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Rates and fluxes of centennial-scale carbon storage in the fine-grained sediments from the central South Yellow Sea and Min-Zhe belt, East China Sea
Wang Jianghai1; Xiao Xi1; Zhou Qianzhi1; Xu Xiaoming1; Zhang Chenxi1; Liu Jinzhong2; Yuan Dongliang3,4
2018
发表期刊JOURNAL OF OCEANOLOGY AND LIMNOLOGY
ISSN2096-5508
卷号36期号:1页码:139-152
通讯作者Wang Jianghai(wangjhai@mail.sysu.edu.cn) ; Yuan Dongliang(dyuan@qdio.ac.cn)
摘要The global carbon cycle has played a key role in mitigating global warming and climate change. Long-term natural and anthropogenic processes influence the composition, sources, burial rates, and fluxes of carbon in sediments on the continental shelf of China. In this study, the rates, fluxes, and amounts of carbon storage at the centennial scale were estimated and demonstrated using the case study of three fine-grained sediment cores from the central South Yellow Sea area (SYSA) and Min-Zhe belt (MZB), East China Sea. Based on the high-resolution temporal sequences of total carbon (TC) and total organic carbon (TOC) contents, we reconstructed the annual variations of historical marine carbon storage, and explored the influence of terrestrial and marine sources on carbon burial at the centennial scale. The estimated TC storage over 100 years was 1.18x10(8) t in the SYSA and 1.45x10(9) t in the MZB. The corrected TOC storage fluxes at the centennial scale ranged from 17 to 28 t/(km(2)center dot a)in the SYSA and from 56 to 148 t/(km(2)center dot a) in the MZB. The decrease of terrestrial materials and the increase of marine primary production suggest that the TOC buried in the sediments in the SYSA and MZB was mainly derived from the marine autogenetic source. In the MZB, two depletion events occurred in TC and TOC storage from 1985 to 1987 and 2003 to 2006, which were coeval with the water impoundment in the Gezhouba and Three Gorges dams, respectively. The high-resolution records of the carbon storage rates and fluxes in the SYSA and MZB reflect the synchronous responses to human activities and provide an important reference for assessing the carbon sequestration capacity of the marginal seas of China.
关键词centennial-scale carbon storage sediment Min-Zhe belt South Yellow Sea area East China Sea
DOI10.1007/s00343-017-6242-y
收录类别SCI
语种英语
资助项目National Basic Research Program of China (973 Program)[2012CB956004] ; Fundamental Research Funds for the Central Universities[16lgjc22] ; National Basic Research Program of China (973 Program)[2012CB956004] ; Fundamental Research Funds for the Central Universities[16lgjc22]
WOS研究方向Marine & Freshwater Biology ; Oceanography
WOS类目Limnology ; Oceanography
WOS记录号WOS:000428050400012
出版者SCIENCE PRESS
引用统计
被引频次:10[WOS]   [WOS记录]     [WOS相关记录]
文献类型期刊论文
条目标识符http://ir.qdio.ac.cn/handle/337002/158768
专题海洋环流与波动重点实验室
通讯作者Wang Jianghai; Yuan Dongliang
作者单位1.Sun Yat Sen Univ, Sch Marine Sci, Guangdong Prov Key Lab Marine Resources & Coastal, South China Sea Bioresource Exploitat & Utilizat, Guangzhou 510006, Guangdong, Peoples R China
2.Chinese Acad Sci, Guangzhou Inst Geochem, Guangzhou 510640, Guangdong, Peoples R China
3.Qingdao Natl Lab Marine Sci & Technol, Funct Lab Ocean Dynam & Climate, Qingdao 266071, Peoples R China
4.Chinese Acad Sci, Inst Oceanol, CAS Key Lab Ocean Circulat & Wave Studies, Qingdao 266071, Peoples R China
通讯作者单位中国科学院海洋研究所
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Wang Jianghai,Xiao Xi,Zhou Qianzhi,et al. Rates and fluxes of centennial-scale carbon storage in the fine-grained sediments from the central South Yellow Sea and Min-Zhe belt, East China Sea[J]. JOURNAL OF OCEANOLOGY AND LIMNOLOGY,2018,36(1):139-152.
APA Wang Jianghai.,Xiao Xi.,Zhou Qianzhi.,Xu Xiaoming.,Zhang Chenxi.,...&Yuan Dongliang.(2018).Rates and fluxes of centennial-scale carbon storage in the fine-grained sediments from the central South Yellow Sea and Min-Zhe belt, East China Sea.JOURNAL OF OCEANOLOGY AND LIMNOLOGY,36(1),139-152.
MLA Wang Jianghai,et al."Rates and fluxes of centennial-scale carbon storage in the fine-grained sediments from the central South Yellow Sea and Min-Zhe belt, East China Sea".JOURNAL OF OCEANOLOGY AND LIMNOLOGY 36.1(2018):139-152.
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