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广泛的分类群采样的质体系统基因组学进一步阐明了次生质体独特的进化起源和时间。

Plastid phylogenomics with broad taxon sampling further elucidates the distinct evolutionary origins and timing of secondary green plastids.

机构信息

School of Biosciences, University of Melbourne, Melbourne, Victoria, 3010, Australia.

Department of Organismic and Evolutionary Biology, Harvard University, Cambridge, Massachusetts, 02138, USA.

出版信息

Sci Rep. 2018 Jan 24;8(1):1523. doi: 10.1038/s41598-017-18805-w.

DOI:10.1038/s41598-017-18805-w
PMID:29367699
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC5784168/
Abstract

Secondary plastids derived from green algae occur in chlorarachniophytes, photosynthetic euglenophytes, and the dinoflagellate genus Lepidodinium. Recent advances in understanding the origin of these plastids have been made, but analyses suffer from relatively sparse taxon sampling within the green algal groups to which they are related. In this study we aim to derive new insights into the identity of the plastid donors, and when in geological time the independent endosymbiosis events occurred. We use newly sequenced green algal chloroplast genomes from carefully chosen lineages potentially related to chlorarachniophyte and Lepidodinium plastids, combined with recently published chloroplast genomes, to present taxon-rich phylogenetic analyses to further pinpoint plastid origins. We integrate phylogenies with fossil information and relaxed molecular clock analyses. Our results indicate that the chlorarachniophyte plastid may originate from a precusor of siphonous green algae or a closely related lineage, whereas the Lepidodinium plastid originated from a pedinophyte. The euglenophyte plastid putatively originated from a lineage of prasinophytes within the order Pyramimonadales. Our molecular clock analyses narrow in on the likely timing of the secondary endosymbiosis events, suggesting that the event leading to Lepidodinium likely occurred more recently than those leading to the chlorarachniophyte and photosynthetic euglenophyte lineages.

摘要

次生质体来源于绿藻发生在 Chlorarachniophytes、光合 Euglenophytes 和甲藻属 Lepidodinium。对这些质体起源的理解最近取得了进展,但分析受到与它们相关的绿藻群内相对稀疏的分类群采样的限制。在这项研究中,我们旨在深入了解质体供体的身份,以及独立内共生事件发生的地质时间。我们使用新测序的绿藻叶绿体基因组,来自与 Chlorarachniophyte 和 Lepidodinium 质体可能相关的精心挑选的谱系,结合最近发表的叶绿体基因组,进行了分类群丰富的系统发育分析,以进一步确定质体的起源。我们将系统发育与化石信息和松弛分子钟分析相结合。我们的结果表明,Chlorarachniophyte 质体可能起源于虹吸管状绿藻或密切相关的谱系的前体,而 Lepidodinium 质体起源于 pedinophyte。Euglenophyte 质体可能起源于 Pyramimonadales 目中的一个前绿藻谱系。我们的分子钟分析缩小了可能的二次内共生事件的时间范围,表明导致 Lepidodinium 的事件发生的时间比导致 Chlorarachniophyte 和光合 Euglenophyte 谱系的事件更近。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/5dde/5784168/667050a39ad8/41598_2017_18805_Fig2_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/5dde/5784168/667050a39ad8/41598_2017_18805_Fig2_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/5dde/5784168/667050a39ad8/41598_2017_18805_Fig2_HTML.jpg

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