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古菌甲烷代谢的演变观点。

An evolving view of methane metabolism in the Archaea.

机构信息

Australian Centre for Ecogenomics, School of Chemistry and Molecular Biosciences, University of Queensland, St Lucia, Queensland, Australia.

出版信息

Nat Rev Microbiol. 2019 Apr;17(4):219-232. doi: 10.1038/s41579-018-0136-7. Epub 2019 Jan 21.

Abstract

Methane is a key compound in the global carbon cycle that influences both nutrient cycling and the Earth's climate. A limited number of microorganisms control the flux of biologically generated methane, including methane-metabolizing archaea that either produce or consume methane. Methanogenic and methanotrophic archaea belonging to the phylum Euryarchaeota share a genetically similar, interrelated pathway for methane metabolism. The key enzyme in this pathway, the methyl-coenzyme M reductase (Mcr) complex, catalyses the last step in methanogenesis and the first step in methanotrophy. The discovery of mcr and divergent mcr-like genes in new euryarchaeotal lineages and novel archaeal phyla challenges long-held views of the evolutionary origin of this metabolism within the Euryarchaeota. Divergent mcr-like genes have recently been shown to oxidize short-chain alkanes, indicating that these complexes have evolved to metabolize substrates other than methane. In this Review, we examine the diversity, metabolism and evolutionary history of mcr-containing archaea in light of these recent discoveries.

摘要

甲烷是全球碳循环中的一种关键化合物,它影响着营养物质循环和地球气候。少数微生物控制着生物产生的甲烷通量,包括产生或消耗甲烷的甲烷代谢古菌。属于广古菌门的产甲烷菌和甲烷营养菌共享一种遗传上相似的、相互关联的甲烷代谢途径。该途径中的关键酶是甲基辅酶 M 还原酶(Mcr)复合物,它催化产甲烷作用的最后一步和甲烷营养作用的第一步。在新的广古菌谱系和新的古菌门中发现的 mcr 和不同的 mcr 样基因,挑战了长期以来在广古菌门中对这种代谢进化起源的观点。最近发现,不同的 mcr 样基因能够氧化短链烷烃,这表明这些复合物已经进化为代谢除甲烷以外的底物。在这篇综述中,我们根据这些新发现,考察了含 mcr 的古菌的多样性、代谢和进化历史。

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