. Annals of the South African Museum = Annale van die Suid-Afrikaanse Museum . 0)Sh 5b o s > to Ifi 5 8 .5? o <u o3 Q !ffl § s —, o & I as a C to ?a m J5 ! OSTEOLOGY OF ERYTHROSUCHUS AFRICANUS BROOM 9 of the Lower Triassic ( Charig & Sues 1976; Anderson & Cruickshank 1978; Sun1980), but the most recent studies ( Ochev & Shishkin 1988; Shubin & Sues 1991;Shishkin & Welman 1994; Shishkin & Ochev 1995) suggest that its vertebrate fauna isinstead consistent with a lowermost Middle Triassic age. Sediments assigned to theCynognathus Assemblage Zone in South Africa are best exposed in t
. Annals of the South African Museum = Annale van die Suid-Afrikaanse Museum . 0)Sh 5b o s > to Ifi 5 8 .5? o <u o3 Q !ffl § s —, o & I as a C to ?a m J5 ! OSTEOLOGY OF ERYTHROSUCHUS AFRICANUS BROOM 9 of the Lower Triassic ( Charig & Sues 1976; Anderson & Cruickshank 1978; Sun1980), but the most recent studies ( Ochev & Shishkin 1988; Shubin & Sues 1991;Shishkin & Welman 1994; Shishkin & Ochev 1995) suggest that its vertebrate fauna isinstead consistent with a lowermost Middle Triassic age. Sediments assigned to theCynognathus Assemblage Zone in South Africa are best exposed in the south-westernFree State and northern part of the extreme Eastern Cape Province (Kitching 1977).Recently, Welman et al. (1991) have also discovered vertebrate-bearing CynognathusAssemblage Zone deposits in the north-eastern Free State. Erythrosuchus africanusspecimens have been collected from a number of the best-known localities (Kitching1977). The holotype originates from Oorlogsfontein, Aliwal North, whereas the othe
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Keywords: ., bookcentury1800, bookdecade1890, booki, booksubjectnaturalhistory
