{"pageNumber":"250","pageRowStart":"6225","pageSize":"25","recordCount":11361,"records":[{"id":70200704,"text":"70200704 - 1993 - Economics and the national oil and gas assessment: The case of onshore northern Alaska","interactions":[],"lastModifiedDate":"2023-01-23T18:02:25.657144","indexId":"70200704","displayToPublicDate":"1993-10-16T13:49:30","publicationYear":"1993","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":701,"text":"American Association of Petroleum Geologists Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Economics and the national oil and gas assessment: The case of onshore northern Alaska","docAbstract":"<p>The National Oil and Gas Assessment of undiscovered recoverable conventional oil and gas resources assigned nearly 36% of the undiscovered U.S. onshore oil resources and 28% of the commercially developable undiscovered oil resources to onshore northern Alaska. Economic screening models were applied to the geologic play assessment to estimate the commercially developable resources. This paper presents the geologic and economic assessment methodology and results; it also focuses on the robustness of estimates of the commercially developable onshore resources to changes in economic assumptions.</p><p>With the economic assumptions used in the national assessment, about 60% or 6.49 billion bbl of oil of the recoverable undiscovered resources of 10.76 billion bbl of oil assessed in fields larger than 1 million bbl of oil are estimated to be commercially developable. Changes in facilities costs induced the most significant cost-related response in the commercially developable resource estimates. Price increases or cost reductions that reduce the minimum commercially developable field size to 250 million bbl from the base case size of 380 million bbl added 1 billion bbl of oil to the commercially developable resources. If, through facilities sharing or satellite-field development, the minimum commercial field size is reduced to just below 100 million bbl, estimated developable oil woul increase to 9.17 billion bbl of oil or more than 85% of the assessed recoverable oil in onshore plays.</p>","language":"English","publisher":"American Association of Petroleum Geologists","doi":"10.1306/BDFF8C72-1718-11D7-8645000102C1865D","usgsCitation":"Attanasi, E., Bird, K.J., and Mast, R.F., 1993, Economics and the national oil and gas assessment: The case of onshore northern Alaska: American Association of Petroleum Geologists Bulletin, v. 77, no. 3, p. 491-504, https://doi.org/10.1306/BDFF8C72-1718-11D7-8645000102C1865D.","productDescription":"14 p.","startPage":"491","endPage":"504","costCenters":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true},{"id":255,"text":"Energy Resources Program","active":true,"usgs":true}],"links":[{"id":358906,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -145.48080420268553,\n              72.71391257340173\n            ],\n            [\n              -170.8889081934487,\n              72.71391257340173\n            ],\n            [\n              -170.8889081934487,\n              66.46646934602157\n            ],\n            [\n              -145.48080420268553,\n              66.46646934602157\n            ],\n            [\n              -145.48080420268553,\n              72.71391257340173\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"77","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5c111a1ce4b034bf6a8194de","contributors":{"authors":[{"text":"Attanasi, Emil D. 0000-0001-6845-7160 attanasi@usgs.gov","orcid":"https://orcid.org/0000-0001-6845-7160","contributorId":198728,"corporation":false,"usgs":true,"family":"Attanasi","given":"Emil D.","email":"attanasi@usgs.gov","affiliations":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":750176,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bird, Kenneth J. kbird@usgs.gov","contributorId":1015,"corporation":false,"usgs":true,"family":"Bird","given":"Kenneth","email":"kbird@usgs.gov","middleInitial":"J.","affiliations":[{"id":255,"text":"Energy Resources Program","active":true,"usgs":true}],"preferred":true,"id":750177,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mast, R. F.","contributorId":210210,"corporation":false,"usgs":false,"family":"Mast","given":"R.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":750178,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70017985,"text":"70017985 - 1993 - Orogenesis, high-T thermal events, and gold vein formation within metamorphic rocks of the Alaskan Cordillera","interactions":[],"lastModifiedDate":"2024-10-07T16:49:53.188542","indexId":"70017985","displayToPublicDate":"1993-09-01T00:00:00","publicationYear":"1993","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2748,"text":"Mineralogical Magazine","active":true,"publicationSubtype":{"id":10}},"title":"Orogenesis, high-T thermal events, and gold vein formation within metamorphic rocks of the Alaskan Cordillera","docAbstract":"<p><span>Mesothermal, gold-bearing quartz veins are widespread within allochthonous terranes of Alaska that are composed dominantly of greenschist-facies metasedimentary rocks. The most productive lode deposits are concentrated in south-central and southeastern Alaska; small and generally nonproductive gold-bearing veins occur upstream from major placer deposits in interior and northern Alaska. Oreforming fluids in all areas are consistent with derivation from metamorphic devolatilisation reactions, and a close temporal relationship exists between high-T tectonic deformation, igneous activity, and gold mineralization. Ore fluids were of consistently low salinity, CO</span><span class=\"sub\">2</span><span>-rich, and had δ</span><span class=\"sup\">18</span><span>O values of 7‰- 12‰ and δD values between −15‰ and −35‰. Upper-crustal temperatures within the metamorphosed terranes reached at least 450-500°C before onset of significant gold-forming hydrothermal activity. Within interior and northern Alaska, latest Paleozoic through Early Cretaceous contractional deformation was characterised by obduction of oceanic crust, low-T/high-P metamorphism, and a lack of gold vein formation. Mid-Cretaceous veining occurred some 50-100 m.y. later, during a subsequent high-</span><span class=\"italic\">T</span><span>&nbsp;metamorphic/magmatic event, possibly related to extension and uplift. In southern Alaska, gold deposits formed during latter stages of Tertiary, subduction-related, collisional orogenesis and were often temporally coeval with calc-alkaline magmatism.</span></p>","language":"English","publisher":"Cambridge University Press","doi":"10.1180/minmag.1993.057.388.03","usgsCitation":"Goldfarb, R., Snee, L., and Pickthorn, W., 1993, Orogenesis, high-T thermal events, and gold vein formation within metamorphic rocks of the Alaskan Cordillera: Mineralogical Magazine, v. 57, no. 388, p. 375-394, https://doi.org/10.1180/minmag.1993.057.388.03.","productDescription":"20 p.","startPage":"375","endPage":"394","costCenters":[],"links":[{"id":228690,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United 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,{"id":70113763,"text":"70113763 - 1993 - History of greenness mapping at the EROS data center","interactions":[],"lastModifiedDate":"2014-06-20T13:54:57","indexId":"70113763","displayToPublicDate":"1993-08-24T13:48:22","publicationYear":"1993","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3018,"text":"Pecora 12 Symposium","active":true,"publicationSubtype":{"id":10}},"title":"History of greenness mapping at the EROS data center","docAbstract":"<p>In 1987, the U.S. Geological Survey's EROS Data Center (EDC)installed a system to acquire, process, and distribute advanced very high resolution radiometer (AVHRR) satellite image data collected over North America.  Using this system, the EDC began an experimental greenness mapping program as part of the U.S. Agency for the International Development Famine Early Warning System.  The program used the greenness information derived from AVHRR data to identify potential outbreaks of locusts and grasshoppers in the Sahelian region of Africa.  In 1988, the EDC began greenness mapping projects in Africa and the northern Great Plains of the United States.  In 1989, the system was augmented to acquire AVHRR information for the rest of the world.  As a result, the greenness mapping program was able to collect data for fire danger assessment, agricultural assessment, and land characterization.</p>\n<br/>\n<p>Illustrations of each of the mapping projects trace the chronology of the greenness mapping program at the EDC.  Displays represent the initial activity in Africa and the transition of the north Great Plains project to the current conterminous U.S. project.  The program's expansion to include Alaska, Eurasia, a prototype North America data set, and ultimately, an experimental global land 1-km product is also shown.  The poster describes major technical advances in data processing, the development of derivative products, the magnitude of the data volume of each level, and major applications.</p>","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Pecora 12 Symposium","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"American Society for Photogrammetry and Remote Sensing","publisherLocation":"Bethesda, MD","usgsCitation":"Van Beek, C., and Vandersnick, R., 1993, History of greenness mapping at the EROS data center: Pecora 12 Symposium, p. 559-559.","productDescription":"1 p.","startPage":"559","endPage":"559","numberOfPages":"1","costCenters":[],"links":[{"id":288987,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53ae773ae4b0abf75cf2c0b7","contributors":{"authors":[{"text":"Van Beek, Carolyn","contributorId":35234,"corporation":false,"usgs":true,"family":"Van Beek","given":"Carolyn","email":"","affiliations":[],"preferred":false,"id":495188,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Vandersnick, Richard","contributorId":108027,"corporation":false,"usgs":true,"family":"Vandersnick","given":"Richard","email":"","affiliations":[],"preferred":false,"id":495189,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70210581,"text":"70210581 - 1993 - Mid‐Cretaceous extensional tectonics of the Yukon‐Tanana Terrane, Trans‐Alaska Crustal Transect (TACT), east‐central Alaska","interactions":[],"lastModifiedDate":"2020-06-10T18:08:54.019251","indexId":"70210581","displayToPublicDate":"1993-06-10T12:56:36","publicationYear":"1993","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3524,"text":"Tectonics","active":true,"publicationSubtype":{"id":10}},"title":"Mid‐Cretaceous extensional tectonics of the Yukon‐Tanana Terrane, Trans‐Alaska Crustal Transect (TACT), east‐central Alaska","docAbstract":"<p><span>Mid‐Cretaceous crustal extension played a fundamental role in the structural evolution of the Yukon‐Tanana terrane (YTT) in the northern Cordilleran interior. In the central portion of the YTT northwest of Delta Junction, Alaska, a mylonitic shear zone juxtaposes greenschist facies rocks in the upper plate against middle to upper amphibolite facies metamorphic rocks in the lower plate, a juxtaposition suggesting elimination of as much as 10 km of crustal section. The mylonites form a partial sheath enveloping a domal footwall structure and kinematic analysis of the mylonite zone yields a uniform transport direction of hanging wall to ESE. These relations suggest analogies to the metamorphic core complexes of the southern Cordillera. However, the YTT structures are entirely ductile, suggesting either a relatively deep erosional level or relatively high geothermal gradients during extension. In the study area remnants of an older preextensional thrusting event are preserved at the highest structural levels at the base of the Seventymile terrane and the leading edge of YTT in the Wickersham terrane. However, most areas display a regional, subhorizontal fabric that is superimposed on older fabrics, and in the study area this latest fabric is subparallel to the mylonitic sheath of the apparent extensional structure. Thus the conventional viewpoint that this latest fabric is related to thrusting needs to be reevaluated and this fabric may be entirely extensional in origin. Further evidence for extension is provided by clear similarities between YTT and characteristic features of other extensional terranes. Thus we suggest that the YTT is a deeply eroded view of highly extended continental crust. The tectonic mechanism for the extensional event and the magnitude of the extension is uncertain because of complications in regional timing relationships and in alternative interpretations of the reconstruction of the crustal section. Three end‐member models based on analogies with Neogene extensional systems are presented as working models to accommodate the alternative interpretations: (1) a Jurassic collision and Cretaceous extension model based on comparisons with the Neogene history of the Mediterranean region; (2) an Early to mid‐Cretaceous syncollisional model analogous to the Carpathian Mountains of eastern Europe; and (3) a syncollisional plateau uplift model with extension driven by gravity spreading.</span></p>","language":"English","publisher":"Wiley","doi":"10.1029/92TC00860","usgsCitation":"Pavlis, T.L., Sisson, V., Foster, H.L., Nokleberg, W.J., and Plafker, G., 1993, Mid‐Cretaceous extensional tectonics of the Yukon‐Tanana Terrane, Trans‐Alaska Crustal Transect (TACT), east‐central Alaska: Tectonics, v. 12, no. 1, p. 103-122, https://doi.org/10.1029/92TC00860.","productDescription":"20 p.","startPage":"103","endPage":"122","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":375498,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Eastern Central Alaska","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -151.78710937499997,\n              64.33990785750463\n            ],\n            [\n              -141.0205078125,\n              64.33990785750463\n            ],\n            [\n              -141.0205078125,\n              67.25505812564363\n            ],\n            [\n              -151.78710937499997,\n              67.25505812564363\n            ],\n            [\n              -151.78710937499997,\n              64.33990785750463\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"12","issue":"1","noUsgsAuthors":false,"publicationDate":"2010-07-26","publicationStatus":"PW","contributors":{"authors":[{"text":"Pavlis, Terry L.","contributorId":52682,"corporation":false,"usgs":true,"family":"Pavlis","given":"Terry","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":790672,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sisson, V.B.","contributorId":101104,"corporation":false,"usgs":false,"family":"Sisson","given":"V.B.","email":"","affiliations":[],"preferred":false,"id":790673,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Foster, Helen L.","contributorId":56195,"corporation":false,"usgs":true,"family":"Foster","given":"Helen","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":790674,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Nokleberg, Warren J. 0000-0002-1574-8869 wnokleberg@usgs.gov","orcid":"https://orcid.org/0000-0002-1574-8869","contributorId":2077,"corporation":false,"usgs":true,"family":"Nokleberg","given":"Warren","email":"wnokleberg@usgs.gov","middleInitial":"J.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":790675,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Plafker, George","contributorId":3920,"corporation":false,"usgs":false,"family":"Plafker","given":"George","email":"","affiliations":[],"preferred":false,"id":790676,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70180795,"text":"70180795 - 1993 - Cruise to the Chukchi Borderland, Arctic Ocean","interactions":[],"lastModifiedDate":"2017-02-03T12:33:17","indexId":"70180795","displayToPublicDate":"1993-06-01T00:00:00","publicationYear":"1993","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3879,"text":"Eos, Earth and Space Science News","active":true,"publicationSubtype":{"id":10}},"title":"Cruise to the Chukchi Borderland, Arctic Ocean","docAbstract":"<p><span>Oceanography and geology were the principal focuses of the U.S. Geological Survey-sponsored expedition Arctic Summer West '92, which traveled to the eastern part of the Chukchi Borderland of the Amerasia Basin, western Arctic Ocean. The expedition took place from August 20 to September 25, 1992, aboard the Coast Guard cutter </span><i>Polar Star</i><span>. USGS investigated the geologic framework and tectonic origin of the borderland, Arctic Quaternary paleoclimate, sea-ice transport of particulate matter in the Beaufort Gyre, and possible radionuclide contamination of the water column and seafloor off Alaska from sources in the Russian Arctic. Researchers from five other institutions studied the area's oceanography, age of the water column, paleoenvironment of the Holocene sediment, physical properties and synthetic-aperture radar backscatter of sea ice, and the drop-stone content of late Quaternary sediment.</span></p>","language":"English","publisher":"AGU Publications","doi":"10.1029/93EO00273","usgsCitation":"Grantz, A., and 1992 Arctic Summer West Scientific Party, 1993, Cruise to the Chukchi Borderland, Arctic Ocean: Eos, Earth and Space Science News, v. 74, no. 22, p. 249-254, https://doi.org/10.1029/93EO00273.","productDescription":"6 p.","startPage":"249","endPage":"254","costCenters":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":334673,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"74","issue":"22","noUsgsAuthors":false,"publicationDate":"2011-06-03","publicationStatus":"PW","scienceBaseUri":"5895a4d4e4b0fa1e59bc1e91","contributors":{"authors":[{"text":"Grantz, Arthur agrantz@usgs.gov","contributorId":2585,"corporation":false,"usgs":true,"family":"Grantz","given":"Arthur","email":"agrantz@usgs.gov","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":662454,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"1992 Arctic Summer West Scientific Party","contributorId":179071,"corporation":true,"usgs":false,"organization":"1992 Arctic Summer West Scientific Party","id":662455,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70243584,"text":"70243584 - 1993 - Sediment export by ice rafting from a coastal Polynya, Arctic Alaska, U.S.A.","interactions":[],"lastModifiedDate":"2023-05-12T16:42:49.176473","indexId":"70243584","displayToPublicDate":"1993-05-01T11:29:12","publicationYear":"1993","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":898,"text":"Arctic and Alpine Research","active":true,"publicationSubtype":{"id":10}},"title":"Sediment export by ice rafting from a coastal Polynya, Arctic Alaska, U.S.A.","docAbstract":"<p><span>Strong offshore winds in early 1989 produced a shore polynya that reached along the entire north coast of Alaska and eastward beyond the mouth of the Mackenzie River in Canada. From January through April, this open water periodically exposed the shelf to sediment entrainment by suspension freezing. This process requires turbulence and supercooled water, which results in the formation of frazil and anchor ice. The resulting granular, sediment-laden ice was observed to extend over 100 km seaward of the outer continental shelf after having been advected offshore. It was sampled to determine sediment type and to quantify the particle load. The particle size was mainly silt and clay, with local admixtures of as much as 27% sand and coarser clasts. Melted ice samples contained from 31 to nearly 600 mg L<sup>-1</sup> of sediment. Combining these data with over 400 km of shipboard and aerial observations, photographs, and computer analysis of a summer Landsat image, we estimated the sediment load per unit area of sea ice. Seaward of the shelf, in regions of dense pack ice, a conservatively estimated sediment load was over 289 t km<sup>-2</sup>. Using a westward summer drift rate of 3 cm s<sup>-1</sup>, the sediment transport through a 1-km-long north-south segment is 67,418 t during 3 mo. In terms of regional sediment dynamics (littoral transport estimated at 10,000 t during the same period) and sediment budget (continental denudation estimated at 10 t km<sup>-2</sup> during the same period), this number is very significant. Benthic microfossils indicate that bottom sediment incorporated in the ice came from water depths ranging from the inner neritic seaward to 50 m. The large load of shelf-derived sediment observed seaward of the continental shelf indicates that ice entrainment and transport cause shelf erosion. Nothing is known about sediment release over the Arctic Ocean Basin from these pulses of dirty ice that are periodically introduced into the Transpolar Drift.</span></p>","language":"English","publisher":"Taylor & Francis","doi":"10.2307/1551544","usgsCitation":"Reimnitz, E., McCormick, M., McDougall-Reid, K., and Brouwers, E.M., 1993, Sediment export by ice rafting from a coastal Polynya, Arctic Alaska, U.S.A.: Arctic and Alpine Research, v. 25, no. 2, p. 83-98, https://doi.org/10.2307/1551544.","productDescription":"16 p.","startPage":"83","endPage":"98","costCenters":[],"links":[{"id":416994,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Arctic Ocean","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -166.1893628235785,\n              68.8510799545711\n            ],\n            [\n              -165.7927784937305,\n              68.60302294479024\n            ],\n            [\n              -163.59571757549665,\n              68.45306559682152\n            ],\n            [\n              -162.10797619040798,\n              69.25615394607448\n            ],\n            [\n              -157.08199600571925,\n              70.07554650332517\n            ],\n            [\n              -151.61365855031693,\n              69.51002606358901\n            ],\n            [\n              -148.49371558067688,\n              69.28203829095418\n            ],\n            [\n              -146.08719200955667,\n              69.23274785479458\n            ],\n            [\n              -142.86278578656948,\n              69.5068404646222\n            ],\n            [\n              -140.99468181589384,\n              69.07584879432568\n            ],\n            [\n              -141.0126515770738,\n              69.62138774277821\n            ],\n            [\n              -140.17191729737542,\n              71.55828011520083\n            ],\n            [\n              -142.89846249283258,\n              71.71808353148506\n            ],\n            [\n              -158.7712581652307,\n              73.17888787382822\n            ],\n            [\n              -166.19595621130796,\n              71.98411374590395\n            ],\n            [\n              -168.2196648555574,\n              69.9431467369302\n            ],\n            [\n              -166.1893628235785,\n              68.8510799545711\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"25","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Reimnitz, Erk","contributorId":17963,"corporation":false,"usgs":true,"family":"Reimnitz","given":"Erk","email":"","affiliations":[],"preferred":false,"id":872450,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McCormick, Michael","contributorId":18791,"corporation":false,"usgs":true,"family":"McCormick","given":"Michael","email":"","affiliations":[],"preferred":false,"id":872451,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McDougall-Reid, Kristin 0000-0001-6026-0718 kris@usgs.gov","orcid":"https://orcid.org/0000-0001-6026-0718","contributorId":1942,"corporation":false,"usgs":true,"family":"McDougall-Reid","given":"Kristin","email":"kris@usgs.gov","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":872452,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Brouwers, Elisabeth M. brouwers@usgs.gov","contributorId":190,"corporation":false,"usgs":true,"family":"Brouwers","given":"Elisabeth","email":"brouwers@usgs.gov","middleInitial":"M.","affiliations":[{"id":501,"text":"Office of Science Quality and Integrity","active":true,"usgs":true}],"preferred":true,"id":872453,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70228807,"text":"70228807 - 1993 - Microfaunal evidence for elevated Pliocene temperatures in the Arctic Ocean","interactions":[],"lastModifiedDate":"2022-02-22T15:16:28.08182","indexId":"70228807","displayToPublicDate":"1993-04-01T09:05:39","publicationYear":"1993","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5790,"text":"Paleoceanography and Paleoclimatology","active":true,"publicationSubtype":{"id":10}},"title":"Microfaunal evidence for elevated Pliocene temperatures in the Arctic Ocean","docAbstract":"<p>The migration of thermophilic marine Ostracoda into the Arctic Ocean during the Pliocene indicates that winter and summer ocean temperatures around Arctic margins were ≥ 0 °C and &gt; 3 °C, respectively, and that ice-free conditions existed for most or all of the Arctic. By at least 3.5–3.0 Ma, probably earlier, the opening of the Bering Strait allowed marine organisms to migrate through the Arctic Ocean, mostly from the Pacific Ocean. Migrant taxa such as<span>&nbsp;</span><i>Cythere, Hemicythere,</i><span>&nbsp;</span>and<span>&nbsp;</span><i>Neomonoceratina</i><span>&nbsp;</span>are known from Pliocene deposits of Alaska and Canada as well as Neogene deposits of the North Pacific and Atlantic oceans. On the basis of ecological and Zoogeographic information on ostracode species from more than 800 modern “core top” samples for the North Atlantic, North Pacific, and Arctic Oceans, we determined winter and summer temperature tolerances for migrant taxa to be at or above about 0 °C and 3 °C. This suggests ice-free summers, and probably, a perennially ice-free Arctic Ocean in some regions. Elevated water temperatures in the Arctic Ocean between 3.5 and 2.0 Ma is supported by evidence for late Pliocene increased meridional heat transport in the North Atlantic Ocean.</p>","language":"English","publisher":"Wiley","doi":"10.1029/93PA00060","usgsCitation":"Cronin, T.M., Whatley, R., Wood, A., Tsukagoshi, A., Ikeya, N., Brouwers, E.M., and Briggs, W.M., 1993, Microfaunal evidence for elevated Pliocene temperatures in the Arctic Ocean: Paleoceanography and Paleoclimatology, v. 8, no. 2, p. 161-173, https://doi.org/10.1029/93PA00060.","productDescription":"13 p.","startPage":"161","endPage":"173","costCenters":[],"links":[{"id":396242,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Bering Strait, Arctic Ocean","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -165.9375,\n              68.52823492039876\n            ],\n            [\n              -140.625,\n              68.13885164925573\n            ],\n            [\n              -125.5078125,\n              68.65655498475735\n            ],\n            [\n              -121.9921875,\n              73.82482034613932\n            ],\n            [\n              -77.34374999999999,\n              82.49482361179574\n            ],\n            [\n              -63.6328125,\n              81.09321385260837\n            ],\n            [\n              -35.859375,\n              82.30889251821553\n            ],\n            [\n              -25.3125,\n              74.01954331150228\n            ],\n            [\n              -41.484375,\n              66.93006025862448\n            ],\n            [\n              26.3671875,\n              69.16255790810501\n            ],\n            [\n              37.265625,\n              64.16810689799152\n            ],\n            [\n              66.796875,\n              67.20403234340081\n            ],\n            [\n              74.1796875,\n              70.1403642720717\n            ],\n            [\n              103.35937499999999,\n              76.76054111175671\n            ],\n            [\n              105.46875,\n              73.22669969306126\n            ],\n            [\n              126.5625,\n              70.49557354093136\n            ],\n            [\n              141.6796875,\n              71.18775391813158\n            ],\n            [\n              187.3828125,\n              65.94647177615738\n            ],\n            [\n              180.35156249999997,\n              84.95930495623836\n            ],\n            [\n              -165.234375,\n              84.95930495623836\n            ],\n            [\n              -165.9375,\n              68.52823492039876\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"8","issue":"2","noUsgsAuthors":false,"publicationDate":"2010-05-04","publicationStatus":"PW","contributors":{"authors":[{"text":"Cronin, Thomas M. 0000-0002-2643-0979 tcronin@usgs.gov","orcid":"https://orcid.org/0000-0002-2643-0979","contributorId":2579,"corporation":false,"usgs":true,"family":"Cronin","given":"Thomas","email":"tcronin@usgs.gov","middleInitial":"M.","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":835574,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Whatley, Robin","contributorId":279858,"corporation":false,"usgs":false,"family":"Whatley","given":"Robin","email":"","affiliations":[],"preferred":false,"id":835575,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wood, Adrian","contributorId":63830,"corporation":false,"usgs":true,"family":"Wood","given":"Adrian","affiliations":[],"preferred":false,"id":835576,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Tsukagoshi, Akira","contributorId":279859,"corporation":false,"usgs":false,"family":"Tsukagoshi","given":"Akira","email":"","affiliations":[],"preferred":false,"id":835577,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Ikeya, Noriyuki","contributorId":101026,"corporation":false,"usgs":true,"family":"Ikeya","given":"Noriyuki","email":"","affiliations":[],"preferred":false,"id":835578,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Brouwers, Elisabeth M. brouwers@usgs.gov","contributorId":190,"corporation":false,"usgs":true,"family":"Brouwers","given":"Elisabeth","email":"brouwers@usgs.gov","middleInitial":"M.","affiliations":[{"id":501,"text":"Office of Science Quality and Integrity","active":true,"usgs":true}],"preferred":true,"id":835579,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Briggs, W. 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,{"id":70018269,"text":"70018269 - 1993 - Late Maastrichtian and Danian ostracode faunas from Northern Alaska; reconstructions of environment and paleogeography","interactions":[],"lastModifiedDate":"2025-03-12T15:13:35.106336","indexId":"70018269","displayToPublicDate":"1993-04-01T00:00:00","publicationYear":"1993","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3000,"text":"Palaios","active":true,"publicationSubtype":{"id":10}},"title":"Late Maastrichtian and Danian ostracode faunas from Northern Alaska; reconstructions of environment and paleogeography","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"GeoScienceWorld","doi":"10.2307/3515168","usgsCitation":"Brouwers, E.M., and De Deckker, P., 1993, Late Maastrichtian and Danian ostracode faunas from Northern Alaska; reconstructions of environment and paleogeography: Palaios, v. 8, no. 2, p. 140-154, https://doi.org/10.2307/3515168.","productDescription":"15 p.","startPage":"140","endPage":"154","costCenters":[],"links":[{"id":226974,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"northern Alaska","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -163.16921984686343,\n              71.33403218038652\n            ],\n            [\n              -163.16921984686343,\n              69.64510229704817\n            ],\n            [\n              -150.40414098978195,\n              69.64510229704817\n            ],\n            [\n              -150.40414098978195,\n              71.33403218038652\n            ],\n            [\n              -163.16921984686343,\n              71.33403218038652\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"8","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a44f0e4b0c8380cd66ee1","contributors":{"authors":[{"text":"Brouwers, Elisabeth M. brouwers@usgs.gov","contributorId":190,"corporation":false,"usgs":true,"family":"Brouwers","given":"Elisabeth","email":"brouwers@usgs.gov","middleInitial":"M.","affiliations":[{"id":501,"text":"Office of Science Quality and Integrity","active":true,"usgs":true}],"preferred":true,"id":379058,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"De Deckker, Patrick","contributorId":41160,"corporation":false,"usgs":true,"family":"De Deckker","given":"Patrick","affiliations":[],"preferred":false,"id":379057,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1008014,"text":"1008014 - 1993 - Reproductive characteristics of female sea otters","interactions":[],"lastModifiedDate":"2024-09-27T15:42:14.878087","indexId":"1008014","displayToPublicDate":"1993-04-01T00:00:00","publicationYear":"1993","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2671,"text":"Marine Mammal Science","active":true,"publicationSubtype":{"id":10}},"title":"Reproductive characteristics of female sea otters","docAbstract":"<p><span>Several important aspects of reproduction in the female sea otter, such as gestation, pupping frequency, period of pup dependency, and annual pupping rate, were unclear when this study was begun. We present data from 75 tagged adult females that indicate gestation is variable, but on average is about 6 months, the length of pup dependency is 6 mo, thus the pupping interval is usually 12–13 mo. 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About 85–90% of adult females pup in a given year.</span></p>","language":"English","publisher":"Wiley","doi":"10.1111/j.1748-7692.1993.tb00440.x","usgsCitation":"Jameson, R.J., and Johnson, A.M., 1993, Reproductive characteristics of female sea otters: Marine Mammal Science, v. 9, no. 2, p. 156-167, https://doi.org/10.1111/j.1748-7692.1993.tb00440.x.","productDescription":"12 p.","startPage":"156","endPage":"167","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":131055,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska, 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,{"id":70208292,"text":"70208292 - 1993 - The Beaufort Sea continental shelf as a seasonal source of atmospheric methane","interactions":[],"lastModifiedDate":"2020-02-03T11:09:42","indexId":"70208292","displayToPublicDate":"1993-02-03T10:59:24","publicationYear":"1993","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1807,"text":"Geophysical Research Letters","active":true,"publicationSubtype":{"id":10}},"title":"The Beaufort Sea continental shelf as a seasonal source of atmospheric methane","docAbstract":"<p><span>Methane concentrations in the Beaufort Sea under the winter ice canopy offshore from northern Alaska are 3 to 28 times greater than they are in late summer when the ice is absent in a similar region offshore from northern Canada where methane is in approximate equilibrium with the atmosphere. These observations suggest that methane concentrates in the water under the sea‐ice cover during winter and ventilates rapidly in late summer as the ice melts and retreats. Conditions similar to those on the Beaufort Sea shelf likely exist on the much larger Siberian shelf, making the Arctic Ocean margin a possible seasonal, high‐latitude, marine source of about 0.1 Tg yr</span><sup>−1</sup><span>&nbsp;atmospheric methane. The small addition of methane likely contributes to the late‐summer increase in atmospheric methane that is observed each year particularly in the northern hemisphere.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/93GL02727","usgsCitation":"Kvenvolden, K.A., Lilley, M.D., Lorenson, T., Barnes, P.W., and McLaughlin, E., 1993, The Beaufort Sea continental shelf as a seasonal source of atmospheric methane: Geophysical Research Letters, v. 20, no. 22, p. 2459-2462, https://doi.org/10.1029/93GL02727.","productDescription":"4 p.","startPage":"2459","endPage":"2462","costCenters":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":371920,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Beaufort Sea","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -157.236328125,\n              69.71810669906763\n            ],\n            [\n              -145.98632812499997,\n              69.71810669906763\n            ],\n            [\n              -145.98632812499997,\n              72.43553464712416\n            ],\n            [\n              -157.236328125,\n              72.43553464712416\n            ],\n            [\n              -157.236328125,\n              69.71810669906763\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"20","issue":"22","noUsgsAuthors":false,"publicationDate":"2012-12-07","publicationStatus":"PW","contributors":{"authors":[{"text":"Kvenvolden, Keith A. kkvenvolden@usgs.gov","contributorId":3384,"corporation":false,"usgs":true,"family":"Kvenvolden","given":"Keith","email":"kkvenvolden@usgs.gov","middleInitial":"A.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":781284,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lilley, Marvin D.","contributorId":45377,"corporation":false,"usgs":true,"family":"Lilley","given":"Marvin","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":781285,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lorenson, Thomas 0000-0001-7669-2873 tlorenson@usgs.gov","orcid":"https://orcid.org/0000-0001-7669-2873","contributorId":174599,"corporation":false,"usgs":true,"family":"Lorenson","given":"Thomas","email":"tlorenson@usgs.gov","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":781286,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Barnes, P. W.","contributorId":8819,"corporation":false,"usgs":true,"family":"Barnes","given":"P.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":781287,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"McLaughlin, E.","contributorId":86509,"corporation":false,"usgs":true,"family":"McLaughlin","given":"E.","email":"","affiliations":[],"preferred":false,"id":781288,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70208097,"text":"70208097 - 1993 - Fluvial response to late Quaternary climatic fluctuations, central Kobuk Valley, northwestern Alaska","interactions":[],"lastModifiedDate":"2020-01-27T14:36:53","indexId":"70208097","displayToPublicDate":"1993-01-27T14:31:43","publicationYear":"1993","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":"Fluvial response to late Quaternary climatic fluctuations, central Kobuk Valley, northwestern Alaska","docAbstract":"<p><span>Much of northwestern Alaska remained unglaciated during the Pleistocene and thus offers a favorable setting for examining long-term records of high-latitude geological and biological change. Epiguruk, a large cut bank 3.5 km long and up to 36 m high on the Kobuk River south of the Brooks Range in eastern Beringia, exposes complex sedimentary successions representing cycles of upper Quaternary alluviation and eolian sedimentation, downcutting, and soil formation. A rich record of plants and mammals is also preserved in the section. Deposits of fluvial channels and flood plains, eolian dunes, sand sheets, loess, and ponds, as well as organic soils (Histosols) are represented. Parallel-bedded fine sand and coarse silt couplets that commonly contain root structures, ripple cross-lamination, and silt drapes are flood-plain sediments apparently deposited at the interface of fluvial and eolian environments. Multiple fluvial-to-eolian depositional sequences were caused by influx of eolian sediment to the river from intermittently active dune fields south of the Kobuk River. Alluviation in the Kobuk Valley was coeval with glaciation in the Brooks Range, whereas downcutting occurred during interstadials when dune stabilization limited sediment supply. The depositional model developed at Epiguruk may be useful in interpreting some of the widespread subhorizontally stratified late-glacial deposits of Europe and North America.</span></p>","language":"English","publisher":"GeoScienceWorld","doi":"10.1306/D4267C12-2B26-11D7-8648000102C1865D","usgsCitation":"Ashley, G., and Hamilton, T.D., 1993, Fluvial response to late Quaternary climatic fluctuations, central Kobuk Valley, northwestern Alaska: Journal of Sedimentary Research, v. 63, no. 5, p. 814-827, https://doi.org/10.1306/D4267C12-2B26-11D7-8648000102C1865D.","productDescription":"14 p.","startPage":"814","endPage":"827","costCenters":[],"links":[{"id":371595,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United 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 \"}}]}","volume":"63","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Ashley, G.M.","contributorId":99313,"corporation":false,"usgs":true,"family":"Ashley","given":"G.M.","email":"","affiliations":[],"preferred":false,"id":780454,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hamilton, T. D.","contributorId":36921,"corporation":false,"usgs":true,"family":"Hamilton","given":"T.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":780455,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70039262,"text":"70039262 - 1993 - Permafrost","interactions":[],"lastModifiedDate":"2012-08-04T01:01:57","indexId":"70039262","displayToPublicDate":"1993-01-01T15:04:00","publicationYear":"1993","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":362,"text":"General Information Product","active":false,"publicationSubtype":{"id":6}},"title":"Permafrost","docAbstract":"In 1577, on his second voyage to the New World in search of the Northwest Passage, Sir Martin Frobisher reported finding ground in the far north that was frozen to depths of \"four or five fathoms, even in summer,\" and that the frozen condition \"so combineth the stones together that scarcely instruments with great force can unknit them.\" This permanently frozen ground, now termed permafrost, underlies perhaps a fifth of the Earth's land surface. It occurs in Antarctica but is most extensive in the Northern Hemisphere. In the lands surrounding the Arctic Ocean, its maximum thickness has been reported in thousands of feet as much as 5,000 feet in Siberia and 2,000 feet in northern Alaska.","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/70039262","usgsCitation":"Ray, L.L., 1993, Permafrost: General Information Product, 15 p., https://doi.org/10.3133/70039262.","productDescription":"15 p.","numberOfPages":"8","costCenters":[],"links":[{"id":261504,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gip/70039262/report.pdf"},{"id":261505,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gip/70039262/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a76a0e4b0c8380cd78214","contributors":{"authors":[{"text":"Ray, Louis L.","contributorId":48527,"corporation":false,"usgs":true,"family":"Ray","given":"Louis","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":465883,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70209661,"text":"70209661 - 1993 - Sulfidization and magnetization above hydrocarbon reservoirs","interactions":[],"lastModifiedDate":"2020-04-20T16:18:40.96928","indexId":"70209661","displayToPublicDate":"1993-01-01T11:11:51","publicationYear":"1993","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"chapter":"13","title":"Sulfidization and magnetization above hydrocarbon reservoirs","docAbstract":"<p><span>Post-depositional iron-sulfide (Fe-S) minerals that are related to hydrocarbon seepage have changed the original magnetizations at Cement oil field (Anadarko basin, Oklahoma), at Simpson oil field (North Slope basin, Alaska), and above deep Cretaceous oil and gas reservoirs, south Texas coastal plain. At Cement, ferrimagnetic pyrrhotite (Fe</span><sub>7</sub><span>S</span><sub>8</sub><span>) formed with pyrite and marcasite in Permian red beds. The Fe-S minerals contain sulfur from two sources: (1) abiogenic sulfide, which has positive δ</span><sup>34</sup><span>S values, derived from thermochemical reduction of sulfate in deep reservoirs; and (2) biogenic sulfide, which has negative δ</span><sup>34</sup><span>S values, produced by reactions mediated by sulfate-reducing bacteria fed by leaking hydrocarbons. At Simpson, ferrimagnetic greigite (Fe</span><sub>3</sub><span>S</span><sub>4</sub><span>) dominates magnetizations in nonmarine Upper Cretaceous clastic beds that contain epigenetic sulfide (δ</span><sup>34</sup><span>S &gt; +20 per mil) and seeping biodegraded oil. In this setting, the authigenic magnetic sulfide mineral apparently incorporated sulfide produced by bacterial sulfate reduction under limited sulfate conditions. An inferred hydrocarbon food source for the sulfate-reducing bacteria links the hydrocarbon seepage to the greigite. The greigite is perhaps forming today. In middle Tertiary sandstones of southeast Texas, pyrite and marcasite formed when abiogenic H</span><sub>2</sub><span>S (enriched in&nbsp;</span><sup>34</sup><span>S) migrated upward from deep reservoirs, or when H</span><sub>2</sub><span>S (depleted in&nbsp;</span><sup>34</sup><span>S) was produced at shallow depths by bacteria that used organic material dissolved in migrating water from depth. The pyrite and marcasite replaced detrital magnetic iron-titanium oxide minerals. The degree of such replacement appears to increase toward faults that connect deep petroleum reservoirs to shallow sandstone. Our results show that abiologic and biologic mechanisms can generate different magnetic sulfide minerals in some sulfidic zones of hydrocarbon seepage. More commonly the magnetizations in such zones would be diminished as a result of the replacement of detrital magnetic minerals by the common nonmagnetic sulfide minerals, or would remain unchanged if such detrital minerals were originally absent.</span></p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Applications of Paleomagnetism to Sedimentary Geology","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"SEPM, Society for Sedimentary Geology","doi":"10.2110/pec.93.49.0167","usgsCitation":"Reynolds, R.L., Goldhaber, M.B., and Tuttle, M., 1993, Sulfidization and magnetization above hydrocarbon reservoirs, chap. 13 <i>of</i> Applications of Paleomagnetism to Sedimentary Geology, v. 19, p. 167-179, https://doi.org/10.2110/pec.93.49.0167.","productDescription":"13 p.","startPage":"167","endPage":"179","costCenters":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"links":[{"id":374117,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"","state":"","otherGeospatial":"","volume":"19","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Reynolds, Richard L. 0000-0002-4572-2942 rreynolds@usgs.gov","orcid":"https://orcid.org/0000-0002-4572-2942","contributorId":139068,"corporation":false,"usgs":true,"family":"Reynolds","given":"Richard","email":"rreynolds@usgs.gov","middleInitial":"L.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":787428,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Goldhaber, Martin B. 0000-0002-1785-4243 mgold@usgs.gov","orcid":"https://orcid.org/0000-0002-1785-4243","contributorId":1339,"corporation":false,"usgs":true,"family":"Goldhaber","given":"Martin","email":"mgold@usgs.gov","middleInitial":"B.","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":787429,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Tuttle, Michele L. mtuttle@usgs.gov","contributorId":1028,"corporation":false,"usgs":true,"family":"Tuttle","given":"Michele L.","email":"mtuttle@usgs.gov","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":false,"id":787430,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70007017,"text":"70007017 - 1993 - Decline of spectacled eiders nesting in western Alaska","interactions":[],"lastModifiedDate":"2023-08-14T14:38:35.449206","indexId":"70007017","displayToPublicDate":"1993-01-01T10:53:08","publicationYear":"1993","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":894,"text":"Arctic","active":true,"publicationSubtype":{"id":10}},"title":"Decline of spectacled eiders nesting in western Alaska","docAbstract":"<p><span>Spectacled eider (</span><i>Somateria fischeri</i><span>) populations in western Alaska are now less than 4% of the numbers estimated in the early 1970s. In 1992, an estimated 1721 nesting pairs remained on the Yukon-Kuskokwim Delta. Causes of this rapid and continuing decline of -14% per year are undocumented. Many aspects of spectacled eider biology remain unknown, including their marine foraging habitats, food items, migratory movements, and population ecology. A review of some biological characteristics and possible threats to the species suggests the importance of quantifying potential impacts from parasites and disease, subsistence harvest, predation during brood rearing, and alteration of Bering Sea food resources. Factors causing the population decline of spectacled eiders must be determined and appropriate actions taken to reverse the trend.</span></p>","language":"English","publisher":"Arctic Institute of North America","doi":"10.14430/arctic1352","usgsCitation":"Stehn, R.A., Dau, C.P., Conant, B., and Butler, W.I., 1993, Decline of spectacled eiders nesting in western Alaska: Arctic, v. 46, no. 3, p. 264-277, https://doi.org/10.14430/arctic1352.","productDescription":"14 p.","startPage":"264","endPage":"277","numberOfPages":"14","costCenters":[{"id":106,"text":"Alaska Biological Science Center","active":false,"usgs":true}],"links":[{"id":490003,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.14430/arctic1352","text":"Publisher Index Page"},{"id":259636,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -152.4512005405596,\n              72.39757971920909\n            ],\n            [\n              -179.9,\n              70.82632744683283\n            ],\n            [\n              -179.9,\n              49.65359199648461\n            ],\n            [\n              -147.94187276411182,\n              57.70908567575026\n            ],\n            [\n              -152.4512005405596,\n              72.39757971920909\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"46","issue":"3","noUsgsAuthors":false,"publicationDate":"1993-01-01","publicationStatus":"PW","scienceBaseUri":"5059fe0ce4b0c8380cd4eaba","contributors":{"authors":[{"text":"Stehn, Robert A.","contributorId":83986,"corporation":false,"usgs":true,"family":"Stehn","given":"Robert","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":355678,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dau, Christian P.","contributorId":26185,"corporation":false,"usgs":true,"family":"Dau","given":"Christian","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":355676,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Conant, Bruce","contributorId":37596,"corporation":false,"usgs":true,"family":"Conant","given":"Bruce","affiliations":[],"preferred":false,"id":355677,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Butler, William I. Jr.","contributorId":105584,"corporation":false,"usgs":true,"family":"Butler","given":"William","suffix":"Jr.","email":"","middleInitial":"I.","affiliations":[],"preferred":false,"id":355679,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70017868,"text":"70017868 - 1993 - Petrology and isotopic composition of Quaternary basanites dredged from the Bering Sea continental margin near Navarin Basin","interactions":[],"lastModifiedDate":"2023-09-21T16:20:46.35207","indexId":"70017868","displayToPublicDate":"1993-01-01T00:00:00","publicationYear":"1993","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1168,"text":"Canadian Journal of Earth Sciences","active":true,"publicationSubtype":{"id":10}},"title":"Petrology and isotopic composition of Quaternary basanites dredged from the Bering Sea continental margin near Navarin Basin","docAbstract":"<p><span>Quaternary basanites were recovered from shallow water depth from the continental margin of the Bering Sea (58°39.0′N, 177°12.9′W) near Navarin Basin. The basanites are highly vesicular flow rock and hyaloclastites similar to other alkalic volcanic rocks erupted repeatedly during the late Cenozoic on islands in the Bering Sea region and in mainland Alaska. K–Ar ages for the basanites indicate at least two episodes of volcanism at about 1.1 and 0.4 Ma. Similar alkalic volcanism occurred sporadically at geographically widely separated centers in the Bering Sea region for at least the past 6 Ma. Chemically, these alkalic lavas are intraplate basalts similar to those erupted from oceanic islands and in some continental settings. Trace-element data indicate these alkalic lavas have been generated by small, but variable, amounts of partial melting of a meta-somatized lherzolite source. The relatively primitive compositions (MgO &gt; 9%), presence of mantle-derived xenoliths in some alkalic lavas, and presence of forsteritic olivine with low CaO and high NiO suggest that magma rose rapidly from greath depth without spending time in large, long-lived magma chambers. Although lavas from different volcanic centers in the Bering Sea region are similar with respect to major elements and many trace-element ratios, isotopic compositions indicate heterogeneities in the source. The Navarin basanites have higher&nbsp;</span><sup>87</sup><span>Sr/</span><sup>86</sup><span>Sr and lower&nbsp;</span><sup>143</sup><span>Nd/</span><sup>144</sup><span>Nd values than any other lavas so far reported from this region. The&nbsp;</span><sup>207</sup><span>Pb/</span><sup>204</sup><span>Pb isotopic ratios indicate involvement of a crustal component, which may have resulted from metasomatism associated with subduction-related magmatic activity during the Early Eocene in this region. Although some volcanic episodes appear to have occurred roughly synchronously at geographically widely separated centers, no large-scale regional extension nor presence of large mantle plumes are indicated. Instead, alkalic volcanism apparently resulted from upwelling and decompressional melting of small isolated mantle diapirs in response to local lithospheric attenuation associated with jostling of blocks during adjustment to regional stresses.</span></p>","language":"English","publisher":"Canadian Science Publishing","doi":"10.1139/e93-081","issn":"00084077","usgsCitation":"Davis, A.S., Gunn, S., Gray, L., Marlow, M.S., and Wong, F.L., 1993, Petrology and isotopic composition of Quaternary basanites dredged from the Bering Sea continental margin near Navarin Basin: Canadian Journal of Earth Sciences, v. 30, no. 5, p. 975-984, https://doi.org/10.1139/e93-081.","productDescription":"10 p.","startPage":"975","endPage":"984","costCenters":[],"links":[{"id":228586,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Russia, United States","state":"Alaska","otherGeospatial":"Bering Sea, Navarin Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -161.02644563755487,\n              64.01937447302842\n            ],\n            [\n              -185.30270672550836,\n              64.01937447302842\n            ],\n            [\n              -185.30270672550836,\n              53.06258501763452\n            ],\n            [\n              -161.02644563755487,\n              53.06258501763452\n            ],\n            [\n              -161.02644563755487,\n              64.01937447302842\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"30","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a7823e4b0c8380cd78649","contributors":{"authors":[{"text":"Davis, A. S.","contributorId":41424,"corporation":false,"usgs":true,"family":"Davis","given":"A.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":377796,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gunn, S.H.","contributorId":65236,"corporation":false,"usgs":true,"family":"Gunn","given":"S.H.","email":"","affiliations":[],"preferred":false,"id":377797,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gray, L.-B.","contributorId":10171,"corporation":false,"usgs":true,"family":"Gray","given":"L.-B.","email":"","affiliations":[],"preferred":false,"id":377795,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Marlow, M. S.","contributorId":76743,"corporation":false,"usgs":true,"family":"Marlow","given":"M.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":377798,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Wong, F. L.","contributorId":87515,"corporation":false,"usgs":true,"family":"Wong","given":"F.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":377799,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70017738,"text":"70017738 - 1993 - Methane in permafrost - Preliminary results from coring at Fairbanks, Alaska","interactions":[],"lastModifiedDate":"2012-03-12T17:19:54","indexId":"70017738","displayToPublicDate":"1993-01-01T00:00:00","publicationYear":"1993","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Methane in permafrost - Preliminary results from coring at Fairbanks, Alaska","docAbstract":"Permafrost has been suggested as a high-latitude source of methane (a greenhouse gas) during global warming. To begin to assess the magnitude of this source, we have examined the methane content of permafrost in samples from shallow cores (maximum depth, 9.5m) at three sites in Fairbanks, Alaska, where discontinuous permafrost is common. These cores sampled frozen loess, peat, and water (ice) below the active layer. Methane contents of permafrost range from <0.001 to 22.2mg/kg of sample. The highest methane content of 22.2mg/kg was found in association with peat at one site. Silty loess had high methane contents at each site of 6.56, 4.24, and 0.152mg/kg, respectively. Carbon isotopic compositions of the methane (??13C) ranged from -70.8 to -103.9 ???, and hydrogen isotopic compositions of the methane (??D) from -213 to -313 ???, indicating that the methane is microbial in origin. The methane concentrations were used in a one dimensional heat conduction model to predict the amount of methane that will be released from permafrost worldwide over the next 100 years, given two climate change scenarios. Our results indicate that at least 30 years will elapse before melting permafrost releases important amounts of methane; a maximum methane release rate will be about 25 to 30 Tg/yr, assuming that methane is generally distributed in shallow permafrost as observed in our samples.","largerWorkTitle":"Chemosphere","language":"English","issn":"00456535","usgsCitation":"Kvenvolden, K., and Lorenson, T., 1993, Methane in permafrost - Preliminary results from coring at Fairbanks, Alaska, <i>in</i> Chemosphere, v. 26, no. 1-4, p. 609-616.","startPage":"609","endPage":"616","numberOfPages":"8","costCenters":[],"links":[{"id":228947,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"26","issue":"1-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a552fe4b0c8380cd6d162","contributors":{"authors":[{"text":"Kvenvolden, K.A.","contributorId":80674,"corporation":false,"usgs":true,"family":"Kvenvolden","given":"K.A.","email":"","affiliations":[],"preferred":false,"id":377419,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lorenson, T.D.","contributorId":7715,"corporation":false,"usgs":true,"family":"Lorenson","given":"T.D.","email":"","affiliations":[],"preferred":false,"id":377418,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":87165,"text":"87165 - 1993 - Annual and Spatial Variation of the Kelp Forest Fish Assemblage at San Nicolas Island, California","interactions":[],"lastModifiedDate":"2018-12-21T13:27:10","indexId":"87165","displayToPublicDate":"1993-01-01T00:00:00","publicationYear":"1993","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Annual and Spatial Variation of the Kelp Forest Fish Assemblage at San Nicolas Island, California","docAbstract":"<p>The kelp forest fishes of San Nicolas Island, California were studied from 1981-1986 to examine the causes of among-site and among-year variation in the fish assemblages. Fish counts and seven physical and biological variables were recorded at six sites around the island every spring and fall. Over the study period, a total of 45 fish species from 18 families were recorded, though members of nive families dominated at all sites. Among-site variation was considereable with two sites on the south side of the island having two to four times as many non-schooling fishes as the other four sites. Three variables, based on stepwise multiple regression techniques, were important predictors of site-specific fish abundance: 1) vertical relief; 2) sand cover and 3) understory algal cover. The total number of fishes varied interannually by a factor of three. Due to recruitment occuring each spring, there was a strong seasonal component to the variation in fish abundance. The extent of seasonal and interannual variaton of fish abundance is an indication of the variable nature of recruitment to this area. Over the 6 yr period, there were three distinct groupings of fish assemblages correspondong to pre- (Fall 1981 - Fall 1982), during spring (Spring 1983 - Spring 1984) and post El Nino (Fall 1984 - Fall 1986) sampling dates. During El Nino sampling period, there was considerable recruitment of southern affinity fish species, increasing both the abundance and diversity of the fish assemblages. Large-scale oceanographic processes, coupled with site-specific features of the reef habitat, produce a moderately diverse, though relatively abundant fish fauna at San Nicolas Island.</p>","largerWorkTitle":"Third California Islands Symposium","conferenceTitle":"Third California Islands Symposium","language":"English","usgsCitation":"Cowen, R., and Bodkin, J.L., 1993, Annual and Spatial Variation of the Kelp Forest Fish Assemblage at San Nicolas Island, California, <i>in</i> Third California Islands Symposium, p. 463-473.","productDescription":"11 p.","startPage":"463","endPage":"473","numberOfPages":"11","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":128089,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"San Nicolas Island","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -119.57794189453125,\n              33.284619968887704\n            ],\n            [\n              -119.56146240234375,\n              33.274861346151496\n            ],\n            [\n              -119.54566955566406,\n              33.28519397154413\n            ],\n            [\n              -119.53056335449219,\n              33.28691595686207\n            ],\n            [\n              -119.4934844970703,\n              33.271990955382115\n            ],\n            [\n              -119.46876525878906,\n              33.267398133880754\n            ],\n            [\n              -119.43031311035155,\n              33.246153192679756\n            ],\n            [\n              -119.42619323730469,\n              33.22605187269161\n            ],\n            [\n              -119.44473266601561,\n              33.211116472416855\n            ],\n            [\n              -119.48043823242189,\n              33.205945932210035\n            ],\n            [\n              -119.52438354492186,\n              33.2139888627714\n            ],\n            [\n              -119.54841613769531,\n              33.22432868739248\n            ],\n            [\n              -119.57382202148439,\n              33.24213329838942\n            ],\n            [\n              -119.58137512207031,\n              33.26280507083056\n            ],\n            [\n              -119.57794189453125,\n              33.284619968887704\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67bc24","contributors":{"authors":[{"text":"Cowen, R.J.","contributorId":71119,"corporation":false,"usgs":true,"family":"Cowen","given":"R.J.","email":"","affiliations":[],"preferred":false,"id":297462,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bodkin, James L. 0000-0003-1641-4438 jbodkin@usgs.gov","orcid":"https://orcid.org/0000-0003-1641-4438","contributorId":748,"corporation":false,"usgs":true,"family":"Bodkin","given":"James","email":"jbodkin@usgs.gov","middleInitial":"L.","affiliations":[{"id":116,"text":"Alaska Science Center Biology MFEB","active":true,"usgs":true},{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"preferred":true,"id":297461,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70017883,"text":"70017883 - 1993 - Natural gas hydrates of the Prudhoe Bay and Kuparuk River area, North Slope, Alaska","interactions":[],"lastModifiedDate":"2023-01-19T18:00:20.943182","indexId":"70017883","displayToPublicDate":"1993-01-01T00:00:00","publicationYear":"1993","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":701,"text":"American Association of Petroleum Geologists Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Natural gas hydrates of the Prudhoe Bay and Kuparuk River area, North Slope, Alaska","docAbstract":"<p>Gas hydrates are crystalline substances composed of water and gas, mainly methane, in which a solid-water lattice accommodates gas molecules in a cage-like structure, or clathrate. These substances commonly have been regarded as a potential unconventional source of natural gas because of their enormous gas-storage capacity. Significant quantities of naturally occurring gas hydrates have been detected in many regions of the Arctic, including Siberia, the Mackenzie River Delta, and the North Slope of Alaska. On the North Slope, the methane-hydrate stability zone is areally extensive beneath most of the coastal plain province and has thicknesses greater than 1000 m in the Prudhoe Bay area.</p><p>Gas hydrates have been inferred to occur in 50 North Slope exploratory and production wells on the basis of well-log responses calibrated to the response of an interval in a well where gas hydrates were recovered in a core by ARCO and Exxon. Most North Slope gas hydrates occur in six laterally continuous lower Tertiary sandstones and conglomerates; all these gas hydrates are geographically restricted to the area overlying the eastern part of the Kuparuk River oil field and the western part of the Prudhoe Bay oil field. The volume of gas within these gas hydrates is estimated to be about 1.0 × 10<sup>12</sup><span>&nbsp;</span>to 1.2 × 10<sup>12</sup><span>&nbsp;</span>m<sup>3</sup><span>&nbsp;</span>(37 to 44 tcf), or about twice the volume of conventional gas in the Prudhoe Bay field.</p><p>Geochemical analyses of well samples suggest that the inferred hydrates probably contain a mixture of deep-source thermogenic gas and shallow, microbial gas that was either directly converted to gas hydrate or first concentrated in existing traps and later converted to gas hydrate. The thermogenic gas probably migrated from deeper reservoirs along the same faults thought to have been migration pathways for the large volumes of heavy oil that occur in the shallow reservoirs of this area.</p>","language":"English","publisher":"American Association of Petroleum Geologists","doi":"10.1306/BDFF8D62-1718-11D7-8645000102C1865D","usgsCitation":"Collett, T.S., 1993, Natural gas hydrates of the Prudhoe Bay and Kuparuk River area, North Slope, Alaska: American Association of Petroleum Geologists Bulletin, v. 77, no. 5, p. 793-812, https://doi.org/10.1306/BDFF8D62-1718-11D7-8645000102C1865D.","productDescription":"20 p.","startPage":"793","endPage":"812","numberOfPages":"20","costCenters":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"links":[{"id":228779,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Kuparuk River area, North Slope, Prudhoe Bay","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -141,\n              72\n            ],\n            [\n              -168,\n              72\n            ],\n            [\n              -168,\n              68\n            ],\n            [\n              -141,\n              68\n            ],\n            [\n              -141,\n              72\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"77","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a6304e4b0c8380cd72251","contributors":{"authors":[{"text":"Collett, Timothy S. 0000-0002-7598-4708 tcollett@usgs.gov","orcid":"https://orcid.org/0000-0002-7598-4708","contributorId":1698,"corporation":false,"usgs":true,"family":"Collett","given":"Timothy","email":"tcollett@usgs.gov","middleInitial":"S.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true},{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true},{"id":255,"text":"Energy Resources Program","active":true,"usgs":true},{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":377831,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1012816,"text":"1012816 - 1993 - Autumn diet of lesser snow geese staging in northeastern Alaska","interactions":[],"lastModifiedDate":"2024-12-04T16:58:01.644744","indexId":"1012816","displayToPublicDate":"1993-01-01T00:00:00","publicationYear":"1993","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2508,"text":"Journal of Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"Autumn diet of lesser snow geese staging in northeastern Alaska","docAbstract":"<p>The coastal plain of the Arctic National Wildlife Refuge (ANWR) is used by lesser snow geese (<i>Chen caerulescens caerulescens</i>) in autumn for premigratory staging. To better understand the potential impacts of human disturbance on snow geese, we investigated species composition of, and temporal and age-related variation in, their diet during staging. Depending on age and time of collection, between 35.2 and 94.1% of the diet (aggregate percent wet mass, <i>n</i> = 75) consisted of 2 species of plants; underground stems of tall cotton-grass (<i>Eriophorum angustifolium</i>), and aerial shoots of northern scouring rush (<i>Equisetum variegatum</i>). The diet varied between August and September (<i>P</i> = 0.0089), morning and afternoon (<i>P</i> &lt; 0.0001), but not between age classes (<i>P</i> = 0.066). Throughout staging, snow geese consumed more tall cotton-grass during the afternoon than during the morning (<i>P</i> &lt; 0.05). Tall cotton-grass was a larger component of the afternoon diet in September than in August (<i>P</i> &lt; 0.05). In September, snow geese consumed more northern scouring rush in the mornings than in the afternoon (<i>P</i> &lt; 0.05). Nighttime freezing, interspecific differences in nutritional quality, and plant senescence likely constrained the diet of snow geese to a small number of food items. Because alternative foods may not be available, human disturbance should be minimized in areas that provide these forage species.</p>","language":"English","publisher":"Wiley","doi":"10.2307/3809000","usgsCitation":"Brackney, A.W., and Hupp, J.W., 1993, Autumn diet of lesser snow geese staging in northeastern Alaska: Journal of Wildlife Management, v. 57, no. 1, p. 55-61, https://doi.org/10.2307/3809000.","productDescription":"7 p.","startPage":"55","endPage":"61","costCenters":[{"id":106,"text":"Alaska Biological Science Center","active":false,"usgs":true}],"links":[{"id":128557,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Canada, United States","state":"Alaska","otherGeospatial":"Arctic National Wildlife Refuge","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -144.6585941797466,\n              70.27784922631818\n            ],\n            [\n              -144.6585941797466,\n              69.20794411165741\n            ],\n            [\n              -140.73936785309067,\n              69.20794411165741\n            ],\n            [\n              -140.73936785309067,\n              70.27784922631818\n            ],\n            [\n              -144.6585941797466,\n              70.27784922631818\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"57","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa9e4b07f02db66809f","contributors":{"authors":[{"text":"Brackney, Alan W.","contributorId":60982,"corporation":false,"usgs":true,"family":"Brackney","given":"Alan","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":318397,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hupp, Jerry W. 0000-0002-6439-3910 jhupp@usgs.gov","orcid":"https://orcid.org/0000-0002-6439-3910","contributorId":127803,"corporation":false,"usgs":true,"family":"Hupp","given":"Jerry","email":"jhupp@usgs.gov","middleInitial":"W.","affiliations":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":117,"text":"Alaska Science Center Biology WTEB","active":true,"usgs":true}],"preferred":true,"id":318396,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70018274,"text":"70018274 - 1993 - Subsurface temperatures and geothermal gradients on the north slope of Alaska","interactions":[],"lastModifiedDate":"2023-09-08T16:51:39.977751","indexId":"70018274","displayToPublicDate":"1993-01-01T00:00:00","publicationYear":"1993","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1264,"text":"Cold Regions Science and Technology","active":true,"publicationSubtype":{"id":10}},"title":"Subsurface temperatures and geothermal gradients on the north slope of Alaska","docAbstract":"<p><span>On the North Slope of Alaska, geothermal gradient data are available from high-resolution, equilibrated well-bore surveys and from estimates based on well-log identification of the base of ice-bearing permafrost. A total of 46 North Slope wells, considered to be in or near thermal equilibrium, have been surveyed with high-resolution temperatures devices and geothermal gradients can be interpreted directly from these recorded temperature profiles. To augment the limited North Slope temperature data base, a new method of evaluating local geothermal gradients has been developed. In this method, a series of well-log picks for the base of the ice-bearing permafrost from 102 wells have been used, along with regional temperature constants derived from the high-resolution stabilized well-bore temperature surveys, to project geothermal gradients. Geothermal gradients calculated from the high-resolution temperature surveys generally agree with those projected from known ice-bearing permafrost depths over most of the North Slope. Values in the ice-bearing permafrost range from&nbsp;</span><span class=\"math\"><span id=\"MathJax-Element-1-Frame\" class=\"MathJax_SVG\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;><mtext>&amp;#x2248;</mtext><mtext>1.5&amp;#xB0;</mtext><mtext>C</mtext><mtext>100</mtext><mtext>m</mtext></math>\"><span class=\"MJX_Assistive_MathML\">≈1.5°C100m</span></span></span><span>&nbsp;in the Prudhoe Bay area to&nbsp;</span><span class=\"math\"><span id=\"MathJax-Element-2-Frame\" class=\"MathJax_SVG\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;><mtext>&amp;#x2248;</mtext><mtext>4.5&amp;#x3B4;</mtext><mtext>C</mtext><mtext>100</mtext><mtext>m</mtext></math>\"><span class=\"MJX_Assistive_MathML\">≈4.5<i>δ</i>C100m</span></span></span><span>&nbsp;in the east-central portion of the National Petroleum Reserve in Alaska. Geothermal gradients below the ice-bearing permafrost sequence range from&nbsp;</span><span class=\"math\"><span id=\"MathJax-Element-3-Frame\" class=\"MathJax_SVG\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;><mtext>&amp;#x2248;</mtext><mtext>1.6&amp;#xB0;</mtext><mtext>C</mtext><mtext>100</mtext><mtext>m</mtext></math>\"><span class=\"MJX_Assistive_MathML\">≈1.6°C100m</span></span></span><span>&nbsp;to&nbsp;</span><span class=\"math\"><span id=\"MathJax-Element-4-Frame\" class=\"MathJax_SVG\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;><mtext>&amp;#x2248;</mtext><mtext>5.2&amp;#xB0;</mtext><mtext>C</mtext><mtext>100</mtext><mtext>m</mtext></math>\"><span class=\"MJX_Assistive_MathML\">≈5.2°C100m</span></span></span><span>.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0165-232X(93)90071-F","usgsCitation":"Collett, T.S., Bird, K.J., and Magoon, L.B., 1993, Subsurface temperatures and geothermal gradients on the north slope of Alaska: Cold Regions Science and Technology, v. 21, no. 3, p. 275-293, https://doi.org/10.1016/0165-232X(93)90071-F.","productDescription":"19 p.","startPage":"275","endPage":"293","numberOfPages":"19","costCenters":[{"id":255,"text":"Energy Resources Program","active":true,"usgs":true},{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":227020,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -166.7096068686938,\n              71.69388395024325\n            ],\n            [\n              -167.08712006649446,\n              65.87803877813585\n            ],\n            [\n              -143.90675430350967,\n              65.87803877813585\n            ],\n            [\n              -143.85405574285585,\n              70.95363676700768\n            ],\n            [\n              -166.7096068686938,\n              71.69388395024325\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"21","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b9d90e4b08c986b31d909","contributors":{"authors":[{"text":"Collett, Timothy S. 0000-0002-7598-4708 tcollett@usgs.gov","orcid":"https://orcid.org/0000-0002-7598-4708","contributorId":1698,"corporation":false,"usgs":true,"family":"Collett","given":"Timothy","email":"tcollett@usgs.gov","middleInitial":"S.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true},{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true},{"id":255,"text":"Energy Resources Program","active":true,"usgs":true},{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":379068,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bird, Kenneth J. kbird@usgs.gov","contributorId":1015,"corporation":false,"usgs":true,"family":"Bird","given":"Kenneth","email":"kbird@usgs.gov","middleInitial":"J.","affiliations":[{"id":255,"text":"Energy Resources Program","active":true,"usgs":true}],"preferred":true,"id":379067,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Magoon, Leslie B. lmagoon@usgs.gov","contributorId":2383,"corporation":false,"usgs":true,"family":"Magoon","given":"Leslie","email":"lmagoon@usgs.gov","middleInitial":"B.","affiliations":[],"preferred":true,"id":379066,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70018300,"text":"70018300 - 1993 - Hydrocarbons in oil residues on beaches of islands of Prince William Sound, Alaska","interactions":[],"lastModifiedDate":"2012-03-12T17:19:23","indexId":"70018300","displayToPublicDate":"1993-01-01T00:00:00","publicationYear":"1993","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2676,"text":"Marine Pollution Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Hydrocarbons in oil residues on beaches of islands of Prince William Sound, Alaska","docAbstract":"Aliphatic and aromatic hydrocarbons were measured on oil residues from beaches on six islands in Prince William Sound, Alaska. In addition to altered products from the Exxon Valdez oil spill of 1989, we also found, at two widely separated locations, residues that are similar to each other but chemically distinct from the spilled oil. Terpanes, steranes, monoaromatic steranes, and carbon isotopic compositions of total extracts were most useful in correlating the altered products of the spilled oil. These same parameters revealed that the two non-Valdez samples are likely residues of oil originally produced in California. The results indicate that oil residues currently on the beaches of this estuary have at least two quite different origins.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Marine Pollution Bulletin","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/0025-326X(93)90593-9","issn":"0025326X","usgsCitation":"Kvenvolden, K., Hostettler, F., Rapp, J.B., and Carlson, P., 1993, Hydrocarbons in oil residues on beaches of islands of Prince William Sound, Alaska: Marine Pollution Bulletin, v. 26, no. 1, p. 24-29, https://doi.org/10.1016/0025-326X(93)90593-9.","startPage":"24","endPage":"29","numberOfPages":"6","costCenters":[],"links":[{"id":487291,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1016/0025-326x(93)90593-9","text":"Publisher Index Page"},{"id":205905,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0025-326X(93)90593-9"},{"id":227376,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"26","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3328e4b0c8380cd5ed98","contributors":{"authors":[{"text":"Kvenvolden, K.A.","contributorId":80674,"corporation":false,"usgs":true,"family":"Kvenvolden","given":"K.A.","email":"","affiliations":[],"preferred":false,"id":379158,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hostettler, F. D.","contributorId":99563,"corporation":false,"usgs":true,"family":"Hostettler","given":"F. D.","affiliations":[],"preferred":false,"id":379160,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rapp, J. B.","contributorId":28987,"corporation":false,"usgs":true,"family":"Rapp","given":"J.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":379157,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Carlson, P.R.","contributorId":97055,"corporation":false,"usgs":true,"family":"Carlson","given":"P.R.","email":"","affiliations":[],"preferred":false,"id":379159,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70017951,"text":"70017951 - 1993 - Possible connection between two Alaskan catastrophes occurring 25 yr apart (1964 and 1989)","interactions":[],"lastModifiedDate":"2024-01-22T13:09:53.499859","indexId":"70017951","displayToPublicDate":"1993-01-01T00:00:00","publicationYear":"1993","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1796,"text":"Geology","active":true,"publicationSubtype":{"id":10}},"title":"Possible connection between two Alaskan catastrophes occurring 25 yr apart (1964 and 1989)","docAbstract":"<div id=\"15575616\" class=\"article-section-wrapper js-article-section js-content-section  \" data-section-parent-id=\"0\"><p>On March 24, 1989, the<span>&nbsp;</span><i>Exxon Valdez</i><span>&nbsp;</span>supertanker grounded on Bligh Reef, spilling North Slope crude oil into Prince William Sound, Alaska. Tracking the geochemical fate of this spilled oil has revealed, in addition to weathered products from the spill, minor oil residues on beaches from a distinctly different source. By using carbon isotopic compositions of whole-oil residues as a principal method of identification, we found that the δ<sup>13</sup>C values of<span>&nbsp;</span><i>Exxon Valdez</i><span>&nbsp;</span>oil (one sample) and its residues (eight samples from six islands) average -29.3 ±0.1‰. In contrast, the non-<i>Exxon Valdez</i><span>&nbsp;</span>residues (15 samples from 12 localities) have an average δ<sup>13</sup>C value of -23.8 ±0.1‰. This tight distribution of carbon isotopic values suggests a single event to explain the non-<i>Exxon Valdez</i><span>&nbsp;</span>residues. This event likely was the Great Alaska Earthquake of March 27, 1964. This quake and the subsequent tsunami destroyed asphalt storage facilities at the old Valdez town site, spilling asphalt (δ<sup>13</sup>C = -23.6‰) into Port Valdez fjord. From there the asphalt apparently advanced south into the sound. Thus, the possible connection between two Alaskan catastrophes, separated by 25 yr, is found in the minor oil- like residues that continue to mark the two events on the beaches of Prince William Sound.</p></div>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0091-7613(1993)021<0813:PCBTAC>2.3.CO;2","issn":"00917613","usgsCitation":"Kvenvolden, K., Carlson, P., Threlkeld, C.N., and Warden, A., 1993, Possible connection between two Alaskan catastrophes occurring 25 yr apart (1964 and 1989): Geology, v. 21, no. 9, p. 813-816, https://doi.org/10.1130/0091-7613(1993)021<0813:PCBTAC>2.3.CO;2.","productDescription":"4 p.","startPage":"813","endPage":"816","numberOfPages":"4","costCenters":[],"links":[{"id":228961,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"21","issue":"9","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a7e13e4b0c8380cd7a313","contributors":{"authors":[{"text":"Kvenvolden, K.A.","contributorId":80674,"corporation":false,"usgs":true,"family":"Kvenvolden","given":"K.A.","email":"","affiliations":[],"preferred":false,"id":378019,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Carlson, P.R.","contributorId":97055,"corporation":false,"usgs":true,"family":"Carlson","given":"P.R.","email":"","affiliations":[],"preferred":false,"id":378020,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Threlkeld, C. N.","contributorId":80271,"corporation":false,"usgs":true,"family":"Threlkeld","given":"C.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":378018,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Warden, A.","contributorId":41946,"corporation":false,"usgs":true,"family":"Warden","given":"A.","email":"","affiliations":[],"preferred":false,"id":378017,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70018382,"text":"70018382 - 1993 - Factors controlling the geochemical evolution of fumarolic encrustations, Valley of Ten Thousand Smokes, Alaska","interactions":[],"lastModifiedDate":"2012-03-12T17:19:24","indexId":"70018382","displayToPublicDate":"1993-01-01T00:00:00","publicationYear":"1993","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2499,"text":"Journal of Volcanology and Geothermal Research","active":true,"publicationSubtype":{"id":10}},"title":"Factors controlling the geochemical evolution of fumarolic encrustations, Valley of Ten Thousand Smokes, Alaska","docAbstract":"Factor and canonical correlation analysis of geochemical data from eight fossil fumaroles suggest that six major factors controlled the formation and evolution of fumarolic encrustations on the 1912 ash-flow sheet in the Valley of Ten Thousand Smokes (VTTS). The six-factor solution model explains a large proportion (low of 74% for Ni to high of 99% for Si) of the individual element data variance. Although the primary fumarolic deposits have been degraded by secondary alteration reactions and up to 75 years of weathering, the relict encrustations still preserve a signature of vapor-phase element transport. This vapor-phase transport probably occurred as halide or oxyhalide species and was significant for As, Sb and Br. At least three, and possibly four, varied temperature leaching events affected the fumarolic deposits. High-temperature gases/liquids heavily altered the ejecta glass and mineral phases adjacent to the fumarolic conduit. As the fumaroles cooled. Fe-rich acidic condensate leached the ejecta and primary fumarolic deposits and resulted in the subsequent precipitation of Fe-hydroxides and/or Fe-oxides. Low- to ambient-temperature leaching and hydration reactions generated abundant hydrated amorphous phases. Up to 87% of the individual element data variance is apparently controlled by the chemistry of the ejecta on which the relict encrustations are found. This matrix chemistry factor illustrates that the primary fumarolic minerals surrounding the active VTTS vents observed by earlier workers have been effectively removed by the dissolution reactions. Element enrichment factors calculated for the VTTS relict encrustations support the statistical factor interpretations. On the average, the relict encrustations are enriched, relative to visibly unaltered matrix protolith, in As, Br, Cr, Sb, Cu, Ni, Pb, Fe, and LOI (an indirect measure of sample H2O content). ?? 1993.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Volcanology and Geothermal Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"03770273","usgsCitation":"Kodosky, L., and Keith, T.E., 1993, Factors controlling the geochemical evolution of fumarolic encrustations, Valley of Ten Thousand Smokes, Alaska: Journal of Volcanology and Geothermal Research, v. 55, no. 3-4, p. 185-200.","startPage":"185","endPage":"200","numberOfPages":"16","costCenters":[],"links":[{"id":227247,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"55","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0ebee4b0c8380cd535de","contributors":{"authors":[{"text":"Kodosky, L.G.","contributorId":62767,"corporation":false,"usgs":true,"family":"Kodosky","given":"L.G.","email":"","affiliations":[],"preferred":false,"id":379388,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Keith, T. E. C.","contributorId":11681,"corporation":false,"usgs":true,"family":"Keith","given":"T.","email":"","middleInitial":"E. C.","affiliations":[],"preferred":false,"id":379387,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70018365,"text":"70018365 - 1993 - Late Pleistocene Vertebrates and Other Fossils from Epiguruk, Northwestern Alaska","interactions":[],"lastModifiedDate":"2012-03-12T17:19:13","indexId":"70018365","displayToPublicDate":"1993-01-01T00:00:00","publicationYear":"1993","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3218,"text":"Quaternary Research","active":true,"publicationSubtype":{"id":10}},"title":"Late Pleistocene Vertebrates and Other Fossils from Epiguruk, Northwestern Alaska","docAbstract":"Sediments exposed at Epiguruk, a large cutbank on the Kobuk River about 170 km inland from Kotzebue Sound, record multiple episodes of glacial-age alluviation followed by interstadial downcutting and formation of paleosols. Vertebrate remains from Epiguruk include mammoth, bison, caribou, an equid, a canid, arctic ground squirrel, lemmings, and voles. Radiocarbon ages of bone validated by concordant ages of peat and wood span the interval between about 37,000 and 14,000 yr B.P. The late Pleistocene pollen record is dominated by Cyperaceae, with Artemisia, Salix, Betula, and Gramineae also generally abundant. The fossil record from Epiguruk indicates that the Kobuk River valley supported tundra vegetation with abundant riparian willows during middle and late Wisconsin time. Large herbivores were present during the height of late Wisconsin glaciation as well as during its waning stage and the preceding interstadial interval. The Kobuk River valley would have been a favorable refugium for plants, animals, and possibly humans throughout the last glaciation.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Quaternary Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1006/qres.1993.1045","issn":"00335894","usgsCitation":"Hamilton, T.D., Ashley, G., Reed, K.M., and Schweger, C.E., 1993, Late Pleistocene Vertebrates and Other Fossils from Epiguruk, Northwestern Alaska: Quaternary Research, v. 39, no. 3, p. 381-389, https://doi.org/10.1006/qres.1993.1045.","startPage":"381","endPage":"389","numberOfPages":"9","costCenters":[],"links":[{"id":205822,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1006/qres.1993.1045"},{"id":226982,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"39","issue":"3","noUsgsAuthors":false,"publicationDate":"2017-01-20","publicationStatus":"PW","scienceBaseUri":"505a4508e4b0c8380cd66f9b","contributors":{"authors":[{"text":"Hamilton, T. D.","contributorId":36921,"corporation":false,"usgs":true,"family":"Hamilton","given":"T.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":379341,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ashley, G.M.","contributorId":99313,"corporation":false,"usgs":true,"family":"Ashley","given":"G.M.","email":"","affiliations":[],"preferred":false,"id":379344,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Reed, K. M.","contributorId":93888,"corporation":false,"usgs":true,"family":"Reed","given":"K.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":379343,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Schweger, C. E.","contributorId":63549,"corporation":false,"usgs":true,"family":"Schweger","given":"C.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":379342,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70018231,"text":"70018231 - 1993 - Stratigraphic Context of Old Crow Tephra, Holitna Lowland, Interior Southwest Alaska","interactions":[],"lastModifiedDate":"2016-09-14T12:16:57","indexId":"70018231","displayToPublicDate":"1993-01-01T00:00:00","publicationYear":"1993","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3218,"text":"Quaternary Research","active":true,"publicationSubtype":{"id":10}},"title":"Stratigraphic Context of Old Crow Tephra, Holitna Lowland, Interior Southwest Alaska","docAbstract":"A thick deposit of Old Crow tephra was discovered in a bluff exposure along the middle Holitna River near the Kulukbuk Hills (61??20???N latitude, 157??10???W longitude) in interior southwest Alaska. This locality is the southwesternmost-known deposit of Old Crow tephra in Alaska. Thickness and grain-size data from this site support a source volcano in the eastern Aleutian arc. Pleistocene stratigraphic sequences in the lowland are dominated by upward-fining eolian sand-sheet deposits and loess separated by organic silt. These deposits record at least two episodes of regional glaciation and an intervening nonglacial period (marine oxygen isotope stage 3, stage 5, or both). Old Crow tephra crops out near the top of the lower upward-fining eolian unit, indicating that the ash erupted near the end of an interval of periglacial eolian sedimentation. The sequence of eolian deposits that contain Old Crow tephra probably accumulated during the latter part of marine oxygen isotope stage 6, whereas the overlying eolian sequence formed during the last glaciation (stage 2). This stratigraphic position is consistent with other stratigraphic contexts for the tephra and with fission-track and thermoluminescence ages of ca. 140,000 ?? 10,000 yr B.P.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Quaternary Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1006/qres.1993.1052","issn":"00335894","usgsCitation":"Waythomas, C.F., Lea, P., and Walter, R., 1993, Stratigraphic Context of Old Crow Tephra, Holitna Lowland, Interior Southwest Alaska: Quaternary Research, v. 40, no. 1, p. 20-29, https://doi.org/10.1006/qres.1993.1052.","startPage":"20","endPage":"29","numberOfPages":"10","costCenters":[],"links":[{"id":227101,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":205850,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1006/qres.1993.1052"}],"volume":"40","issue":"1","noUsgsAuthors":false,"publicationDate":"2017-01-20","publicationStatus":"PW","scienceBaseUri":"505b98c3e4b08c986b31c128","contributors":{"authors":[{"text":"Waythomas, C. F.","contributorId":10065,"corporation":false,"usgs":true,"family":"Waythomas","given":"C.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":378935,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lea, P.D.","contributorId":96028,"corporation":false,"usgs":true,"family":"Lea","given":"P.D.","email":"","affiliations":[],"preferred":false,"id":378937,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Walter, R.C.","contributorId":26796,"corporation":false,"usgs":true,"family":"Walter","given":"R.C.","email":"","affiliations":[],"preferred":false,"id":378936,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
]}