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The Enrichment Mechanism of REE at Sulfate and Methane Transition Zone (SMTZ) of the Northern Part of the South China Sea
Xie Rui1,2,3,4; Wu Daidai3; Wei Jiangong1,2,4; Wang Liaoliang1,2,4; Liu Lihua3; Li Wenjing1,2,4; Wu Gang1,2,4; Guo Xudong1,2,4
2022-02-24
Source PublicationGEOFLUIDS
ISSN1468-8115
Volume2022Pages:13
Corresponding AuthorWu Daidai(wudd@ms.giec.ac.cn) ; Wei Jiangong(weijiangong007@163.com)
AbstractRare earth elements (REE) are important raw materials for electronic products and green-energy technology and deep-sea sediment as an important potential source of REE mineral. It is of great scientific significance to understand the influence of REE in deep-sea sediments. In this paper, thirty sediments samples and eleven sediments samples were collected at the site SH3 and SH1 of Shenhu area, respectively. The trace elements, major elements, and different Fe-Mn minerals were analyzed to investigate the role of anaerobic oxidation of methane (AOM) in the enrichment of rare earth elements in the marine sediments. The result showed that the content of n-ary sumation REE/Ti increased at the top of sulfate and methane transition zone (SMTZ) at site SH1 and SH3. Combined with the analysis of different forms of ferromanganese minerals and the REE patterns, it is inferred that there is little influence of terrigenous input to the REE content. In contrary, the REE-rich carbonate phase and REE-rich Fe-Mn oxides (hydroxides) phase have important contribution of REE enrichment at the top of SMTZ. Meanwhile, the calculations of the quantitative relationship between the REE-rich carbonate phase and REE-rich Fe-Mn oxides (hydroxides) phase also confirm this conclusion. And the AOM caused the decrease of the REE-rich Fe-Mn oxides (hydroxides) phase and increase of the REE-rich carbonate phase. This is the potential explanation of n-ary sumation REE/Ti enrichment at the top of SMTZ. This study is of great scientific significance for the study of REE enrichment mechanism in the methane seeps and provided a new sight of REE enrichment mechanism in deep-sea sediments.
DOI10.1155/2022/7571792
WOS KeywordRARE-EARTH-ELEMENTS ; GAS HYDRATE ; AUTHIGENIC CARBONATES ; SEEP-CARBONATES ; COLD SEEPS ; ANAEROBIC OXIDATION ; ACCRETIONARY PRISM ; SETTLING PARTICLES ; REDOX CONDITIONS ; PACIFIC-OCEAN
Indexed BySCI
Language英语
Funding ProjectKey Special Project for Introduced Talents Team of Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou)[GML2019ZD0201] ; Guangdong Basic and Applied Basic Research Fund Project[2021A1515011509] ; Municipal Science and Technology Program of Guangzhou[201904010311] ; Special project for marine economy development of Guangdong Province[GDME-2018D002] ; Institution of South China Sea Ecology and Environmental Engineering, Chinese Academy of Sciences[ISEE2018YB03] ; Youth Innovation Promotion Association CAS[2014321]
WOS Research AreaGeochemistry & Geophysics ; Geology
Funding OrganizationKey Special Project for Introduced Talents Team of Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou) ; Guangdong Basic and Applied Basic Research Fund Project ; Municipal Science and Technology Program of Guangzhou ; Special project for marine economy development of Guangdong Province ; Institution of South China Sea Ecology and Environmental Engineering, Chinese Academy of Sciences ; Youth Innovation Promotion Association CAS
WOS SubjectGeochemistry & Geophysics ; Geology
WOS IDWOS:000778248200001
PublisherWILEY-HINDAWI
Citation statistics
Document Type期刊论文
Identifierhttp://ir.giec.ac.cn/handle/344007/36072
Collection中国科学院广州能源研究所
Corresponding AuthorWu Daidai; Wei Jiangong
Affiliation1.Southern Marine Sci & Engn Guangdong Lab Guangzho, Guangzhou 511458, Peoples R China
2.Guangzhou Marine Geol Survey, MLR Key Lab Marine Mineral Resources, Guangzhou 510075, Peoples R China
3.Chinese Acad Sci, Guangzhou Inst Energy Convers, Key Lab Gas Hydrate, Guangzhou 510640, Peoples R China
4.Acad South China Sea Geol Sci, China Geol Survey, Sanya 572025, Peoples R China
First Author AffilicationGuangZhou Institute of Energy Conversion,Chinese Academy of Sciences
Recommended Citation
GB/T 7714
Xie Rui,Wu Daidai,Wei Jiangong,et al. The Enrichment Mechanism of REE at Sulfate and Methane Transition Zone (SMTZ) of the Northern Part of the South China Sea[J]. GEOFLUIDS,2022,2022:13.
APA Xie Rui.,Wu Daidai.,Wei Jiangong.,Wang Liaoliang.,Liu Lihua.,...&Guo Xudong.(2022).The Enrichment Mechanism of REE at Sulfate and Methane Transition Zone (SMTZ) of the Northern Part of the South China Sea.GEOFLUIDS,2022,13.
MLA Xie Rui,et al."The Enrichment Mechanism of REE at Sulfate and Methane Transition Zone (SMTZ) of the Northern Part of the South China Sea".GEOFLUIDS 2022(2022):13.
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