A new high-resolution chronology for the late Maastrichtian warming event: establishing robust temporal links with the onset of Deccan volcanism

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A new high-resolution chronology for the late Maastrichtian warming event: establishing robust temporal links with the onset of Deccan volcanism

The late Maastrichtian warming event was defined by a global temperature increase of ∼2.5–5 °C that occurred ∼150–300 k.y. before the Cretaceous-Paleogene (K-Pg) mass extinction. This transient warming event has traditionally been associated with a major pulse of Deccan Traps (west-central India) vo...

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Bibliographic Details
Main Authors:	Barnet, James S.K., Littler, Kate, Kroon, Dick, Leng, Melanie J., Westerhold, Thomas, Röhl, Ursula, Zachos, James C.
Format:	Article
Published:	Geological Society of America 2017
Online Access:	https://eprints.nottingham.ac.uk/48791/

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