State Key Laboratory of Biocontrol and Guangdong Provincial Key Laboratory of Plant Resources, School of Life Sciences, Sun Yat-sen University, Guangzhou, 510275, China.
Shenzhen Dapeng Peninsula National Geopark, Shenzhen, 518121, China.
BMC Plant Biol. 2024 May 27;24(1):459. doi: 10.1186/s12870-024-05181-7.
Relict species are important for enhancing the understanding of modern biogeographic distribution patterns. Although both geological and climatic changes since the Cenozoic have affected the relict flora in East Asia, the contributions of geographical processes remain unclear. In this study, we employed restriction-site associated DNA sequencing (RAD-seq) and shallow genome sequencing data, in conjunction with ecological niche modeling (ENM), to investigate the spatial genetic patterns and population differentiation history of the relict species Rehderodendron kwangtungense Chun.
A total of 138 individuals from 16 populations were collected, largely covering the natural distribution of R. kwangtungense. The genetic diversity within the R. kwangtungense populations was extremely low (H = 0.048 ± 0.019; H = 0.033 ± 0.011). Mantel tests revealed isolation-by-distance pattern (R = 0.38, P < 0.001), and AMOVA analysis showed that the genetic variation of R. kwangtungense occurs mainly between populations (86.88%, K = 7). Between 23 and 21 Ma, R. kwangtungense underwent a period of rapid differentiation that coincided with the rise of the Himalayas and the establishment of the East Asian monsoon. According to ENM and population demographic history, the suitable area and effective population size of R. kwangtungense decreased sharply during the glacial period and expanded after the last glacial maximum (LGM).
Our study shows that the distribution pattern of southern China mountain relict flora may have developed during the panplain stage between the middle Oligocene and the early Miocene. Then, the flora later fragmented under the force of orogenesis, including intermittent uplift during the Cenozoic Himalayan orogeny and the formation of abundant rainfall associated with the East Asian monsoon. The findings emphasized the predominant role of geographical processes in shaping relict plant distribution patterns.
残余物种对于增强对现代生物地理分布模式的理解非常重要。尽管新生代以来的地质和气候变化都影响了东亚的残余植物区系,但地理过程的贡献仍不清楚。在这项研究中,我们采用了限制性相关 DNA 测序(RAD-seq)和浅层基因组测序数据,结合生态位模型(ENM),调查了残余物种广东润楠的空间遗传格局和种群分化历史。
共采集了来自 16 个种群的 138 个个体,基本涵盖了广东润楠的自然分布范围。广东润楠种群内的遗传多样性极低(H = 0.048 ± 0.019;H = 0.033 ± 0.011)。Mantel 检验显示出隔离距离模式(R = 0.38,P < 0.001),AMOVA 分析表明广东润楠的遗传变异主要发生在种群之间(86.88%,K = 7)。在 23 到 21 百万年前,广东润楠经历了一个快速分化的时期,与喜马拉雅山脉的崛起和东亚季风的建立相吻合。根据 ENM 和种群历史动态,广东润楠的适宜面积和有效种群大小在冰期急剧减少,并在末次冰期最大值后扩大。
我们的研究表明,中国南方山地残余植物区系的分布模式可能在中渐新世至早中新世的平原期形成。然后,在造山运动的作用下,植物区系后来发生了破碎,包括新生代喜马拉雅造山运动期间的间歇性隆起和与东亚季风相关的丰富降雨的形成。这些发现强调了地理过程在塑造残余植物分布模式方面的主导作用。