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,{"id":2002183,"text":"2002183 - 1975 - A comparison of observer and camera counts of desert bighorn sheep","interactions":[],"lastModifiedDate":"2012-02-02T00:14:55","indexId":"2002183","displayToPublicDate":"1975-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":91,"text":"Technical Report","active":true,"publicationSubtype":{"id":1}},"seriesNumber":"CPSU/UNLV 006/04","title":"A comparison of observer and camera counts of desert bighorn sheep","docAbstract":"No abstract available at this time","language":"English","publisher":"National Park Service","usgsCitation":"Douglas, C.L., 1975, A comparison of observer and camera counts of desert bighorn sheep: Technical Report CPSU/UNLV 006/04.","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":198853,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b27e4b07f02db6b0f7d","contributors":{"authors":[{"text":"Douglas, C. L.","contributorId":64586,"corporation":false,"usgs":true,"family":"Douglas","given":"C.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":326122,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":16006,"text":"ofr75144 - 1975 - Preliminary description and interpretation of cores and radiographs from Clear Lake, Lake County, California: Core 7","interactions":[],"lastModifiedDate":"2022-05-10T14:42:42.581913","indexId":"ofr75144","displayToPublicDate":"1975-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"75-144","title":"Preliminary description and interpretation of cores and radiographs from Clear Lake, Lake County, California: Core 7","docAbstract":"<p>Clear Lake, California is located in the California Coast Ranges about 120 km north of San Francisco and is the largest freshwater lake wholly within California. The lake basin is tectonically controlled (Anderson, 1936; Brice, 1953, Sims and Rymer, 1974) and the area seismically active (Coffman and von Hake, 1973).</p><p>Interest in this lake was stimulated by hypotheses developed from a study of sediments in Van Norman Reservoir after the 1971 San Fernando earthquake (Sims, 1973). During this study three zones of deformational structures were found in the 1 m-thick sequence of sediments exposed over about 2 km<sup>2</sup> of the reservoir bottom. These zones were correlated with moderate earthquakes that shook the San Fernando area in 1930, 1952, and 1971. Results of this study, coupled with the experimental formation of deformational structures similar to those from Van Norman Reservoir, led to a search for similar structures in Pleistocene and Holocene lakes and lake sediments in other seismically active areas. Clear Lake, California was chosen specifically because of .:s location near the San Andreas fault and the San Francisco-Oakland urban complex, and the probability of obtaining an uninterrupted sediment record from the present into Pleistocene time. Eight 12 to 15 cm diameter continuous cores were taken from the lake sediments (fig. 1) as part of a study of earthquake induced structures in sediments and the tectonic framework of the Clear Lake basin. The eight cores range in length from 13.87 m to 133.09 m (Table 1).</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr75144","usgsCitation":"Sims, J.D., and Rymer, M.J., 1975, Preliminary description and interpretation of cores and radiographs from Clear Lake, Lake County, California: Core 7: U.S. Geological Survey Open-File Report 75-144, 21 p., https://doi.org/10.3133/ofr75144.","productDescription":"21 p.","costCenters":[],"links":[{"id":147491,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1975/0144/report-thumb.jpg"},{"id":400393,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1975/0144/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","county":"Lake County","otherGeospatial":"Clear Lake","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -122.93838500976561,\n              38.91133881927712\n            ],\n            [\n              -122.6081085205078,\n              38.91133881927712\n            ],\n            [\n              -122.6081085205078,\n              39.14071226655259\n            ],\n            [\n              -122.93838500976561,\n              39.14071226655259\n            ],\n            [\n              -122.93838500976561,\n              38.91133881927712\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c649","contributors":{"authors":[{"text":"Sims, John D.","contributorId":60202,"corporation":false,"usgs":true,"family":"Sims","given":"John","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":172079,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rymer, Michael J. mrymer@usgs.gov","contributorId":1522,"corporation":false,"usgs":true,"family":"Rymer","given":"Michael","email":"mrymer@usgs.gov","middleInitial":"J.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":172078,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2001174,"text":"2001174 - 1975 - Toxicity of the lampricide 3-trifluoromethyl-4-nitrophenol (TFM) to nontarget fish in flow-through tests","interactions":[],"lastModifiedDate":"2012-02-02T00:14:57","indexId":"2001174","displayToPublicDate":"1975-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":39,"text":"Investigations in Fish Control","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"61","title":"Toxicity of the lampricide 3-trifluoromethyl-4-nitrophenol (TFM) to nontarget fish in flow-through tests","docAbstract":"Abstract not submitted to date","language":"English","publisher":"U.S. Fish and Wildlife Service","publisherLocation":"La Crosse, WI","usgsCitation":"Marking, L.L., Bills, T., and Chandler, J.H., 1975, Toxicity of the lampricide 3-trifluoromethyl-4-nitrophenol (TFM) to nontarget fish in flow-through tests: Investigations in Fish Control 61, 9.","productDescription":"9","startPage":"0","endPage":"9","numberOfPages":"9","costCenters":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":198565,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ee4b07f02db627f4e","contributors":{"authors":[{"text":"Marking, L. L.","contributorId":90661,"corporation":false,"usgs":true,"family":"Marking","given":"L.","middleInitial":"L.","affiliations":[],"preferred":false,"id":325517,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bills, T.D.","contributorId":6393,"corporation":false,"usgs":true,"family":"Bills","given":"T.D.","email":"","affiliations":[],"preferred":false,"id":325515,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Chandler, J. H. Jr.","contributorId":74333,"corporation":false,"usgs":true,"family":"Chandler","given":"J.","suffix":"Jr.","middleInitial":"H.","affiliations":[],"preferred":false,"id":325516,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":2001399,"text":"2001399 - 1975 - Fish furunculosis","interactions":[],"lastModifiedDate":"2012-02-02T00:15:02","indexId":"2001399","displayToPublicDate":"1975-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":22,"text":"Fish Disease Leaflet","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"43","title":"Fish furunculosis","docAbstract":"No abstract available at this time","language":"English","publisher":"U.S. Fish and Wildlife Service","collaboration":"462/FH","usgsCitation":"Snieszko, S.F., and Bullock, G.L., 1975, Fish furunculosis: Fish Disease Leaflet 43, 10 p.","productDescription":"10 p.","startPage":"0","endPage":"10","numberOfPages":"10","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":198132,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":112248,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://hdl.handle.net/2027/coo.31924000778476?urlappend=%3Bseq=47"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f3e4b07f02db5efac5","contributors":{"authors":[{"text":"Snieszko, S. F.","contributorId":13169,"corporation":false,"usgs":true,"family":"Snieszko","given":"S.","middleInitial":"F.","affiliations":[],"preferred":false,"id":325649,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bullock, G. L.","contributorId":69498,"corporation":false,"usgs":true,"family":"Bullock","given":"G.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":325650,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1014549,"text":"1014549 - 1975 - Fish health: Some concepts, constraints, and comparisons","interactions":[],"lastModifiedDate":"2023-02-24T17:28:36.390522","indexId":"1014549","displayToPublicDate":"1975-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":801,"text":"Annals of the New York Academy of Sciences","active":true,"publicationSubtype":{"id":10}},"title":"Fish health: Some concepts, constraints, and comparisons","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"New York Academy of Sciences","doi":"10.1111/j.1749-6632.1975.tb26826.x","usgsCitation":"Wolf, K., 1975, Fish health: Some concepts, constraints, and comparisons: Annals of the New York Academy of Sciences, v. 245, p. 4-14, https://doi.org/10.1111/j.1749-6632.1975.tb26826.x.","productDescription":"11 p.","startPage":"4","endPage":"14","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":131010,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"245","noUsgsAuthors":false,"publicationDate":"2006-12-16","publicationStatus":"PW","scienceBaseUri":"4f4e49f3e4b07f02db5ef682","contributors":{"authors":[{"text":"Wolf, K.","contributorId":16344,"corporation":false,"usgs":true,"family":"Wolf","given":"K.","email":"","affiliations":[],"preferred":false,"id":320574,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":35748,"text":"b1329 - 1975 - Lithology and uranium potential of Jurassic formations in the San Ysidro-Cuba and Majors Ranch areas, northwestern New Mexico","interactions":[],"lastModifiedDate":"2023-03-14T21:38:34.149489","indexId":"b1329","displayToPublicDate":"1975-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1329","title":"Lithology and uranium potential of Jurassic formations in the San Ysidro-Cuba and Majors Ranch areas, northwestern New Mexico","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b1329","usgsCitation":"Santos, E.S., 1975, Lithology and uranium potential of Jurassic formations in the San Ysidro-Cuba and Majors Ranch areas, northwestern New Mexico: U.S. Geological Survey Bulletin 1329, Report: iii, 22 p.; 2 Plates: 41.96 x 31.50 inches and 17.00 x 23.00 inches, https://doi.org/10.3133/b1329.","productDescription":"Report: iii, 22 p.; 2 Plates: 41.96 x 31.50 inches and 17.00 x 23.00 inches","costCenters":[],"links":[{"id":166371,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1329/report-thumb.jpg"},{"id":63664,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1329/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":63665,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1329/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":63666,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1329/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":414142,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_21435.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"New Mexico","otherGeospatial":"San Ysidro-Cuba and Majors Ranch areas","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -106.777,\n              35.288\n            ],\n            [\n              -106.777,\n              36\n            ],\n            [\n              -107.125,\n              36\n            ],\n            [\n              -107.125,\n              35.288\n            ],\n            [\n              -106.777,\n              35.288\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db635d87","contributors":{"authors":[{"text":"Santos, Elmer S.","contributorId":94312,"corporation":false,"usgs":true,"family":"Santos","given":"Elmer","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":215153,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1001545,"text":"1001545 - 1975 - Fitting Richards' curve to data of diverse origins","interactions":[],"lastModifiedDate":"2017-12-27T13:59:04","indexId":"1001545","displayToPublicDate":"1975-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1868,"text":"Growth","active":true,"publicationSubtype":{"id":10}},"title":"Fitting Richards' curve to data of diverse origins","docAbstract":"Published techniques for fitting data to nonlinear growth curves are briefly reviewed, most techniques require knowledge of the shape of the curve. A flexible growth curve developed by Richards (1959) is discussed as an alternative when the shape is unknown. The shape of this curve is governed by a specific parameter which can be estimated from the data. We describe in detail the fitting of a diverse set of longitudinal and cross-sectional data to Richards' growth curve for the purpose of determining the age of red fox (Vulpes vulpes) pups on the basis of right hind foot length. The fitted curve is found suitable for pups less than approximately 80 days old. The curve is extrapolated to pre-natal growth and shown to be appropriate only for about 10 days prior to birth.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Growth","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Johnson, D.H., Sargeant, A., and Allen, S., 1975, Fitting Richards' curve to data of diverse origins: Growth, v. 39.","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":134075,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"39","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49a0e4b07f02db5bd985","contributors":{"authors":[{"text":"Johnson, Douglas H. 0000-0002-7778-6641","orcid":"https://orcid.org/0000-0002-7778-6641","contributorId":70327,"corporation":false,"usgs":true,"family":"Johnson","given":"Douglas","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":311232,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sargeant, A.B.","contributorId":13171,"corporation":false,"usgs":true,"family":"Sargeant","given":"A.B.","email":"","affiliations":[],"preferred":false,"id":311230,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Allen, S.H.","contributorId":17570,"corporation":false,"usgs":true,"family":"Allen","given":"S.H.","email":"","affiliations":[],"preferred":false,"id":311231,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":1013906,"text":"1013906 - 1975 - You asked for it! Answers to questions about fish farming: Part II","interactions":[],"lastModifiedDate":"2012-08-24T01:02:05","indexId":"1013906","displayToPublicDate":"1975-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1277,"text":"Commercial Fish Farmer and Aquaculture News","active":true,"publicationSubtype":{"id":10}},"title":"You asked for it! Answers to questions about fish farming: Part II","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Commercial Fish Farmer and Aquaculture News","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Richard V. Gallagher","publisherLocation":"Arden, NC","collaboration":"None/FF","usgsCitation":"Giudice, J., 1975, You asked for it! Answers to questions about fish farming: Part II: Commercial Fish Farmer and Aquaculture News, v. 1, no. 6.","productDescription":"1 p.","startPage":"39","numberOfPages":"39","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":132176,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"1","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d6e4b07f02db5de3b6","contributors":{"authors":[{"text":"Giudice, J.J.","contributorId":50841,"corporation":false,"usgs":true,"family":"Giudice","given":"J.J.","email":"","affiliations":[],"preferred":false,"id":319428,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1013907,"text":"1013907 - 1975 - You asked for it! Answers to questions about fish farming: Part IV","interactions":[],"lastModifiedDate":"2012-08-24T01:02:05","indexId":"1013907","displayToPublicDate":"1975-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1277,"text":"Commercial Fish Farmer and Aquaculture News","active":true,"publicationSubtype":{"id":10}},"title":"You asked for it! Answers to questions about fish farming: Part IV","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Commercial Fish Farmer and Aquaculture News","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Richard V. Gallagher","publisherLocation":"Arden, NC","collaboration":"None/FF","usgsCitation":"Giudice, J., 1975, You asked for it! Answers to questions about fish farming: Part IV: Commercial Fish Farmer and Aquaculture News, v. 2, no. 2.","productDescription":"1 p.","startPage":"51","numberOfPages":"51","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":132177,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"2","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d6e4b07f02db5de2f9","contributors":{"authors":[{"text":"Giudice, J.J.","contributorId":50841,"corporation":false,"usgs":true,"family":"Giudice","given":"J.J.","email":"","affiliations":[],"preferred":false,"id":319429,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1013909,"text":"1013909 - 1975 - You asked for it! Everything will FALL in place with good management practices","interactions":[],"lastModifiedDate":"2012-02-02T00:04:23","indexId":"1013909","displayToPublicDate":"1975-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1277,"text":"Commercial Fish Farmer and Aquaculture News","active":true,"publicationSubtype":{"id":10}},"title":"You asked for it! Everything will FALL in place with good management practices","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Commercial Fish Farmer and Aquaculture News","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","collaboration":"None/FF","usgsCitation":"Giudice, J., 1975, You asked for it! Everything will FALL in place with good management practices: Commercial Fish Farmer and Aquaculture News, v. 2, no. 6, p. 38-39.","productDescription":"p. 38-39","startPage":"38","endPage":"39","numberOfPages":"2","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":130767,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"2","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d6e4b07f02db5de2de","contributors":{"authors":[{"text":"Giudice, J.J.","contributorId":50841,"corporation":false,"usgs":true,"family":"Giudice","given":"J.J.","email":"","affiliations":[],"preferred":false,"id":319431,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70010949,"text":"70010949 - 1975 - Canister cryogenic system for cooling germanium semiconductor detectors in borehole and marine probes","interactions":[],"lastModifiedDate":"2021-02-16T13:33:22.284344","indexId":"70010949","displayToPublicDate":"1975-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2906,"text":"Nuclear Instruments and Methods","active":true,"publicationSubtype":{"id":10}},"title":"Canister cryogenic system for cooling germanium semiconductor detectors in borehole and marine probes","docAbstract":"<div id=\"abstracts\" class=\"Abstracts u-font-serif\"><div id=\"aep-abstract-id3\" class=\"abstract author\"><div id=\"aep-abstract-sec-id4\"><p>High resolution intrinsic and lithium-drifted germanium gamma-ray detectors operate at about 77–90 K. A cryostat for borehole and marine applications has been designed that makes use of prefrozen propane canisters. Uses of such canisters simplifies cryostat construction, and the rapid exchange of canisters greatly reduces the time required to restore the detector to full holding-time capability and enhances the safety of a field operation where high-intensity<span>&nbsp;</span><sup>252</sup>Cf or other isotopic sources are used. A holding time of 6 h at 86 K was achieved in the laboratory in a simulated borehole probe in which a canister 3.7 cm diameter by 57 cm long was used. Longer holding times can be achieved by larger volume canisters in marine probes.</p></div></div></div><ul id=\"issue-navigation\" class=\"issue-navigation u-margin-s-bottom u-bg-grey1\"></ul>","language":"English","publisher":"Elsevier","doi":"10.1016/0029-554X(75)90216-5","issn":"0029554X","usgsCitation":"Boynton, G.R., 1975, Canister cryogenic system for cooling germanium semiconductor detectors in borehole and marine probes: Nuclear Instruments and Methods, v. 123, no. 3, p. 599-603, https://doi.org/10.1016/0029-554X(75)90216-5.","productDescription":"5 p.","startPage":"599","endPage":"603","numberOfPages":"5","costCenters":[],"links":[{"id":220950,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"123","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f344e4b0c8380cd4b6d4","contributors":{"authors":[{"text":"Boynton, G. R.","contributorId":82276,"corporation":false,"usgs":true,"family":"Boynton","given":"G.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":359959,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70010162,"text":"70010162 - 1975 - Automated ion-selective electrode method for determining fluoride in natural waters","interactions":[],"lastModifiedDate":"2023-10-20T16:17:33.994276","indexId":"70010162","displayToPublicDate":"1975-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1565,"text":"Environmental Science & Technology","onlineIssn":"1520-5851","printIssn":"0013-936X","active":true,"publicationSubtype":{"id":10}},"title":"Automated ion-selective electrode method for determining fluoride in natural waters","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"American Chemical Society","doi":"10.1021/es60101a008","issn":"0013936X","usgsCitation":"Erdmann, D.E., 1975, Automated ion-selective electrode method for determining fluoride in natural waters: Environmental Science & Technology, v. 9, no. 3, p. 252-253, https://doi.org/10.1021/es60101a008.","productDescription":"2 p.","startPage":"252","endPage":"253","costCenters":[],"links":[{"id":219513,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"9","issue":"3","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","scienceBaseUri":"5059eef5e4b0c8380cd4a077","contributors":{"authors":[{"text":"Erdmann, D. E.","contributorId":30264,"corporation":false,"usgs":true,"family":"Erdmann","given":"D.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":358173,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70010116,"text":"70010116 - 1975 - Short chain aliphatic acid anions in oil field waters and their contribution to the measured alkalinity","interactions":[],"lastModifiedDate":"2021-02-17T14:15:18.281662","indexId":"70010116","displayToPublicDate":"1975-01-01T00:00:00","publicationYear":"1975","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":"Short chain aliphatic acid anions in oil field waters and their contribution to the measured alkalinity","docAbstract":"<div id=\"abstracts\" class=\"Abstracts u-font-serif\"><div id=\"aep-abstract-id6\" class=\"abstract author\"><div id=\"aep-abstract-sec-id7\"><p>High alkalinity values found in some formation waters from Kettleman North Dome oil field are due chiefly to acetate and propionate ions, with some contribution from higher molecular weight organic acid ions. Some of these waters contain no detectable bicarbonate alkalinity. For waters such as these, high supersaturation with respect to calcite will be incorrectly indicated by thermodynamic calculations based upon carbonate concentrations inferred from traditional alkalinity measurements</p></div></div></div><ul id=\"issue-navigation\" class=\"issue-navigation u-margin-s-bottom u-bg-grey1\"></ul>","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(75)90092-7","issn":"00167037","usgsCitation":"Willey, L., Kharaka, Y., Presser, T.S., Rapp, J.B., and Barnes, I., 1975, Short chain aliphatic acid anions in oil field waters and their contribution to the measured alkalinity: Geochimica et Cosmochimica Acta, v. 39, no. 12, p. 1707-1711, https://doi.org/10.1016/0016-7037(75)90092-7.","productDescription":"5 p.","startPage":"1707","endPage":"1711","numberOfPages":"5","costCenters":[],"links":[{"id":218843,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"39","issue":"12","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b8e98e4b08c986b318a24","contributors":{"authors":[{"text":"Willey, L.M.","contributorId":44607,"corporation":false,"usgs":true,"family":"Willey","given":"L.M.","email":"","affiliations":[],"preferred":false,"id":357991,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kharaka, Y.K.","contributorId":23568,"corporation":false,"usgs":true,"family":"Kharaka","given":"Y.K.","email":"","affiliations":[],"preferred":false,"id":357988,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Presser, T. S.","contributorId":93875,"corporation":false,"usgs":true,"family":"Presser","given":"T.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":357992,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Rapp, J. B.","contributorId":28987,"corporation":false,"usgs":true,"family":"Rapp","given":"J.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":357990,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Barnes, I.","contributorId":23678,"corporation":false,"usgs":true,"family":"Barnes","given":"I.","affiliations":[],"preferred":false,"id":357989,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":1007710,"text":"1007710 - 1975 - Productivity and flowering of winter ephemerals in relation to Sonoran Desert shrubs","interactions":[],"lastModifiedDate":"2023-02-15T17:16:44.368988","indexId":"1007710","displayToPublicDate":"1975-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":737,"text":"American Midland Naturalist","active":true,"publicationSubtype":{"id":10}},"title":"Productivity and flowering of winter ephemerals in relation to Sonoran Desert shrubs","docAbstract":"<p><span>Ephemeral plant biomass and density on a Sonoran Desert hill near Cave Creek, Arizona, vary relative to shrub canopy type and shrub density. Higher shrub density associated with increased elevation appears to decrease both ephemeral biomass productivity and density, while ephemeral growth is enhanced under a shrub canopy if it is not too dense or low-hanging. Phenology of ephemerals on the desert study site shows early cool-season germination, low tolerance to heat, and early flowering when compared to shrubs and succulents in the same area.</span></p>","language":"English","publisher":"University of Notre Dame","doi":"10.2307/2424164","usgsCitation":"Halvorson, W., and Patten, D.T., 1975, Productivity and flowering of winter ephemerals in relation to Sonoran Desert shrubs: American Midland Naturalist, v. 93, no. 2, p. 311-319, https://doi.org/10.2307/2424164.","productDescription":"9 p.","startPage":"311","endPage":"319","numberOfPages":"9","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":131368,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Arizona","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -112.04208415078593,\n              33.877324507524676\n            ],\n            [\n              -112.04208415078593,\n              33.79525100962188\n            ],\n            [\n              -111.90084253294029,\n              33.79525100962188\n            ],\n            [\n              -111.90084253294029,\n              33.877324507524676\n            ],\n            [\n              -112.04208415078593,\n              33.877324507524676\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"93","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae3e4b07f02db6891f3","contributors":{"authors":[{"text":"Halvorson, William L.","contributorId":97194,"corporation":false,"usgs":true,"family":"Halvorson","given":"William L.","affiliations":[],"preferred":false,"id":315897,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Patten, Duncan T.","contributorId":124573,"corporation":false,"usgs":false,"family":"Patten","given":"Duncan","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":315896,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1000098,"text":"1000098 - 1975 - Environmental factors affecting the strength of walleye (<i>Stizostedion vitreum vitreum</i>) year-classes in western Lake Erie, 1960-70","interactions":[],"lastModifiedDate":"2016-03-14T10:16:07","indexId":"1000098","displayToPublicDate":"1975-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2543,"text":"Journal of the Fisheries Research Board of Canada","active":true,"publicationSubtype":{"id":10}},"title":"Environmental factors affecting the strength of walleye (<i>Stizostedion vitreum vitreum</i>) year-classes in western Lake Erie, 1960-70","docAbstract":"<p><span>Commercial production of walleyes (</span><i>Stizostedion vitreum vitreum</i><span>) from western Lake Erie declined from 5.9 million pounds in 1956 to 140,000 pounds by 1969. Since 1956, marked irregularity in year-class success has developed. Only four year-classes were considered good during 1959&ndash;70. The rate and regularity of water warming during the spring spawning and incubation periods in 1960&ndash;70 had a positive effect on the density of egg deposits and the resulting year-class strength. Rates of warming were not themselves detrimental, but rather the extended length of the incubation period in cool springs increased the exposure of eggs to such negative influences as dislodgment from the spawning reefs by strong current action generated by spring storms, or siltation and low oxygen tensions. The annual brood stock size had much less influence on year-class strength than did water temperature. Reproductive success was unrelated to fluctuations in size of suitable reef spawning area caused by changes in water level. Apparently the usable spawning area at any water level is more than adequate to serve the limited walleye brood stocks.</span></p>","language":"English","publisher":"NRC Research Press","doi":"10.1139/f75-207","usgsCitation":"Busch, W.N., Scholl, R.L., and Hartman, W.L., 1975, Environmental factors affecting the strength of walleye (<i>Stizostedion vitreum vitreum</i>) year-classes in western Lake Erie, 1960-70: Journal of the Fisheries Research Board of Canada, v. 32, no. 10, p. 1733-1743, https://doi.org/10.1139/f75-207.","productDescription":"11 p.","startPage":"1733","endPage":"1743","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":133074,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"32","issue":"10","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a13e4b07f02db6023b3","contributors":{"authors":[{"text":"Busch, Wolf-Dieter N.","contributorId":46039,"corporation":false,"usgs":true,"family":"Busch","given":"Wolf-Dieter","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":308078,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Scholl, Russell L.","contributorId":26269,"corporation":false,"usgs":true,"family":"Scholl","given":"Russell","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":308077,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hartman, Wilbur L.","contributorId":14763,"corporation":false,"usgs":true,"family":"Hartman","given":"Wilbur","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":308076,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70197223,"text":"70197223 - 1975 - Mineral resource models and the Alaskan Mineral Resource Assessment Program","interactions":[],"lastModifiedDate":"2018-05-23T13:47:47","indexId":"70197223","displayToPublicDate":"1975-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Mineral resource models and the Alaskan Mineral Resource Assessment Program","docAbstract":"<p>The least exacting demand that can be made of any model is that it serves as a device whereby we can predict actual physical happenings. Another demand which could be made is that the physical happenings predicted be in some way relevant to man, either by allowing him to anticipate future uncontrollable events or by demonstrating the possible consequences of various decisions. To date, many mineral resource models have been deficient in meeting these demands.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Mineral materials modeling A state-of-the-art review","language":"English","publisher":"Johns Hopkins University Press","usgsCitation":"Singer, D.A., 1975, Mineral resource models and the Alaskan Mineral Resource Assessment Program, chap. <i>of</i> Mineral materials modeling A state-of-the-art review, p. 370-382.","productDescription":"13 p.","startPage":"370","endPage":"382","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":354425,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5b15d353e4b092d9651e28e7","contributors":{"editors":[{"text":"Vogely, W. A.","contributorId":205178,"corporation":false,"usgs":false,"family":"Vogely","given":"W.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":736294,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Singer, Donald A. dsinger@usgs.gov","contributorId":5601,"corporation":false,"usgs":true,"family":"Singer","given":"Donald","email":"dsinger@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":736293,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":15462,"text":"ofr75249 - 1975 - Dynamics of turbidity plumes in Lake Ontario","interactions":[],"lastModifiedDate":"2024-10-07T21:08:10.580039","indexId":"ofr75249","displayToPublicDate":"1975-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"75-249","title":"Dynamics of turbidity plumes in Lake Ontario","docAbstract":"<p>Large-turbidity features along the 275-kilometre long south shore of Lake Ontario were analyzed using LANDSAT-1 images. The ESIAC system developed by the Stanford Research Institute, was used to obtain enlargements and false-color renditions of turbidity plumes. After projection on a video screen, individual turbidity features were analyzed, mapped, and photographed.</p><p>The Niagara River plume, as much as 500 square kilometres in area, is by far, the largest turbidity feature in the lake. Based on image tonal comparisons, turbidity in the Welland Canal is usually higher than that in any other watercourse discharging into the lake throughout the shipping season. Somewhat less turbid water enters the lake from the Port Dalhousie diversion channel and the Genesee River. Relatively clear water resulting from the deposition of suspended matter in numerous upstream lakes is discharged by the Niagara and Oswego rivers.</p><p>Plume analysis corroborates the presence of a prevailing eastward flowing longshore current along the entire south shore. This current is most persistent at the Oswego River outlet but is quite variable in the Rochester embayment, where rapid shifts in water movement were occasionally detected in LANDSAT images. The position of the spring thermal bar, a zone, of maximum density water corresponding to the 4°C isotherm, was approximately located in images obtained during April 1973. Although eastward moving currents were detected on the inshore side of the thermal bar, westward moving counter currents seem to be dominant along its offshore side.</p><p>Plumes generated by beach erosion were readily detected in the images. Such areas are identified by light to very light, long, narrow plumes paralleling the coastline. Extensive areas of the south shore are subject to erosion, but the most severely affected beaches are situated between Fifty Mile Pt., Ontario and Thirty Mile Pt., N.Y., along the Rochester embayment, and between Sodus Bay and Nine Mile Pt.</p><p>Color illustrations of figure accession numbers EDC-010077 to EDC-010106 are available for purchase from the EROS Data Center, Sioux Falls, South Dakota 57198.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr75249","collaboration":"Prepared in cooperation with the National Aeronautics Space Administration/Goddard Space Flight Center, Greenbelt, Maryland","usgsCitation":"Pluhowski, E.J., 1975, Dynamics of turbidity plumes in Lake Ontario: U.S. Geological Survey Open-File Report 75-249, Report: ix, 59 p., https://doi.org/10.3133/ofr75249.","productDescription":"Report: ix, 59 p.","costCenters":[],"links":[{"id":149041,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1975/0249/report-thumb.jpg"},{"id":462666,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1975/0249/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"Canada, United States","otherGeospatial":"Lake Ontario","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -80.99172224212556,\n              45.15721980352575\n            ],\n            [\n              -80.99172224212556,\n              42.37218583599275\n            ],\n            [\n              -74.39757490950474,\n              42.37218583599275\n            ],\n            [\n              -74.39757490950474,\n              45.15721980352575\n            ],\n            [\n              -80.99172224212556,\n              45.15721980352575\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a59e4b07f02db62f706","contributors":{"authors":[{"text":"Pluhowski, Edward J.","contributorId":87911,"corporation":false,"usgs":true,"family":"Pluhowski","given":"Edward","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":171172,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":16116,"text":"ofr75360 - 1975 - Heavy minerals in stream sands of the southern Hazara District, Pakistan","interactions":[],"lastModifiedDate":"2024-08-12T21:27:49.222054","indexId":"ofr75360","displayToPublicDate":"1975-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"75-360","title":"Heavy minerals in stream sands of the southern Hazara District, Pakistan","docAbstract":"<p>The areal distribution of heavy minerals in 99 samples from stream sands in the southern Hazara District, West Pakistan, indicates that the metamorphic grade of the rocks in the area increases toward the northwest. Minerals of potential economic value in the heavy-mineral samples include scheelite from the Oghi-Batgram-Battal area and hematite from the Galdanian area. The total weight of magnetite sand grains transported down the Indus River past Darband is calculated to be about 200,000 tons per year, a quantity which may be of economic value. Radioactive minerals are not present in any of the samples in sufficient quantity to be of economic importance.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr75360","usgsCitation":"Stauffer, K.W., 1975, Heavy minerals in stream sands of the southern Hazara District, Pakistan: U.S. Geological Survey Open-File Report 75-360, Report: iii, 42 p.; 1 Table: 15.82 x 20.43 inches, https://doi.org/10.3133/ofr75360.","productDescription":"Report: iii, 42 p.; 1 Table: 15.82 x 20.43 inches","costCenters":[],"links":[{"id":432557,"rank":3,"type":{"id":27,"text":"Table"},"url":"https://pubs.usgs.gov/of/1975/0360/table-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":432556,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1975/0360/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":148256,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1975/0360/report-thumb.jpg"}],"country":"Pakistan","otherGeospatial":"Hazara District","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              74.22054290771484,\n              32.78409957394813\n            ],\n            [\n              74.28749084472655,\n              32.78409957394813\n            ],\n            [\n              74.28749084472655,\n              32.831135000359815\n            ],\n            [\n              74.22054290771484,\n              32.831135000359815\n            ],\n            [\n              74.22054290771484,\n              32.78409957394813\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a68e4b07f02db63b17a","contributors":{"authors":[{"text":"Stauffer, Karl W.","contributorId":20760,"corporation":false,"usgs":true,"family":"Stauffer","given":"Karl","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":172262,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70010948,"text":"70010948 - 1975 - Mercury distribution in ancient and modern sediment of northeastern Bering Sea","interactions":[{"subject":{"id":15187,"text":"ofr72268 - 1972 - Mercury distribution in ancient and modern sediment of northeastern Bering Sea","indexId":"ofr72268","publicationYear":"1972","noYear":false,"title":"Mercury distribution in ancient and modern sediment of northeastern Bering Sea"},"predicate":"SUPERSEDED_BY","object":{"id":70010948,"text":"70010948 - 1975 - Mercury distribution in ancient and modern sediment of northeastern Bering Sea","indexId":"70010948","publicationYear":"1975","noYear":false,"title":"Mercury distribution in ancient and modern sediment of northeastern Bering Sea"},"id":1}],"lastModifiedDate":"2013-01-24T14:24:55","indexId":"70010948","displayToPublicDate":"1975-01-01T00:00:00","publicationYear":"1975","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":"Mercury distribution in ancient and modern sediment of northeastern Bering Sea","docAbstract":"Reconnaissance sampling of surface and subsurface sediment to a maximum depth of 80 m below the sea floor shows that typical values of 0.03 p.p.m. and anomalies of 0.2-1.3 p.p.m. mercury have been present in northeastern Bering Sea since Early Pliocene time. Values are highest in modern beach (maximum 1.3 and mean 0.22 p.p.m. Hg) and nearshore subsurface gravels (maximum 0.6 and mean 0.06 p.p.m. Hg) along the highly mineralized Seward Peninsula and in clayey silt rich in organic matter (maximum 0.16 and mean 0.10 p.p.m. Hg) throughout the region. Although gold mining may be partly responsible for high mercury levels in the modern beach near Nome, Alaska (maximum 0.45 p.p.m.), equally high or greater concentrations of mercury occur in buried Pleistocene sediments immediately offshore (maximum 0.6 p.p.m.) and in modern unpolluted beach sediments at Bluff (maximum 1.3 p.p.m.); this suggests that the contamination effects of mining may be no greater than natural concentration processes in the Seward Peninsula region. The mercury content of offshore surface sediment, even adjacent to mercury-rich beaches, corresponds to that of unpolluted marine and fresh-water sediment elsewhere. The normal values that prevail offshore may be attributable to entrapment of mercury-bearing heavy minerals on beaches near sources and/or dilution effects of offshore sedimentation. The few minor anomalies offshore occur in glacial drift derived from mercury source regions of Chukotka (Siberia) and Seward Peninsula; Pleistocene shoreline processes have reworked the drift to concentrate the heavy metals. The distribution pattern of mercury indicates that particulate mercury-bearing minerals have not been widely dispersed from onland deposits in quantities sufficient to increase mercury levels above normal in offshore sediments of Bering Sea; however, it shows that natural sedimentary processes can concentrate this mercury in beaches of the coastal zone where there already is concern because of potential pollution from man's activities.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Marine Geology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","publisherLocation":"Amsterdam Netherlands","doi":"10.1016/0025-3227(75)90006-7","issn":"00253227","usgsCitation":"Nelson, C., Pierce, D., Leong, K., and Wang, F., 1975, Mercury distribution in ancient and modern sediment of northeastern Bering Sea: Marine Geology, v. 18, no. 3, p. 91-104, https://doi.org/10.1016/0025-3227(75)90006-7.","productDescription":"14 p.","startPage":"91","endPage":"104","costCenters":[{"id":387,"text":"Mineral Resources Program","active":true,"usgs":true}],"links":[{"id":220949,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":266423,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0025-3227(75)90006-7"}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 161.98,51.22 ], [ 161.98,66.05 ], [ -157.0,66.05 ], [ -157.0,51.22 ], [ 161.98,51.22 ] ] ] } } ] }","volume":"18","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a5401e4b0c8380cd6ce5c","contributors":{"authors":[{"text":"Nelson, C.H.","contributorId":88346,"corporation":false,"usgs":true,"family":"Nelson","given":"C.H.","email":"","affiliations":[],"preferred":false,"id":359957,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pierce, D.E.","contributorId":88083,"corporation":false,"usgs":true,"family":"Pierce","given":"D.E.","email":"","affiliations":[],"preferred":false,"id":359956,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Leong, Kam","contributorId":103660,"corporation":false,"usgs":true,"family":"Leong","given":"Kam","affiliations":[],"preferred":false,"id":359958,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Wang, F.F.H.","contributorId":87219,"corporation":false,"usgs":true,"family":"Wang","given":"F.F.H.","email":"","affiliations":[],"preferred":false,"id":359955,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70010989,"text":"70010989 - 1975 - Interstitial solutions and diagenesis in deeply buried marine sediments: Results from the Deep Sea Drilling Project","interactions":[],"lastModifiedDate":"2019-12-17T12:57:58","indexId":"70010989","displayToPublicDate":"1975-01-01T00:00:00","publicationYear":"1975","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":"Interstitial solutions and diagenesis in deeply buried marine sediments: Results from the Deep Sea Drilling Project","docAbstract":"<p><span>Through the Deep Sea Drilling Project samples of interstitial solutions of deeply buried marine sediments throughout the World Ocean have been obtained and analyzed. The studies have shown that in all but the most slowly deposited sediments pore fluids exhibit changes in composition upon burial. These changes can be grouped into a few consistent patterns that facilitate identification of the diagenetic reactions occurring in the sediments. Pelagic clays and slowly deposited (&lt;1 cm/10</span><sup>3</sup><span>yr) biogenic sediments are the only types that exhibit little evidence of reaction in the pore waters. In most biogenic sediments sea water undergoes considerable alteration. In sediments deposited at rates up to a few cm/10</span><sup>3</sup><span>&nbsp;yr the changes chiefly involve gains of Ca</span><sup>2+</sup><span>&nbsp;and Sr</span><sup>2+</sup><span>&nbsp;and losses of Mg</span><sup>2+</sup><span>&nbsp;which balance the Ca</span><sup>2+</sup><span>&nbsp;enrichment. The Ca-Mg substitution may often reach 30 mM/kg while Sr</span><sup>2+</sup><span>&nbsp;may be enriched 15-fold over sea water. These changes reflect recrystallization of biogenic calcite and the substitution of Mg</span><sup>2+</sup><span>&nbsp;for Ca</span><sup>2+</sup><span>&nbsp;during this reaction. The Ca-Mg-carbonate formed is most likely a dolomitic phase. A related but more complex pattern is found in carbonate sediments deposited at somewhat greater rates. Ca</span><sup>2+</sup><span>&nbsp;and Sr</span><sup>2+</sup><span>&nbsp;enrichment is again characteristic, but Mg</span><sup>2+</sup><span>&nbsp;losses exceed Ca</span><sup>2+</sup><span>&nbsp;gains with the excess being balanced by SO</span><sub>4</sub><sup>post staggered2-</sup><span>&nbsp;losses. The data indicate that the reactions are similar to those noted above, except that the Ca</span><sup>2+</sup><span>&nbsp;released is not kept in solution but is precipitated by the HCO</span><sub>3</sub><sup>post staggered-</sup><span>&nbsp;produced in SO</span><sub>4</sub><sup>post staggered2-</sup><span>&nbsp;reduction. In both these types of pore waters Na</span><sup>+</sup><span>&nbsp;is usually conservative, but K</span><sup>+</sup><span>&nbsp;depletions are frequent. In several partly consolidated sediment sections approaching igneous basement contact, very marked interstitial calcium enrichment has been found (to 5.5 g/kg). These phenomena are marked by pronounced depletion in Na</span><sup>+</sup><span>, Si and CO</span><sub>2</sub><span>, and slight enhancement in Cl</span><sup>-</sup><span>. The changes are attributed to exchange of Na</span><sup>+</sup><span>&nbsp;for Ca</span><sup>2+</sup><span>&nbsp;in silicate minerals forming from submarine weathering of igneous rocks such as basalts. Water is also consumed in these reactions, accounting for minor increases in total interstitial salinity. Terrigenous, organic-rich sediments deposited rapidly along continental margins also exhibit significant evidences of alteration. Microbial reactions involving organic matter lead to complete removal of SO</span><sub>4</sub><sup>post staggered2-</sup><span>, strong HCO</span><sub>3</sub><sup>post staggered-</sup><span>&nbsp;enrichment, formation of NH</span><sub>4</sub><sup>post staggered+</sup><span>, and methane synthesis from H</span><sub>2</sub><span>&nbsp;and CO</span><sub>2</sub><span>&nbsp;once SO</span><sub>4</sub><sup>post staggered2-</sup><span>&nbsp;is eliminated. K</span><sup>+</sup><span>&nbsp;and often Na</span><sup>+</sup><span>&nbsp;(slightly) are depleted in the interstitial waters. Ca</span><sup>2+</sup><span>&nbsp;depletion may occur owing to precipitation of CaCO</span><sub>3</sub><span>. In most cases interstitial Cl</span><sup>-</sup><span>&nbsp;remains relatively constant, but increases are noted over evaporitic strata, and decreases in interstitial Cl</span><sup>-</sup><span>&nbsp;are observed in some sediments adjacent to continents.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(75)90165-9","issn":"00167037","usgsCitation":"Sayles, F., and Manheim, F., 1975, Interstitial solutions and diagenesis in deeply buried marine sediments: Results from the Deep Sea Drilling Project: Geochimica et Cosmochimica Acta, v. 39, no. 2, p. 103-127, https://doi.org/10.1016/0016-7037(75)90165-9.","productDescription":"25 p.","startPage":"103","endPage":"127","numberOfPages":"25","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":221419,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"39","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3db1e4b0c8380cd63772","contributors":{"authors":[{"text":"Sayles, F.L.","contributorId":77657,"corporation":false,"usgs":true,"family":"Sayles","given":"F.L.","email":"","affiliations":[],"preferred":false,"id":360035,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Manheim, F.T. 0000-0003-4005-4524","orcid":"https://orcid.org/0000-0003-4005-4524","contributorId":55421,"corporation":false,"usgs":true,"family":"Manheim","given":"F.T.","affiliations":[],"preferred":false,"id":360034,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1001316,"text":"1001316 - 1975 - Boreal owl taken near Watertown","interactions":[],"lastModifiedDate":"2018-01-05T10:26:45","indexId":"1001316","displayToPublicDate":"1975-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3441,"text":"South Dakota Bird Notes","active":true,"publicationSubtype":{"id":10}},"title":"Boreal owl taken near Watertown","docAbstract":"Abstract has not been submitted","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"South Dakota Bird Notes","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Rose, W., and Springer, P.F., 1975, Boreal owl taken near Watertown: South Dakota Bird Notes, v. 27, no. 4, p. 64-65.","productDescription":"2 p.","startPage":"64","endPage":"65","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":128939,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"27","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db602ac1","contributors":{"authors":[{"text":"Rose, W.A.","contributorId":93425,"corporation":false,"usgs":true,"family":"Rose","given":"W.A.","email":"","affiliations":[],"preferred":false,"id":310870,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Springer, P. F.","contributorId":56590,"corporation":false,"usgs":false,"family":"Springer","given":"P.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":310869,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70162244,"text":"70162244 - 1975 - Statistical methods for estimating normal blood chemistry ranges and variance in rainbow trout (Salmo gairdneri), Shasta Strain","interactions":[],"lastModifiedDate":"2016-01-19T14:30:23","indexId":"70162244","displayToPublicDate":"1975-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2543,"text":"Journal of the Fisheries Research Board of Canada","active":true,"publicationSubtype":{"id":10}},"title":"Statistical methods for estimating normal blood chemistry ranges and variance in rainbow trout (Salmo gairdneri), Shasta Strain","docAbstract":"<p><span>Gaussian and nonparametric (percentile estimate and tolerance interval) statistical methods were used to estimate normal ranges for blood chemistry (bicarbonate, bilirubin, calcium, hematocrit, hemoglobin, magnesium, mean cell hemoglobin concentration, osmolality, inorganic phosphorus, and pH for juvenile rainbow (</span><i>Salmo gairdneri</i><span>, Shasta strain) trout held under defined environmental conditions. The percentile estimate and Gaussian methods gave similar normal ranges, whereas the tolerance interval method gave consistently wider ranges for all blood variables except hemoglobin. If the underlying frequency distribution is unknown, the percentile estimate procedure would be the method of choice.</span></p>","language":"English","publisher":"NRC Research Press","doi":"10.1139/f75-069","usgsCitation":"Wedemeyer, G.A., and Nelson, N.C., 1975, Statistical methods for estimating normal blood chemistry ranges and variance in rainbow trout (Salmo gairdneri), Shasta Strain: Journal of the Fisheries Research Board of Canada, v. 32, no. 4, p. 551-554, https://doi.org/10.1139/f75-069.","productDescription":"4 p.","startPage":"551","endPage":"554","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":314482,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"32","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"569f6c53e4b0961cf27fd1cc","contributors":{"authors":[{"text":"Wedemeyer, Gary A.","contributorId":30668,"corporation":false,"usgs":true,"family":"Wedemeyer","given":"Gary","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":588970,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nelson, Nancy C.","contributorId":152336,"corporation":false,"usgs":false,"family":"Nelson","given":"Nancy","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":588971,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70162246,"text":"70162246 - 1975 - <i>Phoma herbarum</i>, a fungal plant saprophyte, as a fish pathogen","interactions":[],"lastModifiedDate":"2016-08-15T21:18:26","indexId":"70162246","displayToPublicDate":"1975-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2543,"text":"Journal of the Fisheries Research Board of Canada","active":true,"publicationSubtype":{"id":10}},"title":"<i>Phoma herbarum</i>, a fungal plant saprophyte, as a fish pathogen","docAbstract":"<p><i>Phoma herbarum</i><span>, a fungal plant saprophyte, was isolated from diseased hatchery-reared coho salmon (</span><i>Oncorhynchus kisutch</i><span>), chinook salmon (</span><i>O</i><span>.&nbsp;</span><i>tshawytscha</i><span>), and rainbow trout (</span><i>Salmo gairdneri</i><span>). The disease was observed at 10 national fish hatcheries in Washington and Oregon, but the low incidence of experimental infections indicate that it is only weakly contagious. Histopathological examination suggests that the air bladder is one of the primary organs infected. The visceral organs are also affected in both natural and experimental infections.</span></p>","language":"English","publisher":"NRC Research Press","doi":"10.1139/f75-193","usgsCitation":"Ross, A.J., Yasutake, W.T., and Leek, S., 1975, <i>Phoma herbarum</i>, a fungal plant saprophyte, as a fish pathogen: Journal of the Fisheries Research Board of Canada, v. 32, no. 9, p. 1648-1652, https://doi.org/10.1139/f75-193.","productDescription":"5 p.","startPage":"1648","endPage":"1652","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":314484,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"32","issue":"9","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"569f6c45e4b0961cf27fd1b5","contributors":{"authors":[{"text":"Ross, A. J.","contributorId":105267,"corporation":false,"usgs":true,"family":"Ross","given":"A.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":588973,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Yasutake, W. T.","contributorId":103222,"corporation":false,"usgs":true,"family":"Yasutake","given":"W.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":588974,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Leek, Steve","contributorId":152337,"corporation":false,"usgs":false,"family":"Leek","given":"Steve","affiliations":[],"preferred":false,"id":588975,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70162247,"text":"70162247 - 1975 - Kidney disease postorbital lesions in spring chinook salmon (Oncorhynchus tshawytscha)","interactions":[],"lastModifiedDate":"2016-01-19T14:47:00","indexId":"70162247","displayToPublicDate":"1975-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3624,"text":"Transactions of the American Fisheries Society","active":true,"publicationSubtype":{"id":10}},"title":"Kidney disease postorbital lesions in spring chinook salmon (Oncorhynchus tshawytscha)","docAbstract":"<p class=\"last\">Gross exophthalmos in one or both eyes of yearling spring chinook salmon (Oncorhynchus tshawytscha) was caused by postorbital, granulomatous inflammatory tissue that developed in response to invasion of the site by Corynebacterium sp., the causative agent of bacterial kidney disease.</p>","language":"English","publisher":"Taylor & Francis","doi":"10.1577/1548-8659(1975)104<805:KDPLIS>2.0.CO;2","usgsCitation":"Hendricks, J.D., and Leek, S.L., 1975, Kidney disease postorbital lesions in spring chinook salmon (Oncorhynchus tshawytscha): Transactions of the American Fisheries Society, v. 104, no. 4, p. 805-807, https://doi.org/10.1577/1548-8659(1975)104<805:KDPLIS>2.0.CO;2.","productDescription":"3 p.","startPage":"805","endPage":"807","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":314485,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"104","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"569f6c45e4b0961cf27fd1ad","contributors":{"authors":[{"text":"Hendricks, Jerry D.","contributorId":152338,"corporation":false,"usgs":false,"family":"Hendricks","given":"Jerry","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":588976,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Leek, Steve L.","contributorId":152339,"corporation":false,"usgs":false,"family":"Leek","given":"Steve","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":588977,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
]}