Prehistoric human influence on soil dynamics and slope transformation on the Subcarpathian Loess Plateau, southeastern Poland

IF 0.9 4区 地球科学 Q3 GEOLOGY
Piotr Gębica
{"title":"Prehistoric human influence on soil dynamics and slope transformation on the Subcarpathian Loess Plateau, southeastern Poland","authors":"Piotr Gębica","doi":"10.7306/gq.1732","DOIUrl":null,"url":null,"abstract":"<p><br />This study examines the impact of prehistoric human activities on the landscape of the Subcarpathian Loess Plateau, focusing on areas such as the Kańczuga Plateau in southeastern Poland. Through a multidisciplinary approach that integrates archaeological excavation, soil profile analysis, and geomorphological survey techniques, environmental changes are traced from the Neolithic through the early Middle Ages. A key aspect comprises various soil types, particularly chernozems and brown soils, which have been influenced by early agricultural practices like deforestation and land cultivation. The use of radiocarbon and Optically Stimulated Luminescence (OSL) dating of soil profiles and archaeological sites provides insights into the timeline of human-induced erosional and depositional processes and deposits ranging in age from the Palaeolithic period to the early Middle Ages. The results highlight significant soil erosion and colluvial deposit formation, especially during periods of intensified agriculture. These changes in specific soil types underscore the substantial impact of human activities and climatic variations on land relief and soil cover in the Late Holocene. This study contributes to a deeper understanding of human-driven landscape alterations in loess areas, offering valuable insights for environmental management and conservation on the Kańczuga Plateau, in the Sandomierz Basin, and in other similar geomorphological settings.</p>","PeriodicalId":12587,"journal":{"name":"Geological Quarterly","volume":"96 1","pages":""},"PeriodicalIF":0.9000,"publicationDate":"2024-03-14","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Geological Quarterly","FirstCategoryId":"89","ListUrlMain":"https://doi.org/10.7306/gq.1732","RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q3","JCRName":"GEOLOGY","Score":null,"Total":0}
引用次数: 0

Abstract


This study examines the impact of prehistoric human activities on the landscape of the Subcarpathian Loess Plateau, focusing on areas such as the Kańczuga Plateau in southeastern Poland. Through a multidisciplinary approach that integrates archaeological excavation, soil profile analysis, and geomorphological survey techniques, environmental changes are traced from the Neolithic through the early Middle Ages. A key aspect comprises various soil types, particularly chernozems and brown soils, which have been influenced by early agricultural practices like deforestation and land cultivation. The use of radiocarbon and Optically Stimulated Luminescence (OSL) dating of soil profiles and archaeological sites provides insights into the timeline of human-induced erosional and depositional processes and deposits ranging in age from the Palaeolithic period to the early Middle Ages. The results highlight significant soil erosion and colluvial deposit formation, especially during periods of intensified agriculture. These changes in specific soil types underscore the substantial impact of human activities and climatic variations on land relief and soil cover in the Late Holocene. This study contributes to a deeper understanding of human-driven landscape alterations in loess areas, offering valuable insights for environmental management and conservation on the Kańczuga Plateau, in the Sandomierz Basin, and in other similar geomorphological settings.

史前人类对波兰东南部次喀尔巴阡山黄土高原土壤动力学和坡度变化的影响
本研究探讨了史前人类活动对次喀尔巴阡山黄土高原地貌的影响,重点是波兰东南部的卡祖加高原(Kańczuga Plateau)等地区。通过将考古发掘、土壤剖面分析和地貌勘测技术相结合的多学科方法,追溯了从新石器时代到中世纪早期的环境变化。其中一个重要方面包括各种土壤类型,尤其是受到早期农业耕作方式(如砍伐森林和土地耕种)影响的切尔诺泽姆土和褐土。通过对土壤剖面和考古遗址进行放射性碳和光致发光(OSL)测年,可以深入了解从旧石器时代到中世纪早期的人类侵蚀和沉积过程及沉积物的时间线。研究结果表明,土壤侵蚀和冲积层的形成非常明显,尤其是在强化农业时期。这些特定土壤类型的变化凸显了人类活动和气候变化对全新世晚期地表起伏和土壤覆盖的巨大影响。这项研究有助于加深对黄土地区人为地貌变化的理解,为卡姆丘加高原、桑多梅日盆地以及其他类似地貌环境的环境管理和保护提供宝贵的见解。
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
Geological Quarterly
Geological Quarterly 地学-地质学
CiteScore
2.20
自引率
0.00%
发文量
19
审稿时长
>12 weeks
期刊介绍: The policy of the Geological Quarterly is to publish significant contributions of information and geological insight relevant to an international readership. The journal has been issued since 1957 at the Polish Geological Institute - National Research Institute and, at present, is the leading Earth sciences journal in Poland. All aspects of Earth and related sciences, and universal and broad regional rather than locally oriented topics are covered. The journal is intended to be an international forum for the exchange of information and ideas, particularly on important geological topics of Central Europe.
×
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:481959085
Book学术官方微信