首页> 外文期刊>Molecular biology and evolution >Evolutionary History of True Crabs (Crustacea: Decapoda: Brachyura) and the Origin of Freshwater Crabs
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Evolutionary History of True Crabs (Crustacea: Decapoda: Brachyura) and the Origin of Freshwater Crabs

机译:真蟹(甲壳纲:十足目:Brachyura)的进化历史和淡水蟹的起源

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摘要

Crabs of the infra-order Brachyura are one of the most diverse groups of crustaceans with approximately 7,000 described species in 98 families, occurring in marine, freshwater, and terrestrial habitats. The relationships among the brachyuran families are poorly understood due to the high morphological complexity of the group. Here, we reconstruct the most comprehensive phylogeny of Brachyura to date using sequence data of six nuclear protein-coding genes and two mitochondrial rRNA genes from more than 140 species belonging to 58 families. The gene tree confirms that the "Podotremata," are paraphyletic. Within the monophyletic Eubrachyura, the reciprocal monophyly of the two subsections, Heterotremata and Thoracotremata, is supported. Monophyly of many superfamilies, however, is not recovered, indicating the prevalence of morphological convergence and the need for further taxonomic studies. Freshwater crabs were derived early in the evolution of Eubrachyura and are shown to have at least two independent origins. Bayesian relaxed molecular methods estimate that freshwater crabs separated from their closest marine sister taxa similar to 135 Ma, that is, after the break up of Pangaea (similar to 200 Ma) and that a Gondwanan origin of these freshwater representatives is untenable. Most extant families and superfamilies arose during the late Cretaceous and early Tertiary.
机译:水下布拉基乌拉蟹是甲壳类动物中种类最多的一组,在98个科中约有7,000种被描述的物种,它们出现在海洋,淡水和陆地生境中。由于群体的高度形态复杂性,人们对短臂类家庭之间的关系了解甚少。在这里,我们使用六个核蛋白编码基因和两个线粒体rRNA基因(来自58个科的140多个物种)的序列数据,重建了Brachyura迄今为止最全面的系统发育。基因树证实“ Podotremata”是共生的。在单系Eubrachyura中,支持了两个部分的异性单异种,即Heterotremata和Thoracotremata。但是,许多超家族的单亲物种没有得到恢复,这表明形态学趋同的普遍性以及进一步分类学研究的必要性。淡水蟹起源于Eubrachyura的进化早期,并显示至少有两个独立的起源。贝叶斯松弛分子方法估计淡水蟹与其最接近的海洋姊妹类群相距约135 Ma,也就是说,在Pangea解体(约200 Ma)之后,这些淡水代表的冈瓦南起源是站不住脚的。在白垩纪晚期和第三纪早期,大多数现存的家庭和超家族出现了。

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