相对氧化的液体为地球最早的热水系统提供了食物
Dustin Trail1, Thomas M McCollom2
1Department of Earth and Environmental Sciences, University of Rochester, Rochester, NY 14627, USA.
概括
地球的早期
科学领域:
- 地质化学
- 天体生物学
- 早期的地球科学
背景情况:
- 早期地球上的岩层流体的特性对于了解生命的起源至关重要.
- 这些流体作为地球内部和表面的热水系统之间的通道.
研究的目的:
- 推断大约40亿年前的岩层流体的特征.
- 模拟与生命起源相关的关键金属的可溶性和运输.
主要方法:
- 使用的化学分析.
- 进行实验室实验.
- 使用地质化学建模.
主要成果:
- 压缩的氧气流动性,含量和早期石灰尘流体的温度.
- 确定这些流体比早期的地幔更加氧化.
- 确定与近地水系统的相互作用,例如热水池.
结论:
- 早期的石化流体在有利于前生物化学的环境中放大氧化还原梯度方面发挥了重要作用.
- 这些发现支持了涉及地球深层流体和地表热水系统相互作用的生命起源的情景.
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