Ocean acidification at the Toarcian Anoxic Event captured by boron isotopes in the lime mud record

Abstract The Toarcian Oceanic Anoxic Event (ca. 183 million years ago) marks a global mass extinction coincident with dramatic changes in climate and ocean circulation, likely driven by large igneous province emplacement. Rapid carbon dioxide release may have induced global warming, widespread ocean...

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Bibliographic Details
Main Authors: Simone A. Kasemann, Tina Klein, Richard A. Boyle, Clemens V. Ullmann, Martin Aberhan, Anette Meixner, Luís V. Duarte, Timothy M. Lenton, Veronica Piazza, Rachel A. Wood
Format: Article
Language:English
Published: Nature Portfolio 2025-07-01
Series:Communications Earth & Environment
Online Access:https://doi.org/10.1038/s43247-025-02510-y
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