在前生物海洋中形成和自发氧化中性 [4Fe-4S] 集群
Theodore M Present1, Joan Selverstone Valentine2, Jena E Johnson3
1Division of Geological and Planetary Science, California Institute of Technology, Pasadena, CA 91125, USA.
Journal of inorganic biochemistry
|February 26, 2026
概括
质子氧化了铁 (II) 到铁 (III),使早期地球海洋中的铁-硫集群组合成为可能. 干稳定了这些必不可少的酶共因子,促进了生命代谢的起源.
科学领域:
- 生物地质化学生物地质化学
- 生命的起源研究 生命的起源研究
- 生物物理化学 生物物理化学
背景情况:
- 铁硫集群是生命早期基本的重要酶共因子.
- 古代的海洋富含铁 (II),缺乏足够的铁 (III) 以保持集群的稳定性.
- 了解早期的辅因子组合是破译原始代谢的关键.
研究的目的:
- 为了研究质子在铁硫团形成过程中作为铁的氧化剂的作用.
- 探索连接物如何影响早期铁硫团的稳定性.
- 为了阐明早期地球条件下分子铁硫集群组装的机制.
主要方法:
- 使用密度函数理论 (DFT) 的计算.
- 模拟分析了诸如H3O+,Fe(SH) +和H2S等质子源.
- 纳米粒子板的能量与结合集群的能量进行了比较.
主要成果:
- 已经证明质子会氧化 [2Fe-2S] 集群,并促进 [4Fe-4S] 集群的形成.
- 连接物 (水,二硫化物,) 对于稳定古巴集群状态至关重要.
- 像麦基纳瓦特这样的纳米粒子板和结合的古巴体在能量方面进行了比较.
结论:
- 以质子为媒介的氧化还原反应和连接物协调使铁硫团组装成为可能.
- 这个过程可能发生在早期地球的富含铁,硫化物含水中.
- 这些发现为重要的生物分子辅助因子的起源提供了合理的途径.
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