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The physical environment in Northern Greece at the advent of the Neolithic

机译:新石器时代到来希腊北部的自然环境

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The transition from the Late Pleistocene to the Early Holocene in the Eastern Mediterranean is marked by an abrupt change in sea levels, landforms, ecology and resources. These new geomorphological conditions favored the formation of attractive environmental settings for the early farmers, having at the same time a significant taphonomic impact on the archaeological record of the Late Pleistocene. During the Early Holocene, on the other hand, the abrupt climatic 8.2 ka event has been recorded as a period of hyperaridity in Anatolia and the Levant, associated with pronounced cultural discontinuities. At the same time, increasing humidity and cooling is documented in central Europe, while seasonality and variability characterizes the intermediate zones, whose magnitude and spatial expression are not yet fully understood. This article reviews the geomorphological configuration and palaeoclimatic records of the Late Pleistocene-Holocene transition in Northern Greece, a key location for understanding the pathways of neolithization in Europe. With its fragmentary Early Neolithic record, Northern Greece demonstrates significant geomorphological modifications during the Pleistocene-Holocene transition, while being part of the transitional climatic zone in the 8.2 ka event. The landscape configuration is described, emphasizing the role of wetlands as significant locales for the onset of agriculture, while the environmental-cultural interaction in the first centuries of the neolithization is discussed, combining the paleoenvironmental, stratigraphical and chronological evidence for the first farmers and last hunter-gatherers. (C) 2016 Published by Elsevier Ltd.
机译:东地中海从晚更新世过渡到全新世早期的特征是海平面,地貌,生态和资源的突然变化。这些新的地貌条件有利于早期农民形成诱人的环境,同时对晚更新世的考古记录产生重大的后遗影响。另一方面,在全新世早期,在安纳托利亚和黎凡特记录到,突然的8.2 ka气候事件是高干旱时期,伴随着明显的文化不连续性。同时,中欧地区的湿度和降温有所增加,而季节性和多变性则是中间区域的特征,中间区域的大小和空间表达方式尚未得到充分了解。本文回顾了希腊北部晚更新世-全新世过渡的地貌构造和古气候记录,这是了解欧洲新石器时代路径的关键位置。凭借其零碎的新石器时代早期记录,希腊北部在更新世-全新世过渡期间表现出显着的地貌变化,同时也是8.2 ka事件中过渡气候带的一部分。描述了景观配置,强调了湿地作为农业兴起的重要场所的作用,同时讨论了新石器时代最初几个世纪的环境文化互动,结合了第一批农民和最后一位农民的古环境,地层学和年代学证据狩猎采集者。 (C)2016由Elsevier Ltd.出版

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