南中国海记录 晚期米奥森时期西太平洋深度循环的重组
Shan Liu1,2,3, Hui Chen1,2,3, Ming Su4,5,6
1School of Marine Sciences, Sun Yat-sen University, Zhuhai, China.
Nature communications
|November 25, 2024
概括
这是南中国海.
科学领域:
- 海洋学 海洋学 海洋学
- 海洋地质 海洋地质学
- 古海洋学是古海洋学.
背景情况:
- 海洋门户对全球海洋循环至关重要,但它们对低度深水流的影响尚不清楚.
- 南中国海,一个关键的西太平洋地区,经历了显著的海洋学变化,与赤道和低度门户的动态,因为Oligocene.
研究的目的:
- 研究海洋门户对南中国海深水循环的影响.
- 重建太平洋和印度洋之间的深水连接历史.
主要方法:
- 从深南中国海的地震数据中识别轮形状的特征.
- 来自海洋钻探计划第184号航程和国际海洋发现计划349号和367/368号航程的钻芯分析.
主要成果:
- 从印度洋东部到南中国海的环极深水影响的证据,直到大约1000万年前.
- 大约1000万年前,印度尼西亚大门的关闭扰乱了太平洋和印度洋之间的深水交换.
结论:
- 门口构造学,特别是印度尼西亚门口的关闭,显著重组了全球深水循环.
- 这些构造事件很可能导致了中后米奥森的全球气候和海洋状况变化.
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