Out of the Himalaya-Hengduan Mountains: Phylogenomics, biogeography and diversification of Polygonatum Mill. (Asparagaceae) in the Northern Hemisphere

• Published in: Molecular phylogenetics and evolution Vol. 169; p. 107431
• Main Authors: Xia, Maoqin, Liu, Ying, Liu, Jingjing, Chen, Donghong, Shi, Yan, Chen, Zhongxia, Chen, Dingrui, Jin, Ruofan, Chen, Hongliang, Comes, Hans Peter, Zhu, Shanshan, Li, Pan, Si, Jinping, Qiu, Yingxiong
• Format: Journal Article
• Language: English
• Published: United States Elsevier Inc 01-04-2022
• Subjects: Asparagaceae; Biogeography; Chromosomal evolution; Ecosystem; Himalaya-Hengduan Mountains; Phylogeny; Phylogeography; Plants; Plastome; Polygonatum; Biogeography; Plastome; Polygonatum; Chromosomal evolution; Phylogeny; Himalaya-Hengduan Mountains
• ISSN: 1055-7903; 1095-9513
• DOI: 10.1016/j.ympev.2022.107431

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•This study provided a robust phylogenetic framework of Polygonatum, based on whole-plastome data.•Polygonatum originated in the HHM region during the early Miocene (c. 20.10 Ma), as well as began to radiate and disperse to other regions since the mid-Miocene.•Decreasing dysploidy accompanied by karyotype change and polyploidization in Polygonatum appears to be associated with its diversification and colonization.
Clarifying the process of formation of diversity hotspots and the biogeographic connection between regions is critical in understanding the impact of environmental changes on organismal evolution. Polygonatum (Asparagaceae) is distributed across the Northern Hemisphere. It displays an uneven distribution, with more than 50% of its species occurring in the Himalaya-Hengduan Mountains (HHM). Here, we generated a time-calibrated phylogeny of Polygonatum, based on whole-plastome data, to reconstruct the genus’ biogeographical history and morphological/chromosomal evolution. Our phylogenetic analyses strongly support the monophyly of Polygonatum and its division into three sections (i.e., Verticillata, Sibirica, and Polygonatum). Polygonatum originated from the HHM region during the early-Miocene (c. 20.10 Ma), and began to radiate since the mid-Miocene, driven by the uplift of the Qinghai–Tibet Plateau (QTP), increasingly colder/arid climates following the mid-Miocene Climatic Optimum (MMCO), and intensification of the East Asian winter monsoon. Dispersal from the HHM region to other regions was facilitated by the intensification of East Asian summer monsoon in response to global climatic warming during the MMCO. Decreasing dysploidy accompanied by karyotype change and polyploidization in Polygonatum appears to be associated with its diversification and colonization of new ecological niches. Our results highlight the importance of regional tectonic activities and past climatic changes from the Neogene onwards to the spatial–temporal diversification and distribution patterns of plant lineages with a wide distribution in the Northern Hemisphere. They also contribute to the knowledge of the uneven species richness between East Asia and other regions.