Articles | Volume 14, issue 4
https://doi.org/10.5194/cp-14-441-2018
https://doi.org/10.5194/cp-14-441-2018
Research article
 | 
09 Apr 2018
Research article |  | 09 Apr 2018

Salinity changes and anoxia resulting from enhanced run-off during the late Permian global warming and mass extinction event

Elsbeth E. van Soelen, Richard J. Twitchett, and Wolfram M. Kürschner

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Sci. Dril., 24, 15–40, https://doi.org/10.5194/sd-24-15-2018,https://doi.org/10.5194/sd-24-15-2018, 2018
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Cited articles

Algeo, T. J. and Twitchett, R. J.: Anomalous Early Triassic sediment fluxes due to elevated weathering rates and their biological consequences, Geology, 38, 1023–1026, https://doi.org/10.1130/G31203.1, 2010.
Balme, B. E.: Palynology of Permian-Triassic boundary beds at Kap Stosch, East Greenland, Nyt nordisk forlag, 200, 37 p., 1979.
Benton, M. J. and Twitchett, R. J.: How to kill (almost) all life: the end-Permian extinction event, Trends Ecol. Evol., 18, 358–365, https://doi.org/10.1016/S0169-5347(03)00093-4, 2003.
Bond, D. P. G. and Wignall, P. B.: Pyrite framboid study of marine Permian–Triassic boundary sections: A complex anoxic event and its relationship to contemporaneous mass extinction, GSA Bulletin, 122, 1265–1279, https://doi.org/10.1130/B30042.1, 2010.
Bouimetarhan, I., Marret, F., Dupont, L., and Zonneveld, K.: Dinoflagellate cyst distribution in marine surface sediments off West Africa (17–6° N) in relation to sea-surface conditions, freshwater input and seasonal coastal upwelling, Mar. Micropaleontol., 71, 113–130, https://doi.org/10.1016/j.marmicro.2009.02.001, 2009.
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