Rick J. Schulting , Pavel E. Tarasov , Andrzej W. Weber
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引用次数: 0
Abstract
In this contribution we provide an overview of the potential impacts of the 8.2 ka BP cooling event on hunter-gatherer societies in northwestern Europe and northern/eastern Eurasia. There seems to be a division between the two parts of the continent, with Atlantic Europe generally seeing a stronger climatic and environmental impact compared to continental Eurasia. This plausibly relates to the greater effects on oceanic weather patterns, particularly those of the North Atlantic. The palaeoenvironmental record is more limited for the Pacific coast of northeast Asia, but the evidence to date does not suggest as strong an impact there. We then focus on a case study of the hunter-gatherers of Cis-Baikal in southern Siberia. While the archaeological record for the period pre-8200 cal BP is patchy, we find no clear evidence for any impact on the region’s hunter-gatherer communities. Major visible changes occur only with the appearance of the Kitoi culture from ca. 7600 cal BP, which sees the introduction of pottery, the bow and arrow, and large cemeteries. This appears to be an internal sociotechnological development unrelated to any abrupt changes in the regional climate and environment at this time.
在这篇文章中,我们概述了8.2 ka BP的冷却事件对欧洲西北部和欧亚大陆北部/东部狩猎采集社会的潜在影响。欧洲大陆的两个部分之间似乎存在分歧,与欧亚大陆相比,大西洋欧洲通常受到更大的气候和环境影响。这似乎与对海洋气候模式,特别是北大西洋气候模式的更大影响有关。东北亚太平洋沿岸的古环境记录更为有限,但迄今为止的证据并没有表明那里受到了如此强烈的影响。然后,我们将重点放在西伯利亚南部顺贝加尔湖的狩猎采集者的案例研究上。尽管公元前8200 cal BP之前的考古记录并不完整,但我们没有发现明确的证据表明该地区的狩猎采集社区受到了任何影响。主要可见的变化只发生在大约公元前7600年 cal BP的基托伊文化出现之后,陶器、弓箭和大型墓地开始出现。这似乎是一种内部的社会技术发展,与当时区域气候和环境的任何突然变化无关。