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The eruptive tempo of Deccan volcanism in relation to the Cretaceous-Paleogene boundary
Journal article   Open access   Peer reviewed

The eruptive tempo of Deccan volcanism in relation to the Cretaceous-Paleogene boundary

Courtney J Sprain, Paul R Renne, Loÿc Vanderkluysen, Kanchan Pande, Stephen Self and Tushar Mittal
Science (American Association for the Advancement of Science), v 363(6429), pp 866-870
22 Feb 2019
PMID: 30792301
url
https://escholarship.org/uc/item/8sj8w1rfView

Abstract

ESI Highly Cited Paper (Incites)
Late Cretaceous records of environmental change suggest that Deccan Traps (DT) volcanism contributed to the Cretaceous-Paleogene boundary (KPB) ecosystem crisis. However, testing this hypothesis requires identification of the KPB in the DT. We constrain the location of the KPB with high-precision argon-40/argon-39 data to be coincident with changes in the magmatic plumbing system. We also found that the DT did not erupt in three discrete large pulses and that >90% of DT volume erupted in <1 million years, with ~75% emplaced post-KPB. Late Cretaceous records of climate change coincide temporally with the eruption of the smallest DT phases, suggesting that either the release of climate-modifying gases is not directly related to eruptive volume or DT volcanism was not the source of Late Cretaceous climate change.

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Domestic collaboration
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Web of Science research areas
Geochemistry & Geophysics
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