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早期的光合真核生物栖息在低盐度的生境中。

Early photosynthetic eukaryotes inhabited low-salinity habitats.

机构信息

School of Geographical Sciences, University of Bristol, Bristol BS8 1SS, United Kingdom;

Division of Plant Science, University of Dundee at the James Hutton Institute, Dundee DD2 5DA, United Kingdom.

出版信息

Proc Natl Acad Sci U S A. 2017 Sep 12;114(37):E7737-E7745. doi: 10.1073/pnas.1620089114. Epub 2017 Aug 14.

Abstract

The early evolutionary history of the chloroplast lineage remains an open question. It is widely accepted that the endosymbiosis that established the chloroplast lineage in eukaryotes can be traced back to a single event, in which a cyanobacterium was incorporated into a protistan host. It is still unclear, however, which Cyanobacteria are most closely related to the chloroplast, when the plastid lineage first evolved, and in what habitats this endosymbiotic event occurred. We present phylogenomic and molecular clock analyses, including data from cyanobacterial and chloroplast genomes using a Bayesian approach, with the aim of estimating the age for the primary endosymbiotic event, the ages of crown groups for photosynthetic eukaryotes, and the independent incorporation of a cyanobacterial endosymbiont by Our analyses include both broad taxon sampling (119 taxa) and 18 fossil calibrations across all Cyanobacteria and photosynthetic eukaryotes. Phylogenomic analyses support the hypothesis that the chloroplast lineage diverged from its closet relative , a basal cyanobacterial lineage, ∼2.1 billion y ago (Bya). Our analyses suggest that the Archaeplastida, consisting of glaucophytes, red algae, green algae, and land plants, share a common ancestor that lived ∼1.9 Bya. Whereas crown group Rhodophyta evolved in the Mesoproterozoic Era (1,600-1,000 Mya), crown groups Chlorophyta and Streptophyta began to radiate early in the Neoproterozoic (1,000-542 Mya). Stochastic mapping analyses indicate that the first endosymbiotic event occurred in low-salinity environments. Both red and green algae colonized marine environments early in their histories, with prasinophyte green phytoplankton diversifying 850-650 Mya.

摘要

叶绿体谱系的早期进化历史仍然是一个悬而未决的问题。人们普遍认为,在真核生物中建立叶绿体谱系的内共生关系可以追溯到一个单一的事件,即一个蓝细菌被纳入一个原生动物宿主。然而,仍然不清楚哪些蓝细菌与叶绿体最密切相关,质体谱系最初是何时进化的,以及这种内共生事件发生在什么生境中。我们使用贝叶斯方法进行了系统基因组学和分子钟分析,包括来自蓝细菌和叶绿体基因组的数据,目的是估计主要内共生事件的年龄、光合真核生物的冠群年龄以及独立纳入蓝细菌内共生体的时间。我们的分析包括广泛的分类群采样(119 个分类群)和跨所有蓝细菌和光合真核生物的 18 个化石校准。系统基因组学分析支持这样的假设,即叶绿体谱系与最接近的亲缘关系——一个基础蓝细菌谱系——在大约 21 亿年前(Bya)分化。我们的分析表明,古生菌门由蓝藻、红藻、绿藻和陆地植物组成,它们有一个共同的祖先,生活在大约 19 亿年前。而红藻冠群在中元古代(16 亿至 1000 万年前)进化,绿藻和链形植物冠群在新元古代早期(1000 万至 542 万年前)开始辐射。随机映射分析表明,第一次内共生事件发生在低盐度环境中。红藻和绿藻在其历史早期就已经殖民到海洋环境中,而前绿藻浮游植物在 8.5 亿至 6.5 亿年前多样化。

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