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That team, however, hadn't been able to prove the water hadn't been introduced to the moon rocks on Earth, perhaps through sloppy handling.
One way to determine a water sample's birthplace is to measure the amounts of different hydrogen isotopes inside the water—a technique unavailable to the Nature team, said James Greenwood, a professor of Earth and environmental sciences at Wesleyan University in Middletown, Connecticut.
Isotope measurements can serve as fingerprints. Water from Earth's mantle has a different isotope ratio than water from a comet, for example.
When the Nature study came out, Greenwood was pioneering a technique that allowed him to study the chemical makeups of Martian meteorites. He later applied his method to samples of the mineral apatite, culled from a variety of moon-rock types, to determine the fingerprint of the water molecules inside.
The work proves that the moon-rock water "is not from us," he said at a presentation of his findings at the 41st Lunar and Planetary Science Conference in Houston, Texas.
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