Not exact matches
Like a chemical fingerprint, the isotopic ratio between Earth's
samples and the carbonaceous
chondrites»
samples matched.
But the
chondrite signatures are too heavy to explain the deep Earth
samples, Hallis says.
In the
samples of mantle gas taken by Holland and his colleagues, the krypton measurements were heavy, producing «something that looks rather like gases that are trapped in primitive
chondrites today,» Pepin says.
One type, called carbonaceous
chondrites, contain some of the most - primitive known
samples of Solar System material, including a lot more xenon than is found in our own planet's atmosphere.