Isotopic comparison of K/T boundary impact glass with melt rock from the Chicxulub and Manson impact structures

Astronomy and Astrophysics – Astrophysics

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Cretaceous-Tertiary Boundary, Glass, Isotopes, Melting, Meteoritic Damage, Rocks, Craters, Oxygen 18, Radioactive Age Determination

Scientific paper

Strontium, neodymium, and oxygen isotopic compositions are reported for core samples of impact melt rock recovered from drill holes into the Chicxulub and Manson craters, which are candidate source craters for the catastrophic impact that occurred at the boundary between the Cretaceous and Tertiary periods (K/T boundary). The data are compared with previously published isotopic data from impact glasses from the K/T boundary of the Beloc formation in Haiti. It is found that the Chicxulub melt rocks are isotopically indistinguishable from the K/T impact glass, supporting the hypothesis that Chicxulub is a source crater for the K/T catastrophe. In contrast, the Manson melt rocks have a clearly different isotopic composition.

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