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根据南疆博斯腾湖湖相沉积物碳酸盐稳定同位素、孢粉及化学元素含量的研究，揭示了近12000 aB.P.以来古气候与古水文状况的变化过程与特征，其气候的演化特征与新疆地区地质记录基本一致，具有明显的西风型环境演变特征，表现为冷与相对湿润、暖与相对干旱的水热配置关系揭示了本地区近12000 a B.P.以来出现了一系列冷暖变化，其中暖峰主要出现于11 500～11 000 a、9 400 a、7 500 a、3 000 a和2 000 aB.P.,气候特征以干暖为主，湖泊水文特征总体表现为盐度增加，水位下降，湖面缩小；而冷峰主要出现于11 000～10 000 a、8 800 a、5 000 a、3 300 a和1 500 aB.P，主要表现为湿润程度有所改善，相应地，湖泊膨胀淡化，湖面上升而在7 000～5 000 aB.P.期间出现的相对暖湿的环境特征可能是全新世大暖期暖湿的气候特征的反映，可能与此时西南夏季风势力增强有关
Based on the studies on carbonate stable isotopes, sporopollen and chemical elements in the Bosten Lake facies sediments in the southern region, the process and characteristics of paleoclimatic and paleo-hydrological conditions since 12 000 aB.P. are revealed. The geological records in Xinjiang are basically the same, with obvious westerly-type environmental evolution characteristics, showing the hydrothermal configuration relationship of cold and relative humidity, warm and relative drought. It reveals that a series of cold and warm changes have occurred since the region was nearly 12000 a BP The warm peaks mainly occurred in 11 500 ~ 11 000 a, 9 400 a, 7 500 a, 3 000 a and 2 000 aB.P. The climatic characteristics were mainly dry and warm, and the lake hydrological characteristics generally showed an increase in salinity, While the cold peaks mainly appeared in 11 000 ~ 10 000 a, 8 800 a, 5 000 a, 3 300 a and 1 500 aB.P, which mainly showed an improvement in the degree of wetting. Correspondingly, The desorption and desalination of the lake and the rise of the lake The relatively warm and humid environmental characteristics occurred during 7 000-5 000 aB.P. may be the reflection of the warm and humid climatic characteristics of the Holocene Megathermal, which may be attributed to the enhanced strength of the southwesterly summer monsoon About