南黎凡特的青铜时代中期(距今4200-4000年前)——为什么外约旦的四个城市在城市崩溃中幸存下来?

IF 0.6 Q4 GEOSCIENCES, MULTIDISCIPLINARY
Michal Bieniada
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引用次数: 4

摘要

黎凡特南部的第一个城市文化崩溃,迦南的第一个城市化时期(早期青铜时代I-III)在大约公元前4200年结束。迦南人放弃了他们有城墙的城市,分散开来,开始了游牧生活。然而,南迦南的城市中心并没有被摧毁。这一事实可能指向环境因素的责任,并使人为因素的影响不确定,以及最流行的亚摩利人入侵/破坏假说。当时许多地区发生了巨大的气候变化,影响了古代近东的文化和文明,导致了城市的放弃、移民和巨大的文明变革。在黎凡特南部,几乎所有的城市都成了废墟,但外约旦有一个神秘的例外,那里有四个城市:阿罗埃、阿德、克伯特·伊斯坎德尔和伊克塔努幸存下来,并在整个时期存在。最有可能的是,当西约旦的气候条件排除了城市生活的可能性时,外约旦的气候条件保持不变或在非常有限的范围内发生变化。现在可以清楚地看到,在经历了一段相当湿润和温暖的气候后,4200年后东地中海沿岸地区的降水大幅减少。外约旦的一部分,可能是由于死海的存在,以某种方式创造了影响降水的条件,保持了一个气候利基,雨量充足,使人口能够集中在大城市中心及其周围,城市文明得以延续。沿海地区的变暖改变了露点温度,阻止了犹太山和撒玛利亚山西坡上云层的形成。潮湿的空气被阻止凝结向东输送,在那里它可以到达死海上空出现的上升气流。带着水汽向上移动的空气团可以在外约旦形成雨云。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Intermediate Bronze Age in Southern Levant (4200–4000 BP) – Why Did Four Cities in Transjordan Survive Urban Collapse?
Abstract The first urban culture of southern Levant collapsed and the first period of urbanisation of Canaan (Early Bronze Age I-III) terminated at around 4200 yrs BP. The Canaanites abandoned their walled cities, dispersed and underwent pastoralisation. However, the urban centres of southern Canaan were not destroyed. This fact may point to responsibility of the environmental factor and makes influence influence of anthropogenic factors uncertain, along with the most popular Amorite invasion/destruction hypothesis. A tremendous climatic change occurred at that time in many regions, affecting cultures and civilisations of the Ancient Near East and resulting in abandonment of cities, migrations and great civilizational changes. In southern Levant, virtually all cities were left in ruins with a mysterious exception in Transjordan where four cities: Aroer, Ader, Khirbet Iskander and Iktanu survived and existed throughout the period. Most probably when climatic conditions in Cisjordan excluded possibility of urban life, the ones in Transjordan conditions remained unchanged or altered in a very limited scale. It is now clear that after a period with quite humid and warm climate, the precipitation greatly diminished after 4200 yrs BP in a littoral zone of eastern Mediterranean. A part of Transjordan, probably due to presence of the Dead Sea that somehow created conditions that influenced precipitation, remained a climatic niche with decent rainfall that enabled concentration of population in and around big urban centres and continuation of urban civilisation. Warming in a littoral zone changed dew point temperature preventing formations of clouds above western slopes of Judean and Samarian Hills. Moist air, prevented from condensation was transported eastwards where it could reach ascending currents appearing over the Dead Sea. Masses of air with water vapour moving upwards could form rainy clouds in Transjordan.
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来源期刊
Studia Quaternaria
Studia Quaternaria GEOSCIENCES, MULTIDISCIPLINARY-
CiteScore
1.40
自引率
0.00%
发文量
0
期刊介绍: Studia Quaternaria is designed to publish scientific works concerning the Quaternary, on local, regional and global scale. Studia Quaternaria is interested in all fields of research dealing with stratigraphy and reconstruction of the past environments, including palaeogeography, palaeoecology, palaeoclimatology, palaeohydrology etc. The journal is also open to studies of natural environmental processes, and to recognition of mechanisms involved in the dynamics of our environment. The clue is that the Quaternary is still ongoing and vivid, and understanding of its past and present development support each other.
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