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Prediction of the Maximum Temperature for Life Based on the Stability of Metabolites to Decomposition in Water

机译:基于代谢产物在水中分解的稳定性来预测最高寿命温度

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摘要

The components of life must survive in a cell long enough to perform their function in that cell. Because the rate of attack by water increases with temperature, we can, in principle, predict a maximum temperature above which an active terrestrial metabolism cannot function by analysis of the decomposition rates of the components of life, and comparison of those rates with the metabolites’ minimum metabolic half-lives. The present study is a first step in this direction, providing an analytical framework and method, and analyzing the stability of 63 small molecule metabolites based on literature data. Assuming that attack by water follows a first order rate equation, we extracted decomposition rate constants from literature data and estimated their statistical reliability. The resulting rate equations were then used to give a measure of confidence in the half-life of the metabolite concerned at different temperatures. There is little reliable data on metabolite decomposition or hydrolysis rates in the literature, the data is mostly confined to a small number of classes of chemicals, and the data available are sometimes mutually contradictory because of varying reaction conditions. However, a preliminary analysis suggests that terrestrial biochemistry is limited to environments below ~150–180 °C. We comment briefly on why pressure is likely to have a small effect on this.
机译:生命的组成部分必须在一个细胞中生存足够长的时间,以在该细胞中执行其功能。由于水的攻击速率随温度增加,因此,我们可以通过分析生命各部分的分解速率并将这些速率与代谢物的速率进行比较,来原则上预测最高温度,在该温度以上,活跃的陆地代谢将无法起作用最小代谢半衰期。本研究是朝这个方向迈出的第一步,提供了一个分析框架和方法,并根据文献数据分析了63种小分子代谢物的稳定性。假设水的侵蚀遵循一阶速率方程,我们从文献数据中提取分解速率常数,并估计其统计可靠性。然后将所得的速率方程式用于在不同温度下对相关代谢物半衰期的置信度。文献中关于代谢物分解或水解速率的可靠数据很少,该数据主要限于少数几类化学品,并且由于反应条件的不同,可获得的数据有时相互矛盾。但是,初步分析表明,陆地生物化学仅限于〜150–180°C以下的环境。我们简要评论一下为什么压力可能对此产生很小的影响。

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