Abstract

Direct links between carbonaceous chondrites and their parent bodies in the solar system are rare. The Winchcombe meteorite is the most accurately recorded carbonaceous chondrite fall. Its pre-atmospheric orbit and cosmic-ray exposure age confirm that it arrived on Earth shortly after ejection from a primitive asteroid. Recovered only hours after falling, the composition of the Winchcombe meteorite is largely unmodified by the terrestrial environment. It contains abundant hydrated silicates formed during fluid-rock reactions, and carbon- and nitrogen-bearing organic matter including soluble protein amino acids. The near-pristine hydrogen isotopic composition of the Winchcombe meteorite is comparable to the terrestrial hydrosphere, providing further evidence that volatile-rich carbonaceous asteroids played an important role in the origin of Earth’s water.

DOI

10.1126/sciadv.abq3925

Publication Date

2022-11-18

Publication Title

Science Advances

Volume

8

Issue

46

Publisher

American Association for the Advancement of Science (AAAS)

ISSN

2375-2548

Embargo Period

2024-11-25

Keywords

Carbonaceous Chondrites, Meteorite, Winchcombe

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