首页> 外文期刊>Zeitschrift fur Geomorphologie >Decoding short-term climatic variations from cave sediments over the Mid-Holocene: Implications for human occupation in the Katarraktes Cave System, Northern Greece
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Decoding short-term climatic variations from cave sediments over the Mid-Holocene: Implications for human occupation in the Katarraktes Cave System, Northern Greece

机译:解码来自中全新世中的洞穴沉积物的短期气候变化:北希腊北部Katarraktes洞穴系统的人类占领的影响

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摘要

In this study we resolve the paleoclimatic variability and its impact onto human history over the MidHolocene in the Katarraktes Cave System, Northern Greece. The study area is one of the most important Early Bronze Age archaeological sites of the eastern Mediterranean and comprises a cave and an associate rockshelter, lying on the south flanks of the Krousovitis River canyon. We analyze a clastic sedimentary sequence preserved at the entrance of the Katarraktes Cave by combining sedimentological, mineralogical and geochemical data with magnetic parameter measurements and age constraints. Our results reveal that warm and wet climatic conditions prevail in the area during the Mid-Holocene that were interrupted by short-term cold and dry events. We show that the fluvial response to these climatic variations had a pronounced impact onto human activities, as continuous sedimentation by floodwaters within the cave until similar to 6600 BP prohibit early settlers from using the sheltered environment. However, high incision rates (similar to 1.5 mm/yr) of the Krousovitis River favored the use of the rockshelter during the Mid- to Late Holocene. Our study demonstrates that the interplay between climate and surface processes was the key factor that controlled human occupation in this important archaeological site.
机译:在这项研究中,我们解决了希腊北部卡塔拉克特斯洞穴系统中全新世的古气候变化及其对人类历史的影响。研究区域是东地中海最重要的青铜时代早期考古遗址之一,包括一个洞穴和一个附属岩石掩体,位于Krousovitis河峡谷的南侧。我们将沉积学、矿物学和地球化学数据与磁性参数测量和年龄限制相结合,分析保存在卡塔拉克特斯洞穴入口处的碎屑沉积序列。我们的研究结果表明,在中全新世期间,该地区普遍存在温暖和潮湿的气候条件,这些气候条件被短期的寒冷和干燥事件打断。我们表明,河流对这些气候变化的响应对人类活动产生了显著影响,因为洞穴内洪水的持续沉积直到类似6600 BP,阻止早期定居者使用受保护的环境。然而,在全新世中期至晚期,Krousovitis河的高切割率(类似于1.5毫米/年)有利于使用岩石掩体。我们的研究表明,气候和地表过程之间的相互作用是控制人类占领这一重要考古遗址的关键因素。

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