乙氧化古生物对的CO2生成到F420的减少
Olivier N Lemaire1, Gunter Wegener1,2,3, Tristan Wagner4,5
1Max Planck Institute for Marine Microbiology, Celsiusstrasse 1, 28359, Bremen, Germany.
Nature communications
|October 21, 2024
概括
海洋古生物利用无氧氧化来加工碳化合物. 这项研究揭示了它们的CO2形成酶向F420辅因子传递电子,而不是铁素,从而使乙醇变.
科学领域:
- 微生物学 微生物学
- 生物化学 生化学
- 环境科学 环境科学
背景情况:
- 基的无氧氧化对于减轻海洋碳化合物入至关重要.
- 海洋古生物依赖硫酸盐降解细菌在氧化过程中进行电子转移.
- 古代的二氧化碳形成酶通常被认为与铁素减少结合在一起.
研究的目的:
- 研究在无氧乙氧化过程中二氧化碳生成的分子机制.
- 来自Candidatus Ethanoperedens thermophilum的CO脱酶和formylmethanofuran脱酶的特征.
- 为了阐明电子转移途径在ethanotrophic古物.ea.
主要方法:
- 对纯化的本土酶进行生物化学测试.
- 用X射线晶体学来确定酶复杂结构.
- 在基因组背景下进行元基因组挖掘.
主要成果:
- 氧化碳脱酶和甲基甲甲脱酶向F420辅因子提供电子.
- 这两种酶都有电子桥梁,将氧化中心与依赖黄素的F420减少酶连接起来.
- 观察到强大的结合F420-还原酶活动,与相关生物体不同.
结论:
- 一个新的模型建议在这个生物体的催化氧化过程中向F420输送电子.
- 这一途径促进了对硫酸盐降解伙伴的间接电子转移.
- 这种适应是推动能量节约驱动乙醇养的关键.
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