地球表面的20亿年过渡氧化
Haiyang Wang1,2,3,4, Chao Li5,6,7, Yongbo Peng8
1State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation and Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu, China.
Nature
|August 27, 2025
概括
地球
科学领域:
- 地质科学
- 生物地质化学
- 古气候学
背景情况:
- 地球的氧化是一个逐步的过程,过渡的细节仍然不清楚.
- 大气中的氧气 (O2) 的增加对于了解早期生命演变至关重要.
- 之前的研究缺乏关于长期氧化史的高分辨率数据.
研究的目的:
- 用一个新的代理来重建地球的氧化历史.
- 研究大气中的O2水平与海洋氧化之间的关系.
- 解释新生代碳循环的异常以及复杂生命的出现.
主要方法:
- 在25亿年的沉积硫酸盐 (Δ'17Osulfate) 中分析质量独立的氧同位素.
- 现有的沉积物 Δ33S 数据的整合.
- 定量生物地化学模型.
主要成果:
- 从无氧状态到现代水平的波动大气部分压力2 (pO2) 的2Gyr过渡.
- 在1.0 Ga之后,pO2升高的证据.
- 在新生代碳同位素外流过程中,合下降 Δ'17O硫酸盐和硫酸盐-δ34S,与增加 pO2 相关.
结论:
- 地球的大气和海洋经历了一段漫长而动态的同氧化历史.
- 环节性海洋氧化是由大气中增加的O2流入驱动的,有负反机制.
- 这种动态氧化为新生代的碳循环和复杂生命的出现提供了连贯的解释.
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