Published in

American Association for the Advancement of Science, Science Advances, 9(5), 2019

DOI: 10.1126/sciadv.aax4184

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An extraterrestrial trigger for the mid-Ordovician ice age: Dust from the breakup of the L-chondrite parent body

This paper is made freely available by the publisher.
This paper is made freely available by the publisher.

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Data provided by SHERPA/RoMEO

Abstract

The disruption of a 150-km large asteroid filled the inner solar system with dust that cooled Earth and caused faunal turnovers.