

FOLLOWUS
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
XU Xiaoming, xxm8302@126.com
WANG Jianghai, wangjhai@mail.sysu.edu.cn
收稿:2016-08-11,
录用:2016-9-22,
网络首发:2016-11-10,
纸质出版:2018-01
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祝青, 林佳, 洪跃辉, 等. Centennial-scale records of total organic carbon in sediment cores from the South Yellow Sea, China[J]. 海洋湖沼学报(英文), 2018,36(1):128-138.
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.
祝青, 林佳, 洪跃辉, 等. Centennial-scale records of total organic carbon in sediment cores from the South Yellow Sea, China[J]. 海洋湖沼学报(英文), 2018,36(1):128-138. DOI: 10.1007/s00343-017-6215-1.
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.
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.
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