了解高山生物群是如何对历史环境变化作出反应的，可以提高我们预测和减轻全

Understanding how alpine biota respond to historical environmental changes can improve our ability to predict and mitigate the threats to alpine species from global warming. In the world's rich temperate alpine flora, that is, the alpine flora of the Himalaya-Hengduan region, the phylogenetic reconstruction of the evolution of the biogeographical distribution range shows that the existing lineage appeared in the Early Oligocene and the diversified First Hengduan Mountains. In the early to middle Miocene, the accelerated diversification and colonization of neighboring areas may be driven by the intensification of the orogeny and the Asian monsoon. The Alpine flora of the Hengduan Mountains has been around for longer than any other alpine flora on earth, which illustrates how modern biota has been shaped by past geological and climatic events

了解高山生物群是如何对历史环境变化作出反应的，可以提高我们预测和减轻全球变暖对高山物种的威胁的能力。在世界丰富的温带高山植物区系，即喜马拉雅-横断地区的高山植物区系中，生物地理分布范围演化的系统发育重建表明，现存谱系出现于早渐新世和多样化的第一横断山脉。在中新世早期到中期，加速的多样化和邻近地区的殖民化，可能是由造山运动和亚洲季风的强化共同驱动的。阿尔卑斯横断山脉的阿尔卑斯植物群已经存在的时间比地球上任何其他阿尔卑斯植物群都要长，这说明了现代生物群是如何被过去的地质和气候事件所塑造的

Understanding how Alpine biota responds to historical environmental changes can improve our ability to predict and mitigate the threat of global warming to alpine species. In the world's abundant temperate alpine flora, that is, the alpine flora in the Himalaya Hengduan region, the phylogenetic reconstruction of the evolution of biogeographic distribution range shows that the existing lineage appeared in the early Oligocene and the first Hengduan Mountain. During the early to middle Miocene, the accelerated diversification and colonization of adjacent areas were probably driven by orogeny and intensification of Asian monsoon. The alpine flora of the Hengduan Mountains of the Alps has existed longer than any other alpine flora on earth, which shows how modern biota has been shaped by past geological and climatic events<br>