Archeomagnetic Age of Ceramic Fragments from the Archeological Multilayered Monument Ivanovskoe III

IF 1 4区 地球科学 Q4 GEOCHEMISTRY & GEOPHYSICS
O. V. Pilipenko, Yu. B. Tsetlin
{"title":"Archeomagnetic Age of Ceramic Fragments from the Archeological Multilayered Monument Ivanovskoe III","authors":"O. V. Pilipenko,&nbsp;Yu. B. Tsetlin","doi":"10.1134/S1069351325700387","DOIUrl":null,"url":null,"abstract":"<p>Based on an archeomagnetic study of four ceramic fragments from two cultural layers of the multilayer archeological site Ivanovskoe III, the age of the ceramics is proposed based on the correlation with the <i>VADM</i> reference curve for the central part of the Russian Plain. For two ceramic fragments from the first cultural layer, the age of the Late Bronze Age, determined typologically and by the radiocarbon method, is consistent with the age determined by correlation with the <i>VADM</i> reference archeomagnetic data. Radiocarbon dates from undecomposed wood found in the peat layer beneath the second cultural layer have a wide range of values. Comparison with the graph of the <i>VADM</i> dependence on age for the central part of the Russian Plain allows us to state that one of the ceramic fragments found in the second cultural layer has a Neolithic age. For the second ceramic fragment from the second cultural layer, low <i>VADM</i> values were obtained, uncharacteristic of either the Late Bronze Age or the Developed Neolithic. A distinctive feature of samples with low <i>VADM</i> determinations is that they contain thermally unstable maghemite. The age of the second ceramic fragment may correspond to the Early Neolithic as a result of mixing of layers due to the economic activity of people who repeatedly inhabited this area.</p>","PeriodicalId":602,"journal":{"name":"Izvestiya, Physics of the Solid Earth","volume":"61 3","pages":"334 - 345"},"PeriodicalIF":1.0000,"publicationDate":"2025-08-06","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Izvestiya, Physics of the Solid Earth","FirstCategoryId":"89","ListUrlMain":"https://link.springer.com/article/10.1134/S1069351325700387","RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q4","JCRName":"GEOCHEMISTRY & GEOPHYSICS","Score":null,"Total":0}
引用次数: 0

Abstract

Based on an archeomagnetic study of four ceramic fragments from two cultural layers of the multilayer archeological site Ivanovskoe III, the age of the ceramics is proposed based on the correlation with the VADM reference curve for the central part of the Russian Plain. For two ceramic fragments from the first cultural layer, the age of the Late Bronze Age, determined typologically and by the radiocarbon method, is consistent with the age determined by correlation with the VADM reference archeomagnetic data. Radiocarbon dates from undecomposed wood found in the peat layer beneath the second cultural layer have a wide range of values. Comparison with the graph of the VADM dependence on age for the central part of the Russian Plain allows us to state that one of the ceramic fragments found in the second cultural layer has a Neolithic age. For the second ceramic fragment from the second cultural layer, low VADM values were obtained, uncharacteristic of either the Late Bronze Age or the Developed Neolithic. A distinctive feature of samples with low VADM determinations is that they contain thermally unstable maghemite. The age of the second ceramic fragment may correspond to the Early Neolithic as a result of mixing of layers due to the economic activity of people who repeatedly inhabited this area.

Abstract Image

考古多层纪念碑陶瓷碎片的考古磁年龄
基于对多层考古遗址Ivanovskoe III的两个文化层的四个陶瓷碎片的考古磁研究,基于与俄罗斯平原中部VADM参考曲线的相关性,提出了陶瓷的年龄。对于第一文化层的两块陶瓷碎片,通过类型学和放射性碳方法确定的青铜时代晚期的年龄与VADM参考考古磁数据的对比确定的年龄一致。在第二文化层之下的泥炭层中发现的未分解木材的放射性碳年代测定值具有广泛的价值。与俄罗斯平原中部的VADM依赖于年龄的图表进行比较,我们可以声明,在第二层文化层中发现的陶瓷碎片之一属于新石器时代。对于来自第二文化层的第二个陶瓷碎片,获得了较低的VADM值,既不具有青铜时代晚期的特征,也不具有发达的新石器时代的特征。具有低VADM测定的样品的一个显著特征是它们含有热不稳定的磁铁矿。第二个陶瓷碎片的年代可能对应于新石器时代早期,这是由于反复居住在该地区的人们的经济活动导致的混合层的结果。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
求助全文
约1分钟内获得全文 求助全文
来源期刊
Izvestiya, Physics of the Solid Earth
Izvestiya, Physics of the Solid Earth 地学-地球化学与地球物理
CiteScore
1.60
自引率
30.00%
发文量
60
审稿时长
6-12 weeks
期刊介绍: Izvestiya, Physics of the Solid Earth is an international peer reviewed journal that publishes results of original theoretical and experimental research in relevant areas of the physics of the Earth''s interior and applied geophysics. The journal welcomes manuscripts from all countries in the English or Russian language.
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
确定
请完成安全验证×
copy
已复制链接
快去分享给好友吧!
我知道了
右上角分享
点击右上角分享
0
联系我们:info@booksci.cn Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。 Copyright © 2023 布克学术 All rights reserved.
京ICP备2023020795号-1
ghs 京公网安备 11010802042870号
Book学术文献互助
Book学术文献互助群
群 号:604180095
Book学术官方微信