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Organic and inorganic carbon and their stable isotopes in surface sediments of the Yellow River Estu

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Organic and inorganic carbon and their stable isotopes in surface sediments of the Yellow River Estuary
Yu, Zhitong; Wang, Xiujun; Han, Guangxuan; Liu, Xingqi; Zhang, Enlou
发表期刊SCIENTIFIC REPORTS
ISSN2045-2322
2018-07-17
卷号8页码:10825
关键词EAST CHINA SEAGRAIN-SIZEBOHAI SEACONTINENTAL-SHELFLAKE-SEDIMENTSYANGTZE-RIVERC/N RATIOSMATTERDELTATERRESTRIAL
研究领域Science & Technology - Other Topics
DOI10.1038/s41598-018-29200-4
产权排序[Yu, Zhitong; Wang, Xiujun] Beijing Normal Univ, Coll Global Change & Earth Syst Sci, Beijing 100875, Peoples R China; [Han, Guangxuan] Chinese Acad Sci, Yantai Inst Coastal Zone Res, Yantai 264003, Shandong, Peoples R China; [Liu, Xingqi] Capital Normal Univ, Coll Resource Environm & Tourism, Beijing 100048, Peoples R China; [Zhang, Enlou] Chinese Acad Sci, Nanjing Inst Geog & Limnol, State Key Lab Lake Sci & Environm, Nanjing 210008, Jiangsu, Peoples R China
作者部门海岸带环境过程实验室
英文摘要Studying the carbon dynamics of estuarine sediment is crucial to understanding of carbon cycle in the coastal ocean. This study is to evaluate the mechanisms regulating the dynamics of organic (TOC) and inorganic carbon (TIC) in surface sediment of the Yellow River Estuary (YRE). Based on data of 15 surface sediment cores, we found that TIC (6.3-20.1 g kg(-1)) was much higher than TOC (0.2-4.4 g kg(-1)). Both TOC and TIC were generally higher to the north than to the south, primarily due to the differences in kinetic energy level (i.e., higher to the south). Our analysis suggested that TOC was mainly from marine sources in the YER, except in the southern shallow bay where approximately 75% of TOC was terrigenous. The overall low levels of TOC were due to profound resuspension that could cause enhanced decomposition. On the other hand, high levels of TIC resulted partly from higher rates of biological production, and partly from decomposition of TOC associated with sediment resuspension. The isotopic signiture in TIC seems to imply that the latter is dominant in forming more TIC in the YRE, and there may be transfer of OC to IC in the water column.
文章类型Article
资助机构National Key Basic Research Program [2013CB956602]; China Postdoctoral Science Foundation [2018T110067, 2016M600059]; National Natural Science Foundation [41601107]; Fundamental Research Funds for the Central Universities [312231103]
收录类别SCI
语种英语
关键词[WOS]EAST CHINA SEA; GRAIN-SIZE; BOHAI SEA; CONTINENTAL-SHELF; LAKE-SEDIMENTS; YANGTZE-RIVER; C/N RATIOS; MATTER; DELTA; TERRESTRIAL
研究领域[WOS]Multidisciplinary Sciences
WOS记录号WOS:000438851500001
引用统计被引频次:11[WOS][WOS记录][WOS相关记录]
文献类型期刊论文
条目标识符http://ir.yic.ac.cnhttp://ir.yic.ac.cn/handle/133337/24436
专题中科院海岸带环境过程与生态修复重点实验室_海岸带环境过程实验室
中科院海岸带环境过程与生态修复重点实验室

作者单位1.Beijing Normal Univ, Coll Global Change & Earth Syst Sci, Beijing 100875, Peoples R China;
2.Chinese Acad Sci, Yantai Inst Coastal Zone Res, Yantai 264003, Shandong, Peoples R China;
3.Capital Normal Univ, Coll Resource Environm & Tourism, Beijing 100048, Peoples R China;
4.Chinese Acad Sci, Nanjing Inst Geog & Limnol, State Key Lab Lake Sci & Environm, Nanjing 210008, Jiangsu, Peoples R China

推荐引用方式
GB/T 7714Yu, Zhitong,Wang, Xiujun,Han, Guangxuan,et al. Organic and inorganic carbon and their stable isotopes in surface sediments of the Yellow River Estuary[J]. SCIENTIFIC REPORTS,2018,8:10825.
APAYu, Zhitong,Wang, Xiujun,Han, Guangxuan,Liu, Xingqi,&Zhang, Enlou.(2018).Organic and inorganic carbon and their stable isotopes in surface sediments of the Yellow River Estuary.SCIENTIFIC REPORTS,8,10825.
MLAYu, Zhitong,et al."Organic and inorganic carbon and their stable isotopes in surface sediments of the Yellow River Estuary".SCIENTIFIC REPORTS 8(2018):10825.


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