Also known as type locality of Barasaurus besairiei; Morondava Basin
Where: Fianarantsoa, Madagascar (22.6° S, 45.4° E: paleocoordinates 52.4° S, 27.8° E)
• coordinate based on nearby landmark
• small collection-level geographic resolution
When: Lower Sakamena Formation (Sakamena Group), Lopingian (259.9 - 252.2 Ma)
• The Lower Sakamena Fm. is generally accepted to be of Upper Permian age (see, e.g., discussion in Carroll, 1981, Phil. Trans. R. Soc. Lond. B 293 and Smith, 2000, Paleont. Afr. 36).
• group of beds-level stratigraphic resolution
Environment/lithology: paralic; fine-grained, concretionary, sandy shale
•"There is no evidence of the environment having been anaerobic [...] " (ibidem, p. 339).
•Smith (2000) favoures a purely lacustrine origin for the Lower Sakamena of SW Madagascar. The beds dominated by Barasaurus are considered as lacustrine "offshore" facies (Smith, 2000).
Size class: macrofossils
Preservation: mold/impression, concretion
Collected by H. Besairie; reposited in the MNHN
Primary reference: J. Piveteau. 1955. Existence d’un Reptile du groupe des Procolophonidés à Madagascar - Conséquences stratigraphiques et paléontologiques. Comptes Rendus Hebdomadaires des Séances de l’Academie des Sciences 241:1325-1327 [J. Mueller/T. Liebrecht]more details
Purpose of describing collection: taxonomic analysis
PaleoDB collection 92491: authorized by Johannes Mueller, entered by Torsten Liebrecht on 16.11.2009
Creative Commons license: CC BY (attribution)
Taxonomic list
Reptilia | |
Barasaurus besairiei n. gen. n. sp.
Barasaurus besairiei n. gen. n. sp. Piveteau 1955 parareptile reposited in the MNHN Paris; numbered P1 (type) to P10 in Meckert (1995, PhD thesis)
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