Sedimentary records of paleoenvironmental changes during the last deglaciation in the Ulleung Interplain Gap, East Sea (Sea of Japan) SCIE SCOPUS
DC Field | Value | Language |
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dc.contributor.author | Bahk, JJ | - |
dc.contributor.author | Chough, SK | - |
dc.contributor.author | Jeong, KS | - |
dc.contributor.author | Han, SJ | - |
dc.date.accessioned | 2020-04-21T07:55:37Z | - |
dc.date.available | 2020-04-21T07:55:37Z | - |
dc.date.created | 2020-01-28 | - |
dc.date.issued | 2001-02 | - |
dc.identifier.issn | 0921-8181 | - |
dc.identifier.uri | https://sciwatch.kiost.ac.kr/handle/2020.kiost/5917 | - |
dc.description.abstract | The Ulleung Basin in the East Sea (Sea of Japan) is a semi-enclosed basin surrounded by shallow sills and straits. Detailed observation of X-radiographs and thin sections of core sediments from the Ulleung Interplain Gap reveals five mud facies: laminated mud, crudely laminated mud, homogeneous mud, bioturbated mud and laminated Mn-carbonate mud. The laminated and homogenous muds were most likely deposited from turbidity currents, whereas the bioturbated and crudely laminated muds were formed by pelagic/hemipelagic sedimentation under oxic and anoxic bottom-water conditions, respectively. The laminated Mn-carbonate mud occurs at the lithologic boundary between the turbidite and hemipelagic laminated mud (last glacial) and the pelagic bioturbated mud (Lateglacial to Holocene). Mn-carbonates were formed at the sediment-water interface, probably reflecting an abrupt change in bottom-water oxygenation caused by sea-level rise during the last deglaciation. Profiles of redox-sensitive elements also support an anoxic to oxic change of bottom-water conditions during this period. (C) 2001 Elsevier Science B.V. All rights reserved. | - |
dc.description.uri | 1 | - |
dc.language | English | - |
dc.publisher | ELSEVIER SCIENCE BV | - |
dc.subject | YOUNGER DRYAS EVENT | - |
dc.subject | MARINE-SEDIMENTS | - |
dc.subject | TURBIDITY CURRENTS | - |
dc.subject | LATE PLEISTOCENE | - |
dc.subject | BALTIC SEA | - |
dc.subject | BASIN | - |
dc.subject | MUDS | - |
dc.subject | CALIFORNIA | - |
dc.subject | MANGANESE | - |
dc.subject | HOLOCENE | - |
dc.title | Sedimentary records of paleoenvironmental changes during the last deglaciation in the Ulleung Interplain Gap, East Sea (Sea of Japan) | - |
dc.type | Article | - |
dc.citation.endPage | 253 | - |
dc.citation.startPage | 241 | - |
dc.citation.title | GLOBAL AND PLANETARY CHANGE | - |
dc.citation.volume | 28 | - |
dc.citation.number | 1-4 | - |
dc.contributor.alternativeName | 박장준 | - |
dc.contributor.alternativeName | 정갑식 | - |
dc.contributor.alternativeName | 한상준 | - |
dc.identifier.bibliographicCitation | GLOBAL AND PLANETARY CHANGE, v.28, no.1-4, pp.241 - 253 | - |
dc.identifier.doi | 10.1016/S0921-8181(00)00076-X | - |
dc.identifier.scopusid | 2-s2.0-0035096284 | - |
dc.identifier.wosid | 000167607300019 | - |
dc.type.docType | Article | - |
dc.description.journalClass | 1 | - |
dc.subject.keywordPlus | YOUNGER DRYAS EVENT | - |
dc.subject.keywordPlus | MARINE-SEDIMENTS | - |
dc.subject.keywordPlus | TURBIDITY CURRENTS | - |
dc.subject.keywordPlus | LATE PLEISTOCENE | - |
dc.subject.keywordPlus | BALTIC SEA | - |
dc.subject.keywordPlus | BASIN | - |
dc.subject.keywordPlus | MUDS | - |
dc.subject.keywordPlus | CALIFORNIA | - |
dc.subject.keywordPlus | MANGANESE | - |
dc.subject.keywordPlus | HOLOCENE | - |
dc.subject.keywordAuthor | Mn-carbonate | - |
dc.subject.keywordAuthor | laminated mud | - |
dc.subject.keywordAuthor | paleoceanography | - |
dc.subject.keywordAuthor | Ulleung Interplain Gap | - |
dc.relation.journalWebOfScienceCategory | Geography, Physical | - |
dc.relation.journalWebOfScienceCategory | Geosciences, Multidisciplinary | - |
dc.description.journalRegisteredClass | scie | - |
dc.description.journalRegisteredClass | scopus | - |
dc.relation.journalResearchArea | Physical Geography | - |
dc.relation.journalResearchArea | Geology | - |