{"pageNumber":"2452","pageRowStart":"61275","pageSize":"25","recordCount":185071,"records":[{"id":70207772,"text":"70207772 - 2006 - Changes in the C storage in Las Tablas de Daimiel National Park (PNTD) in the last 1000 years [Cambios en el almacenamiento de C en el Parque Nacional de Las Tablas de Daimiel (PNTD) en los últimos 1000 años]","interactions":[],"lastModifiedDate":"2020-06-15T17:11:48.630654","indexId":"70207772","displayToPublicDate":"2006-01-09T15:55:45","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1065,"text":"Boletin Geologico y Minero","active":true,"publicationSubtype":{"id":10}},"title":"Changes in the C storage in Las Tablas de Daimiel National Park (PNTD) in the last 1000 years [Cambios en el almacenamiento de C en el Parque Nacional de Las Tablas de Daimiel (PNTD) en los últimos 1000 años]","docAbstract":"<p><span>Las Tablas de Daimiel National Park has suffered too many modifications throughout its history, natural as well as anthropic, which have affected the carbon storage in different ways. The study of those variations has been carried out by the analysis of sedimentary record and historical data. The sedimentary record has been studied from the core Ciguela 4. It was sampled with a systematic high resolution method (0.7 cm thickness average) to analyze geochemistry and pollen. The analysis of all data shows that the natural changes (linked with the climate) have more variation ranges than the anthropic ones, are directly related with the climate and not with the concentration of the atmospheric CO2, showing a natural cyclicity with a fast mitigation (decades) of the variations. In the other hand the anthropogenic impacts depend on the proximity and intensity of the impact. The usage changes produced during the second half of the 19th century were an indirect impact with medium intensity. The environment had the capacity to recover the values of a normal storage in less than 50 years. Nevertheless the dissication and overexploitation of the groundwater (second half of 20th century) were direct and high intensity impacts. These impacts caused a fast loss of the water table and the salinization of the environment. Due to that the ecosystem lost capacity to store C. recovery of the normal values by a natural way is difficult now.</span></p>","language":"Castilian","publisher":"Instituto Geologico y Minero de Espana","issn":"0366-0176","usgsCitation":"Dominguez-Castro, F., Santisteban, J., Mediavilla, R., Dean, W.E., Lopez-Pamo, E., Ruiz-Zapata, M.B., and Gil-Garcia, M.J., 2006, Changes in the C storage in Las Tablas de Daimiel National Park (PNTD) in the last 1000 years [Cambios en el almacenamiento de C en el Parque Nacional de Las Tablas de Daimiel (PNTD) en los últimos 1000 años]: Boletin Geologico y Minero, v. 117, p. 537-544.","productDescription":"8 p.","startPage":"537","endPage":"544","costCenters":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"links":[{"id":371131,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Spain","otherGeospatial":"Las Tablas de Daimiel National Park","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -3.779983520507812,\n              39.10182458484289\n            ],\n            [\n              -3.64471435546875,\n              39.10182458484289\n            ],\n            [\n              -3.64471435546875,\n              39.19448036993607\n            ],\n            [\n              -3.779983520507812,\n              39.19448036993607\n            ],\n            [\n              -3.779983520507812,\n              39.10182458484289\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"117","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Dominguez-Castro, F.","contributorId":82996,"corporation":false,"usgs":true,"family":"Dominguez-Castro","given":"F.","email":"","affiliations":[],"preferred":false,"id":779270,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Santisteban, J.I.","contributorId":56118,"corporation":false,"usgs":true,"family":"Santisteban","given":"J.I.","email":"","affiliations":[],"preferred":false,"id":779271,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mediavilla, R.","contributorId":43240,"corporation":false,"usgs":true,"family":"Mediavilla","given":"R.","email":"","affiliations":[],"preferred":false,"id":779272,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Dean, Walter E. dean@usgs.gov","contributorId":1801,"corporation":false,"usgs":true,"family":"Dean","given":"Walter","email":"dean@usgs.gov","middleInitial":"E.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":779273,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Lopez-Pamo, Enrique","contributorId":221636,"corporation":false,"usgs":false,"family":"Lopez-Pamo","given":"Enrique","email":"","affiliations":[],"preferred":false,"id":779274,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Ruiz-Zapata, Maria Blanca","contributorId":221637,"corporation":false,"usgs":false,"family":"Ruiz-Zapata","given":"Maria","email":"","middleInitial":"Blanca","affiliations":[],"preferred":false,"id":779275,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Gil-Garcia, Maria Jose","contributorId":221638,"corporation":false,"usgs":false,"family":"Gil-Garcia","given":"Maria","email":"","middleInitial":"Jose","affiliations":[],"preferred":false,"id":779276,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70046923,"text":"dsNE3071 - 2006 - Drainage areas for selected stream-sampling stations, Missouri River Basin","interactions":[],"lastModifiedDate":"2013-07-09T13:00:39","indexId":"dsNE3071","displayToPublicDate":"2006-01-09T12:49:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":310,"text":"Data Series","code":"DS","onlineIssn":"2327-638X","printIssn":"2327-0271","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"NE-3071","title":"Drainage areas for selected stream-sampling stations, Missouri River Basin","docAbstract":"As part of the U.S. Geological Survey's (USGS) National Water-Quality Assessment Program (NAWQA), an investigation of the Missouri River Basin is being conducted to document trends in surface-water quality, specifically for trends in nutrients and suspended sediment.  Surface-water samples were collected from streams at specific sampling stations.  Water-quality characteristics at each station are influenced by the natural and cultural characteristics of the drainage area upstream from the sampling station.  Efficient quantification of the drainage area characteristics requires a digital map of the drainage area boundary that may be processed, together with other digital thematic maps (such as geology or land use), in a geographic information system (GIS).  Digital drainage-area boundary data for one stream-sampling station in the Missouri River Basin (MRB4) study area is included in this data release.  The drainage divides were identified chiefly using 1:24,000-scale hypsography.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/dsNE3071","usgsCitation":"U.S. Geological Survey, 2006, Drainage areas for selected stream-sampling stations, Missouri River Basin: U.S. Geological Survey Data Series NE-3071, Dataset, https://doi.org/10.3133/dsNE3071.","productDescription":"Dataset","onlineOnly":"Y","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":274766,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Colorado;Iowa;Kansas;Montana;Nebraska;North Dakota;South Dakota;Wyoming","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -110.452497,44.539797 ], [ -110.452497,45.238318 ], [ -109.799224,45.238318 ], [ -109.799224,44.539797 ], [ -110.452497,44.539797 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51dd30e9e4b0f72b44719c6c"}
,{"id":70189441,"text":"70189441 - 2006 - The toxicological geochemistry of Earth materials: An overview of processes and the interdisciplinary methods used to understand them","interactions":[],"lastModifiedDate":"2017-07-13T09:34:45","indexId":"70189441","displayToPublicDate":"2006-01-09T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3281,"text":"Reviews in Mineralogy and Geochemistry","active":true,"publicationSubtype":{"id":10}},"title":"The toxicological geochemistry of Earth materials: An overview of processes and the interdisciplinary methods used to understand them","docAbstract":"<p><span>A broad spectrum of earth materials have been linked to, blamed for, and/or debated as sources for disease. In some cases, the links are clear. For example, excessive exposures to mineral dusts have long been recognized for their role in diseases such as: asbestosis, mesothelioma, and lung cancers (asbestos); silicosis and lung cancer (silica dusts); and coal-workers pneumoconiosis (coal dust). Lead poisoning, particularly in toddlers and young children, has been conclusively linked to involuntary ingestion of soils or other materials contaminated with lead-rich paint particles, leaded gasoline combustion byproducts, and some types of lead-rich mine wastes or smelter particulates. Waters with naturally elevated arsenic contents are common in many regions of the globe, and consumption of these waters has been documented as the source of arsenic-related diseases affecting thousands of people in south Asia and other regions. Exposure to dusts or soils containing pathogens has been documented as the cause of regionally common diseases such as valley fever (coccidioidomycosis) and much rarer diseases such as anthrax. Links between many other earth materials and specific diseases, although suspected, are less clear or are debated. For example, it has been suggested that geographic clusters of diseases such as leukemia are related to exposures to waters or atmospheric particulates containing organic or metal contaminants; however, for many clusters the exact causal relationships between disease and environmental exposure are difficult to prove conclusively. Even for many diseases in which the causal relationship is clear, such as in asbestosis and mesothelioma triggered by asbestos exposure, the minimum exposures needed to trigger disease, the influence of genetic factors, and the exact mechanisms of toxicity are still incompletely understood and are the focus of considerable debate within the public health community. Hence, understanding the health effects resulting from occupational and environmental exposures to a wide variety of earth materials remains a very active and fruitful area of research.</span></p>","language":"English","publisher":"Geological Society of America","doi":"10.2138/rmg.2006.64.2","usgsCitation":"Plumlee, G.S., Morman, S.A., and Ziegler, T.L., 2006, The toxicological geochemistry of Earth materials: An overview of processes and the interdisciplinary methods used to understand them: Reviews in Mineralogy and Geochemistry, v. 64, no. 1, p. 5-57, https://doi.org/10.2138/rmg.2006.64.2.","productDescription":"53 p.","startPage":"5","endPage":"57","costCenters":[{"id":5056,"text":"Office of the AD Energy and Minerals, and Environmental Health","active":true,"usgs":true}],"links":[{"id":343764,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"64","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"596886a3e4b0d1f9f05f59d6","contributors":{"authors":[{"text":"Plumlee, Geoffrey S. 0000-0002-9607-5626 gplumlee@usgs.gov","orcid":"https://orcid.org/0000-0002-9607-5626","contributorId":960,"corporation":false,"usgs":true,"family":"Plumlee","given":"Geoffrey","email":"gplumlee@usgs.gov","middleInitial":"S.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":704602,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Morman, Suzette A. 0000-0002-2532-1033 smorman@usgs.gov","orcid":"https://orcid.org/0000-0002-2532-1033","contributorId":996,"corporation":false,"usgs":true,"family":"Morman","given":"Suzette","email":"smorman@usgs.gov","middleInitial":"A.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true},{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":704603,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ziegler, Thomas L.","contributorId":20381,"corporation":false,"usgs":true,"family":"Ziegler","given":"Thomas","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":704604,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70207731,"text":"70207731 - 2006 - The significance of ground water to the accumulation of iron and manganese in the sediments of two hydrologically distinct lakes in north‐central Minnesota: A geological perspective","interactions":[],"lastModifiedDate":"2020-06-16T15:16:17.162672","indexId":"70207731","displayToPublicDate":"2006-01-08T12:53:09","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1861,"text":"Ground Water","active":true,"publicationSubtype":{"id":10}},"title":"The significance of ground water to the accumulation of iron and manganese in the sediments of two hydrologically distinct lakes in north‐central Minnesota: A geological perspective","docAbstract":"<p><span>Williams and Shingobee lakes are at opposite ends of the local ground water flow system in the Shingobee River Headwaters Area (SRHA) in north‐central Minnesota. Williams Lake, situated near the highest point in the flow system, has no surface inlet or outlet, and ground water and precipitation are the only sources of water. Shingobee Lake, situated at the lowest point in the flow system, has the Shingobee River as an inlet and outlet. Ground water directly contributes an estimated one‐fourth of the water input to Shingobee Lake. The Shingobee River also receives large amounts of ground water discharge along its reach to Shingobee Lake providing a large, indirect source of ground water to the lake. Differences in nutrient concentrations reflect the residence times and nutrient supplies of these two lakes. The average phosphorus content of Shingobee Lake is about twice that of Williams Lake. Consequently, phy‐toplankton productivity in Shingobee Lake is much higher than in Williams Lake, leading to an oxygen‐deficient (&lt;1 ppm dissolved oxygen) hypolimnion within a month after overturn in both the spring and fall. Because of the extreme reducing conditions in the hypolimnion of Shingobee Lake, high concentrations of dissolved iron and manganese are present there during summer stratification. In some years, the manganese concentration in the hypolimnion of Shingobee Lake remains high throughout the year. Precipitation of iron and manganese minerals, presumed to be X‐ray amorphous oxyhydroxides, at periods of fall and spring overturn result in concentrations of iron and manganese in surface sediments of Shingobee Lake that are seven times and 27 times higher, respectively, than can be explained by contributions of iron and manganese from detrital aluminosilicates. These findings indicate that the source and amounts of this excess iron and manganese found in the sediments are correlated to the amount of iron‐ and manganese‐rich ground water discharging to Shingobee Lake. Because iron and manganese oxyhydroxides are efficient adsorbers of phosphorus, concentrations of phosphorus are also high in the sediments of Shingobee Lake. Without this sequestration of phosphorus, the productivity of Shingobee Lake would probably be much higher.</span></p>","language":"English","publisher":"NGWA","doi":"10.1111/j.1745-6584.2003.tb02437.x","usgsCitation":"Dean, W.E., Neff, B., Rosenberry, D.O., Winter, T.C., and Parkhurst, R.S., 2006, The significance of ground water to the accumulation of iron and manganese in the sediments of two hydrologically distinct lakes in north‐central Minnesota: A geological perspective: Ground Water, v. 41, no. 7, p. 951-963, https://doi.org/10.1111/j.1745-6584.2003.tb02437.x.","productDescription":"13 p.","startPage":"951","endPage":"963","costCenters":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true},{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"links":[{"id":371062,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","otherGeospatial":"North-central Minnestoa","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -95.9326171875,\n              49.03786794532644\n            ],\n            [\n              -95.712890625,\n              46.66451741754235\n            ],\n            [\n              -92.8125,\n              46.392411189814645\n            ],\n            [\n              -89.56054687499999,\n              47.931066347509784\n            ],\n            [\n              -90.94482421875,\n              48.29781249243716\n            ],\n            [\n              -91.40625,\n              48.151428143221224\n            ],\n            [\n              -92.21923828124999,\n              48.45835188280866\n            ],\n            [\n              -93.2958984375,\n              48.73445537176822\n            ],\n            [\n              -93.80126953124999,\n              48.63290858589535\n            ],\n            [\n              -94.52636718749999,\n              48.777912755501845\n            ],\n            [\n              -94.9658203125,\n              49.410973199695846\n            ],\n            [\n              -95.185546875,\n              49.439556958940855\n            ],\n            [\n              -95.20751953125,\n              49.023461463214126\n            ],\n            [\n              -95.9326171875,\n              49.03786794532644\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"41","issue":"7","noUsgsAuthors":false,"publicationDate":"2006-03-24","publicationStatus":"PW","contributors":{"authors":[{"text":"Dean, Walter E. dean@usgs.gov","contributorId":1801,"corporation":false,"usgs":true,"family":"Dean","given":"Walter","email":"dean@usgs.gov","middleInitial":"E.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":779103,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Neff, Brian 0000-0003-3718-7350 bneff@usgs.gov","orcid":"https://orcid.org/0000-0003-3718-7350","contributorId":198885,"corporation":false,"usgs":true,"family":"Neff","given":"Brian","email":"bneff@usgs.gov","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":779104,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rosenberry, Donald O. 0000-0003-0681-5641 rosenber@usgs.gov","orcid":"https://orcid.org/0000-0003-0681-5641","contributorId":1312,"corporation":false,"usgs":true,"family":"Rosenberry","given":"Donald","email":"rosenber@usgs.gov","middleInitial":"O.","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true},{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":779105,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Winter, Thomas C.","contributorId":84736,"corporation":false,"usgs":true,"family":"Winter","given":"Thomas","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":779106,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Parkhurst, Renee S. rparkhur@usgs.gov","contributorId":4719,"corporation":false,"usgs":true,"family":"Parkhurst","given":"Renee","email":"rparkhur@usgs.gov","middleInitial":"S.","affiliations":[],"preferred":true,"id":779107,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70207729,"text":"70207729 - 2006 - A continuous 250,000 yr record of oxygen and carbon isotopes in ostracode and bulk-sediment carbonate from Bear Lake, Utah-Idaho","interactions":[],"lastModifiedDate":"2020-06-15T17:17:52.973065","indexId":"70207729","displayToPublicDate":"2006-01-08T11:59:41","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3219,"text":"Quaternary Science Reviews","active":true,"publicationSubtype":{"id":10}},"title":"A continuous 250,000 yr record of oxygen and carbon isotopes in ostracode and bulk-sediment carbonate from Bear Lake, Utah-Idaho","docAbstract":"<div id=\"abstracts\" class=\"Abstracts u-font-serif\"><div id=\"aep-abstract-id9\" class=\"abstract author\"><div id=\"aep-abstract-sec-id10\"><p>Oxygen and carbon isotopes from a continuous, 120-m-long, carbonate-rich core from Bear Lake, Utah-Idaho, document dramatic fluctuations in the hydrologic budget of the lake over the last 250,000&nbsp;yr. Isotopic analyses of bulk sediment samples capture millennial-scale variability. Ostracode calcite was analyzed from 78 levels, mainly from the upper half of the core where valves are better preserved, to compare the isotopic value of purely endogenic carbonate with the bulk sediment, which comprises both endogenic and detrital components. The long core exhibits three relatively brief intervals with abundant endogenic aragonite (50±10%) and enriched<span>&nbsp;</span><i>δ</i><sup>18</sup>O and<span>&nbsp;</span><i>δ</i><sup>13</sup>C. These intervals are interpreted as warm/dry periods when the lake retracted into a topographically closed basin. We correlate these intervals with the interglacial periods of marine oxygen-isotope stages 1, 5e, and 7a, consistent with the presently available geochronological control. During most of the time represented by the core, the lake was fresher than the modern lake, as evidenced by depleted<span>&nbsp;</span><i>δ</i><sup>18</sup>O and<span>&nbsp;</span><i>δ</i><sup>13</sup>C in bulk-sediment carbonate.</p></div></div></div>","language":"English","publisher":"Elsevier","doi":"10.1016/j.quascirev.2005.12.011","usgsCitation":"Bright, J., Kaufman, D., Forester, R., and Dean, W.E., 2006, A continuous 250,000 yr record of oxygen and carbon isotopes in ostracode and bulk-sediment carbonate from Bear Lake, Utah-Idaho: Quaternary Science Reviews, v. 25, no. 17-18, p. 2258-2270, https://doi.org/10.1016/j.quascirev.2005.12.011.","productDescription":"13 p.","startPage":"2258","endPage":"2270","costCenters":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"links":[{"id":371057,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Idaho, Utah","otherGeospatial":"Bear Lake","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -111.42883300781249,\n              41.83682786072714\n            ],\n            [\n              -111.24206542968749,\n              41.83682786072714\n            ],\n            [\n              -111.24206542968749,\n              42.16340342422401\n            ],\n            [\n              -111.42883300781249,\n              42.16340342422401\n            ],\n            [\n              -111.42883300781249,\n              41.83682786072714\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"25","issue":"17-18","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Bright, Jordon","contributorId":76010,"corporation":false,"usgs":true,"family":"Bright","given":"Jordon","affiliations":[],"preferred":false,"id":779096,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kaufman, Darrell","contributorId":215397,"corporation":false,"usgs":false,"family":"Kaufman","given":"Darrell","affiliations":[{"id":39235,"text":"School of Earth Sciences & Environmental Sustainability, Northern Arizona University, Flagstaff, AZ 86011, USA","active":true,"usgs":false}],"preferred":false,"id":779097,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Forester, Richard","contributorId":59523,"corporation":false,"usgs":true,"family":"Forester","given":"Richard","affiliations":[],"preferred":false,"id":779098,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Dean, Walter E. dean@usgs.gov","contributorId":1801,"corporation":false,"usgs":true,"family":"Dean","given":"Walter","email":"dean@usgs.gov","middleInitial":"E.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":779099,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70207728,"text":"70207728 - 2006 - The geochemical record of the last 17,000 years in the Guaymas Basin, Gulf of California","interactions":[],"lastModifiedDate":"2020-06-15T17:14:03.912531","indexId":"70207728","displayToPublicDate":"2006-01-08T11:43:18","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1213,"text":"Chemical Geology","active":true,"publicationSubtype":{"id":10}},"title":"The geochemical record of the last 17,000 years in the Guaymas Basin, Gulf of California","docAbstract":"<p><span>Sediments deposited on the western slope of the Guaymas Basin in the central Gulf of California are composed predominantly of detrital clastic material and biogenic silica (biopal), with minor organic material (average of 2.8% organic carbon) and calcium carbonate. The CaCO</span><sub>3</sub><span>&nbsp;is derived from calcareous plankton and is highly variable ranging from 0% to 16%. In general, the CaCO</span><sub>3</sub><span>&nbsp;content of the sediments varies inversely with the biopal content, reflecting the relative abundance of calcareous and siliceous plankton in the photic zone. Siliceous plankton dominate when winds are predominantly out of the northwest producing strong upwelling. Calcareous plankton indicates weak southeasterly winds that bring warm, tropical Pacific surface water into the Gulf. Based mainly on relative abundances of biopal and CaCO</span><sub>3</sub><span>, the sediments deposited over the last 17,000</span><span>&nbsp;</span><span>years in the western Guaymas Basin can be divided into five intervals. In general, the sediments in the intervals with high biopal and low CaCO</span><sub>3</sub><span>&nbsp;are laminated, but this is not always true. Unlike most other continental margins of the world with well-developed oxygen minimum zones where highest concentrations of organic carbon and redox-sensitive trace metals occur in laminated sediments, the laminated sediments on the anoxic slope of the western Guaymas Basin do not always have the highest concentrations of organic carbon and trace metals such as Mo and Cd.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.chemgeo.2006.02.017","usgsCitation":"Dean, W.E., 2006, The geochemical record of the last 17,000 years in the Guaymas Basin, Gulf of California: Chemical Geology, v. 232, no. 3-4, p. 87-98, https://doi.org/10.1016/j.chemgeo.2006.02.017.","productDescription":"12 p.","startPage":"87","endPage":"98","costCenters":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true},{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true}],"links":[{"id":371056,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Mexico","otherGeospatial":"Guaymas Basin, Gulf of California","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -116.71874999999999,\n              21.94304553343818\n            ],\n            [\n              -104.67773437499999,\n              21.94304553343818\n            ],\n            [\n              -104.67773437499999,\n              32.24997445586331\n            ],\n            [\n              -116.71874999999999,\n              32.24997445586331\n            ],\n            [\n              -116.71874999999999,\n              21.94304553343818\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"232","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Dean, Walter E. dean@usgs.gov","contributorId":1801,"corporation":false,"usgs":true,"family":"Dean","given":"Walter","email":"dean@usgs.gov","middleInitial":"E.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":779095,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70207715,"text":"70207715 - 2006 - Geology of Delaware Water Gap National Recreation Area, New Jersey-Pennsylvania","interactions":[],"lastModifiedDate":"2020-06-15T15:26:01.917941","indexId":"70207715","displayToPublicDate":"2006-01-07T14:17:03","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1724,"text":"GSA Field Guides","active":true,"publicationSubtype":{"id":10}},"title":"Geology of Delaware Water Gap National Recreation Area, New Jersey-Pennsylvania","docAbstract":"<p><span>Many of the parks within the National Park System owe their uniqueness to their geologic framework. Their scenery is the result of diverse natural processes acting upon a variety of rocks that were deposited in varied environments in the geologic past. The Delaware Water Gap National Recreation Area (DEWA) contains a rich geologic and cultural history within its 68,714 acre boundary. Following the border between New Jersey and Pennsylvania, the Delaware River has cut a magnificent gorge through Kit-tantinny Mountain, the Delaware Water Gap, to which all other gaps in the Appalachian Mountains have been compared. Proximity to many institutions of learning in this densely populated area of the northeastern United States (Fig.&nbsp;</span><a class=\"link link-reveal link-table xref-fig\" data-open=\"ch04fig1\">1</a><span>) makes DEWA an ideal locality to study the geology of this part of the Appalachian Mountains. This one-day field trip comprises two stops within the gap itself and will include discussion on stratigraphy, structure, geomorphology, and glacial geology. The first stop will be at the bottom of the gap in Pennsylvania to look at the magnificent exposures in the cleft on the New Jersey side. This will be followed by a traverse to the top of Mount Tammany along a popular trail, where we will compare the geology across the river in Pennsylvania. Much of the information presented in this guidebook is summarized from&nbsp;</span><a class=\"link link-ref link-reveal xref-bibr\" data-open=\"ch04r11\">Epstein (2001a</a><span>,&nbsp;</span><a class=\"link link-ref link-reveal xref-bibr\" data-open=\"ch04r12\">2001b</a><span>,&nbsp;</span><a class=\"link link-ref link-reveal xref-bibr\" data-open=\"ch04r13\">2001c</a><span>) and&nbsp;</span><a class=\"link link-ref link-reveal xref-bibr\" data-open=\"ch04r18\">Epstein and Lyttle (2001)</a><span>.</span></p>","language":"English","publisher":"GSA","doi":"10.1130/2006.fld008(04)","usgsCitation":"Epstein, J.B., 2006, Geology of Delaware Water Gap National Recreation Area, New Jersey-Pennsylvania: GSA Field Guides, v. 8, p. 47-63, https://doi.org/10.1130/2006.fld008(04).","productDescription":"17 p.","startPage":"47","endPage":"63","costCenters":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true},{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true}],"links":[{"id":371046,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New Jersey, Pennsylvania","otherGeospatial":"Delaware Water Gap National Recreation Area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -75.34423828125,\n              41.17038447781618\n            ],\n            [\n              -74.542236328125,\n              41.17038447781618\n            ],\n            [\n              -74.542236328125,\n              41.96765920367816\n            ],\n            [\n              -75.34423828125,\n              41.96765920367816\n            ],\n            [\n              -75.34423828125,\n              41.17038447781618\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"8","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Epstein, Jack B. jepstein@usgs.gov","contributorId":1412,"corporation":false,"usgs":true,"family":"Epstein","given":"Jack","email":"jepstein@usgs.gov","middleInitial":"B.","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true},{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true}],"preferred":true,"id":779076,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70207682,"text":"70207682 - 2006 - Introduction to ‘Antarctic climate evolution: View from the margin’","interactions":[],"lastModifiedDate":"2020-06-08T13:13:12.68654","indexId":"70207682","displayToPublicDate":"2006-01-06T11:38:30","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2996,"text":"Palaeogeography, Palaeoclimatology, Palaeoecology","printIssn":"0031-0182","active":true,"publicationSubtype":{"id":10}},"title":"Introduction to ‘Antarctic climate evolution: View from the margin’","docAbstract":"<p>This special issue on “Antarctic Climate Evolution—view from the margin” presents results from modelling studies and reports on geoscience data aimed at improving our understanding of the behaviour of the Antarctic ice sheet and the climate of the region. This research field is of interest because of the sensitivity of the polar regions to global warming, and because of the influence of the Antarctic ice sheet on global sea level and climate through most if not all of the Cenozoic Era. The Antarctic ice sheet both responds to and forces changes on global climate and sea level. We need to be aware of the scale and frequency of these changes if we are to understand past patterns of environmental change elsewhere on earth. It was only three decades ago that we discovered from strata drilled in shelf basins on the Antarctic margin that the Antarctic ice sheet had a history that predated the Quaternary ice ages by over 20 million years (<a class=\"workspace-trigger\" name=\"bbib16\" href=\"https://www.sciencedirect.com/science/article/pii/S0031018205004773?via%3Dihub#bib16\" data-mce-href=\"https://www.sciencedirect.com/science/article/pii/S0031018205004773?via%3Dihub#bib16\">Hayes et al., 1975</a>). Later that year the first interpretation of Antarctic glacial history through the Cenozoic Era from oxygen isotopes, recorded in foraminifera from deep-sea sediment cores, was published (<a class=\"workspace-trigger\" name=\"bbib30\" href=\"https://www.sciencedirect.com/science/article/pii/S0031018205004773?via%3Dihub#bib30\" data-mce-href=\"https://www.sciencedirect.com/science/article/pii/S0031018205004773?via%3Dihub#bib30\">Shackleton and Kennett, 1975</a>). Revisions with a more extensive database have modified the story a little (<a class=\"workspace-trigger\" name=\"bbib21\" href=\"https://www.sciencedirect.com/science/article/pii/S0031018205004773?via%3Dihub#bib21\" data-mce-href=\"https://www.sciencedirect.com/science/article/pii/S0031018205004773?via%3Dihub#bib21\">Miller et al., 1987</a>,<span>&nbsp;</span><a class=\"workspace-trigger\" name=\"bbib36\" href=\"https://www.sciencedirect.com/science/article/pii/S0031018205004773?via%3Dihub#bib36\" data-mce-href=\"https://www.sciencedirect.com/science/article/pii/S0031018205004773?via%3Dihub#bib36\">Zachos et al., 2001</a>), and there have been recent attempts to resolve the temperature–ice volume ambiguity (<a class=\"workspace-trigger\" name=\"bbib19\" href=\"https://www.sciencedirect.com/science/article/pii/S0031018205004773?via%3Dihub#bib19\" data-mce-href=\"https://www.sciencedirect.com/science/article/pii/S0031018205004773?via%3Dihub#bib19\">Lear et al., 2000</a>). However, reports on strata drilled on the Antarctic margin have unambiguously shown the character of this huge ice sheet, which was oscillating in the Oligocene (<a class=\"workspace-trigger\" name=\"bbib3\" href=\"https://www.sciencedirect.com/science/article/pii/S0031018205004773?via%3Dihub#bib3\" data-mce-href=\"https://www.sciencedirect.com/science/article/pii/S0031018205004773?via%3Dihub#bib3\">Barrett et al., 1987</a>,<span>&nbsp;</span><a class=\"workspace-trigger\" name=\"bbib2\" href=\"https://www.sciencedirect.com/science/article/pii/S0031018205004773?via%3Dihub#bib2\" data-mce-href=\"https://www.sciencedirect.com/science/article/pii/S0031018205004773?via%3Dihub#bib2\">Barrett, 1999</a>) with a period and magnitude comparable with the Northern Hemisphere ice sheets of the Quaternary (<a class=\"workspace-trigger\" name=\"bbib22\" href=\"https://www.sciencedirect.com/science/article/pii/S0031018205004773?via%3Dihub#bib22\" data-mce-href=\"https://www.sciencedirect.com/science/article/pii/S0031018205004773?via%3Dihub#bib22\">Naish et al., 2001a</a>,<span>&nbsp;</span><a class=\"workspace-trigger\" name=\"bbib23\" href=\"https://www.sciencedirect.com/science/article/pii/S0031018205004773?via%3Dihub#bib23\" data-mce-href=\"https://www.sciencedirect.com/science/article/pii/S0031018205004773?via%3Dihub#bib23\">Naish et al., 2001b</a>). In this issue we present further research on the history of the Antarctic ice sheet from Oligocene to recent times, most of them from the Antarctic margin, but with some on the nature of the deep-sea isotope record, and others using recently developed modeling techniques to investigate the influence of atmosphere, ocean and biosphere on past Antarctic climate.</p><p>This special issue is the third in three years on the theme of Antarctic Climate Evolution. The first followed a workshop in Erice, Sicily, in 2001 to report on results from ANTOSTRAT, a SCAR-sponsored project for gathering and analysing circum-Antarctic seismic data for planning and promoting offshore drilling for climate history. The introduction to that issue (Florindo et al., 2003) provides a review of the recent history of circum-Antarctic drilling by the Ocean Drilling Program (Legs 113, 114, 119, 120, 177, 178, 188 and 189) and the Cape Roberts Project. For a more comprehensive review of earlier drilling in the Ross Sea region (Deep Sea Drilling Project Leg 28, Dry Valley Drilling Project, McMurdo Sound Sediment and Tectonic Studies, Cenozoic Investigations in the western Ross Sea) see<span>&nbsp;</span>Hambrey and Barrett (1993). The first of these issues (Florindo et al., 2003) featured a global plate reconstruction of the Southern Hemisphere through Cenozoic time with emphasis on evolution of Cenozoic seaways (Lawver and Gahagan, 2003) along with a study of the inception and early evolution of the EAIS using a new coupled global climate (GCM)–dynamic ice sheet model (DeConto and Pollard, 2003b), as well as data from recent drilling around the margin covering time period from Cretaceous to the present. A second special issue on the same theme (Florindo et al., 2005) also featured a mix of modelling and data papers with a focus on the Eocene–Oligocene boundary and the initiation of ice sheet growth, including a pioneering attempt to evaluate the relative influence of fluvial versus glacial processes in shaping the landscape of the Prydz Bay sector of Antarctica (Jamieson et al., 2005). The remainder of the issue comprised further papers on seismic stratigraphy and reports from drilling around the margin. The papers to be found in this special issue, like the previous two, maintain the mix of modelling- and data-oriented papers that reflect the range of this research.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.palaeo.2005.08.003","usgsCitation":"Barrett, P.J., Florindo, F., and Cooper, A.K., 2006, Introduction to ‘Antarctic climate evolution: View from the margin’: Palaeogeography, Palaeoclimatology, Palaeoecology, v. 231, no. 1-2, p. 1-8, https://doi.org/10.1016/j.palaeo.2005.08.003.","productDescription":"8 p.","startPage":"1","endPage":"8","costCenters":[{"id":520,"text":"Pacific Coastal and Marine Science 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,{"id":70207419,"text":"70207419 - 2006 - Lead isotopic constraints on the metallogeny of middle and late Paleozoic syngenetic base metal occurrences in the Yukon-Tanana and Slide Mountain/Seventymile Terranes and adjacent portions of the North American miogeocline","interactions":[],"lastModifiedDate":"2019-12-19T09:31:19","indexId":"70207419","displayToPublicDate":"2006-01-02T09:28:30","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3458,"text":"Special Paper - Geological Association of Canada","active":true,"publicationSubtype":{"id":10}},"title":"Lead isotopic constraints on the metallogeny of middle and late Paleozoic syngenetic base metal occurrences in the Yukon-Tanana and Slide Mountain/Seventymile Terranes and adjacent portions of the North American miogeocline","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Geological Association of Canada","usgsCitation":"Mortensen, J., Dusel-Bacon, C., Hunt, J., and Gabites, J., 2006, Lead isotopic constraints on the metallogeny of middle and late Paleozoic syngenetic base metal occurrences in the Yukon-Tanana and Slide Mountain/Seventymile Terranes and adjacent portions of the North American miogeocline: Special Paper - Geological Association of Canada, v. 45, p. 261-280.","productDescription":"20 p.","startPage":"261","endPage":"280","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":370461,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States, Canada","state":"Alaska","otherGeospatial":"Yukon Territory","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -154.599609375,\n              61.10078883158897\n            ],\n            [\n              -141.064453125,\n              61.10078883158897\n            ],\n            [\n              -122.958984375,\n              59.7563950493563\n            ],\n            [\n              -122.431640625,\n              64.69910544204765\n            ],\n            [\n              -141.064453125,\n              68.5924865825295\n            ],\n            [\n              -154.599609375,\n              68.5924865825295\n            ],\n            [\n              -154.599609375,\n              61.10078883158897\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"45","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Mortensen, J.K. 0000-0001-8805-9856","orcid":"https://orcid.org/0000-0001-8805-9856","contributorId":201246,"corporation":false,"usgs":false,"family":"Mortensen","given":"J.K.","email":"","affiliations":[],"preferred":false,"id":777942,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dusel-Bacon, Cynthia 0000-0001-8481-739X cdusel@usgs.gov","orcid":"https://orcid.org/0000-0001-8481-739X","contributorId":2797,"corporation":false,"usgs":true,"family":"Dusel-Bacon","given":"Cynthia","email":"cdusel@usgs.gov","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":777943,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hunt, J.","contributorId":18297,"corporation":false,"usgs":true,"family":"Hunt","given":"J.","email":"","affiliations":[],"preferred":false,"id":777944,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Gabites, J.","contributorId":221367,"corporation":false,"usgs":false,"family":"Gabites","given":"J.","email":"","affiliations":[],"preferred":false,"id":777945,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70207418,"text":"70207418 - 2006 - Paleozoic tectonic and metallogenic evolution of the pericratonic rocks of east-central Alaska and adjacent Yukon Territory","interactions":[],"lastModifiedDate":"2019-12-19T09:26:14","indexId":"70207418","displayToPublicDate":"2006-01-02T09:18:55","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3458,"text":"Special Paper - Geological Association of Canada","active":true,"publicationSubtype":{"id":10}},"title":"Paleozoic tectonic and metallogenic evolution of the pericratonic rocks of east-central Alaska and adjacent Yukon Territory","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Geological Association of Canada","usgsCitation":"Nelson, J.L., Colpron, M., Piercey, S., Dusel-Bacon, C., Murphy, D., and Roots, C., 2006, Paleozoic tectonic and metallogenic evolution of the pericratonic rocks of east-central Alaska and adjacent Yukon Territory: Special Paper - Geological Association of Canada, v. 45, p. 25-74.","productDescription":"50 p.","startPage":"25","endPage":"74","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":370460,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":370459,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.sjpgeoconsulting.com/SJPGeoConsulting/Publications.html"}],"country":"United States, Canada","state":"Alaska","otherGeospatial":"Yukon Territory ","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -154.599609375,\n              61.10078883158897\n            ],\n            [\n              -141.064453125,\n              61.10078883158897\n            ],\n            [\n              -122.958984375,\n              59.7563950493563\n            ],\n            [\n              -122.431640625,\n              64.69910544204765\n            ],\n            [\n              -141.064453125,\n              68.5924865825295\n            ],\n            [\n              -154.599609375,\n              68.5924865825295\n            ],\n            [\n              -154.599609375,\n              61.10078883158897\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"45","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Nelson, JoAnne L.","contributorId":221362,"corporation":false,"usgs":false,"family":"Nelson","given":"JoAnne","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":777936,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Colpron, Maurice","contributorId":221363,"corporation":false,"usgs":false,"family":"Colpron","given":"Maurice","email":"","affiliations":[],"preferred":false,"id":777937,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Piercey, Stephen","contributorId":221364,"corporation":false,"usgs":false,"family":"Piercey","given":"Stephen","email":"","affiliations":[],"preferred":false,"id":777938,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Dusel-Bacon, Cynthia 0000-0001-8481-739X cdusel@usgs.gov","orcid":"https://orcid.org/0000-0001-8481-739X","contributorId":2797,"corporation":false,"usgs":true,"family":"Dusel-Bacon","given":"Cynthia","email":"cdusel@usgs.gov","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":777939,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Murphy, Donald","contributorId":221365,"corporation":false,"usgs":false,"family":"Murphy","given":"Donald","email":"","affiliations":[],"preferred":false,"id":777940,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Roots, Charlie","contributorId":221366,"corporation":false,"usgs":false,"family":"Roots","given":"Charlie","email":"","affiliations":[],"preferred":false,"id":777941,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70163007,"text":"70163007 - 2006 - North corridor Silurian-Devonian aquifer study frequently asked questions","interactions":[],"lastModifiedDate":"2016-01-29T15:46:27","indexId":"70163007","displayToPublicDate":"2006-01-01T16:45:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":359,"text":"Fact Sheet","active":false,"publicationSubtype":{"id":6}},"title":"North corridor Silurian-Devonian aquifer study frequently asked questions","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Iowa Water Science Center","publisherLocation":"Iowa City","doi":"10.3133/70163007","usgsCitation":"Iowa Water Science Center, 2006, North corridor Silurian-Devonian aquifer study frequently asked questions: Fact Sheet, HTML Document, https://doi.org/10.3133/70163007.","productDescription":"HTML Document","onlineOnly":"Y","additionalOnlineFiles":"N","costCenters":[{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true}],"links":[{"id":315333,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":315325,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://ia.water.usgs.gov/projects/icproj/FAQ.html"}],"country":"United States","state":"Iowa","county":"Johnson","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-91.3677,41.8603],[-91.3673,41.7745],[-91.3675,41.6855],[-91.3671,41.5987],[-91.3679,41.5107],[-91.3687,41.4235],[-91.4839,41.4222],[-91.4843,41.4286],[-91.492,41.4405],[-91.5033,41.4493],[-91.5026,41.452],[-91.4989,41.4538],[-91.4988,41.4592],[-91.5145,41.4676],[-91.5156,41.4704],[-91.5136,41.4767],[-91.5038,41.4779],[-91.5029,41.4874],[-91.5039,41.4933],[-91.5076,41.4939],[-91.5107,41.4944],[-91.5112,41.4971],[-91.508,41.5016],[-91.5098,41.5034],[-91.5117,41.5016],[-91.5148,41.4985],[-91.5197,41.4981],[-91.5196,41.5027],[-91.5281,41.5078],[-91.528,41.511],[-91.5991,41.5107],[-91.7138,41.511],[-91.8291,41.5116],[-91.827,41.6001],[-91.8337,41.6006],[-91.8335,41.6865],[-91.8327,41.775],[-91.8318,41.8617],[-91.716,41.862],[-91.5989,41.8612],[-91.4836,41.8608],[-91.3677,41.8603]]]},\"properties\":{\"name\":\"Johnson\",\"state\":\"IA\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56ac9b6be4b0403299f53a87"}
,{"id":70162941,"text":"70162941 - 2006 - Research plan and preliminary results: A field research site for emerging contaminants in Iowa","interactions":[],"lastModifiedDate":"2018-10-22T10:41:30","indexId":"70162941","displayToPublicDate":"2006-01-01T16:15:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2555,"text":"Journal of the Iowa Academy of Science","active":true,"publicationSubtype":{"id":10}},"title":"Research plan and preliminary results: A field research site for emerging contaminants in Iowa","docAbstract":"<p>Research has recently documented the prevalence of a wide variety of pharmaceuticals and other emerging contaminants (ECs) in streams across the United States. Wastewater treatment plants (WWTPs) have been found to be an important source and collection point of ECs to streams as many ECs are incompletely removed during treatment. To investigate the complex in-stream processes (e.g., dilution, sorption, degradation, dispersion, etc.) that can affect ECs following their input from a WWTP and determining if such input is having an effect on the aquatic ecosystem requires the integration of multi-disciplinary efforts at a carefully selected field site. Preliminary work has identified an 8-km reach of Fourmile Creek in central Iowa as an ideal research site to investigate such important research questions pertaining to ECs. Unique aspects of Fourmile Creek included: (1) it single source effluent-dominated stream, (2) background data document the input of a wide variety of ECs from WWTP discharge, (3) small basin size, (4) relatively simple flow system, (5) background data suggest that undefined processes are taking place decreasing the level of select ECs during stream transport, (6) the WWTP uses a treatment technology (activated sludge) typical of many towns in Iowa and the United States (7) a hydrogeologic setting of a low-gradient, small stream (average discharge less than 1.41 m&sup3;/s) in glacial drift is typical of many areas in Iowa and across the Midwest, and (8) the existence of a low-head clam approximately 2 km upstream of the WWTP outfall allowing more accurate \"above WWTP\" and \"below WWTP\" comparisons in aquatic ecosystems. Furthermore, the WWTP is scheduled to close by 2011 providing a unique opportunity to determine how stream hydrology, water chemistry and aquatic biota react to the removal of the primary source of flow and ECs in this system. This will allow a novel \"before\" and \"after\" assessment not previously available in EC research. Research to date at the site has included installation of a streamflow gauging station, dye-tracing tests (to determine water travel times), Lagrangian water-quality sampling at two flow/water temperature regimes, and sampling for ECs in bed sediment. Selected fish have been collected for analysis and identification. In addition, basic fish community and fish health assessment for different seasons and spawning conditions are being analyzed. 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,{"id":70200408,"text":"70200408 - 2006 - Fulfilling a paradoxical mandate: can the Environmental Water Account ensure the reliability of freshwater exports from the Sacramento-San Joaquin Delta and simultaneously protect delta smelt (Hypomesus transpacificus) from excessive entrainment?","interactions":[],"lastModifiedDate":"2018-10-16T16:11:19","indexId":"70200408","displayToPublicDate":"2006-01-01T16:11:11","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3914,"text":"Interagency Ecological Program Newsletter","active":true,"publicationSubtype":{"id":10}},"title":"Fulfilling a paradoxical mandate: can the Environmental Water Account ensure the reliability of freshwater exports from the Sacramento-San Joaquin Delta and simultaneously protect delta smelt (Hypomesus transpacificus) from excessive entrainment?","docAbstract":"<p>The San Francisco Estuary (SFE) is often defined by its extremes. It is considered one of the most urbanized estuaries in the world (Conomos 1979, Nichols et al. 1986), and one of the most invaded estuaries in the United States, with hundreds of aquatic nonindigenous species established throughout the system (Cohen and Carlton 1995, Dill and Cordone 1997, Kimmerer and Orsi 1996). It is also one of the most managed estuaries, particularly in relation to freshwater inflow, water circulation, and water quality (Jassby and Powell 1994, CSWRCB 1995, Arthur et al. 1996, Kimmerer 2002). Despite this high level of disturbance, the SFE is one of the most valuable natural resources in the western United States (CALFED 2000). The SFE provides important habitat for numerous native plant and animal species, many of special concern, as well as several species with sport and commercial value (CALFED 2000). Conserving and restoring estuarine habitat and natural resources is a pressing and complex challenge for the responsible government agencies because human water needs continue to increase in concert with continuing urbanization of the watershed.</p>","language":"English","publisher":"Interagency Ecological Program for the San Francisco Estuary","usgsCitation":"Hymanson, Z., and Brown, L.R., 2006, Fulfilling a paradoxical mandate: can the Environmental Water Account ensure the reliability of freshwater exports from the Sacramento-San Joaquin Delta and simultaneously protect delta smelt (Hypomesus transpacificus) from excessive entrainment?: Interagency Ecological Program Newsletter, v. 19, no. 1, p. 28-49.","productDescription":"22 p.","startPage":"28","endPage":"49","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"links":[{"id":358445,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":358444,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://water.ca.gov/-/media/DWR-Website/Web-Pages/Programs/Environmental-Services/Interagency-Ecological-Program/Files/Newsletters/IEP-Newsletter-2006-Vol19-Issue1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"volume":"19","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5c10e014e4b034bf6a7feedb","contributors":{"authors":[{"text":"Hymanson, Zach","contributorId":209753,"corporation":false,"usgs":false,"family":"Hymanson","given":"Zach","email":"","affiliations":[],"preferred":false,"id":748736,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brown, Larry R. 0000-0001-6702-4531 lrbrown@usgs.gov","orcid":"https://orcid.org/0000-0001-6702-4531","contributorId":1717,"corporation":false,"usgs":true,"family":"Brown","given":"Larry","email":"lrbrown@usgs.gov","middleInitial":"R.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":748737,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70129589,"text":"70129589 - 2006 - A semi-empirical model for the estimation of maximum horizontal displacement due to liquefaction-induced lateral spreading","interactions":[],"lastModifiedDate":"2017-12-15T14:48:20","indexId":"70129589","displayToPublicDate":"2006-01-01T16:05:00","publicationYear":"2006","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"A semi-empirical model for the estimation of maximum horizontal displacement due to liquefaction-induced lateral spreading","docAbstract":"<p>During the 1906 San Francisco Earthquake, liquefaction-induced lateral spreading and resultant ground displacements damaged bridges, buried utilities, and lifelines, conventional structures, and other developed works. This paper presents an improved engineering tool for the prediction of maximum displacement due to liquefaction-induced lateral spreading. A semi-empirical approach is employed, combining mechanistic understanding and data from laboratory testing with data and lessons from full-scale earthquake field case histories. The principle of strain potential index, based primary on correlation of cyclic simple shear laboratory testing results with in-situ Standard Penetration Test (SPT) results, is used as an index to characterized the deformation potential of soils after they liquefy. A Bayesian probabilistic approach is adopted for development of the final predictive model, in order to take fullest advantage of the data available and to deal with the inherent uncertainties intrinstiic to the back-analyses of field case histories. A case history from the 1906 San Francisco Earthquake is utilized to demonstrate the ability of the resultant semi-empirical model to estimate maximum horizontal displacement due to liquefaction-induced lateral spreading.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Proceedings of the 8th U.S. National Conference on Earthquake Engineering","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"8th U.S. National Conference of Earthquake Engineering","conferenceDate":"2006-04-18T00:00:00","conferenceLocation":"San Francisco, CA","language":"English","publisher":"Earthquake Engineering Research Institute","publisherLocation":"Oakland, CA","usgsCitation":"Faris, A.T., Seed, R., Kayen, R., and Wu, J., 2006, A semi-empirical model for the estimation of maximum horizontal displacement due to liquefaction-induced lateral spreading, <i>in</i> Proceedings of the 8th U.S. National Conference on Earthquake Engineering, San Francisco, CA, 2006-04-18T00:00:00, 1323; 10 p.","productDescription":"1323; 10 p.","numberOfPages":"10","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"links":[{"id":295702,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"544a18ade4b04d2014abfb03","contributors":{"authors":[{"text":"Faris, Allison T.","contributorId":76248,"corporation":false,"usgs":true,"family":"Faris","given":"Allison","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":503897,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Seed, Raymond B.","contributorId":62162,"corporation":false,"usgs":true,"family":"Seed","given":"Raymond B.","affiliations":[],"preferred":false,"id":503896,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kayen, Robert E. rkayen@usgs.gov","contributorId":2787,"corporation":false,"usgs":true,"family":"Kayen","given":"Robert E.","email":"rkayen@usgs.gov","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":503894,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Wu, Jiaer","contributorId":19102,"corporation":false,"usgs":true,"family":"Wu","given":"Jiaer","email":"","affiliations":[],"preferred":false,"id":503895,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":79526,"text":"sir20065179 - 2006 - Watershed characteristics and pre-restoration surface-water hydrology of Minebank Run, Baltimore County, Maryland, water years 2002-04","interactions":[],"lastModifiedDate":"2023-03-09T20:41:47.458782","indexId":"sir20065179","displayToPublicDate":"2006-01-01T16:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2006-5179","displayTitle":"Watershed Characteristics and Pre-Restoration Surface-Water Hydrology of Minebank Run, Baltimore County, Maryland, Water Years 2002-04","title":"Watershed characteristics and pre-restoration surface-water hydrology of Minebank Run, Baltimore County, Maryland, water years 2002-04","docAbstract":"Stream restoration efforts have been ongoing in Maryland since the early 1990s. Physical stream restoration often involves replacement of lost sediments to elevate degraded streambeds, re-establishment of riffle-pool sequences along the channel profile, planting vegetation in riparian zones, and re-constructing channel banks, point bars, flood plains, and stream-meanders. The primary goal of many restoration efforts is to re-establish geomorphic stability of the stream channel and reduce erosive energy from urban runoff. Monitoring streams prior to and after restoration could help quantify other possible benefits of stream restoration, such as improved water quality and biota.\r\n\r\nThis report presents general watershed characteristics associated with the Minebank Run watershed; a small, urban watershed in the south-central section of Baltimore County, Maryland that was physically restored in phases during 1999, 2004, and 2005. The physiography, geology, hydrology, land use, soils, and pre-restoration geomorphic setting of the unrestored stream channel are discussed.\r\n\r\nThe report describes a reach of Minebank Run that was selected for the purpose of collecting several types of environmental data prior to restoration, including continuous-record and partial-record stage and streamflow data, precipitation, and ground-water levels. Examples of surface-water data that were collected in and near the study reach during water years 2002 through 2004, including continuous-record streamflow, partial-record stage and discharge, and precipitation, are described. These data were used in analyses of several characteristics of surface-water hydrology in the watershed, including (1) rainfall totals, storm duration, and intensity, (2) instantaneous peak discharge and daily mean discharge, (3) stage-discharge ratings, (4) hydraulic-geometry relations, (5) water-surface slope, (6) time of concentration, (7) flood frequency, (8) flood volume, and (9) rainfall-runoff relations.\r\n\r\nSeveral hydrologic characteristics that are typical of urban environments were quantified by these analyses. These include (1) large ratios of peak discharge to daily mean discharge as an indicator of flashiness, (2) consistent shifting of the stage-discharge rating over short periods of time that indicates instability of the stream channel, (3) analyses of hydraulic-geometry relations that indicate mean velocities of 11 feet per second or more while the flow is contained in the stream channel, (4) discharges that are 4 to 5 times larger in Minebank Run for corresponding flood frequency recurrence intervals than in Slade Run, which is a Piedmont watershed of similar size with smaller percentages of urban development, and (5) flood waves that can travel through the stream channel at a velocity of 412 feet per minute, or 6.9 feet per second.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/sir20065179","collaboration":"Prepared in cooperation with the U.S. Environmental Protection Agency","usgsCitation":"Doheny, E.J., Starsoneck, R.J., Striz, E.A., and Mayer, P.M., 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,{"id":70129588,"text":"70129588 - 2006 - Guided to gather: toy plane upgraded with telemetry","interactions":[],"lastModifiedDate":"2017-12-15T14:49:02","indexId":"70129588","displayToPublicDate":"2006-01-01T15:57:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5416,"text":"GPS World","active":true,"publicationSubtype":{"id":10}},"title":"Guided to gather: toy plane upgraded with telemetry","docAbstract":"GPS/INS and infrared optical sensors propel USGS's transformation of a remote-controlled one-quarter scale recreational aircraft into a low-cost unmanned aerial vehicle designed for environmental particulate collection.","language":"English","publisher":"Advanstar Communications","publisherLocation":"Eugene, OR","usgsCitation":"Wiese, V., and Wiese, D., 2006, Guided to gather: toy plane upgraded with telemetry: GPS World, v. 17, no. 2, p. 32-38.","productDescription":"7 p.","startPage":"32","endPage":"38","numberOfPages":"7","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"links":[{"id":295701,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":295700,"type":{"id":15,"text":"Index Page"},"url":"https://www.nxtbook.com/nxtbooks/questex/gps0206/"}],"volume":"17","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"544a18d8e4b04d2014abfb38","contributors":{"authors":[{"text":"Wiese, Vanessa","contributorId":33244,"corporation":false,"usgs":true,"family":"Wiese","given":"Vanessa","email":"","affiliations":[],"preferred":false,"id":503892,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wiese, Dana","contributorId":33644,"corporation":false,"usgs":true,"family":"Wiese","given":"Dana","affiliations":[],"preferred":false,"id":503893,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":79457,"text":"ofr20061295 - 2006 - Preliminary Utah oil shale database","interactions":[],"lastModifiedDate":"2026-02-20T22:09:00.377687","indexId":"ofr20061295","displayToPublicDate":"2006-01-01T15:48:23","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2006-1295","title":"Preliminary Utah oil shale database","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20061295","collaboration":"Prepared under a cooperative agreement with the Utah Geological Survey and in cooperation with the U.S. Department of Energy","usgsCitation":"Dyni, J.R., Donnell, J.R., Berg, V., and Tabet, D., 2006, Preliminary Utah oil shale database: U.S. Geological Survey Open-File Report 2006-1295, 1 CD-ROM, https://doi.org/10.3133/ofr20061295.","productDescription":"1 CD-ROM","costCenters":[],"links":[{"id":500377,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2006/1295/ofr20061295.zip","text":"CD-ROM","linkFileType":{"id":6,"text":"zip"}},{"id":289265,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Utah","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114.05,37.0 ], [ -114.05,42.0 ], [ -109.04,42.0 ], [ -109.04,37.0 ], [ -114.05,37.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53b286f8e4b07b8813a554f4","contributors":{"authors":[{"text":"Dyni, John R. jdyni@usgs.gov","contributorId":756,"corporation":false,"usgs":true,"family":"Dyni","given":"John","email":"jdyni@usgs.gov","middleInitial":"R.","affiliations":[],"preferred":true,"id":289959,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Donnell, J. R.","contributorId":60673,"corporation":false,"usgs":true,"family":"Donnell","given":"J.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":289961,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Berg, Vanden","contributorId":74941,"corporation":false,"usgs":true,"family":"Berg","given":"Vanden","email":"","affiliations":[],"preferred":false,"id":289962,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Tabet, D.E.","contributorId":31536,"corporation":false,"usgs":true,"family":"Tabet","given":"D.E.","affiliations":[],"preferred":false,"id":289960,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70006994,"text":"70006994 - 2006 - Multimodeling: new approaches for linking ecological models","interactions":[],"lastModifiedDate":"2014-06-30T15:48:35","indexId":"70006994","displayToPublicDate":"2006-01-01T15:39:03","publicationYear":"2006","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Multimodeling: new approaches for linking ecological models","docAbstract":"<p>The Everglades region of South Florida presents one of the major natural system management challenges facing the United States.  With its assortment of alligators, crocodiles, manatees, panthers, large mixed flocks of wading birds, highly diverse subtropical flora, and sea of sawgrass, the ecosystem is unique in this country (Davis and Ogden 1994).  The region is also perhaps the largest human-controlled system on the planet in that the major environmental factor influencing the region is water, and water flows are managed on a daily basis--subject to the vagaries of rainfall--by a massive system of locks, pumps, canals, and levees constructed over the past century.  The changes brought about by such control have led to extensive modifications of historical patterns and magnitudes of flow, causing large declines in many native species, extensive changes in nutrient cycling and vegetation across south Florida, and great increases in pollutants such as mercury.  Constrained by the conflicting demands of agriculture, urban human populations, and wildlife for control of water resources, and the varying agendas of hosts of government agencies and nongovernmental organizations, there is now an ongoing effort to plan for major changes to the system with expenditure estimates of eight billion dollars or more over the next several decades (USACOE 1999).  Carrying out such planning, particularly as it impacts the natural systems of the region, provides one of the major challenges to the new field of computational ecology.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Predicting Species Occurences: Issues of Accuracy and Scale","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","publisher":"Island Press","publisherLocation":"Covello, CA","usgsCitation":"Gross, L.J., and DeAngelis, D., 2006, Multimodeling: new approaches for linking ecological models, chap. <i>of</i> Predicting Species Occurences: Issues of Accuracy and Scale, p. 467-474.","productDescription":"p. 467-474","numberOfPages":"8","costCenters":[{"id":275,"text":"Florida Integrated Science Center","active":false,"usgs":true}],"links":[{"id":289263,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Florida","otherGeospatial":"Everglades","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -81.393156,25.842687 ], [ -81.393156,25.873513 ], [ -81.379211,25.873513 ], [ -81.379211,25.842687 ], [ -81.393156,25.842687 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53b286f7e4b07b8813a554e6","contributors":{"editors":[{"text":"Scott, J. Michael","contributorId":98877,"corporation":false,"usgs":true,"family":"Scott","given":"J.","email":"","middleInitial":"Michael","affiliations":[],"preferred":false,"id":508422,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Heglund, Patricia J.","contributorId":51248,"corporation":false,"usgs":true,"family":"Heglund","given":"Patricia J.","affiliations":[],"preferred":false,"id":508421,"contributorType":{"id":2,"text":"Editors"},"rank":2},{"text":"Morrison, Michael L.","contributorId":111417,"corporation":false,"usgs":true,"family":"Morrison","given":"Michael L.","affiliations":[],"preferred":false,"id":508423,"contributorType":{"id":2,"text":"Editors"},"rank":3}],"authors":[{"text":"Gross, Louis J.","contributorId":56705,"corporation":false,"usgs":true,"family":"Gross","given":"Louis","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":355625,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"DeAngelis, Donald L. 0000-0002-1570-4057","orcid":"https://orcid.org/0000-0002-1570-4057","contributorId":88015,"corporation":false,"usgs":true,"family":"DeAngelis","given":"Donald L.","affiliations":[],"preferred":false,"id":355626,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70230101,"text":"ofr20061333 - 2006 - Quality-assurance plan for the analysis of fluvial sediment by the U.S. Geological Survey New Mexico Water Science Center Sediment Laboratory","interactions":[],"lastModifiedDate":"2022-04-05T19:33:28.256475","indexId":"ofr20061333","displayToPublicDate":"2006-01-01T15:33:06","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2006-1333","title":"Quality-assurance plan for the analysis of fluvial sediment by the U.S. Geological Survey New Mexico Water Science Center Sediment Laboratory","docAbstract":"<p>This report describes laboratory procedures used by the U.S. Geological Survey New Mexico Water Science Center Sediment Laboratory for the processing and analysis of fluvial-sediment samples for concentration of sand and finer material. The report details the processing of a sediment sample through the laboratory from receiving the sediment sample, through the analytical process, to compiling results of the requested analysis. Procedures for preserving sample integrity, calibrating and maintaining of laboratory and field instruments and equipment used to analyze samples, internal quality assurance and quality control, and validity of the sediment-analysis results also are described. The report includes a list of references cited and a glossary of sediment and quality-assurance terms.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20061333","usgsCitation":"Stiles, J.A., 2006, Quality-assurance plan for the analysis of fluvial sediment by the U.S. Geological Survey New Mexico Water Science Center Sediment Laboratory: U.S. Geological Survey Open-File Report 2006-1333, v, 13 p., https://doi.org/10.3133/ofr20061333.","productDescription":"v, 13 p.","costCenters":[{"id":472,"text":"New Mexico Water Science Center","active":true,"usgs":true}],"links":[{"id":398142,"rank":2,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2006/1333/report-thumb.jpg"},{"id":398141,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2006/1333/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Stiles, Jessica A. jstiles@usgs.gov","contributorId":289724,"corporation":false,"usgs":true,"family":"Stiles","given":"Jessica","email":"jstiles@usgs.gov","middleInitial":"A.","affiliations":[{"id":472,"text":"New Mexico Water Science Center","active":true,"usgs":true}],"preferred":true,"id":839683,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70129678,"text":"70129678 - 2006 - Sri Lanka field survey after the December 2004 Indian Ocean tsunami","interactions":[],"lastModifiedDate":"2014-10-24T15:27:23","indexId":"70129678","displayToPublicDate":"2006-01-01T15:23:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1436,"text":"Earthquake Spectra","active":true,"publicationSubtype":{"id":10}},"title":"Sri Lanka field survey after the December 2004 Indian Ocean tsunami","docAbstract":"An International Tsunami Survey Team (ITST) consisting of scientists from the United States, New Zealand, and Sri Lanka evaluated the impacts of the 26 December 2004 transoceanic tsunami in Sri Lanka two weeks after the event. Tsunami runup height, inundation distance, morphological changes, and sedimentary characteristics of deposits were recorded and analyzed along the southwest and east coasts of the country. Preliminary results show how local topography and bathymetry controlled the limits of inundation and associated damage to the infrastructure. The largest wave height of 8.71 m was recorded at Nonagama, while the greatest inundation distance of 390 m and runup height of 12.50 m was at Yala. At some sites, human alterations to the landscape increased the damage caused by the tsunami; this was particularly evident in areas of coral poaching and of sand dune removal.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Earthquake Spectra","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Earthquake Engineering Research Institute","doi":"10.1193/1.2205897","usgsCitation":"Goff, J., Liu, P.L., Higman, B., Morton, R., Jaffe, B.E., Fernando, H., Lynett, P., Fritz, H., Synolakis, C., and Fernando, S., 2006, Sri Lanka field survey after the December 2004 Indian Ocean tsunami: Earthquake Spectra, v. 22, no. S3, p. 155-172, https://doi.org/10.1193/1.2205897.","productDescription":"18 p.","startPage":"155","endPage":"172","numberOfPages":"18","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"links":[{"id":295749,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":295748,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1193/1.2205897"}],"country":"Sri Lanka","volume":"22","issue":"S3","noUsgsAuthors":false,"publicationDate":"2006-06-01","publicationStatus":"PW","scienceBaseUri":"544b6a30e4b03653c63fb1e7","contributors":{"authors":[{"text":"Goff, James","contributorId":87476,"corporation":false,"usgs":true,"family":"Goff","given":"James","affiliations":[],"preferred":false,"id":503960,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Liu, Philip L-F.","contributorId":16338,"corporation":false,"usgs":true,"family":"Liu","given":"Philip","email":"","middleInitial":"L-F.","affiliations":[],"preferred":false,"id":503953,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Higman, Bretwood","contributorId":18696,"corporation":false,"usgs":true,"family":"Higman","given":"Bretwood","email":"","affiliations":[],"preferred":false,"id":503954,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Morton, Robert","contributorId":85108,"corporation":false,"usgs":true,"family":"Morton","given":"Robert","affiliations":[],"preferred":false,"id":503959,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Jaffe, Bruce E. 0000-0002-8816-5920 bjaffe@usgs.gov","orcid":"https://orcid.org/0000-0002-8816-5920","contributorId":2049,"corporation":false,"usgs":true,"family":"Jaffe","given":"Bruce","email":"bjaffe@usgs.gov","middleInitial":"E.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true},{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"preferred":true,"id":503952,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Fernando, Haindra","contributorId":81431,"corporation":false,"usgs":true,"family":"Fernando","given":"Haindra","email":"","affiliations":[],"preferred":false,"id":503958,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Lynett, Patrick","contributorId":24298,"corporation":false,"usgs":true,"family":"Lynett","given":"Patrick","affiliations":[],"preferred":false,"id":503956,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Fritz, Hermann","contributorId":106040,"corporation":false,"usgs":true,"family":"Fritz","given":"Hermann","affiliations":[],"preferred":false,"id":503961,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Synolakis, Costas","contributorId":46026,"corporation":false,"usgs":true,"family":"Synolakis","given":"Costas","affiliations":[],"preferred":false,"id":503957,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Fernando, Starin","contributorId":19892,"corporation":false,"usgs":true,"family":"Fernando","given":"Starin","email":"","affiliations":[],"preferred":false,"id":503955,"contributorType":{"id":1,"text":"Authors"},"rank":10}]}}
,{"id":70129584,"text":"70129584 - 2006 - Sedimentary processes in modern and ancient oceanic arc settings: evidence from the Jurassic Talkeetna Formation of Alaska and the Mariana and Tonga Arcs, western Pacific","interactions":[],"lastModifiedDate":"2014-10-23T15:17:22","indexId":"70129584","displayToPublicDate":"2006-01-01T15:10:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2451,"text":"Journal of Sedimentary Research","onlineIssn":"1938-3681","printIssn":"1527-1404","active":true,"publicationSubtype":{"id":10}},"title":"Sedimentary processes in modern and ancient oceanic arc settings: evidence from the Jurassic Talkeetna Formation of Alaska and the Mariana and Tonga Arcs, western Pacific","docAbstract":"Sediment deposited around oceanic volcanic ares potentially provides the most complete record of the tectonic and geochemical evolution of active margins. The use of such tectonic and geochemical records requires an accurate understanding of sedimentary dynamics in an arc setting: processes of deposition and reworking that affect the degree to which sediments represent the contemporaneous volcanism at the time of their deposition. We review evidence from the modern Mariana and Tonga arcs and the ancient arc crustal section in the Lower Jurassic Talkeetna Formation of south-central Alaska, and introduce new data from the Mariana Arc, to produce a conceptual model of volcaniclastic sedimentation processes in oceanic arc settings. All three arcs are interpreted to have formed in tectonically erosive margin settings, resulting in long-term extension and subsidence. Debris aprons composed of turbidites and debris flow deposits occur in the immediate vicinity of arc volcanoes, forming relatively continuous mass-wasted volcaniclastic records in abundant accommodation space. There is little erosion or reworking of old volcanic materials near the arc volcanic front. Tectonically generated topography in the forearc effectively blocks sediment flow from the volcanic front to the trench; although some canyons deliver sediment to the trench slope, most volcaniclastic sedimentation is limited to the area immediately around volcanic centers. Arc sedimentary sections in erosive plate margins can provide comprehensive records of volcanism and tectonism spanning < 10 My. The chemical evolution of a limited section of an oceanic arc may be best reconstructed from sediments of the debris aprons for intervals up to ~ 20 My but no longer, because subduction erosion causes migration of the forearc basin crust and its sedimentary cover toward the trench, where there is little volcaniclastic sedimentation and where older sediments are dissected and reworked along the trench slope.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Sedimentary Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Society for Sedimentary Geology","doi":"10.2110/jsr.2006.044","usgsCitation":"Draut, A.E., and Clift, P., 2006, Sedimentary processes in modern and ancient oceanic arc settings: evidence from the Jurassic Talkeetna Formation of Alaska and the Mariana and Tonga Arcs, western Pacific: Journal of Sedimentary Research, v. 76, no. 3, p. 493-514, https://doi.org/10.2110/jsr.2006.044.","productDescription":"22 p.","startPage":"493","endPage":"514","numberOfPages":"22","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"links":[{"id":295695,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":295694,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.2110/jsr.2006.044"}],"country":"United States","state":"Alaska","otherGeospatial":"Mariana Arc, Talkeetna formation, Tonga Arc","volume":"76","issue":"3","noUsgsAuthors":false,"publicationDate":"2006-04-12","publicationStatus":"PW","scienceBaseUri":"544a190fe4b04d2014abfb74","contributors":{"authors":[{"text":"Draut, Amy E.","contributorId":108424,"corporation":false,"usgs":true,"family":"Draut","given":"Amy","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":503876,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Clift, Peter D.","contributorId":103203,"corporation":false,"usgs":true,"family":"Clift","given":"Peter D.","affiliations":[],"preferred":false,"id":503875,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70129668,"text":"70129668 - 2006 - Tsunami: wave of change","interactions":[],"lastModifiedDate":"2014-10-24T15:03:29","indexId":"70129668","displayToPublicDate":"2006-01-01T15:01:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3355,"text":"Scientific American","active":true,"publicationSubtype":{"id":10}},"title":"Tsunami: wave of change","docAbstract":"No abstract available.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Scientific American","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Nature Publishing Group","doi":"10.1038/scientificamerican0106-56","usgsCitation":"Geist, E.L., Titov, V., and Synolakis, C.E., 2006, Tsunami: wave of change: Scientific American, v. 294, p. 56-63, https://doi.org/10.1038/scientificamerican0106-56.","productDescription":"8 p.","startPage":"56","endPage":"63","numberOfPages":"8","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"links":[{"id":295742,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":295741,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1038/scientificamerican0106-56"}],"volume":"294","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"544b6a32e4b03653c63fb1ed","contributors":{"authors":[{"text":"Geist, Eric L. 0000-0003-0611-1150","orcid":"https://orcid.org/0000-0003-0611-1150","contributorId":15543,"corporation":false,"usgs":true,"family":"Geist","given":"Eric","email":"","middleInitial":"L.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":503946,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Titov, Vasily V.","contributorId":32463,"corporation":false,"usgs":true,"family":"Titov","given":"Vasily V.","affiliations":[],"preferred":false,"id":503947,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Synolakis, Costas E.","contributorId":70315,"corporation":false,"usgs":true,"family":"Synolakis","given":"Costas","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":503948,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
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