Schönswetter P, Popp M, Brochmann C
National Centre for Biosystematics, Natural History Museum, University of Oslo, Norway.
Mol Ecol. 2006 Mar;15(3):709-20. doi: 10.1111/j.1365-294X.2006.02821.x.
Minuartia biflora and Ranunculus pygmaeus are circumarctic plants with a few isolated occurrences in the European Alps. We analysed amplified fragment length polymorphism (AFLP) and chloroplast DNA sequence data to unravel the history of their immigration into the Alps and to provide data on their circumpolar phylogeography. In spite of the similar ecological requirements of the two species, they exhibit strikingly different immigration histories into the Alps. In M. biflora, the Alpine populations are most probably derived from source populations located between the Alpine and Scandinavian ice sheets, in accordance with the traditional biogeographic hypothesis. In contrast, the Alpine populations of R. pygmaeus cluster with those from the Tatra Mountains and the Taymyr region in northern Siberia, indicating that the distant Taymyr area served as source for the Alpine populations. Both species showed different levels of genetic diversity in formerly glaciated areas. In contrast to the considerable AFLP diversity observed in M. biflora, R. pygmaeus was virtually nonvariable over vast areas, with a single phenotype dominating all over the Alps and another, distantly related one dominating the North Atlantic area from Greenland over Svalbard to Scandinavia. The same pattern was observed in chloroplast DNA sequence data. Thus, postglacial colonization of R. pygmaeus was accompanied by extreme founder events.
双花米努草和矮毛茛是环北极植物,在欧洲阿尔卑斯山有一些孤立的分布。我们分析了扩增片段长度多态性(AFLP)和叶绿体DNA序列数据,以揭示它们迁入阿尔卑斯山的历史,并提供有关其环极系统发育地理学的数据。尽管这两个物种有相似的生态需求,但它们迁入阿尔卑斯山的历史却截然不同。对于双花米努草,根据传统生物地理学假设,阿尔卑斯山种群很可能源自位于阿尔卑斯山和斯堪的纳维亚冰盖之间的源种群。相比之下,矮毛茛的阿尔卑斯山种群与来自塔特拉山脉和西伯利亚北部泰梅尔地区的种群聚类,这表明遥远的泰梅尔地区是阿尔卑斯山种群的来源地。这两个物种在曾经被冰川覆盖的地区表现出不同程度的遗传多样性。与在双花米努草中观察到的相当可观的AFLP多样性不同,矮毛茛在广大地区几乎没有变化,单一表型在整个阿尔卑斯山占主导地位,另一种与之亲缘关系较远的表型在从格陵兰岛经斯瓦尔巴群岛到斯堪的纳维亚半岛的北大西洋地区占主导地位。在叶绿体DNA序列数据中也观察到了相同的模式。因此,矮毛茛的冰后期定殖伴随着极端的奠基者事件。