Migration patterns of Gentiana crassicaulis, an alpine gentian endemic to the Himalaya-Hengduan Mountains

The Himalaya-Hengduan Mountain region is one of the hotspots of biodiversity research. The uplift of the Qinghai-Tibetan Plateau (QTP) and the Quaternary glaciation caused great environmental changes in this region, and the responses of many species in the QTP to the Quaternary climate are still largely unknown. The genetic structure and phylogeographical history of Gentiana crassicaulis Duthie ex Burk, an endemic Chinese alpine species in this area, were investigated based on four chloroplast fragments and internal transcribed spacer region of the nuclear ribosomal DNA (nrITS) sequences of 11 populations. The populations with highly diverse chloroplast haplotypes were mainly found at the edge of the QTP. There were two main haplotypes of nrITS clones, one shared by the Yunnan and Guizhou populations, and the other by the remaining populations. The population with the highest diversity was the Gansu population, located at the edge of the plateau. Based on molecular dating, the diversification of G. crassicaulis at the edge of the plateau occurred before the Last Glacial Maximum (LGM), and the species may have completed its expansion from the edge to the platform. Ecological niche models were conducted to predict the distributional ranges of G. crassicaulis at present, during the LGM, and during the last interglacial (LIG) period. The results demonstrated that G. crassicaulis survived on the QTP platform and at the edge during the LGM but afterward retreated from the platform to the southern edge, followed by expansion to the platform.

Automated summary

Gentiana crassicaulis, an endemic alpine species in the Himalaya-Hengduan Mountain region, exhibits high genetic diversity at the edge of the Qinghai-Tibetan Plateau. Molecular dating suggests that its diversification occurred before the Last Glacial Maximum, indicating its expansion from the edge to the plateau. Ecological niche modeling demonstrates its survival on the plateau and retreat to the southern edge during the Last Glacial Maximum, followed by further expansion to the plateau.