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Cynognathus

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(Redirected from Cynognathus crateronotus)

Cynognathus
Temporal range: Middle Triassic, 247–237 Ma
Fossil skull of Cynognathus
Scientific classification Edit this classification
Domain: Eukaryota
Kingdom: Animalia
Phylum: Chordata
Clade: Synapsida
Clade: Therapsida
Clade: Cynodontia
Clade: Cynognathia
Family: Cynognathidae
Seeley, 1895
Genus: Cynognathus
Seeley, 1895
Type species
Cynognathus crateronotus
Seeley, 1895

Cynognathus is an extinct genus of large-bodied cynodontian therapsids that lived in the Middle Triassic. It is known from a single species, Cynognathus crateronotus. Cynognathus was a predator closely related to mammals and had a southern hemispheric distribution. Fossils have so far been recovered from South Africa, Argentina, Antarctica, and Namibia.

Description

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Life reconstruction of Cynognathus crateronotus

Cynognathus was a heavily built animal, and measured around 1.2 metres (3 ft 11 in)[1] in snout-to-vent body length and up to 2 metres (6 ft 7 in) in total length.[2] It had a particularly large head, up to 40 centimetres (1 ft) in length, with wide jaws and sharp teeth. Its hindlimbs were placed directly beneath the body. There has been controversy about whether the forelimbs were also held upright or sprawled outwards in a reptilian fashion, but recent studies suggest cynodonts typically held their front legs in a posture between these two extremes.[3] A study of living mammals concluded that "upright posture" in mammals is a myth based on the posture of mammal species specialized for fast running, such as dogs, hares, and antelopes; modern mammals that are not specialized for running often hold their forelimbs in a semi-sprawled posture.[4]

Possible autapomorphies of C. crateronotus include an extremely elongated postorbital bar and sectorial postcanine teeth with two serrated cusps distal to a recurved apex.[5]

Discovery and naming

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Skull

During 1888 and 1889, the British paleontologist Harry Govier Seeley visited southern Africa. In 1889, near Lady Frere, at a location where earlier Alfred Brown had discovered a tooth, Seeley excavated a skull and partial postcranial skeleton of a cynodontian. In 1894, Seeley named the genus Cynognathus with as type species Cynognathus crateronotus. Simultaneously, he named three other species in the genus: Cynognathus berryi, honouring James Berry who had assisted in the excavations, Cynognathus platyceps, the "flat jaw", and Cynognathus leptorhinus, the "slender nose".[6] The generic name Cynognathus is derived from Greek kyon and gnathos, meaning "dog jaw". In 1895, Seeley published a more comprehensive description of these finds.[7]

Fossil material probably belonging to the genus has been given several different names over the years. Generic synonyms include Cynidiognathus, Cynogomphius, Karoomys, Lycaenognathus, Lycochampsa and Lycognathus. Opinions vary as to whether all remains belong to the same species. The genus Karoomys is known only from a tiny juvenile. Species-level synonyms of Cynognathus crateronotus include Cynidiognathus broomi, Cynidiognathus longiceps, Cynidiognathus merenskyi, Cynognathus berryi, Cynognathus minor, Cynognathus platyceps, Cynogomphius berryi, Karoomys browni, Lycaenognathus platyceps, Lycochampsa ferox, Lycognathus ferox, and Nythosaurus browni.

Distribution

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Distribution of four Permian and Triassic fossil groups used as biogeographic evidence for continental drift, and land bridging. Location of Cynognathus remains shown by red diamonds

Fossils have been found in the Karoo, the Puesto Viejo Formation, Fremouw Formation, in South Africa/Lesotho, Argentina and Antarctica.

Cynognathus lived between the Anisian and the Ladinian (Middle Triassic).[8]

This genus forms a Cynognathus Assemblage Zone in the Beaufort Group of the Karoo Supergroup.[9][10][11]

Classification

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Seeley in 1894/1895 placed Cynognathus in a separate family Cynognathidae, within the Cynodontia. Cynognathus is presently the only recognized member of the family Cynognathidae. Later a clade Cynognathia was named after the genus, within the Eucynodontia.

Cynognathus crateronotus in a cladogram after Stefanello et al. (2023):[12]

Cynognathia

Paleobiology

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In the Karoo Basin in what is now South Africa, Cynognathus lived in open environments with warm, dry summers and cool, wet winters, similar to today's Western Cape region but more arid. Individuals grew rapidly and continuously. Their hunting habits were largely unaffected by the changing seasons.[13] The dentary was equipped with differentiated teeth, with fangs in the front for seizing prey and wider teeth in the rear of the jaw suitable for cutting meat;[14] these show this animal could effectively process its food before swallowing. The presence of a secondary palate in the mouth indicates that Cynognathus would have been able to breathe and swallow simultaneously. All these adaptations are consistent with maintaining a regular, high basal metabolic rate ("warm-blooded"), as in modern mammals.

The possible lack of belly ribs, in the stomach region, suggests the presence of an efficient diaphragm, an important muscle that allows mammals to breathe equally well when they are walking, running, or holding still. Pits and canals on the bone of the snout indicate concentrations of nerves and blood vessels. In mammals, these structures support special sensory hairs (whiskers), so it is likely Cynognathus had whiskers as well.

See also

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References

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  1. ^ Jones & Bartlett Learning, Strickberger's Evolution, 2008
  2. ^ Botha, Jennifer; Lee-Thorp, Julia; Chinsamy, Anusuya (2005-08-01). "The palaeoecology of the non-mammalian cynodonts Diademodon and Cynognathus from the Karoo Basin of South Africa, using stable light isotope analysis". Palaeogeography, Palaeoclimatology, Palaeoecology. 223 (3): 303–316. Bibcode:2005PPP...223..303B. doi:10.1016/j.palaeo.2005.04.016. ISSN 0031-0182.
  3. ^ Lai, Phil H.; Biewener, Andrew A.; Pierce, Stephanie E. (2017-07-21), Three-dimensional mobility and muscle attachments in the pectoral limb of the Triassic cynodont Massetognathus pascuali, doi:10.1101/166587, retrieved 2024-09-27
  4. ^ Jenkins, Farish A. (20 August 2009). "Limb posture and locomotion in the Virginia opossum (Didelphis marsupialis) and in other non-cursorial mammals". Journal of Zoology. 165 (3): 303–315. doi:10.1111/j.1469-7998.1971.tb02189.x.
  5. ^ Wynd, B.M.; Peecock, B.R.; Whitney, M.R. & Sidor, C.A. 2018. "The first occurrence of Cynognathus crateronotus (Cynodontia: Cynognathia) in Tanzania and Zambia, with implications for the age and biostratigraphic correlation of Triassic strata in southern Pangea". pp. 228–239 in: C.A. Sidor and S.J. Nesbitt (eds.), Vertebrate and Climatic Evolution in the Triassic Rift Basins of Tanzania and Zambia. Society of Vertebrate Paleontology Memoir 17. Journal of Vertebrate Paleontology 37(6, Supplement)
  6. ^ H.G. Seeley. 1894. "Researches on the Structure, Organization, and Classification of the Fossil Reptilia. Part IX, Section 5. Abstract. On New Cynodontia". Philosophical Transactions of the Royal Society of London B 56: 291-294
  7. ^ H.G. Seeley. 1895. "Researches on the Structure, Organization, and Classification of the Fossil Reptilia. Part IX, Section 5. On the Skeleton in New Cynodontia from the Karroo Rocks". Philosophical Transactions of the Royal Society of London B 186: 59-148
  8. ^ Trewick, Steve (2016). "Plate Tectonics in Biogeography". International Encyclopedia of Geography: People, the Earth, Environment and Technology. John Wiley & Sons, Ltd. pp. 1–9. doi:10.1002/9781118786352.wbieg0638. ISBN 9781118786352.
  9. ^ A threefold subdivision of the Cynognathus Assemblage Zone (Beaufort Group, South-Africa) and its paleogeographic implications. PJ Hancox, MA Shishkin, BS Rubidge, JW Kitching, South African Journal of Science, 1995
  10. ^ Vertebrate burrow complexes from the Early Triassic Cynognathus Zone (Driekoppen Formation, Beaufort Group) of the Karoo Basin, South AfricaGH Groenewald, J Welman, JA MacEachern - Palaios, 2001
  11. ^ Stratigraphic and sedimentological investigation of the contact between the Lystrosaurus and the Cynognathus assemblage zones (Beaufort group: Karoo supergroup). J Neveling - Bulletin of the Council for Geoscience, 2004
  12. ^ Stefanello, M.; Martinelli, A. G.; Müller, R. T.; Dias-da-Silva, S.; Kerber, L. (2023). "A complete skull of a stem mammal from the Late Triassic of Brazil illuminates the early evolution of prozostrodontian cynodonts". Journal of Mammalian Evolution. 30 (2): 299–317. doi:10.1007/s10914-022-09648-y.
  13. ^ Botha, Jennifer; Lee-Thorp, Julia; Chinsamy, Anusuya (2005-08-01). "The palaeoecology of the non-mammalian cynodonts Diademodon and Cynognathus from the Karoo Basin of South Africa, using stable light isotope analysis". Palaeogeography, Palaeoclimatology, Palaeoecology. 223 (3): 303–316. doi:10.1016/j.palaeo.2005.04.016. ISSN 0031-0182.
  14. ^ "XVI. Researches on the structure, organisation, and classification of the fossil reptilia. Part IX. Section 5. On new Cynodontia". Proceedings of the Royal Society of London. 56 (336–339): 291–294. 1894-12-31. doi:10.1098/rspl.1894.0115. ISSN 0370-1662.

Further reading

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  • Seeley (1895), "Researches on the structure, organization, and classification of the fossil Reptilia. Part IX., Section 5. On the skeleton in new Cynodontia from the Karroo rocks". Phil. Transactions of the Roy. Soc. of London, series B 186, p. 59–148.