对生命起源的冲击挫折
1Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena 91125, USA.
Nature
|February 18, 1988
概括
地球上生命的起源可能是由当撞击变得比生物发生的时间表更频繁时的时间定义的. 深海的热水喷气口表明,生命可能在4,000-4,200万年前开始.
科学领域:
- 天体生物学 天体生物学
- 地质地质地质地质地质地
- 生命的起源研究 生命的起源研究
背景情况:
- 哈第纪和早期阿基纪时期的特点是强烈的小行星撞击.
- 生物起源,即生命从无机物质的起源,是地球历史上的一个关键事件.
研究的目的:
- 根据撞击频率和生物生成时间表来定义生命的起源.
- 为了估计什么时候在不同的早期地球环境中可能发生了生物发生.
主要方法:
- 分析月球和地球撞击记录以量化哈第纪和早期阿赫纪撞击流量.
- 估计与影响相关的过程对拟议的生物发生环境的影响.
- 根据撞击间隔和环境适用性计算生物发生的潜在时间框架.
主要成果:
- 生物生成可能早在4000至4200亿年前就发生在深海热水环境中.
- 在地球表面,生物发生可能发生在3700至4000亿年前.
- 建立自我复制原生体的时间表是一个关键因素.
结论:
- 生命起源的时间被破坏性冲击的频率下降所限制.
- 不同的早期地球环境,比如水热喷口与表面位置,为生物发生的时间提供了不同的可能性.
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