虽然古老,但并非古老:岩石漏的有机碳驱动地下水微生物群
Beatrix M Heinze1, Valérie F Schwab2, Susan E Trumbore3
1Aquatic Geomicrobiology, Institute of Biodiversity, Friedrich Schiller University, Jena, Germany; Department Biogeochemical Processes, Max-Planck-Institute for Biogeochemistry, Jena, Germany.
The Science of the total environment
|December 25, 2024
概括
古代碳酸盐岩石释放出令人惊的新鲜有机物质,为地下微生物生命提供燃料. 这一发现揭示了岩石裂如何储存和释放年轻碳,推动含水层中的微生物代谢.
科学领域:
- 地质化学 地质化学
- 微生物学 微生物学
- 环境科学 环境科学
背景情况:
- 地下微生物生命是巨大的,大部分生物质在大陆地下.
- 沉积岩是有机碳 (C) 的主要来源.
- 已知微生物利用化石碳,但岩石有机碳的作用尚不清楚.
研究的目的:
- 研究岩石有机碳在多大程度上驱动水层中的微生物活动.
- 分析从碳酸盐岩石中出的有机物质的组成和年龄.
- 确定微生物对岩石浸出有机物质的反应.
主要方法:
- 用粉碎的碳酸盐岩石化有氧和无氧地下水.
- 碳池和微生物生物标志物的放射性碳 (C) 分析.
- 对脂衍生脂肪酸 (PLFA) 的分析和微生物种群的预测功能概况.
主要成果:
- 古代岩石释放的有机物质含有高达72.6%的现代C,表明保存的新鲜有机物质.
- 在地下水中发现了岩石浸化合物溶解有机碳 (DOC),这表明在现场释放.
- 微生物生物质 (PLFA) 迅速吸收了岩石浸碳,占生物质C的51%.
- 微生物群落显示出在岩石水中存在的碳化合物的降解潜力.
结论:
- 碳酸盐岩石作为较年轻的有机物质的时间沉.
- 这种有机物质的浸出,与化石碳化合物一起,推动了地下微生物的新陈代谢.
- 地下微生物生态系统是由化石和最近漏的碳来源混合而成的燃料.
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