School of Ecology and Nature Conservation, Beijing Forestry University, Beijing 100083, China.
College of Biological Sciences and Technology, Beijing Forestry University, Beijing 100083, China.
Int J Mol Sci. 2023 Feb 3;24(3):3056. doi: 10.3390/ijms24033056.
The evolutionary history of section , an East Asian endemic lineage, has not been comprehensively studied. In this study, we reconstruct the phylogeny of this section with a complete sampling using a phylogenomic approach. The genome skimming method was applied to obtain the complete plastome sequence, the nuclear ribosomal DNA (nrDNA), and the nuclear SNPs data for phylogenetic reconstruction. Using a Bayesian molecular clock approach and ancestral range reconstruction, we reconstruct biogeographical history and discuss the biotic and abiotic factors that may have shaped the distribution patterns of the section. Both nuclear datasets better resolved the phylogeny of the sect. than the plastome sequence. Sect. was resolved as a monophyletic group sister to a clade mainly containing species from the sect. and sect. . Within sect. , two major clades were resolved by both nuclear datasets. Two continental taxa, and var. , formed one clade. One continental taxon, , and all the other species from Taiwan island, the Korean peninsula, and the Japanese archipelago formed the other clade. Molecular dating results showed that sect. diverged from its sister clade in the Pliocene, and all the current species diversified during the Pleistocene. Our biogeographical reconstruction suggested that sect. evolved and began species diversification, most likely in mainland China, then dispersed to the Korean peninsula, and then expanded its range through the Japanese archipelago to Taiwan island. Island species diversity may arise through allopatric speciation by vicariance events following the range fragmentation triggered by the climatic oscillation and sea level change during the Pleistocene epoch. Our results highlight the importance of climatic oscillation during the Pleistocene to the spatial-temporal diversification patterns of the sect. .
东亚特有谱系 组的进化历史尚未得到全面研究。在本研究中,我们采用系统基因组学方法对该组进行了完整采样的系统发育重建。应用基因组扫掠方法获得了完整的质体基因组序列、核核糖体 DNA(nrDNA)和核 SNP 数据进行系统发育重建。使用贝叶斯分子钟方法和祖先范围重建,我们重建了生物地理学历史,并讨论了可能影响该组分布模式形成的生物和非生物因素。核数据集比质体序列更好地解决了 组的系统发育。 组被解析为一个单系群,与一个主要包含来自 组和 组的物种的分支姐妹。在 组内,两个核数据集都解析出两个主要分支。两个大陆分类群, 和 变种,形成一个分支。一个大陆分类群 和来自台湾岛、朝鲜半岛和日本群岛的所有其他物种形成另一个分支。分子定年结果表明, 组在中新世与姐妹分支分化,所有现存物种在更新世多样化。我们的生物地理学重建表明, 组在中国大陆进化并开始物种多样化,然后扩散到朝鲜半岛,然后通过日本群岛扩展到台湾岛。岛屿物种多样性可能是通过隔离物种形成而产生的,这种形成是由于更新世气候波动和海平面变化引起的范围碎裂导致的。我们的研究结果强调了更新世气候波动对 组时空多样化模式的重要性。