TY - JOUR
T1 - Testing evolutionary hypotheses for the world's main hotspot of temperate alpine flora using Saussurea (Compositae) as a model
AU - Herrando-Moraira, Sonia
AU - Roquet, Cristina
AU - Calleja, Juan Antonio
AU - Chen, You Sheng
AU - Fujikawa, Kazumi
AU - Galbany-Casals, Mercè
AU - Garcia-Jacas, Núria
AU - Kim, Seung Chul
AU - Liu, Jian Quan
AU - Liu, Lian
AU - López-Alvarado, Javier
AU - López-Pujol, Jordi
AU - Mandel, Jennifer R.
AU - Mehregan, Iraj
AU - Sennikov, Alexander N.
AU - Vilatersana, Roser
AU - Xu, Lian Sheng
AU - Susanna, Alfonso
N1 - Publisher Copyright:
© 2025 The Authors
PY - 2025/11
Y1 - 2025/11
N2 - 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).
AB - 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).
KW - Alpine flora
KW - Climatic stability
KW - Evolutionary radiations
KW - Mountain-geobiodiversity hypothesis
KW - Qinghai-Tibetan Plateau
KW - Saussurea
UR - https://www.scopus.com/pages/publications/105011604223
U2 - 10.1016/j.ympev.2025.108420
DO - 10.1016/j.ympev.2025.108420
M3 - Article
C2 - 40695417
AN - SCOPUS:105011604223
SN - 1055-7903
VL - 212
JO - Molecular Phylogenetics and Evolution
JF - Molecular Phylogenetics and Evolution
M1 - 108420
ER -