Protometabolism as out-of-equilibrium chemistry

S. Nader, L. Sebastianelli, S. Mansy
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引用次数: 3

Abstract

It is common to compare life with machines. Both consume fuel and release waste to run. In biology, the engine that drives the living system is referred to as metabolism. However, attempts at deciphering the origins of metabolism do not focus on this energetic relationship that sustains life but rather concentrate on nonenzymatic reactions that produce all the intermediates of an extant metabolic pathway. Such an approach is akin to studying the molecules produced from the burning of coal instead of deciphering how the released energy drives the movement of pistons and ultimately the train when investigating the mechanisms behind locomotion. Theories that do explicitly invoke geological chemical gradients to drive metabolism most frequently feature hydrothermal vent conditions, but hydrothermal vents are not the only regions of the early Earth that could have provided the fuel necessary to sustain the Earth's first (proto)cells. Here, we give examples of prior reports on protometabolism and highlight how more recent investigations of out-of-equilibrium systems may point to alternative scenarios more consistent with the majority of prebiotic chemistry data accumulated thus far. This article is part of the theme issue ‘Emergent phenomena in complex physical and socio-technical systems: from cells to societies’.
原代谢是不平衡的化学反应
把生命比作机器是很常见的。两者都消耗燃料并释放废物来运行。在生物学中,驱动生命系统的引擎被称为新陈代谢。然而,破译代谢起源的尝试并不集中在维持生命的能量关系上,而是集中在产生现存代谢途径中所有中间体的非酶反应上。这种方法类似于研究煤炭燃烧产生的分子,而不是在研究运动背后的机制时破译释放的能量如何驱动活塞和最终驱动火车的运动。明确引用地质化学梯度来驱动新陈代谢的理论最常以热液喷口为特征,但热液喷口并不是早期地球唯一能够提供维持地球第一个(原型)细胞所需燃料的区域。在这里,我们给出了关于原代谢的先前报告的例子,并强调了最近对非平衡系统的研究如何指出与迄今为止积累的大多数益生元化学数据更一致的替代方案。本文是主题“复杂物理和社会技术系统中的涌现现象:从细胞到社会”的一部分。
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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