Comparative evolutionary history of two closely related desert plant, and (Convolvulaceae) from northwest China.

Desert ecosystems are one of the most fragile ecosystems on Earth. The study of the effects of paleoclimatic and geological changes on genetic diversity, genetic structure, and species differentiation of desert plants is not only helpful in understanding the strategies of adaptation of plants to arid habitats, but can also provide reference for the protection and restoration of vegetation in desert ecosystem. Northwest China is an important part of arid regions in the northern hemisphere. and are closely related and have similar morphology. Through our field investigation, we found that the annual precipitation of the two species distribution areas is significantly different. Thus, . and provide an ideal comparative template to investigate the evolutionary processes of closely related species, which have adapted to different niches in response to changes in paleogeography and paleoclimate in northwest China. In this study, we employed phylogeographical approaches (two cpDNA spacers: and ) and species distribution models to trace the demographic history of and , two common subshrubs and small shrubs in northwest China. The results showed the following: (1) Populations of in northwest China were divided into three groups: Tianshan Mountains-Ili Valley, west Yin Mountains-Helan Mountains-Qinglian Mountains, and Qinling Mountains-east Yin Mountains. There was a strong correlation between the distribution of haplotypes and the floristic subkingdom. The three groups corresponded to the Eurasian forest subkingdom, Asian desert flora subkingdom, and Sino-Japanese floristic regions, respectively. Thus, environmental differences among different flora may lead to the genetic differentiation of in China. (2) The west Yin Mountains-Helan Mountains-Qinglian Mountains, and Qinling Mountains-east Yin Mountains were thought to form the ancestral distribution range of (3) and adopted different strategies to cope with the Pleistocene glacial cycle. contracted to the south during the glacial period and expanded to the north during the interglacial period; and there was no obvious north-south expansion or contraction of during the glacial cycle. (4) The interspecific variation of . and was related to the orogeny in northwest China caused by the uplift of the Tibetan Plateau during Miocene. (5) The 200 mm precipitation line formed the dividing line between the niches occupied by . and , respectively. In this study, from the perspective of precipitation, the impact of the formation of the summer monsoon limit line on species divergence and speciation is reported, which provides a new perspective for studying the response mechanism of species to the formation of the summer monsoon line, and also provides a clue for predicting how desert plants respond to future environmental changes.