砾岩和外消旋化合物对过量氨基酸对映体的顺序扩增:迈向手性的合理益生途径。

IF 1.9 4区 物理与天体物理 Q2 BIOLOGY
A Sharma
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引用次数: 0

摘要

一些氨基酸可以从水溶液中结晶为砾岩和外消旋化合物:在快速蒸发后的高过饱和度下,通过多孔沙坝排出的溶解氨基酸表现得像砾岩,而在由此形成的更深的水池中,氨基酸溶液切换到更常见的外消旋化合物体系。我们展示了这两种形式如何在益生元条件下顺序结合,形成同手性的基础。本文对这种氨基酸的双重行为能够串联产生的对映体过量(EE)进行了定量分析:在砾岩系统(CS)中通过优先结晶(PC)进行初始扩增,然后在外消旋化合物系统(RCS)中进一步扩增。以天冬氨酸为模型体系,三元相图显示,溶液EE在RCS共晶点达到50%的最大值,CS中需要1.65的最小过饱和度。导出了该阈值过饱和度与CS和RCS的共晶溶解度的关系式。对于给定的CS中的过饱和,还导出了在CS切换到RCS之前PC必须产生的最小解EE的关系式。对于天冬氨酸中分别为2、5、10的过饱和度,计算出所需的PC诱导的阈值溶液EE为0.194、0.070、0.033。从CS切换到RCS进一步放大了溶液EE,导致天冬氨酸溶液EE从CS中的接近零增长到RCS中的约50%。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Sequential Amplification of Amino Acid Enantiomeric Excess by Conglomerate and Racemic Compound: Plausible Prebiotic Route Towards Homochirality.

Sequential Amplification of Amino Acid Enantiomeric Excess by Conglomerate and Racemic Compound: Plausible Prebiotic Route Towards Homochirality.

Some amino acids can crystallize from aqueous solution both as conglomerates and racemic compounds: under high supersaturation following rapid evaporation, dissolved amino acids draining over porous sand-bars behave like conglomerates whereas in the resulting deeper pool of water, amino acid solution switches to the more common racemic-compound system. We show how the two forms might have sequentially combined under prebiotic conditions to form the basis of homochirality. The paper is a quantitative analysis of enantiomeric excess (EE) this dual behavior of amino acids is capable of producing in tandem: Initial amplification by preferential crystallization (PC) in conglomerate system (CS) followed by further amplification in the racemic compound system (RCS). Using aspartic acid as a model system, ternary phase diagram shows that a minimum supersaturation of 1.65 is required in the CS for the solution-EE to reach its maximum value of 50% at the RCS eutectic point. A relationship is derived for the dependence of this threshold supersaturation on the eutectic solubilities of CS and RCS. For given supersaturation in CS, a relation is also derived for minimum solution-EE that must be produced by PC before CS switches to RCS. Required PC-induced threshold solution-EE of 0.194, 0.070, 0.033 is calculated for supersaturation of 2, 5, 10 respectively in aspartic acid. Switching from CS to RCS further amplifies solution-EE, resulting in an overall growth of aspartic acid solution EE from near-zero in CS to around 50% in RCS.

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来源期刊
CiteScore
3.20
自引率
15.00%
发文量
12
审稿时长
>12 weeks
期刊介绍: The subject of the origin and early evolution of life is an inseparable part of the general discipline of Astrobiology. The journal Origins of Life and Evolution of Biospheres places special importance on the interconnection as well as the interdisciplinary nature of these fields, as is reflected in its subject coverage. While any scientific study which contributes to our understanding of the origins, evolution and distribution of life in the Universe is suitable for inclusion in the journal, some examples of important areas of interest are: prebiotic chemistry and the nature of Earth''s early environment, self-replicating and self-organizing systems, the theory of the RNA world and of other possible precursor systems, and the problem of the origin of the genetic code. Early evolution of life - as revealed by such techniques as the elucidation of biochemical pathways, molecular phylogeny, the study of Precambrian sediments and fossils and of major innovations in microbial evolution - forms a second focus. As a larger and more general context for these areas, Astrobiology refers to the origin and evolution of life in a cosmic setting, and includes interstellar chemistry, planetary atmospheres and habitable zones, the organic chemistry of comets, meteorites, asteroids and other small bodies, biological adaptation to extreme environments, life detection and related areas. Experimental papers, theoretical articles and authorative literature reviews are all appropriate forms for submission to the journal. In the coming years, Astrobiology will play an even greater role in defining the journal''s coverage and keeping Origins of Life and Evolution of Biospheres well-placed in this growing interdisciplinary field.
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