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首页> 外文期刊>Quaternary International >Filling the gap: OSL data expanding ~(14)C chronologies of Late Quaternary environmental change in the Libyan Desert
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Filling the gap: OSL data expanding ~(14)C chronologies of Late Quaternary environmental change in the Libyan Desert

机译:填补空白:OSL数据扩展了利比亚沙漠后期第四纪环境变化的〜(14)C年表

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摘要

Several decades of geomorphological and archaeological research in the Libyan Desert conducted by the Cologne projects B.O.S. and ACACIA have yielded a wealth of radiocarbon data from archaeological sites and, over the last decade, also 48 OSL ages, mainly from aeolian deposits. This paper focuses on the combination of both data sets in order to obtain a synthesis of Late Quaternary occupational and environmental history in this region. Case studies demonstrate that despite a poorer time resolution of OSL chronologies compared to ~(14)C data, OSL ages can be more consistent with the archaeological context, particularly if the dating of charcoals poses problems due to poor quality or re-deposition. Comparison of data sets from the Egyptian sand seas and from the Wadi Howar (Sudan) shows that in both cases, OSL and ~(14)C data cover complementary time slices. On the regional scale, however, contradictory intervals of aeolian accumulation are documented which can be explained by the different environmental histories. The results accentuate that interpretation of OSL data has to be done in the context of the entire environmental systems including the effective geomorphological processes.
机译:科隆B.O.S.科隆项目在利比亚沙漠进行了数十年的地貌和考古研究ACACIA和ACACIA已从考古现场获得了大量的放射性碳数据,在过去十年中,也有48个OSL年龄,主要来自风成矿。本文着重于两个数据集的组合,以便获得该地区晚第四纪的职业和环境史的综合信息。案例研究表明,尽管与〜(14)C数据相比,OSL时间顺序的时间分辨率较差,但OSL年龄可能与考古背景更加一致,尤其是在木炭的定年由于质量差或重新沉积而引起问题的情况下。对来自埃及沙海和来自瓦迪·霍瓦尔(苏丹)的数据集的比较表明,在两种情况下,OSL和〜(14)C数据都覆盖了互补的时间片。然而,在区域尺度上,风积聚的相互矛盾的时间间隔被记录下来,这可以用不同的环境历史来解释。结果强调,必须在包括有效地貌过程在内的整个环境系统的背景下进行OSL数据的解释。

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