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《Journal of Glaciology and Geocryology》 2013-06
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The Salinity Change and Its Environmental Significance in Huahai Lake, Hexi Corridor,Northwest China During the Early-Middle Holocene

LI Zhuo-lun;WANG Nai-ang;LI Yu;CHENG Hong-yi;College of Earth and Environmental Sciences/Center for Climatic Change and Hydrologic Cycle in Arid Region, Lanzhou University;  
Carbonate mineral and sulfate mineral composition changes during the Holocene in Huahai Lake were reconstructed using X-ray diffraction,and the K/Na change was reconstructed using X-ray fluorescence.Then,the lake water salinity change was reconstructed during 10.47-5.5 cal ka BP in Huahai Lake.The results showed that carbonate mineral was the main mineral deposition in the lake sediments during the early(10.478.87cal ka BP)and middle Holocene(8.87-5.5 cal ka BP),except for some particular layers.In addition,K/Na ratio was higher in the early Holocene which indicated that lake water salinity in 10.47-8.87cal ka BP was higher than that in 8.87-5.5cal ka BP.It suggested that the water salinity change was consistent with lake level and effective humidity change during the early and middle Holocene,and the water salinity indicated the change in effective precipitation.In addition,combined with the lake dried up,which indicated that the climate became arid during the late Holocene, one can see that Holocene environmental change in Huahai Lake as follows:climate shifted from arid to humid in the early Holocene,and was most humid in the mid-Holocene and arid in the late Holocene.This pattern is different from Asian monsoon areas and westerly areas,showing that the monsoon-westerly transition zone is not only controlled by the Asian monsoon but also affected by westerly winds.
【Fund】: 国家自然科学基金项目(41301217);; 兰州大学中央高校基本科研业务费专项资金(lzujbky-2013-129;lzujbky-2013-127)资助
【CateGory Index】: P343.3
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