Marine Strontium Isotope Evolution at the Triassic‐Jurassic Transition Links Transient Changes in Continental Weathering to Volcanism of the Central Atlantic Magmatic Province

Marine Strontium Isotope Evolution at the Triassic‐Jurassic Transition Links Transient Changes in Continental Weathering to Volcanism of the Central Atlantic Magmatic Province

Abstract The end‐Triassic extinction (ETE) is one of the most severe biotic crises in the Phanerozoic. This event was synchronous with volcanism of the Central Atlantic Magmatic Province (CAMP), the ultimate cause of the extinction and related environmental perturbations. However, the continental we...

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Bibliographic Details
Main Authors: Bernát Heszler, Joachim Katchinoff, László Palcsu, Anikó Horváth, Zsolt Vallner, Emma Blanka Kovács, Noah Planavsky, József Pálfy
Format: Article
Language:English
Published: Wiley 2024-03-01
Series:Geochemistry, Geophysics, Geosystems
Subjects:
Triassic‐Jurassic boundary
end‐Triassic extinction
CAMP large igneous province
strontium isotope stratigraphy
continental weathering
Sr flux modeling
Online Access:https://doi.org/10.1029/2024GC011464

Internet

https://doi.org/10.1029/2024GC011464

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