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,{"id":66341,"text":"i845G - 1974 - Dissolved-solids content of ground water in the Phoenix area, Arizona","interactions":[],"lastModifiedDate":"2025-08-08T20:01:49.658992","indexId":"i845G","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"845","subseriesTitle":"NONE","chapter":"G","title":"Dissolved-solids content of ground water in the Phoenix area, Arizona","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i845G","usgsCitation":"Kister, L., 1974, Dissolved-solids content of ground water in the Phoenix area, Arizona: U.S. Geological Survey IMAP 845, 1 Plate: 32.29 x 25.76 inches, https://doi.org/10.3133/i845G.","productDescription":"1 Plate: 32.29 x 25.76 inches","costCenters":[],"links":[{"id":493902,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9694.htm","linkFileType":{"id":5,"text":"html"}},{"id":255808,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/0845g/report-thumb.jpg"},{"id":255807,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/0845g/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":255806,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0845g/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","country":"United States","state":"Arizona","city":"Phoenix","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -113,\n              33.921\n            ],\n            [\n              -113,\n              32.75\n            ],\n            [\n              -110.906,\n              32.75\n            ],\n            [\n              -110.906,\n              33.921\n            ],\n            [\n              -113,\n              33.921\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db64a1f9","contributors":{"authors":[{"text":"Kister, L. R.","contributorId":54187,"corporation":false,"usgs":true,"family":"Kister","given":"L. R.","affiliations":[],"preferred":false,"id":274375,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":66509,"text":"i878 - 1974 - Availability of ground water for irrigation, municipal, or industrial use in the Navajo and Hopi Indian Reservations, Arizona, New Mexico, and Utah","interactions":[],"lastModifiedDate":"2025-08-13T19:30:55.69324","indexId":"i878","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"878","title":"Availability of ground water for irrigation, municipal, or industrial use in the Navajo and Hopi Indian Reservations, Arizona, New Mexico, and Utah","docAbstract":"<p>The Navajo and Hopi Indian reservations are located mainly in northeastern Arizona, although the Navajo Indian reservation extends into northwestern New Mexico and southeastern Utah (see location map). The area of this report coincides with the areas of the Navajo and Hopi Indian reservations except in part of New Mexico, where the areas was extended eastward to longitude 108° and southward to Interstate Highway 40 and in southeastern Utah.</p><p>This investigation was conducted by the U.S. Geological Survey at the request of the Bureau of Indian Affairs. The study was undertaken to evaluate the potential for large-scale ground-water development in the Navajo and Hope Indian Reservations. The results given in this report are intended as preliminary guidelines for the development of ground water in sufficient quantity and of suitable quality for irrigation, municipal, and industrial uses. Data are not included for areas in which less than 25 gal min<sup>-1</sup> (gallons per minute) or 95 l min<sup>-1 </sup>(litres per minute) can be developed.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/i878","collaboration":"Prepared in cooperation with the Bureau of Indian Affairs","usgsCitation":"McGavock, E.H., and Edmonds, R.J., 1974, Availability of ground water for irrigation, municipal, or industrial use in the Navajo and Hopi Indian Reservations, Arizona, New Mexico, and Utah: U.S. Geological Survey IMAP 878, 4 Sheets: 48.74 x 34.30 inches or smaller; Cover: 9.15 x 11.92 inches, https://doi.org/10.3133/i878.","productDescription":"4 Sheets: 48.74 x 34.30 inches or smaller; Cover: 9.15 x 11.92 inches","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":494052,"rank":7,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9778.htm","linkFileType":{"id":5,"text":"html"}},{"id":255953,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0878/plate-2.pdf","text":"Sheet 2: Areas where wells will yield at least 200 gallons per minute","size":"18.36 MB","linkFileType":{"id":1,"text":"pdf"}},{"id":255957,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/0878/report-thumb.jpg"},{"id":255956,"rank":2,"type":{"id":8,"text":"Cover"},"url":"https://pubs.usgs.gov/imap/0878/report.pdf","text":"Folio Cover","size":"30 KB","linkFileType":{"id":1,"text":"pdf"}},{"id":255955,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0878/plate-4.pdf","text":"Sheet 4: Areas where wells will yield at least 25 gallons per minute","size":"14.86 MB","linkFileType":{"id":1,"text":"pdf"}},{"id":255952,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0878/plate-1.pdf","text":"Sheet 1: Areas where wells will yield at least 500 gallons per minute","size":"19.92 MB","linkFileType":{"id":1,"text":"pdf"}},{"id":255954,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0878/plate-3.pdf","text":"Sheet 3: Areas where wells will yield at least 75 gallons per minute","size":"17.89 MB","linkFileType":{"id":1,"text":"pdf"}}],"scale":"375000","country":"United States","state":"Arizona, New Mexico, Utah","otherGeospatial":"Navajo Indian Reservations, Hopi Indian Reservations","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -112,35 ], [ -112,37.5 ], [ -108,37.5 ], [ -108,35 ], [ -112,35 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa9e4b07f02db667eda","contributors":{"authors":[{"text":"McGavock, E. H.","contributorId":40679,"corporation":false,"usgs":true,"family":"McGavock","given":"E.","middleInitial":"H.","affiliations":[],"preferred":false,"id":274633,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Edmonds, R. J.","contributorId":78825,"corporation":false,"usgs":true,"family":"Edmonds","given":"R.","middleInitial":"J.","affiliations":[],"preferred":false,"id":274634,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":18555,"text":"ofr741017 - 1974 - MAGDEP - a computer program for finding depth to basement from total field magnetic profiles","interactions":[],"lastModifiedDate":"2012-02-02T00:07:32","indexId":"ofr741017","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"74-1017","title":"MAGDEP - a computer program for finding depth to basement from total field magnetic profiles","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr741017","usgsCitation":"Cooper, A.K., 1974, MAGDEP - a computer program for finding depth to basement from total field magnetic profiles: U.S. Geological Survey Open-File Report 74-1017, 75 p.  ;28 cm., https://doi.org/10.3133/ofr741017.","productDescription":"75 p.  ;28 cm.","costCenters":[],"links":[{"id":151583,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1974/1017/report-thumb.jpg"},{"id":47907,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1974/1017/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7fe4b07f02db648b32","contributors":{"authors":[{"text":"Cooper, A. K.","contributorId":50149,"corporation":false,"usgs":true,"family":"Cooper","given":"A.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":179331,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":63082,"text":"gq1174 - 1974 - Geologic map of the Golconda quadrangle, Humboldt County, Nevada","interactions":[],"lastModifiedDate":"2012-02-10T00:10:45","indexId":"gq1174","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1174","title":"Geologic map of the Golconda quadrangle, Humboldt County, Nevada","language":"ENGLISH","doi":"10.3133/gq1174","usgsCitation":"Erickson, R.L., and Marsh, S.P., 1974, Geologic map of the Golconda quadrangle, Humboldt County, Nevada: U.S. Geological Survey Geologic Quadrangle 1174, 1 map., https://doi.org/10.3133/gq1174.","productDescription":"1 map.","costCenters":[],"links":[{"id":107607,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_10713.htm","linkFileType":{"id":5,"text":"html"},"description":"10713"},{"id":249209,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/1174/report.pdf","size":"26","linkFileType":{"id":1,"text":"pdf"}},{"id":252374,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/1174/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -117.5,40.8675 ], [ -117.5,41 ], [ -117.36749999999999,41 ], [ -117.36749999999999,40.8675 ], [ -117.5,40.8675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b01e4b07f02db69893f","contributors":{"authors":[{"text":"Erickson, Ralph Leroy","contributorId":107263,"corporation":false,"usgs":true,"family":"Erickson","given":"Ralph","email":"","middleInitial":"Leroy","affiliations":[],"preferred":false,"id":268302,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Marsh, Sherman P.","contributorId":42950,"corporation":false,"usgs":true,"family":"Marsh","given":"Sherman","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":268301,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":3118,"text":"wsp2132 - 1974 - Surface water supply of the United States, 1966-70, Part 12, Pacific Slope basins in Washington, v. 1, Pacific Slope basins in Washington except Columbia River basin","interactions":[],"lastModifiedDate":"2017-06-17T12:49:31","indexId":"wsp2132","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2132","title":"Surface water supply of the United States, 1966-70, Part 12, Pacific Slope basins in Washington, v. 1, Pacific Slope basins in Washington except Columbia River basin","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp2132","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1974, Surface water supply of the United States, 1966-70, Part 12, Pacific Slope basins in Washington, v. 1, Pacific Slope basins in Washington except Columbia River basin: U.S. Geological Survey Water Supply Paper 2132, viii, 640 p. ;23 cm., https://doi.org/10.3133/wsp2132.","productDescription":"viii, 640 p. ;23 cm.","costCenters":[],"links":[{"id":30030,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2132/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":139227,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2132/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af5e4b07f02db692271","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":528095,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":35815,"text":"b1308 - 1974 - Geology and placer-gold deposits of the Jicarilla Mountains, Lincoln County, New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:09:40","indexId":"b1308","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"1308","title":"Geology and placer-gold deposits of the Jicarilla Mountains, Lincoln County, New Mexico","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/b1308","usgsCitation":"Segerstrom, K.K., and Ryberg, G.E., 1974, Geology and placer-gold deposits of the Jicarilla Mountains, Lincoln County, New Mexico: U.S. Geological Survey Bulletin 1308, iv, 25 p. :maps(part fold.col.in pocket) ;24 cm., https://doi.org/10.3133/b1308.","productDescription":"iv, 25 p. :maps(part fold.col.in pocket) ;24 cm.","costCenters":[],"links":[{"id":165863,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1308/report-thumb.jpg"},{"id":63734,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1308/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":63735,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1308/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad7e4b07f02db6843dc","contributors":{"authors":[{"text":"Segerstrom, Kenneth K.","contributorId":105276,"corporation":false,"usgs":true,"family":"Segerstrom","given":"Kenneth","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":215273,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ryberg, George E.","contributorId":68167,"corporation":false,"usgs":true,"family":"Ryberg","given":"George","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":215272,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":65038,"text":"i835 - 1974 - Geologic map and sections showing areal distribution of Tertiary rocks near the southeastern terminus of the Wind River Range, Fremont and Sweetwater counties, Wyoming","interactions":[],"lastModifiedDate":"2012-02-10T00:11:07","indexId":"i835","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"835","subseriesTitle":"NONE","title":"Geologic map and sections showing areal distribution of Tertiary rocks near the southeastern terminus of the Wind River Range, Fremont and Sweetwater counties, Wyoming","language":"ENGLISH","doi":"10.3133/i835","usgsCitation":"Denson, N., and Pipiringos, G., 1974, Geologic map and sections showing areal distribution of Tertiary rocks near the southeastern terminus of the Wind River Range, Fremont and Sweetwater counties, Wyoming: U.S. Geological Survey IMAP 835, 2 maps on two sheets., https://doi.org/10.3133/i835.","productDescription":"2 maps on two sheets.","costCenters":[],"links":[{"id":107003,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9665.htm","linkFileType":{"id":5,"text":"html"},"description":"9665"},{"id":189140,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"48000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -108.61749999999999,42.25 ], [ -108.61749999999999,42.5 ], [ -108,42.5 ], [ -108,42.25 ], [ -108.61749999999999,42.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b13e4b07f02db6a380a","contributors":{"authors":[{"text":"Denson, N.M.","contributorId":79458,"corporation":false,"usgs":true,"family":"Denson","given":"N.M.","affiliations":[],"preferred":false,"id":272565,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pipiringos, G. N.","contributorId":11210,"corporation":false,"usgs":true,"family":"Pipiringos","given":"G. N.","affiliations":[],"preferred":false,"id":272564,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":37214,"text":"rp115 - 1974 - Population ecology of the mallard: II. Breeding habitat conditions, size of the breeding populations, and production indices","interactions":[],"lastModifiedDate":"2016-11-09T13:42:16","indexId":"rp115","displayToPublicDate":"1991-08-16T07:00:00","publicationYear":"1974","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":"115","title":"Population ecology of the mallard: II. Breeding habitat conditions, size of the breeding populations, and production indices","docAbstract":"<p><span>This report, the second in a series on a comprehensive analysis of mallard population data, provides information on mallard breeding habitat, the size and distribution of breeding populations, and indices to production. The information in this report is primarily the result of large-scale aerial surveys conducted during May and July, 1955-73. The history of the conflict in resource utilization between agriculturalists and wildlife conservation interests in the primary waterfowl breeding grounds is reviewed. The numbers of ponds present during the breeding season and the midsummer period and the effects of precipitation and temperature on the number of ponds present are analyzed in detail. No significant cycles in precipitation were detected and it appears that precipitation is primarily influenced by substantial seasonal and random components. Annual estimates (1955-73) of the number of mallards in surveyed and unsurveyed breeding areas provided estimates of the size and geographic distribution of breeding mallards in North America. The estimated size of the mallard breeding population in North America has ranged from a high of 14.4 million in 1958 to a low of 7.1 million in 1965. Generally, the mallard breeding population began to decline after the 1958 peak until 1962, and remained below 10 million birds until 1970. The decline and subsequent low level of the mallard population between 1959 and 1969 .generally coincided with a period of poor habitat conditions on the major breeding grounds. The density of mallards was highest in the </span><i>Prairie-Parkland Area</i><span> with an average of nearly 19.2 birds per square mile. The proportion of the continental mallard breeding population in the </span><i>Prairie-Parkland Area</i><span> ranged from 30% in 1962 to a high of 600/0 in 1956. The geographic distribution of breeding mallards throughout North America was significantly related to the number of May ponds in the </span><i>Prairie-Parkland Area</i><span>. Estimates of midsummer habitat conditions and indices to production from the July Production Survey were studied in detail. Several indices relating to production showed marked declines from west to east in the </span><i>Prairie-Parkland Area</i><span>, these are: (1) density of breeding mallards (per square mile and per May pond), (2) brood density (per square mile and per July pond), (3) average brood size (all species combined), and (4) brood survival from class II to class III. An index to late nesting and renesting efforts was highest during years when midsummer water conditions were good. Production rates of many ducks breeding in North America appear to be regulated by both density-dependent and density-independent factors. Spacing of birds in the </span><i>Prairie-Parkland Area</i><span> appeared to be a key factor in the density-dependent regulation of the population. The spacing mechanism, in conjunction with habitat conditions, influenced some birds to overfly the primary breeding grounds into less favorable habitats to the north and northwest where the production rate may be suppressed. The production rate of waterfowl in the </span><i>Prairie Parkland Area</i><span> seems to be independent of density (after emigration has taken place) because the production index appears to be a linear function of the number of breeding birds in the area. Similarly, the production rate of waterfowl in northern Saskatchewan and northern Manitoba appeared to be independent of density. Production indices in these northern areas appear to be a linear function of the size of the breeding population. Thus, the density and distribution of breeding ducks is probably regulated through a spacing mechanism that is at least partially dependent on measurable environmental factors. The result is a density-dependent process operating to ultimately effect the production and production rate of breeding ducks on a continent-wide basis. Continental production, and therefore the size of the fall population, is probably partially regulated by the number of birds that are distributed north and northwest into environments less favorable for successful reproduction. Thus, spacing of the birds in the </span><i>Prairie-Parkland Area</i><span> and the movement of a fraction of the birds out of the prime breeding areas may be key factors in the density-dependent regulation of the total mallard population.</span></p>","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Pospahala, R.S., Anderson, D.R., and Henny, C.J., 1974, Population ecology of the mallard: II. Breeding habitat conditions, size of the breeding populations, and production indices: Resource Publication 115, iv, 73 p.","productDescription":"iv, 73 p.","numberOfPages":"78","costCenters":[],"links":[{"id":193124,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad6e4b07f02db683ef2","contributors":{"authors":[{"text":"Pospahala, Richard S.","contributorId":11677,"corporation":false,"usgs":true,"family":"Pospahala","given":"Richard","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":511196,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Anderson, David R.","contributorId":92722,"corporation":false,"usgs":true,"family":"Anderson","given":"David","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":511197,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Henny, Charles J. 0000-0001-7474-350X hennyc@usgs.gov","orcid":"https://orcid.org/0000-0001-7474-350X","contributorId":3461,"corporation":false,"usgs":true,"family":"Henny","given":"Charles","email":"hennyc@usgs.gov","middleInitial":"J.","affiliations":[{"id":289,"text":"Forest and Rangeland Ecosys Science Center","active":true,"usgs":true}],"preferred":true,"id":511195,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70112317,"text":"70112317 - 1974 - Optical data processing and projected applications of the ERTS-1 imagery covering the 1973 Mississippi River Valley floods","interactions":[],"lastModifiedDate":"2017-01-18T15:18:21","indexId":"70112317","displayToPublicDate":"1990-06-12T14:39:00","publicationYear":"1974","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3718,"text":"Water Resources Bulletin","printIssn":"0043-1370","active":true,"publicationSubtype":{"id":10}},"title":"Optical data processing and projected applications of the ERTS-1 imagery covering the 1973 Mississippi River Valley floods","docAbstract":"<p>Flooding along the Mississippi River and some of its tributaries was detected by the multispectral scanner (MSS) on the Earth Resources Technology Satellite (ERTS-1) on at least three orbits during the spring of 1973. The ERTS data provided the first opportunity for mapping the regional extent of flooding at the time of the imagery. Special optical data processing techniques were used to produce a variety of multispectral color composites enhancing flood-plain details. One of these, a 2-color composite of near infrared bands 6 and 7, was enlarged and registered to 1:250,000-scale topographic maps and used as the basis for preparation of flood image maps. Two specially filtered 3-color composites of MSS bands 5, 6, and 7 and 4, 5, and 7 were prepared to aid in the interpretation of the data. The extent of the flooding was vividly depicted on a single image by 2-color temporal composites produced on the additive-color viewer using band 7 flood data superimposed on pre-flood band 7 images. On May 24, when the floodwaters at St. Louis receded to bankfull stage, imagery was again obtained by ERTS. Analysis of temporal data composites of the pre-flood and post-flood band 7 images indicate that changes in surface reflectance characteristics caused by the flooding can be delineated, thus making it possible to map the overall area flooded without the necessity of a real-time system to track and image the peak flood waves. Regional planning and disaster relief agencies such as the Corps of Engineers, Office of Emergency Preparedness, Soil Conservation Service, interstate river basin commissions and state agencies, as well as private lending and insurance institutions, have indicated strong potential applications for ERTS image-maps of flood-prone areas.</p>","language":"English","publisher":"American Water Resources Association","publisherLocation":"Herndon, VA","doi":"10.1111/j.1752-1688.1974.tb00622.x","usgsCitation":"Deutsch, M., and Ruggles, F., 1974, Optical data processing and projected applications of the ERTS-1 imagery covering the 1973 Mississippi River Valley floods: Water Resources Bulletin, v. 10, no. 5, p. 1023-1039, https://doi.org/10.1111/j.1752-1688.1974.tb00622.x.","productDescription":"17 p.","startPage":"1023","endPage":"1039","numberOfPages":"17","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":288529,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1111/j.1752-1688.1974.tb00622.x"},{"id":288530,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","otherGeospatial":"Mississippi River","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -95.25,29.15 ], [ -95.25,47.5 ], [ -89.09,47.5 ], [ -89.09,29.15 ], [ -95.25,29.15 ] ] ] } } ] }","volume":"10","issue":"5","noUsgsAuthors":false,"publicationDate":"2007-06-08","publicationStatus":"PW","scienceBaseUri":"539acc0ce4b0e83db6d08f9a","contributors":{"authors":[{"text":"Deutsch, Morris","contributorId":69119,"corporation":false,"usgs":true,"family":"Deutsch","given":"Morris","email":"","affiliations":[],"preferred":false,"id":494663,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ruggles, Fred","contributorId":26973,"corporation":false,"usgs":true,"family":"Ruggles","given":"Fred","email":"","affiliations":[],"preferred":false,"id":494662,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70112316,"text":"70112316 - 1974 - Survey of remote sensing applications","interactions":[],"lastModifiedDate":"2022-03-30T18:10:11.452276","indexId":"70112316","displayToPublicDate":"1990-06-12T14:35:00","publicationYear":"1974","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3726,"text":"Water Well Journal","active":true,"publicationSubtype":{"id":10}},"title":"Survey of remote sensing applications","docAbstract":"<p>Data from the first earth resources technology satellite (ERTS) as well as from NASA and other aircraft, contain much of the information indicative of the distribution of groundwater and the extent of its utilization. Thermal infrared imagery from aircraft is particularly valuable in studying groundwater discharge to the sea and other surface water bodies. Color infrared photography from aircraft and space is also used to locate areas of potential groundwater development. Anomalies in vegetation, soils, moisture, and their pattern of distribution may be indicative of underlying groundwater conditions. Remote sensing may be used directly or indirectly to identify stream reaches for test holes or production wells. Similarly, location of submarine springs increase effectiveness of groundwater exploration in the coastal zone.</p>","language":"English","publisher":"National Water Well Association","publisherLocation":"Columbus, OH","usgsCitation":"Deutsch, M., 1974, Survey of remote sensing applications: Water Well Journal, v. 28, no. 7, p. 35-38.","productDescription":"4 p.","startPage":"35","endPage":"38","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":288528,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"28","issue":"7","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"539acc18e4b0e83db6d0900b","contributors":{"authors":[{"text":"Deutsch, Morris","contributorId":69119,"corporation":false,"usgs":true,"family":"Deutsch","given":"Morris","email":"","affiliations":[],"preferred":false,"id":494661,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70234306,"text":"70234306 - 1974 - Prediction of maximum earthquake intensities for the San Francisco Bay region","interactions":[],"lastModifiedDate":"2022-08-08T16:12:44.748867","indexId":"70234306","displayToPublicDate":"1976-04-01T10:40:24","publicationYear":"1974","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Prediction of maximum earthquake intensities for the San Francisco Bay region","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Wind and seismic effects: Proceedings of the sixth joint UJNR panel conference","largerWorkSubtype":{"id":12,"text":"Conference publication"},"language":"English","publisher":"U.S. Department of Commerce","usgsCitation":"Borcherdt, R.D., and Gibbs, J., 1974, Prediction of maximum earthquake intensities for the San Francisco Bay region, <i>in</i> Wind and seismic effects: Proceedings of the sixth joint UJNR panel conference, p. III-84-III-94.","productDescription":"11 p.","startPage":"III-84","endPage":"III-94","costCenters":[{"id":234,"text":"Earthquake Hazards Program","active":true,"usgs":true}],"links":[{"id":404916,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"San Francisco Bay area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -123.21716308593749,\n              36.74328605437939\n            ],\n            [\n              -120.750732421875,\n              36.74328605437939\n            ],\n            [\n              -120.750732421875,\n              38.522384090200845\n            ],\n            [\n              -123.21716308593749,\n              38.522384090200845\n            ],\n            [\n              -123.21716308593749,\n              36.74328605437939\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Borcherdt, Roger D. 0000-0002-8668-0849 borcherdt@usgs.gov","orcid":"https://orcid.org/0000-0002-8668-0849","contributorId":2373,"corporation":false,"usgs":true,"family":"Borcherdt","given":"Roger","email":"borcherdt@usgs.gov","middleInitial":"D.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":848518,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gibbs, James F.","contributorId":95880,"corporation":false,"usgs":true,"family":"Gibbs","given":"James F.","affiliations":[],"preferred":false,"id":848519,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70205111,"text":"70205111 - 1974 - Metallogenic provinces of southeastern Pacific region","interactions":[],"lastModifiedDate":"2019-09-03T14:57:21","indexId":"70205111","displayToPublicDate":"1976-01-01T14:50:54","publicationYear":"1974","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":606,"text":"AAPG Memoir","active":true,"publicationSubtype":{"id":10}},"title":"Metallogenic provinces of southeastern Pacific region","docAbstract":"<p>Metalliferous mineral deposits of the southeastern Pacific region include:<span>&nbsp;</span><strong>(1)</strong>hydrothermal, magmatic, and sedimentary deposits of the Andean region, one of the great mineral belts of the world;<span>&nbsp;</span><strong>(2)</strong><span>&nbsp;</span>scattered hydrothermal deposits in the Antarctic Peninsula; and<span>&nbsp;</span><strong>(3)</strong><span>&nbsp;</span>metal-enriched pelagic sediments and ferromanganese nodules on the seafloor. Andean metalliferous deposits, the chief topic of this report, are for the most part spatially and genetically related to calc-alkaline plutons, subvolcanic intrusions, and volcanic rocks emplaced during the Andean orogeny of Late Triassic to Quaternary age. They are components of a single metallogenic province superimposed on two or more pre-Andean metallogenic provinces of Paleozoic and Precambrian(?) age. Deposits in the Antarctic Peninsula are similar in age and origin to the deposits in the Andes and are considered to belong to the Andean province.</p><p>The Andean metallogenic province may be divided into several subprovinces, each parallel with the Andes and the continental margin and each having a dominant metal or suite of metals. The central Andes of Peru, northern Chile, and Bolivia, which contain the greatest concentration of exploitable deposits and the greatest variety of ore types, have as many as five linear, partly overlapping subprovinces. These subprovinces, from west to east (Pacific coast to the eastern Andean front), are characterized, respectively, by deposits of iron, copper, polymetallic base metals, tin, and gold.</p><p>Calc-alkaline plutonic and volcanic rocks of the Andes, which probably originated by partial melting in the Benioff zone, show a general, though nonuniform progression of decreasing age from west to east. Igneous rocks of Jurassic and Cretaceous age are most abundant near the coast, whereas those of Tertiary and Quaternary age dominate in the Andes. Locally, intrusive rocks and associated ore deposits of widely different ages are juxtaposed. Several sources of the metals are probable; they include oceanic crust and pelagic sediments in the Benioff zone, some of which may have been enriched previously in certain metals at the ancestral East Pacific Rise, and metal-rich zones in the overlying mantle and continental crust.</p>","language":"English","publisher":"GeoScienceWorld","usgsCitation":"Ericksen, G.E., 1974, Metallogenic provinces of southeastern Pacific region: AAPG Memoir, v. 25, p. 527-538.","productDescription":"12 p.","startPage":"527","endPage":"538","costCenters":[],"links":[{"id":367149,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":367148,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.geoscienceworld.org/books/book/1455/chapter/107175923/metallogenic-provinces-of-southeastern-pacific"}],"volume":"25","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Ericksen, George Edward","contributorId":38537,"corporation":false,"usgs":true,"family":"Ericksen","given":"George","email":"","middleInitial":"Edward","affiliations":[],"preferred":false,"id":770062,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70039203,"text":"70039203 - 1974 - EROS: A space program for Earth resources","interactions":[],"lastModifiedDate":"2017-06-05T21:55:56","indexId":"70039203","displayToPublicDate":"1976-01-01T12:01:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":362,"text":"General Information Product","active":false,"publicationSubtype":{"id":6}},"title":"EROS: A space program for Earth resources","docAbstract":"The EROS Program, administered by the U. S. Geological Survey, works with representatives of departmental bureaus and offices to coordinate research and application of remote-sensing technology to the day to-day operations of the department. Most of the research and applications have been made possible by the experimental data acquisition systems of the National Aeronautics and Space Administration (NASA). In particular, the EROS Program uses data from the Earth Resources Technology Satellite (ERTS), from the Earth Resources Experiment Package (EREP) of Skylab, and from NASA's Aircraft Program.","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/70039203","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1974, EROS: A space program for Earth resources: General Information Product, 3 p. (7 columns), https://doi.org/10.3133/70039203.","productDescription":"3 p. (7 columns)","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":261372,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gip/70039203/report.pdf"},{"id":261373,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gip/70039203/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0466e4b0c8380cd50966","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":535241,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70232500,"text":"70232500 - 1974 - Strain-gage measurements in Carlsbad Caverns, New Mexico","interactions":[],"lastModifiedDate":"2022-07-05T17:00:12.200208","indexId":"70232500","displayToPublicDate":"1975-05-01T11:40:09","publicationYear":"1974","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"Strain-gage measurements in Carlsbad Caverns, New Mexico","docAbstract":"<p>Displacement transducers installed on a near-vertical joint in the lunchroom in Carlsbad Caverns measured small movements along the joint with a resolution of 3.7X 10<sup>-6</sup> in (9.4X10<sup>-6</sup> cm). During 1973 the maximum annual displacement horizontally, vertically, and perpendicularly to the plane of the joint was 4.7X10<sup>-4</sup>, 4.0X10<sup>-4</sup>, and 1.1X10<sup>-4</sup> in (1.2X10<sup>-3</sup>, 1.0X10<sup>-3</sup>, and 2.8X10<sup>-4</sup> cm), respectively.</p>","language":"English","publisher":"U. S. Geological Survey","usgsCitation":"McLean, J.S., 1974, Strain-gage measurements in Carlsbad Caverns, New Mexico: Journal of Research of the U.S. Geological Survey, v. 3, no. 3, p. 281-283.","productDescription":"3 p.","startPage":"281","endPage":"283","costCenters":[],"links":[{"id":402987,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":402983,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1975/vol3issue3/report.pdf","size":"19104 KB","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"New Mexico","otherGeospatial":"Carlsbad Caverns","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -104.6619415283203,\n              32.06977442847062\n            ],\n            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       -104.68254089355469,\n              32.091882620021806\n            ],\n            [\n              -104.68254089355469,\n              32.0846107787884\n            ],\n            [\n              -104.68700408935547,\n              32.08402900649112\n            ],\n            [\n              -104.68528747558592,\n              32.04096758222761\n            ],\n            [\n              -104.67636108398438,\n              32.040676557717454\n            ],\n            [\n              -104.67567443847656,\n              32.04766089060862\n            ],\n            [\n              -104.66331481933594,\n              32.04736988737824\n            ],\n            [\n              -104.6619415283203,\n              32.06977442847062\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"3","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"McLean, J. S.","contributorId":116657,"corporation":false,"usgs":true,"family":"McLean","given":"J.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":845704,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70232498,"text":"70232498 - 1974 - Preliminary findings of a leachate study on two landfills in Suffolk County, New York","interactions":[],"lastModifiedDate":"2022-07-05T16:39:06.331896","indexId":"70232498","displayToPublicDate":"1975-05-01T11:20:07","publicationYear":"1974","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"Preliminary findings of a leachate study on two landfills in Suffolk County, New York","docAbstract":"<p>Plumes of leachate-enriched ground water extend 10,600 and 5,000 ft (3,200 and 1,500 m) downgradient from landfills in the towns of Babylon and Islip, respectively, and extend vertically beneath the landfills to the base of the upper glacial aquifer, whose thickness ranges from 71 to 77 ft (22-24 m) at the Babylon site and is 170 ft (52 m) at the Islip site. The Babylon and Islip landfills were started in 1947 and 1933, respectively. The quantities of ground water in the plumes are 2X10<sup>9</sup> gal (8X10<sup>6</sup> m<sup>3</sup>) at Babylon and 1X10<sup>9</sup> gal (4X10<sup>6</sup> m<sup>3</sup>) at Islip. Differences in quantity of water in the plumes and length of the plumes may result partly from a slower rate of refuse accumulation at Islip than at Babylon; however, the rate of travel for the front of the Islip plume is considerably less than the prevailing groundwater velocity would indicate. Distance traveled by the front of the Islip plume was roughly one-third the distance indicated by the calculated minimum ground-water velocity and may result from greater vertical travel distance in the upper glacial aquifer at Islip. Concentrations of HCO<sub>3</sub><sup>-</sup>, Cl<sup>-</sup>, and SO<sub>4</sub><sup>-</sup><sup>2</sup> in the leachate-enriched ground water are higher than those in ambient ground water. Concentrations of Fe and Mn in the plumes are as much as 400,000 <i><span>μ</span></i>g/1 and 200,000 <i><span>μ</span></i>g/1, but concentrations of other metals, including Zn (220 <i><span>μ</span></i>g/1), do not exceed the U.S. Public Health Service drinking-water standards. The concentration of NH<sub>4</sub><sup>+</sup>, the predominant nitrogen species in plume water, is usually more than 10 percent of the total cations in plume water and is greater than NH<sub>4</sub><sup>+</sup> concentrations in ambient ground water; concentrations of NO<sub>3</sub><sup>-</sup> in plume water are less than those in ambient ground water at Babylon and at some locations in Islip.</p>","language":"English","publisher":"U. S. Geological Survey","usgsCitation":"Kimmel, G.E., and Braids, O.C., 1974, Preliminary findings of a leachate study on two landfills in Suffolk County, New York: Journal of Research of the U.S. Geological Survey, v. 3, no. 3, p. 273-280.","productDescription":"8 p.","startPage":"273","endPage":"280","costCenters":[],"links":[{"id":402980,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":402979,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1975/vol3issue3/report.pdf","size":"19104 KB","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"New York","county":"Suffolk 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Grant E.","contributorId":20741,"corporation":false,"usgs":true,"family":"Kimmel","given":"Grant","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":845700,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Braids, Olin C.","contributorId":84368,"corporation":false,"usgs":true,"family":"Braids","given":"Olin","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":845701,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70232496,"text":"70232496 - 1974 - Upward migration of deep-well waste injection fluids in Floridan Aquifer, south Florida","interactions":[],"lastModifiedDate":"2022-07-05T16:17:14.83087","indexId":"70232496","displayToPublicDate":"1975-05-01T11:06:52","publicationYear":"1974","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"Upward migration of deep-well waste injection fluids in Floridan Aquifer, south Florida","docAbstract":"<p>Geochemical data from an industrial deep-well waste injection system southeast of Lake Okeechobee indicate a decrease in sulfate concentration concomitant with an increase in hydrogen sulfide concentration, a result of oxidation of injected organic waste by anaerobic bacteria. Subtle decreases in the sulfate-chloride ratio suggest that the waste migrated upward to a shallow monitor well about 27 mo after waste injection began and again within 15 mo of the resumption of waste injection after the injection well was deepened. The possibility of a hydraulic connection between the injection zone and overlying monitoring zone is implied. The decrease in the sulfate-chloride ratio appears to be a sensitive indicator of waste migration. Potential conflicts exist in the use of the Floridan aquifer for waste disposal and subsequent use as a natural resource.</p>","language":"English","publisher":"U. S. Geological Survey","usgsCitation":"Kaufman, M.I., and McKenzie, D., 1974, Upward migration of deep-well waste injection fluids in Floridan Aquifer, south Florida: Journal of Research of the U.S. Geological Survey, v. 3, no. 3, p. 261-271.","productDescription":"11 p.","startPage":"261","endPage":"271","costCenters":[],"links":[{"id":402976,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":402974,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1975/vol3issue3/report.pdf","size":"19104 KB","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Florida","city":"Belle Glade","otherGeospatial":"Lake Okeechobee","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -80.77903747558594,\n              26.59159724884548\n            ],\n            [\n              -80.50300598144531,\n              26.59159724884548\n            ],\n            [\n              -80.50300598144531,\n              26.820394161280475\n            ],\n            [\n              -80.77903747558594,\n              26.820394161280475\n            ],\n            [\n              -80.77903747558594,\n              26.59159724884548\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"3","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Kaufman, M. I.","contributorId":66847,"corporation":false,"usgs":true,"family":"Kaufman","given":"M.","email":"","middleInitial":"I.","affiliations":[],"preferred":false,"id":845697,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McKenzie, D.J.","contributorId":75134,"corporation":false,"usgs":true,"family":"McKenzie","given":"D.J.","email":"","affiliations":[],"preferred":false,"id":845698,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1700,"text":"otherFL74026 - 1974 - Water quality of Tampa Bay, Florida : dry-weather conditions, June 1971","interactions":[],"lastModifiedDate":"2012-06-27T01:01:43","indexId":"otherFL74026","displayToPublicDate":"1975-01-01T11:16:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"FL-74026","title":"Water quality of Tampa Bay, Florida : dry-weather conditions, June 1971","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/otherFL74026","usgsCitation":"Goodwin, C., Rosenshein, J.S., and Michaelis, D., 1974, Water quality of Tampa Bay, Florida : dry-weather conditions, June 1971: U.S. Geological Survey Open-File Report FL-74026, 85 p. :maps ;27 cm., https://doi.org/10.3133/otherFL74026.","productDescription":"85 p. :maps ;27 cm.","costCenters":[],"links":[{"id":204674,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bc8cde4b08c986b32caf9","contributors":{"authors":[{"text":"Goodwin, Carl R.","contributorId":76284,"corporation":false,"usgs":true,"family":"Goodwin","given":"Carl R.","affiliations":[],"preferred":false,"id":143988,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rosenshein, Joseph S.","contributorId":32904,"corporation":false,"usgs":true,"family":"Rosenshein","given":"Joseph","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":143986,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Michaelis, D.M.","contributorId":44896,"corporation":false,"usgs":true,"family":"Michaelis","given":"D.M.","email":"","affiliations":[],"preferred":false,"id":143987,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70232663,"text":"70232663 - 1974 - Geometry and growth of the White Sands dune field, New Mexico","interactions":[],"lastModifiedDate":"2022-07-11T15:37:37.174588","indexId":"70232663","displayToPublicDate":"1975-01-01T10:33:09","publicationYear":"1974","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"Geometry and growth of the White Sands dune field, New Mexico","docAbstract":"<p>Recent studies of the cores from four drill holes at the White Sands dune field in New Mexico demonstrated that the eolian sand body below the present active dunes ranges in thickness from 23 to 34 ft in the area tested. It consists of one to two older generations of dune and associated interdune deposits, which rest on playa and fluvial deposits. Relatively thick sheets of clean, well-sorted dune sand are separated from one another by thin zones of darker colored interdune deposits. In vertical sections of test trenches and in cores, these interdune deposits appear as thin zones of tan or buff, poorly sorted, subparallel strata between relatively thick units of white cross-stratified sand. The interdune deposits are buried by the advancing foresets of the encroaching dunes and their thickness is limited by the time of exposure. The subsurface dune deposits are relatively thin as compared to the active surface dunes. This difference in thickness apparently results from the beveling or truncation of dunes by the migration of interdune areas.</p>","language":"English","publisher":"U.S. Geological Survey","usgsCitation":"McKee, E.D., and Moiola, R.J., 1974, Geometry and growth of the White Sands dune field, New Mexico: Journal of Research of the U.S. Geological Survey, v. 3, no. 1, p. 59-66.","productDescription":"8 p.","startPage":"59","endPage":"66","costCenters":[],"links":[{"id":403391,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":403390,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1975/vol3issue1/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"New Mexico","otherGeospatial":"Lake Lucero, White Sands dune field","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -106.48292541503906,\n              32.65267275602318\n            ],\n            [\n              -106.14715576171875,\n              32.65267275602318\n            ],\n            [\n              -106.14715576171875,\n              32.87036022808352\n            ],\n            [\n              -106.48292541503906,\n              32.87036022808352\n            ],\n            [\n              -106.48292541503906,\n              32.65267275602318\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"3","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"McKee, Edwin D.","contributorId":60207,"corporation":false,"usgs":true,"family":"McKee","given":"Edwin","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":846208,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Moiola, Richard J.","contributorId":82793,"corporation":false,"usgs":true,"family":"Moiola","given":"Richard","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":846209,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70232660,"text":"70232660 - 1974 - Stratigraphic relationships within the Baraga Group of Precambrian age, central Upper Peninsula, Michigan","interactions":[],"lastModifiedDate":"2022-07-11T15:27:31.051675","indexId":"70232660","displayToPublicDate":"1975-01-01T10:24:50","publicationYear":"1974","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"Stratigraphic relationships within the Baraga Group of Precambrian age, central Upper Peninsula, Michigan","docAbstract":"<p>Details of the stratigraphic section in parts of northern Michigan have been known for many years, but correlation of units between geographically separated areas has been partly speculative. Mapping in the Witch Lake quadrangle has filled the gap between well-studied areas of the Marquette trough and parts of Iron and Dickinson Counties and has helped to correlate units in the Baraga Group (Precambrian X). Iron-formations are important marker beds; because of their magnetic properties they can be traced with certainty through poorly exposed areas. The magnetic Fence River Formation is now known to be stratigraphically beneath the Bijiki Iron-formation Member of the Michigamme Formation but may be equivalent to the Greenwood Iron-formation Member which crops out in parts of the Marquette trough to the east The Hemlock Formation (volcanic) underlies the Fence River and has been traced from near its type locality in Iron County to the south flank of the Marquette trough. These relationships provide the key to understanding the lateral facies changes responsible for the stratigraphic complexities of the Baraga Group.</p>","language":"English","publisher":"U.S. Geological Survey","usgsCitation":"Cannon, W., and Klasner, J.S., 1974, Stratigraphic relationships within the Baraga Group of Precambrian age, central Upper Peninsula, Michigan: Journal of Research of the U.S. Geological Survey, v. 3, no. 1, p. 47-51.","productDescription":"5 p.","startPage":"47","endPage":"51","costCenters":[],"links":[{"id":403385,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1975/vol3issue1/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":403386,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Michigan","otherGeospatial":"central Upper Peninsula","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -88.1982421875,\n              45.729191061299915\n            ],\n            [\n              -86.66015624999999,\n              45.729191061299915\n            ],\n            [\n              -86.66015624999999,\n              46.6268063953552\n            ],\n            [\n              -88.1982421875,\n              46.6268063953552\n            ],\n            [\n              -88.1982421875,\n              45.729191061299915\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"3","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Cannon, W.F. 0000-0002-2699-8118","orcid":"https://orcid.org/0000-0002-2699-8118","contributorId":70382,"corporation":false,"usgs":true,"family":"Cannon","given":"W.F.","affiliations":[],"preferred":false,"id":846204,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Klasner, John S.","contributorId":46591,"corporation":false,"usgs":true,"family":"Klasner","given":"John","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":846205,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70207477,"text":"70207477 - 1974 - Chemical analyses of Red Sea sediments","interactions":[],"lastModifiedDate":"2019-12-19T18:34:36","indexId":"70207477","displayToPublicDate":"1974-12-31T18:34:05","publicationYear":"1974","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1997,"text":"Initial reports of the Deep Sea Drilling Project","active":true,"publicationSubtype":{"id":10}},"title":"Chemical analyses of Red Sea sediments","docAbstract":"<p>One of the prime motives for exploring the deeper subsurface sediments of the Red Sea floor was to gain information on the geochemical systems controlling the hot brine-metalliferous deposits. Accordingly, a strong effort was made to provide both shipboard and laboratory means of analysis of the recovered phases. Shipboard spectrographic analyses (semiquantitative) provided both detailed surveys of chemical properties of the cores and the ability to analyze small subsamples and separated particles such as pyrite, sphalerite, organisms, and similar minute objects. Over 5000 such analyses are provided in Tables 1 to 5. Some supplementary data provided by subsequent analyses for K, Zn, and Ag in the Denver field laboratories of the U. S. Geological Survey have been added to the tables. </p><p><br>A second body of data is provided in Table 6, which gives quantitative data on major and minor constituents, performed by the Washington analytical laboratories of the U. S. Geological Survey. A third group of analyses are partial analyses on evaporitic rocks (anhydrite and rock salt) (Table 18, in Manheim Chapter 38, this volume). In addition to the above, a number of the collaborating laboratories are providing more specific chemical data on special phases and constituents of the Red Sea materials. Most of these data are included in chapters in the Geochemical section of this volume. The significance of the data is discussed in Manheim (Chapter 38, this volume) and in the respective reports of shipboard workers and cooperating share laboratories. </p>","language":"English","publisher":"National Science Foundation","doi":"10.2973/dsdp.proc.23.129.1974","usgsCitation":"Manheim, F.T., and Siems, D.E., 1974, Chemical analyses of Red Sea sediments: Initial reports of the Deep Sea Drilling Project, v. 23, p. 923-938, https://doi.org/10.2973/dsdp.proc.23.129.1974.","productDescription":"16 p.","startPage":"923","endPage":"938","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":488845,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"http://doi.org/10.2973/dsdp.proc.23.129.1974","text":"Publisher Index Page"},{"id":370536,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Red Sea","geographicExtents":"{\n  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]\n}","volume":"23","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Manheim, Frank T. 0000-0003-4005-4524","orcid":"https://orcid.org/0000-0003-4005-4524","contributorId":20770,"corporation":false,"usgs":true,"family":"Manheim","given":"Frank","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":778193,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Siems, David E.","contributorId":221432,"corporation":false,"usgs":false,"family":"Siems","given":"David","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":778194,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70207476,"text":"70207476 - 1974 - Red Sea geochemistry","interactions":[],"lastModifiedDate":"2019-12-19T18:26:08","indexId":"70207476","displayToPublicDate":"1974-12-31T18:17:09","publicationYear":"1974","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1997,"text":"Initial reports of the Deep Sea Drilling Project","active":true,"publicationSubtype":{"id":10}},"title":"Red Sea geochemistry","docAbstract":"<p>The Red Sea drillings reveal a number of new facets of the hot-brine-metalliferous system and other geochemical aspects of the sea, its sediments, and its past history as follows: </p><p>1) Dark shales rich in organic material, and containing enhanced Mo and V concentrations, are characteristic of Plio-Pleistocene strata in the Red Sea. Values as high as 1500 ppm V and 500 ppm Mo were obtained in sediments containing up to 8 percent organic carbon. </p><p>2) Metalliferous sediments in the hot brine deep (Site 226) are similar in composition in both solids and interstitial water to previously analyzed sediments. However, one site (228) well south of the known hot-brine deeps shows zinc mineralization reaching 5 percent Zn in late Miocene shale-anhydrite breccias. </p><p>3) Pore fluid studies show that near-saturated (NaCl) brines having similar total salt concentration to the hot-brine fluids are associated with Miocene evaporites at Sites 225, 227, and 228. However, their chemical and isotopic composition precludes such fluids being part of the \"hot brine plumbing system.\" Hydrogen and oxygen isotope studies demonstrate that fluids trapped between and among the evaporitic rocks have a strong meteoric water component, presumed to have entered the rocks during or shortly after formation in shallow evaporating pans. The composition of pore fluid at Site 227 suggests the presence of late-stage evaporite minerals of the tachyhydrite CaMg<sub>2</sub>Cl<sub>6</sub> • 12H<sub>2</sub>O series in the in situ rocks. </p><p>4) Diffusivity measurements show that the pre-Miocene strata permit dissolved salt or gas diffusion to the extent of from 1/2 to about 1/10 the rate in free solution. However, in anhydrites diffusivity is reduced more than 100-fold, and no diffusion could be detected through halite rock. The rates applied to interstitial salt gradients at Site 225 suggest that less than 1 meter of rock salt is removed per million years by diffusion processes. The diffusion of salt can already be detected a few meters below the sediment-water interface, and based on the interstitial water studies, one can affirm the presence of salt at depth at Sites 228, 230, and possibly 229, where rock salt was not encountered by the drill. </p><p>5) Isotopic measurements on leads show that both leads from Site 228 and the hot brine deep (Site 226) require input from igneous or volcanic sources (e.g., volcanic ash). Elsewhere, however, leads of sedimentary-pelagic origin are noted. </p><p>6) Isotopic and other evidence indicates that the long-distance transport of subterranean brines advocated by Craig (1969) is unlikely. Instead, it is proposed that the source of the hot brines is subevaporite clastic or other aquifers of early to middle Miocene age that have been disrupted by rifting. These discharge in the deeps by virtue of hydrodynamic continuity with heavy brines at higher positions on the nearby flanks of the Red Sea. In this case, the waters might be fossil (middle Miocene) Red Sea waters of relatively normal salinity that have acquired greater salt concentration by diffusion from overlying late Miocene evaporites. The model is consistent with the isolated nature of the brine deeps and suggests that flow might have been enhanced by increased hydraulic gradients during periods of lowered Red Sea levels. </p><p>7) Interstitial water evidence indicates that Pleistocene lowerings of sea level did not cause evaporative conditions leading to actual gypsum or other evaporite deposition in the deeper water zones, as has been postulated. This in turn suggests that sill depths were greater than have been assumed.</p>","language":"English","publisher":"National Science Foundation","doi":"10.2973/dsdp.proc.23.138.1974","usgsCitation":"Manheim, F.T., 1974, Red Sea geochemistry: Initial reports of the Deep Sea Drilling Project, v. 23, p. 975-998, https://doi.org/10.2973/dsdp.proc.23.138.1974.","productDescription":"24 p.","startPage":"975","endPage":"998","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":488224,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.2973/dsdp.proc.23.138.1974","text":"Publisher Index Page"},{"id":370535,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Red Sea","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      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0000-0003-4005-4524","orcid":"https://orcid.org/0000-0003-4005-4524","contributorId":20770,"corporation":false,"usgs":true,"family":"Manheim","given":"Frank","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":778192,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70207475,"text":"70207475 - 1974 - Interstitial water studies on small core samples, leg 23 (Red Sea)","interactions":[],"lastModifiedDate":"2019-12-20T07:07:40","indexId":"70207475","displayToPublicDate":"1974-12-31T18:11:48","publicationYear":"1974","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1997,"text":"Initial reports of the Deep Sea Drilling Project","active":true,"publicationSubtype":{"id":10}},"title":"Interstitial water studies on small core samples, leg 23 (Red Sea)","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"National Science Foundation","doi":"10.2973/dsdp.proc.23.135.1974","usgsCitation":"Manheim, F.T., Waterman, L., Woo, C.C., and Sayles, F., 1974, Interstitial water studies on small core samples, leg 23 (Red Sea): Initial reports of the Deep Sea Drilling Project, v. 23, p. 955-967, 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L.S.","contributorId":25474,"corporation":false,"usgs":true,"family":"Waterman","given":"L.S.","affiliations":[],"preferred":false,"id":778189,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Woo, Ching Chang","contributorId":91126,"corporation":false,"usgs":true,"family":"Woo","given":"Ching","email":"","middleInitial":"Chang","affiliations":[],"preferred":false,"id":778190,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Sayles, F.L.","contributorId":77657,"corporation":false,"usgs":true,"family":"Sayles","given":"F.L.","email":"","affiliations":[],"preferred":false,"id":778191,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70156528,"text":"70156528 - 1974 - Evidence for the presence of a heart in Paleozoic ostracodes inconclusive","interactions":[],"lastModifiedDate":"2015-08-24T13:29:56","indexId":"70156528","displayToPublicDate":"1974-12-31T17:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"Evidence for the presence of a heart in Paleozoic ostracodes inconclusive","docAbstract":"<p>The presence of a heart in some Paleozoic ostracodes has been inferred by analogy with some living myodocopids that have this organ, and an ordinal classification of the leperditiids has been proposed because of this inference. A review of the present knowledge of the internal shell structure of living myodocopids indicates that there is no basis for interpreting certain markings preserved on fossil molds and steinkerns as indicating the presence of a heart.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","usgsCitation":"Sohn, I.G., 1974, Evidence for the presence of a heart in Paleozoic ostracodes inconclusive: Journal of Research of the U.S. Geological Survey, v. 2, no. 6, p. 723-726.","productDescription":"4 p.","startPage":"723","endPage":"726","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":307250,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":307248,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1974/vol2issue6/report.pdf","text":"Report","size":"16.19 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"volume":"2","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"55dc402ee4b0518e354d10fd","contributors":{"authors":[{"text":"Sohn, I. G.","contributorId":70751,"corporation":false,"usgs":true,"family":"Sohn","given":"I.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":569407,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70156523,"text":"70156523 - 1974 - Redescription of the Early Cambrian <i>Helenia bella</i> Walcott, an appendage of <i>Hyolithes</i>","interactions":[],"lastModifiedDate":"2015-08-24T12:22:07","indexId":"70156523","displayToPublicDate":"1974-12-31T17:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"Redescription of the Early Cambrian <i>Helenia bella</i> Walcott, an appendage of <i>Hyolithes</i>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","usgsCitation":"Yochelson, E.L., 1974, Redescription of the Early Cambrian <i>Helenia bella</i> Walcott, an appendage of <i>Hyolithes</i>: Journal of Research of the U.S. Geological Survey, v. 2, no. 6, p. 717-722.","productDescription":"6 p.","startPage":"717","endPage":"722","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":307237,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":307236,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1974/vol2issue6/report.pdf","text":"Report","size":"16.19 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"volume":"2","issue":"6","tableOfContents":"<p>In accordance with the suggestion of Howell and Stubblefield and subsequent workers, <em>Helenia</em> has been reinterpreted as a hyolithid appendage. Isolated specimens of the Early Cambrian <em>H. bella</em> Walcott are flattened, are bladelike in cross section, and have an elaborate, irregular ornament covering both surfaces. The specimens are strongly arched and slightly twisted in the third dimension. Presumably these were paired structures which extended outward from openings between the shell and the operculum of the hyolithid and curved down to touch the substrate midway along their length and then upward and posteriorward at the tips. As suggested earlier, their prime function was to provide lateral stability. There is no obvious way that these appendages could have played a major role in locomotion. However, the upper edges of the appendages could have acted as a fulcrum for the operculum; contraction of small muscles running between the operculum and the appendages assisted the ventral part of the operculum to swing upward.</p>","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"55dc4031e4b0518e354d1119","contributors":{"authors":[{"text":"Yochelson, Ellis L.","contributorId":90802,"corporation":false,"usgs":true,"family":"Yochelson","given":"Ellis","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":569383,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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