The Black Rock to Rooinekke area has been influenced by the Kheis and Namaqua orogenies. Thrusting associated with the Kheis orogeny is well documented throughout the mining area. Thrusting at Rooinekke resulted in the Griqualand West Sequence rocks overlying parts of the Olifantshoek Sequence. At Black Rock lithologies of the Vo~lwater Subgroup have been thrusted onto the Olifantshoek Sequence. A prominent N-S trending graben structure has been observed in the Rooinekke, Beeshoek and Black Rock mining areas. The thrusts are disrupted by these N-S faults. At Rooinekke supergene replacement and enrichment of the iron ore is associated with pre-Olifantshoek N-S faulting. The Namaqua orogeny may also have played a part in upgrading the existing ore bodies under discussion.
The Permian–Triassic global crisis was the only event to have a dramatic impact on insect diversity, with Palaeozoic insect clades disappearing and accompanied by the accelerated rise of modern lineages. To date, most Permian palaeoentomological work has focused on the upper Permian deposits of the Normandien Formation (Beaufort Group), KwaZulu–Natal Province. This paper describes the regional insect fauna preserved close to the Permian–Triassic boundary at Wapadsberg Pass, southern Karoo Basin of South Africa, which provides a rare glimpse into insect life immediately before this global crisis. Here, we describe six insect species from six families within five orders from the two Wapadsberg Pass localities. Mioloptera stuckenbergi (Grylloblattodea) and Permocicada sp. (Hemiptera) were recorded previously from the Lopingian KwaZulu–Natal Province. In addition, we detail the first potential occurrence of South African Permian Tettigoniida (Orthoptera: Tettigonioidea & Hagloidea) and Anthracoptilidae (Paoliida). An Auchenorrhynchan (Hemiptera) nymph and an undetermined insect (order uncertain) also are described.
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