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追溯叶绿体蓝藻祖先的年代。

Dating the cyanobacterial ancestor of the chloroplast.

机构信息

Instituto de Ecología, Universidad Nacional Autónoma de México. 3er Circuito Exterior sn, Ciudad Universitaria, Mexico.

出版信息

ISME J. 2010 Jun;4(6):777-83. doi: 10.1038/ismej.2010.2. Epub 2010 Mar 4.

Abstract

Cyanobacteria have had a pivotal role in the history of life on Earth being the first organisms to perform oxygenic photosynthesis, which changed the atmospheric chemistry and allowed the evolution of aerobic Eukarya. Chloroplasts are the cellular organelles of photoautotrophic eukaryotes in which most portions of photosynthesis occur. Although the initial suggestion that cyanobacteria are the ancestors of chloroplasts was greeted with skepticism, the idea is now widely accepted. Here we attempt to resolve and date the cyanobacterial ancestry of the chloroplast using phylogenetic analysis and molecular clocks. We found that chloroplasts form a monophyletic lineage, are most closely related to subsection-I, N(2)-fixing unicellular cyanobacteria (Order Chroococcales), and heterocyst-forming Order Nostocales cyanobacteria are their sister group. Nostocales and Chroococcales appeared during the Paleoproterozoic and chloroplasts appeared in the mid-Proterozoic. The capability of N(2) fixation in cyanobacteria may have appeared only once during the late Archaean and early Proterozoic eons. Furthermore, we found that oxygen-evolving cyanobacteria could have appeared in the Archaean. Our results suggest that a free-living cyanobacterium with the capacity to store starch through oxygenic CO(2) fixation, and to fix atmospheric N(2), would be a very important intracellular acquisition, which, as can be recounted today from several lines of evidence, would have become the chloroplast by endosymbiosis.

摘要

蓝藻在地球生命史上起着关键作用,是最早进行产氧光合作用的生物,这改变了大气化学性质,使需氧真核生物得以进化。叶绿体是进行光合作用的真核生物的细胞细胞器。虽然最初关于蓝藻是叶绿体祖先的观点受到了质疑,但现在这个观点已被广泛接受。在这里,我们试图通过系统发育分析和分子钟来解决和确定叶绿体的蓝藻祖先。我们发现,叶绿体形成一个单系群,与固氮的单细胞蓝藻(Chroococcales 目)的 I 亚组最为密切相关,异形胞形成的 Nostocales 蓝藻是其姊妹群。 Nostocales 和 Chroococcales 出现在古元古代,而叶绿体出现在中元古代。蓝藻固氮能力可能只在晚太古宙和早元古代出现过一次。此外,我们发现产氧蓝藻可能出现在太古宙。我们的结果表明,一种能够通过产氧 CO2 固定储存淀粉和固定大气 N2 的自由生活蓝藻,将是一种非常重要的细胞内获得物,正如今天从几条证据线索中可以看到的那样,它将通过内共生成为叶绿体。

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