Abstract
The formation of pantropical intercontinental disjunction (PID) in plants has generally been attributed to vicariance, boreotropical migration, and long-distance dispersal. However, this pattern has primarily been examined in herbs, shrubs, and trees, and less commonly studied in interlayer plant taxa. Here we examined evolutionary processes that resulted in the PID of a pantropical woody liana, Uncaria (Rubiaceae). We first constructed a comprehensive phylogeny by employing 73 plastid protein-coding sequences from 29 accessions of Uncaria (including 16 newly sequenced) from different continents. We then inferred divergence time, history and ecological niche evolution of this genus. Our results showed that Uncaria consisted of four well-supported clades that belonged to two geographically distinct lineages: the Asia-Oceania lineage and the Afro-Neotropical lineage. Biogeographic reconstruction showed this genus likely originated in Asia during the early Miocene (ca. 19.03 Ma) and the Middle Miocene Climatic Optimum may have triggered the early diversification of Uncaria. Due to its recent origin and small seeds with long wings, wind or water-mediated long-distance dispersal may have contributed to the distribution of Uncaria in tropical Oceania (via stepping-stone dispersal) and tropical Africa and America (by transoceanic dispersal). Our findings also indicate that diversification of Uncaria was primarily driven by ecological niche divergence, particularly climatic factors. Our study emphasizes the dual role of climatic niche divergence and long-distance dispersal in shaping the PID of Uncaria, providing references for many other extant lineages with similar distributions.