Shang Hui-Ying, Li Zhong-Hu, Dong Miao, Adams Robert P, Miehe Georg, Opgenoorth Lars, Mao Kang-Shan
State Key Laboratory of Grassland Agro-Ecosystem, School of Life Sciences, Lanzhou University, Lanzhou 730000, Gansu, China.
Key Laboratory of Resource Biology and Biotechnology in Western China, Ministry of Education, College of Life Sciences, Northwest University, Xi'an 710069, Shaanxi, China.
Sci Rep. 2015 May 15;5:10216. doi: 10.1038/srep10216.
All Qinghai-Tibetan Plateau (QTP) endemic species are assumed to have originated recently, although very rare species most likely diverged early. These ancient species provide an excellent model to examine the origin and evolution of QTP endemic plants in response to the QTP uplifts and the climate changes that followed in this high altitude region. In this study, we examined these hypotheses by employing sequence variation from multiple nuclear and chloroplast DNA of 239 individuals of Juniperus microsperma and its five congeners. Both phylogenetic and population genetic analyses revealed that J. microsperma diverged from its sister clade comprising two species with long isolation around the Early Miocene, which corresponds to early QTP uplift. Demographic modeling and coalescent tests suggest that J. microsperma experienced an obvious bottleneck event during the Quaternary when the global climate greatly oscillated. The results presented here support the hypotheses that the QTP uplifts and Quaternary climate changes played important roles in shaping the evolutionary history of this rare juniper.
所有青藏高原特有物种都被认为是近期起源的,尽管极稀有种很可能分化得较早。这些古老物种为研究青藏高原特有植物在该高海拔地区因高原隆升及随后的气候变化而产生的起源与演化提供了绝佳模型。在本研究中,我们通过分析239个小果刺柏个体及其五个同属物种的多个核DNA和叶绿体DNA的序列变异来检验这些假设。系统发育分析和群体遗传学分析均表明,小果刺柏与其包含两个长期隔离物种的姐妹分支在中新世早期分化,这与青藏高原早期隆升相对应。种群动态模拟和溯祖检验表明,小果刺柏在第四纪全球气候大幅波动期间经历了明显的瓶颈事件。本文结果支持以下假设:青藏高原隆升和第四纪气候变化在塑造这种珍稀刺柏的演化历史中发挥了重要作用。