{"pageNumber":"5005","pageRowStart":"125100","pageSize":"25","recordCount":184617,"records":[{"id":70207789,"text":"70207789 - 1985 - Cyclic variations in calcium carbonate and organic carbon in Miocene to Holocene sediments, Walvis Ridge, South Atlantic Ocean","interactions":[],"lastModifiedDate":"2020-06-23T14:42:45.714034","indexId":"70207789","displayToPublicDate":"1985-01-10T12:30:38","publicationYear":"1985","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Cyclic variations in calcium carbonate and organic carbon in Miocene to Holocene sediments, Walvis Ridge, South Atlantic Ocean","docAbstract":"<p><span>The entire upper Miocene to Holocene sedimentary sequence recovered in a hydraulic piston core at DSDP Site 532 on Walvis Ridge shows distinct cycles in amount of CaCO sub(3) that correlate with dark and light cycles of sediment color. The average periodicities of the carbonate cycles for the Quaternary, upper Pliocene, and lower Pliocene are about 35, 46, and 28 ky, respectively, with an overall average of about 36 ky for the last 5 my. Most minima in carbonate abundance correspond to dark parts of the color cycles, and most maxmia in carbonate abundance correspond to dark parts of color cycles, The darker parts of the color cycle usually contain higher concentrations of organic&nbsp;carbon, but organic carbon does not follow the color cycles in detail. Organic carbon cycles were analyzed only for the last&nbsp;2.5 my, and for this interval they have an average periodicity&nbsp;of about 34 ky.</span></p><p><span>The carbonate and color cycles persist through more than 5my during which major changes in relative proportions of siliceous-biogenic, calcareous- biogenic and terrigenous- clastic components occurent in response to climate change and to the waxing and waning of the Benguela Current upwelling systems off southwest Africa. The cyclic nature of these sediments probably is the result of dilution by terrigrnous clastic material and not dissolution of carbonate. We believe that the forcing mechanisms that produced the cycliclity was external to the area of site 532. Because of the similarity among the periodicities of the Walvis Ridge cycles and those of carbonate cycles in the northeastern Atlantic, Caribbean and eastern equatorial Pacific, these cycles probably are responses to global events. We conclude that fluctuations om global sea level with an average period&nbsp;of about 36 ky during the last 5 my caused variations&nbsp;in influx of terrigenous clastic materials from the Africans continental margin&nbsp;</span></p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"South Atlantic Paleoceanography","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Cambridge University Press","isbn":"9780521266093","usgsCitation":"Dean, W.E., and Gardner, J.V., 1985, Cyclic variations in calcium carbonate and organic carbon in Miocene to Holocene sediments, Walvis Ridge, South Atlantic Ocean, chap. <i>of</i> South Atlantic Paleoceanography, p. 61-78.","productDescription":"17 p.","startPage":"61","endPage":"78","costCenters":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"links":[{"id":371164,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Walvis Ridge, South Atlantic","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              11.513671874999998,\n              -28.65203063036226\n            ],\n            [\n              18.1494140625,\n              -28.65203063036226\n            ],\n            [\n              18.1494140625,\n              -20.735565905218625\n            ],\n            [\n              11.513671874999998,\n              -20.735565905218625\n            ],\n            [\n              11.513671874999998,\n              -28.65203063036226\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Dean, Walter E. dean@usgs.gov","contributorId":1801,"corporation":false,"usgs":true,"family":"Dean","given":"Walter","email":"dean@usgs.gov","middleInitial":"E.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":779330,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gardner, J. V.","contributorId":114111,"corporation":false,"usgs":true,"family":"Gardner","given":"J.","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":779331,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70207753,"text":"70207753 - 1985 - Sedimentation in a blast-zone lake at Mount St. Helens, Washington—Implications for varve formation","interactions":[],"lastModifiedDate":"2020-06-22T13:00:16.339267","indexId":"70207753","displayToPublicDate":"1985-01-09T12:46:15","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1796,"text":"Geology","active":true,"publicationSubtype":{"id":10}},"title":"Sedimentation in a blast-zone lake at Mount St. Helens, Washington—Implications for varve formation","docAbstract":"<p><span>Sediment collected in traps in a newly formed lake in the blast-impact area at Mount St. Helens recorded a sediment yield that is about two orders of magnitude greater than for comparable basins with vegetation and similar precipitation. Most sediment was mobilized by storms and runoff at the onset of the wet season. The sedimentation response to strongly seasonal precipitation, in the absence of vegetation, produced turbidites and graded annual couplets. The style of sedimentation suggests an alternate mechanism for the formation of long sequences of graded clastic varves.</span></p>","language":"English","publisher":"GSA","doi":"10.1130/0091-7613(1985)13<348:SIABLA>2.0.CO;2","usgsCitation":"Anderson, R., Nuhfer, E., and Dean, W.E., 1985, Sedimentation in a blast-zone lake at Mount St. Helens, Washington—Implications for varve formation: Geology, v. 13, no. 5, p. 348-352, https://doi.org/10.1130/0091-7613(1985)13<348:SIABLA>2.0.CO;2.","productDescription":"5 p.","startPage":"348","endPage":"352","costCenters":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"links":[{"id":371113,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Washington","otherGeospatial":"Mount St. Helens","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -122.35198974609375,\n              46.21310053621607\n            ],\n            [\n              -122.01965332031249,\n              46.21310053621607\n            ],\n            [\n              -122.01965332031249,\n              46.3507193554773\n            ],\n            [\n              -122.35198974609375,\n              46.3507193554773\n            ],\n            [\n              -122.35198974609375,\n              46.21310053621607\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"13","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Anderson, R.Y.","contributorId":22789,"corporation":false,"usgs":true,"family":"Anderson","given":"R.Y.","email":"","affiliations":[],"preferred":false,"id":779194,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nuhfer, E.B.","contributorId":89281,"corporation":false,"usgs":true,"family":"Nuhfer","given":"E.B.","email":"","affiliations":[],"preferred":false,"id":779195,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dean, Walter E. dean@usgs.gov","contributorId":1801,"corporation":false,"usgs":true,"family":"Dean","given":"Walter","email":"dean@usgs.gov","middleInitial":"E.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":779196,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70207702,"text":"70207702 - 1985 - Marine geological and geophysical investigations in the Ross Sea, Antarctica","interactions":[],"lastModifiedDate":"2020-06-15T14:56:05.622096","indexId":"70207702","displayToPublicDate":"1985-01-08T10:27:27","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":812,"text":"Antarctic Journal of the United States","active":true,"publicationSubtype":{"id":10}},"title":"Marine geological and geophysical investigations in the Ross Sea, Antarctica","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"National Science Foundation, Office of Polar Programs","issn":"0003-5335","usgsCitation":"Cooper, A.K., and Davey, F., 1985, Marine geological and geophysical investigations in the Ross Sea, Antarctica: Antarctic Journal of the United States, v. 19, no. 5, p. 80-82.","productDescription":"3 p.","startPage":"80","endPage":"82","costCenters":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":371033,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Ross Sea, Antarctica","volume":"19","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Cooper, Alan K. acooper@usgs.gov","contributorId":2854,"corporation":false,"usgs":true,"family":"Cooper","given":"Alan","email":"acooper@usgs.gov","middleInitial":"K.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":779017,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Davey, F.J.","contributorId":99152,"corporation":false,"usgs":true,"family":"Davey","given":"F.J.","email":"","affiliations":[],"preferred":false,"id":779018,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70013136,"text":"70013136 - 1985 - Speciation and stasis in marine Ostracoda: Climatic modulation of evolution","interactions":[],"lastModifiedDate":"2025-09-29T16:55:43.876111","indexId":"70013136","displayToPublicDate":"1985-01-04T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Speciation and stasis in marine Ostracoda: Climatic modulation of evolution","docAbstract":"<p><span>Morphologic and paleozoogeographic analysis of Cenozoic marine Ostracoda from the Atlantic, Caribbean, and Pacific indicates that climatic change modulates evolution by disrupting long-term stasis and catalyzing speciation during sustained, unidirectional climatic transitions and, conversely, by maintaining morphologic stasis during rapid, high-frequency climatic oscillations. In the middle Pliocene, 4 to 3 million years ago, at least six new species of&nbsp;</span><i>Puriana</i><span>&nbsp;suddenly appeared as the Isthmus of Panama closed, changing oceanographic circulation and global climate. Since then morphologic stasis has characterized ancestral and descendant species during many glacial-interglacial cycles. The frequency and duration of climatic events have more impact on ostracode evolution than the magnitude of climatic changes.</span></p>","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.227.4682.60","issn":"00368075","usgsCitation":"Cronin, T.M., 1985, Speciation and stasis in marine Ostracoda: Climatic modulation of evolution: Science, v. 227, no. 4682, p. 60-63, https://doi.org/10.1126/science.227.4682.60.","productDescription":"4 p.","startPage":"60","endPage":"63","costCenters":[],"links":[{"id":220407,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"227","issue":"4682","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b94e9e4b08c986b31acb5","contributors":{"authors":[{"text":"Cronin, Thomas M. 0000-0001-9522-3992 tcronin@usgs.gov","orcid":"https://orcid.org/0000-0001-9522-3992","contributorId":304640,"corporation":false,"usgs":true,"family":"Cronin","given":"Thomas","email":"tcronin@usgs.gov","middleInitial":"M.","affiliations":[{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true}],"preferred":true,"id":365373,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70168848,"text":"70168848 - 1985 - Water resources of north-central Iowa","interactions":[],"lastModifiedDate":"2025-07-29T20:23:27.606703","indexId":"70168848","displayToPublicDate":"1985-01-01T16:45:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5106,"text":"Iowa Geological Survey Water Atlas","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"7","title":"Water resources of north-central Iowa","docAbstract":"<p>One of man's fundamental needs is water. &nbsp;Modern man needs both a safe and dependable supply of water to maintain his present economic, industrial, and cultural level. &nbsp;In order to use this natural resource in the most efficient and beneficial manner, a basic knowledge and understanding of water sources, and of the occurrence and potential of each source, needs to be gained. &nbsp;To provide this information, the U.S. Geological Survey, in cooperation with the Iowa Geological Survey, has compiled this atlas. &nbsp;It describes the water resources available for development in an 11-county area in north-central Iowa. The report contains information on the quantity, quality, and use of water from all known sources of water. &nbsp;This information is presented to aid water users and developers who are searching for and evaluating sources of water for specific sites. &nbsp;It also will be an aid to water planners and managers who must develop the available water resources on a regional basis.</p>","language":"English","publisher":"State of Iowa","publisherLocation":"Iowa City, IA","collaboration":"Prepared by the U.S. Geological Survey in cooperation with the Iowa Geological Survey","usgsCitation":"Buchmiller, R., Gaillot, G., and Soenksen, P.J., 1985, Water resources of north-central Iowa: Iowa Geological Survey Water Atlas 7, xi, 93 p.","productDescription":"xi, 93 p.","numberOfPages":"103","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true}],"links":[{"id":318601,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":493151,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70168848/IGS_Water_Atlas_Number_7.pdf","text":"Report","size":"12.4 MB","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Iowa","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-92.5536,42.9059],[-92.5549,42.8172],[-92.5548,42.7299],[-92.5554,42.6409],[-92.5553,42.555],[-92.6755,42.5558],[-92.7925,42.556],[-92.9101,42.5557],[-93.0284,42.5562],[-93.1473,42.5561],[-93.2637,42.5564],[-93.3819,42.557],[-93.5002,42.557],[-93.6191,42.5565],[-93.7367,42.5568],[-93.8563,42.557],[-93.972,42.5566],[-93.9714,42.6434],[-94.0942,42.6438],[-94.2101,42.6437],[-94.3279,42.6435],[-94.4457,42.644],[-94.4456,42.7304],[-94.4456,42.8181],[-94.4456,42.9068],[-94.4449,42.9932],[-94.4448,43.0823],[-94.4441,43.1688],[-94.4434,43.2557],[-94.4428,43.3448],[-94.4421,43.4336],[-94.4412,43.5035],[-94.2487,43.504],[-94.0783,43.5043],[-93.9691,43.5044],[-93.6782,43.5047],[-93.6485,43.5045],[-93.4964,43.504],[-93.2844,43.5032],[-93.0502,43.5034],[-93.0238,43.5035],[-92.8805,43.5033],[-92.553,43.5027],[-92.554,43.4304],[-92.5545,43.343],[-92.5545,43.2561],[-92.5544,43.2129],[-92.5538,43.1688],[-92.5543,43.0828],[-92.5543,42.9928],[-92.5536,42.9059]]]},\"properties\":{\"name\":\"Butler\",\"state\":\"IA\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56dabff9e4b015c306f84d39","contributors":{"authors":[{"text":"Buchmiller, Robert","contributorId":82742,"corporation":false,"usgs":true,"family":"Buchmiller","given":"Robert","affiliations":[],"preferred":false,"id":621984,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gaillot, Gary","contributorId":167361,"corporation":false,"usgs":false,"family":"Gaillot","given":"Gary","email":"","affiliations":[],"preferred":false,"id":621985,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Soenksen, P. J.","contributorId":71575,"corporation":false,"usgs":true,"family":"Soenksen","given":"P.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":621986,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":32543,"text":"32543 - 1985 - Networks of ecological research areas","interactions":[],"lastModifiedDate":"2014-08-01T16:01:32","indexId":"32543","displayToPublicDate":"1985-01-01T16:00:46","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Networks of ecological research areas","docAbstract":"No abstract available.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"National atlas of the United States","largerWorkSubtype":{"id":6,"text":"USGS Unnumbered Series"},"language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/32543","usgsCitation":"Turner, M.G., 1985, Networks of ecological research areas, 1 map, https://doi.org/10.3133/32543.","productDescription":"1 map","numberOfPages":"1","costCenters":[],"links":[{"id":291541,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53dca9cbe4b0761578637753","contributors":{"authors":[{"text":"Turner, Monica Goigel","contributorId":82624,"corporation":false,"usgs":true,"family":"Turner","given":"Monica","email":"","middleInitial":"Goigel","affiliations":[],"preferred":false,"id":208657,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":48904,"text":"ofr84725 - 1985 - Geohydrologic data for a low-level radioactive contamination site, Wood River Junction, Rhode Island","interactions":[],"lastModifiedDate":"2014-08-04T15:38:39","indexId":"ofr84725","displayToPublicDate":"1985-01-01T15:36:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"84-725","title":"Geohydrologic data for a low-level radioactive contamination site, Wood River Junction, Rhode Island","docAbstract":"The data, generally presented in table-format, are organized within the following six categories: Administrative, lithologic, hydrologic, chemical, geophysical, and climatological.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr84725","usgsCitation":"Ryan, B.J., 1985, Geohydrologic data for a low-level radioactive contamination site, Wood River Junction, Rhode Island: U.S. Geological Survey Open-File Report 84-725, ix, 296 p., https://doi.org/10.3133/ofr84725.","productDescription":"ix, 296 p.","costCenters":[],"links":[{"id":291631,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Rhode Island","otherGeospatial":"Wood River Junction","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -71.700597,41.433718 ], [ -71.700597,41.452087 ], [ -71.690786,41.452087 ], [ -71.690786,41.433718 ], [ -71.700597,41.433718 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53e09e52e4b0beb42bdca3fd","contributors":{"authors":[{"text":"Ryan, Barbara J.","contributorId":62989,"corporation":false,"usgs":true,"family":"Ryan","given":"Barbara","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":238545,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70006529,"text":"70006529 - 1985 - Growth of submersed macrophyte communities in the St. Clair - Detroit River system between Lake Huron and Lake Erie","interactions":[],"lastModifiedDate":"2016-03-28T14:31:03","indexId":"70006529","displayToPublicDate":"1985-01-01T14:54:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1167,"text":"Canadian Journal of Botany","active":true,"publicationSubtype":{"id":10}},"title":"Growth of submersed macrophyte communities in the St. Clair - Detroit River system between Lake Huron and Lake Erie","docAbstract":"<p><span>Growth of submersed aquatic macrophytes was determined from observation and on the basis of biomass of samples collected from April to November 1978 at seven study sites in a major river system of the Great Lakes, the St. Clair &ndash; Detroit river system between Lake Huron and Lake Erie. Growth usually began between April and June, peaked between July and October, and decreased by late November. Maximum biomass at six of the seven sites (118&ndash;427&ensp;g dry weight m</span><sup>&minus;2</sup><span>) was similar or greater than that reported in other rivers at similar latitudes. Seasonal growth of the abundant taxa followed one of three seasonal patterns at each study site: one dominant taxon grew alone; codominant taxa grew sympatrically without species succession; and codominant taxa grew sympatrically with species succession. Differences in growth and seasonal succession of some taxa were apparently caused by the presence or absence of overwintering plant material, competition, and life-cycle differences.</span></p>","language":"English","publisher":"NRC Research Press","publisherLocation":"Ottawa, Ontario","doi":"10.1139/b85-145","usgsCitation":"Schloesser, D.W., Edsall, T.A., and Manny, B.A., 1985, Growth of submersed macrophyte communities in the St. Clair - Detroit River system between Lake Huron and Lake Erie: Canadian Journal of Botany, v. 63, no. 6, p. 1061-1065, https://doi.org/10.1139/b85-145.","productDescription":"5 p.","startPage":"1061","endPage":"1065","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":262260,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"63","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50de6ceee4b0e31bb02a37e2","contributors":{"authors":[{"text":"Schloesser, Donald W. dschloesser@usgs.gov","contributorId":3579,"corporation":false,"usgs":true,"family":"Schloesser","given":"Donald","email":"dschloesser@usgs.gov","middleInitial":"W.","affiliations":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"preferred":true,"id":354684,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Edsall, Thomas A.","contributorId":84302,"corporation":false,"usgs":true,"family":"Edsall","given":"Thomas","email":"","middleInitial":"A.","affiliations":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"preferred":false,"id":354686,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Manny, Bruce A. 0000-0002-4074-9329 bmanny@usgs.gov","orcid":"https://orcid.org/0000-0002-4074-9329","contributorId":3699,"corporation":false,"usgs":true,"family":"Manny","given":"Bruce","email":"bmanny@usgs.gov","middleInitial":"A.","affiliations":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"preferred":true,"id":354685,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70006914,"text":"70006914 - 1985 - Uptake, biotransformation, and elimination of rotenone by bluegills (Lepomis macrochirus )","interactions":[],"lastModifiedDate":"2012-10-15T17:16:41","indexId":"70006914","displayToPublicDate":"1985-01-01T14:51:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":874,"text":"Aquatic Toxicology","active":true,"publicationSubtype":{"id":10}},"title":"Uptake, biotransformation, and elimination of rotenone by bluegills (Lepomis macrochirus )","docAbstract":"Yearling bluegills (<i>Lepomis macrochirus</i>) were exposed to sublethal concentrations of [<sup>14</sup>C]rotenone (5.2 &mu;g/l) for 30 days in a continuous flow exposure system and then transferred to clean, flowing water for an additional 21-day depuration period. Rates of uptake and elimination and profile of the rotenoid metabolites in head, viscera, and carcass components were evaluated by <sup>14</sup>C counting and by high performance liquid chromatography. Total [<sup>14</sup>C]rotenone derived activity was relatively uniform in all body components within 3 days after initial exposure and remained constant during the ensuing 27 days of exposure. Initial uptake rate coefficients were highest in viscera (K<sub>u</sub> = 80&middot; h <sup>-1</sup>) and were nearly identical for head (K<sub>u</sub> = 14 &middot; h) and carcass (K<sub>u</sub> = 10 &middot; h<sup>-1</sup>). Analyses of tissue extracts by high performance liquid chromatography confirmed the presence of at least six biotransformation products of rotenone. More than 60% of the activity extracted from viscera was present as a single peak which represented a compound that was extremely soluble in water. Rotenone composed only 0.3% of the extractable activity in viscera taken from fish exposed to rotenone for 30 days; however, rotenone accounted for 15.4% of extractable activity in the head and 20.1% in the carcass components. Rotenolone and 6<i>'</i>,7<i>'</i>-dihydro-6<i>'</i>-,7<i>'</i>--dihydroxyrotenolone were tentatively identified as oxidation products in all tissue extracts. Elimination of <sup>14</sup>C activity from all body components was biphasic; both phases followed first-order kinetics. The rate of elimination was nearly equal for all body components during the initial phase but was most rapid from viscera during the second phase of elimination. Bioconcentration factors for the head, viscera, and carcass were 165, 3,550, and 125, respectively, when calculated on the basis of total <sup>14</sup>C activity but only 25.4, 11, and 26 when calculated as the concentration of parent material.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Aquatic Toxicology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","publisherLocation":"Amsterdam, Netherlands","doi":"10.1016/0166-445X(85)90003-7","collaboration":"Abstract has subscript/superscript to be fixed","usgsCitation":"Gingerich, W., and Rach, J., 1985, Uptake, biotransformation, and elimination of rotenone by bluegills (Lepomis macrochirus ): Aquatic Toxicology, v. 6, no. 3, p. 179-186, https://doi.org/10.1016/0166-445X(85)90003-7.","productDescription":"18 p.","startPage":"179","endPage":"186","numberOfPages":"8","costCenters":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":262594,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":262592,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0166-445X(85)90003-7"}],"volume":"6","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50e55f63e4b0a4aa5bb03eb7","contributors":{"authors":[{"text":"Gingerich, W.H.","contributorId":83481,"corporation":false,"usgs":true,"family":"Gingerich","given":"W.H.","email":"","affiliations":[],"preferred":false,"id":355460,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rach, J.J.","contributorId":73948,"corporation":false,"usgs":true,"family":"Rach","given":"J.J.","email":"","affiliations":[],"preferred":false,"id":355459,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70095009,"text":"70095009 - 1985 - Mapping and research in the exclusive economic zone","interactions":[],"lastModifiedDate":"2014-03-25T10:33:18","indexId":"70095009","displayToPublicDate":"1985-01-01T14:20:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Mapping and research in the exclusive economic zone","docAbstract":"By proclamation of the President on March 10, \n1983, the United States claimed sovereign rights and \njurisdiction within an Exclusive Economic Zone \n(EEZ). The United States is responsible for wisely \ndeveloping and managing the EEZ and its marine \nresources and for protecting its environment. \n\nThe U.S. Exclusive Economic Zone is a region that\nextends seaward 200 nautical miles from the coast\nand brings within the national domain over 3 million\nsquare nautical miles of submarine lands. The EEZ\ncontains vital natural resources, both living and nonliving,\nof the seabed, subsoil, and overlying water.\nBecause most of the EEZ has not been explored, its\nresources and their potential remain undefined","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70095009","usgsCitation":"McGregor, B.A., and Lockwood, M., 1985, Mapping and research in the exclusive economic zone, 40 p., https://doi.org/10.3133/70095009.","productDescription":"40 p.","numberOfPages":"42","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":282851,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70095009.jpg"},{"id":284831,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70095009/report.pdf"}],"country":"United States","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 144.616667,13.233333 ], [ 144.616667,71.833333 ], [ -64.566667,71.833333 ], [ -64.566667,13.233333 ], [ 144.616667,13.233333 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"535594b0e4b0120853e8c06c","contributors":{"authors":[{"text":"McGregor, Bonnie A.","contributorId":61022,"corporation":false,"usgs":true,"family":"McGregor","given":"Bonnie","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":491057,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lockwood, Millington","contributorId":91843,"corporation":false,"usgs":true,"family":"Lockwood","given":"Millington","email":"","affiliations":[],"preferred":false,"id":491058,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70170848,"text":"70170848 - 1985 - Confined-drift aquifers studied near the Pomme de Terre and Chippewa Rivers, west-central Minnesota","interactions":[],"lastModifiedDate":"2018-03-12T10:25:04","indexId":"70170848","displayToPublicDate":"1985-01-01T14:15:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":375,"text":"Open-File Report","active":false,"publicationSubtype":{"id":6}},"title":"Confined-drift aquifers studied near the Pomme de Terre and Chippewa Rivers, west-central Minnesota","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70170848","usgsCitation":"Delin, G., 1985, Confined-drift aquifers studied near the Pomme de Terre and Chippewa Rivers, west-central Minnesota: Open-File Report, 2 p., https://doi.org/10.3133/70170848.","productDescription":"2 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":320974,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Minnesota","otherGeospatial":"Chippewa River and Pomme de Terre River","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"572b1d2ee4b0b13d391b4471","contributors":{"authors":[{"text":"Delin, G. N.","contributorId":12834,"corporation":false,"usgs":true,"family":"Delin","given":"G. N.","affiliations":[],"preferred":false,"id":628811,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70120935,"text":"70120935 - 1985 - Discussion of 'Critical water velocity for snail habitats in canals' by W. R. Jobin, A. Laracuente, R. Mercado, and H. Negron-Aponte","interactions":[],"lastModifiedDate":"2024-04-22T15:42:44.25654","indexId":"70120935","displayToPublicDate":"1985-01-01T14:11:37","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2255,"text":"Journal of Environmental Engineering","active":true,"publicationSubtype":{"id":10}},"title":"Discussion of 'Critical water velocity for snail habitats in canals' by W. R. Jobin, A. Laracuente, R. Mercado, and H. Negron-Aponte","docAbstract":"No abstract available.","language":"English","publisher":"American Society of Civil Engineers","publisherLocation":"Reston, VA","doi":"10.1061/(ASCE)0733-9372(1985)111:3(389)","usgsCitation":"Milhous, R.T., 1985, Discussion of 'Critical water velocity for snail habitats in canals' by W. R. Jobin, A. Laracuente, R. Mercado, and H. Negron-Aponte: Journal of Environmental Engineering, v. 111, no. 3, p. 389-392, https://doi.org/10.1061/(ASCE)0733-9372(1985)111:3(389).","productDescription":"4 p.","startPage":"389","endPage":"392","numberOfPages":"4","costCenters":[],"links":[{"id":292463,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"111","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53f25fe0e4b033341871890a","contributors":{"authors":[{"text":"Milhous, Robert T.","contributorId":28646,"corporation":false,"usgs":true,"family":"Milhous","given":"Robert","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":498646,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70120934,"text":"70120934 - 1985 - Summaries of selected mitigation evaluation studies","interactions":[],"lastModifiedDate":"2014-08-18T14:10:27","indexId":"70120934","displayToPublicDate":"1985-01-01T14:09:55","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":9,"text":"Other Report"},"seriesNumber":"WELUT-86/W03","title":"Summaries of selected mitigation evaluation studies","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Fish and Wildlife Service, Western Energy and Land Use Team","publisherLocation":"Fort Collins, CO","usgsCitation":"Horak, G., 1985, Summaries of selected mitigation evaluation studies, 63 p.","productDescription":"63 p.","numberOfPages":"63","costCenters":[],"links":[{"id":292462,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53f25fefe4b033341871895f","contributors":{"authors":[{"text":"Horak, G.C.","contributorId":48112,"corporation":false,"usgs":true,"family":"Horak","given":"G.C.","email":"","affiliations":[],"preferred":false,"id":498645,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70120932,"text":"70120932 - 1985 - Nutritional ecology of a fossorial herbivore: protein N and energy value of winter caches made by the northern pocket gopher, <i>Thomomys talpoides</i>","interactions":[],"lastModifiedDate":"2014-08-18T13:51:10","indexId":"70120932","displayToPublicDate":"1985-01-01T13:49:42","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1176,"text":"Canadian Journal of Zoology","active":true,"publicationSubtype":{"id":10}},"title":"Nutritional ecology of a fossorial herbivore: protein N and energy value of winter caches made by the northern pocket gopher, <i>Thomomys talpoides</i>","docAbstract":"Northern pocket gophers (<i>Thomomys talpoides</i>) are fossorial herbivores that excavate belowground plant parts for food. In subalpine areas during autumn and winter, pocket gophers hoard plant parts in caches placed in or under snow. We examined the size and composition of 17 nival caches and tested the hypotheses that (i) cached food can provide complete energy and protein N sustenance during typical periods when burrowing is precluded by soil conditions, and (ii) cached food is a random sample of items encountered by burrowing gophers during tunnel excavation. Our data indicate that caches provide substantially more energy than protein in terms of a pocket gopher's daily maintenance requirements. Nevertheless, quantities stored are sufficient to allow individuals to endure commonly encountered adverse environmental conditions without entering negative energy or protein balance. Analysis of stomach contents and a comparison of cache composition to availability of plant species suggests that gophers consume high-protein items as they are encountered, and store low-protein items in caches.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Canadian Journal of Zoology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"National Research Council of Canada","publisherLocation":"Ottawa","doi":"10.1139/z85-165","usgsCitation":"Stuebe, M.M., and Andersen, D., 1985, Nutritional ecology of a fossorial herbivore: protein N and energy value of winter caches made by the northern pocket gopher, <i>Thomomys talpoides</i>: Canadian Journal of Zoology, v. 63, no. 5, p. 1101-1105, https://doi.org/10.1139/z85-165.","productDescription":"5 p.","startPage":"1101","endPage":"1105","numberOfPages":"5","costCenters":[],"links":[{"id":292457,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":292456,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1139/z85-165"}],"volume":"63","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53f25fe9e4b0333418718939","contributors":{"authors":[{"text":"Stuebe, Miki M.","contributorId":72311,"corporation":false,"usgs":true,"family":"Stuebe","given":"Miki","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":498642,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Andersen, Douglas C. doug_andersen@usgs.gov","contributorId":2216,"corporation":false,"usgs":true,"family":"Andersen","given":"Douglas C.","email":"doug_andersen@usgs.gov","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":false,"id":498641,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70120928,"text":"70120928 - 1985 - Information needs for natural fire management planning","interactions":[],"lastModifiedDate":"2014-08-18T13:47:19","indexId":"70120928","displayToPublicDate":"1985-01-01T13:44:31","publicationYear":"1985","noYear":false,"publicationType":{"id":4,"text":"Book"},"publicationSubtype":{"id":12,"text":"Conference publication"},"title":"Information needs for natural fire management planning","docAbstract":"The development and implementation of an effective natural fire management program require a clear definition of goals and objectives, an ever-expanding information base, and effective program evaluation.  Examples are given from Sequoia and Kings Canyon National Parks.","largerWorkTitle":"Proceedings, Symposium and Workshop on Wilderness Fire","conferenceTitle":"Wilderness Fire Symposium","conferenceDate":"1983-11-15T00:00:00","conferenceLocation":"Missoula, MT","language":"English","publisher":"Intermountain Forest and Range Experiment Station","publisherLocation":"Ogden, UT","usgsCitation":"Parsons, D., Bancroft, L., Nichols, T., and Stohlgren, T., 1985, Information needs for natural fire management planning, 6 p.","productDescription":"6 p.","numberOfPages":"6","costCenters":[],"links":[{"id":292455,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53f25fe6e4b0333418718922","contributors":{"authors":[{"text":"Parsons, David","contributorId":44090,"corporation":false,"usgs":true,"family":"Parsons","given":"David","affiliations":[],"preferred":false,"id":498635,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bancroft, Larry","contributorId":97831,"corporation":false,"usgs":true,"family":"Bancroft","given":"Larry","email":"","affiliations":[],"preferred":false,"id":498637,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Nichols, Thomas","contributorId":71109,"corporation":false,"usgs":true,"family":"Nichols","given":"Thomas","affiliations":[],"preferred":false,"id":498636,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Stohlgren, Thomas","contributorId":22206,"corporation":false,"usgs":true,"family":"Stohlgren","given":"Thomas","affiliations":[],"preferred":false,"id":498634,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70226902,"text":"70226902 - 1985 - Minor Creek landslide","interactions":[],"lastModifiedDate":"2021-12-20T19:51:11.459255","indexId":"70226902","displayToPublicDate":"1985-01-01T13:36:09","publicationYear":"1985","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Minor Creek landslide","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Redwood country: American Geomorphological Field Group field trip guidebook","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"American Geomorphological Field Group","usgsCitation":"Iverson, R.M., 1985, Minor Creek landslide, chap. <i>of</i> Redwood country: American Geomorphological Field Group field trip guidebook, p. 40-50.","productDescription":"11 p.","startPage":"40","endPage":"50","costCenters":[{"id":157,"text":"Cascades Volcano Observatory","active":false,"usgs":true}],"links":[{"id":393112,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Minor Creek","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -123.84316921234131,\n              40.95941904108161\n            ],\n            [\n              -123.80119800567626,\n              40.95941904108161\n            ],\n            [\n              -123.80119800567626,\n              40.96693739752686\n            ],\n            [\n              -123.84316921234131,\n              40.96693739752686\n            ],\n            [\n              -123.84316921234131,\n              40.95941904108161\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"editors":[{"text":"Savina, Mary E.","contributorId":270217,"corporation":false,"usgs":false,"family":"Savina","given":"Mary","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":828731,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Iverson, Richard M. 0000-0002-7369-3819 riverson@usgs.gov","orcid":"https://orcid.org/0000-0002-7369-3819","contributorId":536,"corporation":false,"usgs":true,"family":"Iverson","given":"Richard","email":"riverson@usgs.gov","middleInitial":"M.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true},{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true}],"preferred":true,"id":828730,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70120926,"text":"70120926 - 1985 - Fire-caused mortality in chamise chaparral","interactions":[],"lastModifiedDate":"2014-08-18T13:37:08","indexId":"70120926","displayToPublicDate":"1985-01-01T13:35:56","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":9,"text":"Other Report"},"seriesNumber":"Gen. Tech. Rep. INT-182","title":"Fire-caused mortality in chamise chaparral","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Department of Agriculture, Forest Service","publisherLocation":"Ogden, UT","usgsCitation":"Stohlgren, T., 1985, Fire-caused mortality in chamise chaparral, 3 p.","productDescription":"3 p.","startPage":"385","endPage":"387","numberOfPages":"3","costCenters":[],"links":[{"id":292452,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53f25fe5e4b033341871891b","contributors":{"authors":[{"text":"Stohlgren, T.J.","contributorId":7217,"corporation":false,"usgs":true,"family":"Stohlgren","given":"T.J.","email":"","affiliations":[],"preferred":false,"id":498633,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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 \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Borcherdt, Roger D. 0000-0002-8668-0849 borcherdt@usgs.gov","orcid":"https://orcid.org/0000-0002-8668-0849","contributorId":2373,"corporation":false,"usgs":true,"family":"Borcherdt","given":"Roger","email":"borcherdt@usgs.gov","middleInitial":"D.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":848557,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bolt, B. A.","contributorId":152427,"corporation":false,"usgs":false,"family":"Bolt","given":"B.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":848558,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70114204,"text":"70114204 - 1985 - Hydrogeology, digital solute-transport simulation, and geochemistry of the Lower Cretaceous aquifer system near Baltimore, Maryland","interactions":[],"lastModifiedDate":"2017-03-08T15:11:45","indexId":"70114204","displayToPublicDate":"1985-01-01T13:01:54","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":121,"text":"Maryland Geological Survey Report of Investigations","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"43","title":"Hydrogeology, digital solute-transport simulation, and geochemistry of the Lower Cretaceous aquifer system near Baltimore, Maryland","docAbstract":"<p>This study was made to develop information on the hydrogeology and ground-water geochemistry of the Patuxent and Patapsco aquifers (Lower Cretaceous) near Baltimore, Maryland. This information is needed to evaluate the availability and chemical quality of water from these aquifers.</p><p>The Patuxent aquifer unconformably overlies Lower Paleozoic and Precambrian basement rocks and consists primarily of medium- to coarse-grained quartz sand. Discontinuous lenses of gravel and silty clay are commonly interbedded with the sand-sized material. The Patuxent aquifer in this area attains a thickness of 250 feet and transmissivities range from 2,000 to 8,000 feet squared per day. The Patuxent is the most productive source of ground water in the Baltimore area. In 1982, approximately 11 million gallons of water per day was produced from this unit. Several cones of depression, ranging from 30 to 50 feet below sea level, have developed in response to this pumping stress.</p><p>The Arundel Formation conformably overlies the Patuxent aquifer. The Arundel is composed predominantly of clay and ranges from 0 to 150 feet thick. The Arundel exhibits very low vertical hydraulic conductivities that are on the order of 10<sup>-9</sup> to 10<sup>-11</sup> feet per second. This unit acts as the upper confining bed of the Patuxent aquifer in much of the project area. The Patapsco aquifer unconformably overlies the Arundel Formation and is a medium- to fine-grained quartz sand. The Patapsco functions as a water-table aquifer in much of the project area. Although the Patapsco has been heavily pumped in the past, pumpage from that aquifer in Baltimore was negligible in 1982.</p><p>Brackish-water contamination of the Patuxent and Patapsco aquifers has been a major water-quality problem since the early 1900's. The Patuxent aquifer presently (1982) contains a circular plume of brackish-water contamination about 5 miles in diameter. This plume is centered on the Harbor district and has enlarged measurably since 1945. The Patapsco aquifer has a smaller zone of brackish-water contamination that has decreased in size since 1945. Borehole data demonstrate that the Arundel Formation has been breached by Pleistocene river channels near the Harbor district. These erosional channels provide a conduit for brackish water to intrude into the Patuxent aquifer. A two-dimensional areal solute-transport model of the Patuxent aquifer was constructed. This model was designed to estimate the future movement of the brackish-water plume based on alternative scenarios of aquifer use. Model simulations suggest that the plume will remain relatively immobile if 1982 pumping patterns continue into the foreseeable future. However, increased pumpage in the Marley Neck peninsula could draw the plume to the southeast and increase contamination of the Fairfield area.</p><p>The water quality of the Patuxent aquifer is extremely variable. Because of this variability, it is useful to divide the aquifer into three water-quality zones: Zone 1 -- This zone corresponds to the plume of brackish-water contamination. Zone 2 -- This zone exhibits evidence of urbanization-related contamination such as measurable concentrations of organic chemicals and elevated concentrations of trace elements and total organic carbon. Zone 3 -- Water composition in this zone is controlled exclusively by naturally occurring chemical processes. These processes are dominated by reactions involving dissolved iron. Near the outcrop area, oxidation of pyrite and lignite consumes dissolved oxygen and produces ledges of iron hydroxide-cemented sandstones and conglomerates. The predominant dissolved iron species in oxic water is Fe(OH)<sub>2</sub><sup>+</sup>. Downgradient, the water becomes anoxic and sulfate reduction becomes an important process. The predominant dissolved iron species in anoxic water is Fe<sup>2+</sup>.</p>","language":"English","publisher":"Maryland Geological Survey","collaboration":"Prepared in cooperation with the United States Department of the Interior Geological Survey","usgsCitation":"Chapelle, F.H., 1985, Hydrogeology, digital solute-transport simulation, and geochemistry of the Lower Cretaceous aquifer system near Baltimore, Maryland: Maryland Geological Survey Report of Investigations 43, Report: vi, 120 p.; 2 Plates: 12.35 x 15.77 inches and 13.82 x 9.30 inches.","productDescription":"Report: vi, 120 p.; 2 Plates: 12.35 x 15.77 inches and 13.82 x 9.30 inches","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":290145,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":290144,"rank":4,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70114204/report.pdf","text":"Report","size":"60.51 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":290142,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70114204/plate-1.pdf","text":"Plate 1","size":"699.75 KB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 1"},{"id":290143,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70114204/plate-2.pdf","text":"Plate 2","size":"369.62 KB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 2"}],"country":"United States","state":"Maryland","city":"Baltimore","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -76.798553,39.025052 ], [ -76.798553,39.45104 ], [ -76.315842,39.45104 ], [ -76.315842,39.025052 ], [ -76.798553,39.025052 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53aa9df3e4b065055fab166b","contributors":{"compilers":[{"text":"with a section compiled by Kean, Tracey M.","contributorId":16756,"corporation":false,"usgs":true,"family":"with a section compiled by Kean","given":"Tracey","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":681410,"contributorType":{"id":3,"text":"Compilers"},"rank":1}],"authors":[{"text":"Chapelle, Francis H. chapelle@usgs.gov","contributorId":1350,"corporation":false,"usgs":true,"family":"Chapelle","given":"Francis","email":"chapelle@usgs.gov","middleInitial":"H.","affiliations":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true},{"id":559,"text":"South Carolina Water Science Center","active":true,"usgs":true}],"preferred":true,"id":495266,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70120906,"text":"70120906 - 1985 - Chronology of migration by American coots in Oklahoma","interactions":[],"lastModifiedDate":"2014-08-18T12:52:01","indexId":"70120906","displayToPublicDate":"1985-01-01T12:47:17","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2508,"text":"Journal of Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"Chronology of migration by American coots in Oklahoma","docAbstract":"American coots (<i>Fulica americana</i>) were studied on large reservoirs in north-central Oklahoma in 1979-1982 to determine chronologies of migrations by age- and sex class.  Coots began migrating into Oklahoma in mid-September, numbers peaked in early to mid-October, and few birds were seen after 1 November.  Some late migrants appeared in mid-December.  In spring, coots began migrating in late February, numbers peaked in mid-April, and the last birds were seen in mid-May.  Generally, adult and juvenile males and juvenile female coots migrated simultaneously in autumn, but adult females completed migration by 1 November.  A few juveniles and adult males migrated in December.  Adult coots preceded yearlings in spring.  Despite annual and between-lake differences in chronology of autumn migration, most coots migrated before waterfowl hunting season in Oklahoma.  Coot hunting seasons in mid-latitude states should commence before the general waterfowl season where management goals are to increase hunter interest and the harvest of birds.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Wildlife Management","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Wildlife Society","publisherLocation":"Washington, D.C.","doi":"10.2307/3801878","usgsCitation":"Eddleman, W.R., Knopf, F., and Patterson, C.T., 1985, Chronology of migration by American coots in Oklahoma: Journal of Wildlife Management, v. 49, no. 1, p. 241-246, https://doi.org/10.2307/3801878.","productDescription":"6 p.","startPage":"241","endPage":"246","numberOfPages":"6","costCenters":[],"links":[{"id":292428,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":292427,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.2307/3801878"}],"country":"United States","state":"Oklahoma","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -103.0025,33.6158 ], [ -103.0025,37.0023 ], [ -94.4307,37.0023 ], [ -94.4307,33.6158 ], [ -103.0025,33.6158 ] ] ] } } ] }","volume":"49","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53f25fdbe4b03334187188fe","contributors":{"authors":[{"text":"Eddleman, William R.","contributorId":40685,"corporation":false,"usgs":true,"family":"Eddleman","given":"William","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":498587,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Knopf, Fritz L.","contributorId":30549,"corporation":false,"usgs":true,"family":"Knopf","given":"Fritz L.","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":false,"id":498586,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Patterson, Craig T.","contributorId":15940,"corporation":false,"usgs":true,"family":"Patterson","given":"Craig","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":498585,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70247994,"text":"70247994 - 1985 - Analysis of gravity data in volcanic terrain and gravity anomalies and subvolcanic intrusions in the Cascade Range, U.S.A., and at other selected volcanoes","interactions":[],"lastModifiedDate":"2023-08-30T17:49:46.327196","indexId":"70247994","displayToPublicDate":"1985-01-01T12:35:19","publicationYear":"1985","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"chapter":"28","title":"Analysis of gravity data in volcanic terrain and gravity anomalies and subvolcanic intrusions in the Cascade Range, U.S.A., and at other selected volcanoes","docAbstract":"<p>Gravity data were investigated to reveal the presence of subvolcanic intrusions. With few exceptions, these intrusions produce a detectable gravity anomaly. In the past, these gravity anomalies have often been overlooked or misinterpreted because the data reduction procedure was inadequate. A pragmatic method for reducing and interpreting reconnaissance gravity data from volcanoes as well as gravity models of a variety of volcanoes is developed.</p><p>Large calderas (diameters greater than 15 km) have relatively low-density intrusions beneath them. All other large volcanic systems that would include small calderas (diameters less than 15 km) have relatively high-density intrusions beneath them. The density contrasts that produce the observed anomalies occur between the intrusion, whose density is usually greater than 2.6 g/cm<sup>3</sup>, and the country rock. Commonly, the shallow country rock is an older volcanic layer with a density less than 2.5 g/cm<sup>3</sup>. The result of the contrast is a positive anomaly over the intrusion. For larger calderas, the surrounding volcanic layer is usually thin and overlies dense metamorphic and plutonic country rocks. In this case, we find the intrusion commonly less dense than country rock. The result is a negative anomaly.</p><p>In modeling volcanoes of the Cascade Range, gravity data and geologic considerations required a bottom on the intrusion. This may be an actual bottom or the depth at which the density contrast between the intrusion and the country rock disappears. The tops of the intrusions are usually shallow and are significantly wider than overlying craters or calderas. Calderas are associated with wider intrusions. Some intrusions are single cooling units, but more commonly they are an accumulation of the unerupted portions of individual magmatic injections. These injections could occur periodically throughout the life of the volcano, and would generally be accompanied by eruption. Comparing the volume of the intrusion and the volume of the volcanic edifice indicates that only a small part of a magma injection erupts, although some of the apparent intrusive material may be reworked older volcanics. Exceptions to the general discussion presented tend to be related to the nature of the country rock.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"The utility of regional gravity and magnetic anomaly maps","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Society of Exploration Geophysicists","doi":"10.1190/1.0931830346.ch28","usgsCitation":"Williams, D.L., and Finn, C.A., 1985, Analysis of gravity data in volcanic terrain and gravity anomalies and subvolcanic intrusions in the Cascade Range, U.S.A., and at other selected volcanoes, chap. 28 <i>of</i> The utility of regional gravity and magnetic anomaly maps, p. 361-374, https://doi.org/10.1190/1.0931830346.ch28.","productDescription":"14 p.","startPage":"361","endPage":"374","costCenters":[],"links":[{"id":420309,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California, Oregon, 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L.","contributorId":10028,"corporation":false,"usgs":true,"family":"Williams","given":"David","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":881452,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Finn, Carol A. 0000-0002-6178-0405 cfinn@usgs.gov","orcid":"https://orcid.org/0000-0002-6178-0405","contributorId":1326,"corporation":false,"usgs":true,"family":"Finn","given":"Carol","email":"cfinn@usgs.gov","middleInitial":"A.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":881453,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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