{"pageNumber":"6732","pageRowStart":"168275","pageSize":"25","recordCount":184552,"records":[{"id":2600,"text":"wsp1539V - 1963 - Availability of ground water in the Bear River valley, Wyoming, with a section on the chemical quality of the water","interactions":[],"lastModifiedDate":"2023-11-01T21:34:49.498797","indexId":"wsp1539V","displayToPublicDate":"1963-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1539","chapter":"V","title":"Availability of ground water in the Bear River valley, Wyoming, with a section on the chemical quality of the water","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1539V","usgsCitation":"Robinove, C.J., Berry, D.W., and Connor, J.G., 1963, Availability of ground water in the Bear River valley, Wyoming, with a section on the chemical quality of the water: U.S. Geological Survey Water Supply Paper 1539, Report: iv, 44 p.; 2 Plates: 25.00 x 42.75 inches and 27.00 x 11.88 inches, https://doi.org/10.3133/wsp1539V.","productDescription":"Report: iv, 44 p.; 2 Plates: 25.00 x 42.75 inches and 27.00 x 11.88 inches","costCenters":[],"links":[{"id":422319,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24743.htm","linkFileType":{"id":5,"text":"html"}},{"id":28882,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1539v/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28881,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1539v/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28880,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1539v/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138893,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1539v/report-thumb.jpg"}],"country":"United States","state":"Wyoming","otherGeospatial":"Bear River Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -110.8033,\n              42.221\n            ],\n            [\n              -111.048,\n              42.221\n            ],\n            [\n              -111.048,\n              41\n            ],\n            [\n              -110.8033,\n              41\n            ],\n            [\n              -110.8033,\n              42.221\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ee4b07f02db66035d","contributors":{"authors":[{"text":"Robinove, Charles Joseph","contributorId":71153,"corporation":false,"usgs":true,"family":"Robinove","given":"Charles","email":"","middleInitial":"Joseph","affiliations":[],"preferred":false,"id":145473,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Berry, Delmar W.","contributorId":25107,"corporation":false,"usgs":true,"family":"Berry","given":"Delmar","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":145472,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Connor, John G.","contributorId":34489,"corporation":false,"usgs":true,"family":"Connor","given":"John","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":887319,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70182047,"text":"70182047 - 1963 - Publications on fish parasites and diseases, 330 B.C.-A.D. 1923","interactions":[],"lastModifiedDate":"2017-02-15T14:01:26","indexId":"70182047","displayToPublicDate":"1963-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"title":"Publications on fish parasites and diseases, 330 B.C.-A.D. 1923","docAbstract":"<p>These references were collected in 1924, but until now this collection has been available only in manuscript:fbrm. Because of the current increased interest in this field, this bibliography is being issued to make it more generally accessible. They include the earliest known references to fish parasites (330 B. C.) as well as a nearly complete collection up to 1924. In some instances only one or two works of a more prolific re\"searcher are cited, therefore it is recommended that the student use the Index-Catalogue of Medical and Veterinary Zoology (U. S. Department of Agriculture) freely. For more current work consult the following, of which Dogiel et al.(1958), Hoffman and Sindermann (1962), Scha'perclaus (1954), and Snieszko et aL(in press) have extensive bibliographies</p>","language":"English","publisher":"U.S. Department of Interior Fish and Wildlife Service","usgsCitation":"McGregor, E., 1963, Publications on fish parasites and diseases, 330 B.C.-A.D. 1923, 89 p. .","productDescription":"89 p. ","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":335584,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58a5770fe4b057081a24eed5","contributors":{"authors":[{"text":"McGregor, E.A.","contributorId":152052,"corporation":false,"usgs":false,"family":"McGregor","given":"E.A.","email":"","affiliations":[],"preferred":false,"id":669383,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70010491,"text":"70010491 - 1963 - Implications of the minor element content of some major streams of the world","interactions":[],"lastModifiedDate":"2020-11-19T18:13:37.174725","indexId":"70010491","displayToPublicDate":"1963-01-01T00:00:00","publicationYear":"1963","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":"Implications of the minor element content of some major streams of the world","docAbstract":"<p>Of 15 or more minor elements in the world's principal river waters only aluminum, iron, manganese, barium and strontium range much over<span>&nbsp;</span><span class=\"math\"><span id=\"MathJax-Element-1-Frame\" class=\"MathJax_SVG\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;><mtext>100 &amp;#x3BC;g</mtext><mtext>l</mtext></math>\"><span class=\"MJX_Assistive_MathML\">100 μgl</span></span></span>. (parts per billion). Most minor elements range at or below<span>&nbsp;</span><span class=\"math\"><span id=\"MathJax-Element-2-Frame\" class=\"MathJax_SVG\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;><mtext>100 &amp;#x3BC;g</mtext><mtext>1</mtext></math>\"><span class=\"MJX_Assistive_MathML\">100 μg1</span></span></span>. and have median (or middle) values of 10 micrograms per liter or less. Significant areal differences in minor element content are found in the river waters. For example, Atlantic Coastal river waters in the aggregate are slightly more enriched in concentrations of silver, chromium, manganese, molybdenum, nickel, strontium and titanium, and slightly deficient in barium and lithium when compared with median values for North America. Median values of ratios<span>&nbsp;</span><span class=\"math\"><span id=\"MathJax-Element-3-Frame\" class=\"MathJax_SVG\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;><mtext>Ba</mtext><mtext>Sr</mtext></math>\"><span class=\"MJX_Assistive_MathML\">BaSr</span></span></span>,<span>&nbsp;</span><span class=\"math\"><span id=\"MathJax-Element-4-Frame\" class=\"MathJax_SVG\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;><mtext>Ni</mtext><mtext>Cr</mtext></math>\"><span class=\"MJX_Assistive_MathML\">NiCr</span></span></span><span>&nbsp;</span>and<span>&nbsp;</span><span class=\"math\"><span id=\"MathJax-Element-5-Frame\" class=\"MathJax_SVG\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;><mtext>Ni</mtext><mtext>Cu</mtext></math>\"><span class=\"MJX_Assistive_MathML\">NiCu</span></span></span><span>&nbsp;</span>are reasonably consistent (within a factor of two) in principal drainage from North America. Noteworthy are consistent median ratios of<span>&nbsp;</span><span class=\"math\"><span id=\"MathJax-Element-6-Frame\" class=\"MathJax_SVG\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;><mtext>Ni</mtext><mtext>Cu</mtext></math>\"><span class=\"MJX_Assistive_MathML\">NiCu</span></span></span><span>&nbsp;</span>for large rivers of United States, but the ratio tends to be slightly greater in global northern latitudes than in southern latitudes. Median values for aluminum, barium, copper, lead, molybdenum and silver in North American runoff are of the same order as published world averages for ocean water.</p><p>Hydrologic and geochemical aspects of continental runoff are strongly implied in observations of minor element content of large rivers. Evidence to date is that median values of<span>&nbsp;</span><span class=\"math\"><span id=\"MathJax-Element-7-Frame\" class=\"MathJax_SVG\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;><mtext>Ba</mtext><mtext>Sr ratios</mtext></math>\"><span class=\"MJX_Assistive_MathML\">BaSr ratios</span></span></span><span>&nbsp;</span>are relatively uniform in global river waters. There is real danger in oversimplifying chemical systems in broad assessments of lower reaches of large drainage basins because individual hydrologic and chemical events upstream are largely obscured.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(63)90069-3","usgsCitation":"Durum, W.H., and Haffty, J., 1963, Implications of the minor element content of some major streams of the world: Geochimica et Cosmochimica Acta, v. 27, no. 1, p. 1-11, https://doi.org/10.1016/0016-7037(63)90069-3.","productDescription":"11 p.","startPage":"1","endPage":"11","numberOfPages":"11","costCenters":[],"links":[{"id":219306,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"27","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a392fe4b0c8380cd6182c","contributors":{"authors":[{"text":"Durum, W. H.","contributorId":78311,"corporation":false,"usgs":true,"family":"Durum","given":"W.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":359050,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Haffty, J.","contributorId":93187,"corporation":false,"usgs":true,"family":"Haffty","given":"J.","affiliations":[],"preferred":false,"id":359051,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70009997,"text":"70009997 - 1963 - New chemical determinations of zinc in basalts, and rocks of similar composition","interactions":[],"lastModifiedDate":"2020-11-19T17:54:18.433365","indexId":"70009997","displayToPublicDate":"1963-01-01T00:00:00","publicationYear":"1963","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":"New chemical determinations of zinc in basalts, and rocks of similar composition","docAbstract":"<p>New determinations of zinc in 124 basalts by the chemical method described (<span class=\"small-caps\">Huff-Man</span><i>et al.</i><span>&nbsp;</span>1963) are reported. Average zinc values, in per cent, for basalts from diverse regions are as follows: Idaho, 28 samples, 0.013; Hawaii, 33 samples, 0.010; Connecticut, 27 samples, 0.0090; Oregon, 17 samples, 0.0081; California, 8 samples, 0.0071; and New Mexico, 11 samples, 0.0086; average, all samples, 0.0099 per cent zinc.</p><p>A plot of differentiation indicator ratios calculated from the conventional rock analyses, CaO/(Na<sub>2</sub>O + K<sub>2</sub>O) as the ordinate and SiO<sub>2</sub>/MgO as the abscissa, was used to select, from different localities, samples essentially the same in chemical composition that were to be used for comparisons of zinc and other minor elements.</p><p>Zinc correlates with MnO and with total iron as FeO. An inverse relationship found for zinc and manganese is related to the total iron content of the basalts. Thus for a given iron concentration as zinc increases, manganese decreases and vice versa.</p><p>Ratios of zinc, the common denominator, to 11 other minor elements determined spectro-graphically show correlations with cobalt, gallium, scandium, yttrium, and zirconium.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(63)90020-6","usgsCitation":"Rader, L., Swadley, W.C., Huffman, C., and Lipp, H.H., 1963, New chemical determinations of zinc in basalts, and rocks of similar composition: Geochimica et Cosmochimica Acta, v. 27, no. 6, p. 695-714, https://doi.org/10.1016/0016-7037(63)90020-6.","productDescription":"20 p.","startPage":"695","endPage":"714","numberOfPages":"20","costCenters":[],"links":[{"id":218695,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"27","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a6560e4b0c8380cd72b94","contributors":{"authors":[{"text":"Rader, L. F.","contributorId":9730,"corporation":false,"usgs":true,"family":"Rader","given":"L. F.","affiliations":[],"preferred":false,"id":357617,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Swadley, W. C.","contributorId":46940,"corporation":false,"usgs":true,"family":"Swadley","given":"W.","middleInitial":"C.","affiliations":[],"preferred":false,"id":357619,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Huffman, C. Jr.","contributorId":20064,"corporation":false,"usgs":true,"family":"Huffman","given":"C.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":357618,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lipp, H. H.","contributorId":47906,"corporation":false,"usgs":true,"family":"Lipp","given":"H.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":357620,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70009998,"text":"70009998 - 1963 - Applications of geohydrologic concepts in geology","interactions":[],"lastModifiedDate":"2020-11-19T18:23:16.28895","indexId":"70009998","displayToPublicDate":"1963-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2342,"text":"Journal of Hydrology","active":true,"publicationSubtype":{"id":10}},"title":"Applications of geohydrologic concepts in geology","docAbstract":"<p>Subsurface water, an active agent in many geologic proceses, must be considered in interpreting geologic phenomena. Principles of the occurrence, distribution, and movement of subsurface waters are well established and readily applicable. In many interpretations in geologic literature, geohydrologic principles have been employed realistically, but in many others these principles have been either ignored or violated.</p><p>Explanations of genesis of underclays and associated deposits afford some examples wherein principles of movement and activity of vadose and ground water have been ignored and others in which they have been used advantageously. Postulates stating that waters percolate downward from swamp areas do not allow for the usual movement of subsurface water in such environments. The idea that sediments were leached by vadose water after uplift satisfies the geohydrologic requirements.</p><p>Weathering and solution form porous and permeable zones subjacent to unconformities in dense rocks such as carbonates and granites; this illustrates the geohydrologic and economic significance of unconformities. Examples are Mohawkian carbonate aquifers of northern Illinois and oil-bearing limestones of Mississippian age of eastern Montana.</p><p>The flushing effects of meteoric water and other hydrodynamic factors active during erosion periods are important elements in the genesis and concentration of brines. Explanation of the origin and occurrence of brines must include consideration of the geohydrologic environments throughout their geologic history.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0022-1694(63)90031-3","usgsCitation":"Maxey, G.B., and Hackett, J.E., 1963, Applications of geohydrologic concepts in geology: Journal of Hydrology, v. 1, no. 1, p. 35-45, https://doi.org/10.1016/0022-1694(63)90031-3.","productDescription":"11 p.","startPage":"35","endPage":"45","numberOfPages":"11","costCenters":[],"links":[{"id":218768,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"1","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059ecc7e4b0c8380cd4949e","contributors":{"authors":[{"text":"Maxey, G. B.","contributorId":76458,"corporation":false,"usgs":true,"family":"Maxey","given":"G.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":357622,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hackett, J. E.","contributorId":72119,"corporation":false,"usgs":true,"family":"Hackett","given":"J.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":357621,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70010839,"text":"70010839 - 1963 - Tertiary lake deposits in western coterminous United States","interactions":[],"lastModifiedDate":"2026-02-25T14:39:34.885888","indexId":"70010839","displayToPublicDate":"1963-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Tertiary lake deposits in western coterminous United States","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.139.3550.107","issn":"00368075","usgsCitation":"Feth, J.H., 1963, Tertiary lake deposits in western coterminous United States: Science, v. 139, no. 3550, p. 107-110.","productDescription":"4 p.","startPage":"107","endPage":"110","costCenters":[],"links":[{"id":219010,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","otherGeospatial":"western coterminous United States","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -125.96491923714473,\n              48.85986140208797\n            ],\n            [\n              -125.96491923714473,\n              31.6162602251043\n            ],\n            [\n              -101.27376596663822,\n              31.6162602251043\n            ],\n            [\n              -101.27376596663822,\n              48.85986140208797\n            ],\n            [\n              -125.96491923714473,\n              48.85986140208797\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"139","issue":"3550","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505ba579e4b08c986b320a8e","contributors":{"authors":[{"text":"Feth, J. H.","contributorId":50495,"corporation":false,"usgs":true,"family":"Feth","given":"J.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":359765,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70010841,"text":"70010841 - 1963 - Hydrogen-water vapor mixtures: Control of hydrothermal atmospheres by hydrogen osmosis","interactions":[],"lastModifiedDate":"2020-11-19T19:09:57.574769","indexId":"70010841","displayToPublicDate":"1963-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Hydrogen-water vapor mixtures: Control of hydrothermal atmospheres by hydrogen osmosis","docAbstract":"<p>Experiments at 700°C and 800 bars total pressure demonstrate positive deviations from ideality for mixtures of hydrogen and H<sub>2</sub>O gases. The deviations are greater than predicted with Stockmayer's method. The composition of the mixture and the fugacity of hydrogen are controlled by diffusing hydrogen through metallic membranes. The results give the fugacities of both H<sub>2</sub>O and oxygen.</p>","language":"English","publisher":"AAAS","doi":"10.1126/science.139.3560.1220","usgsCitation":"Shaw, H.R., 1963, Hydrogen-water vapor mixtures: Control of hydrothermal atmospheres by hydrogen osmosis: Science, v. 139, no. 3560, p. 1220-1222, https://doi.org/10.1126/science.139.3560.1220.","productDescription":"3 p.","startPage":"1220","endPage":"1222","numberOfPages":"3","costCenters":[],"links":[{"id":219012,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"139","issue":"3560","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3352e4b0c8380cd5eeea","contributors":{"authors":[{"text":"Shaw, H. R.","contributorId":23952,"corporation":false,"usgs":true,"family":"Shaw","given":"H.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":359767,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70175634,"text":"70175634 - 1963 - Ground-water discharge from the Edwards and associated limestones, 1955-62, San Antonio area, Texas","interactions":[],"lastModifiedDate":"2016-08-17T14:02:24","indexId":"70175634","displayToPublicDate":"1963-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5177,"text":"Edwards Underground Water District Bulletin","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"2","title":"Ground-water discharge from the Edwards and associated limestones, 1955-62, San Antonio area, Texas","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Edwards Underground Water District","usgsCitation":"Garza, S., 1963, Ground-water discharge from the Edwards and associated limestones, 1955-62, San Antonio area, Texas: Edwards Underground Water District Bulletin 2, 4 p.","productDescription":"4 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":326720,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57b58ad0e4b03bcb0104bbb8","contributors":{"authors":[{"text":"Garza, Sergio","contributorId":88713,"corporation":false,"usgs":true,"family":"Garza","given":"Sergio","email":"","affiliations":[],"preferred":false,"id":645899,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1000140,"text":"1000140 - 1963 - Age and growth of the whitefish in Lake Superior","interactions":[],"lastModifiedDate":"2013-02-04T11:54:57","indexId":"1000140","displayToPublicDate":"1963-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1663,"text":"Fishery Bulletin","printIssn":"0090-0656","active":true,"publicationSubtype":{"id":10}},"title":"Age and growth of the whitefish in Lake Superior","docAbstract":"The average annual commercial production of whitefish in the U.S. waters of Lake Superior dropped from 2,194,000 pounds in 1879-1908 to 504,000 pounds in 1911-59.  The modern production, though far below the earlier, has accounted for more than 10 percent of the total value of the fishery in all but one of the last 20 years. Data are given on growth rate, age and year-class composition, size distribution, and length-weight relation of 1,800 fish collected in 1957-59 at Bayfield, Wis., and Marquette, Whitefish Point, and Dollar Settlement, Mich.  Studies of the body-scale relation, sex ratio, and age and size at maturity were limited to fish collected at Bayfield. The age composition and mean age varied widely by port and year of capture. Oldest fish were those of the 1957 Bayfield samples which were dominated by age group VII and averaged 5.5 years old. The youngest were from Whitefish Point in 1959; age-group III was dominant, and the mean age was 3.2 years. The evidence on the strength of year classes was not clear-cut, but it was obvious that fluctuations in stocks of different areas were largely independent. The percentage of legal-size fish (17 inches or longer) in age groups ranged widely; only 8.6 percent of the V group were legal in the 1957 Bayfield collections, whereas 100 percent of fish of the same age were legal in the 1957-59 collections from Whitefish Point. The weight of whitefish in the combined samples increased as the 3.2408 power of the length. The growth rate from the fastest to the slowest growing stocks ranked as follows: Whitefish Point; Dollar Settlement and Marquette (fish from the two ports reversed ranks after 3 years); Bayfield. The major differences in growth in length among the various stocks occurred during the first years of life. Beyond the fifth year the annual increments were nearly the same in all stocks. The whitefish from Whitefish Point, Dollar Settlement, and Marquette are among the fastest growing in the Great Lakes. The differences among the Lake Superior stocks in age and year-class composition, and in growth rate offer convincing evidence that populations of different areas are entirely independent. The sexes were almost equally represented (51.5 percent males) in the combined Bayfield samples, but males were scarce in age groups older than VIII. Whitefish from Bayfield shorter than 14.5 inches were immature and those larger than 17.4 inches were mature. The youngest mature fish belonged to age-group V,and all older than the VII group were mature.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Fishery Bulletin","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Dryer, W.R., 1963, Age and growth of the whitefish in Lake Superior: Fishery Bulletin, v. 63, no. 1, p. 77-95.","productDescription":"19 p.","startPage":"77","endPage":"95","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":128720,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":266925,"type":{"id":11,"text":"Document"},"url":"https://fishbull.noaa.gov/63-1/dryer.pdf"}],"volume":"63","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae3e4b07f02db6896d5","contributors":{"authors":[{"text":"Dryer, William R.","contributorId":71921,"corporation":false,"usgs":true,"family":"Dryer","given":"William","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":308130,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70010840,"text":"70010840 - 1963 - Unmineralized fossil bacteria","interactions":[],"lastModifiedDate":"2020-11-19T19:07:51.975759","indexId":"70010840","displayToPublicDate":"1963-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Unmineralized fossil bacteria","docAbstract":"<p><span>Unmineralized bacterial cells, mostly Micrococcus sp., but including also Streptococcus sp. and Actinomyces sp., were found in enormous numbers in lake beds of the Newark Canyon Formation of Early Cretaceous age, Eureka County, Nevada. The micrococci are black, and have an average diameter about 0.5 µ. Similar black micrococci (0.4 to 0.7 µ) were found in profusion in the bottom mud of Green Lake, New York. About 80 percent of this mud consists of minute idiomorphic calcite crystals and about 20 percent of these contain enormous numbers of the black micrococci. It is suggested that the Early Cretaceous bacterial cells owe their preservation to occlusion in calcite crystals that grew in a black, bacterial mud in a meromictic lake in which part of the Newark Canyon Formation accumulated.</span></p>","language":"English","publisher":"AAAS","doi":"10.1126/science.141.3584.919","usgsCitation":"Bradley, W.H., 1963, Unmineralized fossil bacteria: Science, v. 141, no. 3584, p. 919-921, https://doi.org/10.1126/science.141.3584.919.","productDescription":"3 p.","startPage":"919","endPage":"921","numberOfPages":"3","costCenters":[],"links":[{"id":219011,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"141","issue":"3584","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bbcd7e4b08c986b328e32","contributors":{"authors":[{"text":"Bradley, W. H.","contributorId":102452,"corporation":false,"usgs":true,"family":"Bradley","given":"W.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":359766,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70010490,"text":"70010490 - 1963 - The precipitation of aluminum, iron and manganese at the junction of Deer Creek with the Snake River in Summit County, Colorado","interactions":[],"lastModifiedDate":"2020-11-19T18:11:13.397378","indexId":"70010490","displayToPublicDate":"1963-01-01T00:00:00","publicationYear":"1963","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":"The precipitation of aluminum, iron and manganese at the junction of Deer Creek with the Snake River in Summit County, Colorado","docAbstract":"<p>The oxidation of disseminated pyrite in relatively acid schists and gneisses of the Snake River drainage basin provides abundant iron sulfate and sulfuric acid to ground and surface water. This acid water dissolves large quantities of many elements, particularly aluminum and surprisingly large quantities of elements, such as magnesium and zinc, not expected to be abundant in the drainage basin. The adjoining drainage to the west, Deer Creek, is underlain by basic rocks, from which the water inherits a high pH. Despite the presence of base- and precious- metal veins in the drainage basin of Deer Creek, it carries less metal than the Snake River.</p><p>The principal precipitate on the bed of the Snake River is hydrated iron oxide with small quantities of the other metals. In Deer Creek manganese oxide is precipitated with iron oxide and large quantities of other metals are carried down with this precipitate. Below the junction of these streams the pH stabilizes at a near-neutral value. Iron is removed from the Snake River water at the junction, and aluminum is precipitated for some distance downstream. The aluminum precipitate carries down other metals in concentrations slightly less than that in the manganese precipitate on Deer Creek. The natural processes observed in this junction if carried to a larger scale could provide the mechanism described by<span>&nbsp;</span><span class=\"small-caps\">Ansheles</span><span>&nbsp;</span>(1927) for the formation of bauxite. In the environment described, geochemical exploration by either water or stream sediment techniques is difficult because of (1) the extreme pH differential between the streams above their junction and (2) the difference in the precipitates formed on the streambeds.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(63)90053-X","usgsCitation":"Theobald, P.K., Lakin, H.W., and Hawkins, D.B., 1963, The precipitation of aluminum, iron and manganese at the junction of Deer Creek with the Snake River in Summit County, Colorado: Geochimica et Cosmochimica Acta, v. 27, no. 2, p. 121-132, https://doi.org/10.1016/0016-7037(63)90053-X.","productDescription":"14 p.","startPage":"121","endPage":"132","costCenters":[],"links":[{"id":219305,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Colorado","county":"Summit County","otherGeospatial":"Deer Creek, Snake River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -105.8639144897461,\n              39.558671574992374\n            ],\n            [\n              -105.85376501083374,\n              39.558671574992374\n            ],\n            [\n              -105.85376501083374,\n              39.56662843724411\n            ],\n            [\n              -105.8639144897461,\n              39.56662843724411\n            ],\n            [\n              -105.8639144897461,\n              39.558671574992374\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"27","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505baec1e4b08c986b3242fc","contributors":{"authors":[{"text":"Theobald, P. K. Jr.","contributorId":70398,"corporation":false,"usgs":true,"family":"Theobald","given":"P.","suffix":"Jr.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":359049,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lakin, H. W.","contributorId":11594,"corporation":false,"usgs":true,"family":"Lakin","given":"H.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":359047,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hawkins, D. B.","contributorId":43366,"corporation":false,"usgs":true,"family":"Hawkins","given":"D.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":359048,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70010783,"text":"70010783 - 1963 - Heat capacity from 12 to 305°K and entropy of talc and tremolite","interactions":[],"lastModifiedDate":"2020-11-19T18:57:32.705083","indexId":"70010783","displayToPublicDate":"1963-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2423,"text":"Journal of Physical Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"Heat capacity from 12 to 305°K and entropy of talc and tremolite","docAbstract":"<p>The heat capacities of talc, Mg<sub>3</sub>Si<sub>4</sub>O<sub>10</sub>(OH)<sub>2</sub>, and tremolite, Ca<sub>2</sub>Mg<sub>6</sub>Si<sub>8</sub>O<sub>22</sub>(OH)<sub>2</sub>, have been measured between 12 and 305°K. Smoothed values of heat capacity, entropy, enthalpy, and free energy are tabulated. At 298.15° K. the values of the thermodynamic functions are: talc, C<sub>p</sub>°= 76.89 <span>±</span>&nbsp;0.23 cal. deg.<sup>-1</sup> mole<sup>-1</sup>, S° = 62.33<span class=\"nowrap\"><span>&nbsp;</span></span><span>±</span><span>&nbsp;</span>0.19 cal. deg.<sup>-1</sup> mole<sup>-1</sup>, H° - H<sub>0</sub>° = 11,206&nbsp;<span>±</span>&nbsp;34 cal. mole<sup>-1</sup>; tremolite, Cp° = 156.7<span class=\"nowrap\"><span>&nbsp;</span></span><span>±</span><span>&nbsp;</span>0.6 cal. deg.<sup>-1</sup> mole<sup>-1</sup>, S° = 131.2<span class=\"nowrap\"><span>&nbsp;</span></span><span>±</span><span>&nbsp;</span>0.5 cal. deg.<sup>-1</sup> mole<sup>-1</sup>, H° - H<sub>0</sub>° = 23,335<span class=\"nowrap\"><span>&nbsp;</span></span><span>±</span><span>&nbsp;</span>90 cal. mole<sup>-1</sup>. From the equilibrium data of Bowen and Tuttle and the entropy of talc, the heat of formation of talc from MgO, SiO<sub>2</sub>, and H<sub>2</sub>O (liq.) is calculated to be <span>Δ</span>H°f<sub>298</sub> = -43.6<span class=\"nowrap\"><span>&nbsp;</span></span><span>±</span><span>&nbsp;</span>1 kcal.</p>","language":"English","publisher":"ACS Publications","doi":"10.1021/j100805a003","usgsCitation":"Robie, R.A., and Stout, J.W., 1963, Heat capacity from 12 to 305°K and entropy of talc and tremolite: Journal of Physical Chemistry, v. 67, no. 11, p. 2252-2256, https://doi.org/10.1021/j100805a003.","productDescription":"5 p.","startPage":"2252","endPage":"2256","numberOfPages":"5","costCenters":[],"links":[{"id":219712,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"67","issue":"11","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","scienceBaseUri":"505a2ff3e4b0c8380cd5d241","contributors":{"authors":[{"text":"Robie, R. A.","contributorId":71237,"corporation":false,"usgs":true,"family":"Robie","given":"R.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":359638,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stout, J. W.","contributorId":53943,"corporation":false,"usgs":true,"family":"Stout","given":"J.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":359637,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2000028,"text":"2000028 - 1963 - The use of alkalinity and conductivity measurements to estimate concentrations of 3-trifluormethyl-4-nitrophenol required for treating lamprey streams","interactions":[],"lastModifiedDate":"2012-02-02T00:14:56","indexId":"2000028","displayToPublicDate":"1963-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":3,"text":"Organization Series"},"seriesTitle":{"id":222,"text":"Technical Report","active":false,"publicationSubtype":{"id":3}},"seriesNumber":"7","title":"The use of alkalinity and conductivity measurements to estimate concentrations of 3-trifluormethyl-4-nitrophenol required for treating lamprey streams","docAbstract":"A method has been devised to estimate the minimum concentration of TFM that will kill sea lampreys and the maximum that will not kill fish.  It is based on the relation of these concentrations to the alkalinity and the conductivity of various waters.  Pretreatment bioassays will continue to be required for precise determination of treatment concentrations, but the estimates made possible by the method will permit a great reduction in the number of bioassays on a single stream.","language":"English","publisher":"Great Lakes Fishery Commission","collaboration":"Out-of-print","usgsCitation":"Kanayama, R.K., 1963, The use of alkalinity and conductivity measurements to estimate concentrations of 3-trifluormethyl-4-nitrophenol required for treating lamprey streams: Technical Report 7, 10 p.","productDescription":"10 p.","startPage":"0","endPage":"10","numberOfPages":"10","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":198774,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":92068,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://www.glfc.org/pubs/TechReports/Tr07.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4efc","contributors":{"authors":[{"text":"Kanayama, Richard K.","contributorId":102974,"corporation":false,"usgs":true,"family":"Kanayama","given":"Richard","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":324951,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70195915,"text":"70195915 - 1963 - Late Pleistocene glacial drainage in the Devils Lake Region, North Dakota","interactions":[],"lastModifiedDate":"2018-03-07T16:17:10","indexId":"70195915","displayToPublicDate":"1963-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1723,"text":"GSA Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Late Pleistocene glacial drainage in the Devils Lake Region, North Dakota","docAbstract":"<p><span>The Devils Lake region of northeastern North Dakota is covered with glacial drift deposited by the Leeds lobe of the Mankato Substage of the Wisconsin Stage of the Pleistocene and is underlain by Pierre Shale of Cretaceous age. Associated with the Sheyenne River, which flows through the southern part of the region in a deep trench, are many stream terraces, spillways, deposits of ice-contact stratified drift, and eroded ground-moraine areas. Six stages of drainage have been established to which these various features can be assigned. In the first two stages the features formed as melt water drained to the glacial James River south of the region and as the ice front stood at and later retreated from the site of the Heimdal moraine, a recessional moraine of the Leeds lobe. The later stages occurred after the valley of the Sheyenne River was free of ice and after glacial Lake Souris northwest of the region drained down the valley to glacial Lake Agassiz in the eastern part of the state. Features originating during the four later stages are largely related to the deposition of the North Viking moraine (another, more northern, recessional moraine of the Leeds lobe) and subsequent retreat of the ice from the moraine. Discharge from the local Devils and Stump lakes and from glacial Lake Souris also were of considerable importance in the genesis of many features.</span></p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1963)74[859:LPGDIT]2.0.CO;2","usgsCitation":"Aronow, S., 1963, Late Pleistocene glacial drainage in the Devils Lake Region, North Dakota: GSA Bulletin, v. 74, no. 7, p. 859-874, https://doi.org/10.1130/0016-7606(1963)74[859:LPGDIT]2.0.CO;2.","productDescription":"16 p.","startPage":"859","endPage":"874","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":352309,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"North Dakota","otherGeospatial":"Devils Lake","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -99.25,\n              47.75\n            ],\n            [\n              -98.25,\n              47.75\n            ],\n            [\n              -98.25,\n              48\n            ],\n            [\n              -99.25,\n              48\n            ],\n            [\n              -99.25,\n              47.75\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"74","issue":"7","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5aff6264e4b0da30c1bfde80","contributors":{"authors":[{"text":"Aronow, Saul","contributorId":59509,"corporation":false,"usgs":true,"family":"Aronow","given":"Saul","email":"","affiliations":[],"preferred":false,"id":730482,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":4091,"text":"cir478 - 1963 - Floods in Wyoming, magnitude and frequency","interactions":[],"lastModifiedDate":"2023-04-27T19:49:17.622715","indexId":"cir478","displayToPublicDate":"1963-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"478","title":"Floods in Wyoming, magnitude and frequency","docAbstract":"<p>This report contains the results of four separate flood-frequency analyses designated A, B, C, and D. Analysis A is for the portion of Wyoming east of the Continental Divide. Analysis B applies to the portion of Wyoming in Part 9, as designated in streamflow reports entitled \"Surface Water Supply of the United Stated\" published by the U.S. Geological Survey, and was extracted fro.m an unpublished study by W. P. Somers in 1959. Analysis C applies to Part 10 and was extracted from Circutar 457 (Berwick, 1962). Analysis D applies to Part 13 and was extracted from a report by C. A. Thomas, H. C. Broom, and J. E. Cummans (1963).</p><p>Methods described in this report can be used to estimate the magnitude of a flood of any selected recurrence interval between 1.1 and 50 years for any unregulated stream in Wyoming, gaged or ungaged, within the scope of the data. Flood-frequency relations are not defined for a large part of the North Platte River basin in south-central Wyoming because of insufficient data. </p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir478","collaboration":"Prepared in cooperation with Wyoming State Highway Department","usgsCitation":"Carter, J.R., and Green, A.R., 1963, Floods in Wyoming, magnitude and frequency: U.S. Geological Survey Circular 478, Report: iv, 27 p.; 2 Plates: 9.36 x 12.59 and 9.18 x 12.67 inches, https://doi.org/10.3133/cir478.","productDescription":"Report: iv, 27 p.; 2 Plates: 9.36 x 12.59 and 9.18 x 12.67 inches","numberOfPages":"32","costCenters":[],"links":[{"id":416456,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_23527.htm","linkFileType":{"id":5,"text":"html"}},{"id":31192,"rank":4,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/0478/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":271068,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/circ/0478/plate-1.pdf"},{"id":271069,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/circ/0478/plate-2.pdf"},{"id":124473,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/0478/report-thumb.jpg"}],"country":"United States","state":"Wyoming","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -111.0569,40.9947 ], [ -111.0569,45.0059 ], [ -104.0522,45.0059 ], [ -104.0522,40.9947 ], [ -111.0569,40.9947 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699af5","contributors":{"authors":[{"text":"Carter, J. R.","contributorId":23128,"corporation":false,"usgs":true,"family":"Carter","given":"J.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":148173,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Green, A. Rice","contributorId":31731,"corporation":false,"usgs":true,"family":"Green","given":"A.","email":"","middleInitial":"Rice","affiliations":[],"preferred":false,"id":148174,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2785,"text":"wsp1765 - 1963 - A layman's look at water in Alabama","interactions":[],"lastModifiedDate":"2023-11-30T20:49:20.940514","indexId":"wsp1765","displayToPublicDate":"1963-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1765","title":"A layman's look at water in Alabama","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1765","usgsCitation":"Swindel, G.W., Williams, M., Geurin, J.W., and Baldwin, H.L., 1963, A layman's look at water in Alabama: U.S. Geological Survey Water Supply Paper 1765, v, 89 p., https://doi.org/10.3133/wsp1765.","productDescription":"v, 89 p.","costCenters":[],"links":[{"id":423107,"rank":3,"type":{"id":36,"text":"NGMDB Index 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,{"id":1149,"text":"wsp1669C - 1963 - Hydrology of upper Black Earth Creek basin, Wisconsin, with a section on surface water","interactions":[{"subject":{"id":52076,"text":"ofr6029 - 1960 - A preliminary report of the geology and ground-water resources of Upper Black Earth Creek Basin, Wisconsin, with a section on surface water","indexId":"ofr6029","publicationYear":"1960","noYear":false,"title":"A preliminary report of the geology and ground-water resources of Upper Black Earth Creek Basin, Wisconsin, with a section on surface water"},"predicate":"SUPERSEDED_BY","object":{"id":1149,"text":"wsp1669C - 1963 - Hydrology of upper Black Earth Creek basin, Wisconsin, with a section on surface water","indexId":"wsp1669C","publicationYear":"1963","noYear":false,"chapter":"C","title":"Hydrology of upper Black Earth Creek basin, Wisconsin, with a section on surface water"},"id":1}],"lastModifiedDate":"2023-11-27T21:46:12.820397","indexId":"wsp1669C","displayToPublicDate":"1963-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1669","chapter":"C","title":"Hydrology of upper Black Earth Creek basin, Wisconsin, with a section on surface water","docAbstract":"<p>The upper Black Earth Creek drainage basin has an area of 46 square miles and is in Dane County in south-central Wisconsin. The oldest rock exposed in the valley walls is the sandstone of Late Cambrian age. Dolomite of the Prairie du Chien Group of Ordovician age overlies the sandstone and forms the. resistant cap on the hills. The St. Peter Sandstone, Platteville and Decorah Formations, and Galena Dolomite, all Ordovician in age, form a narrow belt along the southern boundary of the area. Outwash and alluvium of Pleistocene and Recent age fill the valleys. The eastern half of the area was glaciated and is covered with till. The sandstone of Late Cambrian age and the sand and gravel of the outwash deposits are hydraulically connected. Ground water occurs under unconfined (water-table) conditions in the western unglaciated part of the basin and under artesian conditions beneath the till locally in the eastern part. The source of most of the ground water is direct infiltration of precipitation; however, some ground water enters the area as underflow from the south. About 7 inches of the 30 inches of average annual precipitation recharges the ground-water reservoir. The ground water generally moves toward Black Earth Creek where it is discharged. Some ground water moves out of the basin as underflow beneath the valley of Black Earth Creek, and some is discharged by evapotranspiration or is withdrawn by pumping from wells. Water levels in shallow nonartesian wells respond rapidly to precipitation. The effect of precipitation on water levels in artesian wells is slower and more subdued. Water levels are generally highest in spring and lowest in fall and winter. The flow of upper Black Earth Creek is derived mostly from ground-water discharge, except during short periods of and immediately after precipitation when most of the flow is derived from surface runoff. The runoff from upper Black Earth Creek basin decreased from an average of 8.72 inches per square mile of drainage area in 1955 to 5.55 inches in 1958; the decrease reflects the generally decreasing precipitation and declining water levels in the basin during that period. On July 10, 1958, the discharge from the basin was 0.367 cubic feet per second per square mile, and the greatest discharge was 0.84 cubic feet per second per square mile from the southwest subbasin. The ground water has an average temperature of about 50°F. It is a calcium magnesium bicarbonate type water and is very hard.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Contributions to the hydrology of the United States (Water-Supply Paper 1669)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1669C","collaboration":"Prepared in cooperation with the Wisconsin Geological and Natural History Survey","usgsCitation":"Cline, D.R., and Busby, M., 1963, Hydrology of upper Black Earth Creek basin, Wisconsin, with a section on surface water: U.S. Geological Survey Water Supply Paper 1669, Report: iv, 27 p.; 5 Plates:18.00 x 15.65 inches or smaller, https://doi.org/10.3133/wsp1669C.","productDescription":"Report: iv, 27 p.; 5 Plates:18.00 x 15.65 inches or smaller","numberOfPages":"32","onlineOnly":"N","additionalOnlineFiles":"Y","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":25944,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1669c/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137643,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1669c/report-thumb.jpg"},{"id":25940,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1669c/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25939,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1669c/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":422984,"rank":8,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24862.htm","linkFileType":{"id":5,"text":"html"}},{"id":25941,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1669c/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25943,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1669c/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25942,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1669c/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Wisconsin","county":"Dane County","otherGeospatial":"Black Earth Creek","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -89.81494903564453,\n              43.04079076668198\n            ],\n            [\n              -89.81494903564453,\n              43.21193220073775\n            ],\n            [\n              -89.52999114990234,\n              43.21193220073775\n            ],\n            [\n              -89.52999114990234,\n              43.04079076668198\n            ],\n            [\n              -89.81494903564453,\n              43.04079076668198\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fc7d5","contributors":{"authors":[{"text":"Cline, Denzel R.","contributorId":87910,"corporation":false,"usgs":true,"family":"Cline","given":"Denzel","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":143260,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Busby, Mark W.","contributorId":83099,"corporation":false,"usgs":true,"family":"Busby","given":"Mark W.","affiliations":[],"preferred":false,"id":143259,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1000471,"text":"1000471 - 1963 - Food of the bloater, Coregonus hoyi, in Lake Michigan","interactions":[],"lastModifiedDate":"2016-02-29T10:28:56","indexId":"1000471","displayToPublicDate":"1963-01-01T00:00:00","publicationYear":"1963","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":"Food of the bloater, Coregonus hoyi, in Lake Michigan","docAbstract":"<p>Stomachs were examined from 1,469 Lake Michigan bloaters, Coregonus [Leucichthys] hoyi, greater than 7 inches long which contained identifiable food. An additional 461 ciscoes less than 7 inches long were incorporated into the study; these latter fish were not positively identified, but most of them undoubtedly were bloaters. The specimens were caught in bottom nets except for 49, all less than 6 inches long, taken in midwater trawls. Lake Michigan bloaters under 7 inches long depend heavily on zooplankton. Those larger than 7 inches feed predominantly on Pontoporeia affinis and Mysis relicta, although fish of the 7.0- to 7.9-inch size range commonly eat zooplankton, expecially in shallower water. Generally, Mysis becomes more important, and Pontoporeia less so, as the depth increases and as the season progresses from spring to fall. Incidence of Pontoporeia increases and that of Mysis declines as the fish size increases. Other food items, in decreasing order of importance, are fingernail clams, midges (all stages of development), fish eggs, ostracods, and miscellaneous adult and immature insects other than midges.</p>","language":"English","doi":"10.1577/1548-8659(1963)92[245:FOTBCH]2.0.CO;2","usgsCitation":"Wells, L., and Beeton, A.M., 1963, Food of the bloater, Coregonus hoyi, in Lake Michigan: Transactions of the American Fisheries Society, v. 92, no. 3, p. 245-255, https://doi.org/10.1577/1548-8659(1963)92[245:FOTBCH]2.0.CO;2.","productDescription":"11 p.","startPage":"245","endPage":"255","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":133681,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"92","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d6e4b07f02db5de4f2","contributors":{"authors":[{"text":"Wells, LaRue","contributorId":75476,"corporation":false,"usgs":true,"family":"Wells","given":"LaRue","email":"","affiliations":[],"preferred":false,"id":308593,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Beeton, Alfred M.","contributorId":94247,"corporation":false,"usgs":true,"family":"Beeton","given":"Alfred","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":308594,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1003292,"text":"1003292 - 1963 - Dim and bright views on trout","interactions":[],"lastModifiedDate":"2012-02-02T00:04:09","indexId":"1003292","displayToPublicDate":"1963-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3657,"text":"Trout","active":true,"publicationSubtype":{"id":10}},"title":"Dim and bright views on trout","docAbstract":"Abstract has not been submitted","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Trout","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Lennon, R.E., 1963, Dim and bright views on trout: Trout, v. 4, no. 5, p. 7-8.","productDescription":"pp. 7-8","startPage":"7","endPage":"8","numberOfPages":"2","costCenters":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":129589,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"4","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a96e4b07f02db65abf1","contributors":{"authors":[{"text":"Lennon, R. E.","contributorId":37275,"corporation":false,"usgs":true,"family":"Lennon","given":"R.","middleInitial":"E.","affiliations":[],"preferred":false,"id":313078,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1001484,"text":"1001484 - 1963 - Pseudo-sleeping attitude of the canvasback","interactions":[],"lastModifiedDate":"2023-11-26T16:00:45.121375","indexId":"1001484","displayToPublicDate":"1963-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1318,"text":"Condor","active":true,"publicationSubtype":{"id":10}},"title":"Pseudo-sleeping attitude of the canvasback","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Oxford Academic","usgsCitation":"Cornwell, G., and Bartonek, J., 1963, Pseudo-sleeping attitude of the canvasback: Condor, v. 65, no. 5, p. 444-446.","productDescription":"3 p.","startPage":"444","endPage":"446","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":128725,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"65","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a90e4b07f02db6561c7","contributors":{"authors":[{"text":"Cornwell, G.W.","contributorId":18708,"corporation":false,"usgs":true,"family":"Cornwell","given":"G.W.","email":"","affiliations":[],"preferred":false,"id":311118,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bartonek, James C.","contributorId":38085,"corporation":false,"usgs":true,"family":"Bartonek","given":"James C.","affiliations":[],"preferred":false,"id":311119,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":96388,"text":"96388 - 1963 - Common plants and animals of Memorial Park","interactions":[],"lastModifiedDate":"2012-07-06T01:01:41","indexId":"96388","displayToPublicDate":"1963-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":4,"text":"Book"},"title":"Common plants and animals of Memorial Park","docAbstract":"No abstract available at this time","language":"English","publisher":"San Mateo County (Calif.) Department of Parks and Recreation","usgsCitation":"Rathbun, G.B., 1963, Common plants and animals of Memorial Park, 19 p.","productDescription":"19 p.","numberOfPages":"19","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":127699,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","county":"San Mateo County","otherGeospatial":"Memorial Park","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae5ec","contributors":{"authors":[{"text":"Rathbun, G. B.","contributorId":106044,"corporation":false,"usgs":true,"family":"Rathbun","given":"G.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":299553,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":96387,"text":"96387 - 1963 - Common mammals, birds, reptiles, and shrubs of Huddart Park","interactions":[],"lastModifiedDate":"2012-07-06T01:01:41","indexId":"96387","displayToPublicDate":"1963-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":4,"text":"Book"},"title":"Common mammals, birds, reptiles, and shrubs of Huddart Park","docAbstract":"No abstract available at this time","language":"English","publisher":"San Mateo County (Calif.) Department of Parks and Recreation","usgsCitation":"Rathbun, G.B., 1963, Common mammals, birds, reptiles, and shrubs of Huddart Park, 12 p.","productDescription":"12 p.","numberOfPages":"12","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":127698,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","county":"San Mateo County","otherGeospatial":"Huddart Park","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae5f0","contributors":{"authors":[{"text":"Rathbun, G. B.","contributorId":106044,"corporation":false,"usgs":true,"family":"Rathbun","given":"G.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":299552,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1007572,"text":"1007572 - 1963 - Population analyses, variation and behavior of Anguispira alternata alternata","interactions":[],"lastModifiedDate":"2016-09-27T16:36:51","indexId":"1007572","displayToPublicDate":"1963-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3634,"text":"Transactions of the Kansas Academy of Science","active":true,"publicationSubtype":{"id":10}},"title":"Population analyses, variation and behavior of Anguispira alternata alternata","docAbstract":"<p><i> Anguispira alternata alternata</i> is one of the more common terrestrial snails in the United States. Gregarious by nature, these snails can be collected in large numbers from wooded flood-plains and moist upland wooded areas. \"The range is eastern Canada and the United States, from Nova Scotia to Lake of the Woods; westward in the United States to about the 97th meridian, south to middle Louisiana and Mississippi (Leonard, 1959). Distribution in Kansas is restricted to the eastern one-third of the state.</p>","language":"English","publisher":"Kansas Academy of Science","doi":"10.2307/3626559","usgsCitation":"Douglas, C.L., 1963, Population analyses, variation and behavior of Anguispira alternata alternata: Transactions of the Kansas Academy of Science, v. 66, p. 186-194, https://doi.org/10.2307/3626559.","productDescription":"9 p.","startPage":"186","endPage":"194","numberOfPages":"9","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":130169,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"66","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad6e4b07f02db684345","contributors":{"authors":[{"text":"Douglas, Charles L.","contributorId":10742,"corporation":false,"usgs":true,"family":"Douglas","given":"Charles","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":315648,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1014233,"text":"1014233 - 1963 - Studies on Neogogatea kentuckiensis (Cable, 1935) n. comb.: (Trematoda: Strigeoidea: Cyathocotylidae)","interactions":[],"lastModifiedDate":"2025-05-01T15:02:15.154044","indexId":"1014233","displayToPublicDate":"1963-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2414,"text":"Journal of Parasitology","active":true,"publicationSubtype":{"id":10}},"title":"Studies on Neogogatea kentuckiensis (Cable, 1935) n. comb.: (Trematoda: Strigeoidea: Cyathocotylidae)","docAbstract":"<p><span>The cercaria of <i>N. kentuckiensis</i> was found in <i>Anaplocamus dilatatus</i> (<i>Nitrocris d.</i>) and <i>Mudalia carinata</i>. The metacercaria was found in all fishes examined from Opequon River, West Virginia, except <i>Cottus bairdi</i> which was also refractory to experimental infection. Two species of Centrarchidae, four of Cyprinidae, three of Salmonidae, <i>Etheostoma flabellare</i>, <i>Platypoecilus maculatus</i>, and <i>Trichogaster trichopterus</i> were experimentally infected. The development of the metacercaria and cyst and effect on the fish are described. The histopathology initially consists of hemorrhage and muscle necrosis about the metacercaria, followed by reorganization and formation of a loose connective tissue cyst. The controversial adult names are discussed and an emendation of the genus <i>Neogogatea</i> is presented.</span></p>","language":"English","publisher":"American Society of Parasitologists","doi":"10.2307/3275915","usgsCitation":"Hoffman, G.L., and Dunbar, C.E., 1963, Studies on Neogogatea kentuckiensis (Cable, 1935) n. comb.: (Trematoda: Strigeoidea: Cyathocotylidae): Journal of Parasitology, v. 49, no. 5, p. 737-744, https://doi.org/10.2307/3275915.","productDescription":"8 p.","startPage":"737","endPage":"744","numberOfPages":"8","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":487910,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.2307/3275915","text":"Publisher Index Page"},{"id":131708,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"49","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699d74","contributors":{"authors":[{"text":"Hoffman, G. L.","contributorId":70713,"corporation":false,"usgs":true,"family":"Hoffman","given":"G.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":320006,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dunbar, C. E.","contributorId":96623,"corporation":false,"usgs":true,"family":"Dunbar","given":"C.","middleInitial":"E.","affiliations":[],"preferred":false,"id":320007,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1014271,"text":"1014271 - 1963 - Two new Gyrodactylus (Trematoda: Monogenea) from cyprinid fishes with synopsis of those found on North American fishes","interactions":[],"lastModifiedDate":"2025-05-01T15:05:00.807077","indexId":"1014271","displayToPublicDate":"1963-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2414,"text":"Journal of Parasitology","active":true,"publicationSubtype":{"id":10}},"title":"Two new Gyrodactylus (Trematoda: Monogenea) from cyprinid fishes with synopsis of those found on North American fishes","docAbstract":"<p><span><i>Gyrodactylus atratuli</i> from the blacknose dace (<i>Rhinichthys atratulus</i>) and the pearl dace (<i>Semotilus margarita</i>) is compared with known species of <i>Gyrodactylus</i> from North American fishes and described as a new species. <i>Gyrodactylus margaritae</i> from the pearl dace (<i>Semotilus margarita</i>) is compared with known species of <i>Gyrodactylus</i> from North American fishes and described as a new species. The average number of <i>G. atratuli</i> per blacknose dace in the natural habitat is 7.8 (1 to 32) and in the laboratory at the same water temperature after 55 days in captivity, 5.4 (0 to 11). <i>G. atratuli</i> and <i>G. margaritae</i> fail to live and reproduce on fish kept in nonrunning water at between 19 and 26 C in laboratory aquaria, but will live and reproduce in running spring water at 12 C in laboratory aquaria. An illustrated synopsis with a comparative table of measurements of known North American <i>Gyrodactylus</i> and a list of the species with brief reference to their differentiating characteristics are given.</span></p>","language":"English","publisher":"American Society of Parasitologists","doi":"10.2307/3275760","usgsCitation":"Putz, R., and Hoffman, G.L., 1963, Two new Gyrodactylus (Trematoda: Monogenea) from cyprinid fishes with synopsis of those found on North American fishes: Journal of Parasitology, v. 49, no. 4, p. 559-566, https://doi.org/10.2307/3275760.","productDescription":"8 p.","startPage":"559","endPage":"566","numberOfPages":"8","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":487911,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.2307/3275760","text":"Publisher Index Page"},{"id":130867,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"49","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a48e4b07f02db6239f5","contributors":{"authors":[{"text":"Putz, R.E.","contributorId":42543,"corporation":false,"usgs":true,"family":"Putz","given":"R.E.","email":"","affiliations":[],"preferred":false,"id":320087,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hoffman, G. L.","contributorId":70713,"corporation":false,"usgs":true,"family":"Hoffman","given":"G.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":320088,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
]}