从液体内含物中获得的微生物甲基生成的证据是在早期的古老时代
Yuichiro Ueno1, Keita Yamada, Naohiro Yoshida
1Research Center for the Evolving Earth and Planet, Tokyo Institute of Technology, Meguro-ku, Tokyo 152-8551, Japan. yueno@depe.titech.ac.jp
Nature
|March 24, 2006
概括
这项研究提供了最古老的甲基生物,原始微生物的证据,可以追溯到超过346亿年前. 这些发现表明,早期的甲生物可能通过产生甲来影响地球的古代气候.
科学领域:
- 早期生命研究研究.
- 地质微生物学的生物.
- 古气候学 古气候学
背景情况:
- 甲基生物是古代微生物,对于了解早期生命至关重要.
- 它们在古代气候调节中的作用是假设的,但缺乏直接证据.
- 此前对阿基亚甲原体的证据是间接的,基于煤化物中的碳同位素.
研究的目的:
- 为了找到直接的地质证据,证明古老的甲基生物的存在.
- 为了确定地球上甲基生命最古老的确切日期.
- 研究早期甲基生物在调节地球气候中的潜在作用.
主要方法:
- 在35亿年前的热液沉物中分析含甲的液体含量.
- 粉碎从内含物中提取液体.
- 提取的甲的碳同位素分析.
主要成果:
- 确定了微生物甲,其碳同位素成分枯竭 (<-56千分之一).
- 这种甲是在35亿年前的热沉物中发现的.
- 这些发现提供了超过346亿年前存在的甲基生物的证据.
结论:
- 这项研究提供了迄今为止最古老的甲基生物的直接证据.
- 这一发现早于先前的地化学证据大约7亿年.
- 证实了甲基生物在早期阿基亚时代存在,支持它们在气候调节中的潜在作用.
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