大量的硫同位素变化是否是古代撞击诱导的热水气体火星类型生物特征?
Christopher J Tino1, Eva E Stüeken2,3, Gernot Arp4
1Department of Earth and Planetary Sciences, University of California, Riverside, California, USA.
Astrobiology
|July 27, 2023
概括
撞击坑湖中的硫稳定同位素比率 (δ34S) 可能无法可靠地表明存在生命. 诺德林格里斯火山口的地球研究表明,非生物过程可以产生大 δ34S 变异,挑战它们作为生物标志的使用.
科学领域:
- 天体生物学 天体生物学
- 地质化学 地质化学
- 古生物学的古生物学
背景情况:
- 硫的稳定同位素比率 (δ34S) 被认为是撞击坑古老的生物标志.
- 来自盖尔火山口的火星 δ34S 数据显示了归因于非生物过程的巨大变异.
- 基于地球的研究经常将d34S分离>21‰解释为生物,包括在模拟撞击坑湖中.
研究的目的:
- 调查Nördlinger Ries撞击坑中的 δ34S 属性是否定义了一个生物标志.
- 为了从陆地模拟撞击坑湖环境中分析石质.
主要方法:
- 分析 δ34S,总有机碳 (TOC) 质量%,以及扫描电子显微镜 (SEM) 成像.
- 专注于水热变化的冲击突破和沉积式湖泊填充序列.
- 检查来自米奥生纪里斯撞击坑的多种岩石结构.
主要成果:
- 在里斯火山口的宿主岩层之间观察到 δ34S 的差异.
- δ34S变化的潜在原因包括热化学硫酸盐减少,微生物硫酸盐减少或热水平衡分化.
- 仅基于δ34S变异>21‰的生物性断言被认为是微不足道的.
结论:
- 在撞击坑湖中,不建议使用 δ34S 作为唯一的生物标志.
- 结合地质,生物地化学和纹理背景的独立检查至关重要.
- 在解释 δ34S 数据时,必须全面承认替代假设.
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