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地球学报  2008 

罗布泊盐湖晚更新世末期芒硝岩沉积及其古气候意义

DOI: 10.3975/cagsb.2008.04.01

Keywords: 罗布泊,盐湖,更新世,芒硝岩,冷期气候

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Abstract:

罗布泊位于新疆塔里木盆地的东端,可能是世界最大的单体(干)盐湖。罗布泊从中更新世开始进入盐湖演化阶段,直到晚更新世末以钙芒硝沉积为主,进入全新世出现石盐沉积。一些钻孔揭示在上更新统顶部出现一些芒硝岩薄层,对比研究,确认这些钻孔中的芒硝层属同一时期沉积产物。14C测年显示,芒硝层段年代从13.72~16.92ka,光释光测年结果为19.34~19.83ka,这些与末次冰期最盛期的年代(14~22ka)基本吻合,推断当时罗布泊年均气温在-2~-3℃。至全新世早期,随着短期干冷气候结束,罗布泊转为咸水湖环境,自全新世中期以来,转变为盐湖环境。

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