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Sulfur isotope heterogeneity in Martian shergottites reveals early atmosphere - mantle exchange
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  • Published: 26 March 2026

Sulfur isotope heterogeneity in Martian shergottites reveals early atmosphere - mantle exchange

  • Kiran Patil  ORCID: orcid.org/0009-0000-2355-10061,
  • James W. Dottin III  ORCID: orcid.org/0000-0002-1923-15761,
  • Hairuo Fu  ORCID: orcid.org/0000-0002-1823-20161,
  • Brian Monteleone2,
  • Nilanjan Chatterjee3,
  • Noah Hooper1,
  • Gareth Izon  ORCID: orcid.org/0000-0003-2742-49223,
  • J. Cameron Adams1,
  • Anthony Irving4,
  • Charles K. Shearer  ORCID: orcid.org/0000-0001-5819-42645,
  • Heather B. Franz  ORCID: orcid.org/0000-0001-9716-55976 &
  • …
  • Shuhei Ono  ORCID: orcid.org/0000-0002-1348-95843 

Communications Earth & Environment , Article number:  (2026) Cite this article

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Subjects

  • Geochemistry
  • Inner planets
  • Meteoritics
  • Petrology

Abstract

The study of sulfur isotopes on Mars provides crucial insights into the planet’s formation, differentiation, and volatile evolution. Primordial sulfur isotope compositions help distinguish Martian sulfur sources, including core-mantle interactions, magmatic outgassing, and atmospheric cycling. While bulk analyses have shown limited mass-independent fractionation (MIF-S), the mechanisms introducing MIF-S into Martian magmas remain poorly understood. Using in situ secondary ion mass spectrometry (SIMS), we analysed sulfides in four shergottites: Yamato 980459, Tissint, Gadamis 001, and NWA 11300, and found extreme heterogeneity in Δ³³S (–1.3 ± 0.48‰ to +1.42 ± 0.64‰) and δ³⁴S (–3.5 ± 0.11‰ to +0.73 ± 0.15‰). Large Δ³³S anomalies are observed in both depleted and enriched samples, indicating that MIF-S sulfur was incorporated into Martian magmatic systems through prolonged mantle-atmosphere exchange. This exchange likely began during magma ocean crystallisation and continued into later magmatic stages through ingassing, crustal assimilation, and/or recycling of crustal sulfur.

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Data availability

All the elemental compositions and sulfur isotopic data for the analysed sulfides in this study are available on Zenodo, the main text and the supplementary materials. (https://doi.org/10.5281/zenodo.18760943).

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Acknowledgements

This research was funded by Brown University (J.D. and K.P.) and NASA Solar System Exploration Virtual Institute (# 22-SSERVI4_2-0009 to JD and 22-SSERVI4_2- 0012 to JD and HF).

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Authors and Affiliations

  1. Department of Earth, Environmental and Planetary Sciences, Brown University, Providence, RI, USA

    Kiran Patil, James W. Dottin III, Hairuo Fu, Noah Hooper & J. Cameron Adams

  2. Marine Geology and Geophysics Department, Woods Hole Oceanographic Institution, Woods Hole, MA, USA

    Brian Monteleone

  3. Department of Earth, Atmospheric, and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, MA, USA

    Nilanjan Chatterjee, Gareth Izon & Shuhei Ono

  4. Department of Earth and Space Sciences, University of Washington, Seattle, WA, USA

    Anthony Irving

  5. Earth and Planetary Sciences Department, University of New Mexico, Albuquerque, NM, USA

    Charles K. Shearer

  6. Goddard Space Flight Center NASA, Greenbelt, MD, USA

    Heather B. Franz

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Contributions

K.P.: Conceptualisation, methodology, investigation, visualisation, writing—original draft and review and editing. J.D.: Conceptualisation, methodology, supervision, investigation, visualisation, writing—original draft, review and editing. H.F.: Investigation, visualisation, writing— original draft, review and editing. B.M.: Methodology, investigation, review and editing. N.C.: Methodology, investigation, review and editing. N.H.: Methodology, investigation, review and editing. J.C.A.: Investigation, review and editing. G.I.: Investigation, review and editing. A.I.: Review and editing. C.S.: Review and editing. HBF: Review and editing. S.O.: Review and editing.

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Correspondence to Kiran Patil.

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Patil, K., Dottin, J.W., Fu, H. et al. Sulfur isotope heterogeneity in Martian shergottites reveals early atmosphere - mantle exchange. Commun Earth Environ (2026). https://doi.org/10.1038/s43247-026-03420-3

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  • Received: 09 September 2025

  • Accepted: 10 March 2026

  • Published: 26 March 2026

  • DOI: https://doi.org/10.1038/s43247-026-03420-3

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