홀로세 동안 인도네시아 Aru섬 외해의 환경변화
DC Field | Value | Language |
---|---|---|
dc.contributor.author | Luli | - |
dc.contributor.author | Swasty | - |
dc.contributor.author | Rina | - |
dc.contributor.author | Duddy | - |
dc.contributor.author | 현상민 | - |
dc.date.accessioned | 2020-07-15T10:52:58Z | - |
dc.date.available | 2020-07-15T10:52:58Z | - |
dc.date.created | 2020-02-11 | - |
dc.date.issued | 2018-10-10 | - |
dc.identifier.uri | https://sciwatch.kiost.ac.kr/handle/2020.kiost/23072 | - |
dc.description.abstract | Aru islands is located in the eastern part of Indonesia, to the east of the Banda Sea that is known strongly influenced by the Australian winter monsoon and ENSO circulation (Figure 1). As a part of the Banda Sea, it is interesting to study the Holocene condition in this area, related to both Australian monsoon and ENSO circulation. For this study, we use the quantitative analysis of microfauna foraminifera, that has been known as a potential paleonvironmental proxy due to its sensitivity to the environmental changes. Foraminferal assemblages is studied from a 152 cm length sediment core, retrieved from position 134 | - |
dc.description.uri | 1 | - |
dc.language | English | - |
dc.publisher | ICAMG | - |
dc.relation.isPartOf | ICAMG | - |
dc.title | 홀로세 동안 인도네시아 Aru섬 외해의 환경변화 | - |
dc.title.alternative | Holocene condition off Aru and surrounding, Molucca, Indonesia, reveled from microfaunal assemblages | - |
dc.type | Conference | - |
dc.citation.conferencePlace | CC | - |
dc.citation.endPage | 1 | - |
dc.citation.startPage | 1 | - |
dc.citation.title | ICAMG | - |
dc.contributor.alternativeName | 현상민 | - |
dc.identifier.bibliographicCitation | ICAMG, pp.1 | - |
dc.description.journalClass | 1 | - |