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甲烷:生命起源时的燃料还是废气?

Methane: Fuel or Exhaust at the Emergence of Life?

机构信息

1 Jet Propulsion Laboratory, California Institute of Technology , Pasadena, California.

2 CNRS/Aix-Marseille University , BIP UMR 7281, IMM FR 3479, Marseille, France.

出版信息

Astrobiology. 2017 Oct;17(10):1053-1066. doi: 10.1089/ast.2016.1599. Epub 2017 Sep 26.

Abstract

As many of the methanogens first encountered at hydrothermal vents were thermophilic to hyperthermophilic and comprised one of the lower roots of the evolutionary tree, it has been assumed that methanogenesis was one of the earliest, if not the earliest, pathway to life. It being well known that hydrothermal springs associated with serpentinization also bore abiotic methane, it had been further assumed that emergent biochemistry merely adopted and quickened this supposed serpentinization reaction. Yet, recent hydrothermal experiments simulating serpentinization have failed to generate methane so far, thus casting doubt on this assumption. The idea that the inverse view is worthy of debate, that is, that methanotrophy was the earlier, is stymied by the "fact" that methanotrophy itself has been termed "reverse methanogenesis," so allotting the methanogens the founding pedigree. Thus, attempting to suggest instead that methanogenesis might be termed reverse methanotrophy would require "unlearning"-a challenge to the subconscious! Here we re-examine the "impossibility" of methanotrophy predating methanogenesis as in what we have termed the "denitrifying methanotrophic acetogenic pathway." Advantages offered by such thinking are that methane would not only be a fuel but also a ready source of reduced carbon to combine with formate or carbon monoxide-available in hydrothermal fluids-to generate acetate, a target molecule of the first autotrophs. And the nitrate/nitrite required for the putative oxidation of methane with activated NO would also be a ready source of fixed nitrogen for amination reactions. Theoretical conditions for such a putative pathway would be met in a hydrothermal green rust-bearing exhalative pile and associated chimneys subject to proton and electron counter gradients. This hypothesis could be put to test in a high-pressure hydrothermal reaction chamber in which a cool carbonate/nitrate/nitrite-bearing early acidulous ocean simulant is juxtaposed across a precipitate membrane to an alkaline solution of hydrogen and methane. Key Words: Green rust-Methanotrophy-Nitrate reduction-Emergence of life. Astrobiology 17, 1053-1066.

摘要

由于在热液喷口首次遇到的产甲烷菌大多是嗜热或超嗜热的,并且构成了进化树的较低根系之一,因此人们假设产甲烷作用是最早的途径之一,如果不是最早的途径,那么也是生命的途径之一。众所周知,与蛇纹石化有关的温泉还带有非生物甲烷,因此进一步假设新兴的生物化学只是采用并加速了这种所谓的蛇纹石化反应。然而,迄今为止,最近模拟蛇纹石化的热液实验未能产生甲烷,因此对这种假设产生了怀疑。相反的观点值得争论,即产甲烷作用更早,这一观点受到了“事实”的阻碍,即产甲烷作用本身被称为“反向产甲烷作用”,因此赋予了产甲烷菌的创始血统。因此,试图暗示产甲烷作用可能被称为反向产甲烷作用将需要“忘却”-对潜意识的挑战!在这里,我们重新审视了产甲烷作用早于产甲烷作用的“不可能”,就像我们所称的“反硝化产甲烷乙酸生成途径”一样。这种思维方式提供的优势是,甲烷不仅将是一种燃料,而且还是一种现成的还原碳源,可以与甲酸盐或一氧化碳结合-在热液流体中可用-生成乙酸盐,这是第一个自养生物的目标分子。而用于用激活的 NO 氧化甲烷的硝酸盐/亚硝酸盐也将是用于胺化反应的固定氮的现成来源。在一种热液绿锈产甲烷作用中存在质子和电子反梯度的含绿锈的喷出堆积物和相关烟囱中,这种假定途径的理论条件将得到满足。在高压热液反应室中,可以对这种假设进行测试,在该反应室中,将含有碳酸盐/硝酸盐/亚硝酸盐的早期酸性海洋模拟物冷却并并排放置在沉淀膜上,与碱性氢和甲烷溶液相邻。关键词:绿锈-产甲烷作用-硝酸盐还原-生命的出现。天体生物学 17, 1053-1066。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/beed/5655419/63862b0dee33/fig-1.jpg

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