Gradual warming prior to the end-Permian mass extinction

Gliwa J, Wiedenbeck M, Schobben M, Ullmann C, Kießling W, Ghaderi A, Struck U, Korn D (2022)

Publication Type: Journal article

Publication year: 2022

Journal

Palaeontology Wiley

Book Volume: 65

Journal Issue: 5

DOI: 10.1111/pala.12621

Abstract

The biggest known mass extinction in the history of animal life occurred at the Permian-Triassic boundary and has often been linked to global warming. Previous studies have suggested that a geologically rapid (<40 kyr) temperature increase of more than 10 degrees C occurred simultaneously with the main extinction pulse. This hypothesis is challenged by geochemical and palaeontological data indicating profound environmental perturbations and a temperature rise prior to the main extinction. Using secondary ion mass spectrometry (SIMS), we measured oxygen isotope ratios from Changhsingian (late Permian) ostracods of north-western Iran. Our data show that ambient seawater temperature began to rise at least 300 kyr prior to the main extinction event. Gradual warming by approximately 12 degrees C was probably responsible for initial environmental degradation that eventually culminated in the global end-Permian mass extinction.

Authors with CRIS profile

Wolfgang Kießling Lehrstuhl für Paläoumwelt

Involved external institutions

Leibniz-Institut für Evolutions- und Biodiversitätsforschung / Leibniz Institute for Evolution and Biodiversity Science DE Germany (DE) Helmholtz-Zentrum Potsdam Deutsches GeoForschungsZentrum - GFZ DE Germany (DE) Universiteit Utrecht (UU) / Utrecht University NL Netherlands (NL) University of Exeter GB United Kingdom (GB) Ferdowsi University of Mashhad IR Iran, Islamic Republic of (IR)

How to cite

APA:

Gliwa, J., Wiedenbeck, M., Schobben, M., Ullmann, C., Kießling, W., Ghaderi, A.,... Korn, D. (2022). Gradual warming prior to the end-Permian mass extinction. Palaeontology, 65(5). https://dx.doi.org/10.1111/pala.12621

MLA:

Gliwa, Jana, et al. "Gradual warming prior to the end-Permian mass extinction." Palaeontology 65.5 (2022).

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