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在冰川开始期间,大西洋深处的生物碳储存逐渐增加

Monica Garity1, David Lund1, Hope Jerris1,2

  • 1Department of Marine Sciences, University of Connecticut, Groton, CT 06340.

Proceedings of the National Academy of Sciences of the United States of America
|August 4, 2025
PubMed
概括

深大西洋的碳储存在最后一个冰川周期中显著影响了大气中的二氧化碳 (CO2) 水平. 增强的封存发生在二氧化碳下降期间,而释放发生在变暖期间.

关键词:
二氧化碳是二氧化碳的一种物质.冰川 - 间冰川周期的周期.海洋循环 海洋循环古代海洋学 古代海洋学 古代海洋学

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