巨大的石撞击对古老时代的表面环境和生命的影响
Nadja Drabon1, Andrew H Knoll1, Donald R Lowe2
1Department of Earth and Planetary Sciences, Harvard University, Cambridge, MA 02138.
概括
大型石撞击显著改变了早期地球的环境. 这次S2撞击事件引发了海和升温,影响了微生物,但也提供了营养,推动了铁循环微生物的繁荣.
科学领域:
- 早期地球科学 早期地球科学
- 天体生物学 天体生物学
- 地质化学 地质化学
背景情况:
- 众所周知,大型石撞击影响了早期地球的可居住性.
- 考古时代有至少16次重大撞击事件的证据.
- 这些影响对早期生活的具体影响仍然不太清楚.
研究的目的:
- 评估南非S2冲击事件 (3.26 Ga) 的环境和生物后果.
- 为了分析S2冲击层的沉积岩,寻找地质化学和沉积学证据.
- 了解影响在塑造早期微生物生态系统中的作用.
主要方法:
- 考古岩石的沉积物学分析.
- 沉积物样本的石化检查.
- 碳同位素地质化学 (δ13Ccarb) 来推断生物地质化学过程.
主要成果:
- 这次S2撞击引发了一场巨大的海,导致海洋升温和注入.
- 有机物和可变的 δ13Ccarb 值相关的 siderite 形成的证据.
- 冲击效应包括表面水中的营养和铁丰富.
结论:
- S2的影响对早期生活产生了显著的区域和潜在的全球影响.
- 光合作用微生物的初始破坏随后是铁循环微生物的快速恢复和繁荣.
- 影响引起的环境变化,包括营养的可用性,塑造了微生物社区的动态.
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