泥河湾盆地许家窑遗址古人类生存环境

李潇丽, 马宁. 泥河湾盆地许家窑遗址古人类生存环境[J]. 海洋地质与第四纪地质, 2014, 34(4): 153-161. doi: 10.3724/SP.J.1140.2014.04153
引用本文: 李潇丽, 马宁. 泥河湾盆地许家窑遗址古人类生存环境[J]. 海洋地质与第四纪地质, 2014, 34(4): 153-161. doi: 10.3724/SP.J.1140.2014.04153
LI Xiaoli, MA Ning. PRELIMINARY STUDY ON THE LIVING ENVIRONMENT OF HOMINIDS AT THE XUJIAYAO SITE, NIHEWAN BASIN[J]. Marine Geology & Quaternary Geology, 2014, 34(4): 153-161. doi: 10.3724/SP.J.1140.2014.04153
Citation: LI Xiaoli, MA Ning. PRELIMINARY STUDY ON THE LIVING ENVIRONMENT OF HOMINIDS AT THE XUJIAYAO SITE, NIHEWAN BASIN[J]. Marine Geology & Quaternary Geology, 2014, 34(4): 153-161. doi: 10.3724/SP.J.1140.2014.04153

泥河湾盆地许家窑遗址古人类生存环境

  • 基金项目:

    北京市自然科学基金项目(8133052)

详细信息
    作者简介: 李潇丽(1969-),女,副研究员,主要从事第四纪地质学研究,E-mail:lixiaoli2002@sohu.com
  • 中图分类号: P512.2

PRELIMINARY STUDY ON THE LIVING ENVIRONMENT OF HOMINIDS AT THE XUJIAYAO SITE, NIHEWAN BASIN

  • 许家窑遗址是中国重要的早期智人遗址,在研究东亚现代人及其行为起源和人类生存行为领域具有重要意义。对遗址74093地点地层剖面的粒度、磁化率、碳氧同位素和有机碳分析表明,遗址代表了晚更新世早期至MIS3阶段的梨益沟第三级基座阶地沉积序列,总体显示由牛轭湖逐渐转为河漫滩沉积环境,沉积水动力条件相对较弱。粒度大小和磁化率呈正相关关系,粗颗粒对应较高的磁化率值。剖面沉积经历了由相对温暖湿润→相对稳定的干燥寒冷→波动的干燥寒冷→逐渐转暖4个阶段;古人类集中活动于剖面下部,年代为晚更新世早期,大致对应于MIS5阶段,气候由相对温湿而转为稳定的寒冷环境。动物群指示的古人类活动时期的气候相对冷湿,古植被为疏林草地型景观。
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