Centennial-scale records of total organic carbon in sediment cores from the South Yellow Sea, China

Qing ZHU; Jia LIN; Yuehui HONG; Lirong YUAN; Jinzhong LIU; Xiaoming XU; Jianghai WANG

doi:10.1007/s00343-017-6215-1

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Centennial-scale records of total organic carbon in sediment cores from the South Yellow Sea, China

Updated：2023-04-13

- Centennial-scale records of total organic carbon in sediment cores from the South Yellow Sea, China
- Chinese Journal of Oceanology and Limnology Vol. 36, Issue 1, Pages: 128-138(2018)
- Affiliations：
  
  1.Guangdong Provincial Key Laboratory of Marine Resources and Coastal Engineering/South China Sea Bioresource Exploitation and Utilization Collaborative Innovation Center, School of Marine Sciences, Sun Yat-Sen University, Guangzhou 510006, China
  2.Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China
- Author bio：
  
  XU Xiaoming, xxm8302@126.com
  WANG Jianghai, wangjhai@mail.sysu.edu.cn
- Funds：
- DOI：10.1007/s00343-017-6215-1
  CLC：
- Received：11 August 2016，
  
  Accepted：22 September 2016，
  
  Online First：10 November 2016，
  
  Published：2018-01
- Accepted：
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Qing ZHU, Jia LIN, Yuehui HONG, et al. Centennial-scale records of total organic carbon in sediment cores from the South Yellow Sea, China[J]. Chinese Journal of Oceanology and Limnology, 2018, 36(1): 128-138.
DOI：

Qing ZHU, Jia LIN, Yuehui HONG, et al. Centennial-scale records of total organic carbon in sediment cores from the South Yellow Sea, China[J]. Chinese Journal of Oceanology and Limnology, 2018, 36(1): 128-138. DOI： 10.1007/s00343-017-6215-1.

摘要

Abstract

Global carbon cycling is a significant factor that controls climate change. The centennial-scale variations in total organic carbon (TOC) contents and its sources in marginal sea sediments may reflect the influence of human activities on global climate change. In this study

two fine-grained sediment cores from the Yellow Sea Cold Water Mass of the South Yellow Sea were used to systematically determine TOC contents and stable carbon isotope ratios. These results were combined with previous data of black carbon and

210

Pb dating from which we reconstructed the centennial-scale initial sequences of TOC

terrigenous TOC (TOC

ter

) and marine autogenous TOC (TOC

mar

) after selecting suitable models to correct the measured TOC (TOC

cor

). These sequences showed that the TOC

ter

decreased with time in the both cores while the TOC

mar

increased

particularly the rapid growth in core H43 since the late 1960s. According to the correlation between the Huanghe (Yellow) River discharge and the TOC

cor

TOC

ter

or TOC

mar

we found that the TOC

ter

in the two cores mainly derived from the Huanghe River and was transported by it

and that higher Huanghe River discharge could strengthen the decomposition of TOC

mar

. The newly obtained initial TOC sequences provide important insights into the interaction between human activities and natural processes.

关键词

Keywords

references

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