Département d'Ecologie et de Gestion de la Biodiversité, FRE 2696 - Adaptation et évolution des systèmes ostéomusculaires, 55 rue Buffon, Muséum National d'Histoire Naturelle, 75005 Paris, France.
Mol Phylogenet Evol. 2010 Mar;54(3):857-69. doi: 10.1016/j.ympev.2009.10.016. Epub 2009 Oct 27.
Phylogenetic analyses using up to 1532 base pairs (bp) of mitochondrial DNA from 106 specimens of Neotropical Mabuya, including 18 of the 19 recognized South American and Mesoamerican species, indicate that most species of the genus are monophyletic, including M. nigropunctata that had previously been reported to be paraphyletic. The present results shows that this species includes three highly divergent and largely allopatric lineages restricted to occidental, meridional, and oriental Amazonia. Our dataset demonstrates that previous claims regarding the paraphyletic status of M. nigropunctata and the phylogenetic relationships within this species complex based on the analysis of three mitochondrial and four nuclear genes (approx. 5000bp) were erroneous and resulted from two contaminated cytochrome b sequences. The phylogenetic results indicate that diversification in the Neotropical genus Mabuya started approximately in the Middle Miocene (15.5-13.4Ma). The divergence dates estimated for the Mabuya nigropunctata species complex suggest that the major cladogenetic events that produced the three main groups (occidental (oriental+meridional)) occurred during the Late Miocene. These estimations show that diversification within the M. nigropunctata species complex was not triggered by the climatic changes that occurred during the Pleistocene, as has been suggested by several authors. Rather, our data support the hypothesis that the late tertiary (essentially Miocene epoch) was a period that played a very important role in the generation of biological diversity in the Amazonian forests. Speciation between Mabuyacarvalhoi, endemic to the coastal mountain range of Venezuela, and M. croizati, restricted to the Guiana Shield, occurred during the Middle Miocene and may have been as the result of a vicariant event produced by the formation of the present day Orinoco river drainage basin and the consequent appearance of the Llanos del Orinoco, which acted as a barrier to dispersal between these two species. The split between M. bistriata and M. altamazonica and between the occidental and (meridional+oriental) clades of M. nigropunctata fits very well with the biogeographic split between the eastern and western Amazon basins reported for several other taxa.
使用 106 个新热带 Mabuya 标本的线粒体 DNA 长达 1532 个碱基对(bp)进行系统发育分析,包括 19 种公认的南美和中美洲物种中的 18 种,表明该属的大多数物种都是单系的,包括以前被报道为并系的 M. nigropunctata。目前的结果表明,该物种包括三个高度分化且主要地理隔离的谱系,仅限于西部、中部和东部亚马逊地区。我们的数据集表明,以前关于 M. nigropunctata 的并系地位以及基于三个线粒体和四个核基因(约 5000bp)分析的该物种复合体内部的系统发育关系的说法是错误的,这是由于两个污染的细胞色素 b 序列造成的。系统发育结果表明,新热带 Mabuya 属的多样化始于中新世中期(155-134Ma)。估计 Mabuya nigropunctata 物种复合体的分化日期表明,产生三个主要组(西部(东部+中部))的主要分支事件发生在中新世晚期。这些估计表明,M. nigropunctata 物种复合体内部的多样化并不是由几位作者所提出的更新世气候变化引发的。相反,我们的数据支持这样一种假说,即第三纪晚期(主要是中新世时期)是亚马逊森林生物多样性产生的一个非常重要的时期。特有的委内瑞拉沿海山脉 Mabuyacarvalhoi 和仅限于圭亚那地盾的 M. croizati 之间的物种形成发生在中新世中期,可能是由现今奥里诺科河流域的形成和随之出现的奥里诺科平原造成的,这是一个扩散障碍,导致这两个物种之间的扩散。M. bistriata 和 M. altamazonica 之间以及 M. nigropunctata 的西部和(中部+东部)分支之间的分裂与为其他几个分类群报告的东部和西部亚马逊盆地之间的生物地理分裂非常吻合。