Copper isotope evidence for recycled crustal sulfides in deep mantle plume source

Abstract Earth’s crustal materials are recycled into the mantle through subduction, but the depth and nature of recycled components remain debated. Here we report copper (Cu) isotope evidence for the involvement of recycled crustal materials in a deep-mantle plume source. Permian mantle plume-derive...

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Main Authors: Junhua Yao, Wei Yuan, Zhengrong Wang, Frédéric Moynier, Wei-Guang Zhu, Ya-Dong Wu, Yuchen An, Jiubin Chen
Format: Article
Language:English
Published: Nature Portfolio 2025-06-01
Series:Communications Earth & Environment
Online Access:https://doi.org/10.1038/s43247-025-02468-x
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author Junhua Yao
Wei Yuan
Zhengrong Wang
Frédéric Moynier
Wei-Guang Zhu
Ya-Dong Wu
Yuchen An
Jiubin Chen
author_facet Junhua Yao
Wei Yuan
Zhengrong Wang
Frédéric Moynier
Wei-Guang Zhu
Ya-Dong Wu
Yuchen An
Jiubin Chen
author_sort Junhua Yao
collection DOAJ
description Abstract Earth’s crustal materials are recycled into the mantle through subduction, but the depth and nature of recycled components remain debated. Here we report copper (Cu) isotope evidence for the involvement of recycled crustal materials in a deep-mantle plume source. Permian mantle plume-derived picrites and basalts from the Emeishan large igneous province (Southwest China), excluding three hydrothermally altered outliers, exhibit δ65Cu values up to 0.65‰, obviously higher than typical mantle values (0.07 ± 0.10‰). The δ65Cu values show no correlation with loss-on-ignition (LOI), Mg#, ƐNd(t), Cu/Th, Cu/Pd, or redox state, ruling out magma differentiation or post-magmatic alteration. Instead, the elevated δ65Cu values most plausibly reflect recycled crustal sulfides with elevated δ65Cu value in the mantle source. These findings provide robust evidence for the recycling of Cu-rich sulfides into the deep mantle (potentially the lower mantle), elucidating the ultra-deep geochemical cycling of copper and sulfur within Earth’s interior.
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issn 2662-4435
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publishDate 2025-06-01
publisher Nature Portfolio
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series Communications Earth & Environment
spelling doaj-art-879bc51470bb42e38822dcb2519d03782025-08-20T03:22:57ZengNature PortfolioCommunications Earth & Environment2662-44352025-06-016111110.1038/s43247-025-02468-xCopper isotope evidence for recycled crustal sulfides in deep mantle plume sourceJunhua Yao0Wei Yuan1Zhengrong Wang2Frédéric Moynier3Wei-Guang Zhu4Ya-Dong Wu5Yuchen An6Jiubin Chen7Key Laboratory of Ocean Observation and Forecasting, Center of Deep Sea Research Institute of Oceanology, Chinese Academy of SciencesInstitute of Surface-Earth System Science, School of Earth System Science, Tianjin UniversityDepartment of Earth and Atmospheric Sciences, The City College of New York, CUNYUniversité Paris Cité, Institute de Physique du Globe de Paris, CNRS UMR7154, 1 rue JussieuState Key Laboratory of Ore Deposit Geochemistry, Institute of Geochemistry, Chinese Academy of SciencesState Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of SciencesInstitute of Surface-Earth System Science, School of Earth System Science, Tianjin UniversityInstitute of Surface-Earth System Science, School of Earth System Science, Tianjin UniversityAbstract Earth’s crustal materials are recycled into the mantle through subduction, but the depth and nature of recycled components remain debated. Here we report copper (Cu) isotope evidence for the involvement of recycled crustal materials in a deep-mantle plume source. Permian mantle plume-derived picrites and basalts from the Emeishan large igneous province (Southwest China), excluding three hydrothermally altered outliers, exhibit δ65Cu values up to 0.65‰, obviously higher than typical mantle values (0.07 ± 0.10‰). The δ65Cu values show no correlation with loss-on-ignition (LOI), Mg#, ƐNd(t), Cu/Th, Cu/Pd, or redox state, ruling out magma differentiation or post-magmatic alteration. Instead, the elevated δ65Cu values most plausibly reflect recycled crustal sulfides with elevated δ65Cu value in the mantle source. These findings provide robust evidence for the recycling of Cu-rich sulfides into the deep mantle (potentially the lower mantle), elucidating the ultra-deep geochemical cycling of copper and sulfur within Earth’s interior.https://doi.org/10.1038/s43247-025-02468-x
spellingShingle Junhua Yao
Wei Yuan
Zhengrong Wang
Frédéric Moynier
Wei-Guang Zhu
Ya-Dong Wu
Yuchen An
Jiubin Chen
Copper isotope evidence for recycled crustal sulfides in deep mantle plume source
Communications Earth & Environment
title Copper isotope evidence for recycled crustal sulfides in deep mantle plume source
title_full Copper isotope evidence for recycled crustal sulfides in deep mantle plume source
title_fullStr Copper isotope evidence for recycled crustal sulfides in deep mantle plume source
title_full_unstemmed Copper isotope evidence for recycled crustal sulfides in deep mantle plume source
title_short Copper isotope evidence for recycled crustal sulfides in deep mantle plume source
title_sort copper isotope evidence for recycled crustal sulfides in deep mantle plume source
url https://doi.org/10.1038/s43247-025-02468-x
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