天山小尤尔都斯盆地湖积物的沉积学与孢粉分析研究表明，全新世以来，该区距今4000年以前及以后至少有两次湖泊发育期。该区域湖泊的兴衰历史表明，全新世环境变化显著，气候呈现冷暖与干湿波动。 Sedimentology and sporopollen analysis of the lake sediments in the Tien-Shan Jurduols Basin indicate that since the Holocene, the region has had at least two lacustrine periods before and after 4000 years ago. The history of the rise and fall of lakes in the region shows that the Holocene environment changes significantly, and the climate is warm and wet and wet and dry.