Modderdrift farm: Wordian, South Africa

List of taxa
Where & when
Geology
Taphonomy & methods
Metadata & references
Taxonomic list
Anomodontia
Eodicynodon oosthuizeni Barry 1974
Rubidge et al. 1994 2 specimens
NMQR 2991, 3153; all are postcranial remains "found associated with cranial material and we can therefore be confident of the generic identification"; furthermore, the authors explicitly say that the remains represent the species E. oosthuizeni
Tapinocephalidae
Tapinocaninus pamelae Rubidge 1991
Rubidge 1991
NMQR 2987, NMQR 2985, NMQR 2986, ROZ K95
Therocephalia - Scylacosauridae
Ictidosaurus angusticeps Broom 1903
1 individual
NMQR 2910, partial skull, lacking the occiput and posterior skull roof
Glanosuchus macrops Broom 1904
1 individual
NMQR 2908, much of the antorbital portion of a skull incl. mandible
see common names

Geography
Country:South Africa State/province:Western Cape County:Prince Albert
Coordinates: 33.1° South, 22.5° East (view map)
Paleocoordinates:60.3° South, 37.7° West
Basis of coordinate:based on nearby landmark
Geographic resolution:small collection
Time
Period:Permian Epoch:Guadalupian
Stage:Wordian 10 m.y. bin:Permian 4
Key time interval:Wordian Zone: Eodicynodon Assemblage
Age range of interval:266.90000 - 264.28000 m.y. ago
Stratigraphy
Geological group:Beaufort Formation:Abrahamskraal
Stratigraphic resolution:bed
Stratigraphy comments: "The outcrops on Modderdrift are assigned to the Eodicynodon AZ, which is part of the Abrahamskraal Formation, Beaufort Group, Karoo Supergroup; Middle Permian. [...] Considering the geologic time scale proposed by the International Commission of Stratigraphy (Gradstein and Ogg 2004), we follow Catuneanu et al. (2005) and Rubidge (2005) who assign a Wordian age to this assemblage zone." (Abdala et al., 2008).
Lithology and environment
Primary lithology:nodular calcareous not reported
Secondary lithology: siltstone
Includes fossils?Y
Lithology description: "The specimens were discovered in pedogenic calcareous nodular layers within siltstone successions below the first maroon mudrock of the Abrahamskraal Formation. These rocks are considered to have been deposited in a subaerial delta plain depositional environment (Rubidge 1995; Rubidge et al. 2000)." (Abdala et al., 2008).
Environment:delta plain Tectonic setting:foreland basin
Glacial or sequence phase:regressive
Geology comments: Rubidge et al. (2000, S. Afr. J. Geol. 103(1)) interpret the basal Abrahamskraal Fm. as non-marine part of a second-order highstand systems tract.
Taphonomy
Modes of preservation:body
Size of fossils:macrofossils
Collection methods and comments
Collection methods:mechanical,survey of museum collection
Reason for describing collection:taxonomic analysis
Collection method comments: Specimens were briefly described by Rubidge et al. (1983, Nav. Nas. Mus. 4).
NMQR = National Museum, Bloemfontein, South Africa
Metadata
Also known as:Modderdrift vertebrates
Database number:94649
Authorizer:J. Mueller, J. Falconnet Enterer:T. Liebrecht, J. Falconnet
Modifier:J. Falconnet Research group:vertebrate
Created:2010-03-05 07:30:19 Last modified:2023-06-10 14:52:50
Access level:the public Released:2010-03-05 07:30:19
Creative Commons license:CC BY
Reference information

Primary reference:

32224. F. Abdala, B. S. Rubidge, and J. Heever. 2008. The Oldest Therocephalians (Therapsida, Eutheriodonta) and the Early Diversification of Therapsida. Palaeontology 51(4):1011-1024 [J. Mueller/T. Liebrecht]

Secondary references:

65044 B. S. Rubidge. 1991. A new primitive dinocephalian mammal-like reptile from the Permian of southern Africa. Palaeontology 34:547-559 [G. Lloyd/G. Lloyd]
32298 B. S. Rubidge, G. M. King, and J. P. Hancox. 1994. The Postcranial Skeleton of the Earliest Dicynodont Synapsid Eodicynodon from the Upper Permian of South Africa. Palaeontology 37(2):397-408 [J. Mueller/T. Liebrecht]