![(a) Sandstone classification (after Folk, 1974) and (b) clast source terrane (after Dickinson, 1985) of the Barton and Weaver peninsulas’ beaches. Beach sands of both peninsulas are classified as lithic arenite and plot in the undissected arc field. Q: total quartz; F: total feldspar [K(potash feldspar) + P(plagioclase)]; R and L: total lithic fragments](https://nrms.kisti.re.kr/bitextimages/TRKO202000008032/TRKO202000008032_250_image_1.png "(a) Sandstone classification (after Folk, 1974) and (b) clast source terrane (after Dickinson, 1985) of the Barton and Weaver peninsulas’ beaches. Beach sands of both peninsulas are classified as lithic arenite and plot in the undissected arc field. Q: total quartz; F: total feldspar [K(potash feldspar) + P(plagioclase)]; R and L: total lithic fragments")
![Map of the study region near the Larsen C on the eastern Antarctic Peninsula with swath bathymetry data. The purple circle indicates the location of core EAP13 GC16B and its accompanying box core, EAP13 BC16A (modified from Lavoie et al. [2015]). LGM extent of Larsen Ice Shelf surpasses the scope of this map](https://nrms.kisti.re.kr/bitextimages/TRKO202000008032/TRKO202000008032_537_image_1.png "Map of the study region near the Larsen C on the eastern Antarctic Peninsula with swath bathymetry data. The purple circle indicates the location of core EAP13 GC16B and its accompanying box core, EAP13 BC16A (modified from Lavoie et al. [2015]). LGM extent of Larsen Ice Shelf surpasses the scope of this map")
![Idealized thermograph illustrating the evolution of pCO2 as temperature is raised at a constant rate in a situation where the amount of autochthonous OC may be smaller than a measurable 14C sample. Gaussian modeling has been implemented (G1– G3) to represent the mixture of multiple organic components incorporated in the bulk organic sample [Rosenheim et al., 2013]. The minimum “clean” sample denotes where the lowest temperature aliquot can be taken to collect G1 component ‐ without a mixture of the G2 component](https://nrms.kisti.re.kr/bitextimages/TRKO202000008032/TRKO202000008032_540_image_1.png "Idealized thermograph illustrating the evolution of pCO2 as temperature is raised at a constant rate in a situation where the amount of autochthonous OC may be smaller than a measurable 14C sample. Gaussian modeling has been implemented (G1– G3) to represent the mixture of multiple organic components incorporated in the bulk organic sample [Rosenheim et al., 2013]. The minimum “clean” sample denotes where the lowest temperature aliquot can be taken to collect G1 component ‐ without a mixture of the G2 component")
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| 주관연구기관 | 한국해양과학기술원 Korea Institute of Ocean Science ＆ Technology |
|---|---|
| 연구책임자 | 이재일 |
| 참여연구자 | 유규철 , 이민경 , 김성한 , 문흥수 , 김기태 , 황청연 , 김소영 , 정재우 , 노연호 , 정현영 , 김효진 , 김형준 , 이인애 , 성영배 , 김부근 , 박영숙 , 김진욱 |
| 보고서유형 | 최종보고서 |
| 발행국가 | 대한민국 |
| 언어 | 한국어 |
| 발행년월 | 2020-02 |
| 과제시작연도 | 2019 |
| 주관부처 | 해양수산부 Ministry of Oceans and Fisheries |
| 등록번호 | TRKO202000008032 |
| 과제고유번호 | 1525009359 |
| 사업명 | 극지연구소운영지원(R&D)(주요사업비) |
| DB 구축일자 | 2020-07-29 |
| 키워드 | 남극.고기후.고해양.퇴적물.빙상 안정성.기후지시자.Antarctica.paleoclimatology.paleoceanography.sediment.ice sheet stability.climate proxy. |
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