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How Large Igneous Provinces Have Killed Most Life on Earth—Numerous Times

Grasby, Stephen E.; Bond, David P.G.

Authors

Stephen E. Grasby

Profile image of David Bond

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



Abstract

Evolution has not been a simple path. Since the first appearance of complex life, there have been several mass extinctions on Earth. This was exemplified by the most severe event during the Phanerozoic, the end-Permian mass extinction that occurred 252 million years ago and saw a loss of 90% and 70% of all marine and terrestrial species, respectively. Such mass extinctions have entirely reset ecosystems. Increasing evidence points to the massive eruption and crustal emplacement of magmas associated with large igneous provinces (LIPs) as key drivers of these events. Understanding how LIP events disrupted global biogeochemical cycles is of prime importance, especially as humans alter the atmosphere and biosphere today. We explore the cascading impacts of LIP events on global climate, oceans, and land—including runaway greenhouses, the release of toxic metals to the environment, the destruction of the ozone layer, and how global oceans are driven to anoxic and acidic states—all of which have parallels in the consequences of modern industrialisation.

Citation

Grasby, S. E., & Bond, D. P. (2023). How Large Igneous Provinces Have Killed Most Life on Earth—Numerous Times. Elements: An International Magazine of Mineralogy, Geochemistry, and Petrology, 19(5), 276-281. https://doi.org/10.2138/gselements.19.5.276

Journal Article Type Article
Acceptance Date Nov 17, 2023
Online Publication Date Dec 19, 2023
Publication Date Oct 1, 2023
Deposit Date Jan 19, 2024
Publicly Available Date Jan 31, 2024
Journal Elements
Print ISSN 1811-5209
Electronic ISSN 1811-5217
Publisher Mineralogical Society of America
Peer Reviewed Peer Reviewed
Volume 19
Issue 5
Pages 276-281
DOI https://doi.org/10.2138/gselements.19.5.276
Keywords Large igneous province; Carbon cycle; Mass extinction; Global warming; Marine anoxia
Public URL https://hull-repository.worktribe.com/output/4520292

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