中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Carbon Input and Output at Subduction Zones: Review and Prospect

文献类型:期刊论文

作者Chen, Wei1,2; Zhang, Guoliang1,2
刊名JOURNAL OF OCEAN UNIVERSITY OF CHINA
出版日期2025-06-01
卷号24期号:3页码:657-671
关键词deep carbon cycle subduction zones carbon flux slab decarbonation
ISSN号1672-5182
DOI10.1007/s11802-025-5942-8
通讯作者Zhang, Guoliang(zhanggliang5@mail.sysu.edu.cn)
英文摘要Subduction zones, linking the surface and deep carbon reservoirs, significantly affect the Earth's long-term climate change and habitability. The subducting slabs undergo decarbonation with increasing pressure and temperature, during which partial carbon mobilizes out of the slab and returns to the surface by arc volcanism or degassing, while the residual carbon continues to descend to greater depths in the mantle. The estimated carbon influx at subduction zones depends strongly on the calculation model, with contributions from sediments ranging from 15 to 60 Mt C/yr, altered ocean basalts from 18 to 61 Mt C/yr, and serpentinized perdotites from 1.3 to 36 Mt C/yr. The carbon influx varies in space and time. Carbon removal from subducting slab occurs through metamorphic reactions, carbonate dissolution, diapirism, hydrocarbon formation and melting. Among these decarbonation mechanisms, diapirism and slab meting play a decisive role in dictating the depth at which surface carbonates can subduct. Specifically, diapirism may restrict sedimentary carbonates at shallow depths (<200 km), while slab melting exhausts all carbonates from the altered ocean crust near transition zones (410-660 km). Consequently, a mechanism enabling surface carbonates to reach the lower mantle, i.e., ultra-deep carbon cycle, is required to be in accordance with observations by natural samples.
WOS关键词DEEP CARBON ; PHASE-RELATIONS ; OCEANIC-CRUST ; METAMORPHIC DEVOLATILIZATION ; CALCITE SOLUBILITY ; ATMOSPHERIC CO2 ; CORE COMPLEX ; ECLOGITE ; WATER ; GPA
资助项目Marine S&T Fund of Shandong Province for Pilot National Laboratory for Marine Science and Technology (Qingdao)[2022QNLM050201-3] ; National Key R&D Program of China[2022YFF0801000] ; National Natural Science Foundation of China[92158206] ; National Natural Science Foundation of China[42003049]
WOS研究方向Oceanography
语种英语
WOS记录号WOS:001484623000006
出版者OCEAN UNIV CHINA
源URL[http://ir.qdio.ac.cn/handle/337002/202025]  
专题海洋研究所_海洋环流与波动重点实验室
通讯作者Zhang, Guoliang
作者单位1.Chinese Acad Sci, Inst Oceanol, Key Lab Ocean Observat & Forecasting, Qingdao 266071, Peoples R China
2.Sun Yat Sen Univ, Sch Marine Sci, Zhuhai 519082, Peoples R China
推荐引用方式
GB/T 7714
Chen, Wei,Zhang, Guoliang. Carbon Input and Output at Subduction Zones: Review and Prospect[J]. JOURNAL OF OCEAN UNIVERSITY OF CHINA,2025,24(3):657-671.
APA Chen, Wei,&Zhang, Guoliang.(2025).Carbon Input and Output at Subduction Zones: Review and Prospect.JOURNAL OF OCEAN UNIVERSITY OF CHINA,24(3),657-671.
MLA Chen, Wei,et al."Carbon Input and Output at Subduction Zones: Review and Prospect".JOURNAL OF OCEAN UNIVERSITY OF CHINA 24.3(2025):657-671.

入库方式: OAI收割

来源:海洋研究所

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