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根据10Be和14C记录推断的年轻德里亚斯事件期间深水形成的变化

R Muscheler1, J Beer, G Wagner

  • 1Department of Surface Waters, EAWAG, Dübendorf, Switzerland. muscheler@eawag.ch

Nature
|December 16, 2000
PubMed
概括

年轻干旱时期大气中放射性碳 (14C) 的波动主要是由生产速率的变化驱动的,而不仅仅是碳循环. 使用-10 (10Be) 数据的分析显示,深水形成的变化也影响了14C水平.

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