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Geographical structuring of mitochondrial DNA in Chalcides sexlineatus within he island of Gran Canaria

机译:大加那利岛内Chalcides sexlineatus中线粒体DNA的地理结构

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The skink Chalcides sexlineatus shows clear north-south ecology-correlated variation in morphology within the island of Gran Canaria. Detailed study of this variation previously supported the hypothesis of in situ differentiation arising through climate-mediated variation in selection pressures. The more recent discovery of substantial within-island mitochondrial DNA (mtDNA) sequence divergence suggested an alternative historical vicariance scenario. This paper provides a detailed analysis of geographical structuring in mtDNA, based on a fragment amplified from the 12S rRNA region in 96 individuals. A very clear phylogeographic pattern was detected: three 'deep' lineages were evident corresponding to northern, south-eastern and south-western parts of Gran Canaria with generally low levels of mtDNA introgression. The pattern of among-site differentiation was highly concordant with the pattern of morphological variation. It also provided a close fit to a simple microevolutionary model based on population vicariance during volcanic eruptions known to have occurred during the past 2.8 million years in the north of the island. The minimum number of historical migration events required to explain the mtDNA tree was calculated and a novel randomization test used to show that there were a lower number of putative migrations across the morphology transition zone, relative to migrations within northern and southern zones. Differential adaptation to the two major habitat types and selection against hybrids may explain why the morphology transition zone coincides with the main ecotone and is relatively narrow, respectively.
机译:大加那利岛上的石龙子化石显示出明显的南北生态相关形态变化。对这种变化的详细研究以前支持由气候介导的选择压力变化引起的原位分化的假说。岛内线粒体DNA(mtDNA)序列差异的实质性最新发现表明了另一种历史性的替代方案。本文基于从96个个体的12S rRNA区域扩增的片段,对mtDNA的地理结构进行了详细分析。检测到非常清晰的系统谱模式:三个“较深”谱系明显对应于大加那利岛的北部,东南部和西南部,且mtDNA渗入水平通常较低。位点间分化的模式与形态变异的模式高度一致。它也与简单的微观进化模型非常吻合,该模型基于火山喷发期间的种群变化而闻名,该火山喷发在过去的280万年来一直在该岛北部发生。计算了解释mtDNA树所需的历史迁移事件的最小数量,并使用一种新颖的随机测试表明,相对于北部和南部区域内的迁移,整个形态过渡带的假定迁移数较少。对两种主要生境类型的差异适应和对杂种的选择可能解释了为什么形态过渡带分别与主要过渡带一致且相对较窄。

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