{"pageNumber":"4593","pageRowStart":"114800","pageSize":"25","recordCount":165619,"records":[{"id":36536,"text":"fwsobs82_10_72 - 1984 - Habitat Suitability Index Models and Instream Flow Suitability Curves: Spotted bass","interactions":[],"lastModifiedDate":"2016-09-16T11:08:00","indexId":"fwsobs82_10_72","displayToPublicDate":"1994-01-01T00:00:00","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":"82/10.72","subseriesTitle":"Habitat Suitability Index","title":"Habitat Suitability Index Models and Instream Flow Suitability Curves: Spotted bass","docAbstract":"The Habitat Suitability Index (HSI) models presented in this publication aid in identifying habitat variable important to the growth and survival of spotted bass (Micropterus punctulatus). Facts, ideas, and concepts obtained from the research literature and expert reviews are synthesized and presented in a format that can be used for impact assessment. The models are hypotheses of species-habitat relationships, and model users should recognize that the degree of veracity of the HSI model, SI graphs, and assumptions will vary according to geographical area and the extent of the data base for individual variables.\r\n\r\nA brief discussion of selected Suitability Index (SI) curves as used in the Instream Flow Incremental Methodology (IFIM), and a discussion of SI curves available for the IFIM analysis of Spotted bass habitat are also included.","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"McMahon, T., Gebhart, G., Maughan, O.E., and Nelson, P.C., 1984, Habitat Suitability Index Models and Instream Flow Suitability Curves: Spotted bass: FWS/OBS 82/10.72, vi, 41 p.","productDescription":"vi, 41 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":166089,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":8299,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://archive.usgs.gov/archive/sites/www.nwrc.usgs.gov/wdb/pub/hsi/hsi-072.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a71e4b07f02db641e55","contributors":{"authors":[{"text":"McMahon, Thomas E.","contributorId":93548,"corporation":false,"usgs":true,"family":"McMahon","given":"Thomas E.","affiliations":[],"preferred":false,"id":216493,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gebhart, Glen","contributorId":52237,"corporation":false,"usgs":true,"family":"Gebhart","given":"Glen","email":"","affiliations":[],"preferred":false,"id":216491,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Maughan, O. Eugene","contributorId":43006,"corporation":false,"usgs":true,"family":"Maughan","given":"O.","email":"","middleInitial":"Eugene","affiliations":[],"preferred":false,"id":216490,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Nelson, Patrick C.","contributorId":68799,"corporation":false,"usgs":true,"family":"Nelson","given":"Patrick","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":216492,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":36440,"text":"fwsobs84_10 - 1984 - Endangered and threatened species on U.S Air Force installations","interactions":[],"lastModifiedDate":"2012-02-02T00:09:36","indexId":"fwsobs84_10","displayToPublicDate":"1994-01-01T00:00:00","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":"84/10","title":"Endangered and threatened species on U.S Air Force installations","language":"ENGLISH","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Howard, R., Perry, A., and Herring, P., 1984, Endangered and threatened species on U.S Air Force installations: FWS/OBS 84/10, 1 v. (loose-leaf) : 1 map; 28 cm.","productDescription":"1 v. (loose-leaf) : 1 map; 28 cm.","costCenters":[],"links":[{"id":166321,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a18e4b07f02db60507f","contributors":{"authors":[{"text":"Howard, R.","contributorId":59298,"corporation":false,"usgs":true,"family":"Howard","given":"R.","email":"","affiliations":[],"preferred":false,"id":216327,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Perry, A.","contributorId":107149,"corporation":false,"usgs":true,"family":"Perry","given":"A.","email":"","affiliations":[],"preferred":false,"id":216328,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Herring, P.","contributorId":50047,"corporation":false,"usgs":true,"family":"Herring","given":"P.","email":"","affiliations":[],"preferred":false,"id":216326,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":36537,"text":"fwsobs82_10_74 - 1984 - Habitat Suitability Index Models: Larval and juvenile red drum","interactions":[],"lastModifiedDate":"2022-02-09T15:21:08.728846","indexId":"fwsobs82_10_74","displayToPublicDate":"1994-01-01T00:00:00","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":"82/10.74","subseriesTitle":"Habitat Suitability Index","title":"Habitat Suitability Index Models: Larval and juvenile red drum","docAbstract":"A review and synthesis of existing information were used to develop a habitat model for larval and juvenile red drum. The model is scaled to produce an index of habitat suitability between 0 (unsuitable habitat) and 1 (optimally suitable habitat) for estuarine areas along the Gulf of Mexico and Atlantic coasts. Habitat suitability indices are designed for use with habitat evaluation procedures developed by the U.S. Fish and Wildlife Service. Guidelines for model application and techniques for estimating model variables are provided.","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Buckley, J., 1984, Habitat Suitability Index Models: Larval and juvenile red drum: FWS/OBS 82/10.74, vi, 15 p.","productDescription":"vi, 15 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":166202,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db64987a","contributors":{"authors":[{"text":"Buckley, Jack","contributorId":86402,"corporation":false,"usgs":true,"family":"Buckley","given":"Jack","email":"","affiliations":[],"preferred":false,"id":216494,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":37156,"text":"rp154 - 1984 - Nonconsumptive use of wildlife in the United States","interactions":[],"lastModifiedDate":"2016-11-16T13:41:02","indexId":"rp154","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":79,"text":"Resource Publication","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"154","title":"Nonconsumptive use of wildlife in the United States","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Fish and Wildlife Service","publisherLocation":"Washington, D.C.","usgsCitation":"Shaw, W.W., and Mangun, W.R., 1984, Nonconsumptive use of wildlife in the United States: Resource Publication 154, 20 p.","productDescription":"20 p.","costCenters":[],"links":[{"id":162724,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db69709f","contributors":{"authors":[{"text":"Shaw, William W.","contributorId":102121,"corporation":false,"usgs":true,"family":"Shaw","given":"William","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":217584,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mangun, William R.","contributorId":100440,"corporation":false,"usgs":true,"family":"Mangun","given":"William","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":217583,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":38477,"text":"pp1400B - 1984 - Geohydrology of the High Plains Aquifer in parts of Colorado, Kansas, Nebraska, New Mexico, Oklahoma, South Dakota, Texas, and Wyoming","interactions":[],"lastModifiedDate":"2017-09-20T16:55:52","indexId":"pp1400B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1400","chapter":"B","title":"Geohydrology of the High Plains Aquifer in parts of Colorado, Kansas, Nebraska, New Mexico, Oklahoma, South Dakota, Texas, and Wyoming","language":"ENGLISH","doi":"10.3133/pp1400B","usgsCitation":"Gutentag, E., Heimes, F., Krothe, N., Luckey, R.R., and Weeks, J., 1984, Geohydrology of the High Plains Aquifer in parts of Colorado, Kansas, Nebraska, New Mexico, Oklahoma, South Dakota, Texas, and Wyoming: U.S. Geological Survey Professional Paper 1400, 63 p., https://doi.org/10.3133/pp1400B.","productDescription":"63 p.","costCenters":[{"id":5050,"text":"WY-MT Water Science Center","active":true,"usgs":true}],"links":[{"id":122157,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1400b/report-thumb.jpg"},{"id":65116,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1400b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8974","contributors":{"authors":[{"text":"Gutentag, E. D.","contributorId":70015,"corporation":false,"usgs":true,"family":"Gutentag","given":"E. D.","affiliations":[],"preferred":false,"id":219898,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Heimes, F.J.","contributorId":60654,"corporation":false,"usgs":true,"family":"Heimes","given":"F.J.","affiliations":[],"preferred":false,"id":219896,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Krothe, N.C.","contributorId":76378,"corporation":false,"usgs":true,"family":"Krothe","given":"N.C.","affiliations":[],"preferred":false,"id":219899,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Luckey, R. R.","contributorId":93055,"corporation":false,"usgs":true,"family":"Luckey","given":"R.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":219900,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Weeks, J.B.","contributorId":61426,"corporation":false,"usgs":true,"family":"Weeks","given":"J.B.","email":"","affiliations":[],"preferred":false,"id":219897,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":39846,"text":"b1612 - 1984 - Geochemical features and 40Ar/39Ar age of tholeiitic and mafic-alkalic dikes in Aroostook County, northeastern Maine","interactions":[],"lastModifiedDate":"2012-02-02T00:10:16","indexId":"b1612","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1612","title":"Geochemical features and 40Ar/39Ar age of tholeiitic and mafic-alkalic dikes in Aroostook County, northeastern Maine","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/b1612","usgsCitation":"Gottfried, D., Macdonald, R., Sutter, J., and Pavlides, L., 1984, Geochemical features and 40Ar/39Ar age of tholeiitic and mafic-alkalic dikes in Aroostook County, northeastern Maine: U.S. Geological Survey Bulletin 1612, iii, 23 p. :ill., maps ;28 cm., https://doi.org/10.3133/b1612.","productDescription":"iii, 23 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":170548,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1612/report-thumb.jpg"},{"id":67714,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1612/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae277","contributors":{"authors":[{"text":"Gottfried, David","contributorId":82295,"corporation":false,"usgs":true,"family":"Gottfried","given":"David","email":"","affiliations":[],"preferred":false,"id":222399,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Macdonald, Raymond","contributorId":36614,"corporation":false,"usgs":true,"family":"Macdonald","given":"Raymond","email":"","affiliations":[],"preferred":false,"id":222397,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sutter, J.R.","contributorId":15261,"corporation":false,"usgs":true,"family":"Sutter","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":222396,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Pavlides, Louis","contributorId":79444,"corporation":false,"usgs":true,"family":"Pavlides","given":"Louis","email":"","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":222398,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":38537,"text":"pp1322 - 1984 - Early and middle Bajocian (Middle Jurassic) ammonites from southern Alaska","interactions":[],"lastModifiedDate":"2022-08-30T19:43:22.584779","indexId":"pp1322","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1322","title":"Early and middle Bajocian (Middle Jurassic) ammonites from southern Alaska","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp1322","usgsCitation":"Imlay, R.W., 1984, Early and middle Bajocian (Middle Jurassic) ammonites from southern Alaska: U.S. Geological Survey Professional Paper 1322, iv, 38 p., https://doi.org/10.3133/pp1322.","productDescription":"iv, 38 p.","costCenters":[],"links":[{"id":405940,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_74246.htm","linkFileType":{"id":5,"text":"html"}},{"id":65303,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1322/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":122277,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1322/report-thumb.jpg"}],"country":"United States","state":"Alaska","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -156.65,\n              57.2333\n            ],\n            [\n              -142.55,\n              57.2333\n            ],\n            [\n              -142.55,\n              62.1667\n            ],\n            [\n              -156.65,\n              62.1667\n            ],\n            [\n              -156.65,\n              57.2333\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a54e4b07f02db62c2b4","contributors":{"authors":[{"text":"Imlay, R. W.","contributorId":23118,"corporation":false,"usgs":true,"family":"Imlay","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":220021,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":38634,"text":"pp1066I - 1984 - Trepostome and cystoporate bryozoans from the Lexington Limestone and the Clays Ferry Formation (Middle and Upper Ordovician) of Kentucky","interactions":[],"lastModifiedDate":"2012-02-02T00:10:35","indexId":"pp1066I","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1066","chapter":"I","title":"Trepostome and cystoporate bryozoans from the Lexington Limestone and the Clays Ferry Formation (Middle and Upper Ordovician) of Kentucky","docAbstract":"The Lexington Limestone and the Clays Ferry Formation of Kentucky contain an abundant and diversified fossil invertebrate fauna. This report is concerned with the trepostome and cystoporate bryozoans that constitute a major part of that fauna. The Lexington Limestone, largely a biofragmental fossiliferous limestone, rests disconformably on the Tyrone Limestone (Middle Ordovician). The Clays Ferry Formation consists of approximately equal amounts of biofragmentallimestone and shale, and it overlies conformably, or intertongues with, the upper part of the Lexington Limestone. The Clays Ferry Formation is overlain by the Garrard Siltstone (Upper Ordovician) in central Kentucky and intertongues with the Kope Formation (Upper Ordovician) in northern Kentucky. The MiddleUpper Ordovician boundary falls within the upper part of the Lexington Limestone and laterally equivalent strata of the Clays Ferry Formation. \r\n\r\nThe Lexington Limestone has been divided into 12 members, consisting of calcarenites, calcisiltites, calcilutites, nodular limestones, and shales in various amounts, that intertongue complexly. Because of the great abundance of bryozoans this study is generally limited to bryozoans recovered from, in ascending order, the Grier Limestone Member, the Perryville Limestone Member, the Brannon Member, the Tanglewood Limestone Member, and the Millersburg Member of the Lexington Limestone and from the Clays Ferry Formation and its Point Pleasant Tongue. \r\n\r\nThe trepostome and cystoporate bryozoans discussed are referred to 36 species belonging to 22 genera. The trepostome component includes 29 species belonging to 16 genera: Amplexopora, Atactoporella, Balticopora, Batostoma, Cyphotrypa, Dekayia, Eridotrypa, Hetero-_ trypa, Homotrypa, Homotrypella, Mesotrypa, Parvohallopora, Peronopora, Prasopora, Stigmatella, and Tarphophragma, a new genus. Five of the trepostome species are new: Balticopora arcuatilis, Cyphotrypa switzeriensis, Dekayia epetrima, Eridotrypa sadievillensis, and Homotrypa cressmani. The cystoporate bryozoans include 7 species belonging to 6 genera: Acanthoceramoporella, Ceramophylla, Ceramoporella, Constellaria, Crepipora, and Papillalunaria. One cystoporate species is new: Acanthoceramoporella valliensis. \r\n\r\nThe trepostome and cystoporate fauna on the generic level is, with few exceptions, cosmopolitan. Five genera, Eridotrypa, Parvohallopora, Heterotrypa, Constellaria, and Peronopora, dominate the fauna, comprising about 77 percent of the thin-sectioned specimens. On the species level the fauna is endemic to the Ordovician of eastern North America and is biostratigraphically restricted to strata of late Blackriveran Stage (Middle Ordovician) to early Maysvillian Stage (middle Late Ordovician). In Kentucky the species of this fauna are restricted to strata between the base of the Lexington Limestone (Kirkfieldian Stage, Middle Ordovician) and the top of the Clays Ferry Formation and its lateral equivalent the Kope Formation (Edenian Stage, lower Upper Ordovician), with few species ranging into strata of early Maysvillian Stage (middle Late Ordovician) in adjacent areas of Indiana and Ohio. \r\n\r\nOn the basis of the known geographic distribution of the various species, the fauna in Kentucky consists of an intermingling of immigrant and endemic species. The immigrant component (11 species) is generally limited to the lower half of the Lexington-Clays Ferry depositional sequence and permits the establishment of a degree of biostratigraphic equivalence with outcrop areas in Minnesota-Iowa and New York. On the species level the fauna in Kentucky is dominated by four: Constellaria teres, Heterotrypa foliacea, Parvohallopora nodulosa, and Eridotrypa mutabilis, in decreasing relative abundance. The first three species are restricted to the upper part of the Lexington Limestone and the Clays Ferry Formation. Eridotrypa mutabilis is restricted to the middle part of the Lexington Limestone and the lower half of the Clays Fer","language":"ENGLISH","doi":"10.3133/pp1066I","usgsCitation":"Karklins, O., 1984, Trepostome and cystoporate bryozoans from the Lexington Limestone and the Clays Ferry Formation (Middle and Upper Ordovician) of Kentucky: U.S. Geological Survey Professional Paper 1066, p. I1-I105; 3 plates in pocket, https://doi.org/10.3133/pp1066I.","productDescription":"p. I1-I105; 3 plates in pocket","costCenters":[],"links":[{"id":120364,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1066i/report-thumb.jpg"},{"id":65462,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1066i/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":65463,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1066i/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":65464,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1066i/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":65465,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1066i/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ae4b07f02db624bbf","contributors":{"authors":[{"text":"Karklins, O.L.","contributorId":87609,"corporation":false,"usgs":true,"family":"Karklins","given":"O.L.","affiliations":[],"preferred":false,"id":220195,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":38585,"text":"pp1278 - 1984 - The thrust belt in Southwest Montana and east-central Idaho","interactions":[],"lastModifiedDate":"2013-12-13T13:33:32","indexId":"pp1278","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1278","title":"The thrust belt in Southwest Montana and east-central Idaho","docAbstract":"The leading edge of the Cordilleran fold and thrust in southwest Montana appears to be a continuation of the edge of the Wyoming thrust belt, projected northward beneath the Snake River Plain. Trces of the thrust faults that form the leading edge of the thrust belts are mostly concealed, but stratigraphic and structural evidence suggests that the belt enters Montana near the middle of the Centennial Mountains, continues west along the Red Rock River valley, and swings north into the Highland Mountains near Butte. The thrust belt in southwest Montana and east-central Idaho includes at least two major plates -- the Medicine Lodge and Grasshopper thrust plates -- each of which contains a distinctive sequence of rocks, different in facies and structural style from those of the cratonic region east of the thrust belt. The thrust plates are characterized by persuasive, open to tight and locally overturned folds, and imbricate thrust faults, structural styles unusual in Phanerozoic cratonic rocks. The basal decollement zones of the plates are composed of intensely sheared, crushed, brecciated, and mylonitized rocks, the decollement at the base of the Medicine Lodge plate is as much as 300 meters thick. The Medicine Lodge and Grasshopper thrust plates are fringed on the east by a 10- to 50-kilometer-wide zone of tightly folded rocks cut by imbricate thrust fauls, a zone that forms the eastern margin of the thrust belt in southwest Montana. The frontal fold and thrust zone includes rocks that are similar to those of the craton, even though they differ in details of thickness, composition, or stratigraphic sequence. The zone is interpreted to be one of terminal folding and thrusting in cratonic rocks overridden by the major thrust plates from farther west. The cratonic rocks were drape-folded over rising basement blocks that formed a foreland bulge in front of the thrust belt. The basement blocks are bounded by steep faults of Proterozoic ancestry, which also moved as tear faults during thrusting, and seem to have controlled the curving patterns of salients and reentrants at the leading edge of the thrust belt. Radiometric and stratiographic evidence shows that the thrust belt was in its present position by about 75 million year go.","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/pp1278","usgsCitation":"Ruppel, E., and Lopez, D.A., 1984, The thrust belt in Southwest Montana and east-central Idaho: U.S. Geological Survey Professional Paper 1278, Report: iii, 41 p.; 1 Plate: 27.32 x 21.52 inches, https://doi.org/10.3133/pp1278.","productDescription":"Report: iii, 41 p.; 1 Plate: 27.32 x 21.52 inches","numberOfPages":"45","costCenters":[],"links":[{"id":170194,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1278/report-thumb.jpg"},{"id":279485,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1278/plate-1.pdf"},{"id":279486,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1278/report.pdf"}],"country":"United States","state":"Idaho;Montana","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114.0,43.0 ], [ -114.0,46.0 ], [ -111.0,46.0 ], [ -111.0,43.0 ], [ -114.0,43.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a5fe4b07f02db634a5f","contributors":{"authors":[{"text":"Ruppel, Edward T.","contributorId":7609,"corporation":false,"usgs":true,"family":"Ruppel","given":"Edward T.","affiliations":[],"preferred":false,"id":220112,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lopez, David A.","contributorId":79445,"corporation":false,"usgs":true,"family":"Lopez","given":"David","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":220113,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":38534,"text":"pp1315 - 1984 - Turonian (Eaglefordian) stratigraphy of the Atlantic Coastal Plain and Texas","interactions":[],"lastModifiedDate":"2012-02-02T00:10:16","indexId":"pp1315","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1315","title":"Turonian (Eaglefordian) stratigraphy of the Atlantic Coastal Plain and Texas","language":"ENGLISH","doi":"10.3133/pp1315","usgsCitation":"Valentine, P.C., 1984, Turonian (Eaglefordian) stratigraphy of the Atlantic Coastal Plain and Texas: U.S. Geological Survey Professional Paper 1315, 21 p., https://doi.org/10.3133/pp1315.","productDescription":"21 p.","costCenters":[],"links":[{"id":120238,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1315/report-thumb.jpg"},{"id":65297,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1315/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a49e4b07f02db623ec0","contributors":{"authors":[{"text":"Valentine, P. C.","contributorId":46505,"corporation":false,"usgs":true,"family":"Valentine","given":"P.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":220014,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":36581,"text":"fwsobs82_10_60 - 1984 - Habitat Suitability Index Models: Rainbow trout","interactions":[],"lastModifiedDate":"2022-02-09T15:19:15.342738","indexId":"fwsobs82_10_60","displayToPublicDate":"1994-01-01T00:00:00","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":"82/10.60","subseriesTitle":"Habitat Suitability Index","title":"Habitat Suitability Index Models: Rainbow trout","docAbstract":"A review and synthesis of existing information were used to develop riverine and lacustrine habitat models for rainbow trout (Salmo gairdneri), a freshwater species. The models are scaled to produce an index of habitat suitability between 0 (unsuitable habitat) to 1 (optimally suitable habitat) for freshwater areas of the continental United States. Other habitat suitability models found in the literature are also included. Habitat suitability indexes (HSI's) are designed for use with the habitat evaluation procedures developed by the U.S. Fish and Wildlife Service.\r\n\r\nAlso included are discussions of Suitability Index (SI) curves as used in the Instream Flow Incremental Methodology (IFIM) and SI curves available for an IFIM analysis of Fallfish habitat.","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Raleigh, R.F., Hickman, T., Solomon, R.C., and Nelson, P.C., 1984, Habitat Suitability Index Models: Rainbow trout: FWS/OBS 82/10.60, viii, 64 p.","productDescription":"viii, 64 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":165607,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db6497cb","contributors":{"authors":[{"text":"Raleigh, Robert F.","contributorId":49841,"corporation":false,"usgs":true,"family":"Raleigh","given":"Robert","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":216582,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hickman, Terry","contributorId":21207,"corporation":false,"usgs":true,"family":"Hickman","given":"Terry","affiliations":[],"preferred":false,"id":216580,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Solomon, R. Charles","contributorId":32585,"corporation":false,"usgs":true,"family":"Solomon","given":"R.","email":"","middleInitial":"Charles","affiliations":[],"preferred":false,"id":216581,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Nelson, Patrick C.","contributorId":68799,"corporation":false,"usgs":true,"family":"Nelson","given":"Patrick","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":216583,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":36425,"text":"fwsobs83_31 - 1984 - Seasonal abundance and habitat use patterns of coastal bird populations on Padre and Mustang Island barrier beaches (following the Ixtoc I Oil Spill)","interactions":[],"lastModifiedDate":"2012-02-02T00:09:36","indexId":"fwsobs83_31","displayToPublicDate":"1994-01-01T00:00:00","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":"83/31","title":"Seasonal abundance and habitat use patterns of coastal bird populations on Padre and Mustang Island barrier beaches (following the Ixtoc I Oil Spill)","language":"ENGLISH","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Chapman, B.R., 1984, Seasonal abundance and habitat use patterns of coastal bird populations on Padre and Mustang Island barrier beaches (following the Ixtoc I Oil Spill): FWS/OBS 83/31, x, 73 p. : ill., 2 maps; 28 cm.","productDescription":"x, 73 p. : ill., 2 maps; 28 cm.","costCenters":[],"links":[{"id":166921,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fc429","contributors":{"authors":[{"text":"Chapman, Brian R.","contributorId":19430,"corporation":false,"usgs":false,"family":"Chapman","given":"Brian","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":216300,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":36523,"text":"fwsobs82_10_81 - 1984 - Habitat Suitability Index Models: Blue Grouse","interactions":[],"lastModifiedDate":"2022-02-09T15:23:46.437155","indexId":"fwsobs82_10_81","displayToPublicDate":"1994-01-01T00:00:00","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":"82/10.81","subseriesTitle":"Habitat Suitability Index","title":"Habitat Suitability Index Models: Blue Grouse","docAbstract":"A review and synthesis of existing information were used to develop a Habitat Suitability Index (HSI) model for the blue grouse (Dendragapus obscurus). The model consolidates habitat use information into a framework appropriate for field application, and is scaled to produce an index between 0.0 (unsuitable habitat) to 1.0 (optimum habitat). HSI models are designed to be used with Habitat Evaluation Procedures previously developed by the U.S. Fish and Wildlife Service.","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Schroeder, R.L., 1984, Habitat Suitability Index Models: Blue Grouse: FWS/OBS 82/10.81, vi, 19 p.","productDescription":"vi, 19 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":167270,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db649cbf","contributors":{"authors":[{"text":"Schroeder, Richard L.","contributorId":10368,"corporation":false,"usgs":true,"family":"Schroeder","given":"Richard","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":216467,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":38635,"text":"pp1066J - 1984 - Leperditicopid ostracodes from Ordovician rocks of Kentucky and nearby states and characteristic features of the order Leperditicopida","interactions":[],"lastModifiedDate":"2012-02-02T00:10:35","indexId":"pp1066J","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1066","chapter":"J","title":"Leperditicopid ostracodes from Ordovician rocks of Kentucky and nearby states and characteristic features of the order Leperditicopida","docAbstract":"Leperditicopid ostracodes from the Ordovician formations of Kentucky occur in micritic to fine-grained carbonate rocks believed to represent shallow-water facies. They are found at widely separated horizons in the Middle Ordovician High Bridge Group, the Middle and Upper Ordovician Lexington Limestone, and the Upper Ordovician Ashlock, Bull Fork, and Drakes Formations. In this sequence, the leperditicopes are represented by two genera of leperditiids, Eoleperditia Swartz, 1949 and Bivia Berdan, 1976, and six isochilinid genera, Isochilina Jones, 1858, Teichochilina Swartz, 1949, Ceratoleperditia Harris, 1960, Parabriartina n. gen., Kenodontochilina n. gen., and Saffordellina Bassler and Kellett, 1934; the type species of the hitherto poorly known genus Saffordellina, S. muralis (Ulrich and Bassler, 1923), is redescribed and refigured. In all, 18 taxa, of which 2 are in open nomenclature, are described and illustrated. In addition, the family Isochilinidae Swartz, 1949 is redefined to include genera without marginal brims and with straight ventral contact margins. The morphological characteristics of leperditicopid genera are discussed, and a table listing described genera and their diagnostic features is included.","language":"ENGLISH","doi":"10.3133/pp1066J","usgsCitation":"Berdan, J., 1984, Leperditicopid ostracodes from Ordovician rocks of Kentucky and nearby states and characteristic features of the order Leperditicopida: U.S. Geological Survey Professional Paper 1066, p. J1 - J40, https://doi.org/10.3133/pp1066J.","productDescription":"p. J1 - J40","costCenters":[],"links":[{"id":120365,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1066j/report-thumb.jpg"},{"id":65466,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1066j/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a631d","contributors":{"authors":[{"text":"Berdan, J.M.","contributorId":27913,"corporation":false,"usgs":true,"family":"Berdan","given":"J.M.","affiliations":[],"preferred":false,"id":220196,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":38547,"text":"pp1280 - 1984 - Geologic setting and petrochemistry of the Late Cretaceous-early Tertiary intrusives in the northern Front Range mineral belt, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:10:32","indexId":"pp1280","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1280","title":"Geologic setting and petrochemistry of the Late Cretaceous-early Tertiary intrusives in the northern Front Range mineral belt, Colorado","language":"ENGLISH","doi":"10.3133/pp1280","usgsCitation":"Gable, D.J., 1984, Geologic setting and petrochemistry of the Late Cretaceous-early Tertiary intrusives in the northern Front Range mineral belt, Colorado: U.S. Geological Survey Professional Paper 1280, 33 p.; 1 plate in pocket, https://doi.org/10.3133/pp1280.","productDescription":"33 p.; 1 plate in pocket","costCenters":[],"links":[{"id":104593,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4788.htm","linkFileType":{"id":5,"text":"html"},"description":"4788"},{"id":122310,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1280/report-thumb.jpg"},{"id":65315,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1280/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":65316,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1280/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db68824a","contributors":{"authors":[{"text":"Gable, D. J.","contributorId":36569,"corporation":false,"usgs":true,"family":"Gable","given":"D.","middleInitial":"J.","affiliations":[],"preferred":false,"id":220034,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":38583,"text":"pp1273G - 1984 - Geohydrology of the Madison and associated aquifers in parts of Montana, North Dakota, South Dakota, and Wyoming","interactions":[{"subject":{"id":8614,"text":"ofr82914 - 1982 - Geohydrology of the Madison and associated aquifers in parts of Montana, North Dakota, South Dakota, and Wyoming","indexId":"ofr82914","publicationYear":"1982","noYear":false,"title":"Geohydrology of the Madison and associated aquifers in parts of Montana, North Dakota, South Dakota, and Wyoming"},"predicate":"SUPERSEDED_BY","object":{"id":38583,"text":"pp1273G - 1984 - Geohydrology of the Madison and associated aquifers in parts of Montana, North Dakota, South Dakota, and Wyoming","indexId":"pp1273G","publicationYear":"1984","noYear":false,"chapter":"G","title":"Geohydrology of the Madison and associated aquifers in parts of Montana, North Dakota, South Dakota, and Wyoming"},"id":1}],"lastModifiedDate":"2012-02-02T00:10:14","indexId":"pp1273G","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1273","chapter":"G","title":"Geohydrology of the Madison and associated aquifers in parts of Montana, North Dakota, South Dakota, and Wyoming","language":"ENGLISH","doi":"10.3133/pp1273G","usgsCitation":"Downey, J.S., 1984, Geohydrology of the Madison and associated aquifers in parts of Montana, North Dakota, South Dakota, and Wyoming: U.S. Geological Survey Professional Paper 1273, p. G1-G47; 1 plate in pocket, https://doi.org/10.3133/pp1273G.","productDescription":"p. G1-G47; 1 plate in pocket","costCenters":[],"links":[{"id":120024,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1273g/report-thumb.jpg"},{"id":65395,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1273g/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":65396,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1273g/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8950","contributors":{"authors":[{"text":"Downey, J. S.","contributorId":100013,"corporation":false,"usgs":true,"family":"Downey","given":"J.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":220110,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":36521,"text":"fwsobs82_10_79 - 1984 - Habitat Suitability Index Models and Instream Flow Suitability Curves: Redear sunfish","interactions":[],"lastModifiedDate":"2022-02-09T15:24:41.987631","indexId":"fwsobs82_10_79","displayToPublicDate":"1994-01-01T00:00:00","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":"82/10.79","subseriesTitle":"Habitat Suitability Index","title":"Habitat Suitability Index Models and Instream Flow Suitability Curves: Redear sunfish","docAbstract":"<p>The redear sunfish (Lepomis microlophus), commonly referred to as the shellcracker, is native from the Mississippi River in Missouri and southern Indiana to North Carolina, south through Florida, and west to eastern Texas (Cole 1951; Trautman 1957; Hubbs and Lagler 1964; Wilbur 1969; Pflieger 1975). The species has been successfully introduced into Arizona, California, and southern Michigan and stocked into new waters in Oklahoma,Missouri, Ohio, Indiana, and Illinois (Cole 1951; Beland 1953; Jenkins 1955; Trautman 1957; Lopinot 1961; Hubbs and Lagler 1964; Wilbur 1969).</p>","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Twomey, K.A., Gebhart, G., Maughan, O.E., and Nelson, P.C., 1984, Habitat Suitability Index Models and Instream Flow Suitability Curves: Redear sunfish: FWS/OBS 82/10.79, vi, 29 p.","productDescription":"vi, 29 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":167268,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db649e66","contributors":{"authors":[{"text":"Twomey, Kathleen A.","contributorId":38629,"corporation":false,"usgs":true,"family":"Twomey","given":"Kathleen","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":216459,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gebhart, Glen","contributorId":52237,"corporation":false,"usgs":true,"family":"Gebhart","given":"Glen","email":"","affiliations":[],"preferred":false,"id":216461,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Maughan, O. Eugene","contributorId":43006,"corporation":false,"usgs":true,"family":"Maughan","given":"O.","email":"","middleInitial":"Eugene","affiliations":[],"preferred":false,"id":216460,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Nelson, Patrick C.","contributorId":68799,"corporation":false,"usgs":true,"family":"Nelson","given":"Patrick","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":216462,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":36522,"text":"fwsobs82_10_80 - 1984 - Habitat Suitability Index Models and Instream Flow Suitability Curves: Paddlefish","interactions":[],"lastModifiedDate":"2022-02-09T15:24:14.15771","indexId":"fwsobs82_10_80","displayToPublicDate":"1994-01-01T00:00:00","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":"82/10.80","subseriesTitle":"Habitat Suitability Index","title":"Habitat Suitability Index Models and Instream Flow Suitability Curves: Paddlefish","docAbstract":"<p>The original range of the paddlefish was the Mississippi River drainage and adjacent Gul f Coast dra i nage. It was once found in some of the Great Lakes (Carlson and Bonislawsky 1981). The paddlefish is generally an inhabitant of large rivers, but it occurs in reservoirs and natural lakes connected to large rivers. Much of the original range has been reduced due to habitat alterations: (1) destruction of spawning areas; (2) blockage of movements by dams; (3) channelization and elimination of backwater areas; (4) dewatering of streams; and (5) pollution (Carlson and Bonislawsky 1981). Several States officially consider the paddlefish as rare or endangered (Miller 1972). An indexed bibliography of all known paddlefish work was prepared by Graham and Bonislawsky (1978) and recently updated to include more than 480 citations (Graham and Bonislawsky, in press).</p>","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Hubert, W.A., Anderson, S.H., Southall, P.D., and Crance, J.H., 1984, Habitat Suitability Index Models and Instream Flow Suitability Curves: Paddlefish: FWS/OBS 82/10.80, vi, 32 p.","productDescription":"vi, 32 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":167269,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db649e5c","contributors":{"authors":[{"text":"Hubert, Wayne A.","contributorId":9325,"corporation":false,"usgs":true,"family":"Hubert","given":"Wayne","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":216463,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Anderson, Stanley H.","contributorId":68361,"corporation":false,"usgs":true,"family":"Anderson","given":"Stanley","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":216466,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Southall, Peter D.","contributorId":39844,"corporation":false,"usgs":true,"family":"Southall","given":"Peter","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":216465,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Crance, Johnie H.","contributorId":9326,"corporation":false,"usgs":true,"family":"Crance","given":"Johnie","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":216464,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":38532,"text":"pp1312 - 1984 - The Richmond and Greenwich slices of the Hamburg klippe in eastern Pennsylvania — Stratigraphy, sedimentology, structure, and plate tectonic implications","interactions":[],"lastModifiedDate":"2022-09-12T21:48:12.293122","indexId":"pp1312","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1312","title":"The Richmond and Greenwich slices of the Hamburg klippe in eastern Pennsylvania — Stratigraphy, sedimentology, structure, and plate tectonic implications","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp1312","usgsCitation":"Lash, G.G., and Drake, A.A., 1984, The Richmond and Greenwich slices of the Hamburg klippe in eastern Pennsylvania — Stratigraphy, sedimentology, structure, and plate tectonic implications: U.S. Geological Survey Professional Paper 1312, 40 p., https://doi.org/10.3133/pp1312.","productDescription":"40 p.","costCenters":[],"links":[{"id":406568,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_74325.htm","linkFileType":{"id":5,"text":"html"}},{"id":65295,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1312/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":122276,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1312/report-thumb.jpg"}],"country":"United States","state":"Pennsylvania","otherGeospatial":"Richmond and Greenwich slices of the Hamburg klippe","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -76.0519,\n              40.4614\n            ],\n            [\n              -75.6978,\n              40.4614\n            ],\n            [\n              -75.6978,\n              40.6889\n            ],\n            [\n              -76.0519,\n              40.6889\n            ],\n            [\n              -76.0519,\n              40.4614\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67acbe","contributors":{"authors":[{"text":"Lash, G. G.","contributorId":60648,"corporation":false,"usgs":true,"family":"Lash","given":"G.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":220010,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Drake, Avery A. Jr.","contributorId":81090,"corporation":false,"usgs":true,"family":"Drake","given":"Avery","suffix":"Jr.","middleInitial":"A.","affiliations":[],"preferred":false,"id":220011,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":36538,"text":"fwsobs82_10_75 - 1984 - Habitat Suitability Index Models: Spotted seatrout","interactions":[],"lastModifiedDate":"2022-02-09T15:20:37.161233","indexId":"fwsobs82_10_75","displayToPublicDate":"1994-01-01T00:00:00","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":"82/10.75","subseriesTitle":"Habitat Suitability Index","title":"Habitat Suitability Index Models: Spotted seatrout","docAbstract":"<p>The estuarine spotted seatrout, a primarily estuarine species, is one of the most important sport and commercial fishes in coastal Gulf of Mexico waters (Arnold et a1. 1976). Spotted seatrout rank second by weight in catches by U.S. saltwater sport fishermen (National Marine Fisheries Services 1981) .</p>","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Kostecki, P.T., 1984, Habitat Suitability Index Models: Spotted seatrout: FWS/OBS 82/10.75, vi, 22 p.","productDescription":"vi, 22 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":166203,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db649743","contributors":{"authors":[{"text":"Kostecki, Paul T.","contributorId":55060,"corporation":false,"usgs":true,"family":"Kostecki","given":"Paul","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":216495,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":38580,"text":"pp1273A - 1984 - Stratigraphy and sedimentary facies of the Madison Limestone and associated rocks in parts of Montana, Nebraska, North Dakota, South Dakota, and Wyoming","interactions":[{"subject":{"id":10677,"text":"ofr81642 - 1981 - Stratigraphy and sedimentary facies of the Madison limestone and associated rocks in parts of Montana, North Dakota, South Dakota, Wyoming, and Nebraska","indexId":"ofr81642","publicationYear":"1981","noYear":false,"title":"Stratigraphy and sedimentary facies of the Madison limestone and associated rocks in parts of Montana, North Dakota, South Dakota, Wyoming, and Nebraska"},"predicate":"SUPERSEDED_BY","object":{"id":38580,"text":"pp1273A - 1984 - Stratigraphy and sedimentary facies of the Madison Limestone and associated rocks in parts of Montana, Nebraska, North Dakota, South Dakota, and Wyoming","indexId":"pp1273A","publicationYear":"1984","noYear":false,"chapter":"A","title":"Stratigraphy and sedimentary facies of the Madison Limestone and associated rocks in parts of Montana, Nebraska, North Dakota, South Dakota, and Wyoming"},"id":1}],"lastModifiedDate":"2016-12-22T12:32:49","indexId":"pp1273A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1273","chapter":"A","title":"Stratigraphy and sedimentary facies of the Madison Limestone and associated rocks in parts of Montana, Nebraska, North Dakota, South Dakota, and Wyoming","language":"ENGLISH","doi":"10.3133/pp1273A","usgsCitation":"Peterson, J., 1984, Stratigraphy and sedimentary facies of the Madison Limestone and associated rocks in parts of Montana, Nebraska, North Dakota, South Dakota, and Wyoming: U.S. Geological Survey Professional Paper 1273, p. 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,{"id":36524,"text":"fwsobs82_10_82 - 1984 - Habitat Suitability Index Models: Canvasback (breeding habitat)","interactions":[],"lastModifiedDate":"2022-02-09T15:23:23.504501","indexId":"fwsobs82_10_82","displayToPublicDate":"1994-01-01T00:00:00","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":"82/10.82","subseriesTitle":"Habitat Suitability Index","title":"Habitat Suitability Index Models: Canvasback (breeding habitat)","docAbstract":"<p>Canvasbacks (Aythya valisineria) breed from Alaska south to Montana and the Dakotas, with the highest breeding densities found in the parklands of Southcentral Canada (Bellrose 1976). Canvasbacks nest over water in a variety of wetland habitats, including large marshes, ponds, sloughs, and potholes. Their preferred breeding habitat is shallow prairie marshes, bordered by cattail (~ spp.), bulrush (Scirpus spp.), and similar emergent vegetation (Johnsgard 1975).</p>","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Schroeder, R.L., 1984, Habitat Suitability Index Models: Canvasback (breeding habitat): FWS/OBS 82/10.82, vi, 16 p.","productDescription":"vi, 16 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":167271,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db649b99","contributors":{"authors":[{"text":"Schroeder, Richard L.","contributorId":10368,"corporation":false,"usgs":true,"family":"Schroeder","given":"Richard","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":216468,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":38513,"text":"pp1342 - 1984 - The evolution of the southern California uplift, 1955 through 1976","interactions":[],"lastModifiedDate":"2017-04-25T15:11:50","indexId":"pp1342","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1342","title":"The evolution of the southern California uplift, 1955 through 1976","docAbstract":"<p>The southern California uplift culminated in 1974 as a 150- km-wide crustal swell that extended about 600 km eastward and east-southeastward from Point Arguello to the Colorado River and Salton Sea, respectively; it was characterized by remarkably uniform height changes between 1959 and 1974 of 0.30-0.35 m over at least half of its 60,000-70,000 km<sup>2</sup> area. At its zenith, the uplift included virtually the entire Transverse Ranges geologic province and parts of the Coast Ranges, San Joaquin Valley, Sierra Nevada, Basin and Range, Mojave Desert, Peninsular Ranges, and Salton Trough provinces. The alinement of the western part of the uplift closely paralleled the east-trending Transverse Ranges, whereas the southern flank of the eastern lobe roughly coincided with the west-northwest-trending San Andreas fault. The position and configuration of the uplift associate it with a singularly complex section of the boundary between the North American and Pacific plates that has certainly sustained major modification during the past 5 million years and probably during the past 1 million years. </p><p>Surface deformation can be categorized as tectonic or nontectonic. Nontectonic vertical displacements associated with the activities of man have overwhelmed natural compaction and areally significant soil expansion in the southern California area. Because tectonic displacements are implicitly defined as those that cannot be otherwise explained, those vertical movements that can be reasonably attributed to artificial processes have been subtracted from our reconstructed configurations of the uplift. Hence this reconstruction has necessarily included the assembly and evaluation of an enormous volume of data on oil-field operations, changes in ground-water levels, and measured subsidence (or rebound) associated with changes in the underground fluid regimen. </p><p>Measured changes in height at various stages in the evolution of the uplift have been based chiefly on first-order levelings carried out between 1953 and 1976. Exceptions to this generalization consist largely of the results of pre-1953 surveys through the western Transverse Ranges and the eastern Mojave Desert. Errors in measured height differences derive from blunders, systematic survey errors, random survey errors, improperly formulated orthometric corrections, and intrasurvey movement; the last of these has created the most serious problems encountered in our reconstruction of the basic data. A variety of independent tests indicate that survey error associated with the utilized levelings was generally small and fell largely within the predicted random-error range. Moreover, the redundancy and coherence displayed by the entire data set provide convincing evidence of survey accuracy and the virtual absence of height- and slope-dependent error in particular. </p><p>Our reconstructions of the changing configuration of the uplift derive chiefly from comparisons among sequentially developed observed elevations along the same route. Most of the observed elevations from which the vertical displacements were computed have been reconstructed with respect to bench mark Tidal 8, San Pedro, as invariant in height. Because the San Pedro tide station has been characterized by a history of modest relative uplift, vertical displacements referred to this station are biased slightly toward the appearance of subsidence. Where the observed elevations cannot be conveniently tied to Tidal 8, they have been referred to secondary control points whose history with respect to Tidal 8 can be independently established. Each of the lines of observed elevation changes provides, accordingly, a section athwart or along the axis of the uplift from which the changes in the configuration of the uplift can be roughly generalized. Because relatively few surveys were run in 1955, which we choose as a representative temporal datum, we have commonly incorporated the results of earlier or of somewhat later levelings as the equivalents of 1955 surveys. Although this procedure introduces a certain subjectivity, the probable equivalence between the results of these earlier or later surveys with those that would have been obtained had this leveling been carried out in 1955, usually can be independently tested. Wherever the calculated vertical displacements are based on comparisons between the results of levelings over different routes, the observed elevations have been orthometrically corrected to agree with those that would have been produced had each of these surveys been along the same route. </p><p>The growth of the southern California uplift consisted of two well-defined spasms of positive movement, the second of which was closely followed by partial collapse. Our reconstruction, although it clearly errs in detail, indicates that the uplift, together with marginal and apparently ephemeral tectonic subsidence, nucleated in the west-central Transverse Ranges near Ozena, sometime between the spring of 1959 and the spring of 1960. The uplift expanded rapidly eastward (and probably westward as well), and by the fall of 1961 much of the Transverse Ranges and the Mojave Desert at least as far east as Twentynine Palms had risen by as much as 0.25 m. Between 1962 and 1972 the area included by the initially developed (1959-61) uplift sustained additional but clearly decelerating uplift accompanied locally by oscillatory displacements. Between 1972/ 73 and 1974 a second crustal spasm extended the uplift eastward to the Colorado River and elevated much of the eastern Mojave Desert by values that equaled or exceeded those developed within the western lobe. Between 1974 and 1976, at least the central part of the uplift sustained partial collapse that nowhere amounted to less than 50 percent of the cumulative uplift since 1959. Whether this collapse affected the entire uplift is conjectural, but we now recognize well-defined evidence of major down-to-the-north tilting that must have occurred within the eastern part of the uplift at some time between 1974 and 1976. </p><p>Accumulating evidence indicates that nearly all the area included with the southern California uplift underwent similar uplift and partial collapse during the early part of the 20th century. Thus we infer that the recent uplift represents but a single event in an ongoing, more or less cyclic deformational process characterized by a period of about 50 years. Even though less than two full cycles are expressed in the geodetic&nbsp;record, the cumulative rate of uplift near the center of the recent uplift probably has averaged about 5 mm/yr, a value that is roughly consistent with the uplift rates that have been deduced for the late Quaternary emergent marine terraces along the south flank of the Transverse Ranges. </p><p>Although the evolution of the recent uplift is relatively well defined, its correlation with the regional seismicity is poorly defined. A comparison between the occurrence of southern California earthquakes of magnitude ≥4 during the period 1932 to 1976 with the 1974 configuration of the uplift demonstrates the existence of (1) relatively aseismic areas within the western lobe of the uplift (in the western Transverse Ranges), in the central part of the uplift (in the western Mojave Desert), and along an east-trending zone that extends into the eastern Mojave athwart the south flank of the uplift (north of the Salton Sea) and (2) localized concentrations of seismic activity along the flanks of the uplift. Moreover, 9 of the 10 largest earthquakes recorded within or around the area of the southern California uplift during the period 1932 to 1976 (the 1933 Long Beach, the 1941 Santa Barbara, the 1946 Walker Pass, the 1947 Manix, the 1948 Desert Hot Springs, and the four major 1952 Kern County shocks) occurred before the inception of the uplift in 1959 or 1960. </p><p>The area embraced by the southern California uplift has been identified with geodetically defined horizontal strain, part of which may have accumulated as a major north-south contractional event that roughly coincided with the first spasm of uplift. Nonetheless, continuing contractional strain associated with regionally developed partial collapse argues that the uplift cannot be fully explained simply as the vertical expression of continuing north-south compression. Consideration of the two well-defined historical episodes of uplift and partial collapse indicate that the southern California uplift may be the product of decoupling and viscous flow beneath the seismogenic zone, presumably driven by continuing motion between the irregularly margined plates south of the great bend of the San Andreas fault. Because the magnitude of the maximum uplift associated with each episode was approximately the same, there may be some threshold value above which collapse (viscous flow) may ensue; the absence of total collapse may be a function of precollapse strain hardening within the postulated subseismogenic viscoelastic layer.</p>","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/pp1342","usgsCitation":"Castle, R.O., Elliot, M.R., Church, J.P., and Wood, S.H., 1984, The evolution of the southern California uplift, 1955 through 1976: U.S. Geological Survey Professional Paper 1342, Report: vii, 136 p.; 16 Plates: 48 x 50.5 inches or less, https://doi.org/10.3133/pp1342.","productDescription":"Report: vii, 136 p.; 16 Plates: 48 x 50.5 inches or less","costCenters":[],"links":[{"id":65240,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1342/plate-07.pdf","text":"Plate 7","size":"973.46 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