The Impact of Late Pleistocene—Early Holocene Climatic Changes on Humans in Southwest Asia
The Impact of Late Pleistocene—Early Holocene Climatic Changes on Humans in Southwest Asia
复制标题
晚更新世—早全新世气候变化对西南亚人类的影响
DOI：
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发表时间：
1996
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影响因子：
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通讯作者：
O. Bar‐Yosef
中科院分区：
文献类型：
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作者：
O. Bar‐Yosef
本章的目的是为更新世末期和全新世早期气候波动对西南亚人类文化的影响提供基本证据。气候证据来自东地中海的深海核心和主要来自土耳其和伊朗西北部的陆地花粉记录，少量来自叙利亚和以色列（Fontugne et al. 1994 van Zeist and Bottema 1991）。有关古湖泊和河流阶地的地貌和化学信息可从黎凡特获得。考古信息来自这一时期在黎凡特南部（以色列和约旦）进行的最密集的考古调查，来自黎凡特北部（黎巴嫩和叙利亚）的数据较少，来自邻国的信息也很零散。因此，应该指出的是，这种地理偏见可能会损害更一般性结论的有效性。
The aim of this chapter is to provide basic evidence for the impact of climatic fluctuations on human cultures in southwest Asia during the terminal Pleistocene and early Holocene. Climatic evidence is drawn from deep sea cores in the eastern Mediterranean and terrestrial pollen records mainly from Turkey and northwest Iran, with fewer from Syria and Israel (Fontugne et al. 1994 van Zeist and Bottema 1991). Geomorphological and chemical information concerning paleolakes and river terraces is available from the Levant. Archaeological information comes from the most intensive archaeological investigations of this period conducted in the southern Levant (Israel and Jordan), with fewer data from the northern Levant (Lebanon and Syria) and fragmentary information from neighboring countries. It should therefore be noted that this geographic bias may impair the validity of the more general conclusions.