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NTIS 바로가기한국지구과학회지 = Journal of the Korean Earth Science Society, v.36 no.2, 2015년, pp.190 - 197
박영숙 (전북대학교 자연과학대학 지구환경과학과) , 윤호일 (한국해양연구원 부설 극지연구소 극지기후연구센터) , 유규철 (한국해양연구원 부설 극지연구소 극지기후연구센터) , 이영엽 (전북대학교 자연과학대학 지구환경과학과)
This study investigated the paleoclimatic change using diatoms that were extracted from the high-resolution laminated layers of diatom ooze sediment cores GC08-EB01 in the eastern basin of the Bransfield Strait, Antarctica. The range of diatom valves per gram of dry sediment was from
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핵심어 | 질문 | 논문에서 추출한 답변 |
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브랜스필드 해협은 무엇인가 | 브랜스필드 해협은 남북으로 남극반도와 남쉐틀랜드 군도사이에 위치하는 반폐쇄성 분지(semi-enclosed basin)이다. 브랜스필드 분지는 세 개의 소분지로 나눠진다. | |
벨링스하우젠 해수의 특징은 무엇인가 | , 2002). 브랜스필드 해협에서 표층수 순환은 벨링스하우젠해(Bellingshausen Sea)와 웨델해(Weddell Sea)로부터 유입되며, 벨링스하우젠 해수는 비교적 따뜻하고 저염인 반면에 웨델해수는 차갑고 고염의 특성을 가진다 (García et al., 2002). | |
브랜스필드 해협에서 해빙의 영향 유무에 따라서 무엇이 달라지는가 | 브랜스필드 해협에서 계절적인 해빙(sea-ice)의 분포는 매우 복잡한 양상을 가지며, 겨울철 해빙의 최대 크기가 남극반도의 57oS의 범위까지 확장되나 여름철에는 완전히 해빙의 영향을 벗어난다. 해빙의 영향을 벗어난 공해 (open-water)환경의 시기동안 규질의 유기물들이 대량 유입되는 반면에, 해빙으로 덮여 있는 동안에는 유입되는 규질 유기물의 양이 매우 적다(Abelmann and Gersonde, 1991). |
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