{"pageNumber":"5027","pageRowStart":"125650","pageSize":"25","recordCount":184617,"records":[{"id":70135820,"text":"70135820 - 1985 - Rapid postglacial shoreline changes in the western Gulf of Maine and the Paleo-Indian environment","interactions":[],"lastModifiedDate":"2017-09-19T09:19:08","indexId":"70135820","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":700,"text":"American Antiquity","active":true,"publicationSubtype":{"id":10}},"title":"Rapid postglacial shoreline changes in the western Gulf of Maine and the Paleo-Indian environment","docAbstract":"<p><span>Rapid shoreline regression and transgression along the western Gulf of Maine between 13,000 and 9000 years B.P. are inferred to have produced a nearshore marine environment low in biologic productivity. Paleo-Indians living near the coast of the Gulf were probably forced to rely on nonmarine resources landward of the late-glacial marine limit. Thus, Paleo-Indian sites of the time period in question may be restricted in the region between the marine limit and the postglacial low sea-level stand, or may be altogether absent.</span></p>","language":"English","publisher":"Society for American Archaeology","usgsCitation":"Oldale, R.N., 1985, Rapid postglacial shoreline changes in the western Gulf of Maine and the Paleo-Indian environment: American Antiquity, v. 50, no. 1, p. 145-150.","productDescription":"6 p.","startPage":"145","endPage":"150","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true},{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":296772,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":296771,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.jstor.org/stable/280640"}],"country":"United States","otherGeospatial":"Gulf of Maine","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -67.203369140625,\n              45.058001435398296\n            ],\n            [\n              -70.718994140625,\n              43.715534726205114\n            ],\n            [\n              -71.070556640625,\n              41.52502957323801\n            ],\n            [\n              -65.8740234375,\n              43.96119063892024\n            ],\n            [\n              -67.203369140625,\n              45.058001435398296\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"50","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5492b747e4b00eda8915ad2d","contributors":{"authors":[{"text":"Oldale, Robert N.","contributorId":38953,"corporation":false,"usgs":true,"family":"Oldale","given":"Robert","email":"","middleInitial":"N.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":536911,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70164351,"text":"70164351 - 1985 - Recent volcano monitoring in Costa Rica","interactions":[],"lastModifiedDate":"2016-03-21T15:42:05","indexId":"70164351","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1435,"text":"Earthquake Information Bulletin (USGS)","active":true,"publicationSubtype":{"id":10}},"title":"Recent volcano monitoring in Costa Rica","docAbstract":"<p>The Costa Rican volacno Rincon de la Vieja is loosely but mysteriously translated as the \"Old Lady's Corner.\" It consists of six volcanic centers that form a remote elongated ridge standing some 1300m above the surrounding terraine. Geologically speaking, the Guanacaste province of northern Costa Rica consists of a series of composite volcanic cones built on a shield of ignimbrites (welded and unwelded ash flows) of Pliocene-Pleistocene age (up to 2 million years old), that themselves lie on basement crust of Cretaceious-Tertiary age (up to 90 million years old). the active volcanoes are aligned on a northwest-southeast axis parallel to the Middle American oceanic trench in the Pacific Ocean that is the site of subduction of hte Cocos oceanic plate underneath Central America. &nbsp;</p>","language":"English","publisher":"U.S Geological Survey","usgsCitation":"Thorpe, R., Brown, G., Rymer, H., Barritt, S., and Randal, M., 1985, Recent volcano monitoring in Costa Rica: Earthquake Information Bulletin (USGS), v. 17, no. 2, p. 44-49.","productDescription":"6 p.","startPage":"44","endPage":"49","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":316428,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Costa Rica","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -85.3634262084961,\n              10.840724382155452\n            ],\n            [\n              -85.31158447265624,\n              10.850502899153025\n            ],\n            [\n              -85.2975082397461,\n              10.803967790000689\n            ],\n            [\n              -85.34351348876953,\n              10.793513257694597\n            ],\n            [\n              -85.3634262084961,\n              10.840724382155452\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"17","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56b08fe6e4b010e2af2a5e01","contributors":{"authors":[{"text":"Thorpe, R.","contributorId":156262,"corporation":false,"usgs":false,"family":"Thorpe","given":"R.","affiliations":[],"preferred":false,"id":597088,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brown, G.","contributorId":83293,"corporation":false,"usgs":true,"family":"Brown","given":"G.","affiliations":[],"preferred":false,"id":597089,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rymer, H.","contributorId":87763,"corporation":false,"usgs":true,"family":"Rymer","given":"H.","email":"","affiliations":[],"preferred":false,"id":597090,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Barritt, S.","contributorId":156263,"corporation":false,"usgs":false,"family":"Barritt","given":"S.","email":"","affiliations":[],"preferred":false,"id":597091,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Randal, M.","contributorId":156264,"corporation":false,"usgs":false,"family":"Randal","given":"M.","email":"","affiliations":[],"preferred":false,"id":597092,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70012813,"text":"70012813 - 1985 - Geochemistry: Uses for synthetic fluid inclusions in quartz crystals","interactions":[],"lastModifiedDate":"2012-03-12T17:18:43","indexId":"70012813","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2840,"text":"Nature","active":true,"publicationSubtype":{"id":10}},"title":"Geochemistry: Uses for synthetic fluid inclusions in quartz crystals","docAbstract":"[No abstract available]","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Nature","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1038/315544b0","issn":"00280836","usgsCitation":"Roedder, E., 1985, Geochemistry: Uses for synthetic fluid inclusions in quartz crystals: Nature, v. 315, no. 6020, p. 544-545, https://doi.org/10.1038/315544b0.","startPage":"544","endPage":"545","numberOfPages":"2","costCenters":[],"links":[{"id":205284,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1038/315544b0"},{"id":222680,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"315","issue":"6020","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a172ee4b0c8380cd553f8","contributors":{"authors":[{"text":"Roedder, E.","contributorId":100986,"corporation":false,"usgs":true,"family":"Roedder","given":"E.","affiliations":[],"preferred":false,"id":364593,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70012774,"text":"70012774 - 1985 - A seismic-refraction profile across the San Andreas, Sargent, and Calaveras faults, west-central California","interactions":[],"lastModifiedDate":"2023-10-29T15:27:51.981468","indexId":"70012774","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1135,"text":"Bulletin of the Seismological Society of America","onlineIssn":"1943-3573","printIssn":"0037-1106","active":true,"publicationSubtype":{"id":10}},"title":"A seismic-refraction profile across the San Andreas, Sargent, and Calaveras faults, west-central California","docAbstract":"<p>In 1981, the United States Geological Survey recorded a seismic-refraction profile across the southern Santa Cruz Mountains in west-central California to examine the shallow velocity structure of this seismogenic region. This 40-km-long profile, which consisted of three shotpoints, extended northeastward from near Watsonville, California, to Coyote Lake, crossing the San Andreas, Sargent, and Calaveras faults. This entire region is characterized by a highly heterogeneous upper crust. West of Watsonville, 1 km of alluvium with a velocity of 2.12 km/sec overlies a basement with a velocity 5.45 km/sec. The abrupt deepening of basement by 1.5 km just east of Watsonville at a subsurface fault suggests that the Zayante fault to the north and the Vergeles fault to the south are connected. The Tertiary sediment at the San Andreas fault is 2.5 km thick and has a velocity of 3.34 km/sec. The San Andreas fault is not marked by any distinctive seismic velocity features, whereas a 1-km-wide low velocity zone is found at both the Sargent and Calaveras faults. East of the Sargent fault, the basement surface forms a broad anticlinal structure, with velocities ranging from 5.4 to 6.0 km/sec. From the anticlinal crest, basement dips to the east beneath the Santa Clara Valley and reaches a maximum depth of 1 km on the east side; the overlying alluvium has a velocity of 2.7 km/sec. At the crest of the basement anticlinal structure, a vertical low-velocity zone coincident with exposed serpentine provides strong evidence of faulting.</p>","language":"English","publisher":"Seismological Society of America","doi":"10.1785/BSSA0750010175","issn":"00371106","usgsCitation":"Mooney, W.D., and Colburn, R.H., 1985, A seismic-refraction profile across the San Andreas, Sargent, and Calaveras faults, west-central California: Bulletin of the Seismological Society of America, v. 75, no. 1, p. 175-191, https://doi.org/10.1785/BSSA0750010175.","productDescription":"17 p.","startPage":"175","endPage":"191","numberOfPages":"17","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"links":[{"id":374998,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.geoscienceworld.org/ssa/bssa/article/75/1/175/118661/A-seismic-refract"},{"id":221971,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -122.34924316406251,\n              36.40359962073253\n            ],\n            [\n              -120.41839599609375,\n              36.40359962073253\n            ],\n            [\n              -120.41839599609375,\n              37.17126017626408\n            ],\n            [\n              -122.34924316406251,\n              37.17126017626408\n            ],\n            [\n              -122.34924316406251,\n              36.40359962073253\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"75","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505aaf2be4b0c8380cd8740e","contributors":{"authors":[{"text":"Mooney, Walter D. 0000-0002-5310-3631 mooney@usgs.gov","orcid":"https://orcid.org/0000-0002-5310-3631","contributorId":3194,"corporation":false,"usgs":true,"family":"Mooney","given":"Walter","email":"mooney@usgs.gov","middleInitial":"D.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":364494,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Colburn, Robert H.","contributorId":75275,"corporation":false,"usgs":true,"family":"Colburn","given":"Robert","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":364495,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70012731,"text":"70012731 - 1985 - Precambrian tholeiitic-dacitic rock-suites and Cambrian ultramafic rocks in the Pennine nappe system of the Alps: Evidence from Sm-Nd isotopes and rare earth elements","interactions":[],"lastModifiedDate":"2012-03-12T17:19:02","indexId":"70012731","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1336,"text":"Contributions to Mineralogy and Petrology","active":true,"publicationSubtype":{"id":10}},"title":"Precambrian tholeiitic-dacitic rock-suites and Cambrian ultramafic rocks in the Pennine nappe system of the Alps: Evidence from Sm-Nd isotopes and rare earth elements","docAbstract":"Major element, trace element and Sm-Nd isotope analyses were made of polymetamorphic hornblendefelses, plagioclase amphibolites and banded amphibolites from the Berisal complex in the Simplon area (Italy, Switzerland) to determine their age, origin and genetic relationships. In light of major and rare earth element data, the hornblendefelses are inferred to have originally been pyroxene-rich cumulates, the plagioclase amphibolites and the dark layers of the banded amphibolites to have been tholeiitic basalts and the light layers dacites. The Sm-Nd isotope data yield isochron ages of 475??81 Ma for the hornblendefelses, 1,018??59 Ma for the plagioclase amphibolites and 1,071??43 Ma for the banded amphibolites. The 1 Ga magmatic event is the oldest one ever found in the crystalline basement of the Pennine nappes. The Sm -Nd isotope data support the consanguinity of the tholeiitic dark layers and the dacitic light layers of the banded amphibolites with the tholeiitic plagioclase amphibolites and the ultramafic hornblendefelses. The initial e{open}Nd values indicate that all three rock types originated from sources depleted in light rare earth elements. We suggest that plagioclase and banded amphibolites were a Proterozoic tholeiite-dacite sequence that was strongly deformed and flattened during subsequent folding. The hornblendefelses are thought to be Cambrian intrusions of pyroxene-rich material. ?? 1985 Springer-Verlag.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Contributions to Mineralogy and Petrology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisherLocation":"Springer-Verlag","doi":"10.1007/BF00379452","issn":"00107999","usgsCitation":"Stille, P., and Tatsumoto, M., 1985, Precambrian tholeiitic-dacitic rock-suites and Cambrian ultramafic rocks in the Pennine nappe system of the Alps: Evidence from Sm-Nd isotopes and rare earth elements: Contributions to Mineralogy and Petrology, v. 89, no. 2-3, p. 184-192, https://doi.org/10.1007/BF00379452.","startPage":"184","endPage":"192","numberOfPages":"9","costCenters":[],"links":[{"id":205225,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF00379452"},{"id":222321,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"89","issue":"2-3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a8108e4b0c8380cd7b324","contributors":{"authors":[{"text":"Stille, P.","contributorId":70113,"corporation":false,"usgs":true,"family":"Stille","given":"P.","email":"","affiliations":[],"preferred":false,"id":364378,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tatsumoto, M.","contributorId":76798,"corporation":false,"usgs":true,"family":"Tatsumoto","given":"M.","email":"","affiliations":[],"preferred":false,"id":364379,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70180826,"text":"70180826 - 1985 - Assessment of the fisheries and limnology in Lake F.D. Roosevelt, 1980-1983","interactions":[],"lastModifiedDate":"2017-02-03T14:00:36","indexId":"70180826","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"title":"Assessment of the fisheries and limnology in Lake F.D. Roosevelt, 1980-1983","docAbstract":"<p>No abstract available&nbsp;</p>","language":"English","publisher":"U.S. Bureau of Reclamation","usgsCitation":"Terrell, T., 1985, Assessment of the fisheries and limnology in Lake F.D. Roosevelt, 1980-1983.","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":334708,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5895a4d6e4b0fa1e59bc1ee9","contributors":{"authors":[{"text":"Terrell, T.T.","contributorId":61871,"corporation":false,"usgs":true,"family":"Terrell","given":"T.T.","email":"","affiliations":[],"preferred":false,"id":662532,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70012742,"text":"70012742 - 1985 - Depositional Relations of Umpqua and Tyee Formations (Eocene), Southwestern Oregon","interactions":[],"lastModifiedDate":"2023-01-12T16:31:10.379486","indexId":"70012742","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":701,"text":"American Association of Petroleum Geologists Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Depositional Relations of Umpqua and Tyee Formations (Eocene), Southwestern Oregon","docAbstract":"<p>Studies of the depositional relations of the Umpqua and Tyee Formations (Eocene) in southwestern Oregon indicate a need for reassessing the correlations and currently used terminology. The Umpqua Formation (as herein restricted) consists of as much as 10,000 ft (3,000 m) of mudstone, sandstone, and conglomerate of nonmarine to deep marine origin. A basaltic basement that underlies the sedimentary rocks in most of the area and was formerly included in the Umpqua is herein considered a separate unit and assigned to the Siletz River Volcanics. A proposal to subdivide the Umpqua into three unconformity-bounded formations (in ascending order: Roseburg, Lookingglass, and Flournoy Formations) in the area west of Roseburg, Oregon, is not recognized in this report because of quest onable correlations and limited extent of some units. Foremost of these questionable correlations is that of the Flournoy Formation with rocks formerly assigned to the Tyee Formation in areas as far north as the latitude of Salem, Oregon. My investigations of depositional facies and lithologic criteria do not substantiate this correlation.</p><p>The Tyee Formation, which conformably overlies the Umpqua, is a predominantly sandstone unit about 6,000 ft (1,800 m) thick, deposited in environments ranging from shallow marine and nonmarine deltaic on the south, to slope and deep marine basinal to the north. Deposition across the Umpqua-Tyee boundary contact represents a change in tectonic setting from active plate margin of the Umpqua to more stable marginal basin deposition of the Tyee. This change is also reflected in a change in provenance as indicated by the characteristic arkosic and micaceous aspects of Tyee sandstones.</p>","language":"English","publisher":"American Association of Petroleum Geologists","doi":"10.1306/AD462BB9-16F7-11D7-8645000102C1865D","usgsCitation":"Molenaar, C.M., 1985, Depositional Relations of Umpqua and Tyee Formations (Eocene), Southwestern Oregon: American Association of Petroleum Geologists Bulletin, v. 69, no. 8, p. 1217-1229, https://doi.org/10.1306/AD462BB9-16F7-11D7-8645000102C1865D.","productDescription":"13 p.","startPage":"1217","endPage":"1229","numberOfPages":"13","costCenters":[],"links":[{"id":222494,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Oregon","otherGeospatial":"Umpqua and Tyee Formations","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -124.61573884056492,\n              44.09401586800607\n            ],\n            [\n              -124.61573884056492,\n              42.38533872872969\n            ],\n            [\n              -121.9551006063869,\n              42.38533872872969\n            ],\n            [\n              -121.9551006063869,\n              44.09401586800607\n            ],\n            [\n              -124.61573884056492,\n              44.09401586800607\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"69","issue":"8","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059fd40e4b0c8380cd4e705","contributors":{"authors":[{"text":"Molenaar, C. M.","contributorId":77904,"corporation":false,"usgs":false,"family":"Molenaar","given":"C.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":364405,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70012768,"text":"70012768 - 1985 - Detectability of step trends in the rate of atmospheric deposition of sulfate","interactions":[],"lastModifiedDate":"2012-03-12T17:19:03","indexId":"70012768","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","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":"Detectability of step trends in the rate of atmospheric deposition of sulfate","docAbstract":"[No abstract available]","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Water Resources Bulletin","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"00431370","usgsCitation":"Hirsch, R., and Gilroy, E., 1985, Detectability of step trends in the rate of atmospheric deposition of sulfate: Water Resources Bulletin, v. 21, no. 5, p. 773-784.","startPage":"773","endPage":"784","numberOfPages":"12","costCenters":[],"links":[{"id":221848,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"21","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059ff5ce4b0c8380cd4f144","contributors":{"authors":[{"text":"Hirsch, R.M.","contributorId":58639,"corporation":false,"usgs":true,"family":"Hirsch","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":364473,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gilroy, E.J.","contributorId":20306,"corporation":false,"usgs":true,"family":"Gilroy","given":"E.J.","affiliations":[],"preferred":false,"id":364472,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70012735,"text":"70012735 - 1985 - A new look at deep-sea video","interactions":[],"lastModifiedDate":"2023-09-25T15:48:41.459674","indexId":"70012735","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1369,"text":"Deep Sea Research Part A, Oceanographic Research Papers","active":true,"publicationSubtype":{"id":10}},"title":"A new look at deep-sea video","docAbstract":"<p>A deep-towed photographic system with completely self-contained recording instrumentation and power can obtain color-video and still-photographic transects along rough terrane without need for a long electrically conducting cable. Both the video- and still-camera systems utilize relatively inexpensive and proven off-the-shelf hardware adapted for deep-water environments. The small instrument frame makes the towed sled an ideal photographic tool for use on ship or small-boat operations.</p><p>The system includes a temperature probe and altimeter that relay data acoustically from the sled to the surface ship. This relay enables the operator to monitor simultaneously water temperature and the precise height off the bottom.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0198-0149(85)90057-3","usgsCitation":"Chezar, H., and Lee, J., 1985, A new look at deep-sea video: Deep Sea Research Part A, Oceanographic Research Papers, v. 32, no. 11, p. 1429-1436, https://doi.org/10.1016/0198-0149(85)90057-3.","productDescription":"8 p.","startPage":"1429","endPage":"1436","numberOfPages":"8","costCenters":[],"links":[{"id":222375,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"32","issue":"11","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e4a4e4b0c8380cd467cf","contributors":{"authors":[{"text":"Chezar, H.","contributorId":52321,"corporation":false,"usgs":true,"family":"Chezar","given":"H.","email":"","affiliations":[],"preferred":false,"id":364391,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lee, J.","contributorId":58596,"corporation":false,"usgs":true,"family":"Lee","given":"J.","affiliations":[],"preferred":false,"id":364392,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70012746,"text":"70012746 - 1985 - Ages of tuff beds at East African early hominid sites and sediments in the Gulf of Aden","interactions":[],"lastModifiedDate":"2012-03-12T17:19:06","indexId":"70012746","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2840,"text":"Nature","active":true,"publicationSubtype":{"id":10}},"title":"Ages of tuff beds at East African early hominid sites and sediments in the Gulf of Aden","docAbstract":"The early hominids of East Africa were dated by determining the ages of tuff beds at the sites. Despite much research using palaeomagnetic and K/Ar-dating techniques, some of those ages are still controversial 1,2. To obtain independent age estimates for these tephra layers, we have examined cores from DSDP Sites 231 and 232 in the Gulf of Aden (Fig. 1a) which consist mainly of calcareous nannofossil ooze, but also contain rare tephra horizons3 dated by interpolation from the established nannofossil stratigraphy (Fig. 1b). Chemical analysis confirms that the identity and sequence of these horizons is the same as that at the East African sites. We conclude that the age of the Tulu Bor Tuff is <3.4 Myr and hence that the Hadar hominid specimens are also <???3.4 Myr old. ?? 1985 Nature Publishing Group.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Nature","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1038/313306a0","issn":"00280836","usgsCitation":"Sarna-Wojcicki, A., Meyer, C., Roth, P., and Brown, F.H., 1985, Ages of tuff beds at East African early hominid sites and sediments in the Gulf of Aden: Nature, v. 313, no. 6000, p. 306-308, https://doi.org/10.1038/313306a0.","startPage":"306","endPage":"308","numberOfPages":"3","costCenters":[],"links":[{"id":205258,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1038/313306a0"},{"id":222552,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"313","issue":"6000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e906e4b0c8380cd4804c","contributors":{"authors":[{"text":"Sarna-Wojcicki, A.M. 0000-0002-0244-9149","orcid":"https://orcid.org/0000-0002-0244-9149","contributorId":104022,"corporation":false,"usgs":true,"family":"Sarna-Wojcicki","given":"A.M.","affiliations":[],"preferred":false,"id":364425,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Meyer, C.E.","contributorId":104023,"corporation":false,"usgs":true,"family":"Meyer","given":"C.E.","email":"","affiliations":[],"preferred":false,"id":364426,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Roth, P.H.","contributorId":31911,"corporation":false,"usgs":true,"family":"Roth","given":"P.H.","email":"","affiliations":[],"preferred":false,"id":364423,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Brown, F. H.","contributorId":95597,"corporation":false,"usgs":true,"family":"Brown","given":"F.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":364424,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70013903,"text":"70013903 - 1985 - Instability model for recurring large and great earthquakes in southern California","interactions":[],"lastModifiedDate":"2012-03-12T17:19:33","indexId":"70013903","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3209,"text":"Pure and Applied Geophysics PAGEOPH","active":true,"publicationSubtype":{"id":10}},"title":"Instability model for recurring large and great earthquakes in southern California","docAbstract":"The locked section of the San Andreas fault in southern California has experienced a number of large and great earthquakes in the past, and thus is expected to have more in the future. To estimate the location, time, and slip of the next few earthquakes, an earthquake instability model is formulated. The model is similar to one recently developed for moderate earthquakes on the San Andreas fault near Parkfield, California. In both models, unstable faulting (the earthquake analog) is caused by failure of all or part of a patch of brittle, strain-softening fault zone. In the present model the patch extends downward from the ground surface to about 12 km depth, and extends 500 km along strike from Parkfield to the Salton Sea. The variation of patch strength along strike is adjusted by trial until the computed sequence of instabilities matches the sequence of large and great earthquakes since a.d. 1080 reported by Sieh and others. The last earthquake was the M=8.3 Ft. Tejon event in 1857. The resulting strength variation has five contiguous sections of alternately low and high strength. From north to south, the approximate locations of the sections are: (1) Parkfield to Bitterwater Valley, (2) Bitterwater Valley to Lake Hughes, (3) Lake Hughes to San Bernardino, (4) San Bernardino to Palm Springs, and (5) Palm Springs to the Salton Sea. Sections 1, 3, and 5 have strengths between 53 and 88 bars; sections 2 and 4 have strengths between 164 and 193 bars. Patch section ends and unstable rupture ends usually coincide, although one or more adjacent patch sections may fail unstably at once. The model predicts that the next sections of the fault to slip unstably will be 1, 3, and 5; the order and dates depend on the assumed length of an earthquake rupture in about 1700. ?? 1985 Birkha??user Verlag.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Pure and Applied Geophysics PAGEOPH","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisherLocation":"Birkha??user-Verlag","doi":"10.1007/BF00876385","issn":"00334553","usgsCitation":"Stuart, W., 1985, Instability model for recurring large and great earthquakes in southern California: Pure and Applied Geophysics PAGEOPH, v. 122, no. 6, p. 793-811, https://doi.org/10.1007/BF00876385.","startPage":"793","endPage":"811","numberOfPages":"19","costCenters":[],"links":[{"id":226051,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":205677,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF00876385"}],"volume":"122","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3c23e4b0c8380cd62ade","contributors":{"authors":[{"text":"Stuart, W.D.","contributorId":65865,"corporation":false,"usgs":true,"family":"Stuart","given":"W.D.","email":"","affiliations":[],"preferred":false,"id":367132,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70180834,"text":"70180834 - 1985 - Development of an effective transport media for juvenile spring Chinook salmon to mitigate stress and improve smolt survival during Columbia River fish hauling operations","interactions":[],"lastModifiedDate":"2017-02-03T14:20:25","indexId":"70180834","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"title":"Development of an effective transport media for juvenile spring Chinook salmon to mitigate stress and improve smolt survival during Columbia River fish hauling operations","docAbstract":"<p>No abstract available&nbsp;</p>","language":"English","publisher":"Bonneville Power Administration","publisherLocation":"Portland, OR","usgsCitation":"Wedemeyer, G., Palmisano, A., and Salsbury, L., 1985, Development of an effective transport media for juvenile spring Chinook salmon to mitigate stress and improve smolt survival during Columbia River fish hauling operations.","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":334718,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5895a4d6e4b0fa1e59bc1edc","contributors":{"authors":[{"text":"Wedemeyer, Gary","contributorId":94244,"corporation":false,"usgs":true,"family":"Wedemeyer","given":"Gary","affiliations":[],"preferred":false,"id":662550,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Palmisano, A.","contributorId":54368,"corporation":false,"usgs":true,"family":"Palmisano","given":"A.","email":"","affiliations":[],"preferred":false,"id":662551,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Salsbury, L.","contributorId":179085,"corporation":false,"usgs":false,"family":"Salsbury","given":"L.","email":"","affiliations":[],"preferred":false,"id":662552,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70012728,"text":"70012728 - 1985 - Stable-isotope evidence for a magmatic component in fumarole condensates from Augustine Volcano, Cook Inlet, Alaska, U.S.A.","interactions":[],"lastModifiedDate":"2013-01-21T08:36:00","indexId":"70012728","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1213,"text":"Chemical Geology","active":true,"publicationSubtype":{"id":10}},"title":"Stable-isotope evidence for a magmatic component in fumarole condensates from Augustine Volcano, Cook Inlet, Alaska, U.S.A.","docAbstract":"D/H and  18O 16O ratios have been determined for fumarole condensates from Augustine Volcano, an active calc-alkaline stratovolcano in Lower Cook Inlet, Alaska. The isotopic data for the condensates form a linear ?? D-?? 18O array from low-temperature fluids (< 100??C) which are essentially local meteoric water (?? D {reversed tilde equals} -150???, ?? 18O {reversed tilde equals} -19???) to high-temperature (>450??C) fluids collected at the volcano summit which are enriched in both D and 18O (?? D {reversed tilde equals} -35???, ?? 18O {reversed tilde equals} +3.5???). Several lines of evidence suggest that the D-and 18O-rich condensates likely are \"magmatic\" fluids released into the hydrothermal system during and immediately after the 1976 eruption. Prior to 1976, the Augustine hydrothermal system was dominated completely by local meteoric waters. Between 1976 and 1982, fumarole condensates were observed to be variable mixtures of the \"magmatic\" fluid and meteoric water, with the proportion of the former systematically decreasing as the hydrothermal system cooled following the 1976 eruption. ?? 1985.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Chemical Geology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","doi":"10.1016/0009-2541(85)90152-4","issn":"00092541","usgsCitation":"Viglino, J., Harmon, R., Borthwick, J., Nehring, N., Motyka, R., White, L.D., and Johnston, D.A., 1985, Stable-isotope evidence for a magmatic component in fumarole condensates from Augustine Volcano, Cook Inlet, Alaska, U.S.A.: Chemical Geology, v. 49, no. 1-3, p. 141-157, https://doi.org/10.1016/0009-2541(85)90152-4.","startPage":"141","endPage":"157","numberOfPages":"17","costCenters":[],"links":[{"id":266102,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0009-2541(85)90152-4"},{"id":222275,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"49","issue":"1-3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b968be4b08c986b31b595","contributors":{"authors":[{"text":"Viglino, J.A.","contributorId":8728,"corporation":false,"usgs":true,"family":"Viglino","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":364369,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Harmon, R.S.","contributorId":6585,"corporation":false,"usgs":true,"family":"Harmon","given":"R.S.","email":"","affiliations":[],"preferred":false,"id":364368,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Borthwick, J.","contributorId":18905,"corporation":false,"usgs":true,"family":"Borthwick","given":"J.","email":"","affiliations":[],"preferred":false,"id":364372,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Nehring, N.L.","contributorId":21157,"corporation":false,"usgs":true,"family":"Nehring","given":"N.L.","email":"","affiliations":[],"preferred":false,"id":364373,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Motyka, R.J.","contributorId":49594,"corporation":false,"usgs":true,"family":"Motyka","given":"R.J.","email":"","affiliations":[],"preferred":false,"id":364374,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"White, L. D.","contributorId":14330,"corporation":false,"usgs":true,"family":"White","given":"L.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":364370,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Johnston, D. A.","contributorId":18109,"corporation":false,"usgs":true,"family":"Johnston","given":"D.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":364371,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70180832,"text":"70180832 - 1985 - Bioenergetics of juvenile salmon during the spring outmigration","interactions":[],"lastModifiedDate":"2017-02-03T14:17:18","indexId":"70180832","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"title":"Bioenergetics of juvenile salmon during the spring outmigration","docAbstract":"<p>No abstract available&nbsp;</p>","language":"English","publisher":"Bonneville Power Administration","publisherLocation":"Portland, OR","usgsCitation":"Rondorf, D., Dutchuk, M., Kolok, A., and Gross, M., 1985, Bioenergetics of juvenile salmon during the spring outmigration.","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":334714,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5895a4d6e4b0fa1e59bc1ede","contributors":{"authors":[{"text":"Rondorf, D.W.","contributorId":80789,"corporation":false,"usgs":true,"family":"Rondorf","given":"D.W.","email":"","affiliations":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"preferred":false,"id":662543,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dutchuk, M.S.","contributorId":179083,"corporation":false,"usgs":false,"family":"Dutchuk","given":"M.S.","email":"","affiliations":[],"preferred":false,"id":662544,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kolok, A.S.","contributorId":179084,"corporation":false,"usgs":false,"family":"Kolok","given":"A.S.","affiliations":[],"preferred":false,"id":662545,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Gross, M.L.","contributorId":96628,"corporation":false,"usgs":true,"family":"Gross","given":"M.L.","email":"","affiliations":[],"preferred":false,"id":662546,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70012744,"text":"70012744 - 1985 - The near-source strong-motion accelerograms recorded by an experimental array in Tangshan, China","interactions":[],"lastModifiedDate":"2013-02-13T13:31:11","indexId":"70012744","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3071,"text":"Physics of the Earth and Planetary Interiors","active":true,"publicationSubtype":{"id":10}},"title":"The near-source strong-motion accelerograms recorded by an experimental array in Tangshan, China","docAbstract":"A joint research project on strong-motion earthquake studies between the People's Republic of China and the United States is in progress. As a part of this project, an experimental strong-motion array, consisting of twelve Kinemetrics PDR-1 Digital Event Recorders, was deployed in the meizoseismal area of the Ms = 7.8 Tangshan earthquake of July 28, 1976. These instruments have automatic gain ranging, a specified dynamic range of 102 dB, a 2.5 s pre-event memory, programmable triggering, and are equipped with TCG-1B Time Code Generators with a stability of 3 parts in 107 over a range of 0-50??C. In 2 y of operation beginning July, 1982 a total of 603 near-source 3-component accelerograms were gathered from 243 earthquakes of magnitude ML = 1.2-5.3. Most of these accelerograms have recorded the initial P-wave. The configuration of the experimental array and a representative set of near-source strong-motion accelerograms are presented in this paper. The set of accelerograms exhibited were obtained during the ML = 5.3 Lulong earthquake of October 19, 1982, when digital event recorders were triggered. The epicentral distances ranged from 4 to 41 km and the corresponding range of peak horizontal accelerations was 0.232g to 0.009g. A preliminary analysis of the data indicates that compared to motions in the western United States, the peak acceleration attenuates much more rapidly in the Tangshan area. The scaling of peak acceleration with magnitude, however, is similar in the two regions. Data at more distant sites are needed to confirm the more rapid attenuation. ?? 1985.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Physics of the Earth and Planetary Interiors","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","publisherLocation":"Amsterdam, Netherlands","doi":"10.1016/0031-9201(85)90148-7","issn":"00319201","usgsCitation":"Peng, K., Xie, L., Li, S., Boore, D., Iwan, W., and Teng, T., 1985, The near-source strong-motion accelerograms recorded by an experimental array in Tangshan, China: Physics of the Earth and Planetary Interiors, v. 38, no. 2-3, p. 92-109, https://doi.org/10.1016/0031-9201(85)90148-7.","startPage":"92","endPage":"109","numberOfPages":"18","costCenters":[],"links":[{"id":267337,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0031-9201(85)90148-7"},{"id":222496,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"38","issue":"2-3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bae09e4b08c986b323ecd","contributors":{"authors":[{"text":"Peng, K.","contributorId":31909,"corporation":false,"usgs":true,"family":"Peng","given":"K.","email":"","affiliations":[],"preferred":false,"id":364415,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Xie, Lingtian","contributorId":65209,"corporation":false,"usgs":true,"family":"Xie","given":"Lingtian","email":"","affiliations":[],"preferred":false,"id":364420,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Li, S.","contributorId":41969,"corporation":false,"usgs":true,"family":"Li","given":"S.","email":"","affiliations":[],"preferred":false,"id":364417,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Boore, D.M. 0000-0002-8605-9673","orcid":"https://orcid.org/0000-0002-8605-9673","contributorId":64226,"corporation":false,"usgs":true,"family":"Boore","given":"D.M.","affiliations":[],"preferred":false,"id":364419,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Iwan, W.D.","contributorId":33848,"corporation":false,"usgs":true,"family":"Iwan","given":"W.D.","affiliations":[],"preferred":false,"id":364416,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Teng, T.L.","contributorId":62749,"corporation":false,"usgs":true,"family":"Teng","given":"T.L.","email":"","affiliations":[],"preferred":false,"id":364418,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70012777,"text":"70012777 - 1985 - Linear inversion of transmitted acoustic wave fields for three-dimensional modulus and density perturbations using a born-type approximation","interactions":[],"lastModifiedDate":"2023-10-29T15:20:05.802651","indexId":"70012777","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1135,"text":"Bulletin of the Seismological Society of America","onlineIssn":"1943-3573","printIssn":"0037-1106","active":true,"publicationSubtype":{"id":10}},"title":"Linear inversion of transmitted acoustic wave fields for three-dimensional modulus and density perturbations using a born-type approximation","docAbstract":"<p>A Born approximation is used to linearize the relationship, in the horizontal-wavenumber and frequency domains, between lateral perturbations of modulus and density in a layered half-space and the acoustic wave field observed at the surface when a plane wave is incident from below. The resulting equations can be used to perform a linear inversion of observed acoustic wave fields to obtain lateral perturbations in modulus and density. Since modulus and density effects are separated, gravity observations can be included in the inversion procedure without any assumptions about the relationship between density and acoustic velocity. Tests with synthetic data sets reveal that the inversion method gives useful results when the spatial scales of the inhomogeneities are smaller than several acoustic wavelengths. The inclusion of gravity observations in the inversion reduces the strong negative tradeoff between modulus and density perturbations.</p>","language":"English","publisher":"Seismological Society of America","doi":"10.1785/BSSA0750010093","issn":"00371106","usgsCitation":"Stauber, D.A., 1985, Linear inversion of transmitted acoustic wave fields for three-dimensional modulus and density perturbations using a born-type approximation: Bulletin of the Seismological Society of America, v. 75, no. 1, p. 93-114, https://doi.org/10.1785/BSSA0750010093.","productDescription":"22 p.","startPage":"93","endPage":"114","numberOfPages":"22","costCenters":[],"links":[{"id":222037,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"75","issue":"1","noUsgsAuthors":false,"publicationDate":"1985-02-01","publicationStatus":"PW","scienceBaseUri":"505a40e6e4b0c8380cd65118","contributors":{"authors":[{"text":"Stauber, Douglas A.","contributorId":90870,"corporation":false,"usgs":true,"family":"Stauber","given":"Douglas","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":364500,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70012812,"text":"70012812 - 1985 - The effect of glaciers on streamflow variations","interactions":[],"lastModifiedDate":"2018-02-12T18:16:24","indexId":"70012812","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3722,"text":"Water Resources Research","onlineIssn":"1944-7973","printIssn":"0043-1397","active":true,"publicationSubtype":{"id":10}},"title":"The effect of glaciers on streamflow variations","docAbstract":"<p><span>The effect of temperate glaciers on runoff variations is examined for the North Cascade Mountains of Washington State. The principal influences of glaciers on streamflow are often unexpected contributions to streamflow volume, a delay of the maximum seasonal flow, and a decrease in annual and monthly variation of runoff. The delay of maximum flow is caused by temporary englacial storage of spring meltwater and by peak meltwater production occurring in midsummer. The englacial storage, for one case, is 54% of the potential May runoff. An algorithm is presented that calculates the coefficient of variation of runoff for any arbitrary glacier cover. The results suggest that a minimum in year-to-year variation occurs for basins about 36% glacierized. On a month-to-month basis, maximum variation occurs in July and August for basins with less than 10% glacier cover but is a minimum for basins with glacier covers greater than 30%.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/WR021i004p00579","usgsCitation":"Fountain, A.G., and Tangborn, W.V., 1985, The effect of glaciers on streamflow variations: Water Resources Research, v. 21, no. 4, p. 579-586, https://doi.org/10.1029/WR021i004p00579.","productDescription":"8 p.","startPage":"579","endPage":"586","costCenters":[],"links":[{"id":222679,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"21","issue":"4","noUsgsAuthors":false,"publicationDate":"2008-01-08","publicationStatus":"PW","scienceBaseUri":"505bab2ce4b08c986b322c89","contributors":{"authors":[{"text":"Fountain, Andrew G.","contributorId":10410,"corporation":false,"usgs":false,"family":"Fountain","given":"Andrew","email":"","middleInitial":"G.","affiliations":[{"id":6929,"text":"Portland State University","active":true,"usgs":false}],"preferred":false,"id":364591,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tangborn, Wendell V.","contributorId":32152,"corporation":false,"usgs":true,"family":"Tangborn","given":"Wendell","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":364592,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70012776,"text":"70012776 - 1985 - PROCEDURES FOR ACCURATE PRODUCTION OF COLOR IMAGES FROM SATELLITE OR AIRCRAFT MULTISPECTRAL DIGITAL DATA.","interactions":[],"lastModifiedDate":"2012-03-12T17:19:01","indexId":"70012776","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2348,"text":"Journal of Imaging Technology","active":true,"publicationSubtype":{"id":10}},"title":"PROCEDURES FOR ACCURATE PRODUCTION OF COLOR IMAGES FROM SATELLITE OR AIRCRAFT MULTISPECTRAL DIGITAL DATA.","docAbstract":"Because the display and interpretation of satellite and aircraft remote-sensing data make extensive use of color film products, accurate reproduction of the color images is important. To achieve accurate color reproduction, the exposure and chemical processing of the film must be monitored and controlled. By using a combination of sensitometry, densitometry, and transfer functions that control film response curves, all of the different steps in the making of film images can be monitored and controlled. Because a sensitometer produces a calibrated exposure, the resulting step wedge can be used to monitor the chemical processing of the film. Step wedges put on film by image recording machines provide a means of monitoring the film exposure and color balance of the machines.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Imaging Technology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"07473583","usgsCitation":"Duval, J.S., 1985, PROCEDURES FOR ACCURATE PRODUCTION OF COLOR IMAGES FROM SATELLITE OR AIRCRAFT MULTISPECTRAL DIGITAL DATA.: Journal of Imaging Technology, v. 10, no. 1, p. 16-22.","startPage":"16","endPage":"22","numberOfPages":"7","costCenters":[],"links":[{"id":222036,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"10","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a737ce4b0c8380cd77077","contributors":{"authors":[{"text":"Duval, Joseph S.","contributorId":22314,"corporation":false,"usgs":true,"family":"Duval","given":"Joseph","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":364499,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1003305,"text":"1003305 - 1985 - Invertebrate colonization rates in the tailwater of a Kentucky flood-control reservoir","interactions":[],"lastModifiedDate":"2016-01-14T11:00:16","indexId":"1003305","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2299,"text":"Journal of Freshwater Ecology","active":true,"publicationSubtype":{"id":10}},"title":"Invertebrate colonization rates in the tailwater of a Kentucky flood-control reservoir","docAbstract":"<p class=\"last\">Invertebrate colonization on newly introduced rock substrates was examined from July through October 1982 in the tailwater of Barren River Lake, Kentucky. Chironomidae, the dominant taxon of benthic insects, reached full colonization by day 14. Colonization by Oligochaeta, the other major invertebrate taxon, was not completed by the end of the 95-day period of observation. It may have been delayed because insufficient food (periphyton and detritus) had accumulated on the clean rocks. Rapid recolonization of dewatered substrates may be especially critical for maintaining adequate fish food in tailwaters of flood-control reservoir.</p>","language":"English","publisher":"Oikos Publishers","doi":"10.1080/02705060.1985.9665089","usgsCitation":"Swink, W., and Novotny, J., 1985, Invertebrate colonization rates in the tailwater of a Kentucky flood-control reservoir: Journal of Freshwater Ecology, v. 3, no. 1, p. 27-34, https://doi.org/10.1080/02705060.1985.9665089.","productDescription":"8 p.","startPage":"27","endPage":"34","numberOfPages":"8","costCenters":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true},{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":201738,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Kentucky","otherGeospatial":"Barren River Lake","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -86.18637084960938,\n              36.71576985044291\n            ],\n            [\n              -86.18637084960938,\n              36.96744946416931\n            ],\n            [\n              -85.94329833984375,\n              36.96744946416931\n            ],\n            [\n              -85.94329833984375,\n              36.71576985044291\n            ],\n            [\n              -86.18637084960938,\n              36.71576985044291\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"3","issue":"1","noUsgsAuthors":false,"publicationDate":"2011-01-11","publicationStatus":"PW","scienceBaseUri":"4f4e48b5e4b07f02db53389c","contributors":{"authors":[{"text":"Swink, W.D.","contributorId":66200,"corporation":false,"usgs":true,"family":"Swink","given":"W.D.","affiliations":[],"preferred":false,"id":313092,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Novotny, J.F.","contributorId":95856,"corporation":false,"usgs":true,"family":"Novotny","given":"J.F.","email":"","affiliations":[],"preferred":false,"id":313093,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1003303,"text":"1003303 - 1985 - Observations on twinning in the sea lamprey (Petromyzon marinus) in the laboratory","interactions":[],"lastModifiedDate":"2024-05-09T11:19:46.453325","indexId":"1003303","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2330,"text":"Journal of Great Lakes Research","active":true,"publicationSubtype":{"id":10}},"title":"Observations on twinning in the sea lamprey (Petromyzon marinus) in the laboratory","docAbstract":"<div id=\"preview-section-abstract\"><div id=\"abstracts\" class=\"Abstracts u-font-serif text-s\"><div id=\"aep-abstract-id3\" class=\"abstract author\"><div id=\"aep-abstract-sec-id4\"><p>Forty-five sets of separate, normal twins were produced from four portions of the eggs from one female sea lamprey (<i>Petromyzon marinus</i>) each fertilized by a different male. The percentage of twinning in the different groups of embryos ranged from 1.0 to 1.7. Although the development of some of the twins was slightly slower than average, that of most was within the normal range for sea lamprey embryos. The twins were smaller than non-twins, and one twin was usually smaller than the other. Although the discovery of Siamese twins in fish is not uncommon, separate, normal twins have seldom been reported.</p></div></div></div></div>","language":"English","publisher":"Elsevier","doi":"10.1016/S0380-1330(85)71799-6","usgsCitation":"Hanson, L.H., 1985, Observations on twinning in the sea lamprey (Petromyzon marinus) in the laboratory: Journal of Great Lakes Research, v. 11, no. 4, p. 549-551, https://doi.org/10.1016/S0380-1330(85)71799-6.","productDescription":"3 p.","startPage":"549","endPage":"551","numberOfPages":"3","costCenters":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":131318,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"11","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b4386","contributors":{"authors":[{"text":"Hanson, Lee H.","contributorId":67833,"corporation":false,"usgs":true,"family":"Hanson","given":"Lee","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":313091,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70013251,"text":"70013251 - 1985 - MONITORING THE HYDROTHERMAL SYSTEM IN LONG VALLEY CALDERA, CALIFORNIA.","interactions":[],"lastModifiedDate":"2012-03-12T17:18:33","indexId":"70013251","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"MONITORING THE HYDROTHERMAL SYSTEM IN LONG VALLEY CALDERA, CALIFORNIA.","docAbstract":"An ongoing program to monitor the hydrothermal system in Long Valley for changes caused by volcanic or tectonic processes has produced considerable data on the water chemistry and discharge of springs and fluid temperatures and pressures in wells. Changes in hot spring chemistry that have been recorded probably relate to interactions between the variations in the quantity of liquid and gas discharged. Stable carbon isotope data are consistent with a carbon source either from the mantle or from metamorphosed carbonate rocks. Continuous and periodic measurements of hot spring discharge at several sites show significant coseismic and aseismic changes since 1980.","largerWorkTitle":"Transactions - Geothermal Resources Council","conferenceTitle":"1985 International Symposium on Geothermal Energy. Geothermal Resources Council 1985 Annual Meeting.","conferenceLocation":"Kailua-Kona, HI, USA","language":"English","publisher":"Geothermal Resources Council","publisherLocation":"Davis, CA, USA","issn":"01935933","isbn":"0934412596","usgsCitation":"Farrar, C.D., and Sorey, M.L., 1985, MONITORING THE HYDROTHERMAL SYSTEM IN LONG VALLEY CALDERA, CALIFORNIA., <i>in</i> Transactions - Geothermal Resources Council, v. 9, no. pt 1, Kailua-Kona, HI, USA, p. 423-428.","startPage":"423","endPage":"428","numberOfPages":"6","costCenters":[],"links":[{"id":220470,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"9","issue":"pt 1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a4aebe4b0c8380cd69150","contributors":{"authors":[{"text":"Farrar, Christopher D. cdfarrar@usgs.gov","contributorId":1501,"corporation":false,"usgs":true,"family":"Farrar","given":"Christopher","email":"cdfarrar@usgs.gov","middleInitial":"D.","affiliations":[],"preferred":true,"id":365640,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sorey, Michael L.","contributorId":20726,"corporation":false,"usgs":true,"family":"Sorey","given":"Michael","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":365641,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70013096,"text":"70013096 - 1985 - Low-temperature heat capacity and entropy of chalcopyrite (CuFeS2): estimates of the standard molar enthalpy and Gibbs free energy of formation of chalcopyrite and bornite (Cu5FeS4)","interactions":[],"lastModifiedDate":"2013-03-11T18:43:19","indexId":"70013096","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2208,"text":"Journal of Chemical Thermodynamics","active":true,"publicationSubtype":{"id":10}},"title":"Low-temperature heat capacity and entropy of chalcopyrite (CuFeS2): estimates of the standard molar enthalpy and Gibbs free energy of formation of chalcopyrite and bornite (Cu5FeS4)","docAbstract":"The heat capacity of CuFeS2 (chalcopyrite) was measured between 6.3 and 303.5 K. At 298.15 K, Cp,mo and Smo(T) are (95.67??0.14) J??K-1??mol-1 and (124.9??0.2) J??K-1??mol-1, respectively. From a consideration of the results of two sets of equilibrium measurements we conclude that ??fHmo(CuFeS2, cr, 298.15 K) = -(193.6??1.6) kJ??mol-1 and that the recent bomb-calorimetric determination by Johnson and Steele (J. Chem. Thermodynamics 1981, 13, 991) is in error. The standard molar Gibbs free energy of formation of bornite (Cu5FeS4) is -(444.9??2.1) kJ??mol-1 at 748 K. ?? 1985.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Chemical Thermodynamics","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","doi":"10.1016/0021-9614(85)90147-8","issn":"00219614","usgsCitation":"Robie, R.A., Wiggins, L., Barton, P.B., and Hemingway, B.S., 1985, Low-temperature heat capacity and entropy of chalcopyrite (CuFeS2): estimates of the standard molar enthalpy and Gibbs free energy of formation of chalcopyrite and bornite (Cu5FeS4): Journal of Chemical Thermodynamics, v. 17, no. 5, p. 481-488, https://doi.org/10.1016/0021-9614(85)90147-8.","startPage":"481","endPage":"488","numberOfPages":"8","costCenters":[],"links":[{"id":269086,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0021-9614(85)90147-8"},{"id":219832,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a4a60e4b0c8380cd68d00","contributors":{"authors":[{"text":"Robie, R. A.","contributorId":71237,"corporation":false,"usgs":true,"family":"Robie","given":"R.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":365277,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wiggins, L.B.","contributorId":18776,"corporation":false,"usgs":true,"family":"Wiggins","given":"L.B.","email":"","affiliations":[],"preferred":false,"id":365275,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Barton, P. B. Jr.","contributorId":23683,"corporation":false,"usgs":true,"family":"Barton","given":"P.","suffix":"Jr.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":365276,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hemingway, B. S.","contributorId":7268,"corporation":false,"usgs":true,"family":"Hemingway","given":"B.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":365274,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":1013874,"text":"1013874 - 1985 - Heteropolaria colisarum Foissner and Schubert, 1977 (Protozoa: Epistylididae) or North American freshwater fishes","interactions":[],"lastModifiedDate":"2024-04-02T10:58:38.414717","indexId":"1013874","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2286,"text":"Journal of Fish Diseases","active":true,"publicationSubtype":{"id":10}},"title":"Heteropolaria colisarum Foissner and Schubert, 1977 (Protozoa: Epistylididae) or North American freshwater fishes","docAbstract":"<div class=\"abstract-group \"><div class=\"article-section__content en main\"><p>The peritrichous ciliate<span>&nbsp;</span><i>‘Epistylis</i><span>&nbsp;</span>sp.’ involved in the‘red-sore’ disease of various North American freshwater fishes is identified as<span>&nbsp;</span><i>Heteropolaria colisarum</i><span>&nbsp;</span>Foissner &amp; Schubert, 1977. Its morphology is redescribed from observations of living and silver-stained organisms and biometrically analysed individuals. Extended zooids can be easily identified by their highly characteristic (elongated) body. Silver impregnations show a very high number of silverlines and a band-like, irregularly formed macronucleus. The genus<span>&nbsp;</span><i>Heteropolaria</i><span>&nbsp;</span>belongs to the family Epistylididae and is characterized by the eccentric location of the scopula of the swarmer and a peculiar myoneme in the peristomal disc that branches off the myoneme of the peristomal collar. Autochthonous occurrences of this species are known only from North America. In Europe only the related species<span>&nbsp;</span><i>H. lwoffi</i><span>&nbsp;</span>has been found. Histological sections give some evidence that the terminal platelet of the stalk is embedded in the dermal epithelium. This suggests that<span>&nbsp;</span><i>H. colisarum</i><span>&nbsp;</span>could be a parasite rather than an epizoon and that the often associated bacterium<span>&nbsp;</span><i>Aeromonas hydrophila</i><span>&nbsp;</span>is a secondary invader. However, further studies are necessary. Experiments showed a high infectivity of the ciliate and no host specificity. These characteristics are supported by the observations of other researchers. Preliminary laboratory tests showed that a single treatment with salt solution (NaCl) at a rate of 1.5% for 3h controlled<span>&nbsp;</span><i>H. colisarum.</i></p></div></div>","language":"English","publisher":"Wiley","doi":"10.1111/j.1365-2761.1985.tb01210.x","usgsCitation":"Foissner, W., Hoffman, G.L., and Mitchell, A., 1985, Heteropolaria colisarum Foissner and Schubert, 1977 (Protozoa: Epistylididae) or North American freshwater fishes: Journal of Fish Diseases, v. 8, no. 2, p. 145-160, https://doi.org/10.1111/j.1365-2761.1985.tb01210.x.","productDescription":"16 p.","startPage":"145","endPage":"160","numberOfPages":"16","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":131489,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"8","issue":"2","noUsgsAuthors":false,"publicationDate":"2006-04-07","publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db635b8b","contributors":{"authors":[{"text":"Foissner, W.","contributorId":98267,"corporation":false,"usgs":true,"family":"Foissner","given":"W.","email":"","affiliations":[],"preferred":false,"id":319388,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hoffman, G. L.","contributorId":70713,"corporation":false,"usgs":true,"family":"Hoffman","given":"G.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":319387,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mitchell, A.J.","contributorId":16345,"corporation":false,"usgs":true,"family":"Mitchell","given":"A.J.","email":"","affiliations":[],"preferred":false,"id":319386,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":1013852,"text":"1013852 - 1985 - Temperature comparisons for antibody production in vitro by plaque-forming cells from trout Salmo gairdneri (Richardson), and mice","interactions":[],"lastModifiedDate":"2024-05-07T16:06:21.771768","indexId":"1013852","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2285,"text":"Journal of Fish Biology","active":true,"publicationSubtype":{"id":10}},"title":"Temperature comparisons for antibody production in vitro by plaque-forming cells from trout Salmo gairdneri (Richardson), and mice","docAbstract":"<p><span>Anterior kidney and splenic cells were taken from rainbow trout and splenic cells from BALB/c mice immunized with a T-dependent (sheep red blood cells) or T-independent (DNP-Ficoll) antigen. The cells were incubated at different temperatures in Jerne plaque assays (direct or passive haemolytic plaque assays). The optimum numbers of&nbsp;</span><i>in vitro</i><span>&nbsp;plaque-forming cells (PFC) after incubation with homologous complement were directly correlated with normal body temperatures of the respective species. The optimum incubation temperature was 37°C for mouse cells and 10°C for fish cells. Incubation of mouse cells at lower temperatures of 30, 20, 10, 4 or 0°C appeared to yield a direct line reduction in numbers of PFC. Trout cells developed significantly fewer PFC at 4 and 20°C and none at 30°C or above; however, significant numbers still appeared at 0°C. More PFC per million white blood cells were obtained from the anterior kidney; however, related to temperatures, no differences in development of numbers of PFC could be seen between the spleen and anterior kidney cells of trout. When the incubation time was lengthened for both trout and mouse cells held at low temperatures, the numbers of PFC approached those of the cells incubated at the optimum temperatures for 10 h.</span></p>","language":"English","publisher":"Wiley","doi":"10.1111/j.1095-8649.1985.tb04027.x","usgsCitation":"van Ginkel, F.W., van Muiswinkel, W., Merchant, B., Lizzio, E.F., Dixon, O.W., and Anderson, D.P., 1985, Temperature comparisons for antibody production in vitro by plaque-forming cells from trout Salmo gairdneri (Richardson), and mice: Journal of Fish Biology, v. 27, no. 3, p. 265-272, https://doi.org/10.1111/j.1095-8649.1985.tb04027.x.","productDescription":"8 p.","startPage":"265","endPage":"272","numberOfPages":"8","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":197482,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"27","issue":"3","noUsgsAuthors":false,"publicationDate":"2006-01-24","publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db6857b3","contributors":{"authors":[{"text":"van Ginkel, F. W.","contributorId":69921,"corporation":false,"usgs":true,"family":"van Ginkel","given":"F.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":319348,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"van Muiswinkel, W. B.","contributorId":57783,"corporation":false,"usgs":true,"family":"van Muiswinkel","given":"W. B.","affiliations":[],"preferred":false,"id":319347,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Merchant, B.","contributorId":79432,"corporation":false,"usgs":true,"family":"Merchant","given":"B.","email":"","affiliations":[],"preferred":false,"id":319349,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lizzio, E. F.","contributorId":50471,"corporation":false,"usgs":true,"family":"Lizzio","given":"E.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":319346,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Dixon, O. W.","contributorId":101588,"corporation":false,"usgs":true,"family":"Dixon","given":"O.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":319350,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Anderson, D. P.","contributorId":32469,"corporation":false,"usgs":true,"family":"Anderson","given":"D.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":319345,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":1013929,"text":"1013929 - 1985 - Striped bass restoration - the national perspective","interactions":[],"lastModifiedDate":"2012-03-02T17:16:04","indexId":"1013929","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1655,"text":"Fish and Wildlife News","active":true,"publicationSubtype":{"id":10}},"title":"Striped bass restoration - the national perspective","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Fish and Wildlife News","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"U.S. Fish and Wildlife Service","collaboration":"None/FC","usgsCitation":"Goodyear, P., and Rago, P., 1985, Striped bass restoration - the national perspective: Fish and Wildlife News, no. March-April, p. 5-5.","startPage":"5","endPage":"5","numberOfPages":"1","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":130863,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"issue":"March-April","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4c7c","contributors":{"authors":[{"text":"Goodyear, P.","contributorId":11166,"corporation":false,"usgs":true,"family":"Goodyear","given":"P.","email":"","affiliations":[],"preferred":false,"id":319455,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rago, P.","contributorId":42168,"corporation":false,"usgs":true,"family":"Rago","given":"P.","email":"","affiliations":[],"preferred":false,"id":319456,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
]}