Zhou Nian, Miao Ke, Liu Changkun, Jia Linbo, Hu Jinjin, Huang Yongjiang, Ji Yunheng
CAS Key Laboratory for Plant Diversity and Biogeography of East Asia, Kunming Institute of Botany, Chinese Academy of Sciences, Kunming, Yunnan 650201, China.
University of Chinese Academy of Sciences, Beijing 100049, China.
Plant Divers. 2023 Aug 3;46(2):219-228. doi: 10.1016/j.pld.2023.07.009. eCollection 2024 Mar.
Here, we infer the historical biogeography and evolutionary diversification of the genus . For this purpose, we used the complete plastomes of 64 currently accepted species in the genus (14 plastomes were newly sequenced) to recover the phylogenetic backbone of the genus and a time-calibrated phylogenetic framework to estimate biogeographical history scenarios and evolutionary diversification rates of . Our results suggest that ancient climatic changes and geological tectonic activities jointly shaped the distribution range and drove evolutionary radiation of , including the Middle Miocene Climate Optimum (MMCO), the late Miocene global cooling, as well as the successive uplift of the Qinghai-Tibet Plateau (QTP) and the strengthening of the monsoon climate in East Asia during the late Miocene and the Pliocene. This case study suggests that the unique geological and climatic events in the Neogene of East Asia, in particular the uplift of QTP and the enhancement of monsoonal climate, may have played an essential role in formation of uneven distribution of plant diversity in the Northern Hemisphere.
在此,我们推断了该属的历史生物地理学和进化多样化情况。为此,我们使用了该属64个目前已被接受物种的完整质体基因组(其中14个质体基因组是新测序的)来重建该属的系统发育主干,并构建一个时间校准的系统发育框架,以估计其生物地理历史情景和进化多样化速率。我们的结果表明,古代气候变化和地质构造活动共同塑造了其分布范围,并推动了该属的进化辐射,包括中新世中期气候适宜期(MMCO)、晚中新世全球变冷,以及晚中新世和上新世期间青藏高原(QTP)的持续隆升和东亚季风气候的增强。该案例研究表明,东亚新近纪独特的地质和气候事件,特别是青藏高原的隆升和季风气候的增强,可能在北半球植物多样性分布不均的形成中发挥了重要作用。