地断层驱动深层地表的生物氧化还原循环
Xiao Wu1,2,3, Jianxi Zhu1,2,3, Hongmei Yang1,2,3
1State Key Laboratory of Deep Earth Processes and Resources, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, P.R. China.
Science advances
|July 18, 2025
概括
深层生物圈中的微生物生命使用来自水岩反应的能量. 这项研究表明,由岩石裂变驱动的铁循环维持了地球和潜在的其他行星的这些能源来源.
科学领域:
- 地质化学 地质化学
- 天体生物学 天体生物学
- 微生物生态学 微生物生态学
背景情况:
- 深层生物圈中的微生物群落依赖于来自水岩反应的氧化还原对来获得能量.
- 岩石破裂产生气和氧化剂,但与铁的相互作用尚不清楚.
研究的目的:
- 研究氧化还原梯度的形成和演变.
- 探索铁在地下氧化还原反应中的作用.
主要方法:
- 模拟了激素诱导的水分裂.
- 在模拟的地下条件下分析了铁氧化还原循环 (Fe2+/Fe3+).
主要成果:
- 低氧化剂度 边缘氧化铁 (Fe2+) 到铁 (Fe3+).
- 反应性原子 (•H) 有效地将Fe3+降低回Fe2+.
- 由水岩反应驱动的铁氧化还原循环被证明.
结论:
- 地断裂可以产生氧化还原对,驱动铁氧化还原循环.
- 铁氧还氧循环为地下生命提供了持续的能量来源.
- 这个过程对地球和其他行星上的生命有影响.
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