Molecular phylogeography and historical demography of a widespread herbaceous species from eastern North America, Podophyllum peltatum

系统地理学 生物 生态学 航程(航空) 人口历史 人口 冰期 遗传多样性 遗传结构 进化生物学 古生物学 系统发育学 人口学 生物化学 材料科学 社会学 基因 复合材料
作者
C.B. Wang,Zhao‐Yan Yap,Penglei Wan,Kuangqi Chen,Ryan A. Folk,Dixie Z. Damrel,Wayne Barger,Alvin R. Diamond,Charles N. Horn,Garrie P. Landry,Tharanga Samarakoon,Stephanie Harvey,David R. Morgan,Yingxiong Qiu,Pan Li
出处
期刊:American Journal of Botany [Wiley]
标识
DOI:10.1002/ajb2.16254
摘要

Abstract Premise Glacial/interglacial cycles and topographic complexity are both considered to have shaped today's diverse phylogeographic patterns of taxa from unglaciated eastern North America (ENA). However, few studies have focused on the phylogeography and population dynamics of wide‐ranging ENA herbaceous species occurring in forest understory habitat. We examined the phylogeographic pattern and evolutionary history of Podophyllum peltatum L., a widely distributed herb inhabiting deciduous forests of ENA. Methods Using chloroplast DNA (cpDNA) sequences and nuclear microsatellite loci, we investigated the population structure and genetic diversity of the species. Molecular dating, demographic history analyses, and ecological niche modeling were also performed to illustrate the phylogeographic patterns. Results Our cpDNA results identified three main groups that are largely congruent with boundaries along the Appalachian Mountains and the Mississippi River, two major geographic barriers in ENA. Populations located to the east of the Appalachians and along the central Appalachians exhibited relatively higher levels of genetic diversity. Extant lineages may have diverged during the late Miocene, and range expansions of different groups may have happened during the Pleistocene glacial/interglacial cycles. Conclusions Our findings indicate that geographic barriers may have started to facilitate the population divergence in P. peltatum before the Pleistocene. Persistence in multiple refugia, including areas around the central Appalachians during the Quaternary glacial period, and subsequent expansions under hospitable climatic condition, especially westward expansion, are likely responsible for the species’ contemporary genetic structure and phylogeographic pattern.
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