Li Yan, Gao Qing-Bo, Gengji Zhuo-Ma, Jia Liu-Kun, Wang Zhi-Hua, Chen Shi-Long
Key Laboratory of Adaptation and Evolution of Plateau Biota, Northwest Institute of Plateau Biology, Chinese Academy of Sciences, Xining, China.
College of Life Sciences, University of Chinese Academy of Sciences, Beijing, China.
Front Genet. 2018 Sep 18;9:381. doi: 10.3389/fgene.2018.00381. eCollection 2018.
An increasing number of phylogeographic studies have been conducted for plant species in the Qinghai-Tibetan Plateau (QTP) and its flanking mountains. However, these studies have mainly focused on the determination of glacial refugia and routes of inter-/post-glacial expansions. Rapid intraspecific diversification of plants in this region have not been thoroughly discussed. Herein, we investigate the effects of the Quaternary climate changes on population genetic structure and diversifications of a herbaceous alpine species, , which may have an evolutionary time scale <5 million years in the QTP and Himalayan regions. Using a total of 350 individuals from 29 populations, we studied the evolutionary history of by analyzing cpDNA L-F, 16 and nrDNA ITS sequences. A total of 89 haplotypes and 158 genotypes were detected for cpDNA and ITS sequences, respectively. Only a few haplotypes/genotypes were widespread, while an extremely large number of haplotypes/genotypes were restricted to single populations, which were scattered throughout the current geographical range of . This suggests the existence of microrefugia of this species during the Quaternary glaciations. In addition, the relationships of the haplotypes/genotypes were almost completely not resolved by phylogenetic reconstruction. Combining characteristics in terms of high haplotype richness, large proportion of private haplotypes, and shallow haplotype divergence, we speculate that recent intraspecific diversification has occurred in . Molecular clock analysis estimated that the onset diversification within to be 1.09 Ma (95% HPD = 0.80-1.45), coinciding with the extensive Quaternary glaciations on the QTP which started ca. 1.17 Ma. The Quaternary climatic oscillations may have triggered rapid intraspecific diversification in this QTP-Himalayan species. However, large niche breadth, as well as introgression/hybridization between the studied species and its closely related sympatric saxifrages, may also played a role to some extent on the current genetic structure of , which need to be further studied.
针对青藏高原(QTP)及其周边山脉的植物物种,已经开展了越来越多的系统发育地理学研究。然而,这些研究主要集中在确定冰川避难所及冰期/冰后期扩张路线上。该地区植物种内的快速多样化尚未得到充分讨论。在此,我们研究了第四纪气候变化对一种高山草本物种的种群遗传结构和多样化的影响,该物种在QTP和喜马拉雅地区的进化时间尺度可能小于500万年。我们使用来自29个种群的总共350个个体,通过分析叶绿体DNA(cpDNA)的L-F、trnL-F和核糖体DNA(nrDNA)的ITS序列,研究了该物种的进化历史。分别在cpDNA和ITS序列中检测到89个单倍型和158个基因型。只有少数单倍型/基因型广泛分布,而绝大多数单倍型/基因型局限于单个种群,这些种群散布在该物种当前的地理分布范围内。这表明该物种在第四纪冰川期存在微避难所。此外,通过系统发育重建几乎完全无法解析单倍型/基因型之间的关系。结合高单倍型丰富度、大量私有单倍型以及浅单倍型分化等特征,我们推测该物种近期发生了种内多样化。分子钟分析估计该物种内多样化的起始时间为1.09百万年(95%最高后验密度区间 = 0.80 - 1.45),这与QTP上大约1.17百万年前开始的广泛第四纪冰川期相吻合。第四纪气候振荡可能触发了这个QTP - 喜马拉雅物种的快速种内多样化。然而,较大的生态位宽度,以及所研究物种与其同域分布的近缘虎耳草属植物之间的渐渗/杂交,在某种程度上也可能对该物种当前的遗传结构产生了影响,这有待进一步研究。