2022
DOI: 10.5194/egusphere-egu22-2379
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The Permian-Triassic boundary across the Barents Shelf: an intricate record of climate change, mass extinction, recovery, and basin reorganisation

Abstract: <p>About 252 million years ago, near the end of the Permian, the Earth experienced its most dramatic mass extinction, caused by magmatic intrusions and volcanic eruptions associated with the Siberian Traps Large Igneous Province. This led to catastrophic global climatic changes, impacts of which lasted well into the Early Triassic.</p><p>Here, we summarise the results gathered from the study of sedimentary successions spread across the Barents Shelf that recorded the E… Show more

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