高的二氧化碳水平使TCA循环向后转向自
Lydia Steffens1, Eugenio Pettinato1, Thomas M Steiner2
1Institute for Molecular Microbiology and Biotechnology, University of Münster, Münster, Germany.
Nature
|April 22, 2021
概括
无氧微生物可以逆转三碳酸 (TCA) 循环的碳固定. 高二氧化碳 (CO2) 水平驱动海马的这一循环,使其能够自营生长.
科学领域:
- 微生物学
- 生物化学
- 地质化学
背景情况:
- 通常参与能量生产的三碳酸 (TCA) 循环可以在一些无氧微生物中逆转为自营碳固定.
- 这种逆转循环使用特定的酶,如依赖于铁素的2-酸合成酶,并且需要高度的酸合成酶.
研究的目的:
- 研究热友细菌海 (Hippea maritima) 中逆转氧化TCA循环的条件.
- 阐明高二氧化碳 (CO2) 部分压力的作用.
主要方法:
- 使用热友硫减硫细菌海马 (Hippea) 进行实验分析.
- 在不同的CO2条件下研究了酸盐合成酶和酸盐合成酶的生物化学途径.
主要成果:
- 证明高的二氧化碳部分压力对于驱动海马的逆氧化TCA循环至关重要.
- 通过酸盐合成酶催化,通过降解性碳酸盐去除乙辅酶A (乙-CoA) 在高二氧化碳下至关重要.
结论:
- 逆转的氧化TCA循环是由Hippea maritima的高二氧化碳水平积极推动的.
- 这种途径为自碳固定提供了比降低性TCA循环更节能的替代方案.
- 这些发现表明,这种逆转的TCA循环可能是地球早期大气中二氧化碳固定的一个重要机制.
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