Role of winter monsoon on the flux of planktonic foraminifera and it :implications on paleoclimatology and paleoceanography

DC Field Value Language
dc.contributor.author 신임철 -
dc.contributor.author 이희일 -
dc.contributor.author 권원태 -
dc.contributor.author 정호상 -
dc.date.accessioned 2020-07-17T14:50:36Z -
dc.date.available 2020-07-17T14:50:36Z -
dc.date.created 2020-02-11 -
dc.date.issued 2002-02-21 -
dc.identifier.uri https://sciwatch.kiost.ac.kr/handle/2020.kiost/32651 -
dc.description.abstract The onset of the winter monsoon (late October-November) is responsoble for the planktic foraminifera flux peak during November. This may help to interpret abnormally high abundance of planktic foraminifera, which has paleoclimatic and paleoenvironmental implications in the specific core intervals of the East Sea. -
dc.description.uri 2 -
dc.language English -
dc.publisher 한국고생물학회 -
dc.relation.isPartOf 한국고생물학회 제18차 학술발표회 -
dc.title Role of winter monsoon on the flux of planktonic foraminifera and it :implications on paleoclimatology and paleoceanography -
dc.type Conference -
dc.citation.conferencePlace KO -
dc.citation.title 한국고생물학회 제18차 학술발표회 -
dc.identifier.bibliographicCitation 한국고생물학회 제18차 학술발표회 -
dc.description.journalClass 2 -
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Marine Resources Research Division > Deep-sea Mineral Resources Research Center > 2. Conference Papers
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