首页|鲁中山地黄土区旧石器时代遗存的考古学观察

鲁中山地黄土区旧石器时代遗存的考古学观察

扫码查看
作为气候反映的载体之一,黄土记录了全球气候系统冷暖干湿变化的主要轨迹.鲁中山地黄土区域存在发现旧石器遗址的条件并已被逐步证明.此外本区发育有丰富的天然洞穴以及层级清楚的河流阶地,这些第四纪地层堆积是发现旧石器遗存和开展考古工作的基础.考古工作者通过近10年来持续的野外工作,发现自晚更新世以来不同石器发展阶段的众多遗址.尤其以沂水县跋山遗址和水泉峪遗址最为重要,二者在地层层序、年代与文化发展序列存在一致性与连贯性特点,清楚地再现了本区距今10万年以来旧石器文化连续发展的历史进程.本文在梳理和评述已有考古学材料、分析新发现遗存材料的基础上,进一步结合实际工作提出各地区未来工作潜力,并尝试在山东地区构筑宏观的旧石器文化发展序列.
As one of the carriers reflecting climate change,the loess has recorded the major trajectories of the global climate system's variations in temperature and humidity.The loess region in the central mountains of Shandong province has the potential for discovering Paleolithic sites,which has also been gradually verified.Additionally,this area is characterized by an abundance of natural caves and river terraces with distinct levels.These Quaternary strata deposits form the foundation for discovering Paleolithic remains and conducting archaeological work.Through the continuous field work of archaeologists in the past 10 years,numerous sites of different stone tool development stages have been discovered since the late Pleistocene.In particular,the Bashan Site and Shuiquanyu Site in Yishui County are the most important ones.The consistency and coherence of their stratigraphic sequences,dating,and cultural development sequences clearly reproduce the continuous development of Paleolithic culture in this region since 100,000 years ago.This article organizes and evaluates the existing archaeological materials in the region,with a focus on the material analysis of recently discovered remains.It also proposes the potential for future work in each area based on practical experience and attempts to construct a macroscopic sequence of Paleolithic cultural development in the Shandong region.

The loess region in the central mountains of ShandongPaleolithic

李罡

展开 >

山东省文物考古研究院

鲁中山地黄土区 旧石器时代 跋山遗址群 文化发展序列

国家社会科学基金一般项目山东省社科联人文社会科学课题智库重点项目(2023)

19BKG008

2024

南方文物
江西省文物考古研究所 江西省博物馆

南方文物

CHSSCD北大核心
影响因子:0.131
ISSN:1004-6275
年,卷(期):2024.(2)
  • 57