Polyglyphanodontia, also known as the Borioteiioidea, is an extinct clade of Cretaceouslizards. Polyglyphanodontians were the dominant group of lizards in North America[1] and Asia[2] during the Late Cretaceous.
Polyglyphanodontians were morphologically diverse. Chamopsiids, including Chamops, from North America have tricuspid teeth, and were generally small in size. Members of the family Polyglyphanodontidae primarily known from Europe and North America (including Polyglyphanodon, Paraglyphanodon, Dicodon and Bicuspidon) have large teeth that are transversely orientated, and were likely herbivorous as well as possibly ominivorous. The family Gilmoreteiidae have iguana-like teeth, with some polyglyphanodontians known from Asia having conical teeth. Some gilmoreteiids developed a complete lower temporal bar similar to that found in the tuatara, but is otherwise unheard of in lizards.[3]
The classification of Polyglyphanodontia is contentious. They have been considered to be either most closely related to Teiioidea, or to Iguania, with both positions having been supported in recent studies. Cladogram after Xida, Niu and Evans, 2023.[3]
^Gao K.; Hou L. (1996). "Systematics and taxonomic diversity of squamates from the Upper Cretaceous Djadochta Formation, Bayan Mandahu, Gobi Desert, People's Republic of China". Canadian Journal of Earth Sciences. 33 (4): 578–598. Bibcode:1996CaJES..33..578G. doi:10.1139/e96-043.
^Tiago R. Simões, Michael W. Caldwell and Alexander W. A. Kellner (2015). "A new Early Cretaceous lizard species from Brazil, and the phylogenetic position of the oldest known South American squamates". Journal of Systematic Palaeontology. 13 (7): 601–614. doi:10.1080/14772019.2014.947342. S2CID84446189.
^Carvalho, J. C.; Santucci, R. M. (2023). "A new fossil Squamata from the Quiricó Formation (Lower Cretaceous), Sanfranciscana Basin, Minas Gerais, Brazil". Cretaceous Research. 105717. doi:10.1016/j.cretres.2023.105717.
