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    Volume 50 Issue 7
    Jul.  2025
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    Zhang Junbo, Huang Jing, Xu Rong, Liu Yongsheng, 2025. Mantle Heterogeneity Recorded by Mass⁃Independent Fractionation of Sulfur Isotopes and Dynamic Implications. Earth Science, 50(7): 2482-2497. doi: 10.3799/dqkx.2025.129
    Citation: Zhang Junbo, Huang Jing, Xu Rong, Liu Yongsheng, 2025. Mantle Heterogeneity Recorded by Mass⁃Independent Fractionation of Sulfur Isotopes and Dynamic Implications. Earth Science, 50(7): 2482-2497. doi: 10.3799/dqkx.2025.129

    Mantle Heterogeneity Recorded by Mass⁃Independent Fractionation of Sulfur Isotopes and Dynamic Implications

    doi: 10.3799/dqkx.2025.129
    • Received Date: 2025-06-22
      Available Online: 2025-07-29
    • Publish Date: 2025-07-25
    • Sulfur is a volatile element that is prone to mass-dependent fractionation of sulfur isotopes (MDF-S) during shallow magmatic processes (e.g., fractional crystallization and magma degassing), which limits us to constrain the properties of major mantle chemical reservoirs. The mass-independent fractionation of sulfur isotopes (MIF-S) is a phenomenon in which the fractionation behavior of sulfur isotopes deviates from the mass dependent relationship. MIF-S is mainly produced through photochemical reactions of sulfur-containing molecules under high-energy ultraviolet radiation, and its fractionation mechanism is closely related to the atmospheric evolution on early Earth. It is worth noting that MIF-S signals are commonly preserved in Archean sedimentary rocks, but they disappeared after the Great Oxidation Event (GOE). MIF-S does not rely on mantle redox states and high-temperature processes (such as partial melting, fractional crystallization, magma degassing), and can effectively avoid MDF-S driven by shallow magma processes. And so, MIF-S is crucial for understanding the onset of plate tectonics, mantle redox states, and deep material cycling. On the basis of a brief introduction to the theories of MDF-S and MIF-S, this review summarizes the sulfur isotope composition of major mantle chemical reservoirs, and focuses on the important progress in mantle heterogeneity and onset of plate tectonics recorded by MIF-S in the past two decades.

       

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