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Bruce S. Rubidge

Researcher at University of the Witwatersrand

Publications -  156
Citations -  5379

Bruce S. Rubidge is an academic researcher from University of the Witwatersrand. The author has contributed to research in topics: Beaufort Group & Permian. The author has an hindex of 36, co-authored 150 publications receiving 4740 citations. Previous affiliations of Bruce S. Rubidge include DST Systems.

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The Karoo basins of south-central Africa

TL;DR: In this paper, the authors focus on the Karoo basins sensu stricto of south-central Africa, synthesizing their sedimentological and stratigraphic features in relation to the tectonic and climatic controls on accommodation and sedimentation.
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27th Du Toit Memorial LectureRe-uniting lost continents – Fossil reptiles from the ancient Karoo and their wanderlust

TL;DR: In particular, the enormous palaeontological wealth of the Karoo, covering a period of almost 100 million years from the Permian to the Jurassic, has enhanced understanding of the evolution of important tetrapod lineages, including mammals and dinosaurs as discussed by the authors.
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A lamprey from the Devonian period of South Africa

TL;DR: A marine/estuarine fossil lamprey from the Famennian (Late Devonian) of South Africa is reported, the identity of which is established easily because many of the key specializations of modern forms are already in place, evidence that agnathans close to modern lampreys had evolved before the end of the Devonian period.
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High-precision temporal calibration of Late Permian vertebrate biostratigraphy: U-Pb zircon constraints from the Karoo Supergroup, South Africa

TL;DR: The authors used U-Pb zircon isotope dilution-thermal ionization mass spectrometry (ID-TIMS) dates for five volcanic ashes interbedded with fossils from the Pristerognathus, Tropidostoma, and Cistecephalus vertebrate biozones of the Beaufort Group.
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Evolutionary Patterns Among Permo-Triassic Therapsids *

TL;DR: Synapsids form the bulk of tetrapod diversity from Early Permian to Middle Triassic times and thus can provide critical information on the nature of the Permo-Triassic extinction in the terrestrial realm.