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科学通报  2011 

阿拉善高原晚第四纪高湖面与大湖期的再探讨

, PP. 1367-1377

Keywords: 阿拉善高原,沙漠,MIS3阶段,高湖面,大湖期

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Abstract:

中国西北地区晚更新世湖泊演变和水文循环是第四纪科学研究的热点,但近年来随着研究的深入而存在一些争论,其焦点之一就是晚更新世高湖面形成的时代.通过对阿拉善高原的野外考察、岸堤测量及14C定年,在该区域晚更新世高湖面与大湖期的研究上,不仅获得了更多的地貌学、沉积学证据,而且对高湖面的形成时期有了新的认识,为开展干旱区水循环与水资源演变研究提供了基础资料.考察发现,居延海地区至少存在10道不同海拔高度的砂砾质岸堤,吉兰泰盐湖西北岸发现至少存在4道古湖岸堤,猪野泽东北岸存在9道砂砾质岸堤和一级湖成阶地.对上述古湖岸堤中遗存的瓣鳃类、腹足类生物壳体等14C测年结果及雅布赖盐湖地层年代进行分析,确证MIS3阶段阿拉善高原存在最大高湖面.现有的OSL年代数据虽然与已报道的14C年代及本研究的14C年代结果存在较大分歧,甚至有些OSL年代结果不支持MIS3阶段存在高湖面,但不足以否定MIS3阶段存在高湖面的基本结论.这两种测年结果的差异很可能指示了两个不同时期在同一区域均存在高湖面,也暗示了阿拉善高原可能在MIS5阶段和MIS3阶段早期均存在高湖面.

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