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Ophiacodontidae

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Ophiacodontidae
Temporal range: Late Carboniferous to Early Permian 308–280 Ma
Mounted skeleton of Ophiacodon retroversus in the American Museum of Natural History
Scientific classification Edit this classification
Domain: Eukaryota
Kingdom: Animalia
Phylum: Chordata
Clade: Synapsida
Clade: Metopophora
Family: Ophiacodontidae
Nopcsa, 1923
Subgroups[1]

Ophiacodontidae is an extinct family of early synapsids from the Carboniferous and Permian. Archaeothyris, and Clepsydrops were among the earliest ophiacodontids, appearing in the Late Carboniferous. Ophiacodontids are among the most basal synapsids, an offshoot of the lineage which includes therapsids and their descendants, the mammals. The group became extinct by the Kungurian or the Roadian,[2] replaced by anomodonts, theriodonts, and the diapsid reptiles.

Characteristics

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Ophiacodon mirus restoration.

The lifestyle of ophiacodonts has long been controversial. Some studies suggested that they were semi-aquatic, and some even suggested a fairly aquatic lifestyle, but a recent study based on a quantitative inference model[3] suggested that both Clepsydrops and Ophiacodon were terrestrial.[4] Vertebral morphometric data also support, though ambiguously, a rather terrestrial lifestyle for Ophiacodon,[5] which could reach a length of 3.6 m (12 ft).[6] Archaeothyris may also have been terrestrial, but no detailed study of its habitat has been performed so far. The earliest ophiacodontids resembled varanids in body proportions, while others were larger with elongated skulls and massive shoulder girdles, probably to provide muscle attachment to support the weight of the large head.

Classification

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Traditionally, Archaeothyris, Ophiacodon, Varanosaurus and the briefly described Baldwinonus, Clepsydrops, Echinerpeton, Stereophallodon and Stereorhachis are included in the Ophiacodontidae. Protoclepsydrops was also regarded as ophiacodontid, however there is debate as to whether or not it was a synapsid. Echinerpeton and Sterophallodon were included for the first time in a phylogenetic analysis by Benson (2012).[7] Echinerpeton was found to be a wildcard taxon due to its small amount of known materials. It occupies three possible positions, falling either as the most basal synapsid, as the sister taxon of Caseasauria plus more derived taxa, or as an ophiacodontid more derived than Archaeothyris. Below is a cladogram modified from the analysis of Benson (2012),[7] after the exclusion of Echinerpeton:[7]

References

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  1. ^ Mann, A.; Paterson, R. S. (2020). "Cranial osteology and systematics of the enigmatic early 'sail-backed' synapsid Echinerpeton intermedium Reisz, 1972, and a review of the earliest 'pelycosaurs'". Journal of Systematic Palaeontology. 18 (6): 529–539. doi:10.1080/14772019.2019.1648323. S2CID 202847907.
  2. ^ Didier, Gilles; Laurin, Michel (9 December 2021). "Distributions of extinction times from fossil ages and tree topologies: the example of mid-Permian synapsid extinctions". PeerJ. 9: e12577. doi:10.7717/peerj.12577. ISSN 2167-8359. PMC 8667717. PMID 34966586.
  3. ^ Quémeneur, S.; de Buffrénil, V.; Laurin, M. (2013). "Microanatomy of the amniote femur and inference of lifestyle in limbed vertebrates". Biological Journal of the Linnean Society. 109 (3): 644–655. doi:10.1111/bij.12066.
  4. ^ Laurin, M.; de Buffrénil, V. (2015). "Microstructural features of the femur in early ophiacodontids: A reappraisal of ancestral habitat use and lifestyle of amniotes". Comptes Rendus Palevol. 15 (1–2): 115–127. doi:10.1016/j.crpv.2015.01.001.
  5. ^ Felice, R. N.; Angielczyk, K. D. (2014). "Was Ophiacodon (Synapsida, Eupelycosauria) a Swimmer? A Test Using Vertebral Dimensions". Early Evolutionary History of the Synapsida. Vertebrate Paleobiology and Paleoanthropology. p. 25. doi:10.1007/978-94-007-6841-3_3. ISBN 978-94-007-6840-6.
  6. ^ The Macmillan Illustrated Encyclopedia of Dinosaurs and Prehistoric Animals
  7. ^ a b c Benson, R.J. (2012). "Interrelationships of basal synapsids: cranial and postcranial morphological partitions suggest different topologies". Journal of Systematic Palaeontology. 10 (4): 601–624. Bibcode:2012JSPal..10..601B. doi:10.1080/14772019.2011.631042. S2CID 84706899.
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