Preliminary study on 14C chronology of lop-Nur lacustrine sediments
编号:1235 访问权限:私有 更新:2023-04-09 22:17:07 浏览:156次 张贴报告

报告开始:2023年05月06日 08:00(Asia/Shanghai)

报告时间:0min

所在会场:[SP] 张贴报告专场 [SP-1-1] 1、第四纪地质与全球变化

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摘要
Radiocarbon is the most common method used for dating sediment chronology, especially for lacustrine sediment. However, the ubiquitous Radiocarbon Reservoir Effect hinders the accuracy of lacustrine sediment chronology. Although massive research have studied the Radiocarbon Reservoir Effect in temporal and spatial, fewer studies focus on the Radiocarbon Reservoir Effect and the depositional process. Here we gave particular attention on the Lop Nur, which is the largest playas Located in Central Asia. And the climatic evolutionary process of Lop Nur is tightly bounded up with the Asian inland drying evolution and human activities along the ancient Silk Road. Previous studies have given an ambiguous chronology and large lake reservoir age from different drill due to the complex sediment process. Here, a 1.3m long pits at the top of the Big Ear area was sampled to conduct sedimentological and high-precision chronology studies. We found that grain size changes in Lop Nur sediment correlated with the fluctuation of the radiocarbon age. Taking the apparent sedimentary phase transition at 58cm as the boundary, the coarser particles contain less TOC, and have younger age. Our results suggest that the Radiocarbon reservoir effect of Lop Nur, as the convergence center of rivers in Tarim Basin, is mainly affected by exogenous organic carbon input. In the wetting stage, lacustrine clay adsorbed more old organic matter from the erosion area in upstream of the river. On the contrary, the organic matter carried by aeolian sand in the drought period is limited, resulting in 14C age anomalies.
关键词
radiocarbon,Lacustrine sediments,reservoir effects,organic matter
报告人
炊郁达
中国科学院地球环境研究所

稿件作者
炊郁达 中国科学院地球环境研究所
周卫健 中国科学院地球环境研究所
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重要日期
  • 会议日期

    05月05日

    2023

    05月08日

    2023

  • 03月31日 2023

    初稿截稿日期

  • 05月25日 2023

    注册截止日期

主办单位
青年地学论坛理事会
中国科学院青年创新促进会地学分会
承办单位
武汉大学
中国科学院精密测量科学与技术创新研究院
中国地质大学(武汉)
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