The AD 536/540 climate event in Sweden – a review

IF 2.4 3区 地球科学 Q2 GEOGRAPHY, PHYSICAL
Boreas Pub Date : 2024-08-05 DOI:10.1111/bor.12672
Eirini Anagnostou, Johan Linderholm, Kerstin Lidén
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引用次数: 0

Abstract

The middle of the first millennium AD in Sweden witnessed significant changes in the archaeological record, prompting various discussions about the underlying causes. This paper reviews the research developments surrounding the global climate cooling, which was caused by severe volcanic eruptions in AD 536/540 and is referred to as the Late Antique Little Ice Age or Fimbulwinter, and its potential impacts, with a specific focus on Swedish Iron Age societies, drawing upon published climatic and archaeological data. Furthermore, it discusses the research gaps that impede a comprehensive understanding of the potential relationship between the AD 536/540 event and socioeconomic changes in Iron Age Sweden. Additionally, it suggests that isotopic analysis will offer additional insights and help bridge the research gap.

公元536/540年瑞典气候事件回顾
公元第一个千年中期,瑞典的考古记录发生了重大变化,引发了关于其根本原因的各种讨论。本文回顾了围绕全球气候变冷的研究进展,这是由公元536/540年的严重火山爆发引起的,被称为晚期古小冰河期或芬布尔冬季,以及它的潜在影响,特别关注瑞典铁器时代的社会,利用已发表的气候和考古数据。此外,它还讨论了阻碍全面理解公元536/540年事件与铁器时代瑞典社会经济变化之间潜在关系的研究差距。此外,它还表明,同位素分析将提供额外的见解,并有助于弥合研究差距。
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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来源期刊
Boreas
Boreas 地学-地球科学综合
CiteScore
5.90
自引率
4.50%
发文量
36
审稿时长
>12 weeks
期刊介绍: Boreas has been published since 1972. Articles of wide international interest from all branches of Quaternary research are published. Biological as well as non-biological aspects of the Quaternary environment, in both glaciated and non-glaciated areas, are dealt with: Climate, shore displacement, glacial features, landforms, sediments, organisms and their habitat, and stratigraphical and chronological relationships. Anticipated international interest, at least within a continent or a considerable part of it, is a main criterion for the acceptance of papers. Besides articles, short items like discussion contributions and book reviews are published.
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