Biology:Aleodon
| Aleodon | |
|---|---|
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Scientific classification 
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| Domain: | Eukaryota |
| Kingdom: | Animalia |
| Phylum: | Chordata |
| Clade: | Synapsida |
| Clade: | Therapsida |
| Clade: | Cynodontia |
| Family: | †Chiniquodontidae |
| Genus: | †Aleodon Crompton, 1955 |
| Type species | |
| Aleodon brachyrhamphus Crompton, 1955
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| Other species | |
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Aleodon is an extinct genus of cynodonts that lived from the Middle to the Late Triassic. Relatively few analyses have been conducted to identify the phylogenetic placement of Aleodon, however those that have place Aleodon as a sister taxon to Chiniquodon.[1] Two species of Aleodon are recognized: A. brachyramphus which was discovered in Tanzania, and A. cromptoni which was discovered most recently in Brazil.
The name for the genus Aleodon was created when Alfred W. "Fuzz" Crompton initially discovered the type species, Aleodon brachyramphus. The genus name, "Aleodon" referred to the grinding nature of the postcanine teeth, while "brachyramphus" referred to the relatively short snout of the specimen.[2] The most recently discovered species, A. cromptoni was named after Crompton.[1]
Discovery and Classification
In 1955, Aleodon was initially classified as a gomphodont cynodont based on the partial skull and lower jaw fossils found in 1933 in Tanzania. The classification was based on the presence of three types of post-canines that were identified in the fossil that were similar to another well-known gomphodont, Diademodon tetragonus.[2]
It was later argued in 2001 by Hopson and Kitching that Aleodon be classified under Chiniquodontidae based on less-worn dentition of unpublished specimens.[3] This classification was accepted by many sources.[1] However, a study done the following year by Abdala and Gianni found, based on fossils found in Namibia, that Aleodon (and Cromptodon) both had well developed lingual cingular platforms in their post-canines, a characteristic that Chiniquodontidae did not possess.[4]
While not many analysis have been done to clarify the phylogenetic relationship of Aleodon thus far, those that have been done describe Aleodon as the sister taxon of Chiniquodon.[5]
Description
Dentition
The dentition of Aleodon is the most significant morphological feature to distinguish it against other genera. Crompton pointed out three distinct regions of the postcanine row: anterior circular, transversely expanded ovate, and sectorial posterior teeth (described as “shearing” by Crompton). These three regions of post canines were very similar to a well-known gomphodont, Diademodon tetragonus (which led Crompton to believe that Aleodon was part of Gomphodonta). Crompton also noted that Aleodon uniquely possessed two incisors on the lower jaw which differs from most cynodonts which primitively had four.[2] Based on more fossils, Aleodon was also found to have a long secondary palate, a characteristic that was shared with members of the monophyletic group Chiniquodontidae and resulted in Aleodon's reidentification to Probainognathia from Gomphodonta.[3] Shortly after, specimens of Aleodon showed the possession of well-developed lingual cingular platforms on the post canines. This finding resulted in some researchers removing Aleodon from Chiniquodontidae due to the group not characterized in possessing well-developed lingual cingular platforms.[4] The lingual cingular platform that is expanded in both labiolingual and mesiodistal dimensions relative to the labial portion of the crown is also the most developed of all Triassic Probainognathians.[6] These observations led some researchers to believe that Aleodon (along with Candelariodon) may be specimens that exhibit the gradual development of the cingular platform.[7]
Skull
Based on specimens found in Brazil, Aleodon was found to share the same general cranial morphology of Chiniquodontidae. Diagnostic features of Chiniquodontidae are zygomatic arches flaring laterally, angulation between the ventral edge of the maxillary zygomatic process and the anteroventral margin of the jugal, elongated pterygoid flanges that end in a thin projection, and a long secondary palate.[4] When Aleodon was first characterized by Crompton, he noted the presence of a pineal foramen, however later specimens showed no evidence of a pineal foramen on the skull of Aleodon.[8] Aleodon is also characterized by its relatively short snout.[2]
Geological/Paleoenvironmental Information
Manda Formation (Tanzania)
Specimens of Aleodon were first recovered from the Triassic Manda Beds of Tanzania by Parrington in the 1930s.[2] The Manda Beds were first surveyed by Gordon M. Stockley from June to October 1930.[9] There was further collection by Parrington and Nowack in the 1930s in which Aleodon brachyramphus was later described by Crompton. The collections showed that the Manda Beds contained fauna thecodontians, cynodonts, and dicynodonts, as well as a large amphibian and a rhynchosaur. The formation was described as being 2000 meters thick with purple to brown mudstones with grey sandstones in between. From 60 to 150 meters below the top of the formation reptile bones were found while most (65%) of specimens were found 1180 meters and 1310 meters below the surface.[10]
Omingonde Formation (Namibia)
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Fossil vertebrates in the Omingonde Formation of Namibia were first found and published by Keyser in 1973. Among the fossils he described amphibians, cynodonts and dicynodonts. The cynodonts were initially represented by Cynognathus and herbivorous gomphodonts. After the discovery of Aleodon among other cynodont specimens such as Chiniquodon, Luangwa, and an unidentified traversodontid in 2009, the Omingonde Formation of Namibia is considered to possess the most diverse fauna of Middle Triassic cynodonts in the world. The discovery also provided researchers a definite link between two faunas in South America and East Africa.[8] From this, the Omingonde formation was also considered the key in “reconstructing the biogeography of Southern Gondwana during the Middle Triassic”.[8]
Rio Grande do Sul (Brazil)
Most recently a new species of Aleodon (A. cromptoni) was found in the Rio Grande do Sul in southern Brazil. The specimens were first collected in 1988 by Daniel and Abraão Cargnin.[1]
References
- ↑ 1.0 1.1 1.2 1.3 Martinelli, A.G.; Kammerer, C.F.; Melo, T.P.; Paes Neto, V.D.; Ribeiro, A.M.; Da-Rosa, Á.A.S.; Schultz, C.L.; Soares, M.B. (2017). "The African cynodont Aleodon (Cynodontia, Probainognathia) in the Triassic of southern Brazil and its biostratigraphic significance". PLOS ONE 12 (6): e0177948. doi:10.1371/journal.pone.0177948. PMID 28614355. Bibcode: 2017PLoSO..1277948M.
- ↑ 2.0 2.1 2.2 2.3 2.4 Crompton, Alfred (1955). "On some Triassic Cynodonts from Tanganyika". Proceedings of the Zoological Society of London 125 (3–4): 617–669. doi:10.1111/j.1096-3642.1955.tb00620.x.
- ↑ 3.0 3.1 Hopson, J. A.; Kitching, J. W. (2001). "A Probainognathian Cynodont from South Africa and the Phylogeny of Nonmammalian Cynodonts". Bulletin of the Museum of Comparative Zoology 156: 5–35.
- ↑ 4.0 4.1 4.2 Abdala, F.; Giannini, N. P. (2002). "Chiniquodontid Cynodonts: Systematic and Morphometric Considerations". Palaeontology 45 (6): 1151–1170. doi:10.1111/1475-4983.00280.
- ↑ Ruta, M.; Botha-Brink, J.; Mitchell, S. A.; Benton, M. J. (2013). "The Radiation of Cynodonts and the Ground Plan of Mammalian Morphological Diversity". Proceedings: Biological Sciences 280 (1769): 1–10. doi:10.1098/rspb.2013.1865. PMID 23986112.
- ↑ Martinelli, A. G.; Soares, M. B.; Oliveira, T. V.; Rodrigues, P. G.; Schultz, C. L. (2017). "The Triassic Eucynodont Candelariodon barberenai Revisited and the Early Diversity of Stem Prozostrodontians". Acta Palaeontologica Polonica 62: 527–542. doi:10.4202/app.00344.2017.
- ↑ Oliveira, T. V.; Schultz, C. L.; Soares, M. B.; Rodrigues, C. N. (2011). "A New Carnivorous Cynodont (Synaspida, Therapsida) from the Brazilian Middle Triassic (Santa Maria Formation): Candelariodon barberenai gen. et sp. nov". Zootaxa 3027: 19–28. doi:10.11646/zootaxa.3027.1.3.
- ↑ 8.0 8.1 8.2 Abdala, F.; Smith, R. M. H. (2009). "A Middle Triassic Cynodont Fauna from Namibia and its Implications for the BioGeography of Gondwana". Journal of Vertebrate Paleontology 29 (3): 837–851. doi:10.1671/039.029.0303.
- ↑ Stockley, G. M. (1932). "The Geology of the Ruhuhu Coalfields Tanganyika Territory". The Quarterly Journal of the Geological Society of London 88 (1–4): 610–622. doi:10.1144/gsl.jgs.1932.088.01-04.20.
- ↑ Cox, C. B. (1991). "The Pangea Dicynodont Rechnisaurus and the Comparative Biostratigraphy of Triassic Dicynodont Faunas". Palaeontology 34: 767–784.
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