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在加迪斯湾的甲素活动和微生物多样性,泥火山沉积物
Gordon Webster1,2, Barry A Cragg2, Joachim Rinna2,3
1Microbiomes, Microbes and Informatics Group, School of Biosciences, Cardiff University, Cardiff, Wales, United Kingdom.
Frontiers in microbiology
|June 9, 2023
概括
卡迪斯湾泥火山中的 Prokaryotes 显著影响甲的释放,甲基基生成是关键的过程. 进一步的研究对于了解它们对全球碳循环的贡献至关重要.
科学领域:
- 地质微生物学的生物.
- 海洋地球化学 海洋地球化学
- 大陆的利率动态
背景情况:
- 卡迪斯湾有许多泥火山 (MVs),其中有活跃的甲 (CH4) 透.
- 微生物在这些MV中释放的CH4中的作用仍然在很大程度上未被探索.
研究的目的:
- 调查卡迪斯湾MVs中的 prokaryotic 多样性和活动.
- 评估甲生成和甲无氧氧化 (AOM) 对CH4循环的贡献.
主要方法:
- 在七个MV中分析了微生物多样性,地质化学和甲生成活性.
- 用基质改性泥进行化,以测量潜在的甲基生成和AOM.
主要成果:
- Prokaryotic 种群和活动在 MV 和参考地点之间差异很大.
- 在硫酸盐-甲过渡区 (SMTZ) 下发现的细胞数量低于全球平均水平.
- 甲基变性甲基生成,特别是来自甲基胺,比来自H2/CO2或酸盐更为显著.
结论:
- 甲基变性甲基生成是加迪斯湾 MVs 中的主导的 CH4 生产途径.
- 确定了古生物学和细菌群落,包括特定的甲原体和ANME.
- 这些MV对全球甲和碳循环的贡献需要进一步调查.
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