地表微生物社区结构沿着中美洲火山弧的地质特征发生变化
Marco Basili1,2,3, Timothy J Rogers1, Mayuko Nakagawa4
1Department of Microbiology, University of Tennessee, Knoxville, TN, United States of America.
PloS one
|November 13, 2024
概括
中美洲火山弧中的微生物群落是由深层地球流体和地质环境塑造的,而不仅仅是接近. 这揭示了地质与沿着汇聚边缘的地下生命之间存在着密切的联系.
科学领域:
- 地质微生物学的生物.
- 地质化学 地质化学
- 板块构造学是一种板块构造学.
背景情况:
- 来自科科斯和纳斯卡板块的深层流体为沿中美洲火山弧 (CAVA) 沿着中美洲火山弧 (CAVA) 的碳,,硫和富含铁的地下微生物社区提供燃料.
- 微生物活动影响这些深层流体化合物的分布,氧化还原状态和同位素组成.
- 了解微生物群落沿着融合边缘移动,受到地质特征变化的影响,至关重要.
研究的目的:
- 为了研究细菌群落和地球化学在南部CAVA沿线的变化.
- 检查微生物群落分布与地质变化的关系,包括可可斯山脊的沉积.
主要方法:
- 对细菌16S rRNA基因片的分析.
- 对深层泄漏的地质化学分析.
主要成果:
- 沿着收边际观察到社区组成的变化.
- 微生物群落基于相似的地质环境聚集在一起,不管样本地点的近距离.
- 微生物群落的组成与地质因素相关,如宿主岩类型,热水流体成熟度和板块深度.
结论:
- 地球深层过程与地下微生物活动之间存在密切的联系.
- 地质变量显著控制微生物社区的分布,结构和组成沿着融合边缘.
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