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The palaeodemographic and environmental dynamics of prehistoric Arctic Norway: An overview of human-climate covariation

机译:史前北极挪威的古代分析和环境动态:人类气候协变的概述

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This paper presents the first palaeodemographic results of a newly assembled region-wide radiocarbon record of the Arctic regions of northern Norway. The dataset contains a comprehensive collection of radiocarbon dates in the area (N = 1205) and spans the 10,000-year period of hunter-gatherer settlement history from 11500 to 1500 cal BP. Utilizing local, high-resolution palaeoclimate data, the paper performs multi-proxy correlation testing of climate and demographic dynamics, looking for hunter-gatherer responses to climate variability. The paper compares both long-term climate trends and short-term disruptive climate events with the demographic development in the region. The results demonstrate marked demographic fluctuations throughout the period, characterized by a general increase, punctuated by three significant boom and bust-cycles centred on 6000, 3800 and 2200 cal BP, interpreted as instances of climate forcing of human demographic responses. The results strongly suggest the North Cape Current as a primary driver in the local environment and supports the patterns of covariance between coastal climate proxies and the palaeodemographic model. A mechanism of climate forcing mediation through marine trophic webs is proposed as a tentative explanation of the observed demographic fluxes, and a comparison with inter-regional results demonstrate remarkable similarity in demographic trends across mid-Holocene north and west Europe. The results of the north Norwegian radiocarbon record are thus consistent with independent, international efforts, corroborating the existing pan-European results and help further substantiate super-regional climate variability as the primary driver of population dynamics regardless of economic adaptation.
机译:本文介绍了北挪威北极地区的新组装区域宽的宽弧度记录的第一个古代分析结果。 DataSet包含了该地区(N = 1205)的全面RadioCarbon日期的集合,并跨越了11500至1500年的猎人收集历史的10,000年期间。本文利用本地高分辨率古怪的数据,对气候和人口动态进行多功能相关测试,寻找亨特收集器对气候变异性的反应。该论文比较了长期气候趋势和短期破坏性气候事件与该地区的人口发展。结果展示了整个时期的标志性的人口波动,其特征在于一般增加,以6000,3800和2200年CAL BP为中心的三个显着的繁荣和胸围,被解释为人口统计反应的气候迫使情况。结果强烈建议北角当前作为当地环境中的主要驱动程序,并支持沿海气候代理与古地区分析模式之间的协方差模式。建议通过海洋营养网的气候迫使调解机制作为观察到的人口助势的初步解释,与区域间结果的比较表现出在中东北部和西欧中期中期的人口趋势中表现出显着的相似性。因此,北部挪威无线电碳记录的结果与独立的国际努力一致,证实了现有的泛欧洲成果,并帮助进一步证实超级区域气候变异作为人口动态的主要驱动因素,无论经济适应如何。

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