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.contributor.alternativeName | 이희일 | - |
| dc.identifier.bibliographicCitation | 한국고생물학회 제18차 학술발표회 | - |
| dc.description.journalClass | 2 | - |
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