heterophil whose granules stain pink with the Wright-Giemsa stain. </span></p><p><span>The eosinophil has uniform red-staining granules that make its differentiation from heterophils difficult. Both large and small lymphocytes, monocytes and basophils are present. The total number of white blood cells was comparable to that of common domestic species as were the platelet numbers. No reticulocytes were found.</span></p>","language":"English","publisher":"Wiley","doi":"10.1111/j.1939-165X.1982.tb00822.x","usgsCitation":"Medway, W., Black, D., and Rathbun, G.B., 1982, Hematology of the West Indian manatee (Trichechus manatus): Veterinary Clinical Pathology, v. 11, no. 2, p. 11-15, https://doi.org/10.1111/j.1939-165X.1982.tb00822.x.","productDescription":"5 p.","startPage":"11","endPage":"15","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":130033,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"11","issue":"2","noUsgsAuthors":false,"publicationDate":"2009-02-23","publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db635dbe","contributors":{"authors":[{"text":"Medway, W.","contributorId":97453,"corporation":false,"usgs":true,"family":"Medway","given":"W.","email":"","affiliations":[],"preferred":false,"id":315739,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Black, D.J.","contributorId":72744,"corporation":false,"usgs":true,"family":"Black","given":"D.J.","email":"","affiliations":[],"preferred":false,"id":957092,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rathbun, G. B.","contributorId":106044,"corporation":false,"usgs":true,"family":"Rathbun","given":"G.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":315740,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":5221781,"text":"5221781 - 1982 - Organochlorine residues and shell thinning in Oregon seabird eggs","interactions":[],"lastModifiedDate":"2024-10-09T16:08:42.763965","indexId":"5221781","displayToPublicDate":"1982-04-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2793,"text":"Murrelet","active":true,"publicationSubtype":{"id":10}},"title":"Organochlorine residues and shell thinning in Oregon seabird eggs","docAbstract":"<p>A single egg was collected at 62 nests of 10 seabird species from Oregon in 1979. The eggs were analyzed for organochlorine contaminants; contemporary shell thickness was compared with eggshells collected during earlier time periods. Concentrations of DDE and PCB's in 1979 were generally low with the most contaminated species being the Double-crested Cormorant (<i>Phalacrocorax auritus</i>), Leach's Storm Petrel (<i>Oceanodroma leucorhoa</i>), and Forktailed Storm Petrel (<i>O. furcata</i>). Limited eggshell data provide evidence that shell thinning was more severe along the Oregon coast in the 1950's than in 1979. With the possible exception of the Fork-tailed Storm Petrel, the residues in 1979 posed no known threat to the welfare of the species.</p>","language":"English","publisher":"Society for Northwestern Vertebrate Biology","doi":"10.2307/3535474","usgsCitation":"Henny, C.J., Blus, L.J., and Prouty, R.M., 1982, Organochlorine residues and shell thinning in Oregon seabird eggs: Murrelet, v. 63, no. 1, p. 15-21, https://doi.org/10.2307/3535474.","productDescription":"7 p.","startPage":"15","endPage":"21","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":196977,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":18299,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://www.jstor.org/stable/3535474","linkFileType":{"id":5,"text":"html"}}],"country":"United 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,{"id":1007620,"text":"1007620 - 1982 - Analysis of propeller wounds on manatees in Florida","interactions":[],"lastModifiedDate":"2024-10-30T16:53:27.374349","indexId":"1007620","displayToPublicDate":"1982-04-01T00:00:00","publicationYear":"1982","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":"Analysis of propeller wounds on manatees in Florida","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"Wiley","doi":"10.2307/3808675","usgsCitation":"Beck, C.A., Bonde, R.K., and Rathbun, G.B., 1982, Analysis of propeller wounds on manatees in Florida: Journal of Wildlife Management, v. 46, no. 2, p. 531-535, https://doi.org/10.2307/3808675.","productDescription":"5 p.","startPage":"531","endPage":"535","costCenters":[{"id":651,"text":"Western Ecological Research 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B.","contributorId":17571,"corporation":false,"usgs":true,"family":"Rathbun","given":"Galen","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":315737,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70185626,"text":"70185626 - 1982 - On conducting the modified ‘Slug’ test in tight formations","interactions":[],"lastModifiedDate":"2020-03-09T19:49:29","indexId":"70185626","displayToPublicDate":"1982-04-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3722,"text":"Water Resources Research","onlineIssn":"1944-7973","printIssn":"0043-1397","active":true,"publicationSubtype":{"id":10}},"title":"On conducting the modified ‘Slug’ test in tight formations","docAbstract":"<p><span>The method introduced by Bredehoeft and Papadopulos (1980) for conducting a modified ‘slug’ test in tight formations does not assure the condition of approximate equilibrium necessary at the start of the test. In addition, compressibility in the shut-in well can be significantly larger than the compressibility of water, which Bredehoeft and Papadopulos indicate should be used in the calculations. Errors that may result from using the original test procedure are discussed, and a modified procedure and testing arrangement are presented.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/WR018i002p00439","usgsCitation":"Neuzil, C., 1982, On conducting the modified ‘Slug’ test in tight formations: Water Resources Research, v. 18, no. 2, p. 439-441, https://doi.org/10.1029/WR018i002p00439.","productDescription":"3 p. ","startPage":"439","endPage":"441","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":338327,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"18","issue":"2","noUsgsAuthors":false,"publicationDate":"2010-07-09","publicationStatus":"PW","scienceBaseUri":"58d63042e4b05ec799131125","contributors":{"authors":[{"text":"Neuzil, C.E. 0000-0003-2022-4055","orcid":"https://orcid.org/0000-0003-2022-4055","contributorId":60401,"corporation":false,"usgs":true,"family":"Neuzil","given":"C.E.","email":"","affiliations":[],"preferred":false,"id":686153,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70120265,"text":"70120265 - 1982 - Habitat models for land-use planning: assumptions and strategies for development","interactions":[],"lastModifiedDate":"2014-08-13T14:25:12","indexId":"70120265","displayToPublicDate":"1982-03-26T14:13:00","publicationYear":"1982","noYear":false,"publicationType":{"id":4,"text":"Book"},"publicationSubtype":{"id":12,"text":"Conference publication"},"title":"Habitat models for land-use planning: assumptions and strategies for development","docAbstract":"<p>Wildlife managers have long recognized that management goals must be constrained by the availability and suitability of habitat.  This recognition, combined with ever increasing land development pressures, has resulted in environmental legislation emphasizing systematic approaches to collection and analysis of habitat information.  Wildlife planners have responded with a variety of approached to the development of models that quantify habitat requirements.</p>\n<br/>\n<p>The use of habitat models in wildlife management is certainly not a new concept.  Early models attempted to relate habitat quality and quantity as defined by various life requisites (Trippensee 1948).  Conceptually, these early approaches are identical to many contemporary efforts directed at modeling habitat.</p>\n<br/>\n<p>This paper has two objectives related to contemporary habitat modeling approaches.  The first objective is to characterize the assumptions and limitations inherent to operational habitat models.  Various approaches to habitat modeling, some of which will be discussed at this conference, are described in their own terminology-which tends to obscure the fact that they have common ideals and are subject to the same sets of limitations.</p>\n<br/>\n<p>The second objective of this paper is to describe a strategy for development of habitat models consistent with these potential limitations.  There seems to be two divergent perspectives on operational habitat models.  The first is an ideal perspective, which views operational habitat models with skepticism because the current state of habitat knowledge is limited.  The second is a pragmatic perspective, which recognizes that available habitat information, no matter how incomplete, can be used to improve the credibility of a land-use decision.  The strategy outlined in this paper is directed toward the latter perspective but may help to bridge the gap between the pragmatic and ideal.</p>","largerWorkTitle":"Transactions of the Forty-seventh North American Wildlife and Natural Resources Conference: Population pressures and natural resource management needs","conferenceTitle":"Transactions of the Forty-seventh North American Wildlife and Natural Resources Conference: Population pressures and natural resource management needs","conferenceDate":"1982-03-26T00:00:00","conferenceLocation":"Portland, OR","language":"English","publisher":"Wildlife Management Institute","publisherLocation":"Washington, D.C.","usgsCitation":"Farmer, A.H., Armbruster, M.J., Terrell, J.W., and Schroeder, R.L., 1982, Habitat models for land-use planning: assumptions and strategies for development, 11 p.","productDescription":"11 p.","numberOfPages":"11","costCenters":[],"links":[{"id":292110,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53ec7bcce4b02bf5a7674054","contributors":{"authors":[{"text":"Farmer, Adrian H.","contributorId":107759,"corporation":false,"usgs":true,"family":"Farmer","given":"Adrian","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":498080,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Armbruster, Michael J.","contributorId":16884,"corporation":false,"usgs":true,"family":"Armbruster","given":"Michael","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":498078,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Terrell, James W. 0000-0001-5394-5663","orcid":"https://orcid.org/0000-0001-5394-5663","contributorId":92726,"corporation":false,"usgs":true,"family":"Terrell","given":"James","email":"","middleInitial":"W.","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":true,"id":498079,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Schroeder, Richard L.","contributorId":10368,"corporation":false,"usgs":true,"family":"Schroeder","given":"Richard","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":498077,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70230870,"text":"70230870 - 1982 - California's Central Valley wintering waterfowl: Concerns and challenges","interactions":[],"lastModifiedDate":"2022-04-27T14:00:43.950118","indexId":"70230870","displayToPublicDate":"1982-03-26T08:47:02","publicationYear":"1982","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"seriesTitle":{"id":5322,"text":"Transactions of the North American Wildlife and Natural Resources Conference","printIssn":"0078-1355","active":true,"publicationSubtype":{"id":19}},"title":"California's Central Valley wintering waterfowl: Concerns and challenges","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Transactions of the 47th North American Wildlife and Natural Resources Conference","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"47th North American Wildlife and Natural Resources Conference","conferenceDate":"March 26-31, 1982","conferenceLocation":"Portland, Oregon, United States","language":"English","publisher":"Wildlife Management Institute","publisherLocation":"Washington, D. C.","usgsCitation":"Gilmer, D.S., Miller, M.R., Bauer, R.D., and LeDonne, J.R., 1982, California's Central Valley wintering waterfowl: Concerns and challenges, <i>in</i> Transactions of the 47th North American Wildlife and Natural Resources Conference, Portland, Oregon, United States, March 26-31, 1982, p. 441-452.","productDescription":"12 p.","startPage":"441","endPage":"452","costCenters":[],"links":[{"id":399741,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":399740,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://wildlifemanagement.institute/store/product/37"}],"country":"United States","state":"California","otherGeospatial":"Central Valley, Delta & Suisun Marsh, Sacramento Valley, San Joaquin Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        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D.","contributorId":290672,"corporation":false,"usgs":false,"family":"Bauer","given":"Richard","email":"","middleInitial":"D.","affiliations":[{"id":6987,"text":"U.S. Fish and Wildlife Sevice","active":true,"usgs":false}],"preferred":false,"id":841523,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"LeDonne, John R.","contributorId":290673,"corporation":false,"usgs":false,"family":"LeDonne","given":"John","email":"","middleInitial":"R.","affiliations":[{"id":12939,"text":"California Department of Fish and Game","active":true,"usgs":false}],"preferred":false,"id":841524,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":1007586,"text":"1007586 - 1982 - Lumber spill in central California waters: Implications for oil spills and sea otters","interactions":[],"lastModifiedDate":"2025-12-22T16:51:02.150891","indexId":"1007586","displayToPublicDate":"1982-03-19T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Lumber spill in central California waters: Implications for oil spills and sea otters","docAbstract":"<p><span>A large quantity of lumber was spilled in the ocean off central California during the winter of 1978, and it spread through most of the range of the threatened California sea otter population within 4 weeks. The movement rates of lumber were similar to those of oil slicks observed elsewhere. These observations indicate that a major oil spill could expose significant numbers of California sea otters to oil contamination.</span></p>","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.215.4539.1503","usgsCitation":"VanBlaricom, G., and Jameson, R., 1982, Lumber spill in central California waters: Implications for oil spills and sea otters: Science, v. 215, no. 4539, p. 1503-1505, https://doi.org/10.1126/science.215.4539.1503.","productDescription":"3 p.","startPage":"1503","endPage":"1505","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":129872,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"central California","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -125.01453001470827,\n              39.194787155092456\n            ],\n            [\n              -120.48460325212284,\n              33.48450467089073\n            ],\n            [\n              -118.28209449425341,\n              34.280736888845524\n            ],\n            [\n              -121.64372529379582,\n              39.398525519817156\n            ],\n            [\n              -125.01453001470827,\n              39.194787155092456\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"215","issue":"4539","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7fe4b07f02db6489e2","contributors":{"authors":[{"text":"VanBlaricom, G.R.","contributorId":94239,"corporation":false,"usgs":true,"family":"VanBlaricom","given":"G.R.","email":"","affiliations":[],"preferred":false,"id":315671,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jameson, R.J.","contributorId":56581,"corporation":false,"usgs":true,"family":"Jameson","given":"R.J.","email":"","affiliations":[],"preferred":false,"id":315670,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70208962,"text":"70208962 - 1982 - Mid-Paleozoic age of the Roberts thrust unsettled by new data from northern Nevada ","interactions":[],"lastModifiedDate":"2020-03-09T13:22:00","indexId":"70208962","displayToPublicDate":"1982-03-09T13:10:01","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1796,"text":"Geology","active":true,"publicationSubtype":{"id":10}},"title":"Mid-Paleozoic age of the Roberts thrust unsettled by new data from northern Nevada ","docAbstract":"<p><span>The Roberts thrust is a major thrust in Nevada on which Ordovician to Devonian siliceous facies rocks were carried more than 80 km eastward over contemporaneous carbonate facies. For more than two decades, a mid-Paleozoic age for this structure has been widely accepted. The bases for dating the thrust are (1) the assumption that the Roberts thrust formed at the time of the Antler orogeny—a reliably dated mid-Paleozoic event, and (2) the concept of an overlapping assemblage consisting of sedimentary strata deposited on both the allochthon and autochthon. The first assumption is unproved, and the second relies on another assumption: that the overlap assemblage was not cut and telescoped by the Roberts thrust. In the years since a mid-Paleozoic age for the Roberts thrust became widely accepted, much new information on the stratigraphy and facies relations of Mississippian rocks in northern Nevada has accumulated. One interpretation of these new data suggests that in the Pinon Range, where a mid-Paleozoic age for the thrust was most convincingly displayed, the overlap assemblage actually may have been cut by a major thrust that juxtaposed contrasting facies of Mississippian rocks. If so, the principal evidence used to date the Roberts thrust is compromised, and the time has come for an agonizing reappraisal of all evidence bearing on the question. A mid-Paleozoic age can no longer be taken for granted, and a post-Paleozoic age cannot be ruled out.</span></p>","language":"English","publisher":"GSA","doi":"10.1130/0091-7613(1982)10<298:MAOTRT>2.0.CO;2","usgsCitation":"Ketner, K.B., and Smith, F.J., 1982, Mid-Paleozoic age of the Roberts thrust unsettled by new data from northern Nevada : Geology, v. 10, no. 6, p. 298-303, https://doi.org/10.1130/0091-7613(1982)10<298:MAOTRT>2.0.CO;2.","productDescription":"6 p.","startPage":"298","endPage":"303","costCenters":[],"links":[{"id":373016,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Nevada","otherGeospatial":"Northern Nevada","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -116.52099609375,\n              39.317300373271024\n            ],\n            [\n              -113.99414062499999,\n              39.26628442213066\n            ],\n            [\n              -114.12597656249999,\n              42.01665183556825\n            ],\n            [\n              -117.48779296875,\n              42.00032514831621\n            ],\n            [\n              -117.72949218749999,\n              39.11301365149975\n            ],\n            [\n              -116.52099609375,\n              39.317300373271024\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"10","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Ketner, Keith B.","contributorId":957,"corporation":false,"usgs":true,"family":"Ketner","given":"Keith","email":"","middleInitial":"B.","affiliations":[],"preferred":true,"id":784207,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smith, Fred J. Jr.","contributorId":30864,"corporation":false,"usgs":true,"family":"Smith","given":"Fred","suffix":"Jr.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":784208,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70011801,"text":"70011801 - 1982 - Molecular size of aquatic humic substances","interactions":[],"lastModifiedDate":"2025-03-19T15:47:43.144793","indexId":"70011801","displayToPublicDate":"1982-03-05T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2958,"text":"Organic Geochemistry","active":true,"publicationSubtype":{"id":10}},"title":"Molecular size of aquatic humic substances","docAbstract":"<p><span>Aquatic humic substances, which account for 30 to 50% of the organic carbon in water, are a principal component of aquatic organic matter. The molecular size of aquatic humic substances, determined by small-angle X-ray scattering, varies from 4.7 to 33 Å in their radius of gyration, corresponding to a molecular weight range of 500 to greater than 10,000. The aquatic fulvic acid fraction contains substances with molecular weights ranging from 500 to 2000 and is monodisperse, whereas the aquatic humic acid fraction contains substances with molecular weights ranging from 1000 to greater than 10,000 and is generally polydisperse.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0146-6380(82)90005-5","usgsCitation":"Thurman, E., Wershaw, R., Malcolm, R., and Pinckney, D., 1982, Molecular size of aquatic humic substances: Organic Geochemistry, v. 4, no. 1, p. 27-35, https://doi.org/10.1016/0146-6380(82)90005-5.","productDescription":"9 p.","startPage":"27","endPage":"35","costCenters":[],"links":[{"id":220994,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Arizona, Colorado, Hawaii, Florida, Massachusetts, Minnesota, North Dakota, South Dakota, Wyoming","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"MultiPolygon\",\"coordinates\":[[[[-112.538593,37.000674],[-109.045223,36.999084],[-109.050044,31.332502],[-111.125646,31.348978],[-114.813613,32.494277],[-114.463127,32.901884],[-114.701165,33.086368],[-114.722872,33.398779],[-114.542011,33.542481],[-114.52868,33.947817],[-114.163122,34.255187],[-114.630682,34.866352],[-114.569238,35.18348],[-114.755618,36.087166],[-114.114531,36.095217],[-113.965907,37.000025],[-112.538593,37.000674]]],[[[-104.053249,41.001406],[-102.124972,41.002338],[-102.04192,37.035083],[-109.045223,36.999084],[-109.050076,41.000659],[-111.046723,40.997959],[-111.055199,45.001321],[-104.057698,44.997431],[-103.992467,48.999567],[-95.153711,48.998903],[-95.153314,49.384358],[-94.878454,49.333193],[-94.640803,48.741171],[-93.818375,48.534442],[-92.984963,48.623731],[-92.634931,48.542873],[-92.698824,48.494892],[-92.341207,48.23248],[-92.066269,48.359602],[-91.542512,48.053268],[-90.88548,48.245784],[-90.703702,48.096009],[-89.489226,48.014528],[-90.735927,47.624343],[-92.058888,46.809938],[-92.025789,46.710839],[-92.189091,46.717541],[-92.291976,46.503997],[-92.33859,46.050111],[-92.869193,45.717568],[-92.646602,45.441635],[-92.807362,44.758909],[-91.410555,43.970892],[-91.244135,43.774667],[-91.243183,43.540309],[-96.591213,43.500514],[-96.439335,43.113916],[-96.630311,42.770885],[-96.483592,42.510345],[-97.302075,42.86566],[-98.035034,42.764205],[-98.568936,42.998537],[-104.053127,43.000585],[-104.053249,41.001406]]],[[[-81.582923,24.658732],[-81.451267,24.747464],[-81.298028,24.656774],[-81.765993,24.552103],[-81.582923,24.658732]]],[[[-84.777208,29.707398],[-84.696726,29.76993],[-85.036219,29.588919],[-84.777208,29.707398]]],[[[-82.255777,26.703437],[-82.038403,26.456907],[-82.186441,26.489221],[-82.255777,26.703437]]],[[[-80.250581,25.34193],[-80.611693,24.93842],[-80.192336,25.473331],[-80.250581,25.34193]]],[[[-83.309455,30.634417],[-82.287343,30.573458],[-82.101416,30.366556],[-81.962739,30.813636],[-81.472597,30.713312],[-81.256711,29.784693],[-80.567361,28.562353],[-80.566432,28.09563],[-80.031362,26.796339],[-80.152896,25.702855],[-80.229107,25.732509],[-80.495341,25.199463],[-81.079859,25.118797],[-81.362272,25.824401],[-81.727086,25.907207],[-81.868983,26.378648],[-82.094748,26.48393],[-82.076349,26.958263],[-82.147068,26.789803],[-82.301736,26.841588],[-82.714521,27.500415],[-82.393383,27.837519],[-82.716522,27.958398],[-82.566819,27.858002],[-82.721622,27.663908],[-82.851126,27.8863],[-82.674787,28.441956],[-82.702618,28.932955],[-83.679219,29.918513],[-84.245668,30.093021],[-84.335953,29.912962],[-85.343619,29.672004],[-85.405052,29.938487],[-86.222561,30.343585],[-87.518324,30.280435],[-87.395941,30.643968],[-87.626228,30.857127],[-87.548543,30.997927],[-85.057534,31.000585],[-84.887522,30.741791],[-83.309455,30.634417]]],[[[-155.778234,20.245743],[-155.149215,19.922872],[-154.838545,19.463642],[-155.505281,19.137908],[-155.658486,18.924835],[-155.88155,19.036644],[-156.051652,19.703649],[-155.835312,19.976078],[-155.901452,20.235787],[-155.778234,20.245743]]],[[[-159.431707,22.220015],[-159.295271,22.13039],[-159.408284,21.897781],[-159.788139,22.018411],[-159.699978,22.165252],[-159.431707,22.220015]]],[[[-157.014553,21.185503],[-156.742231,21.176214],[-156.865795,21.057801],[-157.254061,21.090601],[-157.185553,21.205602],[-157.014553,21.185503]]],[[[-156.612012,21.02477],[-155.991534,20.713654],[-156.444242,20.607941],[-156.464043,20.781667],[-156.688969,20.888673],[-156.612012,21.02477]]],[[[-157.010001,20.929757],[-156.838321,20.764575],[-156.949009,20.738997],[-157.010001,20.929757]]],[[[-158.044485,21.306011],[-158.250671,21.557373],[-158.018127,21.699955],[-157.6619,21.3131],[-158.044485,21.306011]]],[[[-70.59628,41.471905],[-70.450431,41.420703],[-70.496162,41.346452],[-70.802083,41.314207],[-70.59628,41.471905]]],[[[-70.092142,41.297741],[-69.960277,41.278731],[-70.256164,41.288123],[-70.092142,41.297741]]],[[[-73.022903,42.741133],[-71.351874,42.698154],[-70.886136,42.88261],[-70.595474,42.660336],[-70.996097,42.271222],[-70.754488,42.228673],[-70.471552,41.761563],[-70.008462,41.800786],[-70.169781,42.059736],[-70.082624,42.054657],[-69.928261,41.6917],[-70.902763,41.421061],[-70.658659,41.543385],[-70.623652,41.707398],[-71.12057,41.497448],[-71.458104,42.017762],[-73.508142,42.086257],[-73.264957,42.74594],[-73.022903,42.741133]]]]},\"properties\":{\"name\":\"Arizona\",\"nation\":\"USA  \"}}]}","volume":"4","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a5d12e4b0c8380cd70137","contributors":{"authors":[{"text":"Thurman, E.M.","contributorId":102864,"corporation":false,"usgs":true,"family":"Thurman","given":"E.M.","affiliations":[],"preferred":false,"id":361988,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wershaw, R.L.","contributorId":62223,"corporation":false,"usgs":true,"family":"Wershaw","given":"R.L.","affiliations":[],"preferred":false,"id":361987,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Malcolm, Ronald L.","contributorId":46075,"corporation":false,"usgs":true,"family":"Malcolm","given":"Ronald L.","affiliations":[],"preferred":false,"id":361986,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Pinckney, D.J.","contributorId":23175,"corporation":false,"usgs":true,"family":"Pinckney","given":"D.J.","affiliations":[],"preferred":false,"id":361985,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":5221778,"text":"5221778 - 1982 - Use of blood levels to infer carcass levels of contaminants","interactions":[],"lastModifiedDate":"2023-12-12T17:35:34.427962","indexId":"5221778","displayToPublicDate":"1982-03-01T12:19:26","publicationYear":"1982","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":"Use of blood levels to infer carcass levels of contaminants","docAbstract":"<p><span>Inferences may be made about the carcass levels of a contaminant based on the contaminant level in blood samples. A method is given for comparing such populations that utilizes bivariate normal distributions and their principal axes, thereby avoiding a dilemma arising from the use of regression techniques. Confidence intervals and power calculations are given. Data from captive barn owls provide partial justification for the use of this method.</span></p>","language":"English","publisher":"Springer","doi":"10.1007/BF01054901","usgsCitation":"Hensler, G.L., and Stout, W., 1982, Use of blood levels to infer carcass levels of contaminants: Archives of Environmental Contamination and Toxicology, v. 11, no. 2, p. 235-238, https://doi.org/10.1007/BF01054901.","productDescription":"4 p.","startPage":"235","endPage":"238","numberOfPages":"4","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":197418,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"11","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dee4b07f02db5e272a","contributors":{"authors":[{"text":"Hensler, Gary L.","contributorId":23111,"corporation":false,"usgs":true,"family":"Hensler","given":"Gary","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":334659,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stout, William C.","contributorId":56756,"corporation":false,"usgs":false,"family":"Stout","given":"William C.","affiliations":[],"preferred":false,"id":334660,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":5221789,"text":"5221789 - 1982 - Ingestion of petroleum by breeding mallard ducks: Some effects on neonatal progeny","interactions":[],"lastModifiedDate":"2023-12-12T17:40:07.155403","indexId":"5221789","displayToPublicDate":"1982-03-01T12:19:23","publicationYear":"1982","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":"Ingestion of petroleum by breeding mallard ducks: Some effects on neonatal progeny","docAbstract":"<p><span>Breeding female mallard ducks consuming petroleum-contaminated food show significant induced increases in the naphthalene-metabolizing properties of microsomes prepared from their livers. Food contaminated with South Louisiana crude oil was more potent than food contaminated with similar concentrations of Prudhoe Bay crude oil and in each instance food contaminated with 3% (v/w) induced greater increases than food contaminated at the 1% level. These increases in hepatic naphthalene-metabolizing activity may reflect their responses to circulating petroleum contaminants derived from ingested crude oil. When incubated, fertilized eggs laid by the females consuming South Louisiana crude oil yielded ducklings that upon emergence possessed high levels of naphthalene-metabolizing activity associated with hepatic microsomes. In contrast, ducklings derived from eggs laid by females consuming food contaminated with Prudhoe Bay crude oil showed no increases in total hepatic naphthalene-metabolizing activity and only those ducklings hatched from eggs laid by females consuming food contaminated with 3% crude oil showed significantly induced levels of specific naphthalene-metabolizing activity at hatching. During the first week of postnatal life both the uncontaminated ducklings and the ducklings hatched from eggs laid by females consuming food contaminated with South Louisiana crude oil showed initial transient rises in specific and total hepatic naphthalene-metabolizing activity. In each instance, these rises were proportional to the level of contamination in the food consumed by the females. Thereafter, the specific activities of the naphthalene-metabolizing enzyme in all ducklings declined to the level found at hatching in uncontaminated ducklings. Similarly, the total hepatic naphthalene-metabolizing activities in ducklings derived from females consuming food contaminated with 3% crude oil also declined to the level at hatching in uncontaminated ducklings. In contrast, after one week, ducklings hatched from eggs laid by females consuming food contaminated with 1% crude oil showed total hepatic naphthalene-metabolizing activities that were more than twice those found at hatching.</span></p>","language":"English","publisher":"Springer","doi":"10.1007/BF01054890","usgsCitation":"Gorsline, J., and Holmes, W.N., 1982, Ingestion of petroleum by breeding mallard ducks: Some effects on neonatal progeny: Archives of Environmental Contamination and Toxicology, v. 11, no. 2, p. 147-153, https://doi.org/10.1007/BF01054890.","productDescription":"7 p.","startPage":"147","endPage":"153","numberOfPages":"7","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":193600,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"11","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e478ee4b07f02db489d49","contributors":{"authors":[{"text":"Gorsline, J.","contributorId":30307,"corporation":false,"usgs":true,"family":"Gorsline","given":"J.","email":"","affiliations":[],"preferred":false,"id":334687,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Holmes, W. N.","contributorId":70497,"corporation":false,"usgs":false,"family":"Holmes","given":"W.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":334688,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70011802,"text":"70011802 - 1982 - Age determination of late Pleistocene marine transgression in western Alaska","interactions":[],"lastModifiedDate":"2024-10-16T15:49:36.594723","indexId":"70011802","displayToPublicDate":"1982-03-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2667,"text":"Marine Geology","active":true,"publicationSubtype":{"id":10}},"title":"Age determination of late Pleistocene marine transgression in western Alaska","docAbstract":"<p>Dating molluscs from sediments representing the Kotzebuan marine transgression in Alaska yields an average uranium-series age of 104,000 <span>± </span>22,000 yrs B.P. This and other selected Pleistocene marine deposits of western Alaska are tentatively correlated with radiometrically dated units of eastern Baffin Island, Arctic Canada.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0025-3227(82)90147-5","usgsCitation":"Szabo, B.J., 1982, Age determination of late Pleistocene marine transgression in western Alaska: Marine Geology, v. 46, no. 1-2, p. M1-M8, https://doi.org/10.1016/0025-3227(82)90147-5.","productDescription":"8 p.","startPage":"M1","endPage":"M8","costCenters":[],"links":[{"id":220995,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"western Alaska","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              188.20764945303154,\n              72.48831967560417\n            ],\n            [\n              188.20764945303154,\n              59.41217547528831\n            ],\n            [\n              200.67139608434223,\n              59.41217547528831\n            ],\n            [\n              200.67139608434223,\n              72.48831967560417\n            ],\n            [\n              188.20764945303154,\n              72.48831967560417\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"46","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e8eae4b0c8380cd47f81","contributors":{"authors":[{"text":"Szabo, Barney J.","contributorId":6848,"corporation":false,"usgs":true,"family":"Szabo","given":"Barney","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":361989,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70208682,"text":"70208682 - 1982 - Cenozoic silicoflagellates from offshore Guatemala, Deep Sea Drilling Project Site 495","interactions":[],"lastModifiedDate":"2020-02-25T07:30:10","indexId":"70208682","displayToPublicDate":"1982-02-24T14:16:05","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1996,"text":"Initial Reports of the D.S.D.P.","active":true,"publicationSubtype":{"id":10}},"title":"Cenozoic silicoflagellates from offshore Guatemala, Deep Sea Drilling Project Site 495","docAbstract":"<p>Diverse lower Miocene to Pleistocene silicoflagellate assemblages occur at Deep Sea Drilling Project Site 495, but many samples are dominated by one or two taxa. Low-latitude zonation can be applied throughout. Cool-indicating Distephanus speculum s. ampl. is only abundant in the upper Miocene; however, relative paleotemperature values (Ts) suggest temperature extremes in the lower Miocene similar to those in the upper Miocene. The lower upper Miocene ap pears to be thinned or missing, because no Dictyocha brevispina Zone assemblages are identified. The lower Miocene assemblages of the Naviculopsis ponticula Zone are an important silicoflagellate reference because of several new taxa and associations. </p><p>New taxa and recombinations described herein include: Corbisema triacantha var. nuda n. var., Dictyocha angulata n. sp., D. delicata n. comb., D. delicata var. bisecta n. var., D. longa n. sp., D. longa var.paxilla n. var., D. ornata ornata n. comb., D. ornata africana n. subsp., D. subaculeata n. comb., Distephanus crux parvus n. comb., D. crux scutulatusn. subsp., D. polyactis var. literatusn. var.,Z speculumpatulus n. subsp., Naviculopsis contraria n. sp., N. lacrima n. sp., N. lata var. obliqua n. var., N. ponticula spinosa n. subsp</p>","language":"English","publisher":"Texas A&M","doi":"10.2973/dsdp.proc.67.112.1982","usgsCitation":"Bukry, D., 1982, Cenozoic silicoflagellates from offshore Guatemala, Deep Sea Drilling Project Site 495: Initial Reports of the D.S.D.P., v. 67, p. 425-445, https://doi.org/10.2973/dsdp.proc.67.112.1982.","productDescription":"21 p.","startPage":"425","endPage":"445","costCenters":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"links":[{"id":488884,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.2973/dsdp.proc.67.112.1982","text":"Publisher Index Page"},{"id":372574,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"67","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Bukry, David 0000-0003-4540-890X dbukry@usgs.gov","orcid":"https://orcid.org/0000-0003-4540-890X","contributorId":3550,"corporation":false,"usgs":true,"family":"Bukry","given":"David","email":"dbukry@usgs.gov","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":782982,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70208505,"text":"70208505 - 1982 - Survival of duck plague virus in water from Lake Andes National Wildlife Refuge, South Dakota","interactions":[],"lastModifiedDate":"2020-03-11T09:52:25","indexId":"70208505","displayToPublicDate":"1982-02-12T10:54:12","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2507,"text":"Journal of Wildlife Diseases","active":true,"publicationSubtype":{"id":10}},"title":"Survival of duck plague virus in water from Lake Andes National Wildlife Refuge, South Dakota","docAbstract":"<p><span>An isolant of duck plague herpesvirus from the Lake Andes Refuge outbreak was seeded in raw and filter-decontaminated water from two locations on the refuge, held at 4 C, and assayed for infectivity intermittently over a period of 2 mo. From an initial level of about 10</span><sup>5</sup><span>&nbsp;PFU per ml, infectivity in the filtered samples uniformly dropped to about 10</span><sup>4</sup><span>&nbsp;PFU per ml. Infectivity in the raw samples declined much more rapidly; infectious virus remaining at the end of 2 mo (ca. 10</span><sup>1</sup><span>&nbsp;PFU per ml) was only about 0.01% of that originally seeded.</span></p>","language":"English","publisher":"BioOne","doi":"10.7589/0090-3558-18.4.437","usgsCitation":"Wolf, K., and Burke, C., 1982, Survival of duck plague virus in water from Lake Andes National Wildlife Refuge, South Dakota: Journal of Wildlife Diseases, v. 18, no. 4, p. 437-440, https://doi.org/10.7589/0090-3558-18.4.437.","productDescription":"4 p.","startPage":"437","endPage":"440","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":480256,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.7589/0090-3558-18.4.437","text":"Publisher Index Page"},{"id":372276,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"South Dakota","county":"Charles Mix County","otherGeospatial":"Lake Andes National Wildlife Refuge","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-98.7959,43.5004],[-98.7094,43.4993],[-98.7069,43.4282],[-98.7058,43.3713],[-98.6769,43.3709],[-98.109,43.1957],[-98.0668,43.1822],[-98.078,43.1679],[-98.0826,43.1625],[-98.0866,43.1562],[-98.0893,43.1508],[-98.0876,43.1439],[-98.0897,43.138],[-98.0962,43.1318],[-98.1026,43.1269],[-98.1053,43.1233],[-98.1055,43.1174],[-98.1038,43.1119],[-98.1027,43.1069],[-98.1047,43.1033],[-98.1094,43.0956],[-98.1099,43.0811],[-98.1098,43.0647],[-98.1034,43.05],[-98.1036,43.0446],[-98.102,43.0386],[-98.1014,43.0359],[-98.0991,43.0317],[-98.0999,43.0268],[-98.105,43.0246],[-98.1094,43.0228],[-98.109,43.0165],[-98.1117,43.0102],[-98.112,43.0033],[-98.1109,42.9988],[-98.1024,42.99],[-98.0964,42.9812],[-98.0916,42.9752],[-98.1004,42.9563],[-98.1007,42.9485],[-98.1058,42.9464],[-98.1059,42.9445],[-98.1041,42.9404],[-98.1036,42.9377],[-98.1062,42.9359],[-98.1087,42.9355],[-98.1099,42.9351],[-98.11,42.9323],[-98.1089,42.93],[-98.1071,42.9277],[-98.1059,42.925],[-98.1073,42.9218],[-98.1093,42.9191],[-98.1106,42.9164],[-98.1107,42.9132],[-98.1126,42.9115],[-98.1139,42.9115],[-98.1164,42.9124],[-98.1201,42.9116],[-98.1209,42.908],[-98.1191,42.9043],[-98.1155,42.9011],[-98.1119,42.8964],[-98.1089,42.8918],[-98.1084,42.8895],[-98.1098,42.8841],[-98.1113,42.8787],[-98.1139,42.8755],[-98.1166,42.8701],[-98.1191,42.8688],[-98.126,42.8694],[-98.1299,42.8649],[-98.1336,42.8645],[-98.1364,42.8578],[-98.1441,42.8506],[-98.1491,42.8512],[-98.1516,42.8526],[-98.1541,42.8526],[-98.156,42.8517],[-98.1573,42.8504],[-98.1573,42.849],[-98.1573,42.8481],[-98.1555,42.8463],[-98.1531,42.8435],[-98.1519,42.8426],[-98.1489,42.8398],[-98.1445,42.8374],[-98.1472,42.8376],[-98.1509,42.8372],[-98.1541,42.8369],[-98.1602,42.8366],[-98.1628,42.8364],[-98.1677,42.8366],[-98.1684,42.8366],[-98.1728,42.8375],[-98.1739,42.8378],[-98.1796,42.8391],[-98.1876,42.8414],[-98.1945,42.8437],[-98.1955,42.8441],[-98.2019,42.8463],[-98.206,42.8479],[-98.2089,42.8492],[-98.2199,42.8553],[-98.2221,42.8565],[-98.2303,42.8604],[-98.2391,42.8645],[-98.2418,42.8656],[-98.2469,42.8671],[-98.2502,42.868],[-98.2524,42.8684],[-98.2592,42.8693],[-98.262,42.8696],[-98.2785,42.873],[-98.2805,42.8736],[-98.3105,42.8823],[-98.3105,42.883],[-98.3248,42.8864],[-98.3348,42.8893],[-98.3446,42.8921],[-98.3497,42.8938],[-98.3566,42.8961],[-98.3658,42.9017],[-98.3706,42.9074],[-98.3711,42.9079],[-98.372,42.9088],[-98.3748,42.9116],[-98.3785,42.9143],[-98.3829,42.917],[-98.3891,42.9199],[-98.3926,42.9211],[-98.397,42.9225],[-98.4008,42.924],[-98.4051,42.926],[-98.4101,42.9268],[-98.4151,42.9275],[-98.4213,42.9285],[-98.4258,42.9285],[-98.4288,42.9288],[-98.4302,42.9289],[-98.437,42.9299],[-98.4382,42.9301],[-98.4432,42.9321],[-98.4444,42.9325],[-98.4492,42.9348],[-98.4523,42.9363],[-98.4534,42.9371],[-98.4567,42.9395],[-98.4573,42.9401],[-98.4614,42.9434],[-98.464,42.9456],[-98.4681,42.9534],[-98.4697,42.9553],[-98.4718,42.9584],[-98.4761,42.9648],[-98.4791,42.9689],[-98.4818,42.9728],[-98.4873,42.9802],[-98.4921,42.9866],[-98.4933,42.988],[-98.4977,42.9943],[-98.5001,42.9977],[-98.5016,43.0125],[-98.5133,43.0283],[-98.5257,43.0412],[-98.5529,43.0567],[-98.5599,43.0578],[-98.5726,43.057],[-98.5929,43.0618],[-98.6232,43.0678],[-98.6751,43.068],[-98.68,43.0689],[-98.6928,43.0794],[-98.7141,43.0943],[-98.7233,43.103],[-98.7336,43.1179],[-98.7399,43.1246],[-98.7478,43.1312],[-98.7572,43.1368],[-98.7885,43.1465],[-98.8229,43.1451],[-98.838,43.1517],[-98.8547,43.1541],[-98.8611,43.1592],[-98.864,43.165],[-98.8649,43.1738],[-98.864,43.1839],[-98.8664,43.1962],[-98.8655,43.2156],[-98.8735,43.2322],[-98.8814,43.2397],[-98.8851,43.2414],[-98.9011,43.2444],[-98.9147,43.2436],[-98.9463,43.2451],[-98.9608,43.2474],[-98.9739,43.2509],[-98.9832,43.2551],[-98.9925,43.2624],[-99.0095,43.2778],[-99.0219,43.2919],[-99.0371,43.2992],[-99.0682,43.3203],[-99.0857,43.3392],[-99.0918,43.3537],[-99.1058,43.3711],[-99.1253,43.3804],[-99.1369,43.3951],[-99.1391,43.4073],[-99.1481,43.4227],[-99.1647,43.4341],[-99.1777,43.438],[-99.1902,43.436],[-99.2503,43.4366],[-99.2803,43.4446],[-99.3045,43.4607],[-99.3095,43.4679],[-99.3091,43.4778],[-99.2919,43.4995],[-98.7959,43.5004]]]},\"properties\":{\"name\":\"Charles Mix\",\"state\":\"SD\"}}]}","volume":"18","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Wolf, Ken","contributorId":106546,"corporation":false,"usgs":true,"family":"Wolf","given":"Ken","email":"","affiliations":[],"preferred":false,"id":782184,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Burke, C.N.","contributorId":96213,"corporation":false,"usgs":true,"family":"Burke","given":"C.N.","email":"","affiliations":[],"preferred":false,"id":782185,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70208403,"text":"70208403 - 1982 - Comment and Reply on ‘Geochemistry of amino acids in sediments from Clear Lake, California’: REPLY","interactions":[],"lastModifiedDate":"2020-02-10T06:41:15","indexId":"70208403","displayToPublicDate":"1982-02-07T11:56:23","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1796,"text":"Geology","active":true,"publicationSubtype":{"id":10}},"title":"Comment and Reply on ‘Geochemistry of amino acids in sediments from Clear Lake, California’: REPLY","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"GSA","doi":"10.1130/0091-7613(1982)10<124b:CAROGO>2.0.CO;2","usgsCitation":"Blunt, D., Kvenvolden, K.A., and Sims, J.D., 1982, Comment and Reply on ‘Geochemistry of amino acids in sediments from Clear Lake, California’: REPLY: Geology, v. 10, no. 3, p. 125-126, https://doi.org/10.1130/0091-7613(1982)10<124b:CAROGO>2.0.CO;2.","productDescription":"2 p.","startPage":"125","endPage":"126","costCenters":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":372138,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","county":"Lake 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D.","contributorId":84759,"corporation":false,"usgs":true,"family":"Blunt","given":"D.","email":"","affiliations":[],"preferred":false,"id":781749,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kvenvolden, Keith A. kkvenvolden@usgs.gov","contributorId":3384,"corporation":false,"usgs":true,"family":"Kvenvolden","given":"Keith","email":"kkvenvolden@usgs.gov","middleInitial":"A.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":781750,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sims, John D.","contributorId":60202,"corporation":false,"usgs":true,"family":"Sims","given":"John","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":781751,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70197817,"text":"70197817 - 1982 - Paleomagnetic study of some Cretaceous and Tertiary sedimentary rocks of the Klamath Mountains province, California","interactions":[],"lastModifiedDate":"2022-12-06T17:46:55.840229","indexId":"70197817","displayToPublicDate":"1982-02-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1796,"text":"Geology","active":true,"publicationSubtype":{"id":10}},"title":"Paleomagnetic study of some Cretaceous and Tertiary sedimentary rocks of the Klamath Mountains province, California","docAbstract":"<p><span>Paleomagnetic investigation of Cretaceous outliers and Tertiary sedimentary strata of the Klamath Mountains province, and of onlapping Cretaceous strata, has shown the rocks to be largely remagnetized. Samples studied are from the Upper Jurassic to Upper Cretaceous Great Valley sequence, Upper Cretaceous Hornbrook Formation, Eocene Montgomery Creek Formation, and Oligocene(?) Weaverville Formation. Cretaceous samples that survived the remagnetization have a mean remanence direction that is very close to the expected direction of the Cretaceous magnetic field at the locality of the Klamath Mountains. Data from both primary and remagnetized samples suggest the possibility of 11.5° ± 15.8° of post-Cretaceous clockwise rotation of the Klamath Mountains province. None of the data from either the primary or remagnetized samples shows evidence of the large amounts (∼ 70°) of clockwise rotation that other workers have measured for the lower Tertiary of the Oregon Coast Range. Our data indicate that the Oregon Coast Range and Klamath Mountains province did not behave as a single rigid block during the early Tertiary. They also suggest that any post-Oligocene rotation of the Klamath Mountains province is less than the approximately 30° post-Oligocene rotation recently proposed for a combined Oregon Coast Range–Klamath Mountains–Cascade Range block.</span></p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0091-7613(1982)10<82:PSOSCA>2.0.CO;2","usgsCitation":"Mankinen, E.A., and Irwin, W., 1982, Paleomagnetic study of some Cretaceous and Tertiary sedimentary rocks of the Klamath Mountains province, California: Geology, v. 10, no. 2, p. 82-87, https://doi.org/10.1130/0091-7613(1982)10<82:PSOSCA>2.0.CO;2.","productDescription":"6 p.","startPage":"82","endPage":"87","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":355231,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Klamath Mountains","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -121.00292610823843,\n              40.15010694428679\n            ],\n            [\n              -121.00292610823843,\n              41.96606648297217\n            ],\n            [\n              -123.73146610355025,\n              41.96606648297217\n            ],\n            [\n              -123.73146610355025,\n              40.15010694428679\n            ],\n            [\n              -121.00292610823843,\n              40.15010694428679\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"10","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Mankinen, Edward A. 0000-0001-7496-2681 emank@usgs.gov","orcid":"https://orcid.org/0000-0001-7496-2681","contributorId":1054,"corporation":false,"usgs":true,"family":"Mankinen","given":"Edward","email":"emank@usgs.gov","middleInitial":"A.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":738642,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Irwin, William P.","contributorId":12889,"corporation":false,"usgs":true,"family":"Irwin","given":"William P.","affiliations":[],"preferred":false,"id":738643,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70011449,"text":"70011449 - 1982 - A new look at the Saturn system: The Voyager 2 images","interactions":[],"lastModifiedDate":"2025-12-22T16:39:57.477017","indexId":"70011449","displayToPublicDate":"1982-01-29T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"A new look at the Saturn system: The Voyager 2 images","docAbstract":"<p><span id=\"_mce_caret\" data-mce-bogus=\"1\" data-mce-type=\"format-caret\"><span>Voyager 2 photography has complemented that of Voyager I in revealing many additional characteristics of Saturn and its satellites and rings. Saturn's atmosphere contains persistent oval cloud features reminiscent of features on Jupiter. Smaller irregular features track out a pattern of zonal winds that is symmetric about Saturn's equator and appears to extend to great depth. Winds are predominantly eastward and reach 500 meters per second at the equator. Titan has several haze layers with significantly varying optical properties and a northern polar \"collar\" that is dark at short wavelengths. Several satellites have been photographed at substantially improved resolution. Enceladus' surface ranges from old, densely cratered terrain to relatively young, uncratered plains crossed by grooves and faults. Tethys has a crater 400 kilometers in diameter whose floor has domed to match Tethys' surface curvature and a deep trench that extends at least 270° around Tethys' circumference. Hyperion is cratered and irregular in shape. Iapetus' bright, trailing hemisphere includes several dark-floored craters, and Phoebe has a very low albedo and rotates in the direction opposite to that of its orbital revolution with a period of 9 hours. Within Saturn's rings, the \"birth\" of a spoke has been observed, and surprising azimuthal and time variability is found in the ringlet structure of the outer B ring. These observations lead to speculations about Saturn's internal structure and about the collisional and thermal history of the rings and satellites.</span></span></p>","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.215.4532.504","issn":"00368075","usgsCitation":"Smith, B., Soderblom, L., Batson, R., Bridges, P., Inge, J., Masursky, H., Shoemaker, E., Beebe, R., Boyce, J., Briggs, G., Bunker, A., Collins, S., Hansen, C., Johnson, T.V., Mitchell, J., Terrile, R., Cook, A., Cuzzi, J., Pollack, J.B., Danielson, G., Ingersoll, A., Davies, M.E., Hunt, G., Morrison, D., Owen, T., Sagan, C., Veverka, J., Strom, R., and Suomi, V., 1982, A new look at the Saturn system: The Voyager 2 images: Science, v. 215, no. 4532, p. 504-537, https://doi.org/10.1126/science.215.4532.504.","productDescription":"34 p.","startPage":"504","endPage":"537","costCenters":[],"links":[{"id":221448,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Enceladus, Hyperion, Iapetus, Phoebe, Saturn, Tethys, Titan","volume":"215","issue":"4532","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e4a5e4b0c8380cd467d5","contributors":{"authors":[{"text":"Smith, B.A.","contributorId":17616,"corporation":false,"usgs":true,"family":"Smith","given":"B.A.","email":"","affiliations":[],"preferred":false,"id":361118,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Soderblom, L.","contributorId":106244,"corporation":false,"usgs":true,"family":"Soderblom","given":"L.","affiliations":[],"preferred":false,"id":361143,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Batson, R.","contributorId":25690,"corporation":false,"usgs":true,"family":"Batson","given":"R.","affiliations":[],"preferred":false,"id":361121,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bridges, P.","contributorId":95198,"corporation":false,"usgs":true,"family":"Bridges","given":"P.","email":"","affiliations":[],"preferred":false,"id":361140,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Inge, J.","contributorId":21687,"corporation":false,"usgs":true,"family":"Inge","given":"J.","email":"","affiliations":[],"preferred":false,"id":361119,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Masursky, H.","contributorId":33823,"corporation":false,"usgs":true,"family":"Masursky","given":"H.","affiliations":[],"preferred":false,"id":361126,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Shoemaker, E.","contributorId":65989,"corporation":false,"usgs":true,"family":"Shoemaker","given":"E.","email":"","affiliations":[],"preferred":false,"id":361131,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Beebe, R.","contributorId":91627,"corporation":false,"usgs":true,"family":"Beebe","given":"R.","email":"","affiliations":[],"preferred":false,"id":361138,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Boyce, J.","contributorId":24918,"corporation":false,"usgs":true,"family":"Boyce","given":"J.","affiliations":[],"preferred":false,"id":361120,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Briggs, G.","contributorId":16567,"corporation":false,"usgs":true,"family":"Briggs","given":"G.","email":"","affiliations":[],"preferred":false,"id":361117,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Bunker, A.","contributorId":84079,"corporation":false,"usgs":true,"family":"Bunker","given":"A.","email":"","affiliations":[],"preferred":false,"id":361137,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Collins, S.A.","contributorId":63947,"corporation":false,"usgs":true,"family":"Collins","given":"S.A.","email":"","affiliations":[],"preferred":false,"id":361130,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Hansen, C.J.","contributorId":72530,"corporation":false,"usgs":true,"family":"Hansen","given":"C.J.","email":"","affiliations":[],"preferred":false,"id":361135,"contributorType":{"id":1,"text":"Authors"},"rank":13},{"text":"Johnson, T. V.","contributorId":79619,"corporation":false,"usgs":false,"family":"Johnson","given":"T.","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":361136,"contributorType":{"id":1,"text":"Authors"},"rank":14},{"text":"Mitchell, J.L.","contributorId":13750,"corporation":false,"usgs":true,"family":"Mitchell","given":"J.L.","email":"","affiliations":[],"preferred":false,"id":361116,"contributorType":{"id":1,"text":"Authors"},"rank":15},{"text":"Terrile, R.J.","contributorId":27194,"corporation":false,"usgs":true,"family":"Terrile","given":"R.J.","email":"","affiliations":[],"preferred":false,"id":361123,"contributorType":{"id":1,"text":"Authors"},"rank":16},{"text":"Cook, A.F. II","contributorId":95184,"corporation":false,"usgs":true,"family":"Cook","given":"A.F.","suffix":"II","email":"","affiliations":[],"preferred":false,"id":361139,"contributorType":{"id":1,"text":"Authors"},"rank":17},{"text":"Cuzzi, J.","contributorId":28366,"corporation":false,"usgs":true,"family":"Cuzzi","given":"J.","affiliations":[],"preferred":false,"id":361125,"contributorType":{"id":1,"text":"Authors"},"rank":18},{"text":"Pollack, James B.","contributorId":12616,"corporation":false,"usgs":true,"family":"Pollack","given":"James","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":361115,"contributorType":{"id":1,"text":"Authors"},"rank":19},{"text":"Danielson, G. E.","contributorId":51890,"corporation":false,"usgs":false,"family":"Danielson","given":"G. 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,{"id":70208103,"text":"70208103 - 1982 - A late Pleistocene glacial chronology for the southern Brooks Range: Stratigraphic record and regional significance","interactions":[],"lastModifiedDate":"2020-01-27T14:52:38","indexId":"70208103","displayToPublicDate":"1982-01-27T14:44:37","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1723,"text":"GSA Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"A late Pleistocene glacial chronology for the southern Brooks Range: Stratigraphic record and regional significance","docAbstract":"<p>Radiocarbon dates from 11 measured sections in the Koyukuk region provide a chronology of the last Pleistocene glaciation. Glaciers were advancing strongly by 24,000 yr ago; they built moraines near the south flank of the Brooks Range, retreated briefly about 22,000 to 20,000 yr B.P., then readvanced at least one more time into their terminal zones. Glaciation was accompanied by alluviation of the Koyukuk and Kobuk drainage systems and by periglacial processes that resemble those taking place today farther north and at higher altitudes. Moraines near the south flank of the range were being revegetated by 13,500 yr B.P. A strong final readvance into end-moraine belts of some northern valleys occurred about 13,000 to 12,500 yr ago, and this event may be synchronous with less extensive glacier readvances in upper valleys of the Koyukuk region. Upper valleys were largely deglaciated by 11,800 yr B.P.</p><p>Dated Stratigraphic sections from the northern Alaska Range show similar ages for initiation and close of glaciation and also suggest a possible interstadial episode about 20,000 yr ago. Scanty records of fluctuations during ice wastage probably reflect the general scarcity of datable wood, peat, and organic soils between about 19,500 and 13,500 yr ago. The Brooks Range and Alaska Range chronologies closely approximate glacial successions determined else-where in eastern Beringia and in Siberia. Advance and retreat of glaciers throughout this region evidently were associated with widespread climatic changes that also controlled the late Wisconsin history of the Laurentide ice sheet.</p><p>The Itkillik II and late Itkillik phases of former usage are part of a single glaciation that was entirely separate from the preceding Itkillik I ice advance. For this reason, the local term \"Walker Lake Glaciation\" is here extended to the last major glaciation of the entire southern Brooks Range, and use of Itkillik phases should be discontinued. The term \"Itkillik Glaciation\" is hereby restricted to the next older ice advance, in accord with its original definition.</p><p>Cold and dry conditions during the last glaciation of eastern Beringia are indicated by (1) relatively small mountain glaciers, (2) slight (200-m) depression of glaciation limits below modern values, (3) periglacial features indicating severe frost action on slopes with little protective plant cover, (4) widespread accretion of eolian sand, (5) low pollen influx rates, (6) scarcity of radiocarbon-datable organic remains, and (7) general absence of carbonaceous paleosols. Plant growth may have been much more restricted than generally believed, with relatively low capacity to support grazing animals and human hunting bands.</p>","language":"English","publisher":"GSA","doi":"10.1130/0016-7606(1982)93<700:ALPGCF>2.0.CO;2","usgsCitation":"Hamilton, T.D., 1982, A late Pleistocene glacial chronology for the southern Brooks Range: Stratigraphic record and regional significance: GSA Bulletin, v. 93, no. 8, p. 700-716, https://doi.org/10.1130/0016-7606(1982)93<700:ALPGCF>2.0.CO;2.","productDescription":"17 p.","startPage":"700","endPage":"716","costCenters":[],"links":[{"id":371601,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Southern Brooks Range","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -156.796875,\n              66.51326044311185\n            ],\n            [\n              -148.88671874999997,\n              66.51326044311185\n            ],\n            [\n              -148.88671874999997,\n              68.65655498475735\n            ],\n            [\n              -156.796875,\n              68.65655498475735\n            ],\n            [\n              -156.796875,\n              66.51326044311185\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"93","issue":"8","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Hamilton, T. D.","contributorId":36921,"corporation":false,"usgs":true,"family":"Hamilton","given":"T.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":780471,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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