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首页> 外文期刊>Evolution: International Journal of Organic Evolution >Evidence for multiple pleistocene refugia in the postglacial expansion of the eastern tiger salamander, Ambystoma tigrinum tigrinum
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Evidence for multiple pleistocene refugia in the postglacial expansion of the eastern tiger salamander, Ambystoma tigrinum tigrinum

机译:东部虎sal冰河扩张后冰期扩张中多次更新世的庇护的证据

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Pleistocene glaciations were important determinants of historical migration and, hence, current levels of genetic diversity within and among populations. In many cases, these historical migrations led to the existence of disjunct populations of plants and animals. However, the origin and timing of arrival of these disjunct populations is often debated. In the current study, we identify potential refugia and estimate the timing of vicariance events of the eastern tiger salamander, Ambystoma tigrinum tigrinum, using mitochondrial sequence data. The results suggest a vicariant event 0.75-2 million years ago, separating the tiger salamanders to the east and west of the Apalachicola River Basin. East of the Appalachians, there appear to be multiple independent refugia with little migration among the remaining populations. In particular, populations along the Atlantic Coastal Plain were likely isolated in a coastal plain refugium in the Carolinas. Migrants from this refugium were the likely source of colonists for populations occupying previously glaciated areas along the northeastern Atlantic Coast. A second potential refugium occurs in the Blue Ridge Mountains of western Virginia. This refugium contains a disjunct population of the eastern tiger salamander, as well as a community of nearly 70 other disjunct plant and animal species. The tiger salamanders here have been isolated from other populations for 200,000-500,000 years. These results suggest that disjunct mountain populations of Coastal Plain species may have existed in situ throughout the Pleistocene in Appalachian refugia. Therefore, these disjunct populations are not of recent origin, but rather exist as relicts of a warmer, more widespread fauna and flora that is now restricted to the Coastal Plain. [References: 94]
机译:更新世冰川是历史迁徙的重要决定因素,因此也是种群内部和种群之间当前遗传多样性水平的重要决定因素。在许多情况下,这些历史性迁徙导致存在动植物种群的分离。但是,这些异族的起源和到达时间经常受到争议。在当前的研究中,我们使用线粒体序列数据来确定潜在的避难所,并估计东部虎,、虎纹小虾的离婚事件的时间。结果表明,0.75到200万年前发生了一次arian灭事件,将老虎separating分为Apalachicola流域的东西方。在阿巴拉契亚山脉以东,似乎有多个独立的避难所,其余人口中很少迁徙。特别是大西洋沿岸平原的居民很可能被隔离在卡罗来纳州的沿海平原避难所中。来自这个避难所的移民是殖民者的可能来源,他们占领了东北大西洋沿岸以前冰川地区。第二个潜在的避难所发生在西弗吉尼亚州的蓝岭山脉。这个避难所包含东部虎sal的不同种群,以及其他近70种其他分离的动植物物种。这里的老虎sal已与其他种群隔离200,000-500,000年。这些结果表明,在阿巴拉契亚保护区的整个更新世中,沿海平原物种的离散山区种群可能就地存在。因此,这些杂乱的种群不是最近才起源的,而是作为温暖的,分布更广的动植物群的遗迹而存在的,这些动植物群现在仅限于沿海平原。 [参考:94]

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