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地球上的渣滓:关于益生元多隔室环境的一种假说

Scum of the Earth: A Hypothesis for Prebiotic Multi-Compartmentalised Environments.

作者信息

Walton Craig Robert, Shorttle Oliver

机构信息

Department of Earth Sciences, University of Cambridge, Cambridge CB2 3EQ, UK.

Institute of Astronomy, University of Cambridge, Cambridge CB3 OHA, UK.

出版信息

Life (Basel). 2021 Sep 16;11(9):976. doi: 10.3390/life11090976.

Abstract

Compartmentalisation by bioenergetic membranes is a universal feature of life. The eventual compartmentalisation of prebiotic systems is therefore often argued to comprise a key step during the origin of life. Compartments may have been active participants in prebiotic chemistry, concentrating and spatially organising key reactants. However, most prebiotically plausible compartments are leaky or unstable, limiting their utility. Here, we develop a new hypothesis for an origin of life environment that capitalises upon, and mitigates the limitations of, prebiotic compartments: multi-compartmentalised layers in the near surface environment-a 'scum'. Scum-type environments benefit from many of the same ensemble-based advantages as microbial biofilms. In particular, scum layers mediate diffusion with the wider environments, favouring preservation and sharing of early informational molecules, along with the selective concentration of compatible prebiotic compounds. Biofilms are among the earliest traces imprinted by life in the rock record: we contend that prebiotic equivalents of these environments deserve future experimental investigation.

摘要

生物能膜的区室化是生命的一个普遍特征。因此,益生元系统最终的区室化常被认为是生命起源过程中的关键一步。区室可能是益生元化学的积极参与者,能浓缩关键反应物并在空间上对其进行组织。然而,大多数在益生元条件下看似合理的区室是有渗漏的或不稳定的,这限制了它们的实用性。在此,我们针对生命起源环境提出了一个新假说,该假说利用了益生元区室的优势并减轻了其局限性:近地表环境中的多区室化层——一种“浮沫”。浮沫型环境受益于许多与微生物生物膜相同的基于整体的优势。特别是,浮沫层介导与更广阔环境的扩散,有利于早期信息分子的保存和共享,以及兼容的益生元化合物的选择性浓缩。生物膜是生命在岩石记录中留下的最早痕迹之一:我们认为这些环境的益生元等效物值得未来进行实验研究。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/7d37/8472051/153653b1592b/life-11-00976-g001.jpg

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