School of Life Sciences, Lanzhou University, Lanzhou, 730000, China.
Key Laboratory of Zoological Systematics and Evolution, Institute of Zoology, Chinese Academy of Sciences, Beijing, 100101, China.
BMC Evol Biol. 2019 Aug 1;19(1):161. doi: 10.1186/s12862-019-1487-z.
Geological events and climatic changes played important roles in shaping population differentiation and distribution within species. In China, populations in many species have contracted and expanded responding to environmental changes with the uplift of the Qinghai-Tibet Plateau (QTP) and glacial cycles during Pleistocene. In this study, we analysed the population structure of Godlewski's Bunting, Emberiza godlewskii, to determine the effects of major historical events, geographic barriers and past climatic changes on phylogenetic divergence and historical demographic dynamics of this species.
A phylogeny based on concatenated mitochondrial and nuclear DNA datasets show two (northern and southern) clades approximately diverged 3.26 million years ago (Ma). The West Qinling Mountains serve as a dividing line between the two lineages. Both lineages experienced a recent demographic expansion during interglacial periods (marine isotope stages (MISs) 2-6). Bayesian skyline plots and the results of ecological niche modelling suggested a more intensive expansion of the northern lineage during the late Pleistocene, whereas the southern lineage was comparatively mild in population growth.
Our results provide insights into the distribution patterns of avian taxa and the possible mechanisms for a south and north divergence model in China. The deep divergence may have been shaped by the uplift of the QTP. Habitat preferences might have facilitated the lineage divergence for E. godlewskii. Moreover, the West Qinling Mountains act as a dividing line between the two lineages, indicating a novel phylogeographic pattern of organisms in China. The difference in population expansion mode between two lineages resulted from different effects caused by the climate of the LGM and the subsequent habitat changes accompanying the arrival of a colder climate in northern and southern regions of China.
地质事件和气候变化在塑造物种内的种群分化和分布方面发挥了重要作用。在中国,许多物种的种群随着青藏高原的隆升和更新世冰期的循环而响应环境变化而收缩和扩张。在这项研究中,我们分析了戈德尔斯基朱雀(Emberiza godlewskii)的种群结构,以确定主要历史事件、地理屏障和过去气候变化对该物种的系统发育分歧和历史人口动态的影响。
基于线粒体和核 DNA 数据集的系统发育分析显示,两个(北部和南部)分支大约在 326 万年前(Ma)分化。西秦岭山脉是这两个谱系的分界线。两个谱系在间冰期(海洋同位素阶段(MISs)2-6)都经历了最近的人口扩张。贝叶斯天空线图和生态位模型的结果表明,在更新世晚期,北部谱系的扩张更为剧烈,而南部谱系的种群增长相对温和。
我们的研究结果为鸟类分类群的分布模式和中国南北分化模型的可能机制提供了深入的了解。青藏高原的隆升可能塑造了这种深分歧。栖息地偏好可能促进了 E. godlewskii 的谱系分化。此外,西秦岭山脉是两个谱系的分界线,表明中国生物具有新的地理模式。两个谱系的种群扩张模式的差异是由于末次冰期和随后伴随中国南北地区气候变冷而来的栖息地变化对气候的不同影响所致。