Lepidosauromorpha (in PhyloCode known as Pan-Lepidosauria[2][3]) is a group of reptiles comprising all diapsids closer to lizards than to archosaurs (which include crocodiles and birds). The only living sub-group is the Lepidosauria, which contains two subdivisions, Squamata, which contains lizards and snakes, and Rhynchocephalia, the only extant species of which is the tuatara.
| Lepidosauromorphs | |
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| Skull of Sophineta cracoviensis | |
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| Collage of five lepidosaurs. From top left to right: Sphenodon punctatus, Dendroaspis polylepis, Iguana iguana, Smaug breyeri and Malayopython reticulatus. | |
Scientific classification 
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| Domain: | Eukaryota |
| Kingdom: | Animalia |
| Phylum: | Chordata |
| Class: | Reptilia |
| Clade: | Sauria |
| Clade: | Lepidosauromorpha Benton, 1983 |
| Subgroups | |
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see text. | |
| Synonyms | |
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Lepidosauromorphs are distinguishable from archosauromorphs (reptiles closer to archosaurs) by their primitive sprawling gait (allowing for the same sinusoidal trunk and tail movement seen in fish), the sliding "joint" between the coracoids and the sternum (for a longer stride), and their pleurodont dentition. In contrast, Archosauromorphs possess a parasagittal gait, a reduction in their dermal girdle, a reduction and/or loss of the sternum, and a more thecodont dentition. Living lepidosauromorphs have retained an ectothermic ("cold blooded") metabolism, unlike the ancestral condition in archosauromorphs.
While some putative stem-lepidosauromorphs like Palaeagama are known from the Late Permian, the oldest definitive lepidosauromorphs, Sophineta and Paliguana, are known from the Early Triassic.[4][5] Taytalura from the early Late Triassic of Argentina is the most complete fossil of an early lepidosauromorph and is one of the few fossils robustly inferred as an early evolving lepidosauromorph.[6] The Kuehneosauridae, a family of reptiles with elongated ribs which allowed them to glide akin to living gliding lizards have been historically typically considered early lepidosauromorphs. However, several recent studies have been found them in other positions within Sauria, including Archosauromorpha.[7] Almost all non-lepidosaurian lepidosauromorphs became extinct by the end of the Triassic, the with the latest non lepidosaur-lepidosauromorphs being Marmoretta from the Middle Jurassic of Britain and an indeterminate form from the Middle Jurassic Moskvoretskaya Formation of Russia, which appear to be closely related to Fraxinisaura from the Middle Triassic of Germany.[5][8][9] Other studies have recovered Marmoretta as a stem-squamate.[10]
Subgroups
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References
edit- ^ Jones, M. E.; Anderson, C.; Hipsley, C. A.; Müller, J.; Evans, S. E.; Schoch, R. R. (2013). "Integration of molecules and new fossils supports a Triassic origin for Lepidosauria (lizards, snakes, and tuatara)". BMC Evolutionary Biology. 13: 208. doi:10.1186/1471-2148-13-208. PMC 4016551. PMID 24063680.
- ^ de Queiroz, K.; Cantino, P. D.; Gauthier, J. A., eds. (2020). "Pan-Lepidosauria J. A. Gauthier and K. de Queiroz, new clade name". Phylonyms: A Companion to the PhyloCode. Boca Raton: CRC Press. pp. 1075–1078. ISBN 978-1-138-33293-5.
- ^ "Pan-Lepidosauria". RegNum.
- ^ Susan E. Evans and Magdalena Borsuk−Białynicka (2009). "A small lepidosauromorph reptile from the Early Triassic of Poland" (PDF). Paleontologica Polonica. 65: 179–202.
- ^ a b Ford, David P.; Evans, Susan E.; Choiniere, Jonah N.; Fernandez, Vincent; Benson, Roger B. J. (2021-08-25). "A reassessment of the enigmatic diapsid Paliguana whitei and the early history of Lepidosauromorpha". Proceedings of the Royal Society B: Biological Sciences. 288 (1957): 20211084. doi:10.1098/rspb.2021.1084. PMC 8385343. PMID 34428965.
- ^ Martínez, Ricardo N.; Simões, Tiago R.; Sobral, Gabriela; Apesteguía, Sebastián (2021-08-25). "A Triassic stem lepidosaur illuminates the origin of lizard-like reptiles". Nature. 597 (7875): 235–238. doi:10.1038/s41586-021-03834-3. ISSN 1476-4687. PMID 34433961. S2CID 237307957.
- ^ Queiroz, Kevin de; Cantino, Philip D.; Gauthier, Jacques A. (2020-04-30), de Queiroz, Kevin; Cantino, Philip; Gauthier, Jacques (eds.), "Pan-Lepidosauria J. A. Gauthier and K. de Queiroz, new clade name", Phylonyms (1 ed.), Boca Raton, FL: CRC Press, pp. 1075–1078, doi:10.1201/9780429446276-255, ISBN 978-0-429-44627-6, S2CID 219018618, retrieved 2021-08-22
- ^ Skutschas, Pavel P.; Sennikov, Andrey G.; Syromyatnikova, Elena V.; Vitenko, Dmitriy D.; Parakhin, Igor A.; Bapinaev, Roman A.; Evans, Susan E. (2021-06-09). "A lepidosauromorph specimen from the Middle Jurassic (Bathonian) Moskvoretskaya Formation of the Moscow Region, Russia". Historical Biology. 34 (3): 566–570. doi:10.1080/08912963.2021.1935921. ISSN 0891-2963. S2CID 236282947.
- ^ Griffiths, E.; Ford, D. P.; Benson, R.; Evans, S. E. (2021). "New information on the Jurassic lepidosauromorph Marmoretta oxoniensis". Palaeontology. ISSN 0031-0239.
- ^ Simōes, Tiago R.; Caldwell, Michael W.; Talanda, Mateusz; Bernardi, Massimo; Palci, Alessandro; Vernygora, Oksana; Bernardini, Federico; Mancini, Lucia; Nydam, Randall L. (30 May 2018). "The origin of squamates revealed by a Middle Triassic lizard from the Italian Alps". Nature. 557 (7707): 706–709. Bibcode:2018Natur.557..706S. doi:10.1038/s41586-018-0093-3. PMID 29849156. S2CID 44108416.
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