Tikitherium is an extinct genus of from India, known from a single upper tooth. Originally argued to be a primitive mammaliaform from the Late Triassic, a 2024 study argued that it actually represented the remains of a shrew from the Neogene.[Datta, P.M. 2005. Earliest Mammal with Transversely Expanded Upper Molar from the Late Triassic (Carnian) Tiki Formation, South Rewa Gondwana Basin, India. Journal of Vertebrate Paleontology. 25(1):200-207.]
History and discovery
Tikitherium copei was first described by Datta in 2005. The first and only specimen is an upper tooth that was thought to have discovered in the lower part of the Late Triassic
Tiki Formation, located in the South Rewa Gondwana Basin,
India. Both the genus
Tikitherium and the species
copei were named by Datta in 2005. The currently only known specimen was deposited in the Paleontology Division of the Geological Survey of India, Calcutta.
Although only a single tooth was found, it showed several derived features that are similar to other early mammalian dentitions, but further detailed comparisons showed the various differences that allowed this tooth to specifically stand out on its own.
Classification
Tikitherium is considered to be mammal based on Datta (2005).
However, the phylogeny based on Luo and Martin (2007) places
Tikitherium and
Docodonta as sister taxa, which are Mammaliformes, based on the shared traits of wear facets and platform on the lingual side of the molars. Although Luo and Martin conclude that
Tikitherium and Docodonta are the most closely related, it is debated that
Woutersia instead may be the sister taxa to Docodonta due to the similarity of their prominent lingual cusps.
A 2024 study argued that the tooth was actually the upper fourth premolar of a shrew belonging to the subfamily Crocidurinae, and actually dated to the Neogene rather than the Late Triassic as had previously been supposed. The authors suggested that T. copei "likely represents a distinct taxon at least at the species level. However, as the validity of T. copei is not certain, Pal/CHQ-009, the holotype of T. copei, should be currently identified as Crocidurinae gen. et sp. indet."
Description
Tikitherium is only known from a single upper tooth, originally argued to be a left molar but currently thought to be a right fourth premolar. The tooth closely resembles members of the modern shrew subfamily Crocidurinae in having a "short horseshoe-shaped
protocone", and the
hypocone being absent. The tooth is broadly similar to those of species of
Suncus. It differs from modern members of Crocidurinae by "a more massive central cusp (paracone) and a more obtuse angle between the paracone axis and the lingual lobe.", which are likely
plesiomorphic features.
Geological and paleoenvironment
Tikitherium was previously thought to have originated from the
Tiki Formation, which is well known for its
Late Triassic vertebrates. However, it has since been argued that
Tikitherium actually was found in reworked sediments derived from erosion of the Tiki Formation that formed much later during the Neogene. A similar issue was previously reported with
Tikiguania which was also previously interpreted as coming from the Tiki Formation, and thus the oldest known squamate, but was later interpreted as modern
agamid lizard coming from Neogene or
Quaternary deposits.
