Wang Xinyu, Li Yuanshuo, Liang Qianlong, Zhang Lei, Wang Qian, Hu Huan, Sun Yongshuai
MOE Key Laboratory for Bio-Resources and Eco-Environment, College of Life Science, Sichuan University Chengdu, 610065, China.
Ecol Evol. 2015 Apr;5(7):1513-24. doi: 10.1002/ece3.1449. Epub 2015 Mar 10.
It has been hypothesized that species occurring in the eastern and the western Qinghai-Tibet Plateau (QTP) responded differently to climate changes during the Pleistocene. Here, we test this hypothesis by phylogeographic analysis of two sister species, Allium cyathophorum and A. spicata. We sequenced two chloroplast DNA (cpDNA) fragments (accD-psaI and the rpl16 intron) of 150 individuals, and the nuclear (ITS) region of 114 individuals, from 19 populations throughout the distributional ranges of these species. The divergence between the two species was dated at 779 - 714 thousand years before the present and was likely initiated by the most major glaciation in the QTP. Analysis of chlorotype diversity showed that A. spicata, the species occurring in the western QTP, contains much lower genetic diversity (0.25) than A. cyathophorum (0.93), which is distributed in the eastern QTP. Moreover, multiple independent tests suggested that the A. spicata population had expanded recently, while no such expansion was detected in A. cyathophorum, indicating a contrasting pattern of responses to Pleistocene climate changes. These findings highlight the importance of geographical topography in determining how species responded to the climate changes that took place in the QTP during the Pleistocene.
据推测,青藏高原东部和西部的物种在更新世对气候变化的响应有所不同。在此,我们通过对两种近缘物种——头花韭和穗花韭进行系统地理学分析来验证这一假设。我们对来自这两个物种分布范围内19个种群的150个个体的两个叶绿体DNA(cpDNA)片段(accD-psaI和rpl16内含子)以及114个个体的核(ITS)区域进行了测序。这两个物种之间的分化时间可追溯到距今77.9万至71.4万年前,很可能是由青藏高原最主要的一次冰川作用引发的。叶绿体单倍型多样性分析表明,分布在青藏高原西部的穗花韭的遗传多样性(0.25)远低于分布在青藏高原东部的头花韭(0.93)。此外,多项独立测试表明,穗花韭种群近期出现了扩张,而头花韭种群未检测到此类扩张,这表明两者对更新世气候变化的响应模式形成了对比。这些发现凸显了地理地形在决定物种如何响应更新世期间青藏高原发生的气候变化方面的重要性。