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Demographic complexity within walnut species provides insights into the heterogeneity of geological and climatic fluctuations in East Asia

东亚 人口 地理 亚热带 每年落叶的 温带落叶林 克莱德 分子钟 陆桥 新近纪 温带气候 全球降温 生物 生态学 气候变化 系统发育树 古生物学 考古 生物扩散 构造盆地 中国 社会学 人口学 基因 生物化学
作者
Fang‐Dong Geng,Meng‐Fan Lei,Naiyu Zhang,Yao‐Lei Fu,Hang Ye,Meng Dang,Xue‐Dong Zhang,Miao‐Qing Liu,Mengdi Li,Zhan‐Lin Liu,Peng Zhao
出处
期刊:Journal of Systematics and Evolution [Wiley]
卷期号:62 (5): 1037-1053 被引量:6
标识
DOI:10.1111/jse.13061
摘要

Abstract East Asia constitutes one of the largest and most complex areas of plant diversity globally. This complexity is attributable to the geological history and climatic diversity of East Asia. However, controversy persists over the biogeographical hypotheses and different studies on this topic. The demographical complexity of temperate deciduous woody plants and heterogeneity of geological and climatic fluctuations in East Asia remain poorly understood. We aimed to assemble the chloroplast and nuclear genomes of 360 individuals from five walnut ( Juglans ) species in East Asia and comprehensively analyze the phylogenetic inference, genetic structure, population demographic, and selection pressure. The results showed that East Asian walnuts could be divided into two major groups, that is, section Juglans / Dioscaryon and sect. Cardiocaryon . Within sect. Cardiocaryon , the samples were categorized into the northern clade and southern clade, both of which were affected by Quaternary glaciation; however, the southern clade was affected to a lesser extent. The population expansion events observed in sect. Cardiocaryon and sect. Dioscaryon since the late Miocene indicated that Neogene climate cooling substantially affected the distribution of Tertiary relict plants in East Asia. Biogeographic analysis results showed that the uplift of the Qinghai–Tibetan Plateau (QTP) might have contributed to the divergence within sect. Dioscaryon . Our findings highlight the heterogeneity of climatic fluctuations in the northern and southern regions of East Asia during the late Neogene and Quaternary periods and suggest that the uplift of QTP could have facilitated the divergence of temperate deciduous woody plants.
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