Where: Ruvuma, Tanzania (10.4° S, 35.0° E: paleocoordinates 53.8° S, 22.6° E)

• coordinate estimated from map

• outcrop-level geographic resolution

When: Cynognathus Assemblage Zone Subzone C other 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; siliciclastic sediments

Size class: macrofossils

Collected by BMNH - University of London joint palaeontological expedition in 1963; reposited in the BMNH

Primary reference: A. W. Crompton. 1972. Postcanine occlusion in cynodonts and tritylodontids. Bulletin of the British Museum (Natural History): Geology 21:27-71 [R. Butler/R. Butler]more details

Purpose of describing collection: taxonomic analysis

PaleoDB collection 159741: authorized by Richard Butler, entered by Richard Butler on 08.08.2014

Creative Commons license: CC BY (attribution)