光驱动的无氧微生物氧化的
Mirna Daye1, Vanja Klepac-Ceraj2, Mihkel Pajusalu3
1Department of Earth, Atmospheric, and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, MA, USA. mirnadaye@gmail.com.
Nature
|December 6, 2019
概括
无氧光合作用微生物可以在没有氧气的情况下产生氧化,这挑战了关于早期光合作用的先前假设. 这一发现表明,早期的地球.
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:
- 氧气光合作用对于地球的生物圈至关重要,但它的起源仍有争议.
- 以前的研究表明,氧化光合作用在约30亿年前的进化,基于氧化的证据.
- 这些假设依赖于只有在氧气或特定光合作用中心的存在下形成的氧化.
研究的目的:
- 在无氧条件下研究微生物对氧化的生物矿化.
- 重新评估早期光合作用代谢和相关的地球化学信号的起源.
主要方法:
- 研究了能够生物矿化氧化物的微生物群落.
- 在严格无氧 (无氧) 条件下进行实验.
- 分析了微生物氧化产生的地化学特征.
主要成果:
- 证明无氧光合作用微生物可以在没有分子氧的情况下生物矿化氧化物.
- 证明在无氧条件下的微生物氧化产生了与以前归因于氧光合作用的地化学信号无法区分的地化学信号.
- 确定这种依赖光的过程可以发生在现代无氧水生环境中.
结论:
- 氧化光合作用的起源可能并不像以前从氧化沉积物中推断的那样古老.
- 无氧光合作用可能在大氧化事件之前产生了类似的地球化学信号.
- 这一过程对了解早期地球的生物地球化学循环和生命进化有重要意义.
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