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扎布耶盐湖位于西藏青藏高原腹地。通过该湖ＺＫ２钻孔的孢粉分析，揭示了约３６０００ａＢ．Ｐ．以来扎布耶地区的气候和湖盆演变。约在３６０００－３３０００ａＢ．Ｐ．，扎布耶地区为森林草原，气候冷、湿；约３３０００－３００００ａＢ．Ｐ．，为灌丛草原，气候温、干；约３００００－２７５００ａＢ，Ｐ．为干旱草原，气候偏暖、湿；约１８０００－１２０００ａＢ．Ｐ．，为干旱草原，环境寒冷，干燥；约１２０００－４０００ａＢ．Ｐ．，扎布耶地区各类草本植物繁茂，气候偏温、干。另外，根据水生藻类化石群的分析，自３６０００ａＢ．Ｐ以来，扎布耶盐湖有三次湖进、淡水湖期，同时也有三次湖退事件。
Zabuye Salt Lake is located in the hinterland of Tibetan Plateau in Tibet. Sporopollen analysis through the lake ZK2 boreholes revealed about 36,000 aB. P. Since the climate and lake basin evolution in Zabuyeh area. About 36000-33000aB. P. , Zabuye region forest grassland, cold and wet climate; about 33000-30000aB. P. , For the shrub grasslands, climate warm, dry; about 30000-27500aB, P. For the dry grasslands, the climate is warm and wet; about 18000-12000aB. P. , Arid steppe, the environment is cold and dry; about 12000-4000aB. P. , All kinds of herbaceous plants in Zabuyeh region are lush, climate is warm and dry. In addition, based on the analysis of aquatic algal fossil populations, since 36000aB. Since P, there have been three lakes and freshwater lakes in the Zaboye Salt Lake and three retreats in the lake at the same time.