Spalacotherium evansae Ensom & Sigogneau-Russell, 2000

Allain, Ronan, Vullo, Romain, Rozada, Lee, Anquetin, Jérémy, Bourgeais, Renaud, Goedert, Jean, Lasseron, Maxime, Martin, Jeremy E., Pérez-García, Adán, Fabrègues, Claire Peyre De, Royo-Torres, Rafael, Augier, Dominique & Bailly, Gilles, 2022, Vertebrate paleobiodiversity of the Early Cretaceous (Berriasian) Angeac-Charente Lagerstätte (southwestern France): implications for continental faunal turnover at the J / K boundary, Geodiversitas 44 (25), pp. 683-752 : 730

publication ID

https://doi.org/ 10.5252/geodiversitas2022v44a25

publication LSID

urn:lsid:zoobank.org:pub:EA12DCB7-A5BE-4763-B805-25087EBD726D

DOI

https://doi.org/10.5281/zenodo.6928946

persistent identifier

https://treatment.plazi.org/id/03C887B9-FF87-FFDA-7678-A30EFA74FB9E

treatment provided by

Felipe

scientific name

Spalacotherium evansae Ensom & Sigogneau-Russell, 2000
status

 

Spalacotherium evansae Ensom & Sigogneau-Russell, 2000

( Fig. 34A, B View FIG )

DESCRIPTION

Three teeth of Spalacotheriidae have been recognized including two molars, which have the characteristic “symmetrodont” pattern with acute angulation of the principal cusps, seen in other spalacotheriids ( Fig. 34A View FIG ; Kielan-Jaworowska et al. 2004). The best preserved of the molars ANG M-26 lacks the posterior root and the hypoconulid (cusp d) ( Fig. 34A, B View FIG ). The protoconid, the metaconid and the paraconid are welldeveloped. The talonid was probably much reduced. Mesially, a single cusp e is lingually placed on the cingulid ( Fig. 34B View FIG ), and allows the identification of this tooth as a left lower molar. ANG M-26 is very similar, if not identical, to a tooth referred to Spalacotherium evansae (DORC GS 360, Ensom & Sigogneau-Russell 2000). Its smaller size compared to that of the molars of other species of Spalacotherium , the incompleteness of the labial cingulid associated with the equivalent height of the paraconid and metaconid, are diagnostic features (Ensom & Sigogneau-Russell 2000), that allow us to assign this specimen to Spalacotherium evansae . The latter species has been decribed from various localities of the Purbeck Group, including the Berriasian Lulworth Formation at Sunnydown Farm, U.K.

GBIF Dataset (for parent article) Darwin Core Archive (for parent article) View in SIBiLS Plain XML RDF