{"pageNumber":"5258","pageRowStart":"131425","pageSize":"25","recordCount":165349,"records":[{"id":70233425,"text":"70233425 - 1978 - Pleistocene rhyolite of the Mineral Mountains, Utah: Geothermal and archeological significance","interactions":[],"lastModifiedDate":"2022-07-20T15:13:07.312731","indexId":"70233425","displayToPublicDate":"1978-01-01T09:56:49","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"Pleistocene rhyolite of the Mineral Mountains, Utah: Geothermal and archeological significance","docAbstract":"<p>Little-eroded rhyolitic tuffs, flows, and domes extend over about 25 km<sup>2</sup> along the western side of the Mineral Mountains, southwestern Utah, which is along the eastern edge of the Roosevelt KGBA (Known Geothermal Resource Area). Initial eruptions resulted in two low-viscosity lava flows of nonporphyritic rhyolite. These were followed by bedded pumice falls and nonwelded ash flows. The youngest activity produced at least nine viscous domes and small lava flows of rhyolite that contain 1-5 percent phenocrysts of quartz, plagioclase, sodic sanidine, and biotite; distinction between domes and eroded flow segments locally is difficult. </p><p>Potassium-argon ages indicate that all the rhyolite of the Mineral Mountains was erupted between 0.8 and 0.5 m.y. ago. The rhyolite rests on dissected granite of the Mineral Mountains pluton, the largest intrusion in Utah, which has yielded published K-Ar ages of 9 and 15 m.y. A small older dissected rhyolite dome, about 8 m.y. old, occurs just west of the range front. Whether the young ages of the pluton represent time of intrusion or of later reheating, they, in conjunction with the Pleistocene rhyolite in the Mineral Mountains, do indicate a major late Cenozoic thermal anomaly, the size and age of which is significant to evaluation of the Roosevelt KGRA. The rhyolite is also the only known source of implement-grade obsidian in the southwest between eastern California and northern New Mexico. </p>","language":"English","publisher":"U.S. Geological Survey","usgsCitation":"Lipman, P.W., Rowley, P.D., Mehnert, H.H., Evans, S.H., Nash, W.P., Brown, F.H., Izett, G., Naeser, C.W., and Friedman, I., 1978, Pleistocene rhyolite of the Mineral Mountains, Utah: Geothermal and archeological significance: Journal of Research of the U.S. Geological Survey, v. 6, no. 1, p. 133-147.","productDescription":"15 p.","startPage":"133","endPage":"147","costCenters":[],"links":[{"id":404116,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":404115,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1978/vol6issue1/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Utah","otherGeospatial":"Mineral Mountains","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -112.7917,\n              38.375\n            ],\n            [\n              -112.45,\n              38.375\n            ],\n            [\n              -112.45,\n              38.5833\n            ],\n            [\n              -112.7917,\n              38.5833\n            ],\n            [\n              -112.7917,\n              38.375\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"6","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Lipman, P. 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P.","contributorId":293487,"corporation":false,"usgs":false,"family":"Nash","given":"W.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":847073,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Brown, F. H.","contributorId":95597,"corporation":false,"usgs":true,"family":"Brown","given":"F.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":847074,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Izett, G. A.","contributorId":21131,"corporation":false,"usgs":true,"family":"Izett","given":"G. A.","affiliations":[],"preferred":false,"id":847075,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Naeser, C. 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,{"id":70114965,"text":"70114965 - 1978 - Indian land areas judicially established","interactions":[],"lastModifiedDate":"2017-03-29T13:13:14","indexId":"70114965","displayToPublicDate":"1978-01-01T09:55:31","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Indian land areas judicially established","docAbstract":"This map portrays the results of cases before the U.S. Indian Claims Commission or U.S. Court of Claims in which an American Indian tribe proved its original tribal occupancy of a tract within the continental United States.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70114965","collaboration":"Prepared under the direction of the Indian Claims Commission","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1978, Indian land areas judicially established, 50.16 x 37.95 inches, 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,{"id":70200526,"text":"70200526 - 1978 - Age of graben systems on the moon","interactions":[],"lastModifiedDate":"2018-10-23T10:10:19","indexId":"70200526","displayToPublicDate":"1978-01-01T09:30:59","publicationYear":"1978","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Age of graben systems on the moon","docAbstract":"<p>The study focuses on the time of formation of the graben. An attempt is made to determine whether the graben are restricted to geologic units of certain ages, and whether and at what time graben formation ceased. It is shown that (1) most preserved graben formed considerably later than the impacts that formed the basins; (2) graben are faults that are reactivated along older basin concentric and radial structures and lunar grid directions; (3) graben formation ceased about 3.6 + or - 0.2 b.y. ago; and (4) graben formation reflects a tensile stress fields that obtained during part of early lunar history. Other features of graben systems on the moon are also identified.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Proceedings of the 9th Lunar and Planetary Science Conference","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"Lunar and Planetary Science Conference","conferenceDate":"March 13-17, 1978","conferenceLocation":"Houston, TX","language":"English","publisher":"Pergamon Press","usgsCitation":"Lucchitta, B.K., and Watkins, J.A., 1978, Age of graben systems on the moon, <i>in</i> Proceedings of the 9th Lunar and Planetary Science Conference, v. 3, Houston, TX, March 13-17, 1978, p. 3459-3472.","productDescription":"14 p.","startPage":"3459","endPage":"3472","costCenters":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"links":[{"id":358655,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":358654,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://ntrs.nasa.gov/search.jsp?R=19790055278"}],"volume":"3","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Lucchitta, Baerbel K. blucchitta@usgs.gov","contributorId":3649,"corporation":false,"usgs":true,"family":"Lucchitta","given":"Baerbel","email":"blucchitta@usgs.gov","middleInitial":"K.","affiliations":[],"preferred":true,"id":749370,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Watkins, Jessica A.","contributorId":203785,"corporation":false,"usgs":false,"family":"Watkins","given":"Jessica","email":"","middleInitial":"A.","affiliations":[{"id":13711,"text":"Caltech","active":true,"usgs":false}],"preferred":false,"id":749371,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70119857,"text":"70119857 - 1978 - A log-linear model approach to estimation of population size using the line-transect sampling method","interactions":[],"lastModifiedDate":"2014-08-11T09:31:00","indexId":"70119857","displayToPublicDate":"1978-01-01T09:28:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1465,"text":"Ecology","active":true,"publicationSubtype":{"id":10}},"title":"A log-linear model approach to estimation of population size using the line-transect sampling method","docAbstract":"The technique of estimating wildlife population size and density using the belt or line-transect sampling method has been used in many past projects, such as the estimation of density of waterfowl nestling sites in marshes, and is being used currently in such areas as the assessment of Pacific porpoise stocks in regions of tuna fishing activity.  A mathematical framework for line-transect methodology has only emerged in the last 5 yr.  In the present article, we extend this mathematical framework to a line-transect estimator based upon a log-linear model approach.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Ecology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Ecological Society of America","publisherLocation":"Brooklyn, NY","doi":"10.2307/1936648","usgsCitation":"Anderson, D., Burnham, K., and Crain, B., 1978, A log-linear model approach to estimation of population size using the line-transect sampling method: Ecology, v. 59, no. 1, p. 190-193, https://doi.org/10.2307/1936648.","productDescription":"4 p.","startPage":"190","endPage":"193","numberOfPages":"4","costCenters":[],"links":[{"id":291926,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":291925,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.2307/1936648"}],"volume":"59","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53e9d8c5e4b008eaa4f3f5f0","contributors":{"authors":[{"text":"Anderson, David R.","contributorId":8413,"corporation":false,"usgs":true,"family":"Anderson","given":"David R.","affiliations":[],"preferred":false,"id":497793,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Burnham, K.P.","contributorId":63760,"corporation":false,"usgs":true,"family":"Burnham","given":"K.P.","email":"","affiliations":[],"preferred":false,"id":497795,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Crain, B.R.","contributorId":19482,"corporation":false,"usgs":true,"family":"Crain","given":"B.R.","email":"","affiliations":[],"preferred":false,"id":497794,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70205844,"text":"70205844 - 1978 - Greater Atlanta region slope map","interactions":[],"lastModifiedDate":"2022-12-26T16:19:40.041731","indexId":"70205844","displayToPublicDate":"1978-01-01T09:16:04","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Greater Atlanta region slope map","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70205844","collaboration":"State of Georgia Department of Natural Resources Geologic and Water Resources Division","usgsCitation":"1978, Greater Atlanta region slope map, 1 Plate: 58.57 x 50.56 inches, https://doi.org/10.3133/70205844.","productDescription":"1 Plate: 58.57 x 50.56 inches","costCenters":[],"links":[{"id":368089,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70205844/report-thumb.jpg"},{"id":368090,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70205844/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"100000","country":"United States","state":"Georgia","city":"Atlanta","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -85.25,\n              33.375\n            ],\n            [\n              -83.75,\n              33.375\n            ],\n            [\n              -83.75,\n              34.375\n            ],\n            [\n              -85.25,\n              34.375\n            ],\n            [\n              -85.25,\n              33.375\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"editors":[{"text":"U.S. Geological Survey","contributorId":210377,"corporation":true,"usgs":false,"organization":"U.S. Geological Survey","id":860010,"contributorType":{"id":2,"text":"Editors"},"rank":1}]}}
,{"id":70012598,"text":"70012598 - 1978 - Mars synthetic topographic mapping","interactions":[],"lastModifiedDate":"2025-02-27T19:32:08.863074","indexId":"70012598","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1963,"text":"Icarus","active":true,"publicationSubtype":{"id":10}},"title":"Mars synthetic topographic mapping","docAbstract":"<p><span>Topographic contour maps of Mars are compiled by the synthesis of data acquired from various scientific experiments of the Mariner 9 mission, including S-band radio-occulation, the ultraviolet spectrometer (UVS), the infrared radiometer (IRR), the infrared interferometer spectrometer (IRIS) and television imagery, as well as Earth-based radar information collected at Goldstone, Haystack, and Arecibo Observatories. The entire planet is mapped at scales of 1:25,000,000 and 1:25,000,000 using Mercator, Lambert, and polar stereographic map projections. For the computation of map projections, a biaxial spheroid figure is adopted. The semimajor and semiminor axes are 3393.4 and 3375.7 km, respectively, with a polar flattening of 0.0052. For the computation of elevations, a topographic datum is defined by a gravity field described in terms of spherical harmonics of fourth order and fourth degree combined with a 6.1-mbar occulation pressure surface. This areoid can be approximated by a triaxial ellipsoid with semimajor axes of&nbsp;</span><i>A</i><span>&nbsp;= 3394.6 km and&nbsp;</span><i>B</i><span>&nbsp;= 3393.3 km and a semiminor axis of&nbsp;</span><i>C</i><span>&nbsp;= 3376.3 km. The semimajor axis&nbsp;</span><i>A</i><span>&nbsp;intersects the Martian surface at longitude 105°W. The dynamic flattening of Mars is 0.00525. The contour intercal of the maps is 1 km. For some prominent features where overlapping pictures from Mariner 9 are available, local contour maps at relatively larger scales were also compiled by photogrammetric methods on stereo plotters.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0019-1035(78)90182-3","issn":"00191035","usgsCitation":"Wu, S., 1978, Mars synthetic topographic mapping: Icarus, v. 33, no. 3, p. 417-440, https://doi.org/10.1016/0019-1035(78)90182-3.","productDescription":"24 p.","startPage":"417","endPage":"440","numberOfPages":"24","costCenters":[],"links":[{"id":493276,"rank":2,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"http://hdl.handle.net/10150/289440","text":"External Repository"},{"id":222153,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"33","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a5226e4b0c8380cd6c1c2","contributors":{"authors":[{"text":"Wu, S.S.C.","contributorId":10421,"corporation":false,"usgs":true,"family":"Wu","given":"S.S.C.","email":"","affiliations":[],"preferred":false,"id":364016,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70012550,"text":"70012550 - 1978 - Prediction of capacity factors for aqueous organic solutes adsorbed on a porous acrylic resin","interactions":[],"lastModifiedDate":"2023-03-10T17:47:53.733634","indexId":"70012550","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":761,"text":"Analytical Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"Prediction of capacity factors for aqueous organic solutes adsorbed on a porous acrylic resin","docAbstract":"<p>The capacity factors of 20 aromatic, allphatic, and allcycllc organic solutes with carboxyl, hydroxyl, amine, and methyl functional groups were determined on Amberlite XAD-8, a porous acrylic resin. The logarithm of the capacity factor, <i>k'</i>, correlated inversely with the logarithm of the aqueous molar solubility with significance of less than 0.001. The log <i>k'</i>-log solubility relationship may be used to predict the capacity of any organic solute for XAD-8 using only the solubility of the solute. The prediction is useful as a guide for determining the proper ratio of sample to column size In the preconcentration of organic solutes from water. The inverse relationship of solubility and capacity is due to the unfavorable entropy of solution of organic solutes which affects both solubility and sorption.</p>","language":"English","publisher":"ACS Publications","doi":"10.1021/ac50027a028","usgsCitation":"Thurman, E., Malcolm, R., and Aiken, G., 1978, Prediction of capacity factors for aqueous organic solutes adsorbed on a porous acrylic resin: Analytical Chemistry, v. 50, no. 6, p. 775-779, https://doi.org/10.1021/ac50027a028.","productDescription":"5 p.","startPage":"775","endPage":"779","numberOfPages":"5","costCenters":[],"links":[{"id":222086,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"50","issue":"6","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","scienceBaseUri":"505a81eae4b0c8380cd7b7d1","contributors":{"authors":[{"text":"Thurman, E.M.","contributorId":102864,"corporation":false,"usgs":true,"family":"Thurman","given":"E.M.","affiliations":[],"preferred":false,"id":363879,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Malcolm, Ronald L.","contributorId":46075,"corporation":false,"usgs":true,"family":"Malcolm","given":"Ronald L.","affiliations":[],"preferred":false,"id":866164,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Aiken, G. R. 0000-0001-8454-0984","orcid":"https://orcid.org/0000-0001-8454-0984","contributorId":14452,"corporation":false,"usgs":true,"family":"Aiken","given":"G. R.","affiliations":[],"preferred":false,"id":866165,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70180239,"text":"70180239 - 1978 - New potassium-argon data on the age of mineralization and metamorphism in the Willow Creek mining district, southern Talkeetna Mountains, Alaska","interactions":[{"subject":{"id":70180239,"text":"70180239 - 1978 - New potassium-argon data on the age of mineralization and metamorphism in the Willow Creek mining district, southern Talkeetna Mountains, Alaska","indexId":"70180239","publicationYear":"1978","noYear":false,"title":"New potassium-argon data on the age of mineralization and metamorphism in the Willow Creek mining district, southern Talkeetna Mountains, Alaska"},"predicate":"IS_PART_OF","object":{"id":4432,"text":"cir772B - 1978 - The United States Geological Survey in Alaska: Accomplishments during 1977","indexId":"cir772B","publicationYear":"1978","noYear":false,"title":"The United States Geological Survey in Alaska: Accomplishments during 1977"},"id":1}],"isPartOf":{"id":4432,"text":"cir772B - 1978 - The United States Geological Survey in Alaska: Accomplishments during 1977","indexId":"cir772B","publicationYear":"1978","noYear":false,"title":"The United States Geological Survey in Alaska: Accomplishments during 1977"},"lastModifiedDate":"2021-03-22T14:34:42.571643","indexId":"70180239","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","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":"772-B","title":"New potassium-argon data on the age of mineralization and metamorphism in the Willow Creek mining district, southern Talkeetna Mountains, Alaska","docAbstract":"<p>The now largely abandoned Willow Creek mining district, southern Talkeetna Mountains, Alaska, produced nearly $18,000,000 in gold and minor silver between 1909 and the early 1950's. Mineralized quartz veins, which contain gold and silver along with minor quantities of base metals (in pyrite, galena, chalcopyrite, sphalerite, molybdenite, and arsenopyrite), cut Late Cretaceous and early Tertiary tonalite and quartzmica schist of probable Jurassic age (Ray, 1954; Silberman and others, 1976; Bela Csejtey, Jr., unpub. data, 1978).</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"The United States Geological Survey in Alaska: Accomplishments during 1977 (Circular 772-B)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/70180239","usgsCitation":"Silberman, M.L., Csejtey, B., Smith, J., Lanphere, M.A., and Wilson, F.H., 1978, New potassium-argon data on the age of mineralization and metamorphism in the Willow Creek mining district, southern Talkeetna Mountains, Alaska: U.S. Geological Survey Circular 772-B, 5 p., https://doi.org/10.3133/70180239.","productDescription":"5 p.","startPage":"B-65","endPage":"B-69","numberOfPages":"5","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":334027,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":334026,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1978/0772b/report.pdf#page=72","text":"Start page in larger work"}],"country":"United States","state":"Alaska","otherGeospatial":"Talkeetna Mountains, Willow Creek mining district","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -146.09619140625,\n              60.78598138475315\n            ],\n            [\n              -144.11865234375,\n              60.78598138475315\n            ],\n            [\n              -144.11865234375,\n              61.70549883819642\n            ],\n            [\n              -146.09619140625,\n              61.70549883819642\n            ],\n            [\n              -146.09619140625,\n              60.78598138475315\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5889c7c7e4b0ba3b075e0658","contributors":{"authors":[{"text":"Silberman, Miles L.","contributorId":23947,"corporation":false,"usgs":true,"family":"Silberman","given":"Miles","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":660856,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Csejtey, Bela Jr.","contributorId":61008,"corporation":false,"usgs":true,"family":"Csejtey","given":"Bela","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":660857,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Smith, James G.","contributorId":98712,"corporation":false,"usgs":true,"family":"Smith","given":"James G.","affiliations":[],"preferred":false,"id":660858,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lanphere, Marvin A. alder@usgs.gov","contributorId":2696,"corporation":false,"usgs":true,"family":"Lanphere","given":"Marvin","email":"alder@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":660859,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Wilson, Frederic H. 0000-0003-1761-6437 fwilson@usgs.gov","orcid":"https://orcid.org/0000-0003-1761-6437","contributorId":67174,"corporation":false,"usgs":true,"family":"Wilson","given":"Frederic","email":"fwilson@usgs.gov","middleInitial":"H.","affiliations":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":119,"text":"Alaska Science Center Geology Minerals","active":true,"usgs":true}],"preferred":true,"id":660860,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70012593,"text":"70012593 - 1978 - Dislocation substructure of mantle-derived olivine as revealed by selective chemical etching and transmission electron microscopy","interactions":[],"lastModifiedDate":"2012-03-12T17:19:08","indexId":"70012593","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3066,"text":"Physics and Chemistry of Minerals","active":true,"publicationSubtype":{"id":10}},"title":"Dislocation substructure of mantle-derived olivine as revealed by selective chemical etching and transmission electron microscopy","docAbstract":"Cleaved and mechanically polished surfaces of olivine from peridotite xenoliths from San Carlos, Arizona, were chemically etched using the techniques of Wegner and Christie (1974). Dislocation etch pits are produced on all surface orientations and they tend to be preferentially aligned along the traces of subgrain boundaries, which are approximately parallel to (100), (010), and (001). Shallow channels were also produced on (010) surfaces and represent dislocations near the surface that are etched out along their lengths. The dislocation etch channel loops are often concentric, and emanate from (100) subgrain boundaries, which suggests that dislocation sources are in the boundaries. Data on subgrain misorientation and dislocation line orientation and arguments based on subgrain boundary energy minimization are used to characterize the dislocation structures of the subgrain boundaries. (010) subgrain boundaries are of the twist type, composed of networks of [100] and [001] screw dislocations. Both (100) and (001) subgrain boundaries are tilt walls composed of arrays of edge dislocation with Burgers vectors b=[100] and [001], respectively. The inferred slip systems are {001} ???100???, {100} ???001???, and {010} ???100??? in order of diminishing importance. Exploratory transmission electron microscopy is in accord with these identifications. The flow stresses associated with the development of the subgrain structure are estimated from the densities of free dislocations and from the subgrain dimensions. Inferred stresses range from 35 to 75 bars using the free dislocation densities and 20 to 100 bars using the subgrain sizes. ?? 1978 Springer-Verlag.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Physics and Chemistry of Minerals","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisherLocation":"Springer-Verlag","doi":"10.1007/BF00311845","issn":"03421791","usgsCitation":"Kirby, S.H., and Wegner, M., 1978, Dislocation substructure of mantle-derived olivine as revealed by selective chemical etching and transmission electron microscopy: Physics and Chemistry of Minerals, v. 3, no. 4, p. 309-330, https://doi.org/10.1007/BF00311845.","startPage":"309","endPage":"330","numberOfPages":"22","costCenters":[],"links":[{"id":205196,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF00311845"},{"id":222089,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"3","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0215e4b0c8380cd4fe96","contributors":{"authors":[{"text":"Kirby, S. H.","contributorId":51721,"corporation":false,"usgs":true,"family":"Kirby","given":"S.","middleInitial":"H.","affiliations":[],"preferred":false,"id":363998,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wegner, M.W.","contributorId":42354,"corporation":false,"usgs":true,"family":"Wegner","given":"M.W.","email":"","affiliations":[],"preferred":false,"id":363997,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70012641,"text":"70012641 - 1978 - Determination of silver, bismuth, cadmium, copper, lead, and zinc in geologic materials by atomic absorption spectrometry with tricaprylylmethylammonium chloride","interactions":[],"lastModifiedDate":"2023-03-10T17:49:47.054281","indexId":"70012641","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":761,"text":"Analytical Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"Determination of silver, bismuth, cadmium, copper, lead, and zinc in geologic materials by atomic absorption spectrometry with tricaprylylmethylammonium chloride","docAbstract":"Interferences commonly encountered in the determination of silver, bismuth, cadmium, copper, lead, and zinc at crustal abundance levels are effectively eliminated using a rapid, sensitive, organic extraction technique. A potassium chlorate-hydrochloric acid digestion solubilizes the metals not tightly bound in the silicate lattice of rocks, soils, and stream sediments. The six metals are selectively extracted into a 10% Aliquat 336-MIBK organic phase in the presence of ascorbic acid and potassium iodide. Metals in the organic extract are determined by flame atomic absorption spectrometry to the 0.02-ppm level for silver, cadmium, copper, and zinc and to the 0.2-ppm level for bismuth and lead with a maximum relative standard deviation of 18.8% for known reference samples. An additional hydrofluoric acid digestion may be used to determine metals substituted in the silicate lattice.","language":"English","publisher":"ACS Publications","doi":"10.1021/ac50030a023","usgsCitation":"Viets, J.G., 1978, Determination of silver, bismuth, cadmium, copper, lead, and zinc in geologic materials by atomic absorption spectrometry with tricaprylylmethylammonium chloride: Analytical Chemistry, v. 50, no. 8, p. 1097-1101, https://doi.org/10.1021/ac50030a023.","productDescription":"5 p.","startPage":"1097","endPage":"1101","numberOfPages":"5","costCenters":[],"links":[{"id":221839,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"50","issue":"8","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","scienceBaseUri":"5059ffc6e4b0c8380cd4f3bb","contributors":{"authors":[{"text":"Viets, John G.","contributorId":84510,"corporation":false,"usgs":true,"family":"Viets","given":"John","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":364120,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70012713,"text":"70012713 - 1978 - Microwave remote sensing of sea ice in the AIDJEX Main Experiment","interactions":[],"lastModifiedDate":"2012-03-12T17:19:10","indexId":"70012713","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1072,"text":"Boundary-Layer Meteorology","active":true,"publicationSubtype":{"id":10}},"title":"Microwave remote sensing of sea ice in the AIDJEX Main Experiment","docAbstract":"During the AIDJEX Main Experiment, April 1975 through May 1976, a comprehensive microwave sensing program was performed on the sea ice of the Beaufort Sea. Surface and aircraft measurements were obtained during all seasons using a wide variety of active and passive microwave sensors. The surface program obtained passive microwave measurements of various ice types using four antennas mounted on a tracked vehicle. In three test regions, each with an area of approximately 1.5 ?? 104 m2, detailed ice crystallographic, dielectric properties, and brightness temperatures of first-year, multiyear, and first-year/multiyear mixtures were measured. A NASA aircraft obtained passive microwave measurements of the entire area of the AIDJEX manned station array (triangle) during each of 18 flights. This verified the earlier reported ability to distinguish first-year and multiyear ice types and concentration and gave new information on ways to observe ice mixtures and thin ice types. The active microwave measurements from aircraft included those from an X- and L-band radar and from a scatterometer. The former is used to study a wide variety of ice features and to estimate deformations, while both are equally usable to observe ice types. With the present data, only the scatterometer can be used to distinguish positively multiyear from first-year and various types of thin ice. This is best done using coupled active and passive microwave sensing. ?? 1978 D. 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,{"id":70174924,"text":"70174924 - 1978 - Field and modeling studies of San Francisco Bay","interactions":[],"lastModifiedDate":"2016-07-28T15:11:11","indexId":"70174924","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Field and modeling studies of San Francisco Bay","conferenceTitle":"Symposium on technical, environmental, socio-economic and regulatory aspects of coastal zone management","conferenceDate":"1978","conferenceLocation":"San Francisco, CA","language":"English","publisher":"American Society of Civil Engineers","usgsCitation":"Conomos, T.J., Nichols, F., Cheng, R.T., and Peterson, D.H., 1978, Field and modeling studies of San Francisco Bay, Symposium on technical, environmental, socio-economic and regulatory aspects of coastal zone management, San Francisco, CA, 1978, p. 1917-1927.","productDescription":"11 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,{"id":70012491,"text":"70012491 - 1978 - Analytical multicollimator camera calibration","interactions":[],"lastModifiedDate":"2013-03-20T19:49:10","indexId":"70012491","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3050,"text":"Photogrammetria","active":true,"publicationSubtype":{"id":10}},"title":"Analytical multicollimator camera calibration","docAbstract":"Calibration with the U.S. Geological survey multicollimator determines the calibrated focal length, the point of symmetry, the radial distortion referred to the point of symmetry, and the asymmetric characteristiecs of the camera lens. For this project, two cameras were calibrated, a Zeiss RMK A 15/23 and a Wild RC 8. Four test exposures were made with each camera. Results are tabulated for each exposure and averaged for each set. Copies of the standard USGS calibration reports are included. ?? 1978.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Photogrammetria","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/0031-8663(78)90009-1","issn":"00318663","usgsCitation":"Tayman, W., 1978, Analytical multicollimator camera calibration: Photogrammetria, v. 34, no. 5, p. 179-197, https://doi.org/10.1016/0031-8663(78)90009-1.","startPage":"179","endPage":"197","numberOfPages":"19","costCenters":[],"links":[{"id":222208,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":269813,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0031-8663(78)90009-1"}],"volume":"34","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059eb6ce4b0c8380cd48dc0","contributors":{"authors":[{"text":"Tayman, W.P.","contributorId":63942,"corporation":false,"usgs":true,"family":"Tayman","given":"W.P.","email":"","affiliations":[],"preferred":false,"id":363745,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1013673,"text":"1013673 - 1978 - Myxosoma cerebralis: Fluorescent antibody techniques for antigen recognition","interactions":[],"lastModifiedDate":"2025-03-03T16:28:51.188828","indexId":"1013673","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","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":"Myxosoma cerebralis: Fluorescent antibody techniques for antigen recognition","docAbstract":"<p><span>Rabbits were immunized with antigens extracted from mature spores or prespore stages of&nbsp;</span><i>Myxosoma cerebralis</i><span>, and the resulting antisera and their globulins were used in direct and indirect fluorescent antibody techniques. Both kinds of antisera reacted with homologous spores and with stages of the organism that precede spores. When tested for specificity against spores of 12 other myxosporidans the direct fluorescent antibody technique showed cross-reactivity with only one other and that was a species of&nbsp;</span><i>Myxosoma</i><span>. The indirect fluorescent antibody technique showed some reactions across generic lines. The antisera have application in studies of the parasite's life cycle and in diagnostics.&nbsp;</span></p>","language":"English","publisher":"Canadian Science Publishing","doi":"10.1139/f78-133","usgsCitation":"Markiw, M., and Wolf, K., 1978, Myxosoma cerebralis: Fluorescent antibody techniques for antigen recognition: Journal of the Fisheries Research Board of Canada, v. 35, no. 6, p. 828-832, https://doi.org/10.1139/f78-133.","productDescription":"5 p.","startPage":"828","endPage":"832","numberOfPages":"5","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":131468,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"35","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b02e4b07f02db698a1f","contributors":{"authors":[{"text":"Markiw, M.E.","contributorId":44865,"corporation":false,"usgs":true,"family":"Markiw","given":"M.E.","affiliations":[],"preferred":false,"id":319018,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wolf, K.","contributorId":16344,"corporation":false,"usgs":true,"family":"Wolf","given":"K.","email":"","affiliations":[],"preferred":false,"id":319017,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70012642,"text":"70012642 - 1978 - Vesicularity of basalt erupted at Reykjanes Ridge crest","interactions":[],"lastModifiedDate":"2012-03-12T17:19:02","indexId":"70012642","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2840,"text":"Nature","active":true,"publicationSubtype":{"id":10}},"title":"Vesicularity of basalt erupted at Reykjanes Ridge crest","docAbstract":"Average vesicularity of basalt drilled at three sites on the west flank of the Reykjanes Ridge increases with decreasing age. This change apparently records concomitant decrease in water depth at the ridge crest where the basalt was erupted and suggests substantial upward growth of the crest during the past 35 Myr. ?? 1978 Nature Publishing Group.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Nature","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1038/274217a0","issn":"00280836","usgsCitation":"Duffield, W.A., 1978, Vesicularity of basalt erupted at Reykjanes Ridge crest: Nature, v. 274, no. 5668, p. 217-220, https://doi.org/10.1038/274217a0.","startPage":"217","endPage":"220","numberOfPages":"4","costCenters":[],"links":[{"id":221840,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":205150,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1038/274217a0"}],"volume":"274","issue":"5668","noUsgsAuthors":false,"publicationDate":"1978-07-01","publicationStatus":"PW","scienceBaseUri":"505bc24fe4b08c986b32aa71","contributors":{"authors":[{"text":"Duffield, W. A.","contributorId":71935,"corporation":false,"usgs":true,"family":"Duffield","given":"W.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":364121,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1003365,"text":"1003365 - 1978 - Compounds registered for fishery uses","interactions":[],"lastModifiedDate":"2012-02-02T00:14:44","indexId":"1003365","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3330,"text":"Salmonid","active":true,"publicationSubtype":{"id":10}},"title":"Compounds registered for fishery uses","docAbstract":"Abstract has not been submitted","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Salmonid","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Schnick, R.A., Meyer, F.P., and VanMeter, H., 1978, Compounds registered for fishery uses: Salmonid, v. 2, no. 4, p. 18-20.","productDescription":"pp. 18-20","startPage":"18","endPage":"20","numberOfPages":"3","costCenters":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":196684,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"2","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b19e4b07f02db6a7f89","contributors":{"authors":[{"text":"Schnick, R. A.","contributorId":106079,"corporation":false,"usgs":true,"family":"Schnick","given":"R.","middleInitial":"A.","affiliations":[],"preferred":false,"id":313181,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Meyer, F. P.","contributorId":96207,"corporation":false,"usgs":true,"family":"Meyer","given":"F.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":313180,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"VanMeter, H.D.","contributorId":65571,"corporation":false,"usgs":true,"family":"VanMeter","given":"H.D.","email":"","affiliations":[],"preferred":false,"id":313179,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":1003364,"text":"1003364 - 1978 - Incidence of disease in warmwater fish farms in the south-central United States","interactions":[],"lastModifiedDate":"2012-02-02T00:14:51","indexId":"1003364","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2665,"text":"Marine Fisheries Review","active":true,"publicationSubtype":{"id":10}},"title":"Incidence of disease in warmwater fish farms in the south-central United States","docAbstract":"Abstract has not been submitted","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Marine Fisheries Review","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Meyer, F.P., 1978, Incidence of disease in warmwater fish farms in the south-central United States: Marine Fisheries Review, v. 40, no. 3, p. 38-41.","productDescription":"pp. 38-41","startPage":"38","endPage":"41","numberOfPages":"4","costCenters":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":196874,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"40","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fce4b07f02db5f5768","contributors":{"authors":[{"text":"Meyer, F. P.","contributorId":96207,"corporation":false,"usgs":true,"family":"Meyer","given":"F.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":313178,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":5221164,"text":"5221164 - 1978 - Coccidia of whooping cranes","interactions":[],"lastModifiedDate":"2025-04-08T16:39:15.171352","indexId":"5221164","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2507,"text":"Journal of Wildlife Diseases","active":true,"publicationSubtype":{"id":10}},"title":"Coccidia of whooping cranes","docAbstract":"<p><span>Coccidial oocysts were observed in 6 of 19 fecal samples from free-ranging whooping cranes (</span><i>Grus americana</i><span>) and 4 of 16 samples from captive whooping cranes.&nbsp;</span><i>Eimeria gruis</i><span>&nbsp;occurred in four free-ranging whooping cranes and&nbsp;</span><i>E. reichenowi</i><span>&nbsp;in two free-ranging and two captive whooping cranes. Fecal samples from two captive cranes contained oocysts of&nbsp;</span><i>lsospora lacazei</i><span>&nbsp;which was considered a spurious parasite. Oocysts of both species of&nbsp;</span><i>Eimeria</i><span>&nbsp;were prevalent in fecal samples collected from three free-ranging Canadian sandhill cranes (</span><i>G. canadensis rowani</i><span>) from whooping crane wintering grounds in Texas. These coccidia were prevalent also in fecal samples from 14 sandhill cranes (of 4 subspecies) maintained in captivity at the Patuxent Wildlife Research Center in Maryland.</span></p>","language":"English","publisher":"Wildlife Disease Association","doi":"10.7589/0090-3558-14.1.24","usgsCitation":"Forrester, D.J., Carpenter, J.W., and Blankinship, D., 1978, Coccidia of whooping cranes: Journal of Wildlife Diseases, v. 14, no. 1, p. 24-27, https://doi.org/10.7589/0090-3558-14.1.24.","productDescription":"4 p.","startPage":"24","endPage":"27","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":487050,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.7589/0090-3558-14.1.24","text":"Publisher Index Page"},{"id":194120,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Maryland, 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W.","contributorId":81854,"corporation":false,"usgs":true,"family":"Carpenter","given":"J.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":333173,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Blankinship, D.R.","contributorId":82010,"corporation":false,"usgs":true,"family":"Blankinship","given":"D.R.","email":"","affiliations":[],"preferred":false,"id":333174,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":47620,"text":"wri7825 - 1978 - Potentiometric surface of the Mississippian aquifer in parts of Trigg, Lyon, Caldwell, and Christian Counties, Mississippian Plateau region, Kentucky","interactions":[],"lastModifiedDate":"2023-05-01T19:47:05.575988","indexId":"wri7825","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"78-25","title":"Potentiometric surface of the Mississippian aquifer in parts of Trigg, Lyon, Caldwell, and Christian Counties, Mississippian Plateau region, Kentucky","docAbstract":"<p>Ground-water levels in a 600 square mile area of the Cumberland River drainage basin in parts of Trigg, Lyon Caldwell, and Christian Counties, Mississippian Plateau Region, Kentucky are shown by means of contours on the potentiometric surface. Generaly, ground water moves toward and with the surface drainage to Lake Barkley and the Cumberland River. The potentiometric map indicates a minimum drilling depth to water. The bedrock is composed largely of sandstone, cavernous limestone, or jointed and fractured limestone. All of these rock types yield sufficient water for domestic and stock purposes. The cavernous limestone is extremely vulnerable to pollution.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri7825","usgsCitation":"Plebuch, R.O., 1978, Potentiometric surface of the Mississippian aquifer in parts of Trigg, Lyon, Caldwell, and Christian Counties, Mississippian Plateau region, Kentucky: U.S. Geological Survey Water-Resources Investigations Report 78-25, 6 Plates: 48.46 x 25.72 inches or smaller, https://doi.org/10.3133/wri7825.","productDescription":"6 Plates: 48.46 x 25.72 inches or smaller","costCenters":[],"links":[{"id":162487,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":416565,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_52485.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Kentucky","county":"Caldwell County, Christian County, Lyon County, Trigg County","otherGeospatial":"Mississippian aquifer","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -88.25,\n              37.125\n            ],\n            [\n              -88.25,\n              36.625\n            ],\n            [\n              -87.625,\n              36.625\n            ],\n            [\n              -87.625,\n              37.125\n            ],\n            [\n              -88.25,\n              37.125\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad4e4b07f02db682f41","contributors":{"authors":[{"text":"Plebuch, Raymond O.","contributorId":15177,"corporation":false,"usgs":true,"family":"Plebuch","given":"Raymond","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":235913,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":26397,"text":"wri7894 - 1978 - Hydrologic appraisal of the water resources of the Homer-Preble Valley, New York","interactions":[],"lastModifiedDate":"2023-03-14T19:44:50.633293","indexId":"wri7894","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"78-94","title":"Hydrologic appraisal of the water resources of the Homer-Preble Valley, New York","docAbstract":"<p>Water resources of Homer-Preble Valley, 1 to 2 miles wide and 9 miles long, in central New York, were appraised because the area is expected to undergo considerable residential development in the near future. The main source of water supply to the residents of the area is the glacial-outwash aquifer. Data indicate that additional pumpage of 5 million to 10 million gallons per day from the aquifer would not seriously reduce the quantity and quality of the water supply. Water-quality analyses indicate that ground water and surface water in the valley are suitable for most uses and generally meet State standards for source waters for drinking.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri7894","usgsCitation":"Buller, W., 1978, Hydrologic appraisal of the water resources of the Homer-Preble Valley, New York: U.S. Geological Survey Water-Resources Investigations Report 78-94, v, 31 p., https://doi.org/10.3133/wri7894.","productDescription":"v, 31 p.","costCenters":[],"links":[{"id":157876,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":266236,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1978/0094/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":414121,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35281.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"New York","otherGeospatial":"Homer-Preble Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -76.208,\n              42.767\n            ],\n            [\n              -76.208,\n              42.642\n            ],\n            [\n              -76.117,\n              42.642\n            ],\n            [\n              -76.117,\n              42.767\n            ],\n            [\n              -76.208,\n              42.767\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a29e4b07f02db6116c2","contributors":{"authors":[{"text":"Buller, William","contributorId":16449,"corporation":false,"usgs":true,"family":"Buller","given":"William","email":"","affiliations":[],"preferred":false,"id":196317,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70012421,"text":"70012421 - 1978 - The moon: Composition determined by nebular processes","interactions":[],"lastModifiedDate":"2012-03-12T17:19:07","indexId":"70012421","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3570,"text":"The Moon and the Planets","active":true,"publicationSubtype":{"id":10}},"title":"The moon: Composition determined by nebular processes","docAbstract":"The bulk composition of the Moon was determined by the conditions in the solar nebula during its formation, and may be quantitatively estimated from the premise that the terrestrial planets were formed by cosmochemical processes similar to those recorded in the chondrites. The calculations are based on the Ganapathy-Anders 7-component model using trace element indicators, but incorportate improved geophysical data and petrological constraints. A model Moon with 40 ppb U, a core 2% by weight (1.8% metal with ???35% Ni and 0.2% FeS) and Mg/(Fe2++Mg)?????0.75 meets the trace element restrictions, and has acceptable density, heat flow and moment of inertia ratio. The high Ni content of the core permits low-Ti mare basalts to equilibrate with metal, yet still retain substantial Ni. The silicate resembles the Taylor-Jakes?? composition (and in some respects the waif Ganapathy-Anders Model 2a), but has lower SiO2. Minor modifications of the model composition (U=30-35 ppb) yield a 50% melt approximating Apollo 15 green glass and a residuum of olivine plus 3 to 4% spinel; the low SiO2, favors spinel formation, and, contrary to expectation, Cr is not depleted in the liquid. There may no longer be any inconsistency between the cosmochemical approach and arguments based on experimental petrology. ?? 1978 D. Reidel Publishing Company.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"The Moon and the Planets","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisherLocation":"Kluwer Academic Publishers","doi":"10.1007/BF00897296","issn":"01650807","usgsCitation":"Morgan, J.W., Hertogen, J., and Anders, E., 1978, The moon: Composition determined by nebular processes: The Moon and the Planets, v. 18, no. 4, p. 465-478, https://doi.org/10.1007/BF00897296.","startPage":"465","endPage":"478","numberOfPages":"14","costCenters":[],"links":[{"id":205181,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF00897296"},{"id":222014,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"18","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505badebe4b08c986b323e63","contributors":{"authors":[{"text":"Morgan, J. W.","contributorId":92384,"corporation":false,"usgs":true,"family":"Morgan","given":"J.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":363512,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hertogen, J.","contributorId":90042,"corporation":false,"usgs":true,"family":"Hertogen","given":"J.","email":"","affiliations":[],"preferred":false,"id":363511,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Anders, E.","contributorId":64803,"corporation":false,"usgs":true,"family":"Anders","given":"E.","email":"","affiliations":[],"preferred":false,"id":363510,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70012407,"text":"70012407 - 1978 - Uranium-lead isotope systematics and apparent ages of zircons and other minerals in precambrian granitic rocks, Granite Mountains, Wyoming","interactions":[],"lastModifiedDate":"2012-03-12T17:18:47","indexId":"70012407","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1336,"text":"Contributions to Mineralogy and Petrology","active":true,"publicationSubtype":{"id":10}},"title":"Uranium-lead isotope systematics and apparent ages of zircons and other minerals in precambrian granitic rocks, Granite Mountains, Wyoming","docAbstract":"Zircon suites from the two main types of granite in the Granite Mountains, Wyoming, yielded concordia-intercept ages of 2,640??20 m.y. for a red, foliated granite (granite of Long Creek Mountain) and 2,595??40 m.y. for the much larger mass of the granite of Lankin Dome. These ages are statistically distinct (40??20 m.y. difference) and are consistent with observed chemical and textural differences. The lower intercepts of the zircon chords of 50??40 and 100+ 75 m.y. for the granite of Long Creek Mountain and granite of Lankin Dome, respectively, are not consistent with reasonable continuous diffusion lead-loss curves but do correspond well with the known (Laramide) time of uplift of the rocks. Epidote, zircon, and apatite from silicified and epidotized zones in the granites all record at least one postcrystallization disturbance in addition to the Laramide event and do not define a unique age of silicification and epidotization. The lower limit of ???2,500 m.y. provided by the least disturbed epidote, however, suggests that these rocks were probably formed by deuteric processes shortly after emplacement of the granite of the Lankin Dome. The earlier of the two disturbances that affected the minerals of the silicified-epidotized rock can be bracketed between 1,350 and 2,240 m.y. ago and is probably the same event that lowered mineral K-Ar and ages in the region. Zircon suites from both types of granite show well-defined linear correlations among U content, common-Pb content, and degree of discordance. One of the zircon suites has an extremely high common-Pb content (up to 180 ppm) and exhibits a component of radiogenic-Pb loss that is apparently unrelated to radiation damage. ?? 1978 Springer-Verlag.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Contributions to Mineralogy and Petrology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisherLocation":"Springer-Verlag","doi":"10.1007/BF00375510","issn":"00107999","usgsCitation":"Ludwig, K., and Stuckless, J., 1978, Uranium-lead isotope systematics and apparent ages of zircons and other minerals in precambrian granitic rocks, Granite Mountains, Wyoming: Contributions to Mineralogy and Petrology, v. 65, no. 3, p. 243-254, https://doi.org/10.1007/BF00375510.","startPage":"243","endPage":"254","numberOfPages":"12","costCenters":[],"links":[{"id":205290,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF00375510"},{"id":222718,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"65","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bbdede4b08c986b3292ef","contributors":{"authors":[{"text":"Ludwig, K.R.","contributorId":97112,"corporation":false,"usgs":true,"family":"Ludwig","given":"K.R.","email":"","affiliations":[{"id":218,"text":"Denver Federal Center","active":false,"usgs":true}],"preferred":false,"id":363467,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stuckless, J. S.","contributorId":6060,"corporation":false,"usgs":true,"family":"Stuckless","given":"J. S.","affiliations":[],"preferred":false,"id":363466,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1007823,"text":"1007823 - 1978 - Sea otter predation and community organization in the western Aleutian Island, Alaska","interactions":[],"lastModifiedDate":"2023-12-18T17:43:34.200964","indexId":"1007823","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1465,"text":"Ecology","active":true,"publicationSubtype":{"id":10}},"title":"Sea otter predation and community organization in the western Aleutian Island, Alaska","docAbstract":"<p><span>Predation by the sea otter (Enhydra lutris) limits epibenthic invertebrates, especially sea urchins (Strongylocentrotus polyacanthus), in turn allowing a luxuriant development of the macroalgal canopy. Where sea otters are abundant, sea urchins are small and scarce in shallow water, and the association of fleshy macroalgae apparently is regulated by competition. Sea urchins are larger and more abundant in deeper water, where they are less accessible to sea otters. Macroalgae are most abundant, and competition in the plant association is severest, near the sublittoral fringe where sea otters can remove sea urchins most efficiently. In deep water, competition among maccroalgae is reduced because the light intensity is lower and grazing by sea urchins increases. On islands where sea otters are absent, sea urchins are abundant, large, and are probably limited by intraspecific competition; and they have eliminated fleshly macroalgae. Available data suggest that the association of Laminaria spp. and Agarum cribrosum contributes most to primary production in nearshore areas of the western Aleutian Islands. Where sea otters are absent and sea urchins have eliminated this plant association, some higher trophic forms also are absent or less abundant than where sea otters are common and the plant association is well developed. Earlier studies of sea otter food suggested that low—density populations of sea otters consume primarily sea urchins and mollusks in the western Aleutian Islands. Later studies of high—density populations showed a wider variety of foods consumed, with fish an important component of the diet. These studies support our observations on the differences in availability of these foods between islands with and without sea otters.</span></p>","language":"English","publisher":"Ecological Society of America","doi":"10.2307/1938786","usgsCitation":"Estes, J.E., Smith, N.S., and Palmisano, J.F., 1978, Sea otter predation and community organization in the western Aleutian Island, Alaska: Ecology, v. 59, p. 822-833, https://doi.org/10.2307/1938786.","productDescription":"12 p.","startPage":"822","endPage":"833","numberOfPages":"12","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":130172,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"59","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fc57d","contributors":{"authors":[{"text":"Estes, J. E.","contributorId":80378,"corporation":false,"usgs":true,"family":"Estes","given":"J.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":316097,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smith, N. S.","contributorId":34864,"corporation":false,"usgs":true,"family":"Smith","given":"N.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":316095,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Palmisano, J. F.","contributorId":49729,"corporation":false,"usgs":true,"family":"Palmisano","given":"J.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":316096,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70010379,"text":"70010379 - 1978 - The crystal structure and thermal history of orthopyroxene from lunar anorthosite 15415","interactions":[],"lastModifiedDate":"2023-12-15T00:22:07.880503","indexId":"70010379","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1427,"text":"Earth and Planetary Science Letters","active":true,"publicationSubtype":{"id":10}},"title":"The crystal structure and thermal history of orthopyroxene from lunar anorthosite 15415","docAbstract":"<p>A single crystal of untwinned orthopyroxene from lunar anorthosite sample 15415, with composition (Mg<sub>1.14</sub>Fe<sub>0.80</sub>Mn<sub>0.02</sub>Ca<sub>0.04</sub>)(Si<sub>1.97</sub>Al<sub>0.03</sub>)O<sub>6</sub>, has a unit cell in space group<i>Pbca</i><span>&nbsp;</span>with<i>a</i><span>&nbsp;</span>= 18.310(15)Å,<i>b</i><span>&nbsp;</span>= 8.904(10)Å,<i>c</i><span>&nbsp;</span>= 5.214(7)Å, containing 2 formula units. A set of 742 counter-measured intensity data made with MoK<sub>α</sub><span>&nbsp;</span>radiation has been used to refine the crystal structure in isotropic thermal mode to<i>R</i><span>&nbsp;</span>= 0.116. Anisotropic refinement led to<i>R</i><span>&nbsp;</span>= 0.092, but thermal parameters are distorted by non-random errors resulting from poor crystal texture. The resulting structure is in close agreement with that obtained by Ghose [9] for a hypersthene from Greenland. A parameter<i>q</i>, which gives (<i>Mg</i><sub>q</sub>Fe<sub>1−q</sub>) for cation site<i>M</i>(1) and (Mg<sub>1.14−<i>q</i></sub>Fe<sub><i>q</i>−0.18</sub>Ca<sub>0.04</sub>) for site<i>M</i>(2), was included in the least-squares analysis, yielding<i>q</i><span>&nbsp;</span>= 0.90(1).</p><p>This orthopyroxene has the high degree of cation order expected of pyroxenes subjected to Apollonian metamorphism at lower than 500–600°C. No evidence exists for a subsequent thermal event of sufficient intensity to disorder the pyroxene. On the basis of previous laboratory studies of argon-release patterns of lunar plagioclase and order-disorder kinetics of terrestrial pyroxenes, we attribute the reported isotopic age (3.9–4.1 AE) to cessation of metamorphism, perhaps caused by impact excavation.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0012-821X(78)90063-8","issn":"0012821X","usgsCitation":"Evans, H.T., Stephen, H.J., and Konnert, J., 1978, The crystal structure and thermal history of orthopyroxene from lunar anorthosite 15415: Earth and Planetary Science Letters, v. 37, no. 3, p. 476-484, https://doi.org/10.1016/0012-821X(78)90063-8.","productDescription":"9 p.","startPage":"476","endPage":"484","numberOfPages":"9","costCenters":[],"links":[{"id":218721,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"37","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505baa74e4b08c986b322840","contributors":{"authors":[{"text":"Evans, H. T. Jr.","contributorId":41859,"corporation":false,"usgs":true,"family":"Evans","given":"H.","suffix":"Jr.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":358781,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stephen, Huebner J.","contributorId":31899,"corporation":false,"usgs":true,"family":"Stephen","given":"Huebner","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":358780,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Konnert, J.A.","contributorId":17640,"corporation":false,"usgs":true,"family":"Konnert","given":"J.A.","affiliations":[],"preferred":false,"id":358779,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":1007828,"text":"1007828 - 1978 - Malic acid accumulation in roots in response to flooding: Evidence contrary to its role as an alternative to ethanol","interactions":[],"lastModifiedDate":"2025-02-04T16:27:19.869213","indexId":"1007828","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2276,"text":"Journal of Experimental Botany","active":true,"publicationSubtype":{"id":10}},"title":"Malic acid accumulation in roots in response to flooding: Evidence contrary to its role as an alternative to ethanol","docAbstract":"<p><span>Across a time course of flooding the malic acid content in roots of the swamp tree&nbsp;</span><i>Nyssa sylvatica</i><span>&nbsp;var.&nbsp;</span><i>biflora</i><span>&nbsp;increased 5-fold from 1 week to 1 month of flooding and remained at that level through a full year of flooding. Alcoholic fermentation rates accelerated within the first month of flooding but dropped to very low levels under long-term flooding. The theory that, under flooding, malic acid accumulates as an alternative anaerobic end product to ethanol is unlikely in this instance since (1) malate is initially associated with high alcoholic fermentation and (2) the reduction in alcoholic fermentation is accounted for by increased internal aeration of the roots.</span></p>","language":"English","publisher":"Oxford Academic","doi":"10.1093/jxb/29.6.1345","usgsCitation":"Keeley, J.E., 1978, Malic acid accumulation in roots in response to flooding: Evidence contrary to its role as an alternative to ethanol: Journal of Experimental Botany, v. 29, p. 1345-1349, https://doi.org/10.1093/jxb/29.6.1345.","productDescription":"5 p.","startPage":"1345","endPage":"1349","numberOfPages":"5","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":130409,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"29","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db649f9e","contributors":{"authors":[{"text":"Keeley, Jon E. 0000-0002-4564-6521 jon_keeley@usgs.gov","orcid":"https://orcid.org/0000-0002-4564-6521","contributorId":1268,"corporation":false,"usgs":true,"family":"Keeley","given":"Jon","email":"jon_keeley@usgs.gov","middleInitial":"E.","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":true,"id":316105,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
]}