新古时代的以氧为基础的循环在通往大氧化事件的路上
Alice Pellerin1, Christophe Thomazo2,3, Magali Ader4
1Laboratoire Biogéosciences, UMR CNRS 6282, Université de Bourgogne, Dijon, France. alice.pellerin-lefebvre@u-bourgogne.fr.
Nature
|August 21, 2024
概括
地球的早期
科学领域:
- 地质化学
- 古生物学
- 地球的早期历史
背景情况:
- 沉积性同位素 (δ15N) 追踪氧化还原过程和早期氧化.
- 大氧化事件 (大约2.45亿年) 显示没有重大 δ 15 N 转移,表明脱的和氧循环.
- 阳性δ15N值 (2.82.6 Ga) 表示氧化的前体,但它们的起源不清楚.
研究的目的:
- 调查前坎布里亚岩石中正值 δ15 的起源.
- 确定早期循环演变的时间和影响.
- 在大气氧气积累之前确定神秘氧气循环的证据.
主要方法:
- 在2.68Gyr的沉积岩中分析同位素组成 (δ15N).
- 对塞拉苏尔形成的地化学研究,亚马逊地.
- 在地球早期的氧化还原条件下循环的解释.
主要成果:
- 在2.68-Ga海洋沉积物中发现强烈正的δ15N值 (>30‰).
- 这些发现归因于与神秘氧气循环相关的区域性氧化.
- 证据表明氧光合作用大约在2.7亿年前就开始.
结论:
- "同位素事件"标志着早期的生态化学重组.
- 这一事件是大气氧化的先兆.
- 它表示大氧化事件的初步步骤.
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