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希腊无腿石龙子Ophiomorus punctatissimus(有鳞目:石龙子科)的分子系统发育:爱琴海中脊海沟对其系统地理学的影响。

Molecular phylogeny of the Greek legless skink Ophiomorus punctatissimus (Squamata: Scincidae): the impact of the mid-Aegean trench in its phylogeography.

作者信息

Poulakakis N, Pakaki V, Mylonas M, Lymberakis P

机构信息

Department of Ecology and Evolutionary Biology and Yale Institute of Biospheric Studies, Yale University, New Haven, CT 06520-8106, USA.

出版信息

Mol Phylogenet Evol. 2008 Apr;47(1):396-402. doi: 10.1016/j.ympev.2007.10.014.

Abstract

Sequence data derived from three mitochondrial markers (cytochrome b, 16S rRNA and 12S rRNA genes) were used to infer the evolutionary history of several insular and mainland populations of the Greek legless skink (Ophiomorus punctatissimus), covering most of its distributional range. All phylogenetic analyses produced topologically identical trees that revealed a well-resolved phylogeny. These trees support two O. punctatissimus clades, which are geographically separated (west and east of the mid-Aegean trench). The assumption of a clock-like evolution could not be rejected, and thus a local clock was calibrated for the O. punctatissimus lineages. The non-overlapping geographic distributions of the major clades suggest a spatial and temporal sequence of diversification that coincides with paleogeographic separations during the geological history of the Aegean region. It seems that O. punctatissimus is an old eastern Mediterranean species that has been differentiating in this region at least from middle Miocene. It is possible that the ancestral form of O. punctatissimus invaded the Aegean region from Anatolia before the complete formation of the mid-Aegean trench, when the Aegean was still a uniform landmass, while other vicariant events have led to its present distribution.

摘要

来自三个线粒体标记(细胞色素b、16S rRNA和12S rRNA基因)的序列数据被用于推断希腊无腿石龙子(Ophiomorus punctatissimus)几个岛屿和大陆种群的进化历史,涵盖了其大部分分布范围。所有系统发育分析都产生了拓扑结构相同的树,揭示了一个解析良好的系统发育关系。这些树支持两个O. punctatissimus分支,它们在地理上是分开的(爱琴海海沟中部的西部和东部)。类钟形进化的假设不能被拒绝,因此为O. punctatissimus谱系校准了一个本地时钟。主要分支的非重叠地理分布表明了多样化的空间和时间顺序,这与爱琴海地区地质历史期间的古地理分离相吻合。似乎O. punctatissimus是一种古老的东地中海物种,至少从中新世中期就在该地区分化。有可能O. punctatissimus的祖先形态在爱琴海海沟完全形成之前,从安纳托利亚侵入了爱琴海地区,当时爱琴海仍然是一个统一的陆地,而其他替代事件导致了它目前的分布。

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