Microscale iron and sulphur isotopic compositions reveal pyritization pathways during early diagenesis

Abstract Sedimentary pyrite iron and sulphur isotope compositions (δ56FePYR, δ34SPYR, Δ33SPYR) are commonly used to reconstruct global ocean properties and the evolving oxidation state of Earth’s surface, motivating exploration of impacts of diagenesis on pyrite-based proxies. Along with auxiliary p...

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Bibliographic Details
Main Authors: Virgil Pasquier, Johanna Marin-Carbonne, Thomas Giunta, Livio Ruffine, Itay Halevy
Format: Article
Language:English
Published: Nature Portfolio 2025-03-01
Series:Communications Earth & Environment
Online Access:https://doi.org/10.1038/s43247-025-02213-4
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