87- The Permian Extinction

Twenty-one episodes ago, we discussed the extinction of the dinosaurs 66 million years before the present. However, this isn't the only mass extinction event the Earth has witnessed. Let's go back to 252 million years ago and watch the Great Dying unfold…

Sources for this episode:

  • Campbell, N. A., Urry, L. A., Cain, M. L., Wasserman, S. A., Minorsky, P. V. and Reece, J. B. (2018), Biology: a global approach, 11th edition (Global Edition), Harlow, Pearson Education Limited.
  • Clennett, C., Locke, J. and Jackson, T. (editorial consultants) (2023), How Biology Works. LonondM Darling Kindersley Ltd.
  • Cohen, K.M., Finney, S.C., Gibbard, P.L. & Fan, J.-X. (2013; updated) The ICS International Chronostratigraphic Chart. Episodes 36: 199-204.
  • Cui, Y. and Kump, L. R. (2015), Global warming and the end-Permian extinction event: Proxy and modeling perspectives. Earth-Science Reviews 149: 5-22.
  • Herron, J. C., and Freeman, S. (2015), Evolutionary Analysis. Harlow: Pearson Education Ltd.
  • Hochuli, P. A., Hermann, E., Vigran, J. O., Bucher, H.and Weissert, H. (2010), Rapid demise and recovery of planet ecosystems across the end-Permian extinction event. Global and Planetary Change 74: 144-155.
  • Kaiser, M. J., Attrill, M. J., Jennings, S., Thomas, D. N., Barnes, D. K. A., Brierley, A. S., Graham, N. A. J., Hiddink, J. G., Howell, K. and Kaartokallio, H. (2020), Marine Ecology: Processes, Systems and Impacts (3rd edition°; Oxford: Oxford University Press.
  • Twitchett, R. J. (2007), The Lilliput effect in the aftermath of the end-Permian extinction event. Palaeogeography, Palaeoclimatology, Palaeoecology 252: 132-144.