Dynamics of the osmotic lysis of mineral protocells and its avoidance at the origins of life

IF 2.7 2区 地球科学 Q2 BIOLOGY Geobiology Pub Date : 2024-07-17 DOI:10.1111/gbi.12611
Yang Ding, Silvana S. S. Cardoso, Julyan H. E. Cartwright
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Abstract

The osmotic rupture of a cell, its osmotic lysis or cytolysis, is a phenomenon that active biological cell volume regulation mechanisms have evolved in the cell membrane to avoid. How then, at the origin of life, did the first protocells survive prior to such active processes? The pores of alkaline hydrothermal vents in the oceans form natural nanoreactors in which osmosis across a mineral membrane plays a fundamental role. Here, we discuss the dynamics of lysis and its avoidance in an abiotic system without any active mechanisms, reliant upon self-organized behaviour, similar to the first self-organized mineral membranes within which complex chemistry may have begun to evolve into metabolism. We show that such mineral nanoreactors could function as protocells without exploding because their self-organized dynamics have a large regime in parameter space where osmotic lysis does not occur and homeostasis is possible. The beginnings of Darwinian evolution in proto-biochemistry must have involved the survival of protocells that remained within such a safe regime.

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矿物原生细胞的渗透溶解动力学及其在生命起源过程中的避免。
细胞的渗透破裂,即渗透溶解或细胞溶解,是细胞膜中进化出的主动生物细胞体积调节机制所要避免的现象。那么,在生命起源时,第一批原生细胞是如何在这种主动过程之前存活下来的呢?海洋中碱性热液喷口的孔隙形成了天然的纳米反应器,其中矿物膜上的渗透起着根本性的作用。在这里,我们讨论了在一个没有任何主动机制的非生物系统中,依赖自组织行为的溶解动力学及其避免,类似于复杂化学可能已开始进化为新陈代谢的第一种自组织矿物膜。我们的研究表明,这种矿物纳米反应器可以作为原电池而不发生爆炸,因为它们的自组织动力学在参数空间有一个很大的范围,在这个范围内不会发生渗透溶解,而且可以实现平衡。达尔文进化论在原生物化学中的开端肯定涉及到保持在这种安全机制内的原细胞的生存。
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来源期刊
Geobiology
Geobiology 生物-地球科学综合
CiteScore
6.80
自引率
5.40%
发文量
56
审稿时长
3 months
期刊介绍: The field of geobiology explores the relationship between life and the Earth''s physical and chemical environment. Geobiology, launched in 2003, aims to provide a natural home for geobiological research, allowing the cross-fertilization of critical ideas, and promoting cooperation and advancement in this emerging field. We also aim to provide you with a forum for the rapid publication of your results in an international journal of high standing. We are particularly interested in papers crossing disciplines and containing both geological and biological elements, emphasizing the co-evolutionary interactions between life and its physical environment over geological time. Geobiology invites submission of high-quality articles in the following areas: Origins and evolution of life Co-evolution of the atmosphere, hydrosphere and biosphere The sedimentary rock record and geobiology of critical intervals Paleobiology and evolutionary ecology Biogeochemistry and global elemental cycles Microbe-mineral interactions Biomarkers Molecular ecology and phylogenetics.
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Issue Information Significance of lignin and fungal markers in the Devonian (407 Ma) Rhynie Chert Controls on authigenic mineralization in experimental Ediacara-style preservation Lateral redox variability in ca. 1.9 Ga marine environments indicated by organic carbon and nitrogen isotope compositions Featured Cover
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