Phylogeny and biogeography of Maianthemum (Asparagaceae: Nolinoideae) revisited with emphasis on its divergence pattern in SW China.
Phylogeny and biogeography of Maianthemum (Asparagaceae: Nolinoideae) revisited with emphasis on its divergence pattern in SW China.
复制标题
重温舞花(天门冬科:Nolinoideae)的系统发育和生物地理学,重点关注其在中国西南地区的分化模式
DOI:
10.1016/j.pld.2021.02.001
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发表时间:
2021-04
期刊:
影响因子:
4.8
通讯作者:
Nie ZL
中科院分区:
文献类型:
--
作者:
Meng R;Meng Y;Yang YP;Nie ZL
Maianthemum is a genus with more than 35 species from the tribe Polygonateae (Asparagaceae), widely distributed between North to Central Americas and eastern Asia with high diversity in the eastern Himalayas to the Hengduan Mountains of SW China. Although most species from SW China form a well-supported clade, phylogenetic relationships within this clade remain unclear. With a broad level of taxon sampling and an extensive character sampling from eight DNA regions, this study intends to revisit the phylogeny and biogeography of the genus to better understand the divergence patterns of species from SW China. Phylogenetic results suggested the monophyly of Maianthemum with recognition of nine strongly supported clades, but backbone relationships among these clades remained largely uncertain. For the SW China clade, individuals from the same species are grouped into different lineages. Our results revealed that the fast radiation of the SW China clade was occurred in the eastern Himalayas, followed by subsequent radiation in the Hengduan Mountains in the Pliocene. Intercontinental disjunctions of Maianthemum in the Northern Hemisphere appear to have occurred multiple times during the late Miocene to the Pliocene, likely resulted by a combination of both vicariance and long-distance dispersal events. Nine lineages are recognized in Maianthemum, corresponding to their biogeographic distribution in the Old and New World. A radiation was occurred in the eastern Himalayas, with eastward diversification in the Hengduan Mountains in the Pliocene. Disjunctions in the Northern Hemisphere appear to have occurred multiple times during the late Miocene to the Pliocene.
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