{"pageNumber":"2","pageRowStart":"25","pageSize":"25","recordCount":43,"records":[{"id":1004000,"text":"1004000 - 2006 - Avian influenza virus and free-ranging wild birds","interactions":[],"lastModifiedDate":"2019-11-13T14:28:58","indexId":"1004000","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2528,"text":"Journal of the American Veterinary Medical Association","active":true,"publicationSubtype":{"id":10}},"title":"Avian influenza virus and free-ranging wild birds","docAbstract":"<p>Recent media and news reports and other information implicate wild birds in the spread of highly pathogenic avian influenza in Asia and Eastern Europe. Although there is little information concerning highly pathogenic avian influenza viruses in wild birds, scientists have amassed a large amount of data on low-pathogenicity avian influenza viruses during decades of research with wild birds. This knowledge can provide sound guidance to veterinarians, public health professionals, the general public, government agencies, and other entities with concerns about avian influenza.</p>","language":"English","publisher":"American Veterinary Medical Association","doi":"10.2460/javma.228.12.1877","usgsCitation":"Dierauf, L.A., Karesh, W., Ip, S., Gilardi, K., and Fischer, J.R., 2006, Avian influenza virus and free-ranging wild birds: Journal of the American Veterinary Medical Association, v. 228, no. 12, p. 1877-1882, https://doi.org/10.2460/javma.228.12.1877.","productDescription":"6 p.","startPage":"1877","endPage":"1882","numberOfPages":"6","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"links":[{"id":477439,"rank":1,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.2460/javma.228.12.1877","text":"Publisher Index 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Leslie A.","contributorId":28947,"corporation":false,"usgs":true,"family":"Dierauf","given":"Leslie","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":314889,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Karesh, W.B.","contributorId":98676,"corporation":false,"usgs":true,"family":"Karesh","given":"W.B.","email":"","affiliations":[],"preferred":false,"id":314891,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ip, S. 0000-0003-4844-7533 hip@usgs.gov","orcid":"https://orcid.org/0000-0003-4844-7533","contributorId":727,"corporation":false,"usgs":true,"family":"Ip","given":"S.","email":"hip@usgs.gov","affiliations":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"preferred":true,"id":314888,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Gilardi, K.V.","contributorId":56620,"corporation":false,"usgs":true,"family":"Gilardi","given":"K.V.","email":"","affiliations":[],"preferred":false,"id":314890,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Fischer, John R.","contributorId":100326,"corporation":false,"usgs":true,"family":"Fischer","given":"John","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":314892,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70030360,"text":"70030360 - 2006 - Rare earths, the lanthanides, yttrium and scandium","interactions":[],"lastModifiedDate":"2012-03-12T17:21:02","indexId":"70030360","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2755,"text":"Mining Engineering","active":true,"publicationSubtype":{"id":10}},"title":"Rare earths, the lanthanides, yttrium and scandium","docAbstract":"In 2005, rare earths were not mined in the United States. The major supplier, Molycorp, continued to maintain a large stockpile of rare-earth concentrates and compounds. Consumption decreased of refined rare-earth products. The United States remained a major importer and exporter of rare earths in 2005. During the same period, yttrium was not mined or refined in the US. Hence, supply of yttrium compounds for refined yttrium products came from China, France and Japan. Scandium was not also mined. World production was primarily in China, Russia and Ukraine. Demand for rare earths in 2006 is expected to be closely tied to economic conditions in the US.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Mining Engineering","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"00265187","usgsCitation":"Hedrick, J., 2006, Rare earths, the lanthanides, yttrium and scandium: Mining Engineering, v. 58, no. 6, p. 51-53.","startPage":"51","endPage":"53","numberOfPages":"3","costCenters":[],"links":[{"id":239444,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"58","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a9523e4b0c8380cd81822","contributors":{"authors":[{"text":"Hedrick, J.B.","contributorId":96717,"corporation":false,"usgs":true,"family":"Hedrick","given":"J.B.","email":"","affiliations":[],"preferred":false,"id":426848,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":57808,"text":"ofr20041290 - 2004 - Mineral commodity profiles: nitrogen","interactions":[],"lastModifiedDate":"2012-02-02T00:12:21","indexId":"ofr20041290","displayToPublicDate":"2004-08-01T00:00:00","publicationYear":"2004","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":"2004-1290","title":"Mineral commodity profiles: nitrogen","docAbstract":"Overview -- Nitrogen (N) is an essential element of life and a part of all animal and plant proteins. As a part of the DNA and RNA molecules, nitrogen is an essential constituent of each individual's genetic blueprint. As an essential element in the chlorophyll molecule, nitrogen is vital to a plant's ability to photosynthesize. Some crop plants, such as alfalfa, peas, peanuts, and soybeans, can convert atmospheric nitrogen into a usable form by a process referred to as 'fixation.' Most of the nitrogen that is available for crop production, however, comes from decomposing animal and plant waste or from commercially produced fertilizers. \r\n\r\nCommercial fertilizers contain nitrogen in the form of ammonium and/or nitrate or in a form that is quickly converted to the ammonium or nitrate form once the fertilizer is applied to the soil. Ammonia is generally the source of nitrogen in fertilizers. Anhydrous ammonia is commercially produced by reacting nitrogen with hydrogen under high temperatures and pressures. The source of nitrogen is the atmosphere, which is almost 80 percent nitrogen. Hydrogen is derived from a variety of raw materials, which include water, and crude oil, coal, and natural gas hydrocarbons. Nitrogen-based fertilizers are produced from ammonia feedstocks through a variety of chemical processes. Small quantities of nitrates are produced from mineral resources principally in Chile. \r\n\r\nIn 2002, anhydrous ammonia and other nitrogen materials were produced in more than 70 countries. Global ammonia production was 108 million metric tons (Mt) of contained nitrogen. With 28 percent of this total, China was the largest producer of ammonia. Asia contributed 46 percent of total world ammonia production, and countries of the former U.S.S.R. represented 13 percent. North America also produced 13 percent of the total; Western Europe, 9 percent; the Middle East, 7 percent; Central America and South America, 5 percent; Eastern Europe, 3 percent; and Africa and Oceania contributed the remaining 4 percent (International Fertilizer Industry Association, 2003b, p. 1-4). \r\n\r\nIn 2002, world ammonia exports were 13.1 Mt of contained nitrogen. Trinidad and Tobago (22 percent), Russia (18 percent), Ukraine (10 percent), and Indonesia (7 percent) accounted for 57 percent of the world total. The largest importing regions were North America with 36 percent of the total followed by Western Europe with 23 percent and Asia with 22 percent (International Fertilizer Industry Association, 2003b, p. 5L-11). \r\n\r\nIn 2002, world urea production was 51.4 Mt of contained nitrogen, and exports were 12.0 Mt of contained nitrogen. China and India, which were the two largest producing countries, accounted for 48 percent of world production. The United States and Canada produced about 10 percent of the total. Russia and Ukraine together accounted for 28 percent of total urea exports; Central America and South America, 27 percent; and Asia, North America, and Western Europe, 10 percent each. North America accounted for 36 percent of the total urea imports; Western Europe, 23 percent; and Asia, 22 percent (International Fertilizer Industry Association, 2003f, p. 1-15). \r\n\r\nAmmonia production capacity in North America and Western Europe is projected to decline through 2004, and capacity in other world regions is projected to increase. Fluctuating natural gas prices are mainly responsible for the capacity decline in North America. Ammonia production capacity is continuing to shift to world regions that have abundant sources of natural gas, and away from those where costs (raw material, labor, environmental compliance) are higher.","language":"ENGLISH","doi":"10.3133/ofr20041290","usgsCitation":"Kramer, D.A., 2004, Mineral commodity profiles: nitrogen (Version 1.0, Online Only): U.S. Geological Survey Open-File Report 2004-1290, 49 p., https://doi.org/10.3133/ofr20041290.","productDescription":"49 p.","onlineOnly":"Y","costCenters":[],"links":[{"id":184933,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":5768,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2004/1290/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0, Online Only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db6358a6","contributors":{"authors":[{"text":"Kramer, Deborah A.","contributorId":69966,"corporation":false,"usgs":true,"family":"Kramer","given":"Deborah","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":257852,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":5211202,"text":"5211202 - 2003 - The Chernobyl Nuclear Power Plant accident:  ecotoxicological update","interactions":[],"lastModifiedDate":"2012-02-02T00:15:23","indexId":"5211202","displayToPublicDate":"2009-06-09T09:23:19","publicationYear":"2003","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"The Chernobyl Nuclear Power Plant accident:  ecotoxicological update","docAbstract":"The accident at the Chernobyl, Ukraine, nuclear reactor on 26 April 1986 released large amounts of radiocesium and other radionuclides into the environment, contaminating much of the northern hemisphere, especially Europe.  In the vicinity of Chernobyl, at least 30 people died, more than 115,000 others were evacuated, and consumption of milk and other foods was banned because of radiocontamination.  At least 14,000 human cancer deaths are expected in Russia, Belarus, and the Ukraine as a direct result of Chernobyl.  The most sensitive local ecosystems, as judged by survival, were the soil fauna, pine forest communities, and certain populations of rodents.  Elsewhere, fallout from Chernobyl significantly contaminated freshwater and terrestrial ecosystems and flesh and milk of domestic livestock; in many cases, radionuclide concentrations in biological samples exceeded current radiation protection guidelines.  Reindeer (Rangifer tarandus) in Scandinavia were among the most seriously afflicted by Chernobyl fallout, probably because their main food during winter (lichens) is an efficient absorber of airborne particles containing radiocesium. Some reindeer calves contaminated with 137Cs from Chernobyl showed 137Cs-dependent decreases in survival and increases in frequency of chromosomal aberrations.  Although radiation levels in the biosphere are declining with time, latent effects of initial exposure--including an increased frequency of thyroid and other cancers--are now measurable.  The full effect of the Chernobyl nuclear reactor accident on natural resources will probably not be known for at least several decades because of gaps in data on long-term genetic and reproductive effects and on radiocesium cycling and toxicokinetics. ","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Handbook of Ecotoxicology","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","publisher":"Lewis Publishers","publisherLocation":"Boca Raton, FL","collaboration":"OCLC:  49952447 ; ISBN: 1-56670-546-0.","usgsCitation":"Eisler, R., 2003, The Chernobyl Nuclear Power Plant accident:  ecotoxicological update, chap. <i>of</i> Handbook of Ecotoxicology, p. 703-736.","productDescription":"1,290","startPage":"703","endPage":"736","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":203109,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"edition":"2nd","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad2e4b07f02db68196b","contributors":{"editors":[{"text":"Hoffman, David J.","contributorId":86075,"corporation":false,"usgs":true,"family":"Hoffman","given":"David","email":"","middleInitial":"J.","affiliations":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"preferred":false,"id":507756,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Rattner, Barnett A. 0000-0003-3676-2843 brattner@usgs.gov","orcid":"https://orcid.org/0000-0003-3676-2843","contributorId":4142,"corporation":false,"usgs":true,"family":"Rattner","given":"Barnett","email":"brattner@usgs.gov","middleInitial":"A.","affiliations":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"preferred":true,"id":507755,"contributorType":{"id":2,"text":"Editors"},"rank":2},{"text":"Burton, G. Allen Jr.","contributorId":111752,"corporation":false,"usgs":true,"family":"Burton","given":"G.","suffix":"Jr.","email":"","middleInitial":"Allen","affiliations":[],"preferred":false,"id":507757,"contributorType":{"id":2,"text":"Editors"},"rank":3},{"text":"Cairns, John Jr.","contributorId":111897,"corporation":false,"usgs":true,"family":"Cairns","given":"John","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":507758,"contributorType":{"id":2,"text":"Editors"},"rank":4}],"authors":[{"text":"Eisler, R.","contributorId":51869,"corporation":false,"usgs":true,"family":"Eisler","given":"R.","affiliations":[],"preferred":false,"id":330383,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":5224075,"text":"5224075 - 2001 - Satellite tracking of two lesser spotted eagles, Aquila pomarina, migrating from Namibia","interactions":[],"lastModifiedDate":"2022-12-23T15:20:46.521965","indexId":"5224075","displayToPublicDate":"2010-06-16T12:18:50","publicationYear":"2001","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2970,"text":"Ostrich","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Satellite tracking of two lesser spotted eagles, <i>Aquila pomarina</i>, migrating from Namibia","title":"Satellite tracking of two lesser spotted eagles, Aquila pomarina, migrating from Namibia","docAbstract":"<p><span>One immature and one subadult Lesser Spotted Eagle,&nbsp;</span><i>Aquila pomarina</i><span>, were followed by satellite telemetry from their non-breeding areas in Namibia. Both birds were fitted with transmitters (PTTs) in February 1994 and tracked, the immature for six months and three weeks, the subadult for eight months and two weeks, over distances of 10 084 and 16 773 km, respectively. During their time in Namibia both birds' movements were in response to good local rainfall. The immature eagle left Namibia at the end of February, the subadult at the end of March. They flew to their respective summer quarters in Hungary and the Ukraine, arriving there 2.5 and 1.5 months later than the breeding adults. The immature eagle took over two months longer on the homeward journey than a breeding male followed by telemetry in a previous study. On returning, the immature eagle followed the narrow flightpath through Africa used by other Lesser Spotted Eagles on their outward migration. It reached this corridor, which run roughly between longitudes 31° and 36° East from Suez to Lake Tanganyika, veering from the shortest route in a direction east-northeast through Angola and Zambia to the southern end of Lake Tanganyika. The route taken by the subadult bird on its return migration differed markedly from that of all Lesser Spotted Eagles tracked to date, running further west through the Democratic Republic of Congo where, level with the equator, it flew over the eastern rainforest of that country. The outward migration, however, followed the same corridor and coincided in time with the migration of adults.</span></p>","language":"English","publisher":"Taylor & Francis","doi":"10.2989/00306520109485281","usgsCitation":"Meyburg, B., Ellis, D.H., Meyburg, C., Mendelsohn, J., and Scheller, W., 2001, Satellite tracking of two lesser spotted eagles, Aquila pomarina, migrating from Namibia: Ostrich, v. 72, no. 1 & 2, p. 35-40, https://doi.org/10.2989/00306520109485281.","productDescription":"6 p.","startPage":"35","endPage":"40","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":202215,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Angola, Democratic Republic of the Congo, Hungary, Namibia, Ukraine, Zambia","otherGeospatial":"Lake Tanganyika","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n  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H.","contributorId":79830,"corporation":false,"usgs":true,"family":"Ellis","given":"D.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":340487,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Meyburg, C.","contributorId":17726,"corporation":false,"usgs":true,"family":"Meyburg","given":"C.","email":"","affiliations":[],"preferred":false,"id":340484,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Mendelsohn, J.","contributorId":82824,"corporation":false,"usgs":true,"family":"Mendelsohn","given":"J.","email":"","affiliations":[],"preferred":false,"id":340488,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Scheller, W.","contributorId":49493,"corporation":false,"usgs":true,"family":"Scheller","given":"W.","email":"","affiliations":[],"preferred":false,"id":340485,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":33066,"text":"b2201E - 2001 - Petroleum geology and resources of the Dnieper-Donets Basin, Ukraine and Russia","interactions":[],"lastModifiedDate":"2024-10-11T10:55:22.655334","indexId":"b2201E","displayToPublicDate":"2001-11-01T00:00:00","publicationYear":"2001","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2201","chapter":"E","title":"Petroleum geology and resources of the Dnieper-Donets Basin, Ukraine and Russia","docAbstract":"The Dnieper-Donets basin is almost entirely in Ukraine, and it is the principal producer of hydrocarbons in that country. A small southeastern part of the basin is in Russia. The basin is bounded by the Voronezh high of the Russian craton to the northeast and by the Ukrainian shield to the southwest. The basin is principally a Late Devonian rift that is overlain by a Carboniferous to Early Permian postrift sag. The Devonian rift structure extends northwestward into the Pripyat basin of Belarus; the two basins are separated by the Bragin-Loev uplift, which is a Devonian volcanic center. Southeastward, the Dnieper-Donets basin has a gradational boundary with the Donbas foldbelt, which is a structurally inverted and deformed part of the basin.\r\nThe sedimentary succession of the basin consists of four tectono-stratigraphic sequences. The prerift platform sequence includes Middle Devonian to lower Frasnian, mainly clastic, rocks that were deposited in an extensive intracratonic basin.\r\n1\r\nThe Upper Devonian synrift sequence probably is as thick as 4?5 kilometers. It is composed of marine carbonate, clastic, and volcanic rocks and two salt formations, of Frasnian and Famennian age, that are deformed into salt domes and plugs. The postrift sag sequence consists of Carboniferous and Lower Permian clastic marine and alluvial deltaic rocks that are as thick as 11 kilometers in the southeastern part of the basin. The Lower Permian interval includes a salt formation that is an important regional seal for oil and gas fields. The basin was affected by strong compression in Artinskian (Early Permian) time, when southeastern basin areas were uplifted and deeply eroded and the Donbas foldbelt was formed. The postrift platform sequence includes Triassic through Tertiary rocks that were deposited in a shallow platform depression that extended far beyond the Dnieper-Donets basin boundaries.\r\nA single total petroleum system encompassing the entire sedimentary succession is identified in the Dnieper-Donets basin. Discovered reserves of the system are 1.6 billion barrels of oil and 59 trillion cubic feet of gas. More than one-half of the reserves are in Lower Permian rocks below the salt seal. Most of remaining reserves are in upper Visean-Serpukhovian (Lower Carboniferous) strata. The majority of discovered fields are in salt-cored anticlines or in drapes over Devonian horst blocks; little exploration has been conducted for stratigraphic traps. Synrift Upper Devonian carbonate reservoirs are almost unexplored.\r\nTwo identified source-rock intervals are the black anoxic shales and carbonates in the lower Visean and Devonian sections.\r\nHowever, additional source rocks possibly are present in the deep central area of the basin. The role of Carboniferous coals as a source rock for gas is uncertain; no coal-related gas has been identified by the limited geochemical studies. The source rocks are in the gas-generation window over most of the basin area; consequently gas dominates over oil in the reserves.\r\nThree assessment units were identified in the Dnieper-Donets Paleozoic total petroleum system. The assessment unit that contains all discovered reserves embraces postrift Carboniferous\r\nand younger rocks. This unit also contains the largest portion of undiscovered resources, especially gas. Stratigraphic and combination structural and stratigraphic traps probably will be the prime targets for future exploration. The second assessment\r\nunit includes poorly known synrift Devonian rocks. Carbonate reef reservoirs along the basin margins probably will contain most of the undiscovered resources. The third assessment\r\nunit is an unconventional, continuous, basin-centered gas accumulation in Carboniferous low-permeability clastic rocks. The entire extent of this accumulation is unknown, but it occupies much of the basin area. Resources of this assessment unit were not estimated quantitatively.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b2201E","usgsCitation":"Ulmishek, G.F., 2001, Petroleum geology and resources of the Dnieper-Donets Basin, Ukraine and Russia (Version 1.0): U.S. Geological Survey Bulletin 2201, 14 p., https://doi.org/10.3133/b2201E.","productDescription":"14 p.","costCenters":[],"links":[{"id":462805,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/2201/E/b2201-e.pdf","text":"Report","size":"1.39 MB","linkFileType":{"id":1,"text":"pdf"}},{"id":161285,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":3239,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/bul/2201/E/index.html","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","contact":"<p><a href=\"https://pubs.usgs.gov/contact\" data-mce-href=\"../contact\">Contact Pubs Warehouse</a></p>","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db687ead","contributors":{"authors":[{"text":"Ulmishek, Gregory F.","contributorId":48971,"corporation":false,"usgs":true,"family":"Ulmishek","given":"Gregory","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":209809,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70023364,"text":"70023364 - 2001 - Conserving large-river fishes: Is the highway analogy an appropriate paradigm?","interactions":[],"lastModifiedDate":"2022-12-21T17:06:04.153572","indexId":"70023364","displayToPublicDate":"2001-01-01T00:00:00","publicationYear":"2001","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2564,"text":"Journal of the North American Benthological Society","onlineIssn":"1937-237X","printIssn":"0887-3593","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Conserving large-river fishes: Is the <i>highway analogy</i> an appropriate paradigm?","title":"Conserving large-river fishes: Is the highway analogy an appropriate paradigm?","docAbstract":"<p>A tenet of the flood pulse concept, the<span>&nbsp;</span><i>highway analogy,</i><span>&nbsp;</span>states that the main channel of large floodplain rivers is used by fishes mainly as a route for gaining access to floodplain habitats. We examined this proposition by analyzing habitat use for freshwater fishes in 4 large rivers in the United States (Colorado, Columbia, Mississippi, Missouri) and 4 in Europe (Danube, Rhine, Rhône, Volga). Fish species from floodplain segments of each river were classified as fluvial specialist, fluvial dependent, and macrohabitat generalist based on literature and expert opinion. We also summarized the proportion of imperiled and introduced fishes present in each of these categories.</p><p>The high proportion (mean ± 1 SD = 29 ± 17.5%) of fluvial specialist fishes inhabiting north-temperate large rivers was inconsistent with the highway analogy. Most members of the families Petromyzontidae, Acipenseridae, Hiodontidae, Osmeridae, Salmonidae, and Gobiidae require flowing water during some life stage. Between 29 and 100% of the native fish assemblage was of conservation concern, and from 50 to 85% of these fishes required riverine habitats to complete their life cycles. Macrohabitat generalists are adapted to capitalize on floodplain habitats and composed from 44 to 96% of introduced fishes in the rivers studied.</p><p>Habitat diversity inherent in main-channel complexes of unaltered large rivers and reestablished in regulated large rivers is essential to meet life-history needs of native fluvial fishes while discouraging expansion of introduced species. Restoration of north-temperate large rivers and their native fish fauna should incorporate the dynamic interplay among main channel, floodplain, and tributary habitats and processes.</p>","language":"English","publisher":"University of Chicago Press","doi":"10.2307/1468321","issn":"08873593","usgsCitation":"Galat, D., and Zweimuller, I., 2001, Conserving large-river fishes: Is the highway analogy an appropriate paradigm?: Journal of the North American Benthological Society, v. 20, no. 2, p. 266-279, https://doi.org/10.2307/1468321.","productDescription":"14 p.","startPage":"266","endPage":"279","costCenters":[],"links":[{"id":232245,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Austria, Bulgaria, Croatia, France, Germany, Hungary, Moldova, Netherlands, Romania, Russia, Serbia, Slovakia, Switzerland, Ukraine, United States","otherGeospatial":"Colorado River, Columbia River, Danube River, Mississippi River, Missouri River, Rhine River, Rhône River, Volga 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,{"id":70022844,"text":"70022844 - 2000 - Silurian K-bentonites of the Dnestr Basin, Podolia, Ukraine","interactions":[],"lastModifiedDate":"2022-08-24T17:59:13.162682","indexId":"70022844","displayToPublicDate":"2000-01-01T00:00:00","publicationYear":"2000","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2545,"text":"Journal of the Geological Society","active":true,"publicationSubtype":{"id":10}},"title":"Silurian K-bentonites of the Dnestr Basin, Podolia, Ukraine","docAbstract":"The Dnestr Basin of Podolia, Ukraine, is an epicratonic basin consisting of neritic carbonate and calcareous mudstone facies including a nearly complete Silurian sequence ranging from late Llandovery to late Pridoli in age. The Silurian section has served as a standard for regional and interregional studies as a consequence of its well-documented macro- and microfaunal assemblages. Approximately 24 mid- to Late Silurian K-bentonites are present in this succession, and their lateral persistence has aided in establishing regional correlations. The K-bentonites range from 1 to 40 cm in thickness and occur in the Bagovitsa (late Wenlock), Malinovtsy (Ludlow) and Skala (Pridoli) Formations. Discrimination diagrams based on immobile trace elements together with rare earth element data suggest the K-bentonites had a volcanic origin in a collision margin setting related to subduction. Thickness and stratigraphic distribution considerations are consistent with a source area in the Rheic Ocean.","language":"English","publisher":"The Geological Society","doi":"10.1144/jgs.157.2.493","issn":"00167649","usgsCitation":"Huff, W., Bergstrom, S., and Kolata, D.R., 2000, Silurian K-bentonites of the Dnestr Basin, Podolia, Ukraine: Journal of the Geological Society, v. 157, no. 2, p. 493-504, https://doi.org/10.1144/jgs.157.2.493.","productDescription":"12 p.","startPage":"493","endPage":"504","costCenters":[],"links":[{"id":233643,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Unkraine","otherGeospatial":"Dnestr Basin, Podolia","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              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W.D.","contributorId":48327,"corporation":false,"usgs":true,"family":"Huff","given":"W.D.","email":"","affiliations":[],"preferred":false,"id":395114,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bergstrom, Stig M.","contributorId":80832,"corporation":false,"usgs":true,"family":"Bergstrom","given":"Stig M.","affiliations":[],"preferred":false,"id":395116,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kolata, Dennis R.","contributorId":79495,"corporation":false,"usgs":false,"family":"Kolata","given":"Dennis","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":395115,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":1000700,"text":"1000700 - 1999 - Changes in the dreissenid community in the lower Great Lakes with emphasis on southern Lake Ontario","interactions":[],"lastModifiedDate":"2016-04-04T11:51:15","indexId":"1000700","displayToPublicDate":"1999-01-01T00:00:00","publicationYear":"1999","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2330,"text":"Journal of Great Lakes Research","active":true,"publicationSubtype":{"id":10}},"title":"Changes in the dreissenid community in the lower Great Lakes with emphasis on southern Lake Ontario","docAbstract":"<p>A field study was conducted in the lower Great Lakes to assess changes in spatial distribution and population structure of dreissenid mussel populations. More specifically, the westward range expansion of quagga mussel into western Lake Erie and toward Lake Huron was investigated and the shell size, density, and biomass of zebra and quagga mussel with depth in southern Lake Ontario in 1992 and 1995 were compared. In Lake Erie, quagga mussel dominated the dreissenid community in the eastern basin and zebra mussel dominated in the western basin. In southern Lake Ontario, an east to west gradient was observed with the quagga mussel dominant at western sites and zebra mussel dominant at eastern locations. Mean shell size of quagga mussel was generally larger than that of zebra mussel except in western Lake Erie and one site in eastern Lake Erie. Although mean shell size and our index of numbers and biomass of both dreissenid species increased sharply in southern Lake Ontario between 1992 and 1995, the increase in density and biomass was much greater for quagga mussels over the 3-year period. In 1995, zebra mussels were most abundant at 15 to 25 m whereas the highest numbers and biomass of quagga mussel were at 35 to 45 m. The quagga mussel is now the most abundant dreissenid in areas of southern Lake Ontario where the zebra mussel was once the most abundant dreissenid; this trend parallels that observed for dreissenid populations in the Dneiper River basin in the Ukraine.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/S0380-1330(99)70727-6","usgsCitation":"Mills, E.L., Chrisman, J.R., Baldwin, B., Owens, R.W., O’Gorman, R., Howell, T., Roseman, E., and Raths, M.K., 1999, Changes in the dreissenid community in the lower Great Lakes with emphasis on southern Lake Ontario: Journal of Great Lakes Research, v. 25, no. 1, p. 187-197, https://doi.org/10.1016/S0380-1330(99)70727-6.","productDescription":"11 p.","startPage":"187","endPage":"197","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":479600,"rank":1,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1016/s0380-1330(99)70727-6","text":"Publisher Index Page"},{"id":131766,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"25","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e5e4b07f02db5e69f7","contributors":{"authors":[{"text":"Mills, Edward L.","contributorId":61387,"corporation":false,"usgs":true,"family":"Mills","given":"Edward","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":309152,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Chrisman, Jana R.","contributorId":106446,"corporation":false,"usgs":true,"family":"Chrisman","given":"Jana","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":309155,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Baldwin, Brad","contributorId":93438,"corporation":false,"usgs":true,"family":"Baldwin","given":"Brad","email":"","affiliations":[],"preferred":false,"id":309153,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Owens, Randall W.","contributorId":23871,"corporation":false,"usgs":true,"family":"Owens","given":"Randall","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":309149,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"O’Gorman, Robert rogorman@usgs.gov","contributorId":3451,"corporation":false,"usgs":true,"family":"O’Gorman","given":"Robert","email":"rogorman@usgs.gov","affiliations":[],"preferred":true,"id":309148,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Howell, Todd","contributorId":38941,"corporation":false,"usgs":true,"family":"Howell","given":"Todd","email":"","affiliations":[],"preferred":false,"id":309151,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Roseman, Edward F.","contributorId":100334,"corporation":false,"usgs":true,"family":"Roseman","given":"Edward F.","affiliations":[],"preferred":false,"id":309154,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Raths, Melinda K.","contributorId":27010,"corporation":false,"usgs":true,"family":"Raths","given":"Melinda","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":309150,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":70020511,"text":"70020511 - 1998 - Prospects for Ukrainian ferrous metals in the post-Soviet period","interactions":[],"lastModifiedDate":"2025-06-24T16:25:24.187577","indexId":"70020511","displayToPublicDate":"2013-05-15T00:00:00","publicationYear":"1998","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3104,"text":"Post-Soviet Geography and Economics","active":true,"publicationSubtype":{"id":10}},"title":"Prospects for Ukrainian ferrous metals in the post-Soviet period","docAbstract":"<p>Two specialists on the mineral industries of the countries of the former USSR survey current problems confronting producers of ferrous metals in Ukraine and future prospects for domestic production and exports. A series of observations documenting the importance of ferrous metals production to Ukraine's economy is followed by sections describing investment plans and needs in the sector, and the role played by Ukraine within the iron and steel industry of the Soviet Union. The focus then turns to assessment of the current regional and global competitive position of Ukrainian producers for each of the major commodities of the sector-iron ore, manganese ore, ferroalloys, steel, and the products of the machine manufacturing and metal working industries. In conclusion, the paper discusses a potential regional industrial integration strategy analogous to that employed in the United States' Great Lakes/Midwest region, which possesses similar types of iron ore deposits and similar transport cost advantages and metallurgical and manufacturing industries.&nbsp;</p>","language":"English","publisher":"Taylor & Francis","doi":"10.1080/10889388.1998.10641072","issn":"10889388","usgsCitation":"Levine, R., and Bond, A., 1998, Prospects for Ukrainian ferrous metals in the post-Soviet period: Post-Soviet Geography and Economics, v. 39, no. 3, p. 151-163, https://doi.org/10.1080/10889388.1998.10641072.","productDescription":"13 p.","startPage":"151","endPage":"163","costCenters":[],"links":[{"id":231143,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Ukraine","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              22.947185835779095,\n              52.28433970544285\n            ],\n            [\n              22.33286273632544,\n              48.13499466452933\n            ],\n            [\n              25.306559224408197,\n              47.56425984942703\n            ],\n            [\n              27.340675182332532,\n              48.256353638844445\n            ],\n            [\n              31.629326557588662,\n              44.54578471861984\n            ],\n            [\n              36.54224275554856,\n              44.107176698288754\n            ],\n            [\n              41.11848740679736,\n              47.730671853393744\n            ],\n            [\n              34.579070887980976,\n              52.392677768952865\n            ],\n            [\n              30.212972963336057,\n              51.88759477372889\n            ],\n            [\n              22.947185835779095,\n              52.28433970544285\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"39","issue":"3","noUsgsAuthors":false,"publicationDate":"2013-05-15","publicationStatus":"PW","scienceBaseUri":"505a8f55e4b0c8380cd7f6d6","contributors":{"authors":[{"text":"Levine, R.M.","contributorId":90050,"corporation":false,"usgs":true,"family":"Levine","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":386494,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bond, A.R.","contributorId":20910,"corporation":false,"usgs":true,"family":"Bond","given":"A.R.","email":"","affiliations":[],"preferred":false,"id":386493,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70020506,"text":"70020506 - 1998 - Basin-centered gas evaluated in Dnieper-Donets basin, Donbas foldbelt, Ukraine","interactions":[],"lastModifiedDate":"2018-02-19T17:17:21","indexId":"70020506","displayToPublicDate":"1998-01-01T00:00:00","publicationYear":"1998","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2941,"text":"Oil & Gas Journal","printIssn":"0030-1388","active":true,"publicationSubtype":{"id":10}},"title":"Basin-centered gas evaluated in Dnieper-Donets basin, Donbas foldbelt, Ukraine","docAbstract":"<p>An evaluation of thermal maturity, pore pressures, source rocks, reservoir quality, present-day temperatures, and fluid recovery data indicates the presence of a large basin-centered gas accumulation in the Dnieper-Donets basin (DDB) and Donbas foldbelt (DF) of eastern Ukraine (Fig. 1). </p>","language":"English","publisher":"PennWell Corporation","publisherLocation":"Tulsa, OK","usgsCitation":"Law, B.E., Ulmishek, G., Clayton, J., Kabyshev, B., Pashova, N., and Krivosheya, V., 1998, Basin-centered gas evaluated in Dnieper-Donets basin, Donbas foldbelt, Ukraine: Oil & Gas Journal, v. 96, no. 47, p. 74-78.","productDescription":"5 p.","startPage":"74","endPage":"78","costCenters":[],"links":[{"id":231063,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":351788,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://www.ogj.com/articles/print/volume-96/issue-47/in-this-issue/general-interest/basin-centered-gas-evaluated-in-dnieper-donets-basin-donbas-foldbelt-ukraine.html"}],"country":"Ukraine","volume":"96","issue":"47","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059efefe4b0c8380cd4a511","contributors":{"authors":[{"text":"Law, B. E.","contributorId":17586,"corporation":false,"usgs":true,"family":"Law","given":"B.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":386476,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ulmishek, G. F.","contributorId":89144,"corporation":false,"usgs":true,"family":"Ulmishek","given":"G. F.","affiliations":[],"preferred":false,"id":386480,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Clayton, J.L.","contributorId":76767,"corporation":false,"usgs":true,"family":"Clayton","given":"J.L.","email":"","affiliations":[],"preferred":false,"id":386479,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Kabyshev, B.P.","contributorId":96448,"corporation":false,"usgs":true,"family":"Kabyshev","given":"B.P.","email":"","affiliations":[],"preferred":false,"id":386481,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Pashova, N.T.","contributorId":69745,"corporation":false,"usgs":true,"family":"Pashova","given":"N.T.","email":"","affiliations":[],"preferred":false,"id":386478,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Krivosheya, V.A.","contributorId":63985,"corporation":false,"usgs":true,"family":"Krivosheya","given":"V.A.","email":"","affiliations":[],"preferred":false,"id":386477,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":23158,"text":"ofr97470E - 1997 - Maps showing geology, oil and gas fields and geologic provinces of the former Soviet Union","interactions":[],"lastModifiedDate":"2024-01-25T16:42:07.461324","indexId":"ofr97470E","displayToPublicDate":"2019-10-11T11:15:00","publicationYear":"1997","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":"97-470","chapter":"E","displayTitle":"Maps Showing Geology, Oil and Gas Fields and Geologic Provinces of the Former Soviet Union","title":"Maps showing geology, oil and gas fields and geologic provinces of the former Soviet Union","docAbstract":"<p>This digitally compiled map includes geology, geologic provinces, and oil and gas fields of the Former Soviet Union. The map is part of a worldwide series on CD-ROM by the World Energy Project released of the U.S. Geological Survey. The goal of the project is to assess the undiscovered, technically recoverable oil and gas resources of the world and report these results by the year 2000. For data management purposes the world was divided into eight energy regions corresponding approximately to the economic regions of the world as defined by the U.S. Department of State. The Former Soviet Union (Region 1) includes Armenia, Azerbaijan, Byelarus, Estonia, Georgia, Kazakhstan, Kyrgyzstan, Latvia, Lithuania, Moldova, Russia, Tajikistan, Turkmenistan, Ukraine, and Uzbekistan. Each region was then further divided into geologic provinces on the basis of natural geologic entities and may include a dominant structural element or a number of contiguous elements. Some provinces contain multiple genetically related basins. Geologic province boundaries for the Former Soviet Union were delineated using data from a number of geologic maps and other tectonic and geographic data (see References). Offshore province boundaries were defined by the 2000 meter bathymetric contour from the map edited by Gabrielyants, 1990 (see References). Each province was assigned a unique number; the first digit is the region number; province numbers follow. An attempt was made to number the provinces in geographical groups; onshore, offshore, and combined on and offshore. The numbering starts in the west.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr97470E","usgsCitation":"Persits, F.M., Ulmishek, G.F., and Steinshouer, D.W., 1999, Maps showing geology, oil and gas fields and geologic provinces of the former Soviet Union: U.S. Geological Survey Open-File Report 97-470-E, 13 p., https://doi.org/10.3133/ofr97470E.","productDescription":"Report: 13 p.; 2 Data Releases","onlineOnly":"N","additionalOnlineFiles":"Y","costCenters":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"links":[{"id":424680,"rank":3,"type":{"id":30,"text":"Data Release"},"url":"https://doi.org/10.5066/P93X2YLR","text":"Geologic Provinces of the Former Soviet Union","linkFileType":{"id":5,"text":"html"}},{"id":155760,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1997/ofr-97-470/OF97-470E/coverthb.jpg"},{"id":368261,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1997/ofr-97-470/OF97-470E/ofr97470E.pdf","text":"Report","size":"12.0 MB","linkFileType":{"id":1,"text":"pdf"},"description":"OFR 97-470-E"},{"id":424681,"rank":4,"type":{"id":30,"text":"Data Release"},"url":"https://doi.org/10.5066/P9GUL0PQ","text":"Generalized Geology of the Former Soviet Union","linkFileType":{"id":5,"text":"html"}}],"otherGeospatial":"former Soviet Union","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              33.75,\n              70.72897946208789\n            ],\n            [\n              27.773437499999996,\n              69.28725695167886\n            ],\n            [\n              34.1015625,\n              61.938950426660604\n            ],\n            [\n              22.5,\n              60.413852350464914\n            ],\n            [\n              25.3125,\n              49.83798245308484\n            ],\n            [\n              35.5078125,\n              44.59046718130883\n            ],\n            [\n              48.8671875,\n              40.44694705960048\n            ],\n            [\n              49.5703125,\n              47.517200697839414\n            ],\n            [\n              69.60937499999999,\n              41.244772343082076\n            ],\n            [\n              130.78125,\n              42.5530802889558\n            ],\n            [\n              153.28125,\n              48.22467264956519\n            ],\n            [\n              184.5703125,\n              61.60639637138628\n            ],\n            [\n              189.140625,\n              67.87554134672945\n            ],\n            [\n              129.0234375,\n              76.9206135182968\n            ],\n            [\n              67.8515625,\n              77.38950400539731\n            ],\n            [\n              33.75,\n              70.72897946208789\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","contact":"<p><a href=\"../contact\" data-mce-href=\"../contact\">Contact Pubs Warehouse</a></p>","tableOfContents":"<ul><li>Introduction</li><li>Data processing steps</li><li>References</li><li>Geologic provinces in the Former Soviet Union, sorted by province name</li><li>Geologic provinces in the Former Soviet Union, sorted by province code</li><li>Map showing geologic provinces of the Former Soviet Union</li><li>Map showing geology, oil and gas fields and geologic provinces of the Former Soviet Union</li></ul>","publishedDate":"1999-05-01","noUsgsAuthors":false,"publicationDate":"1999-05-01","publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db605919","contributors":{"authors":[{"text":"Persits, F.M.","contributorId":51324,"corporation":false,"usgs":true,"family":"Persits","given":"F.M.","affiliations":[],"preferred":false,"id":189545,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ulmishek, G. F.","contributorId":89144,"corporation":false,"usgs":true,"family":"Ulmishek","given":"G. F.","affiliations":[],"preferred":false,"id":189546,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Steinshouer, D.W.","contributorId":18803,"corporation":false,"usgs":true,"family":"Steinshouer","given":"D.W.","email":"","affiliations":[],"preferred":false,"id":189544,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":5210576,"text":"5210576 - 1995 - Ecological and toxicological aspects of the partial meltdown of the Chernobyl nuclear power plant reactor","interactions":[{"subject":{"id":5210576,"text":"5210576 - 1995 - Ecological and toxicological aspects of the partial meltdown of the Chernobyl nuclear power plant reactor","indexId":"5210576","publicationYear":"1995","noYear":false,"chapter":"24","title":"Ecological and toxicological aspects of the partial meltdown of the Chernobyl nuclear power plant reactor"},"predicate":"IS_PART_OF","object":{"id":5200050,"text":"5200050 - 1995 - Handbook of ecotoxicology","indexId":"5200050","publicationYear":"1995","noYear":false,"title":"Handbook of ecotoxicology"},"id":1}],"isPartOf":{"id":5200050,"text":"5200050 - 1995 - Handbook of ecotoxicology","indexId":"5200050","publicationYear":"1995","noYear":false,"title":"Handbook of ecotoxicology"},"lastModifiedDate":"2017-05-18T15:20:25","indexId":"5210576","displayToPublicDate":"2009-06-09T09:23:17","publicationYear":"1995","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"chapter":"24","title":"Ecological and toxicological aspects of the partial meltdown of the Chernobyl nuclear power plant reactor","docAbstract":"<p>the partial meltdown of the 1000-MW reactor at Chernobyl, Ukraine, on April 26, 1986, released large amounts of radiocesium and other radionuclides into the environment, causing widespread radioactive contamination of Europe and the former Soviet Union.<sup>1-7</sup> At least 3,000,000 trillion becquerels (TBq) were released from the fuel during the accident (Table 24.1), dwarfing, by orders of magnitude, radiation released from other highly publicized reactor accidents at Windscale (U.K.) and three-Mile Island (U.S.)<sup>3,8</sup> The Chernobyl accident happened while a test was being conducted during a normal scheduled shutdown and is attributed mainly to human error.<sup>3</sup></p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Handbook of ecotoxicology","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Lewis Publishers","publisherLocation":"Boca Raton, FL","isbn":"0873715853","usgsCitation":"Eisler, R., 1995, Ecological and toxicological aspects of the partial meltdown of the Chernobyl nuclear power plant reactor, chap. 24 <i>of</i> Handbook of ecotoxicology, p. 549-564.","productDescription":"16 p.","startPage":"549","endPage":"564","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":200720,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ee4b07f02db627fcb","contributors":{"editors":[{"text":"Hoffman, David J.","contributorId":86075,"corporation":false,"usgs":true,"family":"Hoffman","given":"David","email":"","middleInitial":"J.","affiliations":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"preferred":false,"id":506717,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Rattner, Barnett A. 0000-0003-3676-2843 brattner@usgs.gov","orcid":"https://orcid.org/0000-0003-3676-2843","contributorId":4142,"corporation":false,"usgs":true,"family":"Rattner","given":"Barnett","email":"brattner@usgs.gov","middleInitial":"A.","affiliations":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"preferred":true,"id":506716,"contributorType":{"id":2,"text":"Editors"},"rank":2},{"text":"Burton, G. Allen Jr.","contributorId":111752,"corporation":false,"usgs":true,"family":"Burton","given":"G.","suffix":"Jr.","email":"","middleInitial":"Allen","affiliations":[],"preferred":false,"id":506718,"contributorType":{"id":2,"text":"Editors"},"rank":3},{"text":"Cairns, John Jr.","contributorId":111897,"corporation":false,"usgs":true,"family":"Cairns","given":"John","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":506719,"contributorType":{"id":2,"text":"Editors"},"rank":4}],"authors":[{"text":"Eisler, Ronald","contributorId":101303,"corporation":false,"usgs":true,"family":"Eisler","given":"Ronald","affiliations":[],"preferred":false,"id":328735,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70207735,"text":"70207735 - 1994 - Varve calibrated records of carbonate and organic carbon accumulation over the last 2000 years in the Black Sea","interactions":[],"lastModifiedDate":"2020-01-08T14:09:28","indexId":"70207735","displayToPublicDate":"1994-01-08T13:57:25","publicationYear":"1994","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1836,"text":"Global Biogeochemical Cycles","active":true,"publicationSubtype":{"id":10}},"title":"Varve calibrated records of carbonate and organic carbon accumulation over the last 2000 years in the Black Sea","docAbstract":"<p><span>Sedimentologic and geochemical studies of box and gravity cores recovered from the Black Sea during the first leg of a multileg international Black Sea expedition in 1988 allow reconstruction of the basinwide Holocene environmental history of the Black Sea. In the deeper parts of the basin, box cores typically recovered a flocculent surface layer (“fluff”), laminated coccolith marls of Unit I (25–45 cm thick), and the upper 5–10 cm of finely laminated, dark‐colored sapropels of Unit II. Fine‐grained, homogeneous mud turbidites are interbedded with Units I and II over much of the basin, but the stratigraphie position of these turbidites differs, from site to site. The deposition of individual turbidites up to 15 cm thick does not appear to have significantly disturbed underlying laminae. Sediment trap deployments in the Black Sea suggest that light and dark laminae couplets represent annual increments of sedimentation (i.e., varves); we have therefore constructed a varve chronology for the sequence in order to correlate and date distinctive sedimentation and paleoenvironmental events. Distinctive groups of laminae in Unit I can be correlated across the entire deeper basin (a distance of more than 1000 km). This implies a remarkable homogeneity in production, accumulation, and preservation of biogenic material over much of the Black Sea during deposition of Unit I. The change from deposition of finely laminated, organic carbon‐rich sapropels (Unit II) to laminated, more calcareous, coccolith‐rich marls (Unit I) is thought to represent the crossing of a salinity threshold for&nbsp;</span><i>Emiliania huxleyi.</i><span>&nbsp;The varve chronology sets this change at about 1.63 ka (1633±100 yr B.P.), but the record of magnetic secular variation measured in several cores produces an age estimate of about 2.0 ka for the base of Unit I, or about 1.2 times the varve age. The average of six calibrated accelerator mass spectrometry radiocarbon ages for the base of Unit I is 2.7 ka, or about 1.7 times the varve age. Following the initial change to coccolith‐dominated sedimentation, deposition of sapropel resumed for at least one significant period, 1.56–1.25 ka. Since 1.25 ka, cycles of carbonate deposition with quasi‐decadal periodicities have produced characteristic darker and lighter assemblages of laminae. These cycles may have been climatically driven. Geochemical analyses coupled with the varve ages adopted herein indicate that accumulation rates of carbonate are nearly an order of magnitude higher in Unit I (averaging 35–45 g m</span><sup>−2</sup><span>&nbsp;yr</span><sup>−1</sup><span>) than in sapropelic Unit II. which contains primarily detrital carbonate. The accumulation of lithogenic components in parts of Unit I is only 1.5 times the rate in Unit II. Deepwater organic carbon accumulation rates are somewhat higher in Unit I (3.5–4.5 g m</span><sup>−2</sup><span>&nbsp;yr</span><sup>−1</sup><span>) than in the upper part of Unit II. Organic carbon accumulation rates in Unit I are somewhat antithetic to those of carbonate, and on the basis of this and additional constraints placed by pyrolysis and carbon isotopic analyses of organic material, it appears that terrestrial organic matter is an important component (perhaps &gt;25%) of total organic carbon burial in the basin. Unit I in the western part of the Black Sea has a higher terrestrial organic component and higher accumulation rates of terrigenous clastic material than Unit I in the eastern part. This difference between eastern and western Black Sea is to be expected because of the major rivers that empty into the western Black Sea from eastern Europe, Ukraine, and Russia. Shallow slope sites, but still within euxinic bottom waters, have lower organic carbon accumulation rates and lower pyrolysis hydrogen indices than deepwater basinal sites, suggesting selective resuspension and oxidation of organic matter at basin margins and focusing of organic matter deposition toward the basin center. A comparison of the Black Sea data with those from several open ocean sites with similar water depths showed no significant difference between organic carbon accumulation rates under oxic and anoxic conditions. For a given bulk accumulation rate the organic carbon accumulation rates, normalized to primary productivity, are about the same in both settings.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/94GB00297","usgsCitation":"Arthur, M.A., Dean, W.E., Neff, E., Hay, B., King, J., and Jones, G.A., 1994, Varve calibrated records of carbonate and organic carbon accumulation over the last 2000 years in the Black Sea: Global Biogeochemical Cycles, v. 8, no. 2, p. 195-217, https://doi.org/10.1029/94GB00297.","productDescription":"23 p.","startPage":"195","endPage":"217","costCenters":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"links":[{"id":371079,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Black Sea","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              28.125,\n              41.64007838467894\n            ],\n            [\n              30.322265625000004,\n              40.713955826286046\n            ],\n            [\n              34.365234375,\n              41.705728515237524\n            ],\n            [\n              40.42968749999999,\n              40.58058466412761\n            ],\n            [\n              41.8359375,\n              41.178653972331674\n            ],\n            [\n              41.8359375,\n              43.32517767999296\n            ],\n            [\n              37.6171875,\n              45.27488643704891\n            ],\n            [\n              39.814453125,\n              47.338822694822\n            ],\n            [\n              34.80468749999999,\n              46.86019101567027\n            ],\n            [\n              34.98046875,\n              45.1510532655634\n            ],\n            [\n              33.75,\n              44.715513732021336\n            ],\n            [\n              33.486328125,\n              45.583289756006316\n            ],\n            [\n              33.75,\n              46.255846818480315\n            ],\n            [\n              31.025390625,\n              46.73986059969267\n            ],\n            [\n              29.355468750000004,\n              45.521743896993634\n            ],\n            [\n              28.212890625,\n              44.653024159812\n            ],\n            [\n              27.158203125,\n              43.26120612479979\n            ],\n            [\n              28.125,\n              41.64007838467894\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"8","issue":"2","noUsgsAuthors":false,"publicationDate":"2012-09-21","publicationStatus":"PW","contributors":{"authors":[{"text":"Arthur, Michael A.","contributorId":90018,"corporation":false,"usgs":true,"family":"Arthur","given":"Michael","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":779126,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"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":779127,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Neff, E.D.","contributorId":221611,"corporation":false,"usgs":false,"family":"Neff","given":"E.D.","email":"","affiliations":[],"preferred":false,"id":779128,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hay, B.J.","contributorId":51772,"corporation":false,"usgs":true,"family":"Hay","given":"B.J.","email":"","affiliations":[],"preferred":false,"id":779129,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"King, J.","contributorId":100143,"corporation":false,"usgs":true,"family":"King","given":"J.","affiliations":[],"preferred":false,"id":779130,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Jones, Glenn A.","contributorId":17779,"corporation":false,"usgs":false,"family":"Jones","given":"Glenn","email":"","middleInitial":"A.","affiliations":[{"id":6706,"text":"Woods Hole Oceanographic Institution,","active":true,"usgs":false}],"preferred":false,"id":779131,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70017463,"text":"70017463 - 1994 - Observations on the geology and geohydrology of the Chernobyl' nuclear accident site, Ukraine","interactions":[],"lastModifiedDate":"2024-03-15T12:11:38.160115","indexId":"70017463","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2020,"text":"International Geology Review","active":true,"publicationSubtype":{"id":10}},"title":"Observations on the geology and geohydrology of the Chernobyl' nuclear accident site, Ukraine","docAbstract":"<div class=\"hlFld-Abstract\"><p class=\"first last\">The most higly contaminated surface areas from cesium-137 fallout from the April 1986 accident at the Chernobyl' nuclear power station in Ukraine occur within the 30-km radius evacuation zone set up around the station, and an 80-km lobe extending to the west-southwest. Lower levels of contamination extend 300 km to the west of the power station. The deposition of this radioactive dust on the surface and the subsequent entombment of the damaged reactor effectively result in the de facto establishment of an above-ground nuclear waste storage site. This site is located on a thick sedimentary sequence of loose, mostly clastic deposits, with a shallow (generally 3-5 m) water table. The geology, the presence of surface water, a shallow water table, and leaky aquifers at depth make this an unfavorable environment for the long-term containment and storage of the radioactive debris. An understanding of the general geology and hydrology of the area is important to assess the environmental impact of this unintended waste storage site, and to evaluate the potential for radionuclide migration through the soil and rock and into subsurface aquifers and nearby rivers.</p></div>","language":"English","publisher":"Taylor and Francis","doi":"10.1080/00206819409465456","issn":"00206814","usgsCitation":"Matzko, J., Percious, D., Rachlin, J., and Marples, D., 1994, Observations on the geology and geohydrology of the Chernobyl' nuclear accident site, Ukraine: International Geology Review, v. 36, no. 2, p. 203-211, https://doi.org/10.1080/00206819409465456.","productDescription":"9 p.","startPage":"203","endPage":"211","numberOfPages":"9","costCenters":[],"links":[{"id":228556,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"36","issue":"2","noUsgsAuthors":false,"publicationDate":"2010-07-06","publicationStatus":"PW","scienceBaseUri":"505a6ad7e4b0c8380cd7439f","contributors":{"authors":[{"text":"Matzko, J.R.","contributorId":56653,"corporation":false,"usgs":true,"family":"Matzko","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":376546,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Percious, D.J.","contributorId":95067,"corporation":false,"usgs":true,"family":"Percious","given":"D.J.","email":"","affiliations":[],"preferred":false,"id":376548,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rachlin, J.","contributorId":43929,"corporation":false,"usgs":true,"family":"Rachlin","given":"J.","email":"","affiliations":[],"preferred":false,"id":376545,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Marples, D.R.","contributorId":80442,"corporation":false,"usgs":true,"family":"Marples","given":"D.R.","email":"","affiliations":[],"preferred":false,"id":376547,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":35693,"text":"b1785 - 1987 - Processing and analysis of commercial satellite image data of the nuclear accident near Chernobyl, U.S.S.R.","interactions":[],"lastModifiedDate":"2017-03-27T14:51:31","indexId":"b1785","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1785","title":"Processing and analysis of commercial satellite image data of the nuclear accident near Chernobyl, U.S.S.R.","docAbstract":"<p>Advanced digital processing techniques were applied to Landsat-5 Thematic Mapper (TM) data and SPOT highresolution visible (HRV) panchromatic data to maximize the utility of images of a nuclear powerplant emergency at Chernobyl in the Soviet Ukraine. The images demonstrate the unique interpretive capabilities provided by the numerous spectral bands of the Thematic Mapper and the high spatial resolution of the SPOT HRV sensor. </p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/b1785","usgsCitation":"Sadowski, F.G., and Covington, S.J., 1987, Processing and analysis of commercial satellite image data of the nuclear accident near Chernobyl, U.S.S.R.: U.S. Geological Survey Bulletin 1785, iii, 19 p., https://doi.org/10.3133/b1785.","productDescription":"iii, 19 p.","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":167285,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1785/report-thumb.jpg"},{"id":63596,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1785/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9be4b07f02db65e502","contributors":{"authors":[{"text":"Sadowski, Franklin G.","contributorId":91552,"corporation":false,"usgs":true,"family":"Sadowski","given":"Franklin","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":215069,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Covington, Steven J.","contributorId":39436,"corporation":false,"usgs":true,"family":"Covington","given":"Steven","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":215068,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70236976,"text":"70236976 - 1987 - Processing and analysis of commercial satellite image data of the nuclear accident at Chernobyl, U.S.S.R.","interactions":[],"lastModifiedDate":"2022-09-23T19:14:22.128389","indexId":"70236976","displayToPublicDate":"1987-09-01T13:57:33","publicationYear":"1987","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Processing and analysis of commercial satellite image data of the nuclear accident at Chernobyl, U.S.S.R.","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"1987 ASPRS-ACSM Fall Convention: ASPRS technical papers","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"1987 ASPRS-ACSM Fall Convention","conferenceDate":"October 4-9, 1987","conferenceLocation":"Reno, Nevada, United States","language":"English","publisher":"American Society for Photogrammetry and Remote 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