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《Journal of Glaciolgy and Geocryology》 2002-01
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MIS 3b (54~44 ka BP) Cold Period and Glacial Advance in Middle and Low Latitudes

SHI Ya-feng, YAO Tan-dong (Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou Gansu 730000, China)  
The records of Guliya ice core showed that there was a MIS 3b cold period between 54~44 ka BP, when temperature was 5 ℃ below present average. In contrast to this, temperatures in the warm periods at MIS 3c (early) and MIS 3a (late) were 3 ℃ and 4 ℃ above present average, respectively. This has been proved to be consistent with the insolation changes caused by a precessional cycle of 23 ka and a significant global impact appeared between 65 N~60 S. From preliminary analysis of the literatures concerning well-dated glacier advances during the Last Glaciation, it has been found that MIS 3b cold period resulted in glacial advances at 23 sites of 12 regions in Asia, Europe, North America, South America and Ocean. In this paper the authors give a brief review to these sites. The plentiful precipitation during MIS 3b coupling with the suppressive effect of low temperature on ice ablation, glaciers advanced beyond the extent of the cold-dry MIS 2 between 25~15 ka BP (LGM). Several new dating methods, such as modified optically stimulated luminescence (OSL) method, infrared stimulated luminescence (IRSC) method, cosmogenic {} 3He, {} 10Be, {} 26Al and {} 36Cl dating method, Uranium series dating method, together with {} 14C method, TL method, ESR method and fission track method, effectively improve the dating of several glacial advances during the Last Glaciation. Despite the importance of the records of Guliya ice core in defining the MIS 3b cold period, few data was held on glacial advance during that time in West China, further study is essential.
【Fund】: 中国科学院知识创新工程项目 (KZCX2 30 1;KZCX1 10 0 2 );; 中国科学院寒区旱区环境与工程研究所冰芯与寒区环境重点实验室基金资助
【CateGory Index】: P343.6
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