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Black carbon traces of human activities in stalagmites from Turkey

机译:来自土耳其石笋的人类活动的黑碳痕迹

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Speleothems are recognized as sensitive recorders of climatic fluctuations in the past and provide precisely dated and highly resolved environmental records. However, their potential as an archaeological archive is not fully acknowledged yet. Here we present several stalagmites containing soot and charcoal layers from various caves in Turkey and provide evidence that these black carbon layers are directly related to human activity. The archaeological artefacts found in Tabak and Kocain caves in SW Turkey support the linkage between soot and charcoal layers existence and human activity in the caves. For this study, we focus on stalagmites from Tabak and Kocain cave. To explore the age and nature of the soot and charcoal layers within stalagmites Ta-9, Ta-10 and Ko-1, Uranium series dating, scanning electron microscope (SEM) and thin section analyses were performed. The episodic soot and charcoal deposition in stalagmites Ta-9 and Ta-10 occurred between 7424 +/- 225 yr BP and 6670 +/- 218 yr BP while the soot and charcoal layers in stalagmite Ko-1 formed between 2830 +/- 189 yr BP and 470 +/- 56 yr BP. In combination with the archaeological inventory in Tabak Cave, the soot and charcoal layers within stalagmites Ta-9 and Ta-10 show that the cave was used repeatedly as a burial site during Chalcolithic period. In Kocain Cave was also used repeatedly between the Iron Age and Medieval Period, most likely for ritual activities and for providing animals with water from a small spring in the entrance to the cave. The soot and charcoal layers within stalagmites from Turkey prove that speleothems are also important as archaeological archives.
机译:洞穴被认为是过去气候波动的敏感记录者,提供精确的年代和高分辨率的环境记录。然而,它们作为考古档案的潜力尚未得到充分承认。在这里,我们展示了几个石笋,其中含有来自土耳其不同洞穴的煤烟和木炭层,并提供证据证明这些黑碳层与人类活动直接相关。在土耳其西南部的塔巴克和科凯恩洞穴中发现的考古文物支持了洞穴中烟尘和木炭层的存在与人类活动之间的联系。在这项研究中,我们重点研究了塔巴克和科坎洞穴中的石笋。为了探索石笋Ta-9、Ta-10和Ko-1中煤烟层和炭层的年龄和性质,进行了铀系定年、扫描电子显微镜(SEM)和薄片分析。石笋Ta-9和Ta-10中的烟灰和木炭沉积发生在7424+/-225年BP和6670+/-218年BP之间,而石笋Ko-1中的烟灰和木炭层形成于2830+/-189年BP和470+/-56年BP之间。结合塔巴克洞穴的考古调查,石笋Ta-9和Ta-10中的煤烟层和木炭层表明,该洞穴在点石岩时期被反复用作墓地。在铁器时代和中世纪之间,科凯恩洞穴也被反复使用,最有可能用于仪式活动,以及从洞穴入口处的一个小泉水向动物提供水。土耳其石笋中的煤烟和木炭层证明,石笋作为考古档案也很重要。

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