Yellow Sea Foraminifera ;preliminary result for paleoclimatic and paleoenvironmental proxies
| DC Field | Value | Language |
|---|---|---|
| dc.contributor.author | 신임철 | - |
| dc.contributor.author | 이희일 | - |
| dc.contributor.author | 권원태 | - |
| dc.contributor.author | 정호상 | - |
| dc.date.accessioned | 2020-07-17T14:50:59Z | - |
| dc.date.available | 2020-07-17T14:50:59Z | - |
| dc.date.created | 2020-02-11 | - |
| dc.date.issued | 2001-11-24 | - |
| dc.identifier.uri | https://sciwatch.kiost.ac.kr/handle/2020.kiost/32678 | - |
| dc.description.abstract | The southern part of the Yellow Sea (high surface water emperature) is more stable and highly productive environment than that of the northern part. Overall, the abundance of planktonic and benthic foraminifera can be used as a proxy for the paleoclimate and paleoenvironment. | - |
| dc.description.uri | 2 | - |
| dc.language | English | - |
| dc.publisher | 한국제4기학회 | - |
| dc.relation.isPartOf | 제30차 한국제4기학회 학술발표대회 | - |
| dc.title | Yellow Sea Foraminifera ;preliminary result for paleoclimatic and paleoenvironmental proxies | - |
| dc.type | Conference | - |
| dc.citation.conferencePlace | KO | - |
| dc.citation.title | 제30차 한국제4기학회 학술발표대회 | - |
| dc.contributor.alternativeName | 이희일 | - |
| dc.identifier.bibliographicCitation | 제30차 한국제4기학회 학술발표대회 | - |
| dc.description.journalClass | 2 | - |
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