大气中氧气度的晚期新生代上升是从遗传学和硫同位素研究中推断出来的
1Max Planck Institute for Marine Microbiology, Bremen, Germany.
Nature
|July 11, 1996
概括
非光合作用细菌的进化和硫化物同位素的转变发生在0.64-1.05亿年前. 这很可能是由大气氧气增加所驱动的,可能触发了动物的进化.
科学领域:
- 地质化学 地质化学
- 微生物学 微生物学
- 古生物学的古生物学
背景情况:
- 新新生态时代 (1.05到0.64亿年前) 见证了显著的环境变化.
- 了解早期微生物进化的驱动因素对于破译地球历史至关重要.
研究的目的:
- 研究微生物进化和地化学变化的同时发生.
- 探索大气氧气升对早期生命的影响.
主要方法:
- 在沉积硫化物中对同位素组成的分析.
- 地化学数据与化石记录的相关性.
主要成果:
- 生物沉积硫化物同位素的显著转变发生在0.64亿至1.05亿年前.
- 非光合作用硫化物氧化细菌的进化与这种同位素转移相吻合.
- 这些事件与大气氧气的提议上升 (5-18%的当前水平) 相一致.
结论:
- 大气中氧气水平的上升很可能推动了微生物进化和地化学变化.
- 这种氧化事件可能是动物随后进化的关键触发因素.
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