N slopes, Etjo Mtn, btwn lower + middle arenaceous layers: Anisian, Namibia
collected by Keyser
List of taxa
Where & when
Geology
Taphonomy & methods
Metadata & references
Taxonomic list
Anomodontia
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1 specimen | ||||||||||
R313, skull | ||||||||||
Renaut et al. 2003 | ||||||||||
Rhopalorhinus etionensis n. gen., n. sp.
Keyser 1973
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1 specimen | |||||||||
R320, skull | ||||||||||
see common names |
Geography
Country: | Namibia |
Coordinates: | 21.1° South, 16.5° East (view map) |
Paleocoordinates: | 37.5° South, 6.3° West (Wright 2013) |
Basis of coordinate: | estimated from map |
Geographic resolution: | local area |
Time
Period: | Triassic | Epoch: | Middle Triassic |
Stage: | Anisian | 10 m.y. bin: | Triassic 2 |
Key time interval: | Anisian | Other zone: | Cynognathus subzone B |
Age range of interval: | 246.7 - 241.464 m.y. ago |
Stratigraphy
Geological group: | Karoo | Formation: | Omingonde | ||
Stratigraphic resolution: | group of beds | ||||
Stratigraphy comments: Referred to as the "Lower Etjo Beds" by Keyser (1973) but now called the Omingonde Formation. "Based on the co-occurrence of Kannemeyeria and Erythrosuchus in subzone B of the Cynognathus Assemblage Zone, the Omingonde Formation may be broadly assigned an Anisian age." (Damiani et al. 2007. Palaeontology 50: 1531-1546)
Abdala & Smith (2009) suggest the possibility of two different faunas in the upper Omingonde Formation; an older one corresponding to Cynognathus Subzone B and the upper possibly to Cynognathus Subzone C. On the basis of the presence of Chiniquodon in the upper fauna, Abdala & Smith (2009) tentatively suggested that the Omingonde could extend into the early Ladinian. Dolichuranus was suggested by Abdala & Smith (2009) to come from the older fauna, and would therefore be early Anisian in age. |
Lithology and environment
Primary lithology: | nodular "shale" | ||
Includes fossils? | Y | ||
Environment: | terrestrial indet. | Tectonic setting: | rift |
Taphonomy
Modes of preservation: | body |
Size of fossils: | macrofossils |
Preservation of anatomical detail: | good |
Temporal resolution: | snapshot |
Collection methods and comments
Collection methods: | field collection |
Reason for describing collection: | taxonomic analysis |
Collectors: | Keyser |
Collection method comments: Specimens in the collections of the Geological Survey of South Africa, Pretoria |
Metadata
Database number: | 99453 | ||
Authorizer: | R. Butler | Enterer: | R. Butler |
Modifier: | R. Butler | Research group: | vertebrate |
Created: | 2010-11-11 23:24:00 | Last modified: | 2025-02-22 15:12:02 |
Access level: | the public | Released: | 2010-11-11 23:24:00 |
Creative Commons license: | CC0 |
Reference information
Primary reference:
34203. | A. W. Keyser. 1973. A new Triassic vertebrate fauna from South West Africa. Palaeontologia africana 16:1-15 [R. Butler/R. Butler] |
Secondary references:
34212 | F. Abdala and R. M. H. Smith. 2009. A Middle Triassic cynodont fauna from Namibia and its implications for the biogeography of Gondwana. Journal of Vertebrate Paleontology 29:837-851 [R. Butler/R. Butler] | |
62280 | A. J. Renaut, R. J. Damiani, A. M. Yates and P. J. Hancox. 2003. A taxonomic note concerning a dicynodont (Synapsida: Anomodontia) from the Middle Triassic of East Africa. Palaeontologia africana 39:93-94 [R. Butler/R. Butler] | |
34213 | R. M. H. Smith and R. Swart. 2002. Changing fluvial environments and vertebrate taphonomy in response to climatic drying in a mid-Triassic rift valley fill: the Omingonde Formation (Karoo Supergroup) of central Namibia. Palaios 17:249-267 [R. Butler/R. Butler] |