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对发育于玉龙山东麓海拔约 ３０００ｍ，年代为 ５００－７００ ｋａＢＰ的古土壤进行了系统研究．结果表明，古土壤经历了典型的红壤化过程，是湿热环境的产物；而当地的现代土壤为寒温条件下形成的弱生草灰化土．这种巨大的差异反映了青藏高原东南部５００～７００ ｋａ以来有过大幅度的隆升．根据现代红壤发育条件作比较保守的估算，该时期以来此地区隆升的幅度超过 ８００ ｍ．
A systematic study was carried out on paleosol that developed at the eastern foot of Yulong Mountain at an altitude of about 3000m with an age of 500-700 ka BP. The results show that the ancient soil underwent a typical process of red soil is the product of hot and humid environment; while the local modern soil is poor grass habitat formation of cold grass. This huge difference reflects that there has been a substantial uplift since 500-700 ka in the southeastern Tibetan Plateau. Based on a more conservative estimate of the developmental conditions of modern red soils, the uplift of this region has been over 800 m since that time.