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山西匼河旧石器遗址作为中国北方重要的早期人类活动遗址,其年代问题长期以来备受学界关注。本文通过对匼河遗址6054地点含匼河文化层上部的黄土—古土壤序列进行详细的岩石磁学及系统的磁性地层学研究,结合已有地质、古生物及考古学资料,重新探讨该遗址的年代及地质意义。匼河遗址的磁性地层序列显示其主要形成于中更新世早期,记录了布容正极性时(Brunhes normal chron),与西侯度遗址、丁村遗址等周边遗址在年代序列上具有连续性,为构建华北地区旧石器时代早期文化序列及古环境演变提供了新的证据,完善了中国旧石器考古年代学框架。
Abstract：The Kehe Paleolithic site in southern Shanxi Province, is a significant early human activity site in northern China, and has long been a focus of academic attention regarding its chronological dating. In this study, detailed rock magnetic and systematic magnetostratigraphic analyses were conducted on the loess-paleosol sequence overlying the Kehe cultural layer at locality 6054 of the Kehe sites. Combined with existing geological, paleontological, and archaeological data, the chronology and geological significance of the site were re-examined. The magnetostratigraphic sequence of the Kehe site indicates that it was formed in mainly the early Middle Pleistocene and recorded the Brunhes normal chron. Meanwhile, it shows chronological continuity with surrounding sites such as the Xihoudu site and the Dingcun site, which provided new evidence for constructing the early Paleolithic cultural sequence and paleoenvironmental evolution in North China, and improved the chronological framework of Chinese Paleolithic archaeology.
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基本信息:
DOI：10.19839/j.cnki.dcxzz.2025.0034
中图分类号:K878;P539.3;P597.3
引用信息:
[1]刘平.山西匼河遗址6054点黄土—古土壤磁性地层年代学再研究[J].地层学杂志,2025,49(04):501-508.DOI:10.19839/j.cnki.dcxzz.2025.0034.
基金信息:
国家自然科学基金(41974075); 国家重点研发计划项目(2023YFF0804503)共同资助
2025-11-28
2025-11-28
2025-11-28