Xia Maoqin, Liu Ying, Liu Jingjing, Chen Donghong, Shi Yan, Chen Zhongxia, Chen Dingrui, Jin Ruofan, Chen Hongliang, Zhu Shanshan, Li Pan, Si Jinping, Qiu Yingxiong
Systematic & Evolutionary Botany and Biodiversity group, MOE Laboratory of Biosystem Homeostasis and Protection, College of Life Sciences, Zhejiang University, Hangzhou, Zhejiang 310058, China; Wuhan Botanical Garden, Chinese Academy of Sciences, Wuhan, Hubei 430074, China.
Systematic & Evolutionary Botany and Biodiversity group, MOE Laboratory of Biosystem Homeostasis and Protection, College of Life Sciences, Zhejiang University, Hangzhou, Zhejiang 310058, China.
Mol Phylogenet Evol. 2022 Apr;169:107431. doi: 10.1016/j.ympev.2022.107431. Epub 2022 Feb 5.
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.
阐明多样性热点地区的形成过程以及各地区之间的生物地理联系,对于理解环境变化对生物进化的影响至关重要。黄精属(天门冬科)分布于北半球。其分布不均,超过50%的物种出现在喜马拉雅 - 横断山脉地区(HHM)。在此,我们基于全叶绿体基因组数据构建了一个时间校准的黄精属系统发育树,以重建该属的生物地理历史以及形态/染色体进化。我们的系统发育分析有力地支持了黄精属的单系性及其划分为三个组(即轮叶组、玉竹组和黄精组)。黄精属在中新世早期(约2010万年前)起源于HHM地区,并自中新世中期开始辐射分化,这是由青藏高原(QTP)隆升、中新世气候适宜期(MMCO)之后日益寒冷/干旱的气候以及东亚冬季风增强所驱动的。在MMCO期间,由于全球气候变暖导致东亚夏季风增强,促进了从HHM地区向其他地区的扩散。黄精属中伴随核型变化和多倍体化的非整倍体减少似乎与其多样化以及新生态位的定殖有关。我们的结果突出了自新近纪以来区域构造活动和过去气候变化对北半球广泛分布的植物谱系时空多样化和分布格局的重要性。它们也有助于我们了解东亚与其他地区物种丰富度不均的情况。