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在最后的冰川最大期和海因里希斯球场1期间,北大西洋深水普遍存在

Patrick Blaser1,2, Claire Waelbroeck3, David J R Thornalley4

  • 1Institute of Earth Sciences, University of Lausanne, Lausanne, Switzerland.

Nature geoscience
|May 16, 2025
PubMed
概括

深海循环极大地影响了冰川和冰川间的气候. 北大西洋深水在寒冷时期持续存在,从通风良好的模式转变为通风较少的模式,影响碳储存和气候预测.

关键词:
古代海洋学 古代海洋学古代气候是一种古气候.

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