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首页> 外文期刊>Zoologica Scripta: An International Journal of Evolutionary Zoology >A molecular phylogeny of heterodont bivalves (Mollusca : Bivalvia : Heterodonta): new analyses of 18S and 28S rRNA genes
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A molecular phylogeny of heterodont bivalves (Mollusca : Bivalvia : Heterodonta): new analyses of 18S and 28S rRNA genes

机译:异齿双壳类的分子系统发育(软体动物:双壳纲:杂齿齿科):18S和28S rRNA基因的新分析

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摘要

A new molecular phylogeny is presented for the highly diverse, bivalve molluscan subclass Heterodonta. The study, the most comprehensive for heterodonts to date, used new sequences of 18S and 28S rRNA genes for 103 species from 49 family groups with species of Palaeo-heterodonta (Trigoniidae, Margaritiferidae and Unionidae) as outgroups. Results confirm previous analyses that the Carditidae/Astartidae/Crassatellidae clade is basal to all other heterodonts including Anomalodesmata (often classified as a separate subclass or order). Thyasiroidea occupy a near basal position between the Crassatelloidea and Anomalodesmata. Lucinidae form a well-supported monophyletic group distinct from Thyasiridae and Ungulinidae. The Solenoidea and Hiatelloidea link as sister groups distant from the Tellinoidea and Myoidea, respectively, where they had been previously associated. The position of the Gastrochaenidae is unstable but does not group with myoidean taxa. Species of four families of Galeommatoidea form a clade that also includes Sportellidae of the Cyamioidea. The Cardioidea and Tellinoidea form highly supported, long branched, individual clades but group as sister taxa. A major clade including Veneroidea, Mactroidea, Myoidea and other families is given the unranked name Neoheterodontei. There is no support for a separate order Myoida (Myoidea and Pholadoidea). Dreissenidae group within the clade including Myidae, Corbulidae, Pholadidae and Teredinidae. The Corbiculoidea is confirmed as polyphyletic with the Sphaeriidae and Corbiculidae forming separate clades within the Neoheterodontei; Corbiculidae grouping with the Glauconomidae. Hemidonacidae are unrelated to the Cardiidae, as previously proposed, but nest within the Neoheterodontei. The Gaimardiidae group near to the Ungulinidae and not with Cyamioidea where most recently classified. The family Ungulinidae, previously classified in the Lucinoidea, forms a well-supported clade within the Neoheterodontei and is elevated to superfamily rank - Ungulinoidea. The monophyletic status of Glossoidea, Arcticoidea and Veneroidea is unconfirmed. A brief review of the fossil record of the heterodonts indicates that the basal clades of Crassatelloidea, Anomalodesmata and Lucinoidea diverged very early in the Lower Palaeozoic. Other groups such as the Hiatelloidea, Solenoidea, Gastrochaenidae probably were of late Palaeozoic origins. The Cardioidea and Tellinoidea originated in the Triassic while major groups of Neoheterodontei radiated in the Late Mesozoic. The phylogenetic position of the Thyasiroidea and Galeommatoidea suggests a longer fossil history than has so far been recognized.
机译:为高度多样化的双壳贝类软体动物杂齿亚纲提出了一种新的分子系统学。这项研究是迄今为止最全面的杂种动物研究,使用了49种科的103种18S和28S rRNA基因的新序列,其中古杂种(Trigoniidae,Margaritiferidae和Unionidae)为外群。结果证实了先前的分析,即it科/ A科/ Cr科的进化枝是包括异齿线虫在内的所有其他异齿类的基础(通常被分类为单独的子类或顺序)。 y虫在Crassatelloidea和Anomalodesmata之间占据近乎基础的位置。 Lucinidae形成一个与Thyasiridae和Ungulinidae不同的,得到良好支持的单系统群体。斑纹目纲和link纲目结为姐妹群,它们分别远离Tellinoidea和Myoidea,它们之前曾在这里联系在一起。 Gastrochaenidae的位置不稳定,但不与类肌体类群合在一起。 Galeommatoidea的四个科的物种形成一个进化枝,其中还包括Cyamioidea的Sportellidae。 Cardioidea和Tellinoidea形成高度支持的长分支个体分支,但作为姊妹类群。包括Veneroidea,Mactroidea,Myoidea和其他家族在内的主要分支被赋予了新等级杂种动物新杂种齿。不支持单独订购Myoida(Myoidea和Pholadoidea)。进化枝中的Dreissenidae群包括Myidae,Corbulidae,Pholadidae和Teredinidae。确认Corbiculoidea是多系的,在新杂齿科内,Sphaeriidae和Corbiculidae形成单独的进化枝。 bic科与绿头科。正如先前所提出的那样,He酸科与to科无关,但巢在新杂齿科内。 Gaimardiidae组靠近Ungulinidae,而不是最近分类的Cyamioidea。 Ungulinidae家族,以前被归类为Lucinoidea,在新异齿龙科内形成了一个有良好支撑的进化枝,并被提升为Ungulinoidea超家族。尚不确定鹰嘴豆科,弧菌和委内瑞拉的单系状态。简要回顾一下异齿动物的化石记录,可以发现,古生代下层很早就出现了Crassatelloidea,Anomalodesmata和Lucinoidea的基面分支。其他种类,如犬齿亚目(Hatelloidea),石斑亚目(Selenoidea),天麻科(Gastrochaenidae),可能是古生代晚期。心脏亚目和碲亚目起源于三叠纪,而新杂齿齿科的主要群体在中生代晚期辐射。 Thyasiroidea和Galeommatoidea的系统发育位置表明,化石历史比迄今为止公认的历史更长。

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