{"pageNumber":"5267","pageRowStart":"131650","pageSize":"25","recordCount":184644,"records":[{"id":70011367,"text":"70011367 - 1983 - Tuffaceous sediments as source rocks for uranium: A case study of the White River Formation, Wyoming","interactions":[],"lastModifiedDate":"2025-03-07T16:58:43.013183","indexId":"70011367","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2302,"text":"Journal of Geochemical Exploration","active":true,"publicationSubtype":{"id":10}},"title":"Tuffaceous sediments as source rocks for uranium: A case study of the White River Formation, Wyoming","docAbstract":"<p><span>Fine-grained tuffaceous sediments of the White River Formation (Oligocene) are evaluated as a possible source of uranium for the sedimentary uranium deposits of Wyoming. The evaluation is based upon a model in which volcanic glass is considered to be a major host of uranium and thorium and in which uranium and silica are released during alteration of glass to montmorillonite. The evaluation scheme is applicable to other tuffaceous sediments in similar geologic settings. The average uranium and thorium contents of glass separates and glassy air-fall ashes of the White River Formation are 8 ppm and 22.4 ppm respectively, and these values approximate the average composition of glass deposited in Wyoming basins in Oligocene time. Comparison of these values with the uranium and thorium concentrations in montmorillonite separates indicates little change in thorium concentrations but reductions in uranium concentrations which average 3.3 ppm. In spite of the apparent major removal of uranium during alteration of glass to montmorillonite, whole-rock samples of tuffaceous siltstones show an average uranium loss of only 0.4 ± 0.4 ppm, because of generally small amounts of clay alteration. This conclusion is generated by comparisons between glassy ash and partially altered vitric siltstones, the latter corrected for dilution of glass and clay-altered glass with uranium- and thorium-poor primary and detrital materials. The original volume of the White River Formation is adequate to generate economically significant quantities of mobile uranium, even with such modest losses. Uranium and silica which are mobilized during glass alteration can coprecipitate as uraniferous secondary silica in areas where solutions become silica saturated. These precipitates indicate pathways of ancient, uranium-rich solutions in tuffaceous rocks. Exploration efforts in the White River Formation and underlying units should concentrate on areas where such pathways intercept reducing environments. Intercepts of this type are present at some uranium deposits in the study area and this lends support to a tuffaceous source rock model.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0375-6742(83)90074-2","issn":"03756742","usgsCitation":"Zielinski, R.A., 1983, Tuffaceous sediments as source rocks for uranium: A case study of the White River Formation, Wyoming: Journal of Geochemical Exploration, v. 18, no. 3, p. 285-306, https://doi.org/10.1016/0375-6742(83)90074-2.","productDescription":"22 p.","startPage":"285","endPage":"306","numberOfPages":"22","costCenters":[],"links":[{"id":221231,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"18","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb8b5e4b08c986b327a1b","contributors":{"authors":[{"text":"Zielinski, R. A. 0000-0002-4047-5129","orcid":"https://orcid.org/0000-0002-4047-5129","contributorId":106930,"corporation":false,"usgs":true,"family":"Zielinski","given":"R.","email":"","middleInitial":"A.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":false,"id":360929,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70011365,"text":"70011365 - 1983 - Isotopic and chemical composition of Parbati Valley geothermal discharges, north-west Himalaya, India","interactions":[],"lastModifiedDate":"2024-04-22T11:08:26.53762","indexId":"70011365","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1828,"text":"Geothermics","active":true,"publicationSubtype":{"id":10}},"title":"Isotopic and chemical composition of Parbati Valley geothermal discharges, north-west Himalaya, India","docAbstract":"<p><span>The isotopic compositions of the waters discharged from Parbati Valley geothermal areas indicate a higher altitude meteoric origin, with discharge temperatures reflecting variations in the depth of penetration of the waters to levels heated by the existence of a ‘normal’ geothermal gradient. On the basis of mixing models involving silica, tritium, discharge temperatures and chloride contents, deep equilibration temperatures of 120–140°C were obtained for Manikaran, possibly reaching 160°C at even greater depth. Geothermometers based on sulfate-water&nbsp;</span><sup>18</sup><span>O exchange and gas reactions point to similar temperatures. Exceptionally high helium contents of the discharges correspond to apparent crustal residence times of the waters in the order of 10–100 Ma; relative nitrogen-argon contents support a largely meteoric origin of the waters with a possible fossil brine, but no detectable magmatic component.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0375-6505(83)90030-5","issn":"03756505","usgsCitation":"Giggenbach, W., Gonfiantini, R., Jangi, B., and Truesdell, A., 1983, Isotopic and chemical composition of Parbati Valley geothermal discharges, north-west Himalaya, India: Geothermics, v. 12, no. 2-3, p. 199-222, https://doi.org/10.1016/0375-6505(83)90030-5.","productDescription":"24 p.","startPage":"199","endPage":"222","numberOfPages":"24","costCenters":[],"links":[{"id":221170,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"12","issue":"2-3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3f95e4b0c8380cd64621","contributors":{"authors":[{"text":"Giggenbach, W.F.","contributorId":33054,"corporation":false,"usgs":true,"family":"Giggenbach","given":"W.F.","email":"","affiliations":[],"preferred":false,"id":360924,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gonfiantini, R.","contributorId":33055,"corporation":false,"usgs":true,"family":"Gonfiantini","given":"R.","email":"","affiliations":[],"preferred":false,"id":360925,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Jangi, B.L.","contributorId":13375,"corporation":false,"usgs":true,"family":"Jangi","given":"B.L.","email":"","affiliations":[],"preferred":false,"id":360923,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Truesdell, A.H.","contributorId":52566,"corporation":false,"usgs":false,"family":"Truesdell","given":"A.H.","email":"","affiliations":[{"id":6672,"text":"former: USGS Southwest Biological Science Center, Colorado Plateau Research Station, Flagstaff, AZ. Current address:  TN-SCORE, Univ of Tennessee, Knoxville, TN, e-mail: jennen@gmail.com","active":true,"usgs":false}],"preferred":false,"id":360926,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70011359,"text":"70011359 - 1983 - Distribution of mineral deposits in accreted terranes and cratonal rocks of western United States","interactions":[],"lastModifiedDate":"2023-09-26T13:43:14.493743","indexId":"70011359","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1168,"text":"Canadian Journal of Earth Sciences","active":true,"publicationSubtype":{"id":10}},"title":"Distribution of mineral deposits in accreted terranes and cratonal rocks of western United States","docAbstract":"<p><span>The western margin of the conterminous United States, covering roughly 300 000 mi</span><sup>2</sup><span>&nbsp;(777 000 km</span><sup>2</sup><span>), is an agglomeration of tectonostratigraphic terranes accreted to the North American craton mainly during Mesozoic time. The terranes represent a number of fundamental crustal types: oceanic crust, island-arc crust, mélange, various combinations of the preceding three, batholithic, miogeoclinal, and platform.The distribution patterns of types of mineral deposits show that miogeoclinal terranes of the craton are characterized by replacement and vein-type lead–zinc–silver, skarn tungsten deposits, molybdenum, and tin, whereas accreted terranes contain all the known volcanogenic massive sulfide deposits, all chromite and chert-associated manganese, and all the large gold quartz-vein deposits, except Goldfield, Nevada. Carlin-type disseminated fine-grained gold deposits occur mostly in windows of Paleozoic miogeoclinal rocks in Nevada, but the only known fine-grained gold deposit in California is in very youthful volcanic rocks overlying oceanic-crust terrane. Large bedded-type barite deposits, although in the same general area and showing the same general trend as fine disseminated gold deposits in Nevada, are in allochthonous oceanic terrane. Mercury and antimony are dominantly in accreted terranes but antimony, in particular, also forms important deposits in cratonal rocks. Most of the large iron deposits are in the craton but a few are in accreted island-arc terranes.</span></p>","language":"English","publisher":"Canadian Science Publishing","doi":"10.1139/e83-092","issn":"00084077","usgsCitation":"Albers, J.P., 1983, Distribution of mineral deposits in accreted terranes and cratonal rocks of western United States: Canadian Journal of Earth Sciences, v. 20, no. 6, p. 1019-1029, https://doi.org/10.1139/e83-092.","productDescription":"11 p.","startPage":"1019","endPage":"1029","costCenters":[],"links":[{"id":221108,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California, Idaho, Nevada, Oregon, Utah, Washington","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              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P.","contributorId":81505,"corporation":false,"usgs":true,"family":"Albers","given":"J.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":360910,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70011357,"text":"70011357 - 1983 - Location of internal hydrogen atoms in the paradodecatungstate polyanion by neutron diffraction","interactions":[],"lastModifiedDate":"2024-05-14T15:03:55.319616","indexId":"70011357","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2519,"text":"Journal of the American Chemical Society","active":true,"publicationSubtype":{"id":10}},"title":"Location of internal hydrogen atoms in the paradodecatungstate polyanion by neutron diffraction","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"ACS Publications","doi":"10.1021/ja00352a054","issn":"00027863","usgsCitation":"Evans, H.T., and Prince, E., 1983, Location of internal hydrogen atoms in the paradodecatungstate polyanion by neutron diffraction: Journal of the American Chemical Society, v. 105, no. 14, p. 4838-4839, https://doi.org/10.1021/ja00352a054.","productDescription":"2 p.","startPage":"4838","endPage":"4839","numberOfPages":"2","costCenters":[],"links":[{"id":221106,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"105","issue":"14","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","scienceBaseUri":"505a4917e4b0c8380cd68361","contributors":{"authors":[{"text":"Evans, H. T. Jr.","contributorId":41859,"corporation":false,"usgs":true,"family":"Evans","given":"H.","suffix":"Jr.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":360907,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Prince, E.","contributorId":100120,"corporation":false,"usgs":true,"family":"Prince","given":"E.","email":"","affiliations":[],"preferred":false,"id":360908,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70011356,"text":"70011356 - 1983 - Taeniolite, an uncommon lithium-mica from Coyote Peak, Humboldt County, California.","interactions":[],"lastModifiedDate":"2012-03-12T17:18:26","indexId":"70011356","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2749,"text":"Mineralogical Record","active":true,"publicationSubtype":{"id":10}},"title":"Taeniolite, an uncommon lithium-mica from Coyote Peak, Humboldt County, California.","docAbstract":"Taeniolite has been found in a late pegmatitic clot in a mafic alkalic diatreme at Coyote Peak; associated species are natrolite, pectolite, aegirine, barytolamprophyllite, rasvumite and sphalerite. The taeniolite is green-brown with sp. gr. (meas.) 2.85(1) and H. 31/2. Optically it is biaxial (-) with alpha 1.541(2), beta = gamma 1.570(2), 2V approx 0o and moderate pleochroism with gamma = beta reddish-brown, alpha pale greenish brown. Single-crystal precession photographs show it to be of the 1M type, with a 5.254(2), b 9.110(4), c 10.187(2) A, beta 99.85(4)o and V = 480.4(1) A3. Combined microprobe and ion probe analyses gave SiO2 53.5, Al2O3 3.00, TiO2 1.06, FeO 3.35, MnO 0.21, MgO 18.3, Li2O 2.4, K2O 11.3, Na2O 0.27, F 6.3 = 99.69; SrO and BaO are both <0.04 wt.%; B, Be, Ca and Cl were not detected. Assuming (F + OH) = 2 and assigning 1.30 wt.% H2O gives 409(K1.01Na0.04)(Al0.01Ti0.06Fe2+0.20Mn0.01Mg1.92Li0.68)(Si3.76Al0.24)O10- (F1.40OH0.60).-G.W.R.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Mineralogical Record","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"00264628","usgsCitation":"Erd, R.C., Czamanske, G., and Meyer, C., 1983, Taeniolite, an uncommon lithium-mica from Coyote Peak, Humboldt County, California.: Mineralogical Record, v. 14, no. 1, p. 39-40.","startPage":"39","endPage":"40","numberOfPages":"2","costCenters":[],"links":[{"id":221042,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"14","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505ba3b1e4b08c986b31fe11","contributors":{"authors":[{"text":"Erd, Richard C.","contributorId":89899,"corporation":false,"usgs":true,"family":"Erd","given":"Richard","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":360905,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Czamanske, G.K.","contributorId":26300,"corporation":false,"usgs":true,"family":"Czamanske","given":"G.K.","email":"","affiliations":[],"preferred":false,"id":360904,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Meyer, C.E.","contributorId":104023,"corporation":false,"usgs":true,"family":"Meyer","given":"C.E.","email":"","affiliations":[],"preferred":false,"id":360906,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70011354,"text":"70011354 - 1983 - A quantitative comparison of Soil Development in four climatic regimes","interactions":[],"lastModifiedDate":"2013-01-26T15:53:47","indexId":"70011354","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","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":"A quantitative comparison of Soil Development in four climatic regimes","docAbstract":"A new quantitative Soil Development Index based on field data has been applied to chronosequences formed under different climatic regimes. The four soil chronosequences, developed primarily on sandy deposits, have some numeric age control and are located in xeric-inland (Merced, Calif.), xeric-coastal (Ventura, Calif.), aridic (Las Cruces, N. Mex.), and udic (Susquehanna Valley, Pa.) soil-moisture regimes. To quantify field properties, points are assigned for developmental increases in soil properties in comparison to the parent material. Currently ten soil-field properties are quantified and normalized for each horizon in a given chronosequence, including two new properties for carbonate-rich soils in addition to the eight properties previously defined. When individual properties or the combined indexes are plotted as a function of numeric age, rates of soil development can be compared in different climates. The results demonstrate that (1) the Soil Development Index can be applied to very different soil types, (2) many field properties develop systematically in different climatic regimes, (3) certain properties appear to have similar rates of development in different climates, and (4) the Profile Index that combines different field properties increases significantly with age and appears to develop at similar rates in different climates. The Soil Development Index can serve as a preliminary guide to soil age where other age control is lacking and can be used to correlate deposits of different geographical and climatic regions. ?? 1983.","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(83)90017-0","issn":"00335894","usgsCitation":"Harden, J., and Taylor, E.M., 1983, A quantitative comparison of Soil Development in four climatic regimes: Quaternary Research, v. 20, no. 3, p. 342-359, https://doi.org/10.1016/0033-5894(83)90017-0.","startPage":"342","endPage":"359","numberOfPages":"18","costCenters":[],"links":[{"id":266561,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0033-5894(83)90017-0"},{"id":221040,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"20","issue":"3","noUsgsAuthors":false,"publicationDate":"2017-01-20","publicationStatus":"PW","scienceBaseUri":"5059e524e4b0c8380cd46b5f","contributors":{"authors":[{"text":"Harden, J.W. 0000-0002-6570-8259","orcid":"https://orcid.org/0000-0002-6570-8259","contributorId":38585,"corporation":false,"usgs":true,"family":"Harden","given":"J.W.","affiliations":[],"preferred":false,"id":360900,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Taylor, E. M.","contributorId":55842,"corporation":false,"usgs":true,"family":"Taylor","given":"E.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":360901,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70011353,"text":"70011353 - 1983 - Correlation of Alaskan varve thickness with climatic parameters, and use in paleoclimatic reconstruction","interactions":[],"lastModifiedDate":"2013-01-26T15:52:37","indexId":"70011353","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","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":"Correlation of Alaskan varve thickness with climatic parameters, and use in paleoclimatic reconstruction","docAbstract":"The thickness of varves in the sediments of Skilak Lake, Alaska, are correlated with the mean annual temperature (r = 0.574), inversely correlated with the mean annual cumulative snowfall (r = -0.794), and not correlated with the mean annual precipitation (r = 0.202) of the southern Alaska climatological division for the years 1907-1934 A.D. Varve thickness in Skilak Lake is sensitive to annual temperature and snowfall because Skilak Glacier, the dominant source of sediment for Skilak Lake, is sensitive to these climatic parameters. Trends of varve thickness are well correlated with trends of mean annual cumulative snowfall (r = -0.902) of the southern Alaska climatological division and with trends of mean annual temperature of the southern (r = 0.831) and northern (r = 0.786) Alaska climatological divisions. Trends of varve thickness also correlate with trends of annual temperature in Seattle and North Head, Washington (r = 0.632 and 0.850, respectively). Comparisons of trends of varve thickness with trends of annual temperature in California, Oregon, and Washington suggest no widespread regional correlation. Trends of annual snowfall in the southern Alaska climatological division and trends of annual temperature in the southern and northern Alaska climatological divisions are reconstructed for the years 1700-1906 A.D. Climatic reconstructions on the basis of varve thickness in Skilak Lake utilize equations derived from the regression of series of smoothed climatological data on series of smoothed varve thickness. Reconstruction of trends of mean annual cunulative snowfall in the southern Alaska climatological division suggests that snowfall during the 1700s and 1800s was much greater than that during the early and mid-1900s. The periods 1770-1790 and 1890-1906 show marked decreases in the mean annual snowfall. Reconstructed trends of the annual temperature of the northern and southern Alaska climatological divisions suggest that annual temperatures during the 1700s and 1800s were lower than those of the early and mid-1900s. Two periods of relatively high annual temperatures coincide with the periods of low annual snowfall thus determined. ?? 1983.","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(83)90015-7","issn":"00335894","usgsCitation":"Perkins, J., and Sims, J., 1983, Correlation of Alaskan varve thickness with climatic parameters, and use in paleoclimatic reconstruction: Quaternary Research, v. 20, no. 3, p. 308-321, https://doi.org/10.1016/0033-5894(83)90015-7.","startPage":"308","endPage":"321","numberOfPages":"14","costCenters":[],"links":[{"id":266560,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0033-5894(83)90015-7"},{"id":221039,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"20","issue":"3","noUsgsAuthors":false,"publicationDate":"2017-01-20","publicationStatus":"PW","scienceBaseUri":"5059fc2ee4b0c8380cd4e175","contributors":{"authors":[{"text":"Perkins, J.A.","contributorId":49769,"corporation":false,"usgs":true,"family":"Perkins","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":360899,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sims, J.D.","contributorId":9230,"corporation":false,"usgs":false,"family":"Sims","given":"J.D.","email":"","affiliations":[],"preferred":false,"id":360898,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70011352,"text":"70011352 - 1983 - Reinterpretation of the exposed record of the last two cycles of Lake Bonneville, Western United States","interactions":[],"lastModifiedDate":"2013-01-26T15:51:48","indexId":"70011352","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","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":"Reinterpretation of the exposed record of the last two cycles of Lake Bonneville, Western United States","docAbstract":"A substantially modified history of the last two cycles of Lake Bonneville is proposed. The Bonneville lake cycle began prior to 26,000 yr B.P.; the lake reached the Bonneville shoreline about 16,000 yr B.P. Poor dating control limits our knowledge of the timing of subsequent events. Lake level was maintained at the Bonneville shoreline until about 15,000 yr B.P., or somewhat later, when catastrophic downcutting of the outlet caused a rapid drop of 100 m. The Provo shoreline was formed as rates of isostatic uplift due to this unloading slowed. By 13,000 yr B.P., the lake had fallen below the Provo level and reached one close to that of Great Salt Lake by 11,000 yr B.P. Deposits of the Little Valley lake cycle are identified by their position below a marked unconformity and by amino acid ratios of their fossil gastropods. The maximum level of the Little Valley lake was well below the Bonneville shoreline. Based on degree of soil development and other evidence, the Little Valley lake cycle may be equivalent in age to marine oxygenisotope stage 6. The proposed lake history has climatic implications for the region. First, because the fluctuations of Lake Bonneville and Lake Lahontan during the last cycle of each were apparently out of phase, there may have been significant local differences in the timing and character of late Pleistocene climate changes in the Great Basin. Second, although the Bonneville and Little Valley lake cycles were broadly synchronous with maximum episodes of glaciation, environmental conditions necessary to generate large lakes did not exist during early Wisconsin time. ?? 1983.","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(83)90013-3","issn":"00335894","usgsCitation":"Scott, W.E., McCoy, W., Shroba, R., and Rubin, M., 1983, Reinterpretation of the exposed record of the last two cycles of Lake Bonneville, Western United States: Quaternary Research, v. 20, no. 3, p. 261-285, https://doi.org/10.1016/0033-5894(83)90013-3.","startPage":"261","endPage":"285","numberOfPages":"25","costCenters":[],"links":[{"id":266559,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0033-5894(83)90013-3"},{"id":220975,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"20","issue":"3","noUsgsAuthors":false,"publicationDate":"2017-01-20","publicationStatus":"PW","scienceBaseUri":"50e4a60ce4b0e8fec6cdc086","contributors":{"authors":[{"text":"Scott, W. E.","contributorId":22773,"corporation":false,"usgs":true,"family":"Scott","given":"W.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":360895,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McCoy, W.D.","contributorId":19165,"corporation":false,"usgs":true,"family":"McCoy","given":"W.D.","email":"","affiliations":[],"preferred":false,"id":360894,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Shroba, R. R.","contributorId":44133,"corporation":false,"usgs":true,"family":"Shroba","given":"R. R.","affiliations":[],"preferred":false,"id":360896,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Rubin, M.","contributorId":88079,"corporation":false,"usgs":true,"family":"Rubin","given":"M.","email":"","affiliations":[],"preferred":false,"id":360897,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70011351,"text":"70011351 - 1983 - Can the earth be dated from decay of its magnetic field?.","interactions":[],"lastModifiedDate":"2024-05-07T16:38:26.184541","indexId":"70011351","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2307,"text":"Journal of Geological Education","active":true,"publicationSubtype":{"id":10}},"title":"Can the earth be dated from decay of its magnetic field?.","docAbstract":"<p class=\"first\">Thomas G. Barnes, Emeritus Professor of Physics at the University of Texas, El Paso, and a creationist, argues that the geomagnetic field was created by unknown processes at the time of creation of the earth and has been decaying irreversibly and exponentially, with a half-life of about 1400 years, since then. He calculates that the field would have been impossibly large in 8000 B.C. and concludes that the earth, therefore, is less than 10,000 years old. He denies that the earth's field has reversed polarity in the past, and attempts to refute the dynamo theory of the origin of the field. Barnes' arguments and conclusions are commonly cited in creationist literature as definitive proof that the earth is very young. Barnes is wrong, and has ignored or misrepresented much of the data on the earth's magnetic field.</p><p>Barnes calculations are based on observatory measurements showing that the earth's dipole field strength has decreased since 1835. But these same measurements also show a corresponding increase in the strength of the nondipole field so that the total field energy external to the core has remained about constant. Paleomagnetic evidence shows that the earth's field has existed for more than three billion years, and that the dipole field both fluctuates in strength and irregularly reverses polarity. The earth's field is generated by a fluid dynamo in the iron-nickel core; all of the elements necessary for a dynamo, including fluid motion and energy sources, are present. Contrary to Barnes' assertions, there are no theoretical reasons why a dynamo cannot exist in the earth.</p><p class=\"last\">There are no properties of the magnetid field that can be used to place an upper limit on the earth's age.</p>","language":"English","publisher":"Taylor & Francis","doi":"10.5408/0022-1368-31.2.124","issn":"00221368","usgsCitation":"Dalrymple, G.B., 1983, Can the earth be dated from decay of its magnetic field?.: Journal of Geological Education, v. 31, no. 2, p. 124-133, https://doi.org/10.5408/0022-1368-31.2.124.","productDescription":"10 p.","startPage":"124","endPage":"133","numberOfPages":"10","costCenters":[],"links":[{"id":480230,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.5408/0022-1368-31.2.124","text":"Publisher Index Page"},{"id":220974,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"31","issue":"2","noUsgsAuthors":false,"publicationDate":"2018-02-13","publicationStatus":"PW","scienceBaseUri":"5059f33be4b0c8380cd4b69b","contributors":{"authors":[{"text":"Dalrymple, G. B.","contributorId":10407,"corporation":false,"usgs":true,"family":"Dalrymple","given":"G.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":360893,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70011349,"text":"70011349 - 1983 - Introduction: seismology and earthquake engineering in Central and South America.","interactions":[],"lastModifiedDate":"2012-03-12T17:18:28","indexId":"70011349","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1435,"text":"Earthquake Information Bulletin (USGS)","active":true,"publicationSubtype":{"id":10}},"title":"Introduction: seismology and earthquake engineering in Central and South America.","docAbstract":"Reports the state-of-the-art in seismology and earthquake engineering that is being advanced in Central and South America. Provides basic information on seismological station locations in Latin America and some of the programmes in strong-motion seismology, as well as some of the organizations involved in these activities.-from Author","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Earthquake Information Bulletin (USGS)","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Espinosa, A.F., 1983, Introduction: seismology and earthquake engineering in Central and South America.: Earthquake Information Bulletin (USGS), v. 15, no. 1, p. 4-6.","startPage":"4","endPage":"6","numberOfPages":"3","costCenters":[],"links":[{"id":220972,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"15","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3e0ee4b0c8380cd63a7c","contributors":{"authors":[{"text":"Espinosa, A. F.","contributorId":63782,"corporation":false,"usgs":true,"family":"Espinosa","given":"A.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":360889,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1014375,"text":"1014375 - 1983 - Branched-chain amino acid aminotransferase activity in the tissues of lake trout","interactions":[],"lastModifiedDate":"2017-05-06T14:01:27","indexId":"1014375","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5296,"text":"Comparative Biochemistry and Physiology, Part B: Comparative Biochemistry","active":false,"publicationSubtype":{"id":10}},"title":"Branched-chain amino acid aminotransferase activity in the tissues of lake trout","docAbstract":"<p></p><p>1. The enzyme branched-chain amino acid aminotransferase (BCAT) was found in five tissues of fingerling lake trout, <i>Salvelinus namaycush</i>, (listed in order of decreasing tissue specific activity): posterior kidney, skeletal muscle, gill, liver, and anterior kidney.</p><p>2. This pattern is consistent with that found in other animals.</p><p>3. The results of this study seem to indicate that BCAT in the liver of lake trout has a higher specific activity than that of the rat and that the specific activity is higher in both the liver and skeletal muscle than it is in these organs of the chick.</p><p></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0305-0491(83)90270-5","usgsCitation":"Hughes, S.G., Rumsey, G.L., and Nesheim, M., 1983, Branched-chain amino acid aminotransferase activity in the tissues of lake trout: Comparative Biochemistry and Physiology, Part B: Comparative Biochemistry, v. 76, no. 3, p. 429-431, https://doi.org/10.1016/0305-0491(83)90270-5.","productDescription":"3 p.","startPage":"429","endPage":"431","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":129552,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"76","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fcdaf","contributors":{"authors":[{"text":"Hughes, S. G.","contributorId":92200,"corporation":false,"usgs":true,"family":"Hughes","given":"S.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":320278,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rumsey, G. L.","contributorId":80604,"corporation":false,"usgs":true,"family":"Rumsey","given":"G.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":320277,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Nesheim, M.C.","contributorId":29357,"corporation":false,"usgs":true,"family":"Nesheim","given":"M.C.","email":"","affiliations":[],"preferred":false,"id":320276,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70011348,"text":"70011348 - 1983 - Submarine hydrothermal metamorphism of the Del Puerto ophiolite, California","interactions":[],"lastModifiedDate":"2023-02-08T17:56:18.22437","indexId":"70011348","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":732,"text":"American Journal of Science","active":true,"publicationSubtype":{"id":10}},"title":"Submarine hydrothermal metamorphism of the Del Puerto ophiolite, California","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"American Journal of Science","doi":"10.2475/ajs.283.4.289","usgsCitation":"Evarts, R.C., and Schiffman, P., 1983, Submarine hydrothermal metamorphism of the Del Puerto ophiolite, California: American Journal of Science, v. 283, no. 4, p. 289-340, https://doi.org/10.2475/ajs.283.4.289.","productDescription":"52 p.","startPage":"289","endPage":"340","numberOfPages":"52","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":480234,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.2475/ajs.283.4.289","text":"Publisher Index Page"},{"id":220901,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Del Puerto ophiolite","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -121.30479833122857,\n              37.513758245858384\n            ],\n            [\n              -121.30479833122857,\n              37.434575381298416\n            ],\n            [\n              -121.18543480940622,\n              37.434575381298416\n            ],\n            [\n              -121.18543480940622,\n              37.513758245858384\n            ],\n            [\n              -121.30479833122857,\n              37.513758245858384\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"283","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b9d29e4b08c986b31d69c","contributors":{"authors":[{"text":"Evarts, Russell C. revarts@usgs.gov","contributorId":1974,"corporation":false,"usgs":true,"family":"Evarts","given":"Russell","email":"revarts@usgs.gov","middleInitial":"C.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":360888,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schiffman, Peter","contributorId":40119,"corporation":false,"usgs":true,"family":"Schiffman","given":"Peter","email":"","affiliations":[],"preferred":false,"id":360887,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70011344,"text":"70011344 - 1983 - Subdivision of the Mg-suite noritic rocks into Mg-gabbronorites and Mg-norites","interactions":[],"lastModifiedDate":"2024-06-28T16:36:33.92881","indexId":"70011344","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":6453,"text":"Journal of Geophysical Research Solid Earth","active":true,"publicationSubtype":{"id":10}},"title":"Subdivision of the Mg-suite noritic rocks into Mg-gabbronorites and Mg-norites","docAbstract":"<p><span>Mg-suite noritic rocks can be divided into two groups, the Mg-gabbronorites and the Mg-norites. The rocks of these groups differ in ratios of high-Ca pyroxene to total pyroxene, compositions of pyroxene and plagioclase, assemblages of Ti-, Nb-, and Zr-bearing minerals, compositions of chrome spinel, bulk-rock Ti/Sm and Sc/Sm, and measured ages. The two groups probably crystallized from different types of parent magmas. Two hypotheses are offered for the differences in composition of the parent magmas. One hypothesis ascribes the differences to compositional heterogeneity of the mantle source areas. The other hypothesis ascribes the differences to variations in extent of partial melting of the mantle source regions and variations in extent of assimilation of the anorthosite and the highly differentiated residual liquid that were produced during the primordial lunar differentiation.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/JB088iS02p0A603","issn":"01480227","usgsCitation":"James, O., and Flohr, M., 1983, Subdivision of the Mg-suite noritic rocks into Mg-gabbronorites and Mg-norites: Journal of Geophysical Research Solid Earth, v. 88, no. S02, p. A603-A614, https://doi.org/10.1029/JB088iS02p0A603.","productDescription":"12 p.","startPage":"A603","endPage":"A614","costCenters":[],"links":[{"id":220897,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"88","issue":"S02","noUsgsAuthors":false,"publicationDate":"2012-09-21","publicationStatus":"PW","scienceBaseUri":"505b9d0be4b08c986b31d5ef","contributors":{"authors":[{"text":"James, O.B.","contributorId":100526,"corporation":false,"usgs":true,"family":"James","given":"O.B.","email":"","affiliations":[],"preferred":false,"id":360883,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Flohr, M.K.","contributorId":80012,"corporation":false,"usgs":true,"family":"Flohr","given":"M.K.","email":"","affiliations":[],"preferred":false,"id":360882,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70011342,"text":"70011342 - 1983 - Nucleation and growth of strike slip faults in granite","interactions":[],"lastModifiedDate":"2024-06-28T16:39:27.307299","indexId":"70011342","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":6453,"text":"Journal of Geophysical Research Solid Earth","active":true,"publicationSubtype":{"id":10}},"title":"Nucleation and growth of strike slip faults in granite","docAbstract":"<p><span>Fractures within granodiorite of the central Sierra Nevada, California, were studied to elucidate the mechanics of faulting in crystalline rocks, with emphasis on the nucleation of new fault surfaces and their subsequent propagation and growth. Within the study area the fractures form a single, subparallel array which strikes N50°–70°E and dips steeply to the south. Some of these fractures are identified as joints because displacements across the fracture surfaces exhibit dilation but no slip. The joints are filled with undeformed minerals, including epidote and chlorite. Other fractures are identified as small faults because they display left-lateral strike slip separations of up to 2 m. Slickensides, developed on fault surfaces, plunge 0°–20° to the east. The faults occur parallel to, and in the same outcrop with, the joints. The faults are filled with epidote, chlorite, and quartz, which exhibit textural evidence of shear deformation. These observations indicate that the strike slip faults nucleated on earlier formed, mineral-filled joints. Secondary, dilational fractures propagated from near the ends of some small faults contemporaneously with the left-lateral slip on the faults. These fractures trend 25°±10° from the fault planes, parallel to the direction of inferred local maximum compressive stress. The faults did not propagate into intact rock in their own planes as shear fractures. Rather, adjacent faults were linked together by secondary, dilational fractures. Extensive secondary fracturing between faults produced larger fault zones that accommodate 10–100 m of left-lateral slip. As deformation progressed, faulting evolved from relatively short, closely spaced faults to longer, more widely spaced fault zones.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/JB088iB01p00555","issn":"01480227","usgsCitation":"Segall, P., and Pollard, D., 1983, Nucleation and growth of strike slip faults in granite: Journal of Geophysical Research Solid Earth, v. 88, no. B1, p. 555-568, https://doi.org/10.1029/JB088iB01p00555.","productDescription":"14 p.","startPage":"555","endPage":"568","numberOfPages":"14","costCenters":[],"links":[{"id":220833,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"88","issue":"B1","noUsgsAuthors":false,"publicationDate":"2012-09-20","publicationStatus":"PW","scienceBaseUri":"505a68d5e4b0c8380cd73a06","contributors":{"authors":[{"text":"Segall, P.","contributorId":44231,"corporation":false,"usgs":false,"family":"Segall","given":"P.","affiliations":[],"preferred":false,"id":360880,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pollard, D.P.","contributorId":7000,"corporation":false,"usgs":true,"family":"Pollard","given":"D.P.","email":"","affiliations":[],"preferred":false,"id":360879,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70011340,"text":"70011340 - 1983 - Variable tolerance to copper in two species from San Francisco Bay","interactions":[],"lastModifiedDate":"2020-01-26T09:47:13","indexId":"70011340","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2664,"text":"Marine Environmental Research","active":true,"publicationSubtype":{"id":10}},"title":"Variable tolerance to copper in two species from San Francisco Bay","docAbstract":"<p>In static toxicity experiments, tolerance to soluble Cu of the bivalve, Macoma balthica, and the copepod, Acartia clausi, varied substantially among populations sampled within San Francisco Bay. Intraspecific tolerance differed ten-fold or more for both species over relatively small distances, suggesting geographical isolation of populations is not a prerequisite for the development of intraspecific differences in tolerance by aquatic organisms.In static toxicity experiments, tolerance to soluble Cu of the bivalve, Macoma balthica, and the copepod, Acartia clausi, varied substantially among populations sampled within San Francisco Bay. Intraspecific tolerance differed ten-fold or more for both species over relatively small distances, suggesting geographical isolation of populations is not a prerequisite for the development of intraspecific differences in tolerance by aquatic organisms.&nbsp;</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0141-1136(83)90002-8","issn":"01411136","usgsCitation":"Luoma, S.N., Cain, D., Ho, K., and Hutchinson, A., 1983, Variable tolerance to copper in two species from San Francisco Bay: Marine Environmental Research, v. 10, no. 4, p. 209-222, https://doi.org/10.1016/0141-1136(83)90002-8.","productDescription":"14 p.","startPage":"209","endPage":"222","numberOfPages":"14","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":220831,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California ","otherGeospatial":"San Francisco Bay","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -123.37646484374999,\n              37.07271048132943\n            ],\n            [\n              -121.728515625,\n              37.07271048132943\n            ],\n            [\n              -121.728515625,\n              38.41055825094609\n            ],\n            [\n              -123.37646484374999,\n              38.41055825094609\n            ],\n            [\n              -123.37646484374999,\n              37.07271048132943\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"10","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bc148e4b08c986b32a4ef","contributors":{"authors":[{"text":"Luoma, Samuel N. 0000-0001-5443-5091 snluoma@usgs.gov","orcid":"https://orcid.org/0000-0001-5443-5091","contributorId":2287,"corporation":false,"usgs":true,"family":"Luoma","given":"Samuel","email":"snluoma@usgs.gov","middleInitial":"N.","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":780293,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cain, D.J.","contributorId":68329,"corporation":false,"usgs":true,"family":"Cain","given":"D.J.","email":"","affiliations":[],"preferred":false,"id":360875,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ho, K.","contributorId":18509,"corporation":false,"usgs":true,"family":"Ho","given":"K.","email":"","affiliations":[],"preferred":false,"id":360874,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hutchinson, A.","contributorId":94035,"corporation":false,"usgs":true,"family":"Hutchinson","given":"A.","email":"","affiliations":[],"preferred":false,"id":360877,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70011336,"text":"70011336 - 1983 - Characteristics of resuspended sediment from Georges Bank collected with a sediment trap","interactions":[],"lastModifiedDate":"2017-11-05T09:19:33","indexId":"70011336","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1587,"text":"Estuarine, Coastal and Shelf Science","active":true,"publicationSubtype":{"id":10}},"title":"Characteristics of resuspended sediment from Georges Bank collected with a sediment trap","docAbstract":"<p>A sediment trap was deployed 3 m from the bottom at a water depth of 62 m on the southern flank of Georges Bank (41°02·2′N, 67°33·5′W) from 30 September 1978 to 10 March 1979 to qualitatively determine the size of sediments resuspended from the bottom by winter storms and to determine if seasonal changes in the phytoplankton could be observed in the trapped sediment.</p><p>Bulk X-ray analyses of the trapped sediment showed layers of distinctly different textures preserved in the collection vessel. The median grain size of sampled layers ranged from 2·7 to 6·5 φ (fine sand to silt), but all layers contained a pronounced mode in the 3 φ (fine sand) range. Nine layers containing relatively large amounts of sand were present. The sand content was 75% in the coarest layers and about 32% in the fine layers. The median grain size of bottom sediments at the deployment site was considerably coarser than the trap samples, although the dominant grain size was also 3 φ.</p><p>Average bottom-current speeds during the deployment period were about 30 cm s<sup>−1</sup><span>&nbsp;</span>with a range of 10 to 50 cm s<sup>−1</sup>. Bottom stress, computed from the observed currents and waves, suggest that 11 storms caused sufficient stress to resuspend 3 φ-sized sediments, in good agreement with the nine layers of relatively coarse sediments collected in the trap. Surface waves had to be included in the calculation of bottom stress because the bottom currents alone were insufficient to cause the resuspension of 3 φ-sized sediment.</p><p>The trapped sediments contain numerous diatoms and coccoliths that are typical of late fall and winter assemblages. No clear seasonal difference in the flora was noted among sampled layers, probably due to the large influx of resuspended material and a reduced primary flux during this period. An undescribed species of<span>&nbsp;</span><i>Thalassiosira</i><span>&nbsp;</span>(G. Fryxell, personal communication), and siliceous scales of unknown systematic position were observed at all levels.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0272-7714(83)90004-5","issn":"02727714","usgsCitation":"Parmenter, C., Bothner, M., and Butman, B., 1983, Characteristics of resuspended sediment from Georges Bank collected with a sediment trap: Estuarine, Coastal and Shelf Science, v. 17, no. 5, p. 521-533, https://doi.org/10.1016/0272-7714(83)90004-5.","productDescription":"13 p.","startPage":"521","endPage":"533","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":220764,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","otherGeospatial":"Georges Bank ","volume":"17","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f49de4b0c8380cd4be05","contributors":{"authors":[{"text":"Parmenter, C.M.","contributorId":43740,"corporation":false,"usgs":true,"family":"Parmenter","given":"C.M.","email":"","affiliations":[],"preferred":false,"id":360862,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bothner, Michael H. mbothner@usgs.gov","contributorId":139855,"corporation":false,"usgs":true,"family":"Bothner","given":"Michael H.","email":"mbothner@usgs.gov","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":360863,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Butman, B.","contributorId":85580,"corporation":false,"usgs":true,"family":"Butman","given":"B.","email":"","affiliations":[],"preferred":false,"id":360864,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70011335,"text":"70011335 - 1983 - Nonequilibrium models for predicting forms of precipitated manganese oxides","interactions":[],"lastModifiedDate":"2020-01-20T19:56:53","indexId":"70011335","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1759,"text":"Geochimica et Cosmochimica Acta","active":true,"publicationSubtype":{"id":10}},"title":"Nonequilibrium models for predicting forms of precipitated manganese oxides","docAbstract":"<p>Manganese oxides precipitated by bubbling air through 0.01 molar solutions of MnCl<sub>2</sub>, Mn(NO<sub>3</sub>)<sub>2</sub>, MnSO<sub>4</sub>, or Mn(ClO<sub>4</sub>)<sub>2</sub><span>&nbsp;</span>at a constantly maintained pH of 8.5 to 9.5 at temperatures of 25°C or higher consisted mainly of hausmannite, Mn<sub>3</sub>O<sub>4</sub>. At temperatures near 0°C, but with other conditions the same, the product is feitknechtite, βMnOOH, except that if the initial solution is MnSO<sub>4</sub><span>&nbsp;</span>and the temperature is near 0°C the product is a mixture of manganite, γMnOOH and groutite, αMnOOH.</p><p>All these oxides are metastable in aerated solution and alter by irreversible processes to more highly oxidized species during aging. A two-step nonequilibrium thermodynamic model predicts that the least stable species, βMnOOH, should be most readily converted to MnO<sub>2</sub>. Some preparations of βMnOOH aged in their native solution at 5°C attained a manganese oxidation state of +3.3 or more after 7 months. Hausmannite aged at 25°C altered to γMnOOH. The latter is more stable than a or βMnOOH, and manganese oxidation states above 3.0 were not reached in hausmannite precipitates during 4 months of aging. Initial precipitation of MnCO<sub>3</sub><span>&nbsp;</span>rather than a form of oxide is likely only where oxygen availability is very low.</p><p>Composition of solutions and oxidation state and morphology of solids were determined during the aging process by chemical analyses, X-ray and electron diffraction and transmission electron micrographs.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(83)90219-3","issn":"00167037","usgsCitation":"Hem, J., and Lind, C.J., 1983, Nonequilibrium models for predicting forms of precipitated manganese oxides: Geochimica et Cosmochimica Acta, v. 47, no. 11, p. 2037-2046, https://doi.org/10.1016/0016-7037(83)90219-3.","productDescription":"10 p.","startPage":"2037","endPage":"2046","numberOfPages":"10","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":220763,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"47","issue":"11","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a676fe4b0c8380cd73325","contributors":{"authors":[{"text":"Hem, J.D.","contributorId":54576,"corporation":false,"usgs":true,"family":"Hem","given":"J.D.","affiliations":[],"preferred":false,"id":360861,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lind, Carol J.","contributorId":36110,"corporation":false,"usgs":true,"family":"Lind","given":"Carol","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":360860,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1008657,"text":"1008657 - 1983 - The relationship between parental age and reproductive effort in the California Gull (Larus californicus)","interactions":[],"lastModifiedDate":"2023-08-25T15:29:33.674442","indexId":"1008657","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":982,"text":"Behavioral Ecology and Sociobiology","active":true,"publicationSubtype":{"id":10}},"displayTitle":"The relationship between parental age and reproductive effort in the California Gull (<i>Larus californicus</i>)","title":"The relationship between parental age and reproductive effort in the California Gull (Larus californicus)","docAbstract":"<p>Reproductive effort was compared among California gulls ranging in age from 3 to 18 years old. Results indicated that reproductive effort increased with parental age. Older parents (11–18 years old) invested more in foraging effort and in defense of offspring than did younger parents (&lt;10 years old), and did so over a greater period of time. Increases with age in the efficiency of parenting could not be demonstrated. Increased levels of reproductive effort, therefore, appeared to be the main factor responsible for age-related increases in breeding success.</p><p>The higher levels of reproductive effort of old parents were associated with higher mortality. Thus, data support the prediction that a cost-benefit system of risk of mortality vs reproductive gain operates in this population. Higher levels of reproductive effort can increase an individual's reproductive success; however, it also increases the likelihood that it will die. Therefore, for the young parent, high risks of mortality involved in current production would be too costly (in terms of loss of future reproductive success) to justify the benefit of high current reproductive output. Parents achieve the highest likelihood of maximizing life-time reproductive output by increasing reproductive effort with age as the cost of mortality diminishes.</p><p>Data testing the relationship between parental age and reproductive effort demonstrate the existence of age-related variation in reproductive investment. They also demonstrate that the concept of reproductive value proposed by Fisher (1930) has validity as a framework which supports much of our theory on life history evolution.</p>","language":"English","publisher":"Springer Link","doi":"10.1007/BF00299919","usgsCitation":"Pugesek, B.H., 1983, The relationship between parental age and reproductive effort in the California Gull (Larus californicus): Behavioral Ecology and Sociobiology, v. 13, p. 161-171, https://doi.org/10.1007/BF00299919.","productDescription":"11 p.","startPage":"161","endPage":"171","numberOfPages":"11","costCenters":[{"id":481,"text":"Northern Rocky Mountain Science Center","active":true,"usgs":true}],"links":[{"id":130802,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"13","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6fe4b07f02db640f12","contributors":{"authors":[{"text":"Pugesek, Bruce H.","contributorId":22668,"corporation":false,"usgs":true,"family":"Pugesek","given":"Bruce","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":318372,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1014396,"text":"1014396 - 1983 - You asked for it! Goldfish farming: Part III","interactions":[],"lastModifiedDate":"2012-02-02T00:04:11","indexId":"1014396","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":855,"text":"Aquaculture Magazine","active":true,"publicationSubtype":{"id":10}},"title":"You asked for it! Goldfish farming: Part III","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Aquaculture Magazine","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","collaboration":"None/FF","usgsCitation":"Martin, M., 1983, You asked for it! Goldfish farming: Part III: Aquaculture Magazine, v. 9, no. 5, p. 30-34.","productDescription":"p. 30-34","startPage":"30","endPage":"34","numberOfPages":"5","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":129380,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"9","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49a2e4b07f02db5be9fb","contributors":{"authors":[{"text":"Martin, M.","contributorId":103217,"corporation":false,"usgs":true,"family":"Martin","given":"M.","affiliations":[],"preferred":false,"id":320301,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1014395,"text":"1014395 - 1983 - You asked for it! Goldfish farming: Part II","interactions":[],"lastModifiedDate":"2012-02-02T00:04:11","indexId":"1014395","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":855,"text":"Aquaculture Magazine","active":true,"publicationSubtype":{"id":10}},"title":"You asked for it! Goldfish farming: Part II","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Aquaculture Magazine","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","collaboration":"None/FF","usgsCitation":"Martin, M., 1983, You asked for it! Goldfish farming: Part II: Aquaculture Magazine, v. 9, no. 4, p. 38-40.","productDescription":"p. 38-40","startPage":"38","endPage":"40","numberOfPages":"3","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":129379,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"9","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49ace4b07f02db5c65ee","contributors":{"authors":[{"text":"Martin, M.","contributorId":103217,"corporation":false,"usgs":true,"family":"Martin","given":"M.","affiliations":[],"preferred":false,"id":320300,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1014394,"text":"1014394 - 1983 - You asked for it! Goldfish farming: Part I","interactions":[],"lastModifiedDate":"2012-02-02T00:04:11","indexId":"1014394","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":855,"text":"Aquaculture Magazine","active":true,"publicationSubtype":{"id":10}},"title":"You asked for it! Goldfish farming: Part I","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Aquaculture Magazine","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","collaboration":"None/FF","usgsCitation":"Martin, M., 1983, You asked for it! Goldfish farming: Part I: Aquaculture Magazine, v. 9, no. 3, p. 38-40.","productDescription":"p. 38-40","startPage":"38","endPage":"40","numberOfPages":"3","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":129378,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"9","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48c7e4b07f02db540a90","contributors":{"authors":[{"text":"Martin, M.","contributorId":103217,"corporation":false,"usgs":true,"family":"Martin","given":"M.","affiliations":[],"preferred":false,"id":320299,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1003837,"text":"1003837 - 1983 - Outbreak of avian cholera on the wintering grounds of the Mississippi Valley Canada goose flock","interactions":[],"lastModifiedDate":"2023-09-23T04:34:35.091178","indexId":"1003837","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","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":"Outbreak of avian cholera on the wintering grounds of the Mississippi Valley Canada goose flock","docAbstract":"<p><span>Avian cholera is reported for the first time in Canada geese,&nbsp;</span><i>Branta canadensis</i><span>, of the Mississippi Valley population. The disease was detected in weekly surveillance transects and was responsible to the loss of about 850 geese during the winter of 1978–1979 at localized areas in southern Illinois. Necropsies performed on 480 geese that died at Union County Conservation Area and on 133 birds at Horseshoe Lake Conservation Area during January and February 1979 revealed that the majority of losses (649%) were caused by avian cholera. Lead poisoning was responsible for the death of 14% of the geese analyzed and the remaining 22%, most of which were decomposed, were undiagnosed. Lethal lead levels and&nbsp;</span><i>Pasteurella multocida</i><span>&nbsp;occurred concomitantly in a few instances.</span></p>","language":"English","publisher":"Allen Press","doi":"10.7589/0090-3558-19.2.95","usgsCitation":"Windingstad, R.M., Duncan, R.M., and Thornburg, D., 1983, Outbreak of avian cholera on the wintering grounds of the Mississippi Valley Canada goose flock: Journal of Wildlife Diseases, v. 19, no. 2, p. 95-97, https://doi.org/10.7589/0090-3558-19.2.95.","productDescription":"3 p.","startPage":"95","endPage":"97","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"links":[{"id":480552,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.7589/0090-3558-19.2.95","text":"Publisher Index Page"},{"id":135784,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United 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,{"id":1003802,"text":"1003802 - 1983 - Research note: Isolation of a herpesvirus from a bald eagle nestling","interactions":[],"lastModifiedDate":"2023-01-12T12:24:51.324845","indexId":"1003802","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":948,"text":"Avian Diseases","active":true,"publicationSubtype":{"id":10}},"title":"Research note: Isolation of a herpesvirus from a bald eagle nestling","docAbstract":"<p>Cloacal swabs collected from wild bald eagle nestlings (<i>Haliaeetus leucocephalus</i>) were tested for viruses. A virus isolated from one of these samples had a lipid coat and contained DNA. Electron microscopy confirmed that it was a herpesvirus. This appears to be the first report of a herpesvirus isolation from a wild bald eagle.</p>","language":"English","publisher":"American Association of Avian Pathologists","doi":"10.2307/1590217","usgsCitation":"Docherty, D.E., Romaine, R., and Knight, R., 1983, Research note: Isolation of a herpesvirus from a bald eagle nestling: Avian Diseases, v. 27, no. 4, p. 1162-1165, https://doi.org/10.2307/1590217.","productDescription":"4 p.","startPage":"1162","endPage":"1165","numberOfPages":"4","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"links":[{"id":131243,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Washington","county":"San Juan County","otherGeospatial":"San Juan Islands","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              236.75537109375,\n              48.96579381461063\n            ],\n            [\n              237.008056640625,\n              48.77067246880509\n            ],\n            [\n              236.74438476562497,\n              48.67645370777654\n            ],\n            [\n              236.88720703125,\n              48.42191010942875\n            ],\n            [\n              236.64550781249997,\n              48.25394114463431\n            ],\n            [\n              237.01904296874997,\n              47.923704717745686\n            ],\n            [\n              236.93115234374997,\n              47.31648293428332\n            ],\n            [\n              237.041015625,\n              47.03269459852135\n            ],\n            [\n              237.535400390625,\n              47.234489635299184\n            ],\n            [\n              237.73315429687497,\n              47.85740289465826\n            ],\n            [\n              237.86499023437497,\n              48.42920055556841\n            ],\n            [\n              237.61230468749997,\n              48.97300592158682\n            ],\n            [\n              236.75537109375,\n              48.96579381461063\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"27","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e481fe4b07f02db4e097b","contributors":{"authors":[{"text":"Docherty, D. E.","contributorId":83469,"corporation":false,"usgs":true,"family":"Docherty","given":"D.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":314344,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Romaine, R.I.","contributorId":60996,"corporation":false,"usgs":true,"family":"Romaine","given":"R.I.","email":"","affiliations":[],"preferred":false,"id":314343,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Knight, R.L.","contributorId":105661,"corporation":false,"usgs":true,"family":"Knight","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":314345,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":1003858,"text":"1003858 - 1983 - Squamous cell carcinoma in a free-ranging white-tailed deer (Odocoileus virginianus)","interactions":[],"lastModifiedDate":"2023-09-23T03:12:11.299522","indexId":"1003858","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2507,"text":"Journal of Wildlife Diseases","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Squamous cell carcinoma in a free-ranging white-tailed deer (<i>Odocoileus virginianus</i>)","title":"Squamous cell carcinoma in a free-ranging white-tailed deer (Odocoileus virginianus)","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Allen Press","doi":"10.7589/0090-3558-19.2.162","usgsCitation":"Stroud, R.K., and Amundson, T.E., 1983, Squamous cell carcinoma in a free-ranging white-tailed deer (Odocoileus virginianus): Journal of Wildlife Diseases, v. 19, no. 2, p. 162-164, https://doi.org/10.7589/0090-3558-19.2.162.","productDescription":"3 p.","startPage":"162","endPage":"164","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"links":[{"id":131103,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Wisconsin","city":"Spring Green","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -90.10110855102539,\n              43.21831254241147\n            ],\n            [\n              -90.11690139770508,\n              43.20680242240334\n            ],\n            [\n              -90.11878967285156,\n              43.197792987132836\n            ],\n            [\n              -90.11913299560547,\n              43.18427633964703\n            ],\n            [\n              -90.11896133422852,\n              43.16499742418806\n            ],\n            [\n              -90.11398315429686,\n              43.15623226883236\n            ],\n            [\n              -90.10917663574219,\n              43.15122304406093\n            ],\n            [\n              -90.087890625,\n              43.143958938834494\n            ],\n            [\n              -90.0684928894043,\n              43.139950787115446\n            ],\n            [\n              -90.0410270690918,\n              43.13882344709952\n            ],\n            [\n              -90.02386093139647,\n              43.140451820450636\n            ],\n            [\n              -90.00806808471678,\n              43.15685839305898\n            ],\n            [\n              -89.99897003173828,\n              43.17225902888736\n            ],\n            [\n              -89.99879837036133,\n              43.19328777057828\n            ],\n            [\n              -90.0025749206543,\n              43.2069275440811\n            ],\n            [\n              -90.01235961914061,\n              43.21868783583851\n            ],\n            [\n              -90.02540588378906,\n              43.22294099990729\n            ],\n            [\n              -90.04222869873047,\n              43.22631830119164\n            ],\n            [\n              -90.07415771484375,\n              43.2255678059647\n            ],\n            [\n              -90.08565902709961,\n              43.224191874050916\n            ],\n            [\n              -90.10110855102539,\n              43.21831254241147\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"19","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e49ed","contributors":{"authors":[{"text":"Stroud, R. K.","contributorId":45660,"corporation":false,"usgs":true,"family":"Stroud","given":"R.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":314482,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Amundson, Terry E.","contributorId":99509,"corporation":false,"usgs":true,"family":"Amundson","given":"Terry","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":314483,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1003836,"text":"1003836 - 1983 - Waterbird mortality from botulism type E in Lake Michigan: An update","interactions":[],"lastModifiedDate":"2023-09-23T02:25:24.804502","indexId":"1003836","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3783,"text":"The Wilson Bulletin","printIssn":"0043-5643","active":true,"publicationSubtype":{"id":10}},"title":"Waterbird mortality from botulism type E in Lake Michigan: An update","docAbstract":"<p><span>Three outbreaks of botulism type E occurring in waterbirds on Lake Michigan since autumn 1976 are discussed. Natural ingestion of food containing type E toxin by Ring-billed Gulls (<i>Larus delawarensis</i>) and the presence of type E toxin in blood from moribund gulls were demonstrated. Concurrent presence of type C and type E botulinal toxins was found in a die-off of Common Loons (<i>Gavia immer</i>). In combination with previous reported outbreaks, these incidents suggest that this disease is geographically widespread in Lake Michigan, and that environmental conditions conducive to type E botulinal toxin production and consumption occur in both summer and autumn.</span></p>","language":"English","publisher":"Wilson Ornithological Society","usgsCitation":"Brand, C.J., Duncan, R.M., Garrow, S.P., Olson, D., and Schumann, L.E., 1983, Waterbird mortality from botulism type E in Lake Michigan: An update: The Wilson Bulletin, v. 95, no. 2, p. 269-275.","productDescription":"7 p.","startPage":"269","endPage":"275","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"links":[{"id":409588,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://sora.unm.edu/node/130032","linkFileType":{"id":5,"text":"html"}},{"id":134127,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","otherGeospatial":"Lake Michigan","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -87.4072265625,\n              41.4509614012039\n            ],\n            [\n              -86.37451171875,\n              41.4509614012039\n            ],\n            [\n              -85.836181640625,\n              42.601619944327965\n            ],\n            [\n              -86.06689453125,\n              43.70759350405294\n            ],\n            [\n              -85.968017578125,\n              44.5826428195842\n            ],\n            [\n              -85.36376953125,\n              44.69989765840318\n            ],\n            [\n              -85.1220703125,\n              45.236217535866025\n            ],\n            [\n              -84.66064453125,\n              45.336701909968106\n            ],\n            [\n              -84.57275390625,\n              46.14939437647686\n            ],\n            [\n              -85.462646484375,\n              46.240651955001695\n            ],\n            [\n              -85.74829101562499,\n              46.08847179577592\n            ],\n            [\n              -86.37451171875,\n              46.042735653846506\n            ],\n            [\n              -87.0556640625,\n              45.96642454131025\n            ],\n            [\n              -87.791748046875,\n              45.46783598133375\n            ],\n            [\n              -88.154296875,\n              44.59829048984011\n            ],\n            [\n              -88.209228515625,\n              44.36313311380771\n            ],\n            [\n              -87.857666015625,\n              44.12702800650004\n            ],\n            [\n              -87.923583984375,\n              43.57243174740972\n            ],\n            [\n              -88.187255859375,\n              43.100982876188546\n            ],\n            [\n              -88.187255859375,\n              42.58544425738491\n            ],\n            [\n              -88.13232421875,\n              41.95949009892465\n            ],\n            [\n              -87.4072265625,\n              41.4509614012039\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"95","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4c58","contributors":{"authors":[{"text":"Brand, Christopher J. cbrand@usgs.gov","contributorId":1186,"corporation":false,"usgs":true,"family":"Brand","given":"Christopher","email":"cbrand@usgs.gov","middleInitial":"J.","affiliations":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"preferred":true,"id":314420,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Duncan, Ruth M.","contributorId":84720,"corporation":false,"usgs":true,"family":"Duncan","given":"Ruth","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":314423,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Garrow, Scott P.","contributorId":44513,"corporation":false,"usgs":false,"family":"Garrow","given":"Scott","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":314422,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Olson, Dan","contributorId":91010,"corporation":false,"usgs":false,"family":"Olson","given":"Dan","email":"","affiliations":[],"preferred":false,"id":314424,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Schumann, Leonard E.","contributorId":27413,"corporation":false,"usgs":false,"family":"Schumann","given":"Leonard","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":314421,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
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