A Martian meteorite that formed ≳4.1 billion years ago samples Mars’ early crust and mantle

Martian meteorites provide a record of the planet’s geological history. However, most are geologically young samples that are not representative of Mars’ surface, which is dominated by ancient rocks. We describe the Martian meteorite Teghaza 001 (Teg 001), a slowly cooled igneous rock that formed at least 4.1 billion years ago. Its composition, mineralogy, and texture are distinct from other Martian meteorites. We determine that Teg 001 is a sample of ancient crust, which formed from a geochemically distinct mantle source with primordial composition. The presence of aqueously altered minerals, combined with bulk and mineral-specific oxygen isotope measurements, indicate that Teg 001 experienced reactions with fluids enriched in 18 O, before ejection into space by an impact.

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Journal
Science
Published
2026-10-29
DOI
https://doi.org/10.1126/science.adz5646
Primary Topic
Astro and Planetary Science
Type
article
Field-Weighted Citation Impact
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article

A Martian meteorite that formed ≳4.1 billion years ago samples Mars’ early crust and mantle

François L. H. Tissot, Elizabeth Ann Bell, Lee M. Saper, Alicia M. Cruz‐Uribe et al.
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Science
Astro and Planetary Science
article

A Martian meteorite that formed ≳4.1 billion years ago samples Mars’ early crust and mantle

François L. H. Tissot, Elizabeth Ann Bell, Lee M. Saper, Alicia M. Cruz‐Uribe, K. Ziegler, Teng Ee Yap, Chi Ma, 云彬 管, C. B. Agee, J. Hu, Claire E. Bucholz, Haoyu Li, Yang Liu, Hayward Melton
article en

Abstract

Martian meteorites provide a record of the planet’s geological history. However, most are geologically young samples that are not representative of Mars’ surface, which is dominated by ancient rocks. We describe the Martian meteorite Teghaza 001 (Teg 001), a slowly cooled igneous rock that formed at least 4.1 billion years ago. Its composition, mineralogy, and texture are distinct from other Martian meteorites. We determine that Teg 001 is a sample of ancient crust, which formed from a geochemically distinct mantle source with primordial composition. The presence of aqueously altered minerals, combined with bulk and mineral-specific oxygen isotope measurements, indicate that Teg 001 experienced reactions with fluids enriched in 18 O, before ejection into space by an impact.

Science
California Institute of Technology (US), Jet Propulsion Laboratory (US), University of California, Los Angeles (US), University of New Mexico (US), University of Maine (US)
National Science Foundation, National Aeronautics and Space Administration
Openalex Percentile: Top 14%
Astro and Planetary Science
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A Martian meteorite that formed ≳4.1 billion years ago samples Mars’ early crust and mantle — François L. H. Tissot, Elizabeth Ann Bell, et al. · Science (2026) | TGRS Research Map | TGRS