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首页> 外文期刊>The holocene >Sea level changes and Neolithic hunter-fisher-gatherers in the centre of Tallinn, southern coast of the Gulf of Finland, Baltic Sea
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Sea level changes and Neolithic hunter-fisher-gatherers in the centre of Tallinn, southern coast of the Gulf of Finland, Baltic Sea

机译:塔林中心海平面变化和新石器时代的猎人-捕捞者-波罗的海,芬兰湾南部海岸

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摘要

Relative sea level (RSL) changes and the palaeogeography of a Neolithic hunter-fisher-gatherer settlement site on the former shore of the Gulf of Finland in the city centre of Tallinn were reconstructed by implementing GIS in landscape modelling based on archaeological, sedimentary and shore displacement data. AMS radiocarbon dating of mammal bones from the cultural layer suggests the existence of the hunter-fisher-gatherer settlement around 5.1-4.8 cal. ka BP on a seaward inclining sandy beach of Tallinn palaeo-bay c. 100 m from the Litorina Sea shoreline and at about 2.4 m above the coeval sea level. The shoreline passed the study site at about 5.8 cal. ka BP and retreated towards northeast with an average speed of 13 m per century, while the RSL lowered by c. 2.5 mm annually. Combining radiocarbon dates of terrestrial and marine mammal bones from the Neolithic cultural layer, a marine reservoir effect of 350 C-14 years for the brackish-water Baltic Sea was calculated. By using high-resolution archaeological data in combination with RSL and other geological proxies, we demonstrate new possibilities to reconstruct the palaeoenvironment of deeply buried coastal settlement sites and to predict a possible continuation of the cultural layer in heavily built-up areas.
机译:通过在基于考古,沉积和海岸的景观建模中实施GIS,重构了相对海平面(RSL)的变化以及塔林市中心芬兰湾前岸新石器时代的猎人-渔民-聚居者定居点的古地理位移数据。从文化层对哺乳动物骨骼进行的AMS放射性碳测年表明,猎人-渔民-采集者聚居区的存在范围约为5.1-4.8 cal。 ka BP在塔林古湾的向海倾斜沙滩上c。距利托里纳海海岸线100 m,且距中世纪海平面约2.4 m。海岸线在大约5.8卡处通过了研究地点。 ka BP并以每世纪平均13 m的速度向东北退缩,而RSL降低了c。每年2.5毫米。结合新石器时代文化层的陆生和海洋哺乳动物骨骼的放射性碳年代,计算了咸水波罗的海的350 C-14年海洋储层效应。通过将高分辨率考古数据与RSL和其他地质指标结合使用,我们证明了重建深埋沿海定居点古环境的新可能性,并预测了人口稠密地区文化层的可能延续。

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