在一个可居住的古老的高温盐水中,放射性地重新处理了古老的有机物
Devan M Nisson1, Clifford C Walters2, Martha L Chacón-Patiño3
1Department of Geosciences, Princeton University, Princeton, NJ, 08540, USA. dnisson@princeton.edu.
Nature communications
|October 3, 2023
概括
南非金矿盐深处热的非生物过程会产生大量的溶解有机碳 (DOC) 池. 这些放射性驱动的碳循环支持缓慢,稀疏的深层生物圈,并指导对外星生命的搜索.
科学领域:
- 地质化学 地质化学
- 天体生物学 天体生物学
- 微生物学 微生物学
背景情况:
- 溶解有机碳 (DOC) 对于地下液体中的微生物生命至关重要.
- 了解非生物和生物的DOC来源是评估可居住性的关键.
- 深层大陆盐水提供了独特的环境来研究这些过程.
研究的目的:
- 调查南非金矿深层盐水中的大型DOC池的起源和组成.
- 确定非生物过程对DOC形成和循环的贡献.
- 评估对微生物可居住性和地球以外生命的搜索的影响.
主要方法:
- 使用激发发射矩阵 (EEMs) 分析溶解有机碳 (DOC).
- 高分辨率质谱 (FT-ICR MS) 使用负电喷射电离 (ESI).
- 碳化合物的同位素分析 (δ2H和δ13C) 和氨基酸分析.
主要成果:
- 盐含有大量的DOC池 (101-283毫克C/L) 在一个古老的,高温的,低生物质的环境中.
- 氧化主要来自放射性氧化丰富的页岩/珊瑚礁,甲和乙,以及较少的碳化合物和有机硫化物.
- 同位素特征证实了C1-C3碳化合物的非生物起源.
结论:
- 水与岩石的相互作用和放射溶解是这种深盐水中氧化还原和碳循环的主要驱动因素.
- 这些非生物过程维持了一个有限的,缓慢生长的深层生物圈.
- 放射性驱动的可居住盐水是寻找外星生命的有希望的目标.
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