多种代谢途径的整合支持活微生物中的高碳沉率
Rachel E Sipler1,2,3, Eric W Isemonger1, Samantha C Waterworth1,4,5,6
1Department of Biochemistry, Microbiology and Bioinformatics, Rhodes University, Makhanda, South Africa.
Nature communications
|December 8, 2025
概括
微生物体或化微生物,有效地捕获和沉二氧化碳. 这些淡水生态系统显示出形成稳定的碳酸盐矿床的重要生物机制.
科学领域:
- 地质微生物学的生物.
- 生物地质化学生物地质化学
- 环境科学 环境科学
背景情况:
- 微生物体是由微生物群落形成的分层结构.
- 它们在通过生物过程的碳循环中发挥作用.
研究的目的:
- 研究细菌社区结构和功能与淡水微生物中的碳吸收/沉率之间的关系.
- 量化这些微生物生态系统每日和每年的碳捕获和降水量.
主要方法:
- 迪尔测试是为了监测24小时周期内的碳动态而进行的.
- 功能基因容量的分析评估了细菌群体的代谢潜力.
- 测量了多孔性和积累率,以估计垂直积累.
主要成果:
- 光合作用是由光独立的碳吸收机制,如生物矿物化和化学自otrophy补充.
- 微生物质以 7-12 g C m-2 24 h-1 的速度捕获无机碳.
- 捕获的碳中有高达87%沉,导致碳酸积累13-23毫米/年.
结论:
- 淡水微生物体表现出一种高度有效的生物机制,用于沉溶解的CO2.
- 这些过程将无机碳转化为地质稳定的碳酸盐矿物质.
- 微生物质对碳封存和矿物质形成有很大的贡献.
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