深海溶解O2的记录来自海底玄武岩中的铁的氧化状态
Daniel A Stolper1, C Brenhin Keller1,2
1Department of Earth and Planetary Science, University of California, Berkeley, California 94720, USA.
Nature
|January 9, 2018
概括
深海氧化对于动物进化至关重要,可能比以前想象的要晚. 新的研究表明,这发生在罗纪,可能直到古老纪晚期.
科学领域:
- 地质化学
- 古代海洋学
- 海洋生物学
背景情况:
- 深海氧化与大气氧气的增加,现代生物地化学循环和早期动物多样化有关.
- 之前估计的深海氧化和大气氧气水平在8亿至4亿年前.
- 目前的方法依赖于大陆架沉积物的间接地化学特征.
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