循序渐进的地球氧化是全球生态化学循环的固有特性
Lewis J Alcott1, Benjamin J W Mills2, Simon W Poulton2
1School of Earth and Environment, University of Leeds, Leeds LS2 9JT, UK. eelja@leeds.ac.uk.
概括
地球的氧化发生在三个阶段. 内部生物化学反,而不是外部事件,驱使这些氧气增加,与光合作用进化后的逐渐氧化一致.
科学领域:
- 地质化学
- 生物地质化学
- 古气候学
背景情况:
- 地球的大气和海洋在古新生代,新生代和古新生代期间经历了三次主要的氧化事件.
- 这些氧化步骤对生物圈产生了重大影响,但它们的主要驱动因素仍有争议.
- 之前的假设提出生物或构造革命为这些逐步增加的氧气的原因.
研究的目的:
- 调查地球阶段性氧化事件的主要驱动因素.
- 要确定是否需要外部强迫来解释观察到的氧化步骤.
- 模拟碳,氧和的长期生态化学循环.
主要方法:
- 一个理论模型的开发和应用.
- 长期生物地化学循环中的内部反分析.
- 模拟碳,氧和的相互作用.
主要成果:
- 该模型表明,逐步氧化是内部生物化学反的自然结果.
- 不需要特定的外部强迫事件来解释氧化步骤的时间或大小.
- 结果与氧化光合作用进化后的逐渐行星表面氧化一致.
结论:
- 地球的氧化事件是由碳,氧和循环的内部反解释的.
- 逐步增加的氧气是地球生物化学系统的内在特性.
- 氧化光合作用的演化启动了一种与观测到的地质记录相一致的逐渐氧化过程.
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