Analiza holoceńskich zmian środowiskowych w rynnie glacjalnej pomiędzy jeziorem Gopło a Jeziorem Szarlejskim i ich wpływ na osadnictwo w okresie od neolitu do nowożytności na podstawie badań osadów jeziornych oraz danych archeologicznych i historycznych

A. Słowiński, Mateusz Robaczewski, Milena Zięba
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Abstract

The aim of the study is to analyze environmental changes in the area between Gopło and Szarlejskie Lakes. The Noteć River flows through this area, connecting both lakes. The lakes could have been connected and functioned as Wielkie Gopło. Geological reconnaissance was based on five boreholes drilled with a soil auger. The samples were subjected to granulometric analyses and the content of organic matter and calcium carbonate was determined. Eight samples were radiocarbon-dated using the AMS method. Recognition of the valley bottom settlement was done through spatial analysis using six Archaeological Project Records sheets. The results of the research allowed separating three phases of the area development: lake, bog and lake again. The beginning of the last lake development phase and its evolution have not been precisely dated and require research. Archaeological data demonstrate the poor settlement use of the glacial trough. Throughout the prehistoric period, settlement was concentrated at an altitude of 80–85 m above sea level, in the edge zone of trough. This means that the area was marshy and inaccessible for settlement. Drainage, regulation works in the Noteć river basin and industrial activities, led to the lowering of the groundwater level and weakened the lake’s recharge. Consequently, the lake disappeared from the studied area.
该研究的目的是分析Gopło和Szarlejskie湖之间地区的环境变化。诺特克河流经这一地区,连接两个湖泊。这两个湖可能连在一起,就像威基一样Gopło。地质勘测是基于用土壤螺旋钻钻的五个钻孔。对样品进行粒度分析,测定了有机质和碳酸钙的含量。用AMS法对8个样品进行放射性碳定年。通过使用六份考古项目记录表进行空间分析,对谷底沉降进行了识别。研究结果将该地区的发展分为三个阶段:湖泊、沼泽和再次湖泊。最后一个湖泊发育阶段的开始及其演变没有精确的日期,需要研究。考古资料表明,对冰槽的利用很差。在整个史前时期,聚落主要集中在海拔80 ~ 85 m的海槽边缘地带。这意味着该地区是沼泽,无法定居。诺特奇河流域的排水、治理工程和工业活动导致地下水位下降,削弱了湖泊的补给。因此,该湖从研究区域消失了。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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