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首页> 外文期刊>Molecular phylogenetics and evolution >The phylogeny and evolutionary timescale of stoneflies (Insecta: Plecoptera) inferred from mitochondria' genomes
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The phylogeny and evolutionary timescale of stoneflies (Insecta: Plecoptera) inferred from mitochondria' genomes

机译:从线粒体(昆虫:plecoptera)的系统发育和进化时间尺度从线粒体的基因组推断出来

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摘要

Phylogenetic analysis based on mitochondrial genomic data from 25 stonefly species recovered a well-supported tree resolving higher-level relationships within Plecoptera (stoneflies). The monophyly of both currently recognized suborders was strongly supported, concordant with previous molecular analyses of Plecoptera. The southern hemisphere suborder Antarctoperlaria formed two clades: Eustheniidae + Diamphipnoidae and Austroperlidae + Gripopterygidae; consistent with relationships proposed based on morphology. The largely northern hemisphere suborder Arctoperlaria also divided into two groups, Euholognatha and Systellognatha, each composed of the five families traditionally assigned to each infraorder (the placement Scopuridae by mt genome data remains untested at this time). Within Euholognatha, strong support for the Glade Nemouridae + Notonemouridae confirmed the northern origin of the currently southern hemisphere restricted Notonemouridae. Other family level relationships within the Arctoperlaria differ from those recovered by previous morphology and molecular based analyses. A fossil-calibrated divergence estimation suggests the formation of two suborders dates back to the Jurassic (181 Ma), with subsequent diversification of most stonefly families during the Cretaceous. This result confirms the hypothesis that initial divergence between the suborders was driven by the breakup of the supercontinent Pangaea into Laurasia and Gondwanaland (commencing 200 Ma and complete by 150 Ma).
机译:基于25个Theelfly物种的线粒体基因组数据的系统发育分析回收了良好支持的树木,解决了Plecoptera(Stoneflies)的更高级别关系。强烈支持目前公认的副的一定程度的支持,与Plecoptera的先前分子分析一致。南半球亚点南克罗拉利亚成立了两种分子:Eustheniidae + indphipnoidae和austroperlidae + gripopterygae;与基于形态学提出的关系一致。主要是北半球亚达尔阿克拉利亚还分为两组,Euholognatha和Systelloghatha,每个组成的包括传统上分配给每种底刀机的五个家庭(MT基因组数据的放置Scopuridae在此时仍未测试)。在Euholognatha,对Glade Nemouridae + Notonemouridae的强烈支持证实了目前南半球的北头起源受到监禁的Notonemouridae。阿克隆内的其他家庭水平关系与先前形态和基于分子分析回收的那些。化石校准的分歧估计表明,两个汇位的形成可以追溯到侏罗纪(181 mA),随后在白垩纪期间随后多样化大多数石蝇家族。该结果证实了假设,副之间的初始分歧是由超大阴影的破碎驱动到劳拉罗西亚和吉隆坡(开始200 mA并完成150 mA)。

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