Skip to main content

Research Repository

Advanced Search

Large igneous provinces and mass extinctions: an update

Bond, David P. G.; Wignall, Paul B.

Authors

Profile image of David Bond

David Bond D.Bond@hull.ac.uk
Palaeoenvironmental Scientist and Schools Liason Officer

Paul B. Wignall



Abstract

The temporal link between mass extinctions and large igneous provinces is well known. Here, we examine this link by focusing on the potential climatic effects of large igneous province eruptions during several extinction crises that show the best correlation with mass volcanism: the Frasnian-Famennian (Late Devonian), Capitanian (Middle Permian), end-Permian, end-Triassic, and Toarcian (Early Jurassic) extinctions. It is clear that there is no direct correlation between total volume of lava and extinction magnitude because there is always sufficient recovery time between individual eruptions to negate any cumulative effect of successive flood basalt eruptions. Instead, the environmental and climatic damage must be attributed to single-pulse gas effusions. It is notable that the best-constrained examples of death-by-volcanism record the main extinction pulse at the onset of (often explosive) volcanism (e.g., the Capitanian, end-Permian, and end-Triassic examples), suggesting that the rapid injection of vast quantities of volcanic gas (CO 2 and SO 2 ) is the trigger for a truly major biotic catastrophe. Warming and marine anoxia feature in many extinction scenarios, indicating that the ability of a large igneous province to induce these proximal killers (from CO 2 emissions and thermogenic greenhouse gases) is the single most important factor governing its lethality. Intriguingly, many voluminous large igneous province eruptions, especially those of the Cretaceous oceanic plateaus, are not associated with significant extinction losses. This suggests that the link between the two phenomena may be controlled by a range of factors, including continental configuration, the latitude, volume, rate, and duration of eruption, its style and setting (continental vs. oceanic), the preexisting climate state, and the resilience of the extant biota to change.

Citation

Bond, D. P. G., & Wignall, P. B. (2014). Large igneous provinces and mass extinctions: an update. In Geological Society of America Special Papers (29-55). Geological Society of America. https://doi.org/10.1130/2014.2505%2802%29

Online Publication Date Jun 10, 2014
Publication Date Sep 16, 2014
Deposit Date May 12, 2015
Publicly Available Date May 12, 2015
Journal Volcanism, impacts, and mass extinctions
Print ISSN 0072-1077
Publisher Geological Society of America
Peer Reviewed Not Peer Reviewed
Volume 505
Pages 29-55
Book Title Geological Society of America Special Papers
ISBN 9780813725055
DOI https://doi.org/10.1130/2014.2505%2802%29
Keywords Mass extinctions, Volcanism
Public URL https://hull-repository.worktribe.com/output/373637
Publisher URL https://pubs.geoscienceworld.org/books/book/674/chapter/3807763/
Contract Date May 12, 2015

Files






You might also like



Downloadable Citations