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• W1990478049 abstract "Research Article| February 01, 1978 Implications of late Neogene fresh-water sediment in the Sea of Japan Lloyd H. Burckle; Lloyd H. Burckle 1Lamont-Doherty Geological Observatory of Columbia University, Palisades, New York 10964 Search for other works by this author on: GSW Google Scholar Fumio Akiba Fumio Akiba 2Japan Petroleum Exploration Co., Ltd., 3190 Hane-Musashino, Hamura-machi, Nishitama-gun, Tokyo, Japan Search for other works by this author on: GSW Google Scholar Author and Article Information Lloyd H. Burckle 1Lamont-Doherty Geological Observatory of Columbia University, Palisades, New York 10964 Fumio Akiba 2Japan Petroleum Exploration Co., Ltd., 3190 Hane-Musashino, Hamura-machi, Nishitama-gun, Tokyo, Japan Publisher: Geological Society of America First Online: 02 Jun 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 Geological Society of America Geology (1978) 6 (2): 123–127. https://doi.org/10.1130/0091-7613(1978)6<123:IOLNFS>2.0.CO;2 Article history First Online: 02 Jun 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Lloyd H. Burckle, Fumio Akiba; Implications of late Neogene fresh-water sediment in the Sea of Japan. Geology 1978;; 6 (2): 123–127. doi: https://doi.org/10.1130/0091-7613(1978)6<123:IOLNFS>2.0.CO;2 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGeology Search Advanced Search Abstract A deep-sea piston core containing more than 3 m of sediment of freshwater origin was recovered from the northeast flank of the Yamato Bank in the central part of the Sea of Japan. We identify this layer on the basis of abundant frustules of fresh-water diatoms with no admixture of marine forms. All data indicate that the layer is in place. Micropaleontological evidence from the overlying marine sediment dates this layer as older than the early Pliocene Denticula kamtschatica zone of Koizumi. These considerations and the pollen data suggest a late Miocene age for the sediment. Possible explanations for the occurrence of this fresh-water deposit are (1) the sediment originated in a turbidity current from the Japanese mainland, (2) it represents a wind-blown deposit, (3) the Yamato Bank originated as an island (with lakes) and subsequently subsided to its present depth, (4) the Yamato Bank was originally a part of the Japanese mainland and subsequently broke off and spread westward, carrying with it continental sediment, and (5) the sediment is an in situ deposit, formed when the Sea of Japan was a fresh-water lake. Restraints imposed by topography and time tend to favor explanation 5. We realize that this fresh-water sediment may occupy the same time frame as the latest Miocene (Messinian) Mediterranean dessication. This content is PDF only. Please click on the PDF icon to access. First Page Preview Close Modal You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
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• W1990478049 title "Implications of late Neogene fresh-water sediment in the Sea of Japan" @default.
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