Li Zhi-Zhong, Lehtonen Samuli, Martins Karina, Wang Qing-Feng, Chen Jin-Ming
Key Laboratory of Aquatic Botany and Watershed Ecology, Wuhan Botanical Garden, Chinese Academy of Sciences, Wuhan 430074, China; Center of Conservation Biology, Core Botanical Gardens, Chinese Academy of Sciences, Wuhan 430074, China.
Herbarium, Biodiversity Unit, University of Turku, Turku 20014, Finland.
Mol Phylogenet Evol. 2022 Jan;166:107334. doi: 10.1016/j.ympev.2021.107334. Epub 2021 Oct 26.
Alismataceae, an ancient lineage of monocots, has attracted attention due to its complex evolutionary history, ornamental value, and ecological role. However, the phylogenetic relationships and evolutionary history of the family have not been conclusively resolved. Here, we constructed the first complete genus-level plastid phylogeny of Alismataceae by using 78 genes and updated the historical biogeography based on the phylogenomic tree. Our results divide the Alismataceae into three major clades with robust support values; one clade comprises the former Limnocharitaceae, and the second clade includes the mainly temperate genera Alisma, Baldellia, Damasonium and Luronium, and the monotypic African genus Burnatia as a sister of the temperate genera. The remaining genera are either tropical or have some temperate species in addition to tropical ones, and they constitute the third major clade. Molecular dating and biogeographic analyses suggest that Alismataceae arose in Neotropical, West Palearctic, and Afrotropical regions during the Cretaceous, followed by the split into three main clades due to a combination of vicariance and dispersal events. Unlike earlier studies, we inferred that the mainly temperate clade likely originated from Afrotropical and West Palearctic regions during the Eocene. The most recent common ancestor of the other two clades lived in the Neotropical area during the Late Cretaceous. Long-distance dispersal and vicariance together seem to contribute to the transoceanic distribution of this family.
泽泻科是单子叶植物的一个古老谱系,因其复杂的进化历史、观赏价值和生态作用而备受关注。然而,该科的系统发育关系和进化历史尚未得到最终解决。在此,我们利用78个基因构建了首个完整的泽泻科属级质体系统发育树,并基于系统发育基因组树更新了历史生物地理学。我们的结果将泽泻科分为三个主要分支,支持值很高;一个分支包括以前的沼草科,第二个分支包括主要分布在温带的泽泻属、矮慈姑属、水筛属和冠果草属,以及单型的非洲属Burnatia,它是温带属的姐妹属。其余的属要么是热带的,要么除了热带物种外还有一些温带物种,它们构成了第三个主要分支。分子年代测定和生物地理分析表明,泽泻科在白垩纪起源于新热带、西古北区和非洲热带地区,随后由于隔离和扩散事件的共同作用而分裂为三个主要分支。与早期研究不同的是,我们推断主要分布在温带的分支可能在始新世起源于非洲热带和西古北区。另外两个分支的最近共同祖先在晚白垩世生活在新热带地区。远距离扩散和隔离似乎共同促成了该科的跨洋分布。