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东海内陆架岩心中木质素的沉积记录
引用本文:刘晓杰,季银利,向荣,张大海,李先国.东海内陆架岩心中木质素的沉积记录[J].沉积学报,2022,40(2):525-533.
作者姓名:刘晓杰  季银利  向荣  张大海  李先国
作者单位:1.中国海洋大学, 海洋化学理论与工程技术教育部重点实验室, 山东 青岛 266100
基金项目:国家自然科学基金(41276067,41476040,41020164005);;国家重点基础研究发展计划(973计划)(2010CB428901)~~;
摘    要:通过对东海内陆架T06岩心样品中木质素的测定,依据木质素参数对古环境、古气候的指示作用,探究了陆源有机碳在该区域的沉积记录,以及8.8 ka B.P.以来浙闽沿岸在不同历史环境下有机物的输送机制.研究结果显示,东海内陆架海域东亚冬季风驱动的水动力输送对沉积物中木质素酚类单体的含量变化及其相关参数起着至关重要的调控作用;...

关 键 词:陆源有机物  木质素  沉积记录  全新世  东海内陆架
收稿时间:2020-03-19

Sedimentary Lignin Records in a Core from the East China Sea Inner Shelf
LIU XiaoJie,JI YinLi,XIANG Rong,ZHANG DaHai,LI XianGuo.Sedimentary Lignin Records in a Core from the East China Sea Inner Shelf[J].Acta Sedimentologica Sinica,2022,40(2):525-533.
Authors:LIU XiaoJie  JI YinLi  XIANG Rong  ZHANG DaHai  LI XianGuo
Institution:1.Key Laboratory of Marine Chemistry Theory and Technology (Ocean University of China), Ministry of Education, Qingdao, Shandong 266100, China2.CAS Key Laboratory of Ocean and Marginal Sea Geology, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, China
Abstract:The sedimentary record of organic carbon from the East China Sea inner shelf was explored by determining the lignin in core T06. The transport mechanism of organic matter in different historical environments along the Zhejiang?Fujian coast was also investigated for the period since 8.8 ka B.P. by the indicator function of lignin on the paleoenvironment and paleoclimate. The results revealed that hydrodynamic transport driven by the East Asian winter monsoon in the East China Sea inner shelf played an important role in the variation of the content and its related parameters of lignin phenols in the sediments. Vise verse, the lignin content and its related parameters in the mud areas along the Zhejiang?Fujian coast indicate the influence of variation in the East Asian winter monsoon in the study area to some extent. Therefore, these are reliable indicators for reconstructing East Asian winter monsoonal climate change. The current study also revealed a “50 years” period during which dramatic data fluctuations were observed. The period might have been due to climate change and continuous flooding in the Yangtze River Basin. This led to the transport of a large amount of non-woody angiosperm residue and surface soil to the study area, which were finally deposited and buried in the sediment core, via hydrodynamic transport and ocean currents.
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