一个表面的酸盐和异酸盐的热水源
Paul B Rimmer1, Oliver Shorttle2,3
1Cavendish Laboratory, University of Cambridge, JJ Thomson Ave, Cambridge CB3 0HE, UK.
Life (Basel, Switzerland)
|April 27, 2024
概括
早期地球上的巨大冲击可能已经创造了富含石墨的地. 然后,这种石墨可以在热水喷口中产生必不可少的益生菌分子,如烯酸和异烯酸,从而帮助生命的起源.
科学领域:
- 天体生物学 天体生物学
- 地质化学 地质化学
- 行星科学 行星科学
背景情况:
- 在地球的Hadean eon期间,巨大的冲击可能会形成富含的大气层,从而导致大气中的碳减少.
- 在大气凝结和表面沉积后,这种减少的碳将被纳入地,并在加热后转化为石墨.
研究的目的:
- 为了研究石墨和的海底岩对益生菌化学的影响.
- 模拟火山气体与石墨丰富的地相互作用的化学产品在表面热水风口场景中.
主要方法:
- 模拟表面热水风口系统,其中含有丰富的火山气体通过石墨和的地.
- 在高温 (15001700 °C) 和高压 (11000 bar) 的情况下模拟条件.
主要成果:
- 与石墨的平衡反应净化了火山气体.
- 产生了大量的益生菌分子,包括烯 (酸[HCN],素[HC3N]) 和异烯 (异酸[HNC]).
- 预计甲基异酸盐度大约为百万分之一 (ppm).
结论:
- 石墨和的海底地是水热喷口中益生菌分子的可信来源.
- 表面或浅水热环境被确定为甲基异酸的关键地质化学来源,对生命构建基石的非酶激活至关重要.
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