87Sr/86Sr stratigraphy from the Early Triassic of Zal, Iran: Linking temperature to weathering rates and the tempo of ecosystem recovery

Denniston, R. F.; Sedlacek, A. R. C.; Saltzman, M. R.; ALGEO, T. J.; Horacek, M; Brandner, R; Foland, K.

doi:10.1130/G35545.1

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87Sr/86Sr stratigraphy from the Early Triassic of Zal, Iran: Linking temperature to weathering rates and the tempo of ecosystem recovery

Author(s): A. R. C. Sedlacek , M. R. Saltzman , T. J. Algeo , M. Horacek , R. Brandner , K. Foland , R. F. Denniston

Publication date Created: August 26 2014

Publication date (Print): July 21 2014

Journal: Geology

Publisher: Geological Society of America

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87Sr/86Sr, δ13C and δ18O evolution of Phanerozoic seawater

Jan Veizer, Davin Ala, Karem Azmy … (1999)

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Lethally hot temperatures during the Early Triassic greenhouse.

Yadong Sun, Michael Joachimski, Paul B. Wignall … (2012)

Global warming is widely regarded to have played a contributing role in numerous past biotic crises. Here, we show that the end-Permian mass extinction coincided with a rapid temperature rise to exceptionally high values in the Early Triassic that were inimical to life in equatorial latitudes and suppressed ecosystem recovery. This was manifested in the loss of calcareous algae, the near-absence of fish in equatorial Tethys, and the dominance of small taxa of invertebrates during the thermal maxima. High temperatures drove most Early Triassic plants and animals out of equatorial terrestrial ecosystems and probably were a major cause of the end-Smithian crisis.