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,{"id":5210336,"text":"5210336 - 1984 - An introduction to statistical and ecological software","interactions":[],"lastModifiedDate":"2013-02-19T20:13:18","indexId":"5210336","displayToPublicDate":"2009-06-09T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"seriesNumber":"845","title":"An introduction to statistical and ecological software","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Statistics in Environmental Sciences: A Symposium","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","publisher":"American Society for Testing and Materials","publisherLocation":"Philadelphia, Pa.","doi":"10.1520/STP30260S","usgsCitation":"Hensler, G.L., 1984, An introduction to statistical and ecological software, chap. <i>of</i> Statistics in Environmental Sciences: A Symposium, p. 74-89, https://doi.org/10.1520/STP30260S.","startPage":"74","endPage":"89","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":201202,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":267809,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1520/STP30260S"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad7e4b07f02db68437f","contributors":{"editors":[{"text":"Gertz, S.M.","contributorId":113103,"corporation":false,"usgs":true,"family":"Gertz","given":"S.M.","email":"","affiliations":[],"preferred":false,"id":506302,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"London, M.D.","contributorId":113868,"corporation":false,"usgs":true,"family":"London","given":"M.D.","email":"","affiliations":[],"preferred":false,"id":506303,"contributorType":{"id":2,"text":"Editors"},"rank":2}],"authors":[{"text":"Hensler, Gary L.","contributorId":23111,"corporation":false,"usgs":true,"family":"Hensler","given":"Gary","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":328219,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":5200226,"text":"5200226 - 1984 - Maui-Molokai forest birds recovery plan, May 1984","interactions":[],"lastModifiedDate":"2012-02-02T00:15:16","indexId":"5200226","displayToPublicDate":"2009-06-08T16:49:39","publicationYear":"1984","noYear":false,"publicationType":{"id":4,"text":"Book"},"title":"Maui-Molokai forest birds recovery plan, May 1984","language":"English","publisher":"U.S. Fish and Wildlife Service","publisherLocation":"Portland, Oregon","usgsCitation":"Kepler, C.B., Burr, T., Cooper, C., Dunatchik, D., Medeiros, J., Scott, J.M., Ueoko, M., and Wong, W., 1984, Maui-Molokai forest birds recovery plan, May 1984, 110.","productDescription":"110","numberOfPages":"110","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":201365,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a27e4b07f02db6100b2","contributors":{"authors":[{"text":"Kepler, C. B.","contributorId":62548,"corporation":false,"usgs":true,"family":"Kepler","given":"C.","middleInitial":"B.","affiliations":[],"preferred":false,"id":327265,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Burr, T.","contributorId":88062,"corporation":false,"usgs":true,"family":"Burr","given":"T.","email":"","affiliations":[],"preferred":false,"id":327266,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cooper, C.B.","contributorId":101777,"corporation":false,"usgs":true,"family":"Cooper","given":"C.B.","email":"","affiliations":[],"preferred":false,"id":327267,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Dunatchik, D.","contributorId":57993,"corporation":false,"usgs":true,"family":"Dunatchik","given":"D.","email":"","affiliations":[],"preferred":false,"id":327264,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Medeiros, J.","contributorId":108228,"corporation":false,"usgs":true,"family":"Medeiros","given":"J.","email":"","affiliations":[],"preferred":false,"id":327268,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Scott, J. M.","contributorId":55766,"corporation":false,"usgs":true,"family":"Scott","given":"J.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":327263,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Ueoko, M.","contributorId":36260,"corporation":false,"usgs":true,"family":"Ueoko","given":"M.","email":"","affiliations":[],"preferred":false,"id":327262,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Wong, W.","contributorId":19667,"corporation":false,"usgs":true,"family":"Wong","given":"W.","email":"","affiliations":[],"preferred":false,"id":327261,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":5200283,"text":"5200283 - 1984 - Masked Bobwhite Recovery Plan","interactions":[],"lastModifiedDate":"2012-02-02T00:15:17","indexId":"5200283","displayToPublicDate":"2009-06-08T16:49:39","publicationYear":"1984","noYear":false,"publicationType":{"id":4,"text":"Book"},"title":"Masked Bobwhite Recovery Plan","docAbstract":"The following steps, as outlined in the plan, must be implemented before considering reclassification of the endangered masked bobwhite: 1) reestablishment of three or more self-sustaining populations in Arizona; 2) maintenance and/or reestablishment of one or more self-sustaining populations in Mexico; and 3) permanent protection of all habitat supporting these populations. (In the plan, a self-sustaining population is defined as an annual average of 200 or more calling males for at least 5 years.) In addition, the plan calls for interim maintenance of a captive population, as well as additional ecological and life history studies.","language":"English","publisher":"U.S. Fish and Wildlife Service, Office of Endangered Species, Region II","publisherLocation":"Albuquerque, New Mexico","collaboration":"Revised narrative by D.H. Ellis; revised implementation schedule by S.J. Hoffman","usgsCitation":"Brown, D., Ellis, D.H., and Hoffman, S., 1984, Masked Bobwhite Recovery Plan (1984 Revision), iii, 82.","productDescription":"iii, 82","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":201373,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"edition":"1984 Revision","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a26e4b07f02db60fcc9","contributors":{"authors":[{"text":"Brown, D.E.","contributorId":91879,"corporation":false,"usgs":true,"family":"Brown","given":"D.E.","email":"","affiliations":[],"preferred":false,"id":327415,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ellis, D. H.","contributorId":79830,"corporation":false,"usgs":true,"family":"Ellis","given":"D.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":327414,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hoffman, S.W.","contributorId":29105,"corporation":false,"usgs":true,"family":"Hoffman","given":"S.W.","email":"","affiliations":[],"preferred":false,"id":327413,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70039514,"text":"70039514 - 1984 - Geographic Names Information System","interactions":[],"lastModifiedDate":"2012-08-11T01:01:51","indexId":"70039514","displayToPublicDate":"2008-01-23T16:11:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Geographic Names Information System","docAbstract":"The Geographic Names Information System (GNIS) is an automated data system developed by the U.S. Geological Survey (USGS) to standardize and disseminate information on geographic names. GNIS provides primary information for all known places, features, and areas in the United States identified by a proper name. The information in the system can be manipulated to meet varied needs. You can incorporate information from GNIS into your own data base for special applications.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70039514","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1984, Geographic Names Information System, 2 p., https://doi.org/10.3133/70039514.","productDescription":"2 p.","numberOfPages":"2","costCenters":[{"id":409,"text":"National Cartographic Information Center","active":false,"usgs":true}],"links":[{"id":261642,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70039514/report.pdf"},{"id":261643,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70039514/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a1756e4b0c8380cd5548d","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":535337,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":80063,"text":"wri82508 - 1984 - Fluoride, Nitrate, and Dissolved-Solids Concentrations in Ground Waters of Washington","interactions":[],"lastModifiedDate":"2012-02-10T00:11:44","indexId":"wri82508","displayToPublicDate":"2007-06-28T00:00:00","publicationYear":"1984","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":"82-508","title":"Fluoride, Nitrate, and Dissolved-Solids Concentrations in Ground Waters of Washington","docAbstract":"This study provides basic data on ground-water quality throughout the State. It is intended for uses in planning and management by agencies and individuals who have responsibility for or interest in, public health and welfare. It also provides a basis for directing future studies of ground-water quality toward areas where ground-water quality problems may already exist. The information presented is a compilation of existing data from numerous sources including: the Washington Departments of Ecology and Social and Health Services, the Environmental Protection Agency, as well as many other local, county, state and federal agencies and private corporations. Only data on fluoride, nitrate, and dissolved-solids concentrations in ground water are presented, as these constituents are among those commonly used to determine the suitability of water for drinking or other purposes. They also reflect both natural and man-imposed effects on water quality and are the most readily available water-quality data for the State of Washington. The percentage of wells with fluoride, nitrate, or dissolved-solids concentrations exceeding U.S. Environmental Protection Agency Primary and Secondary Drinking Water Regulations were about 1, about 3, and about 3, respectively. Most high concentrations occurred in widely separated wells. Two exceptions were: high concentrations of nitrate and dissolved solids in wells on the Hanford Department of Energy Facility and high concentrations of nitrate in the lower Yakima River basin. (USGS)","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/wri82508","collaboration":"Prepared in cooperation with the State of Washington Department of Ecology","usgsCitation":"Lum, W.E., and Turney, G.L., 1984, Fluoride, Nitrate, and Dissolved-Solids Concentrations in Ground Waters of Washington (WRI/OFR 82-508): U.S. Geological Survey Water-Resources Investigations Report 82-508, 4 Sheets (3 maps and 1 data sheet; each sheet 21 x 27 inches), https://doi.org/10.3133/wri82508.","productDescription":"4 Sheets (3 maps and 1 data sheet; each sheet 21 x 27 inches)","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":194716,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":264344,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1982/0508/plate-1.pdf","size":"3794","linkFileType":{"id":1,"text":"pdf"}},{"id":264345,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1982/0508/plate-2.pdf","size":"3646","linkFileType":{"id":1,"text":"pdf"}},{"id":264346,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1982/0508/plate-3.pdf","size":"3745","linkFileType":{"id":1,"text":"pdf"}},{"id":264347,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1982/0508/plate-4.pdf","size":"3568","linkFileType":{"id":1,"text":"pdf"}}],"scale":"1000000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -125,45 ], [ -125,49 ], [ -116,49 ], [ -116,45 ], [ -125,45 ] ] ] } } ] }","edition":"WRI/OFR 82-508","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6aec01","contributors":{"authors":[{"text":"Lum, W. E. II","contributorId":81504,"corporation":false,"usgs":true,"family":"Lum","given":"W.","suffix":"II","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":291610,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Turney, Gary L.","contributorId":72446,"corporation":false,"usgs":true,"family":"Turney","given":"Gary","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":291609,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":80038,"text":"wri83698 - 1984 - Hydrology of Area 62, Northern Great Plains and Rocky Mountain Coal Provinces, New Mexico and Arizona","interactions":[],"lastModifiedDate":"2012-02-10T00:11:41","indexId":"wri83698","displayToPublicDate":"2007-06-20T00:00:00","publicationYear":"1984","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":"83-698","title":"Hydrology of Area 62, Northern Great Plains and Rocky Mountain Coal Provinces, New Mexico and Arizona","docAbstract":"This report summarizes available hydrologic data for Area 62 and will aid leasing decisions, and the preparation and appraisal of environmental impact studies and mine-permit applications. Area 62 is located at the southern end of the Rocky Mountain Coal Province in parts of New Mexico and Arizona and includes approximately 9,500 square miles. Surface mining alters, at least temporarily, the environment; if the areas are unreclaimed, there can be long-term environmental consequences.\r\n\r\nThe land-ownership pattern in Area 62 is complicated. The checkerboard pattern created by several types of ownership makes effective management of these lands difficult.\r\n\r\nThe climate generally is semiarid with average annual precipitation ranging from 10 to 20 inches. Pinons, junipers, and grasslands cover most of the area, and much of it is used for grazing by livestock. Soils vary with landscape, differing from flood plains and hillslopes to mountain slopes.\r\n\r\nThe major structural features of this area were largely developed during middle Tertiary time. The main structural features are the southern San Juan Basin and the Mogollon slope. Coal-bearing rocks are present in four Cretaceous rock units of the Mesaverde Group: the Gallup Sandstone, the Dileo Coal Member, and the Gibson Coal Member of the Crevasse Canyon Formation, and the Cleary Coal Member of the Menefee Formation.\r\n\r\nArea 62 is drained by Black Creek, the Puerco River, the Zuni River, Carrizo Wash-Largo Creek, and the Rio San Jose. Only at the headwaters of the Zuni River is the flow perennial. The streamflow-gaging station network consists of 25 stations operated for a variety of needs. Streamflow changes throughout the year with variation related directly to rainfall and snowmelt. Base flow in Area 62 is zero indicating no significant ground-water discharge. Mountainous areas contribute the highest mean annual runoff of 1.0 inch. Very few water-quality data are available for the surface-water stations. Of the nine surface-water stations that have water-quality data, only one has chemical analyses from more than 10 samples. Therefore, sufficient data to characterize the area in detail are not available. Suspended sediment data are available only for a few surface-\r\nwater stations in the area. Erosion rates generally are less than 1 acre-foot per square mile per year. Greater erosion rates are found within the badland areas.\r\n\r\nWater levels are periodically measured at 21 selected wells in Area 62. These observation wells are located mostly along the Rio San Jose and northeast of Gallup, New Mexico. The recharge to ground-water aquifers generally coincide with areas of greater precipitation in the mountainous areas. Depth to water below land surface is generally less than 200 feet. Well yields of 100 gallons per minute are common in most of the area.\r\n\r\nGround-water quality is variable both within each aquifer and between aquifers. Water quality generally is best near recharge areas.\r\n\r\nHistorical and current data related to stream discharge, water quality, and suspended sediment are available from computer files in the U.S. Geological Survey's National Water Data Storage and Retrieval System (WATSTORE) and through the National Water Data Exchange (NAWDEX).","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/wri83698","usgsCitation":"Roybal, F., Wells, J., Gold, R., and Flager, J., 1984, Hydrology of Area 62, Northern Great Plains and Rocky Mountain Coal Provinces, New Mexico and Arizona (WRI/OFR 83-698): U.S. Geological Survey Water-Resources Investigations Report 83-698, v, 66 p., https://doi.org/10.3133/wri83698.","productDescription":"v, 66 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":124643,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0698/report-thumb.jpg"},{"id":91373,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0698/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -110,34 ], [ -110,36 ], [ -107.5,36 ], [ -107.5,34 ], [ -110,34 ] ] ] } } ] }","edition":"WRI/OFR 83-698","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a17e4b07f02db604a3c","contributors":{"authors":[{"text":"Roybal, F.E.","contributorId":62998,"corporation":false,"usgs":true,"family":"Roybal","given":"F.E.","email":"","affiliations":[],"preferred":false,"id":291539,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wells, J.G.","contributorId":85198,"corporation":false,"usgs":true,"family":"Wells","given":"J.G.","email":"","affiliations":[],"preferred":false,"id":291541,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gold, R.L.","contributorId":97918,"corporation":false,"usgs":true,"family":"Gold","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":291542,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Flager, J.V.","contributorId":72799,"corporation":false,"usgs":true,"family":"Flager","given":"J.V.","email":"","affiliations":[],"preferred":false,"id":291540,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":77059,"text":"fwsobs82_10_73 - 1984 - Habitat Suitability Index Models: Gray partridge","interactions":[],"lastModifiedDate":"2022-02-09T15:12:21.326003","indexId":"fwsobs82_10_73","displayToPublicDate":"2006-07-19T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":20,"text":"FWS/OBS","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"82/10.73","subseriesTitle":"Habitat Suitability Index","title":"Habitat Suitability Index Models: Gray partridge","docAbstract":"This report is part of the Habitat Suitability Index model series which provides\r\nhabitat information useful for impact assessment and habitat management. The\r\nHabitat Use Information section is largely constrained to those data that can be\r\nused to derive quantitative relationships between key environmental variables\r\nand habitat suitability. The habitat use information provides the foundation for\r\nthe HSI model that follows. In addition, this same information may be useful in\r\nthe development of other models more appropriate to specific assessment or\r\nevaluation needs for the gray partridge (Perdix perdix).\r\n\r\nThe HSI model section documents a habitat model and information pertinent to its\r\napplication. The model synthesizes the habitat use information into a framework\r\nappropriate for field application and is scaled to produce an index value\r\nbetween 0.0 (unsuitable habitat) and 1.0 (optimum habitat).","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Allen, A.W., 1984, Habitat Suitability Index Models: Gray partridge: FWS/OBS 82/10.73, vi, 23 p.","productDescription":"vi, 23 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":190839,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db6498ad","contributors":{"authors":[{"text":"Allen, Arthur W.","contributorId":40648,"corporation":false,"usgs":true,"family":"Allen","given":"Arthur","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":288423,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":71002,"text":"wdrFL824 - 1984 - Water resources data, Florida, water year 1982, Volume 4: Northwest Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:13:46","indexId":"wdrFL824","displayToPublicDate":"2005-08-09T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"FL-82-4","title":"Water resources data, Florida, water year 1982, Volume 4: Northwest Florida","language":"ENGLISH","doi":"10.3133/wdrFL824","usgsCitation":"Geological Survey, U., 1984, Water resources data, Florida, water year 1982, Volume 4: Northwest Florida: U.S. Geological Survey Water Data Report FL-82-4, 310 p., https://doi.org/10.3133/wdrFL824.","productDescription":"310 p.","costCenters":[],"links":[{"id":185748,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1982/fl-82-4/report-thumb.jpg"},{"id":90530,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1982/fl-82-4/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f6e4b07f02db5f146d","contributors":{"authors":[{"text":"Geological Survey, U.S.","contributorId":26017,"corporation":false,"usgs":true,"family":"Geological Survey","given":"U.S.","affiliations":[],"preferred":false,"id":283473,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70138,"text":"wri844 - 1984 - Simulation of dynamic floodflows at gaged stations in the southeastern United States","interactions":[],"lastModifiedDate":"2012-02-02T00:13:52","indexId":"wri844","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"1984","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":"84-4","title":"Simulation of dynamic floodflows at gaged stations in the southeastern United States","language":"ENGLISH","doi":"10.3133/wri844","usgsCitation":"Faye, R.E., and Blalock, M.E., 1984, Simulation of dynamic floodflows at gaged stations in the southeastern United States: U.S. Geological Survey Water-Resources Investigations Report 84-4, 114 p., https://doi.org/10.3133/wri844.","productDescription":"114 p.","costCenters":[],"links":[{"id":101499,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/0004/report.pdf","size":"5716","linkFileType":{"id":1,"text":"pdf"}},{"id":191175,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/0004/report-thumb.jpg"}],"scale":"100000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f8e4b07f02db5f2efd","contributors":{"authors":[{"text":"Faye, Robert E.","contributorId":92221,"corporation":false,"usgs":true,"family":"Faye","given":"Robert","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":281931,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Blalock, Merritt E.","contributorId":14065,"corporation":false,"usgs":true,"family":"Blalock","given":"Merritt","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":281930,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70013138,"text":"70013138 - 1984 - Evaluation of the efficiency of streamflow data collection strategies for alluvial rivers","interactions":[],"lastModifiedDate":"2025-04-15T15:32:03.110121","indexId":"70013138","displayToPublicDate":"2003-04-23T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2342,"text":"Journal of Hydrology","active":true,"publicationSubtype":{"id":10}},"title":"Evaluation of the efficiency of streamflow data collection strategies for alluvial rivers","docAbstract":"<p><span>Streamflow discharge is usually determined indirectly from measurements of the river stage at gaging stations and through the use of stage-discharge relationships (rating curves). However, in alluvial streams, stage-discharge relationships change continually and, sometimes, quite markedly. Such changes may be caused by major floods, seasonal variations, or long-term secular trends associated with changes in the river channel. Consequently, reliable estimates of discharge using rating curves are not possible unless frequent direct measurements of discharge are made. Such measurements involve appreciable costs, and it is important to evaluate their contribution in increasing the accuracy of estimation of quantities of interest such as mean daily, monthly or annual flow. A methodology for the evaluation of the efficiency of data-collection strategies for alluvial rivers is developed and applied to stations on the Missouri River, U.S.A. A flexible and expedient model describing the variability of discharges and shifts in the stage-discharge relationship is developed. Procedures for the estimation of parameters and the validation of the model using actual data are presented. The calibrated and validated model is then employed in simulations to evaluate the effect of sampling strategies (such as frequency and accuracy of discharge measurements) on the accuracy of estimated mean daily, monthly and annual flow. Curves relating the cost of sampling to the achieved accuracy can be generated, and the optimization of sampling strategies given accuracy or budget objectives or constraints can be achieved.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0022-1694(84)90186-0","issn":"00221694","usgsCitation":"Kitanidis, P., Lara, O.G., and Lane, R., 1984, Evaluation of the efficiency of streamflow data collection strategies for alluvial rivers: Journal of Hydrology, v. 72, no. 1-2, p. 85-103, https://doi.org/10.1016/0022-1694(84)90186-0.","productDescription":"19 p.","startPage":"85","endPage":"103","costCenters":[],"links":[{"id":220409,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"72","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0ce2e4b0c8380cd52d2a","contributors":{"authors":[{"text":"Kitanidis, P.K.","contributorId":63274,"corporation":false,"usgs":true,"family":"Kitanidis","given":"P.K.","affiliations":[],"preferred":false,"id":365378,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lara, O. G.","contributorId":31001,"corporation":false,"usgs":true,"family":"Lara","given":"O.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":365377,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lane, R.W.","contributorId":86228,"corporation":false,"usgs":true,"family":"Lane","given":"R.W.","email":"","affiliations":[],"preferred":false,"id":365379,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70013169,"text":"70013169 - 1984 - Late quaternary sediments, minerals, and inferred geochemical history of Didwana Lake, Thar Desert, India","interactions":[],"lastModifiedDate":"2025-06-16T15:28:26.891809","indexId":"70013169","displayToPublicDate":"2003-04-22T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2996,"text":"Palaeogeography, Palaeoclimatology, Palaeoecology","printIssn":"0031-0182","active":true,"publicationSubtype":{"id":10}},"title":"Late quaternary sediments, minerals, and inferred geochemical history of Didwana Lake, Thar Desert, India","docAbstract":"<p>Variations in clastic sediment texture, mineralogy of both evaporites formed at the surface and precipitates formed below the lake floor, and the relative chemical activities of the major dissolved components of the chemical precipitates, have allowed reconstruction of the history of salinity and water-level changes in Didwana Lake, Thar Desert, India. Hypersaline conditions prevailed at about the Last Glacial Maximum, with little evidence of clastic sediments entering the lake. Between ca. 13,000 and 6000 B.P. the lake level fluctuated widely, the lake alternately hypersaline and fresh, and clastic sediments were delivered to the lake at a low rate. Deep-water conditions occurred ca. 6000 B.P. and clastic influx increased abruptly. The water level dropped towards 4000 B.P. when the lake dried briefly. Since 4000 B.P. the lake has been ephemeral with a lowered rate of sedimentation and mildly saline conditions rather like those of today. This sequence of changes documented in the lake parallels changes in vegetation recorded in published pollen diagrams from both the Thar and the Arabian Sea. Correlation of the various lines of evidence suggests that the climate of the Last Glacial Maximum at Didwana was dry and windy with a weak monsoon circulation. The monsoon was re-established between ca. 13,000 and a little before 6000 B.P., and, when winter rainfall increased ca. 6000 B.P., the lake filled to its maximum depth.&nbsp;</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0031-0182(84)90006-3","issn":"00310182","usgsCitation":"Wasson, R., Smith, G., and Agrawal, D., 1984, Late quaternary sediments, minerals, and inferred geochemical history of Didwana Lake, Thar Desert, India: Palaeogeography, Palaeoclimatology, Palaeoecology, v. 46, no. 4, p. 345-372, https://doi.org/10.1016/0031-0182(84)90006-3.","productDescription":"28 p.","startPage":"345","endPage":"372","costCenters":[],"links":[{"id":220293,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"India","otherGeospatial":"Didwana Lake, Thar Deser","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              74.20830973397764,\n              27.538838395300488\n            ],\n            [\n              74.20830973397764,\n              27.201083582211524\n            ],\n            [\n              74.785913156556,\n              27.201083582211524\n            ],\n            [\n              74.785913156556,\n              27.538838395300488\n            ],\n            [\n              74.20830973397764,\n              27.538838395300488\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"46","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a4558e4b0c8380cd67238","contributors":{"authors":[{"text":"Wasson, R.J.","contributorId":34780,"corporation":false,"usgs":true,"family":"Wasson","given":"R.J.","email":"","affiliations":[],"preferred":false,"id":365458,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smith, G.I.","contributorId":103694,"corporation":false,"usgs":true,"family":"Smith","given":"G.I.","email":"","affiliations":[],"preferred":false,"id":365459,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Agrawal, D.P.","contributorId":16712,"corporation":false,"usgs":true,"family":"Agrawal","given":"D.P.","email":"","affiliations":[],"preferred":false,"id":365457,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70013909,"text":"70013909 - 1984 - An overview of paleogene molluscan biostratigraphy and paleoecology of the Gulf of Alaska region","interactions":[],"lastModifiedDate":"2025-06-16T15:15:08.632102","indexId":"70013909","displayToPublicDate":"2003-04-22T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2996,"text":"Palaeogeography, Palaeoclimatology, Palaeoecology","printIssn":"0031-0182","active":true,"publicationSubtype":{"id":10}},"title":"An overview of paleogene molluscan biostratigraphy and paleoecology of the Gulf of Alaska region","docAbstract":"<p><span>Paleogene marine strata in the Gulf of Alaska region occur in three geographic areas and may be characterized by their molluscan faunal composition and paleoecology: a western area consisting of the Alaska Peninsula, Kodiak Island, and adjacent islands; a central area encompassing Prince William Sound; and an eastern area extending from the mouth of the Copper River to Icy Point in the Lituya district. Strata in the western area include the Ghost Rocks, Narrow Cape (in part), Sitkalidak, Stepovak, Belkofski, and Tolstoi Formations; in the central area Paleogene strata are assigned entirely to the Orca Group; Paleogene strata in the eastern area include the Kulthieth and Poul Creek Formations and several coeval units. Environments ranging from marginal marine to bathyal and from subtropical to cool-temperate are inferred for the various molluscan faunas. Sediments range from interbedded coal and marine sands to deep-water turbidites. The known Paleogene molluscan faunas of these three southern Alaskan areas permit recognition of biostratigraphic schemes within each area, preliminary correlations between faunas of the three areas, and more general correlations with faunas of the Pacific Northwest, the Far Eastern U.S.S.R., and northern Japan.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0031-0182(84)90082-8","issn":"00310182","usgsCitation":"Marincovich, L., and McCoy, S., 1984, An overview of paleogene molluscan biostratigraphy and paleoecology of the Gulf of Alaska region: Palaeogeography, Palaeoclimatology, Palaeoecology, v. 47, no. 1-2, p. 91-102, https://doi.org/10.1016/0031-0182(84)90082-8.","productDescription":"12 p.","startPage":"91","endPage":"102","costCenters":[],"links":[{"id":226118,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.er.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Gulf of Alaska","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -170.16016898665896,\n              52.53370257192515\n            ],\n            [\n              -165.87722752127797,\n              53.011068953297425\n            ],\n            [\n              -150.56744496884684,\n              57.07373444976588\n            ],\n            [\n              -152.06112809170114,\n              58.543491125197704\n            ],\n            [\n              -157.20426229979498,\n              58.73570361951738\n            ],\n            [\n              -170.08830120094672,\n              53.82391633092445\n            ],\n            [\n              -170.16016898665896,\n              52.53370257192515\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"47","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059eaace4b0c8380cd489e4","contributors":{"authors":[{"text":"Marincovich, L. Jr.","contributorId":16157,"corporation":false,"usgs":true,"family":"Marincovich","given":"L.","suffix":"Jr.","affiliations":[],"preferred":false,"id":367145,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McCoy, S. Jr.","contributorId":75287,"corporation":false,"usgs":true,"family":"McCoy","given":"S.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":367146,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70014083,"text":"70014083 - 1984 - Age and correlation of emerged pliocene and pleistocene deposits, U.S. Atlantic Coastal Plain","interactions":[],"lastModifiedDate":"2025-06-16T15:01:27.053261","indexId":"70014083","displayToPublicDate":"2003-04-22T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2996,"text":"Palaeogeography, Palaeoclimatology, Palaeoecology","printIssn":"0031-0182","active":true,"publicationSubtype":{"id":10}},"title":"Age and correlation of emerged pliocene and pleistocene deposits, U.S. Atlantic Coastal Plain","docAbstract":"<p><span>Paleontologic and paleomagnetic investigations were conducted on several hundred Pliocene and Pleistocene marine samples from five regions of the emerged Atlantic Coastal Plain: (1) the Delmarva Peninsula, (2) eastern Virginia, (3) central and northern North Carolina, (4) southern North Carolina and northeastern South Carolina, and (5) the Charleston area, South Carolina. Molluscan and ostracode interval and assemblage zonations, which are the primary means of regional correlation, have been calibrated using planktic biochronologic, paleomagnetic, radiometric and amino-acid recemization data. These multiple dating criteria were used to determine the age and, where possible, the duration of marine transgressive/regressive sequences. A correlation chart illustrates the age relationships of 27 formations from five regions. One important conclusion is some of the Yorktown Formation of Virginia and North Carolina (including the “Duplin” Formation), and some of the Raysor of South Carolina are late Pliocene in age. The late Pliocene Chowan River Formation of North Carolina is older than the early Pleistocene Waccamaw Formation of South Carolina, which in turn may be older than the James City Formation of North Carolina. During the last 1.0 million years, multiple marine transgressions occurred in each region, but the age of these middle and late Pleistocene formations often may differ from one area to the next.</span></p><p><span>A significant result of the study is the evidence for the lack of time equivalence of formations in the five different regions; that is, the sequence of marine transgressions in one region does not necessarily correspond to that in another. This appears to be the result of differing subsidence and uplift histories, the patchiness of the depositional record, and the limitations of the dating techniques in light of the rapidity and frequency of sea-level fluctuations.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0031-0182(84)90079-8","usgsCitation":"Cronin, T.M., Bybell, L., Poore, R., Blackwelder, B.W., Liddicoat, J.C., and Hazel, J.E., 1984, Age and correlation of emerged pliocene and pleistocene deposits, U.S. Atlantic Coastal Plain: Palaeogeography, Palaeoclimatology, Palaeoecology, v. 47, no. 1-2, p. 21-51, https://doi.org/10.1016/0031-0182(84)90079-8.","productDescription":"31 p.","startPage":"21","endPage":"51","costCenters":[],"links":[{"id":225812,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Delaware, Maryland, North Carolina, South Carolina, Virginia","otherGeospatial":"Atlantic Coastal Plain","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -75.234375,\n              39.13006024213511\n            ],\n            [\n              -75.65185546874999,\n              39.690280594818034\n            ],\n            [\n              -78.06884765624999,\n              39.53793974517628\n            ],\n            [\n              -81.6943359375,\n              33.394759218577995\n            ],\n            [\n              -81.36474609375,\n              32.58384932565662\n            ],\n            [\n              -80.74951171875,\n              32.045332838858506\n            ],\n            [\n              -76.97021484375,\n              34.32529192442733\n            ],\n            [\n              -75.56396484375,\n              35.746512259918504\n            ],\n            [\n              -75.60791015625,\n              37.28279464911045\n            ],\n            [\n              -74.970703125,\n              38.41055825094609\n            ],\n            [\n              -75.234375,\n              39.13006024213511\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"47","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e8d7e4b0c8380cd47eeb","contributors":{"authors":[{"text":"Cronin, T. M. 0000-0002-2643-0979","orcid":"https://orcid.org/0000-0002-2643-0979","contributorId":42613,"corporation":false,"usgs":true,"family":"Cronin","given":"T.","email":"","middleInitial":"M.","affiliations":[{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true}],"preferred":false,"id":367529,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bybell, L.M. 0000-0002-4760-7542","orcid":"https://orcid.org/0000-0002-4760-7542","contributorId":11220,"corporation":false,"usgs":true,"family":"Bybell","given":"L.M.","affiliations":[],"preferred":false,"id":367527,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Poore, R.Z.","contributorId":35314,"corporation":false,"usgs":true,"family":"Poore","given":"R.Z.","email":"","affiliations":[],"preferred":false,"id":367528,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Blackwelder, B. W.","contributorId":104136,"corporation":false,"usgs":true,"family":"Blackwelder","given":"B.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":367532,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Liddicoat, J. C.","contributorId":76781,"corporation":false,"usgs":false,"family":"Liddicoat","given":"J.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":367530,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Hazel, J. E.","contributorId":89187,"corporation":false,"usgs":false,"family":"Hazel","given":"J.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":367531,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70014066,"text":"70014066 - 1984 - Distribution and ecology of deep-water benthic foraminifera in the Gulf of Mexico","interactions":[],"lastModifiedDate":"2025-06-16T15:08:16.465443","indexId":"70014066","displayToPublicDate":"2003-04-14T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2996,"text":"Palaeogeography, Palaeoclimatology, Palaeoecology","printIssn":"0031-0182","active":true,"publicationSubtype":{"id":10}},"title":"Distribution and ecology of deep-water benthic foraminifera in the Gulf of Mexico","docAbstract":"<p><span>Bathyal and abyssal foraminifera in the Gulf of Mexico are distributed among thirteen generic predominance facies. Five predominance facies nearly encircle the Gulf basin along the slope and rise; a sixth predominance facies blankets the Sigsbee Plain, and a seventh is restricted to the Mississippi Fan. The remaining eight predominance facies have more restricted distributions. The areal patterns of these predominance facies can be related chiefly to water mass and substrate characteristics; modifications are brought about by calcite dissolution, upwelling, and sill depth. Analysis of ancient generic predominance facies is useful in predicting relative paleobathymetry and other paleoenvironmental properties.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0031-0182(84)90090-7","issn":"00310182","usgsCitation":"Poag, C.W., 1984, Distribution and ecology of deep-water benthic foraminifera in the Gulf of Mexico: Palaeogeography, Palaeoclimatology, Palaeoecology, v. 48, no. 1, p. 25-37, https://doi.org/10.1016/0031-0182(84)90090-7.","productDescription":"13 p.","startPage":"25","endPage":"37","costCenters":[],"links":[{"id":225487,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alabama, Florida, Louisiana, Mississippi, Texas","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -97.13858134169811,\n              29.197248880700073\n            ],\n            [\n              -97.13858134169811,\n              21.67225015871294\n            ],\n            [\n              -83.08875993352926,\n              21.67225015871294\n            ],\n            [\n              -83.08875993352926,\n              29.197248880700073\n            ],\n            [\n              -97.13858134169811,\n              29.197248880700073\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"48","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a028ae4b0c8380cd500bc","contributors":{"authors":[{"text":"Poag, C. W.","contributorId":16402,"corporation":false,"usgs":true,"family":"Poag","given":"C.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":367485,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70014084,"text":"70014084 - 1984 - Neogene stratigraphy of the submerged U.S. Atlantic margin","interactions":[],"lastModifiedDate":"2025-06-13T16:12:42.564623","indexId":"70014084","displayToPublicDate":"2003-04-14T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2996,"text":"Palaeogeography, Palaeoclimatology, Palaeoecology","printIssn":"0031-0182","active":true,"publicationSubtype":{"id":10}},"title":"Neogene stratigraphy of the submerged U.S. Atlantic margin","docAbstract":"<p><span>Thirty boreholes and several hundred sea-floor samples provide a detailed but incomplete record of Neogene strata and depositional environments along the submerged part of the United States Atlantic margin. Three major sedimentary basins, the Blake Plateau Basin, the Baltimore Canyon Trough, and the Georges Bank Basin, contain Neogene sedimentary prisms as thick as 1200 m, comprising bathyal marine to nonmarine strata. Middle Miocene rocks compose the most widely represented and thickest unit (&gt; 600 m in the Baltimore Canyon Trough). Calcareous microfossils provide excellent biostratigraphic and paleoenvironmental indicators except in some sparsely fossilferous shallow-water intervals and where shallow-water diatomaceous assemblages predominate. However, in outer sublittoral assemblages of the Blake Plateau Basin and Baltimore Canyon Trough, the co-occurrence of abundant diatoms, radiolarians, and planktic foraminifera provide an excellent opportunity for intercalibration of biozones. Preliminary correlations between chronostratigraphic and paleoenvironmental interpretations indicate a close association of depositional sequences with sea-level fluctuations, but some local exception persist.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0031-0182(84)90083-X","issn":"00310182","usgsCitation":"Poag, C.W., 1984, Neogene stratigraphy of the submerged U.S. Atlantic margin: Palaeogeography, Palaeoclimatology, Palaeoecology, v. 47, no. 1-2, p. 103-127, https://doi.org/10.1016/0031-0182(84)90083-X.","productDescription":"25 p.","startPage":"103","endPage":"127","costCenters":[],"links":[{"id":225813,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","otherGeospatial":"U.S. Atlantic margin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -67.21473626467579,\n              45.56400160658059\n            ],\n            [\n              -75.89249608207597,\n              40.57001008222211\n            ],\n            [\n              -81.63246101855188,\n              32.43539505606307\n            ],\n            [\n              -82.04072839900807,\n              30.364306803599554\n            ],\n            [\n              -80.52464146673184,\n              25.886508698926903\n            ],\n            [\n              -77.03753292314397,\n              27.57808131902972\n            ],\n            [\n              -65.43896538425625,\n              43.37717206733501\n            ],\n            [\n              -67.21473626467579,\n              45.56400160658059\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"47","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a6450e4b0c8380cd72983","contributors":{"authors":[{"text":"Poag, C. Wylie","contributorId":52714,"corporation":false,"usgs":true,"family":"Poag","given":"C.","email":"","middleInitial":"Wylie","affiliations":[],"preferred":false,"id":367533,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70013319,"text":"70013319 - 1984 - Neogene molluscan stages of the West Coast of North America","interactions":[],"lastModifiedDate":"2025-06-16T15:21:26.470744","indexId":"70013319","displayToPublicDate":"2003-04-14T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2996,"text":"Palaeogeography, Palaeoclimatology, Palaeoecology","printIssn":"0031-0182","active":true,"publicationSubtype":{"id":10}},"title":"Neogene molluscan stages of the West Coast of North America","docAbstract":"<p><span>Neogene marine sediments of the West Coast of North America were deposited in a series of widely spaced basins that extended geographically from the western and northern Gulf of Alaska (60°N) to southern California (33°N). Rich molluscan faunas occur extensively throughout these deposits and form the basis for biostratigraphic schemes that are useful for correlating within and between individual basins. Early biostratigraphic work was concerned with faunas from particular horizons and with the stratigraphic range of diverse taxa, such as&nbsp;</span><i>Pecten</i><span>&nbsp;and&nbsp;</span><i>Turritella</i><span>, without reference to other fossil groups. Succeeding work increasingly dealt with the relationships of molluscan zones to benthic and, later, planktonic foraminiferal stages. In recent years the age limits of Neogene molluscan stages have become better documented by reference to planktonic microfossils from dated DSDP cores and onshore faunas.</span></p><p><span>Neogene molluscan faunas from California, the Pacific Northwest states (Oregon and Washington), and southern Alaska have been treated separately due to differences in faunal composition and geographic isolation. As a result, a different biostratigraphic sequence has been described for each region. Pacific Northwest stages have been formally named and defined, and their names are also used informally for Alaskan faunas. California Neogene stages were proposed early in this century, are in need of redescription, and their usage is informal. Precise correlations between the three regional sequences have not yet been achieved, due to the low number of co-occurring species and the general lack of planktonic microfossils in these largely shallow-water faunas. The objectives of ongoing research include: fuller documentation of the faunas of California and Pacific Northwest stages; formal description of California stages; improved correlation between regional stage sequences; refinement of age estimates for stage boundaries; and, establishment of Neogene stages for Alaskan faunas.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0031-0182(84)90022-1","issn":"00310182","usgsCitation":"Marincovich, L., 1984, Neogene molluscan stages of the West Coast of North America: Palaeogeography, Palaeoclimatology, Palaeoecology, v. 46, no. 1-3, p. 11-24, https://doi.org/10.1016/0031-0182(84)90022-1.","productDescription":"14 p.","startPage":"11","endPage":"24","costCenters":[],"links":[{"id":220528,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Canada, United States","state":"California, Oregon, Washington","otherGeospatial":"British Columbia","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -140.62983472920033,\n              60.58400932046334\n            ],\n            [\n              -121.64960121391485,\n              33.52522907665377\n            ],\n            [\n              -118.0675797095897,\n              32.45484505685331\n            ],\n            [\n              -114.11428012825937,\n              32.82730499941407\n            ],\n            [\n              -114.5983833681297,\n              35.57473668760612\n            ],\n            [\n              -119.49611318026915,\n              39.15156796516043\n            ],\n            [\n              -119.80273808795062,\n              41.88223308573585\n            ],\n            [\n              -117.17898657848735,\n              42.25894561686526\n            ],\n            [\n              -116.61248280646399,\n              46.341056999454025\n            ],\n            [\n              -116.64659824810718,\n              48.677806603546586\n            ],\n            [\n              -114.77408096538828,\n              49.81429632925091\n            ],\n            [\n              -120.81774730494959,\n              60.19576593940528\n            ],\n            [\n              -140.62983472920033,\n              60.58400932046334\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"46","issue":"1-3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a644ce4b0c8380cd72978","contributors":{"authors":[{"text":"Marincovich, L. Jr.","contributorId":16157,"corporation":false,"usgs":true,"family":"Marincovich","given":"L.","suffix":"Jr.","affiliations":[],"preferred":false,"id":365809,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70013270,"text":"70013270 - 1984 - Unzipping of the volcano arc, Japan","interactions":[],"lastModifiedDate":"2025-08-28T13:19:05.525932","indexId":"70013270","displayToPublicDate":"2003-04-11T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3525,"text":"Tectonophysics","active":true,"publicationSubtype":{"id":10}},"title":"Unzipping of the volcano arc, Japan","docAbstract":"<div class=\"u-margin-s-bottom\">A working hypothesis for the recent evolution of the southern Volcano Arc, Japan, is presented which calls upon a northward-progressing sundering of the arc in response to a northward-propagating back-arc basin extensional regime. This model appears to explain several localized and recent changes in the tectonic and magrnatic evolution of the Volcano Arc. Most important among these changes is the unusual composition of Iwo Jima volcanic rocks. This contrasts with normal arc tholeiites typical of the rest of the Izu-Volcano-Mariana and other primitive arcs in having alkaline tendencies, high concentrations of light REE and other incompatible elements, and relatively high silica contents. In spite of such fractionated characteristics, these lavas appear to be very early manifestations of a new volcanic and tectonic cycle in the southern Volcano Arc. These alkaline characteristics and indications of strong regional uplift are consistent with the recent development of an early stage of inter-arc basin rifting in the southern Volcano Arc.</div><div class=\"u-margin-s-bottom\">New bathymetric data are presented in support of this model which indicate:<ul class=\"list\"><li class=\"react-xocs-list-item\"><span class=\"list-label\">1. (1) </span>structural elements of the Mariana Trough extend north to the southern Volcano Arc.</li><li class=\"react-xocs-list-item\"><span class=\"list-label\">2. (2) </span>both the Mariana Trough and frontal arc shoal rapidly northwards as the Volcano Arc is approached.</li><li class=\"react-xocs-list-item\"><span class=\"list-label\">3. (3) </span>rugged bathymetry associated with the rifted Mariana Trough is replaced just south of Iwo Jima by the development of a huge dome (50–75 km diameter) centered around Iwo Jima. Such uplifted domes are the immediate precursors of rifts in other environments, and it appears that a similar situation may now exist in the southern Volcano Arc.</li></ul></div><div class=\"u-margin-s-bottom\">The present distribution of unrifted Volcano Arc to the north and rifted Mariana Arc to the south is interpreted not as a stable tectonic configuration but as representing a tectonic “snapshot” of an arc in the process of being rifted to form a back-arc basin.</div>","language":"English","publisher":"Elsevier","doi":"10.1016/0040-1951(84)90012-X","issn":"00401951","usgsCitation":"Stern, R.J., Smoot, N.C., and Rubin, M., 1984, Unzipping of the volcano arc, Japan: Tectonophysics, v. 102, no. 1-4, p. 153-174, https://doi.org/10.1016/0040-1951(84)90012-X.","productDescription":"22 p.","startPage":"153","endPage":"174","costCenters":[],"links":[{"id":219845,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Japan","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              141.05378887856648,\n              45.99119377997198\n            ],\n            [\n              138.87881300800817,\n              42.76240361420229\n            ],\n            [\n              138.46187782493524,\n              38.795079496052594\n            ],\n            [\n              131.7792147896455,\n              35.75113762652983\n            ],\n            [\n              128.23943351263787,\n              32.78029353589463\n            ],\n            [\n              129.36478812505305,\n              30.616790006554524\n            ],\n            [\n              141.1030822507787,\n              33.24501689658564\n            ],\n            [\n              143.3813057330311,\n              41.098586091306174\n            ],\n            [\n              146.51973120457893,\n              43.942841141119516\n            ],\n            [\n              141.05378887856648,\n              45.99119377997198\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"102","issue":"1-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bbd0be4b08c986b328ea1","contributors":{"authors":[{"text":"Stern, R. J.","contributorId":8616,"corporation":false,"usgs":true,"family":"Stern","given":"R.","middleInitial":"J.","affiliations":[],"preferred":false,"id":365689,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smoot, N. C.","contributorId":54731,"corporation":false,"usgs":true,"family":"Smoot","given":"N.","middleInitial":"C.","affiliations":[],"preferred":false,"id":365690,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rubin, M.","contributorId":88079,"corporation":false,"usgs":true,"family":"Rubin","given":"M.","email":"","affiliations":[],"preferred":false,"id":365691,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
]}