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中石器时代早期露天遗址费尔施泰纳克(德国福格尔斯贝格县)的石器原材料使用情况。

The use of lithic raw materials at the Early Mesolithic open-air site Feuersteinacker (Vogelsbergkreis, Germany).

作者信息

Hess Thomas, Riede Felix

机构信息

Department of Archaeology and Heritage Studies University of Aarhus Højbjerg Denmark.

出版信息

Geoarchaeology. 2021 Mar-Apr;36(2):252-265. doi: 10.1002/gea.21828. Epub 2020 Oct 23.

DOI:10.1002/gea.21828
PMID:33776201
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC7984161/
Abstract

The open-air site Feuersteinacker near Stumpertenrod has yielded one of the largest lithic assemblages in Central Germany. It repeatedly served as a workshop for the production of stone tools during an early phase of the Mesolithic. The range of lithic raw materials is extremely diverse, but until today, there is only a limited number of archaeological studies on the occurrence of lithic resources in the area. The following study presents the first in-depth investigation of the use of different rock types by Mesolithic hunter-fisher-gatherers at the site. Provenance analyses using petrographic methods permit raw materials to be assigned to a specific source and provide new insights into their formation. Furthermore, this study explores the way in which the materials were processed throughout the reduction sequence. A comparison of topographic parameters suggests that the location was situated on an important transit route during prehistoric times. The presented results contribute to a better understanding of mobility patterns and subsistence strategies of Early Mesolithic groups in Central Germany.

摘要

位于施图普滕罗德附近的费尔施泰纳克露天遗址出土了德国中部最大的石器组合之一。在中石器时代早期,这里曾多次作为石器生产作坊。石器原材料的种类极为多样,但直到如今,对该地区石器资源分布情况进行考古研究的数量仍然有限。以下研究首次对中石器时代的狩猎-捕鱼-采集者在该遗址使用不同岩石类型的情况进行了深入调查。利用岩相学方法进行的产地分析能够将原材料归为特定来源,并为其形成过程提供新的见解。此外,本研究还探究了在整个石器制作过程中材料的加工方式。对地形参数的比较表明,该地点在史前时期位于一条重要的交通要道上。所呈现的研究结果有助于更好地理解德国中部中石器时代早期群体的迁徙模式和生存策略。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0958/7984161/1cf99c8c68c0/GEA-36-252-g001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0958/7984161/edda1bb90131/GEA-36-252-g008.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0958/7984161/382f2ca5bad8/GEA-36-252-g009.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0958/7984161/a9bf08748229/GEA-36-252-g007.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0958/7984161/fe1a849d89e6/GEA-36-252-g006.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0958/7984161/d6fee65091ce/GEA-36-252-g005.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0958/7984161/2a58078f824b/GEA-36-252-g004.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0958/7984161/d2949ba0afc8/GEA-36-252-g003.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0958/7984161/60d976ea4902/GEA-36-252-g002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0958/7984161/1cf99c8c68c0/GEA-36-252-g001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0958/7984161/edda1bb90131/GEA-36-252-g008.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0958/7984161/382f2ca5bad8/GEA-36-252-g009.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0958/7984161/a9bf08748229/GEA-36-252-g007.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0958/7984161/fe1a849d89e6/GEA-36-252-g006.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0958/7984161/d6fee65091ce/GEA-36-252-g005.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0958/7984161/2a58078f824b/GEA-36-252-g004.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0958/7984161/d2949ba0afc8/GEA-36-252-g003.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0958/7984161/60d976ea4902/GEA-36-252-g002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0958/7984161/1cf99c8c68c0/GEA-36-252-g001.jpg

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