Abstract
Located within the continental red beds of the upper Elliot Formation (Eastern Cape, South Africa), the Lower Jurassic Pronksberg bentonite is in close proximity to the boundary between the Triassic and Jurassic, which coincides with one of Earth’s largest mass extinction events. Sedimentological, mineralogical, and major and trace element geochemical data indicates that: (1) the bentonite formed by devitrification of felsic volcanic ash; (2) the deposit was reworked by gentle currents in an ephemeral lake where intense chemical weathering of the volcanic ash occurred; and (3) the source of the original felsic volcanic material was probably in southwest Gondwana (now South America) where explosive silicic igneous activity has been documented not only in the Permian, but also in the Late Triassic and Early Jurassic.
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Acknowledgements
Most of all, we would like to thank Goonie Marsh for the countless stimulating discussions. Our special thanks go to our friends and colleagues Rugshana Daniels, Blair McPhee and Lara Sciscio for field and lab assistance. Albert and Susanna Roodt are acknowledged for graciously allowing us access to the abandoned bentonite pits on Pronksberg. We thank Chris Harris and Agnes Odri for improving an earlier version of the manuscript, and reviewers Jurie Viljoen and Maarten de Wit for their constructive comments. The financial support of the National Research Foundation of South Africa via its African Origins Platform and Completive Program for Rated Researches grants (#82606, #93544) to EMB is hereby acknowledged. Opinions expressed and conclusions arrived at are those of the authors only.
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Bordy, E.M., Abrahams, M. (2016). Geochemistry of the Pronksberg Bentonite of the Upper Elliot Formation (Early Jurassic), Eastern Cape, South Africa. In: Linol, B., de Wit, M. (eds) Origin and Evolution of the Cape Mountains and Karoo Basin. Regional Geology Reviews. Springer, Cham. https://doi.org/10.1007/978-3-319-40859-0_12
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