Polyglyphanodontia, also known as the Borioteiioidea, is an extinct clade of Cretaceous lizards. Polyglyphanodontians were the dominant group of lizards in North America[1] and Asia[2] during the Late Cretaceous.
| Polyglyphanodontia Temporal range: Early Cretaceous-Late Cretaceous,
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| Skeleton of the polyglyphanodontian Polyglyphanodon sternbergi | |
Scientific classification 
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| Domain: | Eukaryota |
| Kingdom: | Animalia |
| Phylum: | Chordata |
| Class: | Reptilia |
| Order: | Squamata |
| Clade: | Scincogekkonomorpha |
| Clade: | †Polyglyphanodontia Alifanov, 2000 |
| Synonyms | |
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Chronology and distribution
editMost polyglyphanodontians are Late Cretaceous in age, with the highest diversity in the group being known from East Asia.[3] The oldest polyglyphanodontian, Kuwajimalla kagaensis, is known from the Early Cretaceous Kuwajima Formation of Japan.[4] Early Cretaceous South American taxon Tijubina, and possibly also Olindalacerta, might also fall within Polyglyphanodontia or be closely allied to the group, but if so, they would be two of only four Gondwanan examples of an otherwise Laurasian clade[5] (the other two, and the only unambiguous ones, being Bicuspidon hogreli from the Kem Kem Beds of Morocco and Cryptobicuspidon pachysymphysealis from the Quiricó Formation of Brazil).[6][7] The group became extinct during the end-Cretaceous extinction event, the only major terrestrial squamate group to do so.[3]
Ecology
editPolyglyphanodontians 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]
Classification
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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]
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References
edit- ^ Longrich N. R., Bhullar A.-B. S.; et al. (2012). "Mass extinction of lizards and snakes at the Cretaceous-Paleogene boundary". Proceedings of the National Academy of Sciences. 109 (52): 21396–21401. Bibcode:2012PNAS..10921396L. doi:10.1073/pnas.1211526110. PMC 3535637. PMID 23236177.
- ^ 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.
- ^ a b c d Xing, Lida; Niu, Kecheng; Evans, Susan E. (January 2023). "A new polyglyphanodontian lizard with a complete lower temporal bar from the Upper Cretaceous of southern China". Journal of Systematic Palaeontology. 21 (1). doi:10.1080/14772019.2023.2281494. ISSN 1477-2019.
- ^ Susan E. Evans & Makoto Manabe (2008). "An early herbivorous lizard from the Lower Cretaceous of Japan". Palaeontology. 51 (2): 487–498. doi:10.1111/j.1475-4983.2008.00759.x.
- ^ 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. S2CID 84446189.
- ^ Romain Vullo; Jean-Claude Rage (2018). "The first Gondwanan borioteiioid lizard and the mid-Cretaceous dispersal event between North America and Africa". The Science of Nature. 105 (11–12): Article 61. Bibcode:2018SciNa.105...61V. doi:10.1007/s00114-018-1588-3. PMID 30291449. S2CID 52924052.
- ^ 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.