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聊聊Sci

120-地球大氧化历史的多阶段演化

24 Sep 2025

Description

这篇论文概述了地球表面持续了二十亿年的过渡性氧化过程,利用沉积硫酸盐中的高分辨率氧同位素(Δ′¹⁷Osulfate)记录作为大气氧分压(pO₂)的代理指标。研究通过将新数据与现有的硫同位素数据结合,提出了地球大气氧化历史的三个主要阶段:从无氧状态(4.0 Ga至2.4 Ga)到低且波动的氧水平(2.4 Ga至0.41 Ga),再到现代水平(0.41 Ga至今)。作者们发现,在第二阶段(1.0 Ga至0.41 Ga)的新元古代负碳同位素漂移事件(δ¹³Ccarb excursions)中,Δ′¹⁷Osulfate 和 δ³⁴Ssulfate 的耦合下降,表明大气氧输入增强引发了短暂的海洋氧化脉冲。这些发现支持了一个动态且漫长的气-海共同氧化历史,解释了新元古代碳循环的异常和复杂生命的阶段性崛起。References:Wang H, Li C, Peng Y, et al. Two-billion-year transitional oxygenation of the Earth’s surface[J]. Nature, 2025: 1-7.

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