细菌进化和氧气适应的地质时间表
Adrián A Davín1,2,3, Ben J Woodcroft4, Rochelle M Soo1
1The University of Queensland, School of Chemistry and Molecular Biosciences, Australian Centre for Ecogenomics, Brisbane, Queensland, Australia.
概括
机器学习和遗传学和解揭示了细菌的进化. 大多数细菌在大氧化事件后变得有氧化,但蓝藻细菌早些时候进化了有氧代谢,可能使氧光合作用成为可能.
科学领域:
- 微生物进化
- 地质化学
- 古生物学
背景情况:
- 微生物生命的化石记录稀少,限制了对深远时代进化的理解.
- 细菌的新陈代谢留下了地化学特征,尤其是大氧化事件 (GOE).
研究的目的:
- 通过机器学习和基因调和,推断祖先的细菌过渡到有氧生活方式.
- 将这些转换与GOE联系起来以校准细菌时间树.
主要方法:
- 使用了机器学习算法.
- 使用了遗传学和解技术.
- 特别是与埃塞俄比亚政府有关的地质化学数据被整合.
主要成果:
- 细菌类的多样性可以追溯到古世和新生代.
- 大多数细菌类是祖先无氧的,在GOE之后采用有氧的生活方式.
- 菌的祖先可能在GOE之前具有有氧代谢.
结论:
- 这项研究提供了细菌新陈代谢的进化历史.
- GOE在塑造细菌有氧生活方式方面发挥了关键作用.
- 蓝藻细菌的早期有氧代谢可能是氧光合作用的前体.
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