The early Earth atmosphere and early life catalysts.

Sandra Ignacia Ramírez Jiménez
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Abstract

Homochirality is a property of living systems on Earth. The time, the place, and the way in which it appeared are uncertain. In a prebiotic scenario two situations are of interest: either an initial small bias for handedness of some biomolecules arouse and progressed with life, or an initial slight excess led to the actual complete dominance of the known chiral molecules. A definitive answer can probably never be given, neither from the fields of physics and chemistry nor biology. Some arguments can be advanced to understand if homochirality is necessary for the initiation of a prebiotic homochiral polymer chemistry, if this homochirality is suggesting a unique origin of life, or if a chiral template such as a mineral surface is always required to result in an enantiomeric excess. A general description of the early Earth scenario will be presented in this chapter, followed by a general description of some clays, and their role as substrates to allow the concentration and amplification of some of the building blocks of life.

早期地球的大气和早期生命的催化剂。
同手性是地球上生命系统的一个特性。它出现的时间、地点和方式都不确定。在益生元的情况下,有两种情况值得关注:一种是一些生物分子最初对手性的轻微偏向,并随着生命的发展而发展;另一种是最初的轻微偏向导致已知手性分子实际上完全占据主导地位。一个明确的答案可能永远无法给出,无论是从物理、化学还是生物学领域。可以提出一些争论,以了解是否同手性对于原生生物的同手性聚合物化学的开始是必要的,如果这种同手性暗示了生命的独特起源,或者如果手性模板(如矿物表面)总是需要导致对映体过量。本章将对早期地球的情况进行一般性描述,然后是对一些粘土的一般性描述,以及它们作为基质的作用,使生命的一些组成部分得以集中和扩增。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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