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黄河中游渑池盆地湖泊沉积记录的古气候变化及其意义

DOI: 10.3969/j.issn.1001-7410.2011.01.19, PP. 150-162

Keywords: 渑池盆地,湖泊沉积物,气候环境变迁,仰韶文化

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Abstract:

渑池盆地位于黄河中游,处在黄土高原向华北平原的过渡地带,该区域也是我国东部湿润区和半湿润区的交汇地带。文章通过对位于渑池盆地池底村厚约4mm古湖泊沉积剖面进行了14C年代(校正为日历年龄)、有机碳含量、粒度和地球化学元素组成等测试分析,重建了研究区19.5cal.kaB.P.以来的气候变化过程。19543~9240cal.aB.P.期间,气候比较干旱,风化淋溶作用较弱,湖泊尚未形成;9240~8039cal.aB.P.为气候过渡时期,气候向暖湿方向转变,古湖泊开始形成;8039~5368cal.aB.P.为暖湿气候类型,对应于全新世大暖期的鼎盛时期,湖盆流域温暖湿润,湖泊的水位较高;5368~3439cal.aB.P.为亚暖湿气候类型;3439~2423cal.aB.P.气候环境比较恶劣,之后气候向干旱化方向发展,又分为两个亚段:3439~2931cal.aB.P.气候出现剧烈波动,2931~2423cal.aB.P.湖泊干枯。盆地的文化演进与环境变化间存在着耦合关系,环境的变化对应黄河中游地区相继发展的裴李岗文化、仰韶文化、龙山文化和夏商文化。

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