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...
| Main Authors: | , , , , , , |
|---|---|
| Format: | Article |
| Published: |
Geological Society of America
2017
|
| Online Access: | https://eprints.nottingham.ac.uk/48791/ |