| Aelurosaurus | |
|---|---|
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| Holotype skull of A. felinus | |
Scientific classification
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| Domain: | Eukaryota |
| Kingdom: | Animalia |
| Phylum: | Chordata |
| Clade: | Synapsida |
| Clade: | Therapsida |
| Clade: | † Gorgonopsia |
| Genus: | †
Aelurosaurus Owen, 1881 |
| Species | |
| Synonyms | |
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Aelurosaurus ("cat lizard", from Ancient Greek αἴλουρος "cat" and σαῦρος "lizard") is a small, carnivorous, extinct genus of gorgonopsian therapsids from the Late Permian of South Africa. It was discovered in the Karoo Basin of South Africa, and first named by Richard Owen in 1881. It was named so because it appeared to be an ancestor for cat-like marsupials, but not yet a mammal itself.[ citation needed] It contains five species, A. felinus, A. whaitsi, A. polyodon, A. wilmanae, and A.? watermeyeri. [1] A. felinus, the type species, is generally well described with established features, while the other four species are not due to their poorly preserved holotypes.
Discovery
Aelurosaurus was discovered in 1881 in the Karoo Basin of South Africa. The skull holotype was missing the postorbital region, so Owen was left to describe the anterior portion. After examining the sutures and teeth, he assumed the first specimen to be from an older, adult Aelurosaurus, seeing that they were no longer in perfect condition. [1]
Species
A. felinus
Originally described by Owen, the orbit is a 2.5 centimeters by 2 centimeters ellipse, and the nostril 1.3 centimeters wide and 0.9 centimeters long. The upper jaw has a maximum width of roughly 3.5 centimeters just below the orbits. At a little more than 7.5 centimeters long and 2 centimeters wide, the mandible spans almost the entirety of the skull. This particular specimen was preserved with the mouth closed, with the upper teeth fully covering the mandibular teeth. On the upper jaw, there are five incisors, a gap of 0.8 centimeters, a canine (1.2 centimeters exposed, roughly 3.6 centimeters in total length), another 0.8 centimeter gap, and then five molars. After Owen removed the alveolar wall of the upper maxillary canine, he exposed the mandibular canine, which he found to be the same size as the maxillary. [1] The semicircular canal found on A. felinus and all other gorgonopsians suggests that their heads were ventrally tilted, a characteristic of predators. [2]
While Owen had originally assumed the holotype to be the skull of an adult, it has been argued that it was actually the skull of a juvenile. Owen only attributed its old age to the state of its sutures and teeth, while others noticed features indicating a young age, including its "...short snout, large orbits, slender postcanine teeth, tooth replacement, numerous small postcanine teeth, well developed foramina, large supraorbital portion of the frontal, anteriorly situated preparietal, slender skull arches, narrow vomer, well developed palatal tuberosities, teeth on transverse apophyses, large ectopterygoids, slender mandible, [and] open symphysis". [3]
A. whaitsi
First described by Robert Broom in 1911. The holotype of A. whaitsi is another skull, but mostly snout, with the main indicator being a flatter symphysis. Its classification went back and forth throughout the entire century since it has very few defining features, all of which could be juvenile features of other genera. [3]
A. polyodon
First described by Broom in 1935. The holotype of A. polyodon is a crushed snout. Originally named Galerhinus polyodon, it was renamed Aelurosaurus polyodon in 1970. [3]
A. wilmanae
First described by Broom in 1940. The holotype is a skull that is the best preserved of all the Aelurosaurus species. The defining feature is a larger snout compared to A. felinus, but overall the skull is still small at just 11 centimeters long. [3]
A.? watermeyeri
First described by Broom in 1940. The holotype is a skull, and was originally named Scylacocephalus watermeyeri. The genus is still under debate, since it shares features with both Aelurosaurus (such as a large orbit and short snout) and Aloposaurus (such as larger preparietal and postfrontal). [3]
Geology/Paleoenvironment
Aelurosaurus felinus was originally obtained in the Gough, of the Karoo Basin of South Africa, which includes the Tapinocephalus and Pristerognathus Assemblage Zones. [4] [5] These assemblage zones are a part of the Beaufort Group and span from the Middle Perimian to the Late Permian. [6] The stratigraphic composition of the Beaufort Group include siltstone, mudstone, and sandstone beds, with evidence of rivers flowing across the land in semi-arid conditions. Findings of dense coprolites consisting of bones suggest that predators lived near these rivers. [7]
While most gorgonopsians have been recovered from the Karoo Basin in South Africa, there have been recent discoveries of gorgonopsians in Russia's Vyazniki Assemblage as well. [8]
References
- ^ a b c Owen, R. 1881. On the order Theriodontia with a description of a new genus and species (Aelurognathus fel. Ow.). Quat. Jour. Geol. Soc. London. (Vol. 37): 261–265.
- ^ Araújo, R., V. Fernandez, M. J. Polcyn, J. Fröbisch, R. M. S. Martins. 2017. Aspects of gorgonopsian paleobiology and evolution: insights from the basicranium, occiput, osseous labyrinth, vasculature, and neuroanatomy. PeerJ. (Vol. 5): 1–45.
- ^ a b c d e Gebauer, E.V.I. (2007). Phylogeny and evolution of the Gorgonopsia with a special reference to the skull and skeleton of GPIT/RE/7113 ("Aelurognathus"? parringtoni) (PDF) (Thesis). Dissertation Universität Tübingen.
- ^ Boonstra, L.D. 1935. On the South African Gorgonopsian reptiles preserved in the American Museum of Natural History. American Museum Novitates. 772: 1–14.
- ^ Kammerer, C.F., R.M.H. Smith, M. O. Day, B.S. Rubidge. 2015. New information on the morphology and stratigraphic range of the mid-Permian gorgonopsian Eriphostoma microdon. Papers in Palaeontology. (Vol. 1) 2: 201–221.
- ^ Angielczyk, K. D., B. S. Rubidge, M. O. Day, F. Lin. 2016. A reevaluation of Brachyprosopus broomi and Chelydontops altidentalis, dicynodonts (Therapsida, Anomodontia) from the middle Permian Tapinocephalus Assemblage Zone of the Karoo Basin, South Africa. Journal of Vertebrate Paleontology, (Vol. 36) 2. DOI: 10.1080/02724634.2016.1078342
- ^ Smith, R. M. H., J. Botha-Brink. 2011. Morphology and composition of bone-bearing coprolites from the Late Permian Beaufort Group, Karoo Basin, South Africa. Palaeogeography, Palaeoclimatology, Palaeoecology (Vol. 312): 40–53.
- ^ Kammerer, C.F. 2016. On the evolutionary history of the Gorgonospia, with new information on their global first and last appearances. International Geological Congress. (Vol. 36): https://www.americangeosciences.org/sites/default/files/igc/4456.pdf
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