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This difference is illustrated using carbon isotope data from freshwater and terrestrial snails, ahermatypic corals, and chemoautotrophic and methanotrophic pelecypods. Literature data from fish otoliths and bird and mammal shell and bone carbonates are also considered.</p><p>Environmental CO<sub>2</sub>/O<sub>2</sub><span>&nbsp;</span>ratios appear to be the major controlling variable. Atmospheric CO<sub>2</sub>/O<sub>2</sub><span>&nbsp;</span>ratios are about thirty times lower than in most natural waters, hence air breathing animals absorb less environmental CO<sub>2</sub><span>&nbsp;</span>in the course of obtaining 0<sub>2</sub>. Tissue CO<sub>2</sub><span>&nbsp;</span>therefore, does not isotopically equilibrate with environmental CO<sub>2</sub><span>&nbsp;</span>as thoroughly in air breathers as in aquatic animals, and this is reflected in skeletal carbonates. Animals having efficient oxygen transport systems, such as vertebrates, also accumulate more respired CO<sub>2</sub><span>&nbsp;</span>in their tissues.</p><p>Photosynthetic corals calcify mainly during the daytime when photosynthetic CO<sub>2</sub><span>&nbsp;</span>uptake is several times faster than respiratory CO<sub>2</sub><span>&nbsp;</span>release. Photosynthesis, therefore, affects skeletal<span>&nbsp;</span><i>δ</i><sup>13</sup>C more strongly than does respiration. Corals also illustrate how “metabolic” effects on skeletal isotopic composition can be estimated, despite the presence of much larger “kinetic” isotope effects.</p></div></div></div><ul id=\"issue-navigation\" class=\"issue-navigation u-margin-s-bottom u-bg-grey1\"></ul>","language":"English","publisher":"Elsevier","doi":"10.1016/S0016-7037(96)00361-4","issn":"00167037","usgsCitation":"McConnaughey, T., Burdett, J., Whelan, J.F., and Paull, C.K., 1997, Carbon isotopes in biological carbonates: Respiration and photosynthesis: Geochimica et Cosmochimica Acta, v. 61, no. 3, p. 611-622, https://doi.org/10.1016/S0016-7037(96)00361-4.","productDescription":"12 p.","startPage":"611","endPage":"622","costCenters":[],"links":[{"id":228040,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Nevada","otherGeospatial":"Ash Meadows, Spring Mountains","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  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T.A.","contributorId":105444,"corporation":false,"usgs":true,"family":"McConnaughey","given":"T.A.","email":"","affiliations":[],"preferred":false,"id":385179,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Burdett, J.","contributorId":103019,"corporation":false,"usgs":true,"family":"Burdett","given":"J.","email":"","affiliations":[],"preferred":false,"id":385178,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Whelan, J. F.","contributorId":45328,"corporation":false,"usgs":true,"family":"Whelan","given":"J.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":385176,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Paull, C. K.","contributorId":86845,"corporation":false,"usgs":false,"family":"Paull","given":"C.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":385177,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70020191,"text":"70020191 - 1997 - Soft-sediment deformation structures interpreted as seismites in the uppermost Aptian to lowermost Albian transgressive deposits of the Chihuahua basin (Mexico)","interactions":[],"lastModifiedDate":"2012-03-12T17:20:19","indexId":"70020191","displayToPublicDate":"1997-01-01T00:00:00","publicationYear":"1997","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1795,"text":"Geologische Rundschau","active":true,"publicationSubtype":{"id":10}},"title":"Soft-sediment deformation structures interpreted as seismites in the uppermost Aptian to lowermost Albian transgressive deposits of the Chihuahua basin (Mexico)","docAbstract":"Several levels of soft-sediment deformation structures (s.-s.d.s.) cut by synsedimentary normal faults have been observed in the transition beds between the \"Las Vigas\" and \"La Virgen\" formations (Cretaceous) in the northeastern part of the Chihuahua basin in Mexico. These structures consisted of four kinds of motifs (floating breccias, flame-like structures, large pillow structures, and wavy structures). They are restricted to five \"stratigraphic\" levels (??1-??5) and surrounded by undeformed beds in fluvio-lacustrine and tidal deposits and can be traced over a distance of several hundred meters. This deformation is interpreted to have resulted from the combined effects of liquidization and shear stress in soft-sediments due to local earthquakes in the area which could have been generated during the rifting stage of the Chihuahua basin. New constraints placed on the age of the \"Las Vigas\" Formation (bracketed by Late Aptian charophytes at the bottom and colomiellids of late Aptian to earliest Albian age at the top) suggest that this synrift tectonism lasted at least until the end of the Aptian.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Geologische Rundschau","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"00167835","usgsCitation":"Blanc, E.J., Blanc-Aletru, M.#., and Mojon, P.#., 1997, Soft-sediment deformation structures interpreted as seismites in the uppermost Aptian to lowermost Albian transgressive deposits of the Chihuahua basin (Mexico): Geologische Rundschau, v. 86, no. 4, p. 875-883.","startPage":"875","endPage":"883","numberOfPages":"9","costCenters":[],"links":[{"id":231357,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"86","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b91d8e4b08c986b319b39","contributors":{"authors":[{"text":"Blanc, E. J.-P.","contributorId":54372,"corporation":false,"usgs":true,"family":"Blanc","given":"E.","email":"","middleInitial":"J.-P.","affiliations":[],"preferred":false,"id":385322,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Blanc-Aletru, M. #NAME?","contributorId":72974,"corporation":false,"usgs":true,"family":"Blanc-Aletru","given":"M.","email":"","middleInitial":"#NAME?","affiliations":[],"preferred":false,"id":385323,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mojon, P. #NAME?","contributorId":25321,"corporation":false,"usgs":false,"family":"Mojon","given":"P.","email":"","middleInitial":"#NAME?","affiliations":[],"preferred":false,"id":385321,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70020109,"text":"70020109 - 1997 - Stochastic point-source modeling of ground motions in the Cascadia region","interactions":[],"lastModifiedDate":"2025-07-28T16:29:42.241608","indexId":"70020109","displayToPublicDate":"1997-01-01T00:00:00","publicationYear":"1997","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3372,"text":"Seismological Research Letters","onlineIssn":"1938-2057","printIssn":"0895-0695","active":true,"publicationSubtype":{"id":10}},"title":"Stochastic point-source modeling of ground motions in the Cascadia region","docAbstract":"A stochastic model is used to develop preliminary ground motion relations for the Cascadia region for rock sites. The model parameters are derived from empirical analyses of seismographic data from the Cascadia region. The model is based on a Brune point-source characterized by a stress parameter of 50 bars. The model predictions are compared to ground-motion data from the Cascadia region and to data from large earthquakes in other subduction zones. The point-source simulations match the observations from moderate events (M < 7) in the Cascadia region. The simulations predict a steeper attenuation than observed for very large subduction events (M ??? 7.5) in other regions; motions are overpredicted near the earthquake source and underpredicted at large distances (>100 km). The discrepancy at large magnitudes suggests further work on modeling finite-fault effects and regional attenuation is warranted. In the meantime, the preliminary equations are satisfactory for predicting motions from events of M < 7 and provide conservative estimates of motions from larger events at distances less than 100 km.","language":"English","publisher":"GeoScienceWorld","doi":"10.1785/gssrl.68.1.74","issn":"00128287","usgsCitation":"Atkinson, G.M., and Boore, D.M., 1997, Stochastic point-source modeling of ground motions in the Cascadia region: Seismological Research Letters, v. 68, no. 1, p. 74-85, https://doi.org/10.1785/gssrl.68.1.74.","productDescription":"12 p,","startPage":"74","endPage":"85","costCenters":[],"links":[{"id":228157,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Canada, United States","state":"Washington","otherGeospatial":"British Columbia","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -131.4115268298872,\n              54.611818856599086\n            ],\n            [\n              -131.4115268298872,\n              42.202387991274804\n            ],\n            [\n              -121.759124118769,\n              42.202387991274804\n            ],\n            [\n              -121.759124118769,\n              54.611818856599086\n            ],\n            [\n              -131.4115268298872,\n              54.611818856599086\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"68","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b984de4b08c986b31bf70","contributors":{"authors":[{"text":"Atkinson, G. M.","contributorId":69283,"corporation":false,"usgs":true,"family":"Atkinson","given":"G.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":385056,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Boore, David M. boore@usgs.gov","contributorId":2509,"corporation":false,"usgs":true,"family":"Boore","given":"David","email":"boore@usgs.gov","middleInitial":"M.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":false,"id":385055,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70020150,"text":"70020150 - 1997 - Assessing hydrogeochemical heterogeneity in natural and constructed wetlands","interactions":[],"lastModifiedDate":"2019-02-13T06:49:06","indexId":"70020150","displayToPublicDate":"1997-01-01T00:00:00","publicationYear":"1997","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1007,"text":"Biogeochemistry","active":true,"publicationSubtype":{"id":10}},"title":"Assessing hydrogeochemical heterogeneity in natural and constructed wetlands","docAbstract":"While 'water quality function' is cited as an important wetland function to design for and preserve, we demonstrate that the scale at which hydrochemical samples are collected can significantly influence interpretations of biogeochemical processes in wetlands. Subsurface, chemical profiles for both nutrients and major ions were determined at a site in southwestern Wisconsin that contained areas of both natural and constructed wetlands. Sampling was conducted on three different scales: (1) a large scale (3 m between sampling points), (2) an intermediate scale (0.15 m between sampling points), and (3) a small scale (1.5 cm between sampling points). In most cases, significant vertical heterogeneity was observed at the 0.15 m scale, which was much larger than previously reported for freshwater wetlands and not detected by sampling water table wells screened over the same interval. However, profiles of ammonia and total phosphorus showed tenfold changes in the upper 0.2 meters of the saturated zone when sampled at the small (1.5 cm) scale, that was not depicted by sampling at the intermediate scale. At the intermediate scale of observation, one constructed wetland site differed geochemically from the natural wetlands and the other constructed wetland site due to application of off-site salvaged marsh surface and downward infiltration of rain. While important differences in dissolved inorganic phosphorus and dissolved inorganic carbon concentrations existed between the constructed wetland and the natural wetlands, we also observed substantial differences between the natural wetland sites for these constituents. A median-polishing analysis of our data showed that temporal variations in constituent concentrations within profiles, although extensively recognized in the literature, were not as important as spatial variability.","language":"English","publisher":"Springer","doi":"10.1023/A:1005889319205","issn":"01682563","usgsCitation":"Hunt, R.J., Krabbenhoft, D., and Anderson, M.P., 1997, Assessing hydrogeochemical heterogeneity in natural and constructed wetlands: Biogeochemistry, v. 39, no. 3, p. 271-293, https://doi.org/10.1023/A:1005889319205.","productDescription":"23 p.","startPage":"271","endPage":"293","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":206074,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1023/A:1005889319205"},{"id":228194,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"39","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059edd8e4b0c8380cd49a47","contributors":{"authors":[{"text":"Hunt, R. J.","contributorId":40164,"corporation":false,"usgs":true,"family":"Hunt","given":"R.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":385208,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Krabbenhoft, D. P. 0000-0003-1964-5020","orcid":"https://orcid.org/0000-0003-1964-5020","contributorId":90765,"corporation":false,"usgs":true,"family":"Krabbenhoft","given":"D. P.","affiliations":[],"preferred":false,"id":385209,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Anderson, Marilyn P.","contributorId":102970,"corporation":false,"usgs":true,"family":"Anderson","given":"Marilyn","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":385210,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70020149,"text":"70020149 - 1997 - Mapping the radon potential of the united states: Examples from the Appalachians","interactions":[],"lastModifiedDate":"2012-03-12T17:19:17","indexId":"70020149","displayToPublicDate":"1997-01-01T00:00:00","publicationYear":"1997","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Mapping the radon potential of the united states: Examples from the Appalachians","docAbstract":"The geologic radon potential of the United States was recently assessed by the U.S. Geological Survey. Results indicate that approximately 33% of the U.S. population lives within geologic provinces where the average indoor radon levels have the potential to be greater than 4 pCi/L (147 Bq/m3). Rock types most commonly associated with high indoor radon include: 1) Uraniferous metamorphosed sediments, volcanics, and granite intrusives, especially those that are highly deformed or sheared. 2) Glacial deposits derived from uranium-bearing rocks and sediments. 3) Carboniferous, black shales. 4) Soils derived from carbonate rock, especially in karstic terrain. 5) Uraniferous fluvial, deltaic, marine, and lacustrine deposits. Different geologic terrains of the eastern United States illustrate some of the problems inherent in correlating indoor radon with geology. The Central and Southern Appalachian Highlands of the eastern United States have not been glaciated and most soils there are saprolitic, derived directly from the underlying bedrock. Regression analyses of bedrock geologic and radon parameters yield positive correlations (R > 0.5 to 0.9) and indicate that bedrock geology can account for a significant portion of the indoor radon variation. In glaciated areas of the United States such as the northern Appalachian Highlands and Appalachian Plateau, the correlation of bedrock geology to indoor radon is obscured or is positive only in certain cases. In these glaciated areas of the country, it is the type, composition, thickness, and permeability of glacial deposits, rather than the bedrock geology, that controls the radon source.","largerWorkTitle":"Environment International","conferenceTitle":"Proceedings of the 1995 6th International Symposium on the Natural Radiation Environment, NRE","conferenceDate":"5 June 1995 through 9 June 1995","conferenceLocation":"Montreal, Can","language":"English","publisher":"Elsevier Science Ltd","publisherLocation":"Oxford, United Kingdom","doi":"10.1016/S0160-4120(96)00190-0","issn":"01604120","usgsCitation":"Gundersen, L., and Schumann, R., 1997, Mapping the radon potential of the united states: Examples from the Appalachians, <i>in</i> Environment International, v. 22, no. SUPPL. 1, Montreal, Can, 5 June 1995 through 9 June 1995, https://doi.org/10.1016/S0160-4120(96)00190-0.","costCenters":[],"links":[{"id":499892,"rank":10000,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://doaj.org/article/b023d5d046414367ac5c9cfedddfb12a","text":"External Repository"},{"id":206065,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/S0160-4120(96)00190-0"},{"id":228159,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"22","issue":"SUPPL. 1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a5086e4b0c8380cd6b742","contributors":{"editors":[{"text":"Hopke P.K.","contributorId":128435,"corporation":true,"usgs":false,"organization":"Hopke P.K.","id":536460,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Gundersen, L.C.S.","contributorId":24501,"corporation":false,"usgs":true,"family":"Gundersen","given":"L.C.S.","email":"","affiliations":[],"preferred":false,"id":385207,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schumann, R.R.","contributorId":14429,"corporation":false,"usgs":true,"family":"Schumann","given":"R.R.","email":"","affiliations":[],"preferred":false,"id":385206,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70020271,"text":"70020271 - 1997 - Unusual carbon and oxygen isotropic ratios of ostracodal calcite from last interglacial (Sangamon episode) lacustrine sediment in Raymond Basin, Illinois, USA","interactions":[],"lastModifiedDate":"2012-03-12T17:20:15","indexId":"70020271","displayToPublicDate":"1997-01-01T00:00:00","publicationYear":"1997","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2411,"text":"Journal of Paleolimnology","active":true,"publicationSubtype":{"id":10}},"title":"Unusual carbon and oxygen isotropic ratios of ostracodal calcite from last interglacial (Sangamon episode) lacustrine sediment in Raymond Basin, Illinois, USA","docAbstract":"The stable isotopic records of ostracode valves deposited during the last interglaciation in Raymond Basin, Illinois, have ??13C and ??18O values as high as +16.5??? and +9.2??? respectively, the highest values yet reported from continental ostracodal calcite. Located in south-central Illinois, Raymond, Pittsburgh, Bald Knob, and Hopwood Farm basins collectively have yielded important long pollen and ostracode records that date from about 130 000 years ago to the present. Although fossils from the present-day interglaciation are not well preserved, these records constitute the only described, conformable, fossiliferous successions of this age from the interior of glaciated North America. The high ??13C values from Raymond Basin are attributed to the residual effects of methane loss either by ebullition or by emission through the stems of senescent emergent aquatic vegetation. A mass balance model suggests that an increase in ??13C of dissolved inorganic carbon on the order of +15??? is possible within a few hours given modest rates of methanogenesis of about 0.02 mol m-2 d-1. The ??13C records from other studies of ostracode valves have values approaching, but not exceeding about +14??? suggesting a limiting value to ???13C enrichment due to simultaneous inputs and outputs of dissolved inorganic carbon. Values of ??18O in ostracodal calcite are quite variable (-4 to +9???) in sediment from the late Sangamon subepisode. A model of isotopic enrichment in a desiccating water body implies that a reduction in reservoir volume of 20% could produce this range of isotopic values. High humidity and evaporation probably account for most of the ??18O variability.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Paleolimnology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1023/A:1007964917875","issn":"09212728","usgsCitation":"Curry, B.B., Anderson, T., and Lohmann, K., 1997, Unusual carbon and oxygen isotropic ratios of ostracodal calcite from last interglacial (Sangamon episode) lacustrine sediment in Raymond Basin, Illinois, USA: Journal of Paleolimnology, v. 17, no. 4, p. 421-435, https://doi.org/10.1023/A:1007964917875.","startPage":"421","endPage":"435","numberOfPages":"15","costCenters":[],"links":[{"id":206922,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1023/A:1007964917875"},{"id":231247,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bbcfae4b08c986b328e84","contributors":{"authors":[{"text":"Curry, B. Brandon","contributorId":104224,"corporation":false,"usgs":true,"family":"Curry","given":"B.","email":"","middleInitial":"Brandon","affiliations":[],"preferred":false,"id":385598,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Anderson, T.F.","contributorId":71345,"corporation":false,"usgs":true,"family":"Anderson","given":"T.F.","email":"","affiliations":[],"preferred":false,"id":385597,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lohmann, K.C.","contributorId":20472,"corporation":false,"usgs":true,"family":"Lohmann","given":"K.C.","email":"","affiliations":[],"preferred":false,"id":385596,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70020304,"text":"70020304 - 1997 - Upper campanian (upper cretaceous) ammonites from the Marshalltown Formation-Mount laurel boundary beds in Delaware","interactions":[],"lastModifiedDate":"2024-06-07T00:10:18.989442","indexId":"70020304","displayToPublicDate":"1997-01-01T00:00:00","publicationYear":"1997","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2412,"text":"Journal of Paleontology","active":true,"publicationSubtype":{"id":10}},"title":"Upper campanian (upper cretaceous) ammonites from the Marshalltown Formation-Mount laurel boundary beds in Delaware","docAbstract":"<div class=\"abstract-content\"><div class=\"abstract\" data-abstract-type=\"normal\"><p>New collections from the Marshalltown Formation and basal Mount Laurel Sand along the Chesapeake and Delaware Canal in Delaware clarify the ammonite dating of the interval. The Marshalltown Formation yields<span>&nbsp;</span><span class=\"italic\">Pachydiscus</span><span>&nbsp;</span>(<span class=\"italic\">Pachydiscus</span>) sp.,<span>&nbsp;</span><span class=\"italic\">Menuites portlocki</span><span>&nbsp;</span>(Sharpe, 1855)<span>&nbsp;</span><span class=\"italic\">complexus</span><span>&nbsp;</span>(Hall and Meek, 1856), a subspecies restricted to the<span>&nbsp;</span><span class=\"italic\">Baculites gregoryensis</span><span>&nbsp;</span>and<span>&nbsp;</span><span class=\"italic\">Baculites scotti</span><span>&nbsp;</span>zones in the Western Interior of the United States, and<span>&nbsp;</span><span class=\"italic\">Didymoceras binodosum</span><span>&nbsp;</span>(Kennedy and Cobban, 1993a) known only from the<span>&nbsp;</span><span class=\"italic\">B. scotti</span><span>&nbsp;</span>zone of the Western Interior and correlatives in Arkansas and Texas. The basal part of the Mount Laurel Sand contains a complex assemblage preserved as phosphatic molds:<span>&nbsp;</span><span class=\"italic\">Nostoceras</span><span>&nbsp;</span>(<span class=\"italic\">Nostoceras</span>)<span>&nbsp;</span><span class=\"italic\">monotuberculatum</span><span>&nbsp;</span>Kennedy and Cobban, 1993a,<span>&nbsp;</span><span class=\"italic\">Nostoceras</span><span>&nbsp;</span>(N.) sp.,<span>&nbsp;</span><span class=\"italic\">Didymoceras platycostatum</span><span>&nbsp;</span>(Kennedy and Cobban, 1993b),<span>&nbsp;</span><span class=\"italic\">D. stevensoni</span><span>&nbsp;</span>(Whitfield, 1877) (previously thought to be from the Marshalltown) and<span>&nbsp;</span><span class=\"italic\">Exiteloceras jenneyi</span><span>&nbsp;</span>(Whitfield, 1877). The last two are index species of their eponymous zones in the Western Interior. This sequence is compatible with ammonites from the Wenonah Formation, which lies between the Marshalltown and Mount Laurel to the north and contains ammonites indicative of the<span>&nbsp;</span><span class=\"italic\">Baculites scotti</span><span>&nbsp;</span>zone, and the fauna from higher in the Mount Laurel Sand, which includes elements of the<span>&nbsp;</span><span class=\"italic\">Didymoceras cheyennense</span><span>&nbsp;</span>and<span>&nbsp;</span><span class=\"italic\">Baculites compressus</span><span>&nbsp;</span>zones of the Western Interior sequence.</p></div></div>","language":"English","publisher":"Paleontology Society","doi":"10.1017/S0022336000038968","issn":"00223360","usgsCitation":"Kennedy, W.J., and Cobban, W.A., 1997, Upper campanian (upper cretaceous) ammonites from the Marshalltown Formation-Mount laurel boundary beds in Delaware: Journal of Paleontology, v. 71, no. 1, p. 62-73, https://doi.org/10.1017/S0022336000038968.","productDescription":"12 p.","startPage":"62","endPage":"73","numberOfPages":"12","costCenters":[],"links":[{"id":231130,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"71","issue":"1","noUsgsAuthors":false,"publicationDate":"2016-05-20","publicationStatus":"PW","scienceBaseUri":"505bbd4fe4b08c986b328f67","contributors":{"authors":[{"text":"Kennedy, W. J.","contributorId":81873,"corporation":false,"usgs":true,"family":"Kennedy","given":"W.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":385744,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cobban, W. A.","contributorId":21577,"corporation":false,"usgs":true,"family":"Cobban","given":"W.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":385743,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70020189,"text":"70020189 - 1997 - Terbuthylazine and deethylterbuthylazine in rain and surface water: Determination by enzyme immunoassay and gas chromatography/mass spectrometry","interactions":[],"lastModifiedDate":"2019-02-04T10:33:02","indexId":"70020189","displayToPublicDate":"1997-01-01T00:00:00","publicationYear":"1997","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":636,"text":"Acta Hydrochimica et Hydrobiologica","active":true,"publicationSubtype":{"id":10}},"title":"Terbuthylazine and deethylterbuthylazine in rain and surface water: Determination by enzyme immunoassay and gas chromatography/mass spectrometry","docAbstract":"<p><span>Rain and surface water samples from Southern Germany were investigated from 1991 to 1995 for terbuthylazine and one of its major metabolites, deethylterbuthylazine. The concentrations observed were compared to the concentrations found for atrazine and deethylatrazine in the same water samples. Concentrations ranged from &lt; 0.02 μg/L to 0.7 μg/L for terbuthylazine and from &lt; 0.02 μg/L to 0.6 μg/L for deethylterbuthylazine, compared to concentrations of &lt; 0.02 μg/L to 3 μg/L and &lt; 0.02 μg/L to 0.5 μg/L for atrazine and deethylatrazine, respectively. The ratios of metabolite concentrations to parent compound concentrations were calculated for deethylterbuthylazine to terbuthylazine (</span><i>DTR</i><span>) and deethylatrazine to atrazine (</span><i>DAR</i><span>). In rain water,&nbsp;</span><i>DTR</i><span>&nbsp;of 0.8…3.0 and&nbsp;</span><i>DAR</i><span>&nbsp;of 0.3… 1.9 were determined with mean values of 0.9… 1.7 for&nbsp;</span><i>DTR</i><span>&nbsp;and 0.6…0.9 for&nbsp;</span><i>DAR</i><span>&nbsp;in the different years. The ratios increased during summer periods. The highest ratios were observed in samples from forest stands, showing that degradation of the herbicide has occurred during transport between the source and the sampling site. The&nbsp;</span><i>DTR</i><span>&nbsp;in rain water were about 50… 100% higher than the&nbsp;</span><i>DAR</i><span>. This indicates a higher degradation rate of terbuthylazine during atmospheric transport. In surface water,&nbsp;</span><i>DTR</i><span>&nbsp;of 0.3… 1.2 with mean values of 0.5…0.8 and&nbsp;</span><i>DAR</i><span>&nbsp;of 0.2…2.2 with mean values of 0.2… 1.3 were observed. The ratios increased from June to September.</span></p>","language":"English","publisher":"Wiley","doi":"10.1002/aheh.19970250102","issn":"03234320","usgsCitation":"Dankwardt, A., Thurman, E., and Hock, B., 1997, Terbuthylazine and deethylterbuthylazine in rain and surface water: Determination by enzyme immunoassay and gas chromatography/mass spectrometry: Acta Hydrochimica et Hydrobiologica, v. 25, no. 1, p. 5-10, https://doi.org/10.1002/aheh.19970250102.","productDescription":"6 p.","startPage":"5","endPage":"10","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":231320,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"25","issue":"1","noUsgsAuthors":false,"publicationDate":"2006-12-18","publicationStatus":"PW","scienceBaseUri":"505ba547e4b08c986b320937","contributors":{"authors":[{"text":"Dankwardt, A.","contributorId":84108,"corporation":false,"usgs":true,"family":"Dankwardt","given":"A.","affiliations":[],"preferred":false,"id":385314,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thurman, E.M.","contributorId":102864,"corporation":false,"usgs":true,"family":"Thurman","given":"E.M.","affiliations":[],"preferred":false,"id":385315,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hock, B.","contributorId":66019,"corporation":false,"usgs":true,"family":"Hock","given":"B.","email":"","affiliations":[],"preferred":false,"id":385313,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70171398,"text":"70171398 - 1997 - Pesticides and volatile organic compounds in shallow urban groundwater of the United States","interactions":[],"lastModifiedDate":"2017-05-19T18:21:05","indexId":"70171398","displayToPublicDate":"1997-01-01T00:00:00","publicationYear":"1997","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Pesticides and volatile organic compounds in shallow urban groundwater of the United States","docAbstract":"<p><span>The widespread use of pesticides and volatile organic compounds (VOCs) over the past half century has led to their detection in many hydrologic systems in the United States. However, few systematic investigations of occurrences have been carried out over multistate regions using a consistent study design. Nine urban studies of shallow groundwater have been conducted to date as part of the U.S. Geological Survey's National Water-Quality Assessment Program. Pesticide compounds were detected in 48.6% of the 208 urban wells sampled. Sixteen different pesticide compounds were detected in samples from these wells. Prometon was by far the most frequently detected pesticide compound, being found in 8 of the 9 urban studies. VOCs were detected in 53.4% of the 208 urban wells sampled, with 36 different VOC compounds being found.&nbsp;</span><br /><br /><span>Measured VOC concentrations exceeded current U.S. Environmental Protection Agency drinking water regulations in 19 wells. Methyl&nbsp;</span><i>tert</i><span>-butyl ether (MTBE), a common fuel oxygenate, was the most frequently detected VOC for this study.</span></p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Groundwater in the urban environment","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"A. A. Balkema","usgsCitation":"Kolpin, D.W., Squillace, P.J., Zogorski, J.S., and Barbash, J.E., 1997, Pesticides and volatile organic compounds in shallow urban groundwater of the United States, chap. <i>of</i> Groundwater in the urban environment, v. 1, p. 469-474.","productDescription":"6 p.","startPage":"469","endPage":"474","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":622,"text":"Washington Water Science Center","active":true,"usgs":true}],"links":[{"id":321885,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"574eb5dbe4b0ee97d51a83eb","contributors":{"authors":[{"text":"Kolpin, Dana W. 0000-0002-3529-6505 dwkolpin@usgs.gov","orcid":"https://orcid.org/0000-0002-3529-6505","contributorId":1239,"corporation":false,"usgs":true,"family":"Kolpin","given":"Dana","email":"dwkolpin@usgs.gov","middleInitial":"W.","affiliations":[{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true}],"preferred":true,"id":630889,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Squillace, Paul J.","contributorId":59415,"corporation":false,"usgs":true,"family":"Squillace","given":"Paul","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":630890,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Zogorski, John S. jszogors@usgs.gov","contributorId":189,"corporation":false,"usgs":true,"family":"Zogorski","given":"John","email":"jszogors@usgs.gov","middleInitial":"S.","affiliations":[],"preferred":true,"id":630891,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Barbash, Jack E. 0000-0001-9854-8880 jbarbash@usgs.gov","orcid":"https://orcid.org/0000-0001-9854-8880","contributorId":1003,"corporation":false,"usgs":true,"family":"Barbash","given":"Jack","email":"jbarbash@usgs.gov","middleInitial":"E.","affiliations":[{"id":622,"text":"Washington Water Science Center","active":true,"usgs":true}],"preferred":true,"id":630892,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70020165,"text":"70020165 - 1997 - AVHRR imagery used to identify hurricane damage in a forested wetland of Louisiana","interactions":[],"lastModifiedDate":"2019-10-02T16:46:21","indexId":"70020165","displayToPublicDate":"1997-01-01T00:00:00","publicationYear":"1997","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3052,"text":"Photogrammetric Engineering and Remote Sensing","active":true,"publicationSubtype":{"id":10}},"title":"AVHRR imagery used to identify hurricane damage in a forested wetland of Louisiana","docAbstract":"Certain events provide a unique opportunity to test the monitoring capability of AVHBR imagery. On 26 August 1992, Hurricane Andrew passed through Louisiana, impacting a large area of forested wetlands. One response to the widespread defoliation resulting from the hurricane impact was an abnormal bloom of new leaves and new growth in the underlying vegetation between September and October. To capture this atypical phenology, a time sequence of AVHRR images was transformed into a normalized difference vegetation index, NDVI, as an indicator of vegetation changes in the forest impacted by the passage of a hurricane. Using geographic information system functions, three sites in the impacted forest were vectorized as polygons, and the inclusive pixels were extracted for subsequent graphical and univariate statistical analysis. Temporal curves of mean NDVIs for the three sites for before, during, and after the hurricane passage, and aggregate curves of the impacted forest to an undisturbed forest, were compared. These comparisons corroborated the atypical phenology of the impacted forested wetland and directly related the cause to the hurricane passage.","language":"English","publisher":"American Society for Photogrammetry and Remote Sensing","issn":"00991112","usgsCitation":"Ramsey, E., Chappell, D., and Baldwin, D., 1997, AVHRR imagery used to identify hurricane damage in a forested wetland of Louisiana: Photogrammetric Engineering and Remote Sensing, v. 63, no. 3, p. 293-297.","productDescription":"5 p.","startPage":"293","endPage":"297","numberOfPages":"5","costCenters":[{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true}],"links":[{"id":227790,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United 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III 0000-0002-4518-5796","orcid":"https://orcid.org/0000-0002-4518-5796","contributorId":72769,"corporation":false,"usgs":true,"family":"Ramsey","given":"Elijah W.","suffix":"III","affiliations":[{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"preferred":false,"id":385262,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Chappell, D.K.","contributorId":26463,"corporation":false,"usgs":true,"family":"Chappell","given":"D.K.","email":"","affiliations":[],"preferred":false,"id":385261,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Baldwin, D.G.","contributorId":24939,"corporation":false,"usgs":true,"family":"Baldwin","given":"D.G.","email":"","affiliations":[],"preferred":false,"id":385260,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70020117,"text":"70020117 - 1997 - Radiation-induced diamond crystallization: Origin of carbonados and its implications on meteorite nano-diamonds","interactions":[],"lastModifiedDate":"2023-12-14T23:38:51.894114","indexId":"70020117","displayToPublicDate":"1997-01-01T00:00:00","publicationYear":"1997","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":"Radiation-induced diamond crystallization: Origin of carbonados and its implications on meteorite nano-diamonds","docAbstract":"<p>Ten carbonados from Central Africa were studied for U-Th-Pb systematics. To extract U, Th, and Pb from the samples, we developed a cold combustion technique wherein diamond was burnt in liquid oxygen. The technique gave low blanks; 25–50 pg for Pb, 3 pg for U, and 5 pg for Th. After very thorough acid treatments of the carbonados with hot HNO<sub>3</sub>, HF, and HCl over one week, most of U, Th, and Pb were removed from the samples. Lead in the acid-leached diamonds was highly radiogenic (<sup>206</sup>Pb/<sup>204</sup>Pb up to 470). However, the amounts of U and Th in the acid-leached diamonds are too low to account for the radiogenic Pb even if we assume 4.5 Ga for the age of the diamonds. Therefore, we conclude that the radiogenic Pb was implanted into the diamonds from surroundings by means of recoil energy of radioactive decays of U and Th. From the radiogenic lead isotopic composition, we estimate a minimum age of 2.6 Ga and a maximum age of 3.8 Ga for the formation of the carbonados.</p><p>The above findings of the implantation of recoiled radiogenic Pb into carbonados is consistent with the process of radiation-induced crystallization which was proposed for carbonado by Kaminsky (1987). We show from some theoretical considerations that when highly energetic particles, such as those emitted from radioactive decay of U and Th, interact with carbonaceous materials, they give rise to cascades of atomic disturbance (over regions of about a few nanometer), and the disturbed atoms are likely to recrystallize to form micro-diamonds because of increasing surface energy due to small size.</p><p>The radiation-induced diamond formation mechanism may be relevant to the origin of nano-diamonds in primitive meteorites.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/S0016-7037(96)00346-8","issn":"00167037","usgsCitation":"Ozima, M., and Tatsumoto, M., 1997, Radiation-induced diamond crystallization: Origin of carbonados and its implications on meteorite nano-diamonds: Geochimica et Cosmochimica Acta, v. 61, no. 2, p. 369-376, https://doi.org/10.1016/S0016-7037(96)00346-8.","productDescription":"8 p.","startPage":"369","endPage":"376","costCenters":[],"links":[{"id":228312,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Africa","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              8.72365452743216,\n              15.21192179474727\n            ],\n            [\n              8.72365452743216,\n              -10.179197368424113\n            ],\n            [\n              34.729452578299686,\n              -10.179197368424113\n            ],\n            [\n              34.729452578299686,\n              15.21192179474727\n            ],\n            [\n              8.72365452743216,\n              15.21192179474727\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"61","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a9396e4b0c8380cd80eff","contributors":{"authors":[{"text":"Ozima, M.","contributorId":49539,"corporation":false,"usgs":true,"family":"Ozima","given":"M.","email":"","affiliations":[],"preferred":false,"id":385100,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tatsumoto, M.","contributorId":76798,"corporation":false,"usgs":true,"family":"Tatsumoto","given":"M.","email":"","affiliations":[],"preferred":false,"id":385101,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70020285,"text":"70020285 - 1997 - Migration by radio-tagged pacific golden-plovers from hawaii to Alaska, and their subsequent survival","interactions":[],"lastModifiedDate":"2017-05-10T09:48:02","indexId":"70020285","displayToPublicDate":"1997-01-01T00:00:00","publicationYear":"1997","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3544,"text":"The Auk","onlineIssn":"1938-4254","printIssn":"0004-8038","active":true,"publicationSubtype":{"id":10}},"title":"Migration by radio-tagged pacific golden-plovers from hawaii to Alaska, and their subsequent survival","docAbstract":"<p><span>Many Pacific Golden-Plovers (</span><i><span>Pluvialis fulva</span></i><span>) and other shorebirds winter in the Hawaiian Islands. This is the first landfall for mid-Pacific migrants after overwater flights of 4,000 km or more from Alaska (Johnson et al. 1989, Johnson and Connors 1996). Previous findings (sightings of marked birds and wing-length measurements) showed Alaska affinities for golden-plovers wintering in Hawaii (Johnson and Connors 1996), but there had been no attempt to demonstrate movements between the two regions using radiotelemetry. We made such an effort in spring 1996 by radio-tagging plovers on wintering grounds in Hawaii just before their migration. Some of these birds were later found at three sites in Alaska, including a breeding ground,</span></p>","language":"English","publisher":"American Ornithological Society","doi":"10.2307/4089259","issn":"00048038","usgsCitation":"Johnson, O., Warnock, N., Bishop, M., Bennett, A., Johnson, P., and Kienholz, R., 1997, Migration by radio-tagged pacific golden-plovers from hawaii to Alaska, and their subsequent survival: The Auk, v. 114, no. 3, p. 521-524, https://doi.org/10.2307/4089259.","productDescription":"4 p.","startPage":"521","endPage":"524","costCenters":[],"links":[{"id":479936,"rank":1,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.2307/4089259","text":"Publisher Index Page"},{"id":231399,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"114","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a56fee4b0c8380cd6d998","contributors":{"authors":[{"text":"Johnson, O.W.","contributorId":20937,"corporation":false,"usgs":true,"family":"Johnson","given":"O.W.","email":"","affiliations":[],"preferred":false,"id":385645,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Warnock, N.","contributorId":80615,"corporation":false,"usgs":true,"family":"Warnock","given":"N.","email":"","affiliations":[],"preferred":false,"id":385648,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bishop, M.A.","contributorId":95426,"corporation":false,"usgs":true,"family":"Bishop","given":"M.A.","email":"","affiliations":[],"preferred":false,"id":385650,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bennett, A.J.","contributorId":32107,"corporation":false,"usgs":true,"family":"Bennett","given":"A.J.","email":"","affiliations":[],"preferred":false,"id":385646,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Johnson, P.M.","contributorId":44179,"corporation":false,"usgs":true,"family":"Johnson","given":"P.M.","email":"","affiliations":[],"preferred":false,"id":385647,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Kienholz, R.J.","contributorId":83701,"corporation":false,"usgs":true,"family":"Kienholz","given":"R.J.","email":"","affiliations":[],"preferred":false,"id":385649,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70180248,"text":"70180248 - 1997 - Upper Snake River white sturgeon biological risk assessment","interactions":[],"lastModifiedDate":"2017-01-26T11:54:38","indexId":"70180248","displayToPublicDate":"1997-01-01T00:00:00","publicationYear":"1997","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":9,"text":"Other Report"},"title":"Upper Snake River white sturgeon biological risk assessment","docAbstract":"<p>No abstract available</p>","language":"English","publisher":"Nez Perce Tribe","usgsCitation":"Carmichael, R., Lestelle, L., Mobrand, L., Statler, D., Carter, R., Hoefs, N., Bennet, D., Chandler, J., Lepla, K., Cochnauer, T., Devore, J., Rien, T., McMullin, R., Parsley, M., and Seamans, A., 1997, Upper Snake River white sturgeon biological risk assessment, 83 p. .","productDescription":"83 p. ","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":334042,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"588b1979e4b0ad67323f9812","contributors":{"authors":[{"text":"Carmichael, R.","contributorId":178753,"corporation":false,"usgs":false,"family":"Carmichael","given":"R.","email":"","affiliations":[],"preferred":false,"id":660905,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lestelle, L.","contributorId":178754,"corporation":false,"usgs":false,"family":"Lestelle","given":"L.","email":"","affiliations":[],"preferred":false,"id":660906,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mobrand, L.","contributorId":178755,"corporation":false,"usgs":false,"family":"Mobrand","given":"L.","email":"","affiliations":[],"preferred":false,"id":660907,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Statler, D.","contributorId":178756,"corporation":false,"usgs":false,"family":"Statler","given":"D.","email":"","affiliations":[],"preferred":false,"id":660908,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Carter, R.","contributorId":13397,"corporation":false,"usgs":true,"family":"Carter","given":"R.","affiliations":[],"preferred":false,"id":660909,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Hoefs, N.","contributorId":178757,"corporation":false,"usgs":false,"family":"Hoefs","given":"N.","affiliations":[],"preferred":false,"id":660910,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Bennet, D.","contributorId":178759,"corporation":false,"usgs":false,"family":"Bennet","given":"D.","email":"","affiliations":[],"preferred":false,"id":660911,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Chandler, J.","contributorId":76663,"corporation":false,"usgs":true,"family":"Chandler","given":"J.","affiliations":[],"preferred":false,"id":660912,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Lepla, K.","contributorId":178761,"corporation":false,"usgs":false,"family":"Lepla","given":"K.","affiliations":[],"preferred":false,"id":660913,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Cochnauer, T.","contributorId":178762,"corporation":false,"usgs":false,"family":"Cochnauer","given":"T.","affiliations":[],"preferred":false,"id":660914,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Devore, J.","contributorId":178763,"corporation":false,"usgs":false,"family":"Devore","given":"J.","email":"","affiliations":[],"preferred":false,"id":660915,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Rien, T.","contributorId":178764,"corporation":false,"usgs":false,"family":"Rien","given":"T.","email":"","affiliations":[],"preferred":false,"id":660916,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"McMullin, R.","contributorId":178765,"corporation":false,"usgs":false,"family":"McMullin","given":"R.","affiliations":[],"preferred":false,"id":660917,"contributorType":{"id":1,"text":"Authors"},"rank":13},{"text":"Parsley, M.J.","contributorId":59542,"corporation":false,"usgs":true,"family":"Parsley","given":"M.J.","email":"","affiliations":[],"preferred":false,"id":660918,"contributorType":{"id":1,"text":"Authors"},"rank":14},{"text":"Seamans, A.","contributorId":178767,"corporation":false,"usgs":false,"family":"Seamans","given":"A.","email":"","affiliations":[],"preferred":false,"id":660919,"contributorType":{"id":1,"text":"Authors"},"rank":15}]}}
,{"id":70181830,"text":"70181830 - 1997 - A comparison of sevoflurane and isoflurane for short-term anesthesia in polecats (Mustela eversmanni)","interactions":[],"lastModifiedDate":"2017-02-14T14:50:17","indexId":"70181830","displayToPublicDate":"1997-01-01T00:00:00","publicationYear":"1997","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2514,"text":"Journal of Zoo and Wildlife Medicine","active":true,"publicationSubtype":{"id":10}},"title":"A comparison of sevoflurane and isoflurane for short-term anesthesia in polecats (Mustela eversmanni)","docAbstract":"<p><span>Twenty-four Siberian polecats (Mustela eversmanni) from 12 litters were anesthetized with either inhaled sevoflurane or isoflurane. With 7% delivered sevoflurane and 5% delivered isoflurane, time to loss of righting reflex (mean +/- SE) with sevoflurane (1.9 +/- 0.1 min) was significantly shorter compared with isoflurane (2.6 +/- 0.1 min). During maintenance at a light plane of anesthesia, systolic arterial pressure was significantly higher with sevoflurane (83 +/- 2 mm Hg) compared with isoflurane (66 +/- 2 mm Hg), and heart rate was significantly lower with sevoflurane (191 +/- 3 beats/min) compared with isoflurane (204 +/- 3 beats/min). There was no difference in respiratory rate jugular venous pH, pCO3, HCO3-, base excess, or recovery of righting reflex. Induction of anesthesia is more rapid and blood pressure is better maintained with sevoflurane compared with isoflurane; therefore, sevoflurane may be less stressful and safer. Inhaled sevoflurane should be an appropriate anesthetic for black-footed ferrets (Mustela nigripes) in laboratory and field conditions.</span></p>","language":"English","publisher":"Wildlife Disease Association","usgsCitation":"Gaynor, J.S., Wimsatt, J., Mallinckrodt, C., and Biggins, D.E., 1997, A comparison of sevoflurane and isoflurane for short-term anesthesia in polecats (Mustela eversmanni): Journal of Zoo and Wildlife Medicine, v. 28, no. 3, p. 274-282.","productDescription":"9 p.","startPage":"274","endPage":"282","costCenters":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"links":[{"id":335387,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"28","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58a42547e4b0c825128ad4c1","contributors":{"authors":[{"text":"Gaynor, J. S.","contributorId":181588,"corporation":false,"usgs":false,"family":"Gaynor","given":"J.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":668752,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wimsatt, J.","contributorId":78289,"corporation":false,"usgs":true,"family":"Wimsatt","given":"J.","affiliations":[],"preferred":false,"id":668753,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mallinckrodt, C.","contributorId":181589,"corporation":false,"usgs":false,"family":"Mallinckrodt","given":"C.","email":"","affiliations":[],"preferred":false,"id":668754,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Biggins, D. E.","contributorId":8781,"corporation":false,"usgs":true,"family":"Biggins","given":"D.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":668755,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70020187,"text":"70020187 - 1997 - Demographic patterns of Ferocactus cylindraceus in relation to substrate age and grazing history","interactions":[],"lastModifiedDate":"2012-03-12T17:20:19","indexId":"70020187","displayToPublicDate":"1997-01-01T00:00:00","publicationYear":"1997","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3086,"text":"Plant Ecology","active":true,"publicationSubtype":{"id":10}},"title":"Demographic patterns of Ferocactus cylindraceus in relation to substrate age and grazing history","docAbstract":"Three subpopulations of Ferocactus cylindraceus, a short-columnar cactus of the Sonoran and Mojave deserts, were sampled in Grand Canyon, Arizona, USA, at sites representing a range of substrate ages and different grazing histories. Age-height relations were determined from annual growth, then used to estimate probable year of establishment for each cohort. Eight years between 1944 and 1992 were especially favorable for establishment. Six of these 8 years coincided with El Nino-Southern Oscillation conditions, indicating that as for many woody plants in arid regions, somewhat unusual climatic conditions are necessary if populations are to replace themselves. Comparison of age structures showed that established and developing populations have somewhat different dynamics in that the rate of population increase was slowest on the youngest terrace. On the ancient terraces, about half the plants were less than 25 years old. Plants older than 40 years were few; however the oldest plants in the study (about 49 years) grew on the ancient terraces. On the recent terrace, 76% of the subpopulation was 25 years or younger, and the oldest living plant was about 36 years of age. The age structures of subpopulations on grazed and ungrazed sites also differed markedly. On ungrazed sites, subpopulations were more or less at equilibrium, with enough young plants to replace old ones as they died. In contrast, the subpopulation on the grazed site was in a state of marked disequilibrium. Grazing before 1981 largely extirpated a palatable subshrub that was probably an important nurse plant. Until the shrub population at Indian Canyon recovers from decades of burro grazing, a rebound in E cylindraceus establishment is not to be expected.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Plant Ecology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1023/A:1009767621391","issn":"13850237","usgsCitation":"Bowers, J.E., 1997, Demographic patterns of Ferocactus cylindraceus in relation to substrate age and grazing history: Plant Ecology, v. 133, no. 1, p. 37-48, https://doi.org/10.1023/A:1009767621391.","startPage":"37","endPage":"48","numberOfPages":"12","costCenters":[],"links":[{"id":206947,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1023/A:1009767621391"},{"id":231318,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"133","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059fe82e4b0c8380cd4ed7b","contributors":{"authors":[{"text":"Bowers, Janice E.","contributorId":18119,"corporation":false,"usgs":true,"family":"Bowers","given":"Janice","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":385310,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70182057,"text":"70182057 - 1997 - Variation in incubation periods and egg metabolism in mallards: Intrinsic mechanisms to promote hatch synchrony","interactions":[],"lastModifiedDate":"2017-02-15T15:39:54","indexId":"70182057","displayToPublicDate":"1997-01-01T00:00:00","publicationYear":"1997","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3551,"text":"The Condor","active":true,"publicationSubtype":{"id":10}},"title":"Variation in incubation periods and egg metabolism in mallards: Intrinsic mechanisms to promote hatch synchrony","docAbstract":"<p><span>We investigated factors affecting incubation time and metabolic rates of Mallard (<i>Anas platyrhynchos</i>) eggs incubated under constant environmental conditions. Time required to reach the star-pipped stage of hatch varied significantly among females, but not with laying sequence or egg size. Metabolic rate of eggs varied positively with position in the laying sequence and tended to vary among females. Metabolic rate did not vary with egg volume or incubation length. Our results indicate metabolic rate may act as one synchronization mechanism for hatch. The role of maternal effects in development time should be considered in subsequent studies of incubation time in ducks.</span></p>","language":"English","publisher":"Cooper Ornithological Society","doi":"10.2307/1370245","usgsCitation":"MacCluskie, M.C., Flint, P.L., and Sedinger, J.S., 1997, Variation in incubation periods and egg metabolism in mallards: Intrinsic mechanisms to promote hatch synchrony: The Condor, v. 99, p. 224-228, https://doi.org/10.2307/1370245.","productDescription":"3 p.","startPage":"224","endPage":"228","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":117,"text":"Alaska Science Center Biology WTEB","active":true,"usgs":true}],"links":[{"id":503094,"rank":0,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://digitalcommons.usf.edu/condor/vol99/iss1/32","text":"External Repository"},{"id":335630,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"99","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58a57704e4b057081a24ee6f","contributors":{"authors":[{"text":"MacCluskie, Margaret C.","contributorId":50643,"corporation":false,"usgs":false,"family":"MacCluskie","given":"Margaret","email":"","middleInitial":"C.","affiliations":[{"id":6752,"text":"University of Alaska Fairbanks","active":true,"usgs":false}],"preferred":false,"id":669424,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Flint, Paul L. 0000-0002-8758-6993 pflint@usgs.gov","orcid":"https://orcid.org/0000-0002-8758-6993","contributorId":3284,"corporation":false,"usgs":true,"family":"Flint","given":"Paul","email":"pflint@usgs.gov","middleInitial":"L.","affiliations":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":117,"text":"Alaska Science Center Biology WTEB","active":true,"usgs":true}],"preferred":true,"id":669425,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sedinger, James S.","contributorId":84861,"corporation":false,"usgs":false,"family":"Sedinger","given":"James","email":"","middleInitial":"S.","affiliations":[{"id":12742,"text":"University of Nevada Reno","active":true,"usgs":false}],"preferred":false,"id":669426,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70020200,"text":"70020200 - 1997 - Reserve growth important to U.S. gas supply","interactions":[],"lastModifiedDate":"2018-02-19T17:23:18","indexId":"70020200","displayToPublicDate":"1997-01-01T00:00:00","publicationYear":"1997","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2941,"text":"Oil & Gas Journal","printIssn":"0030-1388","active":true,"publicationSubtype":{"id":10}},"title":"Reserve growth important to U.S. gas supply","docAbstract":"Reserve growth is a major component of the remaining U.S. natural gas resources. Historical data support this premise, as do estimates of technically recoverable and of economically recoverable gas resources remaining in the U.S. However, reserve growth is still poorly understood. Hence, much work remains to be done on the phenomenon of reserve growth.","language":"English","publisher":"PennWell Corporation","publisherLocation":"Tulsa, OK","usgsCitation":"Schmoker, J.W., and Attanasi, E.D., 1997, Reserve growth important to U.S. gas supply: Oil & Gas Journal, v. 95, no. 4, p. 95-96.","productDescription":"2 p.","startPage":"95","endPage":"96","costCenters":[],"links":[{"id":231511,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":351791,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://www.ogj.com/articles/print/volume-95/issue-4/in-this-issue/exploration/reserve-growth-important-to-us-gas-supply.html"}],"country":"United States","volume":"95","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505aa94ae4b0c8380cd85d0c","contributors":{"authors":[{"text":"Schmoker, James W.","contributorId":52171,"corporation":false,"usgs":true,"family":"Schmoker","given":"James","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":385373,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Attanasi, Emil D. 0000-0001-6845-7160 attanasi@usgs.gov","orcid":"https://orcid.org/0000-0001-6845-7160","contributorId":193092,"corporation":false,"usgs":true,"family":"Attanasi","given":"Emil","email":"attanasi@usgs.gov","middleInitial":"D.","affiliations":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true}],"preferred":false,"id":385372,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70020148,"text":"70020148 - 1997 - Synthesis and revision of groups within the Newark Supergroup, eastern North America","interactions":[],"lastModifiedDate":"2023-12-21T00:03:56.004989","indexId":"70020148","displayToPublicDate":"1997-01-01T00:00:00","publicationYear":"1997","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":"Synthesis and revision of groups within the Newark Supergroup, eastern North America","docAbstract":"<p>The Newark Supergroup currently includes nine stratigraphic groups, each of which applies to part or all of the rock column of only one or a few basins. Because the group nomenclature within the Newark Supergroup is neither inclusive nor parallel in its concepts, nearly half of the strata within the Newark Supergroup lacks any group placement. A new system is proposed herein that (1) establishes unambiguous group boundaries, (2) places all Newark Supergroup strata into groups, (3) reduces the number of group names from nine to three, (4) creates parallelism between groups and three major successive tectonic events that created the rift basins containing the Newark Supergroup, and (5) coincidentally provides isochronous or nearly isochronous group boundaries. These proposed groups are (1) the Chatham Group (Middle Triassic to basal Lower Jurassic sedimentary rocks), (2) the Meriden Group (Lower Jurassic extrusive volcanic and sedimentary rocks), and (3) the Agawam Group (new name) (Lower Jurassic sedimentary rocks above all early Mesozoic igneous intrusive and extrusive rocks).</p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1997)109<0195:SAROGW>2.3.CO;2","issn":"00167606","usgsCitation":"Weems, R., and Olsen, P., 1997, Synthesis and revision of groups within the Newark Supergroup, eastern North America: Geological Society of America Bulletin, v. 109, no. 2, p. 195-209, https://doi.org/10.1130/0016-7606(1997)109<0195:SAROGW>2.3.CO;2.","productDescription":"15 p.","startPage":"195","endPage":"209","numberOfPages":"15","costCenters":[],"links":[{"id":479944,"rank":2,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"http://doc.rero.ch/record/14070/files/PAL_E1159.pdf","text":"External Repository"},{"id":228158,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"109","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505ba34ee4b08c986b31fc59","contributors":{"authors":[{"text":"Weems, R.E.","contributorId":44920,"corporation":false,"usgs":true,"family":"Weems","given":"R.E.","affiliations":[],"preferred":false,"id":385204,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Olsen, P.E.","contributorId":71332,"corporation":false,"usgs":true,"family":"Olsen","given":"P.E.","email":"","affiliations":[],"preferred":false,"id":385205,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70019887,"text":"70019887 - 1997 - A geologic history of the north-central Appalachians, part 2: The Appalachian basin from the Silurian through the Carboniferous","interactions":[],"lastModifiedDate":"2023-02-07T16:56:06.421933","indexId":"70019887","displayToPublicDate":"1997-01-01T00:00:00","publicationYear":"1997","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":732,"text":"American Journal of Science","active":true,"publicationSubtype":{"id":10}},"title":"A geologic history of the north-central Appalachians, part 2: The Appalachian basin from the Silurian through the Carboniferous","docAbstract":"<p><span>The north-central Appalachians occupy a critical position within the 3000+ km-long Appalachian orogen, lying southwest of the boundary between the central and northern Appalachians (CNAB). The one-billion-year-long history of tectonic activity in the north-central Appalachians includes the assembly and breakup of a late Proterozoic supercontinent, the creation and evolution of the Appalachian orogen during the Paleozoic, and the Mesozoic transformation of the active orogen into a passive margin during Pangea's disassembly. An important part of the Middle and Late Paleozoic history is the formation and growth of the Appalachian basin, an enormous, elongate continental basin lying cratonward of the active Appalachian internides along Laurentia's eastern margin. The Appalachian basin developed out of the Taconic orogeny, the second of the four orogenies that formed and modified the character of the Appalachian orogen. Prior to the Taconic orogeny, the eastern margin of Laurentia consisted of a broad carbonate shelf facing the Theic Ocean. The Taconic orogeny obduced various Theic components, including microcontinents, magmatic arcs, and accretionary prisms, onto the carbonate shelf. The resulting Taconic highlands formed a topographic barrier between Theia and the craton's interior. Because tectonic activity in the internides continued more or less throughout the remainder of the Paleozoic, the Appalachian basin never had a direct connection with Theia. The coarse-grained molasse from the newly uplifted Taconic highland spread westward over most of the basin during the Early Silurian. Carbonate deposition gradually encroached eastward over the basin as the siliciclastic input from the southeast waned. A resurgence in the earliest Late Silurian, perhaps related to orogenesis in Newfoundland and the Maritimes, expanded the clastic wedge somewhat. Before long, however, carbonate deposition once again dominated most of the north-central basin for the remainder of the Silurian and into the Early Devonian. The Early-to-Middle Devonian Acadian orogeny began introducing siliciclastic material into the eastern part of the Appalachian basin, thereby ending the largely paralic environment that persisted from the Late Silurian. A number of deltas formed around local sediment-input centers during the Middle Devonian. Continued uplift and/or orogenesis must have continued into the Late Devonian because a vast amount of terrigenous sediment was introduced into the Appalachian basin to form the vast Upper Devonian Catskill delta. Although the principal tectonic activity appears to have centered in New England, the large volume of sediment input suggests that orogenesis may have extended southward to the north-central Appalachians. However, direct evidence of actual Acadian deformation and metamorphism is lacking at this latitude. The north-central Appalachian basin underwent a significant change during the Carboniferous. Prior to this time, the shoreline shifted laterally through transgressions and regressions largely as a function of sediment input and regional subsidence. In the Carboniferous, vertical movements in the basin became more important. During the Early Carboniferous, much of the Mauch Chunk delta was eroded in the central and western parts of the basin. At the end of the Early Carboniferous, an unconformity truncated progressively older rocks to the north toward New York. New sediment transport patterns and depositional environments within the basin during the Late Carboniferous probably reflect significant topographic and tectonic changes, not only in the hinterland, but in the basin itself, perhaps in conjunction with climatic changes. Extensive interfluvial swamps on a lower delta plain accumulated thick organic deposits which would become coal. This delta plain graded southwestward into tidal and marine environments. The Alleghany orogeny in the Early Permian interrupted deposition in much of the north-central Appalachian basin and profoundly altered its structure.</span></p>","language":"English","publisher":"American Journal of Science","doi":"10.2475/ajs.297.7.729","usgsCitation":"Faill, R.T., 1997, A geologic history of the north-central Appalachians, part 2: The Appalachian basin from the Silurian through the Carboniferous: American Journal of Science, v. 297, no. 7, p. 729-761, https://doi.org/10.2475/ajs.297.7.729.","productDescription":"33 p.","startPage":"729","endPage":"761","numberOfPages":"33","costCenters":[],"links":[{"id":488605,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.2475/ajs.297.7.729","text":"Publisher Index Page"},{"id":227734,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"297","issue":"7","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e3fee4b0c8380cd46336","contributors":{"authors":[{"text":"Faill, R. T.","contributorId":79639,"corporation":false,"usgs":true,"family":"Faill","given":"R.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":384276,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70020320,"text":"70020320 - 1997 - SEA96 - A new predictive relation for earthquake ground motions in extensional tectonic regimes","interactions":[],"lastModifiedDate":"2025-07-28T16:13:31.890188","indexId":"70020320","displayToPublicDate":"1997-01-01T00:00:00","publicationYear":"1997","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3372,"text":"Seismological Research Letters","onlineIssn":"1938-2057","printIssn":"0895-0695","active":true,"publicationSubtype":{"id":10}},"title":"SEA96 - A new predictive relation for earthquake ground motions in extensional tectonic regimes","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"GeoScienceWorld","doi":"10.1785/gssrl.68.1.190","issn":"00128287","usgsCitation":"Spudich, P., Fletcher, J.B., Hellweg, M., Boatwright, J., Sullivan, C., Joyner, W.B., Hanks, T.C., Boore, D., McGarr, A., Baker, L., and Lindh, A., 1997, SEA96 - A new predictive relation for earthquake ground motions in extensional tectonic regimes: Seismological Research Letters, v. 68, no. 1, p. 190-198, https://doi.org/10.1785/gssrl.68.1.190.","productDescription":"9 p.","startPage":"190","endPage":"198","costCenters":[],"links":[{"id":231363,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"68","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505aaf1be4b0c8380cd873c4","contributors":{"authors":[{"text":"Spudich, P.","contributorId":85700,"corporation":false,"usgs":true,"family":"Spudich","given":"P.","affiliations":[],"preferred":false,"id":385821,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fletcher, Joe B.","contributorId":8850,"corporation":false,"usgs":true,"family":"Fletcher","given":"Joe","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":385812,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hellweg, M.","contributorId":11344,"corporation":false,"usgs":true,"family":"Hellweg","given":"M.","email":"","affiliations":[],"preferred":false,"id":385813,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Boatwright, J.","contributorId":87297,"corporation":false,"usgs":true,"family":"Boatwright","given":"J.","email":"","affiliations":[],"preferred":false,"id":385822,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Sullivan, C.","contributorId":75959,"corporation":false,"usgs":true,"family":"Sullivan","given":"C.","affiliations":[],"preferred":false,"id":385820,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Joyner, W. B.","contributorId":70746,"corporation":false,"usgs":true,"family":"Joyner","given":"W.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":385819,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Hanks, Thomas C.","contributorId":35763,"corporation":false,"usgs":true,"family":"Hanks","given":"Thomas","middleInitial":"C.","affiliations":[],"preferred":false,"id":385815,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Boore, D.M. 0000-0002-8605-9673","orcid":"https://orcid.org/0000-0002-8605-9673","contributorId":64226,"corporation":false,"usgs":true,"family":"Boore","given":"D.M.","affiliations":[],"preferred":false,"id":385818,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"McGarr, Art 0000-0001-9769-4093","orcid":"https://orcid.org/0000-0001-9769-4093","contributorId":43491,"corporation":false,"usgs":true,"family":"McGarr","given":"Art","affiliations":[],"preferred":false,"id":385817,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Baker, L.M.","contributorId":40608,"corporation":false,"usgs":true,"family":"Baker","given":"L.M.","email":"","affiliations":[],"preferred":false,"id":385816,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Lindh, A.G.","contributorId":24784,"corporation":false,"usgs":true,"family":"Lindh","given":"A.G.","email":"","affiliations":[],"preferred":false,"id":385814,"contributorType":{"id":1,"text":"Authors"},"rank":11}]}}
,{"id":70020321,"text":"70020321 - 1997 - Forecasting drought risks for a water supply storage system using bootstrap position analysis","interactions":[],"lastModifiedDate":"2012-03-12T17:20:20","indexId":"70020321","displayToPublicDate":"1997-01-01T00:00:00","publicationYear":"1997","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Forecasting drought risks for a water supply storage system using bootstrap position analysis","docAbstract":"Forecasting the likelihood of drought conditions is an integral part of managing a water supply storage and delivery system. Position analysis uses a large number of possible flow sequences as inputs to a simulation of a water supply storage and delivery system. For a given set of operating rules and water use requirements, water managers can use such a model to forecast the likelihood of specified outcomes such as reservoir levels falling below a specified level or streamflows falling below statutory passing flows a few months ahead conditioned on the current reservoir levels and streamflows. The large number of possible flow sequences are generated using a stochastic streamflow model with a random resampling of innovations. The advantages of this resampling scheme, called bootstrap position analysis, are that it does not rely on the unverifiable assumption of normality and it allows incorporation of long-range weather forecasts into the analysis.","largerWorkTitle":"Proceedings, Congress of the International Association of Hydraulic Research, IAHR","conferenceTitle":"Proceedings of the 1997 27th Congress of the International Association of Hydraulic Research, IAHR. Part C","conferenceDate":"10 August 1997 through 15 August 1997","conferenceLocation":"San Francisco, CA, USA","language":"English","publisher":"ASCE","publisherLocation":"New York, NY, United States","usgsCitation":"Tasker, G., and Dunne, P., 1997, Forecasting drought risks for a water supply storage system using bootstrap position analysis, <i>in</i> Proceedings, Congress of the International Association of Hydraulic Research, IAHR, v. A, San Francisco, CA, USA, 10 August 1997 through 15 August 1997, p. 645-650.","startPage":"645","endPage":"650","numberOfPages":"6","costCenters":[],"links":[{"id":231364,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"A","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a1316e4b0c8380cd544ff","contributors":{"authors":[{"text":"Tasker, Gary","contributorId":78617,"corporation":false,"usgs":true,"family":"Tasker","given":"Gary","affiliations":[],"preferred":false,"id":385823,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dunne, Paul","contributorId":86794,"corporation":false,"usgs":true,"family":"Dunne","given":"Paul","email":"","affiliations":[],"preferred":false,"id":385824,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70020139,"text":"70020139 - 1997 - Occurrence and concentrations of polycyclic aromatic hydrocarbons in semipermeable membrane devices and clams in three urban streams of the Dallas-Fort Worth Metropolitan Area, Texas","interactions":[],"lastModifiedDate":"2012-03-12T17:19:20","indexId":"70020139","displayToPublicDate":"1997-01-01T00:00:00","publicationYear":"1997","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1226,"text":"Chemosphere","active":true,"publicationSubtype":{"id":10}},"title":"Occurrence and concentrations of polycyclic aromatic hydrocarbons in semipermeable membrane devices and clams in three urban streams of the Dallas-Fort Worth Metropolitan Area, Texas","docAbstract":"Semipermeable membrane devices (SPMDs) and Asiatic clams, Corbicula fluminea (MuLLER), were deployed at stream sites in the Dallas-Fort Worth Metropolitan Area to assess the presence of bioavailable, dissolved polycyclic aromatic hydrocarbons (PAHs). Twenty-four PAHs were detected in SPMDs, 20 of which occurred at all sites. Only three PAHs were detected in the co-deployed clams. Throughout all sites, non-alkylated PAHs were found at greater levels in SPMDs than alkylated forms. Nine of 16 Priority Pollutant PAHs were detected in SPMDs. Estimated concentrations of PAHs in water were generally two to three orders of magnitude less than standard minimum analytical reporting levels; however, for bent (a) anthracene, benzo (a) pyrene, and chrysene, estimated concentrations in water exceeded the U.S. Environmental Protection Agency's human health criteria for these carcinogens in water and aquatic organisms.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Chemosphere","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/S0045-6535(96)00391-8","issn":"00456535","usgsCitation":"Moring, J., and Rose, D., 1997, Occurrence and concentrations of polycyclic aromatic hydrocarbons in semipermeable membrane devices and clams in three urban streams of the Dallas-Fort Worth Metropolitan Area, Texas: Chemosphere, v. 34, no. 3, p. 551-566, https://doi.org/10.1016/S0045-6535(96)00391-8.","startPage":"551","endPage":"566","numberOfPages":"16","costCenters":[],"links":[{"id":206037,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/S0045-6535(96)00391-8"},{"id":228003,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"34","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a6b2de4b0c8380cd74567","contributors":{"authors":[{"text":"Moring, J.B.","contributorId":89165,"corporation":false,"usgs":true,"family":"Moring","given":"J.B.","email":"","affiliations":[],"preferred":false,"id":385175,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rose, D.R.","contributorId":62771,"corporation":false,"usgs":true,"family":"Rose","given":"D.R.","email":"","affiliations":[],"preferred":false,"id":385174,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70020141,"text":"70020141 - 1997 - A new approach for analyzing bird densities from variable circular-plot counts","interactions":[],"lastModifiedDate":"2012-03-12T17:19:19","indexId":"70020141","displayToPublicDate":"1997-01-01T00:00:00","publicationYear":"1997","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":"A new approach for analyzing bird densities from variable circular-plot counts","docAbstract":"An approach for calculating bird densities from variable circular-plot counts is described. The approach differs from previous methods in that data from several surveys are pooled and detection distances are adjusted as if all distances were recorded by a single observer under a given set of field conditions. Adjustments for covariates that affect detection distances such as observer, weather, time of day, and vegetation type are made using coefficients calculated by multiple linear regression. The effective area surveyed under standard conditions is calculated from the pooled data set and then used to determine the effective area surveyed at each sampling station under the actual conditions when the station was sampled. The method was validated in two field studies where the density of birds could be determined by independent methods. Computer software for entering and analyzing data by this method is described.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Pacific Science","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"00308870","usgsCitation":"Fancy, S., 1997, A new approach for analyzing bird densities from variable circular-plot counts: Pacific Science, v. 51, no. 1, p. 107-114.","startPage":"107","endPage":"114","numberOfPages":"8","costCenters":[],"links":[{"id":228041,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"51","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e49be4b0c8380cd4676c","contributors":{"authors":[{"text":"Fancy, S.G.","contributorId":8957,"corporation":false,"usgs":true,"family":"Fancy","given":"S.G.","affiliations":[],"preferred":false,"id":385180,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70020322,"text":"70020322 - 1997 - Bryozoa of the Murdock Mountain formation (Wordian, Permian), Leach Mountains, northeastern Nevada","interactions":[],"lastModifiedDate":"2024-06-06T11:25:18.04459","indexId":"70020322","displayToPublicDate":"1997-01-01T00:00:00","publicationYear":"1997","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2412,"text":"Journal of Paleontology","active":true,"publicationSubtype":{"id":10}},"title":"Bryozoa of the Murdock Mountain formation (Wordian, Permian), Leach Mountains, northeastern Nevada","docAbstract":"<div class=\"abstract-content\"><div class=\"abstract\" data-abstract-type=\"normal\"><p>A thin limestone tongue in the upper part of the Murdock Mountain Formation of northeastern Nevada contains abundant bryozoans of earliest Wordian age. This bryozoan fauna is close to the Kungurian-Kazanian boundary in Russia. These bryozoans are younger than those found in the Kaibab Formation of southern Nevada and slightly older than those in the Gerster Limestone of northern Nevada. This limestone tongue, herein referred to as the<span>&nbsp;</span><span class=\"italic\">Stenodiscus</span><span>&nbsp;</span>beds, lies below the<span>&nbsp;</span><span class=\"italic\">Thamnosia</span><span>&nbsp;</span>beds described by Wardlaw in the Murdock Mountain section of the Leach Mountains. This bryozoan-rich limestone tongue serves as a marker unit for mapping the Murdock Formation in the Leach Mountains.</p><p>Nine new species of bryozoans occur in the<span>&nbsp;</span><span class=\"italic\">Stenodiscus</span><span>&nbsp;</span>beds of the Murdock Mountain Formation:<span>&nbsp;</span><span class=\"italic\">Hinganella felderi, Neoeridotrypella schilti, Stenopora parvaexozona, Stenodiscus murdockensis, Dyscritella acanthostylia, Pseudobatostomella irregularis, Streblotrypa</span><span>&nbsp;</span>(<span class=\"italic\">Streblotrypa</span>)<span>&nbsp;</span><span class=\"italic\">elongata, Morozoviella praecurriensis,</span><span>&nbsp;</span>and<span>&nbsp;</span><span class=\"italic\">Thamniscus erraticus, Hinganella felderi, Neoeridotrypella schilti, Dyscritella acanthostylia,</span><span>&nbsp;</span>and<span>&nbsp;</span><span class=\"italic\">Streblotrypa</span><span>&nbsp;</span>(<span class=\"italic\">Streblotrypa</span>)<span>&nbsp;</span><span class=\"italic\">elongata</span><span>&nbsp;</span>are very similar to species described from Russia.</p></div></div>","language":"English","publisher":"Oxford Academic","doi":"10.1017/S0022336000039159","issn":"00223360","usgsCitation":"Gilmour, E., McColloch, M., and Wardlaw, B.R., 1997, Bryozoa of the Murdock Mountain formation (Wordian, Permian), Leach Mountains, northeastern Nevada: Journal of Paleontology, v. 71, no. 2, p. 214-236, https://doi.org/10.1017/S0022336000039159.","productDescription":"23 p.","startPage":"214","endPage":"236","numberOfPages":"23","costCenters":[],"links":[{"id":231365,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"71","issue":"2","noUsgsAuthors":false,"publicationDate":"2016-05-20","publicationStatus":"PW","scienceBaseUri":"5059f2a1e4b0c8380cd4b26f","contributors":{"authors":[{"text":"Gilmour, E.H.","contributorId":53558,"corporation":false,"usgs":true,"family":"Gilmour","given":"E.H.","email":"","affiliations":[],"preferred":false,"id":385826,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McColloch, M.E.","contributorId":96866,"corporation":false,"usgs":true,"family":"McColloch","given":"M.E.","email":"","affiliations":[],"preferred":false,"id":385827,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wardlaw, B. R.","contributorId":9269,"corporation":false,"usgs":true,"family":"Wardlaw","given":"B.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":385825,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70020138,"text":"70020138 - 1997 - Investigation of aggregation in solvent extraction of lanthanides by acidic extractants (organophosphorus and naphthenic acid)","interactions":[],"lastModifiedDate":"2025-08-15T15:44:49.083366","indexId":"70020138","displayToPublicDate":"1997-01-01T00:00:00","publicationYear":"1997","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3349,"text":"Science in China, Series B: Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"Investigation of aggregation in solvent extraction of lanthanides by acidic extractants (organophosphorus and naphthenic acid)","docAbstract":"<p><span>Three acidic extractants (I) di(2-ethylhexyl) phosphoric acid (HDEHP), (II) 2-ethylhexyl phosphonic acid mono-2-ethylhexyl ester (HEHPEHE) and (III) naphthenic acid were employed in preparing the samples for the characterization of the coordination structure of lanthanide-extractant complexes and the physicochemica nature of aggregates formed in the organic diluent of the solvent extraction systems. Photo correlation spectroscopy (PCS) results on the aggregates formed by the partially saponified HDEHP in n-heptane showed that the hydrodynamic radius of the aggregates was comparable to the molecular dimensions of HDEHP. The addition of 2-octanol into the diluent, by which the mixed solvent was formed, increased the dimensions of the corresponding aggregates. Aggregates formed from the lanthanide ions and HDEHP in the organic phase of the extraction systems were found very unstable. In the case of naphthenic acid, PCS data showed the formation of w/o microemulsion from the saponified naphthenic acid in the mixed solvent. The extraction of lanthanides by the saponified naphthenic acid in the mixed solvent under the given experimental conditions was a process of destruction of the w/o microemulsion. A possible mechanism of the breakdown of the w/o microemulsion droplets is discussed.</span></p>","language":"English","publisher":"Springer","doi":"10.1007/BF02882189","issn":"10069291","usgsCitation":"Zhou, N., Wu, J., Yu, Z., Neuman, R.D., Wang, D., and Xu, G., 1997, Investigation of aggregation in solvent extraction of lanthanides by acidic extractants (organophosphorus and naphthenic acid): Science in China, Series B: Chemistry, v. 40, no. 1, p. 61-71, https://doi.org/10.1007/BF02882189.","productDescription":"11 p.","startPage":"61","endPage":"71","numberOfPages":"11","costCenters":[],"links":[{"id":228002,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"40","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3e7ee4b0c8380cd63e16","contributors":{"authors":[{"text":"Zhou, N.","contributorId":31539,"corporation":false,"usgs":true,"family":"Zhou","given":"N.","email":"","affiliations":[],"preferred":false,"id":385170,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wu, J.","contributorId":56998,"corporation":false,"usgs":true,"family":"Wu","given":"J.","email":"","affiliations":[],"preferred":false,"id":385172,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Yu, Z.","contributorId":32696,"corporation":false,"usgs":true,"family":"Yu","given":"Z.","email":"","affiliations":[],"preferred":false,"id":385171,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Neuman, R. D.","contributorId":27199,"corporation":false,"usgs":true,"family":"Neuman","given":"R.","middleInitial":"D.","affiliations":[],"preferred":false,"id":385169,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Wang, D.","contributorId":13384,"corporation":false,"usgs":true,"family":"Wang","given":"D.","email":"","affiliations":[],"preferred":false,"id":385168,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Xu, G.","contributorId":67235,"corporation":false,"usgs":true,"family":"Xu","given":"G.","email":"","affiliations":[],"preferred":false,"id":385173,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
]}