Anguimorpha

Georgalis, Georgios L., Čerňanský, Andrej & Klembara, Jozef, 2021, Osteological atlas of new lizards from the Phosphorites du Quercy (France), based on historical, forgotten, fossil material, Geodiversitas 43 (9), pp. 219-293 : 270-271

publication ID

https://doi.org/ 10.5252/geodiversitas2021v43a9

publication LSID

urn:lsid:zoobank.org:pub:11D0D852-39D7-449C-9EB3-C3D804114556

DOI

https://doi.org/10.5281/zenodo.4721483

persistent identifier

https://treatment.plazi.org/id/03A1633B-FF96-FFF7-3169-F92AFBDC3FE6

treatment provided by

Felipe

scientific name

Anguimorpha
status

 

Anguimorpha indet.

( Figs 61 View FIG ; 62 View FIG )

REFERRED SPECIMENS. — Five presacral vertebrae (NHMW 2019/0046/0003- NHMW 2019/0046/0007); a partial pectoral girdle (NHMW 2019/0095/0001).

DESCRIPTION AND REMARKS

Presacral vertebrae ( Fig. 61 View FIG )

These vertebrae are relatively large ( Fig. 61 View FIG ), with centrum lengths ranging between 6.9 and 9.3 mm (see Appendix 1).

The vertebrae demonstrate a mix of several features present in the above described specimens of Placosaurus , Anguinae indet., and Palaeovaranus . They have high neural spines, depressed cotyle and condyle, while the ventral surface of their centra is crossed by a wide surface or groove that is unlike the conditions seen above for the other taxa ( Fig. 61 View FIG ). Considering the high intracolumnar variation observed in the vertebrae of extant lizards (e.g., Pseudopus ), we are reluctant in assigning these specimens in a more precise taxonomic rank and we cannot even exclude that they (or part of them) pertain to some of the above described taxa.

Pectoral girdle NHMW 2019/0095/0001 ( Fig. 62 View FIG )

This specimen is incomplete, though preserving in relatively good state the right scapulocoracoid. The glenoid fossa is visible, well demarking the point of attachment with the humerus. Anteriorly to the glenoid fossa, lies the coracoid foramen. Dorsally to the foramen, the scapulocoracoid is of rectangular shape and is dorsoventrally elongated. The ventral portion of the element is anteroposteriorly elongated.

It is readily obvious that this specimen apparently pertains to a rather large-sized lizard. Considering our currently inadequate state of knowledge of the appendicular skeleton of Paleogene European lizards, it is impossible to associate it with any of the above described glyptosaurines, palaeovaranids, and varanids, all of which could attain a considerably large size.

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