The
type specimens,
syntypes SAM-PK-3449 and SAM-PK-3450, were discovered, described and named in 1924 by
Sidney H. Haughton. They were collected from the Triassic Lower
Elliot Formation, dating to the early
Norian, on the north slope of the Thaba 'Nyama (Black Mountain) in
Transkei, South Africa. In 2024,
Melanorosaurus was redescribed and SAM-PK-3449 was designated the
lectotype of the species. However, SAM-PK-3450 differs in many aspects from SAM-PK-3449 so was excluded from
Melanorosaurus, representing a probable sauropodomorph. Haughton also referred SAM-PK-3532 to
Melanorosaurus, a partial skeleton discovered from a different locality than the lectotype. Nevertheless, it too differs from the lectotype in aspects of the ulna and ilium, thus it can only be regarded an indeterminate sauropodomorph for now. In 1985, Peter Galton suggested the referral of NMQR 1551, an exemplar of the postcranial remains of two individuals to
M. readi, and in 2024, this was considered a strong possibility due to similarities with the lectotype specimen. However, the authors stressed that a detailed reassessment of the material was necessary before any formal referrals were to be made. However, this specimen comes from the Upper Elliot, unlike the
Melanorosaurus type material and NM QR1551, rendering its referral to the genus untenable.
Melanorosaurus thabanensis was named in 1993 by Gauffre, based on
holotype MNHN LES-16, a
femur found in the Upper Triassic lower Elliot Formation. However, a recent review of the material demonstrated that the femur, along with six other bones, can't be referred to the genus
Melanorosaurus, and a new combination (
Meroktenos thabanensis) was created. == Classification ==