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Late Holocene human-environmental interactions in the Eastern Mediterranean: Settlement history and paleogeography of an ancient Aegean hill-top settlement

机译:东地中海晚全新世人类与环境的相互作用:古代爱琴海山顶定居点的定居历史和古地理

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Interactions between settlement history and landscape evolution of a hill-top settlement on the West Anatolian Coast near ancient Pergamon (modern Bergama) were studied by a combination of archaeological and geographical investigations. Ceramics, ancient literary and epigraphic texts, numismatics and architectural remains show that the hill-top had been populated since late Bronze Age times. From the sixth century BC until the change of the eras, the hill was occupied by a Greek polis - Atarneus - and was abandoned afterwards. It was newly populated in the second half of the twelfth and the first half of the thirteenth century AD. The lithostratigraphy of nine drilling cores, arranged in three transects and dated by AMS radiocarbon dating, shows that during the past 4000 years the sedimentary plains surrounding the settlement hill were aggraded by braided and meandering rivers, while colluviation and alluvial fan deposition occurred at the foot-slopes. Sedimentation totaled about 5-7 m in the past 4000 years, evidencing a "drowning" of the landscape in terrestrial sediments. Although channels shifted repeatedly and alluvial fan deposition fluctuated, the depositional system did not change in general during the past 4000 years. This striking resistance to the changing settlement and land use intensity is an effect of the distinct modification of the slopes through terracing that countervailed erosion and likewise increased the buffering capacity of the sediment storages on the slopes. There is no evidence that landscape deterioration contributed to the abandonment of the settlement hill. Rather, socio-economic factors were crucial for the rise and fall of the settlements occupying the hill.
机译:通过考古和地理调查相结合的研究,研究了古代佩加蒙附近的西安纳托利亚海岸山顶居住区的居住历史和景观演变之间的相互作用。陶瓷,古代文学和史学文献,钱币学和建筑遗迹表明,这座山顶自青铜时代晚期以来就已人口稠密。从公元前六世纪到时代的变化,这座山被希腊大都会阿塔纽斯(Atarneus)占据,之后被废弃。它是在公元十二世纪下半叶和十三世纪上半叶新填充的。九个钻孔岩心的岩石地层学,分布在三个样带中,并用AMS放射性碳测年法测年,表明在过去的4000年中,定居山周围的沉积平原被辫状和曲折的河流侵蚀,而脚下发生了塌陷和冲积扇沉积。 -连续下坡。在过去的4000年中,沉积物总计约5-7 m,表明陆地沉积物的景观被“淹没了”。尽管通道反复移动且冲积扇沉积物波动,但在过去的4000年中沉积物系统总体上没有变化。这种对不断变化的定居和土地利用强度的强烈抵抗力是通过梯田对坡度进行独特改造的结果,该梯田可抵消侵蚀,并同样增加了坡面沉积物库的缓冲能力。没有证据表明景观恶化导致了居民点山的放弃。相反,社会经济因素对于占领该山丘的定居点的兴衰至关重要。

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  • 来源
    《Quaternary International》 |2014年第4期|84-98|共15页
  • 作者单位

    Department of Earth Sciences, Physical Geography, Freie Universitaet Berlin, Malteserstrasse 74-100, 12249 Berlin, Germany;

    Marie Curie - M4Human Fellow, Via Basilio Bricci 39, 00152 Roma, Italy;

    Department of Earth Sciences, Physical Geography, Freie Universitaet Berlin, Malteserstrasse 74-100, 12249 Berlin, Germany;

    Department of Earth Sciences, Physical Geography, Freie Universitaet Berlin, Malteserstrasse 74-100, 12249 Berlin, Germany;

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