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首页> 外文期刊>Evolutionary biology >Genetic Diversification of Adelphobates quinquevittatus (Anura: Dendrobatidae) and the Influence of Upper Madeira River Historical Dynamics
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Genetic Diversification of Adelphobates quinquevittatus (Anura: Dendrobatidae) and the Influence of Upper Madeira River Historical Dynamics

机译:Adelphobates quinquevittatus(Anura:Dendrobatidae)的遗传多样性和马德拉河上游历史动态的影响

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The effect of large Amazonian rivers as barriers to distribution of species and gene flow has been the subject of debate for more than a century. The Madeira River is the largest tributary of the Amazon River, with the region comprising its basin undergoing complex changes from the Pliocene through the Holocene. Accordingly, the evolution of its drainage seems to have been an important factor in the biological diversification of different taxa. We characterize the phylogeographic pattern of Adelphobates quinquevittatus, focusing on the role of the Madeira River and the environmental changes in the region, as potential barriers to gene flow. For this, we used sequences of two mitochondrial genes from 65 individuals sampled in 15 locations. We identify population structure partially related to the current Madeira River configuration. However the most upstream session does not represent a historical barrier, suggesting that may have attained its current geomorphological configuration recently. Divergence among clades began in the last 1 million years, coinciding with documented changes in this landscape, and may be related to river dynamics associated with the presence of open vegetation areas. This phylogeographic pattern supports the dynamism of the drainage, and the historical complexity of the upper Madeira River.
机译:一个多世纪以来,亚马逊大河作为物种分布和基因流动障碍的影响一直是争论的主题。马德拉河是亚马逊河最大的支流,该地区包括其流域,从上新世到全新世经历了复杂的变化。因此,其排水的演变似乎是不同分类群生物多样性的一个重要因素。我们描述了 Adelphobates quinquevittatus 的系统地理模式,重点关注马德拉河的作用和该地区的环境变化,作为基因流动的潜在障碍。为此,我们使用了来自15个位置的65个个体的两个线粒体基因的序列。我们确定了与当前马德拉河配置部分相关的种群结构。然而,最上游的会话并不代表历史障碍,这表明它可能最近已经达到了目前的地貌结构。分支之间的分化始于最近100万年,与该景观的记录变化相吻合,并且可能与与开放植被区域的存在相关的河流动力学有关。这种系统地理模式支持了排水的动态性,以及马德拉河上游的历史复杂性。

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