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Evidence of transoceanic dispersion of the genus Vanilla based on plastid DNA phylogenetic analysis

机译:基于质体DNA系统发育分析的香草属越洋分散体的证据

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摘要

The phylogeny and the biogeographical history of the genus Vanilla was investigated using four chloroplastic genes (psbB, psbC; psaB and rbcL), on 47 accessions of Vanilla chosen from the ex situ CIRAD collection maintained in Reunion Island and additional sequences from GenBank. Bayesian methods provided a fairly well supported reconstruction of the phylogeny of the Vanilloideae sub-family and more particularly of the genus Vanilla. Three major phylogenetic groups in the genus Vanilla were differentiated, which is in disagreement with the actual classification in two sections (Foliosae and Aphyllae) based on morphological traits. Recent Bayesian relaxed molecular clock methods allowed to test the two main hypotheses of the phylogeography of the genus Vanilla. Early radiation of the Vanilla genus and diversification by vicariance consecutive to the break-up of Gondwana, 95 million years ago (Mya), was incompatible with the admitted age of origin of Angiosperm. Based on the Vanilloideae age recently estimated to 71 million years ago (Mya), we conclude that the genus Vanilla would have appeared ~34 Mya in South America, when continents were already separated. Nevertheless, whatever the two extreme scenarios tested, at least three long distance migration events are needed to explain the present distribution of Vanilla species in tropical areas. These transoceanic dispersions could have occurred via transoceanic passageway such as the Rio Grande Ridge and the involvement of floating vegetation mats and migratory birds.
机译:使用四个叶绿体基因(psbB,psbC,psaB和rbcL),研究了香草属的系统发育和生物地理史,研究对象是留尼汪岛的异地CIRAD收集的47种香草,以及GenBank的其他序列。贝叶斯方法为香草科亚科,特别是香草属的系统发育提供了相当好的支持。区分了香草属中的三个主要系统发育组,这与基于形态特征的两个部分(叶和叶)的实际分类不一致。最近的贝叶斯松弛分子钟方法允许测试香草属系统地理学的两个主要假设。早在9500万年前的冈瓦纳解体后,香草属的早期辐射和由变异引起的多样化(Mya)与被子植物的起源年龄不符。根据最近估计存在于7100万年前(Mya)的香草科年龄,我们得出结论,当南美大陆已经分开时,香草属会在〜34 Mya出现。尽管如此,无论所测试的两种极端情况如何,都至少需要三个远距离迁移事件来解释热带地区香草物种的当前分布。这些越洋分散体可能是通过诸如Rio Grande Ridge之类的越洋通道以及漂浮的植被垫和候鸟的参与而发生的。

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