Rechni, Compsocerops holotype (Triassic of India)

Where: Andhra Pradesh, India (19.3° N, 79.5° E: paleocoordinates 33.1° S, 36.4° E)

• coordinate based on nearby landmark

• outcrop-level geographic resolution

When: Upper Member (Maleri Formation), Norian (228.0 - 208.5 Ma)

• The upper Maleri Formation overlies the lower Maleri and underlies the lower Dharmaram Formation. The underlying lower Maleri Formation has been correlated on the basis of vertebrate biostratigraphy with the Scaphonyx-Exaeretodon-Herrerasaurus biozone of the Ischigualasto Formation of Argentina and the Hyperodapedon Assemblage Zone of the Santa Maria Formation of Brazil (e.g. Novas et al. 2011. Earth Env. Sci. Trans. Roy. Soc. Edin. 101:333-349). The relevant part of the Ischigualasto Formation has been dated as late Carnian in age on radioisotopic data (e.g. Martinez et al. 2011. Science 331: 206-210), and the lower Maleri Formation is commonly considered equivalent in age. As a result, the overlying upper Maleri is likely Norian in age.

• group of beds-level stratigraphic resolution

Environment/lithology: terrestrial; lithology not reported

Size class: macrofossils

Collection methods: surface (float), surface (in situ),

• ISI: Indian Statistical Institute, Calcutta

Primary reference: D. P. Sengupta. 1995. Chigutisaurid temnospondyls from the Late Triassic of India and a review of the Family Chigutisauridae. Palaeontology 38(2):313-339 [R. Butler/R. Butler]more details

Purpose of describing collection: taxonomic analysis

PaleoDB collection 136904: authorized by Richard Butler, entered by Richard Butler on 06.12.2012

Creative Commons license: CC BY (attribution)

Taxonomic list

Amphibia
 Temnospondyli - Chigutisauridae
Kuttycephalus triangularis n. gen. n. sp., Compsocerops cosgriffi n. gen. n. sp.
Kuttycephalus triangularis n. gen. n. sp. Sengupta 1995 tetrapod
ISI A 50 (holotype), complete skull. ISI A 51, 52
Compsocerops cosgriffi n. gen. n. sp. Sengupta 1995 tetrapod
ISI A 33, complete skull