Preliminary study on 14C chronology of lop-Nur lacustrine sediments
ID:1235 View Protection:PRIVATE Updated Time:2023-04-09 22:17:07 Hits:1089 Poster Presentation

Start Time:2023-05-06 08:00(Asia/Shanghai)

Duration:0min

Session:SP 张贴报告专场 » SP-1-11、第四纪地质与全球变化

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Abstract
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.
Keywords
radiocarbon,Lacustrine sediments,reservoir effects,organic matter
Speaker
炊郁达
中国科学院地球环境研究所

Submission Author
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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Important Date
  • Conference Date

    May 05

    2023

    to

    May 08

    2023

  • Mar 31 2023

    Draft paper submission deadline

  • May 25 2023

    Registration deadline

Sponsored By
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
Organized By
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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