和暗氧推动了各种地下水生态系统中的微生物生产力
S Emil Ruff1,2,3, Pauline Humez4, Isabella Hrabe de Angelis4,5
1Department of Geoscience, University of Calgary, Calgary, Canada. eruff@mbl.edu.
Nature communications
|June 13, 2023
概括
古老的地下水维持着多样化的微生物生命,挑战了以前对地下细胞丰富度的估计. 这项研究揭示了深层含水层在现场显著的氧气生产,支持广泛的有氧代谢.
科学领域:
- 地质科学 地质科学
- 微生物学 微生物学
- 环境科学 环境科学
背景情况:
- 地下水是全球约50%人口的重要饮用水来源.
- 地下微生物生态系统及其代谢过程尚未完全理解.
- 估计在地下深处的微生物细胞丰度需要重新评估.
研究的目的:
- 调查加拿大地下水样本的年龄,地质化学和微生物学.
- 了解水层内的大规模生物地质化学循环.
- 在深层地下环境中识别溶解氧的来源.
主要方法:
- 分析了来自加拿大14个含水层的95个监测井的138个地下水样本.
- 地质化学和微生物学分析以确定代谢过程.
- 甲基因组学,氧同位素分析和混合模型来追踪氧气来源.
主要成果:
- 一致的地化学和微生物学趋势表明,甲,和硫循环的广泛传播.
- 较旧的地下水,特别是富含有机碳的地下水,含有较高的微生物细胞密度 (高达1.4×10^7细胞/毫升).
- 在较旧的地下水中发现了显著的溶氧度 (0.52 ± 0.12 mg/L),支持有氧代谢.
结论:
- 古代地下水是令人惊的生产力微生物群落的宿主.
- 现场微生物变异是地下生态系统中"暗氧"的重要来源.
- 这项研究突出了一个被忽视的氧气来源,对于理解地球上过去和现在的地下生命至关重要.
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