{"pageNumber":"5377","pageRowStart":"134400","pageSize":"25","recordCount":184769,"records":[{"id":70011811,"text":"70011811 - 1982 - Seasonal growth in the bivalve Macoma balthica near the southern limit of its range","interactions":[],"lastModifiedDate":"2020-09-02T17:41:34.917836","indexId":"70011811","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1583,"text":"Estuaries","active":true,"publicationSubtype":{"id":10}},"title":"Seasonal growth in the bivalve Macoma balthica near the southern limit of its range","docAbstract":"

Shell-length growth in Macoma balthica from San Francisco Bay, California, as measured on living animals in situ, is highly seasonal despite a mild Mediterranean climate: a long period of near non-growth from May to the following February is followed by a short period of rapid growth between March and May. The rapid-growth period follows the spawning period during January/February and ends as water temperature rises above about 15??C. Despite the shortness of the growth period, M. balthica grows larger at a given age in San Francisco Bay than is recorded elsewhere in the world. Application of a model, developed elsewhere from these same field measurements, shows that (1) measurable growth occurs during the summer/autumn/early winter \"nongrowth\" period, (2) there is an autumn recruitment, and (3) both spring and autumn recruits combine to form a single \"one-year-old\" size grouping. None of these features is detectable through growth-ring analysis of field samples, apparently because of indistinct climatic seasons, or through size-frequency histogram analysis because of the combined effects of slow growth and intermittent recruitment. ?? 1982 Estuarine Research Federation.

","language":"English","publisher":"Springer-Verlag","doi":"10.2307/1352108","issn":"15592723","usgsCitation":"Nichols, F., and Thompson, J., 1982, Seasonal growth in the bivalve Macoma balthica near the southern limit of its range: Estuaries, v. 5, no. 2, p. 110-120, https://doi.org/10.2307/1352108.","startPage":"110","endPage":"120","numberOfPages":"11","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":552,"text":"San Francisco Bay-Delta","active":false,"usgs":true},{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true}],"links":[{"id":221132,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"5","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b88ace4b08c986b316ac9","contributors":{"authors":[{"text":"Nichols, F.H.","contributorId":88020,"corporation":false,"usgs":true,"family":"Nichols","given":"F.H.","affiliations":[],"preferred":false,"id":362012,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thompson, J.K.","contributorId":103300,"corporation":false,"usgs":true,"family":"Thompson","given":"J.K.","email":"","affiliations":[],"preferred":false,"id":362013,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70010435,"text":"70010435 - 1982 - Automated standardization technique for an inductively-coupled plasma emission spectrometer","interactions":[],"lastModifiedDate":"2023-03-07T16:33:07.780652","indexId":"70010435","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":760,"text":"Analytica Chimica Acta","active":true,"publicationSubtype":{"id":10}},"title":"Automated standardization technique for an inductively-coupled plasma emission spectrometer","docAbstract":"

The manifold assembly subsystem described permits real-time computer-controlled standardization and quality control of a commercial inductively-coupled plasma atomic emission spectrometer. The manifold assembly consists of a branch-structured glass manifold, a series of microcomputer-controlled solenoid valves, and a reservoir for each standard. Automated standardization involves selective actuation of each solenoid valve that permits a specific mixed standard solution to be pumped to the nebulizer of the spectrometer. Quality control is based on the evaluation of results obtained for a mixed standard containing 17 analytes, that is measured periodically with unknown samples. An inaccurate standard evaluation triggers restandardization of the instrument according to a predetermined protocol. Interaction of the computer-controlled manifold assembly hardware with the spectrometer system is outlined. Evaluation of the automated standardization system with respect to reliability, simplicity, flexibility, and efficiency is compared to the manual procedure.

","language":"English","publisher":"Elsevier","doi":"10.1016/S0003-2670(01)84186-6","usgsCitation":"Garbarino, J.R., and Taylor, H.E., 1982, Automated standardization technique for an inductively-coupled plasma emission spectrometer: Analytica Chimica Acta, v. 134, no. C, p. 153-165, https://doi.org/10.1016/S0003-2670(01)84186-6.","productDescription":"13 p.","startPage":"153","endPage":"165","numberOfPages":"13","costCenters":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true},{"id":5046,"text":"Branch of Analytical Serv (NWQL)","active":true,"usgs":true}],"links":[{"id":219690,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"134","issue":"C","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059eef6e4b0c8380cd4a087","contributors":{"authors":[{"text":"Garbarino, John R. jrgarb@usgs.gov","contributorId":2189,"corporation":false,"usgs":true,"family":"Garbarino","given":"John","email":"jrgarb@usgs.gov","middleInitial":"R.","affiliations":[{"id":5046,"text":"Branch of Analytical Serv (NWQL)","active":true,"usgs":true}],"preferred":true,"id":358923,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Taylor, Howard E. hetaylor@usgs.gov","contributorId":1551,"corporation":false,"usgs":true,"family":"Taylor","given":"Howard","email":"hetaylor@usgs.gov","middleInitial":"E.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":358922,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70011813,"text":"70011813 - 1982 - An automatic optimum kernel-size selection technique for edge enhancement","interactions":[],"lastModifiedDate":"2017-01-18T14:57:13","indexId":"70011813","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3254,"text":"Remote Sensing of Environment","printIssn":"0034-4257","active":true,"publicationSubtype":{"id":10}},"title":"An automatic optimum kernel-size selection technique for edge enhancement","docAbstract":"

Edge enhancement is a technique that can be considered, to a first order, a correction for the modulation transfer function of an imaging system. Digital imaging systems sample a continuous function at discrete intervals so that high-frequency information cannot be recorded at the same precision as lower frequency data. Because of this, fine detail or edge information in digital images is lost. Spatial filtering techniques can be used to enhance the fine detail information that does exist in the digital image, but the filter size is dependent on the type of area being processed. A technique has been developed by the authors that uses the horizontal first difference to automatically select the optimum kernel-size that should be used to enhance the edges that are contained in the image. 

","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Remote Sensing of Environment","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","doi":"10.1016/0034-4257(82)90005-0","issn":"00344257","usgsCitation":"Chavez, P.S., and Bauer, B.P., 1982, An automatic optimum kernel-size selection technique for edge enhancement: Remote Sensing of Environment, v. 12, no. 1, p. 23-38, https://doi.org/10.1016/0034-4257(82)90005-0.","productDescription":"16 p.","startPage":"23","endPage":"38","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":221198,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"12","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059ea21e4b0c8380cd48665","contributors":{"authors":[{"text":"Chavez, Pat S. Jr.","contributorId":39870,"corporation":false,"usgs":true,"family":"Chavez","given":"Pat","suffix":"Jr.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":362015,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bauer, Brian P.","contributorId":58946,"corporation":false,"usgs":true,"family":"Bauer","given":"Brian","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":362016,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70010416,"text":"70010416 - 1982 - Gamma-emitting radionuclide measurements at the US geological survey national water quality laboratory, Denver, Colorado","interactions":[],"lastModifiedDate":"2012-03-12T17:18:17","indexId":"70010416","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2906,"text":"Nuclear Instruments and Methods","active":true,"publicationSubtype":{"id":10}},"title":"Gamma-emitting radionuclide measurements at the US geological survey national water quality laboratory, Denver, Colorado","docAbstract":"Like sediment samples from Scofield Resevior in Utah were analyzed for 210Pb by the gamma-ray spectrometric method. The top 10 cm of surface sediment yielded excess 210Pb activity (excluding in situ 226Ra supported 210Pb) of 1.05 pCi/g dry weight and decreased to 0.25 pCi/g at a depth of 25 cm. Based on these data, sedimentation rate was approximately 0.49 cm/y for a total of 30 cm of lake sediment and a lake history of approximately 60 y. An alternative method of 210Pb measurements using wet chemical procedures followed by beta counting gave equivalent results. ?? 1982.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Nuclear Instruments and Methods","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"0029554X","usgsCitation":"In, C.Y., and Ambats, E., 1982, Gamma-emitting radionuclide measurements at the US geological survey national water quality laboratory, Denver, Colorado: Nuclear Instruments and Methods, v. 193, no. 1-2, p. 197-201.","startPage":"197","endPage":"201","numberOfPages":"5","costCenters":[],"links":[{"id":219374,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"193","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a14b2e4b0c8380cd54b04","contributors":{"authors":[{"text":"In, Che Yang","contributorId":39934,"corporation":false,"usgs":true,"family":"In","given":"Che","email":"","middleInitial":"Yang","affiliations":[],"preferred":false,"id":358869,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ambats, E.","contributorId":23270,"corporation":false,"usgs":true,"family":"Ambats","given":"E.","email":"","affiliations":[],"preferred":false,"id":358868,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70011815,"text":"70011815 - 1982 - Palladium, platinum, rhodium, ruthenium, and iridium in chromitites from the Massif du Sud and Tiebaghi Massif, New Caledonia","interactions":[],"lastModifiedDate":"2024-01-12T16:43:25.98448","indexId":"70011815","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"Palladium, platinum, rhodium, ruthenium, and iridium in chromitites from the Massif du Sud and Tiebaghi Massif, New Caledonia","docAbstract":"

Massive and disseminated podiform chromitite from 43 mines and other occurrences in the Massif du Sud and Tiebaghi Massif, both ophiolites, in New Caledonia contain up to 9 ppb Pd, up to 45 ppb Pt, up to 31 ppb Rh, up to 410 ppb Ir, and up to 1,130 ppb Ru. The chromitites are strongly depleted in Pt and Pd and mildly depleted in Ir and Ru with respect to an average chondrite composition, as are podiform chromitites from Oman, Turkey, Greece, and northern California. Stratiform chromitites from the Stillwater Complex, Montana, and the Bushveld Complex, South Africa, show inverse patterns of enrichment and depletion. These patterns suggest that either chromitite from ophiolites represents mantle rocks depleted in Pt and Pd or that the magmas that formed the ophiolites were depleted in Pt and Pd, or that the process of forming the chromitite involved the concentration of Os and Ir from a magma. The relatively high contents of Ir and Ru in the New Caledonian chromitite suggest the potential for the occurrence of placers that contain concentrations of Os-Ir alloys.

","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.77.6.1571","issn":"03610128","usgsCitation":"Page, N., Cassard, D., and Haffty, J., 1982, Palladium, platinum, rhodium, ruthenium, and iridium in chromitites from the Massif du Sud and Tiebaghi Massif, New Caledonia: Economic Geology, v. 77, no. 6, p. 1571-1577, https://doi.org/10.2113/gsecongeo.77.6.1571.","productDescription":"7 p.","startPage":"1571","endPage":"1577","numberOfPages":"7","costCenters":[],"links":[{"id":221200,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"77","issue":"6","noUsgsAuthors":false,"publicationDate":"1982-10-01","publicationStatus":"PW","scienceBaseUri":"505a747de4b0c8380cd7768c","contributors":{"authors":[{"text":"Page, N.J.","contributorId":38125,"corporation":false,"usgs":true,"family":"Page","given":"N.J.","affiliations":[],"preferred":false,"id":362018,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cassard, D.","contributorId":57207,"corporation":false,"usgs":true,"family":"Cassard","given":"D.","affiliations":[],"preferred":false,"id":362019,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Haffty, J.","contributorId":93187,"corporation":false,"usgs":true,"family":"Haffty","given":"J.","affiliations":[],"preferred":false,"id":362020,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70011816,"text":"70011816 - 1982 - Sources, sinks and storage of river sediments in the Atlantic drainage of the United States","interactions":[],"lastModifiedDate":"2024-04-26T16:45:34.641676","indexId":"70011816","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2309,"text":"Journal of Geology","active":true,"publicationSubtype":{"id":10}},"title":"Sources, sinks and storage of river sediments in the Atlantic drainage of the United States","docAbstract":"

The history of sediment and its movement in the Atlantic drainage demonstrate some of the difficulties of modeling sediment on a river-basin scale. Soil erosion was accelerated by a factor of at least 10 when European settlers cleared forests and planted crops. Although increasing soil-conservation practice and decreasing crop farming have since reduced the rates of erosion, large quantities of eroded material are still stored on hillslopes and in stream valleys where they continue to augment the sediment loads of the rivers. The sediment from this episode of erosion that is largely past can be expected to emerge from storage for many decades and perhaps even several centuries to come. The reservoirs that have been built on many of the major rivers trap significant portions of the moving sediment which, in some places, may be remobilized by large floods. Essentially all the river sediment that reaches the Atlantic coastal zone is trapped in estuaries and coastal marshlands. Probably less than 5% is deposited on the floor of the continental shelf or the deep sea.

","language":"English","publisher":"University of Chicago Press","doi":"10.1086/628677","issn":"00221376","usgsCitation":"Meade, R., 1982, Sources, sinks and storage of river sediments in the Atlantic drainage of the United States: Journal of Geology, v. 90, no. 3, p. 235-252, https://doi.org/10.1086/628677.","productDescription":"18 p.","startPage":"235","endPage":"252","numberOfPages":"18","costCenters":[],"links":[{"id":221201,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"90","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b93a9e4b08c986b31a604","contributors":{"authors":[{"text":"Meade, R.H.","contributorId":27449,"corporation":false,"usgs":true,"family":"Meade","given":"R.H.","email":"","affiliations":[],"preferred":false,"id":362021,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70011817,"text":"70011817 - 1982 - Active diapirism and slope steepening, northern Gulf of Mexico continental slope","interactions":[],"lastModifiedDate":"2019-12-02T06:50:00","indexId":"70011817","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2670,"text":"Marine Geotechnology","active":true,"publicationSubtype":{"id":10}},"title":"Active diapirism and slope steepening, northern Gulf of Mexico continental slope","docAbstract":"Large diapiric and nondiapiric masses of Jurassic salt and Tertiary shale underlie the northern Gulf of Mexico continental slope and adjacent outer continental shelf. Local steepening of the sea floor in response to the vertical growth of these structures is a serious concern to those involved in the site selection and the construction of future oil and gas production and transportation facilities in this frontier petroleum province. The evidence given in this paper supports the conclusion that the present continental slope region of the northern Gulf of Mexico is undergoing active diapirism and consequent slope steepening. Because most of the sediment on the flanks of diapiric structures consists of underconsolidated muds, slumping will take place regularly in response to further diapiric movement.-from Authors","language":"English","publisher":"Taylor and Francis","doi":"10.1080/10641198209379837","issn":"03608867","usgsCitation":"Martin, R.G., and Bouma, A., 1982, Active diapirism and slope steepening, northern Gulf of Mexico continental slope: Marine Geotechnology, v. 5, no. 1, p. 63-91, https://doi.org/10.1080/10641198209379837.","productDescription":"29 p. ","startPage":"63","endPage":"91","numberOfPages":"29","costCenters":[],"links":[{"id":221202,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":268179,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1080/10641198209379837"}],"otherGeospatial":"Gulf of Mexico","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -97.998046875,\n 18.562947442888312\n ],\n [\n -80.68359375,\n 18.562947442888312\n ],\n [\n -80.68359375,\n 30.44867367928756\n ],\n [\n -97.998046875,\n 30.44867367928756\n ],\n [\n -97.998046875,\n 18.562947442888312\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"5","issue":"1","noUsgsAuthors":false,"publicationDate":"2008-12-23","publicationStatus":"PW","scienceBaseUri":"5059e6aae4b0c8380cd47584","contributors":{"authors":[{"text":"Martin, R. G.","contributorId":100431,"corporation":false,"usgs":true,"family":"Martin","given":"R.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":362022,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bouma, A.H.","contributorId":107281,"corporation":false,"usgs":true,"family":"Bouma","given":"A.H.","email":"","affiliations":[],"preferred":false,"id":362023,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70011792,"text":"70011792 - 1982 - The solubility of quartz in aqueous sodium chloride solution at 350°C and 180 to 500 bars","interactions":[],"lastModifiedDate":"2015-06-05T14:13:41","indexId":"70011792","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1759,"text":"Geochimica et Cosmochimica Acta","active":true,"publicationSubtype":{"id":10}},"title":"The solubility of quartz in aqueous sodium chloride solution at 350°C and 180 to 500 bars","docAbstract":"

The solubility of quartz in 2, 3, and 4 molal NaCl was measured at 350°C and pressures ranging from 180 to 500 bars. The molal solubility in each of the salt solutions is greater than that in pure water throughout the measured pressure range, with the ratio of solubility in NaCl solution to solubility in pure water decreasing as pressure is increased. The measured solubilities are significantly higher than solubilities calculated using a simple model in which the water activity in NaCl solutions decreases either in proportion to decreasing vapor pressure of the solution as salinity is increased or in proportion to decreasing mole fraction of water in the solvent.

","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(82)90136-3","issn":"00167037","usgsCitation":"Fournier, R.O., Rosenbauer, R.J., and Bischoff, J.L., 1982, The solubility of quartz in aqueous sodium chloride solution at 350°C and 180 to 500 bars: Geochimica et Cosmochimica Acta, v. 46, no. 10, p. 1975-1978, https://doi.org/10.1016/0016-7037(82)90136-3.","productDescription":"4 p.","startPage":"1975","endPage":"1978","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":220791,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"46","issue":"10","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb042e4b08c986b324d3a","contributors":{"authors":[{"text":"Fournier, Robert O.","contributorId":73202,"corporation":false,"usgs":true,"family":"Fournier","given":"Robert","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":361969,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rosenbauer, Robert J. brosenbauer@usgs.gov","contributorId":204,"corporation":false,"usgs":true,"family":"Rosenbauer","given":"Robert","email":"brosenbauer@usgs.gov","middleInitial":"J.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":361968,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bischoff, James L. jbischoff@usgs.gov","contributorId":1389,"corporation":false,"usgs":true,"family":"Bischoff","given":"James","email":"jbischoff@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":true,"id":361967,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70010391,"text":"70010391 - 1982 - Stability studies of surficial sediments in the Wilmington-Lindenkohl Canyons area, eastern U.S. margin","interactions":[],"lastModifiedDate":"2012-03-12T17:18:25","indexId":"70010391","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1742,"text":"Geo-Marine Letters","active":true,"publicationSubtype":{"id":10}},"title":"Stability studies of surficial sediments in the Wilmington-Lindenkohl Canyons area, eastern U.S. margin","docAbstract":"Stability analysis, based on infinite slope analysis and geotechnical data from a suite of 34 cores collected from the continental slope between Wilmington and Lindenkohl Canyons, indicates that the Quaternary surficial silty clay sediments on gentle slopes are stable; that sediment stability on steeper slopes (14??-19??) is marginal; and that on precipitous slopes (>50??) only a thin veneer of unconsolidated sediments can exist. Small earthquake-induced accelerations or the effects of internal waves can result in slope sediment instabilities. ?? 1982 A. M. Dowden, Inc.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Geo-Marine Letters","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisherLocation":"Springer-Verlag","doi":"10.1007/BF02462753","issn":"02760460","usgsCitation":"Almagor, G., Bennett, R., Mc Gregor, B., and Shephard, L., 1982, Stability studies of surficial sediments in the Wilmington-Lindenkohl Canyons area, eastern U.S. margin: Geo-Marine Letters, v. 2, no. 3-4, p. 129-134, https://doi.org/10.1007/BF02462753.","startPage":"129","endPage":"134","numberOfPages":"6","costCenters":[],"links":[{"id":204898,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF02462753"},{"id":218947,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"2","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b965ee4b08c986b31b478","contributors":{"authors":[{"text":"Almagor, G.","contributorId":16973,"corporation":false,"usgs":true,"family":"Almagor","given":"G.","email":"","affiliations":[],"preferred":false,"id":358812,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bennett, R.H.","contributorId":34649,"corporation":false,"usgs":true,"family":"Bennett","given":"R.H.","email":"","affiliations":[],"preferred":false,"id":358813,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mc Gregor, B.A.","contributorId":82054,"corporation":false,"usgs":true,"family":"Mc Gregor","given":"B.A.","email":"","affiliations":[],"preferred":false,"id":358815,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Shephard, L.E.","contributorId":53940,"corporation":false,"usgs":true,"family":"Shephard","given":"L.E.","email":"","affiliations":[],"preferred":false,"id":358814,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70011795,"text":"70011795 - 1982 - Chemical and isotopic diversity in basalts dredged from the East Pacific Rise at 10°S, the fossil Galapagos Rise and the Nazca plate","interactions":[],"lastModifiedDate":"2015-06-05T16:08:57","indexId":"70011795","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2667,"text":"Marine Geology","active":true,"publicationSubtype":{"id":10}},"title":"Chemical and isotopic diversity in basalts dredged from the East Pacific Rise at 10°S, the fossil Galapagos Rise and the Nazca plate","docAbstract":"

We present petrographic, chemical and isotopic data for fresh lava samples dredged from three regions: (1) the fossil Galapagos Rise; (2) an elongate volcano near this extinct spreading center; and (3) the East Pacific Rise at 10°S. The samples from the Galapagos Rise are among the first samples from any fossil spreading center to be analyzed. Alkalic picrites from the elongate seamount and transitional basalts from the East Pacific Rise are both somewhat unusual rock types considering their respective tectonic environments.

\n

The dredges from the East Pacific Rise at about 10°S recovered unusual transitional, light rare-earth element (LREE) enriched basalts which show a range of fractionation. On the basis of their chemical and isotopic abundances, it is unlikely that the lavas are related by a single simple process of magmatic differentiation. We suggest that the mantle source region of these basalts was chemically and isotopically heterogeneous. The chemistry of LREE-depleted tholeiitic basalt dredged from near the axis of the extinct Galapagos Rise indicates complex petrogenesis and differentiation. The presence of tholeiitic basalts here indicates that unlike the Guadalupe and Mathematician fossil ridges, the Galapagos Rise has not been the site of voluminous post-abandonment alkalic volcanism. Alkalic basalts of picritic bulk composition dredged from an elongate seamount near the Galapagos Rise do not represent liquid compositions. Instead, we suggest that these alkalic liquids contain added olivine and plagioclase xenocrysts. Although most of the samples analyzed are very fresh, a few have been altered. The latter exhibit characteristic chemical and isotopic effects of seawater alteration.

","language":"English","publisher":"Elsevier","doi":"10.1016/0025-3227(82)90032-9","issn":"00253227","usgsCitation":"Batiza, R., Oestrike, R., and Futa, K., 1982, Chemical and isotopic diversity in basalts dredged from the East Pacific Rise at 10°S, the fossil Galapagos Rise and the Nazca plate: Marine Geology, v. 49, no. 1-2, p. 115-132, https://doi.org/10.1016/0025-3227(82)90032-9.","productDescription":"18 p.","startPage":"115","endPage":"132","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":220860,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"49","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f546e4b0c8380cd4c144","contributors":{"authors":[{"text":"Batiza, Rodey","contributorId":95613,"corporation":false,"usgs":true,"family":"Batiza","given":"Rodey","email":"","affiliations":[],"preferred":false,"id":361976,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Oestrike, Richard","contributorId":23275,"corporation":false,"usgs":true,"family":"Oestrike","given":"Richard","email":"","affiliations":[],"preferred":false,"id":361974,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Futa, Kiyoto 0000-0001-8649-7510 kfuta@usgs.gov","orcid":"https://orcid.org/0000-0001-8649-7510","contributorId":619,"corporation":false,"usgs":true,"family":"Futa","given":"Kiyoto","email":"kfuta@usgs.gov","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":361975,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":1000360,"text":"1000360 - 1982 - Decline of lake herring (Coregonus artedii) in Lake Superior: an analysis of the Wisconsin herring fishery, 1936-78","interactions":[],"lastModifiedDate":"2016-04-01T08:56:17","indexId":"1000360","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1169,"text":"Canadian Journal of Fisheries and Aquatic Sciences","active":true,"publicationSubtype":{"id":10}},"title":"Decline of lake herring (Coregonus artedii) in Lake Superior: an analysis of the Wisconsin herring fishery, 1936-78","docAbstract":"

Annual harvests of lake herring (Coregonus artedii) in American waters of Lake Superior declined from an average of 2 million kg in 1936–62 to less than 25 000 kg in 1978. Analysis of commercial fishing records revealed that the sequential overexploitation of discrete unit stocks caused the collapse of the herring population in Wisconsin waters. In each of six major spawning areas, catch exceeded the productive capacity of the stock and the stock failed. Because stocks in the six areas were exploited sequentially, mostly in groups of two or three simultaneously, the demise of the stocks was not readily apparent until the last two failed in the early 1960s. After the collapse of the last major spawning stock, the fishery dwindled but may have continued to overexploit the remaining small stocks. The residual populations were apparently able only to replace themselves. Some form of density-independent mortality was apparently operating to prevent their recovery during the 1960s and 1970s.Key words: lake herring, overfishing, Lake Superior

","language":"English","publisher":"NRC Research Press","doi":"10.1139/f82-079","usgsCitation":"Selgeby, J.H., 1982, Decline of lake herring (Coregonus artedii) in Lake Superior: an analysis of the Wisconsin herring fishery, 1936-78: Canadian Journal of Fisheries and Aquatic Sciences, v. 39, no. 4, p. 554-563, https://doi.org/10.1139/f82-079.","productDescription":"10 p.","startPage":"554","endPage":"563","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":128957,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"39","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abbe4b07f02db672716","contributors":{"authors":[{"text":"Selgeby, James H.","contributorId":89828,"corporation":false,"usgs":true,"family":"Selgeby","given":"James","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":308451,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1000341,"text":"1000341 - 1982 - Accumulation by fish of contaminants released from dredged sediments","interactions":[],"lastModifiedDate":"2013-01-29T10:45:19","indexId":"1000341","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1565,"text":"Environmental Science & Technology","onlineIssn":"1520-5851","printIssn":"0013-936X","active":true,"publicationSubtype":{"id":10}},"title":"Accumulation by fish of contaminants released from dredged sediments","docAbstract":"Inasmuch as the process of dredging and disposing of dredged materials causes a resuspension of these materials and an increase in bioavailability of associated contaminants, we conducted a series of experiments to examine the potential accumulation by fish of contaminants from suspended sediments. In the first experiment we compared accumulation of contaminants by yellow perch of hatchery and lake origin and found that after 10 days of exposure to nonaerated sediments, fish of hatchery origin accumulated PCBs and Fe, while fish of lake origin accumulated As, Cr, Fe, and Na. Two additional exposures were conducted to evaluate the effects of aerating the sediments prior to measuring bioavailability of associated contaminants. Fish of hatchery origin exposed to nonaerated sediments for 10 days accumulated PCBs and Hg, while fish of hatchery origin exposed to aerated sediments for 10 days accumulated PCBs, DDE, Zn, Fe, Cs, and Se. These results demonstrated not only the potential for uptake of contaminants by fish as a result of dredging but also the potential utility of fish bioassays in evaluating proposed dredging operations.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Environmental Science and Technology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"ACS Publications","publisherLocation":"Washington, D.C.","doi":"10.1021/es00102a006","usgsCitation":"Seelye, J.G., Hesselberg, R.J., and Mac, M.J., 1982, Accumulation by fish of contaminants released from dredged sediments: Environmental Science & Technology, v. 16, no. 8, p. 459-464, https://doi.org/10.1021/es00102a006.","productDescription":"p. 459-464","startPage":"459","endPage":"464","numberOfPages":"5","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":266678,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1021/es00102a006"},{"id":133255,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"16","issue":"8","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","scienceBaseUri":"4f4e4b13e4b07f02db6a353b","contributors":{"authors":[{"text":"Seelye, James G.","contributorId":69919,"corporation":false,"usgs":true,"family":"Seelye","given":"James","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":308424,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hesselberg, Robert J.","contributorId":36074,"corporation":false,"usgs":true,"family":"Hesselberg","given":"Robert","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":308423,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mac, Michael J.","contributorId":16772,"corporation":false,"usgs":true,"family":"Mac","given":"Michael","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":308422,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70011495,"text":"70011495 - 1982 - Post-middle Miocene accretion of Franciscan rocks, northwestern California.","interactions":[],"lastModifiedDate":"2013-02-24T08:41:53","indexId":"70011495","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1786,"text":"Geological Society of America Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Post-middle Miocene accretion of Franciscan rocks, northwestern California.","docAbstract":"Deformed sedimentary rocks assigned to the Franciscan assemblage in the King Range S of Cape Mendocino, N California, are dominantly deep-water argillite and sandstone occurring as thick- to thin-bedded, locally channelized marine turbidities of arkosic to andesitic volcaniclastic composition. The King Range appears to be a displaced terrane of oceanic basement overlain by Palaeogene(?) and Neogene sedimentary and igneous rocks of continental and oceanic derivation.-Authors","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Geological Society of America Bulletin","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1982)93<595:PMAOFR>2.0.CO;2","usgsCitation":"McLaughlin, R.J., Kling, S., Poore, R., McDougall, K., and Beutner, E., 1982, Post-middle Miocene accretion of Franciscan rocks, northwestern California.: Geological Society of America Bulletin, v. 93, no. 7, p. 595-605, https://doi.org/10.1130/0016-7606(1982)93<595:PMAOFR>2.0.CO;2.","startPage":"595","endPage":"605","numberOfPages":"11","costCenters":[],"links":[{"id":221116,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":268107,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1130/0016-7606(1982)93<595:PMAOFR>2.0.CO;2"}],"volume":"93","issue":"7","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a7e69e4b0c8380cd7a51c","contributors":{"authors":[{"text":"McLaughlin, R. J. 0000-0002-4390-2288","orcid":"https://orcid.org/0000-0002-4390-2288","contributorId":107271,"corporation":false,"usgs":true,"family":"McLaughlin","given":"R.","middleInitial":"J.","affiliations":[],"preferred":false,"id":361256,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kling, S.A.","contributorId":64796,"corporation":false,"usgs":true,"family":"Kling","given":"S.A.","email":"","affiliations":[],"preferred":false,"id":361254,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Poore, R.Z.","contributorId":35314,"corporation":false,"usgs":true,"family":"Poore","given":"R.Z.","email":"","affiliations":[],"preferred":false,"id":361252,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"McDougall, K.","contributorId":106260,"corporation":false,"usgs":true,"family":"McDougall","given":"K.","email":"","affiliations":[],"preferred":false,"id":361255,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Beutner, E.C.","contributorId":36220,"corporation":false,"usgs":true,"family":"Beutner","given":"E.C.","email":"","affiliations":[],"preferred":false,"id":361253,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":1000279,"text":"1000279 - 1982 - Subcellular distribution of mercury in liver of lake trout (Salvelinus namaycush)","interactions":[],"lastModifiedDate":"2016-04-01T09:13:33","indexId":"1000279","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1606,"text":"Experientia","active":true,"publicationSubtype":{"id":10}},"title":"Subcellular distribution of mercury in liver of lake trout (Salvelinus namaycush)","docAbstract":"

Mercury was found primarily (80%) in the submicroscopic material (magnification x < 7700) of environmentally exposed adult lake trout from Lake Michigan, USA.

","language":"English","publisher":"Springer","doi":"10.1007/BF01964098","usgsCitation":"Passino, D.M., and Kramer, J.M., 1982, Subcellular distribution of mercury in liver of lake trout (Salvelinus namaycush): Experientia, v. 38, no. 6, p. 689-690, https://doi.org/10.1007/BF01964098.","productDescription":"2 p.","startPage":"689","endPage":"690","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":128919,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"38","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699c04","contributors":{"authors":[{"text":"Passino, D.R. May","contributorId":30573,"corporation":false,"usgs":true,"family":"Passino","given":"D.R.","email":"","middleInitial":"May","affiliations":[],"preferred":false,"id":308328,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kramer, J. Matsumoto","contributorId":103619,"corporation":false,"usgs":true,"family":"Kramer","given":"J.","email":"","middleInitial":"Matsumoto","affiliations":[],"preferred":false,"id":308329,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70011848,"text":"70011848 - 1982 - Cyclic deposits and hummocky cross-stratification of probable storm origins in Upper Cretaceous rocks of the Cape Sebastian area, southwestern Oregon","interactions":[],"lastModifiedDate":"2024-05-21T23:43:55.063153","indexId":"70011848","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2450,"text":"Journal of Sedimentary Petrology","active":true,"publicationSubtype":{"id":10}},"title":"Cyclic deposits and hummocky cross-stratification of probable storm origins in Upper Cretaceous rocks of the Cape Sebastian area, southwestern Oregon","docAbstract":"

Cyclic deposits containing hummocky cross-stratification occur in the upper part of the Cape Sebastian Sandstone of Bourgeois (1980), a shallow marine transgressive sandstone of Late Cetaceous age on the southern Oregon coast. The cycles average 1.6 m in thickness and consist, where complete, of a lower hummocky cross-stratified sandstone, a middle planar and ripple bedded sandstone with a shale bed in its middle part, and an upper bioturbated sandstone. Noteworthy features of the hummocky cross-stratification include the presence of depositional domes in addition to scoured depressions, the absence of significant bedform migration, and the presence of a small proportion of dip angles greater than the angle of repose (>34 degrees ) in addition to the large proportion of low (<15 degrees ) dip angles. The lower, stratified, fining-upward part of the cycle (up to the top of the shale bed) is interpreted as having accumulated under conditions of initially great but gradually decreasing current velocity and deposition rate. The currents probably had a strong oscillatory component, and the depositional event is inferred to have been a storm. The part of the planar- and ripple-bedded sandstone above the shale bed was probably deposited during relatively fair weather after the storm but before re-establishment of a normal benthic fauna. The bioturbated sandstone is interpreted to have been deposited during fair weather or during minor storms separated by long intervals of fair weather.

","language":"English","publisher":"SEPM","doi":"10.1306/212F7EF5-2B24-11D7-8648000102C1865D","issn":"00224472","usgsCitation":"Hunter, R.E., and Clifton, H., 1982, Cyclic deposits and hummocky cross-stratification of probable storm origins in Upper Cretaceous rocks of the Cape Sebastian area, southwestern Oregon: Journal of Sedimentary Petrology, v. 52, no. 1, p. 127-143, https://doi.org/10.1306/212F7EF5-2B24-11D7-8648000102C1865D.","productDescription":"17 p.","startPage":"127","endPage":"143","numberOfPages":"17","costCenters":[],"links":[{"id":221620,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"52","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059fd23e4b0c8380cd4e65b","contributors":{"authors":[{"text":"Hunter, R. E.","contributorId":48148,"corporation":false,"usgs":true,"family":"Hunter","given":"R.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":362108,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Clifton, H.","contributorId":37210,"corporation":false,"usgs":true,"family":"Clifton","given":"H.","affiliations":[],"preferred":false,"id":362107,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70011830,"text":"70011830 - 1982 - Techniques for using iron crucibles in experimental igneous petrology.","interactions":[],"lastModifiedDate":"2013-02-14T09:53:10","indexId":"70011830","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":738,"text":"American Mineralogist","active":true,"publicationSubtype":{"id":10}},"title":"Techniques for using iron crucibles in experimental igneous petrology.","docAbstract":"Some iron crucibles contain impurities of Mn, Ti and other elements. Such impurities may alter the fO2 of the system and induce crucible-charge interactions. Pretreatment of impure iron crucibles in a CO2-CO atmosphere at 1050oC, under conditions slightly more reducing than Fe-Fe1-xO, minimizes undesirable changes in the bulk composition of the charge. -J.A.Z.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"American Mineralogist","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Mineralogical Society of America","issn":"0003004X","usgsCitation":"Thornber, C., and Huebner, J., 1982, Techniques for using iron crucibles in experimental igneous petrology.: American Mineralogist, v. 67, no. 11-12, p. 1144-1154.","startPage":"1144","endPage":"1154","numberOfPages":"11","costCenters":[],"links":[{"id":221392,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":267368,"type":{"id":11,"text":"Document"},"url":"https://www.minsocam.org/ammin/AM67/AM67_1144.pdf"}],"volume":"67","issue":"11-12","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505ba439e4b08c986b3201ac","contributors":{"authors":[{"text":"Thornber, C.R.","contributorId":69302,"corporation":false,"usgs":true,"family":"Thornber","given":"C.R.","email":"","affiliations":[],"preferred":false,"id":362060,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Huebner, J.S.","contributorId":41422,"corporation":false,"usgs":true,"family":"Huebner","given":"J.S.","email":"","affiliations":[],"preferred":false,"id":362059,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70006377,"text":"70006377 - 1982 - Detection of diethylnitrosamine in nitrate-rich water following treatment with Rhodamine flow tracers","interactions":[],"lastModifiedDate":"2026-03-16T16:16:12.072498","indexId":"70006377","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3716,"text":"Water Research","onlineIssn":"1879-2448","printIssn":"0043-1354","active":true,"publicationSubtype":{"id":10}},"title":"Detection of diethylnitrosamine in nitrate-rich water following treatment with Rhodamine flow tracers","docAbstract":"

Extremely carcinogenic diethylnitrosamine (DENA) was found to form in up to 75% yield from the reaction of nitrite with the two commonly used water tracing dyes. Rhodamine B and Rhodamine WT, DENA was detected at trace levels (0.13–7.02 μg −1) in river water samples after treatment with the dye and nitrite. Analysis of these chemically treated environmental water samples required extensive separation techniques prior to acquisition of reliable analytical data using highly sensitive instruments for detection. The occurrence of DENA in nitrite-rich water treated with Rhodamines may pose a health hazard to general populations.

","language":"English","publisher":"Elsevier","doi":"10.1016/0043-1354(82)90111-7","usgsCitation":"Abidi, S.L., 1982, Detection of diethylnitrosamine in nitrate-rich water following treatment with Rhodamine flow tracers: Water Research, v. 16, no. 2, p. 199-204, https://doi.org/10.1016/0043-1354(82)90111-7.","productDescription":"6 p.","startPage":"199","endPage":"204","costCenters":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":258232,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"16","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059ff73e4b0c8380cd4f1c6","contributors":{"authors":[{"text":"Abidi, S. L.","contributorId":19898,"corporation":false,"usgs":true,"family":"Abidi","given":"S.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":354414,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":95194,"text":"95194 - 1982 - The impact of entrainment and impingement on fish populations in the Hudson River estuary : Volume III : An analysis of the validity of the utilities' stock recruitment curve-fitting exercise and \"prior estimation of beta\" technique","interactions":[],"lastModifiedDate":"2012-02-02T00:03:51","indexId":"95194","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":9,"text":"Other Report"},"title":"The impact of entrainment and impingement on fish populations in the Hudson River estuary : Volume III : An analysis of the validity of the utilities' stock recruitment curve-fitting exercise and \"prior estimation of beta\" technique","docAbstract":"No abstract available at this time","language":"English","publisher":"Oak Ridge National Laboratory","publisherLocation":"Oak Ridge, TN","collaboration":"None/FC","usgsCitation":"Christensen, S., Goodyear, C., and Kirk, B., 1982, The impact of entrainment and impingement on fish populations in the Hudson River estuary : Volume III : An analysis of the validity of the utilities' stock recruitment curve-fitting exercise and \"prior estimation of beta\" technique.","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":126969,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a85e4b07f02db64d675","contributors":{"authors":[{"text":"Christensen, S.W.","contributorId":8023,"corporation":false,"usgs":true,"family":"Christensen","given":"S.W.","email":"","affiliations":[],"preferred":false,"id":298652,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Goodyear, C.P.","contributorId":11538,"corporation":false,"usgs":true,"family":"Goodyear","given":"C.P.","email":"","affiliations":[],"preferred":false,"id":298653,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kirk, B.L.","contributorId":40540,"corporation":false,"usgs":true,"family":"Kirk","given":"B.L.","email":"","affiliations":[],"preferred":false,"id":298654,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":96407,"text":"96407 - 1982 - Revised procedures for capturing and reestablishing desert bighorn","interactions":[],"lastModifiedDate":"2012-02-02T00:03:50","indexId":"96407","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Revised procedures for capturing and reestablishing desert bighorn","docAbstract":"No abstract available at this time","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Desert Bighorn Council Transactions","largerWorkSubtype":{"id":9,"text":"Other Report"},"language":"English","usgsCitation":"Wilson, L., and Douglas, C.L., 1982, Revised procedures for capturing and reestablishing desert bighorn, chap. of Desert Bighorn Council Transactions, p. 1-7.","productDescription":"p. 1-7","startPage":"1","endPage":"7","numberOfPages":"7","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":126915,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db602eab","contributors":{"authors":[{"text":"Wilson, L.L.","contributorId":44408,"corporation":false,"usgs":true,"family":"Wilson","given":"L.L.","email":"","affiliations":[],"preferred":false,"id":299587,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Douglas, C. L.","contributorId":64586,"corporation":false,"usgs":true,"family":"Douglas","given":"C.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":299588,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70011789,"text":"70011789 - 1982 - The solubilities of calcite, aragonite and vaterite in CO2-H2O solutions between 0 and 90°C, and an evaluation of the aqueous model for the system CaCO3-CO2-H2O","interactions":[],"lastModifiedDate":"2018-03-21T15:17:40","indexId":"70011789","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1759,"text":"Geochimica et Cosmochimica Acta","active":true,"publicationSubtype":{"id":10}},"title":"The solubilities of calcite, aragonite and vaterite in CO2-H2O solutions between 0 and 90°C, and an evaluation of the aqueous model for the system CaCO3-CO2-H2O","docAbstract":"

Calculations based on approximately 350 new measurements (CaT-PCO2) of the solubilities of calcite, aragonite and vaterite in CO2-H2O solutions between 0 and 90°C indicate the following values for the log of the equilibrium constants KC, KA, and KV respectively, for the reaction CaCO3(s) = Ca2+ + CO2−3: 

\n

\"\"\"\"\"\" where T is in oK. At 25°C the logarithms of the equilibrium constants are −8.480 ± 0.020, −8.336 ± 0.020 and −7.913 ± 0.020 for calcite, aragonite and vaterite, respectively.

\n

The equilibrium constants are internally consistent with an aqueous model that includes the CaHCO+3 and CaCO03 ion pairs, revised analytical expressions for CO2-H2O equilibria, and extended Debye-Hückel individual ion activity coefficients. Using this aqueous model, the equilibrium constant of aragonite shows no PCO2-dependence if the CaHCO+3 association constant is \"\"between 0 and 90°C, corresponding to the value logKCahco+3 = 1.11 ± 0.07 at 25°C. The CaCO03association constant was measured potentiometrically to be \"\" between 5 and 80°C, yielding logKCaCO03 = 3.22 ± 0.14 at 25°C.

\n

The CO2-H2O equilibria have been critically evaluated and new empirical expressions for the temperature dependence of KH, K1 and K2 are \"\", \"\"and logK2 = −107.8871 − 0.03252849T + 5151.79/T + 38.92561 logT − 563713.9/T2 which may be used to at least 250°C. These expressions hold for 1 atm. total pressure between 0 and 100°C and follow the vapor pressure curve of water at higher temperatures.

\n

Extensive measurements of the pH of Ca-HCO3 solutions at 25°C and 0.956 atm PCO2 using different compositions of the reference electrode filling solution show that measured differences in pH are closely approximated by differences in liquid-junction potential as calculated by the Henderson equation. Liquid-junction corrected pH measurements agree with the calculated pH within 0.003-0.011 pH.

\n

Earlier arguments suggesting that the CaHCO+3 ion pair should not be included in the CaCO3-CO2-H2O aqueous model were based on less accurate calcite solubility data. The CaHCO+3 ion pair must be included in the aqueous model to account for the observed PCO2-dependence of aragonite solubility between 317 ppm CO2 and 100% CO2.

\n

Previous literature on the solubility of CaCO3 polymorphs have been critically evaluated using the aqueous model and the results are compared.

","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Geochimica et Cosmochimica Acta","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/0016-7037(82)90056-4","issn":"00167037","usgsCitation":"Plummer, N., and Busenberg, E., 1982, The solubilities of calcite, aragonite and vaterite in CO2-H2O solutions between 0 and 90°C, and an evaluation of the aqueous model for the system CaCO3-CO2-H2O: Geochimica et Cosmochimica Acta, v. 46, no. 6, p. 1011-1040, https://doi.org/10.1016/0016-7037(82)90056-4.","startPage":"1011","endPage":"1040","numberOfPages":"30","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":220722,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"46","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb03ee4b08c986b324d14","contributors":{"authors":[{"text":"Plummer, Niel 0000-0002-4020-1013 nplummer@usgs.gov","orcid":"https://orcid.org/0000-0002-4020-1013","contributorId":190100,"corporation":false,"usgs":true,"family":"Plummer","given":"Niel","email":"nplummer@usgs.gov","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":361964,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Busenberg, Eurybiades ebusenbe@usgs.gov","contributorId":2271,"corporation":false,"usgs":true,"family":"Busenberg","given":"Eurybiades","email":"ebusenbe@usgs.gov","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":361963,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":1007546,"text":"1007546 - 1982 - The nomenclatural enigma of single versus double -i endings for scientific patronyms emended to represent a man's name: A comment and some considerations","interactions":[],"lastModifiedDate":"2023-12-13T11:19:17.018445","indexId":"1007546","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1657,"text":"Fisheries","onlineIssn":"1548-8446","printIssn":"0363-2415","active":true,"publicationSubtype":{"id":10}},"title":"The nomenclatural enigma of single versus double -i endings for scientific patronyms emended to represent a man's name: A comment and some considerations","docAbstract":"

The current inconsistency over the use of single vs. double -i endings for singular masculine scientific patronyms in official lists of scientific names of fishes causes needless confusion and labor. Taxonomists once preferred rules for Latinization calling for double -i endings, but current rules suggest single -i endings. Recent rulings by the International Commission of Zoological Nomenclature make it impossible to produce uniformity in this area. It is suggested that the Committee on Names of Fishes submit a petition to the Commission that modifies the present rules to allow the use of single -i endings in most cases and thus conform with current literature and the opinions of most ichthyologists.

","language":"English","publisher":"Wiley","doi":"10.1577/1548-8446(1982)007<0009:TNEOSV>2.0.CO;2","usgsCitation":"Jennings, M., 1982, The nomenclatural enigma of single versus double -i endings for scientific patronyms emended to represent a man's name: A comment and some considerations: Fisheries, v. 7, no. 5, p. 9-10, https://doi.org/10.1577/1548-8446(1982)007<0009:TNEOSV>2.0.CO;2.","productDescription":"2 p.","startPage":"9","endPage":"10","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":131588,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"7","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b46b0","contributors":{"authors":[{"text":"Jennings, M.R.","contributorId":18296,"corporation":false,"usgs":true,"family":"Jennings","given":"M.R.","email":"","affiliations":[],"preferred":false,"id":315597,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70010369,"text":"70010369 - 1982 - Towards locating earthquakes in a laterally heterogeneous medium","interactions":[],"lastModifiedDate":"2013-02-13T13:36:00","indexId":"70010369","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","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":"Towards locating earthquakes in a laterally heterogeneous medium","docAbstract":"[No abstract available]","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(82)90100-5","issn":"00319201","usgsCitation":"Buland, R.P., 1982, Towards locating earthquakes in a laterally heterogeneous medium: Physics of the Earth and Planetary Interiors, v. 30, no. 2-3, p. 157-160, https://doi.org/10.1016/0031-9201(82)90100-5.","startPage":"157","endPage":"160","numberOfPages":"4","costCenters":[],"links":[{"id":267341,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0031-9201(82)90100-5"},{"id":219686,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"30","issue":"2-3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb5c0e4b08c986b326895","contributors":{"authors":[{"text":"Buland, Raymond P.","contributorId":69294,"corporation":false,"usgs":true,"family":"Buland","given":"Raymond","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":358756,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1004127,"text":"1004127 - 1982 - Chlamydiosis in 2 biologists investigating disease occurrences in wild waterfowl","interactions":[],"lastModifiedDate":"2018-02-27T16:52:57","indexId":"1004127","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3779,"text":"Wildlife Society Bulletin","onlineIssn":"1938-5463","printIssn":"0091-7648","active":true,"publicationSubtype":{"id":10}},"title":"Chlamydiosis in 2 biologists investigating disease occurrences in wild waterfowl","docAbstract":"

Chlamydiosis (ornithosis, psittacosis) is an infectious disease of birds that can be transmitted to humans. Human infections are probably acquired by inhalation of aerosols containing elementary bodies of the causative agent Chlamydia psittaci, from bird droppings, or from tissues. Infected birds do not have to be ill to transmit the organism (Schachter and Dawson 1978). The disease in humans is considered an occupational risk for people working with pet birds (particularly psittacine species) and poultry, but all avian species can be considered as potential reservoirs (Schachter and Dawson 1978). Burkhart and Page (1971) listed >130 species of wild birds as being infected.

The purpose of this report is to draw the disease to the attention of those working with wild birds by describing 2 cases acquired from wild waterfowl and by reviewing other information on human infections associated with wild birds. We do this because the disease can be serious if not treated properly, and because the disease is not usually associated with wild birds the diagnosis may not be considered by physicians without some prompting from the patient.

","language":"English","publisher":"Wiley","usgsCitation":"Wobeser, G., and Brand, C.J., 1982, Chlamydiosis in 2 biologists investigating disease occurrences in wild waterfowl: Wildlife Society Bulletin, v. 10, no. 2, p. 170-172.","productDescription":"3 p.","startPage":"170","endPage":"172","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"links":[{"id":135723,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":15346,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://www.jstor.org/stable/3781740","linkFileType":{"id":5,"text":"html"},"description":"3554.000000000000000"}],"country":"Canada, United States of America","state":"California, Manitoba, Saskatchewan, Texas, Wisconsin","otherGeospatial":"Aransas National Wildlife 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\"}}]}","volume":"10","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49c2e4b07f02db5d3cf0","contributors":{"authors":[{"text":"Wobeser, Gary","contributorId":120268,"corporation":false,"usgs":false,"family":"Wobeser","given":"Gary","email":"","affiliations":[{"id":13248,"text":"University of Saskatchewan","active":true,"usgs":false}],"preferred":false,"id":315230,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brand, Christopher J. cbrand@usgs.gov","contributorId":1186,"corporation":false,"usgs":true,"family":"Brand","given":"Christopher","email":"cbrand@usgs.gov","middleInitial":"J.","affiliations":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"preferred":true,"id":315231,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":2002363,"text":"2002363 - 1982 - Effects of soils and grazing on breeding birds of uncultivated upland grasslands of the Northern Great Plains","interactions":[],"lastModifiedDate":"2017-12-29T12:47:33","indexId":"2002363","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":99,"text":"Wildlife Research Report","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"15","title":"Effects of soils and grazing on breeding birds of uncultivated upland grasslands of the Northern Great Plains","docAbstract":"The principal use of uncultivated upland grasslands in the northern Great Plains is for livestock production. However, on lands set aside for wildlife or for scientific or recreational use, grazing by livestock may be used as a management measure to enhance populations of game species or to create conditions that increase the diversity of plant or animal species. To determine the effects of grazing on the avifauna of various types of Great Plains grasslands, we conducted bird censuses and plant surveys during 1974-78 on 615 plots of lightly, moderately, or heavily grazed native rangeland.Numbers of horned lark (Eremophila alpestris), western meadowlark (Sturnella neglecta), lark bunting (Calamospiza melanocorys), and chestnut-collared longspur (Calcarius ornatus) accounted for 65-75% of the total bird population, regardless of grazing intensity. For the entire area sampled (600,000 km2), horned lark, western meadowlark, and chestnut-collared longspur were the dominant birds. Major differences in composition of the dominant species and species richness occurred among the major soils. Increased mean annual soil temperature seemingly had a greater negative influence on avian species richness than did decreased soil moisture or organic matter content. Differences in total bird density were not significant among soils and among grazing intensities within most soils. For the area as a whole, light or moderate grazing resulted in increased species richness. Of the 29 species studied, 2 responded significantly to grazing for the area as a whole and 6 others to grazing on the soil in which peak densities occurred. Response of several other species to grazing effects evidently varied among strata.A list of plants with mean cover values of more than 1% in any of the 18 combinations of soils and grazing intensities contained less than 25 species, attesting to the relative simplicity of the grassland vegetation in the northern Great Plains. Agropyron spp. and Bouteloua gracilis were the dominant plants that provided greater than average cover on the best habitat for the most bird species. Optimum habitat for each bird species is given in terms of grazing, soils, and dominant plant species. Increased soil temperature probably had a negative effect on plant species richness, especially among soils with a high organic matter content that supported perennial grasses and other mesophytes.","language":"English","publisher":"U.S. Fish and Wildlife Service","publisherLocation":"Washington, DC","usgsCitation":"Kantrud, H., and Kologiski, R., 1982, Effects of soils and grazing on breeding birds of uncultivated upland grasslands of the Northern Great Plains: Wildlife Research Report 15, 33 p.","productDescription":"33 p.","startPage":"0","endPage":"33","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":199139,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":94289,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://hdl.handle.net/2027/mdp.39015012634674?urlappend=%3Bseq=459"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a28e4b07f02db610b2b","contributors":{"authors":[{"text":"Kantrud, H.A.","contributorId":28553,"corporation":false,"usgs":true,"family":"Kantrud","given":"H.A.","email":"","affiliations":[],"preferred":false,"id":326511,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kologiski, R.L.","contributorId":28213,"corporation":false,"usgs":true,"family":"Kologiski","given":"R.L.","affiliations":[],"preferred":false,"id":326510,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":1007551,"text":"1007551 - 1982 - Status and distribution of ants in the Crater District of Haleakala National Park","interactions":[],"lastModifiedDate":"2020-10-01T18:49:16.389843","indexId":"1007551","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2990,"text":"Pacific Science","active":true,"publicationSubtype":{"id":10}},"title":"Status and distribution of ants in the Crater District of Haleakala National Park","docAbstract":"

The Crater District of Haleakala National Park was surveyed for ants. Three species were found. Argentine ants (Iridomyrmex humilis) occurred only within I km of the park headquarters and the nearby research facility. Hypoponera opaciceps was found in small numbers throughout the Crater District. Cardiocondyla emeryi was present only at the head of Kaupo Gap. Possible impacts of these ant species on the endemic, flightless insects of the park are discussed.

","language":"English","publisher":"University of Hawaii","usgsCitation":"Fellers, J., and Fellers, G.M., 1982, Status and distribution of ants in the Crater District of Haleakala National Park: Pacific Science, v. 36, no. 4, p. 427-437.","productDescription":"11 p.","startPage":"427","endPage":"437","numberOfPages":"11","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":131678,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":378969,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://scholarspace.manoa.hawaii.edu/handle/10125/476"}],"country":"United States","state":"Hawaii","otherGeospatial":"Haleakala National Park","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -156.25717163085938,\n 20.580081709180345\n ],\n [\n -156.01547241210938,\n 20.580081709180345\n ],\n [\n -156.01547241210938,\n 20.78693059257028\n ],\n [\n -156.25717163085938,\n 20.78693059257028\n ],\n [\n -156.25717163085938,\n 20.580081709180345\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"36","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66ca1e","contributors":{"authors":[{"text":"Fellers, JoanH","contributorId":48915,"corporation":false,"usgs":true,"family":"Fellers","given":"JoanH","email":"","affiliations":[],"preferred":false,"id":315605,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fellers, Gary M. 0000-0003-4092-0285 gary_fellers@usgs.gov","orcid":"https://orcid.org/0000-0003-4092-0285","contributorId":3150,"corporation":false,"usgs":true,"family":"Fellers","given":"Gary","email":"gary_fellers@usgs.gov","middleInitial":"M.","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":true,"id":315604,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ]}