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  • Huvudmeny

Causes and Effects of the Permian-Triassic Biotic Crisis Inferred from Continental Margin Sections and Modeling

Photo: Steve McLoughlin

Late Permian Glossopteris leaf from the Sydney Basin – one of the major casualties of the end-Permian biotic crisis.


The Late Permian-Early Triassic was marked by major perturbations to the Earth system, including the largest mass extinction of the geological record. This interval saw the final assembly of Pangea, a minimum in the extent of continental flooding by the sea, the development of extreme continentality, and unprecedented expansion of subtropical arid belts.

Geochemical proxy records reveal an Earth system that was primed for catastrophic response to triggers that may have included Siberian Trap volcanism, thermogenic methane and fly ash emission from intrusions into the West Siberian Coal Basin, and/or bolide impact.

This project involves an integrated sedimentological, geochemical, palaeobotanical, and palynological study of the Upper Permian to Lower Triassic stratigraphic records of the Bowen-Gunnedah-Sydney Basin System in eastern Australia, utilizing well-exposed surface sections supported by high-quality, bore core archives. We will synthesize these data with results from climate simulations.

Our investigations will be supported by extensive new, precise geochronological data from the Permian and Triassic succession of eastern Australia and our data will represent a transect through mid-high palaeolatitudes along the Panthalassan margin of Gondwana, allowing us to assess the possibility that the environmental stresses leading to the EPME were not evenly or synchronously distributed.

These environmental stresses identified from stratigraphic records will be integrated with climate sensitivity studies to evaluate possible responses to greenhouse gas, aerosol, and orbital forcing variations.

This research is funded by the National Science Foundation (USA)

Project Participants at the Museum

Stephen McLoughlin (researcher) 

Vivi Vajda (researcher)

External Project Participants

University of Nebraska-Lincoln, USA

Geoscience Australia, Canberra, Australia

University of Texas-Arlington, USA

School of Biological, Earth & Environmental Sciences, University College Cork

Selected Publications

Bomfleur, B., Blomenkemper, P., Kerp, H. & McLoughlin, S. 2018. Polar regions of the Mesozoic–Paleogene greenhouse world as refugia for relict plant groups. Transformative Paleobotany: Papers to Commemorate the Life and Legacy of Thomas N. Taylor. Krings, M., Harper, C.J., Cúneo, N.R., Rothwell, G.W. (eds), Elsevier, Amsterdam, 593-611. ISBN: 9780128130124

Edirisooriya, G., Dharmagunawardhane, H.A. & McLoughlin, S., 2018. The first record of the Permian Glossopteris flora from Sri Lanka: implications for hydrocarbon source rocks in the Mannar Basin. Geological Magazine 155: 907-920. DOI: https://doi.org/10.1017/S0016756816001114external link

Kustatscher, E., Ash, S.R., Karasev, E., Pott, C., Vajda, V., Yu, J. & McLoughlin, S., 2018. Flora of the Late Triassic. In Tanner, L.H. (ed.), Late Triassic of the World. Earth in a Time of Transition. Topics in Geobiology 46, Springer, Cham, Switzerland, 545–622. 10.1007/978-3-319-68009-5_13external link

McLoughlin, S., Bomfleur, B. & Drinnan, A.N., 2018. Pachytestopsis tayloriorum gen. et sp. nov., an anatomically preserved glossopterid seed from the Lopingian of Queensland, Australia. Transformative Paleobotany: Papers to Commemorate the Life and Legacy of Thomas N. Taylor. Krings, M., Harper, C.J., Cúneo, N.R., Rothwell, G.W. (eds), Elsevier, Amsterdam, 155-178. ISBN: 9780128130124

McLoughlin, S. 2017. Australia's Permian vertebrates: where have they gone? Australian Age of Dinosaurs Magazine 14: 70-75.

McLoughlin, S., 2017. Antarctic Glossopteris forests. 52 More Things You Should Know About Palaeontology. Cullum, A. & Martinius, A.W. (eds.). Agile Libre, Nova Scotia, pp. 22–23.

McLoughlin, S. 2016. A new genus of glossopterid fructifications from the Artinskian–Changhsingian of eastern Australia. Ameghiniana 53: 586–598.