A recent study on meteorite relics identified by researchers in the lunar samples brought back by China's Chang'e-6 may fundamentally reshaped the debate on where the moon's water originates, according to a scientist at the institute that oversaw the research.
The study, published in the latest issue of the journal Proceedings of the National Academy of Sciences, was led by a research team from the Guangzhou Institute of Geochemistry (GIG) under the Chinese Academy of Sciences.
Using advanced techniques to examine mineral composition and oxygen isotopes, the researchers scrutinized lunar soil and confirmed that the fragments came from CI-like chondrites -- a type of meteorite rich in water and organic materials that typically originates in the outer Solar System.
This discovery not only indicates that material from the outer Solar System can migrate to the inner Solar System, but also has important implications for explaining the origin of water on the lunar surface, said Lin Mang, a researcher at GIG.
"There are many hypotheses about the origin of the water on the moon. Some say it was generated on the moon, some say it came from the sun, and some say it came from cometary meteorites. The meteorites that we identified are rich in water, but previously we thought the percentage of such meteorites was very small on the moon. The discovery of numerous such meteorites suggests their contribution to the lunar water was underestimated. Further research is needed to quantify the true extent of water brought to the moon by these meteorites," Lin said.
In 2024, Chang'e-6 made history by bringing 1,935.3 grams of lunar far-side samples back to Earth. These samples were collected from the South Pole-Aitken (SPA) Basin, the largest, deepest, and oldest basin on the moon.
Chang'e 6 moon samples reveal new insights into provenance of lunar water: scientist
