A lithostratigraphic reappraisal of a Permian-Triassic fluvial succession at Allan Hills (Antarctica) and implications for the terrestrial end-Permian extinction event

Between Permian to Triassic, the Earth experienced climatic and biotic crises, included the greatest mass extinction at the Permian-Triassic boundary. These climatic and biological changes are reflected in both marine and terrestrial depositional systems. Over this time span, the Gondwana superconti...

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Bibliographic Details
Published in:Palaeogeography, Palaeoclimatology, Palaeoecology
Main Authors: Cornamusini, G., Zurli, L., Liberato, G. P., Corti, V., Gulbranson, E. L., Perotti, M., Sandroni, S.
Format: Article in Journal/Newspaper
Language:English
Published: 2023
Subjects:
Online Access:https://hdl.handle.net/11365/1239394
https://doi.org/10.1016/j.palaeo.2023.111741
https://www.sciencedirect.com/science/article/pii/S0031018223003590?via=ihub