Wan Dong-Shi, Feng Jian-Ju, Jiang De-Chun, Mao Kang-Shan, Duan Yuan-Wen, Miehe Georg, Opgenoorth Lars
State Key Laboratory of Grassland Agro-Ecosystem School of Life Sciences Lanzhou University Lanzhou 730000 Gansu China.
College of Plant Sciences Xinjiang Production & Construction Corps Key Laboratory of Protection and Utilization of Biological Resources in Tarim Basin Tarimu University Alar Xinjiang China.
Ecol Evol. 2016 Feb 24;6(7):1977-95. doi: 10.1002/ece3.2019. eCollection 2016 Apr.
Various hypotheses have been proposed about the Quaternary evolutionary history of plant species on the Qinghai-Tibet Plateau (QTP), yet only a handful of studies have considered both population genetics and ecological niche context. In this study, we proposed and compared climate refugia hypotheses based on the phylogeographic pattern of Anisodus tanguticus (three plastid DNA fragments and nuclear internal transcribed spacer regions from 32 populations) and present and past species distribution models (SDMs). We detected six plastid haplotypes in two well-differentiated lineages. Although all haplotypes could be found in its western (sampling) area, only haplotypes from one lineage occurred in its eastern area. Meanwhile, most genetic variations existed between populations (F ST = 0.822). The SDMs during the last glacial maximum and last interglacial periods showed range fragmentation in the western area and significant range contraction in the eastern area, respectively, in comparison with current potential distribution. This species may have undergone intraspecific divergence during the early Quaternary, which may have been caused by survival in different refugia during the earliest known glacial in the QTP, rather than geological isolation due to orogenesis events. Subsequently, climate oscillations during the Quaternary resulted in a dynamic distribution range for this species as well as the distribution pattern of its plastid haplotypes and nuclear genotypes. The interglacial periods may have had a greater effect on A. tanguticus than the glacial periods. Most importantly, neither genetic data nor SDM alone can fully reveal the climate refugia history of this species. We also discuss the conservation implications for this important Tibetan folk medicine plant in light of these findings and SDMs under future climate models. Together, our results underline the necessity to combine phylogeographic and SDM approaches in future investigations of the Quaternary evolutionary history of species in topographically complex areas, such as the QTP.
关于青藏高原植物物种的第四纪进化历史,已经提出了各种假说,但只有少数研究同时考虑了种群遗传学和生态位背景。在本研究中,我们基于唐古特山莨菪(32个种群的三个质体DNA片段和核内转录间隔区)的系统发育地理模式以及当前和过去的物种分布模型(SDMs),提出并比较了气候避难所假说。我们在两个分化良好的谱系中检测到六种质体单倍型。虽然在其西部(采样)区域可以找到所有单倍型,但在其东部区域仅出现了一个谱系的单倍型。同时,大多数遗传变异存在于种群之间(FST = 0.822)。末次盛冰期和末次间冰期的SDMs显示,与当前潜在分布相比,西部地区范围破碎化,东部地区范围显著收缩。该物种可能在第四纪早期经历了种内分化,这可能是由于在青藏高原最早已知冰川期在不同避难所生存所致,而非造山事件导致的地质隔离。随后,第四纪期间的气候振荡导致该物种及其质体单倍型和核基因型的分布模式出现动态变化。间冰期对唐古特山莨菪的影响可能比冰期更大。最重要的是,单独的遗传数据或SDM都不能完全揭示该物种的气候避难所历史。我们还根据这些发现以及未来气候模型下的SDM,讨论了这种重要的藏药植物的保护意义。总之,我们的结果强调了在未来对地形复杂地区(如青藏高原)物种的第四纪进化历史调查中,有必要结合系统发育地理和SDM方法。