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在最后一个冰河间时期,南大西洋深处的一次停滞事件
Christopher T Hayes1, Alfredo Martínez-García2, Adam P Hasenfratz2
1Department of Earth, Atmospheric and Planetary Sciences, Massachusetts Institute of Technology (MIT), Cambridge, MA 02142, USA. Lamont-Doherty Earth Observatory of Columbia University, Palisades, NY 10964, USA. cthayes@mit.edu.
概括
在最后一个冰河间时期,全球温度升高导致南极地底水 (AABW) 形成减少,影响海洋氧化. 这表明深海循环转移甚至发生在温暖的气候,而不仅仅是在冰河时代.
科学领域:
- 古海洋学是古海洋学.
- 气候科学 气候科学
- 海洋学 海洋学 海洋学
背景情况:
- 最后一个冰河间时期 (约127,000年前) 比现在更温暖,海平面更高.
- 南洋沉积物提供了对过去深水条件的洞察.
研究的目的:
- 调查在最后一个冰河间期间深水氧化减少的原因.
- 确定深海循环模式在冰川和冰川间时期之间是否有所不同.
主要方法:
- 在南大洋沉积芯中对authigenic的分析.
- 重建深水氧化和循环模式.
主要成果:
- 在authigenic的尖峰表明减少了127,000年前南极地底水 (AABW) 的氧化.
- 这种AABW减少似乎与南极冰盖融水有关,而不是开放海洋条件.
- 减少的AABW与增加的北大西洋深水 (NADW) 形成相吻合,反之亦然.
结论:
- 深海循环,以AABW和NADW形成的交替为特征,发生在寒冷 (冰河时代) 和温暖 (间冰期) 的气候中.
- 南极冰盖质量损失可能会对深水形成和海洋循环产生重大影响.
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