{"pageNumber":"5148","pageRowStart":"128675","pageSize":"25","recordCount":184569,"records":[{"id":70014060,"text":"70014060 - 1984 - Monitoring unrest in a large silicic caldera, the long Valley-inyo craters volcanic complex in east-central California","interactions":[],"lastModifiedDate":"2012-03-12T17:19:29","indexId":"70014060","displayToPublicDate":"1984-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1093,"text":"Bulletin Volcanologique","active":true,"publicationSubtype":{"id":10}},"title":"Monitoring unrest in a large silicic caldera, the long Valley-inyo craters volcanic complex in east-central California","docAbstract":"Recent patterns of geologic unrest in long Valley caldera in east-central California emphasize that this large, silicic volcanic system and the adjacent, geologically youthful Inyo-Mono Craters volcanic chain are still active and capable of producing locally hazardous volcanic eruptions. A series of four magnitude -6 earthquakes in May 1980 called attention to this current episode of unrest, and subsequent activity has included numerous earthquake swarms in the south moat of the caldera accompanied by inflation of the resurgent dome by more than 50 cm over the last five years. The seismicity associated with this unrest is currently monitored by a network of 31 telemetered seismic stations with an automatic processing system that yelds hypocentral locations and earthquake magnitudes in near-real time. Deformation of the ground is monitored by a) a series of overlapping trilateration networks that provide coverage ranging from annual measurements of regional deformation to daily measurements of deformation local to the active, southern section of the caldera, b) a regional network of level lines surveyed annually, c) a regional network of precise gravity stations occupied annually, d) local, L-shaped level figures surveyed every few months, and e) a network of fourteen borehole tiltmeter clusters (two instruments in each cluster) and a borehole dilatometer, the telemetered signals from which provide continuous data on deformation rates. Additional telemetered data provide continuous information on fluctuations in the local magnetic field, hydrogen gas emission rates at three sites, and water level and temperatures in three wells. Continuous data on disharge rates and temperatures from hot springs and fumaroles are collected by several on-site recorders within the caldera, and samples for liquid and gas chemistry are collected several times per year from selected hot springs and fumaroles. ?? 1984 Intern. Association of Volcanology and Chemistry of the Earth's Interior.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Bulletin Volcanologique","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisherLocation":"Springer-Verlag","doi":"10.1007/BF01961568","issn":"02588900","usgsCitation":"Hill, D., 1984, Monitoring unrest in a large silicic caldera, the long Valley-inyo craters volcanic complex in east-central California: Bulletin Volcanologique, v. 47, no. 2, p. 371-395, https://doi.org/10.1007/BF01961568.","startPage":"371","endPage":"395","numberOfPages":"25","costCenters":[],"links":[{"id":205622,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF01961568"},{"id":225357,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"47","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a5df9e4b0c8380cd70704","contributors":{"authors":[{"text":"Hill, D.P.","contributorId":27432,"corporation":false,"usgs":true,"family":"Hill","given":"D.P.","email":"","affiliations":[],"preferred":false,"id":367473,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70013179,"text":"70013179 - 1984 - Low-temperature heat capacities of CaAl2SiO6 glass and pyroxene and thermal expansion of CaAl2SiO6 pyroxene.","interactions":[],"lastModifiedDate":"2012-03-12T17:18:35","indexId":"70013179","displayToPublicDate":"1984-01-01T00:00:00","publicationYear":"1984","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":"Low-temperature heat capacities of CaAl2SiO6 glass and pyroxene and thermal expansion of CaAl2SiO6 pyroxene.","docAbstract":"Low-T heat capacities (5-380 K) have been measured by adiabatic calorimetry for synthetic CaAl2SiO6 glass and pyroxene. High-T unit cell parameters were measured for CaAl2SiO6 pyroxene by means of a Nonius Guinier-Lenne powder camera in order to determine the mean coefficient of thermal expansion in the T range 25-1200oC. -J.A.Z.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"American Mineralogist","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"0003004X","usgsCitation":"Haselton, H., Hemingway, B.S., and Robie, R.A., 1984, Low-temperature heat capacities of CaAl2SiO6 glass and pyroxene and thermal expansion of CaAl2SiO6 pyroxene.: American Mineralogist, v. 69, no. 5-6, p. 481-489.","startPage":"481","endPage":"489","numberOfPages":"9","costCenters":[],"links":[{"id":220411,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"69","issue":"5-6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a4a5fe4b0c8380cd68cfd","contributors":{"authors":[{"text":"Haselton, H.T. Jr.","contributorId":83520,"corporation":false,"usgs":true,"family":"Haselton","given":"H.T.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":365482,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hemingway, B. S.","contributorId":7268,"corporation":false,"usgs":true,"family":"Hemingway","given":"B.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":365480,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Robie, R. A.","contributorId":71237,"corporation":false,"usgs":true,"family":"Robie","given":"R.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":365481,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70013982,"text":"70013982 - 1984 - Casto Ring Zone: A 4,500-km2 fossil hydrothermal system in the Challis Volcanic Field, central Idaho","interactions":[],"lastModifiedDate":"2024-01-30T12:33:15.63151","indexId":"70013982","displayToPublicDate":"1984-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1796,"text":"Geology","active":true,"publicationSubtype":{"id":10}},"title":"Casto Ring Zone: A 4,500-km2 fossil hydrothermal system in the Challis Volcanic Field, central Idaho","docAbstract":"

δ18O analyses of granitic and volcanic rocks reveal the largest hydrothermal system ever documented around a single granite pluton, occupying a 4,500-km2 area in central Idaho. The remains of this meteoric-hydrothermal system are principally preserved within a sharply bounded, 15-km-wide, 70-km-diameter annulus of low δ18O rock (+2.0 to −8.8‰) termed the Casto Ring Zone. The zone centered on a less depleted (+4.5) core zone consisting of granitic rocks of the Casto pluton. This 700-km2 Eocene subvolcanic batholith has intruded, domed, and hydrothermally metamorphosed a thick sequence of Challis Volcanics, the stratigraphically low rocks in the 2,000-km2 Van Horn Peak and the 1,000-km2 Thunder Mountain cauldron complexes being most strongly altered. Less extreme 18O depletions occur in the youngest major ash-flow sheets of these complexes, indicating a vertical 18O gradient. Water/rock ratios of geothermal systems are surprisingly insensitive to the circulation scale.

","language":"English","publisher":"Geological Society of America","doi":"10.1130/0091-7613(1984)12<331:CRZAKF>2.0.CO;2","issn":"00917613","usgsCitation":"Criss, R., Ekren, E.B., and Hardyman, R., 1984, Casto Ring Zone: A 4,500-km2 fossil hydrothermal system in the Challis Volcanic Field, central Idaho: Geology, v. 12, no. 6, p. 331-334, https://doi.org/10.1130/0091-7613(1984)12<331:CRZAKF>2.0.CO;2.","productDescription":"4 p.","startPage":"331","endPage":"334","numberOfPages":"4","costCenters":[],"links":[{"id":225226,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"12","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f391e4b0c8380cd4b8b7","contributors":{"authors":[{"text":"Criss, R.E.","contributorId":10075,"corporation":false,"usgs":true,"family":"Criss","given":"R.E.","email":"","affiliations":[],"preferred":false,"id":367308,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ekren, E. B.","contributorId":14371,"corporation":false,"usgs":true,"family":"Ekren","given":"E.","middleInitial":"B.","affiliations":[],"preferred":false,"id":367309,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hardyman, R.F.","contributorId":35326,"corporation":false,"usgs":true,"family":"Hardyman","given":"R.F.","affiliations":[],"preferred":false,"id":367310,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70013223,"text":"70013223 - 1984 - Thermodynamic properties of zeolites: low-temperature heat capacities and thermodynamic functions for phillipsite and clinoptilolite. Estimates of the thermochemical properties of zeolitic water at low temperature.","interactions":[],"lastModifiedDate":"2012-03-12T17:18:38","indexId":"70013223","displayToPublicDate":"1984-01-01T00:00:00","publicationYear":"1984","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":"Thermodynamic properties of zeolites: low-temperature heat capacities and thermodynamic functions for phillipsite and clinoptilolite. Estimates of the thermochemical properties of zeolitic water at low temperature.","docAbstract":"Measured heat capacities between 15 and 305 K and calculated heat capacities, entropies, enthalpy functions and Gibbs energy functions are reported and analysed for phillipsite and clinoptilolite. - J.A.Z.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"American Mineralogist","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"0003004X","usgsCitation":"Hemingway, B.S., and Robie, R.A., 1984, Thermodynamic properties of zeolites: low-temperature heat capacities and thermodynamic functions for phillipsite and clinoptilolite. Estimates of the thermochemical properties of zeolitic water at low temperature.: American Mineralogist, v. 69, no. 7-8, p. 692-700.","startPage":"692","endPage":"700","numberOfPages":"9","costCenters":[],"links":[{"id":220131,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"69","issue":"7-8","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb27be4b08c986b325820","contributors":{"authors":[{"text":"Hemingway, B. S.","contributorId":7268,"corporation":false,"usgs":true,"family":"Hemingway","given":"B.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":365574,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Robie, R. A.","contributorId":71237,"corporation":false,"usgs":true,"family":"Robie","given":"R.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":365575,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70013225,"text":"70013225 - 1984 - Application of mineral-solution equilibria to geochemical exploration for sandstone-hosted uranium deposits in two basins in west central Utah","interactions":[],"lastModifiedDate":"2024-01-11T16:24:07.535841","indexId":"70013225","displayToPublicDate":"1984-01-01T00:00:00","publicationYear":"1984","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":"Application of mineral-solution equilibria to geochemical exploration for sandstone-hosted uranium deposits in two basins in west central Utah","docAbstract":"

A geochemical survey utilizing mainly ground waters was conducted in the Milford and Beaver basins. Waters were collected mainly from wells and springs at 100 sites and analyzed for major and minor elements. A computer model (WATEQ3) was used to calculate the redox potential and the state of saturation of the waters with respect to uraninite, coffinite, and other mineral phases. Several areas in the basins were shown to have ground-water environments of reducing redox potentials which are favorable for precipitation of reduced uranium minerals. In addition, the ground waters in some of these areas were shown to be saturated or near saturation with respect to uraninite and coffinite. These areas do not necessarily coincide with areas containing the highest concentrations of uranium in ground water. The methods described in this study for hydrogeochemical exploration for sandstone-hosted uranium deposits may have wide application, particularly throughout those filled basins in the western United States where nearby sources for uranium exist.

","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.79.2.266","issn":"03610128","usgsCitation":"Miller, W.R., Wanty, R., and McHugh, J.B., 1984, Application of mineral-solution equilibria to geochemical exploration for sandstone-hosted uranium deposits in two basins in west central Utah: Economic Geology, v. 79, no. 2, p. 266-283, https://doi.org/10.2113/gsecongeo.79.2.266.","productDescription":"18 p.","startPage":"266","endPage":"283","numberOfPages":"18","costCenters":[],"links":[{"id":220133,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"79","issue":"2","noUsgsAuthors":false,"publicationDate":"1984-04-01","publicationStatus":"PW","scienceBaseUri":"5059eca7e4b0c8380cd493ec","contributors":{"authors":[{"text":"Miller, W. R.","contributorId":92239,"corporation":false,"usgs":true,"family":"Miller","given":"W.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":365580,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wanty, R. B. 0000-0002-2063-6423","orcid":"https://orcid.org/0000-0002-2063-6423","contributorId":66704,"corporation":false,"usgs":true,"family":"Wanty","given":"R. B.","affiliations":[],"preferred":false,"id":365578,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McHugh, J. B.","contributorId":79462,"corporation":false,"usgs":true,"family":"McHugh","given":"J.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":365579,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":3401,"text":"cir896D - 1984 - Earthquakes in the United States, October-December 1982","interactions":[],"lastModifiedDate":"2023-10-26T20:22:35.005596","indexId":"cir896D","displayToPublicDate":"1984-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"896","chapter":"D","title":"Earthquakes in the United States, October-December 1982","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir896D","usgsCitation":"Stover, C.W., Minsch, J.H., Baldwin, F.W., and Brewer, L.R., 1984, Earthquakes in the United States, October-December 1982: U.S. Geological Survey Circular 896, iv, 33 p., https://doi.org/10.3133/cir896D.","productDescription":"iv, 33 p.","costCenters":[],"links":[{"id":117983,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1984/0896d/report-thumb.jpg"},{"id":30418,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1984/0896d/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":420384,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_23729.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n 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H.","contributorId":27035,"corporation":false,"usgs":true,"family":"Minsch","given":"J.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":146828,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Baldwin, F. W.","contributorId":32905,"corporation":false,"usgs":true,"family":"Baldwin","given":"F.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":146830,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Brewer, L. 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A mineral-resource survey of the area done between 1976 and 1979 found no evidence fore metallic mineral resources. Kyanite, garnet, and building stone are the only mineral resources in the study area, but large quantities of similar material are available outside the study area. Natural gas may possibly be present at great depth, but until some deep drilling is done in or near no estimate of the gas potential can be made.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Wilderness mineral potential: assessment of mineral-resource potential in U.S. Forest Service lands studied in 1964-1984: Volume II (Professional Paper 1300)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","usgsCitation":"Lesure, F.G., and Williams, B.B., 1984, Craggy Mountain Wilderness Study Area and Extension, North Carolina, chap. of Wilderness mineral potential: assessment of mineral-resource potential in U.S. Forest Service lands studied in 1964-1984: Volume II (Professional Paper 1300), v. 2, p. 843-844.","productDescription":"2 p.","startPage":"843","endPage":"844","numberOfPages":"2","costCenters":[],"links":[{"id":225223,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":278634,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1300/report.pdf"}],"country":"United States","state":"North Carolina","otherGeospatial":"Great Craggy Mountain","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -82.416667,35.683333 ], [ -82.416667,35.75 ], [ -82.35,35.75 ], [ -82.35,35.683333 ], [ -82.416667,35.683333 ] ] ] } } ] }","volume":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f2e4e4b0c8380cd4b477","contributors":{"authors":[{"text":"Lesure, Frank G.","contributorId":20068,"corporation":false,"usgs":true,"family":"Lesure","given":"Frank","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":367304,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Williams, Bradford B.","contributorId":6864,"corporation":false,"usgs":true,"family":"Williams","given":"Bradford","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":367303,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70013278,"text":"70013278 - 1984 - Calculations of seabird population recovery from potential oilspills in the mid-Atlantic region of the United States","interactions":[],"lastModifiedDate":"2023-09-29T16:50:52.832258","indexId":"70013278","displayToPublicDate":"1984-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1458,"text":"Ecological Modelling","active":true,"publicationSubtype":{"id":10}},"title":"Calculations of seabird population recovery from potential oilspills in the mid-Atlantic region of the United States","docAbstract":"

Calculations were made of herring gull and common tern population recovery from potential oilspill damage in the U.S. mid-Atlantic Outer Continental Shelf (OCS) oil leasing area. Population recovery was examined using a density-dependent age-specific life history table for each species. Both a deterministic and a stochastic approach were used in the calculations. In the deterministic approach, it was assumed that an oilspill contact to a seabird colony had occurred. Using the density-dependent model, population recovery was calculated for several different mortality scenarios. Assuming that all age classes suffer 95% mortality from an oilspill contact, a worst case scenario, it was estimated that the herring gull and common tern populations could recover to their pre-spill levels in approximately 45 years and more than 100 years, respectively. In the stochastic approach, the probabilities of oilspill contacts to these seabird colonies were calculated using an oilspill trajectory analysis model. Oilspill contacts to these colonies were simulated during the expected 30 year active life of the lease area. For each lease lifetime, the number of oilspill contacts to a seabird colony was sampled from a Poisson distribution and assigned randomly on a seasonal basis. This analysis indicated that the oilspill risks from the development of proposed lease tracts in the mid-Atlantic region pose minimal risk (3–5%) of severe population reduction for both herring gulls and common terns. If the oilspill risks from tanker transportation of crude oil imports are included along with the proposed lease tracts, then the risks of severe population reduction are increased to approximately 10% for herring gulls and 18% for common terns.

","language":"English","publisher":"Elsevier","doi":"10.1016/0304-3800(84)90025-5","usgsCitation":"Samuels, W., and Ladino, A., 1984, Calculations of seabird population recovery from potential oilspills in the mid-Atlantic region of the United States: Ecological Modelling, v. 21, no. 1, p. 63-84, https://doi.org/10.1016/0304-3800(84)90025-5.","productDescription":"22 p.","startPage":"63","endPage":"84","numberOfPages":"22","costCenters":[],"links":[{"id":219970,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","otherGeospatial":"Mid-Atlantic region","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -75.78218772294734,\n 41.41847066117498\n ],\n [\n -76.9461477045258,\n 34.39258601480289\n ],\n [\n -71.60300062228816,\n 34.993219485756725\n ],\n [\n -71.60300062228816,\n 41.41847066117498\n ],\n [\n -75.78218772294734,\n 41.41847066117498\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"21","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f307e4b0c8380cd4b56f","contributors":{"authors":[{"text":"Samuels, William B.","contributorId":13238,"corporation":false,"usgs":true,"family":"Samuels","given":"William B.","affiliations":[],"preferred":false,"id":365709,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ladino, A.","contributorId":6186,"corporation":false,"usgs":true,"family":"Ladino","given":"A.","email":"","affiliations":[],"preferred":false,"id":365708,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70013978,"text":"70013978 - 1984 - Eulerian-Lagrangian solution of the convection-dispersion equation in natural coordinates","interactions":[],"lastModifiedDate":"2018-02-12T17:31:59","indexId":"70013978","displayToPublicDate":"1984-01-01T00:00:00","publicationYear":"1984","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":"Eulerian-Lagrangian solution of the convection-dispersion equation in natural coordinates","docAbstract":"

The vast majority of numerical investigations of transport phenomena use an Eulerian formulation for the convenience that the computational grids are fixed in space. An Eulerian-Lagrangian method (ELM) of solution for the convection-dispersion equation is discussed and analyzed. The ELM uses the Lagrangian concept in an Eulerian computational grid system. The values of the dependent variable off the grid are calculated by interpolation. When a linear interpolation is used, the method is a slight improvement over the upwind difference method. At this level of approximation both the ELM and the upwind difference method suffer from large numerical dispersion. However, if second-order Lagrangian polynomials are used in the interpolation, the ELM is proven to be free of artificial numerical dispersion for the convection-dispersion equation. The concept of the ELM is extended for treatment of anisotropic dispersion in natural coordinates. In this approach the anisotropic properties of dispersion can be conveniently related to the properties of the flow field. Several numerical examples are given to further substantiate the results of the present analysis.

","language":"English","publisher":"American Geophysical Union","doi":"10.1029/WR020i007p00944","usgsCitation":"Cheng, R.T., Casulli, V., and Milford, S.N., 1984, Eulerian-Lagrangian solution of the convection-dispersion equation in natural coordinates: Water Resources Research, v. 20, no. 7, p. 944-952, https://doi.org/10.1029/WR020i007p00944.","productDescription":"9 p.","startPage":"944","endPage":"952","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":226262,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"20","issue":"7","noUsgsAuthors":false,"publicationDate":"2010-07-09","publicationStatus":"PW","scienceBaseUri":"505a0bcbe4b0c8380cd528a0","contributors":{"authors":[{"text":"Cheng, Ralph T.","contributorId":69134,"corporation":false,"usgs":true,"family":"Cheng","given":"Ralph","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":367300,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Casulli, Vincenzo","contributorId":42302,"corporation":false,"usgs":true,"family":"Casulli","given":"Vincenzo","email":"","affiliations":[],"preferred":false,"id":367301,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Milford, S. Nevil","contributorId":92438,"corporation":false,"usgs":false,"family":"Milford","given":"S.","email":"","middleInitial":"Nevil","affiliations":[],"preferred":false,"id":367302,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70013977,"text":"70013977 - 1984 - PLANNING FOR OPTICAL DISK TECHNOLOGY WITH DIGITAL CARTOGRAPHY.","interactions":[],"lastModifiedDate":"2012-03-12T17:19:33","indexId":"70013977","displayToPublicDate":"1984-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"PLANNING FOR OPTICAL DISK TECHNOLOGY WITH DIGITAL CARTOGRAPHY.","docAbstract":"Progress in the computer field continues to suggest that the transition from traditional analog mapping systems to digital systems has become a practical possibility. A major shortfall that still exists in digital systems is the need for very large mass storage capacity. The decade of the 1980's has introduced laser optical disk storage technology, which may be the breakthrough needed for mass storage. This paper addresses system concepts for digital cartography during the transition period. Emphasis is placed on determining U. S. Geological Survey mass storage requirements and introducing laser optical disk technology for handling storage problems for digital data in this decade.","conferenceTitle":"Technical Papers - 1984 ACSM-ASP Fall Convention.","conferenceLocation":"San Antonio, TX, USA","language":"English","publisher":"American Soc of Photogrammetry and American Congress on Surveying & Mapping","publisherLocation":"Falls Church, VA, USA","isbn":"0937294594","usgsCitation":"Light, D.L., 1984, PLANNING FOR OPTICAL DISK TECHNOLOGY WITH DIGITAL CARTOGRAPHY., Technical Papers - 1984 ACSM-ASP Fall Convention., San Antonio, TX, USA, p. 453-467.","startPage":"453","endPage":"467","numberOfPages":"15","costCenters":[],"links":[{"id":226261,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a735fe4b0c8380cd76fcb","contributors":{"authors":[{"text":"Light, Donald L.","contributorId":28011,"corporation":false,"usgs":true,"family":"Light","given":"Donald","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":367299,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70013913,"text":"70013913 - 1984 - Metamorphic history of a high-grade blueschist exotic block from the Franciscan complex, California","interactions":[],"lastModifiedDate":"2024-06-04T21:19:28.976517","indexId":"70013913","displayToPublicDate":"1984-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2420,"text":"Journal of Petrology","active":true,"publicationSubtype":{"id":10}},"title":"Metamorphic history of a high-grade blueschist exotic block from the Franciscan complex, California","docAbstract":"

A high-grade blueschist tectonic block from the Franciscan Complex of the northeast Diablo Range shows evidence of three episodes of retrograde blueschist facies metamorphism ± deformation developed under progressively declining P-T conditions. The first retrograde metamorphism involved formation of an outer rind of actinolite + chlorite + rutile ± phengite, and the growth of coarse-grained chlorite + pumpellyite within the block. During the second event the rind and outer edge of the blueschist were folded, sheared and fractured, and primary glaucophane within the blueschist was replaced by albite, medium-grained chlorite, and glaucophane-crossite. The third retrograde metamorphism was marked by the pseudomorphic replacement of rind actinolite by aragonite and quartz. Aragonite also crystallized extensively within th block, accompanied by lawsonite, chlorite, jadeitic pyroxene, and crossite; this last mineral assemblage is identical to that of the surrounding Franciscan metasedimentary rocks. Features characteristic of the first and second retrograde metamorphic events are readily observed in other high-grade tectonic blocks of the Franciscan Complex and the correlative Otter Point Formation of Oregon. In contrast, evidence of a third retrograde metamorphism, matching that of presently associated Franciscan and Otter Point rocks, has been found in some but not all blocks examined so far.

The high P/T conditions of prograde metamorphism and the available metamorphic age determinations suggest that the tectonic blocks originally formed in a pre-Franciscan subduction zone setting. Fragments of blueschist and eclogite from this metamorphic terrain were tectonically incorporated in a serpentinite diapir, and they developed alteration rinds through interaction with the enclosing ultramafic rock. The available data suggest that the examined exotic block and at least some others were transferred to the Franciscan as detritus from a body of serpentinite that reached the earth's surface. Such blocks were then resubducted and metamorphosed along with their presently associated sedimentary sequences.

","language":"English","publisher":"Oxford Academic","doi":"10.1093/petrology/25.1.126","issn":"00223530","usgsCitation":"Moore, D., 1984, Metamorphic history of a high-grade blueschist exotic block from the Franciscan complex, California: Journal of Petrology, v. 25, no. 1, p. 126-150, https://doi.org/10.1093/petrology/25.1.126.","productDescription":"25 p.","startPage":"126","endPage":"150","numberOfPages":"25","costCenters":[],"links":[{"id":226191,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"25","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a54fee4b0c8380cd6d0c5","contributors":{"authors":[{"text":"Moore, Diane E. 0000-0002-8641-1075","orcid":"https://orcid.org/0000-0002-8641-1075","contributorId":106496,"corporation":false,"usgs":true,"family":"Moore","given":"Diane E.","affiliations":[],"preferred":false,"id":367152,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70013912,"text":"70013912 - 1984 - TOPOLOGICAL STRUCTURING OF RASTER-SCANNED LINE MAP DATA.","interactions":[],"lastModifiedDate":"2012-03-12T17:19:33","indexId":"70013912","displayToPublicDate":"1984-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"TOPOLOGICAL STRUCTURING OF RASTER-SCANNED LINE MAP DATA.","docAbstract":"The U. S. Geological Survey has a requirement for the collection of large amounts of digital map data from existing graphic map separates. Prototype production techniques have been developed to capture line data from the map separates using a raster-scanning input device. After minimal editing in raster form, the data are converted to 'unstructured' vector form. In order to be processed further, the line data must be topologically structured (nodes identified and start-node, end-node, area-left, and area-right tags associated with each line-segment chain). This paper describes the techniques which have been developed at the U. S. Geological Survey to topologically structure the raster-scanned line map data.","largerWorkTitle":"Technical Papers of the American Congress of Surveying and Mapping","conferenceTitle":"Technical Papers of the 44th Annual Meeting of the American Congress on Surveying and Mapping.","conferenceLocation":"Washington, DC, USA","language":"English","publisher":"American Congress on Surveying & Mapping","publisherLocation":"Falls Church, VA, USA","issn":"07483244","usgsCitation":"Fegeas, R.G., and Pearsall, R.A., 1984, TOPOLOGICAL STRUCTURING OF RASTER-SCANNED LINE MAP DATA., in Technical Papers of the American Congress of Surveying and Mapping, Washington, DC, USA, p. 264-272.","startPage":"264","endPage":"272","numberOfPages":"9","costCenters":[],"links":[{"id":226190,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505ba38fe4b08c986b31fd66","contributors":{"authors":[{"text":"Fegeas, Robin G.","contributorId":27033,"corporation":false,"usgs":true,"family":"Fegeas","given":"Robin","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":367150,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pearsall, Richard A.","contributorId":93208,"corporation":false,"usgs":true,"family":"Pearsall","given":"Richard","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":367151,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":1003917,"text":"1003917 - 1984 - Avian cholera in Nebraska's Rainwater Basin","interactions":[],"lastModifiedDate":"2022-08-17T16:38:37.373948","indexId":"1003917","displayToPublicDate":"1984-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3638,"text":"Transactions of the North American Wildlife and Natural Resources Conference","active":true,"publicationSubtype":{"id":10}},"title":"Avian cholera in Nebraska's Rainwater Basin","docAbstract":"

The first report of avian cholera in North America occurred in northwestern Texas in winter 1944 (Quortrup et al. 1946). In 1975, mortality from avian cholera occurred for the first time in waterfowl in the Rainwater Basin of Nebraska when an estimated 25,000 birds died (Zinkl et al. 1977). Avian cholera has continued to cause mortality in wild birds in specific areas of the Basin each spring since. Losses of waterfowl from avian cholera continue to be much greater in some of the wetlands in the western part of the Basin than in the east. Several wetlands in the west have consistently higher mortality and are most often the wetlands where initial mortality is noticed each spring (Figure 1). The establishment of this disease in Nebraska is of considerable concern because of the importance of the Rainwater Basin as a spring staging area for waterfowl migrating to their breeding grounds. The wetlands in this area are on a major migration route used by an estimated 5 to 9 million ducks and several hundred thousand geese. A large portion of the western mid-continental greater white-fronted goose (Anser albifrons) population stage in the Basin each spring. Occasionally, whooping cranes (Grus americana) use these wetlands during migration, and lesser sandhill cranes (Grus canadensis) staging on the nearby Platte River sometimes use wetlands where avian cholera occurs (Anonymous 1981). Our objectives were to determine whether certain water quality variables in the Rainwater Basin differed between areas of high and low avian cholera incidence. These results would then be used for laboratory studies involving the survivability of Pasteurella multocida, the causative bacterium of avian cholera. Those studies will be reported elsewhere.

","language":"English","publisher":"Wildlife Management Institute","usgsCitation":"Windingstad, R.M., Hurt, J.J., Trout, A.K., and Cary, J., 1984, Avian cholera in Nebraska's Rainwater Basin: Transactions of the North American Wildlife and Natural Resources Conference, v. 49, p. 576-583.","productDescription":"8 p.","startPage":"576","endPage":"583","numberOfPages":"8","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"links":[{"id":135845,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United 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\"}}]}","volume":"49","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e484de4b07f02db4fbf42","contributors":{"authors":[{"text":"Windingstad, Ronald M.","contributorId":46046,"corporation":false,"usgs":true,"family":"Windingstad","given":"Ronald","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":314646,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hurt, J. J.","contributorId":93854,"corporation":false,"usgs":true,"family":"Hurt","given":"J.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":314647,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Trout, A. K.","contributorId":12019,"corporation":false,"usgs":true,"family":"Trout","given":"A.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":314644,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Cary, J.","contributorId":37305,"corporation":false,"usgs":true,"family":"Cary","given":"J.","email":"","affiliations":[],"preferred":false,"id":314645,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70013905,"text":"70013905 - 1984 - Moho orientation beneath central California from regional earthquake travel times","interactions":[],"lastModifiedDate":"2020-03-24T14:07:24","indexId":"70013905","displayToPublicDate":"1984-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2312,"text":"Journal of Geophysical Research","active":true,"publicationSubtype":{"id":10}},"title":"Moho orientation beneath central California from regional earthquake travel times","docAbstract":"This paper examines relative Pn arrival times, recorded by the U. S. Geological Survey seismic network in central and northern California from an azimuthally distributed set of regional earthquakes. Improved estimates are presented of upper mantle velocities in the Coast Ranges, Great Valley, and Sierra Nevada foothills and estimates of the orientation of the Moho throughout this region. Finally, the azimuthal distribution of apparent velocities, corrected for dip and individual station travel time effects, is then studied for evidence of upper mantle velocity anisotropy and for indications of lower crustal structure in central California.","language":"English","publisher":"Wiley","doi":"10.1029/JB089iB12p10267","issn":"01480227","usgsCitation":"Oppenheimer, D.H., and Eaton, J.P., 1984, Moho orientation beneath central California from regional earthquake travel times: Journal of Geophysical Research, v. 89, no. B12, p. 10267-10282, https://doi.org/10.1029/JB089iB12p10267.","productDescription":"16 p.","startPage":"10267","endPage":"10282","numberOfPages":"16","costCenters":[],"links":[{"id":226053,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","otherGeospatial":"Central California","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -123.35449218749997,\n 35.42486791930558\n ],\n [\n -118.34472656249997,\n 35.42486791930558\n ],\n [\n -118.34472656249997,\n 39.639537564366684\n ],\n [\n -123.35449218749997,\n 39.639537564366684\n ],\n [\n -123.35449218749997,\n 35.42486791930558\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"89","issue":"B12","noUsgsAuthors":false,"publicationDate":"2012-09-20","publicationStatus":"PW","scienceBaseUri":"505a4ae9e4b0c8380cd6913b","contributors":{"authors":[{"text":"Oppenheimer, David H. oppen@usgs.gov","contributorId":1112,"corporation":false,"usgs":true,"family":"Oppenheimer","given":"David","email":"oppen@usgs.gov","middleInitial":"H.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":367136,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Eaton, Jerry P.","contributorId":22341,"corporation":false,"usgs":true,"family":"Eaton","given":"Jerry","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":367137,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70013893,"text":"70013893 - 1984 - Gas chromatographic analysis of volatiles in fluid and gas inclusions","interactions":[],"lastModifiedDate":"2017-05-03T16:02:39","indexId":"70013893","displayToPublicDate":"1984-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2214,"text":"Journal of Chromatography A","active":true,"publicationSubtype":{"id":10}},"title":"Gas chromatographic analysis of volatiles in fluid and gas inclusions","docAbstract":"

Most geological samples and some synthetic materials contain fluid inclusions. These inclusions preserve for us tiny samples of the liquid and/or the gas phase that was present during formation, although in some cases they may have undergone significant changes from the original material. Studies of the current composition of the inclusions provide data on both the original composition and the change since trapping.

These inclusions are seldom larger than 1 millimeter in diameter. The composition varies from a single major compound (e.g., water) in a single phase to a very complex mixture in one or more phases. The concentration of some of the compounds present may be at trace levels.

We present here some analyses of inclusions in a variety of geological samples, including diamonds. We used a sample crusher and a gas chromatography—mass spectrometry (GC—MS) system to analyze for organic and inorganic volatiles present as major to trace constituents in inclusions. The crusher is a hardened stainless-steel piston cylinder apparatus with tungsten carbide crusing surfaces, and is operated in a pure helium atmosphere at a controlled temperature.

Samples ranging from 1 mg to 1 g were crushed and the released volatiles were analyzed using multi-chromatographic columns and detectors, including the sensitive helium ionization detector. Identification of the GC peaks was carried out by GC—MS. This combination of procedures has been shown to provide geochemically useful information on the process involved in the history of the samples analyzed.

","language":"English","publisher":"Elsevier","doi":"10.1016/S0021-9673(01)89010-5","issn":"00219673","usgsCitation":"Andrawes, F., Holzer, G., Roedder, E., Gibson, E., and Oro, J., 1984, Gas chromatographic analysis of volatiles in fluid and gas inclusions: Journal of Chromatography A, v. 302, no. C, p. 181-193, https://doi.org/10.1016/S0021-9673(01)89010-5.","startPage":"181","endPage":"193","numberOfPages":"13","costCenters":[],"links":[{"id":225860,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"302","issue":"C","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a14c3e4b0c8380cd54b59","contributors":{"authors":[{"text":"Andrawes, F.","contributorId":102643,"corporation":false,"usgs":true,"family":"Andrawes","given":"F.","email":"","affiliations":[],"preferred":false,"id":367110,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Holzer, G.","contributorId":93206,"corporation":false,"usgs":true,"family":"Holzer","given":"G.","email":"","affiliations":[],"preferred":false,"id":367108,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Roedder, E.","contributorId":100986,"corporation":false,"usgs":true,"family":"Roedder","given":"E.","affiliations":[],"preferred":false,"id":367109,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Gibson, E.K. Jr.","contributorId":108256,"corporation":false,"usgs":true,"family":"Gibson","given":"E.K.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":367111,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Oro, John","contributorId":21683,"corporation":false,"usgs":false,"family":"Oro","given":"John","email":"","affiliations":[{"id":33349,"text":"Department of Biophysical Science, University of Houston","active":true,"usgs":false}],"preferred":false,"id":367107,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":70187185,"text":"70187185 - 1984 - The Big Cypress Swamp","interactions":[],"lastModifiedDate":"2017-04-25T17:45:52","indexId":"70187185","displayToPublicDate":"1984-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"The Big Cypress Swamp","docAbstract":"

No abstract available 

","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Environments of South Florida, present and past","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Miami Geological Society","usgsCitation":"McPherson, B.F., 1984, The Big Cypress Swamp, chap. of Environments of South Florida, present and past, p. 69-78.","productDescription":"10 p. ","startPage":"69","endPage":"78","costCenters":[],"links":[{"id":340417,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"59006083e4b0e85db3a5df22","contributors":{"authors":[{"text":"McPherson, B. F.","contributorId":62983,"corporation":false,"usgs":true,"family":"McPherson","given":"B.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":692964,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70013282,"text":"70013282 - 1984 - Bedding types in Holocene tidal channel sequences, Knik Arm, Upper Cook Inlet, Alaska","interactions":[],"lastModifiedDate":"2024-05-21T23:27:45.975971","indexId":"70013282","displayToPublicDate":"1984-01-01T00:00:00","publicationYear":"1984","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":"Bedding types in Holocene tidal channel sequences, Knik Arm, Upper Cook Inlet, Alaska","docAbstract":"

Uplifted convoluted and horizontal to subhorizontal beds of varying thickness in intertidal silt as old as 3,280 + or - 90 yr B.P. are exposed in the banks of tidal channels of unknown depth in the intertidal zone in Knik Arm of Upper Cook Inlet. Internal discordances may occur both within convoluted beds and between convoluted and horizontal to subhorizontal beds. At the base of many convoluted beds, there is a rapid gradation upward into laminae which are severely deformed; that is, in some places, the contortions appear to have originated along a single bedding plane. Where the convoluted sequences are truncated by nearly horizontal sequences, the distortion must have resulted from syndepositional or postdepositional events prior to their burial by the overlying beds. Various forms of gravitational and tidal processes caused the deformation of the Knik Arm deposits; events triggering the movement of the sediment include any or all of the following: (1) seismic activity, (2) sediment or ice loading, (3) wave-induced liquefaction, (4) pore-pressure changes brought on by changing levels of tidewater, (5) undercutting of sediments by channel migration, and (6) freezing and thawing.

","largerWorkType":{"id":2,"text":"Article"},"language":"English","publisher":"SEPM","doi":"10.1306/212F85AD-2B24-11D7-8648000102C1865D","issn":"00224472","usgsCitation":"Bartsch-Winkler, S., and Schmoll, H., 1984, Bedding types in Holocene tidal channel sequences, Knik Arm, Upper Cook Inlet, Alaska: Journal of Sedimentary Petrology, v. 54, no. 4, p. 1239-1250, https://doi.org/10.1306/212F85AD-2B24-11D7-8648000102C1865D.","productDescription":"12 p.","startPage":"1239","endPage":"1250","numberOfPages":"12","costCenters":[],"links":[{"id":220026,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"54","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f03fe4b0c8380cd4a68f","contributors":{"authors":[{"text":"Bartsch-Winkler, S.","contributorId":31388,"corporation":false,"usgs":true,"family":"Bartsch-Winkler","given":"S.","affiliations":[],"preferred":false,"id":365716,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schmoll, H. R.","contributorId":71543,"corporation":false,"usgs":true,"family":"Schmoll","given":"H. R.","affiliations":[],"preferred":false,"id":365717,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70013895,"text":"70013895 - 1984 - Volcanic glasses, their origins and alteration processes","interactions":[],"lastModifiedDate":"2012-03-12T17:19:34","indexId":"70013895","displayToPublicDate":"1984-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2400,"text":"Journal of Non-Crystalline Solids","active":true,"publicationSubtype":{"id":10}},"title":"Volcanic glasses, their origins and alteration processes","docAbstract":"Natural glass can be formed by volcanic processes, lightning (fulgarites) burning coal, and by meteorite impact. By far the most common process is volcanic - basically the glass is rapidly chilled molten rock. All natural glasses are thermodynamically unstable and tend to alter chemically or to crystallize. The rate of these processes is determined by the chemical composition of the magma. The hot and fluid basaltic melts have a structure that allows for rapid crystal growth, and seldom forms glass selvages greater than a few centimeters thick, even when the melt is rapidly cooled by extrusion in the deep sea. In contrast the cooler and very viscous rhyolitic magmas can yield bodies of glass that are tens of meters thick. These highly polymerized magmas have a high silica content - often 71-77% SiO2. Their high viscosity inhibits diffusive crystal growth. Basalt glass in sea water forms an alteration zone called palagonite whose thickness increases linearly with time. The rate of diffusion of water into rhyolitic glass, which follows the relationship - thickness = k (time) 1 2, has been determined as a function of the glass composition and temperature. Increased SiO2 increases the rate, whereas increased CaO, MgO and H2O decrease the rate. The activation energy of water diffusion varies from about 19 to 22 kcal/mol. for the glasses studied. The diffusion of alkali out of rhyolite glass occurs simultaneously with water diffusion into the glass. The rate of devitrification of rhyolitic glass is a function of the glass viscosity, which in turn is a function of water content and temperature. Although all of the aforementioned processes tend to destroy natural glasses, the slow rates of these processes, particularly for rhyolitic glass, has allowed samples of glass to persist for 60 million years. ?? 1984.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Non-Crystalline Solids","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"00223093","usgsCitation":"Friedman, I., and Long, W., 1984, Volcanic glasses, their origins and alteration processes: Journal of Non-Crystalline Solids, v. 67, no. 1-3, p. 127-133.","startPage":"127","endPage":"133","numberOfPages":"7","costCenters":[],"links":[{"id":225921,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"67","issue":"1-3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bc2ede4b08c986b32ae5b","contributors":{"authors":[{"text":"Friedman, I.","contributorId":95596,"corporation":false,"usgs":true,"family":"Friedman","given":"I.","email":"","affiliations":[],"preferred":false,"id":367115,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Long, W.","contributorId":59963,"corporation":false,"usgs":true,"family":"Long","given":"W.","email":"","affiliations":[],"preferred":false,"id":367114,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":2000021,"text":"2000021 - 1984 - Population dynamics and species interactions","interactions":[],"lastModifiedDate":"2023-04-07T14:43:05.519916","indexId":"2000021","displayToPublicDate":"1984-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":3,"text":"Organization Series"},"seriesTitle":{"id":222,"text":"Technical Report","active":false,"publicationSubtype":{"id":3}},"seriesNumber":"40","title":"Population dynamics and species interactions","docAbstract":"

No abstract available.

","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Strategies for rehabilitation of lake trout in the Great Lakes: Proceedings of a conference on lake trout research, August 1983","largerWorkSubtype":{"id":3,"text":"Organization Series"},"language":"English","publisher":"Great Lakes Fishery Commission","usgsCitation":"Hatch, R.W., 1984, Population dynamics and species interactions: Technical Report 40, 6 p.","productDescription":"6 p.","startPage":"4","endPage":"9","numberOfPages":"6","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":199083,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":92048,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://www.glfc.org/glfc-publications-reports.php","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad6e4b07f02db684196","contributors":{"authors":[{"text":"Hatch, Richard W.","contributorId":82245,"corporation":false,"usgs":true,"family":"Hatch","given":"Richard","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":324939,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70195043,"text":"70195043 - 1984 - Relationship of fluviodeltaic facies to coal deposition in the lower Fort Union formation (Palaeocene), south-western North Dakota","interactions":[],"lastModifiedDate":"2018-02-05T16:56:06","indexId":"70195043","displayToPublicDate":"1984-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"seriesTitle":{"id":5617,"text":"Special Publication of the International Association of Sedimentologists","active":true,"publicationSubtype":{"id":24}},"seriesNumber":"7","chapter":"10","title":"Relationship of fluviodeltaic facies to coal deposition in the lower Fort Union formation (Palaeocene), south-western North Dakota","docAbstract":"

Facies analysis of the Ludlow and Tongue River Members of the Palaeocene Fort Union Formation provides an understanding of the relationship between fluviodeltaic environments and associated coal deposition in the south-western Williston Basin. The Ludlow Member consists of high-constructive delta facies that interfinger with brackish-water tongues of the Cannonball Member of the Fort Union Formation. The lower part of the Ludlow Member was deposited on a lower delta plain that consisted of interdistributary crevasse and subdelta lobes. The upper part of the Ludlow Member was deposited in meander belts of the upper delta plain. The delta plain facies of the Ludlow Member is overlain by alluvial plain facies consisting of swamp, crevasse-lobe, lacustrine, and trunk meander belt deposits of the Tongue River Member. The Ludlow delta is believed to have been fed by fluvial systems that probably flowed from the Powder River Basin to the Williston Basin undeterred by the Cedar Creek Anticline. However, the evidence indicates that the Cedar Creek Anticline was prominent enough, during early Tongue River Member deposition, to cause the obstruction of the regional fluvial system flowing from the SW, and the formation of local drainage.

The Ludlow Member contains 18 coal beds in the area studied, of which the T-Cross and Yule coals are as thick as 4 m (12 ft). Abandoned delta lobes served as platforms where coals formed, which in turn, were drowned by mainly fresh water and subordinate brackish water. Repetition of deltaic sedimentation, abandonment, and occupation by swamp led to preservation of the T-Cross and Oyster coals in areas as extensive as 260 km2 (< 100 miles2).

","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Sedimentology of coal and coal-bearing sequences","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"The International Association of Sedimentologists","doi":"10.1002/9781444303797.ch10","isbn":"9780632012862","usgsCitation":"Belt, E.S., Flores, R.M., Warwick, P.D., Conway, K., Johnson, K.R., and Waskowitz, R.S., 1984, Relationship of fluviodeltaic facies to coal deposition in the lower Fort Union formation (Palaeocene), south-western North Dakota, chap. 10 of Sedimentology of coal and coal-bearing sequences: Special Publication of the International Association of Sedimentologists, p. 177-195, https://doi.org/10.1002/9781444303797.ch10.","productDescription":"19 p.","startPage":"177","endPage":"195","costCenters":[],"links":[{"id":351032,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"North Dakota","noUsgsAuthors":false,"publicationDate":"2009-04-28","publicationStatus":"PW","scienceBaseUri":"5a797b98e4b00f54eb1f5e2d","contributors":{"editors":[{"text":"Rahmani, R.A.","contributorId":119467,"corporation":false,"usgs":false,"family":"Rahmani","given":"R.A.","email":"","affiliations":[],"preferred":false,"id":726727,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Flores, Romeo M. rflores@usgs.gov","contributorId":71984,"corporation":false,"usgs":true,"family":"Flores","given":"Romeo","email":"rflores@usgs.gov","middleInitial":"M.","affiliations":[{"id":165,"text":"Central Energy Resources Team","active":false,"usgs":true}],"preferred":false,"id":726728,"contributorType":{"id":2,"text":"Editors"},"rank":2}],"authors":[{"text":"Belt, Edward S.","contributorId":96422,"corporation":false,"usgs":false,"family":"Belt","given":"Edward","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":726729,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Flores, Romeo M. rflores@usgs.gov","contributorId":71984,"corporation":false,"usgs":true,"family":"Flores","given":"Romeo","email":"rflores@usgs.gov","middleInitial":"M.","affiliations":[{"id":165,"text":"Central Energy Resources Team","active":false,"usgs":true}],"preferred":false,"id":726730,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Warwick, Peter D. 0000-0002-3152-7783 pwarwick@usgs.gov","orcid":"https://orcid.org/0000-0002-3152-7783","contributorId":762,"corporation":false,"usgs":true,"family":"Warwick","given":"Peter","email":"pwarwick@usgs.gov","middleInitial":"D.","affiliations":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true}],"preferred":false,"id":726731,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Conway, Kevin M.","contributorId":64949,"corporation":false,"usgs":false,"family":"Conway","given":"Kevin M.","affiliations":[],"preferred":false,"id":726732,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Johnson, Kirk R.","contributorId":16877,"corporation":false,"usgs":true,"family":"Johnson","given":"Kirk","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":726733,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Waskowitz, Robert S.","contributorId":67069,"corporation":false,"usgs":false,"family":"Waskowitz","given":"Robert","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":726734,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}} ,{"id":2000660,"text":"2000660 - 1984 - Brown blood disease (methemoglobinemia) of fishes","interactions":[],"lastModifiedDate":"2012-02-02T00:14:58","indexId":"2000660","displayToPublicDate":"1984-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":22,"text":"Fish Disease Leaflet","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"70","title":"Brown blood disease (methemoglobinemia) of fishes","docAbstract":"No abstract available at this time","language":"English","publisher":"U.S. Fish and Wildlife Service","collaboration":"751/FH","usgsCitation":"Bowser, P., 1984, Brown blood disease (methemoglobinemia) of fishes: Fish Disease Leaflet 70, 6 p.","productDescription":"6 p.","startPage":"0","endPage":"6","numberOfPages":"6","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":112249,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://hdl.handle.net/2027/coo.31924000778476?urlappend=%3Bseq=347"},{"id":198722,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fb2e1","contributors":{"authors":[{"text":"Bowser, P.R.","contributorId":17935,"corporation":false,"usgs":true,"family":"Bowser","given":"P.R.","email":"","affiliations":[],"preferred":false,"id":325196,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70194901,"text":"70194901 - 1984 - Social organization of sea otters in Prince William Sound, Alaska","interactions":[],"lastModifiedDate":"2018-01-26T17:33:24","indexId":"70194901","displayToPublicDate":"1984-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1176,"text":"Canadian Journal of Zoology","active":true,"publicationSubtype":{"id":10}},"title":"Social organization of sea otters in Prince William Sound, Alaska","docAbstract":"

Sea otters in Prince William Sound. Alaska, were spatially segregated into predominantly (97%) male areas at the front of the expanding population and breeding areas with fewer (up to 33%) males. From 1975 to 1984 we captured and marked 267 otters with tags and (or) radio transmitters and investigated their reproductive strategies, social relationships, and patterns of sexual segregation. Mating occurred year-round, but peaked in September and October. Females first bred at 4 years of age and were capable of pupping annually; they generally separated from their pup before mating. Males established breeding territories that enabled prolonged precopulatory interactions that may have prompted female–pup separation and post-copulatory interactions that precluded females from mating with other males. Male mating success was related to age, weight, territory quality, and the length of time they maintained their territory. After the breeding season, territorial males returned to male areas where food was more abundant. Young, dispersing males also entered male areas and remained there until attaining breeding age. In male areas, otters commonly rested in groups of >50 individuals. Gregariousness promoted social interactions and likely enhanced food finding and (historically) predator protection. As food diminished, males moved into adjacent, unoccupied regions; females then occupied former male areas.

","language":"English","publisher":"NRC Research Press","doi":"10.1139/z84-385","usgsCitation":"Garshelis, D., Johnson, A.M., and Garshelis, J.A., 1984, Social organization of sea otters in Prince William Sound, Alaska: Canadian Journal of Zoology, v. 62, no. 12, p. 2648-2658, https://doi.org/10.1139/z84-385.","productDescription":"11 p.","startPage":"2648","endPage":"2658","costCenters":[],"links":[{"id":350732,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Prince William Sound","volume":"62","issue":"12","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5a6c4ca1e4b06e28e9cabb46","contributors":{"authors":[{"text":"Garshelis, David L.","contributorId":89457,"corporation":false,"usgs":true,"family":"Garshelis","given":"David L.","affiliations":[],"preferred":false,"id":726046,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Johnson, Ancel M.","contributorId":91543,"corporation":false,"usgs":false,"family":"Johnson","given":"Ancel","email":"","middleInitial":"M.","affiliations":[{"id":6987,"text":"U.S. Fish and Wildlife Sevice","active":true,"usgs":false}],"preferred":false,"id":726047,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Garshelis, Judith A.","contributorId":76386,"corporation":false,"usgs":false,"family":"Garshelis","given":"Judith","email":"","middleInitial":"A.","affiliations":[{"id":12644,"text":"University of Minnesota, St. Paul","active":true,"usgs":false}],"preferred":false,"id":726048,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70194922,"text":"70194922 - 1984 - Unsaturated-zone instrumentation in coarse alluvial deposits of the Amargosa Desert near Beatty, Nevada","interactions":[],"lastModifiedDate":"2018-01-30T08:30:10","indexId":"70194922","displayToPublicDate":"1984-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":9,"text":"Other Report"},"seriesNumber":"CONF-8409115","title":"Unsaturated-zone instrumentation in coarse alluvial deposits of the Amargosa Desert near Beatty, Nevada","docAbstract":"

No abstract available.

","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Proceedings, sixth annual participants' information meeting (U.S. Department of Energy Low-Level Waste Management Program, CONF-8409115)","largerWorkSubtype":{"id":1,"text":"Federal Government Series"},"conferenceTitle":"Sixth Annual Participants' Information Meeting","language":"English","publisher":"U.S. Department of Commerce","usgsCitation":"Morgan, D.S., and Fischer, J., 1984, Unsaturated-zone instrumentation in coarse alluvial deposits of the Amargosa Desert near Beatty, Nevada, 14 p.","productDescription":"14 p.","startPage":"617","endPage":"630","costCenters":[{"id":465,"text":"Nevada Water Science Center","active":true,"usgs":true}],"links":[{"id":350770,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Nevada","county":"Nye County","city":"Beatty","otherGeospatial":"Amargosa Desert","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5a7192bce4b0a9a2e9dbe0f4","contributors":{"authors":[{"text":"Morgan, D. S.","contributorId":19184,"corporation":false,"usgs":true,"family":"Morgan","given":"D.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":726128,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fischer, J.M. 0000-0003-2996-9272","orcid":"https://orcid.org/0000-0003-2996-9272","contributorId":74419,"corporation":false,"usgs":true,"family":"Fischer","given":"J.M.","affiliations":[],"preferred":false,"id":726129,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70194896,"text":"70194896 - 1984 - Animals as indicators of ecosystem responses to air emissions","interactions":[],"lastModifiedDate":"2018-01-26T16:36:48","indexId":"70194896","displayToPublicDate":"1984-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1547,"text":"Environmental Management","active":true,"publicationSubtype":{"id":10}},"title":"Animals as indicators of ecosystem responses to air emissions","docAbstract":"

With existing and proposed air-quality regulations, ecological disasters resulting from air emissions such as those observed at Copperhill, Tennessee, and Sudbury, Ontario, are unlikely. Current air-quality standards, however, may not protect ecosystems from subacute and chronic exposure to air emissions. The encouragement of the use of coal for energy production and the development of the fossil-fuel industries, including oil shales, tar sands, and coal liquification, point to an increase and spread of fossil-fuel emissions and the potential to influence a number of natural ecosystems. This paper reviews the reported responses of ecosystems to air-borne pollutants and discusses the use of animals as indicators of ecosystem responses to these pollutants. Animal species and populations can act as important indicators of biotic and abiotic responses of aquatic and terrestrial ecosystems. These responses can indicate long-term trends in ecosystem health and productivity, chemical cycling, genetics, and regulation. For short-term trends, fish and wildlife also serve as monitors of changes in community structure, signaling food-web contamination, as well as providing a measure of ecosystem vitality. Information is presented to show not only the importance of animals as indicators of ecosystem responses to air-quality degradation, but also their value as air-pollution indices, that is, as air-quality-related values (AQRV), required in current air-pollution regulation.

","language":"English","publisher":"Springer","doi":"10.1007/BF01868030","usgsCitation":"Newman, J.R., and Schreiber, R.K., 1984, Animals as indicators of ecosystem responses to air emissions: Environmental Management, v. 8, no. 4, p. 309-324, https://doi.org/10.1007/BF01868030.","productDescription":"16 p.","startPage":"309","endPage":"324","costCenters":[],"links":[{"id":350726,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"8","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5a6c4ca1e4b06e28e9cabb48","contributors":{"authors":[{"text":"Newman, James R.","contributorId":91907,"corporation":false,"usgs":true,"family":"Newman","given":"James","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":726016,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schreiber, R. Kent","contributorId":58145,"corporation":false,"usgs":true,"family":"Schreiber","given":"R.","email":"","middleInitial":"Kent","affiliations":[],"preferred":false,"id":726017,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":2000837,"text":"2000837 - 1984 - Aeromonas hydrophila and motile aeromonad septicemias of fish","interactions":[],"lastModifiedDate":"2012-02-02T00:14:58","indexId":"2000837","displayToPublicDate":"1984-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":22,"text":"Fish Disease Leaflet","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"68","title":"Aeromonas hydrophila and motile aeromonad septicemias of fish","docAbstract":"No abstract available at this time","language":"English","publisher":"U.S. Fish and Wildlife Service","collaboration":"586/FH","usgsCitation":"Cipriano, R.C., Bullock, G.L., and Pyle, S.W., 1984, Aeromonas hydrophila and motile aeromonad septicemias of fish: Fish Disease Leaflet 68, 23 p.","productDescription":"23 p.","startPage":"0","endPage":"23","numberOfPages":"23","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":198568,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db689c11","contributors":{"authors":[{"text":"Cipriano, R. C.","contributorId":12400,"corporation":false,"usgs":true,"family":"Cipriano","given":"R.","middleInitial":"C.","affiliations":[],"preferred":false,"id":325242,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bullock, G. L.","contributorId":69498,"corporation":false,"usgs":true,"family":"Bullock","given":"G.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":325243,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Pyle, S. W.","contributorId":86720,"corporation":false,"usgs":true,"family":"Pyle","given":"S.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":325244,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ]}