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首页> 外文期刊>The holocene >Event reconstruction through Bayesian chronology: Massive mid-Holocene lake- burst triggered large-scale ecological and cultural change
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Event reconstruction through Bayesian chronology: Massive mid-Holocene lake- burst triggered large-scale ecological and cultural change

机译:通过贝叶斯年表重建事件:大规模全新世湖性爆发-引发了大规模的生态和文化变革

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摘要

Precise timing of natural and cultural events provides a foundation for understanding how past natural phenomena have driven changes in population and culture. In this study, we used high-resolution Bayesian chronology to describe an event sequence of a massive and abrupt water level decline of a large lake and the contemporaneous cultural changes that occurred in eastern Fennoscandia during the mid-Holocene. The study provides the first transdisciplinary analysis of the causes and effects of the events by using a combination of archaeological, geological and ecological data. Nearly 6000 years ago, ancient Lake Saimaa, estimated to cover nearly 9000km~2at the time, was abruptly discharged through a new outlet. The event created thousands of square kilometres of new residual wetlands. The archaeological record shows a profound cultural replacement and a subsequent sharp human population maximum in the area during the decades after the decline in water level. During the population maximum, the proportion of Alces alces (moose) in the diet rapidly increased and became prominent as a dietary resource. The eventual population decline in the area coincided with ecological development towards old boreal conifer forests, along with the colonization of a new species of tree Picea abies (Norway spruce). The new ecosystem was less suitable for moose to forage in, and this attenuated the dietary role of moose and thus contributed towards the eventual population and cultural decline. The methodological approach described in this paper allowed the reconstruction of past natural and cultural events and demonstrated how they can be causally intertwined.
机译:自然和文化事件的准确时间安排为了解过去的自然现象如何驱动人口和文化变化提供了基础。在这项研究中,我们使用高分辨率的贝叶斯年表描述了一个大湖突然大量水位下降以及整个全新世中期芬诺斯坎迪亚东部发生的同时文化变化的事件序列。该研究通过结合考古,地质和生态学数据,对事件的起因和后果进行了首次跨学科分析。将近6000年前,当时估计覆盖近9000 km〜2的古老塞马湖通过一个新的出口突然排放。这次活动创造了数千平方公里的新残留湿地。考古记录表明,在水位下降后的几十年中,该地区发生了深刻的文化变迁,随后人口急剧增加。在最大的种群数量中,Alces alces(驼鹿)在饮食中的比例迅速增加,并成为饮食资源中的重要部分。该地区人口的最终减少与对古老的针叶林的生态发展以及新的云杉云杉树的定殖相吻合(挪威云杉)。新的生态系统不太适合麋鹿觅食,这削弱了麋鹿的饮食作用,从而导致了人口和文化的最终衰落。本文描述的方法论方法允许重建过去的自然和文化事件,并展示了它们如何因果相互联系。

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