Herrando-Moraira Sonia, Roquet Cristina, Calleja Juan Antonio, Chen You-Sheng, Fujikawa Kazumi, Galbany-Casals Mercè, Garcia-Jacas Núria, Kim Seung-Chul, Liu Jian-Quan, Liu Lian, López-Alvarado Javier, López-Pujol Jordi, Mandel Jennifer R, Mehregan Iraj, Sennikov Alexander N, Vilatersana Roser, Xu Lian-Sheng, Susanna Alfonso
Botanic Institute of Barcelona (IBB, CSIC-Ajuntament de Barcelona), Pg. del Migdia, s.n., 08038 Barcelona, Spain.
Botanic Institute of Barcelona (IBB, CSIC-Ajuntament de Barcelona), Pg. del Migdia, s.n., 08038 Barcelona, Spain.
Mol Phylogenet Evol. 2025 Nov;212:108420. doi: 10.1016/j.ympev.2025.108420. Epub 2025 Jul 20.
The Tibet-Himalaya-Hengduan region (THH) harbours the world's richest temperate alpine flora. To investigate the main evolutionary and ecological processes underlying this outstanding biodiversity, we tested multiple hypotheses focusing in Saussurea (Compositae), a representative genus of ca. 450 species that extensively diversified in THH and adjacent regions. We built a highly-resolved phylogeny based on hundreds of nuclear loci and a broad sampling (70 % of genus richness). We integrated phylogenetic, ecological, geographic, topographic and climatic data with biogeographic and diversification modelling methods. Our results suggest that Hengduan Mountains acted both as evolutionary cradle and museum. Repeated bidirectional biogeographic exchanges between Asian regions substantially contributed to current biodiversity patterns. Uplift and mountain building established favourable conditions for later evolutionary radiations by providing high topographic heterogeneity. However, orogeny alone does not explain the evolutionary radiation of Saussurea and its diversification burst in the Late Miocene with a double-fold increase in speciation rate. Besides orogeny, the main factors associated with current biodiversity are: (1) the interplay of steep altitudinal gradients and topographic heterogeneity with moderate climatic oscillations during the Late Miocene; (2) relative climatic stability during Pleistocene dramatic climatic oscillations, which may have reduced extinction rates; and (3) sufficient annual precipitation (>400 mm).
西藏-喜马拉雅-横断山地区(THH)拥有世界上最丰富的温带高山植物区系。为了探究这种杰出生物多样性背后的主要进化和生态过程,我们针对风毛菊属(菊科)检验了多个假说,该属约有450个物种,在THH及其相邻地区广泛分化。我们基于数百个核基因座和广泛采样(涵盖该属70%的物种丰富度)构建了一个分辨率很高的系统发育树。我们将系统发育、生态、地理、地形和气候数据与生物地理和多样化建模方法相结合。我们的结果表明,横断山脉既是进化摇篮又是博物馆。亚洲各区域之间反复的双向生物地理交流对当前的生物多样性格局有很大贡献。隆升和造山运动通过提供高度的地形异质性为后来的进化辐射创造了有利条件。然而,仅造山运动并不能解释风毛菊属的进化辐射及其在晚中新世的多样化爆发,其时物种形成速率增加了一倍。除了造山运动,与当前生物多样性相关的主要因素有:(1)晚中新世期间陡峭的海拔梯度和地形异质性与适度的气候振荡之间的相互作用;(2)更新世剧烈气候振荡期间相对的气候稳定性,这可能降低了灭绝速率;以及(3)充足的年降水量(>400毫米)。