Sun Y, Farnsworth A, Joachimski M, Wignall PB, Krystyn L, Bond DP, Ravidà DC, Valdes PJ (2024)
Publication Type: Journal article
Publication year: 2024
Book Volume: 385
Pages Range: 1189-1195
Journal Issue: 6714
The ultimate driver of the end-Permian mass extinction is a topic of much debate. Here, we used a multiproxy and paleoclimate modeling approach to establish a unifying theory elucidating the heightened susceptibility of the Pangean world to the prolonged and intensified El Niño events leading to an extinction state. As atmospheric partial pressure of carbon dioxide doubled from about 410 to about 860 ppm (parts per million) in the latest Permian, the meridional overturning circulation collapsed, the Hadley cell contracted, and El Niños intensified. The resultant deforestation, reef demise, and plankton crisis marked the start of a cascading environmental disaster. Reduced carbon sequestration initiated positive feedback, producing a warmer hothouse and, consequently, stronger El Niños. The compounding effects of elevated climate variability and mean state warming led to catastrophic but diachronous terrestrial and marine losses.
APA:
Sun, Y., Farnsworth, A., Joachimski, M., Wignall, P.B., Krystyn, L., Bond, D.P.,... Valdes, P.J. (2024). Mega El Niño instigated the end-Permian mass extinction. Science, 385(6714), 1189-1195. https://doi.org/10.1126/science.ado2030
MLA:
Sun, Yadong, et al. "Mega El Niño instigated the end-Permian mass extinction." Science 385.6714 (2024): 1189-1195.
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