Precise radiometric age establishes Yarrabubba, Western Australia, as Earth’s oldest recognised meteorite impact structure

Timmons M. Erickson (), Christopher L. Kirkland, Nicholas E. Timms, Aaron J. Cavosie and Thomas M. Davison
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Timmons M. Erickson: NASA Johnson Space Center
Christopher L. Kirkland: Curtin University
Nicholas E. Timms: Curtin University
Aaron J. Cavosie: Curtin University
Thomas M. Davison: Imperial College London

Nature Communications, 2020, vol. 11, issue 1, 1-8

Abstract: Abstract The ~70 km-diameter Yarrabubba impact structure in Western Australia is regarded as among Earth’s oldest, but has hitherto lacked precise age constraints. Here we present U–Pb ages for impact-driven shock-recrystallised accessory minerals. Shock-recrystallised monazite yields a precise impact age of 2229 ± 5 Ma, coeval with shock-reset zircon. This result establishes Yarrabubba as the oldest recognised meteorite impact structure on Earth, extending the terrestrial cratering record back >200 million years. The age of Yarrabubba coincides, within uncertainty, with temporal constraint for the youngest Palaeoproterozoic glacial deposits, the Rietfontein diamictite in South Africa. Numerical impact simulations indicate that a 70 km-diameter crater into a continental glacier could release between 8.7 × 1013 to 5.0 × 1015 kg of H2O vapour instantaneously into the atmosphere. These results provide new estimates of impact-produced H2O vapour abundances for models investigating termination of the Paleoproterozoic glaciations, and highlight the possible role of impact cratering in modifying Earth’s climate.

Date: 2020
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DOI: 10.1038/s41467-019-13985-7

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