Liu Dongqi, Hou Feixia, Liu Qin, Zhang Xiuyue, Yan Taiming, Song Zhaobin
Sichuan Key Laboratory of Conservation Biology on Endangered Wildlife, College of Life Sciences, Sichuan University, Chengdu, 610065, People's Republic of China.
Genetica. 2015 Feb;143(1):73-84. doi: 10.1007/s10709-015-9815-8. Epub 2015 Jan 9.
The Tibetan Plateau underwent dramatic geological and climatic changes, which had important implications for genetic divergence and population dynamics of freshwater fish populations. Fluctuations of the ecogeographical environment and major hydrographic formations might have promoted the formation of new subspecies or species. In order to understand the impact of plateau uplift on freshwater fish evolutionary history, we estimated the genetic diversity and population structure in two subspecies of Schizopygopsis chengi (S. c. chengi and S. c. baoxingensis) in upper Yangtze River in Tibetan Plateau area using mitochondrial DNA control region and eight microsatellite markers, which suggested that there was a close genetic relationship. S. chengi showed some significant genetic structure that did not correlate with geographic distance. Bayesian assignment tests indicated that S. chengi samples in the study could be divided into four populations: upstream population, midstream population, tributary population and S. c. baoxingensis population. S. c. chengi and S. c. baoxingensis showed significant genetic divergence. However, phylogenetic analysis, population structure analysis and historical gene flow estimation suggested that there was close genetic relationship between S. c. baoxingensis and the Dawei population which belongs to populations of S. c. chengi. The time that Dawei population suffered from a bottleneck and S. c. baoxingensis underwent population expansion was congruent with the last glacial period on the Tibetan Plateau. The results confirmed the hypothesis that the Dawei River and Baoxing River were once connected, and the Dawei and Baoxing populations originated from a single population, but were isolated into separate populations because of crustal movements and the Baoxing population evolved as S. c. baoxingensis.
青藏高原经历了剧烈的地质和气候变化,这对淡水鱼类种群的遗传分化和种群动态产生了重要影响。生态地理环境的波动和主要水系的形成可能促进了新亚种或新物种的形成。为了了解高原隆升对淡水鱼类进化历史的影响,我们利用线粒体DNA控制区和8个微卫星标记,对青藏高原地区长江上游的中华裂腹鱼两个亚种(中华裂腹鱼指名亚种和宝兴亚种)的遗传多样性和种群结构进行了估计,结果表明它们之间存在密切的遗传关系。中华裂腹鱼显示出一些与地理距离无关的显著遗传结构。贝叶斯分配检验表明,研究中的中华裂腹鱼样本可分为四个种群:上游种群、中游种群、支流种群和宝兴亚种种群。中华裂腹鱼指名亚种和宝兴亚种表现出显著的遗传分化。然而,系统发育分析、种群结构分析和历史基因流估计表明,宝兴亚种与属于中华裂腹鱼指名亚种种群的大维种群之间存在密切的遗传关系。大维种群经历瓶颈和宝兴亚种经历种群扩张的时间与青藏高原最后一次冰期一致。结果证实了大维河和宝兴河曾经相连,大维种群和宝兴种群起源于单一群体,但由于地壳运动而被隔离成不同群体,宝兴种群进化为宝兴亚种的假说。