Primary Sulfur Isotopes of Intraplate Basalts and Implications for Deep S Recycling of Altered Oceanic Crust

Abstract Altered oceanic crust (AOC) is the largest contributor to the subducted sulfur (S) budget and its recycling modulates the redox evolution and S distribution in the mantle. However, the role of AOC in the deep cycling of S remains poorly constrained. Here we probe the primary S isotopes of Cenozoic intraplate basalts in eastern China by investigating sulfide inclusions in magmatic clinopyroxene megacrysts. These basalts were derived from the deep mantle metasomatized by melts derived from recycled AOC but show MORB‐like S isotopes (−0.9–0.9‰), suggesting that AOC‐derived melts transfer negligible sulfate and hardly change the δ 34 S and redox state of the deeper mantle. This contrasts with the generally high δ 34 S values of mantle wedge peridotites and primary arc magmas that reflect the slab addition of sulfate, indicating that S species and isotopes released from the subducted slab and associated f O 2 are not constant and vary with subduction depth.

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Publication Details

Journal
Geophysical Research Letters
Published
2024-12-11
DOI
https://doi.org/10.1029/2024gl111829
Citations
2
Primary Topic
Geological and Geochemical Analysis
Type
article
Field-Weighted Citation Impact
1.07

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article

Primary Sulfur Isotopes of Intraplate Basalts and Implications for Deep S Recycling of Altered Oceanic Crust

Lang Wang, Zaicong Wang, Pu Sun, Stephen Foley et al.
2 citations
Geophysical Research Letters
Geological and Geochemical Analysis
1.07
article

Primary Sulfur Isotopes of Intraplate Basalts and Implications for Deep S Recycling of Altered Oceanic Crust

Lang Wang, Zaicong Wang, Pu Sun, Stephen Foley, Zong‐Feng Yang, Zongqi Zou, Keqing Zong, Zhaochu Hu, Xiang Wang, Wen Zhang, Yongsheng Liu
article en
2 citations

Abstract

Abstract Altered oceanic crust (AOC) is the largest contributor to the subducted sulfur (S) budget and its recycling modulates the redox evolution and S distribution in the mantle. However, the role of AOC in the deep cycling of S remains poorly constrained. Here we probe the primary S isotopes of Cenozoic intraplate basalts in eastern China by investigating sulfide inclusions in magmatic clinopyroxene megacrysts. These basalts were derived from the deep mantle metasomatized by melts derived from recycled AOC but show MORB‐like S isotopes (−0.9–0.9‰), suggesting that AOC‐derived melts transfer negligible sulfate and hardly change the δ 34 S and redox state of the deeper mantle. This contrasts with the generally high δ 34 S values of mantle wedge peridotites and primary arc magmas that reflect the slab addition of sulfate, indicating that S species and isotopes released from the subducted slab and associated f O 2 are not constant and vary with subduction depth.

Geophysical Research LettersVol. 51(24)
Australian National University (AU), Chinese Academy of Sciences (CN), China University of Geosciences (CN), China University of Geosciences (Beijing) (CN), Institute of Oceanology (CN), Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou) (CN), Macquarie University (AU)
National Natural Science Foundation of China, China University of Geosciences, State Key Laboratory of Geological Processes and Mineral Resources, National Key Research and Development Program of China
Life below water
Openalex Percentile: Top 23%
Geological and Geochemical Analysis
1.07
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