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细胞色素氧化酶的进化,一种比大气中的氧气还要古老的酶。

Evolution of cytochrome oxidase, an enzyme older than atmospheric oxygen.

作者信息

Castresana J, Lübben M, Saraste M, Higgins D G

机构信息

European Molecular Biology Laboratory, Heidelberg, Germany.

出版信息

EMBO J. 1994 Jun 1;13(11):2516-25. doi: 10.1002/j.1460-2075.1994.tb06541.x.

Abstract

Cytochrome oxidase is a key enzyme in aerobic metabolism. All the recorded eubacterial (domain Bacteria) and archaebacterial (Archaea) sequences of subunits 1 and 2 of this protein complex have been used for a comprehensive evolutionary analysis. The phylogenetic trees reveal several processes of gene duplication. Some of these are ancient, having occurred in the common ancestor of Bacteria and Archaea, whereas others have occurred in specific lines of Bacteria. We show that eubacterial quinol oxidase was derived from cytochrome c oxidase in Gram-positive bacteria and that archaebacterial quinol oxidase has an independent origin. A considerable amount of evidence suggests that Proteobacteria (Purple bacteria) acquired quinol oxidase through a lateral gene transfer from Gram-positive bacteria. The prevalent hypothesis that aerobic metabolism arose several times in evolution after oxygenic photosynthesis, is not sustained by two aspects of the molecular data. First, cytochrome oxidase was present in the common ancestor of Archaea and Bacteria whereas oxygenic photosynthesis appeared in Bacteria. Second, an extant cytochrome oxidase in nitrogen-fixing bacteria shows that aerobic metabolism is possible in an environment with a very low level of oxygen, such as the root nodules of leguminous plants. Therefore, we propose that aerobic metabolism in organisms with cytochrome oxidase has a monophyletic and ancient origin, prior to the appearance of eubacterial oxygenic photosynthetic organisms.

摘要

细胞色素氧化酶是有氧代谢中的关键酶。该蛋白质复合物亚基1和亚基2的所有已记录的真细菌(细菌域)和古细菌(古菌)序列都已用于全面的进化分析。系统发育树揭示了几个基因复制过程。其中一些是古老的,发生在细菌和古菌的共同祖先中,而其他一些则发生在特定的细菌谱系中。我们表明,真细菌喹啉氧化酶源自革兰氏阳性细菌中的细胞色素c氧化酶,而古细菌喹啉氧化酶有独立的起源。大量证据表明,变形菌(紫色细菌)通过从革兰氏阳性细菌的水平基因转移获得了喹啉氧化酶。有氧代谢在光合放氧之后在进化中多次出现这一普遍假设,在分子数据的两个方面得不到支持。第一,细胞色素氧化酶存在于古菌和细菌的共同祖先中,而光合放氧出现在细菌中。第二,固氮细菌中现存的细胞色素氧化酶表明,在氧气水平非常低的环境中,如有豆科植物的根瘤中,有氧代谢是可能的。因此,我们提出,具有细胞色素氧化酶的生物体中的有氧代谢具有单系且古老的起源,早于真细菌光合放氧生物的出现。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/b9a5/395125/9b4ba6427dc8/emboj00059-0042-a.jpg

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