Overview
- Researchers identified seven microscopic olivine-bearing clasts in far-side lunar soil whose chemical and triple-oxygen isotope signatures match CI-like carbonaceous chondrites.
- The team used scanning electron microscopy, electron probe microanalysis and secondary ion mass spectrometry to confirm the fragments’ non-lunar origin.
- Because the Moon preserves fragile impact debris that Earth’s atmosphere destroys, the result highlights bias in Earth’s meteorite record and suggests more water-rich impactors than previously inferred.
- The authors estimate CI-like material could represent up to about 30% of lunar impactors, a provisional figure that will require more samples and independent checks.
- The same Chang'e-6 suite records two basaltic episodes around 4.2 and 2.8 billion years ago and preserves signs of a transient ancient magnetic field in younger rocks.