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锰如何与氧气相互作用赋予生命活力(反之亦然)。

How manganese empowered life with dioxygen (and vice versa).

机构信息

Div. of Geological & Planetary Sciences, California Institute of Technology, Pasadena, CA, 91125, USA.

Div. of Geological & Planetary Sciences, California Institute of Technology, Pasadena, CA, 91125, USA.

出版信息

Free Radic Biol Med. 2019 Aug 20;140:113-125. doi: 10.1016/j.freeradbiomed.2019.01.036. Epub 2019 Feb 7.

Abstract

Throughout the history of life on Earth, abiotic components of the environment have shaped the evolution of life, and in turn life has shaped the environment. The element manganese embodies a special aspect of this collaboration; its history is closely entwined with those of photosynthesis and O-two reigning features that characterize the biosphere today. Manganese chemistry was central to the environmental context and evolutionary innovations that enabled the origin of oxygenic photosynthesis and the ensuing rise of O. It was also manganese chemistry that provided an early, fortuitous antioxidant system that was instrumental in how life came to cope with oxidative stress and ultimately thrive in an aerobic world. Subsequently, the presence of O transformed the biogeochemical dynamics of the manganese cycle, enabling a rich suite of environmental and biological processes involving high-valent manganese and manganese redox cycling. Here, we describe insights from chemistry, biology, and geology, to examine manganese dynamics in the environment, and its unique role in the history of life.

摘要

纵观地球生命的历史,环境中的非生物成分塑造了生命的进化,而生命反过来又塑造了环境。元素锰体现了这种相互作用的一个特殊方面;它的历史与光合作用和当今生物圈的主导特征 O 两种的历史紧密交织在一起。锰化学在环境背景和进化创新中起着核心作用,这些创新使产氧光合作用的起源和随之而来的 O 的出现成为可能。也是锰化学提供了一个早期的、偶然的抗氧化系统,这对于生命如何应对氧化应激并最终在有氧环境中茁壮成长至关重要。随后,O 的存在改变了锰循环的生物地球化学动力学,使一系列涉及高价锰和锰氧化还原循环的丰富环境和生物过程成为可能。在这里,我们从化学、生物学和地质学的角度来描述对环境中锰动态及其在生命历史中的独特作用的见解。

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