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亚稳态与晶相形成肽键:对生命起源的启示。

Formation of peptide bonds from metastable versus crystalline phase: implications for the origin of life.

作者信息

Viedma C

机构信息

Departamento Cristalografia-Mineralogia, Universidad Complutense, Facultad Geologia, 28040, Madrid, Spain.

出版信息

Orig Life Evol Biosph. 2000 Dec;30(6):549-56. doi: 10.1023/a:1026595809081.

Abstract

Formation of peptide bonds was attempted by thermal activation of dry amino acids from aqueous solution that simulated prebiotic evaporative environments. The evaporation trend of amino acids solutions shows a bifurcation and can lead to either a crystalline phase (near equilibrium) or a metastable non-crystalline phase (far from equilibrium). Only amino acids in this metastable phase are able to form peptide bonds by thermal activation at temperatures that are generated by solar radiation today. We suggest that this metastable phase is the ideal initial material to trigger amino acid assemblage with protein-like structure because provide the driving force (supersaturation) for an intense interaction between monomers of different amino acids and allows activation of these monomers in plausible prebiotic conditions.

摘要

通过模拟前生物蒸发环境的水溶液对干燥氨基酸进行热活化来尝试形成肽键。氨基酸溶液的蒸发趋势呈现出一种分岔现象,并且能够导致形成结晶相(接近平衡态)或亚稳态非结晶相(远离平衡态)。只有处于这种亚稳态的氨基酸能够在如今由太阳辐射产生的温度下通过热活化形成肽键。我们认为,这种亚稳态是触发具有蛋白质样结构的氨基酸组装的理想初始材料,因为它为不同氨基酸单体之间的强烈相互作用提供了驱动力(过饱和度),并能在合理的前生物条件下使这些单体活化。

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