Where: Ruvuma, Tanzania (10.3° S, 35.3° E: paleocoordinates 53.8° S, 23.2° E)
• coordinate estimated from map
• outcrop-level geographic resolution
When: Cynognathus Subzone C zone, Lifua Member (Manda Beds Formation), Anisian (247.2 - 242.0 Ma)
• Lifua Member of the Manda beds is "correlated with Subzone C of the Cynognathus Assemblage Zone. This correlation was based on the shared occurrences of the dicynodont Angonisaurus and the cynodonts Diademodon and Cricodon. Subzone C of the Cynognathus Assemblage Zone is suggested to be late Anisian. The Rio Mendoza Formation of Argentina correlates with Subzone C of the Cynognathus Assemblage Zone(Rubidge 2005), and thus the Lifua Member of the Manda Beds. The top of the Rio Mendoza Formation has been dated at 243 ± 5 Ma (Avila et al. 2006), which is consistent with the Anisian age as predicted by biostratigraphy." (Nesbitt et al. 2010: Nature 464:95-98)
• group of beds-level stratigraphic resolution
Environment/lithology: fluvial-lacustrine; sandstone and marl
Size class: macrofossils
Collected by Parrington in 1932; reposited in the BMNH
Primary reference: A. J. Charig. 1967. Archosauria. In W. B. Harland (ed.), The Fossil Record: A Symposium with Documentation. Geological Society of London Special Publication 2:703-718 [M. Carrano/M. Carrano]more details
Purpose of describing collection: taxonomic analysis
PaleoDB collection 194380: authorized by Richard Butler, entered by Richard Butler on 19.06.2018
Creative Commons license: CC BY (attribution)
Taxonomic list
Reptilia | |
Archosauromorpha indet. Huene 1946 archosauromorph | |
Stenaulorhynchus sp. Haughton 1932 rhynchosaur | |
Mandasuchus tanyauchen n. gen. n. sp.
Mandasuchus tanyauchen n. gen. n. sp. Charig 1967 archosaur NHMUK PV R6792 (holotype), partial skeleton. NHMUK PV R6793, partial skeleton.
| |
Osteichthyes | |
Tetragonias njalilus von Huene 1942 dicynodont |