匼河遗址6054地点黄土-古土壤剖面磁性地层学的年代研究MAGNETOSTRATIGRAPHIC AGE OF PLEISTOCENE LOESS/PALEOSOL SECTIONS AT KEHE,SHANXI
刘平,Reidar Lovlie
摘要(Abstract):
发现于1957年的匼河文化遗址的年代一直存在较大的争议。近四十年来,考古学和地学工作者虽然从化石、地层等多方面研究,但仍未得出令人信服的可靠结论。受许家窑遗址及小长梁遗址的最新磁性地层学研究结果的启示,过去两年对山西南部匼河遗址从磁性地层学的角度进行了深入、系统的研究,研究发现匼河遗址剖面的磁化率曲线呈顶部高,中间2.5m到13m处较宽阔的低值带,具有华北黄土高原黄土L9的特征,底部又呈高值的分布趋势,这种磁化率的分布关系与洛川标准剖面的S7-S12有较好的对应关系,从而得出文化层以上地层剖面的年代范围为0.7-1.02Ma,由此可推算位于底部磁化率高值带以下的文化层的年代至少早于1.02Ma,完全不同于匼河文化遗址0.247Ma的现行认识,而与苏朴、朱日祥等人对许家窑、小长梁遗址,马圈沟遗址年代的最新认识趋向一致。
关键词(KeyWords): 磁性地层学;洛川标准剖面;匼河文化遗址;许家窑遗址;小长梁遗址;马圈沟遗址;更新世;山西
基金项目(Foundation): 2003年度国家最高科学技术奖资助
作者(Author): 刘平,Reidar Lovlie
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