Department of Archaeology, Durham University, Durham, United Kingdom.
Department of Ancient History, Ludwig-Maximilian University of Munich, München, Germany.
PLoS One. 2021 Jan 11;16(1):e0244871. doi: 10.1371/journal.pone.0244871. eCollection 2021.
The rise and fall of ancient societies have been attributed to rapid climate change events. One of the most discussed of these is the 4.2kya event, a period of increased aridity and cooling posited as the cause of societal changes across the globe, including the collapse of the Akkadian Empire in Mesopotamia. Studies seeking to correlate social and climatic changes around the 4.2kya event have tended to focus either on highly localized analyses of specific sites or surveys or more synthetic overviews at pan-continental scales, and temporally on the event and its aftermath. Here we take an empirical approach at a large spatial scale to investigate trends in population and settlement organization across the entirety of Northern Fertile Crescent (Northern Mesopotamia and the Northern Levant) from 6,000 to 3,000 cal BP. We use Summed Probability Distributions of radiocarbon dates and data from eighteen archaeological surveys as proxies for population, and a dataset of all settlements over ten hectares in size as a proxy for the degree of urbanization. The goal is to examine the spatial and temporal impact of the 4.2kya event and to contextualize it within longer term patterns of settlement. We find that negative trends are visible during the event horizon in all three proxies. However, these occur against a long-term trend of increased population and urbanization supported through unsustainable overshoot and the exploitation of a drier zone with increased risk of crop failure. We argue that the 4.2kya event occurred during a period of unprecedented urban and rural growth which may have been unsustainable even without an exogenous climate forcing.
古代社会的兴衰归因于快速的气候变化事件。其中最受讨论的是 4.2 千年事件,一个气候干旱和冷却加剧的时期,被认为是全球范围内社会变革的原因,包括美索不达米亚的阿卡德帝国的崩溃。试图将 4.2 千年事件前后的社会和气候变化相关联的研究倾向于要么专注于特定地点的高度局部分析,要么在泛大陆范围内进行更综合的调查,要么在时间上关注事件及其后果。在这里,我们从经验主义的角度在较大的空间尺度上研究了从 6000 到 3000 年 cal BP 整个北新月沃地(北美索不达米亚和北黎凡特)的人口和定居点组织的趋势。我们使用放射性碳日期的总和概率分布和来自十八个考古调查的数据作为人口的代理,以及一个所有面积超过十公顷的定居点数据集作为城市化程度的代理。目的是检验 4.2 千年事件的空间和时间影响,并将其置于更长期的定居模式中。我们发现,在所有三个代理中,在事件视界期间都出现了负面趋势。然而,这些趋势发生在人口和城市化长期增长的趋势中,这种增长是通过不可持续的过度扩张和对干燥地区的开发以及增加作物歉收风险来支持的。我们认为,4.2 千年事件发生在一个前所未有的城市和农村增长时期,即使没有外部气候强迫,这种增长也可能是不可持续的。